MEMOIRES
DU MUSEUM
NATIONAL
D’HISTOIRE
NATURELLE
TOME 162
ZOOLOGIE
1994
Actes de la feme Conference inter nationale
des Polychetes
Coordonne par
]ean-CJaude DAUVIN
Lucien LAUBIER
Donald RE1SH
4 TH INTERNATIONAL
P 0 t T C H A E T E
CONFERENCE
FRANC E
i 9 9 2
Source : MNHN, Paris
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MU&UM
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Actes de la 4 erne Conference internationale des Polychetes
4 TH INTERNATIONAL
POLYCHAETE
CONFERENCE
ANGER S
FRANC E
i 9 9 2
Source : MNHN. Paris
ISBN : 2-8565 3-214-4
ISSN : 1243-4442
© Editions du Museum national d’Histoire naturelle, Paris, 1994
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MEMOIRES DU MUSEUM NATIONAL D'HISTOIRE NATURELLE
TOME 162
ZOOLOGIE
Actes de la 4eme Conference Internationale
des Polychetes
Jean-Claude DAUVIN* Lucien LAUBER** Donald J. REISH***
* MustSum national d'Histoire naturelle
Laboratoire de Biologie des InvertSbres marins et Malacologie
57, rue Cuvier
F-75005 Paris
** Institut Oceanographique
Laboratoire de Physiologie des Etres marins
195, rue Saint-Jacques
F-75005 Paris
*** California State University
Department of Biology
Long Beach. CA 90804
USA
EDITIONS
DU MUSEUM
PARIS
1994
Source : MNHN. Paris
Source ; MNHN, Paris
CONTENTS
SOMMAIRE
Preface . 9
Acknowledgements . 10
List of participants . 11
List of reviewers . 15
Obituaries . 17
Pierre Fauvel . 17
Ralph 1. Smith . 19
Pavel V. Ushakov . 19
Douglas P. Wilson . 22
Contributed papers . 25
Cytophysiology, development and reproduction . 29
Genetics and morphology . 81
Phylogeny and taxonomy . 145
Ecology and biogeography . 323
Culture and valorisation . 593
Abstracts . 611
Source
Source : MNHN. Paris
PREFACE
Some eight years ago, Professor Kirkec.aard, former Chairman of the International Polychaete Association
and organizer of the Second International Polychaete Conference, suggested dial France, as a European southern
country, should host the Fourth Conference. We fully agreed on this idea, and decided to prepare a proposal which
was submitted to the Association during the Third International Polychaete Conference held in Long Beach,
August 1989. At tiiis time, one of our main difficulties was the choice of die site for this Conference. For several
reasons, most of die french organizers considered the town of Angers as the most appropriate place: the souvenir of
Pierre Fauvel and of his successor Francois Rullier, die availability of convenient facilities, the assistance of
Patrick GlLLET's laboratory in the Institute for Pure and Applied Research of die University Cadioliquc dc l’Ouest,
the opportunity for attendees to discover and copy rare articles and books from Fauvel's library, die touristic
interest of die surroundings of die town of Angers...
During the Long Beach Conference, the French proposal was presented togedier with two odiers proposals, mid
finally adopted by the Association. In accordance with the discussions in Long Beach, we decided to move the
period of the Conference to die end of July instead of the beginning of September; we also considered the
possibility to organize some sampling visits in French classical marine stations and kept in mind the idea of
widening the scope of the Conference to physiology and endocrinology of Polychaetes. More generally, we
followed one suggestion by David George: such an international Conference should not be restricted to ecology
and taxonomy, but should also consider die group as a biological model, and include applied research such as
zootcchny for polychaete farming or search for active molecules such as nereidin or thelepin. The program of die
Proceedings clearly demonstrates dial diis objective has been achieved.
Following die decision of die International Polychaete Association, an Organization Committee was soon
established in France:
President of the Organizadon Committee: Lucien LAUBIER, Bruxelles
Convener: Patrick GlLLET, Angers
G6rard Bellan, Marseille
Michel Biiaud, Banyuls-sur-Mer
Jean-Claude Dauvin, Paris
Daniel DESBRUYkRES, Brest
Andry DHAINAUT, Lille
Nicole DHAINAUT-COURTOIS, Lille
Yves GRUET, Nantes
Christian RETif-RE, Dinard
Jean Vovelle, Paris
Local organization Committee, University Cadiolique de fOuest, Angers:
Elisabeth AILLERIE, Georges LE GUILLANTON, and Anne-Laure Morvan.
The first announcement was sent at die end of December, 1990. In May 1991, we had received 164 posidve
answers, 80 communications titles and 25 posters. A few weeks later, the same figures were respectively 190, 130
and 60.
The Fourth International Polychaete Conference was held July 27-August 1. 1992, at die Centre de Congas,
Angers, France. A total of 200 members from 32 countries attended the Conference. Sessions were conducted over
Source :
10
PREFACE
a six days period wiih two mid-excursions: to the Loire Valley and to Bourgneuf Bay. Several attendees traveled to
the Laboratoire maritime de Dinard following die Conference.
There were 71 oral presentations and 101 posters. Session topics and posters represented the different themes:
cytophysioiogy, taxonomy and phylogeny, biogeography and ecology, reproduction and development. A special
session was organized on polychaete culture and valorisation. Seventy-nine papers were submitted for publication
and analysed by two different reviewers, and by Donald J. Reish. A total of fourteen papers have been rejected by
die reviewers, but abstracts of .ill communications and posters are included in die Proceedings of die Conference.
Lucien Laubier and Patrick GlLLET
ACKNOWLEDGEMENTS
We gratefully acknowledge the financial support and practical assistance to the Conference provided by the
different ministries and various bodies and scientific institutions:
- Ministfcre des Affaires Etrang£res
- Conseil Regional des Pays de la Loire
- Conseil G6n6ral du Maine et Loire
- Vide d' Angers
- Institut Franyais de Recherche pour I'Exploitation de la Mer (IFREMER)
- Universitd Catholique de l'Ouest (UCO)
- Institut de Recherche Fondamentale et Appliqu6e de 1'UCO
- Museum National d'Histoire Naturclle de Paris,
- Museum d'Histoire Naturellc de Nantes.
Special thanks for their help to Yves Gruet and Christian RETltRE who organized excursions, and to
Elisabeth Aillerie for the programme. Thanks arc also extended to Marie-Annick GRUET, Marie-H616ne GlLLET
and Elisabeth AILLERIE for their kind assistance during the Conference.
Many thanks to the Minitextiles Art group for the exhibition on polychaetes.
A special mention must be addressed to the Laboratoire de Biologie des Invert£br6s Marins et Malacologie du
Museum national d'Histoire naturelle, which provided logistic support during the tedious work of preparation of
die present volume.
Source :
LIST OF PARTICIPANTS
ARGENTINA
Amor Analia (La Plata)
BREMEC Claudia (La Plata)
AUSTRALIA
Hutchings Patricia (Sydney)
BELGIUM
Eeckhaut Igor (Mons)
BRAZIL
Lana Paulo Da Cunha (Parana)
NONATO Edmundo Ferraz (Sao Paulo)
Salvador Bei.untani Lara (Sao Paulo)
Santos Maria Auxiadora (Sergipe)
CANADA
Byers Sheila (Toronto)
Caron Alain (Dinard)
Chi a Fu-shiang (Alberta)
DESROSIERS Gaston (Rimouski)
Fournier Judith A. (Ottawa)
Juniper Kim (Montrdal)
Marsden Joan (Montreal)
Masson Stdphane (Quebec)
Miller Retzer Connie (Vancouver)
Miron Gilles (Quebec)
Olivier Marc (Rimouski)
POCKLINGTON Patricia (Halifax)
Qian Pei-Yuan (Vancouver)
White Caroline (Rimouski)
COLOMBIA
LAVERDE-Castillo Juan Jose Antonio (Bogota)
CROATIA
ZAHTILA Elvis (Rovinj)
DENMARK
Hibye-Jacobsen Danny (Copenhagen)
Feldsgaard Pedersen Torben (Aarhus C.)
Hyllberg Jorgen (Aarhus C.)
Kirkegaard Jorgen Bagger (Copenhagen)
Petersen Mary E. (Copenhagen)
CHILE
Carrasco Franklin D. (Concepcion)
CHINA
Wu Baoling (Qing Dao)
FRANCE
BACHELET Guy (Arcachon)
Baudet Joseph (Nantes)
BELLAN Gerard (Marseille)
Bellan-SaNTINI Denise (Marseille)
Bhaud Michel (Banyuls-sur-Mer)
Cha Jae Hoon (Banyuls-sur-Mer)
Dauvin Jean-Claude (Paris)
DESBRUYfeRES Daniel (Brest)
DHAINAUT Andre (Villeneuve d'Ascq)
DHAINAUT-COURTOIS Nicole (Villeneuve d’Ascq)
DuCHfiNE Jean-Claude (B;uiyuls-sur-Mer)
CiENTIL Franck (Roscoff)
Gillet Patrick (Angers)
Gruet Yves (Nantes)
INTES Andre (Brest)
JOUIN-TOULMOND Claude (Paris)
Lambert R6my (Dinard)
Laubier Lucien (Paris)
LECHAPT Jean -Paul (Dinard)
Marcano Guillermo (Arcachon)
Nozais Christian (Banyuls-sur-Mer)
Parreira dos Santos Paulo Jorge (Arcachon)
Pereira de Souza Santos Lilia (Arcachon)
RETlERE Christian (Dinard)
Salen-Picard Chantal (Marseille)
TlllfiBAUT Eric (Roscoff)
Vovellf. Jean (Paris)
GERMANY
Borowski Christian (Hamburg)
DORRESTEIJN Adriaan (Mainz)
12
LIST OF PARTICIPANTS
Fiege Dieter (Frankfurt)
Fischer Albrecht (Mainz)
OOERKE Helmut (Bremerhaven)
Hardege Jorg Detelf (Oldenburg)
Hofmann Dieter K. (Bochum)
Hus EM ANN Fginhard (Bochum)
Richer Frank (Osnabruck)
Plate Susanne (Bochum)
Purschke Gunter (Osnabruck)
Rosenfeldt Pongchai (Hamburg)
Schmidt Hartmut (Osnabruck)
Westheide Wilfried (Osnabruck)
WlNDOFFER Reinhard (Osnabruck)
WRZESINSKI Olgierd (Hamburg)
GREECE
Arvanitidis Christos (Thessaloniki)
Eleftheriou Anastasios (Iraklio)
Papadopoulou K. Nadia (Iraklio)
SlMBOURA Nomiki (Athfcnes)
INDIA
Ayyakkannu K. (Parangipettai)
INDONESIA
ANDI Isdradjat S. (Aarhus C.)
A Rio Raden (Aarhus C.)
BONEKA Farms B. (Aarhus C.)
Erlambang Tanza (Aarhus C.)
Kaligis G. Fontje (Aarhus C.)
Latama Gunarto (Aarhus C.)
Litaay Magdalena (Aarhus C.)
Ompi Medy (Aarhus C.)
Princ.GENIES Delianis (Aarhus C.)
SlREGAR Yusni I. (Aarhus C.)
Soekendarsi Eddy (Aarhus C.)
TANJUNG Afrizal (Aarhus C.)
YULIANDA Fredinan (Aarhus C.)
IRELAND
Allen Hazel
Grehan Anthony J. (Banyuls-sur-Mer)
ISRAEL
Ben-Eliahu Nechama (Jerusalem)
ITALY
Abbiati Marco (Pisa)
Cantone Grazia (Catania)
C'astelli Alberto (Modena)
Gambi M. Cristina (Napoli)
Giangrande Adriana (Lecce)
Gravina M. Flavia (Roma)
Lardicci Claudio (Pisa)
Petrapoli Angela (Lecce)
Prevedelli Daniela (Modena)
Sanfilippo Rossana (Catania)
Sella Gabriella (Torino)
Somashini Alessandra (Roma)
Sordino Paolo (Napoli)
JAPAN
Sato-Okoshi Waka (Sendai)
MEXIQUE
Diaz Victoria (San Diego)
Leon Gonzalez Jesus Angel de (N. Leon)
Molina-Fuentes Enrique (San Nicolas
de los Garza)
Salazar-Vallejo Sergio I. (Chetumal)
SOLIS-WEISS Vivianne (Mexico)
NETHERLANDS
Hove Harry Ten (Amsterdam)
NORWAY
I Iolte Boerge (Tromsoe)
Jorgensen Lis Lindal (Bergen)
Ouc. Eivind (Grimstad)
POLAND
Sicinski Jacek (Todz)
PORTUGAL
Marques Joao Carlos (Coimbra)
Moreira Maria Helena (Aveiro)
PARDAL Miguel Angelo (Coimbra)
Silva Paula Cristina (Aveiro)
RUSSIA
Britayev Temir (Moscow)
Jirkov Igor A. (Moscow)
TZETLIN Alexander (Moscow)
SPAIN
ALOS Calvo Maria Carmen (Barcelone)
LIST OF PARTICIPANTS
13
Brito Maria Carmen (La Laguna)
Capaccioni-AZZati Romana Y. (Valencia)
CARDEL.L Maria Jos6 (Barcclone)
DUESO Ana (Blancs)
Garcia- Arberas Loreto (Bilbao)
Garcia-Martin Salvador F. (Puerto Real)
JUNOY Juan (Madrid)
Lastra Mariano (Santiago)
Lopez Garcia Eduardo (Madrid)
Mendez Muria (Barcelone)
Nunez Jorge (Islas Canarias)
Pinedo Susana (Blanes)
Rallo Ana (Bilbao)
Sarda Rafael (Blanes)
Sanchez Mata Adoracion (Santiago)
San Martin Guillermo (Madrid)
'Lena Medialdea Jose (Valencia)
Torres Gavila Franco Javier (Buijasso)
Vieitez Jose Manuel (Alcala de I Ienares)
Villora-Moreno Santiago (Valencia)
SWEDEN
Akesson Beitil (Goteborg)
Hide Ragnar (Goteborg)
Pleijel Fredrik (Stockholm)
Sigvaldadoti'IR Elin (Stockholm)
TAIWAN
Chen Chang-Po (Taiwan)
Ms I EH Hwey-Lian (Taipei)
THAILAND
Chantrapornsyl Supot (Aarhus)
Nateewathana Anuwat (Phuket)
TRINIDAD
GOBIN Judith (Plymouth)
UNITED KINGDOM
Bamber Roger (Southampton)
Batten Sonia (Southampton)
Bentley Matt (St Andrews)
Chambers Susan (Edinburg)
Coates Amanda (Scotland)
Cunningham Elaine (Tyne and Wear)
Dixon David R. (Plymouth)
Emson Roland H. (London)
George David (London)
Gibbs Peter E. (Plymouth)
Harris Tegwyn (Exeter)
Kendall Michael (Plymouth)
Knic.ht-Jones Phyllis (Swansea)
Knight-Jones Wyn (Swansea)
Mackie Andrew (Wales)
Muir Alexander lan (London)
Olive Peter James William (Tyne)
Paterson Gordon L. J. (London)
Rowe Grant (Southampton)
THORP Clifford H. (Hampshire)
TURNER Geoffrey Simon ( Tyne and Wear)
Warren Lynda (Cardiff)
Woodham Annette (Edinburgh)
UNITED STATES OF AMERICA
Blake James A. (Woods Hole)
DAUER Daniel (Norfolk)
Fauchald Kristian (Washington)
FlTZHUGH Kirk (Los Angeles)
Hilbig Brigitte (Massachusetts)
Jones Howard (Corvallis)
KiRTLEY David W. (Stuart)
Kudenov Jerry D. (Alaska)
Long Charlene D.
Lovell Lawrence L. (California)
Mac Hugh Damhnait (Santa Cruz)
Martin Ann (Redondo Beach)
Mountford Nancy K. (Lusby)
REISH Donald J. (Long Beach)
Rouse Greg (Washington)
Ruff R. Eugene (Needham)
SCHROEDER Paul C. (Pullmann)
Simon Joseph L. (Tampa)
Smith Ralph I. (Berkeley)
Ward Linda (Washington)
Source : MNHN. Paris
Source : MNHN, Paris
LIST OF REVIEWERS
16
LIST OF REVIEWERS
Olive Peter James William (Tyne)
Paterson Gordon L.J. (London)
Warren Lynda (Cardiff)
UNITED STATES OF AMERICA
Blake James A. (Woods Hole)
Butman Cheryl Ann (Woods Hole)
Fauchald Kristian (Washington)
Fitzhugh Kirk (Los Angeles)
Grass le Frederick (New Brunswick)
Grassle Judith (New Brunswick)
Hilbig Brigitte (Massachusetts)
KUDENOV Jerry D. (Alaska)
Levin Lisa A. (La Jolla)
Maurer Don (Long Beach)
Perkins Thomas H. (St Petersburg)
Pettibone Marian H. (Washington)
REISH Donald J. (Long Beach)
Rouse Greg (Washington)
Schroeder Paul C. (Pullmann)
Simon Joseph L. (Tampa)
Obituaries
Pierre FAUVEL (1866-1958),
his life and research on polychaetous annelids
Patrick GILLET
Laboratoire d'Ecoiogie Animale
Institut de Recherche Fondaincntalc et Appliquee
Univcrsite Catholique de l'Ouest
3. place Andre Leroy, B.P. 808
49008 Angers ccdex 01, France
Pierre Louis Andrd FAUVEL (Fig. 1) est nd h Cherbourg le 8 octobre 1866 de Cldmencc Maihilde Cappe
(1851-1909) et de Auguste Alexandre Fauvel (1821-1867), lieutenant dans la marine frangaise. Pierre Fauvel a
suivi ses 6tudes h l'Universit6 de Caen et fut assistant h la station de recherche de Luc-sur-Mer. Le 29 juin 1897, il
obtint son doctoral h TUniversitd de Paris pour son travail sur les Amphar6tiens. II fut alors nomm6 professeur de
zoologie h I'Universitd Catliolique de l'Ouest, puis Doyen de la Faculty des Sciences en 1942.
II 6tudia les polychfctes de diff6rentes regions du monde et de nombreuses expdditions occanographiqucs telles
que celles de 1'IIirondelle, de la Princesse Alice, du Pourquoi Pas ? et de la Calypso. II d6couvrit de nombreuses
espyces nouvelles dont la plus c616bre est Mercierella enigmatica dScouverte dans le canal de Caen par
M. Mercier. Pierre Fauvel avail remarqud les analogies avec Ficopomatus macrodon et ce n'est que ryccmmcnt
que l'espfece fut rebaptis6e Ficopomatus enigmaticus par TEN Hove & WERDENBURG (1978).
II a public environ 170 articles sur les ann61ides polych^tes et r£dige de nombreuses faunes coniine la Faune de
France el la Faune de I'lnde. Ses travaux les plus importants ont porti5 sur l'anatomie compare des Ar<5nicole$, sur
les otocystes, I'gthologie des Pectinaires et une monographic sur les Amphar6tiens. II obtint de nombreux prix et
distinctions dont le Prix Savigny (1915) de FAcademie des Sciences, le Prix Saintour (1926) de I' Academic des
Sciences, et le Prix Gadeau de Kervillc (1930), de la Soci6t6 Zoologique de France.
Pierre Fauvel fit ggalement des recherches de physiologie et de di<5t6lique humaine. II publia une quarantaine
d'articles sur le regime v6g£tarien, la valeur alimentaire des differents pains et l'excrgtion urique. Sous le
pseudonyme d'Flollow-Rim, il signa dgalement une trentaine d'articles sur le cyclisme. Pierre Fauvel mourut le
12 d6cembre 1958 h l'age de 92 ans. Comme l'ficrivait P. Ushakov le 4 mars 1959 h F. Rullier. “Pierre
Fauvel fut un savant Eminent qui a tant fait pour la connaissance des Polych£tes. Les magniliques ceuvres du
professeur Fauvel nous ont servi h tous dans nos 6tudes comme exemple de recherches taxonomiques”.
Pierre Louis Andr6 Fauvel (Fig. 1) was born in Cherbourg in 1866 of C16mence Matliilde Cappe (1851-
1909) and of Auguste Alexandre Fauvel (1821-1867) lieutenant in the French Marine. He was a student of
biology at the University of Caen and became an assistant at the Luc-sur-Mer research station. On June 29, 1897
he passed his doctorate at die University of Paris for his work on Ampharetidae. He was then appointed Professor
of Zoology at the University Catliolique de l'Ouest, and later Dean of the Faculty of Sciences. He studied
polychaetes from different parts of the world and many expeditions such as Hirondelle, Princesse Alice, Pourquoi-
Pas ? and Calypso. He found numerous new species but the most famous of all is Mercierella (Ficopomatus)
enigmatica discovered in the Channel of Caen by M. MERCIER. He had written many fauna such as die Faune de
France, the Fauna of India and won numerous prizes and distinctions including die Savigny Prize (1915), die
18
OB rill ARIES
Saintour Prize (1926) from the Academy of Sciences and the Ciadeau de Kerville Prize (1930) from the Soci6t6
Zoologique de France. Pierre Fauvel died on December 12, 1958, and Francois RULLIER (1907-1981) succeeded
him in the laboratory.
Fig. 1 . Pierre FAUVEL au debut du siecle
REFERENCES
ANONVME. — Cinquante amices d'enseignemenl a VUniversiU Catholique d' Angers ( 1897-1947 ). M. Pierre Fauvel, Doyen
de la Faculte des Sciences. Editions de 1’Ouest, Angers, 31 pp.
Fage L., 1959. — Pierre Fauvel. 1866-1958. Bull. Mus. nat. Hist, nat., Paris , 2c ser., 31:1.
Fauvel P., 1898. — Rechcrches sur les Ampharclidae. Bull. Scient. France Belgique , 30 : 277-489.
Fauvel P.. 1922. Un nouveau Serpulien d’cau saumatre ( Mercierella n. g. enigmatica n. sp). Bull. Soc. Zool. France ,
48 : 424-430.
GlLLET P., 1992. — Travaux de Pierre Fauvel. Francois Rullier el Louis Amourcux sur les Annelides Polychetes de 1894 a
1985. Bull. Soc. Sc. Nat. Ouest de la France, 14 : 20-36.
RULLIER F., 1959. — M. 1c Doyen Pierre Fauvel. Rev. Fac. Cath. Ouest . 2 : 5-27.
1 EN Hove H.. & J.C.A. Werdenburg, 1978. — A generic revision of the brackish-water serpulid Ficopomalus Southern.
1921 (Polychaeta: Serpulidae) including Mercierella Fauvel, 1923, Sphaeropomatus Treadwell, 1934.
Mercierellopsis Rioja, 1945 and Neopomatus Pilai, 1960. Biol. Bull., 154 : 96-120.
Source :
OBITUARIES
19
Ralph Ingram SMITH
1916-1993
Donald J. RF.ISH
Department of Biology
California State University
Long Beach, California 90840, Etats-Unis
Ralph I. Smith, professor Emeritus of Zoology at the University of California at Berkeley, died on May 12,
1993 in Santa Rosa, California. He collapsed after completing The Human Race; he was revived by emergency
workers, but died a few days later. Professionally he was particularly interested in the physiological adaptations of
intertidal invertebrates including polychaetes.
Ralph was born in Braintree, Massachusetts, on July 3, 1916. He attended Harvard University where he
received his doctorate in 1942 under the direction of John Henry Walsh. Following service in the United States
Army during World War II, he joined the faculty of the Zoology Department at the University of California at
Berkeley, a position he held for 41 years until his retirement in 1987. During his tenure at UC Berkeley he served
a term as department chairman, played a major role in the establishment of the University of California's Bodega
Marine Laboratory, and directed 22 doctoral students.
Ralph emphatically denied being a systematist by any stretch of imagination, but he realized the importance of
systematics. He believed in the importance of knowing and using the correct name of an organism. His interests in
this is evident in his taking over Light's Manual (Intertidal Invertebrates of the Central California Coast)
following the death of Dr. S. F. LIGHT. Later he organized and assembled a similar manual for the Woods Hole
region where is often taught in the summer.
His contributions to the knowledge of polychaetes included developmental studies in the nereids and more
recently in the terebellids. He published many papers on salinity tolerance and chloride regulation in nereids which
was based not only with California species but European species as well. He attended die Third and Fourth
International Polychaete Conferences and contributed papers to both.
His wife Todd of 52 years accompanied Ralph in their many travels which included visiting six continents. In
addition to his wife, he is survived by two sisters, five children, and grandchildren.
Pavel Vladimirovitch USHAKOV
1903-1992
Galina BUZHINSKAJA
Zoological Institute
Russian Academy of Sciences
St. Petersburg. Russia
On 25 February 1992, Dr. Professor Pavel Vladimirovitch Ushakov passed away at the age of 88 of cardiac
deficiency in die House of Science Veterans, Pushkin town, St. Petersburg.
The scope of scientific activity of Prof. P.V. USHAKOV included three fields of knowledge: zoology, marine
biology and oceanography. He published about 250 scientific works; eighty of diem, including diree monographs,
deal with systematics and phytogeny of polychaetes. He organized and participated in many marine expeditions
20
OBITUARIES
covering many different regions of the world's oceans, from the Arctic to the Antarctic Regions. He organized two
marine biological stations in the USSR. His works were widely recognized throughout the world. Scientists of
Australia, UK. USSR, USA, France, Germany, Sri-Lanka, named fifty-five marine organisms after him, i.e.
algae, invertebrates and fishes.
He received the degree of Honoris Causa from Aix-Marseilles II University. In 1972, the Oceanographic
Institute in Paris awarded him the Medal of Prince Albert I of Monaco, its highest international award, for his
works on marine biology. The USSR Geographic Society awarded him the Semenov-Tienshansky Gold Medal in
1958 for his works on the Sea of Okhotsk. The USSR Academy of Sciences awarded him the Pavlovsky Gold
Medal in 1983 for his studies of polychaetes.
P.V. Ushakov was born on 27 June 1903 in St. Petersburg into a family of a lawyer. After finishing a
gymnasium in 1920, he entered the Biological Department of the Physico-Mathematicae Faculty of Petrograd
University. He began his marine biological research as a student in 1921. Together with two young scientists
E.K. Guryanova and I.G. Zaks, he studied bionomy of the intertidal zone of Kola Bay and seasonal variations
of its like. This study became a classical work and was widely recognized by marine biologists.
After graduation from the University, Ushakov worked from 1924-1934 in the State Hydrological Institute,
first as a technician, then as a scientist in the Hydrobiology Department. During 1923-1926, Ushakov headed
small research teams on the Novaya Zemlya islands where Uiey studied coastal marine fauna and fauna of relict
lakes. Until 1935, he took part in different expeditions to the White, Barents, Chuckchee, Okhotsk and Japan
Seas. These expeditions resulted in a number of works including the volumes "Fauna and flora of the Chuckchee
Sea" (1952) published on the initiative and under the editorship of P.V. Ushakov and "The Fauna of the Sea of
Okhotsk and conditions of its existence" (1953). it was in the Sea of Okhotsk that Ushakov, then on board the
trawler "Gagara", recovered the first-ever animal specimen from a depth of more than 3,000 m. Among them were
hitherto unknown animals for which the new phylum Pogonophora was later erected.
Based on the study of flora and fauna of the Sea of Okhotsk he suggested for the first time a scheme of vertical
zonation of the sea and showed that tire Sea of Okhotsk and die Pacific Ocean were connected at depth via the
straits between the islands making up die Kuril Island Arc.
In 1931, he organized Kamchatka Marine Station in Avachinskaya Bay. In 1933, he received the degree of
Doctor of Biological Sciences. From 1936 to 1939, he organized Murmansk Biological Station of the USSR
Academy of Sciences in Dalniye Zelentsy and developed investigations there. In 1939, he returned to the State
Hydrological Institute. He supervised and participated in preparing hydrological manuals on the Okhotsk and
Bering seas. During World War II, P.V. Ushakov was in military service in the rank of engineer major and
worked on hydrometeorological manuals for die Navy.
From 1946 to 1982 P.V. Ushakov worked at the Zoological Institute of the USSR Academy of Sciences
(Leningrad). He was die head of the Laboratory of Marine Research of die Institute until 1966. Then he became
Curator of the Department of Annelids and Bryozoans. At that period, he focused on marine fauna, ecology and
biogeography, systematics and phylogeny of polychaetes. In 1948, he participated in die Kuril-Sakhalin expedition
of the Zoological Institute and Pacific Institute of Fisheries and Oceanography on board the "Toporok" research
vessel. Material of this expedition formed an important part of his book "Polychaetes of the Far Eastern Seas of
die USSR" (1955). In 1949, he took part in the first Pacific voyage of the "Vitiaz" research vessel and conducted
trawling in the Kuril -Kamchatka trench, when bottom-dwelling animals were recovered from a depdi of more than
8,000 m for the first time. In 1950 he published "Polychaetes of the Sea of Okhotsk". In 1956, he participated in
the first Soviet Antarctic Expedition on the research vessel "Ob". As a result of the expedition, he published a
number of papers dealing widi quantitative distribution of benthos in Antarctic waters, patterns of vertical
distribution of biocoenoses of bottom fauna and widi systematics of Antarctic polychaetes. In 1957 and 1958, he
worked on the Yellow and South China seas. In 1963, he conducted biological studies in Gulf of Guinea.
P.V. Ushakov visited France several times where he lectured in Marseilles University and in Sorbonne (Paris
University). In 1965, he published "Polychaeta Errantia of the Yellow Sea" widi Wu Baoling. In 1972, he
published his monograph "Polychaetes of the suborder Phyllodociformia of die Polar Basin and die nordi-western
part of die Pacific" and in 1982 "Polychaetes of the suborder Aphroditiformia of die Arctic Ocean and the north¬
western part of the Pacific".
During the last 10 years P.V. USHAKOV lived in Pushkkin town in die House of Science Veterans where he
wrote papers and essays on the history of science, memoirs about fellow scientists, i.e., his friends and
contemporaries. His colleagues and disciples visited him regularly to discuss widi him results of their studies and
new initiatives.
Everyone who was fortunate enough to work and meet widi P.V. Ushakov will keep fond memories of him.
Source :
OBITUARIES
21
Some personal souvenirs of P.V. USHAKOV
Lucien LAUBIER
Institut Oceanographique
195, rue Saint- Jacques
75005 Paris, France
Since the Long Beach Conference, some famous polychaetologists have disappeared. Among others, I am
thinking of Professor David Dean, Professor Pavel Vladimirovitch Ushakov and Professor Douglas P. Wilson.
The death of P.V. Ushakov, at the beginning of this year, was particularly sad for me and I would like to recall
with his friends and colleagues a few souvenirs of the different visits he made in France.
I first met P.V. Uskhakov in Summer 1965. Me came from Marseilles to my laboratory in Banyuls-sur-Mer
and spent a few days there. I remember a one day trip to the Spanish boarder, at a small village called Le Pcrthus.
P.V. Ushakov was astonished to discover that he, a citizen from die USSR, could walk through the custom
freely, from France to Spain and back, without any inquiry from the french and Spanish guards. On die same day.
P.V. Ushakov experienced the french way of eating snails, and found them just delicious. At the end of this
visit, I took him with my car from Banyuls-sur-Mer to Angers: I had a radier fast car, a Citroen DS 19, and speed
limitations were not a major problem for me. P.V. Ushakov remained very quiet at 100 miles per hour, but I
found later on that this journey became one of his frequent story when speaking of our relationship with other
people ! W'e reached Angers without any uouble, and P.V. Ushakov worked a few days with Francois RULLIER.
When die Second Oceanographic Congress took place in Moscow, in 1966, 1 attended the Congress and I had
the opportunity to make a one day trip in Leningrad, now Saint Petersburg. P.V. Ushakov invited me with
Professor M. FONTAINE for a tea party in his small flat, where he lived widi his daughter in law.
P.V. Ushakov came back to Banyuls-sur-Mer in die Winter 1967-68, and spent a full fortnight working on
Mediterranean Polychaetes. We went at sea togcdicr on board die small trawler Nereis, and P.V. Ushakov was
specially interested by a one meter long Eunice rousseaui living in a special glass-tube whick I kept for more dian
six years in my laboratory and exhibited during the easter and summer courses to die students. The regular wave
along the body of die movement of the pectinate branchiae was fascinating... P.V. Ushakov asked me for a
posterior part of die worm, which I knew regenerated easily, and I gave him some 300 segments of diis large
Mediterranean Eunice which quickly recovered. During that visit, we had a party in my flat for Christmas night:
we were all very surprised when P.V. Ushakov quietly asked us about midnight Christmas mass: do French
people usually go to church for Christmas mass? Moreover, he decided he wanted to go to church himself, where
he attended the whole office.
When 1 moved to Brest, beginning of 1969. It was more difficult to Wellcome P.V. Ushakov in my next
laboratory, due to die fact that Brest is also our main naval base for nuclear submarines... Nevertheless, I obtained
that P.V. Ushakov could come for two days under special permission. We had a long discussion about the 1917
Revolution, and P.V. Ushakov told me that he very clearly saw the shots of the cruiser Aurora of die Winter
Palace in Leningrad. At that time, I was working on deep-sea Mediterranean Polychaetes collected in the Hellenic
Trench. I was specially interested by an aberrant tiny worm combining spiomorph and tercbellomorph features.
P.V. Ushakov agreed on die fact diat it should be described as a new genus. In fact, I described it its Ushakovius
enigmaticus , type of a new sub-family, and Professor M. Fontaine told P.V. Ushakov of diis new child when
he gave to Professor Ushakov the Manlay-Bendall medal of die Institut Oceanographique in Paris, a few weeks
after his visit to Brest. A few days later, P.V. Ushakov told me diat it should constitute a new family, which in
fact was recently proposed by B. Molte.
Later on, P.V. Ushakov retired from the Zoological Institute, I had no more opportunity to visit USSR, and
I received some news exchanging letters with him. Me of course wrote in French. Finally, Marina Dolgolenko
was our last link.
I am sure all those who have had the chance to met P.V. Ushakov and experienced his happiness will share
my deep sadness.
22
OBITUARIES
Douglas P. WILSON
1902-1991
David GEORGE
Department of Zoology
Natural History Museum
Cromwell Road
London, SW7 5BD. Royaume Uni
Dr. Douglas P. Wilson died suddenly on 18 December 1991 aged 89. "DP", as he colleagues, was born in
Manchester and educated at William Hulme's Grammar School. After leaving school he started on a career in the
Lancashire cotton industry, but this career was cut short by a dramatic slump in the cotton trade. Having from a
very early age been keenly interested in natural history (particularly aquatic life) he decided to attend evening
classes in zoology at Manchester University and also joined the Manchester Microscopical Society. This led to
him doing practical work on die shore and to a decision that a career in zoology offered him a better life than a
career in business. Consequently he enrolled in 1923 on a BSc course in zoology at Manchester University during
which time he attended marine biology courses at Millport, Port Erin and Plymouth. Having gained a first class
degree he obtained a grant in September 1926 to study polychaete development at die Marine Biological
Association's laboratory at Plymouth, where less than a year and a half later, he was appointed to die staff as
Assistant Naturalist widi special responsibility for development of the public aquarium. DP remained at this
marine station for die rest of his working life, officially over 10 years as Deputy Director, aldiough continuing to
work diere until the end of 1981. From die start of his career at die laboratory until die beginning of the second
world war. D.P. studied in detail die early development of polychaetes of many different families. His ability to
rear polychaete larvae in die laboratory combined widi his skills as a microscopist and a keen eye for detail
contributed in no small measure to the scientific accuracy of his early research publications.
During die 1930's he began to investigate the influence of die substratum on die metamorphosis of larvae of
such species as Scolecolepis fuliginosa and Noiomastus latericeus, but unfortunately the war years and more
applied research intervened. The Plymoudi laboratory had cause to be grateful to DP during die second world war
because it was his team of fire-fighters that saved die majority of die building by putting out die fires started by
incendiary bombs dropped during an air raid.
After the war he returned to his work on habitat selection by metamorphosing larvae and produced a series of
papers using mainly Ophelia bicornis as his experimental animal. He was able to show that larval settlement
could be delayed for some considerable lime if die substratum was not suitable, and that micro-organisms played
an important role in making die substratum attractive to larvae. In 1951 he was awarded the Prix George KOHN,
an award of the Institut Oceanographique, Paris for a summary paper on this research. I Ic had by diis time obtained
his DSc from Manchester University for his investigations on die early development of polychaetes.
In parallel with this work, and continuing until the late 1950’s, DP conducted an interesting series of
experiments on die "quality" of seawater in collaboration with a chemist at die laboratory, F.A.J. Armstrong.
Using sea urchin larvae he was able to show dial larval development took place at different speeds and with
varying degrees of success in seawater from different areas. In effect he had discovered a biological method for
distinguishing seawaters of different origins, which effectively complemented die plankton indicator species
concept developed by colleagues at the laboratory.
He next turned his attention to die biology of British species of magelonid and in die process uncovered some
taxonomic problems which he solved by erecting two new Magelona species in the late 1950’s. Interestingly his
last scientific publication in 1982 returned once again to die genus, describing die larval development of three
species from Idealities near Plymouth and Salcombe. However, most of DP’s later contributions to the study of
polychaetes dealt with British species of the Sabellariidae, the larvae of which he described in one of his earliest
papers in 1929.
Soon after he recommenced work on die sabellariids die “Torrey Canyon” oil-tanker disaster occurred and he
was able to use larvae of Sabellaria spinulosa to assess die long-term effects of low concentrations of die detergent
used to clean up the oil. He followed this by studies on die early development of the reef-building shore-dwelling
honeycomb worm Sabellaria alveolaia and combined the laboratory work widi valuable long-term monitoring of
Source :
OBITUARIES
23
recruitment and succession in colonics of the worm at Duckpool in north Cornwall from the early 1960's through
lo the mid 1970's. He showed that die larvae could delay metmorphosis, sometimes for many weeks, until a
suitable substratum was found, and dial they settled in preference on or near tubes of die same species, being
attracted primarily by the chemical composition of the cement binding die sand grains of die tubes together.
During diese studies he made extensive use of photography to record not only die morphology of the developing
larvae but also die changes in die shore colonies with time.
FlG. 1. Professor Douglas P. WILSON
Source :
24
OBITUARIES
From an early age DP had been interested in the art of photography and he was a pioneer in the photography of
living marine animals on the shore, in tanks, and under the microscope. Indeed, he was almost certainly the first to
adapt electronic flash for the photography of living planktonic organisms, his dark-field photomicrographs being
particularly impressive, even today. It was for his pioneering work in this field that he received an honorary
fellowship of the Royal Photographic Society in 1987.
As well as being remembered by those with a special interest in polychaetes and marine life photography, DP
will be remembered by the many hundreds of students who attended die famous caster vacation courses in marine
biology at the Plymouth laboratory, for it was he who was the principal organizer of these between 1930 and
1948. Neither will his skills as a popular author be forgotten by those who have copies of "Life of the shore and
shallow sea" and "They live in the sea".
Source : MNHN. Paris
CONTRIBUTED PAPERS
Cytophysiology, development and reproduction
1. Evolution of viviparity in the genus Ophryotrocha (Polychaeta, Dorvilleidae) 2 9
Bertil AkeSSON
2. Environmental influences on endocrine systems controlling reproduction
in Polychaetes 3 7
Matthew G. BENTLEY, Jcni BOYLE & Allan A. PACLEY
3. Morphometric analysis of cellular specification in Platy nereis and Pomatoceros
embryogenesis (Annelida, Polychaeta) 4 5
Adriaan W.C. Dorresteijn & Craig Marc LUETJENS
4. Observations on reproduction and growth of Sahella spallanzanii (Polychaeta,
Sabellidae) in the Mediterranean Sea 5 1
Adriana GlANGRANDE & Angela Petrarou
5. The functional significance plexuses in the ecology of Ophelia hicornis Savigny 5 7
Tegwyn Harris
6. Feed-back regulation in Platynereis dumerilii Audouin & Milne-Edwards, 1833:
a status review 6 5
Dietrich K. HOFMANN
7. Bioaccumulation du fer dans lc corps cardiaque de Karicirrus heryli
Petersen & George (Polychaeta, Ctenodrilidae) 7 3
Jean VovELLE, Mary E. PETERSEN. Michele GRASSET & Patricia BEAUNIER
Genetics and morphology
8. Functional ciliary groups of the feeding palps of Spionid polychaetes 8 1
Daniel M. DaUER
9. Attributes of ribosomal DNA in alvinellid polychaetes from hydrothermal vents 8 5
David R. DIXON, Linda R.J. DIXON & Verena TUNNICLIFFE
10. On the nature of the two anterior asetigerous rings in Dorvilleidae and
Dinophilidae (Annelida, Polychaeta) 9 3
Danny Eibye-Jacobsen
11. The head of Maldanidae polychaetes of the subfamily Maldanidae 101
Karen D. GREEN
12. Effects of sample fixation on body shape of Capitella capitata
(Polychaeta, Capitellidae) 1 1 1
Maria Nuria MENDEZ & Maria Jose CaRDELL
13. infrastructure of sense organs and the central nervous system in
Parenterodrilus taenioides and their phylogenetic significance in the
taxon Protodrilida (Annelida, Polychaeta) 119
Gunter PURSCHKE & Claude JOUIN-TOULMOND
14. Genome size in Polychaetes: relationship with body length and life habit 129
R. Soldi. L. Ramella. M. Cristina Gambi, Paolo Sordino & Gabriella Sella
Source :
26
CONTRIBUTED PAPERS - CONTRIBUTIONS
15. Fine morphology of the feeding apparatus of Cossura sp. (Polychaeta,
Cossuridae) from the White Sea 1 3 7
Alexander B.TZETLIN
Phytogeny and taxonomy
16. Polvchaetes of the family Acoetidae (= Polyodontidae) from the Levant and the
Central Mediterranean with a description of a new species of Eupanthalis 145
M. Nechana Ben-Euahu & Dieter FlEGE
17. Prionospio caspersi Laubier (Polychaeta, Spionidae) in the Black Sea:
long-term monitoring of a population 163
Temir A. Britayev. Alberto CASTELLI & Tatiana S. AKSIUK
18. Systematics, ecology and biogeographic relationships in the sub-family
Travlsiinae (Polychaeta, Opheliidae) 169
Jean-Claude Dauvin & Gerard Bellan
19. A new' species of Ophryothrocha (Polychaeta, Dorvilleidae) associated with
ice scours in the Canadian Arctic Archipelago 185
Judith A. FOURNIER & Kathleen E. CONLAN
20. Two new species of Branchiomma (Sabellidac) with rcdcscriptions of closely
related species and comments on Pseudobranchiomma and Sabellastarte 19 1
Phyllis Knight -Jones
21. Redescription of Hipponoa gaudichaudi Audouin & Milne-Edwards, 1830
(Polychaeta, Amphinomidae) 199
Jerry D. KUDENOV
22. Sabellariidae (Annelida, Polychaeta) from south America 2 09
Paulo da Cunha Lana & Claudia Silvia BREMEC
23. The phylogenetic position of the Pilargiidae with a cladistic analysis
of the taxon - facts and ideas 22 3
Frank LlCHER & Wilfried Westheide
24. Pseudatherospio fouchaldi a new genus and species of Spionidae
(Polychaeta, Annelida) from the Southern California, USA 23 7
Laurence L. Lovell
25. Adercodon pleijeli gen. and sp. nov. (Polychaeta, Ampharetidac) from the
Mediterranean Sea 24 1
Andrew S.Y. Mackie
26. The genus Ophryotrocha sensu Into (Polychaeta, Dorvilleidae) in the Tromso
area, Northern Norway 2 5 1
Eivind OUG
27. Distributional patterns and taxonomic notes on Lumbrineridae from Crete
(S. Aegean, eastern Mediterranean) 2 59
K. Nadia Papadopoulou, C. DOUNAS & Chris J. SMITH
28. Autolytinac (Polychaeta, Syllidae) from Cuba and north American Atlantic Ocean 2 69
Guillermo SAN MARTIN
29. New arctic species of Scolelepis (Polychaeta, Spionidae) 279
Andrew V. SlKORSKI
30. A systematic problem of inter- and intra-generic variation in nephromixia
of Terebellidae 2 87
Ralph 1. Smith
31. Morphometric variation in bifurcate notosetae of two Euphrosine species
(Polychaete, Euphrosinidac) 29 1
Ken D. Vogt & Jerry D. KUDENOV
Source :
CONTRIBUTED PAPERS - CONTRIBUTIONS
32. Pseudonotomastus southern! gen. nov., a new capitellid from the Celtic Sea 2 99
Lynda M. WARREN & Miles PARKER
33. A new species of Chaetozone (Polychaeta, Cirratulidae) from Europe,
with a redescription of Caulleriella zctlandica (McIntosh) 307
Annette WOODHAM & Susan CHAMBERS
34. Phylogcny of Alciopidae (pelagic polychaetes): a cladistic analysis 3 1 7
Baoling Wu & Lua Hua
Ecology and biogeography
35. Preliminary observations on a dense population of Plyllochaetopterus socialis
Claparede at the sulphurous water boundary in a Mediterranean submarine cave 3 23
Marco ABBIATI, L. AlROLDI, Alberto CaSTELLI, F. ClNELLI & AJ. SOUTHWARD
36. Contribution of the Polychaetous annelids to the diet of some brazilian fishes 33 1
A. Cecil ia Z. AMARAL. Edmundo F. NONATO & Monica A.V. PETTI
37. Ecology of Pherusa sp. (Polychaeta, Flabelligeridae) 33 9
Analfa AMOR
38. Polychaete fauna associated with the coral Cladocora caespitosa (L.)
in the eastern Mediterranean 34 7
Christos ARVaNITIDIS & Athanasios KOUKOURAS
39. Morphology, ecology, and juvenile development of Cossura pygodactylata
Jones (Polychaeta, Cossuridae) in Arcachon Bay, SW France, with a reassessment
of the geographic distribution of C. pygodactylata and C. soyeri Laubier 3 55
Guy BaCHELFT & Lucien LAUBIER
40. Larvae-substrate relationships of Eupolymnia nebulosa (Montagu, 1818)
(Polychaeta, Terebcllidac): an experimental analysis 37 1
Michel Biiaud & Jae H. Cha
41. Is Owenia fusiformis a cosmopolitan species? 3 83
Jean-Claude DaUVIN & Eric ThiEbaUT
42. Light influence on larval emission and vertical swimming in the terebellid
worm Eupolymnia nebulosa (Montagu, 1818) 4 05
Jean-Claude DUCH&NE & Christian Nozais
43. Polychaeta of the German Bight from the 1987 cruise of the R/V "Senckenberg" 4 13
Dieter FlEGE & Nechama BEN-ELIAHU
44. Selection des grains de sable selon leur nature et leur forme par
Sabe/laria alveolata Linne (Polvchete, Sabellariide) lors de
la reconstruction experinientale de son tube 4 25
Yves GRUET & Yves BODEUR
45. Les vers polychetes et l'estuaire de la Loire au debut du 20eme siecle
par G. FERRONNIERE (1875-1922) 433
Yves GRUET, Joceiyne March and & Joseph Baudft
46. Temporal and spatial patterns in the distribution of infauna] polychaetes
in Jervis Bay, New South Wales, Australia 44 1
Patricia HUTCHINGS & C.A. JACOBY
47. Ecology and biogeochemistry of an Paralvinella sulf incola at
northeast Pacific hydrothermal vents: review and comparison with
A /vine l la spp. of the east Pacific rise 4 53
S. Kim Juniper
48. Polychaete assemblages along a depth gradient in a Spitzbergen Fjord 4 63
Michael A. KENDALL
49. The biogeography of some abyssal polychaetes 47 1
J0rgen B. KirkegaaRD
28
CONTRIBUTED PAPERS - C'ONTRIBUTIONS
50. Preliminary results on recolonization in a small brackish basin on the
island of Elba (western Mediterranean)
Claudio Lardicci & R. Baldi
51. Intertidal sandy beaches polychaetcs of Sao Sebastiao island, Southern Brazil
Eloisa H. Morgado. A. Cecilia Z. Amaral, Edmundo F. Nonato & Lara B. Salvador
52. Influence of the tube-building spionid polychaete Polydora ciliata on
benthic parameters, associated fauna and transport processes
Carol a Use-Marie NOJI
53. Patterns of abundance and diversity from the abyss - Polychaetcs from
northeastern Atlantic abyssal plains
Gordon L.J. Paterson. John D. Gage. P. Lamont. B.J. Be tt & M.T. Thurston
54. Polychaete response to different aquaculture activities
Patricia POCKUNGTON. David B. SCOTT & C.T. SCHAFER
55. Influence of temperature and diet on the larval development and growth
of juveniles Marphysa sanguined (Montagu) (Polychaeta, Eunicidae)
Daniela Prevedelli
56. Ethologie alimentaire d'Annelides Polvchetes endogees : determination
du niveau sedimentairc oil s'effectue la collecte de nourriture
Chantal SalEN-PicaRD, Claire Graham & Magali GERINO
57. Polychaete distribution patterns on Chlamys palagonica of the Magellan Strait
Rossana SANFILIPPO
58. Polychaeta in the cstuarv of the Piaui River, Sergipe, Brazil
Maria A. Santos. C.S.G. Santos & C.M.M. Oliveira
59. Life history of the polychaete Polydora variegata that bores into the shells
of scallops in Northern Japan
Waka Sato-Okoshj
60. Annelid polychaete populations of the Order Eunicida from the southern
Gulf of Mexico
Vivianne Solis-Weiss, Luz Veronica Rodriguez-Viixanueva, Alejandro Granadas-Barba.
Victor Ochoa-Rivera. Luis Miranda-Vazquez & Pablo II ernant>ez- Alcantara
61. Ecological analysis of some Syllidae (Annelida, Polychaeta) from
the central Tyrrhenian Sea (Ponza Island)
Alessandra SOMASCHLM & Flavia Gravina
62. Cyclical changes in the fauna associated with tube aggregates of Ficopomatus
enigmatic us (Fauvel)
Nigel S. Thomas & Clifford IT Thorp
63. Population variation in Ficopomatus enigmaticus (Fauvel) (Polychaeta,
Serpulidae) in a brackish water millpond at Emsworth, West Sussex, U.K.
Clifford H. Thorp
Culture and valorisation
64. Polychaetcs of commercial and applied interest in Italy: an overview
M. Christina Gambi. Alberto CASTELLI. Adriana GlANGRANDE, Daniela PREVEDELLI &
R. ZUNARELLI VaNDINI
65. Polychaeta as a world resource: a review of patterns of exploitation
as sea angling baits, and the potential for aquaculture based production
Peter J.W. Olive
479
4 85
493
503
5 1 1
52 1
527
53 5
5 4 1
54 9
559
567
575
585
5 93
6 03
Source : MNHN. Paris
1
Evolution of viviparity in the genus
Ophryotrocha (Polyehaeta, Dorvilleidae)
Bertil AKESSON
Department of Zoology
University of Goteborg
Medicinaregatan 18
$-413 90 Goteborg. Sweden
ABSTRACT
Brooding is a common feature in the genus Ophryotrocha. Viviparity, the most extreme type of parental care, is
represented by only one species, O. vivipara , but tendencies towards viviparity have also been reported from gonochoric as
w'ell as hermaphroditic species. Except for the viviparous species, all species studied deposit their eggs in a gelatinous matrix.
The surface of the egg mass may remain soft and sticky, but in two distinct species groups the surface hardens to a solid
membrane that encloses gel and eggs. In both groups newly spawned egg masses may occasionally contain a few young larvae.
Such larvae never occur in a young female’s first egg mass. The larvae arc interpreted as originating from fertilized eggs that
have been trapped in the coelom of the female during a previous spawning. They develop inside the female at a retarded rate.
In O. socialis not only lar vae at an early stage of development are released but also larvae/juveniles at more advanced
stages. Usually they are released together with a normal spawn, but they may also appear single. Juveniles with up to 12
setigerous segments have been observed. During the normal course of development, the 12-setiger stage is attained after about
80 days. At that age they have already developing oocytes in the coelom whereas the viviparous progeny with the same number
of segments have not.
Observations of incipient viviparity in three species groups call for a reevaluation of some previous reports on self-
fertilization and on viable larvae obtained in crosses between species that are otherwise reproductively isolated.
RESUME
Evolution dc la viviparite dans le genre Ophryotrocha (Polyehaeta, Dorvilleidae)
C’est un tr ait frequent du genre Opluyotrocha d’incuber ses oeufs. La viviparite, le type le plus extreme du soin parental, est
representee chez une espece, O. vivipara . mais des tendances vers la viviparite out aussi (Ste rapportees chez des especes
gonochoriques aussi bien que chez des especes hermaphrodites. Exception faite des especes vivipares, toutes les especes
etudiees deposent leurs oeufs dans une matrice gelalineuse. La surface de la masse d’oeufs peut rester molle et collante. mais
dans deux groupes d’especes distincts. cette surface durcit en une membrane solide qui renferme le gel et les oeufs. Dans les
deux groupes. des masses d’oeufs recemment deposecs peuvent conlenir, de temps en temps, quelques rares larves/juveniles.
De telles larves n’apparaissent jamais dans la premiere masse d’oeufs d’une jcunc fcmclle. Les larves proviennent probablemcnt
d’oeufs fecondes anterieurement qui sont restes dans le coelome de la femelle ou ils se sonl developpes lentement.
Chez O. socialis des individus larve/juvenile. h un stade avance sont relaches en meme temps que des larves en debut de
developpement. Habituellement elles sont emises en meme temps qu’une ponte norinale, mais elles peuvent aussi apparaitre
AKESSON. B.. 1994. — Evolution of viviparity in the genus Ophryotrocha (Polyehaeta. Dorvilleidae). In: J.-C. Dauvin.
L. Laubihr & D.J. Reish (Eds). Actes de la 4eme Conference internationale des Polychetes. Mem. Mus. natn. Hist, nat., 162 :
29-35. Paris ISBN 2-85653-214-4.
Source . MNHN. Paris
30
B. Akesson
sculcs. Dc tcls juveniles ayant jusqu’a 12 segments sctigeres ont etc observes. Au cours d'un developpcment normal ce stade 12
setigeres n’cst atteint qu'apres environ 80 jours. Ces larves/juveniles ont alors deja developpe dcs ovocytes dans le coelome
Landis qu'il n’y a pas d’ovocytes dans les juveniles issus d'un developpcment vivipare au mcme stade de devcloppement. Les
observations failes sur cette tendance a la viviparite dans les 3 groupes d’especes nous conduisent a une revision des resultats
anterieurs traitant de l'autofecondation et aussi des larves viables qui en realite n'ont pas ete obtenues dans des croisements
enlre especes differences.
INTRODUCTION
Brood protection has evolved many times among boll) invertebrates and vertebrates (Hogarth, 1976;
Clutton-Brock. 1991). The same applies also to viviparity, the most extreme form of brood protection.
Evidence from most groups indicates that viviparity has evolved from oviparous ancestors and that internal
fertilization has been a preadaptation for the evolution of viviparity. In transition stages fertilized eggs have been
retained for progressively longer periods of time. They do not receive any nutrients from the female and tliis holds
true also for species with ovoviviparity, the least advanced form of viviparity. In more advanced viviparous forms,
the female continues to provide the embryos with nutrients. Often a kind of placenta analogue develops or the
embryo/larva receives nutrients from surrounding body fluids of the female.
For the evolution of viviparity from oviparous ancestors to occur, transition stages must also be selected. The
continuing discussion has been widened to involve other aspects of brood protection and its relation to egg size.
Shine (1978) suggested the "safe harbor" hypothesis according to which optimal offspring size is determined by
relative mortality rates of egg stages and free-living juveniles. Selective forces tend to maximize die time spent in
the safest stages of development. In brooders eggs are safer than juveniles which should account for die positive
correlation often seen between brood protection and large egg size (Shine, 1989; Clutton-Brock, 1991).
According to Hogarth (1976), evolution towards viviparity is favoured in species that already produce a
restricted number of eggs. Retention and viviparity protect die progeny against bodi predators and harsh
environmental conditions such as cold climate, desiccation or, for marine animals, suboptimal salinity levels.
Viviparity has been reported from several polychaete families and SCHROEDER & Hermans (1975) have listed
19 species. I lowever, for 9 of these the original reports on viviparity have not been verified in later studies. Many
older reports on viviparity were analyzed by Smith (1950) who provided evidence dial some of them were
erroneous. Some embryos or larvae from inside the body of polychaetes were either developmental stages of
parasitic polychaetes or turbellarians.
The purpose of diis paper is to describe a possible line of evolution towards viviparity in the genus
Opliiyoiroclia of the family Dorvilleidac. Dorvilleid polychaetes arc generally small and many of the smallest,
nonpar aside species belong to the genus Opliiyoiroclia. Only direc species exceed a lengdi of 10 mm. Two of
these are commensals in the gill chamber of crabs (Martin el al. , 1991), die third one is found near geothermal
vents (Blake, 1985). The smallest of all Opliiyoiroclia species, 0. vivipara Banse, 1963, is only 0.8-1 mm long.
Banse's description was based on two specimens from die vicinity of Friday Harbor, Washington. This was the
only record until I collected about 50 specimens in the aquarium of the Tjarno marinbiologiska laboratorium
located about 200 km north of Gothenburg. Opliiyoiroclia vivipara is one of the few species that I have failed to
maintain as a laboratory culture; nondieless Banse's observation of a truly viviparous species could be confirmed.
The juveniles have two or three setigerous segments when released from the posterior end of die female.In contrast
to a uniform adult morphology in most species, reproduction is remarkably variable. In addition to the traits listed
m I able 1. species or species groups may also vary in odier reproductive adaptations such as clutch size and time
between consecudve spawnings, sex ratio in gonochoric species and amount of energy allocated to individual egos
(Akesson, 1973).
Mating behaviour is equally variable. Sella (1985. 1988) analyzed pair formation and egg hading in the
simultaneous hermaphrodite O. diadema. A behaviour has evolved that safeguards against non-reciprocating
partners. In gonochoric species, females often discriminate against males from other geographic populations and
they certainly do so in interspecific crosses (AKESSON, 1972a, 1977b. 1978, 1984). In the protandrous
hermaphrodite O. puerilis, sex reversal may occur several limes in the same individual. In pair cultures with
females, the result ol lights over sex will be that the winner remains female and the loser changes to male
BERG LUND ( 1991) has shown that females prefer small mal es. If a female mates widi a large male, she is at risk of
being challenged to change sex when she is weakened after spawning.
Source :
EVOLUTION OF VIVIPARITY IN THE GENUS OPHRYOTROCHA
31
Table 1. — Reproductive traits in the genus Ophryoirocha.
Incipient viviparity has been reported from the simultaneous hermaphrodite 0. diadema (Akesson. 1973,
1976). Occasionally one or two larvae appear in newly spawned egg masses, but never in a female's first brood.
The fusiform egg masses of 0. diadema are surrounded by a tough wall and larvae cannot enter an egg mass from
the outside.
As in all other known Ophryoirocha species, fertilization in 0. diadema is preceded by a kind of
pseudocopulation similar to that described by Westheide from 0. gracilis (Whstheide, 1984, fig. 3). Selling has
not been observed. Eggs and spermatozoa arc shed into a gelatinous matrix and mingle there. 'The egg mass is
molded to its final shape and usually attached to a substratum. 'Then the surface of the mucus hardens to form the
lough outer wall.
The explanation suggested for the presence of larvae in newly spawned egg masses is that a few eggs have
been trapped in the female part of the coelom during a previous spawning. They have been fertilized by entering
spermatozoa, developed inside the body, and then released together with die next spawn (Akesson, 1976).
The same type of incipient viviparity as in O. diadema has also been observed in several members of the
labronica group, a group of related gonochoric species within the genus (Akesson, 1973). Members of that group
produce a different kind of egg mass that is tube-shaped and contains smaller, but more numerous eggs than that of
0. diadema. Enclosed larvae inside newly spawned egg masses have been observed in 0. labronica ,
0. nologlandidata , and 0. macrovifera , and they may occur in all members of the labronica group.
Ophryoirocha socialis , another simultaneous hermaphrodite, was recently described by OCKELMANN &
Akesson (1989). The gelatinous matrix around the eggs is sparse in this species but there is enough to attach the
eggs to each other forming tubular or irregular egg masses. As in 0. diadema fertilization lakes place after
pseudocopulation. Isolated individuals may self- fertilize but such self-fertilization is external.
In a still ongoing life table study that began with fertilized eggs, O-setiger larvae occasionally appeared in the
bowls when the experiment had continued for about 6 months. The larvae were at die stage of development that is
normally obtained in 3 weeks (OCKELMANN & Akesson, 1989, Fig. 10). Since the adult worms were transferred to
clean bowls once a week, these larvae could not be die result of a previous spawn. Eventually more advanced
larvae could also be collected, i.e., larvae with 1-2 or more setigerous segments. The peak production of such
larvae was observed when the adults were 10 months old and had 19-20 setigerous segments. In one week 40
adults had produced 1 1 0-setiger larvae
Source :
32
B. Akesson
and 17 juveniles with 7-12 setigers (mean 9.9 ± 0.4). In addition, die adults had spawned 919 eggs during the
same week.
After a normal spawning, die progeny develops into functional males with 6 setigers after about 50 days. The
first spawning was observed at an age of 60 days in worms with 10 setigers. Only few worms spawn before the 11-
sedgcr stage (Ockelmann & Akesson, 1989). Not even the largest viviparous progeny had any visible oocytes in
the coelom. They were more slender than larvae widi the same number of setigers that develop after normal
spawning. It has not been possible to determine the age of die viviparous progeny when released from the coelom.
REEVALUATION OF SOME PREVIOUS REPORTS
The observations of incipient viviparity in two species groups as well as mixed oviparity and viviparity in 0.
social is may justify a reevaluation of some previous reports on self-fertilization and on results of crossing
experiments.
Hartmann (1943) and Bacci (1978) reported on rare instances of self-fertilization in 0. puerilis. In some
crosses between die Adamic and Mediterranean subspecies of 0. puerilis, a very low percentage of spawned eggs
were reported to develop into viable larvae (Akesson, 197.3). The possibility should be considered dial these
reports concern incipient viviparity of the same kind as in 0. diadema and the labronica group. However, it is
evident diat some species may reproduce by both cross-fertilization and self-fertilization. This is true of 0.
labronica ( but note die discussion about identity of species in Akesson, 1984), 0. socialis, and a not yet
described species from Florida (La Greca & Bacci, 1962; PaRENTI,1960; Zunarelli, 1962; Zunarelli-
Vandini, 1967; Akesson. 1984; Ockelmann & Akesson, 1989).
In the light of these findings, die previous report on partial success in crosses between die Pacific species 0.
notoglandulala and 0. labronica pacifica should be reevaluated. Akesson (1984) reported dial occasionally a few
(< 10) viable hybrids were obtained in crosses between female O. noioglandulata and male O. I. pacifica. These
supposed hybrids were all female and therefore IA hybrid breakdown could not be tested. No progeny was
obtained in backcross with O. I. labronica males except for a few larvae. As in die first cross, the number of larvae
per egg mass was always below 10. In backcross with O. noioglandulata many egg masses were produced, usually
widi almost 100 % development.
A return to die original data sheets revealed that in the interspecific cross only 5 "hybrids" developed into
normal, mature females. They were first used in backcross widi male O. noioglandulata and then with O. I.
labronica. Previous and subsequent crosses between O. labronica (both subspecies) and 0. noioglandulata proved
to be intersterile. More than 100 egg masses in each reciprocal cross have been observed. Moreover, die "hybrid"
progeny reported by Akesson (1984) was all female. The same was true of all viviparous progeny observed so far
in die diree gonochoric species where incipient viviparity has been recorded. A very likely explanation of die
crossing results (Akesson, 1984) is dial the few larvae obtained were an expression of incipient viviparity.
In recent experiments widi both inter- and intraspecific crosses, individual egg masses have been analyzed for
enclosed larvae. Such larvae are found in less dian 5 % of the egg masses and' only in egg masses produced by
females diat have spawned previously. The fact diat such larvae were produced in two subsequent generations in
the crosses reported by Akesson (1984) may indicate a heritability of die trait, but recent selection experiments
with viviparous progeny has not yet proved diis.
DISCUSSION
For the evolution of viviparity in die genus Ophryotrocha, transition stages between oviparity and viviparity
should have a selective advantage. One such advantage may be dial those embryos that are retained in the female's
body have better chances of survival than die siblings which are fertilized and spawned at the same time. A
brooding worm presumably has better chance of escaping a predator than embryos enclosed in an immobile egg
mass that die female will desert when attacked.
Internal fertilization as a prerequisite for viviparity is not fulfilled in Ophryotrocha, but functionally die kind of
pseudocopulation found in die genus comes close to internal fertilization (WESTHE1DE. 1984). The final stage,
obligate viviparity, is found in the smallest known Ophryotrocha species only. This may be an indication that die
evolution of viviparity is one of many adaptations to 'the problem of being small'. As has been repeatedly
discussed for meiofauna species (Swedmark, 1964; WESTHEIDE, 1984), smaller size is correlated widi changes in
Source : MNHN. Paris
EVOLU TION OF VIVIPARITY IN THE GENUS OPHRYOTROCHA
33
reproductive traits compared to related larger species. WESTHEIDE (1987) demonstrated how progenetic (neotenic)
evolution has been one of the major forces behind adaptation to die interstitial habitat. The morphology of an adult
Ophryotrocha is very similar to the larval morphology of larger cunicid polychaetes, e.g., to the larvae of
Dorvillea rudolphi (Richards, 1967). The evolution of progenesis is also demonstrated in Westheide’s (1987)
series of increasingly juvenile characters in dorvilleid genera where die endpoint is die dinophilid genus
Dinophilus. It has been shown dial dinophilids are closely related to cunicids (Hermans, 1969; Akesson. 1977a;
WESTHEIDE, 1985).
Reproduction in the genus Ophryotrocha is more variable than in any other polychactc taxon of similar size.
Energetic constraints related to small size may be one reason; opportunistic life histories widi often sparse
populations may be another. The most important of those reproduclive traits are listed in Table 1.
WESTHEIDE's (1987) series of successive embryonization in die family Dorvilleidac indicates dial small species
have evolved from larger ones, —"these small interstitial species must then form die end-point of an evolutionary
line which originates in larger benthic species" (WESTHEIDE, 1984, p 266). For die genus Ophryotrocha it has also
been suggested that the alrochal, demersal larvae found in 0. maculata occurred in die larger ancestors
(Zavarzina & Tzetlin, 1991). Obviously the progenedc evolution has been very successful and has triggered an
adaptive radiation.
The egg diameter varies between 240-320 pm in 0. cosmetandra (Oug, 1990) and 56.5 pm in 0. paralabidon
(Hilbig & Blake, 1991). At the end of the brooding period, the progeny of some species is released as
polytrochous larvae with no setigerous segments, whereas other species release juveniles with up to 5 setigers. In
O. vivipara die progeny has only 2-3 setigers when released, but die largest recorded viviparous progeny of O.
socialis had 1 2 setigers.
In summary, die variability in reproductive traits in die genus Ophryotrocha makes ii an extremely valuable
study material, a kind of marine Drosophila. "This genus may be very important for sex allocation studies, since it
contains all three of the basic forms of sexuality found in animals" (Charnov, 1 982, p 20 1 ).
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35
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Source : MNHN. Paris
2
Environmental influences on endocrine systems
controlling reproduction in Polychaetes
Matthew G. BENTLEY , Jem BOYLE * & Allan A. PACEY **
Gatty Marine Laboratory, School of Biological and Medical Sciences
University of Si Andrews, St Andrews KYI 6 8LB. Scotland, U.K.
^present address: Clyde River Purification Board, East Kilbride
Glasgow G75 OLA, Scotland, U.K.
**presenl address: Observaloire Oceanologique, LIRA CNRS 671
B.P.28. 06230 Villefranche-sur-Mer, France
ABSTRACT
Photoperiod and/or temperature are known to influence gametogenesis and spawning in a number of polychaete species.
Information is now available on the nature of endocrine systems controlling gametogenesis and spawning in representatives of
several polychaete families. For relatively few species, however, is information available on the possible transduction of
environmental signals by the endocrine system (BENTLEY & PACEY, 1992). We report here on the effects of photoperiod and
temperature on the action of gonadotropin and spawning hormones in the polychaete Nephtys hombergii, and on the action of a
gonadotropin hormone in the polynoid Hannolhoe imbricata.
RESUME
Influences dcs factcurs externes sur les systemes endocrines controlant la reproduction chez les Polychetes
La photoperiode ct/ou la temperature agissent sur les processus de gametogenesc et de ponte chez un grand noinbre
d’especes de polychetes. Si les differents types de systemes endocrines qui controlcnt la gametogenese et la ponte sont bien
documents chez de nombreuses especes de polychetes. on a, par contre, ties peu d* informations sur les interactions existant
entre les facteurs du milieu et ces systemes endocrines (Bentley & PACEY, 1992). Nous rapportons ici les effets de la
photoperiode et la temperature sur Faction de Fhormone gonadotropique et de F hormone de ponte chez Nephtys hombergii
ainsi que sur Faction de Fhormone gonadotropique, qui a recemment ete decrite, chez Harrnothoe imbricata.
INTRODUCTION
Nephtys hombergii Savigny, 1818 (Nephtyidae) mid Harrnothoe imbricata L., 1769 (Polynoidae) arc both
iteroparous polychaetes witii an annual cycle of reproduction. Nephtys hombergii produces a single batch of
gametes which are spawned in late April or May in populations around the coast of northern England or Scotland
(Olive, 1978; Bentley et ai , 1984). Harrnothoe imbricata , in contrast, produces two consecutive batches of
gametes which are produced and spawned in quick succession in the spring (Daly, 1972, 1974; Garwood,
BENTLEY. M.G.. BOYLE, J. & A. A. PACEY, 1994. — Environmental influences on endocrine systems controlling
reproduction in Polychaetes. In: J.-C. Dauvin, L. Laitbif.r & D.J. REISH (Eds). Actes de la 4eme Conference internationale
des Polychetes. Mem. Mus. natn. Hist . not., 162 : 37-44. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
38
M.G. BEN TLEY. J. BOYLE & A. A. PACEY
1981). Gametogcnesis and spawning in N. hombergii arc controlled by two hormones, a gonadotropin hormone
and a spawning hormone (Olive, 1976: Olive & Bentley, 1980; Bentley & Olive, 1982; Olive & Lawrence,
1990) but to dale, evidence for the influence of any environmental factors on reproduction has been speculative. A
possible correlation was reported, for example, between insolation and daytime spawning of Nephtys caeca
(Bentley et a I ., 1984).
.Studies on Harmoihoe imbricata have revealed a sophisticated photoperiodic control of reproduction
(Garwood & Olive, 1978, 1982; Clark, 1988) but, only recently has a gonadotropin hormone been shown to
operate in the control of oogenesis (Olive et ai, 1990). The first cohort of oocytes requires appropriate
environmental input and endocrine support. The second oocyte cohort has been shown to develop autonomously,
apparently without environmental control.
The results we describe in this paper show that in Nephtys hombergii environmental conditions under which
animals are maintained may affect resorption and the onset of renewed gametogcnesis. Resorption has been shown
to be a common occurrence following spawning failure in this species (Olive et ai , 1981). We also show that
there is endocrine support of development of the second cohort of oocytes in Harmothoe imbricata even though
these do not require continued environmental support. In light of the fact that rapid growth of the first cohort of
oocytes occurs under gonadotropin support apparently associated with increasing photoperiod in the spring
(Clark, 1988) then observations that continued gonadotropin secretion occurs, without further environmental
stimulus, during the rapid vitellogenesis of the second oocyte cohort are as would be predicted.
MATERIALS AND METHODS
Collection and maintenance of specimens. — Specimens o (Nephtys hombergii were collected by digging in
sand at low water of spring tides from three sites: The Black Middens' in the estuary of the River Tyne, North-
East England; Kirkcolm, Wigtownshire, Scotland and from Fairlie Sands, Ayrshire, Scotland. Individuals were
maintained in the laboratory in groups of four in polyethylene containers containing 200ml sea water and sterilised
sand to a depth of 1cm.
Specimens of Harmoihoe imbricata were collected from beneath stones from the intertidal rocky shore at St.
Andrews and Kingsbams, Fife, Scotland. They were maintained individually in small glass jars containing 50ml
of seawater. An empty Patella vulgata shell was included to provide shelter. Animals which were not used within
one week of collection were fed weekly with pieces of Nereis diversicolor presented in forceps.
Light temperature regimes for laboratory maintenance of animals. — Animals were maintained in the
laboratory in Gallenkamp cooled incubators with timed light cycling under a variety of environmental conditions
as appropriate. The particular combinations of photoperiod and temperature were as follows:
Ambient conditions
Summer conditions of daylcngth and temperature 16L: 8D, 15°C
Winter conditions of daylcngth and temperature 8L: 16D, 5°C
Winter daylength/ summer temperature 8L: 16D, 15°C
Continuous illumination, 7°C.
Sampling of coelomic / ovarian oocytes. — Nephtys hombergii were anaesthetized in 0.07% 3-aminobenzoic
acid ethyl ester (Sigma Chemical Co.) in sea water. Samples of coelomic / ovarian oocytes were obtained by
puncturing the body wall in the inter-parapodia! region with a pulled micro-pipette which had been moistened
with filtered sea water. Examination was carried out on a Leitz Diaplan compound microscope using a x40
objective lens.
Extraction of brain homogenates and their preparation for use in tissue culture. — Supra-oesophageal ganglia
(“brains”) were removed from Nephtys hombergii anaesthetized as described above by making a transverse
incision in the dorsal body wall just posterior to the prostomium. Excised ganglia were kept on ice until
homogenization. Homogenization was carried out using an MSE Soniprep 150 ultrasonic disintegrator fitted with
a 9mm titanium steel probe. Crude extracts to be used for immediate bioassay or to be lyophilised for storage were
homogenised in bidistilled water, die aqueous supernatant was then used for injection or lyophilised and stored at
-20°C until used. Heat treated homogenate was prepared by suspending tubes containing crude homogenate in a
water bath at 100°C for I min followed by centrifugation in an MSE micro-centaur; the supernatant was then used
for subsequent addition to tissue culture wells.
Bioassay procedures for SI I in Nephtys. — The bioassay of extracts of supra-oesophageal ganglia for
Spawning Hormone (SH) activity was carried out as follows: gravid specimens of Nephtys hombergii were
Source :
ENVIRONMENTAL-ENDOCRINE INTERACTIONS IN POLYCHAETES
39
anaesthetized as above and injected with extract to be assayed or with filtered sea water as a control. Injections of
lOjil volume were made with a pulled, calibrated glass micropipette. The animals were then placed in an incubator
at 12°C and allowed to recover from the anaesthetic. The spawning response was measured using standard counts
of spawned gametes as described previously (Olive & Bentley, 1980).
Aseptic techniques. — Culture method. Animals were placed in streptomycin (2.5 mg/ml) and penicillin
(5000IU/ml) for a period of 24 h before dissection of ovaries for tissue culture. Animals were anaesthetized as
described above and ovaries were removed by excision of parapodia and lifting out of the ovaries with sterile
watchmaker's forceps. The ovaries from several females were pooled for use in amino-acid incorporation
experiments, where they were explained into culture wells of Cel-Cull 24-well plastic tissue culture plates
(Sterilin) each containing 2 ml of culture medium developed by BENTLEY & Olive (1982) for polychaete organ
culture.
Radio-isotope procedures. — Ten ovaries were added to each tissue culture well. L-[4,5-I I3] leucine
(Amersham International; specific activity 130-190 Ci.mM"1) (=*10,000 counts, well'1) ). The plates were placed in
sealed containers with moist tissue and kept in Gallenkamp cooled incubators at 15°C.
Harvesting of Cultures. — After culture periods of 96 h the ovaries and medium were removed from the wells
and centrifuged briefly in an MSE micro-centaur to sediment the ovaries. The medium was discarded, the ovaries
were resuspended in 1ml of 0.125 M Tris-HCl buffer at pH 8.5 and then homogenised in a Potter glass
homogeniser. An aliquot of 0.5 ml (50%) of the homogenate was stored for subsequent protein analysis using the
Bradford micro-protein determination method (Bradford, 1976). Three ml of ice-cold TCA was added to the
remaining 0.5 ml of homogenate mid this was left overnight at 4°C. The samples were centrifuged (at 2800g) in a
MSE Mistral 3000 centrifuge for 30 min at 4°C. The supernatant was removed and 1ml of 0.15M NaOH was
added to redissolve the proteins. The sample was divided into two, 3 ml Packard emulsifier scintillant 299 was
added mid the sample was then counted for 10 min on a Packard 2000 Tri-Carb liquid scintillation analyzer.
RESULTS
Observations on Nephtys gametogenesis. — Means and ranges of oocyte sizes in individuals which had been
maintained under conditions of: a) winter photoperiod (8L: 16D) and temperature (5°C); c) summer pliotoperiod
(16L:8D) and temperature (15°C); d) continuous illumination at 7°C; or b) recently collected from the field in
September 1990 are represented in Fig. 1. It can be seen that group a) which had been maintained under winter
conditions six of the 19 individuals had no vitellogenic eggs (diameter > 50 |im ) and the mean oocyte diameter
was <80 |im in eight of them. In contrast large vitellogenic eggs were found in virtually all worms in the other
three groups. These observations were made on individuals taken from a field population which did not spawn in
1990 and which at the commencement of the experiment had unspawned vitellogenic oocytes in the coelom. It is
quite clear that resorption of unspawned oocytes is accelerated in individuals maintained under conditions of
winter temperature and photoperiod. Maintenance under low temperature alone (d) does not have the same effect.
Observations on Nephtys spawning hormone activity. — The results of assay of spawning-inducing activity of
Nephtys hombergii supra-oesophageal ganglia taken from individuals which had been maintained under a range of
photoperiod/ temperature regimes for a period of 219 days (from prior to the winter solstice) are shown in Fig. 2.
Individuals injected with supra-oesophageal ganglion homogenate prepared from freshly collected animals show a
response typical of Nephtys hombergii , both in terms of the numbers of gametes released and the percentage of
individuals responding. The response is seen to be highly variable between individuals in that some individuals
spawn out almost completely whereas others spawn only partially. Groups injected with supra-oesophageal
ganglion homogenate prepared from individuals maintained under ambient conditions or under conditions of
winter photoperiod and temperature showed a response similar to that in individuals described above. Groups
injected with supra-oesophageal ganglion homogenate prepared from individuals maintained under summer
conditions, or under conditions of winter photoperiod and summer temperature showed a very low level of
response or no spawning at all.
Observations on gonadotropin hormone activity in Harmothoe imbricata. — Fig. 3 shows the results of amino
acid incorporation into ovaries of Harmothoe imbricata following organ culture for 96 h in the absence or
presence of brain homogenate. Incubation of ovaries of Harmothoe imbricata during the development of the first
cohort of oocytes (8 March 1991) in die presence of brain homogenate and heat treated brain homogenate, and in
medium (all containing H3 leucine) shows enhanced uptake of die amino acid (ANOVA F2,n = 13.04, p=0.001).
40
MG. BENTLEY, J. BOYLE & A. A. PACEY
There is no difference observed on die degree of incorporation between ovaries cultured with fresh or heat-treated
brain homogenate.
a: 8L:16D 5oC, September 1990
20-1
10 -
-o
- 1 - 1 - r - 1 - 1 - 1
0 40 80 120 160 200 240
Oocyte diameter pm (mean and range)
20
■5 10-
ci 16L:8D 15oC, September 1990
40 80 120 160 200 240
Oocyte diameter pm (mean and range)
20
io-
b: Field population September 1990
40
i —
120
160 200
— i
240
Oocyte diameter pm (mean and range)
20
« 10
?2
>
'•5
a
o
d: Constant illumination 7oC
September 1990
40 80 120 160 200 240
Oocyte diameter pm (mean and range)
FIG. 1. — Oocyte diameters (means and ranges) in individuals of Nephtys hdmbergii which have been maintaind for a period
of six months in the laboratory, and from the field in September 1990. The treatment groups were: a) maintained under a
8L:16D photoperiodic regime at 5°C, b) field collected animals, c) maintained under a 16L: 8D photoperiodic regime at
15°C. d) maintained under constant illumination at 7°C. It should be noted that, following spawning failure in the spring,
individuals collected from the field in September still posess vitellogenic oocytes in the coelom.
Incubation of ovaries during the development of the second cohort of oocytes (29 April 1991) in the presence
of brain homogenate prepared either from supra-ocsophageal ganglia excised during development of die first or
second oocyte cohorts also show enhanced uptake of die amino acid compared to the controls (ANOVA F2,i7 =
4.07, p=0.039) but there is no significant difference between die two brain homogenate treatments. This
demonstrates quite clearly the effect of gonadotropin hormGne on ovaries during die development of both the first
and second oocyte cohorts.
DISCUSSION
1 he reproductive cycle ol Nephtys hombergii is known to be controlled by two reproductive hormones (a
gonadotropin and a spawning hormone) which are supposed to be secreted in a cyclical manner during the annual
reproductive cycle (Olive, 1976, Olive & Bentley, 1980; Olive et cii, 1985). It has also been reported that
Source :
ENVIRONMENTAL-ENDOCRINE IN TERACTIONS IN POLYCHAETES
41
Nephtys hombergii is seen to undergo periodic spawning failure which may have an adaptive significance (Olive
et al., 1981). These spawning failures may occur in one of two ways: die production of a cohort of normal oocytes
which are not released as a result of failure to secrete spawning hormone, or (he premature resorption of gametes
prior to the breeding season. It has been proposed that spawning failure and oocyte resorption may occur in
response to ‘poor condition' of the individual (measured by energy levels in die soma) (Olive et al., 1985). The
endocrine system is the means by which environmental (and somatic energy level) information is likely to be
transduced. The results reported here on Neplitys hombergii suggest dial photoperiod may influence die rate of
oocyte resorption in unspawned oocytes and die onset of renewed gametogenesis. Short photoperiod appears to
accelerate this process. Temperature does not appear to exert a marked effect. Photoperiod provides an accurate
means of determining die timing of reproduction (BENTLEY & Pacey, 1992) whereas temperature cycles are less
predictable and are variable from year to year.
id
Z
z
£
<
a.
oo
TREATMENT
FIG. 2. — Spawning response in Nephtys hombergii injected with supra-oesophageal ganglion homogenate which had been
obtained from individuals which had been maintained in the laboratory for a period of 219 days (from prior to the winter
solstice) under: a) ambient photoperiod and temperature, b) a 8L:16D photoperiodic regime at 5°C, c) a 16L: 8D
photoperiodic regime at 15°C, d) a 8L:16D photoperiodic regime al 15°C, or which had been obtained from individuals
recently collected from the field. Control injected animals recieved a dose of lOpl of filtered seawater (solvent vehicle).
Standard counts were those as used by Olive and Bentley ( 1980).
Observations on the production of spawning hormone in Nephtys hombergii show a rather different pattern.
Prolonged exposure to short photoperiod alone is not sufficient to induce production of the hormone in the
supraoesophageal ganglion. Low temperature, in contrast appears to induce spawning hormone production.
Clearly production of spawning hormone is not critical in the timing of reproduction (only the tuning of release
plays a role in this respect), and temperature, therefore, may be an appropriate way of ensuring SH production.
Observations on the field spawning of Nephtys caeca (BENTLEY et al ., 1984), and Nephtys hombergii may be
similar, suggest that temperature may act as a ‘trigger' for spawning. Temperature has been shown to play a role in
controlling spawning of Nereidae (Goerke, 1984) in which there are temperature "windows" for the swarming of
species which are related to their geographical range. It is clear that die control of gametogenesis, hormone
production and readiness to spawn in N. hombergii is a complex process in which temperature and photoperiod
both appear to be involved.
There are few polychaete species in which both environmental and endocrine control of reproduction have
been demonstrated. FRANKE (1983) has demonstrated the transduction of environmental information by the
endocrine system of Typosyttis prolifera in an elegant series of experiments, but there arc at present no other well
42
M.G. BENTLEY. J. BOYLE & A. A. PACEY
documented cases. The reproductive cycle of Harmothoe imbricatci is controlled in a sophisticated manner by
environmental factors, of which photoperiod is the most important (Garwood & Olive, 1978, 1982; Garwood ,
a: March 8, 1991
***
***
□ Control
□ Brain Homogenate
□ Heat treated Brain homogenate
Treatment
FIG. 3. — Incubation of ovaries of Harmothoe imbricatci during: a) the development of the first cohort of oocytes (8 March
1991) in the presence of brain homogenate and heat treated brain homogenate, and in medium (all containing L-[4,5-H3]
leucine) and b) the development of the second cohort of oocytes (29 April 1991) in the presence of brain homogenate,
prepared either from supra-oesophageal ganglia excised during development of the first or second oocyte cohorts, and in
medium only.
1980; Clark, 1988). Photoperiod acts to promote gametogenesis and to prevent abortion of the developing first
cohort of oocytes (Clark, 1988), and this information is relayed to the developing oocytes, at least in part, by a
gonadotropin hormone (Olive et a! ., 1990). The second cohort of oocytes, which develops independently of
continued environmental input, we have demonstrated to be still under the gonadotropin hormone support. It may
Source :
ENVIRONMENTAL-ENDOCRINE INTERACTIONS IN POLYCHAETES
43
be Lliat once gonadotropin hormone secretion is switched on and the critical exposure to short days has been
passed, secretion of die gonadotropin hormone cotinues throughout the development of the two oocyte cohorts.
ACKNOWLEDGEMENTS
The authors are grateful to Dr. Marianne Ghyoot for checking the French abstract. This work was supported by
a Natural Environment Research Council grant (GR3/6841) to MGB.
REFERENCES
Bentley, M.G. & Pachy, A. A.. 1992. Physiological and environmental control of reproduction in polychaetes. Oceanogr.
Mar. Biol. Ann Rev., 30 : 443-481.
BENTLEY, M.G. & Olive, P.J.W., 1982. — An in vitro assay for gonadotrophic hormone in the Polychaetc Nephtys hombergii
Sav. (Nephtyidac). Gen. Comp. Endocrinol.. 47 : 467-474.
BENTLEY, M.G.. Olive, P.J.W., Garwood. P.R. & Wright, N.H., 1984. — The spawning and spawning mechanism of
Nephtys caeca (Fabricius. 1780) and Nephtys hombergi Savigny. 1818 (Annelida: Polychaeta). Sarsia , 69 : 63-68.
BRADFORD, M.M.. 1976. — A rapid and sensitive method for the quantification of microgram quantities of proteins using the
principle of protein dye binding. Anal. Biochem.. 72 : 248-254.
Clark. S., 1988. A two phase photoperiodic response controlling the annual gametogenic cycle in Harmothoe imbricata
(L.) (Polychaeta: Polynoidae). Invertebr. Reprod. Dew. 14 : 245-266.
Daly, J.M.. 1972. — The maturation and breeding biology of Harmothoe imbricata (L.) (Polychaeta: Polynoidae). Mar. Biol.
12 : 53-66.
Daly. J.M.. 1974. — Gametogenesis in Harmothoe imbricata (Polychaeta: Polynoidae). Mar. Biol.. 25 : 35-40.
FraNKE, H.-D., 1983. — Endocrine mechanisms mediating light-temperature effects on male reproductive activity in
Typosyllis pro life ra (Polychaeta. Syllidae). Wilhelm Roux1 Arch. Dev. Biol.. 192 : 95-102
Garwood. P.R.. 1980. The role of temperature and daylength in the control of the reproductive cycle of Harmothoe
imbricata (L.) (Polychaeta: Polynoidae). J. Exp. Mar. Biol. Ecol. , 47 : 35-53.
Garwood, P.R.. 1981. — Observations of the developing female germ cell in the polychaete Harmothoe imbricata (L.). Ini. J.
Invertebr. Reprod., 5 : 333-345.
GARWOOD. P.R. & Olive. P.J.W., 1978. — Environmental control of reproduction in the polychaetes Eulalia viridis and
Harmothoe imbricata. In: D.S. McLuSKY & A.J. BERRY (eds). Physiology and Behaviour of Marine Organisms.
Pergamon Press, Oxford. New York : 331-339.
Garwood. P.R. & Olive, P.J.W., 1982. The influence of photoperiod on oocyte growth and its role in the control of the
reproductive cycle of the polychaete Harmothoe imbricata (L.). Int. J. Invertebr. Reprod., 5 : 161-165.
Goerke, H.,1984. — Temperature dependence of swarming in North Sea Ncreidac. In: A. FISCHER & II. -D. PFANNENSTIEL
(eds), Polychaetc Reproduction. Fortschr. Zool., 29 : 39-44.
Olive, P.J.W. 1976. — Evidence for a previously undescribed spawning hormone in Nephtys hombergii (Annelida:
Polychaeta). Gen comp. Endocrinol., 28 : 454-460.
Olive, P.J.W.. 1978. Reproduction and annual gametogenic cycle in Nephtys hombergii and N. caeca (Polychaeta:
Nephtyidae). Mar. Biol.. 46: 83-90.
Olive. P.J.W. & BENTLEY, M.G., 1980. — Hormonal control of oogenesis, ovulation and spawning in the annual reproductive
cycle of the polychaete Nephtys hombergii Sav. (Nephtyidae). Int. J. Invertebr. reprod. Dew, 2 : 205-221.
Olive. P.J.W.. BENTLEY. M.G.. Wright. N.M. & MORGAN. P.J., 1985. — Reproductive energetics, endocrinology and
population dynamics of Nephtys caeca and N. hombergi. Mar. Biol., 88: 235-246.
Olive. P.J.W.. Clark, S. & Lawrence, A., 1990. Global Warming and Seasonal Reproduction: Perception and
Transduction of Environmental Information. In: M. IIOSHI & O. Yamashita (eds). Advances in Invertebrate
Reproduction. Volume 5. Elsevier. Amsterdam, pp. 265-270.
Olive. P.J.W., Garwood. P.R. & Bentley. M.G., 1981. Oosorption and reproductive failure in Polychaeta in relation to
their reproductive strategy. Bull. Soc. Zool. Fr., 106 : 263-268.
OLIVE, P.J.W. & Lawrence, A.. 1990. Gonadotrophic hormone in Nephtyidae (Polychaeta: Annelida): Stimulation of
ovarian protein synthesis. Invertebr. Reprod. Dev., 18: 189-196.
Source : MNHN. Pahs
3
Morphometric analysis of cellular specification
in Platynereis and Pomatoceros embryogenesis
(Annelida, Polychaeta)
Adriaan W.C. DORRESTEIJN & Craig Marc LUETJENS
Zoologisches Institut (Abteilung 1) der Universitat Mainz
SaarstraBe 21, D-55099 Mainz, Germany
ABSTRACT
Despite differences in size and yolk content, the eggs of two sibling species. Platynereis dumerilii and
P. massiliensis , show the same asymmetrical mode of cytoplasmic segregation. The largest part of the yolk-free
cytoplasm is shunted into the D-quadrant alter second cleavage. The specific cleavage behavior of the D-cell-line
suggests a causal relation between cytoplasmic specification, speed of cell cycles and determination. We have expanded
our morphometric analysis to the development of Pomatoceros triqueter, a polychaete with equal cleavage. However, we
show that small though significant size difference between the quadrants may foreshadow the future dorsoventral polarity
of this embryo. The largest quadrant cleaves asynchronously with respect to the other three quadrants. As in Platynereis .
the speed of cell cycles of blastomeres are positively correlated with the volume of cytoplasm.
RESUME
Analyse morphometrique de specification des cellules de Platynereis et Pomatoceros (Anne-
lide Polychete)
Malgre dcs differences de taille et de contenu de vitellus. les oeufs des deux espdees proches. Platynereis dumerilii et
P. massiliensis . montrent le meme mode de diversification cytoplasmique. La majeure partie du cytoplasme clair et sans
vitellus est repartie dans le quadrant D apres le deuxieme clivage. Le comportement specifique de clivage de la lignee
cellulairc D suggere une relation entre la specification cytoplasmique, la vitesse des cycles cellulaires et la determination.
Nous avons elargi 1’ analyse au developpement de Pomatoceros triqueter. polychete a segmentation egale. Pourtant nous
pouvons montrer que des differences minimes bien que significatives de taille entre les quadrants seraient indicatrices de la
future polarite dorsoventrale de cet embryon. Le quadrant le plus large se divise asynchroniquement par rapport aux trois
autres. Comme chez Platynereis. les vitesses des cycles cellulaires sont reliees positivement au volume du cytoplasme.
INTRODUCTION
Embryogenesis in polychactous annelids is reg<uded as a textbook example of determinative development. In
many such eggs, structural animal-vegetal polarity is apparent before fertilization and foreshadows the future
DoRRESTEIJN. A. W.C. & C.M. LUETJENS. 1994. Morphometric analysis of cellular specification in Platynereis and
Pomatoceros embryogenesis (Annelida. Polychaeta). In: J.-C. Dauvin, L. Laubier & D.J. REISH (Eds), Aclcs de la 4eme
Conference internationale des Polychetes. Mem. Mus. natn. Hist. nat.. 162 : 45-50. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
46
A.W.C. DORRESTHIJN & CM. LUETJENS
antero-posterior axis of die trochophore larva. Even in seemingly apolar eggs this first body-axis is sel up shortly
after fertilization (KLUGE, 1991). Apart from the emergence of polar bodies which mark the animal pole, polarity
is also manifested by ooplasmic segregation leading to a polar distribution of cytoplasmic components.
In nereids, the second body-axis, i.e. the dorsoventral axis, is believed to be set up at first cleavage (Wilson,
1892). In Platyn e re is dumeri lii, the first cleavage produces two daughter blastomeres of unequal size: die small AB
blastomere (27% of the total egg volume) and the larger CD blastomere. Dorresteijn (1990) was able to show
that the cytoplasmic composition of these two cells differs as well. Volumetric analysis revealed that
approximately 80% of die yolk-free cytoplasm, which accumulates at the animal pole prior to first cleavage, is
allocated to the large CD blastomere, despite the fact that diis blastomere includes only 73% of die total egg
volume. Experiments in which we have equalized diese volumetric proportions led to a duplication of dorsoventral
polarity, and of the trunk structures of the young worm (DORRESTEIJN, Bornewasser & FISCHER, 1987). These
data thus support die idea dial the establishment of die dorsoventral axis depends on the differential distribution of
bodi volume and cytoplasmic contents between die first two blastomeres.
In die present paper, we describe die developmental principles encountered in die unequally cleaving embryos
of two sibling species of Platynereis and in the equally cleaving embryo of the scrpulid Pomatoceros triqueter. Our
results indicate dial die creation of cytoplasmic asymmetry among the four embryonic quadrants may set up
dorsoventral polarity even in "equally" cleaving polychaetes. The data also suggest a correlation between
cytoplasmic distribution and cell cycle duration in individual blastomeres.
MATERIALS AND METHODS
Platynereis dumerilii and Platynereis massiliensis were kept in laboratory cultures (Hauenschild & Fischer,
1969) at 18 C. The serpulid, Pomatoceros triqueter , was collected from the seabed round Helgoland. For
Platynereis dumerilii, die mode of fertilization was previously described by Dorresteijn (1990). Ferdlized eggs
from P. massiliensis were collected from brood lubes in culture dishes. To induce spawning in Pomatoceros die
calcareous tubes in which the animals live were opened with sturdy tweezers at the narrow, rear end. Subsequent
agitation of the animal's tentacles made diem crawl backwards by which diey exposed themselves at the artificial
hatch in the tube. Males (with pale abdomen) and females (with red abdomen) were pul into separate bowls of
seawater and started spawning spontaneously. The eggs were washed in seawater several times and were then
fertilized with diluted sperm.
A careful estimate of cell cycle duration of individual blastomeres was achieved by evaluating several video-
time-lapse recordings of die development (at 18 °C) of each of the three polychaetous species.
Procedures to collect morphometric data from serial sections (1 pm) were as described by Schneider, Fischer
& Dorresteijn (1992). For the small Pomatoceros embryos, however, we digitized every second 1 pm section in
serial sections.
RESULTS AND DISCUSSION
An intricate combination of pre-cleavage cytoplasmic segregation and unequal first cleavage during normal
development of Platynereis dumerilii creates daughter-blastomeres which differ both in size and in cytoplasmic
composition. This seems an essential initial step to create and propagate cellular diversity in die nereid embryo. At
second cleavage, die small AB blastomere divides equally and there is no sign of cytoplasmic diversification. The
huge CD blastomere which contains the bulk of yolk-free cytoplasm (see introduction), however, cleaves
unequally and die largest pari of this yolk-free cytoplasm is shunted into die D-quadrant. As a result of this
cleavage strategy, the D-cell obtains 60 % of the yolk-free cytoplasm although it includes only 51% of the total
egg volume. Again, the cleavage introduces inequality in blastomere size and simultaneously regulates the
cytoplasmic composition ot the daughter blastomeres with a disproportional increase of yolk-free cytoplasm in the
largest cell, the D-blastomere. The cleavage pattern of die D-quadrant differs from that of the odier quadrants. Two
descendants of the D-cell-line, the somatoblasts 2d and 4d, are formed at fourdi and sixth cleavage, respectively.
Bodi somatoblasts are exceptionally large cells and contain yolk-free cytoplasm almost exclusively. Dorresteijn
(1990) has shown a positive correlation between die amount of yolk-free cytoplasm tuid die speed of cell cycles for
all blastomeres (Fig. 1 ). As a result of die allocadon of yolk-free cytoplasm, these D-quadrant-derived cells, 2d and
4d, proliferate much more rapidly than comparable cells of odier quadrants. The relatively long initial cell cycle of
Source :
PLATYNERE/S AND POMATOCEROS EM B R Y OGEN E SIS
47
2d compared lo its precursor cell ID and its progeny 2d1 and 2d11, despite the fact that it obtained a large amount
of yolk-free cytoplasm, seems to be exceptional. DORRESTE1JN (1990) proposes that the interval between fourth
and fifth cleavage may be elongated due to cellular interactions which imprint dorsoventral polarity at the 16-cell
stage.
30%
e
15
c
y
t
o
P10
l
•CD
•0
•10
•2d
•2d1
•2d"
•MB
•L-.
• •* |1a” , 1b”
-4-«§
M •
•2d 2
•2c’
& -
— «3d
0
20
40
60 80 100
Cell cycle duration (min)
120
140
Fig. 1. — The amount of yolk-free cytoplasm in blastomeres of successive cleavage stages of Platynereis dunierilii is
positively correlated with the rale of cell division. This diagram shows this correlation for the individual
blastomeres. We have labeled some of the data points to show that CD and D-quadrant-derived cells proliferate more
rapidly than other cells. However, cell cycles last longer after cells (even in the D-quadrant. e.g. 2d2 and 3d) have lost
most of their clear cytoplasm.
Recently, we were able to show experimentally that die cleavage characteristics normal to a D-quadrant can
also be observed in more than one quadrant if such quadrants contain sufficient yolk-free cytoplasm (Dorresteijn
& Eich, 1991).
The eggs of the sibling species, P. mcissiliensis , are structurally polar from the start and extremely yolky.
They have more than 10 times the volume and develop nearly four times slower than the eggs of P. dunierilii.
Should the mode of cytoplasmic diversification found and documented by morphometric data for P. dunierilii be
essential for determination of blastomeres, one would expect the development of this closely related species to
follow essentially die same mode, even though the initial properties of such eggs arc not the same. We have
compared our data (SCHNEIDER, Fischer & DORRESTEIJN, 1992) widi early light microscope observations on the
development of this species (WISTINGHAUSEN. 1891), which was dicn called the "nereidogenic form of Nereis
dunierilii" . Unfortunately, W failed to observe certain cleavages which makes die comparison of his proposed cell
lineage tree widi our cell-lineage results impossible.
Our comparative analysis of early development gave interesting insights into the way blastomeres become
eytoplasmically diverse. The difference in size between the AB and CD blastomeres of P. mcissiliensis is less than
in P. dunierilii. The CD blastomere of P. mcissiliensis measures 65 % of the total egg volume, yet contains
approximately 73 % of die total amount of yolk-free cytoplasm. Thus, cytoplasmic diversification at first cleavage
is a feature common to both species. Unlike the development of P. dunierilii , second cleavage of P. massiliensis
is unequal in both blastomeres. The allocation of die yolk-free cytoplasm to the daughter blastomeres of AB is
48
A.W.C. DORRESTEIJN & C.M. LUETJENS
proportional to tlie volumes of these cells. Although A- and B-blastomeres differ in size, there is no cytoplasmic
diversification between these blastomeres. The cleavage in CD, however, allocates the yolk-free cytoplasm in
proportions deviating from Hie relative volumes of Die daughter cells with die largest amount (54 % of the total)
ending up in the D-blastomere, which represents only 45 % of die total egg volume. Again, the cytoplasmic
diversification of the D-quadranl is accomplished by both sibling species. The cytoplasmic specification or the D-
cell-line is followed by a specific cleavage behavior differing in many respects from the other three quadrants. As
in P. clumerilii , the somatoblasts 2d and 4d are large cells, receive almost exclusively yolk-free cytoplasm and
proliferate more rapidly. Although cell cycles are nearly four times longer in P. massiliensis, a time scale
transformation (Pig. 3 from SCHNEIDER, FISCHER & DORRESTEIJN, 1992) shows that the asymmetries in the
sequence of divisions among both species are similar in all cell lines. In the same paper, the developmental
similarity has been confirmed by reconstructions of embryos and shows dial the asynchronies of blastomcre
proliferation, a result of differing cell cycle durations, can, with a few exceptions, be correlated widi die allotments
of yolk-free cytoplasm to the blastomeres of P. massiliensis as well. The stringency of cytoplasmic allocation in
die two species suggests a causal relation between cytoplasmic specification and determination of die D-quadrani.
We have expanded our morphometric analyses onto die development of the serpulid Pomatoceros iriqueter. The
small (60-70 pm in diameter) egg of this polychaete contains only small amounts of yolk. The essentials of
development were described by von DRASCHE (1884) and revised by Groepler ( 1986). According to these authors,
die first and second cleavage are equal and the quadrants develop in radial symmetry. Thus, although differences in
size and composition of the quadrants allow us to identify die quadrants in nereids, identification of quadrants
seems impossible at early stages of Pomatoceros.
However, our own studies of die development of diis small serpulid, partially reviewed by DORRESTEIJN &
Fischer (1988) showed that die blastomeres do not cleave synchronously. Even die second cleavage is slightly
asynchronous in the first two cells, although the interval is less than a minute. Cleavage asynchrony is maintained
60 %t
50
B
l
a
S 40
t
o
m
m
e
10 -
0 --
0
10
•CD
•AB
•0
«A,B,C
•ID
•••|1a-1d
* w« . I
• lid22- id22 | *1."- Id" J,aj. ^d 2
30 40 50 60 70 80
Cell cycle duration (min)
FIG. 2. — In Pomatoceros iriqueter , blastomeres of successive cleavage stages which were studied up the 32-cell-stage
show a positive correlation between the amount of cytoplasm and the rate of cell division. Since the yolk is
distributed homogeneously within the cytoplasm, the blastomere volumes can be used as a measure of the amount of
yolk-free cytoplasm.
Source : MNHN. Paris
PLATYNEREIS AND POMATOCEROS EMBRYOGENESIS
49
and becomes more pronounced at later stages, especially among the macromeres and the different quartets of cells
along the animal-vegetal axis. Morphometry of sectioned and reconstructed embryos shows small, yet statistically
significant size differences between the blastomeres as early as at the two cell stage. The largest cell, which we
shall call CD (according to the rules for the majority of unequally cleaving spiralians), is larger than AB by 3.5%
(SD=1.3%; n=9) of the total egg volume. At the four cell stage, one of the daughter cells of CD is larger than the
other daughter cell by little more than 2%, and larger than the daughter cells of AB by 3% (SD=1.9%; n=9). The
size differences are maintained in the vegetal macromeres, but eliminated in the quartets of micromeres which are
formed towards the animal pole during the third and subsequent cleavages.
Light microscope investigations of living embryos and morphometric analysis of serially sectioned embryos
resulted in a clear and positive correlation between the sizes of individual blastomeres and the rate of cell division.
From the diagram Fig. 2 it becomes clear that once the blastomeres grow smaller cell cycle duration increases. The
first quartet of micromeres (la- Id) divides nearly equally and the daughter cells, la’-ld1, have cell cycles which tire
nearly 20 min longer than those of the mother cell. Since the yolk remains distributed homogeneously throughout
the cytoplasm of the blastomeres, blastomcrc size must be proportional to the content of yolk-free cytoplasm in
the blastomeres, and we can postulate the same correlation between the amount of yolk-free cytoplasm and the rate
of cell division that we had previously found for P. dumerilii. This supports the idea that the small though
significant size differences between the cells of the Pomaioceros 4-cell stage may cause the asynchronous
development of its quadrants, which is reinforced in the macromeres at later stages. This asynchrony in the
development of otherwise equivalent blastomeres introduces a polarity axis perpendicular to the preexisting animal-
vegetal polarity which may well coincide with a dorsovenual axis which, however, has not yet been rigorously
demonstrated in Pomatoceros embryos. For this reason we are studying the development of Pomaioceros beyond
the stages we have investigated so far and focussing on the development of mesodermal stem cells which is a
developmental aspect limited to the D-quadrant only. Should both mesoderm development and precocious cleavage
in one of the quadrants be correlated aspects of development, setting up of cleavage asynchronies might prove an
important factor to acquire blastomeres with different developmental fate.
ACKNOWLEDGEMENTS
The careful maintenance of the animal stocks by Mr.A. Heinen is gratefully acknowledged. The supply of the
animals was made possible by the Laboratoire Arago (Banyuls-sur-Mer, France) and the Biologische Anstalt
Helgoland (Helgoland, Germany). The collection of data for this paper would have been impossible without the
financial support from the Deutsche Forschungsgemeinschaft, Bonn (grant Do 339/1-2).
REFERENCES
DORRESTEIJN, A.W.C.. 1990. Quantitative analysis of cellular differentiation during early embryogenesis of
Platynereis dumerilii. Wilhelm Roux1 Arch. Dev. Biol., 199 : 14-30.
DORRESTEIJN, A.W.C.. Bornewasser, H. & FISCHER, A., 1987. A correlative study of experimentally changed first
cleavage and Janus development in the trunk of Platynereis dumerilii (Annelida, Polychaeta). Wilhelm Roux ' Arch.
Dev. Biol., 196 : 51-58.
DORRESTEIJN, A.W.C. & ElCH. P.. 1991. — Experimental change of cytoplasmic composition can convert determination
of blastomeres in Platynereis dumerilii (Annelida, Polychaeta). Wilhelm Roux' Arch. Dev. Biol., 200 : 342-351.
DORRESTEIJN, A.W.C., FISCHER, A.. 1988. The process of early development. In: W. Westheidk & CO. HERMANS (eds),
T he Ullrastruciure of Polychaetes. Microfauna Marina , Gustav Fischer, Stuttgart, 4 : 335-352.
DRASCHE, R. von. 1884. Entwicklung von Pomatoceros triqueter L. Beit rage zur Entwicklung der Polychaeten, Heft
1 : 1-10, Wien, published privately.
Groepler, W.. 1986. — Die Entwicklung bei Pomatoceros triqueter L. (Polychaeta. Serpulidae) vom befruchteten Ei bis
zur schwimmenden Blaslula. Zool. Beilr. N. F.. 29 : 157-172.
11 AUENSC1IILD, C. & FISCHER, a., 1969. Platynereis dumerilii. Mikroskopische Anatomie. Fortpflanzung.
Entwicklung. Grofies Zoologisches Praktikum, Heft 10b. Gustav Fischer Verlag. Stuttgart, 1-55.
50
A.W.C. DORRESTEIJN & C.MV LIJETJENS
Kluge, B. 1991 - Cytologische Analyse der friihesien Entu'icklungsvorgange bei Platynereis dumerilii (Annelida,
Polychaeta). Thesis, University of Mainz, 245 pp.
SCHNEIDER. S.. FISCHER, A. & DORRESTEIJN, A.W.C., 1992. — A morphometric comparison of dissimilar early
development in sibling species of Platynereis (Annelida. Polychaeta). Wilhelm Roux’ Arch. Dev. Biol., 201 : 243-
256
Wilson. E.B.. 1892. The cell-lineage of Nereis : A contribution to the cytogeny of the annelid body. J. Morph., 6 :
361-480.
WlSTINGHAUSEN, C. von. 1891. — IJntersuchungen iiber die Entwicklung von Nereis Dumerilii. Ein Beitrag zur
Entwicklungsgeschichte der Polychaeten. Mitt. Zool. Star. Neaped, 10 : 41-74.
Source : MNHN. Paris
4
Observations on reproduction and growth of Sabella
spallanzanii (Polychaeta, Sabellidae)
in the Mediterranean Sea
Adriana GIANGRANDE & Angela PETRAROLl
Diparlimenlo di Biologia
University di Lecce
73100 Lecce. Italy
ABSTRACT
A year of observations on a population of Sabella spallanzanii is reported. In situ measurements of tube length and
correlation of this parameter to other variables such as worm length and biomass gave indications on growth-rate.
Reproduction was followed by monthly samples and examination of gonad maturation. Sex ratio and minimal size at
reproduction were also investigated. In the Mediterranean Sea S. spallanzanii showed a fast growth-rate and reproduced
during February. Oogenesis is of extraovarian type and eggs reach 250 pm. The presence of protandric hermaphroditism
is indicated.
RESUME
Observations sur la reproduction et la croissance de Sabella spallanzanii (Polychaeta,
Sabellidae) en Meditcrranee
Des observations sur la reproduction d'unc population de Sabella spallanzanii ont ctd faites pendant une annee. La
longueur des tubes a ete evaluee par des mesures directes des individus dans leur habitat naturel. Une correlation entre la
longueur de tube, la longueur du ver et la biomassc a pu etre demontree. A partir dc ccs correlations, il est possible d'avoir
une indication sur la croissance du ver. Des 6chantillons ont etc recoltes tous les mois pour suivre la reproduction des
individus. La taille minimale des vers a la reproduction et leur sex-ratio ont <$t 6 calcules. La ponte de S. spallanzanii a
lieu au cours de 1’hiver en Meditcrranee. La taille ovocytaire maximale observde a etc de 250 pm. Neanmoins les premiers
stades de la gametogenese n'ont pas ete observes et des observations complementaires sont necessaires. L'espece
presente un hermaphroditisme proterandrique.
INTRODUCTION
Sabella spallanzanii (Gmelin, 1791) is one of the most "popular" Mediterranean polychaetes. It has been used
as an experimental animal in numerous studies, but almost always under die generic name of Spirographis.
Recently PERKINS and KNIGHT-JONES (1991) synonymized Spirographis spallanzanii Viviani with Sabella
Giangrande, a. & A. PETRAROLL 1994. Observations on reproduction and growth of Sabella spallanzanii
(Polychaeta, Sabellidae) in the Mediterranean Sea. In: J.-C. DAUVIN, L. LaUBIER & D.J. REISH (Eds). Actes de la 4eme
Conference internationale des Polychetes. Mem. Mus. natn. Hist. nat.. 162 : 51-56. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
52
A. GIANGRANDE & A. PETRAROU
penicillus Linnaeus, but suggested to suppress penicillus and other synonyms to stabilize die name Spallanzani i.
They pointed out that the correct name for the species, penicillus , has frequently been used incorrectly for
Sabella pavonina Savigny typical of northern Europe.
Sabella spallanzanii is common along the Italian coast. It can be found in the open sea from 1 to 30 m depth,
as well as in shallow hard bottom areas of harbours, where it reaches high densities. Probably the open sea and die
harbour forms belong to different ecotypes because their behaviour and resistance under laboratory conditions are
different
Despite its wide distribution, and its frequent use in physiological studies (Ivanov, 1908; Fox. 1938;
KlORTSIS & Moraitou, 1965; PARRINELLO & RiNDONE, 1981), its reproduction and life-cycle are poorly known
(McEuen et al.y 1983).
The role of coelomocytes in the maturation of germinal products in some specimens from Naples, which
surely belonged to Sabella spallanzanii. was studied by Dales (1961). While the electron microscopical
investigation on sperm of the species incorrectly referred as Sabella penicillum by Graebner and Kryvi (1973),
should probably be referred to Sabella pavonina.
The present paper deals with a year of observations on in situ growth mid reproduction of a Mediterranean
harbour population of Sabella spallanzanii.
MATERIALS AND METHODS
The study was conducted at the Mai* Grande of Taranto (Gulf of Taranto, Ionian Sea) along an artificial, vertical
cliff. The individuals o (Sabella spallanzanii were distributed in patches. One group measured 2 m deep and 9 m
wide, and was chosen to follow individual growth. In situ measurements of tube length were done by Scuba divers
for about one year. Tubes were measured within an area of 400 cm2, using a plastic square to delimitate the
surface. The tube length was correlated with other features of the worm.
Biomass was estimated as dry weight by drying individuals at 65°C for 24 h. Various sized specimens were
collected monthly from the dense patch under study and from adjacent zones. Size at maturation and sex ratio were
determined. Coelomic fluid was analyzed in the laboratory to examine for sexual maturation.
Specimens were fixed in 5 % glutaraldehyde buffered to pH 7.4 and post-fixed for one hour in 4 % osmium
tetroxide for histological studies. For light microscopy, 1 pm thick sections were cut with a glass knife. Thin
sections were cut on an ultramicrotome with a diamond knife for electron microscopy
The temperature cycle was typical of Mediterranean confined environments with a range of 1 1 °-29 °C. Salinity
values were stable at approximately 38 P.S.U.
RESULTS
Density, growth and biometry. Individuals of Sabella spallanzanii were located within a suspension
feeder community typical of Mediterranean eutrophic zones such as harbours (TURSI et al ., 1985). At the
beginning of the study in May 1991. only small individuals were present within the patch, and the density was
about 300 ind. nr2. The mean tube length in July 1991 was 10 cm (Fig. la). In April 1992 it was 18 cm, and in
August 1992 it reached 20 cm in length (Fig lb), with a density of about 150 ind. m'2.
The tube length was correlated with the length of the worm (Fig. 2a), biomass (Fig. 2b) and die number of
setigers (Fig. 2c). Biomass was estimated at 60 g. nr2, and 75 g. nr2 in July 1991 and August 1992,
respectively.
The crown of Sabella spallanzanii is asymmetric, with one involute lobe having an arrangement of spiralled
radioles, but spiralization is absent in small individuals (KNIGHT-JONES et al., 1991). Correlation of number of
spirals with length showed dial worms up to 9 cm in lengdi do not show any spiralling, whereas large specimens
from 30 to 40 cm in length have up to 4 secondary spirals (Fig. 2d). The ratio of body lengdi to crown increases
widi increasing body length, from 1.5 to 4.7, as observed for odier species (Giangrande, 1991).
REPRODUCTION
As observed by Dales (1961), germinal products in sexually mature specimens are found in the coelomic
cavity. No germinal products were observed in die coelom from May to July 1991. The content of die coelom was
Source : MNHN. Paris
REPRODUCTION AND GROWTH OF SAB ELIA SPALLANZANII
53
bright orange or brown and had a rich creamy consistency due to the presence of large coelomocytes. These cells
measure up to 70 jam in diameter. The peritoneum appeared hypertrophic in July, 1991. The early stages of
tub# length cm
FlG. 1. — Sabella spallanzanii. a: Frequency histograms of tube length in July, 1991; b: Frequency histograms of tube
length in August. 1992.
germinal products were probably present in August and September, but samples relative to this period were not
obtained. Germinal products were well developed in October, 1991, when eggs measured about 100 pm. They
reached about 200 pm in December, 1991. and males contained spermatids predominantly at an early stage of
maturation. Eggs had completed vitellogenesis and measured 250 pm in January, 1992. (Fig. 3a). and ripe
spermatozoa (Fig. 3b-c) together with late spermatid stages were present in the males. Spawning occurred in
February. Some females still retained a few eggs surrounded by a large number of coelomocytes in March. The
coelom of the worms was once again full of coelomocytes in April, 1992, and no germinal products were present.
As observed by Dales (1961 ) the quantity of coelomocytes decreased as oocytes matured.
54
A. GIANGRANDE & A. PETRAROLI
SEX RATIO
File minimal size at maturation was computed as 15 cm in length. Specimens from 15 to 20 cm long were all
males ; females occurred only in specimens greater than 20 cm long. The sex ratio was of 1 : 1 in individuals
from 25 to 30 cm. However, males represented more than 80% of the reproductive population when all sized worm
weie considered.
total worm length cm total worm length cm
Fig. 2. — Sabello spallanzanii. a: Correlation between tube length and total worm length; b: Correlation between worm
length and biomass (Dry weight); c: Correlation between worm length and number of setigers; d: Correlation between
worm length and number of spirals of the branchial crown.
Individuals from die patch under observation with tubes measuring about 15 cm in length were all males.
During the period of study no females were present within this patch. Females were found among larger
individuals collected from adjacent zones.
DISCUSSION AND CONCLUSION
Sabella spallanzanii is characterized by a rapid growth rate, l ube length doubled in 10 months. In the
laboratory, it has been reared using many different food sources, and it can be hypothesized that it can feed also on
particulate organic matter. Size distribution within the patch suggested that it could be the product of a single
recruitment episode. The biomass computed per square meter was quite large, even thougth mortality seemed to be
very high during the period of observation, since the density decreased from 300 to 150 ind. nr2.
Spiralization of the radioles represents a growth strategy in large-sized sabcllids. In this way they can obtain an
efficient respiratory and feeding surface without elongation of die crown, diminishing the risk from predation.
Correlation of die number of spirals with body length is important taxonomically, since one of die features used
to distinguish Spirographis from Sabella was die presence of spiralization in the crown.
Reproduction in Sabella spallanzanii seems to be synchronized among individuals. According to Dales
(1961), spawning occurs in winter. 1 Iowever, samples relative to diis first year were not adequate to investigate die
entire gametogenic cycle, especially concerning the appearance of die early stages of germinal development. Data
of the present work suggests that gametogenesis begins in summer. During die gametogenesis, coelomocytes were
observed to decrease in number, especially in females. After spawning die number of coelomocytes increases
Source :
REPRODUCTION AND GROWTH OF SABELLA SPALLANZANI!
55
rapidly and by spring fill the coelomic cavity. Dales (1961) reported that coelomic cells are organized as storage
Fig. 3. — Sabella spallanzanii. a: Electron micrograph of a section through cortex of ripe egg. showing numerous yolk
bodies, magnification 91.000; b-c: Electron micrograph through heads of ripe spermatozoa, magnification 52.000.
centres for the maturation of gametes. Coelomocytes are derived from die peritoneum as small actively phagocytic
cells. Large coelomocytes eventually rupture and liberate their inclusions into the coelomic fluid to be Liken up by
Source
56
A. GIANGRANDE & A. PETRAROLI
younger cells or by gametes. The oogenesis therefore is of the extraovarian type and is classified by Eckelbarger
(1983) as "with numerous amoebocytcs".
The mature egg diameter is 250 pm ; therefore a lecithotrophic development can be hypothesized. Even
thougth the egg diameter does not agree with that of other sabellids having a broadcaster reproductive pattern
(McEUEN et al. , 1983). The structure of spermatozoa is of die primitive type, adapted for external fertilization. It
is of the ect-aquasperm type, which is die most common type among polychaetes. However, die sabellid ect-
aquasperm type was classified by Jamieson & Rouse (1989) as nco-aquasperm, hypothesizing in some sabellids a
re -evolution of ect-acquasperm from ent-aquasperm type. The sperm morphology is very similar to diat described
for Sabella penicillum (GRAEBNER & Kryvi, 1973), but diis is probably a different species from Sabella
spallcinzanii.
Due to die problems existing in die taxonomy of Sabella spallanzanii (Perkins & Knjght-Jones, 1991),
some difficulties arise in comparing present data to odier previous works. For example, Sabella penicillus is
reported to be a dioecious species (McEuen, et al., 1983), but current data, i.e. deviation in sex ratio from 1 : 1
and size of females, supports die hypothesis for the presence in Sabella spallanzanii of a protandric
hermaphroditism, Probably die individuals examined by Dales (1961) were of large size and this led the author to
consider the species as gonochoric. Further investigations are needed to confirm this hypodiesis.
REFERENCES
DALES, P.R.. 1961. — The coelomic and peritoneal cell systems of some Sabellid Polychaetes. Q. J. Microscop. Sci.,
102 : 327-346.
Eckelbarger, K.J.. 1983. — Evolutionary radiation in polychaete ovaries and vitellogenic mechanisms: their possible
role in life-history patterns. Can. J. Zool., 61 : 487-504.
Fox, M.H., 1938. — On the blood circulation and metabolism of sabellids. Proc. Royal Soc. (B). 125 : 554-569.
GIANGRANDE. A.. 1991. Behaviour, irrigation and respiration in Eudistylia vancouveri (Polychaeta. Sabellidae). J.
mar. biol. Ass. U.K.. 71 : 27-35.
GRAEBNER. I. & Kryvi. H.. 1973. The spermiogenesis and mature sperm of Sabella penicillum (Polychaeta). An
electron microscopical investigation. Norw. J. Zool., 21 : 211-226.
Ivanov. P., 1908. Regeneration des vorderen, und des hinleren Korperendes bei Spirographis spallanzanii. Viv.
Zeitschrift f wissensch. zoologie., 91 : 510-558.
Jamieson, B.G.M. & ROUSE, W., 1989. — The spermatozoa of the Polychaeta (Annelida): an ultrastructural review. Biol.
Rev.. 64 : 93-157.
KIORTSIS. V. & Moraitou M.. 1965. Factors of regeneration in Spirographis spallanzanii. In: V. KlORTSIS & II.A.L..
Trampush (cds). Regeneration in Animals and related problems. North Holland Publ., Co., Amsterdam : 250-261.
KNIGHT- JONES, P., Knight-JONES, W.. & Ergen, Z., 1991. — Sabelliform polychaetes, mostly from Turkey's Aegean
coast. J. Nat. Hist.. 25 : 837-858.
McEuen. F.S.. Wu, B.L., & CHI A, F.S.. 1983. — Reproduction and development of Sabella media, a sabellid polychaete
with extratubular brooding. Mar. Biol., 76 : 301-309.
PARRINELLO, N. & RlNDONE, D.. 1981. Studies on the natural hemolytic system of the annelid worm Spirographis
spallanzanii (Polychaeta). Dev. Comp. Immun. N.Y. 5 : 33-42.
PERKINS, T.H. & KlNGHT-JONES, P.. 199 1. — Towards a revision of the genera Sabella and Bispira (Sabellidae). Ophelia.
Suppl. 5 : 698.
1URSI. A.. MaTarrese, A., CECERE. E. & RlBECCO, N., 1985. Sviluppo di popolazioni bentoniche su pannelli fouling
nel Mar Grande di Taranto. Atti S./.T.E. , 5 : 585-589.
Source : MNHN. Paris
5
The functional significance of blood plexuses
in the ecology of Ophelia bicornis Savigny
Tegwyn HARRIS
Departmeni of Biological Sciences
The University of Exeter, Hatherly Laboratories
Prince of Wales Road, Exeter, EX4 4PS, U.K.
ABSTRACT
The anatomy of the anterior blood vascular system of Ophelia bicornis is described with especial reference to its plexuses
of inflatable blind capillaries. The functional significance of these plexuses under the influence of systolic blood pressure and
their roles in the provision of an efficient burrowing mechanism through relatively dilatent sand whilst, at the same time,
helping to maintain an efficient transport system for dissolved substances is described and discussed within the context of the
ecology of the polychaete. The study has been carried out by direct observation of the living worm, by dissection and by
analysis of absorbed radioactively-labelled glutamic acid.
r£sum£
Signification fonctionnelle des plexus sanguins pour Pecologie d* Ophelia bicornis Savigny
L'anatomie du systeme vasculaire sanguin anterieur d 'Ophelia bicornis est decrite en considerant plus specialcment ses
plexus de capillaires aveugles et dilatables. La signification fonctionnelle de ces plexus, sous 1’influence de la pression sanguine
lors de la systole, leur role dans la mise en oeuvre d'un mecanisme efficace pour 1'enfouissement dans des sables relativement
compacts el le role qu’ils jouent, dans le meme temps, comme systeme de transfer! des substances dissoutes, sont decrits et
discutes dans le contexte de 1'ecologie du Polychete. L’etude a etc conduite par observation directe d’animaux vivants. par
dissection et par l'analyse d'acide glutamique radioactif absorbe.
INTRODUCTION
The mechanisms of digging into, and travelling through, marine sediments by soft-bodied invertebrates has
been studied at some length. Both in the bivalved molluscs (Ansell & Trueman, 1967: Trueman, 1968) and in
the annelids (Chapman, 1950, 1958), it has been shown that effective locomotion is usually achieved by an
interaction of the body-wall musculature and an internally-developed hydrostatic tension in a body fluid, usually
that which fills the coelom.
The most extensive studies of burrowing in the Polychaeta have involved Arenicola marina. Chapman and
Harris, T., 1994. The functional significance of blood plexuses in the ecology of Ophelia bicornis Savigny. In:
J.-C. DaUVIN, L. LaUBIER et D.J. REISH (Eds), Actes de la 4eme Conference internationale des Polychctes. Mini. Mas. nam.
Hist, not .. 162 : 57-63. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
58
T. HARRIS
Newell (1947) and TRUEMAN ( 1966a, b) have discussed the nature and mode of action of the hydrostatic system,
whilst WELLS (1944, 1952. 1954. 1961) has described the mechanical activities of the proboscis and their
significance to the behaviour of die worm. The consensus of this work is dial the primary thrusting force is
generated by the interaction of the internal coelomic fluid pressure and die highly-controlled body- wall muscles
and muscular, eversiblc proboscis.
Wells (1954) and Chapman (1958) pointed out that much of die success of this process is due to die presence
in Are ni co la of an open coelom which results in the deployment, at die anterior, of die total force generated by
extensive areas of body-wall musculature reacting against a "whole-body" hydrostatic skeleton. In association
widi diis, WELLS (1954) also suggested that the diree retained anterior septa of Arenicola serve to resist the at-rest
coelomic pressure in order to restrict unnecessary extension of die proboscis. Ophelia bicornis , too. has a coelom
which is continuous throughout die body and two retained anterior septa, but they are used in a manner which is
totally unlike that of Arenicola. This paper reports the mode of acdon of that coelomic apparatus and of the way in
which it is augmented by the acdvities of die complex blood vascular system.
MATERIALS AND METHODS
a. Anatomical and behavioural study.
Ophelia bicornis was collected from Bull Hill Bank in the estuary of die River Exe, Devon, U.K. Worms were
killed and fixed by immersion for about three hours in 5% neutral formalin in sea water, some after fresh-water
narcotisation, others without pre-treatment. This was necessary since, as reported by Brown (1938) for Ophelia
rathkei , die only agent which is effective for die narcotisation of 0. bicornis is fresh water. Immersion in fresh
water for about twenty minutes induces total narcosis and also causes the worm to extend to its full, straight,
length. Since this is clearly induced by osmodc influx of water into die coelomic compartment, all dissections
were performed on narcotised specimens for clarity and repeated on untreated specimens for confirmation of the
exact state of the organs and tissues. In practice, it was found dial even the most delicate coelomic capillaries were
not modified by the fresh-water treatment.
Locomotory activities were observed in Ophelia provided with semi-transparent artificial sand composed of a
mixture of glass beads of appropriate granularity moistened with sea water. Use of immature worms, with
relatively unpigmented and thin body-walls, permitted a certain amount of direct observation of internal activity.
b. Amino acid uptake.
Amino acid uptake was investigated using L-[U-,4C] glutamic acid (50(iCi. cm-3), supplied by Amersham
International, in a laboratory regime based upon "Analar" quality acid-cleaned sand and artificial sea water as
formulated by Dawson et al (1969).
132 pi of radioactive amino acid were added to 75ml of artificial sea water. This was thoroughly mixed and
added to 150 g of sand and cooled to 10 °C. Experiments were carried out at this temperature. Sand prepared in
this way was found to contain sufficient radioactive material to give 39 072 dpm. g'1 sand at die degree of
dampness used in the experiments (dpm = disintegrations, min'1 as counted in the liquid scintillation counter).
Ophelia bicornis were placed in the prepared sand and allowed to burrow naturally.
Individual worms were removed at intervals of 10 min, 20 min. 30min, 45 min and 60 min, rinsed in artificial
sea water and immediately cut into three portions representing die prostomial and pharyngeal region, the mid-gut
(intestinal) region and the hind-gut (chiefly rectal) region. The mass of diesc portions was determined and they
were prepared for liquid scintillation as follows.
The tissue was placed in glass scintillation vials widi 0.9 ml of "Soluene 350" and digested at 40 °C overnight.
After cooling to room temperature, 0.2 ml propan- l-ol and 0.4 ml 30 % hydrogen peroxide in two 0.2 ml portions
over two hours, were added to decolorize die pigmented solution. After the addition of die second portion of
hydrogen peroxide, the samples were heated to 40 °C to drive off excess peroxide and again allowed to cool.
5.0 ml ’’Packard 299" scintillation fluid were added to each vial and die activity of the mixture was measured
in a Packard "Tri-carb 460 CD" liquid scintillation counter by die sample channels mediod against a quench curve
prepared from measurement of vials containing "Packard 299" fluid with chloroform as the quench reagent.
c. Autoradiography.
Worms destined for autoradiographic study were allowed to ingest die radioactive amino acid-treated sand for
two hours prior to fixation. This relatively lengdiy treatment time was decided upon since the aim of the present
BLOOD PLEXUSES AND ECOLOGY OP OPHELIA BICORNIS
59
investigation was solely to determine the extent of amino acid uptake and its broad distribution within the tissues
of Ophelia bicornis.
Worms were fixed in 3 % neutral formalin in sea water without prior narcotisation and. during fixation, were
divided into 1.0 cm long portions so dial the intestine could be cleared of sand. The fixed tissues were dehydrated
through a standard ethanol series, embedded in paraffin wax and sectioned at 10pm. Sections were mounted on
gelatin-subbed slides as recommended by Kodak Ltd (1978) and ROGERS (1979). They were coated with "Kodak’1
AR10 stripping film and allowed to expose, in the dark, at 15 °C for 14 days. The slides were developed in
"Kodak" D-19 and fixed in "Kodak" F-5.
The Ophelia tissues acquired a pale straw colour during processing which rendered them clearly visible
beyond the developed silver, thus obviating the need for staining.
Control of the technique was effected in two ways: a) by comparison with similarly- processed sections of
tissues which had not been subjected to radioactive labelling and, b) by examination of putative developed silver
grains by dark-field microscopy, as recommended by Rogers (1979).
RESULTS
a. The anterior coelom and its vascular system
The overall pattern of the blood vascular system followed the descriptions of Clapar£de (1870) from Ophelia
radiata and of Brown ( 1938) from 0. raihkei. The constructional design is in two major parts, a posterior system
based upon a series of sinuses and an anterior system of complex blood vessels.
The whole length of the intestine of 0. bicornis is surrounded by voluminous dorsal and ventral blood sinuses,
of which the dorsal is the larger. The ventral sinus more nearly resembles an inflated blood vessel and, for most of
its length, is virtually buried within the ventral tissues of the typhlosole.
40mm
FlG. 1. A semi-diagrammatic drawing of the anterior of Ophelia bicornis dissected from the right side and cut back to
beyond the ventral nerve cord. For the sake of clarity the prostomial part of the pharynx is not shown, bw, vessels to the
body-wall. - eg. cephalic ganglion. - cv, commissural vessel. - dv, dorsal blood vessel. - h. heart. - ij, "injector organ". - ijv.
"injector organ" blood vessel. - is, intestinal sinus. - 1, ligaments. - m, position of mouth. - pp. pharyngeal capillary plexus.
- prp. prostomial capillary plexus. - vc, ventral cistcma.
The anterior blood system is illustrated semi-diagrammatically in Fig.l. The conspicuous parts of die system
arise from the junction of the buccal chamber with the intestine (shown at the left of Fig.l). At this point, the
dorsal intestinal sinus gives rise to a muscular heart which contains a non-return flap- valve (Fig.2). From the
heart, an anterior dorsal vessel gives rise to four paired vessels. From posterior to anterior these are - a pair of
lateral vessels which connect the dorsal and ventral sinuses, a pair of vessels which enter the wall of die buccal
chamber, then two pairs of commissural vessels which link widi a sub-pharyngcal cisterna of chambered
Source :
60
T. HARRIS
appearance. The dorsal vessel then passes through the walls of the "injector organ" to the prostomial coelom
where it divides into two anterior lateral vessels which travel back through the "injector organ" wall, apparently
between the two septal components, and continue as afferents to the sub-pharyngeal cistema.
"Blind appendages" or, perhaps more correctly "blind capillaries", arise in large numbers from the anterior
paired vessels, forming a dense plexus surrounding the pharynx and another within the prostomial coelom, as
shown in Fig.l. Cardiac activity produces alternate swelling and deflating of the blind tips of die capillaries: at
cardiac systole, 1.0 - 1.5mm of die tip swells to such an extent Uiat the capillary wall stretches until it is virtually
invisible under die low power of the microscope; at cardiac diastole, the tubular appearance is resumed.
FIG. 2. A median longitudinal section of the heart of Ophelia bicornis, - dv, dorsal blood vessel. - f. the flap valve. - is,
intestinal sinus. The arrows point toward the anterior of the worm.
The increase in volume of the anterior blood system due to die simultaneous inflation of so large a number of
blind capillaries is considerable. It seems that diis activity is of benefit to 0. bicornis in two ways.
The most obvious purpose of die mechanism is perhaps that of putting a large volume of blood, under
pressure, in close contact with the coelomic fluid and its corpuscles. This may be an important means of
producing coelomic fluid by an ultrafiltration process and of transpordng dissolved molecules between the two
body-fluid systems. This view gains some support from die presence of similar blind capillaries on die nephridial
blood vessels of O. bicornis and from the experimental evidence, based upon amino acid uptake, which is
presented below. Studies such as those of KOECHLIN (1966), Nakao (1974) and Ruppert & Smith (1988)
suggest that efficient internal fluid transfer in polychaetes is often effected under pressure across the thin walls of
capillaries, somedmes organised into plexuses. Such efficiency may be achieved in Ophelia bicornis by means of
the inflatable blind capillaries described here.
There is, however, a more spectacular purpose to this system which is of mechanical nature and easily
observed as it occurs widiin die prostomial coelom. The "injector organ", similar to that described by Clapar£de
(1870) in Ophelia radiata, is a structure formed from the two remaining segmental septa, which seals off die
prostomial coelom of Ophelia bicornis from die main body coelom. Observation of acuve 0. bicornis shows diat
the "injector organ" plays an important role in die increasing of prostomial coelomic fluid pressure, but it is a
passive role. 'Hie walls of the organ do not contract to any appreciable extent in 0. bicornis and dierefore little, if
any, of its contained fluid is squeezed into die anterior chamber. The passivity of die "injector organ" and die
relative inelasticity of the prostomial cuticle combine to make the prostomial coelom not only a sealed chamber,
but also a reladvely inexpandable one.
b. The uptake of dissolved amino acids.
Harris (1991b,c) has indicated diat 0. bicornis probably supplements its diet to a very considerable extent by
the uptake of dissolved organic material from die interstitial water and from die surfaces of die sand grains which
are crammed into die gut during the feeding cycle. Investigations using radioactively-labelled glutamic acid have
Source :
BLOOD PLEXUSES AND ECOLOGY OF OPHELIA BICORNIS
61
shown that the radioactive marker accumulates to a greater extent in the anterior part of 0. bicornis than
elsewhere, as shown in Fig. 3. Autoradiographic investigation of thin sections of the anterior region shows that a
considerable proportion of the labelled amino acid accumulates in the coelomic corpuscles of the sealed anterior
chamber. Fig. 4.
Minutes
Uptake of L-(U-uC)gIutamic acid expressed as DPMg1 wet weight Ophelia tissue
FIG. 3. — A bar chart showing typical uptake by Ophelia bicornis of radioactively-labelled glutamic acid over a sixty minute
period. "Anterior" = the prostomium and buccal region, "Mid gut" = the central part of the body containing the absorptive
part of the intestine, "Hind gut" = the rectum and pygidial papillae. DPM = disintegrations per minute in the scintillation
counter.
DISCUSSION
According to Fauvel (1959) "L'appareil circulatoire des S6dentaires prSsente d'innombrables modifications
on rapport avec la specialisation dcs diffdrentes regions du corps." Even within die context of such variety, die
blood vascular system in the genus Ophelia is outstanding bodi in its structural modificadons and in its functional
relationships widi die hydrostatic system and through both, with the behaviour and ecology of die worm.
Clapar6de (1870) described numerous blind vessels on die lateral vessels of Ophelia radiata: "Sur tout ce
parcours le vaisseau dorsal et le vaisseau ventral sont mis en communicadon par une serie d'anses. Le caracterc le
plus rcmarquable de cet appareil e'est que tous ces vaisseaux, surtout le dorsal et les anses, sont munis de
centaines d'appendices aveugles, contractiles, dont le jeu alternatif de systole et de diastole est fort curieux k
observer." He goes on to say that these structures are most numerous in die peripharyngeal region and are
relatively rare within die prostomial coelom.
Clapar£de (1870) described die "injector organ" as being of a tough, muscular nature and important to die
generation of the prostomial rigidity which is so necessary for die penetration of sand. He said that this is
accomplished by die contraction of die "appareil injecteur" by its own musculature, thus forcing into die enclosed
prostomial coelom an additional volume of coelomic fluid, increasing the overall hydrostatic tension against die
cuticle and so inducing a certain stiffness. In O. bicornis die "injector organ" seems to act only as die inclasdc rear
wall of the enclosed prostomial chamber.
At cardiac systole, die prostomial coelomic fluid is put under considerably increased pressure by die sudden
and simultaneous inflation of the blind capillaries of die prostomial plexus. This pressure, developed against the
inelastic cuticle, provides the necessary turgidity for die penetration of sand. At the same time, pressure is brought
to bear on die anterior part of the pharynx which passes dirough die ventral wall of the "injector organ" and
dirough die prostomial coelom and, due to die inflation of die plexus which lies external to the "injector organ",
upon die posterior part of the pharynx also. This greatly facilitates die eversion, through the mouth, of die
62
T. HARRIS
voluminous pharynx (issues. It is probable that this pressure increase is supplemented by an increase in the
volume of the pharyngeal coelomic fluid due to ultrafiltration through the greatly-expanded walls of the blind
capillaries.
Fig. 4. — Autoradiographs of unstained sections of Ophelia bicomis after uptake of radioactive glutamic acid, a: a cross-
section through the anterior pharyngeal region shows scattered concentrations of silver, b: part of the inner wall and
coelom of the "injector organ" shows great concentration of silver in the coelomic corpuscles and scattered grains in the
coelomic fluid. - cc. coelomic corpuscles. - cf. coelomic fluid. - ij. "injector organ". - p, pharynx. - pp. pharyngeal plexus.
Harris (199 lax) described Hie typical habitat of 0. bicomis in the Exe Estuary as being emersed for
considerable periods, well — il not excessively — drained and meagre in potential food-sources and resistant to
passage by a soft-bodied invertebrate. Chapman and Newell (1947). having described die pressure which can be
developed, within die anterior coelom and proboscis of Arenicola marina state, suggested that diis allows the
worm to dig and to burrow effectively only when provided with thixotropic sand. It is not inappropriate to note
therefore, that die hydrostatic mechanism which is described here for Ophelia bicomis allows die worm to travel
at all times with apparent ease dirough sand which is thixotropic for only relatively brief periods and dilatent for
much longer ones.
1 he thinness of the gut-lining wall of the intestinal sinus of O. bicomis probably ensures the rapid transport of
absorbed dissolved substances directly into the blood from the surfaces of die sand grains around which the walls
of the gut wrap themselves in a totally-enveloping manner. This, coupled with the presence of a defaecation-
enhancing device in die rectum (Harris, 1991b), gives an indication of the means which exist for efficient and
constant nutrient uptake in this polychaete. Provision of a swift transport and storage mechanism, making use of
an already-enhanced vascular system, would seem to be a logical ultimate development.
CONCLUSION
The entire cycle of events may be summarised as follows:
a) Ophelia bicomis travels through highly resistant sand. Enhancement of die pressure within its prostomial
hydrostatic skeleton by blood surges into expandable capillaries from a valved heart assists movement through die
substrate.
b) Co-incidentally, the induced pressure system increases die efficiency of pharyngeal eversion and thus the
intake of sand.
c) Nutrients absorbed from dial sand are passed rapidly into the blood stream and efficiently flushed from the
site of absorption to sites of temporary storage.
d) 1 he same vascular apparatus permits rapid interchange of solutes between the blood and die coelomic fluid
and its corpuscles which may act as one of die sites of food storage.
Source :
BLOOD PLEXUSES AND ECOLOGY OF OPHELIA BICORNIS
63
ACKNOWLEDGEMENTS
I am grateful lo Philip Shears for his unfailing and cheerful support in the laboratory and aquarium, to
Margaret Grapes for die benefit of her skill in handling the radio-isotope materials and to my colleague,
Professor David Nichols for his continued interest, advice and constructive criticism.
REFERENCES
ANSELL, A.D. & TRUEMAN, E.R., 1967. — Burrowing in Mercenaria mercenaria (L.) (Bivalvia, Veneridae). J. exp. Biol.. 46 :
105-115.
BROWN, R.S., 1938. The anatomy of the polychaete Ophelia clulhensis McGuire, 1935. Proc. R. Soc. Edinb ., 58 : 135-160
Chapman, G.. 1950. Of the movement of worms. J. exp. Biol.. 27 : 29-39
CHAPMAN, G., 1958. — The hydrostatic skeleton in the invertebrates. Biol. Rev.. 33 : 338-371
CHAPMAN, G. & Newell. G.E.. 1947. The role of the body fluid in relation to movement in soft-bodied invertebrates. I. The
burrowing of Arenicola. Proc. R. Soc., Ser.B, 134 : 431-455
ClaparEde, E., 1870. — Les annelides chetopodcs du golfe de Naples, seconde partie. Mem. Soc. Phys. Hist. nat. Gendve.
20 : 1-225.
Dawson. R.M.C., ELIJOTT, D.C., Elliott, W.H. & JONES, K.M.. 1969. — Data for Biochemical Research. 2nd Edition,
Oxford University Press, 654 p.
FAUVEL, P.. 1959. — Organes des sens. Pages 95-1 19. In P.-P. GrassG (ed), Traiti de Zoologie. 5, Masson, Paris : 95-119.
Harris, T.. 1991a. — The occurrence of Ophelia bicomis (Polychaeta) in and near the estuary of the River Exe, Devon. J.
mar. biol. Ass. U.K.. 71 : 391-402.
Harris, T.. 1991b. - The rectal organ of Ophelia bicomis Savigny (Polychaeta): a device for efficient defaecation. Zool. J.
Linn. Soc., 103 : 197-206.
Harris. T.. 1991c. Some aspects of the specific habitat requirements of Ophelia bicomis (Polychaeta). J. mar. biol. Ass.
U.K. . 71 : 771-786.
Kodak Ltd., 1978. Kodak materials for autoradiography. Kodak Information Sheet P- 64(4): 1-14.
KOECHUN, N.. 1966. — Ultrastructure du plexus sanguin peri-oesophagien; ses relations avec la nephridie de Sabella
pavonina Savigny. C. r. hebd. Seanc. Acad. Sci., Paris. Ser. D. 262 : 1266-1269.
NakaO, T., 1974. — An electron microscope study of the circulatory system in Nereis japonica. J. Morph.. 144 : 217-235
ROGERS. A.W.. 1979. — Practical autoradiography. Amersham International, Amersham.
Ruppert, E.E. & SMrrH, P.R., 1988. — The functional organization of filtration nephridia. Biol. Rev.. 63 : 231-258.
TRUEMAN, E.R., 1966a. — The mechanism of burrowing in the polychaete worm, Arenicola marina (L.). Biol. Bull., 131 :
369-377.
Trueman, E.R.. 1966b. — Observations on the burrowing of Arenicola marina (L.). J. exp. Biol., 44 : 93-1 18.
TRUEMAN, E.R., 1968. — A comparative account of the burrowing process of species of Mactra and of other bivalves. Proc.
malac. Soc. Land.. 38 : 139-150.
Wells, G.P.. 1944. — Mechanism of burrowing in Arenicola marina L. Nature, lx>nd.. 154 : 396.
WELLS, G.P.. 1952. — The proboscis apparatus of Arenicola. J. mar. biol. Ass. U.K., 31:1- 28.
Wells, G.P.. 1954. — The mechanism of proboscis movement in Arenicola. Q. Jl Microsc. Sci.. 95 : 251-270.
Wells, G.P.. 1961. — How lugworms move. Pages 209-233. In: J. A. Ramsay & V.B. WiGGLESWORTH (eds). The Cell and
the Organism. Cambridge University Press : 209-233.
Source : MNHN. Pahs
6
Feed-back regulation in Platy nereis dumerilii
Audouin & Milne-Edwards, 1833:
a status review
Dietrich K. HOFMANN
Department of Zoology & Parasitology
Ruhr-University Bochum
D-4630 Bochum, Germany
ABSTRACT
in Plaly nereis dumerilii , gametogenesis and heteronereid transformations, as well as growth and regeneration of
posterior parapodial segments, proceed under the endocrine control of presumeably a single hormone, which is produced
by and released from the supraoesophageal ganglion. As the universal principle applying to all gonochoric. monotclic
species in the family Nereidae investigated so far, this hormone controls postlarval development in a concentration-
dependent manner. The juvenile growth-phase and the early stages of gametogenesis are determined by high hormone
levels which, simultaneously, prevent precocious maturation and metamorphosis. Decreasing hormone levels correlate
with gamete maturation, heteronereid metamorphosis and. on the other hand, with a loss of regenerative capacity.
Neither oocyte differentiation beyond the critical stage nor spermiohistogenesis require additional hormone. The decline
in hormone concentration in P. dumerilii is not based on a brain-autonomous control of hormone production and release
but results from a more complex system of exogenous and endogenous factors acting on the cerebral ganglia. Severe
amputation of segments in both maturing females and males was, but transection of the nerve cord was not the decisive
factor for brain hormone activation. Removal of oocytes, injection of oocytes or of spermatogenic cells into juvenile
hosts affect hormonal activity, and juvenile prostomia are inactivated when passaged in maturing males. The results arc
interpreted in terms of inactivation (or reactivation respectively) of brain hormone activity, caused by humoral feed-back
emanating from coelomic cells, probably the germ cells. These findings are similar to but not identical with those
concerning brain-body interactions in female Nereis diversicolor and Perinereis cultrifera . Isolation of a low molecular
weight substance has been reported from the latter species, but the retroacting factor(s) in Platynereis dumerilii have not
yet been analysed yet.
RESUME
Revue de la regulation en retroaction chez Platynereis dumerilii Audouin & Milne-Edwards,
1833
Chez Platynereis dumerilii la gametogenese et la metamorphose heteron6r<5idicnne, ainsi que la proliferation ct la
regeneration de segments parapodiaux sont conditionnees par Taction d’une hormone elaboree par les ganglions
c£r6broides. Comme principe universel des especes de Nereidiens h reproduction gonochorique et monotelique, le controlc
Hofmann. D.K.. 1994. -- Feed-back regulation in Platynereis dumerilii Audouin & Milne-Edwards, 1833: a status
review. In: J.-C. DaUVIN. L. LaUBIER & D.J. REISH (Eds). Actes de la 4eme Conference internationale dcs Polycheles.
Mem. Mus. natn. Hist. nat.. 162 : 65-72. Paris ISBN 2-85653-214-4.
Source MNHN. Paris
66
D.K. HOFMANN
hormonal du developpement posllarvairc s'effeclue cn fonction de la concentration de l'hormone. La phase juvenile de
croissancc ct le debut de la gametogenese sont assurees par un taux hormonal elevc, qui, cn meme temps, inhibe la
maturation et l'epitoquie precoce. Le progres de la gametogdnese, de la metamorphose et l'arret de la regeneration
postcricurc sc relient a une diminution progressive de 1'activite endocrine. Par contre l’ovogenese et la spermatogenese,
au dcla d’une phase critique, sont achevees meme sous des conditions anhormonales. La reduction caracteristique du taux de
l'hormone au cours du cycle vital ne resulle pas du conlrolc autonome de la synthese et de la secretion par le cerveau lui-
meme mais ressort d'actions plus complexes de facteurs endogenes et exogenes sur les ganglions cerebroi'des.
L'amputation d'un nombre substantiel de segments posterieurs allure le status endocrine des vers males et femclles
proches de la maturite sexuelle. N6anmoins. la l<5sion de la chainc nerveuse ventrale, due h l’operation, n'est evidemment
pas la cause de la reactivation endocrine cerebrale que Ton constate. Ccpcndant, I'enlevement des ovocytes ou V injection
d'ovocytes submatures (ou de cellules spermatogenetiques) dans le coelome des vers juveniles, influence 1’activite
endocrine du contexte. En plus, des prostomiums prdlevcs sur des animaux juveniles subissent une deactivation du cervcau
au cours d'un passage dans le coelome des males s'approchant dc la maturite. Ces effets sont considcrcs comme le r^sultat
dune retroaction humorale sur I'activitc endocrine cerebrale provenant vraisemblablement des produits genitaux.
L’interdependance humorale entre le corps et le cerveau constat^ chez Platynereis dumerilii est comparable, mais n est pas
tout h fait identique a celle observee chez Nereis diversicolor et Perinereis cultrifera. Une substance provoquant l'arret de
1'activite hormonale cdrebralc a ete isolee des ovocytes de la derniere espece; par contre un factcur analogue n’a pas encore
ete identifie chez P. dumerilii.
INTRODUCTION
Feed-back control means that a controlled system itself is acting back on its own control unit either to
maintain or to alter a given physiological state. In the case of endocrine control of sexual maturation in nereid
polychaetes, a feed-back phenomenon was first described by DURCHON (1952) in Perinereis cultrifera. He
discovered dial oocytes and associated coelomocytes taken from females approaching maturity ("ovocytes
submatures", diameter > 180 pm) and injected into immature males of die same species caused precocious gamete
maturation and epitokous transformation. Since Durchon (1948, 1952) had found out dial maturation mid epitoky
arc controlled by an inhibitory hormone originating from the prostomium, he concluded that die submature
oocytes released a factor which down-regulated this inhibitory hormone, thus enhancing gamete maturation and
heteronereid metamor-phosis. This was the first indication of possible interaction between the endocrine system
and die maturing body.
All available data agree widi die view that, as an universal principle in nereids, a single hormone, which is
produced most probably in neurosecretory cells of the brain, controls postlarval development in a concentration
dependant manner. It has been found to be neither species specific nor sex specific, and to work in species with and
without epitokous reproductive form.
The present report considers currently available data on the regulation of endocrine activity in Platynereis
dumerilii, one of the most thoroughly investigated nereid species. The following question is asked: is die brain
hormone titer regulated by brain-autonomous control of production and release, or is it determined by a more
complex system ol exogenous and endogenous factors acting on die neurosecretory ganglia? In particular, I review
results of investigations aimed at demonstraung feed-back phenomena during male and female gametogenesis,
metamorphosis and regeneration of posterior segments. These findings are discussed and compared widi studies
bearing on feed-back control in P. cultrifera and on brain-body interaction in Nereis diversicolor (e.g. PORCHET &
Cardon, 1976; PORCHET, 1984; Golding, 1987).
DEVELOPMENT OF PLATYNEREIS DUMERILII
P. dumerilii , originally described from die Mediterranean and the french Atlantic coast, is a gonochoric,
typically monotelic species, which develops a pelagic, epitokous reproductive form. Sex appears to be genetically
controlled and die diploid complement of chromosomes was found to be 28 (Hanske, 1989). The same diploid
chromosome number was found also in the sibling species P. massiliensis and P. megalops (D. JOrg, Univ.
Mainz, pers. comm.). In neither sex are typical gonads present, gametogenesis proceeds in the coelomic fluid.
Recently. Hanske (1989) detected paired, segmental sites at dorsolateral positions, from which small clusters of
spermatogonia appear to be proliferated and released into the coelom (but see die findings in Nereis grubei by
Reish, 1954). Metamorphosis into the reproductive form parallels die final stages of gamete development; die
pelagic heteronereis then broadcasts die fully mature eggs and sperm during pheromone controlled nuptial dances
Source : MNHN. Paris
FEED-BACK REGULATION IN PIATYNEREIS DUMERIIJI
67
(ZEEK et al., 1988 for review). There is no brood protection; early phases of development, including trochophore
and metatrochophore stages, are pelagic. Nectochaeta larvae later start settling and forming tubes on the substratum
from secretions of parapodial glands. In laboratory cultures maintained by now standard methods (HAUENSCHILD,
1951), development from fertilized egg to the heteronereis stage is variable and takes from 3 to 12 months with a
small proportion of "stragglers" taking up to 18 months (HAUENSCHILD, 1966). Of a total of 635 males 65%
reached maturity within 4-8 months (Hanske, 1989); die same author recorded a similar life-span for females.
With its very short life-cycle, correlated widi rapid growth and fast regeneration, P. dumerilii differs considerably
from P. cultrifera and Nereis diversicolor which require 2-3 years to reach ihe reproducuve status in the field.
ENDOCRINE CONTROL OF POSTLARVAL DEVELOPMENT
Results of the pioneer work by DURCHON (1948, 1952), performed first on male Nereis irrorata and Perinereis
cultrifera, suggested that spermatogenesis and epitokous metamorphosis are controlled by an inhibitory, endocrine
factor formed widiin the prostomium. Using female worms, HAUENSCHILD (1956, 1965, 1966) conducted
prostomium amputation experiments on laboratory reared P. dumerilii , focussing on gametogenesis,
metamorphosis and caudal regeneration. His results largely confirmed Durchon's observations, but moreover,
provided a much more detailed hypothesis of the hormonal control mechanism in this species. He concluded that a
single prostomial hormone is responsible for die control of both gametic and somatic development, acting in a
concentration dependent manner. The juvenile growth phase and proliferation of germ cells require a high tiler of
hormone, which inhibits late stages of gametogenesis and epitokous transformations. When oocytes reach
diameters of 80-100 |im, a photoperiodically triggered decrease of hormone concentration initiates a new phase of
oocyte growth and differentiation, stops die addition of new segments, quenches posterior regeneration, and allows
then metamorphosis of somatic tissues. Once die level approaches zero, development of heteronereid swimming
setae is completed and oocytes undergo final maturation. The hetcroncreis then aquires the competence to respond
to sex pheromones, i.e. to perform nuptial dances and to shed the gametes soon after it begins to swim. Since
absolute hormone concentradons could not be measured, HAUENSCHILD (1965) used arbitrary units and suggested,
but did not indicate in his Fig. 19, a logarithmic scale. DURCHON & PORCHET (1971), PORCHET (1973), and
SCHROEDER et al. (1977) arrived at similar conclusions when studying developing individuals of several species
of nereids, despite die fact dial the former audiors were using an entirely different organ-culture system to assay die
hormonal activity of homogenized pros tom ia (sec BERTOUT, 1984 for details of the N. diversicolor
spermatogenesis assay).
The major drawback of the work discussed herein is that die precise site of production and release of the
hormone, its molecular structure, its rate of synthesis and secretion, and its absolute concentrations are not yet
known. We must use live prostomia, or homogenates (fresh or lyophilized) as a source of the active compound,
and we have to deduce or to determine indirccdy relative values of hormone activity (or concentrations respectively)
from biological assays based on morphogenic or cytomorphologic criteria.
All recent evidence confirms die view- diat the hormone concentration in Platynereis dumerilii is maximal in
juvenile animals and decreases to zero in die heteronereid, and a high level of activity is required to sustain
segment formation, to support the proliferation of oogonia and spermatogonia, and to suppress premature
maturation and epitoky (Hofmann, 1975, 1976: Schiedges, 1981; Hofmann & Schiedges, 1984; Meisel,
1990). It has been confirmed diat growdi and regeneration capacity decrease and somatic metamorphosis starts
when die hormone level is lowered. However is has become a matter of dispute whether all successive
developmental events in somatic tissues and germ cells are directly controlled by specific levels of hormonal
activity. HAUENSCHILD (1966) found that oocytes, which, had a critical diameter of about 100 |im, completed a
morphologically normal oogenesis after the prostomium had been removed. No further hormone supply was
required at that stage. On the other hand, implantation of one or two prostomia from juveniles into female
recipients with oocytes of diameters larger than 100 |im significantly prolonged die time of survival, but retarded
and disturbed both oogenesis and metamorphosis when compared to eidier decapitated worms or controls. Though
oocyte development beyond the critical stage can proceed widiout continued hormone secretion, the maturing
oocytes are still sensitive to altered endocrine conditions (Hofmann, 1975).
The same type of experiments led to different results when performed on males. Prostomial removal from
juveniles caused defective development at the end of which die worm fragments were still lacking major
heteronereid characters and did not contain any gametes. Individuals with some small clusters of spermatogonia in
die coelom (early spermatogonia cluster I phase) showed a dual response. Whereas metamorphosis was defective in
68
D.K. HOFMANN
all cases, the course of spermatogenesis was morphologically normal. None of the stages was omitted but the
entire sequence was accelerated : it took only 12.5 days on the average instead of one to several months to produce
mature spermatozoa. If, however, worms were decapitated at the end of the first mitotic proliferation phase (late
spermatogonia cluster I phase), not only spermatogenesis but also metamorphosis was accelerated. At this stage
93% of tiie experimental worms developed normal heteronereid characters (MEISEL, 1990).
Implantation of one to three prostomia from juvenile donors into developing males, from the advanced
spermatogonia cluster stage onward, left spermatogenesis unaffected. Differentiation of sperm proceeded at about
the normal rate. This is in obvious contrast to the findings in females. On die other hand, heteronereid
transformation was strongly affected and disordered by this manipulation of the hormone level, as in the
corresponding experiments on female P. dumerilii (SCHIEDGES, 1981: Hofmann & Schif.dges, 1984).
Gamete development in both sexes and metamorphic events appear to be strictly coordinated in ontogenesis,
but to be experimentally dissociable. Spermatogenesis turns out to be considerably less sensitive to the alteration
of endocrine conditions than oogenesis. It is remarkable that development of heteronereid characters can be
seriously delayed and disturbed by manipulating the endocrine status even very late in gametogenesis. The sibling
species P. massiliensis , although morphologically indistinguishable from P. dumerilii , has an entirely different,
benthic mode of reproduction. These proterandric hermaphrodites do not metamorphose: they deposit, fertilize, and
brood the eggs within their tubes. Posterior regeneration was shown to decrease drastically in die absence of the
prostomium (Casanova, 1955), but no unequivocal proof of brain hormone control of either spermatogenesis or
oogenesis could be developed (Hauenschild, 1970; LOcht, 1987 for review).
FACTORS AFFECTING THE ENDOCRINE ACTIVITY OF THE BRAIN
ENVIRONMENTAL FACTORS
Hauenschild (1966) demonstrated photoperodic control of swarming periodicity in P. dumerilii and has
further shown maturation and epitoky to be hormonally governed. He therefore postulated that the synodic or
experimentally modified light-dark regime acts via the neuroendocrine pathway. However, no detailed study on
light-to-hormone signal conversion is available to prove this hypothesis.
Temperature has been reported to affect hormone gamete-interaction in N. diversicolor (Durchon & Porchet,
1971), but the influence of temperature on development and endocrine activity has not been studied in
P. dumerilii.
REGENERATION OF POSTERIOR SEGMENTS
The number of setigers regenerated following amputation of the posterior end is positively correlated with the
number of segments removed. As mentioned earlier, at a given level of transection, the number of segments
regenerated decreases concomitantly with the progress of gamete maturation and metamorphosis (Hauenschild,
1966: Hofmann, 1966; Schiedges, 1981; Hofmann & Schiedges, 1984). Hauenschild (1966) also noticed
that in maturing females amputation of a significant number of posterior segments led not only to regeneration
but also to retardation of sexual development and to delayed metamorphosis. These results suggest that hormone
production has been stimulated, possibly mediated by the injury of the ventral nerve cord (see Hofmann. 1966 for
discussion of earlier work). More detailed investigations in female P. dumerilii showed that maturation was
delayed and significant regeneration occurred only when about 50 of approximately 70 parapodial segments were
removed. Furthermore, the size of the regenerate and the delay in reaching the heteronereis stage decreased as
individuals of more advanced stages of sexual development were assayed (Hofmann, 1975).
In males, the number of segments regenerated and the delay in heteronereid metamorphosis are likewise
correlated with the number of segments amputated and with die stage of sexual development. However,
spermatogenesis continued unaffected when males from the late spermatogonia! stage onward were assayed. In such
cases we observed males deprived of all but 20 segments which showed posterior regeneration and significant delay
ot metamorphosis, but in which spermatogenesis proceeded independently. They contained mature spermatozoa a
full diree weeks before reaching the heteronereis stage.
I he hypodiesis that the site ot nerve cord lesion causes a position-dependent increase in hormone production
and thus determines the course of regeneration and maturation was tested. In males and females at selected stages of
development, the ventral nerve cord was excised from segments 20 and 21 (or the circumoesophageal connectives
Source : MNHN , Paris
FEED-BACK REGULATION IN PLATYNEREIS DUMERILII
69
deleted) prior to amputation of the posterior end behind segment 40 (Hofmann, 1966, 1975; Schiedges. 1981).
File results did not support the assumption that nerve cord injury activates hormone secretion and thus enhances
posterior regeneration accordingly. Therefore, stimulation of the neurosecretory cells via the nervous system does
not appear to be the decisive control mechanism. There must be other components modulating brain hormone
activity by stimulating its production or by temporarily preventing its decrease. Candidates are die developing
gametes, the somatic coelomocytes interspersed with the gametes, and various somatic tissues.
FEED-BACK ACTIVITY OF GAMETES AND COELOMOCYTES
When deprived of all but 20 segments, female P. dumerilii with oocytes measuring 130- 150 pm in diameter
regenerated up to 12 segments and survived up to 25 days, whereas those cut behind segment 40 did not form
regenerates but transformed into heteronereids within one week, as did the controls. Amputation of about 2/3 of
the animals parapodial segments means dial die hormone "source" has to serve thereafter only a much smaller part
of its "sink". Even at a given, constant production of the factor, a higher concentration may result in the much
smaller body and could account for enhanced regeneration and retarded heteronereid development. If one bears in
mind that some cells of die "sink" acquire the ability to feed back on and to inhibit the hormone producing cells,
cutting off segments involves not only a decrease of the "sink" volume, but also a reduction of die mass of cells
feeding back on die hormone source.
DURCHON (1952) suggested that a coelomic factor associated with the oocytes and clcocytcs of submature
P. cultrifera reduced the endocrine activity of die brain in immature recipients injected with gametocytes and
coelomocytes.
Several lines of evidence indicate dial down-regulating factor(s) exist in P. dumerilii as and are major
components of developmental control (Hofmann, 1975: Schiedges, 1981; Hofmann & Schiedges, 1984;
MEISEL, 1990). In these investigations, the number of segments regenerated by males and females at selected
stages of development, the time period required to form the heteronereis, or the survival time, were used to
determine such effects.
REMOVAL AND INJECTION OF COELOMIC CONTENTS
Removal of oocytes and coelomocytes by stripping following caudal amputation led to enhanced regeneration
and to significantly delayed metamorphosis at stages in which regeneration had normally ceased (HOFMANN,
1975). When intact juvenile worms were deprived of all but 40 segments and were injected with the coelomic
contents of females with oocytes ranging from 100 to 180 pin in diameter, effects on the recipient's development
were observed only when 100 to 120 pm oocytes were injected. Seven out of 15 juvenile recipients started to
regenerate but then stopped and transformed into heteronereis within 1 1 to 17 days, whereas controls took one to
several months (HOFMANN, 1975).
Stripping of gonia from males was much more difficult and could not be done quantitatively. The
experimentals were apparently affected by the manipulation and did not develop well. This will not be considered
further (Schiedges, 1981). Injection of mature spermatozoa and coelomocytes into very young females (oocyte
cluster stage) caused accelerated oocyte growth and metamorphosis, and significantly reduced the regeneration of
posterior segments. Quite unexpectedly, males at the initial stage of gametogenesis did not respond to sperm
injection. On the other hand, juvenile worms, when injected with gonia from spermatocyte/tetrad or tetrad stage
donors, metamorphosed much faster than the controls, i.e. in only about 62 % of the time. However regeneration
was clearly reduced only when the colomic contents of tetrad stage donors was transferred (Schiedges, 1981).
These observations are compatible with the hypothesis that factors, probably stage specific, are associated with
gametes and coelomocytes, which influence development by altering the endocrine activity of die brain. Under
these premises stripping of the oocytes means removal of the feed-back factor and results in hormone production
and, consequently, in enhanced regeneration and delayed metamorphosis. On the other hand, injection of
differentiating gametes and coelomocytes adds such factors which then suppress hormone production in the
immature host. This would account for their limited regeneration and accelerated epitokous development and
maturation.
70
D.K. HOFMANN
PROSTOMIUM TRANSFER EXPERIMENTS
Additional evidence for the existence of coelomic factors which feed back on hormone production has been
provided by prostomium transfer assays. Hauenschild (1966) found that prostomia taken from maturing females
and implanted into decapitated fragments of younger females, exhibited a stronger maturation inhibiting and
regeneration promoting activity than they would have in situ. He assumed that the different "environment" in the
younger recipients had somehow stimulated the activity of the implant. Schiedges (1981) systematically tested
the properties of prostomia taken from males at different spermatogenetic stages and transferred to juvenile,
decapitated hosts. She noticed that prostomia excised from worms at the spermatocyte cluster stage, the
spermatocyte/tetrad stage and at the tetrad stage could be assigned a higher endocrine activity than when tested in
situ , thus confirming and extending HAUENSCHiLD's result.
Schiedges (1981) provided further support through very elegant prostomium passaging experiments performed
on P. dumerilii. Prostomia excised from immature donors were implanted into male intermediate hosts at different
stages of spermatogenesis and were left there for one week. Then die prostomia were excised again and implanted
into definitive, immature, decerebrate 40 segment host fragments.
In individuals receiving prostomia which had been passaged in intermediate hosts ranging from the juvenile
state to die spermatocyte /tetrad stage there was a slight decline in botli numbers of segments regenerated and in
survival time, compared to die controls. However a significant decrease occured only in Uiose receiving prostomia
which had been passaged through intermediate hosts at the tetrad or sperm stage. This proved that die secretory
activity of prostomia is negatively affected when exposed to the coelomic "environment" of maturing males. This
influence appears to be stage dependent and to be strongest during the last two spermatogenic stages. Isolation and
characterization of factors which exert negative feed-back on endocrine acuvity and which do not appear to be sex
specific, has not yet been attempted in P. dumerilii.
FEED-BACK CONTROL OF BRAIN HORMONE ACTIVITY
IN OTHER NEREID POLYCHAETES
Extending DURCHON’s (1952) earlier work, PORCHET (1967), Porchet & DURCHON (1968). and PORCHET &
Cardon (1972, 1976) studied the effect of maturing oocytes ("ovocytes submatures", diameter > 180 pm)
injected with their adhering coelomocyles into recipient male and female worms at different stages of development
in P. cultrifera. In this species, which takes three years to reach sexual maturity, oocyte transfer turned out to
cause long-term effects, observed only after many weeks or even months. Injection of submature oocytes into
juvenile hosts led to precocious gametogenesis: 93 % of die males produced sperm and also transformed into
heteronereids within 110 days. Surprisingly, female recipients underwent only abortive, although accelerated
oogenesis but did not metamorphose, in contrast to the findings in P. dumerili (Hofmann, 1975; Schiedges,
1981; Hofmann & Schiedges, 1984). Injection of coelomic contents was also found to affect posterior
regeneration, i.e. the number of segments regenerated was negatively correlated with the size of the injected
oocytes. Alter carrying submature oocytes for 50 days, initially juvenile recipients failed to regenerate any
segments within a period of 20 days, though controls regenerated an average of 14 segments.
PORCHET & Cardon (1972, 1976) showed that the precocious gametogenesis, epitoky, and inhibition of
regeneration, which followed injection of submature oocytes, was not a response to the injection. They
demonstrated that the eflect is based on a chemical factor, the action of which could only be interpreted in terms of
down-regulation of brain hormone activity in the recipient. In separate assays, they examined the biological effect
of oocytes, coelomocytes, coelomic fluid, and of extracts of somatic tissues on host animals. They found that the
factor causing brain hormone inactivation is associated exclusively with the oocyte fraction. PORCHET & Cardon
(1976) purified the factor from an aqueous cthanolic oocyte extract. The compound appears to be a low molecular
weight substance which is dialysable, heat labile, resistant to proteolytic enzyme action, and ninhydrine positive.
It does not seem to be a peptide, but has been suspected to be a glycoprotein. The feed-back substance is obviously
different from die two peptides, Bj and B2, also isolated from the coelomic fluid of P. cultrifera , which stimulate
the final phase of oocyte differentiation (Porchet al.y 1979).
Golding (1967, 1983, 1985, 1987) provided a large body of evidence for humoral brain-body interaction in
N. diversicolor which corroborates many of the findings and conclusions reported above. N. diversicolor reaches
maturity in the second or third year ol life. It does not develop a pelagic heteronereis but shows an atokous,
benthic reproductive form. Gamete maturation is accompanied by the progressive loss of capacity to proliferate and
Source : MNHN. Paris
FEED-BACK REGULATION IN PIATYNEREIS DUMERIUI
71
regenerate posterior segments. As in the other nereid species considered here, decreasing brain hormone levels
account for this developmental pattern.
Prostomium passaging experiments involving prostomia from female donors at various stages of oogenesis
and using both immature and maturing intermediate hosts, demonstrated that the endocrine activity can be
influenced in either direction. Prostomia from maturing donors, known to exhibit only reduced regeneration
promoting activity, were apparently reactivated when subjected to repeated intracoelomic conditioning in immature
intermediate hosts. On the other hand, deactivation of prostomia was observed after passaging for a prolonged time
period in maturing hosts. Deactivation was readily achieved in prostomia excised from donors at later oogenetic
stages, but failed to occur in some of those taken from juvenile worms. Furthermore, injection of submature
oocytes into immature N. diversicolor had a long-term negative effect on regeneration, provided that the injected
oocytes did not degenerate. However Final oocyte maturation and spawning was not normally observed in these
individuals. Thus, submature oocytes can be assigned a brain hormone deactivating influence in N. diversicolor ,
too.
The results of the prostomium passaging experiments can be interpreted, as proposed in Platy nereis dumerilii,
in terms of inhibition and activation of neuroendocrine activity of the respective prostomia, (hough no information
is available on the regulatory mechanism. Although humoral retroaction on brain hormone activity has been
demonstrated also in male P. dumerilii (SCHIEDGES, 1981: HOFMANN & Schi EDGES, 1984), no corresponding
investigations seem to have been done on male P. cultrifera or Nereis diversicolor. Feed-back control in oogenesis
of Cirratulus cirratus (Olive, 1973) and in spermatogenesis of Arenicola marina (Howie, 1984 for review) are
well-known examples of retroaction in gametogencsis of polychaetes. They are not related, however, to the system
of gamete-brain-soma interaction discussed here for members of the family Nereidae.
ACKNOWLEDGEMENTS
I am indebted to J. Fleck for reading and commenting upon the manuscript. The valuable advice of an
anonymous referee and of D.J. REIS IT is gratefully acknowledged.
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und zur Feinstruktur der Spermalogenese bei Platynereis dumerilii (Annelida: Polychaeta). Doctoral Dissertation.
Ruhr-University, Bochum. 104 pp.
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HAUENSCHILD. C., 1951. Nachwcis der sog. atoken Geschlechtsform des Polychaeten Platynereis dumerilii (Aud. &
Milnc-Edw.) als eigene An auf Grund von Zuchlversuchen. Zool. Jb. Physiol.. 63 : 107-128.
HAUENSCHILD, C.. 1956. Hormonalc Ilcmmung der Geschlechtsreife und Metamorphose bei dem Polychaeten
Platynereis dumerilii. Z. Naturf '., Jib : 610-611.
Hauenschild. C.. 1965. — Hormone bei Nereiden und anderen niederen Wirbellosen. Zool. Jb. Physiol.. 71 : 511-544.
HAUENSCHILD, C.. 1966. — Der hormonelle EinfluB des Gehirns auf die sexuelle Entwicklung bei dem Polychaeten
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Hauenschild, C., 1970. Bezichungcn zwischen Gehirnhormon und Geschlcchtsdifferenzierung beidem
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HOFMANN, D.K.. 1966. — Untersuchungen zur Regeneration des Hinterendes bei Platynereis dumerilii (Audouin & Milne-
Edwards) (Annelida, Polychaeta). Zool. Jb. Physiol.. 72 : 374-430.
HOFMANN. D.K., 1975. Analysis of the relationship between regeneration, maturation and endocrine system in the
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Source : MNHN. Paris
7
Bioaccumulation du fer dans le corps cardiaque
de Raricirrus beryli Petersen & George
(Polychaeta, Ctenodrilidae)
Jean VOVELLE* Man ’ E . PETERSEN ** Michele GRASSET *
<£ Patricia BEAUNIER ***
*Laboratoire d'Mistologie ct Cytologic des In vertebras Marins
Universite P. ct M. Curie
12. rue Cuvier, F-75005 Paris, France
**Zoological Museum, University of Copenhagen
Universitctsparken 15, DK-2100 Copenhagen 0, Denmark
*** Service de Microscopie electronique GRMP
Universite P. el M. Curie
6, rue Cuvier, F-75005 Paris, France
RESUME
Raricirrus beryli , loealement abondant dans les champs petroliferes de la merdu Nord septentrionale. est reconn u comme
une especc indicatrice pour les sediments pollues par les hydrocarbures. Le materiel provient de deux recoltes : a proximite
nord de la Beryl Platform (mai 1982) et a 200 m nord du premier site (mai 1985). Sa conservation a permis d'entreprenclre une
etude microanalytique (au moyen de la microsonde en dispersion de longueur d'onde, du microanalyseur ionique et de la
microsonde en dispersion d'energie) et d'obtenir des indications sur sa structure cytologique. L'organe etudie est le corps
cardiaque. dont le role possible de detoxification peut se traduire par des differences entre les specimens des deux recoltes. Les
elements detectes par la microanalyse sont surtout le fer. et en quantites moindres du calcium, soufre, phosphore et aluminium.
Les autres elements rcperables sont le magnesium, le chlore, des traces de cuivre, de vanadium et de fluor ; zinc et silice sont
absents. Le fer a cte identifie a 1'echelle ultrastructurale sous la forme de particules intracytoplasmiques de ferritine,
concentrees souvent dans des inclusions delimitees par une membrane ou intdgrdes a des granules spherulaires. La difference
entre les deux recoltes se manifesto dans la teneur en fer, trois fois plus forte dans les specimens a proximite de la plateforme.
Chez quelques uns d'entre eux. le fer apparait a 1'echelle ulUastructurale comme un feutrage d’aiguilles entourant certaincs
spherules. Cette surcharge complique la fonction hematopoietique supposee du corps cardiaque, on suggere qu'elle joue un role
dans la detoxification.
ABSTRACT
Iron bioaccuimilation in the heart body of Raricirrus beryli Petersen & George (Polychaeta, Ctenodrilidae)
VovELLE, J.. PETERSEN, M.E., GRASSET. M. & P. BEAUNIER, 1994.- Bioaccumulation du fer dans le corps cardiaque de
Raricirrus beryli Petersen & George (Polychaeta, Ctenodrilidae). In: J.-C. DAUVIN. L. LaUBIER & D.J. REISH (Eds), Actes de
la 4eme Conference intern ationale des Polychetes. Mem. Mus. nain . Hist. nat.. 162 : 73-80. Paris ISBN 2-85653-214-4.
Source : MNHN , Paris
74
J. VOVELLE, M.E. PETERSEN. M. GRASSET & P. BEAUNIER
Raricirrus beryli , which is abundant in the oilfields of the northern North Sea. has been recognised as an indicator species for
hydrocarbon-polluted sediments. The material came from two different sites in the North Sea: one just north of the Beryl
platform May 1982). the other 200 meters north or the platform (May 1985). A microanalytical study was earned out using a
wavelength X-ray spectrometry microprobe, an ion microanalyser, and an energy dispersive spectrometry microprobe. The
cytological structure of the dorsal heart body was studied from sections embedded in araldite. The elements detected under
microanalysis were mainly iron and small amounts of calcium, sulfur, phosphorus, aluminium, magnesium, chlorine, copper,
vanadium and fluorine. Neither zinc nor silica were detected. Iron was identified as a form of inlracytoplasmic ferritin particles
which were concentrated in membrane-bound inclusions or integrated with spherular granules. The main difference between
the two sites was in the amount of iron, which was three times greater in specimens close to the platform as in those from 200
meters. Iron was detected at the ultrastructural level in the form of needles surrounding some of the spherules from some
specimens collected near the platform. This overload of iron is not in keeping with the supposed haematopoietic function of the
heart body, it is hypothezed that it plays a part in the detoxification process.
INTRODUCTION
L'animal retenu pour cette dtude, Raricirrus beryli, a 6t6 ddcrit en 1991 (Petersen & George, 1991) et
reconnu comme une nouvelle esp£ce de polych&te indicatrice pour les sediments polluSs par les hydrocarbures
(Moore, 1991). Les dchantillons qui out permis notre recherche out recucillis dans deux sites diffdrents : l'un
a proximity de la plateforme pdtroli&re Beryl dans la mer du Nord, l'autre 200 m plus loin. Meme si l’dcari de
temps qui sdparc les deux rdcoltes relativise la rigueur de nos conclusions, la difference d’aspect des corps
cardiaques des animaux dans les deux rdcoltes impose l'hypoth£se de leur intervention dans un processus de
detoxification. Leur conservation ne permettait pas d'envisager une etude cytologique fine, mais du moins
l'appreciation de differences significatives dans leur composition eiementaire, par les methodes de la microanalyse
k rechelle structural et ultrastructurale.
L'interpretation du corps cardiaque present chez cinq families de Polychetes a fait I’objet de nombreux travaux.
Si 1'on admet maintenant son homologie avec le tissu chloragogene "extravasal" qu'on trouve dans d’autres
families, on sait aussi que ce dernier a pu etre decrit comme un rein d'accumulation avant qu'on examine son role
dans l'h&natopoifcse. La priorite de cette fonction est dorenavant acceptee aussi bien pour le corps cardiaque que
pour le tissu chloragogene, mais son intervention peut interesser aussi bien la degradation et peut-etre le recyclage
du pigment respiratoire que sa biosynthese. A cote de 1'accumulation de produits accessoires decrite par Kennedy
& Dales (1958) comme le resultat du catabolisme des metalloporphyrines, l'intervention possible des corps
cardiaques dans des processus de detoxification a ete evoquee dans leur potentiality de sequestration d'eiements
exogenes figures ou non (Braunbeck & Dales, 1984). Enfin, dans les incertitudes meme de son utilisation, le
concept de "chloragosome" prend en compte dans les travaux r6cents (Ouaghi & GRASSET, 1991) une possibilite
de bioaccumulation progressive notamment du fer. Une telle bioaccumulation pourrait-elle etre l'indice indirect
d'un etat physiologique modifie par la surcharge environnementale en hydrocarbures? A travers l'hypoth&se d'une
detoxification chez une espece priviiegiee, e'est done aussi k l'interpretation du role du corps cardiaque en
conditions normales que notre travail tente de contribuer.
MATERIEL ET METHODES
Le materiel utilise pour cette etude provient de deux recoltes differentes. Tune et 1'auire de la mer du Nord
septentrionale : l'une pr£Iev6e juste au nord ("close up N" = CU N) de la plateforme petrolifcre Beryl (mai 1982),
l'autre 200 metres au nord (200 N) du point precedent (mai 1985). Les animaux ont ete fixes au formol k 10 % et
le preievement CU N a ete ensuite transfere dans l'alcool ethylique k 80 °C.
Les specimens examines ont ete tromjonnes au niveau du corps cardiaque (au deD du 9e s6tigere) et inclus
dans l'araldite apres deshydratation k l'alcool. L'anatomie microscopique a ete etablie sur coupes transversales
Fig. 1. A. Region dorsale (specimen 15, CU N). Coupe transversale semi-fine coloree au bleu de Toluidine (barre 50 pm);
v : espace sanguin ; B. Detail du corps cardiaque (specimenl3, 200 N), meme preparation (barre 10 pm) ; C, D, E, F.
Micrographies electroniques sans post-osmication ni coloration (barre 200 nm pour C et E. 100 nm pour D et F) ; C.
Spherule entouree d’aiguillcs d'oxyde de fer (specimen 1 8 CU N). D. Granule de ferritine (specimen 5, 200 N), E. Spherule
homogene enrichie supcrficiellement en ferritine (specimen 4, 200 N), F. Particules intracytoplasmiques de ferritine
(spdcimenl8, CU N), G. Images d’emission ionique (sp6cimenl5, CU N). 27+ : Al. 40+ : Ca, 56+ : CaO + Fe (meme
echelle que A).
Source : MNHN. Paris
BIO ACC U M U L. ATION DU FER CHEZ RARICIRRUS BERYU
75
Source ; MNHN, Paris
76
J. VOVELLE, M.E. PETERSEN. M. GRASSET & P. BEAUNIER
semi-fines colonies au bleu de toluidine, l'fetude cytologique ultrasiructurale sur coupes ultra-fines non colorfees.
La fixation initiale et le mode de conservation du materiel ne pouvaient permettre qu'une approche grossifere des
ultrastructures, excluant toute post-osmication et toute identification des organites et des membranes.
L'fetude microanalytiquc a fait appel b trois instruments diffferents.
- sur coupes semi-fines, aprfes montage sur terphane carbon6, microsonde MS 46 Cameca fequipfee dc
spectrographes dispersifs en longueur d’onde b cristaux K AP et PET (diamfetre de sonde 1 pm);
- sur coupes semi-fines fetalfees sur support de platine, microanalyseur ionique Cameca SMI 300 (spectres
acquis sur tout le champ image, diamfetre 260 pm);
- sur coupes ultra-fines montees sur grille de cuivre, microscope felectronique Temscan JEOL JEM CXII
fequipfe d'un d6tecteur de rayons X b selection d'fenergie (EDS) LINK module AN 10000 b cristal SI(LI). Tension
d'accfelferation 60 kV. Surface analysfee pour chaque spectre 50 xlOO nm, temps dc comptage 300 s.
Vingt-cinq individus out fetfe examines b l'fechellc photonique (15 pour 200 N. 10 pour CU N), 20 b 1'fechclle
ultrastructurale, 18 en microanalyse par dispersion de longueur d'onde, permettant la selection des quatre retenus
pour la microanalyse par dispersion d'fenergie el des deux 6ludi6s au microanalyseur par Emission ionique
secondaire.
RESULT ATS
L'examen b la loupe des vers provenant des deux rfecoltes permet de reconnaitre le corps cardiaque, dorsal et
visible b travers l'fepithfelium, comme une ligne pigmentfee plus ou moins sinueuse partant du 8 ou 9 feme sfetigfere
et courant sur les 10 a 15 suivants. Brun noiratre, il apparait plus fonefe et plus fepais pour les individus provenant
du lot CU N que pour ceux de 200 N.
anatomie microscopique ET HISTOLOGIE (Fig. 1A-B). — De section circulate en coupe transversale,
l'organe est suspendu entre l'fepiderme ct le tractus digestif par un mfesotlifelium qui se dilate localement pour
former un ou plusieurs vaisseaux. La masse compacte de cellules constituant le corps cardiaque baigne ainsi dans
un espace vasculaire plus ou moins dfeveloppfe, dfelimitfe par une "basale" extracellulaire ("vascular lamina")
supportant exterieurement les corps cellulaires d'un revetement pferitonfeal (myomfesothfelium), et sans doutc
inflfechie pour delimiter le pourtour du corps cardiaque. Cc dernier prfesente en coupe une douzaine de cellules b
noyau x pourvu d'un gros nuclfeole, pferiphferiques p<u‘ rapport b leurs inclusions de taille et de contraste divers,
certaines trfes opaques, d'autres jaunatres et translucides.
Kennedy & Dales (1958) ayant signalfe l'feventualitfe du dfeveloppement du corps cardiaque avec l'age et la
bioaccumulation, nous avons comparfe pour les deux lots de Raricirrus plusieurs systfemes indicateurs.
Les valours obtenues (n= nombre d'individus fetudifes) ne marquent pas de difference significative en ce qui
conceme :
- le diamfetre du corps au niveau examine :
200 N : 251 ± 16 pm, n = 5; CU N : 274 ± 18 pm. n = 7
- le diamfetre du corps cardiaque :
200 N : 35 ± 9 pm, n = 14; CU N : 36 ± 8 pm, n = 11.
L'intfegritfe des cellules est identique dans les deux lots. Le dfeveloppement de l'espace vasculaire pferiphferique
est variable dans les deux lots, peut etre plus souvent important pour CU N. Par contre, on reconnait davantage
d'inclusions Claires pour 200 N.
CYTOLOGIE (Pig. 1C-D-E). — La preparation du materiel b notre disposition ne permet qu'une appreciation
incomplete des ultrastruc lures : les membranes sont rarement identifiables, les noyaux et certains organites
(mitochondries) alteres et on devinc a peine certains trajets canaliculaires intracytoplasmiques. L'absence la plus
regrettable conceme les vacuoles qui doivent concentrer le pigment respiratoire. Ceci acceptfe, on peut faire
l'inventaire et la description dc divers types d'inclusions, plus ou moins contrastfees et dont l'opacitfe aux felectrons
est en partie attribuable b un mfetal prfesent naturcllcmcnt, que la microanalyse dfesignera comme du fer.
La majoritfe des inclusions des cellules du corps cardiaque correspond dans les deux lots b des sphferules rfeguliferes
de diamfetre moyen 0,9 pm (jusqu'ft 1,5 pm) d'un matferiau homogfene modferfement contrastfe, cl la pferiphferie
desquelles on devine parfois une membrane. Elies peuvent etre regroupfees en amas moruliformes (jusqu'a
2,5 pm), parfois cernfees d’une couche externe moins dense el plus souvent, dans les deux lots, d’une zone
contrastfee de particules que nous reconnaitrons comme de la ferritine (Fig. IE). Cette ferriline peut envahir
complfetement la spherule dans une rfepartition regulifere ou localisfee.
Distincts des sphferules par leur contraste et leur diamfetre moyen (0,3 pm. Fig. ID) des amas arrondis de
ferritine. sans apparence de membrane pferiphferique, sont fegalement prfesents dans les deux lots. Les particules
BIO ACCUMULATION DU FLR CHEZ RARICIRRUS BERYL!
77
constitutes sent plus ou meins organises, encore qu'on n'y observe jamais de plages pseudocristallines telles
flu on en connait dans les inclusions comparables du tissu chloragogfene des Sabellidae (Ouaghi 1989) et
Serpulidae ( Vovelle et al. ,199 1 ). On recommit dans les memes cellules des plages plus petites (0,2 urn) et moins
organises des memes particules, assuremem intracytoplasmiques, it contours iruSguliers (Fig. IF). Ces particules
fenitin like pour quelques auteurs (mais que nous confiimerons par la microanalyse) apparaissent isol6ment en
plus ou moins grande density dans l'ensemble du cytoplasme. A grossissement convenable, leur taillc (environ
12 nm) et leur conformation fournissent un nouvel ei&nent ^identification.
Line partie de ces inclusions est comparable <t cellcs d^crites par divers auteurs (i.a. Friedman & Weiss
1980_; Ouagiii & Grasset, 1991) dans les corps cardiaques el tissus chloragogfenes de diverses Polycheles et
peut etre mterprC-tde dans le cycle de l'h6matopoi6se. Les spherules homogenes sont originales et nous hdsitons it
leur donner un rapport de filiation avec les "granules de ferritinc", meme si elles peuvent se charger de particules.
On les distingue en tout cas des inclusions Claires lipidiques it membrane qu’on peut identifier dans quelques
specimens des deux lots. ^
f255c
'X
FIG. 2. — Microanalyse en selection denergie sur coupes ultra fines (specimen 18. CU N) A. Granule de ferritine. B. parlic
centrale dune spherule homogene. C. Feuirage d’aiguilles peripherique a une spherule. Tension d’acceleration 60 kV, temps
de comptage 300 s. En blanc sur les schemas : surface analysce; c : nombre de coups.
78
J. VOVELLE, M.E. PETERSEN. M. GR ASSET & P. BEAUNIER
II appartienl ft deux individus sur neuf examines dans le lot CU N de presenter une surcharge originate des
spherules homogEnes : dans certaines plages cellulaires elles sent recouvertes sur une Epaisseur de 0,1 pm d’un
feutrage d'aiguilles ft fort contraste, alors que leur matiEre fondamentale est souvent chargee de particules de
ferritine (Fig. 1C). Ccs aiguilles de dimension moyenne 50 nm Evoquent celles que nous avons dEcrites en filiation
d'inclusions°de ferritine dans la biominEralisation cuticulaire des machoires d'un Eunicien (VOVELLE et al., 1989)
ou celle que Coulon el al. (1987) ont reconnues dans des conditions de pollution naturelle ft la surface des
filaments de byssus de moules. Ces auteurs y ont identify des oxydes mEtalliques (hematite principalement) et
celte interpretation est ft prendre en compte pour notre materiel.
M1CROANALYSE. — Sped romet vie de rayons X en dispersion de longueur d'onde. On a d'abord examine deux
individus differents dans chacun des lots. Les elements presents ont EtE reconnus et appreci6s ft partir de
moyennes etablies sur une dizaine de points (1 pm environ) particulierement emissifs dans deux ou trois coupes
voisines de chaque echantillon. Ixs elements reconnus sont en ordre d'importance Fe, S, Ca, P, Al et Cu (traces).
La recherche de Zn et V, suggeree par leur existence dans le tissu chloragogEne des Serpulidac, n’a pas domte de
reponse significative. Les valeurs obtenues pour Al ne presentent pas de variation notable entre les deux lots (non
plus que celles de Cu). Les valeurs moyennes concemant les ElEments majeurs ont EtE companies aux valeurs
maximales obtenues pour chaque Echantillon, par rapport auxquclles elles sont minorees dans la proportion d’un
tiers. Si on compare les deux lots, les moyennes pour Ca et P sont majorEes pour le site CU N, et encore plus en ce
qui conceme S et surtout Fe.
Dans un deuxiEme temps on a done apprEciE systEmatiquement, en retenant les memes dEfinitions de valeurs
moyennes, I'intensitE de rEponse du fer, en parallEle avec celle du soufre, pour 9 individus du lot CU N et 7 du lot
200 N. Les valeurs moyennes et maximales pour Fe sont multiplies par trois pour la rEcolte la plus proche de la
station Beryl. Ce ci reprEsente une moyenne de :
CU N : 145 ± 60 c/s (max. 252), contre 200 N : 58 ±31 c/s (max. 89).
En ce qui conceme le soufre, les valeurs obtenues sont :
CU N : 43 ± 17 c/s (max. 58), contre 200 N : 25 ±10 c/s (max. 36).
Le soufre ne prEsente done pas une Evolution aussi marquEe que le fer. Si 1'on compare les valeurs obtenues ft
cedes concernant le tissu chloragogEne et le corps cardiaque des Sabellidae, Serpulidae el Amphictenidae
(Vovelle el al., 1991), elles apparaissent plus faibles, car obtenues sur coupes semi-fines, mais surtout la
participation du phosphore est minorEe, cede du soufre plus importante.
Microanalyse par emission ionique secondaire. Les renseignements exploitEs concement les spectres
d'Emission d'ions secondaires positifs et nEgatifs et les images obtenues pour les ElEments les plus Emissifs. Un
individu de chaque lot a EtE examinE.
Sur les spectres d’Emission les ElEments identifies sont par ordre d'importance Ca (40+), Fe (56+), Al (27+), S
(32-), Cl (35 ) imputable en partie ft la rEsine, P mal servi par la mEthode mais present dans diverses combinaisons
(POCa 87+), Mg (24+) et Cu (63+) comme intervenants mineurs, et F (19 ) en traces. Ces Evaluations intEgrent
l'analyse d'une surface de 200 pm de diamEtre, supErieure ft cede de l'organe en coupe.
L'analyse des images obtenues ft partir des masses prEsentant la meilleure intensitE d'Emission, 56+, 40+, 27+
(Fig. 1G), impose qu'on tienne compte du contraste entre l’organe considErE et les tissus environnants, pour
apprEcier une concentration locale de 1'ElEment identifiE. La masse 56+ imputable ft Fe plus qu'ft CaO prEsente le
meilleur contraste, alors que Ca et surtout Al sont prEscnts dans les autres parses de la coupe.
Meme si la rEponse du fer est meilleure sur l'Echantillon provenant du lot CU N. cede mEthode ne permet pas
d’apprEcier quantitativement des diffErences significalives entre les vers des deux provenances.
Spectrometrie de rayons X en selection d'tnergie. Cct examen ft l’Echelle ultrastructurale sur coupes fines
fournit des spectres correspondants pour les divers types d’inclusions ft des surfaces analysEes de 100 X 50 nm.
Une approximation de 1’importance relative des divers ElEments presents dans chacun d’eux a EtE obtenue pour
deux Echantillons de chaque lot en comparanl r importance des pics obtenus dans des conditions identiques,
exprimEe en coups. Les ElEments reconnus correspondent dans l’ordrc d’importance aux pics Fe, 0, Al, S. P et Ca.
On les identifie dans les accumulations de ferritine, dans les sphErules homogEnes et dans le feutrage d’aiguilles
pEriphErique ft certaines sphErules du lot CU N.
En ce qui conceme le fer, la rEponse maximale est de 35 ± 9 coups dans le cytoplasme, 86 ± 18 et 102 ± 39
coups au centre des sphErules homogEnes claires (200 N et CU N), mais les sphErules chargEes de ferritine
peuvent en prEsenter davantage, 183 ± 36 (200 N) et 155 ± 20 (CU N) dans les amas arrondis de ferritine, jusqu’ft
277 ± 80 dans le feutrage pEriphErique (CU N).
BIOACCUMULATION DU TER CHEZ RARICIRRUS HER YU
79
La presence de l'oxygfene, notable sur les spectres, est contingente du carbonage des grilles. Celle de
l'aluminium est confirmee dans tous les cas, sans indication d'accumulation particulidrc dans les spherules, ni de
difference marquee selon les provenances.
Le rapport du phosphore au soufre est significatif, leurs deux pics sont altemativement preponderants. Le
phosphore est plus important que le soufre dans les accumulations de ferritine, ce qui n'est pas aussi net dans les
feutrages en aiguilles. Le soufre (organique?) a la priori te au centre des inclusions spherulaircs. La presence du
phosphore dans la ferritine est generalement acceptee ; nous interpretons celle du soufre dans les spherules clairs
en rapport avec une composante protdique probable, comportant dcs acides amines soufr6s.
DISCUSSION ET CONCLUSIONS
Les trois methodes de microanalyse utilisees ne concement pas le meme champ dimcnsionnel, l'unc presentam
la repartition des elements dans I'animal. l'autre dans l'organe, la demi&re au niveau uitrastructural dcs inclusions
cellulaires. Leurs performances mais aussi leurs deficiences par rapport k certains elements sc competent. La
convergence des rdsu I tats obtenus permet de proposer un inventaire des elements majeurs concentres par le corps
cardiaque : fer, calcium, soufre et phosphore, les elements mineurs ou traces ne presentam aucun caractere
original. La presence notable de l'aluminium est confirmee par les trois methodes, elle conccrne l'ensemble des
tissus de I'animal sans enrichissement considerable au niveau du corps cardiaque, ni difference marquee entre les
deux sites. S'agit-il d'un element artefactuel, induit par une des manipulations preparatoircs ? II est impossible
actuellement de le d6montrer. Les elements reconnus dans les deux lots de provenance difl'erentc sont identiques.
Ils sont tous interpretables en rapport avec une fonetion hematopoietique de l'organe. La seule donnde apportee
par l'dtude de microanalyse (microsonde MS 46) pour differencier les vers de CU N et de 200 N concerne
I'abondance du fer dans le corps cardiaque dont la valeur triple k proximite de la plateforme, sans qu'aucun autre
element ne presentc une bioaccumulation correlative.
Cette surcharge imputable k un seul metal implique dans le metabolisme du pigment respiratoire est en bon
accord avec deux autres donnees, morphologique et ultrastructurale. Morphologiquement il s'agit de l'indice de
dep;irt, l'intensite de la pigmentation brun noir de l'organe, rcnforc6e pour le lot CU N. A l'echelle ultrastructurale
il s'agit de la presence spedfique dans des individus du meme lot de depots ferriques en aiguilles peripheriques k
certaines inclusions. Cette forme d'accumulation du metal, dont la reversibilite est moins evidente que pour la
ferritine, dvoque une surcharge qu'on peut raisonnablement mettre en rapport avec une h6matopoiese et un cycle
du pigment respiratoire sollicites par les conditions environnementales. Les conditions de conservation des
animaux ne permettent pas de ddcrire davantage la cytophysiologie des corps cardiaques de Raricirrus, qui pourra
etre prdcisde dans une dtude ultdrieure, mais elles nous autorisent ddjh k envisager un rapport entre celle forme
spdcifique de bioaccumulation du fer et un processus de detoxification dcs animaux exposes h un milieu riche en
hydrocarbures.
BIBLIOGRAPHIE
Brauxbeck. T. & DALES, R. P.. 1984. The role of the heart body and of the extravasal tissue in the disposal of foreign cells
in two polychaete annelids. Tissue & Cel! , 16 : 557-563.
COULON, J.. TRUCHET, M. & MaRTOJA, R., 1987. — Chemical features of mussels (Mylilus edulis) in situ exposed to an
effluent of the titanium dioxyde industry. Annls Inst. Octanogr 63 : 89-100.
FRIEDMANN, M.M. & WEISS, L., 1980. An electron microscopy study of hemoglobin synthesis in the marine annelid
Amphitrile ornata (Polychaeta Terebellidae). J. Morphol. , 164 : 121-138.
KENNEDY, G.Y. & Dales, R. P.. 1958. — The function of the heart-body in the Polychactes. J. mar. biol. Ass. U.K.. 37 : 15-
31.
MOORE, D.C., 1991. — Raricirrus beryli Petersen & George (Ctenodrilidae): a new Polychaete indicator species from
hydrocarbon-polluted sediments. Ophelia Suppl., 5 : 447-486.
OUAGHI, E. M., 1989. — Bioaccumulation naturelle du fer chez Sabella pavonina S. (Annelide Polychete). C.R. Acad. Sci.
Paris , 308 : 237-244.
OUAGHI, E. M. & GRASSET. M., 1991. Synthesc et exocytose de chlorocruorine et mise en reserve du fer par le tissu
perivasculaire d'un annelide polychete. Can. J . Zool.. 69 : 2338-2348.
80
J. VOVELLE, M.E. PETERSEN. M. GR ASSET & P. BEAUNIER
PETERSEN, M. E. & George, j. D.. 1991. — a new species of Raricirrus from northern Europe, with notes on its biology and
a discussion of the affinities of the genus (Polychaeta: Ctenodrilidae). Ophelia, Suppl., 5 : 185-208.
VOVELLE. J.. GRASSET. M. & TRUCHET, M., 1989. — Biomineralisation des mac ho ires chez Hyalinoecia lubicola (Muller)
(Polychete. Eunicida). Annls Inst . Ocdanogr.. 65 : 15-36.
VOVELLE, J.. GRASSET. M. & TRUCHET, M., 1991. — Sites of biomineralization in the Polychaete Pomatoceros triqueter
(Serpulidae) with comments on some other species. Ophelia, Suppl.. 5 : 661-667.
Source : MNHN, Paris
8
Functional ciliary groups of the feeding palps
of Spionid polychaetes
Daniel M. DAUER
Department of Biological Sciences
Old Dominion University
Norfolk. Virginia, USA 23529
ABSTRACT
Functional ciliary groups of the feeding palps of spionid polychaetes are reviewed. Six functional ciliary groups have
been observed: frontal cilia, latero-frontal cirri, lateral cilia, ciliated papillae, non-motile cilia of the frontal surface and
basal transverse cilia. The number of functional ciliary groups present on any species varies from one to four groups.
Some ciliary groups, e.g. frontal cilia, are present on the palps of many species while other groups, e.g. basal transverse
cilia, are unique to a single species. Additional studies are necessary to clarify the roles of and possible interactions
between (1) functional ciliary groups. (2) mucus and (3) hydrodynamics in particle encounter, retention, transport and
rejection.
RESUME
Croupes ciliaires fonctionnels des palpes "trophiques" des polychetes Spionidae
Une revision dcs groupes ciliaires fonctionnels des palpes "nutritionnels" des polychetes Spionidae est entreprise.
Six groupes ciliaires fonctionnels ont ete observes : cils frontaux. cirres latero-frontaux, cils lateraux. papilles cilides,
cils non mobiles de la surface frontale et cils transverses frontaux. Le nombre de groupes ciliaires fonctionnels presents
chez chacune des especes varie de un a quatre. Quelques groupes ciliaires. coinme les cils frontaux. sont presents sur les
palpes de beaucoup d’especes tandis que d’autres groupes, comme les cils transverses basaux. ne sont presents que chez une
espece. Des etudes complementaires sont necessaires pour clarifier les roles et les interactions possibles enue (1) groupes
ciliaires fonctionnels, (2) mucus, (3) hydrodynamique dans la rencontre, la retention, le transport et le rcjet des particules.
INTRODUCTION
Spionid polychaetes are common inhabitants of infaunal and epifaunal communities of marine and estuarine
habitats. The ciliated peristomial palps of spionid polychaetes function in (1) feeding behavior (Fauchald &
JUMARS. 1979), (2) inter- and intraspecific interactions (LEVIN. 1981) and (3) tube construction (MORTENSEN &
Galtsoff, 1944). In feeding behavior die palps may function in particle encounter, retention, transport, and
rejection (e.g. Taghon el al., 1980; Dauer et al. , 1981). Spionid polychaetes use their palps to capture particles
in suspension, bedload transport and deposited at the sediment surface; direct deposit feeding using the everted
DAUER. D.M.. 1994. Functional ciliary groups of the feeding palps of Spionid polychaetes. In: J.-C. Dauvin.
L. LauBIER & D.J. REISII (Eds), Actes de la 4eme Conference internationale des Polychetes. Mem. Mus. natn. Hist, run.,
162: 81-84. Paris ISBN 2-85653-214-4.
Source : MNHN. Pans
82
D.M. DAUER
pharynx has also been observed (Daro & Polk, 1973; Wilson, 1983). The potential rapid flux between
suspended, bedload, and deposited stales caused DAUER et al (1981) to classify spionids as interface feeders. In this
paper studies concerning the role of cilia on the palps are reviewed and areas of future research discussed.
DISTRIBUTION OF FUNCTIONAL CILIARY GROUPS WITHIN AND BETWEEN SPECIES
Studies combining feeding behavior and detailed morphological observations have been performed for eight
spionid species and Table 1 summarizes the distribution of ciliary groups among these species. Spionid
polychaetes with a median ciliated food groove have one or more of the following five functional groups of cilia
on their palps: (1) frontal cilia that line the median groove of the palp, (2) latero-frontal cilia organized as
compound cilia (cirri), (3) lateral cilia that beat in metachronal waves, (4) non-motile cirri located at the tips of
papillae, and (S) basal transverse cilia at the base of the palp. Within a species, the number of functional ciliary
groups varies from one to four. For example, Malacoceros indicus has only frontal cilia lining the food groove
(Dauer & Ewing 1991) and Paraprionospio pinnata has four ciliary groups - frontal cilia, latero-frontal cirri,
lateral cilia and basal transverse cilia (Dauer. 1985). Between species, some ciliary groups, e.g. frontal cilia, are
present on the palps of many species while other groups, e.g. basal transverse cilia, are unique to a single species.
Scolelepis squamata and S. hutchingsae lack a median food groove and die cilia of the palps are non-motile and
organized into numerous transverse rows (Dauer, 1983, 1987).
TABLE 1. — Distribution of ciliary groups among the Spionidae.
(from 1- Dauer, 1983; 2- DaUER. 1984; 3- DaUER. 1985; 4 - DaUER, 1987; 5 - Dauer, 1991; 6 - Dauer & Ewing, 1991).
X: ciliary or cirral group is present. — : ciliary or cirral group is absent.
FEEDING BEHAVIOR
The ciliary groups of the palps of spionid polychaetes may function in particle encounter, retention, transport,
and rejection. Particle capture implies particle encounter and subsequent retention. Particle transport implies the
movement from the site of capture to the pharynx. Particle rejection implies that the particle is not ingested after
capture and would include loss during u*ansport as well as transport away from the pharynx.
Particle encounter in the deposit feeding mode occurs as the frontal surface of the palp is placed onto the
sediment surface and can be predicted as a function of panicle size with larger particles having a higher probability
of being encountered (Jumars et ai, 1982). In the suspension feeding mode, particle encounter prediction is a
function of encounter mechanism (direct interception, inertial impaction, gravitational deposition, diffusional
deposition, electrostatic attraction, SHIMETA & Jumars, 1991). The frontal surface of the palp is the site of
particle encounter, but the ciliary groups of Table 1 probably have no role in particle encounter dynamics of
deposit feeding and could only have a role in suspension feeding if currents produced by the cilia of the palps
altered ambient flow conditions. Dauer (1984, 1985) hypothesized that both the latero-frontal cirri and lateral cilia
of P. pinnata and Streblospio benedicti created currents that increased particle encounter during suspension feeding.
Ciliary currents would be functional only in low ambient flows such as in highly deposilional environments or
close to the sediment surface in the bottom boundary layer.
Source :
FUNCTIONAL CILIARY GROUPS OF SPIONID TROPHIC PALPS
83
Retention of particles in spionid polychaetes is assumed to be due to the adhesive properties of mucus secreted
on the frontal surface and the interaction of mucus and surface properties of the particle (roughness, organic
coatings) (Jumars et al. , 1982). Hydrodynamic particle retention, produced by cilia of the palps (sensu Jorgensen
1981, 1982), again could only occur under low ambient flow conditions or when the collection surface is sheltered
from ambient flow (Shitema & Jumars, 1991). Mucus is particularly important in particle retention of the
Scolelepis spp. The non-motile cilia of the Scolelepis spp. were interpreted by Dauer (1983, 1987) as providing a
rough textural surface to retain die particle-mucus complex which was transported to the pharynx by complete
retraction of the palp frontal surface directly onto the pharyngeal surface. Dauer (1987) hypothesized this
mechanism was an adaptation to the highly turbulent habitat occupied by both species and minimized the loss of
particles during transport along die food groove of the palp as envisioned by Self & Jumars (1978). Particle
retention during transport can also be a function of the depth of the food groove. For example, in P. pinnata the
food groove is deep and wide and particles up to 100 pm in greatest dimension were completely enc-losed by the
lateral edges of the frontal surface during transport to the pharynx (Dauer, 1985). Particles less than 100 pm
make of the vast majority of particles ingested by P. pinnata (Dauer, 1980; Luckenbacti et al .. 1988).
Particle transport to die pharynx, as a particle-mucus complex, is primarily accomplished by the beating of the
frontal cilia in those spionids with a median food groove. For the Scolelepis spp. die non-motile cilia of die
frontal surface serve indirectly in particle transport by holding the particle-mucus complex onto die frontal surface
as die palp contracts onto die pharynx (Dauer, 1983).
Frontal cilia may also function in particle rejection from die pharynx by a reversal of the direction of ciliary
How. This mechanism has been observed only in Polydora ligni (Dauer et al., 1981). The basal transverse cilia of
P. pinnata function in particle rejection by die production of a rejection current within die tube. Particles rejected
at the site of the pharynx are rejected into die current produced by the beating of the basal transverse cilia and the
frontal cilia of the branchiae (Dauer, 1985). Dauer (1988) hypothesized that die particle rejection current of
P. pinnata enabled the animal to reject particles at the site of the pharynx while allowing the prostomium to
remain below' the sediment-water interface and thus potentially reducing predation or browsing. In odier spionid
species the everted pharynx is held al the sediment surface or die edge of die lube and particles are rejected directly
onto the sediment-water interface.
The ciliated papillae of spionids do not appear to have any direct function in feeding behavior. Dauer (1991)
hypothesized that the papillae of the palp arc primarily mechanosensory structures that may be important in
interspecific encounters.
The role of the lateral cilia and the latero- frontal cirri is particularly problematic. DAUER (1984, 1985) by
analogy to lamelli branch bivalves and lophophores concluded diat botii ciliary groups functioned in capturing
suspended particles by creating currents (lateral cilia) and deflecting the padiway of particles onto the frontal surface
(latero-frontal cirri). vSiiitema & Jumars (1991) consider tiiat cilia diat are not protected from ambient flow may
be more important in manipulating and transporting captured particles ratJicr than in creating feeding currents.
Latero-frontal cirri could aid in retaining the particle-mucus complex onto the frontal surface during transport.
However, it is difficult to hypothesize and role lor die lateral cilia except for the creation of a feeding current.
These cilia are adjacent to the frontal surface (to assist to particle retention) and beat in metachronal waves creating
currents directed towards die frontal surface.
CONCLUSION
Spionid polychaetes have been and will continue to be important experimental species in applying optimal
foraging tiieory to marine and estuarine systems (Taghon, 1982; Taghon & Jumars, 1984) and in understanding
the role of near-bottom hydrodynamics in feeding behavior (Jumars, 1993). Spionid polychaetes are excellent
experimental subjects for feeding studies because (1) they feed at the sediment-water interface and are easily
observed, (2) many spionid species, especially estuarine species, are relatively hardy and survive well under
laboratory experimental conditions, and (3) most species place fecal rods at the surface which can be collected and
used to estimate feeding rates quantitatively under various experimental conditions. I Iowever, interpretation of data
and observations concerning feeding of spionids is complicated because (1) they have a mixed feeding mode
(deposit feeding, suspension feeding, bedload feeding) and (2) they posses a variety of morphological features that
may affect feeding behavior. Additional studies are necessary to clarify the roles of and possible interactions
between (1) functional ciliary groups, (2) mucus and (3) hydrodynamics in particle encounter, retention, transport
and rejection.
84
D M. DAUHR
Daro, M.N. & POLK. P., 1973. The autecology of Polydorci ciliata along the Belgian coast. Nelli. J. Sea Res., 6 :
130-140.
DaUER, D.M.. 1980. — Populations dynamics of the polychaetous annelids of an intertidal habitat in Upper Old Tampa
Bay, Florida. Ini. Rev. Ges. Hydrobioi. 65 : 461-487.
DaUER. D.M.. 1983. — Functional morphology and feeding behavior of Scolelepis squamata (Polychaela: Spionidae).
Mar. Biol., 11 : 279-285.
DaUER. D.M.. 1984. — Functional morphology and feeding behaviour of Streblospio benedicti (Polychaela; Spionidae).
In: P.A. HUTCHINGS (cd). Proceedings of the First International Polychaele Conference. Published by the Linnean
Society of New South Wales: 418-429.
DAUER, D.M.. 1985. — Functional morphology and feeding behavior of Paraprionospio pinnata (Polychaela:
Spionidae). Mar. Biol.. 85: 143-151.
DaUER. D.M.. 1987. Potential systematic significance of spionid polychaete tentacular morphology. Bull. biol. Soc.
Wash.. 1 : 4 1-45.
DaUER. D.M., 1991. Functional morphology and feeding behavior of Polydora commensalis (Polychaeta: Spionidae).
Ophelia Supplement 5 : 607-614.
DaUER. D.M. & Ewing, R.M.. 1991. — Functional morphology and feeding behavior of Malacoceros indicus
( Polychaeta : Spionidae). Bull. mar. Science, 48: 395-400.
DaUER. D.M.. MAYBURY, C.A. & EWING, R.M., 1981. — Feeding behavior and general ecology of several spionid
polychactcs from the Chesapeake Bay. J. Exp. Mar. Biol. Ecol., 54 : 21-38.
FaUCJIALD, K. & JUMARS.P.A.. 1979. — The diet of worms: a study of polychaete feeding guilds. Oceanogr. Mar. Biol.
Ann. Rev.. 17 : 193-284.
JORGENSEN. C.B.. 1981. — A hydromechanical principle for particle retention in Mytilus edulis and other ciliary
suspension feeders. Mar. Biol.. 61 : 277-282.
JORGENSEN. C.B., 1982. Fluid mechanics of the mussel gill: the lateral cilia. Mar. Biol.. 70 : 275-281.
JUMARS. P.A.. 1993. Concepts in biological oceanography. An interdisciplinary primer. Oxford University Press,
New York. 348 pp.
JUMARS, P.A.. SELF . R.F.L. & Nowell, A.R.M., 1982. — Mechanics of particle selection by lentaculate deposit-feeders.
J. Exp. Mar. Biol. Ecol.. 64 : 47-70.
Levin, L.A., 1981. — Dispersion, feeding behavior and competition in two spionid polychaetes. J. mar. Res., 39 : 99-
117.
LUCKENBACH, M.W., IlUGGETT . D.V. & Zobrist, E.C., 1988. Sediment transport, biotic modifications and selection
of grain size in a surface deposit-feeder. Estuaries. 11 : 134-139.
MORTENSEN. E. & Gai.TSOFF, P.. 1944. Behavior and tube building of Polydora ligni. Biol. Bull. (Woods Hole), 87 :
164-165.
SELF. R.F.L. & JUMARS. P.A., 1978. New resource axes for deposit feeders ? J. mar. Res., 36: 627-641.
Smimeta, J. & JUMARS. P.A.. 1991. Physical mechanisms and rates of particle capture by suspension feeders. Annual
Rev. Oceanogr. mar. Biol.. 29 : 191-257.
TAGHON, G.L.. 1982. — Optimal foraging by deposit-feeding invertebrates: roles of particle size and organic coating.
Oecologia, 52: 295-304.
Tagiion, G.L. & JUMARS, P.A., 1984. — Variable ingestion rate and its role in optimal foraging behavior of marine
deposit feeders. Ecology, 65 : 549-588.
Taghon, G.L.. Nowell, A.R.M. & Jumars.P.A.. 1980. — Induction of suspension feeding in spionid polychaetes by
high particle fluxes. Science, 210 : 562-564.
Wilson, H.IL. Jr. 1983. — The role of density dependence in a marine infaunal community. Ecology. 63 : 295-306.
Source .
