ISSN 0006 8241 = Bothalia
Bothalia
’N TYDSKRIF VIR PLANTKUNDIGE NAVORSING
A JOURNAL OF BOTANICAL RESEARCH
Vol. 23,1
May/Mei 1993
PUBLICATIONS OF THE NATIONAL BOTANICAL INSTITUTE, PRETORIA
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BOTH A LI A
Bothalia is named in honour of General Louis Botha, first Premier
and Minister of Agriculture of the Union of South Africa. This
house journal of the National Botanical Institute, Pretoria, is devoted to
the furtherance of botanical science. The main fields covered are
taxonomy, ecology, anatomy and cytology. Two parts of the journal
and an index to contents, authors and subjects are published
annually.
Verkrygbaar van die Nasionale Botaniese Instituut, Privaatsak X101,
Pretoria 0001, Republiek van Suid-Afrika. ’n Katalogus van alle beskik-
bare publikasies kan aangevra word.
Bothalia is vemoem ter ere van Generaal Louis Botha, eerste Eerste
Minister en Minister van Landbou van die Unie van Suid-Afrika. Hierdie
lyfblad van die Nasionale Botaniese Instituut, Pretoria, is gewy aan die
bevordering van die wetenskap van plantkunde. Die hoofgebiede wat gedek
word, is taksonomie, ekologie, anatomie en sitologie. Twee dele van die
tydskrif en ’n indeks van die inhoud, outeurs en onderwerpe verskyn
jaarliks.
MEMOIRS OF THE BOTANICAL SURVEY OF SOUTH AFRICA
MEMOIRS VAN DIE BOTANIESE OPNAME VAN SUID-AFRIKA
The memoirs are individual treatises usually of an ecological nature, ’n Reeks van losstaande omvattende verhandelings oor vemaamlik
but sometimes dealing with taxonomy or economic botany. ekologiese, maar soms ook taksonomiese of plantekonomiese onderwerpe.
THE FLOWERING PLANTS OF AFRICA / DIE BLOMPLANTE VAN AFRIKA
This serial presents colour plates of African plants with accompanying
text. The plates are prepared mainly by the artists at the National Botanical
Institute. Many well known botanical artists have contributed to the series,
such as Cythna Letty (over 700 plates), Kathleen Lansdell, Stella Gower,
Betty Connell, Peter Bally and Fay Anderson. The Editor is pleased to
receive living plants of general interest or of economic value for
illustration.
From Vol. 50, one part of twenty plates is published annually. A volume
consists of two parts. The publication is available in English and Afrikaans.
Hierdie reeks bied kleurplate van Afrikaanse plante met bygaande teks.
Die skilderye word meestal deur die kunstenaars van die Nasionale
Botaniese Instituut voorberei. Talle bekende botaniese kunstenaars het
tot die reeks bygedra, soos Cythna Letty (meer as 700 plate), Kathleen
Lansdell, Stella Gower, Betty Connell, Peter Bally en Fay Anderson.
Die Redakteur verwelkom lewende plante van algemene belang of
ekonomiese waarde vir afbeelding.
Vanaf Vol. 50 word een deel, bestaande uit twintig plate, jaarliks
gepubliseer. ’n Volume bestaan uit twee dele. Die publikasie is beskikbaar
in Afrikaans en Engels.
FLORA OF SOUTHERN AFRICA / FLORA VAN SUIDELIKE AFRIKA
A taxonomic treatise on the flora of the Republic of South Africa,
Ciskei, Transkei, Lesotho, Swaziland, Bophuthatswana, Namibia,
Botswana and Venda. The FSA contains descriptions of families, genera,
species, infraspecific taxa, keys to genera and species, synonymy, literature
and limited specimen citations, as well as taxonomic and ecological
notes.
’n Taksonomiese verhandeling oor die flora van die Republiek van Suid-
Afrika, Ciskei, Transkei, Lesotho, Swaziland, Bophuthatswana, Namibie,
Botswana en Venda. Die FSA bevat beskrywings van families, genusse,
spesies, infraspesifieke taksons, sleutels tot genusse enspesies, sinonimie,
literatuur, verwysings na enkele eksemplare, asook beknopte taksonomiese
en ekologiese aantekeninge.
PALAEOFLORA OF SOUTHERN AFRICA / PALAEOFLORA VAN SUIDELIKE AFRIKA
A palaeoflora on a pattern comparable to that of the Flora of
southern Africa. Much of the information is presented in the form
of tables and photographic plates depicting fossil populations. Now
available:
’n Palaeoflora met ’n uitleg vergelykbaar met die van die Flora van suide-
like Afrika. Baie van die inligting word aangebied in die vorm van tabelle
en fotografiese plate waarop fossiele populasies afgebeeld word. Reeds
beskikbaar:
Molteno Formation (Triassic) Vol. 1. Introduction. Dicroidium , by/deur J.M. & H.M. Anderson.
Molteno Formation (Triassic) Vol. 2. Gymnosperms (excluding Dicroidium), by/deur J.M. & H.M. Anderson.
Prodromus of South African Megafloras. Devonian to Lower Cretaceous, by/deur J.M. & H.M. Anderson.
Obtainable from/Beskikbaar van: A. A. Balkema Marketing, Box/POsbus 317, Claremont 7735, RSA.
BOTHALIA
N TYDSKRIF VIR PLANT KUNDIGE NAVORSING
A JOURNAL OF BOTANICAL RESEARCH
Volume 23,1
Scientific Editor/Wetenskaplike Redakteur: O.A. Leistner
Technical Editor/Tegniese Redakteur B.A. Momberg
NATIONAL
INSTITUTE
2 Cussonia Avenue, Brummeria, Pretoria
Private Bag XI01, Pretoria 0001
ISSN 0006 8241
. -G5- i 1
Privaateak X101 PRETORIA 00'v
national botanical.
INSTITUTE
J
1993
Editorial Board/Redaksieraad
D.E Cutler
B.J. Huntley
P.H. Raven
J.P. Rourke
M.J. Werger
Royal Botanic Gardens, Kew, UK
National Botanical Institute, Cape Town, RSA
Missouri Botanical Garden, St Louis, USA
Compton Herbarium, NBI, Cape Town, RSA
University of Utrecht, Utrecht, Netherlands
Editorial Committee
Redaksiekomitee
O.A. Leistner
B.A. Momberg
M.C. Rutherford
CONTENTS — INHOUI)
Volume 23,1
1 . Studies in the Ericoideae (Ericaceae). XU. The placing of the genus Blaeria into synonymy under Erica ;
nomenclatural and taxonomic changes for the southern African region. E.G.H. OLIVER 1
2 . Studies in the Ericoideae (Ericaceae). Xm.. Three new species of Erica from the southwestern Cape.
E.G.H. OLIVER 9
3. The hepatics, Symphyogyna podophylla and Pallavicinia lyellii (Pallaviciniaceae) in southern Africa.
S.M. PEROLD 15
4. A biosystematic study of Pentameris (Arundineae, Poaceae). N.P. BARKER 25
5 . Studies in the Marchantiales (Hepaticae) from southern Africa. 1. The genus Dumortiera and D. hirsu-
ta; the genus Lunularia and L. cruciata. S.M. PEROLD 49
6. Panicum simulans (Paniceae, Poaceae), a new species from southern Africa and its leaf anatomy. L.
SMOOK and R.P. ELLIS 59
7. Notes on African plants:
Allisoniaceae. The hepatic, Calycularia crispula (Metzgeriales) reported from Malawi and
Zambia. S.M. PEROLD 79
Asteraceae. An evaluation of Hutchinson’s ‘beetle-daisy’ hypothesis. J.J. MIDGLEY 70
Fabaceae. Vigna kokii, a new species from southern Africa. BJ. PIENAAR 68
Fabaceae. Notes on the genus Argyrolobium (Crotalarieae) including a new species from southern
Africa. T.J. EDWARDS 77
Oxalidaceae. A new species of Oxalis from the western Cape. E.G.H. OLIVER 72
Pteridophyta— Adiantaceae. A new cytotype for Acrostichum aureum. J.P. ROUX 75
Rosaceae. Observations on Cliffortia micrantha. A.C. FELLINGHAM 65
Rosaceae. Cliffortia fasciculata, a superfluous name for C. amplexistipula. A.C. FELLINGHAM 67
8. First report on the presence of Enterobryus species (Trichomycetes: Eccrinales) in South Africa and
the description of three new species. G.J.M.A. GORTER 85
9. Mycorrhizal status of plants growing in the Cape Floristic Region, South Africa. N. ALLSOPP and
W.D. STOCK 91
10. Pollen morphology of Curroria, Mondia, Socotranthus and Stomatostemma (Periplocaceae) . R.L.
VERHOEVEN and H.J.T. VENTER 105
11. Dynamics of the forest vegetation of the Umtiza Nature Reserve, East London. J.J. MIDGLEY and
P.N. GOBETZ Ill
12 .The vegetation of the northeastern Orange Free State, South Africa: physical environment and plant
communities of the Ea land type. H.C. ECKHARDT, N. VAN ROOYEN and G.J. BREDEN-
KAMP 117
13 . The vegetation of the southern Langeberg, Cape Province. 1. The plant communities of the Boosmans-
bos Wilderness Area. D.J. MCDONALD 129
14. The vegetation of the southern Langeberg, Cape Province. 2. The plant communities of the Marloth
Nature Reserve. D.J. MCDONALD 153
Digitized by the Internet Archive
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https://archive.org/details/bothaliavolume2323unse
Bothalia 23,1: 1-7 (1993)
Studies in the Ericoideae (Ericaceae). XII. The placing of the genus
Blaeria into synonymy under Erica ; nomenclatural and taxonomic
changes for the southern African region
E.G.H. OLIVER*
Keywords: Blaeria, Erica, nomenclature, southern Africa, taxonomy
ABSTRACT
The reduction of the genus Blaeria to synonymy under Erica requires the publication of six new combinations and three
new names for the nine taxa occurring in southern Africa. Four species are reduced to synonymy. Diagnostic features and
distribution maps are provided.
UITTREKSEL
Die plasing van die genus Blaeria in sinonimie onder Erica vereis die publisering van ses nuwe kombinasies en drie nuwe
name vir die nege taksons wat in suidelike Afrika voorkom. Vier spesies word in sinonimie geplaas. Diagnostiese kenmerke
en verspreidingskaarte word voorsien.
INTRODUCTION
In a forthcoming paper (Oliver in press A) the generic
relationship between Blaeria L. and Erica L. will be
discussed in detail. The former genus has been maintained
separate from Erica since 1753 on the single character
difference of four as opposed to eight stamens.
Problems arose with several species in both genera
having a variable number of stamens or even numbers not
included within the circumscription of their genera.
Depending on the stamen complement found in the flowers
examined, one could identify some material as either
belonging to Blaeria or to Erica. Problem species in this
respect are Erica filiformis Salisb., E. esterhuyseniae
Compton and E. pleiotricha S. Moore in which 8- and
4-stamened flowers exist. In several other species the
stamen number varies from 5 to 8.
With the sinking of the genus Philippia into Erica
(Oliver 1987a, 1988, 1989) several additional species from
tropical Africa having variable numbers of stamens were
introduced into the problem. These are: E. rryassana (Aim
& Fries) E.G.H. Oliver with only 4 stamens, very occa-
sionally 5; E. hexandra (S. Moore) E.G.H. Oliver with
6, but 7 or 8 in some or all flowers; E. mannii (Hook,
f.) Beentje has 6 stamens but with 5, 7 or 8 in some
flowers. Several Madagascan species, not yet transferred
to Erica, have also compounded the problem; Philippia
humbertii H. Perrier with 3 or 4 stamens, sometimes 6
and P gracilis (Benth.) H. Perrier with 4-8 stamens.
The genus Blaeria contains approximately 16 species,
all occurring in Africa. In the southern African region the
nine species are confined to the Cape. They can be placed
in several groups of related species, with each group
showing more affinities to different sections within Erica
* Stellenbosch Herbarium, National Botanical Institute, P.O. Box 471,
Stellenbosch 7599.
MS. received: 1992-06-09.
than to the other groups within Blaeria, including those
from tropical Africa.
It is postulated (Oliver in press A) that Blaeria is an
unnatural genus with clear indications of being poly-
phyletic. On the grounds of polyphylesis and the complete
transition between the two genera in the only differentiat-
ing character in certain species, it was decided to reduce
the genus Blaeria to synonymy under Erica. This decision
is formalised in this paper for the species occurring in the
southern African region. At this stage it is not possible
to deal with the nomenclatural changes necessary for the
tropical African species because of the instability of their
taxonomy and of several nomenclatural synonyms within
Erica.
1. Erica barbigeroides E.G.H. Oliver, nom. nov.
Blaeria revoluta Bartl.: 650 (1832), non Erica revoluta (H. Bol.) L.E.
Davidson (1985); Klotzsch: 663 (1833); Klotzsch: 222 (1838); Benth.:
698 (1839); N.E. Br.: 326 (1905). Blairia revoluta (Bartl.) Dietr.: 444
(1839). Type: Kleinriviersbergen, Ecklon s.n. (Bt, holo.; S!). Lectotype
chosen here: Ecklon s.n. [det. Bartl.] (S).
Blaeria barbigera sensu Aim & Fries: 235 (1924); Bond & Goldblatt:
239 (1984); Oliver: 145 (1987b).
This very distinct species was referred to as Blaeria
barbigera based only on the assumption that the material
fitted the description of Salisbury’s Erica barbigera (1802),
there being no extant type specimen. For further details
see below under Insufficiently known species.
The new name is an adaptation of the name by which
this well-known species of the coastal regions of the
Caledon District has been known for many years.
The species is confined to sandy level areas that are often
wet in winter in the coastal region of the southwestern Cape
from Rooi Els in the west to Sondagskloof (Sandies Glen)
near Napier in the east (Figure 1). In this region it may
be found from just above the spray zone near the sea up
to an altitude of 760 m on the nearby mountains.
2
18" 19° 20° 21°
20 0 20 40 60 80 100 km
FIGURE 1. — The known distribution of Erica barbigeroides.
E. barbigeroides forms sparsely branched, virgate
shrublets up to 400 mm tall, is covered with numerous
long hairs and has up to 24 flowers grouped together
in closely packed heads at ends of branches. Heads
often partially pendent. Flowers somewhat sticky due to
secretion of viscid matter from sessile glands on margins
of sepals.
It is allied to two other species mentioned here, E.
ericoides and E. russakiana, both of which occur in the
same area near Hermanus, but never grow together. Both
of the latter species form many-branched shrublets and are
smaller in all parts of the inflorescence and flower.
Vouchers: Ecklon & Zeyher 260 [loc. 58.8] (BOL, G, MO, S, SAM,
W); Ecklon <6 Zeyher s.n. [loc. 58.8] (K, LD, P, UPS, W, Z); Oliver
& Palser 83 (E, MEL, NY, PRE, STE); Schlechter 95U (BM, BOL,
G, K, MO, PRE, STE, W, Z). 70 other collections examined.
2. Erica equisetifolia Salisb. in Transactions of the
Linnean Society 6: 342 (1802). Type: locality & collector
unknown, Herb. Salisb. (K, holo.!).
Blaeria equisetifolia (Salisb.) G. Don: 805 (1834); Aim & Fries: 239
(1924); Salter: 658 (1950); Bond & Goldblatt: 239 (1984); Oliver: 145
(1987).
B. purpurea L. f.: 122 (1782) nom. illegit. non Berg. (1767) [= Simo-
cheilus purpureus (Berg.) Druce]; Thunb.: 8 (1802); Klotzsch: 221 (1838);
N.E. Br. : 323 (1905); Aim & Fries: 239 (1924) pro parte. Type: Thunberg
s.n. (UPS, holo.!).
B. dumosa Wendl.: t .38 (1808); Roem. & Schult.: 170 (1818); G. Don:
805 (1834); N.E. Br.: 323 (1905), synon. nov. Type: Wendl.: t.38.
B. dumosa var. breviflora N.E. Br.: 323 (1905), synon. nov. Syntypes:
Caledon Div., mountains near Genadendal, Bolus 5419 (BOL!, K!, PRE!)
and in Herb. Norm 613 (K!); ibid. Guthrie 3140 (?); without locality,
Drege s.n. (K!) .
B. campanulata Benth,: 698 (1839); N.E.'Br. : 324 (1905), synon. nov.
Syntypes: Cape, Drige s.n. (?); Burchell 7693 (K!); Burchell 7773 (K!,
P!, W!).
B. flava H. Bol.: 239 (1894); N.E. Br.: 322 (1905), synon. nov. Syn-
types: Zwartberg near Caledon, Jan. 1885, 800 m, Bolus 5147 (BOL!,
Bothalia 23,1 (1993)
K!, PRE!, STE!) & sub Herb. Norm. 611 (BM!, BOL!, G!, NH!, P!,
PRE!, SAM!, UPS!, W!).
Erica parvula Guth. & Bol.: 171 (1904), synon. nov. Type: Stellenbosch
Div. ; on a rock near the mouth of the Steenbrass River, 20—30 ft. above
the sea, Guthrie 3710 (BOL, holo.!).
Blaeria oppositifolia L. Guthrie: 21 (1928), synon. nov. Type: Hotten-
tots Holland Mountains, Jan. 1924, Stokoe in BOL 17674 (BOL, holo.!,
K!).
Common and widespread in mountains of southwestern
Cape from Cape Peninsula to Bain’s Kloof in north to
western part of Bredasdorp District in south and occurs
from sea level to summits of mountains at 1 600 m (Figure
2). Highly variable species in habit, flower size and shape,
anther form and in having some collections with more than
usual number of four stamens.
Basic type forms rounded low shrublet with deep pink,
narrowly tubular flowers with four dark brown, exserted
anthers. In some cases, mainly at lower altitudes, plants
can be erect and reach 500 mm in height when growing
in old fynbos. Flowers may be short with corolla 2.5 mm
long and open campanulate to large with corolla 4 mm
long and tubular.
Several species formerly recognised as distinct have been
reduced to synonymy under E. equisetifolia on the grounds
of overlap in characters caused by the variation found in
the numerous collections of this complex. E. equisetifolia
and Blaeria dumosa were distinguished on the single
character of anther shape, the former having straight-sided
anthers whereas the latter had anthers that were obtriangu-
lar in outline with a constriction above the decurrent
appendages. The straight-sided collections come mostly
from the Cape Peninsula and the other material from the
inland mountains. There are collections from the main-
land which fit equally well in either of the two species.
Salisbury’s type is a small branchlet with ‘Equisetifolia
MS’ written in his own hand. It possesses six flowers with
only a single stamen remaining. From this stamen it is
Bothalia 23,1 (1993)
3
seen that the anther is the straight-sided form, most
probably from the Cape Peninsula, and that there is only
one small awn on one side.
Blaeria flava was described by Bolus on the grounds
of the yellow colour of the corolla. This would appear to
be the only character showing any discontinuity in this
complex which has only pink or white flowers. The species
is known only from the original collection from the
Swartberg at Caledon where no pink- or white-flowered
collections have been made. A thorough investigation of
the Swartberg may produce more evidence for assigning
this material some taxonomic status.
The problem of the similarity between E. equisetifolia,
Blaeria camparullata and E. parvula is mentioned (Oliver
in press A) as a case for reducing Blaeria to synonymy
under Erica.
B. campanulata was based on material collected from
rock ledges on the cool, southeast side of the top of the
mountains of Baviaanskloof above Genadendal from where
it is known through only a few collections. Plants are small
and very compact, the white flowers have exserted dark
stamens which range from 5—8 per flower and mostly
3-locular ovaries ( Oliver 8978 & 9081). A recent collec-
tion ( Oliver 8813 ) with only 8-stamened flowers has been
made on the lowest dry northern slopes near McGregor.
This material, in turn, was found to be morphologically
inseparable from E. parvula which is confined to the
Elgin/Betty’s Bay area near the coast. This latter species
also forms compact woody shrublets with white flowers.
It grows mostly on rocks in streambeds. Apart from the
more variable number of stamens and ovary locules the
material of these two species is indistinguishable. There
could, however, be some purpose in recognizing the high
altitude form from Baviaanskloof as a subspecies. This
will need some further investigations and assessment.
Several new species from the Kogelberg and Hermanus
areas that are closely allied to this species are being
described separately (Oliver 1993). One of these is re-
corded as producing a putative natural hybrid with E.
equisetifolia .
An anomalous form with mostly opposite leaves was col-
lected by Stokoe somewhere in the Hottentots-Holland
Mountains. Sometimes one can find an occasional 2-nate
arrangement of leaves on a branchlet in E. equisetifolia,
and in other species, such as the E. tenuifolia L.IE. lutea
Berg, complex, whole branchlets or even branches can
have 2-nate leaves. This condition alone is not regarded
as sufficiently distinct to warrant taxonomic recognition,
especially as it is known only from a single small collec-
tion that cannot be relocated in the field.
Vouchers: Bolus 5420 (BOL, K, LD, NBG, PRE, STE, W); Burchell
7773 (K, P, W); Oliver 8813 (BM , BOL, E, G, MO, MEL, NY, P, PRE,
S, STE, UPS, W); Oliver 9081 (E, MEL, PRE, STE); Schlechter 9639
(BM, BOL, E, G, K, MO, P, PRE, STE, W); Schlechter 10265 (BM,
E, K, MO, P, PRE, S, STE, W); Schlechter 10339 (BM, G, K, MO,
P, PRE, S, W); Sieber 165 (G, G-DC, K, LD, M, MO, P, PRE, S, W).
200 other collections studied.
3. Erica ericoides (L.) E.G.H. Oliver, comb. nov.
Blaeria ericoides L., Species plantarum 1: 112 (1753); L.: 331 (1771);
Willd.: 629 (1798); Thunb.: 7 (1802); Wendl.: 73 (1808); Ait.: 248 (1810);
Roem. & Schult.: 168 (1818); Bartl.: 649 (1832); Klotzsch: 663 (1833);
G. Don: 804 (1834); Klotzsch: 222 (1838); Benth.: 698 (1839); Rach:
788 (1853); N.E. Br.: 325 (1905); Aim & Fries: 233 (1924); Salter: 658
(1950); Bond & Goldblatt: 239 (1984); Oliver: 145 (1987). E. blaeria
Thunb.: 72 (1794); Thunb.: 358 (1823). E. dumosa Salisb.: 296 (1796);
Salisb.: 341 (1802). Lectotype: Hermann s.n. in Hermann Herbarium
vol. 4 fol. 61 (BM, STE, photo!), selected by Oliver (in press B).
Blaeria affinis N.E. Br. : 325 (1905). Type: Caledon Div., mountains
near Vogel Gat, near the mouth of the Klein River, 1500 ft., Schlechter
10418 (K, holo. ! ; BM!, BOL!, P!, PRE!).
This species, the type of Linnaeus’ genus Blaeria, is
very common in dry rocky areas on flats or in the moun-
tains from the Cape Peninsula eastwards along the coast
to just beyond Stanford (Figure 3). In some areas it forms
dominant stands which are very evident due to the strong
honeylike scent emitted by the flowers.
E. ericoides is a very distinct species which is often con-
fused with species from some of the minor genera, namely
Sympieza labialis (Salisb.) Druce, Simocheilus purpu-
reus (Berg.) Druce and Syndesmanthus articulatus (L.)
Klotzsch, all of which have similar looking heads of pale
pink tubular flowers with exserted dark brown anthers. The
Erica can be easily identified by its 4-celled multi-ovuled
ovary which produces a dehiscent capsular fruit.
Aim & Fries correctly placed Brown’s B. affinis in
synonymy under this species. The species was based on
the smaller flowerheads and finer branches of a single
collection from the Hermanus area. The numerous
collections of E. ericoides show a range of variation which
includes this slighter form.
E. ericoides is allied to E. russakiana and to a lesser
extent E. barbigeroides (q.v.).
The typification of E. ericoides is being formalised in
conjunction with R.F. Barrie (BM) for the programme on
the typification of Linnaean taxa (Oliver in press B).
Vouchers: Schlechter 7554 (BM, E, G, K, MO, P, PRE, STE, UPS,
W, Z); Schlechter 10401 (BM, BOL, E, G, K, MO, P, PRE, S, STE,
FIGURE 3. — The known distribution of Erica ericoides.
4
Bothalia 23,1 (1993)
FIGURE 4. — The known distribution of Erica fuscescens, # ; E. klotzschii , O; and E. multiflexuosa , ▲.
UPS, W); Sieber 172 (G-DC, K, LD, M, MO, P, S, STE, W). 170 other
collections examined.
4. Erica fuscescens (Klotzsch) E.G.H. Oliver, comb.
nov.
Blaeria fuscescens Klotzsch: 657 (1833); Benth.: 697 (1839); N.E. Br.:
321 (1905) pro parte excl. synonym Erica sagittate Klotzsch ex Benth.;
Aim & Fries: 239 (1924). Blairia fuscescens Dietr.: 443 (1839). Type:
Cape of Good Hope, Mundt & Maire s.n. (Bf, holo.; E!, G!, K!, P!,
W!). Lectotype chosen here: Mundt & Maire s.n. [det. Klotzsch] (P!).
This species is common on the southern slopes of the
Outeniqua and Tzitzikama Mountains in the southern Cape
(Figure 4). It has also been recorded from the Van Stadens
Mountains where it is sympatric with the closely related
E. sagittata (see below), but does not, as far as I am aware,
grow together with it. The numerous white flowers with
exserted black anthers make this a very striking plant. The
plants are bushy and fairly large, up to 1.5 m tall, whereas
in E. sagittata they are much smaller and sparser with
more crowded flowers due to the different inflorescence
type.
Vouchers: Burchell 5910 (BOL, K, P, UPS); Fourcade 831 (BOL, K,
STE, Z); Galpin 3717 (BOL, K, PRE, SAM); Mundt & Maire s.n. (E,
G, K, P, W) [ex B, det. Klotzsch]; Oliver 9250 (PRE, STE). 65 other
collections examined.
5. Erica klotzschii (Aim & Fries) E.G.H. Oliver,
comb. nov.
Blaeria klotzschii Aim & Fries: 237 (1924). Type: Cape of Good Hope
Lichtenstein s.n. (B|, holo.; S fragm.!). B. pusilla Klotzsch: 659 (1833)
nom. illegit. non Blaeria pusilla L.: 39 (1767) [= Simocheilus purpureus
(Berg.) Druce], non Erica pusilla Thunb.: 70 (1794), non Erica pusilla
Salisb. : 374 (1802); Benth.: 698 (1839); N.E. Br.: 322 (1905). Lecto-
type chosen here: Lichtenstein s.n. (S!).
E. klotzschii was rather anomalous in the genus Blaeria
as it had no close relatives and possessed only a superficial
resemblance to E. longimontana [— B. coccinea ]. The
flowers are very small and are borne at the ends of most
lateral branches on the plant thus producing plants almost
completely covered by pale pink to dull cream flowers.
The anthers are relatively large, exserted and slightly
versatile. This fact coupled with the dull colour of the
corolla, the small size of the flower and the far-exserted
cyathiform stigma strongly suggest wind pollination in
this species. This was substantiated in populations near
Swellendam in which plants gave off clouds of pollen when
disturbed early in the morning.
The species occurs on dry shaley hills and slopes at the
base of mountains from Elim to Swellendam and eastwards
as far as Albertinia often associated with Renosterveld
vegetation (Figure 4).
Vouchers: Bolus 8461 (BM, BOL, K, UPS); Oliver 4297 (BM, PRE,
STE); Zeyher 3331 (BOL, GRA, K, P, PRE, S, SAM, W, Z). 40 other
collections examined.
6. Erica longimontana E.G.H. Oliver, nom. nov.
Blaeria coccinea Klotzsch: 657 (1833), non Erica coccinea L. (1753);
Benth.: 697 (1839); N.E. Br.: 321 (1905); Aim & Fries: 236 (1924). Type:
Cape of Good Hope, Mundt & Maire s.n. (Bf, holo.; K!— BOL, fragm.!,
S! , W!). Lectotype chosen here: Mundt & Maire s.n. [ex B & det.
Klotzsch] (K!).
B. fastigiata Benth. : 697 (1839), non E. fastigiata L. (1771); N.E. Br. :
321 (1905). Type: Cape Colony, Burchell 7331 (K, holo.!; S!).
This species is common along the southern slopes of
the Langeberg from Swellendam to the western Outeni-
qua Mountains at the Robinson’s Pass (Figure 5) where
it is often dominant in seepage zones, hence the new name
chosen for the species.
Aim & Fries were correct in reducing Bentham’s B.
fastigiata to synonymy. This latter species was separated
off on the grounds of having only finely puberulous parts.
This form is found in the Swellendam area were it co-exists
with the form with longer hairs.
Vouchers: Oliver 9106 (BM, E, K, MEL, MO, NY, P, PRE, STE);
Schlechter 2055 (BM, BOL, G, K, PRE, S, UPS). 42 other collections
examined.
7. Erica multiflexuosa E.G.H. Oliver, nom. nov.
Blaeria flexuosa Benth.: 698 (1839), non E. flexuosa Andr. (1798);
N.E. Br.: 324 (1905). Type: at Steenbrass River, prov. Stellenbosch, Niven
s.n. (Herb Lambert; G-DC!). Lectotype chosen here: Niven 6 (Herb.
Lambert in K!).
B. purpurea Aim & Fries: 239 (1924) pro parte.
This species is confined to a small area on the lower
northern slopes of the Kogelberg complex around the
Steenbras Dam (Figure 4) where it grows in open sandy
areas between low restiad clumps. It forms low rounded
Bothalia 23,1 (1993)
5
but sparse shrublets with very intertwined branches which
are sparsely leafy. The flowers are a dull cream colour
and, hanging downwards, are rather inconspicuous.
E. multiflexuosa belongs to the E. equisetifolia complex
but can be distinguished by its intertwined branches, its
obovoid, dull cream, pendent flowers and included
muticous yellow-brown anthers. Like other species of the
complex it can have opposite leaves on some branches.
Brown (1905) was somewhat confused about this species
because he cited Niven 6 &. 7, both from the Steenbrass
River, under Blaeria flava and Niven 6 also under Blaeria
flexuosa.
Specimens examined
CAPE. — 3418 (Cape Town): Kogelberg Forest Reserve, E foothills of
Spinnekopsnes Range, 854 m, (-BB), 2-05-1970, Boucher 1285 (K, STE);
Steenbrass Reservoir valley, (-BB), 14-12-1933, Galpin 12405 (K, PRE);
Steenbrass area, (— BB), 1-05-1948, Levyns 8879 (BOL); ibid., Levyns
U533 (BOL); ibid., 7-12-1926, Middlemost 122 (BOL); ibid., Niven 6
(G-DC, K— BOL fragm.); ibid., Niven 7 (K); NE end of Kogelberg range,
450 m, (— BB), 20-03-1983, Oliver 8824 (PRE, STE); Steenbrass, Wol-
vem Kloof, (— BB), 28-02-1931, Stokoe 2563 (BOL, PRE, STE); Steen-
brass plateau & vlakte, (-BB), 18-02-1921, Stokoe 8917 (BOL); ibid.,
1931, Stokoe 8889 (BOL, PRE); near Steenbrass Reservoir, (-BB),
14-12-1933, Salter 4207 (BM, K, SAM).
8. Erica russakiana E.G.H. Oliver, nom. nov.
Blaeria kraussiana Klotzsch ex Walpers: 728 (1843) non E. kraussiana
Klotzsch ex Walpers: 728 (1843); Klotzsch ex Walpers: 824 (1844); N.E.
Br.: 326 (1905); Aim & Fries: 235 (1924); Oliver: 267 (1984). Type:
Babylon’s Tower, Hemel en Aarde, Krauss 973 (Bf, holo.; BOL!, K!,
M!, S!, UPS!, W!, Z!). Lectotype chosen here: Krauss 973 (K!-BOL
fragm.!).
Acrostemon concinnus N.E. Br. : 351 (1905). Type: Swartberg, Caledon,
Bodkin sub Bolus 9228 (BOL, holo.!; K!).
It is surprising that Brown overlooked the similarity
between his species and that of Klotzsch which he included
in his revision, especially seeing that his taxon was the
only one in Acrostemon with a 4-locular ovary.
The species, of which only four collections exist, is
confined to the northern slopes of the Klein River
Mountains north of Hermanus with one collection from
the Swartberg at Caledon (Figure 5). It forms a sparsely
branched low compact shrublet up to 300 mm tall
which becomes erect and more sparse when very old. The
flowers are superficially similar to those of the common
E. ericoides which occurs in the same area but forms a
large, woody spreading shrub up to 1.0 x 1.5 m. The other
species with similar heads of flowers, E. barbigeroides,
from the same area but near the southern base of the moun-
tains, forms a sparsely branched erect shrublet with much
larger and more numerous flowers per head.
The name chosen above continues to commemorate the
original collector, Ferdinand Krauss, but in anagrammatic
form.
Specimens examined
CAPE.— 3419 (Caledon): Swartberg, Caledon, (-AB), 01-1901, Bodkin
sub Bolus 9228 (BOL, K); Babylon’s Tower near Hemel-en-Aarde,
183-244 m, (- AC/AD), 08-1838, Krauss 973 (BOL, K, M, MO, S, UPS,
W, Z); Klein River Mtns above Diepgat, 610 m, (—AD), 1-02-1971, Oliver
3246 (PRE, STE); ibid., 22-02-1985, Oliver 8688 (STE).
9. Erica sagittata Klotzsch ex Benth. in DC., Prodro-
mus 6: 681 (1839). Type: in Vanstaaden mountains, Dr£ge
s.n., (Bf, holo. —BOL, sketch). Lectotype chosen here:
Vanstaadesberg [Van Stadensberg], 1000 ft., 27-12-1829,
Drege 7725 (P!).
Blaeria sagittata (Klotzsch ex Benth.) Aim & Fries: 238 (1924).
B. grandis N.E. Br.: 320 (1905). Syntypes: Van Stadens Mountains,
Zeyher 718 (K!, BOL fragm.!); ibid. West sub MacOwan 3119 (BOL!,
PRE!, SAM!).
B. juscescens sensu N.E. Br. : 320 (1905) quoad specm. Drege s.n.
Brown (1905) noted that Bolus had examined the type
of Erica sagittata in the Berlin Herbarium and had
informed him that despite its poor quality ‘there can be
no doubt of its identity with Blaeria juscescens Klotzsch’.
Bolus himself made a sketch of the type and some dissec-
tions of the flower and noted in his herbarium that it
contained three branches 12—14 inches long on one sheet
and only one imperfect flower in a capsule and that the
ticket labelled it as Drege 7725 from Van Stadensberg.
Bentham noted the type as ‘defloratum cum fl. unico
delapso’. If the specimen had possessed more flowers
Bolus would have seen that the axillary inflorescence on
an absolute brachyblast differed from the terminal
3-flowered inflorescence on a leafy lateral branchlet in
Blaeria juscescens and that the two species cannot be
confused.
The rather sparse material of Drege 7725 in Paris, con-
sisting of five young plants with two flowers in place on
FIGURE 5.— The known distribution of Erica longimontana , •; E. russakiana, A ; and E. sagittata , O.
6
Bothalia 23,1 (1993)
one plant, clearly matches the sketches of Bolus. It is
undoubtedly from the same collection as the lost Berlin
material.
This species is very localized in the Van Stadens Moun-
tains west of Port Elizabeth (Figure 5) where it is sympatric
with E. fuscescens. E. sagittata can be distinguished from
the latter species on a number of characters. Apart from
the type of inflorescence mentioned above, it has larger
flowers with corolla 6 mm long, not less than 4 mm, leaves
open-backed and 1—2 mm broad, not sulcate and 0.5— 1.0
mm long, and branches glabrous and distincdy ridged, not
puberulous and rounded.
E. sagittata is remarkable in being very similar to Erica
camea L. from Europe which also has flowers borne on
absolute brachyblasts and exserted dark stamens. The two
species could easily be mistaken for one another if the
origin of the material were not known. This is undoubtedly
a case of convergent evolution.
Specimens examined
CAPE.— 3324 (Steytlerville): Elandsrivierberg area in Otterford Forest
Reserve, 762 m, (-DB), 9-09-1973, Oliver 4455 (MO, PRE, STE). 3325
(Port Elizabeth): Blueberg, Loerie Plantation, 22-09-1934, (— CC), Dix
31 (BOL, GRA, K, PRE, STE); Van Stadens Gorge, Witteklip, (-CC),
09-1981, Muller s.n. (STE); Van Stadens Mtns, 305 m, (-CC/CD),
27-12-1829, Drige 7725 (P); ibid. , 09-1909, West 477 (BOL, SAM); ibid.,
West sub MacOwan 3119 (BOL PRE); ibid.. West sub MacOwan 3111
(BOL); ibid., Zeyher 718 (BOL, K); ibid., Zeyher 3266 (SAM).
INSUFFICIENTLY KNOWN SPECIES
Blaeria barbigera (Salisb.) G. Don: 805 (1834). TyPe:
Hottentots Holland, Masson s.n. (?).
Erica barbigera Salisb.: 341 (1802).
Salisbury’s type does not appear to exist, as no specimen
referrable to this species collected either by Masson or
labelled as ‘Herb. Salisb.’ nor one determined by Salisbury,
has been found in Kew or the British Museum, where all
the types of Salisbury’s species of Cape Ericaceae are
known to be housed. Salisbury’s description is insufficient
to be of use to ascertain the true identity of his species.
No mention was made of either the distinct capitate heads
of flowers (10—24) or of the glandular nature of the leaves
and calyx. His description could refer to a number of
species in Blaeria or even some other genera in the
subfamily. Without an authentic specimen it is not possible
to tie down Salisbury’s concept ‘ Erica barbigera'.
Bentham (1839) referred Salisbury’s species to Blaeria
revoluta Bartl. without having seen a type since he did
not cite a Masson collection. This was taken up by most
subsequent authors with Brown citing the synonymy as
‘sec. Benth.’.
EXCLUDED SPECIES
With the description of nunierous species under the
genus Blaeria during the late 1700’s and early 1800’s there
are many combinations under Blaeria which are no longer
in use for species removed to other genera. A full list of
these is given by Aim & Fries (1924: 262, 263) based on
the taxonomy of the family in Flora capensis (Brown
1905). With a revision of the family in southern Africa
currently in progress, many changes to the taxonomy and
therefore nomenclature, will be necessary. For this reason
a listing of all the excluded species is not published at this
stage as new combinations would have to be created of
which many would soon be redundant.
However, one species not covered by the listing of
Aim & Fries is: Blaeria muirii L. Guthrie: 179 (1924) =
Thoracosperma galpinii N.E. Br.: 330 (1905).
REFERENCES
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ALM, C.G. & FRIES, T.C.E. 1924. Monographic der Gattung Blaeria
L. Acta Horti Bergiani 8: 223—267.
ANDREWS, H.C. 1794—1830. Coloured engravings of heaths I— IV.
London.
BARTLING, F. 1832. Plantae Ecklonianae, Ericeae. Linnaea 7: 627—652.
BENTHAM, G. 1839. Ericaceae. In A.P. De Candolle, Prodromus sys-
tematis naturalis regni vegetabilis 7: 580 —733. Paris.
BERGIUS, P.J. 1767. Descriptiones plantarum ex Capite Bonae Spei.
Salvius, Stockholm.
BOLUS, H. 1894. Contributions to the flora of South Africa. Journal
of Botany 1894: 239.
BOND, P. & GOLDBLATT, P. 1984. Plants of the Cape Flora, a descrip-
tive catalogue. Journal of South African Botany, Suppl. Vol. 13.
BROWN, N.E. 1905. Ericaceae. In W.T. Thiselton-Dyer, Flora capen-
sis 4: 315-336.
DAVIDSON, L.E. 1985. A change in status for Erica subverticillaris
var. revoluta from the eastern Transvaal. South African Journal
of Botany 51: 71—73.
DIETRICH, D.N.F. 1839. Synopsis plantarum. Vol. 1. Weimar.
DON, G. 1834. A general system of gardening and botany. Vol. 3.
London.
GUTHRIE, L. 1924. Novitates afficanae. Annals of the Bolus Herbarium
3: 179.
GUTHRIE, L. 1928. Novitates africanae. Annals of the Bolus Herbarium
4: 21.
GUTHRIE, L. & BOLUS, H. 1904. Erica. In W.T. Thistelton-Dyer,
Flora capensis 4: 4-315. Reeve, London.
KLOTZSCH, J.F. 1833. Ericearum a cel. Adelberto de Chamisso descrip-
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KLOTZSCH, J.F. 1838. Ericearum genera et species. Linnaea 12:
211-247.
LINNAEUS, C. 1753. Species plantarum, edn 1. Stockholm.
LINNAEUS, C. 1767. Mantissa plantarum: 65 —66. Stockholm.
LINNAEUS, C. 1771. Mantissa plantarum alterum: 229—236.
Stockholm.
LINNAEUS, C. ftl. 1782. Supplementum plantarum. Braunschweig.
OLIVER, E.G.H. 1984. Studies in the Ericoideae. IV. New species and
some taxonomic and nomenclatural changes in the Cape Flora
Region. South African Journal of Botany 3: 267—284.
OLIVER, E.G.H. 1987a. Studies in the Ericoideae. VII. The placing
of the genus Philippia into synonymy under Erica-, the southern
African species. South African Journal of Botany 53: 455 —458.
OLIVER, E.G.H. 1987b. Ericaceae. In G.E. Gibbs Russell et al.. List
of species of southern African plants. Memoirs of the Botanical
Survey of South Africa No. 56: 140—147.
OLIVER, E.G.H. 1988. Studies in the Ericoideae (Ericaceae). VI. The
generic relationship between Erica and Philippia in southern
Africa. Bothalia 18: 1—10.
OLIVER, E.G.H. 1989. The Ericoideae and the southern African
heathers. Botanical Journal of the Linnean Society 101: 319—327.
OLIVER, E.G.H. 1993. Studies in the Ericoideae (Ericaceae). XHI. Three
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9-14.
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The generic relationship between Erica and Blaeria. Kew Bulletin.
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cation. Regnum Vegetabile.
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26: 788.
ROEMER, J.J. & SCHULTES, J. A. 1818. Systema vegetabilium. Cottae,
Stuttgart.
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SALISBURY, R. A. 1796. Prodromus stirpium in horto ad Chapel Allerton
vigentium. London.
SALISBURY, R. 1802. Species of Erica. Transactions of the Linnean
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SALTER, T.M. 1950. Ericaceae. In R. Adamson & T.M. Salter, Flora
of the Cape Peninsula. Juta, Cape Town.
THUNBERG, C.R 1794. Prodromus plantarum capensium Part 1: 1—83.
Uppsala.
THUNBERG, C.P. 1802. Dissertatio botanicae de Blaeria (P. Elmstedt):
1-12. Uppsala.
THUNBERG, C.P. 1823. Flora capensis ed. J.A. Schultes: 344-373.
Cotta, Stuttgart.
WALPERS, G.G. 1843. Ericaceae. Repertorium Botanices Systematicae
2 : 728.
WALPERS, G.G. 1844. Pflanzen des Cap- und Natal-Landes, gesam-
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Berlin.
Bothalia 23,1: 9-14 (1993)
Studies in the Ericoideae (Ericaceae). XIII. Three new species of
Erica from the southwestern Cape
i E.G.H. OLIVER*
Keywords: Cape Province, Erica, Ericoideae, new species, taxonomy
ABSTRACT
With the recent inclusion of the genus Blaeria under Erica, three new species, formerly regarded as ‘incertae’ in that
genus, are now described: Erica chiroptera E.G.H. Oliver from the Kogelberg Reserve, Erica hermani E.G.H. Oliver and
Erica ioniana E.G.H. Oliver, both highly localised endemics from Hermanus.
UITTREKSEL
Met die onlangse insluiting van die genus Blaeria by Erica, word drie nuwe spesies wat voorheen onder die ‘incertae’
van daardie genus behoort het, nou beskryf: Erica chiroptera E.G.H. Oliver van die Kogelberg Reservaat, Erica hermani
E.G.H. Oliver en Erica ioniana E.G.H. Oliver, albei uiters beperkte endemiese spesies van Hermanus.
INTRODUCTION
The genus Blaeria L. was recognised for over two
centuries as separate from Erica L. based on the single
character difference of four as opposed to eight stamens
in the latter. In a recent paper (Oliver in press) it is shown
that there is an overlap between the two genera and that
there is a clear case for regarding Blaeria as polyphyletic.
As a result the genus Blaeria is being reduced to synonymy
under Erica (Oliver 1993).
Material which had been placed in the ‘incertae’ under
Blaeria and which clearly constituted several new taxa,
has remained undescribed because of the problem with
the delimitation of Blaeria. These taxa are now described
in this paper.
Erica chiroptera E.G.H. Oliver, sp. nov. in genere
distincta propter antheras quatuor inclusas latissimas
dorsiventraliter complanatas, capite aliquorum vespertilio-
num (Chiropteridae) similes, flores albos ad roseos;
affinitate E. equisetifoliae Salisb. sed facie antherarum
exsertarum differt.
Fruticulus erectus ad 500 mm altus. Rami erecti vel
flexuosi glabri trigoni, cortice griseo. Folia 3-nata, 1.5— 3.5
x 0.5— 1.0 mm, erecta appressa, angusta, sulcata glabra
ciliata vel eciliata, breve petiolata. Flores 3 — 6[9] ad
extremis ramorum et ramulorum lateralium; pedicellus
1. 5-3.0 mm longus glaber; bractea submediana 0.5— 1.3
mm longa lineari-oblonga glabra ciliata; bracteolae
bracteae similes minores. Calyx 4-lobatus, cyathiformis
0.8— 1.5 mm longus, glaber; lobi deltoidei, sulcati, sparse
ciliati pihs parvis et glandibus sessilibus. Corolla 4-lobata
2.7-3.6 x 2.0— 2.4 mm quadrangularis cyathiformis base
porcis calyce alternantibus glabra pustulate- rugosa; lobi
late rotundati irregulariter crenulati ad subfunbriati.
Stamina 4 inclusa; filamenta 0.9— 1.6 mm longa recta
glabra; anthera 0.9— 1.4 x 0.8— 1.4 mm erecta terminalia
* Stellenbosch Herbarium, National Botanical Institute, RO. Box 471,
Stellenbosch 7599.
MS. received: 1992-06-09.
late obcuneata dorsiventraliter complanata marginibus
strigulosis, thecis patentibus poro rotundato 'u longitu-
dine thecae append iculatis, cristis late obcuneatis decur-
rentibus. Ovarium 4-loculare 0.7— 1.0 X 0.7— 1.0 mm
distincte quadrangulare late ellipsoideum ad obovoideum
glabrum, nectario reducto vel absenti, ovulis 2 in quoque
loculo, ex placenta apicali pendulis, laterahter compressis;
stylus exsertus 2.0— 2.5 mm longus teres base expansus
glaber; stigma simplex. Fructus late ellipsoideus ad
obovoideus, septis longitudine 2>3 connatis, valvis ellip-
soideis, 1.5 x 1.2 mm, obtusis; semina ellipsoidea,
subreticulata. Figura 1.
TYPE. — 3418 (Simonstown): Cape, Caledon District,
Kogelberg Forest Reserve, neck at head of the Rooi Els
valley near Wynand Louwsbos, 366 m, (-BD), 11
November 1970, Oliver 3097 (STE, holo.; BM, BOL, E,
K, MEL, MO, NY, P, PRE, S, isotypes).
Erect, open or compact shrublet up to 500 mm tall.
Branches erect or wiry and flexuose, glabrous, with slight
infrafoliar ridges and trigonous when young, bark grey
flaking irregularly or mainly below leaves, becoming red-
brown. Leaves 3-nate, erect and appressed, subimbricate,
narrowly ovate to narrowly elliptic to linear-elliptic,
1.5— 3.5 x 0.5— 1.0 mm, subobtuse to acute, markedly
convex abaxially, flat or slightly concave adaxially, sulcate,
glabrous, with or without short fine cilia and marginal
sessile glands, strigulose at apex; petiole 0.3— 0.5 mm long,
glabrous. Flowers 3— 6[9] at ends of main and short sub-
terminal lateral branchlets or brachyblasts, pendent;
pedicel 1.5— 3.0 mm long, terete, glabrous, red; bract
submedian, linear-oblong, 0.5— 1.3 mm long, glabrous,
ciliate, sometimes with marginal sessile glands also, low-
er bracts in an inflorescence larger and sometimes sul-
cate, others not sulcate; bracteoles 2 just above bract and
like bract, 0.3— 0.7 mm long. Calyx 4-lobed to half its
length, cyathiform, 0.8— 1.5 mm long, glabrous; lobes nar-
rowly to broadly deltoid, clasping base of corolla, sulcate
in upper half, green, sparsely ciliate with short hairs and
sessile glands. Corolla 4-lobed, quadrangular cyathiform,
2.7— 3.6 x 2.0— 2.4 mm, dirty white to very pale pink,
4-ridged at base with ridges alternating with calyx lobes,
10
Bothalia 23,1 (1993)
FIGURE 1. — Erica chiroptera: A, flowering branch, x 2; B, close-up of branch with leaves; C, flower; D, androecium; E, anther, side, front
and back views; F, gynoecium; G, ovary, longitudinal section; B— G, X 25. All drawn from the type, Oliver 3097 (STE).
glabrous, pustulate-rugose; lobes erect to slightly spread-
ing, broadly rounded, '/4 the length of corolla, irregularly
crenulate to subfimbriate. Stamens 4 included; filaments
0.9— 1.6 mm long, straight, erect, slightly broadening
downwards, glabrous; anthers erect, placed just above
ovary, terminal, broadly obcuneate, with appendages
0.9— 1.4 X 0.8— 1.4 mm, dorsiventrally flattened, strigulose
on edges; thecae spreading in a broadly V-shaped arrange-
ment, 0.5— 0.9 mm long; pore rounded, 'u the length of
theca; appendages broadly obcuneate, decurrent for just
more than half their length. Ovary 4-locular, distinctly
quadrangular, broadly ellipsoid to obovoid, 0.7— 1.0 x
0.7— 1.0 mm, glabrous, nectaries very reduced or absent,
septa joined for half their length from base; ovules 2 per
locule, pendulous one above other from apical placenta,
laterally compressed; style exserted, 2.0— 2.5 mm long,
terete, enlarging slightly below stigma, occasionally bent
at apex, with enlarged basal portion forming a cap on ovary
apex, glabrous; stigma simple. Fruit broadly ellipsoid to
obovoid, septa joined for 2/3 of their length, valves
broadly elliptic, obtuse, 1.5 x 1.2 mm; seeds ellipsoid,
light brown, subreticulate. Figure 1.
E. chiroptera is a very distinct species on account of
its very broad, dorsiventrally flattened anthers which are
reminiscent of the heads of some bats (Order Chiroptera),
hence the name. It is, however, related to the extremely
variable species complex which is now referred to as E.
equisetifolia (Oliver 1993) and which occurs in the same
region. This latter species forms smaller, more compact
rounded shrublets which can, however, become taller and
erect when old. Its flowers are pink in colour, sometimes
deeply so, and have exserted anthers which are narrow and
elongate with small awns.
The species is confined to the Kogelberg Reserve
between Grabouw and Betty’s Bay (Figure 2) where it
grows in sandy quartzitic ground with short restiads.
Specimens examined
CAPE. — 3418 (Simonstown): Kogelberg Reserve, lower slopes south
of Klein Palmiet River, southwest of Somersfontein, 244 m, (— BB),
27-01-1987, Oliver 8999 (BM, BOL, G, K, NY, PRE, STE, W); Palmiet
River near Elgin, (— BB), 12-1941, Stokoe 6247 sub SAM 55121 (NBG,
PRE, SAM); Kogelbeig Reserve, Somersfontein boundary, 275 m, (— BD),
19-11-1969, Boucher 874 (PRE, STE); Kogelberg Reserve, Louws River
road, 335 m, (— BD), 11-03-1970, Boucher U79 (PRE, STE); Betty’s Bay,
plateau behind Cascades, 450 m, (— BD), 10-02-1956, Levyns 10456
(BOL); Kogelberg Reserve, head of Rooi Els valley near Wynand
FIGURE 2.— Known distribution of Erica chiroptera, •; and E.
hermani, O.
Bothalia 23,1 (1993)
11
Louwsbos, 366 m, (— BD), 11-03-1970, Oliver 3097 (BM, BOL, E, K,
MEL, MO, NY, P, PRE, S, STE). 3419 (Caledon): Arieskraal, (— AA),
30-12-1944, Leighton 915 (BOL); near Elgin, between Grabouw and the
Paardeberg, (-AA), 12-1947, Stokoe sub SAM 62387 (NBG).
Erica hermani E.G.H. Oliver, sp. nov. ex planitie
oraria Hermani, distincta propter folia sessilia appressa,
flores roseos campanulatos, stamina 8, antheras atras
strigosas exsertas mox deciduas; affinitate E. equisetifoliae
Salisb. ex eodem loco sed floribus tubulosis, staminibus
4 rare 5-8 (alteris locis) fuscis ad fulvis non deciduis
differt.
Fruticulus erectus ad 500 mm altus. Rami erecti, trigoni,
infra folia porcati, glabri roseo-brunnescentes, rami veteres
cortice frustris griseis. Folia 3-nata sessilia, appressa
subimbricata, 1.5— 2.8 mm longa, elliptica ad oblongo-
elliptica, acuta, glabra apice sparse strigulosa glandibus
sessilibus marginalibus. Flores 3— 9-nati terminales
pendentes; pedicellus 2.0— 2.8 mm longus, teretus, glaber;
bractea mediana, 0.7— 1.0 mm longa, naviculata, glabra
esulcata, breve ciliata pilis vel glandis sessilibus; bracteo-
lae subapproximatae bracteae similes sed breviores. Calyx
4-lobatus, obconicus ad cyathiformis, 1.2— 1.4 mm longus,
'u — !/3 connatus, base emarginatus; lobi ovato-deltoidei
ad late deltoidei, longe sulcati, ciliati glandis sessilibus
atrosanguineis. Corolla 4-lobata 2.4— 3.5 x 2.5— 3.0 mm,
obconica ad campanulata, interdum late campanulata et
parum quadrangularis, pustulata, pallido- ad atrorosea;
lobi longitudine '/4 — */3 corollae partes aequantes, late
deltoidei et obtusi, erecti ad plus minusve patentes,
irregulariter crenato-fimbriati. Stamina 8 exserta; filamen-
ta linearia ± 3 mm longa, sub anthera angustiora, glabra;
antherae bene exsertae, prope base dorsaliter affixae, post
anthesin mox deciduae, thecis 1.3— 1.5 mm longis, erectis,
appressis, suboblongo-ovatis, apice prognathis, obtusis.
marginibus strigosis ad base barbatis, nigris. Ovarium
4-loculare 0.6-0.8 x 0.6 -0.8 mm, quadrangulare, late
ellipsoideum, glabrum, base nectariis parvis; ovula 7-8
in quoque loculo, ex placenta apical i pendentes; stylus
exsertus, ± 5.4 mm longus, anguste cylindraceus basaliter
amplificatus, glaber; stigma obconica. Fructus late ellip-
soideus, septis longitudine 2/3 connatis, valvis 1.2 x 1.0
mm, late ellipsoideis, truncatis ad emarginatis; semina
complanata ellipsoidea, subreticulata, hepatica. Figura 3.
TYPE. — 3419 (Caledon): Cape, Hermanus, Fernkloof,
sandy lower slopes, 45 m, (-AD), 18 February 1984,
Oliver 8412 (STE, holo.; BM, BOL, E, G, K, MEL, MO,
NY, P, PRE, S, W, isotypes).
Sparse, erect shrub to 500 mm tall. Branches very fine,
erect, mostly leafy, trigonous when young with inffafoliar
ridges, glabrous, becoming round and reddish brown when
old with grey inffafoliar flakes of bark. Leaves 3-nate,
sessile, appressed, subimbricate, 1.5 -2.8 mm long, ellip-
tic to oblong-elliptic, acute, glabrous, sparsely strigulose
at apex, with a few sessile marginal glands when young.
Flowers 3-9-nate at ends of branches, pendent; pedicel
2.0— 2.8 mm long, terete, glabrous; bract median, 0.7— 1.0
mm long, naviculate, glabrous, without sulca, shortly
ciliate with hairs and/or sessile glands; bracteoles sub-
approximate, like bract but slightly shorter. Calyx 4-lobed,
obconical to cyathiform, 1.2— 1.4 mm long, joined for
*/3 — its length, emarginate at base, green to reddish,
lobes ovate-deltoid to broadly deltoid, long sulcate, edged
with sessile dark red glands. Corolla 4-lobed, 2.4— 3.5 x
2.5— 3.0 mm, obconical to campanulate sometimes broadly
so and somewhat quadrangular, pustulate, light to dark
cerise-pink; lobes ’/4 — ‘/3 the length of corolla, broadly
deltoid and obtuse, erect to slightly spreading, irregular-
ly crenate-fimbriate. Stamens 8 exserted; filaments linear,
FIGURE 3.— Erica hermani: A, flowering branch, x 2; B, close-up of branch with leaves; C, flower; D, anther, side front and back views;
E, ovary; F, ovary, longitudinal section; B-F, x 25. All drawn from the type, Oliver 8412 (STE).
12
Bothalia 23,1 (1993)
± 3 mm long, narrowed below anther, glabrous; anthers
well exserted, dorsally attached near base and soon
deciduous after anthesis, thecae 1.3— 1.5 mm long, erect,
appressed, suboblong-ovate, bent forwards at apex, obtuse,
strigose edged to bearded at base, black. Ovary 4-locular,
0.6— 0.8 x 0.6— 0.8 mm, quadrangular, broadly ellipsoid,
glabrous, with very small nectaries at base; ovules 7-8
per locule, pendent from an apical placenta; style exserted,
± 5.4 mm long, narrowly cylindrical with enlarged base
forming a cap to ovary, glabrous; stigma obconical. Fruit
broadly ellipsoid, septa joined for 2/3 their length, valves
1.2 x 1.0 mm, broadly elliptic, obtuse to emarginate; seeds
flattened ellipsoid, subreticulate, brown. Figure 3.
Erica hermani is allied to the variable and widespread
E. equisetifolia, formerly Blaeria equisetifolia (Salisb.)
G. Don and now including Blaeria dumosa Wendl. (Oliver
1993). It differs in having constantly eight stamens with
black, strigose, muticous anthers which are shed very soon
after anthesis; the flowers are also open-campanulate as
opposed to tubular. The shedding of the anthers leaves the
black-tipped filaments clearly visible in the mouth of the
corolla. The anthers of E. equisetifolia are variable in
shape being mostly long and narrow with decurrent awns
in the plants from the Hermanus area. Plants from the
inland mountains, formerly referred to Blaeria campanula-
ta Benth. and now placed under E. equisetifolia (Oliver
1993), have rather similar anthers to E. hermani but with
decurrent awns.
This species is very restricted, occurring only on the
sandy coastal flats near the entrance to the Fernkloof
Nature Reserve at Hermanus, hence the specific epithet,
(Figure 2) where it is locally common in remnant patches
of fynbos. There it co-exists with plants of E. equisetifolia
which looks remarkably similar, but is easily distinguished
on close examination of the flowers.
In the population of the above two species a few plants
with slightly different looking flowers were noted and on
close examination were found to be intermediates between
the two. The possession of nonviable pollen strongly
suggested a hybrid origin for these plants.
Specimens examined
E. hermani
CAPE. — 3419 (Caledon): Hermanus, Fernkloof, (—AD), 05-1986,
Drewe s.n. (STE); ibid., 45 m, 18-02-1984, Oliver 8412 (BM, BOL, E,
G, K, MEL, MO, NY, P, PRE, S, STE, W); ibid., 300 m, 12-01-1981,
Williams 3109 (BOL, PRE, STE); Mossel River flats, (—AD), Williams
sub Baker 3043 (STE).
E. equisetifolia [= Blaeria equisetifolia (Salisb.) G. Don]
CAPE.— 3419 (Caledon): Hermanus, sandy lower slopes at Fernkloof,
45 m, (—AD), 18-02-1984, Oliver 4111 (K, MEL, MO, NY, PRE, STE).
E. hermani x E. equisetifolia
CAPE.— 3419 (Caledon): Hermanus, sandy lower slopes at Fernkloof,
45 m, (—AD), 18-02-1984, Oliver 8413 (PRE, STE).
Erica ioniana E.G.H. Oliver, sp. nov. ex montibus
Hermani in genere distincta propter habitum parvum com-
pactum, flores campanulatos cremeos viscidos in capitibus
pendulis occultos, stamina straminea 4 interdum 5;
affinitatibus E. ericoidis (L.) E.G.H. Oliver et E.
russakianae E.G.H. Oliver sed inflorescentibus erectis,
floribus roseis non viscidis, staminibus fuscis.
Fruticulus compactus ad 150 mm altus. Rami glabri vel
sparse pubescentes ad villosi, sterigmatis infrafoliaceis,
rami veteres irregulariter porcati cicatricibus griseis. Folia
4-nata, 3.5— 5.0 mm longa oblongo-elliptica sparse villosa,
breviter glandulociliata; petiolus appressus, 1.2— 1.5 mm
longus, ciliatus pilis longis et glandibus sanguineis sub-
sessilibus. Flores 12—20 capitis compactis ad extremis
ramorum, dependentes, sub planta occultae; pedicellus
1.3— 1.7 mm longus, sparse villosus; bractea subapproxi-
mata 1.8— 2.5 mm longa, linearis ad lineari-spathulata,
foliacea in dimidio supemo sulcata, sparse villosa,
glandulis sessilibus vel subsessilibus ciliata; bracteolae
approximatae, 1.3— 2.0 mm longae, lineares ad filiformes
aliter bracteae similes. Calyx 4-lobatus, 1.4— 1.8 mm
longus; lobi subliberi anguste oblongo-lanceolati sparse
villosi glandulis subsessilibus sanguineis in marginibus et
in pagina adaxiali apicem versus, sulcatus. Corolla
4-lobata, 2.5 mm longa, campanulata quadrangularis,
glabra, viscida, cremea ad rosea; lobi 1 mm longi expansi
ad recurvi. Stamina 4(5); filamenta 3 mm longa, linearia,
apice latiore flexo; antherae inclusae ad submanifestae,
bipartitae, thecis 0.8 mm longis subellipsoideis, glabris,
super ovario impendentibus; porum longitudine '/3 thecae
partes aequans; pollen in tetradis. Ovarium 4-loculare, 0.6
x 0.6 mm, late ovoideum, 4-lobatum, plus minusve
emarginatum, glabrum, base nectariis grandibus; stylus
2 mm longus, exsertus; stigma simplex. Fructus globosus
vel late ovoideus, valvis 1.0 x 0.8-1.0 mm late ellipticis,
obtusis ad emarginatis; semina ovoideo-ellipsoidea,
reticulata, fusca. Figura 4.
TYPE. — 3319 (Caledon): Cape, Hermanus, Mossel
Neck at SW end of Vogelgat Nature Reserve, 490 m,
(-AD), 22 February 1985, Oliver 8684 (STE, holo. ; BOL,
K, MO, PRE isotypes).
Low compact shrublet to 150 mm tall with slightly
spreading branches. Branches glabrous or sparsely pubes-
cent to villous when young, with slight infrafoliar ridges
when young, bark with slight infrafoliar flakes otherwise
flaking irregularly when old. Leaves 4-nate, 3.5— 5.0 x
3.0 mm long, oblong-elliptic, sparsely villous all over and
sometimes shortly gland-ciliate, becoming strigose; petiole
appressed, 1.2— 1.5 mm long, ciliate with long hairs and
red subsessile glands. Flowers 12—20 in compact heads
at ends of branches, feeing downwards, hidden under plants
and not visible; pedicel 1.3— 1.7 mm long, sparsely vil-
lous, red; bract subapproximate, 1.8— 2.5 mm long, shorter
than calyx, linear to linear-spathulate, foliaceous and sul-
cate in upper half, sparsely villous, edged with sessile to
subsessile red glands; bracteoles approximate, 1. 3-2.0
mm long, shorter than calyx, linear to filiform, otherwise
similar to bract. Calyx 4-lobed, 1.4— 1.8 mm long; lobes
almost free, narrowly oblong-lanceolate, just shorter than
corolla tube, sparsely villous, with subsessile red glands
on edges and adaxially towards apex, sulcate, hairy,
green turning red. Corolla 4-lobed, 2.5 mm long,
campanulate, 4-angled, glabrous, viscid, cream to pale
pink; lobes 1 mm long, spreading to recurved. Stamens
4(5); filaments 3 mm long, linear with a broader bent apex;
anthers included to just manifest, bipartite, pale yellow
FIGURE 4. — Erica ioniana : A, flowering branch, x 2; B, whorl of leaves; C, flower; D, sepal; E, anther, side front and back views; F, gynoecium;
G, mature ovary; B— G, x 25. All drawn from the type, Oliver 8684 (STE).
brown; thecae 0.8 mm long, slightly ellipsoid, glabrous,
bent forwards over ovary; pore V3 the length of theca;
pollen in tetrads. Ovary 4-locular, 0.6 x 0.6 mm, broadly
ovoid, 4-lobed, slightly emarginate, glabrous, with well-
developed nectaries at base; style 2 mm long, exserted;
stigma simple. Fruit globose or broadly ovoid, valves 1.0
x 0.8— 1.0 mm, broadly elliptic, obtuse to emarginate;
seeds ovoid-ellipsoid, reticulate, dark brown. Figure 4.
This distinct species was brought to my attention by Dr
Ion Williams of Hermanus (alter whom the species is
named) who is undertaking surveys of his Vogelgat Reserve
in the Klein River Mountains above Hermanus. He
assumed the plant to be, from the description, Blaeria
affinis N.E. Br. which is known only from the type
collection made in Vogelgat by Schlechter. This latter
species was reduced to synonymy under E. ericoides
(L.) E.G.H. Oliver (= B. ericoides L.) by Aim & Fries
(1924). I have found that Schlechter ’s collection is just a
depauperate form of the common species.
A visit to the area revealed that Williams’ populations
were a distinct new species with an unusual habit. The
plants are low, compact and rounded with the flowers
arranged in pendent heads such that they are not easily
noticeable when the plants are in full bloom. The pale
colour of the corolla and the long hairs of the calyces in
the heads of flowers also help to make the flowers less
visible. In these respects the species is unlike any other
in the area. The other species there with capitate inflores-
cences, namely E. ericoides, E. russakiana and E.
barbigeroides E.G.H. Oliver, have the branches spreading
or erect and different, dark brown, basally winged or
appendiculate, exserted anthers. The anthers in E. ioniana
are pale yellowish brown, muticous, included and are
narrowed in at the base. They are very similar to those
found in E. multiflexuosa E.G.H. Oliver, a restricted
endemic near Steenbras Dam.
The species is restricted to level sandy places in and
near the Vogelgat Reserve, Hermanus, (Figure 5) where
three populations have so far been found. The unusual
habit strongly suggests some form of pollination by
creeping insects with the flowers facing downwards only
a short distance from the ground.
Specimens examined
CAPE. — 3419 (Caledon): Hermanus, Mossel Neck in Vogelgat
Reserve, 490 m, (—AD), 22-02-1985, Oliver 8684 (BOL, K, MO, PRE,
STE); ibid., 480 m, (—AD), 9-02-1985, Williams 3580 (NBG, PRE);
Caledon District, north side of Klein River Mtns above Diepgat, 594
m, (-AD), 22-02-1985, Oliver 8688 (BM, E, K, MEL, NY, PRE, STE);
Hermanus, Femkloof, Mt Pustulata, 610 m, (—AD), 26-02-1984, Williams
3531 (HER, NBG, PRE, P, S).
REFERENCES
ALM, C.G. & FRIES, T.C.E. 1924. Monographic der Gattung Blaeria
L. Acta Horti Bergiani 8: 223—267.
FIGURE 5.— Known distribution of Erica ioniana.
Bothalia 23,1 (1993)
OLIVER, E.G.H. in press. Studies in the Ericoideae (Ericaceae). XI. placing of the genus Blaeria into synonymy under Erica-, nomen-
The generic relationship between Erica and Blaeria. Kew Bulletin. clatural changes for the southern African region. Bothalia 23:
OLIVER, E.G.H. 1993. Studies in the Ericoideae (Ericaceae). XII. The
1-7.
-
. >.
Bothalia 23,1: 15-23 (1993)
The hepatics, Symphyogyna podophylla and Pallavicinia lyellii (Palla-
viciniaceae) in southern Africa
S.M. PEROLD*
Keywords: Hepaticae, Pallaviciniaceae, Pallavicinia lyellii, southern Africa, Symphyogyna podophylla, systematics
ABSTRACT
A detailed description of Symphyogyna podophylla, illustrated with photographs of the thalli and spores, is presented.
It is compared to S. hymenophyllum, with which it may be conspecific. The subcosmopolitan Pallavicinia lyellii, also occurring
in southern Africa, is described and illustrated with photographs.
UITTREKSEL
’n Uitvoerige beskrywing van Symphyogyna podophylla, gefllustreer met foto’s van die tallusse en spore, word gegee. Dit
word vergelyk met S. hymenophyllum waaraan dit gelyksoortig mag wees. Die subkosmopolitiese Pallavicinia lyellii, wat
ook in suidelike Afrika voorkom, word beskryf en met foto’s gefllustreer.
INTRODUCTION
Symphyogyna podophylla is locally quite widespread but
of rarer occurrence in southern Africa than S. brasiliensis,
the other species recorded for the region. The latter was
recently redescribed and illustrated with photographs
(Perold 1992) in order to draw attention to its southern
African synonyms Pallavicinia capensis, Symphyogyna
valida and S. lehmanniana (Grolle 1980). Sporulating
material of S. podophylla held at PRE is rare, Koekemoer
991 (which was recently collected), being only the fourth
specimen of this species which has spores.
Amell (1963), Vanden Berghen (1965), Grolle (1979) and
Grolle & Piippo (1986) regard S. hymenophyllum (Hook.)
Nees & Mont, as conspecific with S. podophylla, but
this has been questioned, since there appear to be some
differences in the spore ornamentation, as seen on SEM
micrographs and in the chemistry of plants from New
Zealand (E.O. Campbell pers. comm.). This description
of 5. podophylla, illustrated with photographs, is given
in the hope that it may help to answer the question whether
S. hymenophyllum is conspecific with S. podophylla or
not.
The subcosmopolitan Pallavicinia lyellii of the same
family Pallaviciniaceae Migula, but different subfamily
Pallavicinioideae (Migula) Grolle, is also redescribed and
illustrated with photographs. Differences between the
genera Symphyogyna and Pallavicinia are briefly discussed
in Perold (1992) and under Pallavicinia lyellii below.
Symphyogyna podophylla (Thunb.) Mont. & Nees
in Gottsche, Lindenberg & Nees, Synopsis hepaticarum:
481 (1846); Amell: 107 (1963); Vanden Berghen: 157
(1965). Type: Cape, ‘Promontorium Bonae Spei’, leg.
Thunberg (25945 UPS, holo.!; S, STR, W, iso.).
Jungermannia podophylla Thunb.: 174 (1800); Thunb.: 738 (1823).
* National Botanical Institute, Private Bag X101, Pretoria 0001.
MS. received: 1992-07-29.
S. rigida Steph.: 112 (1914); Steph.: 69 (1917). Syntypes: Rwanda,
Rugege-Wald: ca. 1 900 m, leg. Mecklenburg 842', Vulkan-gebiet:
Ninagongo ca. 3 500 m, leg. Mecklenburg 2012 (?G). [Syn. fide Vanden
Berghen: 159 (1965)].
