'1 7? \ 01? BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 1976-1977 BRITISH MUSEUM (NATURAL HISTORY) LONDON: 1977 DATES OF PUBLICATION OF THE PARTS No. I . . . . -24 June 1976 No. 2 . . . . . -24 June 1976 No. 3 . . . . -23 September 1976 No. 4 . . . . -23 September 1976 No. 5 ..... 28 October 1976 No. 6 . . . . -25 November 1976 No. 7 . . . . -25 November 1976 No. 8 ..... 27 January 1977 No. 9 ..... 27 January 1977 ISSN 0007-1498 Printed in Great Britain by John Wright and Sons Ltd. at The Stonebridge Press, Bristol BS4 5NU CONTENTS ZOOLOGY VOLUME 30 PAGE No. i. Bats referred to Hesperoptenus Peters, 1869 (Chiroptera : Vesper- tilionidae) with the description of a new subgenus. By J. E. HILL (Pis 1-4) i No. 2. Taxonomy and distribution of the Metapheretima elongata species- complex of Indo-Australasian earthworms (Megascolecidae : Oligo- chaeta). By E. G. EASTON ....... 29 No. 3. The taxonomy of Conchoecia (Ostracoda, Halocyprididae) of the gaussi and edentata groups from the northeast Atlantic with a note on their ecology. By A. J. GOODAY ...... 55 No. 4. Echinoderms from the northern region of the Great Barrier Reef, Australia. By P. E. GIBBS, A. M. CLARK and C. M. CLARK (PI. i) . 101 No. 5. Miscellanea Tilapiine fishes from crater-lakes of Lake Malawi. By E. TREWAVAS (Pis 1-3) 149 A new species of Hemichromis (Pisces, Cichlidae) of Sierra Leone and Liberia. By A. I. PAYNE and E. TREWAVAS (PI. i) . . 159 A possible intergeneric cyprinid hybrid from Lake Tanganyika. By K. E. BANISTER (Pis 1-2) ....... 171 Two new species of large Barbus (Pisces, Cyprinidae) from central Africa. By K. E. BANISTER (PL i) 191 No. 6. Miscellanea A new genus and two new species of copepod parasitic on freshwater fishes. By G. A. BOXSHALL 209 A new species of Chonopeltis (Crustacea : Branchiura) from southern Africa. By G. A. BOXSHALL ....... 217 Microlaophonte trisetosa sp. nov., a new harpacticoid copepod from southern Florida. By G. A. BOXSHALL ..... 223 A new species of Amphithoe (Pleonexes) (Amphipoda : Amphithoidae) from the northeast Atlantic with a redescription of A. (P.) gam- maroides (Bate). By R. J. LINCOLN 229 The first zoeal stage of Scopimera crabricauda Alcock (Crustacea, Brachyura, Ocypodidae). By A. L. RICE 243 Asterozoa from Amsterdam and St. Paul Islands, southern Indian Ocean. By AILSA M. CLARK (Pis 1-6) ..... 247 Restriction of the family Poraniidae, sensu Spencer & Wright, 1966 (Echinodermata : Asteroidea). By F. H. C. HOTCHKISS and AILSA M. CLARK (Pis 1-3) ......... 263 No. 7. Variation in Eurasian shrews of the genus Crocidura (Insectivora : Soricidae). By P. D. JENKINS ....... 269 No. 8. Biology and fine structure of Cryptodifflugia oviformis (Rhizopodea : Protozoa). By R. H. HEDLEY, C. G. OGDEN and N. J. MORDAN (Pis 1-6) 311 No. 9. The larval and post-larval development of the scorpion spider crab, Inachus dorsettensis (Pennant) (Family : Majidae), reared in the laboratory. By R. W. INGLE ....... 329 BATS REFERRED TO HESPEROPTENUS PETERS, 1869 (CHIROPTERA : VESPERTILIONIDAE) WITH THE DESCRIPTION OF A NEW SUBGENUS J. E. HILL BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. i LONDON: 1976 •BATS REFERRED TO HESPEROPTENUS PETERS, 1869 (CHIROPTERA : VESPERTILIONIDAE) WITH THE DESCRIPTION OF A NEW SUBGENUS BY JOHN EDWARDS HILL Pp. 1-28 ; 4 Plates ; 5 Text-figures BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. i LONDON: 1976 THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be completed within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30, No. i, of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation : Bull. Br. Mus. not. Hist. (Zool.) ISSN 0007-1498 Trustees of the British Museum (Natural History), 1976 BRITISH MUSEUM (NATURAL HISTORY) Issued 24 June, 1976 Price £3-20 BATS REFERRED TO HESPEROPTENUS PETERS, 1869 (CHIROPTERA:VESPERTILIONIDAE) WITH THE DESCRIPTION OF A NEW SUBGENUS By J. E. HILL CONTENTS Page SYNOPSIS ........... 3 INTRODUCTION ........... 3 HISTORY ............ 4 Genus Hesperoptenus Peters, 1869 ....... 5 Hesperoptenus (Hesperoptenus) Peters, 1869 ..... 6 Hesperoptenus doriae (Peters, 1869) ...... 7 Hesperoptenus (Milithronycteris) subgen. nov. . . . . . 14 Hesperoptenus tickelli (Blyth, 1851) . . . . . . 15 Hesperoptenus tomesi Thomas, 1905 . . . . . . 19 Hesperoptenus blanfordi (Dobson, 1877). ..... 21 RELATIONSHIPS .......... 24 ACKNOWLEDGEMENTS ......... 25 REFERENCES ........... 26 SYNOPSIS Species currently allocated to the vespertilionid genus Hesperoptenus are reviewed in detail and divided into two subgenera, one, Hesperoptenus (Milithronycteris} with type species Nyctice- jus tickelli Blyth, 1851, proposed as new, to include also H. blanfordi (Dobson, 1877) and H. tomesi Thomas, 1905. The nominate subgenus contains only its type species H. doriae (Peters, 1869), here reported for the first time from Malaya, this being the second record of the species, hitherto known only from its holotype from Sarawak, Borneo. INTRODUCTION BATS of the Asiatic genus Hesperoptenus are, in general, rarely collected and therefore do not feature extensively in museum collections. Consequently, they remain for the most part rather poorly known and, apart from one Indian species, have received only scant attention in the literature. As it is currently recognized, Hesperoptenus is held to include four species, doriae, tickelli, tomesi and blanfordi. Their association together has been considered open to doubt by some authors while the most recent definition of the genus is based upon tickelli rather than upon the type species doriae. In this account the four species are examined and compared and although the number of specimens available remains small in some it has been possible nevertheless to describe the features of each species in detail and to discuss their differences and possible relationships. As a result, Hesperoptenus as previously understood is divided into two subgenera, one described as new, 4 J. E. HILL HISTORY The name Hesperoptenus was proposed by Peters (i86ga : 626) for a subgenus of Vesperus, with type species V. (H.) doriae described concurrently from Sarawak, Borneo. Shortly afterwards, Peters (i869b : 638) described V. (H.) kraussi from Yoruba, Lagos, Nigeria, nowadays considered a synonym of Glauconycteris poensis (Dobson, 1878 : 255 ; Thomas, 1913 : 145 ; Rosevear, 1965 : 275). The two species described by Peters are figured together in his posthumous publication of illustrations of Chiroptera from the Zoologische Museum, Berlin (1906, pi. 26), and in this are referred to Vesperus, with no mention of Hesperoptenus. Dobson (1876 : 112) in a monographic study of the Asiatic Chiroptera placed doriae in the genus Vesperugo, largely repeating the description by Peters, in translation. Dobson remarked that he thought doriae to be closely allied to Vesperugo tickelli (Blyth, 1851) and that when specimens of both could be compared it would be found that they could be included together in the subgenus Hesperop- tenus. Later, Dobson (1877 : 312) described Vesperugo (Hesperoptenus) blanfordi and so implicitly recognized Hesperoptenus as a subgenus. Subsequently, he (1878 : 239) defined Hesperoptenus as a subgenus of Vesperugo, to include doriae, tickelli and blanfordi. In the same work (p. 255) Dobson reduced Vesperus (Hes- peroptenus) kraussi Peters, 1869 to the synonymy of Glauconycteris poensis, where it has since remained. Eventually, Hesperoptenus as understood by Dobson was raised to generic rank (Jentink, 1887 : 278 ; 1888 : 182 ; Wroughton, 1897 : 723 ; Trouessart, 1897 : 116 ; 1904 : 83), with Thomas (1905 : 575) describing a fourth species, tomesi. The essentials of the classification proposed by Dobson have persisted until the present day. Miller, the monographer of bat genera, retained (1907 : 211) generic rank for Hesperoptenus but examined only tickelli, which he employed as the basis for his generic diagnosis. This definition moved from the concept established by Dobson (1878 : 239), who, following Peters, had characterized the subgenus Hes- peroptenus by 'outer upper incisors very small, scarcely raised above the gum, generally posterior to the toothrow ; penis with a distinct bone ; post-calcaneal lobe well-developed ; wings from the base of the toes'. Dobson had not seen doriae which he stated differed from tickelli and blanfordi in that the outer upper incisors were in the toothrow and not posterior to it as in these species. Miller (1907 : 211) diagnosed Hesperoptenus almost entirely by the features of the dentition, relying largely on the configuration and position of the upper incisors. Since, like Dobson, Miller did not examine doriae, he employed Hesperoptenus with some hesitation, considering that the description of doriae by Peters indicated certain features suggesting that it might be generically distinct from both tickelli and blanfordi. Miller did note, however, that peculiarities of the prepuce and the presence of a large bone in the penis might indicate (as Dobson had thought with regard to the os penis or baculum alone) that the three species formed a distinct group (Miller did not include tomesi, of which he appears to have been unaware) but remarked that the value of these characters was not then well understood. More recently, Tate (1942 : 268) considered Miller correct in the supposition that more than one genus was involved, but was unable to study either doriae or blanfordi. BATS REFERRED TO HESPEROPTEN US 5 This author referred to the position of the outer upper incisor in doriae and suggested further that the specialized thumb of blanfordi might be an indication that it too differed widely from its supposed congeners. Ellerman & Morrison-Scott (1951 : 174), who drew attention to this situation, pointed out that the holotype of doriae ap- parently remained unexamined and that the genus Hesperoptenus might prove untenable in the sense in which it was then accepted. Davis (1962 : 42) referred a specimen from Sabah, Borneo, to doriae, noting that in this example the outer upper incisor was displaced posteriorly. This circumstance led Medway (1965 : 65) to consider that the type species thus conformed to the current generic definition, thereby rendering groundless the speculation by Ellerman & Morrison-Scott. The example from Sabah, however, does not represent the type species but instead should be referred to tomesi, of which it is a juvenile male (Hill, 1972 : 38 ; vide infra). It is clear that the taxonomy of Hesperoptenus, so far unresolved, can be clarified only by the detailed examination of the holotype of doriae, upon which any inter- pretation of the genus must turn. The original description by Peters and a brief note of forearm length, colour and incisive dentition by Hill (1972 : 38) appear to be the only published accounts based upon direct examination of the holotype, which is in the Museo Civico di Storia Naturale 'Giacomo Doria', Genoa. This specimen, until recently the only definitively known example of the species, was examined also by Oldfield Thomas, who, in a copy of Dobson's Catalogue of the Chiroptera in the Collection of the British Museum, 1878, now in the Library of the British Museum (Natural History), has annotated the remark 'Specimen sent over 12/1901' to the account of doriae. Thomas has added manuscript notes on the external features, baculum and incisive dentition, with some measurements, to the account by Dobson. Shortly after the holotype was studied during the early preparation of this paper, a second specimen of doriae was obtained quite by chance in Malaya by Lord Medway, almost exactly one hundred years after Peters first acknowledged the species. Genus HESPEROPTENUS Peters, 1869 Hesperoptenus Peters, i86ga : 626 (as a subgenus of Vesperus). Type species Vesperus (Hesperoptenus} doriae Peters, 1869, from Sarawak, Borneo. DIAGNOSIS. Similar to Eptesicus but differing from this genus in relatively wider palate with wide anterior emargination ; in the presence of well-developed basioccipital pits ; in larger, caniniform inner upper incisor (i2), its basal area equal almost to one half that of the upper canine (c1) ; and by the structure of the outer upper incisor (i3) which is low, its tip reaching barely to the cingulum of i2 or of c1, with basin-like cingulum and low central cusp. Dentally similar to Glauconycteris but differing from this genus and from the closely related Chalinolobus in having the posterior margin of the ear terminating on the head at a point not much anterior to the insertion of the anterior margin, not extending almost to the corner of the mouth, and in the absence of a fleshy lappet on the lower lip near this point. The majority of species of Hesperoptenus differ further from Eptesicus, Glauconycteris and Chalinolobus in the marked inward displacement of i3 from the toothrow. 6 J. E. HILL DESCRIPTION. Muzzle low and wide, sparsely furred anteriorly ; narial openings semi-lunate or nearly circular, opening sub-laterally ; usually a small wart-like protuberance above the anterior canthus of the eye, bearing a few long whiskers ; lower lip with broad median pad ; a small naked or nearly naked area immediately beneath the symphysis menti, preceding a low wart which bears a few long hairs. Ear subquadrangular ; anterior margin with rounded or very slightly pointed posteriorly directed basal lobe ; tip of ear rounded ; posterior margin with promi- nently developed antitragal lobe effecting a quadrate junction with the side of the head behind and level with the angle of the mouth, from which it is separated by a low wart bearing a few longer hairs. Tragus slightly hatchet-shaped, its upper part prolonged anteriorly. Metacarpals of third, fourth and fifth digits nearly equal in length, the third usually very slightly the longest ; a well-developed post-calcarial lobe, sometimes supported by a cartilaginous spur ; penis with wide, saccular prepuce with large terminal opening. Skull with wide braincase, the frontal region not especially inflated ; rostrum short ; palate short, wide, the lateral margins of the pre-palatal emargination not extending greatly beyond the inner margins of the inner upper incisors (i2-2) and separated from the canines (c1"1) by a relatively wide ledge of bone ; evident basioc- .21 i 3 cipital pits. Dental formula i -, c -, pm -, m - = 32 ; inner upper incisor (i2) massive, caniniform, unicuspid, with prominent cingulum, the tips of the inner incisors inwardly directed and slightly convergent ; outer upper incisor (i3) low, with basin-like cingulum from which arises a small pyramidal cusp, extending barely to the cingulum either of i2 or of the upper canine (c1) in height ; i3 sometimes displaced inwardly from the toothrow to the extent that it may lie behind or almost behind i2 ; third upper molar (m3) reduced but retaining mesostyle, metacone and three commissures ; third lower molar (m3) usually only slightly reduced, its posterior triangle a little smaller than its anterior triangle, but considerably so in one species. DISTRIBUTION. The genus is distributed through India, Sri Lanka, Burma and the Andaman Islands to Thailand and Malaysia, including Borneo. Subgenus HESPEROPTENUS Peters, 1869 DIAGNOSIS. Ear and tragus membranaceous ; second phalange of third digit markedly longer than first phalange ; braincase slightly inflated, rather globose ; rostrum not especially widened ; supraorbital region only very slightly inflated ; lower maxillary margin of orbit narrow, forming a narrow, tapering ledge alongside the toothrow ; maxillary toothrows nearly parallel ; outer upper incisor (i3) in toothrow or nearly so, not markedly intruded. DISTRIBUTION AND SPECIES. The subgenus is known so far only from Malaysia and includes solely the species Hesperoptenus doriae (Peters, 1869), described originally from Sarawak, Borneo, and here reported for the first time from Malaya. BATS REFERRED TO HESPEROPTENUS 7 Hesperoptenus doriae (Peters, 1869) Vesperus (Hesperoptenus} doriae Peters, i86ga : 626. Sarawak, Borneo. Vesperugo (Vesperus) doriae, Dobson, 1876 : 104, 122. Vesperugo (Hesperoptenus) doriae, Dobson, 1878 : 239. Vesperugo doriae, Dobson, 1880 : 187 ; Hose, 1893 : 40. Vesperugo donriae Hose, 1893 : 40. Lapsus. Hesperoptenus doriae, Trouessart, 1897 : n6 ; 1904 : 83 ; Miller, 1907 : 211 ; Chasen, 1940 : 52 ; Tate, 1942 : 269 ; Ellerman & Morrison-Scott, 1951 : 174 ; Davis, 1962 : 42 (erratum, based on tomesi) ; Medway, 1965 : 65 (erratum, based on tomesi) ; Hill, 1972 : 38. HOLOTYPE. Adult male CE 40094 in the Museo Civico di Storia Naturale 'Giacomo Doria', Genoa, Italy. In alcohol, skull removed. DESCRIPTION. Muzzle with a shallow longitudinal groove immediately behind the widely separated narial openings which are nearly circular ; a few sparse hairs along the upper lip between the nostrils, the internarial region otherwise nearly naked and with only a sparse covering of short hairs above the nostrils and inter- narial pad ; prominent wart above anterior canthus of eye, bearing a few long whiskers ; lower lip with a broad median pad with no more than a trace of a median dividing groove at its posterior border only ; a small naked area beneath the symphysis menti, preceding a low wart which bears a few long hairs. Ears (PI. i) membranaceous, not thick or fleshy, rounded, more or less subquadrangular, the external surface of the conch quite densely clothed with hair for about one half the length of the ear, a few sparse hairs on the inner surface ; anterior margin of ear strongly convex, with rounded, posteriorly directed lobe at its base ; tip rounded ; posterior margin shallowly concave distally but otherwise strongly convex ; well- developed, fleshy antitragal lobe thickened along its outer margin, terminating quadrately behind and level with the corner of the mouth but separated from it by a low wart bearing a tuft of longer hairs. Tragus (Figs la, ib ; PL i) membrana- ceous, about one half the length of the ear, its anterior margin straight proximally, concave distally ; tip rounded, directed anteriorly ; upper margin nearly hori- zontal, sloping only slightly posteriorly, curving convexly to the slightly convex posterior margin which has a large, more or less triangular lobe at its base. 5 mm FIG. i. Tragus of : (a) Hesperoptenus doriae, holotype, Sarawak ; (b) H. doriae, Malaya ; (c) H. tickelli ; (d) H. tomesi; (e) H. Uanfordi. 8 J. E. HILL Thumb long, its upper surface sparsely haired, with a strong claw ; forearm naked except for a few hairs proximally ; upper surface of tibia and of toes with a few scattered hairs ; fur extending sparsely on to the dorsal surface of the uropatagium for about one half its width, the ventral surface similarly but more thinly haired. Third metacarpal the longest, second and fourth very slightly shorter, the fifth the shortest ; second phalange of third digit longer than first phalange ; endopatagium and uropatagium slightly reticulated, remainder of flight membrane striated ; a rounded post-calcarial lobe supported by a poorly defined cartilaginous prop ; penis with saccular prepuce, sparsely haired, with V-shaped preputial opening. Holotype dorsally pale brown, hairs dark brown at the base but pale straw for much of their length, the ventral surface similar but paler, the specimen evidently much bleached by long immersion in alcohol. A second specimen (in alcohol) from Malaya is dark brown above and below, the membranes blackish brown. Skull (PI. i) small, with inflated, slightly globose braincase, more elevated posteriorly than anteriorly, the frontal region slightly inflated ; slight lambdoid crests ; postorbital region sharply constricted ; rostrum short, narrow, with very slight supraorbital ridges, the supraorbital region only very slightly inflated ; a shallow depressed area immediately above anteorbital foramen ; anterior margin of orbit in frontal aspect sloping slightly inwards towards upper surface of rostrum ; shallow median rostral depression. Narial emargination wide, deep, extending posteriorly to a line joining the anterior edges of the anteorbital foramina, in the holotype V-shaped, with rounded apex, in a Malayan specimen U-shaped. Zygomata slender ; anteorbital foramen closed by a narrow bar of bone ; lower maxillary margin of orbit narrow, not especially flange-like ; pre-palatal emargin- ation wide, extending laterally a little beyond the inner faces of the inner upper incisors (i2~2) and posteriorly to a line joining the posterior faces of the canines (c1-1), rounded posteriorly, its lateral margins forming a narrow bony shelf. Palate rather short and wide, the maxillary toothrows nearly parallel ; post-palatal extension long, its lateral margins initially more or less parallel, with a slight convex expansion a little more than halfway along the extension, the margins then conver- gent, the hamulars convergent posteriorly ; post-palatal spine prominent, broad at the base. Soft palate (Fig. 2a) with five post-canine ridges, the first unbroken, the remainder each medianly divided, curved convexly on each side of the palate towards its centre. Basioccipital narrow, with deep, narrow basioccipital pits, separated by a narrow ridge, the bullae relatively large. Baculum (Fig. 3a) of holotype damaged, but has evidently a long, relatively wide, flattened shaft with little sign of any pronounced upward curvature. At the base the baculum is expanded to form paired basal flanges, thick and massive, separated above and below by shallow median fissures. The shaft itself is parallel-sided ; in section its upper surface is slightly convex, the ventral surface in the proximal and central parts of the shaft slightly concave. Towards the tip the shaft is thickened vertically, the tip itself rounded Inner upper incisor (i2) caniniform, large, unicuspid, its basal area one half that of the upper canine (c1), with prominent cingulum. Anterior face rounded, tooth with slight lateral edges, postero-lateral faces scooped out at each side of a posterior BATS REFERRED TO HESPEROPTENUS 2 mm FIG. 2. Palate ridges of : (a) Hesperoptenus doriae, Malaya ; (b) H. tickelli (c) H. tomesi ; (d) H. blanfordi. 10 J. E. HILL C- •^,^."- JV.. ...,i,. .,n.JUii 'j,.!...,. £^v.i:;f;.^v € I I 2 mm FIG. 3. Baculum of : (a) Hesperoptenus doriae, holotype ; (b) H. tickelli (c) H. tomesi, holotype. BATS REFERRED TO HESPEROPTEN US II median knife-like ridge. Outer upper incisor (i3) simple, basal area little more than one quarter that of i2, with basin-like cingulum and simple central cusp, i3 basally slightly ovate, the longer axis lying diagonally to the toothrow ; not displaced or only very slightly intruded, in contact or nearly so with i2 and c1, which is massive, with small anterior and posterior cingulum cusps. Upper pre- molar (pm4) twice as wide as long, not compressed in the toothrow : first and second upper molars (m1-2) with low hypocones, their lingual margins rounded ; third upper molar (m3) about one half crown area of m1, with metacone and three com- missures, the third not greatly reduced. Lower incisors (i!-3) tricuspid, linear, slightly imbricated, i3 a little thickened ; anterior lower premolar (pm2) about one third the crown area of the second lower premolar (pm4) ; entoconid and hypoconid of third lower molar (m3) not greatly reduced, one half the height of the anterior cusps, the tooth only slightly narrowed posteriorly (Pis 2 and 4d). Measurements of the holotype and of a female example from Malaya appear in Tables i and 2. DISTRIBUTION. MALAYA (Selangor) ; BORNEO (Sarawak). Hesperoptenus doriae is known apparently only from the holotype from Sarawak and from a female example (in alcohol, skull extracted) obtained by Lord Medway on 14 February 1969 at the Field Studies Centre, Ulu Gombok, Selangor, Malaya. This further specimen is now in the collections of the British Museum (Natural History). No direct comparison with the holotype has been possible but as far as can be determined the two specimens are in close agreement except for the more rounded, less angular narial emargination of the Malayan example. REMARKS. The inflated, slightly globose braincase of H. doriae removes it rather sharply from Eptesicus and suggests Glauconycteris or the closely allied Chalinolobus, which are thought to be subgenerically related by Ryan (1966 : 86, 89) and by Koopman (1971 : i). However, these differ from Hesperoptenus in the insertion of the posterior margin of the ear and in the presence of a lappet on the lower lip near the angle of the mouth, and the rostrum in general is more shortened. Externally, H. doriae is strongly reminiscent of Eptesicus or Pipistrellus and indeed its baculum is of the long-shafted type associated with the latter genus. Dentally, the species has some features in common with Glauconycteris in which the outer upper incisor (i3) has a wide cingulum with simple central cusp and stands in the toothrow, although in some species a small degree of extrusion is found, to approach the condition usual in Chalinolobus in which the four upper incisors lie on a line in most species. In H. doriae the tendency is for i3, although in the toothrow, to lie towards its inner or lingual border : the inner margins of the inner upper incisor (i2), of i3 and of the upper canine (c1) lie on a line, with the outer margins of i2 and c1 extending considerably beyond the outer margin of i3. Although on occasion a similar situ- ation occurs in Glauconycteris (cf. G. gleni, vide Peterson & Smith, 1973 : 3, fig. 2, centre) the tendency in this genus seems to be for i3 to become extruded. Hesperop- tenus doriae differs further from Glauconycteris in its rounded and not linear post- calcarial lobe and in having the second and third lower incisors (i2-3) linear and imbricated, lacking any low posterior cusp, rather than standing along the line of the " J. E. HILL g o N , CD OTj-Tj-iOrOOOiO'^- CO Tf- CO O M N N M I I I I I I I I Q) 00 ^ *^" vO u~) CT* O *O op N N (S W to s *t •S •B^BIBJ^ ._j_ o gz^'i'i'Z j\[g 'PPV^PT^^^^P ^ ^ SdA^OpJJ lOHTJ-Tt-^H^Tt-Tt- **1 % '•- ^ I '— ' rt P O _ * * * * * * * Cu O Qs ^t" w ^" CO *O O^ " ^-^ OMTt-U-)WNTj-^ p "** • V rt) •••••••• rt O hn OfO't'POioiOMN 173 u gVOHiOiONNiOiO rt M H g fe 3 I I I I I I I I ^ co ^ rH ••..,... ^H V\ C*l t^» 00 M M ^ t^ O O Th romw(v»rom ^ H fT\ — Vi y /-\ I—. - •« S3 vo ^ W ...... v, ,.,. ,4, pj ^O -H 33 uinasnm •EOUSO T Pf^^^PP0? OO 00 u~J vO >O O^ VO "^" c/3 fO CO CO H M fO CO oooooooo flj o S S m o o ,_! _! J J J J J S S Q D •• ^ *-* c ^ a • H 9. Jl • JJ 53 T3 a ^2 C _ C I BATS REFERRED TO HESPEROPTEN US d p M o p "§« 1) rniNj"' "* O O O* C^ OO H OO O HI O •<*• Ha '6 « ^ 2s "° °° 2 Tf (T) N c, "*t b&F'F^ J\[g 'P ^ o-^--^-oo I *K . . - T f^gi'?^ jAig '£ ^" J7 H? N ° I tti JIBABlBg N N POOO uin9snj\[ 4) 5 3 '-P 13 ** --e is g ^-. ... «^^ *—• w^ O X5 2 *" rt "^ •,••••• •• *• •!