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Republiek van
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BOTHALIA
Volume 12, No. 2
Edited by/Onder redaksie van
D. J. B. Killick
Editorial Committee/Redaksiekomitee: B. de Winter, D. Edwards, D. J. B. Killick and/en O. A. Leistner
Botanical Research Institute
Navorsingsinstituut vir Plantkunde
m. VAN LANDBOU-TEBNIESE DIENSTE
BkLIOTEEK
NAV. INSTITUUT VIR PLAN TK WIDE
H 10 1977
PRETORIA
BOTANICAL RESEARCH INSTITUTE
DB1!. OF ASMWIIURAI TECHWCAl SERVICES
Department of Agricultural Technical Services
Departement van Landbou-tegniese Dienste
South Africa/Suid-Afrika
1977
Digitized by the Internet Archive
in 2016
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CONTENTS-INHOUD
Volume 12, No. 2
Page
Bladsy
1. Hans Justus Thode (1859-1932), pioneer plant collector in the Natal Drakensberg. D. J. B.
Killick 169
2. The South African species of Teucrium (Lamiaceae) L. E. Codd 177
3. A note on the Stachys aethiopica Complex. L. E. Codd 181
4. New taxa and a new combination in the genus Cotyledon. H. R. Tolken 191
5. The identity of Erica flavisepala. E. G. H. Oliver 195
6. The identity of Eriosema nanum. C. H. Stirton 199
7. Morphological studies of the Ochnaceae. P. C. V. du Ton 205
8. Leaf anatomy of the South African Danthonieae (Poaceae). I. The genus Dregeochloa. R. P.
Ellis 209
9. Cytogenetic studies in the Eragrostis curvula Complex. T. B. Vorster and H. Liebenberg 215
10. A note on the flowers of Halleria lucida. C. H. Stirton 223
11. The pollination of Canavalia virosa. C. H. Stirton 225
12. Broad-spectrum pollination of Plectranthus neochilus. C. H. Stirton 229
13. Freshwater algae of Southern Africa. II. Triplastrum stipulosum from the Transvaal. M. Isabella
Claassen 231
14. Freshwater algae of Southern Africa. IV. Some Micrasteriae from Rhodesia, including a new
species. M. Isabella Claassen 239
15. Asexual nuclear division in Neocosmospora. K. T. Van Warmelo 247
16. Notes on African plants:
Araceae. A. A. Obermeyer 251
Asclepiadaceae. R. A. Dyer 253
Cyperaceae. P. Vorster 257
Fabaceae. J. H. Ross 257
Frullaniaceae. P. Vorster 257
Poaceae. P. C. V. Du Toit 258
Ranunculaceae. D. J. B. Killick 258
Rutaceae. J. H. Ross 258
Selaginellaceae. P. Vorster 259
Thelypteridaceae. P. Vorster 260
17. World climatic patterns in grassland and savanna and their relation to growing seasons. R. Kirk
Steinhorst and J. W. Morris 261
18. Automatic classification of the highveld grassland of Lichtenburg, south-western Transvaal.
J. W. Morris 267
19. Cape Hangklip area. 1. The application of association analysis, homogeneity functions and Braun-
Blanquet techniques in the description of South Western Cape vegetation. C. Boucher 293
20. A preliminary account of aerial plant biomass in fynbos communities of the mediterranean type
climate zone of the Cape Province. F. J. Kruger 301
21. Silene dewinteri, a new species of the Caryophyllaceae from the south-western Cape. G. Bocquet 309
22. The taxonomic status of the genus Rubidgea. Eva Kovacs-Endrody 313
Book reviews 319
Bothalia : 12,2: 169-175 (1977)
Hans Justus Thode (1859-1932), pioneer plant collector in the Natal
Drakensberg
D. J. B. KILLICK*
ABSTRACT
An account is given of the life of Hans Justus Thode (1859-1932) from the time of his arrival in Cape
Town in 1885 or 1886 until his death in Durban in 1932. Thode was the pioneer plant collector of the Natal
Drakensberg, but also collected wider afield in all four provinces of the Republic. His contributions to South
African botany are assessed.
RESUME
HANS JUSTUS THODE (1859-1932), PREMIER BOTANISTE RECOLTEUR DANS LES
DRAKENSBERG DU NATAL
La vie de Hans Justus Thode (1859-1932) est relatee, depuis le moment de son arrivee au Cap en
1885 (ou 1886) jusqu'a sa mort a Durban en 1932. Thode fut le premier a recolter des plantes dans les
Drakensberg du Natal, mais ses activites se sont egalement exercees en d'autres endroits dans les
quatre provinces de la Republique. Un inventaire est dresse de ses contributions a la botanique sud-
africaine.
INTRODUCTION
As a student of the flora of the Natal Drakens-
berg, it was perhaps inevitable that the author should
become interested in the life of Hans Justus Thode
(Fig. 1), pioneer plant collector of the Drakensberg
and the first to describe its vegetation.
The author was fortunate in obtaining a number of
Thode’s personal papers, some from Miss M. D.
Gunn, former librarian of the Botanical Research
Institute, and some from Mr R. G. Strey, Curator
of the Natal Herbarium. Otherwise, research on
Thode would have been extremely difficult because,
from all accounts, he was a retiring and uncom-
municative person, who rarely spoke of himself.
Fig. 1. — Hans Justus Thode. Portrait taken c. 1920.
* Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria.
BIRTHPLACE
Thode was born in 1859 probably in Germany.
His death notice (Estate No. 18272, Master's Office,
Pietermaritzburg), gives his nationality as Swiss, but
all evidence points to a German origin. All the people
contacted, who knew Thode, accepted him as German
without question. Amongst his manuscripts is a
poem entitled "All Red" obviously written during
or about the time of World War I. The poem is
strongly anti-British and would hardly have been
written by a Swiss, even a German Swiss. In an
article entitled “Journeys in the South African
Mountains”, Thode refers to the “Riesengebirge at
home”. The Riesengebirge or Giant Mountains lie
between Dresden and Breslau (Wroclaw), in what
was formerly Silesia in Germany, but is now in
Poland.
According to Mr H. Struck of Draycott, Natal,
during World War I Thode gave the authorities to
understand that he was Swiss in order to escape
possible internment. This may account for the Swiss
nationality given on his death notice.
Thode had four sisters and one brother. The one
sister Alwine Margarethe Sophie married Carl
Alexander Hammer, a storekeeper who, according
to Mr H. Zunckel of Bergville, lived at Oliviershoek.
In the death notice of this sister, the birthplace is
given as Germany. Another sister, Sylvia, married
a Mr Mummbrauer of Noodsberg. The two remaining
sisters lived in Germany, the one Mrs Kate Putz in
Munich and the other Mrs Suzanna Saphir in
Leipzig. The brother Felix emigrated to Australia.
Mrs Kate Putz’s daughter-in-law, Mrs Emmy Putz,
claims that she remembers seeing a baptism certi-
ficate which indicated that Kate Putz (nee Thode)
was born in Manchester, England (letter from
Dr A. Schreiber, Munich, to Miss M. D. Gunn, 19th
August 1966).
To make tracing of Thode's birthplace even more
difficult there are suggestions that Thode changed
his name on arrival in South Africa. According to
Mrs H. Mummbrauer of San Francisco, U.S.A.,
he was originally called Freylinghausen, while
according to Mr Erich Mummbrauer of Bronkhorst-
spruit, his real name was Von Ettinghausen.
Mr Mummbrauer stated that Thode came of military
stock but, because of his love of botany, rejected a
military carreer and emigrated to South Africa
changing his name at the same time. However, no
evidence to support these statements has been found.
170 HANS JUSTUS THODE (1859-1932), PIONEER PLANT COLLECTOR IN THE NATAL DRAKENSBERG
ARRIVAL AND SOJOURN IN CAPE
In Table 1 Thode’s collections from 1886-1906 are
listed chronologically. The first collection is dated
January 1886-December 1887. From this it would
appear that Thode must have arrived in Cape Town
in 1885 or early 1886. Why he chose to come to
South Africa is not known. While in the south-
western Cape he collected intensively and made
notes on the Cape flora. He published his observations
under the title “Die vier Jahreszeiten am Cap” in
a series of articles in Natuurwissenschaftliche Wochen-
schrift (1892).
TABLE 1. — Thode’s collections between 1886-1906
1. First Cape Series (Jan. 86-Dec. 87), 11 fascicles
(a) First Peninsula Series (Jan. 86-Aug. 87)
(b) 86 Supplement (Du Toit’s Kloof, Mamre, Paarlberg
Caledon) Aug. 86
(c) 87 — (Clarkson, etc.) Dec. 87
2. Kaffrarian Series (Dec. 87-Mar. 99)
(a) First East London Series (Jan. 88-Dec. 89)
(b) 87-88 nr. Supplement (Gamtoos R., Grahamstown,
King William’s Town) Dec. 87-Jan. 88
(c) 99 — (Komga, Tembuland, Pondoland) Feb. -Mar. 99
3. First Natal Coastal Series (May-Oct. 90)
4. First Highland Series (Weenen, Klip R. County, O.F.S.)
Oct. 90-Mar. 91
5. Second Natal Coastal Series (Apr. 91-July 1906)
(a) 91 Durban Series (Apr. -Nov. 91)
(b) 97 Supplement ( Dombeya natalensis, Avoca) June 97
(c) 1901 -(Barringtonia, Zeuxine , etc.). June 97
(d) 1 903— ( Disci polygonoides, Pinetown) Oct. 1903
(e) 1904 -{Habenaria, Mikania , Lower Umkomaas, etc.)
July 1904
6. Second Highland Series (Oliviershoek, ? etc.) Nov. 91-
Dec. 92
7. Third Highland Series (O.F.S., Mont-aux-Sources, etc.)
Jan. 93-June 94
(a) Emberton Supplement ( Cynorchis compacta) Aug. 94
(b) Transvaal Supplement ( Gerbera jamesonii) Dec. 1893
8. First Natal Midlands Series (Noodsberg) Oct. 94-Nov. 95
9. Fourth Highland Series (Lesotho, Witzieshoek). Dec.
1895- Jan. 97
(a) 97 Supplement (Brachycorythis tenuior, Emmaus) Jan. 97
10. Second Natal Midland Series (Umsindusi) Feb.-June 97
11. Second Cape Series (July 97-Jan. 99)
(a) Second Peninsula Series (July 97-Aug. 98)
(b) 98-99 Supplement (Cedarbergen, Bokkeveld) Oct. 98
Jan. 99
12. Fifth Highland Series (Oliviershoek Pass) Aug. 99-
Dec. 1900
13. Sixth Highland Series (Springfontein, Empangweni) June
1902- Jan. 1904
(a) Springfontein Fasc. (June-Nov. 1902)
(b) 1904 Supplement (Empangweni, etc.) Jan. 1904
14. Third Cape Series (Aug. 1903)
(a) Stormberg (Steynsburg) Fascicle
(b) Karoo (Beaufort West) Fascicle
(c) Tulbagh Fascicle
(d) Third Peninsula Series
15. Third Natal Midland Series (Kronsberg, Howick) Jan.
1903- Nov. 1904 (June 1906, Dec.)
(a) 1905 Supplement (Scholia brachypetala, etc.) Aug. 1905
(b) 1906 Supplement ( Eulophia bicolor , Aster erigeroides
etc.) Jan, June 1906
16. Seventh Highland Series (Bushman's Pass Reserve), Jan.
1905
From Table 1 it appears that Thode moved to
British Kaffraria in about December 1887 stopping
en route at the mission station at Clarkson near
Humansdorp. He collected in East London,
Grahamstown and King William’s Town up to
December 1889. It is not known where he was based
while in Kaffraria. His observations on the flora of
British Kaffraria were published in Engler’s Bot
Jahrb. 12: 589-607 (1890).
DRAKENSBERG AND SUBSEQUENT YEARS
In 1890 Thode “first set foot on the blessed soil
of fair Natal.” Between May and October 1890 he
collected along the coast of Natal, but then set off
for the “majestic range of the Kathlambe or Drakens-
berg, which has irresistably attracted and again and
again induced me to climb its lofty heights”. In the
middle of October 1890 he travelled by train to
Estcourt, a 10-hour journey, and saw for the first
time in the distance the still partly snow-clad
Drakensberg. Thode writes: “There it was lying in
front of me, the goal of my long cherished dreams and
expectations, the rarely visited and little known,
almost mythical realm of clouds, once the retreat of
robbing Bushmen, whose curious paintings can still
be found in many a cave below the cliffs of the river
valleys; now a sphere of solitude still unviolated by
the devastating activities of man. What an inex-
pressible incentive to be the first explorer of this
terra incognita, to open this veiled enchanted country
to investigating science and to return with trophies of
its interesting flora in the form of many a plant still
undescribed.” Medley Wood, the Curator of the
Natal Herbarium, tried to dissuade Thode from
exploring the Drakensberg, pointing out that the
mountains were infested with hostile Basothos.
This in no way deterred Thode.
He then travelled to the Empangweni Mission
(maintained by the Berlin Mission Society), which
he had chosen as his “fixed quarters”, because of
its fairly close proximity to the mountains. His first
Drakensberg expedition (29th October 1890) was to
Cathkin Peak and Champagne Castle. Unfortunately
inclement weather and recalcitrant Bantu bearers
prevented him from climbing either of these peaks.
Champagne Castle had been successfully climbed two
years earlier by the Stocker brothers. Thode
described this trip in great detail in a published news-
paper article and mentioned some of the more
striking plants he encountered. Presumably, his haul
of plant specimens was considerable.
A succession of expeditions followed, details of
which are given in Table 2.
To enable Thode to pursue his botanical interests,
he became a tutor at mission schools and on farms,
some situated close to the Drakensberg. He would
advertise his services in newspapers. The following
is an advertisement found amongst his papers:
“Teacher, elderly, ample experience and qualifications
desires re-engagement as tutor on farm (Natal or
Cape). All standards, Afrikaans, music, etc. Salary
£5 p.m. Numerous references.” Thode would spend
some time in one area and having exhausted it
botanically, would take up a post in another area.
This was the pattern of his existence to the end.
Thode sent most of his collections to Dr Adolf
Engler of the Berlin Herbarium, but apparently did
not make much out of his collections financially.
Prof. A. W. Bayer (letter of 3rd June 1965) writes
that “Thode was convinced that science was to serve
mankind and that it was quite wrong for anyone
to receive payment or to make money from scientific
work”. H. Bolus in a letter to A. W. Hill at Kew
(26th August 1908) describes Thode as “too peculiar
to be hired himself”. According to Prof. Bayer,
Thode would bring his specimens to Illings Store
at Ladysmith and this firm would pack and despatch
them to Berlin.
D. J. B. KILLICK
171
TABLE 2. — Thode’s main Drakensberg expeditions
By 1894 he had collected to such an extent and
seen so much of Natal that he was able to publish
an article in Bot. Jahrb. 18, Beibl. 3, 43: 14-45 (1894)
describing very accurately the botanical regions of
Natal.
In 1930 Markotter published a list of plants
collected by Thode at Witzieshoek, Oliviershoek Pass
and Koolhoek. These collections cover the period
1891 to 1914, consequently Thode must have spent
a considerable time in that area. At Oliviershoek he
presumably stayed on occasions with his sister Alwine,
whose husband C. A. Hammer had a store there.
At Witzieshoek it is known that he often stayed
with the Rev. Ross, a missionary, and at “Koolhoek”
(Fig. 2) about 21 km south south-east of Memel,
he was tutor to the Cronje family in 1907. According
to Mr C. J. Cronje, son of Karel Pieter Cronje,
Thode also tutored on the farm of Mrs Moorman
at Witzieshoek for a time.
However, Thode did not spend all his time during
that period in the Witzieshoek-Oliviershoek Pass-
Koolhoek area. From Table 1 it will be seen that he
visited the Cape Peninsula from July 1897 to August
1898 and the Cedarberg and Bokkeveld from
October 1898 to January 1899. He also passed through
the eastern Cape (Komga, Tembuland and Pondo-
land) in February to March 1899 presumably on his
way back to Natal. En route he collected on “Prospect
Farm” (Komga) belonging to H. G. Flanagan. In
August 1903 he visited the Karoo (Steynsburg,
Beaufort West, etc.). In 1904-1906 he was tutor on
the farm “Kronsberg”, Noodsberg, belonging to
Mr Herman Mummbrauer. On this farm he met
H. Rudatis and actually commenced a combined check-
list of birds with Rudatis and Mr G. Mummbrauer.
To gain some idea of Thode’s movements between
1908 and 1920 the writer visited the Stellenbosch
Herbarium, which contains 6309 of his specimens,
and scanned as many of the specimens as possible
in the time available, obtaining localities and dates
from the labels. Judging from the consecutiveness
of some of the dates, it would appear that Thode
had several fixed bases during this period. These
were apparently: “Sweet Home” (Krantzkop), Sept.
1910-Sept. 1911; “Warrock” (26 km west of Lady-
smith), Oct. 1911-March 1913; “Scottspoort” (near
Weenen), Oct. 1913-March 1914; Empangweni Mis-
sion (near Loskop), Nov. 1914-Jan. 1915; Shakas-
Fig. 2. — Homestead on the farm
"Koolhoek” near Memel where
Thode was tutor to the Cronje
family in 1907.
172 HANS JUSTUS THODE (1859-1932), PIONEER PLANT COLLECTOR IN THE NATAL DRAKENSBERG
kraal, April 1914-Sept. 1916 and finally “Yorkshire
Wolds” (near Rosetta), Aug.-Nov. 1918. If more
specimens had been examined, the periods might have
proved to be longer.
Many other localities were noted, some being near
the bases already mentioned. It is clear that Thode
paid regular visits to southern Natal between 1908
and 1920: there are numerous and sometimes annual
collections from “Friedenau”, Kenterton, “Moyeni”,
St Michael’s Mission, Oribi Flats, Marburg, Ivunga
River, Beach Terminus and Park Rynie. It is likely
that Thode visited H. Rudatis and stayed with him
on his farm “Umgai”. There was certainly contact
between Thode and Rudatis, because some of
Thode’s specimens are marked “ex herb. Rudatis”.
In 1911 Thode visited the Transvaal and collected
in Pretoria and Heidelberg and in early 1918 he
travelled to the Cape and collected at Worcester,
Laingsburg, Montagu, Beaufort West and Matjies-
fontein. In 1919 he crossed into Pondoland and
collected in the vicinity of the Mzamba River. In
1920 he again visited the Transvaal collecting in
Pretoria and Rustenburg.
In 1920 Thode was tutor on the farm “Altemooi”
belonging to Mr Adrian Daneel. “Altemooi” is
situated about 19 km SE of Wakkerstroom and
20 km N of Utrecht. He taught the Daneel children,
as well as those of Mr H. Repsold of the farm
“Tweekloof” next door. The portait of Thode (Fig. 1)
was given to the author by Mrs Elizabeth Rachel
Kritzinger (nee Daneel), one of Thode’s pupils.
Thode stayed at “Altemooi” for two years, then
apparently moved to “Tweekloof” for another two
years. Many of Thode’s specimens (1920-1924) were
collected on the farm “Kaffirdrift”, another farm
belonging to Mr Repsold.
Thode’s movements from 1924 to 1931 have been
traced by examining the accession book in the
National Herbarium, Pretoria, and then getting dates
from his specimens in the herbarium (there are 2859
Thode specimens in PRE). In this way Table 3 was
compiled. From Table 3 it will be seen that Thode
spent a considerable time in the Cape and Transvaal.
In 1925-1926 he was tutor on Mr James Trollip’s
farm “Glen Makopo”, Hobhouse, in the district
of Thaba Nchu, Orange Free State.
FINAL DAYS
According to Table 3 Thode must have made his
last collections at Witbank in the Transvaal from
December 1930 to March 1931. No records can be
traced of specimens collected later than this.
It is likely that he spent his last days in Durban
living at 170 Mansfield Road (the address given on
his death notice). It is also possible that he spent
some of his time in the Natal Herbarium naming
his collections. The late Miss Helena M. L. Forbes,
former curator of the Natal Herbarium, wrote to
Miss Gunn (30th October 1953): “Thode had been in
the habit of spending a month or more at the
Herbarium naming his specimens every few years.
I think he came three times after I came here, once
to name up a collection, which he sold to Stellenbosch
University”.
On 30th May 1932 Dr A. P. D. McLean, who was
then stationed at Natal Herbarium, wrote to
Dr I. B. Pole Evans, Chief of the Division of Botany,
stating that Thode was in Addington Hospital in a
critical condition and had been visited by Miss Forbes.
According to Miss Forbes, Thode’s impecunious
state weighed heavily on his mind even when delirious
and he was anxious that his collections be sold.
TABLE 3. — Collecting localities from 1924 to 1931
On 1st June 1932 Thode died and was buried in
a communal grave with no gravestone at Stella
Wood Cemetery, Block N, 1374. Later the grave
site was sold and to-day several gravestones occupy
the site.
David Strachan & Taylor, accountants of Durban,
were asked by the Master of the Supreme Court to
handle Thode’s estate. Thode died insolvent owing
£52. 6s. 6d. It was hoped that the sale of his collection
of 2859 numbers would defray this debt. To this end
negotiations between Strachan & Taylor and the
Division of Botany proceeded protractedly with
Dr McLean pressing for the purchase and the Division
of Botany expressing little interest because, as
Dr E. P. Phillips put it, “The cream of Thode’s
collections i.e. his high mountain gatherings, had
earlier been sold to the University of Stellenbosch”.
Eventually, on 3rd May 1934, the Division of
Botany offered £36 and this was accepted by the
Administrators. There were three or four duplicates
of each specimen, so the collection was made up
into three sets, one for the Natal Herbarium, one
for the National Herbarium, Pretoria, and one for
Kew. The specimens were numbered Al, A2, etc. to
avoid confusion with his other collections. Unfor-
tunately Thode did not adopt a system of continuous
consecutive numbering. This collection was mainly
of Transvaal and Cape plants (see Table 3, which
was based on this collection). The large wooden
trunk in which Thode stored his specimens and other
effects, is still in the Natal Herbarium, Durban.
Thode’s personal effects, beds and odds and ends,
were left to his sister Mrs Alwine Hammer of 340
Vause Road, Durban. Some of his books were sold
by M. Thompson & Co., auctioneers, for 4/6d.
D. J. B. KILL1CK
173
THODE, THE MAN
Fortunately the author was able to contact four
of Thode’s past pupils, namely Mr Erich Mumm-
brauer formerly of the farm “Kronsberg”, Noods-
berg, in Natal, Mr C. J. Cronje formerly of the
farm “Koolhoek” near Memel in the Orange Free
State, Mrs E. R. Kritzinger (nee Daneel) formerly of
the farm “Altemooi” near Utrecht in Natal and
Mrs Lorna Grove (nee Trollip) formerly of the farm
“Glen Makopa”, Hobhouse, in the Orange Free State.
Discussions with these people revealed a
remarkably similar memory of the man. Thode clearly
left a lasting impression on them. He was slightly
built with a moustache and small beard. He always
wore a brown suit buttoned to the top with a wide-
brimmed hat or helmet on his head. His plant press
was slung high up on his shoulders. He was short-
sighted and wore thick spectacles. Thode was an
excellent pianist, being passionately fond of
Beethoven. He showed little patience with his pupils
if they played incorrect notes. Mr Cronje relates how
when the family received visitors the children would
be asked to play the piano. When a mistake was made,
Thode would storm over to the piano and correct
the young pianist. The Cronjes asked him to desist
from this practice, so on similar occasions when
mistakes were made, Thode would walk agitatedly
around the room pretending to put all the pictures
straight.
He seems to have been an accomplished poet (there
are several unpublished poems amongst his papers)
and was very fond of the works of Goethe.
He had a good knowledge of the classics as the
following incident will show. Mr Heinz Lorenz a
former pupil of Thode’s at Empangweni Mission
School told Mr R. G. Strey of the Natal Herbarium
that Thode once taught chemistry and physics at a
school in Pietermaritzburg. In the neighbouring
classroom the headmaster was giving a lesson in
Latin. Thode overhead him incorrectly quoting some
Latin verse or prose. When the headmaster a few
minutes later left the classroom for some reason or
other, Thode quickly nipped into the classroom and
corrected the offending quotation on the blackboard.
On his return, the headmaster was furious that the
quotation had been corrected and promptly sacked
Thode.
Mr E. Mummbrauer recalls that after dinner
Thode would retire to his room and could be heard
walking aroung the room conducting an imaginary
orchestra.
Apparently he never rode on horseback, but used
horses for carrying his equipment.
Thode was fond of good food, but disliked
Mrs Lorenz’s “Mehlklosse”. According to Mr H.
Struck of Draycott, Thode would sometimes outstay
his welcome on the farm and stay for weeks and
weeks. The only way to get rid of him was to put
sago pudding regularly on the table.
Mr Struck tells of an incident when Thode went
visiting the Zunckels in the Bergville area. To get
to the Zunckels, Thode had to cross a river in full
spate. He took off his clothes, tied them into a
bundle and started to ford the river. Unfortunately
the current was strong and he slipped, losing his
clothes in the process. Mr Struck describes the
amusing sight of Thode running from tree to tree to
hide his nakedness and when near the Zunckel
homestead being spotted by the children, who ran
i idoors shouting “There is a naked man outside”.
Thode was no respecter of authority. This is amply
shown in a letter he wrote to the permit secretary
in Durban. He castigated him for his lack of
knowledge of geography and ended off with some
incredibly rude remarks. He was most indignant
when learning from Mr Sydney Barnes, the first
conservator of the Drakensberg Game Reserve that
he would have to pay 6d per day for each of his
party i.e. for himself, Bantu and horse. He wrote:
“The Government, or rather the Forestry Depart-
ment, under whose supervision the Game Reserve
is kept, should know best why and for what purpose
such an absurd system of (taxation) pillaging
travellers has been introduced . . . for our legislators
seem too fond of indulging in measures, the wisdom
of which is shrouded in mystery quite impenetrable
to ordinary common sense”.
He was obviously a man with a short temper.
Prof. A. W. Bayer (letter to author, 3rd June 1965)
tells the story of a collecting trip by ox-wagon made
by Thode with Rudolf Schlechter (probably between
June and October 1893). Schlechter was apparently
rather strict with his Bantu servants and one morning
they found that the servants had deserted. After
No... 3.
Herbarium, University Stellenbosch.
H ERBARIUM I Ex JUSTUS ThODE.
Fig. 3. — Example of the special
label used for Thode’s col-
lection in Stellenbosch Her-
barium. The handwriting is
Thode’s.
174 HANS JUSTUS THODE (1859-1932), PIONEER PLANT COLLECTOR IN THE NATAL DRAKENSBERG
breakfast, they proceeded to break up camp and
to round up and inspan the oxen. Schlechter then
picked up the driver’s whip and announced to Thode
“I will drive; you can voorloop”. Thode was so
annoyed at this brusque instruction that he went up
to the wagon, took his rucksack, turned his back on
Schlechter and disappeared into the bush.
CONTRIBUTIONS TO SOUTH AFRICAN BOTANY
Thode’s contributions to South African botany
lie in the many plant specimens he collected during
his 46 years in the country and in his seven
publications. As already indicated, he was the first
to collect in the Natal Drakensberg, being several
years earlier than H. G. Flanagan and H. Bolus
(summer 1893-94) and Maurice Evans (1894). Thode
was much chagrined when plants like Erica frigida,
E. algida and Gladiolus flanaganii were described
from material collected by Flanagan instead of from
his material collected three years earlier (letter from
Thode to H. Bolus, 5th February 1896).
It is not known how many specimens Thode
collected, because he did not consecutively number
his specimens. He must have sent thousands of
specimens to the Berlin Herbarium; there are 6309
of his specimens in the Stellenbosch Herbarium
(Fig. 3), collected between 1886 and 1920, and
there are 2859 specimens in the National Herbarium,
Pretoria, collected between 1924 and 1931, with
duplicate sets in the Natal Herbarium and at Kew.
The specimens he collected were of good quality, but
often lacked adequate field notes. Oddly enough,
Thode did not collect grasses.
Thode is commemorated in the following species:
Alepidea thodei Diimmer, Athanasia thodei H. Bol.,
Disa thodei Schltr., Erica thodei Guth. & H. Bol.,
Geranium thodei Schltr., Holothrix thodei Rolfe,
Kniphofia thodei Bak., Lessertia thodei L. Bol.’
Manulea thodeana Diels, Osteospermum thodei Mark ’
Rhodohypoxis thodiana (Nel) Hilliard & Burtt’,
Romulea thodei Schltr. and Sebaea thodeana Gilg.
Thode’s papers though few were of a high standard.
The following is a list of his publications:
Thode, J.,* 1890. Die Kustenvegetation von Britisch-
KafFrarien und ihr Verhaltnis zu den Nachbarfloren
Bot. Jahrb. 12: 589-607.
Thode, J„ 1892. Die vier Jahreszeiten am Cap. Naturwissen-
schaftliche Wochenschrift. 7,14: 131-133. 15- 144-147
21:206-207.23:226-228.
Thode, J., 1892. Die botanische Hohenregionen Natals. Bot.
Jahrb. 18. Ill Beibl. 43: 14-45.
Thode, J. 1901. The botanical regions of Natal determined by
altitude. 16 pp. Durban: Durban Field Naturalists’
Society.
Thode, J., 1913. Leucadendron natalense Thode & Gilg.
Notizbl. Bot. Gart. Bert. 5: 290.
Thode, J., 1922. Bowkeria citrina Thode. Kew Bull. 1922- 31
(1922).
Thode, J., 1924. A new Pyrenacantha from Natal. J. Bot.
42: 115-116 (1924).
In his first paper, “Die Kustenvegetation von
Britisch-Kaffrarien und ihr Verhaltnis zu den Nach-
barfloren” (1890), Thode compared the coast
vegetation of British Kaffraria with that of the
south-west Cape and Natal. He showed that although
Compositae and Leguminosae were the two dominant
families in all three regions, the remaining families
differed significantly in their order of importance.
Illustrating his broad knowledge and interest in
floristics and plant geography, Thode compared the
flora of East London with the floras of Ethiopia and
India.
* Thode always omitted the initial of his Christian name, Hans.
TABLE 4. — Location of some Thode localities mainly in Natal
D. J. B. KILLICK
175
His second paper, “Die vier Jahreszeiten am
Cap” (1892) showed a surprising knowledge of the
south-west Cape flora after only a short period of
residence there. Thode described the four seasons
of the Cape and related them to the flora; he com-
mented on the effect of fire on fynbos; he mentioned
the exploitation of the flora and urged that con-
servation measures be adopted.
In 1894 he published “Die botanische Hohen-
regionen Natals”, an accurate picture of altitudinal
zonation of vegetation in Natal. This paper stamps
Thode as a competent plant geographer. His
description of the vegetation of the Natal Drakens-
berg is the first on record and is extremely accurate
as to detail.
In 1901 he published “The botanical regions of
Natal determined by altitude”. This represents a
condensed version of his 1894 paper, translated into
English and read before the Durban Field Naturalists’
Society on 16th May 1901.
The remaining papers were descriptions of new
species.
In conclusion, it may be said that Thode’s
contributions to South African botany were
considerable, especially if it is realized that he was
an amateur botanist, attached to no institution, with
no library facilities and collecting in remote areas
often never collected before. Bolus in writing to
A. W. Hill at Kew (26th August 1905) described
Thode as “wanting in systematic effort and regularity,
and so has not done all he might have done”. This
is a somewhat harsh judgement, but Bolus does
concede that “he has written some valuable papers
on the flora of that region”.
LOCATION OF CERTAIN THODE COLLECTING
LOCALITIES
Taxonomists have frequently found difficulty in
locating some of Thode’s localities. This is partly
due to Thode’s frequent use of farm names. To
assist taxonomists, the exact location of some of the
“problem” localities is given in Table 4.
ACKNOWLEDGEMENTS
Thanks are due to Miss M. D. Gunn for having
done some of the spadework in this research and for
her continued interest in its progress. Thanks are
also due to Miss E. Hagedorn for translating some of
the original manuscripts from German to English.
UITTREKSEL
V i Verslag word gegee van die lewe van Hans Justus
Thode (1859-1932), vanaf s& aankoms in Kaapstad
in 1885 o/" 1886 tot sy dood in Durban in 1932. Thode
was die baanbreker-plantversamelaar van die Natalse
Drakensberge, maar hy het ook verder weg in al vier
provinsies van die Republiek plante versamel. 'n
Waardasie van sy bydraes tot Suid-Afrikaanse plant-
kunde word gemaak.
REFERENCES
Markotter, E. I., 1930. 'n Plantgeografiese skets en die flora
van Witzieshoek, O.V.S.; Oliviershoekpas, Natal en Kool-
hoek, O.V.S. Ann. Univ. Stell. 8, Al : 1-50.
t
Bothalia 12,2:177-179 (1977)
The South African species of Teucrium (Lamiaceae)
L. E. CODD*
ABSTRACT
While writing up the three South African species of Teucrium for the Flora of Southern Africa it became
necessary to replace two well-known names as follows: T. Irifidum Retz. (1779) (=T. capense Thunb., 1800)
and T. kraussii Codd (=T. riparium Hochst., 1845, non Rafin., 1838).
RESUME
LES ESPECES SUD-AFRICAINES DE TEUCRIUM ( LAMIACEAE )
En etudiant les trois especes sud-africaines de Teucrium pour inclusion dans la Flore d'Afrique
australe, il s'est avere necessaire de remplacer comme suit deux noms largement connus: T.trifidum
Retz. (1779) (=T.capense Thunb., 1800) et T.kraussii Codd (= T.riparium Hochst., 1845, non Rafin.,
1838).
Teucrium is a large genus of perhaps 300 species
widely distributed over the temperate and warmer
regions of the world, chiefly in the northern
hemisphere, but with a few species in Australia, South
America and Africa, mainly on the mountains of
north-east tropical Africa and into South Africa.
Three species are recognized in South Africa and,
because the small white flowers are very similar and
provide no diagnostic characters, the species are
distinguished on vegetative and inflorescence
characters. As may be expected, misidentifications
have occurred in herbaria, resulting in miscon-
ceptions regarding distribution.
Considering the fact that the names commonly
applied to these three species have been in use for
well over a century, it came as a surprise to find
that two name changes were required: (1) T. irifidum
Retz. (1779) must replace T. capense Thunb.; and
(2) T. riparium Hochst. (1845) is a later homonym
of T. riparium Rafin. (1838), an American species,
and is replaced by a new name, T. kraussii
Codd.
All three species are used medicinally for stomach
disorders and haemorrhoids, as well as for treating
snake-bite, while meat suspected of being infested
with anthrax is boiled with the plant to render it
harmless to eat. Common names such as Aambeibossie
and Maagbossie refer to these properties, while
Paddaklou and Akkedispoot refer to the variously
lobed leaves.
Key to species
Peduncles usually 1-flowered (rarely 3-flowered) and much shorter than the internodes; shrub-
lets 10-30 cm tall; leaves narrowly 3-fid, 0,5-2, 5 cm long 1. T. africanum
Peduncles 3-7-flowered, often as long as or longer than the internodes; soft shrubs 30-110
cm tall ; leaves 3-5-fid or -lobed, or subentire with a few teeth towards the apex, 2-6
cm long:
Leaves more or less 3-5-fid or -lobed, if subentire then drying greyish 2. T. trifidum
Leaves entire or few-toothed towards the apex, usually drying dark brown 3. T. kraussii
1. Teucrium africanum Thunb., Prodr. 2: 95
(1800); FI. Cap. ed Schult. 445 (1823); Benth.,
Lab. 669 (1835); in E. Mey., Comm. 243 (1837); in
DC., Prodr. 12: 577 (1848); Skan in FI. Cap. 5, 1 : 384
(1910). Type: Cape, without locality, Thunberg s.n.
(UPS, holo.).
Ajuga africana (Thunb.) Pers., Syn. PI. 2: 109 (1807).
Greyish, bushy shrublet 10-25 (-30) cm tall,
branching freely from the base; stems erect to
decumbent, simple or sparingly branched, rather
densely leafy, greyish glandular-tomentose. Leaves
3-fid, 0,8-3 cm long, grey-green; lobes linear to
linear-oblong, 0,5-2, 5 cm long, 1-3 mm broad,
occasionally the median lobe again 3-fid; basal
portion of leaf narrow, up to 3 mm broad. Inflores-
cence simple, occupying the upper third of half of
the stem; flowers solitary or rarely 2 or 3 per peduncle;
peduncles 3-8 mm long, usually distinctly shorter
than the internodes.
Found under fairly arid conditions in macchia,
karoo, coastal or thorn scrub from Bredasdorp to
near Grahamstown and, inland, to Middelburg and
Graaff Reinet.
May be separated from the next species, T. trifidum,
by its smaller stature, rarely exceeding 30 cm tall,
and the usually solitary flowers on short peduncles.
* Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria.
Bentham, Lab. 670 (1835) and in DC., Prodr.
12: 577 (1848) placed T. trifidum Retz. (1799) as
being possibly conspecific, while Skan in FI. Cap,
5,1: 384 (1910) added T. trifidum Wendl. (1798) with
a question mark. These names are discussed under
the next species.
2. Teucrium trifidum Retz., Obs. 1: 21 (1779).
Type: Cape, without locality, right-hand specimen
on sheet in Hb. Retzius (LD, lecto.).
T. trifidum Wendl., Bot. Beobacht. 50 (1798); nom. illegit.
Type- not indicated. T. capense Thunb., Prodr. 95 (1800); FI.
Cap. ed Schult. 445 (1823); Benth., Lab. 667 (1835); in E.
Mey., Comm. 243 (1837); in DC., Prodr. 12: 577 (1848); Skan
in FI. Cap. 5,1: 385 (1910); Wilman, Checklist Griq. W. 231
(1946); Jacot-Guill., FI. Lesotho 236 (1971); Ross, FI. Natal
302 (1972). Type: Cape, near “Zeekoerivier” (Humansdorp
district), Thunberg s.n. (UPS, holo.). T. africanum sensu Wilman,
l.c. (1946).
Ajuga capensis Pers., Syn. PI. 2: 109 (1807).
An erect soft undershrub 30-1 10 cm tall, branching
freely from the base; stems virgate, branching freely
in the upper half or third, woody below, herbaceous
above, thinly and shortly greyish tomentose. Leaves
usually deeply 3-fid or 3-5-partite, rarely almost entire
or shortly toothed towards the apex, 2-6 cm long,
drying greyish-green to grey-brown, thinly tomentose
to almost canescent; lobes linear to lanceolate,
1-3,5 cm long, 3-8 mm broad, often again shortly
lobed or toothed; basal portion of leaf 3-8 mm
broad. Inflorescence a leafy panicle occupying the
178
THE SOUTH AFRICAN SPECIES OF TEUCRIUM (LAMIACEAE)
DOTANISKA
MC't.tT
LUND
N« I lerb , Pretoria
i’RC Nee. No.. 629/
Fig. 1. — Type of Teucrium trifi-
dum in the Retzius Herba-
rium, LD (right-hand speci-
mens selected as the lecto-
type).
upper third of the stem; flowers usually in 3-7-
flowered pedunculate cymes, rarely solitary; peduncles
5-20 (25) mm long, usually longer than the internodes.
Common in the central and south-western
Transvaal, apparently not extending beyond the
Soutpansberg, but extending westwards to the
northern Cape Province and just entering Botswana,
southwards to northern Natal, central Orange Free
State and eastern Cape Province, reaching its south-
westerly limit about Humansdorp. Characteristically
found in dry woodland where it is often gregarious
under thorn trees or in bush groups, particularly on
overgrazed or disturbed places.
The leaves of S’, trifidum vary considerably from
lanceolate and almost entire to deeply 3-5-partite.
It overlaps with T. afrieanum in the southern Cape
from about Grahamstown inland to Queenstown and
occasional specimens, from the latter area particularly,
may be difficult to place with certainty. T. afrieanum
can usually be separated on the basis of the shorter
stature, rarely exceeding 30 cm tall, and the usually
solitary flowers on short peduncles. In the northern
Cape, under semi-arid conditions, T. trifidum tends to
produce plants shorter than usual with somewhat
shorter, but 3-flowered, peduncles. These have often
in the past been identified as T. afrieanum, e.g. in
Wilman, Checklist Griq. W. 231 (1946), but their
affinity lies with T. trifidum.
In eastern Cape, about Komga, T. trifidum overlaps
with T. kraussii and here again occasional specimens
may need careful study to be sure of their identity.
In such cases, specimens of T. trifidum with subentire
leaves can be recognized by the leaves being some-
what smaller and greyish-green, as against the longer
and broader leaves of T. kraussii, which tend to dry
dark brown.
As mentioned under the previous species, the
names T. trifidum Retz. (1779) and T. trifidum Wendl.
(1798) were tentatively included in T. afrieanum by
earlier authors. The type of T. trifidum Retz. is
present in the Retzius Herbarium, Lund, and was
kindly sent on loan to me by the Curator, Dr Ove
Almborn, whose assistance is gratefully acknowledged.
This was examined in relation to the two names
published by Thunberg in 1800, T. afrieanum Thunb.
and T. capense Thunb.
L. E. CODD
179
The type sheet, annotated as Teucrium trifidum N.
by Retzius on the reverse side, has two specimens
mounted on it (see Fig. 1). The left-hand specimen
corresponds with T. africanum Thunb. and the right-
hand specimen with T. capense Thunb. It is, therefore,
necessary to scrutinise the protologue carefully and
a copy of the significant parts is given below:
65. TEUCRIUM trifidum foliis lanceolatis trifidis, pedunculis
axillaribus trifloris.
Habitat ad Cap. B. Spei, unde habui, dono D. BLADH.
Caulis tetragonus, hirtus, ramosus, foliosus.
Folia opposita, lanceolata, majora lobo, minora dente
utrinque acuto incisa, ceterum integra, supra scabra,
subtus tomentosa; tomento flavescente vix conspicuo.
Pedunculi oppositi, axillares, triflori, longitudine inter-
nodiorum.
The epithet trifidum would apply more correctly
to the left-hand specimen, but the short diagnosis is
applicable mainly to the right-hand specimen. The
rest of the protologue describes the significant
characteristics of the right-hand specimen, eg.:
“ Caulis . . . ramosus . . “ Folia lanceolata, majora
lobo, minora dente utrinque acuto inciso, ceterum
integra . . “ Pedunculi . . . triflori, longitudine
internodiorum.” In fact no mention is made of the
characters exclusive to the left-hand specimen (the
deeply trifid leaves and single flowers on short
peduncles), while all the characteristics mentioned
above apply exclusively to the right-hand specimen.
There is thus nothing in the description to compel
one to the view that it is based on a mixture of the
two specimens but, assuming that Retzius had both
before him, it is considered advisable to make the
right-hand specimen the lectotype. This means that
T. capense Thunb. goes into synonymy.
One may speculate how the specimens were acquired
by Bladh, who was a “supercargo” in the Swedish
East Indian Company from 1766 to 1784 and sent
plants from China, Indiafl and South Africa to
several Swedish botanists. He is not known to have
travelled at all in South Africa, but might have
obtained specimens from Thunberg, who had under-
taken an expedition together with Masson in 1773-74
to the Sundays River area, where both species are
found.
T. trifidum Wendl. is an illegitimate homonym.
No specimen is cited but the description suggests that
it is conspecific with T. trifidum Retz.
3. Teucrium kraussii Codd, nom. nov. Type:
Natal, Umlaas River, Krauss 153.
T. riparium Hochst, in Flora 66 (1845); Benth. in DC.,
Prodr. 12: 576 (1848); Skan in FI. Cap. 5,1: 385 (1910);
Compton, FI. Swaz. 66 (1966); Ross, FI. Natal 302 (1972);
nom. illegit., non T. riparium Rafin. (1838). Type: as above.
An erect soft undershrub 50-1 10 cm tall, branching
from the base; stems simple below, branched in the
upper half or third, softly woody below, herbaceous
above, finely to fairly densely tomentose, usually
with spreading hairs. Leaves narrowly lanceolate to
oblong-lanceolate or oblanceolate, 2,5-6 cm long,
remotely 1 — few toothed towards the apex or entire,
subglabrous or sparingly hispidulous above, sparingly
to fairly densely hispid and minutely gland-dotted
below; apex obtuse to acute, base narrowly cuneate.
Inflorescence a leafy panicle occupying the upper
third of the stem, often diffusely branched; flowers
in 2-7-flowered pedunculate cymes; peduncles 6-20
mm long, usually longer than the internodes.
Distributed from Swaziland through semi-coastal
and midland Natal to King William’s Town district
in the Cape, in open bush and grassland.
T. kraussii overlaps with T. trifidum in the eastern
Cape Province and occasional intermediate specimens
may be difficult to place with certainty. The main
distinguishing characters are discussed under T.
trifidum.
UITTREKSEL
Tydens die beskrywing van drie Suid-Afrikaanse
soorte Teucrium vir die Flora of Southern Africa,
het dit nodig geblyk om twee goedbekende name as
volg te vervang: T. trifidum Retz. (1779) (=T. capense
Thunb., 1800) en T. kraussii Codd (=T. riparium
Hochst., 1845, non Rafin., 1838).
Bolhalia 12,2: 181-189 (1977)
A note on the Stachys aethiopica Complex
L. E. CODD
ABSTRACT
The Stachys aethiopica Complex is examined and a key provided to the species recognized. The com-
bination 5. natalensis Hochst. var. galpinii (Briq.) Codd is effected and two new species, S. reticulata Codd
and S. arachnoidea Codd are described.
RESUME
NOTE SUR LE COMPLEXE DES STACHYS AETHIOPICA
Le complexe des Stachys aethiopica est examine et une cle est fournie pour les especes reconnues.
Une nouvelle combinaison est operee: S. natalensis Hochst. var. galpinii (Briq.) Codd; et deux especes
nouvelles sont decrites: S. reticulata Codd et S.arachnoidea Codd.
Among the South African species of Stachys one
of the main taxonomic problems concerns the
delimitation of species in the S. aethiopica Complex.
These comprise mainly soft, nondescript, somewhat
straggly perennial herbs with small ovate cordate
leaves and relatively small, inconspicuous flowers.
The complex extends from the south-western extremity
of the Cape Province, through the eastern summer-
rainfall parts of southern Africa northwards into
tropical Africa.
S. aethiopica L., Mant. 1: 82 (1767) was the first
to be described and was presumably based on
material from the south-western Cape Province.
Further species have been distinguished on the basis
of differences in tomentum, whether the leaves are
petiolate or sessile, on the number of flowers per
verticil and, to some extent, on leaf shape.
Our species were reviewed by Skan in FI. Cap-
5,1: 336-367 (1910), who upheld 19 species in this
complex, namely: S. rehmannii Skan, S. malacophylla
Skan, S. sessilifolia E. Mey. ex Benth., S. galpinii
Briq., S. transvaalensis Guerke, S. rudatisii Skan,
S. parilis N.E. Br., S. aethiopica L., S. scabrida Skan,
S. cooperi Skan, S. harveyi Skan, S. serrulata Burch,
ex Benth., 5. attenuata Skan, S. fruticetorum Briq.,
S. leptoclada Briq., S. flexuosa Skan, S. cymbalaria
Briq., S. priorii Skan, and 5. sublobata Skan, while the
following were treated as “imperfectly known ’’species:
S. capensis Presl, S. graciliflora Presl, S. hispidula
Hochst. and S. natalensis Hochst. The only species
added since then is H. villosissima H. M. Forbes from
Natal.
Most of these entities represent local variations of
restricted extent which may or may not warrant the
rank of species. Due to inadequate collecting, many
of them are still very poorly known and a good deal
more material is required before their status can
be assessed.
In the present study the above 24 “species” are
reduced to 11, while two additional species are
described from the eastern Transvaal and Swaziland.
In few cases are there clear-cut differences between
species and it is often necessary to rely on a com-
bination of characters.
The picture which emerges is of two widespread
and variable species, from which a number of
segregate species have arisen or are in the process
of developing. The two widespread “parent” species,
which can usually be separated on the basis of
pubescence, are:
(1) S', aethiopica L., with a mainly southern
distribution from the south-western Cape to Natal,
Lesotho and the Orange Free State, with the lower
surfaces of the leaves and calyces thinly tomentulose
to hispid or densely glandular;
(2) a more northerly species, to which the name
S. natalensis Hochst. is applied, extending from
Natal to Swaziland, Transvaal and Rhodesia, with
the lower surfaces of the leaves and calyces hispid-
villous (sometimes only on the nerves) to densely
villous (often obscuring the surface), and with
scarcely any glands.
The two species meet in Natal, where a gradation
in pubescence occurs. In this critical area, however,
one can separate them on another character, the
number of flowers per verticil. In S', natalensis the
verticils are 2-flowered throughout its entire range;
in S. aethiopica the verticils appear to be always
4-6-flowered in Natal, Lesotho and the Orange Free
State. In the Cape occasional specimens, some of
them rather depauperate, are found with 2 or 3
flowers per verticil, but these do not have villous
pubescence and would not be confused with S.
natalensis. In this way, the two species can be
maintained as distinct and some of the confusion
of the past concerning the limits of S. aethiopica can
be clarified.
With regard to the number of flowers per verticil,
it must be remembered that there are certain segregate
species related to S. aethiopica which have 2-flowered
verticils (5. rudatisii, S. cymbalaria and S. sublobata),
in the same way that there are species with villous
to densely tomentose pubescence related to S.
natalensis but with 4-6-flowered verticils (5. malaco-
phylla and the newly described S. reticulata). In
other species the number of flowers per verticil is
not constant and may very from 2-6 (S. rehmannii,
S. scabrida and S. flexuosa).
From the foregoing it will be realized that the
construction of a key that will work satisfactorily
for every specimen is not an easy matter. The following
key must, therefore, act mainly as a guide. With the
increase in knowledge as further material comes in,
it is quite likely that our species concepts will be
modified.
182
A NOTE ON THE STACHYS AETHIOPICA COMPLEX
Key to species in the S. aethiopica Complex
Leaves and calyx villous, often densely so, the lower surface of the leaves sparingly hispid-villous to
densely tomentose:
Pubescence stellate 3. S. rehmannii
Pubescence not stellate:
Verticils 2-flowered:
Leaves discolorous, sparingly pubescent and greenish-brown above, white tomentose below: bracts
leaf-like 2. S. arachnoidea
Leaves concolorous; bracts usually differentiated from the leaves:
Leaves densely matted-tomentose below obscuring the surface 6. S. sessilifolia
Leaves densely to sparingly strigose or hispid below, often mainly on the nerves:
Inflorescence compact, 3-6 cm long; corolla purple, the lower lip up to 8 mm long, longer
than the tube 13. S. flexuosa
Inflorescence fairly compact to lax, (4-) 6-15 cm long; corolla whitish, the lower lip 5-7 mm
long, shorter than the tube 7. S. natalensis
Verticils normally 4-6-flowered (an occasional 2-flowered verticil may be present):
Stem with longish appressed retrorse hairs; leaves often discolorous and reticulate-veined
below 4. S. reticulata
Stem spreading-pilose to villous or with short retrorse hairs; leaves concolorous:
Leaves densely matted-tomentose below, obscuring the surface:
Leaves petiolate; uppermost bracts shorter than the calyx 5. S. malacophylla
Leaves usually sessile or subsessile; uppermost bracts longer than the calyx.... 6. S. sessilifolia
Leaves strigose to hispid below, mainly on the nerves:
Leaves drying greenish, truncate to subcordate at the base; inflorescence usually
compact 13. S. flexuosa
Leaves usually drying brownish, deeply cordate at the base; inflorescense usually lax. .8. S. aethiopica
Leaves and calyx subglabrous to hispid or glandular-tomentulose, the lower surface of the leaves glabrous
to hispid (mainly on the nerves) or glandular-puberulous:
Verticils 2-flowered:
Lower surface of leaf and calyx gland-dotted:
Leaves 2-4,5 x 1 ,5-2,5 cm, fairly thick-textured; margin finely and regularly crenulate. .1.5. rudatisii
Leaves less than 2 cm long or, if longer, margin rather coarsely toothed :
Leaves broadly ovate to suborbicular, shallowly crenate 11. 5. cymbalaria
Leaves ovate, usually thin-textured, margin rather coarsely toothed 8. 5. aethiopica
Lower surface of leaves and calyx eglandular or nearly so :
Stem glabrous to sparingly retrorse-scabrid or with scattered longish hairs:
Leaves drying dark brown, ovate-deltoid; hairs on upper leaf surface, when present, bulbous-
based 10. 5. scabrida
Leaves drying greenish-brown; hairs on upper leaf surface not bulbous-based:
Leaf blade broadly ovate to suborbicular, 8-15x6-12 mm; margin shallowly crenate
11. 5. cymbalaria
Leaf blade narrowly triangular, 10-15x4-6 mm; margin deeply crenate 12. 5. sublobata
Stem variously pubescent but not as above:
Stem and rhachis usually hispid-villous, fairly rigid, eglandular (Natal, Swaziland, Transvaal)
7. 5. natalensis
Stem and rhachis shortly retrorse-pubescent to softly pilose often glandular (western Cape)
8. 5. aethiopica
Verticils 4-6-flowered (an occasional 2-flowered verticil may be present):
Stem subglabrous to sparingly retrorse-scabrid or with scattered multicellular retrorse hairs; hairs
on upper leaf surface, when present, bulbous-based 10. 5. scabrida
Stem variously pubescent but not as above:
Inflorescence of 1-4 (rarely more) verticils, often subcapitate to somewhat spaced below; calyx,
rhachis and leaves eglandular; stem shortly and softly retrorse-pubescent 9. 5. graciliflora
Inflorescence usually slender of few to several spaced verticils (rarely subcapitate); glandular hairs
or gland-dots often present on calyx, rhachis and lower surface of leaves; stem variously
pubescent 8. 5. aethiopica
1. Stachys rudatisii Skan in FI. Cap. 5, 1: 347
(1910); Ross, FI. Natal 304 (1972). Type: Natal,
Dumisa, Rudatis 405 (K, holo. ; NH!, PRE!).
Stems glandular hispidulous with retrorse multi-
cellular hairs and copious short glandular hairs.
Leaves petiolate, rather large; blade ovate, (2-)
3-4,5 x(l ,5-)2-2,5 cm, the lower surface densely
glandular-hispidulous; margin finely crenulate. Bracts
leaf-like to somewhat differentiated. Verticils 2-
flowered. Calyx glandular hispid.
A little-known species from southern Natal where
it apparently grows in damp grassy places among
rocks and in shady thickets.
Natal.— 3029 (Kokstad): Ngeli Mt. (-DA), Hilliard &
Burn 3488. 3030 (Port Shepstone): Dumisa (-AD), Rudatis 405.
S. aethiopica (p. 186) often has densely glandular
stems and leaves but the leaves are usually smaller,
broadly ovate and rather coarsely toothed, while the
verticils are normally 4-6-flowered, not 2-flowered
as in S. rudatisii. In the type, Rudatis 405, the bracts
are large and leaf-like, while in Hilliard & Burtt
3488 the bracts are reduced, making it somewhat
intermediate with S. aethiopica. A specimen from the
Hogsback, Rattray sub BOL 14275, may belong here,
but the leaves are broadly ovate and subsessile.
If the specimen were included here, the known area
of the spesies would be extended considerably but
more material, especially from the type area, is
required before the limits of the species can be
assessed.
2. Stachys arachnoidea Codd, sp. nov., a S.
natalensis Hochst. foliis discoloribus, subtus dense
albo-tomentosus et minute flavo-punctatis differt.
L. E. CODD
183
Herba, perennis, aromaticus; caules procumbens
vel subscandens, ramosus, usque ad 1 m longus,
quadrangularis, sulcatus, dense et molliter albo-
tomentosus. Folia subsessilia vel breviter petiolata;
petiolus usque ad 1 cm longus; lamina late ovato-
deltoidea vel subrotunda, 1,8-4 cm longa, 1,5-
3 cm lata, chartacea, supra olivacea tenuiter
pubescens, subtus dense albo-arachnoidea et minute
flavo-punctata, apice obtuso vel rotundato, basi
cordata, margine crenulata. Inflorescentia laxa, 5-15
cm longa; bracteae foliiformes versus apicem leviter
parviores; verticillastri 2-floribus; pedicelli 1,5 mm
longi. Calyx tubuloso-campanulatus, 8-9 mm longus,
dense et molliter albo-tomentosus et minute punc-
tatus; dentes deltoideo-lanceolati, 3-4 mm longi.
Corolla alba, malvino-maculata, subtiliter glanduloso-
pubescens; tubus 8-9 mm longus, 2 mm diam.;
labium posticum ascendens, concavum, 3-4 mm
longum, 3 mm latum, apicem rotundato; labium
anticum horizontale, 8-9 mm longum, lobo medio
obcordato, 4 mm longo, lobis lateralibus rotundatis,
1,5 mm longis. Stamina 4, 2-3 mm fauce exserta.
Stylus bifidus, 2 mm exsertus.
Type. — Swaziland, near Mbabane, Compton 25890
(PRE, holo.!).
Perennial aromatic herb; stems procumbent to
subscandent, branched, up to 1 m long, 4-angled,
grooved, densely and softly white tomentose.
Leaves subsessile to shortly petiolate; petiole up to
1 cm long; blade broadly ovate-deltoid to subrotund,
1 ,8-4 cm long, 1 ,5-3 cm broad, chartaceous, greenish
and thinly pubescent above, the lower surface with a
dense white web-like tomentum and freely supplied
with minute yellowish pustule-like gland-dots; apex
obtuse to rounded, base cordate; margin crenulate.
Inflorescence lax, 5-15 cm long; bracts leaf-like,
slightly smaller towards the apex; verticils 2-flowered;
pedicels 1,5 mm long. Calyx tubular-campanulate,
8-9 mm long, densely and softly white tomentose
and minutely gland-dotted; teeth deltoid-lanceolate,
3-4 mm long. Corolla white spotted with mauve,
finely glandular-pubescent; tube 8-9 mm long,
2 mm in diameter; upper lip ascending, concave
3-4 mm long, 3 mm broad, apex rounded; lower lip
horizontal, 8-9 mm long, median lobe obcordate,
4 mm long, lateral lobes rounded, 1,5 mm long.
Stamens 4, exserted by 2-3 mm. Style bifid, exserted
by 2 mm. Fig. 1.
Found in forest margins and on grassy slopes in
the mountains of eastern Transvaal and northern
Swaziland at altitudes of 1 300-2 000 m.
Transvaal. — 2329 (Pietersburg): near Haenertsburg (-DD),
Codd9453. 2330 (Tzaneen): Westfalia Estate (-CA), Scheepers
729; Woodbush Forest (-CC), Mogg 20300; Agatha (CC),
McCallum s.n. 2430 (Pilgrims Rest): Mariepskop (-DB),
Van der Schijff 4401 ; 5139. 2530 (Lydenburg): 18 km W. of
Sabie (-BA), Codd 9858.
Swaziland. — 2531 (Komatipoort): Havelock area (-CC),
Miller 5858; Compton 30650. 2631 (Mbabane); Forbes Reef
(-AA), Compton 30492; near Mbabane (-AC), Bolus 12242
BOL); Compton 25890; 26481.
Although first collected as early as 1905 by Bolus
near Mbabane in Swaziland, this species has been
confused with S. transvaalensis (now included in
S. natalensis, p. 185) and S. rudatisii. It was listed
under both these names by Compton, FI. Swaz. 66
(1966), but can be distinguished by the rounder,
discolorous leaves with white cobwebby tomentum
and minute yellow gland-dots on the lower surfaces.
It shows no close relationship to any other species
and is probably the most clear-cut member of the
S. aethiopia complex.
Fig. 1. — Stachys arachnoidea, near Mbabane, Swaziland
{Compton 25890 in PRE, holotype), x
3. Stachys rehmannii Skan in FI. Cap. 5,1: 345
(1910). Type: Transvaal, Houtbosch, Rehmann 6178
(K, holo.!).
Stem sparsely to densely stellate-hispid. Leaves
petiolate, blade ovate-deltoid to subrotund, 1,6-
2, 2 x 1,5-2 cm, densely grey stellate-hispid on both
surfaces. Brads differentiated from the leaves towards
the apex. Verticils usually 2-flowered but sometimes
4-6-flowered. Calyx densely and shortly stellate-
villous.
Found among rocks in mountain grassland at
altitudes of 1 300-2 200 m in the northern and
north-eastern Transvaal.
Transvaal. — 2328 (Baltimore): Blouberg (-BB), Codd &
Dyer 9022; Van der Schijff 5399 ; Strey & Schlieben 8515. 2329
(Pietersburg): Houtboschberg (-DD), Schlechter 4454. 2330
(Tzaneen): 2 km E. of Steilkop, New Agatha (-CC), Muller &
Scheepers 73. 2430 (Pilgrims Rest): The Downs (-DD), Rogers
22027.
Readily distinguished from all other members of
the S. aethiopica complex by the presence of dense
stellate pubescence on all parts of the plant.
4. Stachys reticulata Codd, sp. nov., a 5.
aethiopica L. foliis discoloribus, subtus reticulatis
dense tomentosis, dentibus calyce patentibus differt.
Herba, perennis, aromaticus; caules decumbens vel
procumbens, ramosus, usque ad 60 cm longus,
inflorescentiis adscendentibus, dense retrorso-pilosus.
Folia petiolata; petiolus 5-12 mm longus; lamina
ovato-deltoidea, late ovata vel subreniformis,
1-2,5 x 0,8-2, 2 cm, subcoriacea, plerumque discolor.
184
A NOTE ON THE STACHYS AETHIOPICA COMPLEX
supra hispida, subtus reticulata, dense glanduloso-
tomentosa, basi late cordata, apice obtuso vel
subacuto, margine crenulata. Inflorescentia laxa,
4-8 cm longa, interdum subcapitata; bracteae
reductae, superis calyce breviores; verticillastri 4-6
floribus; pedicelli 1 mm longi. Calyx tubuloso-
campanulatus, 7-8 mm longus, dense glanduloso-
hispidus; dentes lineari-lanceolati, acuminati, 2,5-3
mm longi, patentes. Corolla alba vel lilacina, subtiliter
glanduloso-pubescens; tubus 8-9 mm longus, 2 mm
diam.; labium posticum horizontale, oblongum,
4-5 mm longum, concavum; labium posticum
deflexum, 6-7 mm longum, lobo medio subrotundo,
4 mm longo, lobis lateralibus 2 mm longis. Stamina
4, 4 mm fauce exserta; filamenta puberula. Stylus
bifidus, 4 mm exsertus.
Type. — Transvaal, Mariepskop, Werdermann &
Oberdieck 1868 (PRE, holo. !).
Perennial aromatic herb; stems decumbent to
procumbent, branched, up to 60 cm long with the
inflorescences ascending, 4-angled, fairly densely
retrorse pilose. Leaves petiolate; petiole 5-12 mm
long; blade ovate-deltoid to broadly ovate or
subreniform, 1-2,5 x 0,8-2, 2 cm, fairly firm textured,
usually discolorous, upper surface hispid, lower
surface reticulate-veined, densely glandular-tomentose ;
base broadly cordate, apex obtuse to subacute;
margin crenulate. Inflorescence lax, 4-8 cm long,
occasionally subcapitate; bracts reduced, the upper
ones shorter than the calyx; verticils 4-6-flowered;
pedicels 1 mm long. Calyx tubular-campanulate,
7-8 mm long, densely glandular-hispid; teeth linear-
lanceolate, acuminate, 2,5-3 mm long, spreading.
Corolla white to pale mauve, finely glandular-
pubescent; tube 8-9 mm long, 2 mm in diameter;
upper lip horizontal, oblong, 4-5 mm long, concave;
lower lip deflexed, 6-7 mm long median lobe
subrotund, 4 mm long, lateral lobes 2 mm long.
Stamens 4, exserted by 4 mm; filaments puberulous.
Style bifid, exserted by 4 mm. Fig. 2.
Found among rocks in exposed situations in
mountain grassland in the Pilgrims Rest District of
the eastern Transvaal at altitudes of 1 500 to 2 200 m.
Transvaal. — 2430 (Pilgrims Rest): Mariepskop (-DB),
Meeuse 9963; Killick & Strey 2391 ; Werdermann & Oberdieck
1868; Bos 1028; Van der Schijff 4456 ; 4823; near Pilgrims Rest,
Black Hill, Ga/pin 14342; W. of Pilgrims Rest, Meeuse 10047;
God’s Window, 10 km N. of Pilgrims Rest, Davidson & Mogg
33093.
Although confused in the past with S. aethiopica,
5. reticulata may be distinguished by the usually
discolorous leaves, reticulate and densely tomentose
below, and by the spreading calyx teeth, The
tomentum on the stems is also characteristic being
fairly densely appressed pilose. The stem pubescence
of S. aethipica varies from retrorse to antrorse or
spreading, but is usually short and hispid.
From S. natalensis it differs in the 4-6-flowered
verticils, the reticulate venation on the undersides of
the leaves and in the spreading calyx teeth, while
from S. rehmannii it can readily be separated by the
simple, not stellate, pubescence.
It was first collected on the exposed summits of
hills near Pilgrims Rest by Galpin in 1937 and
appears to be restricted to the mountains of the
Pilgrims Rest District, where it usually grows among
rocks of the Black Reef quartzite formation.
5. Stachys malacophylla Skan in Kew Bull.
1909: 421 (1909); FI. Cap. 5, 1 : 345 (1910). Lectotype:
Cape, Queenstown, Galpin 1955 (K, lecto.; PRE!).
Fig. 2. — Stachys reticulata , Mariepskop, Transvaal ( Werder-
mann & Oberdieck 1868 in PRE, holotype), X F
Stem fairly densely spreading-pilose. Leaves
petiolate, blade broadly ovate, 1, 4-3 x 1-2,2 cm,
densely appressed pilose above, matted velvety pilose
below. Bracts differentiated from the leaves. Verticils
usually 4-6-flowered but sometimes 2- or 3-flowered.
Calyx densely hispid-villous.
A little-known species from mountains in the
eastern Cape Province.
Cape. — 3126 (Queenstown); near Queenstown (-DD), Galpin
1955; 5891. 3227 (Stutterheim): King William’s Town (-CD),
Sim 19590.
Closely related to S. sessilifolia from which it is
separated by the petiolate leaves and usually 4-6-
flowered verticils, while the tomentum on the stems
and leaves is less densely woolly. Both species are
very poorly known and further collecting is required
in order to establish how reliable these distinctions
are. See also notes under S. reticulata from the
eastern Transvaal.
6. Stachys sessilifolia E. Mey. ex Benth. in E.
Mey., Comm. 239 (1837); Drege, Zwei Doc. 151
(1843); Benth. in DC., Prodr. 12: 476 (1848); Skan
in FI. Cap. 5,1: 345 (1910) Type: Cape, between
Umzimvubu and Umsikaba Rivers, Drege 4752 (K,
holo. !).
S. bachmannii Guerke in Bot. Jahrb. 26: 75 (1898). Type:
Cape, Pondoland, Bachmann 1169.
Stem densely and softly villous. Leaves shortly
petiolate below, sessile above; blade ovate to ovate-
deltoid or narrowly ovate, 1-2,2 x 0,7-1 , 1 cm,
L. E. CODD
185
densely appressed villous above, densely matted-
villous below. Bracts leaf-like, becoming smaller
towards the apex. Verticils usually 2-flowered (but
up to 6-flowered according to FI. Cap.). Calyx
densely shaggy-villous.
Found in dense grassland in the eastern Cape
Province.
Cape. — 3029 (Kokstad): Mt. Currie (-AD), Tyson 1331. 3129
(Port St Johns): between Umzimvubu and Umsikaba Rivers
(-BD ?), Drege 4752 (K).
A little-known species closely related to S. natalensis
and which may be only an extreme form of that
species, distinguished by the densely matted-villous
lower surface of the leaves. Further material is
required in order to determine how meaningful this
distinction is.
A specimen from northern Natal, Grid 2730
(Vryheid): near Luneburg (-BC), Galpin 9870, has
this type of tomentum and 2-flowered verticils but
differs in having petioles up to 7 mm long. It is
tentatively included in S. sessilifolia until more
material is forthcoming in order to assess the
importance of subsessile versus petiolate leaves.
It may be noted that this character varies a good
deal in the material included in S. natalensis below.
The type of S. bachmannii has not been seen; the
species was included in S. sessilifolia by Skan and,
judging by its description, this decision appears to
be correct.
7. Stachys natalensis Hochst. in Flora 28:65
(1845). Type: Natal, Table Mt., Krauss 1139.
Stems variously pubescent from densely to sparingly
villous or shortly scabrid to softly pubescent. Leaves
subsessile or petiolate; blade ovate to ovate-deltoid,
variable in size, 1-4x0, 6-2,4 cm shortly and
sparingly appressed pubescent to densely strigose
above, less dense, more spreading and mainly on the
nerves below often with some glandular hairs but not
conspicuously glandular. Bracts differentiated towards
the apex. Verticils 2-flowered. Calyx densely villous
to densely and shortly pubescent, usually without
glands.
A widespread and variable species found in grass
on stony hillsides, in semi-shady kloofs and wooded
places in the mountains of northern central and
eastern Transvaal, Swaziland, northern and coastal
Natal as far south as Durban, with an occasional
record from the eastern Cape. Also recorded from
Rhodesia.
No material of the type, Krauss 1139 from Table
Mt., near Pietermaritzburg, has been traced, but the
description is considered adequate to identify it
with the present concept, though Skan, l.c., lists it
as an “imperfectly known species.” The specimen
Schlechter 2894 from near Verulam, Natal, may be
regarded as representative and, if no material of
the type can be found, would be a suitable specimen
to select as a lectotype.