S. rhizobola (Schwaegr.) Nees & Mont.: 68 (1836). Jungermannia
rhizobola Schwaegr.: 31 (1814). Type: Reunion (W, iso.). [Syn. fide
Grolle: 267 (1979)]. See Amell: 109 (1963).
S. harvevana Taylor: 408 (1846). Type: Cape of Good Hope, leg.: W.H.
Harvey (FH, holo.; NY, S, W, iso.). [Syn. fide Sim: 33 (1926)].
Terricolous, on damp soil; thallus, mostly erect,
dendroid shoots in loose mats or tufts, green to olive-green,
medium-sized; proximal branches, after initial dichotomy,
single, ± 4 mm long, then a further 2 or 3 times dichoto-
mously furcate, with 7 or 8(-12) terminal branches, linear
to narrowly ovate, up to 11 mm long, 1.6 -2.0 mm wide,
125 thick over ventrally slightly bulging costa, lacking
rhizoids, but with central, brown conducting strand clearly
visible and forking at dichotomies; apex rarely progres-
sively narrowed with a reversion to stipe-like condition
and arching down, mostly entire or slightly to deeply
notched, bearing 2- celled slime papillae, margins of wings
dentate, lacking slime papillae, plane, not undulating or
hardly so, bilaterally expanded from ascending wingless
stipe (Figure 1H), 4—18 mm long, in transverse section
275 x 500 gm, arising from horizontally creeping and
much branched, cylindrical brown rhizome, with nume-
rous smooth ventral rhizoids, ± 12.5 pm wide. Wings
generally unistratose, but medianly bistratose and grading
into flatfish costa (Figure IK), laterally with marginal
teeth, remote or closer together, occasionally very blunt,
usually with 2(or 3) forwardly directed cells, diverging
at an angle of ± 45°, basal cell 62.5 x 37.5 pm (rarely
with 2 adjacent cells), top cell bluntly conical, 50 x 30
pm\ marginal cells ± rectangular to polygonal
(40.0— )67.5— 90.0 x 27.5—37.5 pm, 30-35 pm thick in
transverse section, their walls and those of l(or 2) rows
of inframarginal cells generally somewhat thicker (Figure
U), coloured pinkish; laminal cells arching toward
margins, polygonal, up to 82.5 x 55.0 pm; epidermal cells
along costa narrowly rectangular or long-hexagonal,
75.0-125.0 x 37.5 pm, occasionally bearing 2-celled slime
papillae above; chloroplasts numerous, ± 5 pm wide,
16
Bothalia 23,1 (1993)
FIGURE 1. — Symphyogyna podophylla, plants and androecia. A, male branches in situ; B, branches with rows of antheridial scales along costa,
C, some antheridial scales above costa, much enlarged; D, E, excised antheridial scales; F, apex of lobe; G, laminal cells with numerous
round chloroplasts and few spindle-shaped oil bodies; H, transverse section of stipe; I, transverse section of costa and central conducting
strand, much enlarged; J, transverse section of lateral and thicker-walled marginal cells of lobe; K, transverse section of lobe; L, toothed
margin of lobe from above. A— F, H— L, Koekemoer 991; G, Koekemoer 994. A, x 4; B, x 5; C, x 70; D, E x 100; F, H, L, x 125;
G, x 500; I, J, X 250; K, x 50. A— L, LM photographs.
FIGURE 2. — Symphyogyna podophylla, female plants. A, B, female branches with capsules above bifurcation ot costa; (J, part ot snoot calyptra
in transverse section; D, young seta in transverse section; E, involucral scale and cluster of archegonia; F, outer cells of capsule wall;
G, transverse section of capsule wall; H, spore and elater. A— G, Koekemoer 991. A, X 10; B, x 8; C, x 100; D, X 125; E, X 50;
F, G, x 250. A— G, LM photographs.
entirely filling cells, or clustered along cell walls, several
oil bodies also present, spindle-shaped (Figure 1G) and
+ 7.5 pm long, or round when viewed end-on. Costa with
central conducting strand, 37.5 x 50.0 pm, consisting
mostly of 12 small, ± 10 x 10 pm, brown, thick-walled,
angular cells, surrounded above and below by 3 rows of
larger, thin-walled parenchymatous cells (Figure II),
20.0-22.5 x 25.0-37.5 pm.
Dioicous. Androecia in 1 or 2 dorsal rows over the cos-
ta (Figure 1A— C); antheridia 200 x 175 pm, short-stalked,
each one individually covered and well hidden by irregu-
larly shaped, forwardly directed scale-like involucre
(Figure ID, E), 175 pm wide at base, up to 450 pm long,
irregularly incised at apex. Gynoecia generally 2 per
frond, dorsally situated above costa at bifurcation of
conducting strand (Figure 2A, B), containing several
archegonia and subtended by posteriorly inserted involucre
(Figure 2E), 675 pm wide at base, deeply laciniate to
filiform above, cells short- to long-rectangular, 45.0-125.0
x 71.5—41.5 pirn. Calyptra thickening and enlarging into
a fleshy shoot calyptra, ± 4 mm long and up to 8 cell
18
Bothalia 23,1 (1993)
rows or 250 /xm thick in transverse section (Figure 2C),
with several unfertilized archegonia remaining attached
near the top (Figure 2 A). Capsule cylindrical , 1800 x 850
pm, opening along several longitudinal valves, remaining
attached above, wall brown, 2 cell layers thick (Figure 2G),
outer cells elongate (Figure 2F), 62.5— 107.5 x 17.5 pm,
walls thickened, inner cells thin-walled. Seta erect when
young, 480 /im in diameter, with ± 36 cortical cells, ±
50.0 x 32.5 )tm, medullary cells slightly larger, 62.5 x
37.5 pm, angular, thin-walled (Figure 2D). Spores light
brown, ± globular, 20—25 pm in diameter, ornamenta-
tion nodular, with some very irregular, broad flattened
granular ridges (Figure 3A— C), meshes sometimes
distinct, but mostly not; proximal face with small round
area with compact, punctate ornamentation (Figure 3D,
E). Elaters brown, hardly tapering toward ends, 305—330
x 7.5 pm, 2-spiral (Figures 2H; 3F).
Symphyogyna podophylla is quite rarely collected in the
Transvaal and Natal, but fairly frequently in southwestern,
southern and eastern Cape. There are no records from the
Orange Free State (Figure 4). From other parts of Africa,
Amell (1960) has reported it from Ethiopia (= Abyssinia)
and Vanden Berghen (1965) has also been reported it from
Ethiopia (= Abyssinia) as well as from Tanzania and the
Congo Republic (Kivu Province) . Best (1990) records both
5. podophylla as well as its synonym, S. harveyana, from
Zimbabwe. Vana et al. (1979) report S. podophylla from
Zaire, Rwanda and Reunion; Bizot & Poes (1974) found
it to occur in Kenya on Mt Kenya and the Aberdare Moun-
tains in montane mossy forests and subalpine moorland;
Bizot et al. (1976) report it from Malawi. Some of these
specimens may, however, belong to Jensenia spinosa
(= Pallavicinia spinosa ), with which S. podophylla has
sometimes been confused (Grolle 1979).
DISCUSSION
In such a wide ranging species one would expect some
local variation. A Sim specimen, PRE-CH 1491, from
Table Mountain has bistratose wing margins, and medianly
there are four layers of cells. The determination was kindly
confirmed by Dr Grolle. Amell (1963) regarded the size
of the marginal teeth in S. podophylla as having no taxo-
nomic significance, nor the thickness of the walls in the
marginal cells. He also did not find distinct differences
between t;ie erect and procumbent forms, there being a
continued gradation between the two.
In a comparison of transverse sections taken at the
middle of the apical lobes of specimens of S. podophylla
and of S. hymenophyllum from Juan Fernandez, Arnell
(1956) stated that the thickness of the ‘nerves’ and the size
of the teeth in the margin of the thalli vary but little. Amell
(1963) also compared specimens of S. hymenophyllum from
Tristan da Cunha and Inaccessible Island as well as from
Reunion and from Kilimanjaro, with numerous specimens
of S. podophylla from the Cape (e.g. Thunberg’s collec-
tions) and could not find any real difference between them.
On the other hand, Gottsche et al. (1846) distinguished
S. podophylla from S. hymenophyllum by the ‘frondis
laciniis basi attenuatis subpetiolatis’ of the former.
In the present study, a photograph of the transverse
section of a lobe (Figure IK) was compared with the
drawing of a section, taken midway of a terminal
lobe, by Hassel de Menendez (1961a: fig. 10c) and the
resemblance is unmistakable. It may thus be that Arnell
(1963) was indeed correct in placing S. hymenophyllum
in synonymy under S. podophylla. Scott (1985) also recog-
nizes the Australian species as S. podophylla. Should
FIGURE 3. —Symphyogyna podophylla, spores and elaters. A, B, distal face; C, distal face much enlarged; D. part of proximal face with punctate
area; E, punctate area on proximal face, much enlarged; F, elaters. A, Koekemoer 991', B— E, Doidge 168', F, Hilner CH 1499. A, X 1835;
B, D, x 1530; C, E, x 2524; F, x 720.
Bothalia 23,1 (1993)
19
FIGURE 4. — Distribution of Symphyogyna podophylla, ▲; and
Pallavicinia lyellii, O, in southern Africa.
S. podophylla and S. hymenophyllum eventually conclu-
sively prove to be conspecific, then S. podophylla would
be circumsubantarctic in its range, since S. hymeno-
phyllum is reported to occur in South America, and
New Zealand is the type locality. Poes (1976), in discuss-
ing the presence of subantarctic bryophytes in tropical
Africa, remarks on the high number of subantarctic ele-
ments that are present and reckons that they may have
migrated northwards by means of mountain hopping.
Symphyogyna podophylla is a less common and smaller
plant than S. brasiliensis . It can be distinguished by: its
growth form which is generally flabellate from an erect
stalk arising from a creeping rhizome; the lobe margins
which are toothed and hardly undulate; it rarely fruits and
the spore ornamentation is characterised by broad, flat,
roughened, irregular ridges, sometimes forming ‘loops’,
and not by narrow, erect ridges as in S. brasiliensis.
Symphyogyna podophylla and S. brasiliensis are the only
two species of Symphyogyna occurring in southern Africa
and are placed in the subfamily Symphyogynoideae (Trev.)
Grolle.
Note: the collector of the type specimens of S. rigida is
stated to be Mildbraed by Stephani (1917) and Geissler &
Bischler (1990). However, Mildbraed was the publisher
of ‘Wissenschaftliche Ergebnisse der Deutschen Zentral-
Afrika-Expedition 1907—1908’; the leader of the
expedition, Adolf Friedrich, Duke of Mecklenburg, should
be cited as collector, as was done by Vanden Berghen
(1965) and now by me.
SPECIMENS EXAMINED
TRANSVAAL.— 2230 (Messina): Zoutpansberg, Piesanghoek, at
Waterfall, (— CC), M. Bosnian 206 (PRE); Piesanghoek, (-CC), M.
Bosnian 943 (PRE); Entabene, (-CC), M. Bosnian 1774 (PRE);
Entabene, (— CC), Bottomley 2865 (PRE); De Hoek State Forest,
Grootbosch Hiking Trail. ± 9.5 km from start, (— CC), Koekemoer 991
(PRE); Zoutpansberg, (— CC), Obermeyer 1941C ex herb. Tvl. Museum,
Obermeyer 3109 (PRE). 2329 (Petersburg): Haenertsburg. (— DD), H.A.
Wager CH 3808 (PRE). 2430 (Pilgrims Rest): Graskop, Fairyland,
(— DD), Glen 2982 (PRE); Hebron Mountain, in second cleft on plateau,
against vertical stream wall, (— DB), Vorster 1000 (PRE); Hebron
Mountain, northern slope, gallery forest along stream in plantation, on
stone and soil, (— DB), Vorster 1635 (PRE); Mariepskop, Blyde River
footpath, on wet earth bank along stream in forest, (— DB), Vorster 1516
(PRE). 2527 (Rustenburg): Magaliesberg, lower Tonquani KJoof, cliff
face, in dripping water, (-CA), H. Anderson 1249, 1250 (PRE); Magalies-
berg range. Crystal Waters, 13 km E of Rustenburg, in constant drip of
waters of sheer chasm, into a stream a few feet below, (— CA), Mogg
34818 (PRE). 2530 (Lydenburg), Kaapsche Hoop, (— DB), V.A. Wager
62 (PRE).
NATAL.— 2731 (Louwsburg): Zululand, Vryheid Dist., Ngoni Forest,
(- CD), Forester CH 1505, CH 1529, CH 1530 (PRE). 2828 (Bethlehem):
Mont-aux-Sources, (-DD), Doidge 168 (PRE). 2929 (Underberg):
Donnybrook, Gala Bush, (— DD), Doidge CH 13112 (PRE). 2930 (Pieter-
maritzburg): Edendale, Gordon Falls, (— CB), T.R. Sim CH 1495 (PRE);
Hilton Road, (- CB), T.R. Sim 8242 (PRE).
CAPE. — 3227 (Stutterheim): Hogsback, Victoria East, (— CA), Van
der Bijl 75 (PRE); Hogsback, in shade, streambank, (— CA), Young CH
1507 (PRE); Evelyn Valley, (-CB), T.R. Sim CH 1522 (PRE). 3318 (Cape
Town): Table Mountain, Disa Gorge, (—CD), S. Amell 1059, 1099, 3932
(PRE); Table Mountain, Window Gorge, (—CD), Bews CH 1517 (PRE);
Table Mountain, Skeleton Gorge, (—CD), Bews 8482 (PRE); top of Table
Mountain, (—CD), Bews 8516 (PRE); Table Mountain, Woodhead Tunnel
Gorge, (—CD), Bews 8519 (PRE); in spring at base of Lion’s Head,
(-CD), Bews CH 1490 (PRE); Table Mountain, (-CD) , Bolus CH 1496
(PRE); Table Mountain, Skeleton Ravine, (-CD), Bolus CH 1521 (PRE);
Table Mountain, (-CD), Michell CH /4<S9(PRE); eastern slopes of saddle
between Table Mountain and Devil’s Peak, on wet and partly shaded
rocks, (-CD), Pillans 3548 (PRE); Devil’s Peak, The Grottos, (—CD),
T.R. Sim CH 1492 (PRE); Table Mountain, Window Gorge waterfall,
(-CD), T.R. Sim CH 1493 (PRE); Table Mountain, Slongoli, (-CD),
T.R. Sim CH 1494 (PRE); Table Mountain, Woodhead tunnel intake,
(—CD), T.R. Sim CH 1506 (PRE); Cape Town, Platteklip stream, (—CD),
T.R. Sim CH 1511 (PRE); Newlands ravine, (—CD), T.R. Sim CH 1527,
CH 1528 (PRE); Table Mountain, (-CD), H.A. Wager 4 (PRE). Without
locality, H.A. Wager 3828 (PRE); Stellenbosch, Paradise Ravine, grow-
ing in dense masses, (— DD), (label in Duthie’s handwriting), ex Herb.,
Sim CH 1510 (PRE); Stellenbosch Mountain, above Brandwacht, lower
slopes facing west, wet streamside, (— DD), Oliver 9028 (PRE). 3319
(Worcester): Tulbagh Dist., Sneeugat Valley, (— AA), Thome CH 2877
(PRE); Groot Drakenstein Mountains, (— CC), Primos CH 1504 (PRE).
3320 (Montagu): Tradouw Pass, S of Barrydale near waterfall in forest-
ed kloof, (-DC), Magill 6174 (PRE). 3321 (Ladismith): Seven Weeks
Poort, (—AD), Thome CH 1543 (PRE). 3322 (Oudtshoom): Meiring-
spoort, in deep shade in cracks of vertical rock wall, almost under water-
fall, (— BC), Jacobsen 2253 (PRE); Montagu Pass, wet rock face near
Stinkhoutdraai, (—CD), S.M. Perold 1547 (PRE); The Wilderness, Ge-
orge, (—CD), Taylor CH 1519 (PRE); Saasveld, Groeneweide, (—DC),
Koekemoer 994 (PRE). 3326 (Fort Beaufort): near Grahamstown,
Paradise Kloof, Coldstream, (— BC), Hilner CH 1499 (PRE). 3227
(Stutterheim): Hogsback, (— CA), Van der Bijl CH 1497 (PRE); Hogsback,
in shade, streambank, (— CA), Young CH 1507 (PRE); Evelyn Valley,
(— CB), T.R. Sim CH 1522 (PRE). 3418 (Simonstown): kloof near Chaplin
Point, (— AB), T.R. Sim CH 1501 (PRE); Kogelberg, near Gordon’s Bay,
(-BB), Mogg CH 939 (PRE); Hottentot Hollands Mts, (— BB), Thome
CH 3096 (PRE). 3419 (Caledon): Riviera Kloof, Herman us Dist., (—AC),
Louwrens CH 2889 (PRE); Mossel River, (—AD), Potts 26 (PRE);
Oudebos, Zonder Einde, (— BB), Thome CH 3106 (PRE).
Pallavicinia lyellii (Hook.) Car ruth, in Journal of
Botany, British and Foreign 3: 302 (1865) ( Pallavicinius)\
Sim: 32 (1926); Muller: 519 (1951-1958); Hassel: 264
(1961b); Hodgson: 223 (1968); Grolle & Piippo: 60 (1986).
Jungermannia lyellii Hook.: tab. 77 (1816). Type: England, Hamp-
shire, New Forest, ‘Cadman bog’, 6 May 1812, Lyell (BM, lecto. fide
Grolle & Piippo 1986).
Pallavicinia pilifera Steph.: 271 (1891); Steph.: 10(1900); Amell: 112
(1963); Vanden Berghen: 164 (1965). Type: W Africa. Sao Tome Island,
Quintas (G 12058) (G, holo.; G, M, S, W, syn.). Synonymy fide Vanden
Berghen: 150 (1972).
For detailed synonymy see Grolle & Piippo (1986).
Terricolous, growing on damp soil; thallus, prostrate
and creeping (Figure 6A), in crowded, overlying,
caespitose mats, dark green, mostly simple, occasionally
dichotomously branched, or ventrally from the midrib,
medium-sized to large, up to 60 x (2.0— )4. 0—6.5 mm,
320—350 gm thick over ventrally bulging costa from
20
Bothalia 23,1 (1993)
which, at intervals, arise dense reddish brown, smooth,
translucent rhizoids 12.5—20.0 /xm wide; central conduct-
ing strand brown, clearly visible from above, forking at
dichotomies; apex entire or with shallow notch, bearing
2-celled slime papillae (Figure 5F), also along margins
of wings, which are undulating, almost entire or with
remote teeth, expanded bilaterally from wingless stipe,
375 x 750 (im in transverse section. Wings unistratose.
bordered by a row of mostly long-rectangular or 5-sided
cells (27.5— )50.0— 62.5 x 27.5—45.0 /xm, marginal teeth
generally small and blunt (Figure 5D), only 1- or 2-celled,
25.0 x 37.5 /xm, toward apex often larger, up to 5-celled,
forwardly directed (Figure 5E); laminal cells polygonal,
some hexagonal, 57.5—87.5 x 27.5—45.0 /xm, in transverse
section 42.5 /xm thick, containing numerous chloro-
plasts, 5.0— 7.5 /xm, oil bodies green, nodular, 8—12 per cell
FIGURE 5 .—Pallavicinia lyellii , plants and androecia. A, male branch with androecia laterally situated above costa; B, male scales more enlarged;
C, part of male scale, excised; D, margin of lobe, with blunt tooth; E, long marginal tooth, near apex; F, notched apex with 2-celled slime
papillae, and long marginal teeth; G, laminal cells from above, containing chloroplasts and rod-like oil bodies; H, transverse section of
costa and central conducting strand, much enlarged; I, transverse section of costa and wing on one side only. A-C, Glen 2882: D-I,
Koekemoer 990. A, x 30; B, X 70; C, x 165; D, x 250; E, F, H, X 125; G, x 500; I, x 25.
Bothalia 23,1 (1993)
21
FIGURE 6 .—Pallavicinia lyellii, female plants. A, lobe with gynoecia along costa; B, involucre much enlarged; C, opened involucre spread out;
D, lobe with capsule still enclosed in pseudoperianth; E, calyptra; F, pseudoperianth; G, transverse section of capsule wall; H, outer cells
of capsule wall; I, transverse section of seta; J, elater and spore. A— C, Koekemoer 990 ; D— F, I, Glen 2882\ G, H, J, Amell 2084. A,
-x 5.5; B, x 55; C, x 70; D, x 11; E, F, x 30; G, H, J, x 250; I, x 80.
(Figure 5G), up to 7.5 /tm long, thin, others seen end-on
and round. Costa abruptly grading into wings, overlying
epidermal cells long-rectangular, 65 — 110 x 21—30 /tm,
sometimes with slime papillae, central conducting strand
50 x 80—125 /tm, consisting of about 32 small, ± 10 /tm
wide, thick-walled, angular brown cells, surrounded by
larger, 35—55 /tm wide, thin-walled parenchymatous cells,
3 rows above and 4 or 5 rows below (Figure 5H).
22
Bothalia 23,1 (1993)
Dioicous. Androecia in 2 parallel dorsal rows, one on
either side of costa (Figure 5A), each a flat band raised
shelflike ± 100 pm above lamina and ± 280 pm wide,
laterally at free margin, expanded into confluent scales,
directed transversely to long axis of shoot (Figure 5B),
210 x 200 pm, with laciniae (l-)2- or 3-celled (Figure 5C),
± 150 x 40 /im; antheridia globular, 170 p m wide, short-
stalked and individually placed, hidden by covering scale,
central area above midrib lacking antheridia and scales.
Gynoecia up to 4 or 5 per frond (Figure 6A), acropetally
arranged and dorsally situated at intervals along costa,
involucre 3—5 layers thick, cup-like, base + 900 pm high,
mouth densely fringed with ciliate laciniae up to 750 pm
long (Figure 6B, C), enclosing a group of 20—30 archego-
nia. Pseudoperianth 6 mm long, tubular (Figure 6F), apex
brownish, long-piliferous (Figure 6D), developing after
fertilization of an archegonium; calyptra (Figure 6E) bis-
tratose, initially enveloping capsule and seta, several un-
fertilized archegonia flattened against sides and at base,
old archegonial neck retained at tip. Capsule oblong-
cylindrical, 2.3— 3.7 mm long, opening along several
valves; wall yellow-brown, 2 cell layers thick (only 1 shown
in Figure 6G); outer cells elongate, 87.5—150.0 x
12.5—22.5 pm, lacking semi-annular thickenings (Figure
6H). Seta with slight swelling at foot, eventually up to 9
mm long, sinuate, 500 pm in diameter, cortical cells
darker, one cell deep, ± 35 x 35 pm, in 45 cell rows;
medullary cells ± 70, + 35 —60 (im wide (Figure 61).
Spores light brown, + globular, 17.5— 23.0 /xm in di-
ameter, ornamentation reticulate with larger areolae on dis-
tal face ± 5 pm wide, further subdivided into smaller
areolae by finer walls (Figure 7A— D); proximal face with
only smaller, irregular areolae (Figure 7C— E). Elaters
light brown, tapering toward ends, up to 470 pm long, 7.5
pm thick, bispiral (Figures 6J; 7F).
northern and central Transvaal, Natal, and southwestern,
southern and eastern Cape (Figure 4), but not many
collections have been made. It is probably more common,
but is undercollected.
The very large number of synonyms listed by Grolle &
Piippo (1986) are an indication of its variability, resulting
from its plasticity. Fertile plants are rare, with male plants
generally smaller and abruptly narrowing to the apex of
the lobe. The marginal teeth are quite variable: mostly
small and blunt, but sometimes up to 5 cells long. In
colour, plants are a deeper green than those of Sym-
phyogyna species and further differ by the androecial
arrangement, by the cup-like involucre, short calyptra, the
presence of a pseudoperianth and by the spore ornamen-
tation. The plants described and illustrated as Pallavinicia
lyellii by Sim (1926) are clearly those of Symphyogyna
brasiliensis.
SPECIMENS EXAMINED
TRANSVAAL. — 2330 (Tzaneen): De Hoek State Forest, Grootbosch
Hiking Trail, + 6.5 km from starting point, (— CC), Koekemoer 990
(PRE). 2430 (Pilgrim’s Rest): Graskop, Fairyland, occasionally on dry
stream bank, (— DD), Glen 2975 (PRE); Mariepskop, Blyde River
footpath, on sandstone slab in forest, (-DB), Vorster 1499 (PRE). 2527
(Rustenburg): Rustenburg Nature Reserve, Cederbergkloof near Utopia,
(— CA), Koekemoer 971 (PRE).
NATAL. — 2731 (Louwsburg): Louwsburg Dist., Ngome Forest,
Cetshwayo waterfall walk, (—CD), Glen 2882 (PRE). 2930 (Pietermaritz-
burg): Blinkwater, (— AB), J.M. Sim CH 1456 (PRE).
CAPE.— 3318 (Cape Town): Table Mountain, (—CD), Michell CH 1481
(PRE). 3322 (Oudtshoorn): George, Van Riebeeck Gardens, on damp
streambank, (—CD), S.M. Perolcl 927 ( PRE). 3326 (Grahamstown): Para-
dise Kloof, Cold spring, near Grahamstown, (— BC), Hilner CH 1478
(PRE). 3423 (Knysna): Knysna, BuffelstNek, streamside, (— AA), S.
Arnell 1515 (PRE); Knysna, Garden of Eden, (— AA), S. Arnell 2084
(PRE).
DISCUSSION
ACKNOWLEDGEMENTS
Pallavicinia lyellii is widely distributed and regarded
as subcosmopolitan. In southern Africa it is known from
I wish to express my gratitude to the following: Dr E.O.
Campbell and Dr R. Grolle for refereeing the manuscript
FIGURE 1. —Pallavicinia lyellii, spores and elaters. A, B, distal face; C, D, side view; E, proximal face; F, elater. A-F, S. Arnell 2084. A,
B, D, x 1850; C, E, x 1905; F, x 189.
Bothalia 23,1 (1993)
23
and for their helpful suggestions; to my colleagues at
NBI, Ms Koekemoer and Dr H.F. Glen, for collecting
specimens; to Mrs A. Romanowski, photographer, for
developing and printing the photographs (taken by the
author) and to Mrs J. Mulvenna, typist, for her valued
contribution.
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Bothalia 23,1: 25-47 (1993)
A biosystematic study of Pentameris (Arundineae, Poaceae)
N.P. BARKER*
Keywords: Arundineae, Arundinoideae, cladistics, conservation status, cytology, leaf anatomy, Pentameris, phylogeny, systematics
This paper is dedicated to the memory of Lucy K.A. Crook (nee Chippindall)
ABSTRACT
A biosystematic study of the endemic southwestern Cape grass genus Pentameris Beauv. is presented. Results of studies
on the macro- and micromorphology, leaf blade anatomy and cytology are discussed and illustrated . The results of a cladistic
study indicate that the genus is monophyletic, united by the synapomorphies of ovary and fruit characters. The conservation
status of the taxa in the genus is assessed, and conservation status codes allocated. A key to the taxa in the genus is presented,
and each species is described. Five new species, Pentameris glacialis N.P. Barker, P. hirtiglumis N.P. Barker, P. oreophila
N.P. Barker, P swart be rgensis N.P. Barker and P. uniflora N.P. Barker, and one new subspecies, P longiglumis (Nees)
Stapf subsp. gymnocolea N.P. Barker, are described and illustrated.
UITTREKSEL
’n Biosistematiese ondersoek van die endemiese Suidwes-Kaapse grasgenus Pentameris Beauv. word aangebied. Resultate
van ondersoeke op die makro- en mikromorfologie, blaarskyfanatomie en sitologie word bespreek en gefllustreer. Die resultate
van ’n kladistiese ondersoek dui daarop dat die genus monofileties is, verenig deur die afgeleide kenmerke van die vrugbeginsel
en vrug. Die bewaringstatus van die taksons in die genus word geraam en bewaringstatuskodes toegeken. ’n Sleutel tot die
taksons in die genus word aangebied, en elke spesie word beskryf. Vyf nuwe spesies, Pentameris glacialis N.P. Barker,
P. hirtiglumis N.P. Barker, P oreophila N.P. Barker, P. swartbergensis N.P. Barker en P. uniflora N.P. Barker, en een
nuwe subspesie, P. longiglumis (Nees) Stapf subsp. gymnocolea N.P. Barker, word beskryf en geillustreer.
CONTENTS
Introduction 25
Morphology 25
Leaf blade anatomy 29
Microhairs 29
Abaxial macrohairs 29
Adaxial macrohairs 30
Prickles 30
Cytology 31
Phylogeny 31
Choice of outgroup 31
Character distribution 32
Taxonomic implications 33
Conservation status 33
Taxonomy 33
Acknowledgements 44
References 46
INTRODUCTION
The genus Pentameris Beauv. occurs in the winter
rainfall region of the Cape Province, South Africa, where
it is restricted to soils derived from Table Mountain
Sandstone or the shale bands associated with this geology.
It may therefore be considered an endemic of the Cape
Flora (Goldblatt 1978). All known species of the genus
are perennial C3 plants.
The genus was erected by Palisot de Beauvois in 1812
on the basis of a specimen sent to him by Du Petit-Thouars.
No collection number or locality is provided in this
description. However, it is known that Du Petit-Thouars,
* National Botanical Institute, Private Bag X101, Pretoria 0001. Present
address: Botany Department, University of Cape Town, Private Bag, Ron-
debosch, Cape Town 7700.
MS. received: 1992-02-20.
a French traveller and botanist, obtained material from the
Cape during a visit in February 1793 (Gunn & Codd 1981).
The genus name is Greek, meaning ‘five parts’, probably
a reference to the apical region of the lemma which is
divided into what Palisot De Beauvois (1812) described as
four bristles (two of which may be more accurately
described as lemma lobes) and a central awn.
Only one species is mentioned under the generic
description: P. thuarii Beauv. (Palisot de Beauvois /.c).
This single species was subsequently placed in Dantho-
nia DC. by a number of early taxonomists (Desvaux 1831;
Nees 1841; Steudel 1855; Durand & Schinz 1895), whereas
others retained it in the genus Pentameris (Roemer &
Schultes 1817; Kunth 1833, 1835). Stapf (1897) expanded
the genus Pentameris to include four other taxa, all charac-
terised by fruit with a free pericarp. Chippindall (1955)
retained the genus in this format, but incorporated two
nomenclatural corrections published by Schweickerdt
(1938). Gibbs Russell et al. (1985) list these five taxa as
Pentameris dregeana Stapf, P longiglumis (Nees) Stapf,
P macrocalycina (Steud.) Schweick., P. obtusifolia (Hochst.)
Schweick. and P thuarii Beauv.
However, the unusual leaf blade anatomy (Ellis 1985d;
Barker 1990) and fruit morphology (Barker 1986, 1989,
1990) of P. obtusifolia places this species within the genus
Pseudopentameris Conert (Barker in prep.a). Pentameris
obtusifolia is therefore not further considered in this study.
MORPHOLOGY
The basal parts of all the species are woody, but the
woolly and/or swollen underground parts that occur
in certain species of Pentaschistis (Nees) Spach and
Merxmuellera Conert are absent. The species are generally
tufted, with stems sometimes branching, but generally only
26
Bothalia 23,1 (1993)
in the basal quarter. In older plants branching results in
a cushion or a bush-like growth form. These branched
structures are referred to here as ‘culms’, although they
do not possess typical culm anatomy. Instead, the anatomy
resembles that of a rhizome (H.P. Linder pers. comm.).
The term ‘aerial culm’ will be used here to denote the
annually produced, few-noded structure which terminates
in an inflorescence.
In P. thuarii, branching can occur at any node on the
culm, and some specimens comprise long, decumbent,
scandent or vertical culms with many shorter vegetative
and reproductive branches arising from the upper regions.
Such branching from cauline innovation shoots results in
an ‘evergreen’, perennial plant, which takes the form of
a divaricate herb. This branching pattern might allow the
plant to grow taller than species possessing only basal
innovation shoots (Linder & Ellis 1990a). Branching and
growth from cauline innovation shoots is also found in a
few species of Pentaschistis, Chaetobromus Nees and
Pseudopentameris . In the latter genus the branched
condition may approximate the extreme development found
in Pentameris thuarii.
The leaf structure of Pentameris is typical of the
Arundineae. The leaf sheaths are persistent, although the
leaf blades may not be. The older culms are thus frequently
covered in the remains of sheaths from previous years of
growth. These sheaths may be appressed to or free from
the culm. The sheath indumentum varies between the spe-
cies, ranging from glabrous to pubescent along the mar-
gins to uniformly pubescent (and sometimes woolly).
These sheath characters are also found in other arundi-
noid genera. The ligule is, as in many other arundinoid
genera, a fringe of hairs. The sheath mouth may be beard-
ed in some species, but this, too, is not unusual. Two spe-
cies, P thuarii and P longiglumis have fairly
well-developed auricles. In the former species these are
a characteristic purple or brown colour. The leaf blade
varies in its internal and epidermal anatomy. Many charac-
ters are shared, although not consistently so, with taxa of
Pentaschistis, and (to a lesser extent) Merxmuellera. Ellis
(1985c, 1986; Ellis & Linder 1992), on the basis of leaf
anatomical studies, is of the opinion that Pentameris is
closely allied to Pentaschistis.
The inflorescence is a panicle which varies from com-
pactly lanceolate to laxly globose. It must, however, be
noted that the panicles of all the species are open and
somewhat lax during the period of pollination. Before and
after this period, the panicles contract to a lanceolate
shape. Panicle shape is therefore difficult to describe as
it depends on the reproductive phase of the plant at the
time of observation or collection. This variation is also
found in numerous other arundinoid taxa, for example
Pentaschistis (Linder & Ellis 1990b). No spicate panicles
are known from this genus.
The spikelets are two-flowered (one exception; P.
uniflora), and the partially developed remains of a third
floret may sometimes be present, particularly in P.
macrocalycina. The two-flowered state is shared with
the vast majority of the species in Pentaschistis (Linder
& Ellis 1990b). When two florets are present, the basal
floret is sessile, the apical floret pedicellate. The florets
are otherwise morphologically identical, and both are
hermaphroditic and fertile, as in Pentaschistis.
The lemma is generally nine- to eleven-nerved. The
majority of the veins anastomose in the basal region of
the central awn and the two lateral bristles. The lemma
lobes on the outside of the bristles are variously adnate
to the bristle, ranging from free (in P. thuarii) to almost
completely adnate (in P. macrocalycina). The shape of this
lobe is also variable, being acuminate, acute or dentate.
Similar variation is found in Pentaschistis (Linder & Ellis
1990b). The central awn is geniculate in all species, the
basal portion is flattened but twisted and shorter than the
attenuating apical portion. The margin of both the basal
and apical regions of the awn are finely serrated. This awn
structure is shared with genera such as Pentaschistis,
Pseudopentameris, Merxmuellera and Chaetobromus as
well as the non-African genus Danthonia.
The palea is bicarinate, apically bilobed and pubescent
between the veins. It exceeds the lemma body in length,
but seldom exceeds the lemma lobes, a situation also found
in species of Pentaschistis, Pseudopentameris and Merx-
muellera.
The lodicules in certain arundinoid genera have been
examined and used for taxonomic purposes (Tomlinson
1985). The lodicules of Pentameris are generally glabrous
and cuneate, but differences have been noted in some
specimens of P. swartbergensis and P distichophylla. The
lodicules in these species are generally apically ciliolate,
and sometimes an arm-like extension arising from one of
the lateral margins is present. Ciliolate lodicules are also
known from species of Pseudopentameris, Merxmuellera
and Pentaschistis (Linder & Ellis 1990b).
All species of the genus have three anthers, which are
usually purple in colour. These vary in size in relation to
the size differences of the florets, but this has not been
incorporated as a taxonomically meaningful character.
The above morphological features can therefore not be
used to clearly differentiate Pentameris from several other
southern African arundinoid genera, notably Pentaschistis.
There are, however, two micromorphological features
which have, in the past, been used to distinguish Penta-
meris from all other southern African arundinoids. Both
features are characters of fruit and ovary. Firstly, the fruit
is an achene, and secondly, the fruit of all taxa possesses
a dense tuft of hairs at the apex of the ovary. These hairs
are retained in developing and mature fruit where they
become reluctantly deciduous.
Stapf (1897: 512) separated Pentameris from Pentaschistis
on the basis of fruit morphology: the crustaceous pericarp
and free seed. He described the structure of the ovary as
being ‘. . . so alike in the five species of this genus that it
is very probable that they agree in the peculiarities of the
ripe fruit which is known only in P. thuarii' and further
stated that ‘... there is in Pentaschistis no approach to
the characteristic structure of the ovary and the fruit of
Pentameris .’
This unusual fruit type, the achene, is described by
Clayton & Renvoize (1986) as a fruit with a thin, hard,
free pericarp attached to the ovule in the region of the
hilum. It is unusual in the tribe Arundineae, and is found
in only three of the approximately 40 arundinoid genera
worldwide. The fruits of the remaining arundinoid genera
are described as caryopses or as caryopses with a variably
separable pericarp (Clayton & Renvoize l.c.).
Bothalia 23,1 (1993)
27
FIGURE 1 .—Pentameris; A, B, SEM of fruit; C— F, SEM of leaf blade. A, P. hirtiglumis N.P. Barker, whole fruit, note colliculate surface features
and apical hairs. B, D, F, P. thuarii Beauv.: B, longitudinal section; D, furrow on adaxial surface; F, ad axial surface showing ribs over
vascular bundles and open furrows between ribs. Note abundance of conventional macrohairs and slightly inclined, sparsely distributed prickles.
C, P. distichophylla (Lehm.) Nees, adaxial microhair. E, P. oreophila N.P. Barker, magnified view of deflated apical cell of adaxial microhair.
Ac, small deflated apical cell; Ah, apical hairs; Be, long basal cell; E, embryo; Em, endosperm; H, hilum; Ma, macrohair, basal portion;
Mi, microhair; P, prickles; Pe, free crustaceous pericarp, seed within; S, stomata. Scale bars: A, 390 /im; B, 541 fan; C, 19 pm; D, 33
/im; E, 6 jim; F, 550 pm.
Scanning electron microscope (SEM) studies on the fruit
of Pentameris have shown the pericarp to be sculptured
(Barker 1986, 1989, 1990) as illustrated here in Figure 1A,
and partly or almost completely free from the seed coat
when viewed in section (Barker 1990) as shown here in
Figure IB. The colliculate surface sculpturing is also
unique among the fruit of the southern African genera of
the Arundineae (Barker in prep. b).
The second feature that characterises the genus is the
presence of hairs on the apical region of the ovary and
fruit. This was first observed by Palisot de Beauvois (1812),
who described the fruit as being crowned with stellate
hairs. Nees (1841) also noted this feature in his descrip-
tions of P. thuarii and the taxon now known as P
macrocalycina. Phillips (1931) considered these hairs to
be characteristic of the genus, using this feature in his
TABLE 1.— Salient anatomical characters differentiating the species of Pentameris. All measurements in micrometres
28
Bothalia 23,1 (1993)
primary vascular bundles; 3' = tertiary vascular bundles.
Bothalia 23,1 (1993)
29
key to the grass genera. Chippindall (1955) describes
Pentameris as having an ovary which is hairy on top, the
hairs being deciduous. This character was also used in the
key to the genera of the tribe Danthonieae. The nature of
these unusual structures has been clarified to a certain
extent by Barker (1986, 1989, 1990), but their ontogeny
and function is not known. These structures, visible on
the apex of the fruit (Figure 1A) appear to be unicellular,
and arise from the apex of the ovule around the base of
the styles.
LEAF BLADE ANATOMY
Leaf blade anatomy has contributed much to the tribal
and subfamilial classification of the grass family. However,
within the tribe Arundineae, the variation of observed
anatomical characters led Renvoize (1981) to comment that
the arundinoid genera could not be readily divided into
the tribal groups on the basis of their leaf anatomy, and
he concluded that other characters such as spikelet
morphology would have to be used to divide the subfamily
further.
The leaf blade anatomy of many of the southern African
arundinoid genera has been documented (Schweickerdt
1942; De Wet 1956; Conert & Tuerpe 1969; Ellis 1980;
1981; 1985a— d).
Ellis (1985a— d, 1986) examined many specimens of
the then five known and one undescribed species of
Pentameris. Additional anatomical information for the new
and undersampled species was obtained by sectioning a
small portion of leaf material obtained from herbarium
specimens. This material was heated in a soapy solution
prior to sectioning by means of a sledge microtome.
Sections thus obtained were 30 to 50 microns thick. The
sections were stained in safranin and fast green and
mounted in Euparol.
To complement the data obtained from the work of Ellis
(1985a-d, 1986) and additional sections, leaf material
from 95 of these previously studied specimens was
prepared from herbarium specimens, mounted on two-
sided tape, coated in gold-palladium and examined using
a ISI-SX-25 scanning electron microscope. The salient
anatomical features obtained from the SEM and light
microscope studies are presented in Table 1.
The abaxial surface is relatively uniform throughout the
genus. It is generally smooth, with ribs observed only
occasionally. No abaxial microhairs or stomata are present,
and the silica bodies are usually rounded, but are tall and
narrow in P thuarii (Ellis 1985b— d, 1986). Abaxial
macrohairs were occasionally present in specimens of
some taxa (Table 1). The adaxial epidermis is far better
endowed with micromorphological structures, including
prickles, microhairs and macrohairs. These epidermal
features are discussed in some detail below.
Microhairs
The genus Pentameris has a ‘festucoid’ type of leaf
epidermis and leaf anatomy (implying the absence of
abaxial microhairs), a poorly differentiated parenchyma
sheath and evenly distributed chlorenchyma sheath (De
Wet 1956). However, Renvoize (1986) places Pentameris
in the ‘core’ of the arundinoids, a group possessing micro-
hairs, and describes the lower epidermis of Pentameris and
Pseudopentameris as possessing long slender papillae
which occasionally bear the remains of a small thin-walled
apical cell. Clayton & Renvoize (1986) note that these
structures distinguish these genera (and certain others such
as Cortaderia Stapf and Centropodia Reichb. f.) from the
rest of the Arundineae.
These ‘papillae’, as described by Renvoize (1986) and
Clayton & Renvoize (1986), appear to differ from those
described by Ellis (1979), who considers papillae to be
protuberances of the cell wall rather than structures
consisting of separate cells. From observations discussed
below, it appears that Renvoize is using the term ‘papillae’
to describe what others, such as De Wet (1956) and Ellis
(1979), call microhairs.
In addition to their structure and appellation, the
recorded distribution of these microhairs is also controver-
sial. Renvoize (1986, discussed above) reported them from
the lower (abaxial) surface of specimens of Pentameris.
However, Ellis (1985a-d, 1986) has found no evidence
of abaxial microhairs on any of the specimens he has
examined. Microhairs were however found on the sides
and bottoms of the furrows of the adaxial surfaces of many
specimens in all the taxa observed (Ellis l.c.). My obser-
vations on material examined, using the SEM, corroborate
Ellis’s observations, and it is clear that there are no abaxial
microhairs present in any of the species of Pentameris.
As illustrated in Figure 1C, D and E, these microhairs
are indeed bicellular, with a minute, deflated apical cell
(shown at high magnification in Figure IE). The length
of the basal cell varies, but it is always very much longer
than the apical cell. Microhairs with this structure were
found on the adaxial surface of all specimens of all taxa
in Pentameris (Barker 1990), and were also reported from
certain species of Pentaschistis (Ellis & Linder 1992).
In addition to their distribution and morphology, varia-
tion in the size of the microhairs is taxonomically useful.
The microhairs were measured from a number of SEM
micrographs in order to determine whether or not there
was any measurable size difference. These varying sizes
are recorded in Table 1. Unfortunately, the limited sample
size does not allow a statistically meaningful compari-
son to be carried out on this potentially very valuable
taxonomic character.
The definite bicellular nature of these microhairs is
comparable to those reported and illustrated by
Amarasinghe & Watson (1988, 1989). However, microhairs
with such unequal cell sizes have not been previously
documented, and perhaps merit recognition as a separate
type of microhair, the ‘pentameroid’ type.
Abaxial macrohairs
Abaxial macrohairs were only observed on the abaxial
surface of some specimens of Pentameris distichophylla,
P. hirtiglumis and P. glacialis. In all these taxa, the hairs
were long, usually produced from the intercostal regions,
had a distinctly swollen base and were surrounded by four
or more cells, termed ‘modified cells’ by Ellis (1986).
The taxonomic value of these structures is limited, as it
30
Bothalia 23,1 (1993)
appears that they are not universally present throughout
all specimens examined of all taxa. Inconsistent sampling
(variation in the region of the leaf from which the samples
were taken, or the age of the leaf blade) may explain the
lack of macrohairs in some samples.
Adaxial macrohairs
Two different hair-like structures were found on the
adaxial leaf surface in some of the taxa of Pentameris,
sometimes both occurring on the same leaf. Conventional
macrohairs, those which have a distinct basal structure
comprised of modified cells, were frequently observed on
the adaxial epidermis in Pentameris thuarii, P glacialis
and P. distichophylla , but were only occasional in P.
swartbergensis. Figure IF illustrates these hairs on the
adaxial leaf blade surface in P thuarii.
The second type of macrohair, termed here a ‘filament’,
is a long, unicellular hair without any obvious basal
differentiation or associated cells. Although no measure-
ments were taken, the filament type of macrohair appeared
to be shorter than the conventional type. Filaments were
frequently observed in the bottom of the adaxial furrows
in specimens of P macrocalycina and occasionally in P.
distichophylla and P. swartbergensis. In P. oreophila
filaments were only found in the furrow nearest the edge
of the lamina. One of these filaments observed in P.
distichophylla is shown in Figure 2A.
Adaxial macrohairs are of slightly greater taxonomic
significance than abaxial macrohairs. The presence and
type of macrohair are useful characters in Pentameris,
although some variability within the species exists. It
appears that the species with open or folded leaves (P.
thuarii, P. distichophylla and P. swartbergensis) possess
conventional macrohairs, whereas those taxa with perma-
nently rolled or folded leaf blades have the second type
of macrohair (P. macrocalycina, P. oreophila, P. disticho-
phylla and P. swartbergensis ). P. swartbergensis and P.
distichophylla thus have both types of macrohair. It is
possible that the filament macrohairs are conventional
macrohairs that have lost the modified cells around the
hair base. The loss of these modified cells may be related
to the evolution of the permanently rolled leaf blade, where
the adaxial surface is not as exposed to the environment.
Prickles
The adaxial surfaces of all the specimens examined had
prickles of one form or another. These different prickle
types (Table 1) are invariant within the taxa of the genus.
FIGURE 2.— Leaf blade SEM of Pentameris. A, P. distichophylla (Lehm.) Nees, adaxial surface; B, P. oreophila N.P. Barker, adaxial surface,
note extreme length of prickles and presence of collar at base of each prickle; C, P. longiglumis (Nees) Stapf subsp. gymnocolea N.R
Barker, adaxial surface, note extreme density and inclination of prickles; D, P. uniflora N.P. Barker, adaxial surface showing prickles
and small microhairs. C, collar; P, prickles; Ma, macrohairs; Mi, microhairs; S, stomata. Scale bars: A, 48 /cm; B, 50 ^m; C, 87 fun;
D, 120 ^m.
Bothalia 23,1 (1993)
31
Characters such as prickle density, distribution, orienta-
tion, length and structural differences are all taxonom-
ically useful for distinguishing taxa within Pentameris
(Figure 2A— D).
The prickles of P. oreophila are long and erect, with
the tips sometimes bent or recurved. In addition to
their unusual length, the prickles possess a basal collar-
like structure (Figure 2B), a character shared with P.
hirtiglumis. The prickles of the latter species are, however,
much shorter, and are almost appressed to the surface of
the leaf, a character shared with P. longiglumis (Figure
2C).
Of the remaining species, P. macro calycina, P. thuarii,
P. glacialis and P. swartbergensis have short, erect
prickles, the tips of which may be bent or curved; are
swollen basally, and the sides are convexly shaped; are
densely distributed, particularly so in P macrocalycina.
The prickles of P. uniflora are also quite densely
distributed and almost erect, as indicated in Figure 2D.
In contrast to the above, P. distichophylla has erect
prickles that are almost straight-sided (as opposed to the
slightly inflated convex sides of the prickles of the other
taxa); they appear to have knobbed tips (Figure 2A) and
are sparsely distributed over the adaxial surface, usually
only on the edges of the ribs. Both the short, inflated
prickle type and the erect, knobbed prickle type have also
been observed in species of Pentaschistis, for example
P. colorata (Ellis & Linder 1992). The long, collared
prickles observed in P. oreophila are unique among the
African Arundineae.
CYTOLOGY
Preliminary cytological studies have shown that
Pentameris distichophylla has a chromosome count of
2n=36, whereas P. thuarii has a count of 2n=12. The
latter figure has been corroborated by H. du Plessis
(pers. comm.). Both these counts were obtained from
meiotic material. P. distichophylla is therefore hexaploid.
Such polyploidy is not unusual in the southern African
Arundineae (see for example counts for Merxmuellera,
Pentaschistis and other genera given by Du Plessis & Spies
1988; Spies & Du Plessis 1988; Spies et al. 1990).
These counts further support the contention that the base
chromosome number for the Arundineae appears to be
x=6 (Davidse 1988), and not x=12 as proposed by Clayton
& Renvoize (1986). Despite the apparent similarities
between Pentameris and Pentaschistis, the different base
chromosome number of the latter genus (x=7 in many of
the known instances) does not suggest a close relation-
ship between these two taxa. It is, however, possible that
Pentameris evolved by means of aneuploidy from a
pentaschistoid ancestor.
PHYLOGENY
The data presented in Table 1 were converted into a data
set suitable for cladistic analysis. The anatomical
characters were augmented by a few morphological
characters, resulting in a data set of 26 characters
(presented in Tables 2 & 3). Four of these characters are
TABLE 2. — Characters used in the cladistic analysis. 1’ = primary
vascular bundles, 3’ = tertiary vascular bundles
Leaf blade characters (t/s)
1. Leaf blade shape in t/s: 0 = flat to curled, 1 = rolled,
2 = permanently rolled
2. 1’ rib shape: 0 = squared, 1 = round
3. 3’ rib shape: 0 = squared, 1 = round, 2 = conical
4. Relative rib depth: 0 = 1’ = 3’, 1 = T <3’
5. Furrow depth: 0 = shallow (<'/2 lamina thickness) 1 = deep
6. Furrow width: 0 = narrow, 1 = wide
7. 1’ Abaxial sclerenchyma girder: 0 = discrete, 1 = continuous
with hypodermis
8. Sclerenchyma cap on leaf margin: 0 = discrete, 1 =
continuous with hypodermis
9. Leaf blade thickness: 0 = uniform thickness, 1 = swollen
near margin
10. Abaxial epidermal cells: 0 = small (< = 25 /im wide),
1 = inflated
11. Silica body shape: 0 = round, 1 = dumbbell-shaped
Adaxial epidermal characters
12. Conventional macrohair type: 0 = absent, 1 = present
13. Filament macrohair type: 0 = absent, 1 = present
14. Prickle type: 0 = inflated basally, 1 = markedly elongated,
2 = apically knobbed
15. Prickle orientation: 0 = erect, 1 = inclined/appressed
16. Prickle base: 0 = unomamented, 1 = collar present
17. Prickle density: 0 = sparse, 1 = dense
18. Microhair type: 0 = basal cell length » apical cell length
1 = basal cell length = apical cell length
19. Microhair length: 0 = short ( < 60 jim), 1 = long
20. Papillae: 0 = absent, 1 = present
Morphological characters
21. Growth form: 0 = unbranched, 1 = branched
22. Glands: 0 = absent, 1 = present
23. Lodicule margin: 0 = entire, 1 = ciliolate
24. Achene surface: 0 = rugose, 1 = colliculate, 2 = reticulate
25. Fruit type: 0 = caryopsis, 1 = achene
26. Ovary appendages: 0 = absent, 1 = present
multistate, and are treated as undirectional in the analysis.
The ‘ie’ option of the cladistic package HENNIG86 version
1.5 was used to analyse the data. Using this method, the
complete set of most parsimonious trees is found (Platnick
1989).
Choice of outgroup
Pentaschistis is the obvious outgroup, although the
recognition of a particular species or group of species
within this genus as the closest to the study group is not
possible on an a priori basis. Six species of Pentaschistis
were therefore chosen as possible outgroup taxa. These
taxa were chosen on the basis of inferences made by Ellis
in his anatomical papers (1985c, 1986), and after discus-
sions with Dr H. P. Linder. The taxa chosen were P. aspera
(Thunb.) Stapf, P. colorata (Steud.) Stapf, P. curvifolia
(Schrad.) Stapf, P. eriostoma (Nees) Stapf, P. glandulosa
(Schrad.) Linder and P. tortuosa (Trin.) Stapf.
Two of these taxa, the glandular P. glandulosa and P.
aspera, were included because they were considered to
be most dissimilar to the study group. Following the
outgroup substitution method of Donoghue & Cantino
(1984), these two least related glandular taxa were used
as the initial outgroup to determine the relationships
between the remaining taxa. Using this method, the single
32
Bothalia 23,1 (1993)
TABLE 3. —Data used in cladistic analyses. Characters marked by asterisks above the data set were removed in the data
set where Pentaschistis curvifolia was used as the outgroup (data set delimited below the dashed line). Characters
appear in the order presented above. The question mark (?) indicates absent data
or few non-study group taxa found to be most closely
related to the study group were then used to perform the
final cladistic analysis on the data set from which the other
outgroup taxa had been removed.
P. swartbergensis share a flat leaf blade with wide furrows
between the adaxial ribs (char. 6). P. glacialis and P.
thuarii share a character that has arisen in parallel else-
where: entire lodicule margins (char. 23).
When the two distantly related taxa are used as the out-
group, one shortest length tree (1. = 60, c.i. = 50, r.i.
= 67) is generated. In this tree (not presented), P. cur-
vifolia is the taxon most closely related to the study group,
and was used as the outgroup (the other Pentaschistis spe-
cies were removed from the data set); the data were re-
analysed after the autapomorphies and invariant charac-
ters had been removed. Once again, HENNIG86 found
one shortest tree, presented in Figure 3 (1. = 34, c.i. =
64, r.i. =70). The phylogeny of the study group in this
tree is identical to that obtained in the initial tree (not
presented) where the two glandular taxa are used as an
outgroup.
Character distribution
In discussing the distribution of the characters on the
tree, the characters from the complete database are used,
although in the smaller data set (where Pentaschistis
curvifolia is the outgroup) some are excluded because they
are constant or autapomorphic. The distribution of the
characters is shown on this tree (Figure 3).
The genus Pentameris is a monophyletic clade supported
by the ovule and fruit characters; the apical appendages
and the achene fruit type (char. 25 and 26, represented
by the star in Figure 3).
Within Pentameris, two smaller clades are recognised.
The first clade comprising P distichophylla, P. thuarii,
P. glacialis and P swartbergensis is supported by the
presence of conventional macrohairs on the adaxial surface
(char. 12). Within this group, P. distichophylla is basal
to the other three taxa and is characterised by the
autapomorhies of knobbed prickles (char. 14) , the rounded
ribs of the tertiary vascular bundles (char. 3) and the rugose
pericarp surface (char. 24). P. thuarii, P glacialis and
The other clade within the genus is supported by the
presence of dense prickles (char. 17), as well as other
characters which undergo reversals in some of the lower
P. glacialis
P. thuarii
P. swartbergensis
P. distichophylla
P. uniflora
P. longiglumis
P. hirtiglumis
P. macrocalycina
P. oreophila
FIGURE 3. — Shortest cladogram produced by HENNIG86 using the
‘ie’ option. The outgroup used was Pentaschistis curvifolia
(Schrad.) Stapf. Length = 34, c.i. = 64, r.i. = 70. Numbers
represent characters (given in Tables 2 & 3; ‘a’ = state 0, ‘b’
= state 1 and ‘c’ = state 2). Solid bars represent apomorphies,
parallel lines represent parallelisms and crosses represent character
state reversals. Star at base of Pentameris clade represents
apomorphic fruit characters: achene fruit type and presence of
apical hairs on ovary.
Bothalia 23,1 (1993)
33
clades (char. 10 and char. 13: abaxial epidermal cell width
and presence of filament macrohairs respectively). P.
unijlora is basal to this clade, characterised by the presence
of one floret (data not included in data set) and short micro-
hairs (char. 19). The remaining four taxa are united
by the presence of a continuous hypodermal band of
sclerenchyma which connects to the abaxial girders and
cap on the leaf margin (char. 7 and 8), and primary ribs
which are deeper than the tertiary ribs (char. 4). P.
longiglumis and P hirtiglumis both have enlarged or
swollen leaf blade margins (char. 9), as does the outgroup.
P. macrocalycina and P. oreophila share conical tertiary
ribs (char. 3) and permanently rolled leaf blades (char.
1). The latter species is distinguished by the autapomorphy
of long prickles (char. 14).
The low consistency index obtained from the analysis
of the complete data set (c.i.=50) indicates the homoplasy
present within the data set. This is further demonstrated
by the increase in the value of the consistency index with
the removal of all but the closest outgroup taxa (c.i. =64).
Characters which are synapomorphies in the reduced data
set are often homoplasic in the complete data set. For
example, the unequal primary and tertiary vascular bundle
thicknesses (char. 4) is a synapomorphic character for the
P. longiglumis, P hirtiglumis, P. macrocalycina and P.
oreophila clade in the analysis based on the reduced data
set. However, in the large data set, this character is also
present in Pentaschistis aspera, P. glandulosa, P. colorata
and P. tortuosa. Similar situations are found in other
characters. Such homoplasy has probably been one of the
root causes bedevilling the efforts of taxonomists, both past
and present, to find an equitable classification for this
group.
Taxonomic implications
The monophyletic status of Pentameris is supported by
the fruit and ovary characters. However, as Pentameris is
undoubtedly closely related to Pentaschistis (at least the
eglandular taxa), the possibility that the latter genus is
paraphyletic ought not to be ruled out. The observation
that Pentameris was placed within, and terminal to, the
Pentaschistis clade in the analysis of the complete data set
provides some evidence as to this possibility. If this is the
case, the name Pentameris would be retained for the
monophyletic assemblage containing the taxa with the
unique fruit characters, while other genera may have to
be erected to accommodate monophyletic groups within
the Pentaschistis assemblage. Only a detailed phylogenetic
study of both Pentaschistis and Pentameris can provide
sufficient data to properly test any hypothesis of paraphyly.
CONSERVATION STATUS
Of the previously known taxa of Pentameris , only P.
obtusifolia is listed in the Red Data Book as a rare,
threatened or extinct species, where it is listed under the
synonym ‘P. squarrosa ’ (Hall & Veldhuis 1985). The
conservation status for this taxon is given as ‘uncertain’.
However, as discussed above, the nomenclature of this
taxon has been found to be confused, and P. obtusifolia
is not included in the genus Pentameris.
Certain species of Pentameris nonetheless require
consideration and recognition as taxa requiring conserva-
tion. Most of the new taxa described below are known from
only a few localities, and should perhaps be regarded as
‘rare’. However, as many of these taxa are found in
inaccessible and thus rarely collected areas, the true
distribution is not fully known. In addition to the problem
of varying collecting intensity, the effects of fire on the
germination, growth and re-establishment of fynbos grass
species are poorly known. Linder & Ellis (1990a) discuss
the various strategies that fynbos grasses have evolved to
escape or adapt to fire. These authors note that grasses
appear in abundance in the first few years after fire, but
are then almost inevitably outcompeted by members of the
Restionaceae and woody fynbos elements. The collection
of fynbos grasses is therefore best carried out in areas that
have been burnt within the previous few years. Such areas
are not always attractive to collectors intent on obtaining
other woody or non-graminoid taxa. Mature, woody fyn-
bos may therefore hide many new or apparently rare grass
species which are present as dormant seeds or under-
ground vegetative structures. Actual species distributions
may therefore be wider than presently known.
In assessing conservation status of the taxa of Penta-
meris, the categories proposed by Rabinowitz (1981) and
modified by Karron (1987) will be used. These categories
record the geographic distribution, demographic structure
and habitat requirements in a two-state form: restricted
or widespread, sparse or abundant, wide or narrow respec-
tively. The demographic component can thus reflect, to
a certain extent, the biological aspects of rarity of the taxa.
As the category of geographic distribution is scale
dependent, it is used here at the level of magisterial
districts or mountain ranges, whichever is more geographi-
cally homogeneous. The allocations of the species of
Pentameris to these categories is presented in Table 4.
Detailed descriptions of distributions and habitats are
provided under individual species descriptions.
TAXONOMY
Taxonomic descriptions of all the taxa are presented.
The dimensions given below for the lemma body, lemma
TABLE 4.— The modified Rabinowitz conservation categories allocated
to each taxon of Pentameris. The allocation of these codes is based
on field observations and data obtained from labels on herbarium
specimens
A = abundant; N = narrow; R = restricted; S = sparse; W = wide;
WS = widespread.
34
Bothalia 23,1 (1993)
FIGURE 4 .—Pentameris uniflora N.P. Barker. A, habit with decumbent, branching culm basally covered in dead, appressed leaf sheaths;
B, ligule, which is a row of hairs, and surrounding leaf parts; C, panicle subcontracted to lax, with few spikelets. D— G, parts of spikelet
and florets: D, glumes; E, lemma (in its normal conformation) showing lemma bristles, lobes (which are adnate to the bristle for most
of their length) and geniculate awn; F, palea; G, ovary with apical hairs and stigmas. A, x 0.5; B, D-F, X 4.7; C, X 1.6; G, x 11.8.
Bothalia 23,1 (1993)
35
lobes and lateral bristles are measured as follows: the
lemma body is measured from the base to the lowermost
point of insertion of the central awn, whereas the lobes
and bristles are measured from this same insertion point
to the apex of the lobe or bristle. The full length of the
lemma (either from base to lobe apex or base to bristle
tip) can be obtained by adding the lemma body length to
the length of the lobe or bristle. The term ‘culm’ is used
in the descriptions below to describe all aerial parts
(branched stems and reproductive culms) despite the
anatomical discrepancies discussed in the introduction.
Pentameris Beauv. , Essai d’une Nouvelle Agrosto-
graphie: 92, t.18, fig.8 (1812); Kunth: 107 (1829); Kunth:
315 (1833); Nees: 336 (1841); Stapf: 512 (1897); Chippin-
dall: 251 (1955); Clayton & Renvoize: 174 (1986); Gibbs
Russell et al. : 251 (1990). Type species: Pentameris thuarii
Beauv.
Perennial; caespitose, cushion-like or decumbent, some-
times branched. Culms 250—2 000 mm in length; woody
and persistent from a woody base; leaf sheaths appressed
to culm or free, persistent; sheath mouth sometimes auric-
ulate; ligule a fringe of hairs; leaf blades linear, 50—550
mm long, rigid or filiform, open and flat, rolled or
acicular; inflorescence paniculate, lanceolate and some-
what contracted to globose and lax; spikelets solitary,
13-25 mm long, laterally compressed, 1-2-flowered,
highly reduced third floret rarely present; glumes two,
more or less equal, 1-nerved, membranous to chartaceous,
minutely scabrid, sometimes hirsute; lemma body uni-
formly pubescent, 7— 9(— ll)-nerved, 2.2— 6.0 mm long,
pubescent, the hairs arising from between the nerves,
nerves anastomosing into the awn base and a 2.5-12.0 mm
long lateral bristle; lemma lobes 0.4-4.0 mm long, acute
to acuminate, sometimes lacerated, partly to fully adnate
to the bristles; central awn geniculate, scabrid, contorted
basally, 2—11 mm long from base to knee, 6—21 mm long
from knee to tip; palea longer than lemma body, bifid at
apex, pubescent between the keels; lodicules two, glabrous
or ciliolate, sometimes with arm-like extensions; stamens
three; ovary apically hairy, these hairs retained until matu-
rity; fruit an achene with free pericarp, fusiform, subglo-
bose to globose or cuneate, surface colliculate or rugose,
hilum up to two thirds the length of the fruit, embryo
small.
A genus of nine species, endemic to the southwestern
region of the Cape Province, South Africa.
Key to species
La Spikelets with one floret 1. P. uniflora
lb Spikelets with two florets, occasionally with a rudimentary third floret:
2a Leaves with purple to dark brown auricles at base of blade; lemma lobes truncate, apically dentate .. 2. P. thuarii
2b Leaves without auricles, or if present then not coloured as above; lemma lobes acute to acuminate:
3a Panicle lax at anthesis, globose, 170-300 mm long; basal leaf sheaths 120 mm or longer, clustered at,
and free from culm base; culm, including inflorescence, usually taller than 1.2 m:
4a Leaf sheaths densely covered in short hairs; glumes 15—18 mm long; lemma body 3.0— 3.5 mm long; known
only from Table Mountain 3a. P. longiglumis subsp. longiglumis
4b Leaf sheaths glabrous; glumes 21—24 mm long; lemma body 5.0— 5.5 mm long; known only from the Kogel-
berg 3b. P. longiglumis subsp. gymnocolea
3b Panicle subcontracted to contracted at anthesis, lanceolate, up to 150 mm long; basal leaf sheaths seldom
longer than 120 mm, partially free or appressed to culm; culm, including inflorescence, seldom taller than
1.2 m;
5a Glumes 14—24 mm long; leaf blades acicular or permanently rolled, rigid, sometimes pungent:
6a One or both glumes pubescent 4. P. hirtiglumis
6b Glumes never pubescent:
7a Leaf blades acicular, usually straight but sometimes curling toward apices, occasionally pungent; leaf
sheaths glabrous, but sheath mouth may be bearded; sheaths closely appressed to culm . 5. P macrocalycina
7b Leaf blades permanently rolled, usually falcate, strongly pungent; leaf sheaths not appressed to culm,
always pubescent, if only at margins 6. P. oreophila
5b Glumes usually 14 mm or shorter; leaf blades usually soft, rolled (not permanently), folded or flat in cross
section, never pungent:
8a Lateral bristle of lemma 5.5-10.0 mm long; leaf sheaths pubescent to densely woolly, especially near sheath
mouth 7. P. distichophylla
8b Lateral bristle of lemma 2. 5-5.5 mm long; leaf sheaths glabrous or pubescent at margin only:
9a Leaves 200 mm long or longer, up to 5 mm wide; panicle with 25 or more spikelets 8. P. swartbergensis
9b Leaves usually shorter than 100 mm, thin and rolled, narrower than 2 mm; panicle with fewer than 15
spikelets 9. P. glacialis
1. Pentameris uniflora N.P. Barker, sp. nov.
A aliis omnibus speciebus Pentameridis flosculo singu-
lari differt.
Pentameris sp. 2. in Gibbs Russell et al.: 253 (1990).
TYPE. — Cape, Riversdale, Sleeping Beauty Peak.
Along edges of overgrown ledges or on steep south slopes.
Dense. 4200ft (1 275 m), 29 Oct. 1967, Esterhuysen 31771
(PRE, holo. ! ; BOL, iso.!).
Plants soft, decumbent; culms thin and flexuous, up to
650 mm long; leaf sheaths glabrous or only pubescent
along margins, appressed to culm; leaf blades soft,
filiform, short, up to 125 mm long, open or folded to some-
what rolled; panicle lanceolate, delicate, 40—60 x 10—20
mm, lax; spikelets 5—20, one-flowered; glumes 11—12 x
0.9— 1.0 mm; lemma body 5.5— 6.0 mm long; lemma lobes
acuminate, 1. 5-3.0 mm long, adnate to 2. 5-4. 5 mm long
lateral bristle for most of their length; awn geniculate,
2.0— 3.5 mm from base to knee, 6.5— 7.0 mm from
knee to tip; palea 5.5— 6.0 mm long; lodicules cuneate,
glabrous; anthers 4 mm long; fruit not known; flowering
time September to December. Figures 2D; 4.
36
Bothalia 23,1 (1993)
FIGURE 5. — Distribution of P. glacialis N.R Barker, ■; P. hirtiglumis
N.P. Barker, O; P longiglumis (Nees) Stapf subsp, longiglumis
N.P. Barker, ▼ ; P. longiglumis (Nees) Stapf subsp. gymnocolea
N.P. Barker, V ; P oreophila N.P. Barker, #; P. swartbergensis
N.P. Barker, *; P uniflora N.P. Barker, ♦; neighbouring locality
of P. hirtiglumis and P. oreophila, C).
This species is the only taxon in the genus with one-
flowered spikelets. Mature fruit have not been seen, but
stylar hairs on the apex of the ovary confirm the position
of this species in the genus Pentameris (Barker 1990).
P uniflora is known from only three localities which
are quite widely separated (Figure 5). Populations at these
localities appear to be quite abundant, but the habitat of
this species (damp, rocky, southern aspects of the Cape
fold mountains), habit (decumbent, hidden under taller
plants), and small, somewhat inconspicuous inflorescences
may account for the paucity of herbarium specimens.
Vouchers: Bond 1581 (SAAS); Ellis 2546 (PRE); Esterhuysen 25025,
32718a (BOL); Esterhuysen 31771 (BOL, PRE).
2. Pfentameris thuarii Beauv., Essai d’une Nouvelle
Agrostographie: 92, t. 18, fig. 8 (1812); Roem. & Schult.:
693 (1817); Kunth: 107 (1829) as ‘thouarsii’; Kunth: 315
(1833) as ‘thouarsii’; Kunth: 270 (1835) as ‘thouarsii’; Stapf:
513 (1897); N.P. Barker in Gibbs Russell etal.: 253. (1990).
Type: Du Petit-Thouars s.n. (P, lecto.!). Lectotype here
designated.
Danthonia thuarii Desv. : 99 (1831); Nees: 337 (1841) as ‘thouarsii’;
Steudel: 243 (1855) as ‘thouarsii’; Durand & Schinz: 854 (1895) as
‘thouarsii’; Durand & Schinz: 854 (1895).
P thuarii Beauv. var. burchellii Stapf: 513 (1897). Type: Riversdale
Div., lower part of the Lange Bergen, near Kampsche Berg, Burchell
6964 (K, holo.!; GRA, iso.!; PRE (fragment), iso.!).
Plants caespitose or decumbent; culms 0.46—1.63 m
long; leaf sheaths pubescent, appressed to culm, with
purple auricle at mouth, persistent; leaf blades up to 500
mm long, folded or flat (rarely rolled); panicle globose,
lax, 70—220 x 40—170 mm; spikelets 16—90, two-
flowered; glumes 15.5—21.5 x 1.8— 3.0 mm; lemma body
2.2— 3.3 mm long; lemma lobes 0.4— 0.7 mm long, acute,
apically lacerate-dentate, almost free from a 4.0— 5.5 mm
long lateral bristle; awn geniculate, 4.5 —7.0 mm from base
to knee, 9.5 — 12.5 mm from knee to tip; palea 2.8— 3.5
mm long; lodicules cuneate, glabrous; anthers 3—4 mm
long; fruit an achene, globose, 2.5 x 1.7— 2.0 mm, surface
colliculately sculptured; flowering time September to
December. Figure IB, D, F.
The spelling of the epithet thuarii, as used in the proto-
logue, differs so obviously from that of the name of the
collector, Du Petit-Thouars, that it is not considered a
typographic error. The epithet thouarsii, used in a number
of subsequent accounts, is therefore not adopted. It is
plausible that Palisot de Beauvois wished to maintain the
phonetic pronunciation of the French name ‘Thouars’, and
thus spelt it ‘thuarii’ in latinised form.