••••• •"•••• am am _ Mean number of spermathecae in posterior batteries FIG. -2. Relationship between the mean number of spermathecae in the anterior (5/6) and posterior (6/7) batteries. Origins of material : • Sumbawa and Komodo ; Q Lombok ; • Borneo ; O Balabac Island ; A Sangihe ; A Kepulaud Taulaud ; A Celebes ; Fig. 2 the positions of specimens along this axis are determined by the distance each occurs from the origin. (The positions of specimens along this axis may be calculated directly from the formula x = -\/(a2 + b2), where a and b are the mean sizes of the anterior and posterior spermathecal batteries.) To facilitate the recog- nition of clusters, members of each sample are linked. Most of the specimens plotted in Fig. 3 form two discrete clusters. The remain- ing individuals are scattered in an area, peripheral to the larger of these clusters, which is characterized by large spermathecal batteries and low setal numbers. The first cluster, characterized by high setal numbers and small spermathecal batteries, contains all of the specimens from Java, Bali, Sumbawa and Komodo (depicted by solid square symbols). The series from which these specimens were selected were remarkable in the high proportion of athecate individuals present : approximately half the clitellate portion of each series lacked spermathecae and therefore had to be excluded from this figure. Setal numbers of athecate individuals agreed closely with the thecate individuals plotted. The second cluster, containing individuals E. G. EASTON Spermathecal number FIG. 3. Relationship between the setal numberof segment vii and the spermathecal number, V(«2 + &2) (scales logarithmic). Members of each series are linked. Origins of material : | Sumbawa, Komodo, Bali and Java ; D Lombok ; • Borneo (individuals with a high setae : volume ratio) ; O Borneo (individuals with a low setae : volume ratio) ; O Balabac Island ; A Sangihe ; A Kepulaud Taulaud ; A Celebes. with a greater range of setal numbers and larger spermathecal batteries, includes all of the specimens from Balabac Island (open circular symbols), Celebes (open tri- angular symbols) and Borneo (solid circular symbols) with the exception of the individuals from Mt Kinabalu (circular symbols with star-shaped centres) which were noted (Fi) for their low setal numbers. Specimens from Lombok (open square symbols) occur in both clusters. Indi- viduals from low altitudes (c. 50 m) however belong to cluster i while, with one exception, those from high altitudes (c. 400 m) belong to cluster 2. The specimens situated peripherally to cluster 2 are those from Sangihe (solid triangular symbols), Kepulaud Taulaud (partially filled triangular symbols) and Mt Kinabalu (circular symbols with star-shaped centres). Since these may be distinguished by the difference in their setal development it is considered that two further clusters should be recognized among material from this area ; one containing the specimens from Sangihe and Kepulaud Taullaud (cluster 3) and the other the Mt Kinabalu specimens (cluster^ . Although the individuals of cluster 4 resemble those of cluster 3 in their relationships between setal and spermathecal development, it should be recalled (Fig. i) that the setal development, compared with the segmental volume, is reduced in members of cluster 4, while the relationship of the segmental METAPHERETIMA ELONGATA SPECIES-COMPLEX 37 volume to the spermathecal development in individuals in this cluster is closer to that found in cluster 2. The two specimens from Buru (depicted by star-shaped symbols in Fig. 2) have not been plotted in Fig. 3 since they did not occur in the main cluster in Fig. 2. They most closely resemble specimens from Sangihe and Kepulaud Taulaud (cluster 3) on setal numbers and the size of the anterior spermathecal batteries. The marker attributes of the five groups of individuals recognized above have been tabulated in Table i. Morphologically groups i, 2 and 3 form a series in which the only differences noted are increases in the sizes of spermathecal batteries in individuals of a similar size. Group 4 resembles group 2 but has lower setal num- bers. Group 5 differs from group 3 only in lacking spermathecal batteries in furrow 6/7. TABLE i Marker attributes of the morphological groups Group 1. (elongata) 2. (evevetti) 3. (stelleri) 4. (kinabaluensis) 5. (phacellotheca) * See text. Setae : segmental volume (Fig. i) high high high low high Positions of spermathecal pores (Fig. 2) 5/6 and 6/7 5/6 and 6/7 5/6 and 6/7 5/6 and 6/7 5/6 only Size of spermathecal batteries (Fig. 3) small (cluster i) intermediate (cluster 2) large (cluster 3) intermediate* (cluster 4) large NOMENCLATURAL CONSIDERATIONS The type-series of nine of the eighteen nominal species and subspecies assigned to the elongata species-complex were examined during the preparation of this report, thus permitting these names to be readily allocated to the appropriate morpho- logical group. The types of elongata Perrier, 1872 and biserialis Perrier, 1875 were not examined, but Michaelsen (igioc) had previously synonymized the taxa and there is no evidence to dispute this decision. On the basis of Michaelsen 's published description, as well as those of more recent workers (Stephenson, 1923 ; Gates, 1972) the types as well as the majority of records of both elongata and biserialis can be assigned to group i as also may one other taxon, acystis Beddard, 1895. Although the type-series of seven other taxa could not be located during the preparation of this report, it is possible to estimate approximate co-ordinates in Figs i, 2 and 3 for each of the taxa from the original descriptions. None of the original descriptions recorded segmental volume but approximate values have been calculated based on the mean segmental lengths (total length/segment number) and the maximum diameters. The estimated co-ordinates and the group to which each taxon is assigned are shown in Table 2 where data regarding stelleri everetti : Michaelsen, 1899 are also recorded. In Table 2 it is uncertain to which group kinabaluensis Beddard & Fedarb, 1895 should be assigned. The original description lacks any data regarding setal numbers E. G. EASTON TABLE 2 Estimated co-ordinates based on published data Taxon baritoensis beranensis beranensis kinabaluensis phacellotheca stelleri annectens stelleri bonensis stelleri everetti (sensu Michaelsen, 1899) stelleri koroensis Segmental volume (mm3) "•5 i-i 47'7 14-2 28-8 95'4 126-2 176-6 Setal number on vii 49 47 46 40 85 60 Positions of spermathecal batteries 5/6/7 5/6/7 5/6/7 5/6 5/6/7 5/6/7 5/6/7 5/6/7 Size of spermathecal batteries 4'7 8-1 IO-I _ * 26 28 8 Group 2 2 2, 3 or 4 5 3 2 3 2 * Size of spermathecal batteries not recorded. so it could belong to any of groups 2, 3 or 4. It seems unlikely to belong to group 3 because the type locality of kinabaluensis is Tamburungare, Mt Kinabalu, Sabah, at an altitude of 2350 m (7700 ft) and only groups 2 and 4 are known from Borneo. It is however proposed to assign kinabaluensis to group 4 since it is evident from Sims & Easton (1972) that group 4 (series A) is the commonest form at altitudes of more than 2100 m. Information on three records from the Borneo-Celebes area, stelleri : Michaelsen, 1896 : 202 ; stelleri (typica) : Ude, 1932 : 155 and elongata : Ude, 1932 : 155, lacks sufficient detail to establish even approximate co-ordinates for this material. Never- theless, as the two records of stelleri are from Borneo at altitudes at which group 2 is believed to be the only representative of the complex present, both are assigned to that group, while the record of elongata, from south Celebes, is allocated to group i. Although all other records from Celebes have been assigned to groups 2, 3 or 5, they are from the north and west which are ecologically distinct from the south which resembles Lombok and Sumbawa where group i is indigenous (see Distribution). Each morphological group may be recognized as forming a distinct taxonomic unit. The status of each and its relationships with the others still require con- siderable study but since there is no evidence of hybridization, although several samples studied contain representatives of more than one group, it is proposed to consider each as a distinct species while retaining them within the elongata species- complex. The senior synonym allocated to each group is given in Table i. TAXONOMY Metapheretima elongata species-complex Metapheretima elongata species-complex : Sims & Easton, 1972 : 252. Metapheretima phacellotheca : Sims & Easton, 1972 : 233. METAPHERETIMA ELONGATA SPECIES-COMPLEX 39 DIAGNOSIS. Metapheretima with male pores within copulatory pouches lacking stalked glands. Spermathecae in paired, ventrolateral batteries opening in inter- segmental furrows 5/6 and/or 6/7. Genital markings simple, large, paired, presetal, on xix and successive segments in line with or slightly ventral to the male pores. DESCRIPTION. External characters. Length 40-360 mm, diameter 1-5-10 mm. 100-220 segments. Clitellum xiv-xvi. First dorsal pore 12/13. Setae regularly distributed around each segment, 20-130 on vii, 36-86 on xx ; setal distance aa = i-2ab ; occasionally setae a and b enlarged. Male pores paired on short penes within shallow copulatory pouches on xviii, c. 0-25 body circumference apart. Female pore single ; midventral xiv. Sperma- thecal pores small, numerous, arranged in paired, ventrolateral batteries each com- prising up to 28 pores, intersegmental in 5/6 and/or 6/7. Genital markings (Fig. 5a) : paired, simple, large, oval presetal papillae on xix and successive segments in line with or slightly ventral to the male pores ; occasionally present on vi, vii and xvii. Internal characters. Septa 4/5-7/8 thickened, 8/9 membranous, 9/10 absent, 10/11-13/14 thickened. Intestine begins in xv. Lateral hearts in x, xi, xii, usually xiii. Holandric ; testes sacs large, paired, extending to the dorsal line in x and xi ; seminal vesicles paired in xi and xii, the anterior pair enclosed in the posterior testes sacs. Coelomic sacs in xiii, xiv. Spermathecae (Fig. 5b) numerous, in paired batteries of up to 28 in vi and/or vii. Copulatory pouches shallow, confined to the body wall of xviii. DISTRIBUTION. Indigenous records : Kepulaud Taulaud ; Sangihe ; Celebes ; Buru ; Balabac Island, Palawan ; Borneo ; ? Madura ; east Java ; Bali ; Lom- bok ; Sumbawa ; Komodo ; ? Gt Bastard Island, Flores. Four of the five species included in this species-complex are known only from the indigenous range. The fifth, elongata, has been introduced into many parts of the world. REMARKS. This species-complex is readily recognized by the positions of the spermathecal pores and the form of the male pores. Three other species of Meta- pheretima with similar features may be distinguished either by the absence of genital markings in the case of M. annamanensis , a bithecal species known only from the Lang Biang Peaks, Vietnam, or by the form of the genital markings in the cases of aringeana from Kelantan, Malaya, and grata from New Guinea. In aringeana the postclitellar genital markings are paired and occur only on xvii and xix as circular pads with many small pores while in grata they are small and numerous, being present only in the region of the spermathecal pores. This latter species also has stalked glands discharging into the copulatory pouches which are large and invade the coelom. Clitellate individuals from the indigenous range of the species-complex are rarely athecate but the majority of specimens examined from introduced popu- lations lack Spermathecae. In these populations athecate individuals may be identified by the arrangement of the genital markings and the form of the copulatory pouch. Outside of the Pheretima domain, identification is easier since only one 4o E. G. EASTON elongata everetti & phacellotheca kinabaluensis & stellen Spermathecal number FIG. 4. Metapheretima elongata species-complex. Relationship between the setal number of segment vii and the spermathecal number, A/(«2-f62), for the member species. other species of Metapheretima is commonly encountered. This species, M. tapro- banae, has paired spermathecal pores in furrow 7/8 and genital markings on vi-ix and xviii-xxii. Additionally it is considerably smaller than the members of the elongata species-complex, rarely exceeding 140 mm in length. The species of the elongata species-complex may be distinguished from one another by comparison of the setal number on vii and the size of the spermathecal batteries (Fig. 4). (The size of the spermathecal batteries is calculated by substituting the mean size of anterior and posterior spermathecal batteries of an individual for a and b in the formula x — -\/(az + b2).) Two pairs of species, everetti-phacellotheca and stelleri-kinabaluensis, need ad- ditional characters to be assessed for differentiation. In the first pair, M. everetti has spermathecae in furrows 5/6 and 6/7 while phacellotheca has spermathecae in furrow 5/6 only. In the second, M. stelleri has very numerous setae on vii (up to 130) while kinabaluensis has few setae (less than 40). Metapheretima elongata (Perrier, 1872) Perichaeta elongata Perrier, 1872 : 124 ; Beddard, 1895 : 431. Megascolex elongata : Vaillant, 1889 : 81. Amynthas elongatus : Beddard, 1900 : 650. Pheretima elongata : Michaelsen, 1900 : 265 ; Cognetti, igosa : 33 ; Michaelsen, igioa : 252 ; ( = biserialis) Michaelsen, igioc : 84 ; Michaelsen, 1913 : 262 ; Michaelsen, 1920 : 68 ; METAPHERETIMA ELONGATA SPECIES-COMPLEX 41 Stephenson, 1920 : 222 ; Michaelsen, 1922 : 32 ; Stephenson, 1922 : 433 ; Stephenson, 1923 : 298 ; Stephenson, 1924 : 339 ; Gates, ig26a : 208 ; Gates, ig26b : 444 ; Gates, I926c : 183 ; Gates, ig26d : 153 ; Stephenson, 1926 : 256 ; Stephenson, 1929 : 237 ; Gates, 1930 : 309 ; Gates, 1931 : 378 ; Stephenson, 1931 : 58 ; Gates, 1932 : 391 ; Gates, 1933 : 525 ; Cernosvitov, 1934 : 49 ; Cernosvitov, 1935 : I][ : Gates, 1936 : 413 ; Gates, I937a : 318 ; Gates, I937b : 352 ; Gates, I937C : 201 ; Gates, 1939 : 87 ; Daweini, 1940 : no ; Gates, 1954 : 86 ; Gates, 1959 : 9 ; Gates, ig6oa : 57 ; Gates, i96ob : 256 ; Gates, i96ia : 62 ; Gates, ig6ib : 308 ; Gates, 1972 : 182 ; [non Ohfuchi, 1956 : 148 ( = Amynthas morrisi}]. Pheretima (Pheretima} elongata : ? Ude, 1932 : 155 ; Michaelsen, i934a : 108. Perichaeta biserialis Perrier, 1875 : 1044 ; Beddard, 1890 : 63 ; Beddard, 1895 : 430 ; Michael- sen, 1897 : 226 ; (= acystis} Horst, 1899 : 202 ; Beddard & Fedarb, 1899 : 803. Megascolex (Perrier a) biserialis : Vaillant, 1889 : 76. Amynthas biserialis : Michaelsen, 1899 : 21 ; Beddard, 1900 : 638. Pheretima biserialis : Michaelsen, 1900 : 256 ; Michaelsen, 1902 : 9 ; Michaelsen, 1904 : 285 ; Cognetti, igo5a : 30 ; Cognetti, igo5b : 2 ; Ude, 1905 : 471 ; Michaelsen, 1907 : 44 ; Michael- sen, igoSa : 187 ; Michaelsen, igoSb : 14 ; Ohfuchi, 1940 : 13 ; Ohfuchi, 1956 : 151. Perichaeta acystis [nom. nov. pro biserialis : Beddard, 1890 (non Perrier, 1872)] Beddard, 1895 : Perichaeta monocystis (lapsus pro acystis} Horst, 1899 : 202. Metapheretima elongata species-complex : Sims & Easton, 1972 : 256, footnote i. Metapheretima elongata : Jamieson (in press). TYPE LOCALITY. Peru. DIAGNOSIS. M. elongata species complex with numerous setae (usually about 80 on mi but up to 130 on large individuals) and small spermathecal batteries (rarely more than 3 spermathecae in a battery) in furrows 5/6/7, or 5/6 or 6/7 only or absent. Spermathecal batteries usually present in about 50% of the clitellate portion of indigenous populations to about only 15% of the clitellate portion of introduced populations. DISTRIBUTION. Indigenous records (Fig. 6). ? Madura ; east Java ; Bali ; Lombok ; Sumbawa ; Komodo ; ? Gt Bastard Island, Flores ; ? south-east Celebes. The establishment of the indigenous range of this species is discussed below (see Distribution). The specimens identified from Bali, Lombok, Sumbawa and Komodo represent new indigenous records for the species. Introduced records. This species has been introduced into many parts of the world ; for a summary of these records see Gates (1972). During the preparation of this paper specimens from Queensland, Australia ; Tahiti ; Antigua, West Indies ; and Oman were identified. These represent new introduced records for the species. Metapheretima everetti (Beddard & Fedarb, 1895) Perichaeta everetti Beddard & Fedarb, 1895 : 69 ; Beddard, 1895 : 428 (non Amynthas stelleri everetti : Michaelsen, 1899 : 43). Perichaeta papillata Beddard & Fedarb, 1895 : 71 > Beddard, 1895 : 428. Perichaeta sarawacensis Beddard & Fedarb, 1895 : 71 ; Beddard, 1895 : 429. Perichaeta bar ami Michaelsen, 1896 : 203. Amynthas stelleri bar ami : Michaelsen, 1899 '.41. Perichaeta stelleri : Michaelsen, 1896 : 202 ; (non Michaelsen, 1891 : 39) ; Horst, 1899 : 205. Amynthas stelleri (typica) : Michaelsen, 1899 : 83. E. G. EASTON 146. Pheretima stelleri (typica} : Michaelsen, 1922 : 25. ? Pheretima (Pheretima) stelleri (typica): Ude, 1932 Amynthas stelleri seriatus : Michaelsen, 1899 : 44. Amynthas stelleri klabatensis Michaelsen, 1899 : 46. Amynthas stelleri bonensis MUhaelsen, 1899 : 45. Pheretima stelleri bonensis : Michaelsen, 1900 : 307. [non Pheretima (Pheretima) stelleri bonensis : Michaelsen, i934a : 108 ( = M. phacellotheca)] Pheretima stelleri koroensis Michaelsen, igiob : 109. Pheretima stelleri mahakkami Michaelsen, 1922 : 25. Pheretima (Pheretima) beranensis Michaelsen, 1928 Pheretima (Pheretima) baritoensis Michaelsen, 1932 ? Pheretima (Pheretima) elongata : Ude, 1932 : 155 ; Pheretima (Polypheretima) beranensis tinjarana Michaelsen, 19345 : 25. Metapheretima elongata species-complex [series B (part)] : Sims & Easton, 1972 : 253. TYPE LOCALITY. Balabac Island, Palawan. Beddard & Fedarb reported that the type locality of Perichaeta everetti is Mt Kinabalu, Sabah. The type series of this species in the collections of the British Museum (Natural History) is labelled as originating from Balabac Island, Palawan. Although Beddard & Fedarb wrote in their introduction that the collection they were reporting was collected from both Borneo and Palawan, no reference to Palawan is made in the general text. It is 23. 9. (non Perichaeta elongata Perrier, 1872). FIG. 5. Metapheretima everetti. (a) Diagram of the papillae pattern on the ventral surface of the anterior region of the body, (b) Spermatheca. METAPHERETIMA ELONGATA SPECIES-COMPLEX 43 proposed to follow Recommendation 72E of the International Code of Zoological Nomenclature and redesignate Balabac Island, Palawan as the type locality for Perichaeta everetti Beddard & Fedarb, 1895. DIAGNOSIS. M. elongata species-complex with numerous setae (up to 130 on mi in large individuals) and intermediate-sized spermathecal batteries (usually 6-12 spermathecae in each battery of large individuals) in furrows 5/6/7. Spermathecal batteries present in aclitellate as well as clitellate individuals. DISTRIBUTION. Indigenous records (Fig. 6) : north and west Celebes ; Balabac Island, Palawan ; Borneo (up to altitudes of 2400 m) ; Lombok (c. 350-450 m only). This species is unknown outside its indigenous range. REMARKS. On Lombok this species has been recorded only from localities at altitudes between 350 and 450 m. (Samples from lower altitudes contained the species elongata which is rare at the higher altitudes. No samples of earthworms are known from above 450 m on Lombok.) Although altitude would appear to be the primary factor governing the distribution of both everetti and elongata, it should be noted that, on Lombok, the samples of everetti were from natural woodland while those of elongata were from cultivated land. All the records of everetti, stelleri and phacellotheca from Celebes are from the northern and western region, an area of forest, while the single record of elongata (as yet unconfirmed as an indigenous population) is from the southeast which is an area of savannah. On Mt Kinabalu, Borneo, the species everetti occurs at altitudes up to 2400 m, being sympatric from 2 100 m with the high altitude species kinabaluensis. Although on Lombok and Mt Kinabalu everetti is sympatric with other members of the elongata species-complex, there is no indication of hybridization among them. Metapheretima kinabaluensis (Beddard & Fedarb, 1895) Perichaeta kinabaluensis Beddard & Fedarb, 1895 : 71 ; Beddard, 1895 : 429- Metapheretima elongata species-complex [series A & series B (part)]: Sims & Easton, 1972 : 253. TYPE LOCALITY. Tamburgare, Mt Kinabalu, Sabah, 2350 m (7700 ft). DIAGNOSIS. M . elongata species-complex with few setae (less than 40 on vii in large individuals) and intermediate-sized spermathecal batteries (usually 6-12 spermathecae in each battery of large individuals) in furrows 5/6/7. Spermathecal batteries present in aclitellate as well as clitellate individuals. DISTRIBUTION. Indigenous records (Fig. 6) : Mt Kinabalu, Sabah (2100-2750 m). This species has not been recorded outside its indigenous range. REMARKS. This species is known only from high altitudes on Mt Kinabalu where the fauna and flora are of a distinct montane type. It is probable that future investigations of the high-altitude earthworm fauna in the Borneo-Celebes area will reveal other population of this species. Although samples collected at 2100 and 2400 m on Mt Kinabalu contained both everetti and kinabaluensis there is no indi- cation of hybridization between these two forms. 44 E. G. EASTON Metapheretima phacellotheca (Michaelsen, 1899) Amynthas phakellotheca (sic) Michaelsen, 1899 : 47. Amynthas phacellotheca : Beddard, 1900 : 640. Pheretima phacellotheca : Michaelsen, 1900 : 293 ; Gates, 1961 : 304. Pheretima (Polypheretima) phacellotheca : Michaelsen, 19345 : 15. Metapheretima phacellotheca : Sims & Easton, 1972 : 233. Pheretima (Pheretima} stelleri bonensis : Michaelsen, 19343 : 108 ; (non Amynthas stelleri bonensis Michaelsen, 1899 : 45). TYPE LOCALITY. Mt Masarang, above Tomohon, northeast Celebes. DIAGNOSIS. M. elongata species-complex with numerous setae (up to 80 on vii in large individuals) and large spermathecal batteries (9-12 spermathecae in each battery in large individuals) in furrow 5/6. Spermathecal batteries present in aclitellate as well as clitellate specimens. DISTRIBUTION. Indigenous records (Fig. 6) : northeast Celebes, Buru. This species has not been recorded outside its indigenous range. REMARKS. This species is the only member of the elongata species-complex known from Buru which is the most easterly indigenous record of the complex. Morphologically it most closely resembles stelleri from which it may be distinguished only by the restriction of spermathecal batteries to furrow 5/6. Its relationships with everetti and stelleri, which also occur in north Celebes, are unknown. Metapheretima stelleri (Michaelsen, 1891) Perichaeta stelleri Michaelsen, 1891 : 39 ; (non Michaelsen, 1896 : 202 ; Horst, 1899 : 205). [non Amynthas stelleri (typica) : Michaelsen, 1899 : 83.] [non Pheretima stelleri (typica) : Michaelsen, 1922 : 25.] Pheretima (Pheretima) stelleri (typica) : Michaelsen, i934a : 108 (non Ude, 1932 : 146). Amynthas stelleri annectens : Michaelsen, 1899 : 42. Amynthas stelleri everetti : Michaelsen, 1899 : 43 ; (non Perichaeta everetti Beddard & Fedarb, 1895 : 69). TYPE LOCALITY. Sangihe. DIAGNOSIS. M. elongata species-complex with very numerous setae (up to 130 on vii in large individuals) and large spermathecal batteries (up to 28 spermathecae in each battery of large individuals) in furrows 5/6/7. Spermathecal batteries present in aclitellate as well as clitellate individuals. DISTRIBUTION. Indigenous records (Fig. 6) : Kepulaud Taulaud ; Sangihe ; north Celebes. This species has not been recorded outside its indigenous range. REMARKS. In Celebes stelleri has been recorded from Bone Valley (c. 400 m) and the Matinang range (c. 1500 m). In both of these areas everetti has also been re- corded but the relationship between the two species and the factors governing their distribution are unknown. No information is available regarding the relationship between stelleri and phacellotheca. METAPHERETIMA ELONGATA SPECIES-COMPLEX 45 DISTRIBUTION All the records attributed to everetti, stelleri, kinabaluensis and phacellotheca (groups 2, 3, 4 and 5) are from Borneo, Celebes or nearby islands and it is con- sidered that these records indicate the indigenous ranges of the species. The species elongata (group i) has been recorded from islands as far apart as Luzon, New Guinea and Sumatra in the Indo-Australasian Archipelago (as well as many other localities throughout the world) but it is thought that this distribution is not entirely natural and that it has been augmented through accidental introduction by man. In the area adjacent to the range of the other members of the complex elongata has been recorded from Sumatra, Java, Madura, Bali, Lombok, Sumbawa, Komodo, Gt Bastard Island, Celebes, Kepulaud Taulaud and the Philippines and it is suspected that at least some of these records are from indigenous populations. Among these localities Lombok and Celebes are of particular interest since the most closely related member of the complex, everetti, has also been recorded from these islands. Although the majority of species of the Pheretima group possess normal her- maphrodite reproductive systems and are assumed to reproduce only sexually, several species are known to occur as morphs lacking portions of the reproductive system. Gates (1972) recognized four principal morphs : H morph, the normal hermaphrodite form ; A morph, lacking spermathecae ; R morph, lacking male terminalia ; and Z morph, lacking testes. (In addition to these basic forms he also recognized AR and ARZ morphs.) He considered that, with the exception of the H morph, all these forms reproduced by parthenogenesis. He recorded 70 species of the Pheretima group from Burma of which 42 were known only from Burma and the adjacent area while 19 were peregrine ; only 6% of the indigenous species but 47% of the peregrine forms are known to possess non-hermaphrodite morphs. This correlation between non-hermaphrodite morphs and peregrine distributions led Gates (1956) to suggest that the peregrine species Metaphire anomala (Michaelsen, 1907) had originated from eastern Burma where the H morph was more common. TABLE 3 Population characteristics of M. elongata from selected islands Number of clitellate Proportion of Island specimens examined H morphs (%) Jamaica 84 18 Sumatra 47 15 west & central Java 13 15 east Java 22 50 Madura 3 (2) * Bali 27 44 Lombok 19 26 Sumbawa 59 "\ Komodo 4 J Kepulaud Taulaud i (o)* Philippines 9 (i) * * For small samples (less than 10 individuals) the number of thecate individuals (rather than the percentage) has been recorded and placed in parentheses. 46 E. G. EASTON Metapheretima elongata similarly occurs as H and A morphs so if the hypothesis is valid then the H morph will be more common in its indigenous range than else- where. Samples of island populations were examined and the incidence of H morphs was calculated from among the clitellate portion of each series. The results of this study are shown in Table 3. (Java was treated as two regions since it may be con- sidered to be composed of two ecologically distinct areas, tropical rain forest in central and west Java and savannah in east Java.) To obtain a comparative value for a population which was known to be introduced, the incidence of H morphs was assessed in a population from Jamaica. The low incidence of H morphs in the introduced Jamaican population (18%) agrees very well with that of the popu- lations from central and west Java and Sumatra (both 15%) but contrasts strongly with populations from east Java, Bali, Sumbawa and Komodo (44-51%). The value calculated for Lombok (26%) is intermediate between the two classes and somewhat anomalous in view of the geographical position of the island. Possibly the small size of the sample may be the causative factor. Assuming the basic assumption to be valid, these calculations indicate that elongata is indigenous in east Java, Bali, Lombok, Sumbawa and Komodo, while the form which is morpho- logically the most similar, everetti, occurs at high altitudes (c. 400 m) in Lombok. These values are consistent in the degree of magnitude with those recorded by Gates (1956) when he recorded 20% H morphs of anomala in eastern Burma but only 0-7% in other parts of Burma. Samples from Kepulaud Taulaud, Philippines and Madura were too small to derive any reliable conclusions from them but it seems unlikely that elongata is indigenous in either Kepulaud Taulaud or the Philippines, although it may possibly occur naturally in Madura. There have been single inconclusive records of elongata from south-east Celebes and Gt Bastard Island but in the former case the specimens cannot be located and in the latter the single extant specimen proved to be indeter- minate and the occurrence of indigenous populations of elongata in both of these islands has yet to be confirmed. The known indigenous distributions of the mem- bers of the elongata species-complex are shown in Fig. 6. The earthworm fauna of south-east Asia has been extensively studied (Gates, 1972) and data from this work and other recent collections in the British Museum (Natural History) have allowed the establishment of the western limit of the indigenous range of the complex. Unfortunately the earthworm faunae of the Philippines, Celebes, Moluccas and Lesser Sunda Islands still require considerable study and it is not practical to estab- lish the northern and eastern limits of the distribution of the complex. However, recent extensive collecting in New Guinea (Easton, in preparation) indicates that the complex is absent from this island except for introduced populations of elongata. The form kinabaluensis is known only from Mt Kinabalu, Sabah, at altitudes of over 2100 m. It is probable that future collections will reveal that it also occurs on some of the other high mountains in Borneo and possibly even Celebes. Likewise the occurrence of everetti in Lombok at altitudes of 400 m may indicate that it occurs at high altitudes throughout the Lesser Sunda Islands. Metapheretima stelleri has been recorded from Sangihe, Kepulaud Taulaud and north Celebes. Michaelsen (1934^ was of the opinion that this species had been METAPHERETIMA ELONGATA SPECIES-COMPLEX 47 FIG. 6. Metapheretima elongata species-complex. Endemic distributions : • elongata ; Tinjar river, Long Lejok, Sarawak, 8C loA, BM(NH) 1933.10.6.12-20 & Hamburg v. 11951 (syntypes of beranensis tinjarana] ; Merabah, Sarawak, 146 I2A, BM(NH) 1904.10.5.1265-70 (syntypes of papillata) ; Putussibau, Kali- mantan, loC I3A, Leiden 1091 (stelleri : Horst, 1899) ; Nangaraun, Kalimanton, 5C gA, Leiden 1903 (stelleri : Horst, 1899) ; 'the Liang Koeboeng' (the exact location of this locality could not be established), iC, Leiden 1904 (stelleri ; Horst, 1899) ; Bendjermasin, Kalimanton, iC, Ham- burg V.4O24 [stelleri (typica) : Michaelsen, 1899] ; Bo river, Kalimanton, 30, Leiden 1900 & Hamburg V.93O7 [stelleri (typica) : Michaelsen, 1922] ; above Mahakkam rivers, Kalimanton, iC, Leiden 1897 (holotype of stelleri mahakkami) ; Birang river, Beran district, Kalimanton, fragments of one or more specimens, Hamburg v. 10576 [type(s) of beranensis}. Lombok : Swela, iC, Berlin 7214 [this specimen is here separated from the type series of Meta- pheretima badia (Ude, 1932)]. 