country) and the eastern Transvaal, with occasional distribution northward in the

Similar documents
Occurrence of Small Land Snail Bradybaena similaris (Ferussac, 1822) (Pulmonata: Stylommatophora) in Yangon Environs

A new species of the operculate land snail genus Maizaniella from Liberia (Gastropoda, Caenogastropoda)

New Pupillid Species from Thailand (Pulmonata: Pupillidae)

New subterranean freshwater gastropods of Montenegro (Mollusca: Gastropoda: Hydrobiidae), with description of one new genus and two new species

BASTERIA, 72: , 2008

A new species of Gulella (Pulmonata: Streptaxidae) from montane forest in the Ndoto Mountains, Kenya

Monthly Overview. Rainfall

The endemic West African GLYCYMERIDIDAE species. summary and presentation of two new species

Chapter 6, Part Colonizers arriving in North America found extremely landscapes. It looked different to region showing great.

On the Validity of the Name teyahalee as Applied to a Member of the Plethodon glutinosus Complex (Caudata: Plethodontidae): A New Name

GEOGRAPHY: PAPER II. 1. Write your examination number in the appropriate blocks provided above.

Explain the impact of location, climate, natural resources, and population distribution on Europe. a. Compare how the location, climate, and natural

M. C. WILLIAMS AND J. BOOMKER

Map Projections. Chapter 4 MAP PROJECTION

56H. This system allows definition of points on the Earth s surface to within 100 meters. Page 20. Navigation Systems Basics of Maps

OF MISCELLANEOUS PUBLICATIONS. Volume 11 Dec. 17, Southern Africa. A.C. van Bruggen. "Your worth is very. I take it, your

Using Map and Compass Together

Canadian Mapping Big Book

Lecture 19 Darwin on Geographic Distribution of Species

1. Match the words in the first column to the meaning in the second column. [5]

ON A NEW SPECIES OF AMPHIDROMUS (SYNDROMUS) (GASTROPODA: PULMONATA: CAMAENIDAE) FROM ROTTI ISLAND, INDONESIA

On altitude dependent characters in Albinaria idaea (L. Pfeiffer, 1849), with a revision of the species (Gastropoda Pulmonata: Clausiliidae)

Some of these parallels are very important. In the Northern Hemisphere, there is the Tropic of Cancer and the Arctic Circle.

MAPPING THE EARTH HOW DO YOU FIND A LOCATION ON THE EARTH?

Downloaded from

Chapter 3 Models of the Earth. 3.1 Finding Locations on the Earth. 3.1 Objectives

By: J Malherbe, R Kuschke

by the Bartlett Expedition near the Azores at 37 13'18" N 28 lj'j, 30" W, proved that a related form existed during the Pleistocene ice ages.

Chapter 3 SECTION 1 OBJECTIVES

Earth / Environmental Science. Ch. 14 THE OCEAN FLOOR

Social Studies. Chapter 2 Canada s Physical Landscape

ON TWO SPECIES OF TERRESTRIAL CRABS OF THE GENUS DROMOTHELPHUSA NAIYANETR, 1992 (CRUSTACEA: DECAPODA: BRACHYURA: POTAMIDAE) FROM THAILAND

INTERNATIONAL INDIAN SCHOOL, RIYADH HALF YEARLY

Big Bend Paleo-Geo Journal

THE EARTH AND ITS REPRESENTATION

Continental Landscapes

The Planetary Circulation System

Earthquakes. Earthquakes are caused by a sudden release of energy

Mosquito Systematics Vol. 6(Z) June 1974

discussion of North America s physical features, including its landforms and bodies of

ON THE SPECIES OF SARMATIUM DANA, R. SERÈNE and C. L. SOH National Museum, Singapore

SAFARI 2000 NBI Vegetation Map of the Savannas of Southern Africa

Map Skills Unit. Note taking unit

2. What does the map scale tell the map reader? a ratio between the actual distance on the ground and the length given to that distance on a map