No locality or specimen number of the type specimen
was cited by Palisot de Beauvois. However, two specimens
of P. thuarii were obtained from the Paris herbarium (P).
One of these specimens is annotated with ‘Herb. Du Petit
Thouars’, which is written on the bottom of the label. The
identity of the handwriting is not known. That one (or
both) of these specimens are type material is further
supported by the observation that the illustration accom-
panying the original description includes a representation
of a mature fruit, a description of which also appears in
the text (Palisot de Beauvois 1812). The type specimen
must therefore have borne mature fruit. This deduction
is compatible with the historical record which indicates
that Du Petit Thouars visited the Cape in Febuary 1793.
February is the time of year when many fynbos grasses,
including P thuarii, are in fruit (pers. obs.). As the
annotated specimen from Paris is in full fruit, this
specimen is regarded as type material. However, this
evidence is considered to be insufficient to warrant
holotype status for this specimen, which is therefore
selected as a lectotype.
Stapf (1897) distinguished two varieties of P thuarii : var.
thuarii, was described as being only 1—2 ft. (300—600
mm) tall with a woody, sometimes branched, suffrutes-
cent base, with leaves only 1 lin. (approximately 2 mm)
wide and with a lax, open or contracted panicle; var.
burchellii Stapf was considered to be taller, simple basally
Bothalia 23,1 (1993)
37
and branching after 1 ft. (300 mm), with leaves 2 lin.
(approximately 4-5 mm) wide and with an effuse panicle.
Stapf added that this latter variety has the appearance
of a robust annual. Chippindall (1955) considers the
characters on which these distinctions are made to be too
variable, and rejects the two varieties, a conclusion
supported by Barker (1990).
This species grows abundantly in moist environments,
and is usually found alongside streams, seeps and drainage
lines. Geographically widespread, it occurs from Stellen-
bosch in the west to Montagu Pass in the east (Figure 6).
Vouchers: Ellis 2221 (PRE); Compton 7494 (BOL, NBG); Levyns 693
(BOL, STE); Parker 4465 (BOL, NBG, SAM); Schlechter 9282 (BOL,
GRA, PRE).
3. Pentameris longiglumis (Nees) Stapf
The following description is based on all the specimens
seen, and the variation reported includes that for both
known subspecies, described below.
Plants densely tufted from a woody base; culms erect,
up to 1.4 m tall, unbranched or branched close to woody
base; leaf sheaths loose and free from culm, wide,
persistent, clustered at base of plant, shortly pubescent
or glabrous, straw-coloured or purple, sheath mouth some-
times with green auricles; leaf blades rigid, rolled, up to
550 mm long; panicle lax, globose, up to 300 x 140 mm;
spikelets 30—100 or more, two-flowered; glumes 15.0—
24.0 x 1.1— 2.4 mm; lemma body 3.0— 5.5 mm long;
lemma lobes 2. 4 -4.0 mm long, long -acuminate, almost
completely adnate to a 3.5—11.0 mm long lateral bristle;
awn geniculate, 3.5—10.0 mm from base to knee, 7.5—21.0
mm from knee to tip; palea 3.0— 9.5 mm long; lodicules
cuneate, glabrous; anthers 3.6-5. 5 mm long; fruit broadly
fusiform, 3.5 x 1.3 mm, surface colliculately sculptured;
flowering time September to December. Figures 8 & 9.
Two subspecies are recognised on the basis of a number
of floral and vegetative characters, as listed in Table 5.
The significance of these differences is demonstrated by
the results of a principal components analysis (PCA)
TABLE 5. — A statistical summary of the variation in characters
differentiating the two subspecies of P. longiglumis (Nees) Stapf.
Measurements in mm
carried out on data obtained for 11 characters from 10
herbarium specimens. The PCA was done using the
numerical taxonomy package NT-SYS, version 1.4 (Rohlf
1988).
The first three axes resulting from the PCA accounted
for 94.2% of the variation in the data, with the first axis
contributing 75.7 % . The first two axes (Figure 7) account
for 88.3% of the variation in the data. The two groups
comprise specimens from two geographically distinct
localities, Kogelberg and Table Mountain. On the basis
of this evidence, the allocation of the rank of subspecies
to these two groups is considered to be justified.
3a. Pentameris longiglumis (Nees) Stapf subsp.
longiglumis
Danthonia longiglumis Nees in Flora africae australioris I: 306 (1841).
TYPE.— Cape, In summo monte tabulare (Dist. Cap.),
Bergius s.n. (B, holo.!; fragment and photo in PRE, iso.!).
Note: Pentameris longiglumis sensu Stapf: 514 agrees
with neither Nees’s description nor the type (see discus-
sion below).
0.6 -
*\ Tay 7231
A
x o.i
subsp. longiglumis
o\
Mar 3063
O Be 15170
Mar 3078
-0
V
O Bark 994
\
Bark 993
Bou 1649
SZ 11292
Ell 2341 /
v---' subsp. gymnocolea
n — i — i — i — i — i — i — i — i — i — i — i — i — — i — i — i — i — i — i — i — i — i — i — i — i — i — i —
-1.2 -1.0 -0.8 -0.6 -0.4 -0.2 0 0.2 0.4 0.6 0.8 1.0 1.2 1.4
Axis 1
FIGURE 7. —First two axes of the
principal components analysis
on data of eight specimens of
Pentameris longiglumis (Nees)
Stapf. Axis 1 accounts for
75.7 % of variation in data, axis
2, 12.6%. Points represent
specimens, annotated as fol-
lows: Bark = Barker, Be -
Bews, Ell = Ellis, Mar =
Marloth, SZ = Stirton &
Zantovska, Tay = Taylor, VanR
= Van Rensburg. Specimens
from BOL, PRE and STE.
38
Bothalia 23,1 (1993)
FIGURE 8 —Pentameris longiglumis (Nees) Stapf subsp. gymnocolea N.P. Barker. A, habit: erect culms, basally covered in loose, dead leaf
sheaths; note long leaf blades, which may be rolled or open, and large, globose, effuse panicle, x 0.8; B, ligule, which is a row of hairs,
surrounding leaf parts, with hairs on leaf sheath, expanded auricles, and sparsely pubescent adaxial basal leaf surface, x 4.7.
Bothalia 23,1 (1993)
39
FIGURE 9. — Pentameris longiglumis (Nees) Stapf subsp. gymnocolea
N.R Barker. Parts of spikelet and florets: A, long, acuminaie
glumes; B, whole basal floret; C, lemma (opened, flattened and
viewed from inside of floret) indicating venation, lemma bristles,
lemma lobes (adnate to bristles for most of their length) and
geniculate awn; D, palea; E, developing fruit, with apical hairs.
A-D, X 3.7; E. x 11.
Stapf (1897) describes P longiglumis as only 1.5 to 2
feet (450-600 mm) tall. Nees does not give any indica-
tion of plant height, but all specimens of this taxon seen,
including the type (Bergius s.n.), have far exceeded this
height. Furthermore, Stapf describes the sheath as glabrous
or sparsely hairy, whereas the type specimen has a
distinctly pubescent sheath, as described by Nees (1841).
In addition, Stapf describes the leaves as being filiform,
6—9 inches (150—220 mm) long. Nees does not provide
leaf lengths in his description, but leaves on the type
specimen were noted to be much longer than 6—9 inches,
broad, rolled and somewhat rigid.
Furthermore, at least three of the four specimens cited
by Stapf under his description of P. longiglumis do not
match the Bergius specimen cited by Nees. The three
specimens in question, Burchell 542, Burchell 598 and
Milne 246 were obtained from The Herbarium, Royal
Botanic Gardens, Kew (K). The fourth voucher cited by
Stapf, Spielhaus s.n. ,was not traced. Unfortunately these
three specimens are of poor quality. The spikelets (when
present) are devoid of florets, and one specimen, Burchell
542, is entirely sterile. Uncertainty about the identity of
the Milne 246 specimen is further borne out by an anno-
tation to the effect that the leaves resemble those of
Pentaschistis pallescens (Schrad.) Stapf, whereas the
inflorescence resembles that of Pentameris thuarii. The
Burchell 598 specimen may possibly be Pentameris longi-
glumis as it has floral parts of a size comparable to those
observed in Nees’s type specimen . However, the basal parts
are absent, so the leaf and sheath characters cannot be
compared.
It is therefore considered that Stapf’s (1897) description
and cited vouchers do not agree with Nees’s description
and type of P. longiglumis . Stapf s Pentameris longiglumis
is therefore regarded as a misapplied name, and it appears
that Stapf described a species of Pentaschistis.
This subspecies is known from a few specimens
collected from Table Mountain, the distribution shown in
Figure 5. Until recently, this taxon was thought to be
extinct, as the most recent specimen seen among the
holdings of eight South African herbaria is dated 1918.
However, a small population has been located in a recent-
ly burnt area on Table Mountain. This population is
growing in a slightly sloping seepage area. The moist
habitat requirement matches that of the other subspecies,
which is, however, found on steeper slopes.
Vouchers: N. Barker 993, 994 (BOL, PRE); Bews 15170 (BOL);
Marlorh 3063, 3078 (PRE).
3b. Pentameris longiglumis ( Nees ) Stapf subsp.
gymnocolea N.P. Barker, subsp. nov.
Differt a P. longiglumi subsp. longiglumi foliorum vagi-
nis glabris et partibus floralibus grandioribus: glumae
21—24 mm longae, lemma 5.0— 5.5 mm longum; sub-
species tantum monte ‘Kogelberg' nominato nota. Figures
2C; 8 & 9.
TYPE. — Cape, summit ridge of Platberg, Kogelberg,
S side, edge of gully; culms 3—4 ft. (1.0— 1.3 m), erect,
coarse, loose tufts, 2650 ft (900 m), 27 Nov. 1967, Taylor
7231 (PRE, holo.!; STE, iso.!).
As shown in Table 5, this subspecies differs from P.
longiglumis subsp. longiglumis in a number of features.
The subspecific epithet chosen for this species describes
one of these distinguishing characters: the glabrous leaf
sheaths.
This subspecies is known only from the Kogelberg
Forest Reserve (Figure 5). It inhabits south-facing moun-
tain slopes in seepage areas where it forms large tussocks.
Vouchers: Boucher 1649 (PRE); Ellis 2341 (PRE); Esterhuysen 13326
(BOL. PRE); Stirton & Zantovska 11293 (STE); Van Rensburg 518 (STE).
4. Pentameris hirtiglumis N.P. Barker, sp. nov.
P. oreophilae similis sed glumis hirsutis facile distincta;
lobis lemmae acutis, usque ad dimidium longitudinis ad
setam adnatis.
40
Bothalia 23,1 (1993)
FIGURE 10. —Pentameris hirtiglumis N.P. Barker, type specimen Kerfoot 6092. A, habit: decumbent, branching culm basally covered in dead
leaf sheaths; note that flowering culm is not normally curved back upon itself, but appeared so on specimen. B— G, parts of spikelet and
florets: B, hirsute glumes; C, whole basal floret; D, lemma (opened, flattened and viewed from inside of floret) showing venation, lemma
bristles, lemma lobes (adnate to bristle for half or less of their length) and geniculate awn; E, palea; F, anthers, with no filaments; G,
ovary with apical hairs and stigmas. A, x 0.5; B— F, x 4.7; G, x 14.
Bothalia 23,1 (1993)
41
TYPE. — Cape, Bosboukloof, Jonkershoek, locally very
common, attractive, 980 ft (600 m), Oct. 1967, Kerfoot
6092 (PRE, holo.!).
Plants cushion-like or densely bushy, branched; culms
somewhat decumbent with numerous nodes, 200-750 mm
long; leaf sheaths pubescent, at least along margins (rarely
glabrous), persistent, not closely appressed to culm, loose
when dead; leaf blades up to 200 mm long, permanently
rolled, falcate; panicle lanceolate, somewhat lax, 75—110
x 20—35 mm; spikelets 15-50, two-flowered; glumes
hirsute, 14.5—21.5 x 1.6— 2.1 mm; lemma body 2. 8— 3.7
mm long; lemma lobes 1—2 mm long, acute, adnate to
a 3.0-6.5 mm long lateral bristle for half or less of their
length; awn geniculate, 4—6 mm from base to knee,
7.5-11.0 mm from knee to tip; palea 4.0-4. 5 mm long;
lodicules cuneate, glabrous; anthers 3.5— 5.0 mm long;
fruit broadly fusiform, 2.4 x 1.2 mm, surface collicu-
lately sculptured (Figure 1A); flowering time September
to October/November.
This species is similar in appearance to P. oreophila ,
but can be readily separated from that species by the
presence of the hirsute glumes (Figure 10B) . Additional
differences between these two taxa are the acute lemma
lobes (Figure 10D) and softer, non-pungent leaf apices
in P. hirtiglumis. However, as is apparent from the
cladogram discussed above (Figure 3), this species is
sister to P longiglumis on the basis of several anatomical
features including swollen leaf margins, inflated abaxial
epidermal cells and dense, strongly inclined adaxial
prickles.
Like P. oreophila, this taxon has a geographically
restricted distribution, and is known only from high
montane regions of the Hottentots Holland Mts (Figure
5). Where found, this species is abundant and locally
dominant. However, it appears to have narrow habitat
requirements, and is restricted to shale bands.
Vouchers: N. Barker 90 (PRE); Ellis 4680 (PRE); Kruger & Haynes
753 (JF, STE).
5. Pentameris macrocalycina (Steud.) Schweick. in
Feddes Repertorium 43: 91 (1938); N.R Barker in Gibbs
Russell et al.: 252. (1990). Type: Cape, in summitate
Montis Tabularis Ecklon 932 (OXF, lecto.!, PRE isolecto.!
(fragments), S, isolecto.!). Lectotype here designated.
Avena macrocalycina Steud.: 482 (1829).
Danthonia speciosa Lehm. ex Nees: 307 (1841). Steud.: 241. (1855);
Durand & Schinz: 854 (1895). Type: In apicis rupestribus montis ad
Genadenthal solo sabuloso-humoso alt. 2000—3000 ft, (Stellenbosch),
et in Dutoitskloof alt. 2500-3000 ft, Drege s.n. (PRE fragments, iso!.).
Pentameris speciosa (Lehm. ex Nees) Stapf: 515 (1897).
Plants caespitose, branched; culms 0.43—1.10 m long;
leaf sheaths sometimes bearded at mouth, persistent,
closely appressed to culm; leaf blades 110—290 mm long,
acicular; panicle lanceolate, somewhat lax, 60—120 x
10-60 mm; spikelets 10-50, two-flowered; glumes 16-24
x 2-3 mm; lemma body 3.5-5.5 mm long; lemma lobes
1.3— 4.0 mm long, acute-acuminate, adnate to a 7.5—12.0
mm long lateral bristle for most of their length; awn
geniculate, 5.5— 10.0 mm from base to knee, 9— 16 mm from
knee to tip; palea 6.5—11.0 mm long; lodicules cuneate.
glabrous; anthers 4.2— 6.0 mm long; fruit broadly fusi-
form, 3.6 x 1.2 mm, surface colliculately sculptured;
flowering time September to December.
Schweickerdt (1938) pointed out that both Stapf (1897)
and Durand & Schinz (1895) had placed Avena macro-
calycina in synonymy under Danthonia macrantha. In
addition, Nees (1832) mistakenly placed Avena macro-
calycina and its type, Ecklon 932, under Pentameris
macrantha. This confusion arose as a result of the fact
that there were two specimens representing different taxa
distributed under the number Ecklon 932. The type
specimen of Avena macrocalycina, one of the Ecklon 932
specimens, was obtained from the Fielding-Druce
herbarium, Oxford (OXF), and is designated here as the
lectotype. A duplicate of this specimen is housed in the
Swedish Museum (S).
This is a widely distributed species, recorded from
Pakhuis Pass in the north to Cape Point in the south and
eastwards to the Groendal Wilderness Reserve (Figure 11).
Vouchers: Adamson 3980 (JF, PRE); Ellis 2540 (PRE); Esterhuysen
23763, 28012 (BOL, PRE); Taylor 11113 (PRE, STE).
6. Pentameris oreophila N.P. Barker, sp. nov.
Species laminis revolutis permanentibus, brevibus
(<105 mm longis), falcatis, et foliorum vaginis saltern
marginibus pubescentibus distinguitur.
Pentameris sp. 1. in Gibbs Russell et al.: 252. (1990).
P. obtusifolia sensu Ellis (1985d), Barker (1986, 1989). Note that P.
obtusifolia (Hochst.) Schweick. is to be transferred to Pseudopentameris.
TYPE. — Cape, Worcester Div., Jona’s Kop, common
on shale band, or on peaty slopes, after fire, in different
aspects but not on steep southern slopes, forming dense
and, in some places, quite extensive patches, leaf tips very
sharp, 5000 ft (1 500 m), 19 Dec. 1971, Esterhuysen 32681
(PRE, holo.!; BOL, iso.!).
Plants cushion-like or densely bushy, branched basally;
culms erect or somewhat decumbent in older, larger tufts
and then with numerous nodes, up to 530 mm long; leaf
sheaths persistent, pubescent along margins, appressed or
free from culm, especially when dead, often purple when
young; leaf blades up to 105 mm long, permanently rolled,
falcate (less so in young plants), strongly pungent; panicle
lanceolate, somewhat lax, 30—80 x 20—40 mm; spikelets
8—20, two-flowered; glumes 14—20 x 2.1— 3.0 mm;
lemma body 3—4 mm long; lemma lobes 1.6— 3.0(— 4.0)
mm long, acuminate, adnate to 7.0—10.5 mm long lateral
bristle for most of their length; awn geniculate, 6—11 mm
from base to knee, 9.5—13.0 mm from knee to tip; palea
5.5— 8.5 mm long; lodicules cuneate, glabrous; anthers
4.0— 5.5 mm long; fruit subglobose, 3.5— 4.0 x 1.6— 2.0
mm, surface colliculately sculptured; flowering time
September to December. Figures IE & 2B.
The species can be distinguished by its permanently
rolled, short (<105 mm long), falcate leaf blades and the
leaf sheaths which are pubescent at least along the margins.
The specific epithet oreophila, or 'mountain-loving', is
chosen because this species is only found at high altitudes
in the Hottentots Holland, Riviersondereinde and Hex
42
Bothalia 23,1 (1993)
FIGURE 11. — Distribution of P. macrocalycina.
River Mountain ranges (Figure 5). Where found, the
species is abundant, especially in years immediately after
fire. Its high altitude habitat receives snow in the ' /inter
months, and the cushion-like growth form (Figr 2) may
be an adaptation to this.
Vouchers: Ellis 4686 (PRE); Esterhuvsen 19788 (BOL, PRE); Forsvth
191 (JF, PRE); Phillips 2109 (SAM); Wasserfall 562 (BOL, NEG).
7. Pentameris distichophylla (Lehm.) Nees in Lin-
naea 7: 314. (1832); Kunth: 317 (1833). Type: Habitat in
Promontorio Bonae Spei, collector unknown (S, lecto.!,
PRE, fragment).
Damhonia distichophylla Lehm.: 41 (1831); Nees: 305 (1841).
Pentameris dregeana Stapf: 515 (1897); N.P. Barker in Gibbs Russell
et al. : 252 (1990).
Plants caespitose, becoming cushion-like with age,
branched basally; culms 0.4— 1.2 m long; leaf sheaths
pubescent to woolly, especially near mouth, appressed to
culm, persistent; leaf blades 80— 190(— 300) mm long,
pubescent, rolled, folded or flat; panicle lanceolate,
somewhat lax, 50—110 x 15—60 mm; spikelets 12—65,
two-flowered; glumes 12-15 x 1—2 mm, occasionally
sparsely pubescent; lemma body 2.3— 3.5 mm long; lemma
lobes 1.0-2.6 mm long, acute, adnate to a 5.0-10.5 mm
long lateral bristle for most of their length; awn genicu-
late, 4—7 mm from base to knee, 6—12 mm from knee
to tip; palea 4—6 mm long; lodicules cuneate, glabrous
or shortly ciliolate, rarely with arm-like extensions;
anthers 3.0— 4.5 mm long; fruit cuneate, 2.0 x 0.9 mm,
surface rugosely sculptured; flowering time September to
December. Figures 1 & 2.
Stapf (1897) created the epithet dregeana for the partial
concept of the taxon which Nees (1841) called Danthonia
distichophylla. Stapf did not agree with Nees on the
inclusion of Lehmann’s description of Danthonia disticho-
phylla, and in a footnote states that Lehmann’s descrip-
tion probably refers to a Pentaschistis . It thus appears that
Stapf did not see the type of Lehmann’s Danthonia
distichophylla.
Lehmann’s description (1831) states that he has seen the
specimen in a dried state (v.s.= vide siccam). According
to Nordenstam (1980), Lehmann’s herbarium comprised
many specimens collected by Ecklon & Zeyher. The
collections of Lehmann now reside in the Swedish
Museum of Natural History (S), from which the type of
Danthonia distichophylla was obtained. The label of this
specimen had been annotated (possibly by Nordenstam)
to the effect that it is written in Lehmann’s hand. Further
confirmation of this was obtained by matching the script
with that of published examples of Lehmann’s handwriting
(Burdet 1976; Nordenstam 1980). As there are no other
labels on the specimen, the original collector of this
specimen is unknown, but as Lehmann never visited
southern Africa, it is possible that the specimen is an
Ecklon & Zeyher collection.
Despite Stapf s comment, the Lehmann specimen is a
good match to the specimens of P. dregeana cited by Stapf
(1897). The name P. dregeana is therefore illegitimate as
it is antedated by Lehmann’s P. distichophylla. This taxon
is therefore correctly named Pentameris distichophylla
(Lehm.) Nees. As there is no conclusive evidence that the
Lehmann specimen from S is the holotype, it is designated
as the lectotype.
This species is one of the most widely distributed in the
genus, ranging from the northern Cedarberg to Paarl and
eastwards to the Tsitsikamma Mountains (Figure 13).
Vouchers: Esterhuvsen 22352, 27321 (BOL, PRE); Hafstrom & Acocks
45 (PRE); Gillett 3835 (STE); Taylor 11590 (PRE, STE).
Bothalia 23,1 (1993)
43
8. Pentameris swartbergensis N.P. Barker , sp. nov.,
P. distichophyllae similis sed foliorum vaginis glabris
differt.
TYPE. — Cape, Toverkop, Swartberg nr Ladismith,
broad ledges at base of high cliffs on S side of peak,
appears to be locally dominant below cave, 6500 ft. (1 875
m), 17 Dec. 1956, Esterhuysen 26755 (PRE, holo.!; BOL,
iso.!).
Plants caespitose or somewhat decumbent, basally
branched; culms up to 560 mm long; leaf sheaths glabrous,
appressed to culm; leaf blades up to 230 mm long, folded
or rolled, sparsely pubescent near base; panicle lanceo-
late, 80—90 x 20—35 mm, somewhat lax; spikelets
22—56, two-flowered; glumes 11.5—13.0 x 1.5— 1.6 mm;
lemma body 2.8— 3.0 mm long; lemma lobes, acuminate,
1.4— 1.5 mm long, adnate to 2.5— 3.5 mm long lateral
bristle for about half their length; awn geniculate, 3 mm
from base to knee, 5.5 -7.0 mm from knee to tip; palea
4.5— 5.0 mm long; lodicules cuneate, ciliolate at apex;
fruit broadly fusiform, 2.0— 2.4 x 1.0 mm, surface collicu-
lately sculptured; flowering time September to December.
Figure 14.
This species may be confused with P. distichophylla,
but differs in such features as the nature of the colliculate
surface of the caryopsis (which is rugose in P. disticho-
phylla), the leaf sheaths (glabrous in P. swartbergensis,
pubescent to woolly in P. distichophylla) and the lateral
lemma bristles, which are substantially shorter in P.
swartbergensis.
This taxon is known from only two localities in the Klein
Swartberg, and is probably endemic to this mountain range
FIGURE 12. — Pentameris oreophila
N. R Barker. A, habit: erect
culms and prickly, cushion-like
basal leaf growth; note also
pubescent leaf sheaths loosely
appressed to stems, falcate,
permanently rolled leaf blades
with pungent apices. B— G,
parts of spikelet and florets: B,
glumes; C, whole basal floret;
D, lemma (opened, flattened
and viewed from inside of
floret) showing venation, lem-
ma bristles, lemma lobes
(adnate to bristles for most of
their length) and geniculate
awn; E, palea; F, anthers with
no filaments; G, ovary with
apical hairs and stigmas. A, X
O. 3; B-F, x 3.7; G, x 11.
44
Bothalia 23,1 (1993)
(Figure 5). It grows at the foot of cliffs or rock walls in
deep shade.
Vouchers: Esterhuysen 18510, 26750, 26751 (BOL, PRE); Linder 5490
(BOL).
9. Pentameris glacialis N.P. Barker , sp. nov., a P.
distichophylla spiculis paucis (< 15), foliis brevibus filifor-
mibus et habitu decumbenti molli distinguitur.
TYPE. — Cape, Oudtshoom, Waboomsberg, growing in
humic gullies on south slopes, 14 Dec. 1991, N.P Barker
995 (BOL, holo.!; B, CANB, G, GRA, J, K, NBG, NSW,
NU, P, PRE, STE, all iso.!)
Plants decumbent; culms thin, flexuous, up to 550 mm
long, tinged with purple; leaf sheaths glabrous or pubes-
cent along margins, loosely appressed to culm; leaf blades
filiform, short, up to 100 mm long, rolled; panicle
lanceolate, to 70 x 30 mm, lax to somewhat contracted;
spikelets 6— 12(— 15), two-flowered; glumes 13.0—14.5 X
1.3— 1.5 mm; lemma body 2.5— 3.0 mm long; lemma lobes
acuminate, 1.0— 1.9 mm long, adnate to 3.5— 4.5 mm long
lateral bristle for less than half its length; awn geniculate,
3.5— 5.5 mm from base to knee, 7.5— 8.5 mm from knee
to tip; palea 3.5— 4.2 mm long; lodicules cuneate,
glabrous; fruit an achene, 2.5 x 1 mm, surface collicu-
lately sculptured; flowering time October to December.
This species, first collected in 1987 by Ellis, bears
superficial resemblance to P macrocalycina, but is
distinguishable from that species by the slender, geniculate
culms, the rolled but not acicular leaf blades, the panicles
with few spikelets, as well as by the size of the floral
structures, which are substantially smaller in P. glacialis.
The species is generally found to be locally abundant,
growing in narrow gullies, rock ledges and overhangs in
black, humic but sandy soils. Such habitats are thought
to become particularly heavily snowed up in winter. This
habitat appears to preclude P. macrocalycina, which is
found in more stony sites, as well as P. distichophylla,
which appears to prefer northern aspects and rock crevices.
The woolly leaf bases and sheaths of P. distichophylla
separate this species from P. glacialis (Figure 15).
When visited in mid-October 1991, the plants and rocks
at the type locality were covered in a thick layer of ice.
Such conditions may persist for three or more months of
the year in the winter and spring, depending on the severity
of the frontal systems associated with the winter rainfall
regime of the southwestern Cape. This harsh, icy environ-
ment gave rise to the specific epithet.
A subsequent visit in mid-December 1991 provided an
indication of the range of climatic extremes in which this
species survives, with very hot, dry conditions prevailing.
The steep-sided, rocky gullies in which this species is
found were, however, cooler, being shaded for much of
the day, and the humic soil was still damp. Figure 5 shows
the distribution of this species.
Vouchers: N. Barker 995. 996 (BOL, GRA, J, NBG. S, STE, UWC),
997 (BOL, K, PERTH, PRE), 1019 (BOL); Ellis 5620 (PRE).
INCERTAE SEDIS
A single unusual specimen, undoubtedly belonging to
the genus Pentameris (possessing an achene with apical
hairs) was collected from Cockscomb Peak by Ellis in 1987.
This specimen, Ellis 5605 (PRE), is morphologi-
cally similar in certain respects to P. glacialis, but differs
in its leaf anatomy.
ACKNOWLEDGEMENTS
I would like to thank Drs K. Balkwill, B. de Winter,
R.P Ellis, G.E. Gibbs Russell, E. A. Kellogg, D.J.B. Killick,
Bothalia 23,1 (1993)
45
FIGURE 14. Pentameris swartbergensis N.P. Barker. A, habit: erect culms (folded back, based on type material) and branched basal parts.
B-F, parts of spikelet and florets: B, glumes; C, whole basal floret; D, lemma (opened, flattened and viewed from inside of floret) showing
venation, lemma bristles, lemma lobes (adnate to bristles for most of their length) and geniculate awn; E, palea; F, developing fruit with
apical hairs, note that fruit appears to develop in a basipetal direction, uppermost region becoming swollen and associated surface sculptured,
appearing at apex first. A, X 0.5; B— E, X 4.8; F, X 14.6.
46
Bothalia 23,1 (1993)
FIGURE 15. — Pentameris glacialis
N.P. Barker. A, habit: show-
ing thin, decumbent culms; B,
indumentum of sheath, pubes-
cent along margin, sheath
mouth and leaf blade. C— H,
parts of s pikelet and florets: C,
glumes; D, whole basal floret
with mature fruit; E, lemma
(opened, flattened and viewed
from inside of floret) showing
venation, lemma bristles, lem-
ma lobes (adnate to bristles for
about half their length) and
geniculate awn; F, palea; G,
fruit with apical hairs; H,
spikelet. A, x 0.4; B— F, x
3.7; G, X 6; H, X 2.4.
O.A. Leistner, H.P. Linder and Mr E.R. Robinson for
their advice, discussions and comments on various aspects
of this work. Drs J. Rourke and O.A. Leistner are thanked
for assistance with the Latin diagnoses. In addition Dr Ellis
is acknowledged for the provision of his many micrographs
of leaf anatomy preparations and for comments on the
manuscript. The curators of the following herbaria are
thanked for providing access to, and/or loans of, their
specimens: B, BOL, GRA, SAAS, now housed in PRE,
K, NBG, OXF, P, PRE, S, SAM, STE and SAAS. I extend
my grateful thanks to Mrs Wilma Roux of the National
Botanical Institute for the illustrations of the new taxa,
Mrs S. Perold for assistance with the SEM and Mrs
A. Romanowski for the photographic work. I also acknow-
ledge the support of the National Botanical Institute, my
employer for the duration of this study. This work was un-
dertaken in partial fulfilment of an M.Sc. degree at the
University of the Witwatersrand.
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RAB1NOWITZ, D. 1981. Seven forms of rarity. In H. Synge, The bio-
logical aspects of rare plant conservation : 205—217. Wiley, New
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RENVOIZE, S.A. 1981. The subfamily Arundinoideae and its position
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.
Bothalia 23,1: 49-57 (1993)
Studies in the Marchantiales (Hepaticae) from southern Africa. 1. The
genus Dumortiera and D. hirsuta ; the genus Lunularia and L. cruciata
S.M. PEROLD*
Keywords: Dumortiera, D. hirsuta , Dumortieroideae, Hepaticae, Lunularia, L. cruciata. Lunula riaceae, Marchantiaceae, Marchantiales, taxonomy,
southern Africa, Wiesnerellaceae
ABSTRACT
The genera Dumortiera (Dumortieroideae, Marchantiaceae) and Lunularia (Lunulariaceae), are briefly discussed. Each
genus is represented in southern Africa by only one subcosmopolitan species, D. hirsuta (Swartz) Nees and L. cruciata
(L.) Dum. ex Lindberg respectively.
UITTREKSEL
Die genusse Dumortiera (Dumortieroideae, Marchantiaceae) en Lunularia (Lunulariaceae) word kortliks bespreek. In
suidelike Afrika word elke genus verteenwoordig deur slegs een halfkosmopolitiese spesie, D. hirsuta (Swartz) Nees en L.
cruciata (L.) Dum. ex Lindberg onderskeidelik.
DUMORTIERA Nees
Dumortiera Nees ab Esenbeck in Reinwardt, Blume
& Nees ab Esenbeck, Hepaticae Javanicae, Nova Acta
Academiae Caesareae Leopoldina-Carolinae Germanicae
Naturae Curiosorum XII: 410 (1824); Gottsche et al.\ 542
(1846); Schiffner: 35 (1893); Stephani: 222 (1899); Sim:
25 (1926); Muller: 394 (1951-1958); S. Amell: 52 (1963);
Hassel de Menendez: 182 (1963). Type species: Dumor-
tiera hirsuta (Swartz) Nees.
Synonymy according to Nelson & Parnell: 35 (1992):
Hygropyla Taylor: 390 (1836).
Hygrophila Taylor (orth. var.) in Mackay: 53 (1836) non
R. Br. (1810).
Hygrophyla Taylor (orth. var.) in Mackay: X (1836).
Hygropila Taylor (orth. var.) in J.D. Hooker & T. Taylor:
576 (1844).
Askepos Griffith 2: 340 (1849).
Thallus, large, flat and thin, dark green, in overlying
patches; on shaded, damp soil or on wet rocks. Branches
with apical innovations or dichotomously furcate, occa-
sionally lateral, moderately divergent, thickened over
midrib, wings gradually thinning toward margins; apex
emarginate.
Dorsal epidermis very thin-walled, temporary, vestigial,
air pores absent, air chambers mostly reduced to 1- or
2-celled vestiges, reported rarely to have reduced chloro-
phyllose filaments, cells containing numerous fairly large
chloroplasts; storage tissue compact, confined to ventral
part of midrib; oil cells rare, each with a single, large oil
body; rhizoids along midrib and ventrally appressed
against wings, mostly smooth, occasionally tuberculate;
scales ventral over midrib, vestigial and evanescent.
* National Botanical Institute, Private Bag X101, Pretoria 0001.
MS. received: 1992-03-31.
Monoicous or dioicous. Antheridia sunken in subses-
sile disciform receptacles, which are fringed with bristles
and borne singly at apex of thallus on short bifurrowed
stalk. Archegonia in groups of 8—16 in saccate, fleshy
involucres, on lower surface of 6-8-lobed disciform
receptacle with marginal sinuses dorsally, raised on stalk
with two rhizoidal furrows; after fertilization and
maturation, each involucre generally containing a single
sporophyte consisting of foot, seta and capsule; capsule
wall unistratose, with annular thickenings, dehiscing irre-
gularly. Spores small, papillose. Elaters slender, tapering,
1— 3-spirate. Gemmae absent.
Dumortiera hirsuta (Swartz) Nees in Reinwardt,
Blume & Nees ab Esenbeck, Nova Acta Academiae
Caesareae Leopoldino-Carolinae Germanicae Naturae
Curiosorum XII: 410 (1824); Gottsche et al.\ 542 (1846);
Spruce: 566 (1885); Stephani: 224 (1899); Macvicar: 41
(1926); Sim: 25 (1926); Muller: 396 (1951); S. Amell: 52
(1963); Hassel de Menendez: 182 (1963). Type: Jamaica,
leg. Swartz s.n. [S, holo.!; MW, iso. (Hb. Hoffm. No.
8497); UPS, fide Grolle 1976],
Marchantia hirsuta Swartz: 145 (1788).
M. irrigua Wilson ex Hooker in Smith: 106 (1833). Hygropyla irrigua
(Wilson) Taylor: 390 (1836); Mackay: 54 (1836); Stephani: 150 (1899).
Dumortiera irrigua (Wilson) Nees: 159 (1838). D. hirsuta var. irrigua
(Taylor) Spruce: 566 (1885). Type: Ireland, Tbrk Cascade, near Killamey,
Mr Wilson.
D. hirsuta var. angustior Gottsche, Lindenberg & Nees: 544 (1846).
D. hirsuta var. intermedia Gottsche, Lindenberg & Nees: 544 (1846).
D. velutina Schiffner: 256 (1893).
Askepos brevipes Griffith: 340 (1849). Type: India, in sylvis umbro-
sis Tingrei agri, II 1836.
Thallus hygrophyllous, large and creeping, broadly and
rather irregularly strap-shaped, uniformly dark green,
translucent, thin and flat, but often marginally undulate,
wet (Figure 1A); crisped and shrivelled, dull, unable to
survive dry; in crowded, overlying patches, once to several
times dichotomously or occasionally laterally furcate or
50
Bothalia 23,1 (1993)
FIGURE 1. — Dumortiera hirsuta. A, dorsal view of thallus; B, ventral view of thallus; C, male plant with disciform receptacles at apex; D, young
female receptacle seen from above; E, young female receptacle seen from below; F, transverse section of thallus; G, margin of thallus
with hairs; H, transverse section of thallus, much enlarged; I, lower cells of costa and vestigial scales in transverse section; J, filiform
scale from top of stalk; K, transverse section of stalk with two rhizoidal furrows; L, capsule wall cells with thickenings; M, transverse
section of capsule wall. A, F-H, S.M. Perold2694: B, 5. M. Perold2634: C, Nicholas 1176: D, E, I, H. Anderson CH 13495: J-L, Doidge
CH 3581. Scale bars: A— C = 2 mm; D— F, J = 1 mm; G, K = 100 jxm; H, I, L, M = 50 /xm. Illustrations by G. Condy.
Bothalia 23,1 (1993)
51
with apical innovations; branches 50-95 x 8— 13(— 22)
mm and ± 500 /tm thick over median, ventrally bulging
midrib (also visible from above), laterally gradually
thinning out into wide wings (Figure IF); apex shortly
emarginate; margins undulate, occasionally scalloped,
sparsely hirsute, hairs ± 250.0 /xm long, ± 12.5 /tm wide
at base, tapering slightly to somewhat blunt tip (Figure
1G).
Epidermis, pores and air chambers absent; dorsal cells
from above, 4—6-sided, variable in shape and size, 27-57
x (17-)22-32 /xm, in cross section ± 15 /on thick,
containing chloroplasts; marginal cells thin-walled, long-
or short-rectangular, 25-62 x 12-20 /im; midrib with
+ 18 rows of cells of which upper 3 rows larger, rounded,
up to 100 x 137 /xm, with somewhat wavy walls and
scattered chloroplasts, lower group of cells angular,
smaller, ± 30 /im wide, lacking chloroplasts; wings
medianly with 3 rows of large cells, decreasing in number
to one row at margin, covered by dorsal and ventral layer
of smaller chlorophyllose cells; oil bodies quite rare, for
the most part confined to scattered cells in the midrib,
yellow-brown, elongate or round, ± 40 /xm across; rhi-
zoids below midrib numerous, mostly smooth, 15-20 /xm
wide, occasionally tuberculate, 5 /xm wide, also in widely
spaced, arching strands below wings, radiating toward
margins and appressed to ventral face of wings (Figure
IB) or scattered; ventral scales hyaline, vestigial (Figure
II), without appendages, evanescent, only near apex.
Monoicous or dioicous. Antheridiophore subsessile, dis-
ciform, 2.75 mm in diameter, 0.6 mm thick in centre, flat-
tening toward sides, containing antheridia, 470 x 250 /im,
± ovate, acropetally arranged, but not in radiating rows,
sunken into disc, borne singly at apical notch of thallus
(Figures 1C; 2A) on very short, 1 mm diameter,
bifurrowed stalk, with rhizoids lining furrows; hyaline, fili-
form scales on ventral face of disc, the latter encircled by
dense outer fringe of bristle-like hairs, 600-1100 pm long,
base 20—25 /xm wide, a few scattered hairs dorsally. Ar-
chegoniophore disciform, 3.75 mm in diameter; dorsal face
(Figure ID) becoming radially grooved by sinuses; ven-
tral face 6— 8-lobed (Figure IE) in radiating rows and then
almost star-shaped, sparingly bristled; archegonia
in groups of 8-16, enclosed in green, fleshy, saccate
involucres, long archegonial necks protruding through
narrow slit-like apical openings; receptacle eventually
raised on stalk arising at apical notch of thallus between
overlapping sides, + 40 mm long and ± 925 /xm wide,
cortical cells + 15.0 x 12.5 /xm, inner cells + 50 x 30
/xm; along its length 2 furrows lined with rhizoids (Figure
IK) and its top (where joined to disc) encircled by nume-
rous filiform, hyaline scales (Figure U), up to 3750 /xm
long and 300 /xm wide at base, apex only ± 3 cells wide,
cells mostly ± 125 x 22 /xm; at maturity generally only
one sporangium borne in each involucre, rarely two and
quite often none, elliptical, 2.5 x 1.5 mm, supported on
elongating seta and protruding from membranous calyp-
tra, pseudoperianth lacking; capsule wall unistratose
(Figure 1M) with annular or semi-annular thickenings
(Figure 1L), dehiscing irregularly via longitudinal suture
lines and releasing large numbers of elaters and spores
(Figure 2B). Spores golden brown, semi-transparent, distal
face rounded, proximal face ± flat to slightly peaked in
the centre, triradiate mark indistinct, 25—30 /xm across
its longer axis, ornamented with numerous nodules or
tubercles, irregular in size and shape (Figure 3A). Elaters
yellow-brown or orange-brown, mostly with doubly spiral
strands (Figure 3B), ends tapering, 225 —470 x 7.5—10.0
/xm in middle and 3.5 /xm wide at tips. Gemmae absent.
Chromosome number, n = 9 (Berrie 1960, Bomefeld
1987); n = 18 (Tatuno 1941); n = 27 (Tatuno 1941, Berrie
1958). According to Tatuno (1938, 1939) the 9, 18 and 27
chromosome sets present different races with different
distributions and edaphic ecology, but he considers them
as belonging to the same species.
Only a few of the specimens examined were fertile; most
of these were dioicous, with male and female receptacles
borne on separate plants. Monoicous plants were quite
rarely found, but have frequently been reported in the
literature and even bisexual receptacles are known (Evans
1919).
All southern African specimens have been identified as
belonging to D. hirsuta : the dorsal face of the thallus is
always + smooth and lacks papilliform cells or traces of
air chambers. D. nepalensis and D. velutina, which our
material resembles, are considered to belong to the poly-
morphic species D. hirsuta (Grolle & Piippo 1984). Amell
(1963) referred to material from southern Africa (Cape
Province, Transvaal, Natal) as D. hirsuta var. nepa-
lensis. Schuster (1992) considers D. nepalensis (Taylor)
Nees to be a distinct taxon under the name of D. hirsuta
subsp. nepalensis (Taylor) Schuster which is not found in
Africa. D. hirsuta is subcosmopolitan and is widespread
in tropical and temperate regions, generally growing in
sheltered, wooded, shaded and damp areas, i.e. it is hygro-
philous. In southern Africa it is known from northern and
eastern Transvaal, Swaziland, Natal, Zululand and eastern,
southern and southwestern Cape (Figure 4). Further north-
wards in Africa, D. hirsuta is reported from (or has been
collected in) Zimbabwe (Best 1990), Zambia [S.M. Perold
2670 (PRE)], East African Mountains (Amell 1956), East
Africa (Bizot etal. 1985), Tanzania, Malawi, Mozambique
(Bizot & Poes 1979), Rwanda and Burundi (Vana et al.
1979).
On the basis of flavonoid data, Campbell et al. (1979)
found chemical affinities between Dumortiera and Wies-
nerella, suggesting that they belong in a common family,
Wiesnerellaceae (Inoue 1976). This was accepted by Grolle
(1983), but Schuster (1984) has retained Dumortiera in the
Marchantiaceae, creating a new subfamily, Dumortie-
roideae Schust., for it and designating Dumortiera as the
type genus. Dumortiera has also been classified in the
Dumortieroideae by Bischler (1988), who regards Dumor-
tiera and Wiesnerella as morphologically remotely related,
although having similar flavonoid patterns. The treatment
of Schuster (1984) is followed here, even though the
phylogenetic position of Dumortiera remains a matter of
some controversy, as conceded by Schuster (1984). Sup-
porting the above treatment are terpene studies of the
genera by Asakawa et al. (1979, 1980a, 1980b, 1981), who
found that Wiesnerella denudata and Conocephalum coni-
cum shared 17 of these terpene compounds, but only had
three in common with Dumortiera hirsuta. Luteolin 5-0-
glucuronide, the flavonoid shared by Dumortiera and Wies-
nerella which was considered diagnostic for the Wiesnerel-
laceae by Campbell et al. (1979), has since also been
52
Bothalia 23,1 (1993)
FIGURE 2. — Dumortiera hirsuta. A,
male plant with subsessile
antheridiophore from above; B,
stalked archegoniophore with
dehisced sporangia, front one
releasing many spores and
elaters. A, B, Koekemoer 989 ,
x 9.
reported for Conocephalum by Porter (1981). Whittemore
(1991) therefore cautions against drawing taxonomic con-
clusions from a small number of compounds.
SPECIMENS EXAMINED
TRANSVAAL. — 2230 (Messina): Entabene, (— CC), Bottomley (PRE);
Entabene, (— CC), Schelpe 6020 (BOL); Soutpansberg, Entabene, (— CC),
Thomas 856 (PRE). 2329 (Pietersburg): Pietersburg, (—CD), Van Vuuren
1469 (PRE); Haenertsburg, ( — DD), Putterill 3604 (PRE). 2330 (Tza-
neen): Woodbush For. Res., Magoebaskloof, near stream, (— CC), H.
Anderson CH 13495, CH 13499 (PRE); Bosnian 3188 , (PRE); De Hoek
For. Res., Debengeni Falls, on stream bank, beyond foot bridge, (— CC),
S.M. Perold 2634 (PRE); Woodbush, locally abundant in deep shade
on streambank, (— CC), Schelpe 6070 (BOL). 2331 (Phalaborwa): Letaba,
(-DC), Scheepers 984 (PRE). 2430 (Pilgrim’s Rest): Farm Cyprus near
Ofcolaco, in gorge named ‘Terrible Hollow’, (— AB), H. Anderson CH
4527 (PRE); Mariepskop Forestry Water Works, on outside of water-
tank, also under overhang, dense shade, (— DB), Vorsier 87C (PRE);
Mariepskop, near dam in KJaserie River, montane forest, on rock against
bank next to stream, in shade, (— DB), Vorster 572; Mariepskop For.,
Bedford footpath in forest on soil of streambed, full shade, (— DB), Vor-
ster 1398 (PRE); Mariepskop For., Blyde River footpath, on exposed
tree root at streamside in forest shade, (— DB), Vorster 1472 (PRE);
Mariepskop, Blyde River footpath , hanging from vertical sandstone rocks
in forest shade, (-DB), Vorster 1473 (PRE); Mariepskop, Magalieskop
Res. For., on damp earth bank, dense shade, (— DB), Vorster 1815 (PRE);
Mariepskop, ( — DB), Van der Schijff 4482 (PRE); Mariepskop, Klaserie
River by dam, beneath rocks, (— DB), Van der Schijff 6291 (PRE); Mount
Sheba Nat. Res., at the ‘Grotto’, on dripping cliffs, forming extended
mats on wet vertical rock face, (—DC), Jacobsen 4421 (PRE); Mount
Sheba Nature Reserve at the ‘Grotto’, on dripping rock cliffs, (—DC),
Perold & Koekemoer 2864 (PRE); Pilgrim's Rest, (— DD), Van der Schijff
6367 (PRE). 2527 (Rustenburg): Nature Res. Cederberg kloof, near Uto-
pia, (— CA), Koekemoer 972 (PRE). 2530 (Lydenburg): Farm Klipsteen,
between Lydenburg and Dullstroom, at waterfall, on rock, (-AB), H.
Anderson CH 13446 p.p. (PRE); Sabie, Lone Creek Falls, on soil near
footpath, (—BA), S.M. Perold 2694 (PRE); Sabie Gorge, (— BB), V.A.
Wager 21 (PRE); on road to Lydenburg, at turnoff to Witklip, Coromandel
Farm, at waterfall, (-AB), Perold & Koekemoer 2839, 2844 (PRE); Nel-
spruit Dist., Rooiwal, (— BC), Bosnian 3180 ( PRE); Rosehaugh, ( — BD),
T.R. Sim CH 1286 (PRE); Kaapsehoop, (— DB), H.A. Wager 47 ( PRE);
Berlin State Forest, Kaapsehoop hiking trail near Battery Creek, (-DA),
Koekemoer 973, 975 (PRE).
Bothalia 23,1 (1993)
53
FIGURE 3. — Dumortiera hirsuta. A, spore, distal view; B, part
of elater. A, B, H. Anderson CH 4527. A, x 1730; B,
x 480. SEM micrographs by S.M. Perold.
SWAZILAND. —2531 (Komatipoort): King Forest, Havelock, occa-
sionally on wet shaded earth bank in forest, (— CC), Schelpe 6195 (BOL).
NATAL.— 2731 (Louwsburg): Ngoma For., bank of river, (—CD),
Gerstner 4386 (PRE); Ngoma For., Cetshwayo waterfall walk, vertical
slope, seepage, in deep shade, (—CD), Glen 2881 (PRE); Ngoma For.,
along path in Ntendeka, alongside streams in forest interior, (—CD),
Nicholas 1176 (PRE); Ngoma Forest, occasionally on deeply shaded earth
banks in forest, (—CD), Schelpe 6237 (BOL); Ngoma For., (—CD), T.R.
Sim CH 1302 (PRE); Ngoma For., Ntendeka, in forest, (-CD), A.E.
van Wyk 6973 (PRE). 2828 (Bethlehem): Mont-aux-sources, (— DD),
Doidge 171 (BOL, PRE). 2831 (Nkandla): Nkandla Forest, common on
rocks in and near water in shade, (— CA), Nixon 57 (BOL); Eshowe,
Signal Hill, (—CD), Van der Plank CH 1290, CH 1298 (PRE); Ngoya,
(-DC), T.R. Sim CH 1289 (PRE). 2929 (Underberg): Mpendle Dist.,
6 miles along Everglades/Boston Road River on stream bank, in shade,
(— DB), Moll 726 (BOL, PRE); Home Rule, Polela, (-DC), T.R. Sim
CH 1305 (PRE); Xumeni For., (— DD), Doidge 3581 (PRE); Donnybrook,
(-DD), Scott 3756 (PRE). 2930 (Pietermaritzburg): Karkloof, (—AC),
T.R. Sim CH1291 (PRE); Buccleugh, (—AD), T.R. Sim CH 1301 (PRE);
Pietermaritzburg, Town Bush, (— CB), T.R. Sim 7523, 7534; Waterfall,
(— CB), T.R. Sim 7548, 7574, 7586 (PRE); Pietermaritzburg, (-CB),
T.R. Sim 1296 (PRE); Sweetwater stream, (— CB), T.R. Sim 1300 (PRE);
Zwaartkop, (— CB), T.R. Sim CH 1328 (PRE).
CAPE.— 3226 (Fort Beaufort): Katberg For., (-BC), Garabedian
S. A.M.H. 49743 (BOL; PRE); Hogsback, (-DB), T.R. Sim 1895; Van
der Bijl 176; Young 1303 (PRE). 3 227 (Stutterheim): Perie Forest, (-CC),
T. R. Sim 7534 (BOL). 3318 (Cape Town): Cape Town, (-CD), H.A.
Wager 28 (PRE). 3322 (Oudtshoom): Rust en Vrede, at Oudtshoom,
(— CA), ex Herb. C. vanden Berghen (BOL). 3323 (Willowmore): Gou-
na Forest, near Lily vlei, (— CC), S. Amell 1736 (BOL); Bloukrans River
Pass, at bridge in forest, on rocks along stream, (—DC), Stirton 9648
(PRE); Bloukrans, along pass in river ravine, on vertical cliff face,
(-DC), Zantovska 155 (PRE). 3419 (Caledon): Oudebos, Rivier-sonder-
end, (— BB), Thome 3617 (BOL, PRE). 3420 (Bredasdorp): Leeuwrivier
Mountains, Swellendam, (— AB), Stokoe 9486 (BOL). 3423 (Knysna):
Knysna, Garden of Eden, (— AA), S. Amell 2096 (BOL); Knysna,
(— AA), T.R. Sim 1292 (PRE).
LUNULA RI A Adanson
Lunularia Adanson , Families des plantes 2: 15 (1763);
Micheli: 4 (1729); Nees ab Esenbeck: 29 (1838); Gottsche
et al.\ 510 (1846); Schiffner: 35 (1893); Stephani; 216
(1899); Howe: 59 (1899); Macvicar: 38 (1926); Sim 123
(1926); Muller: 366 (1951-1958); S. Amell: 73 (1963);
Hassel de Menendez: 125 (1963). Type species: Lunularia
cruciata (L.) Dum. ex Lindb.
Selenia J. Hill: 120 (1773) nom. illeg.
Staurophora Willd. 3: 101 (1809).
Dichominum Neck.: 345 (1790) (as subgenus).
Marsilia O. Kuntze 2: 837 (1891).
Sedgwickia S. Bowdich: 35 (1825).
Thallus large, flat, somewhat glossy, green, in overlying
patches, sometimes in extensive turfs; on damp soil in old
gardens, nurseries and forested areas, may have been
introduced into southern Africa. Branches dichotomously
furcate toward apex, new growth by apical or lateral
innovations; thickened over midrib, gradually thinning
toward slightly undulate, hyaline margins; apex emar-
ginate. Dorsal epidermis persistent, hyaline, cell walls
sometimes thickened at comers or entirely; air pores
simple, elevated and conspicuous, surrounded by several
concentric rings of cells, leading below into individual air
chambers, these in one layer and floored by chlorophyl-
lose layer of 3— 5-celled erect, branched filaments; storage
tissue compact, cells colourless, sometimes with pitted
walls; scattered cells throughout with single, large, brown
oil body; rhizoids numerous, between ventral scales and
on midrib, some smooth, others tuberculate; scales ventral,
in curved parallel rows on either side of midrib, with round
or reniform appendages, several cells con-
taining oil bodies.
Dioicous. Antheridia sunken into slightly elevated, oval
or kidney-shaped, disciform receptacles encircled by
raised, membranous sheath, at sides of male thalli
(although originally terminal). Archegonia enclosed in
terminal receptacles, but by continued growth of thallus
FIGURE 4. — Distribution of Dumortiera hirsuta, #; and Lunularia
cruciata, □, in southern Africa.
54
Bothalia 23,1 (1993)
FIGURE 5 .—Lunularia cruciata. A, dorsal view of thallus with gemma cups; B, female plant with young archegoniophores; C, ventral view
of thallus with new lateral branch; D, transverse section of thallus; E, transverse section of midrib region, much enlarged; F, transverse
section of air chamber; G, air pore seen from above; H, margin of thallus with hyaline cells, seen from above; I, older scale; J, young
scale; K, longitudinal section through young archegoniophore; L, longitudinal section through gemma cup; M, gemma. A, D— H, J,
L, M, S.M. Perold 2821\ B, C, S.M. Perold 1996. Scale bars: A-C = 2 mm; D, E, K, L = 1 mm; I, J = 500 /«n; F, M = 100 ^m;
G, H = 50 /im. Illustrations by A. Pienaar. Figure IK partly after Benson-Evans & Hughes fig. 4.
Bothalia 23,1 (1993)
55
laterally situated, conical, white and bud-like when young,
sheathed in layers of scales and slightly sunken into
rounded depression with distinct rim; after fertilization
and further growth, four tubular involucres in the form
of a cross are formed, each enclosing one or two sporo-
phytes, composed of foot, seta and capsule, raised on
unfurrowed, hairy stalk; capsules eventually exposed by
elongation of seta, the wall unistratose, lacking annular
thickenings, dehiscing by 4 valves. Spores very small,
green or brown, smooth. Elaters long, tapering and
bispiral. Gemmae numerous, disc-shaped, inside crescent-
shaped ridge; wholly diagnostic. Sporophyte virtually
unknown in southern Africa.
Lunularia cruciate (L.) Dum. ex Lindberg, Notiser
Sallskap pro Fauna et Flora Fennica Forhandlingar 9: 298
(1868); Howe: 60 (1899); Macvicar: 40 (1926); Sim: 24
(1926); Muller: 366 (1951-1958); S. Amell: 73 (1963);
Hassel de Menendez: 126 (1963); E.O. Campbell: 31
(1965). Type: In Europae umbrosis [OXF, syn.; H-SOL,
isosyn., fide Grolle (1976)]. For detailed synonymy see K.
Muller (1951-1958).
Thallus moderately large and flat, ribbon-like or margins
somewhat irregular (Figure 5A), glossy, bright green to
yellowish green, with outlines of subdorsal air chambers
faintly visible from above, each of the polygonal areas with
a central air pore, when wet; reticulum indistinct, leathery,
when dry; in crowded overlying patches, dichotomously
or irregularly furcate or with apical or lateral innovations
from ventral side of thallus (Figure 5C). Branches 40—55
x 5 — 8( — 10) mm, ± 650( - 1000 ) pm thick over median,
ventrally bulging midrib, gradually thinning out laterally
into wide wings (Figure 5D); apex emarginate or sinusoi-
dal; margins slightly undulate and somewhat scalloped,
with outer 4(5) cell rows hyaline.
Dorsal epidermal cells hyaline, in one layer, 5- or
6-sided to irregular in shape, 35—50 x 20—30 pirn, thin-
walled to somewhat thicker-walled or only thickened at
corners, in cross section 20—25 pm thick; marginal cells
with outermost row short- to long-rectangular (Figure 5H),
15-27 x 10-12 pm, cells of inner rows polygonal, 17-27
x 25 pm\ air pores simple, oval, raised, 17—25 x 12—20
pm in diameter, bordered by 3—5 rings of curved, smaller,
thin-walled cells (Figure 5G), 7—12 x 17—27 pm, outer
row of cells somewhat larger, 15—20 x 20—22 pun; air
chambers with domed roof (Figure 5F) raised 37—52 pun
above filaments, laterally separated by non-chlorophyllose
1 unistratose partitions obscured by filaments, floored by
dense chlorophyllose layer, ± 70 pirn thick, of 3— 5-celled
erect, branched filaments, filled with chloroplasts, top cell
often clavate, + 20 x 15 pun, others 20 x 12 pm; midrib
below assimilation cells, with ± 15(— 20) rows of com-
pact colourless storage cells (Figure 5E), 50—75 x 45 —50
pun, becoming smaller ventrally, some with pitted walls,
layers gradually decreasing in the wings; scattered cells
with brown oil bodies, round or oval, 30 x 30—45 x 27
pan; ventral epidermal cells 30—40 pirn wide, 15—25 pirn
! thick in cross section; rhizoids on midrib between scales,
numerous, smooth, ± 30 pirn wide, tuberculate, (10—)
17—22 pirn wide. Scales hyaline, some basal cells purple,
on either side of midrib, stretched across ventral face of
wings, near apex of thallus, base ± 1375 x 550 pun, with
rounded, constricted appendage (Figure 5J), ± 400 x 250
pun; cells mostly polygonal, ± 65 x 25 pun, some smaller,
with oil body 22 x 25 pirn, almost entirely filling cell;
older scales larger (Figure 51), base up to 1000 x 4250
pirn, appendage ± 600 pirn wide.
Dioicous. Male plants quite rare in southern Africa.
Anther idiophore on alternate sides, having originally
developed in terminal sinus near apex (Figure 6A), slighdy
raised, ovate, flatfish discs, 2—3 mm in diameter, encircled
by membranous sheath with crenate edges, containing
numerous antheridia, individually sunken in flask-shaped
cavities (Figure 6B) , opening above by pores. Archegonio-
phore originally also developing in terminal sinus near
apex, with further growth of thallus leaving it behind, so
that it appears lateral in position on alternate sides of
thallus (Figure 5B); commences as domed disc ± 200 x
375 pun, bearing several archegonia in radiating rows and
attached by very short stalk to floor of shallow, round hol-
low, 1100 pun wide x 300 pun deep, with crenate rim;
sheathed in ± 3 layers of scales (Figure 5K), outer layer
formed by fused, shaped scales, bulging in centre and con-
stricted below and above, upper edge irregularly fringed
with filiform cellular appendages of up to 7 rectangular
cells, ± 35 x 15 pirn, cells in body of scale thick-walled,
5- or 6-sided, up to 57 x 25 pun, in between numerous
smaller cells, 4- or 5-sided, 25 x 15 pirn, almost entirely
filled with single oil body; between scales and especially
from base of archegoniophore and arching over it,
numerous uniseriate, long hairs of 16—20 cells each.
Further development not recorded as fertilization did
not take place, nor are sporophytes available for study.
Gemmae numerous, disc-shaped (Figure 5M), notched
FIGURE 6. —Lunularia cruciata . A, antheridiophore seen from above;
B, longitudinal section through antheridiophore, with one flask-
shaped antheridium in place. A, Wilman BOL. No. 24870: B.
Koekemoer 1004. A, x 22; B, X 38. A, SEM micrograph; B,
LM photograph.
56
Bothalia 23,1 (1993)
by 2 opposite, lateral growing points, ± 430 in
diameter when mature, developing upright on short stalk,
inside crescent-shaped cupule (Figure 5L), ± 3 mm wide
with crenate to entire ridge on proximal side. Chromo-
some number n = 8 (Heitz 1927); n = 9 = 8 + x/y2
(Lorbeer 1934); n = 9 (Bornefeld 1987).
DISCUSSION
As mentioned in the description, male plants with
antheridial receptacles are exceedingly rare in southern
Africa and the only two, Wilman BOL No. 24870, on loan
from BOL and Koekemoer 1004 (PRE), were received after
completion of Figure 5 and therefore not illustrated there
(see Figure 6). Male plants are so rarely seen, that Sim
(1926) had categorically stated that they are not present
in South Africa, but then added ‘so far as is known’. He
must have been unaware of Saxton’s find. No female plants
with fertilized archegonia and mature sporophytes were
available for study; even plants with young archegonio-
phores are quite rare, judging both from personal
experience and from the literature (Saxton 1931; Good-
man 1956; E.O. Campbell 1965). Saxton (1931) found both
male and female plants in Cape Town in 1908, but had
to wait for almost 20 years for plants with mature
archegoniophores (forwarded from Dartmouth, England)
to complete his studies on the life history of L. cruciata.
Giffen sent plants with young archegoniophores from
Oranjezicht, Cape Town to Sim (Sim 1926) and Auret (as
mentioned in Benson-Evans & Hughes 1954) reported the
regular production of female branches in the vicinity of
Johannesburg. Of my own collections, only S.M. Perold
1996 from Devon Valley Hotel, Stellenbosch (November
1987), had young archegoniophores.
Since so many collections are from nurseries or city
gardens, it would appear that L. cruciata may have been
introduced into southern Africa. It is not frequently found
here, most collections being from the southwestern Cape,
a few from southern Transvaal and some from Natal, and
then quite frequently from nurseries (Figure 4). Further
north in Africa, L. cruciata is known from Zimbabwe
(Best 1990), Malawi (Nyika Plateau, S.M. Perold 2667,
2676 (PRE)); East African Mountains (Arnell 1956);
Tanzania (Serengeti) (Vanden Berghen 1965); Uluguru
Mountains, Rungwe Mountains (Bizot & Poes 1979);
Congo Rep. (Katanga) (Vanden Berghen 1965). Poes (pers.
comm.) states that in East Africa, L. cruciata is found
in many natural habitats in the montane forest belt, mostly
on young volcanoes such as Mt Elgon and Mt Meru and
even on the Comoro Islands.
Lunularia cruciata is quite widespread in the southern
hemisphere but regarded by Engel & Schuster (1982) as
probably Laurasian in origin. Since sexual reproduction
and subsequent spore production are so rare, its gemmae
obviously present a highly effective means of ensuring its
dispersal, which is most likely aided by human activities.
On the basis of its flavonoid chemistry, Campbell et al.
(1979), include it in the Marchantiaceae, but in the present
treatment Grolle (1983) is followed and L. cruciata is
classified in the monotypic family, Lunulariaceae Klinggr.
(1858).
Its phylogenetic position seems rather unclear, Schuster
(1984b) arguing that he would place it ‘low’ in the
Marchantiales on account of its high level of seta re-
tention, 2—3 sporophytes per gynoecium and a capsule
with 4 well-defined valves. On the other hand, he expresses
the viewpoint (Schuster 1984b) that its archegonio-
phore, clearly formed from two dichotomies, each
producing archegonia, is complex and therefore an
advanced feature.
SPECIMENS EXAMINED
TRANSVAAL.— 2528 (Pretoria): Pretoria, Union Buildings Nurseries,
(— CA), Bottomley CH 135 (PRE); Pretoria, National Botanical Institute
Nurseries, (— CA), S.M. Perold 2821 (PRE). 2627 (Potchefstroom),
Vereeniging, ( — DB), T.R. Sim CH 1283 (PRE); Roodepoort, Sterlig
Nursery, on gravel and brick walls of flowerbeds, (— DD), Koekemoer
1004 (PRE).
NATAL.— 2930 (Pietermaritzburg): Hilton Road, (— CB), T.R. Sim
CH 1279, CH 1280 (PRE). 2931 (Stanger): Durban, Silverglen Nurser-
ies, (- CC), S.M. Perold 2805 (PRE).
CAPE. — 3318 (Cape Town): Kirstenbosch, (—CD), S. Arnell 412
(BOL); Window Gorge, Table Mountain, (—CD), S. Arnell 405 (BOL);
Claremont Park, (—CD), Garside 6653 (BOL); near Round House,
(—CD), Garside 6132 (BOL); Oranjezicht, (—CD), Giffen CH 1281
(PRE); Glen Picnic Resort, just below Round House, Lion’s Head,
(—CD), S.M. Perold 645 (PRE); Round House, Lion’s Head, on soil
beneath trees, (—CD), S.M. Perold 650 (PRE); Newlands Forest, on
soil under trees, (—CD), S.M. Perold 662 (PRE); Cape Town, (—CD),
T.R. Sim CH 1278, CH 1282 (PRE); Skeleton Gorge, rock face, very
wet forest, (—CD), Stirton 9415 (PRE); mountain slopes above Kirsten-
bosch, (—CD), Stokoe s.n. (BOL); Kirstenbosch, (—CD), Wilman 24870
(BOL); Stellenbosch, (— DD), Burtt Davy CH 1277 (PRE); Pniel, on
tree trunk mixed with moss, (— DD), Morley 314 (PRE); Stellenbosch,
Devon Valley Hotel at garden fence, on soil, (— DD), S.M. Perold 1990
(PRE); Stellenbosch, Devon Valley Hotel, on soil bank behind hotel,
(— DD), S.M. Perold 1996 (PRE); Stellenbosch, (-DD), T.R. Sim CH
1284 (PRE); S Paarl, Landskroon, in kloof, (— DD), Volk 81/071 (BOL,
PRE). 3319 (Worcester): W of Franschhoek, Waterval Farm, on earth
bank, ditch next to dirt road, (— CC), S.M. Perold 633 (PRE); 4 km
N of Villiersdorp, Elandsriver Road, Du Toitsberge, near waterfall on
Sneeukop, (—CD), S.M. Perold 623 (PRE). 3322 (Oudtshoom): Ge-
orge, NE of Hawthomdene Hotel , at roadside on side of earth water fur-
row, (—CD), S.M. Perold 920 (PRE). 3418 (Simonstown): Constantia,
on soil on damp rock face, (— AB), S.M. Perold 656 (PRE).
ACKNOWLEDGEMENTS
I wish to express my gratitude to Dr R. Grolle for his
information regarding the publication date of ‘Hepaticae
Javanicae’ by Reinwardt et al. , as well as for drawing my
attention to Nelson & Parnell’s publication on the
synonymy of the various forms of Hygropyla etc. under
Dumortiera. I also thank Dr Grolle, Prof. T. Poes and
Prof. O.H. Volk for critically reading the manuscript and
for their valuable suggestions. Further thanks are due to
the curator of BOL for the loan of specimens; to the artists,
Ms G. Condy and Ms A. Pienaar; to the typist, Mrs J.
Mulvenna and to the photographer, Mrs A. Romanowski.
Also to my colleagues at NBI, particularly Drs H.
Anderson and H.F. Glen, as well as Miss M. Koekemoer
for collecting specimens.
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.
'
Bothalia 23,1: 59-64 (1993)
Panicum simulans (Paniceae, Poaceae), a new species from southern
Africa and its leaf anatomy
L. SMOOK* and R.P. ELLIS**
Keywords: leaf anatomy, morphology, Namibia, new species, Panicum, Poaceae
ABSTRACT
Panicum simulans Smook from northern Namibia is formally described. The morphology and leaf blade anatomy in
transection and surface view, as observed under the light microscope, are described. The species is compared to others
with which it has been confused in the past, P. simulans can be readily distinguished from P. novemnerve Stapf and
P. schinzii Hack, on the basis of both anatomical and morphological characters such as the venation of the lower glume
and the photosynthetic anatomy, which is of the NAD-me subtype of the C4 photosynthetic pathway. On this basis it appears
that P. simulans is closely allied to the P. coloratura L. group of species and should be placed in section Panicum of subgenus
Panicum.
UITTREKSEL
Panicum simulans Smook vanaf die noordelike Namibie word formeel beskryf. Die morfologie en blaaranatomie, in deursnee-
en oppervlakaansig, soos met die ligmikroskoop waargeneem, word beskryf. Die morfologie en blaaranatomie van P. simulans
word vergelyk met die van twee ander spesies wat verwarring in die verlede geskep het. P. simulans kan maklik van
P novemnerve Stapf en P. schinzii Hack, onderskei word op grond van die bearing van die onderste gluma en die fotosintetiese
anatomie wat van die NAD-me subtipe van die C4-fotosintetiese weg is. Op grond van hierdie gegewens word P. simulans
in die seksie Panicum van subgenus Panicum geplaas.
Panicum simulans Smook, sp. nov.
Panicum sp. 2 (Giess 8605 ) in Gibbs Russell et al 242 (1990).
Panicum spp. in Group 3a in Ellis (1988).
Panicum simulans Smook, sp. nov., P. novemnervi Stapf
similis sed gluma inferiori uninervi, flosculo inferiori
masculo, paleaque inferiori bene evoluta differt; P. schinzii
Hack, similis sed nodis culmorum adpresso-hirsutis,
apicibus glumae superioris et lemmae inferioris erectis vel
recurvis, atque chloroplastis centripetis, non centrifugis,
differt.
Annual. Plant variable; usually yellowish green in
colour, often flushed purple. Culms erect to geniculate,
600(— 1 200) mm high (from plant base to top of inflores-
cence); sometimes rooting at nodes; nodes with adpressed
silvery white hairs pointing upwards; base covered with
leaf sheaths; internodes usually not visible. Leaf sheaths
glabrous or with bulbous-based hairs varying in length and
size of hair and relative size of base. Ligule a fringed
membrane 1.4 mm long (membranous rim 0.3 mm, cilia
1.1 mm long). Leaf blade linear, 5 — 200(— 250) x 2—15
mm, straight or cordate at base, flat, many-nerved,
bulbous-based hairs present or absent; apex acute to
acuminate; margins white, smooth to scaberulous to
densely scabrid; adaxial surface densely papillate
especially on lower leaves; nerves of abaxial leaf surface
smooth, occasionally densely scabrid especially near leaf
apex (variable on same plant).
* National Botanical Institute, Private Bag X101, Pretoria 0001.
** Agricultural Research Council, Roodeplaat Grassland Institute, Private
Bag X05, Lynne East, Pretoria 0039.
MS. received: 1992-02-13.