3. OTHER RECORDS. Celebes : Koro valley [type(s) of stelleri koroensis] ; Bone valley (types of stelleri bonensis). Borneo : Baram river, Sarawak (stelleri : Michaelsen, 1896) ; Dorf Poh Trap, Brunei [stelleri (typica) : Ude, 1932] ; Boentok, on the Barito river, Kalimanton [type(s) of baritoensis]. Metapheretima kinabaluensis (Beddard & Fedarb, 1895) 1. MATERIAL EXAMINED. Borneo : Mt Kinabalu, Sabah, 126 2A, BM(NH) 1971.19.1-11, 21-23 [series A (part), series B (part) : Sims & Easton, 1972]. 2. OTHER RECORDS. Borneo : Tamburungare, Mt Kinabalu, Sabah [type(s) of kinabaluensis]. Metapheretima phacellotheca (Michaelsen, 1899) MATERIAL EXAMINED. Celebes : Mt Masarang, above Tomohon, several spermathecae and fragments of body wall, Hamburg v.5195 [type(s) of phacellotheca]. Buru : between Mnges'wain and Leksula, iC, Amsterdam V.ol 302 (stelleri bonensis : Michaelsen, 1934) ; Leksula, iC, Amsterdam. Metapheretima stelleri (Michaelsen, 1891) 1. MATERIAL EXAMINED. Sangihe : — , 76 lA, Hamburg v.338, BM(NH) 1904.10.5.162 & Leiden 1903 (syntypes of stelleri) . Kepulaud Taulaud : Lobo, Karakelang, iC, Amsterdam V.ol 303. 2. OTHER RECORDS. Celebes : Matinang range (stelleri everetti : Michaelsen, 1899) ; Bone valley [type(s) of stelleri annectens]. METAPHERETIMA ELONGATA SPECIES-COMPLEX 53 E. G. EASTON, B.Sc. Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) LONDON SWy A LIST OF SUPPLEMENTS TO THE ZOOLOGICAL SERIES OF THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) 1. KAY, E. ALISON. Marine Molluscs in the Cuming Collection British Museum (Natural History) described by William Harper Pease. Pp. 96 ; 14 Plates. 1965. (Out of Print.) 2. WHITEHEAD, P. J. P. The Clupeoid Fishes described by Lacepede, Cuvier and Valenciennes. Pp. 180 ; n Plates, 15 Text-figures. 1967. £4. 3. TAYLOR, J. D., KENNEDY, W. J. & HALL, A. The Shell Structure and Mineralogy of the Bivalvia. Introduction. Nuculacea-Trigonacea. Pp. 125 ; 29 Plates, 77 Text-figures. 1969. £4-50. 4. HAYNES, J. R. Cardigan Bay Recent Foraminifera (Cruises of the R.V. Antur) 1962-1964. Pp. 245 ; 33 Plates, 47 Text-figures. 1973. £10-80. 5. WHITEHEAD, P. J. P. The Clupeoid Fishes of the Guianas. Pp. 227; 72 Text-figures. 1973. £9-70. 6. GREENWOOD, P. H. The Cichlid Fishes of Lake Victoria, East Africa : the Biology and Evolution of a Species Flock. Pp. 134 ; i Plate, 77 Text-figures. 1974. £3'75- Hardback edition £6. Printed in Great Britain by John Wright and Sons Ltd. at The Stonebndge Press, Bristol BS4 5NU GENERAL 2 4 SEP 197 \ ^ LIBRARY THE TAXONOMY OF CONCHOECIA&*L«0 (OSTRACODA, HALOCYPRIDIDAE) OF THE GAUSSI AND EDENTATA GROUPS FROM THE NORTHEAST ATLANTIC WITH A NOTE ON THEIR ECOLOGY A. J. GOODAY BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 3 LONDON: 1976 GENERAL 2 4 SEP 197 THE TAXONOMY OF CONCHOECIA (OSTRACODA, HALOCYPRIDIDAE) OF THE GAUSSI AND EDENTATA GROUPS FROM THE NORTHEAST ATLANTIC WITH A NOTE ON THEIR ECOLOGY BY ANDREW JOHN GOOD AY Institute of Oceanographic Sciences Pp 55-100 ; 22 Text-figures BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 3 LONDON: 1976 THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be completed within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30 No. 3 of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation Bull. Br. Mus. nat. Hist. (Zool.) ISSN 0007-1498 Trustees of the British Museum (Natural History), 1976 BRITISH MUSEUM (NATURAL HISTORY) Issued 23 September, 1976 Price £3.70 THE TAXONOMY OF CONCHOECIA (OSTRACODA, HALOCYPRIDIDAE) OF THE GAUSSI AND EDENTATA GROUPS FROM THE NORTHEAST ATLANTIC WITH A NOTE ON THEIR ECOLOGY By A. J. GOODAY CONTENTS Page SYNOPSIS ........... 57 INTRODUCTION .......... 57 TAXONOMIC SECTION ......... 59 edentata group .......... 59 Conchoecia subedentata sp. n. ....... 60 Conchoecia aff. edentata ........ 69 gaussi group .......... 77 Conchoecia incisa ......... 78 Conchoecia gaussi ......... 85 ECOLOGY. ........... 93 ACKNOWLEDGEMENTS ......... 99 REFERENCES ........... 99 SYNOPSIS Conchoecia subedentata sp. n. and C. aff. edentata are described from the Northeast Atlantic and placed in a new edentata species group based on C. edentata, an Antarctic species. C. edentata was previously assigned to the gaussi group which is here restricted to C. gaussi and C. incisa, both of which are redescribed. C. subedentata sp. n. and C. aff. edentata are commonest at 6o°N and decrease in abundance southwards. C. subedentata sp. n. occurs mainly between 300 m and 900 m depth, C. aff. edentata is most frequent below 800 m. C. gaussi is most abundant at 53°N and C. incisa at 3O°N. C. incisa males are rare and restricted to below 1250 m, while females and juveniles have two peaks of abundance, below 800 m and between 600 m and the surface. C. gaussi occurs mainly below 1000 m. None of the species appears to undergo diurnal vertical migration except for females and juveniles of C. incisa where all specimens in the top 200 m were taken at night. Taken together adults and juveniles of C. gaussi and C. incisa fall into three or four size classes which may have some trophic significance. INTRODUCTION SKOGSBERG (1920 : 676) proposed the gaussi group of species to include Conchoecia incisa Muller, 1906 and Conchoecia gaussi Muller, 1908. Later Rudyakov (1962) placed C. edentata Muller, 1906 close to C. gaussi and Deevey (1974 : 368) included it A. J. GOODAY TABLE i Station details and gear used STATION LOCATION IN NORTHEAST ATLANTIC 58i4 58i6 5818 5819 * 28°N, I4°W 5823 5825.. 6i55" 6156 >• 28°N. 14 °w 6164 i 6176 6l8A 34° 6i93 / 34 N, So °W 6674 11° 35'N, 2I°26'W 7089 i 8° N, 25 °W 7406") 7478 }- 48° N, 20 °W 748oJ 7709 60° 7711 53° N, N, 20 20 °W °W } 8262 8264 8265 8270 8271 8272 i8°N, 25°W 32°N, i6°W" 32°N, 24°W 32°N, 27°W 34°N, 34°W 34°N, 39°W 34°N, 43°W, DATE Sept. to Dec. 1965 >Oct. to Nov. 1966 Jan. to April 1968 Oct. to Dec. 1969 Sept. to Nov. 1970 April to June 1971 Feb. to April 1972 Feb. to March 1973 Discovery CRUISE No. GEAR Nn3 15 21 30 36 39 45 52 RMT 1+8 RMT i + 8 RMT i +8 in the gaussi group, while in a revision of Conchoecia Poulsen (1973 : 103) established the genus Gaussicia for these three species. Unfortunately some of the genera into which Poulsen subdivided Conchoecia are questionable. In this paper I therefore disregard Gaussicia until Poulsen's taxonomy can be thoroughly assessed. I also believe it is wrong to combine C. edentata with C. gaussi and C. incisa. In my view C. edentata and its allies described in this paper differ sufficiently from C. gaussi and C. incisa to warrant their placement in a new edentata group. Plankton samples collected during recent years in the Northeast Atlantic by the RRS Discovery have yielded abundant material of the gaussi and edentata groups. Specimens resembling C. edentata predominate and faU into two size classes The larger form is closer to Miiller's (1906) original description of C. edentata and is assigned here to C, aff. edentata while the smaller form is described as C. subedentata sp. n. In addition, the two poorly known species of the gaussi group, C. gaussi and C. incisa, are redescribed, and the ecology of members of the gaussi and edentata groups is discussed. CONCHOECIA FROM THE NORTHEAST ATLANTIC 59 Material and methods The material was obtained from 27 stations in the Northeast Atlantic during seven cruises by RRS Discovery between 1965 and 1973. Details of the stations are summarized in Table i. On earlier cruises, aim2 net (Nii3) fitted with a catch dividing bucket was employed (Foxton, 1969). This was superseded in 1969 by the combination net (RMTi + 8) described by Baker, Clarke & Harris (1973). Most of the ostracods were caught in the RMT I part of the combination net although a few adult specimens of C. incisa and C. gaussi were picked out from the RMT 8 samples. A few characters measured must be briefly defined here. Carapace length includes the rostrum ; carapace height and breadth are maximum values. Segments i and 2 of the first antenna are measured along their dorsal margins and the first segment is taken to begin at the base of the frontal organ. Protopodite length includes the anterior hook and segments 2-8 of the second antenna exopodite are measured from the distal end of segment i and not from the proximal end of segment 2. TAXONOMIC SECTION edentata group DIAGNOSIS. Both valves bear median ventral glands ; asymmetric glands are in usual positions. Male first antenna with long a and c setae and pad on b seta ; e seta has proximally pointing spines which are difficult to distinguish. Female first antenna has very short dorsal seta, a-d setae are slightly longer or just shorter than e seta which bears group of proximally pointing spines on distal flattened and widened part. Male second antenna with g seta slightly widened and flattened distally ; in female, g seta is rather wider and sword-shaped. Serrated teeth of mandibular basale low with weak primary cusps. Maxilla with only four posterior setae. Labrum has weak hyaline plate and small weak teeth. Female sixth limb with characteristically long and flexible ventral seta and very short dorsal seta on final segment. REMARKS. Conchoecia edentata of Miiller (1906) was included with C. gaussi and C. incisa in the new genus Gaussicia (= gaussi group) by Poulsen (1973). However this species, together with C. aff. edentata and C. subedentata sp. n. described here, differs from C. gaussi and C. incisa in numerous characters which are summarized in Table 5. In contrast the points of similarity are rather few : the presence of the ventral gland, the general character of the b, d and e seta armature on the male first antenna, the shape of the female g seta (second antenna) and e seta (first antenna), the development of minute spines on various segments of the female first antenna and the male and female second antenna and perhaps the same general structure of the cutting edge and tooth lists of the mandibular coxale. Because of the large number of differences (Table 5) it seems sensible to remove C. edentata, C. aff. edentata and C. subedentata sp. n. from the gaussi group and place them in a new edentata group. The arrangement is supported by the fact that many 60 A. J. GOODAY differences between the two groups are concerned with characters of the mandible, maxilla, fifth and sixth limbs and labrum. These limbs are more conservative in their structure than the first and second antennae and so their characteristics must carry more taxonomic weight. The edentata group is characterized by several features, (i) The development of a median ventral gland ; this is also present in C. gaussi and in C. prosadena the right asymmetric gland (not homologous with the ventral gland in the edentata and gaussi groups) is situated at the posterior end of the ventral margin, (ii) The a-d setae of the female first antenna are slightly shorter or slightly longer than the e seta. In no other species of Conchoecia do these setae approach the length of the e seta. The group of proximally pointing spines with expanded bases on the distal part of the e seta are probably also peculiar to this group, (iii) On the terminal segment of the female sixth limb the ventral a seta is very long, thin and flexible, the claw-like median b seta rather longer or shorter and the dorsal c seta is very short. These setae are probably diagnostic for the edentata group although characters of the sixth limb have generally been ignored in species descriptions. However, in all species of Conchoecia for which information is available the terminal setae of this limb are claw-like and shorter than the two ventral setae of the edentata group. The edentata group is probably closely related to the gaussi group. It also shares a number of characters with the mollis group : distally widened g setae on the male and female second antennae and a distally widened e seta on the female first antenna, long a and c setae of the male first antenna and a pad on the b seta of this limb. C. congolensis Poulsen, 1969, which Poulsen (igGga : 116) felt was related to the bispinosa and gaussi groups, may be closer to the edentata group. In the only known specimen, a female, the dorsal seta is short and the a-d setae are long, although not as long as in the edentata species group. However the long, rod-shaped capitulum and the absence of a ventral gland distinguish C. congolensis from species of both the edentata and gaussi groups. Conchoecia subedentata sp. n. (Figs 2-5) DIAGNOSIS. Species of edentata group characterized by small size (male carapace length 1-123-1-280 mm, mean 1-21210-030 mm) and setation of final segment of female limb where ventral a seta is longer than middle claw b seta. MATERIAL. 1447 specimens comprising 388 females, 392 males and 667 juveniles. HOLOTYPE AND PARATYPE. The holotype, a male stained with lignin pink and mounted on slides in Euparal, is deposited in the British Museum (Natural History), reg. no. 1974.736. The type locality is Discovery station 7711, haul 23 ; 52°57'i'- 52°53-i'N, 20°o-o'-20°3-4'W. Depth 200-300 m. Time 2342-0142 hr. Date 19- 20 May 1971. Gear RMTi + 8. The paratype material comprises a dissected female reg. no. 1974.737 and some undissected male and female specimens in 70% alcohol, reg. nos 1974.738-748. CONCHOECIA FROM THE NORTHEAST ATLANTIC 61 10 Numbers 50 40 30 20 10 aff. edentata p IV V VI | n r-i n r-n i"i D i tlj 1 rTf^^^r^Ti irFl^lfon n 0.75 1.00 n1-25 1.50 1.75 " pi prr, [j:::::;| Adult Females subedentata J I 1 ^ Adult Males / y / 0 V VI M / / W !H Stage VI Males IV I Tl Eg;j 1 : •: ~] ~] Other Juveniles ^ ^ x 2 NIGHT DAY 1 45 10J K -1 >3 3S '7 10 « 4J ?4 95 1 4d 2 1SJ \ fl 15 ^3 1<3 n 73 •1 49' ri 53° 173 ~ 3 2C NIGHT DAY I 1 j . 2 < 80 3 0 • ( 2«< 1 44C 903 h S 9( • 8C 2 7J 1 6 •6 13 'I • '1 2 | 1 NIGHT DAY m rs 33 NIGHT i • 72 > 15 '16 1° 5 2J 1 ?» 135 l"32 50 30 58 J k ?4 40? i"10 33C 7 1150 \ 2< 4 , . 21 < M 19C 180 ( II '3 3 > !9 •18 82 • ?16 r29 16 • ?43 r74 80 i ! i • • ?i n 49 500- H 448 323 285 91 131 7 lUUU 1500 ?onn 4 : 4 ; s I r2 1 1? 1 ?3 >4 H M 6 9 5 3 63 245 408 708 FIG. 19. Conchoecia subedentata sp. n. Depth distribution at various latitudes in the Northeast Atlantic Ocean. The number of males, females and juveniles caught with the RMT 1 + 8 during day and night in 100 m horizons down to 1000 m and wider hori- zons between 1000 m and 2000 m are shown. The figures along the bottom of the dia- gram are the total numbers of specimens occurring at each latitude and the figures in the right-hand column give the total numbers of specimens caught in each depth horizon. CONCHOECIA FROM THE NORTHEAST ATLANTIC 95 11 18 30° 40 53 60° N u 500- DEPTH (m) 1000- icnn DAY « 7: j NIGHT DAY i I NIGHT DAY 1 NIGHT DAY '« 1S I 1C U !< 1 ? ; f 3 3. 4! 1C • 1: NIGHT DAY !2 [ ' 2< ; K n • . ^ 6d 20 J ; • I- r NIGHT ! F 1 - | ' 15 < 1C 1C «< 2. * . • • IS ? ' ?' i, rl • 1 ' * J \ e 4 5 3 16 10 43 5 IDUU 2000 1 2 23 1 18 21 37 FIG. 20. Conchoecia ail. edentata. Depth distribution at various latitudes in the Northeast Atlantic Ocean. For explanation see Fig. 19. TABLE 6 Vertical distribution during the day and night of females and juveniles of Conchoecia incisa at 28°N DEPTH (m) o-ioo 100-200 200-300 300-400 400-500 500-600 600-700 700-800 800-900 DAY NIGHT FEMALES JUVENILES FEMALES JUVENILES i 3 i i 7 96 A. J. GOODAY most females and juveniles were caught between 600 m and the surface with a concentration of juveniles at 500-600 m (Table 4 : these data were obtained from Nii3 catches and are not comparable with the data in Fig. 21 which are based on RMT 1 + 8 samples) . This vertical distribution pattern resembles that of Halocypris globosa Claus, 1874. Here the males are deep-living while the females and juveniles have a bimodal distribution with peaks of abundance between 1500 m and 3000 m and in the top 100 m (Poulsen, i96gb : 49, 60). Almost all specimens of C. incisa caught near the surface (0-200 m) were taken at night (Table 4 and Fig. 21) which suggests that shallower members of this species migrate diurnally. However, there is no evidence for diurnal migrations by individuals living below 1000 m (Fig. 21). C. gaussi occurs mainly below 1000 m although a few specimens were caught at shallower depths and a juvenile was obtained from the top 100 m at 53°N (Fig. 22). This species does not seem to migrate vertically although the evidence is sparse. DEPTH (m) u- DAY NIGHT CAY 1, NIGHT DAY NIGHT NIGHT - V j rl 2 500- H i 2> 3 i< 1! ' 2 2S r 2 I — 1? 91 J3 7 3J1 4 1000- — <9 6 7 ii1 11 273 1500- + — 293 4, •» swau* 24SEPW76 ECHINODERMS FROM THE X NORTHERN REGION OF THE GREAT BARRIER REEF, AUSTRALIA P. E. GIBBS, A.M. CLARK AND C.M.CLARK BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 4 LONDON : 1976 ECHINODERMS FROM THE NORTHERN REGION OF THE GREAT BARRIER REEF, AUSTRALIA BY PETER E. GIBBS Marine Biological Association of the U.K. AILSA M. CLARK AND CHRISTINE M. CLARK British Museum (Natural History) Pp 101-144 ; i Plate ; 3 Text-figures ; I Map BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30, No. 4 LONDON: 1976 THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three of four hundred pages, and will not necessarily be completed within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30 No. 4 of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation Bull. Br. Mus. nat. Hist. (Zool.) ISSN 0007-1498 Trustees of the British Museum (Natural History), 1976 BRITISH MUSEUM (NATURAL HISTORY) Issued 23 September 1976 Price £3-35 ECHINODERMS FROM THE NORTHERN REGION OF THE GREAT BARRIER REEF, AUSTRALIA By P. E. GIBBS, AILSA M. CLARK & CHRISTINE M. CLARK SYNOPSIS This paper gives records of about 140 species of echinoderms from the northern region of the Great Barrier Reef collected during the Royal Society-Universities of Queensland Expedition in 1973. One ophiuroid species is new to science, namely Amphiura phrixocantha sp. nov. (p. 121). Ten other ophiuroids, two echinoids and one holothurian are new to the Australian fauna and the ranges of eight more ophiuroids and one holothurian are extended to the Great Barrier Reef Province from other parts of Australia. In addition, a few unpublished records from relevant material in the British Museum collections are included and notes are given on several species of especial interest. In contrast to most shallow-water tropical collections, the one from this Expedition includes a high proportion of burrowing species from soft substrates. A list of some animal associates of the specimens collected is appended. INTRODUCTION EARLY investigations of the echinoderm fauna of the Great Barrier Reef were largely centred on the Torres Strait region and essentially began with the visit of the Challenger Expedition in 1874. The material collected, mostly from dredging, together with that taken by the Alert Expedition in 1881, provided records for a basic list of about 80 species. Subsequently, two land-based expeditions, firstly that of R. Semon in 1892 and later that of the Carnegie Institution of Washington in 1913, increased the number of species known in the area to about 250 (H. L. Clark, 1915, 1921). South of Torres Strait along the east coast of Queensland early records of echinoderms were provided by the observations and collections of Tenison- Woods (i88oa, b) made in the Port Douglas -Trinity Bay area and by the Alert Expedition, collecting particularly from Port Curtis, Port Molle and Port Denison (see Bell, 1884). The next substantial collection was not made until 1924 when W. E. J. Paradice took about 60 species, chiefly between the latitudes of 17° and I9°S (H. L. Clark, 1926 ; McNeill & Livingstone, 1926). This collection also included specimens from Low Isles (i6°23'S), the echinoderm fauna of which is now well known as a result of the surveys by the Great Barrier Reef Expedition in 1928-29 (H. L. Clark, 1932 ; Livingstone, 1932) and the Great Barrier Reef Committee in 1954 (Endean, 1956). In recent years, further echinoderm records (excluding crinoids) have been compiled by Endean (1953, 1961, 1965), while crinoids from the Swain Reefs Expedition of 1962 have been dealt with by A. M. Clark (1975). The Great Barrier Reef as a zoogeographical region has been discussed in detail by such authors as Whitley (1932), H. L. Clark (1946) and Endean, Kenny & Stephenson (1956). In the present paper, the Great Barrier Reef Province is taken 104 GIBBS, CLARK & CLARK to include the sea area east of longitude I42°E (just west of Torres Strait) down to a depth of 200 m, from Anchor and Bramble Cays (between 9°oo'S and g°2o'S) in the north to Fraser Island including Hervey Bay (effectively the latitude of 25°S) in the south. Echinoderm records from the Queensland coast are summarized by H. L. Clark (1946) and, except for crinoids, by Endean (1957) with later additions also by Endean (1961, 1965). Within the geographical limits denned above it appears that about 310 species of echinoderms have been recorded from shallow- water ; however, many of these species are known from relatively few localities and/or specimens and records are particularly sparse for the northern part of the Great Barrier Reef outside the Torres Strait region. Accordingly a list of the echinoderms collected in this area during the 1973 expedition should be of some zoogeographic value, especially as very little systematic dredging or trawling has previously been under- taken in the region as a whole (Dall & Stephenson, 1953). The echinoderm records given in the present paper result from the material collected during the Royal Society- Universities of Queensland Expedition to the Great Barrier Reef which took place from July to November 1 973 . The investigations of Phases I and II of the Expedition were mostly concerned with the structure and ecology of islands and reefs between Cairns and Pipon Island (approximately I7°S to I4°S) but Phase III operations extended northwards to Raine Island (u°36'S). Most of the records given below, particularly those of ophiuroids, originate from a benthic survey carried out using naturalist and anchor dredges (Forster, 1953) and involving bottom sampling at 62 stations in depths of 4- 64m between the latitudes of i6°42'S to n°4o'S. Station data are given in Table i. TABLE i The positions of the stations at which dredge samples were taken in the northern part of the Great Barrier Reef, with depth, description of deposit and date of collection also given STATION LATITUDE LONGITUDE DEPTH DEPOSIT DATE (S) (E) (m) (1973) Di i4°25-2' I44°47'9' 15 Muddy sand with many forams 5 Aug. D2 I4°25'i' i44°48-6' 15 Muddy sand with many forams 5 Aug. D3 I4°24'9' i44°5o-i' 16 Muddy sand with many forams 6 Aug. 04 i4°27-i' i44°53-8' 20 Muddy sand with many forams 6 Aug. 05 i4°28-7' I44°55'7' 18 Muddy sand with many forams 6 Aug. D6 i4°29'2' I44°57'8' 26 Muddy sand with many forams 6 Aug. D7 i4°28-8' i45°o-2' 26 Muddy sand with many forams 7 Aug. D8 i4°28-o' I45°o-o/ 26 Muddy sand with many forams 7 Aug. Dg i4°26-7' i44°58-9' 37 Shell gravel 7 Aug. Dio i4°29-2' i44°57-i' 20 Shell gravel 7 Aug. Dn I4°2i-i' I44°53'6' 22 Muddy sand with many forams 8 Aug. Di2 I4°i7'9' i44°53-4' 24 Muddy sand with shells 8 Aug. Di3 i4°i4-8' i44°53-2' 22 Shell gravel 8 Aug. 014 I4°i5'8' i4405i-i' 33 Muddy fine sand with shells 8 Aug. Di5 i4°22-6' i44°5o-2' 16 Muddy sand with forams 8 Aug. Di6 i4°32-2' i44°53'4' n Muddy sand with shells 9 Aug. Di7 I4°34'2' i44°52-2' 4 Clean medium sand with shells 9 Aug. ECHINODERMS FROM THE GREAT BARRIER REEF TABLE i (cont.) 105 STATION LATITUDE LONGITUDE DEPTH (S) (E) (m) Di8 i4°34-°' i44°5o-5' 4 Dig i4°3i-8' i44°5o-7' 9 D20 i6°4O'4' I45°57'8/ 22 D2I i6°4O*4' i45°59-i' 24 D22 i6°40-3' I46°O'2' 27 D23 i6°3g-2' I46°i'2' 27 024 i6°40-i' I46°i'2 29 025 i6°40'7' I46°i-o' 27 D26 i6°4i-i' i46°o-8' 22 027 i6°38-i' I45°57<8/ 27 D28 i6°39-2' I45°57'6/ 27 029 i6°4i-6' I45°57'3' 9 D3o i5°44-3' I45°27-8' ii D3i I5°44'3' i45°27-7' ii D32 I5°44'0' i45°27-i' 18 D33 I5°43>2/ i45°27-4' 16 D34 i5°43-8' i45°29-2' 27 D35 i5°44-4' i45°3i-i' 27 D36 I5°45<0/ i45°33-o' 37 D37 i5°45-6' I45°35'°' 29 D38 I5042-g' i45°25-6' 21 D39 I5°40-g' i45°22-9' 2O 040 I5°39'3' I45°22'0' 18 041 I5°37'8/ I45°2i-o' 16 042 I5°39'5' i45°2g-4' 16 D43 I5°39'0' i45028-8' 18 D44 I5°38'3/ I45°28-0' 16 D45 i5°37-3' i45°26-5' 22 046 I4044-o' i45°n-6' 9 D47 I4°43'7' I45°i2-i' 9 D48 i4°43-47 i450ii-o' 7 049 i4°42-6' I45°io-i' 7 050 i4°36-8' i45°28-7' 22 051 i4°37-2' i45°26-3' 22 052 I4°39'3' i45°25-7' 24 Ki(A) I3°28-2' I43042'0/ 22 K2(A) 13*12-2' I43°34'I/ II K3(A) n°50-o' I43°34'2' 64 K3(N) ,, ,, ,, K4(A) 1 1 40*4 I43°57'8/ 35 K5(A) i i 40*4 I43058>5/ 34 K6(A) i i 40*4 i43°59-3' 36 K7(N) II°40-2' i44°o-2' 22 K8(N) n°48-4' i43°2i-4/ 18 Kg(N) I2°g-o' I43°I3.2' 24 Kio(N) I2°l8-o' i43°ig-6' 34 DEPOSIT Clean coarse sand with calcareous algae Muddy sand with shells Silty mud with many forams Silty mud with many forams Calcareous mud with few forams Muddy sand with many forams Calcareous mud with many bivalves Calcareous mud with many bivalves Muddy sand with many forams Silty mud with many forams Silty mud with many forams Clean medium sand Muddy fine sand Muddy fine sand Muddy fine sand with forams Sandy silt - few forams Mud with coral fragments Mud Mud with coral and shell Calcareous mud Muddy coarse sand with forams Muddy sand with many shells Muddy sand with much shell Muddy sand with shells Calcareous mud with coral Calcareous mud with coral Coral blocks Muddy sand with many forams Muddy sand with few forams Muddy sand with few forams Muddy sand with few forams Muddy sand with few forams Halimeda sand Silty sand with forams Silty sand with forams Sticky black mud Sticky black mud Silty fine sand with shells Halimeda sand Silty sand with Halimeda Halimeda sand Medium -coarse sand Silty sand with forams Black mud with shells Black mud with shells DATE (1973) 9 Aug. 9 Aug. 16 Aug. 16 Aug. 16 Aug. 17 Aug. 17 Aug. 17 Aug. 17 Aug. 1 8 Aug. 18 Aug. 1 8 Aug. 3i Aug. 3i Aug. 3 1 Aug. 3i Aug. Sept. Sept. Sept. Sept. 2 Sept. 2 Sept. 2 Sept. 2 Sept. 4 Sept. 4 Sept. 4 Sept. 4 Sept. i Oct. i Oct. i Oct. i Oct. 21 Oct. 21 Oct. 21 Oct. 28 Oct. 29 Oct. 3i Oct. 5 Nov. 3 Nov. 3 Nov. 3 Nov. 3 Nov. 6 Nov. 7 Nov. 8 Nov. Stations Di-D52 were sampled with a naturalist dredge, Stations Ki-Kio with anchor (A) and/or naturalist (N) dredge. io6 GIBBS, CLARK & CLARK TABLE 2 Positions of islands and reefs where collections of littoral echinoderms were made. Dates of collection and survey station numbers are given LOCALITY Beesley Bewick Bird Hampton Howick Ingram Lark Passage (reef to N of ) Lizard Low Mid Reef Noble Pelican Pipon Three Turtle I Turtle IV Two Watson LATITUDE (S) I2°I4-5' I4°26-0' I4°33'8' I4°30-2' I4°30-o' I5°o6-o' I4°40-o' I6°23'2' I4°30-V I4°07-4' I5°07-o' I4I44'°' I5°oi'3' I4°28-0' LONGITUDE (E) I43°I2-0' i44°48-6' I44°53'2' i44°58-4' I44°52-8' I45°44'0' DATE 7 Nov. 9 Aug. 6 Nov ii Aug 8 Aug 22/23 Oct 25 Sept SURVEY STATIONS i45°28-o' 21 Oct i45°34-o' 23/30 Aug i44°57'5' 10 Aug i44°46-o' 23 Oct I43°50-o' 29 Oct I44°3i'5' 25 Oct I45°25'5' 6/28 Sept i45°n-3' 29 Sept/i4 Oct I45°I2'2' 8 Oct i45°26-6' 20/22 Sept i44°53-5' 28 July IN.i-IN.3 Z4-Z5 LD/Z3 Li-Lj 3-I-3-H ZI-Z2 TIA-TIC 2-I-2-4 TABLE 3 British Museum echinoderm collection : additional unpublished localities LOCALITY (REEF) Farquharson Lodestone Sudbury Wheeler LATITUDE (S) LONGITUDE (E) i? 47'5 i8°4i-5' I7°oo-o' i8°48-5' i46°3i-o' I47°o6-o' I46°i3-o' DEPTH (m) 3-6 3-6 Littoral investigations were chiefly directed towards a survey of the fauna inhabiting the intertidal sand and mud flats on those islands and reefs visited by the Expedition. Stations are prefixed by the initial letter (s) of the island name (Table 2) : details of this survey will be published elsewhere (Gibbs, 1976). In addition, collections of echinoderms were also made on reef flats ; for the most part these species were living either under coral boulders or in crevices. Sublittoral crinoids were kindly sampled by Mr L. Zell at five localities (designated Z stations), all at 3-5 m depth, as follows : Zi - Three Isles - north end, off sand cay, September 23. Z2 - Three Isles - south-east, off mangrove island, September 26. Z3 - Lizard Island - off north-east promontory, October 21. Z4 - Ingram Island - south-west of sand cay, October 22. Z5 - Ingram Island - north-west of sand cay, October 23. ECHINODERMS FROM THE GREAT BARRIER REEF 107 Map showing collecting localities The Expedition collection is composed of about 450 specimens consisting of about 140 species plus about 12 samples of immature or incomplete specimens not positively identifiable to species. About two-thirds of the species are represented by only one or two specimens but this need not imply rarity in many cases since the larger littoral forms for example, particularly the species of holothurians, were purposely collected only once or twice, although generally common and widespread. The class Crinoidea is represented by 15 species, Asteroidea by 17, Ophiuroidea by 56, io8 GIBBS, CLARK & CLARK Echinoidea by 21 and Holothurioidea by 29 species. Of these totals it would appear that ii ophiuroids (including i new species), 2 echinoids and 2 holothurians* are recorded for the first time from Australian waters and 8 further ophiuroids and I holothurian newly from the Great Barrier Reef Province. These species are indicated in the systematic account. Twenty-two of the species are not listed by A. M. Clark & Rowe (1971) as occurring in some part of the whole of northern Australia, so that the number of species from this area is increased to about 460 ; the total number of species for the Great Barrier Reef Province rises to about 330. Considerable faunistic information is available for Low Isles as a result of the surveys of 1928-29 and 1954. The 1973 expedition spent just seven days at Low Isles but it is worth noting that seven species of echinoderms, previously unrecorded for these islands, were taken. These are Gomophia egyptiaca, Amphioplus (Lyman- ella) bocki, Amphiura diacritica, Schizaster lacunosus, Leptosynapta latipatina, Opheodesoma grisea and Chiridota rigida. The bulk of the echinoderm material collected on the Royal Society- Universities of Queensland Expedition has been deposited in the collections of the British Museum (Natural History). Selected specimens donated to the Australian Museum, Sydney, are indicated in the text by the numbers in square brackets [ ]. The paratype of Amphiura phrixocantha sp. nov. only, is in the Queensland Museum. This report was initiated by one of us (P. E. G.) who drew up the introduction, list of associated animals (see Table 4, p. 141) and record data for the species using identifications made by the others. The notes on individual species of crinoids are by A. M. C., those on echinoids and holothurians by C. M. C., the two combining on ophiuroids so that the new species is the responsibility of both Clarks. SPECIES COLLECTED For each species the locality or station and number of specimens are given, details being found in Tables i and 2. Sight records of distinctive species (not collected) are indicated by 'S'. In the case of those species for which few locality or specimen records from the Great Barrier Reef Province exist, these are cited together with any unpublished records from the British Museum collections (Table 3). The remaining species are considered to be widespread in the Province (see Endean, 1957) and a blanket distribution for them can be assumed. References are kept to a minimum by citing, wherever possible, H. L. Clark (1946), or an alternative reference from which the original description can be traced. Synonyms and other combinations used by H. L. Clark, Livingstone and Endean are included. Class CRINOIDEA COMASTERIDAE Capillaster multiradiatus (Linnaeus, 1758) See : H. L. Clark, 1946 : 27. 