ZOOLOGISCHE MEDEDELINGEN

LOCATIONS IN MELANESIA MOST VULNERABLE TO CLIMATE CHANGE. Stephen J. Leisz Colorado State University

Bulletin Zoölogisch Museum

B. Topographic maps are also called. contour maps

Understanding Projections

OF THREE NEW SUBSPECIES

Page 1. Name:

GEOGRAPHY OCEAN TYPES OF OCEANS Economics Importance of Oceans to Man Relief of the ocean floor Continental Shelf Importance of Continental Shelf

APPENDIX A GLOSSARY. Appendix A.1

A SUMMARY OF RAINFALL AT THE CARNARVON EXPERIMENT STATION,

Phase 1 Cards. Phase 1. Phase 1. How many picnic areas does the park have? Write the answer near the legend.

REVISION: MAPWORK 18 SEPTEMBER 2014

Geographic coordinate systems

The Welsh Borderland. Geologically recent surface deposits. The Welsh Borderland

Map reading notes. It is a very useful kind of map that shows the topography of an area, i.e whether it is flat, undulating, rugged or mountainous

3.13Glaciers past and present

Objectives: Describe the structure of the ocean floor. Describe light intensity and temperature characteristics at different ocean depths.

The Crater Plato as viewed by an

If it ain t broke, then what? Taphonomic filters of late Pleistocene. Terrestrial Gastropod fossils in the Upper Mississippi Valley

GRAAD 12 NATIONAL SENIOR CERTIFICATE GRADE 12

MATHEMATICS: PAPER II. 2. Write your examination number in the space provided in your Answer Book.

Basteria. Tijdschrift van de Nederlandse Malacologische vereniging

A new taxon of the genus Polyommatus Latreille, 1804 from the Transcaucasus (Lepidoptera, Lycaenidae) by A lexandre Dantchenko

Name Date Class. a. High elevation and high relief b. High elevation and level surface c. Flat land and low relief

Chapter 02 The Sea Floor

page - 1 Laboratory Exercise #1 - Introduction to Latitude and Longitude Northern Hemisphere Southern Hemisphere

ZOOLOGISCHE MEDEDELINGEN

Prehistoric sites in the Mount Carmel Area, Israel

Bestwood 1: a newly discovered Earlier Stone Age living surface near Kathu, Northern Cape Province, South Africa

Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE

Microhabitat choice and polymorphism

A new species of Mitra from deep water off South Africa (Gastropoda: Prosobranchia: Mitridae)

THE OHIO JOURNAL OF SCIENCE

Terrain Units PALEOGEOGRAPHY: LANDFORM CREATION. Present Geology of NYS. Detailed Geologic Map of NYS

Student Handout. Write the map s title in the northwest corner of the map. How many picnic areas does the park have? Write the answer near the legend.

Game Ranging / Field Guiding Course. Phylum Mollusca. To gain an understanding of the morphology and biology of common molluscs.

Geographical location and climatic condition of the

The Tswaing Impact Crater, South Africa: derivation of a long terrestrial rainfall record for the southern mid-latitudes

Why study physical features? How does it help me during the course of studying Geography Elective?

Introduction to Geography

THE EARTH S RELIEF SOCIAL SCIENCES 1º ESO

Our Dynamic Earth Unit Unit 5

Dynamic Planet. Student Name. Teacher

Refer to FIGURE 1 which shows how temperatures over a city and its surrounding areas differ. This is an example of microclimate.