Inflorescence a panicle (80-)160-250(— 400) mm long,
narrowly obovate to obovate, occasionally oblanceolate,
sometimes asymmetrical (lowest branch longest,
protruding beyond other branches), moderately branched,
usually ascending and spreading; lowest branches single
or a number arising from same side, not whorled; next
set of branches often whorled or in a pseudo-whorl;
branches naked for a long way up from base with spike-
lets crowded at apices, smaller branches usually scabrid
with prickles becoming denser, longer and larger towards
spikelets; spikelets usually in pairs on long-short pedicels
on branchlets. Spikelets narrowly obovate to obovate-
elliptic, (2.2— )2.4-2.6(-3.0) mm long, acute to acumi-
nate, often flushed purple. Lower glume broadly ovate, '/3
to just over '/2 as long as intact spikelet, clasping base of
spikelet, membranous; central nerve distinct, often
scaberulous to scabrid; lateral nerves obscure, if present,
only visible at base; apex acute to acuminate, sometimes
minutely mucronate or with a brush of prickles. Rachilla
pronounced between glumes. Upper glume 2.4— 2.6(— 3.0)
mm long, longer than lower lemma, membranous, 7—9(11)-
nerved (nerves nearest margins sometimes obscure and
short); central nerve thickened at apex, forming a usually
scabrid mucro; apex acute to acuminate, either erect or
slightly recurved outwards; margins below apex mem-
branous and folding inwards, often flushed purple and then
mainly at apex. Lower floret male only; anthers 3, deve-
loped 1.4— 1.7 mm long or rudimentary, both conditions
present on same inflorescence, dark orange-brown. Low-
er lemma similar to, but shorter than upper glume, fitting
into its apex, (7-)9-nerved; cross venation often visible;
central nerve scaberulous, thickened towards apex; apex
acute to truncate; margins broad and membranous,
either folded in or out, often purple especially near apex.
Lower palea well developed, nearly as long and as wide
as lower lemma. Upper lemma and palea smooth, shiny,
pale, white to straw-coloured, occasionally dark with
60
Bothalia 23,1 (1993)
FIGURE 1. — Panicum simulans. A,
habit, x 0.5; B, node showing
adpressed hairs, x 2.5; C,
ligule, x 2.5; D, spikelet
showing lower glume, X 10;
E, spikelet showing upper
glume, X 10; F, lateral view of
open spikelet, x 10. From
Smook 5108 and Giess 8605.
distinct yellow nerves on upper lemma, both colour forms
sometimes present on same plant. Styles .2, separate;
stigmas plumose, purple to dark brown (on herbarium
specimens). Figure 1.
three species clearly and to justify the recognition of
P. simulans (Table 1). The specific epithet refers to the
superficial similarity between P. simulans, P. schinzii and
P. novemnerve.
TYPE. — Namibia, 1915 (Otjihorongo): 25 km N of
Outjo on road to Okaukuejo, (— DD), Smook 5108 (PRE,
holo.) ( Smook 5108a , PRE, isotype*).
Panicum simulans has been confused with P. schinzii
Hack, and P. novemnerve Stapf in the past, and the
specimens now included in this new species have been
misidentified as either of these two species. However, this
study shows that several characters serve to separate these
* This is the anatomical voucher specimen.
Figure 2 shows the known distribution of P simulans.
It is restricted to northern Namibia but may possibly also
occur in southern Angola. It is associated with various
vegetation types ranging from mopane woodland to
mopane mixed with Acacia, Combretum or Terminalia to
sweet grassland on limestone soils such as occur around
Etosha Pan.
Panicum simulans is hydrophytic and grows typically
in areas with seasonally high moisture regimes as found
in vleis and around fountains. It may even occur in more
Bothalia 23,1 (1993)
61
TABLE 1. Comparison between Panicum novemnerve, P. simulans and
P. schinzii
ephemerally moist situations such as in depressions in
disturbed situations along roadsides or irrigated lands or
in natural hollows in granite outcrops or saturated soil
pockets overlying calcrete.
Specimens examined
NAMIBIA. — 170 (Swartbooisdrift): Kaokoveld, (— DD), Merxmueller
& Giess 35538. 180 (Ohopoho): Kaokoveld, (— BB), De Winter & Leist-
ner 5160. 1815 (Okahakana): Etosha National Game Park, (-DC), Le
Roux 1399. 1817 (Tsintsabis): 56 km S of Namutoni on road to Tsumeb,
(—CD), Smook 5153*'. Farm Falkenhain GR/TS 303, (—DA), Giess 15090.
1914 (Kamanjab): 15 km N of Otjovasandu, (— AB), Giess 9253; Farm
Grootberg, (—CD), Du Toil 236. 1915 (Okaukuejo): Etosha National Game
Park, Vogelnestvley, (-BB), Giess & Mueller 13971 , 10 km S of
Okaukuejo, Giess & Loutit 14143; 9 km E of Okaukuejo, Smook 5109*.
(— BB), Ttnley 1299A; Ombika, (— BD), Le Roux 328; Ombika detour,
Giess & Loutit 14113; near Ombika, Giess 15098; 25 km N of Outjo on
road to Okaukuejo, (— DD), Smook 5108*. 1916 (Gobaub): Etosha National
Game Park, Olifantsbad, (— AA), Ellis 5271* 5273*; Gemsbokvlakte,
(— AA), Smook 5110*; Halali, (-BA), Van der Westhuizen 23. 1917
(Tsumeb): Tsumeb, (—BA), Giess 8605. 1918 (Grootfontein): Farm Sus,
(-AB), Schweickerdt 2144. 2015 (Otjihorongo): Farm Pamela, (-AB),
Volk 2855; Farm Babatsi, (— AB), Gibbs Russell & Smook 5628*; Farm
Straussenheim OUT 133, (— BB), Giess, Volk & Bleissner 6004. 2115
(Karibib): Farm Etemba, (-BC), Giess 10799; Farm Schlucht OM 162,
(-DA), Giess 8435; Farm Ameib, Giess, Volk & Bleissner 5898. De
Winter & Hardy 8072.
LEAF ANATOMY OF PANICUM SIMULANS
In order to obtain further evidence relating to the taxo-
nomic status and position of P. simulans, a detailed
anatomical study was undertaken. The methods used are
described in Ellis (1988) and the terminology used is
defined in Ellis (1976 & 1979). The following abbrevia-
tions 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 or mestome sheath
obs = outer or parenchyma sheath
Leaf blade in transverse section
Outline : expanded blade, flat to very broadly V-shaped;
arms of lamina straight or gently undulating; blade
symmetrical about midrib. Ribs and furrows : shallow and
wide adaxial furrows present between all vbs; slight,
* voucher specimens for anatomical study
rounded ribs occur in association with all vbs; similar ribs
occur over all vbs. No abaxial ribs or furrows present.
Median vascular bundle; variable, either median bundle
only present (this indistinguishable structurally from lateral
l’vbs and without additional parenchyma tissue) (Figure
3A) or keel with associated colourless parenchyma tissue
present (Figure 3B); 1, 3 or 5 vbs incorporated in keel;
all bundles abaxially located; larger keels rounded with
single adaxial groove; no adaxial sclerenchyma developed
and abaxial girders associated with all vbs; no air spaces
in keel. Vascular bundle arrangement; 5, 7, 9 or 11 l’vbs
in transection; 3, 4 or 5 3’vbs between consecutive l’vbs;
narrower leaves without keels, with 5 l’vbs and with three
3’vbs between successive larger bundles. No 2’vbs. All
vbs situated in centre of blade. Vascular bundle descrip-
tion; 3’vbs circular in outline with xylem and phloem
distinguishable, l’vbs circular in shape, lysigenous cavities
present (Figure 3E, F) and metaxylem vessels narrow
(diameters less than those of obs cells) and circular.
Vascular bundle sheaths; obs conspicuous, round, entire
(except with small abaxial interruption in l’vbs) and
without extensions; consists of 6, 7 or 8 cells around 3’vbs
and 11—14 cells around l’vbs; obs cells fan-shaped with
radial walls straight and outer tangential walls inflated
(Figure 3E, F); all cells similar in size and shape;
chloroplasts dense, filling entire cell lumen or concentrated
centripetally, near inner tangential wall. Ibs absent in
3’vbs; complete but inconspicuous in l’vbs; cells very
much smaller than obs cells; adaxial cells slightly larger
and thin-walled; lateral and abaxial cells uniformly
thickened but degree of secondary thickening very vari-
able. Sclerenchyma; minute adaxial and abaxial strands
only associated with l’vbs; no fibrous tissue in associa-
tion with 3’vbs. Small sclerenchyma caps in leaf margin
(Figure 3A). Chlorenchyma; distinctly radiate; single layer
of tabular cells completely surrounds all vbs (except some-
times for a short abaxial interruption with l’vbs); radiating
chlorenchyma of successive bundles in direct contact and
not separated by colourless parenchyma. No colourless
parenchyma tissue present (except in midrib, if present).
Adaxial epidermal cells; bulliform cells small, in rather
extensive groups; central bulliform cell occupies less than
'/4 of leaf thickness; cuticle very thin; no macrohairs,
except rarely in association with margin; no prickles or
hooks evident; cuticular papillae common, much narrower
than epidermal cells and with one per cell as seen in
FIGURE 2. — The known distribution of Panicum simulans.
62
Bothalia 23,1 (1993)
FIGURE 3. — Leaf blade anatomy of Panicum simulans as seen in transverse section. A, outline of specimen without keel; median vascular bundle
only (arrowed), this bundle structurally indistinguishable from other first-order vascular bundles; B, outline of specimen with distinct keel
incorporating four vascular bundles and adaxial colourless parenchyma tissue; C, typical C4 photosynthetic anatomy with prominent paren-
chyma sheaths; D, specimen showing distinct centripetal location of Kranz chloroplasts in outer bundle sheath cells; E, dense chloroplasts
in outer bundle sheath cells and radiate chlorenchyma, note adaxial papillae; F, typical NAD-me type photosynthetic anatomy. A, B, x
100; C, D, X 250; E, F, x 400. A, C, Smook 5108', B, Smook 5720; D, Gibbs Russell & Smook 5268', E, Smook 5153', F, Smook 5110.
section (Figure 3C— F). Abaxial epidermal cells: central
cells of intercostal zones larger and resemble bulliform
cells in transection; cuticle thin; no macrohairs, prickles
or papillae.
Abaxial epidermis in surface view
Zonation: evident but costal zones overlying 3’vbs often
without silica bodies as a result of absence of sclerenchyma
strands in association with these bundles. Intercostal long
cells: elongated (length more than 3 X longer than width),
side walls parallel to outwardly bowed, end walls vertical;
anticlinal walls very thin and slightly undulating, with
degree of sinuosity varying with plane of focus; cell shape
varies across individual intercostal zones with two files
of bulliform- like cells per intercostal zone; these bulliform-
like cells actually represent central files of two intercostal
zones but costal zones are poorly differentiated (Figure
4C, D). Very few tall and narrow short cells present.
Stomata: 2 or 4 files of low dome-shaped stomata per
intercostal zone; usually separated by a single elongated
interstomatal cell. Papillae: absent. Prickles: absent.
Microhairs: bicellular with dehiscent distal cell; only basal
cells remain, basal cell elongated with length much greater
than width; occur in central files of intercostal zones
(Figure 4D). Macrohairs: absent. Silica bodies: very
irregular dumbbell-shaped; horizontally elongated; same
width as adjacent long cells. Costal short cells : 1 or 3 files
of cells comprise costal zones; central file with silica bod-
ies, these alternate irregularly with short to long short
cells. Costal zones often not associated with 3’vbs, only
present over l’vbs.
DISCUSSION
In general appearance P simulans closely resembles
P. schinzii , particularly those forms of both taxa that have
rounded or cordate leaf bases. However, the hairy nodes
(Figure IB) and pointed apex of the spikelets (Figure ID,
E) and colour of plant (yellowish green vs. green) of P.
simulans clearly separate these two taxa (Table 1) (Gibbs
Russell et al. 1990).
Bothalia 23,1 (1993)
63
All specimens from Namibia previously assigned to
P. schinzii have now been re-identified as P. simulans.
There is one exception, Volk 2672. However, there is no
habitat information for this specimen, and it may have been
a weed from a cultivated land and imported with the crop.
Panicum schinzii and P simulans both tend to be hydro-
phytic, but they are clearly separated geographically. Their
natural populations were undoubtedly originally allopatric,
but it can be expected that, with increasing agriculture
under irrigation, P. schinzii will become established in the
range of P. simulans.
In addition to the morphological differences between
Panicum simulans and P. schinzii, there are major differ-
ences in the photosynthetic leaf anatomy between these
two taxa. P. simulans has the NAD-me subtype of the C4
photosynthetic pathway, as the anatomy is Kranz with a
double bundle sheath with the specialized chloroplasts of
the parenchyma sheath centripetally arranged (Ellis 1988).
The Panicum species with this type of photosynthetic
anatomy constitute the ‘true’ Panicum species (Brown
1977) as P. miliaceum L., the type of the genus, belongs
to this group.
Panicum schinzii, on the other hand, characteristi-
cally has the Kranz chloroplasts located against the outer
tangential cell wall. These chloroplasts are relatively small
and often form only a thin peripheral layer in contrast to
the large, dense chloroplasts of P. simulans. The anatomy
of P. schinzii is typical of that of the PEP-ck subtype of
the C4 pathway (Ellis 1988). Brown (1977) considered all
the Panicum species of this PEP-ck subtype, as doubtful
members of the genus and as belonging to Brachiaria,
together with Urochloa and Eriochloa. This applies
particularly to those species with rugose lemmas.
Ellis (1988) grouped Panicum simulans and P. schinzii
in two different subgeneric groups because of these distinct
anatomical differences. P. schinzii was placed in Group
2d whereas P. simulans (as Panicum spp., together with
P. novemnerve) was placed in Group 3b.
Group 2, although the leaf anatomy is typically PEP-ck
throughout, actually consists of two distinct and separate
groups. Group 2d with P. schinzii, together with P. gilvum
Launert, P. impeditum Launert, P. repens L. and P. sub-
albidum Kunth, are all hydrophytic and have pale, glossy
upper lemmas. These taxa are clearly not closely allied
to Groups 2a— 2c, all of which appear to belong to the
panicoid grasses with rugose lemmas. The P. schinzii
group of species (except P. repens) belongs to section
Dichotomiflora (Hitchc. & Chase) Honda of subgenus
Panicum (Zuloaga 1987) and is not closely allied to
P. simulans despite the superficial morphological resem-
blance.
The work of Ohusigi et al. (1982) urges caution in
assigning P. schinzii and its allies to the PEP-ck photosyn-
thetic subtype as they may actually all be NAD-me. The
biochemical typification of these taxa urgently needs
verification before final taxonomic decisions can be made.
However, this has no bearing on the separation of P.
simulans from this group.
In the past P. novemnerve has also been confused with
P. simulans. However, P. simulans has only one distinct
FIGURE 4.— Abaxial epidermal structure of Panicum simulans. A, typical zonation pattern with 5 narrow costal zones located over third-order
bundles between successive first-order bundles; B, leaf margin showing cushion-based macrohair; C. stomata and microhairs in intercostal
zones; D, low dome-shaped stomatal subsidiary cells, basal cells of microhairs and very irregularly dumbbell-shaped silica bodies. A,
B, x 160; C, x 250; D, x 400. A, D, Smook 5153 ; B, Smook 5U0; C, Smook 5109.
64
Bothalia 23,1 (1993)
and obvious nerve on the lower glume (Figure ID) instead
of 3—5 as in P novemnerve. In P. novemnerve the lower
floret is sterile with a reduced palea (Stapf 1920), whereas
in P simulans the lower floret is male with a well-
developed palea (Gibbs Russell et al. 1990). These two
taxa can, therefore, be readily separated on morphological
criteria.
Panicum simulans and P. novemnerve also share similar
damp habitats although P. novemnerve appears to prefer
shady areas. They are sympatric in Namibia, but P. novem-
nerve also occurs in Botswana and the Transvaal.
The leaf anatomy of P novemnerve (as based on Smook
5163 and Gibbs Russell & Smook 5235) and P. simulans
is virtually identical. Both have the NAD-me type anatomy
with very little sclerenchyma development. The only
discernible difference appears to be that the intercostal long
cells in P. novemnerve are often separated by tall and
narrow short cork cells, which is very seldom the case
in P. simulans. Both P simulans and P. novemnerve
specimens were included under Panicum spp. of Group
3a by Ellis (1988) because of this similarity in leaf blade
anatomy. These two annual species, together with P.
arcurameum Stapf and P. atrosanguineum A. Rich.,
undoubtedly belong to the P. coloratum L. group of
species, and show very close similarities with P. pil-
gerianum (Schweick.) Clayton [= Psilochloa pilgeriana
(Schweick.) Launert], another annual hydrophyte. This
latter species has only recently been placed in Panicum ,
and this small group of annual species appears to form
a clear subgrouping within the P coloratum group of
species. They resemble an unnamed perennial entity within
P. coloratum particularly closely, as discussed by Ellis
(1988). Specimens of this taxon are Ellis 1783, 2905 and
2912, all of which are also hydrophytes. Oryzidium
bamardii C.E. Hubb. & Schweick., may also belong to
this assemblage.
Panicum simulans, therefore, appears to belong with the
‘true’ Panicum species of section Panicum of subgenus
Panicum (Zuloaga 1987). These are typical NAD-me
species as suggested by the leaf anatomy but biochemical
typing is required.
REFERENCES
BROWN, W.V. 1977. The Kranz syndrome and its subtypes in grass
systematics. Memoirs of the Torrey Botanical Club 23: 1—97.
ELLIS, R.P. 1976. A procedure for standardizing comparative leaf blade
anatomy in the Poaceae. I. The leaf blade as viewed in trans-
verse section. Bothalia 12 : 65-109.
ELLIS, R.P. 1979. A procedure for standardizing comparative leaf blade
anatomy in the Poaceae. II. The epidermis as seen in surface view.
Bothalia 12: 641—671.
ELLIS, R.P. 1988. Leaf anatomy and systematics of Panicum (Poaceae:
Panicoideae) in southern Africa. Monographs in Systematic
Botany IS: 129-156.
GIBBS RUSSELL, G.E., WATSON, L., KOEKEMOER, M., SMOOK,
L., BARKER, N.P., ANDERSON, H.M. & DALLWITZ, M.J.
1990. Grasses of southern Africa. Memoirs of the Botanical Survey
of South Africa No. 58.
OHUSGI, R., MURATA, T. & CHONAN, N. 1982. C4 syndrome of
species in the Dichotomiflora group of the genus Panicum.
Botanical Magazine (Tokyo) 95: 339—347.
STAPF, O. 1920. Gramineae. In D. Prain, Flora of tropical Africa, Vol.
9. Reeve, Ashford.
ZULOAGA, F.O. 1987. Systematics of New World species of Panicum
(Poaceae: Paniceae). InT.R. Soderstrom et al., Grass systematics
and evolution: 287—306. Smithsonian Institution Press, Washing-
ton D.C.
Bothalia 23,1: 65-83 (1993)
Notes on African plants
VARIOUS AUTHORS
ROSACEAE
OBSERVATIONS ON CLIFFORTIA MICRANTHA
A fresh specimen of a Cliffortia species from the Swart-
berg ( Vlok 2113) clearly showed more than one style and,
following Weimarck’s (1934, 1948) keys, was identified as
C. propinqua Eckl. & Zeyh. (subgenus Digraphidium sec-
tion Complanatae) , but its appearance differed greatly
from that species. It did, however, match C. micrantha
Weim. (subgenus Monographidium, section Costatae or
Bacciformes ; see below) a single-styled species, both in
appearance and by key except for the number of styles.
With the handling of the fresh specimen, it was clear that
the styles were easily shed. A re-evaluation of existing
herbarium collections of C. micrantha seemed, therefore,
necessary. In 15 herbarium specimens examined from three
major Cape herbaria (BOL, NBG, STE), two-styled fruits
were found occasionally on only five of the specimens;
most fruits had no styles and a few only one. The fresh
specimen ( Vlok 2113) was predominantly two-styled with
only a few three-styled fruits.
According to Weimarck (1934, 1948), the number of
styles and achenes correspond. It should therefore be
feasible to count the achenes instead of the styles.
The number of achenes in at least two fruits per
specimen, were counted for the 15 specimens of C.
micrantha. The fruits of the fresh Swartberg specimen
( Vlok 2113) were also examined for number of achenes.
Esterhuysen 28523, identified by the collector as C.
micrantha, but possibly of hybrid origin (see below), was
also examined.
All the fruits of C. micrantha proper contained at least
two achenes. A single specimen from near Prince Albert
{Bond 1680) had two to three achenes per fruit. A
specimen from Noukloof Nature Reserve {Laidler 154) had
two to four achenes per fruit as well as two styles on some
of the fruits. The Swartberg specimen ( Vlok 2113) had two
to three achenes corresponding with the number of styles
(Figure LA— E). The fruit of Esterhuysen 28523 appeared
more oblong and furrowed than the norm for C. micran-
tha and contained only one achene. Closer examination
showed this specimen to differ from C. micrantha in the
shape and size of the leaves as well, tending towards the
characters found in C. cervicomu Weim. (Weimarck 1959).
If it is accepted that one style concurs with one achene
and two (or more) styles with two (or more) achenes con-
sistently enough to subdivide a genus (Weimarck 1934,
1948), then C. micrantha must be regarded as a multiple-
styled species because there were never less than two
achenes per fruit in all the specimens examined. This is
confirmed by the fresh Swartberg specimen {Vlok 2113)
which has two to three styles and two to three achenes.
Weimarck’s (1934, 1948) perception of C. micrantha as
having a single style could be due to the fact that the styles
in his material had been shed. As he equated the number
of achenes to the number of styles, it is most likely that
he did not examine the achenes in this species.
Weimarck (1940) placed C. micrantha in the section
Costatae with C. serpyllifolia Cham. & Schlechtd. and
C. browniana Burtt Davy on the basis of its ribbed fruits
and the mistaken assumption that it has a single style.
C. micrantha can, however, have ribbed or smooth fruits,
depending on the age of the fruit, (Figure LA, F & G) and
was therefore placed in two divisions in his key for the
section Costatae (Weimarck 1948). In the same article,
he placed C. micrantha in his key for the section
Bacciformes as well (Weimarck 1948). He discussed it
under the latter section which contains only one other
species, C. baccans Harv. This latter species has a smooth
and berry-like fruit, resembling the mature fruit of
C. micrantha, but with only one style. If C. micrantha
is retained in either the sections Bacciformes or Costatae,
the number of styles loses its taxonomic importance.
Furthermore, the feasibility of subdividing the genus into
subgenera on this basis becomes questionable.
On the above evidence, C. micrantha should be placed
in the subgenus Digraphidium on the basis of the
predominance of two-styled flowers. This placement is fur-
ther substantiated by the trifoliate leaves, the tetra-
merous flowers and the low stamen count common in this
subgenus. However, fruits of the only section {Complana-
tae) of this subgenus are flattened and hard, and not
berry-like as are the mature fruits of C. micrantha (Figure
LA). The older fruits, however, can appear ribbed and the
two-achened ones are dorsiventrally flattened, to some
extent resembling the fruits in the section Complanatae
(Figure IF & G). C. micrantha might therefore be placed
in the subgenus Digraphidium but in its own section. This
needs further investigation.
The possible occurrence of more than two styles and
achenes in the recognised two-styled species of Cliffortia
also needs investigation.
The probability of the specimen Esterhuysen 28523
being a hybrid between C. micrantha, a two-styled species,
and C. cervicomu Weim., a one-styled species, raises
more questions about relationships. A field trip to collect
fresh material of this probable hybrid was unsuccessful,
but needs to be done again as part of further work on
hybridisation and relationships in the genus.
SPECIMENS EXAMINED
For number of styles
CAPE. — 3320 (Montagu): Touwsberg, in kloof, S slope near top, 1 100
m, 11-07-1941, (-DB), Levyns 7483 (NBG). 3321 (Ladismith): Swart-
FIGURE I. — Cliffortia micrantha : A, mature fruit with two styles (bracteoles in place, covering the stipe). B, mature fruit in longitudinal section
showing flat sides of two achenes (a, a’) covered by two layers of tissue; stipe (b) attached; sepals, styles and bracteoles removed. C, top
view of three-styled fruit; D, styles from C; E, achenes from C; F, old fruit, side and corresponding top views showing ribs and dorsiventral
flattening; G, old fruit, showing four major and four minor ribs in a regular pattern. A— E, Vlok 2113 (STE); F, Laidler 154 (STE); G,
drawn from Boshoff 315 (STE). Scale bar = 2 mm.
berg, top of pass into Gamkaskloof, 1 333 m, 8-05-1963, (— BC), Taylor
4744 (STE); Swartberg, in ravine between Kliphuisvlei and Gamkas-
kloof, 1 250 m, 7-05-1989, (-BD), Vlok 2113 (PRE, STE); Noukloof
Nature Reserve, gentle SE slope, 566 m, 12-07-1982, (— CA), Laidler
154 (STE); Roodeberg, S slope near stream, 24-05-1950, (— CB),
Esterhuysen 17152 (NBG).
For number of achenes
CAPE. — 3320 (Montagu): Anysberg, S slopes, 810 m, 2-08-1956,
(-DA), Wurts 1424 (NBG); Touwsberg, steep rocky lower S slopes to
1 000 m, 1-06-1956, (-DB), Esterhuysen 25933 (BOL); Touwsberg, 1 100
m, 11-07-1941, (-DB), Levyns 7483 (Type) (BOL, NBG, STE). 3321
(Ladismith): Ladismith, koppie 4 miles from town, 566 m, 15-08-1948,
(—AD), Levyns 9030 (BOL); Gamka Mtn Reserve, N slope (moist kloof),
866 m, 03-1976, (— BC), Boshoff P315 (STE); Prince Albert— Gamkaskloof
road, 890 m, 3-08-1979, (— BD), Bond 1680 (STE); Swartberg, in a ravine
between Kliphuisvlei and Gamkaskloof, 1 250 m, 7-05-1989, (— BD),
Vlok 2113 (STE); Noukloof Nat. Res., gentle SE slope, 566 m, 12-07-1982,
(-CA), Laidler 154 (STE); Roodeberg, S slopes near stream, 24-05-1950,
(— CB), Esterhuysen 17152 (BOL, NBG,); Roodeberg, 1 000 m,
10-08-1948, (-CB), Levyns 8981 (BOL, STE).
Probable hybrid (C. micrantha X C. cervicomu)
CAPE. — 3321 (Ladismith): Swartberg foothills between Bosluis Pass
and Die Hel, 10-10-1960, (-BC), Esterhuysen 28523 (BOL).
REFERENCES
WEIMARCK, H. 1934. Monograph of the genus Cliffortia. Gleerupska
Universitet Bokhandeln, Lund.
WEIMARCK, H. 1940. Cliffortia micrantha H. Weimarck spec. nova.
Botaniska Notiser 1940: 97—99.
WEIMARCK, H. 1948. The genus Cliffortia, a taxonomic survey.
Botaniska Notiser 1948: 175—185.
WEIMARCK, H. 1959. Four new Cliffortia species. Botaniska Notiser
112 : 77-79.
A.C. FELLINGHAM*
* Stellenbosch Herbarium, National Botanical Institute, P.O. Box 471,
Stellenbosch 7599.
MS. received: 1992-03-16.
Bothalia 23,1 (1993)
67
ROSACEAE
CLIFFORT1A FASCICULATA, A SUPERFLUOUS NAME FOR C. AMPLEX1STIPULA
In his monograph of the genus, Weimarck (1934) placed
Cliffortia amplexistipula Schltr. under the imperfectly
known species. He quoted Schlechter’s original descrip-
tion in full (Schlechter 1900) but pointed to the lack of
flower and fruit details which did not enable him to identify
the species accurately.
Cliffortia amplexistipula Schltr. in Botanische Jahr-
biicher 27: 140 (1900); Weim.: 157 (1934), sub species non
sat. cog. Type: In sabulosis prope Ezelbank, in montibus
Cederbergen, alt. c. 4000 ped., 2 Sept. 1896, Schlechter
8825 (Bf, holo. ; BOL! lectotype here designated; BM,
GRA, K, isolecto.).
This inadequacy led to the description of C. fasciculata
Weim. (Weimark 1946). Two years later, Weimarck (1948:
174) stated in one short sentence: ‘C. fasciculata has,
however, proved to be identical with C. amplexistipula
Schltr.’ and proceeded to use the latter name in his key.
This fact was also communicated to the Bolus
Herbarium as seen in a handwritten note on the sheet of
an isotype of C. fasciculata Weim. in BOL which reads:
‘Weimarck states in a report on material sent, that C.
fasciculata Weim. is a synonym for C. amplexistipula
Schltr.’ This note is initialled by E. Esterhuysen and dated
10/48.
In Gibbs Russell etal. (1987), both C. fasciculata Weim.
and C. amplexistipula Schltr. are listed as correct names.
Weimarck (1934) examined Schlechter’s type of C.
amplexistipula , ( Schlechter 8825), from five different
herbaria, the one in Berlin presumably being the holo-
type. As this one was destroyed, I hereby choose the Bolus
Herbarium specimen as lectotype of C. amplexistipula
Schltr.
C. fasciculata Weim.: 40 (1946). Type: N Cederberg, between Henning
(Heuning?) Vlei and Koupoort, 21-10-1945, Esterhuysen 12116 (LD, holo.;
BOL!, iso.).
Schlechter’s (1900) original description of C. amplexi-
stipula (as quoted by Weimarck 1934) did not include
flowers and fruit. Weimarck’s (1946) description of C.
fasciculata does include male and female flowers but no
fruit.
Description : to augment the description of this species,
the following observations are made:
Leaf sheaths: ventral apical portion with persistent red
fringe resembling stigma, amplexicaul when young, some-
times splitting when older. Stipules minute when young
to 0.25 mm long later. Leaflets: dorsal surface with raised
round spots to the margins (‘marginibus subscabridis’ of
Schlechter), spathulate with mucro minute and ventral in
young stage, to elliptic with mucro apical and well deve-
loped when mature (Figure 2A & B). Female sepals: 3,
1.0— 1.2 x 0.6— 0.7 mm, fleshy, broadly elliptic, acute,
mucronate, glabrous, dorsally with a few small round
raised spots (Figure 2C). Fruit: (2.6)2 .7 x 0.7(0.8) mm.
FIGURE 2. — Cliffortia amplexistipu-
la, Oliver 10046 (STE): A,
adaxial view of young leaf,
short shoot bearing young fruit
(C) removed; B, adaxial view
of older leaf, sheath opened; C,
young fruit with calyx, stigma
and bracts still attached; D,
mature fruit. Scale bars = 1
mm.
68
Bothalia 23,1 (1993)
narrowly oblong, slightly curved, 7(8)-ribbed with two ribs
flattened and extended around base forming con-
tinuous narrow wing, surface minutely scabrid to papillate
in places (Figure 2D).
Distribution and habitat : C. amplexistipula occurs on
the drier inland mountains, from the Kamiesberg in the
north to the Anysberg in the Little Karoo, in arid fynbos
on sandstones and quartzites, often on southern slopes or
in the lee of a rock.
Specimens examined in addition to the types
CAPE. — 3018 (Kamiesberg): Namaqualand, Welkom, Khamiesberg
near Garies, 1 100 m, 16-10-1954, (-AC), Esterhuysen 2J71I (BOL). 3118
(Vanrhynsdorp): Gifberg, 480 m, 14-07-1974, (—DC), Thompson 2088
(STE). 3119 (Calvinia): Calvinia Lokenburg, arid fynbos of
TMS ridges, 770 m, 28-08-1958, (— CA), Acocks 19719 (BOL); Lokenberg,
on rugged sandstone hills, 31-05-1964, (— CA), Esterhuysen 30707 (BOL).
3218 (Clanwilliam): South Cold Bokkeveld, Ceres, 4-10-1940, (— AB),
Bond 662 (NBG); Baviaansberg, Ceres, 1 450 m, 2-01-1942, (—BA),
Compton 12877 (NBG). 3219 (Wuppertal): Cederberg, Heuning Vlei,
29-12-1941, (-AA), Esterhuysen 7468 (BOL); Clanwilliam Div., Ceder-
berg, Tafelberg, shale band, 25-09-1942, (-AC),
Esterhuysen 8092 (BOL); Clanwilliam Div., foot of Tafelberg, shale band,
1 500 m, 29-12-1947, (-AC), Esterhuysen 14326 (BOL); Clanwilliam
Div., Duivelsgat, S Cederberg (Sneeuwberg area), 11-10-1946, (— CA),
Esterhuysen 13101 (BOL); Ceres Div., Zuurvlakte, E of Bokkeveld
Sneeuwkop area, 20-04-1946, (—CD), Esterhuysen 12744 (BOL, NBG,
SAM); Ceres, Stompiesfontein, Swartruggens, streambanks, 1-11-1961,
(—DC), Esterhuysen 29305 (BOL); Ceres, Stompiesfontein, Swartrug-
gens, rocky plateau, 1 100 m, 1-11-1961, (-DC), Esterhuysen 29327
(BOL). 3319 (Worcester): Gydo, Ceres, 1 000 m, 10-11-1946, (-AB),
Compton 18752 (NBG); Cold Bokkeveld, Winkelhaak area, flats NW
of Jakkalsdam, 960 m, 13-02-1992, (— AB), Oliver 10046 (STE). 3320
(Montagu): Laingsburg, Witteberg, on stony rocky south slopes, 1 300
m, 31-01-1961, (—AD), Esterhuysen 28867 (BOL, NBG); kloof on S slopes
of Anysberg, Little Karoo, 22-05-1950, (-DA), Esterhuysen 17077
(BOL); Anysberg, summit plateau, in lee of rock, 10-08-1991, (—DA),
Fellingham 1537 (STE).
REFERENCES
GIBBS RUSSELL, G.E. etal. 1987. List of species of southern African
plants, edn 2, part 2. Memoirs of the Botanical Survey of South
Africa No. 56: 64.
SCHLECHTER, R. 1900. Plantae Schlechterianae novae vel minus
cognitae describuntur. II. In A. Engler, Beitrage zur Flora von
Afrika. XVIII. Botanische Jahrbucher 27: 86—220.
WEIMARCK, H. 1934. Monograph of the genus Cliffortia. Gleerupska
Universitets Bokhandeln, Lund.
WEIMARCK, H. 1946. Further notes on the genus Cliffortia. Botaniska
Notiser 4 : 407—420.
WEIMARCK, H. 1948. The genus Cliffortia , a taxonomic survey.
Botaniska Notiser 2: 167—202.
A.C. FELLINGHAM*
* Stellenbosch Herbarium, National Botanical Institute, P.O. Box 471,
Stellenbosch 7599.
MS. received: 1992-03-16.
FABACEAE
VIGNA KOKH. A NEW SPECIES FROM SOUTHERN AFRICA
Vigna kokii B.J. Pienaar, sp. nov. (Sect. Micro-
spermae— Papilionoideae), V mudeniae B.J. Pienaar facie
caulibus pedunculis distincte costatis alatis similis;
V. richardsiae Verde. (Sect. Microspermae) stipulis reflexis
auriculis lateraliter libris caule connatis similis; a V
monophylla Taub. (Sect. Haydoniae) glandibus basalibus
verticillo interiore antherarum absentiis differt; styli
extensio ‘tumore’ in textura reducta ubi versus stigma
laterale flexa (non ut in V mudenia extensione ‘digito
primo’ et in V. monophylla tota absentia); reticulum extinae
granorum pollinis vix manifestum.
TYPE. — Transvaal, 2530 (Lydenburg): Schagen, wood-
land 0.8 km from Crocodile Hotel on road to Rosehaugh,
Pienaar 1364 (PRE, holo.; K, P, iso.).
Rootstock carrot-shaped, at length woody. Stem erect in
youth, twining at length, somewhat ridged to alate, scarce-
ly strigose to patent with light hairs. Leaflets oblong with
apex and base rounded in juvenile stage, ± 25—58 x
0.8-30.0 mm, surface smooth to touch, adnately strigose,
thickest along dorsal nerves and lamina margin, rhom-
boid to sublobular with rounded lobes at maturity, ± 80
x 60—70 mm at broadest point, apices abruptly narrowed,
obtuse, apiculate, base cuneate to obtuse, papyraceous,
strigose. Stipules with cordate base, laterally auriculate
at maturity, lanceolate, reflexed, ± 6.0 X 1.5 mm,
acuminate, margins ciliate; in youth base more or less
elongated, truncate (cf. V. mudenia B.J. Pienaar 1991).
Inflorescence contracted, peduncles alate, bearing at
apex one pair of yellowish green flowers, flushed violet,
with vertical row of extrafloral nectary glands between
them (Figure 3B). Calyx campanulate, lobes, ± 2 mm,
acute with broad bases, ± as long as tube or shorter, tube
up to 3.25 mm long, upper pair of lobes connate for '/3
to their length, strigose. Standard ovate to oblate,
emarginate, ± 10—14 mm long, spur straight with inferior
callosities divergent, auricular, superior callosities diver-
gent, narrow (vestigial). Wings narrowly ovate, ± 10.0 x
5.5 mm, auricle slender with raised cell sculpturing
(almost papillate). Keel ± 11 mm long, obtuse, slightly
upturned. Filament tube ± 10 mm long, free filaments
in two whorls, 3 or 4 mm long, anterior filament genicu-
late at base, ± 13 mm long; anthers oblate, glands at
base absent. Ovary pubescent, ± 9-10 mm long, style
broadened and flattened as it curves upward, pollen brush
on anterior face, apically twisted at maturity, accentuated
protuberance of style prolongation absent but stylar tissue
swollen as it bends toward stigmatic papillae at somewhat
more than 90°. Pollen grains scarcely reticulate, muri low,
rounded. Legumes beaked, + 68 mm long, scabrid with
long, stiff hairs along margin, 18-seeded. Seeds 3.4 mm
long, yellowish brown to dark brown, black mottled around
hilum, hilum scarcely eccentric, aril scarcely developed
or absent. Figure 4.
NAMIBIA. — 1724 (Katima Mulilo): 20 km SW of Katima Mulilo,
(— CA), De Winter 9180 (PRE). 1821 (Andara): Caprivi side of river,
near Andara Mission Station, (— AB), De Winter & Marais 4812 (PRE);
Dico, Andara, (-AB), Giess 15572 (WIND).
Bothalia 23,1 (1993)
69
FIGURE 3. Vigna kokii, Pienaar 1364 (PRE): A, style prolongation, reduced to a swelling, x 33; B, extrafloral nectaries, x 30; C, pollen
grain, X 458.
TRANSVAAL. — 2431 (Acomhoek): Nwanetzi, Kruger National Park,
(—AD), Coetzee 6062 (PRE). 2527 (Rustenburg): mountainside,
Saulspoort, (— AA), Germishuizen 514 (PRE). 2530 (Lydenburg):
Schagen, Farm of J.J. van Niekerk, Nelspruit District, (— BD), Liebenberg
3297 (PRE); 0.8 km from Crocodile Hotel on turnoff to Rosehaugh,
(-BD), Kok & Pienaar 1297 ( PRE, PRU), Pienaar 1364 (PRE).
Found in dense undergrowth of dry woodland in the
Transvaal and in Caprivi in northeastern Namibia. Figure
5.
In general facies V. kokii is very similar to V. mudenia
B.J. Pienaar (1991), with the stems and peduncles distinctly
alate and the contracted inflorescence bearing two yellow-
green flowers, but the leaflets are oblong with rounded
base and apex in youth, becoming rhombic or sublobular
at maturity. V kokii is similar to V richardsiae Verde.
(Sect. Microspermae ) in having stipules reflexed, connate
with the stem but with auricles laterally free; it differs from
V monophylla Taub. (Sect. Haydonia) in the absence of
basal glands on the interior whorl of anthers; the style
prolongation (Figure 3A) is reduced to a ‘swelling’ in the
tissue of the style where it bends toward the lateral stigma,
as opposed to the ‘finger tip’ protuberance of V mudenia
and total absence of any prolongation in V monophylla-,
the exine sculpture of the pollen grains (Figure 3C),
appears more rounded than that of V. mudenia as opposed
to the total loss thereof in V monophylla . These charac-
ters support the decision to keep it in the same section
as V mudenia but to accept it as a new species. Its
distribution also differs from that of V mudenia.
The stylar thickening (rather than a true protuberance),
at the bend toward the lateral stigma, may represent an
evolutionary stage more advanced than in other members
of the section Microspermae. This trend probably reflects
an incipient stage toward the loss of the stylar beak, as
displayed in the subgenus Haydonia (Pienaar 1992). The
reticulation of the pollen grains has almost disappeared,
a further development toward the eventual smoothness of
the exine in section Haydonia (e.g. V. monophylla Taub.).
a^lPiewAPR.
FIGURE 4. — Vigna kokii. Pienaar 1344 (PRE): A, leaf, X 1; B, stipule, X 3; C, calyx, x 3; D, standard with two pairs callosities, X 4; E,
wing, x 4; F, anther, X 7; G, style prolongation (s), stigma (st), pollen brush with pollen (p), X 10; H, legumes on peduncle, X 1;
I, legumes, X 1; J, underground tuber, vertical, x 0.25.
70
Bothalia 23,1 (1993)
FIGURE 5. — Known distribution of Vigna kokii in southern Africa.
It gives me great pleasure to name this new species after
Prof. P.D.F. Kok, under whose guidance my taxonomic
work on the genus Vigna was initiated. One of the first
collections (in 1934) of the new species is Liebenberg 3297
(PRE), from a farm in the Schagen District. Prof. Kok
accompanied me on the first field trip to the Schagen area
in search of more material of the new species. He searched
as hard as I did until an immature plant was found in the
thickets and I was able to return to the locality a season
later. He also financed the trip.
ACKNOWLEDGEMENTS
I wish to thank Prof. A.E. van Wyk for his academic
assistance, the University of Pretoria and the National
Botanical Institute for putting their amenities at my
disposal, Mrs S. Perold for the SEM micrographs and Mrs
A. Romanowski for her photographic skills, Dr D.J.B.
Killick for the Latin diagnosis and Miss A. Pienaar for
the line drawings.
REFERENCES
PIENAAR, B.J. 1991. A new species of Vigna Savi (Fabaceae) from
southern Africa. South African Journal of Botany 57: 314—318.
PIENAAR, B.J. 1992. A taxonomic revision of the genus Vigna Savi
(Fabaceae) in southern Africa. M.Sc. thesis. Department of
Botany, University of Pretoria.
B.J. PIENAAR*
* Present address: P.O. Box 44057, Linden, Johannesburg 2104.
MS. received: 1992-08-17.
ASTERACEAE
AN EVALUATION OF HUTCHINSON’S BEETLE- DAISY’ HYPOTHESIS
INTRODUCTION
Some Cape Asteraceae species have conspicuous dark
markings on their ray florets. Such markings are usually
interpreted as ‘guides’ of various sorts (e.g. Faegri & Van
der Pijl 1979). However, Hutchinson (1946) suggested that
the dark raised marks on the ray florets of Gorteria diffusa
Thunb. mimicked herbivorous beetles burrowing head
down in the inflorescences. He noted that this species
appeared to have few beetle visitors and to suffer less
herbivory than other Asteraceae (such as an Arctotis sp.)
growing nearby. He hypothesised that the marks repelled
the beetles. In his review of plant mimicry worldwide,
Wiens (1978) considered this an exceptionally intriguing
example of Batesian mimicry. Despite this there still
appears to be a dearth of information on the interaction
between beetle-daisies and beetles. The purpose of this
note is to extend the concept of beetle -daisies and to test
Hutchinson’s hypothesis.
The beetles which commonly burrow into daisy flowers
are known as monkey-beetles (Coleoptera: Scarabaeidae:
Rutelinae/Hopliinae; Scholtz & Holm 1985). The sub-
family to which they belong is largely centred in the Cape.
Little is known about their ecology against which to test
Hutchinson’s hypothesis. The situation regarding the
relative absence of monkey-beetles on Gorteria diffusa
observed 45 years ago by Hutchinson remains unchanged
today (pers. obs. in Nieuwoudtville District). I did not see
any hopliinid visitors on this species in many hours of
observation in the spring of 1990. Since the hopliinids are
a large group and they visit many other plant species
(Whitehead, Giliomee & Rebelo 1987; pers. obs.),
Hutchinson’s hypothesis may be of more general relevance.
Assuming this, I studied the interaction of Aretotheca
calendula L. (Cape weed), a weedy daisy without dark
markings on the ray florets, and the beetle Heterochelus
sexlineatus Thunb., a herbivorous species with strong
cutting mandibles. This plant species is visited by many
hopliinid species (Scott & Way 1990) and I observed
Heterochelus sexlineatus visiting at least seven other plant
species at the study site, suggesting that there is only a
diffuse relationship between the two study taxa.
In Gorteria diffusa , the so-called beetle-daisy, the
‘beetle’ mark is a dark raised bump on the ray floret with
a white spot in the middle and with yellow ‘legs’. Under
ultraviolet light this ‘beetle’ does not appear significantly
different (pers. obs.). The number of ‘beetles’ per inflores-
cence is very variable (from none to a full ring with marks
on all ray florets) within and between individuals (pers.
obs.). The ‘beetles’ on inflorescences with a full ring
appear to be the least derived condition because they are
poorly differentiated and are similar in appearance to many
other Asteraceae with a ring of conspicuous dark basal
markings on ray florets (e.g. Gazania lichtensteinii). Even
Arctotis species (e.g. A. gumbletonii Hook, f.), which
Hutchinson (1946) suggested suffer more predation, have
complex dark basal markings on the ray florets.
It is thus possible that any dark marks near the base of
the ray floret or darkening of the disc found in other genera
such as Osteospermum, Dimorphotheca and Ursinia may
be mimicking beetles. In the Still Bay area, J. Vlok and
I noted an Ursinia species (close to U. paleacea (L.)
Moench) which also appears to be a beetle-daisy. In this
Bothalia 23,1 (1993)
71
TABLE 1. Number of Heterochelus sexlineatus beetles on manipulated and unmanipulated inflorescences of Arctotheca calendula. For plots
1 and 2 extra beetles were released (see text)
species some of the ray florets have been lost and through
the gaps they have left, large dark involucral bracts appear.
This exceptional modification is equally impressive in the
field as that of Gorteria diffusa. Ursinia is placed in the
tribe Anthemideae whereas all the other genera mentioned
are in the Arctotideae, indicating strong floral convergence.
According to K. Bremer (pers. com.) these types of dark
markings are probably restricted to the Cape Asteraceae.
If all the above modifications are shown to be a response
to monkey-beetles then I estimate that about 30 Cape
species could display the ‘beetle-daisy’ syndrome (see
Midgley 1991 for photographs of most of above examples).
The following information was collected to test Hutchin-
son’s hypothesis; (i) do numbers of beetle visitors differ
between inflorescences with artificial beetle marks and
those without, (ii) do numbers of beetles on unmanipu-
lated inflorescences suggest that the presence of one beetle
deters others?
MATERIAL AND METHODS
The behaviour of the hopliinid Heterochelus sexlinea-
tus was observed on a large ( > 500 individuals) popula-
tion of Arctotheca calendula growing wild in an arboretum
at Saasveld, near George in the southern Cape.
Sampling took place on warm days between 15h00 and
16h00 during October 1990. Inflorescences were manipu-
lated by marking the ray florets with brown, yellow and
black dots using commercial Artline pens. The yellow
marks were not visible (to human eyes) on the yellow ray
florets and thus served as controls to determine any other
non-visual effects of the marks on beetles. Numbers of dots
ranged from two to five and were approximately the same
size as the beetle. To simulate the Ursinia type model
(described above), from three to five ray florets were
removed from a sample of inflorescences. Inflorescences
were checked the following day for numbers of beetles.
In some cases inflorescences became unsuitable subse-
quent to marking and this accounts for unequal numbers
on Table 1. Because the numbers of beetles per inflores-
cence are low (less than 5% — see Results and conclusions)
in some instances beetles were captured from other areas
and released in the vicinity of study plots.
RESULTS AND CONCLUSIONS
Surveys indicated that 10 out of 200, six out of 100 and
nine out of 300 Arctotheca inflorescences had beetle visi-
tors (mean of less than 5% of inflorescences had visitors).
Ursinia anthemoides (L.) Poir. in the vicinity had less than
2% of inflorescences with visitors. The manipulation
experiments indicate that this beetle is virtually indifferent
to markings on the ray florets and to the absence of ray
florets (Table 1). The fact that considerable aggregation
of beetles occurs on inflorescences (e.g. up to eight
individuals in Table 2) suggests that the presence of an
individual is not inimical to others. Approximately twice
as many male beetles as females were found (Table 2).
Relative to the number of inflorescences, the beetles, and
especially the females, are rare. Consequently males
probably visit many inflorescences searching for mates.
The males fight for access to females (Midgley 1992). This
suggests that this beetle would be an effective pollinator
(its hairy body is often covered with pollen) but a rela-
tively insignificant herbivore (a few florets in a few
inflorescences in a population are damaged). The results
concerning manipulated inflorescences suggest that floral
markings have no negative effect on visitation. It is possible
that beetles are actually attracted to the marked florets.
However, on discovering that there are no real beetles on
the florets, they fly off. It was not, however, possible to
observe each visitor as it arrived on all manipulated in-
florescences simultaneously to see whether this was the
case. Although the hopliinid considered in this study is
a herbivore with strong cutting mandibles, many other
hopliininds are merely pollen feeders (Peringuey 1902).
It would make little sense for mimicry to evolve to repel
the non-herbivorous, pollen-carrying hopliinid beetles.
Also there would be little reason for an evolutionary trend
towards reduction in the number of beetle marks, if their
function is repulsion.
TABLE 2. — Distribution by gender of Heterochelus sexlineatus beetles
(M = male, F = female) in three samples of inflorescences of
which each had at least one beetle visitor
72
Bothalia 23,1 (1993)
The above (no repulsion, aggregation and feeding habits)
suggest that Hutchinson’s hypothesis is not complete. If
the markings act as mimics then it is probably to attract
beetles, presumably for their role in pollination. This
would then be a case of reproductive mimicry (sensu
Wiens 1978), similar in a way to pseudocopula tory orchids.
Obviously this study of one beetle and daisy species needs
to be broadened before Hutchinson’s intriguing hypothe-
sis of this little-studied syndrome of Cape plants is fully
tested.
ACKNOWLEDGEMENTS
I thank J. Vlok for field assistance, R. Oberprieler for
identifying the beetle and K. Bremer for his views on
Asteraceae markings.
REFERENCES
FAEGRI, K. & VAN DER PUL, R. 1979. Principles of pollination
biology. Pergamon Press, Oxford.
HUTCHINSON, J. 1946. A botanist in South Africa. Crawthom, London.
MIDGLEY, J.J. 1991. Beetle-daisies and daisy beetles. African Wildlife
45: 318, 319.
MIDGLEY, J.J. 1992. Why do some hopliinids have large hind legs?
Journal of the Entomological Society of Southern Africa 55:
157-163.
PERINGUEY, L. 1900-1902. Descriptive catalogue of the Coleoptera
of South Africa (Lucanidae and Scarabaeidae). Transactions of
the South African Philosophical Society 12: 1—220.
SCHOLTZ, C.H. & HOLM. 'E. 1985. Insects of southern Africa.
Butterworths, Durban.
SCOTT, J.K. & WAY, M .J. 1990. A survey in South Africa for potential
biological control agents against capeweed, Arctotheca calendu-
la (L.) Levyns (Asteraceae). Plant Protection Quarterly 5: 31-34.
WHITEHEAD, V.B., GILIOMEE, J.H. & REBELO, A.G. 1987. Insect
pollination in the Cape flora. In A. Rebelo, A preliminary
synthesis of pollination biology in the Cape flora. S.A.N.S.P. 141.
WIENS, D. 1978. Mimicry in plants. Evolutionary Biology 11: 365—403.
J.J. MIDGLEY*
* CSIR, Division of Forest Science and Technology, Private Bag X5011,
Stellenbosch 7599.
MS. received: 1991-08-16.
OXALIDACEAE
A NEW SPECIES OF OXALIS FROM THE WESTERN CAPE
Oxalis oculifera E.G.H. Oliver, sp. nov. in Sectione
Latifoliolatis , in genere singularis propter tubum corollae
rubrum papillatum partem alteram violaceo-roseum
annulo mediano alba, foliola subpeltata subparallela
glauca.
Planta parva, 5—15 mm alta. Bulbus ovoideus, 8x6
mm, ferragineus, vaginis papyraceis tectus, vaginis in parte
inferiore diagonaliter secedentibus. Folia 1—9; petiolus
2—20 mm longus, sparse glandulopilosus, roseus; foliola
3, interdum 2 vel 1, subparallela, 3.0— 4.5 x 3.0 mm, semi-
conduplicata, oblique subpeltata, basaliter subinfundi-
buliformia, late elliptica ad obovata, interdum oblongo-
elliptica, apice late obtusa vel plus minusve emarginata
base obtusa, glauca, adaxiale dense papillata, abaxiale
glabra sed interdum locis parvis croce is callosis, margine
hyalino et intra zona crocea gracili callosa; petioluli
0.3— 0.6 mm longi. Pedunculi uniflori, 20—37 mm longi,
erecti demum prostrati, sparse glandulopilosi, rosei;
bracteae absentes interdum 1 vel 2 in parte superiore,
filiformes vel lineares, ad 0.6 mm longae, sparse glandu-
lopilosae. Sepala 1.7— 1.9 x 0.7-0.9 mm, appressa, ovata
ad late ovata, interioria angustissima, subacuta, rasilia et
sparse glandulopilosa, zona marginali atropurpurea et zona
proxime interiore aurantiaca callosa, parte cetera viridi
erabescenti. Corolla ± 9—10 mm longa, late salviformis,
violaceorosea fauce cum annulo albo et tubo vinaceorabro;
petala 5—6 mm lata, oblique obovata ad late subspa thulata,
base param conjuncta, abaxiale sparsissime glandulopi-
losa, ecallosa, adaxiale in zona rubra papillata. Stamina
in seriebus tribus, base longitudine 0.5 -0.8 mm con-
juncta; antherae albae marginibus atropurpureis; fila-
menta purpurea sparse glandulopilosa; pollen tricol-
poratum, ellipsoideum, in antheris superioribus medi-
anisque album, in antheris inferioribus luteum. Ovarium
0.7— 1.0 mm longum, ovoideum, uniovulatum, in parte
superiore sparse glandulopilosum; styli in seriebus tribus.
mediani superioresque erecti ad param patentes, inferiores
valde porrecti, sparse glandulopilosi purpurei; stigmata
fimbriata, superiora medianaque purpurea, inferiora alba.
Figura 6.
TYPE. — 3118 (Vanrhynsdorp): Cape Province, Vanrhyns-
dorp Dist., Gifberg/Matsikamma area, central plateau
W of van Taakskom near top of the pass, 595 m,
(-DD), 12-06-1990, Oliver 9558 (STE, holotype; BOL,
K, PRE isotypes).
Dwarf stemless plants 5—15 mm high, aggregated into
clumps. Bulb ovoid, 8x6 mm, light reddish brown,
covered with papery sheaths splitting diagonally in lower
part. Rhizome vertical up to 20 mm long. Stem none or
very short up to 4mm long. Leaves 1—9 per plant; petiole
2—20 mm long, sparsely glandular pilose, pinkish; leaflets
mostly 3, occasionally 2 or 1, subparallel, 3.0— 4.5 x 3.0
mm, semiconduplicate, obliquely subpeltate, basally
subinfundibuliform, broadly elliptic to obovate, occasion-
ally oblong-elliptic, apically broadly rounded or slightly
emarginate basally rounded, glaucous, adaxially densely
papillate, abaxially glabrous, with hyaline margin and
inside this a thin orange callose zone, sometimes with
scattered small orange callose patches abaxially; petiolule
0.3— 0.6 mm long. Peduncle 1-flowered, 20—37 mm long,
erect becoming prostrate, markedly glandular pilose when
young and short, becoming sparsely so when mature,
pinkish; bracts usually absent, sometimes 1 or 2 on upper
part of peduncle, filiform or linear up to 0.6 mm long,
sparsely glandular pilose. Sepals 1.7— 1.9 x 0.7— 0.9 mm,
adpressed to corolla and joined at base, lobes ovate to
broadly ovate with inner ones narrowest, subacute,
glabrous and sparsely glandular pilose, with very dark
purple marginal zone and orange callose zone just inside
that, the rest green becoming reddish. Corolla about 9-10
mm long, broadly salver- shaped, violet-pink with white
FIGURE 6. — Oxalis oculifera : A, plant, X 2; B, leaf, adaxial view, on left, & abaxial view, on right, x 12; C, calyx, X 25; D, petal, abaxial
view, x 25; E, the three trimorphic series of the androecium and gynoecium, X 25; F, gynoecium, x 25. All drawn from the type, Oliver
9558 (STE).
I ring in throat and wine-red tube; petals 5-6 mm wide,
obliquely obovate to broadly subspathulate, joined slightly
at base, very sparsely glandular pilose abaxially on outer
margin, ecallose, papillate adaxially on red zone. Stamens
in 3 series, 2 series per plant, the shortest 1.2 mm long,
the middle 2.0— 2.3 mm long, the longest 3.0— 3.5 mm
long, all joined for 0.5— 0.8 mm at base, the uppermost
manifest, the rest included; anthers white with dark purple
edges; filaments purplish, sparsely glandular pilose; pollen
tricolporate, ellipsoid, in upper and middle anthers white,
in bottom anthers yellow. Ovary 0.7— 1.0 mm long, ovoid,
sparsely glandular pilose in upper half, 1-ovuled; styles
in 3 series, the lowest 0.5 mm long, markedly spreading
and white, the middle 1.2 mm long and the uppermost
series 3 mm long, the latter two series erect to slightly
spreading purplish sparsely glandular pilose; stigmas
fimbriate, the uppermost and middle series purple, the
lower series white. Figure 6.
This new species of Oxalis is remarkable in the genus
on account of the colour of its corolla and the distinctive
shape of its leaves. The corolla tube is wine-red with a
white ring in the throat, the rest of the corolla being violet-
pink. The glaucous leaflets are unusual for being obliquely
peltate with the petiolule attached abaxially to the lamina.
The leaflets are subparallel next to each other and not
spreading. They are semiconduplicate in a broad V-shape
with the basal portion above the petiole often partially
funnel-shaped.
O. oculifera falls within the Section Latifoliolatae which
Salter (1944) described as an unnatural assemblage of
species. It is defined as having those species forming
acaulescent plants with broad, but never linear or oblong,
leaves. Within the section this species is probably most
closely allied to O. petiolulata Bol. f.
O. petiolulata appears to be confined to the central and
northern parts of the Cedarberg near Clanwilliam where
it is known from only three collections, all in BOL ( H .
Bolus 8952, the type; Adamson in BOL 20492 and Po-
cock s.n.). All three have very differently sized leaves with
Adamson in BOL 20492 having the smallest leaves most
similar to those in the new species. The Pocock specimen
has no flowers and was determined with a query by Salter.
In O. petiolulata the plants are very sparsely and
minutely glandular pilose, not glabrous as recorded by
Salter. The sepals are sparsely ciliate with short rather
thick hairs. The leaflets have about six distinct black
callose ‘lumps’ towards the edges and nothing sub-
marginally, whereas in the new species the callose dots
are small, orange in colour and are randomly scattered
and there is a distinct, very thin, submarginal orange
callose line. In O. petiolulata the callose region on the
sepals is black and confined to two large patches near the
apex, whereas in the new species the callose region is
orange and submarginal down the sepal just below the thin
marginal black zone.
The bulbs in O. oculifera are quite different from those
in O. petiolulata. In the former the bulb is small and ovoid,
the tunics splitting with diagonal slits like an inverted V,
whereas in the latter they are narrowly ovoid and attenuate
with longitudinally splitting tunics.
The leaflets in the new species are very distinctive. They
are subparallel, adpressed and partially conduplicate. The
glaucous-grey colour of the leaves is very striking in the
living material. This is produced by numerous translucent,
shortly papillate cells on the upper surface. The remark-
able feature is the position of the point of attachment of
the leaflet to the petiolule. In O. petiolulata the petiolule
74
Bothalia 23,1 (1993)
is attached at the base of the lamina. In O. oculifera the
petiole is attached about one quarter of the way along the
undersurface of the lamina which is thus semipeltate. In
some leaflets the two sides of the basal portion of the
lamina are a little more adnate producing a slightly funnel-
shaped base to the leaflet.
Salter (1944) noted that he had not seen any living
material of O. petiolulata but described the flowers as ‘deep
pink with a purple eye in the throat, tube dull yellow’. F.
Bolus (1918) described the corolla from his father’s
collection as ‘purpurea’ and Adamson gave ‘deep pink with
a dark throat’ on his label. This would indicate that the
corolla was tricoloured with a purple ring at the mouth
of the tube which is yellow, quite unlike the very distinc-
tive wine-red tube forming the eye in O. oculifera. Salter
(1935) when describing his O. oculata (= O. callosa R.
Knuth) gave the colours as ‘roseo-rubra..tubo luteo, in
faucibus purpureo-annulata’ and noted that the dark purple
‘eye’ in the corolla mouth is a character which he found
in some forms of other species, but in O. callosa it
appeared to be always present. His drawing which was
repeated under O. callosa (Salter 1944), shows the dark
‘eye’ as a ring in the mouth of the corolla.
This feature of the red tube was mentioned to Salter
when I made the first collection in 1965. I told him I had
noted that all the flowers in the population possessed the
striking red eye. He remarked that this was unknown to
him in the genus and that the material constituted a distinct
new species.
O. oculifera is confined to one major population and
several nearby smaller populations in a small area on the
summit of the mountain plateau between the Gifberg and
Matsikamma Mountains (Figure 7). I have not been able
to locate any other populations, which could very well
be found on this extensive range with more intensive
searching. The plants occur in shallow gritty sand on
quartzitic sheet rock of the Table Mountain Group. The
main population grows where water seeps over the rock,
in some places as a small streamlet, the plants standing
in the shallow water. The plants are dominant, forming
pure stands of many individuals or clumps which are a
remarkable sight when in full bloom in May and early
June, a month after the first autumn rains.
This contrasts with the spring flowering period,
September/October, for O. petiolulata for the Bolus and
Pocock collections. Surprisingly the Adamson collection
was collected in flower in May 1933. Pocock recorded her
collection as ‘growing in marshy places and slowly flowing
streams’.
Salter (1944) noted that all the native South African
species are trimorphic. He mentioned that overseas
workers had recorded that the pollen in Oxalis was of
different sizes. Salter himself had noted that the colour
of the pollen varied but that he had not recorded the details
for the South African species. O. oculifera is trimorphic
within the populations studied and possesses two distinct
pollen types (Figure 6E). White larger grains are produced
by the middle and uppermost anthers and yellow smaller
grains by the lowest set of anthers. This feature raises the
intriguing problem of pollen selection in the pollination
FIGURE 7. — The known distribution of Oxalis oculifera.
syndrome of the species. In the wild no insect visitors other
than the occasional thrips crawling around in the flower,
were observed.
The material studied for this species included living
material of Oliver 9558 flowering in cultivation at Stellen-
bosch during May 1992.
Specimens examined
O. oculifera
CAPE.— 3118 (Vanrhynsdorp): Vanrhynsdorp Dist., Gifberg/Matsikam-
ma area, central plateau W of Van Taakskom near summit of the pass,
595 m, (-DD), 10-06-1965, Oliver in STE 32028 (PRE, STE, MO);
ibid., 12-06-1990, Oliver 9555 (BOL, K, PRE, STE).
O. petiolulata
CAPE. — 3219 (Wuppertal); Clanwilliam, Cedarberg, Krakadouw,
1 000 m, (— AA), 3-05-1933, Adamson in BOL 20492 (BOL); near
Wuppertal and Krakadouw, 1 000 m, (— AA/AC), 8-10-1897, H. Bolus
8952 (BOL, holo.); Cedarberg, between Middelberg hut and Crystal Pool,
1 220-1 525 m, (-AC), 09-1930, Pocock s.n. (BOL).
REFERENCES
BOLUS, F. 1918. Novitates africanae. Annals of the Bolus Herbarium
1: 19-28.
SALTER, T.M. 1935. Plantae novae africanae. Journal of South African
Botany 1: 129—144.
SALTER, T.M. 1944. The genus Oxalis in South Africa. Journal of South
African Botany , Suppl. Vol. 1: 1—355.
E.G.H. OLIVER*
* Stellenbosch Herbarium, P.O Box 471, Stellenbosch 7599.
MS. received: 1992-06-09.
Bothalia 23,1 (1993)
75
PTERIDOPHYTA— ADIANTACEAE
A NEW CYTOTYPE FOR ACROSTICHUM AUREUM
Acrostichum is a genus with a pantropical distribution
and consists of three, or perhaps more, species. A. aureum
L. is the most widespread of these and also has a
pantropical distribution.
On the west coast of Africa A. aureum occurs from
Guinea-Bissau to northern Angola and on the east coast
from Zanzibar to the Transkei. A. aureum is largely an
estuarine species which is commonly associated with the
upper edge of mangrove communities. It generally grows
in brackish or saline flats of alluvial mud or muddy sands.
Although it is predominantly an estuarine species it occurs
sporadically at considerable distances from the coast. In
Zimbabwe it was found at an elevation of approximately
500 m at a hot spring with salt efflorescences (Jacobsen
1983). Plants have also been recorded 100 km from the
coast in Saudi Arabia, 823 m above sea level, where it grows
in a slightly saline alkaline seepage (Collenette 1991).
Cytological observations in A. aureum have been carried
out on plants from Sri Lanka (Manton & Sledge 1954),
Ghana ( Manton 1959), southern India (Abraham et al.
1962) and Jamaica (Walker 1966). In all events the chromo-
some number reported was 2n = 60.
A collection of A. aureum made by me, Roux 1945
(NBG), in a seasonally marshy area on the banks of the
St Lucia Estuary, on the northern Natal coast, have now
been studied cytologically. Acetocarmine preparations of
root tips taken from this cultivated plant revealed a
chromosome number of 2n = 120 (Figure 8). This plant
may therefore be considered a tetraploid. The suggestion
made by Tryon & Tryon (1982) that polyploidy, which is
a common phenomenon in tropical pteridophytes, never
developed in the genus, can therefore no longer be up-
held. Most chromosomes are of the acrocentric and
telocentric type with few being submetacentric.
* *
v
„ s*.
^ %
A
&
JR* K
\
1
/H
tl
V
FIGURE 8. — Root tip mitosis of
Acrostichum aureum showing
120 chromosomes, Roux 1945
(NBG).
REFERENCES
ABRAHAM, A., NINAN, C.A. & MATHEW, P.M. 1962. Studies on
the cytology and phylogeny of the pteridophytes. VII. Observa-
tions on one hundred species of south Indian ferns. Journal of
the Indian Botanical Society 41: 339—421.
COLLENETTE, I.S. 1991. Acrostichum aureum: an inland record from
Saudi Arabia. Fern Gazette 14: 57.
JACOBSEN, W.B.G. 1983. The ferns and fern allies of southern Africa.
Butterworths, Durban, Pretoria.
MANTON, I. 1959. Cytological information on the ferns of west tropical
Africa. In A.H.G. Alston, The ferns and fern allies of west tropical
Africa: 75—81.
MANTON, I. & SLEDGE, W.A. 1954. Observations on the cytology
and taxonomy of the pteridophyte flora of Ceylon. Philosophi-
cal Transactions of the Royal Society of London, B, 238: 127—185.
TRYON, R.M. & TRYON, A.F. 1982. Ferns and allied plants with
special reference to tropical America. Springer-Verlag, New York,
Heidelberg, Berlin.
WALKER, T.G. 1966. A cytological survey of the pteridophytes of
Jamaica. Transactions of the Royal Society, Edinburgh 66:
169-237.
J.P ROUX*
* Compton Herbarium, National Botanical Institute, Private Bag X7,
Claremont 7735.
MS. received: 1992-05-12.
76
Bothalia 23,1 (1993)
FIGURE 9.—Argyrolobium rotundi folium, Edwards & Ackermann 329 (NU). A, habit; B, leaf; C, fruit; D, standard, frontal view; E, keel; F,
wing; G, calyx; H, androecium. Scale bars: A = 10 mm; B = 5 mm; C = 4 mm; D-F, H = 2 mm; G = 4 mm.
Bothalia 23,1 (1993)
77
FABACEAE
NOTES ON THE GENUS ARGYROLOBIUM (CROTA LAR1EAE) INCLUDING A NEW SPECIES FROM SOUTHERN AFRICA
Argyrolobium rupestre (E. Mey.) Walp. comprises
‘small slender-stemmed few-flowered prostrate or shortly
ascending plants from mountainous areas the length of
eastern Africa’ (Polhill 1968). Tropical representatives of
A. rupestre have been ‘loosely subdivided’ into four
subspecies by Polhill (l.c. ). The complex is notoriously
difficult to classify due to the poor resolution of characters
and Polhill (l.c.) concedes that ‘some of the forms may
possibly have evolved separately from more robust local
species but whatever their origin only slight differences
in habit and indumentum distinguish them’. Whereas his
revision covered high altitude specimens from South
Africa, no mention was made of the lowland element
discussed here and routinely included within A. rupestre.
Argyrolobium rotundifolium T. J. Edwards, sp.
nov., A. rupestri affinis sed habitu prostrato; foliolis sub-
orbiculatis cum pilis rufo-tomentosis; corolla alis sine
sculptura differt.
TYPE. — Natal, 2930 (Pietermaritzburg): between Peace-
vale & Drummond, (— DD), Edwards & Ackermann 329
(NU, holo. ; K, E, PRE, iso.).
Herbaceous perennial, up to 150 mm tall, but usually
prostrate, well branched, stems shortly rufous-tomentose,
becoming glabrous. Leaves moderately tomentose above,
densely tomentose beneath; leaflets broadly ovate to sub-
orbicular 14-32 x 10—25 mm, petiole tomentose, 10-30
mm long; apex obtuse to rounded, apiculate; margins
densely rufous-tomentose; stipules free, setaceous to
lanceolate, up to 10 x 1.5 mm. Inflorescence pseudo-
umbellate, 1— 4(— 6)-flowered, initially terminal but
becoming leaf-opposed; peduncle (30-)40— 150 mm long;
bracts linear or narrowly elliptic, up to 6 x 1 mm,
bracteoles linear, up to 3 mm long. Flowers dimorphic.
Calyx sparsely to densely pilose; upper lobes 8—10 mm
long, lower lip 8—10 mm long, lobes 3—4 mm long.
Corolla bright yellow becoming russet; standard sub-
orbicular, 11-14 x 12—14 mm, adaxial surface sericeous,
base cordate, claw 1.0— 1.5 mm long; wings obovate, 9—12
x 4.5 -6.0 mm, distally pilose, without sculpturing, claw
1.5— 2.0 mm long; keel cymbidiform, 8—10 x 4.5— 5.5
mm, pilose on lower margin, claw 1.5— 2.5 mm. Stamens
monadelphous, sheath fused above. Pistil narrowly oblong;
ovary 6-8 x 1-2 mm; style 3-4 mm long. Fruit rufous-
pilose, compressed, up to 45 x 5 mm. Seed subglobose,
laterally compressed, 2.5— 3.0 mm in diameter, yellow to
light brown, hilar rim raised.
Floral dimensions in the description refer to chasmoga-
mous flowers. Cleistogamous flowers are of no use in
species delimitation.