052-1; K3-i. * One of these is the species here named 'Rynkatorpa sp. nov.'. Since this paper went to press Dr Rowe has provided a specific name and description, to be published shortly in this Bulletin. ECHINODERMS FROM THE GREAT BARRIER REEF 109 Comantheria briareus (Bell, 1882) See : H. L. Clark, 1946 : 34. Three Is (Zz) - 4[i]. Previous records : Port Denison ; Outer Reef between i7°S and I9°S (H. L. Clark, 1946). Comantheria or Comanthus sp. DSI - i. This specimen is immature with only 18 very slender arms, c. 70 mm long, and few division series - hence the uncertainty as to genus. Three arms arise direct from the first (IBr) division series. The proximal ossicles are smooth. The centrodorsal is very reduced, in the form of a flat pentagon marked by subradial clefts. It bears a single cirrus socket and four small 'buds' of cirri. One IIIBr series is present ; this has four ossicles (like all seven IIBr series) and is an outer one. On this account the specimen is more like Comanthus parvicirrus timorensis than Comantheria briareus, which usually has only two ossicles in the IIIBr series. Comanthina schlegeli (P. H. Carpenter, 1881) See : H. L. Clark, 1946 : 33. Three Is (Zz) - i ; Lizard I. (Za) - i. Previous records : Murray Is (3 specimens) ; Percy Is (i specimen), (H. L. Clark, 1946). Comanthus bennetti (J. Miiller, 1841) See : H. L. Clark, 1946 : 36 (as Cenolia bennetti) ; A. M. Clark & Rowe, 1971 : 16 (as Comanthus bennetti) . Lizard I. (Za) - i. B.M. collections : Wheeler Reef, near Townsville (3 specimens). Previous records : Port Denison ; north of N Direction I. (2 specimens) (H. L. Clark, 1946). Comanthus parvicirrus (J. Miiller, 1841) See : H. L. Clark, 1946 : 39 ; A. M. Clark, 1975 : 395. SYNONYMS : Comanthus annulata (Bell, 1882) H. L. Clark, 1921 ; Comanthus callipepla H. L. Clark, 1915 ; Comanthus timorensis (J. Miiller, 1841) H. L. Clark, 1946. Howick I. (north side at 3 metres depth) - [i] ; Three Is (Zi) - 2 ; Ingram I. (Z5) - 2 ; Lark Passage (reef flat) - 2. 6* no GIBBS, CLARK & CLARK Comanthus samoanus A. H. Clark, 1909 See : H. L. Clark, 1946 : 36 (as Cenolia samoana) ; A. M. Clark & Rowe, 1971 : 16 (as Comanthus samoanus}. Ingram I. (Z^) - i ; (Z5) - 2 ; Lark Passage (reef flat) - i. Comatella nigra (P. H. Carpenter, 1888) See : H. L. Clark, 1946 : 25 ; A. M. Clark, 1975 : 392. 052 - 1. B.M. collections : Wheeler Reef, near Townsville (2 specimens). Previous records : Murray Is ; Lizard I. (H. L. Clark, 1946) ; Swain Reefs (A. M. Clark, 1975). This specimen does not help to solve the problem of the distinction between Comatella nigra and Comatella stelligera mentioned by A. M. Clark (1975). It has only 28 arms, so running down to C. stelligera, but the arm length is only c. 55 mm so the infrequency of them could be accountable to immaturity. One of the few mature cirri remaining has as many as 26 segments, the division series are well separated laterally and smooth and the arms feel smooth when stroked distalwards, since only fine grooving develops on the middle and distal brachials, all characters justifying its identification as C. nigra. However, seven specimens of Comatella from the Easter Group, Abrolhos Islands, Western Australia (collected by a recent Aquinas College expedition) do fall easily into two distinct groups. Three of them have c. 54, 59 and c. 60 arms, smooth to the touch, and up to c. 31, 31 (or ? 32) and 35 cirrus segments (cirrals) - agreeing with C. nigra - as opposed to 28, 29, 29 and 29 arms, rough in texture, and up to only 21, 22, 23 and 23 cirrals respectively in the remaining four specimens, which are referable to C. stelligera. The arm length is 75-90 mm in the former (nigra) and 90-110 mm in the latter, giving no significant size difference. The cirri are remarkably reduced in this Queensland specimen, only VII mature ones remaining besides about ix more or less reduced immature ones and about six obsolete cirrus sockets. The number is usually XX-XXX. Comatella stelligera (P. H. Carpenter, 1880) See : H. L. Clark, 1946 : 26. Three Is. (Zi) - i. This specimen has 29 fairly crowded arms, with little space between the division series laterally and up to only 23 cirrus segments, agreeing with C. stelligera. Comatula pectinata (Linnaeus, 1758) See : H. L. Clark, 1946 : 31 ; A. M. Clark, 1975 : 394. K3-i. ECHINODERMS FROM THE GREAT BARRIER REEF Comatula purpurea (J. Miiller, 1843) See : A. M. Clark, 1975 : 394. D8-i. Comatula rotalaria Lamarck, 1816 See : H. L. Clark, 1946 : 29 (as Validia rotalaria) ; A. M. Clark, 1975 : 393 (as Comatula (Validia} rotalaria}. 07-1. HIMEROMETRIDAE Himerometra robustipinna (P. H. Carpenter, 1881) See : H. L. Clark, 1946 : 42. Bewick I. (7 m depth) - 2 ; Three Is (Z2) - i ; Lizard I. (Z^) - 3. B.M. collections : Farquharson Reef (4 specimens) ; Sudbury Reef (i specimen). Previous records : Ellison Reef (2 specimens) (H. L. Clark, 1946). One of the three specimens from Lizard Island is aberrant in three characters. Firstly, its enlarged basal pinnules are almost smooth in profile, the segments not being individually flared at their distal ends, while they number from 26 to as many as 32 on the few that are still intact. In H. robustipinna the maximum number given by A. H. Clark is 24 segments. Secondly, of the up to 39 segments of the peripheral cirri, as many as 20 of the distal ones have a fairly well-developed blunt, nose-like dorsal spine. In H. robustipinna usually less than ten distal segments are described as having a small median tubercle and sometimes this may be negligible. Thirdly, the middle brachials are more markedly flared and more rugose at their distal ends than in the remaining specimens, though A. H. Clark and others appear to give little weight to this character, which is hardly mentioned in the published descriptions of the species of Himerometra. This aberrant specimen seems to approximate to Himerometra bartschi A. H. Clark, 1908, known from Singapore to the Kei Islands, in the relatively large number of segments in the proximal pinnules (though as many as 40 are described for H. bartschi} which are also fairly smooth, and in the greater development of dorsal spines on the distal cirrus segments (about 25 segments being spinose in H. bartschi, described as 'small but prominent') . However, A. H. Clark considers H. robustipinna to be a particularly variable species and in the holotype itself the proximal pinnules are relatively smooth. The difference in the cirri may be more significant but better sampling is needed to show whether or not a second species of Himerometra can be recognized from Australian waters.* * Since completion of this paper, another specimen from Lizard Island (North Reef, 18 m, collected by Neville Coleman) has come to hand. This too has relatively smooth basal pinnules, stout basally but slender and flagellate terminally, PD having up to 27 segments. Two intact mature cirri with 31 and 34 segments have dorsal spines from about the twelfth. Both these characters agree with the aberrant specimen but the brachials, though becoming slightly flared, are not rugose. 112 GIBBS, CLARK & CLARK COLOBOMETRIDAE Colobometra perspinosa (P. H. Carpenter, 1881) See : H. L. Clark, 1946 : 52. Lizard I. Z - i. Oligometra carpenteri (Bell, 1884) See : H. L. Clark, 1946 : 49. D2I - I. TROPIOMETRIDAE Tropiometra afra (Hartlaub, 1890) See : H. L. Clark, 1946 : 53. Ingram I. (Z4) - 6 ; (Z5) - i. B.M. collections : Lodestone Reef, NE of Townsville (i specimen) ; Wheeler Reef, near Townsville (2 specimens). Previous records : Murray Is (3 specimens) ; Bowen (2 specimens) (H. L. Clark, 1946). Subclass ASTEROIDEA ASTROPECTINIDAE Astropecten granulatus Miiller & Troschel, 1842 See : H. L. Clark, 1946 : 76. Kg -i. ARCHASTERIDAE Archaster typicus Miiller & Troschel, 1840 See : H. L. Clark, 1946 : 79. Hampton I. (reef flat) - 3 [2] ; Low Is (I^) - 3 ; Three Is (L5) - S. GONIASTERIDAE Stellaster equestris (Retzius, 1805) See : H. L. Clark, 1946 : 97 (as Stellaster incei) ; A. M. Clark & Rowe, 1971 : 49 (as Stellaster equestris). Stellaster sp. juv. aff. S. equestris (Retzius) K6-i; Kg -i. ECHINODERMS FROM THE GREAT BARRIER REEF 113 OREASTERIDAE Culcita novaeguineae Miiller & Troschel, 1842 See : H. L. Clark, 1946 : 108. Low Is. - S ; Three Is - S. Pentaceraster regulus (Miiller & Troschel, 1842) See : H. L. Clark, 1946 : 107 (as P. australis) ; Endean, 1953 : 54 (as P. australis} ; A. M. Clark & Rowe, 1971 : 55 (as P. regulus). Di7-2; Di8-i. Protoreaster nodosus (Linnaeus, 1758) See : H. L. Clark, 1946 : 106. Di8 - 4. OPHIDIASTERIDAE Fromia sp. juv. Lizard I. (Z3) - i (on crinoid Comanthus bennetti}. Gomophia egyptiaca Gray, 1840 See : Endean, 1965 : 230. Low Is (off NE shore at 3 m depth) - i. Previous record : Heron I. (2 specimens), (Endean, 1965). Linckia taevigata (Linnaeus, 1758) See : H. L. Clark, 1946 : 117. Mid Reef - S ; Three Is - S ; Lark Passage - S. Nardoa mamillifera Livingstone, 1930 See : H. L. Clark, 1946 : 116. 044-1. Previous record : Murray Is (Livingstone, 1930). Nardoa pauciforis (von Martens, 1866) See : H. L. Clark, 1946 : 115. Mid Reef - S ; Three Is - S. Ophidiaster granifer Lutken, 1872 See : H. L. Clark, 1946 : 121. Turtle IV I. (reef flat) - 2. n4 GIBBS, CLARK & CLARK METRODIRIDAE Metrodira subulata Gray, 1840 048 - i (juvenile identified by Mrs Loisette M. Marsh). ASTEROPSEIDAE Asteropsis carinifera (Lamarck, 1816) See : H. L. Clark, 1946 : 109 (as Asterope carinifera) ; Endean, 1956 : 124 (as Asterope carinifera} ; A. M. Clark & Rowe, 1971 : 65 (as Asteropsis carinifera}. Low Is (Tripneiistes spit) - i ; Lark Passage (reef flat) - i. ASTERINIDAE Nepanthia brevis (Perrier, 1875) See : H. L. Clark, 1946 : 141. North of Snake Reef at I4°26-2'S : i45°o-7'E (Grab st. 115), 24m depth, mud- i. Patiriella pseudoexigua Dartnall, 1971 See : H. L. Clark, 1946 : 136 (as Patiriella exigua [part]) ; Endean, 1953 : 54 (as Patiriella exigua) ; 1956 : 125 (as Patiriella exigua} ; Dartnall, 1971 : 43 (as Patiriella pseudoexigua}. [Non Asterias exigua Lamarck, 1816.] Three Is (3.7) - [i] ; Turtle I I. (TIC) - 3. ACANTHASTERIDAE Acanthaster planci (Linnaeus, 1758) See : H. L. Clark, 1946 : 150. Ingram I. (Z4, Zs) - S. Subclass OPHIUROIDEA EURYALIDAE Euryale aspera Lamarck, 1816 See : H. L. Clark, 1946 : 172. K3-2. OPHIOMYXIDAE Ophiomyxa australis Liitken, 1869 See : H. L. Clark, 1946 : 170. K6-i. ECHINODERMS FROM THE GREAT BARRIER REEF 115 OPHIACANTHIDAE Ophiacantha Iconfusa Koehler, 1905 See : H. L. Clark, 1946 : 184. K3-i. AMPHIURIDAE The disc of many burrowing amphiurids is very vulnerable to loss during collection and accordingly several of these specimens cannot be determined as to species. Amphiodia sp. juv. D2 - i ; D2i -2. Amphioplus (Amphioplus) didymus H. L. Clark, 1938 (Fig. la) See : H. L. Clark, 1946 : 206 ; A. M. Clark & Rowe, 1971 : 101, fig. 48d, e. Di - i ; 03-1; Di5 - i(no disc). These specimens provide a new record for the Great Barrier Reef Province. The holotype was taken at Broome, NW Australia, and a paratype at Darwin, the type- locality of the very similar Amphioplus stenaspis H. L. Clark. H. L. Clark's descrip- tions and figures of these two species (1938) indicate that they can be distinguished by the contiguity of the radial and adoral shields and the arrangement of the oral papillae. However, his description contradicts his figure of A. didymus with regard to the adoral shields, which are in fact broadly contiguous in the holotype, as in A. stenaspis, while the present material from Queensland indicates that the radial shields may also be contiguous distally in A. stenaspis. (Incidentally the second point throws further doubt on the validity of Amphioplus iuxtus Murakami, 1943 from the Caroline Islands as distinct from A. stenaspis, commented on by A. M. Clark in 1971.) The character of the arrangement of the oral papillae in a concave row (in A . didymus) as opposed to a straight line concealing more of the oral tentacle scale (in A . stenaspis) used in the 1971 key to distinguish the two, is also now found to be variable. This leaves only the distinctive bihamulate shape of the second from lowest arm spine beyond the arm base in A. didymus as a reliable diagnostic character ; this spine in A . stenaspis is simply blunt distally (Fig. ib) . Amphioplus didymus is also liable to be confused with Amphioplus (Lymanella) bocki Koehler (see below) which similarly has two very large tentacle scales and the second arm spine modified - though in the case of A . bocki no more than broad spatulate in the Queensland specimens. The most obvious distinctions are that A. bocki has only three arm spines proximally, the arms themselves are relatively longer (about 12 times the disc diameter), the radial shields are relatively broader and more fully contiguous and the dorsal arm plates are elliptical rather than blunted rectangular in shape. Ii6 GIBBS, CLARK & CLARK Amphioplus (Amphioplus) impressus (Ljungman, 1867) See : A. M. Clark, 1970 : 63, fig. 9!, m. D22-2; 036-1; D40-[i]. This is a new record for Australian waters. The species was previously known from various localities in the East Indies, including Timor and New Guinea approximating to Australia, from the Philippines and from Marovo lagoon, Solomon Islands, collected by Gibbs in 1965 (unpublished). Amphioplus impressus may be confused with the following species, Amphioplus intermedius, since both are unusual among species of Amphioplus s.s. in having the distalmost oral papilla markedly broadened. Also the disc is fully scaled, often with a sharp edge, the radial shields are more or less fully contiguous, the arm spines number three and the two tentacle scales are moderate in size. The most obvious difference is that A . impressus has coarser, very well-defined disc scales (a minimum of six across the shortest line between two radial shields interradially in a specimen with d.d. 4-5 mm compared with c. 10 in A. intermedius with d.d. 2-5 mm). The rosette is also conspicuous in specimens of impressus with original (as opposed to regenerated) discs, the dorsal arm plates of that species also have a median distal angle and the first ventral arm plate is completely superficial, fitting up against the distal edges of the two outermost oral papillae rather than being overlain by them proximally. Amphioplus (Amphioplus) intermedius (Koehler, 1905) See : A. M. Clark, 1970 : 45, 64. D2-I. This too is a new record for Australian waters. The species was previously known from the East Indies off Java and the Borneo Bank. Comparative remarks with A. impressus are given above. Amphioplus sp. aff. A. intermedius (Koehler) D39- 2 (no discs). Amphioplus (Amphioplus) lucidus Koehler, 1922 See : H. L. Clark, 1946 : 204. D8 - i ; 041 - i ; K$ - i. A new record for the Great Barrier Reef Province. The species was previously known to the west from Broome, NW Australia, and to the south-east from Broken Bay, N.S.W. Amphioplus (Amphioplus) stenaspis H. L. Clark, 1938 (Fig. ib, c) See : H. L. Clark, 1946 : 206 ; A. M. Clark & Rowe, 1971 : 101, fig. 53c-e. D38-i(nodisc) ; K6-i. ECHINODERMS FROM THE GREAT BARRIER REEF 117 A new record for the Great Barrier Reef Province. The species was previously known only from Darwin. Comparative remarks with A . didymus are given under that heading. Amphioplus (Lymanella) bocki Koehler, 1910 (Fig. id-f) See : Devaney, 1974 : 106. Low Is : (L5) - i ; (L6) - [i] ; (Ly) - i ; Three Is (3.2) - 3. These records provide an extension of range to Australian waters for this species, recently revived by Devaney from the synonymy of Amphioplus (Lymanella) laevis (Lyman). The species was previously known from Fiji, the Society Islands, the Tuamotu Archipelago and the Cook Islands, as well as from Marovo lagoon, Solomon Islands, collected by Gibbs in 1965 (unpublished). A specimen from Three Isles has d.d. 5-5 mm and a.l. c. 70 mm, a ratio of c. i : 12. After about a year in alcohol some of the arm spines are stih1 banded with brown and there is a brown spot in the centre of each oral shield ; otherwise the specimen is pale. The disc scaling is rather fine with no distinct rosette ; the margin is distinctly angular. The radial shields are fully contiguous, length : breadth c. 3 : i and the length is about two-fifths of the disc radius, that is slightly smaller than shown in Koehler's photograph of 1927, but conforming with the range in Devaney's material. The oral shields are spearhead-shaped, longer than broad, with a short distal lobe and a sharp proximal angle. The dorsal arm plates are broad elliptical, the distal side straight to convex with no trace of a median angle (Fig. le). The ventral arm plates are pentagonal with the distal side straight. The arm spines number three throughout ; beyond the arm base the second one becomes flattened with the tip abruptly truncated. The two tentacle scales are very large, the one on the ventral arm plate sometimes extending distally beyond the plate. The complete absence of any sort of median distal angle to the dorsal arm plates and the bluntness of the middle arm spine fully justify Devaney's restoration of A. bocki from the synonymy of A. laevis, provisionally recorded here from Australian waters, which has conspicuously slender, sharp pointed arm spines. There is clearly some variation in the degree of modification of the second arm spine in A. bocki. Koehler describes the spines as obtuse and rounded at the tips, the middle one being evidently not distinguished ; Devaney's from SE Polynesia are bluntly pointed, the middle spine widest, which description agrees with the two specimens from the Solomon Islands (Fig. if). The spatulate form of the middle spine in these Queensland specimens (Fig. id) therefore appears to be excessive but does not on its own justify a taxonomic distinction. Amphioplus (Lymanella) depressus (Ljungman, 1867) See : H. L. Clark, 1946 : 205. Di - i ; D2 - i ; D6 - i ; D8 - i ; Dig - i[i] ; K3 - i ; K8 - 2. 6** u8 GIBBS, CLARK & CLARK FIG. i. Twentieth arm segments of Amphioptus species, (a) Amphioplus (Amphioplus) didymus H. L. Clark, d.d. c. 4 mm (actual disc lost), st. Di5, ventral view, (b) and (c) Amphioplus (Amphioplus) stenaspis H. L. Clark, d.d. 3-8 mm, st. K6, ventral view (b) and the corresponding dorsal arm plate (c). (d) and (e) Amphioplus (Lymanella) bocki Koehler, d.d. 5-5 mm, Low Is, ventral view (d) and the corresponding dorsal arm plate (e). (f ) Amphioplus (Lymanella) bocki Koehler, d.d. 6-0 mm, Marovo lagoon, Solomon Is, ventral view, (g) and (h) Amphioplus sp. ? A. (Lymanella) laevis (Lyman), d.d. c. 5 mm (actual disc lost), st. Ka, ventral view (g) and the corresponding dorsal arm plate (h). [The scale represents i mm.] These appear to be the first records of Amphioplus depressus from south of Torres Strait. D.d. in the largest specimen seen by H. L. Clark from Australian waters is 6 mm. One of the present collection has the disc i mm broader. Amphioplus sp. ? A. (Lymanella) laevis (Lyman, 1874) (Fig. ig, h) See : A. M. Clark & Rowe, 1971 : 102, fig. 48b, c. K2 - 2 (no discs). The slight median angle on the dorsal arm plates, relatively slender pointed arm spines and less exaggeratedly large tentacle scales than usual in Lymanella leave little doubt of the identity of these two specimens, but it should be confirmed by intact specimens with radial shields before the range of the species can definitely be extended to Australia. A. laevis was previously known from the Red Sea to the Philippines, the Gilbert Islands and various localities in the East Indies, besides also being taken at Marovo lagoon, Solomon Islands, with Amphioplus (Lymanella) bocki by Gibbs in 1965. ECHINODERMS FROM THE GREAT BARRIER REEF 119 Amphioplus sp. aff. A. (Amphioplus) pectinatus Mortensen, 1933 KIO-I. This small delicate specimen does retain the disc, though it is partly detached. The identification is only provisional on two counts, firstly because Amphioplus pectinatus is only known from as far away as Natal, South Africa, and secondly because there appear to be two distinct forms there, designated A and B by A. M. Clark (1974 : 456) and it is not yet certain to which one the holotype belongs. D.d. in this specimen is c. 4-5 mm. The disc scaling is fairly fine, the radial shields are very long and narrow and barely contiguous distally, the oral shields are pear- shaped, the adorals only contiguous interradially on the jaw with the madreporic oral shield, the dorsal arm plates thin and broad fan-shaped, the arm spines slender and tapering, numbering four or five proximally for a few segments, then three, the second from lowest developing a small, distally directed hook and the tentacle scales numbering two, moderate in size. These characters conform with those of A. pectinatus but none of them are particularly distinctive, even in combination. However, the specimen also has two unusual features : there are spinose processes distal to each radial shield and there is a second oral tentacle scale on the side of the oral plate on the same level as the usual scale above (behind) the two middle oral papillae. The former occurs in both forms of A. pectinatus but the latter only in form B (A. M. Clark, 1974, fig. 8f-i). Amphipholis squamata (Delle Chiaje, 1829) See : H. L. Clark, 1946 : 202. 05-1; D6-i; 046-2; 047-1. Amphiura (Amphiura) ambigua Koehler, 1905 See : Koehler, 1905 : 39 ; H. L. Clark, 1946 : 196. KIO-I. This is a new record for the Great Barrier Reef Province, though a specimen from Port Curtis in the British Museum collections is now also identified as Amphiura ambigua. The species was previously known in Australia from Darwin (H. L. Clark, 1938). The Kio specimen has d.d. only 3 mm ; all the arms are badly broken. The distal oral papilla is small and peg-like, there are seven arm spines proximally, the lowest and uppermost spatulate, the second and third from lowest bihamulate and the others with only distally pointing hooks and there are two large tentacle scales. These characters agree with Koehler's description of the holotype of A. ambigua, from the Sulu Archipelago, Philippines, but not the ventral side of the disc which is naked, not scaled. However, in this it agrees with H. L. Clark's key, although he does not mention the anomaly elsewhere ; presumably his Darwin specimens are partly naked. In contrast, the Port Curtis specimen has fine scaling both dorsally 120 GIBBS, CLARK & CLARK and ventrally ; d.d. is 6 mm and there are eight arm spines, the middle ones hooked ; the distal oral papilla is relatively larger and more rounded than in the smaller specimen. Several species of amphiurids are already known to show considerable variation in the extent of the disc scaling, notably Amphiura acrystata H. L. Clark, 1911, from the North Pacific, so this character alone is no barrier to considering ventrally naked Australian specimens to be conspecific with A . ambigua. Amphiura (Amphiura) bidentata H. L. Clark, 1938 See : H. L. Clark, 1946 : 197. K3-2. Amphiura (Amphiura) catephes H. L. Clark, 1938 See : H. L. Clark, 1946 : 193. D2 - i ; D6 - i. This is a new record for the Great Barrier Reef Province. The species was previously known only from two specimens taken at Port Jackson, N.S.W. Amphiura (Amphiura) constricta Lyman, 1879 See : H. L. Clark, 1946 : 194. Di6 - i ; 046 - i. Amphiura (Amphiura) diacritica H. L. Clark, 1938 See : H. L. Clark, 1946 : 196. Low Is. (L6) - i. The holotype and only other recorded specimen was taken at Black Island, Whitsunday Group (H. L. Clark, 1938). The Low Isles specimen was found in muddy sand at low water mark. Amphiura leptotata H. L. Clark, 1915 See : A. M. Clark & Rowe, 1971 : 95, fig. 5oa-c. Di - 2 ; D2 - 3 ; Dn - 2 ; Di6 - 2 ; D2i - [2] ; 023 - 3 ; 034 - i ; 039 - i ; 048 - i ; 049 - i. These records extend between i4°2i'S and i6°4o'S and provide an extension of range to Australia. The type-locality is in the Philippines and the species was also collected by Gibbs at Marovo lagoon, Solomon Islands, in 1965. It may have escaped attention because of the small size, d.d. in the holotype being only 3-5 mm and not exceeding 3 mm in the other specimens. At d.d. 3 mm the arm length is 30+ mm. The disc is covered with very fine scales above but on the ventral side this gives way proximally to naked skin with ECHINODERMS FROM THE GREAT BARRIER REEF 121 only scattered scales, appearing dark brown in colour. The radial shields are banana-shaped, two-fifths to half as long as the disc radius and with length : breadth c. 3 : i ; they are completely separated by a row of four or five scales. The arm spines number four proximally, falling to three. The second spine from below is much broader than the others with an abruptly truncated tip, not simply tapering to a blunt tip. There are no tentacle scales. The absence of tentacle scales distinguishes this species from all those included in H. L. Clark's key to the Australian species of Amphiura. However, with the partially bare underside of the disc it is shared by a species which H. L. Clark (1946 : 201) referred to Ophionephthys, namely Ophiolepis perplexa Stimpson, 1855, from Port Jackson, referred by Lyman in 1865 to Amphiura, to which it should be restored following A. M. Clark's restriction of Ophionephthys (1970). Amphiura perplexa does not appear to have been recorded from the Port Jackson area since 1855. If further material from N.S.W. proves to be conspecific with that from Queensland, then the name Amphiura leptotata must become a synonym. Amphiura (Amphiura) magnisquama H. L. Clark, 1938 See : H. L. Clark, 1946 : 195. This is a new record for the Great Barrier Reef Province. The species was previously known from off Botany Bay, N.S.W. (H. L. Clark, 1938). Amphiura phrixocantha sp. nov. (Fig. 2, PL i, figs 1-3) TYPE MATERIAL. 