Team Name. Name(s) SSSS Unome Geologic Mapping Test Packet p1

Monthly Overview. Rainfall

Topographic Map Series:

Maps and Globes. By Kennedy s Korner

Some Very Helpful Boundary and Border Definitions

VENUS: DETAILED MAPPING OF MAXWELL MONTES REGION

Parts of a Map. Map Skills. The Title. There are 4 main parts of a map: The Title The Compass Rose The Map Key The Scale

1. The topographic map below shows a depression contour line on Earth's surface.

Surveying I. Unit - I. Different methods and instruments are being used to facilitate the work of

Extra Credit Assignment (Chapters 4, 5, 6, and 10)

Earthquake Location regional triangulation with real data

Directed Reading. Section: The Theory of Plate Tectonics. to the development of plate tectonics, developed? HOW CONTINENTS MOVE

Transcription:

wet) BASTERIA, 49: 47-54, 1985 Distribution and size of Gulella viae Bnp. and G. contraria Conn., two South African streptaxids (Gastropoda Pulmonata) A.C. van Bruggen Systematic Zoology section of Leiden university, c/o Rijksmuseum van Natuurlijke Historie, P.O. Box 9517, 2300 RA Leiden, The Netherlands The Drakensberg range, forming interrupted an eastern escarpment in South Africa and further north, is covered with various types of forest on its eastern ( = slopes. These forests harbour a rich assemblage of land molluscs displaying different patterns of distribution. Normally one would expect the escarpment species to be distributed from the interrupted eastern Cape Province mountains to the almost continuous Natal range with further north again scattered occurrence in Swaziland (a poorly collected country) and the eastern Transvaal, with occasional distribution northward in the eastern escarpment on the borders of Zimbabwe (formerly Rhodesia) and Mozambique. Where the range is discontinuous such as in the eastern Cape Province and Transvaal, more or less well-marked endemism may occur and where the interval is of major historical/ecological significance, such as the ancient and arid Limpopo River valley, it act may as a biogeographical barrier. The detailed distribution of the majority of southern African land gastropods is unknown; although many patterns have emerged, these should be considered with suspicion and a number of these have already been emended by newly collected material. Some patterns may reflect collecting activity rather than natural distributions. This may particularly apply to the Natal mountainous areas, which have been well investigated by Henry Clifden Burnup (1852-1928) and his associates; most of this material has been deposited in the Natal Museum at Pietermaritzburg, where Burnup was honorary curator of molluscs in the years 1904-1928. Collecting activities by the present author in the Transvaal in the period 1962-1966have revealed that a number of the Natal Drakensberg species also occur in the Transvaal escarpment forests and are in fact only limited in their distribution by the low-lying and arid Limpopo River valley. In terms of numbersof species the pulmonate family Streptaxidae with slightly more than 20% ofthe total number of species of land gastropods, occupies a dominant position in southern Africa. The majority of these streptaxids are classified with the genus Gulella L. Pfeiffer, 1856. The numerous species exhibit various types of distribution (see e.g., Connolly, 1939; Van Bruggen, 1969, 1973, 1980). A number of the species occurs on the eastern escarpment, two of which, hitherto known only from Natal, have now been recorded from the Transvaal. Gulella viae was thought to be exclusive to the higher reaches of the Natal Drakensberg, and G. contraria, interesting because of its isolated position among its congeners, was only known from Vryheid, Natal. Therefore no apology is needed for a somewhat detailed treatment of these taxa. Material has been studied belonging to the following collections: British Museum (Natural History), London (abbreviated BM); Durban Museum and Art Gallery, Durban, South Africa (DM); Natal Museum, Pietermaritzburg (NM); Rijksmuseum