Two varieties, based mainly on the degree of
pubescence, are recognized.
Key to varieties
Pubescence on stem, leaves and calyx sparingly villous
to shortly scabrid or tomentose (a) var. natalensis
Pubescence on stem, leaves and calyx densely
villous (b) var. galpinii
(a) var. natalensis.
Stachys natalensis Hochst. in Flora 65 (1845); Skan in FI.
Cap. 5,1: 367 (1910); Ross, FI. Natal 303 (1972). Type: Natal,
Table Mt., Krauss 1139. S. transvaalensis Guerke in Bot. Jahrb.
28: 316 (1901); Skan, l.c. 346 (1910). Type: Transvaal, Lyden-
burg District, Wilms 1136 (BM). S. leptoclacla Briq. in Bull
Herb. Boiss. ser. 2,3: 1084 (1903); Skan, l.c. 351 (1910); Ross
FI. Natal 303 (1972). Type: Natal, Bluekrantz River, Schlechter
6865 (Z, holo.! ;BOL! ). S. aethiopica sensu Letty, Wild Flow.
Transv. 284, t. 141: 3 (1962); sensu Compton, FI. Swaz. 66
(1966).
Stems shortly scabrid or tomentose to sparingly or
fairly densely villous. Leaves petiolate, blade hispid-
villous above, less so and mainly on the nerves below.
Calyx hispid-villous.
Distribution and ecology more or less as for the
species but not prevalent in the mountain grassland
of the eastern Transvaal. Also occurs in Rhodesia.
Transvaal. — 2329 (Pietersburg): Louis Trichardt (-BB),
Breyer sub TRY 20926; Spelonken (-BD), Junod 123. 2330
(Tzaneen): Tshakoma (-AB), Obermeyer sub TRY 31569. 2428
(Nylstroom): Geelhoutkop (-AD), Breyer sub TRY 18105;
Sterkrivierdam Nature Reserve (-BC), Jacobsen 2004; Moord-
drift (-BD), Leendertz sub TR Y 7330; N. of Warmbaths (-CD),
Repton 792; Sidey 1339; Smuts & Gillett 3089; Strey 3947;
Naboomfontein (-DA?), Galpin 13481. 2430 (Pilgrim’s Rest);
Ohrigstad Dam Nature Reserve (-DC), Jacobsen 1436; 1766;
2909. 2527 (Rustenburg): Scheerpoort (-DD), Leendertz sub
TRY 27126; farm Uitkomst 499 (-DD), Coetzee 654. 2528
(Pretoria): Wonderboom Reserve (-CA), Pole Evans 340;
C. A. Smith 104; 240; Koedoespoort (-CB), Leendertz sub TR Y
8570; Obermeyer sub TRY 27657; Botanic Garden (-CB),
Codd 855 ; 35 km E. of Pretoria (-CD), Repton 582; Trigaarts-
poort (-DB), Bruce 97 ; 18 km N.E. of Bronkhorstspruit (-DB),
Codd 2694. 2529 (Witbank): Bundu Inn (-AC), Mauve 4916;
Loskop Dam (-AD), Theron 1376. 2530 (Lydenburg); Crocodile
Valley (-AD), Burtt Davy 7662; Nelspruit (-BD), Liebenberg
2596; Cythna Letty Nature Reserve (-DD), Muller 2219. 2531
(Komatipoort): Barberton (-CC), Edwards 46.
Swaziland. — 2631 (Mbabane): Komati Bridge (-AA),
Compton 26835; 26931; near Mbabane (-AC), Hardy 27;
Hlatikula (-CD), Compton 26265 ; 30228.
Natal. — 2730 (Vryheid): Utrecht (CB), Wahl sub TRY 15536.
2732 (Ubombo): Pongola Poort (-AC), Repton 6020. Mpangazi
(-DA), Strey 5090; Mbazwane (-DA), Yahrmeijer 1133. 2829
(Harrismithj, 34 km N. of Ladysmith (-BB), Codd 8622; Blou-
krans River (-DD), Schlechter 6865 (Z). 2830 (Dundee): Tugela
Ferry (-CD), Galpin 14780; Kranskop (-DD), Galpin 14764.
2832 (Mtubatuba): Hluhluwe Game Reserve (-AA), Hirchins
366; 526; 643. 2929 (Underberg): Estcourt (-BB), West 1332;
Pentz 497. 2930 (Pietermaritzburg): near Durban (-DD),
Medley Wood 59; 6437. 2931 (Stanger): near Verulam (-CA),
Schlechter 2894; Moll 1990.
Cape. — 3228 (Butterworth): Kentani (-CB), Pegler 187.
In general the pubescence is sparingly to fairly
densely villous and grades somewhat into the very
densely villous pubescence of var. galpinii. In Natal
some specimens have hispid or shortly tomentose
pubescence, resembling the condition often found in
S. aethiopica, but may be separated from that species
by the 2-flowered verticils. The type of S. leptoclada
Briq., Schlechter 6865 (Z) from Bloukrans River near
Ladysmith is such a plant. Schlechter 6865 may be
a mixed gathering because the specimen in PRE
with this number is S. grandifolia E. Mey. ex Benth.
or, more likely, the material may have become mixed
when it was distributed. The type of S. transvaalensis
Guerke is more densely pubescent than typical var.
natalensis.
(b) var. galpinii (Briq.) Codd, stat. nov.
S. galpinii Briq. in Bull. Herb. Boiss. ser. 2,3: 1082 (1903);
Skan in FI. Cap. 5,1: 346 (1910); Compton, FI. Swaz. 66 (1966);
Ross, FI. Natal 303 (1972). Type: Transvaal, near Barberton,
Galpin 681 (K!, PRE!, SAM!). S.lupulina Briq., l.c. 1082 (1903).
Type: “Natal, near Claremont, Schlechter 4651” (Z, holo.!;
BOL!). 5. parilis N.E. Br. in Kew Bull. 1901 : 131 (1901); Skan,
l.c. 347 (1910); Ross. l.c. 303 (1972). Type: Natal, Drakensberg,
Tiger Cave Valley, Evans 387 (K, holo.; NH!). S. villosissima
H. M. Forbes in Bothalia 4: 38 (1941); Ross, l.c. 304 (1972).
Type: Natal, Entumeni, Forbes 783 (NH, holo.; PRE!).
Stems erect, branching from the base, 12-20 cm
tall or decumbent to straggling 30-40 cm long; stem
densely villous. Leaves subsessile or petiolate, densely
villous on both surfaces. Calyx densely villous.
186
A NOTE ON THE STACHYS AETHIOPICA COMPLEX
Found in dense grass, often among rocks at high
and medium altitudes in central and eastern Transvaal
and northern Swaziland, extending to northern Natal.
Transvaal. — 2428 (Nylstroom): Moorddrift (-BD), Leen-
dertz sub TRV 7330. 2528 (Pretoria): Wonderboompoort (-CA),
Mogg 15860; near Zoo (-CA), C. A. Smith 3272; Hennops River
(-CC), Repton 1115. 2529 (Witbank): Middelburg (-CD),
Young A 20. 2530 (Lydenburg): 27 km W. of Lydenburg (-AB),
Codd 8063; Dullstroom (-AC), Galpin 13051; near Belfast
(-CA), Leendertz sub TRV 9178; Leistner 510; Machadodorp
(-CB), Galpin 13109; 18 km S.E. of Sewefontein (-CD), Codd
8114. 2531 (Komatipoort): near Barberton (-CC), Galpin 681;
Thorncroft sub TRV 4337; Mauve 4424. 2630 (Carolina): near
Carolina (-AA), Bolus 12241.
Swaziland. — 2531 (Komatipoort): near Havelock Mine
(-CC), Miller 3033. 2631 (Mbabane): near Mbabane (-AC),
Codd 9511; Compton 24559; 25270; 25379; 26707; 26754.
Natal. — 2731 (Louwsburg): Pongola Experimental Farm
(-BC), Nel 199. 2829 (Harrismith): Willowford Station (-DD),
Acocks 10599. 2831 (Nkandla): 6 km S. of Mtonjaneni (-AD),
Codd 1808; near Melmoth (-CB), Mogg 4549 ; 6163; Entumeni
(-CD), Forbes 783. 2832 (Mtubatuba): Dukuduku (-AD),
Strey 5511; Richard’s Bay (-CC), Venter 4975.
This variety can be recognized by the combination
of densely villous pubescence and 2-flowered verticils;
it grades into var. natalensis and many specimens
may be regarded as transitional between the two.
In var. galpirtii the leaves may be petiolate or sub-
sessile and the latter specimens come near to S.
sessilifolia, in which the lower surfaces of the leaves
are densely matted-villous and the stems are softly
tomentose. In S. malacophylla the lower surfaces of
the leaves are also densely pubescent, but the verticils
are usually 6-flowered. The types of S. lupulina Briq.,
S. parilis N.E. Br. and S. villosissima H. M. Forbes
are not appreciably distinct from that of S. galpinii.
Skan, l.c., draws attention to the confusion
concerning the type of S. lupulina. Briquet cites the
specimen as “Natal, Claremontplats prope Claremont,
Schlechter 4651, ann. 1892.” On the type sheet in Z
and an isotype in BOL the label reads: “Claremont
flats prope Cape Town, Schlechter 465, 9. III.
1892”. It is undoubtedly conspecific with S. natalensis
var. galpinii, which does not occur in the Cape, but
could have been collected in northern Natal or the
eastern Transvaal. Skan concluded that it had
probably been introduced at the Cape but there is
no evidence to support this.
8. Stachys aethiopica L., Mant. 1: 82 (1767);
Burm. f., FI. Cap. Prodr. 16 (1768); Ait., Hort. Kew.
2: 302 (1879); Willd., Sp. PI. 3: 102 (1800); Thunb.,
FI. Cap. ed. Schult. 447 (1823); Benth., Lab. 548
(1834); in E. Mey., Comm. 239 (1837); in DC.,
Prodr. 12: 476 (1848); Bol. & Wolley-Dod in Trans.
S. Afr. Phil. Soc. 14: 310 (1904): Skan in FI. Cap.
5,1: 348 (1910); Marloth, FI. S. Afr. 3,2: 180, t.
47B (1932); Salter in FI. Cape Penins. 697 (1950);
Jacot-Guill., FI. Lesotho 237 (1971); Ross, FI.
Natal 303 (1972). Type: Cape Province, LINN 736.
13 (lecto.).
Betonica capensis Burm. f., FI. Cap. Prodr. 16 (1768). Type.
Pluk., Almagest. Bot. t. 315, f. 3 (1696).
S. aethiopica var. grandiflora Burch, ex Benth. in E. Mey.,
Comm. 239 (1837). Type: Cape, Klein Winterhoek, Drege 75d
(K, holo.). — var. hispidissima Benth., l.c. 239 (1837); Skan in
FI. Cap. 5,1 : 348 (1910). Type: Cape, Hex River Kloof, Drege
75h (K, holo.). — var. gtandulifera Skan, l.c. 348 (1910); Phill. in
Ann. S.A. Mus. 16:244 (1917); Jacot-Guill., FI. Lesotho 237
(1971). Syntypes: several, inch Zwartkei River, Baur s.n. (K;
PRE!). — var. parviflora Skan, l.c. 348 (1910); Salter in FI. Cape
Penins. 697 (1950). Syntypes: several, inch Cape Peninsula,
Signal Station, Wolley-Dod 3048 (K; BOL!). S. pulchella
Salisb., Prodr. 83 (1796), nom. illegit. Type: based on S.
aethiopica L. S. serru/ata Burch, ex Benth., Lab. 549 (1834);
in DC., Prodr. 12: 477 (1848); Skan, he. 350 (1910). Type:
Cape, near Knysna, Burchell 5155 (K, holo.!). S. capensis
Presl, Bot. Bemerk. 100 (1844); Skan, l.c. 366 (1910). Type:
Cape, without locality, Krebs 273. S. hispidula Hochst. in Flora
66 (1845); Skan, l.c. 367 (1910). Type: Cape, Humansdorp
District, Krauss 1125. 5. fruticetorum Briq. in Bull. Herb Boiss
ser. 2,3: 1083 (1903); Skan, l.c. 351 (1910). Type: Cape Sir
Lowry’s Pass, Schlechter 1179 (Z, holo.!; BOL!). S', harveyi
Skan, l.c. 350 (1910). Type: Cape, near Cape Town, Harvey
s.n. (TCD, holo.). S. attenuata Skan, l.c. 351 (1910). Syntypes:
Cape, near Bainskloof, Bolus 2896 (K, BOL!), Paarl Mt.
Drege 75b (K).
Stems decumbent or ascending, up to 50 cm long
or more, rather slender, sparingly to freely branched,
variously pubescent with short antrorse hairs, short
or long retrorse hairs often mixed with longish
spreading hairs or glandular hairs, or (especially the
rhachis) densely glandular-tomentulose. Leaves
petiolate; blade broadly ovate to ovate-deltoid,
usually about 0,8-3, 5x0, 6-2, 5 cm, but up to
6x4 cm (Natal coastal form), upper surface usually
shortly hispid to pilose, lower surface hispid to
pilose, mainly on the nerves, often with some glands,
to densely glandular-puberulous, rarely almost
glabrous. Inflorescence usually tapering, of many
whorls, occasionally with few whorls and subcapitate.
Bracts differentiated from the leaves towards the
apex. Verticils usually 4-6-flowered occasionally
2-3-flowered (mainly depauperate specimens). Calyx
sparingly to densely hispid and often glandular.
Distributed from Clanwilliam District to the
Peninsula and along the coast to the eastern Cape
Province and to Natal, Lesotho and the Orange Free
State; found in a variety of habitats from fynbos to
dry woodland and coastal dune bush, extending to
mountain grassland where it is usually found among
sandstone rocks.
O.F.S. — 2827 (Senekal): near Senekal (-BC), Goossens 918;
near Ficksburg (-DD), Potts 3184; Galpin 13831. 2828 (Beth-
lehem): near Bethlehem (-AB), Flanagan 2114; Phillips s.n.;
Scheepers 1412; Werger 244; Slabberts (-AC), Stam 179;
Fouriesburg (-CA), Potts 3265; Clarens (CB), Van Hoepen sub
TRV 18163. 2926 (Bloemfontein): Thaba Nchu (-BB), Roberts
2246.
Natal. — 2830 (Dundee): 14 km S.W. of Nqutu (-BA), Codd
2400; Kranskop (-DD), Strey 4288 (NH). 2831 (Nkandla):
Babanango (-AC), King 255; Melmoth (-CB), Mogg 6167.
2929 (Underberg): Tabamhlope Pasture Research Station (-BA),
West 550; near Sani Pass (-CB), Marias 1434. 2930 (Pieter-
maritzburg) : Tweedie (-AC), Mogg 6764; Dargle (-CA), Hilliard
and Burtt 3194; Pietermaritzburg (-CB), Goossens 131; Mogg
2235; Byrne (-CC), Galpin 11929; Durban (-DD), Strey 4347;
11318; Isipingo (-DD), Ward 3775. 2931 (Stanger): Mt. Edge-
combe (-CA), Medley Wood 1126. 3030 (Port Shepstone):
Dumisa (-AD), Huntley 166 (NH); Port Shepstone (-CB),
Dimock-Brown 475 (NH).
Lesotho. — 2828 (Bethlehem): Leribe (-CC), Dieterlen 101;
Maluti Mts. (-DD), Staples 85. 2927 (Maseru): Teyateyaneng
(-BA), Collett 477; Mamathes (-BB), Jacot-Guillarmod 866;
869; Tebetebeng River, Jacot-Guillarmod 359; Roma (-BC),
Ruch 1689; Mafeteng (-CC), Gerstner 226. 2929 (Underberg):
Sehlabathebe (-CC), Jacot-Guillarmod, Getliffe and Mzamane
154.
Cape. — 3027 (Lady Grey): Barkly East (-DC), Gerstner 206.
3028 (Matatiele): 6 km E. of Kenegha (-BC), Story 524. 3029
(Kokstad); 19 km N. of Swartberg(-AB), Codd 8533; near Kok-
stad (-CB), Coleman 467; Bizana (-DD), Acocks 12225. 3127
(Lady Frere): Cala (-DA), Pegler 1646. 3129 (Port St. Johns):
Port St. Johns (-DA), Howlett 10. 3219 (Wuppertal): Cedarberg
(-AC), Galpin 10546; Citrusdal (-CA), Hanekom 1164. 3224
(Graaff Reinet): Graaff Reinet (-BC), Sister Francis 37. 3225
(Somerset East): National Mountain Zebra Park (-AB),
Liebenberg 6431 ; Boschberg (-DA), MacOwan 559 partly. 3226
(Fort Beaufort); Mungo Mt. (-CB), Galpin 11550; 16 km N. of
Fort Beaufort (-DC), Story 2224; Garfield (-DD), Acocks
23513. 3227 (Stutterheim) : Windvoelberg (-AC), Roberts 1798;
near Happy Valley (-AD), Johnson 1298 ; Kabaku Hills (-CB?),
Acocks 9271; King William’s Town (-CD), Sim 19593; near
Komga (-DB), Flanagan 414. 3228 (Butterworth): near Mazeppa
Bay (-BC), Hilner 422; Kentani (-CB), Pegler 231. 3318
(Cape Town): near Hopefield (-AB), Lettybl; Darling (-AD),
Bolus sub TR V4657; Cape Town (-CD), Young sub TR V 26635;
Mrs. Southey sub Galpin 7849; Lions Head (-CD), Ecklon
s.n.- Marloth 65; Camps Bay (-CD), Thode A143; Sea Point
(-CD), C. A. Smith 2889; Paarl Mt. (-DB), Kruger M 118;
near Stellenbosch (-DB), Parker 3895; Bos 135; Kerfoot 6081.
3319 (Worcester): near Gouda (-AC), Esterhuysen 18787;
L. E. CODD
187
Prospect Peak (-BC), Esterhuysen 15902 ; Gydouw (-AD),
Leipoldt s.n.; Veld Reserve (-CB), Olivier 35; French Hoek Pass
(-CC), Boucher 2343; near McGregor (-DD), Van Breda &
Joubert 1973. 3322 (Oudtshoorn) : between Wilderness & Knysna
(-DC), Wells 3723. 3323 (Willowmore): near Joubertina (-DD),
Van Breda 1168. 3325 (Port Elizabeth): near Kenkelbosch
(-DB), Archibald 5995; Paterson 55; Port Elizabeth (-DC),
Borle 15. 3326 (Grahamstown): Alicedale (-AC) Rogers 12016;
Port Alfred (-DB), Tyson s.n.; Rogers 16654; ' Kowie (-DB),
Britten 810. 3327 (Peddie): East London (-BB), Galpin 1879.
3418 (Simonstown) : Hout Bay Nek (-AB), Hutchinson 103;
Muizenberg (-AB), Pillans 3678. 3419 (Caledon): Enon (-AB),
Thode A2741. 3420 (Bredasdorp): National Bontebok Park
(-AB), Liebenberg 6431 ; Kompanjies River (-AB), Marsh 581 ;
De Hoop (-AD), Van der Merwe 1158; Fort Beaufort (-BD),
Marsh 820; Nachtwacht (-CA), C. A. Smith 3053. 3423
(Knysna): Keurboomstrand (-AB), Codd3565.
Skan attempted to reduce the confusion which
existed in this complex by isolating certain discordant
elements as separate species, and by upholding four
varieties within 5. aethiopica. With the advent of a
good deal of modern material, the position is still
confused, but it appears that a broader concept of
the species should be adopted, while the separation of
varieties within S. aethiopica seems scarcely justified.
Several of the peripheral species upheld by Skan are
still maintained, such as S. rudatisii, S. gracilifiora
(-S. cooperi), S. scabrida ( = S. priorii ), S. flexuosa,
S. cymbalaria and S. sublobata, and the distinguishing
characters are discussed under the respective headings.
Others, such as S. harveyi, S. serrulata, S. attenuata
and S. fruticetorum are now included in S. aethiopica.
Regarding the typification of S. aethiopica, Linnaeus
refers to Pluk., Aim. 245, t. 315, f. 3, while the
description indicates that he had a specimen before
him. Of these two elements, the specimen in the
Linnaean Herbarium No. 736.13 may be regarded
as the type and is a plant with retrorse to spreading
pubescence and lacking glandular hairs. In both
elements the plant referred to has 2-flowered verticils,
but this must be regarded as exceptional as most
specimens which match the type have 2-6-flowered
verticils. The typical form occurs mainly in the
south-western Cape Province, but it grades into the
varieties upheld by Skan.
Bentham based his var. hispidissima on a Drege
gathering with denser and more stiffly spreading
hairs on stems and leaves, but this is scarcely distinct
from the typical form. The other two varieties,
described by Skan, are possibly more distinct but,
due to the many intermediates, it is preferred to
regard them as forms rather than give them taxonomic
rank.
In the plants placed by Skan in var. parviflora, the
hairs on the stem are antrorse and shortly scabrid,
the petioles tend to be shorter and the flowers smaller.
Salter in FI. Cape Penins. 697 (1950) upheld this
variety but, as one moves away from the Peninsula,
the distinction becomes less clear.
The form separated as var. glandulifera is usually
recognizable under magnification by the glandular-
puberulous pubescence on most parts of the plants,
especially the under-surface of the leaf, the rhachis
and the calyx. It appears to be the prevalent form
in the eastern, summer-rainfall part of South Africa,
especially along the Drakensberg escarpment.
Towards the west it grades into typical 5. aethiopica
and the type of S. fruticetorum, Schlechter 1179 from
Sir Lowry’s Pass, is an intermediate specimen.
Another form has been observed along the coast
of Natal in which the leaves are much larger than
usual, up to 6x4 cm. It appears to be a semi-weed
in disturbed areas, and serious consideration was
given to according it separate status of some sort.
However, there is a gradation in leaf size and many
intermediate specimens cannot be allocated with
certainty. At present it is regarded as a form growing
under favourable subtropical conditions. The
pubescence is somewhat similar to the plants discussed
under var. glandulifera.
To summarize, the pubescence in S. aethiopica is
mainly hispid, either antrorse, retrorse or spreading,
sometimes with scattered longish hairs and often
finely glandular, especially on the calyx and under-
surface of the leaves. This can usually be distinguished
from the villous pubescence of S. natalensis but there
should be no confusion between the two because,
in the eastern summer-rainfall areas, S. aethiopica
always has 4-6-flowered verticils, while S. natalensis
is strictly 2-flowered. The two overlap in Natal and
the extreme eastern Cape Province. S. aethiopica is
absent from the Transvaal and rare in Swaziland,
but a very glandular form occurs in Lesotho and
the eastern Orange Free State.
As it often happens in variable species, S. aethiopica
tends to be a repository for specimens which cannot
satisfactorily be placed elsewhere. For example, a
few specimens of rather distinct facies, with stiff
stems and very densely glandular-puberulous stems,
leaves and calyces, but with 2-flowered verticils,
have been collected in the eastern Cape Province,
namely: Stutterheim District, Acocks 2971 and Sim
s.n.; Port St. Johns District, Flanagan 2595. If
S. aethiopica were divided into formal varieties, these
specimens would probably be worthy of varietal
rank.
S. aethiopica normally has a slender tapering
inflorescence of several to many verticils. On the
other hand some specimens in the southern Cape
Province have few verticils with an almost subcapitate
inflorescence, resembling the condition found in
S. gracilifiora ( =S . cooperi ) and to some extent in
S', scabrida. The plants previously included in S.
cooperi usually have larger leaves, while those
described as S. scabrida have subglabrous to sparingly
retrorse-scabrid stems and subglabrous leaves. The
type of S. gracilifiora is somewhat intermediate but
it seems possible to maintain all three species, though
occasional specimens, especially from the Knysna-
Tsitsikama area, may be difficult to place with
certainty (see next species).
9. Stachys gracilifiora Presl, Bot. Bemerk. 100
(1844); Benth. in DC., Prodr. 12: 496 (1848); Skan
in FI. Cap. 5,1: 366 (1910) Type: Cape, without
locality, Krebs s.n. (PRC, holo.!, as to left-hand
specimen on sheet labelled S. gracilifiora Presl; PRE,
photo.).
5. cooperi Skan in Kew Bull. 1909: 420 (1909); FI. Cap. 5,1:
343 (1910); Ross, FI. Natal 303 (1972). Syntypes: Cape, Albany
Division, Cooper 15(K1); Kentani, Pegler 908, collected April
1909 (Kl, PRE!).
Stem shortly and often sparingly retrorse-
pubescent. Leaves petiolate, blade ovate to broadly
ovate, often thin-textured, 2-6, 5 x 1,4-5 cm,
eglandular, sparingly hispidulous or shortly and
sparingly pilose, the hairs on the upper leaf surface
soft and not bulbous-based. Inflorescence of 1-4
(rarely more) verticils, somewhat lax below or often
subcapitate, verticils 4-6-flowered; bracts differen-
tiated towards the apex. Calyx sparingly or softly
hispid, eglandular.
A soft straggling herb of moist places in forest
margins, in grass, fynbos or coastal scrub from
southern Natal to Knysna in the Cape.
188
A NOTE ON THE STACHYS AETHIOPICA COMPLEX
Natal. — 3030 (Port Shepstone): Horseshoe Farm (-CC),
Strev 6 169.
Cape. — 3129 (Port St. Johns): Umgazi River Mouth (-CB),
Wells 3494. 3226 (Fort Beaufort): Katberg (-BC), Galpin 2069 .
3227 (Stutterheim): Pirie Forest (-CC), Sim A; Acocks 9284;
near Komga (-DB), Flanagan 1752. 3228 (Butterworth) :
Kentani (-CB), Pegler 908. 3322 (Oudtshoorn): Wilderness
(-DC), Van Niekerk 236. 3325 (Port Elizabeth): Addo National
Park (-BC), Brvnard 363. 3423 (Knysna): Knysna: (-AA), Keet
635; Keurboomstrand (-AB), Fourcade 6119; Taylor 4914;
Storms River Mouth (-BB), Liebenberg 7765. 3424 (Humans-
dorp): Humansdorp (-BB), Galpin 4427.
There is a gradation in leaf size from the specimens
with larger and softer leaves, described as S. cooperi
Skan, to those occurring further west with smaller
and firmer leaves, which match the type of S. gracili-
flora Presl. The stem pubescence of the latter tends to
be slightly more scabrid and thus approaches the
condition found in S. scabrida Skan (see below).
However in S. scabrida the leaves are somewhat
thicker in texture, dry dark brown and the hairs on
the upper leaf surface are thicker with distinctly
swollen bases. On these grounds S. scabrida is kept
distinct, but the two overlap from southern Transkei
to Knysna and further study in this area is required.
As mentioned under the previous species, S.
aethiopica sometimes has few, fairly condensed
verticils which resemble those of S. graciliflora.
However, these plants usually have a coarser
pubescence on the stems, while gland-dots are often
present on the calyx and on the lower surface of the
leaves. No glandular hairs are found in S. graciliflora.
Specimens with large leaves resemble S. tubulosa
MacOwan, a species not included in the present
treatment, but may be separated, when flowers are
available, by the shorter corolla tube which does
not exceed 10 mm in length. In S. tubulosa the corolla
tube is 12-18 mm long and the species has a more
northerly distribution from East Griqualand to
Swaziland.
10. Stachys scabrida Skan in FI. Cap. 5,1: 349
(1910). Lectotype: Cape, Bruintjieshoogte, Burchell
3037 (K, lecto.!; PRE!).
S. priori i Skan, l.c. 353 (1910). Type: Cape, Algoa Bay,
Prior s.n. (K, holo. !).
Stems subglabrous to scabrid with few strong
retrorse-scabrid hairs to longer scattered multi-
cellular retrorse hairs. Leaves petiolate, firm-textured
and usually drying dark brown, ovate to ovate-
deltoid, 1, 2-3x0, 8-2 cm, subglabrous to sparingly
hispid, the upper surface with scattered short to
longish bulbous-based hairs. Inflorescence fairly
slender, of few verticils, spaced below; bracts
differentiated towards the apex. Calyx sparingly
hispid, eglandular.
A straggling herb in grass, fynbos or coastal scrub,
extending from the southern Transkei to Knysna and,
inland, to Steynsburg and Somerset East Districts.
Cape. — 3125 (Steynsburg): Suurberg (-BD), Schonland 3177.
3225 (Somerset East): Bruintjieshoogte (-CB), Burchell 3037.
3227 (Stutterheim): Hanover (-CD), Sim s.n. 3228 (Butter-
worth): “Gekau” River (-BC?), Drege s.n. ( K ). 3324 (Steytler-
ville): Assegaibosch (-CD), Breyer sub TRV 23323; 20 km W.
of Cambria (-DA), Story 2445. 3325 (Port Elizabeth): Van
Stadens Mts. (-CC), Zeyher 831 (K); Perseverance (-DC),
Long 816. 3326 (Grahamstown): Coldspring (-AD), Gane sub
TRV 25270; near Grahamstown (-BC), MacOwan 559, partly.
3423 (Knysna): (-AA), Breyer. sub TRV 23365.
S. scabrida appears to be related to S. graciliflora,
but the pubescence is coarser and more scabrid,
while the leaves are thicker-textured and the hairs
on the upper leaf surface tend to be bulbous-based.
The inflorescences tend to be more slender, rather
than subcapitate, as in S. graciliflora. The distinction
is by no means clear-cut, as indicated in the discussion
of the latter species, and specimens such as Story
2445 tend to be somewhat intermediate.
11. Stachys cymbalaria Briq. in Bull. Herb.
Boiss. ser. 2,3: 1088 (1903); Skan in FI. Cap 5,1 : 352
(1910); Ross, FI. Natal 303 (1972). Type: Cape,
Cradock, Cooper 416 (K, holo.!; W!).
S. aethiopica L. var. tenella Kuntze, Rev. Gen 3,2: 262 (1898).
Type: Cape, Cradock, Kuntze s.n. S. cymbalaria var. alba
Skan, l.c. 352 (1910). Type: Natal, Richmond, Medley Wood
1846 (K, holo.; NH!).
Stems slender, wiry, subglabrous or with a few
long slender spreading hairs or occasionally shortly
glandular-pubescent. Leaves petiolate, blade small,
broadly ovate-deltoid to suborbicular, 8-15x6-12
mm, subglabrous to thinly appressed-pubescent or
glandular-puberulous. Inflorescence lax of 1-5 verticils;
verticils 2-flowered; bracts differentiated, the upper
shorter than the calyx. Calyx puberulous to
hispidulous.
Found among rocks in exposed mountain grassland,
at altitudes of 1 000-1 800 m; recorded from a few
disjunct localities in southern Natal and the eastern
Cape Province.
Natal. — 2930 (Pietermaritzburg): Zwartkop (-CB), Medley
Wood 11120; Richmond (-CD), Medley Wood 1846 (NH).
3029 (Kokstad): Ngeli area (-DA), Hilliard & Burtt 5834 (NU);
7554 (NU); Strey 6337 (NH).
Cape. — 3039 (Kokstad): Mt. Insizwa (-CB), Schlechter 6467;
Hilliard & Burtt 6568. 3224 (GraafF Reinet): Reitvlei (-AB),
Galpin 10011; Lootsberg Pass (-BD), Acocks 13546. 3225
(Somerset East): Mountain Zebra National Park (-ADJ,
Brynard 295; Liebenberg 7107.
The species is closely related to S. aethiopica but is
characterized by the many wiry stems radiating from
the apex of a slender taproot, the small ovate to
roundish leaves and the 2-flowered verticils.
12. Stachys sublobata Skan in FI. Cap. 5,1: 354
(1910). Lectotype: Cape, Swellendam District, Barry-
dale, Galpin 4425 (K, lecto.; PRE!).
Stems slender, sparsely hispidulous, occasionally
with some longish spreading hairs. Leaves petiolate,
blade small, narrowly triangular, 10-15x4-6 mm,
thickish in texture, sparingly hispidulous on both sur-
faces, sometimes with gland-dots below, margin deep-
ly crenate or almost lobed with 3-5 lobe-like teeth.
Inflorescence lax of 2-5 verticils; verticils 2-(or
rarely 6-) flowered; bracts leaf-like below, differen-
tiated towards the apex. Calyx thinly glandular-
hispid.
Found on hillsides in fynbos at altitudes of 300-
900 m in the south-western Cape Province; known
from a few localities between Caledon and Mossel
Bay and, inland, to Ladismith and Oudtshoorn
Districts.
Cape. — 3320 (Montagu): Barrydale (-DC), Galpin 4425. 3321
(Ladismith): Rooiberg Pass (-DA), Acocks 20779. 3322
(Oudtshoorn): Cango Caves (-AC), Bolus 12244. 3419 (Cale-
don): 10 km W. of Rietpoel Station (-BD), Acocks 22582.
3421 (Riversdale): Klein Berg (-BB), Galpin 4426, partly.
This species resembles S. cymbalaria and, like that
species, is closely related to S. aethiopica, but can be
recognized by the narrowly triangular leaves, rather
thickish in texture and with deeply crenate, almost
lobed margins. It normally has 2-flowered verticils,
but one portion of Galpin 4426 in PRE, which
matches S. sublobata, has 6-flowered verticils. The
other specimen mounted on the same sheet has
larger leaves and is S. aethiopica.
L. E. CODD
189
13. Stachys flexuosa Skan in FI. Cap. 5,1: 352
(1910). Type: Cape, Stockenstroom District, old
Katberg Pass, Galpin 2393 (wrongly listed in FI.
Cap. as 2093) (K, holo.; PRE!, SAM!).
Stems fairly densely villous-pilose with long
spreading hairs and some short glandular hairs.
Leaves petiolate, blade ovate, 1-2x0, 6-1, 5 cm,
somewhat appressed-villous with some bulbous-based
hairs above, hispid mainly on the nerves below, base
not deeply cordate. Inflorescence fairly dense, of few
to several 2-6-flowered verticils; bracts leaf-like
below, becoming smaller towards the apex. Calyx
hispid, often with some glands.
Known from a few localities in the eastern Cape
Province, among rocks in mountain grassland.
Cape. — 3126 (Queenstown): near Hopewell (-DC?), Galpin
8379. 3129 (Port St. Johns): Port St. Johns District (CB?),
Swinny & Baker sub TRV 14143. 3226 (Fort Beaufort): old
Katberg Pass (-BC), Galpin 2393 ; Hogsback (-DB), Rattray 403.
The species is included here because the small
ovate leaves with a rather wide sinus at the base are
reminiscent of the S. aethiopica complex, but the
relationship appears to be with another complex
which includes S. obtusifolia and S. tysonii. From
these it differs mainly in the smaller leaves, and
less densely villous stems and leaves, in contrast to the
markedly glandular pubescence of S. tysonii. As in
many other species of Stachys, a good deal more
material is required before the status of S. flexuosa
can be reliably determined.
UITTREKSEL
Die Stachys aelhiopica-kompleks word ondersoek
en 'n sleutel voorsien tot die soorte wat erken word.
Die kombinasie S. natalensis Hochst. var. galpinii
( Briq .) Codd word gemaak en twee nuwe soorte, S.
reticulata Codd en S. arachnoidea Codd word beskrvf.
Bothalia 12,2: 191-194 (1977)
New taxa and a new combination in the genus Cotyledon
H. R. TOLKEN*
ABSTRACT
Five new species and one variety are described and the combination Cotyledon tomentosa Harv. subsp.
ladismithiensis (V. Poelln.) Toelken is effected. The following new names are published; C. sulphurea Toelken,
C. oceultans Toelken, C. similis Toelken, C. viridiflorum Toelken, C. hallii Toelken and C. pygmaea Barker
var. tenuis Toelken.
RESUME
NOUVEA U TAXA ET NOUVELLE COMBINAISON DANS LE GENRE COTYLEDON
On decrit cinq especes et une variete nouvelles. La combinaison Cotyledon tomentosa Harv.
subsp. ladismithiensis ( V. Poelln.) Toelken est operee. Les nouveaux noms publies sont: C. sulphurea
Toelken, C. oceultans Toelken, C. similis Toelken, C. viridiflorum Toelken, C. hallii Toelken et
C. pygmaea Barker var. tenuis Toelken.
Recent collecting has added more information to
the knowledge of some rare species of Cotyledon
from the north-western Cape Province, so that these
can now be described. This has also allowed a
re-evaluation of the delimitation of other species,
which were previously differently interpreted.
1. Cotyledon sulphurea Toelken, sp. nov. a
C. occultante foliis glabris, florescentia praecociore
et ovulis ovatis differt.
Herbae perennes tuberibus subterraneis ramosis
usque ad 10 cm longis, ramis succulentis laevibus
pauciramosis et rare 2 cm longioribus. Folia alterna,
oblanceolata vel spathulata, 0,5-2, 5 cm longa, 0,2-
0,5 cm lata, cuneata, plerunrque obtusa, dorsoven-
traliter, complanata, leviter sulcata supra et convexa
subtus, glabra sed cellulis pustuliformibus, succulenta,
viridia. Inflorescentia thyrsus corymbiformis 1-4
dichasiis patentibus, pedunculo rigido 1-3 (-5) cm
longo et tecto pilis glandulosis, pedicello 0,4-0, 8 cm
longo et tecto pilis glandulosis, bracteis lanceolatis
deciduis. Sepala triangulari-lanceolata, 0,35-0,45 cm
longa, acuta, tecta sparsim pilis glandulosis patentibus,
succulenta, flavo-virentia. Peta/a oblonga, 1,3-1, 5
cm longa, acuta, connata in tubo 0,8-1 cm longo,
tecta plus minusve etiam pilis glandulosis patentibus
extus et pilis aliquot tenuis intus praecipue tubi
petalorum in partibus inferis, sulphurea. Stamina
1-1,2 cm longa et aequilonga, antheris 0,1-0,12 cm
longis et filamentis rectis pilis patentibus praecipue
in partibus quibus connatis petalorum tubo. Squamae
oblongae 0 , 1-0, 1 3 x 0,02-0,04 cm, plus minusve emar-
ginatae, leviter succulentae, flavae. Carpella ovariis
gracilibus gradate constricta ad stylos erectos et
stigmatibus terminalibus; ovarium 10-14 ovulis ovatis
sine porcis verticalibus.
Type: Cape: near Pofadder, Tolken 3676A (BOL,
holo. !).
Perennial with branched underground tubers up to
10 cm long, with fleshy glabrous stems little branched
and rarely longer then 2 cm. Leaves alternate,
oblanceolate to spathulate, 0,5-2, 5 cm long, 0,2-
0,5 cm broad, cuneate, usually obtuse, dorsiventrally
compressed and slightly grooved above and convex
below, succulent, glabrous but with some large
bulging epidermal cells, green. Inflorescence a flat-
topped thyrse with one to several spreading mono-
chasia, with wiry peduncle 1-3 (-5) cm long and
covered with glandular hairs, with pedicels 0,4-
* Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag XI 01, Pretoria
0,8 cm long and covered with glandular hairs, with
lanceolate bracts deciduous. Sepals triangular-lanceo-
late, 0,35-0,45 cm long, acute, sparsely covered with
glandular hairs, succulent, yellowish-green. Petals
oblong 1,3-1, 5 cm long, acute, fused into a tube
0,8-1 cm long, more or less evenly covered with
spreading glandular hairs on the outside and with
few fine hairs on the inside mainly where the filaments
are fused to the petal-tube, sulphur-yellow. Stamens
1-1,3 cm long and all of equal length, with anthers
0,1-0,12 cm long, with straight filaments, with
scattered hairs mainly where fused to the petal-tube.
Squama oblong 0,1-0,13x0,02-0,04 cm, more or
less emarginate, slightly succulent, yellow. Carpels
with slender ovaries gradually constricted into erect
styles with terminal stigmas; ovary with 24-40 ovate
ovules without distinct vertical ridges.
This species is usually found on quartzite gravel
on the lower slopes of hills and has been recorded
only from the vicinity of Pofadder, but here it is
locally common. It flowers during November and
December, a distinguishing feature between this
species and C. oceultans.
Cape. — 2919 (Pofadder): 4 km N.E. of Pofadder (-AB),
Horn 1011 (NBG); Horn sub NBG 873/61 (NBG); near Pofadder
(-AB), Tolken 3676 A (BOL); Wisura 1961 (NBG); 1 1 km S.E. of
Pofadder (-AB), Tolken 3679A (BOL).
2. Cotyledon oceultans Toelken, sp. nov. a C.
sulphurea foliis paene orbicularibus quibus tectis pilis
glandulosis et florescentia serotinioribus ; a C. pygmaea
ramo brevissimo et trichotomatibus unicellularibus.
Herbae perennes tuberibus subterraneis paucira-
mosis usque ad 6 cm longae, ramis laevibus paucira-
mosis et usque ad 1 cm longis. Folia alterna, spathulata
vel orbicularia, 0,4— 1,2 cm longa, 0,3-1, 4 cm lata,
cuneata vel paene petiolata, obtusa, dorsiventraliter
complanata et leviter sulcata supra, tecta dense tri-
chotomatibus erectis obtusis, succulenta, atrovirentia.
Inflorescentia thyrsus 1 (-3) monochasiis 1-3 floribus,
pedunculo rigido 0,8-1, 5 cm longo et tecto pilis
glandulosis, pedicello 0,5-1, 3 cm longo et tecto
pilis glandulosis, bracteis lanceolatis caducis. Sepala
triangulari-lanceolata, 0,2-0, 3 cm longa, acuta, tecta
pilis glandulosis, succulenta, viridia. Petala oblonga,
1-1,2 cm longa, acuta, connata in tubo 0,6-0, 8 cm
longo, plus minusve etiam tecta pilis glandulosis
extus et pilis aliquot tenuibus intus praecipue in
partibus inferis tubi petalorum. Stamina 1,1-1, 4 cm
longa et aequilonga, antheris 0,1-0,12 cm longis,
filamentis rectis pilis tenuibus sparsis praecipue in
partibus quibus connatis petalorum tubo. Squamae
oblongae, 0,11-0,13x0,02-0,04 cm, plerumque plus
192
NEW TAX A AND A NEW COMBINATION IN THE GENUS COTYLEDON
minusve emarginatae, succulentae, flavae. Carpella
ovariis gracilibus gradate constrictis ad stylos erectos
stigmatibus terminalibus; ovarium 10-14 ovulis
ovatis sed lateriobus ad lateres et porcis verticalibus.
Type: Cape, near Bitterfontein, H. Hall 4289
(PRE, holo. !; NBG).
Perennial with little branched underground tubers
up to 6 cm long, with short glabrous stems little
branched and up to 1 cm long. Leaves alternate,
spathulate or orbicular, 0,4-1 ,2 cm long, 0,3-1 ,4 cm
broad, cuneate or almost petiolate, obtuse, dorsi-
ventrally compressed and slightly grooved above,
densely covered with blunt erect trichomes, deep
green. Inflorescence a thyrse with 1 (-3) monochasia,
each with 1-3 flowers, with wiry peduncle 0,8-1 ,5 cm
long and covered with glandular hairs, with pedicels
0,5-1, 3 cm long and covered with glandular hairs,
with lanceolate deciduous bracts. Sepals triangular-
lanceolate, 0,2-0, 3 cm long, acute, covered with
glandular hairs, succulent, green. Petals oblong,
1-1,2 cm long, acute, fused into a tube 0,6-0, 8 cm
long and more or less evenly covered with spreading
glandular hairs on the outside and with a few fine
hairs on the inside mainly where the filaments are
fused to the petal tube, pale yellow or yellowish-
green. Stamens 1,1-1, 4 cm long and about equally
long, with anthers 0,1-0,12 cm long, with straight
filaments with fine hairs mainly where fused to the
petal tube. Squamae oblong, 0,11-0,13x0,02-0,04
cm, usually more or less emarginate, fleshy, yellow.
Carpels with slender ovaries gradually constricted
into erect styles with terminal stigmas; ovary with
8-20 ovules almost dumbell-shaped and with distinct
vertical ridges.
So far this small Cotyledon has been recorded
from quartzite gravel near Bitterfontein and Steinkopf,
but the fact that these two localities are so far away
from each other suggests that the species is probably
widely distributed over the little known eastern
foothills of the Kamiesberg. Mr H. Hall, the very
observant collector, was the first to draw attention
to this small plant. In addition, the species flowers
in February and March, the driest period in the
Namaqualand, so that it is rarely seen in flower.
Cape. — 2917 (Springbok): 11 km S. of Steinkopf (-BD),
Tolken 4272 (BOL). 3118 (Vanrhynsdorp); near Bitterfontein
(-AB), H. Hall 3960 (PRE): 4289 (NBG, PRE).
3. Cotyledon pygmaea Barker in Flow. PI. S.
Afr. 10: t. 396 (1930). Type: Cape, Vanrhynsdorp,
Vigne sub NBG 2267/29 (K, holo!).
var. pygmaea.
Stems robust and usually (0,4-) 0,5-1 cm in
diameter, with pale yellow rarely greyish bark which
is smooth or peeling in older plants. Leaves densely
covered with heart-shaped trichomes. Squamae trans-
versely oblong to square, 0,08-0,1x0,1-0,13 cm.
Characteristic of C. pygmaea are the multicellular
trichomes which consist of two larger basal cells and
a smaller glandular cell at the apex. The basal cells
are bulging which gives them the heart-shaped
appearance at least on the leaves of var. pygmaea.
The petals are covered with trichomes with oblong
basal cells and the terminal cell is very small. The
latter type of trichomes are found on all parts of
the plants of var. tenuis.
Although extreme forms of the two varieties may
differ in several characters such as the diameter of
steins and their bark, a considerable range of variation
has been recorded and both varieties were found near
Koekenaap. The plant of the typical variety (Hall
sub NBG 587/54) from that area shows somewhat
intermediate characters, but its pollen shows no
abnormality to indicate that the two varieties
hybridize in this region.
var. tenuis Toelken, var. nov., a var. pygmaea
squamis oblongis differt.
Caules tenues 0,2-0, 3 (-0,4) cm in diametro,
cortice griseo plus minusve porcata et non chartaceo.
Folia trichotomibus oblongis sparsim tecta. Squamae
oblongae 0,09-0,12x0,04-0,06 cm.
Type: Cape, near Holrivier Station, H. Hall 3925
(PRE, holo.!; NBG!).
Stems slender 0,2-0, 3 (-0,4) cm in diameter, with
grey bark more or less ridged and not peeling. Leaves
sparsely covered with erect oblong trichomes.
Squamae oblong 0 , 09-0 ,12x0, 04-0 ,06 cm .
Cape. — 3118 (Vanrhynsdorp): near Holrivier Station (-AD),
Hall 3925 (NBG, PRE); 4273 (PRE); Koekenaap (-CB), Hall
2786 (NBG); Hall sub NBG 72/56 (NBG); Vanrhynsdorp (-DB);
Compton et al sub NBG 842a/48 (NBG).
4. Cotyledon similis Toelken , sp. nov. a C. pygmaea
foliis glabris et pilis longissimis in fauce tubi petalorum
differt.
Herbae perennes tuberibus subterraneis paucira-
mosis usque ad 5 cm longis, caulibus erectis rare remo-
sis et usque ad 12 cm longis et usque ad 0,4 cm in
diametro, griseis et porcis nigris verticalibus. Folia
alterna, elliptica vel oblonga, 0,5-1, 3 cm long, 0,2-
0,4 (-0,5) cm lata, acuta vel obtusa, teretia vel
leviter complanata, glabra sed cellulosis pustuliformi-
bus, viridia et saepe rufo-striata. Inflorescentia mono-
chasium 1 (-3) floribus, pedunculo glabro 0,8-3 cm
longo, pedicello glabro 0,4-0, 6 cm longo, bracteis
lanceolatis deciduis. Sepala triangulari-lanceolata,
0,15-0,25 cm longa, acuta, glabra, succulenta, viri-
dia. Petala oblonga, 0,8-1 cm longa, acuta, connata
in tubo 0,6-0, 8 cm longo, extus glabra et intus pilis
longis tenuis praecipue in fauce tubi petalorum,
pallide flavo-virentia vel eburnea. Stamina 0,7-1 cm
longa et aequilonga, antheris 0,08-0,1 cm longis,
filamentis rectis pilis patentibus praecipue in partibus
quibus connatis tubo petalorum. Squamae anguste
oblongae, 0,12-0,14x0,02-0,03 cm, plerumque
penitus emarginatae, leviter succulentae, croceae ad
flavam. Carpella ovariis gracilibus gradate constricta
ad stylos erectos et stigmatibus terminalibus; ovarium
1 0—14 ovulis ovatis sed latioribus ad lateres et porcis
verticalibus.
Type: Cape, N. of Grootmis, Wisura 1303
(NBG, holo!).
Perennial with branched underground tubers up to
5 cm long, each with an erect stem; stems rarely
branched, up to 12 cm long and up to 0,4 cm in
diameter, grey with black vertical ridges. Leaves
alternate, elliptic to oblong 0,5-1 ,3 cm long, 0,2-0, 4
cm broad, acute or obtuse, terete or almost so, gla-
brous but with irregularly bulging epidermal cells,
green, often with reddish-brown stripes. Inflorescence
a monochasium with 1 (-3) flowers, with glabrous
peduncle 0,8-3 cm long, with glabrous pedicels
0,4-0, 6 cm long, with deciduous lanceolate bracts.
Sepals triangular-lanceolate, 0,15-0,25 cm long,
acute, glabrous, succulent, green. Petals oblong,
0,8-1 cm long, acute, fused into a tube 0,6-0, 8
cm long, glabrous on the outside and with long
fine hairs in the throat of the petal tube, pale
yellowish-green to cream. Stamens 0,7-1 cm long and
all about the same length, with anthers 0,08-0,1 cm
long, with straight filaments with spreading hairs
mainly where fused to the petal tube. Squamae nar-
rowly oblong, 0,12-0,14x0,02-0,03 cm, usually
deeply emarginate, slightly fleshy, orange to yellow.
H. R. TOLKEN
193
Carpels with slender ovaries gradually constricted into
erect styles and terminal stigmas; ovary with 10-14
ovules almost dumbell-shaped and with vertical
ridges.
Plants of this species were found either in east-
facing crevices on exposed rock ledges or on quart-
zite gravel on hills mainly west of the mountains
between Komaggas and the Orange River.
The slender grey stems bear leaves only for a very
short period, so that this delicate plant is easily over-
looked. The slender stems are superficially similar to
those of C .pygmaea var. tenuis.
Cape. — 2816 (Oranjemund) : Numees mountain (-BD),
Tolken 3312 (BOL); Holgat River (-DB), Tolken 1857 (BOL).
2917 (Springbok): Augrabies (-AA), Hal! 1362A (NBG); N. of
Grootmis (-AC), Wisura 1303 (NBG); 48 km S.E. of Port
Nolloth (-AC), Acocks 14235 (PRE); 46 km E. of Port Nol-
loth (-AD), M. Schlechter sub SUG 6870 (BOL); Ratelpoort
(-BD), Littlewood sub (NBG) 434/69 (NBG); Komaggas (-CD),
Tolken 2026 (BOI).
5. Cotyledon viridiflorum Toelken, sp. nov. a C.
fragile petalis pubescentibus intra et extra et foliis
dorsoventraliter complanatis glabrescentibus differt.
Fruticuli basis tuberosis, ramis paucis succulentis
usque ad 35 cm longis, erectis, tectis pilis grandulosis
glabrescentibus. Folia alterna, oblanceolata vel ellip-
tica, 2-4 cm longa, 0,8-1 cm lata, cuneata, plerumque
apicibus obtusis, dorsiventraliter complanata et
leviter sulcata supra, tecta pilis glandulosis vel glabres-
centia, succulenta, viridia. Inflorescentia thyrsus spici-
formis (1-) 3-5 floribus, pedunclo 0,8-4 cm longo
et pedicello glabro 0,5-1 (-2,5) cm longo, bracteatis
squamosis. Sepala triangulari-lanceolata, 0, 5-0,6 (-1)
cm longa, acuta, tecta pilis glandulosis patentibus,
succulenta, viridia. Petala oblonga, 2, 4-2, 6 cm longa,
acuta, connata in tubo 1,8-2 cm longo, apicibus
recurvis, tecta pilis plus minusve glandulosis intra et
extra, leviter succulenta, viridia vel flavovirentia.
Stamina 1 ,4-1 ,9 cm longa, antheris nigris 0,4-0, 6 cm
longis, filamentis pilis patentibus et saepe flexibus infra
antheras. Squamae oblongae, 0,1-0,12x0,03-0,05
cm, leviter emarginatae, succulentae, flavae. Carpella
1 ,2-1 ,5 cm longa, ovariis gracilibus gradate constric-
tis ad stylos erectos stigmatibus terminalibus; ovarium
8-12 ovulis elongato-ovatis porcis verticalibus.
Type: Cape, near Modderfontein, Tolken 5327
(PRE, holo!).
Shrublet with tuberous bases, with few brittle fleshy
branches up to 35 cm long, erect, covered at first with
glandular hairs, later glabrescent. Leaves alternate,
oblanceolate to elliptic, 2-4 cm long, 0,4-1 cm broad,
each with cuneate base and obtuse apex, dorsiventrally
compressed and slightly grooved above the central
vein, covered with glandular hairs when young becom-
ing glabrous later. Inflorescence a spike-like thyrse
with (1-) 3-5 flowers, with peduncle 0,8-4 cm long and
pedicels 0,5-1 (-1,5) cm long, with scale-like bracts.
Sepals triangular-lanceolate, 0,5-0, 6 (-1) cm long,
acute covered with spreading glandular hairs, succu-
lent, green. Petals oblong 2, 4-2, 6 cm long, acute,
fused into a tube 1 ,8-2 cm long, with apices recurved
or recoiling, covered with recurved hairs, more or
less glandular on the outside and inside, slightly
fleshy, yellowish-green. Stamens 1,4-1, 9 cm long,
with black anthers 0,4-0, 6 cm long, filaments with
spreading hairs and often with right-angled outward
bend below anthers. Squamae oblong 0,1-0, 12 X
0,03-0,05 cm, slightly emarginate fleshy, yellow.
Carpels with slender ovaries gradually constricted into
erect styles with terminal stigmas; ovary with 8-12
ovules with vertical ridges. Like C. fragilis and C.
vetricosa, this species grows in the shade of overhang-
ing rocks and usually on the south aspect of moun-
tains.
Cape. — 2817 (Vioolsdrif): near Modderfontein (-CC), Tolken
5327 (PRE).
6. C. hallii Toelken , sp. nov. a C. pearsonio habi-
tato erecto-fastigiato et usque ad 40 cm alto, foliorum
cicatricibus paene indistinctis et floribus erectis differt.
C.pearsonii sensu Jacobsen, Hand, Succ. PI. 1 : 289, fig. 286
(1960); Sukk. Lex. 135, t. 40,5 (1970), non Schonl. C. racemosa
sensu Friedr. in Prodr. FI. S.W. Afr. 52: 10 (1968), non Harv.
Fruticuli perennes caulibus succulentis usque ad 5
cm in diametro et leviter ventricosis ad basim, multi-
ramosi et ramis erectis vel paene fastigiata. Folia
alterna, lineari-lanceolata, 0,8-3, 5 cm longa, 0,3-
0,5 cm lata, acuta, teretia vel interdum sulcata supra,
sparsim tecta pilis glandulosis sed glabrescentia,
viridia vel glaucescentia. Inflorescentia thyrsus \-4
monochasiis, pedunculo lignescente 1,5-3, 5 cm
longo, pedicello tenace 1-3 cm longo tecto pilis plan-
dulosis, bracteatis foliiformibus. Sepala triangularia,
0,4-0, 9 cm longa, acuta, tecta pilis glandulosis paten-
tibus, succulenta, viridia. Petala oblonga, 1,7-2 cm
longa, plerumque acutissima, connata in tubo 1-1,4
cm longo, apicibus recurvis sed erectis in fructu, tecta
pilis glandulosis patentibus extus et pilis sparsis tenui-
bus intus, leviter succulenta, viridia vel flavo-viridia.
Stamina 1 ,6-2 cm longa, antheris 0,3-0, 5 cm longis,
filamentis paene glabris et plerumque flexibus infra
antheras. Squamae oblongae 0,12-0,15x0,04—0,06
cm, emarginatissimae, succulentae ad basim, flavae.
Carpella ovariis gracilibus gradate constrictis ad
stylos erectos stigmatibus terminalibus; ovarium 30-36
ovulis ovatis sed latioribus ad lateres et papillosis
plerumque serialis.
Type: Cape, De Hoop, H. Hall 1300 (NBG, holo!).
Perennial shrublet with fleshy stems up to 5 cm in
diameter and slightly swollen towards the base, much
branched and branches erect and almost fastigiate.
Leaves alternate, linear-lanceolate, 0,8-3, 5 cm long,
0,3-0, 5 cm broad, acute, terete or sometimes with
a groove on the upper surface, sparsely covered with
glandular hairs but becoming glabrous, green or yel-
lowish-green. Inflorescence a thyrse with one to several
monochasia, with glandular rarely glabrescent pedun-
cle 1,5-3, 5 cm long and glandular pedicels 1-3 cm
long, with leaf-like bracts. Sepals triangular 0,6-0, 9
cm long, acute, covered with stout spreading glandular
hairs, fleshy, green. Petals oblong, 1,7-2 cm long,
usually very acute, fused into a tube 1-1,4 cm long,
with apices recurved but straightened out again when
fruiting, covered with glandular hairs along the out-
side and in particular the centre of each petal, with
scattered fine hairs or rarely papillose on the inside,
slightly fleshy, green to yellowish-green. Stamens
1,6-2 cm long, with anthers 0,3-0, 5 cm long, with
filaments almost glabrous and usually with a right-
angled outward bend below the anthers. Squamae
oblong, 0,12-0,15x0,04-0,06 cm, strongly emargi-
nate, succulent towards the base, yellow. Carpels with
slender ovaries gradually constricted into erect styles
and with terminal stigmas; ovary with 30-45 elongate
ovules which are usually dumbell-shaped and with
papillae often arranged in irregular rows.
This species occurs on rocky slopes in the mountains
on either side of the Orange River of Vioolsdrif.
S.W. A. — 2717 (Chamaites): near Aiais (-CD), Pillans 65 8
(BOL). 28 16 (Oranjemund) : Kahanstal (-BB), Dimer 8152 (BOL,
K, PRE, SAM); De Winter & Giess 6360 ( PRE).
Cape. — 2817 (Vioolsdrif): De Hoop (-AA), Hall /DO (NBG);
20 km E. of Eksteenfontein (-CD), Leistner 3373 (PRE); 32 km
S.W. of Vioolsdrif (-CD), Werger 405 (PRE).
194
NEW TAX A AND A NEW COMBINATION IN THE GENUS COTYLEDON
7. Cotyledon tomentosa Harv. in FI. Cap. 2: 373
(1862); Schonl. in Rec. Albany Mus. 3: 146 (1915).
Type: Cape, between Groot River and Trumpeter’s
Poort, Zeyher 1085 (S, holo!).
subsp. tomentosa.
C. tomentosa Harv. in FI. Cap. 2: 373 (1862). C. ladismithiensis
sensu Boom in Succulenta, Amst. (1958) 17; sensu Jacobsen,
Handb. Succ.PI. 1 : 284, fig. 278 (I960); Sukk. Lex. 134, T.39, 1
(1970), non V.Poelln.
Shrublets with slender branches, much branched.
Leaves oblanceolate 1,5-2, 5 (-3,5) cm long, 0,8-1, 4
(-1 ,7) cm broad, with 3-5 (-10) apical teeth, more or
less dorsiventrally compressed.
C. tomentosa is a little known species, which is poor-
ly represented in herbaria and at known localities one
finds only a few plants. However, the main obstacle
in interpreting the identity of C. tomentosa was that
Harvey did not mention in his description the three
distinct teeth at the apex of the leaves. The type locality
given by Zeyher was rather vague, but it must be
sought somewhere east of Steytlerville, which lies on
the Gamtoos River (alias Groot River). The plant was
recently collected in the mountains just north of
Steytlerville {Tolken 1778).
Then C. heterophylla Schoenl. non Roxb. was
described from the vicinity of Ladismith, but being a
later homomym it must be replaced by the name
C. ladismithiensis V.Poelln. The latter taxon is here
considered to be a separate subspecies of C. tomentosa,
which is distinguished from the typical subspecies by
its longer almost terete leaves as described below. The
number of teeth on the leaves varies greatly on the
same and different plants, and juvenile plants of both
subspecies seem to have leaves with 1-3 teeth. The
leaves of juvenile plants and of plants of the subsp.
tomentosa growing in deep shade are villose, while
those of the subsp. ladismithiensis are tomentose, but
no seedlings have been seen.
Subsp. tomentosa has been recorded from near
Calitzdorp. Willowmore and Steytlerville, where it
occurs on the slopes of sheltered kloofs. Plants of the
subsp. ladismithiensis occur on rock outcrops between
Laingsburg and the northern slopes of the Lange-
berg near Muiskraal.
subsp. ladismithiensis {V.Poelln.) Toelken, comb,
nov. et stat. nov.
C .ladismithiensis V. Poelln. in Jahrb. Deutsch.Kakt. Ges.
1: 94 (1936); in Fedde Repert. 42: 40 (1937). Type: Cape,
between Ladismith and Laingsburg, E.Pillans sub N.S. Pillans
968 (GRA, holo!; BOL). C. heterophylla Schoenl. in Rec.
Albany Mus. 2: 150 (1907), non Roxb. (1814); in Rec. Albany
Mus. 3: 146 (1915). Type: same as for C. ladismithiensis.
Shrublet with rigid spreading branches, little
branched. Leaves oblong-elliptic (3-) 3, 5-5, 5 (-8) cm
long, 0,8-1, 2 cm broad, with 1 (-3) apical teeth,
usually almost terete and only occasionally the upper
surface is compressed.
Cape. — 2033 (Montagu): Anysberg (-DB), Stokoe 8708
(BOL); western Touwsberg (-DB), Warts 1467 (NBG). 2133
(Ladismith): Ladismith (-AD), Joubert s.n. (BOL); Huisrivier-
pas (-BC), Marloth 13128 (PRE); Ockertskraal (-CA), Hall
1224 (NBG); 16 km S. of Ockertskraal (-CA), Tolken 1699
(BOL); Adamskraal (-CC), Muir sub BOL 30962; Muiskraal
(-CC), Muir sub Marloth 12185 (PRE); between Laingsburg and
Ladismith, E. Pillans sub N.S. Pillans 968 (BOL, GRA).
U1TTREKSEL
Vyf nuwe species en een varieteit word beskryf en die
nuwe kombinasie Cotyledon tomentosa Harv. subsp.
ladismithiensis {V.Poelln.) Toelken word teweeggebring.
Die volgende nuwe name is gepubliseer: C. sulphurea
Toelken, C. occultans Toelken, C. similis Toelken, C.
viridiflorum Toelken, C. hallii Toelken en C. pygmaea
Barker var. tenuis Toelken.
Bothalia 12,2: 195-197 (1977)
The identity of Erica flavisepala
E. G. H. OLIVER*
abstract
The recording of a few scattered plants of E. flavisepala Guth. & Bol. among sympatric populations of
two other species led to a comparison of their morphological characters. From this comparison a putative
hybrid origin was indicated, thus E. X flavisepala Guth. & Bol^E. thunbergii Montin x E. sphaerocephala
Wendl.
RESUME
L'lDENTITE D’ERICA FLAVISEPALA
L' observation de quelques plants <7’E. flavisepala Guth. & Bol., disperses parmi des populations
sympatriques de deux autres especes, a conduit a une comparison de leurs caracteres morphologiques.
Cette comparaison suggere une origine hybride, vraisemblablement E. X flavisepala Guth. & Bol.
= E. thunbergii Montin X E. sphaerocephala Wendl.
In Flora Capensis (1905) Guthrie and Bolus
described E. flavisepala from material that had been
sent to them in a consignment of E. thunbergii Montin
from an unspecified locality in the Cold Bokkeveld.
The species were reported as growing together.
The authors stated that their material was difficult
to place satisfactorily in any of the sections of the
genus and that it constituted a well-marked species
with a general aspect strikingly similar to that of E.
thunbergii. But they noted that it did not have the
peculiar globose corolla-tube of E. thunbergii and,
although anomalous, placed it in the same section,
Cyatholoma.
Since the original collection of E. flavisepala no
material has been collected until recently. Mr G.
Kirsten, a keen collector of ericas, while examining
populations of E. thunbergii in the Loch Lynne area
of the Cold Bokkeveld, came across a few isolated
plants which I was able to confirm were E. flavisepala.
I decided to visit the area myself to study the species
in the wild.
The fine populations of E. thunbergii were located
without any difficulty in the Hartebeeskloof growing
in seepage zones on south-facing slopes being clearly
visible from a distance. Growing in the same seepage
zones were groups of the pink-flowered E. sphaeroce-
Fig. 1. — Erica thunbergii. 1, flo-
wer, x5; la, corolla, x5; 2,
bracteoles, xlO; 3, sepals,
X 10; 4, androecium and
gynoecium, X5; 5, anther,
front, side and back views,
x 20; 6, ovary, x 10; 7, leaf,
X 10 (from Oliver 5139).
* Botanical Research Institute, Department of Agricultural Technical Services, Private Bag X101, Pretoria.
196
THE IDENTITY OF ERICA FLAVISEPALA
T | Fig. 2. — Erica x flavisepala. 1,
I 1 flower, x5; 2, bracteoles,
■fi x 10; 3, sepal, x 10; 4, an-
! ji droecium and gynoecium,
| | x5; 5, anther, front, side
\ and back views, x 20, 6,
\ i ovary, x 10; 7, leaf, x 10.
1 • / (from Oliver 5140).
Fig. 3. — Erica sphaerocephala 1,
flower, x5; 2, bracteoles,
xlO; 3, sepal, xlO; 4, an-
droecium and gynoecium,
x 5 ; 5, anther, front, side and
back views, x20; 6, ovary,
x 10; 7, leaf, x 10. (from
Oliver 5141).
Fig. 4. — Branches of 1, Erica
sphaerocephala ( Oliver 5141);
2, EricaX flavisepala ( Oliver
5140); 3, Erica thunbergii
( Oliver 5139)
E. G. H. OLIVER
197
TABLE 1.— Comparison of morphological characters of E. thunbergii, E x flavisepala and E. sphaerocephala
phala. While investigating E. thunbergii , a few plants
of E. flavisepala were found. It was immediately
suspected that these few scattered plants were hybrids
between the frequently occurring E. thunbergii and
E. sphaerocephala.
E. thunbergii (Fig. 1) is a very distinct species with
yellow, orange and white flowers with globose corolla-
tubes. It belongs to the section Cyatholoma , which it
shares with E. corydalis Salisb. and E. flavisepala
(Fig. 2), the characteristic feature being the globose
corolla-tube with a large dilated cup-shaped limb.
E. corydalis with flowers all white, is also a very dis-
tinct species occurring in the coastal mountains of
the Caledon district. E. sphaerocephala (Fig. 3) belongs
to a completely different section, Pseuderemia, which
is characterized by having the flowers arranged in a
many-flowered capitate head. (See Fig. 4).
A comparison of morphological characters of my
three collections, Oliver 5139, 5140 and 5141 which
are illustrated in the accompanying figures, clearly
shows the intermediate nature of E. flavisepala. The
basic shapes and sizes of the bracteoles, pedicel,
sepals, corolla, anthers and ovary of the two parent
species are very distinct, while those of E. flavisepala
are intermediate in most respects.
E. thunbergii is almost entirely glabrous except tor
a few hairs very occasionally found on the petioles,
whereas in E. sphaerocephala the branches, leaves,
pedicels, bracteoles and sepals are all puberulous and
ciliate, the cilia being plumose. The anthers of E.
thunbergii are distinctly prognathous and are dis-
tinctly aristate. The ovary in E. thunbergii is stipitate
and in E. sphaerocephala it is sessile.
The flower colours are very distinctive. In E. thun-
bergii the large bracteoles and sepals are bright canary-
yellow, the corolla-tube white and the lobes brillian
orange-red. In E. sphaerocephala the bracteoles and
sepals, which are relatively small, are green to reddish
in colour and the corolla is pink. In E. flavisepala the
bracteoles and sepals are yellow tinged with red and
the corolla is bright pinkish red.
The pollen of E. thunbergii and E. sphaerocephala is
typical of the genus Erica , namely in tetrads. The
pollen of the collection Oliver 5140 is abnormal in
consisting of an equal quantity of tetrads and single
grains mixed with some shrivelled grains. This sup-
ports the view of the hybrid nature of E. flavisepala.
The occurrence of only a few scattered plants of
E. flavisepala amongst the populations of the other
two species indicates that the plants were a chance
cross that is not reproductively established. Unfor-
tunately it has not been possible to study the chromo-
somes. The few species of Erica which have so far been
investigated all have n= 12 and their chromosomes are
extremely small. It is therefore unlikely that taxono-
mically useful information could be derived from a
brief investigation of the three taxa.
The facts as set out (in Table 1 ) indicate the putative
origin of E. flavisepala Guth. & Bol. (E. x flavisepala
Guth. & Bol.=£. thunbergii Montin x E. sphaero-
cephala Wendl.).
UITTREKSEL
Die vermelding van 'n paar verspreide plante van E.
flavisepala Guth. & Bol. tussen simpatriese populasies
van twee ander soorte het gelei tot 'n vergelyking van
hid morfologiese eienskappe. Uit hierdie vergelyking
kan 'n veronderstelde hibridiese oorsprong aangedui
word, dus E. x flavisepala Guth. & Bol. = E. thunbergii
Montin X E sphaerocephala Wendl.