036 - 2. i5°45'S : i45°33'E (between Endeavour and Cairns Reefs, opposite Papuan Pass) at 37 m depth. Holotype B.M. reg. no. 1975.6.27.44 ; paratype Queensland Museum no G. 9297. DESCRIPTION. The holotype has d.d. 8mm, a.l. 30+ mm. The arms taper rather abruptly distally ; two of them are regenerating. The disc is covered with relatively large, very thick scales, numbering five to seven across each interradius between adjacent radial shields. No primary rosette is distinguishable. The disc is strongly contracted interradially and on the ventral side and this probably accounts for the almost vertical alignment of the ventral scales. The radial shields are markedly convex abradially, 1-9-2-0 mm in length, with length : breadth c. 2-0 : i and length about half the disc radius. The two of each pair are completely separated by three (or in one case four) large scales. The oral shields are keyhole-shaped, the main part almost circular but with a well-developed distal lobe ; length : breadth is 1-5:1. The adoral shields are broadly contiguous interradially with a rounded end radially ; from the middle half of the proximal side of each arises a relatively huge, very broad rounded distal oral papilla, about as long as the oral plate and about half again as broad, sometimes slightly prolonged interradially towards the block-like infradental papillae. The GIBBS, CLARK & CLARK first oral tentacle scale is compressed vertically and appears very narrow and pointed in ventral view. A most unusual additional scale borders the adradial side of the second (more superficial) oral tentacle pore like a vertical crest, its ventral end curling horizontally to a small extent just behind the large distal oral papilla, so giving the effect of a small conical additional oral papilla. It probably arises from the edge of the first ventral arm plate. The dorsal arm plates are relatively narrow, covering only the midline of the arms, rounded octagonal in shape and broadly contiguous, the distal edge straight or slightly convex, about as broad as long proximally but becoming half as broad again by the twentieth segment. The ventral arm plates are broader than long, rectangular, with blunt distal corners, the proximal and distal sides straight. The number of arm spines is nine proximally, falling to seven by the thirtieth segment but still as many as five on the distalmost segments remaining. Except for the three uppermost, which are simply flattened and blunt, and the lowermost one, which is pointed, all the spines are elaborately hooked, hence the specific name. The hooks are glassy and hyaline. The second from lowest spine is the longest and on the basal segments has a large hook directed proximally ; beyond the disc it becomes bihamulate. The next three spines are mostly also bihamulate but the sixth usually has only the distal-pointing hook. The tentacle scales are unusual. On the first four arm segments there are two large scales on each pore, a rounded proximal one on the lateral arm plate overlying a more elongated but truncated scale projecting at right angles from the side of the ventral arm plate. From about the fifth arm segment, the latter scale becomes gradually reduced in size and inset so as to become barely distinguishable from about the twelfth segment. The paratype has d.d. c 5-5 mm. The disc is again very contracted interradially. The rosette is distinct among the large rounded scales. Proximally there are not FIG. 2. Amphiura phrixocantha sp. nov. Holotype. (a) Twelfth arm segment in dorsal view, (b) Fifth segment in ventral view, (c) and (d) Parts of twelfth and twenty-fifth segments in ventral view, (e) Oblique distal ventrolateral view of seventh arm segment, the lower spines (shown uppermost in the figure) somewhat foreshortened. [The scale represents i mm.] ECHINODERMS FROM THE GREAT BARRIER REEF 123 more than six arm spines. Otherwise it is similar to the holotype, allowing for the smaller size. Both specimens, after about a year in alcohol, still show a yellow colour on the dorsal arm plates, interrupted at intervals by usually one to three unpigmented plates. AFFINITIES. This species has most in common with Amphiura dolia H. L. Clark, 1938, from Port Jackson, to which it runs down in H. L. Clark's Amphiura key of 1946 (p. 191) since it has two tentacle scales, fully scaled disc with coarse scales and numerous arm spines. The very broad distal oral papilla is shared by both, while the disc scaling is also thick and the form of the radial shields similar in A . dolia, allowing for the much larger size of the holotype, d.d. 11-12 mm. However, the arm spines are still only up to eight in number at this large size and are un- specialized, 'pointed but not acute', also the second tentacle scale maintains its size, or even exceeds the proximal scale. Amphiura (Fellaria) octacantha (H. L. Clark, 1915) See : H. L. Clark, 1946 : 200 (as Ophionephthys octacantha} ; A. M. Clark & Rowe, 1971 : 95, fig. 26b (as Amphiura (Fellaria) octacantha). SYNONYM : Ophionephthys decacantha H. L. Clark, 1938. K3-2. Previous records : Torres Strait. Dougaloplus echinatus (Ljungman, 1867) See : H. L. Clark, 1946 : 203 (as Ophiocnida echinata) ; A. M. Clark & Rowe, 1971 : 100 (as Dougaloplus echinatus). 03 - i ; 023 - [i] ; 027 - i. Previous record : Papuan Pass (i specimen) (H. L. Clark, 1932). Ophiocentrus verticillatus (Doderlein, 1896) See : H. L. Clark, 1946 : 198. D6-i. A new record for the Great Barrier Reef Province. Previously the species was known from Broome, NW Australia. OPHIAGTIDAE Ophiactis savignyi Muller & Troschel, 1842 See : H. L. Clark, 1946 : 210. Turtle I I. (reef flat) - 7. Ophiactis sp. juv. 04-1 ; D6-2; Di6-i. 124 GIBBS, CLARK & CLARK OPHIOTRICHIDAE Macrophiothrix belli (Doderlein, 1896) See : H. L. Clark, 1946 : 221. Mid Reef (reef flat) - i ; Turtle IV I. (reef flat) - i. Previous record : Torres Strait. Macrophiothrix koehleri A. M. Clark, 1968 See : Koehler, 1907 : 333 (as Ophiothrix galatheae [part]) ; H. L. Clark, 1932 : 204 (as Ophiothrix longipeda [part]) ; A. M. Clark & Rowe, 1971 : 114, fig. 37p (as Macrophiothrix koehleri) . Three Is (reef flat) - 2; Three Is (3.11) - i. In H. L. Clark's key to the species of Macrophiothrix (1946 : 218) this species runs down to the vicinity of M. spinifera and M. scotia (EE) because of the presence of spinelets on its oral shields, whereas its arm structure agrees far better with that of M . belli, the dorsal arm plates having sharp latero-distal angles and the longer arm spines smooth shafts and clavate tips. Previous records : Probably Koehler's specimen from Torres Strait as well as H. L. Clark's Barrier Reef Expedition one from Low Isles are conspecific with M. koehleri. Macrophiothrix lorioli A. M. Clark, 1968 See : A. M. Clark & Rowe, 1971 : 115, fig. 37 m. Mid Reef (reef flat) - i. This specimen provides a new record for Australian waters. The species was previously known from the South China Sea, the Solomon Islands and the Tonga Islands. In H. L. Clark's 1946 key, M. lorioli runs down to the vicinity of M . callizona, M. calyptaspis and M. michaelseni (GG) because of the unarmed oral shields and non-trapezoidal dorsal arm plates, these being fan-shaped with more or less distinct lateral angles. M. callizona differs in having elliptical dorsal arm plates and the distal side of the ventral arm plates concave rather than convex. M. calyptaspis has the arms relatively short, less than ten times the disc diameter rather than 14-19 times in M. lorioli (17-5 times in this specimen), while M. michaelseni from the west coast of Australia (as opposed to the north-west) has the radial shields more or less bare rather than covered with trifid stumps. Macrophiothrix megapoma H. L. Clark, 1938 See : H. L. Clark, 1946 : 219. ECHINODERMS FROM THE GREAT BARRIER REEF 125 Macrophiothrix sp. aff. M. longipeda (Lamarck, 1816) See : H. L. Clark, 1946 : 221. D2I-I. This specimen agrees in all respects with M. longipeda except that it has the lowermost arm spine hook-shaped with only one or two accessory spines within the main hook, rather than comb-like with multiple accessory spines. There are also only up to six arm spines (d.d. is 15 mm), an unusually small number for M. longipeda. Ophiomaza cacaotica Lyman, 1871 See : H. L. Clark, 1946 : 234. 07 - i (on crinoid Comatula rotalaria) . H. L. Clark (1921) records this commensal (or parasitic) ophiuroid from Comatula purpurea and Comanthus annulatus (i.e. Comanthus parvicirrus) . Other specimens in the British Museum collections from Queensland were from Comatula Solaris, Comantheria perplexa and Zygometra microdiscus. Ophiothela danae Verrill, 1869 See : H. L. Clark, 1946 : 229 (as Ophiothela hadra} ; A. M. Clark & Rowe, 1971 : 116, pi. 14, fig. 5. South-west of Long Reef at I5°O5-2'S : i45°33-o'E (Grab st. 3I4A), 31 m depth - innumerable specimens on a gorgonian [5]. The arm length in these specimens appears to be 3€5-5*o times the d.d., their colour in alcohol is blue on white (the gorgonian contrasts in vermilion but the match may have been better in life) and morphologically also there is no reason why they should not be referred to 0. danae, with which A. M. Clark provisionally synonymized Ophiothela hadra in 1971. Although H. L. Clark (1915) originally distinguished 0. hadra by the arms being only about twice the d.d., in 1946 he amended this to 'hardly' four times the d.d. It is possible that relative arm length may be correlated with the nature of the host, the types of 0. hadra being from a sponge where shorter arms may be at an advantage. This remains to be seen from field studies, when the extent of correlation between ophiuroid and the colour of the host can also be determined, following from Japanese work on these lines. Ophiothrix (Ophiothrix) foveolata Marktanner-Turneretscher, 1887 See : A. M. Clark & Rowe, 1971 : no, pi. 15, fig. 3. D28-2; 051-3. These records represent an extension of range to Australia. The species was previously known from the Aru and Kei Islands, the Sunda Islands and Sulu Archipelago. 126 GIBBS, CLARK & CLARK Because of the completely bare radial shields and arms of moderate length, O.foveolata runs down to Placophiothrix s.l. in H. L. Clark's key to the Ophiotrichidae (1946 : 213). The very pretty colour pattern with the radial shields and distal ends of the arm segments (ventrally as well as dorsally) outlined by narrow bands (dark-red in preserved specimens) serves to distinguish it from the species which H. L. Clark included in Ophiothrix and Placophiothrix while the narrowly contiguous dorsal arm plates exclude it from Placophiothrix. The disc armament is relatively reduced dorsally with only a few scattered spinelets. Four of these specimens have d.d. c. 6 mm and the arm length 5-0-6-7 times as much, while the fifth at d.d. 4 mm has arms 30 mm long, a ratio of i : 7-5. Ophiothrix (Acanthophiothrix) artnata Koehler, 1905 See : H. L. Clark, 1932 : 205 (part, st. 25) (as Ophiothrix stelligera) ; A. M. Clark & Rowe, 1971 : 84, 90, in (as Ophiothrix (Acanthophiothrix) armata). South-east of Long Reef at i5°04'6'S : I45°37-2'E (Grab st. 3I5A) at 31 m depth - 2 (on coral Seriatopora) ; 045 - i. Previous record : Papuan Pass (i specimen) (H. L. Clark, 1932). Since H. L. Clark (1932) did not distinguish the small Barrier Reef Expedition specimen from Ophiothrix stelligera (i.e. 0. ciliaris), Ophiothrix armata is not included in his keys of 1946. It would fall within Placophiothrix in his wide sense, because of the conspicuous, mostly bare radial shields. In the Placophiothrix key (1946 : 223) it runs down to EE, P. elegans (with a single longitudinal dark line on each arm) and P. trilineata, said to have three dark lines separated by two light ones. However, this last observation is surely a mistake since other descriptions of trilineata, which A. M. Clark has referred back to Ophiothrix s.s., give three light lines and two dark ones between them, the limits of the outer light ones sometimes irregular or ill- defined. All four specimens from the Great Barrier Reef are small with slender arms and needle-like spines, the arms being marked with two dark lines without a background of lighter colour. Ophiothrix (Acanthophiothrix) proteus Koehler, 1905 See : A. M. Clark & Rowe, 1971 : in, pi. 15, fig. 5. K6-i. This record provides an extension of range to Australia. The species has previously been recorded in the Pacific from the South China Sea, the Sunda Islands, Kei Islands and New Caledonia. The single specimen belongs to the colour form of 0. proteus which has the double dark lines on each arm green rather than purple, though the radial shields and central disc plates are still pinkish after preservation in alcohol ; the keel of the dorsal arm plates between the green lines is white. The longest arm spine is five to six times the segment length. ECHINODERMS FROM THE GREAT BARRIER REEF 127 Like the species above, 0. (Acanthophiothrix) proteus is likely to run down to section EE of H. L. Clark's 1946 key to the species of Placophiothrix. Again it is a much more slender species than trilineata. Ophiothrix (Acanthophiothrix) purpurea von Martens, 1867 See : A. M. Clark & Rowe, 1971 : 112, fig. 35d, pi. 15, figs 4, n. This record provides an extension of range to Australian waters. The species has previously been recorded through most of the Indo-West Pacific, including the Banda Sea, New Hebrides and Solomon Islands in the neighbourhood of Australia. The specimen is small with d.d. only c. 1-5 mm but has the distinctive narrow dark line on each arm and very slender form. Again it runs down to section EE of H. L. Clark's Placophiothrix key but differs from P. elegans, which A. M. Clark has referred back to Ophiothrix s.s., recorded from Disaster Bay, N.S.W., in the narrow hexagonal rather than broad rhombic dorsal arm plates and more needle-like armament. Ophiothrix (Keystonea) propinqua Lyman, 1861 See : H. L. Clark, 1946 : 232 (as Ophiotrichoides propinqua) ; A. M. Clark & Rowe, 1971 : 107, pi. 15, fig. 7 (as Ophiothrix (Keystonea) propinqua). K4-i. Previous record : Murray Is (H. L. Clark, 1946). Ophiothrix (Theophrix) pusilla Lyman, 1874 See : A. M. Clark & Rowe, 1971 : 107, fig. 35c, pi. 15, fig. 8. D6 - i ; 036 - i ; K3 - i. These records provide an extension of range to Australian waters. The species has previously been recorded from the South China Sea, Philippines, Sunda and Kei Islands. The three specimens have d.d. 2-6-3-5 mm and d.d. : a.l. i : 2-3-3-7, the relative length increasing with size. The colour in alcohol is pale with a bluish tinge and faint blue irregular bands on the arms. This is a small but distinctive species with its thick, elongate, oval dorsal arm plates, much narrower than long, relatively short arm spines not exceeding twice the segment length and complete covering of the disc including the radial shields with trifid stumps. The structure and shortness of the arms serve to distinguish it from all the species included in H. L. Clark's key for Ophiothrix (1946 : 214). OPHIOCOMIDAE Ophiarthrum elegans Peters, 1851 See : H. L. Clark, 1946 : 252. Mid Reef (reef flat) - 8 [2] ; Three Is (reef flat) - 2 ; K4 - i. 128 GIBBS, CLARK & CLARK Ophiocoma dentata Miiller & Troschel, 1842 See : H. L. Clark, 1946 : 246 (as Ophiocoma insularis var. variegata) ; Endean, J953 : 55 » J956 : 126 (both as 0. insularia var. variegata} ; A. M. Clark & Rowe, 1971 : 119 (as 0. dentata}. Mid Reef (reef flat) - 8[i] ; Lark Passage (reef flat) - 2. Ophiocoma erinaceus Miiller & Troschel, 1842 See : H. L. Clark, 1946 : 244. Turtle IV L (reef flat) - i. Ophiocoma scolopendrina (Lamarck, 1816) See : H. L. Clark, 1946 : 243. Three Is (reef flat) - 7[i] ; Lark Passage (reef flat) - i. Ophiocomella sexradia (Duncan, 1887) See : H. L. Clark, 1946 : 206 (as Amphiacantha sexradia} and 247 (as Ophiocoma parva} ; A. M. Clark & Rowe, 1971 : 118, fig. 38c-f (as Ophiocomella sexradia}. Turtle I I. (reef flat) - i. Previous records : Mer, Murray Is [also Lord Howe I.] (H. L. Clark, 1946). OPHIONEREIDAE Ophionereis dubia (Muller & Troschel, 1842) See : H. L. Clark, 1946 : 240 (as Ophionereis stigma and 0. dubia}. DS - i ; D6 - [i] ; Dig - i. As noted in 1953 (Proc. zool. Soc. Lond. 123 : 82) although H. L. Clark's supposition that the 'Alert' specimens from Torres Strait named Ophionereis dubia by Bell are in fact 0. semoni (Doderlein) is largely correct, two of them do have the disc scaling, oral shields and proximal ventral plates unobscured by skin and the arm spines relatively long, thereby justifying the inclusion of 0. dubia in the Australian fauna even if it were not for the inclusion of the north-western Australian Ophionereis stigma H. L. Clark in the synonymy. The present records extend the range south from Torres Strait. Ophionereis porrecta Lyman, 1860 See : H. L. Clark, 1946 : 238. K4-i. Previous record: Murray Is (H. L. Clark, 1921). ECHINODERMS FROM THE GREAT BARRIER REEF 129 Ophionereis semoni (Doderlein, 1896) See : H. L. Clark, 1946 : 240. Previous records : Lindeman I., near Mackay (H. L. Clark, 1938) ; east of Snake Reef (H. L. Clark, 1932) ; Low Is (Endean, 1956). OPHIODERMATIDAE Ophiarachna incrassata (Lamarck, 1816) See : H. L. Clark, 1946 : 253. Watson I. (reef flat) - I ; Mid Reef (reef flat) - 2. Ophiarachnella gorgonia (Miiller & Troschel, 1842) See : H. L. Clark, 1946 : 260. Mid Reef -4[i]. Ophiarachnella infernalis (Miiller & Troschel, 1842) See : H. L. Clark, 1946 : 262. 027 - i ; D5i - i. Ophiochaeta hirsuta Liitken, 1869 See : A. M. Clark & Rowe, 1971 : 127, fig. 44a, b. D6-i. This record provides an extension of range to Australian waters. The species has previously been recorded from Fiji and the Gilbert Islands and there are specimens in the British Museum collections from Aldabra (Indian Ocean) and Tetel (or Gaskell) Island in the Solomon Islands (collected by Dr H. G. Vevers in 1965). Though small (d.d. 4 mm) the specimen shows the mixture of extremely fine spinelets and indented granules on the disc and the spiniform rather than granuliform armament of the oral plates, which serve to distinguish Ophiochaeta hirsuta from all the ophiodermatids included in H. L. Clark's key (1946 : 252). The arm spines are short and appressed and the oral shields are bare. Unusually in this specimen the radial shields are also bare but this may be a juvenile character. The colour in alcohol consists of a light brown central area on the disc bordered with dark brown and then a white peripheral area ; ventrally the disc and arm bases are white but the rest of the arms are banded with brown on both sides. Ophiochasma stellatum (Ljungman, 1867) See : H. L. Clark, 1946 : 259. i; 026-3; D27-[i]; K3-2[i]. 130 GIBBS, CLARK & CLARK Ophiopeza spinosa (Ljungman, 1867) See : H. L. Clark, 1946 : 258 (as Ophiopezella spinosa) ; A. M. Clark & Rowe, 1971 : 127, fig. 446 (as Ophiopeza spinosa}. KS-I; K6-i. Previous records : Torres Strait ; Murray Is (H. L. Clark, 1921). Ophiopsammus yoldii (Liitken, 1856) See : H. L. Clark, 1946 : 257 (as Pectinura yoldii) ; A. M. Clark & Rowe, 1971 : 127, pi. 21, figs 7, 8 (as Ophiopsammus yoldii). K3-u[2]. Ophiodermatid sp. juv. KS-I. OPHIURIDAE Ophiolepis superba H. L. Clark, 1915 See : H. L. Clark, 1946 : 272. Two Is (reef flat) - 3. Ophiura kinbergi (Ljungman, 1867) See : H. L. Clark, 1946 : 270. D2i - i ; 023 - i ; 1)29 - 2[i] ; 031 - 5. Previous record : Murray Is (Endean, 1957). Class ECHINOIDEA CIDARIDAE Prionocidaris bispinosa (Lamarck, 1816) See : H. L. Clark, 1946 : 286. DI7-3M- DIADEMATIDAE Diadema setosum (Leske, 1778) See : H. L. Clark, 1946 : 297 (as Centrechinus setosus) ; Endean, 1956 : 127 (as Diadema setosum). Two Is (reef flat) - i ; Three Is (reef flat) - S. Mespilia globulus (Linnaeus, 1758) See : H. L. Clark, 1946 : 315. Turtle I I. (reef flat) - i ; D5o - 5[i] ; K6 - i. Previous records : Port Denison (Mortensen, 1943) ; Trinity Bay (off Cairns) (Tenison- Woods, i88ob) ; Low Is ; Hardy Reef ; Heron I. (Endean, 1961). Temnopleurus alexandri (Bell, 1884) See : H. L. Clark, 1946 : 311 (as Salmacis virgulata var. alexandri} ; Endean, 1956 : 128 (as Temnopleurus alexandri}. DI-I. Temnotrema phoenissa H. L. Clark, 1926 See : H. L. Clark, 1946 : 314. D50 - 1. This small echinoid, h.d. (horizontal diameter) 15 mm, v.d. 10 mm, is still very distinctively coloured in alcohol. The apical system is greenish, the test aborally dark purplish-red, darker in the interambulacral areas, the aboral spines red with white tips and the primary ones also with white bases ; orally the test is white and the spines pale green. This combination of colours agrees not only with that of the holotype and only recorded specimen of Temnotrema phoenissa from Ellison Reef (h.d. only 6-5 mm) but also with Temnotrema pulchellum (Mortensen), known from the Philippines to the Kei Islands. Mortensen (1943 : 268) has already suggested that the two nominal species may prove to be conspecific. Without material of T. pulchellum to hand this problem cannot be resolved. Temnopleurid sp. 04-1; 039-3. TOXOPNEUSTIDAE Gymnechinus epistichus H. L. Clark, 1912 See : H. L. Clark, 1946 : 326. D2I-I. Tripneustes gratilla (Linnaeus, 1758) See : H. L. Clark, 1946 : 326. Three Is (reef flat) - i. I32 GIBBS, CLARK & CLARK PARASALENIIDAE Parasalenia sp. K4 - i (test only and therefore not positively identifiable). ECHINOMETRIDAE Echinometra mathaei (de Blainville, 1825) See : H. L. Clark, 1946 : 332. Three Is (reef flat) - 2. ECHINONEIDAE Echinoneus abnormalis de Loriol, 1883 See : A. M. Clark & Rowe, 1971 : 158. K4-i. This record provides an extension of range to Australia. The specimen differs from Echinoneus cyclostomus Leske, 1778, known from Low Isles and Heron Island (Endean, 1956) and from Lord Howe Island (H. L. Clark, 1938), in having the spine tubercles perforated and in lacking glassy knobs on the test. E. abnormalis has previously been recorded from Mauritius (the type locality), the Kei Islands, Rotuma in the EUice Islands, Palmyra Island and the Hawaiian Islands ; there is also a specimen in the British Museum collections from Aldabra. Since the species is sympatric in most, if not all, of these localities with the much more common E. cyclostomus, it is possible that E. abnormalis may have gone unrecognized in other samples. FIBULARIIDAE Fibularia ovulum Lamarck, 1816 See : A. M. Clark & Rowe, 1971 : 161, 167. K7-i. This record represents an extension of range to Australia. The species has previously been recorded from most parts of the tropical Indo-West Pacific except from the more remote Pacific islands. Although Mortensen (1948) reckons that most of H. L. Clark's records of Fibularia craniolaris (Leske, 1778) are conspecific with Fibularia ovulum, he makes an exception of the Australian ones, referring them instead to Fibularia oblonga Gray, 1851, which he recorded from 'South, West and North Australia', without precise localities (1948 : 223). However, in H. L. Clark's key to the Australian species of Fibularia (1946 : 347) the present specimen does tend to run down to F. craniolaris on account of its high ovoid test (length : height 4-5 : 3-5 mm) and the rounded ECHINODERMS FROM THE GREAT BARRIER REEF 133 pores forming distinct petals on the aboral side (though they are not appreciably smaller than the genital pores). In these same characters it also agrees with F. oblonga, recorded by Endean (1961 : 294) from Caloundra, southern Queensland, but in intact specimens like this one, as opposed to dead tests, there are important differences in the plating of the peristome and periproct. In F. ovulum the peri- stomial membrane is devoid of plates and the periproct has five triangular plates, as this specimen shows, whereas F. oblonga has multiple smah1 irregular plates in both peristome and periproct. However, dead tests of F. ovulum should be recognizable as having the round or quadrangular periproct as broad as or broader than long, whereas in F. oblonga it is normally elongate oval. According to H. L. Clark the common Fibularia in northern Australia is F. volva Agassiz & Desor, 1847, which should be distinguishable from both F. ovulum and F. oblonga by the relatively low test (length : height c. 2 : i) with more or less tapering ends. Fibulariid sp. 037 - 2 (tests only). LAGANIDAE Laganum decagonale (de Blainville, 1827) See : A. M. Clark & Rowe, 1971 : 162. D4i - 1. Previous records : Torres Strait (Agassiz, 1881) ; Bowen (Mortensen, 1948). This species was excluded from the Australian fauna by H. L. Clark (1946) although in 1925 (p. 156) he cited a Challenger specimen of Laganum decagonale from Torres Strait, following Agassiz. There are now a total of eight Challenger laganids from Torres Strait in the British Museum collections, some acquired since 1925. Although they show considerable variation in the number and development of the genital pores and the shape of the test, several of them agree with Mortensen's description of L. decagonale (1948 : 331) in having five genital pores and an S-shaped groove for the madreporic pores on the apical system, both characters distinguishing them from Peronella. However, the extent of the variation throws some doubt on the generic weight of these characters. The remaining Challenger specimens bridge the gap with, and may even run down to, Peronella lesueuri (Valenciennes, 1841) to which H. L. Clark (1946 : 346) referred them. Laganum depressum Lesson in L. Agassiz, 1841 See : H. L. Clark, 1946 : 343 (Laganum depressum) and 344 (Laganum dyscritum) ; Endean, 1956 : 129, 134 (L. depressum). Low Is : (L5) - 5 ; (L6) - 4 ; Di7 - i ; 027 - i ; 030 - [2] ; 031 - i ; 033 - i ; - i ; D46 - i. 134 GIBBS, CLARK & CLARK This species is very common in muddy sand close to the Anchorage at Low Isles, as also noted by Endean (1956) who agreed with Mortensen (1948) that Laganum dyscritum H. L. Clark, 1932, of which Low Isles in the type locality, is synonymous with Laganum depressum. H. L. Clark had acknowledged the likelihood of confusion between the two but considered that those he called L. dyscritum have significantly broader tests, more posteriorly situated periprocts and relatively larger petaloid areas, besides having more elongated spinelets and a purplish brown coloration, rather than the yellowish-khaki usual in L. depressum. Mortensen attributed the colour difference to the type material of L. dyscritum possibly having been preserved together with comatulids and it is certainly true that most Queensland comatulids are very liable to release copious amounts of purple pigment in alcohol. None of the laganids collected at Low Isles by Gibbs are at all purple. The morphological differences Mortensen discounted as being within the range of variation of L. depressum. His conclusion is supported by a series of measurements made on the present collection together with the material from the Great Barrier Reef Expedition which H. L. Clark referred to both L. depressum and L. dyscritum as well as specimens of L. depressum from various other parts of its extensive Indo-Pacific range. Although H. L. Clark recorded four specimens of Laganum from Low Isles as L. depressum, these are all large spineless tests, length 60 mm or more, and do not compare in size with the numerous specimens from Low Isles which he referred to L. dyscritum where length is 28-42 mm. The three Great Barrier Reef Expedition specimens from st. XXIV (NE of Pasco Reef) with length 32-45 mm are unfortunately not in the British Museum collections and must be either at Harvard or the Australian Museum. H. L. Clark's values for test breadth of L. depressum of 0-80-0-85 (or 80-85%) °f length and c. 20% for distance of the periproct from the posterior edge of the test appear to have been taken from the two tests from the Anchorage area, now measured as 71 and 65 mm in length with breadths 79 and 89% and periproctal distance 19 and 18%. However, 30 specimens of L. depressum with test length c. 25-40 mm from various localities show a much greater breadth range, from 83-93% with a mean of 89%. This compares with a range of 80-94% and again a mean of 89% for 30 of the specimens which H. L. Clark