9
Attributes of ribosomal DNA in alvinellid
polychaetes from hydrothermal vents
David R. DIXON * Linda R.J. DIXON * & Verena TUNNICLIFFE **
* Plymouth Marine Laboratory & Marine Biological Association
Citadel Hill
Plymouth PL1 2PB, UK
** School of Earth and Ocean Sciences
University of Victoria
B.C. Canada V8W 2Y2
ABSTRACT
The ribosomal DNA (rDNA) of three alvinellid polychaetes, Paralvinella palmiformis Desbruyeres & Laubier,
l\ pandorae Desbruyeres & Laubier and P. sulfmcola Desbruyeres & Laubier, from deep-sea hydrothermal vents in the eastern
Pacific Ocean, has been subjected to restriction-endonuclease digestion and the resulting restriction fragments compared with
those of Melinna palmata Grube, a member of a closely-related polychaete family, the Ampharclidae. An interesting feature of
the rDNA of representatives of both polychaete families was the tendency to cut with restriction enzymes containing an
increased number of G-C (guanine-cytosine) bases in their recognition sequences. Increased GC-content is known to confer
greater thermal and chemical resistance to the DNA molecule. This apparent similarity between the chemical composition of
rDNA of representative alvinellids and Melinna palmata , a shallow-water species which tolerates highly-reduced and metal-
rich sediments, suggests that this character may have arisen in the distant past primarily as an adaptation to chemically stressed
environments.
RESUME
Caractcristiques de PADN ribosomal de Polychetes Alvinellides des sources hydrothermales
Les ADN ribosomaux (ADNr) de trois polychetes alvinellides. Paralvinella palmiformis Desbruyeres & Laubier, P.
pandorae Desbruyeres & Laubier et P. sulfmcola Desbruyeres & Laubier. provenant des sources hydrothermales profondes de
lest pacifique. ont etc digeres par une endonuclease de restriction. Les fragments obtenus ont etc compares avec ceux de
Melinna palmata Grube. unc annelide polychete proche de la famille des alvinellides, les amphare tides. Un aspect important de
1’ADNr des polychetes cst leur tendance h se couper avec les enzymes de restriction contenant un nombre important de
sequence de bases G-C (Guanine-Cytosine) dans leurs segments de reconnaissance. L’augmentation de la sequence en G-C esi
connue pour conferer a l’ADN une plus grande resistance thermique et chimique. Cette apparente similarite enlre la
composition chimique de l’ADNr represen tatif des alvinellides et Melinna palmata, une espece d’eau peu profonde qui tolere
les sediments fortement reduils et charges en metaux, suggerent que ce caraclere a du se dcvclopper dans le passe comme une
adaptation au stress chimique de I'environnement.
Dixon. D.R., Dixon. L.R.J. & V. TUNNICLIFFE, 1994. Attributes of ribosomal DNA in alvinellid polychaetes from
hydrothermal vents. In: J.-C. Dauvin. L. KUJBIER & D.J. REISH (Eds). Actes de la 4eme Conference internationale des
Polychetes. Mdm. Mus. natn. Hist, not., 162 : 85-92. Paris ISBN 2-85653-214-4-165-2.
Source . MNHN. Paris
86
D.R. DIXON. L.R.J. DIXON & V. TUNNICLIFFE
INTRODUCTION
The polychaete family Alvinellidae is known only from hydrothermal vents in the Pacific Ocean
(DesbruyFres & LAUBIER, 1991). Two genera are described : Alvinella widi two species and Paralvinella with
nine species at vent sites on both sides of the Pacific. Alvinella species inhabit the sides of smokers on die East
Pacific Rise only and Uicy have substantial morphological alteration such as die insertion of bacterial filaments on
the dorsum. The smoker habitat on Juan de Fuca Ridge and Marianas back-arc basin is occupied by Paralvinella
sulfincola Desbruyfcres & Laubier and Paralvinella hessleri Desbruy£res & Laubier, respectively. Odier
paralvinellid species live among vestimentiferan tubes or in sediments where the potential for high temperature
encounters is low.
The alvinellid family has several characteristics reminiscent of die hypotheucal ancestor of die terebellomorph
order. The current model of systematic relationships among die alvinellid species is based on morphological
analyses (DESBRUYfcRES & Laubier, 1991). Alvinella is the most derived genus. Widiin Paralvinella , there are
four distinct morphological subgroups: P. pandorae is die most distinct and nearest the ancestral form while P.
palmiformis and P. sulfincola belong to one subgroup marked by die form of the buccal tentacles. Although die
latter two species share many features and are often collected togedier, genetic distance based on allozymes
clearly differendates the species (Tunnicliffe et al., in press).
This study examines three species from the Juan de Fuca Ridge: Paralvinella pandorae pandorae Desbruyfcres
& Laubier, P. palmiformis Desbruybres & Laubier and P. sulfincola Desbruyfcres & Laubier. Habitat observadons
suggest that there is a preference for habitats widi vent temperatures increasing in die order listed (Fig. 1). P. p.
pandorae builds mucous sheaths in vestimentiferan clumps while P. palmiformis is sedentary but free-ranging in
these lower temperature clumps and on sulphide chimneys formed by high temperature fluids (TUNNICLIFFE et al.,
1985; DESBRUYkRES & Laubier, 1986). P. sulfincola is only found on sulphide chimneys and, in the greatest
numbers, widiin centimetres of superheated fluids (Tunnicliffe et al. , in press). Observations of die proximity of
certain species to fluid flows in excess of 100 °C challenge current dogma that molecular stabilisation in
metazoans requires temperatures less than 60 °C (Brock, 1985).
+A . pompejana +
+-A . c a u d a t a ►
< — P. sulfincola — h
P . hessleri
Fig. 1. Approximate habitat ranges of alvinellid species. Hotter temperatures may range up to 65 °C as turbulent mixing
carries blasts of hot water over the worms. There are no long-term records of chimney habitat temperatures to document
actual ranges. Spot measurements and observations are the bases for this diagram. Little information is available for P.
hessleri.
P . palmiformis —+
P . g r a s s I e / — ►
P. pandorae
We recently reported die results of experiments which showed diermal stability of rDNA from a range of
hydrothermal vent species (largely alvinellid polychaetes) was positively correlated widi environmental
temperature (Dixon et al, 1992). This was attributed to a supposed increase in G-C (guanine-cytosine) content of
the rDNA molecule. Increased G-C content confers increased thermal and chemical stability to the DNA molecule
which is dependent on the number of hydrogen bonds: A-T (adenine-thymine) base pairs are linked by two bonds
rDNA IN HYDROTHERMAL VENTS POLYCIIAETES
87
whereas G-C pairs arc linked by three (e.g. DARNELL et aL 1986). This paper presents further evidence, based on
restriction analysis results, of increased G-C levels in the rDNA of hydrothermal vent polychaetes and a dose
relative from highly-reduced and metal-rich, shallow-water environments, which suggests this character may have
arisen in the distant past primarily as an adaptation to hostile chemical conditions.
FIG. 2. Hybridisation analysis of genomic DNA from a single Paralvinella palmifonnis. (A) Photograph of 1% agarose gel
after running at 30 volts for 16 h (0.1 volts cm’1 h1) and ethidium -bromide staining, showing numerous satellite bands.
(B) After Southern transfer and hybridisation with the 2.9 kb pVW-PCR ( P . palmifonnis rDNA-) digoxygenin-labelled
probe. Lanes 1 and 14. Lambda-Hindlll DNA molecular-weight marker; Lane 2, Sail-digested Mytilus edulis genomic
DNA (control) showing a characteristic 3.6 kb fragment; Lane 3. DNA molecular weight marker, pBR328 cleaved with
Bgll and Hinfl; Lanes 4-13 , P. palmifonnis genomic DNA: Lane 4, EcoRI/HindBI double digest; Lane 5. BamHI/EcoRI
double digest; Lane 6, Sall/Hindlll double digest; Lane 7. Sall/BamHI double digest. Note, suspected partial; Lane 8,
undigested DNA; Lane 9, Sall/EcoRI double digest; Lane 10, Hindlll digest showing absence of cutting sites within the
repeat unit (cf. also lanes 6 and 13); Lane 11, EcoRI-digest; Lane 12, BamHI-digest; and Lane 13, Sail -digest.
D.R. DIXON. L.R.J. DIXON & V. TUNNICLIFFE
MATERIALS AND METHODS
Specimen collection
The three paralvinellid species were collected by submersibles on Juan de Fuca Ridge at two sites 100 kin
apart. Ten P. palmiformis specimens came from two vents on Axial Seamount (44°58.9' N, 130° 13.3' W)
and one vent on Cleft Segment (44°57.4'N, 130°I3.8'W). The three P. p. pandorae specimens came from one vent
at each site and P. sulfincola , two specimens, came from the base of a smoker at 44°58.9* N, 130° 13.3' W. Another
terebellomorph polychaete, the ampharetid M. palmata and the serpulid Pomatoceros lamarckii were collected
subtidally at Plymouth, England: the dog-whelk Nucella lapillus and the mussel Mytilus edulis came from
intertidal populations in southeast Cornwall.
Tissue handling andDNA extraction
High-molecular-weight DNA was purified by overnight digestion with proteinase K followed by repeated
phenol/chloroform extractions. All DNA samples were treated with RNAse (SAMBROOK et at., 1989). After
ethanol precipitation, DNA was vacuum dried and dissolved overnight in TE (10 mM Tris, 1 mM EDTA, pH 8.0),
and stored at 4°C for short periods or frozen at -20°C. Degraded DNA samples, identified by smearing on gels,
were not included in the analysis.
Restriction analysis
Thirteen 6-cutter restriction endonucleases (Boehringer-Mannheim) were used singly and in combination on
replicate samples of DNA : BamHI, Dra, EcoRI, EcoRV, Hindlll, Kpnl, PstI, PvuII, SacI, Sail, Smal, Xbal and
Xhol.
Approximately 2.5 mg of DNA was cut with restriction endonucleases according to the manufacturer's
instructions. The DNA fragments were sorted according to size by gel electrophoresis using a 1 % agarose gel in
TBE buffer (90 mM Tris-HCL, 0.89 mM boric acid, 2.5 mM EDTA, pH 8.3). Running conditions were 33 volts
for 22 hours at room temperature. Gels were stained with cthidium bromide, photographed using IJV-light, and llie
DNA blotted onto a nylon membrane (Genescreen, Dupont) (Southern, 1975).
rDNA probes
Homologous probes were manufactured by polymerase chain reaction (PCR), using PCR primers flanking
regions 5 to the 18S and 28S genes (e.g. HOLLAND et al. , 1991), and cloned by conventional bacterial methods. A
heterologous probe representing the entire rDNA repeat unit (pCtp 1550), (Schmidt et al., 1982) was used alter it
had first been digested with Hindlll and EcoRI to improve the labelling and hybridisation efficiencies. A non-
radioactive DNA labelling and detection procedure was employed in this study (digoxygenin, KESSLER et al.,
1990).
RESULTS
Restriction analysis
Figure 2 shows digestions of P. palmiformis rDNA with a range of restriction endonucleases, singly and in
combination. Figure 2A is a representative agarose gel stained with ethidium bromide and photographed under
IJV-light to reveal numerous satellite bands. Fig. 2B shows die same panel of DNA when transfered to a nylon
filter and labelled widi a 2.9 kb VW- PCR probe (based on P. palmiformis, 5' 18S - 5' 28S rDNA region). The
DNA fragments revealed by the probe(s) were used to map the rDNA repeal unit.
Table I shows die enzyme cutting results for diree coastal and two hydrothermal-vent species. The probe used
was pCtp 1550 (Schmidt et al., 1982) which has die potential to span the entire length of die repeat unit. Repeat
unit lengdi was estimated for the different species based on die combined lengths of die fragments produced by
Sail digestion. In die case of M. palmata, which lacks a Sail in its repeat unit, the size was estimated from the
combined fragment sizes produced by separate BamHI. EcoRI, SacI and PstI digests. M. edulis DNA was
the only one which cut with all 13 enzymes. With the exception of M. palmata . die number of enzymes which cut
was inversely related to die size of die repeat unit. This relationship held when die comparison was made based on
the size of the large non- transcribed spacer (NTS), indicating that die number of enzymes cutting was not simply
a function of sequence lengdi. Based on the number of G and C bases in the recognition sequences of die enzymes
Source
rDNA IN HYDROTHERMAL VENTS POLYCHAETES
89
which cul within the rDNA, the rDNA of the two hydrothermal vent polychaetes appears GC-rich, i.e. has a
higher G-C index, compared to the three shallow-water species ('Fable 1).
TABLE 1.— Recognition sequences of restriction endonucleases. G-C indices (on a scale of 0 - 6), and individual species
scores: Paralvinella palmiformis, (P. palm. ); P.p .pandorae. (P. pand. ); Melinna palmata, (M. palm. ); Nucella lapillus
(N. lap.); and Mytilus edulis. (A/, edulis).
Paralvinella palmiformis
XS ESm
-TZ -?J.
Sa
-*T
B Sm
▼ ▼
Sm Sa Sm
T T ▼
Sa E
▼ T
- T
P
A"
D
Paralvinella pandorae
xs E
zz z
18S 5.8S 28S
DPS
▼ ▼
3-tH
Sm
B
▼
P Sa
▼ ▼
ITS-1 ITS-2
- 1k.
NTS
1 kb
PIG. 3. — Restriction map of rDNA repeat unit of Paralvinella palmiformis and P. pandorae. Polymorphic restriction sites in
P. palmiformis arc indicated by open triangles. Restriction endonucleases which showed completely different cleavage
patterns in the two species are shown below the restriction map of P. palmiformis. ITS-1 and ITS-2 = internal transcribed
spacers; NTS = large non -transcribed spacer region; and 18S. 5.8S and 28S = the three rRNA-genes coding for the
ribosomal subunits. B = BamHI; D = Dral; E = EcoRI; H = MindHI; P = PvuII; S = Sail; Sa = SacI; Sm = Smal; and X =
Xhol. The estimated 1.5 kb difference in repeat unit size was attributed to inter- specific variation in the size of the NTS
region, indicated by the shaded portion in the map of P. pandorae. However, no enzyme was discovered which mapped to
this region so confirmation must await the results of further investigations.
Source :
90
D R. DIXON, L.R.J. DIXON & V. TUNNICLIFFF.
The diree species of Paralvinella which were analysed for their rDNA slruciure had repeat unit lengths in the
range 11 - 12.5 kb. This was significantly larger than die 7.2 - 7.6 kb values found for the three shallow-water
species (one polychaete, two molluscs). The difference in repeat unit length between P. pandorae and
P. palmiformis was traced to a duplication or some other sequence insertion affecting die NTS (Fig. 3). The
significant differencein repeat unit lengdt between Melinna palmata (7.5 kb) (Family Ampharetidae) and these
diree paralvinellids agrees with the conventional taxonomic separation of diese two polychaete families.
Restriction mapping
Restriction sites for a total of eight enzymes were mapped for P. palmiformis and nine enzymes for P. p.
pandorae-, the extra one being HindNI (Fig. 3). These two species shared 10 restriction sites in common (37 %)
out of a total of 27 mapped (Fig. 4). In contrast, P. sulfincola shared only four sites (22 %) in common with P.
palmiformis , out of a total of 18 identified (Dixon & DIXON, unpublished), which may indicate a closer
relationship between die former two species. (Note: insufficient high-quality DNA was extracted from the few
specimens of P. sulfincola to carry out any detailed mapping of restriction sites.) Allowing for some heterogeneity
between repeats and a degree of inter-individual restriction-site polymorphism, diese data suggest that P.
palmiformis is more closely related to P. p. pandorae than cither is to P. sulfincola. Clearly, molecular adaptation
to high temperature will have played an important part in speciation widiin this group. By way of contrast, the
ampharetid Melinna palmata shared only six enzymes in common with the two paralvinellids (Table 1), and
differed greatly in the number and size of fragments which diese generated. The bulk of die variation in cleavage
sites between P. palmiformis and P. p. pandorae mapped to genic regions widiin die rDNA repeat unit, although
several polymorphisms were traced to the non-coding NTS. Lacking sequence information it is not possible to
distinguish between introns and exons widiin genes. It seems highly probable that at least some of diis inua-genic
variation will involve "silent sequences", i.e. non-coding sequences which typically evolve rapidly (Li et al.,
1985).
DISCUSSION
Recently, we reported die results of experiments designed to investigate die relationship between thermal stability
of DNA and the physical and chemical conditions experienced by hydrothermal vent organisms (DIXON et al„
Paralvinella pandorae
Paralvinella palmiformis
Paralvinella sulfincola
0 10 20 30 40 50 60 70 80 90 100
I _ | _ I _ 1 _ I _ _L - 1 - 1 - 1 - 1 - 1
Percentage difference
FlG. 4. — Unrooted tree based on percentage restriction-site differences between three species of Paralvinella from the Juan
de Fuca Ridge.
rDNA IN HYDROTHERMAL VENTS POLYCHAETES
91
1992). A positive correlation was round between the denaturing temperature of rDNA and environmental
temperature for seven alvinellid species which was thought to be due to an increase in GC-content. In other
organisms, increased GC-content has been shown to confer greater thermal and chemical stability to the DNA
molecule (Darnell et al. , 1986), and is an interesting molecular adaptation to hostile environmental conditions
(e.g. BERNARDI & BERNARDI, 1990a, b). The results of the present investigation provide further evidence of
increased GC-levels in the rDNA of some hydrothermal vent polychaetes and a shallow-water ampharetid, M.
polmata (Table 1). The family Alvinellidae is closely related to, and perhaps derived from, the ampharetid
polychaetes (Desbruy6res & Laubier, 1986). The evidence presented here for increased GC-content in M.
palmcita , which tolerates highly-reduced and metal-rich sediments (Gibbs et al. , 1981), indicates that what may
have arisen originally as an adaptation to harsh chemical conditions in shallow-water sediments, may have
permitted colonisation of the high-temperature, and chemically hostile, hydrothermal vent environment in die
distant past by a common ancestor (TUNNICLIFFE, 1992).
The topology of the unrooted tree shown in Figure 4 is divergent from present systematic relationships based
on morphology which places P. p. pandorae as the most ancestral species of the genus. All other paraJvinellid
species have a different branchial form; among these species P. palmiformis and P. sulfincola form a sub-group
with trifoliate tips on the buccal tentacles (DESBRUYfeRES & Laubier, 1991; TUNNICLIFFE et al ., 1993). A study
of allozyme similarity among these species confirms the distance of P. p. pandorae but also makes a strong
differentiation between P. sulfincola and P. palmiformis (D. Jollivet, pers. comm.). That morphological and
molecular interpretations differ may be a function of the strong selection that is likely present on molecular
functioning in an extreme habitat; morphological response may not be so strong. However, phylogenetic
comparison of sequences that differ by more than 25 % is not recommended (Upholt, 1977); with greater
differences there is increased probability that cleavage sites may be convergent (Dowling et al. , 1990). The
apparently high degree of divergence of these three species (up to 60 %) may reflect long evolutionary time,
strong selection pressures, or both. While no certain fossil record is available, there are Cretaceous vent deposits
with tubes reminiscent of those of Alvinella species (Haymon & Koski, 1985); a large proportion of the vent
fauna may be a Mesozoic relic (TUNNICLIFFE, 1992). High copy number sequences are generally not good
candidates for constructing phylogenetic trees (HiLLlS & Moritz, 1990) and further work is required before good
systematic relationships can be established among these species.
ACKNOWLEDGEMENTS
The bulk of this work was funded by the UK Natural Environment Research Council through a rersearch grant
to Prof. A.J. Southward; VT was funded by NSERC Canada. Dr Peter Holland (Oxford University) kindly
donated several of the rDNA probes. We are grateful to David NICHOLSON for photographic assistance.
REFERENCES
BERNARDI, G. & BERNARDI G.. 1990a. — Compositional transitions in the nuclear genomes of cold-blooded vertebrates. J.
mol. Evol. , 3 1 : 282-293.
Bernardi. G. & BERNARDI G.. 1990b. — Compositional patterns in the nuclear genomes of cold-blooded vertebrates. J. mol.
Evol. ,31 : 265-281.
Brock, T.D., 1985. — Life at high temperatures. Science , 230 : 132-138.
DARNELL. J., LODISH, H. & Baltimore. D.. 1986. — Molecular Cell Biology. Scientific American Books. New York. 1 192
pp.
DesbruyEres, D. & Laubier, L., 1986. — Les Alvinellidae. une famillc nouvellc d'annelides polychetcs infcodccs aux
sources hydrothermales sous-marincs : systematique, biologic etecologie. Can. J. Zool. , 64 : 2227-2245.
DesbruyLres, D. & Laubier, L., 1991. Systematics, phylogeny. ecology and distribution of Alvinellidae (Polychaeta)
from deep-sea hydrothermal vents. Ophelia SuppL. 5 : 31-45.
DIXON, D.R.. Simpson- White. R. & Dixon. L.R.J.. 1992. — Evidence for thermal stability of ribosomal DNA sequences in
hydrothermal -vent organisms. J. mar. biol. Ass. J.K.. 72 : 519-527.
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DOWLING, T.E.. MORITZ. C. & PALMER, J.D.. 1990. Restriction site analysis. In: D.M. HlLLIS & C MORITZ (eds).
Molecular Systematics. Sinauer Associates Inc.. Sunderland. Mass. : 250- 317.
GIBBS. P.E., BRYAN. G.W. & Ryan. K.P.. 1981. — Copper accumulation by the polychaete Melinna palmata: an antipredation
mechanism? J. mar. biol. Ass. U.K. . 61 : 707 - 722.
IlAYMON, R.M. & KOSKI. R.A.. 1985. — Evidence of an ancient hydrothermal vent community: fossil worm lubes in
Crelaceaous sulfide deposit of the Samail Ophiolite. Oman. Dull. Biol. Soc. Wash., 6 : 57-65.
HlLLIS. D.M. & Moritz. C.. 1990. Molecular Systematics. Sinauer Associates Inc.. Sunderland. Mass., 588 pp.
HOLLAND, P.W.H.. Hacker, A.M. & Williams. N.A., 1991. — A molecular analysis of the phylogenetic affinities of
Saccoglossus cambrensis Brambell & Cole (Hemichordata). Phil. Trans. R. Soc. Loud. B., 332 : 185-189.
KESSLER, C.. Holtke, H.J.. Seibl. R.. Burg, J. & Muhlegger. K.. 1990. — Non-radioactive labelling and detection of
nucleic acids: I. A novel DNA labelling and detection system based on digoxygenin: anli-digoxygenin ELISA principle.
Biol. Chem. Hoppe Seyler, 371 : 917-927
Li. W.-H., Wu, C.-I. & LUO, C.-C., 1985. A new method for estimating synonymous and nonsynonymous rates of
nucleotide substitution considering the relative liklihood of nucleotide and codon changes. Mol. Biol. Evol. , 2 : 150- 174.
Sambrook. J .. FRITSCH. E.F. & Maniatis. T., 1989. -- Molecular cloning. A laboratory manual , vol. 1. 2nd edition. Cold
Spring Harbour Laboratory Press.
SCHMIDT, E.R., Godwin. E. A., KEY!., II. -G. & Israelewski, N.. 1982. — Cloning and analysis of ribosomal DNA of
Chironomus thummi piger and Chironomus thummi thummi. Chromosoma (Berlin). 87 : 389-407.
South KILN. E.. 1975. - Gel electrophoresis of restriction fragments. Meth. Eniymol., 68 : 152-176.
TUNNICLIFFE. V., 1992. The nature and origin of the modern hydrothermal vent fauna. Palaios, 7 : 338-350.
TUNNICLIFFE, V.. JUNIPER. S.K. & do BURGH, M.E.. 1985. The hydrothermal vent community of Axial Seamount, Juan dc
Fuca Ridge. Biol. Soc. Wash. Bull.. 6 : 453-464.
TUNNICLIFFE, V.. DESBRUYERES, D.. Jollivet, D. & Laubier, L.. 1993. Systematic and ecological characteristics of
ParalvineUa sulfincola Desbruyeres and Laubier. a new polychaete (family Alvinellidae) from Northeast Pacific
hydrothermal vents. Can. J. Zool., 71 : 286-297.
UPHOLT, W.B., 1977. — Estimation of DNA sequence divergence from comparison of restriction endonuclease digests. Nucl.
Acids. Res.. 4 : 1257-1265.
Source :
10
On the nature of the two anterior asetigerous rings
in Dorvilleidae and Dinophilidae
(Annelida, Polychaeta)
Danny EIB YE-JA COB SEN
Zoological Museum
Univcrsitetsparken 15
DK-2100 Copenhagen 0
Denmark
ABSTRACT
Members of the order Eunicida are apparently characteristic in possessing two more or less clearly separated rings between
the prostomium and the first setigcr. In the family Eunicidae it has previously been shown that these rings represent a
subdivision of the peristomium related to the manner in which the longitudinal muscles are attached to the body wall.
Nevertheless, this character may be a synapomorphy for Eunicida. provided that it is homologous among it s members. This
hypothesis is tested in members of the families Dorvilleidae and Dinophilidae through light microscopic studies of the body
area in question. Recent publications have proposed that Dinophilidae is closely related to or actually a subtaxon of
Dorvilleidae; this conclusion is not contradicted by the results of this investigation.
RESUME
Sur la nature des deux anneaux asetigeres anterieurs reunis chez les Dorvilleidae et les Dinophilidae (Annelida
Polychaeta)
Les membres de 1'ordre Eunicida paraissent caracterises par la possession de deux anneaux plus ou moins nettement
separcs entre le lobe cephaliquc et le premier setigere. Pour la famille des Eunicidae on a demontre que ces anneaux
repre sen tent des subdivisions du peristomium en relation avec la manicre par laquclle les muscles longitudinaux sont attaches
aux parois du corps. Neanmoins, ce caractere peut ctre une synapomorphie pour les Eunicida, a condition qu’il soit homologue
parmi ses membres. Cette hypothese est mise a I'epreuve chez les membres des families des Dorvilleidae et des Dinophilidae
par des etudes microscopiques de cette region du corps. Dans des publications recentes, on a propose que les Dinophilidae sont
effectivement ctroitement allies a un sous-taxon des Dorvilleidae; cette conclusion n'est pas en contradiction avec les resultats
de cette investigation.
INTRODUCTION
In most members of the polychaete family Dorvilleidae the peristomium takes the form of two apodous rings
between die prostomium and die first setiger. In most species diese rings are subequal, but in many die anterior
ElB YE- JACOBSEN, D., 1994. On the nature of the two anterior asetigerous rings in Dorvilleidae and Dinophilidae
(Annelida, Polychaeta). In: J.-C. Dauvin. L. Laubier et D.J. REISH (Eds), Actes de la 4eme Conference internationale des
Polychetes. Mem. Mus. natn. Hist. nat.. 162 : 93-100. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
94
D. EIBYE-JACOBSEN
one is shorter and indistinctly separated from the prostomium. Only few species show no trace of peristomial
subdivision, e.g., four of die five hitherto described species of the genus Exallopus Jumars, 1974 (die exception is
die type species, E. cropion Jumars. 1974). Some confusion has surrounded die nature of diese two rings. Thus,
while many audiors have preferred neutral terms, such as rings, others appear to have regarded them as true
segments (e.g.. Jirkov, 1989). where Dorvilleidae is characterized as having "two peristomial segments without
parapodia, setae or cirri". The use of die word "segment" may in many instances have been coincidental, but in an
evaluation of dorvilleid relationships widi other polychaete groups it is important to understand the true nature of
these rings. Within the order Eunicida conditions similar to (hose in Dorvilleidae are found in Eunicidac,
Lumbrineridae (sensu ORENSANZ, 1990. including Lysaretidae), Hartmaniellidae. Oenonidae (= Arabellidae), and
Iphitimidae (members of the families Histriobdellidae and Ichdiyotomidae are too strongly modified to allow an
assessment of this character). The major group in which only one peristomial ring is present is the family
Onuphidae, which is considered die sister group of Eunicidac (ORENSANZ, 1990; FaUCHALD. 1992). Descriptions
of die larval development of onuphids are not clear as to whether a peristomial subdivision is present during
earlier stages in ontogeny (e.g.. Hsieh & Simon 1987 on Kinbergonupliis simoni). In his discussion of larval
development in Nothria elegans, Blake (1975a) refers to die presence of such a subdivision but this is not
confirmed by his illustrations.
The term peristomium, as it is currently used, is not applied to homologous structures in various polychaete
families. In embryological terms, the peristomium has its origin in the region between the prototroch and the
telotroch of the classical trochophora larva (e.g.. George & Hartmann-Schrodf.r, 1985). This appears to be die
case in Eunicida (see below). However, die adult peristomium of many polychaete families is a compound
structure consisting of the peristomium s. sir. as well as a variable number of anterior segments of teloblastic
origin which have often lost their setae and parapodia and may possess paired tentacular cirri. Examples of these
conditions may be seen in families such as Hesionidae, Syllidae, and Nereidae (Gilpin-Brown, 1958).
For Eunice kobiensis (Eunicidae), Akesson (1967a) gave a very convincing account of the embryological
origin of the peristomium. According to his studies, die first setiger of adults corresponds to the first larval
segment; the peristomium, including both rings and the peristomial cirri, must be intcipreted as presegmentai.
Akesson also provided an anatomical explanation for die strongly developed peristomial subdivision, which is
found in this species. His studies showed that in die posterior region of (he peristomium a number of fibres
belonging to the ventral longitudinal muscle bands branch off in a lateral direction and attach themselves to die
body wall at die level of the subdivision (Akesson, 1967a: Fig. 1 1). In a similar manner, fibres of die dorsal
longitudinal muscles give rise to die dorsal component of die visible, non-segmental furrow.
Assuming that the absence of any peristomial subdivision in Onuphidae may be regarded as a secondary
phenomenon (possibly related to dieir being mostly tubicolous). the presence of two rings of true peristomial
origin may be regarded as an autapomorphic character of Eunicida. Embryological observations indicate diat
Akesson's observations on Eunice are valid for members of Dorvilleidae (e.g., Akesson, 1967b, 1973a, and b on
various species of Ophryotroclw, Blake, 1975b on Dorvillea rudolphi) in die sense that the two asetigerous rings
are of peristomial origin. However, it remains to be demonstrated dial a true homology exists, i.e., that a
homologous pattern of muscle attachment is present.
The primary purpose of this paper is to examine whether anatomical observations on various species of
Dorvilleidae can confirm a homology on diis point.
The family Dinophilidae was previously placed in Archiannelida, which was usually accorded order or class
rank. In recent years, a body of evidence has grown diat points to a close relationship between this family and
Dorvilleidae (Akesson, 1977; Westheide, 1985. 1987; Orensanz, 1990; Eibye-Jacobsen & Kristensen, in
press). However, since dinophilids are greatly reduced and highly specialized, much of die evidence is
FIG. I . A-C. Protodorvillea kefersteini, sagittal section showing ventrolateral longitudinal muscle band and attachment of
accessory peristomial fibres to body wall at mid-peristomial furrow (A); cross section showing accessory peristomial fibres
(in close proximity to ventrolateral longitudinal muscle band) attached to body wall (B); cross section 15-20 mm further
posterior through anterior margin of mandible showing as yet undivided, strongly developed ventrolateral longitudinal
muscle band (anterolateral, accessory mandibular teeth visible on left side) (C). D. Ophryotrocha cf. harlmcmni, cross
section, on right side corresponding to B (pharynx protruded). All scales = 10 mm. Nomarski differential interference
contrast used on all figures. Abbreviations: al = aciculum of first setiger; a2 = aciculum of second setiger; a3 = aciculum
of third setiger: amt = accessory mandibular teeth; ant = anterior peristomial ring (first post-prostomial ring); apf =
accessory peristomial fibres; cc = circumcsophagcal connective; m = mandible; mpf = mid-peristomial furrow; ol =
oesophageal lumen; pb = pharyngeal bulbus; pi = pharyngeal lumen; pos = posterior peristomial ring (second post-
prostomial ring); vc = ventral ciliation; vim = ventrolateral muscle band; vne = ventral nerve cord.
ANTERIOR ASETIGEROUS RINGS IN DORVILLEIDS AND DINOPHIUDS
95
Source : MNHN , Paris
96
D. ED3YE-JAC0BSEN
circumsiantial (larval resemblances, connections through theoretical morphological reduction series, parasite
relationships; see above references for discussion). It has been difficult to find positive apomorphic characters that
support a relationship. To date, the best such indication is the presence of an unpaired, pygidial stylus with a
specific musculature in certain dorvilleid genera and most members of the dinophilid genus Dinophilus
(WESTHE1DE, 1985).
There arc difficulties in the homologisation of segments in dinophilids with those of odier polychaetes, since
parapodia and setae are absent. However, a peri&tomial subdivision resembling that in Dorvilleidae appears to be
present, most clearly in the genus Trilobodrilus . The present study was in part undertaken to isolate yet another
possible character to strengthen the view of a close relationship between these families (or at least, in the present
context, the membership of Dinophilidae in Eunicida).
MATERIALS AND METHODS
Several specimens of each of the following species were examined: Protodorvillea kefersteini (McIntosh,
1869); Parougia eliasoni (Oug, 1978); Ophryotrocha cf. hartmanni Huth, 1933: 0. puerilis siberli (McIntosh,
1885): and Trilobodrilus cf. nipponicus Uchida & Okuda. 1943. The dorvilleid species were taken at various
localities along the north coast of Brittany, France. The specimens of Trilobodrilus were found in samples of
coarse sand and gravel taken off Ellekilde Mage in the southern Kattegat, Denmark.
The specimens were embedded in paraplast using standard techniques, sectioned to a thickness of 4 mm, and
stained using a modification of Masson's trichrome method (Weigcrt's iron haemotoxylin. Ponceau's xylidinc, and
Fast Green). This renders muscle tissue bright red, whereas collagen and other connective structures arc stained
green. After dehydration, die sections were embedded in Entellan.
The sections were studied with a Leitz Ortholux microscope, whereas photographs were taken on a Zeiss
Axiophot microscope, in most cases employing Nomarski differential interference contrast.
RESULTS
Protodorvi Ilea keferstei n i
In the posterior part of die second asetigerous ring a group of muscle fibres (henceforth termed accessory
peristomial fibres) leave die lateral part of each ventrolateral longitudinal muscle trunk (Fig. 1C). They attach to
the body wall ventrolaterally on eidier side, midway along die length of the peristomium (Fig. IB). Figure 1A
shows a sagittal section in which a ventrolateral longitudinal muscle band is seen in the anterior setigers as well as
the attachment of die accessory peristomial fibres to the body wall at the mid-peristomial furrow.
The ventrolateral longitudinal muscle trunks continue forward and insert on the body wall at the lower
(posterior) lip of the mouth opening (not visible on Fig. 1A). These fibres may be confused widi those of die
anterior mandibular protractor muscles, which are also attached to the lower lip (Dales, 1962; not shown on
Akesson's (1967a) figures). However, the latter are inserted in a midventral position, whereas die paired
ventrolateral longitudinal muscle trunks are ventrolaterally attached.
Accessory peristomial fibres also branch off from the dorsolateral longitudinal muscle trunks and are attached
to the body wall furdier forward at the level of peristomial subdivision.
Parougia eliasoni
Observations on diis species were identical to diose described for Protodorvillea kefersteini.
FIG. 2. — Trilobodrilus cf. nipponicus. cross sections showing body becoming increasingly narrow in anterior portion of
second post-prostomial ring, at narrowest point (D) showing subdivision of ventrolateral longitudinal muscle bundle, the
dorsal component of which may be homologous to accessory peristomial fibres in Dorvilleidae. Scale A-D = 10 mm.
Nomarski differential interference contrast used on A-C. Abbreviations: al = aciculum of first seliger; a2 = aciculum of
second setiger: a3 = aciculum of third setiger; amt; = accessory mandibular teeth: ant = anterior peristomial ring (first post-
prostomial ring); apf = accessory peristomial fibres; cc = circumesophageal connective; m = mandible; mpf = mid-
peristomial furrow; ol = oesophageal lumen; pb = pharyngeal bulbus; pi = pharyngeal lumen; pos = posterior peristomial
ring (second post-prostomial ring); vc = ventral ciliation; vim = ventrolateral muscle band; vne = ventral nerve cord.
Source
ANTERIOR ASETIGKROUS RINGS IN DORVILLEIDS AND DINOPHIL.IDS
97
Source ; MNHN , Paris
98
D. EIBYE-JACOBSEN
Ophryotrocha cf. hartmanni
The sectioned material of this species, although of a poorer quality, shows the presence of accessory
peris tomiaJ fibres (Fig. ID) attaching to the bexly wall at die level of the mid-peristomial furrow. As in the other
dorvilleids that were examined, the accessory fibres branch off from die ventrolateral muscle bands in die
posterior part of die second peristomial ring. The animal shown was fixed with the pharynx somewhat protruded:
die accessory peristomial fibres are contracted and therefore the two posterior mandibular rods ;ire visible. It was
not possible to observe whether dorsal accessory fibres are present.
Ophryotrocha puerilis siberti
Observations on diis species were as described for 0. cf. hartmanni.
Trilobodrilus cf. nipponicus
From the middle of die second post-prostomial ring (Fig. 2A) to die furrow between the first and second rings
(Fig. 2D) body width decreases from 54 mm to 38 mm. Observations on the possible presence of accessory
peristomial fibres was hampered by the small size of the animals in question. Thus, in any given cross section each
ventrolateral muscle band consists of 2-4 cells only. However, at die level of die furrow between die first two post-
prostomial rings, die dorsalmost of these cells appears separated from the others. It was not possible to observe
whether it was attached to die body wall at this point, but this cell is absent on more anterior sections, indicating
that its rostral end must be very close to the furrow.
DISCUSSION
In die dorvilleid species studied, subdivision of the peristomium appears to be induced (at least in part) by the
attachment of accessory muscle fibres with an origin in the longitudinal trunks. These observations correspond to
diose reported by Akesson (1967a) for Eunice kobiensis . die only important difference being that die accessory
fibres remain close to the main trunk throughout their entire length. In Eunice (as indicated on Akesson's
drawing) the ventral accessory peristormial fibres and the ventrolateral muscle bands appear to be clearly
separated rostrally. This disparity may be due to differences in degree of muscle contraction.
Recently, Orensanz (1990) has suggested that a number of dorvilleid genera, among diem Ophryotrocha
should be placed in the family Iphitimidae. Doubtless a close relationship between Dorvilleidae and Iphiumidae
exists. However, as the character studied in the present paper is most likely common to die entire order Eunicida, it
probably has no bearing on inter-familial relationships. The question of whether Orensanz* rearrangement of
genera is justified will be treated in a separate paper (Eibye-Jacobsen & KRISTENSEN, in press).
The accessory peristomial fibres and thus the subdivision of die peristomium in Dorvilleidae are very probably
homologous to those in Eunicidae. Although corresponding anatomical studies have not yet been carried out on
members of families such as Eumbrineridae and Oenonidae, and disregarding the aberrant conditions in
Onuphidae, the presence of a secondary peristomial subdivision in association with a specific pattern of muscle
attachment appears to be an autapomorphic character for die order Eunicida. Even though external signs of
genuine peristomial subdivision are lacking in odier polychaete groups, ii would be preferable to lest this
hypodicsis by carrying out corresponding studies on some of them. The sister group of Eunicida would be of
special interest. Unfortunately, it is at the present time difficult to form an informed opinion as to which
polychaete groups are likely candidates, as Eunicida is generally considered a somewhat isolated group (Dales,
1962; Storch, 1968; Fauchald, 1977).
On die basis of the present study of Trilobodrilus , it is neither possible to conclude that accessory peristomial
fibre(s) exist nor diat the two anterior post-prostomial rings represent a subdivided peristomium. The results are
too uncertain and die apparent presence of a muscle cell disassociated from the others of the ventrolateral
longitudinal muscle band (Fig. 2D) may be due to an artifact. The fact that this cell has a dorsolateral position
relative to die longitudinal muscle band (lateral in Dorvilleidae, ventrolateral in Eunicidae) should not be seen as a
hindrance to considering die phenomenon (if it exists) as homologous. In all cases, the fibres that branch off are
the most lateral ones and it is the orientadon of the longitudinal muscle bands which varies. Ultrastructural studies
must, however, be carried out before it can confidently be concluded diat a homology does exist on this point
between dinophilids and eunicidans.
Akesson (1967a) and subsequently other audiors have suggested diat the funedon of die accessory peristomial
fibres is to augment the operation of the complicated jaw apparatus present in members of the order Eunicida. No
Source :
ANTERIOR ASET1GEROUS RINGS IN DORVILLEIDS AND DINOPHILIDS
99
actual mechanism for this has been proposed. In Ougia subaequalis (Ouc., 1978) the pharynx may reach into
setiger 13 with the maxillae placed in setiger 6 in die retracted state. In many other dorvilleids some of the anterior
setigers also house parts ol die pharyngeal apparatus. Thus, although the division of die peristomium may
originally have had an explanation in accordance with Akesson’s hypothesis, it is difficult in light of their
dimensions to credit the accessory peristomial fibres with an important role during pharyngeal protraction in all
dorvilleid species.
Certainly, if it were later to be demonstrated that accessory peristomial fibres are present in dinophilids diey
must be regarded as rudiments or have some other function, as diey arc completely dwarfed by the strongly
developed pharyngeal bulb (Fig. 2D).
ACKNOWLEDGMENTS
I wish to thank Wilfricd Westheide (University of Osnabruck, Germany) for suggesting this line of
investigation and for being a generous host during an extended visit to his institute. The assistance of the staff at
the Station Biologique (Roscoff, France), especially that of Captain Alain Maron. during die collection of most of
the animals used in this study is greatly appreciated. Kurt OCKEI.MANN (Marine Biological Laboratory, Ilelsingpr,
Denmark) kindly furnished the specimens of Trilobodrilus. Margit Jensen (Zoological Museum, University of
Copenhagen) is thanked for the use of her Zeiss Axiophot microscope (Carlsbergfondet grant no. 468). The Danish
Natural Science Research Council provided post-doc funding for this project (grant no. 11-8808).
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OUG, E.. 1978. — New and lesser known Dorvilleidae (Annelida, Polychaeta) from Scandinavian and northeast American
waters. Sarsia , 63 : 285-303.
STORCH. V., 1968. — Zur vergleichenden Anatomic der segmentalen Muskclsysteme und zur Verwandtschalt dcr Polychaeten-
Familien. Z Morph. Tiere. 63 : 251-342.
WESTHEIDE. W„ 1985. — The systematic position of the Dinophilidae and the archiannelid problem. In : S.C. MORRIS. J.D.
GEORGE. R.Gibson & H.M. PLATT (eds). The Origins and Relationships of Lower Invertebrates. 28 : 310-326. The
Systematics Association, Oxford.
WESTHEIDE, W.. 1987. — Progencsis as a principle in meiofauna evolution. J. Nat. Hist.. 21 : 843-854.
11
The head of Maldanidae polychaetes
of the subfamily Maldaninae
Karen D. GREEN
1537 Camino Corto
Fallbrook, CA, 92028, USA
ABSTRACT
The Maldaninae head and proboscis are described based on dissections of Asychis amphiglyptus , Bathyasychis cristatus.
Chirimia lobata , Maldane sarsi , Metasychis disparideniatus, Sabaco elongatus , and Sonaisa meridionalis. Consistent features
among these species include a well-developed cephalic plate with the rim divided by lateral notches, a wide and muscular
palpodc, a tri-lobed mouth, and an asymmetrical proboscis. It is suggested that the feeding structure is an axially-modified
ventral proboscis. Variable features include the development of the cephalic rim, nuchal organs, palpode, mid-dorsal keel, and
proboscis muscles.
RESUME
La tete des polychetes Madanidae de la sous-famillc des Maldaninae
La description de la tele et du proboscis de Asychis amphiglyptus , Bathyasychis cristatus, Chirimia lobata. Maldane sarsi,
Metasychis disparidentatus. Sabaco elongatus elSonatsa meridionalis a ete effectuee a partir de dissections. Les principales
caracteristiques chez ces cspeces sont la presence dune plaque cephaliquc bicn developpee avec un limbe divise par des
echancrures laterales. un palpode large et musculaire, une bouche trilobee, et un proboscis asymetrique. II est suggere que cette
structure pour ralimentation provienl d'un proboscis ventral axial modifie. Des caracteristiques variables ont etc observees sur
le developpement du limbe cephalique. les organes nucaux. le palpode. la carene medio-dorsale et les muscles du proboscis.
INTRODUCTION
The head is a key feature in the taxonomy of Maldanidae polychaetes. The subfamily Maldaninae
(Arwidsson, 1907; Light, 1991) is characterized as having a cephalic plate, which refers to the dorsal surface of
the head being edged by a raised rim. The cephalic rim is divided by lateral notches into a single posterior border
and paired lateral borders. The prostomial palpode is anterior to the plate. Paired nuchal organs occur on the
dorsal surface of the plate immediately behind the palpode. A keel (= carina, intemuchal ridge, median ridge)
refers to a medially raised area between the nuchal organs that may or may not extend into the posterior cephalic
border.
Historically, the height and length of the keel was used in keys to separate the Maldaninae genera Asychis and
Maldane (e.g., Arwidsson, 1907; Fauchald, 1977). However, interpretation of whether the keel is short and
Green, K.D.. 1994. — The head of Maldanidae polychaetes of the subfamily Maldaninae. In: J.-C. Dauvin, L. LAUBIER &
D.J. Reish (Eds), Actes de la 4eme Conference intemationale des Polychetes. Mem. Mus. natn. Hist. nat.. 162 : 101-109. Paris
ISBN 2-85653-214-4.
Source : MNHN. Paris
102
THE HEAD OF MALDANINAE POLYCHAETES
low, or long and high may be difficult (FauchaLD, 1972: note, keel referred to as palpode). In his revision of die
Maldaninae, Light (1991) considered oilier head features to be of generic importance; i.e., palpode shape, nuchal
organ shape, and the development and shape of the lateral borders of the cephalic rim (= lobes, margins) including
the degree offusion or separation of them from the palpode.
In contrast to die above features, the mouth and proboscis have received little attention. Arwidsson (1907)
characterized die maldanin proboscis as being fairly uniform in width, but with a short plate-like bladder at the
base, and lacking papillae. OkRHAGE (1973) histologically examined die foregut of Asychis biceps and
characterized it as a culicularized ventral sac (with an underlying muscle bulb) beneath a ciliated esophagus. He
considered these features to be consistent with Dales (1962) ventral proboscis category.
Muscles concerned with die operation of die maldanin proboscis have not been described. The only available
information concerns the maldanid subfamily Euclymeninae (Pilgrim, 1966; Kudenov, 1977), which have an
axial proboscis (Ullman & Bookhout, 1949; Dales, 1962; Pilgrim, 1966; Orrhage, 1973; Kudenov, 1977;
TZETUN, 1991). In euclymcnins, two paired groups of muscles function as proboscis retractors. The largest set
includes the retractor sheath, which inserts on die cuticularized buccal area; and the gular membrane, which
inserts on the ciliated esophageal area (sometimes referred to as pharynx). The retractor sheath and gular
membrane arc considered derivatives of a single septum; dicir origin on die ventrum marks the boundary between
the head and thorax (Pilgrim, 1966). The smallest set of muscles, termed the accessory buccal retractors, insert
on the anterior portion of die buccal region (KUDENOV, 1977; PILGRIM, 1966).
The purpose of diis paper is to provide additional information about die maldanin head and to describe the
foregut and its musculature. Consistency and variability of head features within the subfamily are addressed by
examination of representatives of Maldaninae genera recognized by GREEN (1987) and LIGHT (1991): Asychis,
Chirimia , Maldane. Metasxchis , Sctbaco , and Sonatsa.
MATERIALS AND METHODS
Non-type specimens were examined from the Allan Hancock Foundation (AIIF) in cooperation with the Los
Angeles County Museum of Natural History, and from the author's collection. Material included: Asychis
amphiglyplus, Antarctica, Hope Bay, 3. 5-7. 5 m, Staten Island station 46-63 (original label as Maldane sarsi)
(AIIF); Bcithyasychis cristatus, South America, Peru-Chile Trench, 8°43'S, 80°40'W, 3,939 m, Anton Bruun
station AB1 1-168 (original label as Sonatsa meridionalis) (AIIF); Chirimia lobata: Southern California, San
Diego Trough, 32°25,-26°0,N, 1 17°26.8'-1 17°28.LW. 1208-1244 m, trawl, Rokop station 71-45 (original label as
Asychis lobata) (AIIF); Maldane sarsi. Arctic Alaska, 71°09.8’N, 15r09.3’W, 45 m (donated by II. JONES);
Maldane cL sarsi, southern California, Santa Monica Bay, 184 m (donated by L. Harris); Metasychis
disparidentatus , southern California, Newport Beach, 100 m (donated by L. Lovell); Sabaco elongatus, northern
California, San Francisco Bay (donated by M. Wicksten); Sonatsa meridionalis , South America, Peru-Chile
Trench, 8°38'S, 80°40'W, 3,590-3,479 m, trawl, Anton Bruun station AB1 1-165 (AIIF). Representatives of all
examined species are retained in the AHF.
Terminology used by Pilgrim (1966) and Kudenov (1977) to describe heads of euclymenins is largely
adopted. However, their use of the term pharynx for the ciliated portion of the proboscis is not followed. T his is
because the term pharynx has been variously defined as a muscular portion of the proboscis (Dales, 1962) or as
die entire stomodeal region involved in the uptake of food (Purschke. 1988). Here, the proboscis is considered
the protrusile part of the gut; I refer to the culicularized portion as the buccal mass, and the ciliated portion as die
esophagus.
Nuchal organ shape is described with reference to stems and tips. The stem is the end most posterior on the
head; the tip is anterior. In the case of recurved nuchal organs, the stem is alongside die internuchal area, and die
tip curves away.
Internal features were studied dirough dissections; a sagittal cut was made dirough the head and at least the
first setiger. Drawings were made using a drawing tube fitted to a dissecting microscope. The surface of die
foregut was characterized as cuticularized (i.e., same appearance as the external integument) or ciliated (i.e.,
finely textured or granular appearance). The presence or absence of cilia was confirmed by examining slide
preparauons of each type of surface using a compound microscope.
Features identified in die figures arc abbreviated, as follows:
A = aboral annulus; ABR = accessory buccal retractors; BM = buccal mass; B.H/T = boundary of head and
K. D. GREEN
103
FlGc' A~ Ven?I1Vr,0f he?d and firsl lh0racic segmenl; B- ven,ral view- proboscis partially retracted;
„mK“ Proboscis everted; D, lateral view, proboscis everted. Asvchis amphiglyptus : E. ventro-latcral view
Eal view wS eVeh ‘ S3nlC ViT aS 1,1 E‘ bU‘ Wi,h ,,1,c,-vcn[ral cut and right side folded back; G. internal ventro-
foreeut anlf™ ,?P g P”rl!°" °f proboscis removed; H. ventral view of G. Maid, me sarsi: I, lateral view with
exoosed vl T exposed; J, ventral view of transverse cm made dorsal to retractor sheath; K, dorsal view of head
abbreviation^ ^ CU L N°‘C: not al1 blood vcssels are showi'- See Materials and Methods for definition of letter
Source :
104
THE HEAD OF MALDANINAE POLYCH AETES
thorax; BEJ = bucco-esophageal junction; CG = cerebral ganglion; CM = circular muscle; CNC =
circumesophagcal nerve connective; DBV = dorsal blood vessel; DM = dorsal mesentery; DV = dorsal valve; E =
esophagus; GM = gular membrane; GMO = gular membrane origin; INM = internuchal muscle; K = keel; LL =
lower lip; LB = lateral border; LM = longitudinal muscle; OM = oblique muscle; M = membrane; MS = muscle
strands; NO = nuchal organs; P = palpode; PB = posterior border; POC = paroesophageal cavity; RB V = retractor
blood vessel; RS = retractor sheath; SP = septum; TM = transverse muscle; UL = upper lip; VB V = ventral blood
vessel; VNC = ventral nerve cord; VS = ventral sac.
RESULTS
Head/f/iorax Boundary. The head extends from the prostomial palpode to the first complete annulus (Fig. 1 A-
D), which includes the ventral origin of the retractor sheath and gular membrane (Fig. IE). The prostomial
palpode is fused to the peristomium, which is ventrally biannulate. A ventro- lateral groove, anterior to the
bifurcation of die nerve cord, separates the mouth from an aboral annulus (Fig. 1 A). The first complete annulus
and the following setous one form die first biannulate thoracic segment, whose posterior boundary is marked by a
septum (e.g.. Fig. 2B).
Cephalic Rim. The cephalic plate has smooth borders in most of die examined species, but they are serrate in
Chirimia lobata and Mctasychis disparidentatus (Fig. 2, dorsal views). The transition between the palpode and
lateral margins is gradual in Sonatsa elongatus, marked by shallow notches in Asychis amphiglyptus ,
Bathyasychis cristatus and Maldane sarsi , or marked by clefts in Chirimia lobata and Metasychis disparidentatus.
Palpode. The palpode is as wide or wider than the mouth in all examined specimens (e.g.. Fig 1 A). The shape
of die palpode complements die shape of die plate (Fig. 2, top views). That is, the palpode is rounded and nearly
the same width of the rounded plate in Asychis amphiglyptus , Bathyasychis cristatus, Chirimia lobata , and Sabaco
elongatus. In contrast, the palpode is spade-shaped and less than 75 % the width of die elongate plate in
Metasychis disparidentatus, Maldane sarsi , and Sonatsa meridionalis. The palpode is upturned in Chirimia
lobata , conical in Sonatsa meridionalis, and angular in profile in die other species. The palpode is muscular
(Fig. 2, sagittal views); transverse muscle development is greatest in Sonatsa meridionalis (Fig. 2B).
Nuchal Organs. The nuchal organs differ in shape and length (Fig. 2, top views). Nuchal organs with nearly
parallel stems have lips that diverge or slightly curve as in Maldane sarsi (Fig. 2A), strongly curve or bend
laterally as in Asychis amphiglyptus and Metasychis disparidentatus (Fig. 2D,F), or recurve as in Chirimia lobata
and Sabaco elongatus (Fig. 2C,G). Stems curve laterally and tips are nearly parallel in Sonatsa meridionalis (Fig.
2B). 'fhe stems and tips both diverge in Bathyasychis cristatus (Fig. 2E). Nuchal organs tire reduced (< 1/6 head
length) in Sabaco elongatus ; short (1/6 to 1/3 head length) in Bathyasychis cristatus, Metasychis disparidentatus,
Maldane sarsi, and Sonatsa meridionalis ; and of moderate length (1/3 to 1/2 head lengdi) in Asychis amphiglyptus
and Chirimia lobata.
Behind the cerebral ganglion and beneath the nuchal organs is a concentration of transversely oriented muscle
bundles, herein termed die internuchal muscle (Fig. 2, sagittal views). This muscle is least developed in Sabaco
elongatus (Fig. 2C) and most developed in Chirimia lobata (Fig. 2G). The length of the internuchal muscle
approximates that of the nuchal organs in Bathyasychis cristatus, Maldane sarsi, and Sabaco elongatus ; the
nuchal organs are slightly longer than the internuchal muscle in Asychis amphiglyptus, Chirimia lobata , and
Metasychis disparidentatus. Keel development obscures die dorsal boundary of die internuchal muscle in Sonatsa
meridionalis (Fig. 2B).
Keel. The keel is convex, long, narrow, and firm in Maldane sarsi and Sonatsa meridionalis (Figs. 2A,B).
These keels are supported by multiple layers of transverse muscle bundles that extend from the palpode to die
posterior border of the plate. However, thedevelopment of the keel muscle differs between diese species. The
transverse muscle bundles tire interspersed within a dense layer of longitudinal muscle in Maldane sarsi. In
contrast, dense aggregations of transverse muscle occur below a layer of longitudinal muscle in Sonatsa
meridionalis.
Most of the odier species have slightly convex (Metasychis disparidentatus and Sabaco elongatus ) to flat
(Asychis amphiglyptus and Chirimia lobata) keels that are marked by a single layer of transverse muscle bundles,
die extent ol which corresponds to keel length. These keel are relatively narrow and compressible (loses shape
when pressed). The keel is relatively wide and firm in Bathyasychis cristatus (Fig. 2E). The firmness probably
reflects a bulging of die proboscis; diere is little space between the esophagus and the inner wall of die head.
Mouth. All examined specimens have a transverse opening and a medially incised upper lip; die lower lip has
K. D. GREEN
105
Fig. 2. Sagittal and dorsal views of heads: A. Maldane sarsi; B, Sonatsa meridional is ; C. Sabaco elongatus ; D, Asychis
amphiglyptus\ E, Bathyasychis cristatus\ F. Met asychis disparidentatus ; G. Chirimia lobata. Notes: All sagittal and dorsal
views, respectively, drawn at same scale; scale for each view shown in Fig. 2A. Equivalent features in all sagittal views
have same shading pattern, see Fig. 2B for detailed labeling. Not all blood vessels and oblique muscles are shown. See
Materials and Methods for definition of letter abbreviations.
Source MNHN , Paris
106
THE HEAD OF MALDANINAE POLYCHAETES
several longitudinal folds (e.g., Fig. 1 A).
Proboscis. Of the examined material, one specimen o t' Maldane has a fully everted proboscis (Fig. 1C-D), and
one specimen of Asychis has a partially everted proboscis (Fig. 1E-F). The proboscis consists of a cuticularized
buccal mass and the anterior part of the ciliated esophagus. The everted part of the esophagus is cushion-shaped;
the everted buccal region is asymmetrical with abasal extension (herein termed ventral sac).
In the retracted state, the proboscis is similar among the examined species (Fig. 2, sagittal views). The
cuticularized region is smooth and slightly folded. Part of it extends from the edges of the upper lips to the
esophagus. Another part infolds from the comer of the mouth and forms the ventral sac below the esophagus (Fig.
1 J-K; Fig. 2, sagittal views).
Transverse muscle may occur beneath die retracted ventral sac. This muscle is relatively well-developed in
Bathyasychis cristatus and Sonatsa meridionalis (Figs. 2B,E), is present in Asychis amphiglyptus and Chirimia
lobata (Figs. 2D,G), and is reduced in Metasychis disparidentatus, Maldane sarsi , and Sabaco elongatus (Figs.
2A.C,F).
The proboscides also differ widi regard to how folded the esophagus is when retracted. The folds are taken
here as an indication of proboscis volume; given this, the largest volume proboscides were noted for Bathyasychis
and Sonatsa.
Proboscis Retractors. On each side of the head, the gular membrane and retractor sheath originate along a path
from the head/thorax boundary towards the level of the lateral notches (Fig. 10-1). From there, the origin of the
gular membrane continues dorsally and anteriorly to the end of the plate. The retractor sheath divergesventrally.
Accessory buccal retractors originate behind the cerebral ganglion and along the line of the circumesophageal
nerve connectives.
Along the origin of the gular membrane, muscular strands extend ventro-lalerally (anterior face) and a thin
membrane extends dorso-latcrally (posterior face) (Fig. II). The muscular part of the origin ends behind the
intemuchal muscle; the membranous part continues anteriorly beneath the internuchal muscle to the dorsal valve
(Fig. 1 1 1-I). The gular membrane inserts on the ciliated esophagus.
This is reversed for the retractor sheath, which has muscular strands on the posterior face and a thin membrane
on the anterior face (veniro-lateral). The retractor sheath inserts on the cuticularized ventral sac and the line of
insertion continues towards the posterior corner of the upper lip (Fig. II).
Accessory buccal retractors lack an obvious membranous sheet, and the muscle strands insert on the buccal
mass nearest the mouth. They are most developed dorso-laterally. and slightly overlap the retractor sheath near
the comer of the mouth. Ventrally, they are less developed; they insert on the ventral buccal mass, but were not
observed where the retractor sheet inserts.
DISCUSSION
Maldaninae is one of the seven subfamilies of Maldanidae: Clymenurinae, Euclymeninae, Lumbriclymeninae,
Maldaninae, Nicomachinae, Notoproctinae, and Rhodininae (Arwidsson, 1907; Detinova, 1985a; Imajima &
Shiraki, 1982). Most subfamilies were established on, the basis of the head and pygidial regions and setal
structure, although glands were used to establish Clymenurinae (Imajima & Shiraki, 1982). The key head feature
has been whether or not the head is modified as a plate.
Results suggest additional head features that may be useful at die subfamily level. The examined specimens
shared the following features in common. The head includes a fused prostomium and peristomium, and the
peristomium is biannulate. The palpode is muscular and at least as wide as the mouth. The mouth is trilobed with
a transverse fissure and medially incised upper lip. Further, all species have an asymmetrical axially-modified
ventral proboscis. These features are discussed further below.
The composition of the maldanid head has been controversial, but it is agreed that the prostomium and
peristomium arc fused (Pilgrim, 1966; Light, 1991). Pilgrim (1966) considered the peristomium of some
euclymenins to include an additional fused segment based on the ventral accessory buccal retractors' origin, which
she associated with an aboral groove on the ventrum. In maldanins, the ventral origin of these muscles is
associated with the nerve connectives rather than the aboral groove. Further, the line oforigin is interrupted by the
retractor sheath, and the accessory retractors lack an obvious membrane. For these reasons, I interpret the aboral
groove as indicative of a biannulate peristomium rather than a septum.
Palpode development and mouth shape need further assessment in maldanids. Instead of a wide muscular
palpode, as in maldanins, some euclymenins have a muscular palpode that is narrower than the mouth (Pilgrim,
K. D. GREEN
107
1966). However, information about the extent and musculature of the prostomial palpode is lacking for most
maldanids. Narrow palpodes are common in clymenurins and cuclymenins, and indistinct palpodes arc common
in the other subfamilies (Imajima & Shirakl 1982). A tri-lobed mouth, as in maldanins, may be unique. Other
maldanids have a transverse or longitudinal fissure (Imajima & Shiraki, 1982; Kudenov, 1977; Pilgrim, 1966;
TZETLIN, 1991); however, since mouths arc rarely mentioned, this feature needs additional study.
Maldanin proboscides appear to differ from the few available reports for other maldanids. ORRHAGE (1973)
characterized Asychis biceps as having a ventral proboscis because a cuticularized ventral sac (with an underlying
muscle bulb) occurs below the ciliated esophagus. He stated that the ventral sac and muscle bulb were less
voluminous in this species than in other species with ventral proboscides; i.e., Nicomache lumbricalis
(Nicomachinae) and Rhodine gracilior (Rhodininae), but further detail was not given. Results indicate that the
ventral sac is common in maldanins, but the development of the underlying transverse muscle (bulb) is variable.
Based on TZETLlN's (1991) illustrations of Nicomache lumbricalis , Nicomache minor , and Praxillura longissima
(Lumbriclymeninae), my impression is that the muscle bulb (ventral pharyngeal organ) is less developed in
maldanins. Further die configuration of die maldanin proboscis differs from the ventral proboscides of Nicomache
minor and Praxillura longissima. In those species, die non-ciliated region primarily is a ventral structure and the
ciliated region primarily is dorso-lateral. In contrast, die non-ciliated region of die foregut is developed bodi
dorsally and ventrally in maldanins. but it forms a narrow sac ventrally.
Because the non-ciliated and ciliated regions evert as a tube-like structure in maldanins, there is some
similarity to die axial proboscides of cuclymenins (Dales, 1962; Pilgrim, 1966; Kudenov, 1977; Tzetlin,
1991). However, the ventral sac at die base of die maldanin proboscis gives it an asymmetrical appearance. This
difference in the ventral development of die proboscis is reflected in the proboscis musculature. In euclymenins,
the gular membrane and retractor sheadi share the same origin (Pilgrim, 1966; Kudenov, 1977). In maldanins,
the retractor sheath diverges and follows a more ventral course. Furdier, accessory buccal retractors, which are
well-developed in euclymenins, tire mainly dorso-lateral in maldanins and only weakly developed ventrally
(presumably due to die ventral padi of the retractor sheadi).
Accordingly, results suggest that maldanins have a axially-modified ventral proboscis. The axial modification
refers to the tube-like appearance of the everted proboscis. However, because die appearance of the tube is
asymmetrical (due to the ventral sac), the retractor sheath is ventrally oriented, and a muscle bulb may be present,
I consider the structure more consistent widi the ventral proboscis category. TZETLIN (1991) provides a hypothesis
of proboscideal evolution within die order Capiteliida in which the ventral state is considered more primitive than
die axial state. Perhaps the axially-modified ventral proboscis of maldanins represents an intermediate state in
Tzetlin's (1991) hypothesis.
Within Maldaninae, several features are variable. Because this study only compares a single representative of
each genus, it is not possible to comment on consistency of features within each genus. However, results do
permit some comment regarding features considered of generic importance, and docs suggest other features dial
may be promising to investigate.
With regard to the cephalic rim, Light (1991) considered the development and shape of the lateral borders and
their separation from the palpode as a generic feature. An additional characteristic that may contribute to
descriptions of tliis feature is die development of die notch or cleft that may separate die borders and palpode.
Light (1991) recognized three shapes of Maldaninae palpode; spade-like, mushroom-shaped, and indistinct.
Results indicate that shape categories are variable within some genera. For example. Light characterized die
palpode of Asychis as spade-like, and that of Metasychis as mushroom-shaped; however, the examined Asychis
amphiglyptus has a rounded palpode, and the examined Metasychis disparideniatus has a spade-like palpode. It is
suggested that descriptions of shape may be improved by considering die profile and thickness of die palpode.
Light (1991) characterized maldanin nuchal organs as four basic shapes (J-shaped, U-shaped, slightly curved,
and crescentic). Additional categories are needed to describe nuchal organs in which the stems diverge (as in
Sonatsa) and in which both stems and tips diverge (as in Bathyasychis). It is suggested that descriptions of nuchal
organs include reference to stem and tip shape and lengdi. The internuchal muscle appears to relate to
characteristics of die nuchal organs (e.g., shape and length), and additional study of this muscle is warranted. The
internuchal muscle, which may be prominent in maldanins, has not been investigated for oilier maldanids.
A cephalic keel, though not considered a generic character by LIGHT (1991), was considered so in the past.
Results indicate that the usefulness of the keel as a taxonomic character may be improved by taking into
consideration compressibility and width when evaluating the more traditional height and length characters.
Examinations of muscle development provides a means to cross check keel designations.
108
THE HEAD OF MALDANINAE POLYCHAETES
Features of tlie proboscis vary among the examined species. Baihyasychis and Sonatsci are similar in having
the densest concentrations of transverse muscles beneath the ventral sac, and the largest volume proboscides of
the examined species. It is not known whether these similarities are due to feeding in a similar environment (both
co-occur at abyssal depths in trenches) or close phylogenetic relationship. Because both taxa have nuchal organs
with diverging stems (the tips also diverge in Baihyasychis ), another feature suggests relationship.
In die past it was questioned whether Sonatsa was distinct from Maldane since they arc morphologically
similar (Arwidsson, 1922: Detinova, 1985b). GREEN (1987) argued for recognition of Sonatsa based on nuchal
organ shape and the presence of an enlarged ventral glandular pad on setiger 5. The similarities in proboscis
development mid nuchal organs between Baihyasychis and Sonatsa support Sonatsa' s generic status. So do the
differences between Sonatsa meridionalis and Maldane sarsi in die muscle development of the proboscis, keel,
and palpode.
Other species provide an additional example where similarity in external morphology does not correspond
with proboscis musculature. For example, Chirimia lobata and Metasychis disparidentatus have serrate cephalic
borders: however, the development of the muscles beneath the ventral sac differ. Proboscis muscles are more
similar between Chirimia lobata and Asychis amphiglyptus ; diese species also arc similar in having well-deve¬
loped intemuchal muscles. Conversely, die appearance of the plaque differs among Metasychis disparidentatus ,
Maldane sarsi , and Sabaco elongatus, but diey are similar in having reduced ventral sac muscles. The intemuchal
muscle is similar between Metasychis disparidentatus and Maldane sarsi , but is unique in Sabaco elongatus.
Although it is not known at this time which features are more reflective of convergence or relationship, this
study supports die status of die genera. It also supports the view that important features include die development
of the cephalic rim and nuchal organs. I suggest that proboscis musculature, keel development, and palpode shape
may be important, but need further study.
ACKNOWI JUDGEMENTS
Special thanks go to Leslie II arris of the Allan Hancock Foundation for the loan of specimens. Larry Lovell
generously allowed use of his microscope with drawing tube. Discussions widi Dr. Kirk FlTZHUGH prompted me
to prepare diis paper, and I appreciate his interest. I am grateful to Drs. Jerry Kudenov, Alexander TZETLIN, and
two anonymous reviewers for dieir comments to an earlier draft of diis paper.
REFERENCES
Arwidsson, I.. 1907. — Studien liber die skandinavischen und arktischen Maldaniden nebst Zusammenstellung der iibrigen
bisher bekannten Arten dieser Familie. Zool. Jhrb., Suppl., 9 : 1-308.
Arwidsson. I., 1922. Systematic notes on some maldanids. Svenska Vetensk. Akacl. Stockholm, Hand., 663 : 1 -46.
Dales, R.P.. 1962. — The polychacte stomodeum and the inter-relationships of the families of Polychaeta. Proc. Zool. Soc.
bond ., 139: 389-428.
Detinova. N.N.. 1985a. Taxonomy, composition and distribution of polychaetes of the subfamily Lumbriclymeninae
(Maldanidae). hr. Polychaeta: Morphology, syslematics, ecology. Proc. USSR Polychaeta Conference. Leningrad. 1983 :
25-29. (in Russian].
Detinova, N.N., 1985b. The taxonomic significance of the structure of the parapodia in some Maldanidae (Polychaeta).
Zool. Zh., 64 : 1487-1492. (in Russian].
FAUCHALD. K.. 1972. — Benthic polychaetous annelids from deep water off western Mexico and adjacent areas in the eastern
Pacific Ocean. Allan Hancock Monogr. mar. Biol., 7 : 1-575.
Fauchald. K., 1977. — The polychaete worms: Definitions and key to the orders, families and genera. Nat. Hist. Mus. Los
Angeles County, Sci. Ser., 28 : 1-190.
Green, K.D., 1987. - Revision of the genus Sonatsa (Polychaeta: Maldanidae). Bull. Biol. Soc. Wash., 7 : 89-96.
IMAJ1MA, M. & Y. SiriRAKI, 1982. Maldanidae (Annelida: Polychaeta) from Japan (Part 1,2). Bull. Nat. Sci. Mus., Tokyo,
8 : 7-88.
K. D. GREEN
109
Light, W.J.H., 1991. — Systematic revision of the genera of the polychaete subfamily Maldaninae Arwidsson. Ophelia
Suppl. , 5 : 133-146.
ORRHAGE, L.. 1973. Two fundamental requirements for phylogenetic-scientific works as a background for an analysis of
Dale’s (1962) and Webb’s (1969) theories. Z. Zool. Syst. Evolut.-forsch., 1 1 : 161-173.
PILGRIM, M.. 1966. — The morphology of the head, thorax, proboscis apparatus and pygidium of the maldanid polychaetes
Clymenella lorquata and Euclymene ocrstedi.J. Zool., Land., 148 :453-475.
PURSCHKE, G.. 1988. — XI. Pharynx. In W. WESTHEIDE & C. O. HERMANS (eds), The Ultrastructure of Polychaeta.
Microfauna Marina . 4 : 177-197. Gustav Fischer Vcrlag, Stuttgart, New York.
TZETLIN, A.B. 1991. — Evolution of feeding apparatus in the polychaetes of the order Capitellida. Zool. Zh 70 : 10-22. [in
Russian].
ULLMAN. A. & C.G. BOOKHOUT. 1949. — The histology of the digestive tract of Clymenella lorquata (Leidy). J. Morph., 84 :
31-55.
Source : MNHN. Paris
12
Effects of sample fixation on body shape of
Capitella capitata (Polychaeta, Capitellidae)
Marfa Nuria MENDEZ & Marfa Jose CARDELL
Departament d’Ecologia, Facultat de Biologia
University of Barcelona
Avda. Diagonal 645
08028 Barcelona Spain
SUMMARY
Formaldehyde fixed specimens of Capitella capitata from the littoral zone of Barcelona showed several body forms :
"contracted C. capitata" (CC) - pointed proslomium. contracted thorax, anterior setigers distinct; "elongated C. capitata"
(EC) - triangular prostomium/peristomium, elongated thorax, anterior setigers indistinct; "intermediate C. capitata" (IC)
- intermediate form between CC and EC. Five fixation tests were performed using different formaldehyde concentrations,
sieving or unsieving before fixation, and different periods between sample collection and fixation. By these tests it was
shown that CC is the regular form, whereas EC and IC are caused by deficiencies in sample fixation. Recommendations are
given for avoiding the fixation aberrant fixation forms which might impair studies in taxonomy and population
dynamics of this species.
RESUMfi
Effets de la fixation dcs ecliantillons sur la forme du corps dc Capitella capitata (Polychaeta,
Capitellidae)
Des specimens preserves de Capitella capitata du littoral de Barcelone monlrent plusieurs formes du corps : "C.
capitata contractee" (CC) - prostomium poinlu, thorax comrade, seligeres anterieurs bien differences ; "C. capitata
allongee (EC) - prostomium/peristomium triangulaire. thorax allonge, seligeres anterieurs pas differencies ; "C. capitata
intermediate (IC) - forme intermediate entre CC' et EC. Cinq experiences de fixation out ete cffectuces avec differentes
concentrations de formol, lamisage el pas de lamisage des (Schantillons avant la fixation el differentes periodes dc temps
entre le prelevement et la fixation. Lcs resultals indiquent que CC esl la forme reguliere. landis que EC el IC sont le resultat
des imperfections de la fixation des echantillons. On propose plusieurs recommandalions pour eviter les formes
aberrantes comme consequence du procede de Fixation qui peut contrarier les etudes de systematique et de dynamique des
populations de cette espece.
INTRODUCTION
Eraditional procedures for treating soft-bottom samples to obtain benthic macrofauna were given, among
MENDEZ. M.N. & M J. CARDELL, 1994. — Effects of sample fixation on body shape of Capitella capitata (Polychaeta.
C apitellidae). In: J.-C. DaUVIN, L. LAUBIER & D..I. REISH (Eds). Actcs de la 4eme Conference internationale des
Polychetes. Mem. Mus. natn. Hist. nat.. 162: 111-117. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
M.N. MENDEZ & M.J. CARDELL
others, by Banse & Hobson (1974), Fauchald (1977), and ELEFTHERiou & Holme (1984). Those techniques
include screening and fixation of samples which may cause alterations to the organisms such as contraction or
damage to soft-bodied animals. Degrees of contraction may vary in some organisms and therefore, changes arc
unpredictable and possibly resulting confusions in identifications.
In previous studies of benthic macrofauna from the littoral zone of Barcelona several body forms of preserved
specimens of Capitella capitatci (Fabricius, 1780) were observed (ROS et cil. , 1990: Ros & CarDULL, 1991:
Flos & Serra, 1992). The different body shapes are found in the same preserved sample and which have not been
distinguished in live specimens. This suggests that treatment of samples may modify the body form of this
species thus impairing taxonomy and population dynamics research. In view of future studies ii is of interest to
determine which sample treatments may produce changes in die body shape of C. capitaia .
MATERIAL AND METHODS
Bottom samples were collected by SCUBA diving from the upper 10 cm of sediment near the Olympic Harbour
of Barcelona (15 m depth) between February and May 1992. The sediment in this site was fine sand (0.125 - 0.250
mm).
Five different tests were designed to evaluate single and combined effects of the following variables of fixation:
formaldehyde concentration, screening of samples and time between collection and fixation of samples.
'Lest 1. — Formaldehyde concentration.
Live specimens were sorted from the sediment and submerged in 1 1 different solutions of formaldehyde in sea
water (from 0.1 to 4%).
Test 2. — Formaldehyde concentration mid screening of samples.
Twenty samples of sediment were collected. The combined effect of die following two variables was tested:
sieving (through a 0.5 mm mesh) or unsieving samples before fixation and formaldehyde concentration (1 and
4 %). Five replicates from each combination were obtained.
Test 3. — Time.
Sixteen samples of sediment were collected. The combined effect of the following three variables was tested:
sieving (0.5 mm) or unsieving samples before fixation, formaldehyde concentration (1 and 10%) and time between
collection and fixation (0. 2, 4 and 6 hours).
In both test 2 and lest 3, sieved samples consisted of 125 ml of sediment and 62.5 ml of seawater, while
unsieved samples consisted of 250 ml of sediment and 125 ml of seawater. The different formaldehyde
concentrations were calculated according to the volume of the overlying water by the addition of concentrated
formaldehyde.
Test 4. — Presence of sediment.
Each of 100 live specimens was transferred to separate jars with 2 ml of a 4% formaldehyde solution, and each
of 100 live specimens was covered by a 3 mm layer of fine sand and fixed by the addition of 2 ml of a 4%
formaldehyde solution.
Test 5. — Volume of sediment.
Five samples of different volumes of sediment were placed and fixed with a 4% formaldehyde solution inside
cylindrical sample jars of several sizes wich were turned several times. After 24 hours of sedimentation, each
sample was divided in three horizontal layers and each level was analyzed separately.
Individuals of the different body shapes were counted in all the tests. A two way ANQVA test and Pearson's
correlations were performed to assess the effect of these variables on the body shape of C. capitatci.
RESULTS
Three different body forms of C. capitatci were distinguished according to their thorax shape. They were called
"contracted C. capitatci " (CC). "enlarged C. capitatci " (EC) and "intermediate C. capitatci " (IC). CC has a rather
pointed prostomium partially withdrawn back into die contracted first setiger, indistinct peristomium and thoracic
setigers are strongly distinct (wider than they tire long). EC presents a prostomium and peristomium widi a
broadly rounded triangular shape, thoracic setigers indistinct (slightly broader than they are long) and a slender
thorax. IC presents an intermediate thorax shape between CC and EC and has a rather pointed prostomium
partially withdrawn
Source : MNHN. Paris
SAMPLE FIXATION AND BODY SHAPE IN CAPITELIA CAP FT AT A
113
Fig. 1. — Anterior end of “contracted Capitella capitata" (CC): a. dorsal view (female), b. lateral view (male), c, lateral
view (juvenile). Anterior end of "elongated C. capitata" (EC): d, dorsal view (male), e, lateral view (female), f. lateral
view (juvenile). Anterior end of “intermediate C. capitata" (IC): g. lateral view (male).
Source : MNHN , Paris
114
M.N. MENDEZ & M.J. CARDELL
back into the contracted first setiger, indistinct peristomium, and thoracic setigers slightly distinct (slightly broader
than thev are long) (Fig. 1). .
Since CC was dominant form in the samples, results only show frequency of EC and IC which were considered
as the modified forms.
Test 1 . — Formaldehyde concentration.
Relative abundances of IC increased with low concentrations of formaldehyde (<0.2%) (Table 1). EC did not
occur. Therefore, individuals which are fixed with low concentrations of formaldehyde probably die slowly and
relaxed thus producing die characteristic enlargement of thorax from IC. This agrees with the suggestion given by
BaNSE & HOBSON (1974) about a relaxed state of animals obtained with few drops of concentrated formaldehyde
in 1 litre of sea water.
Table 1. — Frequency of “elongated Capitella capitata" (EC) and "intermediate C. capilaia" (1C)
at various formaldehyde concentrations (F.C.). N = total number of C. capilaia.
Test 2. — Formaldehyde concentrations and screening of samples.
EC was only present in unsieved samples. Its relative abundance was slightly higher at 1% than at 4%
formaldehyde (Table 2).
The two way anova test showed a significant difference in the relative abundance of EC on sieved/unsieved
samples (F= 10.206, p= 0.006). No significative differences were obtained related to formaldehyde concentrations
(F= 1.506, p= 0.238).
The unsieving procedure seems to be the most important factor to obtain higher quantities of EC.
Nevertheless, a slight formaldehyde concentration effect was observed.
Table 2. — Frequency of “elongated Capitella capilaia" (EC) in sieved and unsieved samples fixed with
1 % and 4 % formaldehyde. Total number of C. capilaia between brackets.
Source :
SAMPLE FIXATION AND BODY SHAPE IN CAPITELLA CAP/TATA
115
Test 3. — Time.
When fixation was performed directly after sampling, EC was only present in unsieved samples (as in test 2).
Nevertheless, when fixation was performed later, EC appeared in sieved and unsieved samples. The relative
abundance was not always higher in unsieved samples. No significative correlations were observed between time
and the other tested variables (Table 3).
Table. 3. — Frequency of “elongated Capitella capitata" (EC) in sieved and unsieved samples Fixed with
1% and 4% formaldehyde at different times after their collection. Pearson’s correlations (r) are calculated
between time and frequency of EC obtained for each procedure. Total number of
C. capitata betwenbrackets. F.C. = formaldehyde concentration.
Depletion of oxygen in sediments has been reported to cause the organisms to crawl near die sediment surface
(Banse & Hobson, 1974). Results obtained in tests 1 and 2 suggest diat lower quantities of EC could result in
samples fixed several hours alter their collection than in samples fixed directly after sampling. Hence, a higher
percentage of individuals wich have a CC shape could be expected when samples are fixed after several hours due to
the upward migration of individuals and the impact of a formaldehyde concentration near to 40 %. However, our
results did not confirm this hypothesis. It is suggested that time produces an unpredictable effect on the amount of
EC.
Test 4. — Presence of sediment.
Fourteen percent of isolated specimens fixed under sediment belonged to EC, whereas this form was not present
among individuals fixed without sediment. A thin layer of sediment, appears sufficient to change the body shape of
some individuals. This was confirmed in test 5.
Test 5. — Volume of sediment.
Results given in Table 4 show that there was a direct relationship between percentage of EC and volume of
sediment inside a jar. Also a gradient was observed: the lower layers had the highest percentages of EC.
Correlations between cumulative volumes (from upper to lower layers) and relative abundance of EC were highly
significative (r= 0.939, p< 0.01, n= 13). High frequencies of EC may be caused by compression increasing and
formaldehyde diffusion decreasing with sample volume.
Table 4. — Frequency of “elongated Capitella capitata ” (EC) in five samples of different volumes of
sediment divided in three equal layers inside a jar. Total number of C. capitata between brackets.
Results obtained in the five tests suggest that the simultaneous presence of the CC, EC and IC in a sample can
be explained by die combined effect of formaldehyde concentration and sediment. Lower formaldehyde
concentrations, during fixation, may induce organisms to change from a contracted (CC) to a more relaxed shape
116
M.N. MENDEZ & M.J. CARDELL
(EC) The combined effect of sediment and formaldehyde in an unsieved sample inside ajar may be explained due
to the thickness of die sediment which can delay Hie diffusion of formaldehyde, and prolonging death. The presence
of large amounts of sediments may be responsible of an increase in the quantities of EC.
DISCUSSION
Traditional techniques used in taxonomy of polychactes are based on collection, screening (before fixation),
fixation and preservation. Neverdicless, in population dynamics studies of C. capitata, fixation is generally
performed before screening (Warren, 1976; Tsutsumi & Kikuchi, 1984; TSUTSUMI, 1987). When fixation is
performed before screening, some EC and IC may be present and thus result in errors of taxonomy and populations
dynamics:
- Taxonomy. The evident peristomium of EC can be confused with the achaetous first segment ot die genus
Capitomastus, although diere are some odier features to distinguish between both genera. This confusion has
recently been studied by WARREN (1991).
- Population dynamics. Population dynamics studies of C. capitata are performed by different thoracic
measures (Warren, 1976; Tsutsumi & Kikuchi, 1984; Tsutsumi, 1987; Martin, 1991), which may be
strongly affected by treatment of samples, so erroneous interpretations can be obtained.
CONCLUSIONS
Treatment of soft-bottom samples during fixation may affect the shape of fixed C. capitata. Body shapes were
related to different combinations of the tested variables. The elongated thorax of IC seems to be associated with
low formaldehyde concentrations. Fixation of samples widiout sieving may produce an increase in the frequency of
EC: compression and weight of sediment inside a sample jar affect die shape of C. capitata, probably because of
decreased formaldehyde diffusion and mechanically prevented body contraction.
Mistakes in taxonomy and population dynamics studies can result from inappropiate fixing procedures.
Therefore, to avoid fixation anomalies in C. capitata it is recommended:
- Sieve (he sample before fixation to avoid effects by compressed sediments. If diis is not possible, fix small
volumes of sediment (e.g. 200 ml) in several sample jars to allow die diffusion of formaldehyde and to minimize
compression.
- Ensure that fixation is done at least at 4% formaldehyde, particularly if the sample cannot be sieved before
fixation.
- Turn the sample jar several times after fixation for about 15 minutes to be certain that all the individuals have
died.
- Maintain the time between collection and fixation constant during the study.
ACKNOWLEDGMENTS
This research was supported by the Villa Olunpica, S.A., Barcelona. We are grateful to Dr. Rafael Sarda Dr.
Josep M. GlLl and Dr. Jordi FLOS for their advice and comments on the manuscript. We wish to thank Dr. Judith
GrasSLE for her constructive comments.
REFERENCES
BaNSE. K. & K. D. Hobson. 1974. — Benthic errantiate polychaetes of British Columbia and Washington. Dull. Fish.
Res. Board Can.. 185 : 1-111.
Eleftheriou. a. & H. HOLME, 1984. — Macrofauna techniques. In: N.A. HOLME & A. D. MclNTYRE (eds). Methods for the
study of marine benthos. Blackwell Scientific Publications. Oxford : 140-216.
FaUCHALD, K., 1977. — The polychacte worms. Definitions and keys to the orders, families and genera. Nat. Hist. Mus.
Los Ang. County Sci. Ser., 2 : 1-188.
Source :
SAMPLE FIXATION AND BODY SHAPE IN CAPITELLA CAP HAT A
117
Flos, J. & J. Serra. 1992. Repercusid ecoldgica i geodindmica de tes actuacions en el front marltim de llevant de
Barcelona. Informe iconic, V.O.S.A., Barcelona, 144 pp.
Martin, D., 1991. Macroinfauna de una bahfa mediterrdnea: esludio de los niveles de organizacidn de las poblaciones
de anelidos poliquelos. Doctoral Thesis. U. Barcelona, 456 pp.
ROS.J.D.. Cardell. M.J., Alva, V., Palacin, C. & I. LLOBET, 1990. — Comunidades sobre fondos blandos afectados por
un aporte masivo de lodos y aguas residuales (litoral frente a Barcelona, Mediterraneo occidental) : resultados
preliminares. Bentos 6 : 407-423.
Ros, J.D. & M.J. CARDELL, 1991. — Effect on benthic communities of a major input of organic matter and other
pollutants (coast off Barcelona. Western Mediterranean). Toxicol Environ, Chem., 31-32 : 441-450.
TSUTSUMI, H., 1987. Population dynamics of Capitella capitata (Polychaeta: Capilcllidae) in an organically polluted
cove. Mar. Ecol. Prog. Ser., 36: 139-149.
TSUTSUMI, II. & T. KlKUCHI, 1984. Study of the life history of Capitella capitata (Polychaeta: Capitellidae) in
Amakusa. South Japan including a comparison with other geographical regions. Mar. Biol., 80 : 315-321.
Warren. L.M.. 1976. — A population study of the polychaetc Capitella capitata in Plymouth. Mar. Biol., 38 : 209-
216.
Warren, L.M., 1991. — Problems in Capitellid taxonomy. The genera Capitella, Capilomastus and Capitellides
(Polychaeta). Ophelia , suppl. 5 : 275-282.
Source : MNHN. Paris
13
Ultrastructure of sense organs and the central nervous
system in Parenterodrilus taenioides and their
phylogenetic significance in the taxon
Protodrilida (Annelida, Polychaeta)
Giinter PURSCHKE * & Claude JOUIN-TOULMOND **
* Spezielle Zoo logic. Fachbereich 5
Universitat Osnabruck
D-49069 Osnabruck. Germany
** Biologie et Physiologic des Organismes Marins
Universite Pierre el Marie Curie
4. place Jussieu
F-75252 Paris Cedex 05. France
SUMMARY
The following sense organs palps, nuchal organs, and presumed unpigmented ocelli, as well as the central nervous system
were investigated by electron microscopy in Parenterodrilus taenioides . The palps are mobile sensory structures bearing motile
cilia and four types of sensory cells, including presumed phaosomous ocelli. The palp canals are small, filled with cell bodies
ol muscle cells and a few coelenchyme cells. The canals are covered by a cord of coelenchyme cells. The comparatively large
nuchal organs are identical in structure with those of the other Protodrilida. There are two types of presumed ocelli located in
posterior ganglionic expansions of the brain. The palps are innervated by three nerves originating from the dorsal and ventral
roots of the circumoesophageal connective. The most exceptional features of the brain are four ganglionic expansions
extending far posteriorly into the head segment. The lateral ones fuse with the small dorsal root of the circumoesophageal
connectives. These findings are compared with the sense organs and the nervous system of the other Protodrilida. They clearly
corroborate the supposed relationship ol the Protodrilida and additional autapomorphies demonstrate the derived position of P
taenioides.
RESUME
Ultrastructure des organes sensoricls et du systeme nerveux central dc Parenterodrilus taenioides et leur signification
Phylogenetique chez les Protodrilida (Annelidcs Polychetes)
Les organes sensoriels tels que palpcs. organes nucaux. structures assimilees a des ocelles non pigmentes, ainsi que le
systeme nerveux central ont ete etudics au niveau ultrastructural chez Parenterodrilus taenioides. Les palpes sont des appen-
PURSCHKE G. & C. Jouin-Tqulmond, 1994. — Ultrastructure of sense organs and the central nervous system in
arenterodrdus taenioides and their phylogenetic significance in the taxon Protodrilida (Annelida. Polychaeta). In:
DauviN' L. LAUBIER & D.J. REISII (Eds). Actes de la 4cme Conference internationale des Polychetes. M£m Mus naln
Hist, not., 162 : 1 19-128. Paris ISBN 2-85653-214-4.
Source : MNHN, Paris
120
G. PURSCHKE & C. JOUIN-TOULMOND
dices sensoriels cilies et mobiles qui portent quatre types de cellules scnsorielles, dont des ocelles de type phaosome. Les
canaux internes des palpes sont minces, remplis par les corps cellulaires des cellules musculaires et par quelqucs cellules du
coelenchyme qui formenl aussi un cordon cellulairc a la peripherie de chaque canal. Les palpes re^oivent trois nerfs issus des
racines dorsales et ventrales des connectifs p£rioesophagiens. Les organes nucaux, relativement larges, ont une structure
identique k ceux des autrcs Protodrilida. Deux autres types de structures, assimilecs a des ocelles non pigmentes, sont logees
dans des expansions ganglionnaires posterieures du cerveau. Les caractiSristiques les plus remarquables du cerveau sont ces
quatres expansions ganglionnaires qui s'etcndent loin vers 1’arriere, dans le segment cephaliquc. Les expansions les plus
laterales fusion nent avec les petites racines dorsales des connectifs perioesophagiens. Ces caractcrcs sont compares k ceux des
autres Protodrilides et les nouvelles autapomorphies revelees par ce travail demontrent que P. laenioides csl une forme derivee.
L'enscmble des res u I tats confirme les relations prelablement etablies au sein des Protodrilida.
INTRODUCTION
The Protodrilida are interstitial polychaetes characterized by a long and slender body, reduced or absent
parapodia, a pair of prostomial appendages (palps), and a pygidium generally with two adhesive lobes. The about
60 known species of the taxon belong to only four genera: Saccocirrus Bobretzky, 1871, Protodrilus Hatschek,
1880, Protodriloides Jouin, 1966 and Parenterodrilus Jouin, 1992. Electron microscopic investigations were
conducted to clarify the functional morphology of selected organs as well as to test the proposed monophyly of
the Protodrilida and tiieir subordinate taxa, to evaluate their relationship and to find synapomorphies with their
supposed sister group, the Spionida (e.g., PURSCHKE & Jouin, 1988; Purschkh, 1990a, 1993). In contrast to the
small body size and the apparently simple organization of these polychaetes, their sense organs and the central
nervous system turned out to be rather complex structures when investigated by electron microscopy (Eakin et
al. , 1977; PURSCHKE, 1990a, 1990b, 1990c, 1992, 1993; PURSCHKE & JOUIN-TOULMOND, 1993). Therefore, these
structures provide numerous characters which might be useful for phylogenetic considerations.
Sense organs present in every species are: the palps, the nuchal organs, and various types of unpigmented
presumed ocelli. Pigmented ocelli only occur in the Saccocirrus species and a few Protodrilus species. These
structures have now been investigated in species of every genus except the monotypic Parenterodrilus , which is
so lar only known lrom sublittoral coral sands of the island of Moorea, French Polynesia. Parenterodrilus
tcienioides is especially remarkable because it is the only known polychaete possessing a vestigial alimentary
canal, without mouth and digestive cavity (JOUIN, 1979, 1992). Thus, the main purpose of the present
investigation was to clarify die functional morphology of die sense organs and die central nervous system of this
rare species, in order to use these supplementary data for a comprehensive phylogenetic discussion of the
Protodrilida. The present findings fit very well into a dendrogram showing die presumed relationship of the
subordinate taxa of the protodrilidans which has previously been suggested (PURSCHKE & JOUIN, 1988) and which
can now be based on an even larger number of characters.
MATERIAL AND METHODS
Specimens of P. laenioides were collected by die junior author in sublittoral sands of die barrier reef at die
type locality in Moorea, French Polynesia (JOUIN, 1979). After relaxauon in a mixture of equal parts of sea water
and 7.7 % MgCl2, specimens were fixed in a cacodylate buffered (0.2 M, pH 7.4) solution of 2 % glutaraldehyde,
adjusted widi NaCI to about 1,300 mosM for 1 h. They were rinsed in die same buffer, postfixed in buffered 1%
OSO4, dehydrated in an ethanol series, and embedded in Epon. Ultrathin secdons of two specimens were cut widi
a diamond knife on a Reichert Ultracut E microtome and ribbons of sections were collected on single slot grids
coated widi piololonn support Film in order to obtain complete series of ultrathin sections. They were stained in
an
Fig. 1 A-F. Parenterodrilus laenioides. Palps. A. Low power TEM micrograph of cross section appr. 25 pm above the palp
base; center occupied by palp canal (pc) and coelenchyme cells ( coc ); palp nerves encircled; arrow points to position of
blood vessel. B. Cross section of palp canal. C. Ventral palp nerve vpnj and longitudinal muscle fibres; note disappearance
ol extracellular lamina (la) between coelenchyme and epidermal cells lateral to vpnj (small arrows ); the large arrow
points to position of palp canal. D. Tangential section of ventral side with ciliated cells ( cce ). epidermal supporting cells
(ep) and sensory cells (arrows). E. Coelenchyme cell with nucleus. F. Blood vessel (bv). - cce ciliated cell, cm circular
muscle fibre, coc coelenchyme cell, cu cuticle, dpn dorsal palp nerve, ep epidermal supporting cell, gc glial cell, gl gland
cell, la extracellular lamina, bn longitudinal muscle cell, pc palp canal, vpnj 4 ventral palp nerve 1,4.
SENSE ORGANS AND CENTRAL NERVOUS SYSTEM IN PARENTERODRILUS TAENIOIDES
121
Source : MNHN , Paris
122
G. PURSCHKE & C. JOUIN-TOULMOND
LKB Ulirosiainer and examined with a Zeiss EM 109 electron microscope. Reconstruction of (he nervous system
was done from low power electron micrographs taken at intervals of between 0.7 pm and 3.5 pm, depending on
(he structures observed.
RESULTS
In Parenterodrilus taenioides the palps arise in an anterior-lateral position from the prostomium. The filiation
of the anterior end is very well developed; in addition to numerous sensory cilia, the palps, prostomium and head
segment (= peristomium) bear mobile cilia as well. The nuchal organs are heavily ciliated, rounded areas of about
25 pm diameter at die posterior end of the prostomium. IJnpigmented ocelli are not visible with light microscopy.
Palps. The palps are circular to oval in cross section. They are composed of cuticle, epidermis, sensory cells,
intraepithelial nerves, a palp canal, a small blood vessel, and so-called coelenchyme cells (Fig. 1A-F). The
epidermis is comprised of supporting cells, with glandular and ciliated cells distributed among them. The latter are
restricted to the ventral side where they are arranged in bands. There are three palp nerves: die medial nerve
( \pti4\ see PURSCHKE, 1993 for terminology) is the largest and contains about 330 nerve fibres; the other nerves
are considerably smaller and consist of 15 ( dpn ) and 35 (vpnj) fibres. Small branches of these longitudinal nerves
form a network of nerve cell processes ventral ly, and around die palp canals. Each nerve is pardy enveloped by
glial cells (Fig. 1 B). In the nerve fibres clear vesicles widi a diameter of 40-60 nm and dense-cored vesicles of VO-
95 nm diameter are present (Fig. 1C). Neuroneuronal and neuromuscular synapses were frequently observed
within die nerve tracts.
Each palp has a small canal, 10-15 pm in diameter (Fig. 1A-C, E-F). The canals are situated ventrally in the
palps and unite behind the neuropile of the brain. They are filled widi muscle cells and a few coelenchyme cells,
surrounded by an extracellular lamina. There arc only a few small muscle fibres outside die palp canals, most of
which arc situated close to the small ventral palp nerve (vpnp. Fig. 1C). Besides these longitudinal fibres diere are
a few small circular fibres in die palp canals. The canals are covered dorsolaterally by coelenchyme cells, which
are electron-lucent with only very few organelles and an irregular outline (Fig. 1 A, C, E). Although of presumably
mesodermal origin, this coelenchyme tissue is not separated from die epidermis by a basal lamina on all sides;
extracellular material was only detectable between die palp canal and die small palp nerve (Fig. 1C). Each palp is
supplied by a small blind-ending blood vessel which is situated at die palp canal opposite to die main palp nerve.
Three types of bipolar sensory cells have been found on the palps and die prostomium (Fig. 2A-F). The
monociliary type-1 sensory cells are so-called collar receptors (e.g. Schlawny el al.t 1991): the cilium passes
through die cuticle and is surrounded by 10 modified microvilli (Fig. 2A-B). A cylinder of electron-dense material
lies below the microvilli. It is connected to die ciliary rootlet just underneadi die basal body. Proximally, thin
filaments originate from this cylinder and enter die microvilli. The dendritic processes are about 1 pm in diameter
and contain 3-4 long mitochondria (Fig. 2A). The second type of sensory cell is multiciliary, widi 3-9 cilia
penetrating the cuticle (Fig. 2C-D). These sensory cells are die most frequent; they eidier occur in isolation or
grouped in two adjacent sensory cells forming a ciliary tuft. The cilia are of different lengdis and may be up to
15 pm long. They usually arise from a slight depression of die cell apex, which creates a raised rim at die
periphery of die sensory cell (Fig. 2D). The cilia are surrounded by short microvilli and anchored by long roodets
(Fig. 2C). Sensory cells of the diird type have non-penetrative (intracuticular) cilia and diey may be isolated or
clustered in groups of up to 9 sensory cells (Fig. 2E-F). Their long dendritic processes extend above die level of
die adjacent epidermal cells and bear one or two horizontal cilia (Fig. 2E). The cilia are about 4 pm long and have
a 9x2+0 axoneme (Fig. 2E, inset). Usually they divide in branches in which the microtubules are successively
lost.
Nuchal organs. The nuchal organs consist of numerous ciliated supporting cells, an average of seven bipolar
sensory cells, and a retractor muscle (Fig. 3A-D), which runs ventromedially and attaches to die posterior end of
the palp canal. Ciliated supporting cells surround die dendritic processes of die sensory cells forming die olfactory
chamber (3.5-4 pm in diameter) in die middle of the ciliated area (Figs 3 A, 4). They bear ail average of 35 cilia
(3.2 cilia per pm2), which are anchored by basal bodies and long striated rootlets. The ciliated supporting cells
give also rise to numerous microvilli; these form a paving-stone-like cover above die cuticle, which is only
penetrated by die cilia of diese cells (Fig. 3B-C). This layer also covers the olfactory chamber. The dilated
microvillar tips are cubic in shape, only 20 nm apart and interconnected by fibrillar material (Fig. 3C). Numerous
clear vesicles, coated vesicles, coated pits and lysosomes indicate a considerable degree of endo- or exocytosis in
SF.NSE ORGANS AND CENTRAL NERVOUS SYSTEM IN PARENTERODRILUS TAENIOIDES
123
Fig 2A-F. — I arenlerodrilus taen, aides. Sensory cells of palps. A. Collar receptors. B. Cilium and microvilli of collar receptor
in cross section. C. Multicihary sensory cell; nucleus (n) situated laterally. D. Cross section of apex of inulticiliary sensory
cell (sc); note clear vesicles accumulating in sensory cell. E. Group of sensory cells with intracuticular cilia; cross
sectioned cilia belong to ciliated epidermal cell; inset: sensory cilia in cross section. E. Presumed ocellus with phaosome
(ph). The arrow points to a sensory cell with intracuticular cilium. - cu cuticle, ep epidermal cell, m mitochondrion mv
microvillus, n nucleus, pc palp canal, ph phaosome. /rootlet, sc sensory cell, za zonula adhaerens.
Source
124
G. PURSCHKE & C. JOUIN-TOULMOND
these eells (Fig. 3A-B). Each sensory cell bears one cilium with a 9x2+0 axoneme and a few microvilli (Fig. 3A,
D). The ciliary rootlets are vestigial: 0.5 jam long and 0.04 pm thick. The ciliary shafts branch. In the branches the
microtubules are successively lost, resulting in structures indistinguishable from regular microvilli (Fig. 3D),
Microvilli and ciliary branches extend into die subcuticular space above die supportive cells outside die olfactory
chamber (Fig. 3A).
Presumed Ocelli. In each palp four presumed ocelli (type 1) have been found close to die main palp nerve
(Fig. 4). They consist of a single sensory cell characterized by an intracellular vacuole (phaosome) containing
numerous microvillus-like ciliary branches (Fig. 2F). There are no pigmented or unpigmented ocelli in the
prostomium of P. laenioides. However, die type-2 and type-3 unpigmented ocelli are located in the peristomium
(= head segment) in the lateral posterior ganglionic expansions of die brain (Figs 3E-F, 4). Each ocellus consists
of a sensory cell and a supporting cell forming an extracellular cavity. These cavities are completely filled with
microvillus-like branches of two cilia in bodi types. There are two of the minute type-2 ocelli (3x2x2 pm; Fig. 3E)
but five of the type-3 ocelli (18x6x4 pm; Fig. 3F) in each specimen investigated. Odier differences concern
position, branching pattern of cilia and arrangement of microvilli. The ocelli will be described in more detail
separately (Purschke & Jouin-Toulmond, 1993).
Central nervous system. The neuropile of the brain is situated in the prostomium in the curve formed by the
palp canals (Fig. 4). Conspicuous features are two pairs of dorsal expansions ( pe in Fig. 4) formed by nerve cell
processes and, posteriorly, by the perikarya of neurons and glial cells. These expansions extend far into the head
segment; the lateral ones contain the presumed ocelli. The ventral nerve cord communicates with the brain
through die circumoesophageal connectives (cc). Anteriorly, before Uiese nerves turn towards die brain, each
connective divides into a ventral (vrcc) and a dorsal root (drcc). The dorsal roots ( drcc ) and die nerve cell
processes of die lateral expansions (pe) enter the neuropile togedicr as one nerve. The nuchal nerve (nn) very
likely emanates from the lateral expansion (pe), whereas die medial expansion gives rise to a posteriorly running
dorsal nerve ( dn ). Although gut and stomodaeum are residual, die stomatogastric nerves are well-developed and
arise ventrally close to die ventral roots of the circumoesophageal connectives (vrcc). The main palp nerve (vpn4)
emanates laterally Irom die anterior part of die brain and receives its fibres from a dorsal and a ventral root. The
other palp nerves emerge directly from the roots of the circumoesophageal connectives: die second ventral palp
nerve ( vpn /) from die ventral root and die diin dorsal palp nerve (dpn) from die common nerve containing the
nerve fibres of the lateral posterior expansion and the dorsal root close to die brain.
DISCUSSION
The sense organs and the central nervous system of P. taenioides are structurally complex. Although the
digestive system is vestigial and not functioning (JOUIN, 1979, 1992), there is no evidence for a reduction of (he
sensory organs compared with other species ol the Protodrilida. However, do dicse organs provide additional
leatures to elucidate die phylogenetic relationship between them? In a phylogenetic tree previously suggested by
PURSCHKE & JOUIN (1988), Protodrilus and Parenterodrilus were sister groups forming die Protodrilidae which
is in turn the adelphotaxon ot Saccocirrus. Finally, these taxa most likely represent the sister group of
Protodriloides. Very likely, the taxon Protodrilida is related to the Spionida or one of its subordinate taxa
(ORRHAGE, 1974; PURSCHKE & JouiN, 1988; PURSCHKE, 1993). At present the Protodrilida is still retained
because its sistergroup has not yet been recognized.
I lie palps of P. taenioides are equipped widi a variety of sensory cells which allow reception of different
sensory stimuli from a wide area around die anterior end. They differ externally from those of Saccocirrus and
most Protodrilus species (except P. brevis-, see JOUIN, 1970) in die presence of modle cilia (Purschke, 1993). In
the Spionida such a filiation is generally present, located in a groove and used for collecting food particles
(Dauer, 1987; Fauchald & Jumars, 1979). Since a moudi is absent in P. taenioides, the remaining functions
10 -A.' - Parenterodrilus taenioides. A-D. Nuchal organ. A. Low power micrograph showing entire organ in cross
secuon: arrows point to sensory cell cilia; subcuticular space with microvilli Unv) and ciliary branches of sensory cells. B.
Ciliated cells with cover of microvillar tips (mvc). C. Microvillar tips in transverse section. D. Sensory dendrites with cilia
... and microvilli. E-F. Presumed ocelli. E. Small ocellus (type 2). F. Large ocellus (type 3); arrow points to sensory cell
dl'urn. - c cilium. cce ciliated supporting cell, coc coelcnchyme cell, cu cuticle, gc glial cell, in mitochondrion, mv
microvillus, mvb microvillus-like ciliary branch, mvc microvillar cover, och olfactory chamber, pe posterior expansion of
brain, r rootlet, nn reUactor muscle, si: sensory cell, sd sensory dendrite, sue supporting cell, za zonula adhaerens.
Source :
SENSE ORGANS AND CENTRAL NERVOUS SYSTEM
IN PARENTERODRILUS TAENIOIDES
125
Source : MNHN. Paris
126
G. PURSCHKE & C. JOUIN-TOULMOND
may be orientation in the interstitial medium and a more rapid exchange of water at the surface o! the animal.
Since motile cilia are also present on die palps of Protodriloides, diis character might be a vestige of a more
developed ciliation which could be assumed for die last common stem species with the Spionida. The sensory
cells with cilia penetrating die cuticle or with non-penetrative cilia are of minor phylogenetic importance, because
similar cells have been found in the other Protodrilida and they are not different from sensory cells generally
present in annelids (Storch & Schlotzer-Schrehardt, 1988; Purschke, 1993). Among the sensory cells of
die palps only the phaosomous ocelli can be considered for phylogenetic considerations. Phaosomes - intracellular
cavities containing die presumed light-sensitive organelles - occur only occasionally in polychaetcs (Purschke &
Jouin-Toulmond, 1993,). They are found neidier in Saccocirrus nor in Protodriloides but arc present in die
palps of several Protodrilus species (Purschke, 1993; Jouin-Toulmond & Martin, unpubl. observ.). These
phaosomes are structurally identical with diose of P. taenioides and, therefore, most likely represent a
synapomorphy of Protodrilus and Parenterodrilus.
With respect to the internal structure, the palps are most similar to those of Protodrilus. They differ from those
of Saccocirrus in die absence of the ampullae, posterior expansions of die palp canals. However, die palp canals
are considerably thinner in P. taenioides. and die musculature outside die canal and die blood vascular system arc
reduced compared with Protodrilus and Saccocirrus (PURSCHKE, 1993). The occurrence of a cord of coelenchyme
cells outside the canal and the loss of the external lamina between diem and the epidermis arc unique for P.
taenioides. These features are very likely correlated with die absence of podocytes, which form part of the wall of
the palp caiuds in die prostomium of Protodrilus and Saccocirrus (Purschke, 1993). In diese genera die palp
canals probably serve as a hydroskeleton filled with movable coelenchyme cells, and the podocytes have been
regarded as the site where fluid is introduced into die canals from the blood. Since movable coelenchyme cells, or
a fluid-filled lumen, are absent in P. taenioides. stiffness of the palps is very likely achieved by the musculature of
the palp canals and the external coelenchyme tissue. Consequendy, podocytes appear to be redundant.
The nuchal organs of all Protodrilida investigated, including P. taenioides , are almost identical in structure and
consist of the same types of cells as usually found in polychaetes (PURSCHKE, 1986, 1990a; Storch &
SchlOtzer-Schrehardt, 1988; RHODE, 1990). In nuchal organs which are not located in deep pits, the ciliated
suppordng cells generally show structural specialisations which cover and protect the cilia and microvilli of die
sensory cells. Paving-stone-like covers of microvillar endings joined by fine fibrils have only been found in the
Spionidae Pvgospio elegans and Scolelepis squamata (SCHLOTZER-SCHREHARDT 1987; RHODE, 1990) and in
every species of the Protodrilida, which indicates a high probability of synapomorphy of diis character.
The sense organs found in the posterior expansions of the brain in P. taenioides show striking similarities to
photoreceptors - for example, a great expanse of plasmalemma in die form of microvillus-like cell processes, and
the position of die organs beneadi the epidermis (Eakin & Hermans, 1988). Such presumed ocelli without
shading pigment have repeatedly been reported for polychaetes and many species possess at least one type of
these ocelli, often in addition to pigmented ones (PURSCHKE, 1992). Their great structural diversity, however,
makes it likely dial unpigmented ocelli evolved convergently several times in annelids. Unpigmented ocelli are
also present in every species of die Protodrilida. Apart from the ocelli (type 1) of the palps, die type-2 and type-3
ocelli of P. taenioides are completely different to any ocellus of Protodrilus. Due to their different position and
structure, die ocelli of P. taenioides are not homologous to the so-called statocysts, to die phaosomes or to die
pigmented eyes occurring in the prostomium of various Protodrilus species (Eakin el al.. 1977; PURSCHKE,
1990b,c). There are also no similarities to the presumed ocelli of Protodriloides (unpubl. observ.). On die odier
hand, there is a certain probability of homology widi die type-1 ocelli of Saccocirrus (PURSCHKE & JOUIN-
Toulmond, 1993). Since die sister group relationship between Parenterodrilus and Protodrilus is well
established by several synapomorphies, diis character may be regarded as a symplesiomorphy taken from die stem
species of saccocirrids and protodrilids.
The structure of die central nervous system and die innervation of die anterior end have great potential in
phylogenetic reconstruction (Orrhage, 1990, 1991). As shown previously, the brain with its nerves and the palp
anatomy of Protodriloides, Protodrilus and Saccocirrus give strong evidence for a relationship to the Spionida
(PURSCHKE, 1993). As was to be expected, the central nervous system of P. taenioides is very similar to dial of
Protodrilus and Saccocirrus and corroborates the general pattern observed; e.g., the roots of the
circumoesophageal connectives, the stomatogastric nerves and die palp nerves arise in corresponding positions,
die main palp nerve vpii4 has a ventral and a dorsal root, and the dorsal root of die circumoesophageal connectives
is much smaller than die ventral root. However, diere are only three palp nerves, which means, that die nerves
vpii2 and vpnj very likely have been lost; furdiermore, there is only one dorsal nerve and die posterior ganglionic
expansions of die brain are unknown in die other taxa. The nuchal nerve probably also has a different posidon.
SENSE ORGANS AND CENTRAL NERVOUS SYSTEM IN
PARENTERODRILUS TAENIOIDES
127
Shc°HREHALTfS7Tr^Spmay,haVe differ?"1 p,,si,ions in ,hc Spionkla as well (Orrhage, 1964 Schi otzer-
Z 1 ,US ,aemo,des- Neuropile of Ore brain (b) and associated nerves. Dorsal view on the left side the dorsal
PZ\°l 'he uC "erV0US SyJS,Cm has been omitted' reconstruction from electron microscopic ^observations cr
orean Pha§eal conn,cc,,ve- fn dorsal nerve. dpn dorsal palp nerve, drcc dorsal root of cr. nn nuchal nerve no nuchal
~ion/ofd^eScUmri T' '• 'ypC‘2 and ty'^-3 ocelli; och olfact°ry chamber, pc palp canal, pe ^sterm? gangTonk
expansion o t brain, sn stomatogastnc nerve, vp/iy 4 ventral palp nerve 1 ,4, vrcc ventral root of cc. g g
,'llC prcsent,tindinl8.s on P- laenioides corroborate its presumed relationship witli die other
the mnn tnt nf f0UP T '"T P 10 Pro'odrilus can be sustained by newly found synapomorphies: loss of
palp canals and presence of tentacular phaosomes. Several additional autapomorphtes clearly
' j *e derived position of P. taemoides : e.g„ coelenchyme cells present outside the palp canal loss of
podocytes in die canal, brain wttii posterior ganglionic expansions, loss of die palp nerves vpn2 and vpnj and loss
^^S^So^CharaCterS ^ l° bC PleSi°m0rphieS ^ 3 bellcr -'derstanding of the
128
G. PURSCHKE & C. JOUIN-TOULMOND
REFERENCES
DAUER, D.M.. 1987. — Systematic significance of the morphology of spionid palps. Bull Biol Soc. Wash., 7 : 41-45.
Eakin, R.M.. Martin. G.G. & Reed, C.T., 1977. — Evolutionary significance of fine structure of archiannelid eyes.
Zoomorphologie, 88 : 1-18.
Eakin, R.M. & Hermans, C.O., 1988. — Eyes. In: W. Westheide & C.O. Hermans (eds). The ultrastructure of Polychaeta.
Microfauna Mar.. 4 : 135-156.
FAUCHALD, K. & JUMARS, P.A.. 1979. — The diet of worms: a study of polychaete feeding guilds. Oceanogr. Mar. Biol. Ann.
Rev.. 17 : 193-284.
JouiN, C., 1970. Recherches sur les Protodrilidae (Archiannelides) : I. Etude morphologique et systematique du genre
Protodrilus. Cah. Biol, mar., 11 : 367-434.
JOUIN. C., 1979. — Description of a free-living polychaete without a gut: Asiomus laenioides n. gen., n. sp. (Protodrilidae,
Archiannelida). Can. J. Zool. , 57 : 2448-2456.
JouiN, C.. 1992. — The ultrastructure of a gutless annelid Parenlerodrilus gen. nov. laenioides (= Asiomus laenioides)
(Polychaeta. Protodrilidae). Can. J. Zool, 70 : 1833-1848.
ORRHAGE, L.. 1964. — Anatomische und morphologische Studien iiber die Polychaetenfamilien Spionidae. Disomidae und
Poecilochaetidae. Zool Bidr. Uppsala. 36 : 335-405.
ORRHAGE, L.. 1974. Ubcr die Anatomic, Histologic und Verwandtschaft der Apistobranchidae (Polychaeta. Sedentaria)
nebst Bemerkungen liber die systematische Stellung der Archianneliden. Z. Morph. Tiere, 19 : 1-45.
ORRHAGE. L., 1990. — On the microanatomy of the supraoesophageal ganglion of some amphinomids (Polychaeta. Errantia)
with further discussion of the innervation and homologues of the polychaete palps. Acta Zool. (Stockh.), 71 : 45-59.
ORRHAGE, E., 1991 . On the innervation and homologues of the cephalic appendages of the Aphroditacea (Polychaeta). Acia
Zool (Stockh.). 72:233-246.
PURSCHKE, G., 1986. — Ultrastruclure of the nuchal organ in the interstitial polychaete Stygocapitella subterranea
(Parergodrilidae). Zool Scr., 15 : 13-20.
PURSCHKE, G.. 1990a. — Comparative electron microscopic investigation of the nuchal organs in Protodriloides , Protodrilus
and Saccocirrus (Annelida, Polychaeta). Can. J. Zool, 68 : 325-338.
PURSCHKE, G., 1990b. — Fine structure of the so-called statocysts in Protodrilus adhaerens (Protodrilidae, Polychaeta). Zool.
Anz.. 224 : 286-296.
PURSCHKE. G., 1990c. — Ultrastructure of the "statocysts" in Protodrilus species (Polychaeta): reconstruction of the cellular
organization with morphometric data from receptor cells. Zoomorphology, 110 : 91-104.
PURSCHKE. G.. 1992. — Ultraslructural investigations of presumed photoreceptive organs in two Saccocirrus species
(Polychaeta. Saccocirridae). J. Morphol., 21 1 : 7-21.
PURSCHKE, G.. 1993. — Structure of the prostomial appendages and the central nervous system in the Protodrilida
(Polychaeta). Zoo morphology, 113 : 1-26.
PURSCHKE, G. & JouiN, C., 1988. — Anatomy and ultrastructure of the ventral pharyngeal organs of Saccocirrus
(Saccocirridae) and Protodriloides (Protodriloidae fam. n.) with remarks on the phylogenetic relationship within the
Protodrilida (Annelida: Polychaeta). J. Zool (Lond.), 215 : 405-432.
PURSCHKE, G. & JOUIN-TOULMOND, C., 1993. — Ultras tructure of presumed ocelli in Parenlerodrilus tcienioides (Polychaeta.
Protodrilidae) and their phylogenetic significance. Acta Zool (Stockh.), 74 : 247-256..
Rhode, B., 1990. Ultrastructure of nuchal organs in some marine polychaetes. J. Mo/phol, 206 : 95-107.
Sen lawny , A.. GRtJNIG, C. & PFANNENSTIEL, II. -Dm 1991. — Sensory and secretory cells of Ophryotrocha puerilis
(Polychaeta). Zoomorphology ,119: 209-215.
SchlOtzer-Schrehardt, U., 1987. — Ultrastructural investigations of the nuchal organs of Pygospio elegans (Polychaeta).
II. Adult nuchal organs and dorsal organs. Zoomorphology. 107 : 169-179.
Storch, v. & SchlOtzer-Schrehardt, U.. 1988. — Sensory structures. In: w. Westheide & C.O. Hermans (eds), The
ultrastructure of Polychaeta. Microfauna Mar.. 4 : 121-133.
Source : MNHN. Paris
14
Genome size in Polychaetes:
relationship with body length and life habit
R. SOLDI * L. RAMELLA * M. Cristina GAMBI **
Paolo SORDINO ** & Gabriella SELLA *
* Department of Animal Biology
University of Turin, via Accademia Albertina 17
10123 Torino, Italy
** Laboratorio di Ecologia del Benthos
Stazione Zoologica " Anthon Dohm"
80077 Ischia, Napoli, Italy.
ABSTRACT
Only a few species of polychaetes have previously been analyzed for nuclear DNA content (CONNER et al. .1972). by
means of microdensi tome trie analysis of the amount of Feulgen-stained DNA in interphase nuclei. We have correlated genome
sizes of 47 species of Polychaeta with mean body length of adult worms. In the species examined genome sizes ranged from
0.07 to 1.2 pg of DNA per nucleus in interstitial species and from 0.4 to 7.2 pg in macrobenthic species. The lowest values are
among the lowest genome sizes of invertebrates so far investigated. Genome size appeared to be significantly correlated with
mean body length (r = 0.30: df = 45; 0.05 < P < 0.01 ), which ranged from 0.9 mm to 250 mm in the species we examined.
RESUME
Taille du genome chez les Polychetes : rapports avec la taille du corps et Phabitat
Le contenu nucleaire en ADN chez les Polychetes a ete jusqu'a maintenant etudie chez ties peu d'cspeces (CONNER et al.,
1972). La taille du genome de 47 especes de Polychetes a ete mesuree a I’aide d'une analyse microdensitometnquc de la
quantite d’ADN dcs noyaux en repos colores par la reaction de Feulgen. Cette taille a ete correlee avec la longueur moyenne du
corps des annelides adultes do chaque espece. La quantite d'ADN haploide varie de 0.07 a 1,2 pg chez les especes de la
meiofaune et de 0,4 pg a 7.2 pg chez les especes macrobenthiques. Les valeurs les plus petites sont parmi les plus faibles
mesurees chez loutes les especes d’invertebres analysees jusqu'a maintenant. La longueur moyenne du corps des especes
examinees cst comprise entre 0,9 mm et 250 mm, et est significativement correlee avec la taille moyenne du genome (r = 0.30 ;
df = 45; 0.05 < P < 0.01 ), chez les especes etudiees.
INTRODUCTION
Genome size (also known as the C-value) is defined as the mass of DNA in a haploid genome (HlNEGARDNER,
Soldi. R., Ramella, L., GAMBI, M.C., SORDINO. P. & G. Sella. 1994. — Genome size in Polychaetes: relationship with
body length and life habit. In: J.-C. Dauvin. L. LAUBIER & D.J. REISH (Eds), Actes de la 4eme Conference internationale des
Polychetes. Mdm. Mus . natn. Hist, not., 162 : 129-135. Paris ISBN 2-85653-214-4.
Source MNHN. Paris
130
R. SOLDI. L. RAMELLA. M.C. GAMBI. P. SORDINO & G. SELLA
1976). Genome size is known to be positively correlated will) cell volume and size, length of cell cycle, duration
of meiosis and developmental rates (Cavalier-Smith, 1985; McKinney & McNamara, 1991). These
correlations are believed not to be a direct function of genome size but to result trom a balance between selective
forces favoring larger cells, and hence larger genomes, and those favoring rapid cell multiplication (more easily
achieved with small cells and small genome sizes).
Very small organisms, such as those in die interstitial marine fauna, have never been examined to test whedier
Uiese relationships apply. In addition to their small size, interstitial organisms have so many biological and
ecological adaptations to life in a harsh and variable environment, such as die sediment interstices, that they can
be considered very specialized living forms (WESTHEIDE, 1984).
Among lower invertebrates, polychaetes show die highest variety in body sizes and morphology; this reflects
their high diversity of niches and life histories. Their morphological variation is probably due to their plasticity
and early evolutionary radiation (Fauchald, 1984). Among polychaetes, nine families arc exclusively
represented by interstitial taxa (WESTHEIDE, 1985, 1990) and many others have intersdtial representatives (e.g.
Mesionidae, Syllidae, Dorvilleidae). These organisms dius could represent good "biological tools" for studying
relationships between genome size, body size and organizadon. Up to now data on genome size for the Polychaeta
are scarce. Only Conner et al. (1972) measured nuclear DNA amounts for several species of polychaetes by
means of microdensitometric determinations of Feulgcn dye content of somatic nuclei and fluorimetric
quantitation of the DNA of sperm cells. However, among the species considered by Conner et al. (1972). diere
were no interstitial taxa.
This report is a first attempt to test the hypothesis that, in polychaetes, a positive corrclauon between genome
size and Ixxly size may be expected, especially when intersdtial forms are included in the study.
MATERIALS AND METHODS
To die 27 species of polychaetes considered by Conner et al. (1972) we added 20 species. They were chosen
on the basis of their availability. Among the species considered, 13 belong to the meiofauna and 34 to die
macrofauna. Among the interstitial species, three belong to exclusively interstitial families (Saccocirrus
papillocercus, Mesonerilla intermedia, Dinophilus gyrociliatus).
Individuals of 0. labronica and 0. puerilis were collected in 1991 in the harbour of Genoa (Italy) and
individuals of D. gyrociliatus were collected in 1992 in die aquarium of Leghorn (Italy). Specimens of 0. robusta
and 0. macrovifera came from strains set up in 1988 with animals collected in die harbour of Genoa. Specimens
of 0. gracilis came from a strain set up with animals collected at the isle of Sylt (Germany) in 1987, specimens of
0. diadema came from a collection made in 1989 at Long Beach (U.S.A.), specimens of O. hartmanni came from
individuals collected in 1990 in Algeciras (Spain). Individuals of 0. I. pacifica were collected from Woods Hole
aquariums in 1984 and individuals of 0. costlowi from aquariums of Tampa (Florida) in 1986. 0. notoglandulata
individuals came from a 1979 collection in die Sagami Bay (Japan). All these strains of Opliryotrocha were
kindly provided to us by Prof. B. Akesson, Individuals of the odier species were collected in autumn 1990 and
spring 1991 in two coastal biotopes of die island of Ischia (Gulf of Naples, Italy).
The interstitial taxa as well as P. kefersteini and O. flexuosus (see Table 1) were collected in very coarse sands
located at around 8-10 m deptli mid characterized by a typical "Ampltioxus- sand" community (Picard, 1965). The
other macrofaunal species (S. prolifera. P. dttmerilii, A. mediterranea, S. Spallanzani and B. luctuosum ) were
collected in very shallow ( 1 -3 m depdi) hard bottoms covered by photophylic algae, mainly die brown macroalgae
Cystoseira crinita and Halopteris scoparia. To measure genome sizes, cellular suspensions of whole animals
were splashed on cool slides, subsequently air-dried and stained with the Feulgen reaction according to the
procedure of Itikawa & Oglra (1954). Evaluation of die Schiff-positive material was carried out widi a Vickers
M86 microdensitometer at a wavelength of 545 ± 5 inn. For absolute DNA calibration mouse sperm and
lymphocyte preparations were stained together with polychaete preparations. For each species several slide
preparations were obtained with 2 to 20 individuals, according to the availability of live material. At least 50
nuclei per species were measured from different slides (including both spermatozoa and spermatids, when
present) except for O. flexuosus mid M. intermedia where only 20 nuclei could be measured. The absorption
values obtained as arbitrary units were plotted as percent frequency distribution histograms in order to identify the
1C, 2C, 4C classes of DNA. When die DNA values of sperm were not available, the 1C class value was inferred
by halving the 2C class. For die evaluation of absolute DNA amounts, values obtained as arbitrary units were
Source :
GENOME SIZE. BODY LENGTH AND LIFE HABIT IN POLYCHAETES
131
'Fable 1. — Range and mean of body length (mm) and haploid nuclear DNA content (in pg) by microdensito-
metric and fluorimetric determination in 47 species of polychaetes. Fluorimctric data are indicated without
standard error. * = meiofaunal species; a = present paper; b = Conner et ai (1972).
132
R. SOLDI. L. RAMELLA, M.C. GAMBI. P. SORDINO & G. SELLA
Tabi E 1 (continuation) - Range and mean of body length (mm) and haploid nuclear DNA content (in pg) by
SSI nuorimetric determination in 47 species of Seated
without standard error. * = mciofaunal species; a = present paper; b = CONNER el al. ( 1 )72).
0 O. obscurus, reported as Podarke obscura in Conner el al. (1972)
° L. ambigua , reported as Pseudeurythoe ambigua in Conner el al. (1972)
° /\. inagna . reported as Onuphis magna in Conner el al. (1972)
* O. labronica pacifica , not yet formally described, Akesson (1984)
** O. robusta and inacrovifcra , not yet formally described. Akesson (1975)
0 L fragilis, reported as Scoloplos fragilis in Conner el al. (1972)
0 C. grandis, reported as Cirralulus grandis in Conner el al. (1972)
0 A. mucosa . reported as Clymenella mucosa in Conner et al. (1972)
0 R. crisp urn, reported as Branchiomma nigromaculaia in Conner el al. (1972)
Source :
GENOME SIZE, BODY LENGTH AND LIFE HABIT IN POLYCHAETES
133
converted into picograms, taking die mouse genome size as 3.9 picograms (Sparrow et al. , 1972). To calculate
the correlation between genome size and organism size, we considered body length as an estimate of body size.
We arc aware that in polychaetes body length is a simplistic measure of body size, and that not always is this
parameter positively correlated with the actual size of the worm (DUCH&NE, 1982). Besides, body length can
greatly change in different populations of the same species according to geographic location (climatic), local
environment and trophic conditions, and laboratory conditions in the case of laboratory reared populations. High
body length variability in polychaetes notwithstanding, in order to compare our data with those of Conner# al .
(1972), we used the body length variable because it was the only size-parameter available from the literature. An
indicative mean body length for each of the species considered was estimated by comparing and averaging body
length data given by different authors. In Table 1 we reported the range of adult body length values, as well as a
mean value obtained by averaging values obtained from literature. For the species in our study, we integrated the
literature data with the values obtained by measuring at least 10 adult individuals from sampled populations. For
the gonochoric species of the genus Ophryotrocha 10 sexually mature males and mature females were considered.
In D. gyrociliatus only females were measured, in simultaneously hermaphroditic species only sexually mature
individuals and in protandric sequential hermaphroditic species, worms were measured when they reached the
female phase.
This approach allowed us to assess at least the actual "order of magnitude" of body length reached within each
single species.
RESULTS AND DISCUSSION
Genome sizes expressed as pg of DNA per haploid nucleus and mean body lengths of the species examined by
us and by CONNER et al. (1972) arc listed in Table 1, ranking them by orders and families according to PETTIBONE
classification (1982). A total of 47 genome sizes are listed, 10 of which were measured by Conner et al. (1972)
with the fluorimetric method. The species examined belong to 23 families and 12 orders and are therefore
representative of a broad evolutionary range within die class and of a wide spectrum of life habits, mainly
represented by shallow- water species.
Genome sizes varied among species from 0.07 pg to 7.2 pg DNA per nucleus. Such a 100-fold range in
genome size is comparable only to die ranges found in insects and teleosts. All other animal classes are much
more conservative in their genome sizes (JOHN & MlKLOS, 1987). Some of the genome sizes observed in
polychaetes are among the lowest found in invertebrates so far investigated. Only Eutardigrada (REDI &
Garagna, 1987) and some nematodes (John & MlKLOS, 1987) have the same or smaller amounts of DNA.
Genome size appealed to be significantly positively correlated with body length (r = 0.30; df = 45;
0.05 < P < 0.01). However, only 9 % (i.e. r2) of the variation in genome size is explained by its relationship to
body length. In die 13 interstitial species included in the sample (Ophryotrocha spp., S. papillocercus , D.
gyrociliatus, M. intermedia ) no significant correlation was observed between genome size and body length, but by
their small body size and small genome size, diey greatly contributed to the significance of die overall r. If they
were excluded, die correlation was no longer significant.
Different and contrasting patterns arise in comparing from an evolutionary view point die DNA content in
polychaetes. At the generic level, die 10 species of Ophryotrocha showed quite homogeneous values, except O.
hartmanni , as discussed by Sella et al. (1993). Furdiermore, P. kefersteini , that, like Ophryotrocha , belongs to
die Dorvilleidae family, showed a comparable value. On the other hand, die Uiree species of the genus Cirriformia
showed quite different DNA amounts (Table 1). At the family level, die Sabellidae (5 species) demonstrated a
high variability in genome size, while the Onuphidae (3 species) and the Polynoidae (2 species) showed more
homogeneous values. The species belonging to exclusively intersutial families (D. gyrociliatus , M. intermedia and
S. papillocercus) have among die smallest DNA amounts. At the order level, one may note that within die
Eunicida, die macrofaunal taxa (Onuphidae, Lumbrineridae) have higher DNA amount than the interstitial ones
(Dorvilleidae) (Table 1).
Although the sample of interstitial polychaetes is still quite small, diese first results suggest that mciofaunal
taxa have on the whole smaller genome sizes than macrofaunal ones.
We speculate diat the small genome sizes characteristic of mciofaunal species may be partially correlated, not
only with body size (not all the interstitial species have necessarily very small dimensions, e.g. S. papillocercus)
but also widi those biological features deriving from an intersutial life habit, such as progenesis (i.e. retention ot
134
R. SOLDI. L. RAMHLLA. M.C. GAMBL P- SORDINO & G. SELLA
juvenile characters produced by a genetically fixed precocious sexual maturation (Gould. 1977), short life-span,
rapid sexual maturation, rapid cycling of generations, few eggs of large size, and brooding.
These features, which are well documented in Opliryotroclia spp., Dinophilus spp. and in many other
meiofaunal polychaetes (SWEDMARK, 1964; WESTHEIDE, 1984), make up life histories with peculiar mosaics of
V and "K" selected parameters. One may also speculate that small genome sizes can be a prerequisite to
interstitial life.
The above considerations are still quite speculative due to the small amount of data to date available on tins
subject; further analyses on genome sizes in other species of macrofaunal and meiofaunal polychaetes are
necessary to corroborate the hypothesis dial interstitial polychaetes have smaller genomes than macrofaunal
polychaetes. On the whole, the DNA content in polychaetes showed a wide range of values and a large variability.
Such features are common to many other biological properties of this highly diversified group of marine
organisms.
ACKNOWLEDGEMENTS
This research was in part supported by a grant from the Italian M.U.R.S.T. (Progetto Genetica
Evoluzionistica). We thank Hie Centro di Studi per 1'Istochimica of die C.N.R. (Pavia) for kindly allowing us to
use their instruments and Paola Protto for her technical assistance.
REFERENCES
Akesson. B. 1975. — Reproduction in the genus Opliryotroclia (Polychaeta, Dorvilleidae). Pubbl. Staz. zool. Napoli. 39
Suppl. : 377-398.
AkessON. B.. 1984. — Speciation in the genus Opliryotroclia (Polychaeta, Dorvilleidae). In: A. FISCHER & H.D.
Pfannenstiel (eds), Polychaete Reproduction. Fortschr. Zool. : 299-316.
Cavalier-Smtih. T.. 1985. — The Evolution of Genome Size. John Wiley & Sons. Chichester. NewYork. Brisbane. Toronto.
Singapore, 523 pp.
CONNER. W. G., HlNEGARDNER, R. & Bachmann. K., 1972. - Nuclear DNA amounts in Polychaete Annelids. Experientia ,
28 : 1502-1504.
DUCHfcNE, J.C.. 1982. Problemes lies a la croissance chez les Annelidcs Polychetes. Ocean is, 3 : 493-504.
FauchalD, K., 1984. — Polychaete distribution pattern, or: can animals with Palaeozoic cousins show large-scale
geographical patterns ? In: P.A. HUTCHINGS (ed.), Proc. First International Polychaete Conference, Linnean Society of
New South Wales: 1-6.
Gould. S.J.. 1977. — Ontogeny and Phytogeny. Belknap Press of Harvard University Press, Cambridge Massachusetts and
London U.K.. 501 pp.
HlNEGARDNER, R., 1976. — Evolution of genome size. In: Ayala (ed.). Molecular Evolution. Sinauer Assoc. Inc. Sunderland.
Massachusetts : 179-199.
Itikawa, O. & Ogura. Y., 1954. — The Feulgcn reaction after hydrolysis at room temperature. Stain Technology. 29: 13-15.
JOHN, B.& Miklos. G.L.G.. 1987. The Eukaryote Genome in Development and Evolution. Allen and Unwin, London. 291
pp.
McKinney, M.L. & McNamara, K.J.. 1991. Heterochrony. The Evolution of Ontogeny. Plenum Press, New York and
London. 437 pp.
PETTIBONE, M.. 1982. — Annelida. In: S.P. PARKER (ed.). Synopsis and Classification of Living Organisms. McGraw Hill,
London : 43 pp.
Picard, J.. 1965. Recherches qualitatives sur les biocenoses marines des substrats meubles dragables de la region
marseillaise. These. Fac. Sc. Nat. University d’Aix-Marseille, 160 pp.
REDI. C.A. & GaraGNA, S., 1987. Cytochemica! evaluation of the nuclear DNA content as a tool for taxonomical studies in
Lutardigrades. In: R. BERTOLANI (ed.). Biology of Tardigrades. Selected Symposia and Monographs U.Z.I. Mucchi,
Modena, 1 : 73-80.
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GENOME SIZE. BODY LENGTH AND LITE HABIT IN POLYCHAETES
135
SELLA. G.. Redi. C.A.. RAMELLA. L.. Soldi. R.. Premoll M.C. — 1993. Genome size and karyotype length in some
interstitial polychaete species of the genus Ophryotrocha ( Dorvilleidae). Genome, 36 : 652-657.
Sparrow, ATI., Price, II.J. & UNDERBRINK, A.G.. 1972. — A survey of DNA content per cell and per chromosome of
prokaryotic and eukaryotic organisms: some evolutionary considerations. In: J. Smith (ed.). Evolution of genetic systems,
Brookhaven Symposia in Biology., 23. Gordon and Breach. New York: 451-494.
SWEDMARK, B.. 1964. — The interstitial fauna of marine sand. Biol. Rev., 39 : 1-42.
WESTHEIDE, W., 1984. — The concept of reproduction in Polychaetes with small body size: adaptations in interstitial species.
In: A. FISCHER & H. D. PFANNENSTIEL (eds), Polychaete reproduction. Fortschr. Zool. , 29 : 265-287.
WESTHEIDE, W.. 1985. — The systematic position of the Dinophiliidae and the Archiannelid problem. In: S. Conway
MORRIS, D. George. R. Gibson & H.M. Platt (eds), The origin and relationships of lower invertebrates. Oxford
University Press. Oxford : 310-326.
WESTHEIDE, W., 1990. — Polychaetes: interstitial families. Synop. Brit. Fauna, 44 : 1-153..
Source : MNHN. Paris
15
Fine morphology of the feeding apparatus of
Cossura sp. (Polychaeta, Cossuridae)
from the White Sea
Alexander B. TZETLIN
Dept, of Invertebrate Zoology
Moscow State University
Moscow, Russia
ABSTRACT
Morphology of the feeding structures and construction of the anterior part of the body cavity of Cossura sp. from the
While Sea were studied using TEM and SEM techniques. Buccal tentacles are the only feeding structures in the spacious
buccal cavity. They are situated on the dorsal surface of the buccal cavity near the esophageal opening. There are about 15
buccal tentacles covered by long cilia inside the proboscideal cavity. In cross sections every tentacle consists of
columnar epithelial ciliated cells and in the central part, inside a ring of basal membrane, there arc two longitudinal
muscle cells and two cells without contractile filaments. The space between body wall and tissues of digestive tract is
occupied by the non-contractile cytoplasmic parts of longitudinal muscle cells of the body wall. Buccal tentacles cannot
be protracted by hydrostaic pressure of the body cavity, as there is no free coelom ic space either in the anterior part of the
body or inside the tentacles. Also Cossura sp. has not circular muscles in the body wall which are usually necessary for
hydrostatic skeleton. It seems that natural position for the buccal tentacles during feeding processes is partly projected
from the very widely open mouth. According to our observations on living specimens, the long unpaired dorsal branchial
filament never takes part in feeding, it is always stretched along the trunk, and has presumably a respiratory function.
RESUME
Morphologie fine de I'appareil alimentaire de Cossura sp. (Polychete, Cossuridae) de la mer
B 1 a n c h e
La morphologic des structures trophiques ct la constitution de la parlie anterieure cavitairc du corps de Cossura sp. de
la mer Blanche ont etc (Studiees en utilisant les techniques de miscroscopie electronique a transmission et de microscopie
electronique a balayage. Les tentacules buccaux sont les seules structures servant a l'alimentation, presentes dans la vaste
cavite buccale. II y a environ 15 tentacules couverts de longs cils a l'interieur de la cavite proboscideale. En coupe, chaque
tentacule esl constitue par des cellules epitheliales cilices en forme de colonnes et dans la partie centrale. a l'interieur d’un
anneau de la membrane basale, il y a deux cellules musculaires longitudinales et deux cellules sans filaments contractiles.
L'espace entre la paroi du corps et les tissus du tractus digestif est occupe par les parties cytoplasmiques non contractiles
des cellules musculaires longitudinales de la paroi du corps. Les tentacules buccaux ne peuvent etre developpes par la
pression hydrostatique de la cavite corporelle, tout comme il n'y a pas d'espace coelomiquc libre ni dans la partie
Tzetlin, A.B., 1994. - Fine morphology of the feeding apparatus of Cossura sp. (Polychaeta, Cossuridae) from the
White Sea. In: J.-C. Dauvin. L. LaUBIER & D.J. REISH (Eds), Actes de la 4eme Conference internationale des Polychetes.
Mem. Mus. natn. Hist, nat ., 162: 137-143. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
138
A. R. TZBTLIN
anicrieurc du corps ni clans les lentacules. De meme. Cossura sp. n'a pas dc muscles circulaires dans la paroi du corps,
lesquels sont habituellemenl necessaires pour le squelettc hydrostatique. En position naturelle durant les phases
d'alimentation. les tentacules buccaux semblent Stic partiellement projetiSs hors de la bouche ties largement ouverte.
Suivant nos observations sur des animaux vivants. le long filament branchial dorsal ne joue aucun role dans
l'alimentation. II est toujours accole le long du tronc et a. probablement. unc fonction respiratoire.
INTRODUCTION
The Cossuridae is one of die most poorly studied polychaete families. We have very nearly no information
even about die general anatomy of Uiese worms. In addition there is almost no information about life style and
feeding in diese°animals (Fauchald & Jumars, 1979; Fournier & Petersen, 1991). Thulin (1921) and later
Fournier & Petersen (1991) described die ciliated "buccal tentacles" of die pharyngeal cavity of Cossura as die
feeding apparatus of these polychaetes. Up to this time die construction, position in the pharyngeal cavity and
functioning of die cossurid mouth parts have remained unknown.
This paper deals widi die fine morphology of the feeding structures and die construction of die anterior part of
die body cavity of Cossura sp. from die White Sea.
MATERIALS AND METHODS
All material (about 100 specimens) was collected within 20 km of Velikaya Salma Straight (Kandalaksha Bay,
the White Sea. 66° 30'N, 33° 30'E), in die depdis varying from 20 to 30 m by means of SCUBA.
The While Sea Cossura sp. inhabits die upper layer (1-2 cm) of muddy sediment in depdis of more dian 20 m.
Previously, this species was identified as Cossura longocirrata Webster & Benedict (Tzetlin,1981), but according
to Petersen (personal communication) die White Sea animals must be referred to anodier, possibly new species.
Live worms were examined in the Laboratory of die White Sea Biological Station of Moscow University. Hie
observations on die Cossura sp. were made in a small aquarium widi a 3 cm sediment layer transferred Irom the
depth of 25 m.
Animals were fixed widi 2,5 % glutaraldehyde, buffered with 0,2 M Na-cacodylate buffer (pH = 7,2-7.4) with
the addition of 0,131 g sucrose per 1 ml of solution (1 hour) and postfixed with 1 % osmiumtelroxide solution in
the same buffer. For SEM observations specimens were critical-point dried after dehydration in an elhanol series
and widi acetone and dien after coating widi gold. They were studied widi a Hitachi S 405 microscope. For TEM
fixed specimens were dehydrated in an ethanol series, treated widi acetone and embedded in Epon. Semidiin sections
were made with glass knifes on a Dupont Ultracut microtome and stained in 1 % toluidine blue. Ultradiin sections
for TEM observations were cut on a LKB-3 Ultracut microtome widi diamond knife, stained in lead citrate and
uranylacetate and then examined with a JEM-lOOb microscope. More dian 50 specimens were studied by light
microscopy in living condition, 25 specimens were observed with SEM. Fifteen of diem were cut in the sagittal
plane by microsurgery knife and the dissected worms examined widi SEM. Four specimens (two sagittal and two
transverse series) were examined with TEM techniques.
RESULTS
Construction of the feeding apparatus. — Cossura sp. are slender polychaetes of 20-30 mm length, with
50-60 setigers. The T-shaped moudi opening is located in die fissure between two secondary "segments" of the
peristomium. The only external appendage on the anterior part of die body is die dorsal branchial filament, which
originates from die border between the second and third setigers. The branchial filament bears a longitudinal row of
cilia. The inner part of die branchial filament contains longitudinal muscle cells, and two blood vessels. There is
also a narrow coelomic space.
The spacious buccal cavity stretches from the anterior border of peristomium to the border between setigers 2
and 3. In the last area is also die junction between foregut and intestine. The exdemely short esophagus is
represented by short funnel widi relatively narrow lumen between stoinodeum and intestine (Fig. 1 A).
Slomodeal epithelium consists of squamous (1,6 pm) cells rarely covered by short microvilli (Fig. 1B-C; Fig.
3. C-D). A collagenous matrix on die surface of the slomodeal epidielium is poorly developed. There are electron
dense secretory spherulae (D =0,5-0,4 pm) in the epidielial cells. The epidielium is underlain by a thin basal
MORPHOLOGY OF FEEDING APPARATUS OF COSSURA SP.
139
lamina (0,4 |im) and peritoneal cells. The wall of buccal cavity lacks muscle cells (Fig. 1, B-C; Fig. 3, C-D).
Epithelial cells in the back region of the stomodeum are covered with cilia (Fig. 1, A, B). These cells are similar
to epithelial cells of the esophageal region and anterior part of intestine.
A b
FIG. 1. — Cossura sp. A. : scheme of sagittal section. Arrows B, C show position of transverse sections. B, C -
transverse sections through the region of the foregut (hemischeme, after TEM -reconstructions). Scale: A - 0.5 mm, B, C
- 0,1 mm. be: buccal cavity, bf: branchial filament, bbf: blood vessel of the branchial filament, bte: buccal tentacle, bz:
basal zone of the buccal tentacle, c: cilia, ch: chaeta. elm: cytoplasmic expansion of the longitudinal muscle cell, coc:
coelomic cavity, dbv: dorsal blood vessel, ep: epitermal epithelium, in: intestine. 1m: longitudinal muscle cell, mo:
mouth opening n: nucleus, nf: nerve filament, nlm: nucleus of- the longitudinal muscle cell, oe: oesophagus, omc: oblique
muscle cell, pco: parapodial complex, r: rootlets, step: stomodeal epithelium, sg: secretory granulae. tep: tentacular
epithelium, vbv: ventral blood vessel, vne: ventral nerve cord.
140
A. B. TZETLIN
Buccal tentacles, the only feeding structures, are located in the spacious buccal cavity. 1 hey are attached to the
dorsal surface of the buccal cavity near the opening into esophagus. There are about 15 buccal tentacles covered
with long cilia occupying almost all space inside the buccal cavity (Fig. I, A. B, C). The length of the buccal
tentacles is 0,6 - 0,7 mm and the widdi about 0,05 mm. The ventral and lateral surfaces of tentacles tire more
densely ciliated than the dorsal surface.
The ciliated epithelium of die buccal tentacles consists of high (20 pm) cells (Fig. 2). Basal bodies and
rootlets (with a length of about 18-20 pm) are well developed especially in the epithelial cells placed laterally on
the tentacles (Fig. 3. B). Ciliated cells have two types of secretory vesicles: electron dense spherulae (D= 0.5-
0,4 pm), the same as in the epithelial cell of the buccal wall. The other type of vesicles (D= 0,8 pm) is lull of
gray, non-structured serous-like matter. The epithelial cells have large nuclei (D= 5 pm).
r
c
Fig. 2. — Cossura sp.: Cross-section of the buccal tentacle (slightly schematic, after TEM-reconstruction). Scale:
0,025mm. For abbreviations, see Figure 1.
The epithelium of the buccal tentacles is underlain by basal lamina (0,16 pm) which rings die central zone.
There arc two groups of nerve fibres located laterally along die both sides ol die basal lamina cylinder.
Transverse sections show two longitudinal muscle cells and two supporting (or coelenchyme-like) cell widi
almost empty cytoplasm, within die ring of basal lamina. It is possible, that die last structures are only
cytoplasmic parts of die muscle cells. The coelomic cavity does not extend into die central cylinder of the tentacles
(Fig. 3, A).
Construction of body wall and coelomic lining of the anterior end of the trunk. — I here are
only longitudinal muscle cells in dirce bundles (two ventro-lateral and one unpaired dorsal longitudinal bundle)
under die ectodermal epidielium mid basal lamina. Circular muscles are very poorly developed and could be seen
only in die areas of inter-segmental fissures. Oblique muscles are located in die region of die parapodial
complexes. All longitudinal muscle cells have a spacious non-contractile cytoplasmic expansion in which the
nucleus is found. These cytoplasmic extension occupy all die space of the body cavity in the anterior setigers and
fit closely to die peritoneal cells which surrounds the foregut (Fig. 3, C). The little space free of cell bodies is
Source :
MORPHOLOGY OF FEEDING APPARATUS OF COSSURA SP.
141
only in the dorsal region of the third setiger. It is directly connected to the coelomic cavity of the branchial
filament.
FIG. 3. Cossura sp.: A. Central part of buccal tentacle in transverse section (TEM); B, ciliated epithelial cell of the
buccal tentacle (TEM); C, part of a transverse section through anterior part of the body (TEM); D. part of the
epithelium of the middle part of the buccal cavity (TEM). Scale: A. 0.003 mm, B, C, 0.014 mm. D. 0.0045 mm.
For abbreviations, see Figure 1.
Living observation. — The worms do not build massive tubes, but continuously produce mucus which is
always covered with sediment particles. The long dorsal branchial filament never takes part in feeding, being
always stretched along the trunk inside the mucous tube presumably having only a respiratory function. After
extraction from the sediment the worms usually break up into fragments and die rapidly.
142
A. B. IZETLIN
Buccal tentacles are normally located inside the buccal cavity. Only few worms with buccal tentacles extended
from die mouth were observed. The tentacles were motionless and non-contractile. All these animals were in bad
condition and convulsively contracted the anterior end. These worms were unable to retract their buccal tentacles.
FIG 4. Co ssura sp.: Hypothetical
position of Co ssura sp. during feeding processes. For abbreviations, see Figure 1.
DISCUSSION
The central cylinder of die buccal tentacles of Cossura consists of longitudinal muscle elements and supporting
(coelcnchyme-like) elements. A small coelomic space free from the cell bodies in die dorsal region of die third
setiger was found (between die branchial filament and the base of die buccal tentacles), but no coelomic space is
present in the buccal tentacles. It is theoretically possible dial powerful contractions of the longitudinal body
muscles, coupled widi a contraction of the branchial filament could cause die extrusion of die buccal apparatus. In
a great number of polychaetes, extrusion of tentacular or palpal structures when hydrostatic pressure is used, is
strongly correlated with the presence of special compartments of die coelom with muscular walls (ampullae of
Spionida, Protodrilidae and Saccocirridae and diaphragms in die Terebcllida).
Thus, it is unlikely that contraction of the longitudinal body muscles, coupled with a contraction of die
branchial filament may be die normal mechanism of tentacle elongation. It is more probable dial die supporting
elements of the central cylinder of die buccal tentacles form a kind of chord, supporting the constant shape mid
volume of the tentacle. Construction of the central cylinder of Cossura is similar to die construction of the palpal
canal of Protodriloides chaetifer (Purschke, 1993). In both cases there are longitudinal muscle elements (without
circular elements) and supporting (coelenchyme-like) elements. P. chaetifer and P. symbioticus differ from odier
Protodrilida (Protodrilidae and Saccocirridae) by die absence of ampullae and circular muscle in die wall of the
palpal canal. Although the diameter of the buccal tentacles of die Cossura is twice as large as diat of die palp of
Protodriloides, die number of longitudinal muscle cells in the central cylinder (two in a cross-section) is rather less
than in the palpal canal of Protodriloides (seven-eight, PURSCHKE, 1993). Considering dieir structure, the buccal
tentacles of Cossura must be little movable. So, die tentacles of Cossura are not able to move actively along die
surface of the substratum and the enormous elongations so typical for tentacles of the Terebellida (SUTTON, 1957).
Living observation (unfortunately very limited) also support diis conclusion. Protraction of die whole buccal
cavity as a component of normal feeding behavior (as suggested by Thulin. 1921 and Fournier & Petersen,
1991) is hardly probable since we did sec observe any system of retractors connected to the tentacles or the foregut.
The only possible hypothesis seems to be diat the buccal tentacles will be exposed to the substratum when the
mouth is opened very wide (Fig. 4). In this case tentacles may be pressed down onto the sediment. The high
density of cilia on die lateral and ventral surfaces of buccal tentacles supports this assumption. However, the
mechanism of contact of the feeding apparatus of Cossura widi sediment is not absolutely clear.
From a functional point of view the cossurid tentacular apparatus appears similar to the ciliated pharynx of
adult Orbiniidae (Fauchaed & JUMars, 1979). In morphological terms, die buccal tentacles of die Cossuridae
differ considerably from the tentacular apparatus of die Terebellida bodi in position and way of action. In the
ferebellidae and Alvinellidae tentacles are located on die outer surface of die upper lip, in die Pecunariidae on die
MORPI IOLOGY OF FEEDING APPARATUS OF COSSURA SP.
143
level of mouth opening, and in Ampharetidae liie tentacles are on the inner surface of the upper lip of the mouth
(Fauvel, 1897; Dales, 1962, DesbruyEres & Laubier, 1986). In contrast, the tentacles of die cossurids are
situated on the dorsal surface of buccal cavity near the esophageal opening. The hydrostatic mechanism of tentacle
elongation is associated with a special organ in the body cavity of Terbellida, in die form of a muscular diaphragm
widi paired reservoirs (Dales, 1962; Sutton, 1957). Such devices are absent in Cossuridae. The ciliated tentacles
of Cossuridae may be derived from ciliated structures on die dorso-Iatcral surfaces of buccal cavity common in a
number of different polychaete families (PURSCHKE, 1984, 1985, 1987; TZETLIN, 1991).
AC KN O W LEDGMHNTS
I am grateful to kindness of Mr. Michail Saponov and Drs. Oleg MALUTIN, Igor Kosevitch and Alexey
Elfimov for assistance in sampling. I am also grateful to Dr. Mary PETERSEN and Mrs. Marina Saphronova for
fruitful discussions and Drs Kristian Fauchald and Don Reish for reviewing die manuscript.
REFERENCES
Dales. R.P.. 1962. — The polychaete stomodeum and the interrelation of the families of Polychaeta. Proc. Zool. Soc.
London . 139 : 389-428.
DESBRUYfcRES, D., & Laubier. 1... 1986. Les Alvinellidae, une famille nouvelle d’annelidcs polychetes infeodees aux
sources hydrothermalcs sous-marines: systematique. biologic et ccologie. Can. Journ. Zool.. 64 : 2227-2245.
FAUCHALD, K.. & Jumars, P.A.. 1979. — The diet of worms: a study of polychaete feeding guilds. Oceanogr. mar. Biol.
Ann. Rev., 17 : 193-284.
Fauvel, P.. 1897. Rceherches sur les Ampharetiens. Lille, Imp. L. Danel. 230pp.
FOURNIER. J.A.. & PETERSEN. M.E.. 1991. — Cossura longocirrata : redescription and distribution with notes on
reproductive biology and a comparison of described species of Cossura (Polychaeta. Cossuridae). Ophelia. Suppl. 5 :
63 -80.
HOLTHE T.. 1986. — Evolution, systematics and distribution of the Polychaeta Terebellomorpha, with a catalogue of the
Taxa and a Bibliography. Gunneria. 55 : 1-236.
PURSCHKE, G., 1984. — Vergleichende analomische und ultastrukturelle Unlersuchungen vcntraler Pharynx Apparaie bei
Polychaelen und ihre phylogenetische Bedeutung. Ph. D. Diss., GotUngen, 372pp.
PURSCHKE., G.. 1985. Anatomy and ultrastructure of ventral pharyngeal organs and their phylogenetic importance in
Polychaeta (Annelida). 2. The pharynx of Nerillidae. Mikrofauna Mar.. 2 : 23-60.
PURSCHKE., G.. 1987. Anatomy and ulUastructure of ventral pharyngeal organs and their phylogenetic importance in
Polychaeta (Annelida). 4. The pharynx and jaws of the Dorvillcidae. Aela Zool.. Stokh.. 68 : 85-105.
PURSCHKE., G.. 1993. — Structure of the prostomial appendages and the central nervous system in the Prolodrilida
(Polychaeta). Zoomorphology. 1 13 : 1-20.
SUTTON, M.F.. 1957. — The feeding mechanism, functional morphology and histology of the alimentary canal of
Terebella lapidaria L. Polychaeta). Proc. Zool. Soc. Ixrnd., 129 : 487-523.
TTlULIN, G.. 1921. — Biologisch-faunistische Untersuchungen aus dem Vresund. VI. Uber Cossura longocirraia Webster &
Benedict und uber die Rohren von Disoma multiselosum Oersted. Lunds Univ. Ersskr. N.F.. Avd. 2, Bd.17. 10: 2-15.
TZETLIN, A.B., 1981. — Fauna and distribution of the polychaetes of the White Sea. Ph. D. diss., Moscow, 1- 355 (in
Russian).
TZETLIN, A.B.. 1991. — Evolution of the feeding apparatus in the order Capitellida (Annelida. Polychaeta). Zool. Zhurn..
70 : 10-22 (in Russian).
Source : MNHN. Paris
16
Polychaetes of the Family Acoetidae (= Polyodontidae)
from the Levant and the Central Mediterranean with
a description of a new species of Eupanthalis
M.Nechama BEN-EUAHU* & Dieter FIEGE **
’ The Life Sciences Collections, The Department of Evolution, Systcmatics and Ecology
The Alexander Silberman Institute of Life Sciences
The Hebrew University of Jerusalem, 91904 Jerusalem
**Forschungsinstitut und Naturmuseum Scnckenberg
Senckenberganlage 25. D-60325 Frankfurt am Main, Germany
ABSTRACT
Five species of Acoetidae are present along the Mediterranean coast of Israel: Eupolyodontes cornishii Buchanan. 1894. a
new record for the Mediterranean and. probably, only the second finding of this species since its description from the mouth of
the Congo River (Africa); Euarche tubifex Hhlers, 1887, also found off Sicily; Polyodontes maxillosus (Ranzani. 1817).
comparatively rare; Panthalis oerstedi Kinberg. 1856 found in deeper waters off the Mediterranean coast of Israel than
previously recorded; and Eupanthalis glabra . n.sp.. from Israel and Cyprus. The new Eupanthalis species can be distinguished
from another Mediterranean species, E. kinbergi McIntosh. 1876. by its smooth rather than papillate palps. The relationship of
body size and depth, and differences in body size between Levant and central Mediterranean populations arc discussed.
RESUME
Polychetes de la famille des Acoetidae dc la Mediterranee levantine et centrale avec la description d'une nouvellc
espece du genre Eupanthalis
Cinq especes de la famille des Acoetidae sont presentes le long des cotes mediterranccnnes israeliennes : Eupolyodontes
cornishii Buchanan. 1894 nouvellc pour la Mediterranee et, probablcment, retrouvee pour la deuxieme fois depuis sa
description originate dans 1’estuaire du Congo (Afrique); Euarche tubifex Ehlers. 1887 egalement trouvee en Sicile;
Polyodontes maxillosus (Ranzani. 1817), comparalivement rare; Panthalis oerstedi Kinberg. 1856 trouvee plus profondement
que lors des recoltes precedenles; et Eupanthalis glabra . n. sp.. trouve en Israel et a Chypre. Cette nouvelle espdee
d' Eupanthalis se distingue de l’aulre espece meditenaneenne. E. kinbergi McIntosh. 1876, par ses palpes lisses depourvus de
papilles. Des relations entre les dimensions du corps et la profondeur de recolle ainsi que les differences de taillc entre les
populations lcvantines et celles de Mediterranee centrale sont discutecs.
BEN Eliahu, M.N. & D. Fiege, 1994. - Polychaetes of the Family Acoetidae (= Polyodontidae) from the Levant and the
Central Mediterranean with a description of a new species of Eupanthalis. In: J.-C. Dauvin, L. Laubier & D.J. Reish (Eds).
Actcs de la 4emc Conference internationale des Polychetes. Mem. Mus. natn. Hist, nat .. 162: 145-161. Paris ISBN 2-85653-
214-4.
Source : MNHN. Paris
146
M.N. BEN ELIAHU & D. FIEGE
INTRODUCTION
The present paper reports on aphroditoid polychaetes of the family Acoetidac Kinberg, collected between
1968 and 1991 in die Levant Basin off the Mediterranean coasts of Israel and Sinai, and off Cyprus, and in the
central Mediterranean off Sicily. Acoetid scaleworms are among the largest polychaete species. They are
characterized by parapodial organs (spinning glands) which produce fibers to build permanent felt-like tubes
packed with clay (Fig. 7a). Acoetids are carnivorous and have powerful jaws (Figs 2d,e: 6b; 9b). Some species are
rarely recorded. Some penetrate to batliyal depths.
A single worm, belonging to the giant species, Eupolyodontes cornishii, was collected off Ashqelon in 55 m by
E. CilLAT and G. Sachnin in 1969. The identification to species was made by comparison with the hololype. The
recent revision of die family Acoetidae by PETTIBONE (1989) enables an appreciauon of die rarity and importance
of this find (Ben-Eliahu & Fiege, 1991); it appears to be the second record since the holotype was described by
Buchanan (1894) from die moudi of die Congo River. Recendy, J. Nunez has found E. cf. cornishii off Tenerife
(NUNEZ, pers. comm.).
Petti BONE's revision (1989) led to recognition of a second, undescribed, Mediterranean species of Eupanthalis
along die coastal shelves of Israel and Cyprus, and it is described below as Eupanthalis glabra , sp. nov.
A gradiud accumulation of acoetid material has come from increasingly deeper sampling off die Mediterranean
coast of Israel, carried out by different projects and institutions: die joint project "Biota of the eastern
Mediterranean and Red Sea" of the Hebrew University of Jerusalem and Smidisonian Institution (H. STEINITZ,
F. D. Por and W. Aron [discussed in Por et ai, 1972]); die Sea Fisheries Research Station, Haifa (E. Gilat); Tel
Aviv University (Ch. Lewinsohn, M. Tom and B. Gaul); die 'Meteor' V expedidon (M. Turkay) obtained some
particularly rich samples of Acoetidae (for stations, see WE1KERT, 1988). Subsequent deep sampling cruises of
polludon monitoring off the northern Israeli coast carried out by S. PlSANTY and D. Golani (Israel Department of
Fisheries and Hebrew University of Jerusalem, respectively); and B. Galil (The Israel Oceanographic and
Limnological Research, Ltd.), have occasionally brought up Panthalis oerstedi (Ben-Eliaiiu, 1990; Ben-Eliahu
et ai, 1991). The combined data provide dcpdi distribution profiles of diese species along die Mediterranean coast
of Israel.
Recently, die 'Poseidon' 172—4 expedition of die Geologisch-Palaontologisches Institut und Museum, Univ.
Kiel to presumed hydrodiermically acuve sites off Sicily (PUTEANUS, 1990), collected Euarche tubifex.
MATERIALS AND METHODS
The samples: samples are listed in Table 1; for Levant sites, see fig. 1 and for Sicilian sites see PUTEANUS,
1990. Abbreviations in die sample codes are as follows: (I) Israel or Cyprus. (TAU) Tel Aviv University; (SFR)
Sea Fisheries Research Station, Haifa; (SLMB) sample of "Biota of die Red Sea and eastern Mediterranean" (POR
et ai, 1972); (SMF) Senckenberg-Museum, Frankfurt; (GPK) Geologisch-Palaontologisches Institut und
Museum, Univ. Kiel; (IOLR) Israel Oceanographic and Limnological Research, Co., Ltd.
Repository of specimens is as follow: I-coded material is at die Hebrew University of Jerusalem (ITUJ); S-
coded material is at die Senckenberg Museum, Frankfurt (SMF). Also, (AMS) Australian Museum, Sydney;
(BMNH) Natural History Museum, London; (MNHNP) Museum National d'Histoire Naturelle, Paris; and
(USNM) National Museum of Natural History, Washington.
Measurement of preserved specimens: for population lengdi comparisons, we used 11+10 (die prostomium and
tentacular segment plus following 10 sedgerous segments), which enabled using fragmented as well as complete
specimens as suggested by K. Fauchald (pers. comm.).
The following data were recorded: (1) Condition of specimen: complete/ anterior fragment/ middle fragment/
posterior fragment; (2) length in mm per number of segments (seg.); (3) length of 11+10 in mm; (4) width in mm
to edge of parapodia without setae, measured at widest part of body; (5) proboscis length (only if extended)
measured from base of prostomium and (6) t, number of teedi on each of the 4 jaws. In addition, for Eupanthalis
glabra , n. sp., relative lengdi of head appendages, as follows: tentacular cirri/ lateral antenna, tentacular cirri/
palps, lateral antenna/ prostomium, palps/ height of prostomium, tentacular cirri/ height of prostomium, length of
proboscis/ height of prostomium; nuchal fold present, absent or not visible due to position of head when
preserved.
Source :
ACOET1DAE FROM THE MEDITERRANEAN WITH DESCRIPTION OF A NEW SPECIES
147
Table I . — Samples collected off Mediterranean coast of Israel, Cyprus and Sicily
1I-IOLR. Haifa, 33°0TN, 34°34.2'E, L3: 1356 m. beam trawl L3; 5. XI. 1990; very rich in rocks and porous
metal either volcanic or industrial slag broken up; coll. S. Pisanty & D. Golani.
2I-IOLR. Haifa, LI- 33°02’01"N, 34° 29 E; 1,470 m, LI; 16.XI1.1992; coll. B. Galil.
3I-IOLR. Atlit; 200 m, beam trawl; 30.1.1990: coll. B. Galil.
41-lOLR. Atlit; 500 m, beam trawl; 31.1.1990; coll. B. Galil.
5I-IOLR. Atlit; 1,000 m, beam trawl; 31.1.1990, coll. B. Galil.
6I-SFR1610. Tantura, Gilat st. 17; 1 10m, dredge A; 3.IV.1968; coll. E. Gilat.
7I-SLMB1 13. Off Alexander River; 123 m, beam trawl; 26.IX.68, coll. G. Sachnin & M. Rapaport
8S-SMF. Jaffa, 32°02.38'N, 34°35.05'E - 32°00.95'N, 34°34.52'E, 'Meteor' V St. 50; 95-103 m, beam
trawl; 26.1.1987; coll. M. Tiirkay.
9S-SMF. Jaffa, 32°00.53'N, 34°33.98'E,'Mcteor' V St. 50; 1 10 m, grab; 26.1.1987; coll. M. Tiirkay.
10S-SMF. Jaffa. 32°01'N. 34°31.4'E — 31°58.9'N, 34°27.3'E, "Meteor" V St. 51; 309 m, beam trawl-
26.1.1987; coll. M. Tiirkay.
1 1S-SMF. Jaffa, 32°19.96'N, 34°31.46'E - 32°19.75'N, 34°31.26’E, 'Meteor' V St. 56; 694-700 m beam
trawl; 27-28.1. 1987; coll. M. Tiirkay.
12I-TAIJ. Palmachim; 35 m; 24-26.XI.1977; coll. B. Galil.
131-TAlJ. Palmachim; 35 m; 5-6.XI.1987; coll. B. Galil.
I4I-SLMB 156. Nabi Yunis (Aslidod); 128 m, beam trawl; 20.XI1.1968; coll. C>. Sachnin & M. Rapaport.
151-SLMB 157. Nabi Yunis (Aslidod); 128 m, dredge B; 20.XII.1968; coll. G. Sachnin & M. Rapaport.
16I-TAU. Nitsanim; 35 m; 28.11.1987; coll. B. Galil.
17I-TAU. Nitsanim; 80 in; 2.1V. 1977; coll. B. Galil.
181-TAD. Nitsanim; 80 m; l.VII. 1977: coll. B. Galil.
I9I-SFR1718. Ashqelon; 201 m, beam trawl; 30.X.1968; coll. G. Sachnin.
20I-SFR. 1742- Ashqelon; 55 m, knife dredge; 7. IV. 1969; G. Sachnin.
21I-SLMB6046. Sinai, Gaza; 36.6 m, beam trawl; 7. 1.70: coll. G. Sachnin.
22I-SLMB6021. el Arish; 137 m, dredge B; 27.VI11.1969, coll. G. Sachnin.
23I-SLMB6023. el Arish; 183 m, dredge B; 24.IX.1969, coll. G. Sachnin.
24I-SLMB6024. el Arish; 183 m, beam trawl, 27.VI1I.1969, coll. C>. Sachnin.
25I-SLMB 178. Sinai, Kalib el Galss (Bardawil); 91.5 m, beam trawl; 4.11,1968, coll. E. Gilat.
261 -SLMB 1545. Cyprus, Famagusta F; 100-110 m, dredge A; 16.11.1968. coll. A. Lurie.
27S-GPK. Graham Bank. 37°09.135'-37°08.90'N, 12o42.90'-12°43.23'E, "Poseidon" 172-4: 185-178 m.
Chain dredge; 2.V. 1990; coll. M. Tiirkay; #645.
28S-GPK. Cimotoe, 37°00.43'-37°00.45'N. 1 2°39.06’- 12°39. 1 l'E, "Poseidon" 172-4; 198-158 m, chain
dredge; 7.V. 1990; coll. M. Tiirkay, #718.
29S-GPK. Cimotoe, 37°00.20’-36°059.82’N, 12°39.08'-12°38.58'E, "Poseidon" 172-4; 224-230 m, chain
dredge; 2.V. 1990; coll. M. Tiirkay, #629.
30S-GPK. Cimotoe, 36°59.82'-36°058.37'N. 12°39.28'-12°39.90'E, "Poseidon" 172-4; 237- 220 m, chain
dredge; 2. V. 1990, M. Tiirkay; #630.
31S-GPK. Cimotoe. 36°059.38'N, 12038.74-E, "Poseidon" 172-4; 214-230 m, Van Veen grab; 1.V.1990;
__co]L M, Tiirkay; #620, _
Statistics were computed by the S AS statistical package. Description of new species gives: holotype parameter
(population mean ± s.d. [range], for N, number of individuals). To conform with Pettibone (1989), the text refers
to segments rather than setigers; in Aphroditoidea the first parapodium bearing setae is the 2nd segment.
Scanning Electron Microscopy (SEM): samples were dehydrated via graded ethanol series, critical-point dried
using C02 and examined in a CAMSCAN-SEM (CS 24).
Source :
148
M.N. BEN ELI AH U & D. FI HOE
FIG. 1 . Sampling sites off Israel (Haifa to Ashqelon) and northern Sinai (Gaza - Bardawil). Black star
white star, Eupolyodontes comishii.
33°
32°
31°
, Eupant kalis glabra ;
Source : MNHN, Paris
ACOETIDAE FROM THE MEDITERRANEAN WI TH DESCRIPTION OF A NEW SPECIES
149
SYSTEMATIC SECTION
Genus Eupanthalis McIntosh, 1876
PErriBONE, 1989: 24.
Eupanthalis glabra , new species
(Figs 2-5)
Material examined. — Samples: 61 (FIG. 2a): 71; 8S, Holotype and 66 paratypes; 9S; 141; 151: 221; 231; 251;
261 (Table 1). Total: 76 specimens, Cyprus, 1; Israel, 75.
REPOSITORY. — Holotype (HUJ). Paratypes: 23 (1IUJ); 24 (SMF 4430); 2 (AMS: W208889, W20890); 7 (BMNII
ZB 1992.305-311); 9 (USNM 157612, 157613, 157614); 2 (MNHNP: UC343-A922, 344-A922) Topoivpe- 1
(SMF 4431). *
Fig. 2. — Eupanthalis glabra, n. sp.: a, anterior end with fully everted proboscis (from Cyprus); b-e (from Israeli coast): b,
anterior end with fully everted proboscis (holotype); c, dorsolateral view of anterior end (paratype); d, frontal view of
proboscis; c, lateral view of same. (Scales, a-e = 1 nun)
150
M.N. BEN ELI AH U & D. F1EGE
Description. — Body elongate. Largest, complete specimen, 65 mm, 64 seg.; H+10, 2.3 mm; width, 3.5 mm.
Hololype (Figs 2b, 3a-j) anterior fragment with pharynx fully extended, 32mm /50 seg. (11+10, 3.0 mm), width
4.0 mm. Population, H+10, 2.8 ± 0.6 nun [2.0- 4.0 mm], N= 20 ; width, 3.5 ± 0.4 mm [2.8-4.0], N= 20.
Fig. 3. Eupanthalis glabra, holotype: a, head; b, left elytrigerous parapodium from segment 2. anterior view; c, left
cirrigerous parapodium from segment 3, anterior view; d, right parapodium from segment 48. anterior view; c, upper
neuroseta from segment 2 ( 1st parapodium); f, lower neuroseta of same; g, upper neuroseta of segment 3; h, middle aristatc
acicular neuroseta from same; i, aristate acicular setae with subdistal tuft from segment 10; j, capillary setae with circlets
of spines (type b) from same. (Scales: a = 1 mm; b-d, 100 pm; e-j, 50 pm).
Source :
ACOETIDAi; FROM THE MEDITERRANEAN WITH DESCRIPTION OF A NEW SPECIES
151
Elytra smooth, elongate-oval, delicate; first pair covering prostomium, second and third covering dorsum,
remainder leaving middorsum uncovered. Posterior elytra very delicate, with lateral pouches.
Prostomium oval, bilobed, with median longitudinal groove (Figs 2c; 3a; 4a-b), with two pairs of sessile eyes,
anterior pair much larger or only slightly larger than posterior pair. Lateral antennae with short ceratophores on
anterior side of prostomium, with tapered styles, 1.7 (1.7 ± 0.3 11.3-2.2], N=17) times longer than prostomium
Palps ventro-lateral to antennae, stout, tapered, smooth, 5.0 (3.4 ± 0.9 mm [2.2-5. 3 mm]. N=19) times longer than
prostomium (Figs 2a-c; 3a).
First (tentacular) .segment distinct dorsally; nuchal lobe observed on holoiype (Figs 3a. 4b); tentaculophores
lateral to prostomium, each with aciculum, without setae, with dorsal and ventral tentacular cirri subequal in
length, 2.2 (2.2 ± 0.4 [1.6-3.3], N= 20) times longer than prostomium, 1.3 (1.3 ± 0.3 [1.0-2 1] N= 17) times
longer and stouter than lateral antennae, and 0.4 (0.7 ± 0.2 [0.4-1 .0], N= 19) shorter than palps (Fig’s 2a-c: 3a; 4b).
FIG. 4. — Eupanthalis glabra , scanning electron micrographs: a, anterior end. dorsal view, b, same, view more frontal, c, right
parapodia of segments 2 and 3. anterior view, d, right parapodium of segment 3 . posterior view. (Scales: a = 1000 pm; b,
d = 300 pm ; c = 1 00 p m ).
Second segment (first setiger) with first pair of elytrophores: parapodia modified, paw-like, sometimes directed
anteriorly, with ventral buccal cirri similar to tentacular cirri, 2.5-3 (N= 2) times longer than following ventral cirri
152
M.N. BEN ELI AH U & D. FIEGE
(Figs 3b-c; 4c-d); notopodium small, rounded acicular lobe on anterodorsal side of larger neuropodium;
neuropodium without notosctae. with bilobed presetal acicular lobe.
Extended proboscis 6.9 (7.3 ± 1.8 [5.2-10.31, N=19) times longer than prostomium (Figs 2a-b-c). Distal border
of proboscis with 13 pairs of conical papillae, middorsal and midventral ones very slightly enlarged both on wide
bases with lateral curved tips (Fig. 2d-e); two pairs of strong honey-colored hooked jaws, each with 2-6 teeth
(holotype with 4,3, 3, 3 teeth), with opposite pattern of dentition in upper left and lower right jaws vis a vis lower
left and upper right jaws (Figs 2d-e).
Fig. 5. — Eupantlialis glabra, scanning electron micrographs: a-c. Neurosetae of segment 2: a. upper, posterior view; b,
same, anterior view; c, lower, anterior view; d, neurosetae of segment 3: left, middle aristate acicular; right, upper
lanceolate; e, neurosetae of segment 10: left, middle aristate acicular with subdistal brush; right, upper, type b capillary; f,
lower neuroseta of segment 4; g. setae of segment 10 from anterior, showing Fine fibers of spinning gland. (Scales: a-d. f =
30 pm; e, g = 100 pm).
Dorsal cirrus on segment 3 with short cirrophore on posterodorsal side of notopodium, with long tapered style,
1.7-2. 3 (N= 4) times height of parapodium, 1.8-2. 3 (N= 2) times longer than ventral cirrus (Figs 3c; 4c-d).
Source :
ACOETIDAE FROM THE MEDI TERRANEAN WITH DESCRIPTION OF A NEW SPECIES
153
Beginning with segment 9, notopoclium wider, rounded flattened, on anterodorsal side of neuropodium with
internal spinning glands. Middle parapodia with dorsal cirri short, slightly shorter than height of parapodium 1 5
tunes shorter than tapered ventral cirri (Fig. 3d). 1 1 ’
Far posterior region with notopodia reduced to conical lobes; neuropodia more elongate, narrower cirri longer
than in anterior region. Integument of posterior region very thin. Parapodial branchial tubercles (as in Fig. 8a) not
present. Pygidium small, rounded, between few posterior small segments with two anal cirri.
Notosetae present from segment 9 to 19-22, very fine setae with one spiny margin emerging from lower side of
notopodium (lug 5g). Neurosctae show some anterior-posterior transition in anterior-most parapodia Neurosetae
in three groups (upper with shafts above aciculum; middle with shafts above and below aciculum- lower with
shafts be low aciculum). Upper neurosetae of two types: type a longer, slender, somewhat lanceolate with spinous
margins (lugs 3e, g; 5a-b-d). present throughout body; increasingly finer and longer posteriorly (in segment 2 ca
1.7 times thicker than m segment 3); type b very line, shorter, with circlets of few widely spaced spines (Figs 3f
5c), lacking in anterior and posterior parapodia.
Middle neurosetae acicular with tips slightly hooked, bearing distal hairy aristae, on segments 3-8 without
subdistal tufts of spines (Figs 3h; 5d); from segment 9 on with subdistal tuft (Figs 3i; 5e).
• L°^r curved’ wiUl Proximal spines on one margin, tapering distally to circumferential, close-set
spines (Figs 31; 5c-f).
Second segment Hirst setiger, lugs 3b; 4c): upper neurosetae, somewhat lanceolate with spinous margins more
massive than in following parapodia, 6 (6-7, 6.3 ± 0.6, N= 4 [Figs 3e: 5a-b]). Lower, 6 (1-6, 3.5 ± 2.1, N= 4 [Figs
Third segment (Figs 3c: 4d): upper neurosetae, 2 (1-2, 1.8 ± 0.4, N= 5), 0.3 (0.3-0.6) times as thick as in 2nd
segment (lugs 3g; .id. right). Middle aristate acicular neurosetae, 6 (5-6, 5.6 ± 0.5, N= 5, lacking subdistal spines
(Figs 3h; 5d, left), 2.2 (4) times as thick as upper. Lower neurosetae, 35 (14-35, 18.4 ± 9.3, N= 5 [Fi»s 3c. 4d[
with fine shafts ca. 1/4 those of upper neurosetae.
_ Fwm and including segment 9: upper neurosetae, type a, 18 [ 13-21, 16.4 ± 2.9] N= 7); type b, 31 [25-42, 32.1
± 5.5] N=7 (Figs 5e-g). Middle acicular neurosetae with subdistal spines, 7 [1-7, 5.7 ± 1 9 N=6] (Fi«s 3F 5e)
Lower neurosetae, 16 [7-16, 12.3 ± 3.3] N= 7 (Fig. 50.
Distribution. Cyprus ( 100-1 10 m), Israel (91.5-183 m [Fig. 1]); note the narrow depth range (Fig. II).
Etymology. — From die Latin, "glaber" meaning smooth, referring to the smooth palps.
Remarks. Pettibone (1989: 241) redescribed Eupanthalis kinbergi according to McIntosh (1876) and
supplemented the description of die holotype, whose palps were missing, with that of a specimen from Naples
McIntosh did not mention die palps.
As die present material shows, dierc are two species of Eupanthalis in die Mediterranean, one widi papillated
palps and one with smooth palps. Unfortunately, since die palps are missing on the holotype and not mentioned by
McIntosh, there is no possibility of ascertaining whether or not E. kinbergi indeed had papillated palps. We
propose that the name kinbergi be retained for the species with die papillated palps, as redescribed in Pettibone
(1989) and the new name, glabra, be applied to the Levant species with smoodi palps. Another difference between
diese species is the color of the jaws, dark in E. kinbergi, honey-colored in E. glabra. E. glabra is of much smaller
size than E. kinbergi. The presence or absence of a nuchal lobe is a difficult character to determine in this
preserved material; it appears to be present in E. glabra (Figs 2a-c; 3a; 4b).
Pettibone (1989) refers to two additional species widi smoodi palps; E. edriopthalma (Potts 1910) from the
Western Indian Ocean and E. elongata (Treadwell, 1931) from die Philippine Islands; bodi species have the
tentacular cirri about as long as die palps (in E. glabra, die tentacular cirri are shorter than the palps); both species
lack a nuchal lobe. E. edriopthalma has much shorter palps relative to the height of the prostomium than E glabra
(syntypes of E. edriopthalma with palps 1.1 ± 0.2 [1.0-1 .3, N= 2[) times longer than prostomium). Within die type
sample containing 67 individuals, the E. glabra population showed considerable variability in the relative lengths
of the head appendages (lengdi of palps vis a vis the antennae and the tentacular cirri, see Figs 2a-c). It may also
be related to the degree of contraction when preserved. None of the 19 individuals measured showed the short
condition as in E. edriopthalma.
E. elongata has different neurosetae on segment two and dark jaws (PETTIBONE, 1989). It also has longer
antennae relative to the prostomium [N= 1]; only one of 19 specimens of E. glabra measured showed the long
condition as in E. elongata.
154
M.N. BEN ELI Mill & D. REGE
The present study points to die difficulty of comparing populations in which variability has been found with
species descriptions based on few specimens. This problem is particularly acute in deep-water species with sparse
material.
Euarche tubifex Ehlers, 1887
(Figs 6; 8e)
Euarche tubifex - PETTIBONE, 1989: 14-18, Fig. 15.
Eupanthalis kinbergi -Fauvel, 1923: 100-101, Figs. 38i-q; AMOUREUX, 1976: 1049
(Not Eupanthalis kinbergi McIntosh, 1876]
Material examined: samples: 31, 3x: 8S; 121; 131; 161; ?16I, 3x; 171; 211; 27S, lx (SMF 4428); 28S, lx (SMI-
4427); 29S. 4x (SMF 4426); 30S, 2x (SMF 4429); 31S (SMF 4425) (Table 1).
Total: 11 specimens from Israel, H+10 length, 5.5 ± 2.2 mm [3-10 mm], N= 9). Largest, AI-, 78 mm, 69
segments (H+10, length, 10 mm); width, 9 mm (from sample 112). Nine specimens from Sicily, H+10 length, 9.00
± 1 .32 mm [8-1 1 mm], N= 9). Largest, AF, 85 mm, 63 segments (11+10, 1 1mm); width, 15 mm; with eggs.
FIG. 6. — Euarche tubifex : a, specimen from Israel, dorsal view of anterior, proboscis fully extended; b. specimen from Sicily,
lateral view of same. (Scales: a. b = 1 mm)
Remarks. — A decapod belonging to the family Pandalidae (M. Turkay, pers. comm.) was removed from die
gut of a Sicilian specimen.
Distribution. — Sicily (158-237 m), Israel (35 - 200 m). Worldwide (Pettibone, 1989): Caribbean, Northwest
Atlantic from Florida to North Carolina, Gulf of Mexico, Panama (Pacific), Southwest Atlantic to South Brazil,
Northeast Atlantic from West to Northwest Africa, Mediterranean, Arabian Sea, 13 to 450 m.
Source :
ACOETIDAE FROM THE MEDITERRANEAN WITH DESCRIPTION OF A NEW SPECIES
155
Eupolyodontes cornishii Buchanan, 1894
(Figs 1; 7; 8a-c)
Eupolyodontes cornishii Buchanan 1894: 438, pi. 227: Figs 1-8. - Pettibonf., 1989: 36, Figs 20-22.
Material. Sample 201 (Table 1). Anterior fragment, 74 setigers, 230 mm (II+10, 22.7 mm)- width 27 8 mm
fragment ol tube. Permanent mounts I IUJ-#361, 367: SMF-SHM #30.
FlO. 7. Eupolyodontes cornishii: a. tube after washing out interwoven clay; b. anterior fragment, dorsal view, with most
elytra missing; c. anterior end, dorsal view, with left lstelytrum pinned back. 1st right elytrum missing. (Scale: c= 1 mm).
Additional material studied. — Africa, off Congo River, 79-86 m, holotype (BMNH 1893.12.8.1).
Remarks. I he anterior fragment was inside the tube (Figs 7a, b). In her review of the Acoetidae, Pettibone
(1989) cites only the holotype; she considered another record of a New Caledonia specimen, deposited at (lie f’aris
Museum (Fauvel, 1897) as doubtful. The present material was collected in 1969 (Ben-Eliahu & Fiege, 1991)
and may be only the second record of E. cornishii since dial of Buchanan in 1894. J. NUNEZ has recently found
E. cf. cornishii from Tenerife from 200 m depth, based on a fragment of some middle setigers (J NuNEZ pers
comm.).
Ihere are some minor differences from the holotype redescribed by Pettibone, mainly in characters which
'aH w‘tl»n species variability; the description was based on a single specimen. The palps are short, but subequal in
length to the ventral tentacular cirri, and slightly surpass the prostomium. Notosetae were observed on the
tentacular segment and on segment 2 but not on segments 3 and 4.
Parapodial branchiae begin on segment 8 (rather than 6); most branchiae are simple, some with one branch (Y-
shaped. Fig. 8a), fewer with double-Y or with single and Y, best-developed between segments 17-31, and
continuing to the end of the fragment. The upper neurosetae (Fig. 8c, cf. Fig 22Ba of Pettibone, 1989) show a
slight swelling ("neck") at die proximal tuft and are somewhat recurved distally. This was confirmed on the
holotype.
156
M.N. BEN ELIAHU & D. F1EGE
Distribution. — Israel (55 m). Worldwide (Buchanan, 1894): Africa, mouth of Congo River, 35m from land,
79-86m; Tenerife, (200 m) (Nunez, pers. comm.) (55 - 200 m).
Fig. 8. — Scanning electron micrographs: a-c, Eupolyodonies comishii : a. 20th right parapodium, posterior view; note
parapodial branchiae; b, middle acicular neuroseta; c. upper neurosetae; d. Polyodontes maxillosus , middle acicular
neurosetae: e, Euarche tubifex : middle acicular neuroseta from 3rd segment, anterior view; f, Pcinlhalis oerstedi, tip of 9th
right neuropodium, left, middle acicular neurosetae; right, upper neurosetae. (Scales: a = 1,000 pm; b-d, f = 100 pm;
e = 60 pm).
Panthalis oerstedi Kinberg, 1856
(Figs 8f: 9a-c)
Panthalis oerstedi Kinberg, 1856: 387 - PETTIBONH, 1989: 53-56, Figs 32-34; BEN-EL1AHU el al. 1991: 62-64.
MATERIAL examined. — Samples II; 21; 31; 41, 5x; 51, 6x; 8S, lx(SMF4407); 10S, 6x (SMF4417); 1 IS. 8x
(SMF 4418) ; 191, lOx; 231; 241, 4x (Table 1). Total: 44 specimens, largest, anterior fragment, 18mm, 32
segments, H+10, 5 mm; width, 6.2 mm. Large complete specimen, 35 mm, 71 segments (11+10= 5.5): width 5
mm. H+10, 2.5 - 5.5 mm [3.6 ±0.8], N=41.
Source :
ACOETIDAE PROM THE MEDITERRANEAN WITH DESCRIPTION OF A NEW SPECIES
157
Remarks. Body broadens after about segment 16 and then narrows. Many individuals of sample 51 with
opaque dark brown bodies in body cavity, presumably parasites (Figs 9a,c). Figure 9c shows the long filament of
the spinning gland in die body cavity. The depdi range is extented to 1.470 m.
Fig. 9. a-c. Pcmthalis oerstedi. a, dorsal view of anterior; b. lateral view of anterior end with proboscis fully extended; c.
parapodium with elytron and long filament of spinning gland in body cavity; dark circles presumed to be cysts of parasite;
d. Polyodontes maxillosui: dorsal view of anterior end. (Scales: a-d = 1 mm).
DISTRIBUTION. — Israel (95 m - 1470 m). Worldwide (PirniBONE, 1989: 56): Sweden, Norway, North Atlantic to
Mediterranean, Northwest Africa (1 1 -760 m); die depdi range is broad, 1 1 - 1,470 m.
Polyodontes maxillosus (Ranzani, 1817).
(Figs 8d; 9d)
Polyodontes maxillosus. — Petobone, 1989: 101-103, Figs 70-72.
Material examined. — Samples 61; 8S (SMF 4421); 121 (Table 1). Total: three specimens, largest, anterior
fragment, 43 mm. 52 segments (11+10, 5 mm): width. 3 mm. 11+10, 3.6-5 mm [(4.2 ± 0.7) N= 3).
158
M.N. BEN ELI AI IU & D. FIEGE
DISTRIBUTION. — Israel (35-110 m). Worldwide (PETTI BONE, 1989): North Atlantic off Spain, Adriatic, Red Sea,
low water to 280 m.
FK3. 10. — Lengths of specimens of Euarche tubifex (11+10 parameter) vs. depth.
KEY TO THE LEVANT ACOETIDAE
1 Eyes stalked (ommatophores); 3 antennae (Figs 7; 9) .
Eyes not stalked, sessile; 2-3 antennae (Figs 2a-c; 6) .
2 Parapodia branchiae absent (Fig. 9d); palps well-developed (Fig. 9a-d);
acicular neurosetae aristate (Fig. 8d-f) .
Parapodial branchiae present (Fig. 8a); palps reduced (Fig. 7c);
neuroacicular; setae not aristate (Fig. 8b); of giant size . £• cornishii
3 Ommatophores white; sessile eyes absent (Fig. 9a);
upper neurosetae pcnicillate (Fig. 80 . P • oerstedii
Ommatophores black; sessile eyes present (Fig. 9d); upper neurosetae
tapered (Fig. 8d) . P • nioxillosus
4 Two antennae (Fig. 2a-c; Fig. 4a-b) . . . 5
Three antennae (Fig. 6a-b) . £• tubifex
5 Palps papillated . £• kinbergi 1
Palps smooth (Fig. 4a-b) . ; . gtabra
DISCUSSION
Mediterranean biogeographers have reported reduced body size (dwarfing) in several different groups in die
Levant marine fauna (sponges, echinoderms, sipunculids and polychaetes [e.g., LAUBIER, 19661). However, the
observation on dwarfing in the Levant has yet to be analyzed properly. Hie present paper describes differences in
length of specimens of Euarche tubifex from die Israeli and Sicilian coasts. The Israeli populadon was of smaller
size than the Sicilian one (Israel, H+10, 5.50 ± 2.17 mm [range, 3-10 mm], N= 9, vs. Siciliy, 11+10, 9.00 ±
1 Not found in Levant. Reported from Italy (Pettibone. 1989).
Source :
ACOETIDAE FROM THE MEDITERRANEAN WITH DESCRIPTION OF A NEW SPECIE S
159
1.32 mm [range 8-11 mm], N= 9) and llie difference between the means was significant (t-test, t= -4.1384,
p = 0.0008, Fig. 10). Information concerning the age of the specimens is lacking. In addition, die depth ranges
sampled may not be comparable: the Israeli E. tubifex population came from a broader range beginning0 in
shallower depths than die Sicilian one (35-200 m : 158-237 m, Israel : Sicily, respectively).
Fig. 11. — Levant (L) and worldwide (W. from PETTIBONE, 1989) depth distribution of aeoedd species: E.g.. Etipanthalis
glabra: P.o., Pamhalis oerstedi ; P.m.. Polyodontes maxillosus ; E.t ..Euarche tubifex: E.c.. Eupolyodontes comishii.
6
5.5
1 5
o 4.5
I 4
B)3,5
s 3
2.5
2
0 200 400 600 800 1000 1200 1400 1600
Depth (m)
Fig. 12. — Length of specimens of Panthalis oerstedi (11+10 parameter) vs. depth.
H+10 length (mm)
FIG. 13. Lengths (H+10) of Israeli Acoetidae. mean ± s.d; N. number measured.
Source :
160
M.N. BEN ELIAIIU & D. FIEGE
To evaluate whether populations from different depths can be compared requires determining whether a
positive correlation exists between depth and body size, as in gastropod populations from intertidal and subtidal
depths (Kohn. 1971; Kohn & Nybakken, 1975). Two species are rare, Eupolyodontes comishii , found only
once, and PolyodontesjnaxiUosus, found only three times. One species, Eupantiialis glabra, appears to have a
very restricted depth range (from 90-183 m. Fig. 1 1). Thus, the proposed correlations for body size and depth
could only be carried out for Euarche tubifex (Israel), and Pcinthalis oerstedi.
For Pcinthalis oerstedi , die deepest species (Fig. 11), and one with a great depth range (95 - 1470 m), the
Spearman correlation between length of specimens and depth was highly significant (r = 0.60500, p = 0.0001,
N= 41, Fig. 12). However, in the Israeli Euarche tubifex population, it was not significant (r = 0 32154 p= 0 3988
N= 9); the largest specimens were from die greatest depth (Fig. 10), however, die smaller worms were not only
iom die shallowest depth. The small depth range (165 m) or die small samplesize (N= 9) may contribute to this
lack ol significance. Unlortunately, on die basis of these results, body sizes of individuals from different areas
which come from different depths cannot be made.
A comparison ol the body sizes of die five Israeli species is given in Fig. 13. Depth distributions of the five
species along the Israeli coast are compared with their worldwide distributions given in PETTI BONE, 1989 (FF
1 1 ). Three of (he species' ranges begin in deeper waters in die Levant than elsewhere. This has previously bec^i
reported lor Levant serpulid Species (Ben-Eliahu. 1991). All four of die smaller species (Figs 1 1; 13) are present
and appear abundant at 100 in. As noted above, die Levant population of P. oerstedi is recorded from 1,470 m
700 in deeper than elsewhere (Fig. 11); die species appears to be abundant from 200 m.
ACKNOWLEDGEMENTS
We thank M. TOrkay of the Forschungsinstitut und Naturmuseum Senckenberg for samples of die 'Meteor' V
and die oseidon 1 72-4 cruises, and for identifying the decapod prey. Samples were made available by E. Gii.at
o the Sea fisheries Research Station; die project, "Biota of die Red Sea and eastern Mediterranean"; the Israel
National Collections of Natural History at Hebrew University and at Tel Aviv University lor loan of material- S
I 'san-i y, Department ol Fisheries. Ministry of Agriculture; D. C.OLANI, The Hebrew University of Jerusalem and
B. Gai.il. Israel Oceanographic Institute. Ltd.; J. Nunez for data. We also thank D. Gateno for assistance with
die statistical analysis: S. IlALBRElCH redrew Figure 3; A. Neev did some of the photographs. R. Barnich for
Fruie h translations; M.L. I RITZ tor invaluable assistance. D. GEORGE and A. Muir for a productive visit to the
British Museum (Natural History). H. BROMLEY-SCHNUR, M. TOrkay, F.D. Por read previous drafts; two
anonymous reviewers made valuable suggestions.
KbII-KLNCFS
AM“!- IX- ‘ israelitica. nouvelle espece dc Serpulidae (Annelidas Polychcles) el une petite
collection annehdienne de la Mediterranee orientale. null. Mus. nail Hist. not. Pahs. 3 ser.. 404 : 1047-1059.
“r- M'N'T11990' ,Sccond preliminary report on Polychaeta from some deep-sea benthic sampling in the eastern
SSnea,nT fCt| 'i MaR™ & B- °AUL Proc. Second Interdisciplinary Conference on L Continental
SlelJ of Israel. I el Aviv University. May, 1990. Inst, for Nature Conservation Research. Tel Aviv University : 28-29.
BEN-ELlAltu. M.N., 1991. — Red Sea serpulids (Polychaeta) in the eastern Mediterranean, pp. 515-528. Ophelia. Suppl.. 5 :
Bl^TtM N-; M',N. * fIEGE: l99L ~ Somc sPecies belonging to the Aphroditoid family Acoetidae (Polychaeta)
horn the Levant and the Central Mediterranean. Abstracts of the Israel Zool. Soc. Meeting. Dec. 2-3. 1991. Tel Aviv : 1 1 -
BEN-EL. AHU. M.N F.D. Por & B. GaLU.. 1991. - A preliminary report on the density and composition of small sbe
Levantine bathyal benthos. Abstract. In : Y. Marth & B. Galii. (eds), Proc. Third Annual Symposium on the
Medttertanean continental margin of Israel. Israel Ocean. & Limn. Res,, Nat. Inst. Oceanogr. ; 62- 64. ' P
BUCHANAN. F.. 1894. - A Polynoid with branchiae ( Eupolyodontes comishii ) Quart. J. Microsc. Sci. (Loud.), 35 : 433-450.
88-n2erVali0nS SUF lEup0ly0d0n,eS cM“ Buchana„ (Annelide Polychete Errante). null. Soc. Linn.
Source : MNHN, Paris
ACOETIDAE FROM THE MEDITERRANEAN WITH DESCRIPTION OF A NEW SPECIES
161
FauVEL. P.. 1923. — Polych&tes Emmies. Faunc de France 5 : 1-494.
Kinberg. EG. FI., 1856. Nya slagten och arter of Annelida. K. Vetensk.-Akad. Fo>/i.(Stokholm). 12 : 381-388.
Kohn. A.J 1971. — Diversity and utilization of resources and adaptive radiation in shallow-water marine invertebrates of
tropica] oceanic islands. Limn. Oceanogr .. 16 : 332-347.
Kohn. A.J. & J.W. Nybakken, 1975. — Ecology of Conus on eastern Indian Ocean fringing reefs: diversity of species and
resource utilization. Mar. Biol., 29 : 211-234. 1
LAUBIER, L., 1966. Sur quelques Annelides Polychctes de la region de Beyrouth. Am. Univ. Beirut Miscell. Pap.. 5 : 9-22.
MCl4™SH W C * 1876 ~ °n lhC Annelida °f ^ PorcuPine Expedition of 1869 and 1870. Trans. Zool. Soc., Lond.. 9 : 395-
PETTIBONE, M.H.. 1989. Revision of the aphroditoid polychaetes of the family Acoetidae Kinberg (= Polyodontidae
Augener) and reestablishment of Acoeies Audouin and Milne-Edwards. 1832 and Euarche Ehlcrs, 1887 Smiths Conir
Zool.. 464 : 1-138.
POR. P.D.. H. Steinitz, I. Ferber & W. ARON. 1972. — The biota of the Red Sea and the Eastern Mediterranean (1967-1972)
A survey of the marine life of Israel and surroundings. Isr. J. Zool.. 21 : 459-524.
Potts, F.A., 1910. — Polychaeta of the Indian Ocean. Part 2: The Palmyridae.
Sigalionidac. Trans. Linn. Soc., London, scr. 2. 13 : 325-353.
Aphroditidae, Polynoidae, Acoetidae, and
PUTEANUSD., 1990. - Cruise Report 'Poseidon' 172 4. MIPAMEHR-MAST I. Volcanism and Hydrothermal Activity in the
Strait of Sicily. Malaga Trapani - Faro, 19.4.-14.5.1990. Reports. Gcol.-PalSont. Inst Univ. Kiel. 41:1-1 16.
TREADWEl-L. A.L., 1931. — Four new species of polychaetous annelids collected by the United States Fisheries Steamer
Albatross during the Philippine Expedition of 1907- 1910. U.S. Nat. Mas. Bull., 100, 6 : 313-321.
Weikert, IT. 1988. — Expeditionsbcricht fiber die "Meteor" -Reise 5, Abschnitt 1. (2. Januar bis 28. Januar 1987 Ostliches
Mittelmeer/ Hamburg Heraklion - Port Said). Inst. f. Hydrobiologie und Fischereiwissenschaft. Berichte aus dent
Zentrumf Meeres- und Klimaforschung der Universitat Hamburg'. 1-39.
Source : MNHN. Paris
17
Prionospio caspersi Laubier (Polychaeta, Spionidae)
in the Black Sea: long-term monitoring
of a population
TemirA. BRITAYEV * Alberto CASTELU** & Tatiana S. AKSIUK*
* A.N. Severtzov Institute of Evolutionary Animal Morphology and Ecology
Russian Academy of Sciences
Leninsky prospect 33, Moscow 1 17071, Russia
** Istituto di Scienze Antropologiche, University di Sassari
Corso Margherita di Savoia 15
1-07100 Sassari, Italy
ABSTRACT
Numerous specimens of the spionid polychacte Prionospio caspersi Laubier were found in benthic samples from Kapsel
Bay. the southeastern coast of the Crimean Peninsula. This was the first record of this species in the Black Sea. P, caspersi was
very abundant in sandy and silty sand communities at depths of 9 to 23 m. We monitored this community from 1986 to 1991, a
period in which the density of P. caspersi varied seasonally, being highest in spring (up to 730 ind. m2) and decreasing in the
months of August and September (to 96 ind. m2). From April 1986 to April 1989. the frequency of occurrence in grab samples
varied from 50 % to 100 %. decreasing at the end of each summer. Interpretation of size-frequency histograms suggests that
recruitment look place in the second half of the summer. In autumn 1989 P. caspersi disappeared from Kapsel Bay and was not
found at the study site or adjacent areas in 1990 or 1991. Possible causes for its disappearance were discussed.
RESUME
Prionospio caspersi Laubier (Polychaeta, Spionidae) en mer Noire : suivi a long ternie d’une population
De nombreux exemplaires du polychete spionide Prionospio caspersi Laubier ont ete recueillis sur les fonds de la baie de
Kapsel. sur lc cotes du Sud-Est de la Crimee, mer Noire. II s’agit de la premiere decouverte de cette espece en mer Noire. P.
caspersi apparait avee une tres grande abondance sur les fonds sableux et sablo-vaseux entre 9 et 23 metres de profondeur.
Nous avons suivi cette communauhS de 1986 a 1991. periode au cours de laquelle la densite de P. caspersi a varid selon les
saisons, atteignant au printemps son maximum (jusqu'a 730 ind. m2) et diminuant ensuite dans les mois d’aoGt et de septembre
(a 96 ind. m2). D'avril 1986 a avril 1989, sa frequence dans les echantillons a vari£ de 50 % a 100 %, diminuant a la fin de
chaquc ete. L' interpretation des histogrammes taille-frcquencc suggere que le recrutement advient dans la seconde moitic de
l'cte. Au cours de l automne 1989, P. caspersi a disparu de la baie de Kapsel, aucun exemplaire n'ayant ete retrouve ni en 1990.
ni en 1991. Les causes possibles de cette disparition sont discutees.
BRITAYEV. T.A.. CASTELU, A. & T. S. AKSIUK, 1994. Prionospio caspersi Laubier (Polychaeta, Spionidae) in the Black
Sea: Long-term Monitoring of a population. In: J.-C. DaUVIN. L. LAUBIER & D.J. REISH (Eds). Actes de la 4cme Conference
internationale des Polychetes. Mem. Mus. natn. Hist, nat., 162 : 163- 168. Paris ISBN 2-85653-214-4
Source : MNHN. Paris
164
A BRITAYEV. A. CASTELLI & T. S. AKSIUK
INTRODUCTION
Prionospio caspersi Laubier, 1962 was first discovered in Venice Lagoon (Laubier, 1962) and later found in
many areas of the western Mediterranean and Adriatic seas (Laubier, 1965; GuBrin, 1970). This species inhabits
sand and silty-sand sediments of the upper sublittoral zone (I.ardicci, 1989). In die Black Sea. P. caspersi was
recently found and described from the southeastern coast of the Crimean Peninsula (Britayev et al, 1991, Fig.
1). In this paper we suggested that P. caspersi had earlier been misidentified as P. malmgreni Clapaitde, 1868 and
that its distribution in the Black Sea was thus probably considerably wider than realized.
FiG. 1. — Study area in Lapse! Bay, the Black Sea. Sampling stations (A-K) indicated by black dots. Shaded areas show
location of mussel (Mytilus galloprovincialis ) farm.
1 lie ecology ol P. caspersi in the northern Adriatic, mainly its secondary production in the vicinity of the Po
Estuary, was investigated by Ambrogi el al., 1985 and AMBROGI, 1990.
During 1986-1991 personnel from the Institute of Fisheries and Oceanology, Moscow, monitored benthic
communities m die Black Sea, near Sudak (PERELADOV el al., 1988). During this period benthic samples were
collected 2-4 times a year. Since P. caspersi was numerically dominant at the study site, die material was suitable
or an evaluation of seasonal and long-term changes in the population structure of this species.
Source :
BLACK SEA POPULATION OF PRIONOSPIO CASPERSI
165
MATERIALS AND METHODS
The study was carried out in Kapsel Bay, near the town of Sudak on die southeastern coast of the Crimean
Peninsula, in the area of a mussel (Mytilus galloprovincialis Lamarck, 1819) farm (Fig. 1). Benthic samples were
collected at the same stations twice a year in 1986-1987 and 1989-1991 (spring and late summer or autumn), and
once every three months in 1988. Although not all stations were sampled each time, all sampling periods except
November 1990 included samples from within and outside the mussel beds, for die most part about half of each
(Table 1). At each station 1-4 samples were taken by a Petersen grab (0.025 m2). The samples were sieved
through 0.5 mm mesh and all P. caspersi were removed, fixed in a 4 % formalin solution and counted. For study
of size-frequency distribution, specimens collected in February, April and August 1988 were used. For each
specimen die surface area of die first 10 setigers was calculated according to die method of Ambrogi ei al. ( 1985).
The material is deposited in the A.N. Severtzov Institute of Evolutionary Animal Morphology and Ecology.
Russian Academy of Sciences, Moscow.
RESULTS
Prionospio caspersi inhabited clean fine sand and silty sand at depths of 9 to 23 m in the community of the
bivalve mollusc Chamelea gallina (L., 1758). At sites where the silty fraction prevailed, P. caspersi was absent. It
was not found at depths greater than 23 m which may have been the results of die predominance of silly sediments
here.
Size- frequency distribution of individuals based on the surface area of die first 10 sedgers is shown in Fig. 2.
The curves were unimodal in February and April and bimodal in August. The modal area of the first 10 setigers
was 0.56 min2 (average: 0.62 mm2, n = 128 specimens) in February, increasing to 0.71 mm2 (average: 0.76 mm2,
n = 146) by April. The first peak of the size-frequency curve in August was formed by individuals with a modal
area of 0.34 mm2. This peak reflected the appearance of a new generation. The second peak was formed by
specimens with a modal area of 0.64-0.71 mm2. This corresponded to die single peak in winter and spring months
formed by specimens of the previous generation. The period from April to August was characterized by negative
growdi of die population probably reflecting the death of die parent population.
No. of specimens
“* February April August
N-128 Nr146 N -84
FlG. 2. - Prionospio caspersi. Size- frequency curves based on surface area of anterior end calculated according to method of
Ambrogi et a/. (1985). Arrow indicates appearance of recruits.
166
A. B RITA YE V. A. CASTELLI & T. S. AKS1UK
FIG. 3. Prionospio caspersi. Seasonal and long-term changes in population density in Kapsel Bay. Black Sea. Arrow
indicates last find of this species.
Prionospio caspersi outstripped other benthic species in terms of density and frequency of occurrence in 1986-
1988. The maximum density was about 2440 ind.m?, and the mean density varied from 96 to 730 ind. m2.
Table 1. — Prionospio caspersi. Frequency of occurrence at 1 1 stations (A-K) in Kapseh Bay, die Black Sea.
Source MNHN. Paris
BLACK SEA POPULATION OF PRIONOSPIO CASPERS!
167
In 1988, hcniliic samples were collected in all seasons, so diis year is more suitable than die others for an
analysis of the seasonal dynamics of the population. Population density was maximal in winter and spring,
decreasing in summer and increasing in autumn (Fig. 3). A decrease of population density in summer was noted
also in 1986 and 1987. The decrease in population density in August-September was accompanied by a reduced
frequency of occurrence (Table 1 ).
As a result of benthic community monitoring from 1986 to 1991, the population of P. caspersi population may
be followed until April 1989 when it was taken for die last time (Fig. 3). P. caspersi was absent from samples
taken in September 1989 through 1991.
DISCUSSION
The size- frequency histograms suggest that a recruitment took place in die second part of die summer. These
data agree with AMBROGl's (1990) observations. He found diat P. caspersi had an annual life cycle widi intensive
recruiunent in die beginning of July in die Adriatic Sea. The decrease in density and frequency of occurrence in
August-September was probably related with the change of generations. High mortality eliminated the parent
population, and at die same time die density of die new generation was low as a result of die prolonged period of
recruitment which was not yet over.
The population density of P. caspersi in die Adriadc Sea (Ambrogi, 1990) was about 15-20 times higher than
in the Black Sea. The trophic conditions in diesc areas are similar. The concentration of organic carbon in the
Black Sea varied from 4.5 to 8.1 gC.kg1 in winter and summer, respectively (Pereladov, pers. comm.). This is
similar to die values found in die Adriatic Sea by Ambrogi (1990) (2. 1-8.2 gC.kg-i). The sediment structure was
similar at both sites. However, die hydrodynamic conditions in the two areas were different. AMBROGI (1990)
emphasized the stability of environmental parameters in die Adriatic. In contrast, Kapsel Bay is an exposed bay
and die upper layer of sediment is influenced by wave action to 15-20 m, the lower depth of die distribution of P.
caspersi. This species inhabits the thin upper layer of sediments and is usually disturbed during storms. Therefore!
wave action is probably die main factor causing a decrease in the density of P. caspersi on die southeastern coast
of Crimea.
This theory provides an explanation for the disappearance of P. caspersi in the atituinn of 1989. In early
September 1989 a storm preceded the disappearance of P. caspersi (Pereladov, pers. comm.). In this period the
entire population was essentially comprised of young specimens. Destruction of the P. caspersi population was
probably due to the co-occurrence of this storm with the most vulnerable period of the life cycle. The absence of
recruitment in 1990-1991 probably reflected the absence of drift larvae from adjacent areas, i.e., die disappearance
of P. caspersi in adjacent areas.
ACKNOWLEDGEMENTS
We are grateful to Mr. M.V. Pereladov for organizing the monitoring of benthic communities in Kapsel Bay
and for fruitful discussion of this paper. We gratefully acknowledge our colleagues Dr. E.G. Zavarzina, Mrs.
N.V. Britayeva and Mr. M.A. Saburin for their assistance in collecting and sorting material. We thank Dr. Y.I.
Kantor and Dr. J.A. CHERNIAEV for help with the English and French translations, respectively. We are grateful
to Dr. M.E. Petersen, whose thoughtful comments improved this manuscript.
REFERENCES
AMBROGI. R.. 1990. — Secondary production of Prionospio caspersi (Annelida: Polychaeta: Spionidae). Mar. Biol.. 104 : 437-
442.
Ambrogi. R., Fontana, P.. & Occhipinti Ambrogi, A., 1985. Un metodo planimetrico per biometrie di invertebrati
marini. Studio preliminare di una popolazione di anellidi policheli. Nova Thalassia. 7 (suppl. 3) : 269-274.
Britayev, T.A.. CASTELLI, A., & AKSIUK. T.S., 1991. — On the finding of Prionospio caspersi (Polychaeta, Spionidae) in the
Black Sea. Zool. Zh., 70 : 5-9 (In Russian, English summary).
168
A. BRITAYEV, A. CASTELLI & T. S. AKSIUK
Gu£RIN, J.-P.. 1970. — Description dcs stades larvaires de Prionospio caspersi Laubier (Annelide polychete). Repartition dcs
larves de Prionospio en Mediterranee Occidentale. Tethys , 2 : 35-40.
Lardicci. C. 1989. Censimento dei policheti dei mari italiani. Spionidae Grubc, 1850. Atti Soc. Tosc. Sci. Nat., Mem., Serie
B, 96: 121-152.
Laubier. L., 1962. — Quelques Annclidcs polychetes de la lagune dc Venise, description de Prionospio caspersi n. sp. Vie <&
Milieu, 13 : 124-159.
Laubier. L.. 1965. Quelques Annelides polychetes de 1’Atlantique reccmment signalees ou nouvellcs en Mediterranee
occidentale. Rapp. P.V. Comm. Ini. Mer Medit. , 18 : 135-138.
Pereladov, M.V., Britayev. T.A., Zavarzina, E.G.. & Aksiuk, T.S., 1988. — The influence of mussel farming on the
benthic communities of Sudak Bay (the Black Sea). Ribnoe Hozaistvo . 9 : 27-30 (In Russian).
Source : MNHN, Paris
18
Systematics, ecology and biogeographical relationships in
the sub-family Travisiinae (Polychaeta, Opheliidae)
Jean-Claude DAUVIN* & Gerard BELLAN**
♦Laboratoire de Biologic des Invertebres Marins et Malacologie, URA CNRS 699
57 rue Cuvier, 7523 1 Paris Cedex 05. France
♦♦Centre Oceanologique de Marseille, URA CNRS 041
Station Marine d’Endoume, rue de la Battcrie des Lions, 13007 Marseille, France
ABSTRACT
The Opheliidae is divided into three monophyletic groups corresponding to the three sub-families defined by HARTMANN-
SchrOder: Ophelininae, Opheliinae and Travisiinae. 'Ihe object of the current paper is to offer a contribution to the knowledge
of the sub-family Travisiinae including taxonomy, ecology, biogeographical distribution. Three genera are studied:
Dindymenides, Kesun and Travisia. Based on previous phenetic and phylogenetic studies of the family and sub-families, we
propose to consider Travisia as the only valid genus in the sub-family. Twenty-seven species and three sub-species are
recognized in this genus. However, many of them are incompletely described and the characters used in species-recognition
varies from one author to the next and the validity on some characters has not been recognized until recently. Most of the
species must be redefined based on recent findings; we are, however, able to propose a preliminary key to species. Species of
Travisia general inhabit a muddy substratum, from the intertidal to abyssal depths (7,800 m). Twenty-one taxa are found on the
continental shelf and 14 of these are limited to shelf depths (< 200 m). Eleven taxa are found at depths below 2,500 m; three
are strictly abyssal. The genus shows a world-wide distribution, but is especially well represented in the Pacific Ocean (21
taxa). Seven taxa are found in the Antarctic Ocean and 10 in the Atlantic Ocean. Sixteen taxa are exclusively to the Pacific
Ocean. Eight species with a large geographical range also show extended bathymetric ranges: T. glandulosa, T. J'orbesi. T.
fusus. T. gravieri, T. japonica, T kerguelensis, T. olens, and T. profundi. A study of the relationship between species and
biogeographical distribution is given.