Shell G. A 48 BASTERIA, Vol. 49, No. 1-3, 1985 van Natuurlijke Historie, Leiden (RMNH); South African Museum, Cape Town (SAM). Other abbreviations used are ale. for alcohol, and 1/d for the ratio length/major diameter of shells, which gives an impression of the shape of the shell (1/d have been calculated from micrometer readings). Acknowledgements are due to the curators in charge for allowing study of their material; particular mention should be made ofdr. E. Gittenberger (RMNH), whose gallant trials to obtain a radula from G. viae unfortunately came to naught, and Dr. P.B. Mordan (BM). H. Heijn (Leiden university) deserves great credit for his professional art work. Van Bruggen (1980) has been followed for style of description, etc. Gulella viae Burnup, 1925 (figs. 1, 3-5) Gulella viae Burnup, 1925, Ann. Natal Mus. 5: 143, pi. 9 figs. 47-51; Connolly, 1939, Ann. S. Afr. Mus 33: 78; Van Bruggen, 1973, Malacologia 14: 422. Diagnostic characters. small, costulate species with a comparatively small and constricted aperture with six-fold dentition consisting of angular lamella, two labral processes, a basal denticle, and a duplex columellarlamella, of which angular lamella and labral complex are comparatively very large. Description of shell. (figs. 1, 3, 4) small, subcylindriform to elongate-ovate or suboval, rimate or with closed umbilicus. Spire produced, sides straight to slightly convex, subparallel, apex flattened to obtusely conical. Whorls 6 [ A-7 %, slightly convex, sculptured with close, regular, fairly straight, oblique and prominent costulae, interstices about as wide as costulae, smooth, under high magnification very finely granulate; sutures (fairly) deeply impressed, (sub)crenellate. First two whorls finely granulate and smooth. Aperture obliquely ovate, actual opening rather narrow and somewhat constricted, peristome thick, expanded, somewhat reflected, white and glossy, aperture much obstructed by six-fold dentition: large and prominent angular lamella, which protrudes beyond the labral complex and is also quite prominent in profile, connected with the apex of the labrum in such a way that in side view an almost circular opening can be seen; labral complex consisting of small upper process, partly hidden by the angular lamella, and a larger lower process (sometimes more like an inrunning lamella) on a common base, the complex corresponding to a deep and extensive outside depression; deeply a set mid-basal tubercle; outer columellar in the process form of a ridge with a cusp at its bottom, inner columellarlamella large and deeply situated. Measurements of shell: 2.8-3.4 x 1.5-1.7 mm, 1/d 1.73-2.25. The type measures 3.1 x 1.6 1/d 1.94. Smallest mm, specimen (Mariepskop Forest Reserve, NM) 2.8 x 1.6 mm, 1/d 1.80, largest shell (Hanglip Forest, NM) 3.4 x 1.7 mm, 1/d 1.96. An average specimen (Van Reenen's Pass, RMNH, fig. 1) measures 3.2 x 1.6 mm, 1/d 2.04, aperture 0.9 x 0.9 last whorl mm, 1.6 mm. Distribution (fig. 5). in both Natal and the Transvaal. viae occurs on the Drakensberg range above about 800 m NATAL: Mt. aux Sources, W. Falcon (NM); Van Reenen's Pass, H.C. Burnup (BM 1925.4.21.9, holotype; BM 1937.12.30.1286-89, 4 paratypes; NM 3548, type 587, 7 paratypes; NM type 587, 1 and 3 paratypes respectively; NM, 3 paratypes;

Pietermaritzburg) Van Bruggen: Gulella viae and G. contraria, South African Streptaxidae 49 NM, RMNH); do., W.G. Rump (NM); do. (DM, Puzey colln. 12); Paulpietersburg (Connolly, 1939: 78). TRANSVAAL: Barberton, R.F. Lawrence (NM ale.); do., H.J. Puzey (DM, Puzey colln. 12; SAM A30001); Pilgrim's Rest District, Mariepskop Forest Reserve, NE. (Nature Reserve), area montane forest at about 1500 m, A.C. & W.H. van Bruggen (NM, NM ale., RMNH, RMNH ale.); Hanglip Forest near Louis Trichardt, c. 1400 m, A.C. & W.H. van Forest near Sibasa, c. 1200 m, A.C. & W.H. van Bruggen (NM). Bruggen (NM); Tate Vondo Type locality: Van Reenen's Pass (c. March, 1918. 1700 m), where first collected by Burnup in Figs. 1-2. Shells of South African Gulella. 1, G. viae Bnp., Van Reenen s Pass, Natal (length 3.2 mm, RMNH); 2, G. contraria Conn., Vryheid, Natal (length 4.5 mm, paratype, NM). Specimens from "Maritzburg" ( = (BM 1956.5.12.15-17, Price- Jones colln.) have been considered wrongly localized. Although G. viae occupies a large area, but obviously with an assemblage of scattered and isolated few differences have been found in the biometrical populations, data, as demonstrated by the following table:

50 BASTERIA, Vol. 49, No. 1-3, 1985 Natal Drakensberg 2.9-3.4 x 1.5-1.7 mm, 1/d 1.84-2.25, n > 100 = Barberton 3.0-3.2 x 1.5-1.6 mm, 1/d 1.92-2.12, n 4 = Eastern Transvaal 2.8-3.3-x 1.6-1.7 1/d mm, 1.73-2.04, n 12 = Northern Transvaal 3.0-3.4 x 1.5-1.7 1/d mm, 1.85-1.96, n 6 = These dataare based on inadequate samples, so that any conclusions drawn should be treated with suspicion. Sufficientmaterial is available for the Natal localities, which are not all that far apart. It is shown that almost the full range of variation already occurs in this, the southern part ofthe area occupied by the species. However, attention might be drawn to the 1/d, where there is a seemingly noticeable difference between the Natal populations (1.84-2.25, mean 2.04) and the Transvaal mean populations (1.73-2.12, 1.92), which implies that the shells in Natal are somewhat more slender than those in the Transvaal. The at the bottom of the outer columellarlamella is sometimes cusp really denticle; a the ridge itself can be very weak indeed. One shell (Van Reenen's Pass, NM) is abnormal, having a repaired aperture with much reduced dentition; a reduced labral complex and inner columellar lamella are all that is left. If this specimen had not been found in a sample of G. viae, it would have been very difficult to identify. At times there is sufficient minor variation in apertural dentition for doubt to arise as regards identity of specimens or populations. Initially the Mariepskop material was considered to represent a separate taxon on a specific or subspecific level. However, there is sufficient overlap in almost all characters for it to be considered part of G. viae, particularly in view of its range of variation as now known. Figs. 3-4 depict the Mariepskop material as compared to a specimen from Natal (fig. 1). Numerous minor differences be may observed, such as shape and costulation, size and shape of the columellar lamella, and size and shape of the labral complex. Also, the aperture in the Mariepskop material is more constricted. In Natal material the aperture is usually about as long as wide (e.g., 0.9 x 0.9 mm in the specimen of fig. 1), in the Mariepskop specimens it is always longer than wide (e.g., 1.0 x 0.7 mm in the specimen of fig. 3). My colleague, Dr. E. Gittenberger of the Leiden museum, has vainly tried to obtain a radula for inspection and comparison with the data in Aiken's 1981 paper. G. viae ranges vertically from approximately 750 m to about 2500 m in various types of forest termed Afromontane by White (1978). Its distribution is restricted by the upper limits of forest on the east slopes of the Drakensberg escarpment, which limits occur at about 2500 m. The total area discontinuously inhabited by the species probably lies between the Limpopo River valley in the north and about 30 S in western Natal. It is confidently expected to occur in the many forests in the Transvaal that so far have been poorly sampled. Indeed, in a voluminous correspondence with Dr. H.E. van Hoepen (Germiston, South Africa), neurologist/psychiatrist and amateur malacologist of note, there are indications of G. viae elsewhere in the Transvaal. Dr. van Hoepen's camera lucida drawings of Gulella shells are very good indeedand onthe strength of his unpublished figures two localities have been provisionally incorporated on the map (fig. 5), viz., Magoebaskloof near Tzaneen and Ofcolaco approximately 50 km south of Tzaneen. Gulella contraria Connolly, 1932 (figs. 2, 5) Gulella contraria Connolly, 1932, Ann. Natal Mus. 7: 88, pi. 4 fig. 17; Connolly, 1939, Ann. S. Afr. Mus 33: 97 between (author erroneously brackets); Zilch, 1961, Arch. Molluskenk. 90: 93.