named L. dyscritum, suggesting that his figure of 90-95% was biased and probably derived from only a few specimens. The mean periproctal distance also practically coincides when these two series are compared, nor is there a significant difference in the relative length of the petaloid area. Laganid sp. juv. K3 - i ; K8 - i. Peronella lesueuri (Valenciennes in L. Agassiz, 1841) See : H. L. Clark, 1946 : 346. K8-i. 135 Peronella orbicularis (Leske, 1778) See : H. L. Clark, 1946 : 346. D2 - i ; 07 - 2 ; Di4 - i ; Di6 - i ; Dig - 2 ; 036 - i ; 048 - i ; 049 - i ; D52-[2]; K2-2; K3 - i. Peronella sp. juv. DI-I. SPATANGIDAE Maretia planulata (Lamarck, 1816) See : H. L. Clark, 1946 : 380 (as Maretia ovata] [non Spatangus ovatm Leske, 1778] ; Endean, 1956 : 129 (as Maretia planulata}. Low Is (Ls) - 15 ; Low Is (Anchorage at 3 m depth) - 2 ; 023 - i ; D26 - [i] ; 029-4; Ki-6; K3-8[6]. Like Laganum depressum this species is common in muddy sand close to the Anchorage on Low Isles. During the period of exposure on day-time spring tides it often comes to the surface of the sand. This habit has also been noted in Lovenia elongata in the Red Sea and elsewhere. LOVENIIDAE Lovenia elongata (Gray, 1845) See : H. L. Clark, 1946 : 381. K7-i. SCHIZASTERIDAE Schizaster lacunosus (Linnaeus, 1758) See : H. L. Clark, 1946 : 368. Low Is (L2) - i. South of Arlington Reef at i6°42-5'S : i45°57-o'E (Grab ARL 16) at 51 m depth - i. [Both from muddy sand.] Previous records : Torres Strait ; Turtle Is (H. L. Clark, 1946). BRISSIDAE Brissus latecarinatus (Leske, 1778) (Fig. 3b) See : H. L. Clark, 1946 : 375. Pelican I. (strand line) - 4 (tests only) ; Dig - i. One of the four specimens from Pelican Island agrees in some ways more with Brissus agassizi Doderlein, 1885, having the posterior end of the test vertically truncated, the posterior interambulacrum being only slightly carinate aborally and 136 GIBBS, CLARK & CLARK FIG. 3. Profiles of (a) Brissus agassizi Doderlein and (b) B. latecarinatus. not prolonged backwards to overhang the periproct and conceal it from dorsal view (Fig. 3a), in contrast to B. latecarinatus (Fig. 3b). Endean (1956 : 129) records as 'Brissus (? latecarinatus)' a dead test from Heron Island which approximates to some extent with this specimen, lacking the overhang above the periproct, though it does have the posterior end of the test 'obliquely truncate as in typical B. latecarinatus'. In the absence of pedicellariae from this specimen it is impossible to determine if it is specifically distinct, the globiferous ones of B. agassizi being unusual in terminating in a slit bordered with long narrow teeth rather than a rounded opening with numerous small teeth, as in B. latecarinatus. Metalia spatagus (Linnaeus, 1758) See : H. L. Clark, 1946 : 372. Low Is (L6) - i. Previous records : Torres Strait ; Low Is (H. L. Clark, 1946). Metalia sternalis (Lamarck, 1816) See : H. L. Clark, 1946 : 372. Low Is : (L6) - i ; (Ly) - i ; 029 - [i]. These three specimens and the single Metalia spatagus were all living in muddy sand. Previous record : Low Is (H. L. Clark, 1946 ; Endean, 1957). Class HOLOTHURIOIDEA HOLOTHURIIDAE Actinopyga Imiliaris (Quoy & Gaimard, 1833) Bird I. (sand flat) - i ; Three Is (reef flat) - i ; Lark Passage (reef flat) - S. The two specimens collected both have extraordinarily few spicules and their provisional identification as A. miliaris is mainly because of the uniformly dark colour. ECHINODERMS FROM THE GREAT BARRIER REEF 137 Bohadschia argus Jaeger, 1833 See : H. L. Clark, 1946 : 425 (as Holothuria argus) ; A. M. Clark & Rowe, 1971 : 176 (as Bohadschia argus}, Three Is (reef flat) - i. Bohadschia bivittata (Mitsukuri, 1912) See : A. M. Clark & Rowe, 1971 : 194. Two Is (2.4) - i. This record provides an extension of range to Australian waters. The species has previously been recorded from southern Japan to the Philippines, Caroline Islands, Fiji, Samoa and the Bismarck Archipelago, north of New Guinea. The single large individual was found almost buried below the surface of muddy sand. After preservation in alcohol for about a year it still shows the very distinctive colour pattern of Bohadschia bivittata with two broad dark brown transverse bands across the otherwise pale yellow upper side. After contraction in preservation the specimen measures 170 mm in length. The more anterior brown band is c. 30 mm wide but is not sharply delimited anteriorly, the area up to and around the ring of 20 tentacles being brownish. The median pale 'saddle' is c. 25 mm wide and the posterior brown band c. 40 mm wide, not sharply delimited posteriorly. The under- side is uniformly pale. H. L. Clark did not distinguish Bohadschia from Holothuria. In his key to Holothuria (1946 : 422) this species, with its rosettes in the body wall, runs down to section C, which includes Bohadschia argus marked with spots and B. marmorata with irregular brown blotches on the upper side. Bohadschia marmorata Jaeger, 1833 See : H. L. Clark, 1946 : 426 (as Holothuria marmorata) ; A. M. Clark & Rowe, 1971 : 176 (as Bohadschia marmorata). Low Is (L3) - i ; Two Is (2.4) - i. Holothuria (Acanthotrapeza) coluber Semper, 1868 See : H. L. Clark, 1946 : 428. Three Is (reef flat) - i. Holothuria (Cystipus) rigida (Selenka, 1867) See : H. L. Clark, 1946 : 432. Two Is (reef flat) - i. Previous records : Murray Is ; Green I. (H. L. Clark, 1946 ; Endean, 1957), 138 GIBBS, CLARK & CLARK Holothuria (Halodeima) atra Jaeger, 1833 See : H. L. Clark, 1946 : 427. Mid Reef - S ; Low Is (L3) - 3 ; Three Is (reef flat) - 4[>] ; Three Is (3.5) - i ; Lark Passage (reef flat) - i. Holothuria (Lessonothuria) pardalis Selenka, 1867 See : H. L. Clark, 1946 : 437. Three Is (reef flat) - 2. Holothuria (Mertensiothuria) leucospilota (Brandt, 1835) See : H. L. Clark, 1946 : 438. Mid Reef - S ; Three Is (reef flat) - 4[i]. Holothuria (Mertensiothuria) ? leucospilota (Brandt) See : H. L. Clark, 1921 : 179. Low Is (L5) - [i] ; Three Is (3.5) - i. When collected these two specimens were dark brown, as usual in H. leucospilota but after preservation in alcohol they turned quite black, whereas the specimens positively identified as H. leucospilota are purplish-brown. In addition, these two were found buried on a sand flat, not on a reef flat where H. leucospilota is usually so conspicuous stretching out from under stones. However, H. L. Clark (1921) notes that older individuals of this species are much more black in colour ; though very contracted now, the two specimens were almost certainly distinctly larger than the rest in life. Their body walls, spicules and cal- careous ring agree very well. Holothuria (Metriatyla) scabra Jaeger, 1833 See : H. L. Clark, 1946 : 430. Pipon Is (sand flat) - 6[i] ; Bird I. (sand flat) - 3. Holothuria (Theelothuria) sp. juv. 032 - 1. This small specimen has the tack-like spicules characteristic of the subgenus Theelothuria but cannot be identified to species. Holothuria (Thymiosycia) arenicola Semper, 1868 (PL i, fig. 4) See : H. L. Clark, 1946 : 438. Low Is (L4) - 5 ; Three Is (3.2 & 3.5) - 2 ; Two Is (2.2) - [i]. ECHINODERMS FROM THE GREAT BARRIER REEF 139 This species is one of the most conspicuous members of the infauna of the sand flats, burrowing to a depth of about 25 cm. One specimen harboured the commensal fish Carapus homei Richardson (see Mukerji, 1932; Jangoux, 1974). Even when preserved in alcohol, these specimens show a conspicuously abrupt change in colour at about 10-20 mm from the anus, from the yellowish-brown with lines of small dark blotches, usually described for this species, to pure white, though after two years this is much less distinct than in the photograph from life shown in Plate i. Among the 55 specimens of H. arenicola preserved in the British Museum collections, two show a distinctly lighter posterior end ; one was collected by Gibbs in the Solomon Islands in 1965 and the other, from the 'Java Sea', was received as long ago as 1889. As far as we can ascertain, this abrupt colour change to white posteriorly has not been recorded in the literature. Holothuria (Thymiosycia) impatiens (Forskaal, 1775) See : H. L. Clark, 1946 : 434. Three Is (reef flat) - 2. Labidodemas semperianum Selenka, 1867 See : H. L. Clark, 1946 : 421. Low Is (L3) - 2. Previous records : Murray Is ; Capricorn Group (H. L. Clark, 1946). STICHOPODIDAE Stichopus chloronotus Brandt, 1835 See : H. L. Clark, 1946 : 417. Mid Reef (reef flat) — S ; Low Is (L3) - I ; Three Is (reef flat) - S ; Lark Passage (reef flat) - S ; Two Is (reef flat) - S. Stichopus horrens Selenka, 1867 See : H. L. Clark, 1946 : 418. Three Is (reef flat) - I. Stichopus variegatus Semper, 1868 See : H. L. Clark, 1946 : 418. Three Is (reef flat) - i ; Di7 - i ; K4 - i. GUGUMARIIDAE Havelockia sp. juv. D3 - i ; D2i - i. It is likely that this species would have been included in Thyone by H. L. Clark. 140 GIBBS, CLARK & CLARK Pentacta australis (Ludwig, 1875) See : H. L. Clark, 1946 : 392. D2I -2. Pentacta cucumis (Semper, 1868) See : H. L. Clark, 1946 : 393. 07-1. Previous records : Torres Strait (H. L. Clark, 1946) ; west of N Direction I. (H. L. Clark, 1932) ; Coppersmith I. (south of Whitsunday Group) (Endean, 1956). Thyone papuensis Theel, 1886 See : H. L. Clark, 1946 : 399. K8-i. PHYLLOPHORIDAE Afrocucumis africana (Semper, 1868) See : H. L. Clark, 1946 : 404 (as Discucumaria africana) ; Endean, 1956 : 130 (as Discucumaria africana} ; A. M. Clark & Rowe, 1971 : 182 (as Afrocucumis africana}. Three Is (reef flat) - [2] Three Is (3.7) - 3 ; Noble I. (reef flat) - I. An additional specimen from the Three Islands reef flat lacks spicules in the body wall and cannot be positively identified. Actinocucumis typicus Ludwig, 1874 See : H. L. Clark, 1946 : 403. D47-i. Phyllophorus (Phyllothuria) cebuensis (Semper, 1868) See : H. L. Clark, 1946 : 409. D48-[i]. We are indebted to Dr F. W. E. Rowe of the Australian Museum for identifying this very small specimen. This record provides an extension of range to Queensland waters from Western Australia, H. L. Clark (1938) having named as P. cebuensis a small specimen from Dongarra, near Geraldton, though expressing a little doubt. Previous records are from the Philippines (the type locality) and Indonesia. SYNAPTIDAE Leptosynapta latipatina H. L. Clark, 1921 See : H. L. Clark, 1946 : 454 (Leptosynapta parvipatina [lapsus]). Low Is (Li) - i. ECHINODERMS FROM THE GREAT BARRIER REEF 141 The single specimen was found among Mesochaetopterus tubes in muddy sand. The species was previously known only from the incomplete holotype, taken at Friday Island, Torres Strait (H. L. Clark, 1921). Opheodesoma grisea (Semper, 1868) See : H. L. Clark, 1946 : 449. Low Is (Tripneustes spit) - i. Rynkatorpa sp. nov. (to be described by F. W. E. Rowe; see p. 108) D33 - 2 pieces [z] (very small). Synaptula recta (Semper, 1868) See : H. L. Clark, 1946 : 453 (as Chondrocloea recta) ; A. M. Clark & Rowe, 1971 : 188 (as Synaptula recta}. Beesley I. (sand flat) - I. CHIRIDOTIDAE Chiridota rigida (Semper, 1868) See : H. L. Clark, 1946 : 457. Low Is: (L3)-3; (L7) - [i]. ACKNOWLEDGEMENTS One of us (P. E. G.) would like to thank the Royal Society for the opportunity to participate in the Expedition to the Great Barrier Reef ; and also Dr D. R. Stoddart (Leader) and other Expedition members, particularly Dr R. F. McLean, Dr J. E. N. Veron and Mr L. Zell, for much assistance in the field. The skilful help of the Masters and crews of the M.V. Calypso (J. Lawlor) and R.V. James Kirby (D. Duncan) in carrying out the dredge survey, often under difficult conditions, is gratefully acknowledged. TABLE 4 List of some associates of these echinoderms, collected simultaneously HOST ASSOCIATE CRINOIDEA Comantheria briar eus Paradyte crinoidicola (Potts) Polychaete Myzostomum sp. Myzostome Comantheria or Comanthus sp. Myzostomum sp. Myzostome Comanthina schlegeli Paradyte crinoidicola Polychaete Myzostomum sp. Myzostome Comanthus bennetti Paradyte crinoidicola Polychaete Galathea elegans Adams & White Decapod 142 GIBBS, CLARK & CLARK HOST Comanthus parvicirrus Comanthus samoanus Comatella stelligera Comatula rotalaria Himerometra robustipinna Colobometra perspinosa Tropiometra afra ASTEROIDEA At -chaster typicus Pentacer aster regulus OPHIUROIDEA Ophiarthrum elegans Ophiocoma dentata Macrophiothrix belli HOLOTHURIOIDEA Actinopyga sp. Bohadschia argus Holothuria coluber Holothuria atra Holothuria leucospilota Holothuria arenicola Stichopus chloronotus Chiridota rigida TABLE 4 (cont.) ASSOCIATE Myzostomum polycyclus Atkins Myzostome Myzostomum sp. Myzostome Paradyte crinoidicola Polychaete Myzostomum sp. Myzostome Galathea australiensis Stimpson Decapod Myzostomum sp. Myzostome Eulimid sp. Gastropod Ophiomaza cacaotica Lyman Ophiuroid Paradyte crinoidicola Polychaete Myzostomum costatum Leuckart Myzostome Myzostomum crosslandi Boulenger Myzostome Galathea elegans Decapod Paradyte crinoidicola Polychaete Paradyte crinoidicola Polychaete Galathea elegans Decapod Ophiodromus sp. Polychaete Hololepidella nigropunctata (Horst) Polychaete Hololepidella nigropunctata Polychaete Hololepidella nigropunctata Polychaete Hololepidella nigropunctata Polychaete Gastrolepidia clavigera Schmarda Polychaete Gastrolepidia clavigera Polychaete Gastrolepidia clavigera Polychaete Gastrolepidia clavigera Polychaete Gastrolepidia clavigera Polychaete Carapus homei Richardson Fish Gastrolepidia clavigera Polychaete 'Leptonid' sp. Bivalve REFERENCES AGASSIZ, A. 1881. Echinoidea. Rep. sclent. Results Voy. Challenger (Zool.) 3 : 1-321, 45 pis. BELL, F. J. 1884. Echinodermata. In Coppinger, R. W. Report on the zoological collections made in the Indo-Pacific Ocean during the voyage of H. M.S. 'Alert' , 1881-2. London : 117- i?7. 509-5*2, pis 8-17, 45. CLARK, A. M. 1970. Notes on the family Amphiuridae. Bull. Br. Mus. not. Hist. (Zool.) 19: 1-81. 1974- Notes on some echinoderms from southern Africa. Bull. Br. Mus. nat. Hist. (Zool.) 26 (6) : 421-487, 3 pis. 1975- The Swain Reefs Expedition : Crinoidea. Rec. Aust. Mus. 29 : 391-406. & ROWE, F. W. E. 1971. Monograph of shallow-water Indo-West Pacific echinoderms. London. 238 pp., 100 figs, 31 pis. ECHINODERMS FROM THE GREAT BARRIER REEF 143 CLARK, H. L. 1915. The comatulids of Torres Strait with special reference to their habits and reactions. Pap. Dep. mar. Biol. Carnegie Instn Wash. no. 8 : 67-125. 1921. The echinoderm fauna of Torres Strait : its composition and its origin. Pap. Dep. mar. Biol. Carnegie Instn Wash. no. 10 : 1-223, 3^ pis. 1925. A catalogue of the recent sea-urchins (Echinoidea) in the collection of the British Museum (Natural History}. London: xxviii + 25o, 12 pis. 1926. Notes on a collection of echinoderms from the Australian Museum. Rec. Aust. Mus. 15 : 183-192. 1932. Echinodermata (other than Asteroidea). Scient. Rep. Gt Barrier Reef Exped. 4 : 197-239, i pi. 1938. Echinoderms from Australia. Mem. Mus. comp. Zool. Harv. 55 : 1-596, 63 figs, 28 pis. 1946. The echinoderm fauna of Australia : its composition and its origin. Publs Carnegie Instn, no. 566 : 1-567. DALL, W. & STEPHENSON, W. 1953. A bibliography of the marine invertebrates of Queensland. Pap. Dep. Zool. Univ. Qd 1 : 21-49. DARTNALL, A. J. 1971. Australian sea-stars of the genus Patiriella (Asteroidea, Asterinidae) . Proc. Linn. Soc. N.S.W. 96 : 39-49, i fig., pis 3, 4. DEVANEY, D. M. 1974. Shallow-water Asterozoans of southeastern Polynesia. 2. Ophiu- roidea. Micronesica 1C : 105-214. ENDEAN, R. 1953. Queensland faunistic records. 3. Echinodermata (excluding Crinoidea). Pap. Dep. Zool. Univ. Qd 1 : 53-60. 1956. Queensland faunistic records. 4. Further records of Echinodermata (excluding Crinoidea). Pap. Dep. Zool. Univ. Qd 1 : 123-140. 1957- The biogeography of Queensland's shallow-water echinoderm fauna (excluding Crinoidea), with a rearrangement of the faunistic provinces of tropical Australia. Aust. J. Mar. Freshwat. Res. 8 : 233-273. 1961. Queensland faunistic records. 7. Additional records of Echinodermata (excluding Crinoidea). Pap. Dep. Zool. Univ. Qd 1 : 289-298. 1965. Queensland faunistic records. 8. Further records of Echinodermata (excluding Crinoidea) from southern Queensland. Pap. Dep. Zool. Univ. Qd 2 : 229-235. KENNY, R. & STEPHENSON, 1956. The ecology and distribution of intertidal organisms on the rocky shores of the Queensland mainland. Aust. J. Mar. Freshwat. Res. 7 : 88-146. FORSTER, G. R. 1953. A new dredge for collecting burrowing animals. /. mar. biol. Ass. U.K. 32: 193-198. GIBBS, P. E. 1976. The macrofauna of the intertidal sand flats on low wooded islands in the northern region of the Great Barrier Reef Province. Phil. Trans R. Soc. B (in press). JANGOUX, M. 1974. Sur 1" 'association" entre certaines Asteries (Echinodermata) et des Poissons Carapidae. Revue zool. afr. 88 : 789-796. KOEHLER, R. 1905. Ophiures de 1'Expedition du Siboga. 2. Ophiures littorales. Siboga Exped. 45b : 1-142, 18 pis. 1907. Revision de la collection des Ophiures du Museum d'Histoire Naturelle de Paris. Bull. sci. Fr. Belg. 41 : 279-351, 5 pis. 1927. Ophiures recueillis aux lies Gilbert, Marshall et Fiji. Goteborgs K. Vetensk.- o vitterhSamh. Handl. 33 (3) : 1-13, i pi. LIVINGSTONE, A. A. 1930. On some new and little-known Australian asteroids. Rec. Aust. Mus. 18 : 15-24, 5 pis. 1932. Asteroidea. Scient. Rep. Gt Barrier Reef Exped. 4 : 241-265, 2 figs, 12 pis. McNeiLL, F. A. & LIVINGSTONE, A. A. 1926. A supplementary list of the echinoderms col- lected by Surgeon Lieutenant-Commander W. E. J. Paradice, R.A.N., in Queensland and North Australia. Rec. Aust. Mus. 15 : 193-199. MORTENSEN, T. 1943. Monograph of the Echinoidea. 3(2). Camarodonta I. Copenhagen. 533 PP-, 321 figs, 56 pis. I44 GIBBS, CLARK & CLARK MORTENSEN, T. 1948. Monograph of the Echinoidea. 4 (2). Clypeastroida. Copenhagen. 471 pp., 256 figs, 72 pis. MUKERJI, D. D. 1932. Biological observations on and instances of commensalism of an ophioid fish with echinoderms from the Andaman Islands. Rec. Indian Mus. 34 : 567-569. POTTS, F. A. 1915. The fauna associated with the crinoids of a tropical coral reef : with special reference to its colour variations. Publs Carnegie Instn no. 212 : 71-96. STEPHENSON, W., ENDEAN, R. & BENNETT, I. 1958. An ecological survey of the marine fauna of Low Is., Queensland. Aust. J. Mar. Freshwat. Res. 9 : 261-318. TENISON-WOODS, J. E. i88oa. On some of the littoral marine fauna of northeast Australia. Proc. Linn. Soc. N.S.W. 5 : 106-131. [Echinoderms pp. 125-131.] i88ob. On the habits of some Australian echini. Proc. Linn. Soc. N.S.W. 5 : 193-204. WHITLEY, G. 1932. Marine zoogeographical regions of Australia. Aust. nat. 8 : 166. DR P. E. GIBBS MARINE BIOLOGICAL ASSOCIATION OF THE U. K. PLYMOUTH AILSA M. CLARK CHRISTINE M. CLARK Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 5BD PLATE i Amphiura phrixocantha sp. nov. Holotype Top. Dorsal view ( x i). Centre, left and right. Dorsal and ventral views ( x 4). Bottom. Holothuria (Thymioscyia) arenicola Semper, photographed in life ( x Bull. Br. Mus. nat. Hist. (Zool.) 30, 4 PLATE i A LIST OF SUPPLEMENTS TO THE ZOOLOGICAL SERIES OF THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) 1. KAY, E. ALISON. Marine Molluscs in the Cuming Collection British Museum (Natural History) described by William Harper Pease. Pp. 96 ; 14 Plates. 1965. (Out of Print.) 2. WHITEHEAD, P. J. P. The Clupeoid Fishes described by Lacepede, Cuvier and Valenciennes. Pp. 180 ; n Plates, 15 Text-figures. 1967. £4.80 3. TAYLOR, J. D., KENNEDY, W. J. & HALL, A. The Shell Structure and Mineralogy of the Bivalvia. Introduction. Nuculacea-Trigonacea. Pp. 125 ; 29 Plates, 77 Text-figures. 1969. £5.40. 4. HAYNES, J. R. Cardigan Bay Recent Foraminifera (Cruises of the R.V. Antur] 1962-1964. Pp. 245 ; 33 Plates, 47 Text-figures. 1973. £11.90. 5. WHITEHEAD, P. J. P. The Clupeoid Fishes of the Guianas. Pp. 227 ; 72 Text-figures. 1973. £10.65. 6. GREENWOOD, P. H. The Cichlid Fishes of Lake Victoria, East Africa : the Biology and Evolution of a Species Flock. Pp. 134 ; i Plate, 77 Text-figures. 1974. £3.75. Hardback edition £6. Printed in Great Britain by John Wright and Sons Ltd, at The Stonebridge Press, Bristol BS4 sNU 270CT197< \. MISCELLANEA BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 5 LONDON: 1976 MISCELLANEA Pp 145-203 ; 7 Plates ; 25 Text-figures GENERAL 270CT1976 BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30, No. 5 LONDON: 1976 THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be completed within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30 No. 5 of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation Bull. Br. Mus. not. Hist. (Zool.). ISSN 0007-1498 Trustees of the British Museum (Natural History), 1976 BRITISH MUSEUM (NATURAL HISTORY) Issued 28 October, 1976 Price £5-35 CONTENTS Page Tilapiine fishes from crater-lakes north of Lake Malawi. By E. TREWAVAS 149 A new species of Hemichromis (Pisces, Cichlidae) of Sierra Leone and Liberia. By A. I. PAYNE & E. TREWAVAS 159 A possible intergeneric cyprinid hybrid from Lake Tanganyika. By K. E. BANISTER 171 Two new species of large Barbus (Pisces, Cyprinidae) from central Africa. By K. E. BANISTER 191 7* TILAPIINE FISHES FROM CRATER-LAKES NORTH OF LAKE MALAWI By E. TREWAVAS SYNOPSIS Tilapia chungruruensis Ahl of a crater-lake in the Rungwe Mountains, about 32 km north of Lake Malawi, is redescribed from the holotype and ten of the 'cotypes' (paratypes). The population is related to the Sarotherodon squamipinnis group of Lake Malawi. The holotype cannot be assigned to any of the four species of this group, nor to the related species of Lakes Mweru and Rukwa, and consequently the name of neither of these can be regarded as its synonym. It may represent the result of hybridization, although this cannot be definitely assumed. Some of the 'cotypes', however, are probably 5. lidole (Trewavas) modified by the environment. Changes in the level of Lake Malawi may have permitted the natural populating of the crater-lake or it may have been stocked by man. All the specimens have relatively bigger heads than their Lake Malawi relatives and are sexually mature at a much smaller size. A comparison is drawn with the Sarotherodon species of a crater-lake in West Cameroon and with isolated populations of other species. Lake Tschungruru is probably the same lake as that now known as Masoko. Two specimens of 5. lidole from Lake Kingiri, a crater-lake nearer to Lake Malawi, are also described. INTRODUCTION THE main object of this paper is to redescribe the types of Tilapia chungruruensis Ahl, 1924, and to relate them to other tilapiine fishes of the genus Sarotherodon (formerly subgenus) to which they belong. I have also considered two specimens of this genus collected by Dr H. Albrecht in Lake Kingiri, north of Lake Malawi, and some juveniles collected in Lake Masoko by Miss C. K. Ricardo (later Dr Ricardo-Bertram) in 1937. I have been privileged to examine the holotype and eleven of the twenty-nine 'cotypes' (paratypes) of T. chungruruensis, thanks to the kindness of Dr K. Deckert, who was in charge of the fish collections in the Berlin Museum at the time of the loan. The meristic characters, the black colour and tasselled genital papilla of the males, the long pectoral fin, the long, slender caudal peduncle and the shape of the lower pharyngeal bone collectively relate these fishes to the Malawi species-flock of the 5. squamipinnis group and distinguish them from 5. rukwaensis and S. macrochir, tasselled Sarotherodon of neighbouring basins. At the time of Ahl's description and Ricardo's determination the four species of the Malawi group had not been distinguished. On the same morphological criteria used for the Malawi group (Trewavas, 1941 ; Lowe, 1952) I find that the holotype and two of the paratypes of 5. chungruruensis belong to one species, not exactly identifiable with either of the Lake Malawi species, eight others to a second species which I identify with S. lidole. (The eleventh 'cotype' is a juvenile of 42 mm SL, too small to be determined.) I Bull. BY. Mus. nat. Hist. (Zool.) 30, 5 Issued 28 October 1976 150 E. TREWAVAS therefore describe them under two headings, grouping the Lake Masoko juveniles tentatively with 5. chungruruensis and the Lake Kingiri specimens with 5. lidole. DESCRIPTION OF THE LOCALITIES Ahl (1924) quoted Fiilleborn's account of the Tschungruru-See. He stated that it is the Kiungvuvu of Cross, near the mission station of Neu-Wangermannshohe. This name is not found on recent maps, but in the Atlas of Stuhlmann's Deutsch Ost-Afrika it is marked at 9°i7'S, 33°5o'E, north of Lake Malawi but within its drainage basin. The crater-lake Masoko lies a few kilometres NW of this at about 9°i6'S, 33°43'E and is probably the same lake under another name. Fiilleborn described Lake Tschungruru as a crater-lake about 500 m in diameter and 45 m deep with no surface outlet. The water did not taste brackish. Lake Kingiri is a crater-lake about 8 km north of Lake Malawi and 3 km north of Ipinda Ferry. DESCRIPTION OF SPECIES Sarotherodon chungruruensis (Ahl) Tilapia chungruruensis Ahl, 1924 : 86. Tilapia squamipinnis (part., nee Giinther ?) ; Ricardo, 1939 : 655. TYPE MATERIAL. Holotype : the 'type' by original designation is the largest specimen, a mature male of total length 193 mm (153 + 40 mm), one of thirty numbered 208 in the Zoological Museum of the Humboldt University, Berlin, collected by Professor Fiilleborn about 1923 in Lake Tschungruru, a crater-lake in the Rungwe Mountains, north of Lake Malawi. Lectoparatypes i1 two specimens, respectively 51 and 69 mm in SL. I assign the eight other 'cotypes' examined to 5. lidole (p. 151). DESCRIPTION. Some of the variation is consistent with the usual allometries, so that the highest ratios for depth of body, length of snout, depth of preorbital, interorbital width and length of jaw are those of the holotype. So also is that of head-length, a less usual trend, but found also in some other phytoplankton feeders (S. linnellii and 5. caroli of Lake Barombi-Mbo, Cameroons), and the length of the pectoral fin. The eye, as usual, is negatively allometric. Proportions as % SL : depth of body 37-6-38-5 ; length of head 37-3-40-5 ; length of pectoral fin 35-42 ; length of caudal peduncle 13-8-16-0 (1-15-1 -3 times its depth). Proportions as % length of head : snout 29-38 ; eye 29-0-20-5 ; depth of preorbital 16-8-24-2 ; interorbital width 31-6-39-7 ; length of lower jaw 32, 32-8 in the small specimens, 39 in the holotype. Teeth in 3-4 series in upper jaw, 4-5 in lower ; 42-78 in outer row of upper jaw ; with slender shafts and curved crowns, the outer bicuspid in the young, 1 Since the holotype is not a lectotype I think that this, and not 'paralectotypes' is the correct title for those 'cotypes' that I recognize as conspecific with the holotype. TILAPIINE FISHES OF CRATER LAKES 151 mixed bi- and tri-cuspid in the holotype, which has many of the crowns broken off ; inner tricuspid, but also many of these are broken in the holotype. Gill-rakers on first arch 2 + 1 + 17. Lower pharyngeal bone : see Tables I and 2 and PI. 3. Scales in 2 or 3 series on the cheek ; 32 in the lateral line series, 4 or 4^ from origin of dorsal to lateral line. Dorsal XIV 12 (holotype), XV n or XV 12. Anal III 10-11. Caudal truncate or very slightly emarginate, not densely scaled, but with small scales extending part-way along upper and lower rays. Genital papilla small in young ; in the holotype with several short branches arising in two groups from a club-shaped base. Vertebrae 30 (14 + 16) in the holotype and one other. Colour. The holotype, a ripening male, is dark all over, including the fins. The colour is now dark brown, probably faded from black. Even the dorsal lappets are now dark. The 69 mm specimen is pale, without markings, the vertical fins faintly dusky. In the 51 mm specimen the dorsal fin and back are dark ; along the middle of the flank are four dark spots produced vertically. ADDITIONAL SPECIMENS. Four young of 35-5-61-0 mm SL were collected in crater-lake Masoko in 1937 by Miss C. K. Ricardo (later Dr Ricardo-Bertram). These also belong to the 5. squamipinnis group and both jaws and pharynx are too well toothed for 5. lidole. There are 32 or 33 scales in the lateral line series, 8 or 9 soft rays in the anal fin, 17 or 18 gill-rakers on the lower part of the first arch. The dorsal formula is XV 10 (f.i), XV n (f.2) or XVI 10 (f.i). The three of 56-61 mm have 4-5 rows of teeth in the upper jaw, 5-6 in the lower ; the length of head is 36% SL. There are 6 dark vertical bars on the body, accentuated above the lateral line. We have not so far succeeded in distinguishing between the four Malawi species at such a small size and in placing these in 5. chungruruensis. I am merely indicat- ing that like the types they are not 5. lidole and may be one of the other species or the result of hybridization between some of them. Sar other odon lidole (Trewavas) Tilapia lidole Trewavas, 1941 : 297 ; Bertram, Borley & Trewavas, 1942 : 34, fig. 46 & D ; fig. 6C ; Lowe, 1952 : 2-65. DESCRIPTION (of eight specimens from Lake Tschungruru and, in brackets, two from Lake Kingiri). The Tschungruru specimens are eight of the paratypes of T. chungruruensis, nos 2 and 4-10 in Table i. The two Kingiri fishes measure 139 + 31-5 and 162 + 39 mm to the end of the middle caudal rays ; they are listed at the end of Table i. Proportions as % SL : depth of body 34-8-40-0 (40-5, 38-4) ; length of head 39-4-42-4 (38-5, 38-6) ; length of pectoral fin 38-0-43-3 (41-5, 40-0) ; length of caudal peduncle 15-3-16-8 (16-3, 15-7) ; length of lower jaw 11-6-14-8. Depth of caudal peduncle contained 1-27-1-5 times in its length. 