RESUME
Systeniatique, ecologie et relations biogeographiques dans la sous-famille des Travisiinae (Polychetes, Opheliidae)
L ensemble des donntSes sur la famille des Opheliidae a etc reuni afin de fournir un etat actuel des connaissanccs sur cette
famille. Les Opheliidae se divisent en trois groupcs monophyletiques correspondant aux trois sous-famille decrites par
HARTMANN -SCHRODER : Ophelininae, Opheliinae et Travisiinae. L’objectif de cette note est de fournir une revue des
connaissanccs sur la taxonomie, lecologic, la distribution biogeographique de la sous-famille des Travisiinae. A partir de
considerations pheneliques et phylogeneliques, il est propose de reunir les trois genres decrits : Dindymenides, Kesun et
Travisia, dans le seul genre Travisia. Vingt-sept especes et trois sous-especes peuvent etre reconnues comme valides,
cependant beaucoup d’especes demeurent incompletement decrites el les caracteres morphologiques utilises changent d’un
DAUVIN. J.C. & G. BELLAN, 1994. Systematics, ecology and biogeographical relationships in the family Travisiinae
(Polychaeta, Ophelidae). In: J.-C. Dauvin, L. LAUBIER & D.J. RE1SH (Eds), Actes de la 4eme Conference intemationale des
Polychetes. Mdm. Mus. natn. Hist, nat., 162 : 169-184. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
170
J.C. DAUVIN & G. BELLAN
auteur & I'autre. Bien que la plupart des especes merite de nouvelles observations, il est propose une cle preliminaire
d'identification dcs especes du genre Travisia. Le genre est typique des substrats vaseux, il est rencontnS depuis la zone
intertidale jusqu'aux abysses (7800 in). Vingt-et-un taxons sont connus du plateau continental, 14 ne depassant pas cc plateau.
Onze taxons ont ete recenses a des profondeurs inferieures a 2500 in, trois d’entre eux sont strictement abyssaux. Le genre a
une distribution cosmopolite, mais il est particulierement bien represent^ dans l'oc^an Pacifique (21 taxons). Sept taxons sont
antarctiques. 11 atlantiques, 16 sont exclusifs clu Pacifique. Huit especes ont une large distribution geographique et
bathymetrique : T. glandulosa, T. forbesi, T. fusus, T. gravieri, I japonica. T. kerguelensis, T. olens, et T. profundi. Les
relations biogeographiques entre les especes ont ete recherchees.
INTRODUCTION
During the course of our research, we have had the opportunity to study the species belonging to family
Opheliidae, including die genus Ophelia (Bellan & Dauvin, 1991; Bellan-Santini et al ., 1992), and die family
in general (Bellan et al ., 1990). In diis last paper, die 12 genera of the family were analyzed to attempt a
coherent classification of the family. Our results confirm the subdivision into diree sub-families originally
proposed by Hartmann-Schroder (1971): Ophelininae, Opheliinae and Travisiinae. This last sub-family seems
particulary suitable to be studied because of die small number of accepted genera: Dindymenides , Kesun and
Travisia , its plesiomorphy, and its undespread ecological and geographical distributions. Neverdicless, one of die
difficulties lies in the incomplete description of many species, and the non-existence of type specimens. The lack
of accuracy of descriptions is due, usually, to age of the specimens, and the small number of specimens described,
but it is also necessary to point out the difficulties inherent to the morphological criteria used for these
descriptions. Our major objectives are to present the various problems remaining widiin the sub-family
Travisiinae, to present die state of die knowledge on this sub-family widi a preliminary key, to discuss the
generally admitted viewpoints, and to propose a certain number of interpretations and hypothesis as a basis for
future work.
TAXONOMIC STATUS OF GFNERA AND SPECIES OF TRAVISIINAE
The sub-family Travisiinae may be defined as following:
Opheliidae with short and grublike body, without lateral and ventral grooves or widi very reduced grooves.
Branchiae generally present, posterior setigers generally with epipodial pads. Anal cylinder usually short,
sometimes furrowed, anal cirri short, and diick setae smoodi or finely spinose.
The genus Travisia was first described by JOHNSTON (1840) as:
Diagnosis: Body short, fusiform or grublike, without distinct groove. Prostomium small, cone-shaped, two
nuchal organs. Branchiae present, lateral eyes absent: posterior epipodial pads more or less developed. Parapodial
small, without presetal lobes. Lateral sense organs present between parapodial rami. Anal cirri usually short and
thick. Setae simple, capillary, or hispid. First setiger appears before the mouth.
Two other genera have been described: Dindymene Kinberg, 1866, and Kesun Chamberlin 1919.
Diagnosis: Dindymene Kinberg, 1866 " Corpus fusiforme, segmenta 3-2 annulata, lobus cephalicus minutus,
lerminalis, nudus; segmenta buccalia tria, primum nudum; os inferum, transversum; pharynx sine papillis et
maxillis; pedes duplices, distantes, setis capillaribus: aliis laevibus, aliis serrulato-ciliatis; branchiae cirrosac,
usque a segmento buccali secundo; segmenta posteriora tuberculis binis utrinque praedita".
Chamberlin (1919) renamed this genus Dindymenides since die original name has been used in 1847 for a
Crustacean. He does not give more details on die diagnosis of the genus.
Bellan etal. (1990), following Fauchald (1977), kept Dindymenides as a valid genus on die basis of a
strong auloapomorphy: die serratulate-ciliale setae. However, these audiors pointed out that these characters
needed to be confirmed. A certain number of Travisiinae belonging to genus Kesun and Travisia have been also
described with hispid and/or scrratulated setae. Hartman (1948), who examined die Kinbcrg's material, did not
mention diese ornamentations. If we consider the position of the first setae with regard to die moudi, Hartman
stated diat die prostomium of die preserved specimen had been unnaturally flattened in a vial, resulting in the
misinterpretation of die anterior part of die animal. Hartman staled: "the first setae arc in front of the oral
aperture". Considering the wide variations of die body of die Travisiinae due to dieir conservation, we accept die
opinion of Hartman at least until we are in position to examine freshly material. Dindymene and thus also
Dindymenides is known only from a single record (Day, 1967). In summary, we prefer to consider diis genus
SYSTEM ATICS, ECOLOGY, BIOGEOGRAPHY IN TRAVISIINAE
171
invalid, following the opinion of Hartman (1948), and more recently Fauchald (in litt.). The only species
known in the genus, originally described as Dindymene concinna, must now be known as Travisia concinna
(KlNBERG, 1866).
Diagnosis: Kesun Chamberlin, 1919. "Body short, pointed at both ends, fusiform or grub-like. Body rounded
cylindrically, without ventral groove. Somites of the middle region triannulate, the others may be only biannulate
or entire. Prostomium small, wholly smooth and rounded, without processes. Parapodial tubercles small and
smooth, or wholly absent. No cirri or branchia on any somite. No eyes. With a series of lateral sensory pits as in
Travisia . Pygidium small, cylindrical, longitudinally furrowed. Segments not numerous (twenty-eight in the
type)".
Kesun was created by CHAMBERLIN(1919) for a species Kesun fusus distinguishable from the other species of
Travisia described at dial time, by the lack of "cirri" which are commonly interpreted as branchiae. Another
feature is the absence of epipodial pads on the last segments and the presence of an anal cylinder. Accepting for
the moment the absence of branchiae as a characteristic feature of the genus Kesun , we have to point out dial other
features mendoned, such as die anal cylinder and die lack of epipodial pads in the last setigers are not unique to
abrianchiate members of die sub-family. The anal cylinder of K. fusus is very short and not really distinguishable
from diat of Travisia profundi and from many odier species of the genus. The absence of epipodial pads is also
not a unique feature either. This leaves only one unequivoqual difference between Travisia and Kesun : die
absence of branchiae in die latter. In a previous paper, BELLAN et al (1990) argued diat this character should not
be used at a generic level. The fact diat members of Kesun are limited to badiyo-abyssal depdis might be used as a
characteristic feature; however this present lime, we propose to discard Kesun and retain only a single genus,
Travisia. Hartman (1965a) had already proposed this synonymy. The definition of die genus corresponding to
diat of the sub-family Travisiinae widi a supplementary character: die presence of pustulae or similar structure on
the body.
The fact that remains only one genus Travisia in die Travisiinae should not change die status of this sub¬
family. In Bellan el al. (1990), die classification of the Opheliidae family was made using sequencing which
means dial the first taxa (Travisiinae) is die sister group of till following groups with a rooted tree by a theoric
ancestor (see Willey, 1981). This classification taking into account the level of apparition in the cladogram was:
Family Opheliidae
Sub-family Travisiinae
Sub-family Opheliinae
Sub-family Ophelininae
This classification regards die very strong differenciation between die Travisiinae and the group Opheliinae +
Ophelininae, and respect the classical use of die three sub-families. In die present slate of the knowledge, it is not
possible to state on the filiation between die Opheliinae and Ophelininae.
ANALYSES OF TRAVISIINAE SPECIES
We have observed available types or specimens from 21 taxa. The examined specimens come from: 1) Natural
History Museum, London, 2) Smithsonian Institution, Washington, 3) Museum National d'Histoire Naturelle and
4) National History Museum of Los Angeles County. The numbers at the end of diese 21 species refer to the
museum where dicy are deposited. A lack of a number indicates that we did not see the specimen. Twenty-seven
species and diree sub-species are now retained. The alphabetical list of these taxa widi indication of the most
complete description available, die list of authors having cited the species, and dieir known geographical
distribution is given below:
• T. antarctica Hartman, 1967, pp. 139-140; Hartman, 1978. South Georgia, Antarctic, South Atlantic Ocean;
2,452-2,727 m. (2)
• T. arborifera Fauvel, 1932, pp. 191-193, fig. 33; Fauvel, 1953. Andaman sea, Gulf of Bengal; British Natural
History Museum Collection, 1 ex. off Burma coast, 35 m. Indian Ocean. 7-100 m. (1)
• T. brevis Moore, 1923, pp. 220-221; Berkeley & Berkeley, 1952, pp. 90-91, fig. 183; Banse &
Hobson, 1968; Hartman, 1969, pp. 343-344, 1 fig. Berkeley & Berkeley, 1942; Imajima, 1961, 1963, 1964;
Reish, 1965; Hartman, 1961, 1965b, 1969; Fauchald, 1972; Loi, 1980 ; Hobson, & Banse, 1981; Fauchald
& Hancock, 1981. Southern California, North-eastern Pacific, Bering Sea, Okhotsk Sea. 18-2,900 m. (2)
• T. carnea Verrill, 1873, pp. 508 & 604; EHLERS, 1887; PETTIBONE, 1954, pp. 296-298; Appy et al ., 1980.
According to Hobson & Banse, 1981, the designation of T. carnea by Berkeley, 1966, 1968 for British
172
J.C. DAUVIN & G. BELLAN
Columbia is incorrect; it is probably T. pupa. We have seen the holotype of T. parva Day, 1973 (p. 94, fig. 13), off
Beaufort, North Carolina. It has: 20 scligers, a posterior asetigerous segment, 19 pairs of branchiae, neither
parapodial lappets nor lateral crenulations. These characters are very similar of those of T. carnea Verrill, 1873,
and it is surprising that Day didn't compare his species with the Verrill's species which are found in the same area
and depth. We consider T. parva as a synonym of T. carnea. North-western Atlantic, Massachussets to long
Island, Arctic Alaska. 5-35 m. (2)
• T. chiloensis Kiikenthal, 1887, pp. 364-365, figs 1-3. Chiloe, South-eastern Pacific.
• T. c/iinensis Grube, 1869, p. 66; Augener, 1922, pp. 38-40. China Sea, North-western Pacific.
• T. concinna (Kinberg, 1866), p. 256; Kinberg, 1910, p. 66, plate 25, fig. 5; Hartman, 1948, pp. 113-1 14.
Algoa Bay, South Africa, 5-20 m.
• T. doellojuradoi Rioja, 1944, pp. 135-136, figs 57-59; Rioja, 1946. Argentina coasts, South-western Atlantic.
115 m.
• T. elongata Grube, 1866, p. 66; EHLERS, 1901, p. 171, plate 22, figs 11-14. AUGENER, 1922, p. 34. Iquique,
Perou, South-eastern Pacific.
• T.foetida Hartman, 1969, pp. 344-345, three figures; Fauchald, 1972, pp. 237-238, plate 49, fig. d; Fauchald
& Hancock, 1981; Moore, 1923, Hartman, 1963, 1965b, 1966a as T. pupa. Redondo Canyon, California,
North-eastern Pacific. 250-3,100 m. (4)
• T. forbesii Johnston, 1840, pp. 373-374, plate 19, figs 11-18; Rathke, 1843, pp. 192-194, plate 10, figs 9-12. de
Saint Joseph, 1898; McIntosh, 1908a, b; Fauvel, 1914, 1925; Annekova, 1937, 1938; Berkeley &
Berkeley, 1942; Stop-Bowitz, 1945, 1948; Wesenberg-Lund, 1950, 1951; Pettibone, 1956; Chlebovitsch,
1961; Day, 1961, 1967; Eliason, 1962; Hartman, 1965a; Hamond, 1966; Cabioch et al., 1968; RetiEre,
1968; GlEmarec, 1969; Kirkegaard. 1969; AMOUREUX, 1971; Levenstein, 1966, 1971/72; WOLFE, 1973;
Averincev, 1977; Holthe, 1977; Hobson, & Banse, 1981. According to Stop-Bowitz (1948) and as Eulers
(1897), the designation of T. forbesii from the coasts of Chile and Antarctic is doubtful. T. forbesii is characteristic
of the northern hemisphere where it is collected to 300 m (Levenstein, 1971/72). One specimen of T.forbesi
with 28 setigers from False Bay, South Africa, is in the collection of die Natural History Museum of London. We
confirm the presence of the species in South Africa. Arctic, Circumpolar: Novaya Zemlya, Davis Strait,
Spitsbergen, Kara sea, Alaska and Canadian Arctic, North-east America, Siberia, Bering sea to Washington
Sound. North Japan Sea, West and east Greenland, Iceland, Faroes, Norway. North sea, western Baltic, Great
Britain, France: off the mouth of the Amazonc, Brazil, South Africa. 0-3,000 m. (1, 3)
• T. forbesii intermedia (Annenkova, 1937), p. 177; Uschakov, 1955; Buzhinskaya, 1985. According to
Buzhinskaya (1985), we have considered T. kerguelensis McIntosh subsp. intermedia Annekova, 1937 as a T.
forbesi subsp. intermedia (Annekova, 1937). Japon Sea, North-western Pacific. 30 m to abyssal.
• T. fusiformis Kudenov, 1975, pp. 215-218, figs 17-23. Gulf of California. Mexico, North-eastern Pacific.
Intertidal. (4)
• T. fusus (Chamberlin, 1919), p. 386. plate 67, fig. 5 and plate 68, figs 1-2; LEVENSTEIN, 1970, 1971/72. Pacific
Ocean. 3,000-7,580 m. (2)
• T. gigas Hartman, 1938, p. 103, figs 46-48; Hartman, 1961, 1963; Berkeley & Berkeley, 1941, 1962;
BERKELEY, 1968; Reish, 1968: Hobson & Banse, 1981. California, North-eastern Pacific. 0-180 m. (2)
• T. glandulosa McIntosh, 1879, p. 506, figs. 15-16. We have seen the only known specimen of T. glandulosa. It
was found in North-western Atlantic at 3,300 in. It has: 7 mm length, no visible branchiae, a very distinct lateral
groove at the last setigers, pustulae in a row by annulus. These characters are very similar to those of Kesun
abyssorum Monro, 1930. Even if T. glandulosa was rather poorly described by MdNTOSH, it does not seem that
Monro compare his specimen with McIntosh's species. Considering the similarity of Kesun abyssorum Monro,
1930 with Travisia glandulosa McIntosh, 1879, we propose the synonymy of the two species. Monro, 1930, p.
167, fig. 69 8 8; Kirkegaard. 1956, p.71, fig. 10; Hartman, 1966b, p. 51: Monro, 1939; Augener, 1932;
Hartman, 1967; Levenstein, 1961a, 1961c, 1971/72, 1975, 1978; Averincev, 1974; Rozbaczylo, 1985.
Pacific Ocean, Antarctic Ocean, Atlantic Ocean. 193-6,850 m. ( 1)
• I granulata Moore, 1923. pp. 219-220; Hartman, 1938, 1961, 1969; Loi. 1980. Southern California, North¬
eastern Pacific. 45-105 m. (2)
• I gravieri (McIntosh, 1908a), pp. 383-384; McIntosh, 1915, pp 29-30, plate 95, fig. 8; Hartman, 1965a, pp.
191-192; Hartman & Fauchald, 1971: Levenstein, 1971/72; Amoureux, 1982; Kirkegaard, 1980. Atlantic
Ocean. 539-7,800 m. (1)
• T. hobsonae Santos, 1977, pp. 559-564, fig. 1; Uebelacker, 1984, pp. 17-4, 17-5, figs 17-1, 17-2. Gulf of
Mexico, North-western Atlantic. 10-110 m. (2)
Source :
SYSTEM ATICS. ECOLOGY. BIOGEOGRAPHY IN TRAVISHNAE
173
• 7. Iiorsti Caullery, 1944, pp. 47-48, fig. 40. Java Sea, Pacific. 959 m.
• 7. japonica Fujiwara, 1933, pp. 91-103, plate I, figs 1-8, plate II, figs. 1-6: Monro, 1934, pp. 373-374, fig. 8 as
T. chinensis Grube, 1869 according to Hartman, 1959; FAUVEL, 1936, pp. 75-78. Fauvel, 1933: USCHAKOV,
1955; Imajima & Hartman, 1964, Berkeley, 1966: Uchida. 1967; Hobson & Banse, 1981; Fournier &
LEVINGS, 1982: Buzhinskaya, 1985. Japan Sea, NorUi-western Pacific. 10-105 m. (1, 3)
• 7. kerguelensis McIntosh, 1885, pp. 357-359, plate 43, fig. 10, plate 36A, figs 1-2: Ehlers, 1897, pp. 97-98,
plate 6, figs. 159-161: Augf.ner. 1922, pp. 36-37; Hartman, 1966b, p. 54. plate 17, figs 4-5; Averincev, 1982
p. 34. plate 5. figs 12-14; EHLERS, 1901, 1908, 1912: AUGENER, 1923, 1932; MONRO, 1930, 1936, 1939; Fauveu
1941; Rioja, 1944, 1946; Hartman 1953. 1967, 1978: Knox, 1962; Averincev, 1974; Day & Hutchings,
1979; Rozbaczylo, 1985; Hartmann-Schroder, 1986; Hartmann-Schroder & Rosenfeldt, 1989.
Kerguelen, Southern Indian, Southern Atlantic, Antarctic Ocean. 0-1,837 m. (1, 3)
•7’. kerguelensis gravieri Monro, 1930, p. 167, fig. 68: Hartman, 1966b; Hartmann-SchrOder &
Rosenfeldt, 1989. Palmer Archipelo, Antarctic Ocean. 259-315 m. (1)
• 7. lilhopliila Kinberg, 1866, p. 256; Augener, 1922, pp. 32-33; Hartman, 1966b, p. 54, plate 17, figs 7-10.
HUTCHINGS & Murray, 1984, p. 79; Hartman, 1952. Australia, South-western Pacific. 20-180 m.
• T. nigrocincta (Ehlers, 1913), p. 525; Hartman, 1966b, 1967. South Pacific, Antarctic. 2,725 m.
• 7. olens Ehlers, 1897, p. 98-99, plate 6, figs 162-163; Augener, 1922, pp. 35-36; Ehlers, 1901, 1912; Monro,
1930: Augener, 1932; Benham, 1950; Hartman, 1966b. 1967; Day & Hutchings, 1979. Hartmann-
Schroder & Hartmann, 1980; Rozbaczylo, 1985. One ex. Discovery st 939, 08/18/1932, 35°49'6S-173°27'E,
87 m. The designation of 7. olens by Fauvel, 1943 from California was probably incorrect, Hartman, 1969 did
not cite the species from California. It may be T. granulate i. Cape Horn. Scotia Sea, South-western Atlantic,
Antarctic, New Zealand, South-eastern Pacific. 0-1,120 m. (i)
• 7 olens Ehlers novae zealandiae Benham, 1927, pp. 12.3-128, plate 2, figs 70-72. Ehlers. 1897, 1907, 1912 as
T olens ; Benham, 1950, Day & Hutchings, 1979. British Natural History Museum Collection: 9 ex. from
Portobello. South Island, New Zealand. New Zealand, South-western Pacific. 0-20 m. (1)
• 7. oregonensis Fauchald & Hancock. 1981, p. 19. Offshore Oregon, North-eastern Pacific. 1,600-1.800 m. (4)
• T. profundi Chamberlin, 1919, pp. 387-389. plate 67, figs 1-4; USCHAKOV, 1955; Kirkegaard, 1956;
LEVENSTEIN, 1960, 1961a. b, 1966, 1970, 1971/72, 1975, 1978: Hartman, 1967. Atlantic (Angola) and Pacific
Ocean (Mid Bassin), Antarctic Ocean. 975-7,290 m. (2)
• T. pupa Moore, 1906, pp. 228-230, plate 11, fig. 29; Treadwell, 1914; Uschakov, 1955; Lf.venstein, 1960,
1961b, 1966, 1971/72; Hartman, 1961; Berkeley, 1966, 1968: Berkeley & Berkeley, 1942, 1952; Hobson
& Banse, 1981. Nordi eastern Pacific. 33-3,012 m. (2)
DISCUSSION OF THE MORPHOLOGICAL CHARACTERS
The shared characters of all species of Travisia include the presence of nuchal organs and interramal sense
organs; the capillary setae are often hispid and all species lack eyes. Characters used to distinguish the species
include the presence of lobes or papillae on the pygidium, the position of the nephridiophores and the total
number of setigers present. Few characters are unique to a single taxon. The body-shape is more variable, more or
less fusiform or grub-shaped, but the shape may vary with the numbers of segments present and with the quality of
fixation. The prostomium is pointed in all species, except in 7. foetida, which is truncate. Lateral and mid-ventral
grooves are generally absent; the development of these grooves characterize die different sub-families, however
Uiey are present, but poorly developed in some taxa. For example, a short lateral groove is present in I
glandulosa and a mid-ventral one in 7. fusiformis, T. gravieri and T. hobsonae. Branchiae are present except in the
species being transferred from Kesun: 7. fusus, T. glandulosa, T. gravieri, and 7. nigrocincta. The branchiae are
cirriform except in T. arborifera which has branching branchiae. They are present from setiger 2, except in T.
hobsonae, sometimes in T. cornea, and T. profundi where they arc present from setiger 3. Unusual lobes or
papillae are present on (he pygidium in T. japonica, T. gigas, 7. kerguenlensis gravieri. Nephridiopores arc
present on setigers 3-14 except in T. brevis (7-25), T. chiloensis (7-14?), 7. japonica (1 1-14 in die original
description but 3-14 in Fauvel, 1933). The number (n) of setigers is relatively stable in a given species (n ± 5)
except in 7. granulata 32-50, 7. japonica 32-39 and 7. litltopliila 44-53. It would be interesting to study die actual
significance of diis variability as a possible character at die specific level.
A last point, is die variability of the degree of papillation in the posterior segments as described in 7.
kerguelensis by Monro (1930). Some difficulties remain in ascertaining the identity of four similar taxa, all
174
J.C. DAUVIN & G. BELL AN
described from southern oceans. They were distinguished on the number of segments and the papillation: T.
kerguelensis (23-27 segments), T. kerguelensis gravieri (25), T. olens (29-36), and T. olens novae zealandiae (38-
40).
PRELIMINARY KEY TO THE TRAVISIINAE
A preliminary key of the species Travisia is presented which is provisional due to the difficulties in correctly
interpreting die available descriptions, some of which are incomplete. The need of a phenetic and phylogenetic
study is necessary in order to test die validity of characters. Before, diis can be done, it is necessary to have a
complete redescription for all species. The following characters must be accurately described in all species:
- color and shape of live specimen;
- presence, shape, and variability of posterior lateral crenuladons and parapodial lappets;
- number and variability of number of segments and setigers;
- number of branchiae;
- distribution of pustulae on die body;
- shape of die pygidium and pygidial papillae.
1 Branchiae absent .
Branchiae present .
2 Lateral groove in the last 10 segments
Lateral groove absent .
3 Body grub-shaped, < 25 segments, mid-ventral groove present, very short setae . 7'. gravieri
Body fusiform, > 25 segments, fascicles of distinguished setae . 4
4 Segment number 28, > 25 setigers . T.fusus
Segment number 25, 17 setigers . 7- nigrocincta
5 Prostomium truncated, 31 setigers, large species . T.foetida
Prostomium pointed conical . 6
6 Branchiae branched . T. arborifera
Branchiae cirri form . 7
7 Mid- ventral groove present . 8
Mid-ventral groove absent . ®
8 Mid-ventral groove slightly developed, 30-31 setigers, parapodial lappets developed ..I hobsonae
Mid-ventral groove and parapodial lappets well developed, 34-35 setigers . T.fusiformis
9 Segment number > 40 . 10
Segment number <40 . 13
10 Posterior parapodia with lobes or lappets . 11
Posterior parapodia without lobes or lappets . 12
1 1 Posterior parapodia with triangular lappets, pygidium collarlike with 6 long
dorsal papillae, length about 10 cm . I gigas
Posterior parapodia with small lappets, knob pygidium, length about 3 cm . T. elongata
12 Epithelium with large, dorsal and ventral coarse pustules, setiger number to
about 45, pygidium with 12-13 irregular papillae . T. granulata
Epithelium finely reticulated, from 44 to 53 setigers, pygidium with 7 cirri . I lithophila
13 Segment number > 30 . 14
Segment number < 30 . 1 8
14 Posterior lappets absent, 26-45 setigers . T granulata
. 2
. 5
T. glandulosa
. . . 3
Source
SYSTEMATJCS, ECOLOGY. BIOGEOGRAPHY IN TRAVISDNAE
175
Posterior lappets and lateral crenulations developed . 15
15 Pygidium widi an oval ventral lobe and 6 laterodorsal palpi . 16
Pygidium shape otherwise . 17
16 Laterodorsal palpi well developed, segment number 32-39, 26-32 branchiae pairs T. japonica
Segment number 35, 33 pairs of branchiae . T. concinna
17 Segment number 29-32 . j 0[ens
Segment number 38-40 . j. olens novae
zealandia
18 Setigers number = 18, 23 segments . T. orogenensis
Setigers number > 20 . 19
19 Parapodial lappets reduced or absent . 20
Parapodial lappets present . 23
20 Setigers number > 20, 25-29 segments, pygidium small, longitudinally furrowed . I cornea
Setigers number > 25 . 21
21 Numbers of branchiae pairs 9-12, 26 setigers and 25-27 segments . I profundi
Numbers of branchiae > 15 . 22
22 Segments number 30-32, 25-28 setigers, 22-25 pairs of branchiae number . T. pupa
Segments number < 30, about 25 setigers, 17-21 pairs of branchiae, anal
cylinder surrounded by a circlet of short papillae . T antarctica
23 Body pigmented in red purple, 17 pairs of branchiae . T. doellojuradoi
Body not pigmented in red purple, > 18 pairs of branchiae . . . 24
24 2 posterior achaetous segments . 25
3-5 posterior achaetous segments . 28
25 Parapodial lappets well developed, posterior part of die body finishing truncated . 26
Parapodial lappets little developed, posterior part of the body tapered to die pygidium . 27
26 Lateral lappets well developed, pygidium cylindrical . T. kerguelensis
Laterals lappets absent a pair of dorsal anal cirri at die end of die anal cylinder . I kerguelensis gravieri
27 Sedgers number 23-26, posterior margin of abdominal segment smoodi,
not scalloped, pygidium ovoid . T. forbesii
Setigers number 26-29, posterior margin of abdominal ondulate or serrulate,
pygidium cylindrical . T. forbesii intermedia
28 Parapodial lappets Iitde developed, pygidial knob pigmented, 23 setigers,
28 segments . j horsti
Parapodial lappets developed, pygidium not pigmented . 29
29 Branchiae number > 20, 27 segments, 24 setigers . T. chiloensis
Branchiae number < 20, 29 segments . 30
30 Sedgers number 23-25 . T. brevis
Sedgers number 27 . T. chinensis
BIOGEOGRAPHICAL DISTRIBUTION
Table 1 summarizes available data of species distribution. Only two species occur in Arctic Ocean; Antarctic
Ocean is richer widi eight taxa. I antarctica is present in die far-south (Soudi Georgia) of die Atlantic Ocean. Ten
species are present in die Atlantic Ocean, two of which are restricted to die northern part, five to die soudiern part
176
J.C. DAUVIN & G. BE LI -AN
and three have an extended distribution. Twenty-one taxa are present in die Pacit.c Ocean, 13 are restricted to the
north with T arborifera found in the Gulf of Bengal which is the single species collected in the Indian Ocean. Six
species arc known to be only from the south Pacific Ocean. Eight species have a large biogeograph.cal
distribution: T. glandulosa. T. forbesi, T. Jusus, T. gravieri. T. japonic". T. kerguelensis. T. olens. and 7. profundi.
Table 1. — Biogeographical distribution of Travisia species from the world's oceans.
BATHYMETRIC DISTRIBUTION
Three species T. chiloensis, T. chinensis and T. elongata were described without indication of original depth,
and were probably littoral species. Among the odier 27 taxa, 16 are present in the bathyal and/or the abyssal
depths and 10 are exclusively badiyo-abyssal (Fig. 1). Eighteen species are found on die continental shelf among
which only five species are collected at depths less dian 100 m.
Source : MNHN. Paris
SYSTEM ATICS, ECOLOGY, BIOGEOGRAPHY IN TRAVISHNAE
177
Depth in m
100 1000 10 000
FIG. 1. — Bathymetric distribution of Travisia species from the world’s oceans.
Source : MNHN, Paris
178
J.C. DAUVIN & G. BELLAN
ECOLOGICAL AND BIOLOGICAL DISTRIBUTION
The data on the ecology of the species are rarely reported and therefore die ecological and biological data are
incomplete. Most of the deeper species are found in bathyal and abyssal mud. The littoral species are found
especially in muddy and fine sand. T. foetida inhabits essentially clean sands in low intertidal and in die upper part
of die subtidal. However, this species has been found also in many different types of soft-bottom subsuates. Due
to its widespread distribution bodi geographical and badiymetric, I forbesii appears to be ubiquitous. This
ubiquity may be the result of die presence of a complex of species. The principally northern species T.forbesi may
have a counterpart in the southern hemisphere widi T. kerguelensis and I olens and their sub-species.
Travisia are considered non-selective deposit-feeders. In the intertidal sand at Tampa Bay, Florida, specimens
of Travisia hobsonae had only sand particles in dieir gut widi no particles finer than 100 pm ; grains as large as
475 pm were removed with a median size of 230 pm (Dauer, 1980). The low level of food specialization in
adults contrasts sharply widi die high level of precision in the selection of substrata by juveniles (RETitRE, 1971,
1972).
Travisia forbesi lives 3.5 years at Dinard (English Channel); die spawning occurs at die end of die autumn and
during die winter; development is direct without larval dispersion (RETlfeRE, 1971, 1972). T. hobsonae reproduces
the year round in Tampa Bay (DAUER, 1980); its densities could reach an annual average of 1,100 nr2 at certain
stations.
DISCUSSION
This paper is a first step toward the study of Travisiinae and to die knowledge of the Opheliidae family. The
sub-family Travisiinae is die most plesiomorph (BELLAN et al., 1990) and is well defined in relation to the two
odier sub-families. This paper proposes to bring together all the species of this sub-family into the one genus
Travisia Johnston, 1840. The examination of available types has allowed us to place into synonymy Kesun
abyssorum Monro, 1930 with Travisia glandulosa McIntosh, 1879, and T. parva Day, 1973 widi T carnea
Verrill, 1873. Five species T. chiloensis, T. chinensis, T. concinna, T. elongata and T. horsti which have not (or
rarely) been found since dieir descripdon, remain doubtful and must be re-examined. Many characters should be
used in defining each species: color and shape of live specimens; presence, shape, and variability of posterior
lateral crenulations and parapodial lappets; number and variability of number of segments and setigers; number of
branchiae; distribution of pustulae on die body; shape of die pygidium and pygidial papillae. The variability of die
number of setigers, segments, and branchiae must be defined using a large number of specimens of each species.
This work would allowed in a further step to study the phenetic and the phylogenetic relationship between the
species. However, genetical studies must be established: 1) the real extended distribution of T. forbesii and
T. forbesii intermedia (nordiern species) ; 1\ forbesii may be a complex widi slight morphological differences; 2)
the genetical distance and variability of die southern species and their sub-species: T. kerguelensis, T. kerguelensis
gravieri, T olens and T. olens novae zealandiae. These four taxa are distinguishable essentially by die number of
segments and setigers, so they show a continuum between T. kerguelensis widi a number of segments which could
be reduced to 23 and T. olens novae zealandiae which a number of segments reaching 40. T. kerguelensis is
known to show a great variability of papillaUon in the posterior segments (MONRO, 1930).
It is clear diat the data on ecological and biological features are insufficient. Biological data are limited to T.
forbesii and T. hobsonae . Such studies must be extended to other species and populations. In the past few years
several works on Ophelia , such as diose of Riser (1987) and Harris (1991) have demonstrated that biological
(type of development) and ecological data (habitat) could be good criteria to ascertain on the validity of a
particular species in this family.
Travisia is typically a deep water Pacific genus. Badiymetric distributions of Travisia and Ophelia (BELLAN &
Dauvin, 1991) show that Ophelia occurs preferentially in shallow waters and in the Atlantic whereas Travisia
species dominate in the bathyal and abyssal depdis in the Pacific. This indicates diat die speciation of these two
genera could be parallel. In Ampeliscidae (Amphipoda), another marine diversified family, Dauvin & Bellan-
Santini (1990) have also distinguished two distribution schemes widi Ampelisca in shallow water and Haploops
in continental and badiyal depths.
New data are need before elucidating die evolution of the genus. Future works and prospects on Travisia
genus, but also on other genera of Opheliidae may reveal correlations between species, phyletic, bathymetric and
biogeographic features.
Source :
SYSTEM ATICS. ECOLOGY. BIOGEOGR API 1Y IN TRAVISDNAE
179
ACKNOWLEDGEMENTS
1'lie authors would like lo thank their colleagues for lending types and specimens deposited in die collections.
Dr Alex MUIR, Natural History Museum, London, Drs K. Fauchald and L. Ward, Smithsonian Institution,
Washington, L.H. Harris, Natural History Museum of Los Angeles County, Dr Fauchald also for his remarks
on die Travisiinae. Dr Alex Muir was particularly hepl'ul during the visit in London of J.C. Dauvin, which was
made possible by a grant from the M.N.II.N. (Bonus Quality Recherche, Musdum 1991, M31). They also wish to
diank P. CiILLET for access to the library of the Cadiolic University of Angers, A.B. Davies, Emory Univ.,
Atlanta, GA, for her help in correcting die manuscript, and D. Reish and K. Fauchald for dieir very constructive
suggestions on die first draft.
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Source ;
19
A new Species of Ophryotrocha
(Polychaeta, Dorvilleidae) associated with Ice Scours
in the Canadian Arctic Archipelago
Judith A. FOURNIER & Kathleen E. CONLAN
Invertebrate Zoology. Collections and Research Division
Canadian Museum of Nature/M usee canadien de la nature.
C.P./P. O. Box 3443. Station/Succ. “D”
Ottawa. Ontario Canada. KIP 6P4
ABSTRACT
Ophryotrocha spatula sp. n. is described from ice scours off Cornwallis Island in the Canadian Arctic Archipelago. This
species resembles O. scarlatoi Averincev. 1989 in having the last 5-12 setigers laterally prolonged into a broad, lobulate flange
but dillers 1mm this species in the structure of the jaw apparatus and setae and in possessing ventral parapodial cirri and a
median anal cirrus.
RESUME
Une nouvclle espece d' Ophryotrocha (Polychcte, Dorvilleidae) associec aux sillons d'icebergs dans I'Archipel
arcti(|iie canadien
L.e polychcte Ophryotrocha spatula sp. n. en provenance dc sillons d'icebergs pres de Cornwallis Island dans I'Archipel
arctiquc canadien est decrit. Cette espece resscmble a O. scarlatoi Averincev 1989. par ses bords dorsaux des 5-12 setigercs
posterieurs elargis en forme de lobe membraneux, mais el le s'en distingue par les soies, la forme des machoires. et la presence
de cirres ventraux paiapodiaux et un ciire median anal.
INTRODUCTION
A joint Canadian/Unitcd Stales team has been studying scour formations caused by grounded multi-year ice
off the coast of Cornwallis Island, Northwest Territories in the Canadian Arctic Archipelago (Queen Elizabeth
Islands). Icescouring is probably the most disruptive and widespread physical disturbance to marine bottom
communities in polar waters. In the Arctic, pressure ridges of ice scour the sea floor to depths of 60 m and larger
icebergs ground as deep as 750 m (Lewis & Blasco, 1990). The team has been investigating the
FOURNIER. J. A. & K.E. CONLAN. 1994. — A New Species of Ophtyotrocha (Polychacia. Dorvilleidae) associated with Ice
Scours in the Canadian Arctic Archipelago. In: J.-C. DaUVIN. L. LaUBIER & D.J. REISH (Eds). Actes de la 4eme Conference
internationale des Polycheles. Mem. Mus. natn. Hist. nat.. 162 : 185-190. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
186
J. A. FOURNIER & K. E. CONLAN
benthic population and community responses to ice scour, documenting the successional stages of biotic recovery
in order to determine whether widespread patterns of zonation and larger spatial and temporal community mosaics
are correlated to the disturbance.
An undescribed dorvilleid of the genus Ophryotrocha was among the most abundant polychaete species and
showed a strong positive association with the disturbed sediments of the ice scours and berms. Mature specimens
of this species have the dorsal surface of die last 5-9 segments laterally prolonged into a lobulated spoon-shaped
flange. The species resembles Ophryotrocha scalatoi Averincev, 1989 from Franz-Joseph Land and Norway
(OUG, pers. comm.) but differs in details of jaw dentition and the presence of ventral parapodial cirri, most
noticeable in die posterior segments.
METHODS
Samples were collected by Hunter S. LENIHAN and Kathleen E. Conlan using diver-operated hand cores
pressed into the sediment. Six cores were collected from locations inside and outside each scour and from the
scour berm itself for a total of 18 samples from each of four scours. The 72 samples yielded a total of 551
specimens of the new species.
Samples were screened through a 0.5 mm mesh, fixed in 4 % formaldehyde solution and later transferred to
70 % ethanol. Final sorting was done in die laboratory under a dissection microscope. Specimens were examined
under dissection and phase-contrast compound microscopes. Drawings were done with a drawing tube. Ocular
micrometers in both compound and dissecting microscopes were used for measurements. Body width
measurements do not include parapodia.
DESCRIPTION OF COLLECTION SITES
Ice Scour 1 : Cape Martyr, Cornwallis Island, 74°4F N, 95°06' W, depdi 15 m; outside scour (one specimen),
scour berm (18 specimens), inside scour (27 specimens) sampled 31 July 1991. Outside of scour had gravel/cobble
substrate over silt, little Laminaria cover, exposed to frequent strong currents. Scour was perpendicular to
shoreline, 3-4 m wide, 1.5-2 m deep into sediment, more than 40 m long, estimated age less than one year,
probably produced during spring breakup of ice. Sediment inside scour loose and very soft, 4-5 cm oxic layer
covering grey anoxic zone. Scour berm with 7-8 mm oxic layer covering sediment. Epifauna outside scour
comprised very abundant echinoderms (ophiuroids, echinoids, asteroids, holothuroids), bivalves (Mya iruncata L.,
Serripes groenlandicus (Brugui£re), Astarte borealis (Schumacher)) and soft corals (Gersemia sp.).
Ice Scour 2: Assistance Bay, Cornwallis Island, 74°39' N, 94° 18' W, depth 7 m; outside (31 specimens), scour
berm (157 specimens) and inside (94 specimens) sampled 2 August 1991. Scour parallel to shore line in semi-
protected bay, well Hushed by strong currents and river flow. Scour estimated to have formed within previous 24
hours, about 6 m wide, 0.5 m deep and over 50 m long. Scour bottom hard with very little loose sediment over
large cobbles. Scour berm 5-10 cm high with stones and cobble. No epifauna visible within scour.
Ice Scour 3 : Resolute Bay, Cornwallis Island, 74°4F N, 94°50' W, depth 10 m; outside scour (zero specimens)
sampled August 4, 1991, scour berm (125 specimens) and inside (44 specimens) 8 August 1991. Circular "crater"
in area of 40-60 % Laminaria cover, estimated to have formed in previous 48 hours, more than 25 m in diameter,
0.25 m deep to hardpan. Berm 2-2.5 m high.
Ice Scour 4: Resolute Bay, Cornwallis Island, 74°41' N, 94°50' W, depth 7 m; outside (1 specimen) scour berm
(51 specimens), and inside (two specimens), 8 August 1991. Scour estimated to have formed within previous 48
hours, about 30 m long, 3 m wide, cut to hardpan, 0.25 m deep. Berm about 1 m high, loose sediment with stones
and gravel. Pockets of anoxic sediment along length of trough. Only a few Buccinum sp. seen within scour, Mya
spp. and Macoma spp. on berm.
Resolute Bay is protected by a sill at the entrance. Bottom was fine sediment and cobble, about 20 cm deep,
over a hardpan base that prevented bivalves such as Mya spp. and Serripes groenlandicus from burrowing deeper.
Scours 3 and 4 were in the central pan of the bay, close to shore, in an area of dense Laminaria cover.
Source :
NF.W SPECIES OF OPHRYOTROCHA FROM ARCTIC CANADIAN ARCHIPELAGO
187
SYSTEMATICS
Ophryotrocha spatula n. sp.
Material Examined. — Holotype: CMN A 1993-0046, mature specimen, 3.7 mm long, 0.5 mm wide anteriorly,
flange 0.8 mm across at widest point. Type Locality: Assistance Bay, Cornwallis Island. Ice Scour 2, Core 2, scour
berm, 7 m depth, collected 2 August 1991.
Paratypes: CMN A 1992-0 158, 79 specimens, remainder of sample from scour berm, core 2, Ice Scour 2
Assistance Bay, Cornwallis Island.
An additional 471 specimens have been found in the rest of the samples (Table 1).
05 mo
Fig. 1. — a. Ophryotrocha spatula sp. n., dorsal view, holotype. most setae omitted, b. Paratype, ventral view, posterior, c.
Paratype. anterior view of median parapodium. d. Posterior view of posterior parapodium. setae omitted except for ventral
simple seta. e. f. Long and short blades of compound falcigers. g. Ventral simple seta. h. Tip of simple seta.
188
J. A. FOUR NI HR & K. H. CON LAN
SPECIES DIAGNOSIS. — Medium-sized Ophryotrocha , 3.7 to 5.5 mm long for 25-43 setigcrs, anterior body width
about 0.5 mm, dorsum of posterior 5-12 segments laterally expanded into a lobulatc flange (Fig. la). Prostomium
with 1 pair each palps and antennae, ovate. Single pair of small eyes usually visible on posterior margin of
prostomium. Jaw apparatus (Fig. 2) darkly sclerotized. mandibles rod-like with toothed, bifid anterior margin,
forceps P-type. inner edge with one row of about 10 large teeth interspersed with smaller ones and secondary ridge
with many fine teeth. Free denticles seven pairs in two groups. Parapodia with both dorsal and ventral cirri, former
difficult to discern in anterior parapodia. Supra-acicular setae simple unidentate blades with very finely serrated
edges. Sub-acicular setae compound, unidentate blades with very finely serrated edges, varying in length by factor
of two. Pygidium flattened, anal cirri ovate, inserted ventrally. Anus ventral or terminal depending on state of
dilation, bearing mid-ventral papilla.
DESCRIPTION ofholotype. — Holotype (Fig. la) 3.7 mm long for 32 setigers, body width 0.5 mm anteriorly,
0.8 mm at widest point of posterior flange. Colour in alcohol off-white. Body sparsely ciliated but setigcrous
segments have extensive glandular regions covering dorsum.
Prostomium rounded, bearing two small ovate antennae dorsally and pair of ventral palps almost identical in
size and shape. Fycs not visible.
Fig. 2. — Ophryotrocha spatula sp. n., jaw apparatus from paratype. a. Mandibles, b. Forceps (base broken), c. d. c. First
group of free denticles, f. g. h. i. second group of free denticles.
Peristomium followed by achactous apparent first segment. Mouth parts (Fig. 2) darkly sclerotized. Forceps
and free denticles forming separate group. Mandibles (l;ig. 2a) partially protruding, rod-shaped with jagged bifid
Source : MNHN. Paris
Ni:w SPECIES OF OPHRYOTROCHA I ROM ARCTIC CANADIAN ARCHIPELAGO
189
leading edge and several unpaired, irregular protrusions along length of shaft. Forceps (Fig. 2b) P-type (IIilbig &
Blake, 1991) with single main tooth, inner edge with row of about 10 large teeth interspersed with at least 20
smaller ones, secondary median ridge bearing row of much finer teeth: main shaft darkly sclerotized but
surrounded by thin flange.
Free denticles, seven pairs arranged in two primary groups (Fig. 2c-i). Denticles closest to the forceps (Fig. 2c-
c) dark and strongly toothed; median member (Fig 2c) fang-shaped. Outer denticles (Fig. 2f-i) thin and broad with
numerous long slender teeth interspersed with several stouter ones.
Parapodia uniform in shape; setae vary only in number. Dorsal and ventral cirri ovate but latter very difficult to
distinguish in anterior setigers. Presctal lobe truncate. Dorsal postsetal lobe rounded; ventral, retractile lobe
triangular and supported by single simple seta that resembles secondary emergent acicula (Fig. lc-d). Aciculae
very long and stout, seated proximally against row of longitudinal muscle group. Supra-acicular setae simple,
unidentate flattened blades with very finely denticulate lower margin (Fig. 1, c-g-h). Second superior seta longer
than others. Subacicular setae compound falcigers with blades varying in length by factor of two. unidentate with
very finely denticulate border, almost identical to supra-acicular setae in size and form.
Setiger 1 with one supra-acicular seta, three compound falcigers and one subacicular simple ventral seta.
Following setigers with four supra-acicular setae, six compound falcigers and one ventral simple seta. Last setiger
with two simple supra-aciculars, two compound falcigers and one ventral seta. Large specimens have more setae
per bundle but pattern invariable.
Last 9 setigers expanded into broad, spatulate flange (Fig. la), free from dorsal cirri which project freely from
below flange. (Fig. Ih).
Pygidium flattened with two ovate anal cirri inserted ventrally (Fig. lb). Anus ventral with opening occupying
ventral surface of last three setigers; stout ventral median papilla.
OTHER SPECIMENS. — Mature specimens reach 5.5 mm with 25 to 43 setigers. No direct linear relationship found
between body length and number ol setigers. Many specimens with adhering sand grains and fine clay particles.
While all were oil -white in colour, a few of the largest specimens had yellowish-brown tinge. Most specimens
have single pair of small eyes on posterior margin of the prostomium, usually covered by part of peristomium.
Posterior flange often curled dorsally, forming a cylinder. Some of largest specimens show little expansion, other
smaller ones, such as the holotype, almost double body width. Not all specimens have anal opening as extended as
holotype; it is sometimes contricted and terminal as illustrated in Figure lb.
No gametes found in the holotype or any of the other specimens examined, including the largest. A few
juveniles, about 2 mm long for 20 setigers, are present in the samples but all appear to be damaged. The jaw
apparatus shows obvious similarities to the adults but the posterior flange is not developed. Instead, the body
appears to terminate in an undifferentiated, asetigerous region. These specimens need more study.
Etymology. — The species name spatula is Latin for spoon ;uid refers to the diagnostic unique structure of die
posterior segments.
Comparison to other species of Ophryothrocha. — The extensive review of I Iilbig & Blake ( 199 1 ) provided
a table of characters of most of the known species in the genus but overlooked 0. scarlatoi Averincev, 1989 which
also has a broad posterior flange. This species was only superficially described and figured. Oug (in prep.) has
discovered several specimens from Norway that resemble 0. scarlatoi. These differ from the present specimens in
having longer mandibles, in details of the maxillae and setae, and in lacking ventral parapodial cirri and a median
anal papilla. It will be necessary to re-examine the types of O. scarlatoi in order to determine whether we are
dealing with one, two or three species or subspecies. Attempts to borrow the type specimens of O. scarlatoi have
been unsuccessful (E. OUG, pers. comm.).
The parapodia and setae of 0. spatula resemble those of 0. puerilis siberti (McIntosh, 1885) as illustrated by
GEORGE & Hartmann-Schroder and Hartmann-Schroder (1985). The parapodia are not as strongly lobed as
those of 0. lobifera Oug, 1978 but that species also has Upuerilis- type” setae. Although IIilbig & Blake (1991)
do not tabulate the presence/absence of anal cirri and papillae, there are species which lack anal cirri ( 0 .
paralabidion IIilbig & Blake, 1991; 0. sp. near scarlatoi Oug), species with cirri reduced to “thread-like”
appendages (0. bacci Parenti, 1961; 0. geryonicola (Esmark, 1874), species with the anus dorsal ( 0 . lobifera
Oug, 1978), and species with a ventral papilla as well as anal cirri (0. longidentata Josephson, 1975; 0. maculata
Akesson, 1973; 0. minuta Levi, 1954; 0. puerilis siberti (McIntosh, 1885)). It is possible that the presence of a
ventral papilla has been overlooked in other species.
190
J. A. FOURNIER & K. E. CONLAN
Fable 1 . — Distribution of Ophryotrocha spatula sp. n., pooled totals of six samples each collected from outside,
the berm and inside four different ice scours off Cornwallis Island, Canadian Arctic Archipelago.
DISTRIBUTION
Ophryotrocha spatula sp.n. is known only from the shallow waters of Barrow Strait off Cornwallis Island. It
shows a strong affinity for the disturbed sediments of ice scour berms or troughs as opposed to the compacted
sediment outside die scour (Table 1 ). It was much more abundant on fresh scours (2, 3, and 4) than the older scour
(1). Analysis of distribution against grain size (mean 0) failed to demonstrate a significant relationship (C = 0.255).
ACKNOWLEDGEMENTS
The authors arc grateful to Diana LAUBITZ, Collection Manager, Invertebrate Zoology for facilitating our
collaboration on diis project and for her constructive criticism of die manuscript. We thank Hunter LlNIHAN,
Brenda Konar, and staff of Moss Landing Marine Laboratories, California, and Buster Welch of die Department
of Fisheries and Oceans, Resolute Marine Laboratory for assistance in the field and laboratory Ed IlENDRYKS
helped widi specimen sorting. Francois GfiNIER, Michel GOSSELIN and Andrd Martf.l corrected the French title
and text.
REFERENCES
AVERINCEV. V.G., 1989. — Sczonnaya dinainika polikhet vysokoarkticheskikh pribrezhnykh ekosistem Zemli Frantsa-Iosifa
(Errantia). [Seasonal dynamics of polychaetes from the high Arctic coastal ecosytcm of Franz-Joseph Land (Errantia).]
Akadcmiya Nauk SSSR Apatity : 1-78. (in Russian).
George. J. D.. & G. IlARTMANN-SCHRODER, 1985. — Polychaetes: British Amphinomida, Spintherida and Eunicida. Synop.
Brit. Fauna (New Series), 32 : 1-221.
HILBIG, B. & J.A. Blake, 1991. — Dorvilleidae (Annelida: Polychaeta) from the U.S. Atlantic slope and rise. Description of
two new genera and 14 new species, with a generic revision of Ophryotrocha. Tool. Seri.. 20 (2) : 147-184.
Lewis. C.F.M.. & S.M. Blasco, 1990. — Character and distribution of sea-ice and iceberg scours : keynote address. / n :
J.I. Clark (ed). Workshop on ice scouring and the design of offshore pipelines , Calgary. Alberta, April 18-19, 1990.
Canada Oil and Gas Lands AdminisUation. Energy, Mines, and Resources Canada : 57-101.
Oug, E.. 1978. — New and lesser known Dorvilleidae (Annelida: Polychaeta) from Scandanavian and northeast American
waters. Sarsia . 63 : 285-303.
Source
20
Two new species of Branchiomma (Sabellidae) with
redescriptions of closely related species and comments
on Pseudobranchiomma and Scibellastarte
Phyllis KNIGHT-JONES
School of Biological Sciences
University of Wales
Swansea U.K.
ABSTRACT
Species of Branchiomma Kolliker (= Dasychone Sars) are reviewed briefly in order to describe two new species. B.
moebii from the Mediterranean and B. spongiarum from the Faroe Islands. Figures of Branchiomma infarction . B.
bahusicnse and B. arcticum (= Sabellastartc arctica) are given for comparison. SHM helps to show (a) specific differences
in uncini and (b) differences between the stylodes of Branchiomma and the "reduced stylodcs" of Pseudobranchiomma
Jones. Pseudobranchiomma should include some species formerly in the genera Branchiomma and Sabellastartc Kroyer.
RESUME
Deux nouvellcs especes de Branchiomma (Sabellidae) avec des redcscriptions des especes
voisines et dcs re marques sur Pseudobranchiomma et Sabellastarte
Les especes de Branchiomma Kolliker (= Dasychone Sars) sont passecs cn revue brievement pour d^crire deux especes
nouvelles. B. moebii de Mediterranee el B. spongiarum des Ties Feroe. Des figures des Branchiomma infarction. B.
bahusicnse et B. arcticum ( = Sabellastarte arctica) sont donnees pour comparison. L'observation au SEM permet de voir
a) les differences spScifiques entre les uncini et b) les differences entre les stylodes de Branchiomma et les "stylodes
reduits" de Pseudobranchiomma Jones. Pseudobranchiomma comprend quelques especes placees autrefois dans les genres
Branchiomma cl Sabellastarte Kroyer.
INTRODUCTION AND METHODS
Collections from the Mediterranean (Knight-Jones el al. , 1991) and the Faroes (Knight-Jones, 1993)
yielded several species of Branchiomma as diagnosed by Johansson (1927) and Fitzhijgh (1989). Most species
were difficult to name, as descriptions ;tre often inadequate and Johansson's review was partial. It was therefore
KNIGHT-JONES, P.. 1994. Two new species of Branchiomma (Sabellidae) with redescription of cloesely related
species and comments on Pseudobranchiomma and Sabellastarte. hr. J.-C. Dauvin, L. LAUBIER & D.J. Reish (Eds).
Actes de la 4eme Conference internationale des Polychetes. Mem. Mus. natn. Hist, nat .. 162 : 191-198 Paris ISBN 2-
85653-214-4.
192
P. KNIGHT- JONES
necessary to study types (or original material) of all known Brancliiomma species. It soon became clear that many
synonyms in the literature were incorrect. Two new species are compared here with those that are morphologically
most similar and B. bahusiense is figured for the first time. Some species arc close to Pseudobranc/iiomma Jones
(1962), so Pseudobranc/iiomma emersoni Jones was also studied and compared with Brancliiomma and
SabeUastane.
Material has not yet been found of species followed here by asterisks, but these were figured in the original
descriptions. All other listed species have been examined and will be compared elsewhere. Original citations of
most species listed here can be found in Hartman, 1959, under Brancliiomma , Dasychone, or Sabella.
Optical microscopy was helped by a Wild drawing attachment. For scanning electron microscopy (Knight-
Jones & Fordy, 1979) alcohol preserved material was washed in distilled water, placed in a weak cleaning
solution (Decon 75) in an ultrasonic bath for 20-30 sec, rinsed in distilled water, dehydrated in an acetone series,
coated in a polaron MK2 sputter coaler, and examined in a JEOL 35 C. Crown radioles were transferred before
coaling to a Polaron MK1 critical point drying unit using CO2 as the intermediate liquid. Fascicles of chaetae
were also studied by SFM but no specific differences in surface detail could be found.
OLD AND NEW SPECIES OF BRANCHIOMMA
Brancliiomma bombyx (Dalyell), B. lucullanum (delle Chiaje), B. violaceum (Schmarda), B. natalense
(Kinberg), B. capense (McIntosh) and B. pseudoviolaceum (Augener) have their dorsal collar margins fused to the
edges of the narrow faecal groove, but the two new species described here are like most Brancliiomma in having
free dorsal margins separated by a wide gap. Their uncinal crests have many rows of teeth, as in Brancliiomma
infarct urn (Kr0yer = Dasychone decora Sars), B. inconspicuum (Sars), B. bahusiense Johansson (as B. infarct a var.
bahusiensis ) and B. arcticum (Ditlevsen = Sabellastarte arctica Ditlevsen) with which they are compared.
The radioles of the new species lack the ‘macrostylodes’ (defined as being three or more times the length of
neighbouring pairs, see KNIGHT-JONES et al., 1991), which are seen in distal halves of dorsal mid lateral radioles
in B. nigromaculatum (Baird) (= Sabella crispa Kr0yer, = Dasychone ponce Treadwell), B. boholense (Grube),
B. bairdi (McIntosh), B.japonicum (McIntosh), B. conspersum (Fillers) (= ? Dasychonopsis arenosa Treadwell),
B. maculatum (Fischli)*, B. gravelyi (Aziz)*, B. loandense (Treadwell) and B. pererai de Silva (as B.cingulata
var. pererai) [some of the latter four species may be synonyms of the others]. Some species which lack distal
macrostylodes, e.g. B. Iiavaiicum (Kinberg), B. cingulatum (Grube), B. luctuosum (Grube), B. curtttm (Fillers),
B. corolliferum (Fillers) and B. galei (Augener), differ from the two new ones in having thoracic uncinal crests
with just two or three rows of few teeth (e.g. Fig. 4g-h). At least the last five of these are distinct species and
will be described elsewhere.
Brancliiomma moebii sp. now — Holotype ZMHUB 2304a (Fig. la-d, f-k); paratype ZMHUB 2304b (Fig.
le) Rovinj, N Adriatic.
Dasychone lucullana — Saint-Joseph, 1906 : 241. Cannes (MNHNP A3 11). Brancliiomma species A. —
KNIGHT-JONES et al ., 1991 : 847. One specimen found in gulley 3-13 m deep SW of Harem point, Bodrum,
Turkey (personal collection).
Additional material: a single specimen from the Bay of Muggia, Trieste (ZMUC), labelled D. lucullana by
Marenzeller.
The following description is based on the holotype, data in parentheses refer to the paratype.
Body 19 by 3.5 (17 by 3) mm with 40 (50) segments of which 8 are thoracic; crown a further 19 (14) mm
long, ventrally involuted at base; radioles 16 (18) on each side connected by a shallow web: each with about 25
(18) pairs of tongue shaped stylodes, larger pairs towards bases of dorsal mid lateral radioles (Fig. lc-d); radiolar
eyes almost obscured by narrow dense pigment bands lying just anterior to bases of (usually) alternate pairs of
stylodes (Fig. Id), but eyes not apparent in paler, more distal bands or areas between bands (more eyes occur in
Bodrum material -see below); apinnulate lips of radioles fine, 1 or (less commonly) 2 mm long; dorsal lips
tapered, grooved (with midrib support), about a quarter of length of crown and with fairly narrow lamellae, the
dorsal lamella attached to base of adjacent radiole, without pinnular support; collar with dorsal gap, small ventral
lappets and no veniro-lateral notches; 1st segment (excluding collar margin) about same length as others in thorax
Source : MNHN. Paris
NEW SPECIES OF BRANCHIOMMA (SABELLIDAE) AND COMMENTS ON RELATED GENERA
193
(measured at sides); thoracic fascicles (segments 2 to 8) with about 10 superior chaetae which are slender and
scarcely geniculate, the 'knee' region scarcely wider than shaft (Fig. lg), and about 20 inferior geniculate chaetae
with knee up to twice width of shaft (Fig. 1 h); thoracic uncini with an extensive crest of small compact teeth
(Fig. 4a- b) not usually seen in light microscopy (Fig. If); thoracic tori long (segment 7 with about 30 uncini),
all but die first two tori reaching ventral shields; most fascicles of abdominal chaetae forming compact tufts,
outer chaetae geniculate (Fig. Ik) with Uiick emergent shafts arranged in a C-shape (see Fig. la, insert) around a
cluster of capillary chaetae (Fig. lj); pigment patterns dark brown, most thoracic ventral shields with two IT-
shaped patches, 1st shield widi paired transversely elongate triangles, dorsal side of thoracic parapodia and inter-
ramal area (between fascicles and tori) widi unusually large patches, and dorsal side of abdominal parapodia with
dark triangles.
Fig. 1. — Branehiomma moebii sp. nov .: a, lateral view of holotypc. — b, ventral thorax. — c, dorsal thorax. - d.
whole radiole. — e, ventral view of paratype. — f, thoracic uncinus. — g, superior thoracic chaeta from 7th thoracic
fascicle. h, same, but inferior thoracic chaeta. j. superior capillary chaeta from 6th abdominal fascicle. k.
same, but inferior chaeta. Scales in mm: b as c; g. h. j as k.
This species is named after Professor K. A. MOBIUS (1825-1908) who collected die largest and best preserved
specimens. Me, Clapar£de & Marenzeller labelled their material Dasychone lucullana , but die dorsal lips of
that species are short (lengdis only two times breadth, Knight-Jones et ai , 1991) and die dorsal collar margins
are fused to die sides of the faecal groove.
On the Bodrum specimen some slylodes next to the web are unpaired, die more basal stylodes from dorsal and
lateral radioles are less crowded (more like those of paratype) and eyes are present between most successive pairs
of stylodes. Eyes not associated with colour bands, however, are smaller with fewer ocular units. Eyes are absent
near the base of the crowm (as in Rovinj material) and between a few other random pairs of stylodes. Frequency of
radiolar eyes was not noted in die material from Cannes and Trieste.
The following four species are die only ones widiin Branehiomma which resemble B. moebii in having
widely separated dorsal collar margins and uncinal crests widi numerous small teeth:
- Branehiomma infaremm (Krdyer, holotype ‘Greenland?’, ZMIIC, Fig. 2a-d, j-k) has stylodes like those of B.
moebii (cf. Figs Id; 2e), but larger specimens of B. infaremm (e.g. Malmgren. 1866, NRS 1252, Fig. 2f-g)
have broader, almost subcircular stylodes towards the bases of the dorsal and lateral radioles. Like B. moebii, B .
infarction is plump (body length 4 to 5 dines breaddi, diorax about as long as broad, widi crown up to three
quarters of body lengdi), but B. infaremm differs in having 1) a more extensive collar (especially vcntrally) with
ventro-lateral notches, 2) very numerous chaetae (about 80 in both thoracic and abdominal fascicles), 3) posterior
194
P. KNIGHT- JONES
inferior thoracic chaetae more slender (‘knee* scarcely wider than shaft Fig. 2k), 4) thoracic uncini with a longer
neck (cf. Figs 2h, j: in, 5) no radiolar eyes and 6) no pigment pattern other than bands on crown and indistinct
inter-ramal spots. Many records of infarctum (c.g. Levinsen, 1886; Ditlevsen. 1937: BERTELSEN, 1937;
ZMUC) are in fact the more elongate species Branchiomma arcticum.
- Branchiomma arcticum (Ditlevsen = Sabellastarte arctica Ditlevsen, hololypc, Baffin Bay “Godfhaab Expd".
Stn 86 ZMUC) has similar stylodes to B. moebii (these had been overlooked by Ditlevsen, as most of his
description referred to specimens from station 166, that had suffered histolysis, ZMUC) but differs Irom
B. moebii in having 1) an elongate shape (crown normally 0.25 to 0.4 of body length), 2) first segment about
twice the length of the following one (measured at sides), 3) prominent ventral collar lappets (Fig. 2t & w,
specimens preserved out of and in tubes respectively), 4) tori with gaps between their ventral ends and ventral
shields, and 5) uncini with broader crests of more distinct teeth (Fig. 4e).
- Branchiomma bahusiense Johansson (syntypes from W Sweden, ZMUU 346 a-b; other material from SE
Faroes, NHMT, KNIGHT-JONES 1992) is like Branchiomma moebii in having a plump body and a crown usually
more than half body length (Fig. 2q), but differs in having 1) no radiolar eyes, 2) narrower stylodes; 3) collar with
prominent ventral lappets; 4) short tori not reaching ventral shields (Fig. 2p); 5) broader thoracic uncini with
fewer crest teeth (Fig. 4D and a longer neck (cf Figs If: 2s); 6) more quadrangular, less distinct pigment blotches
on the ventral shields (Fig. 2p), and 7) much smaller inter-ramal spots.
- Branchiomma inconspicuum (M. Sars, in G. O. Sars, as Dasychone ZMUO) has uncini which seem to be
like those of B. moebii but, unlike moebii , has prominent ventral collar lappets and no colouration except liny
inter-ramal spots.
Branchiomma spongiarum sp. now — Holotype ZMUC, Fig. 3, paralype NMMT, both from Sin 377
(BIOFAR Survey) lat. 61043'53" N, long. 05o42'77" W. depth 274 m. - SEof Faroes.
Branchiomma sp. — KNIGHT-JONES, 1992, Faroes shelf (NHMT).
Additional BIOFAR records : Stn. 27, 61°54T0 N, 05o03*80 W, 225 m (1 specimen); Stn 283, 61°07'30 N,
05°51'20 W, 284 m (2); Sin. 375, 6ri0’04 N. 05°43'35 W 245 m (1); Stn 376, 61°09’51 N, 05°45’45 W, 250 m
(1); Stn 378, 61°44'20 N, 05°42’35 W, 258 m (1) and to the north of the Faroes, Stn 352, 62°43T0 N, 07°22’40
W, 354 m (2).
Found in association with sponges, Thenea levis at Stn 377, and T. valdiviae at Stns 375, 376 and 378, hence
the specific name. Sponge spicules were also with the specimen from Stn 27. The holotype is the largest
complete specimen.
Very small species, body 7.5 by 0.8 mm with 34 segments of which 7 or 8 are thoracic; crown a further
5 mm, involuted ventraliy at the base; 12 radioles on each side, each with small tapered tips, about six pairs of
fine stylodes and no eyes; dorsal lips with tapered and grooved midribs, but no pinnular support, blunt tipped, and
about one fifth length of crown; collar with wide gap dorsally and prominent paired ventral lappets; first segment
similar in length to others in thorax; thoracic fascicles small, each with about 12 chaetae, these and those of
abdomen like those of B. moebii (cf Figs lg to k: 3g to j); thoracic uncinal crests more than half the length of
the head, comprising about 20 fairly long and conspicuous teeth (Fig. 4 c, d); thoracic tori short (15 to 22 uncini
in 5th and 6th tori) not reaching indistinct ventral shields (Fig. 3c); inter-ramal spots fairly large and very distinct,
no other colouration.
As this species is found off Faroes, where the morphologically most similar B. bahusiense is also found, the
possibility of it being a juvenile of the latter was considered. In B. spongiarum , however, the stylodes are
relatively longer, compared with both breadth of slylode and width of radiole. Branchiomma bahusiense also
differs in having 1) at least 5 times as many stylodes per radiole, 2) a crown base only 1/16 of crown length,
compared with 1/6 in B. spongiarum , 3) thoracic uncini with a longer neck (cf. Figs 2s; 30, and 4) uncinal crests
smoother in profile (the small teeth lying closer to main fang) covering only half length of uncinal head (Fig. 40.
The blackish-red inter-ramal spots of B. spongiarum are very obvious against the pale body, whereas the minute
inter-ramal spots of B. bahusiense are less noticeable against a background of pale pinkish-fawn. None of 19
Faroes specimens of B. bahusiense occurred at stations where B. spongiarum was found (although depths, 235-
732 m. were similar) nor does B. bahusiense occur in association with sponges. It was commonly with Sertella.
Source :
NEW SPECIES OF BRANCHIOMMA (SABELLIDAE) AND COMMENTS ON RELATED GENERA
195
Brancliiomma infarction, B. arcticum and B. moebii differ from B. spongiarum in having larger bodies, wider
more numerous stylodes, larger uncinal crests of relatively smaller teeth, and longer tori either approaching or
17IG. 2. Brancliiomma inf a return (Kr0ycr. a to d. j, k. m = hololype; f, g. h = Malmgren's, 1866. material): — a. whole
animal lateral view. b, detail of a. — c, ventral thorax. — d. dorsal thorax. — e. whole radiole and enlarged
stylode (Kroyer's MS). — f. dorsal collar and base of crown. - g. dorsal basal stylodes from f. h and j. thoracic
uncini. k. inferior thoracic chaeta. m. ventral view of type before damage (Kr0yer's MS). B. bahusiense
Johansson. Faroes material: n, dorsal thorax. p. ventral thorax. q, whole animal, inserts showing most of a
dorsal radiole. r, inferior thoracic chaeta. - s. thoracic uncinus. B. arcticum (Ditlevsen), Greenland material: t.
ventral thorax. u. dorsal thorax. v. whole animal. — w. lateral thorax (another specimen). — x. dorsal radiole.
— y, thoracic uncinus. z. inferior thoracic chaeta. Scales in mm: c. d. as b; j. s and y as h: n as p; w and u as t:
z as k.
196
P. KNIGHT- JONES
touching the ventral shields. Branchiomma moebii further differs in having shorter ventral collar lappets, very
large inter-ramal spots, and a distinctive colour pattern. Branchiomma inconspicuum differs in having more
numerous teeth on the uncinal crests.
dorsal thorax. c, dorsal radiole. f, thoracic uncinus. — g and h, inferior thoracic chaetae, side and face view
respectively. j, superior thoracic chaeta. Scales in mm: c and d as b; g and j as h.
STUDIES ON PSEUDOBRANCHIOMMA JONES AND SABELLASTARTE KR0YER
JONES (1962) suggested the genus Pseudobranchiomma for P. emersoni , a species like Branchiomma but with
four thoracic segments and radioles with reduced sty lodes and without eyes. FlTZHUGH (1989) suggested three
more characters separating Pseudobranchiomma from Branchiomma : radioles bearing flanges; dorsal lips without
pinnular support; and abdominal fascicles with longer chaetae in the middle of the group. However, the latter
character is also found in Branchiomma ; presence or absence of pinnular support for a dorsal lip is rarely
important (the holotype of P. emersoni, AMNH, has one of its lips free and the other attached to a pinnule);
whilst possession of few thoracic segments is no more than a specific character, examples occurring in
Branchiomma (e.g. B. curta) and other genera (e.g. Perkinsiana Knight-Jones, 1983). Pseudobranchiomma may
thus seem closer to Branchiomma than envisaged by Jones (1962) and FlTZHUGH (1989).
Source :
NEW SPECIES OF BRANCHIOMMA (SABELLIDAE) AND COMMENTS ON RELATED GENERA
197
FIG. 4. — SEM of thoracic uncini (a to h) and radioles (j tom). — a and b, Branchiomma moebii sp. now — c and d, B.
spongiarum sp. nov. e, B. arcticum Dillcvsen. — f, B. bahusiense Johansson. — g, B. cingulatum (Grube). — h.
B. curt um (Ehlers). j, Pseudobranchiomma emersoni Jones from Cape Verde Islands (NHML). — k. P. orientalis
(McIntosh) from Hong Kong (NMWC). m. Branchiomma moebii sp. nov.
The so-called reduced stylodes of Pseudobranchiomma, however, are very different from Branchiomma
stylodes, which are epithelial flaps arising more or less tranversely to the axis of the radiole (Fig. 4m).
Pseudobranchiomma 'stylodes' are mere discontinuities in paired flanges along the radioles (Fig. 4 j,k). Similar
notched flanges are seen in Sabella (Dasyclione) serratibranchis Grube, Sabella tricolor Grube, Dasychone picta,
D. orientalis McIntosh, D. kumari* Aziz, 1). odhneri Fauvel and Sabella zebuensis McIntosh. These species
should be included in Pseudobranchiomma, although some seem to be synonyms of others (study in progress).
The notches in odhneri and zebuensis, however, are sparse and vestigial. Both species have been placed in
Sabellastarte by Day (1951) and Hartman (1959). Day (1951) synonymised odhneri with Sabellastarte tonga
(Kinberg), but present studies show the two species to be distinct, yet similar enough to place S. longa in
Pseudobranchiomma loo, amending die only significant generic character to:- radioles with paired, longitudinal
flanges, usually notched, but notches sometimes vestigial or absent. Pseudobranchiomma odhneri and P. longa
both have eyes on the radioles so that character too should be amended to :- radioles with or without eyes. They,
like the other species here placed in Pseudobranchiomma, have their dorsal collar margins free, not fused to the
sides of the faecal groove.
1 here seems to be no type material of Sabellastarte indica (Savigny) (type species designated by Hartman,
1959), but species agreeing with Savigny's definition (under "Tribu Sabellae Astarte”) have a double row of
[interdigitating] radioles, as in Sabellastarte magnifica (Shaw) and other species under study. These lack radiolar
flanges (and eyes) and have dorsal collar margins fused to the midline groove. The latter character is not
necessarily generic, for it varies within Branchiomma and both states (fused and free) can occur in a single species
(Megalomma heterops Perkins, 1984). Studies on Pseudobranchiomma and Sabellastarte are continuing so
characters other than radiolar flanges may be found to separate these genera more conclusively. Like Sabellastarte,
Branchiomma lacks such flanges.
Source :
198
P. KNIGHT- JONES
ACKNOWI JUDGMENTS
I am much indebted for facilities, material and information to the directors and staffs of the following
museums (shown in text above by initial letters): The American Museum of Natural History, New York
(AMNH): the Natural History Museums of London (NHML), Paris (MNHNP), Stockholm (NRS) and Thorshavn
(NHMT); the National Museum of Wales, Cardiff (NMWC) and the Zoological Museums of the Humboldt
University, Berlin (ZMIIUB) and of the Universities of Copenhagen (ZMUC), Oslo (ZMIJO) and Uppsala
(ZMUU). I am also very grateful to the Institute for Water Products Research, Bodrum, and die School of
Biological Sciences, Swansea, for research facilities, and to Drs M.R. FORDY for help with SEM, Arne
N0rrevang and Anne Klitgaard for material of Branchiomma spongicinim and information on associated sponges,
Zeki Ergen for help in collecting B . moebii , Mary E. PETERSEN for information about Kroyer's manuscript.
Thomas IE Perkins for valuable comments on this manuscript, die Systematics Association for a Wild
microscope with drawing attachment, die Ray Society and Royal Society for travel grants and the Linnean
Society of London (Applcyard Fund) for SEM costs.
REFERENCES
BERTELSEN, E.. 1937. Contributions to the animal ecology of the fjords of Angmagssalik and Kangerdlugssuaq in East
Greenland. Mcddr Gronland. 108 : 1-58.
Day, 1951. The polychaete fauna of South Africa. Part 1. The intertidal and estuarine Polychaeta of Natal and
Mozambique. Annls Natal Mus .. 12 : 1-67.
DlTLEVSEN. IE. 1937. Polychaeta. The Godthaab Expedition 1928. Meddr Gronland, 80 : 1-64.
FlTZHUGH, K.. 1989. A systematic revision of the Sabcllidae - Caobangiidae - Sabellongidac complex (Annelida :
Polychaeta). Bull. Amer. Mus. nat. Hist. 192: 1-104.
HARTMAN. O.. 1959. Catalogue of the polychaetous annelids of the world. Occ. Bap. Allan Hancock Fdn. 23 : 1-628.
Johansson. K.E.. 1927. — Beitriige zur Kenntnis der Polychaeten-Familien Hermellidac. Sabcllidae und Serpulidae.
Zool. Bidr. Upps.. 11 : 1-184.
JONES, M.E.. 1962. — On some polychaetous annelids from Jamaica, the West Indies. Bull. Amer. Mus. Nat. Hist.,
124 : 169-212.
KNIGHT-JONES. P.. 1983. — Contributions to the taxonomy of Sabcllidae (Polychaeta). J. Linn. Soc. (Zool.), 79 : 245-
295.
KNIGHT-JONES. P., 1992. Sabellariidae and Sabcllidae of the Faroes including some forgotten species. In: Marine
Biology and Oceanography of the Faroe Islands (BIOEAR). A. NorrevaNG (ed )Arbok 1991-92. Nordurlandahusid i
Foroyum, Torshavn. 100 pp.
Knight -Jones, P. & FORDY, M. R.. 1979. Setal structure, functions and interrelationships in Spirorbidae (Polychaeta,
Scdentaria). Zool. Set.. 8: 119-138.
Knight-Jones, P.. Knight-Jones, E.W. & Ergen, Z.. 1991. — Sabelliform polychaetes mostly from Turkey's Aegean
coast. J. nat. Hist.. 25 : 837-858.
Eevinsen, G. M.R. .1886. Kara-Havcts Ledorme (Annulata). In : C.F. LUTKEN & J. HAGERUP (eds). Dijmphna-Togtets
Zoologisk-botaniske lldbytte. Kobenhavn : 288-303
Malmgren. A.J.. 1866. — Nordiska Hafs-annulater. Opersigt. svenska Vetensk - Akad. Fork.. 22 : 355-410.
PERKINS, Thomas IE. 1984. Revision of Demonax Kinberg. Hypsicomus Grube and Notaulax Tauber, with a review of
Megalomma Johansson from Florida (Polychaeta: Sabcllidae). Broc. biol. Soc. Wash.. 97 : 285-368.
Saint -JOSEPH. A. de. 1906. — Les annelidcs Polychetes des cotes de France (Ocean et cotes de Provence). Annls Sci. nat.
Baris, ser. 9, 3 : 145-260.
Source : MNHN. Paris
21
Redescription of Hipponoa gaudichaudi Audouin &
Milne-Edwards, 1830 (Polychaeta, Amphinomidae)
Jerry D. KUDENOV
Department of Biological Sciences
University of Alaska Anchorage
3211 Providence Drive
Anchorage, Alaska 99508 U.S.A.
ABSTRACT
l*he genus Hipponoa (Polychaeta, Amphinomidae) is monotypic. Hipponoa gaudichaudi Audouin & Milne-Edwards. 1830.
probably represents a highly specialized species whose affinities to amphinomids has been questioned. As part of an on-going
study of Amphinomida, both the genus Hipponoa and species H. gaudichaudi are redescribcd and emended. Affinities with
other taxa of the order are briefly discussed.
RESUME
Rcdescription d 'Hipponoa gaudichaudi Audouin & Milne-Edwards, 1830 (Polychaeta, Amphinomidae)
Redescription de Hipponoa gaudichaudi Audouin & Milne-Edwards, 1830 (Polychaeta. Amphinomidae). Ee genre
Hipponoa est monotypique. Hipponoa gaudichaudi Audouin & Milne-Edwards, 1830, represente probablemcnt une espece tres
specialisee dont les affinites avec les Amphinomidae sont discutees. Comme partie d'une etude en cours sur les Amphinomida,
le genre Hipponoa et l’espece H. gaudichaudi sont redccrits ct emendes. Les affinites avec les autres taxa de Pordre sont
brievement discutees.
INTRODUCTION
On-going studies on the phylogenetic systematics of the polychaete Order Amphinomida (cf. Kudenov, 1994)
have revealed both historical questions and undescribed features for the amphinomid Hipponoa gaudichaudi
Audouin & Milne-Edwards, 1830. For example, McIntosh (1885) suggested that the setae of this species are not
calcareous. This feature, coupled to die fact that H. gaudichaudi lacks a caruncle, led McIntosh and others to
suspect dial it was improperly assigned to the Amphinomidae. Indeed, the Order Amphinomida is highly diverged
in the Class Polychaeta (Dales, 1962; CLARK, 1969). Removal of Hipponoa from the Amphinomidae may result
in establishing another polychaete family (for which precedents exists, see Carus, 1863; Baird, 1870). This
decision cannot be made lightly. The purpose of diis paper is to redescribe and emend the original of
KUDENOV. J.D.. 1994. Rcdescription of Hipponoa gaudichaudi Audouin & Milne-Edwards, 1830 (Polychaeta.
Amphinomidae) in Polychaetes. In: J.-C. Dauvin, L. Laubier & D.J. RE1SH (Eds). Actes de la 4eme Conference inlernationale
des Polychetes. Mem. Mils. natn. Hist, nat .. 162: 199-207. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
200
J.D. KUDENOV
Hipponoci gaudichaudi, and to address the question by McIntosh and others about the affinity of this species with
the Amphinomidae.
MATERIALS AND METHODS
Materials of Hipponoa gaudichaadi were obtained both from the Smithsonian Institution (USNM) and the
Allan Hancock Foundation Polychaete collection of the Los Angeles County Museum of Natural History (LACM-
AHF). Tissue sections were made following specifications noted by KUDENOV (1977). Preliminary SHM work was
performed at the USNM on preserved specimens held in the general collection.
Family Amphinomidae Lamarck, 1818
Genus Hipponoa Audouin Sc Milne-Edwards, 1830, emended
Hipponoa Audouin Sc Milne-Edwards, 1830: 156. — Cuvier, 1831: 18; Milne-Edwards, 1838: 464. —
Costa, 1841: 270. — Fauchald, 1977: 102.
Hipponoe Cards, 1863: 28. — Quatrefages, 1865: 409-410. — Treadwell, 1939: 177. — Gardiner,
1975: 103. — Non Treadwell, 1931: 3-4, figs. 10-12.
Hipponoe Audouin & Milne-Edwards, 1834: 1 16. — Hoeven, 1850-1856: 244. — Grube, 1850: 289. —
Schmarda, 1861: 134. —Baird, 1870: 239-240. — Fauvel, 1913: 32; 1923: 132. — Horst, 1886: 170. —
Amoureux, 1972: 51.
Hypponne Audouin Sc Milne-Edwards, 1834: 1 17.
Metamphinome Treadwell. 1940: 1.
Emended Diagnosis. — Body of adult fusiform, dorsoventrally flattened, with up to 105 setigers. Prostomium
with five antennae, two pairs of eyes. Caruncle absent. Nuchal organ present. Mouth ventral. Notopodia on
laterum. Ncuropodia on ventrum. Dorsal cirri numbering one per notopodium. Ventral cirri papilliform. Notosetae
all capillaries. Neurosetae retractile, hooks generally bidentatc; may be unidentate. Branchiae planar, bipinnate.
Anus terminal.
Remarks. — This emended diagnosis differs from those presented previously in that a nuchal organ is present,
branchiae are planar and bipinnate, and the anus is terminal. Neurosetal hooks arc generally bidentatc in specimens
with around 30 or fewer segments, and unidentate in a single specimen with 105 segments.
Hipponoa gaudichaudi Audouin Sc Milne-Edwards, 1 830, emended
Figs 1-2
Hipponoa gaudichaudi Audouin Sc Milne-Edwards, 1830: 156-159, PL III, fig. 4-4a-4b. — AUDOUIN &
Milne-Edwards, 1834: 128-129, PI. II, fig. 10-10 bis. — GuSrin, 1829-1843: 1-14, PI. IV. fig. 3, 3A-3D —
Cuvier, 1831 : 19. — Ibanez, 1973: 124.
Hipponoa gaudichaudi agulhana Day, 1967: 122, fig. 3.1 a-e.
Hipponoa gaudichaudi i Cuvier, 1831: 18. — Milne-Edwards, 1838:464.
Hipponoe gaudichaudi Baird, 1870: 239-240. —McIntosh, 1885: 30-33, PI. I, fig. 5, PI. IV, fig. 3, PI. IIIA,
figs. 13-17. —Horst, 1886: 170-171. — Fauvel, 1913: 32; 1914: 89, PI. I, fig. 2, 12; 1923: 132, Fig. 47 1-p:
1936: 19. — Pettibone, 1963: 57-59, fig 13 a-b. — Fauvel Sc Rullier, 1959: 510. — Amoureux, 1972 : 51.
Hipponoe gaudichaudi Hoeven, 1850-56: 244. —Grube, 1850: 289.
Hipponoe Gaudichaudi Stop-Bowitz, 1948: 15.
Hipponoe Gaudichaudi CUVIER, 1830: 199. -Milne-EDwards, 1836: 31-32, PI VIII, fig 4, 4a,b. — Carus,
1863: 28. — Quatrefages, 1865: 410. — Moore, 1903: 793. — WILLEY, 1910: 180. — Sumner, Osburn &
Cole, 1913: 619. — Augener. 1922: 39. — Okuda, 1950: 49, figs a-b.— Gardiner, 1975 : 103, fig. 5 1-m.
Hipponoe gaudichaudi gigantea Hartmann-Schroder, 1981: 24-25, figs. 1, 2.
Hipponoe multibranchiata Hartman 1951: 29, PL 8, figs. 1-2.
Non Metamphinome multibranchiata Treadwell, 1940: 1-2, figs. 1-3.
Hipponoe cranchii Baird, 1870: 240, PL VI, figs. 7-14.
Non Hipponoe elongata Treadwell, 1931: 3-4, fig. 10-12; 1939: 177-178, Fig. 11.
Source : MNHN. Paris
REDESCRIPTION OF HIPPONQA GAUDICHAUDI
201
FIG. 1. — Hipponoa gaudichaudi Audouin & Milne-Edwards : A. prostomiuin and anterior segments of adult, ventrolateral
view. B, same, anteroventral view. -C, same of juvenile lacking median antenna, dorsal view. — D, same, detail of
nuchal organ, dorsal view. — E, neuropodium, ventral view. — F. sheared capillary notofascicle revealing hollow core
(arrow). Abbreviations: 1A, lateral antenna; mA. median antenna; no, nuchal organ; np, neuropodium; or. notosetal
ornamentation; p, palps; pA, palpal antenna; vc. ventral cirrus; vc 1, padlike ventral cirrus of setiger 1; vc 2. ventral cirrus
of setiger 2. Scales : A = 0.2 mm; B = 0.4 mm; C = 0. 1 mm; D = 20 pm; E = 0.2 mm; F = 10 pm.
Source :
202
J.D. KUDENOV
Material examined. — North Adamic Ocean, Gulf Stream, Surface, R/V Albatross, coll. J.E. BENEDICT, 20
specimens (USNM 16311) ; 3 specimens (USNM 32374). — Bermuda, south shore, 5 Aug 1948, coll. II. Ris,
three specimens (LACM-AMF, n5858 from Hartman ledger).
Caribbean Ocean, Panama, Galeta Point, 14 Jul 1976, in sargassum rafts washed onto reef Bats, coll.
G. HENDLER, 1 specimen (USNM 58724). — Louisiana, Grand Isle, coll. H. Bennett, 4 (LACM-AHF,
n 10183 from Hartman ledger).
North Pacific Ocean, 30°50'N, 121°35'W, 29 May 1954, in Lepas fascicularis Ellis & S dander, coll. D.
HENRY, 19 specimens (USNM 32366); 27°56'N, 1 19°36'W, 23 Apr 1954, in L. anatifera Linnaeus, two specimens
(USNM 32367); 27°56'N, 1 19°36’W, 23 Apr 1954, in L. fascicularis Ellis & Solander, six specimens (USNM
32368); 28°40’N. 129°35’W, Jun 1955, in L. anatifera Linnaeus, two specimens (USNM 32369); 30° N, 1 18° W, 4
May 1954, one specimen (USNM 32370); 26°12'30" N, 1 18027’ W, 24 Aug 1954, in L fascicularis Ellis &
Solander, two specimens (USNM 32371); 30° 50’N, 121°35'W, 29 May 1954, in L. pectinata Spcngle, one
specimen (USNM 32372); 27°56'N, 119°36'W, 23 Apr 1954, in L anatifera Linnaeus, 5 specimens (USNM
32373); Off Japan, 28°02’N, 155°58'E, 29 Apr 1970, coll. G. Chase, 2 specimens (USNM 43205). — ?Pacific
Ocean, 9 Jun 1961, coll. D. Davenport, seven adults + numerous juveniles (LACM-AHF).
Description. — Body of adults fusiform, dorsoventrally flattened, 24-105 mm long, 5-18 mm wide without
setae, totalling 20-46 setigers; dorsum broadly exposed. Color in life bright orange.
Prostomium a small, single, rhomboid-shaped lobe, with 5 cirriform antennae (Fig. lc-d). Median antenna
about as long as prostomium, lacking ceratophore (Fig. 2a). Lateral antennae arising from frontal, dorsomedial
surface, about 0.6 times length of median antenna (Fig. 2a). Palpal antennae arising from anterolateral surfaces of
palps, somewhat more stout and shorter than lateral antennae (Figs la-b; 2b). Eyes numbering two pairs, located
anterior to median antenna, where prostomium is widest, all small, inconspicuous. Caruncle absent. Nuchal organ
present as ciliated patch on posterior prostomium, best observed in specimens with fewer than 15-18 setigers (Figs
lc-d; 2a). Palps fused into single lobe, forming upper lip of mouth and short midventral groove (Figs la-b; 2b).
Mouth ventral, opening between setigers 1-2; setigers 1-2 forming lateral lips of mouth; setiger 2 posterior lip
(Figs la-b; 2b).
Setiger 1 with setigerous notopodia, neurosetae absent, neuropodia only represented by pad-shaped ventral cirri
(Figs la-b; 2b). Parapodia biramous, setigerous from setiger 2 to end of body; rami more widely separated from
one another compared to setiger 1. Notopodia as transverse ellipses in outline in dorsal view, confined to extreme
dorsolaterum; notopodial lobes not raised above general body surface. Neuropodia circular to slight transverse
ellipses in outline in ventral view, confined to ventrum (Fig. le); neuropodial lobes resembling retractable papillae
surrounded by thick, glandular collars of tissue (Fig. le) with papilliform ventral cirri.
Parapodial cirri present on all setigers. Dorsal cirri cirriform, with basal cirrophore two times longer than wide,
distal style about 2-3 times longer than cirrophore; arising from body wall behind inferior notosetal fascicle
margin, not within notosetal fascicle. Ventral cirri papilliform, lacking basal cirrophores, slightly longer than wide;
arising medially from collar of neuropodium that encircles ncurosetal fascicles (Figs la-b, e; 2b).
Notosetal fascicles with numerous setae directed laterally in all setigers. Notosetae hollow (Fig. If, arrow),
slender capillaries with file-like teeth on shafts (Fig. la-b, 0, calcareous, accessory subdistal spurs absent, tapering
distal ly to fine, entire tips (Fig. la-b). Neurosetae from setiger 2 of one kind; chitinous, solid, distally bidentate
hooks with longitudinal striae, numbering around 10 per fascicle (Fig. le). Notoaciculae inconspicuous,
capillariform, numbering 3-5 per fascicle, limited to posterior notopodial margin. Neuroaciculae from setiger 2
distally curved, distally embedded in clear cuticular matrix, non-emergent, numbering 8 per fascicle, in single,
long, dorsal rows along superior or outer lateral margins of neuropodia (Fig. 2c).
Branchiae bipinnate, pinnae branching alternately off primary branchial axis, each pinna in turn branching up
to 6 times basally and having fewer branches distally (Fig. 2d-e); pattern more conspicuous in small specimens.
Branchiae present from setiger 3 to end of body, numbering 1 pair per segment, tending to be planar, particularly
in small specimens (Fig. 2d) than in larger ones (Fig. 2e). Branchial bases broad, arising posterodorsally to dorsal
cirri, not extending beyond notosetae. Branchiae gradually increasing in length and development to midbody,
gradually becoming shorter, less developed to end.
Pygidium with terminal anal cirrus; anus opening through anal cirrus (Fig. 2f).
Distribution. — Cosmopolitan in tropical and warm temperate oceans.
Remarks. — Hipponoa gaudicliaudi has been reported from numerous localities throughout the world, and its
description has not significantly changed since AUDOU1N & Milne-Edwards (1830) first described and Baird
(1870) later emended it. As presently understood, H. gaudicliaudi appears to be a highly modified and specialized
member of the Amphinomidae, probably reflecting the fact dial it is an inquiline of barnacles {Lepas species:
Source :
REDESCRIPTION OP HIPPONOA GAUDICHAUDI
203
Baird. 1870: Aucener, 1910: Kudenov, 1977). Although H. gaudicliaudi retains many features of the
Amphinomida, it is generally quite unlike most amphinomids (Gustafson, 1930 ; Kudenov, 1994).
FlG. 2. Hipponoa gaudichaudi Audouin & Milne-Ed wards: A — B, Proslomium showing only three of five antennae and
setiger 1, dorsal view. - C, neuroaciculae. — D. hipinnate branchia from right setiger 10. anterior view. — E, same, from
left setiger 13, anterior view. — F, pygidium, dorsal view. Abbreviations : see legend for Fig. 1. Scales : 1 = 0.25 mm, F; 2
= 10 pm, D: 3 = 30 pm, E and 5 pm. C: 4 = 0.2 mm. A, B.
For example, H. gaudicliaudi differs from the general amphinomid pattern in that its body is strongly flattened
and fusiform, and is die only known genus with a continuous midventral groove. Its prostomium is strongly
reduced to a single lobe with palpal antennae arising from the anterolateral margins of die prostomium. Palps are
extremely short, narrow, and fused medially, and are confined to the ventral area lying between the moudi and
prostomium (Fig. 2b; Kudenov, 1993). The mouth is present very close to die prostomium at the junction of
setigers 1-2 (Fig. 2b). Setiger 1 is dorsally complete, and is not interrupted by a caruncle. Notopodia arise from die
extreme dorsolaterum; neuropodia from the ventrum. The notosetae are endrely nonspurred capillaries; it is the
only presently known genus of die family in which the notosetae are represented solely by capillaries. The dorsal
cirri arise directly from the body wall as diey do in the Euphrosinidae, and not from within die notopodial field as
is typical of Amphinomidae. Obviously, H. gaudicliaudi is quite unlike the Amphinomidae sensu lato in many of
its features.
Additional traits either confirmed or newly discovered as part of diis study can be added to this list.
H. gaudichaudi is characterized by die: 1) lack of a caruncle: 2) a poorly ciliated, mound-shaped nuchal organ; 3)
absence of bodi neuropodia and ncurosetac in setiger 1: 4) reduced dorsal cirri in seuger 1: 5) lack of cirrTphores
on ventral cirri; 6) hollow calcareous notosetae; 7) solid neurosetae that may be chitinous; 8) planar, bipinnate
branchiae; and 9) a terminal anus opening through an anal cirrus. All except the first and third of these traits are
newly reported.
The nuchal organ is poorly ciliated, and more conspicuous as a mound-shaped lobe on the posterior
prostomium in juveniles and subadults than in larger individuals, such as functionally mature females. This finding
204
J.D. KUDENOV
may be expected, given the fact that H. gaudichaudi is a protandric hermaphrodite (KUDENOV, 1977). It is
hypothesized that immature individuals rely on nuchal organs and chemical senses to a much greater extent
compared to mature worms to maintain body contact with their brooder, to obtain food, and to subsequently locate
other barnacles. The nuchal organ must therefore be relatively better developed in immature individuals.
The lack of neuropodia and neurosetae in setiger 1 was previously noted by Day (1967) who made no further
comments about its significance. In this specialized amphinomid, setiger 1 is strongly modified and forms the
lateral margins of the mouth. It is so small that most light microscopical observations of this segment have lead
workers to assume the presence of neuropodia and neurosetae. The ventral cirri of setiger 1, which are both
reduced and very close to the mouth, may function in feeding. Moreover, H. gaudichaudi is the only described
amphinomid species in which ventral cirri lack cirriphores.
McIntosh (1885) particularly, and other workers generally, questioned whether the setae of H . gaudichaudi
are calcareous as those of other amphinomids. He strongly suggested that H. gaudichaudi is not typical of other
amphinomids whose setae produce gas bubbles when they are treated with weak acetic acid. McIntosh conveys
die impression that he would have assigned Hipponoa to another taxon if he had had additional evidence. Both
Carus (1863) and Baird (1870) had previously proposed die Hipponacea and Hipponoidae, respectively. SEM
studies revealed notosetal ornamentation (Fig. 10 usually associated with the calcareous setae of the
Amphinomida (Kudenov, 1993, 1994). Tissue sections through notosetal fascicles tend to splinter die setae of
non-decalcified specimens, leaving fragments of a clear outer layer assumed to be calcareous (Kudenov,
unpublished). H. gaudichaudi is clearly related to die Amphinomidae also by die fact diat its notosetae are hollow
(Fig. If), a feature shared by all other members of die order (Kudenov, 1994). However, its neurosetal hooks may
not be calcareous. All appear solid in bodi SEM and tissue section preparations, lack ornamentation referred to
above, and have densely packed longitudinal striae reminiscent of chitinous setae. Confirmation of these
observations awaits the receipt of fresh specimens. These setal data are presently insufficient to define
relationships between Hipponoa and other Amphinomida; they will eventually be refined and included in a
cladistic evaluation of the order Amphinomida (KUDENOV. 1994).
The branchiae of H. gaudichaudi have generally been described as being tuft-like, arborescent or dendritically
branched and bushy. All such terms are misleading. In fact, die branchiae are all bipinnate and planar (Fig. 2d-e), a
condition most obvious in juveniles which is clearly retained in adults, and reminiscent of those found in the
Chloeia species complex. However, primary branchial axes in Hipponoa gaudichaudi may be contractile; degrees
of contraction ranging from a long, slender zig-zagging to a stout, basal axis sometimes obscuring die bipinnate
pattern. Bodi taxa also have lateral cirri (mistaken for true dorsal cirri which are present in setigers 1-4 of Chloeia)
arising directly from the body wall and outside the notopodial field. No attempt to imply common ancestry
between these taxa is intended.
Another overlooked character in H. gaudichaudi is die presence of a terminal anus diat opens through die anal
cirrus (the presence of a dorsal anus has been assumed [e.g., Fauvel, 1923]). In other members of die
Amphinomidae, die anus opens on the dorsum of the last few body segments, above an associated, unpaired anal
papilla. The anus of Euphrosinidae is terminal, and opens between or above paired anal cirri (Kudenov, 1994).
The unusual anus of H. gaudichaudi presumably reflects its highly specialized life style, enabling it to void its
feces widiout fouling either itself or its host. This point can only be answered by studying live specimens of both
the worm ai id its host.
The synonymies listed above are not intended to be exhaustive. Analysis of the earliest literature shows
AUDOUIN & Milne-Edwards (1830) original record from Port Jackson, Australia, was quoted by subsequent
workers. Baird (1870) published what appears to be the second record of the species from die eastern equatorial
Atlantic and Madeira. He described a second species, H. cranchii , which his illustrations show to be a juvenile
Amphinome ( Irostrata ), and not a second species of Hipponoa. The diird record of H. gaudichaudi was from die
Challenger expedition, and MclNTOSH (1885) provided extensive observations about it, including die presence of
capillary notosetae having distal ly forked ends. Such notosetae have not been reported for H. gaudichaudi at any
other lime prior or subsequent to his work. Horst (1886) represents die fourth record, after which time the species
was more commonly encountered. Day (1967, Fig. 3.1.a-e) later described the subspecies, H. gaudichaudi
agulhana , based on the absence of notosetae as described by McIntosh (1885). It is suggested that McIntosh
observed frayed or damaged notosetae that appeared distally forked. Another, H. gaudichaudi gigantea Hartmann-
Schroder (1981) was distinguished on the basis of body size and hook morphology. Although the specimens she
examined were up to 105 mm long, neurosetal hook morphology may reflect size-dependent relationships instead
of polyploidy, as implied by Hartmann-SchrOder. Moreover, distinction between the terms "Normalform" and
Source :
REDESCRIPTION OE H1PPONOA GAUDICHAUDI
205
Riesenform used by I Iartmann-SchrGder to describe H. gaudichaudi gigantea are typological, and seem to
preclude a continuum or morphological change associated with allometric growth.
The genus Hipponoa supposedly represents three described species (Fauchald, 1977) including
H. gaudichaudi, H. cranchii Baird, 1870, and H. elongata Treadwell, 1931. Metamphinome mullibrancliiata
Treadwell, 1940 was referred to Hipponoa by Hartman (1951) and H. gaudichaudi by Pettibone (1963). All
previous descriptions and illustrations are sufficiently clear to indicate H. cranchii is probably a juvenile
Amphinome, and H. elongata is most certainly a Linopherus- like species. Therefore, die genus Hipponoa is
presently monotypic.
In summary, the species description of Hipponoa gaudichaudi is emended with certain observations confirmed
and additional characters newly reported. The species seems to be highly specialized and derived: departs
substantially from the general features normally attributed to die Amphinomidae (KUDENOV. 1994); and seems to
be cosmopolitan in tropical, subtropical and warm-temperate oceans. But is this taxon truly cosmopolitiui and
monotypic? Only a thorough systemauc study involving specimens from various points throughout its range can
answer these and odier questions.
ACKNOWI JEDGEMENTS
I am indebted to Kristian FAUCHALD, Greg Rouse and Linda Ward, all from the National Museum of Natural
History, and Len HlRSCH, Office of International Relations, Smithsonian Institution, Washington D.C., for dicir
assistance, support, encouragement and insights offered throughout this study. I especially thank Greg ROUSE for
his assistance widi die SEM. I also diank Kirk FlTZHUGH and Leslie Harris, Los Angeles County Museum of
Natural History, for loan of materials and for verifying literature citations. Editorial comments made by Kirk
FlTZHUGH and an anonymous reviewer improved this paper. Debra LACH1NSK1 provided the initial version of die
abstract in French.
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Gebiet zwischen dem Golf von Biscaya und dem Auftriebsgebiet vor Westafrika. " Meteor " Forsch.-Ergebnisse D. 33 : 23-
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IBANEZ. M. 1973 Catalogo de los anelidos polyquetos citados en las costas espaholas. Cuad. C. Biol.. 2 : 121-140.
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Source ; MNHN, Paris
22
Sabellariidae (Annelida, Polychaeta)
from south America
Paulo da Cunha LANA* and Claudia Silvia BREMEC **
* Centro de Estudos do Mar, Universidade Federal do Parana
Av. Beira-Mar. s/n, 83255-000 Pontai do Sul, Parana, Brazil
** Instituto Nacional de Investigacion y Desarrollo Pesquero
C. C. 175. 7600 Mar del Plata, Argentina
ABSTRACT
This paper summarizes the present taxonomic knowledge of Sabellariidae Johnston. 1865 from South America. Records of
ldanthyrsus annatus Kinberg, 1867, /. pennatus (Peters, 1854). Phragmatopoma attenuate Hartman, 1944, P. peruensis
Hartman, 1944. P. virgini Kinberg, 1867. P. moerchi Kinberg, 1867, P. lapidosa Kinberg. 1867, Sabellaria bella Grube. 1870,
S. bellis Hansen, 1882. S. fissidens Grube, 1870, S. minuta Carrasco & Bustos. 1981. S. nanella Chamberlin, 1919, and
S. wilsoni Lana & Gruel. 1989 are included. Regional synonymies, diagnoses, taxonomic remarks, and occurrence information
are provided for each species, together with an identification key and distributional maps. Discontinuous distribution patterns
of the continental sabellariid fauna may be only partially attributed to incomplete sampling. Many species seem to have
restricted distribution ranges. It is hypothesized that the dispersion patterns of sabellariids in South America do not conform to
the dispersal paradigm that could be expected from then active larval phases.
RESUME
Sabellariidae (Annelida, Polychaeta) d'Amerique du Sud
Petal actuel des connaissances sur les Sabellariidae Johnston. 1865 d'Amerique du Sud est presente. Les lieux de recoltcs
de ldanthyrsus annatus Kinberg, 1867. I. pennatus (Peters. 1854). Phragmatopoma attenuata Hartman. 1944. P. peruensis
Hartman, 1944. P. virgini Kinberg, 1867, P. moerchi Kinberg, 1867. P. lapidosa Kinberg. 1867, Sabellaria bella Grube. 1870.
S. bellis Hansen, 1882. S. fissidens Grube. 1870. S. minuta Carrasco & Bustos, 1981, S. nanella Chamberlin, 1919 et S. wilsoni
Lana & Gruel, 1989 sont donnes. Les synonymies pour cette region, des diagnoses, des remarques taxonomiques et des
informations sur les recoltes de chaque espece soul fournies. Une cle d'identification des especes et des cartes de distributions
soul egalemenl donnees. La distribution discontinue observee 1c long des cotes d'Amerique du Sud pourrait etre due a fabsence
d’observations dans certaines regions. Cependanl. beaucoup d’especes semblent avoir une distribution reduite. I/hypothcse
selon laquellc le mode de dispersion des Sabellariidae d’Amerique du Sud n'est pas conforme au modele correspondant a une
vie larvairc active est avancee.
INTRODUCTION
The Sabellariidae Johnston, 1865 currently comprises seven genera and about 65 species of colonial or non¬
colonial tube-building worms. Some species construct reefs of great extent in temperate or tropical regions.
Lana P., &C. S. BREMEC. 1994. Sabellariidae (Annelida: Polychaeta) from south America. In\ J.-C. Dauvin,
L. LAUBIER & D.J. REISH (Eds), Actes de la 4cme Conference intemationale des Polychetes. Mem. Mus. natn. Hist. not.. 162 :
211-222 Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
210
P. I, AN A & C. S. BREMEC
Representatives of this family occur from nearshore to oceanic depllis (UEBELACKER, 1984).
The present recognized genera are Phalacostremma Marenzeller, 1895, Monarch os Treadwell, 1926,
Gunnarea Johansson, 1927. Lygdamis Kinberg, 1867, Idanthyrsus Kinberg, 1867, Phragmatopoma Moerch, 1863,
and Sabellaria Savigny, 1818, widi only the three latter previously reported from South America. The regional
sabellariid fauna was hitherto poorly known. Relevant taxonomic literature is widely scattered and die level of
consistency in identifications appears to be rather low.
In this paper, we summarize the present taxonomic knowledge of Sabellariidae in South America. We have
attempted to include all published records from this area. Synonymies, diagnoses and the known geographic range
are provided for each species, together with an identification key and distributional maps.
This work is partially based on literature information, and we have not attempted to resolve disputed
taxonomic problems. Some taxonomic assignments are tentative, but can serve as background information for
future revisions based upon type-specimens or topotypes. Specific names are cited as listed in the original
references.
SYSTEMATIC^
Idanthyrsus Kinberg, 1867
Type-species: Idanthyrsus armatus Kinberg, 1867
Idanthyrsus armatus Kinberg, 1867
Idanthyrsus armatus Kinberg, 1867: 349. — JOHANSSON, 1927: 90. — MONRO, 1930: 177, fig. 73. — MONRO,
1933: 1066, fig. 14. — Monro. 1936: 172. — Hartman, 1944: 336, pi. 31, fig. 36. — Hartman, 1953: 10. —
Hartman. 1966: 73, pi. 24. figs 2-6. — Hartman, 1967: 150. — RlNGUELET, 1969: 212. — FAUCHALD 1972'
530. pi. 55, figs h-j. — Orensanz, 1974: 55. — FAUCHALD, 1977: 54. — RULLIER & AMOUREUX, 1979: 188. —
Carrasco & Bustos, 1981: 170, figs 8-1 1. — Hartmann -Schroder, 1983: 271. — Laverde-C, 1986- 128
Pallasia sexungula — Fillers, 1897: 125, pi. 8, figs 194-202. — Ehlers, 1900: 220. — Ehlers, 1901a: 267
Pallasia armata — Ehlers, 1901b: 195.
Sabellaria macropalea — Prait, 1901 : 1 3, pro parte
Pallasia pennata — Fauvel, 1941: 291.
Diagnosis — External paleae directed outward and plumelike, serrated, with a nearly straight shaft; spinelets
widely separated and curved outward (Fig. la). Inner paleae smooth hooks with narrow transverse striae. Uncini
with a double lateral row of 8 teeth, in addition to one median tooth at superior end. 2-4 pairs of nuchal hooks.
Maximum reported length 59 mm.
Distribution — South America: Pacific coast of Colombia; Valparaiso, Concepcion, and other sites of
Genual Chile: Magellan Strait: Beagle Channel; Cape Horn: Malvinas-Falkland Islands; South Georgia Island;
continental shelf off Patagonia and northern Argentina. Odier records: Western Mexico; British Columbia; Alaska;
Australia; Japan.
Remarks — /. armatus has been usually reported from cold waters in die southern and northern sectors of the
Pacific and in the southern West Atlantic. The range of the closely related I. pennants (Peters, 1854) appears to be
circumtropical, extending northward or southward from that of I. armatus. The zones of overlapping are few and
have been reported by Monro (1933), Rioja (1962), FAUCHALD (1977), and Laverde-Castillo (1986) for die
Pacific coasts ol Mexico, Panama and Colombia. However, records of I. armatus from Panama are doubtful, since
Gorgona Island, cited in the literature as a Panamian locality (Monro, 1933; Fauchai.d, 1977) is in fact off the
Colombian coast, about 600 km south of die Canal Zone. In addition, Monro’s illustration of an external opercular
palea (1933, p. 1065) clearly differs from those later provided by Hartman (1944) or Day (1967).
Neither I. armatus nor /. pennants have been recorded from the extensive tropical and subtropical Brazilian
coast. Ihe northern range of /. armatus along the Western Atlantic is clearly conditioned by the Subtropical
Convergence, north of La Plata River, where the colder waters of die Malvinas-Falklands Current meet the more
saline and warmer waters of the Brazil Current.
I. at matus and /. pennatus are known to ditler only in minor details of die outer paleae dentation, tapering in
die first and slender in the second. Besides that, shafts of the outer paleae are curved in /. pennatus and straighter
in /. at matus. femperature dependent variation in the morphology of polychaete hard parts has been previously
Source : MNHN, Paris
SABELLARIIDAE FROM SOUTH AMERICA
211
described by REISH (1977). A careful analysis of this problem should be undertaken in order to clarify the
taxonomic relationships of those species.
Idanthyrsus pennatus (Peters, 1854)
Sabellaria (Pallasia) pennata Peters, 1854: 613.
Idanthyrsus regalis — Chamberlin, 1919: 487, pi. 74, figs 1-8.
Idanthyrsus pennatus — JOHANSSON, 1927: 88. — MONRO, 1930: 176. — MONRO, 1933: 1065, fig. 13. —
Hartman, 1939: 19. — Fauciiald & Reimer, 1975: 90. — Fauchald, 1977: 54. — Laverde-Castillo, 1986:
128.
Diagnosis (modified from Day, 1967) — Opercular crown with two rows of long paleae. External paleac with
curved shafts and slender denticles (Fig. lb). Inner paleae smooth with tapering tips. 1-2 pairs of stout nuchal
hooks.
Distribution — South America: Pacific coast of Colombia and Ecuador; Galapagos Islands. Other records:
Western Panama and Mexico; Mossambique; South Africa; Tropical Indo-West Pacific from Madagascar to Japan.
Remarks — Taxonomic affinities and distribution range of /. pennatus and /. armatus were discussed above.
Phragmatopoma Mocrch, 1863
Type-species: Phragmatopoma caudata Moerch, 1863
Phragmatopoma attenuata Hartman, 1944
Phragmatopoma attenuata Hartman, 1944: 352, pi. 38, figs 90-96, pi. 39, figs 100-101. — Fauchald, 1977:
54. — Laverde-Castillo, 1986: 128.
Sabellaria ( Phragmatopoma ) virgini — MONRO, 1933: 1062, fig. 1 1.
Diagnosis (modified from Hartman, 1944) — Opercular crown slender, prolonged and asymetrical in lateral
view. External opercular paleae with a unique distal appendage, consisting of a palmately filamentous membrane,
directed nearly at right angles to the main shaft. Shaft with a recurved tooth on the ventral-facing side and weakly
scabrous on the upper surface (Fig. lc).
Distribution — South America: Ecuador, Pacific coast of Colombia. Other records: Pacific side of Panama.
Remarks — As far as we know, there were no additional records of P. attenuata since Hartman's original
description, based upon material collected by the Allan Hancock Pacific Expeditions along the Pacific coast of
Colombia and Ecuador.
Material from Pcrlas Islands (Pacific side of Panama), originally referred to Sabellaria (Phragmatopoma)
virgini by MONRO (1933), was correctly ascribed to P. attenuata by Hartman (1944). The original drawing of an
external palea by MONRO (1933, p. 1063) was shown to be slightly misleading by Fauchald (1977), who re¬
examined the material from Perlas Islands and noticed the presence of two distinct teeth on either side of the distal
plumes.
Phragmatopoma peruensis Hartman, 1944
Phragmatopoma peruensis Hartman, 1944: 353, pi. 37. figs 84-85, pi. 39, fig. 99, pi. 41, fig. 104.
Diagnosis (modified from HARTMAN, 1944) — Very small size, less than 10 mm long. Shaft of external paleae
with long, spatulate, distally rounded terminal membrane, strongly curved inward (Fig. Id). Middle paleae with a
conspicuous shoulder at their external edge.
Distribution — Peru.
Remarks — As P. attenuata , P. peruensis seems to be known only from through Hartman’s original
description.
Phragmatopoma virgini Kinberg, 1867
Phragmatopoma virgini Kinberg, 1867: 349. — Kinberg. 1910: 70, pi. 27, fig. 4. — Johansson, 1926: 2, fig.
l(la-b). — JOHANSSON, 1927: 100. — Hartman. 1944: 351, pi. 35. figs 77-78. — 1 1 artmann-Sciikodek, 1962:
155, fig. 202 (as Phragmatopoma c.f. virgini — HARTMAN, 1966: 75, pi. 24, figs 6-8. — RlNGUELET, 1969: 213.-
ORENSANZ, 1974: 55, pro parte.
Source :
212
F. LANA & C. S. BREMEC
Sabellaria macropalea — Pratt, 1901 : 13, pro parte.
Diagnosis — Opercular crown subcircular. External opercular palea with only two main teeth along outer
margins, without any process between them (Fig. le). Middle paleae smooth, very fine and terminating in a hook.
Abdominal uncini with 6 teeth. Maximum reported length 25 mm.
Distribution — Buket Island, San Nicolas Bay, Southern Chile (also spelt Bucket Island by earlier authors,
this site is probably Sanchez Island, according to Hartman, 1966, p. 1); Ramuncho, near Concepcion, Central
Chile; Malvinas-Falkland Islands.
Remarks — P. virgini was originally described from the Strait of Magellan, near Buket Island (= Sanchez
Island), southern Chile. Kinberg (1867) referred to the number and aspect of external paleae ("extemae 66
truncate, spina clongata armatae...") but provided no drawings. Eulers (1901b) re-examined the type material and
considered his species Hermella orbifera (Ehlers, 1901a) a synonym of Sabellaria virgini (Kinberg), since he did
not recognize the name Phragmatopoma. However, in the redescription carried out with complementary
specimens from southern Chile, EHLERS (1901b) figured external opercular paleae with sulcate median processes
(pi. XXIII. fig. 1 1). The type specimen of P. virgini was posteriorly studied by Johansson (1926) and Hartman
(1944). Both described external paleae with only two main teeth along their outer, distal margins, without
dentations or a flange between them. Hartman (1944) explicitly remarked that there was no indication of an
attached flange or other structure along the concave edge. So, die presence of a median process in die external
paleae can be considered a useful diagnostic character to distinguish P. virgini and P. moerchi. Consequently, the
material that EHLERS (1901b) referred to S. virgini belongs in fact to P. moerchi , as already suggested by
Hartman (1944). Orensanz (1974) mentioned P. virgini in a list of magcllanic species, but according to the
provided synonymy he also included earlier findings (EHLERS, 1901a: Monro, 1936) which in fact correspond to
P. moerchi. P. virgini is an intertidal species, known mainly from southern and central Chile. The Malvinas-
Falkland Islands citation (Pratt, 1901; Hartman, 1944) represents its unique record from the Atlantic ocean.
Phragmatopoma moerchi Kinberg, 1867
Phragmatopoma moerchi Kinberg, 1867: 349. — Hartman, 1944: 350,pl. 35, fig. 76, pi. 36, figs 80-83, pi.
39, figs 97-98. — HaRTMANN-SchrOder, 1960: 38. — HARTMANN-SCHRODER, 1962: 154, fig. 201. —
Hartmann-SchrOder. 1965: 304.
Phragmatopoma morchii — JOHANSSON, 1926:4, fig. 1(2-8). — JOHANSSON, 1927: 101.
Hermella orbifera — Ehlers, 1901a: 267.
Sabellaria virgini — EHLERS, 1901b: 199, pi. 23, figs 1-4, 7-12, pi. 24, figs 1-5, pro parte (non KINBERG,
1867).
? Sabellaria (Phragmatopoma) moerchi — Monro. 1936: 171.
Phragmatopoma virgini — ORENSANZ, 1974: 55, pro parte.
Diagnosis — Opercular crown flat and subcircular. External opercular paleae with a rectangular flange, frayed
at the distal end (Fig. If). Middle paleae transversely rugose and slightly roughened on the outer side, terminating
in a hook. Maximum reported length 50 mm.
Distribution — South America: Peru; northern and central coasts of Chile; Patagonia (?). Other records:
Hawaii.
Remarks — P. moerchi is an intertidal and subtidal species, known from Peru to Chile and west to Hawaii.
Sabellaria (Phragmatopoma) moerchi described by Monro (1936) from 43°50' S - 65°0r 51" W (near Dos
Bahias Cape, off Patagonia) could be referred to P. moerchi , since this author found " ... large comb-like processes
...” in die external opercular paleae. This would be die only record of the species in die Atlantic Ocean. However,
MONRO (1936, p. 15) remarked that he could " ... find nodiing significant to distinguish this species from
Johansson's account of Kinberg's Phragmatopoma lapidosa ". We think that this material should be reviewed
before die distribution range of P. moerchi is extended to die Atlantic.
Phragmatopoma lapidosa Kinberg, 1867
Phragmatopoma lapidosa Kinberg, 1867: 349. — JOHANSSON, 1926: 2. — JOHANSSON, 1927: 99. —
Hartman, 1944: 348, pi. 35, figs 73-75, pi. 36, fig. 79, pi. 40, figs 102-103. — Amaral, 1987: 471, figs. 1-5.
? Sabellaria fauveli — Gravier, 1909: 650, pi. 18, figs 60-69.
Source : MNHN. Paris
SABELLARIIDAE FROM SOUTH AMERICA
213
Diagnosis — External paleae witli a long conspicuous pinnate plume arising close to die upper distal margin of
the palea (Fig. lg). Middle paleae strong, uncinate, with a basal tooth. Inner paleae similar, but smaller. Uncini
with 8 teeth. Maximum reported length 23 mm.
Distribution — South America: SE Brazil (from Rio Grande do Sul to Rio de Janeiro, and probably
northward); Peru (?). Ollier sites: Caribbean; Atlantic coast of Mexico; Florida.
Remarks — A number of other forms, including P. caudata Moerch, 1863 (from die West Indies), Sabellaria
(Pallasia) castelnaui Grube, 1870 (from New Zealand), S.fauveli Gravier, 1909 (from Peru) and Genlrocorone
spinifera Treadwell, 1939 (from Porto Rico), have been referred to P. lapidosa by JOHANSSON (1927) and
Hartman (1944). In our opinion, this material, especially the records from the Pacific, needs reexamination. P.
lapidosa is one of the most conspicuous polychaete species along the tropical and subtropical coasts of the
Western Atlantic, building sandy reefs of great extent in the lower intertidal and shallow subtidal zones of exposed
rocky beaches. If really present on the Pacific coast of South America, it should have been consistently reported by
other authors. Amaral (1987) provided a brief characterization of the species, based upon material collected
along the southeastern coast of Brazil. However, her drawing of an external palea is slightly misleading, since the
teeth of the prolonged plume are depicted as round and not tapering.
Sabellaria Savigny, 1818
Type species: Sabellaria alveolata L., 1767
Sabellaria bella Grube, 1870
Sabellaria bella Grube, 1870: 69. — AUGENER,1934: 151, fig. 31a-d. — Cruet & Lana, 1988: 32, figs 1-2.
Sabellaria alcocki — Rijluer & Amoureux, 1979: 1 87, pro parte {non GRAVIER, 1906).
Diagnosis — External paleae asymetrical, with 2-3 lateral spines on each side of a central spike with 5-6
lateral teeth (Fig. lh). Middle paleae alternate long (narrow, basally excavated, with a fine point) and short (spoon¬
shaped, crenulated). Inner paleae geniculate, basally excavated and distally serrated. Uncini with 6 (seldom 5)
tec tii.
Distribution — SE Brazil (Espirito Santo to Santa Catarina States).
Remarks — The opercular paleae were redescribed by GRUET & Lana (1988). Previous records from North
Carolina and Peru (Hartman, 1944) were considered doubtful, on the basis of inner paleae morphology.
Sabellaria belbs Hansen, 1882
Sabellaria belli s Hansen, 1882: 19, pi. 6, figs 5-17. — AUGENER, 1934: 149, fig. 30a-e. — Hartman, 1944:
339, pi. 30, figs. 27-29.— RULLIER & AMOUREUX, 1979: 188.— GRUET & Lana, 1988: 34, figs 3-4.
Diagnosis — External paleae with a broad spiny median spike and two lateral teeth, rarely a small additional
one (Fig. li). Middle paleae all of the same length, short, spoon-shaped and laterally crenulated. Inner paleae long,
concave and distally spiny.
Distribution — SE Brazil (Rio de Janeiro and Santa Catarina Stales).
Remarks — Opercular paleae were also redescribed and illustrated by Cruet & Lana (1988), who restricted
the present distribution range of 5. bellis to die southeastern Brazilian coast.
Sabellaria fissidens Grube, 1870
Sabellaria fissidens Grube, 1870: 69. — EHLERS, 1901b: 196, pi. 24, figs 6-16. — RlNGUELET, 1969: 213.
Diagnosis (modified from EHLERS, 1901b) — External paleae with distal serrations and a simple, bifurcated
tip (Fig. lj). Middle paleae concave, all of the same length. Inner paleae distally simple. Uncini with 7 teeth.
Maximum reported length 28,5 mm.
Distribution — Coast of Chile, without reference to type- locality; Patagonic littoral (?).
Remarks — T he presently available descriptions of S. fissidens correspond to the original material (GRUBE,
1870). fully redescribed by Ehlers (1901b). RlNGUELET (1969) reported the species from the Patagonic littoral,
but provided no descriptions or illustrations.
Source
214
P. LANA & C. S. BREMEC
Sabellaria minuta Carrasco & Bustos, 1981
Sabellaria minuta Carrasco & Bustos, 1981: 167, figs 1-7.
Diagnosis — External paleae serrate, with a long median spike with bifid serrations (Fig. Ik). Middle paleae
alternating long and short. Inner paleae concave and distally simple. Uncini with 5-6 teeth. Probably the smallest
species of the genus, with a maximum reported length of 7 mm.
Distribution — Continental shelf off Central Chile, near Concepcion, at 1 35 and 220 m depth.
Remarks — Sabellaria minuta is known only from the original description. This is the only record, besides S.
fissidens , of the genus along the Pacific coast of South America.
Sabellaria nanella Chamberlin, 1919
Sabellaria nanella Chamberlin, 1919: 261, pi. 2, figs 5-7. — Hartman, 1938: 16, pi. 3, figs 8-10. —
Hartman. 1944: 340, pi. 30, figs 18-20. — Hartman, 1969: 509, figs 1-4. — RULLIER & AMOUREUX, 1979:
188. — Lana & Cruet, 1989: 243.
Diagnosis — External paleae directed outwards, with terminal smooth spikes terminating in a hook; a median
spike stronger and situated in a different plane (Fig. 11). Middle paleae concave and distally flat. Inner paleae
concave, tapering to a point. Uncini with five teeth in two lateral rows and one tooth at superior extreme.
Maximum reported length 18,5 mm.
Distribution — South America: SE Brazil (off Espirito Santo and Rio dc Janeiro States); Argentina (Monte
Ilcrmoso. near Bahia Blanca). Other records: California.
Remarks — According to CRUET (pers. com.) and BREMEC (pers. obs.), material from South America appears
to be morphologically indistinguishable from the type-material, originally described from California.
Sabellaria wilsoni Lana & Cruet, 1989
Sabellaria wilsoni Lana & Cruet, 1989: 239, figs 1-21.
? Sabellaria spinulosa var. alcocki — Fauvel, 1919: 477.
Diagnosis — Outer paleae assymetrical, distally Battened and spinous, with a central penicillate spike (Fig.
lm). Middle paleae of a single kind, directed upward, basally concave with two lateral expansions. Inner paleae
pointing inwards, gcniculated, basally excavated and distally pointed. Uncini with five teeth in two lateral rows,
two or more teeth at posterior end, one median tooth at anterior end. Maximum reported length 22 mm.
Remarks — I)r. Mary PETERSEN (in lilt.), from the Zoological Museum of Copenhagen, has called our
attention to the close similarity between S. wilsoni and S. vulgaris beaufortensis. She kindly provided us with a set
of unpublished drawings of .S’, vulgaris and S. vulgaris beaufortensis from North Carolina and Nova Scotia. S.
wilsoni clearly differs from die North-American material in that its middle paleae are long and nearly straight,
while those of .S', vulgaris and S. vulgaris beaufortensis are much shorter and sharply recurved at die distal end.
Two specimens of Sabellaria spinulosa alcocki reported in Fauvel (1919) from the French Guiana and
mounted on a slide (n. C78, Laboraloire of Zoology, IRFA, Angers, France) were reexamined by Lana & Cruet
(1989) and found to be identical to S. wilsoni. If confirmed through the observation of additional material, this
record will greatly extend the northern range of S. wilsoni.
Comments on other records of Sabellaria from South America — Two specimens from the eastern
Brazilian coast reported as Sabellaria alcocki by Rullier & Amoijreux (1979), were shown to belong in fact to
.S. bella and .S’. wilsoni (Lana & Cruet, 1989). As remarked above, S. spinulosa alcocki , reported from the French
Guiana (Fauvel, 1919), most probably belongs to S. wilsoni.
KEY TO SABELLARIIDAE FROM SOUTH AMERICA
la Opercular crown with two rows of paleae; a pair of large hooks [Idanthyrsus I . 2
lb Opercular crown with three rows of paleae; dorsal hooks absent . . 3
2a External opercular paleae almost straight, with tapered
lateral denticles or spinelets . Idanthyrsus annatus
2b External opercular paleae with curved shafts and slender lateral denticles . Idanthyrsus pennatus
Source :
S ABELL ARHDAE FROM SOUTH AMERICA
215
3a Middle opercular paleae cover the inner ones; operculum a flattened cone [Phragmatopoma I . 4
3I> Middle opercular paleae not concealing the inner ones; operculum open [Sabellaria I . 8
4a External opercular paleae without distal appendage . Phragmatopoma virgini
4b External opercular paleae with distal appendage . . 5
5a Distal appendage long, spatulate, distally rounded, with a smooth margin.... Phragmatopoma peruensis
5b Distal appendage pinnate or comb-like . 6
6a Distal appendage short, rectangular, with a frayed distal border . Phragmatopoma moerchi
6b Distal appendage long, pinnate or brush-like . . . 7
7a Distal appendage a long and nearly straight pinnate plume arising from the upper
distal edge ol the palea . Phragmatopoma lapidosa
7b Distal appendage a palmately filamentous membrane, brush-like, nearly at right
angles to the main shaft . Phragmatopoma attenaata
8a Inner paleae distally serrated or frayed . 9
8b Inner paleae distally simple or tapering to a point . 10
9a Inner paleae distally serrated; middle paleae alternately long and short;
external paleae assymetrical, with 2-3 lateral spines on each side of
a central serrated spike, provided with 5-6 lateral teeth . Sabellaria bella
9b Inner paleae with about 6 distal spines; middle paleae all of the same
length; external paleae with a broad spiny central spike and two (rarely
a small additional one) teeth . Sabellaria bellis
10a External paleae with distal processes in the same plane . 1 1
10b External paleae with a strong median simple spike in a different plane . Sabellaria nanella
11a Median spike of outer paleae a simple, bifurcated tip . Sabellaria fissidens
1 lb Median spike of outer paleae with a conspicuous spiny process . 12
12a Median spike with bifid serrations . Sabellaria minuta
12b Median spike penicillate . Sabellaria wilsoni
BIOGEOGRAPHICAL COMMENTS
Thirteen species of Sabellariidae are presently known from South America (Fig. 2), five in the Atlantic, six in
the Pacific with two in both oceans, not including some doubtful records mentioned above. Idanthyrsus armatus
and Phragmatopoma virgini, the only species common to die two oceans, have been recorded mainly from the
connected sectors of die Soudi Atlantic and Soudi Pacific, or near this area.
The existence of distinct sabellariid faunas along die two margins of the Soudi American continent, with some
degree of convergence towards its southern sector, can be attributed to prevalent oceanographic conditions.
Subantarctic water is of lesser significance in die Atlantic, since Soudi America, owing to its southeastward extent,
deflects large quantities of colder waters along its west coast (Sverdrup et «/., 1942). A tropical or subtropical
sector along the Pacific is not as extensive as in the Atlantic, because of the Humboldt Current. Consequently,
average water temperatures along die west coast of Soudi America are lower than on die east margin.
Hartmann-Schroder (1960) recognized distinct north-temperate, tropical and south-temperate polychaete
faunas in a zoogeographic analysis from Alaska to "Tierra del Fuego”. Widi die current information, it is not yet
possible to draw such putative boundaries for the regional sabellariid fauna. However, a group made up of
Phragmatopoma lapidosa and a more diversified Sabellaria stock, dominant along die wanner waters of die
Atlantic side north of 35° S, is clearly separated from an East Pacific and southern Atlantic group, represented by
several Phragmatopoma species, besides Idanthyrsus armatus, Sabellaria minuta and S. fissidens.
Only P. lapidosa , /. armatus and P. moerchi have been consistently reported from extensive areas in die
region. Gruet & Lana (1991) have suggested, in relation to Sabellaria , that die low number of described species
and discontinuous distribution patterns, mainly along die Pacific coast, are probably due to incomplete sampling or
Source :
216
P. LANA & C. S. BREMEC
to a lack of suitable habitats. However, it is well known that many species of Sabellaria and Phragmatopoma are
very conspicuous members of the rocky intertidal fauna, building sand-reefs of great extent. It would have been
difficult to overlook them during die several faunal surveys carried out along both coasts of South America this
century. We suggest that disjunct distribution, as currently reported for most species, is in fact an actual
zoogeographical pattern of die continental sabellariid fauna.
lOOp
f
d
FlG. I. Outer opercular paleae of sabellariid species from South America, a: Idanthyrsus armatus . b: /. pennatus. c:
Phragmatopoma attenuate i. d: P. pemensis. e: P. virgini. f: P. moerchi. g: P. lapiciosa. h: Sabellaria bella. i: S. bellis. j. S.
fissidens. k: S. minuta. 1: S. nanella. m: S. wilsoni .
Source : MNHN. Paris
SABELLARIIDAE FROM SOUTH AMERICA
217
Larval transport by wave currents has been considered the main recruitment source for benthic shelf species
(Josefson, 1985). One could expect that littoral surface currents be responsible for the continuous distribution of
invertebrate launa along continental shelves. This would be specially true concerning the dispersal of polychaete
species with active larval phases, such as the sabellariids. Larval development, from fertilization to settlement, can
take up to 32 weeks in warm-temperate sabcllariid species, and 3-4 weeks in tropical species (Eckelbarger,
1977). Yet, as shown above, continuous occurrence patterns are not a common feature among die local sabcllariid
fauna. A number of factors could account for this, both in large and small spatial scales. The circulation of die
Pacilic water masses is more sluggish than in the Atlantic and does not allow for an intense mixing of different
water masses (Sverdrup el al„ 1942). In addition, surface winds or inshore upwelling, present on both sides of
the continent, have been previously shown to sweep away pelagic larvae of littoral forms (Roughgarden el al.,
1988). Large-scale physical-oceanographic processes which transport larvae farther offshore also appear to
regulate latitudinal dilferences in die recruitment of marine invertebrates, mainly in the tropics (SUTHERLAND,
1990) . Experimental evidence concerning sabcllariid recruitment in small spatial scales has suggested that larvae
respond first to proper flow conditions and only then to chemical cues diat induce metamorphosis (Pawlik ei al.,
1991) . Unlike die larvae of solitary sabcllariid species, which show no preference for conspecific substrata,'
settlement of gregarious species seems to be highly dependent on the presence of conspecific reefs (Pawlik,
1988). In this context, it is reasonable to suppose that die dispersion of colonial sabellariids is rather through reef
accretion than through the formation of new reefs.
Idanthyrsus
• Idanthyrsus armalus
O Idanthyrsus pennatus
Phragmatopoma
■ Phragmatopoma attenuata
/S Phragmatopoma peruensis
A Phragmatopoma virgini
O Phragmatopoma mocrchi
• Phragmatopoma lapidosa
Sabellaria
• Sabellaria bclla
O Sabellaria fissidens
A Sabellaria bcllis
A Sabellaria nanclla
□ Sabellaria wilsoni
■ Sabellaria minuta
Fig 2. Distribution of sabellariid species in South America.
218
P. LANA & C. S. BREMEC
All these factors may provide an explanation for the disjunt distribution patterns of the regional sabellariid
fauna, through the restriction of stenothermic species dispersal. Despite the presence of extensive sandy reefs ,
distribution of sabellariids can in fact be determined by pre-settlement processes, such as local patterns of larval
transport, which will affect larval survival and recruitment.
These results provide additional evidence in support of an alternate hypothesis to the dispersal paradigm for
sabellariids, previously stated by Fauchald (1984). We suggest that sabellariids, contrary to what could be
expected from their active dispersal phase, can in fact have endemic or geographically restricted distribution
patterns.
ACKNOWLEDGEMENTS
Our thanks to Lie. N. Scarlatto, who translated German papers. Dr. YvesGRUET and Dr. Mary PETERSEN
were most helpful in providing information concerning species of Sabellaria. The second author was partially
supported by a grant from the Brazilian Research Council (CNPq).
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23
The phylogenetic position of the Pilargidae with a cladistic
analysis of the taxon - facts and ideas
Frank L1CHER & Wilfried WESTHEIDE
Universitat Osnabruck, Fachbereich Biologie/Chemic. Spezielle Zoologic
D-49069 Osnabruck, Germany
ABSTRACT
1 he taxon Pilargidae is considered to be a group of derived hesionid species. This view is supported by the fact that
apparent pilargid-specific features also occur in a few hesionid taxa. The idea is also based on the hypothesis that the pilargid
stem species evolved by early maturation ("progenetically") of a juvenile stage of a large-bodied hesionid species. Making use
of all characters available and using a hesionid taxon as outgroup, a cladogram of all pilargid genera was constructed with the
program HENNIG 86. vers. 1.5. It shows well developed prostomial appendages and separate biarticulated palps to be the
plesiomorphic character states. Ihe genera Synelmis and I.itocorsci are newly defined. For phylogenetic systematic implications
the pilargid taxa should be included in the Hesionidae.
RESUME
Position phylogcnetique des Pilargidae avec analyse cladistiquc du taxon - faits et idees.
Le taxon des Pilargidae est considerc comme etant derive d'un groupe d'Hesionidae. Ce point de vue est conforte par le fail
que des caracteres typiques des Pilargidae se rencontrent egalement chez quelques Hesionidae. L'idee est basee sur 1'hypothese
que l'espece souche des Pilargidae a evolue a partir du stade juvenile d’un hesionide de grande taillc qui aurait acquis une
maturite sexuelle prccoce (progenese). En se fondant sur tous les caractdres disponibles et en prenant un hesionide comme
groupe exterieur, un cladogramme de tous les genres de Pilargidae a ete construit a l'aide du programme HENNIG 86, version
1.5. Cela revele que des appendices prostomiaux bien developpes et les palpes biarticules representent l’etat plesiomorphe. Les
genres Synelmis et Litocorsa sont redefinis. Dans une optique de systCmatique phylogcnetique. les Pilargidae devraient etre
inclus dans les Hesionidae.
INTRODUCTION
When he described Pilargis verrucosa , Saint-Joseph (1899) erected the Pilargidae to contain it. starting a
long-lasting discussion on die systematic validity of this polychaete taxon. The first descriptions of pilargid
species were actually much earlier, but the authors considered the worms to be orbiniids ( Sigambra grubii Muller,
LlCHER. F. & W. WESTHEIDE, 1994. — The phylogenetic position of the Pilargidae with a cladistic analysis of the taxon -
Facts and ideas, hr. J.-C. Dauvin. L. LAUB1ER & D.J. REISH (Eds), Actes de la 4eme Conference internationale des Polychetes.
Mem. Mus. naln. Hist. nut.. 162 : 223-235. Paris ISBN 2-85653-214-4.
Source : MNHN, Paris
224
F. LICHER & W. WESTHEIDE
1858 as Amylidea: and Parandalia tricuspis Muller, 1858, as Ariciaea) or syllids (Ancisirosyllis groenlandica
McIntosh 1879: Cabira incerta Webster, 1879: Pilargis tardigrada (Webster, 1879), as Pliroma : Synelmis albini
(Lanoerhans 1881). as Ancisirosyllis. EULERS (1908) was die first to consider diese species to be hesiomds. For
moslpolychaete taxonomists, however, diese species appeared to be too different from "typical hesiomds to be
included in this family. For instance, Hessle (1925) argued dial Ancisirosyllis was neither a syllid nor a hesiomd -
an opinion which has persisted to liie present. . .
One of us (W WESTHEIDE) became extremely interested in pilargids when tirst seeing living Siganwia
individuals at the nordiem coast of China in 1987. The form of these specimens, under a low power dissecting
microscope, and their locomotion seemed so similar to those features of the interstitial hesiomd species
Hesionides maxima Wesiheide, 1967 and Hesionides pelliboneae Westheide, 1987 (WESTHEIDE 1)67, 1987a)
that the later identification of the fixed specimens as a pilargid taxon was radier astonishing. We asked oui selves
whether our many years of experience in recognizing live meiofauna-taxa just by their appearance and locomotory
characters had failed in this case or whedier diis apparent mistake might be due to a very close systematic
relationship between interstitial hesionids and pilargids.
This prompted an investigadon of die phylogenetic systematics within die Pilargidae to see ll diere was any
support for diis hypothesized relationship. Our findings resulted in reinvestigations of several pilargid taxa and a
review of the entire pilargid literature, especially JONES (1961), EMERSON & Fauchald (1971), Bri iaev &
Sapiironova (1981), Fitzhugii & Wolf (1990) and Salazar- Vallejo & SolIs-Weiss (1))2). A
comprehensive analysis of die taxon suffers from die fact that no true anatomical or any ultrastructural details are
available Fitzhugii & Wolf (1990) in their cladogram especially used brain gross morphology as a taxonomic
and systematic character. Although it is based only on die outlines of various brains taken from whole mounted
specimens their cladistic analysis has been of considerable help. However, we do not agree with their
phylogenetic interpretation in all points. Our phylogenedc analysis differs from their results because we make use
of a different outgroup.
CLADISTIC ANALYSIS
Diagnostic features OF THE Pilargidae. — The pilargid body is cylindrical or dorsoventrally flattened,
and anterior segments can be inflated. The integument may be smooth or papillaled. The prostomium bears
antennae (three, two, or none at all) and biardculated palps, consisting of large palpophores and palpostyles ot
different length and shape. Small pigmented eyes may be present. The pharynx is eversible and usually has a
circlet of distal papillae; jaws may be present. ... , , ,r.
The achactous peristomium is usually equipped with two pairs of tentacular cirri, which may be absent. 1 he
parapodia are usually well developed and biramous. In most of the species die notopodia possess a single stout
spine or hook, and a notoacicula; additional capillary chaetae may occur. The neuropodia arc equipped with an
acicula and several simple chaetae, which may be capillary, slightly unidentate, serrated, smoodi, spinous or
furcate. Dorsal and ventral cirri arc usually present, and they may be of different lengdis. Gills exist in one genus.
The pygidium has two or three anal cirri.
The following characters are considered to be autapomorphic, defining the monophyly of die Pilargidae: (1)
possession of a simple specific stout emergent notochaeta, to be reduced in some genera, (2) possession ol
exclusively simple, neuropodial mainly capillary chaetae, and (3) possession ot fleshy biarliculated palps.
List of pilargid genera. — The assumed autapomoiphies of die pilargid taxa arc briefly mentioned; the
material examined during diis study is listed in brackets.
Sigambra Muller, 1858: this first described genus and most species-rich taxon of the family was recognized as
a pilargid not earlier than in die middle of this century (Hartman. 1959; PETTIBONE, 1966). Since die notopodial
hooks are considered by the authors to be plesiomorphic within die Pilargidae the taxon possesses primitive
features only, but see FITZHUGII & Wolf (1990) (Sigambra bassi HSNM 86966: S. grubii USNM 103016; .S'.
lentaculata, USNM 86975; S. wassi, USNM 30987; specimens from Thailand and China).
Ancisirosyllis McIntosh. 1879: the monophyly of the taxon may be based on its five-lobed brain (FITZHUGII &
Wolf. 1990). Ancistargis Jones, 1961. is tentatively included (Pettibonh, 1966; Gardiner, 1976; Wolf, 1984),
aldiough die species of diis genus are clearly separated from Ancisirosyllis in possessing two antennae only. II
Ancistargis were accepted as a separate taxon, no synapomorphic character for Ancistrosyllis-species widi diree
antennae would be available (Ancisirosyllis breviceps LACMNH AIIF POLY 0143, LACMN1I Velero si. 7498-
Source : MNHN. Paris
PHYLOGENETIC POSITION OF THE PILARCIDAE
225
61; A. carolinensis USNM 86909; A. harimanae USNM 30989; A.papillosa USNM 86923, and specimens from
uuicr sources;.
Cabira Webster, 1879: the monophyly of this (axon is clearly shown by the possession of jaws (Britaev &
Sapiironova, 1981) (Cabira incerta USNM 30985). J
Pilargis Saint- Joseph, 1899; since the papillated integument is considered to be a synapomorphy, this taxon
should be closely related to Ancistrosyllis-Ancistargis. Cabira and Paracabira. A notopodial spine or hook is
tT?.a of" Pila,'gid laX,a ' CXCepl °'0ps,s - are equiPPed with spines or hooks the absence of a
cnaetae ol this kind in Pilargis is considered to be a derived character ( Pilargis berkeleyae USNM 86959)
Otopsis Ditlevsen, 1917: the genus resembles Synelmis, but lacks notopodial spines or hooks, which is
interpreted as a loss (see also Pilargis).
50 um
1. tentacular cirrus
2 tentacular cirrus
3 tentacular cirrus
FIG. 1. — Hesionides goliari Hartmann-Schrodcr. 1960 and Sigambra sp. from Yellow Sea, near Qingdao: a. Hesionides
gohari, anterior end. dorsal view. — b. Sigambra sp.. anterior end, dorsal view. — c, anterior end. ventral view. _ d.
parapodium, mid-body region.
Synehrn Chamberlin, 1919: we adopt die view of FlTZHUGH & Wolf (1990) and partition Synelmis species
between complex A” (species widi furcate ncuropodial spines) and "complex B" (species with non-furcate
neuropodia! spines). The non-furcate, less complex chaetal type is considered to be the apomorphic character
state. For die monophyly of the two Synelmis complexes see "Discussion" (Synelmis albini, collection of the
senior author; S. simplex. USNM 19480).
lalehsapia Fauvel, 1932: this monotypic, poorly known taxon is included in the analysis although its
assignment to die Pilargidae has been repeatedly questioned (e.g., Pettibone, 1966, Emerson & Fauchald
1971). mainly because of the possession of jaw-like structures. The shape of the body, especially of the anterior
region, die absence of prostomial and tentacular appendages, the presence of an emergent notopodial spine, die
absence ol notoaciculae and dorsal cirri, and the possession of only simple chaetae suggest a close relationship
226
F. LICHER & W. WESTHEIDE
wiili the Loandalia-Parandalia complex. The possession of jaws is the autapomorphic character of this taxon;
they differ distinctly from those in Cabira.
Loandalia Monro, 1936: this is the only pilargid genus with branchiae, clearly indicating its monophyletic
status.
Glyphohesione Friedrich, 1950: die opinion dial this monotypic taxon should be included in Ancistrosyllis
(Eliason. 1962) or Synelmis (PErriBONE, 1966) is rejected (see also FlTZHUGH & Wolf. 1990, LlCHER, in press)
and die genus Glyphohesione should be retained. Specimens idcndficd as Synelmis klatti (Friedrich, 1950) (six in
the collection of the Zoologisk Museum Copenhagen (ZMUC) and one in the collection of die Senckenberg
Museum Frankfurt (SMF)) differ from all pilargid taxa in possessing elongate, non-papilliform palpostylcs and
lateral antennae which are located near the anterior margin of the prostomium. They also do not possess emergent
neuropodial spines which are characteristic for Synelmis. This is also true for two specimens from Florida in die
collection of die U.S. National Museum Washington, although they differ slightly in odier characters. The
European and die American material bodi belong to Glypholiesione (LlCHER, in press) (Synelmis klatti SMF 4432:
ZMUC-POL-178; USNM 86986).
Litocorsa Pearson, 1970: die diree species in diis genus comprise a rather heterogeneous group in possessing
direc antennae, two antennae or none at all. Monophyly of die genus may be indicated by the presence of
completely fused palps (FlTZHUGH & Wolf. 1990).
Parandalia Emerson & Fauchald, 1971: die genus resembles Loandalia except that branchiae are absent. For
die time being, however, no autapomorphic characters indicate its monophyly (Parandalia ocularis , collection of
L. Harris, LACMNH; P. tricuspis USNM 123092).
Paracabira Britaev & Saphronova, 1981: tutapomorphies of die monotypic taxon are (1) lack of lateral
antennae and (2) lack of dorsal parapodial cirri.
It cannot be completely discounted that Loandalia, Parandalia and Talehsapia do not belong to the Pilargidae at all.
Because they almost or completely lack anterior appendages, their inclusion is mainly based on their comparatively simple
parapodia with a stout notopodial spine. Thus their bearers could well be the endpoint of an evolutionary reductional series
starting from another taxon within the Phyllodociformia (sensu FAUCHALD, 1977). (Omission of the three taxa from the
analysis, however, would influence neither the cladistic results nor our reasoning about the phylogenetic origin of the
Pilargidae.)
Despite Salazar- Vallejo's ( 1986) argumentation, Antonbruunia Hartman & Boss, 1965, is not considered in
our analysis. For the time being there is no convincing evidence for the pilargid nature of this monotypic taxon
(see also FlTZHUGH & Wolf. 1990). The recently erected Nautiliniellidae (Miura & LAUBIER, 1989) have only
superficial similarities to die pilargids.
Outgroup relationship. — Our phylogenetic analysis is based on die assumption dial within the Pilargidae
those taxa are the most primitive which possess (1) die highest number of head appendages (antennae, palps and
tentacular cirri), (2) die best developed appendages, and (3) the highest number of chaetae and chaetal types. That
is, an evolutionary pathway is hypothesized during which considerable reductions occurred, starting from taxa
with three filiform antennae, two pairs of filiform tentacular cirri, biarticulated palps, and filiform dorsal
parapodial cirri and leading to forms widiout any prostomial, tentacular and notopodial appendages (but see
above). The general basis for this hypothesis is the idea that die stem species of the Phyllodociformia was richly
equipped widi head <uid body appendages which became differently and independently reduced within various
taxa, especially in species with a totally endopsanunic way of life.
By this line of argument Sigambra and Glyphohesione should be the most primitive pilargid taxa (LlCHER, in
press). Indeed, they show strong similarities widi those small hesionid species which possess only a small number
of body appendages. Similarities in number and arrangement of head appendages are obvious (Fig. 1). All the
appendages in, e.g., a species of the genus Hesionides Friedrich, 1937 can be found in a Sigambra with die
exception of the third tentacular cirri, which are still notopodial cirri of the first chaetigerous segment in
Sigambra. The anterior-most ventral filiform appendages in Hesionides have a cirrus-like appearance.
Investigations of their innervation, however, could prove them to be palps and therefore most likely homologous
to the more fleshy mid biarticulated palps in the pilargids [ultrastructural mid immunohistochemical investigations
by one of us (F. LlCHER)].
For diese interstitial hesionids a progenetic evolution has been considered (LAUBIER. 1967; WESTHEIDE,
1987b; WESTHEIDE & Rieger. 1987): that is, it has been assumed that their speciation has taken place by
genetically fixed maturation of juvenile stages of macrofaunal hesionid taxa. Now, wc hypothesize that the
pilargid stem species also evolved by progenesis of a larger hesionid's juvenile stage. The juvenile development of
Source :
I’l IYLOGENETIC POSI TION OP Tl IE PILARGIDAE
227
non-in tersuual hcsionid species is characterized among other things by (1) a gradual increase in number
n S,min U’f dfVC fpmCn,a ser,es 01 Flg' 2) Possesses the entire set of five prostomial appendages but only one
achaelous tentacular segment with two pairs of almost smooth cirri (IIaaland & Schram 1983) Thus its'he id
morphology corresponds well with that of some pilargid taxa. ' ' ‘ d
nnenJmfh.c131 5? Pi,argi? Slem species ,niglu have solved by progenesis of a hcsionid taxon caused us to use
one of the hcsionid taxa as the outgroup taxon for die data matrix of our cladogram (Table 2).
METHODS
(rJpEPfSeir analySiS prese",ed1'lere was aided b-v ,ho computer program HENNIG 86, version 1 5
™R,S’ I98! '.n program considers 14 taxa. We considered 28 morphological characters and 68 character
. ales of which 40 are apomorphic (or 69 stales, 41 apomorphic, see below) for the analysis (Table 1) Characters
WoTf noSof Tly fr°m U,le Vari0US descriPlions> including the characters of the brain study bv Fitzhugh &
to. obsemso"s- Mui,is“e ci,aracicrs ■ ** <*• «*«•»
Ontogenesis
"C' t fpci ,lChralr repre.Se,n,a,i0n 0l,pr<)gene"c ori8in of a primitive pilargid secies from a hcsionid juvenile stage: a I -4
SH“ %7lT:r -SCneS °f 3 ,'0n'inI?li,iarl SPCdCS- W"h < ' > 8radual increase in number of achaefous head
n5®”tS' (2’ d *‘aduaI '««•» "> the number of tentacular cirri, and (3) an expansion of articulation in the cirral
ppendages, (see Haaland & Schram. 1983). b, anterior end of a primitive pilargid taxon.
228
F. LICHER & W. WF.STHEIDE
Table 1 . — Characters and character states used in the phylogenetic analysis to set up the cladogram. Characters 10, 12, 17.
18, 22, 26 and 28 are multistate characters. Character 19 is coded twice belonging to different evolutionary ideas
(see text lor details). State "a" is plesiomorphic. subsequent states are apomorphic.
Source :
PHYLOGENETIC POSITION OF THE PILARGIDAE
229
As it is difficult to decide whether the notopodial hook or die notopodial straight spine is die more apomorphic
S owi m d 'rkS a" i Spi"eS 3S h0m0l°80«s) ^ constructed two dam matrices to accommodate
the following different ideas (but see LiCHER, in press): (1) The hook is plesiomorphic and already present in the
EYiedrich 1 i r T and 28 characters used in the phylogenetic analysis. Outgroup is Hesionides
„. ?■ 1 m Character numbers and character states as in Table 1. Character 19 is subdivided belonging
to Afferent evolutionary ideas (see text for details). Cases in which the state is unknown or questionable
are indicated as . . cases in which the character is not present are indicated as
Hesionides
And st rosy II is
Cabira
dyphohesione
IJ to cor so
Loandalia
Otopsis
Paracabira
Parandalia
Para nd alia
Pi iar^ is
Sigambra
\ 234 5
0 0 000
00 100
?0 1 00
00000
? 0 10
11001
00000
Synetmis complex A
Synebnis complex B
Tatehsapia
7 0 10 7
11001
11001
00 100
00000
10000
10010
11001
67 890
00000
11001
11102
1 0070
10 11
11013
100 1
11073
110 13
110 13
1 10 7 1
11000
110 11
11071
11111
1 2 34 5
1 II
00 700
7 1000
1 3 000
0 0 000
71111
-30 11
1 17 7?
- 3 700
- 3 0 1 1
- - 1 73
-30 11
13010
1 0000
11111
7 1111
11112
6 7 8 9 0
070000
021121
012121
00021 1
001211
103210
7 7 1 3 0 7
012121
103210
103210
- 3 7 7 7
011301
0 0 0 1 2 7
101211
101211
773211
22 222
1 2 34 5
00000
0 1010
02110
0 0 111
0 1111
1 3 I 1 I
0 1110
03110
13 111
13 111
0 10 10
000 1 1
0 1111
0 1111
1 3 1 1 7
222
678
000
00
0 1 3
00 0
2 7 1
0 1 2
0 I 7
00?
072
072
00 1
000
1 0 1
2 0 1
002
Source
230
F. I.ICHER & W. WESTHEIDE
stem species of die Pilargidae: the spine is apomorphic and derived from a hook by simplification; the absence of
hooks and spines is secondary, possibly reduced several times. (2) Lack of hooks or spines is plesiomorphic; a
spine is apomorphic and evolved from a simple notochaeta within the Pilargidae; a hook is more apomorphic and
derived from a spine, possibly derived several times (see FlTZHUGH & Wolf 1990). Both ideas are reflected in
our data matrix (Table 2): character 19 (I) corresponds to the first idea, character 19 (II) to the second one.
The cladogram was constructed from the data matrix using the ie* command. This command generates
cladograms by implicit enumeration, producing all possible minimum-length cladograms. Successive character
weighting was carried out using the xs - w command. Computer runs were made on an IBM-compatible 486 DX,
33 MHz computer.
RESULTS
Considering the notopodial hook to be the plesiomorphic character state (coding I for character 19) only a
single cladogram is produced (Fig. 3a). The length is 63 steps, consistency index (c.i.) is 0.66, retention index
(r.i.) is 0.79. An analysis that considers the notopodial hook to be the most apomorphic state (coding II for
character 19) yielded two cladograms, one of which is the same as in coding I (Figs 3a-b). The lengths of the two
cladograms are 63 steps (c.i. 0.65, r.i. 0.78). Successive character weigtiiing yielded one minimum-length tree
(Fig. 3b).
The results of both codings are nearly the same: Glyphohesione is the adelphotaxon of all other pilargids, of
which Sigambra is the sister-group of the remaining 1 1 taxa. The latter genera are arranged in two groups and
Otopsis: (1) Ancistrosyllis , P Hargis, Cabira and Paracabira , and (2) die two Synelmis- complexes, Litocorsa,
Talehsapia , Parandalia and Loandalia . In both cladograms the relationships are identical with the exception of
O tops is (sec Figs 3a-b).
The two cladograms show Glyphohesione to be the pilargid with the highest number of plesiomorphic
characters (e.g., elongate palpostyles, lateral antennae located at die anterior margin of the prostomium). All other
pilargids bear papilla-like palpostyles (state 7b, Table 1 and Fig. 4) and lateral antennae located posteriorly (lib).
Glyphohesione is characterized by three autapomorphies (19c, 23b, 25b, using coding I) or by two
autapomorphies (19c, 23b, using coding II). The monophyly of Sigambra is questionable when the notopodial
hook is considered to be plesiomorphic (coding I).
Fhe Ancistrosyllis-group, Otopsis and the Synelmis- group possess prostomial, tentacular, parapodial and anal
appendages (10b, 12b, 18b, 22b, 28b), which are shorter than in Glyphohesione and Sigambra. The Ancistrosyllis -
group is clearly characterized by the possession of a papillatcd integument (2b) and a diree-lobed hindbrain (17b).
Using coding II the possession of a dorsal hook would be an additional synapomorphy. Ancistrosyllis may be
characterized by its five-lobed hindbrain (17c), whereas die stem-species of Pilargis, Cabira and Paracabira lost
die median antenna (12d). Autapomorphies of Pilargis are the loss of notopodial hooks (19d - reversion) and the
possession of a brain which is much longer than wide (14b). In the stem-species of Cabira and Paracabira further
reductions occurred (10c, 18c, 22c, 23b). Cabira bears jaws (8b) and lacks ventral cirri on chaetiger 1 as well as
anal cirri (27b, 28d). Paracabira lacks lateral antennae and dorsal cirri (lOd, 22d).
Otopsis and die Synelmis-group are equipped widi dorsal cirri on chaetigerous segment 1, which are not longer
than die following ones (23b). Otopsis is characterized by two reductions (19d, 27b). The Synelmis-group
possesses a series of synapomorphic features: a cylindrical body (lb), a pharynx without distal papillae (9b), only
simple capillary neurochaetae (25b), and several characters of brain gross morphology considered to be
characteristic for them by FlTZHUGH & Wolf (1990) (14b, 15b, 16b). Possession of a notopodial spine (19c) is an
additional synapomorphy of diis taxon when the hook is considered to be the plesiomorphic character state.
The two Synelmis complexes and Litocorsa possess two emergent neuropodial spines (26b) and lack nuchal
organs (13b) according to FlTZHUGH & Wolf (1990). The Synelmis -species (= Synelmis complex A plus Synelmis
complex B) can be shown to form a paraphyletic group. Synapomorphies for Synelmis complex B and Litocorsa
are die possession of pointed neuropodial spines (26c) and possession of a prostomium which is somewhat longer
than wide (4b). Autapomorphies for Litocorsa are an "entire" forebrain (16a - reversion) and fused palps. Presence
ol prostomial pigmented eyes may be the autapomorphy of Synelmis complex A. For the time being no
autapomorphies exist for Synelmis complex B.
Talehsapia , Parandalia and Loandalia show several synapomorphies: an inHated anterior body region (3b), a
largely reduced prostomium (5b), loss of lateral and median antennae, tentacular cirri and dorsal ciirfdOd, 12d,
18d, 22d), loss ot notopodial aciculae (21b), loss of ventral cirri on chaetiger 1 (27b). and possession of papilla-
PHYLOGENETIC POSITION OE THE PILARGIDAE
231
l ike anal cirri (28c ). Talehsapia is characterized by die possession of jaws (8b). The notopodia of Loandalia and
Ov, , o/ 'fl arC Ct|Uip.pc(1 Wl,h simP‘e capillary notochaetae accompanying the stout spine (20a - reversion)
PaZSlial rsr,e “ m"' h“ 1051 VCnml Cirri “ ch^’ 1 <27b>- of
DISCUSSION
— »* - -
a)
Hesionides
Glyphohesione
Sigambra
Paracabira
Cabira
Pilargis
A ncistrosyllis
Otopsis
Synelmis complex B
Litocorsa
Synelmis complex A
Talehsapia
Loandalia
Parandalia
b)
= Hesionides
Glyphohesione
Sigambra
Parandalia
Loandalia
Talehsapia
Synelmis complex A
Litocorsa
Synelmis complex B
Otopsis
A ncistrosyllis
Pilargis
Cabira
Paracabira
FlG,3_ h(S0!;'am7f,pi!ar8ld ge!,era usi,,S differem codinSs for character 19: a. the only cladogram produced using coding
I. b. the ictained cladogram after successive character weighting using coding II (see text for details).
A possible nereidid-pilargid relationship was mentioned, e.g., by Glasby (1990). A pilargid progenetic
evolution of nereidid I macroforms appears also conceivable, since nereidids possess a juvenile stage with two pairs
of tentacular cirri (Hauenschild & Fischer, 1969, Fig. 8) which resembles primitive pillrgid taxa e.g.
Sigambra). The nereidid juveniles, however, possess jaws, and lack a median antenna.
We, therefore, strongly support the Hesionidae as closest relatives of die Pilargidae. There is not only the high
similarity between juvenile hesionids and primitive pilargid taxa: both taxa also generally coincide in the
Source
232
F. LICHER & W. WESTHEIDE
morphology of head, parapodia and pharynx. 'Fhc genus Hesionides is only slightly less reduced than primitive
pilargids in possessing two tentacular segments and three tentacular cirri (see Fig. 1). However, die probability of
an independent progenetic evolution of both Hesionides and the pilargid stem species cannot be excluded.
The largest differences between Ilesionidae and Pilargidae were hitherto seen in their chaetation: pilargids
with their acicula-like stout notopodial hooks or spines and exclusively simple neurochaetae versus hesionids with
mostly capillary notochaetae and a neuropodial chaetation which always includes compound chaetae. Chaetation
in the two taxa, however, may be less different than formerly supposed: (1) Spines and hooks arc not homologous
to aciculae, but derived notochaetae, which in some cases occur togedier with a true acicula (as FHZHUGH &
Wolf. 1990 pointed out). (2) Just recently two hesionid species have been found witli apparent pilargid chaetal
features. Microphthalmus simplicichaetosus Wcsllicide & Purschke, 1992, has exclusively simple bidentate
neurochaetae. An undescribed Microphthalmus (WESTHEIDE, in prep.) is equipped with typical notopodial hooks.
Hartmann-Schroder (1962) described a Microphthalmus ancistrosylliiformis [sic!] because of its conspicuous
notopodial spines. A strong notopodial spine is also present in Hesiospina Imajima & Hartman, 1964. Without
doubt none of these species can be used as a sister-group for the Pilargidae. They demonstrate, however, that
potential tendencies toward pilargid chaetation exist in hesionid taxa.
FIG. 4. Cladogram of pilargid genera together with the outlines of anterior ends and parapodia. The outgroup is Hesionides
Friedrich, 1937. Solid rhombs represent apomorphies, open rhombs symbolize character reversals. Numbers refer to
characters in Table 1 .
Unfortunately, most of die hesionid-pilargid similarities may be considered to be plesiomorphic characters
going back to the stem species of the Nereidiformia. The autapomorphie character for the Ilesionidae with the
PHYLOGENETIC POSI TION OF THE PILARGIDAE
233
strongest probability may be a large number of tentacular cirri (eight pairs), which, however, is not present in the
hesionid juvenile stages (see above). Thus, even species assumed to be evolved from hesionid juveniles - the
pilargid stem species in our opinion - cannot possess this character. This renders it extremely difficult to
demonstrate a synapomorphy for Hesionidae and Pilargidae.
RELATIONSHIPS WITHIN the PILARGIDAE. — There is no evidence that a division of the Pilargidae into
Synelminae and "Sigambrinae" (Salazar-Valleio, 1986, 1990, Salazar-Vallejo & SOLlS-WEISS. 1992), or
Synelminae and "Pilarginae" (Salazar-Vallejo & Orensanz, 1991) is justified (see also Fitzhugh & Wolf,
1990). The "Sigambrinae" (="Pilarginae") consisting of Sigambra, Ancisirosyllis, Ancistargis, Pilargis, Ccibira
and Paracabirq are not based on any apomorphic feature.
Considering the absence of a notopodial hook in Pilargis and Olopsis to be a loss is more probable than to be
the plcsiomorphic state. In the latter case one must assume that a notopodial hook was independently evolved
three times: in Sigambra , in Ancistrosyllis, and in the stem-species of Ccibira and Paracabira. Therefore, Olopsis
is likely die adclphoiaxon of the Synelmis-g roup (Fig. 4).
The species of Lilocorsa and Synetmis complex B arc closely related (Fig. 4). Since no autapomorphies for the
latter could be found, inclusion of them in Lilocorsa is proposed. This taxon then contains the following species:
Lilocorsa anna mi la (Gallardo, 1967),
Lilocorsa stremma Pearson, 1970,
Lilocorsa dined (Katzmann, Laubier & Ramos, 1974),
Lilocorsa acuminata (Wolf, 1986),
Lilocorsa antennala Wolf, 1986,
Lilocorsa ewingi (Wolf, 1986),
Lilocorsa denial a Imajima, 1987.
The diagnosis of the genus Lilocorsa thus must be emended and reads as follows: "Body cylindrical.
Proslomium longer than wide, with two, three or without antennae. Palps incompletely or totally fused. Two pairs
of short tentacular cirri. Notopodial emergent spine present, neuropodia with two stout non-furcate spines besides
capillary ones. Pygidium with two short anal cirri."
Synelmis (= Synelmis complex A) differs from Lilocorsa (= Lilocorsa plus Synelmis complex B) in always
possessing three antennae, pigmented prostomial eyes and neuropodia with two stout furcate spines; it includes
ihe following species:
Synelmis albini (Langerhans, 1881),
Synelmis simplex Chamberlin, 1919.
Also for Parandalia no autapomorphies are obvious. Inclusion of the Parandalia- species in Locindalia ,
however, is not suggested. Some Parandalia- species show closer similiarities (synapomorphies?) to Loandalia
(absence of ventral cirri on chaetiger 1 (27b) in P. tricuspis (Miiller, 1858), P. ocularis Emerson & Fauchald,
1971, P. vivianneae Salazar-Vallejo, 1990; possession of a median anal cirrus in P. indica (Thomas, 1963), P.
ocularis Emerson & Fauchald, 1971 aid P. bennei Solis- Weiss, 1983).
Given that the pilargids evolved progenetically from a larger hesionid species, it follows that the Hesionidae
are a paraphyletic taxon if the Pilargidae are kept as an independent family. Phylogenetic systematic implications
consequently require that the Pilargidae be included in the Hesionidae and not be considered an independent
family. This suggestion is not so new at ail; especially Fauvel (1919a, 1919b, 1920, 1923, 1932), but also
Eulers (1908). Horst (1921), Southern (1921), Aucener (1927), Monro (1933), Mesnil & Fauvel (1939),
Berkeley & Berkeley (1941) and Treadwell (1941) positioned pilargid species in the taxon Hesionidae. The
phylogenetic systematical partitioning within such an enlarged family Hesionidae to create, e.g.. subfamilies must
be reserved till a comprehensive revision has been made of the "true" hesionid taxa.
ACKNOWLEDGEMENTS
We are indebted to Prof. Dr. K. Fauchald, Smithsonian Institution Washington (IJSNM), Dr. M.E.
Petersen, Zoological Museum, University of Copenhagen (ZMUC), L.I I. Harris, Los Angeles County Museum
of Natural History (LACMNII), Dr. D. FlEGE, Senckenberg Museum Frankfurt (SMF), and A. Nateewathana,
Phuket Marine Biological Center, Thailand for the friendly loan of pilargid species. Special thanks are due to Dr.
234
F. LICHER & W. WESTHEIDE
D. ElBYE-J ACOBSEN, (ZMUC) for his helpful advice in using IIENNIG86. Many ideas and comments he
provided have been of considerable help in setting up our cladograms.
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Berkeley, E. & BERKELEY, C., 1941. — On a collection of Polychaeta from Southern California. Bulk South. Calif. Acad.
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BRrrAEV, T.A. & Saphronova. M.A.. 1981. — New species of the family Pilargidae (Polychaeta) from the Sea of Japan and
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Eulers, E., 1908. — Die bodensassigen Anneliden aus den Sammlungcn der Deutschen Tiefsee-Expedition. Wiss. Ergeb.
Deutsche n Tiefsee-Exped. 1897-1899. 16 : 1-168.
ELIASON. A.. 1962. — Undersokningar over Oresund. 41: Weitere Untersuchungen uber die Polychaetenfauna des Oresunds.
Lunds Univ. Arsskr.. n.f.. 58 : 1-97.
EMERSON, R.R. & Fauchald. K., 1971. — A revision of the genus Loandalia Monro with description of a new genus and
species of pilargiid polychacte. Bull. South. Calif. Acad. Sci.. 70 : 18-22.
FARRIS, J.S.. 1988. Hennig 86 reference, version 1.5. New York. 41 Admiral Street, Port Jefferson Station 11776, 17 pp.
FAUCHALD. K., 1977. — The polychacte worms. Definitions and keys to the orders, families and genera. Nat. Hist. Mus. Los
Angeles County, California. 28 : 1-190.
FaUVEL. P.. 1919a. — Annelides Polychetes des lies Gambier et Touamotou. Bull Mus. nail Hist. not.. Paris. 25 : 336-343.
FAUVEL. P.. 1919b. — Annelides Polychetes de Madagascar, de Djibouti et du Golfe Persique. Zool. Exp. Gen.. Paris , 58 :
315-473.
FAUVEL, P.. 1920. Les genres Ancistrosyllis et P Hargis (We sionidae). Bull. Soc. Zool. Fr.. 45 : 205-213.
FaUVEL. P.. 1923. — Polychetes Errantes. Faune Fr ., 5: 1-488.
FAUVEL, P.. 1932. — Annelida Polychaeta of the Indian Museum, Calcutta. Mem. Indian Mus., Calcutta. 12 : 1-262.
FlTZHUGH, K. & Wolf, P.S.. 1990. — Gross morphology of the brain of pilargid polychaeles: Taxonomic and systematic
implications. Anier. Mus. Nov.. 10024 (2992) : 1-16.
Friedrich, H., 1937. — Polychaetenstudien I - HI. Kieler Meeresforsch.. 1 : 343-345.
Gardiner. S.L.. 1976. — Errant polychaete annelids from North Carolina. J. Elisha Mitchell Sci. Soc.. 91 : 77-220.
Glasby, C.J.. 1990. — Phylogenetic relationships in the Nereididae (Annelida: Polychaeta), chiefly in the subfamily
Gymnonereidinae, and the monophyly of the Namanereidinae. Bull. Mar. Sci.. 48 : 559-573.
Haaland, B. & SCHRAM, T.A.. 1982. — Larval development and metamorphosis of Gyptis rosea (Hesionidae, Polychaeta).
Sarsia. 67 : 107-118.
Haaland. B. & SCHRAM, T.A., 1983. Larval development and metamorphosis of Ophidromus flexuosus (Delie Chiaje)
(Hesionidae, Polychaeta). Sarsia. Bergen , 68 : 85-96.
Hartman, O., 1959. — Catalogue of the polychaetous annelids of the world. Part 1. 2. Allan Hancock Found. Publ. Occ.
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HarTMANN-SchrOder. G.. 1962. — Zur Kennlnis des Eulitorals der chilenischen Pazifikkiiste und der argentinischen Kiiste
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Mitt. Hamb. Zool. Mus. Inst.. Erganzungsband zu 60 : 57-167.
IlAUENSCHlLD, C. & FISCHER. A.. 1969. Platynereis dumerilii. Mikroskopische Anatomie. Fortpflanzung, Entwicklung.
GroBes Zoologisches Praktikum, Fischer. Stuttgart. Heft 9b : 1-55.
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Horst. R., 1921. — A review of the family of Hesionidae with a description of two new species. Zool. Meded., Leyden. 6 :
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Imajima. M. & Hartman, ().. 1964. — 'Hie polychactous annelids of Japan, pt. 1 .Allan Hancock Found. Pubi Occ. Pap..
26: 1-237.
JONHS. Ml... 1961. — Two new polychaetes of the families Pilargidae and Capitellidae from the Gulf of Mexico. Amer. Mus.
Nov.. 2049 : 1-18.
LaUBIER. L., 1967. — Adaptations chez lcs Annelides Polychetcs interstitielles. Ann. Biol.. 6 : 1-16.
MESNIL. F. & PaUVEL, P.. 1939. — Polychetcs sedentaires de l’expedition du Siboga: Maldanidae. Cirralulidae, Capitellidae.
Sabellidae et Serpulidac. S i bog a -Exp edit ion. 24 : 1-42.
MlURA, T. & LAUBIER, L.. 1989. — Naulilina calyptogenicola, a new genus and species of parasitic polychaete on a
vesicomyid bivalve from the Japan Trench, representative of a new family Nautiliniellidae. Zool Sci., Japan, 6 : 387-390.
Monro. C.C.A., 1933. — On a new species of Polychaeta of the genus Pilargis from Friday Harbour. Washington. Ann. Mag.
Nat. Hist.. 10(11) : 673-675.
PETTI BONE, M.H., 1966. — Revision of the Pilargidae (Annelida: Polychaeta). including descriptions of new species, and
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Paris , 5:41-42.
Salazar- Vallejo, S.I.. 1986. — Pilargidae (Annelida: Polychaeta) de Mexico: Lista de especies, nueva especie y biografia.
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Salazar- Vallejo, S.I.. 1990. Redescriptions of Sigambra grubii Muller. 1858 and Hermundura tricusp is Muller, 1858
from Brazil and designation of neotypes (Polychaeta: Pilargidae). J. Nat. Hist.. 24 : 507-517.
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Salazar- Vallejo. S.I. & SOLfs- WEISS. V.. 1992. Biogeography of the pilargid polychaetes (Polychaeta Pilargidae) of the
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WESTHEIDE, W., 1987a. — The interstitial polychaete Hesionides pettiboneae n.sp. (Hesionidae) from U.S. east coast and its
transatlantic relationship. Bull. biol. Soc., Wash.. 7 : 131-139.
WESTHEIDE, W.. 1987b. — Progenesis as a principle in meiofauna evolution. J. nat. Hist.. 21 : 843-854.
WESTHEIDE, W. & PURSCHKE, G.. 1992. Microphthalmus simplicichaetosus (Annelida: Polychaeta), a new hesionid from
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WESTHEIDE, W. & RIEGER. R.M., 1987. — Syslematics of the amphiatlantic Microphthalmus-listensis species-group
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Source : MNHN. Paris
24
Pseudatherospio fauchaldi, a new genus and species
of Spionidae (Polychaeta, Annelida) from
southern California, USA
Lawrence L. LOVELL
1036 Buena Vista Drive, Vista
California 92083-7411, USA
ABSTRACT
Pseudatherospio fauchaldi . a new genus and species of Spionidae is described from material collected from a depth of
197 m off Huntington Beach, southern California. The main characteristics of the genus are the distribution and shape of
branchiae, the presence of fringed neuropodial setae in anterior setigers and the structure of modified neuropodial hooks
in posterior setigers. Generic affinities are discussed. Pseudatherospio most closely resembles Atherospio Mackie &
Duff, 1986 and Pygospiopsis Blake. 1983.
RESUME
Pseudatherospio fauchaldi , genre et espece nouveaux de Spionidae (Annelides, Polychetes) de
Californic du Sud
Pseudatherospio fauchaldi , genre et espece nouveaux de Spionidae esl decrit a partir de materiel recolte par 197 m de
profondeur au large d Huntington Beach. Californic du sud. La distribution et la forme des branchies presentes des le
premier setigere. la presence de soies neuropodiales frangecs aux setigeres anlericurs et la structure des crochets modifies
des setigeres postdrieurs dont la dent secondaire est situee au-dessous de la dent principale du cote concave du crochet sont
les caracterisliques essenlielles du genre. Les affinites generiques avec les genres les plus proches, Atherospio Mackie &
Duff. 1986 and Pygospiopsis Blake. 1983 sont discutees.
INTRODUCTION
A new genus and species of Spionidae is described from a sample collected at a depth of 197 m off Huntington
Beach, southern California, during July 1991. Specimens were collected by MEC Analytical Systems, Inc.
(contract number 02091) as part of the E.P.A. 301(h) waste water outfall monitoring program of the County
Sanitation Districts of Orange County (CS DOC).
Type material has been deposited in the following museums: Allan Hancock Foundation Polychaete Collection
Lovell, L.L., 1994. - Pseudatherospio fauchaldi , a new genus and species of Spionidae (Polychaeta, Annelida) from
Southern Calilornia. USA. In: J.-C. DaUVIN, L. Laubier & D.J. REISH (Lds). Actcs de la 4eme Conference internationale
des Polychetes. Mem. Mus. natn. Hist, nat .. 162 : 237-241. Paris ISBN 2-85653-214-4.
238
L.L. LOVELL
of the Los Angeles County Museum of Natural History, Los Angeles, California (LACM-AIIF) and National
Museum of Natural History, Washington, D.C. (IJSNM).
SYSTKMATICS
Pseudo therospio gen. nov.
Type species. — Pseudatherospio fauchaldi sp. nov. Gender, feminine.
Diagnosis. — Prostomium longer than wide, anterior margin bilobed, tapering posteriorly; eyes absent;
occipital tentacle present. Branchiae from setigcr 1 to at least setiger 36; outer margin fused with notopodial
lamellae on setigers 7-15 or 16, free otherwise; terminate with short, digitate process. Interramal 'genital' pouches
absent. Setigers 2-16 with dorsal intrasegmental and intersegmental ciliary bands. Parapodia biramous. Notosetac
capillary. Neurosetae include capillary setae; fringed setae; bidentate, strongly-curved, hooded hooks. Sabre setae
absent. Pygidium unknown.
Etymology. — The generic name refers to the close resemblance to Atherospio Mackie & Duff, 1986.
A
0 . 1 mm
Pig. 1. — Pseudatherospio fauchaldi gen. sp. nov. A, Anterior end. dorsal view. B. Anterior end. lateral view. C,
Parapodiuin from setiger 1, anterior view. D, Parapodium from setiger 5. anterior view.
Source : MNHN. Paris
PSEUDA THEROSPIO FAUCHALDI NEW SPIONID FROM SOUTHERN CALIFORNIA
239
Pseudatherospio fauchaldi sp. nov.
(Figs i & 2)
Material. — Pacific Ocean, Southern California, R. V. CRUSADER; collector: C. FULLER, station 25,
33°33,48"N. 1 18°02*1 F'W, 197 in, green mud, 24 July 1991, holotype (LACMNH-AHF1650), 1 paratype
(LACM-AHF1651) and 1 paratype (USNM163804).
Description. — Holotype incomplete, with 36 setigers; total length 9.5 mm; width 0.8 mm (excluding
parapodial lobes) at setiger 1, 1.3 mm at setiger 6. Paratypes incomplete, each with 22 setigers; total length
6.7 mm and 9.6 mm, respectively; width 0.8 and 1.8 mm at setiger 1, and 1.9 and 3.7 mm at setiger 6,
respectively.
Prostomium longer than wide, anterior margin hilobed, tapering posteriorly to setiger 1; eyes absent; occipital
tentacle short, distally tapering, emerging from anterior margin of setiger 1 (Fig. 1A-B). Pair of grooved palps
inserted on peristomium near postero-lateral margins of prostomium, extending to setiger 12. Peristomium poorly
developed, only visable along postero-lateral margin of prostomium, remainder fused to setiger 1. Small,
transverse nuchal organs present behind palps at anterior margin of setiger 1. Everted proboscis delicate, translucent
sac with medial groove and low, conical papillae on the fronto-lateral margin (Fig. 1A-B).
Fig. 2. Pseudatherospio fauchaldi gen. sp. nov. A. Parapodium from setiger 9. anterior view. B, Parapodium from
setiger 26. posterior view. C. Fringed seta and capillary seta from setiger 5. D. Neuropodial ramous from setiger 20.
E. Neuropodial hooded hook from setiger 20.
240
L.L. LOVliLL
Parapodia biramous. Notopodial postsetal lamellae long, triangular on setiger 1 (Fig. 1C); shorter and more
broad bv setiger 5 (Fig. ID); completely fused with outer branchial margin on setigers 7-15 or 16 (Fig. 2 A); long,
triammlar after setiger 15 or 16 (Fig. 2B). Neuropodial postsetal lamellae broadly triangular onset. gerlFig.C;
shorter and more broad by setiger 5 (Fig. ID): a low mound on setigers 7-15 or 16 (Fig. 2A). lamellae short,
broad lv triangular after setiger 16 or 1 7 (Fig. 2D). Ventral scutes or pads absent.
Branchiae begin on setiger 1, on all setigers present. Branchiae cirriform and tree from notopodial lamellae on
setigers 1-6 and 15 or 16-36 (Figs 1C-D. 2B): branchiae fused to lamellae on setigers 7-14 or 15, with inner lateral
margins densely ciliated (Fig. 2A). Branchiae terminate with a short, narrow, digitate process; greatly reduced in
size on setigers 7-14 or 15 (Figs 1C-D, 2A-B). Intersegmcntal ciliary bands on setigers 2-10 poorly-developed (Fig.
1A). Intrasegmental ciliary bands on setigers 2-4 poorly-developed, well-developed on setigers 5-16 (Fig. 1A).
Interram al "genital" pouches absent. Pygidium unknown. Body color white m ethanol.
Notosetae capillary. Neurosetae include capillary setae, fringed setae, and bidentate hooded hooks. Capillary
neurosetae of seugers 1-3 and 7-16 arranged in large superior bundle and small inferior bundle. Neuropodia of
setigers 4-6 with two rows of 8-9 fringed setae each in superior bundle and 5-6 capillary setae in interior bundle
(Fi<f 2C) Neuropodia from setiger 17 with 3-5 strongly-curved, bidentate hooded hooks alternating with paired
capillary setae in the superior bundle; 2-6 capillary setae in the inferior bundle (Fig. 2D). Hooks with secondary
tooth subdistal, inferior to large tooth; hood originating just below secondary tooth and terminating leaving tip ol
distal tooth exposed (Fig. 2E). Sabre setae absent.
Etymology. — This species is named for Dr. Kristian FAUCHALD m honor ol his many contributions to
polychaete systematics and for his support and friendship over die years.
Distribution. — Off Huntington Beach, southern California, 197 m.
Remarks. — Pseudatherospio closely resembles Atherospio Mackie & Duff, 1986 and Pygospiopsis Blake,
1983 Table 1 compares features in the diree genera. The type material of Atherospio disticha Mackie & Dun,
1986 and Pygospiopsis dubia (Monro, 1930) was examined. All three genera possess a bilobed prostomium, a
median occipital tentacle, notopodial lamellae fused to branchiae in setigers 7-12 up to 16, modified anterior
neurosetae. and bidentate neuropodial hooks. The bidentate hooks have a small, secondary tooth inferior to the
large tooth (Figs 2D,E). This arrangement of teeth is the reverse of what is usually found in the Spionidae, and
readily unites these three genera as a group within the family. Contrary to the account ol Mackie & Duff (1786).
the hooks of Pygospiopsis dubia are mostly bidentate, with larger, more worn, hooks being umdentaic or having a
reduced inferior tooth.
Table 1 . — Taxonomic characters of the genera Pseudatherospio gen. nov., Atherospio Mackie & Dull, 1986,
and Pygospiopsis Blake, 1983.
Despite the similarity of branchial structure, die distribution of branchiae distinctly separates Pseudatherospio.
Pygospiopsis and Atherospio from one another. Branchiae occur on setiger 1 to at least setiger 36 in
Pseudatherospio. on setigers 2, 3 and 7 to about 16 in Pygospiopsis and on setigers 7 to 12 in Atherospio. The
distribution of branchiae is an important generic level character in the Spionidae (see Fauchald, 1977 and
Foster, 1971). For example, MACIOLEK (1990) separates Spio and Microspio based on the position of the first
pair of branchiae (setiger 1 vs. setiger 2, respectively).
The presence of anterior neuropodial modified setae is not common in the Spionidae (see Mackie & DUFF ,
1986). Pseudatherospio and Pygospiopsis bodi have fringed neurosetae setae in setigers 4-6 and 4-7 up to 9,
respectively. The presence of these fringed anterior neurosetae in Pygospiopsis was not reported in previous
Source : MNHN. Paris
PSEUDATHEROSPIO FAUCHALDI NEW SPIONID FROM SOUTHERN CALIFORNIA
241
accounts by Monro (1930) or Blake (1983). Atherospio has aristate neuroselae in setigers 4-5 Two other
spionid genera, Scolecolepides (Ehlers, 1907) and Lindaspio Blake & Maciolek. 1992, also have modified anterior
neuropodia] setae; but ihese genera can be separated based on the presence of prostomial frontal horns, die absence
ol an occipital tentacle, and (he presence of notopodial modified hooks in posterior setigers (see Macioi ek 1984
and Blake & Maciolek, 1992).
The anteriorly bilobed prostomium, occipital tentacle, similarity of branchial structure, presence of modified
anterior neuroselae, and structure of neuropodial hooded hooks all suggest that Pseudatherospio, Atherospio, and
Pygospiopsis are a closely related, geographically wide-spread complex of genera. Mackie (pers. comm.) is
currently investigating the status of a second species of Atherospio from the south coast of England, as well as
some related lonns that appear to belong to two undescribed genera. One of the proposed new genera is present in
the coastal waters of both the United Kingdom and Hong Kong, providing further evidence for a widely distributed
complex.
AC KNOW] JUDGEMENTS
1 would like to thank Dr. Doug D1ENF.R MEC Analytical Systems and Tom Gerlinger, CSDOC, for making
die material available. 1 hanks to Leslie Harris for her helpful discussion and examination of specimens: to Tom
1 ARKER, County Sanitation Districts of Los Angeles County and Ron Velarde, Metro Ocean Monitoring
Program, C ity of San Diego lor access to microscope facilities to produce drawings and photos. Fundin'’ for
illustrations and reprints was made possible by Grants 92-2 and 94-1 from the Southern California Association of
Marme Invertebrate Taxonomists. Illustrations were prepared by Julie SCHNEIDER. Special thanks to Dr. Kristian
Fauchald, Andrew S.Y. Mackie. Dr. Kirk FlTZHUGH, Karen GREEN, Leslie Harris, Dr. James A. BLAKE,
and an anomynous reviewer for their valuable comments. Thanks to Michelle Patzius for help in the production
ol the poster version presented at the Fourth International Polychaete Conference Angers, France. Finally, I would
like to thank my wife. Jacqueline, and my children, Andrew and Robin, for dieir love and support during die
preparation of this paper. This paper is Contribution No. 9 of die Southern California Association of Marine
Invertebrate Taxonomists.
REFERENCES
Blake. J.A.. 1983. — Polychaetes of the family Spionidae from South America, Antarctica, and adjacent seas and
islands. Award. Res. Ser. (American Geophysical Union), 39 : 205-288.
Blake, J.A. & N.J. Maciolek, 1992. — Polychaeta from deep-sea hydrothermal vents in the Eastern Pacific. HI. A new
genus and two new species of Spionidae from the Guaymas Basin and Juan de Fuca Ridge with comments on a related
species from the Western Atlantic. Proc. biol. Soc. Wash ., 105 : 723-732.
Fauchald. K.. 1977.— The polychaete worms. Definitions and keys to the orders, families, and genera. Sci. Ser. Nai.
Hist. Mus. lx)s Angeles County. 28 : 1-190.
FOSTER. N.M., 1971. - Spionidae (Polychaeta) of the Gulf of Mexico and the Caribbean Sea. Studies on the Fauna of
Curacao and other Caribbean Islands. 36 : 1-183.
Maciolek. N.J., 1984. — New records and species of Marenzelleria Mesnil and Scolecolepides Ehlers (Polychaeta:
Spionidae) from northeastern North America. In: P.A. HUTCHINGS (ed.), Proc. First International Polychaete
Conference. Linncan Society of New South Wales : 48-62.
Maciolek, N.J.. 1990. A redescription of some species belonging to the genera Spio and Micro s pi o
(Polychaeta: Annelida) and descriptions of three new species from the northwestern Atlantic Ocean J Nat Hist
24: 1109-1 141.
Mackie. A.S.Y. & A.L. DUFF, 1986. — Atherospio disticha gen. et sp. nov. (Polychaela:Spionidac) from Loch Tuirnaie
West Coast of Scotland. Ophelia. 25 : 139-146.
MONRO, C.A.A.. 1930. — Polychaete Worms. Discovery Rep. .2 : 1-222.
Source : MNHN, Paris
25
Adercodon pleijeli gen. et sp. nov. (Polychaeta,
Ampharetidae) from the Mediterranean Sea
Andrew S. Y. MACKIE
Department of Zoology
National Museum of Wales
Cathays Park
Cardiff CF1 3NP, Wales. UK
ABSTRACT
Adercodon pleijeli gen. et sp. nov. is described from muddy sediments (32-95 m depth) off Banyuls-sur-Mer. France
and the east coast of Sicily. Italy. Characterised by 3 pairs of smooth branchiae. 13 thoracic setigers (paleae lacking),
thoracic uncini from setiger 4 and papillose buccal tentacles the new form differs from all known ampharetid genera.
Nevertheless, the possession of a ventral row of buccal teeth suggests an affinity with Gnaihampharete Dcsbruyeres,
1978. The arrangement and position of the teeth along the leading edge of the innermost ventral lip suggests that such
teeth are functional and not an evolutionary remnant. Certain aspects of the taxonomy of the Ampharetidae are discussed.
RESUME
Adercodon pleijeli gen. ct sp. nov. (Polychetes Ampharetidae) cn mer Mediterranee
Adercodon pleijeli gen. el sp. nov. esl decrit dcs substrats vaseux (32-95 in de profondeur) dc Banyuls-sur-Mer, France
et de Sicile orientale, Italie. Caraclerisee par trois paires dc branchies lisses, 13 setigeres thoraciques (pas de patees). des
uncini thoraciques a partir du setigere 4 et des tenlacules buccaux pennes, la forme nouvelle se distingue de tons les autres
genres d'Ampharetiens. Cependant, 1'exislence dune serie unique de dents buccales suggere une affinite avec
Gnaihampharete Dcsbruyeres, 1978.
INTRODUCTION
A small ampharetid worm that could not be assigned to any known genus was first noted during field collecting
at Banyuls-sur-Mer, France in October 1991. The same animal was subsequently found in unidentified samples
collected in Sicily the previous May. Later microscopical examination of specimens from both localities
surprisingly revealed the presence of buccal teeth in addition to papillose tentacles. The new form is described and
compared to Gnaihampharete paradoxa Desbruyfcres, 1978, the only other ampharetid known to possess teeth.
Mackii-:, A.S.Y., 1994. - Adercodon pleijeli gen. et sp. nov. (Polychaeta: Ampharetidae) from the Mediterranean
Sea. In: J.-C. DaUVIN. L. LaUBIER & D.J. REISH (Eds). Actcs dc la 4eme Conference internationale des Polychetes. Mem.
Mus. natn. Hist. not.. 162 : 243-250. Paris ISBN 2-85653-214-4.
244
A. S. Y. MACKIE
MATERIALS AND METHODS
The specimens used in this study were obtained from dredge, or combined dredge and sledge, samples sieved
Usin" a 0 5 mm mesh. The latitude and longitudes of the Sicilian sampling positions were estimated from local
landmarks no position fixing system being available. Most specimens were sorted live and fixed in formalin (20-
30 % in seawater), though some were obtained from bulk Mg Cl2 relaxed samples prior to fixation in formalin
(NMW Z 1992.00.3.8-9) or Bouin’s fluid (NMW.Z. 1992.003.1-2). In all cases specimens were washed in
freshwater prior to preservation in 80 % alcohol. All drawings were prepared with the aid of a camera lucida.
Epidermal glandular regions were highlighted by methyl green staining (NOLTE, 1913; IIofsommer, 1913;
Banse, 1970). Specimens were placed in a strong solution of stain, in 80 % alcohol, lor about one minute.
Excess stain was removed by a quick rinse using clean alcohol. The remaining staining pattern was then noted.
Type material was deposited in the following institutions: National Museum of Wales, Cardiff (NMW);
Musdum National d'Histoire Naturelle, Paris (MN1IN); Swedish Museum of Natural History, Stockholm
(SMNH); United States National Museum of Natural History. Washington, D. C. (USNM); Australian Museum,
Sydney (AM).
SYSTEMATIC ACCOUNT
Adercodon gen. nov.
Type species. — Adercodon pleijeli sp. nov.
DIAGNOSIS. — Prostomium trifid, lacking glandular ridges. Buccal cavity with papillose tentacles and single
series of pointed teeth arranged along leading edge of innermost lower lip. Three pairs of smooth branchiae,
arranged 2: 1 either side; posterior pair followed by pair of short nephridial papillae. Thirteen thoracic setigers from
segment IV; paleae and modified notopodia lacking. Ten thoracic uncinigerous segments from setiger 4 (segment
VU). Notosetae simple, capillary. Thoracic and abdominal uncini aviculopectinate. Pygidium with eyespots and
circlet of anal cirri.
ETYMOLOGY. — The generic name is derived from Aderk.es (Or.) -unseen or unexpected, and odous (Gr.)
-tooth. Gender, masculine.
Adercodon pleijeli sp. nov.
Figs la-g: 2a-d
MATERIAL examined. — France. Banyuls-sur-Mer: sample 5, 42°30.17'N, 3°09.48'E, mud with detritus,
40 m, 7.X. 91, two paratypes (NMW.Z. 1992.003.6-7). — Sample 8, 42°29.75'N. 3°09.00’E, sandy mud, 32 m,
11 X 91, two paratypes (NMW.Z. 1992.003.8-9). — Sample 11, 42°30.00’N, 3°16.50,E, muddy sand, 90 m,
14.X. 91, one paratype (NMW.Z.1992.003.10), five paratypes (SMNH 4535). — Sample 12, 42°30.00'N,
3°1 1.75'E, mud. 80 m, 14.X.91, five paratypes (NMW.Z.1992.003. 11-13). four paratypes (AM). — Sample 14,
42°29.90'N, 3°10.75'E, coarse sandy mud. 65 m, 15.X.91, one paratype (NMW.Z.1992.003. 14). — Sample 15,
42°29.55'N, 3°09.90'E, mud with detritus, 45 m, 15.X.91, holotype (NMW.Z.1992.003. 1), five paratypes
(NMW.Z. 1992.003 .2-5), three paratypes (MNHN, UC 793), two paratypes (USNM 157618). — Italy. Sicily :
sample T 8/9, off Aci Castello, 37o33.00'N, 15°10.70'E, muddy sand, 65-70 m, 16.V.90, four paratypes
(NMW Z. 1992.002.1). — Sample T 15/17, off Aci Castello, 37°32.50'N, 15°10.80'E, muddy sand. 90-95 m,
17.V.90, two paratypes (NMW.Z. 1992,002.2). 4 paratypes (SMNH 4536). — Sample T 32, off Castellucio
(Brucoli), 37°17.00'N, 15°13.00'E, mud with detritus, .35-45 m, 22.V.90, two paratypes (NMW.Z. 1992.002.3),
four paratypes (MNHN. UC 794), four paratypes (USNM 157619). — Sample T 34/35, off Castellucio (Brucoli),
37°18.00'N. 1 5°13.00'E, mud with Phyllochaetopierusl tubes, 60-70 m, 23.V.90, one paratype
(NMW.Z. 1992.002.4).
DESCRIPTION. — Specimens small, 1. 5-5.0 mm long (thoracic width 0.15-0.50 mm), with subcylindrical
thorax and tapering abdomen. Holotype entire, 4.8 mm long (thoracic width 0.5 mm), with partially extruded
upper (tentacular membrane) and lower lips (Fig. la) : branchiae and almost all buccal tentacles missing.
Source : MNHN, Paris
A NEW AMPHARETTD FROM THE MEDITERRANEAN SEA
245
Fig. 1. Adercodon pleijeli. (a. b: hololype: c: NMW.Z..1992.003.6: d-g: NMW.Z. 1992.003 .4-5): a, whole animal,
lateral view (upper and outer lower lips partially extruded); shading represents methyl green staining. — b. head
region, dorsal view (branchiae lacking). - c, head region, dorsal view. — d. thoracic uncini. frontal view. — e.
thoracic uncini. lateral view.— f, abdominal uncini, frontal view. — g, abdominal uncini. lateral view.
Abbreviations: LO, outermost lower lip; LU, upper lip.
Source :
246
A. S. Y. MACK1E
Prostomium trifid (Fig. lb); median part bell-shaped, anterior margin broadly rounded to triangular; lateral
lobes curved pointed, only basally united to median part. Single pair of round red-brown eyes posterolaterally, near
points of fusion of prostomial lobes; several small black supplementary eyespots medially and laterally at
approximately same level. Segment I visible as complete ring, ventral part forming lower margin of mouth.
Segment II narrower Ilian segment I, largely hidden by segment III.
Buccal tentacles retractile, papillose; each densely ciliated with bilaterally arranged papillae d ig. zb).
Tentacular papillae long, filiform; each with swollen tip bearing distal tuft of cilia. Buccal cavity ventrally with
sinde curved and unbroken row of 30-40 triangular teeth along leading edge of innermost lip (Figs 2a, c). In
profile teeth appear- V-shaped. From examination of slide preparations each tooth revealed to be sub-conical,
laterally compressed and hollow (Fig. 2d); superior root somewhat Hared terminating in large projecting peg;
inferior root long, slender and tapered.
Three pairs of ciliated cirri form branchiae (Fig. lc); anterior 2 pairs basally fused, separated by medial gap,
arranged transversely at level of segment III; third pair, shorter, more slender, arising separately behind anterior
pairs. Third branchial pair followed by pair of short rounded nephridial papillae in slightly more medial position
Segment III collar-like, slightly expanded dorsolaterally forming rounded lobes; paleae lacking. Thirteen
thoracic setigers from segment IV; notopodial lobes cylindrical, well-developed with 4-8 slender sheathed capillary
setae; modified notopodia and notosetae lacking. Ten thoracic uncinigerous segments from setiger 4 ; anterior
neuropodial tori inconspicuous with 2-5 uncini, posterior neuropodia more noticeable with 9-12 uncini in vertical
row (usually one lower uncinus situated posterior to row on all except first few anterior uncinigers). Uncini small
with main fang surmounted vertically by one supplementary tooth (latter sometimes lacking), both together being
surrounded cowl-like by one or two rows of 5-8 secondary teeth (Fig. Id) : second row of small denticles often
inconspicuous. Some larger uncini with two supplementary teeth vertically above main fang; others slightly
asymmetrical with secondary teeth arranged in two uneven vertical rows. In profile uncini aviculopectinate with
apparent vertical series of 3-5 teeth (Fig. le).
Ten abdominal setigers; neuropodial tori of anterior two setigers similar to those of thorax (including
arrangement of uncini). remaining neuropodia developed as extended pinnules. Each neuropodial pinnule with 6-14
uncini individually situated on distal tips of single scries of digitiform projections along outer margin; uncini
attached by long tendons. Uncini initially similar to those of thorax but by third or fourth abdominal setiger most
lack supplementary teeth in vertical position above main fang and uncini become smaller, more squat and rounded
in appearance. These and all other abdominal uncini with main Tang surrounded by two obvious rows of 6-9
secondary teeth (Fig. If): third row of tiny denticles sometimes visible. In profile uncini aviculopectinate with
apparent vertical series of 3 or 4 teeth (Fig. lg). Each neuropodium with single cirrus arising from superior
margin; cirri long and very conspicuous on anterior 5 or 6 setigers, becoming increasingly shorter towards
pygidium (Fig. la). Abdominal notosetae lacking but single small rounded ciliated tubercles evident in notopodial
positions (inconspicuous on posteriormost segments). Small triangular papilla evident between each neuropodial
cirrus and ciliated tubercle. Pygidium with terminal anus surrounded by circlet of about six cirriform papillae.
Lateral pair of anal cirri more robust, basally with single small black eyespots.
Use of methyl green (Fig. la) revealed intense staining of pre-branchial region, particularly on prostomial
lobes. Staining of segments I and II slightly lighter. Lateral and ventral parts of segments III-V (setiger 2)
similarly stained. Thereafter (until setiger 11) staining largely restricted to presetal lateral/ventral bands. Dorsal
region of thorax largely unstained; staining only evident as small widely scattered spots. Abdomen unstained.
Specimens (in alcohol) yellowish or pinkish white. Some specimens with remnants of thin mucous lube.
Many specimens ovigerous; ova large, rounded, up to 125 pm diameter.
Etymology. — It is a pleasure to name this new species after Dr. Fredrik Pleijel, my good friend and fellow
researcher, in recognition of his work on the Polychaeta.
Habitat. — I'he new species occurs in muddy sediments, with or without tcrrestrial/seagrass detritus, in
shallow shell' depths (< 100 m). The physical and biological characteristics of the type locality off Banyuls have
been detailed previously by GOT et al. (1968), GuiLLE & Soyer (1968, 1970) and Guille (1970). The species
was found throughout the four subdivisions of the Amphiura filiformis community as recognised by GUILLE &
Soyf.r (1970): Scoloplos armiger facias (samples 8 & 15), Venus ovata subcommunity (samples 5 & 14). Nucula
sulcata subcommunity (sample 12) and Auchenoplax crinata subcommunity (sample 11). However, in all cases its
occurrence was low (one lo six per dredge sample).
Source :
A NEW AMPIIARETID FROM THE MEDrrERRANHAN SEA
247
Fig. 2. — Adercodon pleijeli. (a: NMW.Z. 1992.003.8; b: NMW.Z.1992.003.10; c: NMW.Z.1992.003.7): a. head
region, sagittal section. — b, distal region of tentacle, dorsal view. — c, portion of row of buccal teeth ventral
view. - d. derived shape of individual buccal tooth, lateral view. Abbreviations; Br, branchia; LI, innermost lower
lip; I.O. outermost lower lip; LU, upper lip; Oe, oesophagus; Pr, prostomium; Te, tentacle; To. tooth.
Information on the benthos off eastern Sicily is more limited (see Gambi el al., 1985, for bibliography).
Cantone (1970) and CANTONE & Fassari (1983) provide some information on the polychaetes present in the
Gull of Catania region where Adercodon was found.
Remarks. — According to the literature (e.g. Fauchald, 1977; Holthe, 1986c), Muggoides cinclus
Hartman, 1965 is the only other member of the Ampharetinae to possess three pairs of branchiae and 13 thoracic
setigers with the last 10 uncimgerous. Adercodon pleijeli differs markedly in having buccal teeth and papillose
(not smooth) tentacles, and in lacking dorsally displaced notopodia and modified notosetae. The presence of buccal
248
A. S. Y. MACKE
teeth appears 10 ally Adercodon wiUi Gnatliampliarete Dcsbruyeres. 1978, Hie only oilier ampharctid known lo have
similar structures. Adercodon differs notably in having only three pairs of smooth branchiae rather than four pairs
of penmate ones, in having 13 thoracic setigers with 10 uneinigerous rather than 14 with 12, and in lacking paleae.
Consideration of certain selected characters could possibly align the genus with oilier genera however, in each
case, the differences between the taxa seem more numerous than the similarities. For example, while
Decemunciger Zottoli, 1982 has the same thoracic complement, it differs in having four pairs of branchiae and
smooth tentacles, and in lacking anal cirri. Ymerana Holthe, 1986 would likewise have the same thoracic
complement should the expanded and asetous notopodial expansions of the setiger 14 be interpreted as abdominal
rather than thoracic. Even so, this genus differs in having smooth tentacles; the form of the branchiae and pygidial
region are unknown.
It should be noted that Gnatliampliarete was reported as lacking buccal tentacles and Holthe (1986c: 46)
considered this to be die normal condition in this genus. However, Holthe (pers. commit.) informs me that he
has recently re-examined the holotype of G. paradoxa and found some deeply retracted tentacles. He was unable to
determine whether these were papillose or smooth.
DISCUSSION
It may be significant that the majority of recently described genera (e.g. Gnatliampliarete Desbruyfcres, 1978 ;
Decemunciger Zottoli, 1982; Endecamera Zottoli, 1982; Zatsepinia Jirkov. 1986; Ymerana Holthe, 1986) are
small, generally less than 10 mm long. An increased use of sieves with meshes of 0.5 mm or less, coupled with
an increase in deeper water investigations, makes it inevitable that many more species await discovery. A number
of these may well be referrable to genera that are currently monotypic. Alternatively they may provide additional
taxonomic information that will facilitate die synonymy of some such genera. For the present, I believe it better
to erect new genera than to confuse things further by prematurely expanding existing generic diagnoses.
All die characters separating Adercodon gen. nov. from odier ampharetids have been, and still arc, used to define
ampharctid genera (Day, 1964 ; Fauchald, 1977; HOLTHE, 1986a, c). The resulting profusion of monotypic
genera has increasingly led to questions (e.g. Day, 1964; Chardy & DesbruyEres, 1979; Holthe, 1986b, c)
concerning die relative "usefulness" of the characters and the apparent narrowness of many generic diagnoses. As
yet there have been no new approaches to the problem.
One thing that has received little attention (but see HOLTHE, 1986c: 19-20) is die possible generic
consequences of re-assigning certain anterior abdominal setigers lo the thorax. George (1979) noted diat
SabeUides octocirrata (Sars, 1835) had the same type of uncini on 13 anterior segments, die last two lacking
notopodia, and considered these all thoracic. SabeUides is, however, more usually cited (Day, 1964; FAUCHALD,
1977; Holthe 1986a, c) as having 1 1 thoracic uneinigerous segments. In Adercodon, the abdominal uncini of die
anterior two abdominal setigers are borne on "sessile" tori identical to those of die diorax whereas the remainder
differ, being situated on long projecting pinnules. On diis basis Adercodon could be said to have 15 thoracic
setigers, die last 12 being uneinigerous. Such observations suggest that a re-examination of die 'thoracic'
complements in all ampharetids could perhaps be a fruitful line of investigation.
The enigmatic presence of buccal teeth in Gnatliampliarete and the possible phylogenetic implications
concerning the Ampharetidae and Terebellida as a whole were discussed by DesbruyEres (1978) and Holthe
(1986c). Both workers considered diese to be possible representations of an ancestral condition and the latter
postulated that diey were probably not functional. The discovery of well-defined teedi in Adercodon in addition to
papillose tentacles may indicate odierwise. Their position, form and arrangement along the edge of the innermost
ventral lip strongly suggests dial diey are indeed functional. They could be involved in sorting the particles
collected by the tentacles; deposit-feeding on die sediment surface being die most common feeding method in the
Ampharetidae (Fauchald & Jumars, 1979). On die other hand (though perhaps less likely), it may be that
certain ampharetids arc, in some way, predatory. Ingestion of larval invertebrates has been noted in a number of
amphareuds and other members of the Terebellida (Fauchald & Jumars, 1979; Wilson, 1980; Zottoli, 1982),
though it is unclear whether this was an active or passive process.
Although earlier detailed morphological studies on die Ampharetidae (Fauvel, 1897; Hessle, 1917) made no
mention of buccal teeth, I agree with Holthe (1986c) in believing dial diey may be more common than thought.
Furdier investigation, particularly of the smaller species, could prove rewarding. Certainly the more characters that
can be detailed for the Ampharetidae, die more chance we have of re-evaluating the status of the genera and their
phylogenetic relationships.
Source :
A NEW AMPHARETID FROM HIE MEDITERRANEAN SEA
249
ACKNOWLEDGEMENTS
I would like to thank Alain GUILLE and his staff for access to laboratory and sampling facilities at the
Laboratoire Arago in 1991 and Philippe Bouchet for inviting me to join the Fifth European Marine
Malacological Workshop in Sicily the previous year. For both field trips I am indebted to all who helped with the
collecting; especially Philippe BoucilET, Rudo von Cosel and Anders WarCn in Sicily, and the crews of the
R.V. Nereis and dive boat Rufi in Banyuls. I gratefully acknowledge the National Museum of Wales for funding
both visits. Special thanks to Fredrik PLEIJEL, my co-worker on both sampling trips, for all his help, advice and
discussions. Fredrik Pleijel and Annette Woodham kindly commented on an early draft of this paper. Thanks also
to Torleif Holthe who, as one of the referees, allowed me to refer to his unpublished observations.
REFERENCES
BANSE. K.. 1970. — The small species of Euchone Malmgren (Sabellidae. Polychaeta). Proc. biol. Soc. Wash •
387-408.
CANTONE, G.. 1971. Ricerche sui Policheti della Sicilia. I. Boll. Sed. Accad. gioenia Sci. nat .. (4) 10 : 914-944.
Cantone. G. & Eassari. G., 1983. — Polychaetous annelids of soft bottoms around the Gulf of Catania (Sicily). Rapp. P.
-v. Reun. Comma ini. Explor. scicnt. Mer Medilerr.. 28 : 251-252.
CHARDY, P. & DESBRUYfcRES, D.. 1978. La classification multicritere. Application a la revision de la sous-famille des
Ampharetinae (Annelidcs polychetes). Annee biol.. 18 : 521-537.
Day, J. H., 1964. — A review of the family Ampharetidae (Polychaeta). Ann. S. Afr. Mas.. 48 : 97-120.
DESBRUYERES. D.. 1978. Un Ampharetidae (Annelidcs polychetes sedentaires) a structure buccale aberrante:
Gnathampharete paradoxa gen. sp. n. C. r. hebd. Seanc. Acad. Sci.. Paris , (D) 286 : 281-284.
FaUCHALD. K.. 1977. — The polychaete worms. Definitions and keys to the orders, families and genera. Sci. Ser. nat.
Hist. Mas. Los Ang. Cty.lS : 1-188.
Fauchald, K. & JUMARS, P. A., 1979. — The diet of worms: a study of polychaete feeding guilds. Oceanography mar
Biol., 17 : 193-284.
FAUVEL. P.. 1897. — Recherches sur les Ampharetiens, annelides polychetes sedentaires, morphologic, anatomie,
histologie. physiologie. Bull, sclent. Fr. Belg.. 30 : 277-488.
Gambi. M. C .. Bianciu, C. N., GlANGRANDE, A. & COLOGNOLA. R.. 1985. — Per un censimento della polichetofauna delle
coste Italiane, nota preliminare. Oebalia, 11 : 289-302.
George, J. D., 1979. — The polychaetes of Lewis and Harris with notes on other marine invertebrates. Proc. R. Soc.
Edinb., 77 B 189-216.
Got, II., Gl'ILLE. A.. Monaco. A. & Soyer, J.. 1968. — Carte sedimentologique du plateau continental au large de la cote
catalane frangaise (P. O.). Vie Milieu, (B) 19 : 273-290.
GUILLE, A.. 1970. — Bionomic benthique du plateau continental de la cote catalane fran9ai.se. II- Les communautes de la
macrofaune. Vie Milieu, (B) 21 : 149-280.
G UH.ee, A. & SOYER, J., 1968.— La faune benthique des substrats meubles de Banyuls-Sur-Mcr. Premieres donnecs
qualilatives et quantitatives. Vie Milieu. (B) 19 : 323-359.
GUILLE, A. & SOYER. J.. 1970. — Bionomic benthique du plateau continental de la cote catalane fran9aise. I-
Physiographie. Vie Milieu. (B) 21 : 137-147.
Hartman, O.. 1965. Deep-water benthic polychaetous annelids off New England to Bermuda and other North Atlantic
areas. Occ. Pap. Allan Hancock Fdn. 28 : 1-377.
Hessle, C.. 1917. Zur Kenntnis der tcrebellomorphen Polychxten. Zool. Bidr. Upps.. 5 : 39-258.
HOFSOMMER. A.. 1913. Die Sabelliden-Ausbeute der “Poseidoif-Fahrten und die Sabelliden der Kieler Buchl. Wiss.
Meeresunters. (Kiel.) . 15 : 305-364.
HoLTHE, T.. 1986a. Polychaeta Terebellomorpha. Mar. Invert. Scandinavia, 1 : 1-194.
250
A. S. Y. MACKIE
IIOLTHE. T.. 1986b. — Polychaeta Terebellomorpha from the northern Norwegian Sea and the Polar Sea. with descriptions
of Mugga bathyalis sp. n. and Ymerana pleropoda gen. and sp. n. Sarsia . 71 : 227-234.
IIOLTHE, T.. 1986c. — Evolution, systematics. and distribution of the Polychaeta Terebellomorpha. with a catalogue of
the taxa and a bibliography. Gunneria. 55 : 1-236.
JlRKOV, I. A.. 1986. - Zatsepinia rittichae gen. et sp. n. (Polychaeta. Ampharetidac) from the Norwegian and Barents
Sea. ZooL Zh .. 65 : 289-290.
NOLTE. W.. 1913. — Zur Kenntnis der Maldaniden dor Nord- und Ostsee. Wiss. Meeresunters. (Kiel.), 15 : 1-94.
Wilson. W. 11. 1980. — A laboratory investigation of the effect of a lerebellid polychactc on the survivorship of nereid
polychaete larvae. ./. exp. mar. Biol. Ecol. . 46 : 73-80.
ZOTTOLI, R.. 1982. Two new genera of deep-sea polychaete worms of the family Ampharetidae and the role of one
species in deep-sea ecosystems. Proc. biol. Soc. Wash.. 95 : 48-57.
Source : MNHN. Paris
26
The genus Ophryotrocha sensu lato
(Polychaeta, Dorvilleidae) in the Troms0 area,
northern Norway
Eivind OUG
Norwegian Institute for Water Research
Regional Office S0rlandet
Televeien 1
N-4890 Grimstad. Norway
ABSTRACT
Five species of small dorvilleids. here referred to the genus Ophryotrocha Claparede & Mecznikow, 1869. have been
collected from shallow-water soft-bottom areas near Troms0, Norway. The species are O. baccii Parenti. 1961. O. cf.
scarlatoi Averincev, 1989. O. cosmetandra Oug. 1990. O. cf. puerilis, and one species which is probably new to science.
In O. cf. scarlatoi the last 7-9 segments and pygidium are rimmed by a pair of scalloped longitudinal folds arising
dorsolaterally and appearing to curve and meet across the dorsum. The presumed new species is close to O. littoralis
(Levinsen, 1879) in having similar mandibles with four strong teeth. It differs from this species in having a smaller size,
in the shape of the palps, and in details of the maxillae. The genus Mammiphitime Orensanz. 1990, erected for forms
similar to O. cosmetandra . is discussed.
RESUME
Le genre Ophryotrocha sensu Into (Polychaeta, Dorvilleidae) dans la region de Tromso, nord
de la Norvege.
Cinq petites especes de Dorvilleidiens du genre Ophryotrocha Claparede & Mecznikow-. 1869, out etc recoltees dans
les sediments meubles pcu profonds da la region de Troinso. au nord de la Norvege. Les especes sont O. baccii Parenti.
1961. O. cf. scarlatoi Averincev, 1989. O. cosmetandra Oug, 1990, O . cf. puerilis, et une espece qui probablement est
nouvelie pour la science. Chez O. cf. scarlatoi les derniers 7-9 segments et le pygidium portent dorsalement des plis
longitudinaux. Ces plis ont un bord forme comine des vagucs, ils se courbent et se rencontrent dans la face dorsale.
L’espece supposee nouvelie est proche de O. littoralis (Levinsen, 1879) parce qu’elle a des machoires infericures avec
quatre fortes dents. L’espece se distingue de O. littoralis par sa petite taille. par la forme de ses palpes et par ses machoires
superieures. Le genre Mammiphitime Orensanz. 1990, etabli pour quelques especes ressemblant a O . cosmetandra , est
dScrit et commenle.
OUG. E.. 1994. The genus Ophryotrocha sensu lato (Polychaeta, Dorvilleidae) in the Troms0 Area. In:
J.-C. Dauvin. L.. LaUBIER & D.J. REISH (Eds). Actes de la 4eme Conference internationale des Polychetes. Mem. Mus.
natn. Hist, nal., 162 : 251-257. Paris ISBN 2-85653-214-4.
252
E. OUG
INTRODUCTION
During benthic surveys in the vicinity of Trom$0, Norway, five species referred to the dorvilleid genus
Ophryotrocha Claparfede & Mecznikow, 1869 have been found. The samples were taken in 1980-91, but most
specimens were collected during an environmental impact assessment survey in 1983 (OUG et al. , 1985). The
specimens have been found in shallow water or at moderate depths (< 25 m).
One of the species is probably new to science, but it is close to Ophryotrocha littoralis (Levinsen, 1879) from
Greenland. Type specimens of this species were examined for comparison, especially with regard to maxillary
pans.