Bothalia 12,2: 199-203 (1977)
The identity of Eriosema nanum
C. H. STIRTON*
ABSTRACT
An examination of available evidence leads to the conclusion that Eriosema nanum Burtt Davy must be
regarded as a synonym of E. ellipticifolium Schinz. The relationship between E. ellipticifolium and E. uniflorum
Burtt Davy is discussed.
RESUME
L'IDENTITE D’ERIOSEMA NANUM
Eriosema nanum Burtt Davy doit etre considere comme un synonyme t/’E. ellipticifolium Schinz.
A cette conclusion basee sur I'examen des preuves disponibles est jointe une discussion de la relation
entre E. ellipticifolium et E. uniflorum Burtt Davy.
INTRODUCTION
Eriosema nanum Burtt Davy, together with E.
populifolium Harv. and E. angustifolium Harv., are
among the rarest of the Fabaceae in South Africa.
Recent intensive field studies of Eriosema (Stirton,
1975) showed the widespread occurrence of hybridi-
zation and of morphological variation in the genus
in South Africa. This paper assesses various aspects
of phenotypic plasticity and interspecific hybridi-
zation as they affect the identity and delimitation of
E. nanum.
HISTORY
Schinz, in Vjschr. Naturf. Ges. Zurich 66: 229,
1921, based E. ellipticifolium on Junod 1411 from
Shilouvane and Junod 2534 (Fig. 1) from Marovunge,
both in the Eastern Transvaal. Owing to the absence
of ripe or almost ripe fruits, he was unable to
establish clearly whether he was dealing with a
Rhynchosia or an Eriosema species (“Solange keine
reifen oder nahezu reifen Friichte vorliegen, ist es
vorlaufig ein aussichtsloses Bemiihen, feststellen zu
wollen, ob es sich um eine Rhynchosia — oder eine
Eriosema- Art handelt, sicher ist, dass sie sich mit
keiner der mir bekannten Arten dieser oder jener
Gattung deckt”). Fie commented, however, that the
plant was reminiscent of E. salignum, but differed
Fig. 1. — Junod 2534, lectotype of Eriosema ellipticifolium.
‘Botanical Research Institute, Department of Agricultural
Technical Services. Private Bag X101, Pretoria.
in its lower surface indumentum. The name E.
ellipticifolium has never been taken up.
In 1932 Burtt Davy treated E. ellipticifolium very
briefly under the heading “species not seen”. In this
work, however, he published Eriosema nanum based
on Galpin 1139 from the summit of the Saddleback
Mountain in the Barberton area (Fig. 2). As its
allies he noted E. rufescens Schinz and E. burkei
Benth. and commented also that it was perhaps
closest to E. uniflorum Burtt Davy.
Fig. 2 — Galpin 1139, isotype of Eriosema nanum.
A study of type specimens leaves no doubt that
E. nanum is synonymous with E. ellipticifolium.
Population studies showed that the wide leaf variation
encountered is the result of a dine of decreasing
width in a northerly direction (Stirton, 1975). The
type localities of E. ellipticifolium occur in the
northern extremities of this range. It is unfortunate
that the more descriptive name nanum must be
superseded.
200
THE IDENTITY OF ERIOSEMA NANUM
FIELD OBSERVATIONS
Plants growing in full sun tended to be shorter
and more compact than plants of the same species
found growing under different intensities of shade.
In Fig. 3 plants of E. ellipticifolium that were found
growing in short open grassland (plant 1) are con-
trasted with those growing along a road bank in a
pine forest (plant 2). Plant 1 can be seen to be smaller
and more compact than plant 2. Other obvious
differences, not all observable from the photographs,
are the longer inflorescences, the thinner leaves and
the less prominent secondary and tertiary venation
in plant 2. Plants that grew through a thick canopy
of grass had the same facies as the plants that grew
in or along forest margins. These features can be
clearly seen on Stirton 1431. These various expressions
of morphological form could possibly be the result
of a competition balance of mineral nutrients, degree
of light intensity, extent of water availability, or a
combination of these and other factors. The plants
shown in Fig. 3 were chosen as representative of
the range of variation within the species after a critical
inspection of their populations.
Fig. 3 — Eriosema ellipticifolium. The different facies of plants
growing: 1, in short open grassland (Stirton 1467); 2, on a
roadbank in a pine forest ( Stirton 1486); 3, in burnt veld
( Stirton 1040); 4, in unburnt veld adjacent to 3 (Stirton 1041).
Plants that grew in burnt veld (Fig. 3: 3) had a
more stunted form than plants of the same species
which grew in adjacent unburnt veld (Fig. 3: 4). These
plants were collected on the same day. The various
populations were observed subsequently and it was
found that once the new grass had come away the
“dwarf plants” began to grow lank so that by the
end of the season they were similar, but still shorter,
than plants collected in the adjacent tall unburnt
grassveld. The plants that grew in the burnt veld had
almost completed their flowering period by the time
the plants which grew in the unburnt veld had begun
to flower.
The observations in open veld and in forest, and
in burnt and unburnt veld, were found to be consistent
throughout the range of distribution of E. elliptici-
folium. The results lead me to suspect that once the
type specimen of E. urtiflorum Burtt Davy is compared,
it will probably have a facies similar to plant 2 in
Fig. 3 and hence synonymous with E. ellipticifolium.
Compton (1974, pers. comm.) has indicated that he
intends to incorporate E. urtiflorum under E. nanum
in his revised Flora of Swaziland. Judgement is here
reserved until the type is traced, since the description
of E. urtiflorum has features linking E. ellipticifolium
and Stirton 1482 ( E . sp. nov.) allied to E. cordatum.
On the Galpin 1139 sheet from the Bolus Herbarium
there is a specimen Bolus 11854 that has three Bolus
manuscript names; uniflorum, pumilum and cryptantha.
Appended to the specimen is a note, apparently in
N. E. Brown’s handwriting, that says “We afterwards
decided that this was probably a stunted form of
E. burkei" . The specimen is E. ellipticifolium. Field
studies (Stirton, 1975), however, indicated that
stunted forms of E. pauciflorum Klotzsch, rather than
E. burkei, are deceptively similar to E. ellipticifolium.
The most noticeable variation observed in the field
was the range in number of flowers per inflorescence.
Plants of the same population were found to have
inflorescences bearing from one to ten flowers.
Although most specimens have been reasonably
easy to place in this species there remain a few
problems. Hybridization cannot be ruled out as the
cause of some complexing difficulties encountered in a
recent field trip. Two populations in particular
require a detailed study as in both areas E. elliptici-
folium grows sympatrically with the rare E. angusti-
folium Burtt Davy and an undescribed taxon. A
feature of these populations is their marked
geographical separation viz. Magoebaskloof (N.
Transvaal) and Havelock (Swaziland) and also the
wide range of “intermedates” found. Flower colour,
pubescence and the shape of stipules have been
shown in preliminary hybridization studies (Stirton,
1975) on other species to be reliable indicators of
putative hybrids. These three characters varied
markedly in “intermediate” plants in both popu-
lations. E. angustifolium has a striking, stiff, rufous,
patent indumentum, linear leaves, erect habit, and
yellow flowers, and is not readily confused with
either E. ellipticifolium or Stirton 1445 (E. sp.) The
latter occurs from the N. Transvaal southwards to
Swaziland and although fairly common in isolated
areas has not been previously collected. This multi-
stemmed plant is a pink and yellow flowered perennial
with prostrate habit, and small unifoliolate leaves.
Its closest affinity is E. ellipticifolium. The intermediate
plants at Magoebaskloof seem to be hybrids between
E. angustifolium and E. ellipticifolium ( Stirton 1442),
and between Stirton 1445 (E. sp.) and E. ellipticifolium
( Stirton 1446). Further field studies are necessary
before all three putative parents are clearly delimited.
The inter-relationships of these three species remain
obscure.
Three specimens named E. ellipticifolium in this
study are doubtful: these are Jacobsen 1587, Coetzer
150, and Vahrmeijer 2433. The last two of these,
although very close to E. ellipticifolium, differ in
pubescence and their very acute leaves. All these
will no doubt be easier to place once all the montane
species of Eriosema have been studied.
E. ellipticifolium begins flowering in early September
and reaches a peak in December, occasionally
extending into January. The Natal populations
flower much earlier than those in the Transvaal.
TAXONOMY
Eriosema ellipticifolium Schinz in Vjschr. Naturf.
Ges. Zurich 66: 229 (1921). Syntypes: Transvaal,
Shilouvane, near Sanatorium, Junod 1411 (Z!);
Marouvunge, Junod 2534 (Z!). Lectotype: Junod
2534 (Z!).
Eriosema nanum Burtt Davy, FI. Transv., 2: XXII (1932);
Ross, FI. Natal 208 (1972). Type: Transvaal, Saddleback
Mountain, Galpin 1139 (PRE, holo. !; BOL, NBG, NH).
C. H. STIRTON
201
Fig. 4. — Eriosema ellipticifolium. 1, habit, 1: 2, perennial rootstock, x 1; 3, flower bract, x 74; 4, flower, x 24;
5 calyx opened out, x 74; 6a, standard opened out x 54; 6b, standard closed, x 54; 7, wing, x 54; 8, keel,
x 54; 9, vexillar stamen, x 74; 10, staminal sheath, x 74; 11, discoid floral nectary, x 15; 12, gynoecium,
x 74; 13, stigma, x 33; 14, fruit pod, x 1; 15a, seed with strophiole, face view, x 54; 15b, seed with strophiole,
marginal view showing hilum, x 54-
202
THE IDENTITY OF ERIOSEMA NANUM
Perennial herb (4) 9-12 (25) cm high with one to
six stems from short stylopodium of carrot-like,
usually constricted, underground rootstock. Stems
erect or ascending, 3-10 (23) cm long; terete or
angular, often ribbed, glandular or eglandular,
clothed with short white pubescent and long spreading
pale yellow or white, hairs. Stipules free, 6-15 mm
long, 2, 0-3, 5 mm wide; narrowly ovate to ovate,
often falcate, striate, white or ferruginous hairy.
Leaves trifoliolate, basal leaves unifoliolate; leaflets
4. 0- 7,0 cm long, 1,4-3, 5 cm wide, laterals smaller,
elliptic to narrowly elliptic or narrowly oblong, base
truncate, mucronate, middle nerve slightly sunken
above, prominent and subreticulate below, short
appressed pubescent on both sides, denser on nerves,
densely orange gland-dotted below, lightly above,
terminal leaflet symmetrical, laterals asymmetrical
with bases slightly oblique; young leaves glandular,
long appressed tawny haired on veins with short
curly dense pubescence between; Petiole 4-11 mm
long; Petiolules ca. 2 mm long; rachis 5-8 mm long.
Racemes 1-10-flowered; peduncle (1 ,0) 2,0-3, 5 (7,5)
cm long, canaliculate, with long spreading tawny,
or long white hairs interspersed with short white
deflexed hairs; rachis 0,7-2, 1 cm long; pedicels
ca. 3 mm long. Flowers 6-10 (13) mm long, 3-5 mm
wide, reflexed, corolla barely exceeding calyx, yellow;
bracts 6-8 mm long, 1,0-1, 5 mm wide, lanceolate,
shallow boat-shaped, 3-6-veined, thinly pilose, more
than half length of flower. Calyx 6-9 mm long with
long and short admixed pale yellow or white hairs,
glandular outside, hairy inside at apex of lobes with
smaller hairs scattered on either side of veins; tube
2.0- 2, 5 mm long, slightly longer between horn
lobes; lobes unequal, lanceolate, 3-4 times longer
than tube, horn lobes 7, 5-8,0 mm long curving
inwards, lateral lobes 7, 0-8,0 mm long curving
upwards; keel lobe longest, 8, 0-9, 2 mm long.
Standard yellow (7,5) 9-10 (13,0) mm long, (4,5)
6. 0- 7,0 mm wide, narrowly obovate, often narrowed
towards base, white pubescent and glandular on
back; claw 2, 0-2, 6 mm long; width between auricles
3. 0- 4,0 mm; appendages free of auricles, being
upcurled flaps joined slightly in the middle, (1,5)
3. 5- 4,0 mm from base of claw. Wings 7,5-10,1 mm
long, 2,0-3, 3 mm wide at maximum, longer than
keel blades, eglandular, occasionally very glandular;
claw 1,5-2, 5 mm long, attenuate; auricle (1,2)
1 .5- 1 ,6 mm high, straight. Keel blades 6, 5-7, 5 (8,9)
mm long, 3, 0-4,0 (4,6) mm wide at maximum,
auricle 1,0-1, 7 (2,0) mm high, claw 1, 7-3,0 mm
long, attenuate, apex rostrate. Staminal sheath 5,7-
7.0 mm long, 2, 7-4,0 mm wide at maximum, free
stamen 5, 0-6,0 mm long, basal knee 1,0-1, 3 mm
long. Gynoecium 6, 0-6, 6 mm long; ovary 2,4-
3.0 mm long, subsessile; clothed with long stiff hairs
as far as point of style swelling or flexure; gynophore
0, 1-0,5 mm; style unevenly thickened, widest at
middle of thickening, curvature 2,0-2, 2 (2,7) mm
high; stigma globose, inserted. Nectary 0,4-0, 5 mm
high, discoid, margin erose. Fruits broadly ovate,
1,4-1, 6 cm long, 0, 9-1,0 cm wide, clothed with
appressed light yellow hairs, denser along sutures,
with small stiff hairs between; seeds 0, 5-0,6 cm
long, 0,3 cm wide, black, or greenish yellow with
small faint reddish blotches. (Fig. 4).
Eriosema ellipticifolium is restricted to isolated
mountain “islands” in Swaziland, the Transvaal and
Natal (Fig. 5). This species exhibits a disjunct distri-
bution over a wide area and over diverging ecological
conditions and veld types. If is found between
1 600-2 500 m growing predominantly amongst rocks
in short grassland on dry ridges with a northwest
aspect. A number of populations has been located
on forest margins and along forest roads at the
Witklip, Mariepskop and Woodbush Forest Reserves.
Swaziland. — 2631 (Mbabane): Mbabane (-AC), Rogers
11601 (PRE).
Transvaal. — 2329 (Pietersburg): Haenertsburg (-DD), Pott
4798 (PRE). 2330 (Tzaneen): Magoebaskloof Hotel (-CC),
Stirton 1443 (PRE). 2429 (Zebediela): Donkerfkloof near Chu-
niespoort (-BA), Vahrmeijer 2443 (PRE). 2430 (Pilgrim’s Rest):
The Downs (-AA), Rogers 22057 (PRE); near Reitz’s grave on
Mariepskop (-DB), Stirton 1449 (PRE); Ohrigstad Nature
Reserve (-DC), Jacobsen 1587 (PRE). 2530 (Lydenburg)
Dullstroom (-AC), G at pin s.n. (24-12-1932, BOL); Witklip
Forest Station (-BD), Kluge 195, 626 (PRE); summit of
Saddleback Mountain (-CC), Galpin 1139 (BOL, GRA, NBG,
NH, PRE). 2531 (Komatipoort): Havelock Border Post (-CC),
Stirton 1464 (PRE).
Natal. — 2731 (Louwsburg): Mount Inyati (-CC), Hilliard &
Burtt 5889 (NH, NU). 2830 (Dundee): The Kop (-DD), Stirton
1033, 1040, 1041 (PRE).
Fig. 5. — Eriosema ellipticifolium. Known distribution in
Southern Africa.
Junod 2534 is chosen as lectotype, since the
quantitative data given in the protologue indicates
that Schinz must have based most of his description
on the two specimens on this sheet.
This little-known species has proved to be more
common and widespread than was previously
accepted. The available herbarium material had been
placed under no less than six species. It had been
most commonly confused with Eriosema cordatum
var. cordatum , but is readily separated from this
and all other species by its very long calyx lobes
which almost equal the length of the flower.
Despite its widespread distribution (Fig. 5) this
species is remarkably uniform and distinctive in the
field. Its poor representation in herbaria is probably
attributable to its dwarf habit (Fig. 6) and not to its
scarcity in the field as, during a recent trip to the
eastern Transvaal, it was found to be locally common
throughout the moist highlands.
C. H. STIRTON
203
Fig. 6. — Eriosema ellipticifolium: dwarf habit.
ACKNOWLEDGEMENTS
This article is an extension of part of a thesis
submitted for the M.Sc. degree at the University of
Natal, Pietermaritzburg. I am most grateful to
Dr. K. D. Gordon-Gray for her guidance and advice
during the initial stages of this study and for kindly
providing funds for Fig. 4. I am grateful to the
Director, Botanisches Museum der (Jniversitat Zurich,
for the loan of the types of E. ellipticifolium Schinz.
UITTREKSEL
'n Ondersoek van al die beskikbare gegewens dui
daarop dat Eriosema nanum Burtt Davy 'n sinoniem
van E. ellipticifolium Schinz is. Die verwantskappe
tussen E. ellipticifolium en E. uniflorum Burtt Davy
word ook bespreek.
REFERENCES
Burtt Davy, J., 1932. A manual of the flowering plants and
ferns of the Transvaal with Swaziland, South Africa. London :
Longmans, Green & Co. 529 pp.
Stirton, C. H., 1975. A contribution to knowledge of the genus
Eriosema ( Leguminosae-Lotoideae ) in Southern Africa
(. excluding Mozambique and Rhodesia). Unpublished M.Sc.
thesis, University of Natal, Pietermaritzburg. 182 pp.
APPENDIX
This appendix lists all specimens considered by the author to
belong to Eriosema ellipticifolium Schinz:
Bolus 11854 (BOL); Coetzer 150 (PRE); Galpin s.n. (BOL),
1139 (BOL, GRA, NBG, NH, PRE); Gilmore 2284 (PRE);
Hilliard 2942 (NU); Hilliard & Burtt 3358 (NU), 5889, 5908
(NH, NU); Junod 1411, 2534 (Z); Kluge 195, 626 (PRE); Muller
2012 (PRE); Pott 4798 (PRE); Rogers 1160, 22057 (PRE);
Stirton 1033, 1040, 1041, 1346, 1431, 1436, 1439, 1441, 1443,
1449, 1464, 1467, 1471, 1474, 1475, 1483, 1486, 1487 (PRE);
Vahrmeijer 2433 (PRE); Van der Schijff 6440 (PRE).
Bothalia 22, 2: 205-208(1977)
Morphological studies of the Ochnaceae*
P. C. V. DU TOITj
ABSTRACT
The cause of the characteristic sloughing of the bark of certain Ochna species is described, while the mor-
phology of the growth buds, leaves and stipules of South African genera of the Ochnaceae is discussed. The
taxonomic significance of these features is indicated where relevant.
RESUME
ETUDES MORPHOLOGIQUES SUR LES OCHNACEAE
La cause de la desquamation de Tecorce, caracteristique de certaines especes du genre Ochna,
est dec rite ; on discute la morphologic des bourgeons de croissance, des feuilles et des stipules dans les
genres sud-africains d'Ochnaceae et, quand il y a lieu, on indique la valeur taxonomique de ces carac-
teres.
INTRODUCTION
During a recent morphological study of the family
Ochnaceae, it was found that relatively little was
known of the organography and anatomy of the
family. A wealth of taxonomic literature was avail-
able, but only a few works gave a synoptic treatment
of the anatomy. The aim of this paper is to draw
attention to these taxonomically important and
interesting characteristics and to stimulate the extra-
polation of these finding to other families.
BARK
An interesting characteristic of some of the indi-
genous species of the Ochnaceae is the rhytidome or
outer bark, i.e. all the tissues on the outside of the
periderm, that peels off in strips or scales.
According to Esau (1965) this manner of rhytidome
formation is common in those species where the
phellogen is initiated superficially. While working on
the anatomy of the family it was noticed in two
species, viz. Ochna arborea and O. pulchra, that the
phellogen was initiated in the epidermis, the epidermal
and phellogen cells lying on the same radial lines, but
at the same time, it was also initiated quite deep in
the cortex. In this instance, the phellogen forms an
interrupted undulating band running through the
epidermis and cortex right round the stem. In time
this undulating band breaks up into outward curving
sectors, like shells. These outward curving shells,
which overlap and are superimposed over yet others
like it, are shed at different times, leaving a smooth,
mottled layer of bark (i.e. all the tissues on the outside
of the vascular cambium). In these two species it was
found that the phellogen gives rise to a very thin layer
of phellem, coinciding with the smoothness of the
bark when the outer layers slough off (Fig. 1). In all
the other indigenous species of the Ochnaceae, the
phellogen is initiated relatively deep in the cortex
with, in addition, a thick layer of phellem. The outer
layers slough away gradually and the bark, exposed
after sloughing, is rough and evenly coloured (Fig. 2).
Making use of this character the species can be
separated into two groups, the one group coinciding
exactly with the section Renicarpus to which O.
arborea and O. pulchra belong.
* Forms part of a M.Sc. thesis submitted at the University
of Pretoria.
t Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria.
BUDS AND GROWTH PATTERN
Two interesting features regarding the growth
pattern of the Ochnaceae were observed that have
hitherto escaped notice. The first is the two different
kinds of buds encountered, and the second, the
growth pattern. The first type of bud found in the
family is responsible for the annual growth increment.
The growth buds are laterally compressed and taper
to a sharp point (Fig. 3). The second type of bud is
the flower bud of which two kinds are found. Species
where the flowers are borne singly have easily recog-
nizable pear-shaped and globose buds (Fig. 4). Where
the flowers are borne in clusters or cymes the buds
are produced in a club-shaped structure, similar to the
growth buds (Fig. 5).
Fig. 1.— The smooth, peeling bark of Ochna pulchra .
206
MORPHOLOGICAL STUDIES OF THE OCHNACEAE
Fig. 4. — The single flower buds of Ochna serrulata.
Fig. 5. — The club-shaped compound flo ver bud of Ochna
pulchra.
P. C. V. DU TOIT
207
Fig. 6. — The cyme of Ochna
pulchra; note the two rows of
boat-shaped scales.
Both the growth buds and the compound flower
buds are protected by a series of scales. The scales
are arranged in alternating series. One large serrated
or entire scale, covering the axillary bud. On the
opposite side of the stem, the space between the two
margins of the large scale is covered by a lanceolate
or subuliform scale, which seems to be homologous to
the two stipules of the foliage leaves.
At the end of the growing season, the flower and
leaf buds are already fully developed and open
(unfold) with the first spring rains of the following
season. In both the growth and flowering buds, a
typical feature of the Ochnaceae is displayed, viz. the
growthflush, which takes place in early spring when
the temperature rises and just after the first spring
rains. During the growthflush the scales break away
in two or three series and the stem and peduncle
elongates (Fig. 6). The scales mostly break away in
two series due to their pseudo-distichous arrangement.
The angle of divergence is approximately 150°, but
due to the stem being twisted, the leaves and scales
take on the appearance of being distichous. The
spirally arranged nature of the leaves can be seen
when the young leaves unfold. During the growth-
flush, which lasts for approximately a week, the
annual growth increment of the plant is completed
and the axillary buds of most species are quiescent
for the rest of the growing season. The annual growth
increment can be recognized by the amount of new
growth between the series of scale scars at the tip of
the previous season’s stems and the growth bud. The
quiescent axillary buds in the series of scale scars give
rise to the flower buds and/or sideshoots of the
following season. In some species stems may also be
terminated by flowers.
LEAVES AND STIPULES
The family Ochnaceae in Southern Africa is
represented by two genera, viz. Ochna and Bracken-
ridgea. In distinguishing between these two major
taxa, the morphology of the leaves and stipules was
found to be taxonomically useful. According to
10mm
Fig. 7. — Diagram to illustrate the stipules of A, Ochna and B,
Brackenridgea.
208
MORPHOLOGICAL STUDIES OF THE OCHNACEAE
Fig. 8. — Diagram to illustrate the
types of veins in A, Ochna
and B, Brackenridgea. PV — -
Primary-vein; SV — Seconda-
ry-vein. Arrows point to the
angle of emergence of the
different veins.
Sinnott and Bailey (1914), there is a relationship
between the occurrence of stipules and the dentations
on the leaf margins. In the indigenous species of the
Ochnaceae, the leaf margin is excurrent onto the
adaxial side of the petiole and joined to the stipules.
In these instances the stipules can then be regarded
as the most basally situated teeth of the leaf margin.
In all the species of Ochna the stipules are caducous,
especially in Ochna pulchra , in which the stipules are
shed just after the growthflush and the teeth of the
leaf margin are deciduous with age. The stipules are
lanceolate to spathulate, undivided and entire (Fig.
7A). The stipules of Brackenridgea remain on the
plant for the whole growing season, and are divided
into a number of linear lobes, which may be entire or
dentate (Fig. 7B).
The venation is a useful taxonomic character and
the veins can be divided into primary and secondary
veins (Fig. 8). The primary veins are conspicuously
prominent on the adaxial surface, with the secondary
veins less so. In the case of most of the Ochna species
both the primary and secondary veins arise from the
midrib at an angle of 60°-70°. The veins run parallel
to one another with the secondary veins gradually
lessening in diameter until they disappear. The primary
veins run to the leaf margin, turning distally with
their diameter gradually lessening (Fig. 8A). In the
case of Brackenridgea arenaria and O. confusa, the
primary veins arise from the midrib, at an angle of
30°-40°, with the primary veins anastomosing near
the distal end of the leaf. The secondary veins arise
from the midrib at an angle of 60°-70° and run
parallel to one another, gradually lessening in
diameter until they end at the primary veins (Fig. 8B).
UITTREKSEL
Die oorsaak van die kenmerkende wyse waarop
die bas van sommige Ochna soorte afdop, asook die
morfologie van die groeiknoppe, loofblare en steun-
blare word bespreek. Die taksonomiese toepaslikheid
van die eienskappe word aangedni waar ter sake.
REFERENCES
Esau, K., 1965. Plant anatomy. 338-350. New York: John Wiley
and Son.
Sinnott, E. W. & Bailey, I. W., 1914. Investigations on the
phylogeny of the Angiosperms. Am. J. Bot. 1,9: 441-453.
Bothalia 12,2: 209—213 (1977)
Leaf anatomy of the South African Danthonieae (Poaceae).
I. The genus Dregeochloa
R. P. ELLIS*
ABSTRACT
The anatomical structure of the leaf blade as seen in transverse section, and the abaxial epidermis of
Dregeochloa pumila and D. calviniensis is described and illustrated. A generic description is included and the
relationships of the genus are briefly discussed.
RESUME
ANATOMIE DE LA FEUILLE DES DANTHONIEAE ( POACEAE ) SUD-AFR/CAINES I LE
GENRE DREGEOCHLOA
La structure anatomique du limbe foliaire vu en coupe transversale, ainsi que Vepiderme abaxial
de Dregeochloa pumila et de D.calviniensis son t decrits et il/ustres. On y joint une description du
genre avec une breve discussion de ses relations.
INTRODUCTION
The genus Dregeochloa Conert was described to
accommodate the species Danthonia pumila Nees and
a newly described species Dregeochloa calviniensis
Conert (Conert, 1966). These two species have certain
distinct characteristics of spikelet morphology, leaf
anatomy and especially the structure of the mature
caryopsis, which indicates that this genus occupies a
unique and somewhat isolated position in the Dantho-
nieae. Plants of the genus were previously assigned to
the genus Danthonia DC. (Chippindall, 1955), and
certain authors (De Wet, 1954, 1956; Jacques-Felix,
1962) have suggested their inclusion in Asthenatherum
Nevski. However, they can readily be distinguished
from both genera by the development of the leaves,
the insertion of the central awn and the structure of the
caryopsis (Conert, 1966). In addition, these species
exhibit characteristic leaf anatomy which tends to
confirm their placement together in a separate genus,
but throws little light on the phylogenetic position of
this genus. In the anatomical descriptions which
follow, the following abbreviations will be used:
vb/s — vascular bundle/s
l 'vb/s — first order vascular bundle/s
2'vb/s — second order vascular bundle/s
3'vb/s — third order vascular bundle/s
ibs — inner bundle sheath; mestome sheath
obs — outer bundle sheath; parenchyma sheath
ANATOMICAL DESCRIPTION OF THE GENUS
DREGEOCHLOA
Leaf in transverse section
Leaf outline : U-shaped or canaliculate with two halves
of lamina curved upwards to varying degrees on either
side of median vascular bundle; forming no angle.
Leaves narrow (between 1 , 60 mm and 3 , 50 mm wide),
proportionately very thick (between 0,30 mm and
0,70 mm). Ribs and furrows ; adaxial furrows present
between all vbs; equally sized, rounded, adaxial ribs
present over all vbs irrespective of order. Abaxial ribs
and furrows well developed; furrows equal to or
deeper than adaxial furrows; ribs in form of flat-
topped sclerenchyma caps with horizontal prickles at
edges interlocking over cleft-like furrow. Median
vascular bundle: present; midrib or keel not developed.
Vascular bundle arrangement: 5 1 vbs in blade;
* Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria.
no 2'vbs present; all bundles located nearer abaxial
surface. Vascular bundle structure: all bundles usually
rounded in section although D. pumila exhibits a
tendency for bundles to be vertically elongated and
elliptical; phloem of l'vbs adjoins inner, thickened
sheath; no lysigenous cavity or protoxylem vessels
developed; metaxylem vessels extremely narrow
(diameter less than adaxial ibs cells), angular and only
slightly thickened. Vascular bundle sheaths: round in
shape in all 3'vbs and most l'vbs, but in D. pumila
l'vb sheaths may be slightly elliptical. Obs always
entire with no extensions; comprised of 11-15 cells
around 3'vbs and 12-17 cells around l'vbs; all cells
similar in shape, thin-walled and conspicuous but
not larger than mesophyll cells. Sclerenchyma:
abaxial strands well developed in wide, straight, deep
bands forming caps on flat abaxial ribs; no scleren-
chyma between vbs; fibres thick-walled with lumen
narrow; walls stain blue-green with safranin and fast
green. Margin: sclerenchyma a well developed cap,
somewhat pointed; crescent-shaped or fibres may
extend abaxially. Sclerenchyma of margin never
extends further than directly above and below ultimate
vb. Margin without angular prickles. Mesophyll:
indistinctly radiate; chlorenchyma of elongated,
tabular cells relatively loosely and irregularly
arranged; air spaces frequent. Colourless cells: entirely
lacking except for bulliform cells. Adaxial epidermis:
costal prickle hairs with bases not larger than, and
situated between, normal epidermal cells; frequent;
hairs slender and elongated, those of D. pumila
(±0,10 mm) about twice the length of those of
D. calviniensis (±0,05 mm); no papillae. Abaxial
epidermis: outer tangential wall of cells flattened or
slightly arched; not papillose.
Abaxial epidermis
Intercostal zones: cleft-like, intercostal, abaxial
furrows make study and illustration of cells of this
zone difficult. Intercostal long cells: length slightly
greater than width; parallel-sided; moderate undula-
tions of anticlinal walls. Stomata: appear low-dome
shaped; 1-2 rows on each vertical wall of cleft-like
furrow. Papillae: absent. Prickle-hairs: interlocking
prickles present overlying stomatal furrow; single row
of prickles on edge of costal zones. Micro-hairs:
none observed. Macro-hairs: absent. Silica-bodies:
present throughout costal zone; silica cells alternate
with costal short cells.
210 LEAF ANATOMY OF THE SOUTH AFRICAN D ANTHONIE AE (POACEAE). I. THE GENUS DREGEOCHLOA
ANATOMICAL DESCRIPTIONS OF THE SPECIES
1. Dregeochloa pumila (Nees) Conert
Leaf in transverse section
Leaf outline: U-shaped leaves with base and sides
about equal in length or more commonly less inrolled
with wide, broad base to U. Width from 3,00 mm to
3,45 mm and thickness from 0,63 mm to 0,70 mm in
freshly fixed leaves. Dried herbarium specimens
narrower (2,00 mm wide) and thinner (0,30 mm
thick). Ribs and furrows: adaxial furrows very shallow
relative to leaf thickness; furrows narrow and cleft-
like in sections from dried herbarium material but
with broad bases with relatively steep sides in freshly
fixed material. Abaxial ribs taller than adaxial ribs;
interlocking prickles well-developed and common.
Vascular bundle arrangement : 1 ' vbs separated by
single 3'vb except on either side of median vascular
bundle where there are two 3 'vbs. Vascular bundle
structure: 3'vb diameter almost same as l'vbs.
Vascular bundle sheaths: obs cells rounded or with
radial walls straight and tangential walls inflated;
translucent, without chloroplasts or with few chloro-
plasts similar to those of mesophyll. Ibs not distinct
around 3 'vbs; probably absent; present around l'vbs;
entire, composed of small thickened cells; thickening
may be on inner tangential and radial walls or equally
on all walls when lumen may become more or less
excluded. Adaxial cells of ibs larger than lateral cells;
relatively thin walled. Adaxial sclerenchyma: small
strands developed; shallow sub-epidermal strip or
deeper groups of fibres. Strands similar in size over
all vbs. Mesophyll : indistinctly radiate with chloren-
chyma surrounding each individual bundle divided
by abaxial furrows and large adaxial bulliform cells.
Adaxial chlorenchyma groups narrow and composed
of palisade-like cells between adjacent bulliform cell
groups. Adaxial epidermis: bulliform cells resemble
fan-shaped groups with exceptionally large central
cell with straight sides occupying more than \ the leaf
thickness. Costal epidermal cells unthickened or with
thin cuticle. Abaxial epidermis: bulliform cells small,
in fan-shaped groups situated at base of furrows;
largest bulliform cell not larger than obs cells. Costal
epidermal cells with outer wall slightly thickened.
Located on sides of adaxial ribs are horizontally
projecting prickles with bases not larger than, and
situated between normal epidermal cells; barbs thick
and relatively very long (0, 10 mm), interlocking over
furrows.
Abaxial epidermis
Prickles: short, hook-like base; barb long (±0,10
mm); barb developed from apex of base; barbs lie at
right-angles across abaxial furrows. Silica bodies:
Round, circular to oblong in shape; sometimes shortly
dumb-bell shaped with a wide middle portion (Fig. 8).
Specimens examined
S.W.A. — 2615 (Luderitz): 1,6 km south of Luderitz lagoon
(-CA), Giess & van Vuuren 653. 2715 (Bogenfels): Pomona
(-AB), Din ter 4018.
Cape. — 2816 (Oranjemund): 2 km west of Beauvallon on road
to Alexander Bay (-DA), Ellis 2173, 2174: 9 km west of Beau-
vallon, Tolken 5278.
Discussion
D. pumila is a short (3-10 cm tall), tufted perennial,
often forming small, dense, flat cushions up to 15 cm
in diameter. It grows in crevices or in loose sand
amongst shale-like, schist rocks in a region of extre-
mely low winter rainfall (±50,0 mm), but where
heavy sea mists occur frequently. It appears to be
restricted to the coastal belt, less than 1 5 km from the
sea, from just south of the Orange River mouth to the
Luderitz area in South West Africa (Fig. 13).
This region undoubtedly is a harsh habitat with
extremes of temperature, insolation and precipitation.
The proximity to the sea has a moderating effect on
seasonal temperature range and frequent mists
probably offset the lack of rainfall somewhat, but an
extremely large diurnal temperature range is to be
anticipated on the dark rocks which this plant prefers.
However, xerophytic adaptions are not well reflected
in the anatomy of the leaf of D. pumila. The leaf is
not permanently infolded and the usual copious
sclerenchyma and thickened cuticle, often correlated
with dry localities, is lacking (Figs. 1 and 2). The
stomata are, however, restricted to abaxial furrows
which are further protected by numerous interlocking
prickles. This arrangement must limit excessive water
loss to a certain degree. In addition the leaves are
very short with a leathery, succulent texture and the
plant forms a low, dense cushion. These growth
characteristics are commonly found in xerophytes but
are exceptional in the Poaceae.
No other members of the Danthonieae are found
in the same habitat as D. pumila although Asthena-
therum glaucum (Nees) Nevski and Merxmuellera
rangei (Pilg) Conert are found in the adjoining sandy
areas but they extend further into Namaqualand, the
Namib Desert and even the Kalahari in the case of
A. glaucum. Anatomically these species are easily
seperated.
Sections taken from herbarium specimens have a
somewhat more xerophytic appearance. The adaxial
and abaxial furrows are more narrow and cleft-like
and the bulliform cells appear reduced in size. In fact,
these specimens superficially resemble D. calviniensis
sections (of which only herbarium material was
studied) more closely than fully turgid, freshly fixed
specimens of D. pumila. This should serve as a caution
when anatomical comparisons are made between
sections of herbarium and fresh material. Thus, Dinter
4018 (Fig. 1) resembles the sections of D. calviniensis
(Figs. 9 and 10) and it is only the sequence of the
different orders of vascular bundle and the silica
bodies and prickle hairs (Figs. 5 and 6) of the
epidermis that reveal it to be a typical D. pumila
specimen.
Remarkably little variation in leaf anatomy was
evident in the specimens studied which may be
expected from a species inhabiting a limited area with
uniform climate, and occupying such a specialized
niche. This species can readily be recognised by the
elongated, deep bulliform cells associated with narrow
columns of adaxial chlorenchyma cells, the thickness
of the leaf and the abaxial furrows with interlocking
prickles.
2. Dregeochloa calviniensis Conert
Leaf in transverse section
Leaf outline: U-shaped with base and sides equal
in length to hollow cylindrical condition where
margins almost meet. Generally more tightly inrolled
than D. pumila; width from 1 ,60 mm to 2,30 mm in
dried material. Ribs and furrows: adaxial furrows of
medium depth and at least \ of leaf thickness. (This
greater depth may be due to shrinkage in the herba-
rium material examined). Furrows narrow, cleft-like.
Adaxial ribs same height as abaxial ribs although
shaped differently; not moniliform; interlocking
prickles small and infrequent. Vascular bundle
arrangement : one 3'vb on either side of the median
R. P. ELLIS
2)1
Figs 1 & 2. — Dregeochloa pumila: transverse sections of the leaf blade; 1, Dinter 4018; 2, Ellis 2174.
Figs 3-8.— Dregeochloa pumila: abaxial epidermis; 3 & 4, Ellis 2173; 5 & 6, Dinter 4018; 7 & 8, Giess & Van Vuuren 653.
212 LEAF ANATOMY OF THE SOUTH AFRICAN DANTHONIEAE (POACEAE). I. THE GENUS DREGEOCHLOA
Figs 9-12. — Dregeochloa calviniensis. 9 & 10, transverse sections of the leaf blade; 11 & 12, abaxial epidermis. 9, Erasmus s.n.; 10
11 & 12, Dekkers s.n.
vascular bundle; lateral two l'vbs adjacent to one
another with no 3'vbs present between them. Vascular
bundle sheath: obs cells inflated and rounded; chloro-
plasts appear specialized and concentrated near inner
tangential wall (Figs. 9 and 10). (This observation
needs confirmation using freshly fixed material).
Ibs well developed and distinct around both 1' and
3'vbs, complete, composed of small thickened cells
often with inner tangential and radial walls markedly
thickened. Around l'vbs the walls of cells adjacent
to the phloem very thick with narrow lumen. Adaxial
cells of ibs larger than lateral cells of sheath. Adaxial
sclerenchyma: well developed strand; usually arched
following shape of rib; similar over all vascular
bundles. Mesophyll: indistinctly radiate with the
chlorenchyma surrounding each individual bundle
being divided by abaxial and adaxial furrows.
Adaxial epidermis: bulliform cells appear absent,
or small and present on sides and bases of~
furrows (Fig. 10). Costal epidermal cells all with
outer wall slightly thickened. Abaxial epidermis:
bulliform cells absent or only very small; situated on
the sides and bases of furrows. Costal epidermal cells
with distinct, thick cuticle on outer wall; thickness of
cuticle and outer wall being equal to, or greater, than
depth of epidermal cell. Interlocking prickles with
very short barbs at sides of costal zones.
Abaxial epidermis
Prickles: short, hook-like base; barbs short (±0,05
mm), developed from apex of base; all barbs point
irregularly in direction of leaf apex. Silica-bodies :
Tall and narrow to square; outline smooth, regular
(Fig. 12).
Specimens examined
Cape. — 3019 (Loriesfontein): Handelkraal, E.N.E. of Lories-
fontein (-CD), Dekkers s.n. (PRE, iso). 3022 (Carnarvon):
Brandewynskuii, between Vosburg and van Wyksvlei (-DB),
Erasmus s.n.
Fig. 13. — Distribution of Dregeochloa pumila and D. calviniensis
compiled from specimens at the National Herbarium,
Pretoria (PRE). X indicates localities of specimens studied
anatomically.
Discussion
This rare, perennial species is known only from the
above two localities and collections. At Handelkraal,
on the margin of the Western Mountain Karroo, it
is locally frequent on limestone. In contrast to
D. pumila , this species forms small, dark green, dense
and erect tufts from 15-25 cm high.
Vegetatively D. calviniensis bears little resemblance
to D. pumila, but the leaf anatomy is strikingly
similar as seen in transverse section. Small differences
occur in the shape and size of the bulliform cells
(this may have been accentuated by the fact that only
herbarium specimens were studied), the size and thick-
ening of the epidermal cells and the prickles and
possibly the arrangement of the different orders of
R. P. ELLIS
213
vascular bundles. The abaxial epidermis, however,
shows important differences, especially in the shape
of the silica bodies. Although D. calviniensis has tall
and narrow silica bodies (Fig. 12) and D. pumila
circular or oblong bodies (Figs. 4 and 6), both these
shapes, and the fact that the silica cells and short
cells are solitary or paired, and not in long rows, are
typical festucoid characters (Metcalfe, 1960). This
difference, although striking, can thus be expected
even in two closely related taxa.
There appears to be a specialization and a centri-
petal concentration of chloroplasts in the parenchyma
sheath cells of both D. calviniensis specimens examined
(Figs. 9 and 10) and it is unfortunate that no fresh
material was obtained to confirm this. In addition, the
mesophyll, which is also poorly preserved, appears to
consist of two layers of more or less radially arranged
chlorenchyma cells. This configuration is typical of
the Kranz syndrome but the 12C/13C ratios are
typical non-Kranz (<5=-26, 32; Dekkers s.n.) as are
those for D. pumila (<5=-25, 93; de Winter & Giess
6235). The possibility that D. calviniensis represents
a very early stage in the aquisition (or late stage in
the loss) of the Kranz syndrome still exists, and this
warrants further investigation. If this is in fact the
case then the relationship of Dregeochloa to Asthena-
therum — a Kranz genus in the Danthonieae — becomes
much clearer.
DISCUSSION AND CONCLUSIONS
In the past the leaf anatomy of this genus has, to
a large extent, been misinterpreted. Thus, de Wet
(1954) grouped D. pumila with the species now inclu-
ded in the genus Asthenatherum — all of which have
“chloroplasts localized around the bundles.” This,
together with morphological criteria, he interpreted
as indicating that D. pumila belonged to the genus
Asthenatherum. Jacques-Felix (1962) stated that D.
pumila had typical panicoid structure and also included
this species with Asthenatherum. Conert (1962) noted
that D. pumila did not have elongated radially
arranged mesophyll cells. His observations led him to
disagree with the above authors and he suggested
that D. pumila occupied an isolated position in the
Danthonieae near Danthonia.
In a later paper, de Wet (1960) grouped D. pumila
with those species where the chlorophyll is not loca-
lised around the bundles but uniformly distributed
throughout the mesophyll and which possess a thin-
walled outer bundle sheath. These new observations
led him to postulate that D. pumila formed a direct
link between Danthonia and Asthenatherum. He was
still of the opinion that in all other respects these
two genera resembled one another very closely but
Conert (1962) noted that the formation of the callus
differed in addition to anatomical differences. This
influenced Conert’s (1962) proposal of an isolated
position for Dregeochloa ( =D . pumila ).
Certain epidermal features have also been confused.
De Wet (1954) described the silica bodies of D. pumila
as being spherical and stated that micro-hairs were
absent. In the 1960 publication de Wet described the
silica bodies as dumbell-shaped and micro-hairs were
observed. In the present study no micro-hairs were
found but it must be stressed that, in this genus, the
intercostal zones are difficult to preserve and study
due to the deep adaxial furrows. On all preparations of
D. pumila the silica bodies are horizontally elongated
and oblong in shape although some silica bodies on
Giess and van Vuuren 653 (Fig. 8) have indentations
in the centre and could be described as being dumbell-
shaped.
The observations of this study, based solely on leaf
anatomy, confirm that these two species closely
resemble one another and constitute a unique, dis-
tinct group. Their structure is unique amongst the
Danthonieae and they show little anatomical resem-
blance to any other South African members of this
tribe. This supports Conert’s (1966; 1971) conclusions
that this genus occupies an isolated position within
the tribe. However, Dregeochloa has certain similari-
ties in common with Asthenatherum (abaxial fur-
rows and prickles, spikelet structure and distribution)
which may indicate that these two genera had a com-
mon ancestor which gave rise to Kranz and non-
Kranz groups. The region where these genera occur
is a zone where Kranz genera ( Aristida , Stipagrostis,
Eragrostis etc.) and non-Kranz genera ( Schismus ,
Karoochloa, Chaetobromus and Merxmuellera ) are
equally abundant. Dregeochloa shows no anatomical
affinities with the genus Merxmuellera {— Danthonia )
and its removal from Danthonia appears justified.
ACKNOWLEDGEMENTS
The author is indebted to Miss L. Breytenbach
and Miss A. Vermeulen for capable technical assis-
tance and to Dr J. Vogel and Mrs M. Greyling of the
Natural Isotopes Division, N.P.R.L., C.S.I.R. for
the 13C/12C determinations.
U/TTREKSEL
Die anatomiese struktuur van die blaar in dwarssnee
en die abaxiale epidermis van Dregeochloa pumila en
D. calviniensis word beskryf en geillustreer. 'n Genus
beskrywing is ingesluit en die verwantskappe van die
genus word kortliks bespreek.
REFERENCES
Chippindall, L.K.A., 1955. In Meredith, The grasses and
pastures of South Africa. Johannesburg: C.N.A.
Conert, H. J., 1962. Uber die Gramineen-Gattung Asthena-
therum Nevski. Senckenberg Biol. 43:239-266.
Conert, H. J., 1966. Dregeochloa, eine neue Gattung der
Gramineen. Senckenberg Biol. 47:335-343.
Conert, H. J., 1971. The genus Danthonia in Africa. Mitt. Bot.
Staatssamml. MiXnchen. 10:299-308.
De Wet, J. M. J., 1954. The genus Danthonia in grass phylogeny.
Am. J. Bot. 41:204-211.
De Wet, J. M. J., 1956. Leaf anatomy and phylogeny in the tribe
Danthonieae. Am. J. Bot. 43:175-182.
De Wet, J. M. J., 1960. Leaf anatomy and morphology in
South African species of Danthonia. Bothalia 7:303-310.
Jacques-Felix, H., 1962. Les Graminees d’ Afrique Tropicale.
I. Generalites, Classification, Description des Genres.
Inst, de Recherches Agronomiques Tropicales et des Cultures
Vivrieres, Paris. 1-345.
Metcalfe, C. R., 1960. Anatomy of the Monocotyledons. I.
Gramineae. Oxford: Clarendon Press.
Bothalia 12,2: 215-221 (1977)
Cytogenetic studies in the Eragrostis curvula Complex
T. B. VORSTER* and H. LIEBENBERGf
ABSTRACT
Cytogenetic studies were undertaken in the Eragrostis curvula Complex. Three plants were studied at each
of 16 collecting points. The overall morphology and embryo sac development of all plants were evaluated, while
the chromosome number and microsporogenesis of some of the plants were also studied. The collecting points
were chosen so ^s to represent a variable environment extending from the bushveid to the highveld regions of
the Transvaal. It was found that the embryo sac development of the plants from the bushveid and the highveld
were, for all practical purposes, obligate diplosporic apomicts, whereas the transition area contained obligate as
well as facultative diplosporic apomicts. The same pattern also held as far as the plant morphology, chromosome
number and microsporogenesis were concerned.
RESUME
ETUDES CYTOGENETIQUES DANS LE COMPLEXE ERAGROSTIS CURVULA
Des etudes cytogenetiques out ete entreprises dans le complexe Eragrostis curvula. Trois plants
ont ete etudies pour chacun des 17 points de recolte. La morphologic generate et le developpement du
sac embryonnaire ont ete evalues partout, tandis que le nombre chromosomique et la microsporogenese
de certains plants ont aussi ete etudies. Les points de recolte ont ete choisis de maniere d representer
un milieu variable s'etendant des steppes boisees ("bushveid") aux prairies de montagnes ("highveld")
du Transvaal. On a constate que, dans les steppes comme dans les prairies, le developpemcnt du sac
embryonnaire comporte obligatoirement line apomixie diplosporique, pour tout ce qtT on pent en obser-
ver; tandis que les zones de transition presentent aussi bien des apomictes diplosporiques obligatoires
que des facultatifs. La me me distribution s'observe aussi en ce qui concerne la morphologic de la plante,
le nombre chromosomique et la microsporogenese.
INTRODUCTION
Cytogenetic studies on E. curvula (Schrad.) Nees
and its close relatives have made it clear that they are
probably all part of a large agamic complex. The
mechanism of apomixis is diplospory, as defined by
Gustafsson (1946), followed by parthenogenesis
(Hakansson, 1943) and pseudogamy as the main
means of reproduction (Brown and Emery, 1958;
Liebenberg, 1961; Liebenberg and Pienaar, 1962;
Streetman, 1963; Voight, 1971; Voight and Bashaw,
1972 and Brix, 1974). This is probably the reason
why the taxonomy of this complex has been so
difficult to unravel.
The E. curvula group has a wide distribution
throughout Southern Africa and the existence of
polymorphism within species and intermediate types
between species led De Winter (1955) to treat E.
robusta Stent as a synonym of E. curvula and to
maintain E. chloromelas Steud. as a closely related
species in what is generally known as the E. curvula
Complex.
Unfortunately most of the cytogenetic studies
undertaken on E. curvula and its relatives have been
carried out, for understandable reasons, on those
sections of the complex that are economically
important in pasture breeding. Inevitably these
sections might well comprise robust-growing high
polyploid apomicts. This has created the impression
that the complex was an old one consisting of mostly
obligate apomicts.
It was considered therefore that cytogenetic studies
(especially embryo sac studies) of a naturally growing
and unselected E. curvula Complex population might
be well worth studying in an attempt to elucidate
this problem.
MATERIAL
A region was selected in the Transvaal (South
Africa), which included highveld, a transition area and
lower bushveid. Seventeen collecting points were
* Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria,
t Department of Genetics, University of Pretoria.
selected with three collections at each point in order
to evaluate variation among as well as within
collecting points over a reasonably varied area
(Fig. 1).
Collecting points were selected at regular intervals
on the lower bushveid and highveld, while those over
the transition area were selected (with the help of
Fig. 2) so that the bottom, slopes and summits of
ridges would be included.
Herbarium specimens of each collection were
made and identified at the National Herbarium in
Pretoria, where they are now housed (Table 1).
It was decided that a minimum of fifty embryo sacs
should be investigated for every plant. Additional
embryo sacs of a specific plant were thus sectioned or
new plants were collected when this number was not
available from the collected material. More plants
were therefore collected than were actually used in
the study. All plants collected are reflected in Table 1
and given herbarium numbers. Those plants used
in this study were, however, given additional numbers
(Plant Numbers — Table 1) to identify those plants
originating from one collecting point.
METHODS
The inflorescences for microtome studies were
fixed in Navashin fixative (Stockholm modification —
Maheshwari, 1939). Inbedding and staining techniques
outline in Johansen (1940) were followed using
Heidenheins Haematoxylin as nuclear stain and
Orange G as counter stain.
The propionic carmine squash method of Pienaar
(1955) was slightly modified for the study of micro-
sporogenesis and chromosome numbers.
RESULTS
Although the study of embryo sac development was
the main object ot the present work, micro-
sporogenesis and chromosome numbers were also
investigated as far as possible. One big problem was,
that by the time that microsporogenesis could be
investigated (only after the embryo sacs were studied),
the material had been left in the fixative too long.
HEIGHT ABOVE SEA LEVEL IN METRES
216
CYTOGENETIC STUDIES IN THE ERAGROSTIS CURVULA COMPLEX
JOHANNESBURG
Fig. 1. — Map of the roads between Brits and Johannesburg indicating the collecting points A to Q as well as the distance
kilometres between them; collecting points A to E are defined as the lower bushveld. F to M as the transition area and N to
as the highveld.
DISTANCE IN KILOMETRES
Fig. 2. — A graph indicating the collecting points with regard to the height above sea level and distance.
05'
T. B. VORSTER AND H. LIEBENBERG
217
Fig. 3. — Microsporogenesis stages of some of the collections. A: Diakineses of a rather “regular”
tetraploid with a few distinct heteromorphic bivalents (H) -collection L-3. B: Anaphase I of a rather “regular”
hexaploid -collection H-2. C: Anaphase I of a rather “regular” hexaploid (two laggards with one undergoing
chromatid segregation) as well as one paracentric inversion bridge (P) -collection J-l. D: Anaphase I of a very
abnormal hexaploid (approximately 12 laggards, some of them undergoing chromatid segregation, can be
seen) -collection G-3.
218
CYTOGENETIC STUDIES IN THE ERAGROSTIS CURVULA COMPLEX
Because of the small and compact spikelets of
Eragrostis, fixative penetration is poor with the result
that the material deteriorates soon after fixation.
Analyses were made of the number of monovalents
and laggards during metaphase I and anaphase I
respectively and are recorded with the chromosome
numbers in Table 2. The quality of the slides did not
permit multivalent or any other more complex
analyses.
Paracentric inversion bridges (Fig. 3C) were also
encountered in collections C-2, C-3, H-3 and J-l.
These bridges, however, occurred at a very low
frequency (except for plant J-l which had chromatid
bridges in 16% of the anaphase I cells studied). Apart
from indicating that the polyploids are probably
segmental-allopolyploids, this information was con-
sidered too scanty to be of any further use. Another
phenomenon that was conspicuous in a few
collections, e.g. L-3, and that would support the
segmental-allopolyploid nature of the plants was
the occurrence of heteromorphic bivalents, where
one chromosome was much larger than its partner
(Fig. 3A).
The meiotic analysis showed that plants with low
chromosome numbers tend to have “regular” meioses,
whereas higher polyploids were inclined to have
abnormal meioses although some variation occurred.
A few groups could roughly be distinguished as
regard chromosome number, microsporogenesis
abnormalities and the locality from whence they came:
(1) Hexaploids with abnormal meisoses (all these
plants are from the lower bushveld and the
beginning of the transition area) (Fig. 3D).
(2) Hexaploids with rather “regular” meioses (these
plants are from the transition area and the
beginning of the highveld) (Fig. 3B).
(3) An octoploid with a relative “regular” meiosis
(from the transition area).
(4) A pentaploid with, as expected, a very abnormal
meiosis (from the transition area).
(5) Two tetraploids with relatively “regular”
meioses (from the transition area).
A total of 3 902 embryo sacs was examined and the
results are summarized in Table 1. It was found that
3 306 of these embryo sacs were apomictic by means
of diplospory followed by parthenogenesis and
pseudogamy while 99 were sexual monosporic Poly-
gonum type (Maheshwari, 1950) embryo sacs. One
hundred and nineteen embryo sacs were abnormal or
divergent, while 378 were degenerated (Table 1).
DISCUSSION
Four factors were considered in attempting to
evaluate the natural variation in the E. curvula
Complex in the area of this study.
1 . Morphological variation in collected material
It was quite striking that only true E. curvula was
collected on the lower bushveld as well as the high-
veld, while true E. curvula as well as types which
could not be judged as true were collected in the
transition area (Table 1).
All the E. chloromelas types (true and not true
types) were collected in the transition area. This
indicates a great deal of variation, not only between,
but also within collection points in the transition
area.
2. Variation in chromosome numbers
The E. curvula Complex has a wide range of
chromosome numbers, i.e. 2n=20, 40 and 60 (Pienaar,
1953) and 2n = 50 (De Wet, 1954) for E. curvula,
2n = 40 and 60-63 (Pienaar, 1953) for E. chloromelas
and 2n-=70 and 80 (Pienaar, 1953) for E. robusta.
In this study an additional number of 2n = 80 was
found for E. curvula in the transition area (Table 1,
plant H-3).
Although chromosome counts for only a few
plants were made, it is clear that the numbers in the
transition area are very variable (2n=40, 50, 60 and
80). The few plants in the lower bushveld and highveld,
which were studied in this respect, all had 60
chromosomes and, although it is risky to draw any
definite conclusions, it seems as if there might be a
greater chromosome number variation in the
transition area.
3. Variation in microsporogenesis
Table 2 shows clearly that the meioses of plants are
inclined to become more regular as the transition
area is approached from the lower bushveld. The
two hexaploids on the highveld have rather “regular”
meioses, but it would again be dangerous to draw
any conclusions as to the significance of this
phenomenon, because of the low number of plants
investigated.
4. Variation in embryo sac development
Considerable difficulty was at first experienced
with the classification of some of the sexual embryo
sacs and, because it was important to calculate the
exact degree of sexuality for every plant, this problem
has been attended to in some detail (Vorster &
Liebenberg, in press).
Sexual embryo sacs were sporadically found over
the whole sampling area but they occurred at a higher
frequency in the transition area (Table 1). Not only
was there variation in the embryo sac development
over the area as a whole, but also within collecting
points.
This occurrence of a high percentage sexuality and
obligate apomixis within one collecting point stresses
the discontinuous variation that occurs in the embryo
sac development of the complex.
CONCLUSIONS
The method used in this study to try and evaluate
the natural variation in embryo sac development in
a specific area, proved to be very satisfactory,
especially because it showed that previous studies
did not reflect a true picture of the occurrence of
sexuality in this complex. It would seem that the
group is far from being an old obligate agamic
complex. Since several specimens in the transitional
zone were E. chloromelas types and showed, together
with one E. curvula type, fairly high sexuality, it may
be that E. chloromelas is supplying the source of
sexuality in this area.
Sexual embryo sacs occurred most frequently in
the transition area. Microsporogenesis studies showed,
furthermore, that the meioses were inclined to
become more regular as the transition area was
approached from the lower bushveld, while the
transition area also contained plants with the most
variable morphology as well as the most variable
chromosome numbers.
From these results, one seems justified in expecting
that one or more of the original sexual ancestors of
this agamic complex may still be present in or near
the transition area (east or west from it) as sampled
by this study. According to Stebbins (1950) the
variation pattern in the Crepis Complex indicated
that in the vicinity of diploid sexual ancestors,
variable facultative apomicts occurred, whereas
obligate apomics with great morphological uniformity
T. B. VORSTER AND H. LIEBENBERG
219
TABLE 1. - Number and percentage embryo sac types found for the different specimens
220
CYTOGENETIC STUDIES IN THE ERAGROSTIS CURVULA COMPLEX
x
Diakinesis monovalents
T. B. VORSTER AND H. LIEBENBERG
221
were found far from them. The diploid E. curvula
reported by Pienaar (1953) as well as the diploid
sexual found by Voight (1971) in the variety conferta
lends further evidence that at least some of the diploid
sexual ancestors of the complex still exist.
In conclusion, it is clear from this study, however
limited its scope, that the E. curvula Complex is
inadequately known and understood. If any sense
is to be made out of its problematic morphological
variation pattern, it is clear that a complete cyto-
genetic study is called for. Such a study should
include all related types and even species, over as
much of their distribution area as possible. The
present authors have already begun this task and
it is hoped that in this way the relationships and
therefore the taxonomy of the complex will be
unravelled or at least better understood.
UITTREKSEL
Sitogenetiese studies is onderneem op die Eragrostis
curvula kompleks. Daar is drie plante by elk van die
17 versamelpunte geneem en bestudeer. Hierdie plante
is geevalueer ten opsigte van hul klassifikasie (morfo-
logie) en kiemsakontwikkeling. Sommige van die
plante se mikrosporogenese en chromosoomaantal kon
ook bestudeer word. Die versamelpunte is uitgekies
om 'n variabele omgewing, wat strek vanaf ft laer-
liggende bosveld na die hoeveld, te verteenwoordig.
Dit is gevind dat die kiemsakontwikkeling van die
plante afkomstig vanaf die laerliggende bosveld sowel
as die hoeveld vir alle praktiese doeleindes verpligte
diplosporiese apomikte is, terwyl die plante afkomstig
vanaf die oorgangsgebied verpligte sowel as fakultatiewe
diplosporiese apomikte opgelewer het. Dieselfde patroon
kon waargeneem word ten opsigte van die plantmorfolo-
gie, chromosoomaantal en mikrosporogenese .
REFERENCES
Brix, K., 1974. Sexual Reproduction in Eragrostis curvula
(Schrad.) Nees. J. Plant Breeding 71 : 25-32.
Brown, W. V. & Emery, W. H. P., 1958. Apomixis in the
Gramineae: Panicoideae. Amer. J. Bot. 45: 253-263.
De Wet, J. M. J., 1954. Chromosome numbers of a few South
African grasses. Cyto/ogia 19: 97-103.
De Winter, B., 1955. Eragrostis Beauv. In Meredith, Grasses
and pastures of South Africa. Johannesburg: Central News
Agency. 132-184.
Gustafsson, A., 1946. Apomixis in higher plants. I. The
mechanism of apomixis. Lunds. Univ. Arsskr. N.F. Avd.
„ 2. 42: 1-66.
Hakansson, A., 1943. Die Entwicklung des Embryosacks und
die Befruchtung bei Poaalpina. Hereditas 29: 25-61.
Johansen, D. A., 1940. Plant microtechnique. New York: Me
Graw-Hill.
Liebenberg, H., 1961. Apomiksie by Eragrostis en Themeda.
Ongepubliseerde M.Sc. verhandeling, Universiteit van
Stellenbosch.
Liebenberg, H. & Pienaar, R. de V., 1962. Apomiksie by
Eragrostis en Themeda. Verrigtinge van die 2de Kongres
van die Suid-Afrikaanse Genetiese Vereniging. 150-153.
Maheshwari, P., 1939. Recent advances in microtechnique. II.
The paraffin method Cytologia 10: 251-281.
Maheshwari, P., 1950. An introduction to the embryology of
the angio sperms. New York: Me Graw-Hill.
Pienaar, R. de V., 1953. Cyrological studies in some South
African species of the genus Eragrostis. Unpublished Ph.D.
thesis, University of the Witwatersrand.
Pienaar, R. de V., 1955. Combinations and variations of
techniques for improved chromosome studies in the Grami-
neae. J.S. Afr. Bot. 21 : 1-8.
Stebbins, G. L., 1950. Variation and evolution in plants. New
York: Columbia Univ. Press.
Streetman, L. J., 1963. Reproduction of the lovegrasses, the
genus Eragrostis , i.e. E. chloromelas Steud., E. curvula
(Schrad.) Nees, E. lehmanniana Nees and E. superba Peyr.
Wrightia 3 : 41-51.
Voight, P. W., 1971. Discovery of sexuality in Eragrostis
curvula (Schrad.) Nees. Crop Sci. 1 1 : 424—425.
Voight, P. W. & Bashaw, E. C., 1972. Apomixis and sexuality
in Eragrostis curvula. Crop Sci. 12: 843-847.
Bothalia 12,2: 223-224 (1977)
A note on the flowers of Halleria lucidci
C. H. STIRTON*
ABSTRACT
Studies of sunbirds {Cinnyris spp.) feeding on the nectar of flowers of Halleria lucida L. suggest that
partial protandry may be operative in the breeding system of this cauliflorous tree. Attention is drawn to
certain anomalies depicted in published botanical drawings. These anomalies are discussed in relation to the
sequential development of the androecium and gynoecium in live flowers. Colins colius , the speckled coly, is
reported to eat the fruits of Halleria lucida. This bird also feeds on nectar after piercing the base of the corolla
tube.
RESUME
NOTE SUR LES FLEURS D’HALLERIA LUCIDA
Des observations sur la consommation de nectar par des souimangas du genre Cinnyris ex ploitant
les fleurs rf’Halleria lucida L. suggerent qu'une protandrie partielle pent intervenir dans le systems
reproducteur de cet arbre cauliflore. On attire T attention sur certaines anomalies figurant dans des
dessins botaniques qui ont ete publies et on discute ces anomalies par rapport au developpement sequen-
tiel de Tandrocee et du gynecee dans des fleurs vivantes. Colius colius, la veuve tachetee, est signale
comme mangeant les fruits c/'Halleria lucida. Cet oiseau se nourrit egalement de nectar apres avoir
perce la base du tube de la corolle.
Halleria lucida L. is one of the few cauliflorous
trees in South Africa (Marloth, 1932). The massed
red tubular flowers are visited regularly by various
species of sunbirds ( Cinnyris ) and sugarbirds
( Anthobaphes ) and this has led to the belief that
pollination is ornithophilous (Marloth, 1932. Vogel,
1954). This note has arisen from observations of
Cinnyris spp. feeding on the flowers of a solitary tree
of H. lucida growing in the National Botanical
Gardens, Pretoria.
A close inspection of massed flower clusters revealed
that each cluster was composed of flowers at different
stages of development. Sequential dissections from
bud stages to fully mature flowers suggested that
partial protandry might operate as an outbreeding
mechanism. It was found that the didynamous
stamens expanded at different rates and that the
stigma was always below the lowest pair of these
stamens until their anthers had dehisced. This
sequential development is shown in Fig. 1. Prior to
the opening of the corolla lobes all four anthers
were held at the same level, even though the filaments
of the two pairs were adnate to the corolla tube at
different levels. Steps 1-5 in Fig. 1 show the emergence
of the anthers from the corolla mouth. The outer
pair of anthers (deepest inserted) developed faster
than the inner pair of anthers, so that by the time
the inner pair had dehisced the outer pair had
completely shed their pollen. The style expanded
rapidly once dehiscence of the inner pair of anthers
had begun and eventually either overtopped or
attained the level of the outer pair of anthers. It was
difficult to establish accurately the time of receptivity
of the stigma, but it appears to have occurred once
the stigma had reached the level of the inner pair of
dehisced anthers.
Any interpretations of the phenomenon discussed
above must be made cautiously for a number of
reasons. Firstly, different authors have commented
on different flower types in Halleria lucida and
secondly, different patterns of development have
been reported for the androecium and gynoecium.
Sims (1815), who commented on a rudimentary fifth
filament, compared this species to the genus Lonicera
(Caprifoliaceae) in which Burman (Rar. Afric. 244,
* Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria.
t. 89, fig. 2) had placed it. Verdoorn (1946) drew
attention to anomalous flowers and commented as
follows: “While the majority of flowers on this
shrub are funnel-shaped with an oblique, somewhat
2-lipped mouth, several were found to be trumpet-
shaped with the lobes equally spreading and 4 or 5
in number. In these examples the stamens were also
equally disposed and not unilateral.” Flowers observed
in Pretoria approximated those in t. 961, fig. 4
(Flow. PI. Afr., 1946) of Verdoorn’s article. No
abnormal flowers were found. Vogel (1954), however,
has commented that the stamens and stigma hardly
exsert from the corolla mouth and his Fig. 132: 4
closely approximates t. 961, fig. 8 described as an
abnormal flower by Verdoorn. It is difficult to assess
from these drawings, as well as from the t. 1744
(Bot. Mag. 41, 1815) described by Sims, whether the
relative position of anthers and stigma can be ascribed
to the artist having drawn flowers at different stages
of development. If the flowers drawn were indeed
mature, it must still be decided whether such flower
types are abnormalities or whether they are normal
and may possibly play an important role in the
pollination strategy of the plant. This will require
further field studies.
My assessment of partial protandry is derived
from the observations outlined above. If this is
correct, it would mean that a bird flying from flower
to flower could conceivably transfer pollen from a
flower with only one pair of anthers dehisced to a
flower in which the stigma was completely exerted.
This would constitute a measure of outbreeding if
more than one plant was involved. On the other
hand, the late emergence of the second pair of anthers,
with their dehiscence occurring as it does with the
elongation of the stigma, could guarantee inbreeding.
Limited emasculation and bagging studies of flower
clusters on the Pretoria plant indicated that autogamy
was operative.
An important feature of this cauliflorous tree is
that the flower clusters, consisting as they do of
flowers at all levels of development, ensure a constant
visitation over a long period by potential pollinators.
As Vogel (1954) has indicated, the flowers are rich
in nectar, but non-odoriferous. The fruits of this
plant are relished by the speckled coly, Colius colius,
which also pierces the base of the corolla tube to
feed on the nectar.
Fig. 1. — Sequential developmental stages of the flower of Halleria lucida once the corolla mouth has opened. 1, outer
pair of stamens beginning to emerge from mouth, note stigma well below inner pair of stamens; 2, outer pair of
stamens emerged from corolla mouth; 3, right hand anther of outer pair has begun dehiscence, while the inner
pair has begun to emerge; 4, and 5, the outer pair has dehisced, the inner pair has emerged, as has the stigma;
6, inner pair has dehisced; 7-9, the stigma gradually elongates until it reaches the upper pair of anthers or overtops
them.
An interesting feature of the dehisced anthers is
that they are completely flattened, with the pollen-
shedding surface facing downwards (i.e. towards the
viewers of Fig. 1). This provides a maximum surface
area to brush against any bird’s bill or tongue inserted
into the flower.
Detailed studies on a tree growing in the
Kirstenbosch Botanical Gardens in Cape Town gave
the same results as the studies carried out in Pretoria.