152 E. TREWAVAS Proportions as % length of head : length of snout 34-2-39-0 (32-6, 26-8) ; diameter of eye 21-3-24-4 (24-2, 21-0) with no evidence of allometry ; depth of preorbital 18-7-23-8 (22-4) ; interorbital width 34-0-44-5 (45-2, 44-7) ; length of lower jaw 27-8-39-6 (31-8-32-3). Proportions of lower pharyngeal bone : see Tables i and 2. Pharyngeal teeth very fine, in a restricted area. Teeth in 3 rows in both jaws with an incomplete fourth in a few ; with long, slender shafts and expanded crowns ; those of outer row bicuspid in small specimens, in some bigger fishes with an admixture of tricuspid and occasionally a few unicuspid, often but not always by wear ; a few posterior often simple. Teeth of inner rows tricuspid unless with worn crowns. Number of outer teeth in upper jaw 52 at SL 65-5 mm, 70-82 from 86 to 162 mm. Gill-rakers 2-4 + 1 + 17-20 on first arch. Scales on cheek in 2-3 rows, occasionally a few small scales of a fourth row ; lateral line series 33-34 ; 4, 4| or 5 from origin of dorsal fin to lateral line, about 20 around caudal peduncle. Dorsal XIV-XV 10-11 (XVI n, XVII 10 in Lake Kingiri) ; anal III 8-10. Vertebrae 31 in three counted. Genital papilla of a male of SL 143 mm large, with two groups of short papillae at its distal end, the pore between them. A female of SL 123 mm has enlarged ovaries, in which the biggest egg is 3 mm in long diameter. TABLE i Data from the holotype and ten paratypes of Sarotherodon chungruruensis (Ahl) in order of size No. of SL Head Ph.l. Ph.w. Rows teeth in specimen (mm) %SL % head % head Ph.l/w Ph.bl./dent. lower jaw 1- 51 373 316 316 10 13 4-5 2. 65-5 40-7 36-3 26-2 !-4 1-8 3 3- 690 37-7 346 32-7 1-06 1-2 4 4- 86-0 42-0 36-4 27-8 i'3 2'5 3 5- 93'5 40-6 37-o 26-3 i'4 2-06 3 6. 123-0 39'4 37'5 26-0 J-4 3'4 3 7- 125-0 42-4 39-6 27-0 1-47 3-88 3 8. 126-0 40-8 34-o 25-6 1-32 3'4 3 9- 141-0 40-4 38-0 25-0 i-5 3-0 3-4 10. 143-0 39-6 40-7 28-6 1-42 2-7 3 11. 1540 425 35-5 28-6 124 14 4-5 LAKE KINGIRI 139-0 38-5 37'6 27-2 1-38 1-88 3 162-0 38-6 36-0 26-2 i'37 2-2 3 No. ii is the holotype and nos i and 3 resemble it in the proportions of the lower pharyngeal bone and number of rows of teeth in the jaws ; data for these are in bold type. The other specimens are determined as 5. lidole. The measurements of the lower pharyngeal bone are its median length (Ph.l.), greatest width (Ph.w.), both expressed as % length of head ; the median length divided by the width (Ph.l/w.) and the length of the anterior blade divided by the median length of the dentigerous area (Ph.bl./dent.). For comparison the same data are given for two specimens of T. lidole from Lake Kingiri. TILAPIINE FISHES OF CRATER LAKES 153 TABLE 2 Summary of Table i 5. chungruruensis Other 'cotypes', Two holotype and lectoparatypes determined as S. lidole S. lidole from (Specimens n, i and 3) (Specimens 2, 4-10) Lake Kingiri Ph.l. % head 3i-6-35'5 34'°-4°-7 36-0,37-6 Ph.w. % head 28-6-32-7 25-6-28-6 26-2, 27-2 Ph.l./w. 1-0-1-24 I-3-I-5 x>37. 1*38 Ph.l./dent. 2-2-2-4 2-8-4-8 2-8,3-2 TABLE 3 Pharyngeal proportions in Lake Malawi S. lidole S. squamipinnis and S. saka S. karongae N 12 5 4 SL (mm) 230-285 200-250 150-235 Phar.l./w. 1-33-1-47 1-22-1-38 1-29-1-35 Phar.l./l.dent. 3-0-4-5 2-4-3-1 2-16-2-25 Colour. Small specimens and females with five dark blotches, vertically drawn out, along the side and some with two fainter on the caudal peduncle ; vaguer markings in a more dorsal row ; one male almost uniformly dark. Males with broad dark margin on dorsal fin and dark anal fin, in one with narrow white margin (as preserved). Females with no marginal dorsal band. Smaller specimens with a tilapia-mark. Caudal clear in small specimens ; in mature males of Lake Tschungruru dark or dusky with a white margin or upper corner. Male of Lake Kingiri with caudal dark proximally, distally with a dark reticulum and a pale margin. COMPARISON WITH SPECIES OF LAKE MALAWI S. lidole i. Resemblances I have identified eight Tschungruru specimens with this species because of the proportions of the pharyngeal, the narrow bands of teeth in the jaws and the general shape. (a) Pharyngeal. In adults of Lake Malawi, all bigger than the crater-lake specimens, the median length of the pharyngeal bone is 1-38-1-5 times its greatest width. In the crater-lake the ratio is 1-3-1-5 (Tables i and 2), including specimens down to 65-5 mm SL, thus smaller than the sizes at which the species has been recognized in Lake Malawi. The dentigerous area is restricted and the blade is long, also characters distinguishing 5. lidole. (b) Jaw teeth. The inner teeth of the jaws are set in irregular rows and the formula '3-4', including the outer row, expresses this irregularity rather than variation within the size-range of the crater-lake sample. In Lake Malawi, even in the much bigger adults, 3-5 is the range, in contrast to 4-7 in S. saka, S. squamipinnis and 5. karongae. 154 E- TREWAVAS (c) Plates I and 2 show the characteristic position of the greatest depth of body in front of the dorsal fin in contrast to the other species. 2. Differences from the Malawi population (a) Length of head. 5. lidole in Lake Malawi is credited by the fishermen with a big head and the ratio there shows a higher range, though with a wide overlap, in comparison with that of the other species. It is 34'0-38'5% SL in Lake Malawi in contrast to 39-4-42-4 in the crater-lake. It is true that the Malawi specimens are bigger, but smaller Malawi fishes of indeterminate species, probably including 5. lidole, have head ratios in the lower part of the range. The biggest ratios are found in much bigger, mature fishes. The significance of this will be discussed below. (b) Size at sexual maturity. Lowe (1952 : 24) gives the minimum size at sexual maturity for both males and females of S. lidole as 28 cm TL (about 240 mm SL) . In contrast, the crater-lake male of SL 143 mm (TL about 17-5 cm) already has an enlarged genital papilla terminating in a short tassel, and a female of SL 123 mm (TL 15 cm) has an ovarian egg of 3 mm long diameter. The small size and early age of sexual maturity in pond populations of other species of Sarotherodon are well known (Lowe, 1955 : 365 ; 1958 ; Hickling, 1962, 1963)- In the other crater-lake, Kingiri, the two available specimens have a head ratio at the upper end of the Malawi range. Their gonads were removed, but a short tassel on the papilla of the male shows that here too sexual maturity occurs at a smaller size than in the Great Lake. S. chungruruensis The holotype contrasts with the 5. lidole of the same crater-lake in the shape of the pharyngeal bone as expressed in its length : width ratio as well as the bigger dentigerous area relative to the length of blade (PI. 3 and Table 2). It also has more rows of teeth in the jaws and that this is not only because of its greater size is confirmed by the small lectoparatypes, which also combine a wider tooth-band with a general shape contrasting with that of S. lidole (Pis I and 2). The pharyngeal bone of the holotype contrasts more with that of the S. lidole of Lake Tschungruru than with those of Lake Malawi as figured by Bertram et al. (1942, fig. 6C). Column B of that figure, labelled T. squamipinnis , includes pharyn- geals also from S. saka (Lowe) (at that time not recognized as distinct), but from what we now know of S. saka these would be the pharyngeals with the broadest dentigerous area, and those with a concave-sided dentigerous area would be S. squamipinnis. It is the latter that most resemble the pharyngeals of 5. chungruruensis, but the breeding male of 5. squamipinnis is pale blue with a white head, that of 5. saka black, as S. chungruruensis must have been. The character of the pharyngeal bone may well have changed in the environment of the crater-lake, so this is not a final argument for not identifying 5. chungruruensis with S. saka. The holotype (and indeed some of the others) may have been the result of hybridization between, for example, 5. saka and 5. lidole. TILAPIINE FISHES OF CRATER LAKES 155 SIGNIFICANCE OF THE BIG HEAD Not only is there a high head : body ratio in the S. lidole of the crater-lake, but the same ratio in the type and lectoparatypes of T. chungruruensis is in the highest part of the range for all the species of this group in Lake Malawi. Big heads have been found in small populations of other species of Sar other odon. Two lagoon populations of the type species, 5. melanotheron , have head ratios ranging higher than the range for the rest of this widespread species. The type specimens of S. niloticus eduardianus occupied a small crater-lake on the lower slopes of Ruwenzori, near enough to the shore of Lake George to have received its fish population from that lake during an exceptionally wet season. They had evidently become more crowded as time went on and when caught were stranded on the shore of the shrinking lake. Their head-ratios ranged from 36-6 to 39-8% SL, nearly all greater than in the parent population. The 5. niloticus in Buhuku Lagoon when it was temporarily isolated from Lake Albert (see Lowe, 1958) had head-lengths ranging from 36-4 to 41-0% SL in contrast to 34-3 to 39-6% in a sample of comparable size from the open lake. The S. niloticus vulcani of Crater-lake A on the central island of Lake Rudolf provide a further example. Most of the endemic cichlid species of the Cameroons crater-lake, Barombi Mbo, are characterized by big heads, and S. linnellii and 5. caroli provide an interesting parallel to 5. lidole and the rest of the Malawi species-flock, both structurally and ecologically (Trewavas et al., 1972). The relative growth phenomenon resulting in a big head is known in pisciculture in the 'hunger-form' of the common carp. THE ORIGIN OF THE TSCHUNGRURU (? = MASOKO) FISH POPULATION Dixey (1926) gives the evidence for previous surface levels of Lake Malawi. The level has been falling since the Tertiary, for which epoch two levels have been deter- mined, respectively 300 m and 210 m above the present level. The fall is attributed mainly to subsidence of the rift floor. The Tertiary lake consisted only of the northern part, which extended from about 32 km to the north-west of the present northern end to about the latitude of Deep Bay (io°24'S). During the Quaternary the lake extended southwards and when it was 120 m above its present level still included an area 80 km north of the present north end. Just where the limit was at the time, relatively recent, of the volcanic activity that produced the Rungwe Mountains, including the Masoko crater, is not certain, but it seems quite possible that it was near enough to be supplied naturally with its fish fauna from Lake Malawi or one of its affluent rivers. If it was stocked by man the source would be the same, namely the fry that abound among the grasses and reeds of the banks ; they might have survived a journey of at the most 30 km in a calabash or a cool clay pot. Lowe (1952, 1953) has described the breeding places, seasons and colours that characterize the three tasselled tilapias of the Malawi flock at the south end of the lake. Her stay of one month (March) at Karonga near the north end was not long enough to establish such distinctions, and she found there some specimens that 156 E. TREWAVAS seemed 'equivalent to T. squamipinnis and T. saka at the south end of the lake', that is to a single representative of these two species, as well as some that could be assigned to each of them. The northern species, S. karongae, was also present and there was evidence that S. lidole was caught at a different time of the year (October). None of the examined types of S. chungruruensis has a pharyngeal bone big enough for 5. karongae so that the source-species must be 5. lidole and one or both of the other two. The seasons and topography in the north of Malawi do not provide the same framework as that within which the three southern forms preserve their identity. Still more is this true of Lake Masoko and although S. lidole has kept its chara~ter- istics with but slight modification, I find it impossible to be sure that S. chungruruensis is identical with either 5. squamipinnis or S. saka, or to justify the synonymizing of its name with either the older 5. squamipinnis or the junior S. saka. It seems more expedient to retain the name chungruruensis for the section of the crater-lake population that may be a hybrid between two or more of the southern species or a modified population of 5. saka, and to refrain from suppressing the latter name in favour of that of such a doubtful form. A fresh examination of the Lake Masoko population and its ecology with these possibilities in mind would be interesting. The specimens collected by Ricardo in 1937 are too young to provide evidence, but they do show that fish were still in the lake at that time. REFERENCES AHL, E. 1924. t)ber einen neuen Cichliden aus Ost-Afrika. Zool. Anz. 59 : 86-87. BERTRAM, C. K. RICARDO, BORLEY, H. J. H. & TREWAVAS, E. 1942. Report on the fish and fisheries of Lake Nyasa. London, Crown Agents. DIXEY, F. 1926. The Nyasaland section of the Great Rift Valley. Geogr. J. London. 68 : 117- 140. HICKLING, C. F. 1962. Fish culture. London. 1963. The cultivation of Tilapia. Scient. American 208 : 143-152. LOWE, R. H. 1952. Report on the Tilapia and other fish and fisheries of Lake Nyasa, 1945-47. London, H. M. Stationery Office. 1953. Notes on the ecology and evolution of Nyasa fishes of the genus Tilapia, with a description of T. saka Lowe. Proc. zool. Soc. Lond. 122 : 1035-1041, i pi. 1955. New species of Tilapia (Pisces, Cichlidae) from Lake Jipe and the Pangani River, East Africa. Bull. Br. Mus. nat. Hist. (Zool.) 2 : 349-368, pis 13-17. 1958. Observations on the biology of Tilapia nilotica Linne in East African waters. Rev. Zool. Bot. afr. 57 : 129-170. RICARDO, C. K. 1939. The fishes of Lake Rukwa. /. Linn. Soc. Lond. Zool. 11 : 625-657. TREWAVAS, E. 1941. Nyasa fishes of the genus Tilapia and a new species from Portuguese East Africa. Ann. Mag. nat. Hist, (n) 7 : 294-306. GREEN, J. & CORBET, S. A. 1972. Ecological studies on crater lakes in West Cameroon. Fishes of Barombi Mbo. /. Zool. Lond. 167 : 41-95, i pi. DR E. TREWAVAS Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 5BD PLATE i Above, Sarotherodon lidole of SL 125 mm from Lake Tschungruru. Below, S. chungruruensis, holotype. Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 PLATE i PLATE 2 Above, 5. lidole of SL 65-5 mm from Lake Tschungruru. Below, 5. chungruruensis, a lecto- paratype of SL 69 mm. Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 PLATE PLATE 3 Lower pharyngeal bones of, above, the holotype of 5. chungruruensis ; below, a specimen of S. lidole of SL 125 mm from Lake Tschungruru. ( x 8-25). Bull. BY. Mus. nat. Hist. (Zool.) 30, 5 PLATE 3 A NEW SPECIES OF HEMICHROMIS (PISCES, CICHLIDAE) OF SIERRA LEONE AND LIBERIA By A. I. PAYNE AND E. TREWAVAS INTRODUCTION WHILE the junior author (A. I. P.) was making a general survey of the freshwater fishes of Sierra Leone, he found a hitherto undescribed species of Hemichromis. Some specimens were taken in baited plexiglass traps similar to that described by Breder (1960) as a fry-trap ; others were caught by hook and line. Among earlier collections from Sierra Leone in the British Museum (Natural History) we found that those of Mr N. W. Thomas, received in 1915, and Mr T. S. Jones, agricultural officer in the territory in the 19503, also contained examples of the new species. The juveniles from Mr Jones had been found sufficiently striking to have been labelled with a query as to species. Two from Liberia presented by Mr E. Roloff in 1972 and provisionally labelled 'Hemichromis sp/ also belong to the new species. The description below is based mainly on preserved material, but the colour is described from life. DESCRIPTION OF NEW SPECIES Hemichromis fugax sp. n. HOLOTYPE. 51>o H. letourneuxi) BMNH 1860.4.19.3-4 (syntypes of 90-7, 95-5 H. guttatus) Locality Forest stream, Kassewe Forest Reserve, S.L. Forest stream, Kassewe Forest Reserve, S.L. Gbangbar system nr Moyamba, S.L. Stream nr Njala, S.L. nr Moyamba, S.L. River Taia, nr Njala, S.L. Kassewe, S.L. River Tabe, S.L. 'Victoria, S.L.' Potoru, S.L. 50 km from Monrovia, Liberia Freetown, S.L. Mountain stream, Freetown, S.L. North Sherbro District, S.L. 'Victoria, S.L.' Lake Kwarko, S.L. (7°i8'N, n°59'W) Black 'River', Sherbro Is., S.L. Bonthe, S.L. Bonthe, S.L. RoKupr, S.L. 19 km from Monrovia, Liberia Kiyawa River, nr Katagum, Nigeria Kiyawa River, nr Katagum, Nigeria 'Oued Rhir Constantine' 'Oued Rhir, Constantine, Algeria' Lake Mareotis, Egypt Collector A. I. Payne A. I. Payne A. I. Payne A. I. Payne A. I. Payne A. I. Payne A. I. Payne A. I. Payne N. W. Thomas T. S. Jones E. Roloff R. Dinzey Hopkins N. W. Thomas N. W. Thomas T. S. Jones T. S. Jones T. S. Jones T. S. Jones T. S. Jones C. Steiner LI. Lloyd LI. Lloyd Mus. Hist. Nat. Paris Mus. Hist. Nat. Paris Mus. Hist. Nat. Paris Stevens (pur- chased) NOTE ON THE LOCALITIES Most of the localities mentioned can be found on a modern map and by reference to our Fig. 4, but with two we had difficulty. 'Victoria, Sierra Leone.' The Official Standard Names Gazetteer gives the position of three such places, but in the maps consulted by us only those of an early Handbook of Sierra Leone (Goddard, 1925) mark any of them, and this only one, NEW SPECIES OF HEMICHROMIS 167 nearest to the Gazetteer reference 7°39'N, i2°2o'W. This is a very small place a short way inland at the latitude of the north end of Sherbro Island, north of the delta of River Jong. Among the other fishes sent from this address was one 'Psettus sebae' , which confirms it as a locality near the coast. Potoru. This also has three references in the Gazetteer, but the probable one is some 8 km west of River Moa at its expanded part. This is the only one marked FIG. 4. The site records of H. fugax (A) and H. bimaculatus (•) in Sierra Leone. At one site (?) fishes that were probably H. bimaculatus were observed but no specimens were taken. 168 A. I. PAYNE AND E. TREWAVAS on a map of 1950 (Director of Colonial Surveys, London), the period when Mr Jones was resident in Sierra Leone. It is also marked on the American i : i ooo ooo map NB 29 ser. 1301. 'Oued Rhir, Constantine.' This is the locality given in the register of BMNH for specimens of both H. saharae and H. rolandi. The original descriptions give for H. saharae 'Sahara, aux environs de Touggourth' and for H. rolandi 'Zibans, Sahara, Province de Constantine.' Both these localities are probably in the catchment area of Oued Rhir and Chott Melrhir. These and the specimens of H. letourneuxi in the BMNH are listed as 'types' by Boulenger (1915). Other syntypes remain in Paris. REFERENCES BOULENGER, G. A. 1915. Catalogue of African freshwater fishes. Vol. III. London. BREDER, C. M. 1960. Design of a fry trap. Zoologica N.Y. 45 : 155-159. DUMERIL, A. H. A. 1859 Reptiles et poissons de 1'Afrique occidentale. Arch. Mus. nat. Hist. Paris 10 : 137-268, pis xiii-xxiii. GILL, T. 1862. On the West Africa genus Hemichromis and descriptions of new species in the museums of the Academy and Smithsonian Institutions. Proc. Acad. nat. Sci. Philad. 1862 : 134-139. GODDARD, T. N. 1925. Handbook of Sierra Leone. London. GOSSE, J. P. 1963. Le milieu aquatique et 1'ecologie des poissons dans la region de Yangambi. Ann. Mus. r. Afr. centr. no. 116 : 113-249, pis i-x. GUNTHER, A. 1862. Catalogue of the Acanthopterygii Pharyngognathi in the collection of the British Museum. Vol. IV. London. LOISELLE, P. L. & WELCOMME, R. L. 1972. Description of a new genus of cichlid fish from West Africa. Rev. Zool. Bot. afr. 85 : 37-57. NIEUWENHUIZEN, A. VAN DEN, 1975. Hemichromis fasciatus - gouden schoonheid uit Afrika. II. Het Aquarium Jg. 46 : 30-34, 7 figs. Official Standard names Gazetteer No. 101. Sierra Leone. U.S. Board on Geographical Names. PELLEGRIN, J. 1904. Contribution a 1'etude anatomique, biologique et taxonomique des poissons de la famille des cichlides. Mem. Soc. zool. Fr. 16 : 41-401, pis iv-vii. PETERS, W. C. H. 1857. Neue Chromiden Gattung. Mber. K. preuss. Akad. Wiss. 1857 : 403. SAUVAGE, E. i88oa. Notes sur quelques poissons recueillis par M. Letourneux en Epire, a Corfu et dans le Lac Mareotis. Bull. Soc. philom. Paris (7) 4 : 211-215. i88ob. Description de quelques poissons d'especes nouvelles dans la collection du Musee d'Histoire Naturelle. t.c. 220-228. 1 88 1. Description de quelques poissons d'especes nouvelles dans la collection du Musee d'Histoire Naturelle. Bull. Soc. philom. Paris (7) 5 : 101-107. TREWAVAS, E. 1974. The freshwater fishes of Rivers Mungo and Meme and Lakes Kotto, Mboandong and Soden, West Cameroon. Bull. Br. Mus. nat. Nist. (Zool.) 26 : 331-419, 4 pis. DR A. I. PAYNE LANCHESTER POLYTECHNIC PRIORY STREET COVENTRY DR E. TREWAVAS Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 5BD PLATE i (A) Hemichromis bimaculatus from Bonthe. (B) H. fugax holotype. (C) H. fugax, a Liberian specimen. All to the same scale. Photo BMNH. Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 PLATE i •••••••••••••••••••••••••••••••••••••••••••••••III By K. E. BANISTER CONTENTS Page SYNOPSIS . . . . . . . . . . . .171 INTRODUCTION ........... 171 NOTES ON COUNTS AND MEASUREMENTS . . . . . .172 THE PUTATIVE HYBRIDS . . . . . . . . . . IJ2 THE PUTATIVE PARENT SPECIES . . . . . . . .176 Varicorhinus tanganicae . . . . . . . . .176 Barbus tropidolepis . . . . . . . . . .180 DISCUSSION ........... 183 ACKNOWLEDGEMENTS . . . . . . . . . .189 REFERENCES . . . . . . . . . . .189 SYNOPSIS A series of fishes from Lunkungwe (Lake Tanganyika) were found to have characters inter- mediate between two endemic species, Barbus tropidolepis and Varicorhinus tanganicae. The likelihood of a hybrid origin for the Lunkungwe fishes is discussed and comments are made on the validity of the generic separation of the two putative parent species. INTRODUCTION DURING 1968 and 1969, Dr E. K. Balon of the Zoology Department, University of Guelph, Canada, collected eleven specimens of a cyprinid fish from Lunkungwe (5°45'S, 29°55'E), Lake Tanganyika. The largest specimen (133 mm SL) is now in the Museum of Zoology, University of Michigan (MZM 191573). The other ten specimens are in the Royal Ontario Museum (ROM 28132 and 28167). These fishes are not referable to any known cyprinid species from Lake Tanganyika but are morphologically intermediate between Varicorhinus tanganicae and Barbus tropidolepis, species endemic to the Lake Tanganyika basin. From the data presented below it will be seen that the eleven Balon fishes are unlikely to represent extreme examples of either Varicorhinus tanganicae or Barbus tropidolepis. In this paper I intend to put forward the hypothesis that these eleven fishes are hybrids between Barbus tropidolepis and Varicorhinus tanganicae. Much of the evidence and discussion is, of necessity, similar to that given in Banister (1972). In that case the discovery of some fishes morphologically inter- mediate between Barbus somereni and Varicorhinus ruwenzorii was used as evidence for the hypothesized hybridization of these two species. Without breeding experiments, hybridization cannot be proved, but the circumstantial evidence is worth examining. Previously (Banister, 1972) I noted that the boundary between the African representatives of the genus Barbus and the genus Varicorhinus is Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 Issued 28 October 1976 172 K. E. BANISTER vague. It has been shown (Groenewald, 1958 ; Gaigher, 1975) that under certain conditions some species of Barbus can change their mouth form and simulate the mouth type present in Varicorhinus species. Without an examination of more trenchant characters and without a knowledge of the previous history of the specimen, an individual fish could be placed with equal justification in either genus as the two genera are currently accepted (e.g. the definitions of Boulenger, 1909, and Jubb, 1968). These two definitions are, in the light of the known variation of some species, inadequate. The morphological intermediates described here, and Barbus alluaudi (Banister, 1972), raise further doubts about whether some species have been correctly assigned to the genus Varicorhinus. Work is in progress on the limits of the genera Barbus and Varicorhinus. NOTES ON COUNTS AND MEASUREMENTS The standard length (SL) was taken in the usual manner. The lateral line count (LL) was taken from the first pore-bearing scale behind the head to the scale lying lateral to the end of the hypurals. The body depth (D) is the maximum body depth, usually to be found just in front of the dorsal fin. The anterior limit for the head length (H) and snout length (Snt) was the premaxillary symphysis, with the pre- maxillae retracted. The posterior limit for the snout is the anterior margin of the orbit and for the head length is the most posterior part of the bony edge of the operculum. The term mouth width (MW) refers to the width across the lower jaw at the level of the angle of the mouth. The pectoral fin length (Pet) is the total length of the fin, measured in a straight line from the base of the first fin ray to the distal extremity of the fin. The measurements were taken in this way because of the ease of so doing with dial calipers, which were used on all fish except the smallest when dividers were used. The caudal peduncle length (CP1) is the horizontal distance from the posterior angle at the base of the last anal fin ray to the end of the hypurals and the caudal peduncle depth is the least depth of that part. The interorbital width (IO) was measured as the least distance between the bony edges of the interorbital space. The eye diameter (I) is the horizontal diameter of the visible part of the eye. Dsp symbolizes the height of the dorsal fin from the base of the first spine to the distal extremity of the longest fin ray. With any measure- ments which were repeatable on both sides of the fish (e.g. the anterior barbel, Ab or posterior barbel, Pb) the larger was taken except in cases where a deformity was obvious. The majority of measurements were taken to the nearest millimetre, the exceptions were some measurements on small fishes ; these were taken to the nearest half millimetre. The mean is symbolized by x, the standard deviation by s.d., the standard error by s.e. and the number of fish in the sample by n. THE PUTATIVE HYBRIDS DESCRIPTION. The description is based upon n fishes of 133, 105, 77, 69, 66, 59, 59. 