A. rotundifolium (Figure 9) is allied to A. rupestre but
is distinguished by its consistently prostrate habit (A.
rupestre is better described as ascending or decumbent),
broadly elliptical to orbicular leaflets, shortly rufous-
tomentose indumentum and the lack of sculpturing on
its wing petals. This species is predominantly coastal in
distribution whereas A. rupestre is limited to inland areas
(Figure 10). In southern Natal A. rupestre approaches the
coast on the high lying areas around Kokstad and Harding,
however, no contact zones with A. rotundifolium have been
observed.
NATAL. — 2731 (Louwsburg): Itala Nature Reserve, (— CA), Germis-
huizen 2232 (PRE). 2831 (Nkandla): Ngoye, (-DC), Huntley 852 (NU).
2832 (Mtubatuba): Hluhluwe Game Reserve, Mbhombe, (— AA),
Hitchins 598 (NH, NU). 2931 (Stanger): Nonoti Lagoon, (-AD), Ward
9121 (PRE). 3030 (Port Shepstone): Oribi Gorge, Riverview, (— CA),
Van Wyk 5064 (PRE). 3130 (Port Edward): 7 km from Port Edward on
the Izingolweni Rd, (-AA), Hilliard 1738 (NU).
CAPE. — 3228 (Butterworth): The Haven, (—BA), Gordon-Gray 557
(GRA). 3229 (Talemofu): Hole in the wall, (— AA), Germishuizen 1860
(PRE).
Argyrolobium lotoides Harv. in Flora capensis 2:
595 (1862). Type: Transkei, H. Bowker 366 ( TCD, holo.!;
K!, PRE! iso.). Figure 11.
A. variopile N.E. Br. : 18 (1906); B-E. van Wyk: 395 (1987) synon.
nov. Syntypes: Natal, Volksrust, hillside near Charlestown, Wood 5693
(BOL!, K!, NH!, PRE!), Wood 6355 (K!, NH!, SAM!).
A. hirsuticaule Harms: 179 (1917) synon. nov. Type: Transkei. Zuur-
bergen, Schlechter 6571 (Bf, holo.; BOL, lecto.! selected here).
A. leptocladum Harms: 180 (1917) synon. nov. Type: Kokstad, around
Clydesdale, Tyson 1256 pro parte (Bf, holo.; BM! , icono. selected here).
A. thodei Harms: 184 (1917) synon. nov. Type: Witzieshoek, Thode
20 (Bf, holo.; BM!, icono. selected here).
Lotononis magnistipulata Diimmer: 299 (1913). Type: Faku’s Territory
(probably Transkei), Sutherland s.n. (K, holo.).
Early collections of this species, made by Drege, bear
the name Chasmosyne pilosissima but no published
description was traced. The three names published by
Harms were based on differences in vestiture and leaf
dimensions. These highly variable characters form a
continuum and are thus unsuitable for delimiting species.
The specimens from which A. leptocladum and A. hir-
suticaule were described were destroyed in Berlin. The
drawings of these specimens at BM are therefore selected
FIGURE 10. —The known distribution of Argyrolobium rotundifolium,
#; and A. rupestre, A. in southern Africa.
78
Bothalia 23,1 (1993)
FIGURE 11. — A rgyrolobium lotoides, Browning 183 (NU). A, habit; B, dissected calyx, inner surface; C, standard, adaxial surface; D,
wing; E, keel; F, androecium. Scale bars: A = 10 mm; B— F = I mm.
Bothalia 23,1 (1993)
79
as iconotypes. The type of A. leptocladum is part of
a mixed collection {Tyson 1256)\ unfortunately only
specimens of A. amplexicaule remain from this gathering
(these are listed below under additional specimens
examined).
The species (Figure 12) occurs commonly in highland
sourveld and is frequently associated with rocky outcrops.
TRANSVAAL. — 2630 (Carolina): Chrissiemeer, (—AC), Theron 2383
(PRE). 2729 (Volksrust): hillside near Charlestown, (— BD), Wood 5693
(BOL, K, NH, PRE), Wood 6355 (K, NH, SAM).
ORANGE FREE STATE.— 2828 (Bethlehem): Generaalskop, (-DA),
Roberts 3298 (PRE).
NATAL. — 2730 (Vryheid): Naauwhoek, (—AD), Devenish 2124 (E,
K, NU, PRE, S). 2929 (Underberg): Sani Pass, (-CB), Hilliard & Bum
15534 (E, NU, PRE); Browning 183 (NU). 3029 (Kokstad): Zuurberg
near Weza, (— BC), Hilliard & Bum 8070 (E, MO, NU, PRE).
LESOTHO. — 2927 (Maseru): Molmo Ntuse mountain road, (— BD),
Schmitz 7248 (PRE). 2928 (Marakabei): Semonkong, (— CC), Jacot
Guillarmod 1812 (PRE). 3027 (Lady Grey): Ben McDhui, (— DB), Gal-
pin 6607 (PRE).
CAPE.— 3028 (Matatiele): Quachasnek, hillside facing Maluti Hotel,
(—BA), Gordon-Gray 4042 (E, NU).
Additional specimens examined
Argyrolobium amplexicaule
NATAL. — 3029 (Kokstad): in hills around Clydesdale, (— BD), Tyson
1256 (BM, BOL, K, SAM, UPS).
ACKNOWLEDGEMENTS
My gratitude is extended to the Natal University
Research Fund for financial assistance. The cited herbaria
are thanked for the loan of specimens and Mr M. Lambert
is thanked for translating the Latin diagnosis.
REFERENCES
BROWN, N.E. 1906. II. Diagnoses Africanae, XIV. Kew Bulletin 1906:
15-30.
DUMMER, R. A. 1913. A synopsis of species of Lotononis Eckl. &
Zeyh., and Pleiospora Harv. Transactions of the Royal Society
of South Africa 3 : 275 —335.
HARMS, H. 1917. Weitere Beobachtungen iiber Kleistogamie bei
affikanischen Arten der Gattung Argyrolobium. Berichte der Deut-
schen Botanischen Gesellschaft 35: 175—186.
HARVEY, W.H. 1862. Leguminosae. Flora capensis , Vol. 2. Hodges
Smith, Dublin.
POLHILL, R.M. 1968. Argyrolobium Eckl. & Zeyh. (Leguminosae) in
tropical Africa. Kew Bulletin 22: 145—168.
VAN WYK, B-E. 1987. Taxonomic notes on Argyrolobium variopile
(Fabaceae), and the status of Lotononis magnistipulata. South
African Journal of Botany 53 : 395 - 397.
T.J. EDWARDS*
* UN/FRD Unit for Plant Growth and Development, Botany Department,
University of Natal, P.O. Box 375, Pietermaritzburg 3200.
MS. received: 1992-03-12.
ALLISONIACEAE
THE HEPATIC, CALYC U LARI A CRISPULA (M ETZGERIALES ) REPORTED FROM MALAWI AND ZAMBIA
Calycularia crispula Mitt. , in Journal of the Proceed-
ings of the Linnean Society of Botany 5: 122 (1861); Pande
& Udar: 331 (1956); Jones: 497 (1985). Type: Himalayas,
Sikkim, J.D. Hooker 1679 (G, iso.).
Calycularia golae Gerola: 471-485 (1947). Type: Abyssinia, Vondo,
Valova s.n.
Thallus procumbent, dark bottle-green, to olive-green,
nearly translucent, delicate and easily torn when wet;
almost colourless in dead basal parts, with brownish
margins when dry; in overlying mats, on tree bark or on
soil covering tree boles; firmly adherent to substrate along
midrib throughout its length; 7.5—23.0 mm long, simple
or with a single terminal bifurcation (Figures 13A; 14A),
branches 5.0— 7.5 x 7.5— 9.0 mm, occasionally short lateral
branches arising ventrally near base, basal part semi-
lobate; wings thin and wide, margins slightly scalloped
and strongly undulate, otherwise entire; apex notched
(Figure 13E) with the 2 terminal lobes overlapping
somewhat; ventral scales situated between lobes and visi-
ble from above, arched over edge, small and inconspicu-
ous, mostly confined to apices of ventral face, colourless,
up to 500 pm long, 3 or 4 cell rows wide at base, central
cell row longer and tapering to uniseriate tip, lateral rows
shorter, all ending in and laterally with one to several slime
papillae, ± 50 pm, with spherical top (Figure DC); rhi-
zoids very long and dense, smooth, faintly brown, ± 20
pm in diameter, restricted to midrib ventrally; midrib
± J/5 of branch width, ± 280 pm (or more) thick and
generally consisting of 12— 15 rows of thin-walled homoge-
neous cells (Figure 13D), in cross section 4—6-sided, ±
42.5 x 27.5—32.5 jam, in longitudinal section ± rectangu-
lar, up to 137 pi n long, without a central strand of con-
ducting cells, gradually becoming thinner laterally and
wings eventually unistratose (Figure DD); epidermal cells
of midrib slightly thicker-walled, rectangular to pentago-
nal, generally 55 x 25 pm, in cross section 32.5 x 25.0—
32.5 ^m, containing numerous chloroplasts, ± 5.0 pm
80
Bothalia 23,1 (1993)
FIGURE 13. — Calycularia crispula. A, male thallus with androecia; B, scale-like involucre which individually covers antheridium; C, ventral
scale with slime papillae; D, part of transverse section of thallus, showing one unistratose wing and costa without central conducting strand;
E, ventral face of apex of thallus, showing apical notch and slime papillae; F, chloroplasts and small oil bodies inside thallus cells, seen
from above; G, cells along margin of thallus seen from above. A— C, F— G, S.M. Perold 2677 ; D, S.M. Perold 2668. A, X 9.5; B, X
90; C, x 125; D, E, x 45; F, x 400; G, x 150.
%,w
Bothalia 23,1 (1993)
81
FIGURE 14, — Calycularia crispula. A, female thallus with young sporophyte enclosed in perianth; B, close-up of sporophyte; C, longitudinal
section through capsule; D, involucral scales; E, cluster of archegonia protected by involucral scales, near apex of thallus; F, calyptra showing
unfertilized archegonium at base; G, perianth with laciniate mouth; H. transverse section of capsule wall, rod-like thickenings indicated
by arrows; I, cells in fragment of capsule wall, thickenings from above seen as dots. A— I, S.M. Perold 2668. A, x 6.5; B, C, X 12;
D, x 90; E, x 20; F, G, x 18; H, I, x 300.
82
Bothalia 23,1 (1993)
in diameter, as well as small oil bodies (Figure 13F);
cells in wings, from above, pentagonal or hexagonal,
45-50 x 30—50 /xm; cells at margin rectangular,
32.5—57.5 x 17.5—22.5 /am or pentagonal, 25 x 30 /xm
(Figure 13G).
Dioicous. Androecia consisting of 3 or 4(5) crowded,
± parallel rows of male scales overlying the midrib in the
body of the thallus, reduced to 2 rows in the terminal
branches (Figure 13A), antheridia short-stalked, globular,
± 250 x 240 /xm when mature, each one covered by a
forwardly directed laciniate scale (Figure 13B, C), laciniae
up to 550 /xm long x 250 (im wide at base, composed
of cells 45 —75 x 45 /x m. Gynoecia acropetally arranged
and singly placed dorsally, near the notched apex and when
present, above the furcation of the branches (Figure 14A,
B), slightly raised on a swelling, each with a group of
± 6—11 young archegonia (Figure 14E), ± 325 /xm long,
the necks composed of 6 cell rows and the tips brownish;
just posterior to the archegonia and at their sides subtended
by an involucre of narrow, laciniate scales (Figure 14D),
erect to somewhat forwardly directed; when mature, the
capsule spherical to ovate, leaning obliquely forward, 1750
x 1500 /x m, containing a mass of spores and elaters and
raised on the seta, here only + 1000 ix m long (Figure 14C)
and not maximally elongated; capsule wall brown,
bistratose (Figure 14H), cells square or rectangular, 37.5
X 37.5 to 75 X 20 /x m, cell walls thin, but with some
conspicuous orange-coloured semi-annular bands or
stiffening rods, the latter projecting into the cell lumen
(Figure 141); perianth obconic and large when mature,
enclosing capsule, green, with laciniate mouth (Figure
14G), 3100 ix m long including + 600 /xm long laciniae,
cells ± 75.0 x 37.5 /xm; calyptra delicate and transparent
(Figure 14F), bistratose, cells mostly pentagonal, ± 50.5
x 37.5 n m, with unfertilized archegonia attached to base.
Spores with distal face rounded (Figure 15C, D), proximal
face flat or indented (Figure 15A), light brown, trans-
lucent, diameter 35.0—42.5 /xm, densely echinate, spines
occasionally rather blunt, straight or bent (Figure 15B),
7.5 ix m long and 5.0 /xm wide at base, in between them
small projections arising at corners of shallow areolae.
Elaters bispiral (Figures 15F; 16), 10.0 /xm thick, ± 310
/xm long, tips solid, rounded. Vegetative reproduction by
stipe arising from group of cells in colourless, seemingly
dead marginal or basal parts of thallus, almost lunate, 175
x 375 ix m, soon narrowly winged; also by ventral branches
arising from midrib.
Grows on tree trunks and apparently also on soil, in
sheltered, damp places in montane forest.
DISCUSSION
Calycularia crispula (family Allison iaceae, order Metz-
geriales) is well known in the Himalayas. An excellent
description and line drawings of Indian material were
given by Pande & Udar (1956), who also studied the
ontogeny of the gametangia and the embryogenesis. Jones
(1985) remarked that his records of C. crispula were only
the second report of this species from Africa [Tanzania
and Malawi (which includes part of Chowo Forest)], the
first was by Gerola (1947), when he described C. golae
from Ethiopia (= Abyssinia). Jones believed that this
species should be treated as a synonym of C. crispula.
Arnell (1960) had misidentified a specimen of C. golae ,
collected by Dr John Eriksson in Ethiopia (= Abyssinia),
as Monocolea gottschei Lindb. (Grolle 1985), which does
not, however, grow in Africa. Besides the Himalayas
(and Indomalaya) the genus Calycularia is also known
from Taiwan, Japan, Siberia, Alaska (Schuster 1982), the
Aleutian Islands and Pacific northwest of North America
(Davidson & Smith 1992), as well as Mexico (Grolle
1980), and it is probably of Laurasian origin. Although
FIGURE 15. — Calycularia crispula. SEM micrographs of spores. A, ?proximal face of spore; B, spore seen from side; C, D, distal face ol spore;
E, part of spore much enlarged; F, young spores and elaters. A— E, S.M. Perold 2668', F, S.M. Perolil 2677. A-D, x 995; E, X 1990;
F, X 260. Micrographs by S.M. Perold.
Bothalia 23,1 (1993)
83
A-.'t '
5
FIGURE 16. — Calycularia crispula, LM photograph of elater, S.M.
Perold 2677, x 350.
Stephani (1900) had assigned six species to the genus, it
now appears to have just two, with C. crispula and C. laxa
Lindb. & Arnell [confined to the polar regions of Alaska
and Siberia (Davidson & Smith 1992)], the only species
belonging here, because Schuster (1982) transferred C.
radiculosa to the new monotypic genus, Sandeothallus
Schust.
The specimens collected by me are appreciably smaller
than the thallus sizes reported by Jones (1985), i.e. 20—50
mm long. My collections must be young plants, as only
one mature sporangium was found, which had not yet
dehisced. Pande & Udar (1956) reported it as dehiscing
by 4—6 irregular valves. An elaterophore was not observed
either; apparently it is not well developed in this species.
The seta did not elongate much and the sporangium
remained inside the perianth; with maturity the seta
reportedly elongates and raises the sporangium above the
perianth. The antheridia may not always be in continuous
rows and may grow in groups. The small ventral scales
are mostly confined to the region close to the apices of
the plants examined; their presence distinguishes
Calycularia from Pallavicinia lyelli and Dumortiera
hirsuta, which lack them. The SEM spore micrographs
taken in this study compare well with those of Inoue &
Hibino (1984).
Specimens examined
ZAMBIA. — 1033: Nyika Nat. Park, (—DA), Chowo Forest, on bark
of tree next to path, 15-4-1991, S.M. Perold 2668.
MALAWI.— 1033: Nyika Nat. Park, (-DA), 15 km W of Chilinda,
in forest on Parinari excelsa tree, 16-4-1991, S.M. Perold 2677.
ACKNOWLEDGEMENTS
I wish to express my sincere gratitude to Dr R. Grolle,
Jena, for kindly identifying my two collections and
Dr Grolle and Prof. T. Poes, Eger, for refereeing the
manuscript. My thanks also to the typist, Mrs J. Mulvenna,
and to the photographer, Mrs A. Romanowski, (both of
NBI) for their valuable contributions.
REFERENCES
ARNELL, S. 1960. Hepatics collected by Dr John Eriksson in Abyssinia
in 1958. Svensk Botanisk Tidskrift 54: 187—192.
DAVIDSON, P.G. & SMITH, D.K. 1992. Calycularia crispula (Hepati-
cae) in the Aleutian Islands and Pacific northwest of North
America. The Bryologist 95: 266—269.
GEROLA, F.M. 1947. Epatiche dell’ Abissinia meridionale (Raccolte
dalla Missione Ittiologica in A. O.I. Lavori di Botanica. Istituto
Botanico dell’ Universita Padova 3: 471—485.
GROLLE, R. 1980. Miscellanea hepaticologica 201—210. Journal of
Bryology 11: 325—334.
GROLLE, R. 1985. Miscellanea hepaticologica 231—240. Journal of the
Hattori Botanical Laboratory 58: 197—202.
INOUE, H. & HIBINO, R. 1984. Studies on spore morphology of
hepatics (1). Metzgeriales. Bulletin of the National Science
Museum (Tokyo). Ser. B (Botany) 10: 177—189.
JONES, E.W. 1985. African hepatics XXXV. Some new or little-known
species and some noteworthy records. Journal of Bryology 13:
497-508.
MITTEN, W. 1861. Hepaticae of the East Indies. Journal of the Proceed-
ings of the Linnean Society 5: 89—128.
PANDE, S.K. & UDAR, R. 1956. Studies in Indian Metzgerineae. III.
Calycularia crispula Mitten. Phytomorphology 6: 331—346.
SCHUSTER, R. 1982. Studies on Hepaticae, LIX. On Sandeothallus
Schust., gen. n. and the classification of the Metzgeriales. Nova
Hedwigia 36: 1—16.
STEPHANI, F. 1900. Species hepaticarum. Vol. 1. Bulletin de I 'Herbier
Boissier 6: 300—411.
S.M. PEROLD
MS. received: 1992-03-16.
Bothalia 23,1: 85-90 (1993)
First report on the presence of Enterobryus species (Trichomycetes:
Eccrinales) in South Africa and the description of three new species
G.J.M.A. GORTER*
Keywords: Diplopoda, Eccrinales, Enterobryus spp. nov., gut fungi, millipedes. South Africa, Trichomycetes
ABSTRACT
The occurrence of Trichomycetes in the Republic of South Africa is reported for the first time. Thus far only various
juliform millipedes have been examined for the presence of these fungi. Three new species of Enterobryus have been found
and are described in detail, viz. E. centroboli Gorter, E. chaleponci Gorter and E. zinophorae Gorter.
UITTREKSEL
Die voorkoms van Trichomycetes in die Republiek van Suid-Afrika word vir die eerste keer aangemeld. Tot dusver is
slegs verskillende wurmagtige duisendpote vir die aanwesigheid van hierdie swamme ondersoek. Drie nuwe spesies van
Enterobryus is gevind en word beskryf, nl. E. centroboli Gorter, E. chaleponci Gorter en E. zinophorae Gorter.
INTRODUCTION
Enterobryus species are gut fungi which belong to the
class Trichomycetes, lower fungi which are placed in
the Subdivision Zygomycotina (Lichtwardt 1986). All
Trichomycetes are characterised by the production of
sporangiospores and the presence of a secreted holdfast
with which the thalli are attached, mostly to the internal
cuticular surface of certain Arthropoda. Four orders
have been recognised in the Trichomycetes by Manier
& Lichtwardt (1968), viz. Harpellales, Asellariales,
Eccrinales and Amoebidiales. Sexual reproduction has
been observed only in the Harpellales and in one genus
(Enteropogon) of the Eccrinales (Hawksworth etal. 1983).
None of these fungi have been grown in axenic culture
except a few of the Harpellales ( Smittium spp. and
Trichozygospora chiron omidarum) and one of the
Amoebidiales ( Amoebium parasiticum) (Lichtwardt 1978).
However, this does not imply that they are parasites. Their
relationship with their hosts is considered to be commen-
salistic, the host neither benefitting nor suffering from the
association (Moss 1979). They produce one or more types
of sporangiospores basipetally. Lichtwardt (1954, 1958)
designated these spore types as A, B, C, D, E, F and G.
They are attached by a holdfast to the hindgut cuticle of
Diplopoda, less often Insecta (Coleoptera) and Crustaceae
(Lichtwardt 1986). As noted by Lichtwardt (1978), the
Eccrinales is, from a taxonomic viewpoint, the most
difficult order of the Trichomycetes to study, probably on
account of the unstable morphology of its members and
the inability of researchers to culture them.
Work on the Eccrinales has been done principally in
Europe, particularly in France (Duboscq et al. 1948;
Manier 1950, 1954, 1961, 1963, 1964, 1969, 1970; Pois-
son 1927, 1928, 1929, 1931) and in the United States of
America (Leidy 1849a, b; Lichtwardt 1954, 1957a, b, 1958,
1960a, b), but studies have also been done in India
(Rajagopalan 1967) and Japan (Lichtwardt et al. 1987).
* Plant Protection Research Institute, Private Bag X134, Pretoria 0001.
MS. received: 1992-02-11.
This article records the presence of these fungi for the
first time in South Africa.
MATERIALS AND METHODS
Fungi for study were obtained from live Diplopoda. The
procedures for dissection of the millipedes and observa-
tion for the presence of fungi were similar to those used
by Lichtwardt (1954). However, to facilitate the cutting off
of the head and anal segment, the live millipedes were first
immobilised by placing them in tubes of a suitable dimen-
sion and cooling them in a freezer for 10 or more minutes,
depending on the size of the millipede. The gut was then
removed by grasping the posterior portion of the hindgut
with a forceps and gently pulling the gut from the body.
Next, the gut was cut open with finely pointed, curved
scissors after which the undigested gut content was re-
moved with the aid of a thin jet of water. As the removal
of the cuticle with the fungi from the gut was found to
be laborious and not always successful, most examinations
were made of the fungi in situ, either in water or after
treatment with lactophenol, with or without cotton blue.
Observations on nuclei were made after fixing in Clarke’s
fluid (Bradbury 1973) and staining with Heidenhain’s iron-
alum-haematoxylin.
Millipedes were obtained from various parts of the
country. Studies were confined to the juliform type of
millipedes.
RESULTS AND DESCRIPTIONS
During the rainy seasons of 1989/90 and 1990/91, dozens
of millipedes of different species including common ones
such as Doratogonus setosus (Voges), D. circulus (Attems)
and Orthoporoides pyrocephalus (L. Koch), were exa-
mined for the presence of Trichomycetes. Every species
showed some signs of infestation. However, most of them
lacked primary spores whereas the mycelium with secon-
dary spores had traits similar to those described species
which produce primary spores. This has made identifica-
tion impossible. Nevertheless, in different groups of
86
Bothalia 23,1 (1993)
millipedes, three fungi were encountered which differed
sufficiently from described species to be recognised as
new.
Figures illustrating the newly described species serve
as holotypes because the slides on which they are based
are subject to deterioration.
Enterobryus centroboli Gorter, sp. nov.
Hyphae rectae vel undulatae, 3000-3800 x 7.5—12.5
(—15) ^m, plerumque hyalinae. Cytoplasma granulosum
et obscurum in hyphis laterioribus. Hyphae saepe tumidae
prope basim sed angustiores ad retinaculum. Retinaculi
orbis basalis 10.0— 12. 5(— 15) pm diam., caulis perbrevis,
circa 5.0 x 7.5 pm, vel absens. Sporangiosporae (typus A)
15.0 x 7.5 jtm (uninucleatae) et 40 60 x 7.5 ^tm (quadrt-
nucleatae). Sporae multinucleatae (typus E) 90—125 x
10-20 pm. Sporae uninucleatae (typus F), 5.0-7.5 x 10
pm.
Habitat affixa in intestino posteriore Centroboli spp. ,
Natal, 1991.
TYPUS. — Figura 1A— F nititur laminis vitreis PREM
50874 (NC 20) , PREM 50875 (NC 18) et PREM 50876 (NC
43) Centroboli lawrencei (Schubart).
The fungus develops unbranched thalli which are
attached to the anterior part of the hindgut, just below but
occasionally also just inside the sphincter muscle (the
muscle which divides the fore- and hindgut). Hyphae also
develop towards the posterior end of the hindgut. In both
cases, the hyphae are fairly straight to undulating, 7.5—12.5
(—15) ^m wide, those at the front are up to 3800 pm long
and those at the back up to 3000 pm. Most hyphae are
hyaline but some of those in front tend to become wider
and more opaque as the result of dense granular cytoplasm
towards the hyphal apex. The narrower hyaline hyphae
produce at their apex short or longer type A sporangio-
spores. The short ones (15.0 x 7.5 pm) are uninucleate
and the longer ones (40—60 x 7.5 /rm) are quadrinucleate
(Figure 1A, C). The wider, more opaque hyphae produce
3 to 4 apical or sometimes intercalary spores, 90—125 x
10—20 pm (Figure IF), which appear to be multinucleate
and of Lichtwardt’s type E.
Holdfasts are produced at the straight basal ends of the
hyphae which are often swollen (by 2.5— 5.0 ^im) towards
the holdfast and then narrow towards the point of attach-
ment (Figure IE). The holdfast has a very short stalk which
is often shorter than wide, e.g. 5.0 x 7.5 ^m. The diameter
of the attachment disc is comparatively small, viz.
10.0-12. 5(— 15) pm.
FIGURE 1. — Enterobryus centroboli Gorter. A, left, hyphae with 4-nucleate A spores, right, germinated type A spore fastened to substrate; B,
empty sporangia (arrowed) from which type A spores have escaped; C, germinated type A spores which immediately develop holdfasts
(arrowed); D, stacks of uninucleate primary spores; E, base of hypha which widens towards holdfast; F, type E spores. Scale bars = 25 fim.
Bothalia 23,1 (1993)
87
FIGURE 2. — Enterobryus zinophorae Gorter. A, rounded base of folded spore inside basal part of sporangium; B, apex of developing folded
spore; C, spiral base of hy pha devoid of sporangia; D, mature folded spore inside sporangium in straight part of hypha (spore tip arrowed);
E, holdfast with short stalk (arrowed) on base of straight hypha; F, empty sporangium cell with transverse folds in wall. Scale bars = 25 pm.
Hyphae which produce primary sporangiospores are
rare or absent. These hyphae are found at the posterior
end of the hindgut where they produce stacks of up to 85
uninucleate spores towards their apex (type F) which are
slightly shorter than wide, viz. 5.0— 7.5 x 10 pm (Figure
ID). Here, too, the holdfast has a short stalk, up to 5 pm,
with a small disc diameter of 10.0—12.5 pm.
Habitat: attached to the hindgut lining of Centrobolus
spp. from Natal (Cedara and Mtunzini), 1991.
TYPE. — Figure 1A— F, based on slides PREM 50874
(author’s collection number NC 20), PREM 50875 (NC
18) & PREM 50876 (NC 43) all of Centrobolus lawrencei
(Schubart).
Enterobryus zinophorae Gorter, sp. nov.
Hyphae rectae, flexae vel undulatae, 2000—3000 x
(7.5— )10.0— 12. 5(— 15) pm, raro incurvatae prope basim.
Cytoplasma hyalinum. Hyphae leviter dilatatae ad basim.
Retinaculum cum caule brevissimo, breviore quam lato,
haud longiore quam 6 pm: orbis basalis 12.5—20.0 ^m
diam. Nonnullae hyphae 1—6 cellulas sporangiales
175—300 x 10 pm ad apicem producentes. Sporangia
matura sporam unam longissimam replicatamque
continentia. Sporae basi tumida et rotunda sine palliolo
apicali. Post liberationem sporarum parietes sporangiales
contrahuntur fiuntque multirugosi. Sporae liberatae,
250—350 x 7.5—10 /xm, a (undo germinantes, hyphas
breves cum retinaculo producentes. Formas alias spora-
rum non vidi.
Habitat affixa intra sphincterem intestini Zinophorae
spp.
TYPUS. — Figura 2 A— F nititur laminis vitreis PREM
50877 (MP 4) et PREM 50878 (MP 7) Zinophorae
diplodontae (Attems), Pretoria, Transvaal, Dec. 1990.
Bothalia 23,1 (1993)
The thalli are inside the sphincter muscle. The hyphae
are hyaline, straight, bent or undulating towards their apex
but occasionally hooped near their base (Figure 2C),
2000-3000 x (7.5— )10.0— 12.5(— 15) /mi. Hyphae have
rounded ends and may widen slightly towards their base
where they secrete a holdfast with a short stalk not longer
than 6 /im and usually shorter than wide (Figure 2E).
Some hyphae produce a number of cells 175-300 /cm long
and usually 10 /cm wide towards their apex. These are
sporangia which, when mature, contain long, folded spores
(Figure 2B, D) with a slightly swollen obtuse base (Figure
2A) and a pointed apex without a protecting cap as
illustrated by Manier et al. (1974: fig. IF). These spores
are 250-350 x 7.5-10.0 /cm. The sporangia, from which
they escape, contract to become empty cells with many
folds (Figure 2F). The escaped spores straighten out, im-
mediately develop a hypha from the rounded base and
E
attach themselves to the sphincter lining. The hypha keeps
on growing after which the spore presumably degenerates
(empty filaments at the end of comparatively short hyphae
have been noted). No other type of spore has been
observed.
Habitat: attached to the sphincter muscle lining of
Zinophora spp.
TYPE.— Figure 2A-F, based on slides PREM 50877
( author ’s collection number MP 4) & PREM 50878 (MP
7) of Zinophora diplodonta (Attems), Pretoria, Transvaal,
Dec. 1990.
Enterobryus chaleponci Gorter, sp. nov.
Hyphae hyalinae, satis rectae sed plerumque circulares
prope basim, circa 2500 x (10.0 — )12. 5 — 15.0(— 17.5) /cm,
in circulis plerumque latiores quam alibi; latitudo
FIGURE 3. — Enterobryus chaleponci Gorter. A, short sporangia with folded spores (tips arrowed) inside hoops of swollen hyphae; B, mature
spore inside sporangium in straight part of hypha (spore tip arrowed); C, holdfasts without stalks on straight basal end of hyphae; D, germinated,
straightened-out acicular spore (base arrowed); E, multi nucleate spore of type E; F, germinated multinucleate spore attached to substrate
(holdfast arrowed). Scale bars = 25 ^m.
Bothalia 23,1 (1993)
89
aliquando etiam variat in partibus rectis. Retinaculum sine
caule, vel cum caule perbrevi; orbis basalis (12.5— )L5— 20
pm diam. Sporae longissimae, 125—230 pm, sine palliolo
apicali, replicatae, in sporangiis intra circulos 70 — 85 x
15 pm, in partibus rectis 105 — 150 x 12.5 /xm. Fundus
basalis sporae truncatus cum levi depressione in centro.
Cytoplasma hypharum latiorum dense granulosum prope
apicem. Hyphae latae aliquando cellulas longas (ad 125
/xm) producentes endosporium singulum multinuclearem
continentes.
Habitat affixa intra sphincterem intestini Chaleponci
polechanci Kraus, Baltimore, Transvaal, Mai. 1991.
TYPUS. — Figura 3A-F nititur laminis vitreis PREM
50879 (TB 5) et PREM 50880 (TB 30).
The thalli are inside the sphincter muscle. The hyphae
are hyaline, fairly straight but strongly hooped lower down,
+ 2500 x (10— )12.5— 15.0(— 17.5) pm. The hoops are often
wider than the straight parts of the hyphae, 15—20 pm.
The latter are of variable width, widening by 2 pm and
then narrowing again. A holdfast (Figure 3C) without a
stalk or with a very short one, e.g. 2.5 pm, develops at
the base of a hypha. The disc diameter varies from
(12.5 — )15 — 20 pm. The thicker hyphae and those that
widen from bottom to top, have a dense granular cytoplasm
and often become slightly brown. Folded spores have been
observed in the hooped as well as the straight part of
hyphae (Figure 3A, B). In the first, sporangia are 70—85
x 15 /xm; in the latter, 105—150 x 12.5 pm. The spores
are 125—230 x 10.0—12.5 pm and have a truncated basal
end with a slight depression in the centre. After escaping
from the sporangia, the folded spores straighten, germinate
basally and soon attach themselves to the inside of the
sphincter muscle (Figure 3D). At the apex of a hypha with
dense cytoplasm, a long cylindrical sporangium (up to 125
/xm) is often formed (Figure 3E). These sporangia are
slightly swollen in comparison with the rest of the hyphae
and each contains a multinucleate endospore.
Habitat: attached to the sphincter muscle lining in the
gut of Chaleponcus polechancus (Kraus), Baltimore,
Transvaal, May 1991.
TYPE. — Figure 3A— F, based on slides PREM 50879
( author’s collection number TB 5) & PREM 50880
(TB 30).
DISCUSSION
Apart from reporting the occurrence of Trichomycetes
for the first time in South Africa, a most interesting result
of this investigation was the discovery of sporangia
containing long, folded, pointed spores in some of these
fungi. These have hitherto been found only in millipedes
from Central Africa by Manier et al. (1974/75). They
described a number of species in which acicular, folded
spores are formed but noted that they develop only in the
narrow hyphae. This led Lichtwardt (1986) to pose the
question of whether the thalli with long, folded spores
perhaps belong to one fungal species, whereas the wider
thalli with different spores belong to different fungi. The
latter supposition is apparently supported by our finding
that, in E. chaleponci, the two types of spores present
mostly occurred alone in different specimens of a batch
of 36 millipedes of this species from one locality. However,
the fact that these spore types were found together, albeit
infrequently, and the fact that narrow hyphae could enlarge
to become wider, point to a close relationship.
The suggestion that hyphae with long, folded spores all
belong to one species is probably not valid because I found
clear differences in size between the folded spores of
E. chaleponci and E. zinophorae. The shape of their basal
ends also differed slightly while they develop at a different
locus. In E. zinophorae they develop only in the straight
part of hyphae, while in E. chaleponci also within the
hooped part of hyphae. Furthermore, Manier et al.
(1974/75) observed that in some Eccrinales species the
apex of the folded spore is protected by a solid point devoid
of protoplasm, whereas in other species this protection
is absent. These differences all indicate that different
species are involved.
ACKNOWLEDGEMENTS
I wish to thank the following persons sincerely for the
collection of the millipedes examined: Mesdames Pat
Caldwell, Louise Schutte, Jeany Heinlein and Dr R. L.
Kluge from the Plant Protection Research Institute, and
Prof. Albert Eicker of the University of Pretoria, Mrs Irene
Robinson and Mr H. A. Robinson.
I am also much indebted to Dr Richard L. Hoffman of
the Virginia Museum of Natural History, USA, for iden-
tification of the millipedes. Thanks are also due to Mr Paul
Hasse of the University of Pretoria for checking the Latin
descriptions and to Miss Alice Baxter of our Institute for
reading the manuscript.
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Bothalia 23,1: 91-104 (1993)
Mycorrhizal status of plants growing in the Cape Floristic Region, South
Africa
N. ALLSOPP* and W. D. STOCK*
Keywords: cluster roots, Fynbos, mediterranean-type shrublands, mycorrhizas, root systems
ABSTRACT
A survey of the mycorrhizal status of plants growing in the Cape Floristic Region of South Africa was undertaken to assess
the range of mycorrhizal types and their dominance in species characteristic of this region. Records were obtained by ex-
amining the root systems of plants growing in three Cape lowland vegetation types, viz. West Coast Strandveld, West Coast
Renosterveld and Sand Plain Lowland Fynbos for mycorrhizas, as well as by collating literature records of mycorrhizas
on plants growing in the region. The mycorrhizal status of 332 species is listed, of which 251 species are new records.
Members of all the important families in this region have been examined. Mycorrhizal status appears to be associated mainly
with taxonomic position of the species. Extrapolating from these results, we conclude that 62% of the flora of the Cape
Floristic Region form vesicular-arbuscular mycorrhizas, 23% have no mycorrhizas, 8% are ericoid mycorrhizal, 2% form
orchid mycorrhizas, whereas the mycorrhizal status of 4% of the flora is unknown. There were no indigenous ectomycor-
rhizal species. The proportion of non-mycorrhizal species is high compared to other ecosystems. In particular, the lack of
mycorrhizas in several important perennial families in the Cape Floristic Region is unusual. The diversity of nutrient acquir-
ing adaptations, including the range of mycorrhizas and cluster roots in some non-mycorrhizal families, may promote co-
existence of plants in this species-rich region.
UITTREKSEL
’n Opname van die status van mikorisas by plante wat in die Kaapse Floristiese Streek van Suid-Affika voorkom, is ondemeem
om die omvang te bepaal van verskillende mikorisatipes en hulle oorheersing in spesies kenmerkend van hierdie streek.
Rekords is verkry deur die wortelsisteem van plante in drie laagliggende Kaapse veldtipes, naamlik Weskus-strandveld, Weskus-
renosterveld en Sandvlakte-fynbos, vir mikorisas te ondersoek. Rekords uit die literatuur van toepassing op mikorisas wat
op plante in hierdie streek groei, is ook in ag geneem. Die status van mikorisas by 332 spesies word vermeld, 251 daarvan
nuwe rekords. Lede van al die belangrike families in die streek is ondersoek. Die status van mikorisas is skynbaar
hoofsaaklik met die taksonomiese posisie van die spesie geassosieer. Ons het tot die gevolgtrekking gekom dat 62% van
die flora van die Kaapse Floristiese Streek vesikuler-arbuskulere mikorisas vorm, 23% geen mikorisas het nie, 8% erikoiede
mikorisas vorm, 2% orgidee-mikorisas het, terwyl die mikorisa-status van 4% van die flora onbekend is. Daar was geen
inheemse spesies wat ektomikorisas gevorm het nie. Die proporsie nie-mikorisaspesies is hoog in vergelyking met die wat
in ander ekosisteme aangetref word. Die afwesigheid van mikorisas by verskeie belangrike meeijarige families in die Kaapse
Floristiese Streek is veral ongewoon. Die verskeidenheid aanpassings om voedingstowwe te bekom, insluitend die omvang
van mikorisas en troswortels by sekere nie-mikorisafamilies, mag die gelyktydige bestaan van plante in hierdie spesieryke
streek bevorder.
INTRODUCTION
It is generally accepted that most terrestrial plants
probably form mycorrhizal associations between their roots
and certain fungi, although the vast majority of plants
growing in natural ecosystems have not had their mycor-
rhizal status confirmed (Trappe 1987; Newman & Reddell
1987). The mycorrhizal status of plants reflect both their
taxonomic affinities and their ecology. Investigations on
the mycorrhizal status of plants in various parts of the
world indicate that the major terrestrial biomes can be
characterized by specific mycorrhizal types (Read 1991).
Surveys of mycorrhizas show that trees of forests and
woodlands are either ectomycorrhizal or vesicular-
arbuscular mycorrhizal; herbaceaous plants and shrubs in
grasslands and shrublands usually form vesicular-
arbuscular mycorrhizas; boreal and temperate heathlands
are dominated by ericoid mycorrhizal species; and
disturbed ecosystems by non-mycorrhizal weed species
(see Brundrett 1991 for references). Whereas the mycor-
rhizal status of some floras is well documented (e.g. British
* Department of Botany, University of Cape Town, Private Bag,
Rondebosch 7700, South Africa.
MS. received: 1992-05-12.
Isles by Harley & Harley 1987), little is known about both
the mycorrhizal associations of plants in the Cape Floristic
Region (CFR) and their functional role in low nutrient
ecosystems.
The vegetation of the CFR contrasts sharply, in terms
of taxonomic composition and vegetation structure, with
the surrounding southern African vegetation. The Cape
flora has a high species diversity (± 8 500 species), around
68% species endemism (Bond & Goldblatt 1984), and high
beta and gamma species turnover (Cowling 1990). Agricul-
ture, urbanization and alien plant invasion are a severe
threat to this flora as a result of the limited range of many
plant species, and have led to the destruction of much of
the lowland vegetation (Hall 1983). Mycorrhizas act as soil
nutrient-absorbing organs for the plants. As such they will
influence the physiology of individuals, as well as their
interactions with other plants growing in the same
community (Harley 1989; Read 1991). Recognizing the
patterns of distribution and understanding the ecological
role of mycorrhizal types in a community may be crucial
to understanding the dynamics which shape plant com-
munities (Allsopp & Stock in press).
This study collates published records of the mycorrhizal
status of plants occurring in the CFR as defined by
92
Bothalia 23,1 (1993)
Bond & Goldblatt (1984). In addition, the mycorrhizal
status of plants growing in three lowland vegetation types,
West Coast Strandveld, West Coast Renosterveld and Sand
Plain Lowland Fynbos, is reported for the first time. The
aim of this paper is to provide information on the mycor-
rhizal status of plant species which may be of significance
in explaining vegetation patterns and plant functioning in
the CFR.
STUDY AREAS
Three study sites representing West Coast Strandveld,
at Melkbosstrand (33°45'S 18°27'E), West Coast Renoster-
veld on the hill, Joostenberg, on the farm Hercules Pillar
(33°46'S 18°46'E), and Sand Plain Lowland Fynbos at the
Fynbos Biome intensive study site (33°31S 18°32'E) at
Pella, were chosen to investigate the mycorrhizal status
of a broad range of plants growing in threatened habitats
in the CFR. The classification of the vegetation categories
follows that of Moll et al. (1984). The strandveld vegeta-
tion, growing on coarse/medium sandy soil (organic matter
2.2%, pH of 7.5, total P 422 ^g g-1 (Witkowski &
Mitchell 1987)) is a broad-leaved, sclerophyllous 1.0— 2.5
m high shrubland with a large succulent component
(Boucher 1983). The Renosterveld vegetation, growing on
a fine sand/clayey soil [organic matter 4.9% , pH 4.1, to-
tal P 127 ^ig g-1 (N. Allsopp unpublished)] is an ever-
green, cupressoid or microphyllous shrubland, 1-2 m
high, dominated by Elytropappus rhinocerotis with strong
Lowland Fynbos affinities (Tansley 1982; Boucher 1983).
The Sand Plain Lowland Fynbos growing on medium
textured sandy soil [organic matter 1.4— 3.4%, pH
4.6-4.8, total P 23-34 g-1 (Mitchell, Brown &
Jongens-Roberts 1984)] is an ericoid- leaved, sclerophyl-
lous vegetation, 0.75—1.5 m high with some taller shrubs,
characterized by the presence of Phylica cephalantha
(Boucher 1983). Vegetation surveys at the three sites have
recorded 56, 63 and 215 perennial species at the Strand-
veld (Siegfried 1981), Renosterveld (Tansley 1982) and
Lowland Fynbos (Boucher & Shepherd 1988) sites respec-
tively. In addition annuals and bulbous species are
numerically important components of all three vegetation
types (Boucher 1983; Bond & Goldblatt 1984).
MATERIALS AND METHODS
Root collection
Roots were collected during August, September and
early October when unthickened roots were common while
the soil was moist. Two collections were made at both the
Strandveld (during August 1987 and September 1989) and
Renosterveld sites (during October in 1988 and September
1989). The Lowland Fynbos site was sampled six times
over four years (June and August 1986, August and Sep-
tember 1987, September 1988, August 1989). Two 25 x
25 m plots were set up at a site on each collection day.
The plots at the Strandveld site were situated 60—300 m
inland of the high water mark. The Renosterveld plots were
on the NW-SW-facing lower slopes of Joostenberg. At the
Lowland Fynbos site, plots were randomly scattered
throughout the 269 ha study site.
Roots of one representative of all species occurring in
the plots were sampled. In addition, plant species not in
the plots, but encountered in the vicinity, were sampled.
Smaller plants, including annuals, perennial seedlings and
bulbous plants, were excavated with entire root systems.
Roots of larger shrubs were collected by carefully tracing
the root system from the main stem until young, unthick-
ened roots were encountered. However, for some species,
including members of the Anacardiaceae and Ebenaceae,
few young roots could be found despite extensive excava-
tion along roots down to 1 m. At the Renosterveld site
some species were not sampled because they grew only
in narrow cracks among rocks (e.g. Olea sp.). At the
Strandveld site the large size of dominant shrubs and
density of the vegetation at ground level, as well as
spininess of some species, precluded collection of these
species’ roots.
Young roots were removed from surrounding soil in the
field and immediately placed in vials containing 10% KOH
for clearing. Wherever possible, 500 mm of root per plant
was collected. Roots were cleared for one week at 20 °C,
and then rinsed under running tap water (Smith & Bowen
1979). Where necessary, pigmented roots were decolour-
ized with H2O2 or NaClO. This was followed by acidi-
fication in 1 M HC1 and staining in 0.05% Trypan blue
in lactic acid solution (Kormanik & McGraw 1982). Root
segments were permanently mounted in a polyvinyl acid
solution and inspected at 100 and 400 times magnifica-
tion with a light microscope for mycorrhizal structures.
Plants were classified according to Cronquist (1988) and
species names follow Gibbs Russell et al. (1985, 1987).
Literature survey
All known records of the mycorrhizal status of plants
in the CFR were consulted. Only those records which
reported the mycorrhizas of plants actually growing in the
CFR are listed here. Confirmation of infection status of
some species was undertaken by examining roots of plants
growing in soil from their natural habitats in pot culture.
RESULTS
Vesicular-arbuscular mycorrhizas (VAM), characterized
by the presence of arbuscules in the inner cortical cells
with or without vesicles (Harley & Smith 1983), were the
most common type of mycorrhiza (61% of species
examined) (Appendix). Infections regarded as vesicular-
arbuscular (VA) mycorrhizal but morphologically distinct
from the above types were formed by Aristea dichotoma,
which formed intracellular coils similar to those described
by Brundrett & Kendrick (1990) in Trillium grandiflorum,
while vesicular-arbuscular mycorrhizal fungi in Orphium
frutescens and Sebaea exacoides formed structures typical
of those seen in other members of the Gentianaceae
(Jacquelinet-Jeanmougin & Gianinazzi-Pearson 1983).
Infection formed by the ‘fine endophyte’ (Greenall 1963)
was occasionally seen, but was never exclusively found
on one species. Ericoid mycorrhizas (ERIC) were found
in the hair roots of all members of the Ericaceae examined
(Appendix). They are characterized by the formation of
coiled and branched, fine hyphae in the cortical cells (Read
1983). Orchid mycorrhizas (ORCH) were seen in the two
Disa spp. examined (Appendix) and consist of characteris-
tic coarse, coiled intracellular hyphae (Harley & Smith
1983). No ectomycorrhizal infection was seen in the in-
digenous species examined. Introduced ectomycorrhizal
Bothalia 23,1 (1993)
93
species such as pines, oaks, poplar and eucalypts form
ectomycorrhizas in the CFR but the ectomycorrhizal fun-
gi were in all likelihood introduced with imported saplings
(Van der Westhuizen & Eicker 1987).
Ninety-one of the 332 species reported formed no
mycorrhizas (Appendix). These were concentrated in the
Caryophyllidae and the families Brassicaceae, Cras-
sulaceae, Proteaceae, Santalaceae, Zygophyllaceae,
Restionaceae and Cyperaceae. Plant roots which contained
occasional vesicles but no arbuscules were regarded as
functionally non-mycorrhizal (Hirrel et al. 1978).
Some earlier studies (Laughton 1964; Low 1980) have
reported endophytic mycorrhizas (ENDO) as being present
but descriptions or illustrations do not indicate structures
which are typical of mycorrhizas as they are presently
delimited (Harley & Smith 1983). Non-mycorrhizal fungi
were fairly frequent in both mycorrhizal and non-
mycorrhizal roots examined for this study. Therefore,
reports of fungal infection as ‘endophytic mycorrhizas’
should be viewed with caution. The most common non-
mycorrhizal root inhabiting fungus was Olpidium sp.,
which forms cysts and zoosporangia (Sampson 1939),
which may be mistaken for VA mycorrhizal vesicles if care
is not taken. Unidentified hyphal fungi, including dark,
septate hyphal fungi forming microsclerotia (DSH) similar
to those described by Haselwandter & Read (1980) in
alpine vegetation, were also present. The non-mycorrhizal
roots of members of the Proteaceae have been shown to
support a fungal flora that is distinctly different to that
found in the non-rhizosphere soil (Allsopp et al. 1987).
Infection by Olpidium sp. and other fungi was particularly
heavy in the root systems of members of the Poaceae and
Scrophulariaceae where they could obscure infection by
VA mycorrhizal fungi (Appendix).
DISCUSSION
The mycorrhizal status of many of the taxa recorded here
has not previously been reported, as can be expected, given
the high levels of endemism and species radiation in the
CFR and the paucity of mycorrhizal studies in this region.
All the important families, as well as the twenty largest
genera in the CFR (Bond & Goldblatt 1984), now have
had some of their members examined for mycorrhizas.
The endemic Penaeaceae and near endemic Bruniaceae
have VA mycorrhizal species. Families which need further
investigation are the Anacardiaceae, Ebenaceae, Jun-
caceae, and Celastraceae, as well as the endemic families
Stilbaceae, Grubbiaceae, Roridulaceae, Retziaceae and
Geissolomaceae. The lowland vegetation types have been
well covered and generalizations regarding their mycor-
rhizas can now be made. However, the mycorrhizal status
of the vegetation of habitats such as forests, seasonally
waterlogged soils, limestone and mountain ecosystems are
less well catalogued.
The absence of ectomycorrhizas is a notable feature of
this flora. Ectomycorrhizal structures are reported in many
plants growing in arid regions of Australia which belong
to families and genera also present in the CFR (Warcup
1980; Warcup & McGee 1983; McGee 1986; Bellgard
1991). Ectomycorrhizas are also known to occur in the low
nutrient soils of the Australian mediterranean heathlands
(Chilvers & Pryor 1965; Brundrett & Abbott 1991). In
addition, ectomycorrhizas have been found on trees
growing in other African ecosystems (Redhead 1968;
Hogberg & Piearce 1986). However, shrub vegetation
growing on Kalahari sands adjacent to ectomycorrhizal
woodlands was exclusively vesicular- arbuscular mycor-
rhizal (Hogberg & Piearce 1986). The reasons for the
exclusion of ectomycorrhizas from the CFR are not clear,
although this can possibly be ascribed to the absence of
an organic surface horizon which is usually associated with
the presence of ectomycorrhizas (Read 1991), and to
frequent disturbance by fire. For instance, in Italian
mediterranean ecosystems on calcareous soils, canopy
cover values for ectomycorrhizal plant species nine years
after fire was a quarter of that in unbumt forest (Puppi
& Tartaglini 1991). However, these explanations do not ac-
count satisfactorily for their absence in the CFR, because
ectomycorrhizas occur in fire-prone communities in
Australia with low soil organic matter (Brundrett & Abbott
1991).
The explosive speciation that the genus Erica has
undergone in the CFR (± 530 spp.) implies that ericoid
mycorrhizas are unusually common in this area. Cowling
et al. (1990) have suggested that edaphic specialization of
the endophyte has powered this speciation, but, as yet,
supporting evidence is lacking. An interesting feature of
ericoid mycorrhizal plants in the mediterranean-climate
regions of the world is their co-existence with other plant
species, whereas in more temperate regions they usually
form almost pure stands in areas where soil degradation
has produced soil conditions which plant roots and other
mycorrhizas cannot tolerate (Leake et al. 1989).
All the non-mycorrhizal families in this study have been
reported as such before, although some have had very few
species examined for mycorrhizal colonization (Trappe
1987). Many of the non-mycorrhizal species in this study
fall into the Caryophyllidae which is roughly equivalent
to the Centrospermae (Cronquist 1988) which was origi-
nally regarded as non-mycorrhizal (Gerdemann 1968).
Subsequent studies have shown that many species in this
group are capable of forming mycorrhizas (Tester et al.
1987), and that some families are typically mycorrhizal,
e.g. Cactaceae (Miller 1979). However, despite these
exceptions, 80% of the species in the Caryophyllidae
which have been examined are either non-mycorrhizal or
facultatively mycorrhizal (Trappe 1987). Mechanisms
which enable some species to actively exclude mycorrhizal
fungi, when exposed to viable inoculum, are unclear
(Tester et al. 1987; Koide & Schreiner 1992).
In dicotyledonous species, weedy, herbaceous plants
often lack mycorrhizas or are weakly mycorrhizal (Malloch
et al. 1980; Trappe 1987) and it has been noted that some
species are less likely to form mycorrhizas when coloniz-
ing disturbed sites than adjacent undisturbed areas (Miller
1979; Reeves et al. 1979). In our study, the annuals in the
Scrophulariaceae were usually non-mycorrhizal, although
a few individuals form typical VAM.
Anaerobic conditions in waterlogged soils have been
invoked to explain the absence of mycorrhizas in some
plants (Anderson et al. 1984), and Tester et al. (1987)
advance this as an explanation of the absence of mycor-
rhizas in most of the Cyperaceae. In this study the mem-
bers of the Cyperaceae and the Restionaceae examined
94
Bothalia 23,1 (1993)
were non-mycorrhizal while growing in well -drained soil
with other mycorrhizal plants, although both families are
often associated with waterlogged conditions, and so this
does not seem to be the only reason for the exclusion of
mycorrhizas from these taxa. Although Powell (1975)
reported mycorrhizal structures in some roots of members
of the Cyperaceae, he concludes that they are functionally
non-mycorrhizal due to the possession of a fine root
system. This complements Baylis’ (1975) proposal that the
magnolioid root form with poorly developed root hairs
would be more strongly mycorrhizal than finer root
systems. Two important perennial families in the CFR,
which do not form mycorrhizas (viz. Proteaceae and
Restionaceae), are characterized by the formation of cluster
roots, the rootlets of which are densely covered in long
root hairs (Purnell 1960; Lamont 1972a, 1982). In addi-
tion, cluster roots have been observed on members
of the Cyperaceae (Lamont 1974), the genus Aspalathus
(Fabaceae) (this paper and M. Cocks unpublished data)
and Australian members of the Fabaceae (Lamont 1972b;
Brundrett & Abbott 1991) , which typically have low VAM
infection levels. The absence or low infection levels of
mycorrhizas in the taxa forming cluster roots support
Baylis’ (1975) proposition that mycorrhizas will be less
important when root systems are finer. The loss of the
ability to form mycorrhizas is regarded as an evolutionarily
advanced feature (Trappe 1987).
The mycorrhizal status of the species in the CFR seems
to be a reflection of their taxonomic position, although
Newman & Reddell (1987) warn that very few families
form exclusively one type of mycorrhiza or are consistently
without mycorrhizas. This can be expected when world-
wide the higher taxa of angiosperms are poorly correlated
with their ecological niches (Cronquist 1988). Life form
or environmental factors do not satisfactorily explain the
absence of mycorrhizas in longer lived plants such as
members of the Proteaceae, Restionaceae and Zygo-
phyllaceae in the CFR and this must be regarded as a
taxon-related characteristic for many groups. Reports of
VA mycorrhizal species among the Proteaceae in New
South Wales, Australia (Bellgard 1991) and ectomycorrhizal
Faurea saligna (Proteaceae) in Zambia (Hogberg &
Piearce 1986), indicate that the mycorrhizal status of mem-
bers of this family should be investigated with respect to
soil fertility, as mycorrhizas are absent in members of this
family growing in low nutrient soils of the CFR and
Western Australia (Brundrett & Abbott 1991). Members
of families such as the Aizoaceae and Mesembryan-
themaceae, which are commonly found associated with
disturbed areas in the CFR, are non-mycorrhizal when
growing in undisturbed ecosystems. This supports the
report that at the ecosystem level, patterns of mycorrhizal
and non-mycorrhizal species among weedy species
followed taxonomic divisions irrespective of growth form
(Pendleton & Smith 1983). As most of the data here are
obtained from plants growing in the field and mycorrhizal
status was usually consistent at the family level, generali-
zations can be made regarding the mycorrhizal status of
the Cape Flora, provided cognisance is taken that excep-
tions may arise. The mycorrhizal status of the flora of the
three study sites, representing three lowland vegetation
types is summarized in Table 1. If the mycorrhizal status
of species listed in Bond & Goldblatt (1984) is inferred
from that of taxonomically related species which have been
examined, we conclude that 62% of the flora form VAM,
TABLE 1. —Summary of the mycorrhizal status of the vegetation growing
in Sand Plain Lowland Fynbos, Renosterveld and Strandveld
communities, and the Cape Floristic Region (CFR)
VAM = vesicular-arbuscular mycorrhizal; ABS = non-mycorrhizal;
ERIC = ericoid mycorrhizal; ORCH = orchid mycorrhizal.
plants without mycorrhizas are the next largest group,
ericoid and orchid mycorrhizas are found in less than 10%
of the flora, and the mycorrhizal status of 4% of the flora
is unknown (Table 1).
The proportion of non-mycorrhizal species in the CFR
is high when compared to many other vegetation types
worldwide (Brundrett 1991). As non-mycorrhizal plants are
normally associated with high levels of disturbance, or
edaphically and climatically extreme conditions, the non-
mycorrhizal flora in the CFR is atypical in that represen-
tatives of two families that dominate the vegetation of the
CFR, the Proteaceae and Restionaceae, are non-
mycorrhizal. The evolutionary and ecological significance
of this needs further exploration. The diversity of mycor-
rhizal types is possibly an indication that no one type of
mycorrhiza or other nutrient acquiring adaptation is
pre-eminently suited to the environmental conditions in
the CFR and that the diversity of nutrient acquisition
mechanisms in the CFR has probably promoted species
co-existence.
ACKNOWLEDGEMENTS
We thank C. Allsopp, M. T. Deignan, E. C. February,
J. Jacobs, A. Jensen and H. Vaughan for assistance with
field work; J. Midgley and the nursery at Kirstenbosch
for providing plants; and A. Bean, E. Esterhuysen, C.
Johnson, H. P. Linder, P. Littlewort, J. Manning, F. Powrie
and E. van Jaarsveld for help with identifying plant species.
Mr S. de Wit is thanked for permission to collect roots
on his farm, Hercules Pillar.
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%
Bothalia 23,1 (1993)
APPENDIX -A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert’s Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH - orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
Bothalia 23,1 (1993)
97
APPENDIX — A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert’s Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH - dark septate hyphae.
98
Bothalia 23,1 (1993)
APPENDIX— A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert’s Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
Bothalia 23,1 (1993)
99
APPENDIX— A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert's Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
100
Bothalia 23,1 (1993)
APPENDIX— A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert’s Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
Bothalia 23,1 (1993)
101
APPENDIX — A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
No. Loc. Lit. Myc. Notes
SCROPHULARIACEAE (corn.)
Nemesia
affinis Benth.
versicolor E. Mey. ex Benth.
barbata (Thunb.) Benth.
Phyllopodium heterophyllum (L. f.) Benth.
Polycarena
capensis (L.) Benth.
cephalophora (Thunb.) Le\yns
Sutera linifolia (Thunb.) Kuntze
Zaluzianskya
divaricata Walp.
villosa (Thunb.) F.W. Schmidt
sp.
SELAGINACEAE
Dischisma capitatum (Thunb.) Croisy
Hebenstretia
dentata L.
repens Jarosz
CAMPANULACEAE
Microcodon
glomeratum A. DC.
hispidulum (Thunb.) Sond.
Roella ciliata L.
Wahlenbergia capensis (L.) A. DC.
LOBELIACEAE
Cyphia digitata (Thunb.) Willd.
Lobelia coronopifolia L.
RUBIACEAE
Anthospermum
aethiopicum L.
sp. 1
Galium tomentosum Thunb.
ASTERACEAE
Arctotheca calendula (L.) Levyns
Arctotis
leptorhiza DC.
sp.
Athanasia trifurcata (L.) L.
Cenia turbinata (L.) Pens.
Chrysanthemoides incana (Burm. f.) T. Norl.
Chrysocoma ciliata L.
Cineraria geifolia (L.) L.
Cotula coronopifolia L.
Didelta spinosa (L. f.) Ait.
Dimorphotheca pluvialis (L.) Moench
Elytropappus
glandulosus Less.
rhinocerotis ( L . f. ) Less.
Eriocephalus
sp. 1
sp. 2
sp. 3
Felicia tenella (L.) Nees
Gazania
ciliaris DC.
sp.
Gymnodiscus capillaris (L. f.) Less.
7 P H A & S VAM
12 PMN A&S, B, M&AVAM
ABS in some, Olpidium, other fungi present
ABS in many at P and M, Olpidium. other fungi
present
Or very slight VAM, other fungi present
Or very slight VAM, Olpidium, other fungi present
Other fungi present
Slight VAM infection
Olpidium, other fungi present
DSH, other fungi present
Olpidium, other fungi present
Slight VAM infection
Olpidium present
Slight VAM infection, fine endophyte present
Fine endophyte
Olpidium, DSH, other fungi present
Needs confirmation
Fine endophyte, Olpidium, other fungi present
Other fungi present
Olpidium, other fungi present
ABS in some, Olpidium, other fungi present
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert’s Bay, West Coast Strandveld; O = Olifantsbos. Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references; A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B. M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
102
Bothalia 23,1 (1993)
APPENDIX — A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
* introduced species.
No. - number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert’s Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
Bothalia 23,1 (1993)
103
APPENDIX— A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert’s Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid myconrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
104
Bothalia 23,1 (1993)
APPENDIX— A preliminary list of the mycorrhizal status of plants occurring in the Cape Floristic Region (continued)
* introduced species.
No. = number of specimens examined.
Loc. = locality and dominant vegetation: B = Bainskloof, Mesic Mountain Fynbos; H = Hercules Pillar, West Coast Renosterveld; J = Jonkers-
hoek, Mesic Mountain Fynbos; K = Kirstenbosch Botanical Garden, in cultivation; M = Melkboschstrand, West Coast Strandveld; N
= Nortier Experimental Farm, Lambert's Bay, West Coast Strandveld; O = Olifantsbos, Cape of Good Hope Nature Reserve, Mesic Mountain
Fynbos; OK = Orange Kloof, Afromontane Forest; P = Pella, Sand Plain Lowland Fynbos; S = Saasveld, George, Afromontane Forest;
pot = plant growing in pot culture.
Lit. = literature references: A & S = this paper; ABL = A.B. Low (1980); AG = A. Gubb cited by ABL; B, M & A = R. Berliner, D.T.
Mitchell & N. Allsopp (1989); EML = E.M. Laughton (1964); FC = F. Coley cited by ABL; H & M = M.T. Hoffman & D.T. Mitchell
(1986); M & R = D.T. Mitchell & D.J. Read (1987); RKR = R.K. Robinson (1973); S & M = C.J. Straker & D.T. Mitchell (1985).
Myc. = mycorrhizal type: VAM = Vesicular-arbuscular mycorrhizas; ERIC = ericoid mycorrhizas; ENDO = endophytic mycorrhizas of an
undesignated type (see text); ORCH = orchid mycorrhizas; ABS = no mycorrhizas seen in specimens examined; DSH = dark septate hyphae.
Bothalia 23,1: 105-110 (1993)
Pollen morphology of Curroria , Mondia , Socotranthus and Stomato-
stemma (Periplocaceae)
R.L. VERHOEVEN* and H.J.T. VENTER*
Keywords: Curroria, Mondia, Periplocaceae, pollen morphology, Socotranthus, Stomatostemma
ABSTRACT
The pollen morphology of Curroria Planch., Mondia Skeels, Socotranthus Kuntze and Stomatostemma N.E. Br. was studied.
All the genera are characterized by pollen grains arranged in tetrads. The arrangement of the grains may be rhomboidal,
tetrahedral or decussate. The 4—6 pores present are restricted to the junction area of adjacent grains. The exine is smooth.
Exine structure consists of an outer, homogeneous stratum (tectum) subtended by a granular stratum. The intine is well
developed. The pollen grains of tetrads are connected by wall bridges (cross-wall cohesion). Except for small differences
which may occur between species and genera in pollen size and arrangement of tetrads, the pollen is uniform in morphology.
UITTREKSEL
Die stuifmeelmorfologie van Curroria Planch., Mondia Skeels, Socotranthus Kuntze en Stomatostemma N.E.Br. is bestudeer.
A1 die genera word gekenmerk deur stuifmeelkorrels wat in tetrades gerangskik is. Die rangskikking van die stuifmeelkorrels
kan romboidaal, tetraedries of kruisgewys wees. Vier tot ses poriee kom voor en hulle is beperk tot die aansluitingsgebied
tussen aangrensende stuifmeelkorrels. Die eksien is glad en bestaan uit ’n buitenste homogene stratum (tektum) en granulere
stratum daaronder. Die intien is goed ontwikkel . Die stuifmeelkorrels van tetrades is verbind deur wandbrue (dwarswand-
kohesie). Met die uitsondering van klein verskille tussen spesies en genera in stuifmeelgrootte en rangskikking van tetrades,
stem die stuifmeelkorrels in morfologie ooreen.
INTRODUCTION
Periplocaceae and Asclepiadaceae are two closely allied
families with several features in common. The former was
a subfamily (Periplocoideae) of the latter, but raised to
family status by Schlechter (1924), a concept followed by
Bullock (1957), a well known expert in this group. The
Periplocaceae is related to the Apocynaceae on the one
hand and to the Asclepiadaceae on the other. All three
families have in common a milky latex, flowers with
coronas, fruits composed of paired follicles and seeds with
comas of hairs. The Periplocaceae is distinguished by its
spathulate pollen carriers and pollen grains united in
tetrads. This contrasts with single-grained pollen and
absence of pollen carriers in the Apocynaceae, and pollinia
attached to wishbone-shaped translators in the Ascle-
piadaceae.
Of the 50 genera included in the Periplocaceae, approxi-
mately 20 occur in Africa. Among these Raphionacme
Harv. is the largest with 35 species endemic to Africa
(Verhoeven & Venter 1988) and one endemic to Arabia
(Miller & Biagi 1988). Raphionacme is also the only
herbaceous genus, although a number of its species are
climbers. Most of the other genera are lianous and a small
number are shrubs.
Little information is available on the pollen morphology
of the Periplocaceae. Schill & Jakel (1978) investigated
representatives of the following Periplocaceae in their
study on the pollinaria of the Asclepiadaceae: Crypto-
stegia R. Br., Ectadiopsis Benth., Hemidesmus R. Br.,
Omphalogonus Baill., Parquetina Baill. , Periploca L.,
* Department of Botany and Genetics, University of the Orange Free
State, RO. Box 339, Bloemfontein 9300.
MS. received: 1992-08-21.
Raphionacme, Tacazzea Decne. and Zygostelma Benth.
Data on tetrad size and number of pores for nine collec-
tions of Raphionacme, three species of Periploca, two
species of Tacazzea, and one species of Cryptostegia,
Ectadiopsis, Hemidesmus , Omphalogonus, Parquetina and
Zygostelma are also given. Lebrun et al. (1984) in their
identification of Raphionacme bingeri (A. Chev.) Lebrun
& Stork, give SEM results on seven Raphionacme species.
Verhoeven & Venter (1988) have examined the pollen of
35 Raphionacme species; Verhoeven et al. (1989), five
Tacazzea species and the monotypic genus Petopentia
Bullock; and Venter et al. (1990) three species of Ectadium
E. Mey.
In the present study pollen of Curroria Planch., Mondia
Skeels, Stomatostemma N.E. Br. and Socotranthus Kuntze
was examined with special reference to taxonomy. This
paper thus constitutes part of a comprehensive palynologi-
cal investigation and taxonomic revision of the African taxa
of the Periplocaceae currently being undertaken by the
authors.
Taxonomic aspects and distribution of genera
Curroria comprises five species. C. decidua Planch, is
divided into three subspecies (Bullock 1953). With the
exception of C. decidua subsp. decidua which occurs in
southwestern Africa (Angola, Namibia and South Africa),
all the other Curroria species and subspecies occur in the
desert areas of east and northeast Africa (Tanzania, Kenya,
Somalia, Ethiopia, with outlying stations in the
Hadramawt and Socotra) (Bullock 1953). Curroria species
are robust, erect shrubs or scramblers. The linear to
spathulate leaves are borne in clusters on short shoots and
opposite on long shoots. The petiole is absent or very
short. Flowers are solitary or occur as few-flowered cymes
in the axils of the leaves.
106
Bothalia 23,1 (1993)
Socotranthus is a monotypic genus. S. socotranus (Balf.
f.) Bullock is found on the island of Socotra (Suqutra) east
of the coast of Somalia. This is a large woody shrub of
arid habitats. Its suborbicular leaves are opposite and the
white flowers are grouped together in terminal cymes.
Mondia has two species, M. ecomuta (N.E. Br.) Bullock
and M. whitei (Hook, f.) Skeels. Both species are lianas
of moist forest in tropical and subtropical regions of
Africa. They both bear large, cordate leaves and many-
flowered axillary cymes. The flowers are showy, ranging
from yellowish to reddish in colour.
Stomatostemma also comprises two species, 5. mon-
teiroae (Oliv.) N.E. Br. and S. pendulina Venter & D.V.
Field. The first species is a climber with ovate leaves and
large cymes of whitish-purple flowers, whereas the latter
is a virgate shrub with linear leaves and large cymes of
white flowers. Both species occur in dry forest.
MATERIAL AND METHODS
Pollen was obtained from herbarium specimens. For
light microscopy (LM) pollen was acetolysed according
to the method of Erdtman (1960), mounted in glycerine
jelly and sealed with paraffin wax. Samples were examined
with a Zeiss Photomicroscope. Measurements of tetrad
size are based on a minimum of 15 tetrads per specimen.
For scanning electron microscopy (SEM), pollen was
acetolysed, air-dried on stubs, coated with gold and
examined with a Jeol Winsem 6400 microscope. For trans-
mission electron microscopy (TEM) fresh material was
used. Pollen carriers were fixed in 3% phosphate-buffered
glutaraldehyde, postfixed in 1% osmium tetroxide, dehy-
drated in ethyl alcohol and embedded in Spurr’s low-
viscosity resin. Sections were cut with a glass knife,
stained with uranyl acetate, followed by lead citrate, and
examined with a Philips 300 electron microscope at 60 kV.
Pollen specimens examined
Curroria brevifolia Balf. f., no material available.
C. decidua subsp. decidua Planch., Warmbad, Namibia, Mar. 1986,
Beukes 22 (BLFU); Mariental, Namibia, Sept.-Mar. 1959, Werdermann
& Oberdieck 2261 (K); Usakos, Namibia, Feb. 1969, Jensen 93 (WIND);
Ruacana Falls, Namibia, De Winter <6 Giess 7105 (WIND).
C. decidua subsp. gillettii (Hutch. & Bruce) Bullock, no material
available.
C. decidua subsp. volubilis (Balf. f.) Bullock, Kishen, Socotra, Aug.
1956, Gwynne 96 (BM).
C. macrophylla A.R. Smith, Abd al Kuri, Somalia, Oct. 1966, Virzo
A27 (K).
C. migiurtina (Chiov.) Bullock, no locality, no date, Collenette 198
(K); Eil, Somalia, Nov. 1986, Lavranos <& Carter et al. 24945 (K).
C. volubilis (Schltr.) Bullock, Yaida, Tanzania, Jan. 1970, Richards
25306 (K); Harrar, Ethiopia, Nov. 1970, De Wilde 7TJ9 (WAG); Nyambiti,
Tanzania, Mar. 1953, Tanner 1274 (BR).