The genus Ophryotrocha contains about 30 species. A number of species are similar, but some recently
described species show unusual features not seen in typical forms of the genus. In a recent revision of
Ophryotrocha IIiLBiG & Blake (1991) discussed the character variations, but found it impossible to split the
genus into less heterogeneous new genera. However, Orensanz (1990) erected the new genera Mammiphitime,
Pinniphitime and Palpiphitime for species with special morphological traits. Orensanz (1990) further argued in
favour of separating Ophryotrocha and allied forms from the other dorvilleids. He proposed to transfer the
"ophryotrochas" to the family Iphitimidae, consequently revising the definitions of Dorvilleidae and Iphitimidae.
The species collected in the Tromsd area are presently assigned to Ophryotrocha (in the wider sense), but the need
for a revision of the genera is acknowledged.
METHODS
Troms0 is located in a fjord area sheltered from the open sea (Fig. 1). Annual sea temperature and salinity
variations are 2-10 °C and 31-33 P.S.U. respectively, but higher temperatures and lower salinities may occur in
surface waters.
Samples were taken using a 0.1 m2 van Veen grab or a modified light-weight Ockelmann detritus sled. The
collected material was sieved through a 1 mm screen and preserved in 4 % formaldehyde solution. The material was
subsequently transferred to 70 % alcohol.
PlG. 1. — Map showing location of Tromsp, northern Norway (left) and sampling stations (right). Station numbers re ter
to the environmental impact assessment study in 1983 (OUG el at.. 1985).
Source . MNHN. Paris
'll IE GENUS UPHRYOTROCHA IN I I IE TROMS0 AREA, NORWAY
253
Specimens in alcohol or glycerine were examined for general morphology. Parapodia were removed and
mounted in glycerol for examination of setae and parapodial siruciurcs. Pharyngeal structures were removed by
dissection and mounted in glycerine or (permanent mounts) in Eukitt or Gurr's Hydramount direct mounting
medium. Drawings were made primarily with the aid of a Leitz camera lucida attachment.
SYSTEMATICS
Ophryotrocha baccii Parenli, 1961
Fig. 2 a-g
Ophryotrocha baccii Parenti, 1961: 438-440, fig. I: 1-5, fig. II: 6-7. — HlLBIG & Blake. 1991
Ophryotrocha bacci. Akesson, 1973. George & Hartmann-SchrOder. 1985
MaIERIAE EXAMINED. — Kobhvagen, 27 Nov. 1980. 6 m. inud with II->S: six specimens. — Tromspysund. 24
March 1983. 7m (stn T9), sand-mixed mud: 20 specimens.
Description. — Complete specimens 4.0-4.5 mm long. 0.5-0.8 mm wide excluding parapodia, with 30-38
setigers. Prostomium with digiliform antennae and similar ventrolateral palps (Fig. 2a). Parapodia with distinct
acicular lobes and digitiform dorsal and ventral cirri (Fig. 2d). Setae of three kinds: dorsal to acicula 3-5 capillary
setae, distally slightly dilated, widi an apical curved modi (Fig. 2e), ventral to acicula 4-7 compound setae (Fig. 20
and one needle-thin unjointed inferior seta emerging from setal lobe (Fig. 2g). Mandibles strongly chitini/.ed, each
piece with two distinct serrated teeth (Fig. 2b). Maxillae of p-type, with forceps and seven pairs of denticles in two
rows (Fig. 2c).
Remarks. — The specimens fit the original description of O. baccii well, except dial die maximum number of
segments (38) is greater, and most specimens have a few more bristles than staled by Parenti (1961). The
mandibles differ slightly in shape by having distinct Hat, less chitinized lateral projections behind the teedi (Fig.
2b). Sectioned specimens examined for gonadal products had sperm in 2-3 anterior segments and eggs in the next
approximately 20 segments. Akesson (1973) classified Ophryotrocha baccii as a contemporary hermaphrodite widi
anterior male and posterior female trunk regions.
Fig. 2. - Ophryotrocha baccii: a, anterior end. dorsal view. b. mandibles, c, maxillae, forceps and left denticle row. d,
parapodium. setiger 16. e, supra-acicular simple seta, f, subacicular compound seta, g, inferior simple seta.
254
E.OUG
Distribution. — The species is previously known from France (Roscoff), The British Isles and the Swedish
west coast (Akesson, 1973 ; George & Hartmann-SchrOder, 1985).
Ophryotrocha cf. scarlatoi Averincev, 1989
Fig. 3 a-h
MATERIAL EXAMINED. — Marisletla. 27 Nov. 1980. 15 in, dark mud wiih ITS: four specimens, — Troms0ysund.
24 March 1983. 7 m (sin T2). black inud with IDS: one specimen. 24 March 1988: 1 specimen, — Finnes, 24 March
1983. 7 m (sin Rl). sand-mixed mud: one specimen.
DESCRIPTION. — Complete specimens 4.5-6 mm long, 0.5-0.6 mm wide excluding parapodia, with 26-34
setigers. Last 7-9 segments and pygidium rimmed by two scalloped longitudinal folds arising dorsolateral ly and
curving across the dorsum (Fig. 3a). Setae of four kinds: dorsal to acicula 2-3 thin gradually tapering capillary setae
(Fig. 3e) and 2-4 shorter blunt capillary setae (Fig. 30, ventral to acicula 5-10 compound setae with blunt-tipped
blades (Fig. 3g) and one, occasionally two. unjointed inferior seta emerging from the tip of the setal lobe (Fig.
3h). Some setae with very fine subdistal serration. Maxillae of p-type, with enlarged forceps and seven pairs of
demicles in two rows (Fig. 3c). Some specimens with eggs from setiger 7 to about setiger 20.
Remarks. — The description of Ophryotrocha scarlatoi by Averincev (1989) is brief and illustrated with
simple drawings. Details of jaw elements are not given. The specimens from Troms0 seem to differ by having
slimmer mandibles and bristles with weak or no serrations. A similar form from the Canadian Arctic (Fournier &
ConlaN, 1994), which may belong to 0. scarlatoi , seems to differ from the Tromsd specimens in having
somewhat shorter mandibles, in details of maxillary parts, and in having a ventral cirrus on posterior parapodia.
FlG. 3. Ophryotrocha cf. scarlatoi : a. complete specimen, dorsal view, b, mandibles, c, maxillae, forceps and left
denticle row. d, parapodium, setiger 13. e. f supra-acicular simple setae, g. subacicular compound seta, h, inferior
simple seta.
Source : MNHN. Paris
'll IE GENUS OPHRYOTROCHA IN THE TROMS0 AREA. NORWAY
255
Distribution. — Opliryotrocha scarlatoi is previously reported only from Franz Joseph Land (Averincev.
1989). The species may have a wide distr ibution in the Arctic.
Opliryotrocha cosinetandra Oug, 1990
Remarks. — This species shows a strong sexual dimorphism. Mature males tire characterized by conspicuous
dorsolateral processes on die posterior segments and die pygidium. Only males show the K-type maxillae. Both
sexes are further distinguished by setal morphology and mandibles with three strong teedi (Oug, 1990).
Orensanz (1990) erected die genus Mammiphitime, belonging to the revised family Iphitimidae, for some
Ophryotrocha- related forms with conspicuous dorsal lobes. The species Mammiphiiime trideniaia Orensanz. 1990
trom die soudiem Atlantic is similar to O. cosinetandra in a number of characters, e.g. the shape of die mandibles
with three strong teedi and compound setae of the spiniger type only. Sexual dimorphism was not described. It
seems that 0. cosinetandra and M. tridentata should be referred to die same genus, but Mammiphitime , if adopted,
may need to be redefined.
Distribution. — 0. cosinetandra is the most common dorvilleid in die Tromsd area. It is known from
northern Norway and Greenland (see Oug. 1990 for records) and has recently also been collected in organically
polluted harbours in die Faroes (M.E. Petersen, pers. comm).
Ophryotrocha cf. puerilis Clapaitde & Mecznikow, 1869
Ophryotrocha puerilis. — Fauvel, 1923. — La Greca & Bacci, 1962
Material EXAMINED. — Troms0ysund. 24 March 1983. 25 in (sin T8). sandy mud with gravel and shell fragments:
one specimen.
Remarks. — The specimen fits the descriptions of Ophryotrocha puerilis given by Parenti (1961), La
Greca & Bacci (1962) and Hartmann-Sciiroder (1971). except for the mandibles which appear to have more
than two teedi. The mandibles, however, are worn and presumably damaged. The specimen has K-type maxillae.
Eggs are visible in seligers 8 to 16.
Ophryotrocha puerilis has repeatedly been confused with other species (Akesson, 1973, 1984). Present
descriptions, mostly showing outline drawings of jaw parts, are presumably insufficient or inacurrate for critical
species discrimination. Reports of O. puerilis from world-wide areas may represent a confusion of related species.
Distribution. — The confirmed distribution is in the Mediterranean Sea (ssp. O. p. puerilis) and the eastern
North Atlantic (ssp. O. p. siberti ) (Akesson, 1973, 1984 ; GEORGE & Hartmann-Sciiroder, 1985).
Ophryotrocha sp.
Fig. 4 a-h
MATERIAL EXAMINED. — Marisletta. 27 Nov. 1980. 6-10 m, soft sand-mixed mud: one specimen, 15 June 1987:
two specimens.
Description. — Largest specimen 3.4 mm long for 28 setigers, width 0.3 mm excluding parapodia (Fig. 4a).
Prostomium with two dorsal digitiform antennae and two ventrolateral small sphaerical to ovoid faintly visible
palps. Parapodia uniramous (Fig. 4d), with a dorsal lobe or swelling representing a dorsal cirrus, without ventral
cirrus. Setae of four kinds: dorsal to acicula 1-3 thin gradually tapering capillary setae (Fig. 4e) and 1-2 somewhat
shorter blunt distally dilated capillary setae (Fig. 40, ventral to acicula 3-6 compound setae with blunt-tipped
blades (Fig. 4g) and one needle-thin slightly curved unjointed inferior seta emerging from the tip of the setal lobe
(Fig. 4h). Compound setae with blades of about equal lengths. Mandibles moderately chitinized, each piece with
four distinct teeth (Fig. 4b). Maxillae of p-type, witli 8 pairs of denticles in two rows, posterior small pieces
(‘forceps') weakly fused (Fig. 4c).
256
E. OUC.
Remarks. — This form is close to Ophryotrocha littoralis (Levinsen, 1879), which is the only Ophryotrodia
species hitherto described having mandibles with four strong teeth (Fig. 4i). It seems to differ from it in having a
smaller size, in the shape of the palps, and in details of dentition of the maxillary parts. The mandibles are
FIG. 4. Ophryotrocha sp: a. complete specimen, dorsal view, b, mandibles, c. maxillae, forceps and left denticle row.
d. parapodium, setiger 10. e. f supra-acicular simple setae, g, subacicular compound seta. h. inferior simple seta.
Ophryotrocha littoralis : i. mandibles.
strikingly similar, but are smaller than in 0. littoralis (Figs 4b. i). The specimens may belong to a new species,
but die material at hand was considered insufficient for naming a new species.
The type collection of O. littoralis (= Paractius littoralis) contains numerous specimens which all are well
preserved. Most characters are referred to in the original description (Levinsen, 1879), but the figures fail to show
critical details of jaw parts. The palps appear shorter than originally stated.
ACKNOWLEDGEMENTS
Part of this work was performed during a stay at the Zoological Museum of Copenhagen. I am indebted to
Mary E. PETERSEN (ZMUC) for invaluable help during the stay, for arranging the loan of type specimens of 0.
littoralis . and for suggestions to die manuscript. Alexander TZETLIN, University of Moscow, and Danny E.
Jacobsen (ZMUC) provided and translated Russian literature. I also wish to thank die skipper of R/V 'Ottar’ Kare
Bendiksen for assistance during sampling and Pat DiNEEN and Synn0ve Lassen for language corrections.
Source : MNHN. Paris
11 IE GENUS OPHRYOTROCHA IN THE TROMS0 AREA. NORWAY
257
REFERENCES
^ToTscnp™! 4R5!L55dUC,,0n 'arVa' m°lphol0gy of fivc Ophryotrocha species (Polychaeta, Dorvilleidae).
AKESSON, B., 1984. - Speciation in the genus Ophryotrocha (Polychaeta, Dorvilleidae). Fortschr. Zool.. 29 : 299-316.
AV/wfr‘ Vf’', !?*» -Seaso™l dynamics of polychaeles from the high Arctic coastal ecosystem of Fran--Joseph
Land (Errantia). (In Russian). Akadcmya NAUK. SSSR. J Josepn
FAUVEL, P., 1923. — Polychetcs errantes. Faune Fr.. 5 : 1-488.
^scours’ inAthf CanNadhNn Are,' ‘T'i t "ow species of Ophryotrocha (Polychaeta: Dorvilleidae) associated with ice
scours ,n the Canadian Arctic Archipelago, hr. Dauvin. L. Laubier & D.J. Reish (Eds). Actes de la 4eme
Conference Internationale des Polychetes. Mem. Mus. natn. Hist, nat ., 162 : 185-190.
Gis“rif r”srER- '*• - p<>iyct“Bs: «■*■* **■—*■•
llARTMANN-SCHRODER, G., 1971. — Annelida. Borstenwurmcr, Polychaeta. Tierwelt Dtl., 58 : 1-594.
HlLSfG,wo' t wotne' JA ", M91' ~ Dorvilleidac (Annelida: Polychaeta) from the U.S. Atlantic slope and rise. Description
ol two nev\ genera and 14 new species, with a generic revision of Ophryotrocha. Zool. Scr.. 20 : 147-183.
LA BoU^Z^i &29BA7C‘i8G'' ‘%2' ~~ Una nU°Va Sp^® d‘ °Ph,yo,rocha delle coste tirreniche (Annelida. Polychaeta).
LEV(Denmark)M'9-181879’ °m ‘° SI:CS,er af a'Cliskc ch:eloPocle Annelider. Vidensk. Meddel. nat. Foren. 1879
Grensanz. J.M.. 1990- The eunicemorph polychaete annelids from Antarctic and subantarctic seas. With addenda to
52 E|183 °rPha 8ent'na" ChilU" NCW ZeUland' Auslra,ia- and lh‘ southern Indian Ocean. An, arc. Res tr
°V<kF;;n ‘v,90; ,hM°,,ph0l0gy- and development of a new species of Ophryotrocha (Polychaeta-
Doivillcidac) with strong sexual dimorphism. Sarsia . 75 : 191-201.
Ouo. E., Lein. Holte. B.. Ormerod. K. & N,ES. K.. 1985. - Basisunderspkelse i Tromspsund og Nordhotn 1983
Fag rapport. SM/NIVA report !73b/84 (In Norwegian). Oslo. 160 pp.
R^NH* 43 7 ' 4 4 5^ 1 Ophryotrocha puerilis siberti. O. hartmanni ed (). baccii nelle acque di Roscoff. Cah. Biol. mar..
Source : MNHN. Pahs
27
Distributional patterns and taxonomic notes
on Lumbrineridae from Crete
(S. Aegean, Eastern Mediterranean)
K. -Nadia PAPADOPOULOU, C. DO UNAS & Chris J. SMITH
Institute of Marine Biology of Crete
P.O. Box. 2214, 71003 Iraklio. Crete. Greece
ABSTRACT
Lumbrineridae were collected from soft sediment at 1 1 coastal and shelf areas from the island of Crete. Collections
were made at 182 stations ranging in depth from 10 to 330 m. Eleven species were found. Three species were common and
present throughout the area. Of these, Lumbrineris gracilis, was by far the most abundant species at depths down to 130
m. This species was one of the 10 most dominant macrofaunal species between 40 and 70 m depth. Lumbrineris nonatoi
was the second most abundant species at stations down to 70 in. Scoletoma emandibulata mabili was found in lower
numbers than L gracilis at all depths but was recorded from a wider depth range (10-330 m). Lumbrinerides sp. A is new
for the Mediterranean and its relationship to other species of the genus is discussed.
RESUME
Modeles de distribution et notes taxonomiques sur les Lumbrineridae de Crete (Sud de la mer
Egce, Mediterranee orientale)
Des Lumbrineridae provenant des sediments meublcs ont ete collcctes parmi 11 zones de la cote et de la marge
continental lout autour de Tile de Crete, comprenanl 182 stations situees a des profondeurs variant entre 10 et 330
metres. Onze especes ont etc trouv£es parmi lesquelles irois especes etaient presentes sur toutes les zones de l’etude.
Lumbrineris gracilis etait 1' espece la plus abondante a toutes les profondeurs jusqu’a 130 metres. Entre 40 et 70 metres, L.
gracilis etait une des 10 especes les plus dominantes de la macrofaune. Lumbrineris nonatoi etait la deuxieme espece la
plus abondante de toutes les stations peu profondes jusqu'a 70 metres. Scoletoma emandibulata mabiti etait moins
abondante que L. gracilis, a toutes les profondeurs mais a ete enregistr<5e dans une plus grande gamme de profondeurs (10-
330 m). Lumbrinerides sp. A esl une nouvelle espece pour la Mediterranee et sa relation avec d'autres especes du meme
genre cst discutee.
INTRODUCTION
Our knowledge of the Eastern Mediterranean polychaete fauna is limited. Only a small number of papers on
Papadopoulou. K.N.. DOUNAS, C. & C.J. Smith. 1994. Distributional patterns and taxonomic notes on Lumbrine-
ndae from Crete (S. Aegean, Eastern Mediterranean). In: J.-C. Dauvin. L. Laubif.R & D.J. REISH (Eds), Actes de la 4eme
Conference internationale des Polychetcs. Mem. Mus. natn. Hist, nat ., 162 259-268. Paris ISBN 2-85653-214-4.
260
K.-N. PAPADOPOULOU, C. DOUNAS & C.J. SMITH
ecology or taxonomy have been published to date. None of these were concerned with the Lumbrineridae. 1 he
family Lumbrineridae has been extensively investigated in a number of areas worldwide (Hartman, 1965; Day,
1967; FAl'CHALD, 1970; ORENSANZ, 1973. 1990; PERKINS, 1979; UEBELACKER, 1984; Imajima, 1985;
George & Hartmann-SchrOder, 1985: Frame, 1992). Up to 13 genera are now recognized in die family,
including the recent additions of Abvssoninoe Orensanz, 1990, Eranno Kinberg, 1865, Lumbricalus Frame, 1992,
and Scoletoma Blainville, 1828. Over 200 species have been described in the family and more are being added
(UEBELACKER, 1984). In die Mediterranean, seven genera and approximately 20 species have been recorded.
Information concerning this family in the region has been provided by Ben-Eliaiiu (1976), Ramos (1976),
Cameo Y (1979) and Mrira (1980) and records have also appeared in a number of benthic species lists (CARPINE,
1970; Fredi, 1974; Salen-PICARD, 1982). Previous listings of Lumbrineridae may also include some
misidentified species.
The study by Ramos (1976) remains the most authoritative work for the Mediterranean, but is restricted to the
Western Mediterranean from die Spanish Catalan coast to the Adriatic Sea. There is a large gap in the information
concerning the Aegean area, in particular the Southern Aegean and the area around Crete. This is an important
geographical region where several water masses meet, including from die Atlantic, the Levantine Basin (allowing
for passage of Lesseptian migrants), the Libyan Sea, the Ionian sea and influences from the Black Sea through the
Sea of Marmara and the Aegean. The present study investigates the family Lumbrineridae from around the island ol
Crete over a range of different sediment types and depths.
METHODS AND MATERIALS
Soft bottom lumbrinerid polychaetes were collected from 1 1 coastal and shell areas lrom around the island ol
Crete during several quantitative benthic faunal surveys carried out from 1987 to 1989 (Fig. 1). These were pilot
surveys for the most part. In all, 182 stations were sampled at depths ranging from 10 to 330 m. Most of the
stations were along transects at standard depths of 10, 20, 30, 40, 70, 100, 130, 160 and 190 m. Samples were
taken using a Smith-Mclntyre grab (0. 1 m2). One macrofaunal grab per station was analysed and four undisturbed
cores were taken from an additional grab for physico-chemical measurements. Macrofaunal samples were
immediately mixed into a sea water slurry and washed dirough a 0.5-min sieve. The residues were transferred to
containers and fixed with 10 % buffered formalin. In the laboratory Rose Bengal was added and after 24 hours the
samples were washed with freshwater and screened again through a 0.5-inm mesh size sieve. The stained fauna was
then sorted to major taxa and preserved in 4 % buffered formalin prior to identification to species. Hie material is
deposited at the Institute of Marine Biology of Crete.
STUDY AREAS
The north coast of Crete, where most of the stations were situated, has a generally consistent sedimentary
environment which grades from coarse sands on die beaches to fine silty clays in deeper areas. Exceptions to this
are: the western part of Rethymnon Bay where the sediment at 20-40 m depth is much coarser with high biogenic
detritic content; the enclosed Bay of Souda (which physically resembles a fjord) where sediments are generally
finer; and Mirambelo Bay which has a central shallow seamount where the sediment is coarser and of biogenic
detritic origin.
The south coast, which has rocky shores with only a few bays, is much steeper and the width of the
continental shelf is consequently much narrower. Messara and Ierapetra Bays, however, slope away more gently in
front of open valleys. At Kali Limenes Bay the sediment is gravelly sand with pebbles at 10-20 m depth and
retains a large coarse fraction as far down as 100 m. At the South East stations, the sediment is of biogenic detritic
origin and contains calcareous algal fragments.
Biologically, the Cretan coastal sedimentary environment is characterized by seagrasses from 10 to 25 m depth
and the alga Caulerpa prolifera from 25 to 40 m. At 70 m, numerous dead Turritella and, to a lesser extent,
Dentalium shells are inhabited by hermit crabs and sipunculids. Below this, the environment is rather featureless
except in terms of microtopography caused by the bioturbatory activities of burrowing animals. The benthic
infauna is characterised by the presence of Ditrupa arieiina at 30 to 40 m and Amphiura chiajei and A. filiformis
below 50 m. The crinoid Leptometra phalangium is present in very high numbers from 130 to 200 m depth
(predominantly on the north coast).
Source : MNHN: Paris
DISTRIBl ITION AND TAXONOMY OF LUMBRINERIDS FROM CRETE
261
FIG. 1. — Crete. Sampling stations (K: Kissamos, X: Chania, SD: Souda. R: Rethymnon, H: Iraklio, M: Mirambello, S:
Sitia, SE: South East. 1: Ierapetra. K L : Kali Limenes, MR : Messara). Average depth distribution of S. cmandibulata
mabiri (a). L. gracilis (b) and L nonatoi (c) for each of the study areas.
Source
262
K.-N. PAPADOPOULOU. C. DOUNAS & C.J. SMITH
RESULTS
A total of 1999 Iumbrinerids was found and the following 1 1 species have been identified: Lumbrineris
coccineci (Renier, 1804), L. gracilis (Ehlers, 1868), L. laireilli (Audouin & Milne Edwards, 1834), L nonatoi
Ramos, 1976, Scoletoma emandibulaia mabiti (Ramos, 1976), S. funchalensis (Kinberg, 1865), S.fragilis (O.F.
Muller, 1776), S. impatiens (Claparfcde. 1868), Ninoe armoricana (G16marec, 1968), Lumbrineriopsis paradoxa (de
Saint-Joseph, 1888) and Lumbrinerides sp. A. Presence-absence data for all the species found, number of stations
and depth ranges investigated per sampling area are given in Table 1 .
Lumbrineris gracilis , L. nonatoi and S. emandibulata mabiti were the numerically dominant species.
Abundances for these three species were such that their average depth distribution could be plotted for each of the
study areas (Fig. 1). All three species were found in all locations except for L. gracilis and S. emandibulata mabiti
in the South East (transect SE) stations. Distributions for each of these species are discussed below.
SPECIES NOTES
According to the latest revision of Frame (1992) the genus Lumbrineris Blainville, 1828 has been restricted to
species with composite hooks, simple hooks and simple limbate setae; the genus Scoletoma de Blainville, 1828
has been resurrected to include species with simple hooks and simple limbate setae and the genus Lumbricalus
Frame, 1992 has been erected to include species with composite spinigers, composite hooks, simple hooks and
simple limbate setae. Based on this division, the following keys are given for the Cretan species.
Key to the species of Lumbrineris de Blainville, 1828
1 Elongated parapodial lobes in posterior body region. Mx III bidentate . 2
Not elongated parapodial lobes in posterior body region. Mx III unidentate . 3
2 Presetal parapodial lobes longer than postsetal lobes. Mx II = 3 . L. nonatoi
Presetal parapodial lobes smaller than postsetal lobes. Mx II > 3 . L. gracilis
3 Prostomium round, globular. Blades of composite hooks of
similar length throughout . L coccinea
Prostomium conical. Blades of composite hooks longer
in anterior parapodia . L. la t re i Hi
Key to the species of Scoletoma de Blainville, 1828
1 Limbate setae with terminal hook in the first anterior parapodia . S . emandibulata mabiti
No such setae . 2
2 Prostomium broadly rounded. Aciculae amber . S. funchalensis
Prostomium conical . 3
3 Aciculae yellow. Hooks starting on setiger 1-5 . S. impatiens
Aciculae black. Hooks starting on setiger 22-35 . S. fragilis
Lumbrineris gracilis (Elders, 1868)
Lumbriconereis gracilis Eihlers. 1868 (type locality Hume. Adriatic) FaUVEL. 1923 432, fig. 172 a-f.
DISTRIBUTION. Mediterranean, Black Sea. N. Atlantic, North Sea, intertidal to about 680 m depth.
L. gracilis has always presented problems as to its identification (SALEN-PICARD, 1982). Some authors would
refer to a L. gracilis-latreilli complex rather than separating these two species (Amoureux, 1987). Apart from the
differences used to distinguish the two species, such as the shape of the prostomium and the length of the
compound setae, Ramos (1976) utilised the presence (L. gracilis ) or absence (L. latreilli ) of elongated parapodial
Source :
DISTRIBUTION AND TAXONOMY OF LUMBRINERIDS FROM CRETE
263
lobes in the posterior body region. The number of anterior parapodia with compound hooked setae can also be used
to separate L. gracilis (10-15) from L. latreilli (20-30) (George & Hartmann-Schroder, 1985) However this
is probably only applicable to adults.
L. giacilis was by far the most abundant species (60 % of the lumbrinerid individuals), found at 1 17 of the 18°
stations, on various combinations of gravel, sand, mud, clay, maerl and biogenic detritus, from 10 to 190 m.
Highest abundances were recorded between 30 and 70 m where L. gracilis was one of the 10 most abundant
macro! aunal species. The maximum abundance observed for L. gracilis was 910 ind. m-2 at a 40-m sandv silt
station in Chania Bay. " J
Lumbrineris nonatoi Ramos, 1976
Lumbrineris nonatoi Ramos, 1976: 124, figs 19-21 (type locality: Rosas Bay. Spanish Catalan coasts)
Distribution. — Mediterranean, from 10 to 130 m.
L nonatoi was originally described from a “sandy mud polluted bottom” at 10 m depth (Ramos, 1976) from
die Spanish Catalan coast. Since then, there have been very few records of L nonatoi from the Aegean or the
Tastem Mediterranean. Our findings agree well with Ramos' (1976) description. L nonatoi is a very distinct but
m mute species; prostomium conical, slightly wider than long, composite multidcntate and very short hooded
hooks from setiger 1 Maxillae II with three teedi each, posterior parapodia with elongated presetal lobes, longer
than postsetal lobes. It seems that L. nonatoi is fairly common in the Aegean, but because of its small size" it
may have been misidentified as juvenile L. gracilis .
f * n°nal°l was l,ie second ,nosl abundant species (25 % of the lumbrinerid individuals, present at 69 of the 182
stations). 1 he species prefers coarse sand or shelly bottoms, but was generally found in sand, mud gravel and
various combinations of these, from 10 to 130 m. Large numbers were recorded from 20 to 40 m, dropping
sharply at 70 m. At 20 m the mean abundance was slightly higher than dial of L gracilis. The highest abundance
recorded lor L. nonatoi was 370 md. m- at a 30-m sandy station in Ierapetra Bay, on die south coast, while the
maximum average (round Crete average calculated for each depdi class) abundance, found at 40 m, was only 81 ind.
L nonatoi had maximum abundances in Sitia, Messara and Chania Bay at 30-40 m depth. L. nonatoi has a
similar distributional pattern to L. gracilis , widi maximum abundances at 40 m. It did not extend into as deep
waters as L. gracilis. 1
Lumbrineris latreilli Audouin & Milne Edwards, 1834
Lumbrineris latreilli Audouin & Milne Edwards, 1834 (type locality: France).
Lumbriconeris latreilli : FaUVEL, 1923: 432, fig. 171 m-r.
Distribution. A cosmopolitan species (Greenland, Norway, Iceland to France, Mediterranean. Gulf of Mexico. Indian
Ocean. Red Sea, Japan. West and South Africa), in temperate and warm waters from 10 to 2.000 m.
There has been much discussion on how to separate L. latreilli and L. coccinea. Frame (1992) introduced die
use o! the length of blades of the composite hooks.
A few specimens of L. latreilli were found at only two stations, in mixed substrates at 30-40 m depth. It has
frequently been reported from the Aegean and die Ionian Sea (Harmelin,1969; Bogdanos & Satsmadjis, 1987;
Dounas & Koukouras, 1992); it has probably been occasionally confused widi L. gracilis. It is usually found
in coastal coarse sands and Ditrupa sands (GlCmarec, 1969).
Lumbrineris coccinea (Renier, 1804)
Nereis coccinea Renier, 1804 (type locality: Mediterranean).
Lumbriconeris coccinea : FaUVEL, 1923: 432. fig. 172 g-n.
Distribution. — outside the Mediterranean, L. coccinea has been found in the Atlantic. North Pacific, South Africa. Red
Sea and Indian Ocean, from the intertidal zone to 1.268 m depth.
264
K.-N. PAPADOPOULOU, C. DOUNAS & C.J. SMITH
L. coccinea and L. latreilli can be separated as shown in the key above. The shape of Maxillae III can also be
used to distinguish L. coccinea (Maxillae III: B+B. with two “expansions aliformes non dentelees ”) from L.
latreilli (Maxillae III: A2+A2, with one “expansion alifonne bidentde”) (Miura, 1980).
A single specimen of L. coccinea was found at a gravelly sand station, on the north coast, at 40 m depth. In
the Mediterranean it is known to occur frequently in higher numbers in “coralligfene” substrates (Bellan, 1964).
Scoletotna emandibulata mabiti (Ramos, 1976)
Lumbrineris emandibulata mabiti : Ramos. 1976: 112, figs 7-10 (type locality: Rosas Bay. Spanish Catalan coast).
Distribution. — Mediterranean, from 6 to 330 in.
There are very few previous records of S. emandibulata mabiti from the Aegean or the Eastern Mediterranean
(Dounas & KOUKOURAS, 1992). This is surprising because S. emandibulata mabiti. is also well described and
distinctive: prostomium conical, longer than wide, simple limbatc setae with terminal hook in die first anterior
parapodia, which are gradually replaced by simple pluridentate hooded hooked setae. Maxillae II with four teeth and
Maxillae III with two teedi each.
S. emandibulata mabiti was the third most abundant species (10 % of individuals). It was present at 94 of the
182 stations, from 10 to 330 m depth. S. emandibulata mabiti occurred in a variety of mixed substrates but had its
higher numbers in fine silly sediments. The bathymetric distribution given by RAMOS (1976) (6 to 295 m) for die
Western Mediterranean is essentially within die same depth range. Abundances were generally low throughout die
area, lower than L. nonatoi at die shallow depths and L gracilis at die deeper stations. Maximum numbers of 140
ind. nr2 were recorded at a 40 m silty station in Rethymnon Bay.
.S’, emandibulata mabiti had its maximum numbers in the North West stations, at 40 m depth in Souda and
Rethymnon Bays and at 70 to 190 m in lerapetra Bay, in the South. In terms of distributional patterns, Ierapetra
Bay was an exception as die maximum abundances were found at depdis below 40 in. This is perhaps due to
localised enrichment which was reflected in a slightly modified macrofaunal community.
S. emandibulata mabiti , has the same distributional pattern as L. gracilis but with a wider depdi range and
significantly lower numbers.
Scoletotna impatiens (Clapar£de,1868)
Lumbriconereis impatiens Claparede. 1868 (type locality: Cape of Good Hope, South Africa) — FAUVEL, 1923: 429, fig.
171 a-i.
DISTRIBUTION. — A cosmopolitan species. Atlantic, Mediterranean. Indian Ocean. Red Sea, South West Africa, from the intertidal zone to
a depth of approximately 2500 m.
Thirteen specimens of S. impatiens were found at 9 stations around Crete, from 20 to 160 m, in sand, mud,
broken shell, gravel and mixed bottoms. .S', impatiens has frequendy been reported from both die Western and the
Eastern Mediterranean. It is often confused with .S', emandibulata mabiti (Salen-Picard, 1982) since they are
very similar in appearance. Both have a sharply conical prostomium but S. emandibulata mabiti has simple
limbate setae with a terminal hook in die first anterior parapodia and S. impatiens has simple hooded hooked setae
starting on setigers 1-5.
Scoletotna fragilis (O.F. Muller, 1766)
Lumbricus J'ragilis O.F. Muller, 1766 (type locality : Denmark)
Lumbriconeris fragilis : FAUVEL, 1923: 432. fig. 171 k-1.
DISTRIBUTION. — Mediterranean, N. Atlantic, N. Pacific, North Sea. Bering Sea. Japan, from the intertidal zone to 3.500 in
depth.
S. fragilis was found at a single fine silt station (two specimens), off the north coast, at 130 m depth, in
Iraklio Bay. S. fragilis can easily be separated from S. impatiens and S. funclialensis by the presence of black
aciculae.
It has been reported from sand, mud, gravel and various combinations of these, and among Posidonia meadows
(George & Hartmann-Scmroder, 1985). Ii is commonly found in coastal coarse sands and gravel from atlantic
french coasts (Gl£marec, 1969).
Source : MNHN , Paris
DISTRIBUTION AND TAXONOMY OF I..UMBRDMERIDS FROM CRETE
265
Scoletoma funchalensis (Kinberg, 1865)
Lumb ricnnc re is fu nclialensis Kinberg. 1865 (type locality: Madeira). Fauvel. 1923- 484 fie 172 o r
Distribution. — Mediterranean and Atlantic, to about 100 m depth ' 8
S. funchalensis, along with X. impatient and S.fragilis, lacks compound hooded hooked setae The First 12 70
— - - - -SSS5SS.
5'. funchalensis was found at only two stations in Iraklio Bay. in very low densities at 20 and 80 m denth in
Ninoe armuricana GlGnarec, 1968
S&ES*"**’ l%8: 315' ,i8' |,ype D,y ”f B“»r. shelf). Ramos.
Distribution. - North Eastern Atlantic. Mediterranean, from 6 to 330 in depth.
Vamvakas (1970) found one specimen of Ninoe kinhergi Ehlers, 1887 in Iraklio Bay at 330 m depth This
record, which is the only record of N. kinhergi from the Eastern Mediterranean, may have been misidentified We
vS 10 * ~ 1968 — ^ ZkXZs
sediments’ °" ^ ,n°rtl1 COasl of Crelc; at four stations in Souda Bay. in fine silty
sediments, at 15-265 m depth and at a single station in Iraklio Bay at 160 m. In the Eastern Mediterranean
Kc=^^)PreVI°USly rCC°rdeCl fTm "le N°rUl AeSean' high densities a. 50-70 m depth (Dounas &
Lunibrineri op si s paradoxa (de Saint-Joseph, 1888)
Lumbriconereis paradoxa de Saint-Joseph, 1888. ? FAUVEL. 1923 : 434. fig. 173 a-h.
Lumbriconereis mucronala Fillers. 1908. ORENSANZ. 1973: 377. fig. XIII.
Lumbrineris paradoxa Harmelin, 1964
Lumbrineriopsis paradoxa ORENSANZ, 1973: 375. not GARDINER, 1976: 205. fig 26 m-o
DISTRIBUTION. - Mediterranean. West Africa. Azores. Bermuda. N. Carolina, Mexico from 10 to 1,700 m depth.
B Jns h v reCC',V,f muCh attention 38 10 f* sPe«'^f ascribed and to its synonymy with L. muewnata.
tiS fT'1C,Ze .ASy,U)nymy W,th L mucrona<“ and discussed a Mediterranean form Lumbrineris cf
pauido.xa. I his later species has one penstomial ring and short mandibles with denticulate margin which has been
observed in all previous collections from the Mediterranean and also from this study. These characters have also
S'0b2,le no!!n?eC'.nK'nS fr0m Bcnnuda (I,ARTMAN’ J965) and lmm llle Gulf of Mexico (Uebelacker,
, , in, r x , u" 8 TT" °< lhC genus in,r°duced the use of die shape of die prostomium and die
colour of die aciculae. Me described Lumbrineriopsis gardineri from Gardiner's (1976) "L. paradoxa ” material Ii
seciriAS that some confusion still exists and further work is required.
dcnihs'fromTn^f^11! 1were/°und al 16,of lJlc 182 stalio"s "» coarse sediments such as “ Amphioxus sands” at
Known n - 5 ,6 ? ?' !' abandance ra"Sed from 2 to 4 ind. m-2 with maximum abundance at 40 m
(Be^Ta J 1964 R mo- l97r>Um 3 (BOGDANOS & SATSMADJis. 1987) and die Nordi Western Mediterranean
Lumbrinerides sp. A
wfpl;hEXAM,NEnD- _-?'i UmeneS- seven sPcc',nens at 16 m depth; Chania Bay. 5 specimens at 20 and 30 m
depth, and Rethymnon Bay. eight specimens at 20-40 m. Found in coarse sediments such as -Amphioxus sands", coarse
sands with shell fragments and gravelly sand.
I he body is long and slender and the prostomium is elongate, conical without eyes or eye spots The
penstommm is composed of two equally long rings. Maxillae I with 2 weakly developed small accessory teeth
each. Maxillae II with three round teeth each. Maxillae III dentate subreclangular plates and Maxillae IV cup shaped
266
K.-N. PAPADOPOULOU. C. DOUNAS & C.J. SMITH
oval plates. Maxillary carriers triangular, darker than rest of maxillae. Mandibles Y-shaped, light brown. First 6-7
anterior parapodia minute, with very sm;ill setal lobes, increasing in size from the 8th setiger. They reach their
maximum length at setiger 12-13 and from setiger 22 onward they decrease in size. The setae include simple
hooded hooks from the first setiger, broadly limbatc setae and two pale pointed aciculae. The pygidium is typical
for Hie genus.
Lumbrinerides sp. A differs from the other Mediterranean species of the genus: L. carpinei (Ramos, 1976)
which has one accessory tooth in Maxillae I, one very long peristomial ring and only three minute anterior
parapodia, and Lumbrinerides sp. (Ramos, 1976) (originally identified by Ramos as Lumbrineris acuta) which has
no accessory tooth in Maxillae I and simple hooded hooks from the 16th setiger.
Lumbrinerides sp. A will be described in the near future by us after a revision of the Mediterranean members of
the family and further examination of type material and material from other localities.
DISCUSSION
In considering the biogeographical origins of the Cretan 1 .umbrinerids, three groups can be identified. The first
is the cosmopolitan species, Lumbrineris latreilli. L. cocci nea. Scoletoma impatiens and S.fragilis. These have a
world wide distribution from the Atlantic through the Mediterranean and Red Sea to the Indian mid Pacific Oceans.
The second group includes the Atlanto-Mediterranean species. Lumbrineris gracilis. Ninoe armoricana and
Lumbrineriopsis paradoxa. These arc probably of Atlantic origin, which have penetrated the Mediterranean ;uid, in
die case of L. gracilis , the Black Sea. The last group is the Mediterranean endemic species, L. nonatoi and S.
emandibulata mabiti. No lessepsian migrants have been recorded from the Red Sea. The probable explanation for
the recorded distributions are probably due to factors such as the depdi range of the species, dispersive current
patterns and die temperature mid salinity extremes in die Mediterranean mid Red Sea.
Table 1 . — Occurrence of species, depdis sampled mid number of stations per sampling area
ACKNOWLEDGEMENTS
This work constitutes part of the NATO Science for Stability GR-FISHECO project. The organisational and
financial help from SFS is gratefully acknowledged and much appreciated. We are particularly grateful to
Source :
DISTRIBUTION AND T AXONOMY OF LUMBRINERIDS FROM CRETE
267
Dr I. Karakassis IMBC, for access to his Thesis material and to Dr. M. PETERSEN, Zoological Museum
University of Copenhagen, for critically reading an earlier draft of this manuscript.
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Bellas. G 1964 — Campagne de la Calypso : Mediterranee nord-orientale. 6. Annelides Polychetes. Ann. Inst, octkin.,
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Ben-Euahu, M.N., 1976. — Polychaete cryptofauna from rims of similar intertidal vermetid reefs on
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BOGDANOS. C., & J.. Satsmadjis. 1987. — The Patraikos bottom Fauna. Thalassographica, 10 : 37-71.
Campoy, A 1979. Lista de especies de Anelidos Poliquetos conocidas de las costas de la Peninsula Iberica. Inv. Pesq..
Carpine, c 1970. Geologic de Pelage bathyal dans la Mediterranee occidentale. Mem. Inst, octanogr Monaco 2
146 pp. A
Day J.H.. 1967. — A monograph on the polychaeta of the Southern Africa. Part. 1: Errantia. Trust. Brit Mus (Nat
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DmiNAS (\. & A.. KOUKOURAS, 1992. — Circalittoral macrobenthic assemblages of Strymonikos Gulf (N. Aegean Sea)
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Fauchald. K., 1970. Polychaetous annelids of the families Eunicidac. Lumbrineridae, Iphitimidae. Arabellidae.
Lysaretidae and Dorvilleidae from western Mexico. All. Hanc. Monogr. Mar. Biol., 5 : 1-335.
Fauvel, P., 1923. — Polychetes errantes. Faune Fr., 5 : 1-488.
Frame. A.B.. 1992. The Lumbrinerids (Annelida: Polychaeta) collected in two northwestern Atlantic surveys with
descriptions ol a new genus and two new species. Proc. biol. Soc. Wash.. 105 : 185-218.
PRF.D.I, G 1974. - Essai de stockage cl d' exploitation des donnees en dcologie marine. These Doct. Elat Sciences
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Gardiner, S.L., 1976. — Errant polychaete annelids from North Carolina. Elisha Mitchell Sci. Soc.. 91 : 77-220.
George. J.D., & G. IIarTMAN-SchrOder, 1985. — Polychaetes: British Amphinomida, Spinthcrida and Eunicida. Keys
and notes for the identification of the species. Synop. Brit. Fauna. 32 : 1-227.
GL6MAREC. M.. 1968. — Ninoe armoricana n.sp., polychetc Lumbrineridae de la “Grande Vasiere*’ (Golfe de Gascogne)
Vie Milieu. 19 : 315-322.
GLGMAREC, M., 1969. Us peuplements benthiques du plateau continental nord-Gascognc. These Doct. Elat Sciences
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H ARMELIN. J.G., 1969. Contribution a Fctudc de l’endofaune des prairies d’Halophila stipulacea de Mediterranee
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Source : MNHN. Paris
28
Autolytinae (Polychaeta, Syllidae) from Cuba
and north American Atlantic Ocean
Guillermo SAN MARTIN
Laboratorio dc Invertcbrados Marinos, Unidad de Zoologia
Departamento dc Biologia, Facultad de Ciencias
Universidad Autonoma de Madrid
Canto Blanco, E-28049. Madrid. Spain
ABSTRACT
This paper treats nine species of the subfamily Autolytinae (Polychaeta, Syllidae). principally from Cuba, and also
trom North Carolina and Massachusetts. One new species is described, Aulolytus juventudensis. Four species: Aulolytus
convolutus Cognclti. 1953; A. tamanus Imajima, 1966; A. quindecimdentatus Langerhans, 1884; and A. dentalius
Imajima. 1966. are newly reported for Cuba: all these species except the last are also new to the Caribbean and Gulf of
Mexico. Aulolytus inermis Saint-Joseph. 1887 is new to North Carolina.
RESUME
Autolytinae (Polychaeta, Syllidae) de Cuba et des cotes amcricaincs de I'Atlantique Nord
Ce travail presente unc etude de neuf especes d’ Autolytinae (Polychaeta, Syllidae) de Cuba, de Caroline du Nord et du
Massachusetts (Etats-Unis). On decrit une nouvelic espece, Aulolytus juventudensis. Quatre especes : A. convolutus
Cognetti, 1953 ; A. tamanus Imajima, 1966 ; A. quindecimdentatus Langerhans. 1884 et A. dentalius Imajima, 1966,
sont nouvelles pour Cuba. Ces especes. a ['exception de la dcrnicre, sont aussi nouvelles pour les Carai'bes et le golfe du
Mexique. Aulolytus inermis Saint-Joseph. 1887 est nouvelle pour la Caroline du Nord.
INTRODUCTION
This is die seventh paper treating syllids collecled in Cuba during the “Primera Expedieidn Cubano-Espafiola a
la Isla de la Juventud (Isle of Pines) y Archipidlago de los Canarreos”, and elsewhere in neighbouring areas (San
Martin, 1990, 1991 a, b. c. d, 1992). The material from North Carolina and Massachusetts was loaned by die
Zoological Museum, University of Copenhagen (ZMUC), and were mostly collected by Dr. Mary E. Petersen
during 1961-1963 and 1984.
San Martin, G.. 1994. Autolytinae (Polychaeta: Syllidae) from Cuba and North American Atlantic Ocean. In: 3-
C. Dauvin. L. Laubier & D.J. Reish (Eds), Actes de la 4eme Conference internationale des Polychetes. Mem Mus
natn. Hist. nat.. 162 : 269-277. Paris ISBN 2-85653-214-4.
270
G. SAN MARTIN
MATERIAL AND METHODS
Types and oilier specimens are deposited in (he Museo Nacional de Ciencias Naiurales de Madrid (MNCNM),
Spain, die Zoological Museum, University of Copenhagen (ZMUC), and the author's collection.
Measurements refer to the holotype or the largest specimen studied; width was measured at the proventricular
level, without cirri, parapodia or setae. Microscope mounts were made in glycerine jelly of some of the complete
specimens and some parapodia. Drawings and measurements were made using a compound microscope with
differencial interference contrast optics (Nomarsky). Drawings were made using a camera-lucida drawing tube.
A more extensive introduction and additional information about methods and materials have been given in
San Martin ei al, , (1986).
Perkins & Savage (1975), Uebelacker (1984), Ibarzabal (1986, 1988), Day (1973), and Gardiner
( 1976) were used for determination of the new geographical records.
SYSTEMATICS
Family Syllidac Grube, 1850
Subfamily Autolytinae Rioja, 1925
Genus Myrianida Mi lne-Ed wards, 1845
Myrianida sp.
Material examined. — Cuba: Between Puma del Este, Isle of Pines, and Cayo Matfas, Archipelago dc los
Canarreos, from algae at 18 m depth, two incomplete specimens, from Halinieda sp. in Thalassia tesiudinum beds
at 3 m depth, one incomplete specimen.
Remarks. — The three anterior fragments have a trepan with 50-60 triangular, equal teeth and a small
proventriculus, occupying two segments, with about 10 rows of large muscle cells. Myrianida pinnigera
(Montagu, 1808) from the Mediterranean Sea has a similar trepan, but the proventriculus is longer and with more
muscle cell rows. Other known species of Myrianida have fewer teeth in the trepan, longer proventriculus, and
with more rows of muscle cells than these specimens from Cuba.
Distribution. — Cuba.
Genus Proceraea Fillers, 1864
Proceraea sp.
Material EXAMINED. — Cuba: Punta Pedernales, Isle of Pines in living coral from 1.5 m depth, two
specimens. Canal de los Vapores, Cayo Bocas de Alonso, Archipelago de los Canarreos in sponges on
Rhizophora mangle roots at 0.5 m depth, four specimens. Cayo Matfas, Archipelago de los Canarreos from
Halinieda sp., seven specimens. North Carolina, Bogue Sound in sand and shells, 2-4 m depth, two specimens
(ZMUC).
Remarks. — All species of this genus me very similar. The colour pattern is an important differential
character; since all the examined specimens have lost their colouration, it was not possible to identify them.
Distribution. — Cuba and North Carolina.
Genus Autolytus Grube, 1850
Autolytus convolutus Cognetti, 1953
Autolytus convolutus Cognetti, 1953: 323, pi. I, Fig. 1-2 (type-locality: Gulf of Naples). — Cognetti,
1957: 71* fig. 15. — BEN-ELIAHU, 1972: 217, fig. 14 a-d; 1977: 85, fig. 12. — San Martin, 1984: 413, pi.
111.
Source : MNHN. Paris
AUTOLVITNAfi FROM CUBA AND NORTH AMERICAN ATLANTIC OCEAN
271
Autolytus (Regulatus) convolutus — Imajima, 1966: 47, fig. 12 a-h.
M a FERIAL EXAMINED — ( uba: Canal dc los Vapores, Cayo Bocas de Alonso, Archipelago de los Canarreos
r0P‘ 7"^ r°f at 05 m dePUl’ four specimens. Cayo Mafias, Archipielago dc los
specimens Tu,bina"a tuibmata at 3 in depth, one specimen and from Halimeda sp. at 3 m depth, seven
Remarks. — Three specimens have 16 pharyngeal teeth on the trepan instead of nine as usually reported for
dm speaes; however ,n the original description Coonutt. (1953) described several specimens haX 15 - £
teeth. 1 he remaining characters agree with die diagnosis of this species.
DISTRIBUTION. — Mediterranean Sea, Suez Canal, Japan, Cuba.
Autolytus alexandri Malmgren, 1867
PF-mffiWtor?^rrM^fen’ 1867: pL VI1’ fig‘ 39 (type-locality: Davis Strait, Greenland). -
1 hi riBONE, 1963: 147, fig. 37 f, g.
2 cTg'u c°nifrienS Saint‘JosePh- 1887- - Pauvel. 1923: 319, figs 122 h-k. - GlDHOLM, 1967, figs.
Non Autolytus alexandri — Hartman, 1945: 17, pi. 2, fig. 11.
mZAT?r EXAM1NED; - Massachusetts, off Nobska Light. Vineyard Sound in sand, shells, stones and
masses ot Amaroucium pellucidiun at 6-7.5 m depth, two specimens (ZMUC).
HG. 1.- Autolytus alexandri Malmgren, 1867: A. anterior end. dorsal view. B
simple seta. Scale. A: 0.2 mm. B. C, D. 20 pm.
. trepan. C, compound seta. D. dorsal
272
G. SAN MARTIN
Description. — Body broad, especially anteriorly, dark orange, 0.28 mm wide. 2.5 mm long for 40 seiigers
(Fig. 1). Prostomium small, with four large eyes and close on each side. One specimen also had two additional
small anterior eyespots. Palps small. Median antenna long, cylindrical, originating from the middle of
prostomium; lateral antennae damaged on both specimens. Tentacular cirri broken on both specimens. Nuchal
epaulettes reaching setiger 2. Dorsal cirri of first setiger relatively long, similar in length to body width;
remaining dorsal cirri shorter than body width; cirrophores shorter than parapodial lobes. Parapodial lobes rounded.
Parapodia each with about 5-9 compound setae; blades short, strongly bidentate, with both teeth similar, hooked.
Solitary dorsal simple seta from proven tricular setigers. Pharynx very long, with numerous sinuations. Trepan
with nine large teeth separated by two-three smaller teeth. Proventriculus long through about four-six segments
and with about 40 rows of muscle cells.
REMARKS. — Gidholm (1967) suggested that A. cilexandri from North America and the Arctic Ocean are
identical to A. longeferiens from northern Europe. Since the Massachusetts specimens examined agree with
descriptions of both species, these two species appear to be synonymous.
Distribution. — Arctic, Iceland, North American coasts from Labrador to Massachusetts, and from the
Bering Sea to Washington, European Atlantic coasts from Skagerrak to France.
Autolytus toman us Imajima, 1966
Autolytus (Autolytus) tcinianus Imajima, 1966: 46, text-fig. 1 1 e-k (type-locality: Karasu-jima, nearTamano,
Japan).
Material examined. — Cuba: Punta Pedernales, Isle of Pines in living coral at 1.5 m depth, three
specimens.
Fig. 2. — Autolytus tomanus Imajima. 1966: A. anterior end, dorsal view. B, trepan. C, dorsal simple seta. D, compound
setae. Scale. A: 0.2 mm. B: 40 pm. C, D: 20 pm.
Source :
AtriOLYTTNAE FROM CUBA AND NOR'll I AMERICAN ATLANTIC OCEAN
273
DESCRIPTION. — Body small, without colour markings, 0.48 mm wide, 4 mm long for 38 setigers (stolons
not included). Prostomium rounded with four large eyes in open trapezoidal arrangement (Fig. 2). Antennae,
tentacular cirri and dorsal cirri of first setiger longer than body width; remaining dorsal cirri more or less conical,
alternating as long and short cirri. Nuchal epaulettes not seen. Parapodia rounded, shorter than dorsal cirri, each
with about 15 setae which are provided with long proximal tooth and small distal tooth. Solitary dorsal simple
setae bayonet-shaped on posterior segments. Pharynx long, with one sinuation extending from setiger 2 to setiger
9; trepan with about 90 small teeth. Proventriculus long through about 5 segments provided with about 30-40
rows of muscle cells. Anal cirri conical, much longer than dorsal cirri. One specimen with three attached terminal
sexual stolons.
Distribution. — Southern Japan, Cuba.
Autolytus juventudensis sp. nov.
Material examined. — Cuba: off Punta del Frances, Isle of Pines in dead coral at 1 m depth: holotype and
two paratypes (MNCNM). Punta Pedemales, Isle of Pines in living coral at 1.5 m depth, two juvenile specimens.
FIG. 3. — Autolytus juventudensis n. sp. Holotype: A. anterior end, dorsal view. B, trepan. C, compound seta. D, dorsal
simple seta. Scale. A: 0.2 mm. B: 40 pm. C. D: 20 pm.
274
G. SAN MARTIN
Description. — Body long, slender, holotype 0.28 mm wide, 4.6 mm long lor 60 setigers (Fig. 3).
Prostomiuin small, rounded, with two pairs of large eyes, palps small, fused, not visible dorsally; antennae long,
extending to at least setiger 8. Nuchal epaulettes small, oval, reaching setiger 1. Dorsal tentacular cirri shorter
than antennae; ventral tentacular cirri about half the length of die dorsal cirri. Dorsal cirri of setiger 1 long,
shorter than dorsal tentacular cirri; dorsal cirri of setiger 2 shorter than dorsal cirri of setiger 1; remaining dorsal
cirri proportionally long, alternating irregularly long, similar in length to body width, and shorter. Antennae,
tentacular and dorsal cirri provided with small, rounded, hyaline inclusions. Pygidium small, with two long anal
cirri. Parapodia rounded, each with about 7-8 compound setae with short blades and provided with a proximal a
toodi somewhat larger than distal tooth. Solitary dorsal simple seta bayonet-shaped, slender, from about setiger 8.
Pharynx very long with two long coils, trepan in setiger 3 with about 43 small, equal teeth. Proventriculus from
setiger 14 to setiger 18 with about 25 rows of muscle cells.
REMARKS. — Autolytus juventudensis is characterized by having a slender body with relatively long dorsal
cirri, a long and coiled pharynx and a trepan of more than 40 equal teeth. This species is similar to A. magnus
Berkeley, 1923 from Alaska and Japan, but die blades of die compound setae are very different (see IMAJIMA &
Hartman. 1964). The two teedi of the blades are similar and hooked in A. magnus, in contrast to the typical
shape for the genus in A. juventudensis. Compound setae of A. irregularis Imajima & Hartman, 1964 from Japan
are very similar to those of A. juventudensis : however, die former has a trepan wiih only 21-27 teeth and the
nuchal epaulettes extend through live segments, and die latter has more dian 40 teeth in the trepan and the nuchal
epaulettes are shorter.
The two juvenile specimens have a proportionally shorter pharynx with fewer coils and about 33 teeth in the
trepan; proventriculus shorter and extending through about four segments and provided with about 32 rows of
muscle cells. The juvenile specimens are very similar to A. prolifer ; however, the dorsal cirri are proportionally
longer and are provided with refringent granules which are absent in A. prolifer. Adults of A. juventudensis differ
from A. prolifer in the number of pharyngeal teeth and in die length of the pharynx and proventriculus.
Etymology. — The specific name comes from Isla de la Juventud = Isle of Pines), the type locality of this
species.
Distribution. — Cuba.
Autolytus inermis Saint-Joseph, 1887
Autolytus inermis Saint-Joseph, 1887, p. 237, fig. 117 (type-locality: Dinard, France). — GlDHOLM, 1967:
193, figs 7 D-E, 22.
Autolytus (Autolytides) inermis — Fauvel, 1923: 322, figs 123 h-k.
Material EXAMINED. — North Carolina: Bogue Sound from sand and shells at 2-4 m depth, two specimens
(ZMUC). Core Sound, Cowpen Island from empty shells, one specimen (ZMUC).
DESCRIPTION. — Body proportionally short and broad, yellowish, without colour pattern, 0.32 wide, 4 mm
long for 71 setigers (Fig. 4). Prostomium rounded with two pairs of large eyes in open trapezoidal arrangement;
antennae relatively short and thick, cylindrical. Palps fused, not visible dorsally. Tentacular cirri relatively short,
similar to antennae. Nuchal epaulettes long extending to setiger 4. Segments well marked dorsally. Dorsal cirri
shorter or equal in length to half of body width, with long cirrophores, alternating irregularly long and short
dorsal cirri. Parapodia each with 5-6 similar compound setae with short blades, proximal tooth somewhat larger
than distal tooth. Solitary dorsal simple setae bayonet-shaped on posterior segments. Pharynx from setiger 2 to
setiger 11 with a terminal coil. Trepan indistinct with about 26 very small, subequal teeth. Proventriculus small
extending through about 6 segments with 12-14 rows of thick muscle cells.
Remarks. — The northern European and French specimens described by GlDHOLM (1967) have
proportionally longer antennae and anterior dorsal cirri as well as a longer pharynx. However, I do not think that
these small differences justify erecting a new taxon for these specimens from North Carolina.
Distribution. — Northern-European Atlantic coasts, North Carolina.
Source : MNHN. Paris
AUTOLYTTNAE FROM CUBA AND NORTH AMERICAN ATLANTIC OCEAN
275
Autolytus quindecimdentatus Langerhans, 1884
Autolytus quindecimdentatus Langerhans, 1884: 249, fig. 3 a-b (type-locality: Madeira. Portugal). —
GlDHOLM, 1967: 197. figs 7 f. 12, 23 a. — Campoy, 1982: 241. — San Martin, 1984: 417, pi. 1 13.
PlG. 4. — Autolytus inennis de Sainl-Joscph. 1887: A. anterior end, dorsal view. B. mouth of the pharynx. C. dorsal
simple seta. D, compound seta. Scale. A: 0.2 mm. B. C. D: 20 Jim.
Material examined. — Cuba: Off Cayo Matias from Turbinaria turbinata at 3 m depth, nine specimens,
from Stypopodium zonale at 3 m depth, one specimen. Between Punta del Este and Cayo Matias from algae at
18 m depth, one specimen and from Halimeda sp. in Thalassia testudinuni beds at 3 m depth, two specimens. Off
Punta del Frances, Isle of Pines from algae at 4 m depth, four specimens. Off Cayo Matias from Halimeda sp. at
3 m depth, five specimens.
DISTRIBUTION. — Mediterranean Sea, Atlantic European and African coasts, from Scandinavia to Canary
Islands, Red Sea, Cuba.
Autolytus den tali us Imajima, 1966
Autolytus (Autolytus) dental ins Imajima, 1966: 36, fig. 7 i-1 (type-locality: Senda-Zaki, in Uraga Strait,
Japan). — Day, 1973: 35. — Gardiner, 1976: 127, fig. 10 a-d. — Uebelacker, 1984: 30-12, fig. 30-4.
Material examined. — Massachusetts, off Nobska Light, Vineyard Sound from sand, shells, stones, and
masses of Amaroucium pellucidum at 6-7.5 m depth, one specimen (ZMIJC). North Carolina, Bogue Sound from
shells and sand at 2-4 m depth, 73 specimens (ZMUC). Cuba: Off Punta del Frances, Isle of Pines from in dead
coral at 1 m depth, four specimens. Off Cayo Matias, Archipelago de los Canarreos from Halimeda sp. at 3 m
depth, one specimen. Off Punta del Frances from algae at 4 m depth, one specimen.
Distribution. — Japan, Massachusetts, North Carolina, Gulf of Mexico, Cuba.
276
G. SAN MARTIN
ACKNOWLEDGEMENTS
I wish to express my gratitude to all members of die Cuban-Spanish Expedition, especially to the Cuban
researchers from the Centro de Investigaciones Marinas de la Universidad de La Ilabana. Dr. Mary E. Petersen,
Zoological Museum of die University of Copenhagen, Denmark, loaned die material from Massachusetts and
North Carolina, offered useful advice to me, and revised die manuscript, as well as two anonymous referees.
REFERENCES
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BEN-Eliahu, M. N.. 1977. — Polychaete cryptofauna from rims of similar intertidal vermetid reefs on the Mediterranean
coasts of Israel and in the Gulf of Elat: Exogoninae and Autolytinac (Polychaeta Erranlia: Syllidae). Isr. J. Zool. ,
26 : 59-99.
BERKELEY, E.. 1923. Polychaetous Annelids from the Nanaimo District. Part I. Syllidae to Sigalionidae. Contribs .
Cancid. Biol.. 1 : 203-218.
CaMPOY, A.. 1982. — Fauna de Espaha. Fauna de Anelidos Poliquetos de la Peninsula Iberica. EUNSA (Ediciones de la
Universidad de Navarra. S. A.). 781 pp.
COGNETTI, G., 1953. — Osservazioni sulla biologia riproduttiva di una nuova spece di Autolytus del Golfo di Napoli.
Arch. Zool. It.. 38 : 323-332.
COGNETTI, G.. 1957. — 1 sillidi del Golfo di Napoli. Pubbl. Staz . Zool. Napoli. 30 : 1-100.
Day, J. II.. 1973. — New Polychaeta from Beaufort with a key to all species recorded from North Carolina. NOAA Tech.
Rep. NMFS Circ.. 375 : 1- 140.
FaUVEL, P.. 1923. — Polychetes Errantes. Faune Fr.. 5 : 1- 488.
Gardiner. S. L.. 1976. — Errant polychaete annelids from North Carolina. J. Elisha Mitchell Sci. Soc.. 91 : 78-220.
GIDHOLM, L.. 1967. A revision of Autolytinae (Syllidae. Polychaeta) with special reference to Scandianvian species,
and with notes on external and internal morphology, reproduction and ecology. Ark. Zool.. 19 : 157-213.
HARTMAN, O.. 1945. — The marine annelids of North Carolina. Duke Univ. Mar. Sta. Bull. , 2 : 1-54.
Ibarzabal, D.. 1986. Lista de especies de poliquetos bentonicos cubanos. Rep. Invest. Inst. Oceanol.. 45 : 1-17.
Ibarzabal. D., 1988. — Poliquetos de Punta del Este. Isla de la Juventud. II. Familias Phyllodocidae. Hesionidae y
Syllidae. Poeyana. 359: 1-10.
Imajima, M.. 1966. The Syllidae (polychaetous annelids) from Japan (IT), Autolytinae. Publ. Seto Mar. Biol. Lab.,
14 : 27-83.
Imajima. M. & Hartman. O.. 1964. — The polychaetous annelids of Japan. Allan Hancock Found. Occ. paper , 26 : 1-
452.
LaNGERHANS. P., 1884. — Die Wurmfauna von Madeira. IV. Zeitschr. Wiss. Zool., 40 : 247-285.
Malmgren. A. J. 1861. — Annulata Polychaeta. Spetsberglae. Groenlandiae, Islandiae et Scandinaviae Hactemus
Cognita. Forh. Oefv. K. Vetensk. Akad. Stockholm, 24 : 1-125.
Montagu, G. 1808. New and rare animals found on the South Coast of Devonshire. Trans. Linn. Soc. London. 9 :
108- 111.
Perkins, T. H. & Savage, T., 1975. — A bibliography and checklist of polychaetous annelids of Florida, the Gulf of
Mexico, and the Caribbean region. Florida Mar. Res. Publ., 14 : 1-62.
PETTIBONE. M. IT, 1963. Marine Polychaete worms of the New England region. 1. Aphroditidae through
Trochochaetidae. Bull. U. S. Nat. Mus 227 : 1- 356.
Saint-Joseph. Baron de, 1887. — Les annelides polychetes dcs cotes de Dinard. Ann. Sci. Natur. Zool., ser. 7, 1 : 127-
270.
Source : MNHN. Paris
AUTOLYTINAE FROM CUBA AND NORTH AMERICAN ATI-ANTIC OCEAN
277
San Martin, G., 1984. — Estudio biogeog rdfico, faunistico y sistemdtico de los Poliquetos de la Faniilia Silidos
(Polychaeta: Syllidae) en Baleares. Tesis Doctoral. Ediciones de la Universid Complutense de Madrid, 186 : 529 pp.
San Martin, G., 1990. — Eusyllinae (Syllidae, Polychaeta) from Cuba and the Gulf of Mexico. Bull. Mar. Sci.. 46 :
590-619.
San MARTIN, G.. 1 99 1 a. — Sphaerosyllis and Parapionosyllis (Exogoninae. Syllidae, Polychaeta) from Cuba, Florida
and the Gulf of Mexico. Ophelia Suppl., 5 : 231-238.
San Martin. G.. 1991 b. — Syllinae (Polychaeta: Syllidae) from Cuba and the Gulf of Mexico. Bull. Mar. Sci.. 48 (2) :
227-235.
San Martin. G.. 1991 c. — A new species of Pionosyllis Malmgren. 1887 (Polychaeta: Syllidae: Eusyllinae). from
Cuba. Graellsia , 47 : 17- 20.
San Martin, G., 1991 d. — Gnibeosyllis and Exogone (Exogoninae. Syllidae. Polychaeta) from Cuba, Puerto Rico,
Florida and the Gulf of Mexico, with a revision of Exogone. Bull. Mar. Sci.. 49 : 715-740.
San Martin, G.. 1992. Syllis Savigny in Lamarck. 1818 (Polychaeta: Syllidae: Syllinae) from Cuba, the Gulf of
Mexico, Florida and North Carolina, with a revision of several species described by Vcrrill. Bull. Mar. Sci.. 51 :
167-196.
San Martin, G., Aguirre, O. & BaratECH, L., 1986. — Anelidos Poliquetos procedentes de la I Expedition Cubano-
Espanola a la Isla de la Juventud y Archipielago de los Canarreos. I. Familias Polynoidae, Sigalionidae, Pholoididae
y Pisionidae. Rev. Inv. Mar.,1 (1): 3-16.
UEBELACKER, J. M., 1984. — Family Syllidae Grube. 1850. Itr. J.M. UEBELACKER & P. G. JOHNSON (eds.). Taxonomic
guide to the polychaetes of the northern Gulf of Mexico. Barry A. ViTTOR & Associates. Mobile, 30 : 1-151.
Source : MNHN, Paris
29
New arctic species of Scolelepis
(Polychaeta, Spionidae)
Andrew V. SIKORSKI
Zoological Museum of the Moscow Lomonosov State University
Herzen Street 6, K-9, Moscow 103009, Russia.
ABSTRACT
Three new species of Scolelepis were present in the Russian collections from the Arctic Ocean and the border areas
S . matsugae , S. burkovskii and S. korsuni. All these are from the Barents Sea. S. korsuni is known also from the
nothern part of the North Sea, and S. matsugae from the Kara Sea and Franz- Josef Land. There are no another species of
Scolelepis in the Russian arctic zoological collections. The diagnostic characters for S. korsuni are: presence of superior
flag-like process in middle dorsal lamellae, absence of setae in first notopodiae, shape of hooks and their number; for
S. matsugae : shape of prostomium, shape of hooks, setigcr of hooks starting and pattern of branchiae decreasing.
S. burkovskii separated by complex of characters. Five species with S. squamatus (O.F.Muller, 1806) and 5. foliosus
(Audouin & Milne Edwards. 1833) are now known from the Arctic Ocean and the border areas.
RESUME
Nouvelles especes arcticjues du genre Scolelepis (Polychetes, Spionidae)
Trois nouvelles especes de Scolelepis ont etc trouvees dans les collections russes de l'oc6an Arctique et des mers
polaircs : S . matsugae. S. burkovskii et S. korsuni. Ces trois especes proviennent de la mer de Barents. S. korsuni est
aussi presente dans la partie nord de la mer du Nord, et S. matsugae dans la mer de Kara et pres de la Terre Fran^ois-Joseph.
Les caracteres distinctifs de S. korsuni sont les suivants : la presence d'expansion en forme de drapeau au milieu de la
lamclle dorsale, l’absence de soies dans les premiers notopodes. la forme et le nombre des crochets ; ceux de S. matsugae
sont : la forme du prostomium et des crochets, le niveau d'apparition du premier sitigere avec des crochets el la forme de
la branchie. .S', burkovskii a ete separce des autres especes par plusieurs caracteres. Cinq especes. y compris S. squamatus
(O.F. Muller, 1806) et S. foliosus (Audouin & Milne Edwards. 1833), sont maintenant connues dans l'oc£an Arctique.
INTRODUCTION
Only two species of Scolelepis de Blainville, 1828, S. squamatus (O.F. Miiller, 1806) and S. foliosus
(Audouin & Milne Edwards, 1833), are known from die Arctic Ocean and die border areas. The former lias been
recorded off Iceland (Wesenberg-Lund, 1951) and from the Norwegian Sea (Hartmann-Schrodf.r, 1971);
SlKORSKl, A.V., 1994. — New arctic species of Scolelepis (Polychaeta, Spionidae). In: J.-C. DAUVIN, L. LAUBIER &
D.J. REISH (Eds), Actes de la 4eme Conference internationale des Polychetes. Mem. Mus. natn. Hist, nat .. 162 : 279-
286. Paris ISBN 2-85653-214-4.
280
A. V. SIKORSKI
the latter species is known from the Norwegian coast to Finmark (Sars, 1851, 1873). An examination of all
Russian collections from the area (about 2,500 samples) revealed an additional three new species from the Barents
Sea (with the Franz-Josef Land) and the Kara Sea.
MATERIAL
Specimens described in this paper are deposited in Zoological Museum, Moscow Lomonosov State University
(ZMUM), Zoological Institution of St. Petersburg (ZIN), Zoological Museum. University of Copenhagen
(ZMUC), Museum National d'Histoire Naturelle of Paris (MNHN) and the reference collection of Akvaplan-niva
(AKV), consulting firm, Tromso, Norway.
systp:matics
Scolelepis de Blainville, 1828
Diagnosis. — Prostomium anteriorly pointed or bluntly rounded, extending posteriorly as a narrow caruncle.
Occipital crest generally well developed, sometimes forming occipital tentacle; 0-2 pairs of eyes. Peristomium generally
not fused with setiger 1, lateral wings variously developed. Ncuropodial hooded hooks present, notopodial hooded
hooks present or absent; secondary hoods sometimes present. Sabre setae absent. Flattened branchiae from setiger 2 on
anterior half of body, sometimes continuing to posterior end. Anterior branchiae completely or mostly fused with dorsal
lamellae. Dorsal nuchal organ (according to SODERSTROM. 1920) restricted to small areas on either side of posterior
caruncle. Anus terminal or dorsal. Pygidium with ventral cushion (incised or entire), oval or multilobed membrane. Dark
pigmentation resistant to alcohol, occurs primarily on the prostomium and pygidium.
I agree with the point supported by Blake & KUDENOV (1978) and Maciolek (1987) dial many exceptions
occur with the set of characters making the separation of die genera Scolelepis de Blainville, 1828 and Nerinides
Mesnil, 1896 unfeasible at this time.
Separation of subgenus Parascolelepis proposed by Maciolek (1987) seems interesting, but I am not sure if
it is possible in Scolelepis-ge nus to use the shape of hooded hooks for separating taxa above species. We can see
gradations in the genus between the falciger-likc type of hooks widi 0-3 short apical teedi for subgenus Scolelepis
and sharp-tanged, multidentate hooks lor subgenus Parascolelepis. Moreover, diere are many species in the genus
showing both individual and size variation of die shape of hooded hooks. I think diat more useful character might
be die presence ot a sheath at the base of die palps, but I do not have complete information for all species. I do
not separate these two subgenera herein.
Scolelepis korsuni s p . n o v .
? Nerinides tridentata — Hannerz, 1956: 9-11, Fig.l(a-c). — Kirkegaard, 1969: 79, Fig. 42.
Material EXAMINED. — North Sea. coll. AKV for Elf Aquitaine; stn 4-1 (LILLE FRIGG II), 59°57'42"N, 2C23'44"E,
108 m. 1 1 .V. 1992: holotype (ZMUC). Forty samples (LILLE FRIGG II), from 59°56’ to 60°01’30"N, from 2°20’ to
2 25'45"E. 95-111 m. 7-1 l.V. 1992: 78 paratypes (ZMUM PI 1/883-6/888, 8/890-13/895. 15/897-24/906. 25/910-
45/930 ; ZIN 1/48517. 2/48518 - two specimens; five specimens in AKV; one specimen in MNIIN). Ten samples (N0
FRIGG). from 59 57’40" to 60 0L30"N, from 2*12' to 2o23'30"E. 95-110 m. 13-14 and 1 7- 1 8.V. 1992: 10 paratypes
(ZMUM PI 47/932-51/936; five specimens in AKV). five samples (HEIM DAL), from 59 34’ to 59°36'N. from 2°ir40"
to 2 14T5"H. 114-1 16 m, 15-17. V. 1992: five paratypes (ZMUM PI 7/889, 14/896, 46/931; two specimens in AKV).
Barents Sea. R/V "Tunets": stn 105.20. 73:0LN. 22°00’E, 440-450 m. silt, 1.16 C. 4.VII.I978: one paratype (ZMUM
PI 52/824). 1
1)LS( RIPTION. — Holotype complete, 1.2 mm wide and 13.2 mm long, 46 setigers, widiout palps. Fig.
la-h.
The smallest specimen (ZMUM PI 899), 0.6 mm wide and 6.6 mm long for 34 setisers. The longest
complete specimens (ZMUM PI 882, 886, 901), 1-1.2 mm wide and 11-13 mm long for 40-46 setigers. The
longest incomplete specimen (ZMUM PI 900), 1.6 mm wide and 21 mm long for 51 setigers. The largest
Source : MNHN [ Paris
Fig. 1. — Scold epis korsuni sp. nov.: a. anterior end through first 4 setigers, in dorsal view (palps missing). - b, same
anterior end, in lateral view. - c, palp. - d, parapodium of setiger 8. - e. parapodium of setiger 19. - f, pygidium. - g, a
hooded hook of parapodium 21 (in lateral view). - h. distal end of same seta (in frontal view - scheme). — Scolelepis
burkovskii sp. nov. : i. anterior end through first 4 setigers, in dorsal view (palps missing). - j. first parapodium. -
k. seventh parapodium. - 1. parapodium 17. - m. a posterior, or second last, parapodium. - n, a hooded hook from
parapodium 18, in frontal -lateral view. - o, distal end of same seta. - p, distal end of same seta (in frontal view -
scheme). Scale: a-b, 1 mm; c. f, 1.4 mm; d, 0.6 mm; e. 0.4 mm; g, 0.06 mm; i, 0.56 mm; j-m, 0.28 mm; n,
0.044 mm; o, 0.017 mm.
Source MNHN. Pans
282
A. V. SIKORSKI
incomplete specimen (ZMUM PI 889), 2.1 mm wide and 1 1 mm long for 26 setigers.
Prostomium spindle-shaped, anteriorly projecting, elongate (Fig. 1-a) narrowing posteriorly into pointed
caruncle reaching posterior margin of setiger 2 (visible only if stained with methyl green). Eyes usually absent:
one specimen (ZMUM PI 932) had two pairs small rounded eyespots of nearly equal size arranged in transverse
line slightly curved toward anterior end. Occipital crest more or less pronounced. Occipital tentacle pointed, erected
and oriented usually anteriorly. Grooves between prostomium and pcristomium narrow. Palps long sometimes
reaching middle of body, with cogged basal sheath (Fig. 1-c). Lateral wings of pcristomium are low. There are
small folds surrounding die place of palp's attachment. Pharynx often everscd. The posterior ventral border of
setiger 1 is clearly visible oriented toward the mouth (Fig. 1-b).
Branchiae from setiger 2, completely fused to longer notopodial lamellae (Fig. 1-d). From setiger 14-19
notopodial lamellae deeply notched at level of branchial bases (Fig. 1-e) forming fiag-likc process. As a result,
branchiae and notopodial lobes seem to be fused only at base. Branchiae became of nearly equal size with postsetal
notopodial lobes from setiger 17-28, which gradually decreased in size to the posterior end of body. Posterior
notopodial lamellae small and oval. Neuropodial lamellae of anterior 14-20 setigers are wide and high, rectangular
with rounded margins. Width of inferior half of neuropodial lamellae decreases from setiger 15-21 (Fig. 1-e).
Hooks situated beneath neuropodial lamellae from setiger 17-23. Notopodia shifted dorsally from setiger 16-28.
Segments become longer after setiger 16-21.
Setiger 1 lacks notosetae. Sabre setae or inferior neuropodial fascicle of setae absent. Neuropodial hooded
hooks from setiger 14-18: up to 14 per fascicle, but reaching this number only in largest specimens and in a few
segments (1-3) 'usually from segment 10-15 after starting of hooks. There are three teeth in hooks (in lateral
view), and four teeth (in frontal view): highest tooth paired as a rule (Fig. lg-h). Secondary hood absent.
Notopodial hooded hooks absent. Notopodial capillaries become longer after setiger 14-19.
Pygidiuin with oval more or less flattened, slightly bilobed ventral cushion (Fig. 1-0.
Pigmentation. — None.
Remarks. — The shape of prostomium and the shape of hook in lateral view, the setiger where neuropodial
hooks begin and the presence of a notch on notopodial postsetal lobe makes this species close to Scolelepis
tridentata (Southern, 1914). However the absence of an inferior fascicle in the neuropodium and the characteristic
outline of hook's hood, the presence of four-teeth hooks with different arrangement of apical teeth separated this
taxon from .S', tridentata (Light, 1977, 1978). The absence of notosetae on setiger 1 (Southern, 1914) would
have been similar as in .S’, tridentata and S. korsuni, but Light (1978) reported after studying type material of
S. tridentata that the syntypes do have notopodial fascicle on setiger 1.
Fused branchiae and postsetal notopodial lobes form superior flag-like process in the middle of body so some
researchers may think this species is equal to S. gilchristi (Day, 1961) or S. geniculata Imajima, 1992, but
S. gilchristi and S. geniculata have notosetae on setiger 1 whereas .S', korsuni does not.
This species is also close to S. quinquedentata (IIartmann-Schrodf.r, 1965), S. papillostis (Okuda, 1937)
and S. texana Foster, 1971. .S’, quinquedentata differs in die shape of hooks, the number of hooks per
neuropodium, notopodial lobes shorter than branchiae, anterior and posterior eyespots of different shape.
S. papillostis has entire notopodial lobes on at least 42 anterior setigers with up to 18 hooks per neuropodium.
S. texana differs in the shape of hooks, entire notopodial lobes on anterior 30 setigers and a number of hooks per
neuropodium.
Etymology. — This species is named for Dr. Sergey A. Korsun, Marine Biological Institution of
Murmansk, I Ie is a specialist on Foraminifera and my good friend.
Scolelepis burkovskii sp.nov.
MATERIAL EXAMINED. Barents Sea. R/V "Pomor": stn 17.5l\ 69°08’N, 50 22'E, 19 in, sand, 4.30 'C, 16. VII. 1985.
grab 1: hololype (ZMUM PI 821) and three paratypes (ZMUM PI 822); grab 2: two paratypes (ZMUM PL 823 and
ZMUC).
Description. — Maximum length - 8-9 mm; maximum width - 0,6 mm. The single complete specimen had
50 setigers. Figs 1 i-p.
Prostomium anteriorly pointed with an approximately right angle (Fig. 1-i). Caruncle narrow and pointed,
extending posteriorly to the middle of setiger 2. Two pairs of eyespots. Occipital crest not pronounced. Occipital
Source :
NEW ARCTIC SPECIES OF SCOIELEP1S (SPIONIDAE)
283
tentacle absent. Palps without basal sheath (present in only the holotype) reaching posteriorly to setiger 6-7.
Peristoiniutn without lateral wings.
Branchiae flattened, partly fused basally with notopodial lamellae. Branchiae of setiger 2 approximately 1.5
times longer than notopodial lamellae. On the following setigers the ratio increases to 2 or 3 times (Figs 1 k-1).
Branchiae continuing throughout body, but becoming progressively smaller in posterior third of body with the
upper margins becoming of equal length with notopodial lamellae in die last setigers.
Notopodial lamellae of several anterior setigers slightly elongated becoming more or less semicircular in die
following setigers. Neuropodial lamellae of setiger 1 small and low lamellae becoming higher and semicircular in
the following setigers; they are slightly asymmetrical anteriorly with a wide dorsal half (Fig. 1-j). Notch on
neuropodial lamellae absent.
Setiger 1 with notosctac (Fig. 1-j). An inferior fascicle of capillary setae present in die neuropodium in all
setigers (sabre setae absent). Notopodial fascicle becomes narrow posteriorly consisting of a small number of
capillaries (Fig. 1-m). Neuropodial hooks from setiger 17-19, numbering 6-8 per fascicle”; hooks tridentate widi
pair of widely arranged apical teedi surmounting main tooth (Figs 1 o-p). Notopodial hooks absent.
Pygidium with the scalloped membrane surrounding terminal anus.
PIGMENTATION. — Medial longitudinal narrow dark Strip present from the anterior margin of prostomium to
behind the posterior pair of eyes. In addition, several small spots may be present behind eyes forming 2 dark fields
connected with a longitudinal strip (Fig. I-i).
Remarks. — This species may be confused widi Spio theeli (SOdf.rstrom, 1920) in habiting in the same
area. Maciolek (1987) placed Microspio tlieeli into Scolelepis but this species does belong to Spio- genus group.
The new species can be separated by the shape of the hooded hook and the absence of sabre setae in inferior
fascicle of neuropodium. I attribute this species to Scolelepis because of die shape of pygidium and prostomium,
the absence of segmented nuchal organ and the absence of sabre setae. This species differs from the oilier species
of genus Scolelepis by starting of hooded hooks, shape of hooks, prostomium, parapodial lobes and composition
of setae in neuropodia.
Etymology. — The species is named in honour of Professor Igor V. Burkovski who was my principal
advisor of my Ph. D. Thesis.
Scolelepis matsugae sp.nov.
Material EXAMINED. Barents Sea. Drozdovka Inlet. Exp. of Murmansk Marine Biological Instution. coll.
A.V.Sikorski: stn PI. 68T8’20"N. 38°25'E, grab. 7.5 m. sandy silt with detritus. 1 7. VIII. 1984: holotype (ZMUM PI
818). Franz Josef Land. Hayes Isl. Exp. ZIN. coll. V.G. AVERINTSEV & A. F. PUSHKIN: stns 22. 40. 43. 44. 54, 73, 83:
80 35'N, 57°50’E, 3-7 m, silt and in Maria esculenta on stones, X-XII.1981: 10 paratypes (ZMUM PI 819 and PI 820;
ZIN 2/47388-8/47394: one specimen in ZMUC). Kara Sea. R/V "Zarja". coll. Russian Polar Exp.: stn 12d, 74 28’N.
83°33’E. 52 m. thin clay, 19. VIII. 1900: one paratype (ZIN 1/47387).
Description. — Holotype complete, 1.7 mm wide and 9.5 mm long for 48 setigers; maximal number of
setigers 50; largest specimen incomplete, 2.8 mm wide. Figs 2a-k.
Prostomium with three semicircular anterior projections (Fig. 2-a); middle projection, especially in juveniles,
less prominent than the lateral ones (Fig. 2-c) ; occipital crest high, well pronounced, posteriorly ending abruptly;
caruncle ending at base of setiger 1 ; two pairs of eyes present, with anterior pair larger, crescent-shaped and further
apart spaced than posterior pair. Longitudinal groove on prostomium well developed in adults, and extend from the
base of occipital crest to the anterior margin around middle projection. Pcristomium large in comparison to
prostomium, high, laterally inflated. Pharynx often more or less eversed, resulting in anterior margin of
prostomium being abruptly turned dorsally. Pcristomium distinct from setiger 1, lateral wings lacking; palps
thick, long, without basal sheath extending posteriorly to setiger 14.
Setiger 1 without notosetae but with notopodial lamellae. Branchiae flattened, fused entirely to wide Setiger 1
without notosetae but with notopodial lamellae. Branchiae flattened, fused entirely to wide notopodial lamellae.
Branchiae of setiger 2 are well developed, long and only 1.5 times shorter than longest one on setiger 14 or 15;
fused branchiae mid notopodial lamellae abruptly diminished on setiger 22-29, becoming low, semicircular and not
changing in shape and size posteriorly.
284
A. V. SIKORSKI
Fig. 2. — Scolelepis mcitsugae sp. nov.: a. anterior end through first four setigers, in dorsal view (palps missing), b.
same anterior end. in lateral view, c, anterior end of juvenille specimen, in dorsal view, d, pygidium. e, first
parapodium. f, parapodium 23. g, parapodium 25. h. parapodium 36. i, distal end of a hooded hook (in frontal view
scheme). - j. a hooded hook from parapodium 25. in lateral view. Scale: a and b. 1 mm; c, 0.3 mm; d. 0.8 mm; e-h,
0.5 mm: j. 0.035 mm.
Neuropodial postsetal lamellae of anterior setigers irregularly rounded, with notch starting from setiger 16-18;
ventral parts of neuropodial postsetal lamellae on following segments reduced, resembling narrow membrane and
absent on posterior setigers. Almost all neuropodial fascicles of anterior half of body shorter than the upper part of
neuropodial postsetal lamellae. Superior notopodial capillares of anterior setigers longest. Sabre setae or inferior
fascicle of neuropodium absent. Neuropodial hooks present from setiger 11-22, numbering up to 9 per fascicle.
Only young specimens (< 0.5 mm width) have hooks from setiger 11-13. Shedding of hooks connected with age
confirmed by presence of one hook in neuropodium 14 of holotype; the next neuropodium with hooks in the
holotype was in setiger 17. Notopodial hooded hooks begin at setigers 13-26, numbering up to 5 per fascicle.
Hooks are tridentate in side view, but in frontal view main tooth clearly surmounted by pair of apical teeth and a
single, unpaired (Figs 2 i-j).
Anus terminal, sometimes slightly displaced to dorsum (Fig. 2h). Pygidium with ventral transverse cushion.
PIGMENTATION. — A slight dark stripe present along posterior part of longitudinal groove on prostomium
with two dispersing stripes in front of eyes (Fig. 2-a). One juvenile specimen with transverse dark stripes behind
anterior pair of eyes (Fig. 2-c). Proximal part of eversed pharynx usually with dark ring. One specimen with
pigment on tip of notopodial postsetal lamellae on setiger 3. Anal cushion pigmented. Palps with diffused
pigment.
Remarks. — This species resembles Scolelepis oligobranchus (Chlebovitsch, 1959). However, S.
mcitsugae differs from .S', oligobranchus in its smaller size, fused branchiae and notopodial postsetal lamellae
reduced more anteriorly, absence of an inferior fascicle of neuropodium, shape of pygidium and shape ol hooks.
Hooks of S. oligobranchus are bifid in side view but their apical tooth paired; it had not been mentioned in
original description but it is clearly visible in die holotype.
Source :
NEW ARCTIC SPECIES OF SCOLELEPIS (SPIONIDAE)
285
ETYMOLOGY. — The species is named for my mother Nina Pavlovna SlKORSKA. Her maiden name was
MATSUGA.
There are now five valid species of genus Scolelepis known from the Arctic Ocean.
Key to species of Scolelepis from the Arctic Ocean
1 Prostomium pointed anteriorly . 2
Prostomium rounded or trifid anteriorly . 4
2 Anterior branchiae completely fused to dorsal lamellae;
setiger 1 without notosetae . S. korsuni
Anterior branchiae free distally; setiger 1 with notosetae . 3
3 Neuropodial hooks from setiger 17-19; ventral lamellae without notch;
notopodial hooded hooks absent . S. burkovskii
Neuropodial hooks from setiger 26-42; ventral lamellae with
a notch after setiger 18-20; notopodial hooks from setiger 60-75 . S. squamatus
4 Neuropodial hooks from setiger 1 1-22; branchiae become
very short abruptly on setiger 22-29 . S. matsugae
Neuropodial hooks from setiger 50-67; branchiae diminish gradually
becoming very short near end of body . S. foliosus
ACKNOWLEDGEMENTS
I would like to thank Drs. I. A. JlRKOV, M.A. Safronova, A.B. TZETLIN for reviewing the manuscript ;
M.V. Kolesnikov, a.K. Karamyshev, Drs. V.G. Averintsev, A.F. Pushkin, N.A. Anisimova, the
consulting firm Akvaplan-niva and Elf Aquitaine Norge AS for helping in collectioning the specimens. I am
especially grateful to die referees of the manuscript for their critical review and to Dr. M.E. PETERSEN for
valuable advise.
REFERENCES
Blake, J.A. & KUDENOV, J.D, 1978. — The Spionidae (Polychaeta) from southeastern Australia and adjacent areas with a
revision of the genera. Mem. Nat. Mus. Victoria. 39 : 171-280.
BLAINVILLE, H. de, 1828. — Dictionnaire des Sciences naturelles. 57 : 368-501.
CHLEBOVITSCH. V.V., 1959. Species of polychaete worms from the Kuril Islands, which are new or recorded for the
first time on the USSR (Leningrad). Zool. Zh.,3$ : 167-181 (in Russian).
Day, J.H., 1961. — The polychaete fauna of South Africa. Part 6. Sedentary species dredged off Cape coasts with a few
new records from the shore. J. Linn. Soc. Zool. , 44 : 463-560.
FOSTER, N.M.. 1971. — Spionidae (Polychaeta) of the Gulf of Mexico and the Caribbean Sea. Stud. Fauna Curasao, 36 :
1-183.
HaNNERZ. L., 1956. — Larval development of the polychaete families Spionidae Sars, Disomidae Mesnil, and
Poecilochactidae n. fam. in the Gullmar Fjord (Sweden). Zool. Bidr. Uppsala, 31 : 1-204.
HartmaNN-SchrODER, G., 1965. — Die Polychaeten des Sublitorals. In : G. HARTMANN-SCHRODER & G. HARTMANN
(eds.), Zur Kenntnis des Eulittorals der chilenischen Kiiste unter besonderer Beriicksichtigung der Polychaeten und
Oslraeoden. Mitt. hamb. zool. Mus. Inst.. Suppl. 62 : 59-305.
HARTMANN-SCHRODER. G., 1971. — Annelida. Borstenwiirmer. Polychaeta. Die Tierwelt Deutschlands, 58 : 1-594.
Imajima, M., 1992. Spionidae (Annelida, Polychaeta) from Japan VIII. The genus Scolelepis. Bull. Nam. Sci. Mus.
Tokyo. Ser.A, *18 : 1-34.
Kirkegaard. J.B., 1969. — A quantitative investigation of the central North Sea. Spolia. 29 : 8-285.
286
A. V. SIKORSKI
LIGHT. W.J., 1977. — Spionidae (Polychaeta; Annelida) from San Francisco Bay. California: a revised list with
nomenclatural changes, new records, and comments on related species from the northeastern Pacific Ocean. Proc.
Biol. Soc. Wash., 90: 66-88.
LIGHT. W.J.. 1978. — Spionidae ( Polychaeta ; Annelida). Invertebrates of the San Francisco Bay Estuary System, Pacific
Grove. California. 211 pp.
Maciolek. N.J.. 1987. — New species and records of Scolelepis (Polychaeta: Spionidae) from the east cost of North
America, with a review of the subgenera. Bull. Biol. Soc. Wash., 7 : 16-40.
MESNIL, F.. 1896. Etudes de morphologie externe chcz les Annelides. Les Spionidiens des cotes de la Manche. Bull.
Sci. France Belg.. ser.4,. 29 : 110-287.
OKUDA, S., 1937. — Spioniform polychaetcs from Japan. J. Fac. Sci. Hokkaido Univ., Ser. 6. Zool 5 : 217-254.
Sars. M.. 1851. — Beretning om en i Sommeren 1849 foretagen zoologisk Reise i Lofoten og Finmarken. Nyt Mag.
Naturv. Oslo. 6 : 121-211.
Sars. M.. 1873. Bidrag til Kundskaben om Norges Annelider. Vidensk. Selsk. Christiania, Forh. : 1-51.
SODERSTROM, A.. 1920. — Studien iiber die Poly chat en-familie Spionidae. Dissertation. Uppsala, 286 pp.
SOUTHERN, R.. 1914. — Archiannelida and Polychaeta. Roy. Irish Acad. Dublin., 31 : 1-160.
Wesenb ERG -Lund, E., 1951. Polychaeta. Zoology Iceland, 2 : 1-182.
Source : MNHN. Paris
30
A systematic problem of inter- and intra-generic
variation in nephromixia of Terebellidae
Ralph /. SMITH
Department of integrative Biology
University of California
Berkeley. California, 94720, U.S.A.
ABSTRACT
The nephromixial systems of Pista fimbriata Moore, 1923 (a typical Pista) and of two aberrant " Pista ", P. don gat a Moore,
1909 and P . pacifica Berkeley & Berkeley, 1942. are described. The latter two species do not belong in Pista, but no described
genus can accomodate them. If they are congeneric, the differences between their reproductive nephromixia exceed any intra¬
generic variation previously reported in the nephromixial system of any terebellid genus. Some taxonomic and phylogenetic
implications are discussed.
RESUME
Un probleme systematique de variability inter- et intra-generique dans la nephromixie des Terebellidae
Ees systemes nephromixiaux de Pista fimbriata Moore. 1923 (une Pista typique) et de deux "Pista" aberrantes. P. elongata
Moore, 1909 et P. pacifica Berkeley & Berkeley, 1942. sont decrits. Les deux dernieres espfcces n’appartiennent pas au genre
Pista, ni a aucun autre genre connu. Si clles sont congeneriques. les differences entre leurs nephromixies reproduc trices
surpassent toutes les variations intragencriqucs decrites parmi les genres de lerebellides. Quelques implications taxonomiques
et phylogenetiques sont discutees.
Nephromixia (Goodrich, 1895, 1945; SMITH, 1988) are complex segmental organs serving excretory and
reproductive fonctions. Their morphology show great inter-generic variations in the Terebellidae (MEYER, 1887;
Hessle, 1917; SMITH, 1989), but intra-generic variation in these organs has not previously been described. The
study reported herein is the subject of a longer <uid fully-illustrated paper in die Journal of Morphology (Smith,
1992). Most of the illustrations used in the oral presentation at diis Conference will be found in that paper and so
will not be reproduced here. Reprints will be furnished to Conference participants upon requests.
Two Californian species, Pista elongata Moore, 1909 and P. pacifica Berkeley & Berkeley, 1942, have been
found to differ markedly in nephromixia and other respects from typical Pista , type P. cristata (O.F. Muller. 1776).
Pista fimbriata Moore, 1923 are described and illustrated, and it is confirmed that typical Pista (insofar as has
Smith. R.I.. 1994. A systematic problem of inter- and intra-generic variation in nephromixia of Terebellidae. In: J.-C.
DaUVIN, L. LaUBIER & D.J. REISH (Eds), Actes de la 4eme Conference internationalc des Polychetes. Mem. Mus. natn. Hist,
nat .. 162 : 287-289. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
288
R.I. SMITH
Typical Pi si a is characterized by two, often unequal, pairs of dendritic branchiae, prominent lateral lappets, and
especially by distinctive crested, long-handled, avicular, anterior uncini. In die present study the nephromixia of
been reported) has one pair of anterior, pre-septai, non-reproductive, "excretory" nephromixia (ENMX) opening
by obscure "renal” apertures on segment III. Post-septally occur two pairs of reproductive nephromixia (RNMX)
dial open on genital papillae located dorsally, just posterior to the notopodia of segments VI and VII. These
RNMX are not united by lateral common ducts (Figs IB, E). The tubes of Pista are usually reported as thick -
walled and muddy, without apertural ornamentation.
Fig. 1. — A-D. "Procrustacean Bed” representation of nephromixial systems of an hypothetical archetypical lerebellid and of
Pista fimbriata Moore, P. pacijica Berkeley & Berkeley, and P. elongata Moore. The nephromixia are fitted into a
common bed for comparison. E. HESSLE’s schema of the nephromixial system of Pista.
In contrast, Pista pacifica is easily recognized in its habitat in muddy sand flats by its long, chitinous, sandy,
vertical tube with a distinctive fringed hood at the surface aperture and a button-like plaque with a cross-shaped
slit at its lower end. Pista pacifica has lappets and its anterior uncini are long-handled, but are stout and crochet¬
like, unlike those of typical Pista. It differs most markedly from typical Pista in its nephromixia (Fig. 1C). There
are two pairs of ENMX but three pairs of ciliated renal funnels. The First pair of funnels supply a pair of ENMX
opening by papillae at the tops of the second lappets (segment III). The second and third pair of funnels supply the
second ENMX, which open by papillae on the third lappets (segment IV). Post-septally, are three pairs of large
Source : MNHN. Paris
VARIATION IN TEREBELLII) NEPHROMIXIA
289
and complex RNMX, those on each side united by a lateral common duct with posterior extension and
discharging by obscure genital papillae on segments VI, VII and VIII.
I ista elongate/ occupies rock crevices and pholad bore-holes. Its tough, membranous, sand-encrusted tube
opens within a bilobed reticulated hood. It is pointed out that the morphology of such tubes is often as specifically
distinct as other morphological characteristics, as much as is a gastropod shell, and should be included in specific
descriptions. P. elongate/ has long-handled anterior crochet-like uncini indistinguishable from those of P. pacif/ca.
Likewise, it has been the same arrangement ofENMX, three pairs of ciliated funels supplying two pairs of ENMX
opening on lappets of segments Ill and IV. But it differs from P. pacif/ca in having 9-1 1 pairs of relatively simple
RNMX united on each side by a common duet (Fig, ID). The number of RNMX exceeds the number of genital
papillae, and small, vestigial, genital funnels may occur posterior to the common ducts. This suggests that die
posterior extensions of die common ducts seen in P. pacif/ca, as well as in certain odier species, may have
resulted from the losse of die more posterior RNMX in evolution.
Hessle (1917) has shown dial nephromiwia of terebellid polychaetes exhibit great inter-generic variation but
he suggested little or no intra-generic variation. The differences between P. pacif/ca and P. elongata on die’ one
hand and typical P/sla on die odier in respect to anterior uncini, tube morphology, and in ENMX and RNMX are
sufficient to justify removal of die two former species from Pista but, on present information, no described genus
can accomodate them. Further, die differences in RNMX between these species is a great as might characterize
separate genera, although on die bases of branchiae, lappets, tubes, anterior uncini, and ENMX they appear
congeneric. I he differences in RNMX represent a degree of intra-generic variation not previously reported in die
rerebel lidae. Possibly the patterns of ENMX here demonstrated are only die extremes of intra-generic variation
m which intermediate patterns may have been lost or not yet discovered. Might sub-generic status be justified1’
Paradoxically, an "intermediate" condition of die RNMX is shown by Lanice conchilega, which has four pairs of
RNMX joined by common ducts, but in tiiis species die anterior uncini are of an entirely different avicular form,
and die ENMX differ as well (Meyer, 1887). Nephromixial patterns seem to have evolved quite independently of
the form ot the uncini, and the similarity between the latter might represent convergent adaptations to life in
comparable lubes.
I he information implicit in the diverse patterns of nephromixial morphology in terebellid polychaetes may be
uselul in phylogenetic studies, and should be included whenever possible in specific descriptions within the
Terebellidae.
REFERENCES
GOODRICH. E.S., 1895. — On the coelom, genital ducts and nephridia. Q. J. micr. Sci .. 37 : 253-267.
Goodrich. E.S.. 1945. — The study of nephridia and genital ducts since 1895. Q. J. micr. Sci.. N.S., 86 : 113-392.
IlESSLE, C.. 1917. — Zur Kenntniss der terehellomorphen Polychaeten. Zool Bidrag fran Uppsala . 5 : 39-258.
Meyer. E., 1887. — Studien iiber der Korperbau der Anneliden, I-III. Mitth. Zool. Sia. Neapcl. 7 : 592-741 .
SMl'm. R.I.. 1988. Mixonephridia or nephromixia in terebellid polychaetes? A clarification. Comp. Biochem. Physiol..
91G . 265-272.
Smith. K.I.. 1989. — Observations on spawning behavior of Eupolymnia nebulosa and comparisons with Ixmice conchilega
(Annelida, Polychaeta. Terebellidae). Bull. mar. Sci.. 45 : 406-414.
SMITH, R.I.. 1992. — Three nephromixial patterns in polychaete species currently assigned to the genus Pista (Annelida
Terebellidae). J. Morph.. 213 : 365-393.
Source : MNHN. Paris
31
Morphometric variation in bifurcate notosetae
of two Euphrosine species (Polychaeta, Euphrosinidae)
Ken D. VOGT & Jerry D. KUDENOV
Department of Biological Sciences
University of Alaska Anchorage
321 1 Providence Drive
Anchorage, Alaska 99508 U.S.A.
ABSTRACT
Univariate and multivariate analysis of covariance based on four morphological factors reveal that prong lengths and ratios
of bifurcate notosetae in two Euphrosine species (Polychaeta, Euphrosinidae) vary systematically along both the body axis and
within setal fascicles in relation to body size. Body size was measured as a function of two covariates: total numbers of
segments and body weights. Principle component analysis revealed that the majority of notosetal variation in these species is
attributable to body size ; the remainder to setal position within notofascicles. Discriminant analysis correctly distinguished
between the notosetae of these species in nearly all cases. These preliminary results tend to validate the traditional use of prong
lengths and ratios to describe the bifurcate notosetae of euphrosinids.
RESUME
Variation morphometrique des soies dorsales bi fur (pices de deux cspcccs <\' Euphrosine (Polyclicte, Euphrosinidae)
Les analyses univariees et multivariees de la covariance basee sur qualre c aide teres morphologiqucs revelent que la
longueur des branches des soies fourchues el les proportions des soies notopodiales bifides des deux especes d 'Euphrosine
(Polychetes, Euphrosinidae) varient selon leur position dans 1'axe du corps et avec les fascicules des soies en relation avec la
taille du corps. La taille du corps a etc mesurce comnie une fonction de deux variables liees : le nombre total de segments et le
poids du corps. L'analyse en composantes principales montre quo la variation majeure des soies notopodiales de ces especes est
lice a la taille du corps ; les autres variations sont liees a la position dans les faisccaux dorsaux. L'analyse discriminante permet
de distinguer correctement, dans tous les cas, les soies notopodiales des especes. Ces resultats preliminaires proposent la
validation de 1’util isation traditionnelle des longueurs des branches des soies fourchues et de leur proportion pour decrire les
soies notopodiales bifides des euphrosinides.
INTRODUCTION
Although the setae of polychaetous annelids are generally recognized to be highly variable morphological
traits that vary over time and space (Fauchald, 1991 ), morphometric studies on setal variation have only recently
Vogt, K.D. & J.D. KUDENOV. 1994. - Morphometric variation in bifurcate notosetae of two Euphrosine species
(Polychaeta, Euphrosinidae) In: J.-C. Daovin. L. LaUBIER & D.J. REISH (Eds), Actes de la 4eme Conference internationale des
Polychetes. Mem. Mus. nain. Hisi. not., 162 : 291-298. Paris ISBN 2-85653-214-4.
Source : MNHN . Paris
292
K.D. VOGT & J.D. KUDENOV
begun (Gaffney, 1973; Garwood & Olive, 1981; Bhaud, 1983; Orrhage & Sundberg, 1990; Fauchald,
1991 1992). The need to incorporate such data into polychacte systeinalics is critical since: 1) simple linkages
between morphology and the distinctions between biological species probably do not exist (GRASSLE & GRASSLR
1976- LEVIN 1984; Orrhage & Sundberg, 1990) ; 2) systematically significant morphological variation exists
in species previously considered to be cosmopolitan or widely distributed (HARTLEY, 1984; Williams, 1984); and
3) setal morphology may be variously influenced by combinations of environmental tactors as has been
documented in oligochaetes (Schroeder, 1984; Chapman & Brinkhurst. 1987, but see Gaffney, 1973).
There have been no quantitative studies of setae published on the Order Amphinomida, although setal variation
has been noted (MOORE, 1905; HORST, 1912), and Gustafson (1930) illustrated the kinds of setae present in the
oenera included in his study. KUDENOV (1987) suggested that bifurcate notosetac should be studied quantitatively
fo validate their use in the systeinalics of Euphrosine. This paper reports preliminary findings on morphometric
variation of die bifurcate notosetac in two species of Euphrosine-. E. borealis Oersted, 1843 and E. bicirrata
(Moore, 1905). Work continues on morphometry of neurosetal variation and will be reported elsewhere.
FIG. 1. Prong lengths of bifurcate notosetac of Euphrosine borealis (A. B) and E. bicirrata (C. D). involving measurements
between points 1-2 for long prongs, and points 2-3 for short prongs. A, C, superior notosetae. B. D. inferior notosetae.
MATERIALS AND METHODS
In all, 15 preserved, complete specimens (four of E. bicirrata ; 11 off. borealis ) examined as part ot this study
were obtained on loan through the Deparunent of Biology, Moscow State University, and the P.P. Shirshov
Institute of Oceanology. Unfortunately, locality data have not yet been made available.
A two stage stratified sampling routine was used in which setae were collected from the top and bottom ol
notosctal fascicles of anterior (setiger 6), middle (14-18), and posterior (24-30) body regions. Setal measurements
include long prong length (LP) and short prong lengdi (SP) (Fig. 1); long to short prong ratios (LP/SP) were
calculated. Abbreviations are used as subscripts for probability values given below. All setal measurements were
made at 400 limes magnification, and repeated nonconsecutively. Body si/e was estimated using two covariates:
total numbers of setigers (S) and body weight (W). Body weights, recorded as wet weights of specimens stored in
alcohol, were measured using an analytical balance. .
Statistical analyses (Analysis of Covariance [ANCOVA] : MONTGOMERY, 1984; Multiple Analysis of
Covariance [M ANCOVA]: Manly, 1990) were carried out for natural-, square root- and logc-transformed data.
Confirmation of normality was prerequisite to all parametric tests used (Montgomery, 1984; Manly, 1990).
Nonparametric uni-and multivariate tests were used for borealis data that could not be normalized (Conover,
1980). Principal component analysis was calculated for both species (Manly, 1990). Discriminant analysis ot
prong lengths and ratios for both species was constrained to a nonparametric multivariate test (K-NEAREST
Source : MNHN. Paris
MORPHOMETRIC VARIATION IN EUPHROSINE BIFURCATE NOTOSETAE
293
NEIGHBOR: Hand, 1989) on prong lengths and ratios vs. body size and fascicle position for both species since E.
borealis data could not be normalized. K values (1-5) were used initially for both species ; those for which the
fewest misidcntifications occurred were selected for further analysis. Blocks for anterior, middle and posterior
body regions for all statistical tests were taken to represent total numbers of segments.
Statistical software packages used for all ANCOVA and MANCOVA analyses are found in Statistical
Packages for the Social Sciences, version 4.0 (SPSS Inc., 1990) and Statistical Analyses Software, version 6.06
(SAS INSTITUTE Inc., 1990). Probability limits were set at P = 0.05.
RESULTS
In all, 953 notosetae were measured (432 from four E. bicirrata', 521 from 11 E. borealis). In E. bicirraia,
body segment numbers and body weights ranged from 24-31 and from 0.117-0.129 g, respectively; in E. borealis
they ranged from 23-41 and 0.06-2.7 g. Results of statistical analyses for both species reveals the presence of
continuous and verifiable variation both along the body axis and within notopodial fascicles.
The notosetae of Euphrosine bicirrata
Within-cell MANCOVA treatment of prong lengths vs body size and setal position within fascicles reveals the
lengths of both prongs simultaneously increase from the top to bottom of a fascicle (MANCOVA: Fig. 2a-b,
Plp = psp = 0.002, Wilkes-lambda = 0.08) and along the length of the worm as body size increases (MANCOVA:
Fig. 2a-b. Ps = Pw = 0.002, Wilkes-lambda = 0.08). Although long prongs appear to increase in length, they were
found to vary independently of body size when tested alone (MANCOVA: Fig. 2c, P§ =.062, Pw = 0.072). In
contrast, short prongs directly influence this multivariate association when examined separately. Short prongs
increase in length towards posterior segments as body size increases (MANCOVA: Fig. 2d, Ps = Pw = 002,
Wilkes-lambda = 0.08).
Partial cell MANCOVA treatment of prong lengths vs fascicle position (holding the influence of body size
constant), reveals that both prongs increase in length from the top to bottom of fascicles (MANCOVA:
Pj p = Psp=.002, Wilkes-lambda= 0.07),
Loge-transformed ratios of prong lengths decrease from top to bottom of notofascicles (ANCOVA: P, p/sp =
0.025) and along the length of the worm (ANCOVA: PLP/sp = 0.005) as body-size increases. Prong lengths are
positively correlated to total body segment numbers (r = +.512, N = 432), and negatively correlated to total body
weight (r= -0.531, N = 432).
Principle component analysis disclosed that 91.3 % of total observed variation in this study is explained by
body size while the remaining 8.7 % is attributable to setal position within notofascicles.
The notosetae of Euphrosine borealis
In contrast to data obtained for E. bicirrata , only the data for prong ratios could be normalized, and analyzed
by ANCOVA; univariate analyses of prong lengths were otherwise tested nonparametrically.
Lengths of both long and short prongs, each tested separately, have statistically constant lengths and vary
independently of body size (Kruskae- Wallis: Fig. 3a, PLP = 0.6458 ; Fig. 3b, Psp = 0.4059). However, both
long and short prongs, tested separately, increase in length from top to bottom of notofascicles (KRUSKAL-
Wallis: Fig. 4a-b, PLP < 0.0001, Psp = < 0.0001).
Loge-transformed ratios of prong lengths, normalized through a logc transformation, decrease from top to
bottom of notofascicles (ANCOVA: PlP/sP = < 0.0001), and along die length of die worm widi increasing
numbers of body segments (ANCOVA: Plp/sp < 0.0001), and are independent of total body weight (ANCOVA:
Plp/sp = 0.133). Loge-transformed ratios of prong lengths are also positively correlated to total body segment
numbers (r = +0.995, N = 521) and independent of total body weight (r = 0, N = 521).
Principal component analysis revealed diat 72.0 % of die total observed variation in this study is accountable
by body size while the balance of 28.0 % is associated with setal positions within notofascicles.
Discriminant analysis of Euphrosine bicirrata and E. borealis
The fewest number of notosetal misidcntifications for both species occurred when K = 3. A total of four
notosetae (two from each species) were incorrectly assigned to the other species. None had any body axis or
fascicle location in common, and no pattern to these errors could be discerned. In all, 99.6 % (949/953) of all
294
K.D. VOGT & J.D. KUDENOV
notoselae were correctly identified on tlic basis prong lengths of notosetae from known positions within fascicles
and segments.
C
Z
o
E T
o
D-
U3
-3
D
o B
tn
<
U-
0.0 0.1 0.2 0.3 0.4
LONG PRONG - LENGTH (mm)
D
z
o
E T
CO
o
Cl¬
uj
_J
u
<
u.
0.00 .01 .02 .03 .04 .05
SHORT PRONG - LENGTH (mm)
- 1 - 1 - r
C— •— O
- c— — •— o
- I - 1 - 1 - 1 -
FIG. 2. — Euphrosine bicirrata Moore: A. mean length of long prongs from top and bottom of notofasciclcs along the body
axis. B. mean length of short prongs from top and bottom of notoFascieles along the body axis. C, mean length of long
prongs in relation to position along the body axis (influence of body size removed). D. mean length of short prongs in
relation to position along the body axis (influence of body size removed). A. M. P denote anterior, middle and posterior
body regions; solid dots represent means; open circles ± 1 standard deviation.
Similar results were obtained for E. borealis prong ratios when K = 1 through 4, in that 99.6 % (949/953) of
die notosetae in each of four tests were correcdy identified; till E. bicirrata notosetae were correctly identified.
DISCUSSION
Bifurcate notosetae of botii Euphrosine bicirrata and E. borealis vary systematically within notofasciclcs along
the lengtii of die body in worms of increasing body size. Few other studies are available that report similar patterns
of setae variation along the body of polychaetes. The only work about which we are aware is that of Fauchald
(1992) which found diat total lengdi of setae vary systematically along the body of preserved Palola species
whereby: 1) all setae are initially short in anteriormost segments, becoming longest in the anterior third, and
decreasing gradually in length to die end of the body; 2) setae change from top to bottom of fascicles, and tiiat
these patterns vary systematically between species; and that the 3) blades of all compound seuie also vary along
die body, being longest in middle body segments. Similar, but not necessarily identical, relationships also exist in
the bifurcate notosetae of die two Euphrosine species examined in die present study. In E. bicirrata, prong lengths
Source MNHN. Paris
MORPHOMETRIC VARIATION IN EUPHROSINE BIFURCATE NOTOSETAE
295
simultaneously increase in length from top to bottom of nolofascicles in segments along the length of the worm as
body size increases. This relationship appears to be controlled more by the length of the short than long prong for
0.1
AMP
BODY POSITION
B
0.04
s
s,
33
E-
g 0.03
-J
l 0.02 -
0.00
0.01
AMP
BODY POSITION
^ c
s 06
D
X
H
O
Z
W
>-3
o
z
o
X
x
o
o
«— 3
0.5 -
0.4
0.3
0.2
BODY POSITION
AMP
BODY POSITION
Fig. 3. — Euphrosinc borealis Oersted: A, mean length of long prongs in relation to position along the body axis. B. mean
length of short prongs in relation to position along the body axis. C, mean length of long prongs from top of notofascicles
along the body axis. D. mean length of short prongs from bottom of notofascicles along the body axis. A. M. P denote
anterior, middle and posterior body regions: T, B denote top and bottom region of notofascicles; solid dots represent mean
values; open circles ± 1 standard deviation.
Source : MNHN, Paris
296
K.D. VOGT & J.D. KUDENOV
the parameters tested. Variability in die latter may be directly related to some other morphological factor not
included in diis study. Changes detected in prong lengths within notofascicles arc not influenced by size. Prong
lengths in E. borealis vary independently of body size, and increase from top to bottom of notofascicles.
Little if any biological significance should be attached to these findings when results for E. bicirrata and E.
borealis are compared since die different stadsdcal analyses employed make vastly disparate assumptions about
the independent-dependent nature of variables examined (WlLLlG el ai , 1986; Orrhage & Sundberg, 1990). For
instance, prong lengths are assumed to be dependent variables in euphrosinids since a given seta is generally
produced by a single chaetoblast cell in polychaetes (O’CLAIR & Clone*, 1974; SCHROEDER, 1984; SPECHT,
1988; Kryvi & SORVIG, 1990). Multivariate tests used for E. bicirrata recognize the concommitent nature of
prong lengths and die influence of body size; univariate tests for E. borealis assume all factors to be independent
(WILLIC. et al., 1986). Moreover, seasonal and ecological variation between samples can not presently be
explained until collection data become available.
Fauchald (1991) stated diat variable morphological traits in eunicids may be: 1) dependent on body size; 2)
independent of bodi body size and other morphological traits; or 3) independent of body size but strongly related
to one another. The first two of these relationships apply to results described above from univariate analyses of
notosetal prong lengdis of E. borealis, in which size was assumed to be independent. It may be informative to
reconfirm Fauchald's results using multivariate techniques.
Natural log-transformed ratios of prong lengths decrease from top to bottom positions of notofascicles and in
different segments along the length of die body in both euphrosinids. These ratios decrease along die body axis in
both species, but relate differently to one of the two covariales used to estimate body size. For example, ratios
change in E. bicirrata in relation to increasing body size, and are positively correlated to total segment number,
and inversely to body weight: those for E. borealis change only in relation and are directly correlated to increasing
numbers of segments, being independent of body weight. These correlations probably mirror actual relationships,
but caution is again urged against attaching undue significance to these findings for two reasons: 1) body weights
were estimated from preserved specimens long stored in alcohol; and 2) sample size, particular for E. bicirrata ,
may have biased the results. Although one seldom has the luxury of examining live or recently preserved
euphrosinids, additional specimens of E. bicirrata will be examined to address the latter point.
Body size underlies the majority of total notosetal variation in both species, and position of setae within
notofascicles accounts for the remaining balance of the two factors studied.
Patterns of both notosetal prong lengths and ratios along the length of the body and within fascicles are highly
diagnostic for both E. bicirrata and E. borealis, provided the locations from which setae are sampled are known
and compared using discriminant analysis. Although the process of accumulating these data is laborious, this
technique should be used more widely in polychaete systematics.
The use of ratios in biological studies have arithmetic properties which tend to have Cauchy distributions
(ROSS, 1988), lack means and variances, and can provide spurious results that are untestable (Atchley et al. ,
1976). Both Atchley et al. (1976) and Atchley & Anderson (1978) present statistical arguments opposing the
use of ratios in biological studies. Prong ratios describing bifurcate notosetae in euphrosinids seem to reflect
expected trends, provided one knows the locations from which setae are derived! However, identifications of
Euphrosine species should not be based on this character alone, particularly if the body locations are unknown,
and a database does not exist.
Setal trends reported above confirm that prong lengths and ratios of bifurcate notosetae in E. bicirrata and
E. borealis vary systematically along the body. Prong lengths and ratios of bifurcate notosetae arc here confirmed
to be statistically valid characters that have been used traditionally in euphrosinid systematics (KUDENOV, 1987),
provided setal locations both within fascicles and along the body axis are known. Euphrosinids should not be
identified solely on the basis of bifurcate notosetal prong ratios. It is suggested that future descriptions of
euphrosinid taxa include prong lengths and ratios for bifurcate notosetae from the top and bottom of notosetal
fascicles from anterior, middle and posterior body segments. However, prior assumptions regarding the systematic
importance of prong lengths and ratios should probably not be extrapolated to other Euphrosine species until the
results of this study are corroborated in oilier congeners.
ACKNOWLEDGMENTS
We are indebted to K. FAUCHALD, Smithsonian Institution, for assistance provided, in generously summarizing
and sharing the results of his studies on Eunices, and for commenting on this manuscript. Specimens were kindly
made available by I. Jirkov, Moscow State University, and R. Y. Levenstein, P.P. Shirshov Institute of
Source :
MORPHOMETRIC VARIATION IN EUPHROSINE BIFURCATE NOTOSETAE
297
Oceanology, Moscow. Statistical advice was provided by K. Thirugnanasambanthan and J. Egenolf, Dept, of
Mathematics, graphics software assistance given by J. Kennish, Dept, of Chemistry, and R. Kullberg, Dept, of
Biology, University of Alaska Anchorage; assistance with our French abstract was generously provided by D.
Lachinski. We also thank K. Fitzhugh, Los Angeles County Museum of Natural History, and an anonymous
reviewer for helpful comments that improved this paper.
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Source : MNHN. Paris
32
Pseudonotomastus southerni gen. nov. sp. nov.
a new capitellid from the Celtic Sea
Lynda M. WARREN* & Miles PARKER **
* Centre for Marine Law and Policy. Cardiff Law School. University of Wales
Cardiff. P O Box 427. Cardiff CF1 1XD. UK
** Department of the Marine. Fisheries Research Centre
Abbotstown. Castlenook. Co. Dublin, Ireland
Present address: Ministry of Agriculture, Fisheries and Food
17 Smith Square. London SW IP 3JR, UK
ABSTRACT
A new genus and species of Capitellidae has been found in the Celtic Sea off the south coast of Ireland. The genus
differs from other genera in having 1 1 thoracic segments, the first of which is achactous. the second has capillary chactae
in the notopodia only and the remaining nine have capillary chactae only. There are no capillary chaetae in the anterior
abdominal segments. The type species. P. southerni, often shows a distinctive colour pattern.
RESUME
Pseudonotomastus southerni gen. nov. sp. nov., un nouveau Capitellide en mer Celtique
Un nouveau genie de Capitellidae a ete trouve en mer Celtique pres de la cote sud de 1’Irlande. Le genic differ e des autres
genres de la famille par la presence de 1 1 segments thoraciqucs. dont le premier est achete, le deuxieme n’a des soics
capillaircs que dans les notopodes. ct les neuf restant nc possedent que des soies capillaircs. II n'y a pas de soics
capillaires dans les segments anterieurs abdominaux. L'espece type, P. southerni, montre souvent une coloration
distincte.
INTRODUCTION
Specimens of the capitellid described below were collected between 1974 mid 1982 in the course of baseline mid
monitoring surveys off the coast of Cork, Ireland, in the Celtic Sea. They were taken from the vicinity of a
disposal site for an industrial organic waste from a fermentation plant. Initially it was thought that the worm
could be assigned to the genus Notomastus , which also occurs in the area, but, despite strong similarities in gross
W arren. L.M. & M. Parker, 1994. — Pseudonotomastus southerni gen. nov. sp. nov. a new capitellid from the
Celtic Sea. In: J.-C. DaUVIN, L. LaUBIER & D.J. REISH (Eds), Acles dc la 4eme Conference internationalc des
Polychetes. Mem. Mus. natn. Hist, nat., 162 : 299-306. Paris ISBN 2-85653-214-4.
Source :
300
L.M. WARREN & M. PARKER
morphology, the newly described capitcllid can be readily distinguished by its thoracic chaetal formula. The
unusual colouration displayed by some specimens (alternating brown and orange bands) is a more obvious, if less
reliable, distinction and it was this that first drew our attention to the animal. It is by no means certain, however,
that this colour pattern is a natural characteristic of the species. Capitellids usually lose colour in alcohol and
appear uniformly pale cream or even colourless aldiough occasionally red pigment spots may persist as, lor
example, in Capitella “punctate” described by Hartman (1961) (see WARREN, 1976). The distribution of the
coloured bands in this species was reasonably consistent from specimen to specimen but we cannot be certain that
it is a natural characteristic. It is possible that the industrial organic waste hits resulted in some sort of chemical
reaction, perhaps involving gland cells in die epidermis, that has caused a change in colouration. On the other
hand, methyl green staining did not reveal any comparable patterns of gland cells either in banded or unhanded
^Specimens were collected by 0.1m- grabs during a scries of surveys extending from 1974 to 1982 (unpublished
reports held by the Fisheries Research Centre, Dublin). Samples were fixed in die field using 4 % formalin and
later sorted and transferred to 70 % alcohol. Specimens for examination under scanning electron microscopy
(SEM) were air dried before coating widi gold. Alcohol preserved worms were stained in a I % soluuon ol methyl
green in 70 % alcohol following Banse (1970).
Pseudonotomastus n. gen.
Type species. — Pseudonotomastus southern n. sp.
Diagnosis. — Thorax with 11 segments; peristomium and first segment achaetous; first chactiger with
capillary chaetae in notopodia only; following 9 chaetigers with capillary chaetae only in both rami; abrupt
transition between thorax and abdomen.
ETYMOLOGY. — The generic name derives from the superficial resemblance to Notoniastus Sars, 1850.
Pseudonotomastus s out he mi n. sp.
Material examined. Holotype, incomplete 48 min long and 26 segments (BM(NH).ZB. 1982.89). and 33
paratypes [BM(NH).ZB. 1982.90-122] in 18 samples, all incomplete and including several abdominal fragments. Three
paratypes were prepared for SEM. These specimens have been deposited in the British Museum (Natural History) as part of
a collection of Irish polychaetes by the second author in 1983.
Type locality. — Celtic Sea, off Cork, Ireland. The holotype was collected at 8°20' W, 51°30' N; die
remaining specimens in an area between 7°50' to 8°26' W, and 51°27' to 51°42' N.
Etymology. — Named after Rowland SOUTHERN (1882-1935), sometime naturalist with the Fisheries
Branch of the Department of Agriculture and Technical Instruction, the original antecedent of today's Fisheries
Research Centre of die Irish Department of the Marine (GREENE, 1936). Southern wrote many papers on the
annelids of Ireland, including one on die annelids of Dublin Bay (SOUTHERN, 1910) and the archiannelid and
polychaete section of die Clare Ireland Survey (SOUTHERN, 1914). These were among the first, and remain among
the most important, systemadc analyses of the Irish polychaetes.
MORPHOLOGY. — The species has a robust appearance. No complete specimen has been recorded but it is
estimated from die size and shape of die material available that the total length might be more than 150 mm. Ihe
body is divided into a muscular thorax with no clear parapodial ridges followed by a slightly thinner, tapering
abdomen in which there are distinct parapodial ridges (Fig. lc). The length of the diorax is about 8 to 10 mm and
the width about 1.2 mm. There are distinct grooves running along die length of die abdomen in a dorso-lateral
position in the space between the notopodia and neuropodia and less clear lateral and ventral grooves (Fig. la).
The prostomium is triangular in outline with a concave surface ventrally. It is surmounted by a prominent
palpode (Fig. Id). In some specimens die peristomium is drawn forward over the prostomium like a hood so diat
only die palpode is visible (Fig. lc). Large nuchal organs were apparent in one specimen but were odierwise
indistinct. Eyes were not detected.
Source : MNHN. Paris
A NEW GENUS AND SPECIES OF CAPITELIJD FROM THE CELTIC SEA
301
The peristomium is a distinct ring about as wide as the following segments and considerably more prominent
than the prostomium. There is a large eversible proboscis which is heavily papillated (Fig. Id) although in some
specimens the papillae are not easily visible because of proboscis has become flaccid in preservation.
Fig. 1. — Pseudonotomasius southern! n. sp. a, anterior abdominal segments, dorsal view (a, notopodium. b,
neuropodium), b, anterior abdominal segments, ventral view (arrow indicates boundary between thorax and abdomen,
a - neuropodium), c, thorax and anterior abdomen (arrow indicates boundary between thorax and abdomen), d.
prostomium and everted proboscis (SEM) (a, prostomium. b, palpode. c, proboscis, scale bar = 100 Jim), e, thorax,
showing reticulation and capillary chaetae (SEM) (scale bar = 100 pm), f. abdominal segments (SEM) (a - notopodia,
scale bar = 1 mm), g. abdominal neuropodial hooks (SEM) (scale bar = 10 pm).
The thorax consists of 1 1 segments and can be divided into two regions separated by a transitional zone.
Segments 1-4 arc wide with few constrictions either between segments or on them so that the overall impression
302
L.M. WARREN & M. PARKER
is of a smooth rounded outline. The surface is, however, heavily reticulated (Fig. le). Segments 7-11 are slightly
narrower. There are usually deep constrictions between segments and each segment is divided into two equal halves
by a deep annulus. The outline is thus somewhat angular and truncated. The surface is smooth with only slight
reticulations in some specimens. Segments 5 and 6 are transitional, die degree of reticulation and constriction
varying from one specimen to another. There are no parapodial lobes or ridges on any thoracic segments.
The division between thorax and abdomen is very distinct (Figs lb-c). Abdominal segments are about one and a
half limes as long as thoracic segments in die anterior region and become progressively longer furdier back. The
parapodia are present as prominent ridges in die case of the neuropodia and a fleshy pad in the case of the notopodia
(Figs la.b,f). The neuropodia almost meet mid-veil tr ally and extend around die sides of the worm terminating in a
fleshy cirrus, which may have a branchial function, on the dorsal surface (Fig. 2). The notopodial pads coalesce so
that in most specimens a single pad is visible situated mid-dorsally between die neuropodia (Figs la. If, 2). The
lateral margins of die notopodia are drawn out into small cirri. In one specimen pores, presumably nephridial, are
prominent immediately posterior to these cirri in all abdominal segments present (i.e. fifteen). We do not know
why these pores are not obvious in other specimens but suggest diat the differences may reflect sexual condition.
Several of the specimens show an unusual pattern of colour banding (Figs la-b). The basic colour in alcohol is
pale creamy yellow. The pattern is most obvious on die abdomen where there are brown/orange bands around the
neuropodial ridges sometimes extending into the immediate vicinity of the chaetae and always extending for a
small way eidier side of the neuropodium. Dorsally the band usually stops at die neuropodial cirri but diere is
occasional light staining on the notopodial pad. In die thorax the pattern is much more variable but is usually
darker on segments 7-1 1 and is often absent from the peristomium. The prostomium is never coloured. On the
diorax die colour only occurs on the Hat surfaces, i.e. the lops of the reticulations and the main body of die hind
thorax. There is no colouration in the cracks and deep annuli. Under high power light microscopy the colouration
appears as dark orange irregularly shaped and sized granules in the epidermis. It must be noted that diis colour
pattern is not present in all animals. Its presence could not be correlated with size or sexual condition. It is
possible that the pattern is an artifact caused by differential staining by something in die sediment. Staining the
worms with methyl green produced no obvious staining pattern. Colour was taken up evenly by die worms but
was lost most rapidly from the prostomium and everted proboscis.
There are 10 thoracic chaetigers, all with capillary chaetae only. These are arranged in four bundles with die
neurochaetae situated ventro-laterally and the notochaetae much closer together mid-dorsally. The first segment after
die peristomium is achaetous. T his is followed by a segment with notochaetae only. The remaining 9 segments
have both noto- and neurochaetae thus giving the dioracic chaetal formula of 1 -, 2C, 3-1 1C. The number and size
of the capillaries increases posteriorly. On segments 2 and 3 they can be difficult to see and there are usually only
4 or 5 per bundle. By segment 11 there may be over 20 per bundle (Fig. le). In most cases the bundles on
segments 7-1 1 are prominent whereas the anterior ones are less readily detected. The chaetae have a delicate, feather-
like appearance under light microscopy and are only slightly tapered with no wings. This structure is confirmed
under SEM.
Hooded hooks are the only type of chaetae found on the abdomen but, as no complete specimens have been
examined, it is possible that other types may occur. The notopodial hooks are borne in bundles of between 30 and
36 in the first few abdominal segments, decreasing to about 25 hooks by abdominal segment 10. On the
abdominal neuropodia hooded hooks are borne in a single row extending from the ventral surface around onto the
dorsal surface of the worm and number in excess of 40 (Fig. lg). There was little individual variation in chaetal
numbers.
Both notopodial and neuropodial abdominal chaetae are small short-handled hooded hooks protruding only a
short way from the body of the worm. The hoods are prominent and light filling, extending from about half way
up the shaft and enveloping the main fang of the hook so that only the tip is visible. The main fang is long and
pointed (Fig. lg) and is surmounted by numerous equally-sized minute teeth that give the impression of a ridge.
None of the specimens is complete. The longest specimen exceeds 1 10 mm but most are no more than 40 mm.
There are at least 26 abdominal segments.
ECOLOGY. — Little is known about the ecology of this species. The area from which these specimens were
taken lies some 20 to 30 km south of die entrance to Cork Harbour, in 70-90 m depth of water. The area is
characterised by mixed poorly sorted sediments, slightly coarser at shallower sites closer to shore and muddier
offshore. Faunal density is generally low, of an “Amp/iiura filiformis” type assemblage (THORSON, 1957), with
dominant polychaete species including Lumbrineris gracilis, Spioplumes kroyeri <uid Owenia fusifonnis.
Source :
A NEW GENUS AND SPECIES OF CAPITF.LLID FROM TI IE CEI ;nc SEA
303
The centre of the collection area has been used since 1975 for the disposal of organic waste from a fermentation
plant in Cork, but there were no obvious signs of organic enrichment in die sediment, or site-related perturbations
in the faunal distribution. The samples collected in 1974 in any case pre-date the disposal operation.
Fig. 2.
Dorsal view of last thoracic and first two abdominal segments. Width of First abdominal segment is 1.5 mm.
There are no obvious differences to distinguish sex. One abdominal fragment, presumed to belong to this
species, contains small, rounded eggs.
DISCUSSION
The diagnosis of new genera, and even species, of capilcllids is often not completely satisfactory because there
are few suitable morphological characteristics and too few specimens to determine variations within a species.
We believe that die most reliable generic character is die number of dioracic chaetigers especially where, as in
diis case, the distinction between diorax and abdomen is clear. It should be noted, however, dial diere has been
considerable confusion as to die number of achaetous segments at the front end of a capilellid (sec Warren,
1991). Sometimes die peristomium is regarded as prc-segmental; in other cases it is counted as an achaetous
segment. On some occasions it has been referred to in bodi ways within a single paper. Often, also, figures
illustraung species characteristics do not accord with the written description (see, for example, Kirkegaard, 1983
in which the description of Paraeapitella refers to die peristomium as an achaetous segment but the drawing
appears to indicate a peristomium and an achaetous first segment).
The number of thoracic chaetigers alone will not suffice to disdnguish all genera and it is necessary to resort to
characteristics of the chactae and their distribution. This must be done with caution, however, as chaetal
distributions, especially in die posterior thorax, change widi age.
The overall body shape and the relative prominence of the prostomium and, if present, the palpode are known
to be affected by fixation so diat diese characteristics are not reliable for diagnosis. It is worth noting, however,
that the blunt-endcd appearance in some specimens of Pseudonoiornastus, caused by the peristomium being drawn
forward like a hood, is reminiscent oi Notomastus and unlike die appearance of odier capitellids such as Capitella
where the fusion of die peristomium prevents it from being drawn forward.
References to long- or short- handled hooded hooks occur in most descripuons of capilellid species. We describe
those of Pseudonoiornastus as being short-handled but we concede that this is a subjective observation and further
note that the character might be affected by fixation. The detailed structure of the hook is of greater potential value
for diagnosis although not usually for identification purposes because differences are only apparent under high
magnification. The numbers of teeth above die main fang in Pseudonoiornastus are too great for easy counting and
we concluded dial precise number counts could not be obtained with any degree of accuracy. Of greater importance
304
L.M. WARREN & M. PARKER
than the numbers of the teeth may be the fact that all the teeth tire the same size unlike the case with some
capitellid species where the central tooth is larger than the rest.
Because no complete specimens have been examined we cannot be certain dial hooded hooks are the only
chaetae on the abdomen. It is not uncommon among capitellids for there to be different types of chaetae on
posterior abdominal segments.
One of the most distinctive features of some of the specimens of P. southerni is the colour banding.
Pigmentation is not unknown in capitellids and has, for example, been recorded in Capitellethus dispar Thomassin,
1970 where the last thoracic and first abdominal chaetigcrs are patterned with brown rings made up of small
pigment spots. We think, however, that the diagnostic significance of this feature will only become apparent when
further populations of Pseucionoiomastus are found and examined. The lack of any staining pattern with methyl
green, however, contrasts with results obtained from an extensive range of museum material belonging to
Notomastus which produced a staining pattern that highlighted die parapodial ridges. It is possible that tiiis feature
could be of use in sorting material of the two genera.
We conclude that the distinctive features of the genus Pseudonotomastus are that it has 1 1 thoracic segments,
with 10 thoracic chaetigers on die first of which chaetae are restricted to die notopodia. All thoracic chaetae are
simple capillary chaetae.
Five genera of capitellids widi 10 dioracic chaetigers have been described. Three of these (i.e. Mediomastus
I lartman, 1944, Parheteromastides Hartmann-Schroder, 1962 aid Neomediomastus Hartman, 1969) may be readily
distinguished from Pseudonotomastus by die presence of hooded hooks in the diorax. Neonotomastus Fauchald,
1972 and Pseudoleiocapitella Harmelin, 1964 both have an achaetous first segment followed by 10 thoracic
chaetigers with capillary chaetae. In Neonotomastus the first dioracic chaetiger has capillary chaetae in die
notopodia only whereas Pseudoleiocapitella has the first chaetiger complete. These genera may be distinguished
from Pseudonotomastus by the presence of capillary chaetae in die first two abdominal segments.
Decamastus Hartman, 1963 is most like Pseudonotomastus in its chaetal formula but lacks die first achaetous
thoracic segment. The type species, D. gracilis , has a full complement of capillary chaetae on all 10 thoracic
chaetigers but D. nudus Thomassin, 1970 is distinguished by the absence of neuropodial chaetae on the first
chaedger.
Capitellethus Chamberlin, 1919, as typified by C. dispar (Ehlers, 1907) may be distinguished from
Pseudonotomastus by die presence of 1 1 chaetigers with capillary chaetae, of which die first has only notopodial
chaetae. There is no mention of an achaetous segment and it is possible diat some confusion of segment counts
might have occurred. (This certainly happened in Fauchald (1977) which lists Capitellethus as having 10
dioracic chaetigers). Apart from the different number of thoracic chaetigers, Capitellethus differs from
Pseudonotomastus in having an indistinct boundary between die thorax and die abdomen and in having long hooks
on die abdomen.
Despite similarities between Pseudonotomastus and bodi Decamastus and Capitellethus , the new genus is most
like Notomastus Sars, 1850 and strongly resembles it in gross morphology, including the arrangement of the
parapodial ridges and the shape of the thorax. Pseudonotomastus can be disdnguished from Notomastus only by
die presence of an extra dioracic chaedger in Notomastus.
It is, perhaps, unwise to speculate on the affinities of this genus on the basis of so few data but die similarity
with Notomastus is so striking as to merit comment. The specimens of Pseudonotomastus were collected with
Notomastus later iceus Sars, somedmes in die same sample. Notomastus is a very large genus, subdivided by some
into sub-genera.
The description of this new species as typical of a new genus raises some questions concerning diagnostic
characters in capitellids. The number of thoracic chaetigers is one of the few reliable diagnostic features of
capitellids and its usefulness presumably reflects genotypic characteristics that are susceptible to change. Some
species have chaetae in bodi rami of all dioracic chaetigers; in others die first chaetiger has notopodial chaetae
only. Similarly, Decamastus nudus is placed in the same genus its D. gracilis even though it lacks chaetae in the
neuropodia of the first chaetiger. In this paper, die presence of a first chaetiger with chaetae restricted to die
notopodia is regarded as being of generic significance. We made this decision for die following reasons.
Intraspecific variadon in die distribution of chaetae on the anterior thorax is unusual. Given our knowledge of the
development of capitellids (see, for example, Wilson, 1933; RASMUSSEN, 1956) diis is not surprising. The
presence or absence of notopodia on the first chaetiger is, therefore, likely to be of significance. Until now this
feature has been used both as a specific and a generic distincuon without further explanation. In die absence of die
detailed information necessary to reach a definitive decision on this point, we diink diat it is in order to use die
feature as a generic character in order to prevent confusion. We accept diat furdier knowledge may refute our
Source : MNHN. Paris
A NEW GENUS AND SPECIES OF CAPITELLID FROM IT IE CEI -TIC SEA
305
diagnosis and, indeed, we hope that by raising this issue here we may stimulate a thorough review of this feature
in capitellids.
ACKNOWLEDGEMENTS
We are indebted to die Polychaete section of the British Museum (Natural History) and to the National
Museum of Wales for providing research facilities and to the staff at the Electron Microscope Unit of the
University of London Goldsmiths' College for technical assistance. We gratefully acknowledge the assistance of
B.A. Thomas in preparing the illustrations. M. Parker gratefully acknowledges the assistance of the Fisheries
Research Centre and access to unpublished information. We are also indebted to Ivor Rees of the University
College of North Wales who provided samples from the 1974 survey.
REFERENCES
BANSE. K.. 1970. — The small species of Euchone Malmgren (Sabellidae, Polychaeta). Proc. biol. Soc. Wash., Hi :
387-408.
CHAMBERLIN, R.V., 1919. — The annelida polychaeta. Mus. Comp. Zool. Harvard, Mem., 48 : 1-514.
EULERS, E.. 1907. — Neuseelandischen Anneliden II. Abh. K. Ges. wiss. Gottingen , Math.-Phys. Kl. n.F..i : 1-80.
FaUCHAJLD, K.. 1972. Benthic polychaetous annelids from deep water off western Mexico and adjacent areas in the
eastern Pacific Ocean. Allan Hancock Monogr. mar. biol., 7 : 1-575.
FaUCHALD, K., 1977. The polychaete worms. Natural History Museum of Los Angeles County. Science Series. 28 : 1-
190.
GREENE. A.C.. 1936. Rowland Southern, Obituary. J. Cons. Perm. Ini. Explor. Mer.. 11 : 3-6.
IlARMELIN, J.G.. 1964. Elude de I’cndofaunc des mattes d'herbieres de Posidonia oceanica Delib. Rec. Trav. Stn. Mar.
Endoume. 51 : 43-105.
Hartman, O., 1944. - Polychaetous annelids from California, including the descriptions of two new genera and nine
new species. Allan Hancock Pacif Exped.. 10 . 239-310.
HARTMAN, O., 1961. Polychaetous annelids from California. Allan Hancock Pacif Exped., 25 : 1-226.
Hartman, O.. 1963. — Submarine canyons of Southern California Pt. III. Systematics: Polychaetes. Allan Hancock
Pacif Exped., 27: 1-93.
Hartman, O.. 1969. — Allas of the Sedentariate Polychaetous Annelids from California. Allan Hancock Foundation.
California. 812 pp.
HarTMANN-SCHRODER, G., 1962. — Zweiter Beitrag zur Polychaeten fauna von Peru. Kieler Meeresforsch. 18 : 109-147.
KlRKEGAARD, J.B.. 1983. Bathyal benthic polychaetes from the north east Atlantic Ocean, south west of the British
Isles. J. mar. biol. Ass. UK. 63 : 593-608.
RASMUSSEN. E.. 1956. — The reproduction and larval development of some polychaetes from the Isefjord. with some
faunistic notes. Biol. Meddr., 23: 1-84.
Sars, M., 1850. — Beretning om en i Somineren 1849 foretagen zoologisk Reise i Lofoten og Finmarken. Nyt Mag.
Naturvid,6 : 121-211.
SOUTHERN. R.. 1910. — The marine worms (Annelida) of Dublin Bay and the adjoining district. Proc. R. Irish Acad..
XXVIII. B. 6 : 215-246.
SOUTHERN, R., 1914. - Clare Island Survey. Part 47. Archiannelida and Polychaeta. Proc. R. Irish Acad., XXXI. 47 : 1 -
160.
THOMASSIN. B., 1970. — Contribution a letude dcs polychetes de la region de Tulear (S. W. de Madagascar). III. Sur les
Capitellidae des sables coralliens. Rec. Trav. Stn mar. Endoume suppl.. 10 : 71-101.
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L.M. WARREN & M. PARKER
THORSON, G.. 1957. — Bottom communities (sublittoral or shallowshelf). In: J.W. HEDGPETH (ed.). Treatise on Marine
Ecology and Palaeoecology, vol 1, Ecology. Geological Society of America : 461-534.
Warren, L.M., 1976. — A review of the genus Capitella (Polychaeta. Capitellidae). ./. ZooL, land.. 180 : 195-209.
Warren. L.M.. 1991. Problems in capitellid taxonomy. The genera Capitella, Capitomastus and Capitellides
(Polychaeta). Ophelia suppl.. 5 : 275-282.
Wilson. D.P.. 1933. The larval stages of Notomastus latericeus Sars. J. mar. biol. Ass. UK. 18 : 511-518.
Source : MNHN. Paris
33
A new species of Chaetozone
(Polychaeta, Cirratulidae) from Europe,
with a re-description of Caulleriella
zetlandica (McIntosh)
Annette WOODHAM* & Susan CHAMBERS **
* Environment and Resource Technology Ltd
Old St. James Church. Port Edgar. South Queensferry. EH30 9SQ. U.K.
** National Museums of Scotland
Chambers Street, Edinburgh. EH1 1JF, U.K.
ABSTRACT
Chaetozone setosa Malmgren, 1867 is common in soft sediments from the intertidal zone to the deep sea and is
recorded as having a cosmopolitan distribution. It has been apparent for some time that more species of Chaetozone
may be present than are currently recognised. During benthic monitoring in the English Channel, a distinct species of
Chaetozone . C. gibber sp. nov. was recognised. The new species is described in detail and distinguished from C. setosa.
As Caulleriella zetlandica (McIntosh, 1911) is similar in overall appearance and lacks a full description, this species is
re-described from material obtained near the type locality. Although the spines of both species are unidentate in fully
grown individuals, C. zetlandica can be distinguished from C. gibber by the lack of spines in the notopodia. The need for
re -definitions of the genera Chaetozone and Caulleriella is discussed.
RESUME
Une nouvelle espece de Chaetozone (Polychetcs, Cirratulidae) en Europe, avec une
redescription de Caulleriella zetlandica (McIntosh)
Chaetozone setosa Malmgren. 1867 est une espece commune dans les sediments meubles, depuis la zone intertidale
jusqu'aux grandes profondeurs et presente une distribution cosmopolite. Depuis quelques temps, il s’est avere qu’il
existait davantage d’especes de Chaetozone qu'on ne l'admettait habituellement. Au cours d’un suivi des peuplements
benlhiques de la Manche. une espece distincte de Chaetozone, C. gibber sp. nov. a ete reconnue. La nouvelle espece est
decrite en detail et comparee a C. setosa. Caulleriella zetlandica (McIntosh, 1911), espece d'aspect general similaire et
dont on ne possedait pas de description complete, est redecrite d’apres des specimens obtenus pres de la localite type.
Quoique les epines des deux especes soient unidentees chez les individus adulles, C. zetlandica peut etre distinguee de
C. gibber par 1’absence d'epines au notopode. Le besoin d’une redefinition des genres Chaetozone et Caulleriella est
common te.
WoODHAM, A. & S. CHAMBERS, 1994. A new species of Chaetozone (Polychaeta, Cirratulidae) from Europe, with a
re-description of Caulleriella zetlandica (McIntosh). In: J.-C. Dauvin. L. LAUBIER & D.J. REISH (Eds). Actes de la 4cmc
Conference internationale des Polychetes. Mem. Mus. natn. Hist, nat., 162 : 307-316. Paris ISBN 2-85653-214-4.
Source MNHN. Paris
308
A. WOODHAM & S. CHAMBERS
INTRODUCTION
Chaetozone setosa Malmgren, 1867 has been recorded from the intertidal zone to die deep sea, and from such
widespread areas as the Arctic (Malmgren, 1867), north Pacific (Hartman, 1961) and West Africa (Day,
1967). It is the only species of Chaetozone recorded from the eastern North Atlantic area (Southern, 1914;
Fauvel, 1927; Hartmann-SchrOder, 1971; HOWSON el at, 1987), although its apparent variability in form
has been noted (Christie, 1985; Lechapt, 1983; pers. obs.).
During benthic monitoring in the English Channel, an undescribed bi-tentaculate cirratulid was discovered. It
possesses spines with unidentate tips only and, following the definitions of Hartman (1961), is assigned to
Chaetozone. The new species is most similar in appearance to Caulleriella zetlandica (McIntosh, 191 1), a species
common around the British Isles but originally described from a posterior fragment only. This species is re¬
described using abundant material collected during surveys close to the type locality in Shetland. A syntype of
Caulleriella caputesocis (de Saint-Joseph, 1894), another species distinguished by spines with unidentate tips and
recorded from European waters, was also re-examined.
MATERIALS AND METHODS
The bulk of the specimens of Chaetozone gibber sp. nov. and Caulleriella zetlandica were collected using a
van Veen grab during benthic monitoring surveys off Folkestone, Kent, U.K. and in Sullom Voe, Shetland, U.K.
respectively. Samples were sieved through a 1.0 mm (C. gibber $p. nov.) or 0.5 mm (C. zetlandica) mesh and
the retained material fixed in an approximately 10 % formalin solution, later being transferred to a 2 %
phenoxytol solution containing Rose Bengal stain to aid sorting. Material for scanning electron microscopy
(SEM) was relaxed for two hours in magnesium chloride solution before fixation. After washing in distilled
water, it was dehydrated through an acetone series, critical point dried and gold-coated. Specimens were examined
using a Wild M7 stereomicroscope and a Cam Scan Series 4 SEM. All drawings were prepared with die aid of a
camera lucida.
Additional material from die National Museum of Wales (NMW), National Museum of Ireland (NMI), British
Museum (Natural History) (BMNH), Museum National d'Histoire Naturelle (MNIIN) and the Plymouth Marine
Laboratory (PML) was also examined.
SYSTEMATICS
Chaetozone gibber sp. nov.
Material EXAMINED. — U.K,: off Folkestone, Kent, SE England, very fine silt-medium sand, 3.5-20.5 m, numerous
specimens collected by Environment and Resource Technology Ltd (ERT) and deposited in the National Museums of
Scotland, NMSZ 1992.89; Turnaware Point, Cornwall, SW England, 4.3 m, two specimens, NMWZ 1992.046.5; Milford
Haven, S Wales. 46 specimens, NMWZ 1985.083 and .087. France: Banyuls-sur-Mcr. 40-45 m, two specimens, NMWZ
1992.03.
TYPE material. — One holotype and nine paratypes from Folkestone are deposited in the National Museums of
Scotland (Holotype NMSZ 1992.87, Paratypes NMSZ 1992.88). The holotype measures 19 mm for 115 chaetigers.
Paratype material is also deposited in the British Museum (Natural History) (BMNH 1992.427-432), the National
Museum of Wales (NMWZ 1993.009) and the Museum National d'Histoire Naturelle (MNHN 1992 U.C.355).
Description. — Length of body up to 20 mm for approximately 200 segments. Body surfaces smooth;
dorsal surface swollen anteriorly between chaetigers 7-30 approximately, giving a characteristic hump-backed
appearance (Figs lc & 3a); ventral surface flattened with a longitudinal groove; posterior region bluntly tapered,
dorso-ventrally compressed with lateral surfaces somewhat flattened giving almost rectangular shape in cross
section (Fig. le). Segments broad, short and crowded in anterior region, becoming narrower and longer
posteriorly, without intersegmental constrictions. Colour of preserved material (in alcohol) creamy white.
Prostomium conical with acutely pointed tip. Pair of subdermal eyes, round to elongate, near lateral posterior
margins; shallow nuchal groove below and behind each eye (Fig. lc).
Source :
A NEW SPECIE S OF CHAET07ONE IN 'll IE ENG I .ISI I CHANNEL
309
Fig. 1. — Chaetozone gibber sp. nov. from Folkestone: a, complete animal, holotype. b, anterior end. dorsal view. c.
anterior end. lateral view. d. posterior region, dorsal view. e. cross section of posterior segment, f. slender
capillary chaeta. g. stout awl-shaped capillary chacta from mid-body notopodium. h. spine with blunt unidentate tip
from posterior chaetiger.
Source :
310
A. WOODHAM & S. CHAMBERS
Peristomium achaelous, smooili, partially divided into 3 annuli, pair of grooved tentacular palps originating
from dorsal surface of posterior annulus, measuring approximately 1/3 of body length. First pair of branchiae
arising immediately posterior to tentacular palps, on first chaetiger (Fig. lb). Mouth ventral (Fig. Ic).
Parapodia all biramous with notochaetae and neurochaetae; parapodial lobes flattened mounds, extending
further from the body posteriorly. Pair of branchiae arising dorsal to notopodial lobes (Figs lb,c & 3b) on every
chaetiger in anterior region, occurring less regularly in mid-body region and absent posteriorly (precise occurrence
of branchiae uncertain as frequently only scars remain in preserved specimens); branchial filaments simple,
cylindrical and smooth, of variable length up to approximately 2 mm, thickest and longest in anterior region.
Notopodia and neuropodia slightly separated with chaetac arranged in single dorsal-ventral rows (Fig. le).
Chaetae directed laterally in anterior and mid-body regions and more anteriorly in posterior third of body. Chaetae
of three types; i) slender capillaries (Fig. If) in both rami of all chaetigcrs; ii) stout awl-shaped capillaries (Figs,
lg and 3d) in notopodia between approximately segments 40 and 90; iii) spines with unidentate tips (Figs, lh
and 3c) in notopodia from mid-body (segments 90-100) to end of body and in neuropodia from anterior region
(segments 30-80) to end of body; number of spines in each ramus increasing posteriorly from 1 to 4; each ramus
in posterior region of body typically with four unidentate spines and four slender capillaries alternating with each
other (Fig. le); left and right chaetal rows well-separated, spines not forming complete rings around segments.
Pygidium with small ventral lobe (Fig. Id).
Remarks. — Chaetozone gibber cm be readily recognised by its characteristic shape (a dorsal hump anteriorly
and a tapering, dorso-ventrally flattened posterior end) and by its distinct eyes.
Nine complete specimens of Chaetozone setosa Malmgren, 1867 from Spitzbergen, collected by M. Kendall
(PMI.) have been examined. The largest specimen measures 14 mm for 80 segments. The diagnostic characters of
complete rings of spines and intcrsegmental constrictions giving a concertina-like appearance to die posterior third
of the body, extremely long capillary chaetae in die middle diird of body, and absence of eyes agree well widi
Malmgren’s description and figures. A full re-descripdon of C. setosa is required in order to provide a basis for die
re-examination of eyeless Chaetozone in northern European waters; this is outside the scope of die present paper.
C. gibber is distinguished from C. setosa by die presence of eyes and the anterior dorsal hump, and by the
flattened shape of the posterior region with its lack of bodi "concertina" segments and complete rings of spines.
Eight specimens collected by J-P. LECH APT from die Ranee estuary and labelled Cirratulidae sp. A have been
examined. Although these resemble C. gibber very closely, Lechapt (pers. comm.) has found plumose chaetae in
his material and diese have not been observed by us in die C. gibber material from Folkestone and other
localities.
Chaetozone gibber is most similar in overall appearance to Caulleriella zetlandica (McIntosh, 1911): both
species possess a distinct pair of eyes and a broader anterior region widi flattened, tapering posterior end. It can be
separated from C. zetlandica by the presence of a distinct dorsal hump, and of blunt unidentate spines in bodi
rami, rather than in the neuropodium only. Caulleriella zetlandica also possesses bidentate spines in small
individuals; an examination of a wide range of sizes has failed to reveal these in C. gibber.
In European waters, Caulleriella caputesocis (de Saint-Joseph, 1894) is die only other bi-tentaculate cirratulid
reported to have eyes and to possess unidentate spines in bodi rami. As die precise identity of this species is
unclear, and the original figures uninformative, a syntype of Heterocirrus caputesocis (MNF1N A 1 8 1 ) was
examined. It is in poor condition and in diree pieces, measuring 13 mm for 73 segments in total. The eyes figured
and described by Saint-Joseph are not visible. The specimen does not closely resemble the original figures, but
unidentate spines are present in the posterior region and these do not form complete rings around the body. The
overall shape of die body and of the head clearly separates C.gibber from diis specimen, which cannot be assigned
to any known species from the UK.
Etymology. — The specific name gibber is die Latin word meaning hump-backed.
Distribution and habitat. — The species has been recorded from the soudi coasts of England and Wales
and die Mediterranean coast of France, from depdis of 3.5-43 m. It has been found in silty and sandy sediments
and in abundances of up to 245 ind. in -. The bendiic fauna at Folkestone, England, U.K. (type locality) has been
monitored annually since 1983 and is very similar to the Abra alba-Melinna palmata community described by
Ibanez & Dauvin (1988) from the Bay of Morlaix area of the western English Channel (Institute of Offshore
Engineering/ERT, unpublished reports). Chaetozone gibber sp. nov. has appeared constantly in samples collected
each year throughout this period. A species identified as C. setosa is present in die same community.
Source :
A NEW SPECIES OF CHAETOZONE \N TIIE ENGLISH CHANNEL
311
Re-description of CaullerielUi zetlandica (McIntosh, 1911)
Chaetozone zetlandica McIntosh, 1911: 161 (type locality: St. Magnus Bay, Shetland, U.K). — Southern,
1914: 1 15, pis 12 and 13, Figs 29 A-K
Heterocirrus zetlandica. — Fauvel, 1927: 99, Figs 34 i-n
Cautleriella zetlandica. — Day, 1976: 507
Material EXAMINED. — U.K.: Holotype of Chaetozone zetlandica, St. Magnus Bay, Shetland, Scotland. 100 fathoms
(~ 170 m), posterior fragment in two pieces. BMNH 1921.5.1.3232; Sullom Voe, Shetland, Scotland, very fine to
medium sand. 17-31 m, numerous specimens collected by ERT April 1991 and April 1992, identified as Cautleriella
zetlandica. NMSZ 1992.89. Ireland: Fahy Bay, Clare Island, six specimens collected by Southern and assigned by him to
Chaetozone zetlandica "stage A", NMI 77.1908.
DESCRIPTION. — The following description is based on die recently-collected material from Shetland. This
material is abundant, in good condition and includes whole specimens of a wide range of sizes. For consideration
of other material (including die holotype), see Remarks.
Lengdi of body up to 24 mm for approximately 154 segments. Body surfaces smoodi, slightly irridescent.
Dorsal surface of anterior half of body rounded, becoming flatter posteriorly; ventral surface flattened with
longitudinal groove; posterior region bluntly tapered, dorso-ventrally compressed to give an oval shape in cross
section (Fig. 2b). Segments of relatively even lengdi, without intersegmental constrictions.
Prostomium conical with long, acutely pointed tip. Pair of subdermal eyes, round to elongate, near lateral
posterior margin; shallow nuchal groove posterior to each eye (Fig. 2a).
Peristomium achaetous, smooth, partially divided into three annuli, pair of tentacular palps originating from
dorsal surface of posterior annulus (only stumps present on all specimens). First pair of branchiae originate
immediately posterior to tentacular palps, on first chaetiger. Mouth ventral (Figs 2a & 4a).
Parapodia all biramous with neurochaetae and notochaetac; parapodial lobes flattened mounds, extending
further from body posteriorly. Pair of branchiae arising dorsal to notopodial lobes (Figs 2a & 4a) and occurring on
every chaetiger in anterior region then irregularly in mid-body and posterior regions (precise occurrence of
branchiae uncertain as frequently only scars remain in preserved specimens); branchial filaments simple, smoodi,
of variable length up to approximately 4 mm.
Notopodia and neuropodia slightly separated, with chaetac arranged in single dorsal-ventral rows, directed
latero-posteriorly in anterior and mid-body regions and more anteriorly in posterior third of body. Chaetae of 5
types: i) slender capillaries (Fig. 2c) in notopodia only in all chaetigers; ii) stout awl-shaped capillaries of
medium length (Fig. 2d), occurring in both rami of all chaetigers; iii) short stout awl-shaped capillaries (Fig. 2e),
in mid-body neuropodia only; iv) spines with unidentate lips (Figs 2f & 4c) in neuropodia of posterior region; v)
spines with bidentate lips (e.g. Figs 2g & 4d) in neuropodia of juvenile or small specimens only. Spines with
bidentate tips found in individuals 4-5 mm long, although those in dorsal position of same neuropodia approach
unidentate forms (Fig. 4c). All spines in larger individuals with unidentate tips only.
Pygidium with small ventral button-like lobe.
Remarks. — Chaetozone zetlandica McIntosh, 1911 was described from a single headless fragment dredged
from St Magnus Bay, Shetland. Examination of the holotype has shown it to be in very poor condition and in
two parts, the anterior section measuring 15 mm by 1 mm for 46 chaetigers and die posterior section including
die pygidium 1 mm by less than 1 mm for 7 chaetigers. Most of the chaetae are broken, but are clearly in w'ell-
separated rows; not forming complete rings around die body in die posterior segments. Both capillary and acicular
chaetae (spines) are present but, due to die poor condition, it is difficult to interpret dorsal and ventral surfaces of
the body. Tips of all complete spines are unidentate. No bidentate tips were seen. McIntosh separated his
specimen from Chaetozone setosa Malmgren, 1867 because it had spines in the neuropodia only: he was aware
that C. setosa had rings of spines around the posterior segments because he had material, collected by
Malmgren, from Finmark (BMNII 1921.5.1.3226).
Southern (1914) described material from Clare Island, northwest Ireland, which he assigned to Chaetozone
zetlandica after examining McIntosh’s holotype. Mis collection included three forms, which he believed
represented diree different stages of development (Stages A, B and C; table and summary p. 1 18). Six specimens of
Southern’s stage A, the smallest of die forms he described, were examined in the present study. The smallest
individual is 5 mm by 0.5 mm for 43 chaetigers and the largest 6 mm by 0.5 mm for 75 chaetigers. The bidentate
312
A. WOODHAM & S. CHAMBERS
a
Fig. 2. — Caulleriella Zetland ica from Sul lorn Voe: a. anterior end, lateral view, b, cross section of posterior segment,
c, slender capillary chaela. cl, stout awl-shaped capillary chaeta, medium length, e. stout awl-shaped capillary
chaeta, short, f, spine with unidentate tip. g, spine with bidentate tip from indvidual of 5 mm length.
Source : MNHN. Paris
A NEW SPECIE S OF CHAETOZONE IN THE ENGLISI I Cl I ANNEL
313
Fig. 3. — Scanning electron micrographs of Chaetozone gibber sp. nov.: a. anterior end. dorsal view showing position
of hump. b. anterior end, dorsal view, showing arrangement of appendages (only stumps of tentacular palps
present), c, posterior end, lateral view, showing arrangement of chactae in notopodia and neuropodia, d. mid-body
segments with stout awl-shaped capillary chactae in notopodium.
Source :
314
A. WOODHAM & S. CHAMBERS
Pig. 4. Scanning electron micrographs of Caulleriella zetlcindica from Sullom Voe: a, anterior end, dorsal view,
showing arrangement of appendages (only stumps of tentacular palps present) - b - cl. posterior end, lateral view of
small specimen (5 mm long) showing: b. presence of spines on neuropodium only - c. both unidentate and bidentate
spines - d, bidentate spines from ventral side of neuropodium.
Source : MNHN. Paris
A NEW SPECIES OF CHAETOZONE IN THE ENG LIS! 1 CHANNEL
315
crochets (- spines) described and figured by Southern are clearly visible in the material examined and occur only
in the neuropodium.
In his monograph McIntosh (1915), expanding on his original description, figured one chaeta and mentioned
the material of Southern (1914), but neither figured nor described bidentale chaetae. He suggested that his
specimen obtained in July was a mature female, and that Southern's material was of a young pelagic form found
between March and August.
Numerous specimens identified as C. zetlandica from Sullom Voe, very close to the type locality, were
examined and compared widi both McIntosh's fragment and Southern’s material. The Sullom Voe material
includes specimens ranging from 4 mm for 54 chaetigers to 24 mm for 154 chaetigers. The presence of bidentatc
spines on posterior segments of small specimens is confirmed (Figs 2g & 4d), together with the absence of such
tips from larger specimens. Examination of a full size range of specimens has confirmed Southern's assumption
that the three forms described by him represented different developmental stages of the same species. All of this
material clearly belongs to die same species, which is distinguished from other members of die genus Caulleriella
by die presence of acicular spines in the neuropodium only. Following Hartman (1961) and Hartmann-
Schroder (1971), die presence of bidentate hooks in small individuals, and lack of complete rings of spines,
justify its continued placement within the genus Caulleriella , although die original diagnosis of diis genus
(CHAMBERLIN, 1919) included species with acicular chaetae in bodi neuropodia and notopodia.
DISCUSSION
Hartman'S (1961) definitions of the bi-tentaculate cirratulid genera Tharyx , Caulleriella and Chaetozone are
under review and have been partially revised by Blake (1991). As several authors have observed, all members of
diis group arc similar in appearance, having a pointed prostomium, elongate peristomium bearing a pair of
tentacular palps, and reduced parapodia. Currently these genera are separated according to the type and arrangement
of die chaetae: these include smooth ( Aphelochaeta Blake, 1991) or serrated ( Monticellina Laubier, 1961) capillary
chaetae only or. additionally, unidentatc ( Chaetozone Malmgren, 1867), knob-tipped ( Tharyx Webster & Benedict,
1887) or bidentate (Caulleriella Chamberlin, 1919) spines. Spines, when present, can occur on die neuropodium
only or on both rami, and may commence from the first chaetiger or (more commonly) further back; die
arrangement of chaetae at the posterior end frequently being of key importance in identification.
The genus Chaetozone was erected for C. setosa Malmgren, 1867 but no generic diagnosis was included. Later
workers (e.g. Fauvel. 1927: Berkeley & Berkeley, 1952; Hartmann-Schroder, 1971) have defined it as
having a complete ring of unidentatc spines on posteriormost segments; species with unidentate spines not
arranged like this were referred to Caulleriella Chamberlin, 1919. Day (1967) modified the definiuon slightly to
those having spines in a continuous dorso-ventral arc. The definition of Chaetozone by Hartman (1961),
however, includes all of the species widi unidentate (entire) spines. Christie (1985) described populations of
"C. setosa" in which the rings of spines are less than complete. The discovery of C. gibber and the apparent
variability in form of C. setosa, together widi the problems posed by species such as C. zetlandica, highlight die
need for re-definitions of the genera Chaetozone and Caulleriella.
The status of C. caputesocis needs further examination. This species was transferred to Caulleriella by
Chamberlin (1919), but die definitions of Hartman (1961) suggest that, due to the presence of unidentate
spines only, it should be referred to Chaetozone. Records of C. caputesocis from British waters need to be re¬
examined, and may be found to refer to C. gibber.
ACKNOWLEDGEMENTS
The material from Folkestone and Sullom Voe was collected and processed by staff at ERT Ltd. We arc
grateful to the National Rivers Audiority, Southern region, and to BP Petroleum Development Ltd., who
commissioned the surveys at Folkestone and Sullom Voe respectively, for permission to use material and for
supplying sediment data. We would like to thank Andrew S.Y. MACKIE (NMW) for loan of undescribed material.
Additional material was kindly loaned by J.M.C. Holmes (NMI), M. Lowe (BMNH), J.-C. Dauvin (MNHN),
J.-P. LECHAPT (MNHN, Dinard) and M. KENDALL (PML). We are very grateful to Andrew S. Y. MACKIE and
Iain M. T. Dixon for discussions and suggestions on the manuscript, and to David HEPPELL for advice on
316
A. WOOD1 1AM & S. Cl IAMBERS
nomenclature, Paul WlLTHEW for assistance with SEM, Graham Clark for printing the photographs, Dorothy
Hartley for assistance with word processing and Sue Hamilton for proof-reading.
REFERENCES
BERKELEY, E. & BERKELEY. C. 1952. — Canadian Pacific Fauna. 9. Annelida. 9b (2). Polychaeia Sedentaria. Fisheries
Research Board of Canada. The University of Toronto Press. Toronto. 139 pp.
BLAKE. J. A.. 1991. — Revision of some Genera and Species of Cirratulidae (Polychaeta) from the Western North
Atlantic. Ophelia Supply 5 : 17-30.
Christie. G.. 1985. — A comparative study of the reproductive cycles of three Northumberland populations of
Chactozone seiosa (Polychaeta: Cirratulidae). J. mar. bioi Ass. UK .. 65 : 239-254.
CHAMBERLIN. R. V., 1919. — The Annelida Polychaeta. Mem. Mus. comp. Zool. Harv., 48 : 1-514.
Day. J.. 1967. - A monograph on the Polychaeta of Southern Africa. Part 2 Sedentaria. Trustees of the British Museum
(Nat. Hist.), London : 459-878.
FaUVEL, P.. 1927. — Polychetes Sedentaires. Faune Fr. 5 : 1-494.
Hartman. O.. 1961. — Polychaetous Annelids from California. Allan Hancock Pacif Exped ., 25 : 1-226.
HARTMANN-SCHRODER, G., 1971. — Annelida. Borstenw urmer, Polychaeta. Tierwelt Deutschlands und der angrenzenden
Meercsteile 58 : 1-594.
Howson, C. M.. Hartley, J. P.. Mackie. A. S. Y. & O’Connor. B.. 1987. — Annelida. In: C.M. Howson (ed), Directory
of the British Marine Fauna and Flora. Marine Conservation Society. Herefordshire, pp. 76-123.
IBANEZ. I. & Dauvin, J.-C., 1988. Long-term changes (1977 to 1987) in a muddy fine sand Abra alba-Melinna
palmata community from the western English Channel: multivariate time-series analysis. Mar. Ecol. Prog. Ser.,
49 : 65-81.
Laubier. L.. 1961. — Monticellina heterochaeta n. g.. n. sp.. Ctenodrilide (Polychetes Sedentaires) des vases cdtieres
de Banyuls-sur-Mer. Vie Milieu . 11 : 601-604.
LECHAPT, J-P., 1983. Chactozone seiosa Malmgren, 1867 (Annelida Polychaeta Cirratulidae). Observations en Ranee
Maritime. Etude morphologique. Position systematique. Bulletin Soc. Sci. Bretagne, 55 : 25-30.
Malmgren. A. J.. 1867. — Annulata Polychaeta Spetsbergiac, Groenlandiae. Istandiae et Scandinaviae hactenus
cognita. K. Vetenskakad. Forh. Stockh ., 24 : 127-235.
McIntosh, w. C.. 1911. — Notes from the Gatty Marine Laboratory. St. Andrews. No XXXII. Ann. Mag. nat. Hist., 7 :
145-173.
McIntosh. W. C.. 1915. — A monograph of the British marine Annelids. 3 Polychaeta, Ophelidae to Ammocharidac.
Ray Society. London, 368 pp.
SAINT- JOSEPH (Baron de). A., 1894. — Les Annelides polychetes des Cotes de Dinard. 1st Part. Annls. Sci. nat., 7th
series. 3rd part., 17 : 1-395.
SOUTHERN. R., 1914. — Clare Island Survey. Part 47. Archiannelida and Polychaeta. Proc. Roy. Ir. Acad., 31 : 1-160.
Webster. H. E. & BENEDICT. J.E., 1887. — The Annelida Chaetopoda from Eastport. Maine. Rep. U.S.Commis. Fish.
1885 : 707-755.
Source : MNHN. Paris
34
Phylogeny of Alciopidae (pelagic polychaetes):
a cladistic analysis
Baoling WU & Lua HU A
Department of Marine Biology, First Institute of Oceanography of SOA
Hongdao Road 13, Qingdao 266003, P. R. China
ABSTRACT
The phylogenetic relationships of the nine genera in the family Alciopidae arc reexamined using a cladistic
analysis. Three phyllodocid genera Eulalia , Phyllodoce and Notophyllum are used as outgroups to polarize the 13
morphological characters. The results indicate that the nine genera can be divided into two groups which agrees with the
ideas of STOP-B(>witz (1948) and RICE (1987). It is proposed that two subfamilies can be recognized in the Alciopidae:
(1) Watelinae, which includes the genera Alciopina, Krohnia , Plotohelmis. Rhynchonerella and Watelio , and (2) the
Alciopinae, containing the genera Alciopa, Naiades . Torrea and Vanadis.
RESUME
Phvlogenie des Alciopidae (polychetes pelagiques): une analyse cladistique
Les relations phylogenedques de neuf genres de la famille des Alciopidae sont rcexaminees a l'aide de 1'analyse
cladistique. Trois genres de phyllodociens Eulalia , Phyllodoce et Notophyllum sont utilises comme groupes exterieurs
pour polariser les 13 caracteres morphologiques. 11 apparait que les neuf genres peuvent etre divis<$s en deux groupes, ce
qui est en accord avec les idees de Stop-Bowitz (1948) et RICE (1987). On propose que les Alciopidae soient partagecs en
2 sous-familles: (1) Watelinae, incluant les genres Alciopina. Krohnia. Plotohelmis. Rhynchonerella et Watelio. et (2)
Alciopinae. incluant les genres Alciopa. Naiades. Torrea et Vanadis.
INTRODUCTION
The pelagic family Alciopidae is composed of nine genera which spend their entire life in die water column
(Rice, 1987). Genera in this family include Alciopa , Alciopina, Krohnia , Naiades. Plotohelmis , Rhynchonerella ,
Torrea, Vanadis and Watelio . Alciopid polychaetes form a monophyletic group as indicated by the two large
telescopic eyes. This characteristic is not found in other polychaetes. Alciopids also possess five small cephalic
tentacles, an eversible proboscis with soft marginal papillae or two lateral horns, 3-5 pairs of tentacular cirri in
die direc anterior segments, uniramous parapodia and a transparent to semitransparent body.
Wu, B.L., & L. HUA, 1994. — Phylogeny of Alciopidae (pelagic polychaetes): a cladistic analysis. In:
J.-C. Dauvin, L. Laubier & D.J. REISH (Eds). Actes de la 4eme Conference internationale des Polychetes. M<hn. Mus.
natn. Hist, nat., 162 : 317-321. Paris ISBN 2-85653-214-4.
Source MNHN. Paris
318
B.L. WU & L. HUA
Two major views on the evolutionary relationships among the nine genera of Alciopidae have been proposed.
The first view, represented by HERING (1892), APSTEIN (1900) and Stop-Bowitz (1948), is that die Alciopidae
can be divided into two groups: (1) in die first group die proboscis has two long lateral horns, females with one
or two pairs of receptacula seminis, setae of only one type, eidier simple or compound. This group includes
Alciopa , Naiades, Torrea and Vanadis. (2) The second group the proboscis lacks lateral horns, females lack
receptacula seminis, and at least two kinds of setae are present. This group includes Alciopina, Plolohelmis,
Krohnia, Rhynchonerelta and Watelio.
DALES (1955) also places die nine genera into two groups based on setal type. The first group only has
simple setae and contains Alciopina and Krohnia. The second group possesses compound setae except, for
Naiades, which has only simple setae, and includes Alciopa, Naiades, Plolohelmis, Rhynchonerella, Torrea and
Vanadis. The genus Watelio is intermediate between the two groups.
Recently. Rice (1987) has utilized morphological and reproductive characters in his study of generic
relationship in die Alciopidae. His resulLs fully widi diose of Stop-Bowitz (1948). The purpose of this study is
to use cladistic methods to reevaluate die phylogenetic relationships of alciopid genera.
MATERIAL AND METHODS
Thirteen morphological characters were used in the present analysis, all of which have been used in traditional
alciopid taxonomy (Stop-Bowitz, 1948; Fauvel, 1953; Dales, 1957; If.bble, 1960; Day, 1967,
Uschakov. 1972; WU, 1978; Rice, 1987). The character states of die alciopid genera and of die outgroups are
listed in Tables 1 and 2. All character states are consistent among a genus except for die proboscis of Vanadis
longissima which has small marginal papillae but no lateral horns. The odier 12 species of Vanadis have lateral
horns, and we treat die proboscis of all Vanadis as having lateral horns.
Prostomium and Eyes (I-1I): Alciopidae are characterized by two large eyes with red lenses which may be
directed anteriorly, laterally, upward or downward. This character is chosen to distinguish the nine alciopid taxa
from the outgroup. The prostomium of some genera extends in front of die eyes, but in others the eyes project
forward, with the small prostomium between diem.
Proboscis (III-V): The eversible proboscis of Alciopidae is eidier long or relatively short, some with soft
marginal papillae or two lateral horns which arc provided with mucus secreting cells (Dales, 1955).
Tentacular cirri (VI): There are 3-5 pairs of tentacular cirri in the first diree segments, the formula is
(USCHAKOV, 1972): 1+1/0 or 1+1/0 or 1 or N, in which 1 = tentacular cirrus, 0 = tentacular cirrus absent,
N = normal podial cirrus.
Parapodia and receptacula seminis (VII-VIII): Several anterior parapodia arc reduced in some alciopid genera but
fully developed in the others. All normal parapodia are uniramous. Mature females of some genera, such as
Vanadis, often bear 1-2 pairs of dorsal cirri (from segment 4-5) modified into receptacula seminis for reproduction.
Setae (IX-XI): Four types of setae occur in alciopids, diey are capillaries, simple aciculae, compound aciculae
and compound spinigers. Some genera have either capillaries or spinigers; odiers may possess two or three kinds
of setae.
Distal paraodial cirrus (XII): one or two cirriform terminal appendages often exist at die distal end of die
podial lobe of some alciopid genera.
Body transparency (XIII): Some genera such as Alciopa, Alciopina and Rhynchonerella have strong muscular
bodies and are semitransparent to opaque when alive. The other six genera lack such a developed muscular system
and have transparent bodies.
The alciopids clearly arose from bendiic phyllodoeids somewhat like the present day phyllodocid genus Eulalia
(Dales, 1955; Uschakov, 1972). Pleuel (1991) used cladistic analysis to divide die family Phyllodocidae into
diree subfamilies in which die genera Eulalia, Pliyllodoce and Noiophyllum occupied die central position. These
diree genera were selected as outgroups to polarize die 13 characters.
l"he BRANCH AND BOUND algorithm from die phylogenetic computer package PAUP (version 2.4.1,
David L. Swofford, Ill. State Nat. Hist. Surv., Urbana 61820) was used to find out the most parsimonious trees.
All of die muldstate characters are treated as ordered. All characters were given equal weight. The IBM computer
at die First Insdtute of Oceanography was also used in this work.
Source : MNHN, Paris
PHYLOGENY OF ALCIOPIDAE
319
RESULTS AND DISCUSSION
Thirty-three cladograms obtained, all widi a consistency index of 0.60 and a length of 25 steps. But there is
only one cladogram (Fig. 1) with the lowest E value of 0.201, So only this cladogram has been chosen to do the
analysis work. The analysis indicates:
Alciopinae Watelinae
13
Fig. 1. — Cladogram of the Alciopidae, with phyllodocid genus Eulalia as outgroup. Consistency index is 0.600, F
value is 0.201. Progression = " — ", regression = "X", Parallelism = "=" . Numbers in parentheses indicate character-
state changes in multistale characters, e.g., IV (1-2) indicates that character IV goes from state 2 to state 3.
1. The plesiomorphic character states for the common hypothetical ancestor of the nine alciopid genera are:
The prostomium project in front of the eyes; the eyes are enlarged; die sucking proboscis with soft papillae but
no lateral horns; die second ventral cirri present; the parapodia uniramous and all fully developed; both capillaries
and compound spinigers setae present; one distal parapodia cirrus present; widi transparent body. It is very clear
that diis hypodictical alciopid ancestor lived a pelagic life, but it still leaves some primitive features similar to
its ancestral benthic form.
Source :
320
B.L. WU&L. HUA
Table 1 . — Coding of morphological characters for the alciopid genera. The numbers correspond
to those in the data matrix in Table 2 and the cladogram in Fig. 1 .
Table 2. — Matrix of character states of the nine alciopid genera and their outgroup. The numbers
correspond to those in Table 1 and Fig. 1.
2. The family Alciopidae can be divided into two major groups and the division pattern agrees with Stop
Bowitz (1948) and Rice (1987) rather than by DALES (1955). The two subgroups are all monophyletic ones
specified by several characteristics. In order to express the phylogenetic relationships among alciopid genera
clearly, we suggest that two subfamilies exist within Alciopidae.
(1) Alciopinae. Contains four genera: Alciopa , Naiades , Torrea and Vanadis. Their common hypothetical
ancestor is as follows: prostomium does not extend anterior to the eyes; the eversible proboscis with lateral horns
but lacks soft papillae; second pair of ventral tentacular cirri absent; females with one or two pairs of receptacula
seminis, parapodia with capillaries and compound spinigers seme, and one podial cirrus.
(2) Watelinae. Contains five genera: Alciopina , Krohnia , Plotohelmis , R/iynchonerella and Watelio. Their
common hypothetical ancestor is similar to the genus Watelio and has the following characteristics: proboscis
relatively short; no lateral horns; females lacking special receptacula seminis; parapodia with capillaries and
compound spinigers setae and one podial cirrus; body transparent.
3. Alciopidae can not be divided into subgroups based on setae type. However, in the evolution of the family
into subfamilies, this character changes greatly which gives it an important status in genus classification. Finally
it should be emphasized that the above views need testing when more information on alciopids are available,
which will make it possible to do a cladistic analysis at the species level.
Source : MNHN. Paris
FI IYLOGENY OF ALCIOPIDAE
321
ACKNOWl JUDGEMENTS
We wish to tliank Prof. Ju-Shey Ho of California State University, Long Beach, USA for providing us the
PAUP program. Special thanks are due to Mrs. Wang XUEMEI and Mr. Mu Hong-Lin for typing this paper.
This research is supported by a grant from National Natural Science Foundation of China, number 3870080.
REFERENCES
Apstein. C\, 1900. Die Alciopiden und Tomopteriden der Plankton Expedition. Ergeb. Plankt. Expect., 11 : 1-61.
Dales, R.P., 1955. — The evolution of the pelagic alciopid and phyllodocid polychactes. Proceed. Zool. Soc. London ,
125: 41 1-420.
Dales. R.P., 1957. — Pelagic polychaetes of the Pacific Ocean. Bull. Scripps Instit. Oceanogr., 7 : 95-167.
DALES. R.P. & G. PETER, 1972. — A synopsis of the pelagic polychaeta. J. nai. Hist.. 6 : 55-92.
Day. J.H., 1967. — Polychaete of Southern Africa. Part 1. Errantia. British Museum (Natural History) London, 458pp.
Fauvel. P.. 1953. — The Fauna of India. Annelida Polychaeta. Allahabad. 507pp.
Merino, E.. 1892. — Zur Kennlnis der Alciopiden von Messina. Sitzb.K. Akad. Wiss. Wien. Math. nat. Kl, 101 :
713-768.
PLEIJEL, E.. 1991. Phylogeny and classification of the Phyllodocidac (Polychaeta). Zool. Scr ., 20 : 225-261.
RICE, S. a.. 1987. — Reproductive Biology. Systematics, and evolution in the polychaete family Alciopidae. Biol. Soc.
Wash. Bull... 7: 114-127.
Stop-Bowitz, C\. 1948. — Polychaete from the Michael Sars North- Atlantic Deep-Sea Expedition 1910. Rep. scient.
Res. "Michael Sars" North-Atlantic Deep-Sea Exped., 5 : 1-91.
TEBBLE, N.. 1960. The distribution of pelagic polvchactes in the South Atlantic Ocean. Discovery Rep.. 30 : 161-
300.
Wiley, E.O.. 1981. Phylogenetics: The Theory and Practice of Phylogenetic Systematics. John Wiley and Sons,
Inc.. New York, 439 pp.
USCHAKOV, P.V.. 1972. Polychaetes, Vol. I . Fauna of USSR. Akademia Nauk, Zoological Institute. Series N°102.
259 pp.
Wu, B.L. & SllN. R.. 1978. Preliminary studies on geographical distribution and evolution of pelagic polychaetes
from South China Sea Islands. Oceanol. Lininol. Sinica. 9 : 215-223.
Source : MNHN. Paris
35
Preliminary observations on a dense population
of Phyllochaetopterus socialis Claparede
at the sulphurous water boundary in a
Mediterranean submarine cave
Marco ABBIATI * L. AIROLDI * Alberto CASTELLI **,
F. CINELLI * £ A.i. SOUTHWARD ***
* Dipartimcnto di Scienze dell’Ambiente e del Territorio, University di Pisa, Via Volta 6, 1-56126 Pisa, Italy
** Islituto di Scienze Antropologiche. University di Sassari, Via Margherita di Savoia 15. 1-07100 Sassari. Italy
*** Levcrhulme Unit, Marine Biological Association of the U. K.. Citadel Hill, Plymouth, PL1 2PB. U.K.
ABSTRACT
The Grotta Sulfurea (Sulphurous Cave) at Capo Palinuro, southern Tyrrhenian Sea. is characterised by the presence of
springs of sulphidc-rich water. The issuing water accumulates below the roof of the cave and supports thick mats of
Be$giatoa -type sulphur bacteria. A dense assemblage of Phyllochaetopterus socialis was found in the inner part of the
cave, where the sulphurous water extends to the bottom. Specimens showed peculiar morphological features. They
occurred immediately below the sulphurous boundary and their tubes extended into the sulphurous water. There was a
thick layer of filamentous sulphur bacteria on the tubes. The abundance of the P. socialis assemblage in the Grotta
Sulfurea appeared to be related to the presence of the sulphide springs and the growth of sulphur bacteria. Preliminary
results of stable carbon isotope analyses on P. socialis support the hypothesis that most of the worm’s carbon comes
from bacteria.
RESUME
Observations preliminaires sur des populations denses de Phyllochaetopterus socialis
Claparede a la 1 i mite des eaux sulfurcuses dans tine grottc sous-marine mediterraneenne
La grottc "Grotta Sulfurea" (Cap Palinuro. Mer Tyrrhenicnne meridionale) est caracterisee par une circulation d'eau
riche en sulfures qui s'accumule au-dessous de la voute de la grotte et perrnet le developpement d'une epaisse couche de
bacterics chimiosynthetiques. Dans la partie la plus interne, oil le fond de la grotte remonte au niveau de 1’eau sulfureuse,
un peuplement dense a Phyllochaetopterus socialis a ete d^couvert. Les individus vivent immediatement en dessous des
eaux sulfurcuses; leurs tubes sont recouverts de bacterics. On pensc que la forte densite du peuplement a P. socialis est en
relation avec la presence de la source sulfureuse. Les rSsultats preliminaires de 1'analyse des sources de carbone sur P.
socialis confirment cette hypothese.
ABBIATI, M., AIROLDI, L., Castelli. A., ClNELLI, l7. & A..I. SOUTHWARD, 1994. Preliminary observations on a
dense population of Phyllochaetopterus socialis Claparese at the sulphurous water boundary in a Mediterranean
submarine cave. In: J.-C. Dauvin, L. LAUBIER & D.J. REISH (Eds). Actes de la 4emc Conference internationale des
Polychetes. Mem. Mus. natn. Hist, nat .. 162 : 323-329. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
324
M. ABBIATI, L. AIROLDI. A. CASTELLI, F. CINELLI & A.J. SOUTHWARD
INTRODUCTION
The biological communities inhabiting hydrothermal vents at mid-ocean ridges have been studied intensively
in recent years (Desbruy^res el al., 1985; Grassle, 1985; Jannasch, 1985; Southward, 1989;
Tunnicliffe, 1991; Childress & Fisher, 1992). Hydrothermal environments that occur in shallow-water
provide an opportunity to study such complex systems at sites with easier access than mid-ocean ridges
(Tarasov el al., 1990). We carried out preliminary surveys of a marine cave system at Capo Palinuro (southern
Tyrrhenian Sea) in connection with an international co-operative study devoted to shallow-water hydrothermal
communities. This system includes several caves characterised by die presence of underwater sulphurous springs
(Abbiati el al., 1992) which support dense mats of Beggiaioa- like sulphur bacteria. During our surveys a dense
assemblage of the tube-dwelling chaetopterid polychaete Phyllochaetopterus socialis Claparede was found in the
Grotta Sulfurea where it occurred at die boundary between sulphurous water and sea- water.
Submarine caves are usually considered to be oligotrophic environments widi reduced fauna and flora and low
biomass (O'lT & Svoboda, 1976; Harmelin el al., 1985; FlCHEZ, 1990). The abundance of P. socialis in the
Grotta Sulfurea appeared unusual. It was hypothesized diat diis abundance was related to bacterial chemosynthetic
production which was supplementing the meagre input from photosynthetic sources. Investigations are in
progress to verify this hypothesis and to study the complex trophisms of the Grotta Sulfurea and similar
sulphurous caves.
The abiotic and biological features of die cave and the morphological viability and possible food sources of
P. socialis are presented in this paper.
ECOLOGY AND DISTRIBUTION OF PHYLLOCHAETOPTERUS SOCIALIS
Phyllochaetopterus socialis Claparede 1868 is a gregarious species belonging to the family Chaetopteridae. In
die original description from the Gulf of Naples ClaparCde (1868) pointed out that it occurred in high densities
and considered it to be the most abundant polychaete in die Gulf of Naples. P. socialis occurs from 10 m to more
dian 300 m in depdi on different substrates (muddy bottoms, organogenic sand and hard bottoms) where it often
forms dense mats. It has been reported from several different geographical regions: Mediterranean Sea (Fauvel,
1927; Bellan, 1964; Laubier, 1966; Reyss, 1971; Biiaud, 1974, 1977; Bhaud & Amouroux. 1975),
Atlantic Ocean (Day, 1967, 1973; Me Carty. 1974; GETTLESON el al., 1985), Pacific Ocean (Gibbs, 1971),
Indian Ocean (Day, 1967). This wide geographic and bathymetric distribution indicates a cosmopolitan species
(GETTLESON et al., 1985) although there are questions concerning the validity of some records (Bhaud, 1977).
MATERIAL AND METHODS
Study site. — The Grotta Sulfurea is located at Capo Palinuro (southern Tyrrhenian Sea) (Fig. 1). It is a
narrow sloping tunnel that opens into carboniferous rocks. It is characterised by the presence of springs of
sulphide-rich water, normally warmer than ambient sea-water and of lesser salinity. This less dense water
accumulates below the roof of die cave giving rise to a diermal oxic-anoxic interface. Preliminary data on the
speleological characteristics of the cave are reported by Muscio (1985) and Muscio & Sello (1989).
Sampling methods. — The Grotta Sulfurea cave was sampled in May 1991 and May 1992 by SCUBA
diving. A detailed survey of die cave as far as 40 m inside the entrance was carried out following die procedures of
Alvisi (1991). A permanent 40 m long transect was established by means of a tape line. Changes in the
composition and richness of the biological community along the transect were investigated by visual and
photographic surveys. Outside-inside light gradient was measured by means of an irradiance meter (Biospherical
Instruments Inc., QSI 140). Temperature and salinity vertical gradients across the sulphurous water boundary were
surveyed at point D (Fig. 1). Temperature was measured from 5.5 to 9.5 m in depth by means of an underwater
digital thermometer (Idronaut Sri). Water samples for salinity measurement were collected across the sulphurous
water boundary by means of eight 20 ml syringes spaced every 15 cm on a one meter long Plexiglas bar.
Salinity of the samples was estimated from readings of a portable sodium electrode (Iloriba Compact Salt Meter,
C-121). Dissolved sulphide in water samples from the sulphurous layer was estimated by the method of CLINE
(1969). Specimens of P. socialis were collected and fixed in buffered 4 % formalin for later analysis. Other
Source :
PHYLLOCHAETOPTERUS SOC/ALIS IN SULPI IUREOUS SUBMARINE M E DFIP, R R AN E AN CAVE
325
specimens and samples of the bacterial mats were treated with 10 % HC1, dried at 50 °C and powdered for stable
carbon isotope analysis.
COAST-LINE
UNDERWATER
ENTRANCE
ABOVE SEA-LEVEL
^ CAVE
UNDERWATER
CAVE
SEA-LEVEL
ROCKY VAULT
SULPHUROUS WATER
UNDERWATER ENTRANCE
ROCKY B0TT0A
ion
F G LAKE 2
ROCKY VAULT
AERIAL CAVITY
FIG. 1. — Location of Grotta Sulfurea cave (Tyrrhenian Sea, Italy). A, plan of the cave and location of the transect. B.
longitudinal section of the cave (plotted along points A. B. C. D, E. F. G).P. socialis assemblage (asterisks) occurs
at points E, F and G.
RESULTS
The peculiarity of the Grotta Sulfurea is the occurrence of sulphide-rich waters. The source of the sulphurous
spring outlets was not determined since they arise in the innermost part of the cave which is difficult and
dangerous to explore. The sulphurous water, which was lower in density than normal sea-water, accumulated
Source
326
M. ABBIATL L. AIROLDI, A. CASTELLI. R CINELLI & A.J. SOUTHWARD
below the vault of the cave (Fig. 1,B). The temperature and salinity measurements across the sulphurous-
water/sea-water interface indicated a sharp thermo- chemocline. Temperature and salinity values ranged from
18.7 °C and 36.5 P.S.U. to 25.9 °C and 30 P.S.U. in die sea-water and in the sulphurous water, respectively
(Fig. 2). Preliminary analyses of the sulphurous water in May 1992 indicated millimolar levels of dissolved
sulphide compared with zero below die interface.
Salinity (S‘
6 5 -
30 31 32 33 34 35 36 37 38 39 40
i- 1 - 1 - 1 - 1 - 1 - 1 - 1 - 1 - 1 - 1
Salinity
Temperature
Temperature (°C)
Fig. 2. — Temperature (°C) and salinity (P.S.U.) vertical gradients at the sulphurous boundary level.
The sulphurous water boundary was located at about 8.7 m and separated two different biological assemblages.
White bacterial mats lined the rocky surface which was in contact widi the sulphurous water. The thick
Beggiatoa- like mats thinned out near die boundary between die sulphurous water and normal sea-water. Large
numbers of a small lubificid oligochaete were found widiin die thick bacterial mats. Below die diermo-
chemocline a reduced benthic community occurred which showed a decrease of the number of species and
specimens towards the inside of the cave. At die entrance of die cave (Fig. 1, point A) light was 3.88 E 14
quanta, cm-2, sec1 and crustose coralline algae were present. At point B and C (Fig. 1) die light was reduced to
5 % and to 1%, respectively. Total darkness occurred at point D, and a reduced community was observed on die
walls of die cave (sponges and scleractinians) and bottom (ophiuroids). In die completely dark inner part of die
tunnel (Fig. 1, points E, F, G) at about 8.7 in in depdi the sulphurous water extended to the bottom. Just to the
seaward of diis level, where the tunnel deepened and die chemocline began to lift off die bottom, diere were diick
aggregates of P. social is on die bottom and sides of die cave (Fig. 1). The worm colonies were composed of
several hundred individuals and covered all die boundary belt where the sulphurous water mixed with die sea-water.
The lubes were about 10 cm long, and die worm's tentacles extended just into the sulphurous water. The tubes
were covered with a layer of filamentous bacteria which became diicker near die distal end of the lubes. Beyond
point G (Fig. 1) die walls and the bottom were completely covered by bacterial mats inhabited by oligochaetes.
One specimen of die andiozoan Alicia mirabilis was found on die bottom.
Morphological analysis of die specimens agreed with the original description of P. socialis (ClaparCde,
1868) and with the redescription by Bhaud & Amouroux (1975) and Bhaud (1977). P. socialis is characterised
by one stout specialised seta on setiger IV. The morphology of the modified seta agreed with die description by
Bhaud (1977: 210, Fig. lc-d). However, variability in the number of die stout setae was observed in die Grotta
Sulfurea specimens; a few individuals (about 5 %) had two stout setae at die setiger IV or one stout setae in bodi
die setigers IV mid V. When two setae were present in die same segment, the second seta appeared slightly diinner
and longer than the typical one. The number of setigers in the anterior region of P. socialis ranges from 10 to 18
with 13-14 usually present (Fauvel, 1927; Day, 1967; Bhaud & Amouroux, 1975). In die population the
Source : MNHN. Paris
PHYLLOCHABrron'ERUS SOCIALISM SULPHUREOUS SUBMARINE MEDITERRANEAN CAVE
327
number of setigers ranged from 13 lo 18 with 15 the most common. About 60% of the individuals had a different
number of setigers on the left and right side of the body (Table 1). The number of setigers in the posterior region
of the body ranged from 10 to 20 which agreed with previous descriptions (CLAPARfcDE, 1868; Fauvel, 1927;
Day, 1967; Bhaud & Amouroux, 1975).
Table l. — Setiger number in the anterior region of the body in Grotta Sulfurea
specimens of P. socialis (N = 129)
Carbon isotope analyses were carried out in Texas by Dr M.C. KENNICUTT. There was much depletion of the
heavy isotope in the tissues of P. socialis , and a similar depletion was shown by die bacterial mats. The
similarity of the values (DC depletions of -30.1 and -30.9, as parts per diousand compared with the usual PDB
standard) indicates close trophic coupling.
DISCUSSION
The high density of P. socialis in the inner part of die Grotta Sulfurea is unusual for a submarine cave. As
already noted, typical submarine caves show a reduedon in die biota along a gradient from outside to inside (Ott
& Svoboda, 1976; Harmelin et al, 1985; FlCHEZ, 1990, 1991). This decrease corresponds to the decrease in
photosynthetic production and of penetration of food particles from die sea. This biological gradient was noted on
substrata in contact widi die sea-water. In contrast, surfaces washed by die sulphurous water were covered by diick
mats of sulphur bacteria. The bacteria were mostly different kinds of the genus Beggiatoa and contained much
elemental sulphur which is typical for the group. The preliminary assumption is dial diere is high
chemoautotrophic production by die bacteria which use energy obtained by oxidation of sulphide.
We can presume diat the high biomass of P. socialis is related to the bacterial production which provides a
food source. The abundant biota at odier deep sea and shallow-water hydrodiermal habitats are also supported by
chemoautotrophic production either by free-living bacteria or by symbiodc bacteria, based on the mixing of vent
water containing reduced sulphur widi oxygenated sea-water (Southward, 1987; Fisher, 1990; Childress &
FISHER, 1992). In die Grotta Sulfurea die localised position of the colonies of P. socialis in die transition zone
between the sulphurous water and sea-water points to the need for a combinadon of the same extremes - reduced
sulphur <uid oxygen - for sustenance. The stable carbon isotope values indicate that die bacteria provide the main
or only food source for P. socialis : however, it is not yet clear exactly how the worms feed on the bacteria.
The Grotta Sulfurea populadon of P. socialis showed considerable morphological variation. The specialized
stout setae on the setiger IV is one of die primary taxonomic characters in P. socialis. It is considered to be
unaffected by morphological variations in relation to different geographic localities (Bhaud, 1977). The
variability in the number of stout setae and die asymmetry of die number of parapodia in the anterior region is a
328
M. ABBIATI, L. A1ROLDI. A. CASTELLI. F. CINELLI & A..I. SOUTHWARD
peculiar feature of Grotta Sulfurea specimens. The cause of such a high morphological variability is unknown.
However, enhanced levels of morphological variation have been reported for polychaetes from physically-stressed
environments (Zunarelli Vandini, 1971; CoGNETTl, 1978).
Vent ecosystems are characterised by sharp temperature and salinity gradients and high concentrations of toxic
compounds (Childress & FISHER. 1992). The occurrence of P. socialis population in this extreme environment
suggests a high adaptive capability of this species. However, many marine polychaetes with wide ecological
distribution have been demonstrated to be complexes of species (CiRASSLE & Grassle, 1976; GufeRiN &
Kerambrun, 1984; Abbiati, 1989). The same condition may be occurring in P. socialis as in these other
species.
Further studies are in progress on the ecology and population genetics of P. socialis , and on the role of
chemosynthesis in the trophic webs of the Grotta Sulfurea and other sulphurous caves at Capo Palinuro (Abbiati
etal. , 1992).
ACKNOWLEDGMENTS
We thank Dr. F.C. SOUTHWARD and Dr C.N. Bianchi for stimulating discussions and the helpful co¬
operation during llie field work; Dr M.C. KENNICUTT and Dr J. Alcala-Herrera, Geochemical and
Environmental Research Group, Texas A & M University, for the stable carbon isotope data: Dr M. Alvisi for
his revision of the Grotta Sulfurea drawing. We also thank Mr. L. Ghelia, Mr. F. Barbieri and the staff of the
diving centre Pesciolino Sub for logistic support.
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Source : MNHN, Paris
36
Contribution of the polychaetous annelids
to the diet of some brazilian fishes
A. Cecilia Z. AMARAL * Edmundo F. NONATO **
<£ Monica A.V. PETTI **
* Depto. Zoologia, IB
Universidade Estadual de Campinas
CP. 6109. 13081-970 - Campinas, SP, Brazil
** Depto. Oceanografia Biologica. TO
Universidade de Sao Paulo
CP. 9075, 05508 - Sao Paulo, SP. Brazil
ABSTRACT
Otter trawls for fish were taken between the three offshore islands. Anchieta, Vitoria and Couves off the southeast
coast of Brazil in order to determine their food habits. The stomachs of 2834 specimens of fish belonging to 77 species
were examined; 1076 were found to be empty and 595 contained polychactcs. Sixty-five species of polychactes were
identified, with the most frequent ones belonging to the genera Notoniastus. Onuphis, Anaitides , Pherusa . Ixionice,
Diopatra and Euclymene. The polychaete families were grouped according to their habitat, that is, the bottom, in
subsurface sessile, subsurface mobile, surface sessile and surface mobile. The subsurface mobiles had the highest
percentage (42.8 %) in the stomach contents with food present.
RESUMfi
Le role des annelides polychetes dans le regime alimentairc de certains poissons bresiliens
Dans le but d’estimer la part des polychetes dans le regime alimentairc des poissons benthiques et "demersaux" de la
cote Sud-Est du Bresil, une serie de prelevements a ete realisee a 1'aidc d'un chalut a panneaux du type "otter trawl" dans la
region comprise enlre les lies Anchieta. Vitdria et Couves a des profondcurs comprises entre 10 ct 50 m. Le contenu
stomacal de 2834 individus de poissons appartenant a 77 especes a ete examine : 1076 estomacs etaient vides et 595.
soit 33,8 % des autres, contenaient des polychetes. Environ 65 especes do polychetes ont et6 identifiees, les plus
frequentes appartenant. par ordre decroissant d'importance numerique, aux genres Notoniastus, Onuphis, Anaitides.
Pherusa. Laonice, Diopatra et Euclymene. Les families de Polychetes out ete groupees suivanl la position qu’elles
occupent sur le fond, soit : sub-surface sessile, sub-surface mobile, surface sessile et surface mobile. Les sub-surfaces
mobiles sont les plus frequentes (42,8 %) dans le contenu des estomacs examines.
Amaral, A.C.Z.. NONATO, E.F. & M.A.V. Petti, 1994. — Contribution of the polychaetous annelids to the diet of
some brazilian fishes. In: J.-C. Dauvin, L. LAUBIER & D.J. REISH (Eds), Actes de la 4eme Conference internationale
des Polychetes. Mini. Mus. natn. Hist, not ., 162 : 331-337. Paris ISBN 2-85653-214-4.
332
A.C.Z. AMARAL, E.F. NONATO & M.A.V. PETTI
INTRODUCTION
The role of polychaetes as food for fish has been limited to such authors as Kawakami & Amaral (1976,
1983), Amaral & Migotto (1980), Ben-Eliahu, Gqlant & Ben-Tuvia (1983), Badalamonti & Riggio
(1989) and Ben-Eliahu & Golani (1990). Their objective was to determine the position polychaetes occupy
among the prey eaten by fish.
Since earlier studies off die coast of Brazil had indicated a high incidence of polychaetes as food for fish, our
primary objective was to determine in greater detail their role as a major food element. We also attempted to
clarify those factors conditioning the apparent selectivity of certain species of fish when catching food as related to
the ecological position occupied by die polychaetes.
STUDY AREA
Lhe samples were taken from die northern coast of the State of Sao Paulo between the islands of Anchieta,
Vitoria and Couves (23°3T - 23°45' S and 44°58‘ - 45°06' W, Fig. 1) from 10 to 50 m in depth. The bottom
sediments consist of sandy mud with occasional patches of sand or shell fragments near die islands. Off Vitdria
Island in 40 and 50 m depth die sediment is muddy with sporadic presence of lime plates. Throughout the area
low temperature water (< 1 8 °C) (die so called South Atlantic Central Water - SAGA) occurs near the bottom
during die summer months (Castro Filho et al ., 1987).
FIG. 1. — Location of catches between the islands Anchieta. Vitoria and Couves.
Source : MNHN. Paris
POLYCHAETES IN TOE DIET OF SOME BRAZILIAN FISHES
333
MATERIAL AND METHODS
The samples comprised 30 trawl net hauls taken August 1978 through May 1979 and September 1982
through May 1985. 'Flic organisms caught in the net' were sorted and packed on ice for future analyses of the
digestive tract. Seventy percent of the specimens of the more abundant species were kept; whereas, all specimens
were retained for those species with fewer numbers. In die laboratory the stomachs were removed and preserved
individually with 10 % formaldehyde. The contents of each fish was analyzed individually under a dissecting
microscope, and the food items recorded.
The polychaetes were separated and identified to the lowest possible taxon. The numerical frequency was used
to analyze the results, each fragment possessing a head was counted. The polychaetes were grouped according to
life habits, following the criteria proposed by FAUCHALD & JUMARS (1979) and GASTON (1987).
The families of polychaetes were distributed into four groups on the basis of their spatial location on the
substrate or mobility as subsurface sessile, subsurface mobile, surface sessile and surface mobile.
RESULTS AND DISCUSSION
Of the 2834 stomachs examined from 77 species of fish, 1076 (38 %) were empty and not included in further
analyses. A total of 1398 polychaetes were encountered from 595 fishes (34 %) of which 1 134 could be identified
at least family.
The examination of the Polychaela present in the stomachs of the fish permitted the identification of 28
families, 42 genera and 65 species (Table 1). Those species which were numerically the most abundant arc
indicated with an asterisk in Table 1.
Table 1 . — Polychaete occurrence, number of individuals and numerical frequency
found on stomach contents of demersal and benthic fishes.
334
A.C.Z. AMARAL, E.F. NONATO & M.A.V. PETTI
Table 1 (continued). — Polychaete occurrence, number of individuals mid numerical frequency
found on stomach contents of demersal mid benthic fishes.
* Indicates most frequently occurring polychactes in the stomach of fish.
Table 2 lists the 10 most frequently caught species of fish with die number of stomachs containing food in
their stomach mid the percent occurrence of polychactes.
The feeding habits of die 10 species listed in Table 2 characterize as bendiic feeders and fed specially on
crustaceans, polychaetes, ophiuroids, molluscs and fish. Polychaetes were present in 38.5 % to 88.0 % of die
stomachs analyzed.
Other fish, among which Dasyatis americana Hildebrand & Schroeder, 1828 and Narcine brasiliensis
(Olfers, 1831), fed upon polychaetes regularly but were not included herein due to die small number collected.
The above results confirm the observations of Kawakami & Amaral (1983), who showed that up to
86.0 % of the total volume of organisms present in the stomach of two species of flat-fishes, Etropus
longimanus and Symplmrus jenynsi were polychaetes. Amaral & Migotto (1980) also observed a high
incidence of polychaetes in the stomachs of Paralonchurus brasiliensis (77.3 %), Micropogonias furnieri
(68.5 %) mid Orthopristis ruber (39.9 %) in Ubatuba region of Brazil.
The grouping of polychaete families as a function of habits constitutes mi effective way to clarify why they
are preferred by certain fishes. As discussed by Chao & MUSIK (1977) for young Sciaenidae, the search for food
Source : MNHN. Paris
POLYCHAETES IN THE DIET OF SOME BRAZILIAN FISHES
335
Table 2. — List of the most frequently caught fish species, number of stomachs with food
and percent occurrence of polychaetes in the stomach contents.
Species_ Stomach with contents Frequence polychaete
depends more on die habits of die prey than on selective preference. We grouped the families of polychaeta in
accordance to die position they occupy in the bottom and dieir presumed ability to escape die predator. The
polychaete families were distributed in four groups as indicated in Table 3.
Table 3. — Polychaete families distributed according to the position
they occupy in the sediment.
The 10 most frequently caught fish species were placed into three groups on die basis of dieir feeding
behaviour (Pig. 2). One group of species feed mainly on subsurface mobile polychaetes; these were:
Eucinostomus gula, Genidens gen i dens, Micropogonias furnieri, Zapteryx breviroslris and Umbrina canosai. A
second fed on subsurface mobile ones; diese were: Etropus crossotus and Conodon nobilis. The diird group
336
A.C.Z. AMARAL, E.F. NONATO & M.A.V. PETI’I
B
Conodon nobills
4141
Etropua crosaolus
ES3 SURFACE MOTILES
L J SURFACE SESSILES
SUBSURF MOTILES
SUBSURF. SESSILES
NON IDENTIFIED
FIG. 2. — Species of fish grouped in function of preferences on polychaeles position and mobility. A, those eating
mainly surface mobile forms. B. those feeding on subsurface mobile ones. C, those revealing no definite preference.
showed no defined preferential habit to the position on the substrate or mobility of the polychaetes they caught;
these were: Orthopristis ruber , Paralonchurus brasiliensis and Dules auriga.
The results of the study on the distribution of die polychaetes in die same area carried out by MORGADO
(1988), when analyzed under die same criterion, showed values very similar to diose corresponding to die stomach
contents.
This comparison between the polychaetes found in the area and die polychaetes ingested indicates that these
animals are being preyed upon by members of die fish community in accordance to their availability. However,
when one analyses die data species by species, it becomes obvious diat die preference for one or another group of
polychaetes by a determined species of fish can occur. This indicates the influence of other factors, such as
morphological adaptations or the capacity to explore die substract in a different way.
The group of fish which feed mainly on subsurface mobile polychaetes have the capacity to churn up the
sediment in the search for food and frequently uses this manner to capture their prey. On the other hand, Etropus
Source : MNHN. Paris
POLYCHAETES IN II IE DIET OF SOME BRAZILIAN FISHES
337
crossatus and Conoclon nobilis present certain limitations concerning this capacity, restricting themselves more to
the capture of a group less available in the environment, the surface mobiles.
The criterion of accessibility herein adapted may contribute to a better evaluation of the role of polychaetes as
more frequent or preferential prey of different marine organisms, and also to clarify the existence of specific food
selection processes on the part of their habitual predators.
ACKNOWLEDGEMENTS
We arc particularly indebted to the Instituto Oceanogr^fico (IO-USP) for the logistics support. Special thanks
should be given to Dr. Claudia ALVES Magalhaes and Jacques Vielliard for their suggestions. We are also
grateful to Dr. Donald REISH and two anonymous reviewers who improved earlier versions of this work. This
research was supported by funds from the "Conselho Nacional de Pesquisa (CNPq)". "Funda^ao de Amparo h
Pesquisa do Estado de Sao Paulo (FAPESP)" and "Coinissao Intel-ministerial rle Recursos do Mar (CIRM)".
REFERENCES
AMARAL, A.C.Z. & MlGOTTO, A.E., 1980. lmportancia dos anelideos poliquetas na alimenta^ao da macrofauna
demersal e epibentonica da regiao de Ubatuba. Bohn Inst, oceanogr.. S. Paulo. 29 : 31-35.
BADALAMENTI. F. & RIGGIO, S.. 1989. — I policheti dei contenuti stomacali di Mullus surmuletus L. (Pisces: Mullidae) nel
Golfo di Palermo. Oebalia, 15 : 79-87.
BEN-ELIAHU, M.N. & GoLANL D., 1990. Polychaete annelids on gut content of goal fish (Mullidae) with new
polychaete records. Mediterranean coast and the Gulf of Eilat (Red Sea). Mar. Ecol. 11 : 193-205.
BEN-ELIAHU, M.N., GOLANL D. & BEN-TUVIa, A.. 1983. On predation on polychaetes (Annelids) by the squirrelfish
Adioryx ruber (Holocentridae). with a new polychaete record for the mediterranean coast of Israel. Tethys, 11 15-
19.
Castro filho, B.M.. Miranda. L.B. & Miyao. S.Y.. 1987. Conduces hidrograficas da plataforma continental ao
longo dc Ubatuba : Varia^oes Sazonais em media escala. Bohn Inst, oceanogr.. S. Paulo. 35 : 135-151.
Chao. L.N. & MUSIK. J.A., 1977. - Life history, feeding habits and functional morphology of juvenile Scianidae fishes
in the York River estuary. Virginia. Fish. Bull., 75 : 657-702.
FauGHaLD. K. & Jumars, P.A., 1979. — The diet of worms: a study of polychaete feeding guilds. Ann. Rev. Oceanogr.
mar. Biol.. 17 : 193-284.
Gaston, G.R.. 1987. Benthic polychaeta of the middle Atlantic Bight: feeding and distribution. Mar. Ecol. Prog.
Ser., 36: 251-262.
Kawakami, E. & Amaral. A.C.Z., 1976. — lmportancia dos anelideos poliquetas no regime alimentar de alguns
pleuronectiformes. Supl. Cienc. Cult.. S. Paulo, 28 : 420.
Kawakami. E. & Amaral. A.C.Z., 1983. lmportancia dos anelideos poliquetas no regime alimentar de Etropus
longimanus Norman, 1983 e Symphurus jenynsi Evermann Kendall, 1902 (Pisces, Pleuronectiformes) Iheringia.
Ser. Zool., Porto Alegre. 62 : 47-54.
Morgado, E.H., 1988. Anelideos Poliquetos do Sublitoral da Regiao de Ubatuba - SP, comp re end i da entre as Ilhas
Anchieta e Vitdria. Tese de Doutorado. Universidadc Estadual de Campinas, Instituto de Biologia, 181pp.
Source : MNHN. Paris
37
Ecology of Pherusa sp. (Polychaeta, Flabelligeridae)
Anah'a AMOR
Institute de Embriologia. Biologia e HistolOgfa, Hacultad de Ciencias Medicas
Universidad Nacional de I.a Plata (CONICET), calle 60 y 120
1900 La Plata, Argentina
ABSTRACT
Pherusa sp. is an endolithic species which burrows into hard substrates (loess) with a range of cohesion from 0 to
254.6 kg. cm’2. The burrow is a tube which is closed posteriorly. The shape of the tube reflects in saggital section the
position of the animal inside it. The wall of the burrow is lined with aragonite. The lining is thickest near the opening
of the tube. A dorsal shield on the first 3 chaeligers function as a lid to the burrow when the animal is withdrawn. During
feeding the two palps and the branchiae play a very important role. The food reaches the mouth by different prostomial
ciliary grooves. As with many other boring marine animals, Pherusa sp. is a microphaga and detritous feeder. Waste
products and gametes are discharged to the sea through the two nephridiopores located in the head near the inner line of
branchiae. The first 36 segments of the body are longer and thicker than the rest which resembles a tail. The anus is
located on the terminal end of the tail which is reflexed, making the body U-shaped. The mouth is ventral with respect to
the anus. The intertidal population studied inhabits a loess which on the exposed surface presents a large and dense
stratum of coralline algae. Endolithic species such as Polydora sp.. Themiste petricola, Lithophaga paiagonica. etc.,
surround the holes of Pherusa sp. The density of the species in the intertidal loess of Santa Elena, province of Buenos
Aires, Argentina was 14 specimens in a quadrant of 100 cm2. The species shows indirect development and some of its
larval stages can be collected by washing the epilithic coralline algae from November to February. Pherusa sp. shows
characteristics of tubicolous animals. The gradient of cohesion (0 to 254.6 kg. cm*2) suggests that this species
possesses a physical as well as chemical mechanism for burrowing. The presence of acid mucopolysaccharides in the
tegument gland secretion confirms this deduction. The lining of the tube, thicker around the aperture could indicate a
function of consolidation of the burrow in substrates of low cohesion, but this thickening was also present in high
cohesion substrates. The aragonite lining deposited by Pherusa sp. on the burrow- walls contributes to loess particles
cementation and rock hardness increase.