UITTREKSEL
Waarnemings op suikerbekkies (Cinnyris spp.) wat
op die nektar van blomme van Halleria lucida L. voed,
skep die indruk dat gedeeltelike protrandrie werksaam
mag wees in die voortplantingstelsel van hierdie boom,
waar die blomme op die stam gedra word. Aandag word
gevestig op sekere afwykings wat aangedui is in
gepubliseerde plantkundige tekeninge. Hierdie
afwykings word bespreek in verhouding tot die opeen-
volgende ontwikkeling van die androecium en gynoecium
in lewende blomme. Dit word berig dat Colius colius,
die gespikkelde muisvoel, die vrugte van Halleria lucida
eet. Hierdie voel voed ook op nektar nadat dit die basis
van die kroonbuis deurboor het.
REFERENCES
Marloth, R., 1932. The flora of South Africa. 3,1: 133-134,
t.35. Cape Town: Darter.
Sims, J., 1815. Halleria lucida L. Bot. Mag. 41 : 1. 1 744.
Verdoorn, I. C., 1946. Halleria lucida L. Flow. PI. Afr. 25:
t.96 1 .
Vogel, S., 1954. Bliitenbiologische Typen als Elemente der
Sippengliederung, pp. 67, 242. Jena: Veb. Gustav Fischer
Verlag.
Bothalia 12,2: 225-227 (1977)
The pollination of Cancivalia virosa by Xylocopid and
Magachilid bees
C. H. STIRTON*
ABSTRACT
The floral morphology of Canavalia virosa (Roxb). Wight & Arn. is discussed in relation to pollination by
Xylocopa flavorufa De Greer and Megachile combusta Sm. It was found that the relationship between size of
flower and bee influenced the type of pollinating strategy and its success. Bees smaller than M. combusta proved
ineffective pollinators.
RESUME
LA POLLINISA TION DE CANAVALIA VIROSA PAR LES ABEILLES XYLOCOPIDES ET
MEGA CHILI DES
La morphologie florale de Canavalia virosa (Roxb.) Wight & Arn. est discutee en rapport avec
sa pollinisation par Xylocopa flavorufa De Greer et Megachile combusta Sm. On a constate que la
relation entre dimensions de I'abeille et de la fleur influence la technique de pollinisation et son succes.
Des abeilles plus petites que M.combusta se sont averees inefficaces pour la pollinisation.
INTRODUCTION
Canavalia virosa (Roxb.) Wight & Arn. has been
commonly known in South Africa as Canavalia
ferruginea Piper. Although often confused with
C. ensiformis (L.) DC. and C. glochidiata (Jacq.) DC.,
it is usually kept separate (Sauer, 1964, Verdcourt,
1971). However, it has been recently suggested that
these three species may belong to one species. C.
ensiformis, which includes wild and cultivated types
(Westphal, 1974). The existence of this complex is
not surprising if one considers the widespread
cultivation of these plants in modern times as
vegetables, fodder and cover crops. C. virosa is used
here in the sense of Westphal (1974).
GEOGRAPHICAL DISTRIBUTION
C. virosa extends southwards from Arabia, Socotra
and India through tropical Africa into north-east
South Africa (Westphal 1974). Its distribution south
of the Limpopo River is shown in Fig. 1.
FLORAL MORPHOLOGY
The general morphology of C. virosa has been
adequately reviewed by Piper & Dunn (1922), Sauer
(1964), Verdcourt (1971), and Westphal (1974).
Piper et al. (1922) and Scott Elliot (1891) have written
generalized accounts of the structural relationships
of the various flower parts of C. maritima (Aubl.)
Thours. and C. ensiformis (L.) DC. respectively.
Vogel (1954) drew attention to analogies between the
flowers of C. maritima and Salvia africana L. and
also discussed pollination in both species. No account
appears to have been given of the pollination of
C. virosa. However, since, as Sauer (1964) has
commented, Canavalia spp. generally have mono-
tonous corollas and broad flowering schedules, it is
to be expected that the genus is probably minimally
adapted to specific pollinators. This implies that
pollination is similar in most cases.
The flower structure of C. virosa hardly differs
from the majority of known Canavalia spp. Flowers
are generally held in an upright position with the
standard facing downwards (e.g. Fig. 4 in Westphal,
1974). But, as Piper et al. (1922) pointed out, the
flowers are commonly inverted i.e. standard below
and facing upwards (e.g. Fig. 2 in Vogel, 1954). So
far only inverted flowers have been observed in the
* Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria.
Transvaal. A front view of such a flower is shown
in Fig. 2: 1. An outstanding feature of this flower
is the longitudinal bulging along the upper surfaces
of the two wings (arrowed in Fig. 2: 1). This feature
plays a prominent role in pollination and it is
surprising that very little attention has previously
been drawn to it. In Fig. 2: 2 and 3 the bulges are
arrowed relative to their position to the standard (S)
and keel (K). The two peglike callosities at the base
of the standard (S) rest on the portion of wing tissue
between the bulges and auricles of the wings.
The auricles of the wings articulate with the
standard at the point marked * in Fig. 2: 4. This
articulation allows the keel and wings of both upright
and inverted flowers to return to their original
position after being depressed by a visiting insect.
Fig. 1. — Known distribution of Canavalia virosa south of the
Limpopo River (based on collections housed at the National
Herbarium, Pretoria).
226
THE POLLINATION OF CANAVALIA VIROSA BY XYLOCOPID AND MEGACHILID BEES
3
Fig. 2. — Canavalia virosa
showing various views of
the flower: 1, front view
of flower with an arrow
indicating the opening
caused by the bulging of
the upper wing margins;
2, side view of flower
with one wing and keel
blade removed to show
relative position of stan-
dard, wing and keel; 3,
enlargement of centre
portion of 2 showing
wing pulled aside from
the upper margin of the
keel; 4, side view of
opening flower to show
relative position of wing
and standard auricles.
(K. = keel, S = standard,
W = wing). Arrows indi-
cate longitudinal bulging
of upper wing margins.
POLLINATING VECTORS AND THEIR STRATEGIES
In 1964 Sauer wrote that the available information
on pollinating insects in Canavalia was meagre.
Xylocopid bees have been reported to pollinate
C. maritima e.g. Xylocopa violacea (Scott— Elliot, 1891)
and X. aestuans (Piper et al. 1922). Vogel (1954)
reported that Anthophora sp. also pollinates this
species. Lepidoptera may also visit C. maritima
(Scott— Elliot, 1891).
Recent field studies in the Nelspruit District of the
eastern Transvaal, revealed that only tw'o types cf
bees were able to depress the keel of C. virosa
effectively. These bees differed markedly in size and
adopted different pollinating strategies.
Xylocopa flavorufa De Greer (Fig. 3: 1) is a noisy
fast-flying solitary bee found in coastal bush, montane
savanna woodland, fynbos and dry savanna woodland
(Watmough, 1974). Both male and female bees were
caught feeding on the flowers of C. virosa in the
Nelspruit Botanical Gardens. The bee lands on the
inverted standard with some force causing the
whole inflorescence to shudder. This insect fits snugly
into the area presented by the standard and maintains
a hold by grasping the standard mainly near the
peg-like callosities. Its head lies near the opening
formed by the longitudinal bulges of the wings of the
flower (Fig. 4: 1). To trip the mechanism the bee
raises its abdomen and thorax and then thrusts its
head against the opening. This movement forces the
keel and wings away from the staminal sheath thereby
exposing the stigma and anthers, which dust the back
of the bee’s thorax. This sequence is identical to
that shown in Fig. 2 of Vogel (1954) in which he
depicts Anthophora sp. visiting flowers of C. maritima.
Megachile combusta Sm. (Fig. 3: 2) is a smaller
and lighter bee than Xylocopa flavorufa. It is incapable
of landing and maintaining its position as does
X. flavorufa. This bee lands more or less on the side
of the standard and after repeatedly slipping on the
shiny area above the callosities, it eventually
manoeuvres its body into a position that brings its
abdomen into line with the tip of the keel (Fig. 4: 2).
When it pushes its head against the opening (Fig.
2: 1) it depresses the keel and wings and causes its
abdomen to brush against the exposed stigma and
anthers. The wings and keel retract when the insect
alights.
Apis mellifera L. and other bees smaller than
M. combusta were common visitors to flowers of
C. virosa. These bees were unable to depress the keel.
They collected loose pollen and in flowers damaged
by beetles that fed on nectar. Lepidoptera were
common visitors.
DISCUSSION
In his discussion of the process of speciation in
Canavalia Sauer (1964) noted that almost nothing
was known about pollination or sterility barriers
that could protect the divergent adaptations of
subpopulations of diverging species. From his
observations that isolated greenhouse plants could
set seed, he deduced that facultative self-pollination
1
t i
1 cm
2
i 1
1 cm
Fig. 3. — Photographs of bees. 1, Xylocopa flavorufa ; 2,
Megachile combusta.
C. H. STIRTON
227
Fig. 4.— Positions adopted by X. flavorufa (1) and M. combusta (2) when operating the pollination mechanism of Canavalia virosa.
Arrows indicate that pollen is dusted onto the thorax of X. flavorufa and onto the underside of the abdomen of M. combusta.
was possible, but he pointed out that the attractiveness
of flowers to bumble bees and butterflies indicated
cross-pollination.
Watmough (1974) noted that many indigenous
Papilionaceae in Southern Africa apparently have no
regular effective pollinators other than carpenter bees,
which alone possess the power and weight necessary
to operate the floral mechanisms. Canavalia appears,
from the available evidence, to fall into such a class
of plants. Plants of C. virosa in the eastern Transvaal
tend to set between 2-4 seed pods per inflorescence,
a factor which could indicate outbreeding as bees
did not forage in inclement weather. If inbreeding
was operative, one would expect a much higher seed
set. It may, therefore, be advantageous to breed
and release xylocopid bees in those areas where
C. virosa and C. ensiformis are being cultivated.
Watmough (1974) cites a number of references,
which indicate that the introduction of these bees
has improved the pollination and/or yield of a number
of other agricultural crops.
Of the bees studied in this paper, X. flavorufa
seems a more “natural” pollinator, whereas M.
combusta and other bees smaller than it show every
sign of being opportunists. M. combusta has
“developed” a method whereby it can utilize nectar
and pollen, but one which is not always successful.
Since few bees appear to be large enough to
pollinate C. virosa successfully, it would appear that
the large inverted flowers of this species constitute
a possible isolating mechanism. M. combusta is the
smallest known bee, which can operate the floral
mechanism. A comparative study of sympatric
Canavalia spp. with respect to pollinating vectors
could give a better insight into the mechanisms which
protect the divergent adaptations of subpopulations
of diverging species, particularly those in complexes
such as that of C. ensiformis.
ACKNOWLEDGEMENTS
My sincere thanks to Mrs E. Buitendag and
Mr E. van Jaarsveld of the Lowveld Botanic Gardens,
Nelspruit, for their help and hospitality; to Mr R. H.
Watmough of the Plant Protection Research Institute,
Pretoria, for naming the insect collection; to Miss M.
Scott for the line drawings and to Mrs A.
Romanowski for the photographs.
UITTREKSEL
Die blommorfologie van Canavalia virosa ( Roxb .)
Wight & Am. word bespreek in verhouding tot
bestuiwing deur Xylocopa flavorufa De Greer en
Megachile combusta Sm.. Dit is gevind dat die ver-
houding tussen grootte van blom en by die tipe
bestuiwingstrategie en die sukses daarvan beinvloed.
Bye kleiner as M. combusta het ondoeltreffende
bestuiwers blyk te wees.
REFERENCES
Piper, C. V. & Dunn, S. T., 1922. A revision of Canavalia.
Bull. Misc. Inf. Kew 4: 129-145.
Sauer, J., 1964. Revision of Canavalia. Brittonia 16: 106-181.
Scott Elliot, G. F., 1891. Notes on the fertilization of South
African and Madagascar flowering plants. Ann. Bot. 5,14:
332-405.
Verdcourt, B., 1971. Leguminosae 4. Papilionoideae 2. In E.
Milne-Redhead & R. M. Polhill, Flora of Tropical East
Africa. London: Crown Agents for Overseas Governments
and Administrations.
Vogel, S., 1954. Bliitenbiologische Typen als Elemente der
Sippengliederung. Jena: Veb Gustav Fischer. 338 pp.
Watmough, R. H., 1974. Biology and behaviour of carpenter
bees in Southern Africa. J. Ent. Soc. Sth. Afr. 37,2: 261—
281.
Westphal, E., 1974. Pulses in Ethiopia, their taxonomy and
agricultural significance. Belmontia, New Series 3,9:
1- 363.
Bothalia 12,2: 229-230 (1977)
Broad-spectrum pollination of Plectranthus neochilus
C. H. STIRTON*
ABSTRACT
The pollination ecology of Plectranthus neochilus Schltr. is discussed and compared with that of another
garden plant, Plectranthus barbatus Andr.. Pollinators and flower visitors of P. neochilus include members of
the Megachilidae, Anthophoridae, Syrphidae, Bombyliidae, Sphingidae, Apidae.
RESUME
EVENTAIL DE POLLINISATION DE PLECTRANTHUS NEOCHILUS
L'ecologie de la pollinisation de Plectranthus neochilus Schltr. est discutee et comparee avec cede
d'une autre plante de lardin, Plectranthus barbatus Andr. On a releve, parini les insectes qui pollinisent
et visitent les fleurs de P. neochilus, des representants des Megachilidae, Anthophoridae, Syrphidae,
Bombyliidae, Sphingidae, Apidae.
INTRODUCTION
The insect-plant relationships of plants under
cultivation are often very different from those of the
same species growing under natural conditions. The
“wild” pollinators may be absent in gardens and the
successful transference of an outbreeding plant will
then depend on either its potential for vegetative
reproduction or on the plasticity of its pollination
strategies.
This paper assesses the plant-insect relationships of
Plectranthus neochilus Schltr., an indigenous species
cultivated in gardens in the Pretoria area.
GENERAL MORPHOLOGY
P. neochilus is mostly a perennial, decumbent to
erect, often much branched and bushy (Fig. 1),
unpleasantly aromatic, 12-50 cm tall herb (Codd,
1975). Although it is variable in vegetative characters
it is relatively constant in floral characters. The inflo-
rescence is a 4-angled spikelike raceme 3-4 cm long
when in the bud stage. It is composed of 4 rows of
densely imbricate, ovate, acuminate bracts (Fig. 2A).
Flowering proceeds by the gradual opening of each
verticil of flowers. This is accompanied by the shedding
of the bracts surrounding each verticil and by the
elongation of the rhachis between the opened verticils
(Fig. 2C). Thirteen spaced verticils can be seen in
Fig. 2C, with the rhachis also cleany visible between
the verticils. Open flowers can be seen in Fig. 2B.
POLLINATION ECOLOGY
Over a period of three weeks plants of P. neochilis
were observed in the Pretoria National Botanic
Gardens, Brummeria. They cover large areas in massed
displays, a feature seldom found in the wild. These
displays are rich sources of nectar and attract
numerous insect visitors such as bees, hoverflies and
butterflies. The following insects represent the
commonest visitors:
Megachilidae Megachile maxillosa Guer.
Megachile chrysorrhoeae Gerst.
Megachile sp. (leaf cutter)
Megachile combusta Sm.
Megachile sp. cf. combusta Sm.
Anthophoridae Xylocopa caffra (L.)
Xylocopa senior Vachal
Xylocopa sichele Vachal
Anthophora sp.
Apidae Apis mellifera L.
Syrphidae . Asarcina cf. rostrata Wied.
Bombyliidae unidentified flies
Sphingidae Macroglossum trochilus (Hbn.)
Of these insects, only the bees effectively worked the
pollination mechanism every time. The syrphids,
bombylids and sphingids insert their probosci without
touching either the androecium or gynoecium.
In all cases, the bees landed on the horizontal lower
boat-shaped lip of the flower, depressing it and
exposing the stamens and stigma (which then rubbed
against the lower abdomen as the insect began
Fig. 1. — Plectranthus neochi-
lus growing among rocks
8 km S.E. of Barberton.
Note the large number
of inflorescences. Photo:
L. E. Codd.
Botanical Research Institute, Department of Agricultural Technical Services, Private Bag X101, Pretoria.
230
BROAD-SPECTRUM POLLINATION OF PLECTRANTHUS NEOCHILUS
Fig. 2. — Plectranthus neochilus : A, region of densely imbricate,
ovate, acuminate bracts; B, region of opening flowers;
C, region of opened verticils showing gaps between the
verticils (numbered 1 — 1 3). Pole Evans 4775, cultivated at
Prinshof (1954-01-19).
feeding). The most active feeding times were between
1 lhOO and 14h00., especially on calm, bright and sunny
days.
Scott Elliot (1891) recorded the following insects
on P. ecklonii Benth.: Apis mellifera collecting pollen,
a bombylid sucking and effecting cross-fertilization, as
well as two lepidoptera.
Although the flower beds could not be observed
continuously, it was clear that, as the inflorescences
gradually opened and expanded, there were definite
changes in the numbers and types of insects seen
visiting the plants over a three week period. It is
apparent that the gradual opening of the inflorescence
verticil by verticil, the abundant nectar production,
the small flowers, and many inflorescences on a single
plant all ensure a steady visitation by pollinators over
a long period.
During two months of observations in the wild,
however, only megachilid bees have been observed
visiting P. modulus.
Plectranthus barbatus Andr. is an attractive garden
plant cultivated in various parts of the world and,
according to Codd (1975), it has become semi-
naturalized in parts of South Africa. This plant is
grown in the Pretoria National Botanic Gardens in
the vicinity of P. neochilus, which is a less robust
plant with smaller flowers. Of the insects visiting
P. neochilus, only Xylocopa sichele Vachal, X. senior
Vachal and Macroglossum trochilus (Hbn.) also
visited P. barbatus, the latter two very rarely. Both
species of Plectranthus are new feeding records for
M. trochilus (Hbn.).
It may be concluded that P. neochilus possesses
inherent features, which have enabled it to be visited
by a broader spectrum of insect visitors in cultivation
than in the wild. The limited “garden strategy” of
P. barbatus needs further investigation, particularly
with reference to its original habitat.
ACKNOWLEDGMENTS
My sincere thanks go to Dr R. H. Watmough for
identifying the insects and to Dr L. E. Codd for his
interest and identification of the Plectranthus material.
UITTREKSEL
Die bestuiwings-ekologie van Plectranthus neochilus
Schltr. word bespreek en vergelyk met die van ’n
ander tuinplant, P. barbatus Andr.. Bestuiwers en
blombesoekers van P. neochilus sluit lede van die
Megachilidae, Anthophoridae, Syrphidae, Bombyliidae,
Sphingidae en Apidae in.
REFERENCES
Codd, L. E., 1975. Plectranthus (Labiatae) and allied genera in
Southern Africa. Bothalia 11: 371-442.
Scott Elliot, G. F., 1891. Notes on the fertilization of South
African and Madagascar Flowering Plants. Ann. Bot. 5:
333-405.
Bothalia 12, 2: 231-237 (1977)
Freshwater algae of Southern Africa. II. Triplastrum spinulosum
from the Transvaal
M. ISABELLA CLAASSEN*
ABSTRACT
The presence of Triplastrum spinulosum (Kisselev) Gauthier-Lievre (Desmidiaceae) in South Africa is
reported for the first time. The characters of T. spinulosum varieties spinulosum, indicum (Iyengar & Ramanathan)
Gauthier-Lievre and africanum Gauthier-Lievre were found to be exhibited by specimens collected at Ottosdal
in the south-western Transvaal. The differences among specimens of the populations studied are ascribed to
variation within one variable species and therefore the varieties indicum and africanum are relegated to syn-
onymy.
RESUME
ALGUES DULCICOLES D'AFRIQ UE AUSTRALE. II. TRIPLASTRUM SPINULOSUM
DU TRANSVAAL
La presence de Triplastrum spinulosum ( Kisselev ) Gauthier-Lievre ( Desmidiaceae ) en Afrique du
Sud est signalee pour la premiere fois. On a constate que les caracteristiques des varietes spinulosum,
indicum ( Iyengar & Ramanathan) Gauthier-Lievre et africanum Gauthier-Lievre de Vespece T. spinu-
losum se rencontrent dans les specimens recoltes a Ottosdal dans le sud-ouest du Transvaal. Les diffe-
rences entre specimens des populations etudiees sont attribuees a la variation intraspeciftque d'une
espece variable et les varietes indicum et africanum sont des lors placees en synonymie .
INTRODUCTION
Samples containing Triplastrum spinulosum were
collected by the author during April 1972 and
February 1975 from a small pan 16 km east of Ottosdal
in the south-western Transvaal and by Mr G. Germis-
huizen, Botanical Research Institute, Pretoria, during
February 1974 from a small pool on the banks of the
Nyl River on the farm Mosdene near Naboomspruit,
central Transvaal.
Both habitats contain water during the rainy
season, but may dry up partially or completely during
the dry season (winter). During December 1974,
which was an exceptionally dry summer, the Ottosdal
pan was completely dry.
The hydrogen-ion concentration and the tempera-
ture of the water at the time of collection were pH 7,7
and 24°C, and pH 7,5 and 27°C for April 1972 and
February 1975 respectively at Ottosdal and pH 6,1
and 26°C at Mosdene.
METHODS
The material was preserved with 4% formalin.
Slides were made by mounting a sample droplet in a
drop of glycerine. The methods used for the drawings
and photomicrographs were the same as those given
in the first paper of this series (Claassen, 1973).
OBSERVATIONS AND DISCUSSION
Iyengar and Ramanathan (1942) found a desmid
in material collected during December 1940 in a paddy
field near Madras, South India, which resembled the
species Triploceras abbreviatum Turner (Krieger, 1937;
Turner, 1892) and Triploceras simplex Allorge
(Krieger, 1937). One of the main characters of the
genus Triploceras Bailey is the presence of numerous
whorls of knotlike projections (verrucae). As this
character was lacking in both Turner’s and Allorge’s
species as well as in their own taxon, Iyengar and
Ramanathan (1942) decided to establish the new genus
Triplastrum to accommodate these taxa, the consti-
tuent species being Triplastrum indicum Iyengar &
Ramanathan, the desmid collected near Madras,
Triplastrum abbreviatum (Turner) Iyengar & Rama-
nathan and Triplastrum simplex (Allorge) Iyengar &
Ramanathan. However, they were unaware of the
existence of Triploceras spinulosum Kisselev (Krieger,
* Department of Botany, University of Pretoria, Pretoria.
1937), the description of which was based on a single
specimen collected in Turkestan in 1930. Triploceras
spinulosum closely resembles Triplastrum indicum and
in 1960 Gauthier-Lievre reduced the latter to a variety
of the former, thus Triplastrum spinulosum (Kisselev)
Gauthier-Lievre var. indicum (Iyengar & Ramanathan)
Gauthier-Lievre.
Gauthier-Lievre (1960) also described a new variety
based on material collected in Africa, namely Triplas-
trum spinulosum var. africanum. The name of this new
variety proposed by Gauthier-Lievre was not validly
published, however, since it was not accompanied by a
Latin description or diagnosis as stipulated by Article
36 of the International Code of Botanical Nomencla-
ture (Stafleu, 1972).
Turner (1892) described the apices of Triploceras
abbreviatum as three- or four-lobed. Iyengar and
Ramanathan (1942) incorporated this into their
description of the genus Triplastrum. Krieger (1937)
mentioned only three-lobed apices in his description
of Triploceras abbreviatum Turner, and Gauthier-
Lievre mentioned only three-lobed apices in her
description of the genus Triplastrum. In the material
collected in the Transvaal the Ottosdal specimens have
either three-lobed apices (Figs 1-3, 16 - upper cell,
17-22, 31, 32, 33 - cell on left, 34-38) or four-lobed
apices (Figs 4, 9, 16 - lower cell, 25, 33 - cel! on right)
while some specimens have one semicell with a
three-lobed apex and the other semicell with a four-
lobed apex (Figs 10, 11, 26-28, 39). The Mosdene
specimens have only four-lobed apices (Figs 5-8, 14).
Gauthier-Lievre (1960) described Triplastrum spinu-
losum var. spinulosum as having weakly dilated apices,
divided into three hardly divergent lobes which are
bi-, tri- or quadridenticulate. Krieger's figure of this
variety (1937, PI. 53, Fig. 7), one of Gauthier-Lievre’s
figures of her var. africanum (1960, Fig. 2t, cell on
left), and Figs 1 and 13 (upper semicell) in the present
paper as well as some of the specimens with four-
lobed apices (Figs 7, 8, 14) resemble one another in
that the apices are weakly dilated, and the polar lobes
hardly divergent and bi- or tridenticulate and seldom
quadridenticulate (Fig. 13).
According to Gauthier-Lievre (1960), Triplastrum
spinulosum var. indicum differs from the typical variety
in its larger dimensions and longer more divergent
polar lobes. Iyengar and Ramanathan’s figures for
232 FRESHWATER ALGAE OF SOUTHERN AFRICA. II. TRIPLASTRUM SP1NULOSUM FROM THE TRANSVAAL
this variety agree with Figs 2 (lower semicell) and 17
(cell on left) of the present paper as well as with some
of the cells with four-lobed apices (Figs 4-6). The
dimensions of these cells overlap both those of the
type and var. indicum.
Triplastrum spinulosum var. africanum (Gauthier-
Lievre, 1960) differs from the typical variety in that the
cells are slightly narrower below the apices and the
polar lobes are strongly divergent, bidenticulate and
seldom tridenticulate. The majority of the Ottosdal
specimens (Figs 2 - upper semicell, 3, 19-22, 31, 32,
34-38) agree with Gauthier-Lievre’s figures for this
taxon (1960, Figs 2q-t), but bidenticulate and tridenti-
culate polar lobes are approximately equal.
Iyengar and Ramanathan (1942) observed two
chloroplasts each with a central pyrenoid in each
semicell. Gauthier-Lievre (1960) reported 1 or 2
pyrenoids per semicell for the type and 1-3 pyrenoids
for her var. africanum. In the material collected in
Transvaal, the majority of the specimens observed had
two chloroplasts per semicell (Figs 1 , 2, 4-8, 11, 12, 14,
19, 21, 23, 24, 26-28, 31, 32, 41), some had three
chloroplasts per semicell (Figs 9, 25) or one semicell
contained two chloroplasts and the other three
(Figs 3, 20, 22). Each of these chloroplasts contained
a central pyrenoid. Only a few specimens were
observed in which the delineation of the chloroplasts
was indistinct and there appeared to be only one
chloroplast per semicell, but each contained two pyre-
noids.
In the Ottosdal material one specimen (Figs 9, 25)
was found which was considerably larger than the
others: length without spines 141 /am, with spines
144 pm; maximum width 14 pm; width of isthmus 11
pm; width of apices 17-18, 5 pm. If this specimen is
also taken into consideration, the dimensions of the
Transvaal specimens overlap those of Gauthier-
Lievre’s three varieties of Triplastrum spinulosum. The
dimensions of the other Transvaal specimens are as
follows:
Ottosdal Mosdene
length without spines 61-97 pm
length with spines. . . 63-102,5 pm
maximum width 9-11 ^m
width of isthmus. .. . 8,5-10,5 /xm
width of apex 11-18 pm
56-66 pm
59-68 pm
9,3-10 fim
8, 8-9, 3 pm
10, 5-14 pm
Zygospores, found in the Ottosdal material col-
lected during April 1972 (Figs 17, 18, 34-39), resemble
those found by Iyengar and Ramanathan (1942) but
are slightly smaller. The dimensions are 34-38 x
36^40 /am.
When all the characters found in the Transvaal
specimens were taken into consideration it was
decided that the specimens studied belonged to one
species, namely Triplastrum spinulosum and that the
two varieties indicum and africanum should be regarded
as synonyms.
Diagnosis
Cellulae parvae, circiter 6-10-plo longiores quam
latiores, in medio leviter at manifeste constrictae;
semicellulae rectae, cylindricae, lateribus paene paral-
lels vel leviter a basi paene usque ad apicem attenua-
te, apices aliquatenus inflati, trilobi vel quadrilobi;
qui lobi singuli 2-4 spinas breves ferunt; cellulae paries
incolor, pori perparvuli. Chloroplasti axiales bini vel
terni in semicellulis singulis, in seriem mediam dis-
positi, quorum unicuique laminae radiantes vel
stellatae cum pyrenoide medio. Zygospora sphaerica
(-subsphaerica) pariete spisso, margine crenato.
Longitudo sine spinis 56-99, 5 (141) pm, cum spinis
59-105 (144) pm; latitudo ad basim semicellulae
9-14 pm; isthmi latitudo 8, 5-12 pm; apicis latitudo
11-18 (18,5) ^.m; zygospora 36-42x38-42 ^m.
Cells small, about 6-10 times longer than broad,
with a slight but well-defined median constriction;
semicells straight, cylindrical, with sides nearly parallel
or slightly attenuated from base to just below the
apex; apices more or less inflated, three- or four-lobed,
lobes slightly to strongly divergent, each lobe bearing
2-4 short spines; cell wall colourlesss, pores minute.
Chloroplasts axial, 1 (?) or 2-3 in each semicell,
arranged in a median series, each chloroplast with
radiating plates (stellate) and a central pyrenoid.
Zygospore spherical to subspherical, thick-walled,
margin crenate. Length without spines 56-99,5 (141)
pm. with spines 59-105 (144) ^m; maximum width
near base of semicell 9-14 ^m; width of isthmus
8,5-12 pm; width of apices 11-18 (18,5) pm;
zygospore 38-42x36-42 pm.
The geographical distribution of this species is:
Asia. — Turkestan (in a rice-swamp near Weljko-Alexewskoje).
India (in a paddy field near Madras, December)
Africa. — Sudan (in a swamp of the River Niger near Gao,
December). French Equatorial Africa (Ubangi-Shari, February).
Uganda (in a swamp on the road from Masaka to Kampala,
August). Transvaal (in a small pool on the banks of the Nyl
River near Naboomspruit, February; in a small pan near Ottos-
dal, February and April).
It seems that this species is very rare and that
usually only a few specimens are found in samples
collected. In the samples collected near Ottosdal
during April 1972, however, it was fairly abundant.
As could be expected in a fairly large population
anomalous specimens were also found. In the Ottosdal
material one specimen was found where, in each
semicell, one of the polar lobes was under-developed,
without spines and somewhat subapical (Figs 12,
41). In another specimen only one of the semicells
was like this (Fig. 13, lower semicell). Several asym-
metrical cells were found (Figs 1 1, 29, 40) and one very
narrow semicell was observed (Fig. 30). The most
anomalous specimen was a single semicell with a
prominent basal inflation encircled by a whorl of
eight lobes similar to the polar lobes (Figs 15, 42-44).
In the Mosdene material one anomalous specimen
was found with the polar lobes of one semicell
undeveloped (Fig. 14).
The two varieties are thus placed into synonymy
and the circumscription of the species is amplified.
Triplastrum spinulosum ( Kisselev ) Gauthier-Lievre
in Revue Algol., 5, 1960, p. 64.
Syn.: Triploceras spinulosum Kisselev in Trans. Uzbekistan
Inst. Tropic. Med. 1, 1930, p. 50, PI. 4, Fig. 5; Krieger in
Rabenhorst’s Kryptogamenflora 13(1), 1937, p. 449, PI. 53, Fig.
7.
Triplastrum indicum Iyengar & Ramanathan in J. Indian Bot.
Soc., 21, 1942, p. 228, Figs 1-5. T. spinulosum (Kisselev)
Gauthier-Lievre var. indicum (Iyengar & Ramanathan)
Gauthier-Lievre in Revue Algol., 5, 1960, p.64. - var. africanum
Gauthier-Lievre, l.c. PI. 64, Fig. 2, q-t, non rite publ.
ACKNOWLEDGEMENTS
I wish to thank the Council for Scientific and
Industrial Research and the Research Committee
of the University of Pretoria for financial assistance,
Mr G. Germishuizen for collecting the Mosdene
samples and Prof. Dr H. L. Gonin, who kindly
prepared the Latin diagnosis.
UITTREKSEL
Triplastrum spinulosum ( Kisselev ) Gauthier-
Lievre (Desmidiaceae) is vir die eerste keer in Suid-
Afrika aangetref. Daar is gevind dat verteenwoordigers
M. ISABELLA CLAASSEN
233
wat naby Ottosdal in die suid-westelike Transvaal
versamel is die kenmerke van T. spinulosum varieteite
spinulosum, indicum ( Iyengar & Ramanathan) Gaut-
hier-Lievre cn africanum Gauthier-Lievre weerspieel.
Verskille tussen verteenwoordigers van hierdie popidasie
word as variasie in die self de takson aanvaar en die
varieteite indicum cn africanum word dus as sinonieme
beskou.
REFERENCES
Claassen, M. Isabella, 1973. Freshwater algae of Southern
Africa. 1. Notes on Gloeotrichia ghosei R. N. Singh. Br.
Phycol. J., 8: 325-331.
Gauthier-Lievre, L., 1960. Les Genres Ichtyocercus* , Triploce-
ras et Triplastrum en Afrique. Revue Algol., 5: 55-65.
Iyengar, M. O. P. & Ramanathan, K. R., 1942. Triplastrum,
a new member of the Desmidiaceae from South India.
J. Indian Bot. Soc., 21 : 225-229.
Krieger, W., 1937. Die Desmidiaceen Europas mit Berucksich-
tigung der aussereuropaischen Arten. 1. Teil. In Raben-
horst’s Kryptogamenflora von Deutschland, Osterreich und
der Schweiz, 13(1): 1-712.
Stafleu, F. A. (Chairman), 1972. International Code of Botanical
Nomenclature. Utrecht: A. Oosthoek’s Uitgeversmaat-
schappij NV.
Turner, W. B., 1892. The freshwater algae of East India.
K. Svenska Vetensk.-Akad. Handl., 25: 1-187.
* The original spelling of the name of this genus by its
authors was Ichthyocercus (West, W. & G. S. West, 1897,
Welwitsch’s African freshwater Algae, J. Bot., 35: 80).
234 FRESHWATER ALGAE OF SOUTHERN AFRICA. II. TRIPLASTRUM SPINULOSUM FROM THE TRANSVAAL
F,GS I “18. —Drawings of Triplastrum spinulosum. 1, cell with three-lobed apices, lobes tridenticulate; 2, cell with three-lobed apices,
obes bi- or tridenticulate; 3, cell with one semicell containing three chloroplasts and the other semicell two; 4-8, cells with four-
lobed apices, lobes bi- or tridenticulate; 9, large specimen with four-lobed apices, lobes tridenticulate, each semicell with three
chloroplasts; 10, cell with one three-lobed and one four-lobed apex, lobes bi- or tridenticulate; 11, asymmetrical cell with one
three-lobed and one four-lobed apex, lobes bident iculate; 1 2, anomalous cell with one polar lobe in each semicell under-developed,
without spines and slightly subapical, normal lobes bidenticulate; 13, anomalous cell with one polar lobe in one semicell under-
developed, without spines and slightly subapical, normal lobes bi-, tri- or quadridenticulate; 14, anomalous cell with polar lobes
of one semicell undeveloped; 15, anomalous semicell with a prominent basal inflation encircled by a whorl of eight lobes; 16,
conjugating cells showing protuberances; 17, conjugating cells with young zygospore; 18, conjugating cells with mature
zygospore. (Figs 1-4, 9-12 and 15-17: scale B. Figs 5-8, 13, 14 and 18: scale A).
M. ISABELLA CLAASSEN
100/um
Figs 19-31. — Photomicrographs of Triplastrum spinulosum. 19, 21, cells with three-lobed
apices and two chloroplasts per semicell; 20, 22, cells with three-lobed apices, one
semicell with two chloroplasts and the other semicell with three; 23, 24, cells with
four-lobed apices; 25, large specimen with four-lobed apices and each semicell
with three chloroplasts; 26-28, cells each with the upper apex four-lobed and the
lower apex three-lobed; 29, asymmetrical cell with upper semicell broader than
lower semicell; 30, abnormally narrow semicell; 31, two cells after division re-
maining attached to each other, (c, chloroplast; p, pyrenoid; n, nucleus).
236 FRESHWATER ALGAE OF SOUTHERN AFRICA. II. TRIPLASTRUM SPINULOSUM FROM THE TRANSVAAL
'•**•*-
0
3
;
Figs 32-36. — Photomicrographs of Triplastrum spinulosum 32, two
cells just before conjugation, the dirt particles represent the margin
of the mucilaginous envelope; 33, conjugating cells showing protuber-
ances; 34, conjugating cells with young zygospore; 35, 36, further
stages in developement of zygospore. (Fig. 32: scale A. Figs. 33-36:
scale B).
M. ISABELLA CLAASSEN
237
Figs 37-44. — Photomicrographs of Triplastrum spinulosum. 37, immature zygospore
showing crenate margin; 38, 39, mature zygospores; 40, asymmetrical cell; 41,
anomalous cell with one polar lobe in each semicell under-developed, without
spines and slightly subapical; 42-44, anomalous semicell with a prominent basal
inflation encircled by a whorl of eight lobes, photographed at various focussing
adjustments.
Bothalia 12, 2: 239-245 (1977)
Freshwater algae of Southern Africa. IV. Some Micrasteriae from
Rhodesia, including a new species
M. ISABELLA CLAASSEN*
ABSTRACT
Micrasterias ambadiensis (Gronblad & Scott) Thomasson, M. crux-melitensis (Ehrenberg) Hassall forma
minor Turner, M. decemdentata (Nageli) Archer, M. pinnatifida (Kutzing) Ralfs var. incudiformis West & West,
M. radiata Hassall var. brasiliensis Gronblad sensu lato, and M. tropica Nordstedt var. tropica are discussed.
A new species, M. schweickerdtii Claassen, is described.
RESUME
ALGUES DULCICOLES D'AFRIQUE AUSTRALE. IV. QUELQUES MICRASTERIAE DE
RHODESIE, INC LU ANT UNE NO UVELLE ESP EC E
On discute Micrasterias ambadiensis (Gronblad & Scott) Thomasson, M. crux-melitensis (Ehren-
berg) Hassall forma minor Turner, M. decemdentata (Nageli) Archer, M. pinnatifida (Kiitzing)
Ralfs var. incudiformis West & West, M. radiata Hassall var. brasiliensis Gronblad sensu lato, et
M. tropica Nordstedt var. tropica. Une nouvelle espece est decrite: M. schweickerdtii Claassen.
INTRODUCTION
A sample containing a rich assemblage of desmids
was given to me by Prof. Dr H. G. W. J. Schweickerdt,
formerly head of the Department of General Botany,
University of Pretoria. He collected the material
during July 1957 from a small pool on dolomite rocks
near Rusape, Rhodesia, but provided no physical or
chemical data.
The sample contained seven different Micrasterias
taxa amongst a number of other desmids. Although
this sample was poorer in taxa, the taxon-composition
showed a remarkable resemblance to that of Lake
Ambadi, Sudan (Gronblad, Prowse & Scott, 1958).
METHODS
The material was preserved in 4% formalin.
Slides were made by mounting a sample droplet
in a drop of glycerine.
Drawings were made with a Zeiss binocular bright
field/phase contrast microscope using a Leitz micro-
meter-net-ocular and specially printed squared paper,
the squares being 2x2 cm. The lenses used were a
12, 5 x eye-piece and a 40 x objective.
Photomicrographs were taken on Adox KB 14
film using a 35 mm Willd microscope camera on a
Zeiss Nomarski contrast microscope. A 6x eye-piece
and a 40 x objective were used.
All dimensions are given in micrometres (^m).
OBSERVATIONS AND DISCUSSION
The following taxa were identified in the sample
collected by Schweickerdt:
1. Micrasterias ambadiensis ( Gronblad & Scott)
Thomasson (1960, p. 22, Figs 4: 10 & 10: 4; Lind,
1971, p. 542, PI. 2, Fig. 3).
Syn.: M. radians Turner var. ambadiensis Gronblad & Scott
(Gronblad, Prowse & Scott, 1958, p.21, PI. 11, Fig. 119 & PI. 26,
Fig. 363; Gronblad, 1962, p.7, PI. 1, Fig. 9).
Some variation with regard to the delineation of
the lateral lobes occurred in the Rusape specimens
(Figs 1 1-14 and 26-29). In the type figures by
Gronblad & Scott (1958, Figs 119 and 363) as well
as Thomasson’s figure (1960, Fig. 4: 10) the inferior
lateral lobes have three spines each and the superior
lateral lobes either three or four. In the specimen
depicted in Gronblad’s Fig. 9 (1962) both inferior
and superior lateral lobes have four spines each and
* Department of Botany, University of Pretoria, Pretoria.
in Lind’s specimen (1971, PI. 2, Fig. 3) both inferior
and superior lateral lobes have three spines each.
In the Rusape specimens the number of spines in
both inferior and superior lateral lobes varies from
two to four. In a single specimen one inferior lateral
lobe was completely absent and another consisted of a
single spine (Fig. 12, bottom semicell). An abnormal
coalescence of the cell wall in the inner portion of the
sinus was observed in another specimen (Fig. 26).
This specimen also showed abnormal cell wall
thickenings at the base of each incision between the
inferior and superior lateral lobes and between the
superior lateral lobes and the polar lobe (upper
semicell) as well as a large granule in the centre of the
apical margin of the polar lobe. Length without
spines 114-136, with spines 140-168; width without
spines 98-1 13, with spines 1 12-131 ; width of isthmus
23-24; maximum width of polar lobe without spines
44-48, with spines 60-72. Very common.
2. Micrasterias crux-melitensis ( Ehrenberg ) Hassall
forma minor Turner (1892, p. 92, PI. 5, Fig. 4c;
Gronblad, Prowse & Scott, 1958, p. 19, PI. 11,
Fig. 124 & PI. 25, Fig. 358; Hinode, 1969, p. 199,
Fig. 7: 11; Krieger, 1939, p. 65, PI. 115, Fig. 1).
In some of the Rusape specimens the basal portion
of the polar lobe is noticeably broader than in the
typical form (Fig. 15). Length without spines 74-76,
with spines 87-89; width without spines 80-82, with
spines 86-89; width of isthmus 15-17; maximum
width of polar lobe 42-44. Rare.
3. Micrasterias decemdentata ( Nageli ) Archer
(Borge, 1918, p. 66, PI. 5, Fig. 23; Gronbald &
Croasdale, 1971, p. 11, PI. 4, Fig. 47; Gronblad,
Scott & Croasdale, 1964, p. 15, PI. 9, Fig. 219;
Krieger, 1939, p. 34, PI. 104, Figs 9-11; Lind, 1971,
p. 542, PI. 1, Fig. 29).
Syn.: M. decemdentata (Nag.) Arch. var. galpinii Claassen,
1961, p. 585, PI. 17, Figs 4-7.
Specimens with 10 spines per semicell were rather
rare; more common were specimens with 6 (Figs 16
and 17, upper semicells) or 9 (Fig. 17, lower semicell)
spines per semicell. Fig. 16 represents a specimen
in which one of the polar lobes is undeveloped (lower
semicell). Length 47,5-50; width without spines
46-50, with spines 56,5-62; width of isthmus 10-12;
maximum width of polar lobe without spines 30-31,
with spines 36-40,6. Rare.
240 FRESHWATER ALGAE OF SOUTHERN AFRICA. IV. SOME MICRASTERIAE FROM RHODESIA, INCLUDING A
NEW SPECIES
4. Micrasterias pinnatifida ( Kutzing ) Ralfs var.
incudiformis West & West (1895, p. 48, PI. 6, Fig. 5;
Gronblad & Croasdale, 1971, p. 11, PI. 4, Fig. 49;
Krieger, 1939, p. 19, PI. 100, Fig. 3).
These specimens (Figs 18-21) more closely resemble
the plant represented in Gronblad & Croasdale’s
Fig. 49 than the type specimen but their dimensions
agree better with that of the type. Length 56-60;
width without spines 57-62, with spines 61-67;
width of isthmus 11-12; maximum width of polar
lobe without spines 38-46,8, with spines 44-52.
Very common.
5. Micrasterias radiata Hassall var. brasiliensis
Gronblad sensu lato, 1945, p. 15, PI. 4, Figs 82 & 83;
Forster, 1969, p. 41, PI. 11, Fig. 5 & PI. 12, Fig. 1;
Thomasson, 1960, p. 24, Figs 4: 8 & 6: 12.
Syn.: M. radiata Hassall pro parte, in Krieger, 1939, p. 68,
PI. 117, Fig. 4 (non PI. 116, Figs 4-6 & PI. 117, Figs 1-3);
M. radiata Hassall forma Nordstedt (1869, in Borge, 1925, p. 29,
PI. 2, Fig. 7) in Forster, 1974, p. 156; M. radiata Hassall var.
groenbladii sensu Forster, 1974, p. 156, PI. 7, Fig. 1 (non PI. 5,
Fig. 80 in Scott, Gronblad & Croasdale, 1965); M. radians
Turner var. brasiliensis (Gronblad) Krieger in Forster, 1964, p.
380, PI. 18, Figs 1 & 2; Krieger & Scott (1957, p. 135) in Forster,
1974, p. 156.
The plant referred to here and all the cited figures
seen by the present author more closely resemble
Gronblad’s Fig. 83 than his Fig. 82. A broad inter-
pretation of M. radiata var. brasiliensis has been
adopted because, as the following discussion reveals,
there is no name available for the plant illustrated in
Fig. 83, and it is felt that, in view of the rather confused
nomenclature, it would be unwise to describe a new
taxon at this stage.
When Gronblad (1945) created M. radiata var.
brasiliensis he illustrated it with two figures. In his
Explanation of Plates he said “Fig. 82 is the most
frequent form, Fig. 83 is a larger form with more
slender processes'’ (Scott, Gronblad & Croasdale,
1965, p. 40). Croasdale (Scott, Gronblad & Croasdale,
1965) felt that the plant represented in Gronblad’s
Fig. 83 should be distinguished from the plant
represented in Fig. 82. She included this plant (Fig.
83) in the new variety M. radiata var. groenbladii
Croasdale (Scott, Gronblad & Croasdale, 1965, p. 39,
PI. 5, Fig. 80) and thereby it could possibly be con-
strued that she indirectly made Gronblad’s Fig. 82
the lectotype of M. radiata var. brasiliensis. As
Croasdale failed to indicate a type, the name M.
radiata var. groenbladii was not validly published
(Stafleu, 1972, p. 41, Art. 37). Forster (1969, p. 41)
decided that the plants depicted in Gronblad’s Fig. 83
and Croasdale’s Fig. 80 represented different varieties.
He transferred the plant represented in Gronblad’s
Fig. 83 back to M. radiata var. brasiliensis and
incorporated the plant represented in Croasdale’s
Fig. 80 in his new variety M. radiata var. croasdaleae
Forster (1969, p. 41, PI. 12, Fig. 2) as a synonym.
The name M. radiata var. croasdaleae was also not
validly published as no type was indicated, although
Forster mentioned on the first page of his paper
where slides containing new described taxa are
preserved.
When Forster (1969, p. 41) discussed M. radiata
var. brasiliensis he cited only Gronblad’s Fig. 83
and not Fig. 82 and it is not clear whether he meant
that his plant was M. radiata var. brasiliensis Gron-
blad, pro parte, quoad Fig. 83.
Later Croasdale (Gronblad & Croasdale, 1971,
p. 40) indicated her Fig. 80 in Scott, Gronblad &
Croasdale, 1965, as the type for M. radiata var.
groenbladii Croasdale. This validated the publication
of the variety and means that the name M. radiata
var. croasdaleae Forster is superfluous and illegitimate
and Forster’s concept of M. radiata var. groenbladii
Croasdale in Forster, 1974, p. 156, is incorrect.
When Forster (1974, p. 156) recognized Croasdale’s
variety groenbladii, he excluded Fig. 80 and cited
Gronblad’s var. brasiliensis, pro parte, quoad Fig. 83
as one of the synonyms. Thomasson (1960, p. 24,
Figs. 4: 8 and 6: 12) recorded M. radiata var.
brasiliensis Gronblad, 1945, cf. Fig. 83 for Lake
Bangweulu and although this paper appears in
Forster’s list of references (1974, p. 195) Thomasson’s
figures were not cited amongst the above-mentioned
synonyms.
Fig. 24 of the Rusape specimens resembles
Thomasson’s Fig. 4; 8 (1960, p. 15) and Fig. 9
resembles Thomasson’s Fig. 6: 12 (1960, p. 19) and
Forster’s PI. 7, Fig. 1 (1974, p. 213).
In the Rusape specimens there is a noticeable
variation in the width of the basal portions of the
polar lobes of mature semicells (Figs 9, 10, 24 and
25). An abnormal coalescence of the cell wall was
observed in the inner portion of the sinus (Fig. 24)
between the superior lateral and polar lobes (Fig. 24)
and between the lobules of the inferior and superior
lateral lobes (Fig. 25, mature semicell). The latter
also showed abnormal cell wall thickenings in the
diverging processes of the polar lobe. Length with
spines 180-208; width with spines 138-150; width of
isthmus 20-22; maximum width of polar lobe 80-100.
Common.
6. Micrasterias schweickerdtii Claassen, sp. nov.
(Figs. 1-8).
DIAGNOSIS
Inter species descriptas nulla affinitas obvia.
Cellulae amplae circiter 1 , 2— 1,3-pIo longiores quam
latiores, ellipticae, penitus constrictae, sinus apertus;
semicellulae trilobae. Lobus polaris magnus, sub-
cuneatus, anguli laterales deorsum curvati, apex
incisura mediana signatus, margini apicis spinae sunt
plerumque curvatae, 6 vel 7 utrimque ab incisura
mediana. Lobi laterales incisuris non profundis in
lobulos quattuor inaequales divisi; lobulus superior
sursum curvatus, tribus vel quattuor spinis
marginalibus ac curvatis instructus; quarum ima
maxima, vel in formam lobuli parvi et bidenticulati
delineata; lobuli mediani aut binis spinis marginalibus
instricti, aut in binos lobulos minores et bidenti-
culatos subdivisi, aut ex singula spina magna et
lobulo parvo et bidenticulatu constant; lobulus
inferior deorsum curvatus, tribus, spinis marginalibus
instructus. Cellulae paries porosus, plurimis instructus
spinis quae in series subradiatas in lobis polaribus et
lateralibus sunt dispositae; modo aliquot spinae in
semicellula media admodum supra isthmum
inveniuntur, modo nullae. Longitudo sine spinis
256-307 //m, cum spinis 284-337 //m; latitudo sine
spinis 201-234 /^m, cum spinis 227-262 /rm; isthmi
latitudo 41-45,5 /*m; lobi polaris latitudo maxima
sine spinis 124-146 /urn, cum spinis 139-161 ptm.
Iconotypus: fig. mihi 5.
This species does not correspond to any other
Micrasterias in literature available to the author.
Cells large, about 1,2-1, 3 times longer than
broad, elliptic, deeply constricted, sinus open;
semicells 3-lobed. Polar lobe large, subcuneate,
lateral angles curved downwards, apex with a median
notch, apical margin with 6-7, generally curved,
spines on each side of the median notch. Lateral lobes
divided into 4 unequal lobules by shallow incisions;
superior lobule curved upwards, furnished with 3-4
M. ISABELLA CLAASSEN
241
marginal curved spines, lowermost spine largest or
delineated as a small 2-denticulate lobule; median
lobules furnished with 2 marginal spines each or
subdivided into 2 smaller 2-denticulate lobules or
consists of one large spine and a small 2-denticulate
lobule; inferior lobule curved downwards, furnished
with 3 marginal curved spines. Cell wall porose,
furnished with numerous spines arranged in sub-
radiate rows within the polar and lateral lobes, with
or without a few spines in die middle of each semicell
just above the isthmus. Length without spines 256-
307, with spines 284-337; width without spines
201-234, with spines 227-262; width of isthmus
41-45,5; maximum width of polar lobe without
spines 124-146, with spines 139-161. Very rare.
Several unsuccessful attempts were made to turn
the cells over, so that they could be studied in lateral
or apical views.
The specimen depicted in Figs 3, 4 and 8 was
slightly anomalous in that one side of the sinus was
linear and not open.
7. Micrasterias tropica Nordsledt var. tropica
(Krieger, 1939, p. 56, PI. 112, Fig. 4).
In the polar lobes of the Rusape specimens (Figs
22, 23, 30 and 31) the diverging processes are longer
than in the type. These specimens fall rather in
between the plants represented in Krieger’s Fig. 4
(1939, PI. 112) and his Fig. 7 (1939, PI. 113) for
M. tropica var. elegans West & West as the lateral
and polar lobes are more slender than in the typical
variety and less slender than in var. elegans. The
semicell depicted in Fig. 23 could be compared with
var. elegans but for the shorter polar lobe. Length
92-104; width 80-106; width of isthmus 14-17,7;
maximum width of polar lobe 58-63,5. Rare.
ACKNOWLEDGEMENTS
I am indebted to the University of Pretoria for
research facilities, to Prof. Dr H. G. W. J.
Schweickerdt for the sample provided and to Prof.
Dr H. L. Gonin, who kindly prepared the Latin
diagnosis.
UITTREKSEL
Micrasterias ambadiensis ( Gronblad & Scott )
Thomasson, M. crux-melitensis ( Ehrenberg ) Hassal
forma minor Turner, M. decemdentata ( Ncigeli )
Archer, M. pinnatifida ( Kutzing ) Ralfs var. incudi-
formis West & West, M. radiata Hassall var. brasi-
iiensis Gronblad sensu lato, en M. tropica Nordstedt
var. tropica word bespreek. 'n Nuwe spesie, M.
schweickerdtii Claassen, word beskryf.
REFERENCES
Borge, O., 1918. Die von Dr. A. Ldfgren in Sao Paulo gesam-
melten Susswasseralgen. Ark. Boi. 15: 1-108.
Claassen, M. I., 1961. A contribution to our knowledge of the
freshwater algae of the Transvaal Province. Bothalia
7: 559-666.
Forster, K., 1964. Desmidiaceen aus Brasilien. 2. Teil: Bahia,
Goyaz, Piauhy und Nord-Brasilieri. Hydrobiologia 23 :
321-505.
Forster, K., 1969. Amazonische Desmidieen. 1. Teil: Areal
Santarem. Amazomiana 2: 5-116.
Forster, K., 1974. Amazonische Desmidieen. 2. Teil: Areal
Maues-Abacaxis. Amazoniana 5: 135-242.
Gronblad, R., 1945. De Algis Brasiliensibus, praecipue
Desmidiaceis, in regione inferiore fluminis Amazonas a
Professore August Ginzberger (Wien) anno MCMXXVII
collectis. Acta Soc. Sci. Fenn. 1 1 : 1-43.
Gronblad, R., 1962. Sudanese desmids II. Acta Bot. Fenn.
63: 2-19.
Gr5nblad, R. & Croasdale, Hannah, 1971. Desmids from
Namibia (S.W. Africa). Acta Bot. Fenn. 93: 2-40.
Gronblad, R., Prowse, G. A. & Scott, A. M., 1958. Sudanese
desmids. Acta Bot. Fenn. 58: 2-82.
Gronblad, R., Scott, A. M. & Croasdale, Hannah, 1964.
Desmids from Uganda and Lake Victoria collected by Dr
Edna M. Lind. Acta Bot. Fenn. 66: 1-57.
Hinode, T., 1969. On some Japanese desmids (6). Hikobia
5: 196-201.
Krieger, W., 1939. Die Desmidiaceen Europas mit Berucksich-
tigung der aussereuropaischen Arten. 2. Teil. In Raben-
horst’s Kryptogamenflora von Deutschland, Osterreich und
der Schweiz 13(2): 1-117.
Lind, Edna M., 1971. Some desmids from Uganda. Nova
Hedwigia 22: 535-585.
Scott, A. M., Gronblad, R. & Croasdale, Hannah, 1965.
Desmids from the Amazon Basin, Brazil. Acta Bot. Fenn.
69: 1-94.
Stafleu, F. A. (Chairman), 1972. International Code of Botanical
Nomenclature. Utrecht: A. Oosthoek's Uitgeversmaat-
schappij N.V.
Thomasson, K., 1960. Notes on the plankton of Lake Bangweulu
Part 2. Nova Acta R. Soc. Scient. Upsal. 17: 1-43.
Turner, W. B., 1892. The freshwater algae (principally Des.
midieae) of East India. K. Svenska Vetensk. -Akad. Hand-
25 : 1-187.
West, W. & West, G. S., 1895. The freshwater algae of Mada-
gascar. Trans. Linn. Soc. Lond. (Bot.) 5: 41-90.
242 FRESHWATER ALGAE OF SOUTHERN AFRICA. IV. SOME MICRASTERIAE FROM RHODESIA, INCLUDING A
NEW SPECIES
Figs 1-4. — Micrasterias schweickerdtii ; 4, semicell showing spines in surface view.
M. ISABELLA CLAASSEN
243
Figs 5-8. — Micrasterias schweickerdtii.
244 FRESHWATER ALGAE OF SOUTHERN AFRICA. IV. SOME MICRASTERIAE FROM RHODESIA, INCLUDING A
NEW SPECIES
Figs 9, 10. — Micrasterias radiata var. brasiliensis; 9, mature cell; 10, cell in divisional stage. 11-14, M. ambadiensis,
various specimens showing variation of lateral lobes.
Fig. 15. — Micrasterias crux-melitensis forma minor. 16, 17, M. decemdentata. 18-21, M. pinnatifida var. incudiformis ;
18, 19, front view of cell; 20. apical view of semicell; 21, basal view of semicell. 22, 23, M. tropica var. tropica.
M. ISABELLA CLAASSEN
245
Figs 24, 25. — Micrasterias radiata var brasiliensis; 24, mature cell; 25, cell after division with anomalous upper semicell. 26-29, M. ambadiensis,
various specimens showing variation of lateral lobes. 30, 31, M. tropica var. tropica.
Bothalia 12, 2: 247-250 (1977)
Asexual nuclear division in Neocosmospora*
K. T. VAN WARMELOf
ABSTRACT
A fungus isolated from soybean stem material showed marked similarities to two existing species of
Neocosmospora , i.e. N. vasinfecta E. F. Smith and N. africana von Arx. The processes of somatic nuclear division
in authentic cultures of these two species and the new isolate were examined to determine the nature of the
mechanism of nuclear division and whether there were any differences among the cultures. No significant
differences were observed. The divisions showed asynchronous anaphase disjunction but there was no evidence
of aneuploidy or irregular reconstitution of daughter nuclei. Nuclear division was interpreted as being strictly
mitotic.
RESUME
CA R YOCINESE ASEXUEE CHEZ NEOCOSMOSPORA
Une moisissure isolee de tiges de soya a montre des ressemblances marquees avec deux espices
existantes de Neocosmospora, so it N. vasinfecta E. F. Smith et N. africana von Arx. Les processus de
caryocmese somatique ont ete examines dans des cultures authentiques de ces deux especes et dans le
nouvel isolat pour determiner la nature du mecanisme caryocinetique et noter les differences entre cultures
s'il y en a. On n'a pas observe de differences significatives. Les divisions ont montre une dislonction
asynchrone a V anaphase , mais il ny avait aucun signe d'aneuploidie ou de reconstitution irreguliere
de noyaux-fils. La caryocinese a ete interpretee comme etant strictement mitotique.
REVIEW
Reported mechanisms of somatic nuclear division
in the fungi seem to fall into two basic categories,
i.e. divisions which are essentially mitotic, differing
only slightly from the classical concept, and non-
mitotic divisions in which completely different
processes are operative.
Divisions in a large variety of fungi were shown to
differ from mitosis in higher plants only in that the
nuclear membrane was persistent throughout the
division (Thyagarajan, Conti & Naylor, 1962; Moor,
1966; Robinow & Marak, 1966; Heath & Greenwood,
1968; McManus & Roth, 1968; Aist, 1969; Aldrich,
1969; van Winkle, Biesele & Wagner, 1971). The
spindle was thus fully intranuclear (Ichida & Fuller,
1968; Motta, 1969; Zickler, 1970).
Persistence of the nuclear membrane was, however,
not an invariable condition, as fungi were reported
in which the membrane broke down during division
(Robinow, 1963; Namboodiri & Lowry, 1967; Motta,
1969; Brushaber & Jenkins, 1971).
An additional difference between somatic divisions
in fungi and higher plants was the variable presence
of centrioles. Several fungi, representative of widely
differing taxonomic groups, were reported as lacking
centrioles (Namboodiri & Lowry, 1967; McManus &
Roth, 1968; Aldrich, 1969) whereas their presence was
demonstrated in others (Moor, 1966; Robinow &
Marak, 1966; Brushaber & Jenkins, 1971; van
Winkle et al., 1971).
Despite the differences referred to above, however,
the divisions in a large number of fungi have been
described as essentially mitotic (Robinow, 1963;
Hosford & Gries, 1966; Knox-Davies, 1966, 1967;
Finley, 1970; Brushaber & Jenkins, 1971, van
Warmelo, 1971).
The actual arrangement of chromosomes imme-
diately prior to, and during, separation has been the
subject of intensive investigation and a large number
of different mechanisms of chromosomal separation
have been proposed as a result.
The formation of typical metaphase plates was
reported (Robinow, 1963; Finley, 1970) and also the
separation of discrete chromatids on a well-defined
* Based on a Ph.D. (Agric.) thesis submitted to the University
of Stellenbosch, 1973. Promoter: Prof. P. S. Knox-Davies,
Ph.D. (Wis.).
t Rand Afrikaans University, P.O. Box 524, Johannesburg.
spindle (Knox-Davies, 1966, 1967; Ichida & Fuller,
1968; McManus & Roth, 1968; Motta, 1969;
Brushaber & Jenkins, 1971). Aist (1969), however,
maintained that instead of forming a true metaphase
plate the chromosomes became attached to the
spindle at different points. During anaphase separation
the chromatids thus became strung out on the
spindle.
Instead of separate chromosomes, the presence of a
single coherent strand, formed by the linked chromo-
somes has been reported (Weijer, Koopmans &
Weijer, 1965; Dowding, 1966; Weijer & Weisberg,
1966; Brushaber, Wilson & Aist, 1967; Laane, 1967;
Namboodiri & Lowry, 1967; Heale, Gafoor & Raja-
singham, 1968; Brushaber & Jenkins, 1971). The
single nuclear strand is thought to replicate to form
a double strand which then separates in a number of
ways. Movement of each replicated strand on a well
defined spindle was reported by Heale et al. (1968).
Spindles were, however, apparently absent in the other
fungi showing filamentous nuclei. Shearing of chro-
matids by cytoplasmic streaming was suggested by
Weijer et al. (1965) but, whereas this proposal received
some support (Laane, 1967), it has not been
generally accepted. In the absence of a spindle
the exact mechanism of chromatid disjunction and
movement is not yet fully understood.
Judging from the conflicting descriptions given
above it seems possible, as suggested by Bracker
(1967), that there may be a number of mechanisms of
somatic nuclear division in the fungi, instead of one
common process.
MATERIALS AND METHODS
Three cultures were examined in this investigation:
1. Neocosmospora vasinfecta E. F. Smith; CBS
237.75.
2. Neocosmospora africana von Arx; CBS 237.
3. Neocosmospora sp. isolated from soybean
stem, Pietermaritzburg, South Africa.
Referred to in the following text as “isolate
P.”
Somatic divisions were studied using the macerated
mycelium technique described by Ward & Ciurysek
(1962). After being stained using the HCl-Giemsa
technique (van Warmelo, 1971) the hyphae were
flattened under a coverglass which was then sealed
with paraffin oil.
248
ASEXUAL NUCLEAR DIVISION IN NEOCOSMOSPORA
Figs 1-8. — Mitosis in Neocosmospora vasinfecta, x3000. 1, early prophase; 2, prophase
with clearly visible chromosomes; 3, late prophase with short chromosomes; 4, mid
metaphase with six distinguishable chromosomes; 5, metaphase/anaphase; 6, mid
anaphase showing chromosomes between clearly visible centriolar plaques; 7, early
telophase with spindle bridge apparently enclosed within nuclear membrane;
8, early telophase.
Figs 9-16. — Mitosis in Neocosmospora africana, x 3000. 9, early prophase with visible
chromosomes; 10, prophase; 11, prometaphase in polar view with visible centriolar
plaques (arrowed); 12, very early metaphase with forming spindle (arrowed);
13, early metaphase; 14, anaphase; 15, early telophase with spindle bridge; 16,
telophase.
Figs 17-24. — Mitosis in Neocosmospora isolate P, x 3000. 17, early prophase with visible
chromosomes and nuclear membrane; 18, prophase in large hypha with clearly
visible chromosomes; 19, prophase with shortened chromosomes; 20, mid metaphase
with formed spindle; 21, early anaphase; 22, late anaphase with chromosome
disjunction almost completed; 23, late anaphase showing residual interzonal fibres;
24, late telophase.
K. T. VAN WARMELO
249
RESULTS
As the mechanisms of somatic division in the
three cultures did not show any significant differences,
the processes of division will not be described
separately. Individual isolates will be highlighted
only where necessary.
The interphase nuclei were large and typical. The
onset of prophase was shown by the delimitation of
chromosomes within the nuclei (Figs 1, 9 and 17).
Initially long and thin, the chromosomes were
shorter and more distinct at mid-prophase (Figs 2,
10 and 18). Nucleoli which were clearly distinguishable
at early prophase, were usually absent at mid-
prophase. The size of the somatic cell appeared to
affect the size of the nucleus. In isolate P (Fig. 18)
cells of large diameter were found in which the
nuclei were much larger, and the chromosomes much
clearer, than in the more common narrow hyphae.
At late prophase the chromosomes were appreciably
shorter than at early prophase, but could not be
counted (Figs 3 and 19). Occasional persistent
nucleoli were seen at this stage.
At prometaphase (Fig. 11) centriolar plaques were
sometimes distinguishable.
During early metaphase the chromosomes had
condensed further and were shorter than at late
prophase (Fig. 12). At metaphase they were situated
midway between the two centriolar plaques and
incipient spindles were observed (Figs 12 and 13).
At mid-metaphase the spindle was clearly distin-
guishable (Figs 5 and 20).
Occasionally individual chromosomes were distin-
guished at metaphase (Figs 4 and 20) and a count
at this stage gave an estimated number of six.
Anaphase was a variable stage and chromosome
separation appeared to be asynchronous, as a variety
of nuclear figures were found (Figs 6, 14, 21 and 22).
At late anaphase the interzonal fibres between the
terminal chromosome aggregations were occasionally
observed (Fig. 23).
At early telophase the two daughter nuclei became
reconstituted but were frequently connected by a
chromosome or spindle bridge (Figs 7 and 15)
apparently still enclosed within the nuclear membrane.
The bridge then broke and shortened (Fig. 8). The
divisions thus appear to be entirely intra-nuclear.
Mid- and late-telophase nuclei (Fig. 16) were dense
and smaller than post-division interphase nuclei
(Fig. 24) which were identical with pre-division
interphase nuclei.
At no stage were nuclear strands observed or
stages seen which would have suggested linking-up
of individual chromosomes.
DISCUSSION
No significant differences in nuclear division were
found to occur in these three cultures. This agrees
with their close similarity in other respects.
Due to the small diameter of most somatic hyphae
there is probably insufficient space available for the
formation of a typical metaphase plate, as found in
higher organisms, and for the simultaneous disjunction
and movement of chromatids on the spindle. The only
mechanism which would ensure an equal distribution
of chromatids under such conditions would be a
sequential or asynchronous separation. Pairs of
chromatids would then separate and move away from
the central spindle area before separation of the next
chromatid pair, thus ensuring non-interference by
non-sister chromatids destined for different daughter
nuclei.
Although anaphase separation was asynchronous
there was no evidence of irregular chromosome
disjunction or aneuploidy. This was deduced from the
absence of lagging chromosomes or fragments at late
telophase or interphase, indicating complete recon-
stitution of daughter nuclei, the constancy of chromo-
some numbers and the phenotypic stability of the
cultures.
The consistent presence of observably separate
chromosomes during nuclear division, coupled with
the absence of stages showing linking of chromosomes,
indicates that somatic nuclear division in Neocosmos-
pora can be interpreted as strictly mitotic.
ACKNOWLEDGEMENTS
This study was supported by research grants from
the Rand Afrikaans University, Johannesburg and
the Council for Scientific and Industrial Research,
Pretoria.
UITTREKSEL
n Swamsoort afkomstig van sojaboon weefsel het
duidelike ooreenkomstes getoon met twee bestaande
Neocosmospora soorte, nl. N. vasinfecta E. F. Smith
en N. africana von Arx. Die somatiese kerndelings-
prosesse in outentieke kidture van hierdie twee
organismes en in die nuwe isolaat is ondersoek om
vas te stel wat die delingsmeganismes was en of daar
verskille tussen die kulture aanwesig was. Geen
wesenlike verskille tussen die kulture is opgemerk nie.
Die delings het asinkroniese anafaseskeidings getoon
maar daar was geen tekens van aneuploiedie of onreel-
matige vorming van die dogterkerne nie. Die meganisme
van kerndeling is suiwer mitoties.
REFERENCES
Aist, J. R., 1969. The mitotic apparatus in Fungi, Ceratocystis
fagacearum and Fusarium oxysporum. J. Cell Biol. 40:
120-135.
Aldrich, H. C., 1969. The ultrastructure of mitosis in myxamoe-
bae and plasmodia of Physarum flavicomum. Am. J. Bor.
56: 290-299.
Bracker, C. E., 1967. Ultrastructure of fungi. A. Rev.
Phytopath. 5: 343-374.
Brushaber, J. A. & Jenkins, S. F., (Jr.) 1971. Mitosis and
clamp formation in the fungus Porta monticola. Am. J. Bot.
58: 273-280.