Mondia ecomuta (N.E. Br.) Bullock, Pangani District, Tanzania, May
1950, Faulkner 558 (K); Kilifi District, Kenya, June 1973, Musyoki <&
Hansen 956 (K); Monyondzi, Congo, Nov. 1964, Bouquet 631 (P).
TABLE 1. — Diameter of pollen tetrads (/zm)
Bothalia 23,1 (1993)
107
FIGURE 1. — SEM of tetrads of species. A, Curroria volubilis, Richards 25306 (K), rhomboidal tetrad. B, C, C. decidua subsp. decidua'. B,
tetrahedral tetrad, De Winter & Giess 7105 (WIND); C, decussate tetrad, Beukes 22 (BLFU). D— F, Mondia whitei: D, rhomboidal tetrad.
Venter 9068 (BLFU); E, tetrahedral tetrad, Scheepers 1058 (PRU); F, decussate tetrad. Venter 9068 (BLFU). G— I, Stomatostemma monteiroae,
Pooley 293 (NU); G, rhomboidal tetrad; H, tetrahedral tetrad; I, decussate tetrad. Scale bars = 10 pm.
M. whitei (Hook, f.) Skeels, Duiwelskloof, South Africa, Nov. 1960,
Scheepers 1058 (PRU); Bloemfontein (glasshouse). South Africa, Dec.
1984, Venter 9068 (BLFU).
Socotranthus socotranus (Balf. f.) Bullock, Aola, Socotra, Mar. 1953,
Popov 275 (BM).
Stomatostemma monteiroae (Oliv.) N.E. Br., Josini, South Africa, Nov.
1983, Venter 8988 (BLFU); Umfolozi Game Reserve, South Africa, Dec.
1961, Ward 3921 (PRE); Ndumu Game Reserve, South Africa, Dec. 1968,
Pooley 293 (NU).
S. pendulina Venter & D.V. Field, Namina, Mozambique, July 1962,
Leach & Schelpe 11441 (K).
RESULTS
Pollen morphology
The pollen grains in the four genera are united in tetrads,
with the grains arranged rhomboidally (Figures 1A, D, G;
2A, D, G), tetrahedrally (Figures IB, E, H; 2B, E, H)
or decussately (Figures 1C, F, I; 2C, F, I; 3). The number
of pores of individual grains of the tetrads may vary, but
the morphology and position are the same for all the genera
investigated. The pores are round, oval or irregular and
are restricted to the junction area of adjacent grains. Pores
are sometimes covered with a thin layer of exine material.
Curroria
Pollen grains are arranged rhomboidally (Figures LA;
2A), tetrahedrally (Figures IB; 2B) or decussately (Figures
1C; 2C). In C. volubilis (Schltr.) Bullock the most com-
mon arrangement is rhomboidal, whereas in the other spe-
cies it is tetrahedral and decussate. Size of tetrads varies
from 27-42 x 22—34 pm (tetrahedral) to 34—55 x
24—33 pm (rhomboidal) (Table 1). Individual grains of
tetrads have 4—6 pores.
Mondia
Pollen grains are arranged rhomboidally (Figures
ID; 2D), tetrahedrally (Figures IE; 2E) or decussately
(Figures IF; 2F). Although rhomboidally arranged grains
are present, the most common arrangements are tetra-
hedral and decussate. Size of tetrads varies from 39-49
x 36—45 pm (tetrahedral) to 48—67 x 38-58
(rhomboidal) (Table 1). Individual grains of the tetrads
have 4-6 pores.
108
Bothalia 23,1 (1993)
FIGURE 2. — LM photographs of tetrads of species. A, Curroria volubilis, Richards 25306 (K), rhomboidal tetrad. B, C, C. decidua subsp. decidua,
Beukes 22 (BLFU): B, tetrahedral tetrad; C, decussate tetrad. D, E, Mondia ecomuta, Faulkner 558 (K); D, rhomboidal tetrad; E, tetra-
hedral tetrad. F, M. whitei. Venter 9068 (BLFU), decussate tetrad. G— I, Stomatostemma monteiroae: G, rhomboidal tetrad. Venter 8988
(BLFU); H, tetrahedral tetrad, Pooley 293 (NU); I, decussate tetrad, Pooley 293 (NU). Scale bars = 10 /im.
B
FIGURE 3. — Decussate tetrad of Soco-
tranthus socotranus, Popov 275
(BM). A, SEM; B, LM photo-
graph. Scale bars = 10 ^m.
Bothalia 23,1 (1993)
Socotranthus
Pollen grains are arranged decussately (Figure 3) or
tetrahedrally, very seldom rhomboidally. The decussate
arrangement differs from that observed in other genera,
in that the cells are arranged more parallel to each other
and not perpendicular. Size of tetrads varies from 28—36
x 22—27 /tm (tetrahedral) (Table 1). Individual grains of
the tetrads have 4-6 pores.
Stomatostemma
Pollen grains are arranged rhomboidally (Figures 1G;
2G), tetrahedrally (Figures 1H; 2H) or decussately
(Figures II; 21). The most common arrangements are tetra-
hedral and decussate. Size of tetrads varies from 29—58
x 27—54 fim (tetrahedral) to 39—61 x 28—51 pm (rhom-
boidal) (Table 1). Individual grains of the tetrads have 4—6
pores.
Exine structure
The exine is smooth and covered with a thin electron-
dense layer (Figure 4A, arrow). Exine structure con-
sists of an outer, homogeneous stratum (tectum) subtended
by a granular stratum (Figure 4B). The tectum and
granular stratum have the same electron density but the
granular stratum has an irregular appearance because of
channels which occur throughout it. The two layers are
separated by a discontinuous line of osmiophilic substance.
The fibrillar intine is well developed. The internal walls
have the same structure as the exterior wall. Wall bridges
consisting of intine and granular layer occur between
adjacent grains (Figure 4C). The intine wall bridges
indicate the position of pores in the internal wall of aceto-
lysed pollen grains.
DISCUSSION
Compound pollen grains occur in more than 56 families
of angiosperms (Erdtman 1945; Walker & Doyle 1975;
Knox & McConchie 1986). The cohesion mechanisms in
mature polyads were discussed by Knox & McConchie
(1986). The cohesion of compound pollen occurs by
attachment of the tectum (simple cohesion) or by connec-
ting wall bridges (cross-wall cohesion). In cross-wall
cohesion wall bridges are present in the common wall
between adjacent grains, and these bridges comprise intine
and granular layer in the Periplocaceae.
Pollen tetrads and polyads are common in a number of
families and have been used in systematic treatments to
separate genera and species (Oldfield 1959; Skvarla et al.
1975; Takahashi 1986). In the Mimosoideae extensive use
of tetrads and polyads is made to separate genera (Guinet
1981a, b; Niezgoda et al. 1983). In the Periplocaceae,
Raphionacme can be distinguished palynologically from
the other genera by the 8—16 pores per pollen grain
(Verhoeven & Venter 1988) as against 8— 10 in Baseonema
Schltr. & Rendle and 4—6 in the other genera. The mono-
typic Petopentia natalensis (Schltr.) Bullock can be
distinguished from the other genera by the presence of
linear and T-shaped tetrad arrangements (Verhoeven
et al. 1989). In Tacazzea, T. tomentosa Bruce differs
significantly from the other species by the width of the
rhomboidal tetrads (Verhoeven et al. 1989).
109
FIGURE 4. — A, B, TEM of pollen wall: A, Curroria decidua subsp.
decidua, Beukes 22 (BLFU); B, Mondia whitei, Venter 9068
(BLFU). C, M. whitei, Venter 9068 (BLFU), internal wall. G,
granular stratum; I, intine; T, tectum. Scale bars = 1 /an.
The present study shows that Stomatostemma pendulina
differs in tetrahedral size (32 x 30 /im) from S. motiteiroae
(48 x 47 /an). In Curroria, C. volubilis differs from the
other species in that rhomboidal tetrad arrangement is
predominant. Socotranthus can be identified by the un-
usual decussate arrangement of the tetrad.
110
Bothalia 23,1 (1993)
The exine structure, consisting of a solid stratum
(tectum) subtended by a granular stratum, appears to be
without much variation in the representatives of the Peri-
plocaceae studied thus far. The exine structure shows a
resemblance with the general exine structure in the Apocy-
naceae. In the Apocynaceae the granular stratum is
however, more variable, e.g. consisting of elements of un-
equal size and shape; subtended by a sole; larger granules
towards the base and partly fused to a sole; faintly defined
and delimited stratum with irregular voids containing
traces of osmiophilic material (Nilsson 1986; 1990).
Although small differences may occur, the pollen mor-
phology of the taxa investigated is rather uniform and thus
of little value in the distinction o> the species and genera
investigated. The different, predominantly rhomboidal
arrangement of the pollen tetrads of Curroria volubilis may
indicate that this species should be placed in a different
genus. It is significant that other floral characteristics show
that C. volubilis does not belong in Curroria or to any
of the genera investigated but to a new genus.
ACKNOWLEDGEMENTS
The financial support by the Foundation for Research
Development and the University of the Orange Free State
is gratefully acknowledged. All the herbaria mentioned
are thanked for the kind loan of their specimens.
REFERENCES
BULLOCK, A. A. 1953. Notes on African Asclepiadaceae. III. Kew
Bulletin 9: 360-362.
BULLOCK, A. A. 1957. Notes on African Asclepiadaceae. VIII. Kew
Bulletin 1956, 12: 503.
ERDTMAN, G. 1945. On the occurrence of tetrads and dyads. Svensk
Botanisk Tidskrift 39: 286-297.
ERDTMAN, G. 1960. The acetolysis method: a revised description.
Svensk Botanisk Tidskrift 54: 561—564.
GUINET, P. 1981a. Comparative account of pollen characters in the
Leguminosae. In R.M. Polhill & P.H. Raven, Advances in legume
systematics 2 : 789 —799. Royal Botanic Gardens, Kew.
GUINET, P. 1981b. Mimosoideae: the characters of their pollen grains.
In R.M. Polhill & R. H. Raven, Advances in legume systematics
2: 835 — 857. Royal Botanic Gardens, Kew.
KNOX, R.B. & McCONCHIE, C.A. 1986. Structure and function of
compound pollen. In S. Blackmore & I.K. Ferguson, Pollen and
spores: form and function : 265-282. Academic Press, London.
LEBRUN, J.P., NILSSON, S. & STORK, A.L. 1984. La veritable
identite du Brachystelma bingeri A. Chev. (Asclepiadaceae).
Bulletin du Museum national d’histoire nature lie, Paris 6:
225-231.
MILLER, A.G. & BIAGI, J.A. 1988. Studies in the flora of Arabia XXIII:
five new species from Oman. Notes from the Royal Botanic
Garden Edinburgh 45 : 61—72.
NIEZGODA, C.I., FEUER, S.M. & NEVLING, L.I. 1983. Pollen
ultrastructure of the tribe Ingeae (Mimosoideae: Leguminosae).
American Journal of Botany 70: 650—667.
NILSSON, S. 1986. The significance of pollen morphology in the
Apocynaceae. In S. Blackmore & I.K. Ferguson, Pollen and
spores: form and function : 359-374. Academic Press, London.
NILSSON, S. 1990. Taxonomic and evolutionary significance of pollen
in the Apocynaceae. Plant Systematics and Evolution, Suppl. 5:
91-102.
OLDFIELD, F. 1959. The pollen morphology of some of the west
European Ericales. Pollen et Spores 1: 19-48.
SCHILL, R. & JAKEL, U. 1978. Beitrag zur Kenntnis der Asclepia-
daceen-Pollinarien. Tropische und subtropische Pflanzenwelt 22:
1-122.
SCHLECHTER, R. 1924. Periplocaceae. In E. Rob & C.E. Fries,
Beitrage zur Kenntnis der Flora des Kenia, Mt Aberdare und Mt
Elgon, V. Notizblatt des Botanischen Gartens und Museums zu
Berlin-Dahlem 9: 23—24.
SKVARLA, J.J., RAVEN, P.H. & PRAGLOWSKI, I. 1975. The evolution
of pollen tetrads in Onagraceae. American Journal of Botany 62:
6-35.
TAKAHASHI, H. 1986. Pollen polyads and their variation in Chimaphila
(Pyrolaceae). Grana 25: 161—169.
VERHOEVEN, R.L. & VENTER, H.J.T. 1988. Pollen morphology of
Raphionacme (Periplocaceae). South African Journal of Botany
54: 123-132.
VERHOEVEN, R.L., VENTER, HJ.T. & KOTZE, I.D.S. 1989. Pollen
morphology of Petopentia and Tacazzea (Periplocaceae). South
African Journal of Botany 55 : 207—214.
VENTER, H.J.T. , KOTZE, J.D.S. & VERHOEVEN, R.L. 1990. A
taxonomic revision of Ectadium (Periplocaceae). South African
Journal of Botany 56: 113—124.
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Bothalia 23,1: 111-116 (1993)
Dynamics of the forest vegetation of the Umtiza Nature Reserve, East
London
J.J. MIDGLEY* and P.N. GOBETZ**
Keywords: dynamics, eastern Cape, forests, grain, size-class distribution
ABSTRACT
The forest community at the Umtiza Nature Reserve near East London was surveyed using 24 plots (0.04 ha) in which
all woody stems >0.5 m tall were enumerated. Based on a classification using numbers of stems of canopy species, it was
assumed that basically only one forest community was sampled. Further multivariate analyses suggest that this forest is
fine-grained. Sample plots were similarly placed in ordination space irrespective of whether woody species occurrence was
used as importance value or if species occurrence per size class was used separately [seedlings (0.5 — 1.0 m), saplings (1—5
m) or canopy individuals (>5 m)]. An analysis of size-class distributions of the most common canopy species indicated
that the majority of species exhibited inverse J-shaped size-class distributions. This is the expected pattern for a fine-grained
forest. In these measures of dynamics, this forest is not fundamentally different to the more temperate Afromontane forests.
UITTRJEKSEL
’n Opname is gemaak van die woudgemeenskap in die Umtiza- natuurreservaat naby Oos-Londen; alle houtagtige stamme
>0.5 m hoog is in aanmerking geneem. Gebaseer op ’n klassifikasie waarin aantal stamme van blaredakspesies gebruik
word, is daar aangeneem dat basies slegs een woudgemeenskap ingesluit is. Verdere veelvoudige variantanalises dui daarop
dat hierdie woud fyn gegrein is. Monsterpersele is eenders in ordinasieruimte geplaas ongeag of voorkoms van houtagtige
spesies as belangrikheidswaarde gebruik is en of voorkoms van spesies per grootteklas afsonderlik gebruik is [saailinge (0.5— 1.0
m), jong borne (1—5 m) of blaredak-individue (>5 m)]. Ontleding van grootteklas-verspreidings van die mees algemene
blaredakspesies het getoon dat die meeste spesies omgekeerde J-vormige grootteklas-verspreidings vertoon het. Dit is die
verwagte patroon vir 'n fyngrein-woud. In hierdie metings van dinamika, verskil hierdie woud nie fundamenteel van die
meer gematigde Afromontaanse woude nie.
INTRODUCTION
In brief, forest dynamics is the complex product of inter-
actions between disturbance regime (e.g. type of disturb-
ance, turnover rate), life histories of constituent species
along a shade-tolerant to shade-intolerant continuum and
particulars of the regeneration arena (e.g. regeneration bot-
tlenecks due to biotic or abiotic events) . As such the study
of dynamics needs several inputs. In this preliminary study
we concentrated on aspects of the grain and life history
components of dynamics. By life histories we mean
whether a species is relatively shade-tolerant ‘climax’ or
shade-intolerant ‘pioneer’ and this we have inferred from
size-class distributions.
By grain we mean ‘the mosaic of structural phases’
(Whitmore 1989); or the spatial patterns of seedlings/
saplings and canopy individuals of the different species.
Coarse-grained forests tend to have at least some (recently
disturbed) areas which are dominated by shade-intolerant
species. When plotted in ordination space, coarse-grained
forests should show clear separation of plots according to
whether pioneers or climax species are present, especially
when their sizes are considered. In fine-grained forests
most species can regenerate close to adults and therefore
there are no great differences in species composition or
size-class distributions amongst plots. In other words
* Division of Forest Science and Technology, Jonkershoek FRC, Private
Bag X5011, Stellenbosch 7600.
** Cape Provincial Administration, Umtiza Nature Reserve, PO. Box
5185, Greenfields 5208— deceased 11 February 1992.
MS. received: 1991-12-09.
the successional process occurs on a small spatial scale
in fine-grained forests.
Recent work has shown that in many different forests
at any one time gaps occupy about 1—2% of the area
(Barden 1989; Connell 1989). In forests not subject to
catastrophes these values suggest that stems in the small
size classes of shade-intolerant species should be rare in
comparison to the large bank of advance regeneration of
shade-tolerant species. Thus the size-class distributions
of shade-intolerant species should be flatter than those of
shade-tolerant species. A forest comprised of many species
with relatively flat size-class distributions should thus be
a relatively coarse-grained forest.
Very little has been published on the dynamics of South
African forests. At the moment there is therefore no model
to predict the grain of a South African forest either for
a given environment (e.g. climate and soils) or for forest
structure (e.g. whether there is a preponderance of large
or small-sized individuals). Midgley et al. (1990) indicated
that the southern Cape forests [part of White’s (1983)
Afromontane Forest type] were extremely fine-grained.
At the scale of 0.04 ha plots, most species were able
to recruit continuously and most canopy species were
shade-tolerant. This was interpreted as being due to the
unproductive environment (cool climate, poor soils) and
conservative disturbance regime (few large gaps) which
has favoured shade-tolerant species and restrained both
woody and herbaceous shade-intolerant species.
In contrast to the southern Cape forests, our working
hypothesis for tropical and subtropical gap-phase forests.
112
Bothalia 23,1 (1993)
such as are found at our study site, is that they can be
expected to have a greater component of shade-intolerant
species, of both herbaceous and woody types. This is due
to their situation in a more productive environment (higher
temperatures, summer rainfall) which increases the
opportunities for regeneration of fast-growing pioneer
species. Such forests should therefore be more coarse-
grained due to intermittent recruitment of shade-intolerant
canopy dominants leading to spatially segregated size
classes. Thus an ordination or classification of sample plots
using the occurrence of a species in the seedling, sapling
or canopy size classes, should reveal spatially distinct
groups in a coarse-grained forest. In a fine-grained forest,
where species are able to regenerate close to their own
adults, data of species occurrence by size class should have
little influence on classifications or ordinations.
Our survey was done in a coastal forest of the eastern
Cape. According to Acock's (1988) classification these
forests appear to fall between the Coastal Tropical Forest
Type (Veld Type No. 1) and Valley Bushveld (Veld Type
No. 23). White (1983) mapped these forests as the
Tongaland-Pondoland Forest type and most recently they
have been mapped as Dune Thicket (Lubke, Tinley &
Cowling 1988). Information on forest dynamics in the
eastern Cape is conspicuous by its absence in the over-
view of vegetation in the eastern Cape by Lubke, Tinley
& Cowling (1988) and in Everard (1987).
Our objectives were to use information from plots to:
1, briefly describe the vegetation; 2, compare ordinations
of plots using information on presence/absence of potential
canopy species in the seedling, sapling or canopy layers,
to infer grain; and 3, analyse the size-class distributions
of the important species to infer their life histories.
STUDY AREA
The study area is situated in the Umtiza Nature Reserve
(33°02'S; 27°47'E) which is located on a northeast-facing
slope of the Buffalo River Valley, about 10 kilometres from
East London. Thicket/forest vegetation covers about 550
ha of the reserve. One of the aims of this reserve is to afford
high conservation status to two forest tree species: Umtiza
listeriana Sim, belonging to a monotypic genus of the
Fabaceae, and Buxus macowanii Oliv. , the box-wood much
exploited in the eastern Cape in the past.
Maximum altitude in the reserve is 180 m and many
streams dissect the area giving it a variety of aspects. The
geology of the area has been mapped as Beaufort Group
(Rust 1988) and the soils are mapped as weakly developed
soils on rock with black to brown clays and clay loams
(Hartmann 1988).
At East London, annual precipitation is 919.2 mm which
falls mainly in summer. Mean maximum and minimum
temperatures are 22.7°C and 14.0°C respectively. East
London is extremely windy (mean wind speed of 4.7 ms-1)
as opposed to Cape Town (4.0 ms1) and George
(2.5 ms1). (Climate information from Weather Bureau,
Pretoria.)
METHODS
Sampling
The broad vegetation communities of the Umtiza Nature
Reserve were mapped from aerial photographs and essen-
FIGURE 1. —The location of the 24 sample plots at the Umtiza Nature Reserve in the eastern Cape. The shaded-in areas represent Acacia karroo
grassland and the clear areas forest.
Bothalia 23,1 (1993)
113
TABLE 1.— A species list, based on 24 sample plots, of the forest
vegetation of the Umtiza Nature Reserve
tially two types were found to occur; an Acacia kar-
roo! grassland and a thicket/fores t type. A grid was placed
over a 1:10 000 map of the reserve and 24 sites were select-
ed at random in the forest communities (Figure 1). At each
site a square plot of 20 x 20 m was laid out and all woo-
dy plants >0.5 m tall were enumerated. These plots were
demarcated permanently for further studies on distur-
bance, mortality and growth. At each sample plot each
stem was allocated to one of three size classes: seedlings
(0.5— 1.0 m in height), saplings ( < 5 m in height) and cano-
py (>5 m). Stem diameter at breast height (dbh) was
measured for stems > 5 m. Identifications were made in
the Albany Herbarium, Grahamstown. Nomenclature fol-
lows Gibbs Russell etal. (1987). The forest canopy ranged
from 5— 8 m in height with an occasional emergent up to
15 m. At each plot, slope and aspect were noted and two
soil samples were taken for standard chemical analyses
by the Agricultural Research Institute at Dohne.
Analysis
Initially we classified the forest vegetation using the
multivariate package TWINSPAN (Hill 1979a), with
numbers of stems as the importance values and the default
settings of the package. In total about 60 species occurred
in the canopy (>5 m in height; Table 1) in our 24 plots.
By using species occurrence in seedling, sapling or canopy
levels as separate species, we could increase the apparent
number of ‘species’ to about 150 and the apparent number
of ‘plots’ to 72.
In the second part of this study we used multivariate
techniques to represent grain or succession in space.
Multivariate techniques have long been used for discerning
successional trends, e.g. Fox (1990) used community
trajectories in multivariate space to study mammal
succession over time. We made comparisons between
classifications and ordinations of plots but using the two
data sets (i.e. 60 spp. versus 150 ‘spp.’ and 24 versus 72
‘plots’). The eigenvalues produced by an ordination/classi-
fication give an indication of the variance explained
by an axis [low eigenvalue ( < 0.5) = poor separation of
samples]. The breadth of an ordination axis gives an
indication of the homogeneity amongst samples, with a
value of 400 (4 s.d.) indicating that species occurring at
one end of an axis are almost completely absent at the
other end (Hill 1979b). At this stage there are no rigorous
tests for comparing ordinations, although some progress
has been made (Grossman, Nickerson & Freeman 1991).
We merely visually inspected the package outputs for
114
Bothalia 23,1 (1993)
differences in eigenvalues and breadth of axes, for the
various classifications/ordinations we performed.
We also calculated the position of centroids for ordi-
nations of plots using presence/absence of canopy species
in seedlings, saplings and canopy size classes separately.
A meaningful successional trajectory would be indicated
by significant directional trend in ordination space as
defined by information from each size class.
Our expectations were that in a coarse-grained forest,
significantly different eigenvalues or breadth of axes would
result when data from each size class were used separately,
rather than when information about the canopy layer only,
was used. We expected centroids to be widely separated
in ordination space when species by size-class informa-
tion was incorporated.
For the second part of the study, the DECORANA
(DCA-option)/TWINSPAN packages (Hill 1979a, b) were
again used. Presence/absence (due to the great discrepan-
cies in numbers of stems amongst size classes) was used
as the importance value, and again we used the default
settings of the package.
RESULTS
Environmental data
Soil colours recorded included very dark brown, dark
red-brown, dark brown and brown-black, and soil texture
was sandy clay loam. The soils also had a relatively high
pH and calcium content (Table 2). Slopes were mostly gen-
tle and aspect was predominantly between 90° and 270°.
Vegetation description
Very little phytosociological data have been published
on the eastern Cape forests and thickets. Furthermore,
vegetation patterns are complex (see Acocks 1988). For
this reason we have appended an annotated species list
(Table 1). The maximum number of stems observed per
0.04 ha sample for the canopy size class was 74, for
seedlings it was 454 and for saplings 25. The maximum
number of seedlings per sample plot was high for the
following species: Ptaeroxylon obliquum (421), Buxus
macowanii (189) and Ilex mitis (256). Species richness per
0.04 ha of woody plants ranged from 13—36.
The separation of the forest into types, based on abun-
dance of canopy individuals, was weak (eigenvector =
TABLE 2. — Environmental information pertaining to the study area. For
slope and aspect classes, numbers represent numbers of plots.
Values in brackets indicate the variance
TABLE 3. —Sample plots belonging to first two groups, and associated
eigenvalues, produced by TW1NSPAN using presence/absence
data for canopy species (60 spp.) and canopy species in three
size classes separately (about 150 spp.)
0.376). Furthermore, axis 1 was only a maximum of 2.5
s.d. units broad and axis 2 only 2.3 s.d. units. This
probably reflects the overlapping distribution of the
common species and many rare species (Table 1). Down-
weighting for rare species made a negligible difference
in eigenvalues. We have taken this weak separation of types
and small spread in ordination space of the forest to
indicate that only one vegetation community was present.
Most of the canopy species are well represented in the
seedling and sapling (Table 1) size classes. Essentially
the forest is dominated by Ptaeroxylon obliquum, Harpe-
phyllum caff rum, Olea woodiana, Chaetacme aristata,
Umtiza listeriana and Buxus macowanii (see Table 1).
Vegetation dynamics
The groupings of samples produced at the first division
using 60 species (i.e. only canopy species) versus 150
species (i.e. canopy species per size class separately),
whilst having different orderings, were identical (Table 3)
and both had similar and small eigenvalues (0.26 compared
to 0.29). This indicates that species by size-class data do
not produce a different classification or a different sepa-
ration of samples.
The ordination using 72 ‘plots’ and the 60 canopy species
shows considerable overlap of the three size-class groups
(Figure 2A, B, C). This is clearly depicted by the similarity
of position of each centroid and their relatively close
proximity to the origin. There is no suggestion of orderly
directional trend of movement of centroids. This could
indicate that there is no consistent difference in succes-
sional status amongst plots. The spread along the first
ordination axis is narrow (about 3 s.d.) and the eigen-
vector was also small (0.279).
Size-class distribution
Most of the common canopy species have typical inverse
J-shaped size-class distributions (Table 4). To this group
could be added many of the less common species we
encountered but which had similar size-class distributions.
This includes species such as Maytenus heterophylla,
M. peduncularis, Cussonia spicata, Euclea natalensis,
Brachylaena elliptica and Olea capensis subsp. capensis.
DISCUSSION
We interpret the multivariate analysis to indicate that
this subtropical forest is fine-grained. This forest is there-
Bothalia 23,1 (1993
115
FIGURE 2. — Ordination diagrams using woody species in size classes: A, canopy; B, seedling; C, sapling. All 72 plots were ordinated together
but represented separately for clarity. The dots indicate the centroids. In A, samples 22 and 23 are superimposed.
TABLE 4. — Numbers of individuals per size class of the most common canopy species encountered in the Umtiza Nature Reserve
fore fairly similar to the more temperate southern Cape
forests (Midgley et al. 1990). Both have an abundance of
species with inverse J-shaped size-class distributions and
co-occurrence of different size classes within a species.
These results indicate that large-scale disturbances are not
important in determining community composition of both
these forest types.
From a conservation perspective, because the shifting
mosaic of structural phases (sensu Whitmore 1989) is
fine-grained (or stationary) at Umtiza, relatively small
patches of forest may be viable because most species can
regenerate on a small spatial scale. Obviously, other factors
need to be taken into account (edge effects, visits by
dispersers) to complete the picture. We predict that the
disturbance regime at Umtiza will be conservative (prepon-
derance of small gaps) and that advance regeneration will
inherit most gaps.
Finally, it is clear from this survey that Umtiza listeriana
and Buxus macowanii, the two species of special conser-
vation importance, are both abundant and apparently
regenerating adequately. They appear to be well conserved
in the Umtiza Reserve.
ACKNOWLEDGEMENTS
We thank D. MacDevette for initiating the project. Dept.
Water Affairs and Forestry for funding and D. Everard,
H. van Daalen and especially C. Geldenhuys and anony-
mous referees for comments on the manuscript and
Dominique du Toit for doing much of the sampling.
REFERENCES
ACOCKS, J.RH. 1988. Veld types of South Africa, 3rd edn. Memoirs
of the Botanical Survey of South Africa No. 57.
BARDEN, L.S. 1989. Repeatability in forest gap research studies in Great
Smoky Mountains. Ecology 70: 558, 559.
CONNELL, J.H. 1989. Some processes affecting the species composition
in forest gaps. Ecology 70: 560—562.
EVERARD, D.E. 1987. A classification of the subtropical thicket in the
eastern Cape, based on syntaxonomic and structural attributes.
South African Journal of Botany 53: 329—340.
FOX, B.J. 1990. Changes in the structure of mammal communities over
successional time scales. Oikos 59: 321—329.
GIBBS RUSSELL, G.E., WELMAN, W.G., RETIEF, E., IMMEL-
MAN, K.L., GERMISHUIZEN, G., PIENAAR, B.J., VAN
WYK, M., NICHOLAS, A., DE WET, C., MOGFORD, J.C.
& MULVENNA, J. 1987. List of species of southern African
plants, part 2, edn 2. Memoirs of the Botanical Survey of South
Africa No. 56.
GROSSMAN, G.D., NICKERSON. D. & FREEMAN, M.C. 1991.
Principal component analysis of assemblage structure data: utility
of tests based on eigenvalues. Ecology 72 : 341—347.
HARTMANN, M.O. 1988. The soils of the eastern Cape. In M.N. Bruton
& G.W. Gess, Towards an environmental plan for the eastern
Cape : 37—43. Rhodes University, Grahamstown.
HILL, M.O. 1979a. TWINSPAN—a fortran program for arranging
multivariate data in an ordered two-way table by classification
of the individuals and the attributes. Cornell University, Ithaca,
New York.
HILL, M.O. 1979b. DECORAN A — a fortran program for detrended
correspondence analysis and reciprocal averaging. Cornell
University, Ithaca, New York.
LUBKE, R.A., TINLEY, K.L. & COWLING, R.M. 1988. Vegetation
of the eastern Cape. In M.N. Bruton & F.W. Gess, Towards
an environmental plan for the eastern Cape: 68—87. Rhodes
University, Grahamstown.
MIDGLEY, J.J., SEYDACK, A., REYNELL, D. & MCKELLY, D.
1990. Fine-grain pattern of southern Cape plateau forests. Journal
of Vegetation Science 1: 539—546.
Bothalia 23,1 (1993)
RUST, l.C. 1988. The geology of the eastern Cape. In M.N. Bruton & WHITE, F. 1983. The vegetation of Africa. Unesco.
F.W. Gess, Towards an environmental plan for the eastern Cape: WHITMORE, T.C. 1989. Canopy gaps and the major groups of forest
12—23. Rhodes University, Grahamstown. trees. Ecology 70 : 536 - 538.
Bothalia 23,1: 117-127 (1993)
The vegetation of the northeastern Orange Free State, South Africa:
physical environment and plant communities of the Ea land type
H.C. ECKHARDT*, N. VAN ROOYEN* and G.J. BREDENKAMP*
Keywords: Braun-Blanquet method, classification, geology, Grassland Biome, land types, soils
ABSTRACT
The research was carried out in the Ea land type of the northeastern Orange Free State, with the objective of reclassifying
and refining Acocks’s veld types. TWINSPAN classification results were further refined by Braun-Blanquet procedures. The
100 releves distributed over the Ea land type resulted in the recognition of four major vegetation types which may be divided
into nine plant communities. The communities were hierarchically classified, described and ecologically interpreted.
DECORANA ordination was used to determine vegetation/environmental gradients and relationships.
UITTREKSEL
Navorsing is gedoen op die Ea-landtipe in die noordoostelike Oranje-Vrystaat met die doel om Acocks se veldtipes te
herklassifiseer en te verfyn. Die resultate van die TWINSPAN-klassifikasie is met behulp van Braun-Blanquetprosedures
verder verwerk. Die 100 releves wat oor die hele Ea-landtipe versprei is, het vier hoofplantegroeitipes opgelewer wat in
nege plantgemeenskappe onderverdeel kan word. Die gemeenskappe is hierargies geklassifiseer, beskryf en ekologies geln-
terpreteer. Plantegroei- en omgewingsgradiente is met behulp van DECORANA-ordening bepaal.
CONTENTS
Introduction 117
Study area 117
Geology 118
Physiography 119
Soils 119
Climate 120
Methods 120
Description of communities 121
1. Artemisia afra-Rhus dentata shrubland of the
slopes 121
1.1 Hyperthelia dissoluta— Eragrostis curvula shrub-
land of steep slopes 121
1.2 Hyparrhenia hirta—Diospyros lycioides shrub-
land of moderate slopes 121
2. Themeda triandra—Elionurus muticus grassland
of relatively dry undulating midslopes/plains 124
2.1 Elionurus muticus— Trachypogon spicatus grass-
land of relatively dry, rocky, shallow soils .. 124
Vernonia oligocephala— Trachypogon spica-
tus grassland of relatively dry, rocky, shal-
low soils 124
Harpochloa falx— Trachypogon spicatus grass-
land of relatively moist, rocky, shallow soils . . 124
2.2 Microchloa caffra- Elionurus muticus grassland
of relatively moist soils 124
Tristachya leucothrix— Elionurus muticus varia-
tion 124
Heteropogon contortus— Eragrostis plana varia-
tion 124
3. Themeda triandra— Eragrostis plana transitional
dry/wet grassland 124
4. Eragrostis plana— Eragrostis curvula wet/moist
grassland 124
* Department of Botany, University of Pretoria, Pretoria 0002.
MS. received: 1991-10-29.
4.1 Eragrostis curvula— Setaria sphacelata moist
grassland 125
4.2 Eragrostis plana— Paspalum distichum wet grass-
land 125
Ordination 125
Conclusion 125
Acknowledgements 127
References 127
INTRODUCTION
The Grassland Biome of South Africa covers approxi-
mately 27% of the country. As a result of intensive
agricultural practices and urbanization, together with in-
dustrialization, the deterioration of the grassland led to
concern amongst decision-makers, resulting in the launch
of the Grassland Biome Project (Mentis & Huntley 1982).
This project aims at developing a better knowledge and
understanding of the grasslands of South Africa to permit
efficient land-use planning, utilization, conservation and
management. To reach these goals, it is necessary to re-
classify Acocks’s (1988) Veld "types. This reclassification
means a more detailed identification, description and map-
ping of the present grassland types (Scheepers 1986). The
northeastern Orange Free State was identified as an area
for which little or no phytosociological data exist. This
study will also contribute to the syntaxonomic synthesis
presently being undertaken by the Botany Department of
the University of Pretoria (Bredenkamp et al. 1989; Kooij
1990; Fuls et al. 1992a, b; Bezuidenhout 1988).
STUDY AREA
The total study area is situated in the northeastern comer
of the Orange Free State, i.e. between 29° 00' and 29°
47' E longitude and 27° 00' and 28° 00' S latitude, bor-
dering Transvaal and Natal (Figure 1). It covers approxi-
mately 5 600 km2 and comprises five land types, namely
land types A, B, C, E and F (Land Type Survey Staff
1984), which can be further subdivided (Figure 2).
118
Bothalia 23,1 (1993)
FIGURE 1. — Map of South Africa indicating the total study area situated
in the Highveld Region.
One third of the area (184 000 ha) is covered by the Ea
land type which is dealt with in this report. The other land
types are to be discussed in detail in later papers. A land
type is an area which is uniform with respect to terrain
form, soil pattern and climate. Towns situated in the area
are Vrede and Memel (Land Type Survey Staff 1984).
According to Acocks (1988), the study area represents six
veld types: Patchy Highveld to Cymbopogon—Themeda
FIGURE 2.— Map indicating the distribution of the different land types
(Land Type Survey Staff 1984).
FIGURE 3. — The distribution of the different veld types within the total
study area according to Acocks (1988).
Veld Transition (No. 53), covering approximately 50% of
the total study area, is restricted to the northern and central
parts. The Highland Sourveld (No. 44) stretches along the
Natal border in the east. Smaller patches of Cymbopogon-
Themeda Veld (No. 48) and Highland Sourveld to
Cymbopogon—Themeda Veld Transition (No. 56) occur
in the southwestern and southern parts. The Turf High-
veld to Highland Sourveld Transition (No. 54) stretches
over the central eastern part, while one olated patch of
Southern Tall Grassveld (No. 65) occurs to the south of
Memel (Figure 3).
GEOLOGY
KAROO SEQUENCE
The Karoo Sequence occupies the total study area
(Figure 4). Two important groups which can be disting-
uished here, are the Ecca and Beaufort Groups. The
Clarens, Elliot and Molteno Formations are also part of
this sequence, but they are limited in extent.
Ecca Group
This group is restricted to the north and northeastern
parts of the study area, bordering Transvaal (Figure 4).
The Ecca Group can be subdivided into a Lower Ecca
sandstone and shale, a Middle Ecca shale, and an Upper
Ecca sandstone and shale [South African Committee for
Stratigraphy (SACS) 1980]. Ecca shales are in general dark
grey and carbonaceous. Ecca sandstone was deposited in
an aquatic environment.
Bothalia 23,1 (1993)
119
FIGURE 4. — The geology of the total study area (adapted from Dept,
of Mineral and Energy Affairs 1984).
Beaufort Group
The Beaufort Group covers more than 80% of the study
area. It can be subdivided into three subdivisions,
namely the Lower, Middle, and Upper Beaufort Beds. The
argillaceous rocks are massive or blocky weathered. The
mudstones are greenish grey, blue-grey or red. Cross-
bedded sandstones are common.
Clarens Formation
The Clarens Formation, previously known as Cave
Sandstone, is a massive, fine-grained rock type, which
reaches a thickness of up to hundreds of metres. Under
weathering conditions, this formation features fantastic
shapes in the form of pillars and caves. Exposed surfaces
are white or cream-coloured, whereas its base is pink or
deep red. A few isolated hills in the central and southern
part of the study area have the characteristic shapes of this
formation as described above. The main components are
subangular to rounded grains of quartz and subordinate
feldspar. The accumulation of sandstone is probably of
aeolian origin, being re-arranged later by flowing water
(Du Toil 1954).
Elliot Formation
Molteno Formation
This formation is distinguished by the typical grey and
blue colouration of the shales, and the coarse grain and
‘sparkling’ appearance of the dominating sandstones.
Between Harrismith and Memel the Molteno Formation
occurs only as a single thin grit, covered by the Elliot
Formation and underlain by the Beaufort Group (Du Toit
1954).
Alluvium, sand, calcrete
Alluvium and sand are more recent by-products of
erosion, most probably originating from the Beaufort
Group (pers. obs.). A narrow strip of these deposits,
together with calcrete, occurs in the Seekoeivlei area,
which is drained by the Klip River (Department of Mineral
and Energy Affairs 1984).
Dolerite
The dolerites intruded the sediments of the Karoo
Sequence during the last stages of the Drakensberg
volcanicity. These intrusions are either horizontal, evenly
inclined or undulating sheets (SACS 1980). The dolerite
dykes are restricted to the eastern part of the study area.
PHYSIOGRAPHY
The study area is part of the inland plateau region or
highveld (Figure 1) and consists of plains with moderate
relief to closed hills and mountains with moderate and high
relief (Kruger 1983; Mentis & Huntley 1982). The alti-
tude is between 1 500 and 2 000 m with some peaks
reaching heights of up to 2 200 m. There is a clear gradient
in the physiography of the area from south to north. Three
broad divisions can be distinguished.
The southern and eastern parts are characterized by
isolated hills and mountains with moderate and high relief.
The middle part is depicted by lowlands, hills and moun-
tains with a moderate to high relief. This part can further
be described as strongly undulating irregular land,
gradually changing over into plains with moderate relief.
These plains are slightly irregular, undulating, with
occasional hills scattered over the area. This region is most
suitable for cultivation purposes, whereas the rest of the
area is more suited to cattle farming.
The Drakensberg forms a clear watershed, separating
the tributaries of the Vaal River, west of the escarpment,
from the tributaries of the Tugela River, east of the
escarpment. The study area is situated in the catchment
area of the Vaal River. The Klip River is the main drainage
line into which several smaller rivers and spruits flow
(Figure 5). The northern part of the study area is mainly
drained by the Spruitsonderdrift and Kommandospruit,
which are both perennial streams. There is a gradual
flattening towards the north, resulting in less deeply incised
low to moderate undulating plains in the north. These are
in strong contrast to the deeply incised mountainous
southern part.
Purple and red mudstones and shales, together with red
sandstones and thick beds of yellow and white feldspathic
sandstones are characteristic of this formation (Du Toit
1954). It is well distinguished by its prevailing coloura-
tion as can be seen on the slopes of the few koppies in
the study area.
SOILS
According to Land Type Survey Staff (1984), the soils
are undifferentiated and can have one or more of either
vertic, melanic and red structured diagnostic horizons. The
names and descriptions of the different soil forms are
120
Bothalia 23,1 (1993)
TABLE 1.— The mean monthly temperatures and extreme temperatures (°C) for two weather stations closest to the study area
used according to the Soil Classification Working Group
(1991). The Glenrosa and Mispah Forms are restricted to
terrain units 1 and 2 and very often occur together to form
a complex. These soils are shallow ( < 200 mm) and have
a low clay content (15-20%) and are mostly not arable.
Terrain units 3 and 4 are characterized predominantly by
pedocutanic, lithocutanic and yellow-brown apedal B
horizons. Soils are relatively deep ( > 350 mm) and have
a higher clay content ( > 35%). Although the Ea land type
is generally more suitable for crop production than the
rest of the study area, large areas are non-arable because
of the high clay content of the soils. Terrain unit 5 is
characterized by either rock and alluvium or the vertic
Rensburg and Arcadia soil forms. The last two forms have
a high clay content (>55%) and are deep (>500 mm).
CLIMATE
Rainfall
The study area is situated in the summer rainfall zone
with an average annual rainfall of 750 mm. Precipitation
takes place mostly in the form of thunderstorms, between
November and March. Midsummer droughts occur
towards the end of December until middle of January
(Department of Agriculture and Water Supply 1986).
Rainfall data for weather stations at Frankfort and
Standerton are given in Figure 6 (Weather Bureau 1986).
Temperature
Mean annual maximum and minimum temperatures for
the period 1985—1990 and extreme temperatures recorded
at Frankfort and Standerton are given in Table 1. The frost
period extends from April to October, which means a frost-
free period of approximately 150 days a year (Weather
Bureau 1986).
METHODS
Releves were compiled in 100 stratified random sample
plots. Stratification was based on terrain units (De Beer
1988; Land Type Survey Staff 1984). Sampling of the
different terrain units was done on a subjective basis. Five
different topographical positions were distinguished,
namely 1 = crests, 2 = scarps, 3 = midslopes, 4 = foot-
slopes and 5 = valley bottoms, floodplains or drainage
lines (Land Type Survey Staff 1984). Minimum plot sizes
of 16 m2 are considered to be adequate for grassland
surveys (Scheepers 1975) . Nevertheless, it was decided to
fix the plots at 100 m2 because of the large scale on
which this survey was conducted, and to ensure that scarce,
possible diagnostic species were included. This
FIGURE 5. — The drainage of the total study area with the Klip River
as main drainage line.
Bothalia 23,1 (1993)
121
Frankfort (1499 m) 15,2 690
| [30] | | |
A I B D E
Standerton (1581 m) 15,0 705
[80-33]
FIGURE 6. — Climatic diagrams for two weather stations. A, station; B, height above sea level; C, duration of observations in years (indicates
temperature and precipitation respectively); D, mean annual temperature in °C; E, mean annual precipitation in mm; F, mean daily minimum
temperature (coldest month); G, lowest temperature recorded; H, mean daily maximum temperature (hottest month); I, highest temperature
recorded; J, mean daily temperature fluctuation; K, mean monthly temperature; L, mean monthly precipitation; M, dry season; N, wet
season; O, very wet season (mean monthly precipitation (>100 mm); P, cold season (mean daily minimum below 0°C); Q, month with
absolute minimum below 0°C; R, frost-free period (Weather Bureau 1986).
is essential for efficient Braun-Blanquet type data process-
ing and also in accordance with the aim of identifying areas
for possible conservation. The floristic composition in
each sample was determined by using the Braun-Blanquet
cover-abundance scale (Mueller-Dombois & Ellenberg
1974). In accordance with Werger (1973), scale-unit 2 was
divided as follows: A, covering 5—12% of the sample plot
area and; B, covering 13—25% of the sample area. Taxon
names conform to those of Gibbs Russell et al. (1985 &
1987). Structural classification was according to Edwards
(1983). The following habitat data were recorded in each
sample plot: geology, topography, terrain unit, slope and
aspect, rockiness, soil types and erosion.
To derive a first approximation of the vegetation types,
two-way indicator species analysis (TWINSPAN) (Hill
1979a) was applied. This was further refined by Braun-
Blanquet procedures (Behr & Bredenkamp 1988;
Bredenkamp et al. 1989). The results obtained are
presented in a phytosociological table (Table 2). Detrended
correspondence analysis (DECORANA) (Hill 1979b) was
applied to the floristic data set to determine vegetation
gradients and illustrate vegetation/environmental rela-
tionships.
DESCRIPTION OF COMMUNITIES
The Ea land type is characterized mainly by the con-
stant presence, mostly with high cover-abundance values
of Themeda triandra, and Eragrostis curvula and E. plana
(species group L, Table 2). The number of species
recorded in the releves varies between 15 and 25, with an
average of 19 species.
1. Artemisia afra—Rhus dentata shrubveld
This shrubveld is situated on moderate to steep scarps
(30° -90°) (terrain unit 2) facing rivers and streams
(Figure 7). Shallow, rocky soils of the Glenrosa and
Mispah Forms are typical of this terrain type (Figure 8).
The average rock size is more than 500 mm in diameter,
covering more than 20% of the surface. Clear signs of
erosion can be observed, which are ascribed mainly to
the steepness of the slopes. The utilization of the vegeta-
tion by dassies ( Procavia capensis Pallas 1766) is apparent
in some areas.
The vegetation is characterized by species group C
(Table 2) and the diagnostic species include the shrubs Ar-
temisia afra, Rhus dentata and Diospyros austro-africana.
Bidens pilosa and Hibiscus trionum are weeds and are
often associated with disturbed areas. Dominant woody
species are the diagnostic shrub species. Con-
spicuous and dominant grasses include Themeda triandra,
Eragrostis curvula and E. plana of species group L, and
Aristida congesta and A. junciformis of species group I
(Table 2). The herbaceous layer of terrain unit 2 is more
conspicuous and better developed than those of other
terrain units.
1.1 Hyperthelia dissoluta— Eragrostis curvula shrubveld
This shrubveld is situated on steeper (40° — 90°) slopes
and displays patches of bare soil with a relatively high
degree of erosion (Figures 7 & 8). Diagnostic species
include the dominant grass species Hyperthelia dissoluta ,
the forbs Clutia natalensis, Garuleum woodii, Sutera
polelensis, the xerophytic fern Pellaea calomelanos and
the grass Melica racemosa (species group A, Table 2).
Themeda triandra, Eragrostis curvula and E. plana are
among the most constantly present companion grass
species occurring in this community. An average of 15
species was recorded per sample plot.
1.2 Hyparrhenia hirta— Diospyros lycioides shrubveld
This shrubveld is characterized by species group B
(Table 2) and can be further distinguished from the
122
Bothalia 23,1 (1993)
TABLE 2. — Phvtosociological table of the vegetation of the Ea land type in the northeastern Orange Free State
Community number
3
4
1.1 1.2 2.1
2.2
2.1.1 2.1.2 2.2.1
2.2.2
4.1 4.2
Re I eve number
Species group A
Hyper the / / a disso/uta
C/utia nata / ens is
Garu / eum wood i i
So ter a pole! ens is
Pellaea ca / ome / a nos
Melica racemosa
Species group B
Hyparrheni a hirta
D i ospyros lye io ides
Zinnia peruviana
Grew i a occidental i s
Heteromorpha tr i fot iata
Pollichia campestris
Monsonia angust i f o / / a
Species group C
Bidens pi II os a
Artemisia af ra
Rhus dentata
Salvia re pens
D i ospyros austro-afr i cana
Commelina africana
H i bi scus tr i onum
Species group D
Trachypogon spicatus
Acalypha punctata
Striga bilabiata
Polygala hottentotta
Species group E
T ephros i a c a pens i s
Dicoma anomala
Rhus discolor
Hypoxis rigidula
Vernonia oligocephala
Indigofera hi laris
Species group F
Harpoch / oa falx
Tr i st achy a I eucothr ix
Vernonia nata / ens i s
00000 000000 00000000 00000000 000000000 000000000000000000000000000000000 000000000 00000000000000000 00010
11452 829927 75566654 23288609 949466911 478655573349821870289057513226714 349208630 77883173160003441 90305
10656 284806 70742162 56910083 577458697 003981212350712885351444949747981 189274646 35690628331237395 29503
I 1A5I
l+RA |
l+A H
IAR |
M +1
I R 1 I
I B | 334B4A |
13 4 | RB+3BR |
I Mill I
I A5 1 +
I 4 + |+R
I 1+M
I A3A433R IA3A4+ I
I 1 1111111 RBI A 1 |
1+1+ 111 R 1 RR | 1
I R 1 | RR | +
I + +111 I
+ 1 + 11 I 1
I R R +1
|1R 1 | R
Species group G
Eli onurus mu t icus
Heteropogon contortus
Eragrost i s c a pens is
Eragrost i s racemosa
Brachiaria serrata
He / ictotr i chon turgidu/um
Aristida diffusa
Crabbea acau/is
T r i choneura grand i g I umi s
Berkheya onopord i f o / / a
Species group H
He / ichrysum rugu I osum
M icroch I oa caffra
Hap / ocarpha scaposa
Anther i cum transvaa I ens i s
If toga g / omerata
Geigeria as per a
Sutera aurant i aca
D i g i tar i a eriantha
Species group I
Aristida bi partita
Berkheya p i nnat i f i da
Hermann i a depress a
Setaria sphace I ata
Halafrida dens i f / ora
Indigofera obscura
Cymbopogon p lur i nod i s
Aristida junc i form/' s
Aristida congest a
Oenothera tetraptera
So/anum pandur i forme
1R I 1 R
1+ I11++
R+ | 1
A | 1++R1A1
1 +R | +
11RI+1 +
I 11
I 1
RR R1RRR R ++RR| 1
| 1 +1 11 | A 1 1 1 + 1 + I+ 1 + 1 1 1 A | 111 ++ 11 1 1 1 R1 1 1 1 All 1 1 11 1++11I 1++1 + 1I+ 1 111 1
A+1 11 A+1 1 111+1
1111111 1 1 I
1 11 +1 11 1+
111 1
| 1 1 11RR
| 111 +
| 11 1 | 1 1 | + BI 1 |+
| R+ +| + ++ + |+ R R |
| 1 1 1 | 11111 1|11111 I 1
|1 11 1| + |+ A I ++A11
+|1+ I 1 1+ R I 11
111 | 1111111111 +| ++
| 11+11+1+ A+A 1 | +A
|+ 3 +1 14 3 A 1 A | + I 113A 1
| + 1R1 | 1 I 1++ I
|1+ I 1 R 1 I 1 RR I
+ | 1 1 1 1A 13 1
RR | 1 1 11 +
1 I 1 1 1 11+1
| 1 1 1 1 1 B+ 1
I +1
IB +1 1 11 ++1+RI 1 5++3
R1R 1 1 +1 + 1 +R+ | R++++
11 111 1 1 1 A 11 1 1| 11
1 R 1 1 1 11 +++ 5+ I 1
R1 1+++R + +1R 1 | + +++
1 1 1 1 1 111 HI
++ + 1 1 +A 1A B I + 1 1 1
331 BI A 313 1 |343
11+ABB11++ 1 | 3
+ 11
I
Species group J
Conyza sumatrens i s
Pseudognapha / ium ol i g and rum
Cynodon dactyl on
Paspalum d i / atatum
Eragrost i s micrantha
He / / chrysum dregeanum
Cepha / ar i a scab i os a
Species group K
Paspalum d / st i chum
Cyperus longus
Mari scus congestus
Bidens bi pi nnat a
Chenopod i um ambros i o ides
A r gyro / ob i um pauc i f I orum
Juncus exserptus
S i um repandum
Dev err a burchel lit
Gerber a ambigua
Cymbopogon excavatus
Cyperus marginatus
Diplachne fusca
Sc hoe nop I ectus dec i pi ens
I 1
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
R 1
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
RRR
| R 11 1+11 R
| 11 +++R1
j A+A+ 1
| R + R R
| 1 R 1R
| 1 1+ + 1 +
| A + 1 R
I 11 + 1
I 111+1
I AA |
1 I 1 + B 1 |
I +A+ |
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I
I 3B3 1
+ 1 134 I
I BI 1 I
I 11 I
Species group L
Themed a tr fa ndr a
Eragrost i s curvu/a
Eragrost i s plana
Conyza podocepha / a
1+ I++
I A3 1 3 1 +
I + 1 R 11 +
I + +1 1
+ 14131 I B 33BA31
A1 1 AA | A BA1 4 , . -
+ABI+R A+A I+1++111 31
+ 1 | R +
Bothalia 23,1 (1993)
123
1.1 Hyperthelia dissoluta-Eragrostis curvula shrubveld
1 . 2 Hyparrhenia hirta -Diospyros lycioides shrubveld
2.1.1 Vernonia oligoccphala-Trachvpogon spicatus grassland
2.1.2 Harpochloa falx-Trachypogon spicatus grassland
2.2.1 Tristachya leucothrix-Elionurus muticus variation
2.2.2 Heteropogon contortus-Eragrostis plana variation
3 Themeda triandra-Eragrostis plana grassland
4.1 Eragrostis curvula-Setaria sphacelata grassland
4.2 Eragrostis plana-Paspalum distichum grassland
FIGURE 7. —A schematic represen-
tation of the terrain units with
the associated plant communi-
ties identified in the Ea land
type.
1.1 1.2 2.1.1
2.1.2
2.2.1 2.2.2 3 4.1
4.2
FIGURE 8.— Hierarchical diagram to
indicate the prominent habitat
characteristics which are as-
sociated with the respective
plant communities.
124
Bothalia 23,1 (1993)
Hyperthelia dissoluta—Eragrostis curvula shrubveld by the
presence of conspicuous and constantly present grass
species of species group I (Table 2). Diagnostic species
include the tall and dominant grass species Hyparrhenia
hirta, the shrubs Diospyros lycioides, Grewia occidentalis
and Heteromorpha trifoliata and the weedy Zinnia
peruviana and Monsonia angustifolia (species group B,
Table 2). A further characteristic of this community is the
presence of serai and pioneer species listed in species
group I, for example the grasses Aristida junciformis,
A. congesta and A. bipartita. An average of 23 species
was recorded per sample plot.
2. Themeda triandra— Elionurus muticus grassland
This plant community is to a great extent similar to
grasslands described by Bezuidenhout (1988) and Kooij
(1990), except for the prominence of Eragrostis plana and
other species typical of the moister eastern grasslands of
the Orange Free State. This community compares well to
the Elionurus muticus— Themeda triandra alliance de-
scribed by Fuls et al. (1992a). This grassland type covers
more than 60% of the Ea land type enclosed by the study
area. A great diversity of soil forms occur, including
Mispah, Glenrosa, Mayo, Inhoek, Westleigh, Swartland,
Clovelly, Oakleaf, Glencoe, Bonheim and Arcadia. Soil
depth varies from 100 to more than 700 mm. Deeper soils
(>500 mm) display higher clay contents (35—55%). Most
of these soils have been ploughed, and cultivated lands re-
place this grassland community to a great extent (Figure 7) .
This grassland is characterized by species group G
(Table 2) and the diagnostic grass species are the
prominent and conspicuously present Elionurus muticus,
Heteropogon contort us, Eragrostis capensis, E. racemosa,
Brachiaria serrata, Helictotrichon turgidulum, Aristida
diffusa and Trichoneura grandiglumis. Diagnostic forbs
are Crabbea acaulis and Berkheya onopordifolia (Table
2). Other prominent species are Themeda triandra,
Eragrostis plana and E. curvula, while the asteraceous
forbs Helichrysum rugulosum and Berkheya pinnatifida
are conspicuously present.
2.1 Elionurus muticus— Trachypogon spicatus grassland
This grassland is situated on terrain unit 1 and the
higher-lying parts of terrain unit 3, with low to moderate
slopes (2°— 30°) (Figure 7). Soils are shallow ( < 300 mm)
(Figure 7) and have a relatively low clay content.
Species group D (Table 2) characterizes this grassland
and includes the diagnostic co-dominant grass species
Trachypogon spicatus, as well as the forbs Acalypha
punctata, Striga bilabiata and Polygala hottentotta (Table
2). Prominent species include Elionurus muticus, Themeda
triandra, and Eragrostis curvula.
Two variations can be distinguished, namely the
Vemonia oligocephala— Trachypogon spicatus variation
and the Harpochloa falx-Trachypogon spicatus variation.
These two variations are distinguished by the presence of
species groups E and F respectively (Table 2). No clear
differences in the habitat can be found to explain the
occurrences of the two variations, but soil moisture regime
seems to be decisive in the delimitation of the two
variations.
2.2 Microchloa caffra— Elionurus muticus grassland
This grassland covers the largest part of the Ea land type
within the study area with respect to the other plant
communities. It occurs on a wide range of soil types, for
example vertic Arcadia to orthic Glenrosa Forms. This
grassland occurs on crests, slopes and plains (Figure 7).
The terrain as a whole is gently undulating with slopes
of 0°-8°. Overgrazing, especially by sheep, often results
in patches of bare soil, which are prominent in this grass-
land. The reason for patch-overgrazing is the dispropor-
tionate utilization of the veld, resulting in patches being
over-utilized (Fuls 1992). These patches are gradually
retrograding until bare patches of soil develop.
This grassland is the typical form of the Themeda
triandra— Elionurus muticus grassland and is character-
ized by the presence of species group G and the absence
of species group D (Table 2). Dominant grass species
include Elionurus muticus, Heteropogon contortus,
Eragrostis curvula, Themeda triandra and Eragrostis
plana. The forb Helichrysum rugulosum is constantly
present but less conspicuous. An average of 20 species
was recorded per sample plot. Two variations can be
distinguished, the Tristachya leucothrix— Elionurus
muticus and Heteropogon contortus —Eragrostis plana
variations. The former is characterized by the presence
of species group F, and is further distinguished from the
other variation by a higher percentage surface rock and
lower soil moisture regime (Figure 8). The Heteropogon
contortus— Eragrostis plana variation is clearly dis-
tinguished by higher cover-abundance values for Eragrostis
curvula and E. plana (Table 2) , indicating a higher soil
moisture content with respect to the former variation.
3. Themeda triandra— Eragrostis plana dry /wet grassland
This grassland represents a transitional zone between
relatively dry and wet grasslands, separating the relatively
drier communities on the higher-lying terrain units from
the relatively moister communities on the lower-lying
terrain units (Figure 7). The soils are deep (>500 mm)
and moist (Figure 8). Overgrazing in this grassland can
be observed to a lesser extent in the form of bare soil
patches, but rather as dense patches of Eragrostis plana,
invading the disturbed areas.
The transitional grassland is differentiated by the
presence of species groups H and I, and the absence of
species group G (Table 2). No diagnostic species could
be identified for this grassland. The dominant species
include Eragrostis plana, Themeda triandra, Eragrostis
curvula and Aristida bipartita. The herbaceous layer is
not well developed and open and includes species such
as the forbs Helichrysum rugulosum and Berkheya
pinnatifida, indicating a degree of degradation. An average
of 15 species per sample plot was recorded, indicating a
decrease in species diversity with an increase in soil
moisture.
4. Eragrostis plana— Eragrostis curvula wet grassland
This grassland represents the vegetation falling within
moist to wet areas, including footslopes and drainage lines
(Figure 7). The areas adjacent to drainage lines, display
gentle slopes (0°— 5°) and subsequently show few signs
Bothalia 23,1 (1993)
125
of erosion. Rivers and streams in contrast, often used by
cattle and sheep as drinking places, frequently show
serious signs of erosion. Seasonal and perennial water pans
occur widely scattered over the area, often attracting a
variety of birds. These pans are also accessible to cattle
and sheep. Since most of the rivers and streams flow
throughout the year, they may be used by stock at any time.
This grassland is characterized by species group J (Table
2), and the diagnostic grass species are Paspalum dilata-
tion, Cynodon dactylon, Eragrostis micrantha , and the
forbs Conyza sumatrensis, Pseudognaphalium oligandrum,
Helichrysum dregeanum and Cephalaria scabiosa (Table
2). Two communities can be distinguished.
4.1 Eragrostis curvula— Setaria sphacelata moist grassland
This grassland represents the vegetation found in moist
areas adjacent to drainage lines, and is transitional to grass-
land (Figure 7). This is indicated by the presence of spe-
cies groups H and I, which are differential species for this
community. Soils are deep (>500 mm) and without any
surface rocks. These areas are not suitable for cultivation
due to the high clay content (>55%) of the soils. Cover-
abundance values for the diagnostic and dominant species
are relatively high, indicating a dense vegetation cover.
Conspicuous and constant species are the grasses
Eragrostis curvula, Aristida bipartita, Setaria sphacelata,
Theme da triandra and Eragrostis plana, as well as the
forbs Berkheya pinnatifida and Hermannia depressa (Table
2). An average of 17 species was recorded per sample plot.
4.2 Eragrostis plana— Paspalum distichum wet grassland
This grassland represents the vegetation found along
rivers, streams and pans (Figure 7). Riverbeds and
streambeds are degraded to a large extent, often displaying
bare rock surfaces and alluvium (Figure 8). Soils found
here are of the Rensburg Form, being deeper than 500
mm. Few widely spaced pans do occur in the area; they
are restricted to depressions. Trampling effects by cattle
and sheep are noticeable especially on the margins of these
pans, where the animals normally drink. The vegetation
in these marginal zones is clearly disturbed.
A decrease in species diversity can be observed, if the
species-richness of this community is compared with that
of other vegetation types. This grassland is characterized
by species group K (Table 2), and the diagnostic species
include the grasses Paspalum distichum, Cymbopogon
excavatus and Diplachne fusca, the herbs Cyperus
longus, Mariscus congestus, Bidens bipinnata, Chenopo-
dium ambrosioides , Argyrolobium pauciflorum, Juncus
exsertus, Sium repandum, Deverra burchellii, Gerbera
ambigua, Cyperus marginatus and Schoenoplectus
decipiens (Table 2). Other conspicuous species are the
grasses Eragrostis plana, Cynodon dactylon, Paspalum
dilatatum and Eragrostis micrantha, and the herbs Pseu-
dognaphalium oligandrum and Conyza sumatrensis.
The herbaceous layer is prominent, but not dominant
to the grass layer. The presence of species group K and
the simultaneous absence of species groups H and I dis-
tinguishes this community from the Eragrostis curx'ula —
Setaria sphacelata grassland. An average of only 13
species was recorded per sample plot.
ORDINATION
Figure 9 represents the distribution of all 100 releves
along the first and second axes of a DECORANA
ordination. No discontinuities are observed and by inspec-
tion it is clear that the vegetation communities are
distributed along a moisture/trophic gradient. This gradient
is extracted by the first axis of the DCA ordination.
McDonald (1987) found in his study on the vegetation of
the Swartboschkloof that soil moisture played a secondary
role next to the major role being played by soil geology.
In his study on the vegetation of the mire Northern
Kisselbergmosen, SE Norway, Okland (1990) found that
depth to the water table had a major influence on the dis-
tribution pattern of the vegetation . The communities found
under extreme conditions, namely the dryland and wet-
land communities, occur on the periphery of the diagram.
The dryland community is represented by the Artemisia
afra-Rhus dentata shrubveld, occurring on dry, sandy,
dystrophic soils to the top left of the diagram.
The wetland community, Eragrostis plana— Eragrostis
curvula grassland, occurs on wet, clayey, eutrophic soils
to the right of the diagram. The Themeda triandra—
Elionurus muticus and Themeda triandra— Eragrostis
plana grasslands are situated in an intermediate position.
No separation occurs in Figure 9, concerning the last two
grassland types. A gradient along the second axis can also
be observed. Communities at the top of the axis occur on
scarps and slopes, whereas the bottom part represent
communities occurring on undulating terrain.
Figure 10 represents an ordination of only the Themeda
triandra— Elionurus muticus grassland. The releves of
variations 2.2.1 and 2.2.2 are more or less situated to the
right of the releves of community 2.1. The fact that no
clear discontinuity can be observed emphasizes the in-
distinct, gradual change from dryland to wetland commu-
nities associated with the gradually undulating terrain.
Releves to the right of the diagram are situated on wetter
lower-lying bottomland areas with deep, clayey vertic soils.
The left part of the diagram represents drier higher-lying
areas with shallow, sandy orthic soils. No gradient can
be observed along the second axis.
CONCLUSION
The application of Braun-Blanquet procedures to refine
the results of the TWINSPAN classification was success-
ful. Four major vegetation types were identified, which
are further subdivided into nine plant communities. These
units do exist in practice and can be incorporated in veld
management programmes.
It is of the utmost importance that the farmer considers
each unit on its own and that management programmes
take into account the characteristics of each unit (see
Eckhardt et al. submitted). Communities, which are
considered as having conservation value, are those occur-
ring on steep slopes (40° — 90°) adjoining wet grass-
land communities. The Hyperthelia dissoluta— Eragrostis
curvula shrubveld and Eragrostis plana— Paspalum
126
Bothalia 23,1 (1993)
FIGURE 9. — A scatter diagram of the
ordination of the vegetation on
the Ea land type.
distichum grassland together form a complex in some
areas, which is worthwhile conserving. Some of these
areas are partly or totally inaccessible to cattle and sheep
and therefore still remain in a relatively undisturbed
state.
The results obtained by ordination (DECORANA)
indicate the response of vegetation types to different
environmental conditions. Moisture and trophic regimes
have a strong influence on the distribution of vegetation
types. A correlation between these two habitat factors and
the vegetation can be observed. The application of the
Braun-Blanquet method for the B, C and F land types
should result in the identification of many more vegeta-
tion units, since these land types appear to be heterogene-
ous with respect to their topography.
Axis 1
A Elionurus muticus-Trachypogon spicatus grassland (2.1)
□ Tristachya leucothrix-Elionurus muticus variation (2.2.1)
o Heteropogon contortus-Eragrostis plana variation (2.2.2)
FIGURE 10. — A scatter diagram of the
ordination of plant commu-
nity 2.
Bothalia 23,1 (1993)
127
If farmers are to benefit practically from the results
obtained in this study, it is advisable to bring to their
attention the diagram presented in Figure 8. This diagram
serves as an important key for the delimitation of vegeta-
tion types and habitat units, which are to be managed in
accordance with the characteristics of each.
ACKNOWLEDGEMENTS
The research was financially supported by the Depart-
ment of Environmental Affairs. Prof. G.K. Theron is
thanked for administration of finances. Special thanks to
Mrs M.S. Deutschlander for all her assistance during data
processing. The University of Pretoria is thanked for
providing facilities.
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classification of the Witwatersrand National Botanical Garden.
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BEZUIDENHOUT, H. 1988. 'n Plants osiologiese studie van die Mooi-
rivieropvangsgebied Transvaal. M.Sc. thesis, Potchefstroom
University for Higher Christian Education.
BREDENKAMP, G.J., JOUBERT, A.F. & BEZUIDENHOUT, H. 1989.
A reconnaissance survey of the vegetation of the plains in the
Potchefstroom-Fochville-Parys area. South African Journal of
Botany 55: 199—206.
DE BEER, A.S. 1988. Plantspesievoorkeure van vleisbeeste in die
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Bothalia 23,1: 129-151 (1993)
The vegetation of the southern Langeberg, Cape Province. 1. The plant
communities of the Boosmansbos Wilderness Area
D. J. MCDONALD*
Keywords: classification, forest, fynbos, Langeberg. phytosociology
ABSTRACT
An analysis of the fynbos shrublands and forests of the Boosmansbos Wilderness Area, southern Langeberg, Cape Province,
South Africa, is presented. Data were collected at 119 sites in mature fynbos vegetation (>10 years old) and at five sites
in patches of Afromontane Forest. Emphasis was placed on the fynbos shrublands and sample sites were subjectively located
along a transect from south to north across the Langeberg range in the study area. This south to north orientation follows
a complex gradient of changes in aspect, slope, geology, soil form and climate. Data were initially analysed using TWINSPAN
and the resulting classification refined using Braun -Blanquet procedures. One forest subassociation and 12 fynbos communities
were identified and described. A proposed hierarchical classification of the fynbos communities is presented.
UITTREKSEL
’n Analise van die fynbos en woude van die Boosmansbos Wildernisgebied, suidelike Langeberge, Kaapprovinsie, Suid-
Afrika, word aangebied. Data is van 119 monsterpersele in volwasse fynbosplantegroei (> 10 jaar oud) en vyf monsterper-
sele in Afro-montane woude versamel. Klem is op die fynbosstruikveld gele en monsterpersele is subjektief langs 'n transek
van suid na noord oor die Langeberge in die studiegebied uitgele. Die suid tot noord orientasie volg ’n komplekse gradient
van veranderings in aspek, helling, geologie, grondform en klimaat. Data is aanvanklik d.m.v TWINSPAN ontleed en die
resultaat met behulp van Braun-Blanquet-prosedures verfyn. Een woudsubassosiasie en 12 fynbosgemeenskappe is geidentifiseer
en beskryf. ’n Hierargiese klassifikasie van die fynbosgemeenskappe word voorgestel.
CONTENTS
Introduction 129
Study area 130
Location 130
Physiography 130
Geology 131
Soils 131
Climate 132
Methods 133
Vegetation 133
Afromontane Forest 137
Fynbos 137
1. Erica hispidula Shrublands 139
1.1 Erica hispidula— Spatalla nubicola Shrub-
lands (A) 139
1.2 Erica hispidula— Restio inconspicuus Shrub-
lands 139
1.2.1 Restio inconspicuus— Anthochortus crinalis
Shrublands (B) 140
1.2.2 Restio inconspicuus— Protea grandiceps
Shrublands (C) 141
1.2.3 Restio inconspicuus— Protea aurea subsp.
aurea Shrublands (D) 141
1.2.4 Restio inconspicuus— Hypodiscus aristatus
Shrublands (I) 142
1.2. 4.1 Hypodiscus aristatus— Leucadendron
eucalyptifolium Shrublands (E) 142
1.2. 4. 2 Hypodiscus aristatus— Berzelia inter-
media Shrublands 144
1.2. 4. 2.1 Berzelia intermedia— Erica melanthera
Shrublands (F) 144
* National Botanical Institute, P.O. Box 471, Stellenbosch 7599.
Present address: Conservation Biology Unit, NBI Kirstenbosch, Private
Bag X7, Claremont 7735.
MS. received: 1992-03-20.