Van Bruggen: Gulella viae and G. contraria, South African Streptaxidae 51 Figs. 3-4. Shell of Gulella viae Bnp., Mariepskop Forest Reserve, Transvaal (length 3.0 mm, RMNH); the aperture is highly enlarged in order to show the dentition in detail.

G. A Shell 52 BASTERIA, Vol. 49, No. 1-3, 1985 Diagnostic characters. small, smooth species with the aperture much obstructed by six-fold dentition consisting of angular lamella, double labral lamella, a basal denticle, a large superficial columellar process, and an insignificant inner columellar lamella. Description of shell. (fig. 2) small, cylindrical to elongate-ovate, (sub)rimate. Spire produced, sides subparallel, slightly convex, apex obtusely conical. Whorls 6 Vi-7%, flattish, smooth or with faint traces of growth striae; sutures fairly shallow, simple. Aperture elongate-ovate, slightly constricted and well obstructed by six-fold dentition: well-developed angular lamella, flattened in front view, connected with the apex of the labrum; duplex labral lamella shaped like an inverted V, apex usually with acute denticle, outer superficial, inner arm arm ofinverted V more deeply situated, correspondng to a longish and shallow outside depression; deeply situated basal denticle to the left of the base, corresponding to insignificant outside depression; squarish and superficial outer columellar process protruding far as as the middleof the aperture; insignificant inner columellar fold. Measurements of shell: 3.7-4.7 x 1.8-2.2 mm, 1/d 1.97-2.19.The type measures 4.7 x 2.2 mm, 1/d 2.14. Smallest specimen (Mbabane, NM) 3.7 x 1.9 mm, 1/d 1.97, largest shell (type), second largest shell (Vryheid, NM) 4.5 x 2.2 mm, 1/d 2.06. An average specimen (Vryheid, SAM) measures 4.3 x 2.2 mm, 1/d 1.97, aperture 1.4 x 1.1 mm, last whorl 2.2 mm. Distribution (fig. 5). contraria is only known from altitudes of over 750 m in northern Natal, Swaziland and adjoining of the Transvaal. parts NATAL: Vryheid, H.J. Puzey (BM1937.12.30.1289, holotype ;BM1931.6.3.54-59, 6 paratypes; DM, Puzey colln. 22; NM type 543, 2 paratypes; SAM A7653, SAM A7659). SWAZILAND: Mbabane, R.F. Lawrence (NM). TRANSVAAL: Barberton, H.J. Puzey (DM, Puzey colln. 22; NM). Type locality: Vryheid, where first collected by Puzey some time before 1931 Two specimens from "Zululand", H.C. Fulton (RMNH) have ex not been included in the above distribution records. Although the uplands of north-western Zululand might well harbour the present species (fig. 5), this record has been ignored for the present, because the experience learns, that the general label "Zululand" in most causes indicates lowland rather than the higher areas. Little material (a total of 28 specimens from 4 localities) is available; nevertheless it seems worth while to compare the measurements: Vryheid 4.0-4.7 x 1.9-2.2 mm, 1/d 1.97-2.14, n = 13 Mbabane 3.7-3.8 x 1.8-1.9 mm, 1/d 1.97-2.10, n = 6 Barberton 4.1-4.5 x 2.0-2.1 mm, 1/d 2.03-2.19, n = 7 The material from Vryheid and Barberton agrees well in size and shape. Incidentally, the "Zululand" shells have measurements entirely within the range of variationof the Vryheid/Barberton specimens. In this context it is interesting to mention that Barberton is about 300 m lower than Vryheid and also approximately 2 latitude further north; Barberton indeed enjoys a much warmer climate than Vryheid. The Swaziland specimens are considerably smaller than the others; Mbabane is only a little lower in elevation than Vryheid and is situated some 60 km south of Barberton. There is little difference in climate between Mbabane and Barberton. This once again shows that aknowledge of the local topography does not always solve problems such as these.