RESUME
Ecologic dc Pherusa sp. (Polychaeta, Flabelligeridae)
Pherusa sp. est une espece endolithique qui perfore les substrats durs (loess). La perforation consiste en un tube ferine
dans la partie posterieure dont la forme, en section sagittale. indique la position de l'animal a l'interieur du tube. La paroi
du tube est couverte d’aragonite dont lepaisseur augmente autour de l’ouverture du tube. Une plaque dorsale sur les trois
premiers segments de l'animal ferme l'ouverturc du tube lorsque l'animal se retracte. Pendant I'alimentation, les deux
palpes et les branchies jouent un role ties important. Les aliments arrivent a la bouche par plusieurs sillons cilies
AMOR. A., 1994. Ecology of Pherusa sp. (Polychaeta, Flabelligeridae) In: J.-C. Dauvin, L. LaubIER &
D..I. Reish (Eds), Actes de la 4eine Conference internationale des Polychetes. Mem. Mus. nain. Hist. nat.. 162 : 339-
346. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
340
A. AMOR
du prostomium. Comine beaucoup d'animaux marins sedentaires, Pherusa sp. est microphage et mangeur do detritus. Lcs
dcchets el lcs gametes sont libercs dans la mer par les ncphridiopores situes dans la tele, pres dc la ligne interne des
branchies. Les 36 premiers segments du corps du ver sont plus longs, plus larges et plus hauts quo les autres lesqucls
ressemblent d’ailleurs '& une queue. L'anus se trouve posterieurement, il se replie sur le corps formant un u 11 cn resulte
que la bouche est ventrale par rapport a l’anus. La population inlertidale etudiee habite un loess qui presente, sur la
surface exposee, unc strate dense et peuplee d’algues corallines. Des especes endolithiques comme Poly dor a sp.(
Themiste petricola, Lithophaga patagonica. etc., entourent les trous de Pherusa sp. La densite de lespece a Santa Llena
(Argentine) atteint 14 specimens dans un earn* de 10x10 cm I/espece etudiee montre un developpement indirect et
quelques stades larvaires peuvent etre recueillis en lavant les algues corallines epilithiques de novembre a fevrier.
Pherusa sp. presentc les caracteristiques des animaux tubicoles. Le gradient de cohesion (0-254.6 kg. cm'2) suggere que
cette espcce possede un mecanisme physique et un autre chimique pour perforer les substrats durs. La presence de
mucopolysaccharides acides dans la secretion des glandes du tegument confortc cette deduction.
INTRODUCTION
The first objective of the "Bioturbations of the Buenos Aires Loess" program initiated in 1987, was to
establish the relationship between the endolithic macrofauna and the characteristics of the hard substrate (AMOR et
al, 1991). The second goal was to determine the role of die endolithic fauna in the deterioration of the intertidal
loess of Santa Elena beach in the province of Buenos Aires, Argentina. The results of this study on the ecology
of Pherusa sp. contribute to the knowledge of how Pherusa sp. leads to deterioration of die loess.
MATERIALS AND METHODS
The adults of Pherusa sp. tire endolithic and were collected during low ude on the rocky beach of Santa Elena
(37°56’02" S; 58° 1 r35" W) in the province of Buenos Aires, Argentina.
The shoal consists of a bank 5 m high widi a shelf widi drainage channels (Fig. la). Tubes were found on die
sides of small pools located within coralline algae at the mid-tide level (Fig. lb). Rock samples were collected
using a hammer and chisel and transported to die laboratory in buckets of seawater. In die laboratory die sanplcs
were divided according to the study objectives: a) Direct observation of die worms within the rock in order to
study their feeding behaviour. The samples were placed in plastic boxes containing sea-water of 32 P.S.U.
salinity and kept at 24 °C which was similar to the environmental conditions. The worms were fed microscopic
algae from cultures. Observations on feeding behaviour were made under a stereomicroscope, b) Adults were
separated from dieir tubes and fixed with neutral 10 % formalin for staining with Alcian blue (Martoja &
Martoja, 1967). c) The heads of a group of animals were fixed in Bouin's fluid, stained widi Ehrlich's
hematoxylene-eosin, and cut into secdons 5 pm thick, d) The anterior region of die body was fixed in 2.5 %
glutaraldehyde in Millonig's phosphate buffer adjusted to 970 milliomsmoles for scanning electron microscopic
examination. Following dehydration in alcohol and acetone, the material was dried in liquid carbon dioxide in a
criucal point drier, coated with gold palladium and observed in a JEOL microscope, e) Fractions of the tube lining
were separated from the rock and dieir mineral composition was determined using a Philips DRX x-ray
diffractometer model PW 101 1/00 with a copper tube, wavelengdi 1.5454 A, 18 A, 40 kV, goniometer velocity
2°. min1, paper speed 1200 mm. h1.
The pi I of the seawater occupying the space between die animal and die wall of the tube was determined using
"pHYDRION" pH test papers of two ranges: 0-13 and 3-5.5.
The population density was estimated by sampling at low tide using a systematic sampling plan (Krumbain
& Graybill, 1965) which consisted of tracing seven transects perpendicular to die coastline, designated A, AB,
BA, B, BC, CB, and C. Transects A, B, and C extended from the top of the bank to die sea. AB, BA, BC, and
CB ran from the upper inhabited level of the beach to the sea (Fig. 4c).
The study area was 132 m wide (distance between A and C), the bank 5 m high (levels 1, 2 and 3), the beach
36 m long (from the base of the bank to die sea), and the sampled beach 6 m long (levels 4 and 5). The high tide
reaches die bank at level 3. A square frame (10 x 10 cm) was used to count holes with animals at levels 4 and 5.
Source : MNHN. Paris
ECOLOGY OE P HER USA SP. IN ARGENTINA
341
PIG. i. _ Pherusa sp.: a, general view of the collection area on Santa Elena beach, b. view ot a rocky sample in the
intertidal coralline algae zone with burrows, c, lateral view of the worm (drawing), d, burrow, c, burrow with worm
inside it (composed).
Source : MNHN. Paris
342
A. AMOR
RESULTS
Pherusa sp. is an endolithic worm which burrows in hard substrates (Fig. lc). The substrate in the sampling
zone has been described as a loess which is continuously eroded by the sea (AMOR et z//., 1991). The cohesion of
die loess was found to range from 0 to 254.6 kg. cm- in its resistance to compression. Pherusa sp. is found in
loess throughout diis range of resistances along with odier species such as Themisie petricola, Polydora sp..
Lilhophaga patagonica. Petricola paiagonica and Saxicava solida. This suggests Uiat Pherusa sp. and the other
species possess a chemical mechanism in addition to a physical mechanism, which permits diem to burrow into
highly cohesive rock (254.6 kg. cm-2). Preliminary studies indicate that the glands of die tegument of Pherusa
sp. secreted acid mucopolysaccharides as shown by die Alcian blue technique.
The burrow of Pherusa sp. is a blind-ended tube measuring up to 3 cm in lengdi (Fig. Id). Sagital cut of the
tube indicates die position occupied by die animal. The tube walls are covered with aragonite (Fig. 2). The lining
is thicker near the opening than elsewhere in the tube. A dorsal shield on die first 3 chactigers function as a lid to
die burrow when die animal is wididrawn. The seawater lying between the animal and die burrow has a pH of 5.
Fig. 2. — Pherusa sp.: a, diffractogram of the burrow lining.
The structures of the head and the chactae which participate in feeding arc described according to their
functional role.
The head of Pherusa sp. can be either introverted or extended. It is usually found withdrawn into a chamber
formed by a membrane extended in front of the first chaetiger. When the head is introverted, the membrane
invaginates with it. The head is protruded followed by the chaetal cage during feeding. The chactae of die First
Uiree segments of the body form the chaetal cage. The length of die chaetae decreases from die first to the third
segment, and diey are all oriented anteriorly (Fig. 3c). During feeding the chaetae are separated and moved
backwards forming a filtering system.
The prostomium consists of die prostomial lobe with four eyes in die base, die ciliary grooves, a solid ridge
between the right <uid die left ciliary grooves, the nuchal organs, the dorsal lip, the two palps and die two pads.
The two prostomial tracts of cilia originate at the base of the two dorsal branchiae (Fig. 3a,b and d; Fig. 4a). The
ciliated grooves flank the solid medial ridge up and surround die prostomial lobe. These grooves are prolonged as
far as the ciliated fossae of the nuchal organs. The ciliated grooves continue to the base of die palps, cross over
the pad to each side of the dorsal lip to the mouth. The palps originate in the ventral border of die prostomial
lobe.
Source :
ECOLOGY OF PHERUSA SP. IN ARGENTINA
343
FIG. 3. — Pherusa sp.: a, schematic frontal view of head; P. prostomium; PL, palp; DL, dorsal lip; CG, ciliary groove;
NP, nephridiopore; ML, median lip; S, chaeta. b, head evaginated with the buccal capsule extruded (palps cut), c. the
chaetae of the first three segments are separated like fans in this worm shown on the rock. d. branchiae impel food
particles to the ciliary grooves.
Source :
344
A. AMOR
FlG. 4. - Pherusa sp.: a. beginning of the left ciliary groove on the branchial membrane, b, a section of the head
showing the nephridia which also act as gonoducts (dorsal arrows) and the nephridiopores which also acts as
gonopores (ventral arrows), c, study area 132 m wide; bank 5 m high (E); beach 36 m long (B); sampled beach 6 m
long (comprised levels 4 and 5); transects A. AB, BA. B. BC, CB. and C; dotted pattern, low cohesion: vertical
striped, medium cohesion; horizontal striped, high cohesion: plain, presence of Pherusa sp.
They are extensible, retractable, deciduous and rounded distally. The palp is horseshoe shaped with a ciliated
almost straight base in the centre of which there is a ciliated slit (the ciliated groove of the palp) and a cavity
separated by a septum. This separation of the cavity disappears towards the end of the palp. The circular and
longitudinal muscles and the fluid-filled cavities of the palp form a hydrostatic skeleton. When the animal feeds,
the ciliated base of die palps sweeps across the chaetal cage. The captured particles are moved by the cilia towards
the medial groove. The ciliary current of die groove, which transports the particles, is rapid and arrives at die
mouth passing between the dorsal and medial lips of each side.
Source :
ECOLOGY OF PHERUSA SP. IN ARGENTINA
345
The branchiae of Pherusa sp. arise from an achaetous segment between the first chaetiger and the head during
the pelagic larval stage. They surround the prostomium in adults. They are filiform, contractile and ciliated along
their length with an unusual distribution of cilia. There are between 80 and 90 branchiae divided into two groups
on each side of the prostomium. The two groups are united dorsally by a pair of branchiae (Fig. 3a,b, and d). The
dorsal branchiae arc longest. The ciliated branchiae produce movement of the water and particles in suspension in
the space limited by die chaetae of the first chaetiger. Food particles are concentrated and moved to the base of the
two dorsal branchiae (Fig. 3d; Fig. 4a). The food particles are transported by the ciliary current of the prostomial
grooves to the mouth. Pherusa sp. is a microphage and detritus feeder and feeds by day similar to other boring
marine animals.
The two nephridiopores of Pherusa sp. are located in the branchial membrane near the internal line of
branchiae and on each side of die prostomial ciliated grooves (Fig. 4b). Waste products and gametes are discharged
through these pores.
The first 36 segments of die body are longer and wider than the rest which resembles a tail. The anus is
located on the terminal portion. The tail is reflexed to give die body a U-shaped appearance. The mouth is ventral
to die anus.
The population inhabits a loess which is covered with a dense growth of coralline algae. By systematically
sampling the intertidal population, the density at Santa Elena was estimated to be 14 ind./lOO cm2. The species
shows indirect development during November to February. Some of die larval stages can be collected by washing
the coralline algae during this time.
The histochemical studies of the secretion of the tegumentary glands indicated the presence of acid
mucopolysaccharides (Alcian blue at pH 5).
DISCUSSION AND CONCLUSION
The paper by SPIES (1975) on the functional anatomy of the flabelligerid head was used as a basis for
interpretation of the head.
Studies on the ecology of endolidiic species of flabelligerids are limited. Bleakney el al. (1980) mentioned
Flabelligera affinis living in vacant burrows of die pclccypod Zirfaea crispata. This species is not a true endolidiic
worm since it does not burrow; it is a typical worm of cryptopfauna crevices.
Pherusa sp. is similar to a typical tubiculous animal in which die mouth, branchiae and nephridiopores are
found in die anterior end. The anus is located at the posterior end of the body but die reflexed tail located the anus
near the open end of die tube. All apertures of the body are at approximately the same level and near the opening
of the tube.
The slightly acidic pH of the seawater within die tube could account for the absence of other organisms or
ectoparasites on the body or widiin the tube. The acid mucopolysaccharids detected in die secretions of die
tegumentary glands support die idea that Pherusa sp. possesses a chemical mechanism for burrowing in addition
to a physical one.
Population density was estimated from 14 samples in which a high density. 14 burrows in 100 cm2 with live
animals was found in only seven suggesting diat die population in the study area is distributed in dense patches
of worms.
The lining of the tube is thicker mound die aperture which could aid in establishing the burrow in substrates
of low cohesion, but diis diickening was also present in high-cohesion substrates.
The aragonite lining of the tube of Pherusa sp. could contribute to die cementation of the rock and increase its
hardness in the same way as die caleite deposits of the burrow walls of Lilhophaga patagonica, Petricola
patagonica, tuid Saxicava solida which also inhabit die same area.
REFERENCES
Amor. A.. LOPEZ Armengol. M.F.. Iniguez Rodriguez. A.M. & Traversa. L.P.. 1991. — Intertidal endolidiic fauna and
it's relationship to the mineralogical. physical and chemical characteristics of the substrate. Mar. Biol., Ill :
271-280.
346
A. AMOR
BLEAKNEY, J.S., ROBINSON. S.M. & WAUGH. J.C., 1980. — Endolithic fauna of vacated Zirfaea crispata L. burrows in
Blomidon shale, minas basin. Nova Scottia. Proc. N.S. Inst. Sci., Nova Scotia, 30 : 55-63.
Krumbain. W.C. & GRAYBILL. F.A., 1965. — An introduction to statistical models in geology. Me Graw Hill Book Co..
New York, 475 pp.
MARTOJA. R. & MARTOJA-PlERSON. M., 1967. — Initiation aicx techniques de Vhistologie animate. Masson ct Cie.,
Paris, 345 pp.
Spies, R.B.. 1975. Structure and function of the head in flabelligerid polychaetes. J. Morph., 47 : 187-208.
Source : MNHN. Paris
38
Polychaete fauna associated with the
coral Cladocora caespitosa (L.)
in the eastern Mediterranean
Christos ARVANITIDIS & Athanasios KOUKOURAS
Department of Zoology
University of Thessaloniki
540 06 Thessaloniki. Greece
ABSTRACT
Analysis of the polychaete fauna in 14 colonies of Cladocora caespitosa at two localities of Chalkidiki Peninsula. N.
Aegean Sea. revealed 87 species. 58 of which are recorded for the first time as associated with this scleractinian coral. Larger
colonies (up to 7 kg) contained more species, more individuals and a greater biomass. In one location, depth 3-5 m, Serpulidae
were dominant ( Vermiliopsis infundibulum, Hydroides pseudouncinata pseudouncinata, Vermiliopsis striaticeps,
Spirobranchus polytrenia and Serpula vennicularis) but at 16-19 m these were rivaled in abundance by errant species,
especially Ceratonereis costae.
RESUME
Faune de polychetes associee au scleractiniaire Cladocora caespitosa (L.) en Mediterranee orientale
L' analyse de la faune annelidienne trouvee dans 14 colonies de Cladocora caespitosa provenant de deux stations de
profondeur 3-5 m et 16-19 m sur la peninsule de Chalkidiki, mer Egee, Nord de la Cnece, a montre qu'une faune diversifiee de
polychetes est associee. Des 87 especes nSeoltees. 58 sont reconnues pour la premiere fois comine hotes de ce scleractiniaire.
Dans la station a 3-5 m, les Serpulidae etaicnt dominants ( Vermiliopsis infundibulum, Hydroides pseudouncinata
pseudouncinata, Vermiliopsis striaticeps, Spirobranchus polytrenia et Serpula vennicularis), alors qu‘a 16-19 m ils etaient
surpasses en abondance par des especes errantes, en particulier Ceratonereis costae.
INTRODUCTION
The coral Cladocora caespitosa (L., 1767), is unique among the scleractinian species living in the
Mediterranean due to die presence of large zooxandiellate colonies. The diameter of its colonies may exceed lm
(Zi brow tus, 1980). The base and dead parts as well as the living parts of C. caespitosa provide suitable sites for
attachment of many animal species. They may attach themselves to die surface, bore into die skeleton, or may be
sheltered or confined within the interlacing branches. As a result, the associated fauna is highly diversified
(Vaughan & Wells, 1943; Vafidis, 1993).
ARVANITIDIS. C. & A. Koukouras, 1994. — Polychaete fauna associated with the coral Cladocora caespitosa (L.) in the
eastern Mediterranean. In: J.-C. Dauvin, L Laubifr & D.J. Rt-ISH (Eds). Actes de la 4eme Conference internationale des
Polychetes. Mem. Mus. natn. Hist. not.. 162 : 347-353. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
348
C. ARVANITTDIS & A. KOUKOURAS
In ihe North Aegean Sea. C. caespilosa colonies may contribute significantly to the formation of submarine
banks, together with other organisms, such as calcareous algae, sponges, polychaetes, etc. (KOUKOURAS &
KUHLMANN, 1991; KUHLMANN el at., 1991). Although it is well known that the fauna and flora in these banks are
especially rich, information concerning die organisms associated is limited (Laborer, 1961; Lumare, 1967;
Spada, 1968; Zibrowius, 1980 and Vafidis, 1993). Some data has been given by Zibrowius (1968, 1969,
1979) and Scisciou & Nuzacci (1970), concerning polychaetes living within these colonies. The present study
provides additional information on the composition and the relationships ot the macrobenthic communities
associated with C. caespilosa colonies.
MATERIALS AND METHODS
Sampling was carried out in autumn 1987 at two stations on Chalkidiki Peninsula (Fig. 1). At station 1
(Pirgadikia) the depth was 3 to 5 m and at station 2 (Vourvourou) it was 15 to 19 m. The colonies were detached
from the substrate according to the method of McCl.OSKEY (1970) and KOUKOURAS el at. (1985).
FIG. L — Map indicating the two sampling areas: 1. Pirgadikia (depth 3-5 m); 2. Vourvourou (depth 15-19 m).
Each colony was weighed and its volume measured by means of water displacement. The polychaetes present
were identified to species and their dry biomass measured. The correlation between the volume and weight ot
colonies, on one hand, and the number of species, number of individuals and biomass of polychaetes, on the other,
was based on the “rank correlation coefficient” or Spearman test (Schwartz, 1963) since none of the above
parameters was normally distributed. To estimate the faunal affinity between colonies, based on the polychaete
composition, the quantitative coefficient given by Czekanowski (Bray & Curtis, 1957) was used, and the
relevant dendrogram constructed as described by Lance & Williams (Daget, 1976). In order to quantify die
contribution of the various species, the biological index, the frequency of appearance, the mean and cumulative
dominance were estimated according to die mediods proposed by GuiLLE (1970).
Source :
POLYCHAETE FAUNA ASSOCIATED WITH CLADOCORA CAESP1TOSA
349
RESULTS
Tabic 1 lists the 87 polychaete species present in die 14 colonies examined. In figure 2, the positive correlation
between the volume and weight of the colonies, on the one hand, and the number of species, individuals and
biomass of the polychaetes on the other hand, can be seen.
IT = 3-021 >1 12:0.010
lT = 3.168 IT >'12:0.005
n =6.060 rr>l 12:0.005
y = .046x + 72.068
tT=5.4 It >« 12:0.005
IT = 3.309 IT >« 12;0.005
tT = 2.986 IT >112:0.010
y = 3.223E-3x + 20.791
Fig. 2. — Correlations between volume and weight of the examined colonies and the number of species, individuals and dry
weight biomass of polychaetes. Note: t12; o.OlO = 2.681, tj 2; 0.005 = 3.055.
A dendrogram groups the colonies according to the polychaete faunal affinity (Fig. 3). Symbols C1-C7
represent the colonies from die shallow station 1, C8-C14 the colonies from die deeper station 2 (Fig. 1). The
colonies are divided into two groups corresponding to die two sampling stations with the exception of Ci(). The
highest affinity between colonies Cjo and C4 could be attributed to diese two colonies were among the most
voluminous and heaviest and were the richest in number of individuals (262 in C4 and 260 in C10).
The 10 most abundant species are presented in 'Fable 2 according to tiieir biological indices a) for the total of
the colonies (values marked with t), b) for die colonies coming from die shallow station 1 (values marked with s).
and c) for die colonies coming from the deeper station 2 (values marked with d).
350
C. ARVANITIDIS & A. KOUKOURAS
Table 1. — List of polychaete species found associated witli C. caespitosa colonies.
The species marked with a star are reported for die first time as inhabitants of this coral.
Nereis ram Ehlers. 1 868
* Acrocirr us front ifilis (Grube. 1860)
*Amphiglena mediterranea (Lcydig, 1851)
*A mphi trite va riabili s (Risso, 1826)
* Arabella 'tricolor (Monlagu. 1804)
*Bhawania reyssi Katzmann, Laubier& Ramos, 1974
*Branchiomma bombyx (Dalyell, 1853)
Branchiomma sp.
Ceratonereis costae (Grube, 1840)
*Cirrifonnia tentaculata (Montagu. 1808)
* Dasy branch us gajolae Eising. 1887
*Demonax brachychona (Claparede. 1870)
*Dodecaceria concha rum Oersted, 1843
*Dorvillea rubrovittata (Grube, 1855)
*Euclymene oerstedi (Claparede. 1863)
Eulalia viridis (Linnaeus, 1767)
* Eum id a san guinea (Oersted, 1843)
Eunice sp.
Eunice torquata Quauefages, 1 865
Eunice vittata (delle Chiaje, 1828)
Euphrosine foliosa Audouin & Milne Edwards, 1833
*Eupolymnia nebulosa (Montagu. 1818)
*Eupolymnia nesidensis (delle Chiaje, 1828)
Eusyllis sp.
*Glycera tesselata Grube. 1863
*Goniada maculata Oersted, 1843
*Haplosyllis spongicola (Grube, 1855)
*Hannoihoe antilopis McIntosh. 1876
*Hannothoe areolata (Grube, 1 860)
*Hannothoe spinifera (Ehlers, 1864)
* Heteromast us filiform is (Claparede, 1864)
Hydroides pseudouncinata pseudouncinata Zibrowius, 1968
*Kefersteinia cirrata (Keferstein. 1862)
Leoc rates chinens is Kinberg, 1866
Lepidasthenia elegans (Grube. 1840)
*tepidonotus clava (Montagu. 1808)
*Lumbrineris coccinea (Renier. 1804)
*Lum b ri ne ris frag ilis (O. F. Muller, 1776)
*Lumbrineris func ha lens is ( Ki nberg. 1 865 )
*Lumb rine ris latreilli Audouin & Milne Edwards, 1834
Lysidice ninetta Audouin & Milne Edwards, 1833
*Matphysa fallax (Marion & Bobretzky, 1875)
*Nainereis laevigata (Grube, 1855)
*Nematonereis unicornis (Grube. 1840)
Nephtys sp.
*Nereis zonata Malmgren. 1867
Nerinides sp.
*Nicolea venustula (Montagu. 1818)
*Notomastus late rice us Sars, 1851
*Notophyllum sp.
Palolo siciliensis (Grube, 1840)
*Perincreis cidtrifera (Grube. 1840)
*Petaloproctus terricola Quatrefages. 1865
Pherusa sp.
Phyllodoce sp.
*Piromis eruca (Claparede, 1870)
*Placostegus ctystallinus sensu Zibrowius, 1968
Polycirrus aurantiacus Grube, 1860
*Poniatoceros triqueter (Linnaeus, 1767)
Pontogenia chtysocoina (Baird. 1865)
Prionospio sp.
*Proceraea sp.
Protula sp.
*Pseudopotamilla reniformis (O. F. Muller. 1788)
*Pterocirrus macroceros (Grube, 1860)
Sabella Spallanzani i (Viviani, 1805)
Sabellaria spinulosa Leuckart, 1849
*Schistomeringos rudolphi (delle Chiaje, 1828)
*Sclerocheilus minutus Grube. 1863
Serpula concharunt Langerhans, 1880
Serpula vennicularis Linnaeus, 1767
*Sphaerosyllis pirifera Claparede, 1868
*Sphaerosyllis sp.
Spirobranchus polytrema (Philippi. 1844)
*Syl!idia armata Quatrefages. 1865
*Syllis gracilis Grube, 1840
*Terebella lapidaria Linnaeus. 1761
*Thelepus set os us (Quatrefages, 1865)
*Tric hob ranch us glacialis Malmgren, 1865
*Trypanosyllis zebra (Grube, 1860)
*Typosyllis hyalina (Grube, 1863)
*Typosyllis krohni (Ehlers, 1864)
*Typosyl l is prolife ra (Krohn. 1852)
*Typosyllis variegata (Grube, 1860)
Vermiliopsis infundibulum (Gmelin, 1788)
*Venniliopsis labial a (Costa, 1861)
Vermiliopsis striaticeps (Grube, 1862)
POLYCHAETE FAUNA ASSOCIATED WITH CLADOCORA CAESPITOSA
351
Among the 10 abundant species (Table 2), six are sedentary forms, including five Serpulidae. The 10 abundant
species comprise 63 % of the cumulative dominance (Table 2). The serpulid Hydroides pseudouncinata
pseudouncinata Zibrowius, 1968 had die highest biological index and mean dominance. The serpulids
Vermiliopsis infundibulum (L., 1788) and Vermiliopsis striaticeps (Grube, 1862) were next with significant
difference in values of biological index and mean dominance. These three species showed a high value of
cumulative dominance (28.24 %).
FIG. 3. — Dendrogram showing the polychaete faunal affinity among the C. caespitosa colonies.
In the colonies from the shallow station 1 (Table 2), the same species appeared in die first 10 of the biological
index classification, except diat Lepidonolus clava (Montagu, 1808) replaced Ceratonereis costae (Grube, 1840).
Bodi diese species are euryoecius and non-sedentary.
Flowever, in die colonies from the deeper station 2 (Table 2), more significant differences existed both in
relation to die shallow station 1 and to the total number of colonies examined. In die deeper water colonies, only
four out of 10 dominant species were sedentary forms (diree serpulids). Furthermore, in the colonies from the
deeper station 2, the euryoecius non-sedentary species Ceratonereis costae (Grube, 1840) and Kefersteinia cirrata
(Keferstein, 1862) are first and third in order of biological index; in die total of die colonies and in die colonies of
the shallow water area, diese two species are not at all classified or have a low biological index.
DISCUSSION
Of die 87 polychaete species associated with die C. caespitosa colonies 58 are here reported for die first time
as inhabitants of this coral where previously only 40 associated had been reported. The total number has been
raised to 98, considering die species added by die present study.
The fact that serpulids were dominant in the colonies from the shallow station 1, whereas errant polychaetes
were dominant in those from die deeper station 2, could be attributed to die different feeding opportunities offered
by die different environment. Serpulids are filter feeders (Fauchald& Jumars, 1979) and would benefit from
water movement and from being near the source of primary production, whereas errant polychaetes being further
up die food pyramid would mostly benefit from die sedimentation of material raining down from above and from
other organisms living in die colonics.
352
C. ARVANITIDIS & A. KOUKOURAS
TABLE 2. — Table of biological indices (lb), frequency of appearance (F), mean dominance (Dm) and
cumulative dominance (Dc) of polychaetes: a) in the total of the colonies (values marked with 0,
b) in the colonies from the shallow station 1 (values marked with s), c) in the colonies
from the deeper station 2 (values marked with d).
REFERENCES
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27 : 325-349.
DAGET. J., 1976. — Us modifies mcithematiques en dcologie. Ed. Masson, 172 pp.
GuiLLE. A.. 1970. — Bionomie benthique du plateau continental de la cote catalane francaise. II. Les communautes de la
macrofaune. Vie Milieu , 21 : 149-280.
Fauchald. K. & Jijmars. P.A., 1979. - The diet of worms: a study of polychaetc feeding guilds. Oceanogr. mar. Biol. arm.
Rev., 17 : 193-284.
KOUKOURAS. A.. VOULTSIADOU-KOUKOURA, E.. CHINTIROGLOU. H. & DOUNAS, C.. 1985. Benthic bionomy of the North
Aegean Sea. III. A comparison of the macrobenthic animal assemblages associated with seven sponge species. Call.
Biol, mar., 26 : 301-319.
KOUKOURAS, A. & D.H.H. KCjhlmann, 1991. - Rasenkorallen als Biotope in der Agiiis. Naturw. Rundsch., 44 : 444-445.
KOHLMANN. D.H.H., CHINTIROGLOU, II.. KOUTSOUBAS, D. & KOUKOURAS, A.. 1991. — Korallenriffe im Mittelmeer ?
Naturw. Rundsch., 44 : 316.
Laborel. J., 1961. - Sur un cas particular de concretion nement animal. Concr6tionnement a Cladocora caespitosa (L) dans
le golfe de Talantc. Rapp. Comm. ini. Mer Mtfditerr., 16 : 429-432.
Lumare. F.. 1967. — Sulla scogliera a Cladocora di Crotone e le sue biocenosi. Rend. Accad. Naz., 16-17 : 101-131. pi. 1-3
McCLOSKEY, L.R., 1970. — rI'he dynamics of the community associated with a marine scleractinian coral, hit. Revue ges.
Hydrobiol., 55 : 13-81.
Sciscioli. M. & NUZZACI, G., 1970. Annelidi polichcti associati a Cladocora caespitosa (L.) del litorale pugliese. Alt. Soc.
Peloritana, 16 : 151-157.
Spada, G.. 1968. Osservazioni sull' habitat della Coralliophila (Babelomurex) babelis R6quien, 1848. Conchiglie. Milano,
4 : 170-176.
Schwartz. I).. 1963. — Mcthodes siatistiques a I’ usage des mtdecins el de biologistes. Editions medicales Flammarion.
Paris, 296 pp.
Source : MNHN. Paris
POLYCI-IAETE FAUNA ASSOCIATFD WITH CLADOCORA CAESPITOSA
353
VaFIDIS. D.. 1993. Systematical, zoogeographical and ecological study of Anthozoa (excluding Actiniaria) from the
continental shelf of the North Aegean Sea. Ph.D. Thesis, University of Thessaloniki, Thessaloniki.
Vaughan. T.W. & Wells, J.W., 1943. — Revision of the suborders, families and genera of the Scleractinia. Geol. Soc.
America, spec. Pap., 44 : 1-363.
ZlBROWius, II., 1968. — Etude morphologique, systematique et ccologique des Serpulidae (Annelida Polychaeta) de la region
de Marseille. Rcc. Trav. Stat. Mar. Endoume , 59, Bull. 43 : 81-253.
ZlBROWius, IE, 1969. — Quelques nouvelles recoltes de Serpulidae (Polychaeta Sedentaria) dans le golfc de Gabes et en
Tripolitaine. Bull. Inst. Oceanogr. Peche, Salammbo. 1 : 123-137.
ZlBROWius, H., 1979. — Quelques recoltes de Serpulidae (Annelida Polychaeta) sur les cotes nord de la Tunisie. Bull. Off.
natn. Pech. Tunisie. 2 : 211-222.
ZlBROWius, IE, 1980. — Les scleractiniaires de la Mediterranee et de l’Atlantique nord-oriental. Mem. Inst, oceanogr..
Monaco, 11 : 1-284.
Source : MNHN, Paris
39
Morphology, ecology and juvenile development of
Cossura pygodactylata Jones (Polychaeta, Cossuridae)
in Arcachon Bay, SW France, with a reassessment
of the geographical distribution of C. pygodactylata
and C. soyeri Laubier
Guy BACHELET *& Lucien LAUBIER **
Centre d'Oceanographie et de Biologie marine
CNRS & Universile de Bordeaux I
2, rue du Professeur Jolyet
33120 Arcachon, France
** Laboratoire de Physiologie des Btres Marins
Institut Occanographique
195, rue Saint- Jacques
75005 Paris, France
ABSTRACT
During a quantitative survey of subtidal infauna in Arcachon Bay (Bay of Biscay. NB Atlantic), more than 1.000
specimens of Cossura were collected in two muddy, shallow channels of the bay. Comparison of these specimen* with the
types of C. pygodactylata Jones. 1956 and C. soyeri Laubier, 1963 showed that the cossurids from Arcachon wen1 almost
identical with the former species. Only the noto- and neurosetal bundles of the first biramous setigers tended to be more spaced
in the french specimens than in the holotype of C. pygodactylata ; this minor divergence does not justify the erection oi a new
species. Examination of many juveniles, some of them being as small as four setigers, allowed the description ol post-
settlement juvenile development. During a two-year survey in the Courbey channel, the highest densities (ca 1.500 ind./m-)
were recorded in April-May. As noted by several authors, there are few useful taxonomic characters in the genus Cossura
Specimens are often collected as anterior fragments, whereas species identification necessitates an examination ol different
regions of the body. For example, the two closely related species C. pygodactylata and C. soyeri differ only by the number <>l
thoracic setigers and the structure of the pygidium. Re-examination of several specimens previously identified as C soyeri
showed that some of them were actually C. pygodactylata. The geographical distribution of C. pygodactylata is extended from
the Pacific coast of North America to both sides of northern Atlantic, whereas C. soyeri appears to be restricted to the
Mediterranean Sea and the northern Gulf of Mexico.
BACHELET, G. & L. Laubier, 1994. — Morphology, ecology and juvenile development of Cossura pygodactylata Jones
(Polychaeta. Cossuridae) in Arcachon Bay, SW France, with a reassessment of the geographical distribution of
C. pygodactylata and C. soyeri Laubier. In: J.-C. Daiivin. L. LAUBIER & D.J. REIS1I (Eds). Actes de la 4eme Conference
Internationale des Polychetes. Mem. Mus. natn. Hist, nat ., 162 : 355-369. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
356
G. BACHELET & L. LAUBIER
RESUME
Morphologic, ecologie et devcloppcmcnt juvenile de Cossura pygodactylata Jones (Polychacta, Cossuridae) dans le
bassin d'Arcachon, SW France, et mise an point sur la distribution gcographique de C. pygodactylata et C. soyeri
Laubier
Lors d’une etude quantitative de 1’endofaune subtidale du bassin d'Arcachon (golfe de Gascogne. Atlantiquc NE). plus d'un
millier de specimens appartenant au genre Cossura ont etc echantillonnes a faible profondeur (3 a 5 in) dans les fonds vaseux
de deux chenaux. La comparaison de ces specimens avee les types de C. pygodactylata Jones. 1956 et de C. soyeri Laubier.
1963 a inontre que les cossurides d'Arcachon sont identifiables a la premiere esp&ce. Seuls les faisccaux de soies des noto- el
neuropodes des premiers setigeres birames ont tendance a etre davantage espaccs chez les specimens arcachonnais que sur
1'holotype de C. pygodactylata : cette divergence mineure ne justifie pas la creation d’une nouvelle espece. L'examen d’un grand
nombre de juveniles, a partir de slades a quatre setigeres. a permis la description des premieres phases du developpement
benthique. Au cours d’un suivi de deux annees dans le chenal du Courbey. les densites les plus elevees (environ 1500 ind./nr2)
ont ete rclcvees en avril-mai. Ainsi que 1'ont note plusieurs auteurs, peu de criteres taxonomiques sont utilisables dans le genre
Cossura. Les specimens sont souvent recoltes a l’etat de fragments anterieurs. alors que I'identification specifique necessite
l’examen des differentes parties de l'animal. Ainsi, les especes voisines C. pygodactylata et C. soyeri different seulement par le
nombre de setigeres thoraciqucs et la structure du pygidium. Un reexamen de plusieurs specimens prealablement identifies
comme C. soyeri a inontre que certains d'entre eux ctaient en realite des C. pygodactylata. La distribution gSographique de
C. pygodactylata est etendue de la cote Pacifique nord-americaine aux deux cot6s de l'Atlantique Nord, alors que C. soyeri
parait limitec a la Medi terra nee et au nord du golfe du Mexiquc.
INTRODUCTION
Cossurids arc small thread-like polychaetes characterized by a single median tentacle inserted on the dorsum
of an anterior setiger. Other characters of the family Cossuridae Day, 1963 include a prostomium without
appendages, reduced parapodial lobes, parapodia uniramous on one or more anterior segments or entirely
biramous, all setae simple, and a pygidium with anal cirri (see Ewing, 1987, for a revised diagnosis of the
family). The family includes two genera, Cossura Webster & Benedict, 1887 with 17 species and Cossurella
Hartman, 1976 with five species. The genus Cossurella is characterized as having a body distinctly divided into
two regions and, in addition to simple setae, a single acicular seta in each ramus of die posterior parapodia
(Gardiner & Wilson, 1977; Ewing, 1987). Although Fournier & Petersen (1991) distinguished three body
regions, there are no clear-cut divisions along the body in Cossura species, and all parapodia have only simple
capillary setae.
As noted by Day (1967), there are few useful taxonomic characters which may be used for identifying
cossurids. The principal diagnostic features are the number of asetigerous peristomial segments, the segment of
insertion of the mid-dorsal tentacle, the number of uniramous setigers, the types of setae, the number of thoracic
setigers and the structure of the pygidium (Ewing, 1984; FOURNIER & PETERSEN, 1991). Unfortunately, the
number of peristomial segments appears to be an artifact of fixation, biramous setigers have been interpreted as
uniramous by several authors when the bundles of setae were close together, and the posterior end is often missing
(Fournier & Petersen, 1991; sec below). The most important specific character in Cossura is the setiger from
which the single dorsal appendage arises; although a greater or lesser part of the tentacle tip may be lost during
collection and sieving, the entire structure is never broken off (THUUN, 1921; Laubier, 1963). FOURNIER &
PETERSEN (1991) also found that the number of thoracic setigers might be, in spite of some local variation,
species-specific. Taxonomic difficulties are not the unique problem in cossurids. Although occurring from
shallow waters to abyssal depths, they are often recorded in low numbers and on a single occasion within a
geographical area. T herefore, little is known about their ecology and population dynamics.
During a quantitative survey of macrobenthic assemblages in subtidal areas of Arcachon Bay, SW France,
several specimens of Cossura sp. were collected in two muddy, shallow channels of the bay (DE Montaudouin,
1988). Later, while processing a collection of polychaetes collected during a two-year study of bivalve
recruitment in one of the above channels (Madam, 1989), one of us (GB) found more than 900 extra specimens
of Cossura. These worms were tentatively identified as C. soyeri Laubier, 1963, which was the most commonly
cited species in European temperate waters. However, comparison of our specimens with the types of C. soyeri
Laubier and C. pygodactylata Jones, 1956 showed that the cossurids from Arcachon should be referred to the
latter species. According to Fournier & Petersen (1991), both species belong to a group of Cossura with the
dorsal branchial filament arising from the second setiger, but differ by the number of thoracic setigers (17-19 in
C. pygodactylata vs. 30-31 in C. soyeri) and the shape of the pygidium.
Source : MNHN. Paris
MORPHOLOGY. ECOLOGY AND DEVELOPMENT OF COSSURA PYGODA Ct'YlA TA
357
In (lie present paper, we describe adult and juvenile stages of C. pygodactylata from Arcachon. To clear up the
confusion between C. pygodactylata and C. soyeri, specimens from different collections are reexamined and tiie
geographical distribution of both species is reassessed.
MATERIAL AND METHODS
A total of 1 ,100 specimens of C. pygodactylata were obtained from mud in two channels, Courbey and
Cousse, of Arcachon Bay (44°40'N, 1°10'W), at depths of 3-5 m below mean low water. In the Courbey channel,
three stations were sampled monthly from February 1985 to January 1987, using a 225 cm2 Ekman grab. Three
replicate box-cores (depth of penetration generally 15 cm) were taken at each station, thus covering a total surface
of 0.2 m2 at each sampling date. Samples were fixed in 4 % buffered formaldehyde solution, then gently sieved
through a 0.2 mm screen, transferred to 70 % alcohol and sorted after staining with Rose Bengal.
Samples were also collected in February 1988 in the Cousse channel and in a single station of Courbey
channel. At both stations, six samples were taken using an Ekman grab. The content of four grabs was sieved on a
1.0 mm mesh; three 8 cm2 cores were taken in each of the two other grabs and washed through sieves of 1.0 and
0.1 mm mesh opening. Samples were processed as above.
Specimens were studied using Wild stereomicroscope and compound microscope. Drawings were made by-
means of a camera-lucida drawing tube; measurements were made with an ocular reticule.
Specimens for SFM were transferred in glutaraldehyde, critical-point dried in carbon dioxide and individually
mounted on aluminium stubs. After coating in gold, the specimens were viewed and photographed with a Jeol
JSM-840A scanning electron microscope using an accelerating voltage of 10 kV.
Cossura pygodactylata Jones, 1956
Figs 1-4
Cossura pygodactylata Jones, 1956: 127, fig. la-f. — REIS 1 1, 1958: 53, Fig. 1. — LAUBIER, 1963: 840 (in key),
841 (in table). — llARTMAN, 1969: 273, figs 1-3. — FAUCHALD, 1972: 207 (in key). — ORENSANZ, 1976: 5 (in
key). — Fournier & Petersen, 1991: 66, table 1.
Cossura longocirrata — Berkeley & Berkeley, 1956: 544, fig. 6. — ? Banse, 1963: 204. — Gibbs, 1969:
314. table 1, 319, table 3, 324. — Curtis, 1977: 31: 1979: 2. — ? Rallo, 1988: 137, 140, fig. 2 ( non Webster &
Benedict, 1887).
Cossura , nr. longicirrata — Hartman, 1954: 11, 15.
Cossura Candida — Ha reman, 1955: 44, pro parte.
Cossura soyeri — Gardiner & Wilson, 1977: 169, fig. 4a-c. — ? Dauvin & Gentil, 1980: 8. — Banse,
1981: 633, pro parte. — HOBSON & Banse, 1981: 55.— ? Aguirrezabalaga, 1984: 122 (in table). — ?
AguerREZabalaga et al ., 1984: 103. — ? Sola & Ibanez, 1986: 172, 173, 175 (in tables) (non Laubicr. 1963).
Cossura sp. — DeMontaudouin, 1988: 18.
Material examined. — Eastern North Pacific: San Francisco Bay, off Point Richmond, California, mud, 16
Apr 1955, one complete specimen (Holotype, USNM 27609). — Orcas Island, Harney Pass, Washington, mud,
Jul 1967, coll. I LL. Sanders, one complete specimen + 37 anterior ends (USNM 42014, labelled 25 specimens).
Western North Atlantic: Southport. North Carolina, black silt, 3-10 m, Sept 1976, coll. T. Finn, 10 ant. ends +
one posterior end + three fragments of abdominal region (USNM 54141).
English Channel: Stonehouse Pool, Sta. 11, Plymouth Sound, silt/clay, 5 m, 25 Jul 1967, coll. P.E. Gibbs, four
complete specimens + 16 ant. ends (BMNII ZB 1980. 341-360). — Bay of Morlaix, Brittany, France, muddy
sand, 15 m. Apr 1980, four ant. ends, coll. J.C. Dauvin (Reference collection of Station Biologique de Roscoff).
Bay of Biscay: Courbey channel, Arcachon Bay, France, mud, 3-5 m, Mar 1985 - Feb 1988, 59 complete spec.
+ 723 ant. ends + five post. ends. — Cousse channel, Arcachon Bay, France, mud, 3 m, 15 Feb 1988, 109
complete spec. + 49 ant. ends + 27 post, ends (all specimens from Arcachon, coll. C». Bachelet; part of this
material is deposited in the MNHN (UC 351)1- — Bidasoa estuary, Spain, sandy mud, 2.5 m, May 1992, coll.
J.C. Sola, seven ant. ends (INSUB). — Basque coast, off San Sebastian, muddy sand, 100 m, Sta. Gl, three ant.
ends; Sta. G4, two ant. ends; Sta. C»6, one ant. end; Sta. G8, five ant. ends. — Basque coast, off Bilbao, muddy
sand, 100 m, Sta. B8, one ant. end (all specimens from Basque coast, coll. F. Aguirrezabalaga, INSUB). —
Basque coast, off the Ria de Gernika, 100 in. coll. A. Rallo, 1 slide with one ant. end (UPV).
358
G. B ACHELET & L. LAUBIER
Diagnosis. — A species of Cossura with dorsal tentacle arising from posterior margin of setiger 2. Proboscis
with 4-8 finger-shaped processes. Setiger 1 uniramous, following setigers biramous. Thorax with 13-21 setigers.
Pygidium wltli three long anal cirri (iwo dorsolateral and one mid-ventral) and 10-20 intercirral papillae. Juveniles
without pygidial processes and with fewer thoracic setigers than adults.
MATERIAL FROM ARCACHON
DESCRIPTION of ADULTS (Figs 1-2). — Body is slender, threadlike, rounded in section, tapered to both ends.
T he longest complete specimen is 0.35 mm wide, 5.7 mm long for 43 setigers. The animals are usually colorless
in alcohol, however some are uniformly yellow ochre.
The prostomium is bluntly conical, without appendages or eyespots, about twice as long as the peristomium.
No nuchal organs have been observed. Tlie peristomium is achaetous and without appendages, as long as the next
segment. Some specimens seem to have two peristomial segments. However, when material is abundant within a
sample, a complete gradation may be found, with some specimens apparently having two asetigers, others having
a single asetiger, and others with only a slight, circular dip in die middle of the prostomium. In specimens with
one peristomial segment, the mouth opens vcntrally between the prostomium and peristomium. In those with two
apparent asetigers, the buccal aperture is situated between these two "segments". Sagittal sectioning of anterior
ends of such specimens does not show any septum in line with die prostomial dip. It is thus clear dial there is only
a single peristomial segment in our specimens, as found by JONES (1956) in C. pygodactylaici from San Francisco
Bay and by THU LIN (1921) and Fournier & PETERSEN (1991) for C. longocirrata. The first apparent asetiger in
some specimens is actually the basal portion of the prostomium which looks like a segment as longitudinal
muscles contract (Thulin, 1921; JONES, 1956). The proboscis has been seen partially protruded in two worms
only; according to Jones ( 1956), it terminates in 4-8 finger-shaped processes.
Fig. 1. — Cossura pygodactylala Jones, Arcachon Bay. A, entire w'orm, left lateral view. B, posterior end in lateral view.
Scale bars : A = 200 pin. B = 75 pm.
The single median tentacle is inserted dorsally on die posterior end of die second setigerous segment. This
branchial filament (BERKELEY & BERKELEY, 1956; LAUBIER, 1963; FOURNIER & PETERSEN, 1991) shows circular
and irregular wrinkles over its whole lengdi and is constricted near its point of insertion. The tentacle is usually
longer than die body (up to 3x) but, due to its high contractility, diere is no relationship between body length and
tentacle length.
Source : MNHN. Paris
MORPHOLOGY. ECOLOGY AND DEVELOPMENT OF COSSURA PYGODA CI'YIA TA
359
Fig. 2. — Cossura pygodactylata , SEM figures of adult specimens from Arcachon Bay. A. anterior end in dorsal view. B.
same animal in frontal view. C. single bundle of setae of setiger 1. in posterior view. D. setiger 6 in dorso-lateral view. E,
bundles of setae from posterior abdominal region, in lateral view. F. detail of capillary notosetae from setiger 2. in frontal
view. Scale bars : A-B = 100 pm. C-E = 10 pm, F = 1 pm.
Source :
ML
360
G. BACHELET & L. LAUBIER
Although consisting of numerous similar segments, the body may be divided into three weakly separable
regions according to the number and position of the setae in each segment and the respective length of setigerous
segments. As in other cossurids there tire no defined parapodial lobes and die setae arise directly from the lateral
body wall.
The thoracic region extends to setiger 16-21; it is characterized by short (50-8 5 pm long), crowded segments
with setae arising in bundles close to the anterior edge of each setiger. Setiger 1 is uniramous; thereafter all
setigers are distinctly biramous. A mid-dorsal groove extends from the base of the unpaired tentacle over the
whole thoracic region. As noted by Laubier (1963) in C. soyeri and Fournier & Petersen (1991) in
C. longocirrata , some specimens have a transition zone of 1-2 setigers between the thorax and abdomen, where
segmental length increases and setae migrate backwards; other specimens show more abrupt transition from
anterior to mid-region.
In the abdominal region (7-20 setigers) segments are longer (70-160 pm) than in the thorax. Fragmentation
always occurs within a few segments posterior to the thorax- -abdomen transition, i.e. after setiger 17-30; this
pattern seems to be characteristic (Jones, 1956; FOURNIER & PETERSEN, 1991). In some specimens there are
poorly marked intersegmental constrictions in the mid-region; in others the abdomen hikes on a moniliform
aspect, with, for example, abdominal segments 160 pm long x 240 pm wide vs. thoracic segments 70 pm long x
170 pm wide measured on an entire specimen. The setae are similar to those of thoracic region and emerge from,
or just behind, the middle of each segment. In ovigerous females, oocytes are present from setiger 19-20 to setiger
26.
The posterior region consists of 2-10 setigers followed by a few (2-3 ?), poorly marked achaetous segments.
The segments are short and crowded, as in the thoracic region. The setae emerge mid-laterally of each segment
and are smaller and fewer than in die abdomen.
The pygidium of adult specimens is cleft mid-dorsally and bears three long, thin anal cirri, 130-250 pm in
length and 8-10 pm in di tune ter; one pair of cirri is inserted dorsolateral ly on die edge of die anal lobes, whereas
the diird cirrus arises mid-ventrally. In addition to these cirri, 5-10 short (ca. 30 pm long) finger-like papillae are
arranged laterally on the margin of each anal lobe. Cirri and papillae do not seem to be retractile.
file setae are all simple capillaries of two. slightly different kinds : shorter and thicker (4-5 pm wide) setae in
the anterior row of thoracic setigers (see below), longer and thinner (2-3 pm wide) setae in die posterior row.
Under transmitted light the setae appear to be slightly limbate and minutely spinulose along one margin; die
ultras tructural arrangement of longitudinal filaments and the occurrence of very thin channels in die outer layer of
die setae (Specht, 1988) also give the impression of longitudinally-striated shafts. SFM reveals that die setae arc
roughly cylindrical, have a smooth proximal shaft and are covered with dense, minute hairs along most of their
length. This pilosity is directed upwards in neurosetae, downwards in notosetae.
The first setiger bears a single bundle of 5-7 setae on either side. The setae are arranged in two rows; the
anterior row is composed of 2-4 short, fairly coarse, bluntly tapering setae which are directed perpendicular to die
body; the posterior row consists of 2-4 longer, slender setae, tapering gradually towards the tips and slightly
curved posteriorly. This setal arrangement in two parallel vertical series, i.e. an anterior row of setae thicker and
shorter than those of a posterior row, persists in the biramous dioracic setigers; in these segments, there are 9-
15 setae on cither side, distributed in nearly equal numbers between die noto- and neuropodia (4-8 setae) and
between the anterior and posterior rows. The highest number of setae (7-8 per ramus) is found in setigers 2-12.
The setae of the anterior row project laterally, while those of the posterior row are directed posteriorly and
dorsally in the notopodium, posteriorly and ventrally in the neuropodium.
In die abdominal region die setae are positioned mid-laterally in each segment, but without indication of rows.
All setae become long, slender capillaries; dieir number decreases to 4-9 on either side. Progressively the tips of
all setae tend to be directed forward. In the preanal region, the number of setae is gradually reduced to 1-4 on each
side; all setae are thin capillaries, some arc long (90-100 pm), whereas others (developing setae ?) are short (20-
40 pm).
Description of benthic juveniles (Fig. 3). — Several morphological characters are common to both adults
and juveniles: the shape of prostomium and peristomium, die mid-dorsal tentacle inserted on posterior margin of
setiger 2. the lack of parapodial lobes, die first setiger uniramous, and the following setigers biramous. The most
conspicuous differences between juveniles and adults lie in die body regions and the anal segment.
Segmentation is barely visible in young specimens. Therefore, the segmental length and die position of setal
bundles on each segment cannot be used to distinguish body regions. However, with the exception of the very
Source :
MORPHOLOGY. E- COLOG Y AND DEVELOPMENT OF COSSURA PYGODACTYIATA
361
. 3. Cossura pygodactylpta . benthic juveniles from Arcachon Bay. A, 4-setiger stage, lateral view. B. 1 1-setiger stage,
lateral view. C, 1 4-setiger stage, dorsal view. D, 24-setiger stage, ventral view. Scale bars : A-B = 100 Jim, C-D = 200 Jim.
362
G. BACHI-LET& I. LAUBIER
small worms, thorax and abdomen may be separated by observation of the setae. In the thoracic region, setae are
numerous (4-5 on either side of setiger 1,4-11 in each of the biramous setigers); they belong to the two types
found in adults (i.e., some capillaries short and coarse, others long and thin) and are directed nearly perpendicular
to the body axis. In the abdominal region, setae are fewer in number (2-6 per segment), all of the same slender
type, and tilted forwards. The preanal region is poorly individualized, with one or two setigerous segments (with
1-2 short, fine capillaries) and a few segments devoid of setae.
The length of thoracic region changes during development. In the smallest specimen collected (four setigers,
245 pm long and 65 pm wide), the body cannot be divided into distinguishable regions. Ten-setiger stage worms,
which are die next smallest specimens, are 400-500 pm long and have 7-8 thoracic setigers. The number of
thoracic setigers gradually increases in longer worms until about 20 setigers tire reached, which means that some
abdominal segments of the early juveniles progressively change into dioracic segments. The total number of
setigers also increases widi die overall lengdi, showing dial growth occurs by addition of abdominal segments.
The pygidium of juveniles is devoid of terminal processes. FOURNIER & PETERSEN (1991) also noted diat diere
were no anal cirri in very small specimens of C. longocirrata . In C. pygodcictylatci from Arcachon, the smallest
specimens with bodi anal cirri and intercirral papillae were 26-setigers long.
Ecology and population dynamics. — In the Bay of Arcachon, C. pygodcictylatci was collected in two
shallow channels where bottom water temperature fluctuated between 7 °C (January) and 21 °C (August); annual
salinity range was 27-34 P.S.U.. Highly developed seagrass {Zostera marina) beds induce an increased
sedimentation of fine particles in both sites, which are also relatively sheltered from strong tidal currents and
waves (BouciiET, 1968). Sediment is an organic-rich (loss on ignition: 1 1.2 %) black mud (silt-clay content:
60.1 % in Courbey channel, 73.7 % in Cousse channel); only the top 2-3 mm layer is oxidized. As deep as the
grab penetrates, mud is mixed with high quantities of decaying leaves of Zostera spp. (16.5 % in dry weight in
Courbey channel, and 27.9 % in Cousse channel) (DE Montaudouin, 1988).
Horizontal sectioning of some cores showed that C. pygodactylata lives in the upper 2 cm layer of mud. As
observed by TIIULIN (1921) and Jones (1956), cossurids produce loosely constructed tubes: in some worms, part
of the body is faintly wrapped in membranous fragments, incrusted by very Fine mineral grains. Diatoms and sand
grains are often seen by transparency in the gut; cossurids were classified as subsurface deposit-feeders by
FAUCHALD & JUMARS (1979).
Although most specimens collected at Arcachon were juvenile stages, some ovigerous females were found
every year from February to April. The yolky oocytes were oval and about 1 10 pm long by 70 pm wide; these
sizes are smaller than those given by Jones (1956) for C. pygodactylata (140 pm x 100 pm) and Banse (1981)
for C. soyeri (150 pm x 100 pm), but larger than those found by FOURNIER & PETERSEN (1991) in C. longocirrata
(75 pm x 35 pm); however, these dimensions may refer to different developmental stages. In all our specimens,
the number of oocytes never exceeded eight per segment, whereas, in the same species, JONES (1956) noted that a
single segment might contain as many as 40.
Figure 4 shows the seasonal pattern of abundance in the Courbey channel with recruitment peaks of ca. 1,500
ind./m2 in April 1985 and May 1986. Densities were considerably higher in February 1988 in the Courbey and
Cousse channels, with 4,800 and 32,000 ind./m2 respectively. Numbers dramatically decreased in the next one or
two months following recruitment and the population almost disappeared until the next spring. A similar collapse
of bivalve populations in the Courbey channel has been ascribed to summer oxygen deficiency by Madani
(1989).
OTHER MATERIAL
In his description of C. pygodactylata, JONES (1956) indicated that "the 1st setiger bears a bundle of about six
setae on either side"; then "the 2nd to 6th setigers carry approximately 12 setae on either side, and all setae, to the
6th setiger, appear to arise with no indication of noto- and neurosetal bundles", and "at about die 7th to 8th setiger,
it is possible to differentiate noto- and neurosetal bundles" (p. 128). These assertions have been differently
interpreted by various authors. Following REISH (1958) who indicated in the legend of his figure 1 that "the setae
of the notopodium and neuropodium [in setigers 1-6] are continuous ", Laubier (1963), Fauchald (1972) and
Orensanz (1976) gave keys of the family Cossuridae with C. pygodactylata having 6-7 uniramous anterior
setigers; however, Reish used the same symbol (the single letter S in his figure 1) for the 1st setiger of C. delta in
which "the first setigerous segment is biramous with the setae forming a continuous lateral series" (REISH, 1958:
54). On the other hand, Hartman (1969: 273) noted in her diagnosis of C. pygodactylata : "third segment the first
Source : MNHN , Paris
MORPHOLOGY, ECOLOGY AND DEVELOPMENT OF COSSURA P YGODA CTYLA TA
363
setigerous, its setae in biramous fascicles, as are those farther back". Therefore, it seems that there has been some
confusion in the interpretation of Jones's description of C. pygodactylata , as was also the case with
C. longocirrata (Fournier & Petersen, 1091). Reexamination of die holotype of C. pygodactylata definitely
shows that setiger 1 is uniramous, widi six setae on either side; in the next Five setigers, die setae form almost a
continuous series but, by transparency, it may be seen diat die setae originate clearly from two muscular sheaths
on either side (suggested by Jones's figure lb); die last dioracic setigers are distinctly biramous. In most
specimens from Arcachon die noto- and neurosetal bundles of die first biramous setigers (from setiger 2) are more
spaced than in die holotype; in few of diem, however, the rami of biramous setigers are also very close together.
Other characters of die holotype, especially the number of thoracic setigers and die structure of die pygidium, are
consistent widi Jones's description.
All specimens herein re-identified as C. pygodactylata have in common a single uniramous scdger, die dorsal
tentacle inserted on posterior margin of setiger 2 and 13-21 dioracic setigers (Table 1). Although diverging a little
from die range found in type specimens (17-19), this difference in die number of thoracic sedgers does not appear
to be taxonomically significant.
Very few specimens are complete. When present, die pygidium has always three long anal cirri and a large
number (10-19) of intercirral papillae. In the collection from Plymouth, these papillae are present in two
specimens widi 20 and 22 setigers, i.e. at a smaller size dian at Arcachon. It is also notable that, over the hundreds
of specimens examined, none exhibits a protruded proboscis; a single worm, collected by J.C. Sola, San
Sebastian, in the Bidasoa estuary, has a parually protruded buccal organ. In freshly collected specimens from die
Bidasoa, the dorsal tentacle shows a central, red blood vessel throughout its length.
Numbers m'2
Fig. 4. — Seasonal mean abundance (±1
February 1985 to January 1987.
S.D.) of Cossura pygodactylata in the Courbey channel, Arcachon Bay. from
364
G. B ACHELET & L. LAUBIER
The number and size of oocyies vary between locations. In an anterior fragment collected in September in
North Carolina, there are about 30 oocytes (70 pm x 35 pm) per segment, i.e. a similar number of oocytes, but
smaller by half in size, than those found in April in California (Jones, 1956). Oilier specimens have considerably
fewer oocytes in each segment, as those from Arcachon: eight oocytes (100 pm x 80 pm) in the Bidasoa estuary
(May), six oocytes (80 pm x 60 pm) in Plymouth Sound (July), or even four oocytes (80 pm x 40 pm) in the
worm collected by Rallo (1988).
There remains some doubt about the identity of specimens from the Bay of Morlaix and die Spanish Atlantic
coast where complete worms have never been collected (Table 1). The number of thoracic setigers recorded in
these worms is characteristic both of C. pygodactylata and C. longocirrata ; only the structure of the pygidium.
with numerous intercirral processes in the former species and none in the latter, differs between both species
(Fournier & Petersen, 1991). However, due to the arctic-boreal distribution of C. longocirrata (Fournier &
PETERSEN, 1991) and the neighbouring occurrence of C. pygodactylata at Plymouth and Arcachon, die specimens
of Cossura from Morlaix and die Basque coast are likely to be referable to C. pygodactylata.
Remarks. — Banse (1981) examined specimens from several sites in Washington, that he referred to as
C. soyeri. It may be inferred from his description that the abdominal region begins after the first 30 setigers
(p. 633). However, he reported further (p. 634) that some animals had segments from about setiger 17 packed with
oocytes. Some of these specimens have been reexamined by us and identified as C. pygodactylata : in this lot
(USNM 42014) there was also an anterior fragment of 19 setigers and 2.2 mm long, widi the dorsal tentacle
inserted on the posterior margin of setiger 3 (probably " Cossura sp." in Banse's paper, p.634). Specimens of
Cossura from diis area may belong to two or three species.
Cossura soyeri Laubier, 1963
Fig. 5
Cossura soyeri Laubier, 1963: 833, fig. la-h; 1965: 137. — REYSS, 1971: 542, tabic 1, 552, 609, table 21. —
Fauchald, 1972: 207 (in key). — ORENSANZ, 1976: 5 (in key). — ? Banse, 1981: 633, pro parte. — ? Hobson
& Banse, 1981: 55. — ? Amoureux, 1982: 184. — ? Lopez-Jamar, 1982: 261. table 2. — Ewing, 1984: 4-4, 4-
6, fig. 4-4a-d. — ? Salazar Vallejo & Donath Hernandez, 1984: 61, fig. la-c. — Gambi & Giangrande,
1986: 852. table 1. — ? LOPEZ-Jamar & MEJUTO, 1986: 98. 101, 103 (in tables). — ? ROSENFELDT, 1989: 214.
234. — Fournier & Petersen, 1991: 66, table 1.
Cossura soyerii - DesbruyEres, GuiLLE & Ramos, 1972: 357 (in table).
Cossura sojeri - COGNETTI-VARRIALE & ZUNARELLI-VANDINI, 1978: 42. table 1.
Cossura cf. soyeri - ? Amoureux, 1987: 574.
Cossura longocirrata - ? Banse, 1963: 204 ( non Webster & Benedict, 1887).
Not Cossura soyeri - Gardiner & Wilson, 1977: 169, fig.4 a-c. — Dauvin & Gentil, 1980: 8. —
Aguirrezabalaga, 1984: 122 (in table). — AGUIRREZABALAGA era/., 1984: 103. — AGUIRREZABALAGA,
Ibanez & Ros, 1986: table 1. — Sola & Ibanez 1986: 172, 173, 175 (in tables).
Material examined. — Western Mediterranean Sea: off baie du Troc, Banyuls-sur-Mer, France, mud, 35 m,
27 June 1962, one anterior end (Ilolotype, LA 1052 Gllla); 16 Jun 1962, one ant. end (Paratype, LA 1051 GHIa).
— ? Banyuls-sur-Mer, France, one complete specimen + one ant. end (LA, widi paratype). — off Palavas-les-
Flots, Languedoc, France, muddy sand, 20-25 m, Jun 1991, 18 ant. ends, coll. J.M. Amouroux (LA).
Gulf of Mexico: off Florida, Sta. 12, 90 m, Nov 1980. three ant. ends (USNM 89499); Sta. 33, 145 m, Jul
1981, one ant. end (USNM 89500). — Off Mississippi, Sta. VI — 2638, 24 m, Jun 1975, three ant. ends (USNM
75148). - South Timbalier Lease area, off Louisiana, Sta. 03P, 30 m, Jan 1979, one ant. end (USNM 89504). —
Off Port Aransas, Texas, Sta. 11-1, 22 m, Nov 1976, three ant. ends (USNM 89501); Sta. II-4, 36 m. Nov 1976,
two ant. ends (USNM 89503); Sta. II- 1, Dec 1976, diree ant. ends (USNM 89502).
Eastern North Pacific: Bahia de San Quintin, Sta. 4, Baja California, Mexico, 4 Dec 1981, numerous dried
specimens, coll. L.E. Calderon Aguilera (CICESE).
DIAGNOSIS. — A species of Cossura widi dorsal tentacle arising from posterior margin of setiger 2. Proboscis
with about seven short processes. Setiger 1 uniramous, following setigers biramous. Thorax with 20-31 setigers.
Pygidium with diree long anal cirri (two dorsolateral and one mid-ventral), widioul intercirral processes.
Source : MNHN. Paris
MORPHOLOGY. ECOLOGY AND DEVELOPMENT OF COSSURA P YGODA CTYIATA
365
FIG. 5. — Cossura soyeri Laubier. Banyuls-sur-Mcr, "specimen B". A. entire worm in ventral view, dorsal tentacle broken. B,
posterior end in ventral view. Scale bars : A = 200 mm. B = 100 mm.
Remarks. — The holotype and paratype are anterior fragments, with 39 and 21 setigers respectively, in die
original description two "peristomial segments" were counted, increasing die number of segments to 41 and 23.
respectively. In the holotype the first 28 setigers are similar in shape, with setae arising in bundles at the anterior
edge of each segment; setigers 29-31 become increasingly longer and the setal bundles migrate posteriorly; die
last eight setigers are abdominal setigers, about twice as long as thoracic setigers, and with setae emerging from
the middle of segments.
Within the vial containing the paratype, there was a tube with two specimens, hereafter designated A and B.
Specimen A is an anterior end, about 2.1 mm long and 0.36 mm wide, widi 23 setigers; diis specimen is dark
brown in color, as are die holotype and paratype, and is likely to be the third C. soyeri collected by Laubier
(1963, 1965) off die baie du Troc. The 23 setigers of specimen A, as well as the 21 setigers of the paratype, are all
thoracic setigers. Specimen B is a complete worm, 2.6 mm long, 0.17 mm wide, with 33 setigers; its origin is
unknown but it might have been collected in die area of Banyuls-sur-Mer. The first 23 setigers are similar in
shape (about 55 |im long), separated by marked intersegmental constrictions, as in most specimens reexamined.
The abdominal region consists of 10 setigers, longer (100-1 10 pm) and widi fewer setae than in the thorax. The
preanal region consists of only five short (about 20 pm long), achaetous segments. The pygidium has a slight mid¬
dorsal cleft and bears three long anal cirri, one pair lateral and the other midventral; dicrc are no intcrcirral
processes. Although the first 23 setigers are "thoracic" by their shape, the number of setae decreases by setiger 19-
20 and die setae become more posterior in each segment.
The longest specimen collected off Palavas is an anterior fragment of 0.35 mm wide and 6.7 mm long for
45 setigers; the anterior region extends to setiger 26, as in an other incomplete worm of 28 setigers. Setigers are
all thoracic in the other 16 anterior ends (17-29 setigers). In this collection, most specimens show a partially
protruded proboscis; in one of diem, die proboscis is globular and terminates in seven short processes.
Several specimens from the Gulf of Mexico are damaged posteriorly; the transition from diorax to abdominal
regions is difficult to determine in these specimens. Nevertheless, six anterior ends with 20-30 setigers have only
thoracic segments. In two anterior ends of 21 setigers (USNM 89499) the thoracic region extends to setiger 20. In
the longest anterior fragment (USNM 89501: 4.0 mm long, 33 sedgers) the thoracic region consists of 29 setigers.
In complete specimens from die same area, Ewing (1984) observed and figured (fig. 4-4d) a pygidium with three
filamentous caudal cirri, similar to die pygidium of specimen B.
The principal morphological characters of all reexamined specimens of C. soyeri lire summarized in Table 1.
366
G. BACHELET & L. LAUBIER
Table I . — Comparison of the main morphological characteristics of specimens referred to as (1)
Cossura pygodactylata Jones and (2) C. soyeri Laubier in the present paper.
Data from reexamination of specimens unless otherwise specified.
a Jones (1956). b Fournier & Petersen (1991). c Three lobes between each pair of cirri, according to Berkeley &
BERKELEY (1956), but at least five lobes and several stubby intercirral processes, according to FOURNIER & PETERSEN (1991 ).
“ ATI. ARlSlO, Pamplona (pers. comm.). e EwiNG (1984).
GEOGRAPHICAL DISTRIBUTION
Records of C. pygodactylata have been infrequently listed in the literature, perhaps because of the non¬
occurrence of the characteristic pygidium in most collected specimens and also the possible confusion with both
C. longocirrata (Fournier & Petersen, 1991) and C. soyeri. Originally recorded from central - San Francisco
Bay (Hartman, 1954, 1955; Jones, 1956)- and southern California - Hueneme canyon, off Los Angeles
(Hartman, 1969) -, C. pygodactylata is also present more northerly in the Eastern North Pacific, i.e. in British
Source : MNHN. Paris
MORPHOLOGY, ECOLOGY AND DEVELOPMENT OF COSSURA PYGODACTYLATA
367
Columbia (FOURNIER & PETERSEN, 1991). Fhe present study extends its geographic distribution to the Western
(North Carolina) and Eastern North Atlantic (English Channel, Bay of Biscay). The species may also be present in
Disko Bay, West Greenland, where specimens referred to C. longocirrata by Curtis (1977, 1979) have been
reexamined and identified as C. cf. pygodactylata %by Fournier & Petersen (1991). It occurs in muddy
sediments, from silt to muddy sand; with the exception of the Spanish Basque coast, where it may be found at
depths of about 100 m, C. pygodactylata usually inhabits shallow waters between 1 and 30 m.
Unlike the former species, C. soyeri is sometimes considered as a cosmopolitan species. It is basically known
from die Western Mediterranean — French and Spanish Catalan coast (Laubier, 1963, 1965; Reyss. 1971;
DesbruyLres et al ., 1972), Gulf of Lions (this study), Tyrrhenian Sea (Gambi & Giangrande, 1986), Adriatic
(COGNETTI-VARRIALE & ZUNARELLI-VANDINI, 1978) — where it occurs in muddy bottoms, at depths between
12-35 m, but also up to 1,000 m (Reyss, 1971). The re-examination of specimens collected by Ewing (1984)
confirms its occurrence in the NorUiem Gulf of Mexico, in fine sediments at depths of 21-189 m. Additional
records (not examined because die collections could not be located) of C. soyeri include several locadons in die
Celtic Sea — 610-1,400 m (AMOUREUX, 1982) — , in the Bay of Biscay — Galician rias (Lopez-JamaR, 1982;
Lopez-Jamar & Mejuto, 1986); Banc Le Danois, 450-1,500 m (AMOUREUX, 1987) — , and off Portugal - 320-
1,040 m (Amoureux, 1987) -; dicse records need to be confirmed by collecting new specimens.
Specimens collected in Ensenada Harbour, Baja California, Mexico and referred to C. soyeri by Salazar
Vallejo & Donath Hernandez (1984) were anterior fragments with die dorsal tentacle arising from die
posterior margin of setiger 2. Unfortunately, these specimens became dried during storage. We examined some
dried worms, labelled "C. soyeri ", from a neighbouring location; die worms were impossible to determine but, in
one of them, the tentacle was clearly inserted on the anterior margin of setiger 3 as in C. Candida Hartman
collected from die same area and also re-examined. It is hypothesized that cossurids from the Mexican Pacific
coast widi die dorsal tentacle on seuger 2 might be C. pygodactylata radier dian C. soyeri.
Another disconcerting record of C. soyeri is dial of RoSENFELDT (1989) in die central Red Sea at 601 m depdi.
The single specimen was an anterior end of 41 setigers. 1.5 mm (sic] long. No detail is given about the dorsal
tentacle or the number of thoracic setigers, so this record is doubtful.
In conclusion, the geographical distribution of C. pygodactylata is extended to die entire Pacific coast of North
America and to both sides of die nordiern Atlantic, whereas C. soyeri appears to be restricted to the Mediterranean
Sea and the northern Gulf of Mexico. Such a latitudinal distribution of these two species in the Adantic seems
ecologically justified, whereas the extended distribution of C. pygodactylata on the Pacific coast from California
to Washington is more difficult to explain. It is also clear that the very few morphological characters available to
distinguish these two species do not strengthen this conclusion. From this point of view, it would be desirable to
confirm the morphological results using genetical mediods of species identification.
ACKNOWLEDGEMENTS
I. Madani, X. de MONTAUDOUIN, J.L. Crabos, P.J. Labourg and G. Ollivier are thanked for their
assistance in the field. R. LE MENN, D6partement de Microscopie, Universite de Bordeaux I, is also gratefully
acknowledged for preparing the specimens and SEM micrographs. Thanks are extended to the following persons
and institutions for providing material or unpublished information: Michel Bmaud and Jean-Michel Amouroux,
Laboratoire Arago (LA), Banvuls-sur-Mcr, France; Kristian Fauchald, National Museum of Natural History
(USNM), Smithsonian Institution, Washington, D.C., USA; Jean-Claude Dauvin. Museum National d'Histoire
Naturelle (MNIIN), Paris, France; Florencio Aguirrezbalaga and Carlos Sola, Sociedad Cultural INSIJB, San
Sebastian, Spain; Peter E. Gibbs, Plymouth Marine Laboratory, UK; Alex Muir, British Museum (Natural
History) (BMNH), London, UK; Sergio I. Salazar Vallejo, Centro de Investigaciones de Quintana Roo,
Chetumal, Mexico; Arturo II. Arino, Universidad de Navarra, Pamplona, Spain; Luis E. Calderon Aguilera,
Centro de Investigation Cientifica y de Education Superior de Ensenada (CICESE), Mexico; Ana Rallo,
Universidad del Pais Vasco (UPV), Bilbao, Spain. We are also very indebted to Judith A. FOURNIER, Canadian
Museum of Nature, Ottawa, for helpful comments on earlier drafts and encouragement.
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Source ; MNHN, Paris
40
Larvae-substrate relationships of Eupolymnia nebulosa
(Montagu, 1818) (Polychaeta, Terebellidae):
an experimental analysis
Michel BHAUD & Jae Hoon CHA
Observatoire Oceanologique de Banyuls, University P. ct M. Curie
et Unite Associee au CNRS
Laboratoire Arago. 66650 Banyuls-sur-mer. France
ABSTRACT
The transition from the plankton to the benthos has been investigated experimentally with a terebellid annelid. Tests on
artificial and natural sediments lead to the following results. 1) Larvae were able to displace particles with a greater weight than
their own. but this was possible only if larvae had access to a perfectly immobile platform. Larvae required two kinds of
substrate for settlement, one forming support, the other for building the tube. 2) Mechanisms of the substrate selection by
larvae do not suppose a "choice" from several sediments presented at the same lime and equally accessible; larvae were either
able to use the particles which they contact or unable to do so. in which case they returned to the water column. These tests
indicated more an ecological opportunity than a choice. 3) The reduced selectivity of larvae with age corresponded to an
increasing ability to use particles. Larvae, at each stage of development, were able to manipulate only a well defined size range
of particles. This range increased as development proceeded, and the result was the progressive utilisation developing in the
direction of increasing grain sizes. 4) Selection of sediment by larvae was accomplished on the short term and did not assure
the future of individuals. The result of the transition from the planktonic to the benthic phase was unrelated to the subsequent
success or failure of recruitment. A contrast became visible between limited requirements in terms of grain size and shape
defining a large potential zone for larval settlement, on the one hand, and a spatially limited adult area, on the other hand
These two features were made compatible by the existence of an egg mass in the life cycle.
RESUME
Relations larves-substrat chcz la polychete terebellide Eupolymnia nebulosa (Montagu, 1818): analyse experimentale
La transition plancton/benthos a etc analysee experimentalement sur une annelide polychete terebellide. Les tests realises
sur des substrals arlificiels et naturels ont conduit aux rcsultats suivants. 1 ) Les larves sont capables de deplacer des particules
d'un poids superieur a leur propre poids; ccla est rendu possible par l'acces des larves a un point d'appui parfaitement immobile.
A l'echelle des larves. la fabrication du premier tube benthique necessite deux categories dimensionnelles de particules: les
unes constituant le support et les aulres les elements du tube. 2) Les mecanismes d'etablissement des larves sur un substrat ne
reposent pas sur un choix entre plusieurs sediments presences simultanement et egalement accessibles. Les larves peuvent ou
non. uliliscr les particules qu’elles contactent et dans le cas negalif, dies rctournent dans la colonne d’eau pour preparer un
BHAUD, M. & J.1L CHA. 1994. — Larvae-substrate relationships of Eupolymnia nebulosa (Montagu. 1818) (Polychaeta.
Terebellidae): an experimental analysis. In. J.-C. Dauvin. L. Laubier & DJ. REISII (Eds), Actes de la 4eme Conference
internationale des Polychetes. Mem. Mus. natn. Hist. not.. 162 : 371-381. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
372
M. BHAUD& J.H.CHA
nouveau test. Cette succession d'essais independants traduit une opportunity ccologique el non un choix. 3) L'apparente
diminution de selectivity avec l'age rcpresentc une augmentation des capacites (('utilisation des particules par les larves. A
chaque stade de developpement, dies manipulent une gamine de taille bien definic qui s'elaigit avec l'age; le resultal est une
utilisation progressive vers les tailles elevees d'un sediment heterogene. 4) Les larves selectionnent le substrat sur un court
terine en fonction de leur capacity de manipulation. Liles n'assurent pas necessairement la reussite des stades ulterieurs. Un
contraste apparait entre d'une part les faibles exigences granulometriques des larves conduisant a definir une large zone
potentiellement favorable a leur fixation cl d'autre part la zone de presence dcs adultes particulierement reduite. Ces deux
elements sont rendus compatibles par la presence d'une structure de retention des larves dans le cycle dc vie.
INTRODUCTION
A study was undertaken in the Bay of Banyuls in order to determine the factors influencing the composition
and maintenance of benthic communities. Recruitment success has been discussed as an important process
regulating communities. Larval behaviour, predation, local hydrodynamic patterns and substrate characteristics
were the most frequently cited factors controlling larval settlement (Eckman, 1983; Butman, 1986;
Watzin,1983). Several hypotheses have been presented to explain die long term structure of communities. From
reaction patterns of first contact, active habitat selection has been suggested as opposed to passive deposition
(Butman, 1987). Habitat selection (Meadows & Campbell, 1972) was proposed along with ecological
opportunity (MOORE, 1975). In this second pair of hypotheses, the local distribution of adults was viewed as
largely determined by selection of larvae. Other field observations supported the hypothesis of constrained
settlement, i.e., this pattern resulted in a local distribution determined more by availability of suitable sites than by
selection between equally accessible alternatives. These hypotheses, which are based on field observations, are
probably not as conflicting as suggested by MOORE (1975); they must be tested in the laboratory. We approached
this problem by using Eupolymnia nebulosa, Polychaeta. In the Bay of Banyuls, E. nebulosa is one of the most
abundant species for which a large body of biological information is available. Its life cycle has been described
(Bhaud & GREMARE, 1988. 1991) and preliminary experimental studies investigating settlement requirements
have also been done (Bhaud, 1990b; Cha & Bhaud, 1991).
MATERIAL AND METHODS
EXPERIMENTAL DESIGN. — Four types of experiments were conducted (Table 1) to answer the following
questions; what kind of sediments separately presented are larvae able to use? If they are able to use a given
sediment, how does this ability vary with larval age and increasing particle size? What is the behaviour of larvae
when offered a variety of sediments including unsorted heterogeneous sediments, artificial or natural sediments ?
1) The initial experiments were conducted to determine whether or not the larvae had the ability to use a
particular sediment. Sediments of various nature, size, settling velocity and organic matter content were tested.
One type of sediment was placed in a separate glass peui dish 9 cm in diameter. Rates of larval settlement were
determined after four days. During preliminary experiments (Bhaud, 1990a & b) we had observed that a
heterogeneously distributed sediment of variable thickness resulted in more tubes being present on the margins of
Hie dish where the sediment layer was thinner. The number of introduced larvae was approximately 300; the
percentage of free larvae was calculated after counting 100 larvae with or without tubes, at five places chosen at
random but avoiding the margins. Free larvae were classified as those swimming or lying on the bottom; in the
latter case, no tube has been constructed .
2) To test the effects of larval age on the ability to use a given sediment, 14-day old and 18-day old larvae were
introduced into an aquarium containing either a series of sediments consisting of microbeads (MB), or decanted
silt (DS) (Table 2, iicms 7 and 8. respectively), each available as a thin (t) or thick (T) layer. Four plates were
tested in an aquarium, and each paired aquaria represented a replicate. Sediments were deposited in each aquarium
on plates ot equal surface area. The number of tubes on each test sediment in an aquarium, counted after four days,
was expressed as a percentage of the total number present on all sediments of this aquarium.
3) To test the ability to use different sized grains of one sediment, 14 day old larvae were tested in sediments
consisting of fractions of the fine sand in a range of eight degrees of fineness. Oservations were made daily on
each sediment for six days.
4) In an earlier study (Cha & Bhaud, 1991), and in experiment number 2 (present paper), a greater number of
larvae settled in thin layers of sediment, whether it was mud or microbeads, than in thick layers of sediment. It was
Source : MNHN , Paris
L AR V A E-SUB STR ATE RELATIONSHIPS OF E. NEBULOSA
373
suggested that access to a hard substrate, as a result of the thin layer of sediment, facilitated settlement. To
complement the earlier findings on the role of a heterogeneous substrate, larvae were offered two types of
sediment combined in three substrates: decantation silt (DS. Table 2: no 8) in a thick or a thin layer, and a fraction
of Fontainebleau sand (160-200 pin; Table 2: no 3) with traces of DS (approximately in the ratio 1/500). Only one
enclosure was provided with 3x5cm plates in alternate positions. In addition to these perfectly sorted sediments,
two natural sediments were also tested: the silty sand from the Nephtys hombergii community and the fine sand
from the Spisula subtruncata community.
Supply of larvae. — Larvae were obtained from egg masses (BHAUD, 1990a) which were maintained in a tank
60 cm (1) x 40 cm (w) x 16 cm (h) filled with 50 litres of filtered sea water. Filtering was achieved by passing the
water through synthetic fiber- wool. The water was circulated at a rate of 0.5 1 /min using a now-through system,
the surface water was drained away by an overflow. When larvae were close to hatching from the mucoid mass,
they were removed to a one litre vessel and gently agitated. After 2 hours, the emerged larvae were transfered to a
second vessel with filtered sea water. Larvae were used either immediately or kept for several days until die
desired developmental stage was reached. Estimates of numbers were made from a subsample obtained by
immersing a tube of known diameter in the vessel containing larvae and gently agitating to obtain a homogeneous
suspension (Razouls, 1972). A range of 500 to 60,000 larvae were collected from one egg mass with an average
of about 5,000 larvae. They were collected from late February to early June.
Two methods of collecting larvae of varying age were used, a) Newly produced egg masses were collected at
particular intervals and maintained at the same temperature: b) Egg masses were divided and each half was
incubated at a different temperature. Development was shortened by 6 days when the temperature was increased
from 12 to 18 °C for eight days.
Morphology of larvae introduced into enclosures. — Morphology and age were calculated from a known
time-development series determined at the beginning of the reproductive season in March (Bhaud, 1988a).
Growth rate was positively correlated with temperature (Bhaud, 1988b). Larvae of five setigerous segments in
March is 14 day-old but is only eight day-old in early June. This variation in rate of larval development was
minimized by characterizing die larvae by morphology rather than by age. The date of each experiment was
recorded in the course of the reproductive period. Experiments were conducted in March. Larvae measured 430 to
510 pm in length in experiments 1, 2, 3 and 4; they had five setigers, each with one pair of provisional club-
shaped setae and the first 4 setigers with one pair of capillary setae. They were 14 days old. A second group of
larvae, also used in experiment 2, had eight setigers, each with one pair of provisional club-shaped setae, and the
first six setigers with one pair of capillary setae. They were 18 days old.
Criteria for settlement. — Settlement success was measured by the appearance of the primary tubes of
juvenile benthic stages. This method ensured that the number of tubes counted represented the number of animals
present in the sediment. Counts were verified by inspecting all tubes under a binocular microscope for the
presence of living, dead or abandoned tubes. All larvae built tubes and never abandoned them in these short
experiments. Mortality was negligible. The change from planktonic to benthic life was not a cause of mortality
(Bhaud & Cha, 1992). In order to confirm that we would be able to find dead larvae, 10 larvae with six
setigerous segments, were sacrificed (repeated three times). These dead larvae were still recognizable six days
later. This confirmed the absence of dead larvae at the time of observations made four days after the introduction
of larvae.
Feeding. — It was not necessary to feed these larvae during these experiments since they still had yolk
reserves present in their digestive tract after eight days (Cha. 1990. BHAUD, 1991).
Duration of experiments. — Our study was designed to explore the behaviour of larvae at the time of
settlement and the interaction between settling larvae and natural and artificial sediments. Settlement involved
behaviour indicative of the benthic life stage (BUTMAN, 1987) and was defined as the first lasting contact with the
bottom (KEOUGH & DOWNES, 1982). Tube building was used as an indication that settlement had occurred. The
distribution of larvae was determined among several substrates four days after the introduction of larvae
(Experiments 1, 2 and 4). However, this did not exclude daily observations, allowing us to register intermediate
steps and in particular provisionally settled larvae as in experiment 3.
Sediment type. — The following sediments were used in one or more of the experiments. Mud obtained by
sedimentation from the laboratory running sea- water supply (decantation silt: DS) then sieved through 40 and
60 pm mesh. Fontainebleau sand (FS) (Prolabo, France) was composed of grains between 100 and 315 pm in
diameter. This sand was separated according to the following diameters: 100 to 160 pm. from 160 to 200 pm.
from 200 to 250 pm, and from 250 to 315 pm. An artificial sediment was used (Ferro Prod., Cataphote division,
USA) with microbead sizes measuring 45 to 60 pm and 100 to 150 pm. A second artificial sediment of equal sized
374
M. BHAUD& J.H.CHA
Pyrex particles (OSI, France) was used. Two natural sediments from Banyuls Bay were used: a) silty sand from
the Nephtys fiombergii community which was composed of 5 to 20 % clay (< 40 |im), 50 to 80 % fine sand
(> 40 pm and < 200 pm) and less than 5 % of medium-sized sand (> 200 pm); b) fine sand from the Spisula
subtmncata community which was composed of 5-10 % clay, 80-90 % fine sand and 5-10 % medium-sized sand.
A fraction >40 and < 63 pm of these natural sediments (Nil and SS for Nephtys hombergii and Spisula
subtmncata) was isolated and the settling rate compared with that of the other sediments. All sediments used are
reported in Table 2 with the following characteristics: size, shape, sinking velocity and ability of larvae to use
sediments.
Table 1. Main features of the experimental design. Number of sediments used in one experiment is related
to the nature of particles; number of substrates used in the same experiment is deduced from the pattern of
presentation (thick or thin layer, sorted or not sorted...): replicates are given by the number of aquaria,
even if several equivalent supports are present in one aquarium; S= sediment.
Among well-sorted sediments, only decanted silt (items 8 and 9 in Table 2) has some organic content (1.13 mg.
g-1 dry weight of organic material) and probably also a large amount of microbial biomass; these elements are
known to be strongly correlated with the surface area of the particles (DeFlaun & Mayer, 1983). Previous
experiments (Biiaud, 1990a, b) have shown that the suitability of a substrate was not correlated with the relative
or absolute quantity of organic matter, which suggested the importance of physical characteristics of sediment for
larval settlement.
Characteristics of the sediments may have changed during experiments if their introduction into sea water was
made at die beginning of the experiment, just before adding the larvae. Sediments were prepared in filtered sea
water one week before use in enclosures with the same water to avoid the possibility of a sudden development of
microfauna.
Source : MNHN. Paris
LARVAE-SUBSTRATE RELATIONSHIPS OF E. NEBULOSA
375
'I'able 2. - Sinking velocity and preference for several sediments types by larvae of E. nebulosa. The ability of these larvae
to use the sediment and to construct or attempt to construct tubes is assigned a value from 0 (grains not displaced) to ++++
(well constructed tubes). E S: Fontainebleau sand; MB: microbeads; DS: decantation silt; PY: Pyrex; SS: fine sand of
Spisula subtruncaia community; Nil: silty sand of Nephtys hombergii community. Observations four days after introduction
of larvae. Origin is either synthetic product (S) or a natural product (N). Sediments were sorted in sea water (sw) with a silk
plankton net or sorted in dried conditions (dc) with a metallic sieve or the size range directly furnished (*df). In the column
"shape", is given the ratio of longitudinal to transverse axis. The different levels of the use of sediments (observed in two
replicates) have been photographed and presented elsewhere (Cha & BHAUD. 1992). Free larvae are live larvae,
in the water column or on the sediment but without attached particles. S: sediment.
Preparation of sediments. — Supports of sediments were set out on the bottom of aquaria. These were
movable plates allowing for easy manipulation (Cha, 1990). Sediments were deposited with a pipette onto these
Source
376
M. BHAUD&J.H.CHA
plates in thick or thin layers. Thick layers were 1 and 2 pm thick, which prevented die larvae from reaching die
bottom of die movable plates, and thin layers were one to two layers of particles (approximately 120-300 pm),
which allowed die larvae to reach the surface plates and dins could be considered as a hard substratum.
Speed of sediment deposition. — Sinking sediment was limed in a test chamber 42 cm high and 6.5 cm in
diameter. The chamber was filled with seawater having a salinity of 37.58 %c, and the temperature maintained at
18 °C. The settling velocity was calculated from Stokes' Law:
V= r2C, with C= constant, or V= (D/2)2 x 2(d, -d2)g /9 z d2
with D: diameter of grains, dp density of the particle. d2: density of water, g: gravitational acceleration, z:
kinematic viscosity of the fluid (BUCHANAN, 1971). The vessel was placed in a controlled temperature room and
surrounded by plastic plates disposed on four sides and on the top. For measuring rate of descent of the particles,
the lower part of one side was open in order to observe the particles reaching die bottom. A drop of dye was
added and observed to establish that temperature gradients did not exist.
Hydrodynamic conditions. — All experiments were conducted in aquaria measuring 60 x 40 x 20 cm
containing still sea water 15cm deep. In this set up, the distribution of tubes could only arise from the larvae’s
ability to move. Larvae made multiple passes over die plates; visits of diese plates were followed by a return to die
water column, after leaving a mark on the sediment. Light and temperature were similar for all experiments.
Observation of larvae. — Larvae were observed at the surface of the sediment using two compound
microscopes: one with a horizontal line of sight, the other with a vertical line of sight. These two microscopes
were set on supports equipped with rollers which enabled them to travel on two long horizontal guides (Cha,
1990).
Quality of the biological materials. — Spawned egg masses were available in large numbers which permitted
the use of large volumes in contrast to "finger bowl" ecology (Scheltema, 1986). The synchrony of development
within one egg mass provided individuals at die same developmental stage. The egg masses were laid in the field.
The success of settlement was recorded by counting die number of tubes present. Tube building did not stop once
it had commenced. All larvae appeared healdiy and the number of live individuals did not change significantly
during die experiments in spite of a change from pelagic to benthic ecosystems.
RESULTS
Manipulation of particles by larvae with no choice of sediment. — (exp. nb. 1 in Table 1). Table 2 shows
dial die maximum particle size for transport and agglomeration was about 160 pm. The optimal particle size for
construction of a clearly defined individual tube was 60 pm. The use of sediment seemed to be related to the ease
with which the particles could be manipulated. There was an inverse correlation between the sedimentation rate of
particles and die ability of the larvae to manipulate particles and construct a lube. Sedimentation rates of live
larvae were also measured as for the sediments. For 12 to 16 day old larvae, the mean, of 30 trials, (Table 2: n° 15)
was one-half that for the finest silt particles (n° 9) and onc-lourth dial of the larger silt particles (n° 7 and 8). Items
7, 8 and 9 were the most used particles.
Comparison of the net weight of larvae and particles may explain diese results. Net weight is given by 6 z (dr
dj) V D/2. Larvae are viewed as spheres of 120 pm D. and are compared to sediment 7 (Table 2) which contained
the larger particles (D= 60 pm) used in tube construction. All parameters giving net weight were known except for
dl'. however, the density of organic matter of larvae was certainly lower than that of die sediments and (d,-d2) is
thus lower lor larvae. II Dlarvae is twice Dsediment, and Vlarvae is four times lower than Vsediment, the net
weight ol larvae is one-half that of the sediment. I he problem of manipulating particles arises from die fact that
the net weight of die larvae is lower than die particles. Under these conditions how may larvae grasp particles? We
observed that for sediments 1-5, and for 6-7 (each group with same dj), strength of use grew when D and V
decreased, or when net weight of particles decreased. That suggested that use of particles by larvae was correlated
widi die weight of particles.
Effect of larval age.— (exp. nb. 2 in Table 1). Two stocks of larvae (14 and 18 day old, respectively) were
presented (Fig. 1) with two types of sediments (microbeads, MB and decanted silt DS, items 7 and 8 in Table 1)
widi each sediment presented as a thick and a thin layer. Each experiment was run in two enclosures, each
enclosure receiving one age class and four substrates. Ten replicates were carried out. Only a summary is given
with die quantitative data reduced as the percentage of the total number of tubes in each of the four sediments.
Younger larvae preferred the thin layer of sediment. Presence (in DS) or absence (in MB) of organic matter was
not a source ol variance. The greatest difference which occurred between die highest and lowest number of lubes
Source :
LAR V AE-SUBSTRATE RELATIONSHIPS OF E. NEBULOSA
377
was 41.8 and the coefficient of variation was 88.2. The nature and die thickness of the sediment were of lesser
importance for the old larvae than for younger. The greatest difference in the number of settled larvae was only
22.5 % with a coefficient of variation of 47.1. A comparison test (%2) of the two series gave a significant
difference at a confidence level of 0.05. An age difference of four days resulted in highly modified settlement.
Older larvae were less susceptible to differences between substrates; they had a settlement capability greater than
younger larvae, and they were distributed more evenly between different sediments.
1 4 day-old larvae 1 8 day-old larvae
FIG. 1. — Effect of larval age on selectivity with four sediments, as shown by comparing settlement on various sediments by
larvae 14 (left) and 18 (right) days old. Blocks represent the percentage of the number of lubes which appeared after 4 days
for each age group in each series of four sediments. Mean from 10 replicates. Vertical bars represent standard deviations.
DS: decanted silt < 60 pm; MB; microbeads 60-45 pm; T: thick layer; t: thin layer.
Effect of duration of incubation. — (exp. nb. 3 in Table 1). Approximately 2,000 larvae were introduced into
an enclosure with eight size fractions of fine sand from the S. subtruncala community. The numbers of tubes
constructed were observed daily, and these data are summarized in figure 2. Twenty-four hours after the
introduction of larvae, the rates of settlement were highest on the finer sediments (1,2 and 3), lower on middle-
grade ones (4 and 5) with no settlement on the coarser ones (6, 7 and 8). Sediments of grades 1 and 2 were the
preferred substrate on day 6. Sediments of grade 4 had a similar number of tubes as grade-3 sediment alter six
days, but they appeared later. Very few tubes were made in sediment grades 6, 7 and 8 and they were not formed
until day 6.
Addition of tubes formed on each sediment grade was normalized to 100 (Fig. 2), but the number of tubes built
on each sediment was not the same. Comparison of the real number of settled larvae on substrates just after
disappearing from the water column (horizontal boxes "hrs2"), with the number of lubes counted on day 6
(horizontal boxes "day 6"), allows one to conclude that a numeric rearrangement occurs. Larvae settling on
sediment 6-7-8 cannot use it but can still return to the water column. This increased the probability of reaching
easy to use sediments. A small fraction of larvae visiting 6-7-8 and registered in boxes "hrs2" do not leave these
sediments. They can wait for several days during which morphological development proceeds. Accordingly,
unused sediment on the first day may be used four or six days later. On sediments 4 and 5, tubes appeared only on
the third day. Sediments most easily manipulated at the start of the experiment had the highest density of tubes at
the conclusion. Larvae which sedimented on sediment 1-2-3 had the opportunity to settle and did not leave.
Use of heterogeneous sediments. — (exp. nb. 4 in Table 1). The preceding experiments 1 to 3) were not
directly relevant to die Bay of Banyuls where sediments arc more or less heterogeneous. The most homogeneous
sediment (the Well Sorted Fine Sand) is formed of 70 % of 100 to 200 pm particles plus a small fraction of larger
(200 to 500 pm) and smaller (< 40 pm) particles (GUILLE, 1970). We used natural calibrated sediments, isolated or
mixed together, and two natural, unsorted sediments in reconstructing natural sediments for laboratory
experiments.
a) Natural sediment, artificially sorted. — The larvae were offered three sediments with five replicates each
and were placed in one aquarium. The number of tubes were counted at day four. Treatments were randomly
distributed. The three sediments were: (a) silt in thick layer giving a very fluid boundary layer, (b) silt in thin
378
M. BHAUD & J.H. CHA
layer, (c) sand in thick layer with a thin layer of sill on die surface. Statistical comparison (Table 3) showed that a
& b, and a and c, were significantly different but treatments b mid c were not.
day 6
3 a
particle grades
day 1
Fig. 2. Rates ot tube-building by 14-day-old larvae of E. nebulosa in different fractions of sand from the Spisula
subtruncata community. For each sediment grade, blocks give the number of newly built tubes, per day. The block values
in each sediment add up to 100. In fact, the number of tubes built on each sediment is not constant; the real situations for
days 1 and 6 are given in horizontal boxes, below and above, respectively. The reordering is deduced from comparison of
horizontal boxes "hrs 2" (distribution of larvae without tube, two hours after their introduction) and horizontal boxes "day
6" (juveniles in tube, no larvae without lube).
A grain of sand 160-200 pm in diameter was too large for tube building (Table 1). The tubes in series c were
made from silt but not from the sand. The difference in colour between silt and sand made the grey silt tubes
conspicuous against die white sand (Cha & Bhaud. 1992). These results suggest that conditions for settlement
were similar in b and c: the material used to build tubes in both cases was silt and the large grains of sand, in c,
were not used. To explain these observations, we examined die larvae in detail under a compound microscope.
This experiment suggested dial a solid base is necessary for aggregation of particles with mucus by larvae and
for positioning larvae as the tube is built. Construction seemed to be impossible on a fluid substrate which
continually gives way and contained no solid components. This explained why the results from treaunents b and c
were similar as large sand grains in c acted as stable bases for settlement, similar to die bottom of dishes in
treatments b.
b) Natural sediments. — The larval requirements for settlement, as identified by the preceding experimental
observations, allow one to predict which natural sediments are suitable for juveniles of E. nebulosa. Juveniles
required a minimum of clay and medium-sized sand grains. The silty sand of die N. hombergii community seems
Source . MNHN. Paris
LARVAE-SUBSTRATE RELATIONSHIPS OF E. NF.BULOSA
379
suitable, as well as the fine sand of the S. subiruncata community. Experiments confirmed that these sediments
were potential substrates for E. nebulosa larval settlement. In each of 10 replicates, 50 larvae introduced into
enclosures with these two natural substrates produced 50 formed tubes and inhabited by well-developed juveniles.
The important result was demonstrating the ability of the larvae to use a fraction of a heterogeneous sediment.
Photographs and additional results have been presented elsewhere (Ciia & Bhaud, 1992).
TABLE 3. Number of tubes distributed among three substrates, each presented on five plates in one aquarium: surface
of plates 63 cm-. ANOVA shows that total means are significantly different from each other,
which justifies comparisons in pairs showing that b and c are not different.
DISCUSSION AND CONCLUSIONS
The four groups of experiments described provided information concerning several aspects of larval settlement:
(1) the need for a heterogeneous substrate, (2) the importance of the age of larvae at the time of first contact with
the sediment, mid (3) the mechanism of substrate selection. Sediment preferences may change as larvae increase in
size and age. This may not be applicable to oilier species; a behavioural variability may occur (Raimondi &
Keough, 1990).
A solid settlement base is required for coordinated movements of the animal. These coordinated movements
assume that the compression of the coelomic fluid, permitting extension of the body, is possible. The manipulation
and arrangement of particles is then possible. This dual constraint (solid base plus manipulate building particles)
is related to the nature of the substrate. It differs from previous conclusions which suggested that only grain size
was important for settlement (Wilson, 1948, 1952 for Ophelia bicornis ; Gray, 1967 for Protodrilus
rubropharyngeiis: DORSET, 1961 and Hempel, 1957 for Polydora ciliata). Our experiments show also the
importance to settlement of the thickness of the layer of sediment. Similar observations have been made for
Polydora ciliata (Lagadeuc, 1991) and Thelepus setosus (DuCHfiNE, 1983). Wilson (1952), among the 29 points
of his summary, and Butman ( 1987), in her review, did not approach this question.
Larvae at each stage of development are able to manipulate only a well-defined size range of particles. This
range increases as development proceeds. The older the larvae are when they touch die substratum for the first
time, the weaker their ability to return to the water column if the substrate is unsuitable. In the same way, the
suitable particle size range increases with age, and the probability of successful settlement increases. These
behavioural modifications are probably very frequent during development. They are linked to the morphological
development by the increasing number of tentacles, seligcrs and oncinial plates in E. nebulosa. These
modifications have also been observed in molluscs (Aabel, 1983, 1984; Labourg & Lasserre, 1980).
The mechanism of substrate selection is dependent upon whether the larvae can use a particular particle or not.
In this context it is possible to refer settlement to opportunity rather than choice. A choice supposes a comparative
action on a small time and space scale between equally and simultaneously accessible alternatives. Opportunity
results from tests developed by larvae faced with only a single sediment size present.
Application of experimental results to the life cycle of E. nebulosa under natural conditions is limited.
Experimental work on E. nebulosa settlement can only be partially transferred to the field. Larvae were able to
settle on two natural sediments: the fine sand and silty sand of .S’, subtruncata and N. hombergii communities,
respectively. However, juveniles have not been collected from these sediments during a one year study of the Bay
of Banyuls (Grehan, pers. comm.) nor in epibenthic sledge samples collected two months after the first spawning
period (Bhaud & Cha, pers. obser.). Adults have not been found in soft substrates in the Bay of Banyuls (GUILLE,
1970). Adult habitat requirements of E. nebulosa suggest that their absence in both die N. hombergii and the 5.
subtruncata communities is not surprising. Adults of E. nebulosa are collected among rhizomes of the seagrass
Posidonia in Banyuls (KERNELS. 1960). Laubier (1966) stated dial E. nebulosa is present in low numbers on
coralline substrates on the French Mediterranean Catalan coast. This species also occurs on algae of the upper part
of the infralittoral level, on die "silty coastal bottoms" and in the Lacazc-Duthiers canyon (Laubier & Paris,
380
M. BHAUD & J.H.CHA
1962). A detailed study in the English Channel (Lang, 1986) showed that individuals were protected by boulders
buried in the sediment; their tubes were located on the lower side of the boulders, in close contact with the
sediment. Thus, E. nebulosa is a species that lives at the interface of hard and soft substrate. Heterogeneity of
substratum is acknowledged as a requisite for settlement of larvae and points to the way of life of adults. While
larvae can settle on a variety of substrates, these may not be able to support adult populations. The presence of egg
masses restricts the dispersal of larvae, and larval retention represents die coordination between two elements of
the life cycle: modest granulometric requirements defining a large potential tirea for settlement, and a spatially
limited adult distribution. The mucous structure makes these two elements compatible by limiting larval dispersal.
ACKNOWLEDGEMENTS
This work is a contribution to die French National Program on die Determinism of Recruitment (PNDR) and
was supported by a grant to the authors from IFREMER and CNRS. Special thanks go to P. Hutchings, I). Reish
and S. v. BOLETZKY for their comments on die manuscript and improvements of die English text.
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Source : MNHN. Paris
41
Is Owenia fusiformis Delle Chiaje
a cosmopolitan species ?
Jean-Claude DAUVIN *& Eric THIEBAUT **
“Museum national d'Histoire naturellc, Laboratoirc de Biologic dcs Invertebres Marins et Malacologie
UR A CNRS 699. 57. rue Cuvier 75231 Paris Ccdex 05. France
**Observatoire Oceanologique. Universile P. & M. Curie. Paris VI et CNRS-UPR 4601
B.P. 74. 29682 Roscoff. France
ABSTRACT
Some works on Polychaetes report that a very large fraction of the class is widely distributed with a large bathymetric
range. Nevertheless, several recent studies have shown limited distribution of species or genus in the world; it has also
been questioned whether or not any "cosmopolitan" polychaete species exists as a single species. The tube-building
polychaete Owenia fusiformis is considered to have a world wide distribution with depths ranging from shallow littoral to
4.554 m. However, geographical and bathymetric distribution of this species remains uncertain. The objective of this
paper was to bring together all available data in order to present an up-to-date review of the knowledge on the genus
Owenia. Moreover, some observations of macroscopic morphological characters (the presence of a thoracic collar and
eye-spots, the structure of the tube) of specimens collected in Atlantic. Pacific and Indian Oceans were presented. From
this study, only two species remain valid: O. lobopygidiata, which is a bathyal and abyssal Pacific species, and
O. fusiformis. O. collaris described in the eastern Pacific and Carribean and O. caudisetosa . which was only known from
the Salvador coasts, are junior synonyms of O. fusiformis. Although there is some variability of microscopic and
macroscopic morphological characters, these variations do not allow for the identification of several species from
O. fusiformis populations. O. fusiformis seems truly cosmopolitan which is absent only in Antarctic waters. It is a
typical sandy and muddy-sandy species. The species is abundant only in shallows waters (0-40 m). but it is found with
certainly to 2.325 in. The records from greater depths are doubtful insofar as the specimens arc usually fragmented and
may be reported as the bathyal species O. lobopygidiata. The species is able to develop different reproductive strategies
in relation to latitude. Further work is necessary to complete the biological studies of populations especially from the
coldest and warmest waters, and to investigate if there are isolated genetic populations.
RESUMli
Owenia fusiformis Delle Chiaje est-elle une espece cosmopolite ?
Chez les Polychetcs, de nombreux travaux ont mis en evidence une preponderance d'especes possedant une large
repartition geographique et bathymetrique. Toutefois. des etudes recentes ont remis en cause ce cosmopolitisme. divisant
Dauvin. J.C. & E. THIEBAUT, 1994. — Is Owenia fusiformis Delle Chiaje a cosmopolitan species ? In\ J.-C. Dau-
vin. L. LaUBIER & D.J. REISH (Eds). Acles de la 4eme Conference internationale des Polychetcs. Mem. Mus. natn. Hist,
nat ., 162 : 383-404. Paris ISBN 2-85653-214-4.
Source : MNHN . Paris
384
J.-C. DAUV1N & F, TH1EBAUT
les especes largcment distributes en plusieurs especes distinctes. L'annelide polychete tubicolc Owenia fusiforniis est unc
de ces especes avec unc distribution geographique etenduc ; clle est presente des eaux littorales aux zones abyssales,
jusqu’a 4554 m. Toutefois. cctte repartition demeure incertaine. L'objeetif de cet article est de presenter une synthese de
I'ensemble des donnces recueillies sur le genre Owenia. De plus, les resultats d'observations de caracleres morphologiques
macroscopiques (presence d'une collercttc thoracique et de laches oculiformes. structure du tube) de specimens recoltes
dans les oceans atlantique, pacifique et indien sont presentes. Deux especes demeurent valides : O. lobopygidiata .
presente dans les zones pacifiqucs bathyales et abyssales et O. fusiforniis. O. collaris . dccrite dans lest Pacifique et les
Caraibes et O. caudisetosa, dccrite et signalee uniquement sur les cotes du Salvador doivent ctre considerees comme
synonymes d'O. fusiforniis. O. fusiforniis semble done etre une veritable especc cosmopolite, absente seulemenl de
l’Ocean Antarctique. Caracteristique des sediments sableux et sablo-vaseux, clle est abondante uniquement dans les eaux
coheres (0-40 m) et trouvee avec certitude jusqu'a 2325 m. Les signalisations plus profondes sont douteuses dans la
mesure ou les specimens recoltes sont rarement entiers et peuvent sc referer a fespece abyssale O. lobopygidiata. O.
fusiforniis est capable de developper differentes strategies reproductivcs en fonction de la latitude. A l’avcnir, il est
necessaire de (1) completer les etudes de biologic des populations, principalement dans les eaux froides et tropicales el (2)
tester si les differentes populations sont genetiquement separees.
INTRODUCTION
FAUVEL (1959) reported that there are no biogeographical regions for the polychaetes. Available data on the
polychaetes confirm that a very large fraction of the class is widely distributed or with a large bathymetric range
(Holthe, 1978). Nevertheless, several studies show limited distribution of the species or genus in the world wide
ocean (Wells, 1963: KNIGHT-Jones et aiy 1991). The tube-building polychaete Owenia fusiforniis Delle Chiaje
is reported to have a world wide distribution from low-water mark to 4,554 m (Hartman, 1965). Ilowewer, the
geographical and bathymetric distribution of 0. fusiforniis is uncertain as it is questionable whether any
"cosmopolitan" polychaete species is a single species (Nilsen & Holthe, 1985). .Since the beginning of the
century, a large geographical distribution of the species was cited by Gravier (1906). The objective of this paper
is to bring together all available data in order to present an up-to-date review of bathymetry, ecological and
geographical distribution, biology and morphology of 0. fusiforniis. This work is limited by several
methodological problems such as: (1) most of the available data came from ecological studies which had not
confirmed the species true identity; (2) many authors had just seen the tubes of Owenia and automatically referred
them to 0. fusiforniis without examining the specimens. Therefore, in a preliminary work, to define the
occurrence of one or more species of Owenia , some morphological characters of specimens from different localities
of the Atlantic, Pacific and Indian oceans were examined.
HISTORICAL
Although the synonymy of differents species was not always confirmed by the examination of type specimen,
Hartman (1959) considered six valid species of Owenia in her catalogue:
Owenia artifex (Verrill. 1885). Ammochares artifex VERRILL, 1885: 439.
Owenia fusiforniis Delle Chiaje, 1841; Owenia fusiforniis Delle Chiaje, 1841: 31. Ammochares aedificator
Andrews, 1891: 296, pi. 14, figs 42-45. Ammochares assimilator CAULLERY, 1944: 49 [error for A. aedificator
Andrews, 1891]. Ammochares assimilis Sars, 1851: 201. Malmgren, 1867: 210, pi. 12, fig. 65. Ammochares
ottonis GRUBE, 1846: 164, pi. 5, fig. 2. Ops digitata Carrington, 1865: 187. Owenia assimilis Levinsen,
1883: 148. Wollebaek, 1912: 30, pi. 1, fig. 6 Owenia brachycera Marion, 1876: 312. Owenia filiformis
-Claparede, 1868: 446, pi. 26, fig. 5.-' Ammochares brasiliensis Hansen, 1882: 19, pi. 5-6, figs 33-36, 1-4. ?
Ammochares occidentalis (JOHNSON, 1901 : 420, pi. 14, figs 140-142. ? Ammochares sundevalli KlNBERG, 1867
: 343 ? Ammochares tegula KlNBERG, 1867: 343.
Owenia collaris Hartman, 1955. Owenia fusiforniis collaris Hartman. 1955: 46, pl.2, figs 6-7. Owenia collaris
Hartman, 1969: 493.
Owenia lobopygidiata Uschakov, 1950. Owenia lobopygidiata Uschakov, 1950: 214, fig. 31. Owenia
lobopygidiata Uschakov, 1955: 347, fig. 128 E-J.
Source : MNHN. Paris
OWEN I A FUSIFORM IS A COSMOPOLITAN SPECIES ?
385
Owenia orientalis (Grube, 1878). Ammochares orientalis Grube, 1878 : 204, pi. 10, fig. 6.
Owenia tenuis (Haswell, 1883). Ammochares tenuis Haswell, 1883: 633. pi. 12, fig. 2.
Since Hartman's catalogue, only one species Ow enia caudisetosa Hartmann-Schroder, 1959 has been described
from Esiero Jaltepeque, Salvador, Pacific. Hartman (1969) then raised O.fusifonnis collaris Hartman, 1955 to
specific rank as 0. collaris , again clearly stating that 0. fisiformis lacks a collar. Fauvel (1953) gave
Ammochares orientalis Grube, 1878 as a synonym of 0. fisiformis. EHLERS (1901), then RULLIER (1965b) and
Day & Hutchings (1979) considered O. tenuis (Haswell, 1883) as O. fusiformis. The species Owenia artifex
(Verrill, 1885) from Cape Cod has not been cited since its description although many studies have been made in
this region. This species is doubtful as its description corresponds to 0. fusiformis ; it is probably a synonym of
O.fusifonnis. From this summary, the genus Owenia would include four species: 0. caudisetosa , O. collaris, 0.
fusiformis and O. lobopygidiata.
MORPHOLOGICAL DIFFERENCES BETWEEN SPECIES
The principle morphological characters of O.fusifonnis are: crown of tentacles projects forward from the head
region, tentacular crown divided into two lobes, latero-ventral eye-spots, uncini with two teeth side by side, and
pygidium with a pair of weakly developed lobes. DELLE Chiaje (1841) did not indicate the presence of a collar in
Mediterranean specimens. From primary description, the characters distinguishing the other species from 0.
fusiformis are: O. lobopygidiata, absence of ventral eye-spots and a pygidium with nine finger-shaped papillae: O.
collaris , presence of a high, thoracic, membranous collar, and uncini with much longer teeth and without a
shoulder; O. caudisetosa : small size, absence of ventral eye-spot and capillary setae on the first thoracic segment
and the presence of one row of dark pigmentation at the branchial base. Three specimens of 0. caudisetosa were
examined. In contrast, with the original description these specimens have three thoracic segments with capillary
setae. The presence of a pigmented row at the branchial base and the absence of eyes spots should not be considered
as a specific character (see Table 1). All distinctive characters of this species are very similar to those of 0.
fisiformis , and the synonymy of the two species is proposed.
Table 1 gives the principle macroscopic morphological characters observed on specimens from several
localities, including individuals from California named as 0. fusiformis collaris and 0. collaris by Hartman. A
thoracic collar is present in all the individuals, but it is more or less developed. Specimens having a thickly
developed collar are found on the American Pacific and Atlantic coasts, and Kuwait coast. On the North American
coasts, there are specimens with or without a developed collar independent of latitude. On the contrary, on the
European and African coasts, all the specimens have a smaller and thinner collar. The eye-spots are absent only in
a few cases, but this may be due to preservation. A brown pigment band across a branchial lobes is present in
specimens from the Senegal coasts (Table 1). Milligan (1984) reported such brown pigmentation for individuals
from the Gulf of Mexico. Different thorax pigmentation (one or two pigmented rows at the branchial base, or
general pigmentation) are present principally on subtropical and tropical populations. The lube shows variable
granulometric composition and arrangemen: grains of quartz and calcareous fragments piled like roof tiles or
conglomerated sand grains or sand grains in a fibrous matrix. This tube structure seems to be related to the habitat
of the worm. The pygidium does not vary in shape, and all specimens have three setigerous thoracic segments.
Worms with a thick developed collar have a shorter branchial crown with die exception of Louisianan specimens
which exhibit both short and long branchial crowns. In summary, ihis study shows that there is more intraspecific
variability of some morphological characters than occurrence of several Owenia species. Since die thoracic collar
occurs in specimens representing records from all parts of die world, the separation between 0. collaris and 0.
fusiformis seems unjustified. Now, we consider that tiiese two forms should be as O. fusiformis.
T he number of segments and the number of uncini rows in each torus which were primarily used to distinguish
Owenia species arc correlated with age (Thiebaut & Dauvin, 1992). SEM observations of uncini (TTiomassin
& Picard, 1972; Nielsen & Holthe, 1985; Imajima & Morita, 1987; Gambi. 1989; Thi6baut & Dauvin,
1992) from Mediterranean, Pacific, Atlantic and Indian populations, show a homogeneous shape to this character.
Thomassin & PICARD (1972) have observed some differences between Mediterranean and Indian specimens; the
two teeth arranged side by side do appear be at the same level for die Indian specimens. In summary, only two
species known remain in the genus: 0. fisiformis and 0. lobopygidiata.
386
J.-C. DAUVIN & E. THIEBAUT
Table 1. Morphological characters (thoracic collar, latcro-ventral eye-spots, colouring of the thoracic region and tube
structure) of Owenia specimens from different localities. N: number of observed specimens; n: number > 10; o : absent;
* : present: * * : well developed. * identified as Owenia collaris. ** identified as Owenia caudisetosa.
Source : MNHN. Paris
OWEN I A FUSIFORMIS A COSMOPOLITAN SPECIES ?
387
ECOLOGICAL AND BIOLOGICAL CHARACTERISTICS
0. fusifonnis is a typical soft-bottom species. It is found in a large granulometric spectrum from mud to
coarse sand but it usually inhabits muddy sand/sandy sediments. In the English Channel, 0. fusifonnis is present
only in bays and estuaries where fine sediments are confined in relation to low tidal currents (Cabioch, pers.
comm.). On the contrary, in the North Sea, 0. fusifonnis is widely distributed according widespread occurence of
fine sediment (Dewarumez, pers. comm.). On the Texas continental shelf, it is found in sandy sediment with a
relatively low mud content (Flint & Rabalais, 1980).
O. fusifonnis can feed in an uprighi position or bent over towards the substratum; thus i( can be either a filter-
feeder or surface deposit-feeder (Flint & Rabalais, 1980; Gambi, 1989). It forms a crater around its tube, and ii
plays an important role in surface bioturbation (Gambi, 1989). Ii is reported as a common prey for some fiat
fishes in (he area where die population is dominant (EMMETT et ai. 1987; MENARD et ai, 1989).
The species can live three or lour years in die English Channel. It is a polythelic polychaete, and only some
specimens can reproduce at one year (MEnard et ai. 1989; Gentil et al. , 1990). The effective fecundity is
correlated widi (he length of die female which varies from 6,000 oocytes for a female of 40 mm in length to
85,000 oocytes for a female of 1 10 mm in length (ThiEbaut & Dauvin, 1991).
Owenia is known to produce a distinctive planktotrophic larvae (Wilson, 1932). In the Bay of Seine, English
Channel, Gentil et al. (1990) reponed an annual reproduciivc cycle wiih a short summer sexual pause, a gonadial
development during the autumn and spawning occurring from May to June. Recruitment occurred at the end of
spring (Dauvin, 1992). WILSON (1932) also reported mature adults from March to July with spawning in June in
Ihe Plymouth area. BllAUD (1972) compared his planktonic data from subtropical conditions (western
Mediterranean) with results from boreal waters (southern Scandinavia). He showed a shorter occurrence of the
mitraria larvae in northern waters (mid-June to mid-August) compared widi soudiem waters (February to the end of
June). CAZAUX (1973) reported the presence of larvae in planktonic samples from February to April in the
Arcachon Bay. Buchanan et al. (1978) observed a marked summer recruitment in a population from die South
Northumberland coasts. North Sea. These observations with an annual reproductive cycle are obviously different
from those of Me Nui.ty & LOPEZ (1969) who described a year-round breeding population in (he subtropical
waters of Biscayne Bay, Florida, but die life span is shorter in these warm waters. Eager (1964) for a Californian
population, which lives at least two years, observed a main spring recruitment, but also some new recruits through
the year. In Disko Bay, West Greenland, O. fusifonnis reproduced asexually by fragmentation and regeneration in
die absence of favourable conditions for gametogenesis and spawning (CURTIS, 1977).
388
J.-C. DAUVIN & E. THIHBAUT
Fig. 1. The bathymetric distribution of 0. fusiformis. The thick line indicates effective depths of sampling, and the
thin line the possible area of bathymetries. From: 1: AMOUREUX (1966), 2: ANDREWS (1891), 3: de SAINT JOSEPH
(1898), 4: Vovelle (1963), 5 : JELDES & LEEEVERE (1959). 6 : NlCOLAlDOU et al (1988), 7 : CAPACCIONI el al (1991),
8: NlCOLAlDOU & PAPADOPOULOU (1989), 9: COGNF.TTI-V ARRIALE & ZlINARELLI- V ANDINI( 1979), 10: COGNETTI-
Varriale& Zunarelli-Vandini (1978). 11: Giangrande & Gambi (1986), 12 : Gibbs (1971), 13 : George (1974). 14:
CHARDY et al (1987), 15: FAUVEL & RULLIER (1959a), 16: WOLFF (1973), 17: GlLLET (1985), 18: ELIASON (1962), 19:
Rullier (1965a), 20: Hartmann-SchrOder & Hartmann (1965), 21: Hartman (1944b). 22: Clavier & Garrigue
(1990), 23: RULLIER & AMOUREUX (1979), 24: BERKELEY & BERKELEY ( 1952), 25: IMAJIMA (1961). 26: WlLLEY (1902),
27: BRUCE et al. (1963). 28: DUMITRESCO (1960), 29: MlCHAELSEN (1897), 30 : FOURNIER & LEVINGS (1982), 3 :
Fauvel (1909), 32: iNTfcS & LE LOEUFF (1977), 33: BELLAN (1969b). 34: IMAJIMA (1963), 35: Day (1961). 36 :
MILLIGAN (1984), 37: Th£EL (1879), 38: AMOUREUX (1973), 39: WESENBERG-LUND (1951), 40 : IMAJIMA & MORITA
(1987), 41: FAUVEL(1911), 42: BlDENKAP (1907), 43: AMOUREUX (1972), 44: BlDENKAP (1894), 45: DANIELSSEN
(1859). 46: IlARTMANN-SCHRODER (1974a). 47: WOLLEBAEK (1912), 48: HARTMANN-SCHRODER (1986), 49: EHLERS
(1875). 50: Day (1967), 51: WES ENB ERG - LUND ( 1 950b) , 52: USCHAKOV (1955). 53: KlRKEGAARD (1959), 54:
CAULLERY (1944). 55: MclNTOSH (1915), 56: KlRKEGAARD (1983), 57: WESENBERG-LUND (1950a). 58: Bilyard &
Carey (1979), 59: Fauvel(1932), 60: HARTMAN (1966), 61: MclNTOSH (1879), 62: KlRKEGAARD (1980), 63:
Hartman (1965). 64: Eliason (1951).
Source : MNHN. Paris
OWEN 1 A FU SI FOR MIS A COSMOPOLITAN SPECIES ?
389
Table 2. — Records of Owen i a species at depths below 500 in. Condition of sampled individuals is given.
BATHYMETRIC DISTRIBUTION OF OWENIA SPECIES
O.fusiformis is found on the continental shelf 0-200 m (Fig. 1) with only 10 records exceeding 500 m and six
2,500 m. Few specimens arc found depths greater than 500 m, and usually the animal is incomplete or only tube
fragments are found. Most of reports citing O. fusiformis from below 500 m (Table 2) are not precise for the
O. fusiformis status. These include: 1) tubes or tube fragments without worms but with foraminiferan tests
proving the bathyal or abyssal origin; 2) identification with doubt as OP. fusiformis or Owen i a ? sp. or ?
Owenici sp.; and 3) incomplete worms that do not permit a specific identification. It is probable that many of the
Owenia specimens found in deep water are O. lobopygidiata. The maximum depth of O. fusiformis appears to be
2,325 m in the Beaufort Sea (Bilyard & Carey. 1979).
O. lobopygidiatci is a western Pacific species present in Ohkotsk Sea and Bering Sea from 1 10 to 1366 m
(Usci IAKOV, 1955) mid with doubts in the abyssal Bmida Trench at 6,490-6,650 m (Kirkegaard, 1956).
BIOGEOGRAPHIC AL DISTRIBUTION OF OWENIA FUSIFORMIS
Owenia fusiformis occurs both sides of the Atlantic Ocean except along the north Brazilian coasts where the
observations of polychaetcs are limited (Fig. 2). In die eastern Atlantic, it has been observed from the north ol
Norway to South Africa. It is absent from the Baltic Sea. In the Mediterranean waters, it presents principally in the
western part. It has been reported from the Bosphore in the Black Sea. In llie western Atlantic, it is present from
the Gulf of St Lawrence to Rio de la Plata, Argentina. I11 the Arctic, it is reported along both coasts of southern
Greenland at 75 °N latitude. It reaches 80°N latitude, at Spitzbcrg Island and the New Zemble Island. It is also
reported in the Kara Sea and die Beaufort Sea (Figs 2-3).
Source
390
J.-C. DAI IVIN & E. niir.BAUT
FlG. 2. — The atlantic distribution of O. fisiformis. From AMOUREUX (1966. 1970. 1971. 1972, 1973, 1976). ANADON
(1980). Andrews (1891). Augener (1928). Bachelet (1981), Bakalem & Romano (1978). Bakalem (pers. comm.),
Bellan (1969a, b). Bidenkap (1894, 1907). Bruce et al. (1963), Buchanan (1957), Buchanan et al. (1978).
Capaccioni -Azzati ei al. (1991), Castelli et al. (1991), ClaparEdf. (1868), Cognetti-Varriale & Zunarelli-
Vandini (1979). Curtis (1972, 1977), Dalecj al. (1989). Danielssen (1859), Day (1961. 1967), Day et al. (1971),
Dewarumez (pcrs. comm.). Diapoulis & Bogdanos (1983), Dumitresco (1960), Eagle (1973). Eagle & Hardiman
(1976), Eulers (1875), Ei.iason (1962), Fauvel (1909. 1911. 1936, 1937), Fauvel & Rullier (1959a,b).
Frankenberg & Leiper (1977), Gage (1972), Gambi & Gangrande (1986). George (1974), Giangrande & Gambi
(1986), GiLLET (1985. 1988). GlEmarec (1969). GUELORGET & Michel (1979), Guillaumont & IIamon (1983),
Hamond (1966), FIartman (1944), Hartmann-SchrOder (1971, 1974b). Hassam (1991). Holthe (1977b). Ibanez
Aguirre & Solis Weiss (1986). Intes & Le Loeufe (1977), Jeldes & Lefevere (1959). Johnson 1 1901). Kinberg
(1867). Kirkegaard (1959. 1969. 1978, 1983). Laborda (1987). Laubier (1962). Laverde-Castillo & Gomf.z
(1987), Lopez-Jamar (1981), Lopez -Jamar ei al. (1986), LUNA (1967). McCall (1977), McIntosh (1879, 1915),
McIntyre (1958). McNulty & Lopez (1969), Malmgren (1867), Marinov (1977). MassE (1971),
Michaelsen(1897, 1898). Milligan (1984). Nicolaidou ei al. (1988), Nicolaidou & Papadopoulou (1989). Nilsen
& Holthf. (1985). Nonato & I.una (1970). Orensanz & Gianuca (1974). Peer ei al. (1980), Probert (1981),
Quintino & Gentil (1987). Rees (1983). Rees et al. (1976). Rioja (1917). Rullier (1963. 1965a), Rullier &
AMOUREUX (1979). Sanz (1986), Shin et al. (1982), Steimle (1982). Torres-Gavila et al. (1990). Treadwell ( 1948).
Tunberg (1982), Vovelle (1963), Wacasey el al. (1979), WESENBERG-LUND (1950a, b, 1951, 1953), ZGHAL & BEN
Amor, (1980), Zunarelu-Vandini & Cogneiti-Varriale (198 1 ).
Source : MNHN, Paris
OWEN I A FUS1FORMIS A COSMOPOLITAN SPECIES ?
391
In the eastern part of the Pacific Ocean (Fig. 3), it is recorded from Alaska to south California and along die
Peruvian and Chilian coasts where it was named 0. fusiformis or 0. collaris. In die western part, it is reported
from the Bering Sea to Tasmania and New Zealand. It has not been reported from die mid central ocean islands. In
die Indian Ocean (Fig. 3), it is present in Bengal Gulf, Arabic Gulf, Mozambic Channel and along Madagascar
coasts. It is unknown from die Arabic peninsula to the Mozambique coasts.
In summary, 0. fusiformis is present along most of die coasts of the Atlantic and Pacific Oceans, it appears
less extended in the Indian Ocean and absent in die Antarctic Ocean. Several audiors reported 0. fusiformis as
present in this soudiem Ocean, but the single reference (Hartman, 1966) is doubtful because die fragments of
tubes w'erc named as ? Owenia sp. (Table 2). Therefore, the species occurs in tropical, temperate and arctic areas.
FIG. 3. — The indo-pacific distribution of O. fusiformis. From BERKELEY & BERKELEY (1952), BlLYARD & Carey (1979),
Caullery (1944), Chardy ei al. (1987). Clavier & Garrigue (1990). Day (1961. 1967), Day & Hutchings (1979).
Ehlers (1901), Fager (1964), Fauvel (1911, 1919, 1921. 1932), FOURNIER & Levings (1982), GIBBS (1971), Grube
(1878). Hartmann-Schroder & Hartmann (1965), Hartmann-SchrOder (1979. 1980, 1981, 1989, 1990),
IIaswell<1883), Hobson & Banse (1981), Hutchings (1973), Hutchings & Rainer (1979), Imajima (1961. 1963).
Imajima & Morita (1987). Lee (1976), Levenstein (1960). Lie & Kisker (1970), Nako (1982), Okuda (1937), Plante
(1967), Rainer (1981), Rozbaczylo (1985), Rullier (1965b). Sarti Martinez & Solis-Weiss (1987). Shin &
THOMPSON (1982), STEPHENSON & CAMPBELL (1977), TAMPI & RaNGARAJAN (1964), THEEL (1879). USCHAKOV (1955).
Wesenberg-Lund (1949), Willey (1902),Wiren (1883).
392
J.-C. DAUVIN & E. THIEBAUT
TABLE 3. Records of the main populations of Owenia fusiform is (maximal density higher than 100 ind. m-2
or average density higher than 50 ind. m-2). Site, depth and type of community arc precised
(sieving on 1 mm mesh, except 1: 0,280 and 2: 0,5 mm).
Source :
OWENIA FUSIFORMIS A COSMOPOLITAN SPECIES ?
393
POPULATION DISTRIBUTION OF OWENIA FUSIFORMIS
Maximal density (> 100 ind. nr2) or mean density (> 50 ind. nr2) found in the literature are shown in the
Table 3. Maximal densities are found in shallow waters (0-40 m) from fine sand to muddy sand in Venus , Tellinci
or Abra alba communities (Table 2). On 0.5 mm sieve mesh, the densities reach a maximum of 300,000
juveniles, nr2 during July in the Bay of Seine, English Channel (Dauvin, 1992), and 50,000 ind. nr2 during
September on the Oregoncoast (EMMET el ai, 1987, 1988). Densities about 5,000 ind. nr2 are also reported from
llie French Mediterranean (Mass! 1971), the Gold coast, Guinea, California, Peru, Chili, and New Zealand (Table
2).
The greater densities were found in cold-temperate waters rather than tropical waters. The other quantitative data
with lower densities were: N.E. Atlantic, Norway (Holthe, 1977a), North Sea (Me Intyre, 1958), Spanish
coasts (Anadon, 1980: Lopez Jamar, 1981; Lopez Jamar et al, 1986), Morocco (Gillet, 1988);
Mediterranean, Roussillon coasts (Guille, 1971)), Ionian Sea (Vatova, 1975), Tyrrhenian Sea (Giangrande &
Gambi, 1986), Yugoslavia (Gillet, 1985/1986); N.W. Atlantic, Mexican coasts (Ibanez Aguirre & Solis-
Weiss, 1986), North Carolina (Day et a!., 1971); N.E. Pacific, Columbia coast (FOURNIER & LEViNGS, 1982);
N.W. Pacific. Bering Sea (Levenstein, 1960), Japanese Sea (LEE, 1976; Nakao, 1982); S.W. Pacific,
Chesterfield Island (Clavier & Garrigue, 1990), New Caledonia (Chardy et al., 1987); Indian, Nosy Be
(Plante, 1967). No relationship between densities and latitude were noted, except in boreal and Arctic waters
where lower densities were reported.
DISCUSSION
The presence of nine shaped papillae around the pygidium is the principal character separating O. lobopygidiata
from O. fusiformis. The other taxa described as O. ononis or O. assimilis , which arc very close to O. fusiformis,
are considered as synonyms of O. fusiformis. Their descriptions were based on some morphological characters: e.g.
number of segments, or number of uncini rows for each torus, which varied with the age of the worms
(Caullery. 1944: Thiebaut & Dauvin, 1992), and cannot be considered as significant taxonomic characters.
The status of O. collaris characterised principally by the presence of a high, thoracic, membranous collar has been
always uncertain, sometimes defined as a valid species (Hartman, 1969), and sometimes as a subspecies of
O. fusiformis (Hartman, 1955, 1959). In the Gulf of Mexico, Milligan (1984) does not state the identity of
collected specimens possessing a collar. Moreover, Andrews (1891) described O. aedificator having a delicate
membranous collar; later Hartman (1959) considered this species as a junior synonym of O. fusiformis.
Our study demonstrated the presence of a thoracic collar in all examined specimens from all parts of die world.
It showed a more or less important thickness, and this sole morphological difference is insufficient to separate:
O. co/laris from O. fusiformis. In conclusion, the Owenia genus seems composed of two species: O. fusiformis
and O. lobopygidiata. All other taxa described must be considered as synonymous widi O. fusiformis.
Except in the Antarctic, the distribution of O. fusiformis extends world wide from the cold Arctic to tropical
waters. It ranges in depdi from low-water mark to the bathyal zone at 2,350 m. Dense populations were limited to
shallow waters between 0 to 40 m depth from sandy-mud communities. The greatest densities occurred in areas
where fluxes of suspended matter were important: e.g. at the mouth of rivers. Bay of Seine (Dauvin & Gillet,
1991), or in upwelling zones, Oregon coasts (Emmett et a!., 1987, 1988) or Peru and Chili coasts (Tarazona et
al. , 1985: Oyarzun et ai, 1987). Low salinities limited its distribution, as in the Baltic. Temperature was not a
limiting factor; it is recorded from -1 °C in Arctic waters to more than 30 °C in tropical waters. This result is not
a general feature for the polychaetes. Wells (1963) showed that the distribution of the genera Arenicola and
Abarenicola were correlated with temperature, with the 10 °C and 20 °C surface-water isotherms constituting the
most effective barriers for species distribution. Nevertheless, a latitudinal dine of the reproductive period is
observed from cold to tropical waters. O. fusiformis shows an absence of sexual reproduction in Disko Bay where
the species is at its northern limit of distribution forming probably a pseudo-population (Curtis, 1977).
In the English Channel and North Sea, the species shows a spring and summer spawning and recruitment. In
the "Golfe du Lion" and Arcachon Bay a winter spawning and recruitment occurred when llie sea bottom
temperatures were above 12 °C. Recruitment occured throughout the year in Florida (Key Biscayne) where the
water temperature ranged between 23 °C and 28 °C (Me Nulty & Lopez, 1969). This showed that O. fusiformis
adapts its reproductive strategy to a very broad temperature scale.
The rate of endemism described in some regions (Hartman, 1955) should become less as soon as the
distribution of some of the species is better known (Kirkegaard. 1969). The Polychacta arc generally ancient and
394
J.-C. DAUVIN & E. TIIIEBAUT
seem to be very conservative (I-Iolthe, 1978), which should explain the wide geographical distribution of some
species (Fauchald, 1984). Cosmopolitan distribution is known for several species of Polychaeta. Nevertheless,
three cases of cosmopolitism can be defined: 1) true cosmopolitan distribution: the distribution of a species is
really world wide as is 0. fusiformis ; 2) die species is distributed world wide but sibling species have been
demonstrated: e.g. Capitella capitata (Grasslh & GRASSLE, 1976): or 3) several species have been confused under
the same name: e.g. Terebellides stroemi which was divided into five species after a morphological study of
specimens from several geographical areas (Williams, 1984) or Spio filicornis which was used for several species
of Spio (Dauvin, 1989). Finally, the number of cosmopolitan species could be overestimated (Biiaud, 1982).
This is due to three principal causes: 1) the absence of adequate identificatory keys for many parts of the world, 2)
tiie frequent identification of polychaetes by benthic ecologists doing identification work strictly from need, and 3)
die poor description of many species (Fauchald, 1984).
Recent taxonomic studies of Australian material have revealed in many cases that the species previously
identified as die cosmopolitan species Lanice conc/iilega (Pallas, 1766) and Eupolymnia nebulosa (Montagu, 1818)
were in fact new species (HUTCHINGS & Glasby, 1988). Moreover Australia is known to have a high speciation
nite.
No relationship between the type of development and die range of the distribution of a species has been note
(Biiaud, 1982. 1984). Larval stages of certain species could play a role in dispersion (Bhaud, 1982). The main
explanation for a wide distribution seems to be die specific responses to physico-chemical, especially temperature
conditions (Biiaud, 1982; Golikov et a /., 1990). Within the entire distributional area of a species there exists a
distinct interrelation between the genetically determined requirements of its individuals and the environment. The
distribuuonal pattern indicates a certain unity between the species and its environment, and Golikov et cil. (1990)
suggested the term "ecogenocomplex" for this kind of relationship.
From the data set collected in this work, 0. fusiformis seems to be a true cosmopolitan! species. Since its
description by DELLE Chiaje (1841), several authors have described different species of Owenia or, suggested die
existence of races of 0. fusiformis (CaULLERY, 1944; Thomassin & Picard, 1972) by some morphological
characters such as the presence of a dioracic collar, die number of segments, the shape of uncini, the length of
thoracic setae. However, the morphological and physiological characters used seem to be the result of an
interindividual variability and do not permit to separation widiout ambiguity distinct species. Therefore, most of
Owenia species described since Delle Chiaje have later been considered as a junior synonym of 0. fusiformis. It
is clear that now, as in the past, the macroscopic and microscopic observations or comparison* of morphological
characters alone are insufficient to distinguish some possible distinct species of 0. fusiformis.
In the future, it should be necessary to study Owenia with biological and molecular points of view to define its
status. Studies must be developed on: 1) the variability and adaptations of reproductive strategy in relation to
latitude including extreme conditions as the Arctic and tropical seas; 2) enzymatic and mtDNA polymorphism. For
example, Grassle & GRASSLE (1976) showed that sibling Capitella species with slight morphological differences,
and close life histories could be distinguished by genetical characters.
ACKNOWLEDGEMENTS
The authors would like to thank their colleagues for loan of specimens deposited in their collections: Dr
K. Fauchald and L. Ward, Smithsonian Institution, Washington, Dr M.C. Gambi. Stazione Zoologica,
Naples, L.H. Harris, Natural History Museum of Los Angeles County, Dr G. Hartmann-Schrodei^.
Zoologisches Museum, Hamburg, and Dr P. HUTCHINGS, Australian Museum, Sydney. We are also grateful to
P. GlLLET for access to the library of the Catholic University of Angers and Drs M. Biiaud, K. Fauchald and
D. REISH for their very constructive suggestions on the first draft
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Source : MNHN. Paris
42
Light influence on larval emission and vertical swimming
in the terebellid worm
Eupolymnia nebulosa (Montagu, 1818)
Jean-Claude DUCHENE & Christian NO'ZAIS
Observatoire Oceanologiquc de Banyuls
Laboratoire Arago
F-66650 Banyuls-sur-mer, France
ABSTRACT
I he reproduction of a population of the terebellid worm, Eupolymnia nebulosa. was studied at the Arago Marine
Laboratory in the western Mediterranean. As many as four spawnings occur from early March to mid June. Eggs are released
within jelly masses, counted and collected from a 30 m2 area at various times. Larval outputs from the egg masses were
observed. 1 he corresponding swimming activity of the trochophores was measured by mean of an actographic device. The
apparatus developed for that purpose allowed fast localisation of sets of up to 400 larvae on a motionless area, or tracking of a
single larva by means of computer driven video camera located on translators. The real time video tracking of the swimming
larvae allowed precise spatial localisation within gradients. The influence of light was tested on early larvae. Cocoons were
analysed in normal and controlled conditions, in order to quantify the number of emerging larvae at different temperatures and
growth rates. Larval growth increased with temperature. The larval output from the jelly masses was faster at lower
temperatures and high density of larvae within the cocoon. The larval output was closely related to light, increasing the larval
swim : most of the larvae were emitted in the plankton during day light. Observations indicated large differences between the
lour spawnings with implications lor recruitment. The first spawning period with lower temperatures, a high phototropy and
highei swimming rate ol the trochophores resulted in wide larval dissemination. The remaining spawnings, with lower egg
density, a higher temperature associated with a faster growth rale, lower swimming activity and longer retention within the
cocoon, ensured a good local recruitment.
RESUME
Influence de la lumiere sur remission ct la nage verticale des larves chcz le terebcllide Eupolymnia nebulosa
(Montagu 1818)
Cette etude concerne la reproduction d'une population d 'Eupolymnia nebulosa , Annelide Tercbellidae, silucc en face du
laboratoire Arago. en Mediterranee occidentale. La periode de ponlc setend de mars a juin. avee quatre pics. Les oeufs sont
pondus dans des cocons muqueux. qui sont recueillis et comptes a diverses periodes sur unc surface de reference de 30 m2.
L emission Iarvaire a parlir de ces cocons est eludiec. L'activite de nage des trochophores rccueillies est mesuree a 1’aide d'un
systeme actographique, developpe dans ce but. Ce systeme permet les enregistrements rapidcs des positions d’un maximum de
400 larves dans un nuage sur un champ lixe. ou le suivi en temps reel d'un seul individu au moyen de cameras video fixees
DUCHL-.NI*. J.C. & C. Nozais, 1994. — Light influence on larval emission and vertical swimming in the terebellid worm
Eupolymnia nebulosa (Montagu. 1818). In. J.-C. Dauvin, L. LaUBIER & D.J. Reish (Eds). Actes de la 4eme Conference
internationale des Polychetes. A lent Mus. natn. Hist. nat.. 162 : 405-412. Paris ISBN 2-85653-214-4
Source : MNHN. Paris
406
J.-C. DUCHfiNE & C. NOZAIS
sur des translatcurs pilotes par un ordinatcur. Lcs cnregislremenls en temps reel des larves permettent un position nemenl precis
des larves dans des series de gradients avec estimation de leur vitesse de nage. L'influence dc la lumiere a etc testee sur les
jeunes larves emiscs a par tir des cocons, maintenus en conditions controlecs, de maniere a apprecicr lc nombre dc larves
cmises dans le temps. La croissance larvaire s’accroit avec la temperature. La sortie des larves hors des cocons cst plus rapide
aux basses temperatures ct pour des hautes densites larvaires a l’intcricur des cocons. L emission larvaire est liee a la lumiere.
qui augmenlc l'activite de nage des Lrochophores et provoque une sortie maximale durant la phase eclairee. Les implications
des 4 pontes sur lc recrutcmenl sont ties differences : la premiere periode de ponte, lorsque les temperatures sont basses, la
photolropie elevee ct lc comportement natatoire des larves tres actif. favorise une large dissemination. Les pontes suivantes. qui
pr^sentent une densite d'ceufs plus faible. une temperature plus elevee associee a un taux dc croissance superieur, une activite
de nage plus faible et une retention accrue au sein des cocons muqueux. favorisent quant a elles un bon recrutement local.
INTRODUCTION
I he reproductive trends of the polychaete Eupolymnia nebulosa has been studied for several years in front of
the Arago marine laboratory in Banyuls on the western Mediterranean. Personal field observations made by scuba
diving revealed that synchronous spawning occurred. On a small submarine cliff, diver observations showed that
cocoon production starts at night and lasts until the following week. There were up to four spawning peaks from
early March to earlv June. Records are known for a breeding-ground in front of the laboratory, but concerned only
the number of cocoons (Gr£mare, 1988; BHAUD & GrEmare, 1988; DucufiNE & Nozais, 1992). Larval
settlement was analysed in laboratory experiments involving types of sediment and settling in a hydrodynamic
flume (Bhaud, 1991; Chia & Bhaud . 1991). Observations were made in order to estimate the quantity of larvae
present over the sediment (Duch£ne & Nozais, 1992). It appeared that the larval development was highly
dependent on external parameters such as temperature (DuCHfiNE, 1982). This modified larval growth and the lime
when larvae arc released from die protective cocoon. Cocoons having different eggs densities were found during
die spawning period (DuCHfiNE & NOZAIS, 1992). The first peaks, in March, involve dense cocoons with up to
30,000 eggs. In late May, the mean number of eggs per cocoon had fallen to about 3,500 eggs. The larval density
within the cocoon seems to have an influence on die larval release by modifying the structure of die jelly mass. A
closer look indicated that larval output from the protective cocoons occured only at certain times of die day. Light
appears to be an important synchronising factor for the larval release from the protective cocoon. In order to
estimate the influence of the light on larval swimming and behaviour, we developed an actographic device which
was able to quantify the displacement of larvae in aquaria widi a precision of some microns. The small si/e of the
young Eupolymnia larvae led us to adapt the recording system. This involved the use of a small video camera with
a magnifying lens mounted on a set of translators allowing large displacement. The field sampled by this camera is
very small and compensated by the displacement of the 10 pm precision translators. The only way to automatize
diis apparatus was to perform a real time analysis on a computer. The camera is then moved by the computer in
order to follow the larval displacement.
MATERIAL AND METHODS
Eupolymnia nebulosa larvae are released in the plankton from protective cocoons. The age of every cocoon
studied is known from quadrat recordings on the coast in front of die laboratory. The cocoons were gently
collected by diver from the rocks from a depth of one meter or less. Each cocoon was isolated in a tank with
controlled temperature and light. All the larvae swimming in the tanks were collected and counted every four
hours. Individuals were then used for measurement of swimming speed and displacements in controlled light
conditions. External recordings of light intensity were used to adapt the controlled light conditions in the tanks.
The age of all larvae used in die measurements was known widi a precision of four hours for the March
experiments and 12 hours for the other experiments. Larval observations were made within horizontal and vertical
tanks. The horizontal tanks were small sized black coaled containers with a 6 mm water layer : larvae tire attracted
by a lateral light source in a non-coaled area and when Uicy stop swimming diey remain on die bottom of the tank.
The vertical tanks were aquaria of various sizes, die most commonly used was 10 x 20 x 40 cm in height.
A set of equipment has been used in diis study for locating and counting the young larvae as soon as diey are
liberated from die mucous cocoon (Fig. 1). Besides the delayed observations realised widi the digitizing tablet and
the video tape recorder, a real time computer based recording system has been developed in order to achieve a
Source : MNHN, Paris
LIGHT INFLUENCE ON LARVAL EMISSION IN A TEREBELLID
407
nearly automatic record of larvae locations within an aquarium. This system is presented on the upper right side of
figure 1.
Fig. 1 . Actographic device used for larval displacement measures. Delayed records are made with a video camera connected
to U-Matic tape-recorder and with a 16 mm movie camera with intervallometre in order to obtain various recording speeds.
The treatment involves a set of digitizers. The real time recordings are made by a computer driven system with video
cameras attached on translators allowing size independant measurements (with various optical devices). In the present
analysis the size of Eupolymnia larvae was between 100 and 220 pm. Motionless measurement of up to 400 larvae or
tracking of a single larva over a 1 m distance (length of the longer 12.5 microns precision translator) is possible with the
home made software. The real lime measurements allow shape extraction and treatment of 4 to 12 frames per second.
A video camera was attached on a X-Y translator driven by step motors. A second camera was mounted at a
right angle on the same support to provide depth indications. The step motor translator (CharlyRobot™) allows
displacement of video cameras with 12.5 |im steps. Twenty four frames per second are sent to a video digitizer
board (MCB™ from Lumiere Technology) connected to a micro-computer (Apple Macintosh Ilex). A program
was developed to insure the video signal analysis. It used MPW- Pascal and MPW-C for the program shell and
specific machine language routines (using MPW-Asm) for fast computing related to video acquisition. This
resulted in the storage and computation of a pixel matrix followed by the saving of larval location information on
text files usable by standard spread sheet programs. The program drives die translators and computes relative
displacements. The recording/computing process allowed a mean speed of about 4-12 frames. s_1, depending on
the type of recording.
Two different modes were tested during larval analysis :
- a "cloud" analysis of a set of up to 400 larvae (generally we used 50 larvae) with recordings of die analysed
video field every tenth of a second. In this case the computer system is used like die standard tape recording video
408
J.-C. DUCHfiNE & C. NOZAIS
analysis systems with a real time analysis instead of a delayed study of die shapes. We used a motionless camera
mode for the study (the barycenter of the larval group may be calculated with associated camera translation). This
allowed us to make precise estimations of the light conditions for every place in the video field.
- a single individual tracking, with long displacements (the larger translator allows a maximum displacement
of 1,020 mm). When the larva was about to quit a control area, the computer sends indications to the electronic
board controlling the camera translators. The shape is then brought back to the centre of the survey zone and its
displacement is taken into account.
Irradiances used in the experiments remain within the range observed in the field (maximum of 9 x 1016
Q. cm'2 s'1 at a 20 cm depth). We selected a range corresponding to the transition observed from positive to
negative phototaxic response (1 to 1.8 x 1016 Q. cm -, s'1).
RESULTS
The larval output from the protective cocoons begins early in March mid ends in late May. Observations on the
number of larvae swimming out of the protective egg mass indicated a diurnal emission : the maximum number of
larvae emerging from the cocoons occurred between 10 AM and 6 PM (Fig. 2).
Time in hours
Fig. 2. Number of larvae swimming out of the protective cocoon at different hours of the day. The cocoons arc empty after 8
days. The presented percentages are summed up for every class of time and for 3 different egg masses in March 91. The
main larval output occurs between 10h30and 18h30.
Clear photoposilivc reaction was measured in die first free swimming stages: all the individuals between three
and 10 days were found close to die light source within a few minutes. The swimming speed of the three day old
larvae increased with light intensity. The four day old larvae swim actively toward the light source and remain
1.0 mm from the surface. The photopositivity decreased with age: the 10 day old larvae were found in a 5 mm
layer below the surface.
I he swimming behaviour of E. nebulosa larvae consists of short periods of fast swimming towards die light
source and long, scattered periods of rest or slow motion. As shown in Table 1, 24 % of the swimming of a three
day old larva is directed toward the light with an average speed of 0.982 mm. s->, and 76 % of the displacement
are active sinking periods with a slow upward motion compensating passive sinking, resulting in a downward
movement with a mean speed ot 0.35 mm. s_I . This is demonstrated by records of anaesthetized larvae presenting
a downward displacement with values ranging from 1.3 to 1 .7 mm. s_L
Observations were made to find the illumination corresponding to a general switch from photopositive to
negative displacement in a light gradient (Fig. 3). For the observations made in the vertical tanks, the negative
displacements consisted in a reduction of Hie active upward swimming phases, resulting in semi-passive sinking.
Source : MNHN. Paris
LIGHT INFLUENCE ON LARVAL EMISSION IN A TEREBELLID
409
In horizontal tanks movements were active in both directions. The illumination level did not change during the
Table 1 . — Swimming speed of Eupolymnia nebuloso larvae of different ages. The range and the mean of the upward and
downward speeds of non anaesthetized animals are given, for the variations are important depending on the intensity of the
light. The 95 % confidence interval is shown for anaesthetized individuals. Numbers of measures is 4,275 for 3-4 days
larvae, 1.023 for 7 days larvae, 502 for anaesthetized 4 days larvae, and 184 for anaesthetized 7 days larvae.
resting phase, because of the larval settling on the bottom of die tank. The larvae had to swim actively away from
die light source. The scale differences in the net displacements, in figure 3, reflect this major difference: a
reduction in swimming in a vertical lank results in sinking (negative speed in the gradient) when the same
reduction in die horizontal tank may result in a settling, with a null speed.
95% Error Bars A
1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 1 .8.1 01 6 2.4.1016 3.1016
Light Intensity (Q.cnA r»).10^ Light Intensity (Q.cm-.s*1)
FIG. 3. Measurements on larval swimming as a function of light intensity in vertical ( A and C) and horizontal (B and D)
tanks. Net displacements correspond to the mean displacement of a set of several larvae for 2 different ages ( A-B: 4 day old
larvae; C-D: 7 day old larvae). The grey line corresponds to neutral buoyancy. N represents the number of larvae used for
the 95 % confidence interval.
410
J.-C. DUCHfiNE & C. NOZAIS
From figure 3 it appears that the switch from positive to negative swimming occurs for light intensities ranging
from 1 to 2 x 1016 Q.cnr2. s'1. Lower illuminations always correspond to sinking, higher illuminations to upward
swimming. The differences between four day and seven day old larvae depended on the position and the pattern of
the inversion: older larvae needed a stronger stimulus to increase their swimming rate. The maximum mean speed
toward the stimulus, computed by considering only the positive displacements is :
- 1.34± 0,09 mm. s-' for an illumination of 1.6 x 1016 Q. cm’2, s'1 for4 day old larvae:
- 1.17± 0,04 mm. s-> for an illumination of 1.4 x 1016 Q. cnr2. s'1 for 7 day old larvae.
The net displacement is not only related to the mean speed of movement toward the light source but also to the
swimming/rest ratio. The data in figure 3 suggest that this ratio increased with the intensity of the stimulus and
reached higher values for older larvae at higher light intensities, in the vertical tanks the records concerning larvae
remaining close to the surface have been eliminated.
DISCUSSION AND CONCLUSIONS
Studies involving terebellid polychaeles revealed the importance of early protection during the first
developmental stages within egg masses. The positive phototropic response of trochophores of Eupolymnia in first
stages increased the dispersion of larvae by causing them to swim toward the surface. This had been observed with
the subantarctic polychaete, Thelepus extensus (DucHfcNE, 1982). In both cases the first free swimming stages
emerging from the cocoon were usually strongly sensitive to light. Larvae may change their response toward
specific physical parameters during their planktonic life. A late negative phototropy was found in many cases
which lead to increased settling on the benthos.
When the larvae were released to the plankton they can remain in a free swimming period for varying lengths
depending upon the environmental conditions and the specific abilities of the larvae. These terebellid trochophores
have lecithotrophic development and may be present in the plankton as long as 2-3 days, however, the settling
trials start shortly after die release from die egg mass. Local modifications may be found: it seems likely that die
early Thelepus extensus larvae released from the outer parts of the cocoon stay within the plankton for a longer
time than the inner larvae (personal observations, in Kerguelen Archipelago). These later ones continue their
development within die spherical chambers inside the cocoon and the free swimming stage is then reduced. Larvae
are likely to slay for a longer or shorter time in the plankton depending on the positional the cocoon. Eupolymnia
larval densities inside the jelly masses appear to modify the emission patterns (Duch£ne & Nozais, 1992). There
is also a possible relationship between physical parameters and vitellogenesis. Differences in die number of eggs
per spawn are important. The number of eggs in the cocoons is high during the first spawning period in March
when the water temperature is low and die larval growth slow. A high proportion of young stages is emitted to die
plankton. At dial period only a part of the oocyte production is spawned. The physical size of die mucous cocoon
may be involved in this limitation together with the state of oocyte maturation. An active selection of large-sized
oocytes is made by die ciliated nephrostome. The smaller oocytes remain widiin the coelom. Selection is probably
achieved by a mechanism which detects the shape of spherical mature oocytes within the coelomic cavity as
opposed to immature ones which are flattened.
Numerous attempts to measure animal displacements have been made including real time analysis systems
(ROONEY & Cobb, 1991; Bakchine-Huber et a I ., 1992; Boisclair, 1992). The real time device with robotized
cameras used in this study allows flexible analysis of larval movements on large surfaces. Planktonic larvae are
often swimming rather fast with spiral, undulating direction components, making the precise localisation difficult.
The analysis of response to physical stimuli is dierefore complex, due to (he inherent complexity of the normal
larval displacement. A spiral swimming movement may be distorted by a response to positive light influence. The
general trend will be a displacement toward the light emission. In that particular case (stimulus easy to localize
and to interpret) the correlation is simple and die observer is able to describe die overall larval response. With
odier stimuli such as salinity, temperature gradients or sediment attraction, identification of the source of die larval
displacement is difficult to make and developmental stage must be taken into consideration.
To determine the relationship between hydrodynamics and the movement of larvae, the abilities of some
invertebrate larvae to move horizontally or vertically have been investigated by Konstantinova (1966, 1969),
Mileikovsky (1973) andCHlA et al (1984); but swimming direction was not always specified. More recently
Butman et al. (1988) measured swimming speeds and sinking velocities of two sibling species of Capitella. Their
swimming speed varied between 2 and 4 mm. s"1. Horizontal movements of huge amplitude or the transportations
of long duration seem to be die characteristic of ciliated larvae endowed with efficient trochae. This is found in the
Source :
LIGH T INFLUENCE ON LARVAL EMISSION IN A TEREBELLID
411
larvae of Nephtyidae, Spionidae or Chaetopteridae (Cazaux, 1981). The use of parapodia is found in the
nectochaetes of Aphroditidae. Nectosomcs of Poecilochaetidae move by snake-like undulating movements
(Bhaud & Cazaux, 1988). Larvae without swimming apparatus or reduced cilia, for example Orbiniidae,
Lumbrineridae. do not possess the ability to rise in the water column and are observed rarely in planktonic
samples. However, some species such as Lattice conchilega with aulophore larvae lack a swimming device and
are collected in large numbers in die water column.
Observations on larval motion appear to be of interest when dissemination and settling considerations are
analyzed. If large-scale dispersal of planktonic larvae is determined mainly by oceanic circulation (SCHELTEMA,
1971; Palmer, 1988), larval behaviour may influence settling probability at very small spatial scales (CRISP,
1974; ECKMAN, 1983). The larval swimming speed is generally too low in comparison with currents to have an
effect on horizontal movements. As pointed out by Chia et al. (1984) larval swimming may however influence the
vertical migrations. Vertical distribution is likely to be controlled by vertical motions except when stratification
exists (Mileikovsky, 1973). Thorson (1964) proposed vertical movements could be die result of ontogenic
changes in photoresponse which appear sometimes during larval life. Those predictions have been confirmed by
laboratory observations (Marsden, 1984, 1986, 1990), field observations (YOUNG & Cm A, 1982a. b) and
correlated data (FORWARD et al. , 1984). Many studies show that light strongly influences larval behaviour
(Forward & Costlow. 1974; Via & Forward, 1975).
The larval emission recorded in these experiments shows that the release in the plankton of more than 90% of the
Light intensity necessary to switch from positive to negauve motion appears to be located in a rather narrow
range for die young E. nebulosa studied in diis set of experiments (4-7 days old). The response to a light stimulus
corresponds to an increase of die swimming speed with a posiuve/negative heading and to a modification of the
larval behaviour (rest/swim ratio or settling tendency/light stimulation constraint). In March, response to light
induces upward swimming proportional to the intensity of the stimulus. In this case, the light stimulus seems to
increase the dissemination phase (first spawning). Later in the season, when natural light intensity increases, the
larvae are emitted in the plankton in lower densities and at a later developmental stage, resulting in a reduced
photosensitivity and a reduced swimming phase. The positive displacement of seven day old stages at high
illumination levels is still possible, but most these stages arc usually found within the jelly masses. In die bay
facing the marine laboratory in Banyuls, rotary motion currents allow planktonic larval retention over precise
areas. The continuous current speed observations indicate clearly that the larvae are unable to swim against the
current flow. On the contrary, die vertical motions observed indicate clearly a possible vertical displacement from
the shallow water sediment, where the larvae are emitted to die surface and back. The vertical structure of the
water masses shows a clear and rather constant reversal of the current direction depending on the depth
(DuCHfiNE, 1994, in prep.). In these conditions a short vertical migration may induce a complete reversal in
passive transportation by the currents. The vertical swimming observed in the Eupolymnia larvae is sufficient to
allow this transition from an out of the bay to an inward motion.
ACKNOWLEDGEMENTS
This study is a contribution to die French National Program on the Determinism of Recruitment by a grant
conceded to the Laboratory.
REFERENCES
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exploratory behavior of small animals. Naturwissenschafien . 79 : 39-42.
Bhaud M., 1991. Larval release from the egg mass and settlement of Eupolymnia nebulosa (Polychaeta. Terebcllidae).
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Bhaud, M. & C. Cazaux. 1988. — Description and identification of Polychaele larvae; their implications in current
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BHAUD, M.. GrEmare A.. 1988. Larval development of the terebellid Polychaete Eupolymnia nebulosa (Montagu. 1818)
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BoiSCLAIR. D., 1992. — An evaluation of the stereocinematographic method to estimate fish swimming speed. Can. J. Fish.
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Bitman. C.A.. GraSSLE, J.P., BUSKEV. E.J.. 1988. — Horizontal swimming and gravitational sinking of Capitella capital a
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Cazaux. C.. 1981 . — Evolution el adaptation larvaires chez les Polychetes. Oceanis, 7 : 43-77.
Cha. J.H.. Biiaud, M., 1991. Etude experimentale du recrutcment henthique en canal hydrodynamique el en milieu calme.
C.R. Acad. Sci.. 312 Ser.3 : 1 13-1 18.
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Crisp. D.J.. 1974. Factors influencing the settlement of marine invertebrate larvae. In: P.T. Grant & A.M. Mackik (eds).
Chemoreception in marine organisms. Academic Press. 1974.
DuCHfcNH, J.C., 1982. — Pjude c.omparee de la biologie d Amud ides Polychdtes consid trees en differentes zones climatiques.
These de Doctoral d'Elat. es Sci. Nat., Univ. P. & M. Curie, 1-315 pp.
DuciiEne J.C.. Nozais, CM.. 1992. - Etude de remission dcs stades larvaires precoces d 'Eupolymnia nebulosa (Polychacta :
Terebellidae). Annales Inst. Oceanogr.. 68 : 15-24.
ECKMAN. J.E., 1983. — Hydrodynamic processes affecting benthic recruitment. Limnol. Oceanogr.. 28 : 241-257.
FORWARD. R.B.. Jr.. Costlow. J.D.. Jr.. 1974. The ontogeny of phototaxis by larvae of the crab Rhithropanopeus harrisii.
Mar. Biol.. 26 : 27-33.
Forward. R.B., Jr., CRONIN. T.W., STEARNS. D.E.. 1984. Control of diel vertical migration: Photoresponses of a larval
crustacean. Limnol. Oceanogr., 29 : 146-154.
Gr liMARE, A.. 1988. Aspects quantitatifs de la reproduction c/tez quelques Annelides Polychetes : In tt rets et perspectives.
These Doctoral d’Elat. Univ. P. & M. Curie. 218 pp.
Konstantinova, M.I.. 1966. — Characteristic movement of pelagic larvae of marine invertebrates. Dokl. Akad. Nattk. SSSR.
170 : 726-729.
Konstantinova. M.I.. 1969. Movement of polychaete larvae. Dokl. Akad. Nauk. SSSR. 188 : 942-945.
MARS DEN, J.R.. 1984. Swimming in response to light by larvae of the tropical serpulid Spirobranchus giganteus. Mar.
Biol, 83 : 13-16.
MaRSDEN, J.R.. 1986. — Response to light by trochophore larvae of Spirobranchus giganteus. Mar. Biol., 93 : 13-16.
MARSDEN. J.R.. 1990. - Light responses of the planktotrophic larva of the serpulid polychaete Spirobranchus polvcerus..
Mar. Ecol. Prog. Ser.. 58 : 225-233.
MILEIKOVSKI. S.A.. 1973. - Speed of active movement of pelagic larvae of marine bottom invertebrates and their ability to
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PALMER. M.A.. 1988. Dispersal of marine meiofauna: a review and conceptual model explaining passive transport and
active emergence with implications for recruitment. Mar. Ecol. Prog. Ser .. 48 : 81-91.
Rooney. P.. Cobb. J.S.. 1991. Effects of time of day, water temperature, and water velocity on swimming by postlarvae of
the American Lobster, Homarus americanus. Can. J. Fish. Aquat. Sci.. 48 : 1944-1950.
SCHELTEMA, R.S.. 1971. Larval dispersal as a means ol genetic exchange between geographically separated populations of
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Via. S.E.. Forward. JR.. R.B., 1975. — The ontogeny and spectral sensitivity of polarotaxis in larvae of the crab
Rhinthropanopeus harrisi (Gould). Biol. Bull.. 149 : 251-266.
YOUNG . C M.. Chia, F-S.. 1982a. Ontogeny of phototaxis during larval development of the sedentary polychaete. Serpula
vermicularis (L.). Biol. Bull.. 162 : 457-468.
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Source : MNHN. Paris
43
Polychaeta of the German Bight
from the 1987 cruise of the R/V "Senckenberg"
Dieter FIEGE* & M. Nechana BEN-ELIAHU **
*Forschungsinstitut Senckenberg, Sektion Marine Evertebraten II
Senckenberganlage 25 D-6000 Frankfurt/M., Germany
**The Life Sciences Collections. The Hebrew University of Jerusalem
91904 Jerusalem, Israel
ABSTRACT
The present paper reports on the collections of Polychaeta of the 1987 cruise to the German Bight. "DEB 1987".
Fifty-one samples from 25 stations covering a depth range from 14 to 46 m were analyzed. The samples contained about
1,500 polychaetes in 46 genera in 29 families. Altogether, 67 separate taxa were determined, of which 63 were identified
to species. As many as 26 species per sample were found. The distribution of species in the samples is discussed.
RESUME
Polychetcs de la grande baie allcmande recoltees par le R/V "Senckenberg" an cours de la
campagne de 1987
Dans cette note les resultats des recoltes dcs polychetes de (’expedition 1987 dans le golfe allemand, "DEB 1987".
sont presentes. Cinquanle et un echantillons provenant de 25 stations, dont les profondeurs varient entre 14 ct 46 m. ont
etc analyses. Les echantillons contenaient environ 1500 polychetcs apparlenant a 46 genres de 29 families. Soixante
sept especes ont ete distinguees, dont 63 ont pu etre determinees. On a trouve jusqu'a 26 especes par echantillon. La
distribution des especes dans les echantillons est discutec.
INTRODUCTION
Benthic communities and species distribution in the North Sea have been studied by various authors (Stripp,
1969; Stripp & Gerlach, 1969; GlEmarEC, 1973: McIntyre, 197S; Rachor & CiERLACH, 1978;
Ziegelmeier. 1978; Salzwedel et al.. 1985; Basford et al.. 1989; Frauenheim et al. , 1989; KCnitzer.
1990). Investigations with special emphasis on the distribution of Polychaeta in the area have been carried out by
MICHAELSF.N (1897), FRIEDRICH (1938). HARTMANN-SCHRODF.R & STRIPP (1968). and KIRKEGAARD (1969).
Piece, D. & M. N. BEN-EliaHU, 1994. — Polychaeta of the German Bight from the 1987 cruise of the R/V
"Senckenberg". In: J.-C. DaUVIN. L. LAUBIER & D.J. REISH (Eds). Actes de la 4eme Conference internalionale des
Polychetes. Mem . Mus. train. Hist, nai., 162 : 413-423. Paris ISBN 2-85653-214-4.
414
D. FIEGE & M. N. BEN-ELIAHU
The latter reviews the previous collections in tJie North Sea. Earlier investigations were often limited to particular
areas within the North Sea (Turkay, pers. comm.). The fauna of the northern North Sea is still poorly known in
regards to both in- and epifaunal benthic invertebrates (Basford et al. (1989).
" The Senckenberg Research Institute began a long-tenn study of epizoobenthos in the Nortli Sea in 1977 in
order to obtain a comprehensive view of the distribution of different taxa and to establish baseline data for
monitoring possible changes in the future.
Fifteen annual cruises have been carried out during summers to different areas within the North Sea. More than
200 stations have been sampled to date. The present paper reports on the collections of Polychaeta made during the
1987 expedition to the German Bight "DEB 1987".
FlG. 1. — Map of stations of the DEB 1987 expedition.
MATERIALS AND METHODS
The DEB 1987 sampling sites are given in Table 1 and Figure 1. The sampling was done with a van Veen grab
(0.2 m2), beam trawl (2 m wide, 1 cm mesh size in cod end), and ring dredge (1 m diameter, 1 cm mesh size).
Twenty-four, 21, and 6 samples, respectively, were taken with these samplers; three stations were sampled with all
three gear (Table 1). Trawling was usually carried out for 20 minutes at each station (except stn. 6 [21 '] and stn. 7
126']) at 1-2 knots after the gear had reached the bottom. An area of about 1 nautical mile length and 2 m width
was covered with each trawl. Samples were sieved through 0.63 mm mesh size and fixed in 10 % formaldehyde. In
tiie laboratory, polychaetes were determined to species level whenever possible (Table 2).
Faunistic attributes were analyzed separately for both types of samples. Van Veen grab samples arc more
comparable than beam trawl samples, since the beam trawl passes through different patches of the sea floor which
may obliterate differences between benthic assemblages. Therefore, only those samples taken with the grab were
considered here. We used the statistical package for comparing marine samples, PRIMER vcr. 3.1 (Gray et al. ,
Source :
POLYCHAETA OF II IE GERMAN BIGHT
415
1988; MED POL, 1992a, b), to compute the following univariate indices: N (the number of individuals in the
sample), S species richness (the number of species^ in a sample), H' species diversity (the Shannon-Wiener
information index computed to the base e), and J' the evenness corollary of the Shannon-Wiener index.
Table 1. — List of stations of North Sea expedition to German Bight DEB 1978
1/ Bt (beam trawl); vV (van Veen grab); Rd (ring dredge). 2/ According to information in FlGGE, 1981. +; gravel. -7
Ranked from 1-7 (class 7 with largest sand grain size 500-2000 pm; class 6 with largest sand grain size 500-2,000 pm
and also with smaller grains; class 5 with sand grain size 250-500 pm; class 4 with sand grain size 250-500 pm and
also with smaller grains; class 3 with sand grain size 63-250 pm; class 2 with sand grain size 63-250 pm and also with
5-10% clay; class 1 with sand grain size 63-250pm and also with 11-20% clay). 4/ Two samples. 5/ n.d.: no data
available, i. e., station not on sediment map.
A one-way analysis of variance (ANOVA) was done of S and IT against depth using die Statgraphics package
to test the hypothesis that faunal attributes reflect depth. The DEB 1987 sampling program did not encompass
replicate sampling; thus, for ANOVA, samples were sorted into four depth classes (I: 14-19 m, II: 20-29 m, III:
30-39 m, and IV: 40-46 m), regardless of their location. Members of a depth class served as "replicates".
To discriminate between samples on the basis of their faunislic attributes, we used die PRIMER package to
carry out hierarchical agglomerated classification based on die Bray-Curds similarity coefficient calculated on
square root transformed abundances, employing group average sorting (Gray el al ., 1988). An ordination analysis,
multidimensional scaling (MDS), which expresses the rank order of the dissimilarities was done based on the
ranked Bray-Curds similarity matrix and plotted with die superimposed scaled environmental variables of depth and
substrate type (MED POL, 1992a, b; Gray el al ., 1992). Van Veen samples 3 and 5 seemed to prevent other
samples from clustering, i.e. they arc "degenerate samples"; according to accepted practise diey were omitted from
the respective analyses (MED-POL, 1992a, b; M.R. Carr, pers. comm.). A 11011-paramctric analysis of variance
was used to compare die Bray-Curlis similarities with the depdi categories.
416
D. RKGE & M. N. BHN-liUAHU
Tabi.f. 2.— Dislribution of taxa in samples. All gears. N° of individuals taken for each depth category
(% of samples at each depth category containing species in question)
Source : MNHN. Paris
POLYCI IAETA OF 11 IE GERMAN BIGHT
417
Table 2 (continued)
^ vV = van Veen grab. Bt = beam trawl. Rd = ring dredge. ^ sensu I lARTMANN-SCHRODER (1971).
Source .
418
D. FIEGE & M. N. BEN-ELIAHU
Analysis of samples with respect to the sediment was done by cluster analysis. The information on substrate
grain size is from a map, "Sedimentverteilung in der Deutschcn Bucht" (FiGGE, 1981) (Table 1). Sediment was
divided into 7 classes ranked by decreasing size (for raw data and ranks see Table 1). A correlation between depth
and substrate classes was made.
RESULTS AND DISCUSSION
Polychaetes were analyzed from 51 samples taken at 25 stations and covered a depth range from 14 to 46 m.
There were about 1,500 specimens in 46 genera and 29 families. Sixty-seven species were determined of which 63
were identified to species (Table 2).
For analysis of depth distributions samples were arbitrarily grouped into four depth categories. Fourteen species
were present in the entire depth range, including the most frequently encountered species; these were, Scoloplos
armiger, Spiophanes bombyx and Ophelia limacina , which were present in >30 % of the samples; Nephtys
hombergii , N. caeca. N. longosetosa, Magelona mirabilis (presumably mistaken for M . papillicornis previously,
see JONES, 1977) and Chaetozone setosa , which were present in 20-30 % of the samples; Eumida sanguinea ,
Nepthys assimilis , Goniadella bobretzkii , Scolelepis bonnieri , which were present in 10-19 % of the samples.
Two species, Magelona type A and Diplocirrus glaucus, were present in all the deptli ranges sampled but present in
fewer than 10 % of the samples. Among the abundant species, Aphrodite aculeata and Pholoe minuta (>20 % of
the samples), were found only below the depth of 20 m; Hannothoe (Eunoe) nodosa , Pectinaria koreni and
Peciinaria auricoma (10-19 %) were found only below the depth of 30 m. Altogether, five species were found only
at depths less than 30 m (Pisione remota , Eteone longa , Eusyllis blomstrandi, Phyllodoce groenlandica ,
Dodecaceria concharum ), whereas 32 species were found only at depths greater than 30 m, with 29 of these present
only at depths greater than 40 m (Table 2).
Seventy-six percent of the species, i.e., 51, were found in fewer than 10 % of the samples and are thus
comparatively rare (Table 2). The six most abundant species were Autolytus edwarsi, Pholoe minuta , Scoloplos
armiger , Ophelia limacina , Spiophanes bombyx , and Magelona mirabilis. These comprised 8.9 % of all species.
The large species, Aphrodite aculeata , was also abundant in deeper waters with 78 individuals (Table 2). Fifteen
species (22.4 % of the total) were represented by 1 1-55 individuals. Eighteen species (26.9 %) were represented by
two individuals and 18 species (26.9 %) by only one.
Ziegelmeier (1978) found that about two-thirds of all polychaetes sampled belonged to Spiophanes bombyx ,
Magelona papillicornis , and Scoloplos armiger. Magelona papillicornis also was the most common species in the
study of Rachor & Gerlach (1978). Magelona papillicornis in both these studies was probably M. mirabilis (see
Jones, 1977).
Table 2 lists the gear used to collect the material. Most of the individuals of Aphrodite aculeata and some
additional polychaetes such as polynoids were taken with the beam trawl. Spiophanes bombyx was only collected
with the grab. The number of polychaete species per sample was 3 to 26 for the van Veen collections, 1 to 18 for
beam trawl collections, and 1 to 4 for the ring dredge collections (Table 3).
Comparison of the mean species richness S indicated an increase with increasing depth (7.2 ± 4.0 in depth
class I, 8.0 ± 4.6 in depth class II, 13.0 ± 6.6 in deptli class III, and 1 1.4 ± 6.3 in deptli class IV for the van Veen
grab samples). However, an ANOVA test, carried out with the data from the van Veen grabs found that the
difference in number of species with deptli was not statistically significant. The species diversity index, H', also
increased with depth (Table 3); while the ANOVA test for significance with IT calculation was higher than for S,
the difference between die depth classes with IT was not significant (p> 0.05; d.f. 3.47). The richest van Veen
sample was number 6 from a high fraction of clay at 46 m with 26 species and the highest species diversity
(H = 2.9) (Table 1). According to Hartmann-Schroder (1971), species found at this station cither prefer muddy
substrate or arc not known to have any substrate preference. Stripp (1969) and KUNITZER (1990) also found that
species richness, respectively number of individuals of macro- and meiofauna, increased from coarse to fine
sediment. Regarding only the van Veen collections of this study, those with the fewest species include stations 9
and 19 at a depth of 17-25 m (3-4 species each). These stations had the largest substrate grain size. However, there
were also stations with few species in deeper waters with fine grain size (stations 7 and 14, 41 and 42 m,
respectively). According to Ziegelmeier (1978) the poorest stations with lowest biomass were situated close to
the coast of Schleswig-Holstein, which he attributed to the fine to coarse sand, which is very mobile due to the
strong tidal currents in this area. Among die stations of the present study sampled with vV, 9, 10 and 1 1 are
aligned with 8°E along the coast of Schleswig-Holstein in quite shallow water. They belong to those with the
largest substrate grain size. Stations 9 and 11 show low species diversity (three and four species, respectively).
Source ; MNHN, Paris
POI ,YCHAETA OF HIE GERMAN BIGHT
419
Station 10 is also very shallow, and has the same substrate as the other two but shows a higher diversity (8
species). According to HARTMANN-SCHRODER (1971), species found at these stations either prefer sandy substrate
( Goniadella bobretzkii , Spiophanes bombyx , and Ophelia limacina ) or are not known to have any preference
(Nephtys caeca , N. longosetosa, and Scoloplos armiger).
Table 3. — Number of individuals (N), species richness (S),
species diversity (IT) and evenness (T) in individual samples.
Depth frequently correlates with substrate characteristics as indicated by THORSON (1957) and HYLLEBERG &
NATEEWATHANA (1984). We looked for indications that this might apply to the present material. First we
considered the relationship between the depth classes and substrate grain size and found them to be positively
correlated (r= 0.641, d.f. 20, p < 0.01). There was a significant relationship between the depth classes and the
ranked grain size classes (one way ANOVA, pcO.Ol. d.f. 3.18). Actually, there was very little difference
between the mean grain size ranks of the first two depth classes (5.8 ±1.3, 5.5 ± 2.4, 2.8 ±0.8, 2.1 ± 0.7).
Next we conducted a cluster analysis for faunistic similarity between samples. The dendrogram of the van Veen
samples (Fig. 2a), showed three clusters (marked A, B, and C). Cluster A comprises samples only from depth
category IV, cluster B comprises some samples from depth category IV and all the samples from depth category III,
while cluster C comprises all vV samples from depth categories II and I. The dendrogram thus broadly classifies
the samples according to the depth categories and, similarly, according to the substrate size. The corresponding 2-
dimensional ordination plots based on the Bray-Curtis similarities with superimposed depth (Fig. 2b) and substrate
grain size (Fig. 2c) show this clearly. An indication of the goodness of fit of the plot is given by its stress value
420
D. FIEGE & M. N. BEN-EIJAHU
(an expression of the defonnation necessary to transform die model from a 3-dimensional one to a 2-dimensional
one); the lowest stress value for the van Veen MDS plot was 0.172 (0.182. 0.218). Lower stress values (0.1)
would indicate a more accurate presentation of the samples (M.R. Carr, pets. comm.). Due to these somewhat
hi-'her stress values, we must conclude that the plots of the samples' Bray-Curtis similarity based on their faunal
attributes is a fair (rather than an excellent) representation, and it reflects the correspondence between the faumstic
attributes of the samples and their depth distributions ;ts well as die grain size parameters. The correspondence with
both these parameters is most obvious for cluster C - die shallowest samples with the coarsest grains - but also
holds true for cluster A widi the finest grain size (Fig. 2b-c). The non-parametric analysis of similarity vis a vis
depth for the van Veen samples showed significant differences (p < 0.05) only between samples less dian 20 m
deep and those deeper than 40 m. The fact diat the grain size data was obtained from a map. and not from analysis
of substrate collected with the samples must introduce error, the extent of which we cannot know. The impact of
any local sediment patchiness on die faunal attributes actually measured cannot be determined. Presumably, the
actual correspondence with substrate is better than that shown on the plot.
The van Veen samples contained 80.5 % of the 67 species collected by the expedition. The nature of the
samples themselves with as many as 50 % of the species represented by only one individual contributed to die low
similarities between samples (Fig. 2a). For greater significance, larger samples or replicate sampling with
similarities computed on the mean abundance data has been suggested (M.R. Carr, pers. comm.)
Among the common species, some occur in considerably higher numbers in certain samples than in the odiers
(Aphrodite aculeata, Pholoe minuta, Scoloplos armiger, Spiophanes bombyx, Mcigelona mirabilis, Ophelia
limacina) (Table 4). Station 6 was the richest in species and in number of individuals with both the van Veen and
the beam trawl samplers. At this station Autolytus edwarsi was found in large numbers, but it was not collected at
many stations (Table 4).
Table 4. — Species of DEB 1978 found in great number (% of individuals = % of Jill individuals
of this species taken at all stations)
Although die stations overlapped with some of those sampled by Hartmann-Schroder & Stripp (1968), it
is not possible to compare species composition and abundances between die two studies since a smaller sieve mesh
size was used by diem. Hartmann-SchrOder & Stripp (1968) included some meiobenthic species lacking in die
present study, which might have been lost because of the greater mesh size used here: Hesionura augeneri ,
Microphthalmus similis.M. listensis, Sphae rosy His hystrix.S. tetralix , but also Anaitides subulifera , Eumida
bahusiensis , E. punctifera , Polydora (Pseudopolydora) pule lira , and Tharyx marioni . Among the common species
mentioned by Hartmann-Schroder & Stripp (1968), Sthenelais limicola , Goniadelta bobretzkii, Scolelepis
bonnieri , Aonides paucibranchiata , and Ampharete fmmarchica were found in the present DEB sampling but in no
more than 7-16% of the samples.
Among the interesting species collected by the expedition, Lysilla loveni (DEB-stations 1, 2, 6, and 15) has
only been found twice earlier in the North Sea, i.c., off Oostende/Belgium (Channel) and close to the Norwegian
Trough (Hartmann-Schroder & Stripp, 1968). According to Michaelsen (1897), this species does not occur
in the North Sea proper, but in the Skagerrak, Kattegat, the Sound, and die Bells. HOLTHE (1985) showed a map
with the location of living specimens which were primarily from die Scandinavian coast. The type locality is
Bohuslan/ Sweden.
Source : MNHN, Paris
POI .YCHAETA OF THE GERMAN BIGHT
421
6 1 4 2 23 14 15 13 16 7 8 21 22 17 18 12 20 9 19 25 10 11 SAMPLE
46 43 43 44 43 42 41 40 38 41 31 30 36 33 29 25 18 17 25 19 16 14 DEPTH
FIG. 2. DEB 1987 van Veen samples (stations 3 and 5 omitted), a. Classification analysis of polychaete data from DEB
1987 expedition (square root-transformed data with Bray-Curtis dissimilarities). The sample numbers and
corresponding depths are shown on the abscissa, b and c. MDS ordination plot of the same data with grouping
showing clustering of samples based on species faunistic attributes and with superimposed corresponding scaled
environmental parameters, b: depth of samples. The shallowest samples with the shortest lines (cluster C); the
deepest samples (cluster A) with the longest lines, c: substrate grain size. The sediment was ranked into seven classes
(see Table 1). The largest circles (cluster C) represent the coarsest grain size.
Source : MNHN , Paris
422
D. FIEGE & M. N. BEN-ELIAIIU
In conclusion, the depth range sampled was sufficiently broad to identify differences in the distribution of some
species. The faunal attributes separated broadly both by depth and by substrate type. The selected depth categories
were found to comprise some mixture of the substrate categories. Since the German Bight is surrounded by rivers
which carry sediment, substrate categories are not only a simple matter of depth. In order to determine whether
depth or substrate is controlling the species attributes, it would be of interest to compare the classification of
samples according to their granulometry with that obtained from classifying by depth. However, this comparison
can only be done if the granulometry is determined from sediment collected with the sample. Since depth and
substrate grain size are highly correlated, it is difficult to distinguish which of these factors is the most important
one in controlling the distribution of the species. Moreover, some of the present differences may be artifacts which
could be eliminated by additional sampling.
ACKNOWLEGEMENTS
We thank M. TURKAY for the samples of Polychaeta, M.-L. Tritz (both of the Senckenbergmuseum,
Frankfurt) for processing die samples and skillful technical assistance, D. Eibye-Jacobsen and M.E. PETERSEN
(both of the Zoological Museum, Copenhagen) for taxonomic advice, as well as M.R. Carr (The Plymouth
Marine Laboratory) and E. Papathanassiou (The National Centre for Marine Research, Athens) for discussing
the data and for making the PRIMER software available. M.N. Ben-Eliahu thanks the Senckenberg Museum for
enabling a working visit to examine the collections, and the Marine and Coast Environment Division of the Israel
Department of the Environment for enabling participation in the FAO/IOC/UNEP Training Workshop MED POL-
Phase II on the Statistical Treatment and Interpretation of Marine Community Data at Bar Ilan University.
M. Turkay, II.J. Bromley. D. Gateno, mid R. Lotan read various drafts.
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FlGGE. K., 1981. Sedimentve rteilung in der Deutschen Bucht. 1: 250000 Karte Nr. 2900. Dt. Hydrogr. Inst.. Hamburg.
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FRIEDRICH. H.. 1938. — Die Tierwelt der Nord- und Osisee. Bd. V/b. Polychaeta. Akademische Verlagsgesellschaft.
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GlEmarec. M.. 1973. — The benthic communities of the European North Atlantic continental shelf. Oceanogr. Mar.
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Gray. J.S., Aschan, M., Carr, M.R.. Clarke, K.R., Green, R.H.. Pearson, T.. Rosenberg. R. & Warwick, R.M.,
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Gray, J.S., McIntyre, A.D. & STIRN, J., 1992. Manual of Methods in Aquatic Environment Research, part 11-
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Fischer Verlag. 594 pp.
H ARTMANN-SCHRODER, G. & STRIPP. K.. 1968. Beitriige zur Polychaetenfauna der Deutschen Bucht. Veroff Inst.
Meeresforsch. Bremerh., 11 : 1-24.
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Hylleberg. J. & Nateewathana. a.. 1984. Responses of polychaetes to monsoon and offshore mining associated
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on polychaetous annelids in memory of Dr. Olga Hartman. Allan Hancock Foundation, University of Southern
California, Los Angeles : 247-266.
Source : MNHN. Paris
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Source : MNHN. Paris
44
Selection des grains de sable selon leur nature
et leur forme par Sabellaria alveolata Linne
(Polychete, Sabellariide) lors de la reconstruction
experimentale de son tube
Yves CRUET* & Yves BODE UR**
Univcrsite de Nantes, 2 rue de la Houssiniere
44072 Nantes Cedex. France
* Laboratoire de Biologic Marine
** Laboratoire de Gcologie
RESUM fi
Bn laboratoire. le Polychete Sabellaria alveolata a la capacite de reconstruirc son tube casse a la condition de lui en
laisser une portion d'au moins 1 cm. Different* types de sediments, purs ou melanges, ont cte mis a la disposition de vers
isoles et cleves dans des conditions comparables. Les taux de reconstruction et les pourcentages des grains utilises ont etc
calcules. Les resultats montrent un net refus pour les fragments de monies (tres anguleux et allonges) ou encore pour les
micas plats et a bords tranchants. Les taux de reconstruction sont ties bas pour ces sediments. Au contraire les vers
reconstruisent vite. en presence de sables mixtes parmi lesquels ils choisissent d’abord les grains arrondis ou plus ou
moins ovoides de quartz et ensuite ceux de feldspath a la micromorphologie plus rugeuse. La forme et la
micromorphologie des grains et non leur nature mineralogique, semblent etre les facteurs decisifs pour un fort taux de
reconstruction.
ABSTRACT
Shape and coni positional selection of sand grains by Sabellaria alveolata Linnaeus
(Polychaeta, Sabellariidae) in the experimental reconstruction of the tube
Sabellaria alveolata can rebuild its broken tube under laboratory conditions providing there is a least one centimeter
present. Sand grains of different types were introduced into dishes containing worms. The rates of tube reconstruction and
the percentages of different grains used were calculated. Worms selected inore-or-less ovoid quartz or felspathic sand
grains and reconstructed their tubes rapidly. On the other hand, worms generally rejected those grains which were either
sharp edged mussel shell fragments or thin plated mica. If the worm accepted these latter grains, tube reconstruction rates
were low. The shape and the micromorphology of the sand grain seemed to be the deciding factor in selection for
reconstruction rather than the chemical nature of the sand grain.
CRUET, Y. & Y. Bodeur. 1994. Selection des grains de sable selon leur nature et leur forme par Sabellaria alveolata
Linne (Polychete sabellariide) lors de la reconstruction experimentale de son tube. In: J.-C. DAUVIN, L. LaUBIER &
D.J. REISH (Eds), Actes de la 4eme Conference internationale des Polychetes. Mem. Mas. natn. Hist. nat.. 162 : 425-
432. Paris ISBN 2-85653-214-4.
Source :
426
Y. GRUET&Y. BODEUR
INTRODUCTION
L'individu de Sabellaria alveolata (Linne), long de 1 k 3 cm, vit k l'interieur dun tube forme dc deux gaines
concentriques : l'une interne, uts mince, de nature organique, riche en soufre (Vovelle, 1965) ; I'autre exteme,
afenacee, de 2 it 5 mm dYpaisseur de paroi, 6^15 mm de dianfetre total, ct jusqu'St 50 k 70 cm de long. Les grains
de sable constituant lc tube exteme sont collects dans le milieu environnant au moyen de filaments buccaux
(ORRHAGE, 1978), puis tries et englu^s par un ciment organique (GRUET et til., 1987) au niveau de l'organe
constructeur. Get organe grossit au cours dc la croissance de l'animal, en meme temps que le dianfetre interne du
tube ainsi que la taille des grains de sable utilises (CRUET, 1984). 11 en r6sulte des tubes plus ou moins flexueux,
croissant verticalement en s'epaulant mutuellemcnt. Cela donne naissance k des colonies parfois trfes importantes
comme en baie du Mont-Saint-Michel (Gruet, 1986). Le tube afenace de l’esp^ce S. alveolata est constitute pour
l'essentiel de sables moyens (200 k 500 pm), moyennement classes, tr£s bioclastiques (Hommeril, 1962;
Gruet, 1982 ; Vovelle, 1965).
La question pos£c ici est de verifier experimenialement si le choix de l'animal, lors du processus de
construction, est influence par la nature mineralogique, done chimique, et surtout la forme des grains de sable.
MATERIEL ET METHODES
Preparation du matEriel EtudiE. - Des blocs de Sabellaria alveolata vivantes sont fecoltes au lieu-dit "les
Roches de la Fosse", k Noirmoutier (Vendee, France) et rapportes rapidement au laboratoire. Les tubes sont
deiicatcment separes les uns des autres. Puis, ils sont cassds transversalement dans leur portion terminale, dc
manure k ne laisser qu'une longueur de 10 mm (minimum) & 21 mm (maximum). Seuls sont conserves les plus
gros individus, non 16s6s au cours de cettc manipulation. Chaque animal est alors dispose k plat dans un
cristallisoir numerate. II est immerge dans 2 k 3 cm d' eau de mer de salinite identique (35 P.S.IJ.) k celle du lieu
d'origine des vers. Cette eau contient de la nourriture k base dune culture d'algues unicell ulaires. La non production
de feces etant un indice de mauvais etat de l'animal, ceux-ci seront alors eiimines et remplac6s avant le debut de
Texperimentation. L'eau contenant la nourriture est changec tous les jours apfes une mise k sec de 4 heures,
simulant une mar6e basse, mais non en phase avec le cycle lunaire.
- Une experience preliminaire (Gruet, 1982) permet d'apprecier l'effet de la temperature sur la vitesse de
reconstruction. Trois lots de quinze individus chacun ont 6t6 testes aux temperatures constantes (salles climatisees)
de 13 °C, 16 °C et 20 °C.
- Deux autres experiences ont et6 menees en 1988 et 1989, mais k la meme periode (mois de mars), dans lc
meme local, les memes recipients et selon le meme protocole experimental. Toutefois les conditions de
temperature n'etaient pas identiques : en 1988 (du 9 au 25 mars, soit 17 jours) la temperature de l'eau varie entre
12 °C et 16,5 °C ; en 1989 (du 1 1 au 25 mars, soit 14 jours) la temperature oscille entre 14,5 °C (minimum) et
18,5 °C (maximum) pour des mesures effectuecs vers 11 heures du matin. Or la temperature est un facteur
determinant pour la vitesse de reconstruction comme nous le montrons (Gruet, 1982) en experience preliminaire.
Chaque experience a porte, au depart, sur des lots de 20 individus en 1988 et de 15 en 1989. Les animaux morts en
cours d'experience sont cnleves et le nombre d’individus vivants est precise dims les tableaux ( Tableaux 1, 2).
Le sEdiment mis A la DISPOSITION des sabellaria (Tableau 3). — Les diffgrents sediments proposes aux
hermelles sont consumes de grains dune granulometric comprise entre 500 et 710 pm, ce qui correspond aux
valeurs modules des tailles de grains utilises dans la nature par des Sabellaria alveolata adultes dont le dianfetre
anterieur du tube oscille entre 2,3 mm et 3,5 mm (Gruet, 1984). Les different lots de sediment, composes
d’eiements de meme taille, different en revanche par la forme et la nature de ceux-ci :
- en 1982 : Texpgrierice preliminaire a ete menee avec le meme sable pour tous les individus. II est a priori trfcs
favorable car provenant de la desagregation de tubes. Sa nature est essentiellement quartzeuse avec quelques
fragments coquilliers.
- en 1988 : coquilles de moules (carbonate de calcium) cassees donnant des fragments allonges en aiguilles
ac6r6es (lot A’) ; sable de Loire compose de grains de quartz arrondis (61 %), de feldspaths sub-arrondis k anguleux
(23 %), de micas aplatis et tranchants (0,8 %), de fragments divers dont surtout des mingraux lourds (15 %) (lot
B') ; enfin un melange en proportions egales de fragments de moules et de sable de Loire (lot C') ;
- en 1989 : les memes sediments qu'en 1988 (moules : lot A ; sable de Loire : lot B) ; mais aussi un sable
composite (lot C) r6colt6 sur la plage dc Ploemeur (Morbihan) forme de quartz subarrondis (51 %), de feldspaths
Source :
SELECTION DES GRAINS DE SABLE PAR SABELLARIA ALVEOLATA
427
subarrondis k anguleux (32 %), de micas aplatis et k bords relativement iranchants ( 16 %) et de bioclastes arrondis
(1 %) ; un sable de plage de St-Gildas (L.-A.) (lot D) ; ce mcme sable mais "traite" (lot E) pour en arrondir les
grains. Ce sable us 6 par une longue agitation dans l'eau reste trfcs proche du precedent, mais les grains sont un peu
plus arrondis el emouss6s.
Tableau l. — Experience de mars 1988 (17 jours). Lots A’, B’ et C’. Longueurs moyennes des tubes reconstruits par les
Sabellaria en presence de differents types de sediments (500 & 710 urn) a differents jours de l'expcrimentation.
Le nombre est celui dcs individus de l’experience. Toutes les dimensions sont en mm.
MODE OPfiRATOiRH ET mesures. — Dans chaque cristallisoir, devant l’ouverture de chaque tube, est dispos6e
une quantity identique de sediment. L'animal reconstruit son tube en ulilisant des grains mis k sa disposition. Du
sediment est r6guli£rement remis devant l'animal de telle fagon qu'il n’en manque jamais. La portion de tube
reconstruite, nettement visible, est mesur&j pdriodiquement. Cela pennet d’6tablir une courbe des longueurs de tube
reconstruit en fonction du temps 6coulC Ces courbes obtenues dans les memes conditions seront done comparables
entre elles en fonction de la temperature pour l'cxpdrience de 1979, en fonction du type de sediment pour celles de
1988 et 1989.
Les valeurs moyennes obtenues out 6te compares entre elles par le test II de Kruskall et Wallis (Schwartz,
1963), test non parametrique adapte au faible nombre de valeurs.
En fin d’experience, nous procedons au comptage des grains de diverses natures utilises par l’animal le long de
l’axe longitudinal du tube reconstruit, e'est-^-dire entre le debut et la fin de l'experience. Cela permet d'etablir s'il y
a eu, ou non, choix par l'animal d'un certain type de grain.
Les CONDITIONS n6cess AIRES a LA reconstruction. — La m6thodc est celle employee par Vovelle (1965)
qui a montre la necessite d'un reste de tube, le caractere artificiel et "anormal" du tube reconstitue, mais "n'en ayant
pas moins une valeur fonctionnelle dans la mesure ou il realise une protection, d6jk efficace au bout de 48 heures"
(Vovelle, 1965, p. 68). Le fondement de cette metiiode tient au fail qu'un animal isoie dont on a casse le tube
tend rapidement k le reconstruire, k condition qu'il ait du sediment "convenable" k sa portee. La vitesse de
reconstruction depend notamment de la temperature de l'eau. Celle-ci doit etre sup6rieure k 4 °C pour avoir une
reconstruction mesurable (CRUET, 1982).
L'experience preiiminaire de 1982 montre (voir plus loin) que 1'on a interet k se situer entre 16 °C et 20 °C
pour que cette vitesse soit nettement mesurable. Les conditions de l'experience de 1989 s'en approchent. Pour
1'annee 1988 elles sont a priori moins favorables.
Enfin, la vitesse de reconstruction ralentit nettement au bout dune quinzaine de jours, l’animal ayant reconstruit
son "espace vital tubulaire". Continuer alors I'experimentation n'apporte rien de plus. D’autre part, il n'est pas
exclu que la taille du morceau de tube en debut d’expdrience, mais egalement l'age de l'animal soient aussi des
facteurs influant sur la vitesse de reconstruction. C'est pour cela que nous nous sommes situ6s dans un intervalle de
taille moyenne de 16,8 mm a 21,1 mm pour la longueur de tube de depart, et un diametre anterieur du tube variant
entre 2,6 et 3,3 mm, e'est-ct-dire que nous avons £cartd les individus jcunes ou ages (Gruet, 1982). Dans ces
experimentations, pour une meme temperature, les differences de vitesses de reconstruction indiqueront done une
plus ou moins grande capacite k utiliser un certain type de sediment caracterise par la forme de ses grains.
428
Y. CRUET & Y. BODEUR
Tableau 2. - Experimentation de mars 1989 (14 jours). Lots A. B. C. D el E. Longueurs moyennes des tubes reconstruits
par les Sabellaria en presence dc differents types dc sediments (500 a 710 pm) a differents jours de Texperimentation.
Le nombre est celui des individus de Texperience. Toutcs les dimensions sont en mm.
RESULT ATS
Les courbes de reconstruction onl, pour la plupart, une allure gdndrale qui permel de les diviser en trois
portions : d'abord une phas'\ de construction rapide (environ les sept premiers jours), puis une phase de
ralentissement, se terminant par un palicr. Les valeurs moyennes en fin d'experience donnent une idde sur la vitesse
de reconstruction.
TABLEAU 3. — Nature des grains du tube reconslruit des Sabellaria des lots B' et C (Experience de 1988); des lots B el C
(experience de 1989). Pourcentages de grains du sediment de depart (D) et dc celui du tube reconslruit (R).
Experience prEliminaire : action de la temperature (Gruet, 1982). — Trois lots de 15 individus chacun
ont 6i6 test6s aux temperatures constantes (salles climatisdes) de 13 °C, 16 °C et 20 °C. Les rdponses
individuelles sont tr£s hdtdrogdnes. Mais malgrd cette forte variability le test de Kruskall et Wallis montre que les
effets des temperatures sont signilicativemenl differents sur la reconstruction du tube (95 % de confianee). La
signification est forte entre le deuxidme et le neuvidme jour. Les valeurs moyennes maximales du tube reconslruit
en 13 jours avoisinent 25 mm h 20 °C, 20 mm h 16 °C et 7,5 mm k 13 °C. La vitesse maximale a ete observee h
20 °C : 13 mm le premier jour, puis 6,7 mm par jour avant d'atteindre le palier de la courbe.
Source : MNHN. Paris
SELECTION DES GRAINS DE SABLE PAR SABELLARIA ALVEOLATA
429
20-
15-
L (mm)
1-
H — • — h
B’
A — i — -
,7t
L (mm)
c
2 A 7 II 14 17
ElG. 1. — Vitesses de reconstruction (valeurs moyennes el deviations standards) des tubes au cours de ('experimentation de
mars 1988. L : longueur du lube reconstruit, en mm ; t : temps de reconstruction, en jours.
Experimentation de mars 1988 : influence du type de sEdiment (Tableau I, Fig. 1). — Lot A*. Dans les
conditions de ('experience, lcs longueurs du lube reconstruit par les Sabellaria h l'aide dun sediment compost
exclusivement de coquilles de inoules broydes (lot A) sont extremement rcduites. Au bout de 17 jours, la moyenne
des portions de tubes reconstruits n'atteint que 1,6 mm et d£s le 7£me jour la croissance est quasi nulle. La pi u part
des grains utilises pour la reconstruction sont en fait tombes de l'ancien tube lors des manipulations et reutilisds
pctr l'animal.
Lot B'. Dans les memes conditions, mais en presence d'un sable de riviere (Loire) consume de grains de quartz,
de feldspath, de mica et de "divers" (lot B'), la reconstruction du tube est trfcs nettement plus rapide (huit fois plus
que pour le lot A') avee une moyenne de 12,9 mm au bout du meme intervalle de temps. Le ralentissement de la
croissance h partir du 7fcme jour est h peine sensible. Les pourcentages de grains utilises (Tableau 3) montrent une
nette preference des vers pour les grains de quartz, une moindre capture des grains de feldspath, un refus des micas et
des "divers".
Lot C'. Toujours en conditions identiques, mais en presence d'un melange des deux sables precedents en
quantites egales, le tube est reconstruit <i une vitesse intermediate (qyatre fois plus rapide que pour le lot A' et 2
fois moins que pour le lot B') avec une moyenne de 6,9 nun au bout des 17 jours. L'analyse et le comptage des
grains utilises (Tableau 3) montre que l'animal refuse en general (de 50 % h 1,2 %) les moules cass£es pour
utiliser environ 80,8 % de grains de quartz (30,6 % au depart), 1 1,4 % de feldspath pour 1 1,3 % au depart soil
une meme proportion, 0 % de mica (0,4 % au depart), 6,6 % de "divers" (7,5 % au debut).
Le test de Kruskall et Wallis applique h ces trois lots montre des differences significatives (95 % de confiance)
entre le deuxidme jour et le onzi&me jour ; puis du quatorzieme jour (90 % de confiance) au 176me (10 %) la
signification diminue.
430
Y. GRUET&Y. BODEIJR
2 4 6 9 12 14
L (mm)
B
I — f— I — f-
2 4 6
L (mm)
1
►
L (mm)
30
20
10- -
©
t
i — ♦ — ' — * — I — ♦ — 1 — I — ' — ' — I — ' — I - ►
2 4 6 9 12 14
f
f
t
►
2 4 6 9 12 14
Fig. 2. — Vitesscs de reconstruction (valcurs moyennes cl deviations standards) des tubes au cours de l'experimentation de
1989. L : longueur du tube reconstruit en mm ; t : temps de reconstruction, en jours.
Experimentation de mars 1989 : influence du type de sEdiment (Tableau 2, Fig. 2). — Cette
experimentation rdp&te partiellement celle de 1988 mais en la compliant avec d'autres types de sediments.
Lots A et B. Les rdsultats (valeurs moyennes) pour ces deux premiers lots, constituds exactement des meme
sables qu'en 1988, sont lout b fait semblables h ccux de 1988. Seules les valeurs absolues different 16gerement.
Elies sont plus eicvecs en 1989 (2,5 fois plus pour le lot A et 1,7 fois pour le lot B), ce qui peut s'expliquer
simplement par la temperature de l'eau, plus forte en 1989. Les conclusions concemant la nature du sediment sont
similaires : il y a un ties net refus des moulcs brisdes et des micas, une preference pour les quartz et un peu moins
pour les feldspaths.
Lot C (Tableau 2, Fig. 2). II est constitue d'un sable de plage marine compose dun melange de quartz (51 %),
de feldspath (32 %), de mica (16%) et de bioclastes (1 %). La reconstruction du lube est la plus rapide que nous
Source : MNHN. Paris
SELECTION DES GRAINS DE SABLE PAR SABELLARIA ALVEOLATA
431
ayons obtenue, 1,6 fois plus dlevde que pour le lot B. II y a bien un ralentissement au bout de 7 jours mais le
palier ne parait pas encore atteint en fin d'expdrience z\u bout de 14 jours. Les grains de quartz et les bioclastes sont
pr6f6rentiellement choisis, les feldspaths un peu moins. Par contre les micas sont nettement "repousses" (de 16 k
0,5 %) ainsi que les "divers".
Lots D et E (Tableau 2, Fig. 2). Ces experiences comptementaires r<5cdis6es k partir dun sable de haute plage
riche en grains de quartz et en bioclastes, mais aussi en feldspaths et micas, donnent une vitesse de reconstruction
pratiquement identiquc k celle du lot B (sable de la Loire). Elies confortent l’ensemble des rdsultats precedents.
Le test de Kruskall et Wallis applique k ces courbes pcrmct de dire que la signification statistique diminue du
2eme jour (98% de con fiance), au 4eme (5 k 10 %), au 6£me (10 & 20 %), au 9£mc (20 %), au 12eme (20 k
30 %), au 14fcme (30 k 50 %). Ce test n’autorise pas k dire que les conclusions avancdes sont fausses, mais
qu'elles ne sont pas statistiquement valables si Ton rctient le seuil de 95 % de confiance. Cela tient k la forte
variability individuelle qu'il aurait fallu compenser par un bcaucoup plus grand nombre d'individus ce qui est
difficilement realisable pour des raisons pratiques.
DISCUSSION ET CONCLUSIONS
Aprds ces experimentations menses en laboratoire, nous pouvons dire que la nature mindralogique, done
chimique, des grains de sable utilises par Sabellaria alveolata ne semble pas jouer de role decisif dans le choix des
FIG. 3. — Grains dc differences natures et morphologies ayant ete utilises au cours des experimentations. 1 : moule brisee :
2 : bioclaste ; 3 : mica ; 4 : quartz (Q) et feldspath (F).
432
Y. GRUET& Y. BODEUR
grains de sable par eelui-ci. La morphologie des grains, par contre, sembje etre un factcur determinant pour une
memo sranulomdtrie du sediment. En el'fel :
- les monies brisees arlificielleinent (lot A' dc 1988) correspondent aux vitcsses de croissance les plus Rubles el
soul pou riant constitutes de carbonate de calcium, de meme que les bioclastes qui soni eux associts ,3 des
croissances rapides (lots C, D el H de 1989). La seule difference vienl de la morphologic de ces tltmenis, tfes
an-uleux el en aiguilles dans le premier cas, bien arrondis dans le second cas (Fig. 3. photos 1 el 2).
c. les proportions de quartz utilises sont toujours su peri cures a cclles de depart el le quartz esi un peu plus
employe que le feldspath. Ce choix relatif entre quartz el feldspatli esi peut-elre a inettre en relation avec la
micromorphologie ltgfcrcmenl plus lisse des quartz (Fig. 3. photo 4), plutot que de 1'atlribuer h de subtiles
differences chimiques entre ces mineraux tous deux silicates.
- le trfes net rejet des grains de micas, plats ct a bords tranchants (Fig. 3, photo. 3), corrobore 1 hypothec du
point precedent, les micas ttant eux aussi des mineraux silicates, chimiqucment proches des feldspaths.
- on pourrait enfin se poser la question d'une evcntuelle influence "dc type eataiyseur des melanges de grains,
par rapport aux sediments mono-mintraux ?
On a deja monlrt (GRUET, 1984) que ces Annelidcs Polychdles choisissent la taille des grains de sediment, ct
cela en relation avec les dimensions de I'organe construcleur p;tr ou chaque grain passe pour etre engine de ciment
avail t d'etre colic stir le tube. Les Sabellaria onl-elles, aussi, la capacity d'estimer la geometric des maleriaux mis a
leur disposition ? Ces experimentations le demontrent. Le refus de grains de formes anguleuses, allongdes ou
apiatis peut se realiser h plusieurs niveaux du mecanisme conslructeur deer it par VOVELLE (1965) : au moment ou
le filament oral capte le grain, plus lard lors de son cheminement le long des goutlieres Glides et enfin au niveau de
I’organe construcleur en fer i) cheval.
REMHRCIEMHNTS
Nous exprimons nos remerciements d M. le Professeur J. Vovellf. qui nous a toujours encourages dans nos
recherches et qui a relu noire manuscrit, a M.A. Cossard (Laboratoire de Geologic, University de Nantes) et a
M.G. Maura Y qui out contribuc a I'elaboration du "poster" auquel correspond cet article.
REFERENCES
GRUET. Y.. 1982. Recherches sur Ideologic lies "reefs" d'hermelles edifies par VAnnelide Polychile Sabellaria
alveolata (Linne). These de Doctorat d’Etat es Sciences. Univ. Nantes, 234 pp.
Gruet. Y.. 1984. _ Granulometric evolution of the sand tube in relation to growth of the Polychacte Annelid Sabellaria
alveolata (Linne) (Sabellariidae). Ophelia. 23 : 181-193.
Gruet. Y., 1986. — Spatio-temporal changes of sabellarian reefs built by the sedentary Polychaete Sabellaria alveolata
(Linne). Marine Ecology. 7 : 303-319.
GRUET. Y.. Vovelle. J. & Grasset. M.. 1987. — Composante biominerale du ciment du tube chez Sabellaria alveolata
(L.), Anuelide Polychete. Can. J. Zool.. 65 : 837-842.
HOMMERIL, P.. 1962. — Etude locale (Gouville-sur-mer. Manche) de la retenue des sediments par deux Polychetes
sedentaires: Sabellaria alveolata (Hermelle) el Lattice conchilega. Cah . occanogr.. 15eme annee (4) : 245-257.
ORRHAGE. L.. 1978. On the structure and evolution of the anterior end of the Sabellariidae (Polychaeta, Sedentaria).
With some remarks on the general organisation of the polychaete brain. Zool. Jahrb. Abt. Anar.. 100 : 343-374.
SCHWARTZ. I).. 1963. — Mcthodes statist iques a I'usage des medecins et des biologisles. Editions Flammarion, Paris.
358pp.
VOVELLE, J.. 1965. Le tube de Sabellaria alveolata (L.) Annelide Polychete Hermellidae et son ciment. fitude
ecologique. experimentalc. histologique et histochimique. Arch. Zool. exp. gen.. 106 : 1-187.
Source : MNHN. Paris
45
Les vers polychetes et l'estuaire de la Loire au debut du
20eme siecle par G. FERRONIERE (1875-1922)
Yves GRUET, Jocelyne MARC HAND & J. BAUDET
Laboratoire de Biologie Marine. 2. rue de la Houssiniere
44072 Nantes Cedex 03. France
RESUME
G. FERRONIERE, architecte de profession, realisa des etudes de geologic et de biologie marine : il fut I’un des pionnicrs de
lecologie experimenlale. Ses travaux de systematique (Oligochetes et Polychetes) lui ont confere une reputation internationale.
Ses eludes de faunistique, notamment sa cartographic biologique de l'estuaire de la Loire (1901), constituent des documents de
reference pour en eslimer revolution temporelle. Ainsi. en 90 ans. les especes euryhalines ont progresse vers Pamont de
l’estuaire : Boccardiella ligerica de 22 km et Nereis diversicolor de 1 1 km. Par contre. I'espece stenohaline Arenicola marina
conserve la memo distribution spatiale.
ABSTRACT
The polychaete worms and the estuary of the river Loire at the beginning of the 20th century bv G. FERRONIERE
(1875-1922)
G. FkrroniEre was an architect by profession but also a scientist, lie published results in the fields of geology and biology
and was one of the pioneers of ecology. He remains well-known for his works of taxonomy oligochaetes and polychaetes. The
biological changes in the estuary of the Loire can be estimated since his studies on the distribution patterns of benthic species
( 1901). In 90 years, the euryhaline species have moved up-stream in the the estuary: 22 km for Boccardiella ligerica and 1 1 km
for Nereis diversicolor from the previous point. On the contrary, the pattern distribution of the stenohaline worm Arenicola
marina remains as it was.
INTRODUCTION
Georges FerroniCre est ne le 5 juin 1875 a Nantes. Sa famille paternclle vivait du nggoce tandis que celle de
sa mfcre comportait plusieurs architects. II restera fidfcle h cette tradition familiale en devenant lui aussi architecte.
Son enfance passee dans le port de Nantes lui donne probablement le gout de la mer. En outre, durant les
vacances, il descend la Loire en bateau pour passer une partie de l'6t 6 sur la cote du Croisic. Brillant iM&ve. il
devient bachelier fes-Sciences h dix sept mis. A lTJniversitd Catholique d'Angers, il prepare el obtient la Licence
£s-Sciences naturelles. D£s cette Spoque il frequentc d'illustres naturalistes et participe h la vie de vSoeidtds
GRUET Y.. March and . J. & J. BAUDET . 1994. Les vers polychetes et l'estuaire dc la ILire au debut du 20eme siecle par
G. FERRONlf-Rl- (1875-1922). In: J.-C. Dauvin. L. Laubier & D.T REISII (Eds). Actes de la 4eme Conference internationale des
Polychetes. Mem. Mus. natn . Hist, nat., 162 : 433-439. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
434
M.Y. GRUET. J. MARCHAND, & J. BAUDET
Scieniifiques et de Musdes. Ses relations amicales avec le Dr. Louis BUREAU, Directeur du Musdum de Nantes, Ini
pennettent de connattre Edouard BUREAU, Professeur de Gdologie au Museum national d'Histoire nalurelle de
Paris qui l’aidc h acqudrir des competences dans cettc discipline. Parallclcment, il prepare a l'Ecole des Beaux Arts
Paris son diplome d'architecte. En plus de ses activites profcssionnelles, il prepare, de 1897 h 1901, unc these de
Biologie h la Sorbonne h Paris. Il choisit un sujet de biologie marine, auquel il peut se consacrcr dans le petit
laboratoire qu'il s'est amenage dans la villa familiale sur la cote battue du Croisic, it proximite de l'estuaire de la
Loire et des marais salants. En 1901 il presente son memoire intitule : "Etudes biologiques sur la faune supra-
littorale de la Loire Inf6rieure". Son deuxieme sujet de these comportait une etude de botanique et unc etude de
Geologie. Ce travail d'6cologie fut jugd avec mention "Tres Honorable", par Yves Delage, biologiste marin,
Gaston Bonnier, ceiebre botaniste et Munier-Chaemas, geologue. En 1901. il epouse Augustine Gouin ; lls
auront sept enfants. 11 consacre son energie h sa profession d'architecte, a ses recherches en biologie et geologie
ainsi quit plusicurs charges d'enseignement. Ainsi, il a assure des cours de geologie it l'Ecole Supdrieure
d' Agriculture d'Angers ; il fut aussi Charge d'enseignement de l'Histoire de l'Art il la Faculte des Lettres d' Angers
et meme dun cours sur les "marchandises" ou "matidres commercialisables" il l'Ecole Superieure de Commerce de
cette meme ville. La variete de ces charges illustre la diversity des competences de cc travailleur qui devait
par laser son temps entre Nantes, Angers et Paris. Ses qualitds pddagogiques sont confirmdes par les nombreuses
conferences pour lesquelles il ctait sollicitd. Il partieipa activement h la vie des Socidtds Scieniifiques locales
(Baudet et al„ 1991). 11 fut membre et parfois fondateur de Socidlds de Sciences Naturelles, de Geologie,
d'Archdologie, d'Ocdanographie. Il a aussi oeuvrd h la erdation et il ['extension de collections coniine celles du
Musde lapidaire de Nantes dont il fut conservateur. Il mourut subitement, il 47 ans, laissant inachevds certains
travaux. C'est son ami Joseph PEneau, qui prit soin de rdunir ses publications et notes scientifiques et qui rddigea
sa notice ndcrologique. Nous prdsentons son activitd de biologiste se rapportant aux travaux d inventaires,
d'expdrimentauons, de morphologie et de systdmatique d'Anndlides.