1.2. 4. 2. 2 Berzelia intermedia— Erica blenna var.
blenna Shrublands (G) 144
1.2. 4. 3 Hypodiscus aristatus— Erica versicolor
Shrublands (H) 145
2. Cannomois parviflora Shrublands 146
2.1 Cannomois parviflora— Leucadendron euca-
lyptifolium Shrublands 146
2.1.1 Leucadendron eucalyptifolium— Protea
lorifolia Shrublands (J) 146
2.1.2 Leucadendron eucalyptifolium— Staberoha
cemua Shrublands (K) 147
2.2. Cannomois parviflora— Passerina obtusi-
folia Shrublands 148
2.2.1 Passerina obtusifolia—Leucospermum
calligerum Shrublands (L) 148
2.2.2 Cannomois parviflora— Passerina obtusi-
folia Shrublands ‘Typicum’ (M) 149
Discussion and conclusions 149
Acknowledgements 150
References 150
INTRODUCTION
The position of the Langeberg on the west-east axis of
the Cape Fold Belt places it between the mountains of
the southwestern Cape and those of the southern Cape
(Figure 1). It therefore forms an important highland
phytogeographical link between the montane floras of these
respective regions.
The southern Langeberg is defined as the Langeberg
Range between Kogmanskloof and the Gouritz River. The
description and classification of the plant communities of
the Boosmansbos Wilderness Area presented in this paper
form part of a broad-scale phytosociological study of the
southern Langeberg.
130
Bothalia 23,1 (1993)
FIGURE 1. — Map of the mountains of the Fynbos Biome showing the position of the Langeberg and the location of the Boosmansbos Wilderness
Area (BWA): B, Barrydale; C, Cape Town; G, George; H, Heidelberg; M, Mossel Bay; P, Port Elizabeth; R, Riversdale; S, Swellendam
and W, Worcester.
Separate papers cover the description and classification
of the vegetation of two other similar transects at Swellen-
dam and Bergfontein (near the Gouritz River) (McDonald
1993a & b).
STUDY AREA
Location
The Boosmansbos Wilderness Area (BWA) near Heidel-
berg, Cape Province, is more or less centrally situated in
the southern Langeberg and extends across its widest part
(13 km). The area forms part of the Grootvadersbosch State
Forest and was proclaimed a wilderness area in 1978. The
mountain catchments are managed for conservation,
limited -access recreational hiking and production of
potable water. The Duivenhoks River has its origins in
these catchments.
The BWA is approximately 14 200 ha in extent. It is
bounded on the south side by agricultural land, on the
north side by a private nature reserve and on the west and
east sides by privately owned mountain land.
An access road, the Barend Koen Road, traverses the
area from the lower south slopes, adjoining the farm
Goedehoop, to Helderfontein at 1 150 m. The road is used
for management and forms part of the hiking trail network
in the area. During this study the road and paths gave ready
access to the area for sampling purposes.
The transect was arbitrarily delimited through the centre
of the BWA, straddling the Barend Koen Road on the south
slopes and the path to Witbooisrivier on the north slopes.
It does not follow a straight line over the mountain range
but was positioned to cover as much topographical varia-
tion and plant community variation as possible. The
transect area was approximately 3 000 ha.
Physiography
The southern plateau-like footslopes of the Langeberg
in the BWA are deeply incised by the Duivenhoks River.
At higher elevations, fault valleys such as Vaalrivierkloof,
Bobbejaankloof, Platbosrivierkloof and Saagkuilkloof,
which feed the Duivenhoks River, are encountered. Saag-
kuilkloof and Platbosrivierkloof fall within the delimited
transect and have north- and south-facing slopes. North
of Platbosrivierkloof is Repeater Kop, a high west-east
ridge lying approximately between Vaalrivierkloof and
Helderfontein. Behind (north of) Repeater Kop is the
Helderfontein Valley and north of that a high ridge runs
westwards from Grootberg. The Moeras River and
Helderfontein Stream start at the watershed behind
Repeater Kop. Moeras River drains northwestwards
towards Barrydale. Grootberg is the highest peak (1 627
m) in BWA and directly below it is the deep Boosmans-
bos Valley. The stream from Helderfontein runs through
this valley, through a gorge below Noukrans Peak (1 443
m) and Horingberg (1 487 m) to join the Duivenhoks River
outside the wilderness area.
North of Grootberg is a series of sandstone ridges with
interspersed shallow valleys. There is one main, relatively
broad valley with a shallow gradient eastwards towards
Brandrivier. North of the valley is Deception Ridge, so
named because of its deceptive height. The north slopes
of Deception Ridge are steep and rocky, giving way lower
down to mesa-like plateaux of gravels and sandstone
conglomerate (see below).
Bothalia 23,1 (1993)
Geology
The Langeberg is one of the west-east trending mountain
ranges with northward-verging folds, in the eastern zone
of the Cape Fold Belt. It consists mainly of sediments of
the Table Mountain Group (Cape Supergroup) and in part,
of pre-Cape Malmesbury Group sediments. The range was
formed during the Cape orogeny when the rocks of the
Cape Supergroup were folded in a single phase, multiple
event orogeny of Permian to Late Triassic age (De Villiers
1944; Halbich et al. 1983). The core of folding in the
Langeberg is at Tradouw Pass where the massive folding
has resulted in what Le Roux (1974) describes as the
Langeberg megastructure.
A transect over the Langeberg at any given locality has
its own peculiar local geology owing to folding, faulting
and consequent positioning of strata and fault valleys. Only
one detailed geological study of a section of the Lange-
berg exists (Le Roux 1974, 1983). Fortuitously this
coincides in part with the area proclaimed as BWA and
with the vegetation sampling transect chosen for this study.
Five formations of the Table Mountain Group are found
in the study area. The Peninsula Formation sandstone
makes up the southern slopes from about 400—1 600 m
a.s.l. At 1 150 m the Cedarberg Formation is represented
by a relatively thin band of shale in the vicinity of
Helderfontein. It is deeply incised and eroded at the
headwaters of the Moeras and Duivenhoks Rivers.
North of the Cedarberg Formation are the sandstone
sediments of the Nardouw Subgroup comprising the
Goudini, Rietvlei and Skurweberg Formations. For the
purposes of this study, the Nardouw Subgroup is equated
with the Peninsula and Cedarberg formations since the
finer distinctions are of secondary importance. Nardouw
Subgroup sandstone is also found on the south side of the
mountain between Tradouws Pass and Grootvadersbosch
Forest Station, Ertjiesvleiberg and in a narrow band
eastwards from below Horingberg to beyond Palmyra (Le
Roux 1974, 1983). However, Nardouw sandstones were
not encountered on the south side of the range on the
vegetation transect as designated in BWA.
Above Witbooisrivier, on the north side of the transect,
high terrace gravels are found (Lenz 1957; Le Roux 1974).
These gravels are cemented by a siliceous matrix, forming
resistant silcrete caps or duricrusts (Schloms et al. 1983)
and are remnants of the African Erosion Surface (Partridge
& Maud 1987).
Gravels of the Enon Formation are found at the southern
extremity of the vegetation transect. Le Roux (1974)
described the Enon sediments as ‘weakly consolidated
gravels and mudstones in alternating strata ... composed
of vein quartz, quartzite (derived from the Table Moun-
tain Group), greenish sandstones and shales (apparently
from the Bokkeveld Group), as well as conglomerates
older than the Enon Formation.’
Soils
The soils of BWA agree with the general pattern describ-
ed by Campbell (1983) for southern Cape coastal moun-
tains and the classification follows the system of the Soil
131
Classification Working Group (SCWG 1991). The soil
forms encountered, their positions in the landscape and
their relationship to the geological formations are outlined
below.
Oakleaf Form
Soils of this form have an orthic A-horizon over a diag-
nostic neocutanic B-horizon. The detailed definition of a
‘neocutanic’ horizon is given by SCWG (1991); briefly it
is a horizon derived from recent sediments and other un-
consolidated materials. It shows little colour differentia-
tion and weak structural development.
At low altitude (350 m), at the southern extremity of
the BWA vegetation transect, Oakleaf Form soils are
encountered. These soils result from the weathering of
Enon Formation sediments (see above). At one site (Releve
59) on the Cedarberg Formation shale at Helderfontein,
the soil was identified as Oakleaf Form. This soil has
formed by weathering of shale in a moist situation as
opposed to the formation of a Clovelly Form soil
(described below) under slightly drier conditions.
Cartref and Houwhoek Forms
Cartref and Houwhoek Form soils are found from low
(425 m) to high (1 600 m) elevations on south-facing
slopes, mainly on parent rock of the Peninsula Formation.
The form encountered at any position in the landscape is
dependent on the land facet (convexity or concavity), its
steepness and consequent drainage. The Houwhoek Form
soils display weak ferrihumic character in the B-horizon
and are very close to the more common Cartref Form soils
with lithocutanic B-horizons, showing no podzolization.
Champagne Form
Champagne Form soils are found at sites where drainage
is impeded and where deep accumulation of organic matter
has occurred. This soil form is typically found at ‘seeps’
where Restionaceae form dense, matted peat-like deposits.
On some of the high peaks (e.g. Grootberg, 1 627 m) and
ridges (Repeater Kop, 1 506 m) Champagne Form soils
are found on south aspects, on steep slopes. The slopes
have a mean gradient of 30° and organic material has
accumulated to an average depth of 700 mm. Podzoliza-
tion may occur in the parent rock beneath, but this would
presumably have little influence on the vegetation which
is rooted in the humus.
Mispah Form
At sites where bedrock is close to the surface and where
soil development is poor (due to a combination of excessive
drainage, high insolation, low organic matter accumula-
tion), Mispah Form soils with shallow orthic A-horizons
over hardrock are found. This form is found on the high-
altitude north-facing slopes of Repeater Kop ridge, Groot-
berg and on the terraced gravel-conglomerates above
Witbooisrivier.
Glenrosa Form
Soils of the Glenrosa Form are also found on the north
aspect of the ridges and peaks of BWA but on the middle
132
Bothalia 23,1 (1993)
to lower slopes. Here the form is diagnosed by presence
of Orthic A and Lithocutanic B-horizons. This form
typically occurs on the well-drained terraced ridges of the
Nardouw Subgroup strata north of Grootberg.
Clovelly Form
Clovelly Form soils are found at three different locali-
ties in BWA. These soils with a Yellow-Brown Apedal B
diagnostic horizon below an Orthic A-horizon have mainly
but not exclusively resulted from accumulation of trans-
ported material. The exception is on the Cedarberg
Formation shaleband near Helderfontein where the in
situ shale, with its fine-grained matrix has weathered to
Clovelly Form soils.
The south-facing slope of the ridge west of Grootberg
is a debris slope of Nardouw Subgroup sandstone. These
slopes which lie above the contact with the Cedarberg
Formation and which are moderately well-drained, exhibit
Clovelly Form soils (Releve 64).
In the eastward-trending intermontane valley north of
Grootberg, deposits of material eroded from Nardouw
Subgroup sandstones have given rise to we 11 -developed
Clovelly Form soils. These soils are well drained and in
one pit examined (Releve 130) pieces of reworked ferricrete
were found at 700 mm depth. On Deception Ridge (north-
most ridge on the transect), the south-facing terraced
slopes have a mixture of Clovelly and Glenrosa Forms
depending on the presence or absence of apedal and
lithocutanic B-horizons respectively.
Climate
Local climate of the Boosmansbos Wilderness Area is
poorly documented. A rainfall recording station is situated
at Grootvadersbosch Forest Station (Strawberry Hill),
however, this inadequately reflects rainfall as it occurs and
changes in the montane environment along the BWA
transect. The limited data available at best reflect low-
altitude conditions on the south slopes. Fuggle (1981) warns
of the dangers of interpolation between climatic stations.
However, since no climate measurements were made
during this study, limited available data from Weather
Bureau records (Strawberry Hill 025/599) and Fuggle
(1981) are used to obtain at least seasonal trends in climate.
Mean annual precipitation estimates were obtained from
isohyet maps prepared by Dent et al. (1987).
Wind
In summer the prevailing winds from the southeast and
southwest influence the Boosmansbos Wilderness Area the
most. The onshore, moisture-laden southeast winds are
trapped by the Langeberg and orographic rain occurs.
During the winter the winds blow primarily from the
northwest and southwest also bringing rain following cold
fronts. Berg winds occur in winter heralding the approach
of cold fronts (Fuggle & Ashton 1979; Fuggle 1981;
Heydorn & Tinley 1980; Tyson 1964, 1969).
Temperature
Temperature data for the study area are non-existent.
This situation is commonly found since few weather
stations are situated in the Cape mountains (Bond 1981;
Fuggle & Ashton 1979; Fuggle 1981). Temperatures in
STRAW. HILL (442 m)~K. RIVIER (192 m)
10 - - 20
Jul Aug Sep Oct Nov Dec Jan Feb Mar Apr Mav Jun
FIGURE 2.— Walter-Lieth climate diagram representing the climate
on the southern slopes of the Boosmansbos Wilderness Area.
Rainfall data from Strawberry Hill (Grootvadersbosch Forest
Station) and temperature data from the nearest station at
Karringmelksrivier, near Heidelberg.
mountain areas vary considerably from place to place;
therefore it is only possible to make generalized statements
about the effect of latitude and altitude on temperature
(Fuggle 1981.)
The nearest reliable temperature data are from Karring-
melksrivier (192 m a.s.l.) near Heidelberg, well away from
the BWA. However, these data are used to give general
trends in seasonal temperature variation. In Figure 2 they
are combined with rainfall data from Strawberry Hill to
give an approximation of the climate of the southern slopes
of the BWA.
Precipitation
Precipitation in the BWA occurs mostly as rain.
However, fog or mist from low stratus cloud plays a con-
siderable, but unmeasured, role in contributing to total
precipitation. Snowfalls occur in September, October and
occasionally November.
As for other climatic parameters, rainfall is not meas-
ured on a regular basis in the study area. It is clear from
observation that topography and aspect significantly affect
rainfall distribution. Interpolated data from Dent et al.
(1987) show that the lower south slopes of the study area
receive approximately 600 mm mean annual precipitation.
With an increase in altitude this value increases to almost
1 300 mm on the high peaks. The largest part of the study
area receives 1 000 mm precipitation on average each year.
With a decrease in altitude on the north slopes, bordering
the Little Karoo, a steep gradient exists, with the lower
slopes receiving less than 300 mm mean annual precipi-
tation (nearby Barrydale receives 276 mm p.a.; Fuggle
1981).
The seasonal distribution of rainfall on the south aspects
of the study area are reflected in the data from Strawberry
Hill weather station, and on the lower north slopes by data
from Klein Doornrivier, Figure 3. No month is without
rain but most rain falls in spring and autumn. Rainfall
results from post-frontal anticyclonic (onshore) air move-
ment over the subcontinent from August to November. In
the autumn months of March, April and May rainfall
results from the progression of cold fronts along the
Bothalia 23,1 (1993)
Month
FIGURE 3.— Mean monthly rainfall at Strawberry Hill (1978-1990) and
Klein Doomrivier (1982-1990) located at the lower south and
north extremes of the Boosmansbos sample transect respectively.
Rainfall peaks occur in spring (October) and autumn (April) at
Strawberry Hill and in autumn at Klein Doomrivier.
southern coast. Occasional cut-off lows occur which may
result in extensive rains (Van Heerden & Hurry 1987),
affecting rainfall over the Langeberg as well.
Solar radiation
No measured data are available for incoming solar
radiation on the slopes of the Langeberg. However,
estimates of incoming radiation will be obtained from the
RADSLOPE model (Schulze & Lambson, unpublished)
and presented in a later paper (McDonald, unpublished).
Bond (1981) calculated potential radiation for a range
of slopes and aspects for 33° 30' south latitude using
Swift’s (1976) algorithm. Incoming radiation in summer
was shown to be similar on all slopes and aspects, whereas
in winter steep north slopes receive the highest and steep
south slopes the lowest radiation. This is true for the
Langeberg, and since the range lies between 33° 30' and
34° South, Bond’s results could safely be extrapolated
here. Similar to the Outeniqua Mountains and the Swart-
berg, the Langeberg is also often capped with cloud,
further limiting incoming radiation, particularly on the
high-elevation south slopes.
METHODS
Methods employed in sampling the vegetation of Boos-
mansbos Wilderness Area follow those of McDonald
(1983, 1988) where rectangular plots of 5 x 10 (50 m2)
were used to sample fynbos shrublands; 5 x 10 m plots
are commonly used in surveys of fynbos (e.g. Boucher
1978; Bond 1981; Campbell 1985; Boucher 1987). The long
axis of each plot was oriented parallel with the contour,
with the plot being subdivided into 10 equal-sized subplots
to facilitate data recording.
In Afromontane forests circular plots with a radius of
11.3 m ( = 400 m2) were used to collect both floristic and
structural data (Geldenhuys et al. 1988; Knight 1989).
Only permanently recognizable species were recorded.
Geophytes such as Bobartia spp. were recorded and
included in the analyses. In general ‘ephemeral’ geophytes
and annuals encountered were noted but not used in the
analyses. The Braun-Blanquet (BB) cover-abundance scale
was applied as shown in Tables 1 & 2. The midpoint of
133
the BB values given as percentage cover is as follows:
5 = 87.5%; 4 = 62.5%; 3 - 37.5%; 2 = 15.0%; 1 =
2.5%; + =0.1%;R = value ignored (Mueller-Dombois
6 Ellenberg 1974; Werger 1974). A border zone of 1.5 m
from the perimeter of each plot was searched for any
species not found in the marked plot. Species occurring
outside the plot are represented by ‘O’ in the phytosocio-
logical tables. Structural data were collected where the
strata and their respective cover (BB scale) were recorded
at each sample site. The structural characters of stems (e.g.
woody, herbaceous) and leaves (e.g. simple, cupressoid,
sclerophyllous, leptophyllous) were also evaluated using
the BB scale.
TWINSPAN (Hill 1979) was used for initial analysis of
the floristic data. The classification was then refined
further by sorting the phytosociological tables with the aid
of PCTables (Boucher unpublished).
Boosmansbos Wilderness Area is the only area of the
Langeberg for which 1:20000 colour aerial photography
is available (Job 824). It was therefore possible to stratify
the study area, identify major land type/vegetation units
and predetermine general location of plot positions in these
units prior to fieldwork. Precise positions of sample plots
were subjectively determined with plots placed in stands
of mature fynbos ( > 10 years old).
Floristic composition of communities was compared
using diagnostic or character species of each community
as the main criteria. Those communities that were not
immediately obviously equivalent were subjectively judged
on the basis of character species, taxonomic relatedness
or morphological similarity e.g. Berzelia lanuginosa found
in the southwestern Cape versus B. intermedia found on
the Langeberg, in similar habitats. These relationships do
not reflect strict ‘synonymy’ but serve as a guide for future
synthesis of communities found in fynbos vegetation.
VEGETATION
Boosmansbos Wilderness Area is named after the well-
preserved Afromontane Forest patch in the deep ravine
below Grootberg Peak. There are a number of other
smaller patches of forest below Repeater Kop as well.
These forest patches represent one vegetation type of
limited extent in the study area. Shrubby fynbos covers
the greater proportion of BWA and is described in greater
detail.
Muir (1929) recognised three major categories of fynbos
in the Langeberg: 1, The Succession of Bare Rock Surfaces
and Cliffs; 2, The Sclerophyllous Vegetation of the
Langeberg; and 3, The Langeberg Forest and Mountain
Streams. In the present study emphasis is placed on the
Sclerophyllous Vegetation which Muir subdivided into (a)
Heath, (b) Macchia (c) (Vegetation of ...) Upper Southern
Slopes and Summit and (d) (Vegetation of ...) Northern
Slopes and Base.
The fynbos communities are described in the order of
the proposed classification. Each community is given a
species-binomial name which has no syntaxonomic
hierarchical rank (McDonald 1988). The communities are
placed in context in the Fynbos Biome (see Rutherford
& Westfall 1986) by attempting to relate them to commu-
nities described by other workers; based on both floristic
and structural similarities. The structural formation of each
134
Bothalia 23,1 (1993)
Table 1. A Dhytosociological table of the Erica hispidula Shrubland Communities south of Grootberg, Boosmansbos Wilderness Area, Langeberg
Relevb number
<'66778992*23333366778889992*6678*855556* 1688* 1111*111122222777* 123337889*223366792
*59089563*11346701470360120*2311*867894*13847*36890126*458905678356*457720599254*392867234
Altitude (m) .11111111,1111111111111111.1111.111111. 11, . . 1111111.111111111
.24412406.01211044610132451.2212,312112.33233.56643444.578877665566.586812100133.011022135
.89691660.58231633187341585.9384.021751.98193.13253278.160510474077.187511999581.995485804
.64362066.29842739286612448.5402.389389.61963.84575728.828361012006.841329270188.758200935
.12122122.111232222222211 1.1111.21 222,32 23.22121222,212111 11321.33 33 3 . 12
.81842921.92402621061 135498.6492,25852 1.09152.76705098.090288887 103.3325362 995 1 . 151 1 141 1
.05055055050250000.5005.000000.00050.05000000.500500500005.000500050355.050050557
Aspect
Bothalia 23,1 (1993)
135
Table 1. Cont.
Relev6 nunber * it 1* * t t t t t \
*66778992*23333366178889992*6678*855556* 1688* 1111*111122222777* 123337889*223366792
*59089563*11346701470360120*2311*867894*13847*36890126*458905678356*457720599254*392867234
Species connon to Connunitles (1.2.2 i 1.2.3)
136
Bothalia 23,1 (1993)
Table 1. Cont. ...
Re1ev6 number * It It t t t t t t i
*66778992*23333366778889992*6678*855556* 1688* 1111*111122222717* 123337889*223366792
*59089563*11346701470360120*2311*867894*13847*36890126*458905678356*457720599254*392867234
Bothalia 23,1 (1993) 137
'
Table 1. Cont . ...
Relevb number * 1 * 1* * * * * * » 1
*66778992*23333366778889992*6678*855556* 1688* 1 1 1 1*1 1 1 1222227??* 123337889*22336679 2
*59089563*11346701470360120*231 1*867894* 13847*368901 26*458905678356*457720599254*39286723 4
community is given following the system for the Fynbos
Biome proposed by Campbell et al. (1981).
Riparian communities were not sampled because they
form narrow ribbons along streams, and are restricted to
the streambanks. Typical dominants found in the non-forest
riparian communities are: Brachylaena neriifolia, Cuno-
nia capensis, Elegia capensis, Empleurum unicapsulare,
Laurophyllus capensis, Rapanea melanophloeos, Todea
barbara and Virgilia oroboides.
Afromontane Forest
The forest patches in the BWA are typical Afromontane
Forest. They are found in deep secluded gorges which are
cool and moist. These forests are floristically all of one
type, based on tree species composition. The Boosmans-
bos Forest tends to be much wetter than the other patches
sampled, shown by the high cover-abundance of Cyathea
capensis which favours such conditions. An apparently
drier-phase forest patch (Releve 122) is characterized by
Plectranthus fruticosus. However, this observation is at
variance with that of Muir (1929) who presented an early
general account of the ‘Langeberg Forest’ at Riversdale.
He maintained that P. fruticosus is strongly moisture
demanding. McKenzie (1978) gives detailed descriptions
of the Boosmansbos forests which he classified as the
Cunonia capensis— Platylophus trifoliatus Subassociation.
A number of ‘variations’ were distinguished within the
Subassociation according to relative wetness and dryness.
No additional information was recorded or change in the
classification proposed based on the five 400 m: plots
sampled in the present study. Structurally the forests are
classified as Wet High Forest (w-HF) following Gelden-
huys (1983). The canopy height varies from 20—30 m and
the species recorded, with synoptic Braun-Blanquet values
in parentheses, are as follows:
Trees: Cunonia capensis (5), Halleria lucida (4),
Hartogiella schinoides (2), Ilex mitis (2), Kiggelaria
africana (1), Maytenus acuminata (3), Ocotea bullata (4),
Olinia ventosa (1), Platylophus trifoliatus (4), Podocarpus
latifolius (2), Pterocelastrus rostratus (5), Rapanea
melanophloeos (5), Virgilia oroboides (3).
Shrubs: Diospyros whyteana (1), Plectranthus frutico-
sus (1).
Ferns: Asplenium adiantum-nigrum (2), Blechnum
giganteum (5), B. punctulatum (2), B. tabulare (2),
Cyathea capensis (5), Hymenophyllum tunbridgense (2),
Rumohra adiantiformis (1), Todea barbara (2).
Climbers: Myrsiphyllum scandens (3).
Herbs: Epischoenus adnatus (2), Galium undulatum (1),
Osmitopsis osmitoides (1), Peperomia retusa var. retusa
(1), Schoenoxiphium lanceum (5).
Epiphytes: Elaphoglossum angustatum (3), Microsori-
um ensiforme (4).
Geophytes: Oxalis purpurea (4).
Fynbos
The cool south slopes of the southern Langeberg are
covered with physiognomically uniform plant communi-
ties over large areas. The slopes are moist and may be
likened to an extensive seepage zone. Apart from Muir’s
(1929) classification the vegetation has been variously
referred to as: Wet Sclerophyll Bush (Adamson 1938);
Hygrophilous Macchia or Fynbos (Phillips 1931; Taylor
1978); False Macchia (Veld Type 70) by Acocks (1988);
Wet Mountain Fynbos (Moll et al. 1984) and Wet Erica-
ceous Fynbos (Campbell 1985). The apparent uniformity
is deceptive, however, with close examination showing that
the vegetation can be subdivided on species composition
into the eight shrubland communities described under ‘A’
below.
138 Bothalia 23,1 (1993)
TABLE 2. — A phytosociological table of the Cannomois parviflora Shrubland Communities north of Grootberg, Boosmansbos Wilderness Area, Langeberg
*2445555999000011*44400111*044000011*4455
*4792345789012334*12845012*234678956*5601
Altitude (m) .11111111111111 1.11111 1.
.0001013000001190.10010990.577477655.5579
.5993932679662073.38959880.904822999.9991
.8771786050001606. 42117550. 417577744.4424
Aspect (') .1 1 1111 2 1,111 1111. 31 I 3.2
.439343470921 097.99988997.8331 4121.2 33
.0000000550062605.06550650.550570000.0000
Releve No. *0000000000111111*00011111*000111111*0000
*2445555999000011*44400111*044000011*4455
*4792345789012334*12845012*234678956*5601
In the intermontane valley between Grootberg and
Deception Ridge (north of Grootberg) the vegetation has
a high cover of tall proteoid shrubs and fits the category
of Mesic Mountain Fynbos (Moll et al. 1984) or Dry
Proteoid Fynbos (Campbell 1985). On the north slopes
of Deception Ridge above Witbooisrivier the vegetation
resembles that of the inland ranges and is classified as Dry
Mountain Fynbos (Moll et al. 1984) or Dry Asteraceous
Fynbos (Campbell 1985).
Bothalia 23,1 (1993)
139
The most striking feature of the fynbos of the BWA is
the clear division between the vegetation of the southern
and northern sides of the mountain. Erica hispidula , a
common dominant on the south slopes, is almost com-
pletely absent on the north slopes. Although a number of
other species transgress the south-north boundary, for
example Leucadendron eucalyptifolium , it is clear that a
definite floristic distinction can be made between the
shrublands on the south and north sides of the mountain.
This distinction is reflected in the treatment of the data
from the respective areas in separate syntaxonomic tables
(Tables 1 & 2), where a hierarchical arrangement of com-
munities is also presented.
Using the default options, TWINSPAN clearly separated
the mesic to dry shrublands north of Grootberg from the
largely mesic to wet shrublands of the catchments south
of Grootberg at Level 1. This is reflected in the treatment
of the releves in two separate phytosociological tables
(Tables 1 & 2). Releves 41 and 48, however, were included
in Table 2, contrary to the TWINSPAN classification.
In the mesic to wet Erica hispidula Shrublands, TWIN-
SPAN separates those releves (except releves 31, 33, 34,
36 & 37) which correspond with the Erica hispidula—
Spatalla nubicola and the Restio inconspicuus— Anthochor-
tus crinalis Shrublands in the BB classification from the
remaining releves which constitute the Erica hispidula—
Restio inconspicuus Shrublands, at Level 2. Correlations
between the two classifications from TWINSPAN levels
3—6 are not good but show general similarities. Nine com-
munities are identified using the BB classification method,
whereas TWINSPAN separates the releves into 15 groups.
In the mesic to dry shrublands the distinction between
the Cannomois parviflora— Leucadendron eucalyptifolium
Shrublands and the C. parviflora- Passerina obtusifolia
Shrublands (see below and Table 2) correlates directly with
the separation indicated by the TWINSPAN classification
at Level 2. Correlation at lower levels (3—6) is not good.
The BB classification results in four communities being
identified, with further subdivision into 13 groups, as in-
dicated by TWINSPAN, considered to be too fine.
1. Erica hispidula Shrublands
Typical of the shrublands of the moist south-facing
slopes of the southern Langeberg is the ubiquitous shrub
Erica hispidula. This species is characteristic of much of
the mesic to wet ericaceous fynbos of the mountains of
the southwestern and southern Cape (Boucher 1978;
Kruger 1979; Bond 1981; McDonald 1988), and is there-
fore used as a descriptor for these shrublands.
In BWA E. hispidula is widespread and links the south-
slope shrublands floristically across physiognomic bounda-
ries, with Restio inconspicuus playing a subordinate role.
R. inconspicuus is absent only from the Erica hispidula—
Spatalla nubicola Community, a feature attributed to the
dense, waterlogged, humic substrate. R. inconspicuus in
turn, however, links all the communities falling under the
Erica hispidula— Restio inconspicuus Shrublands in the
classification. These shrublands are equivalent to the
Heathland, Mixed Sclerophyllous Scrub and Broad-
sclerophyllous Scrub communities of Kruger (1979).
1.1 Erica hispidula— Spatalla nubicola Shrublands (A)
Differential species: Spatalla nubicola, Helichrysum
capense.
Dominant species: Anthochortus crinalis, Brunia
alopecuroides, Platycaulos anceps.
Structural formation: Closed Restioland with Mid-high
Mid-dense Shrubland Overstorey.
Relationships: Brunia alopecuroides— Restio bifidus
Community (Kruger 1974); Subcommunity E2 of the
Erica— Penaea Community (Glyphis et al. 1978); Restio—
Hypolaena Subcommunity (H & I) (Laidler et al.
1978); Ericoid-Restioid Zone Fynbos (Taylor 1978); Low
Narrow-sclerophyllous Heathland (Kruger 1979);
Simocheilus carneus— Restio anceps Community (Bond
1981); Wet Mountain Fynbos (Moll et al. 1984); Ruiters-
berg Wet Ericaceous Fynbos (Campbell 1985); Erica
hispidula— Brunia alopecuroides Shrublands (McDonald
1993a).
This community (Figure 4) is found on the steep, cool,
moist southerly slopes of the BWA, mostly at altitudes
above 1 200 m. The community is found in the ‘mist zone’
where low stratus cloud commonly occurs around the high
ridges and peaks. Annual precipitation is estimated at 1 200
mm and insolation is generally low. There is a consequent
accumulation of organic material. Champagne Form soils
with a strongly acid organic horizon (pH 2.9 in 0.01 mol/1
CaCL) as deep as 700 mm in some cases, form the sub-
strate of this community.
These shrublands were sampled mainly on the south side
of the ridge of Repeater Kop (Releves 65, 69, 70, 78, 95
& 96), on Grootberg Summit (Releve 123) and on the
southwest side of the high ridge between Grootberg and
Horingberg (Releve 89).
Spatalla nubicola (Proteaceae) is endemic to this com-
munity whereas Helichrysum capense, the second differen-
tial species has a wider distribution, being found at other
localities in the Langeberg. Presence of at least one of these
species is necessary to determine this community. The
dominant species Brunia alopecuroides gives these shrub-
lands their characteristic 'brunioid' appearance. The B.
alopecuroides shrubs seldom exceed 1.2 m in height and
their closed canopy provides dense shade for the under-
storey restioid and ericoid elements. Anthochortus crinalis
and Platycaulos anceps (Restionaceae) dominate the dense
understorey stratum. Grasses are conspicuously lacking
and are only represented by Ehrharta setacea subsp.
scabra, a rare endemic in the fynbos biome (Gibbs Russell
et al. 1990), in some stands.
A population of the rare Spatalla colorata was found
in this community on the summit of Repeater Kop in close
proximity to an undescribed endemic Erica species. These
species apparently favour moist, high-altitude habitats with
highly leached soils.
1.2 Erica hispidula— Restio inconspicuus Shrublands
This community comprises all the shrublands apart from
the Erica hispidula— Spatalla nubicola Shrublands. Restio
inconspicuus and several prominent species, namely
140
Bothalia 23,1 (1993)
FIGURE 4. — Erica hispidula— Spatal-
la nubicola Shrublands on high
altitude, steep south-facing
slopes. Note the shrubby en-
demic S. nubicola next to the
range rod.
Tetraria cuspidata, Ehrharta dura, Erica melanthera and
others (see Table 1) are not found in the latter community.
The soils on which the Erica hispidula—Restio incon-
spicuus Shrublands occur are generally either more free-
ly drained, with less accumulation of organic material,
or are derived from non-sandstone substrates.
1.2.1 Restio inconspicuus—Anthochortus crinalis
Shrublands (B)
Differential species: none.
Dominant species: Anthochortus crinalis. Erica hispi-
dula, Ehrharta dura and Platycaulos anceps.
Structural formation: Closed Graminoid Shrubland.
Relationships: Brunia alopecuroides— Restio bifidus
Community (Kruger (1974); Subcommunity E2 of the
Erica— Penaea Community (Glyphis et al. 1978); Restio—
Hypolaena Subcommunity (H & I) (Laidler et al. 1978);
Ericoid-Restioid Zone Fynbos (Taylor 1978); Low
Narrow-sclerophyllous Heathland (Kruger 1979);
Simocheilus carneus— Restio anceps Community (Bond
1981); Wet Mountain Fynbos (Moll et al. 1984); Ruiters-
berg Wet Ericaceous Fynbos (Campbell 1985); Erica
hispidula— Brunia alopecuroides Shrublands (McDonald
1993a).
This community (Figure 5) has no differential species
but shares many species with the Erica hispidula— Spatalla
nubicola Shrublands (see Table 1); is characterized by
absence of Spatalla nubicola and Helichrysum cape use',
and is found at altitudes higher than 1 000 m on east-,
southeast-, south- and southwest-facing slopes. Sample
quadrats were located at five general localities; on the
upper south-facing slopes above Saagkuilkloof (Releves
21 & 74), on the lower south- and southwest-facing slopes
of Repeater Kop above Platbosrivierkloof (Releves 34, 36,
37, 77, 80, 83, 120), on the south-facing slopes of the ridge
west of Grootberg Peak ( Releves 60, 61 & 86), on the
slopes southeast of Grootberg Peak overlooking Boos-
mansbos (Releves 90 & 91) and on the east-facing slopes
overlooking Boosmansbos (Releves 31 & 33).
FIGURE 5. — Restio inconspicuus—
Anthochortus crinalis Shrub-
lands at altitudes above I 000
m on southerly slopes.
Bothalia 23,1 (1993)
141
Rainfall is between 1 000 and 1 200 mm annually,
depending on altitude and aspect and the Restio incon-
spicuus-Anthochortus crinalis Shrublands are found
mainly on highly leached Cartref Form soils (see SCWG
1991; Campbell 1983). Two samples (Releve 90 & 91)
were located on Champagne Form soils and show
strong floristic affinity with the Erica hispidula—Spatalla
nubicola Shrublands. However, these stands lack the
differential species of the latter community.
Shrubs and graminoids are co-dominant, with the shrubs
not exceeding 1 m. Widdringtonia nodiflora is present in
some stands and is emergent up to 2 m. Erica hispidula
and Ehrharta dura dominate with Anthochortus crinalis
and Platycaulos anceps less conspicuous, forming part of
the graminoid component.
A number of releves (31, 36 & 92) do not have any of
the differential species of the Restio in conspicuus— Antho-
chortus crinalis Community. They are regarded as samples
from depauperate stands and are included here on the basis
of dominant species and geographical position on the
sample transect and in the landscape.
1.2.2 Restio inconspicuus— Protea grandiceps Shrubland
(C)
Differential species: Protea grandiceps.
Dominant species: Erica hispidula, Tetraria flexuosa,
Tetraria bromoides.
Structural formation: Closed Graminoid Shrubland.
Relationships: Tetraria bromoides— Erica plukenetii
Community (Kruger 1974); Protea— Tetraria Dry Short
Fynbos (Boucher 1978); Wet Mountain Fynbos (Moll et
al. 1984); Boesmansbos Azonal Restio id Fynbos (Camp-
bell 1985); Pentaschistis malouinensis— Tetraria bromoides
Shrubland (McDonald 1993a).
This community (Figure 6) is localized on the south-
facing lower to mid-slopes of the ridge west of Grootberg,
overlooking the Helderfontein Valley, at 1 180—1 295 m
altitude. This locality lies more or less on the contact
between the Cedarberg Formation and the Nardouw
Subgroup. The soils are mainly Cartref Form, where
sandstone is the parent rock (Releves 62, 63 & 71) and
Clovelly Form, where shale is the parent rock (Releve 81).
Mean annual precipitation at this locality is 1 000—
1 100 mm and the soils are well drained but slightly more
nutrient-rich than soils derived from Peninsula Formation
sandstone (G.N. Schafer pers. comm.). The poleward
aspect permits lower insolation, and P. grandiceps ap-
parently favours the cooler slopes and richer soils.
This community is structurally similar to those of most
other parts of the high-altitude slopes. E. hispidula
dominates the shrub component with P. grandiceps having
notable cover-abundance in only two of the four plots
sampled (Releves 62 & 63). Sedges such as Tetraria
flexuosa and Tetraria bromoides dominate the herbaceous
component. Close affinity exists between the Restio
inconspicuus— Protea grandiceps Shrubland and the Restio
inconspicuus— Protea aurea Shrubland, with these two
communities sharing species not common to other com-
munities (see Table 1).
1.2.3 Restio inconspicuus— Protea aurea subsp. aurea
Shrublands (D)
Differential species: Protea aurea subsp. aurea.
Dominant species: Protea aurea subsp. aurea.
Structural formation: Mid-high to Tall Proteoid Shrub-
land with a Closed Graminoid Shrubland Understorey.
Relationships: Tetraria bromoides— Erica plukenetii
Community (Kruger 1974); Protea— Tetraria Dry Short
Fynbos (Boucher 1978); Protea aurea— Pteridium aquili-
num Community (Bond 1981); Wet Mountain Fynbos
(Moll et al. 1984); Boesmansbos Azonal Restioid Fynbos
(Campbell (1985); Pentaschistis malouinensis— Tetraria
bromoides Shrubland (McDonald 1993a).
In BWA this community (Figure 7) occurs at altitudes
above 1 100 m on the Cedarberg shaleband, near Helder-
fontein. The shales of the Cedarberg Formation weather
to produce fine-grained, clay-rich yellow-brown Clovelly
Form soils, and Protea aurea is found almost exclusively
on these soils. This correlation is found throughout the
<•
FIGURE 6. — Restio inconspicuus—
Protea grandiceps Shrubland
localized on the south-facing
slopes west of Grootberg.
142
Bothalia 23,1 (1993)
FIGURE 7. — Restio inconspicuus—
Protea aurea subsp. a urea
Shrublands found on the
Cedarberg Formation shale
near Helderfontein.
Langeberg, regardless of the altitude at which the shale-
band is exposed. P. aurea can therefore be used as a mar-
ker indicating the exposure of the Cedarberg Formation
in the highly folded strata of the Langeberg.
Sample plots were located between Helderfontein and
Boosmansbos (Releves 56, 57, 58 & 59) on northeast-,
southeast- and southwest- facing slopes. Two plots (Releves
64 & 88) were also located on the lower south- and
southwest-facing slopes of the ridge west of Grootberg,
above the watershed between the Helderfontein and
Moeras River Valleys. Releve 88 represents a transitional
situation between Communities 2.2 and 2.3 but since P
aurea has a relatively high BB value (3), and since the
soil is Clovelly Form, it is included in the Restio
inconspicuus— Protea aurea Shrublands.
1.2.4 Restio inconspicuus— Hypodiscus aristatus Shrub-
lands ‘Typicum’ (I)
Differential species: none.
Dominant species: H. aristatus, R. inconspicuus,
Ehrharta dura.
Structural formation: Closed Graminoid Shrubland.
Relationships: Tetraria thermalis— Hypodiscus aristatus
Community (Kruger 1974); Mixed ericoid and restioid
fynbos of the xeric slopes (Boucher 1978);, Leptocar-
pus membranaceus— Hypodiscus aristatus Community
(McKenzie et al. 1977); Subcommunities B & C of the
Erica— Penaea Community (Glyphis et al. 1978); Tetraria
thermalis Bergpalmietveld (Taylor 1978); Low ericoid
open-heath or open graminoid-heath (Kruger 1979); Erica
viridescens— Hypodiscus aristatus Community (Bond
1981); Mesic Mountain Fynbos (Moll et al. 1984); Nuwe-
berg Mesic Ericaceous Fynbos (Campbell 1985); Erica
hispidula— Hypodiscus aristatus Shrublands (McDonald
1993a).
The releves grouped here (23, 29, 32 , 38, 66, 67, 72,
93, 124) represent the ‘typicum’ of the Restio inconspi-
cuus—Hypodiscus aristatus Shrublands (Figure 8). This
‘typicum’ or ‘background community’ has no floristic
elements which allow subdivision into lower-ranking com-
munities; as such it is regarded as depauperate.
These shrublands occur on shallow (0.1—0.15 m), well-
drained and highly leached Cartref and Houwhoek Form
soils at altitudes from 1 000-1 500 m. Parent rock is main-
ly Peninsula Formation sandstone with Nardouw Subgroup
sandstone found in plots 92 and 124. Aspect is generally
north- and northwest-facing, with two exceptions, plots 29
and 30 which face south and southeast. Surface rock cover
ranges between five and 75 % ; boulders were found in
all plots and exposed bedrock in more than 50 % . Although
rainfall probably exceeds 1 000 mm per annum, high in-
solation coupled with good drainage is most likely the rea-
son for the depauperate nature and low stature of the
community.
Shrubs such as Erica hispidula and Penaea cneorum
subsp. ruscifolia are emergent up to 1.2 m but grasses
( Ehrharta dura, Pentaschistis colorata), restios ( Hypo-
discus aristatus , Restio inconspicuus) and sedges ( Tetrar-
ia spp.) dominate the low stratum (<0.5 m). Although
strongly similar structurally and in species composition
to the Restio inconspicuus— Anthochortus crinalis Shrub-
lands, the Restio inconspicuus— Hypodiscus aristatus
Shrublands have Hypodiscus aristatus dominant, whereas
it is absent from the former community. Apparently north
versus south aspects and relative wetness-dryness account
for the change in species dominance and consequent dis-
tinction between these two communities.
1.2. 4.1 Hypodiscus aristatus— Leucadendron eucalyptifo-
lium Shrublands (E)
Differential species: none.
Dominant species: Leucadendron eucalyptifolium.
Structural formation: Mid-high to Tall, Mid-dense to
Closed Proteoid Shrublands.
Relationships: Berzelia— Leucadendron Moist Tall Fyn-
bos (Boucher 1978); Mixed Sclerophyllous Scrub (Kruger
1979); Protea neriifolia— Leucadendron eucalyptifolium—
Erica triceps Community (Bond 1981); Mesic Mountain
Bothalia 23.1 (1993)
143
FIGURE 8. — Restio inconspicuus—
Hypodiscus aristatus Shrub-
lands found on shallow, well-
drained, highly leached sand-
stone soils at altitudes from
1 000-1 500 m.
Fynbos (Moll et al. 1984); Robinson Mesic Proteoid
Fynbos (Campbell 1985).
Leucadendron eucalyptifolium is a tall proteoid shrub
ubiquitous on the Langeberg. It is found at localities on
south and north sides of the range. In the BWA, L. euca-
lyptifolium occurs in the Mesic Proteoid Fynbos north of
Grootberg as well as at the southern end of the sample
transect, on the shaleband at Helderfontein and at the head
of the Moeras River Valley. Where L. eucalyptifolium
occurs with Protea aurea it is found on Clovelly Form soils
but in the community described here (Figure 9) the soils
are either of Oakleaf or Cartref Forms.
L. eucalyptifolium shrubs up to 2.5 m high dominate
the community and it is the only species found in all
releves. Releves 1 and 13 show marked floristic affinities
with the Restio inconspicuus— Protea aurea Shrublands,
whereas the remaining three releves do not. This is
attributed to the nature of this community to transgress
soil types.
Plots 1, 13 and 84 were situated in localized stands of
the Hypodiscus aristatus— Leucadendron eucalyptifolium
Shrublands on Oakleaf Form soils derived from con-
glomerates of the Enon Formation, detailed above. The
soils are loamy with pH 4.3 (in 0.01 mol/1 CaCF) in the
A-horizon increasing to pH 5.3 in the B-horizon. Aspect
is west to southwest at altitudes of just less than 400 m.
Mean annual precipitation at these sites is estimated at
800-900 mm.
In contrast, plots 68 and 87 were located in extensive
stands of the community at altitudes 1 200—1 340 m on
slopes with a northwesterly aspect. Parent rock is Penin-
sula Formation sandstone with Cartref Form soils. These
soils are somewhat more leached and acid (pH 3.2 in 0.01
mol/1 CaC^) in the A- and E-horizons than the loamy
FIGURE 9. — Hypodiscus aristatus—
Leucadendron eucalyptifolium
Shrublands on a northwest-
facing slope on sandstone soil
west of Helderfontein.
144
Bothalia 23,1 (1993)
FIGURE 10. — A dense stand of the
Berzelia intermedia— Erica
melanthera Shrublands on the
lower south slopes of BWA.
Oakleaf Form soils. Mean annual precipitation is estimated
at 1 000 mm .
1.2. 4. 2 Hypodiscus aristatus— Berzelia intermedia
Shrublands
The Hypodiscus aristatus— Berzelia intermedia Shrub-
lands comprise two communities, the Berzelia inter-
media—Erica melanthera Shrublands and the Berzelia
intermedia— Erica blenna Shrublands. These shrublands
occur at altitudes not higher than 875 m (330—860 m)
on the south slopes of the BWA, and give these slopes their
characteristic ericoid-brunioid (fine-leaved) appearance.
The parent rock is Peninsula Formation sandstone through-
out. Berzelia intermedia is conspicuously present through-
out these shrublands.
1.2. 4. 2.1 Berzelia intermedia— Erica melanthera
Shrublands (F)
Differential species: Lobelia coronopifolia, Pentaschistis
sp.
Dominant species: Erica hispidula, Erica melanthera,
Hypodiscus aristatus, Penaea cneorum subsp. ruscifolia,
Tetraria cuspidata.
Structural formation: structure of this community varies
between a Low Closed Ericoid Shrubland and a Closed
Graminoid Shrubland depending on the density and cover
of the shrub component.
Relationships: Fynbos of the ericoid-restioid zone
(Taylor 1978); Low Ericoid Heathland (Kruger 1979); Erica
arachnoidea—Pentameris dregeana Community (Outeni-
qua Mountains) and the Erica petraea— Erica nervata and
Protea punctata- Erica melanthera, E. andraei Commu-
nities (Swartberg) (Bond 1981); Mesic Ericaceous Fyn-
bos (Moll et al.); Landdros Mesic Ericaceous Fynbos
(Campbell 1985).
The dominant species. Erica melanthera is characteristic
of this community (Figure 10). Dense stands of this erica
are visible from a long distance, flowering on the lower
slopes of the Langeberg in spring (Muir 1929; McDonald
pers. obs.). Since the Hypodiscus aristatus— Erica melan-
thera Shrublands are poorly defined by inconspicuous
differential species and because Erica melanthera is easily
identified, it was chosen for the naming of this community.
Erica hispidula is less dominant than Erica melanthera
but is nevertheless well represented, as is Penaea cneorum
subsp. ruscifolia. The dominant graminoids are Hypodis-
cus aristatus (Restionaceae), Tetraria cuspidata (Cyper-
aceae) and Ehrharta setaceae subsp. scabra (Poaceae).
Together with other restios, sedges and grasses such as
Pentaschistis spp. they constitute the co-dominant grami-
noid component.
The altitude at which these shrublands are found ranges
from 330—625 m with a mean of 490 m. The soils are
shallow (100—150 mm), acid (pH 3.2 in 0.01 mol/1 CaCL,
A-horizon) Cartref Form throughout the community. Mean
annual precipitation is estimated at 900—1 000 mm.
Typically these shrublands occur on gentle slopes with a
mean gradient of 10° (5°— 21°) with extremely variable
amounts of exposed rock (0—75% cover).
1.2. 4. 2. 2 Berzelia intermedia— Erica blenna var. blenna
Shrublands (G)
Differential species: none.
Dominant species: Berzelia intermedia. Erica blenna
var. blenna, Erica hispidula, Psoralea pinnata, Widdring-
tonia nodiflora.
Structural formation: the community is classified as a
Low to Mid-high Closed Shrubland with a Mid-dense to
Closed Graminoid Understorey.
Relationships: Berzelia lanuginosa— Osmitopsis asteris-
coides Community (Werger et al. 1972): Erica— Osmitopsis
Seepage Fynbos and Chondropetalum— Berzelia Upper
Hygric Fynbos (Boucher 1978); Hygrophilous Fynbos
(Taylor 1978); Variation 1 of the Restio—Hypolaena Sub-
community (Laidler et al. 1978); Mixed Sclerophyllous
Scrub (Kruger 1979); Berzelia- Osmitopsis Seepage
Fynbos on permanent seeps (Taylor 1984); Wet Mountain
Fynbos (Moll et al. 1984); Keurbos Wet Ericaceous
Fynbos (Campbell 1985); Berzelia lanuginosa- Merx-
muellera cincta Tall Closed Shrubland (McDonald
1988); Erica hispidula— Berzelia intermedia Shrublands
(McDonald 1993a).
Bothalia 23,1 (1993)
145
As noted above, Berzelia intermedia is characteristic of
the Hypodiscus aristatus- Berzelia intermedia Shrublands
(1.2. 4. 2). It is most dominant in the Berzelia intermedia—
Erica blenna Shrublands (Figure 11). Erica hispidula also
attains its highest degree of dominance in this communi-
ty. Erica melanthera is present but much less evident than
in the Berzelia intermedia -Erica melanthera Shrublands.
Widdringtonia nodiflora is a conspicuous emergent shrub
(up to 4 m) in most stands, whereas it is almost totally
absent from the latter community. E. blenna var. blenna
is endemic to the Langeberg and is restricted to the
Swellendam-Heidelberg part of the range. It is used in
the name of the Berzelia intermedia— Erica blenna Shrub-
lands because it has its strongest expression here and the
community is otherwise poorly defined. Psoralea pinnata
is also found commonly here but it has a wider tolerance,
occurring in other communities as well (Table 1). Two
other species of particular note which occur in this com-
munity are the rare Langeberg endemics Linconia
alopecuroides L. (Bruniaceae) and Carpacoce gigantea
Puff (Rubiaceae).
This community is also found on highly leached, low
pH, shallow ( < 300 mm) soils of Cartref and Houwhoek
Forms. Rock cover is mostly 2% or less except in plots
18 (10%) and 76 ( 25%). The slopes where these shrub-
lands are located vary in aspect from east- to south-facing;
one sample plot (73) was located on a west-north-west-
facing slope. The mean gradient of the slopes is 19°
(10° — 33°). Altitudinal range of the community is from
500—850 m with a mean of 670 m. The Berzelia inter-
media—Erica blenna Shrublands thus occupy the zone of
higher, steeper slopes than the Berzelia intermedia— Erica
melanthera Shrublands but occur below the zone occupied
by the Restio inconspicuus—Anthochortus crinalis Shrub-
lands (1.2.1) and Restio inconspicuus— Hypodiscus arista-
tus Shrublands (1.2.4). Mean annual precipitation is
estimated at 1 000—1 100 mm.
Structurally the Berzelia intermedia— Erica blenna Shrub-
lands are variable. In general the upper shrub stratum does
not exceed 1.5 m in height. The exceptions are where
Berzelia intermedia is dominant and reaches 2.5— 3.0 m
in heiaht with a high projected canopy cover (Releves 26 &
76) or where Widdringtonia nodiflora reaches 3—4 m and
exceeds 10% projected canopy cover (Releves 20 & 25).
1.2. 4. 3 Hypodiscus aristatus— Erica versicolor Shrublands
(H)
Differential species: Erica versicolor, Centella virgata
and Tetraria involucrata.
Dominant species: Erica versicolor. Erica hispidula.
Erica melanthera, Hypodiscus aristatus and Tetraria
flexuosa.
Structural formation: Closed Graminoid Shrubland or
a Closed Herbland with a Mid-high Mid-dense Ericoid
Shrubland Overstorey.
Relationships: Mesic Mountain Fynbos (Moll et al.
1984); Hypodiscus aristatus— Erica versicolor Shrublands
(McDonald 1993a).
This community (Figure 12) is typically found on rocky
sandstone outcrops on northwest-, north- and northeast-
facing slopes, but on the south side of the range (i.e. south
of Grootberg).
Soil development on the rocky outcrops where the
Hypodiscus aristatus— Erica versicolor Community is
found is poor, consisting of accumulations of sand and
organic material in shallow (100 mm deep) pockets
amongst the rocks. These lithosols are therefore regarded
as poorly developed Mispah Form soils.
Erica versicolor has the habit of favouring almost any
well-drained rocky situation and the Hypodiscus
aristatus— Erica versicolor Shrubland Community is
usually interspersed amongst other more uniformly dis-
tributed communities, forming a mosaic with the latter
from low to high altitudes (400—1 200 m). The commu-
nity is characterized as much by presence of Erica
versicolor as by marked absence of a number of widely
distributed species, e.g. Cyclopia sessiliflora, Drosera
aliceae, Tetraria compressa and Gnidia oppositifolia ,
which prefer habitats where the soils are deeper and less
readily drained.
The stature of Erica versicolor ranges from low ( < 1
m) to mid-high (1—2 m) and therefore the structural form
FIGURE 11. — Berzelia intermedia—
Erica blenna Shrublands
which occur on highly leached
acid sandstone soils at altitudes
from 1 000—1 100 m mainly
on wet south-facing slopes.
146
Bothalia 23,1 (1993)
F1GU RE 12 . — Hxpodiscus aristatus—
Erica versicolor Shrublands
found on rocky sandstone out-
crops on the south side of the
Langeberg in BWA.
of the Hvpodiscus aristatus— Erica versicolor Community
varies between the two forms stated above.
2. Cannomois parviflora Shrublands
Species with distribution common to all plant commu-
nities and with high cover-abundance are not a feature of
the vegetation on the north slopes of the Langeberg in the
Boosmansbos Wilderness Area. Broad-scale characteri-
zation of the plant communities occurring in this area is
therefore not simple. Cannomois parviflora has been
chosen as the ‘base’ species equivalent to Erica hispidula
on the south slopes, since it is readily identifiable and
found in all the communities in question (Table 2). Camp-
bell (1985) notes that Cannomois parviflora (his Elegia
parviflora) is common as a dominant in Mesic Restioid
Fynbos and is also a feature of Dry Restioid Fynbos and
Dry Proteoid Fynbos. This supports the use of this species
in the nomenclature of the shrublands described here.
The Cannomois parviflora Shrublands are found on soils
derived exclusively from sandstone of the Nardouw Sub-
group. The communities described may or may not reflect
the respective geological formations within the Nardouw
Subgroup but distinctions in geological formation were not
recorded and correlations between plant communities and
geological formations are therefore not possible here. Four
communities are identified and described, two as subdi-
visions of the Cannomois parviflora— Leucadendron eu-
calyptifolium Shrublands and two as subdivisions of the
Cannomois pan’iflora—Passerina obtusifolia Shrublands.
2.1 Cannomois parviflora — Leucadendron eucalyptifolium
Shrublands
The soils are mainly accumulations of well-drained sand
resulting in Clovelly Form soils. The ridges have a some-
what more xeric climate with shallow well-drained
lithosols usually of Glenrosa Form.
This community is found in the above-mentioned inter-
montane valley and on the ridges but not on the arid north-
facing slopes of Deception Ridge. They are locally exten-
sive and are divided into two communities, the Leucaden-
dron eucalyptifolium— Protea lorifolia Shrublands and the
Leucadendron eucalyptifolium — Staberoha cernua Shrub-
lands which are characterized by high cover-abundance
of Leucadendron eucalyptifolium, Protea repens and Tetra-
ria bromoides. The presence of Leucadendron eucalyp-
tifolium indicates a close relationship between these shrub-
lands and the Hypodiscus aristatus— Leucadendron
eucalyptifolium Shrublands (1.2. 4.1) described above.
Their overall species composition and habitat differ,
however, and they are therefore treated as separate com-
munities. The tall shrub Protea eximia occurs sporadical-
ly throughout the Cannomois parvi flora— Leucadendron
eucalyptifolium Shrublands and as a dominant in the Leu-
cadendron eucalyptifolium— Staberoha cernua Shrublands
described below.
The Leucadendron eucalyptifolium— Protea lorifolia
Shrublands are found on the rocky ridges north of Groot-
berg, forming a mosaic with the Leucadendron eucalypti-
folium—Staberoha cernua Shrublands which occur in
bottomland situations. Physiognomically the former com-
munity differs very little from the latter. Both have a Mid-
dense to Closed Graminoid stratum with Mid-high to Tall,
Open to Mid-dense to Proteoid Shrub Overstorey. It is
therefore difficult to distinguish these communities on the
basis of structure.
Northeast of Grootberg is a shallow intermontane valley
forming part of the catchment of Brandrivier. There are
also a number of east-trending rocky ridges, the highest
of which is named Deception Ridge in this study. Altitude
diminishes eastwards towards Brandrivier. The valley has
a mesic to dry climate compared with the wet south slopes
and the arid north slopes adjacent to the Little Karoo.
2.1.1 Leucadendron eucalyptifolium— Protea lorifolia
Shrublands (J)
Differential species: Agathosma ce refolium. Erica ver-
sicolor, Indigofera pappei, Lightfootia tenella, Metalasia
gnaphalodes, Protea lorifolia, Stoebe aethiopica, Stoebe
saxatilis, Ursinia nudicaulis.
Bothalia 23,1 (1993)
147
FIGURE 13. — Leucadendron eucalyptifolium— Protea lorifolia Shrub-
lands found on the ridges north of Grootberg, showing the proteoid
shrub overstorey with P. lorifolia in the left foreground.
Dominant species: L. eucalyptifolium, Elegia filacea.
Protea repens, Tetraria bromoides, Thoracosperma gal-
pinii.
Structural formation: Mid-dense to Closed Graminoid
Shrubland with a Mid-high to Tall, Open to Mid-dense
Proteoid Shrubland Overstorey.
Relationships: Proteoid Zone Fynbos (Taylor 1978);
Broad-sclerophyllous Scrub or Open-scrub (Kruger 1979);
Elegia galpinii—Metalasia pulcherrima Community (Ou-
teniqua Mountains) and Protea repens— Protea lorifolia —
Hypodiscus striatus Community (Swartberg) (Bond (1981);
Mesic Mountain Fynbos (Moll et al. 1984); Thomas Dry
Proteoid Fynbos (Campbell 1985).
This community (Figure 13) is found on the ridges north
of Grootberg. It is best expressed on Deception Ridge
where there are terraces of shallow sandy loam Clovelly
Form soil (Releves 24, 52, 53, 55, 97, 98, 99, 100) and
more poorly expressed where Glenrosa Form soils occur
(Releves 47, 49, 102, 113).
Mean annual precipitation is estimated at 600-700 mm.
The general aspect is northeasterly but varies at local sites
from north through east to south. Although most sites are
well exposed and in many respects equivalent, local site
aspect apparently plays some role in determining the
distribution of the community. This is currently being
investigated (McDonald, unpublished).
This community is structurally variable. The lowest
stratum is always dominant, with sedges, restios and
ericoid shrubs in more or less equal proportions. The
upper stratum consists mainly of proteoid shrubs. The
broad-leafed P. lorifolia is particularly characteristic and
apart from some transgression into the Leucadendron
eucalyptifolium— St aberoha cernua Shrubland (see Table
2), the dominant Protea repens could be viewed as charac-
teristic of this community as well.
The presence of Erica versicolor in the Leucadendron
eucalyptifolium— Protea lorifolia Shrublands indicates
some affinity between this community and the Hypodis-
cus aristatus— Erica versicolor Shrublands described
above. However, E. versicolor tends to be a ubiquist on
rocky outcrops if the moisture regime is high enough and
the limited presence of the species in this community is
thought to indicate the limit of its range on the south-north
gradient. Erica barrydalensis H. Bol., a rare endemic
species, with similar rocky habitat preferences to E.
versicolor, was recorded on Deception Ridge (McDonald
& Oliver 1987) and may replace E. versicolor since it
apparently tolerates xeric conditions more readily.
2.1.2 Leucadendron eucalyptifolium— Staberoha cernua
Shrublands (K)
Differential species: Cyphia zeyheriana, Erica cerin-
thoides, Helichrysum rotundifolium , Lachnaea penicillata,
Staberoha cernua.
Dominant species: Leucadendron eucalyptifolium. Pro-
tea eximia, Tetraria bromoides, Elegia filacea.
Structural formation: Mid-dense to Closed Graminoid
Shrubland with a Mid-high to Tall, Open to Mid-dense
Proteoid Shrubland Overstorey.
Relationships: as for 2.1.1 above.
The differential species of this community (Figure 14)
are not well- represented. It could be argued therefore that
distinction between the Leucadendron eucalyptifolium—
Protea lorifolia Shrublands and the Leucadendron euca-
lyptifolium—Staberoha cernua Shrublands is tenuous.
However, the proteoid stratum of the latter community is
dominated by Protea eximia and Leucadendron euca-
lyptifolium with Protea repens almost absent. In the
Leucadendron eucalyptifolium— Protea lorifolia Shrub-
lands, the opposite is true with P. eximia poorly repre-
sented and L. eucalyptifolium and Protea repens co-
dominant. Absence of a number of species such as
Anomalanthus sp. , Ficinia lacineata, Hypodiscus argen-
teus, Hypodiscus striatus, Phylica mairei, Relhania
calycina subsp. apiculata and Stoebe microphylla from the
Leucadendron eucalyptifolium— Staberoha cernua Shrub-
land reinforces the distinction as well (see Table 2).
Structurally the Leucadendron eucalyptifolium— Stabe-
roha cernua Shrublands are similar to the Leucadendron
eucalyptifolium- Protea lorifolia Shrublands. The lower
stratum is marginally more graminoid and the upper
proteoid stratum more uniformly mid-dense. Other dis-
tinctions are negligible.
The Leucadendron eucalyptifolium- Staberoha cernua
Shrublands are found mainly in bottomland situations with
south- and southeast-facing aspects. One sample (Releve
48) was on a 30° slope but mostly the community occurs
148
Bothalia 23,1 (1993)
FIGURE 14. — Leucadendron euca-
lyptifolium—Staberoha certiua
Shrublands in bottomland
situations. Note the dense
graminoid understorey with
Protea exirnia dominant in the
proteoid shrub stratum.
where there is little or no relief apart from a shallow
gradient eastwards towards Brandrivier. The soils have
resulted from accumulation of sand and are all distinctly
yellow and of the Clovelly Form. A typical pH 4.6
increasing to pH 4.8 (in 0.01 mol/1 CaCl2) was measured
for samples from the A- and B-horizons respectively of
soil at Releve 105.
2.2. Cannomois parviflora— Passerina obtusifolia
Shrublands
This community is found on the exposed north-facing
slopes of Deception Ridge below an altitude of 1 000 m
and on the mesa-like sandstone plateaux above the con-
tact with the Bokkeveld Formation shales of the Little
Karoo. This is the most arid aspect of the transect, with
high incoming radiation and rainfall ranging between
300—600 mm p.a. Two communities are described, the
first being the Cannomois pan’ijiora— Passerina obtusifolia
‘Typicum’ and the second the Passerina obtusifolia— Leu-
cospermum calligerum Shrublands.
Passerina obtusifolia is a widespread species found on
sandstone soils on the dry aspects of the mountains from
Clanwilliam Division in the west to Grahamstown in the
east (Thoday 1924). Occurrence of this species on the
lower north slopes of the Langeberg clearly places the
Cannomois parviflora— Passerina obtusifolia Shrublands
within the context of Dry Mountain Fynbos (Moll et al.
1984).
The species shared between the two communities show
definite affinities with Karroid vegetation; succulents in
the genera Adromischus, Crassula, Maehairophyllum and
Ruschia indicate the transition from fynbos to Succulent
Karoo. The endemic Leucospermum erubescens is found
in these shrublands but was not encountered in any of the
sample plots. Its distribution appears to be erratic on the
north slopes of the Langeberg from Witbooisrivier to
Garcia’s Pass.
2.2.1 Passerina obtusifolia— Leucospermum calligerum
Shrublands (L)
Differential species: Elytropappus cyathiformis, Leuco-
spermum calligerum, Lobostemon decorus, Muraltia
heisteria, Paranomus spathulatus, Serruria balanocepha-
la, Thamnochortus karooica, Thesium subnudum.
Dominant species: Leucospermum calligerum, Metala-
sia densa, Passerina obtusifolia, Pentaschistis eriostoma,
Serruria balanocephala.
Structural formation: Mid-high Mid-dense Graminoid
Shrublands.
Relationships: Arid Fynbos (Taylor 1978); Arid Fynbos
(Kruger 1979); Phyllica axillaris— Felicia filifolia Commu-
nity (Outeniqua Mountains) and Passerina obtusifolia —
Felicia filifolia- Pentaschistis eriostoma Community
(Swartberg) (Bond 1981); Dry Mountain Fynbos (Moll et
al. 1984); Sebrafontein Dry Asteraceous Fynbos (Camp-
bell 1985).
This community (Figure 15) is found on the lower north-
facing slopes above Witbooisrivier at altitudes from
485—745 m. The habitat is not much different from that
of the Cannomois parviflora— Passerina obtusifolia Typi-
cum’ except that the mean gradient of the sample sites is
8° (6°— 22°). With this difference in mean gradient,
changes in drainage and other subtle factors may account
for the development of this community.
Leucospermum calligerum is a widely distributed
proteoid species on the arid aspect of the fynbos of the
northwestern and western mountains (Lokenberg and
Gifberg) and on the dry north slopes of the Langeberg to
the Gouritz River in the east (Rourke 1972). It therefore
links this community with the widely distributed Arid
Fynbos ( sensu Taylor 1978; Kruger 1979), Dry Mountain
Fynbos (Moll et al. 1984) or Dry Asteraceous Fynbos
(Campbell 1985). At a local scale, however, endemic
species such as Paranomus spathulatus and Serruria
balanocephala Rourke ined., characterize the Dry Moun-
Bothalia 23,1 (1993)
149
tain Fynbos of the north slopes of the Langeberg; a more
refined definition of this community may be possible with
more extensive sampling.
2.2.2 Cannomois parx’iflora— Passerina obtusifolia
Shrublands ‘Typicum’ (M)
Differential species: none.
Dominant species: Hypo discus striatus, Passerina ob-
tusifolia, Pentaschistis eriostoma.
Structural formation: Open Graminoid Shrubland with
ericoid shrubs emergent to 2 m.
Relationships : As for 2 . 2 . 1 above and Leucadendron euca-
lyptifolium—Hypodiscus argenteus Shrubland (McDonald
1993a) in part.
Four releves, 45, 46, 50 & 51, represent this communi-
ty. The first two sample plots were located on the lower
north slopes above Klein Witbooisrivier at 594 m a.s.l.
The soils are of Mispah Form reflecting poor soil develop-
ment. Releves 50 & 51 are at 792 and 914 m a.s.l. respec-
tively on the rocky north-facing slopes of Deception Ridge.
The soils at these sites are classified as Glenrosa Form.
The mean gradient of the sites is 24° and rock cover is
not less than 95% at any of the sites.
All the species in the Cannomois pa rviflora— Passerina
obtusifolia Shrublands are shared with other communi-
ties. The xeric conditions at the above sites limit the
survival of many plant species and the community conse-
quently lacks species requiring more favourable conditions.
DISCUSSION AND CONCLUSIONS
Much debate has surrounded the classification of the
fynbos vegetation of the Cape Floristic Region. Various
methods have been used in attempts to classify the floristi-
cally complex vegetation into ecologically meaningful yet
‘practical’ units interpretable by scientist and manager
alike.
Two approaches to the classification of the fynbos of
mountain ecosystems in the Cape have been used since
the early 1970’s: (i) the floristic approach and (ii) the struc-
tural approach. The floristic approach has been based
mainly on the methodology of the Ziirich-Montpellier
school of phytosociology (Mueller-Dombois & Ellenberg
1974; Werger 1974). However, one of the problems facing
phytosociologists in the fynbos of the Cape mountains is
the great diversity of habitats and attendant high diversity
of plant taxa (Werger et al. 1972). Floristic techniques have
demanded high skills in identifying plants in the field, for
example according to Bond (1981), ‘high species turnover
along geographic gradients places high demands on the
ecologist’s ability in field taxonomy for limited returns in
ecological understanding. ... This reduces the generality
and usefulness of a formal phytosocio logical approach to
parochial studies in small areas.’ Campbell (1986a & b)
affirmed Bond’s statement and severely criticised floristic
techniques. However, despite this major area of difficulty
the mosaic of small, localized studies that have been done
have been useful in generating an overall picture of at
least the broad fynbos communities present in the Cape
mountains.
On the Langeberg, Muir’s (1929) early descriptions,
Taylor’s (1955) documentation of Grootvadersbosch Forest,
McKenzie’s (1978) study of the forests and Campbell’s
(1983, 1985, 1986a) structural classification were the only
studies of the vegetation prior to the present study. Camp-
bell (loc. cit.) placed 21 samples in BWA on his ‘Lange-
berg Transect’ which he classified into six subseries (i)
Azonal and (ii) Mesic Restioid Fynbos, (iii) Mesic and
(iv) Wet Ericaceous Fynbos and (v) Mesic and (vi) Dry
Proteoid Fynbos; 12 types were described. However,
although Campbell’s (1985) classification provides a
comprehensive typology of Cape mountain vegetation
(Cowling & Holmes 1992) it lacks floristic information
found in phytosociological studies, which Bond et al.
(1992) and Cowling et al. (1992) found appropriate for
testing ecological and phytogeographical hypotheses. The
application of the Braun-Blanquet method in this study was
time-consuming but ultimately yielded an acceptable
classification of the fynbos plant communities of the BWA.
The classification is ecologically meaningful and easily
interpretable if the user is familiar with the character
species which form only a small proportion of the diverse
FIGURE 15. — Passerina obtusifolia—
Leucospermum calligerum
Shrublands on the dry lower
north-facing slopes at Wit-
booisrivier, bordering the
Little Karoo.
150
Bothalia 23.1 (1993)
flora. The floristic data assembled in this study also
provide a basis not only for description and hierarchical
classication of fynbos plant communities but also for bio-
geographical studies.
The fynbos of mountain catchments of the southern
Langeberg accords with Taylor’s (1978) broad zonation
classification of Cape mountain vegetation. In BWA,
however, complex environmental gradients exist from the
mesic lower south slopes through a number of fault valleys
to wet high-altitude slopes and exposed peaks and ridges
and then to the mesic to dry shallow valleys and ridges
and very dry, exposed north slopes. This has profound
local effects on the distribution of vegetation associations.