Brushaber, J. A., Wilson, C. L. & Aist, J. R., 1967. Asexual
nuclear behavior of some plant pathogenic fungi. Phyto-
pathology 57 : 43-46.
Dowding, E. Silver, 1966. The chromosomes in Neitrospora
hyphae. Can. J. Bot. 44: 1121-1125.
Finley, D. E., 1970. Somatic mitosis in Ceratobasidium flaves-
cens and Pellicularia koleroga. Mycologia 62: 474-485.
Heale, J. B., Gafoor, A. & Rajasingham, K. C., 1968. Nuclear
division in conidia and hyphae of Verticillium albo-atrum.
Can. J. Genet. Cytol. 10: 321-340.
Heath, I. B. & Greenwood, A. D., 1968. Electron microscopic
observations of dividing somatic nuclei in Saprolegnia .
J. Gen. Microbiol. 53 : 287-289.
Hosford, R. M. & Gries, G. A., 1966. The nuclei and para-
sexuality in Phymatotrichum omnivorum. Am. J. Bot. 53:
570-579.
Ichida, A. A. & Fuller, M. S., 1968. Ultrastructure of mitosis
in the aquatic fungus Catenaria anguillulae. Mycologia 60:
141-155.
Knox-Davies, P. S., 1966. Nuclear division in the developing
pycnospores of Macrophomina phaseoli. Am. J. Bot. 53:
220-224.
Knox-Davies, P. S„ 1967. Mitosis and aneuploidy in the vegeta-
tive hyphae of Macrophomina phaseoli. Am. J. Bot. 54:
1290-1295.
Laane, M. M., 1967. The nuclear division in Penicillium expan-
sum. Can. J. Genet. Cytol. 9: 342-351.
McManus, Sister M. A. & Roth, L. E„ 1968. Ultrastructure
of the somatic nuclear division in the plasmodium of
the Myxomycete Clastodenna debaryanum. Mycologia 60:
426-436.
250
ASEXUAL NUCLEAR DIVISION IN NEOCOSMOSPORA
Moor, H., 1966. Ultrastrukturen im Zellkern der Backerhefe
J. Cell Biol. 29: 153-155.
Mot'ta, J. J., 1969. Somatic nuclear division in Armillaria
mellea. Mycologia 61 : 873-886.
Namboodiri, a. N. & Lowry, R. J., 1967. Vegetative nuqear
division in Neurospora. Am. J. Bot. 54: 735-748.
Robinow, C. F., 1963. Obervations on cell growth, mitosis, and
division in the fungus Basidiobolus ranarum. J. Cell Biol.
17: 123-152.
Robinow, C. F. & Marak, J., 1966. A fiber apparatus in the
nucleus of the yeast cell. J. Cell Biol. 29: 129-151.
Thyagarajan, T. R., Conti, S. F. & Naylor, H. B., 1962.
Electron microscopy of Rhodotorula glutinis. J. Bad. 83:
381-394.
Van Warmelo, K. T., 1971. Somatic nuclear division in
Stemphylium botryosum. Bothalia 10: 329-334.
Van Winkle, W. B., Biesele, J. J. & Wagner, R. P., 1971. The
mitotic spindle apparatus of Neurospora crassa. Can. J.
Genet. Cytol. 13: 873-887.
Ward, E. W. B. & Ciurysek, K. W.. 1962. Somatic mitosis in
Neurospora crassa. Am. J. Bot. 49: 393-399.
Weijer, J., Koopmans, A. & Weijer, D. L., 1965. Karyokinesis
of somatic nuclei of Neurospora crassa. III. The juvenile
and maturation cycles (Feulgen and crystal violet staining).
Can. J. Genet. Cytol. 7: 140-163.
Weijer, J. & Weisberg, S. H., 1966. Karyokinesis of the somatic
nucleus of Aspergillus nidulans. I. The juvenile chromosome
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Zickler, Denise, 1970. Division spindle and centrosomal
plaques during mitosis and meiosis in some Ascomycetes.
Chromosoma 30: 287-304.
Bothalia 12,2: 251-259 (1977)
Notes on African plants
VARIOUS AUTHORS
ARACEAE
A NEW SPECIES OF GONATOPUS FROM SOUTHERN AFRICA
Gonatopus rhizomatosus Bogner & Oberm. sp. nov.,
G. boivinii ( Decne.) Engl, affinis, sed rhizomate
cylindraceo longo horizontali non globoso et petiolo
non geniculato differt.
Planta rhizomatosa 20-40 cm alta. Folium unum
annuum decompositum proteranthum; petiolus tenuis
15-25 cm longus; lamina a basi ternata supra 1-2
divisa; pinnae oppositae vel suboppositae decurrentes.
Spadix breve pedunculata c. 10 cm longa. Spatha
angusta c. 7 cm longa margine ad basi libero. Flores
masculi superiores; tepala paribus oppositis semi-
prismatica truncata 3 mm longa. Staminum filamenta
ponnata. Flores steriles in medio masculini et feminei.
Flores feminei inferiores. Gynoecium ampulliformum
bilocularum; ovulum anatropum. Bacca oblongo-
globosa c. 15 mm longa; semen anguste ellipsoideum,
12 mm longum.
Type: Transvaal, 2531 (Komatipoort): 5 km S. of
Kaalrug Police Station near Swedish Mission (-DA),
Codd 7814 (PRE, holo.; M, iso.).
Herbaceous plant producing annually one leaf and
later beside it 1 or rarely 2 inflorescences. Rhizome
horizontal, 20 cm long and 3 cm in diameter, or longer,
cylindrical, tuberous, somewhat contracted irregularly
at intervals, forming much-branched mats, brown
outside with white flesh; roots scattered, fairly thick.
Fig. 1. — Gonatopus rhizomatosus.
Eastern Transvaal ( Codd
7814), x}.
252
NOTES ON AFRICAN PLANTS
Fig. 2. — Gonatopus rhizomatosus. 1, male perianth, x 6; 2,
stamens and sterile ovary from above, x 10; 3, stamens
seen from side, xlO; 4, female perianth, x6; 5, outer
tepal x 6; 6, inner tepal x 6; 7, ovary, X 6; 8,
longitudinal section through ovary, x 10; 9, fruits, x^.
( Moll 4974A).
Fig. 3. — Pollen grains (x500) of Gonatopus rhizomatosus
Photo: W. Barthlott.
VARIOUS AUTHORS
253
Leaf e rect, with a petiole 15-25 cm long, dull grey with
lighter mottling, surrounded by cataphylls at the base;
lamina somewhat fleshy, decompound, 3- branched
at the base, once or twice branched above it, pinnae
opposite or subopposite, linear to oblong, attenuate
above and below, 4-8 cm long, all or only the terminal
decurrent on rhachis, often with a small side-lobe.
Spadix on a short peduncle c. 10 cm long, grey,
mottled; spathe constricted, green in bud, turning
pinkish buff with black stripes but soon drying up, c.
7 cm long, closely enveloping spadix, apiculate, not
fused below, the upper part reflexed at anthesis, the
lower enclosing the female part for some time,
dropping off when fruit is set. Male flowers compressed
in spiral series on upper half of cylindrical, obtuse
spadix; tepals in 2 opposing free pairs, semi-prismatic,
thick, truncate, c. 3 mm long; stamens 4, with the
filaments fused into a tube, surrounding the sterile,
clavate gynoecium; anthers arranged in a circle,
thecae opening apically towards the centre. Pollen
grains depressed globular, 95-1 10// x 30-40//, meri-
dionosulcate, exine sparsely covered with very small
foveolae. Female flowers on lower part of spadix, with
sterile flowers in between male and female flowers;
tepals similar to male flowers; stamens absent;
gynoecium flask-shaped, laterally compressed, 2-
locular with an anatropous basal ovule in each locule;
style short; stigma discoid, large, green, just protruding
from perigon. Berries bilocular, oblong-globose, c.
15 mm long, in a globose cluster surrounded basally
by the persistent tepals and unfertilized flowers, walls
soft, thin. Seed narrowly ellipsoid, 12 mm long, coat
thin, without endosperm. Chromosomes: 2n=c.68
(N. Jacobsen). Figs 1, 2 & 3.
Eastern Transvaal, northern Natal, Mozambique,
Rhodesia; common in undergrowth of dune forest in
northern Natal, often in shady rock pockets in low-
lying bushveld areas of eastern Transvaal; flowering
November to February.
Transvaal. — 2331 (Phalaborwa): Gorge (-DD), Van der
Schijff 2387. 2431 (Acornhoek): 21 km E. of Skukuza (-DC),
Codd 5045. 2531 (Komatipoort) : 4 km W. of Lower Sabie
Camp (-BB), Codd 5707 (M, PRE); Kaap Muiden (-CB),
Mogg 13687 ; 5 km S. of Kaalrug Police Station near Swedish
Mission (-DA), Codd 7814 (PRE, holo.; M. iso.).
Natal. — -2632 (Bela Vista): Mtombeni Forest, slopes facing
Nhlange Lake (-CD), Tinley 396. 2731 (Louwsburg): Josini
Dam, slopes (-BD), Strey 5278. 2732 (Ubombo): Ngwavuma,
on road to Ndumu (-AA), Venter 5215; Lebombo foot hills on
road to Pongola River (-AC), Strey 6580; Makatini flats near
Mbazwane (-BC), Vahrmeijer & Toelken 208. 2831 (Nkandla):
Umfolozi Game Reserve (-BD), White 10357; 16 km W. of
Empangeni on Melmoth Road (-DD), Moll 4974a. 2832
(Mtubatuba): Hluhluwe Game Reserve (-AA), Ward 1967;
near Mtubatuba (-AC), Codd 9619.
Mozambique. — Inhaca Island, M. Moss sub. J. 28428.
Rhodesia. — Beitbridge district, 16 km S. of Lundi River,
Wild 7610.
Two species of Gonatopus occur in southern Africa,
namely G. boivinii (Decne.) Engl., a tropical eastern
African species, which reaches its southernmost limit
in northern Natal, and G. rhizomatosus, the species
here described, which has been recorded from northern
Natal, eastern Transvaal Lowveld, Mozambique and
Rhodesia.
In G. boivinii , a taller plant, the underground part
consists of a globose often depressed tuber, the petiole
forms a swollen articulation in the middle and the
decompound lamina has sessile or petiolate paired
pinnae, which are not decurrent. In G. rhizomatosus
the underground part consists of a long horizontal
tuberous rhizome, the petiole is without a swollen
central articulation and the decompound lamina has
the pinnae opposite or subopposite and decurrent.
There is also a difference in the size of the pollen
grains for they are much larger than those of G. boivinii
and the exine is more sparsely covered withf oveolae.
Mr Josef Bogner of the Botanical Garden of
Munich, co-author of G. rhizomatosus , is an authority
on the Araceae. He assisted me most generously in
clarifying the position of this species and the tropical
ones described by A. Pet?r under the latter’s genus
Microculcas. Mr Bogner will deal with these taxonomic
problems at a future date. He assures me that our
southern rhizomatous tpecies differs from Microculcas
marattioides described by Peter from Tanzania. The
latter also possesses a horizontal rhizome but, in
addition, develops long stolons which swell up to
about the thickness of a finger and produce a leaf at
their ends. The petiole too, is swollen basally, but
becomes attenuated and thin above.
A. A. Obermeyer
ASCLEPIADACEAE
A NEW SPECIES OF CARALLUMA FROM THE CAPE
Caralluma multiflora R. A. Dyer sp. nov., C.
mammilliari (L.f.) N.E. Br. affinis, corolla alabastro
plusminusve oblonga, obtusa; corollae lobis replicatis
carinatis, plusminusve oblongis, apicem versus
incurvis, carina infra medium et fauce dense papillosis
distinguitur.
Planta carnosa ramosa, usque ad 15 cm alta;
caules 4-5-angulati, circiter 2 cm crassi, tuberculati;
tubercula triangulata, 6-7 mm prominentia, apicem
versus indurata, acuta. Flores multi, fasciculati.
Corolla alabastro plusminusve oblonga, obtusa,
5-angulata, circiter 1,5 cm longa, glabra, atropur-
purea, breviter tubulata; tubus campanulatus, circiter
4 mm longus, intus pallidus, sparse pubescens et
maculatus; faux dense papillosa; lobi plusminusve
oblongi, erectopatentes, apicem versus incurvi,
replicati, carinati; carina infra medium papillosa.
Corona breviter campanulata; lobi exteriores suberecti,
profunde bifidi, dentibus 0,5 mm longis; lobi
nteriores incumbenti-erecti, basi in lobulum sub-
quadratum vel ovatum producti. Pollinia circiter
0,25 mm longa. Folticuli 2 (1), 13-14 cm longi,
7-8 mm diam, longistrorsum maculati.
Type. — Cape, 3119 (Calvinia): Kareeboomfontein,
west of Rebunie (-DA) 17th October 1975, W. J.
Hanekom 2475 (PRE, holo.).
Succulent plant up to about 15 cm tall, freely
branching and rooting from the basal branches;
branches 4-5-angled, prominently tuberculate along
the angles, with a spread of 2,5-2,75 cm, bluish-green
to purplish red-brown; tubercles triangular in side
view, spreading 6-7 mm, with a sharp hard apex.
Flowers mainly from flowering eyes towards the apex
of branches between or along the angles, in fascicles
of up to 12 flowers together, opening more or less
together; pedicels 4-5 mm long. Sepals linear-
lanceolate, about 3 mm long. Corolla in bud more or
less oblong in outline, but broadest slightly above
middle, 5-angled, 1 ,5 cm long, glabrous outside, dark
maroon to black with short yellowish-green to light
254
NOTES ON AFRICAN PLANTS
coloured tube; tube campanulate, about 4 mm long,
with scattered hairs within and maroon-marked,
densely papillate round mouth of tube; papillae with
acute apex bent at right-angles; lobes more or less
oblong in outline, suberect, with incurving tips and
recurving margins, obtusely keeled down inner face,
with few papillae down keel towards base. Corona
shortly cup-shaped or campanulate at base; outer
lobes deeply bifid and alternating with spreading basal
lobule of inner corona-lobes, teeth of outer lobes about
0,5 mm long, suberect; inner corona-lobes about
2 mm long, incumbent-erect into a cone-shaped apex
above the staminal column, with a spreading ovate or
subquadrate basal lobe (variable) alternating with the
outer corona-lobes and about the same length.
Pollinia about 0,25 mm long with very short weak
connectives; carrier very shortly winged. Follicles
Fig. 4. — Caralluma multiflora. 1, open flower, x3; 2, corolla
opened out, x3; 3, papilla with sharp tip turning at
right-angles, xlOO; 4, corona, xl5; 5, pollinia and
carrier, x 60. ( Hanekom 2335).
(1) 2 on a separate plant without flowers, towards base
of branches, upright, 13-14 cm long, 7-8 mm thick,
longitudinally striped and mottled. Fig. 4.
Cape. — 31 19 (Calvinia): Kareeboomfontein, west of Rebunie-
kop (-DA), rocky ground with some protection from shrublets,
24/8/74, Hanekom 2335 ; 17/10/75, Hanekom 2475.
This is a relatively robust succulent which, like so
many members of the Stapelieae, is found on rocky
slopes in the halt-shade of shrublets. Under favourable
conditions in the field it may be so floriferous that the
flowers almost obscure the branches. Up to 12 flowers
are produced in fascicles from each flowering eye, all
developing together. It is presumed that under normal
conditions of warmth and sunshine, all flowers would
be open together, but this has not actually been
observed. The first plants collected by Mr W. J.
Hanekom flowered after a short period in cultivation
at the Botanical Research Institute in Pretoria and
were not considered to be entirely normal. In 1975
Mr Hanekom brought two specimens direct from the
veld, one in the initial stages of flowering and the
other with several follicles. A few flowers were open
with the lobes erect-spreading, whereas those not open
showed a tendency for the corolla-lobes to remain
slightly cohering at the tips. The papillae-like hairs on
the inside of the corolla have an unusual shape, being
bent approximately at right angles about the middle
and acuminate. The corolla is dark maroon to black.
In spite of enquiries among Cape collectors, no
record of the species other than the present one seems
to have been made. One wonders how it happens that
such an interesting species should remain unheralded
for so long.
The fruiting specimen brought by Mr Hanekom
showed the follicles arising from flowering eyes
towards the base of the branches, whereas the flowers
on the other specimen were from younger flowering
eyes towards the tips of the branches. This illustrates
a feature of Stapelieae, where the fertilized ovary
undergoes a protracted resting period, after which the
follicles elongate fairly rapidly to maturity. The
number of follicles is usually very small by comparison
with the large number of flowers. This is a result of
the highly specialized and frequently unsuccessful
mechanism for insect pollination. But nature has
introduced compensations by providing an abundance
of seeds in each follicle: each seed is attached to a
very light and delicate cluster of hairs, which act as
parachutes for wide seed dispersal.
R. A. Dyer
TWO NEW SPECIES OF BRACHYSTELMA
Brachystelma canum R. A. Dyer, sp. nov., B.
macropetalo (Schltr.) N.E. Br. affine, foliis oblongo-
ellipticis breviter pubescentibus canis, floribus minori-
bus lobis intus glabris, corona breviter campanulata,
lobis interioribus parvis pulvinatis differt.
Herba erecta, usque 30 cm alta, breviter pubescens,
basi 1-2 ramosa, (? radicibus fasciculatis incrassatis),
internodiis 2-4 cm longis. Folia elliptico-oblonga,
2-4 cm longa, 5-10 mm lata, sensim basin versus
attenuata, molliter pubescentia cana, marginibus
leviter undulatis, plus minusve plicatis. Flores (1)
2 extra axillares producti; pedicelli circiter 1 cm longi.
Sepala lineari-lanceolata, circiter 4 mm longa. Corolla
9-11 mm longa, basi 1,5 mm connata; lobi lineari-
lanceolati, extus pubescentes, intus glabri, leviter
replicati. Corona 0,25 mm supra corollae basin
expansa, campanulata, 1,75-2 mm diam., 5-saccata
margine integro; coronae lobi interiores parvi
pulvinati.
Type: Transvaal, 2625 (Delareyville): 25 km N.E.
of Setlagoli, on road to Mafeking, sandy Terminalia-
veld (-AB), rare, about 1300 m alt., 16th February
1956 /. P. H. Acocks 18774 (PRE, holo.).
Herb erect, up to about 30 cm tall, with underground
stem up to 6 cm long or more (roots not recorded but
assumed to be succulent, fascicled, more or less
cylindric or fusiform); branches 1-2 from the base,
unbranched above, shortly and softly pubescent,
basal internodes 2-4 cm long becoming gradually
shorter as growth continues. Leaves elliptic-oblong,
2-4 cm long, 5-10 mm broad, gradually tapering to
the base with no distinct petiole, finely pubescent, grey,
margins slightly undulate inclined to fold upwards.
Flowers usually 2 together, extra axillary, opening in
succession. Calyx divided to base, with segments
linear-lanceolate, about 4 mm long, pubescent.
Corolla 9-11 mm long, lobed almost to the base
(united for 1,5 mm); lobes linear-lanceolate, with
VARIOUS AUTHORS
255
margins somewhat replicate, finely pubescent on outer
surface, glabrous on inner surface. Staminal column
1 ,5 mm high. Corona appearing to arise 3- up staminal
column 1,5 mm high, more or less campanulate,
1,75-2 mm broad, forming 5 pockets with outer
margin entire; inner corona lobes represented by 5
swellings at base of filaments; filaments conspicuous,
oblong with slight narrowing at the middle. PoUinia
subpyriform, about 0,25 mm long with very short
connectives to carrier. Fig. 5.
Fig. 5. — Brachystelma canum. 1, staminal column and
corona, Xl5; la, outer margin of outer corona-pocket;
lb, rudimentary inner corona lobs pressed on base of
anther; lc, anthers; 2, pollinia, with carrier, X60.
( Acocks 18774).
This is a further species known only from a single
specimen collected by J. P. H. Acocks nearly twenty
years ago. Because of the sandy nature of the soil
the root system was comparatively deeply buried
below ground level and the collector did not record
whether it was a single tuber or a cluster of fleshy roots.
The habit of growth and floral structure indicate a
close relationship with B. macropetalum (Schltr.)
N.E. Br., and for this reason it is suggested that the
plant has a cluster of fleshy roots. This was one of the
characters on which Schlechter in Bot. Jahrb. 20,
Beibl. 51:50 (1895), established the genus Brachystel-
maria as distinct from Brachystelma R. Br., but N.E.
Brown in FI. Cap. 1908 did not uphold Schlechter’s
segregations.
Brachystelma ngomense R. A. Dyer, sp. nov., herba
tuberosa prostrata; corolla circiter 10 mm longa, infra
medium connata tubulata; corona late campanulata,
4 mm diam. 2,5-3 mm alta, margine incurvata
distinguitur.
Tuber subglobosa, 2-3 cm diam.; rami 1-3 annui
prostrati, usque 10 mm (cult. 20 mm) longi, sparsim
ramulosi, glabri vel minute pubescentes. Folia ovata
vel lanceolata, usque circiter 1,5 cm longa (cult.
2 cm x 1,5 cm), breviter petiolata, glabra. Flores 1-2
extra axillares producti; pedicelli 5-10 mm longi.
Sepala lanceolata, 2-3 mm longa. Corolla circiter
10 mm longa, infra medium connata, late campanu-
lata: tubus circiter 5 mm diam., intus albidus rubro-
maculatus; lobi ovato-triangularcs, ± 5 mm longi,
patentes, leviter replicati, atropurpurei, apice albido.
Corona exterior campanulata, 4 mm diam., 2,5-3 mm
alta, 5-marsupiiformis, margine incurvata, lobis
interioribus confluens; lobi interiores breves. PoUinia
±0,25 longa, subpyriformes, caudiculis brevissimis.
Type: Natal, 2731 (Louwsburg), Ngotshe district,
Ngome (-CD), near sawmill on rock-sheets, 7
December 1975, Hilliard & Burtt 8441 (PRE, holo.;
NU).
Tuber subglobose, 2, 0-3,0 cm diam., with 1-3
annual stems. Stems slender, prostrate, glabrous or
minutely pubescent, sparsely branched, about 10 cm
long (up to 20 cm under cultivation). Leaves ovate to
lanceolate, up to about 1 ,5 cm long (2 cmx 1 ,5 cm
under cult.) glabrous. Flowers 1-2, subaxillary;
pedicels ±1 cm long, ascending. Sepals lanceolate,
2-3 mm long. Corolla with the tube slightly bulging
in bud, 1 cm long, divided to about way; tube
campanulate, ±5 mm diam. with flatfish base, slightly
bulged inwards below the sinuses, making the mouth
obtusely 5-angled; white within and purple mottled;
lobes triangular-ovate, ±5 mm long, spreading-
recurved, concave on upper side towards base,
replicate towards apex, dark red or maroon, with the
apex a small white mucro. Corona campanulate,
4 mm diam., 2, 5-3,0 mm high, overtopping the
staminal column, forming 5 deep pockets, with
minutely toothed incurved outer margin, confluent
with the short incurved inner corona-lobes; inner
corona-lobes pressed to base of anthers. Pollinia
±0,25 mm long, subpyriform, with translucent upper-
inner margin, attached by very short caudicles to
carrier with minute lateral bulges. Fig. 6.
Fig. 6. — Brachystelma ngomense. 1, twig, natural size; 2,
corona, x7,5; 3, pollinia, with carrier, x60. ( Hilliard &
Burtt 8441).
This species was discovered by Dr Olive Hilliard
and Mr Bill Burtt on a collecting expedition in
December 1975, when they were asked to make records
of any form of Brachystelma pulchellum (Harv.)
Schltr. which they might encounter. B. ngomense
seems to have no close relationship to any known
species. Several tubers were collected in Natal near
Ngome in a small area on the edge of sheets of exposed
rock, but no plants were seen in the open veld.
The corolla-lobes were described as rich dark satiny-
red, while inside the tube was white with crimson
mottling; the corona was dull mustard, overlaid red.
A tuber flowered at the Botanical Research Institute in
February 1976, when it was figured for eventual
publication in Flowering Plants of Africa.
R. A. Dyer
CEROPEGIA MAFEKINGENSIS, A NEW COMBINATION
In Flora Capensis 4,1:854 (1908) N. E. Brown
described the species Brachystelma mafekingense. He
based it on a small branch preserved in formalin
received from Dr S. Schonland at the Albany Museum,
Grahamstown. Dr Schonland, later Professor of
Botany, Rhodes University, had received a plant from
Mr Graham Green at Mafeking in November 1906
and had divided it between the Albany Museum
256
NOTES ON AFRICAN PLANTS
collection and the Royal Botanic Gardens Kew. A
scrap of material of less than 2 cm high has remained
in a capsule for nearly 70 years in the Albany Museum
with no record of its distribution other than near
Mafeking in the north-western Cape on the border of
Botswana.
My work on the genus Brachystelma has been
disjointed, because it has been a sporadic time filler
between many other projects. Nevertheless, from time
to time in recent years I have been specially curious to
know what relationship B. mafekingense has to other
species, since from Brown’s description it seemed to
be an odd man out.
Without this problem in mind, however, the Dinter
material of Brachystelma in the South African
Museum Herbari am, was borrowed from the National
Botanic Gardens, Kirstenbosch in 1969. Two dwarf
specimens puzzled me particularly at the time,
Dinter 2701 and an unnumbered one. Dinter 2701
from near Grootfontein in South-West Africa had
first been named in manuscript by Dinter as Ceropegia
sp. which he later changed to Blepharanthera nigra.
The second specimen although manifestly the same
species, bears the name B/epharoste/ma avasmontanum
Dinter. This was from the Auasberge south of Wind-
hoek. A note on the sheets indicated that P. G. Green-
way had examined the specimens in 1924 and had not
been able to name them nor was E. P. Phillips prepared
to do so when he studied them 1940. Because of my
own indecision in classifying them in 1969, no mention
of them was made in my article, including Dinter’s
other specimens, in Bothalia 10,2:373 (1971).
Belatedly in 1974, 1 became aware of the publication
of a species under the name Ceropegia patriciae
W. Rauh and G. Buchloh in Kakteen und andere
Sukkulenten (1964). This species was based on a
solitary specimen collected near Hammanskraal some
40 kilometres north of Pretoria on a joint expedition
by Dr Rauh and Dave and Patricia Hardy. In spite of
the 1600 km odd gap in the distribution records,
I had no hesitation in identifying Dinter 2701 and its
companion as specifically equal to Ceropegia patriciae.
The recorded distribution of C. patriciae from
northern and central South-West Africa via the
north-eastern Cape to the northern Transvaal is
by no means unique. Species such as Brachystelma
dinteri Schltr.have a very similar recorded distribution
pattern.
In 1975 all the material of Brachystelma was
borrowed from the Albany Museum, Grahamstown.
It did not take long to establish that B. mafekingense
N.E. Br. is conspecific with Ceropegia patriciae
Rauh & Buchloh, with the former specific epithet
taking priority. The question arose into which of the
two genera the species should be classified. Both
Brachystelma and Ceropegia embrace a wide range of
corolla and corona forms and the relative lengths of
the corolla-tube and -lobes are the main distinguishing
features. The distinction between the genera is not
always clear-cut such as in the present case but, in my
opinion, the weight of evidence is in favour of
Ceropegia , with C. pygmaea Schinz being the nearest,
yet distant, known relative. This makes it necessary to
validate the new combination Ceropegia mafekingensis ,
which is done below. Among the material of the genus
Brachystelma borrowed in 1975 from the Bolus
Herbarium were two specimens collected by Dr
F. Z. van der Merwe, Nos 46 and 92. They were sent
to the Bolus Herbarium in 1942 from a bushy plain
near Zeerust only about 50 km from the type locality
of B. mafekingense, which they were found to match
very closely.
Ceropegia mafekingensis (N.E. Br.) R. A. Dyer
comb. nov. Type: Cape, near Mafeking, Green sub
GRA 1683 (K, holo.; GRA1).
Brachystelma mafekingense N.E. Br. in FI. Cap. 4,1 : 854
(1908).
Ceropegia patriciae Rauh & Buchloh in Kakteen und andere
Sukkulenten 8:151 (1964). Type: Transvaal, near Hammans-
kraal, Rauh 12369 (HEID). C. sp. Dinter ms. (No. 2701).
Blepharanthera nigra Dinter ms. (No. 2701).
Blepharostelma avasmontanum Dinter ms. (specimen without
number).
Tuber ±8 cm diam., more or less depressed, 0-7 cm
below ground, producing one or mo;e annual stems.
Stems branching from near base and appearing tufted,
1,5-5 cm high, puberulous. Leaves tapering into a
short petiole or rounded at the base, oblong-lanceolate,
spreading, 7-30 mm long, up to 7 mm broad, with
margins half folded upwards, ± undulate, puberulous
below, glabrous above. Flowers in 10-20-flowered
umbellate cymes, the last terminal; pedicels 3-8 mm
long, puberulous. Sepals narrowly lanceolate, 2-4 mm
long. Corolla 10-12 mm long, divided to more than \
way; tube 4-6 mm long, 3-3,5 mm diam., obtusely
5-angled, slightly narrowed to the mouth, outside
minutely puberulous or papillate on the upper part,
maculate with dark purple, glabrous within, yellow
and purple punctate; lobes 6-7 mm long, free at tips,
connivent at first, becoming slightly spreading,
obovate-oblong, ±2 mm broad, auriculate at base,
inflexed, acute at apex, margins replicate, minutely
puberulous outside, glabrous, verrucose, and blackish
on inner surface. Corona campanulate at base;
outer lobes forming 5 pockets with the outer margin
extending into lobules behind the base of the inner
corona-lobes; inner corona-lobes arising from within
the base of the outer corona, linear, obtuse, 2 mm
long, incumbent-erect, much overtopping the staminal
column with obtuse connivent tips minutely papillate.
Pollinia globose-pyriform, ±0,25 mm long, with
translucent beaked upper margin, with short, delicate
caudicles and small carrier.
Cape. — 2525 (Mafeking): near Mafeking, Nov. 1906, Green
sub GRA 1683 (GRA).
Transvaal. — 2526 (Zeerust): bushy plain near Zeerust, Van
der Merwe 46; 92 (BOL). 2528 (Pretoria): Hammanskraal,
Rauh 12369 (HEID).
S.W.A. — 1918 (Grootfontein): near Grootfontein Dinter
2701 (SAM); 2217 (Windhoek) Auasberge, Dinter s.n. (SAM).
Two statements in Brown’s original description
helped to confuse my concept of the species. Firstly,
the statement that the flowers were in a terminal,
10-12-flowered umbel and secondly, that the stems
were “richly branched from near the base 4-7 cm
above the tuber (Schonland)”. The flowers are falsely
terminal and the 4-7 cm length refers to the depth of
the tuber below ground level. The height of the stem
above ground of the type was only 1,5-2 cm. Rauh
and Buchloh state that the stem may be up to 5 cm
long in C patriciae, but in the single specimen they
cite the tuber was more or less at ground level.
In conclusion, for the historical record. Miss M.
Gunn was able to supply the following information
about Mr Graham Green, who collected the type
material of C. mafekingensis. Mr Green was appointed
as a clerk in the Cape Colonial Service in 1887.
Most of his appointments were in the eastern Cape,
including Grahamstown. He was promoted to the
post of magistrate of Mafeking in 1903, whence in
1906 he despatched the type material to the Albany
Museum in Grahamstown.
I wish to express my appreciation of the loan of the
material, which made this investigation possible.
R. A. Dyer
VARIOUS AUTHORS
257
CYPERACEAE
CYPERACEAE NEW TO THE FLORA OF NATAL
Since the publication of Ross’s Flora of Natal ( 1 972)
two species of Cyperaceae new to the province have
been recorded:
Courtoisia cyperoides (Roxb.) Nees ( Vorster 2702;
2703) was found in April 1975 in the Mkuze Game
Reserve along the borders of pans, growing on wet
mud.
Material of Mariscus squarrosus (L.) C.B. Cl.
( Vorster 2700) was collected at the same time and
place. Another specimen, Arnold 865, was collected
about 20 km from Cathedral Peak on the road to
Estcourt in March 1975. In naming these specimens 1
follow Hooper in FI. W. Trop. Afr. ed. 2, 3:294
(1972), who reduced M. aristatus Rottb. to a synonym
of M. squarrosus.
Both these species are widely distributed throughout
the hot, dry areas of Africa and Asia. Although they
occur mostly in areas of low rainfall, they never occur
far from seasonal pans usually growing intermingled
with each other on wet mud along the shores. Both
species are known from Botswana, South West Africa
and the drier parts of Transvaal, and M. squarrosus
also from the high, dry parts of Lesotho.
P. Vorster
FABACEAE
SOME OBSERVATIONS ON ELEPHANTORRHIZA BURKEI AND E. ELEPHANT1NA
In a revision of the genus Elephantorrhiza Benth., in
Bothalia 11:252 (1974), it was stated that “£. burkei
appears to have smaller seeds than E. elephantina, but
more fruiting material is required to confirm this.”
In an attempt to glean further information on this
matter, populations of these two species growing
naturally in the Pretoria National Botanic Garden
were kept under observation from spring 1974 until
the end of winter 1975.
In E. elephantina the flowering racemes are usually
confined to the lower part of the stem with the result
that the pods are normally suspended just above the
ground or else rest on the ground where they tend to
be inconspicuous. In E. burkei, however, the flowering
racemes are borne on the branched stems some
distance from the ground and so the pods are conspi-
cuous, especially when mature or approaching
maturity.
Seeds of both species were collected, particularly
those of E. burkei about which less was known and
which were far more numerous. Considerable variation
in the shape of the seeds was noted in E. burkei,
seeds varying from elliptic to almost quadrate, the
latter as a result of the seeds being tightly compacted
and laterally compressed in the pods. The seed
dimensions recorded for E. burkei were 9-15 X 8-12 X
5-7 mm and those for E. elephantina 17-26X 1 3—1 8 x
6-13 mm. These measurements confirmed the
suspected existence of a difference in seed size between
the two species, the seeds of E. burkei apparently
being consistently smaller than those of E. elephantina.
As indicated in Bothalia l.c., the pods of E. burkei
tend to be longer and narrower than those of E.
elephantina.
At maturity the valves of the pods in both species
separate from the margins, the margins persisting as
an almost continuous but empty frame in a manner
reminiscent of most species of Entada (see illustration
in Palmer & Pitman, Trees S. Afr. 2:827, 1973). This
is particularly conspicuous in E. burkei where the
valves roll back and together with the margins usually
persist on the plant for many months. In E. elephantina
the pods tend to disintegrate and disappear more
rapidly.
A considerable amount of variation in the size of
individual plants was noted in the population of
E. elephantina. Scattered in amongst the population
were several plants that were substantially larger
than the surrounding plants, almost as though they
had been the recipients of a heavy application of
fertilizer. A cytogenetical study of this population
may yield interesting results and would give an
indication of whether or not polyploidy is involved.
J. H. Ross
FRULLANIACEAE (HEPATICAE)
TYPIFICATION OF FRULLANIA SYLVESTRIS
When Sim described Frullania sylvestris in Trans.
Roy. Soc. S. Afr. 15:40 (1926), no specimens were
cited. In the only subsequent work dealing with this
species, Arnell, Hepaticae of S. Afr. 138 (1963), no
type was designated or any specimens cited, although
the distribution is cited as “ Knysna. Natal,
several localities.”
In the main collection of Sim’s specimens, which is
housed at PRE, there is only one specimen of this
species, Sim s.n. in PRE Cryptogamic Herbarium
(Hepaticae) 1740, annotated as follows in Sim’s own
hand:
“ Frullania sylvestris Sim
Giants Castle, Natal. 5000'
Sept 1903, T.R. Sim.”
I conclude that Sim’s description was probably
based on this specimen, and consequently regard it
as the holotype.
P. Vorster
258
NOTES ON AFRICAN PLANTS
POACEAE
ODONTELYTRUM: A NEW GENERIC RECORD FOR SOUTH AFRICA
During an aquatic weed survey in December, 1974,
Mr F. de W. Brand, a member of the Transvaal
Provincial Administration, collected an aquatic grass,
Odontelytrum abyssinicum Hack., in the municipal
dam at Belfast (c. 2 000 m) in the eastern Transvaal.
This gathering, Brand 44, represents a new generic
record for South Africa. It has subsequently been
re-collected by the author at Belfast, Du Toit 1083.
The monotypic genus Odontelytrum , first described
by Hackel, was based on a Schimper specimen,
collected in Ethiopia (Abyssinia) in stagnant water
between Paffat and Dewra Tabor (c. 2700 m). The
nearest known locality outside Ethiopia is Oljoro
Nyuki on the Ngorongoro crater floor (c. 1900 m), in a
Cypm/s-swamp in Tanzania. The grass seems to prefer
a cool climate in stagnant or slow-flowing water. It is
possible that this grass spread to South Africa via
the eastern mountain ranges being dispersed by
waterbirds. This view is strengthened by the
observations of Mr Brand, who stated that waterbirds
relish the seeds and young shoots.
Although superficially resembling Oryza longistami-
nata, the wild rice, and Oryzidium barnardii, Odonte-
lytrum is closely allied to Pennisetum, a genus with
which it cannot be confused. On close examination,
the long “awn” of Odontelytrum proves to be an
elongate bristle of the involucre surrounding the
spikelet. In the case of Oryza and Oryzidium, the awn
arises from the lemma.
The specimen from the eastern Transvaal was
identified in time for the genus to be included in
Volume 2 of The Genera of Southern African
Flowering Plants by R. A. Dyer (1976). Readers are
referred to this publication for a full description of the
genus. To facilitate identification and to encourage
further observations on its distribution, a brief
diagnostic description is given here.
Odontelytrum abyssinicum Hack, in Oestr. Bot
Zeitschr. 48: 86 (1898); Stapf in Hook.Ic.P1.31.t. 3074
(1922). Type: Aethiopia, between Paffat and Dewra
Tabor, Schimper 1121.
Aquatic perennials, with soft spongy culms, leaves
light green or purplish, minutely scabrid. Inflorescence
a stout raceme, sheathed at the base. Spikelets
solitary, purple or straw-coloured, and enveloped by
an involucre of partially fused bristles. Spikelets
two-flowered, the lower male, the upper bisexual.
At maturity spikelets fall entire with the involucre.
P. C. V. Du T oi
RANUNCULACEAE
THE CORRECT NAME FOR ANEMONE CAPENSIS
In his write-up of Anemone capensis in Flower.
PI. Afr. 40: t. 1569 (1969), Oliver attributed the
binomial to Lamarck (1783), pointing out that
Lamarck made no mention at all of Atragene capensis
L. (1753) in his description of Anemone capensis in
Encycl. 1 : 164 (1783) and therefore Lamarck was the
sole author of Anemone capensis. Oliver also stated
that the combination Anemone capensis (L.) Harv.
(1860) based on Atragene capensis L. (1753) was a
later homonym of Anemone capensis Lam. and there-
fore illegitimate.
This is true, but unfortunately Oliver overlooked
Atragene tenuifolia L.f. (1781), which is conspecific
with Anemone capensis Lam. and antedates it by two
years. I have not been able to trace the holotype of
Atragene tenuifolia, but Thunberg specimen No. 12999
in Herb. Thunberg, Uppsala, which is probably an
isotype, agrees with our concept of Anemone capensis.
The correct name to use, therefore, is Anemon
tenuifolia (L.f.) DC. (1824).
The relevant synomy is as follows —
Anemone tenuifolia (L.f.) DC., Prodr. 1 : 18 (1824).
Type: Cape, Thunberg (holotype not traced, but
isotype probably specimen No. 12999 in Thunberg
Herbarium, UPS; PRE, photo.!).
Atragene capensis L., Sp. PI. 543 (1753). Type: Cape (LINN
711.3; PRE, photo). A. tenuifolia L. f., Suppl. 270 (1781), as
above. A. tenuis Thunb., FI. Jap. 239 (1784). Type: none cited.
Anemone capensis Lam., Encycl. 1:164 (1783); Oliver in
Flower. PI. Afr. 40 :t. 1 569 (1969). Type: Cape (specimen in
Herb. Jussieu, P). A. arborea Hort. in Steud. Nom. ed. 95 (1840),
nomen nudum. A capensis (L.) Harv. in FI. Cap. 1 : 3 (1859-60),
nom. illeg. ; Adamson in FI. Cap. Penins. 401 (1950). A capensis
(L.) Harv. var. tenuifolia Harv., l.c.
Pulsatilla africana Spreng., Syst. 2: 664 (1825). Type: none
cited. P. tenuifolia (L.f.) Spreng., l.c.
D. J. B. Killic
RUTACEAE
ZANTHOXYLUM LEPRIEURII*, A NEW RECORD FOR SOUTHERN AFRICA
The first specimen of this Zanthoxylum from
Southern Africa was collected by Drs Codd and Dyer
(No. 4564) in the Sibasa district of the Transvaal
near Punda Milia in the Kruger National Park in
October 1948. However, in the absence of fertile
material, this specimen, like each of those collected in
the Kruger Park and in north-eastern Natal (Tonga-
land) during the next twenty years, remained unidenti-
fied. In December 1969 good flowering material of
both male and female plants was collected (A/o//4887,
4889) near Makanes Drift in Tongaland and it is
these specimens which finally enabled the plants to be
identified. There is still no fertile material from the
Transvaal, although there is a photograph in the
National Herbarium, Pretoria, of a fruiting branchlet
collected by Mrs E. Jenkins north-east of Sibasa in the
northern Transvaal.
’•‘The taxonomic position of the genera Zanthoxylum L. and
Fagara L. has long been a source of controversy. Most early
taxonomists, for example, Benth. & Hook.f., Gen. PI. 1 : 297
(1862), regarded the two as congeneric, but later opinion
favoured the argument advanced by Engler in Pflanzenfam.
3 , 4 :95— 102 (1 896), which supported the retention of both genera.
In recent years evidence has accumulated which supports the
view that the genera are not distinct. Following Hartley, in
J.Arn.Arb. 47:171-221 (1966), and Waterman, in Taxon
24:361-366 (1975), Fagara and Zanthoxylum are here regarded
as congeneric, Zanthoxylum being the correct name for the
combined genera.
VARIOUS AUTHORS
259
The specimens are referable to Z. leprieurii Gu ill. &
Perr., a species described from Senegal, but widespread
in the forests of west tropical Africa to the Equatoria
Province of the Sudan, Uganda, Tanzania, northern
Mozambique, Zaire and Angola. Although not
specifically distinct, the Southern African plants do
nevertheless differ from typical Z. leprieurii in certain
characters.
In typical Z. leprieurii the inflorescence is a very
robust structure up to 30 cm long with the axis 2-3 mm
in diameter basally, and the axis and its many lateral
branches are sparingly to densely glandular-puberu-
lous, particularly the lateral branches. It is not clear
whether the inflorescence is carried erect or whether it
is pendulous as none of the collector’s notes refer to
this feature. The inflorescence in the Tongaland plants
(and presumably in the Transvaal) is smaller, seldom
attaining a length of 20 cm and the axis is slender
and ±1 mm in diameter basally. The inflorescence
in these plants is pendulous and glabrous, and the
lateral branches are fewer and more widely spaced so
that the inflorescence forms a more open lax panicle.
The flowers are more consistently aggregated into
fascicles along the lateral branches, particularly in the
male, and there are fewer flowers per lateral branch.
This contrasts with the tropical material where the
flowers are more often solitary.
The Southern African specimens also differ from
material of typical Z. leprieurii in having consis-
tently smaller leaves with fewer pairs of smaller
leaflets, but there is no discontinuity in any of these
characters between specimens from the two areas.
Typical Z. leprieurii is a forest species which grows
to a height of 27 m, while the Southern African plants
grow on sandy soils as shrubs or small trees and
seldom attain a height of 8 m. Plants are known from
only two localities in Tongaland, namely, False Bay
Park and the Makanes Drift-Sihangwane area where
they form one of the constituents of the sand-forest
and grow in association with species such as A/bizia
forbesii Benth., Newtonia hildebrandtii (Vatke) Torre
and C/eistanthus schlechteri (Pax) Hutch., to name but
a few. Only six male plants have been found at False
Bay Park, but in the Makanes Drift-Sihangwane
area plants are locally quite common.
In Tongaland the specimens of Z. leprieurii are
entirely leafless in winter. In spring the young leaves
and inflorescences appear together, but while the
leaves develop the young flower buds remain closed
for several months before finally opening. The male
inflorescences are relatively long and conspicuous and
project beyond the leaves, while the female inflores-
cences are usually smaller and are sometimes partially
hidden in amongst the leaves.
Zanthoxylum leprieurii Guill. & Perr., FI. Seneg.
Tent. 141 (1831). Type: Senegal, Leprieur (P, holo.!).
Fagara leprieurii (Guill. & Perr.) Engl, in Pflanzenfam-
3,4:118 (1896). F. angolensis Engl, in Bot. Jahrb. 23 : 148 (1896).
Type: Angola, without locality, Welwitsch 4575 (K, iso.!).
F. nitens (Hiern) Engl., Pflanzenw. Afr. 3,1 :749 (1915). F. sp.,
Ross, FI. Natal 213 (1973); Palmer & Pitman, Trees S. Afr.
2:982-3 (1973).
Zanthoxylum nitens Hiern, Cat. Afr. PI. Welw. 1:112 (1896).
Type: Angola, Golungo Alto, road to Bango, Welwitsch 4558
(K, iso. !).
The following specimens from Southern Africa
have been examined: —
Transvaal. — 2231 (Pafuri): Kruger National Park, 5 km
N.E. of Punda Milia, Codd & Dyer 4564; Kruger National Park,
Punda Milia, Van der Schijff 2)30; 3803.
Natal. — 2632 (Bela Vista): 8 km W. of Muzi border post,
Moll 5654 (NH). 2732 (Ubombo): 3,2 km N.E. of Makanes
Drift, Moll 4887; 4889; Ross 2368; near Jobe’s Kraal, Garland
442; 10 km Pongolo bridge/Maputa, Moll 4382; Sihangwane,
Tinley 901 (E,NU); Pooley 727 (E, NU); 2 km W. of Sihangwane
Store, Moll 4880; False Bay Park, Ward 3850; Ross 2229.
J. H. Ross
SELAGINELLACEAE (LYCOPSIDA)
SELAGINELLA IMBRICATA IN THE FLORA OF SOUTHERN AFRICA AREA
During August 1956 a specimen of Selaginella
imbricata ( Story 5841) was collected in the Kapupa
Valley (12°34' E, 17°21' S) in the northwest of South
West Africa. This species was not included in Prodr.
FI. S.W. Afr. The presence of S. imbricata in South
West Africa is rather unexpected, as this species
usually occurs in rather moist forest situations. The
specimen was reported as occurring “along fissures in
rocks in mountain gorge”. Judging from the geo-
graphical situation, the area where the specimen
was collected, must be extremely dry.
The find is of interest, firstly because it adds another
species to the flora of South West Africa, and secondly,
because it extends the known range of the species
westwards by 1300 km. The nearest point from which
it was previously known, is the Victoria Falls.
This is the first time the genus has been recorded
from South West Africa, although a number of species
occur in adjacent territories.
Two other specimens in the National Herbarium,
also proved to be S. imbricata (Forsk.) Spring ex
Decne. Apparently these two specimens, Galpin s.n.
in PRE Cryptogam ic Herbarium (Pteridophyta)
3532 from Devil’s Hoek in the Royal National Park
in 1928, and Esterhuysen 10823 from the “Turret”
and “Amphlet” in the Cathkin Peak area in 1956,
represent the only two collections from which this
species is known in South Africa. This is about
1500 km south of the nearest known locality near
Melsetter in Rhodesia.
Selaginella imbricata is widespread throughout the
eastern part of Africa, from the escarpment between
Mozambique and Rhodesia in the south to Arabia in
the north. It occurs westwards along the Zambesi
valley to at least as far as the Victoria Falls and, as
already mentioned, is found in the extreme north-
western part of South West Africa.
It would seem that the plant must be very rare in
South Africa to have escaped more frequent collection,
as it is quite a distinct and conspicuous species. It
can easily be distinguished from other South African
species because of the rhomboid outline of the
branched stem system, which stands erect, as it is
rather stiff, and is arranged in one plane like a fern
frond, instead of being procumbent and closely
adpressed to the substrate. It occurs in moist, shady
forest situations against earth banks. Under dry
conditions the plant rolls up into a series of ball- or
clockspring-like structures, but unrolls again after
rains.
While some species of Selaginella occur under moist
conditions and cannot withstand drought, many
species are xerophytes of the “resurrection” type.
Such species are dry and inactive and more or less
rolled up during the greater part of the year. As soon
as they are moistened, however, the leafy branches
unfold and the tiny leaves attain a green colour once
again. S. imbricata is intermediate in this respect.
Its habitat is generally not dry at all, but it is capable
of surviving dry spells by going into quiescence.
P. VORSTER
260
NOTES ON AFRICAN PLANTS
THELYPTERIDACEAE
NEW COMBINATIONS IN THELYPTER1S
Holttum in J. S. Afr. Bot. 40: 123—168 (1974)
stated that the estimated 1 000 species in the family
Thelypteridaceae can either be regarded as belonging
to a single genus, Thelypteris, or they can be placed in
a number of different genera. In Blumea 19: 17-52
(1971) he adopted the latter course by grouping the
450-500 Asian-Malesian species into various genera.
“For comparative purposes”, Holttum (1974) also
classified the 55 African species of the family Thelyp-
teridaceae according to this scheme. He added,
however, that “. . . .for persons who are concerned
only with Africa, or a part of Africa, it is reasonable to
adopt one genus Thelypteris, as Prof. Schelpe has
done in his account of the ferns in Flora Zambesiaca
(1970)”.
I agree with this approach, with the possible excep-
tion of Ampelopteris , a monotypic genus, which can
easily be recognized by the unicellular forked hairs
and numerous gemmae on the fronds.
The characters used to differentiate between the
genera of Thelypteridaceae (pinna veins anastomosing
or not, reduction of lower pinnae, hairiness or scaliness
of fronds) are, in my opinion, not sufficient in the
African context to justify division into genera. The
presence or absence of indusia may be useful for
subgeneric division, but will have to be studied in
conjunction with other characters.
Holttum (1974) pointed out that some of the
African taxa described in that paper still lack names
in Thelypteris. For two of the South African species
these combinations are made below, as they have not
been proposed by Schelpe (in press):
Thelypteris altissima ( Holtt .) Vorster comb. nov.
Christella altissima Holtt. in J. S. Afr. Bot. 40: 141 (1974).
Thelypteris prolifera ( Retz .) Vorster comb. nov.
Hemionitis prolifera Retz., Obs. Bot. 6:38 (1791).
Ampelopteris prolifera (Retz.) Copel., Gen. Fil. 144 (1947).
P. Vorster
Bothalia 12, 2: 261-265 (1977)
World climate patterns in grassland and savanna and their relation
to growing seasons
R. KIRK STEINHORST* and J. W. MORRISf
ABSTRACT
The climate at eleven IBP savanna or grassland study sites from five continents are described and principal
components analysis is used to compare them. A multivariate linear discriminant function based on mean
monthly precipitation, mean monthly temperature, latitude and altitude, is used to predict the length of the
growing season at each site. At most sites, the actual and predicted start and end of the growing season agreed
closely. It is concluded that growing season on a world-wide basis may be predicted fairly reliably from a
small number of abiotic variables by means of a multivariate discriminant function.
RESUME
CYCLES CLIMATOLOGIQUES MONDIAUX EN PRAIRIE ET SA VANE ET LEU R RELATION
AVEC LES SAISONS DE CROISSANCE
Les climats en onze points d' etude de la savane on de la prairie, choisis par le Programme Biologique
International sar les cinq continents, sont decrits et compares par le moyen de V analyse des principaux
composants. Une fonction discriminante lineaire multivariee, basee sur les moyennes mensuelles de la
precipitation et de la temperature , sur hi latitude et T altitude , est utilisee pour predire la longueur de la
saison de croissance en chaque endroit. Dans la plupart des cas, il y a un excellent accord entre le calcul
et T observation pour le debut et la fin de la saison de croissance. On en conclut que cette saison peut,
d l echelle mondiale, faire Vobjet d'une prevision assez sure a partir d'un petit nombre de donnees abioti-
ques et en utilisant une fonction discriminante multivariee.
INTRODUCTION
In this article we consider a variety of savanna and
grassland sites and one tundra site, characterize their
climates and relate climate to the conditions for
growth of the natural vegetation of the sites. By so
doing, we hope to better understand the factors
involved in growing season determination. By growing
season, we mean that period of the year from the
time when environmental factors cease to limit
growth, usually in spring, until they limit it again,
usually in autumn.
With the present world population and limited food
supplies it is important that we use all available land
in an efficient manner for either agriculture, grazing,
wood production, or conservation. As recently
pointed out by Newman & Pickett (1974), the one
uncontrollable factor which limits land productivity
is weather. Success or failure of crops and of forage
production are dramatically affected by whims of
weather. Newman & Pickett suggest that knowledge
of world climate will enable us to predict productive
uses for each area. To apply this strategy, however,
knowledge of how crops and other vegetation respond
to climatic factors is required. For crops, and
monospecific communities in general, physiological
studies give us the required information concerning
responses to light, temperature, precipitation, and
other factors. For savanna, grassland, or tundra
communities of many species, physiological studies
give us no single answer. Another solution is required
if we are to utilize such communities efficiently on a
world-wide basis for grazing or fodder production.
The International Biological Program (IBP) gives
us a unique opportunity to study these communities
of many species. In this paper we include data from
IBP grassland sites and one tundra site (eutrophic
mire) falling in a range from 6° to 60° latitude,
north and south of the equator from five continents
(Table 1). Each site represents typical savanna,
grassland or tundra vegetation under grazing, haying,
or fallow conditions. The data include short-term
specific weather records on at least a monthly basis
and the associated growing seasons as determined
subjectively by the investigators at each site. In order
to predict conditions for growth of the local
vegetation, we consider monthly precipitation and
average temperature along with latitude and altitude.
* Natural Resource Ecology Laboratory, Colorado State
University, Fort Collins, Colorado, U.S.A. (Now at: Institute
of Statistics, Texas A & M University, College Station, Texas).
t Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria, 0001.
TABLE 1. — Study sites and sources of data
262 WORLD CLIMATE PATTERNS IN GRASSLAND AND SAVANNA AND THEIR RELATION TO GROWING SEASONS
CHARACTERIZATION OF CLIMATE TYPES BY
PRINCIPAL COMPONENTS ANALYSIS
There is a wide range of climates, both tropical
and temperate, represented in the sites included in
the study. Of the tropical climate sites, Lamto,
Ivory Coast, has uniform temperatures with heavy
precipitation from March to October with a brief
respite in mid-summer. The two Indian sites have
three seasons; a rainy season from mid-June to
September, a cool dry season from October to
February, and a hot dry season from March to mid-
June. Welgevonden, South Africa, is a dry sub-
tropical savanna site with summer rainfall. The
temperate sites range from 30 to 60° from the equator.
They have seasons dictated by the angle of the sun’s
incoming rays. Armidale, Australia, is a cool
temperate rangeland with moderate precipitation,
which is fairly uniform but heaviest in summer.
Temperate sites w'hich are relatively humid are
Lanzhot, Czechoslovakia: Glenamoy, Ireland:
Terschelling, Netherlands; Hardangervidda, Norway;
and Moor House, U.K. The season of rainfall varies
greatly among temperate sites. For example, Ireland’s
heavy precipitation occurs in November, December
and January, whereas Terschelling has uniform
rainfall throughout the year. The Pawnee Site in the
United States is very dry relative to the other sites.
A number of these sites have climates which are
influenced by geographical features. The Netherlands,
Norway, Ireland, Ivory Coast and United Kingdom
sites are influenced by proximity to the ocean. Both
the Czechoslovakian and the United States sites are
continental. The Pawnee (U.S.) site's weather is
furthermore modified by the north-south Rocky
Mountain Range, a few kilometres to the west.
Czechoslovakia on the other hand is bounded by the
major east-west mountain ranges of Europe. Another
site affected by mountains is the northern India site
(Kurukshetra), whose climate is influenced to some
extent by the Himalayas.
All in all, these sites have a fairly predictable
pattern of monthly temperature based on incoming
radiation, but they present a mosaic of precipitation
regimes. Principal component analysis (PCA) (Seal,
1964) was used to illustrate this contrast. For
temperature, using the twelve monthly values as
attributes over the eleven sites (entities), the first
component (an average temperature component)
accounts for 94% of total variability in the data and
the second component brings the cumulative per
cent to 99%. The second component contrasts
summer and winter temperatures, yielding a range
from very uniform monthly temperatures (Ivory
Coast, Ireland and U.K.) to strongly seasonal ones,
including U.S. A. and Czechoslovakia (Fig. 1). The
first component separates warm sites, such as the
Indian and the Ivory Coast sites, from cold ones such
as U.K. and Norway. As a hierarchical cluster
analysis (Johnson, 1967) on temperature correlation
or seasonal patterns grouped the sites in the same
manner as component two of the PCA, except for
the U.S. site which, for these data, showed a monthly
temperature pattern similar to the Moor House site,
these results are not presented. A hierarchical cluster
analysis using euclidian distance, that is, temperature
magnitudes rather than patterns, yielded clusters
predictably similar to the first component of the
PCA and is also not presented.
For mean monthly precipitation values over the
eleven sites, the first three principal components
account for only 52%, then 75%, then 86% of the
total variability. There is no discernable pattern of
rainfall along latitudinal or altitudinal gradients.
This result follows from the above characterization
of climate types since the precipitation at these sites
is variously affected by oceans, mountains, and other
non-regular causes. In contrast to the sun’s orbit,
which is the principal regulator of temperature,
there is no single unifying phenomenon that controls
precipitation.
DETERMINATION OF GROWING SEASON BY
DISCRIMINANT ANALYSIS
If one were to take a plant physiological approach
to the specification of conditions for growth, one
would consider available solar radiation, maximum
and minimum air temperature, soil temperature,
number of daylight hours (related to latitude),
available moisture and phenological stage. We have
taken four variables as integrators of all these factors,
namely: mean monthly temperature, monthly pre-
cipitation, latitude and altitude. The growing seasons
for the 1 1 sites do not simply commence and end as
the sun progresses to and from the equator. If this
were so, either average monthly temperature or
latitude would suffice to predict growing seasons.
Fig. 1. — First and second princi-
pal components of monthly
mean temperature data for the
eleven sites.
First Principal Component
R. KIRK STEINHORST AND J. W. MORRIS
263
A step-wise discriminant algorithm (Dixon, 1971) was
applied to determine if some combination of these
four variables was a good indicator of growth. Each
month, at each site, was classified as either a growing-
or non-growing-season month according to the
dates defining the length of the growing season
supplied by each investigator. The means for the
four response variables are given in Table 2, and the
pooled covariance matrix is given in Table 3.
TABLE 2.— Mean values (F) over the eleven sites for the four
responses
TABLE 3. — Pooled covariance matrix(E) of variances and
covariances among the four responses
Data from South Africa and Australia were
displaced by six months for the calculations so that
“summer” and “winter” seasons would coincide
with northern hemisphere seasons. Growing season
months clearly have more rainfall and are warmer
(Table 2). The latitude and altitude means differ in the
two groups only in so far as the sites at different
latitudes or altitudes have greater than or less than
6 months of growth. Curiously, there are relatively
more growing season months at greater latitudes
than non-growing months at those latitudes (group
means of 38,9 and 38,1 respectively), although the
difference is not significant.
The most important single variable is precipitation
(t-test between growing and non-growing groups
yield a significance of p <0,0005). However, when
used as an indicator of growth, this variable by itself
incorrectly labels 35 growing season months as
non-growing months while correctly categorizing
84 months. The remaining 13 months were non-
growing months mis-specified as growing months.
The best discriminant function uses either all four
variables, in which 29 of 132 months are mis-specified,
or all variables excluding altitude for which 29 of,
132 months are also mis-specified. Latitude i ; needed
in addition to precipitation and temperature in
order to predict growth more accurately for some
cool sites. Using all four variables, the multivariate
t-test for groups yields a significance of p <0,0005.
While it is clear that the largest difference between
the growing and the non-growing months is their
precipitation, precipitation alone is not sufficient to
predict suitable conditions for growth.
Using all four variables the discriminant function
for group i is
— i/rh T /di £_1;c=ai-f-b1iX
where //, is the four-variate mean for group i in
Table 2, Z is the pooled estimate of the variance-
covariance matrix (Table 3), and x is the four variate
response for a particular site and month. For the
growing season group, ax= — 27,6731 and b\=
(0,02709, 1,20478, 0,71537, 0,00781); for the non-
growing season months one obtains a2= — 19,60077
and b\=(0, 01511, 0,99291, 0,61318, 0,00681).
After cancelling constant terms the posterior
probability of being in group i is:
aj + bfix
n\t
ai ~\-b'l1x a 2+b12x
nxe +ft2e
where n \ and n2 are the prior probabilities of being
in the growing and non-growing groups, respectively
(Dixon, 1971). Both n1 and n2 are taken to be one-half
in this case. Prior probabilities are those based on the
assumption or hypothesis under investigation, in this
instance, that a month has an equal chance of being
either a growing or a non-growing month. The two
posterior probabilities, in this instance, are the
chances of a month being a growing and non-growing
month, calculated by substitution in the above
equation of the month’s precipitation, temperature,
latitude and altitude values using (al5 blx) and
(a2, b 12), respectively. Posterior probabilities were
calculated for each month at each site and each
month as classified as growing or non-growing,
depending on which posterior probability was greatest.
In Fig. 2 the growing seasons as given by the
investigators are compared with the calculated growing
seasons from the four-variable discriminant analysis.
There are a total of 103 of 132 months correctly
specified, whereas 17 growing season months were
incorrectly classified as non-growing months and
12 non-growing season months were specified as
suitable for growth. Half of the misclassified months
were for tropical countries where growth would
appear to be regulated by something in addition to
rainfall and temperature. Predictions for both Indian
sites and the Ivory Coast were particularly poor while
those for South Africa and Australia are acceptable.
On the other hand, the growing season was precisely
predicted at Hardangervidda. Other temperate
locations were treated relatively well, except that the
linear discriminant technique was not able to
accurately predict initiation of growth at Glenamoy,
Ireland.
DISCUSSION AND CONCLUSIONS
Although the 1 1 sites represent vastly differing
climates, including various combinations of tem-
perature and moisture regimes, use of multivariate
linear discriminant analysis suggests that, over a large
portion of the globe, growing season is basically
a function of precipitation and temperature with
some modification due to latitude. Given these three
variables, altitude may be of slight additional signi-
ficance. Growth in tropical areas is dependent upon
other or additional factors, including possibly mean
monthly minimum temperature. The unsatisfactory
predictions could also be accounted for by the use of
one or two years’ records instead of long-term
averages in the calculations. The success in correctly
classifying conditions conducive to growth using a
multivariate linear function of three or four variables
suggests that a plant community approach, as opposed
to species-specific physiological approaches, can be
successful.
It is possible to predict conditions suitable for
growth at the community level on a global basis using
a few abiotic variables. Future research can be directed
at finding particular response curve relationships
between initiation and termination of growth and
264 WORLD CLIMATE PATTERNS IN GRASSLAND AND SAVANNA AND THEIR RELATION TO GROWING SEASONS
_____ discriminant analysis
actual
S.lndia
USA
UK
S- Africa
Norway
Netherlands
Ivory Coast
Ireland
N. India
Czechoslovakia
Australia
Fig. 2 — Comparison of actual and predicted length of growing season at each site.
"i m r
J T J
Months
i a r
"I O I N I D~
these factors. Until such research is done, the dis-
criminant function used here gives us a reasonable tool
for determining growing season. Management strate-
gists can use this function to predict the possible
outcomes of various strategies under conditions which
have not occurred previously. For example, if one
anticipates a cool wet spring, representative pre-
cipitation and temperature figures can be supplied
and the effect on the start and end of the growing
season may be predicted.
ACKNOWLEDGMENTS
Authors who contributed data for this study are
thanked. We also wish to thank J. Dodd, K. P.
Haddock, J. G. W. Jones, S. Jonsson and J. J. P. van
Wyk for stimulating discussions during the IBP
Grassland and Tundra Modelling Workshop in August
1972 at Fort Collins, Colorado, from which this paper
developed. This paper reports on work supported in
part by U.S. National Science Foundation Grants
GB — 31862X and BMS73— 02027 A02.
UITTREKSEL
Elf IBP savanne- en grasveldstudiegebiede ( vanaf
vyf vastelande) se klimaat word beskryf en met be/ndp
van lioofkomponentanalise vergelyk. 'n Veelvoudige
lineere diskriminantfunksie word gebruik om die lengte
van die groei-seisoen vir elke gebied te bereken. Die
gemiddelde maandelikse reenval, gemiddelde maande-
likse temperatuur , lengtegraad en hoogte bo seespieel
word gebruik om hierdie funksie te bereken. Vir die
meeste van die gebiede was daar min verskil tussen die
werklike en die berekende aanvang en einde van die
groeiseisoen. Daar word tot die gevolgtrekking gekom
dat die groeiseisoen redelik betroubaar, wereldwyd
bereken kan word met behulp van 'n veelvoudige
diskriminantfunksie en 7z klein aantal abiotiese
gegewens.
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chercheurs de Lamto, numero special 1974, fascicule II.
R. KIRK STEINHORST AND J. W. MORRIS
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Wala, G., 1972. An approach to system analysis of a
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of a tropical grassland at Kurukshetra, India. Ecol.
Monogr. 44: 351-376.
Skarveit, A., Ryden, B. E., & Karenlampi, L., 1975. Climate
and hydrology of some Fennoscandian tundra ecosystems.
In F. E. Wielgolaski (ed.), Fennoscandian tundra ecosy-
stems. Part /, Plants and micro-organisms. Berlin: Springer-
Verlag.
Smi'd, P., 1972. Fundamental climatological and hydrological
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PY-PP Report No. 2.
Bothalia 12,4: 267-292 (1976)
Automatic classification of the highveld grassland of Lichtenburg,
south-western Transvaal*
J. W. MORRIS!
ABSTRACT
A qualitative, semi-detailed plant ecological study of the area between 25° 54' and 26' 22' E and 26‘ 00'
and 26° 20' S, situated around the town of Lichtenburg in the south-western Transvaal, South Africa, is
reported. Mean annual temperature of the study area is 17 °C and annual rainfall is about 600 mm. A basic
difference is recognised between the Bankenveld Land System and the CT Grassland Land System. The former
is underlain by dolomite with lithosolic soils, Bankenveld vegetation and cattle ranching as the chief land-use,
whereas the latter is underlain by granite, Ventersdorp lavas, Dwyka tillite and surface limestone with Shorrocks,
Mangano and Lichtenburg series soils, Cymbopogon-Themeda Veld vegetation and extensive cultivation of maize
as the chief land-use. One hundred and ten 16 m2 quadrats were placed within each Land System by means of a
stratified-random strategy. Of the 247 species encountered, nearly 100 occurred in less than six quadrats.
Themeda triandra, Aristida congesta, Elionurus argenteus, Anthospermum rigidwn and Justicia anagaloides were
common throughout. Two association analyses were carried out and 15 final groups were interpreted out of a
total of 21 groups.
RESUME
CLASSIFICATION QUANTITATIVE DE LA PRAIRIE DE IIAUTES TERRES DE LICrlTEN-
B'JRG, SUD-OUEST DU TRANSVAAL
On expose les resultats d’une etude phyto-ecologique quantitative et semi-detaillee de !a region
comprise entre 25° 54' et 26° 22' E. et 26°00 et 26° 20' S., autour de la ville de Lichtenburg dans le sud-
ouest du Transvaal, Afrique du Sud. La moyenne annuel le de la temperature y est de 17 C et la hauteur
de pluie d' environ 600 mm. On recommit une difference fondamentale entre le Bankenveld Land System et
le CT Grassland Land System. Le premier est supporte par de la dolomite avec des lithosols, une vegeta-
tion du type Bankenveld et Televage du betail const ituant la principale utilisation du terrain : tandis qu'au
second sont sousjacents du granite, des laves de Ventersdorp, de la tillite de Dwyka et des calcaires de sur-
face avec des sols des series de Shorrocks, Mangano et Lichtenburg sur lesquels pousse une vegetation de
prairie d Cymbopogon — Themeda et dont la principale utilisation est la culture extensive du mats. Cent
et dix carres de 16 m de cote ont ete repartis sur chaque systeme selon la technique de stratification
aleatoire. Des 247 especes rencontrees, pres de 100 ont ete trouvees sur moins de six carres. Themeda
triandra, Aristida congesta, Elionurus argenteus, Anthospermum rigidum et Justicia anagaloides
etaient communes partout. Deux analyses d' association ont ete executees et d'un total de 21 groupes,
15 groupes finals ont ete interpretes.
CONTENTS
Page
Introduction 267
1. Description of study area 268
1.1 Location 268
1.2 Climate 268
1.3 Geomorphology and geology 270
1.4 Soils. 271
1.5 Vegetation 272
1.6 Land-use 273
1 .7 CT Grassland and Bankenveld Land
Systems 274
2. Procedures used in this study 274
2.1 Sampling strategy 274
2.2 Association analysis 274
2.3 Presence and indicator value 276
2.4 Re-allocation 276
3. Classification of the vegetation by
association analysis 276
3.1 Summary statistics of data 276
3.2 Total association analysis 276
3.3 Bankenveld association analysis. .. . 282
4. Discussion and conclusions 289
4.1 Sampling strategy 289
4.2 Methodological aspects 289
4.3 Vegetational aspects 290
Acknowledgements 290
Uittreksel 291
References 291
* Forms part of a Ph.D thesis submitted to the University
of Natal (Morris, 1973).
t Botanical Research Institute, Department of Agricultural
Technical Services, Private Bag X101, Pretoria.