LES TRAVAUX D'INVENTAIRE
La thdse de G. FERRONI&RE comporte une premidre partie intilulde ” Etude de divers facids de la zone
supralittorale. Distribution des vers supralittoraux" avec quatre chapitres : -I- zone supralittorale dans les eaux
vives ; -II- "Le traict" du Croisic ; -III- Marais salants ; -IV- Eaux saumatres et douces. Les rdsultats de ses
nombreuses excursions dans des milieux aussi diversifids lui out pennis d'inventorier et cartographier de rids
nombreuses espdees. L'auteur s'dtait particulidrement attache il leur distribution spatiale scion les gradients halins :
de l'cau douce de la Loire jusqu'aux eaux marines puis de l'eau de mer jusqu'aux eaux sursaldes des marais salants.
Il avail relevd le fait que certaines formes aquatiques habitent aussi bien les eaux sursaldes que dessaldes et qu'ellcs
sont rids rdsistantes. II avail egalement abordd la notion, particulidrement importante en cstuaire, de la distribution
verticale des espdees. ride il la sriatilication des eaux en fonction de leur salinitd. Nous retiendrons sa cartographic
des espdees (supralittorales) caractdristiqucs de la Basse Loire. Ce riavail est en etfet indispensable pour apprdcier
les changements biologiques qui sont intervenus pendant le 20dmc sidcle (Fig. 1). Depuis le 19eme sidcle,
l'estuaire de la Loire a connu de vastes travaux d'amdnagement qui ont profonddment moditid sa morphologie, sa
bathymdriie et son hydrologie.
Dans le secteur aval (Donges), le chenal de navigation a dtd creusd de 4,25 m entre 1953 et 1976, puis de 3,25
m. Par ailleurs, depuis 1945. des centaines d’hectares de zones humides ont dtd remblaydes et endigudes pour
I'implantation de zones indusriiellcs. De ce fait le lindairc de berges naturelles est passd de 300 km h 50 km et
l’envasement des estrans s'est accdlerd. D'un point de vue hydrosddimentaire, ces amdnagements ont eu pour
consdquence de provoquer la remontde de la marde dynamique de 30 km en 75 ans, eerie du front de salinitd
(0,5 P.S.U.) de 20 km et eerie du bouchon vaseux de 10 km avec un doublement du volume des matidres en
suspension (environ 700 000 tonnes). Depuis le ddbul du sidcle, les changements hydrosddimentaires ont enrialnd
la progression vers l'amont des limites de distribution d’un certain nombre d'espdees bendiiques estuariennes,
comparativement h ce qu'avait cartography FERRONNifiRE. Ainsi, depuis 1901, Nereis diversicolor a progressd
d'environ 1 1 km et BoccardieUa ligerica de 22 km, tandis que les limites de distribution d 'Arenicola marina n'ont
pratiquement pas evolud (Marchand, 1972). Par ailleurs, les espdees h cycle court comme Boccardiella ligerica
peuvent s'implanter temporairement bien en amont de leurs limites habituelles lors des amides de grande
sdcheresse. II est certain que le surcreusement du chenal de l'estuaire et la destruction de nombreuses zones
humides ont eu pour consdquence la perte d'une grande partie des potentialitds biologiques de cet dcosystdme,
notamment de ses potentialitds nourricidres.
Source : MNHN, Paris
LES VERS POLYCHETES DE L'ESTUAIRE DE LA LOIRE ETC. FERRONIERE
435
Tableau 1. - Evolution des distributions spatiales de trois espfcces de polych&tes
dans l'estuaire de la Loire, depuis 1901.
FIG. 1 . Carle de France situant les lieux de travail de Georges FERRONIERE et carles comparant la distribution de quelques
espcces en 1900 d'apres FERRONNlERE et en 1980 d'apres Marciiand.
Source
436
M.Y. GRUET. J. MARCHAND. & J. BAUDET
LES EXPERIMENTATIONS
G. FERRONlfeRE voulail demon ti er quo la repartition des espdees intenidales depend des facteurs du milieu et
de leurs variations : "II nous resie maintenant a reproduire experimentalement ces changements de milieux el a
e indie r les consequences qui en decoulent pour cJiaque esp'ece .". Pour prouver que certaincs espdees sont adaptees
aux changements cycliqucs de conditions (mardes, cycles de mardes, saisons) et qu elles ont die sdlectioimees p.u
les contraintes environnementales, il a expdrimentd dans quatre domaines. La seconde partic dc sa tlidsc . Etude
expdrimentale de quelques conditions dc milieu agissant sur les animaux supralittoraux" comporte quatre cliapitres
principaux traitanl de : 1- la dessication : II- 1c passage dc l'eau de mer a 1'eau douce ; III- le passage de l'cau de
mer a l'eau sursalde ; IV- I'influence de la lumidre. Ces tiidmes sc pretaient a une experimentation simple,
rdalisable dans son petit laboratoire et caractdrisaient bien la zone des mardes (dessication, variation de la lumidre)
et le gradient halm croissant de I'estuaire de la Loire, a la mer, jusqu'aux mantis salants. De nombreux groupes de
vers marins, dul?aquicoles et memo terrestres ont dte testds : Planaires, Ndmertes, Oligochdtes et surtout
Polychdtes. Pour ce dernier groupe, 1’expdrimentateur rdcoltait sur I’estran des animaux frais, tenail compte de leur
taiiie, de leur dtat de maturitd et meine de leur provenance sur les dilTdrents niveaux de l'estran. L'expression des
rdsultats dtait aussi simple que revaluation des paramdtres ; l'auteur ddcrivait la reaction des animaux aux stimuli,
dessinait dventuellement leurs ddplacements. La plupart du temps la resistance des vers aux changements de
conditions est exprimde en temps de survie. Grace a scs experimentations qui nc faisaient varicr qu’un seul facteur
cnvironnemental a la l'ois. il pouvait apprdcier la toldrance des espdees. La richesse faunistique de la cote du
Croisie a permis a G. FerroniErk de tester plus de cinquante especes de Polychdtes parmi lesquelles nous avons
note :
- Syllidae : Syllis altemoseiosa ; S. gracilis ; S. prolifera : S. vivipara ;
- Phyllodocidae : Eulalia viridis ; E. quadrilineata ; E. rubiginosa \PhyUodoce biUneata ; P. laminosa ;
- Aphroditidae : Sthenelais idunae : Lepidonotus clava ; L. squamatus : Lagisca extenuata ; Halosydna
gelatinosa : Eteone picta ;
- Eunicidae : Lysidice ninelta ; Marphysa sanguinea : M. bellii ;
- Nereidae : Nereis longipes : N. cultrifera (y compris la forme Heteronereis) ; N. pelagica ; Hedisie (Nereis)
diversicolor ; N. dumerili ; N. irrorata :
- Spionidae : Boccardia ligerica ; B. polybrancliiata ; Malacoceros vulgaris : Polydora ciliata : P. caeca ;
- Sabellidae : Fabricia sabella ;
- Cinatulidae : Dodecaceria concharum :Audouinia teniaculata ; Cirratulus fdiformis ;
- Capitellidac : Capitella capitaia ;
- Chloraemidae : Flabelligera affinis : Stylarioides plumosus ;
- Arenicolidae : Arenicola marina ; A. grubei : A. ecaudata ;
- Terebellidae : Polycirrus hemaiodes ; Terebella lapidaria ; Lanice conchylega ;
- Serpulidae : Pomaloceros triqueter .
Dans ce travail G. FerroniEre fait preuve dune grande cuiiositd scientifique et se tient au courant des travaux
de ses contemporains (chaque chapitre est introduit par un "dtat de la question").
TRAVAUX EN MORPHOLOGIE ET SYSTEMATIQUE D'ANNELIDES
G. FerroniEre avail tout d'abord entrepris des dtudes sur les Oligochdtes, s'appuyant sur une bibliographic
mondiale complete. Travaillant sur la frange supdrieurc des estrans et sur des points d'eau douce temporaires, i!
dludia des espdees aux modes de vie sub-aquatiques. Les Oligochdtes aquatiques (Aelosomatidds, Naidides,
Tubificides et Haplotaxidds) furent dgalement abordds. Systdmaticien et faunisticien renommd pour les
Oligochdtes (Brinkhurst. 1963), il l'cst dgalement pour les Polychdtes.
C'est dans la premidre de ses trois "contributions a I'etude de la faune de la Loire-Inferieure" qu'il reprend la
description de deux espdees dc Protodrilus (Archianndlides). Son nom resie attachd <t Boccardiella ligerica
(Spionidae), espdee nouvelle qu’il ddcrit en 1898. Jeune chercheur, il ddcouvre celte espdee dans les vasidres de la
Basse Loire et lit dddic ;) ce fleuve ( Liger en latin). Ce ver "liabitait des tubes de vase, sous les pierres ou dans des
femes de rockers d demi envahis par la boue noire etfine qui forme, presque partout, lefond, dans cette par-tie de
V embouchure de la Loire". Dans sa description, l’auteur s'altache aux ddtails qui diffdrencient cette espdee de
Polydora ciliata et de Polydora ( Boccardia ) polybrancliiata. La publication illustrde perinet d’identifier avec
certitude I'espdce, mais le fail qu'il n'y ait apparemment pas eu ddpot dc type ou de paratype pcul, en partic.
Source :
LES VERS POLYCI1ETES DE L ESTUAIRE DE LA LOIRE ETG. FERRONIERE
437
expliquer les confusions cl redescriptions quc d’autres aulcurs fircnt par la suite (Fig. 2). Ainsi, R. Horst ddcrit en
1920 Polydora redeki du Zuiderzee (Pays-Bas) ej en 1927, P. Fauvel, recommit 1'existence de deux espdees
diffdrentes P. ligerica et P. redeki dans sa faune des "Polychdtes Sddentaires". En 1960, F. Rullier, h partir
d'dchantillons de Normandie (France), reprend la morphologic de Polydora (Boccardia) redeki, sans faire le
rapprochement avec B. ligerica de la Loire. Ce n'est qu'en 1971 que Blake & Woodwick rdexaminent l'ensemble
des dchantillons et demontrent la synonymic entre P. redeki Horst, 1920 et B. ligerica Ferronnidrc, 1898. Selon la
rdglc d'antdrioritd, la seconde denomination est la seule valide. Avec la revision des genres de Spionides, publide
par Blake & Kudenov en 1978. apparait Boccardiella gen. nov. auquel ccs auteurs rattachent Boccardia ligerica
qui ddsormais devient Boccardiella ligerica (Ferronnidre, 1898)
G. FERRONNIERE 1898
Boccardia ligerica Ferronniere, 1898
estuaire de la Loire, France
i
P. FAUVEL 1927
Polydora ligerica Ferronniere, 1898
= Boccardia ligerica
\
J.H. DAY 1967
Boccardia cf ligerica Ferronniere, 1898
Province du Cap, Afrique du Sud
R. HORST 1920
Polydora redeki Horst, 1920
Akmaarder Meer, Pays-Bas
l
F. RULLIER 1960
Polydora redeki Horst, 1920
Normandie, France
/
J.A. BLAKE, K.H. WOODWICK 1971
Boccardia ligerica Ferronniere, 1898
( = Polydora redeki Horst 1920 )
J.A. BLAKE, D. KUDENOV 1978
Boccardiella ligerica Ferronniere 1898
( = Boccardia ligerica )
FIG. 2. Schema resumant l'histoire de la nomenclature du Ver Polychcte Spionide Boccardia ligerica Ferronniere. 1898.
devenu Boccardiella ligerica (Ferronniere. 1898) en 1978 (BLAKE & KUDENOV, 1978).
Espdce suspensivore, ce ver serait favorisd par renvasemenl. II peut former des revetements denses de tubes
sur les blocs, au bas de I'estran (Fig. 3). D'aprds Robineau, 1986, cette espdce d’eau saumatre s'accomode de
salinit^s variant de 18 ^ 0,5 P.S.U., avec un ddveloppement maximum entre 1 1 et 7,7 P.S.U.. Longtemps connue
du seul estuaire de la Loire, Boccardiella ligerica presente actuellement une large distribution en zone iempt‘ree,
dans des stations envasdes, souvent associde au Serpulidd Ficopomatus enigmaticus (Fauvel). On la trouve aux
Etats-Unis (cote est), mais aussi en Afrique du Sud (DAY, 1967). II est probable que les transports maritimes aient
favorisd cette large rdpartition.
CONCLUSION
Le sujet de thdse de G. FerroniLre se silue tout h fait dans dans les iddes "mode me s" de la fin du 19dme
sidcle : le but est d'expliquer la distribution gdographiquc des animaux, d'elucidcr les questions d'origine de la
faune. de montrer comment les espdees s'acclimatent aux diffdrents milieux... Le choix de l'esutm a l’avantage de
presenter une trds grande diversite de facids ecologiquement bien diffdrencids. Par ailleurs. il a fait preuve
d'innovation en abordant I'dtude des zones sursaldes des marais salants et les seeteurs dessalds de I'estuaire de la
Loire. La cartographic des espdees caracteristiques de la Basse-Loire, effcctuee en 1901, reste une reference
regionale et constitue un "etat initial" essentiel pour apprdcier I'dvolution dcologique de I'estuaire suite aux
Source :
438
M.Y. GRUBT. J. MARCHAND, & J. BAUDET
FIG. 3. — Quelques aspects des populations de Boccardiella ligerica dans l'estuaire de la Loire. Certains blocs sont recou verts
d un tapis continu de tubes (Photo Le MAGUERESSE & GRUET).
profondes modifications physiques (chenalisation) qu'il a subies. Le chercheur G. FERRONlf.RE partagea son
6ncrgic et sa passion entre la biologie, la geologic et sa profession d'architecte. Son oeuvre scientifique n'en fut pas
moins remarquable ; die est toujours consuMe et cet auteur rcste reconnu , notamment cn systdnatique, comme
un "specialiste" ; k ce litre, il figure toujours dans les bibliographies. Son nom restera li6 k celui de 1'espfcce
nouvelle qu'il ddcouvrit en Loire.
LISTE DES TRAVAUX DE G. FERRONNIERE EN BIOLOGIE
1898 a — Ide contribution k 1’Ltudc de la faune de la Loire-Inf6rieure (Polygordiens, Spionidien, Ndncrtien).
Bull. Soc. Sc. nat. Ouest Fr., Nantes, (3-4) : 101-113.
1898 b — Quelques vers recoils au Croisic. Polych&tes, Polygordiens, Ndmertiens. Bull. Soc. Sc. nat. Ouest Fr ..
Nantes, (3-4). : XXI-XXI1I.
Source : MNHN, Paris
LES VERS POLYCHETES DE L'ESTUAIRE DE LA LOIRE ETC. FERRONIERE
439
1898 c — Quelques vers de Loire- In fkrieure. Bull. Soc. Sc. nat. Ouest Fr., Nantes, (3-4): 31-42.
1899 a — 2km e contribution b Tlttudc de la faune de Loire-Infdrieure (Pseudo-scorpions, Myriapodes, Anndlidcs),
Bull. Soc. Sc. run. Ouest Fr., Names, (2) : 137-146.
1899 b — 3kme contribution b TEtude de la faune de la Loire-Infkrieure (Oligochktes littoraux et supralittoraux).
Bull. Soc. Sc. nat. Ouest Fr., Nantes, (3) : 229-298.
1900 a — Sur Gryllotalpa vulgaris, courtilikre variktk foncke des Marais salants. Bull. Soc. Sc. nat. Ouest Fr.,
Nantes, : 15.
1900 b — line Anndlidc intermkdiaire entre les Spionidiens et les Cirrhatulidiens. Bull. Soc. Sc. nat. Ouest Fr.,
Nantes : 16.
1901 a — Eludes biologiques sur la faune supralittorale de la Loire-Infkrieure. Premikre thkse. Faculty des
Sciences de Paris, Sdrie A, n° 392, n d'ordre : 1063, 453 pages. Imprimeur-Editeur R. Guist'hau, A. Dugas,
Nantes.
1901 b — Eludes biologiques sur les zones supralittorales de la Loire-Inferieure. Bull. Soc. Sc. nat. Ouest Fr.,
Nantes, (1-2): 1-453.
1902 a — Sur un Phyllopode kclos b la Sorbonne dans des bocaux contenant de la boue provenant de la
Rdpublique Argentine. Bull. Soc. Sc. nat. Ouest Fr.. Nantes, (1-4) : 25.
1902 b — Sur Aepophilus Bonnairei , Anurida maritima , etc.. Bull. Soc. Sc. nat. Ouest Fr., Nantes, ( 1-4) : 26.
1906 — Observation sur Aepus Robini. Bull. Soc. Sc. nat. Ouest Fr., Nantes, (1-4) : 34.
1907 — Envoi au Museum de Nantes dune Epinoche pechke b la Bemerie. Bull. Soc. Sc. nat. Ouest Fr., Nantes,
(3-4) : 5.
1910 — A propos du travail du Dr Horst : De Anneliiden der Zuiderzee. Bull. Soc. Sc. nat. Ouest Fr., Nantes, (3-
4) : 8.
REFERENCES
BAUDET, J.. CRUET, Y., Lebel, A.. Maillard, Y.. MaRCHAND, J., 1991. Georges Henri Joseph FERRONNlfcRE. Son oeuvre
en Biologic marine. Bull. Soc. Sc. nat. Ouest Fr., Nantes, suppl. hors serie : 50-75.
BLAKE, J.A. & Kudenov,D.,1978. — The Spionidac (Polychaeta) from southeastern Australia and adjacent areas with a
revision of the genera. Mem. Nat. Mils. Vic.. 39 : 171-280.
Blake, J.A. & WOODWICK. K.H., 1971. — A review of the genus Boccardia Carazzi (Polychaeta: Spionidae) with descriptions
of two new species. Bull. So. Calf. Acad. Sci.. 70 : 31-42.
BRINKHURST. R.O., 1963. Taxonomical study on the Tubificidae (Annelida Oligochaeta). Inst. Rev. Ges. Hydr., suppl.. 2 :
1-83.
Day, J.H., 1967. A Monograph on the Polychaeta of Southern Africa. Part 2. Sedentaria. 'Trustees of the Brit. Mus. (Nat.
Hist.), London, 878 pp.
FaUVEL, P.. 1927. — Polychetes Sedentaires. Faune Fr. 16 : 1-494.
Horst. R.. 1920. — Polychactc Anneliiden uit het Alkmaarder Meer door Dr. R. Horst. Tool. Meded.. Leiden, 5 : 110-111.
MaRCHAND. J.. 1972. Bionomie benthique de Testuaire de la Loire I. Observations sur Tcstran maritime de la mer a
Cordemais. Rev. Trav. Inst. Pec lies marit., 36 : 47-67.
Robineau. B.. 1986. Les peuplements benthiques dans I'estuaire de la Loire. These de Doctorat, llniversite de Bretagne
occidentale, 330 pp.
RULLIER, F., 1960. — Morphologie et developpement du Spionidae (Annelide : Polychete) Polydora (Boccardia) redeki Horst.
Cah. Biol. mar.. I : 231-244.
Source :
Source : MNHN. Paris
46
Temporal and spatial patterns in the distribution of
infaunal Polychaetes in Jervis Bay,
New South Wales, Australia
Patricia A. HUTCHINGS * & Charles A. JACOBY **
* The Australian Museum, P.O. Box A285. Sydney South, NSW 2000 Australia
** Marmion Marine Laboratories, CS1RO Division of Fisheries
P.O. Box 20, North Beach WA 6020 Australia
ABSTRACT
A series of quantitative infaunal samples were taken between February 1989 and July 1991 at 10 sites in Jervis Bay. a
protected marine embayment on the south coast of New South Wales. Six sites had muddy/sand sediments and four sites were
in beds of the seagrass Posidonia australis. Replicate samples were taken at each site in every time period to produce a
quantitative baseline with estimates of variability. This baseline can be used to assess future changes in the infaunal
assemblages in Jervis Bay. Polychaetes were a major component of the fauna in terms of numbers of individuals and numbers
of species. The polychaetc faupa was represented by 171 species in 36 families. Assemblage data were analysed using
multivariate classifications. Assemblages tended to differ between the two habitats and among some sites within a habitat.
These differences remained stable through time. Some species were widely distributed across sites and habitats, and the
patterns in assemblage composition were due primarily to the restricted distribution of some rarer species. Density data for the
dominant polychaetc species wtgre used in analysis of variance in an attempt to assess spatial and temporal patterns in their
abundances. Densities of most species varied in a complex manner with spatial patterns being more obvious than temporal
ones. Patterns in abundance are difficult to explain or predict because of the limited information available on life histories of
these or related species and the absence of similar studies conducted elsewhere.
RESUME
Structures tcmporclles et spatiales dc la distribution des Polychctes end ogees dc la baie dc Jervis, Nouvelles Gallcs
du Sud, Australie
Une elude quantitative de l'cndofaunc de substrat meuble a etc realistic sur la cote Sud du NSW (Australie) a Jervis Bay.
une baie peu profonde et protegee de la houle. Dix stations ont etc echantillonnees ; quatre au sein de fherbier de Posidonia
australis el six en dehors de I'herbier. Les prelevements ont ete effeclucs tous les quatre mois dc fevrier 1989 a juillet 1991.
Les Polychctes sonl. en nombre d’especes cl en nombre d'individus, les organismes les plus abondants de cctte endofaune : 36
families et 171 especes ont etc identifies. Toutes les donnees ont etii Bailees avec le "Pattern Analysis Package". II en ressorl
que les replicals d'un meme substrat tendent a fusionner, indiquant ainsi la preponderance du facteur site sur le facteur saison.
Une analyse de variance portant sur les principales especes de Polychctes montre que si les facteurs sites ou saisons sont
preponderants pour la distribution dc nombreuses especes, ils agissenl aussi en synergic. Ces modeles de distribution sont
HUTCHINGS, P.A. & C.A. Jacoby. 1994. Temporal and spatial patterns in the distribution of infaunal Polychaetes in
Jervis Bay. New South Wales, Australia. In: J.-C. DaUVIN. L. LAUBIER& D..I. Rf.ish (F.ds), Aclcs de la 4cme Conference
Internationale des Polychctes. Mem. Mus. natn. Hist, nat ., 162 : 441-452. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
442
P.A. HUTCHINGS & C.A. JACOBY
discutes en detail en tenant compte des faibles donnees existant sur le cycle de vie de ces especes. I.es resultals obtenus sonl
egalement compares a ceux fournis par des etudes similaires realises dans d’autre regions du monde. rien de comparable
n'ayant ele fait en Austral ie.
INTRODUCTION
Jervis Bay, a temperate marine embayment on the south coast of New South Wales, is highly regarded for its
environmental quality and is listed on the Register of die National Estate. The bay is currently used for tourism,
commercial and recreational fishing and Department of Defence training exercises. Population growth in the
surrounding area is increasing. Concern about the possible impacts of current uses and proposed additional uses
led die Deparuncnt of Defence to fund a diree year program of inventory and baseline studies (Ward & Jacoby,
1992). One of these studies aimed to quantify spatial and temporal patterns in die abundances ol infauna in the
muddy/sand and vegetated sediments around the Bay. This paper discusses die preliminary findings from this
study widi an emphasis on polychaetes, which were a major component of the infauna and an essential part of any
baseline that characterises die existing status of Jervis Bay.
METHODS
Jervis Bay (35°08'S, 150°45'E) is a kidney-shaped marine embayment. It reaches a maximum depth of about
30 m, has a surface area of 102 km2, and opens onto die continental shelf through a 3.5 km wide entrance. The bay
has a relatively small catchment which docs not contain a major river but does include several small creeks.
Mangroves and saltmarshes line diese creeks. The shores of die bay are primarily sandy beaches bounded by creek
mouths and shallow rocky reefs. Extensive beds of seagrass Posidonia australis occur in the shallow, subtidal
areas (above 10 m) in die northern and southern parts of die bay. Beyond the rocky reefs and seagrasses (below
10 m), are characterised by extensive muddy/sand areas.
Four sites were selected in P. australis beds (vegetated sites) and six were chosen in deeper, muddy/sand
sediments (Fig. 1). Depths at the vegetated sites varied in depth from 2-6 m (Callala Boat Ramp 2 m, Hare Bay 3
m. Green Island 6 m and Hole in die Wall 5 m). Four muddy/sand sites, Hole in the Wall. Montague Roadsted,
Green Point and Plantation Point 'shallow', were at 12 in and two sites, Honeymoon Bay and Plantation Point
'deep' were at 20 m.
Nine sets of infaunal samples were collected at each site between February 1989 and June 1991. Sampling
periods were separated by two to five months. At each vegetated site, infauna were collected by SCUBA divers
using a hand operated corer (11 cm internal diameter; surface area of 0.01 m2). Four replicates were collected
from each of two plots (2 m x 2 m) separated by about 50 m. At muddy/sand sites, live replicate samples were
collected using a Smith-Mdntyre grab (sampling area 0.06 in2). All samples were put into bags made of 1 .0 mm
mesh, washed, stained with Biebricht Scarlet and fixed in 7 % neutralised formalin. In the laboratory, animals
were extracted, identified and counted. The mesh size was selected after consideration ol lime and funds available
for sorting and the main objective of the study, i.e., description of the overal distribution and abundance of the
benthic macroinfauna within the bay.
Assemblage data were analysed to assess spatial and temporal patterns in species composition. All data were
log 10 (x + 1) transformed prior to analyses. Multivariate classifications were based on Bray-Curtis dissimilarity
measures (Belbin, 1989). These measures were classified by hierarchical, polythetic, agglomerate fusion using
unweighted pair group arithmetic averaging (UPGMA), with no order or adjacency constraints and a beta
coefficient of - 0.01). The results of die fusion were used to construct a dendrogram from which groups of samples
were defined on the basis of fusion patterns. In addition, multivariate classifications of species according to their
occurrences in samples were conducted using two-step dissimilarity measures in a UPGMA fusion with no
constraints on adjacency or order and a beta of -0.01 (Belbin. 1989). Species groups were defined from a
dendrogram constructed from the results of the classification. The relationships between species groups and site
groups were examined using two-way tables.
Spatial and temporal patterns in the distribution of common species were investigated using univariate
analyses of variance. The ANOVAs based on data from grab samples had sampling periods and sites as random
factors. The ANOVAs based on core samples, also had sampling periods and sites as random factors, as well as,
plots as a random factor nested within sites. Prior to conducting die ANOVAs, data were tested for homogeneity
Source :
SPATIO-TEMPORAL PATTERNS OF POLYCHAETES FROM JARVIS BAY. AUSTRALIA
443
of variance using Cochran's test. All data required logio(x+l) transformation to achieve homoscedasticity. Some
data remained heterogeneous, and Uiese data were not analysed.
FIG. 1. Map of Jervis Bay showing location of vegetated and muddy/sand sites. Site 1, Hole in the Wall; Site 2, Honeymoon
Bay. Site 3; Montague Roadsted; Site 4, Green Point and Site 5. Plantation Point "shallow"; Site 6. Plantation Point
"deep".
RESULTS
Over 630 infaunal species were collected, including 248 crustaceans, 197 molluscs, 171 polychaetes and 15
echinoderms as well as representatives of Nemertea, Sipuncula, Phoronida, Turbellaria and Coelenterata which
were not identified to species. A majority of the 171 species of polychaetes (representing 31 families) have
previously been recorded from New South Wales waters (Hutchings & Murray, 1984).
Analyses were confined to a data set composed of counts of polychaetes, molluscs, and echinoderms from nine
sampling periods. To date, crustaceans have been identified only in the first four sets of samples.
A series of classifications were performed. Initially, a multivariate analysis, was performed using 558
replicates as separate samples. The resulting distribution of dissimilarity measures was strongly skewed towards
high values which suggests that single replicate samples varied greatly. It is unlikely that single samples
adequately represented an assemblage; therefore replicate samples from each combination of site and time periods
were summed (i.e., n = 5 for grab samples and n = 8 for core samples) and the analysis was repeated. This
classification revealed a strong dissimilarity between core and grab samples, i.e., samples from vegetated and
muddy/sand sites. This dissimilarity may have been partly due to biases introduced by the two different types of
sampling gear. These biases will be investigated in a separate paper. Subsequent analyses considered samples
from vegetated and muddy/sand sites separately.
Source :
444
P.A. HUTCHINGS & C.A. JACOBY
F89 _ GIs(
F89 _ CaBi
F89 _ HiW (
F89 _ HaB (
J89 _ HaB (
S90 _ HaB (
J91 _ HaB (
N89 _ HaB (
F90 _ HaB (
M90 _ HaB (
J89 _ GIS {
A89 _ GIs (
M90 _ GIS (
N89 _ GIs <
S90 _ GIS (
A89 _ HiW {
N89 _ HiW(
M90 _ HiW (
S90 _ HiW{
F90 _ GIs |
F90 _ HiW I
F91 _ HiW (
A89 _ CaB|
N89 _ CaB (
M90 _ CaB (
•191 _ CaB (
F91 _ CaB(
J89 _ CaB (
J89 _ HiW (
A89 _ HaB (
F90 _ CaB (
S90 _ CaB (
F91 _ GIs (
F91 _ HaB <
J91 _ GIs {
J91 _ HiW<
0.3680 0.4548 0.5416 0.6284 0.7152 0.8020
0.3680 0.4548 0.5416 0.6284 0.7152 0.8020
Bray-Curtis Dissimilarity Measure
FIG. 2. T he results of the fusion generated by multivariate classifications based on Bray-Curtis dissimilarity measures, for
the vegetated core sites. F= February. J= June. A= August. N= November. M= May. S= September, 89 = 1989. 90 = 1990.
91 = 1991. GIs-Green Island. CaB -Call ala Boat Ramp. HaB Hare Bay. HiW- Hole in the Wall.
Separate classifications based on data from grab and cores revealed that species composition differed primarily
among sites and was reasonably stable among sampling times (Figs 2 & 3). Exceptions were the February 1989
core samples which had relatively unique species composition regardless of their site of origin (Fig. 2). 1 he grab
samples from shallow (12 m) muddy/sand sites (Hole in the Wall, Green Point and Montague Roadsted) tended to
group together (Fig. 3). All the samples from Plantation Point deep (20 m) and most of the samples from
Honeymoon Bay (20 m), formed distinct groups (Fig. 3). The overall species composition of these two sets of
samples were clearly different from those found in the samples taken at the other muddy/sand sites (Fig. 3).
The distribution of species which led to differentiation of site groups were determined by examining two-way
tables. These tables showed that many species were abundant at all sites. Sile groups were most clearly
characterised by a few rare species with restricted distributions.
Assemblage composition did not show change dramatically through time, but the abundances ol individual
species may have varied between sampling periods. Univariate ANOVAs provided a means ot assessing these
variations. More than 25 % of the species recorded from the 558 samples were represented by less than
10 individuals, but some polychaete species were present in sufficient samples for detailed analyses of their
distribution among sites and through time. Following Cochran's tests, data for three species from core samples and
five from grab samples were examined using ANOVAs.
Analyses of variance indicated that the densities varied among combinations of sampling lime mid site. The
exceptions were Eunice australis and Owenia fusifonnis from vegetated sites. Their densities varied significantly
only with time. Our knowledge of the reproductive biology of these common species, or their relatives, is limited,
and this makes predictions or interpretations of temporal patterns in abundances difficult. Some preliminary
comments can be made.
Source : MNHN. Paris
SPATIO-TEMPORAL PATTERNS OF POLYCHAETES FROM JARVIS BAY, AUSTRALIA
445
0.8130
J89.
A89.
M90.
N89.
F90.
S90.
J91.
F90.
_Hon_
_Hon_
_Hon_
_Hon_
_Hon_
_Hon_
_Hon_
PPs.
I _
I _
I I I I I
0.3070 0.4082 0.5094 0.6106 0.7118
Bray-Curtis Dissimilarity Measure
0.8130
FIG. 3. — The results of the fusion generated by multivariate classifications based on Bray-Curtis dissimilarity measures, for
the muddy/sand grab sites. F= February. J= June, A= August, N= November. M= May, S= September. 89 = 1989.
90 = 1990, 91 = 1991. IliW Hole in the Wall. Hon-Honeymoon Bay. MRd Montague Roadsted. CPt-Green Point, PPs-
P1 an tat ion Point "shallow", PPd Plantation Point "deep".
Eunice australis was taken primarily in core samples. All four sites had relatively high numbers in the summer
(February) and spring (November) of 1989, but the overal mean density of Eunice was always low (Fig. 4). This
makes interpretations ol temporal patterns difficult. Eunice australis probably breeds annually after reaching
Source : MNHN. Paris
446
l’.A. HUTCHINGS & C.A. JACOBY
maiuriiy in its second year. Il is almost certainly a broadcaster and recruits by pelagic larvae. The life-span of this
species is greater than one year, which may explain why some individuals were always present in the vegetated
core samples although numbers varied over lime. If increases in numbers were due to recruitment, it appeared to
be poor in 1991.
All sites combined
FIG. 4. - The mean numbers of Eunice australis present at all vegetated sites on nine occasions between February 1989 and
June 1991.
Owenia fusiformis was recorded from both vegetated and muddy/sand sites. Peaks numbers of individuals
were observed at all four vegetated sites in February of 1989, 1990 and 1991. The mean densities of Owenia were
low, which complicates interpretations of variations in mean density. Densities of this species were higher in
samples from muddy/sand sites, with the highest densities recorded in samples from the deeper sites. Numbers of
Owenia taken from die muddy/sand sites fluctuated over time, but no consistent pattern were evident. Temporal
patterns in abundance are difficult to predict because nothing is known about the reproduction of this species. It
probably breeds annually by broadcasting because evidence of brooding was never observed when individuals
were extracted from their tubes, and it probably recruits via pelagic larvae. Owenia fusiformis is currently
regarded as a cosmopolitan species, but a detailed study of the genus Owenia in Australia may disprove this and
reveal one or more undescribed species. All specimens collected in Jervis Bay appeared to belong to one species.
Notomasius chrysosetus was taken in greatest numbers from vegetated sediments at Hole in the Wall (Fig. 5).
At diis site, numbers tended to be slightly higher in die summer (February) and spring (November) of die first
year. If these peaks were due to recruitment, the data suggest that there was litde recruitment in 1991. This species
probably breeds annually and produces a benthonic larval stage with limited ability to disperse.
Magelona sp.l was present primarily in the muddy/sand sediments at the 'deep' and 'shallow' sites at
Plantation Point. Its numbers fluctuated through time widiout a clear pattern. Furdier research is needed to clarify
die biological significance of temporal variations in numbers of this species and to identify the factors dial appear
to limit its distribution to certain sites.
Nephtys inornala was taken primarily at five of die six muddy/sand sites. Densities tended to vary with lime in an
unpatterned way, although samples from all muddy/sand sites showed an increase in numbers during February
1991 (Fig. 6). This suggests that widespread recruitment may have occurred prior to diis time. There was some
evidence that recruitment had occurred in die summer during the two previous years, but only at some sites (Fig.
6). Nephtys is almost certainly an annual breeder widi mass spawning giving rise to pelagic larvae. Our data
suggest that levels of successful recruitment varied among years and locations.
Augeneria verdis was found primarily in the muddy/sand sediments with numbers varying inconsistently over
time (Fig. 7). Honeymoon Bay always had the lowest number of individuals present (Fig. 7). Although studies
have not been undertaken on the reproductive strategies employed by this species or related ones, we suspect dial
it breeds annually by broadcasting and recruits via pelagic larvae.
Mediomastus n.sp., was referred to as Mediomastus californiensis in earlier reports (CSIRO, 1991) and by
Hutchings & Murray (1984) but it is a new species of Mediomastus, which is being described by Warren et
al. (in press). Mediomastus n.sp. occurred predominantly at die six muddy/sand sites (Fig. 8). During at least one
sampling period, mean densities were above 10 at all sites, except Plantation Point 'shallow'. Densities of diis
species increased in February or May 1990 at all sites except Plantation Point 'shallow' (Fig. 8). Recruitment may
Source : MNHN. Paris
SPATIO-TEMPORAL PATTERNS OF POLYCHAETES FROM JARVIS BAY. AUSTRALIA
447
have occurred at this time. We suspect dial this small species (5-10 mm in length) breeds annually, produces few
Green Island (6 m)
Hole in ihe Wall (5 m)
Cailala Boat Ramp (2 m)
Hare Bay (3 m)
FtG. 5. — The mean numbers of Noiomaslus chrysosetosus present at all the vegetated sites on nine occasions between
February 1989 and June 1991.
gametes and does not survive spawning. Judging from the protracted period of increased numbers, the breeding
season may be fairly extended. In addition, it may have been several weeks alter settlement before new recruits
would have been sampled by our techniques, and this may explain why die increase in numbers were spread over
several months.
DISCUSSION
Both types of analyses indicated that the densities of polychaetes and odicr infauna varied in a more consistent
manner among sites than among sampling times. The species composition of the infauna from muddy/sand
sediments appeared to vary between die two depths diat were sampled. Multivariate analyses indicated that
differentiation among sites at different depths was due mainly to the distributions of less abundant species, and
Owenia fusiformis also followed this trend. Although the results are not reported here, a tendency for species
composition to vary among sites and remain similar at a site through time was also seen when data for molluscs
and echinoderms were included in die analyses.
It appeared that many species occurred in both vegetated and muddy/sand sites, but muddy/sand sites
generally yielded more species. This trend may be partly due to the different sampling techniques employed in die
different habitats.
Source
448
P.A. HUTCHINGS &C.A. JACOBY
Planiaiion Point doop (20 m)
Fig. 6. The mean numbers ol' Nephtys inomata present at each of the muddy/sand sites on nine occasions between February
1989 and June 1991.
The majority of polychaete species were not sufficiently numerous or common for analyses of their
distributions over time. 01 the 171 species, only seven were common enough for univariate analyses. Temporal
variation in densities of common species would be due to a combination of recruitment and mortality of older
individuals. The available data do not provide strong evidence for consistent patterns in these events either within
or among years. Evidence of temporal patterns in mortality could be obtained by examining die size classes
represented in the samples. All material has been retained for future examinations. Direct evidence of recruitment
was not expected because recruits of most species are too small to have been retained by the 1.0 mm mesh
employed during this study. The mesh size used was die most appropriate for determining the overall distribution
and abundance ol infauna, the primary goal of tiiis study. Two hypotheses suggested by the results of this study
are: (1) polychaete recruitment is not equal at sites separated by a few kilometres and (2) many species of
polychaetes recruit annually but die intensity varies among years.
Source : MNHN, Paris
SPATIO-TEMPORAL PATTERNS OF POLYCHAETES FROM JARVIS BAY. AUSTRALIA
449
Hole in the Wall (12 m)
Green Point (12 m)
Honeymoon Bay (20 m)
10-
Ui
</>
* 8-
p
>
g 6-
a>
S J S’ £ S £ S £ S
U. ' < Z U. 2 CO U_ —>
Plantation Point shallow (12 m)
Montaguo Roadsted (12 m)
Plantation Point deep (20 m)
FIG. 7. The mean numbers of Augeneria verdis present at all muddy/sand sites on nine occasions between February 1989
and June 1991.
Mullivariate analyses also indicated that the polychaete fauna differed between vegetated and muddy/sand
sites. Samples from vegetated sites contained a subset of the suite of species which occurred in the muddy/sand
sites.
The study also highlights the need for more information on die reproductive strategies of these common
species in Jervis Bay. In all cases we have put forward our opinion of their reproductive strategies on the basis of
what is known for related species and, in some cases, information on egg sizes observed for these species either in
individuals from Jervis Bay or elsewhere in southern Australia.
450
P.A. HUTCHINGS & C.A. JACOBY
All tiie common species in Jervis Bay have been found in vegetated and muddy/sand sediments throughout
southern Australia (Hutchings & Murray, 1984). Although the number of quantitative studies conducted in
southern Australia has increased considerably over the past 20 years no other studies have examined changes in
die densities of individual species over time.
Honeymoon Bay (20 m)
Montague Roadsted (12 m)
Plantation Point deep (20 m)
FlG'.Lr T.h? mcan numbers of Med‘0i"as"is n.sp. present at all the muddy/sand sites on nine occasions between February
1989 and June 1991. 3
Stephenson et al. (1974, 1977) sampled the benthos of Moreton Bay, in southern Queensland on a regular
basis over many years and they found that changes in die composition of the fauna between years was more
important than seasonal changes, and diat sporadic floods were a major force structuring these communities. In a
Source : MNHN. Paris
SPATIO-TEMPORAL PATTERNS OF POLYCHAETES FROM JARVIS BAY. AUSTRALIA
451
subsequent study STEPHENSON (1980) found that the benthic community changed over time with the frequency of
change varying between sites. A 3 year cycle was typical at inshore sites and 5.5 year cycles were found at the
more oceanic sites. Changes in density of individual species were not examined in detail. After more than a
decade of intensive sampling, Stephenson et al. (1977) were unable to predict community structure and they
stressed the unpredictability of the species composition of these benthic communities. Our studies in Jervis Bay
would generally support these conclusions, although we suggest that all sites (both vegetated and muddy/sand)
had a core of common species. Variation in the communities was due to a number of rarer species. The exact
composition of an assemblage may be largely determined by chance recruitment events of the rare species. 'Fhese
recruitment events are presumably influenced by factors such as local water flow patterns and sediment
characteristics, as well as the supply of larvae and the interactions with the existing suite of species at a particular
site. The widely distributed species in Jervis Bay were relatively long-lived. Recruitment failure in one of the
three years that made up this study may not have appeared as a change in adult populations.
No other studies of the temporal or spatial variations in the infaunal communities have been undertaken in
Australian seagrass beds (Howard et al. , 1989). This is despite their importance as nursery habitats for
commercial species of fish and prawns (Bell & Pollard, 1989). Gambi et al. (1991) published an abstract
describing a study of spatial and temporal patterns in polychaete distributions in Mediterranean beds of Posidonia
oceanica , but the complete paper has yet to be published so a comparison with our Findings can not be made.
Similar studies have not been undertaken elsewhere in the world, in part because of taxonomic difficulties. A
recent study by CROUCH (1991) investigated die polychaetes associated with the rocky intertidal surfgrass
Phyllosadix scouleri and P. torreyi in California, however this represents a very different environment to
Posidonia australis communities, and dierefore her findings have little relevance to tiiis study. Hopefully this lack
of knowledge of Posidonia communities will change in die future. The Australian Museum is currently sampling
the muddy/sand sediments of Botany Bay (another sheltered bay about 100 km north of Jervis Bay) over an
extended period of time. This study is revealing a fauna similar to that found in Jervis Bay and detailed
comparisons will be made once this study is completed.
This study has provided a detailed baseline lor die distribution and abundance of macroinfauna in Jervis Bay.
The baseline will facilitate management of the bay including a recently declared Australian Marine National Park
and a proposed New Soudi Wales Aquatic Reserve. A program of long-term monitoring may be introduced in
Jervis Bay. and diis study could act as a basis for the design of a benthic monitoring program.
ACKNOW 1 .EDGMENTS
We should like to thank the Department of Defence for funding diis project through CSIRO Division of
Fisheries. Angela Meza. Fiona McKillup and Rob PATTERSON, assisted in the collection and sorting of this
material. Cassie ROSE and Angela Meza assisted in die analyses of die data.
REFERENCES
Bell, J.D & Pollard. D.A.. 1989. — Ecology of fish assemblages and fisheries associated with seagrasses. In: A.W.D.
Lark™. A.J. McComb & S.A. SHEPHERD (eds), Seagrasses: Treatise on the Biology of Seagrasses with special reference
to the Australasian Region. Elsevier. Amsterdam : 565-609.
Belbin, I ... 1989. PATN Pattern Analysis Package. Technical Reference. CSIRO Division of Wildlife and Ecology. 222 pp.
CROUCH, C.A., 1991. Infaunal polychaetes of a rocky intertidal surfgrass bed in southern California. Bull. mar. Sci..
48 : 386-394.
CSIRO.. 199 1 . Jervis Bay Baseline Studies. Progress Report. December J99J. CSIRO Division of Fisheries, Jervis Bay.
Gambi. M.C.. Giangrande. A.. Martinelli. M & Chess a. L.A.. 1991. — Polychaetes of the Mediterranean seagrass
Posidonia oceanica: Spatio-temporal distribution and feeding guilds analysis. Bull. mar. Sci.. 48(2) : 596 p.
Howard, R.K., Edgar, G.H. & Hutchings. P. A. .1989. — Faunal assemblages of seagrass beds. In: A.W.D. LARKUM, A.J.
McComb & S.A. SHEPHERD (eds). Seagrasses: Treatise on the Biology of Seagrasses with special reference to the
Australasian Region. Elsevier. Amsterdam : 536-582.
HUTCHINGS. P.A. & MURRAY. A.. 1984. Taxonomy of polychaetes from the Hawkesbury River and the southern estuaries
of New South Wales. Rec. Aust. Mus.. 36 (suppl.3) : 1-119.
Stephenson. W.. 1980. Time patterns of macrobenthic species in Moreton Bay. Aust. J. Ecol.. 5 : 245 262.
452
P.A. HUTCHINGS & C. A. JACOBY
STEPHENSON. W\. COOK. S.D & RAPHAEL. Y.I.. 1977. The effects of a major Hood on the macrobenthos of Bramble Bay.
Queensland. Mem. Qd. Mus.. 18 :9 8-1 19.
STEPHENSON. W.. Williams. W.T. & COOK. S.D.. 1974. The benthic fauna of soft bottoms, southern Morelon Bay. Mem.
Qd. Mus.. 17 :73— 123.
Ward. T.J. & Jacoby. C.A.. 1992. A strategy for assessment and management of marine ecosystems: baseline and
monitoring studies in Jervis Bay. a temperate Australian embayment. Mar. Poll. Bull.. 25 : 163-171.
Warren, L.M.. HUTCHINGS, P.A & Doyle, S. (in press). A revision of the genus Mediomastus Hartman. 1947 (Polychaeta:
Capitellidae). Rec. Aust. Mus.
Source : MNHN, Paris
47
Ecology and biogeochemistry of Paralvinella sulfincola
at northeast Pacific hydrothermal vents: review and
comparison with Alvinella spp.
of the east Pacific rise
S. Kim JUNIPER
Geotop & Dcpartement des Sciences Biologiques
University du Quebec a Montreal
C.P. 8888, succ. A. Montreal (Quebec)
H3C 3P8 Canada
ABSTRACT
The "sulfide worm" Paralvinella sulfincola Desbruyeres & Laubier 1993, of northeast Pacific hydrothermal vents, builds a
mucous lube on the surface of high temperature chimneys, as does Alvinella spp. on the East Pacific Rise. P. sulfincola is a
deposit feeder and likely grazes on thermophilic chimney bacteria. It is argued that deposit feeding is also the primary source of
nutrition for Alvinella spp. The influence of both worms on the sulfur cycle and on chimney mineralization processes is
discussed. While Alvinella appears to be more elaborate in its adaptations to the high temperature chimney environment, the
functional significance of some of these apparent adaptations remains unclear. Observed effects of P. sulfincola on chimney
mineralization suggest that the question of how Alvinella spp. influences chimney growth patterns needs to be re-addressed.
Two previously proposed roles for the epibiotic bacteria in Alvinella spp.. nutrition and detoxification, can be accomplished by
P. sulfincola without the aid of episymbionts. This is a strong argument for a re-evaluation of the nature of the Alvinella-
bacteria symbiosis.
RESUME
Ecologie et biogeochimie du ver Paralvinella sulfincola des sources hydrothermales du Pacific|ue Nord-Est :
revue et coinparaison avec le genre Alvinella de la dorsale du Pacifique oriental
De fa?on identique aux Alvinella spp. presents au niveau de la dorsale du Pacifique oriental, le «ver sulfure», Paralvinella
sulfincola. des sources hydrothermales siluees dans le Pacifique Nord-Est, construit un lube de mucus a la limite des events des
cheminees d’oii jaillit le fluide hydrothermal a haute temperature. Detritivorc, P. sulfincola broute probablement des bacleries
thermophiles prcsentes sur les cheminees. Pout Alvinella spp., l'alimentation detritique pourrait aussi etre la source principale
de noun ilure. L'influence des deux vers sur le cycle du soufre et sur la mineralisation des cheminees est analysee. Bien que les
Alvinella spp. scmblent etre mieux adaptes a un environnement de temperatures extremes, la fonction de certaines de ses
adaptations apparentes nest pas encore claire. Les effets observes de P. sulfincola sur la mineralisation des cheminees sugge-
JUNIPER, S.K.. 1994. - Ecology and Biogeochemistry of Paralvinella sulfincola at Northeast Pacific Hydrotermal Vents:
Review and Comparison with Alvinella spp. of the East Pacific Rise. In: J.-C. DaUVIN. L. Laubier & D.J. REISII (Eds), Actes
de la 4emc Conference intern ationale des Polycheles. Mem. Mus. natn. Hist, nai ., 162 : 453-462. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
454
S.K. JUNIPER
rent que toute la question de l'influence d 'Alvinella spp. sur la croissance dcs chemin«5es a besoin d'etre reformulee. Ainsi, les
deux roles envisages pour les bacterics epibiotiques chez Alvinella spp., soit la nutrition et la detoxification, peuvent dire
accomplis par P. sulfincola sans I'aidc d cpisymbiontes. Ceci est un argument important qui entraine le reexamen de la nature
de la symbiose d ’Alvinella avec les bacteries.
INTRODUCTION
Since the discovery of hydrothermal vent biological communities in 1977, numerous new vent-specific species
have been described, many of which have unusual adaptations for bacterial-invertebrate symbiosis and for life at
high temperatures. The intimate association of several species with mineral deposition processes has inspired
studies of biomineralization (Juniper et al. , 1988, 1992). High temperature microorganisms have been the focus
for most work on sulfide chimneys. In addition to thermophilic and ultra-thermophilic bacteria that grow within
the plumbing system of chimneys and on chimney surfaces, a specialized chimney fauna flourishes in this extreme
and rapidly changing environment (TUNNICLIFFE & Juniper, 1990). Adaptations of the chimney fauna to its
habitat and its influence on mineralization processes are newly emerging areas of research.
Among die first organisms to colonize newly-formed chimney surfaces are the alvinellid worms (Juniper et
al., 1992). At northeast Pacific vent sites, the "sulfide worm". Par alvinella sulfincola Desbruydres and Laubier
(1993) [in TUNNICLIFFE et al. , 1993], occupies a niche similar to that of Alvinella pompejana and A. caudala and
occasionally Paralvinella grasslei on the East Pacific Rise (EPR) (DESBRUYfcRES et al., 1985; DesbruyEres &
Laubier, 1986; TUNNICLIFFE et al. , 1993). Ihe sulfide worm was originally thought to be a form of Paralvinella
palmiformis that colonized environments where mineral precipitation is heavy, forming loose tube structures with
its otherwise amorphous mucous secretions (Juniper et al., 1988; TUNNICLIFFE & JUNIPER, 1990). Later
morphological, genetic and behavioral studies recognized a separate species, Paralvinella sulfincola
(TUNNICLIFFE et al., 1993). These tube-building worms colonize large areas of newly-formed portions of high-
temperature chimneys (Juniper et al., 1988; Tunnicliffe & Juniper. 1990). Ongoing studies reveal a number of
physiological, molecular and behavioral adaptions that allow this organism both to tolerate an extreme
environment and to exploit the resources present. Other work indicates that the worm can influence mineralization
processes on chimney surfaces. This paper develops an overview of the ecology and biogeochemistry of P.
sulfincola mid compares them with the Alvinella species to highlight present understanding and future research
directions. Since most previous studies on species of Alvinella do not distinguish between A. pompejana and A.
caudata , discussion here will generally refer to them as Alvinella spp.
THE HIGH TEMPERATURE CHIMNEY ENVIRONMENT
The smoking chimneys and spires that develop around high temperature vents are the focal points of sulfide
mineral precipitation on sediment- starved spreading ridges (H£kinian et al., 1983; H&kinian & FOUQUET, 1985;
Tivey & Delaney, 1986; Hannington & Scott. 1988). Growth of these sulfide edifices passes through two
major phases that correspond to changes in the environment of mineral deposition within the chimney structure.
Haymon & Kastner (1981) and Haymon (1983) proposed that chimney growth begins when seawater entrained
into a jet of high temperature (350 °C) fluid is heated to supersaturation witJi respect to CaS04 This causes the
precipitation of anhydrite and die upward growth of primitive chimney walls in the form of a porous anhydrite
shell. Induration of this shell by further precipitation of anhydrite and other minerals eventually begins to isolate
hydrothermal fluid within the structure from surrounding seawater to the point where significant physico-chemical
gradients develop across the chimney walls. This initiates the second phase of chimney development. While
anhydrite continues to accrete on the outer walls and on the distal portion of die growing chimney, hydrodiermal
fluids migrate outward through die walls, dissolving and replacing anhydrite with sulfide minerals. At die same
time, high-temperature, low-pll conditions within the chimney conduit favor die inward growth of Cu-Fe rich
sulfides. Chimneys grow in this manner up to several metres in height, accrcdng new anhydrite material around
the vent orifice, and later infilling and replacing it widi sulfides. Not all chimneys form in this way. Instead of
anhydrite, direct precipitation of barite or sphalerite can form the early shell (Paradis et al., 1988). The
subsequent processes are essentially die same in all cases. Early walls are replaced and sealed by outflowing
hydrothermal fluid that is precipitating sulfide.
The zone of early sulfide mineralization on growing chimneys is the preferred habitat of die sulfide worm
(Juniper et al., 1988; Tunnicliffe & Juniper, 1990) (Fig. 1). Prior to worm colonization, a thickening of die
Source :
ECOLOGY AND BIOCHEMISTRY OF PARA LVINELLA
455
anhydrite walls of die chimney appears be necessary to reduce surface temperatures to levels the worms can
tolerate (Juniper el al., 1992). TlVEY el al. (1990) recorded formation and thickening of an anhydrite shell within
a thermistor collar fitted around a smoker orifice. An outer wall temperature of 67 °C was recorded at the end of
their experiment. No worms had colonized the shell at that point (M. Tivey, pers. comm.). It is difficult to define
PlG. i. — Schematic representation of the colonization of high-temperature chimneys by the sulfide worm Pcmdvinella
sulfincola. Worms cover extensive surfaces in newly-formed areas of chimney that are undergoing infilling and
replacement by sulfide minerals (light shading). Dark shading in lower part of structure represents zone of massive sulfide.
Light cap at top indicates a higher temperature zone that is not inhabited by the worms. Insert represents cross-section
through chimney wall with location of marcasite crusts (M) indicated beneath worm tubes (T). Right to left in insert is
equivalent to moving from the chimney surface toward the interior.
precisely die range of conditions dial constitute die worm's habitat. All physico-chemical habitat information must
be collected remotely from submersibles, and in diis milieu ol sharp physico-chemical gradients, remote
manipulation of sensors or sampling devices is simply not accurate enough to reliably record conditions widiin die
worm's immediate microenvironment. Temperatures of 20 - 80 °C have been measured on surfaces colonized by
sulfide worms (JUMPER el al., 1992), and it is most likely that the worms regularly experience temperatures within
die lower part of diis range. Alvinella spp. is frequently found at temperatures near 40 °C (FUSTEC el al.. 1987)
and has recently been reported moving over a 105 °C surface (ChevaldonnF el al.. 1992). TUNNICLIFFE el al.
(1993) emphasize the importance of turbulence and likelihood of occasional blasts of hot water in die upper part
of the 20 - 80 °C range.
Source :
456
S.K. JUNIPER
TUBE BUILDING
Paralvinella sulfincola is one of two northeast Pacific species of ParalvineUa known to build a tube (Fig. 2).
The other species, P. pandorae , secretes a thin translucent mucous sheath attached to surfaces such as
vestimentiferan tubes (Tunnicliffe et al.. 1986) The tube of P. sulfincola is a more complex multilayered
structure (Fig. 3 A) that resembles the tube of Alvinella spp., although it is less ordered at the ullrastructural level
(Fig. 4A) than the tubes of A. pompejana. The outer surface of the tube remains soft and not tanned as in Alvinella
spp., and as a result the tubes tend to aggregate mineral particles. l ube mineral content tends to resemble that of
underlying chimney material (JUNIPER el al. , 1986).
FIG. 2. — Sulfide worm ParalvineUa sulfincola and its tube (T).
from edge of lube.
In left of photo, bacterial filaments can be seen protruding
Alvinella spp. has an unusual and abundant epibiotic bacterial flora whose biological relationship with the
worms is not fully understood (Gaill & HUNT, 1986, DESBRUYfeRES et al.y 1983). Large numbers of filamentous
bacteria also occur attached to the inner surface of the tubes of Alvinella spp. and enclosed within the organic
matrix of the tube wall (Gaill et aly 1988; Gaill & Hunt, 1986; Gaill & Hunt, 1991). P. sulfincola has a
similar abundance of filamentous bacteria within the tube matrix (Fig. 2), but no equivalent epidermal flora.
Scanning electron micrographs reveal that both the inner and outer surfaces of the tubes are colonised by
filamentous bacteria, with filaments being most abundant on the inner tube surface (Fig. 3B-C). Transmission
electron microscopy shows layers of bacteria between consecutive layers of mucus (Fig. 4B). Assuming that new
lube layers are added from the inside, the layers of bacteria likely represent cells that were trapped under
successive layers of mucus. Bacterial growth on the inner tube wall must alternate with periods of mucus secretion
and tube building, as has been suggested for A. pompejana (Gaill & Hunt, 1991).
As chimneys grow upward, surfaces colonized by alvinellid worms cool and eventually lose their supply of
fluids. Time lapse camera studies have revealed that adult P. sulfincola respond to this change in habitat
conditions by abandoning their tubes and migrating upward to colonize newly-formed chimney surfaces (JUNIPER
et al., 1992; Tunnicliffe et al. , 1993). Similar conclusions (for Alvinella spp.) were reached by Fustec (1985)
after comparing colonization patterns and chimney dimensions over a three year interval at 13° N on the East
Pacific Rise.
Source :
ECOLOGY AND BIOCHEMISTRY OE PARALVINEUA
457
FOOD SOURCES
Paralvinella sulfincola is apparently a deposit feeder, using its oral tentacles to gather particles that are then
transfered to the mouth (TUNNICLIFFE el al., 1993). Microscopic examination of gut contents reveals grains of
sulfide, globules of elemental sulfur and remains of bacterial cells. Bacteria growing on die chimney surface are
probably the main source of nutrition. Baross & Deming (1985) observed that bacteria (mainly filamentous
forms) are able to colonize most external surfaces of high-temperature sulfide chimneys. Thermophilic bacteria
isolated from this habitat include one extreme diennophile isolated from homogenized sulfide worms (PLEDGER &
Baross, 1989. 1991). Thermophilic or extremely thermophilic bacteria may even represent the principal food
source for the sulfide worm, since they are likely die dominant bacteria in diis environment (Pledger & Baross,
1989). If so, this would be the first example of a high-temperature trophic link. While die influence of
thermophilic bacteria on geochemical processes is often discussed (Baross el al., 1982; Jannasch & Morn.,
1985), these organisms are rarely, if ever, considered as a possible food source for metazoans. Alvinella spp. is
Fig. 3. — Scanning electron micrographs showing layered structure of the tube (end-on view) of P. sulfincola (A) and
colonization of outer (B) tube surface by bacteria. Outer surface of tube is on right in A.
also known to ingest particles, and this is its most likely mode of nutrition, although the tube bacteria are
implicated in a hypothesis concerning a nutrition-related symbiosis with the worm. AlaySE-DAnet el al. (1986)
proposed that these bacteria secrete dissolved organic matter (DOM) that accumulates within the worm's tube and
is subsequently absorbed by Alvinella spp. across its epidermal surfaces. They demonstrated incorporation of
radioactively labelled compounds by epidermal tissues of Alvinella spp. and proposed this as evidence for their
hypothesis. However, there tire no published data on DOM levels within the tube of Alvinella spp. In a study of
die digestive tract of Alvinella pompejana, Saulnier-Michel et al. (1989) note unusual (for polychaetes)
evidence for enzymatic breakdown of bacteria in die anterior portion of die digestive tract and suggest diat
bacterial cells represent an important part of the ingested food. Although they also note an abundance of
particulate metals and sulfur in the gut, they do not link diis to ingestion of bacteria on chimney particules.
Instead, diey conclude dial the filamentous bacteria inside die alvinellid tubes are the more probable nutritive
source (Saulnier-Michel etal, 1989).
ROLE IN SULFUR TRANSFORMATIONS
Fhe principle effect of P. sulfincola on the sulfur cycle at vents may be related to the detoxification of 1LS in
the tissues of the worm. Hydrogen sulfide has two main toxic effects: it competes widi molecular oxygen for
binding sites on haemoglobin molecules, leading to asphyxia, and it destroys the porphyrin structure of
cytochrome C in the cellular electron transport system, thereby interfering with energy metabolism (Somero et
458
S.K. JUNIPER
al., 1989). Assays of (issues of P. sulfincola have revealed die presence of enzymatic sulfide oxidation (Juniper el
al., 1992), commonly found in polychaete worms from reducing environments, possibly as a detoxifying agent
(Somero el al., 1989; ViSMANN, 1990). Rates of sulfide oxidation by the worms appear to be high enough to lead
to accumulations of elemental sulfur in dieir mucous secretions and tubes. Alvinella spp. accumulates elemental
sulfur in its lube and epidermal tissue, presumably also as a result of HoS detoxification. In this case, the epibiotic
bacterial flora has been implicated in sulfide oxidation (Laubier el al., 1983), although this activity has yet to be
quantified. Sulfide oxidation in the tissues of Alvinella spp. also remains unmeasured.
FIG. 4. Transmission election micrograph showing layered structure of tube P. sulfincola (A) and flapping of bacteria
between layers of mucus (B). Tube external surface is on right in both photos.
EFFECTS ON CHIMNEY MINERALIZATION
Essentially all newly-formed chimney surfaces arc colonized by migrating sulfide worms within a matter of
days (JUMPER et al., 1992). The effect of worms on chimney mineralogy was studied by examining die texture
and composition of chimney material beneath worm tubes. Sections through the outermost layers of older
chimneys generally revealed a 2 mm-thick crust of the sulfide mineral marcasite (FeS2)^ beneath the mucous
tubes (Paradis et al., 1988; Juniper et al., 1992) (Fig. 1). Since die worms generally occur in dense aggregations,
die marcasite crust may be extensive enough to affect chimney wall porosity which in turn controls progress of die
second stage of chimney mineralization.
The fact that marcasite precipitation is spatially associated widi die worm tubes suggests diat die worm-
bacterial complex alters local geochemistry to favor die precipitation of this mineral. How might diis occur ?
Formauon of bodi marcasite and pyrite usually requires die presence in solution of intermediate sulfur compounds
and FeS precursors; at pH < 5 the precipitation of marcasite is favored over that of pyrite (MUROCHICK &
Barnes, 1986). High percentage levels of elemental sulfur have been measured in die tube mucus (JUNIPER et al.,
1986; Juniper, 1988) and similar sulfur concentrations occur in the tubes of Alvinella pompejana (Gaill &
Hunt, 1986). Paradis et al. (1988) suggested that interacuon of II2S from hydrothermal fluid widi diis elemental
sulfur could form intermediate sulfur compounds such as polysulfide.
1 Marcasite and pyrite have the same molar ratio of sulfur to iron (FeS2). but their crystallographic characteristics are quite
different, as are their physico-chemical properties.
Source : MNHN. Paris
ECOLOGY AND BIOCHEMISTRY OF PARALVINEUA
459
Mineralogical and time-lapse camera data studies provide independent lines of evidence linking tube building
to crust formation (JUNIPER el al, 1992: TUNNICLIFFE el al, 1993). As well, the proposed role of tube mucus in
this process (Paradis el al. , 1988) is supported by recent experimental work on die formation of iron disulfides
from solutions. Reaction of elemental sulfur with water generates high concentrations of thiosulfate, polysulfides
and polythionates at the sulfur-water interface (SCHOONEN & Barnes, 1991c). This high local concentration of
intermediate sulfur species apparently can cause iron disulfides to form directly on elemental sulfur grains
(Goldhaber & Stanton, 1987; Schoonen & Barnes, 1991a, b, c). Thus a local source of elemental sulfur in
tube mucus can cause marcasite precipitation both by direct reaction with FeS precursors, or indirectly through the
generation of intermediate sulfur species.
DISCUSSION
The alvinellid worms (Alvinella spp. and Paralvinella spp.) probably evolved from a common ancestor that
colonized the East Pacific Rise and die Juan de Fuca Ridge when diey were contiguous (TUNNICLIFFE el al,
1993). Since the separation of the two ridge systems some 25 million years ago. Alvinella spp. and P. sulfincola
have probably evolved separately. Alvinella spp. is the more derived form; epidermal structures that accomodate
epibiotic bacteria and organized tube ultrastructure are two examples of die specialized traits that have appeared in
this genus. DESBRUYEres & LAUBIER (1991) propose an early separation of die genus Alvinella from evolutionary
lines taken by the Paralvinella species.
The fact that Paralvinella sulfincola colonizes die same high temperature, high sulfide environment as
Alvinella spp. raises questions about die importance of die Alvinella spp. epibiodc bacteria. P. sulfincola is able to
enzymatically oxidise sulfide, as are many benthic polychaetes from non-vent environments. Alvinella spp.
probably does die same, and the example of P. sulfincola indicates that this capability should be enough to allow
die animal to survive and grow on sulfide chimneys. Then why die symbiosis? The elaborate adaptation of die
epidermis to accomodate bacteria indicates that diis is more than a simple case of epizooic growth of bacteria.
Perhaps die symbiosis reduces die energetic cost of sulfide oxidation to animal. This may explain the larger body
size of Alvinella spp. compared to P. sulfincola. Average wet weights for A. caudata and 4. pompejana are 845
and 783 mg, respectively (TUNNICLIFFE, pers. comm.), whereas wet weights for P. sulfincola me around 325 mg
(Juniper etal. 1992).
The type of nutritional relationship between Alvinella spp. and its episymbionts first proposed by ALAYSE-
Danet el al. (1986) has never been demonstrated in any other organism. Apart from an ability for DOM uptake
by the epidermis of Alvinella spp., not uncommon among invertebrates, there is little evidence to support any
transfer of metabolites from die epibiotic bacteria to die worm. On die odier hand, there is good reason to suppose
diat Alvinella spp. and die sulfide worm are deposit feeders. Both worms are anatomically capable of deposit
feeding and bodi are known to ingest particulates from dieir immediate environment. Widiout furdiur evidence for
symbiosis in Alvinella spp., deposit feeding remains its most likely mode nutrition. The fact dial P. sulfincola is
able to nourish itself in die same habitat widiout episymbionts further supports deposit feeding as the primary
mode of Alvinella spp. nutridon. A similar grazing/detritivorous mode of nutrition appears to have been adopted
by die Bresiliid shrimp on chimneys al Mid-Adantic Ridge vents. In die absence of vent polychaetes, swarms of
shrimp ingest mineral particles and adhering bacteria from die surfaces of black smoker chimneys (V an Dover el
al. 1988; Segonzac, 1992).
The influence of Alvinella spp. on chimney mineralization has not been examined in die same detail as have
die effects of P. sulfincola. From descripdons by Haymon & Kastnf.r (1981) and DesbruyEres el al. (1985), it
would appear dial Alvinella spp. influences chimney morphology to a greater degree than does P. sulfincola. In
their account of the texture of black smoker chimney samples from East Pacific Rise vents, Haymon and
KASTNER (1981) note an abundance of interconnected caviues in die outer part of die chimney that are clearly
remains of Alvinella spp. Another type of edifice, die white smokers or snow ball diffusers of EPR vents are
referred to as biogenic edifices created by Alvinella spp. (FUSTEC el al, 1987). No equivalent structures are known
from northeast Pacific vents, even though the chemistry of the source fluids for edifice construction is similar
(TUNNICLIFFE el al, 1986: Von Damm & BlSdlOFF, 1988; BUTTERFIELD, 1990). How Alvinella spp. shapes
chimney morphology is not known. One possible mechanism may involve the effect of convective circulation of
cold seawater through die worm's U-shaped tube. Alvinella spp. contructs its tube so that the central portion of die
lube is cemented against the chimney wall, with the anterior and posterior openings extending into die surounding
seawater. This configuration allows a convective movement of seawater through die tube, that is driven by heat
460
S.K. JUNIPER
How into the lube from the chimney wall. Mineralogical studies of Alvinella spp. lubes indicate that convective
cooling around the tubes locally reduces chimney wall temperatures enough to saturate metal-bearing fluids and
cause mineral precipitation (DESBRUYkilES et al .. 1985). This convectively driven MsupercoolingM extracts heat
from the entire chimney structure. It may occasionally be of great enough magnitude to reduce temperatures deep
inside the chimney wall, increasing local precipitation of minerals from high temperature fluids. This could
increase outward accretion of chimney material at the expense of upward accretion, and cause some young
chimneys to develop into snow’ ball structures. Whatever die mechanism, it is clear that Alvinella spp. is capable
of a much greater degree of habitat modification than its counterpart at northeast Pacific vents, Paralvinella
sulf incola. One notable difference between East Pacific Rise (EPR) and northeast Pacific vents is die relative
rarity of vestimentiferans on chimneys at EPR. Is this a result of habitat modification by Alvinella spp ?
CONCLUSION
While P. sulfincola and Alvinella spp. both exploit the high temperature chimney habitat of their respective
spreading ridges, Alvinella spp. appears to be more elaborate in its adaptauons to diis environment. The functional
significance of some of these adaptauons remains to be clarified. Alvinella spp. may react to chimney growth by
frequently abandoning lubes and migrating to new areas, as has been observed for P. sulfincola. Or, the more
elaborate tube architecture and greater influence of Alvinella spp. on chimney morphology may be indicative of an
organism diat is better able to control its local microenvironment, and so reduce the frequency (compared to the
sulfide worm) of tube abandonment. Time lapse photography was used to study tube building and migration of
sulfide worms (JUNIPER et al. , 1992; TUNNICLIFFE et al ., 1993), and could probably be used to determine whether
or not Alvinella spp. behaves similarly. In light of recent work on die effects of sulfide worms on chimney
mineralization, the entire question of how Alvinella spp. influences chimney growth patterns needs reexamining.
As well, this comparison has shown dial die two roles proposed for the epibiotic bacteria in Alvinella spp.,
nutrition and detoxification, can be accomplished by P. sulfincola without the aid of episymbionts. This is a strong
argument for a re-examination of the nature of the Alvinella -bacteria symbiosis.
ACKNOWLEDGMENTS
Financial support for tiiis work was provided by the NSERC Canada. Comments by Verena TUNNICLIFFE and
Ian JONASSON were valuable in developing tiiis manuscript. Daniel DesbruyEres and an anonymous referee
provided helpful reviews, llenriette Gagnon prepared the figures.
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Source : MNHN. Paris
48
Polychaete assemblages along a depth gradient
in a Spitsbergen Fjord
Michael A. KENDALL
Plymouth Marine Laboratory
Prospect Place
Plymouth PL1 3 Dll, U.K.
ABSTRACT
Samples were taken at five depths in Sassenfjord. Spitsbergen (78°23’N - 16°23'E) during July 1990. Although
essentially Arctic in character, this west coast fjord is also affected by the Atlantic water of the West Spitsbergen Current
and both influences can be seen when one investigates the biogeographical affinities of the polychaete fauna. Diversity
did not differ significantly from analogous sites previously sampled at lower latitudes. Polychaetes were numerical
dominants at all stations and biomass dominants at all but one. The shallowest stations (30-95 m) appeared to be
influenced by seasonal sediment deposition from an adjacent stream and could be shown to be in an intermediate state of
disturbance. At these shallow sites the characteristic species were Chaetozone setosa, Lumbrineris magnidenta, Tharyx
sp. indet., Cossura longocirrata, Polycirrus arcticus and Chone duneri. At the deepest site (123 m) the faunal
composition of the assemblage changed considerably and the standing crop wet weight biomass increased to in excess of
100 g.m-2. This substantial increase was largely due to four polychaete species, Maldane sarsi, Spiochaetopterus
typicus, Terebellides stroemi and Pectinaria hyperborea.
RESUME
Assemblages annelidiens le long d'un gradient de profondeur dans un fjord du Spitzberg
Des prelevements out ete effectues a cinq profondcurs dans le Sassenfjord, Spitzberg (78°23’N - 16°23'E), en juillct
1990. Bien que de caractere essentiellement arctique, cette cote ouest du Spitzberg est aussi sous l’influence des eaux
atlantiques du courant du Spitzberg occidental el les deux influences peuvent etre constatees lorsqu'on etudie les affinites
biogeographiqucs de la faune de polychetes. La diversite ne differe pas sensiblemcnt dcs sites analogues precedemment
(Studies a des latitudes plus basses. Les polychetes etaienl numeriquement dominants dans toutes les stations et leur
biomasse aussi, a l'exception d’une station. Les stations les moins profondes (30-95 m) apparaissaient etre influencees
saisonnierement par les apports sedimentaires d'un courant adjacent et pourraient etre considerees comme presentant un
stade intermediate d'instabilite. Les especes caractSristiques de ces sites peu profonds etaient Chaetozone setosa,
Lumbrineris magnidenta. Tharyx sp. indet., Cossura longocirrata. Polycirrus arcticus and Chone duneri. A la station la
plus profonde, la composition faunistique du peuplement etait considerablement changee et la biomasse exprimee en
poids humide etait supcrieure a 100 g. nr2. Get accroissement substantiel etait essentiellement dQ a quatre especes de
Polychetes. Maldane sarsi. Spiochaetopterus typicus, Terebellides stroemi et Pectinaria hyperborea.
KENDALL, M.A.. 1994. — Polychaetes assemblages along a depth gradient in a Spitsbergen Fjord. In: J.-C. DAUVIN,
L. LAUB1ER & D.J. REISH (Eds), Actes de la 4cme Conference internationale des Polychetes. Mem. Mus. natn. Hist. nat..
162 463-470. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
464
M.A. KENDALL
INTRODUCTION
A number of authors (Abele & Walters, 1979 a, b; Warwick & Ruswahyuni, 1987) have challenged
Sanders (1968) assertion that a gradient in macrobenthic diversity exists between the poles and the tropics.
Warwick & Ruswahyuni 0987)" suggested that the issue should be re-addressed by the collection ol new data
sets which should be collected and analysed using fully standardised methods. I'o this end, they compared the
diversity profiles of shallow sediments in Java and in die North Sea and showed no sigmficant difference in a
diversity between analogous sites in die two areas. The comparison has been extended to the fauna ol Sassentjord,
Spitsbergen (78°N), by Kendall & Aschan (1993) who were also unable to find dilferences between the three
areas in the diversity of die infaunal macrobenthos.
At all of die stations studied in die Sassenfjord, polychaetes were the single most abundant phylum, but in the
context of their paper, Kendall & Aschan (1993) were unable to describe their pattern of distribution along the
depth gradient which was sampled. One aim of this paper is to redress that shortcoming, as comparatively tew data
from such hi°h latitudes exist and the comparison of those that do is fraught widi ditficulties resulting from
methodological inconsistencies. In the context of die latitudinal diversity study referred to above, an attempt will
be made to determine if die fauna of the area studied can be regarded truly representative of Arctic latitudes.
MATERIAL AND METHODS
Five stations near Gipsvika. a bay in the Sassenfjord (west coast of Spitsbergen), were investigated. Stations
will be referred to by their depth (Fig. 1). Samples were collected during July 1991 using a van Veen grab operated
from the R V lohann Ruud. The sediment at the four shallowest stations was a silt with < 6 h sand, while at the
123 in station the silt contained 13 % sand. Kendall & Aschan (1993) have used the ABC method of
Warwick (1986) to show that there is a disturbance gradient between the 30 m and 123 m sites.
PlG. 1. The location of the sampling sites in the Sassenfjord. The sites are referred to by their depth. The inset map of
the Svalbard Archipelago indicates the position of Sassenfjord.
Source . MNHN. Pahs
POLYCIIAETES ASSEMBLAGES IN SPITSBERGEN FJORD
465
The fauna was extracted from each of the five replicates taken at each station by gently washing the sediment
through a 0.5 mm square aperture sieve. l'he residue was fixed in formalin and preserved in 70 % ethanol. In the
laboratory, all animals were extracted from the residual debris with the aid of a binocular microscope and were
identified to putative species. Where possible, speciqs have been named following I IOWSON (1987). At all depths
the samples contained large numbers of cirratulid polychaetes, many of which were damaged. For the purposes of
community analyses the following genera have been grouped together: Chaetozone, Caulleriella and Tharyx. In
many other cases complete identification has not yet been possible and so a full species list will not be presented
in this paper, full details are available from the author. The blotted wet weight of each putative species was
determined, as dry weighing destroys potentially valuable taxonomic material. Instead, dry weights have been
estimated its 25 % of the wet weight (Warwick & Ruswahyun, 1987). Species abundance data were subjected to
non parametric multidimensional scaling (MDS analysis) using the Bray Curtis measure of similarity and group-
average sorting after double square root transformation.
RESULTS
COMMUNITY ANALYSIS. — MDvS analysis of the data on taxa from all phyla shows a clear pattern which can be
related both to depth and to sediment granulometry. All the replicates taken between 30 m and 95 m lie in order
along the central axis of the plot (Fig. 2) with the shallowest sites at the top right-hand side and the deepest sites
to the bottom left. This indicates a gradual change in die composition of the fauna with increasing depth The
MDS Plot for Sassenfjord Macrofauna
Fig. 2. MDS plot comparing stations at different depths on the basis of all species present. Each replicate is plotted
separately.
deepest station was clearly distinct from die shallower sites; on die MDS plot all replicates cluster together in the
top left-hand corner. Figure 3 shows dial at all depdis annelids account for between 46 % and 59 % of all species
and between 50 and 67 % of all individuals. Their contribution to the standing crop biomass is more variable
(28 % at 73 m to 95 % at 123 m) but nevertheless they can be considered the dominant phylum.
Patterns in annelid distribution. — Although there were 69 annelid taxa recorded, 14 of diese account for
95 % of die individuals and 17 account for 95 % of the annelid biomass. The mean number of taxa per sample
was greatest at the shallowest (30 m) site with a mean of 31 ± 3 (SD) but subsequently fell to between 23 and 24.
No more dian 36 annelid taxa were recorded in any single grab sample.
466
M.A. KENDALL
%
100
30 35 72 95 123
Depth metres
1H % Species ESM % Biomass 1 1 % Individuals
Fig. 3. Bar histogram demonstrating the importance of polychaetes in the Sassenfjord assemblages.
MDS was used to cluster together species with similar patterns of distribution. For this analysis only the 14
most abundant species were considered. Figure 4 shows a major group of 10 species with four outliers. The two
MDS: Polychaete abundance MDS: Polychaete biomass
Fig. 4 (left). — MDS plot comparing polychaete species in terms of their abundance at each depth. Key: Agl =
Aglophamus malmgrenr, Amp = Amp hare te finmarcliica\ Api = Apistobrcinchus tullbergi'r, Aric = Aricidea indet.; Bin
= B rada inhabilis ; Bvi = Brada villosa; Cho = Chone duneri\ Cir = Cirratulidae; Cos = Cossura longocirrata\ Dorv =
Dorvillia rubrovitiata : Mel = Heteromasius filiformis\ Lao = iMonice sarsi\ Lang = Langerhansia comma: ; Lev =
Levinsenia gracilis ; Lfr = Lumbrineris fragilis\ Ltet = Lumbrineris magnidenta ; Msar = Maldane sarsi; Nep = Nephiys
ciliata ; Pec = Pectinaria hyperborea ; Pho= Pholoe synopihalmica : Phy = Phyllodoce groenlandica : Pol = Polycirrus
arcticus \ Sco = Leiioscoloplos indet.; Spc = Spiochaetopicrus typicus\ Tstr = Terebellides stroemi.
Fig. 5 (right) — MDS plot comparing polychaete species in terms of their biomass at each station. For key see Fig. 4.
Source : MNHN , Paris
POLYCHAETES ASSEMBLAGES IN SPHZB ERGEN FJORD
467
species positioned above (his group, Pholoe synopthalmica and Aricidea indet. are shallow water animals with
poor penetration to greater depths. Chone duneri has a somewhat similar distribution but is more strongly
represented below 35 m. The species lying to the right of the main group ( Dorvillia rubrovittata and
Spiochaetopterus typicus) are characteristic of deeper water. The remaining taxa were well represented at all depths
but Lutnbrineris magnidenta , die Cirratulidae, Cossura longocirrata mid Maldane sarsi were particularly abundant at
the 35 m station. In the latter case, most individuals at such shallow depths were small and immature.
Leitoscoloplos indet. was evenly distributed between sites but Terebellides stroemi showed peaks in abundance at
die shallowest and the deepest site. Once again, there was a substantial difference in the size of the animals with
depth, the smallest individuals being at die shallowest sites.
A slightly different view of the assemblage emerges when one considers die distribution the various annelid
species in terms of their biomass rather than dieir abundance. Only the 17 species accounting for 95% of die total
biomass were included in the analysis. While many species which were considered important on the basis of
abundance remain for consideration, they are joined by odiers which are larger but less common. In die MDS plot
based on biomass data (Fig. 5) diere is a central grouping of species having a broad dcpdi distribution. This bears
similarities to central grouping of die abundance plot (Fig. 4) as it contains the cirratulids, Lutnbrineris
magnidenta , Maldane sarsi , Terebellides stroemi and Leitoscoloplos indet. Above this group lie Laonice sarsi and
Polycirrus arcticus : the first of these was best represented at 72 m while the latter was numerous at die 35 m
station. Below the central grouping in Fig. 5 lie species which were characteristic of the 123 m site: Pectinaria
hyperborea , Spiochaetopterus typicus and Terebellides stroemi At diis depth polychaetes account for 95 % of the
mean community wet weight biomass (101 ± 3 g. m-2) and the greatest part of this is due to diese diree species
plus large individuals of Maldane sarsi . The remaining species in diis grouping. PhyUodoce groenlandica occurred
throughout the depdi range but at shallower sites it was only represented by small individuals. Around the clusters
which have already been discussed lies an arc of species which are included in die analysis by virtue of dieir large
body size but, as they tire comparatively rare, were not efficiently sampled by the sampling strategy which we
employed: little importance can be attached to dieir distribution on the MDS plot. This group is composed of
Aglophamus malmgreni, Nephtys ciliata , Lutnbrineris fragilis. tui unidentified species of Euclymene , Brada villosa
and B. inhabit is.
DISCUSSION
The benthic fauna of muddy sediments in Sassenfjord undergoes a gradual change in composition between
30 m and 93 m but before 123 m there is a clear transition from a moderately diverse community of animals of
small body size, to an assemblage which has a high standing crop biomass and is dominated by large polychaetes.
l'his does not appear to be a simple function of depth alone. Sassenfjord lies more than 70 km from the open sea
and is ice-covered for much of die year: wave-induced disturbance is unlikely to be significant at any but the most
shallow of sites. As KENDALL & Ascii AN (1993) have pointed out, it is more likely dial the intensity of sediment
deposition from the Ciipselva stream will vary with distance from its outflow and with depth and so influence the
benthic fauna. A similar situation is described in the Hornsund Fjord in the south of Spitsbergen by Gorlish el
ai (1987) who suggest that the high rate of sediment deposition close to a glacier dilutes any available organic
matter with indigestible material. This condition is exacerbated by low levels of bioturbation in the sediment and
low primary production in die turbid water column. As die rate of sediment deposition decreases and bioturbation
increases so does die abundance of benthic life. In such situations in die Canadian Arctic, Syvitski et al. (1989)
have described a transition from a shallow assemblage dominated by the bivalve YoldieUa to a deeper assemblage
characterised by Maldane sarsi ; such a sequence was observed in die Sassenfjord.
In surveys around Raudfjord (N. Spitsbergen) and van Mijen Fjord (W. Spitsbergen), GULLISKEN et al. (1985)
found the most abundant fauna outside the fjords with a decrease towards the innermost transects where diey
recorded no more than 8-10 species of all phyla in each 0.1 m2 sample. They attribute this impoverishment to
high levels of siltation and poor water exchange. Direct comparison with studies such as this and that of Gorlish
et al. (1987). is difficult as the sampling methods used were not consistent; while GULLISKEN et al. (1985)
separated die fauna from die sediment using a 1 mm mesh, GORLISH et al. (1987) employed one of 2 mm. It is
equally difficult to be sure how the results of their analyses compare with those of the Sassenfjord study. While die
larger meshes would tend to underestimate the abundance of species with small body size, there would be little
difference in estimates of biomass. Nevertheless, it seems that the Sassenfjord fauna might be unusually rich as
GULLISKEN et al. (1985) record diversity values similar to those which have been calculated in the present study.
468
M.A. KENDALL
despite the probability that they underestimated the abundance of the smallest individuals. WESLAWSKI el al
(1990) consider the area unusually rich in comparison with other Spitsbergen fjords. Although the sampling sites
in S asset) fjord were clearly under the influence of suspended matter deposited by the Gipselva stream, if the
conditions described by Whslawski et al. (1990) are typical (Sccchi disc depths of 3-8 m) then it is unlikely that
,hc sedimentation regime is as severe as in the other tjords. It is also possible that local upwellmg (Wesi.awski et
al.. 1990) may stimulate primary production in the water column to levels greater than those elsewhere in
Spitsbergen. Such intermediate levels of disturbance accord well with the ABC plots of Kendall & Aschan
(1993) and may well account for the high diversity of this area.
Sanders (1968) claimed dial there was a polar- tropical gradient in the macrobcntliic fauna ol solt sediments.
When the fauna of the 123 m site in Sassenljord was compared with a similarly disturbed offshore sandy mud in
the North Sea. using directly comparable methods, little difference could be observed in their a-diversily protiles
(Kendall & Aschan. 1993). The polychaete component of the infauna of the two areas was broadly similar,
both in the number of species and in wet weight biomass, although at the Arctic site the mean density of
individuals was higher (Kendall, unpublished). These observations support THORSON's (1957) assertion that die
infauna does not show the same degree of latitudinal variability as the epifauna. However, such an inference
assumes that both of the locations have a faunal diversity which is typical of their latitude. While there is no cause
to question the representativeness of the North Sea site, it is not clear just how well Sassenfjord represents Arctic
conditions. Certainly, physical data suggest that the area is a good example; al 78°N the sun is below the horizon
from the start of November until the end of February, fjords are ice-covered from 6-10 months of the year
(Eilerstsen et al., 1989) and in die Sassenfjord itself the bottom temperature during summer is less than 0.5 °C
(WESLAWSKI et al.. 1990). On the other hand, faunal evidence suggests that the area is not fully Arctic.
While the composition of the Sassenfjord fauna shows strong Arctic influences, boreal and/or cosmopolitan
polychaete species appear to be disproportionately important when their contribution to die total abundance or
biomass is considered. Many of die species sampled in the Sassenfjord are also commonly recorded in die North
Sea (cf. Buchanan & MOORE, 1986) This confirms a finding from other Ijords on die nordi and west coasts ol
Spitsbergen (Gt'LLISKEN et al.. 1985). In reporting their study they claim that all the polychactcs dicy encountered
were recorded from both Arctic and boreal waters. STROMBERG (1989) loo records the importance of boreal species
in this area and attributes their importance to the influence of the Atlantic water of the northern-flowing West
Spitsbergen Current. In the Beaufort Sea (71°N). Bilyard & Carey (1980) have also observed substantial
numbers of non-endemic species in water shallower than 300m, but rather than attributing their presence to
wanning currents they relate their presence to inter-glacial invasions. The real extent of this boreal intrusion into
Spitsbergen waters may not, however, be as great as die data immediately suggest. The status of a number of the
more important boreal, or cosmopolitan species of the area has been questioned in recent years; among these are
Terebellides stroemi (Williams, 1984). Tharyx (Blake, 1991), Cliaetozone (Christie, 1985), Cossura
longocirrata (FOURNIER & PETERSEN, 1991) while Light (1991) lists four sub-species of Maldane sarsi. It is
possible that other "species" with very broad ranges might similarly prove to be complexes of sibling species. It is
unlikely that the existence of a substantial proportion of non-endemic species in Sassenfjord is in any way unusual
for a shallow water Arctic assemblage.
Zenkevitch (1963) recognised six major macrofaunal assemblages in the adjacent Barents Sea and none of
these had the faunal characteristics recorded in Sassenfjord. In a broad scale study of the Arctic Chukchi Sea and the
sub- Arctic Bering Sea. Grebmaier et a/., (1989) have described 1 1 different assemblages which vary substantially
in die identity of the dominant phylum. In doing so, they demonstrated the relationship between the properties of
the sediment and the community it supports. Nevertheless, the most northerly mud community which was
described, and hence that which was most comparable to that in Sassenfjord, was clearly dominated by amphipods
rather than by polychaeles. This serves to emphasise die potential for variation in the structure of Arctic
assemblages and so brings the present study into perspective. The comparison between an Arctic site and
analogous sites in the North Sea and Java (Kendall & ASCHAN, 1993) has shown few differences in die a-
diversity of either the whole community or the polychaete component ol' it. On the basis of such a limited
comparison it would be unrealistically hasty to dismiss existing hypotheses concerning latitudinal variability in
patterns of infaunal diversity. Even in a study in which an effort is made to hold variables such as sediment type
and depth as constant as possible, we must expect to encounter a variety of communities each of which will have
its own diversity properties. As yet we cannot be sure of die position of the Sassenfjord sites within such a range.
For this reason, if we are to address the problem of latitudinal patterns of diversity we must first establish die
range of variation within die areas which we are comparing.
Source :
POLYCHAETES ASSEMBLAGES IN SPrrZB ERGEN FJORD
469
ACKNOWLEDGEMENTS
I would like to thank Michaela Aschan of the University of Tromso for arranging my visit to Spitsbergen,
and Dr R.M. Warwick for his comments on the manuscript.
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BlLYARD. G.R. & Carey Jr.. A.G.. 1980. Zoogeography of western Beaufort Sea Polychaeta (Annelida). Sarsia , 65 :
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BLAKE, J. A. 1991. — Revision of some genera and species of Gilratulidae (Polychaeta) from the western North Atlantic.
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CHRISTIE, G. 1985. — A comparative study of the reproductive cycles of three Northumberland populations of Cliactozone
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FOURNIER J.A. & PETERSEN, M.E., 1991. - Cossura longocirraia: Redescription and distribution, with notes on
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63-80.
GORLICH, K.. WesLAWSKII. J.M. & Zaj ACKOWSKl. M.. 1987. Suspension settling effect on macrobenthos biomass
distribution in the Hornsund Fjord. Spitsbergen. Polar Research . 5 : 175-192.
GREBMEIER. J.M.. FEDER. I I.M. & McRoy, C.P.. 1989. — Pelagic benthic coupling on the shelf of the northern Bering
and Chukchi Seas. II Benthic community suucture. Mar. Ecol. Prog. Ser., 51 : 253-268.
GULLIKSEN B.. HOLTE, B. & JAKOLA. K-J.. 1985. — The soft bottom fauna in van Mijen fjord and Raudfjord. Svalbard. In :
J.S.GRAY & M.E.CHRISTIANSEN (eds). Marine Biology of Polar Regions and Effects of Stress on Marine Organisms.
John Wiley & Sons : 199-211.
IIOWSON. C.. 1987. - Directory of the British marine fauna and fora. A coded checklist of the marine Jlora and fauna of
the British Isles and its surrounding seas. Marine Conservation Society. Ross on Wye. 471 pp.
Kendall, M.A. & Aschan. M., 1993. — Latitudinal gradients in the structure of macrobenthic communities: a
comparison of Arctic temperate and tropical sites. J. exp. mar. Biol. Ecol. 172 : 157-169.
Light. W.J.IL, 1991. — Systematic revision of the genera of the polychaete subfamily Maldanidae Arwidsson. Ophelia.
suppl. 5 : 133-146.
SANDERS. ILL.. 1968. - Marine benthic diversity : a comparative study. Am. Nat.. 102 : 243-282.
ST ROM BERG, .1-0.. 1989. Northern Svalbard waters. In : L. REY. L. and V. ALEXANDER (eds). Proceedings of the 6th
Comite Arctique International. 13- 15 May 1985. Brill. Leiden : 402-426.
Syvitski, J.P.M.. Farrow. G.E.. Atkinson, R.J.A.. Moore, PC.. & Andrews, J.T.. 1989 Baffin Island Fjord
Macrobenthos: Bottom Communities and Environmental Significance. Arctic. 42 : 232-247.
THORSON. G. 1957 Bottom communities (sublittoral or shallow shelf). In : J.W. I-lEDGPETH (ed.). Treatise on marine
ecology and paleoecology. Geological Society of America: New York 461-534.
Warwick R.M.. 1986. A new method for detecting pollution effects on marine macrobenthic communities. Mar.
Biol.. 92 : 557-562.
Warwick. R.M. & RUSWAHYUNI. R.M.. 1987 Comparative study of the structure of some tropical and temperate
marine soft bottom macrobenthic communities. Mar. Biol. 95 : 641-649
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WESLAWSKI. J.M.. WASNIEWSKI, S.K.. S.SWERPWL, S., WlCTOR. L. AJACZKOWSKl, NL. OSTROWSKI. M. & SlWECKI. R. ,
1990. Summer environmental survey of Gipsvika, Svalbard. Norsk Polarinstitutt Rapport, 62 111-131.
WILLIAMS S L. 1984. The status of Terebellides stroemi (Polychaeta Trichobranchidae) as a cosmopolitan species
based on a world-wide morphological survey including descriptions of two new species. In: P.A. HUTCHINGS (edO,
Proceedings of the First International Polychaete Conference. Sydney. Linnean Society ol New South Wales: 118-
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Source : MNHN. Paris
49
The biogeography of some abyssal Polychaetes
J0rgen B. KIRKEGAARD
Zoological Museum, Universitetsparken 15
K-2100 Copenhagen. Denmark
ABSTRACT
The Danish Galathea Expedition obtained polychaetes from 83 stations in the bathyal and abyssal zones of the South
Atlantic. Indian, and southern Pacific Oceans; 104 species were identified. On the basis of the distribution of some of these
species and results from earlier publications a biogeographical analysis is given. The species treated in detail were: Laelmonice
benthaliana McIntosh, Leanira quatrefagesi Kinberg. Aglaophamus elamellaia Eliason. Bathyeliasona kirkegaardi
(Uschakov), B. nigra (Hartman) and Paradiopatra paucibranchis (Ehlers). This analysis showed a worldwide distribution of
many abyssal polychaetes. The abyssal and hadal polychaetes are derived from the polychaete fauna in the bathyal zone. Many
of these species were eliminated during the glacial ages when temperatures in the deep sea dropped from 10 °C to 2 °C. The
present deep-sea polychaete fauna consists of eurythermic and curybathic species, relics of a preglacial fauna, and new
invaders from the bathyal zone.
RESUME
Biogeographic dc quclqucs Polychetes abyssaux
L 'expedition danoise de la "Galathea" a recolte dcs polychetes dans 83 stations, dans les zones bathyalc ct abyssale de
l'Atlantique du Sud. de I 'Ocean Indien et du Pacifique du Sud. Cent qualre especes out ete identifies. II cst fourni, sur la base
de la distribution dc quelques unes de ces especes et de resultats anterieurs, une analyse biogeographique. Les especes
suivantes out ete etudiees en detail : Laelmonice benthaliana McIntosh. Leanira quatrefagesi Kinberg, Aglaophamus
elamellaia Eliason. Bathyeliasona kirkegaardi (Uschakov),/?. nigra (Hartman) et Paradiopatra paucibranchis (Ehlers). Les
polychetes abyssaux et hadaux derivenl de la faune de polychetes de la zone bathyale. Plusieurs de ces especes out disparu au
cours des periodes glaciaires. quand les temperatures dans l'ocean profond baissaient de 10 °C a 2 °C. II en resulte que la faune
actuelle de polychetes de l'ocean profond se compose d'cspcces eury therm es et curybathes, des restes d'une faune pre-glaciaire.
et de nouveaux envahisseurs de la zone bathyale.
INTRODUCTION
The polychaetes have long been considered to be a group with many cosmopolitan species. In recent years
polychaete specialists have reexamined so-called cosmopolitan species resulting in revision of genera and species
KIRKEGAARD, J.B.. 1994. — The biogeography of some abyssal Polychaetes. In: J.-C. DaUVIN, L. LaUBIER & D.J. Rf.ISII
(Eds). Actes de la 4cme Conference Internationale des Polychetes. Mdm. Mus. natn. Hist, nat., 162 : 471-477. Paris ISBN 2-
85653-214-4.
Source MNHN , Paris
472
J.B. KIRKEGAARD
in many families. This has shown liiat in many cases (he purportedly cosmopolitan distribution in the oceans was
due to inadequate descriptions or lack of comparison with type specimens. As a result many of (he so-called
cosmopolitan species have been splil up into several species with a more restricted distribution. However, (Ins is
probably not true of polychaetes living in (lie deep sea.
DEEP-SEA POLYCHAETES
Before 1940 little was known about the deep-sea fauna. Our knowledge of the deep-sea polychaetes was based
mostly on the investigation of the "Challenger" expedition (MCINTOSH, 1885). Since die late 1940s several
expeditions have investigated deep-sea fauna widi research vessels such as die Swedish "Albatross", die Danish
"Galathca", the Soviet "Vitiaz" and the American "Anton Bruun". Later, British, German, French, and Japanese
research vessels sampled bathyal, abyssal and hadal bottoms. We now have more detailed knowledge of the
polychaete fauna of the deep sea, however, since more than half of die world's oceans is occupied by the abyss,
only a small part has been sampled.
The Danish "Galathea" expedition round the world in 1950-52 collected polychaetes from 97 deep-sea
stations. These stations were situated in die Southeast Atlantic, die Indian Ocean and the South Pacific. Fourteen
of the stations were located in trenches deeper dian 6,000 m. die so-called hadal region, from which 15 species
were obtained (Kirkegaard, 1956). The remaining 83 stations were from the abyssal (43) and bathyal (40)
regions. The errant species from these 83 stations have been identified and comprise 104 species from 17 families
(Kirkegaard, in prep.). These species were obtained using several different gears, including sledge trawls,
commercial trawls, dredges, and Petersen grab. The material was washed through sieves of different mesh size, the
smallest with a mesh of 1 nun. However, die results from this expedition and from other expeditions (Levenstein,
1962, 1971. 1975, 1978a. b. 1984, 1991: USCHAKOV, 1955) make it possible to draw some conclusions on the
biogeography of deep-sea polychaetes.
The abyssal plains stretch from soudi of Greenland southwards through the Atlantic, south of Africa to the
Indian Ocean, south of Australia and into the Pacific. These plains occupy the bottom of nearly all of the large
oceans, 27.3 million kmT The conditions for life are similar throughout these large areas: 2-4 °C, 35 P.S.U.
salinity, oxygen: 4 ml. H pressure: 200-600 atm., and darkness (Bruun, 1956). It is on these large areas with
similar conditions for life from one ocean to another that cosmopolitan species, if they exist, might be expected to
occur.
RESULTS
Laetmonice benthaliana McIntosh, 1885
(Day, 1967, fig. 1.1 f-i) Fig. 1.
RECORDS. — Laetmonice pwducta var. benthaliana McIntosh, 1885 p. 45 pi. 8, figs 4-5, pi. 4A. tig. 12, pi.
5A figs 1-2. — Laetmonice producla benthaliana HARTMAN, 1964 p. 12. pi. 1 figs 4-5. — Laetmonice
benthaliana Uschakov. 1962 p. 147: Day, 1963 p. 356, 1967 p. 33.
MATERIAI. examined. — St. 186. SE of Natal, 32°33'S, 32°01'E, 3620 m. SOT. two specimens: 50 x 20 mm
(complete. 34 setigers), 50 x 20 mm (bad condition). St. 192, off Durban, 32°00'S, 32°41'E, .3,530 m, SOI. live
complete specimens, 34 setigers: 20 x 5, 35 x 15, 40 x 15, 45 x 15, 45 x 20 mm; one destroyed specimen. St. 198.
off Durban, 30°32'S. 34°27'E. 2,700 m, STI00, one complete specimen, 34 setigers: 34 x 12 mm. St. 217,
Mozambique Channel, 14°20'S. 45°09'E, 3,390 in, HOT, one complete specimen, 34 setigers: 40 x 15 mm. St.
233, N of Madagascar, 7°24'S, 48°24'E. 4.720 in, ST300, one specimen, 34 setigers: 55 x 20 mm. St. 2.35. E of
Mombasa, 4C47\S 46°19'E, 4,810 m, HOT, 1 specimen, 34 setigers: 60x15 mm. St. 238. off Kenya, 3°23'S,
44°04'E, 3.960 m, 43 specimens: 50 x 20 mm. St. 241, off Kenya, 4°00'S, 41°27'E, 1,510 m, HOT. one specimen:
10 x 5 mm (smashed). St. 601, SW of New Zealand, 45°51’S. 164°32'E, 4,400 m, HOT. seven complete
specimens, 34 setigers: 35 x 10-45 x 15 mm. three fragments: 20 x 8-40 x 15 mm. St. 607, SW of New Zealand,
44°18'S, 166°46'E, 3,580 m, HOT, 10 specimens, 34 setigers: 10 x 5-33 x 15 mm. St. 661. Kermadec Trench,
36°07'S, 178°32'W, 5340 in. ST600. three complete specimens: 23 x 10, 30 x 12, 35 x 12 mm. St. 663, Kermadec
Trench, 36°31'S, 178°38’W, 4,410 m, HOT. 181 specimens 33-34 setigers: 35 x 10-15x5 mm. St. 664,
Source :
BIOGEOGRAPHY OF SOME ABYSSAL POLYCHAETES
473
Kermadec Trench, 36°34'S, 178°57'W, 4,540 in, IIOF, 76 specimens, many destroyed: 35 x 12 mm. St. 665,
Kermadec Trench, 36°38'S, 178°2TE, 2.470 m, HOT. three complete specimens: 20 x 10, 20 x 10. 25 x 12 mm;
one fragment. St. 716, Gulf of Panama, 9°23rN, 89°32'W, 3,570 m. HOT, one specimen: 30 x 10 mm.
Remarks. — This species was originally described as a subspecies of Laeimonice producia by McIntosh
(1885). Uschakov (1962) raised it to species level and Day (1963) agreed. It differs from the stem species by its
smooth venter and by always having 15 pairs of elytra compared to 18-20 pairs in L . producta. The number of
setigers is also smaller, 33-34 in L. be ntha liana , 45-47 in L. producta.
DISTRIBUTION. — Antarctic; Indian Ocean, E and S of Africa, Ambian Sea, S of Ceylon; Pacific, W of New
Zealand, Kermadec Trench, Japan, Central Pacific, Gulf of Panama. 50-6,875 m.
FIG. 1. — Distribution of Laeimonice benthalionci (1). Lcanira quatrefagesi (2), Aglaophamus elameUata (3), Bathyeliasona
kirkegaardi (4), Paradiopatra paucibrcmchis (5), and Bathyeliasona nigra (6).
Leanira quatrefagesi Kinberg, 1855
(PETT1BONE, 1970, figs 1-3), Fig. 1.
RECORDS. — Pethbone. 1970 p. 4: WESENBERG-LUND. 1962, p. 27. Leanira hystricis Day, 1963. p. 360.
Material. — St. 214, off Beira, 20°12'S, 35°15'E, 380 m, PG 0,2, one specimen: 25 x 5 nun (anterior end).
St. 443, Mindanao Sea, 8°48'N, 124°09'E, 1,500 m, ST300, three specimens: 32 x 7, 30 x 8, 22 x 6 mm (anterior
end). St. 453, Makassar Strait, 3°56’S, 1 18°26'E, 2,000 m, ST300, one specimen: 45 x 4 mm. St. 480, S of Bali,
8°49\S 1 1 5°00'E, 440 m, PG 0,2, one specimen: 8 x 0.5 mm (anterior end). St.491, Makassar Strait, 4°56’S,
1 17°39'E, 1,560 m, ST300, one specimen: 22 x 4 mm (anterior end), one fragment. St. 554, Great Australian
Bight, 37°28’S, 138°55'E, 1,340-1.320 m, ST300, 16 specimens: 33 x 1-9 x 0.5 mm (anterior ends). St. 626, W of
New Zealand, 42°10’S, 170°10'E, 610 m, HOT, 10 specimens: 22 x 1-5 x 1 mm (anterior ends), two posterior
Source :
474
J.B. KJRKEGAARD
ends, three fragments. St. 665, Kermadec Trench, 36°38'S. 178°21’E, 2,470 m, HOT, 13 specimens: 32 x 6-12 x 1
mm (anterior ends), eight fragments. ? St. 668, Kermadec Trench, 36°23'S, 177°4rE, 2640 m, HOT, one fragment
(only parapodia with seiae).
Remarks. — This fairly huge number of specimens from different parts of die world agrees with Peltibone's
description and figures.
DISTRIBUTION. — South Atlantic off Argentina, West and South Africa, Indian Ocean oil Mozambique,
Malaya Archipelago, Pacific off Chile, W of New Zealand, Kermadec Trench, Magellan area, Falkland Islands,
Antarctic. 0-6,150 m.
Aglaophamus elamellata (Eliason, 1951)
(ELIASON, 1951, fig. 2), Fig. 1.
RECORDS. — Nephlliys elamellata Eliason, 1951. p. 133: KIRkegaard. 1956, p. 68 fig. 7.
Material. — St. 101, off Angola, 8°50'S 12°32'E, 990 in. ST300, two specimens: 20 x 2 mm (anterior ends).
St. 108. off Lobito, Angola, 12°00'S 13°00'E, 1,470 m, one specimen: 20 x 2 mm (anterior end). St. 192, off
Durban, 32°00'S. 32°41'E, 3,430 m, ST 100, one specimen: 20 x 3 mm (anterior end). St. 193. off Durban, 32°34'S
31°52'E, 3.680 m, SOT. 4 specimens: 22 x 3. 10 x 4, 6 x 2, 3 x 2 mm (anterior ends). St. 194, off Durban, 34°09'S
30°45'E, 4.360 m, SOT. diree specimens: 25 x 2. 18 x 2, 5 x 2 mm (anterior ends). St. 241. off Kenya. 4°00'S,
41°27'E. 1.510 m, HOT. one specimen: 10 x 2 mm (anterior end). St.279, SW of Ceylon, 1°00'N. 76°17'E, 4.320
m, one specimen: 5 x 0.5 mm (complete), juvenile? St. 574. Tasman Sea, 39°45'S 159°39'E, 4,670 m, S 1 600, one
specimen: 22x4 mm (anterior end). St. 601, W of New Zealand, 45°51'S 164°32E, 4,400 m, HOT, diree
specimens: 25 x 5, 16 x 5, 20 x 5 mm. St. 607, off SW New Zealand, 44°18'S: 166°46’E, 3.830 m, VC, 0.2, four
specimens: 15x3, 15 x 3, 15 x 3. 10 x 2 mm (anterior ends). St. 654. Kermadec Trench. 32°10'S 175°54'W,
5.850-5,900 m, HOT, two specimens: 40 x 5, 38 x 5 mm (complete, 54 setigers). St. 663, Kermadec Trench,
36°31'S 178°38’W, 4,410 m, HOT, 18 specimens: 40-10 x 5 mm (anterior ends). St. 664, Kermadec Trench,
36°34'S, 178°57'W, 4,540 m. HOT, one specimen: 15 x .3 mm.
Remarks. — This species was described from specimens found in the Central Atlantic. It was later recorded
by me (Kirkegaard. 1956) from the bottom of die Kermadec Trench. The present records are from many
intervening places and from other stations in the Kermadec Trench. I can find no differences between the Atlantic
specimens and diose from deep water in the Indian Ocean and around New Zealand. It appears that this is a deep
water species widi a cosmopolitan distribution.
Distribution. — Atlantic (Azores, Canary Islands, off West Africa). 990-4,600 m. Indian Ocean (off East
Africa, Ceylon). 1,510-4,360 m. Pacific (Tasman Sea, Kermadec Trench). 3,830-7,000 m.
Bathyeliasona kirkegaardi (Uschakov, 1971)
(PETTIBONE, 1976, figs 15-17), Fig. 1.
Records. — Uschakov, 1971, p. 37; Pettibone, 1976, p. 27; Hartmann-SchrOder, 1975, p. 53.
Macellicephala abyssicola Kirkegaard. 1956, p. 64.
MATERIAL. — St. 654. Kermadec Trench, 32°10'S, 175°54'W, 5,850-5.900 m, HOT. two fragments, two
proboscises.
REMARKS. — The species was idenufied by the setae on an anterior and a posterior end
DISTRIBUTION. — Aleutian Trench, Kermadec Trench, Sunda Trench, off Portugal. 5275-7880 m.
Source :
BIOGEOGRAPHY OF SOME ABYSSAL POLYCHAETES
475
Bathyeliasona nigra (Hartman, 1967)
(PETTIBONE, 1976. figs 18-19). Fig. 1.
Records. — Pettibone. 1976, p. 30. Herdmanella nigra Hartman, 1967, p. 25.
Material. — St. 194, off Durban, 34°09'S, 30°45’E. 4,360 m, SOT, one specimen: 40 x 20 mm. St. 281, SW
of Ceylon, 3°38'N, 78°15'E, 3,310 m, ST300, one specimen: 35 x 10 mm.
Remarks. — The specimen from St. 281 is in bad condition, but the shape of the setae and die black pigment
together with the number of segments and the prostomium agree with Pettibone's description and figures.
However, tlie specimen from St. 194 lacked setae on segment 1 ,
Distribution. — Antarctic (Soudi Sandwich Isl.), Indian Ocean (E of South Africa and S of Ceylon). 2,553-
4,360 in.
Paradiopatra paucibranchis (Ehlers, 1908)
(Elders, 1908, pi. 10 figs 12-16, pi. 1 1 figs 1-6), Fig. 1.
RECORDS. — Diopatra paucibranchis Ehlers, 1908, p. 81. Sarsonupliis paucibranchis Fauchald, 1982, p. 77.
Paradiopatra paucibranchis Paxton, 1986, p. 38.
Material. — St. 182, SE of Durban, 33°28'S, 38°32'E, 5,1 10 m, SOT, one specimen: 18 x 1 mm (bad
condition). St. 192, off Durban, 32°00'S, 32°41'E, 3,430 in, ST100, one specimen: 26 x 1 mm (anterior end). St.
550, NE of Sydney, 3I°27'S, 153°33’E, 4.530 m, ST200, two specimens:20 x 1. 10 x 1 mm (anterior ends), four
fragments. St. 665. Kennadec Trench. 36°38’S, 178°21'E, 2,470 m, HOT, six specimens: 32, 32, 28, 20 x 3 mm,
18 x I. 20 x I mm (anterior ends), fragments, lubes. ? St. 668, Kermadec Trench, 36°23'S, 177°41'E, 2,640 m,
HOT, one specimen: 10 x 0.5 mm (anterior part), one fragment. All in bad condition.
Remarks. — All specimens have six rings on the ceratophores, ventral cirri are cirriform in the first three
setigers and digitate posterior lobes tire present in the first seven setigers. The beginning of branchiae varies
between setigers 16-20. subacicular hooks arc present in some specimens from sedger 9 (as in the hololype). but
in some others from sedger 10.
Distribution. — Antarctic Ocean, 63°16'S 57°5TE, 4,636 m, off South Africa, 3,430-5.1 10 m, Tasman Sea,
4,530 m, Kermadec Trench, 2,470 m.
ORIGIN OF THE ABYSSAL POLYCHAETES
The abyssal fauna is probably derived from die bathyal fauna, from which species that can live under the high
pressure and at low temperatures have spread downwards. Levknstein (1984) pointed out. on the basis of her
analyses of the distribution of die deep-sea polynoids (especially die Macellicephalinae), that these polychaetes
must have had two distribution centers, i.c., the eastern Atlantic Ocean and the western Pacific, which are the
margins of the ancient Tethys Sea. However, during Oligoccne (30-20 MY 13. C.) die temperatures in abyssal
depths decreased from around 10 °C to about 2 °C. This was shown by EMILIANI & Edwards (1953), who
examined the oxygen isotopes of benthic Foraminifera of probably Oligoccne age (30 MY) from the eastern part
of die Central Pacific. This temperature change must have been catastrophic for abyssal and hadal faunas since
only the eurythermic species survived.
The present polychaete fauna of the abyssal and liadalzones must be relics of a preglacial abyssal and hadal
fauna, but besides these old components diere must have been a new and still ongoing invasion of species from die
bathyal zone to the abyss and to the hadal zone. Levenstein (1984) suggested dial additional centers of
distribution could be the eastern Pacific, die Arctic and die Antarctic.
The invasion to the hadal zone must have been from the abyss. Levenstein (1991) showed that of 80
identified species of polychaetes from this zone, 26 (32.5 %) were endemic to the trenches. Seventeen of these
species were found to be endemic to only one trench, whereas die remaining nine were known from two-six
Source :
476
I B. KIRKEGAARD
different trenches, some of them from neighbouring trenches, but also from trenches isolated by great distances in
the Pacific Ocean. Bathykennadeca hcidalis (Kirkegaard, 1956) (Polynoidae) is recorded from the Japan,
Philippine, Yap. Kermadec, Bougainville and Banda trenches. This species is possibly a relict of an old preglacial
polychaete fail na. _ ^ „ T
1 y DISCISSION
As appears from this investigation, there is very little variation in morphology and size over large geographical
distances. Laetmonice benihaliana, which is represented by a fairly large collection, showed no difference from
East Africa to New Zealand and the Gulf of Panama and agreed wife descriptions from fee Antarctic and Central
Pacific. Other species, i.e., Leanira (/uairefagesi, Batliyeliasona kirkegaardi and Baihyeliasonci nigra arc
represented in die material by fewer specimens, but all three species have been revised by PETTI BONE (1970, 1976)
and no differences were found between specimens from localities separated by long distances, i.e.. South
Amcrica-Africa (L qualrefagesi), Kermadec Trench, Aleutian Trench, and Portugal (B. kirkegaardi). PETI'IBONE
(1976) examined a small collection of B. nigra from the Antarctic, but her description and figures agree well with
the present material from off South Africa and south of Ceylon. Similar to this. Paradiopatra paucibrancliis was
revised by Fauchald (1982) on a small collection from Antarctic. His redescription of the holotype agrees well
with the "Galathea" material from south of Africa and east of Australia. A few characters varied from the
holotype, i.e.. the place where branchiae (seiigers 17-36 compared to 16-20) and subacicular hooks begin (9
compared to 10). but this is also known for other species of the genus. Aglaophamus elamellata (Eliason, 1951) is
a species which has only been recorded by me since the original description. However, I have a fairly large
collection from Africa, Ceylon and Australia-New Zealand and compared them with the type and found no
morphological differences.
Some of the material from the "Galathea" was badly damaged, but in many cases fee setae of these damaged
specimens were so characteristic that identification was possible. Many different sampling devices were used, but
there were no connection between fee number, the size or the condition of fee specimens with the type of gear
used. However, all material of the "Galathea" was washed through a 1.0 mm sieve. As mentioned before, many
small polychaetes must have passed through these sieves. Later. 1 (1980) showed feat when a 0.5 mm sieve is
used, small polychaetes are retained on the screen. These species have a wide geographical distribution. Thus
78 % of the 23 species found in the northeastern abyssal part of the Atlantic, were common to the polychaetes in
the abyssal area between New England and Bermuda.
CONCLUSIONS
The present investigation shows that of fee six named species from the "Galathea" expedition, four are
distributed throughout the World, viz. Leanira qualrefagesi, Aglaophamus elamellata. Batliyeliasona kirkegaardi
and B. nigra. The remaining two species: Laet monice bentltaliana and Paradiopatra paucibrancliis. are recorded
from the Indian Ocean and the Pacific and will probably be found in the Atlantic wife additional studies.
Several abyssal species are shown to have a cosmopolitan distribution and several more probably occur.
However, endemism in the deep sea does exist as was shown by Levenstein (1991) in her paper on the
polychaetes in deep-sea trenches, in which 16 of the 26 hadal species in fee trenches were endemic to one trench.
REFERENCES
BRUUN, A.F.. 1956. — The Abyssal Fauna: its ecology, 'distribution and origin. Nature. 177 : 1 105-1 108.
Day, J.H., 1963. The Polychaete Fauna of South Africa. Part 7: Species front Depths between 1,000 and 3.300 Metres
West of Cape Town. Atm. S. Afr. Mus., 46 : 353-371.
Day, J.H., 1967. -- A Monograph of the Potychaeta of Southern Africa. Brit. Mus. (Nat. Hist.), London. 878 pp.
Eulers. E., 1908. Die bodensassigen Anneliden aus Sammlungen der deutschen Tiefsee-Exped. Wiss. Ergebn. deutsch.
Tiefsee-Exped. Valdivia 1898-1899. 16: 1-168.
Eliason. A.. 1951. Polychaeta. Rep. Swed. Deep-Sea Exped.. 2 : 129-148.
EMIL1AN1, C. & Edwards, G.. 1953. Tertiary Ocean Bottom Temperatures. Nature. 171: 887-888.
Source :
BIOGEOGRAPHY OF SOME ABYSSAL POLYCI IAETES
477
FAUCHALD, K., 1982. Revision of Onuphis , Nothria and Paradiopatra (Polychaeta: Onuphidae) Based upon Type Material.
Smithson. Conir. ZooL . 356 : 1 109.
I lARTMAN. O.. 1964. Polychaeta Errantia of Antarctica. Antarctic Res. Ser. Washington , 3:1 131.
Hartman. O.. 1967. — Polychaetous Annelids Collected by USNS "Ellanin" and "Staten Island" Cruises Chiefly from
Antarctic Seas. Allan Hancock Monogr. mar. Biol.. 2 : 1 -387.
Hartmann SCHRODER, G.. 1975. Polychaelcn der Iberischen Tiefsee gesammelt auf dcr 3. Reise der Meteor im Jahre
1966. Milt. Hamb. ZooL Mus. Inst.. 12 : 47-73.
KlRKEGAARD. J.B.. 1956. Benthic Polychaeta from Depths Exceeding 6,000 Metres. - Gcilathea Rep.. 2 : 63-78.
KlRKEGAARL). J.B.. 1980. Abyssal Benthic Polychaetes from the Northeast Atlantic Ocean. Southwest of the British Isles.
Steenstrupia. 6 : 81-98.
LEVENSTEIN. R.Y., 1962. Polychaete Worms from Three Abyssal Trenches of the Pacific Ocean. ZooL Zhur. Akad. Nauk
SSSR. 41 : 1142-1148.
LEVENSTEIN, R.Y., 1971. — Polychaete Worms of the Genus Macellicephala and MaceUicephaloides (Family Aphroditidae)
from the Pacific Ocean. Trudy Inst. Okeanol. P.P. Shi rshov Akad. Nauk SSSR. 92 : 18-35.
LEVENSTEIN. R.Y., 1975. The Polychaetous Annelids of the Deep-Sea Trenches of the Atlantic Sector of the Antarctic
Ocean. Trudy Inst. Okeanol. P.P. Shi rshov Akad. Nauk SSSR. 103 : 1 19-142.
LEVENSTEIN. R.Y.. 1978a. Polychaetes of the Family Polynoidae (Polychaeta) from the Deep-Water Trenches of the
Western Part of the Pacific. Trudy Inst. Okeanol. P.P. Shi rshov Akad. Nauk SSSR. 112. 162-173.
LEVENSTEIN. R.Y.. 1978b. — Annelida (Polychaeta) from the Deep Waters of the Pacific Region of Antarctic. Trudy Inst.
Okeanol. P.P. Shi rshov Akad. Nauk SSSR. 113 : 73-87.
LEVENSTEIN. R.Y., 1984. — On the Ways of Formation of the Deep-Sea Polychaeta Fauna of the Family Polynoidae. In: P.A.
HUTCHINGS (ed). Proceedings of the First International Polychaeta Conference, Sydney. Linn. Soc. New South Wales : 72-
85.
LEVENSTEIN, R.Y.. 199 1 . Distribution Patterns of Polychaeta in Deep-Sea Trenches. Ophelia. Suppl. 5 : 587 -592.
MCINTOSH, W.C.. 1885. Report on the Annelida Polychaeta Collected by H.M.S. Challenger During the Years 1873 76.
Rep. Scient. Results explor. Voyage Challenger. (ZooL). 12:1 554.
PAXTON, IL. 1986. Generic Revision and Relationships of the Family Onuphidae (Annelida: Polychaeta). Rec. Aust. Mus..
38 : 1-74.
PETTIBONE. M.H., 1970. Revision of Some Species Referred to Uanira Kinberg (Polychaeta: Sigalionidae). Smithson. Conir.
ZooL. No. 53 : 1-25.
PETTIBONE. MIL. 1976. — Revision of the Genus Macellicephala McIntosh and the Subfamily Macellicephalinae Hartmann
Schroder (Polychaeta: Polynoidae). Smithson. Contr. ZooL. 229 : 1-71.
Uschakov, P.V.. 1955. — Polychaete Worms of the Family Aphroditidae from the Kurile-Kamchatka Trench. Trudy Inst.
Okeanol. P.P. Shi rshov Akad. Nauk SSSR. 12 : 311-312. (In Russian, translated 1969 by the Israel Program for Scientific
Transl. for the Bureau of Commercial Fisheries).
Uschakov, P.V.. 1962. — Polychaetous Annelids of the Families Phyllodocidae and Aphroditidae from the Antarctic and
Subantarctic. Biol. Res. Soviet Anta ret. Exped. I955-5S. 1: 129 189.
Uschakov, P.V.. 1971. On a New Abyssal Species of Macellicephala McIntosh (Polychaeta, Errantia) from the Aleutian
Trench. Fauna of the Kurile Kamchatka Trench. Trudy Inst. Okeanol. P.P. Shirshov Akad. Nauk SSSR. 96 : 36-40.
WESENBERC. -Lund, E.. 1962. — Reports of the Lund University Chile Expedition 1948-49. 43. Polychaeta Errantia. Lunds
Univ. Arsskr.. N.F. Avd. 2. 57 : 1 199
Source : MNHN, Pahs
50
Preliminary results on recolonization in a small
brackish basin on the island of Elba
(western Mediterranean)
Claudio LARDICCI & R. BALDI
Dipartimento di Scienze dell'Ambiente e del Territorio
V. Volta 6, 56126 Pisa. Italy
ABSTRACT
The recolonization of polychaetes in a small brackish basin of Elba Island has been studied to determine how the abundant
species respond to artificial disturbance. Results have shown that recolon izalion in this small brackish basin was characterized
by two species ( Capitella cf. capitata and D rani a oculata). that colonized the substrate in every months.
RESUME
Resultats preliminaires sur la recolonisation d'lin petit bassin saumatre dc Pile d’EIbe (Mediterranee occidentale)
La recolonisation d’un peuplement dc Polychetes d’un petit bassin saumatre de file d’EIbe a ete ctudiec pour mettre en
evidence les reponses des especes les plus abondantes a une defaunation artificielle. Les resultats ont mis en evidence quo la
recolonisation est caracterisee par C. cf. capilala et D. oculata. Ces especes sont capables de coloniser le substrat defaune
pendant tous les mois etudies et d'eue dominantes au cours des premieres phases dc la succession.
INTRODUCTION
The recolonization of polychaete assemblage (we defined as assemblage the ensemble of the most abundant
species which characterized the community) in a small brackish basin of Elba Island was the puipose of this study.
This assemblage has shown high persistence in time, due to die characteristics adaptive strategies of its species
(Lardicci, 1991). The successional sequences in zoobenthos have been studied extensively in recent years
through the use of experimental boxes (GuGrin, 1970; Mass6& GuGrin, 1978; McCall 1978; Arntz &
Rumour, 1982; Zajac & Whitlatch, 1982a, b; Levin, 1984; Whitlatch & Zajac, 1985; Diaz-Castaneda,
1987; Diaz-Castaneda & Safran, 1988; Diaz-Castaneda et ai, 1989; Frid, 1989; Berge, 1990). However,
concerning the successional dynamics and the response of polychaete assemblage along the Mediterranean coasts
to artificial disturbances, few data exist (Diaz-Castaneda & Safran, 1988; Lardiccl 1992).
LARDICCI . C. & R. BaLDI, 1994. - Preliminary results on recolonization in a small brackish basin on the island ol Elba
(western mediterranean). In: J.-C. Dauvin. L. Laubier & D.J. RF.ISH (Eds). Actes de la 4eme Conference internationale des
Polychetes. Mem. Mus. natn. Hist. not.. 162 : 479-483. Paris ISBN 2-85653-214-4.
Source MNHN , Pans
480
C. LARDICCI & R. BALDI
MATERIAL AND METHODS
The studied area (called Salina) is located in Portoferraio Bay. Elba Island (Fig. 1). It is a shallow intertidal
basin surrounded by a series of barriers which permit water exchange only during high tide. A small drainage
channel is a major input of fresh water into the basin. The dynamics and the general feature of recruitment in tins
basin have been previously described (Lardicci. 1991, 1992).
FiG. 1. — Study area and sampling station.
Recolonization was studied bv deploying experimental boxes (50 x 50 x 20 cm) containing defaunated air
dried sediment in a silty-sand area which measures 5 x 5 in. All boxes were dug into sediment with die top ol the
box flush with die surface of the sediment.
Two series of experiments were performed: the first consisted of boxes that were sampled, removed ana
replaced monthly to determine monthly settlement from July 1990 to November 1991. These boxes were reterred
to as the monthly boxes. The second experiment consisted of seven boxes which were deployed at the start ol die
study on July 9. 1990 and sampled after 7, 14, 30. 60. 120, 240 and 477 days to follow recolonization. These
boxes were referred to as the successional boxes.
Samples were collected using corcrs with a 6 cm inside diameter and pushed 20 cm into the sediment during
low tide Four cores per month were taken from the monthly boxes, four from the successional boxes for each
sampling date and four from die natural sediment. We wish to emphasize that die observations concerning the
experimental boxes and natural sediment are to be considered as comparisons of physical locations, rather than
treatment per se (HURLBERT, 1984) and a great deal of caution must be employed in the interpretation of the
results. Samples were washed through a 250 pm sieve. Sample residues were fixed in 4 % formalin. All samples
were sorted under a dissecting microscope and all animals, where it was possible, identified to species.
Polychaeies were the most important group collected (68.7 %) while molluscs and crustacean constituted
respectively the 25 % and 6.3 % of die total species. Twenty-two species of polychaetes belonging to 10 families
were collected during the course of this study (Table 1). > , ......
The temperature in die water ranged from 1 1.9 °C in January 1991 to a high value ol 35.4 C in July 1971.
Salinity ranged from 30.6 P.S.U. in May 1991 to 38.3 P.S.U. in September 1991 in the study period.
RESULTS
Monthly sampled boxes: polychaetes were the only species of macrozoobenthos with many unidentified
turbellarians and nematods collected in experimental boxes. These species were Capiiella cl. capiiaia. Drama
oculata, Streblospio shruhsolii, Peri nereis rullieri, Syllides edemata and Cirrophorus furcatus. Capiiella cl.
capitala was the most abundant species collected from the boxes with a pattern that seemed to follow its
fluctuations in the ambient. D. oculata and S. sltrubsolii were present nearly every month but their distribution in
the boxes was quite different from that of their ambient numerical levels. S. sltrubsolii showed large fluctuations
in the natural sediment, whereas, there were fewer specimens within the box. II. oculata was abundant in the
ambient but showed a low level of abundance nearly all the months. P. rullieri appealed to colonize the
Source : MNHN, Paris
RECOLONIZATION IN A MEDITERRANEAN BRACKISH BASIN
481
defaunated sediment only from March through July 1991, .S', edemata was present in the last four months of 1990,
and June and July 1991, Cfurcaius was only collected in September 1990.
Succession^ trends: polychaetes were the only species of macrozoobenthos with many unidentified
lurbellarians and nematods collected up to 120 days in these boxes. The amphipod Melita palmata and the
tanaidacean Leptochelia savigny were also present after 120 days with few specimens while the bivalve Abra
ovata began to appear at 477 days in this box. Only C. cf. capital a and B. oat lata were collected at die first phase
of succession. C. cf. capitata showed a relatively constant numerical increase from 30 to 240 days after which it
declined. Fewer B. oculata occurred for the first 60 days then it continued to increase until 240 days after which
the number of specimens remained at the same level to the end of die experiment. Three additional species
appeared at 120 days; these were S. shrub solii which reached its highest level at 477 days, M. fuliginosus
decreased after its appearance and continued to decline in number to die end of the experiment and S. edentata
tluctuated in its occurrence during the remainder of the experiment. P. rullieri was only present at 240 days, D.
ornata appeared at 240 days and decreased and C. fiircatus colonized the defaunated sediment at 477 days (Fig.
2).
FIG. 2. — Suceessional trends of the collected species in the experimental boxes. The error bars are standard errors.
C. cf. capitata — B. oculata o—o — o — o;
S. shrubsolii A— A — A— ▲ S. edentata □— o— o—o ;
M. fuliginosus • - • - •- — * P. rullieri -t - 1 - 1 - F ;
C. tentaculata ■ D. ornata — ♦ — * -* ;
DISCUSSION
Life-history features are important factors that allow settling and exploitation of the disturbed habitats (Zajac
& Whitlatch. 1982a . b; Wiiitlatch & Zajac, 1985; Diaz-Castaneda & Safran, 1988). Most of the species
collected in monthly boxes are considered opportunistic but only B. oculata and C. cf. capitata were able to
colonize the defaunated habitat in all the study months. The settling periods of many species which were present
within experimental boxes were observed between May and September (Lardicci, 1992). Recolonization could
also be due to both postlarvae and adult movements in addition to larval settlement. The presence of benthic adults
in the water column was previously reported in this basin (Lardicci, 1992) and it may be of importance in
maintaining the persistence of the assemblage in shallow water (Levin, 1984: Frid, 1989). Variability in
recolonization may be explained by fluctuations in abiotic parameter fluctuations. Many of the species were
482
C. I.ARDICCI & R. BALDI
surface or near surface deposit-feeders, and their food resource could be influenced by processes such as
sedimentation, resuspension and transport of particulate organic matter (Zajac & WHITLATCH, 1982a). Fifteen
days after the setting of experimental boxes, the substrate was covered by a thin layer of sediment which had been
resuspended and deposited bv the tidal current. This sediment constituted a very favourable habitat for II oculata
and C. cf. capitaicr, this last species was particularly attracted by organically enriched sediment (Diaz-
Castaneda et a!., 1989; Tsutsumi, 1990; TSUTSUMI et al., 1990). The lime of disturbance was another
important factor which could affect the processes of settlement (Zajac & Whitlatch, 1982b; Diaz-Castaneda
el al, 1989). In the period beginning in July an early phase was noted up to 60 days in which only C. cf. capitata
and B. oculata. This was followed after 120 days with the occurrence of other species such as S. shnibsolii, .S'.
edemata and Al fuliginosus began to appear. C. cf. capitata is a well-known opportunistic species (GRASSLE &
Grassle. 1974) and it appeared able to colonize successfully the defaunated sediment both in successional and
monthly experiment in this basin. B. oculata is not a so-called opportunistic species but the presence of external
gestation and adult mobility could be the mechanisms that allow this species to quickly colonize the substrate.
Colonization by post larval stages, and particularly by adults carrying a full complement of young, permits
extremely rapid local increases in population size following very few colonization events (Levin, 1984). Hence
the recolonization in this small brackish basin was characterized by two species (B. oculata and C. cf. capitata )
which are able to colonize the substrate in all months of the study and were die dominant species in the initial
phase of successional dynamics. Future research will have to clarify if the observed trend was only a matter ol
seasonal effect or a constant rule in this basin.
TaBLB 1 . List of species.
ACKNOWLEDGEMENTS
We would like to thank Prof. D. .1. REISH for the critical revision of the manuscript and two anonymous rewiers
for comments and suggestions.
REFERENCES
ARNTZ, W. E. & RUMOHR 11.. 1982. — An experimental of inacrobenlhic colonization and succession and the importance ol
seasonal variation in temperature latitudes. J. Exp. Mar. Biol. Ecol ., 64 : 17-45.
BERGE, J. A.. 1990. Macrofauna recolonization of sublidal sediments. Experimental studies on defaunated sediment
contamined with crude oil in two Norwegian fjords with unequal eutrophication status. I. Community responses. Mar.
Ecol. Prog. Ser ., 66: 103-1 15.
Diaz- Castaneda. V., 1987. Recolonisation benthique d’un sediment dans des enceintes experimentales replacees dans le
milieu nature! (etage infralittoral d’une baie mediterraneenne. Toulon. France). Cah. Biol. mar.. 28 : 551-566.
Diaz-Castaneda, V. & Safran, P.. 1988. — Dynamique de la colonisation par les annelides polychetcs de sediments
defaunes par la pollution dans des enceintes experimentales en rade de Toulon (France). Ocean. Ada. 3 : 285-297.
Source : MNHN. Paris
R I- COLONIZATION IN A MEDITERRANEAN BRACKISH BASIN
483
DlAZ-CASTANEDA, V.. Richard, a. & FRONTIER. S., 1989. Preliminary results on colonization, recovery and succession in
a polluted area of southern North Sea (Dunkerque's harbour. France). Scieni. Mur.. 53 : 705-7 16.
FRID, C. L. J., 1989. - The role of recolonizalion processes in benthic communities, with special reference to the
interpretation of predator- induced effects. J. exp. mar. Biol. Ecol. 126 : 163-171.
GRASSLE, J. F. & GRASSLE. .1. P.. 1974. — Opportunistic life histories and genetic systems in marine benthic Polychactcs. J.
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Guerin. .1. P.. 1970. — Etude experimental de I'etablissement d’un peuplement de substrat meuble a partir do larves
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species based on assessment of dominance and diversity. J Nat. Hist.. 17 : 859-874.
LaRDICCI, C.. 1991. - Le peuplement de polychetes d’un petit bassin saumatre dc File d'Elbe (Mer Mediterrannee). Vie Milieu.
41 . 195-201.
LARDICCI. C.. 1992. General characteristics of recruitment and recolonization in Polychaete assemblage in a small brackish
basin on the island of Elba (Western Mediterranean). Oebalia. 18 : 69-81.
Levin. I... 1984. Life history and dispersal patterns in a dense infaunal Polychactcs assemblages: community structure and
response to disturbance. Ecology. 65 : 1 185-1200.
Mass£, IF & Guerin. J. P. 1978. Etude experimentale sur le recrutement des especes de la macrofaune benthique des
substrat mcubles. Donnees sur les cycles biologiques des Polychetes et des Bivalves. Tethys. 8 : 283-294.
McCall. P.. 1978. Community patterns and adaptive strategies of the infaunal benthos of Long Island Sound. Journ mar.
Res.. 35 : 221-266.
TSUTSUMI, FL, 1990. — Population persistence of Capiiella sp. (Polychaeta; Capitel 1 idae > on a mud Hat subject to
environmental disturbance by organic enrichment. Mar. Ecol, Prog. Ser.. 63 : 147-156.
TSUTSUMI, IF. FUKUNAGA. S.. FUJITa. N. & SUM1DA, M.. 1990. — Relationship between growth of Capitella sp. and organic
enrichment of the sediment. Mar. Ecol, Prog. Ser.. 63 157-162.
Whitlatch. R. B. & ZAJAC. R. N.. 1985. Biotic interactions among estuarine infaunal opportunistic species. Mar. Ecol
Prog. Ser.. 21: 299-311.
Zajac. R. N. & WHITLATCH. R. B.. 1982a. Responses of estuarine infauna to disturbance. I Spatial and temporal variation
of initial recolonization. Mar. Ecol. Progr. Ser.. 10 : 1-14.
Zajac. R. N. & Whitlatch. R. B.. 1982b. — Responses of estuarine infauna to disturbance. IF Spatial and temporal variation
of succession. Mar. Ecol. Prog. Ser.. 10 : 15-27.
Source : MNHN. Paris
51
Intertidal sandy beaches Polychaetes of
Sao Sebastiao island, southern Brazil
Eloisa H. MORGADO * A. Cecilia Z. AMARAL*
Edmundo F. NONATO ** & Lara B. SALVADOR ***
* Depto. Zoologia, IB - UNICAMP. CP:6109
13081-970 - Campinas. SP. Brazil
** Depto. Oceanografia, Biologia. IO - USP. CP: 9075
05508 - Sao Paulo. SP. Brazil
*** Pos-Gradua^ao, UN PSP
Rio Claro, SP, Brazil
ABSTRACT
The composition and distribution of polychaete fauna along sandy beaches of Sao Sebastiao Island (southern Brazil) and
their relation with sediment variables were examined. Functional feeding groups were used to investigate distribution patterns
of intertidal polychaetes. The beaches were dominated by detritivorcs. Surface-deposit feeders and suspension -feeders
presented higher relative abundances in very fine sand, whereas carnivorous polychaetes and subsurface-deposit feeders were
more abundant in coarser sands. The proportion of subsurface-deposit feeders increased in medium sediments with higher
percentages of organic carbon. Sessile polychaetes generally inhabited physically stable habitats, and occurred in low
proportion. The distribution and abundance of feeding groups seem to be related to sedimentary conditions and environmental
stability.
RESUME
Polychetes Intertidaux des plages sableuses de Pile de Sao Sebastiao, Bresil meridional
La composition et la distribution de la faune de polychetes ont etc examinees de long des plages sablonneuses de file de
Sao Sebastiao (Bresil meridional) en relation avec les caracteristiques sedimentaires. Les modeles de distribution des
polychetes intertidaux out etc recherches en utilisant les groupements fonctionncls alimentaires. La distribution cl I'abondance
selon les groupes trophiques paraissent en relation avec les conditions sedimentaires et la stabilile du milieu. II a ele observe
que 1 ) les especes delritivores sont numeriquement dominanles dans les groupements macrobenthiques. la classe Uophique des
detritivorcs de surface etanl la plus abondante ; 2) la proportion de ces derniers et des suspensivores peu mobiles atteint son
maximum dans le sable ties fin, tandis que les especes carnivores ont leur plus grande abondance
dans les sables grossiers ; 3) les delritivores de subsurface sont dominants dans la plupart des habitats el leur abondance croit
dans les sediments mo yens avec les taux le plus eleves de earbonc organique : 4) les especes sessiles se rencontrent
generalement dans les habitats physiquement stables.
Morgado, E.H., Amaral, A.C.Z., Nonato. E.F. & L.B. Salvador, 1994. - Intertidal sandy beaches Polychaetes of Sao
Sebastiao island, southern Brazil hr. J.-C. DAUVIN. L. LAUBIER & D.J. KgISII (Eds). Actes de la 4eme Conference
internationalc des Polychetes. Mem. Mus. ncitn. Hist. rial.. 162 : 485-492. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
486
K.II. MORGADO. A.C.Z. AMARAL. L.F. NONATO & L.B. SALVADOR
INTRODUCTION
Sediment structure is an important factor determining organization of soft-bottom benthic communities. The
inter-relationships of habitat, resource availability, and feeding mechanisms are fundamental aspects of the
animal -sediment interactions. In this regard, trophic group analysis can play a significant role in the determination
of distribution patterns and benthic community organization (SANDERS. 1958; LEVINTON, 1972; WHITLATCH.
1980.1981). ^
Polychaetes have a relevant participation in the productivity ol marine ecosystems. They present high levels ot
trophic functional diversity (Fauchald & JUMARS, 1979) allowing their application on the determination of soft-
bottom communities trophic structure (MAURER & LEATIIEM, 1981; BlANCHI & Morri, 1985; Paiva, 1990).
However, information on polychaete feeding biology and trophic-group interactions is limited for the intertidal
system.
The purpose of this study was to define the polychaete fauna composition and to examine aspects such as
feeding biology and trophic structure of the macrobenthic species along beaches of Sao Sebastiao Island.
Sediment attributes of the intertidal region, i.e., granulometry and organic-matter content were also studied and
used to interpret the spatial patterns of polychaete trophic-groups. Species distribution patterns and polychaete
community structure of these beaches were described by Amaral et al. (in press).
MATERIAL AND METHODS
The polychaete fauna of 12 beaches on the innerside of S3o Sebastiao Island, southeastern Brazilian coast
(23°44' to 23°52'S - 45°21' to 45°26'W), was examined between May 1990 and March 1991. The island is
separated from the mainland by a deep channel (Fig. 1). Many contiguous protected beaches are present on the
north side. The intertidal zone is usually relatively narrow, but may increase in size because of sand or boulder
barriers covered with the angiosperm Halodule. The central part of the island is a typical low energy environment
with a wide intertidal zone and gently sloping gradients. Small narrow beaches with steep slopes characterize the
exposed southern coast.
Eighty two biological samples were taken from the intertidal region. The macrofauna was collected from
within a rectangular iron sampler of 0.025 in2 and 10 cm depth. Two replicates were taken at each station. The
sediment was washed through sieves of 1 .0 and 0.5 mm mesh. The organisms retained were preserved in 70 %
alcohol for later identification. Parallel sediment samples were taken. These were dry sieved for granulometric
analyses (Suguio, 1973). The organic matter content was determined by calcination (Amoureux, 1966).
All polychaetes present were classified according to trophic categories proposed by Fauchald & JUMARS
( 1979). Each species was allocated to one of these classes on the basis of their gut-contents and previous studies.
Since beach sediments are continuously ressuspended by wave action, the detritivores were subdivided into
surface, subsurface and suspension feeders. Some species were assigned to more than one trophic group because
they have alternative feeding mechanisms.
RESULTS
Polychaetes were absent from the samples taken from the southern and northern exposed beaches. A total of
1765 individuals in 38 species were present in the samples from seven beaches.
The beaches of Barra Vclha. Pereque, Engenho d'Agua, Fora and Siriuba had a largest number of species and
specimens (Table 1). The greatest polychaete densities (ind. 0.05 nr2) were Scolelepis squcmuua (304) al Siriuba ;
Heteromastus filifonnis (96), Capitella capilata (66). Laeonereis acuta (64), and Isolde t pulchella (33) at Barra
Velha ; Scoloplos (. Leodomas ) sp. (22). and Oweniafusiformis(\6) at Fora, and Armandia agilis (15) at Pereque.
Detritivores numerically dominated the polychaete fauna, comprising 96 % of the individuals. Surface deposit-
feeders. primarily represented by S. squamata , C. capilata, and /. pulchella. were the most abundant feeding group
throughout the area (39. 1 %) (Fig. 2). Subsurface deposit- feeders (36.2 %) dominated the central part of the island
(Barra Velha) which had the highest concentration of organic matter (Table 1). L. acuta, S. ( Leodamas ) sp. and H.
filifonnis were the most abundant of the 10 species present. The proportion of suspension feeders was low in most
beaches and increased at Siriuba and Garapocaia (Fig. 2) due to abundance of .S’. squamata. Carnivores were the
less abundant feeding group (4.2 %) and were mainly represented by Langerltansia cornuta, Marphysa sanguined
Source :
SANDY BEACHES POLYCHAETES FROM SAO SEBASTIAO, BRAZIL
487
Fig. 1. — Location of the station locations at Sao Sebastiao Island.
and Lumbrinereis tetraura. The number of carnivores was greatest in very coarse sand at Pereque, Engenho
D'Agua and Fora.
File most abundant and diverse polychaete fauna occurred in medium sands (Fig. 3). Mobile subsurface
deposit-feeders and carnivores were dominant in coarse grains. On the other hand, surface deposit-feeders and
suspension feeders were rare or absent in coarser grains and increased in numbers in fine sands.
Motile polychaetes were common in coarse and medium sediments, while discretely motile ones preferred
very fine sand. Sessile polychaetes, although more abundant in medium grains, were present in low proportions
(< 20 %) in all substrates.
Jawed forms were rare, whereas soft-proboscis species occurred in high proportions (> 30 %) in all sediments,
except in very fine sand. Tentaculate species dominated in fine sands (96 %) as surface detritivores and
suspension-feeders.
Source :
488
l-.II. MORGADO. A.C.Z. AMARAL. E.F. NONATO & L.B. SALVADOR
Individuals
BV Pe EA Fo Ba SI Ga
Sampling location
Species
BV Pe EA Fo Ba SI Ga
Sampling location
Fig. 2. — Trophic groups distribution (A= individuals and B= species, in percentage) at different sampling locations: Barra
Velha (BV); Pereque (Pe); Engenho D'Agua (EA): Fora (Fo); Barreiros (Ba); Siriuba (Si); Garapocaia (Ga). Carnivore (C);
Surface deposit-feeders (S); Subsurface deposit-feeders (Bl; Suspension-feeders (F).
Source : MNHN, Paris
SANDY BEACHES POLYCHAETES FROM SAOSEBASTIAO, BRAZIL
489
Feeding Habit
Motility
Morphological Structure
JTX. JTX. J T X . JTX. JTX.
VCS CS MS FS CFS
Fig. 3. Individual percentages of feeding habitats (A), motility (B) and morphological structure (C). in granulometric
classes. Categories: Carnivore (C); Surface deposit- feeders (S): Subsurface deposit- feeders (B); suspension-feeders (F);
Motile (M); Discretely motile (D); Sessile (S); Jawed (J); Tentaculate (T); Other structures (X). (VCS: very coarse sand;
CS: coarse sand; MS: medium sand; FS: fine sand; CFS: very fine sand).
Source : MNHN. Paris
490
E.H. MORGADO, A.C.Z. AMARAL. E.F. NONATO & L B. SALVADOR
Table I . — Sediment average physico-chemical parameters, and polychaete species occurrence, total number of
individuals and functional trophic groups (FIG), at different sampling site: Barra Velha (BV) ; Pereque (Pe) ,
Engenho D'Agua (EA) ; Fora (Fo) ; Barreiros (Ba) : Siriuba (Si) ; Garapocaia (Ga).
SAMPLING LOG ATION S
Sampling numbers
coarse
SAND (%) medium
fine
ORGANIC MATTER (%)
Podarke pallida (Claparede. 1864)
Loatuialia americana Hartman, 1947
Sigambra grubii O.F. Muller. 1858
Lange rhansia cornu ta (Raihke. 1843)
Ceratonereis mimbilis Kinberg, 1866
Laeonereis acuta (Webster. 1879)
Glycera americana Leidy. 1 855
Giycinde multidens Miiller. 1858
Goniada lit torva Hartman. 1950
Diopatra cuprea (Bose. 1802)
Diopatra omata Moore. 1911
Diopatra splendidissima Kinberg. 1865
Marphysa sanguinea Nonato, 1965
Nematonereis hebes (Montagu. 1815)
Lumbrineris tetraura (Schmarda. 1861)
Ilaploscoloplos f rag i I is (Verrill. 1873)
Naineris setosa (Verrill. 1900)
Scoloplos (Leodamas) sp.
Aricidea fra gi l is Webster. 1879
Dispio remand Friedrich, 1956
Lion ice branchiata Nonato. 1981
Polydora websteri Hartman. 1943
Prionospio dayi (Foster. 1969)
Prionospio steenstrupi Malmgren, 1867
Scolelepis sqitamala (Muller. 1806)
Magelona variolamellata Bolivar e Lana, 1986
Chaetopterus variopedatus (Reiuer. 1804)
Cirriformia tentaculata (Montagu, 1808)
Armandia agilis (Andrews. 1891)
Capitella capitata (Fabrieius. 1780)
lleteromastus fiUformis (Claparede. 1 864)
Mediomastus calif omiensis Hartman. 1944
Nonatus longilitieus Amaral. 1980
Notonuistus lobatus Hartman. 1947
Owenia fusiformis delle Chiaje. 1841
Isolda pulchella F. Miiller. 1858
Loimia medusa (Savigny. 1818)
Terebellides anguicomus (F. Miiller, 1858)
TOTAL OF INDIVIDUALS
S PEC I ES NUM B ER/LOC ATION
DISCUSSION
Low-density polychaete assemblages characterized the area. In physically stressed environments, such as die
intertidal sandy beaches, dense assemblages seldom, if ever, develop. In diis situation recruitment and abiotic-
factors such as turbulence tend to maintain population densities at low-levels (WILSON, 1984). On the other hand,
in physically stable habitats, population densities increase, so that competition and predation regulate community
structure (PETERSON, 1979). Habitat differences in sediment structure related to local hydrological conditions
determined the distribution of trophic groups and consequently the community structure. Similar observations
were reported by Gaston & Nasci (1988), and Gaston et al. (1988) in estuaries in Louisiana.
Surface deposit- feeders dominated most beaches because they can explore a wider resource spectrum in the
sediment/water interface (Eagle & Hardiman. 1977; Josefson, 1986). Species which are able to use alternative
strategies, such as Oweniidae and Spionidae (cither surface-deposit feeders or suspension feeders), are able to
occupy rich organic sediments as well as sediments with huge amounts of suspended material. Scolelepis
squamcila. the most abundant spionid, presents morphological and etliological adaptations which allow its survival
in harsh environments. Unlike other spionids it has permanent palps, allowing the occupation of sand habitats
Source : MNHN, Paris
SANDY BEACHES POLYCHAETES FROM SAO SEBAS’llAO, BRAZIL
491
where deciduous palps are easily lost by the action of turbulence and where predation rates are low (Dauer,
1983).
Subsurface-deposit feeders are usually associated with very fine sediment particles and rich in organic matter
(LANA, 1981; Maurer & Leathem, 1981; Gaston, 1987; Morgado. 1988). Nevertheless, in this study these
polychaetes were rare in very fine sand and dominated in other kind of sediments. At Barra Velha, for example,
high levels of organic matter were found in medium and fine sand with large populations of Laeonereis acuta and
Heteromastus filiformis. This beach is located in the island urban zone, with the sediments enriched by domestic
sewage. According to Dauer & Conner (1980), coarser sand sediments with low silt-clay contents and low
nutrient retention capacity tend to be organically richer under moderate nutrient addition than finer sediments
which is similar to this area.
Greater relative abundance of carnivorous polychaetes in coarser sediments is related to substrate physical
characteristics. Many of the intertidal carnivores are small, depending on size of the sediment interstices to
locomotion and prey capture (Gaston, 1987).
The dominance of motile forms and the scarcity of sessile ones reflect the dynamic sediment nature. In more
stable habitats, with a high content of silt-clay and organic carbon, sessile polychaetes become more abundant
(Maurer & Leathem, 1981; Gaston, 1987).
Detriiivores distribution and abundance throughout the sites suggest that most of die particulate organic matter
occurred in the sediment-water interface. In the richest sediments, resources were also available for subsurface
deposit-feeders.
ACKNOWLEDGEMENTS
This work is part of a project that studies die macrofauna of Sao Paulo state beaches, developed by the
Zoology Department (IB - IJN1CAMP) with logistical support of the Marine Biology Center (CEBIMar - LISP)
and financial support of the Conselho Nacional de Desen volvimen to CientiTico e Tecnologieo (CNPq) and Fundo
de Apoio ao Ensino e Pesquisa (PALP - UNICAMP). We are grateful to Elcio Soares Marinho (IB -
UNICAMP) and ELSO (CEBIMar-USP technician) who were very helpful in field work and to Claudia
Magalhaes and Jacques Vielliard for assistance in manuscript preparation. Dr. Donald Reish and two
anonymous reviewers improved very much earlier versions of the manuscript.
REFERENCES
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entrcmarcs cm praias da 1 1 h a de Sao Sebastiao (SP). Bolm. hist, oceanogr.. S. Paulo.
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203-214.
DAUER, D.M., 1983. - Functional morphology and feeding behavior of Scolelepis squamata (Polychaeta: Spionidae). Mar.
Biol., 77 : 279-285.
DAUER, D.M. & CONNER, W.G., 1980. - Effects of moderate sewage input on benthic polychaete populations. Estuar. Coast,
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Eagle, R.A. & HaRDIMAN, R.A.. 1977. — Some observations on the relative abundance of species in a benthic community In:
B.F. Keegan, P. O'CElDIGH & P..I.S. BOADEN (eds). Biology of Benthic Organisms. Pcrgamon Press. Oxford. New York :
197-208.
FAUCHALD. K. & J UMARS, P.A.. 1979. The diet of worms: a study of polychaete feeding guilds. Oceanogr. mar. Biol. Ann.
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251-262.
GASTON, G.R. & NASO, J.C., 1988. Trophic structure of macrobenthic communities in the Calcasieu Estuary. Louisiana.
Estuaries, 11:201-211.
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Gaston. G.R., LEE. D.L. & Nasci. J.C., 1988. — Estuarine macrobenthos in Calcasieu Lake. Louisiana: community and
trophic structure. Estuaries. 11(3): 192-200.
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structure. Estuar. Coast. Shelf Science, 23 : 147-169.
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Estado de Sdo Paulo. M. Sc. Thesis. Universidade de Sao Paulo, Inslituto Occanografico. 1 1 1 pp.
LEVINTON, J.S.. 1972. — Stability and uophic structure in deposit-feeding and suspension-feeding communities. Amer. Natur..
106 : 472-486.
Maurer, D. & LeaTHEM. W.. 1981. — Polychaete feeding guilds from Georges Banks. USA. Mar. Biol.. 62 : 161-171.
Morg ADO. E.H., 1988. — Anelideos Poliquetos do Sublitoral da Regido de Ubatuba - SP . compreendida entre as llhas
Anchieta e Vitoria . Ph. D. Thesis, Universidade Estadual de Campinas, Inslituto de Biologia. 181 pp.
PaIVa. P.C.. 1990. — Padroes de Distribuicdo e Estrutura Trdftca dos Anelideos Poliquetos da Platafonna Continental do
Litoral None do Estado de Sdo Paulo. M. Sc. Thesis, Universidade de Sao Paulo, Inslituto Occanografico. 146 pp.
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Whitlatch, R.B.. 1981. Animal-sediment relationships in intertidal marine benthic habitats: some determinants of
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Wilson. W.H.. JR., 1984. Non-overlapping distribution of spionid polychactes: the relative importance of habitat and
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Source :
52
Influence of the tube-building spionid polychaete
Polydora ciliata on benthic parameters,
associated fauna and transport processes
Carola Ilse-Marie NOJI
Institute of Fisheries and Marine Biology University of Bergen
Thormohlensgt 55. N-5008 Bergen. Norway
& Institute of Marine Research
P.O. Box 1870. N-5024 Bergen. Norway
ABSTRACT
The influence of the tube-building spionid Polydora ciliata Johnston on benthic community, sediment properties and
exchange processes through the sediment surface was investigated. Findings showed that spionid tube lawns (eight or more
tubes, enr2) lowered sediment stability and enhanced accumulation of suspended particles. Organic matter was selectively
transported into the sediment via feeding, which enriched sediments by up to 100 %. Only a slight increase in fluid transport in
the upper sediment layers was attributed to P. ciliata . Polydora tube lawns significantly increased abundance and diversity of
meio- and macrofauna. Further, they increased food input to the sediments and substrate area for colonization by micro- and
meiofauna. Their fecal pellets may serve as a food source for meiofauna and chemotrophs in deeper sediment layers. Hence.
Polydora ciliata . a well known pioneer species, reconditions disturbed sediments, where it may represent a food item for
benthic grazers.
RESUME
Influence du Polychete Spionide tubicole Polydora ciliata sur les parametres benthiques, la faunc associee et Ics
processus de transport
On a etudie f influence' du polychete Spionide tubicole Polydora ciliata Johnston sur la communaute benthique. sur les
proprictcs des sediments el sur les processus d'echange a travers la surface du sediment. Les resultats ont montre que les
pelouses de tubes de spionides (huit ou plus tubes par cm2) reduisaient la stabilite du sediment tandis qu’elles favorisaient
f accumulation des parlicules en suspension. De la maliere organique etait selectivemenl transports dans le sediment a travers
le processus de nourrissage. ce qui enrichissait le sediment jusqu'a 100 %, Seule une laible augmentation du transport des
fluides dans les sediments superficiels a pu etre attribute a P. ciliata. Les pelouses de lubes de Polydora augmentent
significativcment Fabondance el la diversity de la meio- et de la macrofaune. De plus, dies augmentent fapport de nourriture
dans les sediments et crcent le substrat pour la colonisation par la micro- et meiofaune. Leurs excrements peuvent servir
comme source de nourriture pour la meiofaune et les chemotrophes dans les couches profondcs de sediment. Ainsi. P. ciliata,
espdee opportuniste bien connue, ameliore les sediments perturbes, oil elle peut representer une source de nourriture pour les
No.U. C. I.-M.. 1994. Influence of the tube-building spionid polychaete Polydora ciliata on benthic parameters,
associated fauna and transport processes. In: J.-C. DaUVIN. L. LAUBIER & D.J. RQSH (Eds). Actes de la 4eme Conference
internationale des Polychetes. Mem. Mas. natn. Hist, nat., 162 : 493-501. Paris ISBN 2-85653-214-4.
Source MNHN , Paris
494
C. I.-M. NOJI
brouteurs benthiques.
INTRODUCTION
Tube-building benthic organisms significantly affect processes at the sediment-water interface by their
behavior, c.g. feeding, burrowing, defecation and tube irrigation (ALLER. 1978; FTral, 1989; FRITHSEN &
Doering, 1986; McCall & Tevesz, 1982; Noji & Noil, 1991; Rhoads, 1974; Schmager, 1988; Weinberg &
Whitlatch, 1983; Weinberg, 1984; Whitlatch & Zajak, 1985). Tubes which protrude into the water column
influence direction and speed of die laminar bottom current (Carey, 1983; Vogel, 1981), the sedimentation rate
of sinking particles (Carey, 1983) and sediment stability (ECKMAN et al. , 1981). Therefore, tube-building
organisms affect associated fauna (Eckman & Thistle, 1991; Olafsson et al ., 1990; Reichardt, 1986,
Trueblood, 1991, Woodin, 1981). The extent of this influence depends upon tube diameter, density of
colonization (Nowell & CHURCH, 1979), microbial binding of the sediment surface (Fager, 1964; ECKMAN et
al. , 1981) and sediment structure (Rhoads et al., 1978).
In Kiel Bight (western Baltic Sea) the spionid polychaete. Polydora ciliata Johnston is one of the most
important opportunistic species (Kolmel. 1979). After deterioration of environmental conditions P. ciliata can
occur in high densities. Eight or more tubes per cm2 sediment surface arc here defined as Polydora lube lawns. In
a study by WEIGELT (1991) a mass occurrence of opportunistic species ( Polydora sp., Capitella capitata , Diastylis
rat like i, Harmothoe sarsi) was used to indicate oxygen depletion.
This study concentrated on the influence of this spionid on benthic organisms, sediment parameters and
transport processes through the sediment-water interface. A comparison of natural sediments from Kiel Bight with
and without Polydora lawns addressed the following questions: 1. Does a dense lube lawn stabilize or destabilize
the sediment ? 2. Do the activities of P. ciliata have an impact on other organisms ? 3. What is the influence on
processes of fluid transport ?
MATERIAL AND METHODS
Sediment and fauna were sampled 10 times between May and November 1987 at a fixed station
(54°33'N,10°14'E) with a depth of 19 m in Kiel Bight. Baltic Sea. Sediment with and without lube lawns was
collected using a Reineck grab (20 x 30cm opening). Subsamples were extracted with cylindrical Plexiglas cores
of 10 cm (redox and biomass analyses) and 5 cm (meiofauna) diameter. Macrofauna was collected with a Van
Veen grab (0.1 m2 collecting area). Fluid transport rates in the sediment were studied in 30 cm long Plexiglas
cores (10 cm in diameter) containing "artificial" sediment prepared by sieving through 500 pm mesh, incubation
without aeration for 5.5 weeks mid homogenization. Polydora was added to half the samples, and tube lawns were
soon established.
In 1-cm intervals relative sediment stability using a tall cone penetrometer (Geonor AS, Oslo, Ekman, 1947),
grain size (ATTERBERG, 1905, modified) and water content (gravimetric) were measured. Relative stability was
estimated from the penetration depth of a vertically falling cone which is released directly above the surface of the
studied sediment layer. The measurements were conducted shipboard to avoid transport related artifacts. Redox
potential was measured with a platinum Eh-electrode (Ingold. PI-4800-M5) in 0.5 cm intervals.
For biomass analyses sediment was cut into 0.5 and 1 cm layers for intervals above and below 3 cm,
respectively, five parallels for chlorophyll a and pheopigments (UNESCO method, JEFFREY & Humphrey, 1975).
adenosine triphosphate (ATP ; Pamatmat et al, 1981) and organic matter (POM) (combustion at 500 °C for 24 h)
were measured for respective intervals from five cores. Individuals of P. ciliata were randomly selected and
measured for ATP.
For meiofauna analyses defined volumes of sediment from 1 cm intervals were preserved in a buffered
formalin/seawater solution (4 %) with Rose Bengal (stains protoplasm). Meiofauna (> 45 pm) was extracted
according to JENSEN (1983). Macrofauna was sieved (500 pm) and preserved in a buffered formalin/seawater
solution (4 %). Numeration and identification of major taxa were made using a dissecting microscope.
Source : MNHN, Paris
INFLUENCE OF POLYDORA Cl LI AT A ON BENTHIC CONDITIONS
495
Fluid transport (DlCKE, 1986; Kitlar, 1991) in the sediment was measured using sodium bromide solution
added to water above the sediment to a concentration about 50 times higher than natural. For lour days water was
regularly monitored for changes in concentration, after which sediments were sectioned, porosity determined and
bromide concentration in the porewater measured (Kremling, 1983).
RESULTS
Analyses of grain size and redox potential revealed that the sediment was silly sand (Shepard. 1954) and
became anoxic (J0RGENSEN & FENCHEL, 1974) below 1 cm depth. The data for redox potential and grain size
spectra showed no related differences over time or between the sediments with and without Polydora lawns. For
all sampling dates relative sediment stability increased with depth, reflecting an increase in sand content from
about 42 to 55 % from the surface to 8 cm depth. Relative stability of sediment with tube lawns was slightly
lower, i.e. the fall cone penetrated 1 to 3 mm deeper into the sediment. The porewater content generally decreased
from about 60-70 % wet weight at the sediment surface to about 36 % in 6-8 cm depth; for samples with a tube
lawn values were about 5-10 % higher (Fig.l). In 5.5 cm sediment depth die porewater content of the samples
widiout a lawn are starting to be huger than the values for the samples with lawns.
Porewater Content (HWW)
27 Aug '87
O 20 40 eo
Chi a Content (pg«cm-3). 1 July 87
Abundance of Foramlnlfera (Ind*cm3)
8 May '87 ATP Content (po’cm-J). 8 May 87 ATP Content O>0*cm-3), 1 July B7
- • — Sample with tube lawn - O— Sample without tube lawn
FIG. 1. Porewater content (% of sediment wet weight (VVW)) of the sediment on 27 August 1987. Mean values with
standard deviations (bars) of three measurements per sediment depth layer. Fig. 2. — Abundance of foraminifera in the
sediment on 8 May 1987. Mean values with standard deviations (bars) of five measurements per sediment depth layer (two
measurements per depth layer below 5cin). FlG. 3. — Chlorophyll a content of the sediment. Mean values with standard
deviations (bars) of five measurements per depth layer, (a) 8 May 1987. (b) 1 July 1987. FIG. 4. ATP-content of the
sediment. Mean values with standard deviations (bars) of five measurements per depth layer in a mixed sample, (a) 8 May
1987, (b) 1 July 1987.
Significant differences between sediments with and without lawns were found for biomass parameters in the
sediment. Chlorophyll a content at the surface of samples with a lawn was approx. 2.5 times higher than in die
sediments without a lawn on 8 May 1987 (Fig. 3a). On 1 July both sediment types had similar mean
496
C. I.-M. NOJI
concentrations in the surface layers (Fig. 3b). Likewise, mean ATP-concentrations in sediments with a tube lawn
were 10 times higher in the surface layer (Fig. 4a). After subtraction of Polydora- ATP, the ATP-content in the
sediments with a tube lawn was still 5.5 times higher. On 1 July die difference between the sediments was smaller,
but the total ATP content had increased (Fig. 4b). The organic matter content was very similar in both sediment
types on 1 July 1987. and surface values of 22-24 mg POM. cm*3 increased to about 28mg POM. cm 3 below 1 cm
sediment depth.
The meiofauna analysis showed differences in diversities and abundances between the two sediment types.
Representatives of the following groups were found: Nemaloda, Harpacticida, Ostracoda, Halacarida, Turbellaria,
Foraminifera, Tardigrada, larvae of Decapoda, Molluscaand Priapulida. In sediments with a tube lawn meiofauna
was more diverse and 2 to 3 times more abundant than in die sediments without a lawn, i.e. 112.6 vs. 44.9
individuals, cm-3 in the upper cm of the sediment. Corresponding differences for nematodes (84 vs. 40 ind. cm-3 in
0-0.5 cm) and the foraminifer Elphidium sp. (approx. 13.6 vs. 1.5 ind. enr3 in 0-0.5 cm) (Fig. 2) were especially
large. Regarding macrofauna, mostly juvenile organisms were found, and diversity and abundance were greater in
sediments with a moderate Polydora population (Tab.l). Besides Polydora ciliaia die agglutinated foraminifer
Ammotium cassis Parker was die most common species (3519 vs. 157 ind. 0.1 nr2 in sediments widi and without a
lawn, respectively). The foraminifera were located directly below or between Polydora tubes.
Table 1. — Macrofauna abundance (ind. 0.1 nr2) in sediments widi a moderate (less dense than a tube lawn)
population of P. ciliaia and with few P. ciliaia.
Studies on fluid transport in artificial sediments showed slightly increased transport rates (0.1 -0.2 mg bromide.
cm-3 in addition to molecular diffusion) down to 6cm sediment depth in the samples with a tube lawn (Fig. 5). It
was assumed that the samples without tube lawn represent the pure tracer input by molecular diffusion as all
Source : MNHN. Paris
INFLUENCE OF POLYDORA CIUATA ON BENTHIC CONDITIONS
497
macrofauna was excluded before the experiments were started. The molecular diffusion coefficient (Ds = 5.0+/-
0.8. 10"6cm. s-i) is quite low compared to the coefficient in natural sediments in Kiel Bight (KlTLAR, 1988).
DISCUSSION
Characteristics of polydora ciliata johnston. Polydora ciliata Johnston (body length < 30 mm) is a
cosmopolitan polychaete (Ramberc, & SCHRAM, 1983) which expresses typical opportunistic life patterns
especially in disturbed environments (Pearson & ROSENBERG, 1978; RUMOUR. 1980) and reproduces nearly die
whole year round with pelagic larvae (Ramberc. & Schram, 1983). It is able to increase very rapidly forming
spionid tube lawns. One reason for the concentrated settlement of spionid larvae next to adult individuals may be
the chemosensory recognition of conspeciftc lubes or of chemical analogs of the tube cement (JENSEN, 1991).
Video sequences from die present study site showed that Polydora tube lawns covered an area of 10 to 20m2.
Within these lawns were tubeless zones of 0.8 to I m2 area, reasons for diis colonization pattern are unknown. P.
ciliata builds an approx. 5-cm long U-shaped tube which protrudes out of the sediment. The polychaeies eidier
filter feed on suspended particles in the bottom water or deposit feed on sediment when die current falls below
acertain speed (Dauer et ai, 1981; Tag I ion et at. , 1980). Filter feeding can be important for maintenance of
water quality within moderately polluted systems (Davies et ai. 1989). Filler feeding by pelagic spionid larvae
can influence phytoplankton stocks (WATRAS et ai, 1985) via selectivity during feeding. The fecal pellets are
stored in specific parts of die lube between 1 and 3 cm sediment depdi (Schafer, 1962).
Fluid Transport
Fig. 5. Biogenic fluid transport in artificial sediment with tube lawns measured by the concentration of bromide in the
sediment pore water in three parallel experiments. (Samples without lube lawns were assumed to represent the pure tracer
input by molecular diffusion. They served as base line (0-value in the graphs) in the calculations).
EFFECT ON SEDIMENTS. Decreased relative sediment stability and higher water content are associated with
burrowing, tube building, defecation and irrigation of the tubes by P. ciliata populations. The expected differences
in grain size (FFral. 1989: LUCKENBACH et ai , 1988) between the sediments with and without a tube lawn were
not evident and could be caused by the sample treatment, as samples were treated with hydrogen peroxide to
destroy organic aggregates. Redox profiles will be discussed later.
EFFECT ON BIOMASS IN THE SEDIMENT. - Differences in total biomass parameters between sediment types
can be attributed to behavior and life history of Polydora ciliata. The 2.5-fold higher concentration of chlorophyll
a in the samples with a Polydora lawn at die beginning of May may result from active suspension feeding and
passive trapping of sedimenting algae by tubes protruding out of the sediment (Abler & Aller. 1986; Bailey-
498
C.I.-M.NOJI
brock, 1984; Carey, 1983). Laminar current is reduced to about 20 to 30 % on die lee side of tubes (Carey,
1983). which accordingly, increases sedimentation rates (Buhr. 1979; Warner, 1979). Samples with tube lawns
contained approx. 50 fig chi a . cm*3 more than the ones without lawns. Expressed as organic carbon (Corg : chi a
= approx. 40 : 1, Banse, 1974) this additional amount of organic carbon corresponds to sedimentation during a
regular spring phytoplankton bloom in this region (SMETACEK, 1980). In addition large amounts of benthic fecal
pellets and flocculant detritus were trapped between the tubes. This highly concentrated organic material
represented an ideal food source for other fauna. A study by Yap (1991) showed increased numbers of benthic
organisms in response to greater food supply. Results of the ATP measurements and meio- and macrofauna
analyses are hence not surprising. The higher meiofauna diversity and abundances down to 9 cm sediment depth
in die samples with a Polydora lawn were presumably a result of increased amount of organic matter (ALONGI,
1985), enlarged substrate surface for meiofaunal and bacterial colonization on oxygenated tubes (Bell & Coen,
1982; BELL, 1985), and of the deep-reaching bioturbation of the more diverse and abundant macrofauna in these
sediments. Large standard deviations in meiofauna abundances and diversities might be caused by patchiness in
sedimented material induced by minor differences in water current and bottom topography (ECKMAN & Thistle,
1991). Nematodes and foraminifera seemed to be best adapted to these fast-changing environmental conditions
(LlNKE & LUTZE, 1993). MOODLEY (1990) found for the southern North Sea that living benthic foraminifers
(including Elphidium sp.) were enriched in areas with large amounts of organic carbon. The populations increased
with rising temperature and increasing input of organic carbon. Enriched foraminifer densities were not restricted
to die surface sediment but also extended into deeper sediment layers. The fact that the macrofauna was mainly
comprised of juvenile organisms might be an indicator of a recent oxygen deficiency situation which had killed
the benthos.
On 1 July the situation had changed. Differences in sediment biomass between the two sediment types were
much smaller. During summer phytoplankton populations in the western Baltic Sea are strongly regulated by
intense zooplankton grazing. This results in a large reduction of sedimenting chi a (Smetacek, 1980).
Consequently, no or only little additional food could be trapped between the tubes. The fresh phytoplankton
material that had sedimented in May very probably was consumed by fauna within days (Graf. 1987). This is
supported by the concentration of organic matter at the sediment surface, which with 22-24 mg pom. cm 3 was low
compared to POM data at this station throughout the year (Eversberg, 1990). The increased sediment
temperatures (8 May 1987: 3.4 °C vs. 1 July 1987 : 6.4 °C) very possibly caused the general increase in ATP-
biomass in both sediment types. The difference in the degree of food input between both sediment types in May
resulted in dissimilar growth rates and development of biomass. The sediments with a tube lawn showed a
significant ATP maximum at die sediment surface, which may be directly associated with the tube lawns (Bell,
1985), whereas sediments without lawns were characterized by an ATP maximum below the 1-cm deep
chemocline. This subsurface maximum may be due to chemoautotrophic bacteria and sulfate consumers. During
periods with very little sedimentation of organic matter such a subsurface ATP maximum has been observed in
other studies (Graf, 1986, 1987).
IMPACT ON FLUID TRANSPORT RATES. — Only slightly increased fluid transport rates in the sediments with
tube lawns were observed. In natural sediments of the same area Kitlar (1988) found that Nephtys sp., Pectinaria
koreni Malmgren and Haliayptus spinulosusV on Seibold exerted a stronger influence relative to results of this
study. Because of the behavior (e.g. lube irrigation) and life strategy of P. ci licit a one would expect largely
increased transport rates for fluids. In addition the surface for diffusion processes is largely increased by a dense
colonization by U-shaped tubes (FOSTER-SMITH, 1978). Aller (1983), on the other hand found that tight tubes
which ;u*e coated by organic material hinder the exchange of anions because of their negatively charged tube
walls. This might lead to low fluid-transport rales. This could also explain why there were no significant changes
in the redox potential of the sediment. It seems that these U-shaped P. ciliata lubes represent a nearly closed
system which allows only a minor exchange between the sediment surface and deeper sediment layers.
ECOLOGICAL IMPLICATIONS
This study indicates that dense P. ciliata tube lawns can significantly improve the environmental conditions for
oilier benthic species by loosening the sediment texture, increasing fluid transport into the sediment, increasing the
concentration of easily degradable POM and enriching the diversity and abundance of benthic fauna. Therefore, in
areas with disturbed sediments dense assemblages of this spionid polychaete arc important as reconditioners of the
Source : MNHN. Paris
INFLUENCE OF POLYDORA CIL/ATA ON BENTHIC CONDITIONS
499
sea bottom. As the conditions in certain areas of the sea floor worsen from year to year, e.g. due to eutrophication,
oxygen deficiency and trawl-fishing, animals such as P. ciliaia become important for the re-establishment of a
benthic community.
SUMMARY
This study addresses the influence of Polydora ciliata on sediment properties, associated fauna and transport
processes through die sediment surface. The investigation area was a 19 m deep station in Kiel Bight (western
Baltic). Samples were taken from sediments with and without Polydora tube lawns with a box corer and grab
during 10 cruises between May and November 1987. Each lawn was approximately 10 to 20 m2 within which
tubeless zones were present. Sediments were analyzed for redox potential, shear strength, grain sizes, porevvater,
particulate organic matter, chlorophyll a , living biomass as ATP and composition of macro- and meiofauna. In
addition, experimental studies on dclaunated sediments were conducted to address transport of fluids.
Relative to sediments without lube lawns the sediment stability in samples with a lawn was greater, and
porevvater content was lower. After sedimentation of the phytoplankton bloom in May, chlorophyll a and ATP
concentrations were about 2.5 and 10 times higher in the sediment surface of the samples with a lawn compared
with those without, respectively. In sediments with lawns, diversity and abundance of meiofauna and macrofauna
were greater. Only slightly increased fluid transport rates through the sediment surface in the presence of tube
lawns was observed.
The enhanced accumulation of organic matter by dense Polydora assemblages is a result of both the filter¬
feeding activity of the polychaetes and of the trapping effect of the lube. This additional food source and increased
tube-related substrate area for colonization significantly improve the environmental conditions for other benthic
organisms. Therefore, dense P. ciliaia assemblages can be important its reconditioners of disturbed sediments.
ACKNOWLEDGMENTS
I thank Dr. G. Graf and Prof. Dr. S.A. Gerlach for critical discussions and support during the field work for
this study. Also thanks to Dr. T.T. Non for comments on the manuscript and on the language. Dr. G. BIANCHI
helped in translating die abstract into the French language.
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Source : MNHN, Paris
53
Patterns of abundance and diversity from the
abyss - polychaetes from northeastern Atlantic
abyssal plains
Gordon L. J. PATERSON * John D. GAGE**, P. LAMONT **
B. J. BETT *** & M. H. THURSTON***
* The Natural History Museum. London SW7 5BD
** Scottish Marine Biological Association
PO Box 3. Oban, Argyll PA34 4AD
Institute of Oceanographic Sciences Deacon Laboratory
Brook Road, Wormley, Godaiming, Surrey GU8 5UB. IJ.K.
ABSTRACT
Preliminary results are presented from an intensive study of three abyssal plain sites in the NE Atlantic. The aim of this
study was to assess the similarity of polychacte faunas from sites with different trophic characteristics. Analysis of polychaete
families from die Porcupine, Madeira and Tagus abyssal plains showed differences in composition and richness. Comparisons
with other deep abyssal studies provide further evidence that polychacte faunas of abyssal basins vary regionally.
RESUME
Abundance ct diversite des Polychetes des plaines abyssales du nord-est atlantiquc
Les resultats preliminaries d'unc elude intensive de trois sites des plaines abyssales de l'Atlantique nord-est soul presentes.
Le but de cette etude etait d'evaluer la similarite des faunes de polychetes provenant d’cmplacements aux caracteristiques
trophiques differentes. L'analyse de quelques families de polychetes des plaines abyssales de Porcupine, de Madere el du 'Page
a montre des differences de composition et de richesse. Des comparisons avec d’autres travaux en zone abyssale profonde
apportenl des preuves supplementaires sur la variation regionale des faunes de polychetes dcs bassins abyssaux.
INTRODUCTION
The abyssal plains of the world ocean represent approximately 40 % of the surface of the Earth, making them
one of the largest habitats on the planet. They have been perceived as vast open, physically monotonous habitats
without definable limits. However, pan-ocean studies carried out by the former Soviet Union have detected broad
patterns of animal distributions (Vinogradova, 1979) and have lead to general trophic classifications of the deep
Paterson. G.L..L, Gage. J.D., Lamont. P., Bett, b.j. & M.H. Thurston, 1994.- Patterns of abundance and diversity
from the abyss - polychaetes from northeastern Atlantic abyssal plains. In: J.-C. Dauvin, L. Laubier & D.J. Reish (Eds).
Actes de la 4eme Conference internationale des Polychetes. Mem. Mus. natn. Hist, nat., 162 : 503-51 1. Paris ISBN 2-85653-
214-4.
Source . MNHN. Paris
504
M.G.I. PATERSON. J.D. GAGE. P. LAMONT. B.J. BEIT & M.H. THURSTON
ocean fauna (Sokolova. 1972). Despite these studies our understanding of the processes which operate within
deep-ocean basins, and of local settles of faunal distributions, remains poor. To date there have been relatively few
quantitative studies which have concentrated on a single abyssal plain site, e.g. Hhssler & J umars (1974, Climax
site - North Pacific); KHRIPOL'NOFF el al. (1980. Verna Fracture Zone); LAUBIER & MONNlOT (1985. Bay of
Biscay); Nowell & Hollister ( 1985. Hubble. Northwestern Atlantic), Sibuet et al. (1984, Dcmerara Abyssal
Plain), THIEL et al. (1989, BIOTRANS site - Northeastern Atlantic) and Wilson & Hessler (1987, ECHO - N.
Pacific).
In 1989. as part of a European Community Marine Science and Technology (MAST) programme, three
Northeastern Atlantic abyssal plains were selected for intensive study. Each site was characterised by differences
in the trophic regime. An aim of this continuing programme is to assess how differences in the physical
environment, particularly nutrient flux, affect the abundance, diversity and trophic structure of the benthic
populations.
We present, herein, a preliminary analysis of the polychaete fauna at these sites, concentrating on the familial
similarity. We ask a basic question: are the polychaete faunas of abyssal plains dominated by die same families?
Several authors have noted that nearly all polychaete families have representatives in the deep sea, e.g. Eliason
(1951) and Hartman (1965. 1971). but it is less clear whether certain families predominate. Answering such a
question is a first step in assessing biodiversity amongst the sediment dwelling fauna of deep ocean basins.
To broaden the scope of our study, we compare our results with published data from two oilier deep abyssal
sites, HEBBLE in the Northwestern Atlantic and ECHO in the eastern tropical Pacific.
STUDY SITES
The three sites investigated were: Porcupine Abyssal Plain (PAP) - 48°50'N 16°30'W, c.4,850m; Madeira
Abyssal Plain (MAP) - 31°10’N 21°10’W, c.4,900m and Tagus Abyssal Plain (TAP) - 38°00'N 11°40'W, c.
5080 m. Studies on the PAP and MAP sites were initiated as part of the Institute of Oceanographic Sciences
Deacon Laboratory Deepseas programme, while the Tagus was studied as part of the Scottish Marine Biological
Association deep-sea benthos programme.
The PAP and MAP sites were selected to be: distant from the continental margin, of comparable depth, as
representative of Hal abyssal plains, and under oceanic regions exhibiting markedly different depths of winter
mixing (A. L. Rice. pers. comm.). Surface productivity is somewhat greater over the PAP site than at the MAP
(BERGER, 1989). Data from nearby sites suggest that PAP and MAP experience seasonal fluxes of organic matter,
with lower values at MAP reflecting lower surface productivity (LAMPITT, 1992; Honjo & MANGAN1NI, 1993).
Seasonal deposition of phytodetritus, characteristic of northeastern Atlantic waters (BlLLETT et al. , 1983; RICE#
al ., 1986: THIEL et al. , 1988/89) occurs at PAP but not at MAP (A. L. RICE, pers. comm.). TAP is a semi-enclosed
abyssal basin. Overlying productivity values suggests a nutrient regime intermediate or higher than MAP and PAP
(BERGER, 1989: Koblenz- MlSHKE# al ., 1970). It is not known if there is a seasonal component to nutrient flux
in the benthos.
There are comparable published data on the polychaete fauna from two other abyssal sites: HEBBLE (42°24'N
63°7.4W and 42°24’N 63°9.6W, 4,626 m Nowell & Hollister, 1985), which although not strictly on the
abyssal plain, lies at a similar depth to our sites; and ECHO in the equatorial eastern Pacific (14°40'N: 125°25'W,
c.4,500 m SPIESS et al. 1987). HEBBLE is subject to extreme physical disturbance which structures the
community (Thistle et al ., 1985) making an interesting comparison with the more quiescent NE Atlantic sites.
ECHO lies in an oligotrophic to mesotrophic region of the eastern Pacific and was the site of a manganese nodule
mining trial (Wilson & HESSLER, 1987). In the present comparison, data from die six control samples, collected
at a distance from the trial site, were used.
MATERIALS & METHODS
Samples from PAP and MAP were taken with a modified 0.25 m2 USNEL spade box corer (SBC). Cores were
sectioned into 0-1, 1-3, 3-5 and 5-10 cm layers, and washed through 1, 0.5, 0.3 and 0.25 mm sieves. One core
from PAP (0.25 m2) and three cores from MAP (0.75 m2) were analysed. TAP samples were taken with a
vegematiemodified SBC, with the inner nine cores, each 0.01 m2. processed through a 0.3 mm sieve. Five cores
from TAP were analysed (0.45 in2). All samples were preserved in 4 % buffered formaldehyde on the ship then
Source :
POLYCHAETES FROM ATLANTIC ABYSSAL PLAINS
505
30
0
Porcupine Abyssal Plain
30
20
10
0
Tagus Abyssal Plain
CIrratulldae L
■ Splonldae
□ Pilargidae
□ Ophslildae
in Paraonidaa
74.3%
30
20
10
0
Madeira Abyssal Plain
a Sabtllldae l - 75.9%
« Flaballigeridaa
ECHO
HEBBLE
■ Splonldae
a Clrratulldae
-) Paraonldae
Flabelllgerldae
Q Sy II Id a e
70
60
I50
I 40
|30
§20
1 10
0
5 Ampharalldae
ID Paraonldae
■ Splonldae
a Clrratulldae
a Hesionidae
■■ . .
Fig. I A comparison of familial abundance at each of the NF Atlantic sites studied. Hie five most abundant families were
compared. Also shown is the familial abundances of the HEBBLE high energy site. NW Atlantic and ECHO, an equatorial
eastern Pacific manganese nodule mining site. The total percentage abundance of the five dominant families is also given.
sorted and identified in Lhe laboratory. Analyses were carried out on pooled data. The number of samples used
from each site is given in figure 3. Only specimens retained on 0.3 mm sieve were used. Where more than one
sieve size was used. i.e. PAP and MAP. all specimens were counted from the 0.3 mm and greater sieves. Analysis
of familial similarity and richness at die different sites utilized methods which were relatively sample-size
independent to avoid biases due to differences in sample abundances. Familial richness was analysed using
Hurlbert rarefaction (Sanders, 1968 - as modified by Hurlbert, 1971). Comparisons of family compositions
were made using Normalised Expected Species Shared (NESS) - Grassle & Smith (1976). NESS is based on die
probability of the number of Operational Taxonomic Units (OTU i.e. species, trophic groups, family groups)
expected to occur in common between random sub-samples drawn from die original samples. The size of the sub¬
sample can be determined by varying die number of individuals to be compared, m. Where m is large, upto half
die size of die original sample, NESS is sensitive to the less abundant OTUs. Where m is low, NESS similarity
will be based on the dominant OTUs. NESS sub-sample value, m, was set at 42 individuals. Group average
clustering was used to classify the sites.
Source :
506
M.G.I. PATERSON. .ID. GAGE. P. LAMONT. B..I. BEIT & M.H. THURS'I'ON
RESULTS AND DISCUSSION
General observations. — Polycliaeies represented 17 % of all metazoans retained on a 0.3 nun sieve at
PAP, 27 % at MAP and 25 c/< at TAP. These apparently low values reflect the high numbers of meiofauna.
particularly nematodes and harpacticoid copepods. which were collected. If only commonly accepted macrofaunal
groups are considered, then polychaetes represented 35 % of the fauna at PAP. 58 % at MAP and 49 % at TAP.
Polychaetes from all the sites were generally small (c.l-5inm) and were collected primarily on the 0.3 mm sieve.
Specimens appeared to be sexually immature, although most showed adult features. Large individuals were rare
and vverc collected only in appreciable numbers by towed gears (Thurston ei al., submitted).
Detailed taxonomic studies are in progress, but some initial comments can be made. Several undescribed
species of Sigambra, Aphelocliaetct and Prionospio appear to be present at all three sites. Species recorded from
other abyssal sites, which have been found at our sites, include Pisionura abyssorum Hartman & Fauchald, 1971.
A ricidea tetrabranchia Hartman & Fauchald. 1971 from the NW Atlantic, abyss and Aurospio dibranchiata
Maciolek, 1981 from several North Atlantic deep-sea localities. Occurrence of the latter species suggests that
elements of the abyssal polychaete fauna may have a wide distribution. PATERSON (1985) noted that ophiuroids
from die Atlantic abyssal plains tended to have cosmopolitan distributions. However, Hartman (1971) estimated
that fewer that 10 % of the polychaete species recorded from depths greater than 2,000m had cosmopolitan
distributions.
Family COMPOSITION. — None of our sites showed any marked dominance by a particular family although in
common with other deep-sea sites the Spionidae, Cirratulidae and Paraonidae were common elements of the
fauna. The percentage abundance of individual families differed among the three sites (Fig. 1). Spionidae and
Cirratulidae were most abundant at TAP and PAP while Sabellidae and Flabelligeridac were dominant at MAP.
There were variations in the other abundant families, notably die Pilargiidae (represented by one species of
Sigambra) at TAP and Pisionidae at MAP (represented by Pisionura abyssorum).
The HEBBLE and ECHO sites had different compositions and less even distribution of families compared to
0
10 .
20 .
30 .
40 .
50 .
60 .
70 .
60 .
90 .
100 .
Family similarity among the abyssal sites using
NESS
m=42
ECHO PAP MAP TAP HEBBLE
Fig. 2. — A classification of the abyssal plain sites studied using NESS similarity measure. m= 42. and clustered using group
average clustering.
Source :
POLYCHAETES PROM ATLANTIC ABYSSAL PLAINS
507
the NE Atlantic sites (Fig. I). HEBBLE was dominated by one species of ampharetid accounting for c. 60 % of
the macrofauna (THISTLE et ai, 1985), and had three of die dominant families in common with our NE Atlantic
sites, whereas ECHO shared four families (Wilson & HESSLER, 1987). Familial similarity among all the sites was
high as might be expected at this level of discrimination (Fig. 2). The NESS classification separated HEBBLE
first. Thistle et cil. (1985) noted low diversity and high dominance at this site, which they linked to high
disturbance. The remaining sites split into two groups: the first linked PAP and ECHO while the second grouped
TAP and MAP. These groupings do not appear to reflect surface productivity. Estimates of productivity in die
waters over these sites suggest ECHO would have the highest at 125 g. Cm 2, y-i, while PAP, 'PAP mud MAP
have 40-60, 60-90 and 40 gC. nr2, y-1 respectively. However, relating composition to trophic regimes is difficult.
For example, ECHO was subject to sediment resuspension due to die action of the mining equipment (Wilson &
HESSLER, 1987) so it is possible that this disturbance affected the benthos in a similar way to the dramatic inputs
of phytodetritus at the PAP, hence the similarity of die familial fauna between these two sites.
Familial richness. — Rarefaction curves for the different sites (Fig. 3) showed that the Tagus and Porcupine
Abyssal plains had a higher diversity than Madeira Abyssal Plain. It is not possible to compare PAP and PAP
directly because the curves intersect, nevertheless, it is interesting to note the high diversity of PAP from the
single sample analysed to date. Despite differences in sample numbers at each site there was no correlation
between sample number and numbers of families or numbers of individuals (r2 = 0.3 and 0.35 respectively, d.f.
= 3). It should be noted that familial diversity is not a substitute for species diversity; die species to family ratio
estimated from samples currently being analysed is at least 2:1. So to answer our original question: the same
polychaete families do not dominate the fauna although the Spionidae, Cirratulidae and Paraonidae are often
among the most abundant families. Continuing studies at the species level will provide greater resolution to assess
how biodiversity of polychaetes varies in different abyssal plains and how this might be linked to the trophic
regime. Abyssal plains appear to differ despite dieir open, seemingly featureless expanses.
Fig. 3. — Family richness curves using rarefaction. n= total number of individuals, ns = number of samples pooled. There was
no correlation between number of samples and number of families or number of individuals.
508
M.G.I. PATERSON. J.D. GAGE. P. LAMONT. B.J. BE IT & M.H. THURSTON
ACKNOWLEDGEMENTS
We would like to acknowledge the support and help of the Masters, crew and scientific parties of RRS
Discovery cruises 185, 186. and 194. Thanks are due to Prof David Thistle (Florida State University) for
supplying the rarefaction programme and information on the HEBBLE site, Dr Eugene Gallagher (University
of Massachusetts) who supplied the NESS programme and Dr George D. F. WILSON (Australian Museum) for
data on the ECHO site. We would also like to thank Drs John Lambshead & Tim FERRERO for commenting on
the manuscript, and to Jim Chimonides for computer assistance. This reseach was carried out as part of EC
MAST contract 0037-C(EDB).
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HESSLER. R.R., & Jumars. P.A.. 1974 Abyssal community analysis from replicate box cores in the central North Pacific.
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KHRIPOUNOFF. A.. DESBRUYfcRES, D. & Chardy. P.. 1980. — Les pcuplemenls benthiques de la faille VEMA: donnees
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KOBLENZ-M ishke. O.J., VoLKOViNSKY. V.V. & Kabanova. J.G.. 1970. — Plankton primary production of the World Ocean.
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LAMPITT, R.S.. 1992. — The contribution of deep-sea macroplankton to organic remineralisation: results from sediment traps
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Laubier. L. & MONNIOT, C., 1985. - Peuplements profonds du golfe de Gascogne. Brest. IFREMER. 629pp.
Nowell, A.R.M. & Hollister. C.D.. 1985. Deep ocean sediment transport - preliminary resullts of the High Energy
Benthic Boundary Layer Experiment. The objectives and rationale of HEBBLE. Mar. Geol. , 66 : 1-11.
PATERSON. G.L.J.. 1985. Deep-sea Ophiuroidea of the N. Atlantic Ocean. Bull. Br. Mus. nat. Hist. Zool.. 49 : 1-162.
Rice, A.L. . BilleTT, D.S.M.. Fry.J.. John. A.W.G.. LAMPITT. R.S.. Mantoura. R.F.C. & Morris, R.J., 1986. — Seasonal
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Sanders. ILL... 1968. - Marine benthic diversity: a comparative study. Am. Nat., 102 : 243-282.
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Peuplements benthiques et caracleristiques trophiques du milieu dans la plaine abyssale de Demerara. Oceanol. Acta . 7 :
345-358.
Sokolova. M.N.. 1972. Trophic structure of deep-sea macrobenthos. Mar. Biol.. 16 : 1-12.
Spiess. F.N., HESSLER, R.R.. Wilson. G. & WEYDERT, M.. 1987. — Environmental effects of deep-sea dredging. Scripps
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nimu FI.. PFANNKUCHE.O., SCHRIEVER. G.. LOCHTE, K.. GOODAY, A.J.. IlEMLEBEN, C.IL. MANTOURA, R.F.G.. TURLEY.C.M..
Patching.!. W.. Rieman,F.. 1989. — Phytodetritus on the dccp-sea floor in a central oceanic region of the NT Atlantic.
Biol. Oceanog .. 6 : 203-239.
THISTLE, D.. Yingst. J.Y. & Fauchald. K.. 1985. A deep-sea benthic community exposed to strong near-bottom currents.
Mar. Geol.,6 6:91-112.
THURSTON, M IL. Bett, B.J.. RICE, A.L. & Jackson. P.A.B (submitted). — Variations in invertebrate abyssal megafauna in
the North Atlantic Ocean. Deep-Sea Res.
Vinogradova. N.G.. 1979. The geographical distribution of the abyssal and hadal (ultra-abyssal) fauna in relation to
vertical zonalion of the ocean. Sarsia , 64 : 41-50.
Wilson. G & FIessler, R.R.. 1987. The effects of manganese nodule test mining on the benthic fauna in the North
Equatorial Pacific. In: F.N. SPIESS, R.R. I lESSLLR. G. Wilson & M. WEYDERT (eds>. Environmental effects of deep-sea
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Source
Source : MNHN, Paris
54
Polychaete response to different aquaculture activities
Patricia POCKUNGTON* David B. SCOTT* & C.T. SCHAFER **
* Centre for Marine Geology. Dalhousie University
Halifax. NS B3II 3J5. Canada
** Atlantic Geoscience Centre. Bedford Institute of Oceanography
Dartmouth. NS B2Y 4A2. Canada
ABSTRACT
The benthic macrofauna was examined at four aquaculture sites in Eastern Canada over a period of one year to determine if
the heavy organic loading had a detrimental effect on the benthic communities. Two sites, one in Prince Edward Island and one
in Nova Scotia, were occupied by blue mussel lines, and two sites, one in Nova Scotia and one in New Brunswick, were
occupied by Atlantic salmon culture operations. Polychaete communities beneath each site plus reference sites were analyzed
for comparative diversity, dominance, and the presence of indicator species such as "opportunistic" or "pioneer" species. The
polychaetes which dominated the fauna beneath the mussel lines were different than those from beneath the fish cages. In both
geographical locations, the sediment beneath the shellfish lines was black, finely pelletized and had high organic material
content and the dominant macrofaunal organism was Nephtys neotena. The sediments beneath the lish cages in the New
Brunswick site were black, smelled strongly of IKS, had high organic material content and at limes were covered with a
Beggiatoa sp. bacterial mat. The dominant and sometimes only species was Capitclla copilata. a species known for its
tolerance to anoxic conditions and high organic enrichments. 'Hie dominant polychaete found under the fish pens at the smaller
Nova Scotia site was Nereis diversicolor . The difference in the two fish farm sites is explained by the scale and duration of the
operation. Similarly, degree of dominance at the two shellfish sites corresponds with the density of mussels and duration of
operation.
RESUME
Reponse des poly cli fetes a differentes activites aquacoles
La macrofaune benthique de quatre sites d'aquaculture de I'Est du Canada a ete etudiee durant une annee pour determiner si
les rejets organiques avail un effel defavorable sur les communautes benlhiques. Deux sites. Pun sur file du Prince Edouard et
I'autre en Nouvelle Ecosse etaient occupes par des cordes a moules et deux autres sites, fun en Nouvelle hcosse et I autre dans
le Nouveau Brunswick correspondaient a des fermes a saumons. Les communautes de Polychctes sous chaque site el dans des
stations de reference furent analysees en terme de comparaison de la diversite. de la dominance de la presence d’especes
indicatrices idles que les "opportunistes" ou les "pion meres". Les polychctes qui dominaient la faune sous les cordes a moules
etaient differentes de celles situees sous les cages a poissons. Dans les deux sites, les sediments sous les cordes a coquillages
etaient noirs. finement pelitises et avaient une forte concentration en matiere organique, forganisme dominant etait la Nephtys
POCKUNGTON, P.. SCOTT. D.B. & C.T. SCHAFER 1994. — Polychaete response to different aquaculture activities In: J.-
C. Dauvin, L. LAUBIER & D.J. RBISH(Eds), Actes de la 4eme Conference internationale des Polychctes. Mem. Mus. natn. Hist .
nat.. 162:511-520. Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
512
P. POCKLINGTON. D.B. SCOTT & C.T. SCHAFER
neotena. Lcs sediments sous Ics cages a poissons dans le Nouveau Brunswick etaient nous, avaient unc forte odour d Il’S. une
forte concentration en carbolic organiquc ct etaient, momentanement, recouverts d'une couciie bactenenne a Beggtaota sp.
1 ,’espeee dominante, parfois unique, etait CapUe.Ua copitala. connue pour sa tolerance aux conditions anoxiques ct aux fortes
concentrations organiques. i.c polychete dominant trouve sous les cages a poissons en Nouvelle Ecosse etait Nereis
diversicolor. I.a difference entre les deux fermes a poissons est expliquec par fee he lie et la duree de Population. De meine. le
degre de dominance dans les deux sites a coquillages correspond a la densite des moules et a la duree de I'exploitation.
INTRODUCTION
One of the reported effects of sustained aquaculture activity on coastal environments is the deposition and
accumulation of organic rich sediments under the aquaculture site (Anonymous. 1987; Gowen & Bradbury,
1987; Larsson, 1985; O'Connor et at., 1989; Prakash, 1989; Weston, 1990). A main source of organic
material (OM) under shellfish lines is faeces and pseudofaeces deposited by the shellfish (KAUTSKY & Evans,
1987). Conversely, the main source of organic material found under the fish cages at fin-fish culture sites is
derived from (he deposition of uneaten food in addition to the excretory products of the fish. At peak filleting
time, an intensive culture of shellfish can completely filter the water contained in a bay having a volume of 548 x
106 nU in seven days (DANKERS & KOELEMAIJ, 1989) and can deposit 10 kg. nr2 of OM per annum to the
sediments (TENORH et at.. 1982). Similarly, levels of 10 kg. nr2 of "mixed" or multisource OM per annum
(Gowen & Bradbury. 1987) can be deposited under a fish farm.
The consequences of the build-up of organic wastes in both types of aquaculture operations can include a
change in die sedimentary regime (Mattson & LINDEN, 1983; Ottman & SORNIN, 1985). an increase in oxygen
consumption by the sediment (K as par et ai, 1985). formation of anoxic sediments (Brown et a!., 1987) and the
production and release of harmful gasses (e.g. methane, hydrogen sulphide and carbon dioxide) from the
sediments to the water column (DahlbaCK and Gunnarsson, 1981; Brown et at. , 1987). These conditions can
influence die structure of the benthic macrofaunal community inhabiting the affected sediments (Brown. Gowen,
& McClusky, 1987): Ritz et at., 1989; Weston, 1990). and in severe conditions even affect the fish above
(Brown et at.. 1987).
It has been found that when the capacity of some sites to assimilate wastes is exceeded, it is necessary to
abandon or move the installations (ROSENTHAL & RANGELEY, 1989; SORNIN, 1981; Sea Farm C anada Inc.,
personal comm.). A search for methods to detect the change in conditions in (he environment before critical
conditions develop is one of the objectives of this work. Polychaetes are widely used as indicator organisms for
marine environmental quality studies (BELLAN, 1984, 1991; GlEmarEC & HlLY, 1981; see also review by
POCKLINGTON & Wells, 1992) and have been employed in this study to provide a measure of local benthic
environmental impact for fin fish and shellfish aquaculture operations.
The amount of organic material in sediments under and around four aquaculture installations in eastern
Canada was measured to establish that organic material was higher under the aquaculture installations than
background levels. The macrobenthic community of these sediments was then examined seasonally over one year,
with particular attention to the change in the polychaetc fraction of the macrofauna. We wanted to determine if the
effects of organic enrichment to the benthic environment from fin-fish aquaculture could be distinguished from
that derived from shellfish culture activities based on the response of the polychaeie community to the two types
of OM loading. Quantitative approaches which have been shown to be useful in such studies such as change in
diversity and degree of dominance were used. Also, we endeavoured to identify indicator species (i.e.
"opportunistic" or "pioneer" species) to augment our quantitative community structure observations and to act as
sentinels for monitoring environmental change between control and aquaculture sites.
METHODS
Four aquaculture sites were monitored over one year. These include a salmon farm in the Bay ol Lundy, a
salmon farm with mussel lines in St. Margaret's Bay, N.S.. and mussel leases in Cardigan River Estuary, P.E.I.,
and Lunenburg Bay, N.S. (Fig. I). At each location, samples were taken directly under the aquaculture site, at a
local reference site 25-50 in away from the aquaculture site and at reference sites 1.5-2 km away. T he sites were
sampled in spring, summer, fall and winter using a 225 cm2 Ekrnan grab. Samples were sieved on a 0.5 mm mesh
sieve and all benthic macrofauna was recovered and identified to the lowest taxon, counted and stored in 70 %
alcohol. Sediment from all the samples was analyzed for organic carbon content based on weight loss on ignition
at 500 °C for 2.5 hours.
Source :
POLYCHAETE RESPONSE TO AQUACULTURE ACTIVITES
513
65 63 61
FIG. 1. Map of eastern Canada showing location of aquaculture sites studied. PEI = Prince Edward Island: NS = Nova
Scotia: NB = New Brunswick.
Polychaete macrofauna data were analyzed for diversity using the Shannon Weiner information statistic IT
(Shannon & Weaver, 1964), dominance curves were generated by calculating cumulative per cent dominance of
species (Lambshead el al.y 1983); in addition, the faunal lists were examined for indicator species sensu
Pearson &Rosenberg (1978). All stations were subjected to cluster analysis on seasonal basis to determine
natural groupings based on macrobenthic species composition. We examined these data to see if sites subjected to
similar aquaculture activities were more similar than sites subjected to different aquaculture activities, or to no
aquaculture activity.
RESULTS
Organic material. — Organic material (OM) content was higher at all aquaculture sites and their closest
reference sites than at their more distant reference stations (Fig. 2).
Diversity. — In general, the diversity (IT) of the macrofaunal community in the sediments directly beneath
the aquaculture installations was lower than at the respective reference sites (Fig. 3). For example, directly
beneath the fish cages in Bliss Harbour, diversity was found to be 0 in both winter and summer compared to the
more distant reference site where die value of IE reached 2.2 in the winter and 2.7 in die summer. In contrast,
diversities calculated for the fish farm sites in St. Margaret's Bay were relatively high in both winter and summer
(IT = 1.3 and 1.1) respectively. At the 25-50 m reference sites in St. Margaret's Bay, IT ranged between 1.6 in
winter and 0.56 in summer. Diversity of fauna under the shellfish lines at the Cardigan Bay location was
calculated to be 0.08 in the winter and 0 in die summer with similar values at the local reference site (i.e. 0.05 and
0 respectively). Though our Cardigan Bay winter reference sample was invalid. H' for the most distant reference
station in the summer was 1.07 suggesting higher diversity in summer dian winter. Diversity under the mussel
lines in Lunenburg Bay was slightly higher than at the near reference site in both seasons (IT = 0.9 vs 0.09 in
winter and IT =1.1 vs IT = 0.38 in summer). This is thought to be due to die increased surface area provided by
the mussel lines as well as the mussels themselves which provide additional substrate for attachment by other taxa
514
P. I’OCKLINGTON. D.B. SCOTP & C.T. SCHAFER
which enhanced colonization (Grant el al„ in press). Diversity at die distant reference site in Lunenburg Bay was
higher than at either the mussel line or the local reference (IT = 1.55). In general, diversity is higher in winter than
summer at all locations. Diversity calculated for the fish farm sites in St. Margaret's Bay were consistently higher
30
Lunenburg
Cardigan Bay
St. Margaret's Bay
Mussel Lease
□
Reference site at 25-50m
Fish Farm
Reference site at 1.5-2km
Bliss Harbor
FIG. 2. — Percent organic material in sediment of site, near reference and distant reference of each aquaculture operation in
summer.
than at the Bliss Harbour fin fish operation suggesting that the local impact from this installation was not as severe
as at other fish farm site. As well, diversity at the mussel lease of Lunenburg Bay was higher than diversity in
Cardigan Bay suggesting that the former is less impacted.
Wint Summ Wint Summ Wint Summ Wint Summ
BUSS HAR80UR ST MARGRETS BAY CARDIGAN BAY LUNENBURG BAY
FISH FARM FISH FARM MUSSEL LEASE MUSSEL LEASE
E22 Site
Near Ref.
Far Ref.
FIG. 3. - Diversity in winter and summer at the site, near reference and distant reference of each aquaculture operation. Wint
= Winter; Summ = Summer.
Source : MNHN, Paris
POLYCHAETE RESPONSE TO AQUACULTURE ACTTVITES
515
DOMINANCE. — The dominance of the benthic community was relatively pronounced at both the fish hum and
the shellfish line sites. One species accounted for, in most cases, more than half of the individuals collected at
these sites. Comparative dominance curves showing per cent cumulative abundance versus species rank are given
in Fig. 4 (a, b, c, d). For example, at the fish farms, when animals were found in the sediments directly under the
fish cages, the percent dominance ranged from 85 to 100 % of all macrofauna collected. It is worth noting that, in
Bliss Harbour, under conditions of maximum temperature in die late autumn, no macrofaunal specimens were
found in the sediments. Dominance at die closest reference site was not as high as at the cage site in winter. At the
a Dominance: Summer
°1 23456789 10
Rank
b Dominance: Summer
St. Margaret's Bay fish farm
Rank
Dominance: Winter
Bliss Harbour fish farm
°1 2 3 4 5 6 7 6 9 10 11 12 13 14 15
Rank
<6
Dominance: Winter
St. Margaret's Bay fish farm
A
15
Aqua, site
Near ret. — Far ret.
Fig. 4 a. — Dominance curve at Bliss Harbour in summer. There were no macrofaunal animals present under the fish cages in
summer (August). Hence no line; only one species Capitella capitaia group was collected at near reference site (30 m
from fish cage), hence the * at 100 %: the cumulative abundance of species collected at the reference site 1.5 2 km away is
shown. Dominance curves at Bliss Harbour in winter show greatest dodininanceoccurs at the site under fish cage (82 % of
animals collected were 1 species Capitella capitaia ) individuals collected at reference site nearest the cages are
distributed over a greater number of species. At the reference site 1.5-2 km from fish cages distribution of individuals
among species shows little variation from summer.
FlG. 4 b. Dominance curves at fish cage and near reference location in St. Margaret's Bay in summer show little difference,
whereas the distant reference site shows a more even distribution of individuals among species with no species accounting
for more than 32 % of individuals. Dominance curve in winter similar to that in summer, animals are distributed over a
greater number of species.
fish farm in St. Margaret's Bay, dominance seemed to be shared between two species ( Pholoe minuta and Hediste
(Nereis) diversicolor), each of which accounted for about 30 % of total number of individuals. I lerc. the closest
Source :
516
P. POCKLINGTON, D.B. SCOTT & C.T. SCHAFER
reference site was dominated by Nereis diversicolor but not to the same extent as under the fish cages. At the
shellfish lease site in Cardigan Bay, 55-100 % of the individuals collected at both the shellfish lines and the near
reference site were Nephtys neotena. Tliis same species represented 31 to 63 % of die individuals collected at die
mussel lease in Lunenburg Bay and 76 to 87 % of the individuals collected at the local reference site. At the more
distant reference sites for most of the locations studied, no one species accounted for more than 30 % of the
i ndi vid uals col lected .
Dominance: Summer
| 40
20
10
°i 23456789 10
Rank
d Dominance: Summer
Lunenburg Bay mussel lease
Dominance: Winter
Cardigan Bay mussel lease
Dominance: Winter
Lunenburg Bay mussel lease
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15
Rank
Aqua, site ■ A - Near ref. Far ref.
Fig. 4 c. At Cardigan Bay in summer, the macrofauna at both mussel line and its near reference here shows 100%
comprised dominance of only one species Nephtys neotena. Far greater numbers at near reference site than mussel lease
site. The distant reference was dominated by Scoloplos armiger. At Cardigan Bay in the winter, musseul lease and its near
reference site only one species. Nephtys neotena. was collected. 'Hie distant reference site had to be discarded.
Fig. 4 d. At Lunenburg Bay in summer, there is little difference in dominance curves between the mussel line, its near
reference and its distant reference, the number of species at distance reference is greater. In winter the dominance was
greatest and diversity greatest at the distant reference site.
Source : MNHN. Paris
POLYCHAEIE RESPONSE TO AQUACULTURE ACUVITES
517
Indicator organisms. — Dominant organisms under Hie fish cages varied with geographic location. At the
late February sampling under and amongst the fish cages in Bliss Harbour, Capitelta capitate: occurred in very
large numbers in till grabs (average of 1 1,581 ind. in-2) and dominated the fauna, averaging 92 % of all individuals
collected (range 85-98 %) under the fish cages (Fig. 5). The sediment from which they were taken was black,
oozy materiaflhai smelled strongly of H2S and that was covered by a thin bacterial mat of Beggiatoa sp. In
August, Capitella capitate was tlie only species found under the fish cages but numbers at that time were very low
(44°ind. nr2). Similarly in November, it was the dominant species found associated with sediment under the fish
pens but its numbers were still relatively low (440 ind.m-2). Away from die cages, at die local reference site faunal
composition reflected a different temporal pattern. Diversity was higher and no one species represented more than
25 % of the individuals collected; diis was the case during all seasons.
Though many individuals of Capitella capitaia were found in die sediments under the fish pens at St. Margaret's
Bay, this species was not the dominant taxon at this location. For example, in July, amphipod crustaceans ol a
surface dwelling and scavenging feeding type were the dominant organism of the benthic macrofauna under the
pens and also at a reference site 20 m from the pens. It was noted that a considerable amount of algae and eel grass
was collected at both of these sites. In August, however, a small scavenging polychaete Pltoloe mi mu a shared
dominance with H. diversicolor at a site amongst the cages while another site under the cages contained no
macrofaunal animals whatsoever. Inshore of the cages. H. diversicolor was the dominant species, but in subjacent
offshore environments benthic community diversity was higher and different species dominated. In November
(the winter sampling), the dominant taxon under the cages was H. diversicolor, while away from the fish pens, the
distribution of individuals among species was comparatively uniform with no one species dominant.
The dominant organism at the shellfish sites of both Lunenburg Bay and Cardigan Bay in all seasons was
usually a small nephtyid, Nephlys neotena. However, there were exceptions. One exception occurred in November
(winter) under the mussel line in Lunenburg Bay. At that time Capitella capitaia was the dominant species
comprising 42 % of all individuals (it should be noted dial number of species and individuals at die Lunenburg
Bay site was relatively low in winter). The oilier exception occurred in Cardigan Bay, in die spring, when Nephtys
neotena was superceeded by a spionid polychaete, Polydora socialis which comprised 55 % of the individuals
collected. Neplttys neotena was dominant bodi under die mussel lines and at the reference sites suggesting dial the
reference site was not far enough away from die experimental site. Dominance was also higher at the reiercncc
site than under the mussel lines in Lunenburg Bay. More distant reference stations from other parts of Lunenburg
Bay did not contain represen tad ves of N. neotena. At Cardigan Bay. the percent dominance was approximately the
same at both the shellfish line and the reference site. A more diverse fauna was observed at the distant reiercncc
site in Cardigan Bay with several of the species collected being characteristic of fine-grained organic-rich
sediments found in estuaries (e.g. Scoloplos anniger, Lumbrineris sp. and Eteone sp.).
DISCUSSION
Under the fish cages in Bliss Harbour, the polychaetes most frequently associated with severely deteriorated
conditions Capitella capitaia, prevailed. Large numbers of small specimens of this species were collected. Larvae
of this species arc known to use sulphur dioxide as a settlement cue (CUOMO, 1985). One reason this species may
withstand the conditions that have developed in the aquaculture site sediments is thought to be the ability ol
females to build a membranous tube in which to incubate eggs which we interpret as a means ol keeping the
developing eggs from direct contact with the sediments. Capitella capitaia. on the other hand, was only
occasionally found associated with the shellfish leases. A different species. Neplttys neotena, .appears to be an
indicator of organic enrichment from biodeposition at shellfish line sites. Like Capitella capitaia. it is a small
burrowim' deposit-feeding species which can occur in very large numbers to the exclusion of other species in
sites of organic enrichment. Though many species of the genus Neplttys arc aggressive carnivores, the stomach
contents of Neplttys neotena was examined whenever it was encountered and found to contain only fluidized
detrital particles, suggesting a deposit-feeding mode of nutrition. Furthermore, the presence of external branchiae
on this species (and not on Capitella capitaia) suggests that it requires the presence of some oxygen m the
sediment for respiratory purposes. The environmental interpretation based on this evidence is that though the
levels of organic material in the sediments under the shellfish leases tire very high, they do not become as anoxic
as quickly as at the fish sites. _ , , , N .