Correlation between environment and plant communi-
ties enhances the descriptive and predictive value of
any phytosociological classification (Campbell 1983;
McDonald 1987; Deall et al. 1989). Such correlations have
necessarily been superficially described in this paper.
Therefore, attempts to explain the gradients underlying the
distribution of the communities described here will be
presented in a later paper (McDonald, unpublished) where
data from two additional sample transects will be available.
In attempting to show relationships between the com-
munities described in this paper and those described
by other workers in Mountain Fynbos, difficulty was
experienced in equating one community with another. This
is due to high geographic turnover (gamma diversity) of
species in roughly similar montane habitats (Cowling &
Holmes 1992). The relationships of communities shown
in this paper are open to modification as greater under-
standing of the composition and functioning of commu-
nities is gained. As the synthesis of fynbos proceeds, the
recognition of regional associations of limited extent or
geographical races of an association may have to be
recognized (Werger et al. 1972; Cowling & Holmes 1992)
to overcome the problems of equivalence between com-
munities. For instance this may ultimately result in the
recognition of southwestern Cape, southern Cape and
southeastern Cape zones of the Fynbos Biome.
The vegetation of the BWA was almost completely
burned in a summer wildfire in February 1988, subsequent
to the sampling of releves reported on here. After three
years (April 1991), apart from the predominance of ‘fire-
ephemerals’ such as Ursinia trifida which dominate over
large parts of the south slopes, the communities of BWA
as described here are identifiable. As succession proceeds
it is predicted that the robustness of the floristic classi-
fication will become even more evident as the fire
ephemerals disappear and the perennial shrublands reach
their mature expression.
ACKNOW LEDGEMENTS
The contributions of the following institutions and
people are gratefully acknowledged: the Director-General
Environment Affairs for permission to work in the Boos-
mansbos Wilderness Area and the generous support of the
Department of Environment Affairs and latterly the Chief
Directorate of Nature and Environmental Conservation,
Forestry Branch, Cape Provincial Administration; Mr T.J.
van der Merwe and Mr C. Martens, foresters at Groot-
vadersbosch Forest Station for logistical support; Miss M.
Morley and Mr C. Ruiters for field assistance; my col-
leagues at the Stellenbosch Herbarium, NBI for assistance
with plant identification and my supervisors. Dr J.C.
Scheepers, Dr C. Boucher and Prof. R.M. Cowling for
their guidance. Without the indulgence of my wife Anne,
and my family, during my frequent absences from home,
this study would not have been possible. I am indebted
to them for their support.
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Bothalia 23,1: 153-174 (1993)
The vegetation of the southern Langeberg, Cape Province. 2. The plant
communities of the Marloth Nature Reserve
D.J. MCDONALD*
Keywords: classification, forest, fynbos, Langeberg, phytosociology
ABSTRACT
The Marloth Nature Reserve, encompassing the mountain catchments of the southern Langeberg immediately above
Swellendam, Cape Province, South Africa, is described. The vegetation of the reserve was sampled along a transect representing
the variation in plant communities over the range from the lower south to the lower north slopes. Eighty-three sample sites
were subjectively located in mature stands of fynbos vegetation ( > 10 years old). The releve data were initially classified
using TW1NSPAN and then refined by Braun-Blanquet (BB) phytosociological procedures. The Afromontane Forest patches
which occur mainly on the lower south slopes were not sampled but are briefly discussed. The fynbos plant communities
are described, based on tables, and a hierarchical classification is proposed.
UITTREKSEL
Die Marloth Natuurreservaat wat die bergopvanggebiede van die suidelike Langeberge bokant Swellendam, Kaapprovinsie,
Suid-Afrika, insluit, word beskryf. Die plantegroei van die reservaat is versamel langs 'n transek wat die variasie in
plantgemeenskappe oor die bergreeks vanaf die onderste suidelike tot die onderste noordelike hange verteenwoordig.
Drie-en-tagtig monsterpersele is subjektief in volwasse fynbos (>10jaar oud) uitgele. Die releve-data is aanvanklik deur
middel van TWINSPAN geklassifiseer en toe deur Braun-Blanquet (BB) fitososiologiese prosedures verfyn. Die Afro-montane
woudgemeenskappe wat hoofsaaklik op die onderste suidelike hange voorkom, is nie gemonster nie maar word kortliks bespreek.
Die fynbosplantgemeenskappe word kortliks beskryf, gebaseer op tabelle, en 'n hierargiese klassifikasie word voorgestel.
CONTENTS
Introduction 153
Study area 154
Location 154
Physiography 154
Geology 156
Soils 156
Climate 157
Methods 157
Vegetation 158
Afromontane Forest 158
Fynbos 158
1. Cliffortia serpyllifolia Shrublands of the
lower south slopes 158
1.1 Cliffortia serpyllifolia— Widdringtonia
nodiflora Shrublands 158
1.1.1 Widdringtonia nodiflora— Rhodocoma
fruticosa Shrublands (A) 158
1.2 Cliffortia serpyllifolia— Leucadendron
eucalyptifolium Shrublands 159
1.2.1 Leucadendron eucalyptifolium— Hippia
pilosa Shrublands (B) 163
1.2.2 Leucadendron eucalyptifolium — Erica
vestita Shrublands (C) 164
2. Erica hispidula Shrublands of the high
elevation zone 165
2.1 Erica hispidula— Brunia alopecuroides
Shrublands (D) 165
2.2 Erica hispidula— Berzelia intermedia
Shrublands (E) 166
2.2.1 Berzelia intermedia— Erica conferta
Shrublands (F) 166
* National Botanical Institute, P.O. Box 471, Stellenbosch 7599.
Present address: Conservation Biology Unit, NBI Kirstenbosch, Private
Bag X7, Claremont 7735.
MS. received: 1992-03-20.
2.2.2 Berzelia intermedia— Grubbia rosma-
rinifolia Shrublands (G) 167
2.2.3 Berzelia intermedia— Cliffortia grandi-
folia Shrublands (H) 168
2.3 Erica hispidula— Pentaschistis malouinen-
sis Shrublands (I) 168
2.3.1 Pentaschistis malouinensis—Tetraria bro-
moides Shrublands (J) 169
2.4 Erica hispidula— Hypodiscus aristatus
Shrublands (K) 169
2.4.1 Hypodiscus aristatus— Phylica pinea
Shrublands (L) 170
2.4.2 Hypodiscus aristatus— Erica versicolor
Shrublands (M) 170
2.4.3 Hypodiscus aristatus— Restio strictus
Shrublands (N) 171
2.4.4 Hypodiscus aristatus— Erica multum-
bellifera Shrublands (O) 171
3. Leucadendron eucalyptifolium Shrublands
of the extreme north slopes 172
3.1 Leucadendron eucalyptifolium— Erica
melanthera Shrublands (P) 172
3.2 Leucadendron eucalyptifolium— Hypodiscus
argenteus Shrublands (Q) 172
Discussion and conclusions 173
Acknowledgements 174
References 174
INTRODUCTION
This paper is the second in a series describing the plant
communities of the southern Langeberg, Cape Province.
The fynbos plant communities occurring in the Marloth
Nature Reserve (Swellendam State Forest) are described
and classified. The Afromontane Forest patches found in
the study area were not sampled but are briefly discussed
based on the studies of McKenzie (1978).
154
Bothalia 23,1 (1993)
STUDY AREA
Location
The Marloth Nature Reserve (MNR) is situated in the
mountain catchments of the southern Langeberg above the
town of Swellendam (Figure 1). In 1928 a deputation of
Swellendam residents petitioned the Minister of Lands and
Forestry, General Kemp, to set aside a part of the mountain
behind Swellendam as a nature reserve. The well-respected
chemist and botanist Dr Rudolf Marloth proposed approxi-
mately 190 ha on the lower slopes of the Langeberg behind
Swellendam, as a suitable area. This area which included
the forest patches of Koloniesbos and Duiwelsbos, was
proclaimed as a nature reserve and named in honour of
Dr Marloth (Liickhoff 1981).
More recently, in accordance with the policy of the
former Directorate of Forestry and Environmental Con-
servation to extend reserves for more effective manage-
ment, the MNR was enlarged to more than 11 000 ha in
June 1981. At the same time the Swellendam Hiking Trail
was opened for recreational hiking in the MNR (Liick-
hoff 1981). Similar to the Boosmansbos Wilderness Area,
the MNR is bounded on the north and south sides largely
by agricultural lands and on the west and east sides by
privately owned mountain land.
The sample transect selected in the MNR extended from
the lower south slopes at the foot of 12 O’Clock Peak to
the ‘Plaat’ or plateau and from there up the south-facing
slopes of 12 O’Clock Peak. The transect was then ‘broken’
and continued from 10 O’Clock Peak down the north-
facing slopes into Boskloof Valley and up the opposite
south-facing slope to the summit of Hermitage Ridge.
From this point samples were taken, roughly following
the route of the Swellendam Hiking Trail to Goedgeloof
Hut on the extreme lower north slopes of the range. This
route gave ready access to the area. Although the transect
covered a narrow belt and consequent relatively small
area compared with the whole MNR, it allowed for sam-
pling of the variety of fynbos plant communities present
(Figure 2).
Physiography
The south slopes of the Langeberg above Swellendam
are steep and rise rapidly to the famous ‘Clock Peaks’
(Figure 3). On the lower south slopes, however, the
steepness is broken by the ‘Plaat’ at an elevation of
approximately 500 m. This plateau is the result of down-
faulting of the Worcester Fault along this part of the
Langeberg Range. On the north side of 10 to 12 O’Clock
Peaks the slopes drop steeply into the Boskloof inter-
montane valley (Figure 4). Between 12 O’Clock Peak and
One O’Clock Peak to the west is the deeply faulted,
dissected and inaccessible Hermitage Kloof. This kloof
lies below Hermitage Peak (1 154 m) and Misty Point or
Goedgeloof Peak (1 710 m), the highest peak of the
Langeberg. To the north of and overlooking Boskloof
Valley is the rocky Hermitage Ridge, which gives way in
turn to the dissected area of Zuurplaats and the open high-
altitude valley of Langkuilen. North of Langkuilen is
Goedgeloof Ridge which lies adjacent to the Little Karoo.
West of Misty Point is Protea Valley which extends west-
wards over Dwariganek into the Twistniet Valley. The
topography from Protea Valley westwards to Nooitgedacht
River is dominated by a series of peaks; Kruispad Peak
(1 365 m), Leeurivierberg (1 628 m), Middelrivierberg
(1 405 m) and Klipspringerkop (1 127 m). The south slopes
of these peaks are steep but uniform and not deeply
100km
Fynbos Biome Mountains
Langeberg
N Cities & Towns
MNR Transect
FIGURE I. — Map of the mountains of the Fynbos Biome showing the position of the Langeberg and the location of the Marloth Nature Reserve
(MNR) transect. B, Barrydale; C, Cape Town; G, George; H, Heidelberg; M, Mossel Bay; P. Port Elizabeth; R, Riversdale; S, Swellen-
dam and W, Worcester.
Bothalia 23,1 (1993)
155
FIGURE 2. Portion of topographical map 3320CD Scheepersrus, showing part of the MNR with positions of the sample plots. (Map reproduced under Government Printer's copyright authority dated
30 October 1991).
156
Bothalia 23,1 (1993)
FIGURE 3. —The steep south-facing
slopes of the Langeberg above
Swellendam. Photograph taken
from Twelve O'Clock Peak.
dissected. In contrast, the north slopes are much more
dissected and less uniform, particularly when compared
with the north slopes below Misty Point.
Leeukloof, Wolfkloof, Hermitage Kloof, and Boskloof
drain the mountain catchments of the area to the south and
southeast. On the north slopes numerous streams such as
the Rietrivier, Knapsakkraalrivier, Warmwaterrivier and
Dwarigarivier have their sources at high altitude and drain
the dry north-facing slopes, supplying water for agricul-
ture on the north flank of the Langeberg.
in the MNR consist of Peninsula Formation sandstone.
Hermitage Peak and Misty Point, which have a more
northerly position, consist of Nardouw Subgroup sand-
stones (South African Committee for Stratigraphy, SACS
1980). The distinction can be made by tracking the position
of the intervening Cedarberg Formation shaleband. Soils
derived from weathered Cedarberg Formation shale are
encountered in the Boskloof Valley westwards to
Hermitage Kloof. The extreme folding in Hermitage Kloof
obscures the position of the shaleband, but it is once again
evident in Protea Valley, at Dwariganek and into the
Twistniet Valley.
Geology
Extending from Goudini, which lies beyond the
Langeberg in the northwest, along the lower southwest side
of the Langeberg, to the proximity of Sparrebosch (im-
mediately east of Swellendam) is a ‘band’ of Malmesbu-
ry Group sediments. The exposure of these sediments
follows the Worcester Fault and in the MNR they are found
on the lower slopes of the peaks listed above, but below
the ‘Plaat’ (i.e. below 500 m) (De Bruyn et al. 1974).
The main massif of the mountain in the MNR is com-
posed of Table Mountain Group (TMG) sediments. All
the high peaks on the south side of the Langeberg Range
A silcrete mesa extends from the base of the Langeberg
below Goedgeloof Ridge northwards. The Nardouw Sub-
group sandstones of the northernmost slopes thus make
contact with the silcrete cap which in turn covers the
Bokkeveld Group shales. The silcrete mesa forms a water-
shed with streams draining eastwards to the Tradouws
River and westwards to the Kingna River.
Soils
The soil forms (Soil Classification Working Group 1991)
occurring in MNR are summarized in Table 1, indicating
their parent material, diagnostic characteristics and
position in the landscape. No attempt has been made to
FIGURE 4 — Boskloof, behind the
Clock Peaks, as seen from the
high altitude south-facing
slopes of Hermitage Ridge.
Bothalia 23,1 (1993)
157
TABLE 1. — Soils of the Marloth Nature Reserve
identify all possible soil forms found in MNR, but rather
to give a broad overview of major forms; particularly those
encountered on the sample transect.
Climate
Climatic data for Langeberg montane environments are
scant and the climate measured at the Swellendam and
Weltevrede weather stations (Soil and Irrigation Research
Institute, SIRI 1986), i.e. those stations closest to the
MNR, does not accurately represent the montane climate.
Climate diagrams for these stations. Figure 5A & B,
represent the climates at the lower south and north
extremes of the MNR transect.
The climate of the MNR is typical of the southern
Langeberg since it falls within the transition zone between
winter and year-round rainfall areas. The mean annual
precipitation for the high peaks is estimated to be more
than 1 400 mm (Dent et al. 1987). However, the climate
on the south side of the range is distinctly different from
that on the north side. The south slopes of the southern
Langeberg experience the highest rainfall in autumn
(April) and late winter to spring (August and October) with
rainfall in excess of 40 mm for every month except May,
the driest month. This bimodality is not evident in the
rainfall pattern on the north slopes of the range which are
in a rainshadow. Here a peak in rainfall occurs in autumn
(April) with a dry period in May preceding a somewhat
elevated winter to spring rainfall. Figure 5A. The rainfall
exceeds 40 mm only in April and August. The mean
summer maximum and mean winter minimum tempera-
tures for Swellendam are 29.4°C (January) and 6.6°C
(July) respectively. On the opposite side of the mountain
at Weltevrede (33° 56' S, 20° 37' E), on the lower north
slopes of the Langeberg, the equivalent temperatures are
30.0°C (February) and 2.9°C (July), Figure 5B.
The windiest months at Weltevrede are December and
February and at Swellendam, May. Hot, strongly desic-
cating fohn-like berg winds occur mainly in May, June
and July.
METHODS
During 1988, 1989 and 1990, 83 plots were sampled
along a predetermined transect in the study area (Figure
2). The area was not stratified since no suitable aerial
photographs were available. Consequently plots were sub-
jectively placed in what were taken as the major landscape
features and plant communities. The rectangular sample
quadrats were 50 m2, subdivided into 10 equal-sized sub-
plots to facilitate data collection (McDonald 1988, 1993).
Only permanently recognizable species were recorded.
Geophytes and annuals encountered were noted but not
used in the analyses. The Braun-Blanquet cover-abundance
scale (Mueller-Dombois & Ellenberg 1974; Werger 1974)
was applied. A border zone of 1.5 m from the perimeter
of each plot was rapidly searched for any additional species
not found in the marked plot.
Only the sclerophyllous fynbos was sampled since the
mixed evergreen (Afromontane) forests are well docu-
mented by McKenzie (1978).
(A) SWELLENDAM (242 m)
FIGURE 5. — Walter-Lieth climate diagrams for A. Swellendam and B,
Weltevrede, on the northern side of the Langeberg.
158
Bothalia 23,1 (1993)
Phytosociological tables were compiled by obtaining
a ‘first approximation’ classification using TWINSPAN
(Hill 1979) and then by successive refinement using
Braun-Blanquet procedures with PCTables (Boucher
unpublished).
Each community is described following the order in the
proposed classification; the structural description follows
the system advanced by Campbell et al. (1981). Relation-
ships between the communities described here and com-
munities described in other studies of mountain fynbos
are given as far as possible. These relationships were
determined by comparing the floristic composition of the
communities of this study with the respective communi-
ties of other studies as indicated below [note that Camp-
bell (1985) gave ‘floristics’ for each of his lowest level
structural units].
VEGETATION
The greater part of the Marloth Nature Reserve is
covered by sclerophyilous fynbos typical of the mountains
of the western and southern Cape (Taylor 1978; Kruger
1979). Afromontane Forest communities in the MNR are
confined to moist kloofs on the south side of the Lange-
berg range.
Afromontane Forest
Numerous mixed evergreen Afromontane forests (Gel-
denhuys 1989) are found in the MNR. These forests were
exploited for hardwood timber in early colonial days, for
wagon-making, furniture and general construction. The
accessible forest patches are known variously as Kolonies-
bos, Duiwelsbos, Doktersbos and Grootbos with less
accessible forests being found in Boskloof, Hermitage
Kloof, Wolfkloof and Leeukloof. McKenzie (1978)
described the ‘ Rapanea melanophloeos—Hartogiella
schinoides—Podocarpus latifolius Forest Association’ as
the general type found in the southwestern Cape. This
association was divided into three subassociations, two of
which are found in the MNR: Cunonia capensis—
Platylophus trifoliatus Subassociation and Carissa
bispinosa—Canthium ventosum—Canthium mundianum—
Pterocelastrus tricuspidatus Subassociation. Only one of
the variations of the Cunonia capensis— P. trifoliatus
Subassociation, the Cunonia capensis— Todea barbara
Variation was identified in MNR, whereas two variations
of the second subassociation, Buddleja saligna—Scolopia
mundii Variation and Rothmannia capensis— Olinia
ventosa—Canthium ventosum — Canthium mundianum
Variation were identified (McKenzie 1978).
The three variations of forest subassociations identified
in MNR occur on a moisture gradient. The Cunonia
capensis— Todea barbara Variation occurs in wet situations
along streams, the Rothmannia capensis — Olinia
ventosa—Canthium ventosum—Canthium mundianum
Variation is found on seasonally wet to dry sites and the
Buddleja saligna—Scolopia mundii Variation on relatively
dry sites.
Fynbos
The complexity of the fynbos vegetation of the Marloth
Nature Reserve has necessitated subdivision of the data
into three parts for treatment in separate phytosociologi-
cal tables (Tables 2, 3 & 4). These subdivisions represent
logical separations which have facilitated definition of the
fynbos shrubland communities.
The TWINSPAN analysis separated the data into 23 sub-
divisions. The division at Level 1 indicated the separa-
tion of the data into two groups; releves in Tables 2 &
3 on the one hand and Table 4 on the other. TWINSPAN
separated the releves of Table 4 into two groups at Level
2 and finally into three subdivisions at Level 3; a finer
classification than presented in Table 4.
At Level 2, the remaining releves are separated into two
groups; communities A— C and 1-0 on the one hand and
communities D— H on the other. At Level 3 communities
A— C (Table 2) are separated from communities 1-0
which are treated together with communities D— H in
Table 3. At the lower levels of the TWINSPAN classifica-
tion there is some agreement between this analysis and
the BB-classification, however, the latter classification is
favoured since it yields fewer units that are more easily
interpreted and identified in the field.
1. Cliffortia serpyllifolia Shrublands of the lower south
slopes
The shrublands of the lower south slopes of the Lange-
berg at Swellendam are conspicuously dominated by
Cliffortia serpyllifolia which is hardly found higher than
the edge of the ‘Plaat’. The edge of the ‘Plaat’ represents
the contact between the TMG sediments and the basement
rock of the Malmesbury Group with which C. serpyllifolia
appears to be strongly associated. A logical separation of
the lower slope plant communities on Malmesbury Group
sediments [Main Quartzite of the Lower Group of the
Boland Formation (De Bruyn et al. 1974)] (Table 2) from
the Erica hispidula shrublands (Table 3) of higher eleva-
tion on TMG sediments is therefore possible. It is impor-
tant to note, however, that many of the species are common
to both shrubland types.
1.1 Cliffortia serpyllifolia- Widdringtonia nodiflora
Shrublands
Only one poorly defined shrubland community is
included here. This community lies at the transition
between the Erica hispidula Shrublands of the high
elevation zone and the Cliffortia serpyllifolia— Leucaden-
dron eucalyptifolium Shrublands.
1.1.1 Widdringtonia nodiflora— Rhodocoma fruticosa
Shrublands (A)
Differential species: Rhodocoma fruticosa, Tetraria
brevicaulis, Ehrharta ramosa, Tetraria ustulata, Edmon-
dia sesamoides, Ursinia nudicaulis.
Dominant species: Cliffortia serpyllifolia, Erica hispi-
dula, Erica versicolor, Penaea cneorum subsp. ruscifolia.
Structural formation: Mid-high, Mid-dense (Ericoid)
Shrubland with a Mid-dense Graminoid Shrubland Un-
derstorey.
Relationships: unclear.
Bothalia 23,1 (1993)
159
TABLE 2. — A phytosociological table of plant communities on the lower south slopes of the Langeberg on a transect through the Marloth Nature
Reserve, Swellendam
Conmuni ty
1
1.1 1.2
A 0 C
Releve number *11*11111*11111
*35*23333*22223
*12*92345*56780
Altitude ( m)
.55.35543.22332
.88.17159.44229
.00.00500.22000
Aspect C) . 2.1221 2.22 22
.43.72131.99798
.05.00500.55005
Lightfootia tenella Lodd.
Mai rea microcephala (Less.) 0C.
Ursinia scariosa (Ait.) Poir. subsp. scariosa
Tetraria cuspidata (Rottb.) C.B. Cl.
This community is represented by only two releves (131
& 152), found on the rocky ridge marking the edge of the
‘Plaat’, at an altitude of 580 m. Sample plot 131 was
situated on the north-north-east aspect of the ridge, with
a slope of 14°, and sample plot 152 was located on the
south-south-west aspect of the ridge with a slope of 7°.
These differences appear to have affected dominance only.
The soils are lithosols and are of the Mispah and Glenrosa
Forms at the two sites respectively.
The Mid-dense Graminoid Shrubland is dominant and
contains all the differential species. Emergent from this
stratum ( < 1 m) is a Mid-high Open to Mid-dense Shrub-
land, with dominants as above. In releve 152, Laurophyllus
capensis dominates the upper stratum.
1.2 Cliffortia serpyllifolia— Leucadendron eucalyptifolium
Shrubland
This community includes two shrubland communities
both of which are found below the ‘Plaat’ in a very com-
160
Bothalia 23,1 (1993)
TABLE 3. —A phytosociological table of the Erica hispidula Shrublands along a transect through the Marloth Nature Reserve, Langeberg,
Swellendam
Bothalia 23,1 (1993)
161
TABLE 3. — A phytosociological table of the Erica hispidula Shrublands along a transect through the Marloth Nature Reserve, Langeberg,
Swellendam (continued)
Releve Nuiber *1222*11112*11111111*1111112*11111*1111*11111*11112*11111111*111112*111*11
*7000*55550*33344566*3566660*44569*6777*77789*79990*44444788*688990*678*99
<9*56*56787*67957401*8323452*08996*7456*13780*83781*12346209*627123*801*45
162
Bothalia 23,1 (1993)
TABLE 3. — A phytosociolog ical table of the Erica hispidula Shrublands along a transect through the Marloth Nature Reserve, Langeberg,
Swellendam (continued)
Releve Nuaber *1222*11112*11111111*1111112*11111*1111*11111*11112*11111111*111112*111*11
*7000*55550*33344566*3566660*44569*6777*77789*79990*44444788*688990*678*99
*9456*56787*67957401*8323452*08996*7456*13780*83781*12346209*627123*801*45
! Differential species of the Hypodiscus aristatus-Restio strictus Shrubands ( N )
I Restio strictus N.E. 8r.
1131112
jspecies cosion to coiaaunities D--N
I Erica hispidula L.
(Elegia juncea L.
| Anthochortus crinalis (Hast.) Linder
j Ehrharta setacea Nees ex Inn. subsp. scabra (Stapf
jChrysithnx capensis L,
j Platycaulos coioressus (Rottb.) Linder
iClutia alaternoides L.
jProtea cynaroides (L.) L.
| Pentaschistis colorata (Steud.) Stapf
jSenecio cordifolius L.f.
IBlaeria coccinea Klotzsch
Petalacte canescens DC.
Kniphofia uvaria (L.) OKen .
Hairea hirsuta OC.
Restio fragilis Esterhuysen
i Leucadendron spissifoliu* (Salisb, ex Knight)
| Platycaulos anceps (Hast.) Linder
I Epischoenus quadrangularis (Boeck.) C.B. Cl.
I Species coaaon to cosaumties E--k
! Lobelia neglecta Roe*. K Schult.
jEdiondia sesaioides (L.) Hilliard
jletraria brevicaulis C.B. Cl.
jPenaea cneoru* Heerb. subsp. ruscifolia Oahlg.
ICentella lanata Coipton
I Psoraiea pinnata L.
j Erica daphniflora Salisb.
jletraria flexuosa (Thunb.) C.B. Cl.
jstruthiola eckloniana Heisn.
jCoryabiua glabru® L. var. glabrui
IHetalasia densa (La*.) Karis
iChondropetalui »ucronatu» (Nees) Pillans
iGleichema polypodioides (L.) J.E. S».
jlndigofera sarientosa L.
jSchizaea pectinata (L.) Sw.
j Anenone tenuifolia (L.f.) DC.
IBobartia parva J.B. Gillett
I Euryops pinnatipartitus (0C.) 8. Nord.
jletraria capillacea (Thunb.) C.B. Cl.
jUrsinia scariosa (Ait.) Poir. subsp. scanosa
j Erica bracteolaris La*.
jOthonna quinauedentata Thunb.
lOsteosperiu* coryibosu* L.
ICentella stenophvlla Adaison
| Restio tnticeus Rottb.
Bothalia 23,1 (1993)
163
TABLE 3. — A phytosociological table of the Erica hispidula Shrublands along a transect through the Marloth Nature Reserve, Langeberg,
Swellendam (continued)
Reieve Nuiber <1222*11112*11111111*1111112*11111*1111*11111*11112*11111111*111112*111*11
*7000*55550*33344566*3566660*44569*6777*77789*79990*44444788*688990*678*99
*9456*56787*67957401*8323452*08996*7456*13780*83781*12346209*627123*801*45
plex geological zone of metamorphism, at the contact
between rock of the Malmesbury Group and the Table
Mountain Group (see De Bruyn etal. 1974). These shrub-
lands reflect the presence of soils derived from shales and
other more nutrient-rich sediments.
1.2.1 Leucadendron eucalyptifolium—Hippia pilosa Shrub-
lands (B)
Differential species: see Table 2.
Dominant species: Clijfortia serpyllifolia. Erica hispi-
dula, Erica versicolor, Penaea cneorum subsp. ruscifolia,
Tetraria flexuosa.
Structural formation: varies from a Low Closed Grami-
noid Shrubland with Mid-high Emergent Shrubs to a Mid-
high to Tall Closed Shrubland with an Open to Mid-dense
Graminoid Understorey.
Relationships: Enon Mesotrophic Proteoid Fynbos
(Campbell 1985).
This community (Figure 6) is found at a mean alti-
tude of 447 m (310 —570 m) on the cool lower slopes
below the 'Plaat’. The parent rock is Peninsula For-
mation sandstone and all the soils are classified as
164
Bothalia 23,1 (1993)
TABLE 4 — A phytosociological table of plant communities on the extreme north slopes of the Langeberg, on a transect through the Marloth
Nature Reserve, Swellendam
Community
4
4.2 4.1
P Q
Releve number *1112*11111
*4550*88889
*9010*34569
Altitude (m) .11
.0098.98768
.6600.00384
.0000.00500
Aspect (") .2323.21253
.5002.50053
Glenrosa Form. Aspect of the sample sites is mainly
southerly, ranging from east-south-east to south-south-
west. Mean gradient is 23.4° (14° -32°, n = 5). Rock cover
is low ( < 1% ) with one exception of 25 % in plot 133. Litter
cover is conversely high ranging from 70—85%, with vege-
tation cover 100% in all samples.
This community is weakly differentiated but has strong
affinity to the Penaea cneorum — Widdringtonia nodiflora
Shrublands described below. The most striking feature is
the dominance of Cliffortia serpyllifolia.
1.2.2 Leucadendron eucalyptifolium- Erica vestita Shrub-
lands (C)
Differential species: Erica vestita, Lanaria lanata, Cym-
bopogon marginatus and others, see Table 2.
Dominant species: Cliffortia serpyllifolia, Erica hispi-
dula, Leucadendron eucalyptifolium, Penaea cneorum
subsp. ruscifolia.
Structural formation: Mid-high to Tall Sparse to Closed
Proteoid Shrubland with a Low Closed Graminoid Shrub-
land Understorey or a Low Closed Ericoid Shrubland with
a Mid-dense Graminoid Understorey.
Relationships: Enon Mesotrophic Proteoid Fynbos
(Campbell 1985).
This community (Figure 7) is found on the complex zone
of Malmesbury Group sediments which are exposed below
the ‘Plaaf. There is strong correlation between this com-
munity and the relatively nutrient rich soils of the Malmes-
bury Group sediments. The soils of releves 127, 128 & 130
were 0.2— 0.3 m deep and classified as Glenrosa Form,
whereas those of releves 125 and 126 exceed 1.0 m and
were classified as Clovelly Form soils. The five releves
were sampled at a mean elevation of 283 m (242—320 m)
with a mean gradient of 12.2° (5°— 20°). Cover of exposed
rock was recorded as nil except for sample plot 127 where
a high value of 90% was recorded. Vegetation cover
averaged 96% and litter cover 66%. Four of the five
sample sites had a westerly aspect with the remaining one
on a northeast-facing slope.
Erica vestita is a prominent, easily identifiable differen-
tial species in this community. It has three colour forms,
two of which are found on the Langeberg. The colour form
found in the Leucadendron eucalyptifolium— Erica vestita
Shrublands below the ‘Plaaf is pink, whereas in the Erica
hispidula-Hypodiscus aristatus Shrublands (described
below) the flowers are crimson red. Of further particular
note in this community are Lanaria lanata, Cymbopogon
marginatus and Erica pubigera which appear to favour
soils with a high clay fraction.
Bothalia 23,1 (1993)
165
FIGURE 6. — The Widdringtonia nodi-
flora— Hippia pilosa Shrub-
lands on the lower south slopes
of MNR below the 'Plaat', with
tall Leucadendron eucalypti-
folium in the foreground.
2. Erica hispidula Shrublands of the high elevation zone
The Erica hispidula Shrublands described in this paper
are broadly equivalent to those described by McDonald
(1993). E. hispidula is present in all but one community,
the Hypodiscus aristatus— Erica multumbellifera Shrub-
lands. Speculation as to the reason for this absence is given
below in the description of the latter community. Restio
inconspicuus , which assumes a distinctive yet subordinate
position to E. hispidula in the shrublands of Boosmans-
bos Wilderness Area (McDonald 1993), is less prominent
in MNR.
anceps Community (Bond 1981), Ruitersberg Wet Erica-
ceous Fynbos (Campbell 1985).
Similar to the Erica hispidula— Spatalla nubicola Shrub-
lands of BWA (McDonald 1993), the Erica hispidula—
Brunia alopecuroides Shrublands are found mainly on the
high altitude south- to southwest-facing slopes of the peaks
and ridges of the MNR, in the cool, moist ‘mist zone’
(Figure 8). The substratum consists of decomposed organic
material, forming a deep acid peat, which is classified as
Champagne Form soil.
2.1 Erica hispidula— Brunia alopecuroides Shrublands (D)
Differential species: Brunia alopecuroides , Carpacoce
spermacocea, Erica curviflora, Erica omninoglabra,
Hippia integrifolia, Mairea microcephala, Stylapterus
dubius.
Dominant species: Anthochortus crinalis, Brunia alo-
pecuroides.
Structural formation: Low to Mid-high Closed Brunioid
Shrubland with Closed Restioid Understorey.
Relationships: Brunia alopecuroides— Restio bifidus
Community (Kruger 1974); Simocheilus car neus— Restio
Although the Community is found on the Clock Peaks,
it was not sampled here. Most sample plots (204, 205 &
206) were located on the high-altitude south-facing slopes
of Hermitage Ridge, overlooking Boskloof, with one
sample (Releve 179) situated above the south tributary of
Zuurplaats Stream.
The Erica hispidula— Brunia alopecuroides Shrublands
typically have a low to mid-high (1.0— 1.5 m) closed
brunioid-ericoid overstorey, dominated by Erica curviflora
and Brunia alopecuroides. The understorey is dominated
by Anthochortus crinalis with other herbaceous species
playing an inconspicuous role.
FIGURE 7. — The Leucadendron
eucalypti folium— Erica vestita
Shrublands found on the com-
plex zone of Malmesbury
Group sediments below the
'Plaat'.
166
Bothalia 23,1 (1993)
FIGURE 8. — The Erica hispidula—Brunia alopecuroides Shrublands
found on the high altitude south slopes in the ‘mist zone’.
Of particular note in this community is the presence of
Erica omninoglabra (single occurrence in releve 179), a
rare Langeberg endemic species found sprawling amongst
the matted restioid understorey, Klattia partita (Iridaceae),
a shrubby species with non-fugaceous flowers and the
endemic Stylapterus dubius (Penaeaceae).
2.2 Erica hispidula—Berzelia intermedia Shrublands
These shrublands include four communities which range
from the typical form of the Erica hispidula—Berzelia
intermedia Shrublands (E) to the Berzelia intermedia —
Erica conferta Shrublands on organically rich soils.
Erica hispidula—Berzelia intermedia Shrublands
‘Typicunf (E)
Differential species: none.
Dominant species: Erica hispidula, Tetraria ustulata.
Structural formation: Low Closed Ericoid Shrubland
with sparse Mid-high Emergent Shrubs.
Relationships: Keurbos Wet Ericaceous Fynbos (Camp-
bell 1985).
The Erica hispidula- Berzelia intermedia Shrublands
(Figure 9) have no differential species but have many
species in common with communities F, G and H. These
shrublands may therefore be considered as the ‘back-
ground’ of the mosaic of communities found mainly, but
not exclusively, on the south- to southeast-facing slopes
of Hermitage Ridge and below the Clock Peaks. The
releves (140, 148, 159, 169) representing this community
were located at elevations ranging from 600—1 200 m, with
a moderate mean gradient of 22.5°. The soils are derived
from Peninsula and Goudini Formation sandstone and are
classified as Cartref Form. They are well drained and
shallow with a mean depth of 0.15 m (0.1— 0.2 m) and with
a generally low average surface rock cover of 5%
(2—10%). Projected vegetation canopy cover, in contrast,
is high, ranging from 95-100%.
The dominant stratum of the Erica hispidula—Berzelia
intermedia Shrublands is a Closed Graminoid Shrubland
( < 1.0 m) with dominance shared by the woody shrubs,
Erica hispidula and Fenaea cneorum subsp. ruscifolia, the
sedges Tetraria ustulata and Tetraria flexuosa and the
ubiquitous Restio inconspicuus.
2.2.1. Berzelia intermedia— Erica conferta Shrublands (F)
Differential species: Helichrysum capense.
Dominant species: Anthochortus crinalis, Erica hispi-
dula, Elegia juncea.
Structural formation: Low Closed Ericoid Shrubland
either with Sparse Mid-high Emergent Shrubs or a Tall
Closed Brunioid Shrubland Overstorey.
Relationships: Ruitersberg Wet Ericaceous Fynbos
(Campbell 1985); Simocheilus earn eus— Restio anceps
Community (Bond 1981); Erica hispidula— Spatalla
nubicola Shrublands (McDonald 1993).
This community (Figure 10) is represented by five
releves (155, 156, 157, 158, 207). The only true differen-
tial species is Helichrysum capense since other species
characterizing this community, namely Erica conferta,
Lobelia pubescens and Syncarpha eximia are shared with
FIGURE 9. — The Erica hispidula—
Berzelia intermedia Shrublands
occurring mainly on the south-
facing slopes of the Clock
Peaks and Hermitage Ridge,
forming a ‘background’ to the
mosaic of communities.
Bothalia 23,1 (1993)
167
FIGURE 10. -The Bene lia inter-
media—Erica conferta Shrub-
lands occurring on moist
south-facing slopes below the
Clock Peaks and on Hermitage
Ridge.
the closely allied Erica hispidula—Brunia alopecuroides
Shrublands. On the sample transect the community is
found on the south- and southeast-facing slopes of 12
O’clock Peak at elevations around 1 000 m, on shallow
‘organic phase’ Cartref Form soils. It is also found on the
upper south-southwest-facing slopes of Hermitage Ridge,
above Boskloof (releve 207), where it forms part of a
mosaic with the Erica hispidula—Brunia alopecuroides
Community.
The dominant stratum of this community is a low closed
ericoid layer dominated by Erica hispidula but with a
number of other Erica species such as E. cordata, E. con-
ferta and E. daphniflora. Anthochortus crinalis, Elegia
juncea and Tetraria ustulata are the most important grami-
noid elements. Emergent from the low stratum in some
stands is the fern Blechnum tabulare , with a mid-high to
tall shrub stratum dominated by Berzelia intermedia.
2.2.2 Berzelia intermedia — Grubbia rosmarinifolia
Shrublands (G)
Differential species: Erica regerminans, Grubbia rosma-
rinifolia, Spatalla parilis, Raspalia virgata.
Dominant species: Erica hispidula, Grubbia rosma-
rinifolia, Platycaulos compressus.
Structural formation: Mid-high to Tall Closed Shrub-
land with Closed Graminoid Shrubland Understorey.
Relationships: Brunia alopecuroides— Restio bifidus
Community (Kruger 1974); Chondropetalum— Berzelia
Upper Hygric Fynbos (Boucher 1978); Keurbos Wet
Ericaceous Fynbos (Campbell 1985).
On the sample transect this community (Figure 11) is
found as localized stands on the south-facing midslopes
below the Clock Peaks. One sample (Releve 147) was
located at 1 320 m on the south-facing slopes of Goed-
geloof Ridge, immediately west of Het Goedgeloofnek.
On the mid-slopes of 12 O’Clock Peak at elevations from
600—800 m the community forms part of a mosaic with
other communities in the broader Erica hispidula -Ber-
zelia intermedia Shrublands.
The Berzelia intermedia— Grubbia rosmarinifolia Shrub-
lands are mainly associated with local, apparently
seasonally waterlogged sites. All the releves typical of this
community (136, 137, 139, 147, 154 & 160), were situated
where the soils are boggy. In contrast, releve 161 which
is atypical, and where G. rosmarinifolia was recorded
outside the plot (see Table 3), was located on a more rocky,
well-drained substrate.
FIGURE 11. — The Berzelia interme-
dia—Grubbia rosmarinifolia
Shrublands mainly localized on
the south-facing mid-slopes of
the Clock Peaks. Note the mid-
high G. rosntarinifolia forming
the overstorey.
168
Bothalia 23,1 (1993)
Grubbia rosmarinifolia is strongly differential for this
community. It forms a mid-high to tall, open to closed
shrubland. The understorey may be subdivided into two
strata in some stands. In some cases a mid-high open to
closed ericoid stratum is found immediately below the tall
stratum followed by a closed restioid field layer. In other
stands the ericoid and restioid components combine to
form a low closed field stratum.
In the samples taken, Spatalla parilis (Proteaceae) is
restricted to the Berzelia intermedia— Grubbia rosmarini-
folia Shrublands. Restio arcuatus together with Platycau-
los compressus dominates the restioid component and
Erica regerminans and E. cubica form the greater part of
the ericoid component.
2.2.3 Berzelia intermedia— Cliffortia grandifolia
Shrublands (G)
Differential species: Cliffortia grandifolia, Senecio has-
tatus.
Dominant species: Cliffortia grandifolia, Erica hispi-
dula, Penaea cneorum subsp. ruscifolia, Restio arcuatus.
Structural formation: Low Closed Ericoid Shrubland
with Closed Restioid Understorey and Mid-high to Tall
Open Shrubland Overstorey.
Relationships: Keurbos Wet Ericaceous Fynbos (Camp-
bell 1985).
The Berzelia intermedia— Cliffortia grandifolia Shrub-
land community (Figure 12) also occurs as part of the Erica
hispidula— Berzelia intermedia Shrubland mosaic. It was
sampled mainly on the southeast- to southwest-facing mids-
lopes of 12 O’Clock Peak but occurs in patches over an
extensive area on the south slopes below the Clock Peaks
at elevations from around 600-700 m (above the ‘Plaat’).
The soils are ‘organic phase’ Cartref Form.
The community also occurs on the lower north- to
northeast-facing slopes below the Clock Peaks, in the
Boskloof Valley. These stands are represented by releve
202 situated near Boskloof Hut at an altitude of about 900
m. Here the soils are of Glenrosa Form.
Cliffortia grandifolia is a striking species. It is a tall,
sparingly branched shrub with a thin trunk, often reaching
five metres in height. This species clearly characterizes
the community structurally due to its stature and floristi-
cally due to its faithfulness. Cliffortia grandifolia forms
a mid-high to tall open stratum above a low closed grami-
noid shrubland understorey, dominated by Erica hispidula
and Restio arcuatus. Penaea cneorum subsp. ruscifolia also
contributes significantly to the low stratum (Table 3).
2.3 Erica hispidula— Pentaschistis malouinensis
Shrublands
Differential species: Pentaschistis malouinensis.
Dominant species: Chrysithrix capensis, Erica hispi-
dula, Tetraria flexuosa.
Structural formation: Low to Mid-high Closed Grami-
noid Shrubland.
Relationships: Simocheilus cameus— Restio anceps
Community (Bond 1981); Ruitersberg Wet Ericaceous
Fynbos (Campbell 1985).
This community has no differential species, but shares
P. malouinensis with the Pentaschistis malouinensis—
Tetraria bromoides Shrublands and many other species
with communities E— H (see Table 3). These shrublands
are distinctly graminoid in character, having an abundance
of restios ( Elegia , Platycaulos, Restio), grasses ( Penta-
schistis) and sedges ( Chrysithrix , Epischoenus, Tetraria).
The shrub component is dominated by ericas.
These shrublands are found on north- and south-facing
slopes overlooking Boskloof and on north-facing slopes
in the Langkuilen Valley at altitudes which range from
770—1 330 m. The gradients of sites sampled ranged from
almost level (3°) to moderate (29°). The shallow soils are
derived from Peninsula and Goudini Formation sandstone
and are classified mainly as Cartref and Mispah Forms.
The soil of releve 188, located at the almost level site, con-
sists of organic material in excess of 0.3 m and was clas-
sified as Champagne Form. Rock cover was generally less
than 10% except for releve 172 where 80% was recorded.
The dominant stratum of the Erica hispidula— Penta-
schistis malouinensis Shrublands is a Low Closed
Graminoid Shrubland (<1.0 m) with dominance shared
between the woody ericoid shrubs, Erica hispidula and
FIGURE 12. — The Berzelia inter-
media-Cliffortia grandifolia
Shrublands occurring in pat-
ches over extensive areas of the
south slopes of the Clock Peaks
and in Boskloof. Note the
characteristic tall, slender
Cliffortia grandifolia.
Bothalia 23,1 (1993)
169
FIGURE 13. — The Pentaschistis malouinensis—Tetraria bromoides Shrub-
lands found in Boskioof.
Blaeria coccinea and certain graminoids, particularly
Chrysithrix capensis and Tetraria flexuosa. Psoralea pin-
nata and Widdringtonia nodiflora occur as sparse emergent
shrubs up to 2 m high in some stands.
2.3.1 Pentaschistis malouinensis—Tetraria bromoides
Shrublands (J)
Differential species: Erica pubigera, Helichrysum pan-
durifolium, Leucadendron eucalyptifolium, Leucadendron
salignum, Protea aurea, Tetraria bromoides.
Dominant species: L. eucalyptifolium, P. aurea, T. bro-
moides.
Structural formation: either a Closed Graminoid Shrub-
land with Mid-high Open Shrubland Overstorey or a Mid-
high Closed Shrubland with Tall Mid-dense Proteoid
Shrubland Overstorey.
Relationships: Tetraria bromoides— Erica plukenetii
Community (Kruger 1974); Protea -Tetraria Dry Short
Fynbos (Boucher 1978); Protea aurea— Pteridium aquili-
num Community (Bond 1981); Boesmansbos Azonal
Restioid Fynbos (Campbell 1985); Restio inconspicuus-
Protea aurea Shrublands (McDonald 1993).
The Cedarberg Formation shales crop out in a narrow
band in a west-east direction in the Boskioof Valley.
Drainage is to the east and where the shales are exposed,
they support stands of the Pentaschistis malouinensis—
Tetraria bromoides Shrublands. Three of the sample sites
(Releves 167, 175, 176) were located on shale-derived
yellow-brown, Clovelly Form soils with mean pH 3.8 for
the A-horizon. The fourth releve (174) was situated on
Glenrosa Form soil (pH 3.6) derived from Nardouw
Subgroup sandstone. The estimated mean annual precipi-
tation for the area where these shrublands are found is 800
mm. Elevation ranges from 840—950 m and the gradient
from level (4°) to moderate (36°). Vegetation cover is
usually high (mean 95%) and mean surface rock cover
conversely low at 2.5%.
This community (Figure 13) is classified structurally as
Low to Mid-high Closed Graminoid Shrublands with a
Mid-high to Tall Open (Proteoid) Shrub Overstorey (see
Campbell et al. 1981). Floristically these shrublands are
not well defined compared with the equivalent communi-
ty, the Restio inconspicuus— Protea aurea Shrublands
found in the Boosmansbos Wilderness Area (McDonald
1993). In Boskioof, MNR, Tetraria bromoides is the
most constant differential species with Protea aurea and
Leucadendron eucalyptifolium each found in two of the
four plots. Protea aurea was most abundant in a sheltered
position on the edge of the riparian forest dominated by
Virgilia oroboides (Releve 175). The otherwise marked
absence of stands of P. awmz-dominated vegetation on
the Cedarberg shaleband in Boskioof suggests that this
serotinous, seed regenerating species may have been
adversely affected by past land use regimes (e.g too
frequent or unseasonal fires). L. eucalyptifolium is some-
what more common but its distribution is patchy. This
could indicate scattered outcropping of shale, but since
this species also occurs on sandstones of the Nardouw
Subgroup, no clear reason can be given for its local
distribution pattern.
2.4 Erica hispidula—Hypodiscus aristatus Shrublands (K)
Differential species: none.
Dominant species: Cliffortia heterophylla , Erica hispi-
dula, Restio inconspicuus.
Structural formation: either a Low to Mid-high, Mid-
dense to Closed Shrubland or a Mid-high Closed Shrub-
land with a Low Mid-dense Graminoid Understorey.
Relationships: Nuweberg Mesic Ericaceous Fynbos
(Campbell 1985).
This community (Figure 14) is found mainly on north-
to northeast-facing slopes of the Clock Peak ridge, over-
looking Boskioof, but also on the crest of 10 O’clock Peak
and on north-facing slopes above Langkuilen Valley.
FIGURE 14. — The Erica hispidula-Hypodiscus aristatus Shrublands
found on the north- to northeast-facing slopes of the Clock Peak
ridge. Cliffortia heterophylla dominates the overstorey in this
stand.
170
Bothalia 23,1 (1993)
FIGURE 15. — The Hypodiscus aristatus—Phylica pinea Shrublands found
on the north-facing slopes of Goedgeloof Ridge and on rock
outcrops in the Boskloof Valley.
Elevation of the shrublands ranges from about 1 000 m
to 1 300 m on moderate slopes with a mean gradient of
27° (24°— 28°). Rock cover varies from site to site over
a range from 10—80%, with vegetation cover ranging from
70—95%. Estimated annual precipitation is from 800—900
mm.
The A-horizon of the soils have a mean pH 3.4. They
are derived from Peninsula Formation and Goudini
Formation sandstone and are classified as Cartref Form
(Releves 168 & 170) and Mispah Form (Releve 181).
As indicated above, the community is structurally
variable. The reason for presence of a mid-high closed
stratum dominated by Cliffortia heterophylla in releves 168
& 170 is not clear.
The Erica hispidula— Hypodiscus aristatus Shrubland
community is the typical or 'background' community of
the shrublands where Cliffortia densa, Erica vestita,
Hypodiscus aristatus, Pentameris macrocalycina, Stoebe
cinerea and Thamnochortus cinereus are common ele-
ments (see Table 3). It may be argued that description of
the Erica hispidula— Hypodiscus aristatus Shrublands
based on three releves is tenuous. However, this indicates
inadequate sampling, not the non-existence of the com-
munity.
2.4.1 Hypodiscus aristatus—Phylica pinea Shrublands (L)
Differential species: Ceratocaryum decipiens, Phylica
pinea, Tetraria thermalis.
Dominant species: Erica versicolor, Phylica pinea, Te-
traria ustulata.
Structural formation: Mid-high, Mid-dense Graminoid
Shrubland.
Relationships: Tetraria thermalis— Hypodiscus aristatus
Community (Kruger 1974), Erica viridescens— Hypodiscus
aristatus Community (Bond 1981), Nuweberg Mesic Eri-
caceous Fynbos (Campbell 1985).
This community (Figure 15) is generally Open to Mid-
dense Graminoid Shrublands with a Mid-high Open to
Closed Ericoid Shrubland Overstorey (see Campbell et
al. 1981). This community is found on the north-facing
slopes of Goedgeloof Ridge and on rock outcrops in
the Boskloof Valley. The rocky substrate, with a usual high
percentage of boulders and exposed bedrock, results
in shallow lithosols (<0.20 m) classified here as Glenrosa
and Mispah Forms. In Boskloof the community was
sampled at 920 m (Releves 178 & 201) whereas on Goedge-
loof Ridge the mean altitude for the three sample plots
(Releves 193, 197, 198) was 1 173 m. The area sampled
by the latter plots is mesic and represents a transition zone
from the cooler, moister areas south of Goedgeloof Ridge
to the drier lower slopes (see Table 4 and communities
P & Q).
Phylica pinea is the most constant differential species
in this community. Both Tetraria thermalis and Cerato-
caryum decipiens have a wider distribution on the dry,
north-facing slopes (see Table 4) , therefore their differen-
tial value is diminished. Erica atropurpurea is faithful to
this community but has a low cover-abundance. Domi-
nance in the mid-high shrub stratum is held by Erica
versicolor , which typically favours north-facing rocky
outcrops (McDonald 1993). The lower stratum does not
have a strikingly dominant species but Tetraria ustulata
does stand out as having a higher cover-abundance than
most.
2.4.2 Hypodiscus aristatus— Erica versicolor Shrublands
(M)
Differential species: none.
Dominants: Edmondia sesamoides, Ehrharta setacea
subsp. scabra. Erica hispidula, Hypodiscus aristatus,
Tetraria cuspidata.
Structural formation: Open to Closed Graminoid Shrub-
land.
{
i
FIGURE 16. — The Hypodiscus aristatus— Restio strictus Shrublands are
found at elevations from 1 200- 1 400 in on exposed rocky sites
with shallow soil.
Bothalia 23,1 (1993)
171
Relationships: Nuweberg Mesic Ericaceous Fynbos
(Campbell 1985); Hypodiscus aristatus— Erica versicolor
Shrublands (McDonald 1993).
The habitats in which the Hypodiscus aristatus— Erica
versicolor Shrublands and Hypodiscus aristatus -Restio
strictus Shrublands occur are very similar. This is reflected
in the structural and floristic similarity of these commu-
nities. They differ only in the respective presence and
absence of Erica versicolor and Restio strictus and relative
dominance of the graminoid species. The most apparent
difference is that the Hypodiscus aristatus— Erica versi-
color Shrublands are found on north-facing slopes as
opposed to the south aspect of the Hypodiscus aristatus -
Restio strictus Shrublands. This aspect difference appears
to control the presence or absence of Restio strictus and
Erica versicolor , therefore the difference between the com-
munities is subtle.
Dominance of Hypodiscus aristatus in the graminoid
component is important to note. Rhodocoma alpina Linder
& Vlok (Restionaceae) a species endemic to this commu-
nity (H.R Linder pers. comm.) was not found in any of
the releves but was collected separately.
2.4.3 Hypodiscus aristatus— Restio strictus Shrublands (N)
Differential species: Restio strictus.
Dominants: Chrysithrix capensis, Edmondia sesamoi-
des, Erica hispidula, Ehrharta setacea subsp. scabra,
Pentaschistis colorata.
Structural formation: Closed Graminoid Shrubland.
Relationships: Nuweberg Mesic Ericaceous Fynbos
(Campbell 1985),
This community (Figure 16) is found at elevations from
1 200—1 400 m. These Low Graminoid Shrublands (<1
m) vary from mid-dense to closed, depending on the
locality. They may occur either on exposed rocky sites with
shallow pockets of sandy soil or on sites with deeper soil
and less rock exposed on the surface. The soils derived
from Nardouw Subgroup sandstone vary in depth from
15—30 mm and are classified as Cartref and Mispah
Forms. Aspect is mainly south- and southeast-facing, on
slopes with a moderate gradient (mean 16°). The com-
munity receives an estimated mean annual precipitation
of 1 000—1 200 mm, the soils are highly leached and litter
accumulation is low.
This community is distinct and well differentiated by
Restio strictus. Although ericoid shrubs are well repre-
sented, the graminoid nature of the Hypodiscus aristatus—
Restio strictus Shrublands stands out. Ehrharta setacea
subsp. scabra, Pentaschistis colorata and Chrysithrix
capensis dominate with Restio inconspicuus and Restio
strictus and various sedges playing a subordinate role.
Ursinia trifida has low cover-abundance but is remarkably
constant in the releves and it is interesting to note the
presence of Erica daphniflora. Notable absences are
Lobelia neglecta, Psoralea pinnata and Kniphofia uvaria,
but of prime importance is the absence of Erica versicolor.
This absence distinguishes the community from the Hypo-
discus aristatus— Erica versicolor Shrublands.
FIGURE 17.—' The Hypodiscus aristatus— Erica multumbellifera Shrub-
land found on the north slopes of Goedgeloof Ridge.
2.4.4 Hypodiscus aristatus— Erica multumbellifera
Shrublands (O)
Differential species: Erica multumbellifera, Staberoha
cernua .
Dominant species: Erica melanthera, Staberoha cernua,
Tetraria ustulata.
Structural formation: Closed Graminoid Shrubland.
Relationships: some affinities to the Acid Sand Flats
Community (Boucher 1978).
The description of this community (Figure 17) is based
on two releves, 194 & 195. This small sample size places
a question on the validity of this community concept but
since it is distinctly different from all other communities
described, it is retained for completeness. These shrub-
lands show affinity to the shrublands of high elevation on
shallow soils (Table 3).
The Hypodiscus aristatus— Erica multumbellifera Shrub-
lands were sampled at 1 180 and 1 300 m on the north
slopes of Goedgeloof Ridge. The sites were almost level
with a mean gradient of 6°. The Cartref Form soils were
0.2— 0.4 m deep and almost no rock was exposed on the
surface. Litter was very low and vegetation cover exceeded
95%.
Releve 194 had a more abundant graminoid component
than Releve 195, whereas Erica melanthera was more
abundant in the latter sample. Presence of E. melanthera
suggests impeded drainage in the soil, and a possible
explanation for the existence of this community is wet soil
conditions for part of the year and extremely dry soil for
the remainder. This would preclude species intolerant of
such conditions. A similar regime was found by Boucher
(1978) in the Acid sand flats communities’ where Erica
multumbellifera was also found. Further sampling of the
Hypodiscus aristatus— Erica multumbellifera Community
over a wider range may provide more information about
the habitat factors determining the distribution of this com-
munity.
172
Bothalia 23,1 (1993)
This community is transitional between the communi-
ties of the cool, moist high elevations and those of the
highly insolated, drier north-facing slopes of Goedgeloof
Ridge described below. The transition is reflected in the
species shared with both groups of communities.
3. Leucadendron eucalyptifolium Shrubiands of the
extreme north slopes
The two shrubland communities included in this section
show strong floristic affinities to the shrubiands on the
lower south slopes on the sample transect. This is most
likely due to the apparent equivalent nutrient status of the
soils of the two extreme ends of the transect. Further
investigation of these respective communities and their
underlying environmental relationships is necessary before
this hypothesis can be conclusively tested.
3.1 Leucadendron eucalyptifolium — Erica melanthera
Shrubiands (P)
Differential species: Erica melanthera, Penaea cneorum
subsp. ruscifolia, Psoralea pinnata, Staberoha cernua,
Ursinia nudicaulis (i.e. species occurring in at least three
of four releves).
Dominant species: Leucadendron eucalyptifolium, Te
traria ustulata.
Structural formation: Open to Closed Graminoid Shrub-
land with Mid-high to Tall Open Proteoid Shrubland
Overstorey.
Relationships: Protea neriifolia— Leucadendron euca-
lyptifolium—Erica triceps Community (Bond 1981); Robin-
son Mesic Proteoid Fynbos (Campbell 1985).
This community (Figure 18) is found on the moderately
steep (22°) north-facing slopes of Goedgeloof Ridge
between 800—1 060 m. They are found mostly on shallow
Glenrosa Form soils, but one notable exception was releve
150 where the soil was sandy, 1.5 m deep with a bleached
E-horizon and a podzolised B-horizon. This localized soil
FIGURE 18. — The Leucadendron eucalyptifolium— Erica melanthera
Shrubiands are found on the moderately steep north-facing slopes
of Goedgeloof Ridge.
FIGURE 19. — The Leucadendron eucalyptifolium— Hypodiscus argen-
teus Shrubiands found in a mosaic with the Leucadendron
eucalyptifolium— Erica melanthera Shrubiands on the moderately
steep north-facing slopes of Goedgeloof Ridge.
was classified as Lamotte Form, which is exceptional for
this area. Surface rock cover is highly variable, ranging
from 6-85% and the habitat is well drained.
As delimited here, the Leucadendron eucalyptifolium—
Erica melanthera Shrubland is not floristically clearly
defined. It appears that although a community definition
is possible, the community represents fragments of two
or perhaps more undersampled and undefined communi-
ties. They are grouped together by virtue of commonness
of a few widespread ‘differential’ species but the ‘strings’
of single occurrences in Table 4 support the above con-
clusion. As defined, the community shows affinity to the
communities of the lower south slopes and the high
elevation zone described above under sections 1—3. How-
ever, high cover-abundance of Leucadendron eucalypti-
folium and presence of Elegia galpinii, Hypodiscus striatus
and Anomalanthus scoparius clearly place this commu-
nity apart from those described above.
The Leucadendron eucalyptifolium —Erica melanthera
Shrubiands have two strata. The dominant stratum is
an Open to Closed Graminoid Shrubland which does
not exceed 1 m in height. Above this is an overstorey of
Leucadendron eucalyptifolium (proteoid shrubs) which
varies from open to mid-dense and from mid-high to tall
(1— >2 m).
3.2 Leucadendron eucalyptifolium— Hypodiscus argenteus
Shrubiands (Q)
Differential species: Heteropogon contortus, Hypodis-
cus argenteus, Lanaria lanata, Lobelia capillifolia (i.e.
species with four or more occurrences in five releves).
Dominant species: L. eucalyptifolium, Tetraria ustula-
ta, Restio filiformis.
Structural formation: Open to Closed Graminoid Shrub-
land with Mid-high Open Proteoid Shrubland Overstorey.
Bothalia 23,1 (1993)
173
Relationships: in part, this community is equivalent to
the Phylica axillaris— Felicia filifolia Community (Ruiters-
bos) and Passerina obtusifolia — Felicia filifolia Commu-
nity (Swartberg) of Bond (1981) and Sebrafontein Dry
Asteraceous Fynbos (Campbell 1985).
This community is found on the moderately steep north-
facing slopes of Goedgeloof Ridge, in a mosaic with the
Leucadendron eucalyptifolium— Erica melanthera Shrub-
land at elevations from 680—900 m. The soils, derived
from Nardouw Subgroup sandstone, are classified as Glen-
rosa and Mispah Form. Surface rock cover exceeds 90%
in all releves representing this community but despite this
there is considerable vegetation with a mean projected
canopy cover of 78 % . Estimated mean annual precipita-
tion is 700— 800 mm.
In the Leucadendron eucalyptifolium— Hypodiscus ar-
genteus Shrublands (Figure 19), Leucadendron eucalyp-
tifolium does not exceed 1.2 m and in two releves (185 &
186), Leucospermum calligerum is the dominant proteoid
in the overstorey. The upper stratum varies from a Mid-
high Open to Tall Open Proteoid Shrubland and the lower
(dominant) stratum varies from an Open to a Closed
Graminoid Shrubland.
There are a number of affinities between this Commu-
nity and the communities of the lower south slopes of the
Langeberg above Swellendam. Equally there are numerous
similarities between the Leucadendron eucalyptifolium—
Hypodiscus argenteus Shrublands and the Cannomois
parviflora Shrublands north of Grootberg (McDonald
1993). The Leucadendron eucalyptifolium— Hypodiscus
argenteus Shrublands are mesic in character but may once
again be represented by a group of releves which through
commonness are associated but which may truly be
fragments of other communities, e.g. part of the more arid
Passerina obtusifolia— Leucospermum calligerum Shrub-
lands. This requires further clarification.
DISCUSSION AND CONCLUSIONS
The classification presented in this study was developed
from a phytosociological perspective but with management
of the fynbos shrublands of the Langeberg in mind
(McDonald 1993). Some of the units defined are limited
in extent, and from a management viewpoint it would not
be practical to treat them separately from broader vegeta-
tion units. However, since the classification is hierarchi-
cal, similar communities are grouped together according
to the level of the hierarchy. It is therefore possible for
any manager of the fynbos shrublands of the Langeberg
to select the appropriate level required for any particular
management treatment. Those communities grouped at the
same level may then be treated similarly.
Two problems have been encountered with the methods
used in this study. Firstly, since no initial stratification of
aerial photographs of the study area was done, some com-
munities were undersampled. There is no satisfactory way
of detecting this before analysis of the data. Both the
TWINSPAN and Braun-Blanquet methods of classifica-
tion have indicated communities that have been under-
sampled. The most obvious is the P. malouinensis—
Tetraria bromoides Shrubland found on the Cedarberg
shaleband. Another example is the Hypodiscus aristatus—
Erica multumbellifera Shrubland for which a description
is given. Ideally this community requires further sampling
upon which an adequate description may be based. Frag-
ments of communities recognized in other parts of the
Langeberg are included in the L. eucalyptifolium Shrub-
lands of the extreme north slopes of the transect. In the
TWINSPAN analysis this was shown by releves 185 and
186 being separated from releves 151, 183, 184 and 199
(see also Table 4). Further sampling would clarify whether
this is due to too few samples or that the communities are
simply poorly represented in this part of the Langeberg.
It was not possible to obtain further samples of these com-
munities in this study because the area had been burnt soon
after the initial samples were taken.
It may be argued that a community may be character-
ized by one or two species whose presence is a result of
differential post-fire recruitment (Van Wilgen et al. 1992).
This possibility would increase if the sample size for a
given community is small, which in turn could lead to an
artificial classification. However, each community is not
based solely on the character species but is based on a
specific combination of species for each community. These
combinations should be seen as the key to identifying each
community.
The complexity of the metamorphosed Malmesbury
Group sediments that occur below the ‘Plaaf is reflected
in the vegetation occurring in this part of the MNR. Here
fynbos communities characterized by constant presence
of Clijfortia serpyllifolia are found on soils derived from
quartzites and shales. The Afromontane forests also occur
on the Malmesbury Group shales, but in this case in moist
kloofs.
Although it has been stated that P. aurea may be used
as a ‘marker’, indicating the position of the Cedarberg
Formation shales in the folded strata along the length of
the Langeberg (McDonald 1993), this is a misconception.
A large stand of fynbos dominated by P aurea is found
at the base of 10 O’clock Peak, below the ‘Plaaf, on
Malmesbury shale-derived soil. The response of P aurea
is therefore to the fine-textured shale-derived soils with
higher nutrient status, regardless of their lithological origin
or stratigraphic position.
The vegetation of the MNR appears more complex than
that of the Boosmansbos Wilderness Area (BWA)
(McDonald 1993). This could be ascribed to more com-
plex environmental gradients and a greater diversity of
habitats. However, detailed analysis of environmental data
is needed to substantiate such a claim.
No equivalent of the Restio inconspicuus— Leucadendron
eucalyptifolium Shrubland which is widespread in BWA
is found in the MNR. The Restio inconspicuus— Antho-
chortus crinalis Shrublands of BWA and the Erica
hispidula—Berzelia intermedia Shrublands of MNR are
essentially similar. The communities on the Cedarberg
Formation shale of the two areas are similar except that
the Pentaschistis malouinensis -Tetraria bromoides Shrub-
land is poorer in species. The Cliffortia serpyllifolia Shrub-
lands of the lower south slopes of MNR have no equivalent
in BWA. The reason for the absence of these shrublands
or their equivalent in BWA is not clear but it may be due
174
to the absence of shale-derived soils on the lower south
slopes of the BWA transect.
The Cannomois parviflora Shrublands of BWA are
represented in part by the Leucadendron eucalyptifolium
Shrublands of the extreme north slopes of the MNR
transect, but more extensive sampling and more detailed
analysis is necessary to clarify the classification of these
communities.
Communities identified in different studies from differ-
ent mountain ranges can not be simply equated (McDonald
1993). At the landscape scale there does not appear to be
much difference between the fynbos vegetation of the
Marloth Nature Reserve and the Boosmansbos Wilderness
Area (McDonald 1993). Apparent differences are more
at the level of communities which are micro-habitat rela-
ted. Closer examination is therefore required of (i) the
patterns of distribution of communities on the Langeberg
and (ii) the high turnover of species between communi-
ties and landscapes on the Langeberg. This is beyond the
scope of the present paper but forms a principal part of
further detailed analyses of the vegetation and flora of the
Langeberg (McDonald unpublished).
ACKNOWLEDGEMENTS
Permission granted by the Director-General, Environ-
ment Affairs and the Chief Director, Nature and Environ-
mental Conservation, Cape Provincial Administration
to work in the Marloth Nature Reserve is gratefully
acknowledged. The support of Mr P. van Zyl, Forester,
Swellendam State Forest, and the assistance of Messrs C.
Ruiters, W. Marais, P. Zeier and J. Solomons with field
work is much appreciated. My colleagues at the Stellen-
bosch Herbarium, NBI, Mr E.G.H. Oliver and Mesdames
J.B.P. Beyers and A.C. Fellingham, gave freely of their
expertise in identifying plant collections, and my super-
visors, Dr J.C. Scheepers, Dr C. Boucher and Prof. R.M.
Cowling gave me valuable guidance. My wife, Anne and
my family have also given me much support for which
I am sincerely grateful.
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BOTHALIA
Volume 23,1
May/Mei 1993
CONTENTS — INHOUD
1 . Studies in the Ericoideae (Ericaceae). XII. The placing of the genus Blaeria into synonymy under Erica\
nomenclatural and taxonomic changes for the southern African region. E.G.H. OLIVER 1
2 . Studies in the Ericoideae (Ericaceae). XIII. Three new species of Erica from the southwestern Cape.
E.G.H. OLIVER 9
3 . The hepatics, Symphyogyna podophylla and Pallavicinia lyellii (Pallaviciniaceae) in southern Africa.
S.M. PEROLD 15
4. A biosystematic study of Pentameris (Arundineae, Poaceae). N.P. BARKER 25
5 . Studies in the Marchantiales (Hepaticae) from southern Africa. 1. The genus Dumortiera and D. hirsu-
ta; the genus Lunularia and L. cruciata. S.M. PEROLD 49
6. Panicum simulans (Paniceae, Poaceae), a new species from southern Africa and its leaf anatomy. L.
SMOOK and R.P. ELLIS .V 59
7. Notes on African plants:
Allisoniaceae. The hepatic, Calycularia crispula (Metzgeriales) reported from Malawi and
Zambia. S.M. PEROLD 79
Asteraceae. An evaluation of Hutchinson’s ‘beetle-daisy’ hypothesis. J.J. MIDGLEY 70
Fabaceae. Vigna kokii, a new species from southern Africa. B.J. PIENAAR 68
Fabaceae. Notes on the genus Argyrolobium (Crotalarieae) including a new species from southern
Africa. T.J. EDWARDS 77
Oxalidaceae. A new species of Oxalis from the western Cape. E.G.H. OLIVER 72
Pteridophyta— Adiantaceae. A new cytotype for Acrostichum aureum. J.P. ROUX 75
Rosaceae. Observations on Cliffortia micrantha. A.C. FELLINGHAM 65
Rosaceae. Cliffortia fasciculata, a superfluous name for C. amplexistipula. A.C. FELLINGHAM 67
8. First report on the presence of Enterobryus species (Trichomycetes: Eccrinales) in South Africa and
the description of three new species. G.J.M.A. GORTER 85
9. Mycorrhizal status of plants growing in the Cape Floristic Region, South Africa. N. ALLSOPP and
W.D. STOCK 91
10. Pollen morphology of Curroria, Mondia, Socotranthus and Stomatostemma (Periplocaceae). R.L.
VERHOEVEN and H.J.T. VENTER 105
1 1 . Dynamics of the forest vegetation of the Umtiza Nature Reserve, East London. J.J. MIDGLEY and
P.N. GOBETZ Ill
12 .The vegetation of the northeastern Orange Free State, South Africa: physical environment and plant
communities of the Ea land type. H.C. ECKHARDT, N. VAN ROOYEN and G.J. BREDEN- KAMP
117
1 3 . The vegetation of the southern Langeberg, Cape Province. 1. The plant communities of the Boosmans-
bos Wilderness Area. D.J. MCDONALD.... 129
14. The vegetation of the southern Langeberg, Cape Province. 2. The plant communities of the Marloth
Nature Reserve. D.J. MCDONALD 153
Abstracted, indexed or listed in AGRICOLA, Biological Abstracts, Current Advances in Plant Science, Current Contents, Field Crop Abstracts,
Forestry Abstracts, Herbage Abstracts, Excerpta Botanica, Revue of Plant Pathology, Revue of Medical and Veterinary Mycology and The Kew
Record of Taxonomic Literature.
ISSN 0006 8241
© and published by/obtainable from the National Botanical Institute, Private Bag X101, Pretoria 0001, South Africa. Typesetting: S.S. Brink (NBI).
Reproduction and printing by Execuprint Printers, Adriana Crescent, Gateway Industrial Park, Verwoerdburg. Tel. (012) 661-5131. / Gepubliseer
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