INTRODUCTION
The overall model for the ecological survey of the
natural and semi-natural vegetation of the Highveld
Agricultural Region of South Africa was designed by
D. Edwards and J. C. Scheepers of the Botanical
Research Institute. At an early stage, they decided
that instead of spreading surveying efforts equally
over the whole Region of approximately 1 1 655 000
ha, the Key Area approach, whereby efforts would
initially be concentrated in the Lichtenburg, Maquas-
sie, Kroonstad, Bethlehem and Villiers Key Areas,
would be used. Each Key Area is a quarter degree
square in extent and covers approximately 69 000 ha.
Individual surveys of these five areas would be
followed by extrapolatory surveys linking the areas.
The aim of the survey reported here, a contribution
towards the Highveld Region survey, was an account
of the plant ecology of the Lichtenburg Key Area.
A report on the Kroonstad and Bethlehem Areas
(Scheepers, 1975) has already been produced.
The basic sampling strategy of 4 by 4 m quadrats,
with a stratified-random distribution, was chosen
during preliminary studies for the Kroonstad Area
and the Lichtenburg and Bethlehem surveys followed
suit to aid later comparison and extrapolation. The
technique of association analysis was chosen to
synthesize the results of each survey.
Two Land Systems (Dowling, 1968; Mabbutt,
1968) occur in the Lichtenburg Key Area. In this
communication they are referred to, for convenience
and brevity, as CT Grassland and Bankenveld Land
Systems. The former includes Dry Cymbopogon-
Themeda Veld and Sandy Cymbopogon-Themeda
Veld and the latter covers part of Bankenveld (Acocks,
1953). The main features of and differences between
the two Land Systems are detailed later. Briefly,
Bankenveld lies on an area of dolomitic lithosol
268
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
north of Lichtenburg where a great deal of the
natural and semi-natural vegetation (physiognomi-
cally a grassland) remains and the main land-use
activity is cattle and sheep farming. CT Grassland is
an extensively-cultivated area south, east and west
of Lichtenburg where maize is the chief crop. Natural
and semi-natural vegetation is rare but, where still
encountered, the physiognomic structure is grassland
or savanna. In general, it is only small rock outcrops
and poorly-drained areas which are not ploughed in
the CT Grassland Land System.
1. DESCRIPTION OF STUDY AREA
1 . 1 Location
The location of the study area and its position
relative to towns in the South-western Transvaal,
South Africa are indicated in Fig. 1. Lichtenburg is
the only town situated in the area. Initially, the area
for study was the 2626AA quarter degree square but
as parts were extensively cultivated the area was
enlarged, as illustrated in Fig. 1, to enable placement
of enough sampling points in relatively undisturbed
vegetation. A rectangular shape was retained even
though much of the enlarged area was not sampled.
The quarter degree square covers about 69 000 ha
and the whole study area about 177 000 ha.
1 . 2 Climate
Apart from precipitation and air temperature
records, no climatic data are available from within
the study area. Data from Potchefstroom, and even
Pretoria, are used to complete the description of
climate given below. Where data from outside the
study area are used, they are intended as indications
of conditions prevailing within the area and no more.
1.2.1 Radiation and sunshine
Few meteorological stations in South Africa record
radiation. The station nearest to Lichtenburg is at
Pretoria, half a degree further north and 200 km east.
The instrument at Pretoria is a Kipp solarimeter and
all measurements are from a horizontal surface. The
percentage radiation received at the top of the atmos-
phere, but not reaching the surface of the earth at
Pretoria, averages 39 percent annually with a maxi-
mum attenuation of 45 percent in December and
minimum of 31 percent in June (Schulze, 1965).
Fig. 1. -Locality of study area. Dark shading indicates 2626AA quarter degree square and lighter shading the enlarged
study area. Inset: position in South Africa.
J. W. MORRIS
269
The monthly march of radiation at Pretoria is
given by Weather Bureau (1968). The highest mean
daily sums occur in summer from October to February
when the global radiation exceeds 530 cal/cm2/day
and the lowest mean daily sums in June and July
(less than 360 cal/cm2/day). Radiation increases
sharply from July to September and then stays fairly
constant during summer before starting to decrease
in February. The levelling off of radiation in summer
is due to an increase in cloudiness compensating for
radiation increases during this season. Diffuse radia-
tion varies from over 150 cal/cm2/day in summer to
less than 80 cal/cm2/day in winter. The highest sum of
radiation recorded on a single day (800 cal/cm2)
occurred during the month of January and the lowest
(27 cal/cm2) during July (Schulze, 1965).
1.2.2 Air temperature
Although air temperature data have been recorded
at Lichtenburg since 1905, observations until 1950
are the most recently published statistics (Weather
Bureau, 1954). During that period the mean of daily
maximum temperature varied from over 28 °C in
December and January to under 20 °C in June and
July. Mean of daily minimum was about 15 °C in
January and February and less than 2 °C in June and
July. Of more interest ecologically are the extreme
maxima and minima (Walter & Leith, 1960). Extreme
maximum temperatures in summer (September to
February) exceed 35 °C while in winter the maximum
recorded temperatures exceed 25 °C (July). Extreme
minima below -5°C occur from May to August. In
mid-summer (December to February) the extreme
minimum temperature is above 3 °C.
1.2.3 Grass minimum temperature and frost
Mean grass minimum temperature at Potchef-
stroom (Schulze, 1965) varies from 11 °C in December,
January and February to below -5 °C in June and
July. The maximum exceeds 16 °C from November
to March and drops to 8 °C in July while the minimum
temperatures throughout the year (except February)
are below 1 °C. The extreme minimum of -17 °C
was recorded during July.
In the absence of observations on frost occurrence,
climatologists have used various air temperatures to
indicate the occurrence of frost. If the criteria of the
publication Weather Bureau (1954), namely a mini-
mum temperature less than 0 °C in a Stevenson
screen 1,2 m above the surface, are accepted, Lichten-
burg averages 106 days per annum (30-year records)
with a possibility of experiencing frost. The average
first date is 19th May and the average last date is
2nd September. As the average number of days on
which frost actually occurs is 26, frost may be expected
one night in four from the middle of May until the
end of August. The extreme first date was 16th April
and the extreme last date on which frost has been
recorded was 26th September.
1.2.4 Soil temperature
Soil temperatures have been recorded at Potchef-
stroom for five years (Schulze, 1965). The highest
monthly mean temperatures have been recorded at
1400 hours in November, December, January and
February when the temperature exceeded 29 °C at
10 cm and 24 °C at 20 cm. The lowest temperatures
(0800 hours) in June and July at these depths, where
most plant roots are located, were 8,3 °C at 10 cm
and 10,2 °C at 20 cm.
1.2.5 Surface wind
No information on surface wind is available from
within the study area but the general features may be
determined from a knowledge of air circulation
patterns over South Africa and from observations of
wind speed and direction at nearby meteorological
stations. In general, there seems to be little seasonal
change in wind direction or force. Winds with a
northerly component predominate, but it is difficult
to assign any one prevailing direction according to
Schulze (1965). The northerly component results from
the normal anticyclonic circulation of air around a
high pressure cell located over the interior of South
Africa throughout the year.
TABLE 1.— Mean monthly rainfall in mm (r) and mean number of days with rain (d) at the seven stations with recording periods
of over 20 years from Weather Bureau (1965)
270
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
1.2.6 Precipitation
Precipitation within and near the study area is
almost entirely in the form of rain, most of which
falls during summer. While severe hail storms are
experienced with a fairly high frequency, snow is
rare. Data from a number of meteorological stations
measuring rainfall within the study area are given in
Table 1. Mean annual rainfall at Lichtenburg is just
over 600 mm, with 85 percent falling during the six
summer months from October to March. Rain may be
expected to fall on ten days each month during Decem-
ber and January and on only one day per month in
winter (Table 1), with an average of about 60 days per
year.
1.2.7 Climate classification and summary
According to Schulze (1947), the Lichtenburg study
area is in the BSkw class of Koppen. The climate is
arid (steppe), cold and dry with a mean annual
temperature below 18 °C. Mean temperature of the
hottest month exceeds 18 °C and the dry season is
during winter. Following the Thornthwaite classifica-
tion (Schulze, 1947; 1958), the study area lies on the
border between DB’d to the west and CB’d to the
east. DB’d is a semi-arid warm (steppe) climate and
CB’d is subhumid warm. In both climates, moisture
is deficient throughout the year. Following the clas-
sification of UNESCO-FAO (1963) the climate is
accentuated temperate tropical. In other words, there
is a dry period of between one and eight months
coinciding with the period of shortest day-length, the
mean temperature of the coldest month is between
0 °C and 10 °C and the xerothermic index is between
150 and 200.
The climate of the study area is summarized in Fig.
2 (modified after Walter & Leith, 1960) and is
described by Schulze (1965), on which the following
description is based. The average daily maximum
temperature is about 28 °C in January and 18 °C
in July but in extreme cases temperatures may rise to
37 °C and 25 °C, respectively. Average daily minima
range from about 15 °C in January to 2 °C in July,
whereas extremes may drop to 6 °C and -10 °C,
Lichtenburg (1477m) 17° 602mm
Fig. 2. — Climate diagram for Lichtenburg (a = altitude,
b == mean annual temperature, c = mean annual
precipitation, d = mean daily minimum temperature
of coldest month, e = absolute minimum temperature,
f = mean daily maximum temperature of hottest
month, g = absolute maximum temperature, h = mean
range of temperature, i = curve of mean monthly
temperature, j = curve of mean monthly precipitation,
k = dry season, 1 = wet season, m = mean monthly
precipitation over 100 mm, n = months with absolute
daily minimum temperature below 0°C, p = mean dura-
tion of frost-free period in days).
respectively. The period during which frost is likely
to occur lasts, on average, for 106 days from May to
September, during which period frost occurs on about
26 days. Sunshine duration in summer is about 60
percent and in winter 80 percent of the possible.
Mean annual precipitation is about 600 mm.
Rainfall is almost exclusively due to showers and
thunderstorms. Winter months are normally dry and
about 85 percent of the annual precipitation falls
during the summer months from October to March. A
small rainfall peak occurs in January. Heavy falls of
125 mm to 150 mm are occasionally recorded in a
few hours. The average annual number of thunder-
storms is about 75. These storms are often violent with
severe lightning and strong, but short-lived, gusty,
south-westerly winds and are sometimes accompanied
by hail. The area has a high hail frequency with an
average of four to seven occurrences annually.
1 . 3 Geomorphology and geology
1.3.1 Relief
The study area lies between 1460 m and 1520 m
above sea level. It consists of a large, undulating
plain characterised by the absence of any marked
topographical features. Gentle rises and shallow
hollows throughout, and shallow valleys of the Harts
River and its tributaries in the south are the most
noteworthy topographical features.
Even in this very monotonous landscape a clear
relationship between topography and geology is
evident. The south-eastern corner is underlain by
by Archaean granite, which forms dome-shaped hills.
This slightly-raised portion is part of the divide
between the Harts River to the west and Schoon
Spruit in the east. The area occupied by Ventersdorp
lava, south and south-east of Lichtenburg, is usually
devoid of physiographic features. Volcanic brecchia
appears in dome-shaped outcrops and volcanic tuff
usually forms a featureless topography. The area
covered by dolomite, to the north of Lichtenburg, is
very flat, being relieved by occasional chert ridges,
shallow depressions, dry watercourses and, more
frequently, by sink-holes. Surface limestone, west of
Lichtenburg, builds extensive flat plains.
1.3.2 Geological strata
The geology of the area has been described by Von
Backstrom et al. (1953), on which the following
account is based.
Although Archaean granite occurs south-east of
Lichtenburg, outcrops are rare. It is usually overlain
by sandy surface drift.
Deposits of the Ventersdorp system are found in a
belt along the southern edge of the area from the
south-western corner to a point south of Lichtenburg
and then occur again along the eastern boundary of
the area. The system consists mainly of andesitic lava.
Intercalated are agglomerate and volcanic conglome-
rate, pyroclastic sediments or tuff and clastic sediments
including boulder conglomerate.
Rocks of the Dolomite series of the Transvaal
system are, for the most part, covered by more recent
deposits, particularly of gravel and surface limestone.
Small outcrops occur north and north-east of Lichten-
burg, on the boundary of the study area. The Dolomite
series consists mainly of blue-grey, massive, dolomitic
limestone, with intercalated lenses and layers of
chert and shale, the latter being developed more
particularly near the base of the Series. In many
places dolomite has been weathered chemically and
numerous sink-holes are found as a result.
J. W. MORRIS
271
Dwyka series tillite and shale of the Karoo
system occur over a fairly wide area south and east
of Lichtenburg. Owing to fast weathering and the
softness of the formation, rocks are seldom exposed
at the surface. Tillite is composed of a soft, clayey,
unstratified matrix in which unsorted fragments are
spread at random. The fragments are mostly of chert
and various quartzites. Examples of glaciated pave-
ments and other distinct signs of glaciation are found.
Economically, the Tertiary and recent deposits are
the most important in the area. They consist of gravel,
surface limestone, sand and alluvium.
Gravel is found mainly overlying Dolomite series
rocks in a belt along the northern edge of the area. The
deposits, which vary in depth from a few centimetres
to over 50 m, are made up of rounded alluvial material
with which is mixed angular, eluvial chert. The alluvial
material consists mainly of white, cream-coloured or
light grey pebbles of chert and chalcedony although a
variety of pebbles derived from other geological
systems are also encountered. The eluvial material
is composed of angular and irregularly-shaped
fragments of chert and concretionary grains of iron,
or manganese-iron, derived from weathering of the
dolomite floor. Dolomite series rock includes a
proportion of very hard, white or grey chert in
layers, lenses and veins. As the matrix is dissolved by
chemical action, chert remains behind as angular
rubble.
Surface limestone covers a large area west of
Lichtenburg. It is not generally exposed at the surface,
but is covered by a thin, sandy, overburden usually
from 20 cm to one metre thick. The thickness of the
limestone itself is difficult to determine but it is
known to occur as a thin, hard, crust although it is
usually much thicker. Depths between 10 m and 38 m
have been recorded. The quality of the limestone
varies from some of great purity to some that can
be described as calcrete. At the surface, the limestone is
usually hard and massive while at greater depths it
is softer, granular, friable and slightly stratified.
In the area north-west of Lichtenburg the older
formations are overlain by red and yellowish Kala-
hari sand, consisting in the main of slightly rounded
grains of quartz, less than one mm in diameter.
South-east of Lichtenburg, coarse-grained sand covers
a fairly extensive area. It consists of subangular
grains of quartz and felspar with flakes of mica and
is mainly derived from underlying Archaean granite.
1.3.3 Erosion surfaces
Erosion surfaces of the Highveld Agricultural
Region have been mapped by Harmse (1967). Dolo-
mite, and gravels overlying dolomite, north of Lichten-
burg are of the Karst structural phase of the African
surface. Sand overlying the rest of the study area is
of the aggradational phase (aeolian sand) of the
African surface. Sand was transported from the
north-west.
1.3.4 Economic geology
As the surface mining of diamonds and limestone
within the study area influence the natural vegetation,
these activities are described briefly.
The first diamond in the Lichtenburg district was
discovered during 1921, although diamonds were
being mined in the South-western Transvaal before
1914 (Wagner, 1914; Du Toit, 1951; Draper, 1928;
Williams, 1930). As diamond discoveries increased at
Lichtenburg, more and more fortune hunters arrived
and many spectacular ‘rushes’ were held, culminating
in the famous ‘charge’ on the farm Grasfontein in
March, 1927 when some 25 000 runners participated.
In August, 1926, an estimated 56 000 non-Europeans
were employed. According to Williams (1930), a
population of over 100 000 was resident on the new
diamond fields shortly after their discovery. The
presence of this large population, concentrated in a
small area north of Lichtenburg, must have had a
marked effect on the natural vegetation. In addition
to direct disturbance by trampling, digging and
clearing, the keeping of livestock, gathering of fire-
wood and cultivation of crops probably caused rapid
deterioration of vegetation near the diggings. Very
little activity is evident on the diggings now and only
an occasional miner is encountered.
A large proportion of the area underlain by surface
limestone has been purchased by two cement com-
panies with factories in the area. The thin, sandy
overburden is bulldozed away and surface limestone
is mined by open-cast methods.
1 . 4 Soils
Soils of the 2626AA quarter degree square have
been described and mapped by Van der Bank (1968).
His map of 17 soil series, four soil complexes and
three land classes has been simplified in collaboration
with E. Verster (pers. comm.) to eight soil series to
conform with present soil nomenclatural concepts of
the Soils and irrigation Research Institute, Pretoria.
The soil survey by Van der Bank (1968) clearly
illustrates from one side the differences in emphasis
placed by pedologists and plant ecologists in the
same area. He describes, in detail, soils which are
under heavy cultivation while the Dolomite lithosol
receives scant mention. To the botanist, on the other
hand, the natural vegetation of the ploughed area is
solely of historical interest while the vegetation of the
unploughed areas (the lithosols) has great economic
and academic value. These differences in emphasis
naturally hinder close correlation between results of
these and other soil and vegetation surveys of the
same area.
1.4.1 Shorrocks, Mangano and Lichtenburg Series
Shorrocks series soils occur in small patches north-
west of Lichtenburg. Mangano series soils occur very
locally within the Dolomite region north of Lichten-
burg, while Lichtenburg series soils cover relatively
small areas near the Harts River in the south-eastern
corner of the study area.
Shorrocks, Mangano and Lichtenburg Series are
well-drained soils. They are characterised by good
internal drainage and weak structure. They have
high, fine sand and low clay content, prominent red
colours and an absence of mottling. Horizons that
impede drainage are absent. Kaolinite is the principal
clay mineral and the exchange capacity varies between
two and eight milli-equivalents percent. Calcium and
magnesium are the dominant exchange cations
throughout the profile.
1.4.2 Soetmelk Series
Soetmelk is the non-lithosol series covering the
largest area in the quarter degree study area. It
occurs throughout the area not underlain by dolomite.
Restricted drainage is a characteristic of Soetmelk
soils. With increasing depth the clay content increases
and the structure becomes weak medium blocky.
Red and yellow mottles associated with uncsmented
iron concretions are distinctive features of the lower
horizons. Principal clay minerals are kaolinite and
illite. Montmorillonite tends to increase in the lower
272
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
horizons. Exchange capacities vary between four and
eight milli-equivalents percent. Calcium and magne-
sium are the dominant cations.
1.4.3 Rensburg, Bonheim and Lindley Series
The Rensburg, Bonheim and Lindley series are
poorly-drained soils. Poor permeability, high clay
content, high exchange capacity and strong blocky or
prismatic structure are the salient features of these
Series.
The occurrence of these soils, either collectively
or singly, is limited in extent. Rensburg series occurs
in the bed of the Harts River while Bonheim series
soils are restricted to slopes of the Harts River valley,
where the river leaves the dolomite substrate. Lindley
series occurs in small patches north and north-west of
Lichtenburg. It is usually underlain by dolomite.
1.4.4 Kalkbank Series
The feature common to Kalkbank sandy type and
Kalkbank loamy type soils is the underlying surface
limestone formation encountered at shallow depths.
Where the limestone is buried deeper the soil is
usually Soetmelk series. The parent materials are
either aeolian sand, drift materials, or both.
These soils cover areas of moderate size, usually in
complexes, to the west of Lichtenburg.
1 . 5 Vegetation
The vegetation of the study area is described by
Acocks (1953) in his survey of the veld types of
South Africa (Fig. 3).
In the South-western Transvaal, Dry Cymbopogon-
Themeda Veld (Veld Type 50) occurs in an arc from
Lichtenburg to south-west of Delareyville and then
south to Wolmaransstad. This arc, comprising the
northern variation of the Veld Type, is found on
sandy soils. The dominant species is Themeda triandra.
Cymbopogon plurinodis is the tallest grass, but is
usually not common. This Veld Type lies between
altitudes of 1 280 m and 1 370 m on flat, sandy
country with a summer rainfall of 430 to 580 mm per
annum and with frosty winters. Species of general
occurrence are given in Table 2.
Species of less general occurrence include : Cynodon
dactylon, Digitaria argyrograpta, D. eriantha, Panicum
coloration and Stipagrostis uniplumis.
Sandy Cymbopogon-Themeda Veld (48) occurs in
the rough square bounded by Lichtenburg, Venters-
dorp, Klerksdorp and Ottosdal, to the immediate
east of the arc of Dry Cymbopogon-Themeda Veld.
The square comprises the northern variation of the
Veld Type where the altitude ranges from 1 310 m to
25°
26°
2 7‘
J. W. MORRIS
273
TABLE 2. Relative abundance values (in thousands) of those species of general occurrence, according to Acocks 0975) with
relafye abundances of over 1 000 in Dry Cymbopogon-Themeda Veld (50), Sandy Cymbopogon-Themeda Veld (48) and Baker,-
vela (oi )
1 520 m and summer rainfall is from 510 to 690 mm.
Winters are frosty. Species of general occurrence are
listed in Table 2. Species of less general occurrence
include Cynodon dactylon, Cynodon incompletus,
Digitaria argyrograpta and Helichrysum rugulosum.
According to Acocks, this Veld Type merges into the
western variation of Bankenveld and needs more
study. Dry Cymbopogon-Themeda Veld usually occurs
at a slightly lower elevation than Sandy Cymbopogon-
Themeda Veld and usually receives slightly less rain.
Sandy Cymbopogon-Themeda Veld and Dry Cym-
bopogon-Themeda Veld are both Pure Grassveld
Types while Bankenveld (61) is a False Grassveld
type. Bankenveld occurs in a belt from east of Venters-
dorp, to Klerksdorp and Parys. The Western varia-
tion occurs near Lichtenburg. It is found on sandy
plains and low, rocky ridges, ranging in altitude from
1 370 m to 1 680 m and receives 560 to 690 mm rain,
mostly in summer. It is a rather sparse, sour, strongly
tufted vegetation and, in the nature of its grasses, is
clearly transitional, according to Acocks, from Sandy
Cymbopogon-Themeda Veld to Sour Bushveld (20),
which occurs north of the study area. The climax was
possibly an open savanna with Acacia caffra. Species
of general occurrence are given in Table 2. Species
of less general occurrence include Anthospermum
rigidum, Digitaria eriantha, D. monodactyla, Eus-
tachys mutica, Kohautia amatymbica and Pygmaeo-
thamnus zeyheri.
Tentative boundaries to Veld Types drawn by
Acocks (1953) for the South-western Transvaal may
be re-drawn after more intensive study. Limits ot
Bankenveld near Potchefstroom and Ventersdorp,
east of the study area, have been accurately mapped
by Grunow (1959). Photographs from NASA/
ERTS-1 flights will greatly aid the further mapping
of vegetation in this area at reconnaissance scales.
Bankenveld is actually found as far south as Lichten-
burg, as far west as a line from Lichtenburg to Mafe-
king and as far east as a line from Lichtenburg to
Rustenburg, although this is not apparent from
Acocks’s map.
1 . 6 Land-use
Broad land-use categories are closely tied to
geology, soils and vegetation in the study area. The
parts with deep, well-drained soils overlying all
geological systems except dolomite (Dry Cymbopogon-
Themeda- and Sandy Cymbopogon-Themeda Veld
Types) are extensively ploughed. Van der Bank
(1968) comments that, in practice, all soils that are
ploughable have already been ploughed. The principal
crop is maize and limited quantities of sunflowers,
grain sorghum, groundnuts and cattle fodder are
grown. It is estimated by Van der Bank (1968) that
the average yield of the maize crop is about 1 170
kg/ha although some farmers reap 1 550 or more
kg/ha.
Cattle ranching is the chief occupation of farmers
on the dolomitic lithosols (Bankenveld Veld Type)
north of Lichtenburg. Occasional sink-holes in the
area, which have become filled with aeolian sand, are
invariably cultivated for cash crops like maize. Some
irrigation, using the good supplies of water from
boreholes, is undertaken.
An alarming activity is the open-cast mining of
surface limestone in the area by two cement companies.
Relatively large tracts of land have been acquired and
274
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
are being systematically laid desolate as no attempt
appears to have been made to stabilise and re-
vegetate stripped areas.
1.7 CT Grassland and Bank env eld Land Systems
According to Dowling (1968) and Mabbutt (1968),
the land of a region is conceived as a series of Land
Systems, each of which contains typical land facets,
which have similar features wherever they occur and
which can be readily identified on aerial photographs.
When relief, geology, geomorphology, soils, vegeta-
tion and land-use are considered, two Land Systems
may be recognised in the study area. These two
Land Systems were treated separately in the sampling
and analysis of vegetation reported in this account.
One Land System, named CT Grassland, is under-
lain by granite, Ventersdorp lavas, Dwyka tillite and
surface limestone on the aggradational phase (aeolian
sand) of the African erosion surface. Soils of Shor-
rocks, Mangano and Lichtenburg series are generally
sandy and well-drained. The natural vegetation was
Dry Cymbopogon-Themeda Veld or Sandy Cymbopo-
gon-Themeda Veld but most of it has been destroyed
for the cultivation of maize, the chief land-use.
The second Land System, named Bankenveld, is
underlain by dolomite, variously covered by alluvial
gravels on the Karst structural phase of the African
erosion surface, and has lithosolic soils. The Veld
Type is Bankenveld and cattle ranching is the main
land-use.
2. PROCEDURES USED IN THIS STUDY
2 . 1 Sampling strategy
The most important consideration in designing the
vegetation sampling strategy was ensurance of
compatibility with other component projects of the
ecological survey of the Highveld Agricultural Region.
A common sampling strategy will enhance possibili-
ties for integration with and extrapolation between
individual surveys, including some by other officers.
As J. C. Scheepers of the Botanical Research Insti-
tute, Pretoria, who is responsible for surveying the
eastern half of the Region, had started field sampling
before the study reported here was initiated, his
general strategy, as outlined below was followed.
2.1.1 Sample placement and size
Initially, the 2626AA quarter degree square (Fig. 1)
was taken as the study area. All lands under culti-
vation, or showing signs of past cultivation, as well
as the town of Lichtenburg and the bed of the Harts
River were excluded from the area to be sampled.
The remaining area was stratified into Bankenveld
and CT Grassland Land Systems (see 1.7) and phy-
siognomic-physiographic units were delimited on
1 :36 000-scale aerial photographs. Morris (1973)
details the stratified-random sampling strategy that
was used to mark 220 sample positions within the
study area and gives reasons for the study area
having to be enlarged to that illustrated in Fig. 1.
Briefly, insufficient suitable sampling sites were
found within the quarter degree square.
The sample size of 4x4 m, chosen during pilot
studies for the Highveld Survey Project, was retained
for uniformity. Pilot studies had shown that a sample
area of 16 m2 was both the smallest adequate sample
for grassland vegetation of this kind and the largest
area that could be sampled in an economically-
justifiable time (J. C. Scheepers, pers. comm.). Species
present in a belt, approximately two metres wide,
around the perimeter of the sample were also recorded
to aid re-allocation of samples mis-classified by asso-
ciation analysis owing to the chance absence of a
positive dividing species. Details of quadrat location
in the field are given in Morris (1973).
2.1.2 Habitat data
A limited amount of habitat information was
gathered. Physical factors recorded for each site
included geology, geomorphology, aspect, angle of
slope and exposure. Soil series (Van der Bank, 1968)
and depth were recorded and then for each horizon,
soil pH, soil reaction to dilute hydrochloric acid
(HC1), moist soil colour (Munsell) and soil texture
were noted. Biotic influence was noted by animal type
and by degree on a four-point scale from absent to
very intense.
2.1.3 Vegetation data
Total basal cover and height and basal cover of
each constituent stratum were estimated for the 16 m2
sample and the presence of all permanently-recognis-
able plant species was recorded. Cover-abundance on
the Braun-Blanquet scale (Werger, 1973) was also
noted for each species.
2 . 2 Association analysis
At the time of sampling, the only objective method
for classifying vegetation known to be suitable was
the hierarchical technique of the Southampton-
Canberra school (Williams & Lance, 1958; Williams
& Lambert, 1959, 1960, 1961; Lambert & Williams,
1962). The original technique, association analysis,
has been used by a number of ecologists with varying
degrees of success in a number of vegetation types in
South Africa, including Van der Walt (1962) in
grassland, mountain scrub and karoo vegetation,
Grunow (1965a, 1965b, 1967) in bushveld, Downing
(1966) in vlei vegetation, Roberts (1966), Miller (1966),
Miller & Booysen (1968) and Scheepers (1969) in
grassland, Taylor (1969) and Boucher (1972) in
fynbos, Downing (1972) in savanna and woodland
vegetation and Coetzee (1972) in Bankenveld.
Although more advanced analyses had been carried
out successfully (for example: Grunow & Lance,
1969), the computer programs were not available in
South Africa when the analyses reported here were
carried out.
The monothetic-divisive technique of association
analysis, used for classification in this account, is so
well known as not to require detailed description.
Briefly, quadrats to be classified are hierarchically
divided on the basis of the presence or absence within
each quadrat of the species with the highest association
[Chi-squared (x2) in one or other form] with every
other species. Division by this strategy has been found
to remove most heterogeneity from the parent popula-
tion of quadrats, resulting in groups with a higher
degree of homogeneity than any other grouping.
An analysis was carried out on the 220 quadrats
(16 m2) of the study area and then another was
carried out on the 110-quadrat subset of Bankenveld
Land System quadrats. The former, known below as
the Total analysis, was done to obtain an overall
classification of the vegetation of the area and, in
particular, to distinguish the main vegetation types.
The second analysis, known as the Bankenveld
analysis, was done to obtain more detailed information
about Bankenveld, the area whose natural and semi-
natural vegetation was of most importance. The
Bankenveld analysis was necessary as the Total
analysis did not separate the Bankenveld from the
CT Grassland Land System clearly enough. In both
analyses, the division parameter used was £( x2/N)L
Number of species
J. W. MORRIS
275
Species frequency classes
Fig. 4. — Number of species present in each species frequency class over entire study area, within Bankenveld and within
CT Grassland Land Systems.
Fig. 5. — Association analysis hierarchy of Lichtenburg
study area. N. = total number of quadrats in each
group and C — TG is number of CT Grassland Land
System quadrats in group. Dividing species are: 1 =
Schizachyrium sanguimum, 2 = Kohautia omahekensis,
3 = Brachiaria serrata , 4 = Stipagrostis uniplumis , 5 =
Crabbea angustifolia , 6 = Heteropogon contortus, 7 =
Triraphis andropogonoides , 8 = Eustachys mutica , 9 =
Bulbostylis burchellii, 10 = Loudetia simplex , 11 =
Indigofera daleoid.es , 1 2 = Barleria macrostegia , 1 3 =
Eragrostis lehmanniana , 1 4 = Hermannia depressa , 1 5 =
Blepharis integrifolia , 16 = Vernonia oligocephala.
276 AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
Subdivision was terminated when the highest
single x2 (with Yates’s correction) failed to exceed
3,84 (p=0,05), or less than eight quadrats remained
in the group. (The neutral term ‘group’ is preferred
to ‘association’, which has a specific meaning in the
Braun-Blanquet sense (Werger, 1973), while other
neutral terms like ‘community’ could have been
used). For each analysis, species occurring in fewer
than six quadrats were masked as it was presumed
that those species were rare enough not to have
Indicator value. Their exclusion greatly increased
the speed of computation. In each analysis, straight
lines were drawn across the hierarchies at fairly
low highest single X 2 levels and groups existing at
those levels were numbered from left to right. From
that level, groups were interpreted downwards to
the final groups of the analysis and upwards to the
first division.
Although, for economy of reference in the text,
groups are usually referred to by numbers and letters,
it was required that defined groups be given names as
well. The suffix ‘Bankenveld’ was used to name all
groups of the Bankenveld Land System and ‘Grass-
land’, ‘Woodland’ and ‘Savanna’ suffixes were used
for association analysis groups of the CT Grassland
Land System. One or two species were chosen for
inclusion in the name. Where possible, positive divi-
ding species from the association analysis were used
but species with significant Indicator values or high
cover-abundance ratings (see later) were also used.
In order to create unique names, it was sometimes
necessary to overlook a species which appeared
suitable as it was even more appropriate for another
group.
2 . 3 Presence and Indicator value
Presence and presence percentage were calculated
for every species in every group. Presence is the
number of times a species occurs in the quadrats of
a group and presence percentage is presence expressed
as a percentage of the number of quadrats in the
group.
Indicator value (Goodall, 1953) for each species
was also calculated. Indicator value, according to
Goodall, expresses the presence of a species in a
particular group against its presence in all other
groups.
2.4 Re-allocation
Inspection of final groups suggested that because
their habitat data were markedly dissimilar from
those of other quadrats of the group, certain quadrats
were misclassified. By reference to species listed from
the area surrounding each 4 by 4 m quadrat they
were re-allocated to other groups on the basis of the
dividing species of the hierarchy. Some quadrats,
which, from inspection, appeared misclassified but
which could not be satisfactorily re-allocated by the
above method were left in their original groups and are
discussed with those groups, as misplaced quadrats.
3. CLASSIFICATION OF THE VEGETATION BY
ASSOCIATION ANALYSIS
3 . 1 Summary statistics of data
The total number of species encountered in the 220
quadrats was 247. Within Bankenveld, 211 species
were noted, only 36 fewer than in all the quadrats,
whereas only 165 species were found in CT Grassland
quadrats. Proportions of common and uncommon
species are summarised in Fig. 4. The shapes of all
three graphs indicate that many species are uncommon
(have low overall presence) and that a few species
are very common (have high overall presence).
Within the entire area nearly 100 species occurred
in fewer than six quadrats. Of these, 35 occurred in
only one quadrat and 26 in only two quadrats. As
nearly 40 percent of the species were uncommon
(defined as species occurring in five or fewer quadrats),
it was decided to mask uncommon species from the
association analyses. Within Bankenveld, 92 species
occurred in fewer than six quadrats, 42 species
occurred in only one quadrat and 24 were found in
only two quadrats.
The commonest species in Bankenveld were
Aristida congesta, Justicia anagaloides and Themeda
triandra, occurring in 97, 87 and 86 of the 1 10 quadrats,
respectively. Over the entire study area, Themeda
triandra was the species occurring most frequently
(in 184 quadrats). Other commonly-occurring species
were Aristida congesta (171 quadrats), Elionurus
argenteus (150 quadrats), Anthospermum rigidum (149
quadrats) and Justicia anagaloides (136 quadrats).
A Bankenveld quadrat contained most species (54).
In CT Grassland, the highest number of species in a
quadrat was 36. In Bankenveld, the lowest number of
species was 18, and in CT Grassland it was 11. The
average number of species in a Bankenveld quadrat
was 36,5 [standard deviation (SD)=7,5] and in CT
Grassland the average was 24,3 (SD=5,5). The
overall average was 30,4 (SD=9,0).
3 . 2 Total association analysis
3.2.1 Description of hierarchy
The association analysis hierarchy classifying all
220 quadrats is given in Fig. 5. The quadrats are
divided into four major groups. These four groups are
very distinct, being maintained from a level of H.S.
X2>54,0 (H.S. x2 is the abbreviation used for highest
single chi-square throughout this account) to H.S.
X2<28,5 in the case of the third and fourth groups
and more than double that amount in the case of the
first group. At a level of H.S. x2 = 20,0 there are
nine groups and at a level of H.S. x2 — 15,0 there
are 14 groups. At the 14-group level the mean number
of quadrats per group is 15,7. Inspection of the
results showed that certain subgroups of the fourth
major group could be profitably subdivided to a lower
level than H.S. x2 = 15,0. Thus, divisions above
H.S. x2 = 7, 5 are shown for this major group in
Fig 5, where different base lines are used to indicate
the two levels of subdivision. As the fourth major
group contains more than one third (36 percent) of
the quadrats, sub-division to a lower level results in
groups that are, in general, not much smaller than
those in the other major groups (Table 3).
TABLE 3. — Statistics of major groups
tat H.S. x2=15,0
* at H.S. x'2 = 7,5
There are three final groups in the first major group,
two in the second, four in the third and nine in the
fourth major group. The mean number of quadrats
in the final groups of each major group is given in
Table 3. At H.S. x2 = 15,0 the mean number of
J. W. MORRIS
277
quadrats per final group is remarkably similar for the
four major groups. The standard deviation of the
mean for each major group, however, indicates more
variation in number of quadrats per group within
the second and third major groups than within the
first and fourth groups. At H.S. y2 = 15,0 the overall
mean number of quadrats per final group is 15,7
with a standard deviation of 0,76. With the finer
sub-division of the fourth major group to H.S. y2 =
7,5 the mean becomes 12,1 (SD = 3,5).
Groups are numbered from 1 to 9 at the H.S. y2 =
20,0 level and further subdivisions are labelled
alphabetically and numerically. Groups are usually
referred to in the text by number for brevity although,
as was mentioned previously, groups are also named
after dominant species and appropriate habitat
features.
3.2.2 Re-allocation
Following the procedure described earlier, quadrat
114, originally in Group 3a, was transferred to 4b,
quadrat 112 from 3b to 5b, quadrat 152 from 9a to
7a and quadrat 126 from 9c to 9a. Except where
otherwise indicated all results given above and below
and including results in all tables and figures relate to
groups after re-allocation.
3.2.3 Interpretation of major groups
The association analysis did not completely separate
Bankenveld from CT Grassland Land Systems. The
first two major groups are, however, largely Banken-
veld and the last two mainly CT Grassland. Before
re-allocation, the first major group consisted of 47
Bankenveld quadrats and no CT Grassland quadrats
and the second major group of 34 Bankenveld and two
CT Grassland quadrats. After re-allocation, the first
two major groups consisted entirely of Bankenveld
quadrats. Thus, the presence of either Schizachyrium
sanguineum or Kohautia omahekensis (the first two
dividing species) in a quadrat is a good indication of
Bankenveld. The absence of these species does not,
however, indicate CT Grassland as 29 of the 110
Bankenveld quadrats also contain neither of these
species. Nine of these 29 quadrats make up Group 4a,
two occur in Group 5a, five in Group 5b, seven in
Group 6, four in Group 7c and two in Group 8. The
H.S. x2 division levels indicate that quadrats of the
first major group are very distinct and are not related
to any quadrats outside Bankenveld. The second major
group is almost as distinct. The slight admixture of
Bankenveld quadrats in the third and fourth major
groups suggests that some Bankenveld quadrats are
floristically related to some CT Grassland quadrats
but that the reverse does not hold.
3.2.4 Final groups
As a separate association analysis of Bankenveld
quadrats was carried out, a description is not given of
the first two major groups and their final groups and
of Group 4a, which are made up entirely of Banken-
veld quadrats. As presence percentage data are pre-
sented in a modified Roman table (Werger, 1973),
where groups and species have been shuffled to
highlight noda, the following discussion of groups is
not strictly in the order in which groups were split
off the hierarchy.
(a) Group 4b (Short Stipagrostis uniplumis Cal-
careous Grassland)
Group 4b is the first CT Grassland group to be
split off. The quadrats form a homogeneous group
with regard to species composition and habitat, with
the exception of three quadrats, which are somewhat
aberrant with regard to habitat. As it was not possible
to re-allocate these three quadrats by reference to the
species in the surrounds, they were retained in the
Group.
With two exceptions, all quadrats occur on shallow
aeolian sand overlying surface limestone. In a few
cases the sand deposit is over 30 cm deep, so that the
soil may be classified as Soetmelk series, but in general
it is a 2,5 to 10 cm deep lithosol. All quadrats are
situated on a flat plain with virtually no relief. Soil
pH is usually 7,5 but occasionally 7,0 or 8,0. Soil
HC1 reaction is usually strong or moderately strong in
shallow soil and weaker where the soil is deeper. A
negative correlation, significant at p — 0,01 was
found between soil depth (in cm) and HC1 reaction
recorded on a 0, 1, 2, 3 intensity scale. Grazing was
light, or absent, for most quadrats of this Group. In
about one third of the quadrats selective grazing was
observed and in four quadrats heavy grazing and
trampling were recorded. Basal cover data are given
in Table 4 together with mean number of species per
quadrat. As the overall average number of species per
quadrat in CT Grassland is about 24, quadrats of this
Group are relatively rich in species. Species com-
monly occurring in quadrats of Group 4b are listed
in Table 4. All species with a presence greater than 39
percent are listed and species with lower presence
but positive, significant Indicator values are also
included. Brachiaria serrata, Stipagrostis uniplumis
and Themeda triandra occur in all 21 quadrats of the
Group. Possible indicator species, i.e. species which
are common within the Group but are uncommon
through the rest of the study area, include Finger-
huthia africana, Geigeria burkei and Convolvulus
ocellatus var. ornatus, although the latter is present
in only 12 of the quadrats of the Group.
(b) Group 6 (Tall Stipagrostis uniplumis Calcareous
Grassland)
Group 6 is a small group of 13 quadrats, of which
six were located in CT Grassland. All the quadrats
are located west of Lichtenburg, some near the town
and some as far as 25 km away. All but one of the
quadrats occur on flat plains underlain by surface
limestone deposits. Slope is negligible and sites are
very exposed. One quadrat occurs on a fiat plain
where sand, over 100 cm deep, overlies dolomite and
gravels of the Transvaal System.
Soil over the limestone is sandy and usually 30 to
50 cm deep. Soil pH is 7,0 or 7,5 and soil HC1
reaction is slight or absent. Grazing was usually light
and average total basal cover for both strata was
13,7 percent. While Stipagrostis uniplumis is the only
species occurring in all six CT Grassland quadrats of
Group 6 (Table 4), the Group is too small for any
Indicator values to be significant. Both Stipagrostis
uniplumis and Themeda triandra reach high cover-
abundance values in quadrats of this Group. No
species with a presence of over 49 percent is restricted
in distribution to quadrats of this group.
(c) Similarities between Groups 4b and 6
Groups 4b (Short Stipagrostis uniplumis Calcareous
Grassland) and 6 (Tall Stipagrostis uniplumis Cal-
careous Grassland) have many features in common.
In addition to the similarity of dividing species (Fig. 5),
these Groups share the same geological substrate,
geomorphology and soils. Soils are, however, slightly
deeper in Group 6 and HC1 reaction is only slight, or
absent, in contrast with the strong or moderately
strong reaction in Group 4b. Mean basal cover ot the
tall grass stratum in Group 6 was double that in
Group 4b. The mean number of species per quadrat
278
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
TABLE 4. — Mean number of species per quadrat and mean basal cover by stratum and presence percentage of common species in
each group where arrangement of species and groups follows a Braun-Blanquet Roman Table order. X indicates a high cover-
abundance rating for the species in most, if not all, quadrats of the group and a dash ( — ) indicates a value of less than 40%
Specimens of Morris & Boucher 70 and Morris & Engelbrecht 1267, housed in National Herbarium, Pretoria.
J. W. MORRIS
279
was the same in both Groups. Three species, Stipa-
grostis uniplumis, Fingerhuthia africana and Convol-
vulus ocellatus var. ornatus were common in these two
Groups but nowhere else.
Most of the area formerly occupied by Short and
Tall S. uniplumis Calcareous Grassland has been
ploughed for maize cultivation. Most of the rest,
where the soil is too shallow for ploughing, has been
excavated to supply limestone for local cement
factories or has, at least, been bought for this use in
future. The area covered by Tall and Short S. uni-
plumis Calcareous Grassland is decreasing rapidly as
a result of this activity.
(d) Group 5b ( Elionurus argenteus Secondary Grass-
land)
As Group 5b is the last group of the third major
group of the hierarchy, a certain amount of hetero-
geneity in fioristics as well as in habitat was expected.
Heterogeneity will be apparent from the description
which follows.
Quadrats of this Group occur in three main clusters
north-west, north-east and south of Lichtenburg,
respectively. Various geological substrates underlie
quadrats of this Group. Half are underlain by Venters-
dorp lava, quartzites, brecchia or conglomerate, four
are on deep sand overlying dolomite and chert of the
Transvaal system and two quadrats each are found on
surface limestone, Archaean granite and Dwyka
tillite. Three quadrats face north on very gentle
slopes and the others occur on flat plains or crests of
hills. Half the quadrats in this Group have soil over
80 cm deep and the rest are on shallower soil with an
average depth of 15 cm. All quadrats are found on
Soetmelk soil series. Soil pH is usually 6,5 but values
of 6,0 or 7,0 are occasionally recorded. Biotic
influence varied widely. Some quadrats were only
lightly grazed while others were heavily grazed and
some showed signs of soil erosion. All heavily-grazed
quadrats were located on deep soil while only light
grazing was recorded on shallow soils. Mean total
basal cover was slightly lower than in Group 4b and
mean number of species per quadrat was almost the
Fig. 6. — Salvia radula, 50 cm
tall, in Short Stipagrostis
uniplumis Calcareous Grass-
land. Grasses include 5.
uniplumis , Brachiaria serrata ,
Themeda triandra , Aristida
diffusa var. burkei and Elio-
nurus argenteus. Hendriks-
rust, Lichtenburg District.
Fig. 7. — Desolation of an aban-
doned, flooded open-cast
calcrete mine. Plant colo-
nisation of such areas is slow.
This site was previously
Stipagrostis uniplumis Cal-
careous Grassland. East of
Lichtenburg on Town Lands.
280
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
same in both groups (Table 4). Species commonly
occurring in quadrats of Group 5b are listed in Table
4. Only Brachiaria serrata occurs in all quadrats.
Elionurus argenteus, after which the Group is named,
is the only species with high cover-abundance in many
quadrats of the Group. No species with high presence
percentage have significant Indicator values. Only
Chascanum hederaceum and Helichrysum zeyheri are
not recorded in the fioristic summary of any other
group.
(e) Group 8 ( Eliomirus argenteus Primary Grassland)
Quadrats of Group 8 occur mainly at two places,
east of and west of Lichtenburg, respectively.
Five quadrats occur on Ventersdorp conglomerate,
lava or quartzites, three on sand overlying dolomite
and gravels and one on Dwyka tillite. Quadrats are
on extensive flat plains or on gentle waxing slopes.
The soils developed from the three rock types all
belong to Soetmelk series. Soils are usually 60 cm to
over one metre deep, soil pH is usually between 6,5
and 7,0 and no soil HC1 reaction is recorded. With
only one exception, the quadrats of this Group were
not grazed or were only lightly grazed and in good
condition. Species present in more than 39 percent
of the quadrats of Group 8 are listed in Table 4.
Heteropogon contortus is the only species occurring
in all 9 quadrats of this Group. The Group is too
small for any indicator values to be significant. High
cover-abundance values were only rarely recorded for
species in quadrats of this Group. In addition to the
widespread grass, Eliomirus argenteus, Eragrostis
gununiflua and Eustachys mutica were the only species
with high cover-abandance values in three or more
quadrats.
(f) Similarities between Groups 5b and 8
Groups 5b (Eliomirus argenteus Secondary Grass-
land) and 8 ( Eliomirus argenteus Primary Grassland)
have a number of features in common and the reason
for the association analysis split is not clear. Most
quadrats of both Groups are found on rocks of the
Ventersdorp System, on flat plains and where the
soil series is Soetmelk. In Group 5b, half the quadrats
are on shallow soil (mean depth 15 cm), while the
other half are on deeper soil (over 80 cm) while in
Group 8, soils are usually over 60 cm deep. Soil pH
and HC1 reaction are similar in the two Groups. In
Group 5b, quadrats on the deeper soils were heavily
grazed while quadrats on the shallower soils were
rested or only lightly grazed. In Group 8, where the
soil is generally deep, grazing is light or the vegetation
has been rested. One of the main differences is, thus,
a disturbance factor of grazing pressure interacting
with the occurrence of shallow soil, resulting in the
names ‘primary’ and ‘secondary’ for these Elionurus
argenteus Grasslands. Basal cover of the tall grass
stratum is slightly higher in Group 8 than in Group
5b but cover of the short grass stratum is the same.
A slightly greater number of species occur in quadrats
of Group 5b than in those of Group 8. Hibiscus
microcarpus and Lasiosiphon capitatus were the only
species which occurred commonly in these two Groups
and nowhere else. Nine species (Table 4) occurred in
over 60 percent of the quadrats of both Groups 5b
and 8. Species which are common in Group 5b (in
over 60 percent of the quadrats) but are either rare
in, or do not occur in Group 8 (less than 60 percent
of the quadrats) include Brachiaria serrata (the divi-
ding species between the two groups), Aristida diffusa
var. burkei, Crabbea angustifolia and Justicia ana-
galoides. Eustachys mutica is the only species found in
over 60 percent of the quadrats of Group 8 and in
fewer than 40 percent of the quadrats of Group 5b.
(g) Group 7
Fifteen quadrats of Group 7, defined by the presence
of both H. depressa and B. integrifolia, form a distinct
Group, 7a, made up entirely of CT Grassland qua-
drats (Fig. 5). The Group defined by the absence of
B. integrifolia, 7b, contains only three quadrats and
as it appears related to Group 7c, it is discussed with it.
Quadrats of Groups 7b and 7c occur scattered
through the study area. Fioristic parameters are
summarised in Table 4. The quadrats are found on a
number of geological substrates and soil series. T.iree
quadrats are located on surface limestone (Soetmelk
soil series), three on sand overlying dolomite and
gravels (Soetmelk series), one on granite and one on
Ventersdorp brecchia and conglomerate. All are on
exposed, flat sites. In most quadrats, grazing was
light or the vegetation had been rested for some time
before sampling. Heavy grazing was recorded from
two quadrats. Species occurring in more than three
of the eight CT Grassland quadrats of these Groups
are listed in Table 4. Only two species, Crabbea
angustifolia and Themeda triandra occur in all eight
quadrats. Themeda triand-a, Heteropogon contortus
and Setaria flabellata had high cover-abundance
Fig. 8. — Extensive maize cultiva-
tion in CT Grassland Land
System. This area was
Elionurus argenteus Grass-
land before cultivation.
Exotic Eucalypus sp. shown
on right, shallow valley of
Harts River in middle dis-
tance and town of Lichten-
burg on horizon. Rietgat,
Lichtenburg District.
J. W. MORRIS
281
estimates in most quadrats of the Groups. The com-
bined Group is too small for any Indicator values
to be significant.
Groups 7b and 7c do not form distinct units. As a
number of quadrats apparently belonging to other
Groups appear to be included in these Groups,
evidenced by the lack of uniformity in habitats, and
as they are small groups, they are not named.
Only one quadrat (120) appears mis-classified in
Group 7a ( Cymbopogon plurinodis Grassland). As it
could not be re-allocated by reference to the species
in the surround, it was left in the Group. Quadrat 152
was re-allocated to this Group from 9a. Quadrats of
Group 7a occur in two clusters near each other. One
cluster borders Lichtenburg to the south-east and the
other is east of the town. With the exception of qua-
drat 120, quadrats of this Group are located on flat
plains underlain by Dwyka tillite. Slope is one percent
or less and sites are exposed. The soil series in all
quadrats is Soetmelk. Average soil depth is about one
metre and soil pH is 7,5 or 8,0. A slight soil HC1
reaction is occasionally recorded. On the other hand,
quadrat 120 occurs in a slight hollow on a flat plain
covered with surface limestone. The soil series is
Kalkbank. Soil depth is about 40 cm with a pH of
7,5 and no soil HC1 reaction. Within Group 7a,
biotic influence was most variable. Some quadrats
enjoyed total protection from grazing, as within the
Lichtenburg aerodrome reserve, while others in the
municipal commonage were heavily grazed and
trampled. All species with a presence exceeding 39
percent in quadrats of Group 7a are listed in Table 4.
Blepharis integrifolia, Hermannia depressa and Theme-
da triandra occur in all 15 quadrats. High cover-
abundance values were recorded for Elionurus
argenteus, Cymbopogon plurinodis and Aristida canes-
cens. Eragrostis stapfii, Rhynchosia totta. Euphorbia
pseudotuberosa and Crabbea hirsuta are not common
enough to be included in the floristic summary of
any other Group.
(h) Group 9
Twelve quadrats are split off Group 9 at H.S. y2
= 16,0 to form Group 9a, within which two slightly
different subgroups (9a i and 9a ii) are recognised.
Group 9c is the last group of this analysis and is
defined by the absence of all dividing species. Quadrat
126 was re-allocated from Group 9c to the first
subgroup of 9a and quadrat 152 was re-allocated from
the first subgroup of 9a to Group 7a on the bases of
species recorded in the surrounds of these quadrats.
Subgroups of Group 9 have a number of features in
common. Most of the quadrats are on Ventersdorp
system rocks. The soil is usually deep with a pH of
6,0 or 7,0. In nearly all quadrats, grazing was heavy
and trampling was recorded. Grass basal cover was
low and the mean number of species per quadrat
was about 20, the lowest of any group of the analysis.
Quadrats of Group 9a ( Acacia karroo Savanna)
(9a i) and Secondary Cymbopogon plurinodis Grassland
(9a ii) occur scattered through the area east of Lichten-
burg. Four quadrats occur together with a cluster of
Group 9c quadrats. One quadrat (126), which was
re-allocated to this Group, occurs west of Lichtenburg
and differs from the rest of the Group in other respects
as well.
Quadrats of the first subgroup of Group 9a (9a i),
named Acacia karroo Savanna, occur on Ventersdorp
quartzites while those of the second subgroup (9a ii),
named Secondary Cymbopogon plurinodis Grassland,
are found on Dwyka tillite substrate. Quadrat 126, the
aberrant, re-allocated quadrat, occurs on a surface
limestone deposit. Quadrats of the first subgroup
occur on extensive flat plains or on waning slopes to
streams while those of the second subgroup occur
on flat plains or waxing slopes. In all cases, slopes are
very slight (one degree or less). About half the qua-
drats are moderately-exposed and half are exposed.
A number of soil series are represented in the first
subgroup, including Lichtenburg, Soetmelk and Rens-
burg, while all three quadrats of the second subgroup
are on Soetmelk series. Soils are relatively deep,
averaging about 90 cm. Soil pH varies between 6,0
and 7,0 and no soil HC1 reaction is recorded. In all
the quadrats of this Group, grazing was heavy and the
vegetation had been trampled. Trees were invading
grassland at a number of Group 9a i sites. The most
common tree was Acacia karroo which occurred as a
seedling or full-grown tree up to 4 m tall. Z iziphus
mucronata occurred occasionally as well as the follo-
wing shrubs: Asparagus laricinus, Diospyros lycioides
and Maytenus heterophylla.
Basal cover was low in quadrats of Group 9a i.
Average total basal cover was only 6,3 percent.
Mean number of species per quadrat in both sub-
groups was about 22,0. Species present in more than
39 percent of the quadrats of Group 9a i are listed in
Table 4. Aristida congesta is the only species occurring
in all quadrats of the Group. Eustachys mutica,
Triraphis anclropogonoides, Eragrostis gummiflua, E.
lehanniana and E. curvula have high cover-abundance
estimates in most quadrats of the Group. Species
present in more than one of the three quadrats of
Group 9a ii are listed in Table 4. As there are only
three quadrats in the Group, these presence values
should not be relied on. Both Groups 9a i and 9a ii
are too small for any Indicator values to be significant.
Species which are more common in Group 9a i than
Group 9a ii include: Digitaria argyrograpta, Eragrostis
gummiflua, E. superba, Lippia scaberrima, Thesium
costatum and Sporobolus africanus. As Group 9a ii
is so small, species presence in it are not known accu-
rately. The following species, however, appear more
common in Group 9a ii than in 9a i: Cymbopogon
plurinodis, Elionurus argenteus, Euphorbia inequilatera,
Barleria macrostegia and Hibiscus pusillus.
There are many similarities between Group 7a
( Cymbopogon plurinodis Grassland) and Group 9a ii
(Secondary Cymbopogon plurinodis Grassland). Group
9a ii is, however, too small for a detailed ecological
analysis and interpretation. The two Groups have
geological, geomorphological and soil characteristics
in common. Soils are slightly shallower in Group 9a ii
than in Group 7a. Biotic influences were variable in
Group 7a but grazing was heavy and trampling marked
in Group 9a ii. Mean basal cover and number of
species per quadrat were lower in the latter Group.
As grazing and trampling are generally more severe
in Group 9a ii than in 7a, the former Group is called
Secondary Cymbopogon plurinodis Grassland and the
latter, Cymbopogon plurinodis Grassland.
Quadrats of Acacia karroo Open Woodland
(Group 9b) are distributed in two clusters, south
and south-east of Lichtenburg, respectively. Nine of
the ten quadrats of this Group are situated on Venters-
dorp System rocks. Ventersdorp lava, conglomerate,
brecchia and quartzites are represented. The remaining
quadrat is located on granite. Most of the quadrats are
located on flat plains or the crests of hills where slope
is too slight to measure. Most of the quadrats are
sheltered or moderately sheltered, in marked contrast
to the quadrats of other groups described above.
Sheltering is usually by the presence of trees in, or near,
the quadrats. Soetmelk series, Soetmelk lithosol and
Lichtenburg series are the most common soils recorded
282
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
for these quadrats. Soil is usually 60 cm to one metre
deep with a pH of 6,0 to 6,5. Nearly all the quadrats
showed signs of heavy grazing and trampling. The
condition of the vegetation of even those quadrats in
which grazing appeared moderate was recorded as
being poor, probably as a result of heavy grazing in
the past.
Basal cover in quadrats of Group 9b was low. Total
average basal cover was only 5,4 percent. The number
of species per quadrat was low, the average being
20,7 and 24 being the highest number of species
recorded in a quadrat of the Group. Species present
in more than 39 percent of the quadrats of Group 9b
are listed in Table 4. Barleria macrostegia is the only
species occurring in all ten quadrats. Brayulinea
densa and Lasiocorys capensis have significant Indica-
tor values. High cover-abundance was recorded for
Cynodon dactylon, Sporobolus africanus and Eragrostis
curvula within the Group. Trees and shrubs are recor-
ded from the surrounds of six quadrats. The most
common tree is Acacia karroo, which attains a
height of 4,5 to 6 m. Occasional, or co-dominant with
A. karroo is A. caffra. Other trees found occasionally
include Celtis africana (7,5 m), Ziziphus mucronata
(5,5 m). Acacia robusta (rare) and Rhus lancea. In
Acacia karroo Open Woodland the trees are usually
one to three crown-diameters apart. Shrubs include
Maytenus heterophylla, which can encroach on shallow
soil with mismanagement, Xeromphis rudis, Grewia
flava (occasional, or common, in understorey),
Asparagus laricinus and Diospyros lycioides.
Six quadrats of Drainage Basin Acacia karroo
Open Woodland (Group 9c) are located east of
Lichtenburg along a tributary of the Harts River.
The other quadrat (183) occurs south-east of Lichten-
burg with quadrats of Groups 9a and 9b. Although the
bed of the Harts River was not sampled, the whole
drainage basin is probably covered by this Woodland.
The geological formation underlying all the quadrats is
Ventersdorp series quartzites. Two quadrats are on
flat plains, four on waning slopes to drainage lines
and one is in a drainage basin. Most quadrats are
north-facing on gentle slopes. Four of the quadrats
are sheltered by having trees in and near them.
A number of soil series are represented in Group
9c. Three quadrats are on Rensburg series alluvial
clay, two on the transition between Rensburg and
Soetmelk series and two on Lichtenburg series.
Soils are usually one metre deep and pH varies between
6,0 and 7,0. Soil HC1 reaction is recorded from two
quadrats. Heavy grazing and trampling were recorded
for five of the quadrats but in two quadrats the vegeta-
tion was in good condition and grazing had been
light. Total basal cover was low (6,2 percent), but
slightly higher than in Group 9b. The mean number of
species per quadrat was by far the lowest value for this
analysis. Species present in more than 39 percent of
the quadrats of Group 9c are listed in Table 4.
Digitaria argyrograpta, in six of the seven quadrats,
is the most common species. D. argyrograpta, Eragros-
tis curvula and Themeda triandra have high cover-
abundance estimates in quadrats of the Group.
Three species, Panicum coloratum, Acacia karroo and
Aptosimum indivisum are not listed as present in any
other group of the analysis (Table 4). Trees and shrubs,
similar to those of Group 9b, were recorded from four
quadrats.
Individually, Groups 9b and 9c are too small to
produce many significant Indicator values. Conside-
ring that they are the last Groups of the analysis,
however, cTsurprising number of significant Indicator
values are found in the combined Group. Seven
species ( Felicia muricata, Digitaria argyrograpta,
Lippia scaberrima, Solanum supinum, Hibiscus pusillus,
Panicum coloratum and Brayulinea densa) out of the
18 species occurring in more than five of the 17
quadrats of the combined Group have significant
Indicator values. Cynodon dactylon, Sporobolus afri-
canus and Eragrostis curvula have high cover-abun-
dance estimates in quadrats of the combined Group.
3 . 3 Bank env eld association analysis
3.3.1 Description of hierarchy
The association analysis hierarchy resulting from
classification of the 110 Bankenveld Land System
quadrats is given in Fig. 11. The first three divisions
yield four distinct major groups, labeled A to D for
Fig. 9. — Four metre tall Acacia
karroo trees in Acacia karroo
Open Woodland. Rietgat,
Lichtenburg District.
J. W. MORRIS
283
Fig. 10. — Harts River in flood,
January 1976. Trees on
banks are mostly exotic
Salix and Eucalypus species.
Floodplain grassland of
Drainage Basin Acacia
karroo Open Woodland in
foreground. Rietgat, Lich-
tenburg District.
Fig. 11. — Association analysis hierarchy of Bankenveld
Land System. Dividing species are: 1 = Diheteropogon
amplectens , 2= Chascanum hederaceum, 3 = Stipagros-
tis uniplumis, 4 = Eragrostis racemosa , 5 = Sporobolus
pectinatus, 6 = Ursinia nana , 7 = Oropetium capense,
8 = Schizachyrium sanguineum, 9 = Corchorus aspleni-
folius, 10 = Heteropogon contortus.
convenience. The first Group, A, is small, consisting
of only 12 quadrats. It is very homogeneous with
regard to species associations as it does not divide
from H.S. x2 > 30,0 until H.S. x2 = 7,2. In addition
to being a major group it is also Final Group 1.
Group B contains 33 quadrats. At H.S. x2 = 8,0 it
is divided into four Final Groups, named 2a, 2b,
2c and 2d. Group C contains 28 quadrats and is
divided into two Final Groups at H.S. x2 = 15,0.
Three Final Groups are obtained from major Group
D, which contains 37 quadrats. Final Groups in A
and B were obtained by terminating division at
H.S. x2 = 8,0 and final groups C and D by termina-
ting division at H.S. x2 = 10,0. These levels were
chosen arbitrarily, for naming purposes, and divisions
below these levels are discussed at appropriate
places in the text.
Based on hierarchy division levels (H.S. x2),
Groups A and B, on the one hand, are most dissimilar
from Groups C and D on the other. Groups C and D
differ more from each other than does Group A
from B, as the former divide further at a higher H.S.
x2 than the latter. The small number of splits above
H.S. x2 = 15,0, at which level there are only five
groups, suggests that the sample consists of a few,
large groups, which are rather homogeneous. The
homogeneity of A has already been mentioned.
Major Groups C and D are also homogeneous, the
former being maintained from H.S. x2 > 35,0 to
H.S. x2 = 18,0 and the latter from H.S. x2 > 35,0
to H.S. x2 = 12,7.
The mean number of quadrats in each final group
is fairly constant. Fewest quadrats are found in
Final Groups 2a, 2b, 2c and 2d (8,2 average). On
average, twelve quadrats are found in each final
group of major Groups A and D. The average number
of quadrats in Final Groups 3 and 4 is 14,0.
Re-allocation was not required in this analysis
and the few quadrats which do not fit the description
of a particular group as a whole are discussed in the
group description.
Group 7 is the last group of the hierarchy and is
defined by the absence of all dividing species. Quadrats
of this group do not form a meaningful unit, being
scattered diffusely across the northern and southern
boundaries of the area. This group is neither named
nor discussed further as it is considered a collection of
quadrats which should have been included in other
groups but which, by chance, lacked the necessary
defining species. Re-allocation of these quadrats
was not considered worthwhile.
3.3.2 Species distribution within groups
When lists of species commonly occurring in each
final group were drawn up as part of the interpretation
of each group, it was found that large numbers of
species seemed common to many groups and that
there were few species that were restricted to only
one or two groups. To study these findings at greater
depth, a species-in-groups Table was drawn up.
Five Final Groups, namely 1, 3, 4, 5 and 6 and Group
B (consisting of Final Groups 2a, 2b, 2c and 2d)
were used for the six columns of the Table. The
presence percentage of every species in each group
284
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
was computed and rows of the Table were then formed
by the 84 species, each of which had a presence of
over 39 percent in at least one group. These presence
percentages are given in Tables 5 and 6 where species
with wide and restricted distributions, respectively,
are listed. Mean number of species per quadrat and
mean basal cover percent are also given in Table 5.
The mean number of species per quadrat decreased
steadily from almost 50 in Group 1 to 36,5 in Group
6. At the same time the standard deviation of the
mean increased, indicating that as the mean decreases,
the range within a group increases (Table 5). Total
basal cover and the cover of the tall and short grass
strata are highest in Group 1 and are fairly similar in
all the other groups.
All species with a presence greater than 19,9
percent in all groups, and in all groups but one, are
listed in Table 5. In particular, Aristida congesta and
Themeda triandra are common throughout the area
if a presence of 75 percent is taken as a criterion for
within-group abundance. The presence percentages
of most of the other species vary from one group to
another. Twenty four species have a presence greater
than 19,9 percent in all groups and 22 have a presence
of less than 20 percent in only one group.
The 38 species with a presence greater than 19,9
percent in four or fewer groups are listed in Table 6.
It is noteworthy that only three species, Eragrostis
gummiflua, Euphorbia sp. and Fingerhuthia africaua,
are restricted to only one group, and all three are
found in Group 6 quadrats. Eight species have a
presence exceeding 19,9 percent in only two groups.
Many species, including Diheteropogon amplectens,
Barleria pretoriensis and Eragrostis racemosa, have
a similar pattern of distribution, being found with
a high presence percentage in Groups 1 and B.
Another group of species, including Oropetium
capense, Sporobolus africanus and Hermannia tomen-
tosa, are found in Groups 4, 5 and 6 although they
are not all restricted entirely to these groups.
TABLE 5. — Mean number of species per quadrat, mean basal cover percentage and presence percentage for widely distributed species
within each group. X indicates a high cover-abundance rating for the species in most, if not all, quadrats of the groups and a
dash ( — ) a value of less than 20%
* Specimen housed in National Herbarium, Pretoria.
J. W. MORRIS
285
TABLE 6.— Presence percentage for species with restricted distributions within each group. X indicates a
for the species in most, if not all, quadrats of the group and a dash (— ) a value of less than 20%
high cover-abundance rating
* Specimen housed in National Herbarium, Pretoria.
3.3.3 Final Groups
(a) Group 1 ( Diheteropogon-Stipagrostis Primary
Bankenveld)
Two small patches of quadrats of Group 1 ( Dihete-
ropogon-Stipagrostis Primary Bankenveld) are found
north and north-east of Lichtenburg. Other quadrats
of this Group occur scattered singly through the
north-central and north-western parts of the study
area. This small group represents Bankenveld on
relatively deep, dolomite-derived soils that have
been rested in the recent past or have at least been
protected from mismanagement.
Nearly all quadrats are located on the crests of
small rises, typical of the area, or on waxing slopes
from rises. Two quadrats occur in small hollows.
Slope is usually so slight as to be unmeasurable.
Chert fragments and loose dolomite rocks are usually
found on the ground surface in these quadrats. Soil
depth varies from 5 to 10 cm. Soil pH is usually 6,5
and occasionally 7,0. Biotic factors were uniform
within the Group. Grazing intensity was light, or
moderate, and often the vegetation appeared to have
been rested for some time before sampling. Average
total basal cover was 14 percent (Table 5), 6,3 percent
being contributed by the tall grass stratum (60 to
90 cm tall with many 75 cm tall tufts) and 7,6 percent
by the short grass stratum (about 16 cm tall but
ranging from 5 to 35 cm tall). Quadrats of this group
are rich in species, containing the highest average
number of species of any Bankenveld group studied.
Species present in over 19,9 percent of the quadrats
of Group 1 are given in Tables 5 and 6.
(b) Group 2 ( Diheteropogon-Schizachyrium Banken
veld)
As a whole. Group 2 ( Diheteropogon-Schizachyrium
Bankenveld) appears homogeneous, being retained as
an entity from H.S. x2 = 30,0 to 13,1. At a level of
H.S. x2 = 8,5, however, the 33 quadrats of this
Group are divided into four groups. Group 2 will be
described as a whole and peculiarities of each Final
Group will be mentioned. Quadrats of this Group
form a belt from east to west across the study area.
Group 2b is concentrated in the eastern and central
parts of the belt. Group 2a is restricted to three qua-
drats in the south-western corner and quadrats of
Group 2c occur among those of Group 2b. Quadrats of
Group 2d are found at the western end of the belt and
along the south-central edge of the belt. In comparison
with some other groups, whose quadrats are scattered
through the study area, this is an easily delimited
Group.