Maputo, Pretoria, Port Van Bruggen: Gulella viae and G. contraria, South African Streptaxidae 53 Fig. 5. Distribution of Gulella viae Bnp. (dots; unconfirmed localities shown as circles) and of G. contraria Conn. (triangles). The following abbreviations have been used for major towns: B = Bloemfontein, D = Durban, EL = East London, J = Johannesburg, M = P = PE = Elizabeth. Obviously G. contraria does not exhibit a size cline nor can be divided into subspecies. Scattered populations have become isolated from each other with concurrent lesser gene flow, which in many cases would be absent altogether. The activities of man, mainly in the form of (selective) cutting of the forest greatly fosters this the process; isolation of populations of land snails, or for that matter, any cryptozoic organism inhabiting leaflitter on the forest floor, will become more pronounced in the near future. This means that flow will become gene even more restricted. The apertural dentitionof G. contraria, described by Connolly (1932, 1939) as fivefold because of the absence of an inner columellar lamella, may just as well be con-

, Ann. Arch. Rev. Zool. Zool. Ann. Ann. 54 BASTERIA, Vol. 49, No. 1-3, 1985 sidered six-fold since a close scrutingy reveals the presence of an insignificant process on the columella deep down in the aperture. A duplication ofthe columellar process is not uncommon in the Gulella; about genus a third of the southern African species does show this character. A duplex labral complex to be appears rare. In southern Africa it has also been observed in G. incurvidens Van Bruggen, 1972, from the Mariepskop Forest Reserve, but the shellof this species is unusual to such a degree that this character would almost be overlooked. However, it appears that in G. incurvidens the duplex labral process is also shaped like an inverted V. There are a few other species with a double labral lamella north of the Zambezi River. Connolly (1932: 88) refers to G. porcina Connolly, 1930, from Uganda, in many respects also vastly different from G. contraria, not only by its apertural dentition, but also by its giant size. The genus Gulella displays an enormous diversity in the Afrotropical Region. While some distribution patterns are seemingly straightforward and explained without too much trouble, much remains a mystery in this context. Van Bruggen (1980: 58) writes "Analysis of clinal variation and subspecies has failed to reveal a common pattern of correlation between shell characters and biotic/abiotic factors". Variation in shell biometrical data of the above treated two cases shows, that at least in these it may be a sequel to interruption of once continuous ranges. Increasing aridity of Africa has resulted in the fragmentation of formerly continuous forest complexes and their faunas, which must account for the sometimes noticeable differences in shell size and shape. REFERENCES AIKEN, D.W., 1981. Differentiation of the radula of South African species of the genus Gulella into three types (Gastropoda Pulmonata: Streptaxidae). J. Conch. Lond. 30: 317-323. BRUGGEN, A.C. VAN, 1969. Studies on the land molluscs of Zululand with notes on the distribution of land molluscs in southern Africa. Verh. Leiden 103: 1-116., 1972. On a peculiar new species of Gulella (Mollusca, Gastropoda Pulmonata: Streptaxidae) from the Transvaal. Zool. Bot. Afr. 85: 169-173. 1973., Distribution of the patterns Gulella genus (Gastropoda Pulmonata: Streptaxidae) in southern Africa. Malacologia 14: 419-425. 1980. Size clines and subspecies in the streptaxid genus Gulella Pfr. (Mollusca, Gastropoda Pulmonata) in southern Africa. Verh. Leiden 180: 1-62. BURNUP, H.C., 1925. On some South African Gulellae, with descriptions of new species and varieties. Natal Mus. 5: 101-158. CONNOLLY, M., 1932. New South African Gulellae, with notes on certain other species. Mus. 7: 67-90. Natal, 1939. A monographic survey of South African non-marine Mollusca. S. Afr. Mus. 33 1-660. WHITE, F., 1978.The Afromontane region. In: M.J.A. WERGER (4 A.C. VAN BRUGGEN), ed., Biogeography and ecology of southern Africa (1): 463-513. The Hague. ZILCH, A., 1961. Die Typen und Typoide des Natur-Museums Senckenberg, 24: Mollusca, Streptaxidae. Molluskenk. 90: 79-120.