In general, the impact of aquaculture activities in Nova Scotia (both fish farms and mussel leases) appeals to
be less than similar activities in New Brunswick and Prince Edward Island. It seems that a mix of natural and
Source :
518
P. POCKLINGTON. D.B. SCOTT & C.T. SCHAFER
anthropogenic factors are involved in determining the degree of impact of an aquaculture operation on the local
marine environment. One must consider the physical setting. The two Nova Scotian sites are located in hays
having relatively unrestricted exchange will) the Atlantic. Studies have shown that complete flushing of both St.
Margaret's Bay and Lunenburg Bay etui occur in a matter of 2 to 2-1/2 days (Siiaraf el at, 1970; M. Dowd, pcrs.
comm.). However, die Lunenburg Bay site had a causeway emplacement 20 years ago which has affected
circulation in the location of the shellfish lines. Cardigan Bay, on the other hand, is a low energy way environment
most of the summer, there is a greater exchange of water in the system during storms in the autumn (DRINKWATER
& Petrie, 1988; T. Sephton, pers. comm.). In winter, die ice cover in Cardigan Bay prevents wave-generated
Hushing. In Bliss Harbour, on the LTtang Inlet of die Bay of Fundy, though die tidal range generally is relatively
vigorous, there is only partial flushing of bays and inlets in this system (R. TRUES, pers. comm.), a condition
which could contribute to die uninterrupted flux of organic material. Temperature range at the Nova Scotia sites
are different from the other two sites. For example, maximum temperature in Lunenburg Bay is 22 °C and
minimum temperature is -1.5 °C (A. Hatcher, pers. comm.). St. Margaret's Bay is similar except the lower end
temperature never reaches below -0.5 °C (Siiaraf el al, 1970). Maximum temperature in Bliss Harbour is about
14 °C while minimum to date is +2 °C (R. TRUES, pers. comm.). No precise data were available for Cardigan Bay
but temperatures can get as high as +26 °C and below 0 °C in the winter (T. SEPHTON, pers. comm.) and it is an
environment in which species with southern affinities are found (FOURNIER & Pockungton, 1984;
POCKLINGTON & Tremblay, 1987). Cardigan Bay also has had a causeway emplacement in the last 30 years that
affects circulation in die area of aquaculture.
Along widi contrasts in the rate and extent of Hushing of die sites, there are other differences. One of diese is
density of organisms cultured and the length of time the installations have been in place. The Nova Scotian sites
are much smaller and much more recent operations than die Bay of Fundy and Cardigan Bay sites. For example,
there are an estimated 40,000 fish in the St. Margaret's bay operation whereas die fish farm in Bliss Harbour is
about 10 times larger. Similarly, there is one mussel lease operating in the Lunenburg Bay site whereas, at last
report, 10 leases were in operation in Cardigan Bay each with an estimated 35 x 106 mussels per lease (T.
SEPHTON & S. Bates, pers. comm.). All of diese factors can contribute to the observed differences in impact on
the local fauna that we have observed, together with causeway emplacements.
CONCLUSION
Analysis of the benthic macrofauna suggests dial fish farms in Bliss Harbour have a greater impact on die
environment than die fish farm in St. Margaret's Bay. Low diversity and dominance by large numbers of Capitella
capitata and die occurrence of a Beggiaioa sp. bacterial mat indicate that the Bliss Harbour sediments are severely
impacted locally as a result of high organic loadings from the fish pens compounded by increased bacterial
activity due to the lack of aeration of the sediments by Hushing. The shellfish lines at the Cardigan Bay and
Lunenburg Bay locations have less negative impact than the fish pens at Bliss Harbour. Sediments under and
adjacent to the mussel lines continue to support populations of the small, relatively oxygen dependent, deposit
feeding species ( Nephtys neotem) which is commonly associated with the fine sediments having a high organic
content. N. neotena is typical of estuarine environments and is common in the organic enriched and relatively fine
sediments found in these nearshore settings. The occurrence suggests dial, under worst case scenarios, given their
location and natural setting, the impact of shellfish lines is not as deleterious as that of die fish farms.
Benthic macrofauna are useful organisms for monitoring the impact of aquaculture operations on the marine
environment, and they also appear to be helpful in defining the stage of degradation. It appears that more severely
impacted environments have a characteristic fauna which shows anomalous dominance and low diversity.
ACKNOWLEDGEMENTS
The authors gratefully acknowledge Eric Collins, Annamarie Hatcher, Craig Emmerson, John Grant of
Dalhousie University, and Roger POCKLINGTON, PCS, Bedford Institute of Oceanography, for their help producing
figures for the manuscript, and T. SEPHTON, C. Bryant (Dept, of Fisheries, Canada), Chloe YOUNGER and Tom
DliFFETT (Dalhousie) for help in the field and organic material determinations. We also thank Paul KEIZER and
Bill Silvert of the Habitat Ecology Laboratory, Bedford Institute of Oceanography. Thanks also to the
anonymous reviewers.
Source :
POLYCHAETE RESPONSE TO AQUACULTURE ACTTVITES
519
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Source : MNHN. Paris
55
Influence of temperature and diet on the larval
development and growth of juveniles Marphysa sanguined
(Montagu) (Polychaeta, Eunicidae)
Daniela PREVEDELLl
Dipartimento di Biologia Animale, Universita di Modena
Via Universita 4, 1-41 100 Modena. Italy
ABSTRACT
The effects of temperature and food type on development and growth rate of the eunicid polychaete Marphysa sanguined
have been investigated under controlled laboratory conditions from the beginning of the larval feeding. Development and
growth rate was evaluated under vegetarian diet (filamentous green algae), meat diet (Liebig meat extract and Gerber meat
homogenates), and mixed diet containing both the two previous foodstuffs. Each diet was tested at five temperatures (13 °C.
18 °C, 24 °C. 27 °C. and 30 °C). Development and growth rate was influenced both by diet and temperature.
RESUME
Influence de la temperature et du regime alimentaire sur le developpement larvaire et la croissance de Marphysa
sanguined (Montagu) (Polychaeta, Eunicidae)
Les effets de la temperature el du regime alimentaire sur le developpement larvaire el sur la croissance du polychcte
Marphysa sanguined out ete ctudies en conditions controlees au laboratoire a partir du moment ou les larves commencent a
s'alimenter. Le developpement et la croissance out etc comparees en nourrissant les larves avec un aliment vegetal (algues
vertes filamenteuses), de la viande (extrail de viande Liebig et viande Gerber homogeneise) et avec un aliment mixte compose
d’algues et de viande. Chaque type d'aliment a ete teste a cinq temperatures (13 °C. 18 °C. 24 °C. 27 °C. el 30 °C). Le
developpement larvaire et la croissance ont ete influences par la nature de l'aliment et la temperature.
INTRODUCTION
Environmental factors strongly affect all phases of the life cycles of many marine invertebrates living in
temperate waters. Temperature, photoperiod, dissolved oxygen, food quantity and composition, and salinity are
among the principle environmental factors influencing seasonal cycles of reproduction, development and growth.
Among these, temperature and food availability, which influence individual development, growth rates and
PREVEDLLLI, D.. 1994. - Influence of temperature and diet on the larval development and growth of juveniles Marphysa
sanguined (Montagu) (Polychaeta. Eunicidae). In: J.-C. DaUVIN, L. LaubIER & D.J. REISII (Eds). Actes de la 4eme Conference
internationalc dcs Polychetes. Mem. Mus. natn. Hist, nat., 162 : 521-526. Paris ISBN 2-85653-214-4.
Source . MNHN. Paris
522
D. PREVEDELLI
survivorship, are essential in determining population dynamics (BHAUD, 1988: Marsh & 1ENORE, 1990) and
consequently the structure of marine benthic communities (Rhoads & YOUNG, 1970 : WHITL.ATCH, 1980.
198D. ' ......
The role of temperature and food type on development and growth rate has been extensively investigated tor
"opportunistic" polychaetes with short life spans, of the order of months, short generation times, and semi-
continuous reproduction, such as Capitellidae (Thnore, 1977, 1983; Tenore & Chesney, 1985; Marsh el al.,
1989; Marsh & Tenore, 1990) and Spionidae (Wible, 1984; Levin & Creed, 1986; Zajac, 1986; Chu &
Levin, 1989). Only Tew studies have investigated die influence of environmental parameters on polychaetes
defined as "equilibrium" species with longer life spans, of the order of years, slow development and fewer
reproductive periods per unit time (Ivleva, 1970; NEUHOFE, 1979; Bhaud, 1988; PREVEDELLI, 1991. 1992).
The eunicid Marpliysa sanguined exhibits all the characteristics of an "equilibrium" species according to die
definitions of GRASSLE & GRASSLE (1974), McCall (1977), and Zajac & WHITLATCH (1989). Along die Italian
coast, M. sanguined is very abundant in the Lagoon of Venice, a polyhaline lagoon widi limited fluctuations in
salinity but large seasonal changes in temperature. This species is considered to be omnivorous (Day, 1967;
F'AUCHALD & JUMARS, 1979); indeed the availability of both plant and animal food source in die Venice Lagoon is
very high.
The present paper is a part of a study of the life-history of M. sanguined to elucidate the life-history traits
adopted by this polychaete for the colonization and survival in brackish waters (PREVEDELLI, 1989). In the Venice
Lagoon temperature fluctuations is the main source of environmental instability while the variety of potential food
type is always high. It is therefore of interest to conduct an experimental study on the effects of temperature and
diet on the development and growth of this species.
MATERIALS AND METHODS
Field COLLECTIONS. — Bottom samples were collected from the Lagoon of Venice in February 1988 about
two months before spawning. Adult specimens of M. sanguined were extracted by hand from mud immediately
after collection.
Reproduction. — In the laboratory the worms were placed in tanks containing filtered lagoon mud and
lagoon water under constant oxygenation. The mud was screened through a 0.5 mm sieve to remove algae,
mollusc shells etc. Salinity was maintained around 30 P.S.U., which corresponded to the collection site. The tanks
were maintained at 24 °C and 12/12 light/dark photoperiod. Fertilization occurred after about 30 days.
Gamete emission and growth experiments. — Thirty larvae of five setigerous segments just beginning to
feed (20 days old) were used to study Hie development mid growth rate in relation to temperature and diet. They
were placed in 15 small glass tanks with 30 ml of filtered lagoon water and maintained at five different
temperatures (13. 18. 24, 27 and 30 °C) with constant 12/12 light/dark photoperiod. The 13-30 °C temperature
limits adopted, slighty exceed the lower and upper lagoonal water temperatures during larval emergences. The
salinity was kept around 30 P.S.U. Larvae were fed with vegetarian, carnivorous and mixed diets at each tested
temperature. The vegetarian diet consisted of filamentous green algae reared in the laboratory. The meat diet
consisted of Liebig meat extract (0.1 g in 50 ml of distilled water) integrated with meat homogenates. The mixed
diet contained both of these foods. Food was always given in abundance but food excess was avoided to prevent
water anoxia. Water was changed twice a week and glass tanks were replaced with clean ones every month.
Somatic growth was recorded weekly by counting the number of setigerous segments.
Statistical analysis. — The SPSS (Nuiei al ., 1975) software package was used for statistical calculations.
Effects of food type and temperature regime were analyzed using a two-way analysis of variance (ANOVA).
When the ANOVA showed treatment differences to be significant (p < 0.05), the treatment means were analyzed
by an a posteriori Least Significant Difference (LSD) lest.
RESULTS
Experimental results are reported in table 1 and figure 1.
Source :
DEVELOPMENT AND GROWTH OF MARPHYSA SANGUINFA
523
Table 1 . — Mean lenglh (number of setigers) of Marphysa sanguined at each treatment
(in brackets standard deviation).
Large differences were found in developmental stage and body size of worms reared under the different
experimental conditions, indicating that botii development and growth rate of M. sanguinea were influenced by
temperature and diet.
Development seemed to be positively correlated with temperature at 15 days, whereas no effect was noted with
different foods (Fig. 1). After the 45 days temperature effects were more pronounced : specimens maintained at
13 °C reached a length of 6 seligcrous segments, at 18 °C growth was still slow but worms reached a lenglh of 8
setigerous segments. At temperatures of 24, 27 and 30 °C, the specimens attained 15-19 setigers. This pattern
continued to the end of the experiment. After almost 5 months the larvae reared at 13 °C still had 6 setigers (Fig.
1). In these larvae only slight changes in morphology occurred over time. The jaws became thicker, the eyes and
capillary setae appeared but larvae lacked antennae, gills and new setigerous segments. At 18 °C some specimens
had the central and the two median antennae. At the higher temperatures a great variability occurred within each
group, whereas the difference between groups was limited (Fig. 1). At 30 °C the within-group variability was
lower due to a more rapid and uniform growth. At the rearing temperature of 30 °C some specimens had five
antennae and had completed larval development.
Table 2. — Results of two-way ANOVA testing the effects of temperature and diet
on growth rate of Marphysa sanguinea .
Table 3. — Results of LSD test testing the effect of temperature on growth rate of Marphysa sanguinea
(the straight line denotes means not significantly different at 0.05 level).
Source :
524
D. PREVEDF.LLI
FIG. 1 . - Growth rate patterns of Marphysa sanguined at each treatment, (a) algae; (• ) mixed; (■) meat.
Growth rates were significantly affected by temperature and diet and a significant interaction was found
between each of the two factors tested (two-way ANOVA) (Table 2). For temperature die LSD comparison of
means indicated dial only die means of die groups reared at 18 °C and 24 °C were not significantly different
(p > 0.05) (Table 111). For diet, the LSD test indicated that die mean growdi rate observed in the groups fed with
mixed or carnivorous diet were not significantly different (p > 0.05), whereas these were significantly different
from die algae group (p < 0.05) (Table 4).
Table 4. — Results of LSD test testing effects of diet on growdi rate of Marphysa sanguinea
(the straight line denotes means not significantly different at die 0.05 level).
DISCUSSION
Three conclusions can be shown from diis experiment.
First, the development and growth rate of juvenile M. sanguinea is positively correlated with water
temperature. This agrees with die findings for other species (Mangum, 1978; Wible, 1984; PESCII el ai, 1987;
Biiaud, 1988; Yokoyama, 1988; Chu & Levin, 1989; Esnault el ai, 1990 ; Miron el ai, 1992; Prevedelli,
1992) and with observations performed in the natural environment. Indeed previous studies on the life cycle of
Source :
DEVELOPMENT AND GROWTH OF MARPHYSA SANGUINEA
525
M. sanguined found the spawning period to be from April to May, related to an increase in water temperature
(Prevedelli, 1989). These larvae can arrest development and growth for long periods of time at lower
temperature conditions. However, they maintain their potential for development under more favorable temperature
conditions. If the temperature increases, the larvae* will resume growth and development. This has been confirmed
in laboratory studies where individuals reared at 13 °C began to grow again when placed at 18 °C. This feature is
an important adaptative characteristic that permits the successful colonization of brackish waters, with variable
temperatures. Seasonal fluctuations at the benthic level are stronger in lagoonal than marine environments. In
particular, thermal conditions in autumn can lead to a sudden fall in temperature; in this period the larvae must be
sufficiently developed to dig into sediment and reach a habitat with greater thermal stability. Temperature is an
important factor regulating development and somatic growth, and its function seems especially crucial in
"equilibrium" species. These species have offspring with long larval development and slow growth and must
adopt strategies to reduce mortality. A strategy to maximize survival of offspring may time the reproductive
period with the optimal conditions for die new generation (METrAM, 1980).
Second, the diet is a very important factor in regulating development, growth rate and survival which was
lower with vegetarian diets.
Third, the findings on dietary preference demonstrate that M. sanguined acquires its final omnivorous feeding
habits at an early developmental stage. It is, thus, an omnivorous species, even though the vegetarian diet given
did not prove to be suitable for an optimum growth.
ACKNOWLEDGEMENTS
This paper was supported by grants from Italian MURST (Ministero deHTJniversit<t e della Ricerca sciemifica
e tecnologica).
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Source :
56
Ethologie alimentaire d'annelides polychetes
endogees : determination du niveau sedimentaire
ou s’effectue la collecte de la nourriture
Chant al SALEN-PICARD * Claire GRAHAM ** & Magali GERINO*
* Station Marine d'Endoume, Centre Ocenologique de Marseille
LIRA CNRS 41. rue de la Batterie des Lions, 13007 Marseille, France
** Texas A & M University at Galveston. Department of Marine Biology
4700 Avenue U. Building 303. Galveston. USA
ABSTRACT
Feeding ethology of infaunal polychactous annelids: a method to determine the sediment
layer at which food is collected
Little is known about the sediment layer al which infaunal deposit feeders collect their food. A method was developped
to determine the proportion of ingested sediment at a given level using a coloured marker. Individuals of the species that
was investigated were placed into cores of sediment that had been previously homogenized. A layer of sediment 1 cm
thick, previously mixed with fluorescent pigment of similar grain size, was placed in each core al varying depths.
Animals were removed after four days and fecal pellets were collected and oven dried. Pigments were extracted and
quantified using a spcctrofluorimeter. Pigment concentrations in sediment and in fecal pellets allowed us to calculate the
proportion of ingested sediment at a given depth. The method was used for the polychactous annelid Capitella capitaia.
Results showed that for individuals of mean dry weight comprised between 0.75 and 1.5 mg. 54.3 ± 15.1 % of total
ingested sediment was taken between 1 and 2 cm. However, some amount of sediment was ingested at deeper levels (5.4 ±
1,4 % below 3 cm deep). This, together with an inclusion of gaieties and with observations in thin aquaria, suggests that
Capitella capitaia is capable of vertical movements of greater amplitude than was suspected.
RESUME
Le niveau sedimentaire auquel s’effectue la collecte de la nourriture chcz les especes endogees depositivores est
generalement mal connu. Une methode utilisant un traceur colore a etc inisc au point afin de determiner la proportion de
sediment ingere a un niveau donne. Les individus de l'especc testee sont places dans des carottes de sediment
prealablement homogeneise. Une couche de 1 cm d'epaisseur de sediment melange a un pigment fluorescent de
granulometrie semblable a celle du sediment est intercalee dans chaque carotte a differentes profondeurs. Au bout de quatre
jours les animaux sont recuperes par tamisage. leurs pelotes fecales sont recollees et sechees a letuve, Le pigment est
extrait et dose a l'aide d'un spectrofluorimetre. Les concentrations du pigment dans le sediment d'origine et dans les
pelotes fecales permettent de calculer la proportion de sediment ingere a une profondeur donnee. La methode testee pour
l'annelide polychetc Capitella capitaia a montre que des individus d'un poids moyen compris entre 0.75 et 1.5 mg de
matiere seche collectent 54.3 ± 15.1 % du sediment total qu'ils ingerent entre 1 et 2 cm de profondeur ; cependant une
quantite non negligeable de sediment (5.4 ± 1.4 %) est prelcvce au-dessous de 3 cm. Ce resultat joint a l'observation des
galeries du polychete en aquarium extra plat et d’apres un moulage suggere que l’esptice est capable de deplacements
verticaux d’une amplitude superieure a ce qui est generalement admis.
SaLEN-Picard, C., Graham, C. & M. GLrino. 1994. Influence of temperature and diet on the larval development
and growth of juveniles Marphysa sanguinea (Montagu) (Polychaeta, Eunicidae). In: J.-C. Dauvin. L. Laubier & D.J.
Reisii (Eds). Actes de la 4eme Conference internationale des Polychetes. Mem. Mas. natn. Hist. nat.. 162 : 527-533.
Paris ISBN 2-85653-214-4.
Source : MNHN. Paris
528
C. SALEN-PICARD. C. GRAHAM & M. GERINO
INTRODUCTION
La quantification des flux entre lcs differents compartiments dcs systfemes inarins littoraux et les tenialivcs
d'etablissement de hi Ians dc carbone ou d'azote au sein de ces sys&mes inettent souvent en Evidence 1c manque de
donndes relatives au role joue par la faune cndog6e (Rodhouse & Rhoden, 1987 ; Kemp et ciL 1990). Or. cette
dernifere, par sa physiologic el son etliologie repr6sente 1c vecteur principal des flux et des modifications de ces flux
k l'intfiricur de la colonne s6dimentaire et k l'interface eau-s£dimem. L'influence des organismes sur les propri6tes
physiques et chimiques dcs sediments (bioturbation) depend, en effel. d'un certain nombrc de parametres
aut6cologiques coimne les modes d'alimentation, la profondeur d’alimentation par rapport k l'interface, le degre de
mobility la laille des organismes, la densitc de population, la profondeur des galeries et, si l’organisme est
tubicole, la density, la repartition et la longueur des tubes (Rhoads & Boyer, 1982). Ind6pendamment de la taille
dcs organismes et de la density des populations les methodes utilis6es pour determiner ces differents parametres
sont les suivantes : 1) aquariums plats permettant l'observation directe des individus dans lcurs galeries ou terriers
(Clavier, 1984 ; Dobbs & Scholly, 1986), 2) photographies et radiographies de profils s6dimentaires (Rhoads
& YOUNG, 1970). 3) realisation de moulages des galeries ou terriers, technique qui permet d'appr6hender leur
architecture en trois dimensions (de Vaugelas & BUSCAIL, 1990 : GfiRiNO, 1992), 4) incorporation au sediment
de traceurs radioaclifs ou colores afin de determiner le sens et I'intcnsife des ^changes entre l'interface eau-sediment
el les differents niveaux de la colonne s6dimentaire (Maiiaut & CiRAE, 1987 ; GGrino, 1990) ou bien le taux
d'ingestion pour les esp£ces depositivores de surface (Cammen, 1980a). Les esp&ces dc I'endofaune sont, pour
beaucoup d'entre dies, depositivores et ces differentes methodes, exception faite pour les espfcces qui s'alimentent k
l'interface eau-s6dimem ou pour celles qui construisent dcs terriers permanents, ne permettent pas de determiner la
profondeur k laquclle dies collectent leur nourriture.
Dans le but d'integrer la faune endogee dans les bilans de nutriments d'une baie des parages de Marseille occupde
par un eievage de Mytilus galloprovincialis (anse de Carteau, golfe de Fos), nous avons ete amends k acqudrir des
infonnations sur l'dthologie alimentaire de 1'annelide polych&te Capitella capitata present en densite 61ev6e (jusqu'a
400 000 ind. nr2) dans le sediment sous jacent aux cultures de moules (Baudinet et at ., 1990). Nous avons,
pour cela, mis au point une methode experimental utilisant un traceur colore permettant non seulement de
visualiser le niveau s6dimentairc auquel l'espfece collecte sa nourriture mais aussi de determiner la proportion de
sediment ingdrd k un niveau domic. L'observation dcs galeries en aquarium extra plat (1 mm d'6paisseur) et la
realisation d'un moulage out permis de completer nos observations sur le comportement de l'espece.
MATERIEL ET METHODES
1 ) UTCLISATTON D’UN TRACEUR COLORS.
Principe de la methode. — Le but du travail 6tait de mettre au point une methode permettant de determiner le
niveau sedimentairc auquel les esp^ces de I'endofaune collectent preferentiellement leur nourriture. Des individus de
l'espece test (Capitella capitata) ont 6le introduits dans des carottes de sediment rcconstituees comportant k une
profondeur donn6e une couche de sediment colore. Le substrat colore a ete obtenu en meiangcant au sediment un
pigment fluorescent. Le dosage, par une methode optique, du pigment contenu dans les pelotes fecales des animaux
devait pennettre d’evalucr la proportion de sediment ingeie k une profondeur donnec.
L'espece tesl6e C. capitata provient des biodepots issus de 1'eievage de Mytilus galloprovincialis. Le ou les
types de C. capitata presents sous les cultures dc moules n'ont pas ete determines. Tous les individus utilises au
cours des differentes experiences sont cependant issus d'un meme couple et proviennent d'un eievage realise au
laboratoire k temperature et k salinite constantes (17 °C et 33 P.S.IJ.).
Le sediment utilise a ete r6‘colt6 sous les cultures de moules par 5 m de profondeur ; seule la partie superficielle
du substrat (0-2 cm) a ete preievee, tamisee sur une maille de 0,5 mm, homogeneisee puis congeiee afin d'en
eliminer la faune vivante. Le pigment employe pour colorer le sediment est un pigment fluorescent servant de base
pour des peint ures industrielles, pulverulent, non soluble dans l'eau mais soluble dans l'acetone et d'une
granulometric voisinc de celle du sediment utilise (plus de 90 % d'eiemcnts d'un diam6tre < 0,063 mm). Apr6s
addition du pigment le sediment a ete k nouveau homogeneise.
Protocole experimental. — Des carottiers en plexiglas d'un diamfclre interieur de 7,5 cm ont ete remplis d'une
couche de sediment de 8 cm d'epaisseur a raison d'un carouier temoin sans colorant, de quatre carottiers ayam
respectivement une couche coloree de 0 a 1 cm, de 1 k 2 cm, de 2 k 3 cm et de 3 k 8 cm et d'un earottier ne
contenant que du sediment colore. Au fur et k mesure du remplissage des carottiers, des echantillons dc sediment
ont ete preieves aux diflerents niveaux ; aprfes lyophilisation, lcurs teneurs en azote et carbone ont ete detcrminees
(Cl IN analyser LEGO) ; la fraction organique a ete obtenue par difference entre teneur en carbone total et teneur en
carbone aprfcs combustion k 450 °C (Kristensen & Andersen, 1987) ; les rfsultats ont ete exprimes en
pourcentage du poids de matiere s^che.
Source :
lill IOLOGD0 A1IMENTAIRE DE POLYCHfeTES ENDOGEES
529
Vingi individus de C. capiiata de taille moyenne (environ 1 mg de mature xedie) out die- imroduiis dans chaque
carottier ; irois rcplicals oni etc rdalisds. Le systdme a eld mainienu pendani 4 jours i't 17°C dans un courant
continu d'eau de mer adrde ; aucun apport de nourrituie n'a did effeciud pendant ceiie pdriode.
, Hn fin d'expcrience, les animaux ont die rdcupdrds par tamisage sur une maille de 0,3 mm ; lous les animaux
n'ayant pas dtd rdcuperds (mortalild, fuite), on n'a conservd pour chaque carottier qu'un nombre d’individus
correspondanl an nombre minimum rdcupdrd soil 10 individus. Les vers ont dtd iransfdrds dans de l'eau de mer
lillrde sur 0,2 pm et laissds pendant 12 h. Les pelotes fdcales dmises pendant ce laps de temps ont dtd au fur et a
mesure prdlevdes a la micropipette, rincdes 4 l'eau distillde afin d'en dliminer l'excds de sel, rdcoltdes sur liltres
Cil /C prdpcsds (toutes les pelotes provenant des 10 individus conservds pour un memo c;irottier ont dtd regroupdes)
puis sdchdes it ldtuve 4 40 °C pendant 12 h. Le poids de matidre seche des feces a ensuite did exprimd a 10 Lie
prds.
L'extraction du pigment dans de l’acdtone 4 90 % et son dosage ont dtd rdalisds selon le meme procddd que celui
utdisd pour le dosage des pigments chlorophylliens (Aminot & Chaussepied, 1983). Les densitds optiques ont
did lues sur speclrofluorimdtre Kontron SFM/B ; outre une puissance de dosage dlevde, le speclrofluorimdtre a
permis de determiner les longueurs d'onde d'excitation maximum (464 nm) et d'dmission (493 nm) du pigment
utilisd. La rdalisaiion d'une gamine dtalon a partir de concentrations connues du pigment a permis de determiner,
pour chaque dchantillon, la concentration du pigment dans l'acdtone (en mg. ml-') puis dans les leces (en ng. mg-i
de matidre sdchc). De la memo fa?on. la concentration moyenne en pigment du sediment d'origine a dtd ddterminde.
I.c pourcentage de sddiment colord ingdrd par rapport au sddiment total ingdrd est donnd par la formule :
Cf x 100
Pl=— cT~
ou : Pi = pourcentage de sediment colord ingdrd
Cf = Concentration du pigment dans les fdces
Cs = Concentration du pigment dans le sddiment colord utilisd.
On a testd statistiquement (ANOVa et test t) 1) l'influence du pigment sur la quantitd de sddiment ingdrd, sur le
taux de survie et sur la richesse en carbone et en azote du sddiment : 2) la non assimilation et l'absencc de selection
du pigment : on a ddtermind si la concentration du pigment dans les fdces des animaux ayant sdjournd dans les
carottiers remplis uniqueinent de sediment colord est comparable 4 la concentration du pigment dans le sddiment ;
3) si la quantitd de sddiment colore ingdrd est significativement diffdrente en fonction de la profondeur. L'intervalle
de contiance sur toutes les moyennes qui ont did calculdes est exprime avec un coefficient de sdcuritd de 95 %.
2) Observation des galeries.
L'observation des galeries a dtd effectude grace 4 la rdalisaiion de deux aquariums extra plats demontables pour
en faci liter le remplissage et d’un moulage. Le moulagc a did exdcutd selon la technique de Pervesler &
Dworschak (1985) adaptde par GfiRlNO & STORA (1991). Le resultat obtenu correspond aux galeries rdalisdes par
cinq individus de taille moyenne aprds quatre semaines de conditions in viuo dans un carottier analogue 4 ceux ddj4
utilisds.
RF.SU L.TATS
1. ClAMME fiTALON DU PIGMENT ET CONCENTRATION DANS LE SEDIMENT COLOR f.
La gainme dtalon rdalisde 4 partir de six concentrations connues du pigment a permis d'etablir l'dquation de la
droitc de rdgression dc la concentration du pigment dans l'acdtone en fonction de la densitd optique :
C = 0,00027 .DO + 0,0012, ou C = concentration du pigment dans l'acdtone en mg. ml1 : DO = Densitd
optique ; r = 0,995 ** (P > 99 %).
La concentration moyenne en pigment du mdlange sddiment + colorant est de 0,0765 ± 0.043 g par g de
sddiment sec.
2. Influence du pigment sur la richesse en carbone et en azote du sediment.
L' ANOVa rdalisde d'apres I’anaJyse des diffdrents dchantillons a montre que I'addition de pigment augmente de
fagon significative les teneurs en carbone el en azote mais que l'homogdndisation a dtd suffisante pour qu'il n'y ait
pas dc diffdrence entre les couches colordes des divers caroltiers. Le tableau I donne les teneurs moyennes en azote
et en carbone total du sddiment et du melange sddiment + colorant en fonction de la profondeur. La teneur en
carbone organique dgale 4 environ 50 % du carbone total dans le sddiment d'origine atteint 70 % dans le mdlange
sddiment + colorant.
530
C. SALEN-PICARD. C. GRAHAM & M. GERINO
Tableau 1. — Teneurs moyennes en carbonc total el en azote dans le sediment et dans le melange
sediment + colorant en fonction de la proton deur.
3. INFLUENCE DU PIGMENT SUR LA QUANTITE DE FECES EMISES ET SUR LE NOMBRE DE StJRVIVANTS.
Le poids moyen individuel de feces 6mise$ est de 1,37 ± 0,25 mg de mati&re sfcche. II n'y a pas de difference
significative entre les divers traitements ; on ne peui pas conclure h une influence du colorant sur la quantity do
pelotes fecales emises.
Le nombre d'individus survivants varie do 10 h 19. La difference entre les diff£rents carottiers n'est pas
significative. Le nombre moyen d'individus survivants pour l'ensemble des traitements est de 12 ± 2 individus.
4. Test de non assimilation et dabsence de selection du pigment.
Le test t effectud entre la moyenne (0,0765 ± 0,043 g. g_1 de sediment sec) des concentrations du pigment dans
le sediment colore et la moyenne (0,0688 ± 0,027 g. g i de matifere s&che) des concentrations du pigment dans les
pelotes fecales des individus ayant s6journe dans les carottiers remplis en totalite de sediment colore ne pennet pas
de conclure avec un coefficient de securite suffisant (P < 60 %) h une difference entre les deux concentrations.
5) Proportion de sediment colorE ingErE en fonction de la profondeur de la couche colorEe.
La figure 1 donne, pour chaque profondeur, la proportion moyenne de sediment colore ing£r£ par C. capitata. Le
maximum de sediment colore a etc ing£r£ (54,3 ± 15,1 %) lorsque la couche coloree est situee entre 1 et 2 cm. La
difference entre les divers niveaux est hautement significative. De plus, l'ecart entre les concentrations du pigment
dans les ftces aux differentes profondeurs est statistiquement superieur <t rh£t6rog6n£it£ des concentrations dans le
sediment colore utilise.
o
i
20
40
— 1—
i.
5£l
80
100
I
Profondeur (cm )
Fig. I. — Pourcentage dc sediment ingere par Capitella capitata en fonction de la profondeur.
6) Observations des galeries.
Dans les deux cas (aquariums extra plats et inoulage) on a observe une forte concentration de galeries dans les
deux premiers cm du sediment (Fig. 2) ; cependant on remarque la presence de galeries descendant jusqua plus dc
10 cm dc profondeur. Les galeries pr6sentent de nombreuses bifurcations et plusieurs orifices de communication
avec 1'interface eau-s6diment, orifices par ou sont evacuees les pelotes fecales.
Source :
EH IOLOGIF. Al JMENTAIRE Dli POI .YCHETES liNDOGEES
53 i
FlG. 2. — Moulage des gaieties construites par cinq individus de Capilella capilaia apres quatre semaines de conditions in
vitro.
DISCUSSION CONCLUSION
La mEtliode a mount de fagon significative que les individus testEs out un niveau prEfErentiel de collecte de leur
nourriture. Dans les Eludes consacrEes h 1'Ethologie alimentaire des espEces dEpositivores, les traccurs colorEs
n'avaient guEre EtE utilises qu’en tant que marqueurs qualitatifs (Haven & Morales-Aeamo, 1966 ; Jacobsen,
1967 ; Cammen, 1980 a, b ; DOBBS & Whitlatch. 1982). Le fail d'uliliser un pigment lluorescent soluble dans
1'acEtone a permis son extraction et sa quantification. La comparison avec le tEmoin sans colorant a montrE que le
pigment n'est pas, lout au moins h court terme, toxique pour les animaux et qu'il ne modifie pas la quantity de
pclotes Scales emises. Pour que le rapport concentration du pigment dans les fEces/concentration du pigment dans
le sediment ingErE soit reprEsentatif de la proportion de sediment colors ingErE, il faut 1) que le pigment ne soit pas
assimilable, 2) que 1'espEce testae ne soil pas trop selective dans la collecte de sa nourriture ; toutes conditions qui
ont EtE rEunies dans le cas present. Plutot que d'uliliser un sediment ayanl conserve sa stratification naturelle, nous
avons prEfErE employer un sediment homogEnEisE afin d'Eliminer l'influence de la richesse du substrat. L'addition
du pigment enrichit ccpendant le sediment en azote total et en carbone organique mais I'homogEnEisation du
melange sEdiment + colorant a etc suffisante pour que l'enrichissement soit Equivalent quel que soit le niveau
colorE considErE. Les rEsultats obtenus sont indEpendants de la richesse du substrat et traduisent bien un
comportement de 1'espEce.
De nombreux travaux rEccnts menEs par TENORE et ses collaborateurs (Marsh el ai, 1989) ont EtE consacrEs
au role jouE par la quantitE el par la qualitE de ralimentation sur la croissance individuelle et la dynamique de
population de C. capitata type I. Le taux d'Egestion et la variabilitE de ce dernier en fonction de contraintes
physicochimiques (tempErature, oxygEne) ou individuelles (croissance) ont EtE EludiEs par Forbes & Lopez (1990)
mais 1'Ethologie et I'influence des espEces du genre Capilella sur le sEdiment restent mal connues. Contrairement
aux grands terriers permanents construils par des espEces qui ont d'importantes capacitEs de bioturbation, les
532
C. SALEN-PICARD. C. GRAHAM & M. GER1N0
structures biogfenes produites par les esp£ces pionni&res oni rcyu pcu d'attemion (Alongi, 1985). D'aprfcs
Fauchald & Jumars (1979) Capitello consiruil des tubes muqueux pits de la surface du sddiment ; Rhoads &
Boyer (1982) consid6rant que les espfcccs pionni&res s'alimentent <i ou au dessus de ['interface eau-sediment
stipulenl que leur influence sur le subsirat est limitde <i une epaisseur inferieure h 2 cm. Notre methodc a
clairement d6montr6 que C. capitata est une esp£ce deposit ivore de subsurface, la zone d’ingestion maximale pour
des individus de taillc moyenne se trouvant localis6e entre 1 et 2 cm de profondeur. Une quantity encore
importante de sediment est ingeree au dessous de 3 cm ; ce rgsultat associe aux observations realis6es en aquariums
extra plats et au moulage des galeries confirme le fail que I'esp&ce est capable de mouvements verticaux d'une
amplitude sup6rieure h ce qui est gdncralement admis. Ltlude du peuplement de Capitello capitata install^ sous les
cultures de moules a revele une stratification des individus en fonction de leur taille et de leur age : les individus
juveniles et de petite taille sont localises entre 0 et 1 cm, ceux de grande taillc (poids > 1,5 mg) out un maximum
d'abondance entre 4 et 6 cm de profondeur. La mlthode appliqu6e aux difterentcs classes de taille d'une population,
devrait done penneltre de determiner la zone d'ingestion maximale <T l'Cchelle de la population ; de hi, connaissant la
distribution verticalc dans le sddiment dun certain nornbre de macro et de micronutriments, il sera possible de
mieux apprChender les besoins de fesp&ce el revolution de ces besoins en fonction de 1'age des individus. De plus,
chez les esp&ces deposit ivores de subsurface qui Cvacuent leurs pelotes fdcales <i la surface du sediment, le fait de
connaitre la proportion de sediment ing6r6 <i une profondeur donnfe pent rendre plus aisee la determination des taux
de remaniement sedimentaire en limitant la rCcolte des pelotes fCcales aux seuls elements colores ou aprCs
utilisation de techniques de traitement d'images.
REMERCIEMENTS
Ce travail a ete execute, pour l'une d'entre nous, dans le cadre du programme de bourses ERASMUS ; il a
bCneficie du souticn du Groupement Scientifique CNRS Universite d'Aix Marseille II. Societe Nationale Elf
Aquitaine : Cycles biogCochimiques. Devenirde la matiere organique dans le milieu littoral marin.
REFERENCES
ALONGI, D.M.. 1985. Microbes, meiofauna and bacterial productivity on tubes constructed by the polychaete
Capitello capitata. Mar. Ecol. Progr. Ser.. 23 : 207-208.
AMINOT. A. & CHAUSSEPIED. M.. 1983. — Manuel des analyses chimiques en milieu marin. C.N.E.X.O. Publ.. Brest,
395 pp.
Baudinet. D., ai.i.iot. E.. Berland. B.. Grenz. C.. Plante cuny. M.R., Plante. R. & Salf.n picard. C.. 1990. —
Incidence of mussel culture on biogeochemical fluxes at the sediment water interface. Hydrobiologia . 207 : 187-196.
Cammen, L.M., 1980a. A method for mesuring ingestion rale of deposit feeders and its use with the polychaete
Nereis succinea. Estuaries. 3 : 55-60.
Cammen. L.M.. 1980b. The significance of microbial carbon in the nutrition of the deposit feeding polychaete
Nereis succinea. Mar . Biol.. 61 : 9-20.
Clavier. J.. 1984. Production due to regeneration by Euclymene oerstedi (Claparede) (Polychaeta: Maldanidae) in
the maritim Basin of the Ranee (Northern Britany). J. exp. mar. Biol. Ecol.. 75 : 97-106.
Dobbs. F.C. & SCHOLLY, T.A.. 1986. - Sediment processing and selective feeding by Pectinaria koreni (Polychaeta:
Pectinariidae). Mar. Ecol. progr. Ser.. 29: 165-176.
DOBBS, F.C. & WHITLATCH, R.B.. 1982. — Aspects of deposit feeding by the polychaete Clymenella torquata.
Ophelia. 2 1 : 159-166.
FAUCHALD, K. & JUMARS. P.A.. 1979. The diet of worms: a study of polychaete feeding guilds. Oceanogr. mar.
Biol. Ann. Rev.. 17 : 193-284.
Forbes. I.L. & LOPEZ. G.R.. 1990. Ontogenic changes in individual growth and egestion rates in the deposit
feeding polychaete Capitello sp. I. J. exp. mar. Biol. Ecol.. 143 : 209-220.
G£RINO, M., 1990. - The effects of bioturbation on particle redistribution in Mediterranean coastal sediment.
Preliminary results. Hydrobiologia. 207 : 251-258.
G£RlNO, M.. 1992. — Etude experimentale de la bioturbation en milieux littoral et profond. Quantification des
structures de bioturbation et modelisation du remaniement biologique du sediment. These Doct. Univ. Aix Marseille II
207 pp.
GfiRINO, M. & STORA. G., 1991. Analyse quantitative de la bioturbation induite par la polychete Nereis
di versicolor. C. R. Acad. Sci.. Paris. 313 : 489-494.
Source : MNHN. Paris
ETHOI XXjIE ai jmentaire de tolyci ietes endogees
533
Haven, D.S. & MoRALEvS alamo. R.. 1966. — Use of fluorescent particles to trace oyster biodeposits in marine
sediments. J. Cons. perm. Ini. Explor. Mer. 30 : 267-269.
JACOBSEN, V.H., 1967. The feeding of the lugworm Arenicola marina (L.). Quantitative studies. Ophelia. 4 : 91-
109.
Kemp. W.M.. Sampou. P., Caffrey. J.. Mayer, M., Henri ksen, K. & Boynton. W.R.. 1990. — Ammonium recycling
versus denitrification in Chesapeake Bay sediments. Limnol. Oceanogr., 35 : 1545-1563.
KRISTENSEN. E. & ANDERSEN, F.O.. 1987. Determination of organic carbon in marine sediments ; a comparison of
two CHN analyzer methods. J. exp. mar. Biol. Ecoi. 109 : 15-23.
MAHAUT, M.L.& Graf. G.. 1987. — A luminophore tracer technique for bioturbation studies. Oceanol. Acta . 10 :
323-328.
Marsh. A.G., GREMARE. A. & Tenore. K.R., 1989. Effect of food type and ration on growth of juvenile Capitella
sp. I (Annelida: Polyehaeta): macro and micronutrients. Mar. Biol.. 102 : 519-527.
Pervesi.fr. P. & DWORSCHAK, P.C.. 1985. Burrows of Jaxea noctuma Nardo in the gulf of Trieste. Senckcnbergiana
maril. . 17 : 33-53.
Rhoads. D.C. & Boyer. L.F., 1982. — The effects of marine benthos on physical properties of sediments. A
successional perspective. In: P.L. Me CALL & M.J.S. TEVESZ (cds). Animal sediment relations. Plenum N.Y. : 3-52.
RHOADS. D.C. & Young. D.K.. 1970. The influence of deposit feeding organisms on sediment stability and
community trophic structure. J. mar. Res.. 28 : 150-178.
RODHOUSE, P.G. & RODEN, C.M.. 1987. — Carbon budget for a coastal inlet in relation to intensive cultivation of
suspension feeding bivalve molluscs. Mar. Ecoi Progr. Ser.,5 6 : 225-236.
VaUGELAS, J. de & BUSCAIL. R.. 1990. Organic matter distribution in burrows of the thalassinid crustacean
Cal licit inis laurae. Gulf of Aquaba (Red Sea). Hydrobiologia. 207 : 269-277.
Source
Source : MNHN. Paris
57
Polychaete distribution patterns on
Chlamys patagonica of the Magellan Strait
Rossana SAN FILIPPO
Islituto Policattedra di Oceanologia e Paleoecologia
Corso Italia, 55
95129 Catania, Italy
ABSTRACT
The composition of the community with epibiont polychaetes on a population of Chlamys patagonica (King &
Bodrerip) was studied together with the rates of covering on the opposite valves and the distribution patterns. A clear
differentiation was noted between the covering of the right valves and the left ones, which on average, for the
polychaetes is 0.7 % an the right valves but 4.2 % on the left ones. Differences were noted in the patterns and rates of
colonization of some polychaete species. Serpula narconensis and the sabellariid Idanthyrsus annatus were rare on small
Chlamys . but very common on medium and large ones, averaging about 9% cover on the left (uppermost) valve in large
Chlamys. but less than 1 % on the right valve. They ranked fourth, behind bryozoans, sponges and algae, in their
contribution to a rich epizoan community, which covered about half the surfaces of both valves, even in small Chlamys.
and became denser with age. In contrast the spirorbid Protolaeospira lebruni was much more numerous on right than left
valves, and on small than large Chlamys, suggesting that initial colonisation by spirorbids may occur during the
juvenile stage, when the Chlamys are attached to rocks.
RESUME
Modalites dc distribution de Polychetes sur Chlamys patagonica du detroit dc Magellan
La composition dun peuplemenl de polychetes epibiontes sur une population de Chlamys patagonica el ses rapports
avec les autres organismes sessiles out ete etudiees. On a examine les taux de recouvrement sur les valves opposees ainsi
que les modalites de distribution des epibiontes. Une nette differenciation de ces recouvrements a etc observee : ils ont
(pour les polychetes) des valeurs moyennes de 0.7 % sur les valves de droite cl de 4.2 % sur les valves de gauche. Le
recouvrement total croit rapidement avec la tail le des Chlamys. De profondcs differences ont egalement 6te relevees dans
les modalites et le temps de colonisation chez quelques espfcces de polychetes. Serpula narconensis et le sabellariide
Idanthyrsus annatus suivent la tendance generate d'augmentation du recouvrement au cours de la croissance des Chlamys,
atteignant un recouvrement d'environ 9 % sur les valves de gauche des Chlamys les plus ag£s. mais seulement l % sur les
valves de droite. Ces especes participent. en quatrieme position, apres les bryozoaires, les eponges et les algues. a la
formation d’une riche communaute d'epizoaires laquelle reeouvre environ la moilte de la surface des deux valves, memo
chez les jcunes Chlamys . et qui devienl plus dense avec lage. Au contraire, le spirorbe Protolaeospira lebruni presente
une colonisation initiale rapide des deux valves des Chlamys de petite taille, ce qui suggere que celte colonisation initiale
des spirorbes peut avoir lieu durant la periode juvenile des Chlamys, lorsqu’ils sonl encore attaches aux rochers.
S ANF1LIPPO. R., 1994. — Polychaete distribution patterns on Chlamys patagonica of the Magellan Strait. In:
J.-C. Dauvin. L. Laubier & D..I. REISH (Eds). Actes de la 4cme Conference internationalc des Polychetes. Mem. Mus.
natn. Hist. not.. 162: 535-540. Paris ISBN 2-85653-214-4.
Source : MNHN, Paris
536
R. SANFILIPPO
INTRODUCTION
As pari of an Iialian research program on subamarciic areas, an oceanographic expedition visited the Magellan
Strait in February-March 1991. The station examined was rich in the pectinid bivalve Chlamys patagonica (King
& Broderip). Specimens measured up to 8 cm in length and were densely covered with epibionts. This scallop is
commercially important and is fished along the Argentinian shelf. Adults belong to the vagile epi fauna whereas
juveniles attach lo the substratum by means of die byssus, but these juveniles were rare in the population
examined. This is probably because juveniles do not live in the same area as the adults as in other pectinids
(Waloszek & Waloszek, 1986; Dl Geronimo & Rosso. 1990). When at rest, adults lie on the substratum on
the right valve, which is white and slightly convex, whereas the left valve is turned up, brownish red and more
convex. Swimming occurs briefly and rather rarely. Chlamys patagonica lives on soft bottoms that can be
characterized as sandy to gravelly-sandy. Its shells are among the larger available substrata for attachment of sessile
epifauna.
MATERIAL
The study is based on 50 specimens of C. patagonica obtained alive at station 21, 52°52,7' S, 70°31,8' W, at
a depth of 80 m, Nordi-East of Punta Arenas, in the southernmost part of Paso Ancho, near the mouth of the
Segunda Angostura (Fig. 1).
0 50 100 Km
FIG. 1. Location of station 21
The area is characterized by a sustained hydrodynamism and by turbulent iuid irregular currents (Brambati et
a /., 1991). The substratum is gravelly sand with no muddy fraction. Chlamys patagonica is both alive mid dead
(disarticulated valves). Large pebbles and the scallop shells ;ire densely colonized by numerous epibionts. The
station is also characterized by the abundance of sponges, gasteropods (trochids), decapod crustaceans, echinoids,
asteroids, ophiuroids and ascidians. Mollusk shells dominate die thanatococnosis (Dl GERONIMO et al. , 1992).
METHODS
The percentage of the surface occupied by polychaete tubes was calculated for each valve wilh respect to die
total area. The sample of Chlamys was then subdivided into three size classes each corresponding to a different
growdi stage (Table 1 ). The growth rate of C. patagonica is slow; according to Waloszek & Waloszek (1986),
Source : MNHN, Paris
POLYCHAETES- DISTRIBUTION ON CHLAMYS PATAGONICA
537
this species needs 3 -5 years to reach a size of 50-60 mm. The average dominance value of each polychaete species
is given for each size group, the composition of die epifauna varying with die age (i.e. size) of die single peelinid.
The patterns of encrusting species found on each shell (left and right valves) were drawn, showing die position and
relative areas covered hy each of the polychaete species. The shells mapped were arbitrarily divided into nine
regions and the percentage cover of each species was estimated for each region and was then calculated for die three
size classes, roughly following the method used by Ward & Thorpe (1991).
Table 1 . — Subdivision into diree size classes of die sample of Chlamys paiagonica.
1 he area is characterized by a sustained hydrodynamism and by turbulent and irregular currents (Brambati el
al., 1991). The substratum is gravelly sand with no muddy fraction. Chlamys paiagonica is both alive and dead
(disarticulated valves). Large pebbles and the scallop shells are densely colonized by numerous epibionts. The
station is also characterized by the abundance of sponges, gasteropods (trochids). decapod crustaceans, echinoids.
asteroids, ophiuroids and ascidians. Mollusk shells dominate the lhanatocoenosis (Di Geronimo el al., 1992).
RESULTS
The data collected provided information on the composition of the epifauna and distribution of die polychaete
species and other epibionts. Epibionts (Rosso & SANF1L1PPO, 1992) essentially belong to a few group of
organisms (Table 2).
Table 2. — Epibiont groups on Chlamys paiagonica.
Hpizoan community on Chlamys paiagonica
Bryozoans and sponges are dominant, followed by the green algae; whereas, polychaetes and hydroids are
subordinate. The composition of the epifauna differed between the right and left valves. The left valves are
colonized by epibionts which develop in height like large agglu tinant polychaetes. colonies of celleporifonn
bryozoans. large barnacles, brachiopods and erect hydroids. On the contrary, the right valves are dominated by less
voluminous forms like inembraniporiform bryozoans and spirorbids. The differentiation between the opposite
Source
538
R. SANFILIPPO
valves is also shown by the average total covering: 51.6 % on the right valves, 65.3% on the left valves. On
some valves the covering may even reach and exceed 100 %. The total covering tends to increase from the smaller
sized scallops to llie larger ones, a phenomenon particularly evident in bryozoans and hydroids.
Five species of polychaetes were identified including three Spirorbidae, one Seipulidae and one Sabellariidae
(Table 3). Four were common and widespread around the southern p<irt of South America and Magellan strait
(Hartman, 1966; KN’IGHT-Jones & Knight-Jones, 1984, 1991), whereas Romanchella cf. invent is was here
recorded for the fust time. Instead R. inventis was only known from die subantarctic Tristan da Cunha and Marion
Islands (Harris, 1969: Knight-Jones & Knight-Jones, 1984).
Tubes of Serpula narconensis from Magellan station 21 and odier subantarctic areas have a pink or light orange
colouring, whereas tubes from high laUtudc Antarctica were entirely white and opaque. In fact, the Magellan Strait
tubes have a thin, coloured, transparent outer layer. It was also observed that juvenile tubes were morphologically
different: they were devoid of die pigmented transparent outer layer and appeared white, widi diree longitudinal,
toothed keels. The keels disappear in die adults and the tube tends to become smooth, in contrast to young
specimens.
Table 3. — List of polychaete species identified on C/ilamys pcitagonica.
Polyehaete community on Chlamys patagon ica
The average total surface covering by these species showed a higher rate of encrustation on the left valves
(4.2 %) than on die right (0.7 %). Similarly, the total covering increased as the pectinids grew larger. Although
the serpulids and sabellariids were more common in larger scallops, the reverse was true for the spirorbids (Fig. 2).
.S', narconensis was not present on the smallest pectinids (group A) and colonized only medium to Targe
scallops which thereby followed the general trend of the other epibionts (Fig. 2). The average covering by S.
narconensis was higher on the lclt valves (0.4 % and 0.6 % of groups B and C) compared to the right ones
(0.2 % and 0.2 % of groups B and C).
I he sabellariid Idanthyrsus armatus showed, even more markedly, the same distribution trend as 5.
narconensis: its big agglutinant tubes encrust only the left valves of medium and large sized scallops, with
covering values from 1.9 % to 8.6 %.
Fhe spirorbid Proiolaeospira lebruni colonizes all diree size groups. More right valves are covered than left ones
which is die reverse of that observed in the serpulid and sabellariid. It colonizes first the right valves of the smaller
scallops (group A) with a 0.6% dominance which progressively decreases to 0.4 % (group C). Moreover, P.
lebruni predominantly settles on the umbonal region of bodi valves (Fig. 2). The other species of spirorbids’ are
rare and are present only on the larger siz.e groups.
Source :
POLYCHAETES DISTRIBUTION ON CHU\MYS PATAGONICA
539
CONCLUSIONS
%
The frequency of polychaetes lends lo increase from the smaller valves to the larger ones which follows the
general trend of the other epibionts. However, the principle spirorbid species colonizes the smaller scallops,
whereas the other polychaetes encrust only medium or large sized scallops. This could be due to different strategies
depending on the species. Some species appear to be pioneer forms that colonize die newly available substrata
(young pectinids), whereas others appear only when the community is already mature, on medium and large sized
pcctinids.
The larger seipulids and sabellariids colonize only die left upturned valves, a survival strategy related more to
the size of their tubes, rather than to a phototropism. In contrast, the principle spirorbid species, which are
abundant on the low profiled right valves, appear better adapted to the physical abrasion effects, in direct contact
with the substratum. KNIGHT-JONES & KNIGHT-JONES (1984) also concluded dial P. lebnmi has die capacity of
widistanding sand abrasion. This was hypodiesized by Ward & THORPE (1991) for bryozoans. The spirorbid
distribution was not homogeneous on the right valve, but showed a concentration towards die umbonal regions,
particularly on the posterior side. The higher umbonal density may be due to more prolonged settlement, since this
area has been available for colonisation for a longer period than the younger peripheral parts of the shell. It is
unlikely to be related lo the swimming of Clilamys. This is caused by two jets of water emitted from between die
valves dorsally (Moore & Trueman, 1971), but swimming excursions are brief and very infrequent.
It seems possible that the asymmetrically posterior distribution of spirorbids may be related to the pattern of
eddies set up by the excurrent stream from the Clilamys mantle cavity, which could conceivably bring in settling
larvae and nutrients in suspension. Probably, moreover, much of die initial spirorbid settlement occurs during the
juvenile stage, when the Clilamys is attached widi the anterior side partially in contact with the substratum. The
relative abundance of spirorbids on smaller Clilamys could be due to their having been recently in juvenile
situations, with byssal attachments to larger rocks in shallower water, where spirorbids are more dominant
(KNIGHT-JONESS. com. pers.) The much denser algal cover also suggests dial diey may have been recently in
shallower water, although it must be admitted dial algae are among die earliest colonisers of new surfaces.
FIG. 1. — Diagrams showing changes in abundance of covering of some significant polychaetes species depending on
shell size (covering percentage for each of the nine mapped areas).
• < I % • = 10 % to 30 %
• = 1 % to 10 % £ > 30 %
Source :
540
R. SANFILIPPO
ACKNOWLEDGEMENTS
The author is grateful to Drs. P. and E.W. KNIGHT-JONES for help in identifying spirorbid species and for
useful discussions; and to Prof. I. Di Gf.ronimo mid Dr. A. Rosso of the University of Catania for helpful
suggestions; and to Caty Standley. B.A. for linguistic help. Research financially supported by P.N.R.A.
(Italian National Research Program in Antarctica), Biological Oceanographic Sector, Program on Benthic
Communities, Unit of Catania, Responsible Prof. I. Di Geronimo, paper n° 14.
REFERENCES
Brambati. A.. FONTOLAN. G. & SlM EON I, U., 1991. Recent sediments and sediinentological processes in the Strait of
Magellan. Boll. Oceana! .. 9 : 217-259.
DI GERONIMO. I. & ROSSO. A., 1990. First Italian Oceanographic Expedition in the Ross Sea. Antarctica. Benthos: a
preliminary report. Nat. Sc. Com. Ant., Ocean. Camp. 1987—88. Genoca, Data Report: (1990) l : 407-421.
Di GERONIMO, 1.. Privitera, S. & VALDOVINOS. C.. 1992. Molluskan Thanatocoenoses of the Magellan Strait. Mem.
Biol. Mar. e Oceanogr.. 19 : 205-208.
Harris, T.. 1969. - Spirorbid species (Polyehaeta: Scrpulidae) from the South Atlantic. Discover t Rep.. 35 : 135-
178.
HARTMAN, O.. 1966. — Polyehaeta Myzostomidae and Sedentaria of Antarctica. Antarctic Res. Ser.. 7 : 1-158.
Knight-Jones. 1*. & Knight-Jones. E.W., 1984. — Systemalics, ecology and distribution of southern hemisphere
Spirorbids (Polyehaeta; Spirorbidae). In: P.A. HUTCHINGS (cd). Proceedings of the First International Polychaete
Conference. Sydney. Linnean Society of New South Wales. Sydney : 197-210.
KNIGHT-JONES, P. & Knight-Jones. E.w.,1991. — Ecology and distribution of Serpuloidea (Polyehaeta) round South
America. Ophelia, suppl. 5 : 579-586.
MOORE. J.D. & Trueman, E.R.. 1971. — Swimming of the scallop. Chlamys opercularis (L.). J. exp. mar. Biol. Ecol..
6 : 179-185.
Rosso. A. & SANFILIPPO, R., 1992. Epibiont distribution pattern on Chlamys patagonica (King & Broderip) of the
Magellan Strait. Mem. Biol. Mar. e Oceanogr.. 19 : 237-240.
Waloszek, D. & WalOSZEK. G.. 1986. — Ergebnisse der Forschungreisen des EES "Walther Herwig" nach Sudamerika.
LXV. Vorkommen. Reproduktion. Wachslum und mogliche Nutzabarkeit von Chlamys patagonica (King & Broderip,
1832) (Bivalvia, Pectinidae) auf dem Schelf vor Argenlinien. Arch. Fisch.-Wiss., 37 : 69-99.
Ward. M.A. & Thorpe. J.P.. 1991. Distribution of encrusting bryozoans and other epifauna on the subtidal bivalve
Chlamys opercularis . Mar. Biol.. 110: 253-259.
Source :
58
Polychaeta in the estuary of the Piaui River,
Sergipe, Brazil
Maria A. SANTOS, C.S.G. SANTOS & C.M.M. OLIVEIRA
Departamento de Biologia
Campus Universitario
49000 Aracaju. Sergipe. Brasil
ABSTRACT
I he distribution o! infaunal polychaetcs was examined in order to discriminate polychaete assemblages in the estuary. In
March 1987. 4.398 specimens were collected in 123 samples from 15 areas. A cluster and ordination analysis was used to
define benthic polychaete assemblages. Two associations were present which were related to the high and low energy
deposit ion al environments and hydrological gradients. The first group, restricted to the upper reaches of the estuary, was
composed of Laeonereis acuta. Amphicteis gunneri , Heteromastus similis . Neanihes succinea and Scolelepis texana. The
second group, present in the middle section of the estuary, was dominated by Prionospio (P.) cf. dubia, Scoloplos sp..
Euclymene sp.. lsolda pulchella and Mage Iona papillicomis.
RESUME
Polychetes de Pestuairc de la riviere Piaui, Sergipe, Bresil
Cette etude porte sur la distribution de la faune des Polychetes de l’estuaire du fleuve Piaui. 4 398 specimens furent recolles
en mars 1987. cn 123 echantillons de 15 regions. L’analyse en composantes principals et la classification hierarchique
permellent dc definir les assemblages des Polychetes benthiques. Deux groupes out etc identifies: le premier est restreint a la
partie amont de 1'esEUaire du Piaui; il est forme de Laeonereis acuta. Amphicteis gunneri. Heteromastus similis. Neanthes
succinea cl Scolelepis texana. Le deuxiemc groupe est present dans la panic moyenne de Pestuairc. avec les espcces
dominanles Prionospio (P.) cf. dubia. Scoloplos sp., L uc.lymene sp.. lsolda pulchella et Magelona papillicomis.
INTRODUCTION
The estuary of die Piaui River is located in die state of Sergipe, Brazil. A qualitative study of polychaer.es was
made off-shore (Nonato & Luna. 1970 a. b) and in the Sergipe River Estuary (Santos, 1979) which provided
information on the distribution of polychaetcs and other animals. Studies were made in the Piauf-Fundo-Real
system to characterize die region, according to physicochemical variations (Alves, 1989). zooplankton (Araujo,
1989), sediment and Foraminifera distribution (Zucon. 1989) and phytoplankton (Franco, 1991). Macrobenthic
Santos. M.A., Santos, C.S.G. & C.M.M. Oliveira. 1994. - Polychaeta in the estuary of the Piaui River Sergipe, Brazil.
In: J.-C. Dauvin. L. Laubier & D.J. RE1SH (Eds). Actes dc la 4eme Conference internationale des Polychetes. Mem. Mus.
natn. Hist. not.. 16 2 : 541-547. Paris ISBN 2-85653-214-4
Source : MNHN , Paris
542
M.A. SANTOS. C.S.G. SANTOS & C.M.M. OLIVEIRA
fauna studies in other estuarine regions of die Brazilian Coast have been made by Bemvenut (1987), Lana
(1986) and Lana ei al. (1989). The objective of this paper is to describe the distribution and diversity of subtidal
polychaetes in a tropical estuary located in northeast Brazil.
STUDY AREA
The Piaui River is part of the estuarine complex, located in Scrgipe, Brazil (11°22'30" S / 32°22'33" W)
(Fig. 1). It is approximately 40 km long and 50-5.000 m in width. The depth ranges from 1-27 m (Franco. 1991).
The water temperature ranged from 24 to 29.5 °C in 1986/87 (Alves, 1989). The region is characterized by dry
and wet periods. The rainfall ranges from 241.5 mm/month in July to 46.1 mm/montli in December (ALVES,
1989). The sediment of die Piaui River varies from coarse sand poorly selected in die upper estuary to fine sand
well selected at the mouth. The total granulomeuical distribution has a median value of 2.5 (± 1.1) and varies
from coarse sand to day. The highest percentage of line sand was 43.6 (ZUCON, 1989). The selection varies from
1.16 % well selected sediment to 53.18 poorly selected sediment. The areas 7 to 10 (Fig. 1) are characterized by
biodetritus.
The salinity varies as a result of seasonal fluctuations of rainfall, river run-off, and tidal amplitude (Franco,
1991). These waters can be divided into diree categories: 1) limnetic water from river flow in die upper part of die
estuary. 2) mixohaline waters from die mixture of river and coastal waier and 3) mixoeuhaline waters at the mouth
of the river (Alves, 1989).
Dissolved oxygen generally ranged from 2.2 to 6.8 mg. N (Alves, 1989). The median estuarine region
showed the highest level of nutrients, diatom density and zooplankton (Alves, 1989: Franco, 1991: Araujo,
1989). The changes in nutrients are probably a consequence of die annual climatological and hydrographical
pattern. °
Source :
POLYCHAETA IN THE ESTUARY OF THE PIAUI RIVER. SERGIPE. BRAZIL
543
MATERIAL AND METHODS
Samples were taken in March 1987. Fifteen areas were sampled along 35 km of die estuary (Fig. 1). A total of
123 samples were taken using a 10 liter Van Veen grab. Three stations were sampled in each area, and four
replicates were taken at each station, one for sediment analysis and Uirec for biological analysis. Only two stations
were sampled in areas 12 - 15. Each biological sample was washed through a 0.5 mm sieve. Larger animals were
picked from the sieve. Remaining material was stained with Bengal Rose and fixed in formalin. Samples were
transferred to 70 % alcohol prior to identification. Environmental parameters and other biological aspects of die
Pi auf estuarine system were studied concurrently (Alves, 1989: Araujo, 1989; Fontes, 1989; Zucon 1989-
Franco, 1991).
The species were ranked according to occurrence, abundance and percentage of total number of specimens.
The Shannon-Wiener diversity index and evenness indices were used (Gray. 1981). A matrix data with the
abundance of 80 species and 41 samples was used for die data analysis. The replicates were summed up by area
•or cluster and ordination analysis. The variables indicating abundance were logarithmically transformed using die
expression Y,, = log (x,, + 1) (Green, 1979).
The matrix was subjected to a cluster analysis (WPGMA), employing the Czekanowski Coefficient of
similarity. The multivariate similarity patterns were also studied with a Q-mode Principal Component Analysis
(PC A). The analysis in Q mode was done because of die huge number of species. A computer program ACOMP
written by J. L. VALENTIN (IEAPM - MM) was used.
RESULTS
A total of 4,398 specimens was collected which belonged to 81 taxa in 32 families. The dominant taxa were
identified by occurrence and abundance. The most abundant species were Prionospio (P.) cf. dubia, Laeonereis
acuta, Euclymene sp. and Isolda pulcliella (Table 1). The diversity ranged from 0.01 to 2.8 and was higher from
areas 2 to 10. The lowest value was found at areas 1 1 to 15 (Table 2).
c
57
SIMILARITY
Fig. 2. Dendrogram for 80 species of polychaetes, considering 15 areas. The abundance of the species was summed up in
each area.
Cluster analysis indicated: 1) Area 1 at the mouth of die river is euhaline and is separated from the others. The
salinity was about 35,0 %o, and die sediment was principally well sorted fine sand. 2) Areas 2 to 1 1 were clustered
together with two groups: areas 2. 3, 5 and 4. 7, 8. 9. 10, 11. The salinity ranged from 18-30, P.S.U. and the
544
M.A. SANTOS, C.S.G. SANTOS & C.M.M. OLIVEIRA
Table 1. — Rank and abundance of the most common polychaetes taxas collected in die Piauf River, Sergipe.
Source : MNHN, Pans
POLYCHAETA IN THE ESTUARY OF THE PIALII RIVER. SERGIPE. BRAZIL
545
sediment ranged from sand 10 sill and clay and was characterized for biodelritus in areas 7 toll. 3) Areas 12 lo 15
were characterized by salinity ranging from 1 to. 15 P.S.U., going from mesohaline to oligohaline zones. The
sedimem was mostly coarse sand.
I’ABLii 2. — Diversity and evenness values
These groups of areas, clustered together, were partially influenced by changes in polychaete density.
However, these results divided the Piauf River in 3 regions: die mouth, area 1. the lower estuary, area 2 to 1 1 and
the upper estuary, area 12 to 15.
"
PRINCIPAL. COMPONCNT I
•V
;2*’3
0.0 . 0.3 • U>
PRINCIPAL COMPONENT I (31,6%)
FIG. 3. - Position of 15 areas on principal components: left, I. U and HI: right. I and IV showing principally area 1 .
By projecting the scores in the orthogonal space of the first three principal components (Fig. 3A), it was
Possible to see that groups of stations were perfectly discriminated. The first axis was related to die abundance of
Prionospio (P.) cf. dubia, Scoloplos sp„ Euclymene sp„ I soldo pulchella and Ceratocepliala crosslandi.
indicating the most similar areas from 2 to 1 1 divided into two groups: 2 to 5 and 7 to 1 1 . The second axis was
Source :
546
M.A. SANTOS. C.S.G. SANTOS & C.M.M. OLIVEIRA
related to the abundance of Laeonereis acuta , Amphicteis gunneri. Scolelepis texana , Hemipoclus sp. in areas 12 to
15. The fourth axis was probably related to the negative abundance of species (Fig. 3B). Almost the same groups
were obtained by cluster analysis: area 1 isolated, areas from 2 to 1 1 clustered together and areas 12 to 15
clustered together (Fig. 2).
DISCUSSION
Tropical estuaries are influenced by the seasonal rain pattern and the resulting effects due to sedimentation,
erosion, dissolved oxygen and nutrients. Nearly all the benthic surveys of tropical estuaries have been taken along
the east and west coast of India, (ALONGI, 1990). The most extensive investigations of subtropical estuarine
macrobenthos were near Brisbane in Queensland. Australia (STEPHENSON et al ., 1972; STEPHENSON el al ., 1977).
STEPHENSON et al. (1972) stated that workers in the subtropics and tropics failed to find communities with only a
few dominant species.
Maurer & Vargas (1984) found a depauperated infauna in the soft bottom benthos in the Gulf of Nicoya,
Costa Rica. They concluded that tropical estuarine communities were generally low in density and biomass. The
mean Shannon-Wiener diversity for polychaetes was of 1.91, range = 0 to 3.09 (Maurer et al. 1988).
In the Piaui River the diversity was similar to die values found in Costa Rica (Maurer*/ al, 1988). The
influence of industrial wastes in the Piaui River estuary could be considered as a factor causing the low diversity.
Comparison of die polychaetes obtained in the Piaui River estuary and die Sergipe estuary in the northeastern
region of Brazil (Santos, 1979) showed die same pattern of species composition and species abundance.
Zones of changes occurred in the Piaui River, and it was possible to divide the river in three region, the moudi,
the lower estuary and the upper estuary. Similar regions were found in foraminiferan studies of Piaui River
(ZUCON, 1989) and macrobendiic studies of Sergipe River (Santos, 1979).
The upper part of the Piaui Estuary, areas 12 to 15. was dominated by L. acuta and A. gunner! . The occurrence
of L. acuta as dominant species, in the upper river, was observed in Sergipe Estuary (Santos, 1979). The
occurrence of L. acuta and H. siniilis association in the upper river was also observed in die southeastern coast of
Brazil (Lana, 1986; Bemvenuti, 1987). These species are euryhaline with reduced mobility.
In die lower estuary areas 2 to 1 1 widi mixohalinc waters, the greatest abundance of polychaetes, plankton and
nutrients were present (Alves, 1989; Franco, 1991). This suggested diat die benthic population distribution was
influenced not only by salinity and sediment but also for nutrients and productivity (ALONGI, 1990). The
occurrence of Prionospio (P.) cf. dubia , Scoloplos sp., Euclyniene sp., I soldo pulchella and Ceratocephala
crosslandi association was also found in Sergipe Estuary (Santos, 1979).
Area 1 was located at die moudi of the estuary, in a region of continuous sedimentation, and was separated
from the others by cluster and PC analysis.
The pattern of distribution of die polychaetes in the Piaui River are directly influenced by die physicochemical
gradients, sediment types and by topography. It is possible to notice groups of dominant species in each one of the
three regions, and the decrease of die diversity from die inoudi to the head of die estuary.
ACKNOWLEDGEMENTS
We are grateful to M Sc C. R. P. Franco for critically reading die manuscript, to Dr. Paulo da C. Lana for help
us in polychaete identification and A. F. Diniz for ordenation analysis. This study was supported through grant
from the Interministry Commission for Marine Resources.
REFERENCES
Alves, J. P. 1L, 1989. Projeto integrado para avalia^ao da potencialidade do estuario dos rios Piam-Fundo-Real: Vol. II.
Caractensticas fisico-quunicas da agua e comportamento dos nutrientes. Report . Aracaju/SE, UFS. 43p.
ALONGI, D. M.. 1990. The ecology of tropical soft-bottom benthic ecosystems. Oceanogr. mar. Biol. Ann. Rev.. 28 : 38 1 -
496.
Araujo, II. M. P., 1989. Projeto integrado para avalia^ao da potencialidade do estuario dos rios Piauf-Fundo-Real: Vol. 111.
Biomassa do zooplancton. Report, Aracaju/SE, UFS. 130 pp.
Source :
POLYCHAETA IN THE ESTUARY OF THE PIAUf RIVER. SERGIPE. BRAZIL
547
BEMVENUTI, C. E.. 1987. — Macrofauna bentonica da regiao estuarial da Lagoa dos Patos, RS. Brasil - Simposio sobre
ecossistemas da costa sul e sudeste brasileira. Publ. ACIESP , 54 : 428-459.
FoNTES, A. L.. 1989. — Projeto integrado para avalia$ao da potcncialidade do estuario dos rios Piauf-Fundo-Real: Vol. I.
Caracteriza^ao geomorfologica da bacia do Mangue Seco (Piaui-Fundo-Real). Report. Aracaju/SE, UFS. 22 pp.
FRANCO, C. R. P.. 1991. Plancton diatoms of the Piauf river estuary (Brazil): seasonal distribution and biogeographic
affinities. Master Thesis, University of Rhode Island. Kingston. 169 pp.
Gray. J. S.. 1981 — The ecology of marine sediments. Cambridge University Press, London. 185 pp.
GREEN, R. H.. 1979. Sampling design and statistical methods for environmental biologists. John Wiley & Sons. New York.
257 pp.
Lana. P. C.. 1986. Macrofauna bcntica de fundos sublitorais nao consolidados da Baia de Paranaeua (Parana) Neriticci I
79-89.
Lana, P. C., Almeida. M. v. o.. Freitas. C. a. F., Couto. E. C. G.. Conti. L. M. P.. Gonzalez- Peronti. a. I... Giles,
A.G.. LOPES. M. J. S., Silva, M. II. C. & PEDROSO. L. A.. 1989. — Estrutura espacial de associasoes macrobcnticas
sublitorais da Gamboa Pereque (Pontal do Sul. Parana). Nertlica. 4 : 129-136.
Maurer. D. & Vargas, J. A.. 1984. Diversity of soft-bottom benthos in a tropical estuary: Gulf of Nicoya, Costa Rica.
Mar. Biol.. 81 : 97-106.
MAURER, D., Vargas. I. A. & DEAN, H., 1988. Polychaetous annelids from the Gulf of Nicoya, Costa Rica Ini Rev.
Gesamten Hydrobiol.. 73 : 43-59.
NonaTO. E. F. & LUNA, .1. A. C.. 1970a. — Sobre alguns poliquetas de escama do Nordeste do Brasil. Bohn. Inst. Oceanogr..
Sao Paulo, 18 : 63-91
Nonato. E. F. & Luna. J. A. C.. 1970b. Anelideos poliquetas do Nordeste do Brasil. I. Poliquetas bentonicos da costa de
Alagoas c Sergipe. Bohn. Inst. Oceanogr.. Sao Paulo. 19 : 57-130.
Santos, M. a., 1979. MacroJ'auna benlica do estuario do Rio Sergipe ( Eslado de Sergipe. Brasil). Doctor Thesis.
Universidade de Sao Paulo. Sao Paulo, 128 pp.
STEPHENSON, W.. Cook, S. D. & Raphael, Y. I.. 1977. — The effect of a major flood on the macrobenthos of Bramble Bay,
Queensland. Mem. Queensl. Mus.. 18:95-1 19.
STEPHENSON, w., Williams, W. T. & Cook. S. D.. 1972. — Computer analyses of Petersen's original data on bottom
communities. Ecol. Monogr.. 42 : 387-409.
Zucon, M. II.. 1989. — Distribuigdo dos fo ram inferos e tecamebas do estuario do rio Piaui-Sergipe. Master Thesis.
Universidade Federal do Parana, Curitiba, 54 pp.
Source :
Source : MNHN. Paris
58
Life history of the Polychaete Polydora variegata
that bores into the shells of Scallops
in Northern Japan
Waka SATO-O KOS HI
Laboratory of Biological Oceanography
Faculty of Agriculture, Tohoku University
Sendai 981, Japan
ABSTRACT
The genus Polydora (Polychaeta, Spionidae) is widely known for its boring activities in mollusean shells. Here we
describe the life history of Polydora variegata, which causes considerable damage to scallops sown in the waters of
Abashiri Bay. off the Okhotsk Sea coast of Hokkaido. Japan, by spreading blisters and penetrating the shells. The life
span of P. variegata was 2.5 years after settlement, and the main spawning period of both 0- and 1-yr-olds was from
August to October. 1'hree-setiger larvae hatched from the egg capsule mainly from September through November.
Settlement of 17-setiger larvae took place during the drift-ice period. There was a tendency for the earliest settlement of P.
variegata to occur on a narrow band around the periphery of the left valve of the scallops. A large body size, high
reproductive activity and a long life span seem to be characteristic of this species of boring polychaete.
RESUME
Cycle dc vie du Polychete Polydora variegata , cspece perforantc des Coquilles Saint Jacques
dans le nord du Japon
Le genre Polydora (Polychetes, Spionidae) esl bien connu pour ses aclivilcs dc perforation des coquilles de
mollusques. Ce travail decrit le cycle de vie de Polydora variegata, espcce qui cause des dommages considerables aux
coquilles Saint-Jacques de la baie d'Abashiri. au large des cotes d'Hokkaido, en mer d’Okhotsk. Japon. par I'elendue des
boursouflures et la penetration des vers dans l’epaisseur des coquilles. La duree de vie de P. variegata est de deux ans et deini
apres la fixation, et la principale periode de reproduction pour les deux groupes d'individus d age 0 et d age 1 s’etend d’aout
a octobre. Les larves a trois setigeres sorlenl dc la capsule de foeuf principalemenl de septembre a novembre. La fixation
des larves a 17 setigeres se silue au moment de la debacle des glaces. On a note une tendance des P variegata a se fixer
d'abord sur une bande etroite aulour de la peripheric de la valve gauche des coquilles Saint-Jacques. Une grande taille
corporelle, une aclivite rcproductricc elevee et une longue duree de vie semblc etre les caracteristiques de cello espcce de
polychete perforante.
Sato-Okoshi. W.. 1994. — Life History of the Polychaete Polydora variegata that bores into the shells of Scallops
in Northern Japan In: J.-C. Daiivin. L. LAUBIF.R & D.J. REISH (Eds), Actes dc la 4eme Conference international des
Polychetes. Mem. Mus. natn. Hist, not., 162 : 549-558. Paris ISBN 2-85653-214-4.
Source :
550
W.SATO-OKOSin
INTRODUCTION
The spionid genus Polydora is found in a wide variety of substrates that range from soft clays or mud to hard
calcareous materials (Blake & Rvans, 1972). The life history and population dynamics of the genus have been
discussed by DoKSETT (1961), Daro & POLK (1973), GUDMUNDSSON (1985), and Zajac (1992). Nearly all the
previous studies have dealt with Polydora that inhabit soft-bottom habitats, but there have been only few studies
on dealing with those species which bore into shells.
Infestation by Polydora of commercially important molluscan shells is an important problem in aquaculture.
Polydora not only reduces the value of molluscs but causes considerable damage to die shell, especially diose in
cultures. The species that bore into the shells of Patinopecten yessoensis do not feed on the host's tissue; die shell
is used only as a refuge (Sato-Okoshi & Okosiii, 1992). Therefore, the polychaete is an inhabitant of die
molluscan shell and not a parasite. Nonedieless, some worms do penetrate die inner surface of the shell and induce
secretion by the shell of a thin layer of a dark or black organic material. Natural scallops with sufficiently thick
shells suffer little damage even with heavy penetration by Polydora. However, cultured scallops have thin shells, a
low growdi rate and as a result, considerable damage when subjected to a heavy infestation by Polydora.
The Okhotsk Sea coast of Hokkaido is well known for its natural supply of scallops. Sowing of cultures was
started in the waters of Abashiri Bay in 1977 in order to counteract the instability of the natural population. In
these cultures, worms were observed to bore into the left valves, an average of 162 per shell; a maximum of 327
worms per shell have been counted (Sato, 1988). Very few' worms bored into die right valve. The reproductive
characteristics of Polydora variegata have been reported by Sato-Okoshi et al. (1990). Details of its infestation
and the nature of die burrows have been characterized for population in Abashiri Bay and elsewhere (Mori et al .,
1985; Sato-Okoshi & Nomura, 1990). The present study summarizes the life history of P. variegata in
Abashiri Bay where it causes considerable damage to the scallops.
143°E
145°E
45°N
45°N
44° N
143°E
145°E
43° N
FIG. 1. — Location of sampling area.
Source :
LIFE HISTORY OF POLY DORA VARIEGATA INTO SHELLS OF SCALLOPS
551
MATERIALS AND METHODS
Three- to five-year-old scallops were collected monthly by dredging from April 1982 to December 1986
(excluding 1985) from a depth of 30 to 50 m in Abashiri Bay, on the Okhotsk Sea coast of Hokkaido, Japan
(Fig. 1), The scallops collected in 1982-1984 were the same cohort and their juveniles were collected in 1979 and
sown in 1980, and scallops collected in 1986 were sown in 1984 from (heir juveniles collected in 1983. Two to 1 1
scallops were examined each month.
The scallop flesh was removed, and the left valve was broken into small pieces with pliers, and P. variegata
were removed with forceps under a stereomicroscope. The presence of gametocytes was checked by rupturing
segments and transferring the coelomic contents onto a microscope slide. Body size was determined by measuring
the width of the fifth setiger after fixation in a neutralized 10 % solution of formalin.
Egg capsules were collected from the burrows of adults. The egg capsules were carefully removed from the
burrows with forceps and placed in culture dishes that contained filtered seawater. Alter hatching from the egg
capsule, larvae were maintained in 200-300 ml of filtered seawater in glass beakers at 12 °C. Larval development
was observed under a stercomicroscope until settling and metamorphosis. The seawater was changed every 3-5
days. Larvae were fed a mixture of Skeletonema costatum and Chaeloceros spp. taken from Onagawa Bay.
RESULTS
Settlement patterns and size-frequency distributions. — Strong growth-inhibition rings were found
on the shells of 4-year-old cultured scallops that had been sown in Abashiri Bay (Fig. 2). These rings corresponded
to the times at which (1) scallops had been sown in June (Rl): (2) the first winter season (R2); (.3) the second
winter season (R3); eic. (Sato-Okoshi el a/., 1990). In die winter season, die Okhotsk Sea coast of Hokkaido is
generally covered widi dril l ice from January to March and referred to as die "drift-ice period".
Fig. 2. — Growth-inhibition rings of scallops collected from Abashiri Bay. Rl: Ring formed when scallops were sown in
June; R2: ring formed during the first winter season; R3: ring formed during the second winter season (from Sato-
Okoshi el at., 1990)
Size distributions of P. variegata in 1982, 1983. 1984 and 1986 are shown in Figure 3. A large number of P.
variegata were observed to have bored around the inhibition rings, R2, R3 and R4, of die left valves. The size of
the worms from each inhibition ring was investigated. The widdi of the fifth setiger was used as an index of die
age of die worms (Mori et ai, 1985).
Source :
552
W. SATO-OKOSHI
Fig
. 3. — (1) on the left, (2) on the right. Size-frequency distributions of Polydora varicgata that had bored into the left
valves of scallops from April 1982 to December 1986 (excluding 1985). The worms in 1982-1984 were extracted
from a population of scallops of the same age (juveniles collected in 1979 and sown in 1980). The worms in 1986
were extracted from scallops that had been sown in 1984 (juveniles collected in 1983). ( 1. individuals that settled
around R2; . individuals that settled around R3; ■■ , individuals that settled around R4; l::::l. individuals that
settled around R5. (adapted from MORI el al. , 1985 and from SATO-OKOSHI el al., 1990). n, number of P. variegata
examined; sn. number of scallop shells examined.
Source : MNHN. Paris
I .IFF HISTORY OF POLYDORA VARIEGATA INTO SHELLS OF SCALLOPS
553
Young juveniles ofaboul 20 segments appeared around the periphery of the left valve in April, after the drift-
ice period. This observation suggests that the peripheral regions of the left valve during the drift-ice period
subsequently become growth-inhibition rings, and that worms that settled on the peripheral regions grew around
the inhibition rings. Thus, if both the age of the scallop and the boring region of the worms are known, it is
possible to estimate the age of P. vciriegata individuals.
Worms around R3 appeared to have setUcd on the peripheral regions of the left valve during the period when
the bay was frozen in 1982, while worms around R4 appeared to have settled on the peripheral regions during the
same period in 1983.
The worms that settled on R3 in die drift-ice period of 1982 seemed to survive until die summer of 1984 but
had disappeared by September. Thus, the life span of P. vciriegata seems to be approximately 2.5 years after
settlement on a shell. The widths of the Fifth setiger of newly setded worms varied from about 0.2 to 0.3 mm in
April and grew to approximately 1.0 mm in December, about eight months after settlement. Once they had reached
1.0 mm in width, the worms grew slowly. The width of the fifth setiger did, however, varied from 0.8 mm to 1.5
mm in the second summer.
There was a small influx of newly settled worms around R3 throughout the period from August to December,
1982 (Fig. 3). Furthermore, some small worms found around R3 in April 1983 were obviously the newly settled
young of 1983, demonstrating that, while almost all the juveniles settled around the peripheral region of the left
valve, some settled around the other rings.
The same tendency was observed in 1986. Newly settled worms of 1986 during the drift ice period were
observed to grow around R3 (0-year-olds) and larger worms which appeared to have settled in 1985 were observed
to grow around R2 (1 -year-olds).
From the data for 1982-1986, there seemed to be some years in which there was no settlement, for example,
the winter of 1981. No worms were observed to settle around R2 in spite of the large number of worms around R3
and R4. These results suggest that the number of worms that settle on a shell fluctuates annually.
Reproduction. — The reproductive patterns of 0- and 1 -year-olds have been described previously (Sato-
Okoshi el a /., 1990). Table 1 shows the number and percentage of worms that contained gametocytes in the
coelom and egg capsules in tubes in 1983 and 1986. Oocytes in the coelom of the female were shaped like an oval
disc with the di June ter of the long axis measuring 30 to 170 pm. Diameters of 130 to 140 pm were common in
August in 0-year-olds and those of 130 to 140 pm were common in May to September in 1 -year-olds in 1986
(Sato-Okoshi ei al , 1990).
The proportion of worms that contained gametocytes increased to above 70 % among 0-year-olds in September
and October, as the seawater temperature increased to 16-17 °C at a depth of 30 m. Some 0-year-olds measuring at
least 0.6 mm wide contained gametocytes in the coelom, and females produced egg capsules. Brooding females
appeared among the large worms of more than 0.8 mm in width in August and September, with an increase in
October. Plural number of egg capsules made an egg string, and each egg string contained about 300 to 1,000
eggs. When the drift-ice period ended, almost all the 1 -year-olds contained mature gametocytes. They were found in
almost all the 1 -year-olds throughout the ye;ir with a higher proportion of brooding females. Previous reports have
indicated that the main reproductive season is from August to October (Mori el al ., 1985; Sato-Okoshi et al. ,
1990). Egg strings were observed throughout die year. Females seemed to have the potential for producing egg
string repeatedly, with about 800 to 5,700 eggs produced per batch, during the period from August to October
predominantly. The relationships between the width of the fifth setiger of the brooding female and die number of
eggs per egg suing for 0-year-olds and 1-year olds are, respectively, as follows:
InY = -1.10 lnX + 7.80 (r2 = 0.092, n = 7) and InY = 1.05 lnX + 6.19 (r? = 0.082, n= 25) [X,
widdi of 5th setiger (mm): Y, no. of eggs/string].
Larval development. — Larvae remained in the capsules until die Uiree-seuger stage at which lime diey
hatched. The time from the initial deposition of eggs to hatching was approximately 2 weeks at 15 °C. The long
diameter of the oval fertilized egg was 150-160 pm widi mi average of 152.5 ± 1 1.0 pm. Asetigerous larvae
measured 160 to 230 pm in length. Large macromeres filled the central portion of each larva. Two small circular
eye spots were located dorsal ly. The larvae elongated and one or two distinct setigerous segments appeared. One-
and two-setiger larvae measured 220-240 pm and 230-280 pm in length, respectively. Both early and late diree-
setiger larvae (Fig. 4A-B ) were positively phototactic. Yolk was still present within the gut. Four eyes were
located on the dorsal surface of the head. Black pigmentation was seen on the dorsal surface of the third setiger and
at the posterior end. Both the number and die length of die setae increased as this larval stage grew.
554
W. SATO-OKOSMI
Table 1 . — Numbers and frequencies of sexually mature worms of Polydora variegata in Abashin Bay in 1983
and 1986. Numbers in parentheses show die frequency (%).
Larvae were released from the egg capsules during the late three-setiger stage, and they were able swimmers.
Larvae were planktotrophic until they reached die 17-setiger stage, a process dial required more than two months at
15 °C. The length of planktonic three-setiger larvae was 250-320 pm. The embryonic yolk was no longer present
by the six-setiger stage. The 13-setiger larvae were about 750 pm long, and palps were present. Gasirotrochs were
located on setigers 3, 5, 7 and 10. The 14- ( Fig. 4C) and 15-setiger larvae were about 800 and 950 pm long,
respectively. A modified prostomium and yellow pigmentation were apparent. The 16- and 17-setiger larvae (Fig.
4 D) were 1.0 and 1.25 mm long, respectively. Palps were elongated to the end of die fifth setiger and four eye
spots were in trapezoidal arrangement. Distinct black pigmentation was present on the dorsal surface of llie 15th,
16th and 17th setigers, and gasirotrochs were present on setigers 7, 10, 13 and 15. The modified spines and
accompanying companion setae on setiger 5 developed and emerged at this stage; they were present on some
worms at the 15-setiger stage. A caruncle gradually developed and appeared at the 14-setiger stage. The 17-setiger
stage was reached in a minimum of 36 days and a maximum of 65 days.
The larvae of P. variegata were not easily induced to settle and metamorphose. Only five out of 200 larvae
completed metamorphosis. These larvae took more than two months to settle and metamorphose after hatching.
Almost all the 17-setiger larvae were alive for more than two months and up to as much as three months without
settling and metamorphosing. There was no apparent change in morphology of these larvae apart from slight
elongation.
DISCUSSION
A large number of worms of llie genus Polydora were found to have bored into the shells of sown cultured
scallops in Abashiri Bay. The boring species were P. variegata, P. websteri . P. concharum, P. concharum
Source : MNHN, Paris
I JFE HISTORY OF POLYDORA VARIEGATA INTO SI IFLLS OF SCAI .LOPS
555
subspecies and P. convexa. The relative frequencies of these species were 55.5 %, 17.3 %, 0.4 % 26.6 % and
0.2 %, respectively, throughout die year. We have studied die reproduedve characteristics and settling periods of P
websten and P. concharum subspecies.
Fig. 4. Photographs of larvae of Polydora variegata. A. Early three-setiger larva; B. late three-setiger larvae; C. 14-
setiger larva; D. 17-setiger larva.
I here are two reproductive populations of P. websteri which are found in early summer and in autumn (Sato,
1988). Females apparently produce egg string only once with approximately 500 eggs per batch. Their juveniles
tend to settle on die ventral edge of die left valve, in the same way as P. variegata, after approximately one
month's planktonic life. Their life span seems to be one year' .
No mature individuals were observed in die case of P. concliarum ssp. The strong regenerative activity and die
fact that more than two worms inhabit each burrow suggest that asexual reproduedon might be occurring in diis
species. Five species of die genus Polydora. which coexist in the same scallop shell, seem to have different life-
cycle patterns.
There are many reports with descriptions of the reproduedon of the genus Polydora (WlLSON.1928; llKMPEL,
1957; Hatfield, 1965; Mizumoto. 1966; Blake, 1969; Rasmussen, 1973; Day & Blake, 1979; Anger.
ANGER & Hagmeier, 1986; Radashevskii, 1986). For many species of Polydora, the life span has been
reponed to be about one year or less and diey die after their first or several spawnings within a year (S0DERSTROM,
1920; Lambeck & Valentijn, 1987). Under natural conditions, only the example from northeast England offers
the possibility of some worms surviving for more than a year and spawning again (GUDMUNDSSON, 1985). In die
case of P. variegata, however, all the worms seem to survive for 2.5 years after having settled on die scallop
shells. They spawn during the first year and also in the subsequent year, producing one to several batches of egg
strings during the main spawning season. P. variegata produced 300 to 1,000 eggs per batch in die first year and
800 to 5,700 eggs in the second. Moreover, die 1 -year-olds apparently produced egg strings year round. The
Source
556
W. SATO-OKOSin
maximum body size of 30 mm in length and 1.6 mm in width, the high reproductive activity and a long life span
are characteristic of die boring polychaete P. variegata.
The life history of P. variegata is shown schematically in figure 5.
Pic. 5. — Schematic diagram showing life history of Polydora variegata.
Live Polydora worms were found only in the shells of live scallops or in shells just after the death of scallops.
No worms were collected from the benthos. From a depth of 15 to 45 m in Abashiri Bay, Tectonatica
janthostomorides , Mercenaria stimpsoni , Fusitriton oregonensis, Glycymeris yessoensis, Chlamys swift i and
Buccinum ochotence live among high densities of natural mid sown scallops. We have observed live Polydora
species only in the shells of T. janthostomoides and F. oregonensis. Some worms of P. websteri were taken from
the shells of T. janthostomoides, and many worms of P. concha rum ssp. were extracted from those of F.
oregonensis. P. variegata was never extracted from any of Uiese species.
P. variegata and P. websteri settle on the ventral edge of the left valve. In contrast, P. concharum ssp. seems to
have no tendency in settling region. However, its burrows are found in aggregates. In die case of P. websteri and
P. concharum, each species was found in only a few shells into which no other species had bored. Very few worms
of P. variegata were taken from diese shells. The number of Polydora extracted from one shell fluctuated greatly
which may be the result of patchy distribution of larvae.
The tendency of P. variegata to settle on the ventral edge of die left valve seems to suggest that (1) larvae are
induced to settle by some chemical substance(s) contained in the newly formed periostracum, and (2) it is more
advantageous to settle on this edge of the left valve for feeding. Indeed, Polydora worms tire basically suspension
feeders mid die scallop always tends to face the oncoming water current.
Identification of the species in the genus Polydora has been somewhat confused in Japan. P. variegata was
mistaken for P. ciliata until it was redescribed as a new species by IMAJIMA & Sato in 1984. The distribution of
P. variegata has not yet been investigated. We have reported that P. variegata is distributed in the Okhotsk Sea,
Mutsu Bay and along the Pacific coast of Tohoku district (Mori et al. , 1985; Sato-Okoshi & Nomura, 1990).
Our present data indicate dial P. variegata is distributed extensively in die northern part of Japan.
It would be advantageous to prevent the settlement of P. variegata on die shells of scallops during the first
winter season after sowning, and it would seem belter to harvest scallops after two years in Abashiri Bay. We
Source :
LIFE HISTORY OF POLY DORA VAR1EGATA INTO SHELLS OF SCALLOPS
557
mentioned previously that when numerous worms settle on the ventral edge of die left valve of 1-year-old sown
scallops in the first winter season after sowing, the site of attachment of the adductor muscle to the left valve
overlaps tiie region of the shell that is heavily infested with 1 -year-old worms because die adductor muscle inceases
in size and shifts its position toward the ventral side during growth in the following year (Mori et ell., 1985;
Sato-Okoshi el ai, 1990). Scallops that are heavily infested widi Polydora at die site of attachment of the
adductor muscle may be weakened and penetration at this site may be fatal (Mori el at., 1985). Furthermore,
worms become a year old before harvesting the scallops when they settle on scallop shells during die first winter
season, and the 1 -yr-old worms produce many offsprings.
It would be of importance to determine the length of the planktonic period and the mechanism of settling of the
worm, as well as to determine why the larvae prefer to settle on the ventral edge of the left valve rather than the
right valve of the scallop. Experimentation in die laboratory may help to clarify these issues.
ACKNOWLEDGEMENTS
We are indebted to Prof. Tadashi NOMURA of the Department of Fishery Science. Faculty of Agriculture,
Tohoku University, for making it possible for us to carry out this study. Thanks are also due to the staff of die
Abashiri Scallop Research Laboratory, Abashiri, for their assistance in collecting the materials, and to Dr. Kenji
OKOSHI of die Department of Biotechnology. Senshu University of Ishinomaki, for his critical comments on the
manuscript.
REFERENCES
ANGER. K.. ANGER. V. & HAGME1ER. F... 1986. — Laboratory studies on larval growth of Polydora ligni. Polydora ciliala
and Pigospio elegans Polychaeta Spionidae. Helgolander Meeresunters, 40 : 377-396.
Blake, J.A.. 1969. — Reproduction and larval development of Polydora from northern New-England (Polychaeta;
Spionidae). Ophelia . 7 ; 1-63
Blake. J.A. & FVANS. J.W.. 1972. — Polydora and related genera as borers in mollusk shells and other calcareous
substrates (Polychaeta; Spionidae). Vellger, 15 : 235-249.
Daro. M.II. & POLK, P., 1973. — The autoecology of Polydora ciliata along the Belgian coast. Neth. J. Sea Res., 6 :
130-140.
Day, R.L. & Blake, J.A.. 1979. — Reproduction and larval development of Polydora giardi Mesnil (Polychaeta;
Spionidae). Biol. Bull. mar. biol. Lab., Woods Hole. 156 : 20-30.
DORSETT, D.A.. 1961. — The reproduction and maintenance of Polydora ciliala (Johnsl.) at Whitstable. J. mar. biol. Ass.
U.K ., 41 383-396.
GUDMUNDSSON. H.. 1985. — Life history patterns of polychaelc species of the family Spionidae. J. mar. biol. Ass. J.K..
65 : 93-1 1 I.
Hatfield, P.A., 1965. — Polydora commensalis Andrews Larval development and observations on adults. Biol. Bull,
mar. biol. Lab., Woods Hole. 128 : 356-368.
HEMPEL, C\, 1957. — Uber den Rohrenbau und die Nahrungsaufnahme einiger Spioniden (Polychaeta Scdenlaria) der
Deutschen kiisten. Helgolander wiss. Meeresunters, 6 : 100-135.
IMAJIMA, M. & Sato. W.. 1984. — A new species of Polydora (Polychaeta. Spionidae) collected from Abashiri Bay.
Hokkaido. Bull. Nam. Sci. Mus., Tokyo (Ser. A), 10 : 57-62.
LamBECK, R.II.D. & ValentijN, P.. 1987. — Distribution dynamics and productivity of a colonizing Polydora
quadrilobala and an established Polydora ligni polydorid polychaete in Lake Grevelingen. an enclosed estuary in the
southwest Netherlands. Neth. J. Sea Res., 21 : 143-158.
MlZUMOTO, S., 1966. — Studies on the disease of the shells of pearl oyster ( Pinciada mariensii). 2. On the seasonal
variation in occurrence Polydora ciliala in shells of pearl oyster. Bull. nail. Pearl Res. Lab., 11 : 1368-1377.
Source
558
W. SATO-OKOSHI
Mori. K.. SaTO. W.. Nomura. T. & IMAJIMA, M.. 1985. — Infestation of the Japanese scallop Paiinopecien yessoensis
by the boring polychaeles, Poly do ra, on the Okhotsk Sea coast of Hokkaido, especially in Abashin waters. Bull.
Jap. Soc. Scient. Fish.. 5 1 : 371-380.
RADASHEVSKII. V.I.. 1986. — Reproduction and larval development of the polychaete Polydora ciliata in Peter the Great
Bay of the Sea of Japan Russian SFSR USSR. Biol. Morya. Vladivost. 6 : 36-43.
RASSMUSSEN. K.. 1973. — Systematics and ecology of the Isefjord marine fauna. Ophelia . 11 : 1-495
Sato. W.. 1988. — Species, life history and infestation of the boring polychaeles. in the genus Polydora. in Japan.
Dissertation. Tohoku University, Sendai. Japan. 115 pp.
Sato-Okoshi. W., Sugawara. Y. & NOMURA. T.. 1990. — Reproduction of the boring polychaete Polydora variegata
inhabiting scallops in Abashiri Bay. North Japan. Mar. Biol.. 104 : 61-66.
SATO-OKOSHI. W. & NOMURA, T.. 1990. — Infestation of the Japanese scallop Paiinopecien yessoensis by the boring
polychaeles Polydora on the coast of Hokkaido and Tohoku District. Nippon Suisan Gakkaishi. 56 ( 10): 1593-1598.
Sato-Okoshi, W. & Okosiii. K.. 1992. — Polydora-Sc allop Interactions: Structural defenses in resistance to burrowing.
Aquabiology , 14 113-119.
Soderstko.M, A.. 1920. — Studien iiber die Polychaetenfamilie Spionidae. Inaugur. Dissert. University Uppsala, 286 pp.
Wilson, D.P., 1928. The larvae of Polydora ciliata Johnston and Polydora hoplura Claparede. J. mar. biol. Ass. U.K..
15 : 567-596.
Zajac. R.N.. 1992. — Population ecology of Polydora ligni (Polychaeta: Spionidae). 1. Seasonal variation in
population characteristics and reproductive activity. Mar. Ecol. Prog. Ser.. 11 : 197-206.
Source : MNHN. Paris
60
Annelid
polychaete populations of the Order Eunicida
from the southern Gulf of Mexico
Vivianne SOLIS-WEISS, Luz Veronica RODRIGUEZ-VILLANUEVA,
Alejandro GRANADOS-BARBA, Victor OCHOA-RIVERA
Luis Ml RAN DA -VAZQUEZ & Pablo HERNANDEZ- ALCANTARA
Institu to de Cicncias del Mar y Limnologia, UNAM
Apdo. Postal 70-305, Mexico, D.F.04510, Mexico
ABSTRACT
The Polychaete populations of the Order Eunicida, in the Mexican section of the Gulf of Mexico were analyzed.
Seventy six stations on soft bottoms were sampled from the continental shelf region (15 to 200 m) from Tampico to
Progreso covering approximately 46.000 km2. Sediments varied from fine muds to mixed sediments in the "terrigen"
western zone to calcareous sands and coralline fragments in the eastern "carbonated" zone. A total of 3,135 organisms
were identified. Among the five families present, 54 species were distributed as follows: Onuphidae: 17 (920 individuals).
Lumbrineridae: 16 (1808). Eunicidae: 14 (326). Arabellidae: 4 (76), Dorvilleidae: 3 (5). Four zones were identified. The
dominant species in zone 1 was Lumbrineris coccinea, in zone 2: L latreilli and in zones 3 and 4: S. verrilli. Sediment
composition and depth were the major factors in the distribution of the polychaeles. 'I he greatest diversity of this group
occured in shallow seas with calcareous sands.
RESUME
Les populations d'Annelides Polychetes de I'Ordre des Eunicida de la region meridionale du
golfe du Mexique
Les populations de Polychetes de I'Ordre des Eunicida du Golfe du Mexique out etc analysees. Soixante seize stations,
sur fond meuble ont ete retenues sur la plateforme continentale (de 15 a 200 m) de Tampico a Progreso dans une zone
couvrant environ 46 000 km2. Les sediments varient depuis les vases fines jusqu’aux sediments heterogenes dans la zone
occidental "Lerrigene". Dans la zone orientale "carbonatee", les sediments sont constilues de sables grossiers calcaires
et de fragments de coraux. Au total. 3135 Polychetes furent denombres. Parmi les cinq families presentes. 54 especes
furent identifies : Onuphidae : 17 (920 individus), Lumbrineridae : 16 (1808), Eunicidae : 14 (326). Arabellidae : 4 (76),
Dorvilleidae : 3 (5). Quatre zones ont ete identifies. L'especc dominante dans la zone 1 est Lumbrineris coccinea. dans la
SOLIS-WEISS, V.. RODRIGUEZ-VILLANUEVA, L.V., GRANADOS-BARBA. A. OCHOA-RlVEKA. V.. MIRANDA- VaZQUEZ. L. &
P. HERNANDEZ- Alcantara, 1994. — Annelid Polychaete Populations of the Order Eunicida from the Southern Gulf of
Mexico hr. J.-C. DaUVIN, L. LAUBIER & D.J. Reish (Eds), Actes de la 4eme Conference internationalc des Polychetes.
M6m. Mtis. natn. Hist. not.. 162 : 559-566. Paris ISBN 2-85653-214-4.
Source
560
V. SOLIS- W RTSS Kl ALII
zone 2 : L latreilli et dans les zones 3 el 4 : S. verrilli. La composition sedimentaire et la profondeur sonl les facleurs
preponderant* expliquant la distribution des Polychetes de cct Ordre, les sables calcaires et les eaux peu profondes leur
fournissant les conditions les plus favorables.
INTRODUCTION
The polychaeie fauna of ihe continental shelf in the U. S. region of the Gulf of Mexico is reasonably well
documented. The checklist of species and complete list of references include Perkins & Savage (1975) and die
recently published updated checklist by Salazar-Vallejo (1992). The taxonomic guide to die polychaetes of die
northern region of (he Gulf by UEBEI.ACKER & JOHNSON (1984) is the most modern and comprehensive work for
the area. FAUCHALD's (1992) recent worldwide review of the genus Eunice was also a useful reference for this
study. However, it is clear from diese publications that most of die work has been done outside the Mexican
Fig. 1. - Study area: Southern Gulf of Mexico. Shading indicates the extent of the carbonated zone.
region of the Gulf. Information on this region is relatively scarce, especially from the continental shelf since
Rioja (1961, 1962), Hartman (1951), Solis-weiss & Carreno (1986) Ibanez-Aguirrh & Solis-Weiss
(1986); previous studies concentrated on sampling beach areas or coastal lagoons (Rioja, 1946a, 1946b, 1958,
1959, Mendez-Ubach, Solis-Weiss & Carranza-Edwards, 1986; Salazar-Vallejo et aL 1989;
Hernandez-alcantara & Solis-Weiss, 1991).
The first extensive sampling of the continental shelf of die Mexican Gulf region was initiated by our group in
1987 thanks to die acquisition, a few years earlier, of the R/V "Justo Sierra". Several cruises were undertaken,
especially in the Soudi Western area of the Gulf. As expected, the polychaeie fauna collected was very abundant
and diverse. The best represented polychaetes diere were those of the order Eunicida, bodi in terms of diversity and
abundance (Solis-Weiss et ai , 1991, Granados-Barba & Solis-Weiss, 1994).
Source : MNHN, Paris
EUNICIDA FROM 11 IF SOUTI 1FRN GUI F OF MEXICO
561
The purpose of this paper is to analyze those populations in their structure and distribution, and to determine
the influence of the environmental factors on the distribution of this order of polychaetes.
STUDY AREA
The continental shelf of the Gulf of Mexico from Tampico to Progreso is an extensive area between longitudes
90°23' and 97°45' and latitudes 18°20' to 22°3T. The influence of the discharge from rivers to the sea occurs only
in the northern and central regions. This terrigen zone (YANES-CORREA, 1971) is characterized by mixed or muddy
sediments while to the east, biogenic or carbonated calcareous sands and coral reef rubble are the main components
of the sediment (Fig. 1). The area is shallow (up to about 50-60 m) with several small coralline islands dotting
the outer continental shelf.
The environment is influenced, in the terrigen zone, by the intensive off-shore activity of the oil well drilling
and production where the majority of the oil fields of Mexico are found. This area also supports a rich fishery and
the most productive area for shrimps in Mexico.
The principal current flow comes from the North East (Yucatan peninsula) and follows the shore to the north
with some reversal in die winter (Vidal et al .. 1990) .
MATERIALS AND METHODS
Sampling was done on board the R/V "Justo Sierra" as part of the interdisciplinary institutional projects
"Determinacion del impacto ambiental provocado por las actividades de extraction petrolera en la Sonda de
Campeche a traves de estudios bioldgicos, geoquimicos y sedimentoldgicos (IMCA), and "Din&nica ocednica y su
relackSn con el deterioro ambiental en la porcion sur del Golfo de Mexico" (DINAMO) (Solis-Weiss et al ., 1991).
The area was divided into four zones according to latitude and type of sediment predominantly present (Figs. 1 &
2). Zones 1 (stations 1-13) and 2 (stations 14-20) are characterized by a narrow shelf, mixed sediments and river
discharge, but the two zones are oriented differently and latitudinally apart sufficiently so that die hydrologic
conditions are different. Zone 3 (stations 21-50) presents a widening continental shelf where oil platforms are
present. Zone 4 (stations 51-76) begins at the limit of the terrigen and die carbonated zones. The shelf edge is
close to its maximum extension (245 Km), the influence of river run-off is non existent and die sediments tend to
be coarser and coralline in nature.
Transects were taken along die continental shelf at depths ranging from 15 to 200 m. and covered an
approximate area of 46,000 km2. Seventy six stations were selected for this study (Fig. 1).
The fauna was collected with a 0.1 m2 (10 1) Smith McIntyre grab. Three cruises me considered herein (IMCA
II (September 19-29,1988), IMCA IV (September 25-Oclober 8, 1989) and DINAMO II (October 25-November 8,
1990).
The samples were sieved through a 0.5 mm screen, fixed with formalin (10 %), then sorted and preserved with
alcohol (70 %) following the methodology of Fafchald (1977). A solution of methylene blue was routinely
used for assistance in identification.
Density is defined as the number of individuals per 0. 1 in-.
Frequency is expressed as the percentage of occasions in which the species was present in die stations of eaeli
zone. Species richness is the number of species present per station. Diversity indexes were calculated for the four
zones. The SHANNON- WIENER index was calculated as well as the Evenness index following PlELOli (1977), and
the Simpson index (Odum. 1971). These results are shown in Figure 3.
RESULTS AND DISCUSSION
The Eunicida were represented by 3,135 individuals, grouped into five families, 18 genera and 54 species (Table
1). There were two new records for Mexico : Lumbrineris lieteropoda and L. paradoxa, and about seven new species
which are now under study.
The five families were distributed as follows: the Onuphidae accounted for 17 species and 920 organisms, the
Lumbrineridae 16 species and 1808 organisms, the Eunicidae 14 species and 326 organisms, die Arabellidae 4
species mid 76 organisms and die Dorvillcidae 3 species and 5 organisms.
562
V. SOLIS-WEISS ET ALII
Table J . — Frequency (FREQ.) and Mean Density (DE) values for die species of Eunicida
found in die study area.
The dominant family in terms of abundance was the Lumbrineridae although there were different dominant
species with the latitude (see below).
The distribution of the five families present in the study area is shown in Table 2. The lumbrinerids accounted
for more than 55 % of the organisms in the order in all zones and up to around 70 % in zone 2. The dorvilleids
were poorly represented (3.49 % in zone 2; 0.20 in zone 4. none in zones 1 and 3). The onuphids accounted for
Source : MNHN. Paris
HUNK 'IDA FROM THE SOUTHERN GULF OF MEXICO
563
about 1/4 of the population in each zone, and were best represented in zone 3 (40.94 %). 'The eunicids varied from
2.6 % in zone 3 to 12.45 % in zone 4.
ZONE 1
ZONE 2
SEDIMENTS (%)
DENSITY (OtgyO.1 m)
1 2 3 4 5 6 7 8 9 10 II 12 13
STATION
□ gravel QsAND DmUD DENSITY
SEDIMENTS (%) DENSTTi' (Crg./0. 1 m )
ZDNE3
ZONE A
SEDIMENTS (%) DENSfD' (Org./O. 1 m )
STATION
SEDIMENTS (%)
DENSITY (Org /01m)
30-
80-
70
50-
10
30-
S TATI ON
□ gravel QsAND DmUD *■ DENSITY
CDgravbl Dsand Dmud * density
Fig. 2. — Sediment composition and density of the populations of Eunieea in the study area.
The highest diversity and density occured in zone 4. As seen in Table 2, mean densities were significantly
higher from zone 4 for each family, except for die dorvillcids which are very poorly represented from all zones
(Table 2). Zone 4 is characterized by shallow waters and coarse biogenic sediments (Fig. 2). In the other zones, the
highest densities were also found in shallow waters in mixed or coarse sediments (Fig. 2). Densities decreased with
increasing depdi.
The highest diversity or species richness w'as found in zone 4 (43 species). Around eight species per station
were found, compared to an average of diree species per station at zones 1-3. Diversity values were higher in zones
1 , 2 and
4 (Fig. 3). However, higher variations in those values were noted in zone 1. Again, there was a tendency for lower
values as depdi increased in all zones with less contrast in zone 4 (Fig. 3). Evenness and dominance values varied
more in zones 3 and 4.
The distribution patterns were directly related to die dominance of some species analyzed below.
In zone 1 (Table 2), 10 species w-ere found to be both abundant and frequent: Lumbrineris coccinea, L. ernesti,
L verrilli, S. tenuis , L. latreilli, Ninoe leptognatha, Diopatra tridentata, D. cuprea , Kinbergonuphis orensanzi and
Marphysa bellii. The dominant species were: L. coccinea L ernesti and S. verrilli.
Among die frequent species in zone 2 (Table 2), only one had a density value larger than 1: L. latreilli . and six
were found with values greater than 0.5: L umb ri ne rides dayi, Kinbergonuphis orensanzi, Eunice vittata, S. tenuis ,
Source :
564
V. SOLI S-W HISS UTAH I
L coccinea, L. sp. 2. The dominant species were: L. latreilli, L. tenuis , L coccinea and Lumbrinerides dayi in
zone 2.
Four species in zone 3. which combine high densities with high frequency values can be considered dominant:
S. verrilli. K. orensanzi, Diopatra cuprea and S. tenuis (Table 3).
Species richness was highest in zone 4. where 10 species combined high densities with high Irequencies:
.S', verrilli, S. tenuis. K. orensanzi, E. vittata, N. leptognatlia, K. simoni, D. cuprea, Mooreonuphis sp. 1.
L. latreilli and L. ernesti (Table 3). The dominant species were: S. verrilli. S. tenuis and K. orensanzi.
Table 2. — Mean Densities (ind. 0.1 nr2) of individual families and percentage (%) of the total populations
of Eunicida found in die study area.
As can be seen, die lumbrinerids were dominant but die dominant species varied with the latitude. Henceforth,
in zone 1 it was L. coccinea (15.81 % of the population) and S. ernesti (13 %) followed by S. verrilli (12.7 %).
Together they represented 41.51% of the total population in that zone. In zone 2, L. latreilli was the best
represented (25.79 % of the population) followed by Scoletoma tenuis (8.48 %) and L. coccinea (8.08 %)
representing 47.45 % of the population. In zone 3, S. verrilli (23.62 %) dominated lollowed by S. tenuis
(13.94 %) and K. orensanzi (16.26 %) to total 53.82 %. In zone 4: S. verrilli (30.63 %) .S', tenuis (13.75 %) and
K. orensanzi (10.17 %). to total 54.55 %. The most abundant and widely distributed species for the study area
was ,S. verrilli. however it was not the dominant species in all samples.
Scoletoma verrilli is a species originally described from Florida by PERKINS (1979). It had been previously
reported from very shallow depths (3-1 1 m) in sandy and coarse calcareous sands. It is widely distributed in the
northern Gulf of Mexico at depths from 10 to 189 m from coarse sands to silty clays (IJEBELACKER. & JOHNSON,
1984).
Correlations with the distribution of these organisms with the parameters studied indicated the strongest
relations with the type of sediment and depth. The sediments encountered (Fig. 2) were mixed with a tendency
towards small grain sizes in zone 1. Zone 2 was mostly sandy. Zone 3 was predominantly muddy with some sand
at stations 30, 36. 37, 39, 43. 45 and 49. Zone 4. in contrast, consisted of coarse, sandy sediments, which were
derived from organic matter. Muddy sediments became a smaller fraction towards the East ;uid Nordieast as the
influence of rivers discharge became non existent.
CONCLUSIONS
The Eunicea from the soft bottoms of the continental shelf of the Gulf of Mexico consisted of five families, 1 8
genera and 54 species. The lumbrinerids were the dominant family in terms of abundance whereas lire onuphids
ranked higher in diversity with 17 species compared to 16 for die former. The dominant species varied according to
latitude with Lumbrineris coccinea in zone 1, L. latreilli in zone 2 and .S', verrilli in zones 3 and 4. Scoletoma
verrilli was die most characteristic species in terms of abundance and distribution duoughout die area.
AC KNOW I .EDGEMLNTS
We would like to thank especially DGAPA-UNAM (project DINAMO IN209789) for its financial support at
all stages of this project. Thanks are also due to the members of the Sedimcniology and Marine Chemistry Labs of
Source :
EllNICIDA FROM 'll IF SOUTHERN GUI .F OF MEXICO
565
the ICML-UNAM lor their help in ihe environmental data and lo all participants in the IMCA and DINAMO
oceanographic cruises.
BITS/IND. ZONE 1
DIVERSITY ♦ EVENNESS DOMINANCE
BITS/IND. ZONE 3
STATION
+ DIVERSYTY * DOMINANCE ♦EVENNESS
BITS/IND. ZONE 2
BITS/IND. ZONE 4
STATION
-• diversity ♦evenness dominance
Fig. 3. Diversity, Dominance and Evenness values recorded for the populations of Eunicea in the study area.
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FaUCHALD. K.. 1977. The Polychaete Worms. Definitions and keys to the orders, families and genera. Nat. Hist. Mus.
of Ixis Angeles County. Sci. Ser.. 28 : 1-190.
FaUCHALD. K.. 1992. — A review of the Genus Eunice (Polychaeta: Eunicidae) Based upon Type Material. Smithsonian
Contr. to ZooL. 523 : 422.
GRANADOS-barba A. & SOLIS-WEISS. V., 1994. New records of Polychactous Annelids (Order: Eunicida) from the
Southeastern Gulf of Mexico. Bull. Mar. Sci.. 54 : 420-427.
Hartman, O.. 1951. — The littoral Marine Annelids of the Gulf of Mexico. Pub. Texas Univ. Inst. Mar. Sci.. 2 : 7-124.
Hernandez- Alcantara, P. & Solis-Weiss. V.. 1991. — Ecological aspects of the polychactous populations associated
with the red mangrove Rhizophora mangle at the Laguna de Tenninos, southern part of the Gulf of Mexico. Ophelia
Suppl.. 5 : 451-462.
IbaNez- Aguirre. A. L. & Solis-Weiss, V.. 1986. - Anelidos poliquetos de las praderas de Thalassia testudinum del
noroeste de la Laguna de Terminos. Campeche. Rev. Biol. Trop.. I : 35-47
Mendez-Ubach. M. N.. Solis-Weiss. V. & Carranza-Edwards. A.. 1986. — La importance de la granulomelna en la
distribucion de organismos bentonicos. Estudio de playas del eslado de Veracruz. Mexico. An. Inst. Cienc. del Mary
Limnol.. Univ Nal. Auton. Mexico . 13 : 45-56.
ODUM. E. P.. 1971. Fundamentals of Ecology. 3d. Edition Saunders, Philadelphia. 574 pp
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Perkins, T. I-I. & Savage. T.. 1975. — A bibliography and checklist of polychaetous annelids of Florida, the Gulf of
Mexico, and the Caribbean Region. Florida Mar. Res. Pub.. 14 : 1-62.
PlELOU. E. C.. 1977. Mathematical Ecology. Wiley Interscience, New York. 3S4 pp.
Rioja. E.. 1946a. — Estudios Anelidoldgicos XIV. Observaciones sobre algunos poliquetos de las costas del Gollo de
Mexico. An. Inst. Biol. Univ. Nal. Autdn. Mexico. 17 : 193- 203.
Rioja, E.. 1946b. — Estudios Anelidologicos XV. Nereidos de agua salobre de los esleros del litoral del Golfo de Mexico.
An. Inst. Biol.. Univ. Nal. Anton. Mexico. 17 : 205-214.
Rioja, E., 1958. — Estudios Anelidologicos XXI. Observaciones acerca de algunas especies de serpuidos de los generos
Hydroides y Eupomatus de las costas mexicanas del Golfo de Mexico. An. Inst. Biol. , Univ. Nal. Autdn. Mexico.
28 247-266.
Rioja, E.. 1959. — Estudios Anelidologicos XXII. Datos para el conocimiento de la fauna de anelidos poliquetos de las
costas orientales de Mexico. An. Inst. Biol.. Univ. Nal. Autdn. Mexico, 29 : 219-301.
Rioja, E.. 1961. Estudios Anelidologicos XXIV. Adiciones a la fauna de anelidos poliquetos de las costas orientales de
Mexico. An. Inst. Biol.. Univ. Nal. Autdn. Mexico. 5 1 : 289-316.
RlOJA, E., 1962. — Estudios Anelidologicos XXV. tin nuevo genero de la familia Parculepidae (= Eulcpelhidae). del Golfo
de Mexico. An. Inst. Biol.. Univ. Nal. Autdn. Mexico , 32 : 235-249.
SALAZAR- Vallejo. S. I.. DE LEON GONZALEZ, J. A. & II. SalaICES-PolaNCO, 1989. Poliquetos (Annelida: Polychaeta) de
Mexico : Generalidadcs. Claves ilustradas para familias y gdneros. y Bibliografia-Lisia de especies. Libros Univ.
Auton. Baja Calif. Sur. La Paz, 212 pp.
SaLAZAR-Vallejo. S.. 1992. — Updated checklist of Polychaetes (Polychaeta) from the Gulf of Mexico, the Caribbean
Sea and adjacent areas in the Western Atlantic Ocean. In: Navarro. D. & E. SUAREZ M(eds). Diversidad Bioldgia en la
Reserva de la BiosJ'cra de Sian Ka'an Quintana Roo. Mexico. Vol. II. CIQRO/SEDESOL: 43-76.
SOLIS-WEISS, V. & Carrenio. S.. 1986. — Estudio prospectivo de la macrofauna bentica asociada a las praderas de
Thalassia testudinum en la Laguna de Terminos, Campeche, Mexico. An. Inst. Cienc. del Mar y Linmol., Univ. Nal.
Auton. Mexico. 13: 211-228.
Solis-Weiss,. v.. Hernandez- Alcantara, P. Granados-Barba. a..Lopez-Granados, E.. Miranda-Vazquez, L..
RODRIGUEZ- Villanueva. L. V. & OoHOa-Rivera, V., 1991. Estudio de la macrofauna bentica : las poblaciones de
anelidos poliquetos de la plataforma continental del sur del Golfo de Mexico y su relacion con el deterioro ambiental.
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UEBELACKER. .1. M. & Johnson. P. Cl.. (Eds.), 1984. — Taxonomic Guide to the Polychaetes of the Northern Gulf of
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Vidal, V. M.. Vidal. E. V., & HERNANDEZ, A. F., 1990. Atlas Oceanogrdftco de! Golfo de Mexico. Instituto de
Investigaciones Electricas. Mexico, vol. 2, 707 pp.
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Campeche. Biol. Soc. Geol. Mexicana. 32 : 75-115
Source : MNHN. Paris
61
Ecological analysis of some Syllidae
(Annelida, Polychaeta) from the central
Tyrrhenian Sea (Ponza Island)
A. SOMASCHINI & M. F. GRAVINA
Dipartimento di Biologia Animalc e deirUomo
University “La Sapienza’*
Viale dell'Universita, 32 - 00185 Roma Italy
ABSTRACT
New data are given on the ecology of some syllids from soil bottom and an adjacent Posidonia oceanica seagrass bed
in the Tyrrhenian Sea. Multivariate analysis discriminated five communities distributed along a coenocline based on
granulometry of sediments, from fine to coarse sand, and from low to high shoot density within the Posidonia bed. Along
the coenocline, replacements of some species belonging to the genera Grubeosyllis, Sphaerosyllis. Brania . Exogone ,
and Syllis were observed.
RESUME
Eco logic dc q u el q lies Syllidae (Annelida, Polychaeta) de la partie ccntralc de la mer
Tyrrlienienne (lie de Ponza)
On a etudic 1'ccologic des Syllidiens des fond meubles sableux el d'uue prairie de Posidonia oceanica de file de Ponza
(Italie-Latium). La discrimination de cinq groupemcnts annelidiens en relation avec la structure du substrat (granulometrie
des sediments et densite des faisceaux foliaires) a penrvis de preciser les preferences ecologiques des cspeces les plus
abondantes.
INTRODUCTION
Syllids are one of the most important polychaete families in littoral communities of the Mediterranean Sea.
They are the richest taxon in both abundance and species composition in rocky bottoms and seagrass beds
(Abbiati, 1987; Bellan, 1964; Colognola el al ., 1984; Gambi et al., 1989; Giangrande, 1985; 1988: San
Martin & Vieitez, 1984: San Martin et al. , 1990), whereas in the soft bottoms they are frequently represented
by many interstitial species primarily belonging to the subfamilies Exogoninae and Eusyllinae (COGNETTl, 1962:
SOMASCHINI, A. & M.F. Gravina. 1994. — Ecological Analysis of Some Syllidae (Annelida. Polychaeta) from the
central Tyrrhenian Sea (Ponza Island) In: J.-C. DAUVIN, L. Laubier & D.J. Reish (Eds). Actes de la 4eme Conference
internationale des Polychetes. Mem. Mus. natn. Hist. nat.. 162 : 567-573. Paris ISBN 2-85653-214-4.
Source : MNHN, Paris
568
A. SOMASCHINI & M.r. GRAV1NA
San Martin, 1984a; 1984b; Westheidk, 1974). Historical data on the ecology of this group are available in
many works (e.g. Bellan, 1964; COGNETTI, 1954; 1957; WESTHEIDE, 1974; San Martin. 1984a;
Giangrande, 1989-1990). but recent revisions of several genera and descriptions of many new taxa have changed
(he taxonomic position of many Mediterranean species (e.g. Banse, 1971; Perkins. 1981; San Martin, 1984a;
1984c; 1991). Furthermore, ecological information on Mediterranean syllid species is still largerly incomplete.
This study presents new data based on current knowledge on the distribution and ecology of some species from soft
bottoms and seagrass beds.
MATERIALS AND METHODS
Samples were collected at Ponza Island in die central Tyrrhenian Sea (Italy-Latium) (Fig. 1). The study area.
Gala Fcola, is a broad bay with a bed of Posidonia oceanica ranging in depths from 1 m to 40 m and surrounded by
soft bottom areas ranging in depths from 5 m to 40 m. Patches of dead mats (dead rhyzomes without leaf stratum)
are distributed within the Posidonia bed. The inner part of the bay is a sheltered area of shallow water (1-2 m
depth).
Fig. 1. The study area. SB marks the soft-bottom sampling stations; HP those of the live Posidonia mat, and M the
dead mat stations in the Posidonia bed. Numerals following letter abbreviations refer to station depths in meters.
Source :
ECOLOGICAI . ANALYSIS OF SYU JDS FROM THE TYRRHENIAN SEA
569
Samples were collected in June 1988 in depths from 1 m to 30 m. Five samples were collected from a live
Posidonia mat (HP); three samples were collected^ from the dead rhyzome mat (M); and four samples were collected
from neighbouring soft bottom areas (SB) (Table 1). The shoot Posidonia density in a square meter was computed
on live mat before collecting samples. The fauna of the Posidonia bed was collected by means of a hand net
measuring 20 x 20 x 15 cm. In the live mat, fauna was collected after removing the blades of grass, whereas the
dead mat fauna was collected directly. Fauna in soft bottom areas was collected with a Charcot dredge (volume: 50
I). Corers of sediment were collected in the soft bottom areas for grain si/.c analysis (Somaschini, 1992;
SOMASCIIINl el al. , in press).
Table 1. — Biotope features: granulometric composition of soft bottom stations (SB); shoot density values of
Posidonia bed and exposure to water movement (HP indicates stations
of live matte M indicates stations of dead mat).
Frequency data of the total polychaete fauna at each station were computed and logarithmically transformated.
Principal Component Analysis (PC A) was employed on the correlation matrix to order the sampling stations
(Somaschini et al., in press). In the obtained ordination model, Euclidean distances were computed between the
sampling station points, to order them along the principal coenocline. This coenocline was used in order to study
the distribution patterns of the most abundant syllids. Only syllids with a frequency higher than 1 % of the total
polychaete fauna were analyzed. The distribution patterns along the coenocline of the selected species were studied
computing the weighted mean of three successive sets of data (Curtis & McIntosh, 1951; Gaijch, 1982).
Additional details on the mathematical methods used in this study can be found in Somaschini (1992).
RESULTS AND CONCLUSIONS
A total of 15,232 individuals belonging to 218 species of polychaetes was found (Somaschini, 1992). Syllidae
were the richest family in both abundance and species richness (7,381 individuals and 76 species). Three new
species of Syllids were described and a new report for the Mediterranean Sea was carried out (Somaschini, 1992).
Exogoninae and Syllinae were very abundant and diverse in the Posidonia bed, whereas from the soft bottom only
Eusyllihae and Exogoninae were collected.
Multivariate analysis on the total fauna discriminated five communities related to sediment type, Posidonia
shoot density, and the exposure to water movement (Somaschini et al., in press). Communities of fine sand (5 +
20 + 30 in) and of coarse sand (10 m) were identified in the soft bottom areas. A community was found in die
deeper Posidonia samples with a low shoot density (20 + 30 m), whereas two communities were found in the
Source :
570
A. SOMASCHINI & M.F. GRAVINA
Exogone naid/na
Grubeosyllis vieitezi
%
Parapionosyllis labronica
Sphaerosyllis piriferopsis
Sphaerosyllis pirifera
Exogone parahomoseta
Grubeosyllis limbata
Parapionosyllis brevicirra
Sphaerosyllis brevicirra
Brania pusilla
Exogone rostrata
%
Grubeosyllis clavata
%
i *
14
1.2
1
0.8
0.8
0.4
0.2
| C8 P8 | BM | EM |
Sphaerosyllis g/andulata
1.6
14
1 2
1
0A
0.8
04
02
Sphaerosyllis xarifae
Brania oculata
i%
QA
0.8
04
02
*1=8 C8 P8 _ | 8M | EM_ _ |
FIG. 2. Percent distribution of the most abundant syllid species (frequency on total polychaete fauna >1%) along the
ecological gradient observed. On the horizontal axis: FS = Fine sand (SB20; SB30; SB5); CS = coarse sand (SB 10); PS
= deep Posidonia bed (HP20; I-IP30; M20); SM = sheltered shallow Posidonio mat (IPS; 1M); FM = exposed Posidonia
mat (5PS; 5M; 10PS).
Source : MNHN, Paris
ECO! XXjICAI . AN Al .YSIS OF SYLUDS FROM 11 IF TYRRHENIAN SEA
571
Pionosyllis lamelligera
Elhersia ferrug'na
Haplosyllis spongicoia
Syllis lutea
Syllis variegata
Xenosyllis scabra
%
Fig. 2 (continued). — Percent distribution of the most abundant syllid species (frequency on total polychactc fauna > 1%)
along the ecological gradient observed. On the horizontal axis: FS = fine sand (SB20: SB30; SB5); CS = coarse sand
(SB10); PS = deep Posidonia bed (IIP20; HP30; M20); SM = sheltered shallow Posidonia mat (IPS: 1M); EM =
exposed Posidonia mat (5PS: 5M; 10PS).
shallow Posidonia bed with high shoot density (1 + 5 + 10 in depth), respectively on sheltered (1 m) and exposed
(5 + 10 in depth) habitats.
Source
572
A. SOMASCHINI & M.F. GRAVINA
Euclidean distances ordered the sampling stations along a coenocline from fine to coarse sand, and within the
Posidonia bed from low to higher shoot densities and water movement exposure (SB20; SB30: SB5; SB 10: HP20;
HP30; M20; IPS; 1M; 5PS: 5M; 10PS). Distributions of the most abundant syllids (frequency > 1%) along die
ecological gradients are shown in figure 2. Detailed results of die study can be found in Somaschini (1992).
The fine sand was inhabited by a few dominant species, such as Exogone naidina Orsted and ParapionosyUis
labronica Cognetti. Apparendy, die presence of many interstices in the coarse sand made the sediment more similar
to the mat samples and suitable for many syllids (e.g. Sphaerosyllis glandulata Perkins, Sphaerosyltis tciylori
Perkins, Syllides convolutus Webster & Benedict, and StreplosyUis websteri Southern as dominant species).
In the shallower stations (1 + 5 m depth) of the Posidonia bed, the polychaete community changed according to
the exposure to water movement (Somaschini, 1992). The sheltered stations (1 m depth) of die Posidonia bed
were inhabited by many species known to be associated with the sediment deposition, such as Syllis garciai
Campoy, Syllis prolifera Krolin, Sphaerosyllis pirifera Claparfcde, and Elhersia ferrugina Langerhans. The same
species were also present in the deepest stations (20 + 30 m) among the more sparse Posidonia rhizomes. Other
syllid species, such as Pionosyllis lamelligera Saint- Joseph, Sphaerosyllis xarifae Hartmann-SchrOdcr, Exogone
rostrata Naville and Brania pitsilla Dujardin occurred more abundantly at the shallower stations of die Posidonia bed
which, however, were more exposed to water movement (5 + 10 m depth). Pionosyllis lamelligera and Brania
pusilla are commonly reported for shallow rocky bottoms, whereas E. rostrata is reported for sciaphilic algal
communities (Abbiati el al., 1987; Nunez et aL 1992).
In die literature many syllid species are reported to have broad distributions on rocky as well as in soft, littoral
substrata (Bellan, 1964; Bellan-Santini, 1969). The current data give more detailed information about the
autoecology of some of these species in that a replacement of some congeneric species along the coenocline was
observed (Fig. 2). Among the Exogoninae, Grubeosyllis vieitezi San Martin, Grubeosyllis limbata Claparede and
Grubeosyllis clavata Claparede substituted for each other in relation to die different conditions within the Posidonia
bed. G. vieitezi was more abundant in the deep Posidonia samples, whereas G. limbata and G. clavata were more
abundant in shallow waters with high shoot density, in sheltered and exposed conditions respectively. In the genus
Brania . B. pusilla occurred more abundantly in the deepest stations of the Posidonia bed as well as at the more
exposed ones, whereas B. oculata Hartmann-Schroder was quite abundant in the sheltered Posidonia habitat. In the
genus Syllis. S. prolifera and Syllis westheidei San Martin were more abundant in the shallowest sheltered area; S.
garciai occurred more abundantly in the deeper Posidonia bed with low shoot density, whereas Syllis variegata
Grube and Syllis columbretensis Campoy were more abundant in the more exposed Posidonia environment. In the
shallowest sheltered area, Sphaerosyllis pirifera substituted for Sphaerosyllis xarifae. Sphaerosyllis brevicirra
Hartmann-Schroder and Sphaerosyllis piriferopsis Perkins which, however, were common at the other stations of
the Posidonia bed. Only Sphaerosyllis glandulata was a characteristic species of the coarse sand stations. Finally,
in fine sand, Exogone parahomoseta Hartmann-Schroder and Exogone naidina replaced Exogone rostrata , typically
recorded in Posidonia beds.
REFERENCES
Abbiati. M.. 1987. Policheti di fondo roccioso del promontorio di Romito (Livorno). Aui Soc. 7'osc. Sci. Nat. Mem.
Serie B. 94 : 215-233.
Abbiati. M.. BiaNCHI, C. N. & Castelli, A. 1987. - Polychaete Vertical Zonation along a Littoral Cliff in the Western
Mediterranean. P.S.Z.N.I. Marine Ecology. 8: 33-48.
BANSE, K„ 1971. A new species and addition to the description of six other species of Syllides Orsted (Syllidae:
Polychacta). ./. Fish. Res. Board. Canada. 28 : 1469-1481.
Bellan, G.. 1964. — Contribution a I'etudc systematique bionomique et ecologique des Annelides Polychetes de la
Mediterranee. Rec. Trav. St. mar. Ehdoume. 49 (33) : 1-372.
BELLAN SANTINI, D., 1969. Contribution a l'clude des peuplements infralittoraux sur substrat rocheux (elude qualitative
et quantitative de la frange superieure). Rec. Trav. St. mar. Endoume, 47 (63) : 1-294.
COGNETTI, G.. 1954. Ricerche sui Sillidi del Golfo di Napoli. Pubi Staz. Zool. Napoli. 26 : 1-11.
Cognetti. G.. 1957. I Sillidi del Golfo di Napoli. Pubi Staz. Zool. Napoli. 30 : 1-100.
COGNETTI. G.. 1962. I Policheti dei fondi a sabbia grossolana del litorale livornese. Boll. Zool.. 29 : 1-7.
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ECOLOGICAL ANALYSIS OF SY1 A JDS FROM THE TYRRI IENIAN SLA
573
COLOGNOLA, R.. CHESSA, C . A.. FRESI, E.. Russo, G.P.. PETRIN1. L.. 1984. — Zoobenthos clella rada di Palau (Sardegna) : I
Syllidae (Polychaeta). Nova Thalassia . 6 (suppl.) : 569-574.
Curtis. J. T.& MclNTOSII. R. P., 1951. — An upland forest continuum in the prairie-forest border region of Wisconsin.
Ecology, 32 : 476-496.
C.AMBL M.C., GIANGRANDE. A.. CHESSA. L. A.. MaNCONI, R.. Scardi. M.. 1989. — Distribution and ecology of
Polychaetes in the foliar stratum of a P . oceanica bed in the bay of Porto Conte. In : C.F. BOUDOURESQUH. A. MEINESZ,
E. FRESI & V. GRAVEZ (eds.), International Workshop Posidonia oceanica Beds. G1S Posidonie publ., Fr.. 2 : 175-188.
Gaucil II. G., Jr. 1982. Multivariate analysis in community ecology . Cambridge studies in ecology. Cambridge
University Press : 298 pp.
GIANGRANDE. A.. 1985. — Policheli dei rizomi di P. oceanica L. Delilc di una prateria dcll'isola di Ischia (Napoli). Atti
Soc. Tosc. Sci. Nat. Mem. ser.B. 92 : 195-206.
GIANGRANDE. A.. 1988. Polychaete zonation and its relation to algal distribution down a vertical cliff in the western
Medileranean (Italy) : a structural analysis. J. exp. mar. Biol. Ecoi. 120 : 263-276.
GIANGRANDE. A.. 1989/90. Distribution and reproduction of syllids (Annelida. Polychaeta) along a vertical cliff (West
Mediterranean). Oehalia. 16. N.S.: 69-85.
NUNEZ, J.. San Martin, G. & Del Carmen Brito M.. 1992. — Exogoninae (Polychaeta: Syllidae) from Canary Islands.
Sci. Mar.. 56 : 43-52.
PERKINS, T.H.. 1981. Syllidae (Polychaeta), principally from Florida, with description of a new genus and twenty-one
new species. Proc. Biol. Soc. Wash.. 93 : 1080-1172.
San Martin. G.. 1984a. — Estudio biogeografico, faunistico y sistematico de los Poliquetos de la Jamilia Silidos
(Syllidae : Polychaeta ) en Baleares. Doctoral Thcsys. F.diciones de la Universidad Complutcnse de Madrid. n° 187 • 1-
529.
San Martin. G.. 1984b. Biogeography of the Syllidae (Polychaeta) from the Spanish Mediterranean Coasts. In: P. A.
HUTCHINGS (ed.). Proceedings of the First International Polychaete Conference Linnean Society of New South Wales
303-322.
San Martin. G., 1984c. Descripcion de una nueva especie y revision del genero Sphaerosyllis. Cah. Biol. Mar.. 25 :
375-392.
San Martin. G.. 1991. — Grubeosyllis and Exogone (Exogoninae, Syllidae, Polychaeta) from Cuba, the Gulf of Mexico,
Florida and Puerto Rico, with a revision of Exogone. Bull. Mar. Sci.. 49 : 715-740.
SAN Martin G. & VlEITEZ J.M., 1984. Anelidos poliquetos de los rizomas de Posidonia oceanica en las costas del Cabo
de Palos (Murcia. Espana). In : C.F. BOUDOURESQUE, A. JEUDY DE GRISSAC & J. Olivier (eds.). International workshop
on Posidonia oceanica beds. GIS Posidonie publ.: 149-157.
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Poliquetos de rizomas de Posidonia oceanica en la costas de Almeria. Bol. Inst. Esp. Oceanogr.. 6 : 41-58.
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(rhizome and matt strata) and neighbouring soft and hard bottoms. P.S.Z.N.I. Marine Ecology.
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Source : MNHN. Paris
62
Cyclical changes in the fauna associated with tube
aggregates of Ficopomatus enigmaticus (Fauvel)
Nigel S. THOMAS * Clifford H. THORP **
* Southern Science Ltd., Hampshire Laboratory
Otterbourne, Hants. S021 2SW. U.K.
** University of Portsmouth. School of Biological Sciences, Marine Laboratory
Ferry Rd., Hayling Island, Hants, POl 1 ODG, U.K.
ABSTRACT
Studies were undertaken on the fauna associated with the tube aggregations of Ficopomatus enigmaticus in a brackish
water lagoon, in southern England, from 1982-1992. During this time a population crash and partial recovery was observed.
Aggregates, consisting of living animals, were occupied in abundance by the amphipods Leptocheirus pilosus. Corophium
insidiosum and Melita palmala. with numbers declining in dead colonies. Initially moribund aggregates were invaded in large
numbers by the isopod Lekanesphaera hookeri. At the same time the polychaete Hediste (Nereis) diversicolor showed an
increase in numbers. Leptocheirus pilosus returned in abundance by 1989. The fluctuations in associated species were related
to the ability of F. enigmaticus to prevent deposition and accumulation of sediment and organic material. Parallel sampling of
the adjoining muddy sediments revealed catastrophic disappearance and re-appearance of species, similar to that shown by F.
enigmaticus. These included the rare lagoonal polychaete. Alkmaria romijni. Both living and dead aggregates of F. enigmaticus
provide an extensive benthic sub habitat. The living aggregates may also regulate invertebrate food resources. The ecology of
the benthos was controlled by the interaction of this factor with variables such as saline intrusion.
RESUME
Changements cycliques de la faune associee aux agregats de tubes de Ficopomatus enigmaticus (Fauvel)
Des etudes ont etc entreprises sur la faune associee aux agregats de tubes de Ficopomatus enigmaticus dans une lagune d'eau
saumatre au sud de l'Angleterre de 1982 a 1992. Au cours de cette periode, on a observe la disparition puis la reconstitution
partielle de la population de F. enigmaticus. Les agregats constitues par des animaux vivants etaient colonises en abondance
par les amphipodes Leptocheirus pilosus, Corophium insidiosum et Melita palmala, dont le nombre decroissait dans les
agregats morts. Les agregats de moribonds ont etc initialement, envahis. en grand nombre. par l'isopode Lekanesphaera
hookeri. Simultanement, les polychetes Hediste (Nereis) diversicolor ont montre une ties forte augmentation nuinerique.
leptocheirus pilosus a retrouvc une grande abondance en 1989. Les fluctuations des especes associees sont liees a la capacitc
de F. enigmaticus d'empecher le depot el (accumulation de sediments et de matiere organique. Des echantillons. preleves
simultanement sur les sediments vaseux voisins, ont revele une disparition catasUophique puis une reapparition d'une faune
similaire a celle deja rencontree dans les agregats de F. enigmaticus. L'espece lagunaire. Alkmaria romijni, espece rare, a ete
recoltee dans ces echantillons. Les deux types d’agregals vivants et morts de F. enigmaticus fournissenl un large sous habitat
I'HOMAS, N.S. & C.II. THORP. 1994. — Cyclical changes in the fauna associated with tubes aggregates of Ficopomatus
enigmaticus (Fauvel) In: J.-C. Dauvin. L. LaUBIGR & D.J. RlilSH (Eds), Actes de la 4eme Conference internationale des
Polychetes. Mem. Mas. natn. Hist. nat.. 162 : 575-584. Paris ISBN 2-564783-165-2.
Source : MNHN , Paris
576
N.S. THOMAS &C.H. THORP
benthique. Les agnSgats vivants peuvent reguler les rcssources en nourriture des invcrt<$bres. L'ecologie du benthos etait
contiolce par l’interaction de ce facteur avec des variables telles que les intrusions salines.
INTRODUCTION
Fal’vhl (1933), in describing the distribution of the serpulid (Mercierella) Ficopomatus enigmaticus,
frequently mentioned the varied fauna associated with the aggregated tubes. Observations by FlSCH F. r-PIETTE
(1925 1928). Bertrand (1938), Ruluer (1943), EUZET & Pujol (1963) and VUILLEMIN (1965) showed that this
associated fauna was similar in species composition. The sessile species were generally limited to a few species ot
bryo/.oa, Bakin us and ascidians. In contrast the mobile fauna were quite diverse, consisting mainly ol amplupods,
isopods and polychaetes. There was a high degree of uniformity in the family groups observed, although the
species frequently vary. Principal amongst these were species of Corophium , Gammarus and Lekanesphaera
(Sphaeroma ). The am phi pod Leptocheirus pilosus Zaddach, 1844 appeared to be almost universally found. Spatial
and temporal variation in species composition has been observed by Ruluer (1943) and Euzei & Pujol (1963),
and related to fluctuations in local conditions and die health of the aggregates.
The populations of F.enlgmaiicus in the brackish water of the Fmsworth, Slipper and Peter, millpond complex
(Fig. 1) have been investigated since 1982 by Thorp (1987, 1994). These studies have revealed considerable
population variations, with a "crash" occurring in 1986. consisting of Ihe apparent death of the adult population
and a massive reduction in larval settlement. This event was followed in 1989-91 by a recovery in larval
settlement, with some aggregates demonstrating regeneration and others appearing as new aggregates on die mud
surface The population decline was attributed to the age of die adult population, lack of overwintering reserves
and a failure of recruiuncnt (THORP. 1992). The last two are regulated by phytoplankton levels during summer,
which in turn are controlled by sunlight, temperature and salinity. Recruitment success was also thought to depend
on availability of suitable substrata for settlement.
The millpond complex in Emsworth (Fig. 1) has a combined area ol 2.7 hectares and, apart trom a deeper
water entrance and channel, a maximum depth of less than 1 .5 m (THORP, 1987). Seawater enters on high spring
tides from Chichester Harbour, through tide gates at the southern end. Fresh water enters from die River Fins in
die north. Winter and spring bottom salinities vary from 0 to .30 and summer to autumn salinities are normally
from 10 to 34. The substratum is composed of silty muds (median diameter 0.022 mm to 0.047 mm) and high
levels of organic material (9 % to 16 %) (unpublished data), although stones and odier hard substrata, such as
broken bottles, are scattered over die surface. These hard objects are the surfaces upon which die aggregations of
F. enigmaticus occur.
Concurrent with the study by THORP (1994) on fluctuations in the population of F. enigmaticus , the
opportunity was taken to determine how the associated fauna varies with die healdi ol the aggregates. I he present
paper describes and attempts to explain some of the changes observed, and relates these to die benthic faunal
communities of the millpond complex.
MATERIALS AND METHODS
Samples of sediment and aggregates of F. enigmaticus were collected in die autumns of 1982. 1987. 1989 and
1991. On each occasion at least five small aggregates of F. enigmaticus were collected, with volumes between
0.5 and 1.5 litres. At the same time two cores (9 cm diameter x 15 cm deep) of mud were collected from each of
five sites (Fig. 1). Additional cores were collected, in the latter three years, for the analysis of sediment particle
size and organic material content. All the samples were taken to the laboratory where the aggregates were frozen
and die sediment samples sieved through a 0.5 mm mesh.
Each frozen aggregate was measured by placing it into a plastic bag and then plunging it into a Eureka can to
determine the volume. The plastic bag was then removed and the volume measured again. A final volume was
taken once till die sediment had been washed from die aggregate. It was possible dien to calculate die interstitial
space and die percentage of that space occupied by sediment. The sediment removed from die aggregates was also
washed through a 0.5 mm sieve and all animals sorted, preserved and identified to species where possible.
Particle size analysis was undertaken using an initial wet sieving technique followed by dry sieving of die
> 0.063 mm fraction and wet suspension of the < 0.063 mm fraction; organic content was estimated by loss on
ignition (Holme & McIntyre, 1971).
Source :
FAUNA WITH AGGREGATES OF F. ENIGMATIC JS
577
RESULTS
The full species list for both aggregates and adjacent sediment is given in Table 1, showing liic composition
and abundance of die species, in both the aggregates and die sediment, over die four sampling periods. The
changes in the species numbers arc demonstrated in Figure 2. There is an apparent inverse relationship between
the number of species in the aggregates and in the sediments. The number of species was greatest in thcaggregates
in the period 1987 to 1989. This period corresponds to die lowest species numbers in the sediment. The reverse
was true in 1982 mid 1991, aldiough species numbers in the 1991 aggregates were relatively high.
The state of health of the aggregates can be seen to be related to die number of species and abundance of
individuals (Fig. 3). Although lower species numbers occurred in the live aggregates, they supported a greater
number of individuals. The physical condition of die aggregates can be related, to some extent, to die quantity of
sediment they contain. Figure 3 demonstrates that greater quantities of sediment occupied the dead and
regenerating aggregates widi levels as high as 40% in the latter.
ElG. 1. — Sampling sites in the Emsworth millpond complex, with its location indicated in the Solent Harbours system, on the
south coast of England.
578
N.S. THOMAS & C.H. THORP
Table 1 . — List of fauna associated with live, dead and regenerating Ficopomam aggregates (Agg) and in die
mud of the Emsworth millpond complex. *: low abundance, **: medium abundance, ***: high abundance.
The principal species found in the aggregates show clear differences in abundance between aggregate types
(Fig. 4). The live aggregates were co-dominated by the amphipods Leptocheirus pilosus , Corophium insidiosum
Source : MNHN. Paris
FAUNA WITH AGGREGATES OF F. ENIGMATICUS
579
Years
Total no. species in aggregates Mean no. species in aggregates
— *- Total no. of species in sediment Mean no. species in sediment
FIG. 2. — Mean and total number of species in the aggregates and in the sediment. 1982 9 1 . (mean number of species ± s.e.).
Crawford. 1937 and Melitci palmata (Montagu, 1804). The former species dominated in all aggregate types,
whereas C. insidiosum occurred only in live aggregates. Several other species, but most noticably Lekanespliaera
hookeri (Leach, 1814), Cyatlntra carinata (Kroyer, 1847) and Hediste diversicolor (O.F. Muller, 1776) were
found in the greatest numbers in dead or regenerating aggregates, although all were found in the live aggregates
on at least one occasion. L. hookeri and H. diversicolor in particular dominated the dead aggregates during 1987.
By further examining the changes in abundance that have occurred over the 10 year period and comparing
these with Figure 4, it is possible to determine whether the state of health of the aggregates is the most important
influencing factor. Figure 5 confirms that L. pilosus and probably M. palmata have responded to factors in
addition to die collapse in the health of the aggregates, with low values occurring in 1987 followed by high values
in 1989, both periods when dead aggregates were prevalent. C. insidiosum in contrast disappeared by 1987 and
failed to re-appear, indicating that it may have been specific to live aggregates.
Of die secondary dominants, the three species L. hookeri , C. carinata and H. diversicolor all showed increases
in abundance after the disappearance of the live aggregates (Fig. 6). This has been most pronounced for L. hookeri
which was the dominant aggregate species in 1987. The changes in C. carinata and H. diversicolor have been less
dramatic but were greatest in die period 1982 to 1987. Both of these species have stayed at relatively uniform
levels in the adjacent mud (Fig. 7) suggesting that the death of die aggregates could be die most important factor
influencing the changes observed.
The stability of H. diversicolor and C. carinata in the mud contrasts with several other species that were
abundant in die sediments (Fig. 8). The polychaete species Streblospio shrubsoli (Buchanan, 1890) and Alkmaria
romijni Horst, 1919 have undergone considerable variations. An equally large change has also been shown by the
anthozoan Nematostella vectensis Stephenson, 1935 which disappeared by 1987 and was not found subsequently.
Data on die sediment particle size and organic material levels have not been complete over the 10 year period
but there has been no evidence of long term changes in either. Percentage sediment less than 0.063 mm in
diameter has been recorded as between 60 to 80 % and organic material at an almost uniform 13 %.
580
N.S. THOMAS & C.II. THORP
FlG. 3. — Species number, abundance and percentage interstitial sediment in live, dead and regenerating aggregates, (species
numbers are means ± s.e., abundances are mean numbers per cm3 ± s.e. and percentage is mean ± s.e.).
Live
Leptocheirus pilosus
Lekanesphaera hooker i
Dead
Melita palmata
Cyathura carinata
Regenerating
Corophium insidiosum
Nereis diversicolor
FIG. 4. — Abundance of dominant species in different aggregate types, (mean number of individuals per line).
Source : MNHN. Paris
FAUNA WITH AGGREGATES OF F. ENIGMA 7 ICUS
581
-m- Melita palmaia Leptocheims pilosus
—a— Corophium insidiosum
Fig. 5. Changes in the abundance of dominants in aggregates. (logiQ. mean number of individuals per litre ± s.c.).
Lekanesphaera hookeri Cyathura carinaia
Nereis diversicolor
Fig. 6. — Changes in abundance of secondary dominants in aggregates. (log10. mean number of individuals per litre ± s.e.).
DISCUSSION
Two of the most commonly occurring species in the live aggregates of F. enigmaticus ; L. pilosus and C.
insidiosum, are tubicolous amphipods (Lincoln. 1979) which exploit particulate material suspended in moving
water, such as that found in the millponds complex. They are unable to tolerate the high silt mid clay levels in the
sediments, which are more suited to the burrowing polychaetes and crustaceans. Both species were found by
Goodhart (1939), living in a brackish water sluice pond, similar to the millpond. There L pilosus constructed its
tubes on the thallus of Chondrus crispus thus remaining in moving water above die soft sediment floor. C.
insidiosum has also been found by S header (1978) in high turbidity waters associated with mats of Rliodochorton
Source
582
N.S. THOMAS & C.I I. THORP
sp. M. palmata differs in thal ii is normally found amongst stones and gravel in silty environments (Lincoln,
1979) and is probably occupying the sill filled areas at the base of the aggregations.
Cyathura carinaia
Nereis diversicolor
Lekanesphaera hookeri
FIG. 7. Changes in the abundance of dominants in sediments. (logiQ, mean number of individuals.m2 ± s.e.).
-*- Nemaiostella vectensis Alkmaria romijni
Streblospio shrubsoli
Fig. 8. — Changes in abundance of secondary species in sediments, (logio. mean number of individuals m2 ± s.e.).
The death of the aggregates of F. enigmaticus in 1987 may have contributed lo several of the changes
observed in the associated fauna. Most important amongst ihcsc was the demise of C. insidiosum. The other two
abundant species, although they almost disappeared in 1987, were able to return to dominance in 1989.
The burrowing and mobile scavenging fauna which developed in 1987 evidently responded to the increased
area available for occupation, created by the greater quantitiesof particulate material within the aggregates. Similar
Source : MNHN. Paris
FAUNA WITH AGGREGATES OF F. ENIGMATIC US
583
changes were observed by RULLIER (1943), who found that H. diversicolor was present in abundance in recently
dead aggregates. The accumulation of sediment may also have prevented some of the live aggregate species from
occurring, such as C. insidiosum , although the quantity of sediment was never sufficient to eliminate all of the
mobile amphipods. These species are still able to exploit the remaining space and utilise the high levels of
suspended particulate material found in the water. As a consequence the dead aggregates are able to support a
wider range of species than the live aggregates. Likewise the regenerating aggregates contain greater levels of
sediment, principally in a central degenerated area, surrounded by an atoll of regenerating individuals. As a result
the regenerating aggregates retain an equally diverse fauna.
The lack of sediment makes live aggregates unsuitable for burrowing species, but an additional factor reducing
die diversity of the associated fauna could be competitive exclusion. KNIGHT-JONES & MOYSE (1961) have
indicated that the growth form of Filograna aggregations optimises food utilisation, and Ficopomaius has
somewhat similar spacing of individuals within die aggregates. The limited species numbers but large numbers of
individuals found in live aggregates indicate dial L. pilosus , M. palmata and C. insidiosum may have specific
feeding requirements that do not conflict with that of F. enigmaticus. Between diese species full exploitation of the
available food resources may well occur, thus excluding other species. While conditions are stable die aniphipod
populations are likely to remain in balance with F.enigmaticus, maintaining themselves by larval brooding and
direct settlement (LINCOLN, 1979).
The filler-feeding activity of F. enigmaticus is also likely to have an effect on the total energetics of the
millpond. Davies et at. (1989) in a study of die Marina de Gama, near Cape Town, calculated that F. enigmaticus
had die potential to reduce the particulate load of the water within die lagoon by 50 % each day. This ability to
change die water quality has die potential to affect die fauna profoundly, widiin both the aggregates and the
adjacent mudflats. The disappearance of live F. enigmaticus aggregates in 1987 corresponded with changes in die
mud flat fauna, particularly a reduction in diversity. The remaining species, such as H. diversicolor and L. hookeri ,
mostly exhibited non-specialised feeding habits. These species were probably able to exploit die increased levels
of suspended food that were not previously available to the sediment fauna. A further feature, related to die loss of
the aggregates, was the substantial reduction in die numbers of F. enigmaticus larvae (Thorp, 1994) which may
have formed an important food source for some of the species with more specialised feeding habits. A good
example of this is the polychaete Eteone longa (Fabricius, 1780), which Fauchald & Jumars (1979) have
indicated feeds specifically on other annelid larvae. With the reappearance of the live aggregates, and hence
reduction in suspended food and an increase in larval numbers, it could be expected that the bcndiic species
numbers in the sediment would increase. To some extent this situation has occurred, species numbers falling in die
aggregates and increasing substantially in the sediment.
Considerable variation in the benthic fauna is evident, however, which cannot be explained wholly by the
death of F. enigmaticus. Clearly other factors operate in the millpond which affect die benthic fauna and may have
contributed to the demise of F. enigmaticus. Of principal importance amongst these is the intrusion of high
salinity water. In 1982 the benthic fauna was composed of a range of species, that included several marine species,
commonly occurring in Chichester Harbour; for example, E. longa. Tliaryx marioni (de Saint-Joseph, 1894),
Manayunkia aestuarina (Bourne, 1883) and Cerastoderma edule (L., 1758) (Thomas, 1987). The disappearance
of this group in 1987 and the appearance of several low salinity species, for example Gammarus zaddachi Sexton,
1912 mid Gammarus salinus Spooner. 1947 suggests that a period of iow salinity may have eliminated most of the
marine species. THORP (1987) has indicated that protracted periods of low salinity occurred during the winter and
spring of 1983-1987. The species most successful during this period were the typically euryhaline species,
H. diversicolor and Cyathura carinata. The appearance of marine species in 1989 Ascidietla aspersa (O.F. Miiller,
1771) and Ciona intest inalis (L., 1767) was localised in the vicinity of die tide gates where maximum salinities
occur. This was followed in 1991 by the re-appearance of several species which clearly entered from Chichester
Harbour; specifically Ostrea edulis L., 1758, Eteone longa Jassa falcata (Montagu, 1880) and Hydrobia ulvae
(Pennant, 1777). All of these species occurred in die year which followed a winter of almost constant high
salinities, widi zero salinity recorded only 15 % of die time.
These fluctuations in salinity, in combination with die biological effects due to die changes in health of die
aggregates, have created a dynamic and unstable environment in the millpond. This is demonstrated by
fluctuations in abundance of several of die benthic species, particularly N. vectensis and A. romijni , both of which
are protected species in the U.K. These species, in keeping with many others Uiat occupy extreme environments,
can exploit to die maximum suitable conditions when they occur. Extreme conditions have also been cited by TEN
HOVE (1979) as a factor in the development of mass occurrences of serpulids. These may be followed by dramatic
declines, with, in the case of die serpulids. only the dead tubes to provide evidence of previous existence.
584
N.S. THOMAS & C.I-I. THORP
ACKNOWLEDGMENTS
We would like to express our thanks to the following students; Clare Wimble, Carolyn Atkins, John
Hopkins. Peter Nicholls- and Ewen Wilson, for their valuable assistance with the collection of the faunal data.
We would also like to express our gratitude to the trustees and members of the Slipper Millpond Preservation
Society and Mrs Elizabeth Kinloch for allowing the studies to take place. Particular thanks arc also due to Mr.
Bruce HAILSTONE for his unstinting assistance in the field.
REFERENCES
Bertrand. 1938. — Sur quelques Crustaces Malacostraces de la region Dinardaise. Bull. Lab. Ditiard, 20 : 26 3 1 .
Davies. B.R., Stuart. V. Sc VillieRS, de V., 1989. — The filtration activity of a serpulid polychaete population (Ficopomatus
enigmaticus) (Fauvel) and its effects on water quality in a coastal marina. Est. Coastal Shelf Sci., 29 : 613-620
Euzet, L. Sc PUJOL, M., 1963. La faune associee a Mercierella enigmatica Fauvel (Annelida Serpulidae) dans quelques
stations des environs de Sete. Rapp. P.v. Comm, intern. Explor. scient. Mediterr., 17 : 833-842.
Fauvel. P.. 1933. — Histoire de la Mercierella enigmatica Fauvel Scrpulien d’eau saumatre. Arch. Zool. exp. gen.. 75 : 185
193.
FAUCHALD. K. Sc JUMARS, P.A.. 1979. — The diet of worms: A study of polychaete feeding guilds. Ocecinogr. mar. Biol. Ann.
Rev.. 17 : 193-284.
FISCHER Piette, F... 1925. Sur la faune de la Ranee et la presence de Mercierella enigmatica Fauvel. Bull. Soc. Zool.
France. 50 : 347-350.
Fischer— Piette. E.. 1928. Recherches de bionomie et d'oeeanographie littorale sur la Ranee et Ic littoral de la Manche.
Ann. Inst. Oceanogr.. 5 : 310-31 1.
CjOODHart. C.B.. 1939. Notes on the bionomics of the tube dwelling amphipod Leptocheirus pilosus (Zaddach). J. mar.
bioL Ass. U.K.. 23 .311 325. —
Holme, N.A. & Me. INTYRE, A.D.. 1971. — Methods for the study of the marine benthos. Blackwell Scientific Publications.
Oxford, 331 pp.
Hove. H.A.ten.. 1979. Different causes of mass occurrence in serpulids. In: G. Larwood Sc B.R. Rosen (eds), Systematics
Association Special 1 1. Biology and Systematics of Colonial Organisms. Academic Press, London and New York : 281
298.
Knight '-Jones, E.W. & MOYSE, J.. 1961. — Intraspecific competition in sedentary marine animals. Symp. Soc. exp. Biol., 15 :
72-95.
Lincoln, R.J., 1979. — British Marine Amphipods (Gammaridae). British Museum (Natural History). London., 657 pp.
Rullier. F., 1943. Observations sur Mercierella enigmatica Fauvel dans la Ranee canalisee. Bull. Lab. marit. Dinard, 25 :
36-44.
SHEADER. M., 1978. — Distribution and reproductive biology of Corophium insidiosum (Amphipoda) on the north east coast
of England. J. mar. biol. Ass. U.K. . 58 : 585-596.
Thomas. N.S.. 1987. — Aspects of the ecology of the macroinvertebrates in the intertidal soft sediments of Chichester
Harbour. Ph.D. Thesis, Portsmouth Polytechnic, 343 pp.
THORP, C.H.. 1987. Ecological studies on the serpulid polychaete Ficopomatus enigmaticus (Fauvel) in a brackish water
millpond. Pore. NewsL, 4 : 14-19.
Thorp, C.H.. 1994. Population variation in Ficopomatus enigmaticus (Fauvel) (Polychaeta- -Serpulidae) in a brackish water
millpond, (1982-1992). Mem. Mus. natn. Hist. nat.. 162 : 585-591.
VuiLLEMIN. S.. 1965. Contribution a I'etude ecologique du lac de Tunis. Biologic de Mercierella enigmatica Fauvel. These
Doctoral d'Etat es-Sciences Naturelles, Universite de Paris, 554 pp.
Source :
63
Population variation in Ficopomatus enigmaticus (Fauvel)
(Polychaeta, Serpulidae) in a brackish water
millpond at Emsworth, West Sussex, U.K.
Clifford H. THORP
Marine Laboratory. University of Porsinouth, School of Biological Sciences
Ferry Road. Iiayling Island. Hampshire. POl 1 ODG. U.K.
ABSTRACT
Since 1982 a population of Ficopomatus enigmaticus has been monitored with respect to larval settlement and tube
accumulation on settlement panels. Prodigious settlements (1.3 x I07.m 2 max.) were recorded over the period 1982-85 and
globular, reef-like aggregations increased in number on the muddy floor of the pond but. prior to the onset of breeding in 1986.
the population crashed' dramatically. While live adults were not observed in the years 1986-88 larval settlements continued,
but with greatly reduced and decreasing maxima (1.6xlOTm-2. 1986; l.lxKP. nr*2, 1987 and 9.7 x 102. m 2, 1988). Since
1989 the adult population has recovered, being observed on the tide-gates and adjacent walls in particular ( 1989-90) and as
small aggregates on the pond bottom (1991). The increase in the adult population has been reflected in iifreasing settlement
densities (2.8 x 105. m-2, 1989 to 2.5 x 106. irr2. 1991). Evidence is offered to explain the population "crash" of 1986 and it is
suggested that it resulted from the age ol the adult population and a lack of both overwintering reserves and recruiunent. It is
also suggested that serpulid polychaeles which exhibit population "explosions", such as F. enigmaticus , are equally likely to
suffer population "crashes" and, further, that population numbers may well fluctuate in a cyclical manner.
RESUME
Variation de la population de Ficopomatus enigmaticus (Fauvel) (Polychaeta, Serpulidae) dans une retenue d’eau
sau mat rc a Emsworth, West Sussex, RU.
Depuis 1982. une etude, concernant 1 etablissement de larves et 1'accumulation de tubes sur les panneaux experimentaux. a
etc menee sur une population de Ficopomatus enigmaticus. De 1982 a 1985. des fixations considerables out etc enregistrees et
des agregals de forme spherique semblabies a des reeifs augmenterent en nombre sur lc fond vaseux du bassin de retenue.
Cependant. la population s'effondra de fa^on drastique el ccci avant le debut de la periode de developpemenl de 1986. Alors
qu aucun adulle vivanl ne fut observe de 1986 a 1988, la fixation de larves continuait mais leur abondancc etait exlrememenl
reduite et continuait a decroitre (1.6 x lOLm 2 en 1986; 1 . 1 x 103. nr2 en 1987 el 9.7 x 102. in 2 en 1988). Depuis 1989. la
population adulle s’est retablie et die lul observee sur les portes des marces et sur les parois adjacentes, lout particulierement
en 1989 et 1990. En 1991. de petites agregats s’etablirent au fond du bassin de retenue. L’augmentation de la population adulle
est le reflet de cette densile d etablissement larvaire (2.8 x 105. m~2 en 1989 a 2.5 x I06. in-2 en 1991 ). Quelques hypotheses
sont
THORP. CUE. 1994. — Population variation in Ficopomatus enigmaticus (Fauvel) (Polychaeta-Serpulidae), in a brackish
water millpond at Emworlh, West Sussex. U.K. In: J.-C. DaUVIN. L. LaUBIER & D.J. REISH (Eds). Actes de la 4eine
Conference internationale des Polychetes. Mem. Mus. natn. Hist, not .. 162 : 585-591. Paris ISBN 2-85653-214-4
Source : MNHN, Paris
586
CM. THORP
avancees afin d'expliquer reffondrement de la population de 1986. 11 csl suggere qu'elle lut causee par 1'age dc la population
adulte. et par 1'abscnce de reserves hivernales ainsi quo par I'absence de recrutement. 11 est aussi suggere que les serpules qui.
comme les F. enigmaticus, connaissent des explosions de leurs populations, pourraient de la meme fason. subir un
effondrement drastique de celles-ci. Dc surcroit. il se pourrait que ces populations nuctuent de fa^on cyclique.
INTRODUCTION
The scipulid Ficoponiatus enigmaticus (Fauvel), first reported in Britain from die London Docks in 1921
(Monro, 1924), has been recorded from a number of brackish water sites, mostly confined to southern coasts
(Zi brow i us & THORP, 1989). Although transitory populations have been recorded from Danish waters,
(WESENBURG— LUND, 1941; Hartmann-Schroder. 1971), and a population sustained by heated power station
effluent (Rasmussen, 1958), F. enigmaticus is considered to reach its northern limit of reproduction on British
coasts, several records again being associated with warm water effluents (Naylor, 1959; Markowski, 1962).
F. enigmaticus was first recorded from Chichester Harbour, West Sussex, in 1974 (THORP, 1980) and since
1980/81 has flourished in the brackish water millpond of the now defunct Slipper tideinill at Emsworth. West
Sussex (50°50.5'N, 0°56’W). The millpond has a surface area of 2.7 ha and, apart from a meandering deeper water
channel, has a maximum depth < 1.5 m (Thorp, 1987). Seawater enters from the adjacent Chichester Harbour
through tide-gates at the south end during spring tides > 4.3 m while fresh water enters from the north as part of
the River Ems. A relatively constant water level is maintained within the pond during low tide periods by the tide-
gates (Thorp, 1987). Within the pond limited hard substrata are readily "colonised" by F. enigmaticus, from the
tide-gates and adjacent brick walls to the stems of fringing reeds, but the most characteristic growths are globular
mini-reefs (aggregates). The aggregates, apparently resting on the soft mud substratum in depths of 0.75-1.0 m
(cf. Rullier, 1943), have resulted from larval settlement on small solid objects such as pebbles, stones, cans,
bottles, etc.
Since May 1982 water temperature, salinity and F. enigmaticus settlement have been monitored weekly.
Temperature and salinity are very variable and, despite the shallowness of the ponds, exhibit frequent and marked
discontinuities between the surface and the pond bottom at 0.75-1.0 m (Thorp, 1987). The overall salinity regime
(0.3—34. 1 P.S.U.) of the bottom waters, where greatest growth of the aggregates occurs, is both lower and more
variable in winter/spring than in summer/autumn (THORP, 1987). The overall pattern of salinity variation is of
high salinity over spring tide and low salinity over neap tide periods. Apart from when the River Ems is in spate,
spring tide salinities are gradually reduced over the neap tide period with an abrupt return to high salinity at the
next springs, fhe temperature range of the bottom waters also varies, from 5.5-30 °C in the wanner months of the
year (May-October) to -1-20 °C (November-April). Larval settlement is confined to the period May to
October/November, when the minimum bottom water temperature is > 10°C, and exhibits a marked lunar
periodicity with settlement occurring over the neap tides (Thorp. 1987 and unpublished data). Maximum
settlements have exceeded 10 x 106. m~2 (Thorp. 1987). In water temperatures > 10 °C spawning is apparently
initiated (triggered) by an influx of higher salinity water (spring tides). The minimum salinity required has not
been determined and spawning can be delayed in the absence of adequate phytoplankton levels (Thorp, 1987).
Although there are many records of the incidence of Ficoponiatus spp., several giving data for a few years
(Tebble, 1953; Hill. 1967; Straughan, 1972) and/or detailed seasonal data (Hill, 1967; Straughan, 1972;
Dixon, 1981), continuous observations of a single population over a long period are lacking. The present paper,
therefore, presents some results from monitoring a population of F. enigmaticus over the period 1982-92 and
suggests reasons to explain the pattern of variation.
MATERIALS AND METHODS
Panel studies employed 25 x 25x 0.6 cm Tufuol" panels attached horizontally to a frame, constructed from
1.8 cm "Durapipe". The panels were held 15cm above the pond bottom at 0.75-1.0 m depth. Settlement was
assessed using weekly (6-8 days) panels while seasonal panels were used to assess tube accumulation (weight).
Settlement density was determined using a 10 x 10 cm grid within a 2 cm wooden frame. Light settlements were
scored by placing the grid in each of the four corners of the panel and counting the total number of worms within
thelOx 10 cm grid area under a binocular microscope. Progressively heavier settlements were scored using
random numbers to select 10 1 x 1 cm squares within each grid and/or using a squared eyepiece grid within the
Source : MNHN. Paris
POPULATION VARIATION IN FICOPOMATUS ENIGMATICUS
587
I x 1 cm squares. Mean values were expressed as numbers/m2. Seasonal panels were weighed weekly on a spring
balance after standard drainage and removal of silt, attached algae and crabs.
RESULTS
Seasonal SETTLEMENT. — Figure I presents weekly settlement data for the years 1982-1992. Settlement
begins in mid to late May and ends in late October/November. The overall pattern demonstrates a series of peaks
and troughs which result from settlement occurring over neap tides (THORP. 1987 and unpublished data). The lack
of precision in figure. 1 reflects that weekly sampling was dictated by teaching commitments rather titan a precise
relation to the tidal phases. Thus, panel changing in the course of a set of neap tides could result in consecutive
panels attracting heavy settlements. The 10-year period can be split into three phases. Firstly 1982-85, which saw
a prolonged period of high settlements, several > lx 106. m 2 and some > 10 x 1(K\ m-2. This prolific phase was
followed by greatly reduced settlements from 1986-88. In early March 1986 the population suffered a catastrophic
2 -
2 -
1987
I - r
1989
I7IG. 1. — Settlement density of F. enigmaticus on weekly settlement panels, 1982-92.
"crash"; all aggregates died and live adults were not observed within die pond. Despite the apparent lack of live
adults, small settlements (max. 1600 m 2) occurred during shortened settlement seasons. The third phase, 1989—
91, witnessed an increase in both the length of the settlement season and settlement density, settlements
> 1 x 106. m~2 being recorded in both 1990 and 1991. Live adults again became abundant on the tide-gates and
adjacent brick walls and, in 1991, small irregular aggregates were observed on the muddy pond bottom. The 1992
season began well, with promising settlements in May and June. Late June, however, witnessed very extensive
and dense (80-90 % cover) growth of the green alga Diva lactuca on the pond bottom and July saw a dramatic
588
C.H. THORP
reduction in settlement. Throughout August and September the pond was allowed to flush tidally to give low-tide
aecess for repairs to a road bridge which crosses the pond and no further settlements were recorded. The 10-year
period, therefore, exhibits a cyclical pattern of initial abundance followed by a dramatic decline and subsequent
recovery.
TUBE accumulation. — Table 1 demonstrates considerable variation in the weight ol worms (+ tubes)
accumulating on weekly panels which does not appear to be related to settlement density. Increase in weight of
Table 1. — Tube accumulation (g dry weight) of F. enigmaticus on weekly panels.
seasonal panels also fails to reveal any trend (Table 2). There is again no apparent relationship between weight
increase and initial settlement density in the long term although, in 1983, the later panel (12.8.83) initially
increased in weight more rapidly which may reflect the greater settlement density. This, however, is not supported
by the different initial settlements in 1984. In both 1983 and 1984 the initial low settlements were probably
augmented by much greater settlements within three weeks (Table 2).
The explosive increase of F. enigmaticus in 1982/83 encouraged a considerable increase in the number of
shore crabs ( Carcinus maenas L.) within the pond which resulted in predatory damage to both the naturally-
occurring aggregates aid those on the panels, seriously affecting the late season accumulation.
DISCUSSION
Seasonal settlement. — Settlement is confined to summer/autumn when the minimum bottom temperature is
> 10 °C (THORP, 1987) which contrasts with a minimum of 18 °C in the Thames Estuary (Dixon, 1981). In the
first four years (1982-85) prodigious settlements occurred but it is possible to observe the onset of the 1986-88
decline during 1985. In that year only three weekly panels attracted more than 1 x 106. in-2 in contrast to 9, 6 aid
1 1 panels in the previous three years respectively. The cause of the reduced settlements can be deduced from the
physical conditions prevailing throughout summer/autumn 1985. Through April, and particularly May, 1985 little
or no sunshine prevented any phytoplankton increase. Strong sunshine in the last week of May, however, resulted
in a rapid increase in visible phytoplankton levels which probably triggered spawning, with small settlements in
the first two weeks of June. This was followed by settlements > 2 x 106. m-2 in July and a subsequent decline until
late September. The sunny period of late May/early June was followed by a long period of poor summer weather
during which pond water clarity suggested very low phytoplankton levels. In mid-September 2-3 weeks of better
weather promoted a small plankton increase. As the bottom water temperature was > 10 °C throughout this period
it is probable that the decline in settlement can be attributed to low phytoplankton levels. The "events" of die 1985
summer most probably led, at least in part, to the catastrophic decline of the adult population in March 1986.
Overwintering adults withdraw to the lowermost levels of their tubes during cold winters and assume a state of
torpor (Zi brow i us & THORP, 1989). Consequently, organic and inorganic debris settling from the water column
accumulate within upward-facing tubes and must be cleared before normal activity can be resumed. That this does
not always happen is inferred from aggregates where the central area, containing the upward-facing lubes, dies
out leaving the more oblique and lateral-facing tubes to form atoll-like structures. It is probable that, with winter
inactivity and zero phytoplankton levels, F. enigmaticus has to overwinter on reserves built up over the previous
summer/autumn. 'The low phytoplankton levels through 1985 could have resulted in reduced somatic reserves for
overwintering, causing weakened animals, unable to clear their lubes, to perish. KNIGHT-JONES & Moy.se (1961)
reported that gregarious animals can assume a growth form to maximise their feeding potential, and it is this
POPULATION VARIATION IN FICOPOMATUS ENIGMATICUS
589
strategy which results in F. enigmaticus tubes being evenly spaced and their feeding apparatus (branchial crown)
deployed to its best advantage. In practice the^ branchial crowns of adjacent animals are contiguous, largely
preventing the settlement of larvae or sediment within the aggregates. While the longevity of F. enigmaticus
remains unclear it is possible that by 1986 the aggregates comprised animals which were 4-5 years old. This is
based on the likelihood that there is little or no secondary settlement as long as die aggregates maintain their
integrity and also, that die limited hard substrata within the pond complex were rapidly occupied. Thus "old age"
and a lack of overwintering reserves could have resulted in debility which led to die massive mortality.
Table 2. — Tube accumulation (Kg wet weight) of F. enigmaticus on nseasonal panels. Is: Initial settlement
density. Is+3: Additional settlements withing 3 Is. c : Crab predation of tubes.
Through 1986-88 a few adults must have survived to provide die small settlements observed, but these years
were also notable for low phytoplankton levels. The years 1989-91 not only witnessed very hot and prolonged
summers, particularly 1989, but also increased and extended phytoplankton "blooms". Consequently, not only did
die breeding season of F. enigmaticus increase in length, but maximum settlements increased, with four weekly
counts > 1 x 106. m 2 in 1991.
It was expected that 1992 might witness a population explosion. Thick and prolonged ice-cover in February
1991, while it may have caused considerable mortality in the adult population, crushed the remaining "dead"
aggregates freeing additional hard substrata. After good settlements in mid-May, which accompanied high
phytoplankton levels, settlement declined markedly in July. While this failure can be associated widi a crash’ in
the phytoplankton level it can not be related to reduced sunshine levels. It does, however, appear to be associated
with the very heavy growth of Ulva lactuca which developed on the bottom of the pond from early June.
I Iimmelmann (1980) reported the significance of phytoplankton levels in the synchronisation of spawning in
marine invertebrates and. while the Ulva undoubtably 'blanketed' the existing aggregates its true effect probably
was to greatly reduce the nutrients available to sustain die phytoplankton and consequently remove an essential
spawning trigger. While Ulva featured in the millpond as shortlived, dense growths in previous years, notably
1991 (Thorp, unpublished data), it was the density and prolonged nature of the 1992 growth that was significant.
With 1992 being the fourth 'dry' year in succession in Britain the fresh water flow from the River Ems has been
greatly reduced bothnaturally and through increased abstraction by the local water authority. Consequently the
weekly bottom water salinity only fell below' 20 twice in 1992 (Jan/July). Seawater entering the millpond is
probably high in dissolved nutrients, as a result of the high sewage effluent loading of the adjacent and connected
Langstone Harbour (Portsmouth Polytechnic, 1976). Thomas (1987) also referred to localised increases in
organic pollution in Chichester Harbour arising from both small sewage discharges and land drainage from the
surrounding agricultural land. Not only do point discharges occur in the area of the harbour adjacent to the
millpond but the River Ems also drains a considerable area of farmland. Thus Ulva , which grows prolifically in
Langstone Harbour, has been able to flourish in relatively high salinity, warm, nutrient-rich water at the expense
of possibly brackish water phytoplankton species.
Tube accumulation. — Mass formation of serpulids has been variously attributed to a complex of
environmental factors including competition for space and food; reduced predation: gregarious behaviour: larval
retention: primary productivity and hydrographic factors such as temperature and salinity (SCHROEDER &
590
C.II. THORP
Hermans, 1975; Bosence, 1979; Hove, 1979). Significantly Hove (1979) also stated that decreased competition
with other animals, mainly for space, may lead to massive numbers in species at the periphery of their ranges. In
optimum conditions the millpond embraces all these factors, acting as a brackish lagoon and experiencing elevated
temperatures, limited substrate availability and high primary productivity. The tide-gate control of water level will
encourage larval retention and there are no major competitors for space or food. It is rather the success of F.
enigmaticus which creates the problems.
While the length of settlement season is governed by temperature, tube accumulation within seasons may be
affected by both food availability and initial settlement density. Tube accumulation in both 1983 and 1984 can be
related to the length of the immersion period (Table 2) and there appears to be some support for the idea that
initial settlement density is involved within years, cf. 14/7 and 12/8 in 1983 particularly at 9 weeks. Similar data
for 1984 (15/5 and 27/6), however, more likely reflects the high subsequent settlements on the 27/6 panel. In the
absence of phytoplankton data it is difficult to comment on the effect of food level, although the 1985 panel (5/6)
suggests a strong connection. While the low rate of accumulation in 1985 may reflect the small initial settlement
(1.5 x K)-45. nr2) when compared to the 1990 panel (7/6), it may well result from the low- phytoplankton levels
observed in 1985. Heavy metal levels in Chichester Harbour will be very low (Thomas, 1987) and unlikely to
have any deleterious effect. Although there are >8.000 small boats (98.7% < 12 m in length) moored or berthed in
marinas in the harbour, as 74 % (2.1 15 ha) of the total harbour, area (2,849 ha) is intertidal (Chichester Harbour
Conservancy, pers.comm), it is probable that tidal flushing greatly reduced any effects of organo-tins prior to the
ban on their general use in antifouling paints in 1987.
'Hie overall pattern, of population proliferation followed in turn by a catastrophic decline and subsequent
recovery, possibly represents the normal pattern in a species with great fecundity, relative longevity and
occupying a habitat with limited available substrata. Indeed BOSENCE (1979) stressed the importance of limited
substrata in die rapid build-up of tube aggregates in Serpula vennicularis. Massive settlement of F. enigmaticus
would quickly occupy all available hard substrata within perhaps one or two seasons and the close packing and
disposition of the tubes would prevent significant recruitment and lead to an ageing population prone to disaster. It
is suggested dial disaster struck due to a lack of overwintering reserves resulting from the poor summer of 1985.
Thus, gregarious species with an epidemic spawning capacity could be expected to exhibit an alternating pattern
of success and decline. In diis respect it is interesting to note that die invasive serpulid. Hydro ides ezoensis Okuda.
exhibited a similar, if partial, population decline in Southampton Docks in 1987/88. H. ezoensis, first recorded as a
single specimen from the intake channel of Fawley Power Station, Southampton Water, in 1977, formed massive
encrustations (30cm thick) in the intertidal region of most dock structures (Thorp el ai, 1987). The population on
the Town Quay, however, died and sloughed off in 1988/89, this event preceding demolition and reconstruction of
the quay (THORP, unpublished data).
Keene (1980) and Davies et ai (1989) both reported an apparent beneficial interrelationship between
populations of F. enigmaticus and sediment and nutrient levels within semi-enclosed waters. Circumstantial
evidence from the present study suggests a similar relationship within the Slipper pond where high phytoplankton
levels complement high settlement densities. While it is truly a "chicken and egg" situation as to which comes
first, elsewhere it has been shown that the overall economy of the pond can be related to the success of F.
enigmaticus (THOMAS & THORP, 1994).
ACKNOWLEDGEMENTS
I am happy to acknowledge the kindness that the trustees and members of die Slipper Millpond Preservation
Association have extended towards me in allowing me to work in the pond. I tun also indebted to Havant Borough
Council, and particularly Alistair Martin, for making the Hayling Island, Beachlands, meteorological records
available to me. I also acknowledge the assistance of James HEPBURN in making this a more complete record by
covering some of my absences.
REFERENCES
Bosence. D.W.J., 1979. The factors leading to aggregation and reef formation in Serpula vennicularis L. In: G. Larwood
& B.R. ROSEN (eds). Systematics Association Special Volume No. IJ. Biology and Systematics of Colonial Organisms.
Academic Press. London and New York : 299-318.
Davies. B.R.. Stuart. V. & Villiers. de V.. 1989. — The filtration activity of a serpulid polychaete population ( Ficopontaius
enigmaticus Pauvel) and its effects on water quality in a coastal marina. Est. Coastal Shelf Sci., 29 : 613-620.
Source : MNHN. Paris
POPULATION VARIATION IN FICOPOMATUS ENIGMATICUS
591
Dixon, D.R. 1981. Reproductive biology of the serpulid Ficopomatus ( Mercierella ) enigmaticus in the Thames Estuary,
S. E. England. 7. mar. biol. Ass. U.K.. 61 : 805-815.
HARTMANN -SCHROEDER, G.. 1971. Zur Unterscheidung von Neopomatus Pillai und Mercierella Fauvel (Scrpulidae,
Polychaeta). (Mill neuen Beitragen zur Kenntnis der Okologie und dcr Rohrenform von Mercierella enigmalica). Mill,
hamb. zool. Mus. Inst.. 67 : 7-27 .
HILL M.B.. 1967. — The life cycles and salinity tolerance of the serpulids Mercierella enigmalica Fauvel and Hydroides
uncinata (Philippi) at Lagos, Nigeria. 7. Anini. Ecol. 36 : 303-321.
HlMMELMAN. J.IL. 1980. — Synchronisation of spawning in marine invertebrates by phytoplankton. In: W.H. CLARKE Jr &
T. S. ADAMS (eds), Invertebrate Reproduction . Developments in Endocrinology . Elsevier, North Holland. Amsterdam : 3-
19.
Hove, 1 1. A. ten., 1979. — Different causes of mass occurrence in serpulids. In: G. Larwood & B.R. Rosen (eds).
Systematic^ Association Special Volume No. II. Biology and Systematics of Colonial Organisms. Academic Press, London
and New York: 281-298.
KEENE, Jr.. W.C., 1 980. - The importance of a reef-forming polychaete, Mercierella enigmalica Fauvel. in the oxygen and
nutrient dynamics of a hypereutrophic subtropical lagoon. Est. Coastal Shelf Sci.. 1 1 : 167-178.
KNIG I rr-JONES , E.W. & MOYSE, J.. 1961. — Intraspecific competition in sedentary marine animals. Symp. Soc. exp. Biol.. 15 .
72-95.
Markowski. S.. 1962. Faunistic and ecological investigations in Cavendish Dock. Barrow-in-Furness. 7. Anim. Ecol.,} 1
42-52.
Monro, C.C.A.. 1924. — A serpulid polychaete from London Docks ( Mercierella enigmatical. Fauvel). Ann. Mag. nat. Hist..
(9) 13 : 155 159.
Naylor, E., 1959. 'ILe fauna of a warm dock. Proc. XVth intern. Congr. Zool., London 1958 : 259-262.
PORTSMOUTH POLYTECHNIC, 1976. Langstone Harbour Study - The effect of sewage effluent on the ecology of the harbour.
Portsmouth Polytechnic. Report to the Southern Water Authority, 365 pp.
Rasmussen. E.. 1958. Emigranter.l. Kobenhavns Sydhavn. Naturens Werden.. 8 : 231-234 and 246-248.
RULLIER. F., 1943. Observations sur Mercierella enigmalica Fauvel dans la Ranee canalisee. Bull. Uib marit. Dinard. 25 :
36-44.
SCHROEDER. P.C. & Hermans, C.O., 1975. Annelida : Polychaeta. In: A.C. GlESE & J.S. PEARSE (eds). Reproduction of
Marine Invertebrates, 3. Annelids and Echiurans. Academic Press, New York and London : 1-213.
STRAUGHAN, D.. 1972. Ecological studies of Mercierella enigmalica Fauvel (Annelida: Polychaeta) in the Brisbane River.
7. Anim. Ecol.. 41: 93-135.
'PEBBLE. N.. 1953. A source of danger to harbour structures - encrustation by a tubed marine worm. 7. Inst, mimic. Engin..
80 : 259-265.
Thomas. N.S.. 1987. Aspects of the ecology of the macroinvertebrates in the intertidal soft sediments of Chichester
Harbour. Ph. D Thesis. Portsmouth Polytechnic, 343 pp.
THOMAS, N.S. & Thorp. C.H.. 1994. — Cyclical changes in the fauna associated with lube aggregates of Ficopomatus
enigmaticus (Fauvel). Mem. Mus. Nat. Hist. nat. Zoologie.. 162 : 571-580.
lYlORP, C.H.. 1980. — The benthos of the Solent. In: The Solent Estuarine System: an assessment of present knowledge.
Natural Environment Research Council Publication, London (C) 22 : 76-85.
Thorp. C.H., 1987. — Ecological studies on the serpulid polychaete Ficopomatus enigmaticus (Fauvel) in a brackish water
millpond. Pore. News!.. 4 : 14 19.
Thorp, CM.. Pyne, S. and West. S.A.. 1987. — Hydroides ezoensis Okuda. a fouling serpulid new to British coastal waters. 7.
nat. Hist.. 21 : 863-877.
Wesenberg LUND, E.. 194 1. Notes on Polychaeta I. 1. Harmolhoe bathydomus Hj.Ditlevsen refound. 2. On the sabellid
genus Fabricus. 3. Three polychaetes from Ringkjobing Fjord, unrecorded in Denmark. 4. Mercierella enigmalica Fauvel.
a serpulid new to Denmark. Vidensk. Medd. Dansk. Nat. Foren. Kobenhavn. 105 : 31-47.
ZlBROWius. II. & THORP, (MI.. 1989. A review of the alien serpulid and spirorbid polychaetes in the British Isles. Cah.
Biol. mar.. 30 : 271-285.
Source : MNHN. Paris
64
Polychaetes of commercial and applied
interest in Italy: an overview
M. Christina GAMBI * Alberto CASTELLI00, Adriana GIANGRANDE ***
p. LANERA **** Daniela PREVEDELLI ** & R. ZUNARELLI VANDINI**
* Laboratories di Ecologia del Benthos-Stazione Zoologica "Anton Dohrn". Ischia, Napoli. Italy
00 Diparlimcnto di Scienze Antropologiche. Universita di Sassari. Italy
** Dipartimento di Biologia Animale, Universita di Modena, via dell'Universita 4, Modena. Italy
*** Dipartimento di Biologia. Universita di Lecce, via Monteroni di Lecce. Lecce. Italy
*** *Bioservice Soc. Coop., vico San Domenico Maggiore 9. Napoli. Italy
ABSTRACT
The commercial interest of polychaetes is mainly due to their use as bait in recreational fishing and as food in
aquaculture. 'I he species of worms collected in Italy for these commercial and applied purposes is reviewed. Light species
of worms are collected for bait in Italian waters. Hediste diversicolor, Perinereis cull rif era , Perinereis rtdlieri and
Marphysa sanguined are collected from the Venice Lagoon. Lumbrineris impatiens is harvested in the Gulf of Naples,
while Diopatra cuprea cuprea is collected from a littoral lagoon in Southern Sardinia and Sabella Spallanzani i from other
coastal areas of Sardinia. Finally. Eunice aphroditois is collected along the coasts of Apulia. A review of the literature on
the effects of worm exploitation on the population, the associated communities and the environment, pointed out
different results and patterns, and suggested the need for further studies and for legislation to control indiscriminant bait
collecting to ensure a balance between the environment and the polychaete resource. Moreover, for the species that are
imported from Korea. Japan, U.S.A. and other European countries, there is a risk of their accidental introduction into
local biotopes. In this study we show that small-sized, "r-slrategist" polychaetes. such as Spio decoratus or Polydora
ciliata, are suitable food for juveniles of fish and crustaceans in aquaculture.
RESUME
Les Polychetes d’interet commercial et applique en Italic : line revue
Les Annul ides Polychetes sont devenus un marche important car ils sont de plus en plus utilises comme appal pour la
pechc "au gros" et comme nourriture en vue de lelevage dans des fermes aquatiques. Cette etude est factual isation de ce que
nous savons en Italic sur (’utilisation des vers dans ces huts commerciaux. Hint especes de polychetes sont utilisees
comme appat dans les eaux italiennes. Hediste diversicolor, Perinereis cult rife ra , Perinereis rullieri et Marphysa
sanguined sont peches dans la lagune de Venise. Lumbrineris impatiens est capture par des plongeurs professionnels dans
le golfe de Naples, alors que Diopatra cuprea cuprea et Sabella spallanzanii se pechent dans les zones littorales de la
GAMBI. M.C.. CASTELLI. A.. GlANGRANDE, A.. LaNERA. P.. PREVEDELLI, D. & R. ZUNARELLI VaNDINI, 1994. — Poly¬
chaetes of commercial and applied interest in Italy: an overview. In: J.-C. DaUVIN, L. LAUBIER & D.J. REISH (Eds). Actes
de la 4cm e Conference inter nation ale des Polychetes. Mem. Mus . natn. Hist, not., 162 : 593-603. Paris ISBN 2-85653-
214-4
594
M.C.GAMBI ET ALU
Sardaigne. L'cspccc Eunice aphroditois csl pechce par des inarins profcssionncls ct dcs pcchcurs "au gros" Ic long de la
cole des Pouilles. Les etudes effecluees a ce jour sur les effets de la pechc des vers sur le niveau dcs populations, sur les
communautes associees et le biotope ont conduit a des resultats qui suggerent la necessite d'autres rechcrchcs el d’une
legislation adequate pour assurer un equilibre entre I’environnement et cetle ressource en Polycheles. Com me beaucoup
d’autres especes etrangeres sont importees des Etats-Unis, de la Coree, du Japon et d'autres pays curopccns, il resle aussi le
risque de leur introduction accidentelle dans les biotopes locaux. Dans ccttc etude on montre egalement que des especes de
Polychdtes de peliles dimensions el a strategic "r". comme Spio deco rat us ou Polydora ciliata. peuvent servir de nourriture
complementaire h de jeunes poissons et de jeunes crustaccs eleves dans un but commercial.
INTRODUCTION
Polychaeious annelids are gaining significant commercial importance because they are increasingly used as bait
for amateur and professional fishing. The widespread and ancient activity of worm collecting for angling is
relatively well documented but quantified only in a few cases, mainly along the North American coasts (D'Asaro
& Chen, 1976; Creaser et al. , 1983), in East Asia (Choi, 1985) and in Northern Europe (Blake, 1979a, b;
Heiligenberg, 1982; Olive, 1994 a). The commercial value of the most exploited species have been documented
by various authors (Klawe & Dickie, 1957; Creaser et al , 1983; Sarda, 1989; Chen, 1990). Recently
Olive (in press) summarized the different patterns of worm exploitation and the potential for their aquaculture-
based production. In most countries, including Italy, species tire harvested from field populations (Klawe &
Dickie, 1957; Blake, 1979a, b; Choi, 1985), and only a few cases of commercial rearing are known (Ryther et
al ., 1975; Kurihara, 1983; Olive, 1994).
Polychaetes are also used for other applied purposes, such as food in maricullure, decomposers of domestic and
aquaculture organic wastes (TENORE & Gopalan. 1974; TENORE et al .. 1974; Ryther et al. , 1975) and test
animals for toxicological studies (REISH, 1980). The aim of this study is to review the species of polychaetes that
are harvested as bait, or have a potential applied interest in Italy, and describe their known biology and their
methods of harvesting.
RESULTS
Eight species of polychaetes arc commercially collected from natural populations in Italy. The sites of more
intensive harvesting for each of these species are shown in figure 1. Species are generally dug from tidal flats or
from lagoons and shallow littoral biotopes by professional and amateur fishermen who use special raking hoes or
shovels. A few species are harvested by SCUBA divers by hand or with small shovels in shallow waters from soft
or hard substrates (GAmbi et al.. 1992; BELLO, 1993). Data on number of diggers and on quantity of specimens
collected, their seasonality and commercial value are largely unavailable from die commercial companies involved
in this market which is only just developing in Italy.
Hediste diversicolor ( O.F. Miiller, 1778).
This euryhalinc species is common in various Italian brackish zones (CiI.angrande et al.. 1983-84), and it is
commercially harvested mainly from the Venice Lagoon (Fig. 1). Here H. diversicolor colonizes areas of low
salinity, and reproduces from March to April (Ansaloni et al ., 1986). However, the spawning period of this
species varies between different geographic areas (SCAPS, 1992). The specimens may reach 20 cm in length in
Italy, but their commercial size is from 10-12 cm. H. diversicolor is sold as "Trcmolina”, however, it is often
confused with other species of the genus Perinereis. The cost in 1992 was about US $ 1 for a box of 8-10 worms.
It is also imported from France.
Perinereis cultrifera (Grube, 1840).
This species is common along the Italian coasts both in soft sediments and in shallow, algal covered hard
bottoms. Commercial harvesting is mainly from the Venice Lagoon (Ansaloni et al , 1986) (Fig. 1) where it
thrives in shallow muddy bottoms forming burrows in the upper 10 cm. It is collected by shoveling and sieving
the mud through large-mesh screens. Amateur anglers collect P. cultrifera from several other coastal areas,
including the coasts ot Sicily, where a C11SO4 solution is used to force the worms out of their burrows. In the
Venice Lagoon, P. cultrifera reproduces in March following epitokal modification (ANSALONI et al ., 1986).
Source :
POLYCHAETES OF COMMERCIAL INTEREST IN ITALY
595
However, other authors in hie Mediterranean observed reproduction in different seasons and without epitoky (P£r£s
& RaN'CUREL, 1948: DURCHON, 1957; MARCEL^ 1962). In hie Mediterranean P. cult rife ra reaches a maximum
length of 15 cm, while in the Atlantic it reaches 25 cm. The species is known commercially as "Saltarello
veneziano", and it is often confused with Perinereis rullieri and sometimes with H. diversicolor. The commercial
price is similar to dial of H. diversicolor and a large number of P. cultriferci are also imported from France.
FIG. L Map of Italy with the location of the main harvesting sites for each of the eigth species of polychactes
exploited as bail. Only the areas of intensive commercial collecting are indicated.
Perinereis rullieri Pilato, 1974.
P. rullieri has been recorded only along die Italian coasts, and it is probably endemic to the Mediterranean Sea
(PREVEDELLI el at., 1990). The commercial digging occurs mainly in the Venice Lagoon where P. rullieri reaches
18-20 cm in length. It is harvested commercially from 8-10 cm. Worms are collected from the intertidal zone from
a substrate of gravel, muddy sand and small stones (Prevedelli et al, 1990). Spawning is generally in April, but
not via epitoky. and fertilisation takes place on the bottom. Fertilized eggs are embedded in gelatinous envelopes
which are attached to the stones where they form large, green coloured clumps. The hatched larvae are nectochaetae
with three setigerous segments (Prevedelli et al., 1990: Prevedelli & Zunarelli Vandini, 1992). The
species is often confused with die co-generic P. cultrifera, and is labelled and sold at the same prices of the odier
nereidids.
Source :
M.C.GAMB1 ET ALII
596
Diopatra cuprea cuprea (Bose, 1802).
Along the Italian coasts D. cuprea cuprea is found generally in shallow depths in sandy sediments mixed with
mud. This species is commercially collected mainly in the littoral lagoon of Santa Gilla, near to Cagliari and in a
few other shallow and sheltered areas nearby (Fig. 1) (COTTIGL1 a, pers. comm). This species is sold as
"Tremuligione", and is collected both using a spade in shallow water, and by SCUBA diving at 2 m depth.
Number of bail diggers varies from about 25 in autumn and winter, to about 40 in spring and summer. The
demand was great for this species, however, its harvest has been reduced recently because of die use of other local
and imported bait worms (Cotliglia, pers. comm.). The number of worm dug depends on market demand and
season, and ranges from a mean of 3-4,000 per day in winter, to a mean of 20, 000 in summer, resulting in an
estimated 3.5 million of worms being harvested each year (Cotliglia, pers. comm.). D. cuprea cuprea can reach 30
cm in length but is collected from about 20 cm. Its reproductive cycle is unknown, but as other large onuphids
(FAUCHALD, 1983), it could have a life span of several years.
Marphysa sanguined (Montagu, 1815).
M. sanguined has been recorded from several Italian coastal areas in intertidal and shallow littoral muddy
bottoms (PREVEDBLLI, 1989). In the Venice Lagoon, where it is commercially harvested, it burrows deep in die
sediment, below die layers colonized by the nereidids. The species grows to 50 cm in length, and specimens 20-30
cm long are used for commercial purposes. In the Venice Lagoon this species reaches a density up to 60 ind. in:,
and it is collected by digging up sediment that is sieved through coarse screens. In the Venice Lagoon M.
sanguined reproduces seasonally in April, ;uid widiout morphological modification. The spawning is synchronized
and occurs on die bottom (Prevedelll 1989). This species is the most valuable bait of all species collected in
Italy. It is commonly sold as "Muriddo", with regional names of "Murone, "Bacone" and " Venue sanguigno". A
box of 6-8 worms was sold in 1992 at about IJS $ 4. Specimens labelled as M. sanguined are imported from the
U.S.A. and Korea.
Eunice aphroditois (Pallas, 1788).
E. aphroditois is a coastal species occurring at depdis of 10-15 m in soft bottoms where it lives inside a
characteristic U-shaped parchment tube. Small specimens may also occur on hard substrates (Fauvel, 1923). In
Italian waters it reaches over 1 m in length (BELLO, 1993), and specimens of larger dimensions have been reported
from the Atlantic (Fauvel. 1923). Reproduction and life cycle is unknown, however, because of the large size
reached and like other related species (Fauchald, 1983; GiaNGRande, 1989a), E. aphroditois may be a
long-lived species. In Italy E. aphroditois is known as "verme di Rimini" and is mainly collected along the Apulia
coasts (Fig. 1) where is called "Vermara". Worms arc collected both by SCUBA diving up to 10 m depth, and by
using a special long, thin stick from a boat (Bello, 1993). E. aphroditois is a suitable bait to catch fish of the
family Sparidae, and it is used also by commercial fishermen to bail their lines (Bello, 1993). The price of a
single specimen reached in 1992 US S 1.5.
Lumbrineris impatiens Claparfcdc, 1868.
Along the Italian coasts L. impatiens is commonly reported in sandy, muddy-sand and detritic soft bottoms
(Gambi & Giangrandh, 1986) where it lives below the sediment in temporary burrows. Specimens collected in
shallow waters (1-5 m depth) are of greater dimensions measuring up to 40 cm in length, than those collected from
deeper waters (10-20 m) which are only a few centimeters in length. This suggests age class distribution according
to depth, or an ecotype determined by different trophic and ecological conditions. However, the existence of
"sibling" species cannot be excluded. The biology of L. impatiens is poorly known. McNULTY & Lopez (1969)
observed mature eggs throughout the year in Florida, but with a decrease in frequency in winter. Cazaux (1972)
studied die larval development of a population of the north Atlantic French coast, and he found that the larva is
planetotrophic with a pelagic phase of about 15 days. Biological data of the Mediterranean Sea population of this
species are lacking. For commercial purposes L. impatiens is mainly harvested from shallow sandy areas in the
Gull of Naples. Within the Gulf it is particularly abundant at the mouth of the Sarno river which is enriched with
organic matter deriving from agricultural industry wastes. Worms are collected by about 10 SCUBA-divers who are
organized in a cooperative. There is a great demand for this species which is locally called "Esca rossa" or also
rremolina". A single diver may collect over 200 worms a day. The commercial size of the worms is generally
over 20 cm long and the cost in 1992 varies form US S 0.5 to US I S for a single specimen.
Source :
POI .YC\ IAHTES OF COMMHRCIAI . INTEREST IN I TALY
597
Sabella spallanzanii (Gmelin, 1791).
S. spallanzanii , belter known under its original generie name of Spirographis, is very common on hard
substrate along the Italian coasts (Giangrande, 1989, b). It is found in the open coastal areas from 1 to 30 m
depth, and in shallow confined areas such as harbours, where it often reaches very high densities. S. spallanzanii
reproduces in winter, and die egg dimensions suggest a lecidiotrophic development (Giangrande & Petraroli.
in press). Specimens can reach up to 40 cm in length and preliminary observations suggest a growth rate of about
10 cm per year (Giangrande & PETRAROLI. 1994). Since this species is a suspension feeder, it can be fed in
laboratory with various kinds of suspended food, including probably particulate organic matter, and it may be
suitable in die treatment of domestic and aquaculture wastes. The use of Uiis species as a bait by anglers is limited
to some localities in Sardinia where it is known as "Tremuligione amaro". It seems particularly suitable its bait for
catching large Sparidae (RlGHlNl, 1991). The potential for a larger market for this species is supported by the
results of some preliminary tests conducted with amateur anglers (Giangrande, unpublished data). It is also
likely that other large-sized sabellids with growth rate and ecological requirements similar to those of S.
spallanzanii may be suitable for bait (e.g., Branchiomma luctuosum (Grube)) (Sordino & Gambi. 1992).
A few other polychaete species belonging to the genera Sabellaria and Ophelia, are collected as bail in various
coastal areas by local amateur anglers, but are not commercialized. A list of some of the polychaete species
harvested as bait in Italy and in other countries is given in Table 1. The list is probably incomplete and the
number of species taken is likely underestimated because such information is usually not reported. However, about
32 species are exploited in various countries, and share some general features : a) relatively large adult dimensions
(between 15 to 30 cm in length); b) wide geographic and ecological distribution, indicating a broad tolerance to
different environmental conditions; c) a variety of feeding behaviour and food sources, with most of them being
detritivores or omnivores; d) life spans generally longer that one year, and frequently 3 to 5 years; e) many are
polytelic (= ileroparous) species breeding more than once per lifetime, but some (e.g., Nereididae and Glyceridae)
are monotelic (= semclparous) (Olive, 1983). The life span of the monotelic species varies between 1-2 years in
the case of H. diversicolor , and up to three or more years in others.
OTHER APPLICATIONS AND USES OF POLYCHAETES
Small-sized polychaetes, such as various Spionidae and Capitellidae, are used in aquaculture to supplement die
diet of commercial fish and crustaceans (GiTrin, 1978). These species generally show many "r-sirategy" traits in
their life histories. In an integrated polyculture system for the treatment of acquaculture wastes, Capitella capitata
was used as food for juvenile stages of the commercial fish Pseudopleuronectes americamis (Ryther el ai, 1975).
In a semi-intensive culture of Penaeus japonicus in Italy, the spionid polychaete Polydora ciliata played an
important role in the diet of the shrimp and was consumed in large amounts from the bottom of the culture tanks
(Zl'PO el ai, 1989). Several species of spionids aid capitellids are relatively easy to rear in the laboratory from
larvae collected from plankton, (Chi: & Levin, 1989). The culture of spionids throughout their life cycle has been
documented for Malacoceros fuliginosus (Gu£rin, 1987), for Boccardia semibranchiata (Guerin, 1991) and for
Streblospio benedict ii (LEVIN. 1984). Spio decoratus has been retired from larvae collected in plankton to mature
adults (Giangrande et al., 1992). This species is polytelic, a feature common to several Spionidae
(Gudmansson, 1985). It has a short life span and reproduces continuously alter reaching maturiry at six months ;
egg laying then occurs about every other month. The above studies suggest dial several species of spionids may be
suitable to be reared in the tanks with cultured fish and crustacean to supplement their diet.
DISCUSSION
The bail polychaetes which are commercially the most valuable in Italy are likely to be the species with the
longest life spans: M. sanguined, L. impatiens, D. cuprea cuprea and E. aphrodiiois. Because of their long life
cycle, the long term exploitation of these species needs a knowledge of their biological and ecological requirements
for management that optimizes their harvest and minimises the impact of collecting on their populations and on
their habitat. However, apart from M. sanguined and P. rullieri, studies on the life cycle and population dynamics
598
M.C. GAMBI ET ALII
Table 1. — Bail species harvested and/or cultured in Italy and in other countries.
The data are from literature, market surveys and other sources.
of the commercial species in the exploited sites in Italy are lacking. They are harvested with no regard to their life
history and the potential destructive effects of collecting. Moreover, worms are generally harvested without
appropriate legislation to regulate periods of collecting and number of individuals which can be removed.
Geographic variability in reproductive mode and time has been documented in different cospecific populations
(e.g., H. diversicolor or P. cultrifera). In addition, population structure may vary and not all populations may be
commercially viable (Olive, 1994). A few studies have examined how harvesting may affect population
parameters such as fecundity, growth rate, mortality and genetic variability. The spawning stock and the
population structure of Glycera dibranchiata (Klawe & Dickie, 1957) and of Neanthes virens and Arenicola
marina (Blake, 1979 a, b) were not effected by digging. On the oilier hand, for a different population of Glycera
Source : MNHN. Paris
POI -YCI IAETES OP COMMERCIAL INTEREST IN I' I'M .Y
599
dibranchiata, intensive harvesting reduced heterozygosity, enhanced genetic drift and altered rapidly the genetic
structure of the population (Vadas & Bristow, 1985).
The commercial harvesting of polychaetes also has general implications at community and environmental
level, and raises problems of resource management dial arc common to other cases of marine resource exploitation.
Digging for worm collection causes great physical disturbance to the substrate and this affects the benthic
community. A study on the rocky coasts of South Africa (Van Herwerden, 1989) demonstrated dramatic
destruction of the environment and of biotic resources, particularly mussel beds, caused by the collection of
Pseudonereis variegata . Digging for the bait Arenicola marina along the Norfolk coast (U.K.) caused massive death
of the cockle, Cerastoderma edule (JACKSON & JAMES, 1979). On the oilier hand, investigations on Hie effects of
digging lor Arenicola on a tidal Hat in The Netherlands (Heiucenberg, 1982) and on an estuary in the U.K.
(McLUSKY et al ., 1983) revealed dial, after an initial period of community collapse, die density of some benthic
species was enhanced, and diere was a rapid population recovery of the worms, mainly due to die above-surface
migration of adults from surrounding areas. A similar recolonization pattern, observed for a different population of
Arenicola (Olive, in press), suggests diat periods of exploitation alternating with periods of recovery from reserve
zones could be a suitable management method for diis species, as well as for odier exploited worms ( e.g AL
sanguinea ; Choi. 1985).
These few reports and dieir different results demonstrate the need for systematic studies to evaluate the
environmental impact of long term exploitation of worm populations. There is an increasing awareness of diis
problem also in the Venice Lagoon and in other Italian areas where habitat damage coupled with competition
among professional and amateur fishermen is starting to limit these worm resources (Bello, 1993).
Another important environmental risk is diat die importation of allochtonous species which are generally sold
alive (in Italy mainly the tropical Perinereis spp.), may increase die risk of accidental introduction of foreign taxa.
To reduce and overcome these environmental problems, commercial rearing is an attractive solution both
scientifically and economically, lo date a few polychaete species are commercially reared (Ryther el al.. 1975 ;
Rf.ish, 1980; Kurihara, 1983; Olive, 1994), and various biological problems related to their large scale
production, such as diseases, parasites, supply of larvae, still need to be resolved (Scaps, 1992; Olive, in press,
a). Some of the Italian species are potentially suitable for commercial culturing. Those species arc the nereidids
that have short life spans, and AL sanguinea or L. impatiens that can fed various organic detritus. S. spallanzanii
which has a fast growth rate and can udlize organic compounds produced and released in die water column by odier
cultured organisms (e.g.. mussels) is another potential species.
The main aim and the scientific challenge of the research on the biology of the bait polychaete species should
be to develop rearing techniques for intensive production that, increasing resource supply, would greatly reduce the
harvest impact on natural populations, associated organisms and biotopes.
ACKNOWLEDGEMENTS
We wish to thank Dr. P.J.W. Olive and Prof. D. Reish for their critical reading of the manuscript and die
usefull comments. Thanks are also due to Dr. R. Sarda Borroy for data on collection of worm bail species
along the Spanish coasts, and to Dr. C. COTTIGLIA for harvesting data on Diopatra cuprea cuprea in the Santa
Gilla lagoon (Sardinia, Italy).
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65
Polychaeta as a world resource: a review of patterns
of exploitation as sea angling baits and the potential
for aquaculture based production
Peter J. IV. OLIVE
Department of Marine Sciences and Coastal Management
University of Newcastle upon Tyne
Newcastle upon Tyne, NE1 7RU, United Kingdom
ABSTRACT
Exploited Polychaeta are drawn from several families notably: Arenicolidae, Glyccridae. Nereidae. Nephtyidac and
Eunicidae. Worms have been exploited as bait for sport and commercial fishing operations for generations but new
demands for polychaete biomass arise from the growth of the aquaculture industries for f infish and Crustacea. Several
types of exploitation can be recognised ranging from the collection of worms by spoil fishermen from local populations
primarily for their "own use", to highly organised collection on a commercial scale with nationally important economic
value. There is increasing concern about the environmental impact of both professional and amateur bait digging. Two
case studies where exploitation was in conflict with conservation proposals are discussed. They show that the
management of stocks for sustainable yield may be incompatible with conservation interests but some populations may
be amenable to effective management. Substantial fisheries for bait have developed in Korea, China, NE USA and, on a
smaller scale, in Europe to meet the demand for bait by sport fishermen. In Europe demand exceeds supply and both
importation and intensive aquaculture have developed to supplement the supplies taken from the natural environment in
european coastal regions; the management implications of these developments are discussed.
RESUME
Les Polychetes en tant que rcssources mondiales : revue dcs systemes d'exploitation coniine
appats ct potentie) pour une production par aquaculture
La majorite des polychetes d'interet economique sont des membres dcs families dcs Arenicolidae. Glyccridae et
Nereidae ; quelques especes appartiennent a I'ordre Eunicida. Depuis des siecles les vers inarins sont utilises comme appats
par les pecheurs professionnels el amateurs. Dc nos jours la demande s'intensifie en raison dc lessor dc la pechc de loisir
el du developpeinent de (’aquaculture dcs crustaces ct dcs poissons. Sexploitation dcs vers consiste dans leur recolte par
les pecheurs sportifs pour leur usage personnel et dans celle, bien organisee, eflectuee par les professionnels a des fins
commerciales ; la valeur economique de cette dernierc, lice a l'exportation sur les marches mondiaux. est loin d'etre
negligeablc au plan national. Ainsi sur les 1500 a 2000 tonnes de polychetes qu’utilise le Japon. la plus grande part est
iinportee. Mais la collectc des vers nest pas sans effet sur le milieu naturel ; a cet egard, les resultats de deux etudes traitant
des conflits d'interet entre exploitation et protection de l'environnement sont pnSsentes h litre d’exemple. Des centres de
Olive, P.J.W.. 1994. — Polychaeta as a world resource: a review of pattern of exploitation as sea angling baits and
the potential for aquaculture based production. In: J.-C. Dauvin. L. Laijbier & DJ. REISH (Eds), Actes de la 4eme
Conference internationale des Polychetes. Mem. Mus. nain. Hist. nat.. 162: 603-610. Paris ISBN 2-85653-214-4
Source : MNHN. Paris
604
P.J.W. OLIVE
production important, destines a satisfaire les besoins des pccheurs sporlifs, ont ete crees parliculierement en Coree. en
Chine, aux Etats-Unis el a une moindre echellc en Europe ou la demande depasse largement la production naturelle. Par
consequent raccroissement des importations et le developpement conjoint de 1'aquaculture s’averent indispen sables pour
alimenter le marche europeen.