Over two thirds of the quadrats of Group 2 occur
on crests of rises or on very gentle waxing south- and
north-facing slopes. The other third, which are found
scattered through all four Final Groups, are in very
shallow depressions, on waning slopes to drainage
lines, or in small sand-filled sink-holes. Soil is usually
5 to 8 cm deep with chert gravel littered on the soil
surface. A solid sheet of dolomite is not found in any
quadrat. Soil pH varies between 6,5 and 7,0 and no
soil HC1 reaction is recorded. With five exceptions all
quadrats were lightly grazed or rested and the vegeta-
tion was in good condition. Some of the samples were
from inside fenced maize lands on soil too shallow for
286
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
ploughing. Vegetation in these situations was usually
protected from grazing. The exceptional quadrats
were heavily grazed and trampled and dolomite was
often exposed in them. These quadrats are not exclu-
ded from the Group because some, if not all of
them, could have been heavily grazed for too few
years for their species composition to have altered
from this treatment. Average total basal cover in
Group 2 was 5,0 percent for the tall grass stratum
(usually 75 cm but ranging from 60 to 90 cm in height)
and 5,7 percent for the short grass stratum (usually in
the range 15 to 30 cm tall). The averages for Group 2b
were slightly greater than the overall averages and
those for groups 2a, 2c and 2d were equal to, or slight-
ly less than, the averages for Group 2 as a whole.
Species present in over 19,9 percent of the quadrats
of Group 2 are given in Tables 5 and 6.
On the grounds of the species common to the sub-
groups and the similar habitat and management
features of the quadrats of Group 2 it was decided not
to subdivide the Group for description even though it
is the largest Group of the analysis. Diheteropogon-
Schizachyrium Bankenveld is also the most widespread
Group in the analysis. It is considered to be the
‘normal’ or ‘typical’ Bankenveld of the study area. In
distribution, Diheteropogon-Stipcigrostis Primary Ban-
kenveld (Group 1) forms an extension of this Group
and represents a higher successional stage (less
disturbance) in the Bankenveld Land System.
Fig. 12. — Featureless Banken-
veld Land System scene
north of Lichtenburg in
Diheteropogon-Schizac/iyrium
Bankenveld showing selec-
tive grazing. Short grass is
mostly Themeda triandra and
larger tufts are of Dihetero-
pogon amplectens and Stipa-
grostis uniplumis. Trees are
mostly Acacia karroo. Hout-
haalbomen, Lichtenburg
District.
Fig. 13. — Sand-filled sinkhole
partly under cultivation in
Diheteropogon-Schizachyrium
Bankenveld. Trees on hori-
zon are exotics at home-
steads. Hendriksdal, Lichten-
burg District.
J. W. MORRIS
287
(c) Group 3 ( Chascanum-Eragrostis racemosa Sandy
Bankenveld) and Group 4 ( Chascanum-Anthephora
pubescens Sandy Bankenveld).
These two Groups are discussed together as they are
split at the low H.S. x1 level of 1 8 , 1 . The homogeneity
of each Group is indicated by neither’s being further
subdivided until H.S.x2 9,5. The combined Group,
3 and 4, is also homogeneous, being maintained as a
Group from H.S. x2=38,6 to H.S. x2=18, 1. Thus,
as a combined Group and as separate entities, Groups
3 and 4 are relatively homogeneous.
Quadrats belonging to both Groups occur along
the western boundary of the area, in a round patch in
the north-west, and the few other samples occur
scattered through the remainder of the sampled area.
Quadrats of both Groups occur together at each
locality. Group 4 is the larger of the two and the usual
pattern is for a quadrat of Group 3 to occur among a
cluster of Group 4 quadrats.
Groups 3 and 4 form a clear ecological nodum
associated with a thin, sandy overburden to dolomite.
In the majority of quadrats, soil is shallow (5-10 cm),
but is occasionally over one metre deep. In most
quadrats, the soil surface is free of rock, or contains
only scattered, small, chert fragments. It is possible
that aeolian sand of Kalahari origin has blown from
the west onto the edge of the area, forming a thin
veneer over dolomite. Such a movement of sand would
be in agreement with the views of Harmse (1967).
Within the study area, wind-blown sand has collected
in sink-holes and other depressions to form a similar
habitat. In Group 4, four quadrats are located in local
depressions while a number of quadrats from both
Groups occur on flat plains or crests of rises on which
sand could easily accumulate. A remarkable feature is,
however, that over half the quadrats in Group 3 and
over a third of the quadrats in both Groups occur on
slightly sloping ground where it would be expected that
erosion of sand would be greatest and accumulation
least. As the rainfall is relatively low and run-off in the
dolomite minimal, sand deposited on a slope is,
however, not transported easily. Soil pH is about 6,5
in both Groups. Moderate to moderate-heavy grazing
was found in most quadrats of both Groups. When
light grazing was recorded, another disturbance
factor, like proximity to diamond diggings, was usually
noted. Mean number of species per quadrat in Groups
3 and 4 were 46,6 and 41 ,0, respectively. The tall grass
stratum was 60 to 75 cm high in both Groups, with a
maximum of 90 cm in Group 3. The short grass
stratum was 10 to 30 cm high in Group 3 and 10 to
20 cm high in Group 4. Total basal cover of both
Groups was low (Table 5). Species present in over 19,9
percent of the quadrats of Groups 3 and 4 are given in
Tables 5 and 6. Many species are common to both
Groups and about eight species are found particularly
in one or other of the two Groups.
(d) Group 5 ( Corchorus-Ursinia Bankenveld of
Disturbed Sites)
The secondary nature of the vegetation in the
quadrats of this Group brought them together on the
hierarchy. Some of the quadrats are laid out near
diamond diggings, others on abandoned lands and the
rest on heavily trampled and overgrazed vegetation.
Quadrats of this small Group are scattered through
the study area.
Many physiographic combinations are represented.
Some quadrats are on crests of rises, some in hollows
and some in intermediate positions. North- and south-
facing aspects, as well as level sites, are found. Soils are
usually shallow, being, in general, from two to eight
cm deep and often being gravelly where occurring in
fossil river courses. Deeper soil is found occasionally,
the deepest for this Group being recorded as 0,5 m.
Mean number of species per quadrat was 40,0. Total
basal cover averaged 10,6 percent, only 2,8 percent of
which was accounted for by the tall grass stratum
(usually 60 cm tall but occasionally 90 cm tall). The
low total cover and large percentage thereof accounted
for by the short grass stratum (15 to 25 cm high) is a
further indication of the disturbed nature of the vege-
tation. Species present in over 19,9 percent of the
quadrats of Group 5 are given in Tables 5 and 6.
Group 5 represents areas of disturbed vegetation
within the study area. Thus, the areas next to aban-
doned diamond diggings belong to this Group, even
though few quadrats were located there. The influence
on the vegetation surrounding the diggings of over
100 000 people (Williams, 1930) who flocked to the
diamond fields from 1926 to 1929 must have been
great and it is unlikely that the vegetation has fully
recovered yet.
Fig. 14. — Graves of diamond
miners in typical Bankenveld
vegetation with abandoned
diamond diggings on ridge
in background. Grass in
flower is Themeda triandra.
Bakerville, Lichtenburg Dis-
trict.
288
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
(e) Group 6 (Fingerhuthia-Oropetium Bankenveld of
Dolomite Sheets)
With the exception of three quadrats, which occur
scattered through the study area, the quadrats of this
Group occur to the immediate north of Lichtenburg,
in the southern-most part of the Bankenveld Land
System.
Quadrats of this Group occur on extensive plains,
in slight hollows and on gentle slopes near crests of
plains. Quadrats are found on shallow soils where solid
dolomite sheets are exposed on the surface. Soil, if it is
present, is usually only 2 to 5 cm deep. Soil pH is
usually 7,0 to 7,5, in other words, slightly more alka-
line than in most other groups. In three quadrats a
slight soil HC1 reaction was recorded. Grazing in
seven quadrats was light and the vegetation appeared
undisturbed. In the other five quadrats of the Group,
grazing was moderately-heavy to heavy. Average total
basal cover was just under 10 percent, with approxi-
mately equal contributions from the tall (usually 75
cm, but ranging from 60 to 120 cm in height) and short
(either 10 to 15 cm or 30 to 45 cm tall) grass strata. The
mean number of species per quadrat was low (36,5)
but the standard deviation of the mean was high (SD =
7,4), indicating that while some quadrats were very
poor in species, others were rich. Species present in
over 19,9 percent of the quadrats of Group 6 are given
in Tables 5 and 6.
The Group is named after Oropetium capense, a
diminutive grass found in every quadrat of this Group.
Gaff (1971) reported that O. capense could withstand
virtually complete desiccation, a necessary prere-
quisite for survival on rock sheets with little soil as
found in quadrats of this Group.
Fig. 15. — Spoil heaps from aban-
doned diamond diggings in
Corchorus-Ursinia Banken-
veld of Disturbed Sites.
Bakerville, Lichtenburg Dis-
trict.
Fig. 16. — Dolomite outcrop in
Fingerhuthia-Oropetium
Bankenveld of Dolomite
sheets. Hendriksdal, Lich-
tenburg District.
J. W. MORRIS
289
4. DISCUSSION AND CONCLUSIONS
4 . 1 Sampling strategy
It is well documented that strictly systematic and
random sampling, although deemed statistically
justifiable and even preferable, are inefficient (Taylor,
1969; Werger, 1973). This is chiefly because such
strategies result in the inclusion of narrow ecotones in
collections of samples, which are then heterogeneous
(Grunow, 1965a; Lambert, 1972). It also leads to
undersampling generally-recognised but small vege-
tation units, such as vleis (marshes) and dolerite dyke
communities, and over-sampling of large units. Small
vegetation units might then not be identified by a sta-
tistical method, such as association analysis, which is
programmed to terminate at a certain minimum num-
ber of samples. Even a group of two or three samples
will, of course, be identified by association analysis if
its constituent quadrats are sufficiently similar to each
other and sufficiently different from other quadrats.
In a vegetation survey such as the present one, more
interest is vested in dominant vegetation communities
than in narrow ecotones and vegetation units of small
area, while areas of intermediate size should be ade-
quately sampled to enable identification and charac-
terisation by the statistical process used. The stratified
sampling strategy used for this study ensured that a
representative sample of the variation was obtained
(see also Werger, 1973), while the random element
ensured that the sampling was statistically acceptable.
Such a strategy is of particular importance where the
number of samples is strictly limited, as it was in this
study.
It is preferable to establish optimum sample size in
the study area instead of using a size derived elsewhere
(Lambert, 1972). In this study, it was considered that
compatibility between studies was of greater impor-
tance than the derivation of a unique size for this
project. Furthermore, results of pilot studies showed
that a slightly smaller sample (12 m2) would have been
adequate and 16 m2 was considered large enough to be
a ‘safe’ minimum size for the entire Highveld Ecolo-
gical Survey (J. C. Scheepers: pers. comm.).
Extensive cultivation in the CT Grassland Land
System made sampling difficult. Not only are clusters
of samples situated far apart, but great difficulty was
experienced in getting samples representative of all
vegetation types which were presumed to have existed
in the area previously. Some types have almost cer-
tainly disappeared completely. As it is vegetation on
soils that are less suitable for cultivation which
remains, a marked sampling bias towards vegetation
on these soils and away from that on soil suitable for
cultivation is likely to have taken place.
The number of samples in both Land Systems is
small. In CT Grassland there was the physical problem
of fitting samples into a restricted area of natural
vegetation while in Bankenveld it was considered that
the major vegetation types had been adequately
sampled by 110 samples. The limited period for
fieldwork during the present study also affected the
number of samples which could be taken.
There were two reasons for the small number of
habitat variables recorded at each site. Firstly, as the
study was conceived as a semi-detailed survey of short
duration, intensive study of ecological interrelation-
ships was not planned. Secondly, the number of
habitat factors which can be studied in Bankenveld is
limited by the nature of the soil. In many places, sheets
of dolomite are exposed at the surface and the plants
are rooted between rocks. Measurement of field
capacity, wilting point, and similar measures are
difficult as a result.
4 . 2 M ethodological aspects
The broad differences between Bankenveld and CT
Grassland Land Systems, outlined in section 1.7, are
shown to be supported by quantitative analysis of the
vegetation. The Total association analysis separated
most quadrats laid out in Bankenveld from those laid
out in CT Grassland. Nineteen Bankenveld quadrats
occurred in groups consisting mainly of CT Grassland
quadrats but Bankenveld groups never included CT
Grassland quadrats. It was therefore concluded that
certain Bankenveld vegetation quadrats resembled
vegetation of CT Grassland groups in their floristic
composition, but that no CT Grassland samples
resembled Bankenveld groups. Of Bankenveld qua-
drats classified with CT Grassland groups, 42 percent
were from Group 7 of the Bankenveld hierarchy and
37 percent were from Group 6 of the same classifi-
cation. Group 7, the last group of the Bankenveld
classification, was found to be a heterogeneous group
of quadrats. The species composition of many Group 7
quadrats could be such that, by chance, they did not
contain the dividing species necessary to include them
in a group in which they would have been appro-
priate. In the Total analysis also, these quadrats were
shown to be a heterogeneous collection by their being
scattered through a number of final groups.
Apart from strong, positive species associations
within quadrats of each Land System and negative
associations between them, floristic richness may be
partly responsible for the major automatic division
between Bankenveld and CT Grassland. A floristi-
cally-rich group of quadrats is defined as one with a
relatively high mean number of species within each
quadrat of the group and a floristically-poor group is
the converse. That floristic richness of quadrats may
influence the nature of the resulting hierarchy was
noticed on inspection of the mean numbers of species
per quadrat in each final group of both hierarchies.
In the Bankenveld classification, the mean decreases
steadily from Group 1 (49,5) and Group 2 (43,6) to
Groups 6 (36,5) and 7 (32,9), across the hierarchy
from left to right. Thus, floristically-rich groups split
off first and floristically-poor quadrats generally
remain until last. Although evidence is not available,
it is conceivable that more positive species associations
are present in floristically-rich collections of quadrats,
making the collections more homogeneous and there-
fore more likely to be split off. A similar decrease from
left to right in mean number of species per quadrat was
found in the Total analysis. The overall mean number
of species per quadrat is, however, much lower. The
overall average in the 110 Bankenveld quadrats
exceeds 40. In CT Grassland Groups 4b, 5b, 6 and 7a,
which contain most species per quadrat, the mean is
less than 27. The average decreases steadily to the
last Group, 9c, with a mean of 15,2. Thus, if floristic
richness is a factor controlling the results of the
classification, the marked division between Banken-
veld and CT Grassland Land Systems would be expec-
ted. It is also the possible explanation for floristically-
poor Bankenveld quadrats of Groups 6 and 7 occur-
ring with floristically-poor CT Grassland groups in the
Total analysis.
To obtain the greatest amount of information from
the association analyses they had to be interpreted
at more than one stopping level. A single stopping
rule, as initially proposed by Williams & Lambert
(1959, 1960), was not adequate. It is considered,
furthermore, that experience with use of the method
greatly improves the result that is obtained. Associa-
tion analysis should be considered as an aid in the
study of vegetation and not as a tool to be applied by
technicians with no training in its use and misuse.
290
AUTOMATIC CLASSIFICATION OF THE HIGHVELD GRASSLAND OF LICHTENBURG, S.W. TRANSVAAL
Although a few quadrats could not be successfully
re-allocated, the use of species recorded around the
edge of the quadrat to re-allocate quadrats was
successful. Had total tloristic composition also been
taken into account in the re-allocation procedure and
not only habitat features and species in the surrounds
of quadrats, an even more successful re-allocation
may have been realized.
Indicator values were of use for determining
significance levels for species occurring more common-
ly inside a group than outside it. Used in conjunction
with positive and negative dividing species and cover-
abundance estimates, Indicator values enabled good
floristic definitions of groups to be made. On the
other hand, negative Indicator values, given to species
occurring more frequently outside a group than
inside it, were of limited use (see Morris, 1973).
Although no objective criteria for measuring suc-
cess are known, it may be concluded that the tech-
nique of association analysis performed adequately
in providing a generally interpretable classification of
the vegetation. A perfect classification of a data set
of this size probably does not exist and the utility of
a particular strategy as an aid for the study of the
vegetation should be the criterion on which the
classification is judged.
4 . 3 Vegetational aspects
In the Total association analysis, division between
Bankenveld and CT Grassland quadrats is fairly
clear. As the Bankenveld area was considered most
important from a vegetational point of view and as
there was some mixture of Bankenveld quadrats in
groups of predominantly CT Grassland quadrats, a
separate analysis of the 110 Bankenveld Land System
quadrats was undertaken. It was not considered
profitable to interpret Bankenveld final groups in both
the Total analysis and the Bankenveld analysis. In
a general way, results of the Bankenveld analysis and
Bankenveld part of the Total analysis are similar.
In CT Grassland, eleven final groups are recognised
and described. Two final groups, Short and Tall
Stipagrostis uniplumis Calcareous Grassland, occur
on soils overlying surface limestone deposits with the
same geomorphology and soil series. Soils are gene-
rally slightly deeper and basal cover of tall grasses is
double in quadrats classified as Tall Grassland in
comparison with quadrats of Short Grassland. In
both Groups grazing is usually light. The community
is found around Lichtenburg and in a belt extending
west of the town.
Another two final groups, Elionurus argenteus
Secondary Grassland and E. argenteus Primary
Grassland, occur on rocks of the Ventersdorp system.
Heavy grazing and soil erosion are often recorded
from quadrats of the former while the vegetation is
usually in good condition in the latter Group. Most
Elionurus argenteus Grassland is found south-west of
Lichtenburg.
Two final groups also occur on Dwyka tillite sub-
strate. They are Cymbopogon plurinodis Grassland and
Secondary Cymbopogon plurinodis Grassland. The
difference between these two Groups is also in degree
of biotic influence but, as there are only three quadrats
in the latter Group, the distinction does not carry
much weight.
Three final groups, Acacia karroo Savanna, Acacia
karroo Open Woodland and Drainage Basin Acacia
karroo Open Woodland are found on the medium-
and poorly-drained soils of the area. Heavy grazing
and trampling are usual in quadrats of these Groups.
Most quadrats are situated on Ventersdorp Series
rocks. In all three Groups a woody element is present
with Acacia karroo as the dominant tree and shrub
species.
It is concluded from the description given that the
major vegetational differences in the CT Grassland
Land System can be related to the geological substrate
and gross soil characteristics. Within major groups,
management is often an important factor although,
in some cases, there are not enough quadrats in a
group for even a reasonable degree of certainty. Two
final groups, one of only three quadrats, from adjacent
legs of the hierarchy could not be interpreted.
In the Bankenveld association analysis ten final
groups are distinguished. For discussion, the four
final groups of Group 2 are lumped and Groups 3
and 4 are also lumped. Suggested relationships between
Bankenveld groups are indicated in Fig. 17.
It is considered that Group 2 ( Diheteropogon -
Schizachyrium Bankenveld) is the typical vegetation
of the Bankenveld Land System. Group 1 ( Diheteropo -
gon-Stipagrostis Primary Bankenveld) consists of
quadrats laid out in vegetation that had been well
managed. Group 1 is closely related to Group 2 but
has experienced less selective or heavy grazing and
trampling in the past. It may be considered as the
‘climax’ vegetation type, although it possibly occurs
in a slightly different habitat.
Quadrats of Groups 3 and 4 ( Chascanum-Eragrostis
racemosa Sandy Bankenveld and Chascanum-Anthe-
phora pubescens Sandy B mkenveld) occur together on
the western edge of the Bankenveld Land System and
in a circular patch in the north-west of the study area.
Differences between the two Groups are not clear.
Both are found where sand overlies dolomite. It
is suggested that aeolian sand has been blown from
the west over the dolomite and provided the habitat
for these Groups.
Past distil bance in the area was discussed earlier. It
is suggested that quadrats of Group 5 ( Corchorus -
Ursinia Bankenveld of Disturbed Sites) are those in
vegetation which has been disturbed in the past.
Exposed sheets of dolomite are characteristic of
parts of Bankenveld, particularly in the area to the
immediate north of Lichtenburg. Group 6 ( Finger -
huthia-Oropetium Bankenveld of Dolomite Sheets) is
the vegetation typical of such areas.
ACKNOWLEDGEM ENTS
Prof. J. O. Grunow of the Department of Plant
Production, University of Pretoria is thanked, as
co-promoter, for his interest in this project, for his
most helpful suggestions during the preparation of the
thesis on which this paper is based and also for
reading this manuscript. I thank Dr D. Edwards and
my colleagues, of the Botanical Survey Section of the
Botanical Research Institute, for support and encou-
ragement during the execution of this project. In
particular, I am grateful to Dr M. J. A. Werger for
fruitful discussions, leading to many improvements
in this account and to Dr J. C. Scheepers for his
co-operation in the planning of this part of the High-
veld Region Survey. For assistance in the field I thank
Messrs C. Boucher, D. Muller and G. J. Engelbrecht.
Mr B. J. Coetzee kindly assisted me with the con-
struction of Table 4. Mrs E. van Hoepen and her
staff at the National Herbarium named the plants
collected from the area. Dr E. Verster of the Soils
and Irrigation Research Institute kindly gave me the
most recent soil classification system applicable to
the area. The Extension Officer, Department of
Agricultural Technical Services, Lichtenburg, is
thanked for the facilities of his office, which were
put at my disposal during field work.
J. W. MORRIS
291
Fig. 17. — Suggested relationships
between Bankenveld associa-
tion analysis groups.
UITTREKSEL
'n Kwantitatiewe , semi-gedetaileerde plantekologiese-
studie is gedoen vir die gebied tussen 25°54' en 26°22'
0 en 26°00' en 26°20' S, gelee rondom Lichtenburg in
suidwes-Transvaal. Die gemiddelde jaarlik.se tempera-
tuur van hierdie studiegebied is 17 °C en die jaarlikse
reenval is omtrent 600 mm. 'n Basiese verskil kan
waargeneem word tussen die Bankenveld Land Sisteem
en die CT Grasveld Land Sisteem. Eersgenoemde bet
'n onderlaag van dolomiet met litosoliese grond,
Bankenveld plantegroei en veeboerdery as vernaamste
bodembenutting. In teenstelling daarmee bet laasge-
noemde ’« onderlaag van graniet, Ventersdorp lavas,
Dwyka kleileem (tillite) en oppervlakkalksteen met
Sborrocks, Mangano en Lichtenburg grondseries,
Cymbopogon-Themeda Veld plantegroei en eksten-
siewe mielieboerdery as hoof bodembenutting. Een
bonderd en tien 16 m2 kwadrate is geplaas in elke land
sisteem deur middel van gestratifiseerde ewekansige
monstering. Van die 247 spesies wat teegekom is, bet
amper 'n bonderd in minder as 6 kwadrate voorgekom.
Themeda triandra, Aristida congesta, Elionurus
argenteus, Anthospermum rigidum en J usticia ana-
galoides bet deurgaans baie algemeen voorgekom.
Twee assosiasie-analises is gedoen en 1 5 finale groepe is
geinterpreteer vanuit 'n totaal van 21 groepe.
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Bothalia 12,2: 293-300 (1977)
Cape Hangklip area. I. The application of association-analysis,
homogeneity functions and Braun-Blanquet techniques in the
description of south-western Cape vegetation
C. BOUCHER*
ABSTRACT
Releve data were collected in two phases from, respectively 150 and 100 sampling points distributed by
stratified random means through almost 24 000 ha of vegetation. Association-analysis, Braun-Blanquet and
homogeneity function methods were used to treat the data. Only the “normal” association-analysis method
was applied. Three sorting techniques for tabulating the data were tested and were compared with a fourth
method. Homogeneity functions were used to construct a dendrogram and to determine the degree of similarity
between individual releves and groups of releves. After compaiison of the methods, it was concluded that the
Braun-Blanquet method is consistently more efficient and more exact, even in the floristically rich vegetation
of the south-western Cape Province of South Africa.
RESUME
REGION DU CAP HANGKLIP. I. L' APPLICATION DE U ANALYSE D' ASSOCIATION ,
DES FONCTIONS D'HOMOGENEITE ET DES TECHNIQUES DE BRA UN-BLANQUET A LA
DESCRIPTION DE LA VEGETATION DU SUD-OUEST DE LA PROVINCE DU CAP
Les donnees des releves out ete rassemblees en deux phases a partir de 150, puis de 100 points de
recolte distribues par stratification aleatoire sur pres de 24 000 ha de vegetation. Le traitement de ces
donnees a ete effectue suivant les methodes d'analyse d'association, de Braun-Blanquet et de fonctions
d'homogeneite. Seule la methode d'analyse d'association “ normale ” a ete employee. Trois techniques
de triage pour la confection de tables de donnees ont ete testees et comparees a une quatrieme methode.
Les fonctions d'homogeneite ont ete employees pour construire un dendrogramme et determiner le
degre de similitude entre les releves individuels et les groupes de releves. Apres comparaison des
methodes, on a conclu que la methode de Braun-Blanquet est plus efficiente et plus exacte, et ceci d'une
facon consistante, me me dans la vegetation floristiquement riche du sud-ouest de la Province du Cap en
Afrique du Sud.
INTRODUCTION
Little descriptive work has been done on the vege-
tation of the south-western Cape Province of South
Africa. Acocks (1953) has remarked that the Cape
Fynbos vegetation “is a complex vegetation, and to
divide it simply into Macchia and False Macchia is
like dividing the tropical vegetation into grassveld
and bushveld . . .
Statistical approaches have been used by Rycroft
(1951), Grobler (1964), Taylor (1969) and Hall (1970)
as aids in the description of this vegetation. The
largest area of vegetation described and mapped in
detail is the 7 680 ha of the Cape of Good Hope
Nature Reserve (Taylor, 1969). This latter study was
the first attempt at applying association-analysis
(Williams & Lambert, 1959, 1960, 1961; Lambert and
Williams, 1962) and Zurich-Montpellier methods
(Braun-Blanquet, 1932; Becking, 1957; Kuchler, 1967)
to the Fynbos element (Taylor, 1972) of the South
Western Cape vegetation. The Zurich-Montpellier
principles, expressed by Braun-Blanquet and further
developed theoretically by many followers (Werger,
1973b), will here be termed the Braun-Blanquet
method. The Braun-Blanquet method has subsequent-
ly been used to describe some 373 ha of Fynbos
vegetation in the Jonkershoek State Forest near
Stellenbosch (Werger, Kruger & Taylor, 1972).
A method was required in the south-western Cape
that would be most suitable for the evaluation,
description and classification of large tracts of Fynbos
vegetation. The Cape Hangklip area was floristically
rich and included many variations of habitat. It would,
therefore, be an exacting test of the suitability of any
method. This served as the stimulus to apply homo-
* Botanical Research Unit, P.O. Box 471, Stellenbosch.
geneity functions (Hall, 1967a & b, 1969a, b & c and
1970), association-analysis and Braun-Blanquet tech-
niques.
The study area consists of about 24 000 ha of coast
and mountain vegetation. The boundaries were taken
as those of the 1:50 000 Topographical Survey Sheet
341 8BD Hangklip (Trigonometrical Survey, 1968) and
the portions of the Kogelberg State Forest which
occur outside this sheet.
METHODS
The sampling method
Releve data were obtained from 150 and 100 sites
scattered respectively over 1 1 506 and 12 354 ha. Sites
were distributed randomly within physiographic-
physiognomic units delimited on aerial photographs.
In the first phase of 150 releves, each of the 10 x 5 m
releves were strictly laid out with the longest axis on
a north-south magnetic bearing. In the second phase
each of the 100 releves was so positioned that a maxi-
mally homogenous sample was recorded.
For comparative purposes, only permanently
recognizable species were listed, others being listed
merely for record purposes. An additional list ot
species, occurring in the surrounds of the releve
within the community being sampled, was also made.
Listed species were given cover-abundance and
sociability values (Becking, 1957). A modified scale of
abundance, similar to that described by Hanson
(Brown, 1954), was used to assist in describing each
community.
As required by association-analysis and homoge-
neity functions, a standard releve size of 10x5 m was
used throughout. This size is identical to that used by
Taylor (1969) for conformity in the event of compari-
sons being made. Comparisons of sample size versus
294
CAPE HANGKLIP AREA. I. THE APPLICATION OF ASSOCIATION-ANALYSIS, HOMOGENEITY
FUNCTIONS AND BRAUN-BLANQUET TECHNIQUES IN THE DESCRIPTION OF
SOUTH-WESTERN CAPE VEGETATION
information recorded are made in Table 1. The data
used in these comparisons were obtained from visibly
different communities.
TABLE 1. — Average species-area curve comparisons (from
Boucher, 1972)
The following additional information was recorded
at each sampling site: soil type, soil moisture, degree
and type of stoniness, local climatic data, geology,
geomorphology, species dominance, species height,
vegetation age, disturbances, etc.
The association-analysis method
The various forms of association-analysis, namely,
“normal”, “inverse” and “nodal” analyses, have been
fully described by the developers of the method and by
numerous other workers. South African workers who
have applied this method include Van der Walt (1962),
Grunow (1965), Downing (1966), Roberts (1966),
Woods & Moll (1967), Miller & Booysen (1968),
Scheepers (1969) and Taylor (1969).
Scheepers (1969) found that the inverse analysis
produced a stepwise arrangement of species grouping
(also known as “chaining”) which was difficult to
interpret. Morris (pers. comm.) considered this step-
wise arrangement to be a fairly regular feature of the
method when large numbers of species were involved,
as in this case. It was considered advisable to restrict
treatment of the data to the normal type of analysis.
Information gained from inverse and nodal analyses
would, in most instances, not warrant the extra
expenditure in computer time. A programme for the
nodal analysis was not locally available at the time_
The subdivision parameter used was the highest
y2
— value which Williams and Lambert (1959,
N
1960) considered to result in the most efficient sub-
division, although the optional facilities of Z x2 or
x ^
Z-i-r were available. Termination of subdivision
N
took place when there were less than eight releves left
in the group or when the highest single x2 equalled
3,841 or less.
The Braun- Blanquet method
The Braun-Blanquet method, commonly used in
Europe and elsewhere, has been little used in South
Africa. The only English source of information on
this method was Fuller and Conard’s (Braun-Blanquet,
1932) authorized translation of Braun-Blanquet’s
first edition of Pflanzensoziologie (Braun-Blanquet,
1928). More recent English descriptions of the method
were published by Poore (1955), Becking (1957) and
Kiichler (1967), amongst others.
Taylor (1969) was the first to use the method in
South Africa. He prepared a synthesis table from data
collected in systematically distributed releves and
obtained associations which were recognizable in the
field. Werger, Kruger & Taylor (1972) then applied
the phytosociological technique as further described
by Ellenberg (1956) and Braun-Blanquet (1964), to
test its usefulness in the floristically rich Fynbos
vegetation in a portion of the Jonkershoek State
Forest. A practical classification into communities
based on floristic criteria was obtained. This method
has subsequently been used by, amongst others,
Coetzee (1972) in the Jack Scott Nature Reserve, by
Werger (1973a & b) in the Upper Orange River Valley,
and by Musil, Grunow & Bornman (1973) on aquatic
vegetation in the Pongola Pans, Zululand.
Aids have recently been developed to assist in
sorting tabulated data. Muller et al. (1972) designed a
mechanical sorting apparatus for ordering data by
shifting aluminium strips on which the information
is symbolized by coloured rivets. A computer program-
me, TABSORT, developed by the Department of
Forestry at Jonkershoek near Stellenbosch, allows the
data matrix to be manipulated simply by listing the
releve and species sequences in the required new order.
Ceska and Roemer (1971) have developed a computer
programme that identifies species-releve groups in
vegetation, thereby removing the much disputed
personal bias from table-work.
Method using homogeneity functions
Homogeneity functions for identifying groups in a
matrix of vegetation d ta have been developed by
Hall (1967a & b, 1969a, b & c and 1970). A function,
given as Hqm, is written, for the subset of t=l ... k
sample plots and all the j= 1 . . . p species, as follows:
k
where sajk and shjk are the standard deviations of the
subset’s actual data row for the yth species, and a
dummy maximally heterogeneous row, respectively;
aj, is the value for the y'th species in sample plot t.
These methods have only been tested on small vegeta-
tion data matrices from the Bains Kloof area of the
Cape Province. A simplified form of this homogeneity
function determines the similarity between the average
members of each major group, subgroup, sibling-
group (Hall, 1969a) or core and each releve, thereby
indicating the “goodness of fit” of each releve in each
vegetation group delimited.
The similarity between two items or average mem-
bers t and k can be given by this simplified version of
the homogeneity function. By similar notation,
Hm= *Mj(}-\a'jra'jk\)
Here, the modulating factor Mj is calculated exactly
as before. The homogeneity expression that follows,
uses abundance values scaled to a range with a maxi-
mum of one, a'jt and a y*. The scaling of the yth
species is based on its largest operational value
(Hall, 1970).
RESULTS AND DISCUSSION
Association-analysis
For practical reasons collection and treatment of
the data were divided into two separate phases.
Fig. 1. — First-phase association-analysis hierarchy from Boucher (1972).
294
inforrr
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80m2..
70m2..
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50m2..
40m2..
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ASSOCIATION -ANALYSIS HIERACHY
295
Fig. 2. — Second-phase association-analysis hierarchy.
HOMOGENEITY - FUNCTION DENDROGRAM
Fig. 3. — Homogeneity-function dendrogram from Boucher (1972).
C. BOUCHER
297
In the first phase, 150 releves were ordered into 32
final groups in the association-analysis hierarchy
(Fig. 1). The hierarchy was constructed following the
the conventional procedure of listing positively
defined releves, at each subdivision, on the left-hand
limbs and the negatively defined releves on the right-
hand limbs. To present the information in a more
practical fashion, a logarithmic, instead of a linear
scale, was used for values of highest single x2. The
linear representations are inset in Figs 1 and 2.
The hierarchy showed relatively uniform divisions
with little tendency to chaining, except in the final
negatively associated portion, where the more distinc-
tive communities such as the coastal dune vegetation
and wet seepage communities, occurred. A reversal,
or increase, in level of subdivision of a subsequent
group, following the removal of a more homogeneous
group, occurred after group 12 had been delimited.
In certain instances, such as in the subdivision of
groups six and seven, two species could equally well
have been used to effect the subdivision, both resulting
in the smallest total of residual significant associations
in the two resulting subclasses. When such an ambi-
guity occurred, the computer was instructed to sub-
divide on the species with the lowest coding number.
In most cases communities proved to be under-
sampled rather than oversampled. In very few
instances would the recombination of adjacent final
groups have resulted in ecologically valid larger
groups.
A major difficulty, probably more commonly found
in monothetic divisive techniques was the occurrence
of apparent misclassifications. These were found
especially during the first major subdivisions when
large numbers of releves were involved. Here the
chance absence of a species within a particular releve,
although it occurred within the community being
sampled, could result in the misclassification of the
releve. This contingency was largely overcome by
listing species not found inside the releve but occurring
in its immediate vicinity, within the same community.
The reclassification of any releve could be undertaken
on these grounds. In a number of instances the cause
was found to be the misidentification of the dividing
species. This was attributed to the drought conditions
prevailing at the time and to the problem of identifying
vegetative specimens. The collection of 114 species of
Ericaceae, characterized by ericoid leaves, underlines
the reality of this problem. More than 1 400 different
species were collected during this survey.
Eleven releves were regrouped after the relevant
dividing species were found in the surround lists,
while five were found to be wrongly grouped because
of misidentifications. Two were transitional. The final
groups in the hierarchy were found to vary in the
degree of their floristic and ecological homogeneity.
Insufficient sampling could be a possible reason.
The description and mapping of the vegetation of a
portion of the study area was based on these final
groups because they showed highest correlation of
communities with habitat. A hierarchical arrangement
has the advantage of providing a dichotomous key for
the identification of communities.
In the second phase of the study, 97 of the 100
releves were divided into 25 final groups (Fig. 2).
(Data from 3 additional releves were collected at a
later stage to strengthen some of the Braun-Blanquet
groups.) In contrast to the previous and most other
normal analysis hierarchies, a total chaining of groups
occurred. There was virtually no correlation of groups
with habitat factors, but groups 1, 2 and 4 showed
some correlation with Braun-Blanquet groups. The
remaining groups did not appear to be correlated
floristically or with habitat factors and were, therefore,
not used in the description of the vegetation.
Braun-Blanquet
The conventional technique of manually rewriting
the table while sorting the data was used initially. (No
other facilities were then available.) A few major
groups were distinguished which were further com-
pared using homogeneity functions. Further refining of
the data was attempted once the TABSORT program-
me became available. A few more communities were
extracted and the complex interrelationships between
the communities were better shown (Boucher, Part II,
in preparation).
The Ceskar & Roemer programme for identifying
species-releve groups was tested on the same data. The
criteria applied for grouping were 50% and 66%
species occurrence within a group, each species having
a maximum of either 10% or 20% occurrence outside
that group. The groups delimited conformed to the
major groups that were readily identifiable using con-
ventional sorting methods. Considerable further refine-
ment of the table using another method would there-
fore appear to be necessary after using this programme.
This suggests that it could be a useful tool only for the
initial sorting of the data.
In the second phase, where the collection of releve
data conformed more to the principles laid down by
Braun-Blanquet, the data could be refined to a fairly
detailed level with the aid of the TABSORT program-
me (Boucher, Part II, in preparation). The subjective
location of sampling sites resulted in their most effi-
cient distribution within the many variations occurring
in the vegetation. An understanding of the vegetation,
gained during the first phase, resulted in fewer
transitional areas being sampled. The Braun-Blanquet
groups obtained in the second phase were therefore
clearer than those obtained in the first phase.
The TABSORT programme was used to study the
meaning of the association-analysis groups in terms of
the Braun-Blanquet community concept. The species
rows were rearranged to determine whether any
pattern of distribution would support the association-
analysis groups. Releves were also rearranged within
each of these groups but not between the groups. On
the basis of Braun-Blanquet differential species, some
of the association-analysis groups were heterogeneous.
This is possible when the grouping is based on total
species complement in each releve. A relationship of a
different type, such as fire-age, might be indicated.
This detracts from the acceptance of the association-
analysis, in comparison to the Braun-Blanquet, groups
for community classification.
Homogeneity functions
The initial subdivision of the data before applying
homogeneity functions was done using the Braun-
Blanquet method. The easily extractable, obvious
groups were accepted prior to being further analysed
using homogeneity functions. The residual data
matrix consisted of 108 releves having 185 perma-
nently recognizable species occurring in more than
two releves. This matrix was still too large for analysis
by this method with the available computer facilities.
It was, therefore, further reduced by excluding the
species of less frequent occurrence until 86 species
remained.
A chaining effect was obtained in the homogeneity
function dendrogram (Fig. 3) with virtually no
distinct clustering. A broad moisture gradient could
be discerned in the arrangement with drier sites
linking onto the matrix at the higher homogeneity
298
CAPE HANGKLIP AREA. I. THE APPLICATION OF ASSOCIATION-ANALYSIS, HOMOGENEITY
FUNCTIONS AND BRAUN-BLANQUET TECHNIQUES IN THE DESCRIPTION OF
SOUTH-WESTERN CAPE VEGETATION
levels and wetter sites linking at the lower homogeneity
levels. This was similar to the association-analysis
grouping where the wet seepage communities linked
at the lower highest single x2 values.
The data matrix for comparison using the homo-
geneity functions consisted of the less distinct com-
munities. The absence of the species of rarer occur-
rence probably reduced the sensitivity of the method
to an excessive degree. The end product was, therefore,
unsuitable for the description or the mapping of the
vegetation.
The distinctness of the recognized groups, and of
the members in each group, to their average member
was determined using the simplified form of the homo-
geneity function. With this method a member, when
compared to itself, would be 100% similar. All the
groups recognized were compared to each other,
whether they were those delimited by the Braun-
Blanquet method or were indistinct groups or arbitrary
cores extracted from the homogeneity function dendro-
gram. The distinctness of the Braun-Blanquet groups
was confirmed {vide the example in Fig. 4, where the
length of the bar indicates the degree of similarity).
The degree of similarity between the releves in the
complex data matrix was also readily shown diagram-
matically by the length of the bars.
Affinities between groups and the best location of
transitionary releves are easily shown by this method.
CONCLUSIONS
The releve size (10 mx 5 m) was found to result in
an adequate sample of each community, at the scale
of study involved. The releve shape could possibly
have been more flexible, for instance in sampling the
riparian communities which form narrow bands along
streams. The less rigid sampling arrangement of the
second phase, where the releve was not placed in a
fixed direction, but in a position to ensure maximum
homogeneity, resulted in fewer transitions being
sampled and thereby proved to be more satisfactory.
Although the mechanical table sorter was not used
to re-arrange the data during this study, experience in
its use indicates that it has certain advantages and
disadvantages over the TABSORT programme. It is
quicker to compare releves with one other and with
developing groups with the mechanical table sorter,
because direct comparisons are possible. This is most
easily simulated with the TABSORT programme by
strip-cutting the data, although this can be tedious and
liable to error. Copies of new arrangements must
frequently be made. The TABSORT programme has
the advantage of providing an immediate neatly typed
copy of the table of any required stage. This could be
useful for comparison between stages of refinement,
particularly for teaching purposes. The mechanical
table sorting method is more liable to human trans-
cript errors. The size of the data matrix (150x363)
was not limited by the computer capacity during this
study but rather by the number of releves and species
which could be efficiently dealt with in the actual
arranging. The mechanical sorter data matrix size is
limited by practical design and ease of handling
(124x 130 in the prototype).
Taylor found that association-analysis revealed
groups which were ecologically meaningful, but that
most of the groups represented ...” such small
isolated fragments of natural units that they do not
give a harmonious picture of the vegetation” (Taylor,
1969). In the first phase of the Hangklip survey, the
ecologically meaningful groups required little sub-
jective ordering to form a more harmonious picture of
natural units. The groups in the second phase were
found, in contrast, to represent isolated fragments
which would require considerable subjective rear-
rangement. This was in agreement with Taylor’s
findings. The latter result was unexpected, because
care had been taken to ensure the most efficient
sampling.
The Braun-Blanquet method was found to be more
consistent, primarily because the communities are
better defined in that they do not depend on single
species presence or absence for final group forming.
In addition the relationship between the communities
is readily demonstrated. Donselaar who used the
Braun-Blanquet method in the savannas of Northern
Surinam is mentioned by Werger et al. (1972) as stating
that the number of species must be moderate for this
method to be successful. The latter workers, in con-
trast, found the method to be practical in floristically
rich fynbos vegetation. During the present study more
than 1 400 different species were collected. In the first
phase releves containing 365 species (species occurring
in fewer than three or less releves were not included in
the analysis) were satisfactorily ordered in a table.
This method, therefore, proved satisfactory with a
fairly large data matrix. The data matrix, in contrast,
proved too large for analysis using homogeneity func-
tions. Initial Braun-Blanquet groups had to be defined
prior to further analysis. The homogeneity function
tests on these groups showed them to be reasonable.
Little further subdivision of these groups using homo-
geneity functions was effected although the degree of
similarity between individual members and groups was
readily demonstrated.
The Ceska & Roemer programme for identifying
species-releve groups only resulted in the delimitation
of the major groups which were readily delimitable
using less sophisticated and cheaper facilities.
ACKNOWLEDGEMENTS
The research undertaken during the first phase was
submitted to the University of Cape Town for a M.Sc.
degree under Dr A. V. Hall.
The Secretary of the Department of Forestry gave
permission for data to be collected in a State Forest.
Considerable assistance was received from staff
members of the Botanical Research Institute, the
University of Stellenbosch, the Department of Forestry
at Jonkershoek and the University of Cape Town.
UITTREKSEL
Monsterperseeldata is versamel in twee fases van
1 50 en 100 elk, versprei deur byna 24 000 ha plantegroei.
Assosiasie-analise, Braun-Blanquet en homogenitiets-
funksie metodes is op die data getoets. Slegs die
“ normale ” assosiasie-analise metode is toegepas. Drie
metodes van datasortering vir tabulering is getoets en is
vergelyk met ’n vierde metode. Homogeniteitsfunksies is
gebruik om ’n dendrogram op te trek en om die graad van
ooreenkoms tussen die individuele monsterpersele en
groepe daarvan te bepaal. Die verskillende metodes
word vergelyk. Die Braun-Blanquet metode is gereeld
meer doeltreffend en presies as die ander metodes
getoets in die floristies ryk plantegroei van die Suidwes
Kaap Provinsie van Suid-Afrika.
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«
c »-
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50
Relev6
no.
GROUP SIMILARITY ANALYSIS
l i i I I
k£) ro guA ^ UA CM ,H CM CO '"'A C- M3 ^ 'tO'OOr-OH'^'X) H H Ox O CO rH
rH^CM^O'^-^'^ICM inrOrorOfnHHHHM-M-COinaiOOOOH
UA .H
CM ro
100-
©
o>
w Z.
- 50
<D W
O —
« E
d> ..
Q. </)
I i i i i i i i i
I i
Relevg
no.
o CO C~- MO ^ M3 CM O 03 CM C — CO CM CM iH H O CM UA O CA CO M3 O CA CM
cn CM CM CM C\1 Or- IMOOO H M" MXl M3 M3 CA CT< CO 0O h- O H O CM
100
©
o> >
2 Z 50
s -
o —
• .!
o. «
Relev6
no.
I t 1 i I I
i I
! ( I • I . I
vfl ^ tr, H ^ A- M3 rOrOCM CO IA O 00 MO rnCAOOOOMSUACOCO'tf- C^tA
H^O^CTiH'MDinCMH^HOtOCnCMCM^^CnO LA M- MDsO MO 03 A- C" rH
rH «H rl rl I-H iHi—trli— I >H H
100
4)
o> >.
*0 —
c ” 50
© «
o —
5 .!
CL <0
Relev6
no
i i
J _i •a-O M in O 00 O cn lA fA O CT\ c'l H CM O 03 A- rH
rH fH i-H H iH H r-i i— i t—i i—l r-l |H ^
100
= 50
© _
o —
- E
M o
Relev6
no
rH H i— I H i-H rH M rH rH rH
oo
Note: The group similarity determinations were undertaken on
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Fig. 4. — Group similarity analysis from Boucher (1972).
300
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Bothalia 12, 2: 301-307 (1977)
A preliminary account of aerial plant biomass in fynbos communities
of the Mediterranean-type climate zone of the Cape Province
F. J. KRUGER*
ABSTRACT
Aerial plant biomass has been sampled by harvesting on several sites in fynbos communities of the south-
western Cape Province.
Biomass in stands of about two years old ranged from about 2 200 kg per ha to about 7 500 kg per ha.
Mature stands comprised about 1 1 000 to 1 5 000 kg per ha in heaths and 1 5 000 to 26 000 kg per ha in sclerophyl-
lous scrub. The data indicate a maximum annual growth rate of 1 000 to 4 000 kg per ha early in the develop-
ment of a stand, but growth rates appear to decline rapidly as communities age.
Young stands are dominated by hemicryptophytes, which comprise about 2 000 to 6 000 kg per ha, or
about 60 to 75 per cent of the biomass in stands of about four years old. Shrubs become prominent later, but
the hemicryptophytes persist.
The data indicate that the biomass, growth rates and the shape of the growth curves of fynbos communities
are on the whole similar to those of analogous vegetation in other zones of mediterranean type climate. However,
there are important structural differences in that analogues of the northern hemisphere (garrigue, chaparral)
do not have a significant component of persistent hemicrytophytes. Although Australian heath communities
do have this feature, the hemicryptophytes are not as prominent as in fynbos.
RESUME
RAPPORT PRELIMIN AIRE SUR LA BIOMASSE DE LA VEGETATION AERIENNE DANS
LES MAQUIS ( FYNBOS ) DE LA ZONE CLIMATIQUE DE TYPE MEDITERRANEEN EN
PROVINCE DU CAP
On a obtenu un echantillonnage de la biomasse de la vegetation aerienne en en recolt ant a divers
endroits du maquis ( fynbos ) du sud-ouest de la Province du Cap.
Dans des stations vieilles d' environ 2 ans la biomasse a varie de 2 200 a 7 500 kg par ha ( approxi -
mativement). A maturite, ces chiffres se montent a 1 1 000-1 5 000 kg par ha dans les bruyeres et 1 5 000-
26 000 kg par ha dans les brousses sclerophylles. Les donnees indiquent un taux de croissance annuel
maximal de 1 000 a 4 000 kg par ha au debut du developpement d'une station, mais les taux de
croissance semblent diminuer rapidement quand les communautes vieillissent.
Les jeunes stations sont dominees par des semi-cryptophytes qui comprennent environ 2 000 a 6 000
kg par ha, ou de 60 a 75 pour 100 de la biomasse dans des stations agees d'environ quatre ans. Plus
tard les arbrisseaux predominent mais les semi-cryptophytes persistent.
Les donnees indiquent que la biomasse, les taux de croissance et la forme de la courbe de
croissance de ces maquis sont au total semblables a celles des associations vegetales analogues dans
d'autres zones du type climatique mediterraneen. Neanmoins, il y a d'importantes differences struc-
turelles en ceci que les analogues de T hemisphere Nord ( garrigue , chaparral ) n'ont pas une constituante
significative de semi-cryptophytes persistants. Bien que les associations de bruyeres australiennes
possedent cette caracteristique, les semi-cryptophytes n'y sont pas aussi importants que dans le fynbos.
INTRODUCTION
The ecology of natural communities of Mediter-
ranean-type ecosystems has recently received con-
siderable attention, particularly from the point of
view of ecosystem convergence, and much more
information on plant communities has become avail-
able (Specht, Rayson & Jackman, 1958, and previous
papers; Specht, 1969a, 1969b; Jones et al., 1969;
Mooney et al., 1970; di Castri & Mooney, 1973).
However, few data on the Cape fynbosf have reached
the press.
In this paper data have been collated on the biomass
of fynbos communities, which have become available
during the course of ecological studies from 1967 to
1974. The studies were not aimed at measuring com-
munity production nor are the data such that they
may be used as direct measures of productivity.
Nevertheless, they represent an index of productivity
and contain other useful information.
STUDY AREAS
Biomass surveys were conducted on various sites
in three research areas, each described below.
1. Jonkershoek Forest Research Station (sites 1 . 1-1 .4).
The research area at Jonkershoek is situated at about
33°57'S and 18°55'E. The ecosystem has been
* Jonkershoek Forest Research Station, Stellenbosch.
f Also known as sclerophyll bush (Adamson, 1938), and
including the types described by Acocks (1953) as Macchia,
False Macchia and Coastal Macchia.
described by Wicht et al. (1969). The communities
sampled are situated on the slopes and near the bottom
of a steep-walled valley (Fig. 1) and occur on soils
derived from Cape granites. Soils are about one metre
deep with a brown structureless loam A-horizon on
a yellow-brown apedal B. They are acid, with pH
ranging from about 4,50 to 5,00. Extractable phos-
phorus (citric acid extract) amounts to about 12 to
40 p.p.m. and total nitrogen and organic carbon con-
tent amount to 0, 1 to 0,2 per cent and three to eight
per cent respectively, in the A-horizon (Joubert,
1965).
2. Zachariashoek Research Catchment (sites 2. 1-2.3).
This catchment research area is situated at 34°49'S
and 19°02'E and has been described by van der Zel
(1974). The communities studied are situated in the
Kasteelkloof subcatchment (Fig. 2). Soils are derived
from sedimentary orthoquartzites and shales of the
paleozoic Table Mountain Group. The soils here
have not been studied, but would resemble those at
Jakkalsrivier rather than those at Jonkershoek. Site
2.2 is phreatic and the soil has an organic A-horizon.
Few climatic data are available. Rainfall at the top
of the catchment amounts to about 1 300 mm per
annum, and at the bottom, 1 100 mm per annum
(six-year records at 701 m and 274 m a.s.l., respect-
ively).
3 Jakkalsrivier Research Catchment (sites 3.1-3.10).
Plathe & van der Zel (1969) and Kruger (1974) have
described the Jakkalsrivier area in some detail (Fig.
302
A PRELIMINARY ACCOUNT OF AERIAL PLANT BIOMASS IN FYNBOS COMMUNITIES OF THE
MEDITERRANEAN-TYPE CLIMATE ZONE OF THE CAPE PROVINCE
Fig. 1. — View of sclerophyllous
scrub community at site 1 . 2,
Jonkershoek, shortly after
sampling. Prominent shrubs
are Rhus tomentosa and Ati-
thospermum aethiopicum.
Asteraceae dominate the
lower shrub stratum.
Fig. 2. — View of open sclero-
phyllous scrub community
at Zachariashoek (site 2.1)
at age five years. Here, the
sclerophyllous shrubs have
not yet emerged and the
community is dominated by
Restionaceae : Chondrope-
talum paniculatum, Hypodis-
cus argenteus and Cannomois
virgata are prominent.
Fig. 3. — View of microphyllous
evergreen dwarf scrub (low
heath) community at Jak-
kalsrivier (site 3.7), at age
14 years. The shrub stratum
is dominated by Erica hispi-
dula.
F. J. KRUGER
303
3). It is centred at 34°09'S and 19°09'E. Soils are
derived from the orthoquartzites and shales of Table
Mountain Group. In most cases, these are coarse
rocky sands with a humic A-horizon, dystrophic,
with pH ranging from 3,5 to 5,0, total exchangeable
cations from 0,2 to 7,9 me/ 100 gm, and cation
exchange capacity from 0,5 to 44,0 me/ ICO gm. Base
saturation is very low. Phosphorus is present at about
one to four parts per million (Bray No. 2 extract).
Total nitrogen ranges from 0,01 to 0, 1 per cent, and
organic carbon from about two to four per cent, in
the A horizon.
The principal climatic features of Jonkershoek and
Jakkalsrivier are illustrated by means of Walter dia-
grams (Walter, 1963) in Fig. 4. The mean total radia-
tion for the region is 450 to 500 cal per square centi-
metre per day. Table 1 summarizes the principal
physical features of the sample sites, and includes
names of plant communities. Fosberg’s (1967) struc-
tural-functional classification was used and refers to
the mature community. Community names based on
Fig. 4. — Walter diagrams for Jonkershoek
character species are given where possible and are
those assigned in prior studies (Kruger, 1972; 1914).
Figs. 1, 2 and 3 illustrate typical communities.
METHODS
Communites which appeared structurally homo-
geneous were selected for sampling. Stratified random
sampling was used wherever conditions permitted,
and in these cases a ranked-set sampling procedure
(Halls & Dell 1966) was followed. Most samples
were collected in late summer or early autumn, when
the communities are nearly dormant. Successive
harvests were completed on sites 2.1, 2.2, 2 3 3 1
3.2, 3.3, 3.4, 3.5 and 3.6.
Biomass was determined by clipping aerial plant
parts from one-metre-square quadrats in all cases
except site 1.1, where 0,5 m2 plots were used, and
the six-year stand at 2.2, where 2, 5x2, 5 m plots
were used. In most cases an apparatus described by
Hetherington (1967) was used to define the cylinder
within which material was collected. Plants were
House Station) and Jakkalsrivier (Main Station).
TABLE 1. — Communities and physical factors for each sample site
304
A PRELIMINARY ACCOUNT OF AERIAL PLANT BIOMASS IN FYNBOS COMMUNITIES OF THE
MEDITERRANEAN-TYPE CLIMATE ZONE OF THE CAPE PROVINCE
TABLE 2. — Aerial plant biomass statistics for each site
* Includes sub-shrubs.
t Could not be calculated — non-random samples,
tt Dash = could not be collected; = 0 = trace collected.
clipped as close to the soil surface as possible, using
secateurs. If litter was present in significant quantities,
it was collected by raking the soil surface with the
fingers. Dead plants were included as litter. Clipped
material was segregated into growth-form categories
during the clipping routine. The plant material was
stored in 2 mm-mesh plastic-coated fibre-glass gauze
bags and hung in a well-ventilated place until it
could be treated in the laboratory.
The categories used for the segregation of clipped
material are detailed below.
(i) Shrubs: microphanerophytes and nanophanero-
phytes of families such as Proteaceae, Ericaceae and
Leguminosae.
(ii) Sub-shrubs: sub-ligneous nanophanerophytes
and chamaephytes of genera such as Stoebe and
Metalasia (Asteraceae).
(iii) Graminoid: hemicryptophytes typical of Po-
aceae and Cyperaceae.
(iv) Restioid: leafless hemicryptophytes of the
family Restionaceae and, sometimes, Cyperaceae,
described as assimilating stem type hemicryptophytes
by Adamson (1931).
(v) Herbs (forbs): non-ligneous elements not in-
cluded in above categories, and including ferns.
In the laboratory the fresh mass of the contents of
each bag was determined before the material was
chopped mechanically in lengths of 0,5 to 3,0 cm.
A sample of four 50-100 gm units was drawn from
the chopped material after thorough mixing. The
moisture content of these was determined by normal
oven-drying procedures (105°C for 24 hours). The
mean moisture content of the subsample was used to
estimate the oven-dry mass of the original material.
Table 2 includes the ‘age’ of the communities. This
represents the time since the last burn and closely
approximates the real age of the shrubs that have
regenerated from seed. Age was determined from
Department of Forestry records or, where this was
not possible, by node-counts on Proteaceae as
described by van der Merwe (1969).
RESULTS AND DISCUSSION
Data are presented in detail in Table 2 and further
depicted in Fig. 5. The curves in Fig. 5 were drawn
by hand and fitted to represent the approximate upper
and lower limits of the data set.
AGE IN YEARS
Fig. 5. — Approximate regression of biomass on age. Dots
represent actual data points from Table 2.
Sample efficiency
The coefficients of variation for total biomass shown
in Table 2 clearly indicate that, in many cases, random
samples of clipped quadrats need to be large for
reasonably precise biomass estimation. The number of
sample units used here was seldom adequate to
ensure a confidence interval equal to or less than 20
per cent of the mean, at five per cent probability of
error. For a confidence interval of 20 per cent of the
mean, about thirty to sixty quadrats would be required
(and in some cases a great deal more). Furthermore,
the samples were not large enough to show a signifi-
cant difference (at P=0,95) between harvests in suc-
cessive years on the same site, though the vegetation
had obviously grown.
These estimates are much less precise than those
reported by Jones & Specht (1967) and Jones (1968),
who obtained estimates with 95 per cent confidence
interval of about 12 per cent of the mean, using 12 to
20 one-metre-square quadrats. These authors con-
cluded that successive harvests were not appropriate
in production studies in heath.
Since the information reported here was collected
with the aim of monitoring long-term trends in
F. J. KRUGER
305
biomass, it was not thought profitable to improve
precision by increasing sample size. Nevertheless,
future studies would benefit if larger quadrats were
used. Where greater precision is required and alter-
native techniques of production measurement (such
as gas-exchange measurement) are not feasible, a
combination of sampling by vegetation strata and
allometric subsampling of dominant species popula-
tions should solve some of the problems due to
heterogeneity in fynbos communities.
Precision in these data sets is felt adequate for the
purposes of this discussion.
Rates of growth
Fig. 5 may be used to indicate means and ranges
in the rate of growth of fynbos communities. The
data do not cover a full range of fynbos communites:
old stands of tall sclerophyllous scrub are hardly
represented. Nevertheless, a reasonable picture has
emerged. The highest rate was exhibited by the phre-
atic community at site 2.2 — about 4 000 kg per ha
per annum during the first two years. In contrast,
the heath community in the same locality, at site 2.3,
grew at about 1 000 kg per ha per annum during the
same period. These values are close to the upper and
lower limits of mean annual increment represented
by the curves in Fig. 5. A rate of 2 500 kg per ha per
annum appears to be a reasonable average.
Growth rates appear to fall off rapidly as com-
munities age.
Sclerophyllous scrub (represented by sites 1 . 1 to
1 . 3) would seem to grow about as fast as the phreatic
community, although that at Jakkalsrivier (site 3.5)
appears subnormal. Heath communties show rates
between normal and the minimum.
Fynbos as fuel
Fynbos communities readily sustain a running fire
under average summer conditions once they have
reached four years of age and may burn at three
years under severe fire hazard conditions.
Several communities of about four years old have
been sampled. These had biomasses of about 5 000
to 10 000 kg per ha, which may be accepted as reason-
able minimum fuel levels for a successful burn. Site
3 . 4, with about 7 000 kg per ha at four years, sustained
a hot fire in a prescribed burn 1 1 months later.
At four years of age most communities are domin-
ated by graminoid and restioid plants. These are
all fine fuel (i.e. with particle diameters less than six
millimetres). Furthermore, cured material forms
a significant proportion of the fuel after the second
or third year when leaves and stems from the first
and second growing seasons die, but remain attached
and erect for a further one or two seasons. At this
stage, therefore, the vegetation provides a fine, porous
but reasonably compact fuel bed, much like a grass-
land fuel. This would explain why they burn readily
at this age in spite of the rather small quantities of
available fuel.
The rapid rate of growth of a phreatic community
like that at site 2.2 does not necessarily imply inflam-
mability at an earlier age. Plant material in such com-
munities is green and does not cure readily in the
early stages: in fact, an inflammable stage is often
delayed longer than in other communities.
Heaths from Jakkalsrivier have a low biomass
(11 000 to 15 000 kg per ha at 16 years), but dead
plants and litter can comprise up to a quarter of the
total. As a result, and because the communities are
dominated by plants with fine leaves and branches,
they burn fiercely under dry conditions, and fires are
often extremely difficult to control.
The mature sclerophyllous scrub communities at
Jonkershoek provide considerably more fuel, but
much of this is coarse and available only under
extreme fire hazard conditions.
Community structure and development
Most plants in the fynbos sprout after fire (Wicht,
1945; van der Merwe, 1966). The graminoid and
restioid plants are almost all of this nature, whereas
many shrubs and subshrubs are not. Communities in
the early stages are dominated by the former (which
comprise about 60 to 75 per cent of the biomass at
three to four years) and the vegetation has the phy-
siognomy of a grassland. Since individual shoots and
leaves of the hemicryptophytes do not live longer
than about two years, and fall after another two
years, this component reaches its maximum in about
the fourth year. Thereafter woody elements become
prominent if conditions are suitable, although herbs
persist and maintain their biomass for many years.
Communities on moist or wet sites (as at 2.2 and
3.3) have a rather different initial physiognomy, since
they frequently contain a high proportion of sprouting
shrubs, which reach early prominence in develop-
ment.
CONCLUSION
Considerable data on growth and biomass of shrub
communities in mediterranean type ecosystems have
become available recently.
Specht (1969a, 1969b) has compared analogous
communities from the southern regions of France,
California and Australia. He estimated mean annual
increments (M.A.I.) for the first five years after fire,
as follows:
M.A.I.
kg per ha
Montpellier 4 200
San Dimas 1 200
Dark Island, S. Australia 640
Southern Victoria 1 500
Maximum biomass reported was about 49 700 kg
per ha at 13 years for garrigue, and 49 100 at 37
years for chaparral (of which 21 800 kg consisted of
standing dead sticks).
Specht suggests that his data for the garrigue near
Montpellier are atypical, and this is confirmed by
Long & Thiault (pers. comm.). Data from more
typical garrigue indicate a mean annual increment of
about 1 400 kg per ha per annum during the first
six years, and total biomass of about 15 000 kg per
ha at 18 years (Long et al., 1967 in Specht, 1969b;
Long & Thiault, pers. comm.). These also show that
the garrigue growth curves also resemble the typical
cases illustrated by Specht (1969b) and Jones et al.
(1969).
Aerial biomass of an evergreen chaparral communi-
ty of unspecified age at Echo Valley, California (mean
annual precipitation 450 mm) amounted to 23 000
kg per ha; that of a similar community on a similar
site in Chile amounted to about 7 400 kg per ha
(Mooney, pers. comm.).
Jones et al. (1969) have collated growth data for
Australian heath communities. They produced two
curves for growth of aerial portions of the com-
munities, one representing the drier and the other the
wetter limits of the geographical range of heat in
Southern Australia. Growth rates during the first
five years amount to about 800 kg per ha per annum
in the first instance, and 1 500 kg per ha per annum
306 A PRELIMINARY ACCOUNT OF AERIAL PLANT BIOMASS IN FYNBOS COMMUNITIES OF THE
MEDITERRANEAN-TYPE CLIMATE ZONE OF THE CAPE PROVINCE
in the second. Maximum biomass for coastal sites
was about 16 000 kg per ha at 18 years (sand heath
at Tidal River, Victoria). They caution that: “The
growth curves do not necessarily indicate the maxi-
mum production of each site. This may be influenced
by the development (or invasion) of taller-growing
species . . . Such cases are reported by Specht
et ah (1958). Communities dominated by Banksia
ornata have a biomass of almost 20 000 kg per ha
at 15 years of age.
The data for fynbos are similar to those for analo-
gous communities in other areas with mediterranean
type climates. The curves in Fig. 5 indicate a mini-
mum rate of growth of about 1 000 kg per ha per
annum, and a maximum of 3 400, over the first five
years after fire. The most vigorous community is
that on the phreatic site (2.2), but the maximum
biomass measured is that of a 17-year old sclero-
phyllous scrub community at Jonkershoek: this is
about the same as that of the 18-year old chaparral
community sampled by Specht. The mature heath
communities at Jakkalsrivier, however, have a lower
biomass than all those of equivalent age studied
elsewhere except the mallee-broombush (Specht,
1969b), which is not a good fynbos analogue.
On the whole the figures support Specht’s conclu-
sion that “The growth rates of these distinctive plant
communities, composed of entirely different species,
are largely controlled by the major factors — solar
radiation and available water. In similar homoclimes
essentially the same growth rate results.” More infor-
mation is necessary to explain differences within the
data sets, but there is good evidence that soil moisture
availability overrides the effect of soil fertility, and
that community production is strongly affected by
the presence or absence of tall long-lived shrubs, at
least in Australia and South Africa.
Data for the biomass of growth-form categories in
fynbos stands provide a limited basis for comparisons
of community structure. They do indicate that
persistent perennial herbs, particularly hemicrypto-
phytes, are a feature which distinguishes fynbos
from northern analogues. Chaparral is known for
the rich herbaceous annuals which appear after fire,
with peak abundance within one to five years, and
disappear almost completely thereafter (Sweeney,
1956; Vogl & Schorr, 1972; Mooney & Parsons,
1973; Biswell, 1974). These comprised 75 and 14
per cent respectively of total live biomass in one-
and three-year old chaparral sampled by Specht
(1969b), but were absent in the nine-year old stand.
The herbaceous flora of the mediterranean maqui
and garrigue also respond strongly to fire, but include
perennials which persist in old stands in small quanti-
ties (Naveh, 1974; Long & Thiault, pers. comm.),
though their biomass is never large. The communities
studied by Specht were dominated from the start by
phanerophytes and chamaephytes: herbs amounted
to 30 per cent of total biomass in the first year after
fire, of which hemicryptophytes contributed about
500 kg per ha or 10 per cent of total biomass. The
hemicryptophytes became insignificant after the
sixth year of development, but other herbs persisted.
Long & Thiault report that biomass of herbs may
often be over 10 per cent of the total in the first year.
In fynbos, herbs contribute up to about 4 500 kg
per ha after two growing seasons; as noted, hemi-
cryptophytes dominate communities up to at least
four years after burning. Herbs in sixteen-year old
heaths have biomasses up to 8 000 kg per ha, with
restioid and graminoid plants predominant.
Australian communities are similar in this respect,
but the perennial herbaceous component is not as
large as in fynbos. Data from a “sand heath” at
Frankston, Victoria (Jones & Specht, 1967; Jones,
1968) show that hemicryptophytes (Restionaceae and
Cyperaceae) reached a maximum of about 2 100 kg
per ha at four years, comprising about 32 per cent
of the biomass. At eight years the proportion was
26 per cent. Comparative studies on Wilson’s Pro-
montory in the same State (Groves & Specht, 1965)
showed that hemicryptophytes in a “wet heath” had
twice the mass of those in a “ sand heath” (2 000 vs
1 000 kg per ha), but persisted in old (twelve-year)
stands in both cases. Specht et ah (1958) noted, of
Dark Island “sand heath”, that certain understorey
plants including hemicryptophytes regenerate rapidly
after fire and persist for 25 years in the ageing com-
munity. Some Restionaceae and Cyperaceae continue
to increase as the community develops, but the bio-
mass of the herbaceous elements does not appear to
have exceeded about 1 000 kg per ha.
Certain Australian communities of infertile soils,
such as the Gymnoschoenus hummock sedgelands or
“Button-grass plains” and Restionaceous sedgelands
of Tasmania (Jackson, 1965; 1972; Paton & Hosking,
1975) and forb heaths of Southern Queensland (Coal-
drake, 1961) have a high proportion of perennial
hemicryptophytes, and resemble fynbos in this way.
Fynbos and the Australian equivalents therefore
have a characteristic persistent herbaceous com-
ponent, which distinguishes them from analogous
shrublands elsewhere, but they differ in that the
component is more prominent in the former.
ACKNOWLEDGEMENTS
This report is based on work undertaken as part
of the catchment conservation research programme
of the South African Department of Forestry and
published with the permission of the Secretary for
Forestry.
Most of the field work was undertaken by research
foresters of the Jonkershoek Forest Research Station.
In this connection, the work of Ross Haynes and
Maarten van der Riet was invaluable, as was their
assistance in the preparation of this paper.
Dr G. Long and M. M. Thiault of the Cepe, Mont-
pellier, very kindly supplied new information on
garrigue biomass and composition. Prof. R. L. Specht
provided useful comment on the manuscript.
UITTREKSEL
Bogrondse plantbiomassa van fynbosgemeenskappe is
bemonster op verskeie groeiplekke in die suidwestelike
Kaapprovinsie.
Biomassa van opstande met 'n ouderdom van onge-
veer twee jaar wissel van omtrent 2 200 kg per ha tot
7 500 kg per ha. Volwasse opstande bestaan uit om
en by 11 000 tot 15 000 kg per ha in heideveld, en
15 000 tot 26 000 kg per ha in sklerofiele struikgemeen-
skappe. Die data toon 'n maksimum jaarlikse aanwas
van 1 000 tot 4 000 kg per ha in jong opstande, maar
groeitempo's neem waarskynlik vinnig af soos gemeen-
skappe ouer word. Jong opstande word gedomineer
deur hemikriptofiete , waarvan die massa ongeveer
2 000 tot 6 000 kg per ha beslaan, d.w.s. 60 tot 75
persent van die biomassa in die opstande van min of
meer vier jaar oud. Struike word prominent in ouer
opstande alhoewel die hemikriptofiete bly voortbestaan.
Volgens die data is die biomassa, aanwas en vorm
van groeikurwes van fynbosgemeenskappe oor die
F. J. KRUGER
307
algemeen dieselfde of gelykstaande aan die van gelyk-
soortige plantegroei in ander werelddele wet 'n medi-
terreense klimaattipe ( garrigue , chaparral). Daar is
egter belangrike strukturele verskille. Die analogiese
plantegroei van die noordelike hemisfeer bevat nie 'n
beduidende deel van hemikriptofiete nie. Alhoewel die
Australiese fteide' -gemeenskappe bier die eienskap
vertoon is die hemikriptofiete nie so prominent as in
fynbos nie.
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Bothalia 12,2: 309-311 (1977)
Silene dewinteri , a new species of the Caryophyllaceae from
the south-western Cape
GILBERT BOCQUET*
ABSTRACT
A new species of Silene, S. dewinteri Bocquet, is described from the sand-dunes of the coastal region of the
south-western Cape. The species is closely related to S. crassifolia L. and S. clandeslina Jacq.
RESUME
Une nouvelle espece de Silene, S. dewinteri Bocquet, est decrite des dunes de sable de la cote du sud-ouest de
la province du Cap. Elle est etroitement apparente aux S. crassifolia L.et S. clandestina Jacq.
INTRODUCTION
During the course of a journey undertaken to collect
material for a revision of the South African species of
the genus Silene, 1 had the opportunity of collecting
extensively in the region of Cape Town. One of the
localities visited was the coastal area in the vicinity
of Table View, 18 km north of Cape Town. This is one
of the localities often cited by Ecklon and Zeyher in
their “Enumeratio” (1834) under the name of “Riet-
valley” or “Riedvalley”. I was trying to trace an
elusive species listed as “ Silene Constantia" in Ecklon
and Zeyher’s work — a species closely related to 5.
clandestina Jacq. I found the plant growing in popu-
lations on the sand dunes of the coast between Table
View and Melkbosstrand mostly side by side with
populations of S'. crassifolia L.
The plant is an annual species with a spreading
habit, fleshy leaves, thickened calyx and protruding
calyx nerves. Unfortunately, the name S. constantia
cannot be given to this species, because it applies to
another species (see p.000 under Nomenclature). 1
therefore name the plant S. dewinteri in honour of Dr
B. de Winter, Director of the Botanical Research
Institute, Pretoria.
DESCRIPTION
Silene dewinteri Bocquet sp. nov., S. clandestinae
Jacq. valde affinis, a quo tamen habitu diffuso, foliis
crassis, calyce incrassato nervis prominentibus differt.
S. constantia Eckl. & Zeyhr., Enum. 32 (1834), quoad descr.,
typo et synonymia excludendis.
Radix simplex, tenuis. Caulis 7-20 cm altus, e basi
ramosus, ramis expansis, procumbentibus, interdum
quasi geniculatis, pilis retrorse appressis. Folia
anguste elliptica vel anguste oblanceolata, 3-6 (-10) X
15-40 (-60) mm magna, plus minusve hirta, margini-
bus hirtis, basin versus ciliatis, succulenta, circa 1 mm
crassa, id est statu sicco valde rugata. Racemus 3-7-
florus, floribus secundis, primum vix cernuis, maturi-
tate fructus perfecta erectis. Calyx incrassatus, hir-
sutus, anthesi campanulatus et 4-5x12 mm, maturi-
tate fructus conspicue clavatus et turn 5-6x12 mm
magnus, nervis crassis prominentibusque. Petala bifi-
da, ungue calycem breviter superante, in fauce
appendicibus binis 0,5-1 mm altis praedita, limbo
5-8 mm longo, intus sordide bianco, extus virides-
cente vel brunnescente. Gonophorum 4-5 mm altum,
glabrum. Ovarium viride, ovoideum. stylis 3 praedi-
tum. Capsula brunnea, 3x8-9 mm magna. dentibus 6
Fig. 1. — Silene dewinteri. Holotype plant
(Bocquet 17774) growing on sand
dunes at Table View, south-western
Cape. The maturing capsules, broa-
der calyx with bulging nerves, thick
leaves and spreading habit of the
whole plant are evident.
Eidgenossische Technische Hochschule, Zurich, Switzerland.
3 10 SILENE DEWINTERI, A NEW SPECIES OF THE CARYOPHYLLACEAE FROM THE SOUTH-WESTERN CAPE
se aperiens, calycem maturitate fructus perfecta
superans. Semina fusca, dorso alis 2 undulatis in
ambobus lateribus circumdato. n=12. FiG. 1.
Type. — Cape Province, Table View, 18 km N of
Cape Town, low undulating sand dunes between
coastal dune and marshy hinterland, on semi-barren
sand in disturbed area near a new settlement, 1 975—
11-09, Bocquet 17774 (ZT, holo.).
The species is endemic to the south-western Cape.
See Fig. 2.
Fig. 2.— Distribution of S. dewinteri. 1, type locality; 2, Onrus
River Mouth where Bocquet 17881 (chromosome count,
n=12) was collected; 3 &4, Ecklon and Zeyher’s localities,
“prope Constantiam” and “Hottentotsholland”.
Cape. — 3318 (Cape Town): Bok Bay, WSW of Malmesbury
(-CB), “flowers white”, 1940-09-14, Compton 9389 (NBG);
Table Bay, between Bloubergstrand and Melkbosstrand, north
of Cape Town (-CD), scattered at the foot of the coastal dune
on the sea side, on half-colonized sand, bordering an extensive
colony of S. crassifolia, 1975-11-09, Bocquet 17781; 17783
(ZT; PRE; NBG); seeds and preserved material from same
population, Bocquet 17818 (ZT); Bloubergstrand (-CD),
1954-09-10, Stokoe 67560 (NBG); Robben Island, N of Cape
Town (-CD) 1932-10, Adamson s.n. (BOL); Robben Island,
1943-08-20, Walgate 512 (NBG); Table View, 18 km N of
Cape Town (-CD), Bocquet 17774 (holo., ZT); 17775 ; 17776
(Z); “in locis arenosis (alt. 1) collium capensium prope Con-
stantiam et Hottentotsholland” [these two localities are rather
indeterminate: they correspond roughly to Muizenberg (-BA)
and Strand (-BB)], s.d., Ecklon & Zeyher s.n. (NBG). 3419
(Caledon): Onrus River mouth, 7 km W of Hermanus (-AC),
sandy areas between bushes on the low undulating dunes
between rocky strand and new settlement, very near the shore,
locally abundant, 1975-11-17, Bocquet 17881 (seeds, ZT);
17882 (ZT); “Onrus riv. Sand dunes”, 1958-09-28, Willems
57 (NBG).
OBSERVATIONS
1. Ecology, biology. S. dewinteri is an annual grow-
ing scattered in the half-colonized parts of coastal
dunes, in open localities on semi-stabilized sand. It is
often accompanied by S. crassifolia, a perennial
species, that prefers more unstable sqnd. The two
species are rarely found in mixed colonies: they
usually occur in contiguous colonies occupying diffe-
rent ecological situations. The ecological relations
between the two species are shown in Fig. 3, a schema-
tized section of the Bloubergstrand locality ( Bocquet
17781). S. dewinteri occupies the immediate foot of
the dune, where the sand is half-colonized and semi-
fixed, while S. crassifolia occurs abundantly on the
undulating area between sandbank and dune on very
sparsely colonized and entirely unstable sand.
Flowering times are different for the two species:
S. dewinteri flowers in August and September, and S.
crassifolia from October to January. A biological
barrier therefore exists between the two species. No
trace of introgression or morphologically intermediate
specimens was observed in the localities visited. S.
dewinteri seems to be equally distinct from S. clande-
stina. The latter species is also an annual, but is not
found as near the sea shore as S. dewinteri. S. dewinteri
seems to be strictly limited to the immediate proximity
of the sea.
2. Taxonomy. S. dewinteri has rarely been collected,
probably because the more common S. crassifolia
occurs in the same localities and depauperate forms
of the perennial S. crassifolia can easily be mistaken
for the annual S. dewinteri.
The affinities are clear : S. dewinteri is closely allied
to both S. clandestina and S. crassifolia, but can be
distinguished as follows:
(a) from S. crassifolia by its annual character,
smaller calyx and thin root: S. crassifolia always has,
even in the youngest stages, a thickened root; the
older specimens build up a nearly bulbous root.
(b) from S. clandestina by the thicker leaves,
clavate, broader and very fleshy calyx, as well as the
spreading habit. Material was cultivated in Switzer-
land under glass from seeds of the three populations
Bocquet 17818, 17774 and 17881. The plants are some-
what more flaccid and the leaves bigger, but the essen-
tial characters can be recognized, namely the thick-
ness of leaves, spreading habit and broader calyx with
bulging nerves.
3. Nomenclature. Ecklon and Zeyher intended
describing our plant as a new species under the name
of S. constantia (the specific epithet refers to Constan-
ts, a suburb of Cape Town). The description, locali-
ties and herbarium material agree with S. dewinteri
However, Ecklon and Zeyher cited S. crassifolia L
Fig. 3. — Transect of the Bloubergstrand locality ( Bocquet 17781; 17783). 1, strand; 2, distribution of S. crassifolia on the undulating
ground in front of the coastal dune (sparsely colonized and unstable sand); 3, S. dewinteri, at the foot of the coastal dune (semi-
fixed and half-colonized sand).
GILBERT BOCQUET
311
var. angustifolia Bartling (1832) in synonymy and
therefore S. constantia is automatically typified by the
type of this variety. The type specimens of var.
angustifolia were collected in the vicinity of King’s
Blockhouse (“Beim obersten Blockhause”) on the
north-eastern slopes of Devil’s Peak above Rhodes
Monument. These specimens represent a local form of
S. clandestina, an ecotype of dry barren hillslopes that
is commonly encountered in the Table Mountain and
Lion’s Head region between 100 and 400 m. It is a
small, erect plant with very narrow leaves, but there is
no good reason why it should be recognized and
described as a distinct infraspecific taxon.
4. Cytology. Chromosome counts on flower buds
of cultivated material yielded the number n— 12.
Material: Bocquet 17881; Carnoy-acetocarmine treat-
ment; 10 counts from 3 slides and 2 buds. Fig. 4 shows
an anaphase; the chromosomes are small, but not as
contracted as they usually are in meiotic phases of
Silene species. In most Silene species they appear at
this stage as more or less isodiametric spots.
ACKNOWLEDGEMENTS
This work has been carried out with the aid of a
grant from the Societe helvetique des Sciences Naturel-
les and additional assistance from the ETH-adminis-
tration. I thank these authorities.
UITTREKSEL
’ n Nuwe species van Silene, S. dewinteri Bocquet,
word beskryf van die sandduine van die kusstreek van
die suidwestelike Kaap. Die species is naverwant aan
S. crassifolia L. en S. clandestina Jacq.
Bothalia 12, 2: 313-317 (1977)
The taxonomic status of the genus Rubidgea
EVA KOVACS-ENDRODY*
ABSTRACT
The genus Rubidgea Tate of the fossil family Glossopteridaceae was reduced to a synonym of Glossopteris
by Seward (1907). Seward’s conclusion is now confirmed by a study of a wide range of imprints from a quarry
near Hammanskraal, South Africa. The upper and lower surface imprints of a single leaf found on a split
fragment of carbonaceous shale provides the main evidence presented. The finely striated upper surface imprint
of the leaf could be identified with Rubidgea , whereas the lower surface imprint represents the typical strong
venation of a Glossopteris. The type species of Rubidgea is transferred to Glossopteris as G. mackayi (Tate)
Kovacs comb. nov. The characteristics of upper and lower surface imprints of a number of Glossopteris
species are discussed.
RESUME
STATUT TAXONOMIQUE DU GENRE RUBIDGEA
Le genre Rubidgea Tate de la famille fossile des Glossopteridaceae fut consider e par Seward (1907) comme
un synonyme de Glossopteris. La conclusion de Seward se voit confirmee par T etude d'un vaste eventail d’em-
preintes en provenance d’une carriere pres d‘ Hammanskraal en Afrique du Sttd. Les empreintes superieure e>
inferieure d'une meme feuille, trouvees stir un fragment de ciivage d’un schiste carbonifere, fournissent le principal
argument qui est presente ici. L ’empreinte finement striee de al face superieure de la feuille pourrait etre idem idee
comme Rubidgea, tandis que I’empreinte de la face inferieure presente la forte nervation typique de Glossopteris.
L'espece-type de Rubidgea est transferee au genre Glossopteris, so it: G. mackayi (Tate) Kovacs comb, nov
Les caracteristiques des empreintes superieures et inferieures de plusieurs especes de Glossopteris sount discut ees.
INTRODUCTION
The family Glossopteridaceae appeared approxi-
mately in the Upper Carboniferous and disappeared
more or less synchronously in the Lower Triassic.
Though the species changed in time due to evolution
and adaptation to changing climatic conditions, they
are nevertheless generally recognizable as glossop-
terids. All evidence points to the family Glossopteri-
daceae of the Order Pteridospermales being a mono-
phyletic and natural group of plants. As in most
fossil groups, the classification presents considerable
difficulties. Recently doubts have been expressed
about the feasibility of a classification of the Glossop-
teridaceae based on leaf impressions when no cuticles
or attached fructifications are available. In this and
other papers, the author defends the point of view
that taxa, at least at the specific level, may be distin-
guished by normal taxonomic methods, provided that
sufficient good material, which is synchronous, is
available and is studied in detail. The basic venation
patterns of leaves are typical for all members of the
group, but venation characters display definite and
useful differences. The fact is that all fossil plants
represent once living plants and this realization is
necessary for real progress to be made. A knowledge
of living extant plants should form an essential part
of the equipment of the palaeobotanist.
In the investigation here reported the author has
attempted to apply these views to the study of a rich
deposit of glossopterid fossils. Special attention is
given to the taxonomic status of the genus Rubidgea
Tate. The material for this study was collected on the
farm of Mr J J Brits, 30 km north of Pretoria near
Hammanskraal. The carbonaceous shales, in which
the leaf impressions are preserved, are of Ecca age.
All the specimens studied are deposited in the offices
of the Geological Survey, Pretoria, South Africa.
THE IDENTITY OF THE GENUS RUBIDGEA
The genus Rubidgea was described by Tate in Q.
J1 Geol. Soc. Lond. in 1867. The description is as
follows:
“Rubidgea Mackayi, gen. et spec. nov.
Frond oblong, obovate, rounded and obtuse at the apex;
secondary veins very slender, very much crowded, dicho-
tomous, oblique. There is no indication of anastomosis of
* Geological Survey, Private Bag 112, Pretoria.
the veins. Localities. Bloemkop, near the Sunday’s River,
Graaff Reinet (Dr Rubidge); East London, at the mouth
of the Buffalo River (Mr. McKay).”
In the preamble to this description Tate, however,
says the following:
“With the above-mentioned specimens from Bloemkop are
some of an apparently, at first sight, second species of
Glossopteris ; these do not exhibit fructification. Dr Rubidge
however, has communicated a drawing (by Mr McKay) of
a specimen of this species obtained by Mr McKay near
East London: and I find that it presents characters generi-
cally distinct from those of Glossopteris ; for the position of
the fructification is indicated by a few large elevated rings,
arising from many veins, and somewhat regularly arranged
in a row coincident with the margin, and not by numerous
spots, small in size, supported by one vein, distributed over
much of the surface of the frond”.
Whereas the description of the new genus and
species is clearly based on the leaf, Tate’s comments
in the second paragraph quoted here, show that it
is only because of the so-called fructifications that he
considered creating a new genus. It so happens that
the two specimens cited by Tate have, in spite of several
searches, not been traced. A comparison of the speci-
mens with the McKay drawing has thus not been
possible. It seems clear that Seward (1907), who
regards Rubidgea as a synonym of Glossopteris , also
did not see Tate’s syntypes. Since the specimens are
missing, there seems to be no alternative but to accept
the drawing by McKay published by Tate as Plate 5,
Fig. 8, as the lectotype of Rubidgea Tate. It has already
been pointed out by Seward (1907) that the so-called
fructifications depicted by McKay, are artefacts and
I agree with this view.
THF, RELATIONSHIP BETWEEN RUBIDGEA AND
GLOSSOPTERIS
When studying the fossil flora of the Hammanskraal
quarry, many leaf impressions were found which show
the characteristic venation described and figured by
Tate for his genus Rubidgea. A venation, such as
figured by Tate, is difficult to interpret morphologi-
gically. The very fine veins arise from the median line
of the leaf, but are apparently not joined into a true
midvein. A closer examination of these "Rubidgea
leaves from Hammanskraal shows that some of them
exhibit areas of stronger venation with anastomoses
typical of the genus Glossopteris (Fig. 3). It seems
314
THE TAXONOMIC STATUS OF THE GENUS RUBIDGEA
Figs 1 & 2. — Glossopteris sp.* Counterpart “Rubidgea”. Catalogue Nos HI 103a & b. x2.
♦ The species of Glossopteris discussed and figured in this paper was recently described by me as G. pseudoeommunis (1976).
However, this name is a later homonym of G. pseudoeommunis Pant & Gupta (1968) and consequently illegitimate. I therefore rename
the species, G. andreanszkyi in honour of Professor G. Andrednszky, my mentor in palaeobotany at the University of Budapest.
Glossopteris andreanszki Kovacs, nom. nov.
G. pseudoeommunis Kov&cs in Palaeontogr. Afr. 19: 81 (1976) non G. pseudoeommunis Pant & Gupta in Palaeontogr. 124B: 57
(1968).
fiVA kovacs-endr5dy
315
fairly certain that in these leaves part of the upper
surface has decayed or peeled off revealing the nerva-
tion of the lower surface. In other instances both
kinds of “venation” are seen on the leaf as if super-
imposed. On these imprints dense and fine lines are
visible between the typical Glossopteris veins (Fig. 4).
Amongst the many slabs of slate split, one showed an
almost entire leaf with clear upper and lower surface
imprints. These imprints are dissimilar, one being
typical of Glossopteris, the other of Rubidgea (Figs 1
and 2). It is obvious also that the impression
of the lower surface, which shows Glossopteris
characters, represents the imprint of the venation.
The very slender lines of the Rubidgea imprint, which
do not match the nervation of the lower surface,
have to be interpreted as fine grooves found on the
upper surface of some Glossopteris species. The leaves
of many extant species of plants would show feature-
less upper surface imprints, because their veins are not
raised. There are many examples of these three states,
viz. parts of Glossopteris leaves which show Rubidgea
characters or vice versa and both kinds of “venation”
next to one another on the same leaf.
These observations indicate that the genus Rubidgea
and some species of Glossopteris were based on impres-
sions of upper and lower surfaces of leaves respec-
tively, Rubidgea representing impressions of the upper
and Glossopteris of the lower surface. There is real
proof, therefore, that the genus Rubidgea must be
regarded as a synonym of Glossopteris as concluded,
on rather slender evidence, by Seward.
Fig. 3. — Glossopteris sp. “Rubid-
gea" surface with patches of
Glossopteris venation. Cata-
logue No. HI 10a. x 1 , 3
Fig. 4. — Glossopteris sp. With
“fibres”. Catalogue No. HI
165. x 3,4.
316
THE TAXONOMIC STATUS OF THE GENUS RUBIDGEA
The study of several glossopterid species of the
Hammanskraal fossil flora showed that in all species
investigated, except for G. indica, the upper and lower
surfaces differed in a characteristic and specific
manner. In G. indica both surfaces were more or less
similar. Of the species examined, all leaves with
“Rubidgea” features proved to belong to the same
species (Kovacs, 1976). It is possible, however, that
other species may also exhibit a “Rubidgea” type of
upper surface.
As I mentioned before, in some instances the imprint
of what appears to be both upper and lower surfaces,
can be seen on the same leaf impression (Fig. 4). In
such cases there are thinner lines between the strong,
anastomosing veins. This feature merits further
discussion. Pant (1958) described two new species,
namely Glossopteris fibrosa and G. hispida, based
mainly on cuticular examinations. He mentions that
G. fibrosa : “looks much like many of the figures
given by various authors under the names G. brow-
niana var. indica (G. indica), G. angustifolia, G. brow-
niana var. australasica, ( G . browniana) and G. com-
munis ... All are clearly different because they lack
fibres in vein meshes”.
On the evidence of the leaves from Hammanskraal,
I interpret such fibres as being the markings of the
upper (or “Rubidgea”) surface showing through on
the lower surface. This interpretation is to some extent
confirmed by Pant (1958). He mentions that G. fibrosa
and G. hispida, which both show the so-called fibres
in the vein meshes, have rather thin laminae. Prior to
these studies, differences between upper and lower
surfaces of a Glossopteris leaf were already reported
for G. browniana by Dana (1849, p. 717).
In the light of the foregoing, it is of some interest
to establish how it has come about that the upper and
lower surface leaf impressions were described as
separate genera and why, one hundred years later
these genera were still being recognized and expanded.
The description and identity of Rubidgea have
already been discussed. It is clear, as stated before,
that Tate believing these plants to be ferns, separated
the new genus from Glossopteris mainly because of the
presence of so-called “fructifications”. In his diagnosis
of the species he does not comment on the presence
of a midrib, but implies this by stating: “secondary”
veins very slender, very much crowded. The “secon-
dary” veins arise from the midline of the blade and
not from the base, which logically indicates a mid-
vein or a structure resembling a midvein.
Feistmantel’s (1881, p. 91) statement when com-
paring Palaeovittaria with Rubidgea, viz. “this latter
(i.e. Rubidgea) showing no indication of a midrib in
the lower part”, is therefore incorrect. On the drawing
by McKay, published by Tate, the lower part of the
leaf is missing but, as already indicated, shows the
situation where the “secondary” veins arise from the
median part of the leaf. In spite of this, Rubidgea is
still usually characterized by the absence of a midrib
as was done recently by Maheshwari (1965, p. 37).
Maithy (1965) accepted Rubidgea as a generic
entity, but amended it to accommodate several
species found in the Karharbari Beds of the Ciridih
Coalfield in India. Maithy (p. 42) also starts the
description of the venation with the statement
“devoid of a midrib”. The characterization of taxa
such as Gangamopteris and Rubidgea by the “absence
of a midrib”, and the failure of authors to refer back
to the type specimens, contributed to the confusion
which arose. The morphological terms applied to
extant plants are not always appropriate to extinct
groups: “midrib” does not mean the same in Glossop-
teridaceae as it does, for example, in Angiosperms.
Glossopteris leaves have a bundle of veins down the
middle, but no clear single midrib. When Maithy
writes of “numerous veins arising from the median
longitudinal position of the frond, occasionally
simulating a false midrib”, he accurately describes
Tate’s drawing. Later in his paper, Maithy refers to
median veins, however, and omits the important
character mentioned in Tate’s description, that the
secondary veins are very slender and closely crowded
together. Ignoring this character, he described two
new species, Rubidgea obovata and R. lanceolatus,
both of which have rather strong veins. On the photo-
graphs of the leaf impressions of the two species,
three of the four leaves have parallel veins fanning
out from the narrowed base, yet Mainthy himself
chracterizes Rubidgea by “veins arising from the
median longitudinal position”.
At the end of his paper, Maithy indicates that the
leaf of Lanceolatus palaeovittarius Plumstead “appears
to be a Rubidgea because no midrib is evident, and the
median region of the leaf seems to be occupied by
the subparallel veins”. In Feistmantel’s time the more
crowded subparallel median veins of glossopterid
leaves were described as a midrib, and it is possible
that this condition is found in Palaeovittaria Feistm.
(1876, p. 368).
In Plumstead’s figure (1958, PI. 16, Fig. 1) the
strong, rigid, straight veins clearly do not resemble
those of Rubidgea as defined by Tate. The leaf of
Lanceolatus palaeovittarius, however, resembles Rubid-
gea lanceolatus, a fact also mentioned by Maithy.
Furthermore it is likely that Rubidgea lanceolatus
Maithy (PI. 1, Fig. 5) represents the same species as
Palaeovittaria kurzii Fstm.
Maithy also mentions Gangamopteris obovata
Carruthers as a possible Rubidgea, because “secon-
dary veins emerge from median veins”. Carruthers’s
figure (1869) depicts a whole leaf and the equally
strong subparallel veins radiate from the base.
Dr C. R. Hill of the British Museum of Natural
History checked the holotype (v.229, Geol. Surv.,
British Museum Nat. Hist.) at my request. He found
the drawing remarkably accurate, except in showing
the anastomoses between the veins.
The confusion that exists in the taxonomy of
Glossopteris and related genera can be attributed to
poor descriptions and circumscription of new taxa;
to the difficulties inherent in the interpretation of
what represents a “midrib” of the leaf of the Glossop-
teridaceae; and to the fact that the differences in the
upper and lower surfaces of glossopterid leaves are
usually ignored.
If progress is to be made with the taxonomy of the
Glossopteridaceae, these pitfalls will in future have
to be avoided.
A NEW COMBINATION IN GLOSSOPTERIS
In order to comply with the Rules of Botanical
Nomenclature the formal transfer of the type species
of Rubidgea to Glossopteris is hereby made.
Glossopteris mackayi {Tate) Kovacs comb. nov.
Basionym: Rubidgea mackayi Tate in Q. J1 Geol.
Soc. Lond. 23: 141 (1867).
ACKNOWLEDGEMENTS
The author is grateful to Dr S. H. Haughton for
critical reading of the manuscript; to Dr B. de Winter
thanks are due for useful comments and interesting
discussions; to Dr S. Endrody-Younga for help with
£va kovacs-endrody
317
the taxonomy; to Dr A. W. Keyser for his support.
The photographs were taken by Dr R. P. Stapleton,
Dr H. C. Klinger and Mrs Ruth Fregona.
U/TTREKSEL
Die genus Rubidgea Tate van die fossiele familie
Glossopteridaceae is in 1907 gereduseer tot 'n sinoniem
van Glossopteris dear Seward. Seward se opinie word
bevestig deur die bestudering van ’n wye reeks van
blaarafdrukke afkomstig van ’n steengroef naby
Hammanskraal, Suid-Afrika. Die beste bewys hieroor
is vervat in die afdrukke van die onderste en boonste
blaaroppervlak van ’n enkele blaar op ’n gesplete
fragment van skalie. Die fyngestreepte afdruk van die
boonste blaaroppervlak kan met Rubidgea geidenti-
fiseer word, terwyl die afdruk van die onderste oppervlak
die tipiese sterk be-aring van 'n Glossopteris verteen-
woordig. Die tipe-soort van Rubidgea word oorgeplaas
na Glossopteris as G. mackayi {Tate) Kovacs comb,
nov. Die kenmerke van die boonste en onderste afdrukke
van die blaaroppervlakte van ’n aantal Glossopteris-
soorte word bespreek.
REFERENCES
Arber, E. A. N., 1905. Catalogue of the fossil plants of the
Glossopteris flora in the Department of Geology, British
Museum ( Natural History). London.
Carruthers, W., 1869. On the plant remains from the Brazilian
Coal Beds, with remarks on the genus Flemingites. Geol.
Mag. 6: 151-156.
Dana, J. D., 1849. In Wilkes's United States Exploring Expe-
dition. 10 Geology. Text and Atlas 714-20. Philadelphia
Feistmantel, O., 1876. Contribution towards the knowledge
of the fossil flora in India. Pt. I. On some fossil plants
from the Damuda Series in the Raninganj Coal-field,
collected by Mr J. Wood-Mason. J. Asiat. Soc. Beng 45
2, 4: 329-82.
Feistmantel, O., 1881. The fossil flora of Gondwana System:
The flora of the Damuda-Panchet Divisions. Mem. Geol.
Surv. India, Palaeont. indica Ser. 12,3 (3).
Kovacs-endrody, E., 1976. Notes on some Glossopteris species
from Hammanskraal (Transvaal). Palaeont. Afr. 19:
67-95.
Maheshwary, H. K., 1965. Studies on the Glossopteris flora
of India-31. Some remarks on the genus Glossopteris
Sternb. Palaeobotanist 14, 1-3: 36-45.
Maithy, P. K., 1965. Studies in the Glossopteris flora of India-
17. On the genus Rubidgea Tate. Palaeobotanist 13,1:
42-44.
Pant, D. D., 1958. The structure of some leaves and fructifi-
cation of the Glossopteris flora of Tanganyika. Bull. Br.
Mus. Nat. Hist. {Geol.) 3, 4: 127-175.
Plumstead, E. P., 1958. Further fructifications of the Glossop-
terideae and a provisional classification based on them.
Trans. Geol. Soc. S. Afr. 61 : 51-76.
Seward, A. C., 1907. Notes on fossil plants from South Africa-
Geol. Mag. N.S. Decade V, 4: 481-487.
Tate, R., 1867. On the secondary fossile from South Africa.
Q. Jl Geol. Soc. Land. 23: 140-149.
319
Book Reviews
Wild Flowers of Natal (Coastal Region) by Janet M.
Gibson. Durban : The Trustees of the Natal Publishing Trust
Fund. 1975. Pp. xix+136, 886 colour figures. Price R13,50.
Illustrated books on the flora of Natal are few. One imme-
diately thinks of Wood and Evans’s Natal Plants (1898-1912),
scientific rather than popular, Mairn Hulme’s Wild Flowers of
Natal (1954) and Winifred Wright’s Ramblers Pocket Guide:
Natal (1963). None of these works, however, can claim to have
been as acceptable to plant lovers as say Cythna Letty’s Wild
Flowers of the Transvaal (1962) and some of the books on
Cape plants. It is therefore with pleasure that one welcomes two
new illustrated works on the Natal flora both of which are
reviewed in these pages.
Wild Flowers of Natal (Coastal Region) is written and illus-
trated by Janet M. Gibson. Initially, Janet Gibson started off by
painting the Wild Flowers of the Krantzkloof Nature Reserve
near Durban, but was persuaded to enlarge the scope of her
work to include the whole of the coastal region of Natal as
defined by Ross in his Flora of Natal (1973). In all, Janet
Gibson has illustrated 810 species with 886 paintings.
The text is carried on the left-hand pages and relates to the
plants illustrated on the opposite pages. The text comprises the
family name, binomial and authority, sometimes the common
name, cross-reference to the corresponding page in Ross’s
Flora of Natal, the generic number and brief notes. The notes
are generally confined to a description of the habit of the plant,
flower colour, frequency and habitat. Up to 12 species are illus-
trated on a page.
The illustrations in colour are simple and clear, but somewhat
stylized. On the whole they tend to be flat without depth; the
figures of the Ipomoea species on Plates 85 and 86 clearly show
this. Globose fruits are given highlights, but the corresponding
shadows are often omitted (see fruits of Solanum giganteum,
Plate 92, 2). White paint has been liberally used to give the
impression of highlights but, with reproduction, the white has
blurred to give very unrealistic highlight effects (see Plates 27, 5 ;
60, lc and 77, 4). Several plants are barely recognizable, for
example Pittosporum viridiflorum (Plate 38, 1), Trema orientalis
(Plate 27, 3) and Trichilia dregeana (Plate 52, la). Janet Gibson
has used poster paint, a medium which lends itself to strong
reproduction, but does not produce the delicate and life-like
effects of water-colour. Although one may not entirely approve
of Janet Gibson’s technique, one must acknowledge that the
illustrations are effective and, after all, this is the important
thing.
Two plant names have been incorrectly spelled: Moraea
stewartae (Plate 18,3) should be M. stewartiae and Scabiosa
colombaria (Plate 104,6) should be S. columbaria. S.W. is given
as the combining author of Helichrysum herbaceum. This is a
most unusual abbreviation for Sweet. A printer’s devil has set
the “1 ” of C.B. Cl. in roman instead of italics on p. 96.
In spite of the few criticisms mentioned, the reviewer finds
this book a most useful and well-presented work — the best
available to-day on the flora of Natal and one which is good
value for money.
D. J. B. Killick
Natal Wild Flowers by Barbara Jeppe. Cape Town : Purnell.
1975. Pp. xiii+118, 56 colour plates, 25 pencil sketches. Price
R20.
This book, the second new book on the Natal flora, is written
and illustrated by Barbara Jeppe, well-known for her book on
the South African aloes and her illustrations in Trees and Shrubs
of the Witwatersrand (1964). 248 species are illustrated mainly
in colour, but a few are in pencil. Several species are illus-
trated per plate rather in the manner of Cythna Letty in Wild
Flowers of the Transvaal (1962) and Auriol Batten and Hertha
Bokelman in Wild Flowers of the Eastern Cape (1966), where
the illustrations often overlie one another making a com-
posite picture. As one would expect from an artist, who illus-
trated so exquisitely common South African weeds for Ciba-
Geigy (1975), the paintings are, on the whole, good but spoilt
by poor colour reproduction. Barbara Jeppe must have been
mortified to see such desecration of her work.
The plants are dealt with family by family. The species are
described as follows: common names in English and/or Afri-
kaans, distribution, brief morphological description in non-
technical language, flowering times, cultivation if applicable
and sometimes horticultural potential.
The identification of the species depicted cannot be faulted,
except in the case of Brunsvigia natalensis (Plate 1 la), which my
colleague, Dr R. A. Dyer, says is certainly B. undulata Leighton.
Something went wrong in her description of the family
Flacourtiaceae on p. 48. The constituent species do not all
have “attractive white flowers crowded at the ends of branch-
lets” and the family cannot be characterized by the statement
that “This shrub is a worthwhile subject as it grows well in
cultivation and is frost hard.” Obviously Barbara Jeppe was
referring to a particular species of Flacourtiaceae, whose name
was unfortunately omitted.
Typographical errors are few. The only two noticed were
Acacia Karroo (capitalization of specific epithet) on p. 52 and E.
May. instead of E. Mey. as one of the authors of Dissotis
cane see ns on p. 72.
The cover, lay-out and quality of paper used are excellent.
Unfortunately the poor colour reproduction will spoil this book
for most people. The price of R20 is high, especially if compared
with the price of Janet Gibson’s book, which covers four times
as many species.
D. J. B. Killick
Veld Plants of Southern Africa by N. K. Hobson, J. P.
Jessop, M. C. v.d. R. Ginn & Jane Kelly. Johannesburg'.
Macmillan South Africa. 1975. Pp. 310, 110 black and white
figures, 1 10 colour figures. Price R25.
The title of this book is misleading. In the foreword Professor
Brian Roberts describes the book as a significant work on our
karoo flora. In the introduction the first author, N. K. Hobson,
makes no mention of the karoo or karoo plants, but states that
the distribution of many of the plants is far flung, embracing all
four provinces. South West Africa and neighbouring states. In
his “Notes to the text” he makes frequent references to the karoo
and its plants. Also, he writes that the "plant colours are those
of specimens collected in the Pearston District”, which lies in
the karoo. In spite of the title, therefore, the book is about karoo
plants, some of which are also found outside the karoo. The
book appears to be an enlarged and de luxe successor to the
authors’ successful little book Karoo Plant Wealth (1969). The
50 karoo species included in Karoo Plant Wealth are all included
in the present work.
The various features of each of the 109 species are given
briefly in the following order: botanical name and author,
distribution, origin and meaning of the generic and specific
names, common names in English and/or Afrikaans, family
name, height, grazing value according to Hobson denoted by
1-5 stars, brief morphological description, frequency, degree
to which plant is grazed, regrowth after rain, economic uses
and, when available, palatability according to Henrici. Each
species is illustrated by means of a black and white habit sketch
and a 2x colour close-up painting. Usually four species are
illustrated in colour on a page. The book ends with a glossary
and index.
The colour illustrations by Michael Ginn are generally good,
but sometimes lacking in detail as in Plate 22. The 2x enlarge-
ments make some of the plants look grotesque (see Gasteria sp.,
Plate 2). The black and white habit sketches by Michael Ginn
and Jane Kelly are poor and, for the most part, are merely
wispy impressions of the plants depicted.
There are far too many mis-spelt plant and other names for
a book of this class. I counted eight incorrectly spelt plant
names, all appearing as captions to the colour figures. There are
annoying cases of capitalization of the first letter of the specific
epithet, for example Helichrysum Laneum on p. 170, Selago
Zeyheri on p. 226 and Walafrida Geniculata on p. 227.
In the Explanation of Scientific Name Authors, pp. 15-17,
there are several spelling mistakes. For example, Wessels Marais
should be Wessel Marais and Robert Allan Dyer should be
Robert Allen Dyer. Sheila Hooper, presently cyperologist at
Kew Herbarium, would be highly dismayed to learn that she
has been written off as of the “19th Century”.
This book contains much useful information to karoo farmers
ind the layman, but why put the book beyond the reach of
such people by producing a de luxe work costing R25. The
'easons for the high cost are obvious: the format is large (28,5 x
25,5 cm), also the print size (16 point), high quality paper has
jeen used and much space has been wasted throughout the book,
rhe misleading title of the book will undoubtedly influence
nany people, who can afford it, into buying the book. A book
m the lines of Karoo Plant Wealth would have been much more
icceptable.
Vegetation Sudosteuropas. Geobotanica Selecta, Band IV.
By I. Horvat, V. Glavac & H. Ellenberg. Stuttgart:
Gustav Fischer Verlag. 1974. Pp. xxxii + 768, 412 figures, 153
tables, 2 vegetation maps. Price DM 360 (R90).
When Horvat, who was professor in botany at Zagreb Univer-
sity, Yugoslavia, died in 1963, he left a manuscript on the general
ecological background of Southeastern Europe and piles of
notes, tables and literature references which were to have formed
320
the basis for a description of the vegetation of that vast area.
His student Glavac, who can read most of the many languages
of Southeastern Europe in which papers on the vegetation were
published, decided to continue the work of Horvat, and persua-
ded Ellenberg to help and take on the task of editing the final
manuscript. It proved to be an immense task that took nearly
eight years of hard work to complete. Glavac and Ellenberg
always try to give interpretations with which they thought Hor-
vat would have agreed. Otherwise, they give their own opinion
and Horvat’s opinion separately. Although the authors claim
that the book has become a joint effort of all three, it is inevita-
ble that the work bears the recognizable stamp of each author
particularly Ellenberg.
The book treats the vegetation of Southeastern Europe, the
Balkan peninsula south of 46° N latitude, against a background
of geographical interrelationships. After a general part in which
definitions and concepts are clarified and general ecological,
climatological, pedological and phytogeographical information
is provided, seven major vegetation zones or climax complexes,
with the communities and the ecology of each major zone, are
described in successive parts. These major zones are : ( 1 ) the ever-
green mediterranean zone; (2) the deciduous sub-mediterranean
mixed forest zone; (3) the zone of continental mixed
forest and wooded steppes (“Waldsteppe”); (4) the central
European lowland zone; (5) the montane beech forest zone;
(6) the montane and subalpine coniferous zone; and (7) the
alpine zone.
It is obvious that, despite the integration of data from a large
number of scientific publications, published in many languages
in a wide variety of journals and often difficult to obtain, a
number of generalizations had to be made in the present book.
Material from a few sites is sometimes described and presented
as being generally representative for a wide area, probably main-
ly on the basis of climatological, topographical and phytogeo-
graphical data. But even with these drawbacks, this presenta-
tion of the variety of Southeastern European vegetation types
and their ecological interpretation in one integrated and clear
text is an enormous achievement for which the authors should
be complimented.
The book contains many summarized phytosociological
tables from which differences and similarities between related
vegetation types are apparent. Photographs and diagrams
richly illustrate the text and are instructive in showing the struc-
ture of plant communities and specific ecological features. The
book has a reference list of about 1 500 publications, as well as a
species index with author’s names, an index of plant community
names, an index of geographical names and a subject index.
Two coloured vegetation maps show the vegetation zones of
the entire area at scale 1 :3 000 000, and the vegatation of the
Northwest Yugoslavian Karst area at scale 1:500 000. A very
brief summary in English explains some technicalities concern-
ing tables and species, and of community, personal and geogra-
phical names used in the book.
For anyone concerned with the vegetation of Southeastern
Europe the book will prove to be indispensable as a source of
information on general ecology and as an example of what is
possible in the field of integration and presentation of wide-
spread local data. This book should be available in every bota-
nical library.
M. J. A. Werger
Schwermetall vegetation der Erde. Geobotanica Selecta,
Band V. By W. H. O. Ernst. Stuttgart : Gustav Fischer Verlag.
1974. Pp. X+194, 45 figures, 100 tables. DM 130 (R32).
This fifth volume in Fischer’s series Geobotanica Selecta
summarizes the present knowledge on the ecology of plant
species and plant communities on heavy metal soils and des-
cribes the structure and floristic composition of the vegetation
types on these sites. Professor Ernst, who has himself worked in
Europe and in Africa on this subject, writes that so much speci-
fic knowledge on the biological consequences of heavy metals in
soils has been gathered during the past twenty years, that it
seems worthwhile to summarize it in a general form and draw
causal conclusions. Besides, there is a need for a compilation of
existing knowledge on this subject, since most of these plant
communities are rapidly disappearing because of large-scale
open pit mining.
In the first few chapters, Ernst compares figures of total
percentages of heavy metals in the soil and the amounts that
are available for plants, discusses the importance of microbial
activity in those soils, and summarizes the autecological litera-
ture on plants known to occur specifically on those soils. Experi-
ments have shown that heavy metal resistance is genetically
controlled. Ernst points out that many species described from
heavy metals sites can only be regarded as varieties and ecotypes
of widespread species. He discusses some examples of “cata-
strophic selection” in some species, leading to a rapid develop-
ment of heavy metal resistance in some populations. Resistant
populations of some other species are rather ancient, however
as must be concluded from their relic type of distribution area
After a description of succession on heavy metal soils in the
Euro-West Siberian Region and of vegetation zonation on such
sites in Europe and Africa, Ernst starts with the description of
vegetation types, which covers more than half of the book.
For description of the vegetation, Ernst follows the principles
of the Braun-Blanquet method. This allows a ready comparison
of the various vegetation types, but because it requires data
sampled in an appropriate way, Ernst must largely restrict his
descriptions to types occurring in Europe, Japan and Central
Africa, where scientists have used this method. Very limited is
the existing knowledge on species composition and structure of
vegetation types on heavy metals soils in North America, con-
tinental Asia, Australia, Polynesia and South America. Ernst
gives concise descriptions of the communities and provides notes
on their ecology and distribution area. Many phytosociological
tables are given, showing species composition and facilitating
comparison. Photographs, maps and tables illustrate the des-
criptions.
Indices of species, including author’s names, and of geogra-
phical localities quoting latitude and longitude, increase the
reference value of this book.
This book presents a valuable and fairly complete inventory
of the literature on vegetation of heavy metal soils; it summari-
zes the data and draws conclusions, but at the same time stimu-
lates further research by clearly pointing out the gaps in our
knowledge of this subject.
M. J. A. Werger
Flore et Vegetation de Madagascar. Flora et vegetatio
mundi. Band 5. By J. Koechlin, J.-L. Guillaumet & Ph.
Morat. Lehre : J. Cramer Verlag & Vaduz : A. R. Gantner
Verlag Commanditgesellschaft . 1974. Pp. xiv + 688, 29 figures, 23
maps, 188 photographs. DM 250 (R60).
The extraordinary and most interesting flora and vegetation
of the large island Madagascar, about 500 km off the coast of
Mozambique, has been well-described in the present book.
Madagascar became disconnected from the remnants of Gond-
wanaland about a hundred million years ago and has since been
isolated. This has resulted in an unusually high degree of ende-
mism in the flora (about 400 genera are endemic) and fauna.
Apart from this high degree of endemism, the flora is also extre-
mely rich, amounting to about 12 000 species of which only
a small number is not indigenous. Owing to its latitudinal
situation in the Indian Ocean and to its varied topography (the
highest point reaching 2876 m), Madagascar is characterized by
strongly contrasting environments, which bring about a great
diversity in vegetation types. Some of these vegetation types, like
the baobab forests and the thorny shrub formations dominated
by Didiereaceae, are structurally unique in the world. This
unique piece of nature is, however, severely threatened by over-
exploitation. In Madagascar the vegetation is continuously
damaged by too frequent fires and by a cattle population that
is twice as large as the already considerable human population.
To all these aspects of the environment the authors pay appro-
priate attention in the first part (four chapters) of their book.
The second part presents in eleven chapters a detailed account
of flora and vegetation. It starts with a chapter on the botanical
exploration and classical phytogeographical subdivision of
Madagascar, discussing mainly the important works of H. Per-
rier de la Bathie and H. Humbert concerning the phytogeogra-
phy of Madagascar. The vegetation is described on a structural
basis, paying much attention to the physiognomy of vegetation
formations as proposed in the Yangambi system and to growth
forms and organs of the taxa (grouped according to families)
encountered in these formations. Ten chapters successively
describe in detail the evergreen forest of lower altitudes and the
coastal forest, the dry forests of western Madagascar, the
sclerophyllous forest of middle high altitudes, the xerophilous
vegetation of south-western Madagascar, the montane forests,
the degradation stages of forest vegetation, the graminoid forma-
tions, the xerophilous rupicolous vegetation, the swamp and
fresh water vegetation, and the halophilous vegetation. Parti-
cularly the montane forests, grasslands, and rupicolous vegeta-
tion appear to have a considerable floristic affinity with corres-
ponding vegetation types in South Africa, but the rupicolous
Madagascan vegetation especially, is very much richer in pecu-
liarly formed species. The text is illustrated with instructive
drawings and structural profiles, as well as with photographs of
the various vegetation types. It is a pity that, in a book of this
standing, the photographs generally are of such poor quality.
They do not always show the characteristics of the vegetation,
are grey and without contrast, and some even appear to be not
entirely in focus. Maps show the distribution of the various
formations over the island.
The third part of the book gives a resume of the general
characters of the vegetation and flora of Madagascar. The
authors return to the theme of the degradation of the vegetation
321
on Madagascar and put forward the question of why the original
Malagasian ecosystems are so fragile. They conclude that a
changing climate and unfavourable pedological conditions are
important factors causing the fragility of the original ecosys-
tems, which through the action of man have been rapidly
destroyed. The last chapter also contains a quantitative phyto-
geographical analysis of the flora of Madagascar, and a brief
essay on speciation in Madagascar which, in some genera, is
extraordinarily large. The authors point out the favourable past
and present conditions of Madagascar allowing such an abun-
dant speciation, and conclude that Madagascar certainly
must be one of the most favourable places to study evolu-
tion in the plant kingdom. A species index citing author’s names
is added to the text.
This work is an invaluable addition to our understanding of
this interesting, but generally little-known paradise of plant
life.
M. J. A. Werger
The Flora of Swaziland by R. H. Compton. Kirstenbosch:
Trustees of the National Botanic Gardens of South Africa.
Supplementary Volume No. 1 1 to Journal of South African
Botany. 1976. Pp. 684. Price R15.
On a subcontinent with a flora as rich as that of southern
Africa regional floras are an invaluable tool to the field botanist.
Such works, however, are still very scarce in this part of the
world. Professor Compton’s magnum opus, which was published
on the 6th of August 1976, his 90th birthday, is therefore most
welcome.
The work describes about 2 118 indigenous species of flower-
ing plants which are included in 134 families and 783 genera.
Families and genera are arranged, numbered and also largely
circumscribed according to Phillips’s Genera of South African
Flowering Plants (1951). Species are presented in alphabetical
sequence in their genus. A key to families is unfortunately not
provided, but the key in Dyer’s Genera of Southern African
Flowering Plants (1975, 1976) can obviously be used. Parallel
keys, printed in 8 pt, are provided to genera and species. They
are largely artificial and make use of simple characters, and few
contrasts occupy more than a single line. No reasons are given
why parallel keys were decided on in preference to indented
ones which at a glance convey some insight into the grouping
of the taxa being dealt with. The additional space which indented
keys would have occupied could most probably have been
made up by omitting the heading given to every single key and
by setting the left margin of the species keys less far in. Occasio-
nally the reader has to choose between more than two contrasts.
This is taken to the extreme in the key to the species of Crassula
on p. 221 which is difficult to comprehend. The saving of a few
lines thus effected seems hardly justified. In the keys to genera
no reference or page number is assigned to the names of genera
to help the reader find the treatment of the genus in the text.
This is a disadvantage especially in the larger families.
As the author points out, the descriptions of families and of
genera, as well as the keys, are often partly based on those in
Phillips’s Genera and in the Manual of Flowering Plants and
Ferns of the Transvaal with Swaziland by Burtt Davy (1926,
1932). Species descriptions are newly drawn up with reference
to plants collected in Swaziland. Technical terms “with which
systematic botany is overburdened” have been avoided as far
as possible and descriptions are short and image-creating.
This is of great importance in a flora containing no illustrations.
The average species description is no longer than 50-60 words
and genus descriptions seldom exceed 100. The lack of a glossary
will probably not be noticed by anyone with some botanical
training especially as unavoidable “technicalities” in families
such as grasses and composites are explained in the family
descriptions.
Notes on the region, the habitat, flowering times and voucher
specimens with collecting localities are given for every species.
In some instances as many as 15 vouchers are cited. The reason
for this is not obvious especially as localities are not identified
in terms of districts, regions or the degree reference system. An
alphabetical list of all localities quoted in the text is provided,
but unfortunately only the altitude in metres is indicated. It
is thus difficult to form a clear picture of the distribution of a
species within the country. No reference is made to the occur-
rence outside Swaziland.
No synonyms are cited either in the text or in the index, but
a list of recently changed names, not taken up in the text, is
given as an appendix. An asterisk has been placed in the text
against each species for which an alternative name is provided
in this appendix. The meaning of the asterisk remained obscure
to the reviewer until he found the explanation in the appendix
on p. 675. No reference is made to literature or the economic
value of species and abundance is only occasionally mentioned.
Common English names are given for some families and si-
Swati names are mentioned for numerous species. No index to
common names is provided.
Prof. Compton began his botanical survey of Swaziland during
1955 Eleven years later he published his Annotated Check-list
of the Flora of Swaziland as supplementary Volume No. 6 of
the Journal of South African Botany. During the same year he
began to compile the present flora, which is largely based on
the material he collected for his check list. The author mentions
that he did not think it necessary to repeat most of the specia-
lized information in the flora. In the reviewer’s opinion it
would have been justified to repeat at least the map of the area
and the alphabetical lists of common plant names and to give
a short resume of the notes on the vegetation of Swaziland.
The work ends with an index listing only current names of
families and genera. Much attention was apparently given to
proof-reading, but more care could have been taken with abbre-
viations of author names. This is particularly evident on pp. 460
and 675. The title of the work, repeated in the top margin of
every page, could rather have been replaced by the name of the
family being dealt with on the page in question.
The Flora of Swaziland is neatly printed and well-bound,
true to the tradition of the Journal of South African Botany.
The work is warmly recommended to all serious students of
the flora of Swaziland and of regions beyond its borders. At a
price of R15 this is the “Botanists’ Bargain of the Year”.
We wish to congratulate Professor Compton on setting up
this milestone along the long road to a fuller understanding of
the southern African flora.
O. A. Leistner
A Generic Monograph of the Meliaceae by T. D. Pen-
nington & B. T. Styles. Blumea 22: 419-540 (1975).
In their introduction the authors state that, for its size, the
family Meliaceae probably contains a wider range of floral and
fruit structures than any comparable group. Further, that the
family is among the more useful to man for its high quality
timbers. There have, however, been persistent disagreements
for the past 200 years as to the number of families and genera
to be included in Meliaceae. These are very good reasons for
undertaking a thorough generic monograph of the family.
The project is divided into two main sections, the first being a
critical evaluation of earlier work and a sharp focus o i aspects
of general morphology, wood structure and pollen. The con-
clusions to be drawn from the results are clearly summarized.
The second part is a conspectus of the family as a whole, where
the circumscription of the family and the 51 genera accepted
for it is given in detail, accompanied by full references to litera-
ture and synonymy. The differential floral structures of the
genera are illustrated by clear diagramatic line drawings, which
are of a consistently high standard.
As far as the monograph concerns the genera present in
southern Africa, the two most controversial being Nymania and
Ptaeroxylon, the authors state that their results show convin-
cingly that the former is Meliaceous and that the latter must be
excluded.
In the Genera of Southern African Flowering Plants 1 :
296-299 (1975), before the present work was available, I followed
Harvey and Sonder in Flora Capensis 1: 242-243 (1860) by
giving both genera family rank, the “un-Meliaceous-like
looking” Nymania in Aitoniaceae and Ptaeroxylon in Ptaero-
xylaceae.
Now the authors of the monograph show that the character
of the pollen grains of Nymania and the structure of the secon-
dary xylem place it clearly in Meliaceae, with Turraea, also
present in southern Africa, a close relative. Nymania will
consequently be “reassigned” to Meliaceae in the Flora of
Southern Africa.
As for Ptaeroxylon, it was confirmed that it has a strong
affinity with Cedrelopsis in its pollen morphology, unlike that
of any accepted Meliaceae. Although there is apparently some
affinity with Sapindaceae and Rutaceae, the most satisfactory
solution is to give the two genera family rank as Ptaeroxylaceae.
In this decision 1 am pleased to agree, having been guided by
the treatment of the family by White & Styles in Flora Zam-
besiaca 2: 547 (1966).
The authors’ treatment of Nymania and Ptaeroxylon gives
one a feeling of confidence in the monograph as a whole.
R. A. Dyer
GUIDE FOR AUTHORS
GENERAL
Bothalia is a medium for the publication of botanical
papers dealing with the flora and vegetation of Southern
Africa. Papers submitted for publication in Bothalia should
conform to the general style and layout of recent issues of
the journal (from Vol. 1 1 onwards) and may be written in
either English or Afrikaans.
TEXT
Manuscripts should be typed, double-spaced on one side
of uniformly-sized A4 paper having at least a margin of 3 cm
all round. Latin names of plants should be underlined to
indicate italics. All other marking of the copy should be left
to the editor. Metric units are to be used throughout. Manu-
scripts should be submitted in duplicate to the Editor, Bothalia,
Private Bag XI 01, Pretoria.
ABSTRACT
A short abstract of 100-200 words preferably in both
English and Afrikaans should be provided. In the abstract
the names of new species and new combinations should not
be underlined.
FIGURES
Black and white drawings, including graphs, should be in
jet-black Indian ink preferably on bristol board. Lines should
be bold enough to stand reduction. Indicate the desired lettering
lightly in pencil: the printer will insert the final lettering. If
authors prefer to do their own lettering, then use some printing
device such as stencilling, letraset, etc. It is recommended
that drawings should be twice the size of the final reduction.
Photographs submitted should be of good quality, glossy,
sharp and of moderate, but not excessive contrast. Photograph
mosaics should be composed by the authors themselves: the
component photographs should be mounted neatly on a
white card base leaving a narrow gap between each print;
number the prints using some printing device.
Figures should be planned to fit, after reduction, into
a width of 8 cm, 11 cm or 17 cm with a maximum vertical
length of 24 cm.
The number of each figure and the author’s name should
be written on the back of the figure using a soft pencil.
Captions for figures should be collected together and typed
on a separate page headed Captions for Figures. A copy of
each caption should be attached to the base of each figure.
Do not underline plant names in captions — -only collectors’
names and numbers.
Authors should indicate in pencil in the text where they
would like their illustrations to appear.
TABLES
Tables should be set out on separate sheets and numbered
in Arabic numerals.
CITATION OF SPECIMENS
In citing specimens the grid reference system should be
used (Technical Note: Gen. 4,4c). Provinces/countries shoud
be cited in the following order: S.W. Africa, Botswana,
Transvaal, Orange Free State, Swaziland, Natal, Lesotho and
the Cape. Grid references should be cited in numerical sequence.
Locality records for specimens should preferably be given to
within a quarter-degree square. Records from the same one-
degree square are given in alphabetical order i.e. (-AC)
precedes (-AD), etc. Records from the same quarter-degree
square are arranged alphabetically according to the collectors’
names; the quarter degree references must be repeated for
each specimen cited. The following example will explain the
procedure :
Natal. — 2731 (Louwsburg): 16 km E. of Nongoma (-DD),
Pelser 354; near Dwarsrand, Van der Merwe 4789 , 2829
(Harrismith): near Groothoek (-AB), Smith 234; Koffiefontein
(-AB), Taylor 720; Cathedral Peak Forest Station (-CC),
Marriott 74; Wilgerfontein, Roux 426, Grid ref. unknown
Sterkstroom, Strydom 12.
Records from outside Southern Africa should be cited
from north to south i.e. preceding those from Southern Africa,
The abbreviation “distr.” should be added to all district
names, e.g.
Kenya. — Nairobi distr. : Nairobi plains beyond race course,
Napier 485
GIDS VIR SKRYWERS
ALGEMEEN
Bothalia is ’n medium vir die publikasie van plantkundige
artikels wat handel oor die flora van Suidelike Afrika. Artikels
wat voorgele word vir publikasie in Bothalia behoort ooreen
te stem met die algemene styl en rangskikking van onlangse
uitgawes van die tydskrif (vanaf Vol. 11). Dit mag in Engels
of in Afrikaans geskryf word.
TEKS
Manuskripte moet getik wees in dubbelspasiering slegs
op een kant van ewegroot A4 papier, met reg random 'n
rand van minstens 3 cm breed. Latynse name van plante moet
onderstreep word om aan te dui dat dit kursief gedruk moet
word. Alle ander merke moet aan die redakteur oorgelaat
word. Metrieke eenhede moet deurgaans gebruik word.
Manuskripte moet in tweevoud ingedien word by die
Redakteur, Bothalia, Privaatsak X101, Pretoria.
UITTREKSEL
'n Kort uittreksel van 100-200 woorde moet voorsien
word, verkieslik beide in Engels en Afrikaans. In die uittreksel
moet die name van nuwe soorte en nuwe kombinasies nie
onderstreep word nie.
AFBEELDINGS
Wit en swart tekeninge, insluitende grafieke, moet met
pikswart Indiese ink geteken word, verkieslik op “bristol
board”. Lyne moet dik genoeg wees om verklein te kan word.
Dui die verlangde byskrifte liggies in potlood aan: die drukker
sal die uiteindelike byskrifte invoeg. Indien skrywers verkies
om hulle eie byskrifte te maak, gebruik dan een of ander
hulpmiddels soos letraset of ’n sjabloon. Dit is wenslik dat
tekeninge tweemaal so groot as die uiteindelike verkleining
sal wees.
Fotos wat ingedien word, moet van hoe kwaliteit wees—
glansend, skerp en van matige maar nie oordrewe kontras.
Fotomosaleke moet deur die skrywer self saamgestel word:
die afsonderlike fotos moet netjies monteer word op ’n stuk
wit karton met 'n smal strokie tussen die fotos; nommer die
fotos met behulp van een of ander druk-hulpmiddel.
Afbeeldings moet so beplan word dat hulle na verkleining
sal pas in 'n breedte van 8 cm, 1 1 cm of 17 cm met ’n maksimum
vertikale lengte van 24 cm.
Die nommer van elke afbeelding sowel as die skrywer
se naam moet op die rugkant van die afbeelding geskryf word
met ’n sagte potlood.
Onderskrifte vir afbeeldings moet bymekaar getik word
op ’n afsonderlike bladsy met die opskrif Onderskrifte vir
Afbeeldings. ’n Afskrif van elke onderskrif moet aan die
onderkant van elke afbeelding vasgeheg word. Moenie plant-
name in onderskrifte onderstreep nie, slegs versamelaarsname
en -nommers.
Skrywers moet met potlood in die teks aandui waar hulle
graag hulle afbeeldings wil he.
TABELLE
Tabelle moet op afsonderlike velle papier kom en
genommer word met Arabiese nommers.
SITERING VAN EKSEMPLARE
Wanneer eksemplare siteer word, moet die ruitverwysing-
stelsel gebruik word (Tegniese Nota: Gen. 4, 4c). Provinsies/
Iande moet in die volgende volgorde siteer word: Suidwes-
Afrika. Botswana, Transvaal, Oranje-Vrystaat, Swaziland,
Natal, Lesotho en die Kaapprovinsie. Ruitverwysings moet
in numeriese volgorde siteer word. Lokaliteitsrekords vir
eksemplare moet verkieslik tot binne kwartgraadvierkante
gegee word. Rekords uit dieselfde eengraadvierkant word in
alfabetiese volgorde aangebied, nl. (-AC) kom voor (-AD)
ens. Rekords uit dieselfde kwartgraadvierkant word alfabeties
gerangskik volgens die versamelaars se name, en die kwart
graadverwysings moet herhaal word vir elke eksemplaar wat
siteer word. Die volgende voorbeeld sal die metode verduidelik:
Natal— 2731 (Louwsburg): 16 km O. van Nongoma
(-DD), Pelser 354; naby Dwarsrand, Van der Merwe 4789,
2829 (Harrismith): naby Groothoek (-AB), Smith 234; Koffie-
fontein (— AB), Taylor 720; Cathedral Peak Bosboustasie
(-CC), Marriott 74; Wilgerfontein, Roux 426; Ruitverwysing
onbekend: Sterkstroom, Strydom 12.
Rekords van buite Suidelike Afrika moet siteer word van
noord na suid, d.w.s. dit gaan die van Suidelike Afrika vooraf.
Die afkorting “distr.” behoort by alle distriksname gevoeg
te word, bv.
Kenya.— Nairobi-distr.: Nairobivlakte anderkant die ren-
baan, Napier 845.
324
REFERENCES
References in the text should be cited as follows: “Jones
(1955) stated . . or . . (Smith, 1956)” when giving a
reference simply as authority for a statement. The list of
references at the end of the article should be arranged alphabe-
tically and the literature abbreviations used should conform
to the list of Literature Abbreviations (Technical Note: Tax.
6/1) issued by the Botanical Research Institute, thus:
Hutchinson, J., 1946. A botanist in Southern Africa. London:
Gawthorn.
Morris, J. W., 1969. An ordination of the vegetation of
Ntshongweni, Natal. Bothalia 10: 89-120.
If, as in many taxonomic papers, periodicals or books
are mentioned in the text, usually in the species synopsis, they
should be cited as in the following examples: Gilg & Ben. in
Bot. Jahrb. 53: 240 (1915) and Burtt Davy, FI. Transv. 1:
122 (1926).
REPRINTS
Authors receive 75 reprints gratis. If there is more than
one author, this number will have to be shared between or
among them.
VERWYSINGS
Verwysings in die teks moet as volg siteer word: “Jones
(1955) beweer . . .” of “. . . (Smith, 1956)” wanneer ’n
verwysing slegs as outoriteit vir ’n stelling gegee word. Die
verwysingslys aan die einde van die artikel moet alfabeties
gerangskik wees en die literatuurafkortings wat gebruik word,
moet in ooreenstemming wees met die lys van Literatuur-
afkortings (Tegniese Nota: Tax. 6/1) wat uitgegee is deur die
Navorsingsinstituut vir Plantkunde, as volg:
Hutchinson, J., 1946. A botanist in Southern Africa. London:
Gawthorn.
Morris, J. W., 1969. An ordination of the vegetation of
Ntshongweni, Natal. Bothalia 10: 89-120.
Wanneer, soos in baie taksonomiese artikels die geval
is, tydskrifte of boeke in die teks genoem word, gewoonlik
in die soortsinopsis, behoort hulle siteer te word soos in die
volgende voorbeelde: Gilg & Ben. in Bot. Jahrb. 53: 240
(1915) en Burtt Davy, FI. Transv. 1 : 122 (1926).
HERDRUKKE
Skrywers ontvang 75 herdrukke gratis. Wanneer daar
meer as een skrywer is, sal hierdie aantal tussen hulle verdeel
moet word.
PUBLIKASIES VAN DIE NAVORSINGSINSTITUUT VIR PLANTKUNDE
Beskikbaar van die Afdeling Landbou-inligting. Departement van Landbou-tegniese Dienste, Privaatsak X144, Pretoria, Repubiiek
van Suid-Afrika.
FLORA VAN SUIDELIKE AFRIKA
’n Taksonomiese behandeling van die flora van die Repubiiek van Suid-Afrika, Lesotho, Swaziland en Suidwes-
Afrika.
Aanvanklik in volumes, maar in die toekoms as dele.
Reeds beskikbaar:
Vol. 1 (1966) Prys Rl,75. Oorsee: R2,20. Posvry.
Vol. 13 (1970) Prys RIO. Oorsee: R12. Posvry.
Vol. 16,1 (1975) Prys R13,50. Oorsee: R16,75. Pos vry.
Vol. 26 (1963). Prys R4,60. Oorsee: R5,75. Posvry.
DIE BLOMPLANTE VAN AFRIKA
Hierdie publikasie word uitgegee as ’n gei'llustreerde reeks, baie na die aard van Curtis se “Botanical Magazine”. Die
doel van die werk is om die skoonheid en variasie van vorm van die flora van Afrika aan die leser bekend te stel, om
belangstelling in die studie en kweek van die inheemse plante op te wek, en om plantkunde in die algemeen te bevorder.
Die meeste van die illustrasies word deur kunstenaars van die Navorsingsinstituut vir Plantkunde gemaak, dog die
redakteur verwelkom geskikte bydraes van ’n wetenskaplike en kunsstandaard afkomstig van verwante inrigtings.
Onder huidige omstandighede word twee dele van die werk gelyktydig gepubliseer, maar met onreelmatige tussenpose;
elke deel bevat 10 kleurplate. Intekengeld bedra R1 ,50 per deel: 4 dele per band. Vanaf Band 27 is die prys per band
in linne gebind RIO, 00; in moroccoleer gebind R14,00.
BOTHALIA
Bothalia is ’n medium vir die publikasie van plantkundige artikels oor die flora en plantegroei van Suidelike Afrika.
Een of twee dele van die tydskrif word jaarliks gepubliseer.
Die volgende dele is beskikbaar:
Vol. 3 Deel 1 Uit druk
2 1937 75c
3 1938 75c
4 1939 75c
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2 1971 R3
3 1971 R3
4 1972 R3
Vol 11 No. 1 & 2 1973 R6
3 1974 R3
4 1975 R3
Vol. 12 No. 1 1976 R5
MEMOIRS VAN DIE BOTANIESE OPNAME VAN SUID-AFRIKA
Die memoirs is individuele verhandelings, gewoonlik ekologies van aard, maar soms handel dit oor taksonomiese
of ekonomiese-plantkundige onderwerpe. Een-en-veertig nommers is reeds gepubliseer waarvan sommige uit druk is.
BOTHALIA
VOL. 12, No. 2 APRIL 19'
CONTENTS— INHOUD
Page
Bladsy
1. Hans Justus Thode (1859-1932), pioneer plant collector in the Natal Drakensberg. D. J. B.
Killick 169
2. The South African species of Teucrium (Lamiaceae). L. E. Codd 177
3. A note on the Stachys aet/iiopica Complex. L. E. Codd 181
4. New taxa and a new combination in the genus Cotyledon. H. R. Tolken 191
5. The identity of Erica flavisepala. E. G. H. Oliver 195
6. The identity of Eriosema nanum. C. H. Stirton 199
7. Morphological studies of the Ochnaceae. P. C. V. du Toit 205
8. Leaf anatomy of the South African Danthonieae (Poaceae). I. The genus Dregeochloa. R. P.
Ellis 209
9. Cytogenetic studies in the Eragrostis curvula Complex. T. B. Vorster and H. Liebenberg 215
10. A note on the flowers of Halleria lucida. C. H. Stirton 223
11. The pollination of Canavalia virosa. C. H. Stirton 225
12. Broad-spectrum pollination of Plectranthus neochilus. C. H. Stirton 229
13. Freshwater algae of Southern Africa. II. Triplastrum stipulosum from the Transvaal. M. Isabella
Claassen 231
14. Freshwater algae of Southern Africa. IV. Some Micrasteriae from Rhodesia, including a new
species. M. Isabella Claassen 239
15. Asexual nuclear division in Neocosmospora. K. T. van Warmelo 247
16. Notes on African plants:
Araceae. A. A. Obermeyer 251
Asclepiadaceae. R. A. Dyer 253
Cyperaceae. P. Vorster 257
Fabaceae. J. H. Ross 257
Frullaniaceae. P. Vorster 257
Poaceae. P. C. V. du Toit 258
Ranunculaceae. D. J. B. Killick 258
Rutaceae. J. H. Ross 258
Selaginellaceae. P. Vorster 259
Thelypteridaceae. P. Vorster 260
17. World climatic patterns in grassland and savanna and their relation to growing seasons. R. Kirk
Steinhorst and J. W. Morris 261
18. Automatic classification of the highveld grassland of Lichtenburg, south-western Transvaal.
J. W. Morris 267
19. Cape Hangklip area. 1. The application of association analysis, homogeneity functions and Braun-
Blanquet techniques in the description of south-western Cape vegetation. C. Boucher 293
20. A preliminary account of aerial plant biomass in fynbos communities of the mediterranean type
climate zone of the Cape Province. F. J. Kruger 301
21. Silene dewinteri, a new species of the Caryophyllaceae from the south-western Cape.
G. Bocquet 309
22. The taxonomic status of the genus Rubidgea. Eva Kovacs-Endrody 313
Book reviews 319
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