INTRODUCTION
The Polychaeta play an important role in the ecology of marine communities partly clue to the diversity of their
structure and function. A relatively small number of species are also of commercial importance. This arises mostly
from their use as live bait in support of the sea angling industry which in some developed economies is the single
hugest participatory leisure activity. The Polychaeta arc likely to become increasingly important as a resource in
relation to the development of world aquaculture for Crustacea (Penaeidae) since it has been found that polychaetes
can provide a nutritionally correct balance of polyunsaturated fatty acids which are essential for egg maturation in
cultured prawns (LYTLE et ai, 1990) or can provide other factors essential for egg maturation (CROZ et aiy 1988).
The markets for Polychaeta have characteristics which give suitable live polychaete biomass particularly high
monetary value, considerably higher for instance than is obtained in most markets for human food.The value of
polychaetes varies of course between markets and like any commodity is also subject to short term fluctuations.
The price of ragwonns from the USA fishery in Maine rose sharply from mid 1950's and then remained relatively
high. The value in dollars per thousand worms to the Maine fishery increased from about SI 5 per thousand in 1960
to c.S38 per thousand in 1980. Greaser et al. (1983) and Greaser & Clifford (1986) give values for the Maine
(USA) bait worm fishery and CHOI (1985) discusses the value of Korean bait worm export markets. In general
whole sale values of $US 0.1 per specimen or 15-25 IJSS per Kg have been sustained over a number of years in
the USA and Japanese markets while values in die European markets appear to be even higher, current wholesale
values being in the region of S70 - $90 per thousand worms according to size. There is also evidence of substantial
added value in distribution and marketing.
In the scientific literature bait digging has been discussed primarily in relation to the potential impact on
marine communities. Greaser & Clifford (1982, 1986) and Greaser et ai (1983) however discuss the
characteristics of the Maine (USA) fishery and the population dynamics of die two bait species (Nereis virens and
Glycera dibranchiata) diat are exploited commercially in that fishery. Details of the life history of G. dibranchiata
in relation to die fishery were also provided by Klawe & Dickie (1957) and Simpson (1962).
There is no doubt dial bait digging is the cause of serious environmental disturbance (Cryer et ai , 1987;
Jackson & James, 1979; McLusky et ai . 1983; Van Den IIeiligenberg, 1987) but it would be wrong to
draw simplistic conclusions. There is a wide variety of bail digging activity ranging from the collection of bait by
individual anglers for dieir own use to fully organised professional activity. Each will have its own particular
effects on biological communities (see Olive, 1993 for discussion of two case histories).
The bail supply industry has a crucial role in the support of sea angling - a world wide leisure industry
including manufacturing and distribution of hard ware and many associated tourism and leisure time related
commercial activities - and in some economies it represents a very significant contribution to the local economy
(see CIToi 1985; Creaser et ai, 1983 for discussion).
The high price of die worms supplied to the sea angling leisure industry reflects the relative shortage and labour-
intensive nature of current supply routes. This paper will review the patterns of supply and consider the
management options and the potential for the application of aquaculture techniques to polychaete production which
would ameliorate die potential conflict between die market and the demands of environmental conservation.
PRINCIPLE POLYCHAETE BAIT SPECIES AND PATTERNS OF EXPLOITATION
The principle species of Polychaeta used as bail are listed in Table 1 together with the principle countries of
origin and known export destinations.
The most important species are the European lugworm ( Arenicola marina L.), the North American sand worm /
European rag worm ( Nereis virens Sars), die Korean blue ragworm ( Ferine reis spp.), Korean red ragworm
( Marphysa sanguinea) and the American blood worm (Glycera dibranchiata Elders). All of these species support
well established commercial fisheries diat have been sustained over several decades. Such fisheries can only develop
Source : MNHN. Paris
POLYCHAETA AS A WORLD RESOURCE
605
on substantial populations and the fishery frequently has an important role in the host economy. Management of
the fishery as a sustainable natural resource is then an important objective. The location of these major fisheries
for Polychaeta mid the distribution routes from them arc shown in figure l.Thc main routes of distribution are i)
from the South China Sea (Korea and mainland China) into Japan but with an increasing quantities being
transported from Korea to Europe and USA; ii) from NE Coast of USA (Maine) to Gulf States and California in
USA, and to Europe. Within Europe there is substantial distribution of ragworms from Northern coastal regions
(Netherlands, N. Ireland, Brittany) to the Mediterranean coasts and distribution from Venetian lagoon to southern
Italy. Since die worms are distributed live and used in the natural habitat there is a potential impact on the
geographical distribution of some species.
■ Marphysa sangutnea
▲ Aremco la marina
•> Per i nereis nun to var brevicirrus
□ Marphysa le idy i Onuphis teres
FlG. 1. Map showing some of the principle centres for the commercial exploitation of hail worms and the pattern of
distribution from them.
Choi (1985) gives values for the export of the two Korean bait worms. The peak export volume recorded was
in 1979 when some 900 metric tonnes were exported, most was sent to Japan, but 27.4 tonnes were exported to
France. The export of substantial quantities of material from this source to Europe has continued and exports to
Japan may have increased in recent years.
CREASER el al. (1983) discuss the economics of the Maine fishery and attempt to evaluate the catch per unit
effort. The analysis of the data suggests that die Maine bait fishery is restricted by limited entry and that the
optimal sustainable yield (OSY) can be related to the numbers of diggers for each species in the fishery. The
authors suggest that peak catch is at about 36 million worms (TV. virens and G. dibranchiata combined) per annum
representing the effort of "very roughly" 1,100 licensed diggers and representing the supply of c. 180 tonnes to the
world markets.
A similar analysis of major European and Far Eastern fisheries for bait worms is urgently required.
In addition to these Fisheries there is, in many countries, a long established tradition of collection of bait by
anglers for their own use and there is a gradual transition from this type of exploitation through ad hoc /
opportunistic commercial exploitation to fully professional digging for bait with organised distribution. Olive
(1993) investigated die impact of bail collection on local populations of bait species in conservation areas and
suggested a classification of bait collection that would take into account the marked differences between substantial
sustainable fisheries and other forms of collection (see below).
Source :
606
P.J.W. OLIVE
Three types of exploitation can be recognised :
- Type I. — Collection by anglers for their own use.
- Type II. — Collection by semi-professional bait diggers for ad hoc commercial sides.
- Type III. — Collection by professional diggers contracted to wholesaler/distributors.
Each type of bait collection will develop under different circumstances and will generate different management
problems but in general bait digging of Types I (own use) and Type II (ad hoc semi-professional digging) are more
likely to be directed at non-sustainable resources than Type III as discussed above. Conflicts between Types I and II
are to be expected. A particularly worrying development is die appearance of teams of itinerant professional diggers
targeting non-sustainable resources as is now happening in the South of England and elsewhere in Europe.
Type I exploitation — Anglers digging bail for their own use will only give rise to resource management
problems near substantial centres of population or in areas where there is inward movement of leisure anglers from
urban centres but in such areas the problems may become acute. In the UK a variety of measures have been taken
by local authorities and conservation agencies to restrict access for bait digging purposes in some beaches (Olive ,
1993). This may involve the designation of specific areas for bait digging. To be effective an accurate estimate of
both demand and sustainable yield is required but this information is not usually available to the legislators.
The most severe management problems are associated with die temporary use of resources by semi-professional
bait diggers for whom bail digging is not the main or sole source of income. In these circumstances the over¬
exploitation of resources may be severe. Since the exploitation is opportunistic there is likely to be chronic over¬
exploitation of dwindling stocks. When the return per unit effort falls below a profitable level the bail digging
pressure will be reduced and diggers will look elsewhere so that beaches will be subject to alternating periods of
depletion and subsequent recovery.
Olive (1993) described such a situation in NE England in which a designated area of an estuary (Budle Bay)
containing substantial population of the lugworm A. marina was set aside for bait collection. The project was
discussed in detail with a local Sea Angling Association and was designed to provide local anglers with access to
bait within a National Nature Reserve within which for conservation purposes bait collection would more
generally be restricted. The area set aside was substantial - approx 200 m x 2 km but it was totally deprived of
lugworms within six weeks of the onset of bait digging. It was estimated dial in this case some 4 million worms
were taken in this time. The management plan had seriously underestimated the predation pressure on die beach
most of which could be classified as Type II semi-professional ad hoc collection for commercial outlet and not
demand by local anglers.
Inevitably access to the bail stocks within this part of the Nature reserve was prohibited and diere was rapid
recovery of die population to normal levels once severe exploitation ended.
1 his case study reveals features in die life history and recruitment of die lugworm Arenicola marina dial would
encourage the development of management techniques in sutable areas. The juveniles of die lugworm A. marina
occupy nursery areas physically separated from dense populations of adults (Beukema & de Vlas, 1979; Newell
1948, 1949; Olive, 1993). Moreover in the area studied by Olive (1993) die adults exhibited a high degree of
mobility and substantial numbers of adult worms migrated into die depleted areas from unexploited neighbouring
tracts of beach within a few weeks of the ending of bait digging. The observations suggest that a system of
progressive exploitation ol areas alternating with periods of recovery from reserve areas could be an effective
management technique for this species on extensive tidal sand Hals.
Similar management techniques seem to be effective for die Type Ill commercial fishery for Perinereis and
Marphysa in Korea where the tidal flats arc divided into rectangular areas which are only dug over once each year
(Choi, 1985).
Whereas huge extensive intertidal flats may be managed in this way such techniques are not appropriate for
smaller pocket beaches. In such cases a judgement is required about die relative importance of bait collection, die
requirements ol oilier users of a beach and the importance of the beach fauna for conservation and educational
purposes. Such value judgements can only be made by careful and sympathetic consideration at a local level.
Consideration must also be given to die population structure of die exploited species and important differences
may be revealed between exploited and non-exploited populations. Braeield & Chapman (1967) demonstrate the
dramatic change in weight frequency in a natural population of N. virens before and after the breeding season.
These are semelparous worms and the data suggests that virtually all animals breed and die in the second or (fewer
worms) third year of life. After the breeding season the population is dominated by 1-group worms 3 and 1 lg in
weight. The population structure of die worms caught by the summer Maine fishery is exactly comparable
(CREASER et al ., 1983). In contrast the population of this species exploited by anglers in North wales (Menai
Strait) was still dominated by much larger worms up to 60 g weight even after the breeding season (Olive, 1993)
Source : MNHN. Paris
POI .YCHAETA AS A WORI .D RESOURCE
607
and in this beach the worms appear to live much longer. The rate of entry to the fishery will be smaller and the
OSY consequently much lower. The Menai Straits population could not therefore sustain a substantial fishery.
Table 1. — Principle Polychaele bait species, countries of origin and export destinations.
I. Production from wild stocks.
Studies of the population structure of exploited populations of bait worms suggest that only in relatively few
areas are conditions suitable for a sustained fishery. The value of bait worms in world markets suggests that these
fisheries alone are not able to meet all the demand.
THE ROLE OE AQUACULTURE IN PROVISION OF BAIT SPECIES
The last 20 years has seen the phenomenal growth of aquaculture for crustaceans (LEE & Wickins, 1992).
Current EAO statistics suggest sustained development of this sector at about 18 % pa to give output by 1988 in
excess of 200,000 metric tonnes. Could the development of aquaculture for bait species similarly alleviate the
problems caused by the excess of demand over the Optimal Sustainable Yield of bait fisheries ? The problem is
Source
608
P.J.W. OLIVE
Particularly acute in Europe where by far the greatest bait fishery effort is directed at 11011-sustainable resources and
where bait collection ol I ypes I and II may service die greater part of the use of bait by leisure anglers.
Since one ol die objectives of the development of an aquaculture system would be alleviation of environmental
pressure it is important that the aquaculture should be fully intensive ic it should have the following elements :
i) Specific holding facility;
ii) Self contained brood stock and larval rearing system;
iii) Artificial diets.
Lully intensive aquaculture now contributes to Far East and European markets aldiough the quantities be i ire
pioduccd are small m relation to die market. In Taiwan approximately 25 tonnes of die nereid Perinereis brevicirrus
are produced annually lor export to Japan by fewer dian 10 small farmers (CHEN, 1990) mid small farms produciire
Perinereis arc also found in southern Japan. °
I he development of polychaete culture in Europe has been driven by perceived commercial opportunity aid a
number of enterprises have been initiated notably in Netherlands and in the UK but dicre are no published accounts
of dieir success, most are not thought to have established viable economic activity but one in NE Em-laid (sec
below) is now making a significant contribution (15 tonnes in 1992/3) to UK supplies of ragwonn and expansion
ol this source material is expected.
A major problem in the aquaculture of Perinereis brevicirrus arises from the life history characteristics of this
species. It is a semelparous annual; breeding occurs in late March aid juvenile worms do not reach market size
(minimum 1 g) until September. Since the principle market demand in Japan is between May and October these
lw° montlK of “* s®so” “d ca” onlJ' represe“ * “«*»« 10 a
In l9e19. Ihe University of Newcastle upon Tyne (UK) began a research progranme to select a suitable bait
spcucs toi intensive aquaculture in Europe and to establish the operational parameters that would permit economic
bait production In 1986 the partly developed technology was transferred to the private sector for further
development I his initiative has now established an economically viable production site for the bait worm N.
vnens on the North East Coast ol England. Modern distribution methods mean that a single production site can
i's'deinant! ° ^ K WlUMn 24 hfS and “ is clear tllal a sin8le production site can supply bait wherever there
Intensive aquaculture provides a means of supplying the specific market for live baits without recourse to
predation of natural stocks and with little adverse environmental effect. The production system operatiire in NE
England makes use ol power station effluent and supplies the market throughout Ihe year. The introduction of
SK" "xn-mJ hs^wk1 beC,rT "f c"!husiasm * user and the specialised trade literature m.d is
Inhinis^ nSTfsi r ? ,S pr0dutls Wlli inevi,ab,y compete with those derived from natural
o re U ve Y ,'VC a SUlhlllS,"S in,luencc 011 Ulc ,narkcl P'ice for bt.it worms. This in turn will help
0,1 m environment that arise from the demand for bait in support of the leisure
RISKS ASSOCIATED WITH AQUACULTURE OF BAIT SPECIES
hi^SS^KS'r bUS,ineSSeS '"C aquacnl,urc of Pclycl.ae.cs for use as bait must be perceived as a
nackinc faci eO , " , °C Prf UCt,0n C0S,S assoc,aled wi,h caPi,al Provision (brood tanks harvesting and
SSS SftSS ““““8 “W* — 1™. — risks associated with loss of stock
The Newcastle University/Seabait Ltd project has revealed the existence of previously unrenorted nadiooens
« Sed1^:^ and hU'“y pmcedurcs bu‘ ^ couk, cause sever? losses in
wilh? n^ClnC,°n|dUK)n p,rw.f°"ally n;uncd Tenlade Wasting Disease (Olive & McGrath, in prep) is associated
a flagellated vibrio cl O brio parahaemolylicus . This condition causes ;t progressive loss of die sensory or-ans
n , ion t eventually to abnormal behaviour and death. The condition can be induced in laboratory cultured by
kmged exposure to adverse conditions and can achieve epidemic proportions. A number o odie pecific
^ been discovered including a specific anaemia and a condition resulting in S
, ons. As all forms of aquaculture die effectiveness of management techniques in avoiding conditions which
Source : MNHN. Paris
POI .YC MALTA AS A WORI ,D RESOURCE
609
encourage the ousel of pathogenenicily in organisms usually present but benign will he of paramount importance
in the economic viability of systems of worm culture.
OPPORTUNITIES ARISING FROM THE CULTURE OF BAIT WORM
The development of a viable system for aquaculture of bail worms in NE England establishes a new source of
biological raw materials. The culture of bait generates a specific biomass with properties known to be valuable in
the support of other forms of aquatic production. The worms have a high proportion of unsaturated fatty acids
PUFA and the specific long chain PUPA known to be essential in the diets of marine Crustacea arc present (Olive
et al., 1992). These fatty acids contribute to the viability of artificially reared Penaeidae (Lyttle el al., 1990;
Middleditch el al., 1979, 1980; Kanazawa el al., 1979) and a new source of materials in suitable form is
likely to have a beneficial effect if incorporated into the diets of brood slock prawns.
The development of Nereis virens aquaculture establishes in effect mass cultures of worms of known parentage.
Johns el al. (1989) have established that the growth rate of Nereidae can form the basis of a useful sediment
bioassay. The value of this technique is currently under investigation in collaboration with Seabail Ltd. a private
company who have developed techniques for cryopreservation of larvae. The growth of very young (4 - 6 setiger
stage nechtochaetes) is easily quantifiable from segment proliferation rates and the growth rate of commercially
available cryopreserved nechtochaetes (Seabait Ltd) is not significantly different from that of fresh unfrozen larvae
under a variety of different test conditions when measured in this way (Olive & Lang, in prep).
The development of mass cultures of genetically uniform stocks and the application of cryopreservation
techniques to juveniles should assist in the development of international sediment bioassay protocol.
CONCLUSIONS
Polychaeta have their greatest economic value as bait in support of the leisure Sea Angling Industry. There
appear to be relatively few places where a substantial commercial fishery can be sustained over decades.
Consequently the price of suitable bait species is high and this leads to two consequences :
i) A large number of Sea Anglers dig their own bail from intertidal beaches;
ii) There is a substantial semi-professional exploitation of intertidal populations that frequently
exceeds the sustainable yield.
In Europe there is evidence of increasing concern at the effects that such ad hoc bait digging has on beaches that
are used for other recreational purposes or which lie in conservation areas.
The recent advent of commercially viable operations for the production of Polychaeta in self contained fully
intensive aquaculture will help to alleviate price driven over exploitation of limited resources. At present cultured
worms are perceived by some sections as offering definale advantages over die wild caught supplies tuid the average
price of cultured worms in the UK may be higher than dial of comparable worms taken from die wild.
There is a clear need for further studies of the dynamics of populations subject to different types of collection
pressure. Some sites should be managed to sustain the Optimum Sustainable Yield. Local controls to regulate die
exploitation of more limited slocks may be necessary especially where dieir is a clear conflict of interest.
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ClIEN. Lo chaH. 1990. Aquaculture in Taiwan. Fishing News Books: Oxford. 273 pp.
Choi. LIT. 1985. Lugworms - from harvesting to exporting. Infojish marketing Digest. 6/85 : 49-52.
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estuary, Maine USA. Fish. Bull.. 80 : 735-743.
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Cryer. M., Whittle, G.N. & WILLIAMS. R., 1987. — The impact of bait collection by anglers on marine intertidal
invertebrates. Biol. Conserv 42 : 83-93.
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of commercial and applied interest in Italy: an overview. Mem. Mus. natn. Hist. nat.. 162 : 593-601.
JACKSON, M.J. & James. R.. 1979. — The influence of bait digging on the cockle Cerastoderma edule . populations in
North Norfolk. J. App. Fcot.. 16 : 671 - 679.
Johns. D.M.. Ginn, I.C. & Reish. D.J., 1989. The effect of contaminated sediments on the growth of the Polychaete
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effects of docohexaenoic acid on growth. Bull Jpn. Soc. Sci. Fish., 45 : 1151 -1153.
Klawe. W.L. & DICKIE. L.M.. 1957. — Biology of the bloodworm Glycera dibranchiata. Bull. Fish. Res. Bd.. Canada.
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LeeD. O'C. & WICKINS. J.F.. 1992. Crustacean farming. Blackwell Scientific Publishers : Oxford. 392 pp.
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Source : MNHN. Paris
ABSTRACTS
RESUMES
MORPHOLOGICAL AND GENETIC DIFFERENTIATION OF HEDISTE DIVERSICOLOR AND NEANTHES SUCCINEA
POPULATIONS IN IIIE MEDITERRANEAN SEA. ABBIATI, M. — (Dipartimento di Scienze dell'Ambiente e del Territorio
University di Pisa. Via A. Volta 6. 1-56 1 26 Pisa, Italy). — Hedisie diversicolor, like many other brackish water species,
shows a high degree of morphological variability (MOUS, 1967a). The variation in the numbers of paragnaths on the
eversible proboscis is the most studied morphological parameter in H. diversicolor (MOUS, 1967b; COGNETTI VaRRIaLE,
1973; BARNES & Head. 1977; Barnes, 1978; Khlebovich et ai, Gillet, 1987, 1990; Abbiati. 1989. 1991; ABBIATI &
COGNETTI VARRIALE, 1990; IlATELEY el ai, 1992). The observed inlerpopulalion differences in H. diversicolor have
prompted speculations that there may be isolated races in this species (MOUS. 1967a). In order to obtain information on
the level of intraspecific differentiation in H. diversicolor and to relate it to the level of interspecific differentiation, a
study has been made of the morphological variation and genetic structure of three H. diversicolor and one Neanlhes
succinea populations, all collected along the Italian coasts. About one hundred individuals from each population were
examined. The morphological character chosen for observation was the number of proboscis paragnaths, both in each
group and on the whole. Differences among mean number of paragnaths present in each group of the proboscis were
evaluated by Tukey's test to verify the level of significance. On this basis it was possible to recognise only two
discriminant groups for all populations. In fact the eight proboscis groups are a useful tool for nereidids taxonomy, but
they do not correspond to the functional unity of the proboscis (Abbiati. 1989; IlATELEY el ai . 1992). Looking at the
total mean number of paragnaths of each population, significant differences between all populations were pointed out
Hierarchical relationships between all populations, based on the differences in the total mean number of paragnaths were
defined. Genotypes were analysed by means of isozyme electrophoresis on cellulose acetate membrane. Fifteen enzyme
systems were investigated; 17 and 21 loci were scored in H. diversicolor and N. succinea respectively. The percentage of
polymorphic loci (0.99 cutoff criterion) and the mean number of alleles for the studied populations ranged from 23.5 % to
47.1 % and from 1.38 to 1.588 respectively. Comparison between H. diversicolor samples revealed that the populations
are heterogeneous. Nei’s identity and distance indices measure the relatedness of populations and species and are based on
allelic variation at each locus (NEI. 1987). Genetic distance between H. diversicolor populations ranges from 0.272 to
0.351 and reveal that pairs of populations were significantly different from one another. The values found are those
typically associated with local populations (NEI, 1987). Hierarchical relationships between all populations, based on
genetic distance values were defined. The morphological and genetic distance between H. diversicolor and N. succinea w'as
used as references for the respective scales. Comparison of the two dendrograms reveals a high degree of correspondence
between the genetic and morphological differentiation levels. This result confirms the validity of the hypothesis
proposed by many authors, based on morphological data, about phenomena of differentiation among H. diversicolor
populations.
SPATIAL DISTRIBUTION OF POLYCI IAETA IN HARD-SUBSTRATE IN TI IE NORTHERN LITTORAL OF CAP DE CREUS
(SPAIN, NW MEDITERRANEAN). ALOS, C. — (Departament de Biologia Animal, Universitat de Barcelona. Diagonal.
645. 08028 Barcelona, Spain). The polychaeta associated with hard substrate was studied in the northern littoral of
Cap de Creus (NW Mediterranean) from 1981-1985. in the context of a general bionomic study of this zone (Programa de
Bentos Cap de Creus). Starting from these data, it has been possible to establish a relationship between polychaeta
populations and the environmental conditions which determine their spatial distribution. Ninety-one samples were
studied from the main facies of this littoral, in which the three bionomic levels were included: surface facies with strong
hydrodynamics (mediolittoral and upper infralittoral levels), photophilic algae biocoenose. P. oc.eanica beds,
precoraligenous communities and coral igenous biocoenose. However, the high number of polychaeta species identified
(235). the disparity in their appearance frequencies and the ambiguity in their ecological requirements make it very
difficult to associate any species with a determinate bionomic level. In order to study the spatial distribution, different
cluster analysis was made between samples and also between species, with the purpose of assigning to each group of
species the ecological characteristics of substrate with which they are related. Results show that the high variety of facies
appearing in hard-substratum does not correspond to characteristic populations of polychaeta. They are distributed
according to microhabitats that are often the same in facies under different general conditions. The different populations
612
ABSTRACTS - RESUMES
of polychaeta in this zone can be associated as follows: 1. Species from surface facies with strong hydrodynamics:
Lepidonotus clava, Eulalia viridis, Grubeosyllis vieitezi , Syllis prolife ra, S. arnica, Fabricia sabella. 2. Species
associated to calcareous concretions from calm environments: Lysidice ninetta, Xenosyllis scabra, Syllis ferrani.
Autolytus sardai, Opisthodonta morena, Polydora flava. 3. Species from sciaphi lie environments independently of
substrate: Harmothoe spinifera, Pholoe minuta, Sphaerosyllis pirifera, Pionosyllis lamclligera, Fabriciola cf bahica. 4.
Species from environments with a high degree of sedimentation (P. occanic.a rhizomes and cavities could be filled up by
sediment): Parapiono syllis brevicirra, Ehlersia ferrugina, Exogone rostrata. Prionospio cirrifera , Kefersteinia cirrata .
Sphaerosyllis brevicirra. 5. Species with imprecise ecological requirements or with a high degree of cosmopolitisme.
They are preferently located in the photophilic algae biocoenose and P. oceanica leaves: Exogone naidina, Grubeosyllis
clavata, Odontosyllis gibba, Pionosyllis serrata.
GAMETES, FERTILIZATION AND DEVELOPMENT OF PHERUSA SP., AN ENDOLITHIC WORM (POLYCHAETA.
FLAB E L LIG ER I D A E) . AMOR. A. - (Instituto de Embriologia Biologia e Ilistologia, calle 60 y 120 1900, La Plata,
Argentina). The polytclic worm Pherusa sp. is a gonochoric animal inhabiting hard substrates. Males and females
could only be recognized during the reproductive season: the body of the males is white and that of the females green. In
the laboratory, both sexes spontaneously spawn in seawater leading to normal fertilization. The eggs are green in colour
and inesure about 140 pm in diameter. The spermatozoa are of primitive type. After fertilization the egg shows evident
morphological changes of the surface and the pattern of the egg development is clearly spiral. The two blastomeres
resulting from the first cleavage express differences in colour. AB is green and CD is white. All the egg pigment is
concentrated in the small cell. The development is indirect comprising a larval pelagic stage, a pelago-benthic stage and
a benthic stage. The pelagic and pelagobenlhic stages develop in seven days and the larvae are lecitotrophic. A terminal
organ appears in the pelagic larvae which becomes retractable and which secreted adhesive substances at the end of the
pelago-benthic stage. Early in the pelagic development a dorsal depression appears indicating the location of the future
anus. The mouth and the anus are both functional at the begining of the benthic life of the larvae. On the head, a pair of
palps appear and there is an increased number of eye spots. The number of branchiae behind the head and the appearance
of setae, different to those of the adults are the most notable. During all larval development new characters appear, with
only the loss of the pelagic cilia of the larvae.
THE IMPACT OF FISHING HARBOUR CONSTRUCTION ON THE DENSITY OF BENTHIC POLYCHAETES OF THE
COLEROON ESTUARY ON THE SOUTHEASTERN COAST OF INDIA. Ayyakkannu, K. — (Centre of Advanced Study in
Marine Biology, Annamalai University, Parangipettai. 608502 Tamilnadu. India). A fishing harbour was constructed
in the Colero on estuary (1 1 °2 1 *N. 79°50'E) on the southeastern coast of India during the years 1985-86 to accommodate
about 300 fishing vessels. A quantitative benthic survey of polychactes in this region was made in the years 1985-86 and
1986-87 during construction and after the fishing harbour started functioning and the data obtained on the population of
these polychactes was interesting for they throw light on the effect of dredging on these organisms. Evcnthough the
total number of species did not show great variations when compared to the earlier report from this region (JEGADEESAN,
1986). a reduction in the number of polychaetes was found. In earlier reports, 35 species of polychactes were counted
whereas 32 species was recorded during the construction and 29 species arc recorded after the fishing harbour started
functioning. The total number of polychaetes recorded was 174 ind. m'2 during harbour activities; 224 ind. m*2 after
construction against 680 ind. m ~ reported earlier. The following species were dominant: Nephtys polybranchia,
Ancistrosyllis constricta, Heteromastus similis, Lumbriconereis simplex, Ccratonereis costae and Prionospio pinnata.
However, these species though present, were found in a lesser number during and after the construction of the fishing
harbour. The earlier report found Ancistrosyllis constricta as highly dominant species (68 ind. nr2), but the present study
revealed that the numerical abundance of A. constricta was poor compared to its associate species Nephtys polybranchia.
From this, it is inferred that A. constricta proves to be a sensitive species and is unable to withstand even a slight
disturbance of the substratum compared to N. polybranchia. The impact of dissolved oxygen concentrations, nutrients,
salinity, temperature and sediment texture on the density of the polychaetes is discussed.
MONITORING THE GROWTI 1 OF SABELLAR/A ALVEOLATA IN THE FIELD. B amber. R.N. & Irving . P. W. (FAWLEY
aquatic research laboratories Ltd. Marine & Freshwater Biology Unit. Fawley. Southampton S04 ITW, UK). — An
extensive population of the reef-building worm Sabellaria alveolata (L., 1767) exists in the Severn Estuary, southwest
Great Britain, predominantly sublittorally and concentrated around the 20 m isobath. Significant littoral colonies occur
on the rocky foreshore of Ilinkley Point, Somerset, at and below 2 m above Chart Datum. Fwo nuclear power stations,
Hinkley Point A and B . are sited on this headland. The discharge canal for the power station cooling water crosses the
shore, allowing heated water from the outfall to flow across the rocks near low water mark. Water temperatures here are up
to 10 °C above ambient. I he individual units of S. alveolata reef growing within the How of the cooling water effluent are
substantially larger (by 5 to 10 times the volume) than reef units elsewhere on the shore. Hypotheses to account for this
difference arc: 1. More individual worms per unit area at the outfall. Analysis of quantitative core samples of outfall and
control reefs showed that, if anything, the worms are less dense at the outfall site (8,000 ind. in'2 compared to 13.000. in'
- at control areas). 2. I he worms at the outfall are not S. alveolata. Morphologically, the worms are S. alveolata; they arc
not S. spinulosa Leuckarl. 1849. 3. Greater longevity of the reef units at the outfall. We do not know how to age a
RESUMES - ABSTRACTS
613
Sabellaria reef: the worms are of identical size ranges at outfall and control sites. 4. Faster growth of worms or tubes at
the outfall. Potential causes of differential growth are (a) a response to the greater water temperature at the outfall
(although the worms themselves are no larger at the outfall site; however, winter growth or activity may be enhanced) or
(b) increased input of material from the effluent flow (although at LWST turbidity is greater at the control site). We are
currently investigating this possibility. The main work to date has been determining a suitable technique for non¬
destructive monitoring of reef growth in the field. We have tested four methods: 1. In situ volumetric displacement. Reef
units were enclosed in a bottomless bin. lined with a plastic bag which was then filled with water: the weight of the water
pressed the plastic closely to the reef, the bedrock and the bin sides. The difference between this volume of water and the
volume of the bin was a measure of reef volume. In practice, errors on replication were up to 100 %! This method was
rejected. 2. Frame-grid measurement. A cage of rigid plastic mesh supported around a tubular frame, and of known
dimensions, was lowered around the reef, and measurements were made normally from each of the 5 cm interval
intersections of the mesh to the reef face (top or side: the reef base is flat on the rock so can be reasonably assumed to be
0 cm above the frame base). A computer program calculated the volume of the subtended rectangular cuboid from the mean
reef dimensions. Modelling tests on this technique suggested that it may underestimate the reef volume by ca 5 %; errors
between replicates were commonly of the order of 10 %. This method was laborious, and was rejected. 3. Photography. In
a manner not dissimilar to method two in its logic, photographs of marked reef units were taken from four sides (N. E, S.
W) and the cross-sectional areas calculated. From these, the volume of the subtended rectangular cuboid was calculated.
This procedure inevitably overestimates the volume. The data will be retested assuming the reef to be an oblate
hemispheroid. but these results will still be prone to error owing to the irregular shape of the reef units. However, with
the comparative ease of this technique, we are persisting with it in comparison to method four, to determine its
suitability for more general use. 4. Displacement of detachable reef units. Individual reef units of ca 1.5 litres volume
have been detached from the rock and mounted on plywood panels using an epoxy resin (WRA System 22). Previous
laboratory tests had shown that this adhesive would cure under seawater, would adhere to the reef material after minimal
drying, and when cured was stronger than the mucopolysaccharide adhering the reef grains. Larger base panels. 60 x 60
cm, were fixed to the shore bedrock using 10 cm silicon bronze screws. The panels bearing the reef units, after 24 hours
curing in a rock pool on the shore, were screwed to these base panels. On each visit to the site, the units can be removed,
their volume measured by direct displacement in a bin of sea-water, and they are then reattached to the shore to grow on.
The 13 deployed reef units have survived intact for six months to date. The error margin between replicates (standard
deviation) was 3.5 %. Not only is this method satisfactory and beginning to give results, it has allowed us to deploy
control-site units at the outfall and vice versa. In conclusion, the technique of volumetric displacement of detachable reef
units gives results of sufficient accuracy to detect growth. The complex initial preparation suggests that photographic
analysis is worth further investigation, cross-calibrated with the displacement method, as it would prove convenient for
use at other sites and involves less lime on the shore.
THE ECOPHYSIOLOGY OF HED/STE (NEREIS) DIVERSICOLOR 0. F. MULLER (POLYCHAETA) IN THE BAIE DE
SOMME, FRANCE. Batten, S.D, Hawkins, L.E., Hutchinson, S.. Desprez, M., Rybarczyk, H.. Paterson, G.L..
Lambshead, P.J.D. & Ducrotoy, J.P. — (Southampton University Department of Oceanography. Southampton, S09
5NH, U.K.). Hediste (Nereis) diversicolor has a wide distribution in the intertidal areas of the Baie de Somme estuary.
The polychaete has been sampled from two sites for a 12 month period, one site being relatively more disturbed. The
population fluctuations have been studied from quantitative core samples sieved through a 0.5 mm sieve and fixed with
4 % formalin. Individuals were also frozen in situ in liquid nitrogen for physiological assay. The physiological
components that have been measured are total lipid, carbohydrate and protein and the metabolites ATP. ADP. AMP.
glucose, glycogen and creatine phosphate. Correlations between the population studies and the physiological assays
have been made and provide much information on the reproductive cycles of this polychaete. Differences in the
physiology and reproductive ability of the populations at the two sites have been noted. Further investigations to
confirm the effects of the disturbance have been proposed.
SOME OBSERVATIONS FROM THE POLYCHAETA TO AID UNDERSTANDING OF THE RELATIONSHIP BETWEEN
LARVAL DISPERSAL AND THE GEOGRAPHIC BOUNDARY OF SPECIES. BllAUD, M. & MARCANO, G, (Observatoire
Oceanologique de Banyuls, Laboratoire Arago, 66650 Banyuls-sur-mer. France). It is not definitively clear whether
species whose life history includes a planktonic larval stage will have as a consequence a larger distributional area than
species lacking such a free drifting stage. The present contribution to this problem bears on five points: 1. definition of
a non-biaised sample; two approaches are possible: the selection of isolated examples with well known area boundaries,
preventing generalizing of results, or the selection of a large number of species correctly defined in terms of geographic
distribution and reproductive strategies but occupying necessarily a heterogeneous environment which may obscure the
relationship between larval dispersion and distributional area. 2. correct larval identification: a large amount of work is
still needed as conclusions about geographic distribution drawn from family level identifications are not pertinent to the
question of larval flow which must be examined at a lower systematic level. 3. modulation of larval life duration in terms
of latitudinal position of the observation and larval behaviour with active or passive displacement in the face of physical
oceanic structures are two additional elements determining the dispersal area of a species. 4. data on molecular population
genetics of marine organisms must be discussed in order to include life style, population size, potential gene flow (larval
614
ABSTRACTS - RESUMES
life) and environmental factors. 5: the model of a geographical boundary (Mesochaetopie rus minuius, Chaetoplcridac)
shows the displacement between larvae and adults distribution, opens the possibility of pscudopopulations and probably
renders to the benthic stage the key for the determination of the specific geographic range. It is concluded that
distributional range is not accounted for by the inherent dispersal capacities related to larval type: such a conclusion
raises the question of the meaning of a dispersal stage within the life cycle.
HIGH POLYCHAETE DIVERSITY IN THE DEEP SEA: HOW MANY SPECIES? Blake, J.A. & Hu. BIG, B. — (Science
Applications International Corporation. 89 Water Street, Woods Hole. Massachusetts 02543. U.S.A.). Recent studies
on benthic infaunal communities in the western North Atlantic have revealed a remarkably high species diversity.
Approximately 1600 species of benthic invertebrates were discovered in 550 quantitative box cores taken on the
Canadian boundary to off South Carolina in depths ranging from 250-3,500 in. An equally rich infauna of approximately
600 species has recently been discovered from 67 box cores taken on the continental slope off northern California in
depths of 550-3.100 in. In both of these studies polychaetes accounted for 45-48 % of all species, with 53 % of the
Atlantic and 51 % of the California species being new to science. For some families from the western North Atlantic, the
proportion of new species to known species was high: Capitellidae (29/35: 82 %), Chrysopetalidae (9/10: 90 %),
Cirratulidae (33/40: 82 %). Dorvilleidae(28/34: 82 %). Hesionidaef 1 1/15: 73 %), Orbiniidae (17/24: 70 %). Oweniidae
(17/20: 85 %). Paraonidae (30/49: 61 %), Phyllodocidae (23/37: 62 %). Sabcllidac (15/24: 62 %). Spionidae (62/80: 77
%). Syllidae (16/22: 72 %). and Terebellidae (21/25: 84 %). The total area sampled was 49.5 m2 on the Atlantic slope and
6.7 nr in California. When considered in the context of the vast continental margins and ocean basins on the planet, the
area covered by these samples is insignificant, but docs provide an opportunity to estimate the potential richness of
polychaete genetic diversity. In the most homogeneous region of the U.S. continental slope off Delaware and New
Jersey, GRASSLE and MaCIOLEK (1992) demonstrated that rates of species accumulation in 233 pooled box cores never
leveled off. When taken in the context of the more heterogenous environments off New England and the Carolinas and the
relatively small total surface that has been sampled in 550 box cores, the potential number of species of polychaetes
actually present on the continental slope of the U.S. Atlantic is greatly underestimated. The data that are accumulating
from the eastern Pacific from a fewer number of samples suggest that an equally high rate of species accumulation occurs
with repeated sampling. These findings support the conditions of GRASSLE and MaCIOLEK (1992) that the deep sea
contains a vast reservoir of species richness. When taken in the context of the size of the unexplored continental
margins and ocean basins, the high percentage of polychaetes in benthic assemblages, and rates of species accumulation
with repeated sampling, it is possible that the total number of polychaete species in the deep sea may lie somewhere
between 450.000 and 4 millions. A great genetic reservoir of polychaete diversity thus occurs in the deep sea. Some
species have been determined to have broad geographic and depth distributions and this may serve to reduce these
estimates. Nevertheless, even with a 50 % reduction, the remaining totals are far in excess of the numbers of presently
known polychaete species.
BENTHIC MACROFAUNA AND POLYCHAETES FROM AN EXPERIMENTAL AREA IN THE DEEP PERU BASIN (SE
PACIFIC). BOROWSKI, C. — (Zool. Inst. & Mus. Univ. Hamburg. Martin-Luther-King-Pl. 3, D-2000 Hamburg 13,
Germany). — During the Disturbance and Recolonization Programme (DISCOL) of the Institut fur Hydrobiologic und
Fischereiwissenschalt (IHF-IIamburg, Germany) a disturbance experiment was operated on the bottom of the Peru Basin,
in a water depth of 4.150 in. Several boxcore samples were taken before and after the disturbance in a circular
experimental area with a diameter of two miles. The samples were sieved with 1,000 pm and 500 pm mesh size and
investigated quantitatively for sediment-dwelling macrofauna. Preliminary results from some selected undisturbed
samples show that the majority of the infaunal animals is of a very small size that passes through the 1.000 pm mesh.
More than 70 % are living in the uppermost 2 cm of the sediment, only about 5 % being found underneath 5 cm depth.
The polychaetes make up the major element of the macrofaunal community (about 50 % of all animals), followed by
isopods and tanaids (about 15 % each). Within the infaunal Polychaetes 78 species belonging to 34 families occurred.
The highest numbers of species were found within the families Opheliidae (9), Syllidae (7), Spionidae (6) and Cirratulidae
(5). Only lour species were abundant enough to appear in nearly every sample (one Pilargiidae, one Paraonidae, two
Spionidae): most of the others are rare. The hard substratum of the manganese nodules represents another common
polychaete habitat. A total of 17 species (one Ampharetidae, 14 Serpulidae and two Spirorbidae) living on the nodule
surfaces could be distinguished. Additionally, 12 infaunal species were found living in the nodule crevices. Six of them
did not occur in the sediment samples.
PRIONOSPIO CASPERS I LAUBIER (POLYCHAETA. SPIONIDAE) IN THE BLACK SEA: ECOLOGICAL NOTES. BRTTAYEV,
l .A.. CASTELU, A., AKSIUK. T.S. & SEVERTZOV, A.N. — (Institut of Evolutionary Animal Morphology and Ecology,
Russian Academy ol Sciences. Moscow, 117071. Russia). Numerous specimens of the spionid polychaete Prionospio
caspersi Laubicr. were found in the benthic samples from Kapsel Bay (on the southeastern coast of Crimea). This was the
lirst record ol this species in the Black Sea. P. caspersi is very abundant in sandy or silty sand communities at depths of 9
to 23 m in which the bivalve Chamelea gallina predominates. We have studied the density of population and frequency of
occurrence of this species from 1986 to 1989. Density varied seasonally. It was highest in Spring (up to 730 ind. m*2)
and fall decreased in August-September (to 96 ind. m2). The maximum density was about 2.440 ind. nr. The frequency of
Source : MNHN. Paris
RESUMES - ABSTRACTS
615
occurrence in grab samples varied from 53.6 % to 100 % and also declined at the end of summer. This data was in
agreement with that of AMBROGI concerning the annual life cycle and the beginning of settlement in the last half of
summer. In 1989. P. caspers i completely disappeared from benthic samples from Kapsel Bay and was replaced, as the
dominant species, by the pardon id Aricidea (Allia) claudiae Laubier.
PELAGIC POLYCHAETES FROM EL HIERRO (TFMCBM/91) IN THE CENTRAL- EAST ATLANTIC. BRrro, M. C.. NUNEZ,
J. & BARQUIN, J. — (Departamento de Biologia Animal (Zoologia). Universidad de la Laguna. 38206 La Laguna, Tenerife.
Canary Islands, Spain). Seventeen quantitative plankton samples from the island El Hierro (Central-East Atlantic
Ocean) have been studied: in sixteen of them pelagic polychaetes have been collected. From a total of one hundred and
one specimens, seventeen species of polychaetes were identified. One of these unidentified species, genus and family.
Furthermore, five species were recorded for the first time in the Canary Islands (Tomopteris nationalis . T. euchaeta,
Lopadorrhynchus henseni, Vanadis minuta and Rhynchoncrella petersi). Details are given about the density and frequency
of the species, as well as a biogeographical analysis of them.
TRANSPORT AND SURVIVAL OF I .ARVAL POI .YCI IAETES IN BAI .LAST WATER OF OCEAN-GOING VESSELS H EADED
FOR THE GREAT LAKES. BYERS. S.C., LOCKE. A. & BllAUD, M. - (Royal Ontario Museum, Department of Invertebrate
Zoology. 100 Queen's Park. Toronto, Ontario. MSS 2C6, Canada). — Great Lakes Ballast Water Control Guidelines were
established by the Canadian Coast Guard in 1989 to minimize introductions of exotic species into Great Lakes
ecosystems. Such introductions, including the zebra mussel, Dreissena polymorpha, have been attributed to
intercontinental transport in the ballast water of ocean-going vessels. According to the guidelines, ships destined for the
St. Lawrence Seaway and Great Lakes voluntarily replace all water ballast taken on in fresh or brackish areas with mid¬
ocean water. The rationale for mid-ocean exchange is that theoretically the freshwater and coastal organisms would be
Hushed out or killed by the water from the high seas. A study was launched in 1990 to a) determine the compliance of
inbound ocean-going vessels with ballast water exchange guidelines, and b) to establish the effectiveness of open-ocean
exchange of ballast water in reducing or eliminating the presence of limnetic and estuarine organisms in ballast water
discharged in the Upper St. Lawrence River and Great Lakes. Compliance of vessels with the guidelines was 95 % (all
vessels) or 89 % (excluding vessels not carrying ballast water). Effectiveness of mid-ocean ballast water exchange in
eliminating live freshwater zooplankton from ships originating in freshwater ports was estimated to be 67 %. Twelve
phyla of zooplanktonic organisms were identified from ballast tank samples, numerically dominated by copepods.
cladocera and rotifers. Polychaeta, though not significant numerically, were represented by pelagic larval stages of the
families Spionidae (Poly do ra, "Poly dor a complex", Spiophancs), Phyllodocidae (Eteone. and sub-family Phyllodocinae),
and Cirratulidae. Successful introduction and dispersal of a species to the Great Lakes are most likely for species that are
eurytopic, fecund, and vagile. The last two attributes apply to most marine species of Spionidae. Phyllodocidae and
Cirratulidae. The first attribute may be characteristic of certain species of Spionidae. No representatives of the two most
numerically abundant freshwater polychaete families (Nereidae, Sabellidae) were encountered in this study. It is feasible,
however, that such polychaetes could tolerate the mixohalinc properties associated with the Hushing or exchange of
ballast water and flourish on introduction into the Great Lakes ecosystems, though no significant ecological threat would
be expected. Brackish water polychaete families (19), of which Spionidae and Cirratulidae are representative, may survive
the ballast water exchange but not necessarily subsequent limnetic conditions. Marine species taken on in the ballast
water from the high seas would pose little threat of introduction.
BENTHIC POLYCHAETOUS ANNELIDS OF OGNINA BAY (EASTERN SICILY, ITALY). Caneone . G. & FassaRL G.
(Mollica E Dipartimento di Biologia Animate, University di Catania, via Androne, 81-95124 Catania, Italia). The
Polychaetous Annelids of Ognina bay have been studied. Forty-three stations, along eight transects perpendicular to the
coast, at depths from 30 cm to 112 m. have been sampled. Twenty-eight stations were located on rock surfaces and
samples were collected by scraping quadrants of 25 x 25 cm; on soft substrates a "CHARCOT-PICARD" dredge (50 dm*'
capacity ) was used. One hundred and thirty five species were collected, leading to the recognition of typical biocenoses
and "facies of transition". Shannon’s index, redundancy and equitability for each station have been calculated, whereas to
test the similitude between the stations, we made use of Kulczynski's index. Three different types of population are
recognizable - photophilic and sciaphilous populations arc found on hard substrates, and a third type exists on soft
substrates. Following examination of the samples, no evidence of pollution has been found.
SPATIAL DISTRIBUTION OF AN EPITOKOUS NEREID SPECIES IN AN INTERTIDAL ESTUARINE: THE ROLE OF THE
HYDRODYNAMIC'. Caron. A.. Olivier. M.. Desrosiers, G.. Hudier. E. & Retire. C. — (Centre d'Occanographie.
Departement d'Occanographie, University du Quebec a Rimouski, 310 allce des Ursulines. Rimouski, Quebec, Canada G5L
3A1). — From observations made in a sheltered inlet ("Anse a rOrignal". lower St Lawrence estuary. Canada), we discuss
the influence of hydrodynamic processes on the spatial distribution of a community of Nereis virens. Data obtained
during this study revealed an edaphic segregation between sexually mature and immature individuals. This observation
has been correlated with the sediment thickness. Highest densities of the nectochaete larvae occured at the uppermost part
of the intertidal Hat in which we observed a weak flow regime associated with fine parlicules deposit. Highest adult
densities were found in the diffusion area of waters ebbing away from the bay. These results suggest that during the short
616
ABSTRACTS - RESUMES
period of time of their pelagic life the larvae will he transported in the water column and settle in weak flow regime areas.
After a growth period of three or four years individuals will reach their sexual maturity and begin a migration toward the
lower part of the intertidal flat. Despite their swimming ability it seems that migration is a passive one and is mainly
controlled by hydrodynamics processes.
SEDIMENT PORE-WATER TOXICITY TESTING WITH THE POLYCHAETE DINOPH1LUS GYROC1UATUS. Carr. R.S. -
(U.S. Fish and Wildlife Service. NFCR Field Research Station. CCSU. Box 315, Corpus Christi. Texas 78412. USA). —
The results of recent studies suggest that it is the contaminants associated with pore (interstitial) water that control the
toxicity of contaminated sediments. Studies with the polychaete Dinophilus gyroc Hiatus exposed to pore water obtained
from contaminated sediments demonstrated highly significant correlations between reproductive suppression and the
concentration of a variety of contaminants in the sediments including polycyclic aromatic hydrocarbons, pesticides, and
various trace metals. The short life-cycle of D. gyrociliatus allows effects on reproduction to be determined after a one-
week exposure. Recent studies have focused on (1) optimizing pore-water collection procedures to minimize the loss of
contaminants during the extraction process, and (2) comparing the Dinophilus life-cycle test with other sensitive
toxicity tests (c.g.. fertilization, morphological development, and genotoxicity assays with the sea urchin, Arbacia
punctulata). Results to dale indicate that the sensitivity of the polychaete test is comparable to test results with the sea
urchin assays and other toxicity tests with sensitive life-stages of sensitive species. These pore-water toxicity tests are
now being used routinely in large sediment surveys throughout the United States to determine the quality of the marine
and estuarine sediments.
TEMPORAL. VARIABILITY OF BENTHIC MACROFAUNA: THE DYNAMICS OF PARAPRIONOSPIO PINNATA (EHLERS)
(POLYCHAETA, SPIONIDAE) AT BAHIA CONCEPCION, CHILE. CARRASCO , F.D.& Gauardo. V.A. — (Departamcnto de
Oceanologia. Universidad de Concepcion, P.O Box 2407, Concepcion, Chile). — Temporal oscillations of numerical
density of macrobenthic organisms were studied on Concepcion Bay, Central Chile, during a 3-year survey of the infauna
at a 22 m deep fixed station. A relatively low species richness (40 species) but with a high ecological resilience were
observed. The spionid Paraprionospio pinnata (Ehlcrs) conformed the most important population in the 0.5 mm sieved
muddy sediments of the area both in terms of its contribution to the density (ca. 97 %) and biomass. This high
ecological dominance explain the low species diversity values encountered for this macrofaunal assemblage. The
polychaete Cossura chilensis ranked second far behind. The abundance curve for P. pinnata showed at the beginning of
the study period, early 1988, medium to high numerical abundances with a maximum peak in July 1988 (76,459 ind. m~2).
Thereafter a sharp decrease in density was observed, until a minimum of only a few specimens was reached in January
1989. From this time the worms practically dissapeared from the samples, situation which persisted for throughout the
year 1989 till March 1990. This defaunation was also observed with the rest of the macrofaunal species. In May 1990 the
numerical density of the P. pinnata population began to recover, reaching a maximum peak (63,694 ind. m*2) in
November 1990 to decrease again towards the end of the study period. The shape of abundance curve, and thus temporal
variability, of P. pinnata is not to be expected according previous studies, specially in cases of the dramatic defaunations
reported. We suggested that the 1989 defaunations were induced by the action of long and persistent (several weeks) very
low levels of bottom water dissolved oxygen concentration. These hypoxias, which are common but aperiodic and of
short duration in the area, probably caused the die of organisms and precluded larval recruitment.
EFFECTS OF WATER MOVEMENT DISTURBANCE ON POLYCHAETE STRATIFICATION IN INFRALITIORAI . MUDDY
BOTTOMS. Castelu, A. & Prevedelu, D. (Dipartimento di Biologia Animate, Universita di Modena, Via University 4,
1-41100 Modena. Italy). According to well known patterns the benthic distribution is influenced by quality and
intensity of hydrodynamics; however, knowledge about the stratification of infralittoral muddy bottom macrobenthos
under high hydrodynamic conditions is scanty. In order to study this problem, the polychaete stratification dynamics
have been analyzed in an annual cycle, with parallel recording of water motion as an index of hydrodynamic energy. The
sampling site is located on muddy bottoms in an area facing the Po River delta (Northern Adriatic Sea), at 10 m depth.
Samples have been collected by a box-corcr during six surveys performed between September 1989 and September 1990.
Each sample was splitted in four vertical layers: 0-2 cm, 2-5 cm, 5-10 cm. and 10-20 cm. The hydrodynamic conditions
clearly influence the extension of the layer colonized, considering both the entire polychaete assemblage and single
groups of species identified according to their trophic and ecological requirements. A total of 47 species have been
collected. Individual abundance and species richness usually sharply decrease between the first and the second layer. The
dominant species in the superficial layer arc small-sized surface deposit-feeders such as the spionids Polydora Jlava and
Prionospio cirrifera and the paraonids Aricidea assimilis, A. claudiae, and Levinsenia gracilis. In the deepest layer
tubicolous species of great dimension dominate (i.e. Maldane sarsi and Melinna palmata). Deep burro wers, such as
Nephtys incisa. are uniformely distributed along the whole sediment profile. A preliminary consideration on the
collected data pointed out that the substratum thickness colonized by small-sized surface deposit-feeders tends to increase
after the summer and early autumnal calms and tend to decrease after the storm periods (winter and spring). The
assemblage colonizing the deepest layer (below 10 cm), however, did not vary significantly. Furthermore, alter the
period of stronger storms, abundance of the smaller specimens colonizing the superficial layer significantly decreases.
RESUMES - ABSTRACTS
617
probably in relation to the substantial resuspension of the superficial layer of the sediment. Role of hydrodynamics in
respect to the strategy of the recorded species and in structuring the polychactc assemblage is also discussed.
CENSUS OF POLYCHAETES OE THE ITALIAN COASTS. G.P.I. (Gruppo Polichetologico Italiano). CASTELLI. A. —
(Dipartimento di Biologia Animate, Universila cli Modena. Via Universita 4. 1-41100 Modena, Italy). At the
Polychaete Conference of Long Beach (California), the G.P.I. (Gruppo Polichetologico Italiano) presented a programme,
co-ordinated by A. CASTELLI. devoted to a census of the species recorded so fax* along the Italian coasts. This programme is
a preliminary part of a large scale international project (promoted by I.C.S.E.M. and co-ordinated by G. BELLAN) devoted
to studying the polychaeto-fauna of the Mediterranean Sea. The first results of this census, concerning families and
species recorded (779 species belonging to 68 families) and first dichothomic keys available (Paraonidae - by A.
CASTELLI - with 24 species belonging to seven genera), were summarized in a contribution presented at the Long Beach
Conference. Successively, several other contributions on this topic became available; in particular those concerning
Flabelligeridae, Poccilochaetidae, Hesionidae. Spionidae, Sabcllidae, Capitellidae, and Pilargidae. The contents of these
new reports may be summarized as follows: the census of Flabelligeridae (by A. CASTELLI) points out the occurrence of
eight species belonging to six genera. The census of Poecilochaetidae (by G. CANTONE) points out the occurrence of three
species all belonging to the genus Poecilochaetus. The census of Spionidae (by C. LARDICCI) points out the occurrence of
39 species belonging to 15 genera. The census of Sabcllidae (by A. GlANGRANDE) points out the occurrence of 45 species
belonging to 20 genera and three subfamilies. The census of Capitellidae (by M.F. Gravina & A. SOMASCHINI) points out
the occurrence of 20 species belonging to 12 genera. Lastly the census of Pilargidae (by A. CASTELLI) points out the
occurrence of six species each belonging to different genera. In addition, the contribution on Syllidae (which is by far the
largest family along the italian coasts). Nepthyidae. Serpulidae, Spirorbidae. Nereididae. Aphroditidae, Polynoidae,
Polyodontidae. and Sigalionidae are in press.
REPRODUCTIVE BIOLOGY OF AMPHITR/TE SP. (POLYCHAETA. TEREBELUDAE) IN TAIWAN. CHEN, C-P. & Chen .
R.B. (Institute of Zoology. Academia Sinica, Taipei, Taiwan 1 15. Republic of China). — Amphitrite sp. is distributed
commonly in the intertidal sandflats of the west coast of Taiwan (and is probably a new species, Hutchings, pers.comm.).
Adult worms are about 10 cm in length. Worms live in "U" shaped tubes, which aggregate closely to form a cluster of
about 10 cm in diameter. Field samplings were conducted monthly from September 1990 to August 1991 at Hsin-Chu (N
24°50’; E 120°54’), Taiwan. Among 660 intact individuals collected. 141 were male. Ill female and 408 sex-
indeterminable. Worms are dioecious with a sex ratio of 1 : 1. Males had an average of 105.8 (sd. 16.2) segments; females
103.6 (sd. 15.2). The smallest male had 74 segments and the smallest female had 66 segments. The septa between
segments is incomplete. Mature ova are 120 to 180 pm in diameter, and fecundity is 55.000 (sd, 25,000). Seasonal
change of the incidence of sexual determination and oocyte-size distribution pattern reveals that spawning may occur in
both spring and fall. Aulophore larvae of less than 10 segments having one tentacle within a hyaline lube were found
benthically in association with tubes of adults. Juvenile recruitment occurred mainly during the summer with a minor
recruitment in late spring.
NERVOUS SYSTEM OF PSEUDO POT A MILLA REN/FORMIS BRUGUIERE AND SOME OTHER SAB ELLI FORM
POLYCHAETES. CHUGHTAI, I. & Knight-Jones, E.W. — (School of Biological Sciences, University of Wales. Swansea. U
.K.). — Most emergent tubes of PseudopotamiUa are so orientated that the dorsal side of the expanded crown faces away
from the substratum. Phis crown forms a bilaterally symmetrical fan. with most of the radiolar compound eyes facing
dorsally and thus towards incident light and the main incoming water current. The nerves from the crown connect
dorsolaterally with the brain, which is much thicker than the segmental commissures. Above it two horn-shaped lobes
Hank the dorsal groove and contribute pedunculate processes. Near these paired giant axons originate, decussate and run
back in the circumoesophageal connectives. On each side a lateral lobe contains a cerebral eye. but the anterior part of
the ventral nerve ladder shows no cephalisation. The intersegmental positions of the ventral ganglia may be associated
with the septal attachments of the chaetal musculature; they also leave room for segmental development of the ventral
gland shields, which are particularly (hick in this species. Each ventral cord is in close contact with a paramedial group of
longitudinal muscle fibres, and about half the cross-sectional area of each cord is occupied by a giant axon, throughout
most of the thorax and anterior abdomen. These axons are joined via some transverse commissures and each is linked to
many neurones of various sizes. More posteriorly, where the coelom is full of sex products and the muscles are reduced to
a thin layer, giant axons are reduced or absent. The peculiarities of sabellid nervous systems will be compared with those
of related forms and other polychaetes.
MOLECULAR CHARACTERIZATION OF A METALLOPROTEIN OF HED/STE (NEREIS) DIVERSICOLOR (ANNELIDA
POLYCHAETA). ITS PHYLOGENIC INTEREST. DHA1NAUT, A.. Sa LZET-Ra VEIUON, B., DEMUYNCK, S. <£ DhaINAUT-Gouktois,
N. (Univcrsite de Lille I. Laboratoire de Phylogenie Moleculaire des Annelides, URA CNRS 148. 59655 Villeneuve
d'Ascq Cedex. France). — Physiological parameters able to provoke the synthesis and releasing of the metalloprotein
MP II seem to be various: metallic exposition, bacteria agression, osmotic stress,. ..In order to precise how modulated is
the expression of genes encoding MP II, a cDNA probe was produced. From the MP II amino acid sequence known, two
oligonucleotidic probes were synthetized. Using PCR (Polymerase Chain Reaction), a 250 bp fragment corresponding to
618
ABSTRACTS - RESUMES
Ihe exon encoding MP II was obtained and has allowed us to realize in situ hybridation experiences. First results reveal
the presence of a genic expression in ccelomic cell clumps and in some muscles. Quantitative estimation of this
expression was studied by mRNA extraction and Northern Blotting. Characterization of the molecule MP II is interesting
with regard to phylogcnic considerations. MP II shares high similitudes with hemerythrins and myohemerythrins of
sipunculids described in the littcrature. Moreover, works done in our laboratory by other people have shown the
existence of related molecules in oligochaete and achaete species. Evaluation of its distribution in other invertebrate
phyla is now under progress. Results in that field would be of importance for the understanding of phylogcnic
relationships between some invertebrates.
RESPONSE OF ESTUARINE BURROWING INVERTEBRATES TO METALLIC POLLUTION. Dhainaut-Courtois . AC
SEPTIER, F.. ROMO NT, R.. Demuynck. S. & Dhainaut , A. — (University de Lille I. Laboratoire de Phylogenie Moleculaire
des Annelides, UR A CNRS 148. 59655 Villeneuve d'Asccj Cedex, France). — Estuarine burrowing species constitute good
models to appreciate biological impacts of micropollutants having a continental origin. Among the available species at
the different sites studied by ourselves in the North of France, much attention was paid to the particularly abundant
species Hediste (Nereis) diversicolor (Annelida, polychaela) having all the criterias required to serve as a bioindicator.
The aim of the ecoepidemiological studies was to check correlations between the metallic content of sediments and
animals. In addition to these in situ studies, experimental laboratory works were carried out to detect interactions between
metals and physical parameters (pH, salinity, t0...) able to modify the concentration factors. Moreover, cytopathological
effects due to several metals were checked by means of electron microscopy. By atomic absorption spectrophotometry,
chromatography and electrophoresis, two iron-containing proteins called MP I and MP II able to bind cadmium ions were
detected. Results which were obtained by biochemical and ultrastructural methods and by radioautography using 109Cd
appear to indicate that the high molecular weight protein (MP I) would be the extracellular hemoglobin. The latter protein
(MP II) which is not a metallothionein was found to be able of bacteriostatic activities. This protein, close to 13,5 kDa
has been sequenced and revealed high homologies with two respiratory proteins: hemerythrin and myohemerythrin.
Using poly- and monoclonal antibodies raised against MP II. a possible site of synthesis was found to be granulocytes
cells (G I). To conclude, MP II protein seems to play different roles: possible intervention in a detoxication process by
its capacity to bind toxic heavy metals; bacteriostatic activity(ies) occurring by iron deprivation of bacterias. At the
moment, the role of MP II in the transport of dioxygen remains uncertain.
POLYCHAETES FROM THE ISLAND OF BARBADOS. W.I. SETTLEMENT AND SUCCESSION. DlAZ, V. - (Dep. Ecologia.
CICESB, P.O. Box 434843. San Diego. CA 92143, U.S.A.). — Settlement and temporal succession of organisms on coral
plates (Montastrea annularis) were examined at two fringing reefs on the west coast of Barbados: Spring Garden (polluted
area) and Six Men's (non disturbed area). Two series of coral plates (60 cm2) were fixed at 10 m depth. Series A was
immersed the 28/02 and series B the 8/05/1990, they were constituted by 15 and 12 plates respectively. It is clear that
the most abundant animal colonisers are Polychaetes. The first animals to colonize the bare surfaces were polychaeles
and crustaceans (amphipods). On upper surfaces pioneer polychaetes are represented in series A by Nereis sp, Glycera
abranchial a. Exogone genunifera and some Syllidae in S. Garden whereas in S. Men's we have Polydora sp, Ce rat one re is
mirabilis, Syllis sp. and some Filograna sp. In B we collected Dondllca cerasina, Polyophtalmus piclus , Amphinomidac
and some CirratuUdae in the polluted reef area and in S. Men’s: Salmacina sp. Polycirrus medusa and some Nereidae. On
lower surfaces, encrusting colonial organisms were important in the initial colonization process (ascidians, bryozoans).
Serpulidac was the dominant family of polychaeta ( Salmacina sp, Pseudovermilia occidentals. Hydroides mucronatus, H.
mongeslospesi, H. parvus. H. bispinosus. Pomaioslegus sp), followed by Spirorbidac ( Spirorbis epichysis. S. cf.
kn igh rjonesi,. . . ). we also found some Nereidae ( Ceratonereis mirabilis ). The most abundant polychaetes on upper
surfaces were nereids. syllids, terebellids and spionids in Series A, and eunicids, syllids and capitellids in series B. On
lower surfaces were serpulids. spirorbids. spionids and syllids in series A and serpulids, spirorbids and syllids in B. Algal
lilms seem important to induce polychaele settlement. Globally, there is a trend towards increasing abundance over time.
Diversity and abundance were higher on the polluted area. Diversity was higher on upper surfaces, whereas densities were
higher on lower surfaces. A great proportion of Polychaetes were deposit-feeders exploiting the abundant organic matter
(2 to 24 mg sed. d !. cm'- in S .Garden, 0.5 to 7 mg sed. d'1. cm'- in S. Men's). In conclusion. Polychaetes play an
important role in the colonization process in hard tropical bottoms. The pattern of early colonization on the reef is
different for surfaces exposed to light and sedimentation than it is for surfaces protected from these factors. The two
courses of colonization create different ecological assemblages.
LIFE CYCLE AND PRODUCTION OF POLYCHAETE SPECIES IN THE AIGUAMOLLS SALT MARS! I (ROSE S, GIRONA.
NE SPAIN). DUESO, A. Sarda. R. — (Centre d'Estudis Avai^ats de Blanes. Cami de Santa Barbara s/n, E-17300, Blanes.
Girona. Spain). — Mediolittoral and infralittoral muddy and silty sand sediments in brackish waters of the Mediterranean
Sea are characterized by the presence of a typical macroinfaunal assemblage dominated by the polychaetes Hedisle
diversicolor and Streblospio shrubsolii. the bivalve Cerastoderma edule and the amphipods Corophium ssp. Although
abundant data o( densities can be found in the literature, the dynamics of this particular assemblage is poorly known.
Benthic macroinfaunal populations in several areas (five stations, three replicates by station) of Els Aiguamolls Salt
Marsh (Roses. Girona, NE Spain) has been monitored from April 1991 to date using a corer (3.5 cm in radius). Samples
RESUMES - ABSTRACTS
619
were processed through 500 pin mesh and the mud going through the mesh was sorted under binocular microscope to
count the smaller size fraction of the different populations. To calculate biomass of the species, digitized lengths of all
specimens were recorded using a computer aided programme. Regressions of length vs dry weight were calculated to
estimate biomass from length. We employed ELEFAN software to analyze growth and production of the different cohorts
observed. In this paper we presented the population structure, seasonal dynamics and production of the two dominant
polychactc species: H. diversicolor and S. shrubsolii in tidal creeks of the salt marsh during the first year. Both species
shows an extended spawning season with constant recruitment through the year although pe aks of recruitment were
detected in early winter. Abundance data ranged from 2,036 ind. m'2 in August to 16,305 ind. m'2 in December (average of
11,798 ind. m"“) for S. shrubsolii, and from 390 ind. m'2 in September to 14,898 ind. m*2 in January (average of 5,145
ind. in’2) for H. diversicolor. Biomass data ranged from 0.63 g. m*2 in August to 5.22 g. m"2 in December (average of 2.50
g. m'-) for S. shrubsolii, and from 0.11 g. m’- in November to 7.41 g. m'2 in July (average of 2.83 g. m“2) for H.
diversicolor. Population abundances peaked during winter and there was a sharp decrease in densities through summer.
The total benthic secondary production in the creeks for these two species, estimated as increases in biomass fron one
sampling dale to the next, was 17.97 g. m'2 (9.58 g. m'2 for H. diversicolor and 8.40 g. in*2 for S. shrubsolii). P/B ratios
for these two species were estimated as 3.38 for H. diversicolor and 3.36 for S. shrubsolii. The results found in Els Aigua-
molls Salt Marsh are compared with data from temperate zones of the Mediterranean and Atlantic Coast.
FEEDING BEHAVIOUR AND FUNCTIONAL MORPHOLOGY OF THE INTROVERT AND DIGESTIVE SYSTEM OF
MY70STOMA CIRRIFERUM ( MYZOSTOM1DA). Eeckhaut, I., DOCHY, B. & JANGOUX, M. (Universite de Mons-
Hainaut, 19 avenue Maistriau. 7000 Mons, Belgium). — Myzostomids are poorly known annelid-related invertebrates
associated with echinoderms, particularly comatulid crinoids. One of the interests that the myzostomids get from the
symbiosis with the comatulids is the alimentary supply furnished passively by the host: most of the myzostomids feed
on alimentary particles catched by the host. However, except anecdotal observations, very little is known of both their
feeding behaviour and the structure of their digestive system. For this work, we studied the symbiotic pair Antedon bifida
(Pennant. 1777) (Crinoidea) and Myzostoma cirriferum Leuckart. 1836 which were collected by Scuba diving at Morgat
(Brittany, France). All postmetamorphic stages of M. cirriferum feed on alimentary particles carried by the ciliary current
of the host's ambulacral grooves. They feed preferentially at the level of the pinnular grooves (myzostomids of 0.07 to
0.6 mm long) or the arm grooves (myzostomids of 0.6 to I mm long) or the calycinal grooves (myzostomids of 1 to 2.4
mm long). The digestive system of M. cirriferum is made of a pharynx included in an antero-ventral protrusive introvert
(the mouth opens at the apex of the introvert), a stomach from which start blind digestive caeca, and an intestine which
opens to the exterior by a postero-ventral anus. The mouth is surrounded by a sensory lip and four pairs of sensory
papilla. The pharyngial lumen is bordered by a cuticuled pseudostratified myoepithelium which is surrounded by a highly
developed musculature. The rest of the digestive system is made of a non-cuticuled monostratified epithelium surrounded
by a less developed musculature: the stomachal epithelium consists of microvillar ciliated club-shaped cells; the caecal
epithelium of microvillar vacuolar cells which have been observed under different metabolic stages (viz. they are
flattened and without vacuoles or include either numerous small vacuoles or one very large vacuole); the intestinal
epithelium of flattened microvillar cells. Digestive transit of alimentary particles has been studied through in vivo and
histophysiological observations (using small coloured particles or ferritine as alimentary particles). When the
myzostomid introvert is applied in an ambulacral groove, few alimentary particles are pumped and carried to the stomach
by the contractions and the elongations of the pharyngial muscular fibers. In the stomach, they are chased out by means
of ciliary beatings to the caeca where they are endocyted by caecal cells which are the site of intracellular digestion. After
digestion, the alimentary residues included in large caecal vacuoles are exocyted by apocriny in the caecal lumen and are
chased out to the stomach by the contractions of the caecal musculature. There, vacuoles and their residues are embedded
in stomachal secretions to form a compact faecal mass which is expulsed through the anus by the contractions of the
stomachal and intestinal musculature.
COST OF REPRODUCTION IN OF HR YOl ROCHA DIADEMA (POLYCHAETA. DORVILLEI-DAE). Eide, R. & AKESSON. B.
— (Department of Zoology. University of Goteborg. Box 25059, S-400 31 Goteborg, Sweden). Ophryotrocha
diadema is a simultaneous, cross-fertilising hermaphrodite. After pair formation each individual alternate in male and
female function. Isolated individuals do not shed eggs. Reproductive costs were measured by comparison of life-tables
obtained in four different experimental treatments. Reproduction, survival and growth (as number of setigerous segments)
was recorded weekly during the whole lifetime of the animals. In older stages (> 20 weeks) a subjective "condition index"
was estimated to evaluate sub lethal effects. For each experimental treatment 54 to 60 individuals were employed. The
treatments were: 1. Continuous reproduction. Two individuals were permanently kept together with continuous possi¬
bility to reproduce. 2. Single. Individuals were isolated singly during their whole lifetime. 3. Half-time social.
Reproducing pairs lived together for two weeks, they were then separated and each of them was placed together with an
individual of Ophryotrocha sp., that is a sibling species. The two species have social interactions similar to intra
specific ones, but inter specific mating does not occur. After two weeks with alien partners, the worms were placed with
their conspecifics for the next two-week period of normal reproduction. Such two- week cycles continued during the
animals' whole lifetime. This treatment was designed to lower physical reproductive effort but still maintain the social
interaction. 4. Half-time single. This treatment resembles the one in n°3, but during the alternating two-week periods
620
ABSTRACTS - RESUMES
with no reproduction the worms were kept singly isolated with no opportunity for social interactions. During peak
reproduction (exp. weeks 7-8) the individuals with continuous reproduction had the best performance, followed by half¬
time single individuals. Lowest reproduction was found in the group of half-time social animals. All differences were
significant. When the animals grew older the reproduction became similar in all three groups. During week 1-12 of the
experimental period the fastest growth rate was found in the group of single individuals, followed in order by half-time
single, half-time social and continuously reproducing individuals. All groups significantly differed from each other. At
the end of the experiment, half-time single individuals were largest, while continuously reproducing and half-time social
animals attained the same size. The lowest condition index was found in the group of single individuals during week 20-
47. Half-time social animals had the highest condition index during week 20-25 but the lowest during week 47-52.
A FIRE WORM WITH A SHELTERED LIFE; STUDIES OF B ENTH OS CO LEX CUDANUS (AMPHINOMIDAE), AN
INTERNAL PARASITE OF THE BATIIYAL SEA URCHIN ARCHEOPNEUSTES HYSTRIX. EMSON, R.H. , YOUNG, CM. &
Paterson. G.J.L. — (Division of Life Sciences, King's College. University of London. Campden Hill Road. Kensington.
London W8 7AH. U.K.). Benthoscolex cubanus an amphinomid described by Hartman (1942). has been found in
populations of the spatangoid sea-urchin Archeopneustes hystrix from bathyal depths (430-616 m) at several widely
separated sites in the Bahamas area. The polychaelc was found inhabiting the intestine of the sea-urchin where it feeds by
selecting foraminiferans and other organic fragments from the gut of the sea-urchin. Twenty three species of sea-urchin
were surveyed for the worm but B. cubanus appeared to be specifically associated with A. hystrix. The worm was abundant
in that sea-urchin with an overall prevalence of 65 % and some populations were 100 % infected. Either one or rarely two
worms were found in each urchin. The worm can move about easily in the gut of the sea-urchin but is not thought to leave
the sea-urchin in normal circumstances. Mature worms were found in the populations at all times of year sampled and
maturity was related to size. Sexes were equal and no difference in the size range of mature males and females was evident.
B. cubanus was found to have small (80 pm) non-buoyant thick walled eggs and is likely to have a benthic or
planktotrophic larva. Few obvious adaptations for life inside the gut of a sea-urchin were apparent but the structure of the
cuticle was compatible with its having a protective function. B. cubanus is one of very few polychaetes living inside
other animals and the only known internal parasitic polychaete of sea-urchins. Avoidance of predation appears to be the
most likely reason for the evolution of this unusual relationship.
TAXONOMY AND POPULA TION DYNAMICS OF DIOPATRA CF. BREV/CIRRIS (POLYCHAETA. ONUPHIDAE) FROM
THE MOROCCAN ATLANTIC COAST 1990-1992. Fadiaoui, S.. lECHAPT. J.P. & RETI&RE, C. (Laboratoire Maritime,
17 avenue George V. B.P. 28. 35801 Dinard, France). - Diopatra cf. brevicirris was collected near the south Moroccan
Atlantic coast (North to South range: 31°58‘ to 31°52'; East to West range: 9°26’ to 9°36'), at depths ranging from 16 to
40 m. D. cf. brevicirris is the dominant species in the benthic Abra alba community. This community is found in fine
sediments which contain a varying degree of silt and are more or less compact. Thermal variations are not important
because of the upwelling due to trade-winds. This species had not been reported from this coast until now. as it was
probably confused with Diopatra neapolitana , a species from which it differs in certain characters. The structure and
kinetics of this population were studied and the biological cycle of this species was described taking into account the
climatic particularities of this area. Two sites were compared; site 1 was near the coast at a depth of 16 m. and site 2 was at
a depth of 36 m. Partial weight of wiped subjects preserved in formalin was chosen as the biometrical criterion. Total
weight was not used because the posterior part of individuals was frequently amputated during sampling and sifting, or
following predatory attempts or autotomy. A frequency distribution histogram (N = 400) showed that most worms were
broken at segment 10. Partial weight of the first ten segments was highly correlated with jaw lenght (r = 0.95). During
the period of this study, spawning and recruitment periods were estimated from analysis of frequency distribution
histograms; two periods of recruitment were identified in spring and summer 1990 due to consecutive winter and spring
spawnings which take place in the tubes ol adults and are followed by incubation and larval development unside these
tubes. During summer 1991 we again observed recruitment, similar to that of the summer 1990. The reproduction cycle is
certainly reproducible each year. Presence of some worms (partial weight < 5. 10'3g) during winter and automn 1990 and
observation of some worms, in July 1991, carrying eggs in tubes, suggest that order less important recruitments take
place. In addition, as there were more young recruits at site 2 and adults were larger at site 1. we suggest that recruitment
should take place at deep sites where the level of pelitc is high.
CATALOGUE AND BIBLIOGRAPHY OF THE POLYCHAETES. FAUCHALD, K. & Ward. LA. (National Museum of
Natural History. Smithsonian Institution. NHB Slop 163 Washington, D.C. USA). — Olga Hartman’s publication of
Catalogue ol the Polychaetous Annelids of the World" in 1959 (supplement published in 1965) was a major event for
polychaete systematise and ecologists. The catalogue made it possible to look up the original description for almost all
polychaete species published, when used in association with Hartman's previously published bibliography. References
to combinations of genus and species names other than as originally published were also included. As at no time before,
we had a single source of information of names at the species, genus and family-levels. The number of new taxa described
in recent years has risen exponentially, in part due to the presence of the catalogue. Even the supplement is now close to
30 years old and a new edition is sorely needed. Computer applications for micro -computers are excellent for these kinds
°f publications. We have prepared a set of interlinked databases containing: 1. A listing of the original name for all
RESUMES - ABSTRACTS
621
polychaele species; 2. References to new combinations of genus and species names, and 3. Complete bibliographic
references to the polychaele literature from 1758 to date. This material will be issued as a compact disc. Printed copy can
be prepared, or any data downloaded from any database on the disc. The disc will be a closed application: no more new
material nor any additional queries for reports can%bc written to the disc. We will demonstrate the look and feel of the
catalogue as currently devised. We would like the conference participants to spend lime using the catalog, advise us about
what kinds of documentation arc needed and what uses to which they would put the catalog. We are at this point in the
process of editing the content (probably a never-ending job!) but we are less concerned about having every last synonym
entered, than we are about making the catalogue useful. Once we have a good format, we can continously edit the
catalogue, taking into account new findings. We plan to issue periodic updates perhaps with 5 year intervals once the
first version has become available. Polychaete systematics is an on-going task. We have been more concerned about
having all current and recent points of view on a problem represented than about presenting a single, codified view of the
systematics of any group. For this reason, we have been conservative in accepting proposed synonymies and have taken
distinctly "agnostic" points of view in several conflicts.
PHYSIOLOGY OF OOGENESIS IN POLYCHAETES. Fischf.r . A. — (University of Mainz. Zoological Institute. Saarsir.
21, 6500 Mainz. Germany). - Oocytes generally are extremely large cells specialized for two purposes: storage of
reserves and fusion with one male gamete. This review on physiology of oogenesis therefore gives account of the
processes of growth and reserve accumulation in the oocyte and its differentiation as a gamete and, on the other hand,
reports data on the physicochemical conditions the maternal soma is providing for the growing oocytes. In the period of
vitellogenesis, the cytoplasm of the oocyte gets increasingly packed with storage inclusions containing yolk protein,
lipid and carbohydrates, respectively. The cell membrane of the oocyte contains a receptor protein recognizing and
internalizing yolk precursor protein at a specific rate. The various storage elements, more or less intermingled during
vitellogenesis, are sorted out in a rapid process of egg maturation immediately prior to spawning in nercid eggs.
Structural and biochemical differentiation of the vitelline envelope has been described in sabellids (LEE and coworkers).
Which are the extracellular conditions required by growing polychaete oocytes? Environmental and hormonal parameters
controlling oogenesis are known for a number of polychaetes, but physicochemical conditions immediately affecting the
oocytes are defined in a few instances only. However, "diffuse" oogenesis without ovaries, common among polychaetes.
offers favorable conditions for analyzing the immediate prerequisites for oocyte survival, growth and differentiation.
Oocytes of Nereis virens can be kept in cell culture and their requirements, such as ionic composition, nutrient and
oxygen contents of their medium can be defined. Likewise, oocyte physiology can be studied in the oocyte-nurse cell
complex of Ophryotrocha. The specific conditions encountered in polychaete oogenesis thus may enable us to provide
insights of general interest into the physiology of oogenesis.
CLADISTIC ANALYSIS OF RELATIONSHIPS AMONG THE POLYCHAETE FAMILIES. FlTZHUGH, J. <£ FauchaLD, K. —
(Natural History Museum of Los Angeles County, Los Angeles, CA 90007. USA). Some major taxa. e.g.. the
aphroditids and eunicids, both sensu Into, have been recognized consistently as natural groupings for 100 years. The
traditional separation of the polychaetes into two groups and all other proposed groupings into suprafamilial taxa have
been only moderately successful. Classsificatory studies differ from evolutionary studies in that the presence of links
between the groups need not be specified. Most systemalists believe that their classification, including the order in
which the taxa arc presented, reflect phylogeny. Any phylogeny based on these schemes would uncover paraphyletic
groupings. We are here presenting a new phylogenetic analysis of the relationships among the polychaete families. We
have analyzed the characters traditionally used to define taxa at the family-level and defined character states so that
members of all families can be scored unequivocally. We have added, mostly anatomical, characters previously rarely
considered, or at least considered only one at a time. We scored, if possible, the characters for a specimen of the type
species of the type genus for each family (on classificatory rather than cladistic grounds): medium-sized to large
specimens were used preferentially. Small specimens and indeed all specimens of small species, tend to have less
developed anterior appendages, less complicated parapodia and often fewer kinds of chaetae than larger specimens (or
species). We also assumed initially that all families as currently recognized were monophyletic. The cladistic program
used was Hcnnig-86; options will be presented in the talk. Autapomorphic characters defining single terminal taxa were
excluded from the analysis. We find it unlikely that for example the joint absence of the ventral shield of the sternaspids
carry much weight as a synapomorphic feature for all non-sternaspid polychaetes. Outgroup taxa included echiurans and
sipunculans in addition to oligochaetes. The major taxa listed above were confirmed as being monophyletic. The families
of the Phyllodocida can be ranged together; similarly families with dorsal feeding palps (or some modification of these)
can be grouped in a single sequence. We are at this point debating the position of other families, especially the orbiniids,
paraonids. maldanids. capitel I ids. opheliids and the small families usually listed near these families.
POLYCHAETE POPULATIONS OF THE LEAF STRATUM OF A POSIDONIA OCEANICA BED: A YEAR CYCLE. Gambl
yV/.C. & LANERA, P. — (Laboratorio di Ecologia del Benthos, Stazione Zoologica "Anton Dohrn". Napoli. Italy). — In the
framework of an investigation on vagile fauna of the Mediterranean seagrass Posidonia oceanica, Polychaetes were
sampled in the leaf stratum of a continuous Posidonia meadow off Lacco Ameno (Island of Ischia, Gulf of Naples, Italy).
Samples, taken by Scuba diving using a hand-towed net (400 pm mesh size), were collected monthly, from July 1981 to
622
ABSTRACT'S - RESUMES
June 1982. and along a transect, at 1 m, 3 m. 10 m. 15 m and 25 in depths. Monthly data, grouped in four seasons
(summer, autumn, winter and spring) were analyzed by means of the Factorial Analysis of Correspondence. A total of
1.765 individuals and 134 species have been documented so far. Thirty seven taxa occurred only once with one
individual, while 27 taxa (445 individuals) belonged to sessile forms and were not considered in this analysis. The best
represented family was that of Syllidae (55 species and 865 individuals). A clear depth zonation of the populations was
recognizable, especially in summer and spring when environmental differences between shallow and deep stands of the
Posidonia bed arc more pronounced. Seasonal differences were more evident at shallow depths (from 1 to 10 m). while
these were almost negligible in deepest samples (25 m) where the environment is seasonally more stable. The most
abundant species, best contributing to these spatio-temporal patterns were Grubeosyllis clavata. G. limbata. G. vieitezi,
Syllis prolifera, Platy nereis dumerilii. Amphiglena mediterranean Oriopsis armandi and Raphidrilus nemasoma
particularly abundant at shallow depth and in summer and spring, and Sphaerosyllis pirifera, S. hystrix, Eurysyllis
tuberculoid. Odontosyllis gibba, Nereis rava and Kefersteinia cirrata mostly occurring in deeper samples, especially in
winter and autumn. As a whole, spatial and seasonal distribution of Polychaetes in the Posidonia leaf stratum was
consistent with the environmental conditions of the bed and with the behaviour of other groups of the vagile fauna
studied.
FEEDING ECOLOGY OF PLATYNEREIS DUMERILII (POLYCHAETA. NEREIDIDAE) IN POSIDONIA OCEANICA
ECOSYSTEM. Gambi. M.C., Zupo.V. & Mazzella, L. (Laboratorio di Ecologia del Benthos. Stazione Zoologica
"Anton Dohrn". Napoli. Italy). - The Mediterranean seagrass Posidonia oceanica is characterized by a highly complex
plant epiphytic community that shows successional stages culminating with a climax and a maximum of production in
summer, especially at shallow depths. Most of this production is transferred to secondary producers by way of various
species of grazers. Platy nereis dumerilii is one of the most abundant Polychaetes in Posidonia oceanica meadows,
representing almost 10 % of the total Polychaete abundance. This species is a hervivore mesograzer occurring in leaf
stratum as well as in the rhizome layer of the plant, and it is particularly abundant at shallow stands of the beds (1-3 m
depth) and in spring and summer. The feeding ecology of P. dumerilii was therefore studied to better define its trophic
behaviour and its role in the food web of the Posidonia system. Specimens of P. dumerilii were collected in a shallow
Posidonia bed of the Island of Ischia (Gulf of Naples, Italy) and in the surroundings hard bottoms, and reared in the
laboratory (in a closed water system) for food-item choices and grazing experiments. All the experiments were conducted
on starved animals divided in three size classes. Food choice experiments were conducted in binary chambers utilizing
various species of macroalgae and Posidonia leaves differently epiphytized (without epiphytes, with encrusting
corallinaceae algae and with erect algae). On the basis of the food choice results, forced grazing experiments were
performed using plant-epiphylized Posidonia leaves. The fecal pellets produced were periodically removed and analyzed
by means of optical and scanning electron microscopy. Grazed leaves were also examined for bite marks and other traces
ol grazing. Food choice experiments revealed that Posidonia with erect epiphytes was significantly preferred to the other
items except for the brown alga Dictyota dichotoma; while Posidonia without epiphytes was heavely ever selected. This
emphasises that epiphytic layer plays a greater role than the Posidonia tissues in the trophic ecology of this species, and
it is consistent with the spatio-temporal distributional pattern of the species in such a system. Fecal pellet analysis
showed the prevalence of macroalgae tissue in the diet of worms, regardless of their size class. However, fluorescence
microscopy, revealed traces of undigested clorophyll in the fecal pellet material. Posidonia leaves grazed by larger worms
(up to 15 mm length) showed clear grazing marks on erect macroalgae. These results help to better define the feeding
behavior of P. dumerilii and demonstrate its potential role in the energy transfer at the Posidonia epiphyte level.
SOFT BOTTOM INTERTIDAL POLYCHAETES ASSEMBLAGES IN THREE ESTUARIES IN THE BASQUE COUNTOY
(GULF OF BISCAY): TAXONOMIC STRUCTURES AND BIOCENOTIC AND ECOLOGICAL RELA TIONSHIPS. GARCIA-
ABERAS. L. & R\LLO, A. (Facultad de Ciencias, Zoologia. Universidad del Pais Vasco. Apdo, 644, 48080 Bilbao.
Spain). — A general survey of polychaete fauna from littoral soft bottoms of three estuaries (La Arena. Plentzia y
Mundaka-Basque Country, Spain) was done during the year 1989. and related to physicochemical conditions of the
sediment and localisation of the sampling site. Over fifty species have been identified. Sample sites and the three
estuaries as a whole have been characterised by launistic richness, abundances, dominances and diversity indexes. Two
main communities are present: the reduced Macoma in sites with mud (marshes) and the Tellina in sandy places. The
accompanying species are investigated and discussed. A comparison has been made between the study areas based on the
differing environmental gradients (granulometric data, organic enrichment, conductivity, temperature, pH. 02
concentration and redox potential of the sediment) in order to determine the spatial distribution and temporal changes of
polychaetes assemblages, and find out correlations between presence and abundance of species with those environmental
conditions. It is concluded that granulometry and organic content are the most important factors determining the
community structure.
CONTRIBUTION TO THE STUDY OF THE POLYCHAETOUS ANNELIDS FROM SOUTHERN IBERIAN PENINSULA: THE
BAY OF ALGECTRAS (( ADIZ. SPAIN). Garcia- MARTIN, S. F. (Biologia. Facultad de Ciencias del Mar, Universidad de
Cadiz, Apartado 40. 1 1510 Puerto Real. Cadiz, Spain). The bay of Algeciras (Cadiz. Southern Spain) spreads over 70
km-, with maximum depths of 500 m. During last decades it has undergone both considerable industrialization and human
RESUMES - ABSTRACTS
623
population increase. Several harbour constructions in this bay cause decreased water renewal rates in some areas.
However, the bay of Algeciras is located in a region with a strong hydrodynamic regimen (Strait of Gibraltar); this
location counteracts the effects of sewage and industrial waste discharges. This preliminary report presents a checklist of
Polychaetous Annelids (about 100 species) from several areas of the bay of Algeciras (depths of 0 to 27 m) The data
obtained are discussed in relation to human activities and type of bottoms, and compared with others from adjacent areas
which are pressumably unpolluted.
NOTOMASTUS IATERICEVS VS N A IN ERIS LAEVIGATA, TWO CONFLICTING STRATEGIES COMPETING IN THE
SAME HABITAT. GlANGRj\NDE, A. & PETRAROU. A. — (Dipartimcnto di Biologia, University di Lecce, 73100 Lecce. Italy).
A study over three years in the Aequatina lagoon (South Adriatic Sea, Italy) was carried out to investigate the
reproductive strategies of several polychaele species. The life-history traits of dominant species, Naineris laevigata
Grube and Notomastus latericeus Sars, showing contrasting reproductive strategics, were compared. The first species is a
polytelic long lived form characterized by a slow growth rate and high juvenile mortality. N. latericeus is a monotelic
annual species characterized by fast growth and high adult mortality. The N. laevigata reproductive cycle seems to
correspond to a bet-edging strategy with a storage effect, which allows this species to respond to a fluctuating
environment, and to maintain stable trends of abundance and biomass. By contrast the survival pattern of N. latericeus.
showing a rapid increase in favourable periods, could be classified within the opportunistic scheme of large recruitment
over a very short period of time followed by high adult mortality. This leads to very variable trends in abundance and
biomass of this species. The abundance of N. latericeus in the lagoon is mainly the result of successful recruitment
strongly related to the variation in salinity and competition with other polychaele species. During most of the lime, in
which the salinity ranged from 20 to 30 P.S.U. N. laevigata seems to be competitive superior and N. latericeus remains
confined in well defined patches. Some evolutionary problem arising from the reproductive strategy of N . latericeus are
also discussed.
DISTRIBUTION OF ON U PH ID POLYCHAETA IN THE NORTH ATLANTIC, FROM TROPICAL TO ARCTIC PROVINCE.
GlLmarEC. M.. iNTks, A. & POCKLINGTON, P. — (University de Bretagne Occidental, 6 Avenue lc Gorgeu. 29287 Brest
Cedex, France). — The taxonomy of Onuphid family has been well reviewed by a number of authors, allowing to define
the different ways of colonization in the whole North Atlantic Ocean. Bathymetric and latitudinal distributions are the
main sources of informations helping to recognize biogeographic contingents. A previous study for the Northeast
Atlantic showed high diversity of the bathyal slope, compared to the shelf area. Stable conditions provided shelter to the
marine fauna, after the "Pliocene-Pleistocene" variations of sea level. From this stable area, abyssal plains might have
been colonized since the recolonization of the shelf appeared when the glaciers declined. The authors propose to transfer
these concepts to the Northwest Atlantic. In this geographic area, actual and quaternary hydroclimatic conditions should
be different. The distribution of Onuphids in the eastern Tropical Atlantic was studied according to the same principles
(bathymetry and latitude), especially on the continental shelf of Ivory Coast. Climatic regions (etages) can be compared
to the european system. The horizontal distribution shows faunal cuts in relation with the seasonal settling of the frontal
zones. Submergence of temperate species in these tropical latitudes, emergence of some other contingents and relative
scarcity of tropical species, can be explained by the regional hydroclimatic characteristics. Relations with the eastern
South Atlantic on one hand, and with the Caribbean region on the other hand, can be inferred. Amphi-atlantic
distribution of Onuphids in arctic, temperate and tropical provinces can be also estimated for the shelf, bathyal and
abyssal zones.
A COMPARISON OF SPECIES DIVERSITIES OF POLYCHAETES FROM TEMPERATE AND TROPICAL LOCALITIES.
GODIN. J.F. (Plymouth Marine Laboratory, West Hoe. Plymouth PL1 3DH. U.K). — Artificial substrate units (nylon
pan scourers) were deployed on rocky bottom substrates in the South West of England (UK) and in Trinidad and Tobago
('IT), West Indies. Units were left submerged for similar durations of lime (April -October 1990 in the UK and January-Iuly
1991 in IT). Some units were retrieved at fixed intervals (colonisation experiment) and all others were retrieved after the
5 month period (final diversity). 1.817 individuals representing 73 species were identified for UK and 1,842 individuals
of 93 species were counted for TT. Diversity indices (SWI) for UK samples ranged between 0.75 and 2.5 and for 'IT
between 1.7 and 2.45. Species of the family Syllidae were the initial colonists and also the most dominant family in both
areas. Initial colonisation was much faster in TT but the final polychaete diversities were similar for both localities. For
both sets of samples, species were aggregated into families and showed similar development of "parallel communities"
(THORSON, 1957). Results appear to be contradictory to the latitudinal gradient in species richness theory.
UNUSUAL FATE OF PCBS IN HED/STE (NEREIS) DIVERSICOLOR (POLYCHAETA, NEREID AE). Goerke. H. & Weber. K.
( Alfred- Wegcner-Institut fur Polar-und Meeresforschung. Am Handelshafen 12, Postfach 120161, D-2850
Bremerhaven. Germany). — The elimination kinetics of six polychlorinated biphenyl components were investigated in
Hediste diversicolor and for comparison also in Platichthys Jlesus. Animals from the Weser estuary were maintained at 10
°C and 10 P.S.U. in water continuously filtered through charcoal and given 10 oral doses of a mixture of the PCB
components 52, 44. 95. 101. 87, 153 (IUPAC Nos.; total dose per component: 1 pg.g'1 wet wt.). At regular intervals
during the subsequent elimination period, specimens were analyzed for the six components. The observed PCB
624
ABSTRACTS - RESUMES
concentrations in the animals enabled elimination half-lives to be determined. Ragworms eliminated all components,
except Nos. 95 and 153, faster than flounders. The slow elimination of No. 95 in ragworms is remarkable, because this
component has unsubstituled carbon atoms in 3.4 position, which generally facilitates biotransformalion. These results
indicate specific PCB elimination pathways in H. diversicolor rather than a generally enhanced elimination rate. The
analysis of the fate of component 52, which had been l4C-labelled, revealed that its faster elimination was due to
significant biotransformation: H. diversicolor contained considerably more polar transformation products than P.
Jlesiis. H. diversicolor from the upper, more contaminated Weser estuary also formed more ,4C-labelled polar compounds
than those from the lower estuary. Since different salinities did not influence the PCB elimination, the elevated
biotransformalion capacity of H. diversicolor from the upper estuary is explained by enzymatic induction. The patterns
of PCB elimination half-lives in H. diversicolor and P. flesus were in accordance with the PCB concentration patterns
determined in environmental samples of the species. While PCBs in P. flesus were similiar to Clophen A60 presumably
prevailing in the field, this was not true in H. diversicolor. Therefore, it is concluded that species-pecific PCB
elimination influences the PCB concentration pattern in H. diversicolor significantly.
POLYCHAETE LARVAL SETTLEMENT DYNAMICS IN THE BAY OF BANYULS. NW. MEDITERRANEAN. GREHAN, A.J.
(Observatoire Oceanologique de Banyuls, Laboraloire Arago. 66650 Banyuls-sur-mer, France). — This study was
undertaken to highlight the major differences in benthic invertebrate settlement patterns at two sites in the Bay of
Banyuls. NW Mediterranean. The sites, although in close proximity spatially, are characterised respectively as
belonging to a fine sand Spisula sub/runcata community (20 m) and a muddy sand Nephtys hombergii community (30 m).
Intensive weekly diver sampling of the superficial sediment (0-2 cm) at both sites was undertaken during the main spring
settlement period (March-July). Samples were sieved at 100 pm to ensure complete census of settlers. The results of this
study, for the Polychaeta, are reported and discussed in the light of measured environmental parameters.
SPECIES RECOGNITION AND REPRODUCTIVE ISOLATION IN NEREIDS (ANNELIDA POLYCHAETA). Hardege J.D. .
Bartels-HarDEGE, H. & Zeeck, E. (University of Oldenburg, Inst. Chem. Biol. Mar. Eiivironm., C.v. Ossietzky Sir..
W-2900 Oldenburg. Germany). 'The reproductive form of Nereis succinea and Platynereis dumerilii is the
metamorphosed heteronereis, which is highly specialized for reproduction, has a distinctive reproduction behaviour the
swarming and nuptial dance and die after fertilization. The induction of metamorphosis to ripe hetcronereids and the
determination of dale of swarming are controlled by endogenous rhythms, temperature regimes and moon light
("zeitgeber"). In the Danish Isefjord P. dumerilii reproduces in summer at 3 rd. quarter of the moon cycle while N. succinea
swarms around the new moon phase. However there is an overlap of swarming activity of these species during the week
after new moon phase due to weather conditions. The sex pheromone of P. dumerilii. 5-methyl-3-heptanone was likewise
found in N. succinea where it is also active. 'The pheromone induces an increase in swarming activity during the nuptial
dance behaviour, allows sex recognition by use of sex specific enantiomers and the release of a small cloud of sperm in
males. In N. succinea the threshold concentration of the pheromone is 25 times higher than in P. dumerilii. Here species
recognition and reproductive isolation is provided by the sex pheromone which prevents direct contact of the two
species.
HIGH POLYCHAETE DIVERSI TY IN THE DEEP SEA: PATTERNS OF a AND B, DIVERSITY. HlLBlG, B. & Blake, J.A.
(Science Applications International Corporation. 89 Water Street, Woods Hole, Massachusetts 02543. IJ.S.A). —
Diversity may be described as the number of species in a spatially defined point (a-diversity) or the turnover of species
across a gradient (B-diversity). Data on species diversity is typically described in terms of local or a-diversity in a
restricted spatial setting. We know little about the restriction of individual species, especially in the deep sea where there
are few barriers to long distance distributions. One difficulty in assessing the distributions of deep-sea polychaetes has
been the lack of appropriate samples and the lack of opportunities for single investigators to examine samples from
widely separated geographic locations. We have been able to identify polychaetes from continental slope depths on both
the western North Atlantic and eastern Pacific from similar depths (550-3,000 m). Samples from the western North
Atlantic included 550 quantitative box cores taken from the Canadian boundary to off South Carolina. Samples from the
eastern Pacific were focused in the Gulf of the Farallones off San Francisco and included 67 quantitative box cores. Some
additional material from ambient sediments on the Gorda Ridge in 3.000 m off Oregon were also examined. All samples
were sieved through 300 pm screens and subsequently processed in the same manner. We found a total of 708 polychaete
species on the U.S. Atlantic slope and at least 250 species in the eastern Pacific. The number pf Pacific species is
preliminary because investigations on this material are still on-going. We expect the number of Pacific deep-sea species
to increase. Of the Atlantic species, 315 were widely distributed throughout the entire study area, while 92 species were
restricted to the slope off New England, 42 species were found only off Delaware and New Jersey, and 177 species were
restricted to the slope off the Carolinas. About 50 species were shared between the Atlantic and Pacific slopes. It seems
therefore that we can distinguish between several distributional patterns of deep-sea polychaetes: local (restricted to a
small area, found at only one or a few stations in either the Atlantic or the Pacific), regional (present at many stations on
either the Atlantic or the Pacific slope), and global (present in both the Atlantic and Pacific oceans, often along depth
contours). The largest group of polychaetes with global distribution was the Dorvilleidae with 10 species belonging to
eight genera; other families including a fairly large number of globally distributed species were the Paraonidac (six
RESUMES - ABSTRACTS
625
species, four genera), Ainpharetidae (five species, five genera), and Spionidae (five species, three genera). Additional
families, represented by one or two species, were Apistobranchidae, Cirratulidae, Fauveliopsidae, Glyceridae,
Mesionidae. Nereididae, Onuphidae, Opheliidae. Paralacydoniidae, Pholoidae. Phyllodocidae, Pilargiidae,
Scalibregmatidae, Syllidae, and Trichobranchidae.
A CLADISTIC ANALYSIS OF SPIRASERPULA REGENIIARDT, 1961 (SERPULIDAE, POLYCHAETA); CHARACTERS
AND CHARACTER STATES. Hove, H.A., Ten & PlLLAl, T.G. — (Instituut voor Taxonomische Zoologie, P.O. Box 4766.
1009 AT Amsterdam, Nethcrland). — In the course of a revision of the genus Serpula (PlLLAl. in prep.), a unique and in
serpulids hitherto unknown set of internal lube structures (i.t.s.) was discovered in a yet undescribed species from the
Cape Verde Islands and Florida. The hunt in our collections for more tubes with these longitudinal internal ridges of
startling complexity resulted in another 15 new species, from various (sub)tropical localities. Some are scissiparious. a
so far for the genus Serpula unknown reproductive method. Though overlooked in the descriptions of S. lineatuba. S.
massiliensis and S. minuta, these taxa too showed i.t.s. Finally i.t.s. were found in the type-species of Spiraserpula.
S. spiraserpula. erected by REGENHARDT (1961) for Cretaceous-Palcocene species. The recent species can be included in
this genus, apparently of Tethyan origin. Delimited by a clear-cut synapomorphy, presence of i.t.s., it is monophylctic.
The additional character set of internal tube structures (and a fossil record) makes the genus Spiraserpula more suitable for
phylogenetic analysis than other serpulid genera without i.t.s. By its setal complement and Serpula- type operculum (if
present), Spiraserpula evidently is a member of the Serpula/ Crucigera / Hydroides clade. As outgroup we have selected
Serpula oshimae and S. rubens. Evidence from various transformation series was conflicting, and a manual construction
of a phylogenetic tree was out of the question. We had to recourse to the following programs for PCs: HENNIG 86 (for
MsDOS machines), Paup & MacClade (for Macintoshes). Characters used are numerical, meristic and/or morphological;
states may vary from simple yes/no to complicated hypotheses of transformation series, with up to 10 stales. They
included tube, operculum, branchiae, thorax, setae and uncini. Each type of character presents its peculiarities: in
morphological data questions of homology and polymorphy have to be solved; although numerical and meristic data are
discrete, delimiting size classes poses problems. Some of these problems may be exemplified by the character "internal
dorsal ridge". Its stales are: none = 0; loose teeth =1; toothed ridge = 2; smooth triangular = 3; smooth plate with
thickened edge. T = 4; Y (inverted, stalked V) = 5; askew = 6. The sequence of character states 4-5 is found along a single
ridge in two species. There are two reasons to assume that the character evolved from state 5 to 6 and not the other way
around: 1) bilateral symmetry is the plesiomorphous condition in Sabellida. 2) asymmetry might be a functional
response to a curved tube (although in spirorbids it rather appears to be the other way around). A possible transformation
series is given below. It is neither known if there has been a direct step 1-3 or 0-2. nor if the sequence has been 0-1-2 or
rather 0-2-1. Thus states 0-3 should be treated as unordered, but the assumption ordered (irreversibly) might apply to
states 4-5-6. In computer analysis, "unordered" may be best for the entire set of states, even though this probably
implies some loss of information. In the course of the analysis, the choice of characters was narrowed down. The final
matrix, consisted of 20 species (including outgroup) and 22 characters. HENNIG 86 option mhennig*, bb* results in 1
cladogram (1 = 148, ci = 41, ri = 57). The relatively low consistency index indicates that it still should be regarded as a
preliminary hypothesis.
HABITAT SELECTION BY SETTLING LARVAE OF THE SPIONID PSEUDOPOLYDORA DIOPATRAE. Hs/Ell. H.L.
(Institute of Zoology, Academia Sinica. Taipei, Taiwan 11529, Republic of China). — The natural populations of the
spionid Pseudopoly dora diopalrae predominantly inhabit the tube-caps of the onuphid Diopatra bilobata and rarely found
in bare sand areas. Habitat selection by competent larvae of P. diopalrae was studied in the laboratory from December
1990 to August 1991. The relative importance of chemical and physical characteristics of tube-caps to larval settlement
was examined. Experimental results showed that the spionid larvae made choices among the habitat types provided.
Larvae significantly preferred the tube-caps rather than bare sand, a pattern consistent with the spatial distribution of
Source
626
ABSTRACTS - RESUMES
their natural populations. When the tube-caps were disassembled, the larvae no longer chose to settle in the remains,
regardless of retained chemical characteristics. The larvae seemed to respond to physical setting of the habitat rather than
chemical one. The physical setting of the tube-caps was characterized as stable, firm and structural. The larvae that settled
on the lube-caps within 10 days were larger than those on other habitat types, implying that there is selective advantage
for those individuals choosing tube-caps as settling sites.
MORPHOLOGICAL INVESTIGATIONS ON SOME POLYCHAETE LARVAE OF THE PLANKTON AROUND HELGOLAND
(GERMAN BIGHT). H USEMANN, E. & PlATE S. — (AG Entwicklungsphys. d. Tierc. Lehrstuhl f. Spez. Zool. & ParasitoL,
Ruhr-Universitat Bochum. Postfach 10 21 48. D-W4630 Bochum 1. Germany). — During a three year plankton
monitoring in the German Bight near Helgoland, pelagic larvae of 57 benthic polychaete species were found. Literature
descriptions of developmental stages are missing or incomplete for 15 of the observed species. Here the discriptions of
some so far unknown larval stages of four species are given. The earliest planktonic stages of all four species are eggs
and trochophores. respectively. Pelagic trochophorcs of Scoloplos anniger (Orbiniidae) are ovoid and possess a strong
ciliation. At the beginning of segmentation one pair of red eyes becomes visible. The metatroch segment and three
presumptive setigers arc differentiated first. At settlement larvae possess 11 segments, all bearing chaetae except the
metatroch segment. A pair of gills becomes visible at the 10 th setiger. The ciliation which is present in all segments is
reduced up to settlement from anterior to posterior. IJncleaved eggs are the earliest pelagic stage of Scolelepis bonnieri
(Spionidae). They are ovoid and characterized by a thick, sculptured egg membrane. The egg membrane is first penetrated
by the prototroch cilia which serve for active movement and later by the larval chaetae of the developing embryo. In the
3-segment stage the egg membrane fuses with the larval cuticle. The prostomium of older larvae becomes trapezoid and
possesses two pairs of red eyes and a retractile tip. Larvae with 10 segments have a length of 650 pm. Olive-brown
pigmented trochophores with a mean length of 300 pm are the earliest planktonic larval stage of Eulalia viridis
(Phyllodocidae). They possess a well developed prototroch and one pair of eyes. The prostomium of the
metalrochophores is blunt conical and 4 antennae buds become visible. In this stage 6-7 segments are developed.
Tentacular cirri originate in the 1st and 2nd segment, ventral cirri occur from the 3rd and dorsal cirri from the 4th segment
onward. Composed chaetae are present from the 2nd segment onward. The average length of early nectochaeta with eight
segments is 500 pm. The prostomium is now trapezoid, longer than wide, and anterior, in front of the eyes, a 5th median
antenna becomes visible. The 4th pair of tentacular cirri appears in the 17-19 setiger stage. The opaque trochophores of
Pholoe minuta (Sigalionidae) are 150-200 pm long and possess a well developed prototroch. Metalrochophores with five
segments have a mean length of 450 pm. Their only differentiation at the prostomium arc two pairs of eyes, while the
trunk segments are well developed and bear parapodia with chaetae. Elytrophores with papillae are present in the 2nd. 4th
and 5th segment, a small conical dorsal cirrus in the 3rd segment. The development of elytra starts before the prototroch
is reduced completely, so the latest pelagic stages possess small round elytra.
10W ARDS GENERIC REVISION OF AMPHARETIDAE. JlRKOV, /. A. — (Hydrobiology Department. Biological Faculty.
Moscow Stale University, Moscow. 119899. Russia). — Seventy seven considered as valid ampharetids genera include
only 200 valid species. It means one ampharetids genus consist of only about three species or three lime less than other
polychaete genus do. Forty seven genera arc monotypic the highest amount within Polychaeta. An investigation of
individual variation of external morphological (including structure of setae) features, using or proposed for using as
taxonomical ones on specific or generic level shows that some features are distinctly length -related, such features can be
used even at specific level carefully. Other features are not length-related, among them are features of specific, generic or
higher levels. Some features are age-related and variation of them in adults reflects preservation of juvenile conditions.
And minimum one feature is length-related in some genera and is not length-related in other ones. An investigation of
rules of interspccilic variation of a feature, an estimate of relation and correlation between features, leads not only to
more precisely specific description, but also at present time allows to determine the taxonomical value (to do feature
weighting) almost of all external morphological features. One of the basis idea of this estimate is: if a variation of a
feature is intraspecific this feature cannot be used for generic classification. Despite the idea is obvious, it immediately
crashes modern system. It is offered to base generic classification on following characters: within Ampharetinae a type
of prostomium and a type of modification of thoracal segments, amount of branchiae; within Melinninae
presence/absence of dorsal hooks and crest. vSuch features as amount of thoracal setigers and uncinigers. branchial
structure, all features of abdomen and above this within Ampharetinae degree of the paleac developing, and within
Melinninae amount of the branchiae, presence of buccal tentacles of different size and amount of dorsal crests and hooks
should not be used for this porpoise. As a result near 1/3 of the whole number of ampharetids genera (at least 25) have to
be turn to junior synonyms. Some features allow to group genera and make conclusions about the most possible ways of
evolution within ampharetids and theirs relations with other Tcrebellomorpha and group Ampharetinae in four tribes.
THE ULTRASTRUCTURE OF A GUTLESS ANNELID. PARENTERODR/LUS G. N. TAENIOIDES (= ASTOMUS
TA ENIOIDES)( POLY CM AET A, PROTODRILIDAE). JOUIN-TOULMOND. C. — (Univcrsite Paris VI. 4 Place Jussieu. 75252
Paris Cedex 05 et Station Biologique CNRS-UPR 4601. 29680 Roscoff Cedex, France). An ultrastructural
investigation of the mouthless protodrilid Parentcrodrilus laenioidcs (JOUIN, 1979) shows that the residual gut. with its
very narrow, ciliated lumen has lost any digestive function. Salivary glands are retained in some anterior segments and
RESUMES - ABSTRACTS
627
their canals converge in a ventral area of the prostomium and open at the epidermal surface. The epidermal ciliation is
much more developed than in any other protodrilid species. In the middle and posterior body segments, the enlarged
epidermal surface area is covered by a cuticle bearing an array of epidermal microvilli which probably are the site of
active transport of dissolved organic compounds. Tlje presence of numerous subcuticular coated vesicles and lysosomes
in the support cells suggests that particulate material from the ambient milieu is taken up by cndocytosis and finally
digested in the epidermis. The origin and nature of the organic substances that constitute the food of P. taenioides arc still
unknown. Experiments have been made on living animals with ferritin added directly to the seawater and left in contact
with the animals for different times. After a contact of 30 min with ferritin, the epidermis of P. taenioides has few
subcuticular coated vesicles containing ferritin, this substance being already concentrated in endosomes in the apical part
of the epidermal cells and in secondary lysosomes, more basally. There are no symbiotic bacteria in the cuticle,
epidermis or residual gut of P. taenioides. Abundant intracellular crystals in the nonfunctional gut indicate that this
residual organ plays a role in the bioaccumulation of environmental substances which enter the body through the
epidermis. The epidermis is the only absorptive surface of this unique polychaele devoid of both a functional gut and
symbiotic bacteria.
POLYCHAETES OF THE RIA DE FOZ (GALICIA. SPAIN). JVNOY. J. & VitlTEZ. J. M. - (Departamento de Biologia
Animal. Universidad de Alcala de Henares, E-28871 Alcala de Ilcnares, Madrid. Spain). — Polychaele macrofaunal (> I
mm) species distribution and community structure of an intertidal soft-bottom estuary, the Ria de Foz (Galicia, northwest
Spain) was investigated during the years 1984, 1985 and 1986. The sampling programme consisted in two sampling
periods. First period (December 1984 to March 1985) was adjusted to provide adequate information of polychaele species
and consisted of 99 samples widely distributed along the estuary. These samples yielded 9.419 individuals belonging to
40 polychaete species. Manayunkia aestuarina, Alkniaria romijni and Ophelia rathkei were firstly recorded for the
Spanish waters. The analysis indicated that sediment characteristics and tidal height were the most important factors
governing the distribution and abundance of polychaete species. On the second sampling period (June 1985 to April
1986) eight stations were visited at six occasions to know the fluctuations of the most abundant polychaete species (e.
g.. Pygospio elegans, Spio martinensis, Capitella capitata , Heteromastus filiformis , Hediste diversicolor). A total of
38,659 individuals of 38 polychaete species were collected at these 48 samples.
THE EXPERT SYSTEM "NEREIS" FOR POLYCIIAETOUS ANNELIDS FROM FRANCE. JUSSIEN, N.. Verger. V.. Ghjj:i \ P.
& L'HospitaUER. Y. — (Universitc C'atholique de l’Ouest, 3 place Andre Leroy. BP 808. 49008 Angers Cedex 01, France).
In his Faune de France volume on the errantiatc polychaetous annelids, FaUVEL (1923) listed only 15 families (not
counting the parasitic Hislriobdellidae and Ichthyotomidae). There are presently 30 families found along the coast of
France and it was therefore necessary to revise the key to the families for a computerised systematics software program.
The program "Nereis" was developed by "Syspertec" using the language "Xi Plus".
THE TAXONOMY AND COMPARATIVE MORPHOLOGY OF THE GENERA IN THE FAMILY SABELLARIIDAE
JOHNSTON. 1865 (ANNELIDA, POLYCHAETA). KlRTLEY. D.W. - (Florida Oceanographic Society. Hutchinson Island
Coastal Science Center, 890 N.E. Ocean Boulevard. Stuart. Florida 34996. U.S.A.). - An extensive reexamination of
accessible specimens in repositories, personal field collections, and material received through loans and donations
coupled with a critical review of accessible taxonomic accounts in the literature (KlRTLEY, in press) discloses the presence
of certain well defined morphological characteristics within the various genus- and species-groups in the family
Sabellariidae. These anatomical variations can be applied as criteria for the organization of the known taxa into two
subfamilies and some 11 genera. The subfamily Sabellariinae comprehends all the sabellariid genus-groups 3
paralhoracic segments. The subfamily Lygdaminae includes all the known genera of Sabellariidae having four
parathoracic segments (KlRTLEY. in press). This proposed ordering is consonant with the observations of CAULLERY
(1913) who enunciated the same principle in proposing two genus-group names: Pallasia, sensu stricto for those species
with three paralhoracic segments and Tetreres for those species with four. Subsequent authors, notably JOHANSSON (1927)
and HARTMAN (1944) found CaULLERY's usage essentially inappropriate and grouped the known species into the seven
genera recognized at that time. Both authors included the genus Cryptopomatus Gravier, 1908. This name is now
considered to be an invalid synonym of /dan thyrsus Kinberg, 1867 (KlRTLEY, in press). The previously recognized six
genera, namely: SaheU aria Lamarck, 1812; Phragmatopoma Morch, 1863; Idanthyrsus Kinberg, 1867; Lygdams Kinberg.
1867; Phalacrostemnia Marenzler, Gunnarea Johansson, 1927 are complemented by an additional four genera which have
been defined and included in the family. LECH APT & GRUET (1993) have reccnty described yet another previously unknown
genus-group from off New Caledonia in the southwest Pacific Ocean; bringing the number of presendy recognizable
genera to 1 1. The criteria invoked to systematize the nomenclature of the genus groups and the specific characteristics
that define and identify the many species within these genera are outlined and discussed.
THE ORDER AMPHINOMIDA: A REVISION OF THE FAMILIES (ANNELIDA, POLY-CHAETA). KUDENOV. J.D
(Department of Biological Sciences. University of Alaska Anchorage, 3211 Providence Drive. Anchorage. Alaska 99508
U.S.A.). The order Amphinomida (Annelida) sensu Fauchald (1977) is monolypic (Fauciiald. 1974). and strongly
isolated in the class Polychaeta. No other living order or family approaches the Amphinomida. Although this order is
628
ABSTRACTS - RESUMES
well recognized within the class, the assignation of families within can be rather controversial. The basis of this
continuing argument centers on the nature of one’s understanding about this group and personal philosophy (KUDENOV.
1991. 1992). Workers today recognize one of two classification systems. (1) a single family ( Amphinomidae)
representing three subfamilies (Amphinominac. Euphrosininae. Archinominae); or (2) three separate families without
subfamilies. Irrespective of which classification is preferred, the order contains at least one paraphyletic family; its
resolution into monophyletic laxa produces a revised family classification and redistribution of existing genera. The
purpose of this study is to present preliminary results of cladistic analyses based on detailed morphological
examinations of species for 18 of 24 described genera in the order Amphinomida. Type materials were examined
whenever possible. It was sometimes necessary to examine specimens of well known species since those of the type
genus were not readily available. The following genera were examined: Amphinome rostrata (Pallas. 1766); Archinome
rosacea (Blake. 1985); Benthoscolex microcarunculata (Treadwell. 1901); Branchamphinome antarctica Hartman. 1967;
Chloeia Jlava (Pallas. 1766); Euphrosine myrtosa Lamarck, 1818; Euphrosinella cirratoformis (Averincev, 1972);
Euphrosinopsis antipoda Kudenov, 1992; Eurythoe complanata (Pallas, 1766); Hermodice carunculata (Pallas, 1766);
Hipponoa gaudichaudi Audouin & M. Edwards. 1833; Noiopygos crinita Grube, 1855; Paramphinome pulchella Sars,
1872; Paremythoe japonica Gustafson. 1930; Pherecardia lobata Horst. 1886; and Pseudeuiythoe paucibranchiata Eauvel,
1932. Species not included in this study generally reflect the unavailability of specimens; these are discussed. In all, 72
characters including 173 binary and multistate characters-suites were analysed using HENNIG 86. The analysis is
unpolarized since a suitable outgroup does not seem to exist. A cladogram having minimum tree lengths is presented for
the order; Cl and RI values are also reported. Separate groups are recognized and discussed. Transformation series are
presented for each family and genus. Phylogenetic relationships between families and genera are also discussed,
particularly in regards to ideas advanced by GUSTAFSON ( 1930).
POPULATION DYNAMIC OE POLYCI IAJETES IN 'll IE SUBUDAL SOFT BOTTOMS IN IT IE BAY OF SANTANDER (NORT1 1
OF SPAIN). Lastra. M.. Sanchez. A .. Palacio. J. .<£ Mora. J. — (Departamento dc Biologia Animal, Uni vers idad de
Santiago de Compostela, 15706 Santiago de Compostela. La Coruna. Espana). Polychaetes are the dominant taxa in
the softbottoms of the subtidal environments in the Bay of Santander. Its seasonal dynamics takes on an differential
behavior in various environments analized. The inner areas of the bay are occupied by faunistically rich communities,
where Melinna palniata, Spiochaetopterus costdrum and Chaetozone selosa are the main species. The presence of this
tube dwelers Polychaetes (M. palniata and S. costarum) can promote the settling process of many species (YOUNG &
RHOADS. 1971). Ill the terminal inner areas of the bay. the Polychaetes community, settled on clayish sediments, is
similar to (he rest of the inner areas but with an evident qualitative and quantitative reduction. In the areas affected by
harbor dredging activities. C. setosa. Notomastus late rice us. Polycirrus pallid us and Mediomastus fragilis , are the more
abundant species, and its density hardly increase when the dredging activities disappear. In the areas affected by urban
sewage, the community is dominated by subsurface deposit feeders, specially N. laiericeus and Euclyniene oerstedii.
whose densities ranged between 50 and 300 ind. m'2 and make up 60 % of the total density of the community. In the
oceanic influenced area, faunistically dominated by small Crustaceans (amphipods and pagurids). Nephthys cirrosa is the
only Polychaete present during all year, making up the 10 % of the total density in the community, and the 5 % of its
biomass.
BATHYAL AND ABYSSAL S ABELL ARIIDAE (ANNELIDA POLYCHAETA) FROM NEAR NEW CALEDONIA (PACIFIC
OCEAN). LECHAPT, J.P. & KlRTLEY. DAY. (Laboratoire maritime de Dinard, MNITN. 17 av. George V, 35800 Dinard
Cedex, France). — Except for the relatively limited accounts of HoaGLAND (1920). TREADWELL (1926). CaULLERY (1944)
from the Philippines and Indonesia, and that of GIBBS (1971) from the Solomon Islands, the benthic polychaete fauna
from great depths of this geographic area remains poorly known. New information has been provided by study of benthic
collections made during several French cruises conducted in recent years near New Caledonia. Specimens described in this
work were collected during the BIOCAL and BIOGEOCAL cruises in 1985. which were organized by the Museum National
d’Histoire Naturelle. The material was received from the "Centre National de Tri" (Brest, France). All of the 488 specimens
in the collection, collected from depths between 440 and 1.870 m. belong in the subfamily Lygdaminae defined by
KlRTLEY (in press). This group is characterized by the presence of four paralhoracic segments. Among these specimens we
are able to identify a total of four genera, including the newly described genus Baihysabellaria Lechapl & Gruel. 1993.
and six species which are thought to be new to science. The collection includes a new species in the genus Lygdamis
Kinberg. 1867; two new species in the genus Phalacrostemma Marenzeller, 1895; a new species in the genus Tetreres
Caullery. 1913; and two new species in the new genus Bathysabellaria. Sabellariids, like most benthic organisms, appear
to be uniquely adapted and constrained to relatively restricted biogeographic and depth domains. In the sabellariid groups
apparently restricted to the near shore "surf zone this stenotopic habit is emphatically demonstrated.
NEREIS RIISEI GRUBE 1857 (POLYCHAETA. NEREIDIDAE): RELATIONSHIP BETWEEN BODY LENGTH. SPECIES
SPECIFIC CHARACTERS, AND REPRODUCTIVE STATE. LONG, C.D.& SCHOENER, A. — (The Buffum Group. 21 1/2
Buffum Street, Salem. MA 01970. U.S.A.). Specimens of Nereis riisei Grube. 1857 (limited to the Caribbean and
associated waters) from museums in Europe and the United Slates were studied for relationship between body length and
Source : MNHN. Paris
RESUMES - ABSTRACTS
629
(1) number of paragnaths (by area), (2) appearance of the first notopodial falciger in asexuals, (3) reproductive slate, and
(4) development of sexual products.
SOFT BOTTOM POLYCIIAETES FROM THE WESTERN COAST OP BAJA CALIFORNIA SUR, MEXICO: ON IJ PHI DAE.
LEON -GONZALEZ, J.A. DE. (Laboratorio de Zoologia dc Invertebrados. Eacultad de Ciencias Biologicas. Universidad
Autonoma de Nuevo Leon, Apartado Postal 5. Sue. "F". San Nicolas dc los Garza. Nuevo Leon. 66451 Mexico). — Eleven
species and four genera of Onuphidae have been identified from the soft bottom environment along to the western coast
of Baja California Sur. Mexico, in the continental shelf at 40 to 220 m depth: Diopatra farcillonemis Fauchakl, 1968.
Diopatra mexicana n. sp.. Diopatra obliqua Hartman, 1944. Diopatra ornala Moore, 1911. Diopatra splendidissima
Kinberg. 1857. Kinbergonuphis cedroensis (Fauchald. 1968), Kinbergonuphis pulchra (Fauchald. 1980), Mooreonuphis
nebulosa (Moore. 1911). Mooreonuphis pumae n. sp., Onuphis eremita parva Berkeley & Berkeley. 1941, and Onuphis
vexillaria Moore, 1911.
POLYCHAETA (HARD BOTTOMS) FROM THE CHAFARINAS ISLANDS (SPAIN). Lopez. E. & San Martin, G.
(Departamento de Biologia. Unidad de Zoologia. Facultad de Ciencias, Universidad Autonoma dc Madrid, Canto Blanco.
28049 Madrid. Spain). The Chafarinas Islands are a very small Spanish archipelago in the Mediterranean Sea. placed
in front to Morocco and Algeria borderline. These islands are almost uninhabited so they are very well preserved. Because
of their location in the Mediterranean Sea. both Atlantic and Mediterranean influences can be expected, but no studies
have been made on benthic fauna. A project for the study of benthos of hard bottoms is being made at present, suported
by a grant of the "Comision Interininisterial de Ciencia y Tecnologia". In this contribution, we present the results of the
first year of resarch. A provisional list of about 130 species of polychaetes identified until now is given. Also two
schematic profiles of typical hard-bottom communities at the Chafarinas Islands are given. Descriptions of two new
species are being prepared. The description of Exogone (Parexogone) sp.. that has been found also in the Italian coasts,
is being made in collaboration with Drs. P. Lanera & P. SORDINO. Pionosyllis sp. has been found only in Chafarinas
Islands.
ERRANT POLYCHAETES FROM THE CAPE VERDE ISLANDS. Lopez E. & San Martin. G. — (Departamento de Biologia.
Unidad de Zoologia. Facultad dc Ciencias. Universidad Autonoma de Madrid, Canto Blanco, 28049 Madrid). In August,
1985 the "I Expedicion Iberica" to the Cape Verde Islands was undertaken. In that expedition samples of algae and sand
for the study of some invertebrate taxa, among them the Polychacta, were collected. The list of collecting stations and a
map with their locations are given. In this contribution we present the results of the studies of the "errant" families of
polychaetes. Seventy two species, belonging to 15 families, arc recorded; 37 species are new records for the Cape Verde
Islands, 12 of them arc, furthermore, new to the region of the East Atlantic between Canary Islands and the Gulf of
Guinea. A new species of Dentatysyllis Perkins, 1981 is described. Other interesting species, all them new records for the
Cape Verde Islands, are Acholoe orbiculata Treadwell. 1921; Lumbrineris crassidentata Fauchald. 1970; Opysthosyllis
viridis Langerhans, 1879; Mirianida sp.; Syllis coraUicoloides Augener, 1924; Eusyllis kupfferi Langerhans. 1879;
Pionosyllis gesae Perkins, 1981; P. spinisetosa San Martin, 1990; P. procera Hartman, 1965; Exogone (Exogone) lourei
Berkeley & Berkeley, 1938; Exogone (Sylline) naidinoides Westheide, 1974 and Sphaerosyllis magnidentata Perkins,
1981.
WHY DO A FEW POLYCHAETE FAMILIES ACCOUNT FOR SO MANY POLYCHAETE GENERA? MCHUGH, D. & FONG,
P.P. — (Biology Board, University of California. Santa Cruz. CA 95064. U.S.A.). — Within most taxonomic
assemblages one or a few taxa dominate in terms of numbers of subtaxa. Recently. MaRZLUFF & Dial (1991) suggested
that non-random patterns in taxonomic domination may be linked to life history traits that promote speciation and
reduce extinction rates, i.e., short generation time and high resource availability. We investigated the phenomenon of
taxonomic domination in the class Polychaeta. The class has about 80 families. 1.000 genera, and 7.000 species. The
family Polynoidae accounts for > 8 % of all polychaete genera, and almost 30 % of all genera belong to just five of the 80
polychaete families (Polynoidae, Ampharetidae. Terebellidae, Syllidae and Serpulidae). Data for several genera in 20
families were collected on body size, egg size, fecundity, age at first reproduction, and life span. There is no significant
con-elation between body size and taxonomic diversity of families. Dispersal potential, as interpreted from egg size, also
fails to explain the observed pattern of taxonomic domination. Our results indicate that there are significant negative
correlations between age at first reproduction and life span, and the diversity of polychaete families.
NEW RECORDS OF THE TEREBELLID AULOPI 10RE LARVAE FROM H IE FRENCH COASTS. MaRCANO, G. <£ BtbWD, M.
— (Laboratoire d’Oceanographie Biologique, 2 rue du Professeur Jolyet, 33120 Arcachon. France). Planktonic
Terebellid larvae collected in the Bay of Banyuls (Western Mediterranean) are accorded to the genus Laimia. The term
aulophorc describes a pelagic larval stage bearing a transparent tube. These larvae, regularly observed since many years,
were wrongly reported to be Lattice conchilega. The presence of a very large gelatinous lube without a well defined form
in Loimia and the presence of a smaller, more rigid and well outlined gelatinous tube in Lanice is the main difference
between the two genera. Other distinctive features are the pattern of the ocular spots, the body shape and the type of
uncinial plates. Some specimens of a third larval type, already described for the French Atlantic coast as Lanice sp, have
630
ABSTRACTS - RESUMES
also been observed. Only L conchUega has been recorded from the numerous benthic samples taken in these areas, thus
the recording of two new types of Terebellid aulophore larvae confirms the value of taking planktonic larval samples in
increasing the faunistic knowledge of a region. In addition, larval research is important in assessing the biogeographic
area of a species as larval dissemination may prevent or allow mixing of species populations.
ADULT ABUNDANCE, RECRUITMENT AND MORTALITY IN A SERPUliD POLYCHAETE COMMENSAL WITH FIRE
CORAL IN BARBADOS. MaRSDEN, J.R. (The Bellairs Research Institute. St. James. Barbados). The 7-spined
morphotype of Spirobranchus polycerus appears to be an obligate associate of live coral, occurring most commonly on
Millepora complanala. It is reproductively isolated from the 2-spined morphotype and is hermaphrodite, whereas the 2-
spined form is gonochoristic. A study of adult abundance and net recruitment on single blades of coral show that these
parameters arc significantly lower at SMB. the northernmost of four reefs studied. At MB. the southernmost reef,
variation in adult abundance depends largely on variation in mortality rather than recruitment. The converse is true at the
other reefs. At Us, variation in recruitment depends largely on variation in blade base perimeter, i.e. on space available
for recruitment. At the other reefs variation in recruitment depends largely on variation in the availability of recruits, i.e.
on the availability of settling larvae and the survival of juveniles. At SMB low adult abundance appears to be the
consequence of a recruitment limited to the past 1-4 years, rather than 5-12 years as at other sites. This situation is
consistent with a population extending northward along the west coast of Barbados and with colonization of northern
reefs dependent upon a pool of larvae produced on southern reefs where larval availability is high. A study of the
distributions of blade height and worm tube aperture diameter indicates that, although worms may live for up to 12-14
years, most of them do not survive for more than two years, due to the destruction of tall (old) blades of coral by wave
action. Possibly, simultaneous hermaphroditism in S. polycerus may have co-evolved along with the commensal habit,
since the latter results in a discontinuous distribution on a short-lived substrate, a situation commensurate with difficulty
in achieving fertilization in the gonochoristic condition.
CHANGES IN POLYCHAETE POPULATIONS FOLLOWING TERMINATION OF A SLUDGE DISCHARGE LOCATED IN
SOUTHERN CALIFORNIA. Martin. A.. Phillips. C.A.. Dojiri, M. £ Thompson. B. - (City of Los Angeles, Hyperion
Treatment Plant. Environmental Monitoring Division, 12000 Vista del Mar. Playa del Rey, CA. 90293, USA). — For
thirty years the City of Los Angeles disposed digested sludge from the Hyperion Wastewater Treatment Plant through a
submerged outfall into the Pacific Ocean. The sludge was discharged at the head of a submarine canyon located in Santa
Monica Bay, an embayment of the southern California coastline. Changes in polychaete populations reflect
environmental conditions before and after termination of the sludge discharge. Three undescribed species of
Ophyrotrocha were most abundant prior to termination and decreased in abundance post-termination. Subsequently, other
opportunistic species colonized and dominated the area as sediment conditions improved. Post-termination sediment
conditions were characterized by lower levels of contaminants, such as sulfides, chlorinated hydrocarbons, and some
trace metals. As conditions improved from degraded (very high contaminant levels) to polluted (high to moderate
contaminant levels), Capitella capilata dominated the area. As recovery continued Peclinaria cciliforniensis became the
dominant polychaete, representing a benthic community transitional between polluted and natural conditions.
MACROINFAUNAL POLYCIIAETES OF A MEDITERRANEAN, SHALLOW-WATER BAY: A HIERARCHICAL
APPROACH. Martin. D. & PaLaCIN. C. — (CenUe d'Estudis Avansals de Blanes. Cami dc Santa Barbara s/n, E- 17300.
Blancs, Girona, Spain). Descriptive studies of the biosphere are organized hyerarchically by a series of successive
integration levels. Among these levels. Ecology deals mainly with the Ecosystems, Communities and Populations. This
hierarchical approach was applied to our investigations, using the Annelida Polychaeta as a biological descriptor: the
entire bay was spatially mapped (ecosystem), some of their components (communities) were seasonally described and
dynamics of single species (populations) were analyzed through lime. The study was carried out in Alfacs Bay (Ebro River
delta), a semi-enclosed shallow-water area which is located in the North-East coast of the Iberian Peninsula (North-
Western Mediterranean 40° 33’-38' N. 0° 32'-44' E). Alfacs Bay can be characterized as a "paralic" environment (sensu
GUELORGET & PERTUISOT. 1983). In the ecosystem level, the spatial pattern of the benthic communities of the bay
was desen ved and correlated with the environment. Four communities were identified: clean-sand, stressed-mud. deep
central-mud and a boundary community (placed between the first two communities and the deep one). Seasonal patterns in
clean-sand and stressed-mud communities were descrived and analyzed in relation with the environment in the
community level. The former showed higher species richness and biomass, and a less fluctuant composition. The
latter was mainly characterized by higher abundances (Autumn to Spring) followed by a practically total defaunation
(eaily Summer). Finally, population dynamics of the two more representative Polychaeta species of the stressed-mud
community, Capitella capitala (Capitellidac) and Slreblospio shrubsoli (Spionidac). were analyzed in the population
level. Both were opportunistic species, with annual life-cycles and constant recruitment (lower in winter) in the bay. A
single population of S. shrubsoli (production of 7.16 g. m‘2. average biomass of 4.10 g. nr2, and P/B of 1.99) and two
ditierent populations of C. capitala (productions of 2.90 and 20.76 g. nr2, average biomasses of 0.38 and 5.06 g. nr2,
and 1>/B of 7.70 and 4.10. respectively), were identified and followed annually. The population level involves certain
degree ol simpliiication. because dynamics of a single-species population is always related to. and controlled by, the
Source : MNHN. Paris
RESUMES - ABSTRACTS
631
other components of the community. Nevertheless, one must consider it as a good tool to quantify, pcrmiting to go hack
towards a more precise view of the community and ecosystem levels.
COMPARATIVE FEEDING BIOLOGY OF TWO VICARIOUS SPECIE S OF THE MACOMA BALTHICA COMMUNITY,
NEREIS VIRENS AND HEDISTE ( NEREIS ) DIVERSICOLOR. MASSON, S.. Olivier. M., DESROSIERS. G. & R EH ERE. C. —
(Centre d'Oceanographie de Rimouski. Departement d’Oceanographie. Universite du Quebec a Rimouski. 310 allee des
Ursulines. Rimouski . Quebec. Canada G5L 3A1). A study on sharing out trophic rcssources have been realized on two
vicarious species of the Macoma baltltica tidal Hat communities. Nereis virens from the lower St Lawrence estuary
(Canada) and Hediste diversicolor from the bay of Mont Saint-Michel (the English Channel). The species gut contents
analysis revealed that both diet varies with field conditions and also individual ages. Juveniles of both species are
essentially deposit feeders and N. virens adults are almost exclusively carnivorous. Diet temporal variations which are
observed in the different habitats showed opportunistic features of these nereidians. It could play an important part in the
mixing mechanisms of the particulate organic matter. N. virens adults, throughout the predatory relationship and
cannibalism are susceptible to occur in the regulation of the population of this oligospecific estuarine community.
TEMPORAL CHANGES IN T1 IE POLYCHAETE COMMUNITY AT AN ABANDONED SALMON FARM SITE. MiUJiR REITER,
C.L. — (Department of Biology. University of Victoria. P.O. Box 1700. Victoria. B.C. V8W 2Y2 Canada). — The
polychaete community was studied at an abandoned salmon farm site (following 2.5 yrs of operation) at Village Bay,
Quadra Island. British Columbia. Benthic samples were collected for macrofauna and sediment analyses six wks. six
months and one yr following closure of the facility. Initially the polychaete community at the farm was dominated
almost exclusively by one capilellid species. After six months this species continued to dominate, but after one year the
numbers approached those recorded at the reference station. Although species richness at the farm site increased during
the course of the study it was lower than the reference station after one year. Analysis of sediment TOC and TON
concentrations also indicated that partial recovery had taken place after one year of abandonment. Data analyses are
ongoing with the ABC method (abundance, biomass comparison: Warwick. 1986). multivariate analyses and
comparison of functional (trophic) groups; but preliminary results based upon 95 % of the total individuals (113 species)
indicate that the polychaete community at the abandoned farm site changed very rapidly over the six months to twelve
months period. After one year the farm site supports a transitional community which is characteristic of the "transitional
zone" described by PEARSON & Rosenberg's (1978) SAB diagram (of community changes in a gradient of organic
enrichment): low to moderate richness, low biomass and low to moderate abundance.
DISTRIBUTION OF THREE NEREID POLYCHAETES IN RELATION TO SULFID CONCENTRATION WITHIN THE
SEDIMENT IN DANISH COAST AL WATERS. MlRON, G. & KRISTENSEN, E. — (Institute of Biology. University of Odense.
Campusvej 55. DK-5230 Odense. Denmark). - Results from field data (Kerteminde Fjord and Vellerup Vig. Denmark)
suggested that hydrogen sulfid in the sediment influence the spatial distribution of the nercid polychaetes Nereis virens.
N. succinea and Hediste diversicolor. Analysis showed that N. virens is confined in low sulfidic areas while N. succinea is
found in high sulfidic sediments. H. diversicolor , on the other hand, showed a broader distribution in respect to hydrogen
sulfid. Laboratory tank-experiments, however, indicated that all three species prefered non-sulfidic sediments in
allopatry conditions. Preliminary results also showed that //. diversicolor was excluded from the tanks non-sulfidic side
in sympatry conditions with each of the other two species. N. virens equally shared the non-sulfidic side with N.
succinea. However, in these conditions, only N. succinea was found in the sulfidic portion of the tank. Overall. N. virens
was the least tolerant species while the other two species showed some sort of adaptation in regard to sulfidic conditions.
Results finally illustrated that competition between H. diversicolor and the other two species was high, particularly with
N. succinea. Differences between field data and results from the laboratory tank-experiments, however, suggest that the
distribution of N. succinea may also be dependant on other factors.
POLYCHAETE DISTRIBUTION AND COMMUNITY STRUCTURE ALONG A SALINITY GRADIENT’ (CANAL DE MIRA,
RIA DE AVEIRO. PORTUGAL). MOREIRA , M.H.. FlGUEIRA. E. M. & Cuniia. M. R. (Universidade de Aveiro, Campo de
Santiago. 3800 Aveiro. Portugal). The species composition and structure of the polychaete community of Canal de
Mira (Ria de Aveiro) were studied. Four seasonal sampling surveys were carried out between December 1985 and
September 1986. At each survey, samples were collected in a total of 40 stations (21 intertidal, 19 subtidal), distributed
over 13 transects covering a distance of 21 km and a salinity range from 35 P.S.U. to 0 P.S.U. A total of 47 species were
recorded. Structural indices (number of species, density and Shannon- Wiener diversity index) were determined for each
station and sampling occasion. A cluster analysis was performed using Morisita similarity index. For each of the five
groups of stations suggested by this analysis, the polychaete community was characterized using the average values of
the structural indices (average number of species per station and sampling occasion = AVS: average number of individuals
per square meter = AVD: average diversity = AVH') as well as the constancy, fidelity and relative dominance of the species
present. In intertidal and shallow areas at the lower reaches of the channel (Group A), with fine sediment and high
salinity, the number of individuals and species and the diversity is high (AVS = 12.1; AVD = 1.459.6; AVH’= 2.26)
and the polychaete community shows low dominance of the most abundant species (Heteroniastus fdifonnis. Tharyx
marioni, Owenia Jus form is). In deeper areas with coarser sediment and more intense hydrodynamic conditions (Groups E
632
ABSTRACTS - RESUMES
and B). the impoverished community (Group E: AVS = 2.4. AVD = 38.3. AVH' = 0.93; Group B: AVS = 4.6.
AVD = 263.3. AVIT =1.33) is strongly dominated by one species (Nephthys cirrosa and Scoloplos anniger
respectively). In the middle and inner sections of the channel (Subgroups Cl and C2 and Group D). with high tidal and
seasonal salinity variation, diversity, species richness and abundance gradually decline (Subgroup Cl: AVS = 5.3.
AVD =1451.8. AVH' = 1.04; Subgroup C2: AVS = 3.2, AVD = 769.3, AVIT = 0.99; Group D: AVS = 1.0,
AVD = 289.5. AVH* = 0.0) and the community becomes strongly dominated by euryhaline species ( Hediste
diversicolor and Amage adspersa ). The results point out the influence of both salinity and hydrodynamic conditions as
ihe main structuring factors of the polychaetc community.
NOTEWORTHY COLLECTION RECORDS OF POLYCIIAETES FROM ESTUARINE AND NEAR COASTAL WATERS OF
THE U.S. MID-ATLANTIC REGION. MOUNTFORD, N.K.. Morris. C.T & Arcuri. S.L. — (Cove Corporation. 10200
Breeden Rd.. Lusby, MD. 20657. USA). Noteworthy collection records of polychaetes from coastal waters of the U.S.
mid-Atlantic region are presented. These include: (1) northern or southern range extensions for eight species. (2) the first
report of two species from the east coast of North America, and (3) the discovery of three species new to science. The
significance of this presentation is to disseminate useful taxonomic information to the scientific community.
EVIDENCE OF A CADMIUM BINDING PROTEIN IN ALLOLOBOPHORA CALIGINOSA (ANNELIDA. OLIGOCIIAETA):
DISTINCTION FROM M ETALLOTHIONEINS AND HOMOLOGIES WITH HEMERYTHRINS. Nfjmeddine, A.. Baert. J.L .
SAUTlkRE, P. & DHAINAUT-COURTOIS, N. (Universite Cadi Ayyad, Faculte des Sciences de Marrakech I, Morroco). —
Among annelids, earthworm oligochaetes generally show a good tolerance for heavy metal contaminants and. to the best
of our knowledge, only metallothioneins (MTs) have been reported to play a role in the detoxification process (MORGAN
el al.. 1989). Previous studies have showed that the oligochaete A. caliginosa . collected from the sewage spreading fields
in the city of Marrakech (Morroco), presents a good tolerance to heavy metals and accumulates high level of Cd, Zn and
Cu (SEDKI. 1990). We have thus investigated the detoxification mechanisms in this species. Following gel filtration
chromatography on Scphadex G75, one Cd-binding peak was detected in an extract from A. caliginosa contamined with
cadmium. Two subsequent cation-exchange chromatograhies allowed the purification of Cd-binding protein which was
called Cd-BP14. This protein is a monomer with a molecular weight of 14 kDa and has an isoelectric point of 6.5.
Althrough this molecular weight is rather similar that of MTs. a comparison of the amino acid composition revealed
several major differences. Indeed, while MTs have a high cystein content (>30 %), cystein was present in Cd-BP 14.
Fulhermore, CD-BP 14 contains a high level of aromatic acids (11 %) and histidine (6 %), amino acids not present in
MTs. A marked difference also occured between Cd-BP 14 and MTs when the level of bound metal was compared. On the
basis of these results we conclude that Cd-BP 14 is different from metallothioneins described in mammals or other
invertebrates. lo our knowledge, such a Cd-binding protein has never been described in oligochaete annelids. On the
basis of the characteristics described above, Cd-BP 14 is similar to an Cd-binding protein (MP II) isolated from an
annelid polychaete Hediste diversicolor (Nejmeddine el al .. 1988). This analogy was confirmed by the determination of
the first 33 amino acids al the NII2 extremity of Cd-BP 14 which revealed 61 % homology with the N-terminal part of MP
II (Demuynck ci al.. 1991). The N-terminal sequence of Cd-BP 14 shares also 40 to 65 % homology with that of
sipunculid hem erythrins, non-heme iron-binding proteins. Phis homology with hemerythrins was confirmed on the
basis ol characteristics including molecular mass, iron content UV/visible spectrum, amino acid composition and
immunological cross-reaction using antibody against Cd-BP 14. Homology between hemerythrins and MP II from H.
diversicolor . marine animal, has been described (DEMUYNCK el al.. 1991). By contrast, to our knowledge, it is the first
time that homology between hemerythrins and a protein from a terrestrial animal is reported.
TROPHIC RELATIONS BE’ TWEN POLYCHAETOUS ANNELIDS AND BRACHYURAN CRABS IN THE SOUTHERN
BRAZILIAN COAS I Nonato. L.F. . Pe/TI. M.A.V. & Paiva , P.C. — (Institute Oceanografico, Universidade de Sao Paulo.
Pia<?a do Oceanografico, 191-05508, Sao Paulo, SP. Brazil). — The polychaetous annelids constitute an important
leeding resource tor several species of the benthic and demersal marine fauna. The group is of particular interest since
through the family recognition it is possible to obtain various information regarding their feeding behavior and
motility: detritivores (deposit and suspension -feeders) arc generally sessile or discreetly motile, carnivores and
omnivores normally have greater locomotion capabilities. Considering that the brachyuran crabs are the main
meg a be nt hie group and the polychaetes the main macrobenthic group in the studied area, their inter-relations arc
fundamental lo the understanding ol the local trophic web. In this way the contribution of the polychaetes to the diet of
the main brachyuran crabs species was studied on the inner shelf (between 10 and 42 meters depth). 2.715 stomachs
belonging to six species ( Persephona medilerranea. Ponunus spini/nanus. P. spinicarpus. Callinecles ornatus. Hepaius
pudibundus and Libinia spinosa) were analysed. Out of 1,815 stomachs whose contents were indentifiable. 513 had
polychaetes, with considerable variations between the different species. Notwithstanding the identification of the
leeding content in brachyuran crabs being made difficult by the process of ingestion and trituration, regarding the
polychaetes the task is facilitated by the presence of certain structures more resistant to digestion such as setae, uncini,
hooks, mouthpieces and opercula. 30 families, 15 genus and five species were determined. 28.6 % of the polychaetes
encountered could not be identified. 26.6 % were carnivores, mainly of the order Eunicida; 39.9 % were deposit- feeders,
mainly Capilellidae, Maldanidae and Terebellidae; 3.6 % were suspension-feeders (families Sabellidae and Serpulidae) and
Source : MNHN. Paris
RESUMES - ABSTRACTS
633
1.3 % were omnivores. In Persephona mediterranea the greatest occurrence of polychaetes was found (in 80.3 % of the
stomachs). The deposit- feeders, the most abundant polychaete trophic group in the area, where the commonest food item
for the brachyuran crabs, except for Poriunus spinicarpus and Caliinecles ornatus in the stomachs of which the carnivores
were more important; this, probably, ow'ing to a great predating capability of these agile Portunidac.
NEW RECORDS AND ZOOGEOGRAPI IICAI . STUDY OF THE FAMILY NEREIDIDAE FROM CANARY ISLANDS. NUNEZ J.
— (Facultad do Biologicas. Departamento do Biologia Animal, Universidad de La Laguna, 38206 La Laguna. Tenerife,
Canary Islands, Spain). — The family Nereididae is represented in the Canary Islands by three subfamilies,
Nothophycinae, Namanereidinae and Nercidinae, and 18 species belonging to nine genera. Micronereis (one spec.).
Lycastopsis (one spec.), Websterinereis (one spec.), Rullierinereis (one spec.), Nereis (two spec.). Ncanthes (four
spec.), Ceralorereis (two spec.). Peri nereis (four spec.) and Platy nereis (two spec.). In this paper, three species
previously unknown from Canarian waters are recorded. Neanthes fucatci (Savigny, 1820), Ceraionereis vittata
Langerhans, 1884 and Platynereis coccinea (Delle Chiaje, 1841), Juvenile specimens of Nereis funchalensis.
(Langerhans. 1880) are described; they are very similar to N. jacksoni Kinberg, 1866 (Hutchings & Turvky, 1982).
Perinereis taorica Langerhans, 1881 is redescribed from 15 specimens, from Puerto de la Cruz, the type of this species
described from the same area having been lost. In addition, a illustrated key and zoogeographical analysis of the family is
maked.
COMPARATIVE STUDY OF THE PROVENTRICULUS IN FOUR SPECIES OF SYLLINAE (POLYCHETA. SYLUDAE).
OCANA, 0 .. Nunez, J. <£ Talavera, J. A. — (Facultad de Biologicas. Departamento de Biologia Animal, Universidad de La
Laguna. 38206 La Laguna, Tenerife, Canary Islands, Spain). — The proventriculus is used as taxonomic character in the
family Syllidae (size, morphology and number of the muscle cell rows). Nevertheless, these studies are usually about
external morphology. A proventriculus morphology-microscopy study is given for four representative species of sy I lids
collected in Canary Islands ( Haplosyllis spongicola, Syllis arnica . S. gracilis and S. armillaris).
ECOLOGICAL DISTRIBUTION AND SEASONAL VARIATION OF SUBTTDAL POLYCHAETES POPULATIONS IN THE
MONDEGO ESTUARY (PORTUGAL). Pardal, M. A., Marques. J. C. & Bellan, G. (Departamento de Zoologia. Fac.
Ciencias e Tecnologia, Universidade de Coimbra, 3049 Coimbra Codex. Portugal). The Mondego estuary is under
severe environmental pressure, essentially due to human activities. It consists of two arms, north and south, with very
different hydrographic characteristics. The north arm, which is the location of Figueira da Foz harbor, is deeper, while the
south arm is almost silted up in the upstream areas. This causes the fresh water to flow essentially by the north arm, while
the circulation in the south one is mostly due to tides and to the usually small fresh water input of a tributary, the Pranto
river. In addition, due to differences in depth, the tidal penetration faster in the north arm, which causes daily changes in
salinity to be much stronger, whereas daily temperature changes are higher in the south arm. The type of substrate is also
clearly different in both estuarine arms. In the north one bottoms are mainly composed of medium to coarse sand, with
low fractions of organic matter, while muddy bottoms with higher fractions of organic matter are predominant in the
south arm. particularly in the upstream areas. Fine to medium sand bottoms can also be find in downstream areas of the
south arm. Despite of the increasing environmental pressure, there was no reference data on the Mondego estuarine
system until 1985, namely for the biological communities, from which the impact of human activities over the structure
and functioning of the ecosystem could be assessed. From 1985 to 1990 a general survey of the benthic communities was
carried. The aim was to characterize the macroinvertebrate communities structure in relation to the physical and chemical
environmental parameters and to identify the most important species in the observed structure (number of individuals and
biomass), which might have a key role in the ecosystem functioning. The present paper was based on data from a
sampling program over the subtidal communities carried out from December 1989 to September 1990. Samples provided
about 4.800 polychaetes from 20 species. Aniage adspersa was the most abundant species (maximum of 4.1 15 ind. m - in
June 1990). representing 79.8 % of the sampled specimens. However, it was found almost exclusively in the south arm of
the estuary and in the Pranto river. Streblospio shrubsolii was the second most abundant species (9.8 % of the sampled
specimens) being found in all the studied area. Capitella capitata and Poly do ra ciliaia , both considered as indicators of
organic pollution, were found only in the south arm and in the Pranto river. Hediste diversicolor was found almost only in
the upstream areas of the north arm. presenting relatively small densities (maximum of 464 ind. m'~). A comparison with
previous data allowed to think that it is decreasing both in density and area of distribution. Nevertheless, this fact needs
further confirmation. Five species. Nepluys cirrosa, N. longosetosa, N. hombergi, Eulalia sp.. and Lag is koreni were
found only near the mouth, were the marine influence is stronger. Species richness changed seasonally, with a maximum
in the summer (14 species in September) and a minimum in the winter (eight species in March). The highest populations
densities were found in late spring (June) (54.6 % of the total number of individuals sampled). Species richness and
population densities were clearly lower in the north arm, mainly due to bottom disturbance related to the harbor facilities,
and probably to strongly daily variations in water parameters. The south arm. where the circulation depends mainly on
tides, despite of more organic pollution, lower dissolved oxygen levels, and higher nutrients concentrations in the water,
still presents higher species richness and populations densities. In a general way, the species richness in the Mondego
estuary is low in comparison with data from other studied estuarine systems.
634
ABSTRACTS - RESUMES
PSEUDOCIRRATULUS KINGSTON ENSIS AUGENER. 1922: NOT A CIRRATULID BUT AN ANNELID OF UNCERTAIN
AFFINITIES (POL YCI I AETA?: PSEU DOCI R R ATU LIDA NEW ORDER, PS EU DOCI R R ATULI DAE NEW FAMILY).
Petersen . M.E. — (Zoological Museum, University of Copenhagen, Universitetsparken 15. DK-2100 Copenhagen 0.
Denmark). Pseudocirratulus kingstoncnsis Augener, 1922, from the intertidal zone of the West Indies, is an
earthwormlike species described from a few large specimens questionably assigned to the polychacte family Cirratulidae.
No filamentous appendages of any kind were observed, and all setae were reported to be gently curved unidentate hooks.
The species has been known only through the brief, unillustrated original description, the correctness of which has been
doubted. A reexamination of the types and of a nontype specimen recently found in the collections of the Zoological
Museum, University of Copenhagen, has revealed that the species is correctly described but not a cirralulid or referable to
any known family or order of polychaetes; although not an oligochaete (e.g.. the gut is simple and not specialized; none
of the specimens have a clitellum; there are no reproductive organs of oligochaete type), it is most likely to be confused
with earthworms (Oligochaeta: suborder Lumbricina). The species is figured for the first time, redescribed and transferred
to the Pseudocirratulidae, new family of the new order Pseudocirratulida. A lectolype is designated and the affinities of the
species, family and order are discussed.
HERMAPHRODITIC Cl RR ATU LIDS (ANNELIDA. POLYCHAETA) FROM DANISH WATERS, WITH NOTES ON EARI Y
DEVELOPMENT. DESCRIPTION OF A NEW SPECIES OF APHELOCHAETA BLAKE AND REVIEW OF
HERMAPHRODITISM AMONG IHE CIRRATULIDAE. PETERSEN, A EE. — (Zoological Museum, University of
Copenhagen. Universitetsparken 15, DK-2100 Copenhagen 0. Denmark). — Three species of Danish Cirratulidae are
known to be hermaphroditic. Tharyx vivipara Christie, 1984. originally described from estuaries of northeast England,
and Caulleriella fragilis (Leidy. 1855). originally described from under stones at Point Judith. Rhode Island, U.S.A., are
newly reported from Danish waters. Aphclochaeta new species, is new to science. All three species are described and
figured and a key to known species of Aphelochaela is provided. Tharyx vivipara is infaunal, whereas both C. fragilis and
Aphclochaeta n.sp. are cryptofaunal. occurring in crevices in dead mollusc and barnacle shells and other calcareous matter
in Laminaria holdfasts and similar habitats. At least Aphclochaeta n.sp., and perhaps also C.fragilis, brood their young.
Some early stages of both species are described and figured, and C.fragilis is differentiated from C. viridis (Langerhans,
1880) and C.bioculata (Keferstein, 1862). similar species with which it has been confused. The status of Caulleriella
bioculata parva Gillandt, 1979 and Tharyx multibranchis (Grube, 1863) is commented. Hermaphroditism among the
( irratulidae is reviewed and it is suggested that the phenomenon is probably more widespread among Polychaeta than
usually realized. Some problems of dispersal for species with direct development and brood care arc pointed out.
ABUNDANCE DYNAMICS OF MEROPLANKTONIC POLYCHAETE LARVAE AT "HELGOLAND ROADS" (GERMAN
BIGHI). PlATE, S. & Hus EM ANN, E. — (AG Entwicklungsphys. d. Tiere, Lchrstuhl f. Spez. Zool. & Parasitol.. Ruhr-
Universitat Bochum. Postfach 10 2148. D-W-4630 Bochum 1. Germany). — During a three year plankton monitoring at
the island ol Helgoland (German Bight. North Sea) a total of 212 quantitative plankton samples were collected by
horizontal, surface-near hauls twice a week. We observed meroplanktonic polychaete larvae of 57 species out of 22
families. With 15 and height species, respectively, the families Spionidae and Phyilodocidae were the most dominant
members of the polychaete plankton. Highest larval abundances occurred in La nice conchilega (Terebellidae) with 8,870
md. nr . Magelona mirabilis (Magclonidae) with 5,424 ind. nr3, Malacoceros fuliginosus (Spionidae) with 5,250 ind. nr
and Polydora ciliata (Spionidae) with 1.170 ind. m' \ Since the presence of meroplanktonic larvae is a criterion of
reproduction, it is possible to make some conclusions on the timing of reproduction. The meroplanktonic larvae of some
species occurred over more than six months in the plankton of "Helgoland Roads". Examples for species with a semi-
continuous reproduction arc Polydora ciliata (larvae from February to September), Laonice cirrata (Spionidae) (larvae
from May to February) and Ixmice conchilega (larvae from February to November). Larvae of P. ciliata were continuously
present during the whole breeding season, but we recognized two or three main reproductive phases, characterized by
increased larval abundance. Field studies showed a distinct temperature dependence of larval development. At water
temperatures between 1 and 4.5 °C. larval development from the first planktonic stage with three setigers to the 12-
setiger stage look about 70 days. At temperatures from 8 to 1 1.5 °C. only 27 days were needed to reach the same stage.
Short larval appearance, which points to reproduction with distinct gamete releases, was recognized for Eulalia viridis
(Phyilodocidae), Eteone longa (Phyilodocidae), Scoloplos armiger (Orbiniidae), Polydora flava (Spionidae) and some
other species. In many cases, the onset of reproduction showed a temperature dependence. In S. armiger, E. viridis and E.
longa low winter temperatures led to a delayed reproduction. The reproduction of P. flava was found to be adapted to high
water temperatures. Larvae, first occurring in the plankton at the 6-seliger stage, could be observed in August and
September. At this time, temperature reaches its maximum. The occurrence of the larvae was always restricted to a period
°f four weeks. This points to a synchronized reproduction and a short pelagic development. Pomatoceros tnqueter
(Serpulidae) is known for producing ripe gametes throughout the year. During the present study larvae occurred only
between the end of July and the end of October. Reproduction always started at temperatures above 13 °C. The pattern of
larval records pointed to the release of several batches of gametes, which followed a lunar or semi-lunar rhythm.
(POLYCHAETA-PHYLLODOCIDAE). P LEU EL, F. (Natur-historiska Riksmuseet. Box
50007, o- 104 05 Stockholm. Sweden). - The phylogeny of thirteen species of the polychacte genus PhyUodoce is
Source : MNHN. Paris
RESUMES - ABSTRACTS
635
estimated with 26 unordered morphological characters and 60 character states. The genus is large (over one hundred
nominal species) with many poorly known members and the analysis is based on a small selection only. Following
recent, higher-level phylogenetic studies Chaeloparia nilssoni and a selection of Para nail is -species were chosen for
outgroups. Six equally parsimonious trees with a Cl of 0.79 were obtained. The data set is examined for cladistic structure
in a permutation tail probability test, the result ol which clearly indicate presence of non-random, hierarchical pattern.
The genus is reclassified and divided in three subgenera: Phyllodoce, Zverlinum, Anailides, and the hypothesized
synapomorphies arc used for subgeneric allocation of the remaining species in the genus.
EFFECT OF FOOD QUANTITY ON GROWTH AND REPRODUCTIVE CHARACTERISTICS OF CAPITELLA SP.
(ANNELIDA. POLYCHAETA). Qian, P.Y. & CHIA., F.S. — (Department of Zoology, University of British Columbia,
Vancouver, B. C, Canada V6T 1Z4). — Effects of food quantity on growth, fecundity (defined as number of eggs deposited
in the first spawning), egg size, egg energy content, and total reproductive output (total egg volume or total energy
invested in spawned eggs) of Capitella sp. were examined in the laboratory. Results indicate that food quantity affected
fecundity, egg size, egg energy content, and total reproductive output of Capitella sp. Fecundity increased with
increasing food quantity, whereas egg size and egg energy content decreased with increasing food quantity. These results
suggest that there is a trade-off between fecundity and egg quality (in terms of egg size and egg energy content), thus
supporting the hypothesis that when food-limited, polychaetes produce fewer, but higher quality offspring. Results
further show that Capitella sp. is very sensitive to change in food quantity. Minor changes in food quantity (<0.1 mg
dry Ulva. worm*1, day*1) gave rise to measurable changes in fecundity and egg size, suggesting that life history
characteristics in Capitella sp. is flexiable and can be easily modified by environmental factors, such as food quantity.
IN SITU MEASUREMENT OF RECRUITMENT. MORTALITY. GROWTH. AND FECUNDITY OF CAPITELLA SP
(ANNELIDA. POLYCHAETA). Qian, P.Y. CHIA, F.S. — (Department of Zoology. University of British Columbia. B. C.
Canada). Recruitment and mortality of post-larval stages of Capitella sp. were determined in situ at two sites near
Bamfield Marine Station, B. C. Recruiting rates of juveniles into settling trays placed in the mid-intertidal region were
not significantly different at the two study sites, even though larval abundance at one site was about one order of
magnitude higher than that of the other site. This suggests that recruitment in these areas is not affected by larval
abundance. Mortality rate (% loss x day*1) was more than 3 % for young juveniles (body volume < 3 mm3) and less than
0.3 % for larger than ones (> 10 mm3). These indicate that juvenile mortality governs directly recruitment pattern and
population dynamics in our study area. A method of marking polychaetes with vital dye was introduced and this enabled
us to follow the growth and reproduction of Capitella sp. in the field. Growth rale of marked sibling individuals measured
in situ was similar to that of laboratory reared animals. Marked sibling juveniles were succesfully raised in situ to
sexually maturity and their reproductive characteristics measured. Among 147 females developed from the marked sibling
juveniles of a single spawning. 142 individuals produced small numbers of large eggs. On average, each animal produced
764 ± 207 (N = 42) eggs x spawning*1: each egg measured 7.3 ± 0.01 x 10'3 mm3, and contained 88 ± 9.5 microjoules
energy. These large egg developed into lecithtrophic larvae in the adult’s tube. The other five females produced small
eggs that measured 0.63 ± 0.40 x 10 10' 3 mm3, contained 8.6 ± 1.56 microjoules energy, and developed into
plank to trophic larvae that had a pelagic larval life of 2-3 weeks. Mean fecundity of these five individuals was 6.890 ±
3,116 eggs x spawning*1. Plasticity of life-history strategy of Capitella . which has been demonstrated in the previous
laboratory studies, was confirmed in the field.
THE LIFE HISTORY OF THE POLYCHAETOUS ANNELID HALOSYDNA JOHNSON!. REISH, D.J. & Rossi. M.M. —
(Department of Biology. California State University, Long Beach, California 90840-3702. U.S.A.). - The life cycle of
the polynoid polychaete was completed under laboratory and field conditions. Both eggs and sperm were shed free into
the water through the nephridial papillae. The fertilization membrane appeared shortly thereafter with the first cleavage
occurring in one hour. Additional division were rapid at 18° C with a swimming blastula present at four hours. The
trochophore with eyespots was observed at 24 hours and began to feed on phytoplankton at two days. Metatrochophore I
stage was formed by seven days and consisted of seven segments. Metatrochophore II possessed setae, median antenna,
anal cirri, eight segments, and four pairs of elytrae at 12 days. Metamorphosis occurred at day 14 at which time the larvae
consisted of nine setigerous segments and five pairs of elytrae. Worms attained 26 segments at 40 days. 32 at 80 days,
and 37. the adult number, at 100 days. Both sexes spawned at nine months. Settlement of juvenile worms in the field
occurred throughout the year in southern California with peaks occurring in early spring and mid-summer. This is the first
report of rearing a member of Family Polynoidae through sexual maturity in the laboratory .
SPACE OCCUPATION MODALITIES FROM THREE SPECIE S OF TUBICULOUS INTERTIDAL NEREIDS: HEDISTE
(NEREIS DIVERSICOLOR) O.F. MULLER, NEREIS VIRENS SARS AND PERINEREIS CULTRIFERA (GRUBE). RETlLRE,
C.. DESROS/ERS. G., Scaps. P. & Miron , G. — (Laboratoirc Maritime, 17 avenue George V. B.P 28, 35S01 Dinard,
France). Hediste diversicolor and N. virens. two major components of the Macoma balthica oligospecific community,
inhabits muddy sands in shallow estuarine soft-bottoms. Perinereis cultrifera, a widespread species, is found in particular
biotops which correspond to zone ol interface between heterogeneous sediments and rocky substrates. The distribution
Source :
636
ABSTRACTS - RESUMES
modalities of individuals from these three species were studied in the Saint Lawrence estuary (N. virens) and in the
English Channel, on the north coast of Brittany (H. diversicolor and P. cullrifera). On an observation site scale (coves,
intertidal zones), the dimensional structure and the population density of both N. virens and P. cullrifera vary with the
bathymetry and certain sediment characteristics, juveniles occupying preferentially, in greater number, the highest
levels. Differently, juveniles and adults of H. diversicolor coexist on the area occupied by the population. The first
distribution type is probably the result of the swarming of epitokous individuals in flow period, leading to a passive (and
may be active) transport of gravid individuals and/or sexual products of P. cullrifera and N. virens young larval stages
(which pelagic life does not exceed a few hours) to the higher levels of the intertidal zone. A migration in an offshore
direction, during the growth period, could control the structuring of the population. Inversely, the atokous reproduction
of H . diversicolor, with the possibility of egg incubation within the galery inhabited by the female and the liberation of
erpochaetes. restrains considerably the dispersion of the individuals. At small-scale, individuals of these three species
are distributed in patches. Though individuals accept that their feeding area may be forage by congcnerics of the same
size, individuals defend harshly their territory, i.e., their galery which shape and size are related to density. The agonistic
behaviour, expressed in the course of the burrow development within the substrat. appears to be an important factor in
the regulation of populations. It also express itself, at least for H. diversicolor, in migrations, not related to reproduction
or growth, in the water column and contribute to the dispersion of individuals which favors, when they return to the
bottom, encounters between burrow occupants and intruders trying to enter a new burrow. In H. diversicolor, cannibalism
between adults and juveniles could hold an non-negligible role. Thus, it appears that the space occupation modalities
expressed by these three Nereid species are determined by the coupling between reproductive mechanisms and
hydrodynamism and individual behaviour, the former exerting effects and the latter expressing itself at very different
spatial scales.
AMPHARET1 DAE (ANNELIDA, POLYC’HAETA) FROM ANTARCTIC WA FERS, ATLANTIC SECTOR. ROSENFELDT, P. —
(Zoologisches Inslitut und Zoologisches Museum der Universitat Hamburg. Martin-Luther-King-Platz 3, 2000 Hamburg
13, Germany). — The study material was sampled during cruise ANT V/l of the German RV «Polarstcrn» to Antarctica
from May to June 1986. The samples were obtained at 26 stations off the Elephant Island and the Antarctic Peninsular by
van Veen Grab at 9-532 m. Eleven ampharetid species were found, of which ten were known before in the area: Amage
sculp ta Ehlers. 1908; Ampharete kerguelensi McIntosh. 1880; Amphicteis gunneri anlarlica Hessle.1917; Anobolhrella
antarctica (Monro, 1939); Eusamythella sexdentata (Hartman, 1967); Melinna cristata (Sars. 1851); Neosabellides
elongatus (Ehlers.1912); Neosamytha gracilis Hartman. 1967; Parampharele weddellia Hartman, 1971 and Sosanopsis
kerguelensis Monro, 1939. 1 he 11 th species of the genus Asabellides was unknown to science and will be presented here
with detailed illustrations. It is distinguished from congenus by different morphology of its gills, uncini, and lower
number ol abdominal segments (8-11). Two species inhabit the Antarctic/Sub antarctic region, as well as waters of
Southern S. America. Five species arc endemic to Antarctica. One species is of cosmopolitan distribution. The remaining
species inhabit the Antarctic region, as well as waters of South Africa. M. cristata was the most abundant species, with
185 individuals only at Station 142, at 466 in.
EVOLUTION OF REPRODUCTIVE MECI IANISMS IN 'll IE .SAB E LIT DAE (POLYCHAETA). Rouse, G. W. - (Department of
Invertebrate Zoology, Smithsonian Institution. Washington D.C. 20560. U.S.A.). — Polychaeles have a great range of
reproductive mechanisms. However the general assumption persists that polychaeles spawn small eggs and simply
structured sperm into the sea-water; fertilization takes place in the water as does early development through a larval stage:
the trochophore. Ihcse traits have consistently been viewed as primitive. In order to assess whether external
fertilization, concomitant with "primitive" sperm (FranzGn 1956). small eggs and planktonic larvae, has been re¬
expressed (or re-evolved") the study of monophyletic groups with various forms of reproductive methods should be
informative. Recent rigorous cladistic analyses of the Sabellidae by FlTZHUGH (1989, 1991) allow the possibility of
testing hypotheses regarding the evolution of reproductive mechanisms. FlTZHUGH (1989) re-defined two sub-families of
sabcllids, the Fabriciinae and the Sabcilinae. Examination of the cladograms produced by FlTZHUGH indicates a general
trend oi increasing size from small plesiomorphic fabriciins to large apomorphic sabellins. All of the Fabriciinae are
continuous brooders ol directly developing larvae. Sperm storage by females is indicated in every genus (Rouse, 1992).
I lesiomoiphic sabellins such as Oriopsis spp. are also small and have a similar reproductive mechanism to the
Fabriciinae. though the homologies of reproductive structures are unclear. Intratubular brooding is rare in the more
apomorphic sabellins. Broadcast spawning or extratubular brooding (with a dispersal phase) is found in all other genera,
except [qy Pot am ill a and Amphiglena . The most apomorphic sabellins, Eudistylia and Scliizobranchia are broadcast
spawners. The sister group to the Sabellidae is the Serpulidae. Knight-Jones & Bowden (1984) suggested that brooding is
pi imitive for the Sabellida based on the idea that the Spirorbinac, all brooders, are the most primitive of the Sabellida.
However ten Hove (1984) and FlTZHUGH (1989) have shown the spirorbins are the most apomorphic of the Serpulidae.
Plesiomorphic serpulids. the Filograninae. do have intratubular brooding but species in other sub-families, apart from
the spirorbins, have broadcast spawning and feeding trochophores. Careful examination of the breeding patterns in the
SerpulKlae is needed. I he feeding trochophore of the serpulids may also be secondary. FlTZHUGH's classification of the
Sabellidae implies that broadcast spawning with non-feeding Trochophores' have evolved from intratubular brooders
with directly developing larvae. More data is needed on reproduction in the Sabcilinae to properly understand this
Source : MNHN. Paris
RESUMES - ABSTRACTS
637
development. Because of the increased-size trend in the Sabellidae phenomena such as paedomorphosis should be taken
into account when examining character states in this family. For this reason studies on larval development are also
needed.
REPRODUCTIVE STRUCTURES AND SYSTEM A'fTGS OF THE FABRICUNAE (POLYCHAETA: SABELLIDAE). Rouse,
G.W. (Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution,
Washington D.C. 20560. U.S.A.). Males and females of at least one species from each of the following nine sabellid
genera, AugcnerieUa, Fabricia , Fabriciola. Fabricinuda. Novafabricia . Manayunkia, Parafabricia, Pseudofabriciola and an
undescribcd new genus A (FlTZHUGH el al. in preparation) were examined by light and electron microscopy. These genera,
along with Pseudofabricia aberrans, currently comprise the sub-family Fabriciinae. The reproductive systems were
examined in order to assess the proposed monophyly of this assemblage. Females of all species examined brood directly
developing larvae within their lubes. Outgroup comparisons were made with the other sabellid sub-family, the Sabellinae
and the Serpulidae. Males of species in all nine genera were found to have a dorsal, ciliated, sperm duct running directly
beneath the faecal groove of the thoracic region. The sperm duct, containing only mature spermatozoa, terminated
immediately behind the radiolar crown. No sabellins have this duct. It is also absent in members of the Serpulidae. All of
the Fabriciinae have spermatids developing in large clusters of several hundred cells. Serpulids (except for spirorbins)
and sabellins have sperm developing in tetrads. The Fabriciinae also have a sperm structure distinct from the Sabellinae
and the Serpulidae. Within the family there were differences between genera in mature sperm structure. These differences,
that could be useful in systematics, involved the structure of the sperm midpiece, elongation of the acrosome and the
degree of coiling of the nucleus. Females of the species in the genera Manayunkia genus A. Fabricia, Parafabricia and
some species of Fabriciola were found to have a pair of spermathecae associated with the radiolar crown or peristomium.
Females in the remaining genera were found to have no specialized organs for sperm storage. Females of AugcnerieUa and
Fabricinuda store sperm in epidermal cells of either the proximal inner surface of the radiolar crown or just inside the
buccal cavity. The spermathecae of Manayunkia, some species of Fabriciola and genus A comprised of a simple blind duct
lined with heavily pigmented cells. The spermathecae of Fabricia and Parafabricia were more complex with three distinct
regions. The monophyly of the Fabriciinae (sensu FlTZHUGH, 1989) is well supported by this analysis. A number of
autapomorphies for the sub-family, based on reproductive characters are established. Genera originally in the Fabriciinae
such as Oriopsis and C hone are clearly sabellins. The status of Caobangia is still unresolved and a close examination of
this genus is warranted. Within the Fabriciinae it appears that Fabriciola will have to be split into two genera, one of
which is the sister group to Manayunkia. Elucidation of the reasons for presence of spermathecae in some genera and not
in others, when the other variables in the reproductive method are maintained, requires further investigation.
INTERACTIVE PROCESSES IN A l AN ICE CON CHI LEG A (POLYCHAETA. TEREBELLIDAE) DOMINATED INTERTIDAL
COMMUNITY. Rowe, G.A., Hawkins, L.E.. Hutchinson, S ., Sheader. M. & Hirst , A.G. (Southampton University
Department of Oceanography, Southampton. S09 SNH. U.K.). The benthic macrofauna and sediment at an intertidal
midshore site on the eastern shore of Southampton Water, U.K. have been sampled for 12 months. The large tube
building polychaete Lattice conchilega (Pallas) was the numerical and biomass dominant of the community. The density
of L. conchilega varied both spatially across the region and temporally over the sampling period. Disturbance of the
sediment, depletion ol the percentage bioavailable protein and harsh climatic conditions were accompanied by declining
faunal abundance and species richness during winter. T he distribution of L. conchilega was. for the most part, contagious
throughout the sampling period. Increased mortality of the population in February and March was less pronounced in
dense patches giving a highly contagious distribution. Dense aggregations of tubes increased stability by resisting
erosion and facilitating accumulation of sediment, bringing about local seasonal changes in topography. Major
recruitment of young L conchilega adults ( > 500 pm) was seen in June, and spawning has been estimated to occur as
early as late March. Initial settlement and growth of recruiting individuals was more successful in areas of higher adult
density. The numbers of animals and species richness have been positively correlated with the density of L . conchilega
tubes. The study suggests that L conchilega, through direct and indirect interactions, plays a major role in structuring the
community at the site.
UPDATED Cl IECKl AST OF POLYCHAETES (POLYCI IAETA) FROM THE GULF OF MEXICO, THE CARIBBEAN SEA. AND
ADJACENT AREAS IN THE WESTERN ATLANTIC. SaiazaR -VaLLEJO, S.l. - (Centro dc Investigaciones de Quintana Roo.
Apdo. Postal 424. 77000 Chetumal QR. Mexico). The only checklist of polychaetes from the tropical and subtropical
Western Atlantic was published almost 20 yr ago (PERKINS & Savage. 1975). Since then, some 40 new genera and almost
180 new species have been described; further there have been several modifications and suppresions so an updated list is
really needed. By following PETTIBONE (1982) taxonomic array, there arc now over 1,100 valid species recorded in 20
orders. 71 families and 423 genera. The list of references since 1975 is made of almost 130 works. In order to make this
checklist as complete and useful as possible, and because my library might lack some important papers, any help or
discussion will be appreciated.
SPATIO-TEMPORAL VARIABILITY OF POLYCHAETE POPULATIONS IN A SUBTTDAL ESTUARINE AREA. SANCHEZ, A.,
Mora. J., GLEMAREC, M. & Lastra. M. — (Universidad de Santiago, Facultad de Biologia. Departamento de Biologia
638
ABSTRACTS - RESUMES
Animal. 15706. Santiago de Compostela. Spain). Environmental variability is an important cause of fluctuations in
marine ecosystems. In order to assess the contribution of a particular environmental factor we need to know not only how
strongly it is coupled to the biological components, but also how responsive the ecosystem is to fluctuations on that
space-time scale. This study describes the results of polychaete spatial distribution studied in 48 sites at Ria de Ares-
Betanzos (NVV Spain) and one year monthly survey of two soft sediment stations at its estuarine inner part. The aims were
to compare in a spatio-temporal scale the degree of biological organization of polychaete populations and the magnitude
of variability due to environmental factors as sediment grain-size, organic matter and redox potential condition as well as
to bottom water hydrological parameters (pH. salinity, temperature and oxygen contents). A Diplocirrus glaucus-
Stylarioides plumosa-Owenia fusiformis-Diopatra neapolitana assemblage occurred at 3-15 in deep muddy fine sandy
bottoms of the estuarine internal part with organic carbon values up to 3 % while Aponuphis bilineaia-Glycera
convoluta-Nephlhys hombergii were found in association up to 43 m depth in medium and coarse clean sands located at
the Ria outer zone with organic carbon values under 0.5 %. Seasonality was marked by Spiochaetopierus cosiarum, D.
g la uc us and Chaetozone setosa highest numbers all the surveing period long; fluctuations seemed to be linked to
variations on sediment organic matter contents, grain-size and water temperature.
POPULATION DYNAMICS AND PRODUCTION OF SCOLELEPIS GAUCHA (POLYCHAETA, SPIONIDAE)ON HIE SANDY
BEACHES OF' SOUTHERN BRAZIL. Santos. PJ.P. (Universite de Bordeaux I. Institut de Biologic Marine. 2 rue du
Professeur Jolyet, 33120 Arcachon France). — Endemic in southern Brazil. Uruguai and Northern Argentina. S. gaucha
(ORENSANZ & GlANUCA. 1974) is the polychaete species with greatest intertidal abundance with densities up to 100.000
ind. irf2. Four transects each with five stations were surveyed between 05/88 and 07/89. Sediment samples were sieved
through 0.3 pm screens after preservation in 10 % formalin. After counting the animals, the width of the 5th setiger of
100 individuals, randomly chosen, was measured to determine the population structure. The program Compleat Elefan
(version 1.10) was used to estimate growth parameters and mortality rate; production was estimated using both the
Allen's method (Z = P/B) and Crisp's growth method 3 A (production for stocks with recruitment, age classes not
separable). S. gaucha presented a multiannual life cycle (with two cohorts each year) which was related to the diffusion
pattern necessary to maintain its endemic distribution on a coast with strong seasonal processes. The large numerical
variation observed between the two cohorts was interpreted as a result of densodependent mechanisms. The spatial
differences observed for mortality rates (Z varying from 3.25 to 11.40) were associated to variations of the intertidal
stability as expressed by the different sedimentological zones which were found between transects. Although differences
in growth were observed between the cohorts, a general von Bertalanffy model modified for seasonal growth was
proposed: L(t) = 0.88 ( 1 -exp[2. 655 (t + 0.036) - (0. 1 27 )sin( 2tt (t-0.05))] ) . These differences were caused by the
temporal modification of beach profile which benefited the first cohort food uptake. The high values of mean annual
biomass (between 2 and 35 g.m'1 AFDW) and production (between 6 and 1 14 g. in ', yr'1 AFDW for ALLEN's method) reveal
the importance of this species as one of the principal components of the midlittoral community.
AN ULTRASTRUCTURAL STUDY OF NEPH RIDIAL SYSTEM IN T WO NERILLIDS: NERILIA JOUINAE AND
1 ROCHONERILLA MOBILIS (POLYCHAE I A). Saphonov, M.V. & Tzltlin, A.B. (Department of Invertebrate Zoology.
Moscow State University. Moscow, 1 19899, Russia). — Fine structure of nephridia of representatives of two nerillids
genera Nerilla jouinae and Trochonerilla mobilis were studied with the help of TEM technics. Nephridia of nerillids are
paired segmental organs, they are absent in genital segments. Protonephridia of Trochonerilla mobilis consist of
terminal cell, channel part and pore cell. Terminal cell forms a weir formed by approximately 40 rods and has 9-12 long
cilia. Nucleus of this cell situated terminally. Lumen of nephridial duct belongs to extracellular type. There are microvilli
and cilia in the duct's lumen. The endocytotic activity on the membrane of channel cells was found. Aberrant nephridia
without terminal component (funnel or weir-system) were observed in one of fertile males of T. mobilis. N. jouinae has
metanephridia. typical for this genus. Ducts has a loop and this part of nephridia forms a compact cell-mass, surrounded
by squamous coelomic epithelium. In the area of the loop ducts lumen is intracellular. Cilia and microvilli also
represented in the channel lumen. Nephridia of studied nerillids have the different levels of organization. On the one
hand, correlation between metanephridia and presence of well developed blood system in N. jouinae and between
protonephridia and absence of blood system in Trochonerilla on the other hand agree with RUPPERT & SMITH view on the
diversity of nephridia.
THE EFFECTS OF RATE OF FOOD SUPPLY. INTRA-SPECIFIC DENSIT Y. INTERINDIVIDUAL RELATIONSHIPS AND
ENVIRONMENTAL STRESS ON THE GROWTH OF JUVENILE HED/STE [NEREIS) DIVERSICOLOR (ANNELIDA:
POLYCHAETA) UNDER LABORATORY CONDITIONS. SCAPS, P., Ret/Lre, C. DESROSIERS. G. & M/RON.G. — (Laboratoire
Maritime, 17. avenue George V, B.P. 28. 35801 Dinard, France). In a series of controlled experiments designed to
determine the factors wich regulate the growth of juvenile Hediste ( Nereis ) diversicolor (O.F. Muller), tetramin was used
as food, under conditions of constant temperature (19 ± 1°C) and salinity (38 P.S.U. ± 3). A ratio of 3.33 mg tetramin.
ind' day1 maintains an optimal growth rate but does not increase the rate of survival. When intra-specific density is
above 3.000 ind. m'-. the effect is manifested in a decrease in both weight per individual and rale of survival. Due to the
effects of mortality (50 to 60 %), the densities of individuals obtained at the end of the experiment were similar to those
observed in our sampling site in spring (about 2,000 ind. nr2). Following a period of 50 days of rearing under controlled
RESUMES - ABSTRACTS
639
conditions, individuals attained the same weight as adults collected in situ. A certain number were sexually differentiated
(36-64 %) or mature (0-17 %). According to published data, adults do not mature until they are between 12 or 36 months
old (depending on geographical location). Laboratory rearing of several month old juveniles did not lead to an increase in
density (compared to that in nature) despite the absence of predators. Instead, the high frequency of handling of the
worms (including changes of temperature), produces similar negative results. A variability is obtained between "weights
of individuals reared either in isolation or in groups, depending on whether the juveniles are collected in winter or spring.
The weight of juveniles collected in spring is reduced when reared in isolation; but that of juveniles collected in winter is
not affected in either conditions.
PROTEINS AS TAXONOMIC MARKERS IN THE POLYCHAETE TAXON NEPHTYS . SCHMIDT, H. & WESI'HEIDE . W. —
(Spezielle Zoologie. Fachbercich Biologie/Chcmie, Universitat Osnabruck. Postfach 4469. D-4500 Osnabruck,
Germany). — Species of the genera Nephtys and Aglaopha/nus from intertidal and subtidal sediments of the Baltic, the
Kattegatt. the southern North Sea and the western Channel area were investigated for (1) six isozymes and (2) for
unspecitic protein patterns. I he separation of proteins was performed in polyacrylamid gels by isoelectric focusing
(IFF). All of the nephlyid species which Rainer recently listed for this region could be discriminated by these two
biochemical methods. There is evidence, however, that Nephtys longosetosa is a complex of two morphologically
identical species. Suitability of protein data obtained by IFF is especially high for the separation and identification of
single juvenile nephlyid specimens which usually are difficult to distinguish on conventional morphological features.
Surprisingly the investigations showed lack of any genetic polymorphism within populations and between
geographically separated populations of Nephtys caeca . N. cirrosa and N. hombergii
REPLACEMENT OF CHAETAE IN ATOKOUS NEREIS GRUB El (ANNELIDA. POLYCHAETA. NERFIDIDAE). SCHROEDER,
P.C. — (Dept, of Zoology. Washington State University. Pullman. WA 99164. USA). — In addition to the well-known
replacement ol atokous chaetae with paddle chaetae during reproductive metamorphosis (SCHROEDER, 1967) nereid
polychaetcs regularly replace old atokous chaetae with new ones. Autoradiograms of sections of gameteless and young
female individuals injected with tritiated thymidine reveal not only that chaetal replacement takes places periodically in
regular cohorts, but that developing atokous chaetae incorporate the radiaoaclive precursor into their matrix, providing
an indicator for the rate of matrix deposition. The acicula of some individuals also incorporate H3-TdR into the basal
portion of their matrix. The cycle of setal replacement will be described, and the utility of this information for future
studies of the cellular mechanisms of chaetogenesis will be discussed.
GENOME SIZES AND CONSTITl JTIVE I IETF ROC 1 1ROMAT1N IN SPECIES OF OPHRYOTROCHA (POLYCHAETA). Sella,
G., RED!, C. A., RAMELLA, L. & Soldi, R. - (Department of Animal Biology. University of Turin. Italy). — Genome size
is a widely used parameter in studies on the evolution of various groups of organisms. We examined the helerochromatic
and 2C nuclear DNA content of the ten best known species of the Polychaete genus Ophryotrocha , by means of C-
banding technique and microdensitomctric determination of Feulgen dye content of interphasic nuclei. Mesopsammic
polychaete of the genus Ophryotrocha are very small, progenetic and morphologically very similar worms. They have
been widely used in studies on problems of general evolutionary biology. Diploid chromosome numbers are either 6. 8.
or 10. according to the species. Chromosomes are all metacentric or submetacentric and no interspecific significant
differences were observed in karyotypic lengths. As for genome sizes, 8 out of 10 species showed a mean basic value of
0.4 pg. This value is among the lowest of the genome sizes of invertebrates so far investigated. A group of four
gonochoric and morphologically indistinguishable species with 2n = 6 appears to be heterogeneous with regard to DNA
content since one species (O. . macrovifera) has a genome size which is twice the basic value of the genus. Among the
hermaphroditic species, one (O. hartmanni) has a mean genome size which is the triple the basic value. These
interspecific differences in genome size appear to be paralleled by interspecific differences in constitutive
helerochromatin content and could thus be due to saltatory replication of repetitive DNA. Moreover, in all species
polyploid somatic nuclei were observed. Hypotheses about selective pressures that maintain such low amounts of nuclear
DNA in this taxon are discussed.
THE POLYCHAETE ASSEMBLAGES INI IABITING DIFFERENT TYPES OF' BOTTOM SEDIMENTS IN ADMIRALTY BAY
(AN I ARC ITCA). Sicinski, J. (University of Lodz, Department of Invertebrate Zoology and Hydrobiology, Laboratory
ol Polar Biology. 12/16 Banacha sir.. 90-237 Lodz, Poland). — 'The variety of habitats of different sediments in the
nearshore zone ol Admiralty Bay (King George Island, South Shetland Islands) is clearly reflected in the diversity of
bottom fauna assemblages. The nature of sediments is highly dependent on the phenomena occuring on land near the
shore. The neighbourhood of glaciers and the suspended particulate matter inflow through the subglacial streams seem to
be the most important factors influencing the nature of sediments and in consequence the character of bottom
assemblages. 1 he distribution of 52 polychaete species in chosen regions of Admiralty Bay in the depth range between 4
and 150 m, evidently related to the kind of sediments, was studied, applying multivariate classification analysis
Leitoscoloplos kergnelensis and Ophelina syringopyge were eurytopic and dominant species, reaching in the almost
whole investigated area a high values of abundance, except of the shallowest parts of sandy bottom. In the parts of the
bottom neighbouring the glaciers last sedimentation of suspended matter occurs, forming a thick layer of clayey-silly
640
ABSTRACTS - RESUMES
sedinents. The polychaeie assemblage occuring here is characterized by low values of species richness and species
diversity. Ophelina cylindricaudata, A ricidea (Aedicira) antarctica and T/tatyx cincinnatus were here the dominant species.
The polychaete fauna of nearshore areas situated far from glaciers was clearly different. In the sandy bottom of shallow
subliltoral neighbouring the stony and sandy beaches to the depth down to about 30-40 m. the peculiar assemblage with
Scoloplos (Leodamas) marginal us, Capilella capitata, Rhodine sp., Cirrophorus brevicirralus and Travisia kerguelensis
as dominant species can be distinguished. In this area at greater depths sandy and silly-sandy botton prevails, settled by
an extremely rich, diversified and most abundant assemblage. Truberia gracilis and Aricidea (Acesta) strelzoni were here
very abundant, representing a group of dominant species. At greatest depths studied ( 1 00- 1 50 m). also in the areas
situated far from glaciers, silly sediments occur. Polychaete assemblage, resembling in general the last described one.
was characterized here by the specific group of co-occurring species namely Ephesiella sp., Artacama proboscidea,
Streblosoma sp., Thelepus cincinnatus and Perkinsiana antarctica. Apart from the assemblages detecting the gradual
changes of polychaete fauna distributional patterns, corellated with increasing median particle diameter (very fine silt-
fine silt-coarse silt-very fine sand), have been also observed.
WHAT ARE PRIONOSPIO STEENSTRUP/, P. FALLAX AND P. DUB! A? SlGVALDADOTTIR, E. & MACK1E, A.S.Y. —
(Department of Zoology. Stockholm University, S-106 91 Stockholm). — MaLMGREN (1867) erected the genus
Prionospio to accomodate P. steenstrupi, a new spionid polychaete from northern Iceland. Characterized by four pairs of
branchiae from setiger 2 (first and fourth pairs with pinnules, other pairs apinnatc). the precise identity of this, the type
species of the genus, has proven elusive. Consequently the taxonomy of the P. steenstrupi -complex has been subject to
considerable confusion and instability. In the present study the three species of the complex occurring in the Northeast
Atlantic ( P . steenstrupi. P. fall ax Soderstrom, 1920 and P. dubia Maciolek, 1985) arc re-defined following examination
of type and other available material. All are morphologically distinct species and have different geographical
distributions. P. steenstrupi can be recognized by having first and fourth pairs of branchiae of equal length and with dense
pinnules laterally, by having low dorsal crests on setiger 6 and on subsequent setigers, and by having neuropodial hooks
from setigers 15-17. Further, it appears more northerly distributed than the two other species. P.fallax can be recognized
by having first and fourth pairs of branchiae of equal length and with sparse pinnules laterally, by having high dorsal
crest on setiger 7 and by having neuropodial hooks from setigers 12-13. The distribution is more southerly than for P.
steenstrupi; from the North Sea to the Mediterranean. P. dubia can be recognized by having branchiae four much shorter
than branchiae one and with dense posterior pinnules on both, by an absence of dorsal crests, and by having neuropodial
hooks from setigers 18-21. The type locality for P. dubia is South Africa and the distribution for this species therefore
seems very wide; from the North Sea to South Africa.
CHECKLIST AND BIBIJCXIRAPHY OF PQLYCHAETES FROM GREECE WITH SOME RECENT ADDflJONS. SlMBOURA, N.
<£ Nicoiaidou. a. — (National Centre for marine Research Aghios Kosmas, 16604 Hellinikon, Athens, Greece). — A
checklist and bibliography of polychaetes from Greece, which lists 570 species of benthic polychaetes belonging to 46
families. For each species a list ol the geographical localities where this has been recorded along with the respective
bibliographical citations is provided. Some new findings for the polychaete fauna of Greece are reported. These are:
Auclienoplax crinita Ehlcrs, 1887; Galathowenia oculata (Zaks. 1922); Hesiospina similis (Hessle, 1925); Hydroides
dianthus (Verril. 1873); H. nigra (Zibrowius, 1971); Lumbrinerides amoureuxi Miura, 1980; Opisthodonta pterochaeta
Southern, 1914; Polycirrus plumosus (Wollebacck. 1912); Sphaerosyllis brevicirrata Ilartmann-Schroeder, 1960; Syllis
torquata (Marion & Bobretsky. 1875). A list of the references used as a source is supplied.
REPRODUCTIVE BIOLOGY AND LIFE CYCLE OF BRAN CHI OM MA LUCIVOSUM (GRUBE, 1869) (POLYCHAETA,
SAB EL LI DAE) IN THE MEDITERRANEAN SEA. SORDINO. P. & GAMBl, M.C. (Laboratorio di Ecologia del Benthos,
Stazione Zoologica Anton Dohrn' . Napoli. Italy). — Data on the reproductive traits and the life cycle of Polychaetes are
still scarce with respect to the diversification of these organisms and to the implications that these aspects have for their
ecology and phylogeny. In this optics we studied the reproductive biology of Branchionima luctuosum (Grube. 1869). a
rare Sabcllid recently reported for the Mediterranean Sea. The population of B. luctuosum studied was lbund in a shallow
Cymodocea nodosa meadow and in the surrounding hard substrates of the Island of Ischia (Gulf of Naples. Italy). From
July 1990 to July 1991. at least 10 specimens of Branchionima of different size classes were collected monthly, measured
and fixed for the histological and ultrastrutural analysis of the gametogenesis. B. luctuosum proved to be a simultaneous
hermaphrodite, because mature sperms and developing ovocytes were present in the coelom from July. Ripe eggs were
observed in late September and October and garnet spawning occurred in Oclober-November; in December all specimens
were in a ’spent" stage. From January germ cells occurred on the coelomic walls indicating the starting of a new
gametogenic cycle. No discrete gonads were observed suggesting infra coelomic gametogenesis, a finding supported by
the ultrastructural features of the immature ovocytes. The mature sperm has a typical "ect-aquasperm" structure that is
considered a primitive character and is consistent with the free-spawning habit. Yet to be confirmed is the occurrence of
sell -fertilization. No egg protection, such as cocoons or tube incubation, was observed in the field, suggesting the
existence ol a pelagic larva, also supported by the size of the mature eggs. In the light of these data B. luctuosum seems
to be a perennial iteroparous species with a discrete synchronic spawning event. This is the first reported case of such a
mosaic of life cycle traits in Sabellid Polychaetes.
RESUMES - ABSTRACTS
641
ECQPHYSIOLOGY OF THE SANDY BEACH INTERSTITIAL POLYCHAETE POLYGORD/US ESCHATURUS
(POLYGORDIIDAE): TOLERANCE AND PREFERENCE EXPERIMENTS. Sousa-Santos . L P.& Silva, V.M.A. da.
(Dcpartemento de Zoologia. Universidade dc Rio.de Janeiro, RJ-Brazil). Laboratory experiments on tolerance and
preference were designed to elucidate the importance of some ambicntal factors on the ecology of Polygordius escliaturus ,
and to help the understanding of the distribution pattern of this interstitial species on a sandy beach in southeastern
Brazil. The lirst results indicated that this species could be easily maintained for some weeks in mini-aquariums provided
with sand and daily renovated sea water. The tolerance results were expressed by an index that considers both behaviour
and survival of the animals, and were analysed by non-parametric statistics. P. escliaturus showed a great salinity
tolerance since the animals survived in salinities between 10 and 50 P.S.U. and their behaviour was not affected between
20 and 40 P.S.U. These limits were the same for both gradual and abrupt salinity changes. For the temperature tolerance it
was found that at 10 °C the animal behaviour was affected, at 20 °C and 30 °C the animals were not affected by temperature
and at 40 °C all the animals died. At the salinities and temperatures tested, little interaction between these factors was
observed. P. escliaturus showed photonegative and geoposilive behaviour, nevertheless, migration toward the highest
oxygen tension layer may overlay this last behaviour. This species has no attraction for single sediment grades, and may
even die it maintained in those sediments. The animals showed a preference for natural sediment in contrast to sediment
without organic matter. This species occurs at the midlittoral level of a coarse-sand beach where the salinity and
temperature changes may be great, but the animals are present mainly between 10 and 20 cm in the sediment, probably to
not be exposed to the greatest surface changes. Since the animals were attracted to the highest oxygen tension, at that
depth the oxygen tension should be high, probably due to a good percolation of water through the coarse sediment. The
specificity of this species to its natural sediment was probably related to the sediment selection and porosity and may
explain its horizontal distribution on the beach. However, more experiments are necessary to confirm this hypothesis.
PR El -IMINARY REPORT OF POLYCHAETE ASSEMBLAGES IN THE SOFT BOTTOMS OF 'THE Cl I AFARIN AS IS1 ,ANDS
(SOUTHWESTERN MEDITERRANEAN). Torres-Gav/ia, F.J., CAPACCIONI-Azzati. R.. Tena, J. & Garcl\-Carrascosa, AM.
- (Invertebrate and Marine Biology Laboratory. Department of Animal Biology. Faculty of Biological Sciences.
University of Valencia. Burjassot E-46100. Valencia. Spain). — The Chafarinas Archipelago is located in the southern
basin of the Alboran Sea, two miles from the Moroccan coast, near the Oued-Moulouya river mouth. This archipelago is
composed of three volcanic rocky islets: Congreso, Isabel II and Rey Francisco. These islets are located on a horizontal
shallow shelf. The shelf is about 15 m deep on its Southern side, but reaches depths of about 30-35 m on the Northern
side. The bottoms around the islets are subject to an important discharge of fine sediments from the Oued-Moulouya river
mouth. I his supply of sediments determines to a great extent the settlement of different marine communities and
particularly the polychaete fauna in this area. Here we present results of a study of the annelid polychaete assemblages on
soft bottoms of the sedimentary shelf at 40 sampling stations distributed among the different sediment types found
around the islets. We conducted a comparative analysis of the polychaete fauna in three major types of sediment (coarse
muddy, fine sandy and gravel and coarse sandy bio-detrilic bottoms) distinguished on the basis of their granulometric
characteristics. Other environmental factors affecting the distribution of species are also discussed.
ON THE BIOLOGY AND ECOLOGY OF SACCOCIRRUS PARVUS G ERLACH, 1953 (POLYCIIAETA. SACCOCIRRIDAE).
VtLLORA-MORENO , S. (Invertebrate and Marine Biology Laboratory. Department of Animal Biology. University of
Valencia, Burjassot E-46100. Valencia, Spain). — Saccocirrus parvus is an interstitial polychaete inhabiting the
midlittoral zone ol the Mediterranean sandy beaches. This species is included in the "papillocercus- group" because the
absence ot pharyngeal bulb, presence ol genital organs on both sides of the segments, and lack of venual ciliary patches
or tracks. Despite the cosmopolitan condition attributed to "papillocercus- group", S. parvus is known only from the
Mediterranean Sea, and information on this species after its original description (GERLACH, 1953) is scarce. In this
paper, a rcdescription of the species is provided through vital and post mortem coloration techniques for optical
microscopy and SEM observations. Details of the male and female reproductive systems, morphology of epidermic
metameric glands, and adhesive glands, morphology of the three types of setae and other features from SEM micrographs,
are given lor the species. These last characters are helpful for species differentiation in the "papillocercus- group" A
quantitative study on spatial distribution of S. parvus was achieved using a standard corer. The different zones of the
beach were sampled. Abundance of .S', parvus increased in the turbulent zones, reaching a maximum in the
O topi a nabioceno sis level, with densities ol 660 ind. ml'1. A long-time survey of three years allowed us to determine the
fertile period of the species. Mature individuals were observed during the temperate months, from April to September. The
size ol the specimens as well as the morphology of the pygidium seems to be correlated with the sediment granulometry.
A discussion of these observations is reported through a morphometric study. Finally, some results of feeding are in
agreement with figures found by authors for other co-generic species. The carnivorous preferences of this species is
deduced from the observation of Harpaclicoids and Nematodes in the gut contents of living specimens.
THE ELECTRONIC' PALOIA OR COMPUTER PUBLICATION OF SYSTEMATIC PAPERS. Ward. LA. <fc Fauchald, K.
(National Museum of Natural History, Smithsonian Institution, Nil B Slop 163 Washington D.C.. IJ.S.A.). Very few
journals will accept large systematic studies. They are expensive to print and the audience is limited. Recent computer
Source : MNHN. Pans
642
ABSTRACTS - RESUMES
software makes electronic publishing an attractive alternative. Within a fixed, electronic "journal" format, an author can
create a publication with keys. text, illustrations and cited literature. An electronic "journal" may be issued four times a
year as a compact disc, or perhaps only once a year. Under any circumstances, if the editor of a journal receives a
computer file in good condition from the author, the cost of such a journal would be about 1/4 of current printing costs for
the same amount of material. Reviewing papers for such publication is as easily arranged as that of paper publications.
The security of a computerized paper does not differ in kind from that of a normal journal: copiers and optical character
readers makes it possible for any interested person to copy and computerize, as a database or a word-processing document
any paper in print. It may be slightly easier to download a portion of a computerized publication, but that difference is
trivial. As an example, wc have transferred into computer format a recently completed (and submitted) paper describing
types of Palola. We will demonstrate advantages and drawbacks in this new technology and will also discuss the
ramifications of this kind of development for production of journals by non-profit corporations, such as various
societies and by profit-making ventures such as the various publishing houses.
STUDY OF THE BIOGEOCHEMICAL GRADIENTS SURROUNDING POLYCHAETE TUBES IN SEDIMENTS OF THE
LAUREN I IAN I ROUGH. White, C.. JUNIPER, S.K. & DESROSIERS, G. — (Centre Oceanographique de Rimouski. 310, Allee
des Ursulines, Rimouski, Quebec. G5L 3AI. Canada). — This study compares biogeochemical gradients generated by
tube construction and irrigation by two species of polychaete (Maldane sarsi and Amphorele acutifrons) in deep-water
sediments (350 in) of the Lauren lian Trough. While both species arc detritivores. M. sarsi lives and feeds in a head-down
position in its tube. Trace metal and organic matter content, granulometric properties and bacterial abundance were
analysed in lubes and surrounding sediments for each species. Gramulometric analysis show that both species sort
sediments while building their lubes. Bacterial counts, organic matter and trace metals were most concentrated in
sediments of the inner tube wall of both species. Vertical gradients are also evident and appear to reflect different feeding
habits and depths at which each species occurs in its tube. Using abundance data for both species we extrapolate to assess
the overall impact of tube construction and occupation on sediment biogeochemical processes in the Laurcnlian Trough.
I M M 1 1 NO HI STOC HEMIC A I . OBSERVATIONS ON THE NERVOUS SYSTEMS OF TWO D/NOPHILUS SPECIES
DEMONSTRATE DIFFERENCES IN NEURON A I . ARRANGEMENT AND NEUROCHEMICAL EQUIPMENT. W/NDOFFER, R.
& WESTHEIDE, W. (University Osnabruck. Fb Biology Chemistry, Barbarastr. 1 L D-W-4500 OsnabrUck. Germany). —
Investigations of the nervous system of Dinophilus gy roc Hiatus and D. taeniatus with immunohistochemical methods
lead to information on the nervous anatomy and the chemical nature of their neuroactivc substances. The results gave new
insights into special characteristics of these aberrant polychaetcs, their proposed progenetic origin, the extreme
dimorphism of D. gyrociliatus and the obligate encystment within the life cycle of D. taeniatus. Antibodies against the
amines octopamine and serotonin, and the peptides FMRFamide, CCK and SCPB stained various subsets of perikarya and
fibers. Antibodies against several other peptides showed no positive reactions leading to the assumption of a reduced
neurochemical equipment in Dinophilus compared to other polychaetcs. This is in accordance with a proposed highly
derived nature of the Dinophilidae.There is a general correspondence in the staining pattern of the females of D.
gyrociliatus and D. taeniatus with most antibodies. Nevertheless, important differences can be shown in details, e.g. in
the neuronal arrangement and neurochemical equipment of the stomatogastric nervous system and the nerves of the body
wall. These variations can be explained by different feeding behaviour and ciliation of the body wall. Further
dissimilarities cannot be explained in this way. Octopamine- like immunoreactivity can only be found in D. taeniatus.
Anti-Serotonin and anti-FMRFaiftide stained a wide range of nervous elements in both species with clear differences in
number and position of positive neurons. Even immunogold stainingS show different populations of neurovesicles in
both species. These results are surprising because of the assumption that serotonin. FMRFamide and octopamine should
be involved in fundamental neuronal activities such as movement and central neuronal integration which should be more
or less identical in both species. These differences might be related to a rearrangement of the D. taeniatus nervous
system that enables encystment.
PRELIMINARY REPORT ON VEGETATIVE REPRODUCTION OF MALDANE SARSI ARDWIDSSON. 1911
(POLYCIIAETA, MALDANIDAE) OFF ELEPHANT ISLAND, ANTARCTICA. WRZESINSKI , O.J. (Univers. Marlin Luther
King Plat/. 3. 2000 Hamburg 13). A rare case of a wide-scale vegetative reproduction of Maldane sarsi is described. The
material was collected during the V International Antarctic Expedition on board of the r/v "Polarstern". cruise 9 (1986).
northwards of Elephant Island on the depth of 227 m. Respective stages of that phenomenon! are presented.
CONTRIBUTION TO KNOWLEDGE OF OFFSHORE POLYCHAETE FAUNA IN 'll IE NORTI IERN ADRIATIC. Z unit a. E. —
(Center for Marine Research. "Ruder Boskovic" Institute, 52210 Rovinj. Croatia). At three coenobioses located in the
North Adriatic offshore area, qualitative and quantitative structures of the Polychaete fauna have been studied, within the
period 1982 to 1987. A total, ol 101 species were noted. The faunal composition, and species distribution, with regards
to sediment characteristics and trophic relations were discussed.
Out collabore a la realisation de cel ouvrage :
Saisie des lexles el niise en page :
G. BELLAN, M. BHAUD, J.-C. DaIJVIN, J.-C. DUCHHNE, P. GlLLET, L. LAUBIER el C. RETIRE
Verification des manuscrits el des epreuves :
J.-C. Dauvin, D. Reish et J. Vovelle
La mise en forme du manuscrit final a 6t6 r£alis6e par L. Laubihr
sur Macintosh Ilci avec logiciel WORD 5.1
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BIBL.
MUSE'
PARIi
☆
Source : MNHN. Paris
Source : MNHN. Paris
DERNIERS TITRES PARUS
RECENTLY PUBLISHED MEMOIRS
A parlir dc 1993 (Tome 155). les Afemoires du Museum sont publies sans indication de serie.
From 199.1 I Volume 155). the Memo'ires du Museum are published without serial titles.
Tome 161 : Alain Crosnier (ed.), 1994 Resultats des Campagnes MusorStom. Volume 12 610 nn
(ISBN 2-85653-212-8) 600 FF.
Tome 160 : Nicole Boury-Esnault. Maurizio Pansini, & Maria Jesus Uriz, 1994 Spongiaires bathyaux
de la mer d'Alboran et du Golfe ibero-marocain. 174 pp. (ISBN 2-85653-213-6) 300 FF.
lome 159 Pierre Robbe, 1994 Les Inuit d'Ammassalik, Chasseurs de I'Arctique. 389 np (ISBN
2-85653-270-1) 360 FF. M
Tome 158 : Alain Crosnier (ed.). 1993 Resultats des Campagnes Musorstom. Volume 1 1 426 pp (ISBN
2-85633-208-X) 500 FF.
Tome 157 : Loic Matile, Judith Najt & Simon Tillier (eds), 1993 Zoologia Neocaledonica. Volume 3
218 pp. (ISBN 2-8563-205-5) 280 FF.
Serie B (Botanique) :
Tome 32 : Claudine Friedberg, 1990 Lc savoir botanique des Bunaq. Percevoir et classer dans le Haut
Lamaknen (Timor. Indonesie). 304 pp. (ISBN 2-85653-177-6) 350 FF.
Iome 31 : Odile Poncy, 1985 Le genre Inga (Legumineuses. Mimosoideae) en Guyane franchise.
Systematique, Morphologie des formes juveniles. Ecoiogie. 124 pp. (ISBN 2-85653-135-0) 210 FF.
Tome 30 : Lucile Allorge, 1985 Monographic des Apocynacees Tabernaemontanoidees amerieaines.
216 pp. (ISBN 2-85653-132-6) 280 FF.
Tome 29 : Monique Keddam-M alplanche, 1985 Le Pollen et les stomates des Gardeniees (Rubiacees) du
Gabon. Morphologie et tendances evolutives. 109 pp. (ISBN 2-85653- 1 3 1 -C-8) 220 FF.
Tome 28 : Marie-France Roquebert, 198 1 Analyse des phenomenes parietaux au cours de la conidiogenese
chez quelques champignons microscopiques. 79 pp. (ISBN 2-85653-116-4) 130 FF.
Serie C (Sciences de la Terre) :
Tome 56 : Jean-Paul Saint Martin, 1990 Les formations recifales coralliennes du Miocene superieur
d'Algerie el du Maroc. 373 pp. (ISBN 2-85653-170-9) 392 FF.
Tome 55 : Georges Busson (ed.). 1988 Evaporites et hydrocarbures. 144 pp. (ISBN 2-85653-155-5)
180 FF.
Tome 54 : Monettc Veran. 1988 Les elements accessoires de Parc hyoi'dien des poissons teleostomes (Acan-
thodiens et Osteichthyens) fossiles et actuels. I 14 pp. (ISBN 2-85653-154-7) 150 FF.
Tome 53 : Donald E. Russell, Jean-Pierre Santoro and Denise Sigogneau-Russell. 1988 Teeth
Revisited : Proceedings of the Vllth International Symposium on Dental Morphology. 462 pp (ISBN
2-85653-148-2) 625 FF.
lome 10 : Jacques Roger. 1962 (Reimpression Reprint 1988) Bufeon. Les Epoques dc la nature. Edi¬
tion critique. 344 pp. (ISBN 2-85653-160- 1 ) 100 FF.
Prix hors taxe, valides jusqua decembre 1995. Frais de port en sus. Vente en France : TVA 2.10%.
Prices in French Francs are valid until December 1995. Postage not included.
Source ; MNHN, Pans
Every three years, since 1983, an International Polychaete Conference has been organized to
provide a forum for the communication of our knowledge of this group. The proceedings of these
Polychaete Conferences have remained important reference books for the study of Polychaetes, in the
absence of a scientific journal specialized on these organisms. This volume of “ Memoires du Museum
national d'Histoire naturelle ” publishes all the communications presented at the fourth International
Conference held in Angers in 1992, with a total of sixty five papers selected on the basis of a peer review
process following the Conference, and 101 abstracts. The papers are classified into five topics as a large
amount of studies on polychaete demonstrate the various approaches in this group : Cytophysiolpgy,
development and reproduction (seven papers), Genetics and morphology (eight papers), Phylogeny and
taxonomy (19 papers). Ecology and biogeography (29 papers) and Culture and valorisation (two papers).
Up to date reviews of several subjects are included, with a significant number of new data. The
phylogenetic positions of some families are discussed as a basis for new hypotheses on the relationships
between Polychaete families. Three genera and 10 species new to science are described in this volume. The
future of polychaetes exploitation should be their culture and valorisation.
Jean-Claude Dauvin, Dr es Sciences, spent thirteen years as a researcher with the Centre National
de la Recherche Scientifique at the Biological Station of Roscoff, Brittany, and is now Professor at the
Museum national d’Histoire naturelle, Curator of worms. He is particularly interested in benthic
communities and Polychaete populations from the English Channel, and focuses on the systematics and
the phylogeny of Opheliidae.
Lucien Laubier, Dr es Sciences, Director at the Institut Frangais de Recherche pour l’Exploitation
de la Mer (IFREMER), Professor at the Institut Oceanographique de Paris, is Counsellor for Science and
Technology in the Permanent Representation of France to the European Union in Brussels. He has studied
Polychaetes for some 35 years and is still active in systematics, phylogeny and biogeography of
Polychaetes, in particular Alvinellids from deep-sea hydrothermal vents and Mediterranean Polychaetes.
Donald J. Reish, Ph. D„ Emeritus Professor at California State University in Long Beach, is
currently consultant with U.S. Bureau of Standard and U.S. Army Corps of Engineers. He has studied
Polychaetes for more than 40 years and his classic work “ An ecological study of pollution in Los Angeles
Long Beach harbors ” (1959) is considered to be the corner stone of modern benthic studies in polluted
areas. He is currently involved in toxicological studies using Polychaetes as test organisms.
EDITIONS
DU MUSEUM
57,
RUE CUVIER
75005 PARIS
ISBN 2-85653-214-4
ISSN 1243-4442
PRIX : 398 FF TTC (France)
390 FF HT (Etranger)
Source : MNHN. Paris
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