58, 55, 55, 55 mm SL from Lunkungwe, Lake Tanganyika, ROM 28132, 28167 and MZM 191573. The largest specimen is shown in Fig. i. AN INTERGENERIC CYPRINID HYBRID 2cm FIG. i. The largest putative hybrid, a fish of 133 mm SL. X s.d. s.e. range SL - - - 55 -133 mm D 25-8 i'5 0-4 23-5-28-6 H 27-0 1-7 0'5 23-5-29-3 I 8-5 o-5 O-2 7-8- 9-3 10 7'5 0-6 0-2 6-8- 8-8 MW 6-9 0-6 0-2 6-4- 8-5 Pet 21-3 i-i 0-3 19-6-28-6 CP1 18-9 i'5 o-5 15-3-21-0 CPd 10-9 0-7 0-2 9-8-11-7 Snt 7-8 i-i 0-6 6-8- 9-8 Ab 1-8 0'3 O-I i-5- 2-3 Pb 3'2 o-5 O-2 2-5- 3-8 Unless stated otherwise, all measurements are expressed as a percentage of the standard length. The body is compressed, with smooth dorsal and ventral profiles. The deepest part of the body is just in front of the dorsal fin. The eye is large, protuberant and just visible in ventral view. The fleshy, rounded snout terminates in a rostral flap which is level with, but does not overhang, the mouth. The anterior margin of the lower jaw is gently curved ; it has a sharp edge but lacks the conspicuous horny sheath present in specimens of Varicorhinus tanganicae (PL 2). Nevertheless, it has a shiny, padded appearance suggesting that a tough integument is present. The lower jaw is only slightly wider at its articulation than it is distally. The ventral face of the lower jaw is concave and the skin in this and the contiguous gular region bears numerous small papillae. No lateral line pores are visible on the ventral surface of the lower jaw. There are two pairs of barbels. The short anterior barbels are usually hidden in a groove between the ventral edge of the lachrymal bone and lips. In the second largest I74 K- E- BANISTER specimen (105 mm SL) a few isolated tubercles are present on the skin of the snout and the dorsal half of the lachrymal bone. The tubercles are about four times the diameter of the lateral line pores of the lachrymal bone. In nine of the specimens the gill filaments could be seen clearly through a trans- parent zone in the centre of the opercular bone. In the other two fishes a dark patch of pigment was present through which the gill filaments could only just be discerned. The peritoneum is dark grey /brown in the two specimens examined. The alimentary canal is narrow and much convoluted. There are 20 + 21 (fi), 20 + 22 (13), 21 + 20 (fi), 21 + 21 (12), 21 + 22 (13) or22 + 2i (fi) vertebrae including those comprising the Weberian mechanism. From radiographs it can be seen that the angle of insertion of the pectoral fin is different in the three samples of fishes. The angle of insertion of the pectoral fin is here defined as the angle that a line through the mid-point of the first and last pectoral radials subtends with a line from the mid-point of the occipital condyle to the mid-point of the ural centrum. In the largest fish this angle is 30° ; in the other specimens it varied from 21° to 41°. Dorsal fin. The dorsal fin has 4 simple rays and 9 (fn) branched rays. The last simple ray is thickened into a straight smooth spine (x = 26-3, s.d. = 1-5, s.e. = 0-5, range = 23-8- 28-5). A low sheath of scales is present at the base of the dorsal fin. FIG. 2. The right pharyngeal bone of the largest hybrid. AN INTERGENERIC CYPRINID HYBRID 175 FIG. 3. Occlusal views of the pharyngeal bones of hybrids of 133 and 59 mm SL to show the arrangement of the tooth rows. This sheath is highest anteriorly and is reduced to the level of the body contour by about the seventh or eighth branched ray. The origin of the dorsal fin is in advance of the pelvic fin. Squamation. In the lateral line series there are 46 (fi), 47 (fi), 49 (f2), 50 (fi), 51 (fi), 52 (fa), 53 (fi), 54 (fi) or 56 (fi) scales. From the dorsal mid-line to the lateral line there are io| (f5) or n| (f6) scales. From the lateral line to the ventral mid-line there are io£ (12), n£ (f3) or 12^ (13) scales. This count was unobtainable on some specimens. Between the lateral line and the base of the pelvic fin there are 5 1 (f5), 7 (fi) or 7! (f4). Around the mid-point of the caudal peduncle there are 22 (f5) or 24 (f4) scales. The scales bear slightly diverging striations (Fig. 5). Pharyngeal bones and teeth. The pharyngeal teeth number 2.3.5-5.3.2. The right pharyngeal bone of the largest specimen is shown in Fig. 2. The first (anterior) tooth of the inner row is short and slender and its alignment is more or less parallel with the adjacent edge of the second tooth. This tooth is large and stout with a mamilliform crown surmounted by a small recurved hook. The third, fourth and fifth teeth become progressively more slender and spatulate. The teeth of the second and third rows are smaller versions of the third, fourth and fifth teeth of the inner row. From the occlusal view of the pharyngeal bones the alignment of the middle and outer tooth rows can be seen. In about half of the specimens these two rows diverge from the first tooth of the middle row. In the rest of the specimens the rows are parallel. In two specimens one pattern is present on one bone and the others on its partner. The mean tip-to-tip length of the pharyngeal bones of a specimen 105 mm SL is 10 mm and the mean length in a specimen of 59 mm SL is 6-3 mm. These figures 10 I76 K. E. BANISTER should be compared with the measurements of the pharyngeal bones of equal-sized Barbus tropidolepis and Varicorhinus tanganicae (pp. 179 and 183). Gill-rakers. There are 15 (f5), 16 (f5) or 18 (fi) gill-rakers on the lower limb of the first gill-arch. The shape of the gill-rakers is intermediate between those of the putative parents ; i.e. they are moderately thick with a clubbed or T-shaped extremity. Coloration. These colour notes are based on alcohol-preserved specimens. The smaller fishes are lighter than the larger fishes. The body colour is yellow-brown, darker on the back than below the lateral line. The belly in some specimens has a pink tinge. There is a dark, broad mid-lateral stripe 3 or 4 scales deep caused by a concentration of pigment along the posterior edge of alternate scales in the rows at the edge of the band and on all the scales of the central rows. A distinct mid-dorsal stripe is present in several specimens. These stripes become less distinct in larger fishes as the body colour becomes progressively darker. All but two of the specimens have a clear spot on the operculum. The dorsal fin has a dark margin in small fishes but this becomes progressively fainter in larger fishes. DISTRIBUTION. All the specimens came from Lunkungwe, Lake Tanganyika. Dr Balon kindly provided the following details of the locality. The Lunkungwe River empties into a large bay on the eastern shore of central Lake Tanganyika about 100 km south of Kigoma in Tanzania. The river flows from the Kingwe mountains in a valley flanked by very steep foothills. The river gradient is steep. The width varies from 4 to 10 m, and there are rapids between rock outcrops and large boulders on the river bed. The fish were sampled about 2 km before the river empties into the lake. The river at this point flows swiftly but there are some pools with a plant resembling Fontinalis sp. The river is muddy when it empties into the lake and is bordered with reed thickets. The fish were poisoned with toxophene. THE PUTATIVE PARENT SPECIES Varicorhinus tanganicae (Boulenger, 1900) Capoeta tanganicae Boulenger 1900 : 478. Varicorhinus tanganicae : Boulenger, 1905 : 43 ; Poll, 1953 : 97. LECTOTYPE. A fish of 282 mm SL from the north end of Lake Tanganyika, one of the two syntypes, BMNH reg. no. 1906.9.6:9-10. The lectotype is the largest of the two specimens, the smaller specimen being designated a paralectotype. MATERIAL EXAMINED. Apart from the syntypes the following specimens were used in this study : BMNHi936. 6.15:731-751 ; 1955.12.20:900-903 ; 1955.12.20:881. DESCRIPTION. Two separate samples of Varicorhinus tanganicae from Lake Tanganyika have been measured. One sample, of 24 fish from 48 to 282 mm SL, is intended to show the morphometric and meristic variation of the species. The other sample consists of five fishes of 59, 59, 80, 104 and 139 mm SL which are all the specimens available close to the size range of the hybrids. These are included to enable a detailed comparison to be made limiting, as far as possible, any distortion from allometry. AN INTERGENERIC CYPRINID HYBRID 177 Sample i (n = 24) x s.d. s.e. range SL 48 -282 mm D 25-9 2-1 0-4 23-0-30-0 H 22-7 2-4 0-5 14-6-26-0 I 6-3 0-9 0-2 4-6- 8-3 IO 9-1 0-9 9-2 7-4-10-6 MW 8-0 0-5 o-i 7-1- 9-5 Pet 19-7 1-2 0-2 16-6-21-4 CP1 17-2 0-9 0-2 15-1-18-9 CPd 12-8 0-9 0-3 10-4-14-7 Snt 7-3 0-6 o-i 6-4- 8-3 Ab + Pb + Dsp 19-8 3-0 0-6 12-6-24-8 It should be noted that although two pairs of barbels are invariably present in the specimens examined they are minute in the large fishes. Consequently barbel lengths are not included in this sample but are included in the 59-139 mm SL sample below. Sample 2 (n = 5) x s.d. s.e. range SL 59 -139 mm D 26-3 1-2 0-5 25-0-28-0 H 24-8 2-0 0-9 22-3-27-1 I 7-3 0-3 o-i 6-9- 7-6 IO 8-8 0-3 o-i 8-5- 9-3 MW 8-7 0-5 0-2 7-9- 9-3 Pet 20-5 1-2 0-5 18-9-22-0 CP1 15-4 1-4 0-6 I3-5-I7-3 CPd 10-5 0-5 0-2 lo-o-ii-o Snt 6-8 0-5 0-2 6-3- 7-5 Ab (n = 4) 1-3 i-o 0-5 o-i- 2-6 Pb 3-1 1-3 0-6 1-4- 5-1 Dsp 23-9 2-3 i-o 21-2-27-3 Unless stated otherwise all measurements are expressed as a percentage of the standard length. The body is compressed and streamlined, with smooth dorsal and ventral profiles. The snout is fleshy and bluntly rounded. The rostral flap almost overlaps the margin of the upper j aw on the ventral surface of the snout. The eye is large and protuberant usually visible from below, a feature that is more conspicuous in smaller specimens. In fishes of less than about 60 mm SL the anterior edge of the lower jaw is gently curved and lacks a horny covering. The lower jaw is straight-edged in larger fishes and has a sharp horny cutting edge. A series of six or seven lateral line pores is usually conspicuous on the skin of the ventral surface of each ramus of the lower jaw. Two pairs of small barbels are I78 K. E. BANISTER FIG. 4. Varichorhinus tanganicae (from Boulenger, 1901). present. The anterior barbels can best be described as small prolongations of the postero-ventral corners of the rostral flap. The groove below the lachrymal bone is much narrower than in the Balon specimens. A few of the larger (more than about 200 mm SL) specimens have a scattering of small, poorly defined tubercles on the skin covering the lachrymal bone. The tubercles are non-contiguous and are about the same absolute size as those in the putative hybrids. The peritoneum is dark grey-brown and the intestine is more convoluted than in the putative hybrids. There are 20 + 21 (fi), 21 + 21 (12), 21 + 22 (14), 22 + 21 (12) or 22 -I- 22 (fi) vertebrae in the ten specimens radiographed. The angle of insertion of the pectoral fin varies between 37° and 51° in the ten specimens examined. Dorsal fin. There are 4 unbranched rays and 8 (14), 9 (fiy) or 10 (13) branched rays. The fourth simple ray is ossified into a straight smooth spine. The shape of FIG. 5. A scale of a specimen of Varichorhinus tanganicae of 139 mm SL (left) a hybrid of 133 mm SL (centre) and a Barbus tropidolepis of 134 mm SL (right). AN INTERGENERIC CYPRINID HYBRID 179 FIG. 6. The right pharyngeal bone of Varicorhinus tanganicae of 139 mm SL. the dorsal fin is shown in Fig. 4. The anterior half of the base of the dorsal fin is surrounded by a low sheath of scales. The origin of the dorsal fin is in front of the origin of the pelvic fin. Squamation. There are from 57 to 67 scales in the lateral line series : 57 (£2), 58 (fi), 60 (£2), 61 (14), 62 (f2), 63 (£4), 64 (£4), 65 (£4), 67 (fi). There are i2| (£12), 13 (£9) or 14-! (£3) scale rows from the dorsal mid-line to the lateral line. Between the lateral line and the ventral mid-line there are I2| (fi), 13^ (£5), 14! (£6), 15^ (£5), i6| (£2) or 17^ (f i) scale rows. These scales could not be counted on some specimens. From the lateral line to the base of the pelvic fin there are 8 (fio), 9 (£12), 10 (fi) or ii (fi) scales. Around the least circumference of the caudal peduncle there are 29 (fi), 30 (£5), 31 (£3), 32 (£6) or 33 (£2) scales. The striations on the scales are radiate, but they tend to be more divergent in smaller fishes than in larger ones. Pharyngeal bones and teeth. The pharyngeal teeth number 2.3.5-5.3.2 (Fig. 6). The teeth are slender and the posterior teeth in each row have spatulate crowns. The teeth are arranged in three parallel rows. The mean tip-to-tip measurement of the pharyngeal bones of a specimen of 104 mm SL is 8-9 mm and of a 60 mm SL specimen 6-0 mm. i8o K. E. BANISTER Gill-rakers. In the 14 specimens examined the number of gill rakers on the lower limb of the first gill arch is 17 (fi), 18 (f4), 19 (fy) or 20 (f2). The gill rakers are slender, conical and bear small lateral projections. Coloration. Live fishes were described by Poll (1953) as brown to grey on the back, paler ventrally. A silver sheen is usually present and the fins are pale grey. Preserved specimens are usually a pale yellow/brown in colour although the larger specimens tend to be greyer. DISTRIBUTION. This species is confined to the Lake Tanganyika basin. Accord- ing to Poll (1953) it is found in both the lake and the affluent rivers, even in the rapids of the inflowing streams. In the lake it is commonest in rocky areas near to the mouths of streams. It ascends rivers to breed. Small fishes (less than 80 mm SL) are rare in the lake and seem to spend the early part of their lives in the streams. In both the lake and the feeder streams Varicorhinus tanganicae is found feeding in sandy, gravelly or rocky regions, rummaging for insect larvae. Ostracods, worms and diatoms mixed with grains of sand are also found in the alimentary canal (Balon, pers. comm.). Barbus tropidolepis Boulenger, 1900 For synonymy see Banister (1973). MATERIAL EXAMINED. In addition to the syntypes, the following specimens were examined : BMNHi955. 12. 20:737-740 ; 1955.12.20:775-792 ; 1955.12.20:795-799 ; 1955.12.20:806-815 ; 1955.12.20:1169-1171. DESCRIPTION. Two separate samples of Barbus tropidolepis were measured. The first, a sample of 47 fishes from Lake Tanganyika, are between 99 and 365 mm SL and serve to show the variation of morphometric characters in the species (taken from Banister, 1973). The second sample is of ten fishes and represents all the available specimens within the size range of the putative hybrids. These ten fishes are of 56 (2), 59 (2), 60, 66, 69, 75, 105 and 134 mm SL. FIG. 7. Barbus tropidolepis (from Boulenger, 1901). AN INTERGENERIC CYPRINID HYBRID 181 Sample I (11 = 47) X s.d. s.e. range SL - - - 99 -365 mm D 28-8 2-7 0-6 25-0-33-7 H 27-0 1-4 0-3 24-8-30-1 I 9-4 i'3 o-3 7-0-11-0 10 9-0 i'5 9'3 7-4-11-4 MW 6-4 0-8 0-2 5-2- 8-8 Pet 20-8 i-o O-2 19-1-23-9 CP1 14-9 1*2 0-3 12-9-17-7 CPd 11-7 0-9 O-2 10-1-13-7 Snt 8-4 i-o 0-2 5-2- 9-3 Dsp 25-8 2-7 0-6 20-8-30-0 Sample 2 (n = 10) X s.d. s.e. range SL - - - 56 -134 mm D 26-3 2-2 0-7 23-4-30-6 H 27-2 0-7 O-2 25-9-28-8 I 8-8 0-6 O-2 8-2-IO-2 IO 8-7 0-6 0-2 7-6- 9-7 MW 5-9 o-5 0-1 5-1- 6-7 Pet 20-4 1-7 o-5 16-6-22-6 CPU M-3 I-O o-3 12-0-15-3 CPd II-2 0-6 0-2 10-5-12-1 Snt 7-3 0-6 O-2 6-5- 8-2 Dsp 28-2 i'5 o-5 25-0-30-6 All measurements are expressed as a percentage of the standard length unless stated otherwise. The body has a compressed, fusiform shape. The blunt snout lacks a rostral flap. Only a very shallow groove is present between the edge of the lachrymal bone and the snout. The eye is protuberant and conspicuous in ventral view. The mouth is subterminal. The lower jaw is narrow with a soft, curved, anterior margin. The lower lip is often discontinuous medially. A few specimens have the lips slightly thickened. The gular surface is deeply folded. There is no anterior barbel and the posterior barbel is represented by a very small papilla. Although invariably present, this barbel is too short to measure accurately. Small, scattered tubercles are present on the skin covering the dorsal part of the lachrymal bone as well as between the orbit and the nostrils. The tubercles are smaller than those of Varicorhinus tanganicae or the Balon specimens. In common with Varicorhinus tanganicae a series of 6 or 7 lateral line pores is conspicuous on the ventral surface of each ramus of the lower jaw. The peritoneum is mid-brown in colour. In the 14 specimens radiographed there are 18 + 22 (fi), 19 + 21 (£4), 19 + 22 (f8) or 19 + 23 (f i) vertebrae. The angle of insertion of the pectoral fin varies from 12° to 23° in the specimens radiographed. Dorsal fin. There are 4 unbranched rays (not 3 as reported by Boulenger, 1911, and Worthington & Ricardo, 1937). The last unbranched ray forms a smooth i82 K. E. BANISTER straight spine. There are 9 (rarely 10) branched rays. The dorsal margin of the dorsal fin has a characteristic shape which can be seen in Fig. 7. The origin of the dorsal fin is directly above or slightly in advance of the pelvic fins. Squamation. There are from 39 to 44 scales in the lateral line series : 39 (fa), 40 (fg), 41 (fn), 42 (fi3), 43 (fg), 44 (13). There are 8| (rarely 7^) scale rows between the dorsal mid-line and the lateral line and 8| (rarely 7^, very rarely g%) scale rows between the lateral line and the ventral mid-line. Around the least circumference of the caudal peduncle there are 16 (f34), 17 (f6) or 18 (17) scales. The ridges of fat that may occur on the scales of this species (see Banister, 1973) do not occur in the putative hybrids nor in Varicorhinus tanganicae. The scale striations are more or less parallel. The posterior margin of each scale is markedly lobate. Pharyngeal bones and teeth. The pharyngeal teeth usually number 2.3.5-5.3.2. The first tooth of the inner row is very small and may be absent. When absent, its locus is marked by a small pinnacle of bone. The second tooth of the inner row is stout with a molariform crown. The remaining three teeth in this row become progressively thinner. The crowns of especially the third and fourth teeth are almost as wide as that of the second tooth but are not so long, i.e. they are kidney- shaped when viewed from an occlusal position (see Fig. 9). The alignment of the second and third rows is characteristic in that the first tooth of the second row is displaced slightly so that the second and third tooth rows FIG. 8. The right pharyngeal bone of Barbus tropidolepis (from Banister, 1973)- AN INTERGENERIC CYPRINID HYBRID 183 5mm FIG. 9. Occlusal view of the right pharyngeal bone of Barbus tropidolepis (from Banister, 1973). appear to radiate from it, rather than lying parallel to each other. The mean tip-to-tip length of the pharyngeal bones from a specimen of 105 mm SL is 13-5 mm and the mean for the pharyngeal bones from a fish of 60 mm SL is 7-5 mm. Gill-rakers. There are 13 (fio), 14 (f4) or 15 (f2) gill-rakers on the lower limb of the first gill-arch in the 16 specimens examined. The gill-rakers are broad based with the outside edge produced forwards as a hook. Coloration. The colour of live fishes, as described by Poll (1953), is grey or olive on the back, lighter ventrally. There is no noticeable colour pattern. Preserved fishes are brown on the body. Small specimens (less than about 90 mm) have a dark margin to the dorsal fin ; otherwise the fins are pale brown. Habitat. This species is found in Lake Tanganyika to a depth of 25 m. It also occurs in feeder streams, especially in the breeding season (Poll, 1953). DISCUSSION There are three possible ways of regarding Balon's anomalous fishes. They could represent a new species, they could be hybrids or they could represent extreme representatives of a known species. The Balon specimens are very much rarer in the wild than either Barbus tropidolepis or Varicorhinus tanganicae and they have only been found at one locality. Hubbs, Hubbs & Johnson (1943) quote, for two species of North American Catostomidae captured in the same river system, a proportion of hybrids to parents of 4-2 and 6-4%. They also state that some hybrids are much rarer and the proportion may be about i%. There is no quantitative information available about the Balon specimens. However, Balon (pers. comm.) has stated that they occur with Barbus tropidolepis and Varicorhinus tanganicae and are very much rarer than either. This information, coupled with the conspicuous morphological intermediacy between Barbus tropidolepis 184 K. E. BANISTER and Varicorhinus tanganicae possessed by the Balon fish, suggests it is unlikely that they represent a true species. The consistent differences between Barbus tropidolepis and Varicorhinus tanganicae in morphometric and meristic characters leave no doubt as to their specific distinct- ness. The differences in mouth form and associated feeding structures could arguably be the result of particular responses to the environment (Groenewald, 1958), but this is unlikely because of the discrete differences in other, and apparently unrelated, characters. The morphometric intermediacy of aquarium-bred, and thus indisputable, hybrids has often been noted (e.g. Holcik & de Witt, ig62a, b ; Hubbs & Miller, 1952). Hubbs (1955) described the morphological intermediacy of hybrids in the wild. Berry & Low (1970) and Hubbs (1955) advocate intermediacy as a very significant character of hybridization. Unfortunately, the supporting evidence for hybridization that was used in the case of Barbus alluaudi (Banister, 1972) has not been available in this instance. For example, I have not been able to examine the gonads because of their inadequate preservation and I have but little information of the frequency of the occurrence of the Balon fishes in the wild. Therefore, the case rests solely on morphological evidence. The ii Balon fishes have 45-56 scales in the lateral line series. This is a wide range for a small sample. There are only five species of large Barbus and Varicorhinus in Lake Tanganyika. Barbus tropidolepis has 39-44 (n = 47) scales ; Varicorhinus tanganicae has 57-67 (n = 24) ; Varicorhinus leleupanus has 42 or 43 (n = 2) ; Barbus platyrhinus has 38-41 (n = 7) ; and Barbus caudovittatus has 24-30 (n = 47). Considering just the lateral line scale counts, no overlap exists between any of the recognized species and the Balon specimens ; which alone tends to render unlikely the hypothesis that these specimens represent extreme forms of any known species. Only one of the five species of Varicorhinus and large Barbus in Lake Tanganyika has smaller scales than the fishes under consideration, i.e. Varicorhinus tanganicae with 57-67 scales in the lateral line series. This species, therefore, is a certain candidate as one of the parents of the putative hybrids. On the basis of the scales alone, Barbus caudovittatus can surely be eliminated as the other parent, but this still leaves Barbus platyrhinus, Barbus tropidolepis and Varicorhinus leleupanus. The bulky body of Barbus platyrhinus is not reflected in the streamline shape of the Balon fishes. A hybrid between Varicorhinus leleupanus and Varicorhinus tanganicae would be very likely to have a wide, horny-edged 'sector' mouth. The Balon fishes do not have a wide, horny-edged 'sector' mouth. Furthermore, Varicorhinus leleupanus has not been recorded from the Lunkungwe area of Lake Tanganyika. In the wild, the Balon fishes occur together with both Barbus tropidolepis and Varicorhinus tanganicae. The range, mean and one standard deviation each side of the mean for seven morphometric characters of the putative hybrids and probable parent species are given in Table 2. The characters chosen (H, I, IO, MW, Dsp, Ab, Pb) are the same as were considered when discussing the hybrid origin of Barbus alluaudi AN INTERGENERIC CYPRINID HYBRID 185 (Banister, 1972). The choice was made partly for comparison with the Barbus alluaudi situation and partly because these are the only morphometric characters in which the putative parent species differ significantly from each other and/or from the hybrid. The samples of Barbus tropidokpis and Varicorhinus tanganicae are from the same size range as the putative hybrids. The number of vertebrae and the number of gill-rakers on the lower limb of the first gill-arch in the Balon fishes are intermediate between those of the putative parents (Table i). The pharyngeal bone length and the angle of insertion of the Total no. of vertebrae B.t. 40-42 (n = 14) Hyb. 40-43 (n = u) V.t. 41-44 (n = 10) TABLE i Gill-rakers 13-15 (n = 16) 15-18 (n = n) 17-20 (n = 14) Pectoral insertion angle 12-23° (n = 9) 21-40° (n = n) 37-51° (n = 12) Mean length of pharyngeal bones SL Ph. length (mm) (mm) V.t. 60 6-0 V.t. 104 8-9 Hyb. 59 6-3 Hyb. 105 10-0 B.t. 60 7'5 B.t. 105 13-5 pectoral fin show the same intermediacy, as does the alignment of the pharyngeal teeth. The possibility that the Balon fishes represent an extreme example of either putative parent species must now be considered. The techniques of Schultz & Schaeffer (1936) and of Hubbs, Hubbs & Johnson (1943) have been used to evaluate the probability of a character of the sample under examination falling within the 35- 30- 25- 20- 15- 10- 5- 16 1718 19 2021 22232425 262728293031 3233 FIG. 10. A histogram of the frequencies of the lateral line scale counts in Barbus tropidolepis (left), the hybrids (black, centre) and Varicorhinus tanganicae (right). i86 K. E. BANISTER 12- 10- 8- 6- 4- 2- 384042444648505254565860626466 FIG. ii. A histogram of the frequencies of the scale counts around the least circumference of the caudal peduncle in Barbus tropidolepis (left), the hybrids (black, centre) and V aricorhinus tanganicae (right). 25 26 27 28 H 23 24 25 26 27 FIG. 12. A comparison of the range, mean and standard deviations of the head length in the three forms. The base line represents the range, the vertical line the mean and the black area covers one standard deviation either side of the mean. The figures are the lengths of the heads expressed as a percentage of the standard length. B = Barbus tropidolepis, V = Varicorhinus tanganicae, H = hybrids. 8-0 8-5 9-0 9-5 H 8O 8-5 9-0 7-0 7-5 8-0 8-5 7-0 7-5 8-5 90 FIG. 13. Comparisons of the eye diameter (left) and interorbital width (right) in the three forms. Details as in Fig. 12. AN INTERGENERIC CYPRINID HYBRID 187 range of that character in either of the putative parent species. The results are shown in Table 2. TABLE 2 Character n x s.d. % B % V P H V. t. 5 24-82 2-05 0-4 Hyb. ii 26-97 I-72 91 9 B. t. 10 27-18 0-77 0-7 I V. t. 5 7-30 0-30 o-i Hyb. ii 8-54 0-55 81 19 B. t. 10 8-83 0-61 0-25 IO V. t. 5 8-78 0-31 o-i Hyb. ii 7-46 0-63 B. t. 10 8-66 0-66 o-i MW V. t. 5 8-72 0-55 o-i Hyb. ii 6-86 0-63 52 48 B. t. 10 5-90 0-51 o-i Dsp V. t. 5 23-94 2-35 0-4 Hyb. ii 26.34 1-52 44 56 B. t. 10 28-2 1-59 o-i Ab V. t. 5 1-35 1-06 o-i Hyb. ii i -80 0-28 B. t. 10 Pb V. t. 5 3-06 1-36 0-78 Hyb. ii 3-24 0-54 B. t. 10 For the characters H, I, MW and Dsp the mean for the hybrid lies between the means for the other two species. The % B refers to the percentage proximity of this mean to the mean for Barbus tropidolepis and the % V refers to the percentage proximity to the Varicorhinus tanganicae mean. The probability, P, refers to the probability of observing a mean equal to the Balon specimen value if the sample had come from one of the other two species. The morphometric measurements of the putative hybrids are satisfactorily intermediate for the characters MW and Dsp. However, the head length results are not as significant as they were for Barbus alluaudi (Banister, 1972). In that case the percentage likeness of the head length to each of the putative parents is i88 K. E. BANISTER 1-5 2-0 2-5 3-0 3-5 O5 1O 1-5 2-0 2-5 1-5 2-0 2-5 3-0 3-5 4-0 4-5 5-0 FIG. 14. Comparisons of the anterior (left) and posterior (right) barbel lengths in the three forms. Details as in Fig. 12. 25 26 27 28 29 30 5-0 5-5 6-0 6-5 26 27 80 8-5 FIG. 15. Comparisons of the dorsal spine length (left) and the mouth width (right) in the three forms. Details as in Fig. 12. 69 and 31% respectively. It can be seen from Table 2 that the head-length of the Balon fish is much closer to that of Barbus tropidolepis than to that of Varicorhinus tanganicae (% 6 = 91 ; % V = 9). One striking similarity between Barbus alluaudi and the Balon fishes can be seen in the interorbital width. In both cases, the hybrid interorbital width is less than that of the putative parents, the latter differing but little from each other in this character. Although generally it is true to say that African Barbus species have longer barbels than African Varicorhinus species, it is not true in this case. What little difference exists between the putative hybrids and Varicorhinus tanganicae shows that the hybrid has slightly longer barbels. The results of the morphometric characters analysed in Table i and the characters described in the earlier part of the text indicate that it is unlikely that the Balon specimens are extreme forms of either Barbus tropidolepis or Varicorhinus tanganicae. The degree of intermediacy hints most strongly at a hybrid origin. The evidence for the hybrid origin of the Balon fish is circumstantial and rests solely on the fact that in many characters these specimens are intermediate between Barbus tropidolepis and Varicorhinus tanganicae. This is the second example of hybridization between species of the genera Barbus and Varicorhinus in Africa. Such intergeneric hybridization raises doubts about the validity of the two genera. The mouth shape is the main character used to distinguish the two genera and yet this has been shown (Groenewald, 1958 ; Banister, 1973) to be a variable feature of little value at the generic level. Some Barbus species show extra-limital variation and achieve the Varicorhinus facies, or at least a close approximation to it. In AN INTERGENERIC CYPRINID HYBRID 189 all probability the true situation is that the genus Varicorhinus is polyphyletic and contains some species whose phyletic status may be best expressed by placing them in the genus Bar bus. A full revision of the genus Varicorhinus is needed to clarify these anomalies. This work is in progress. ACKNOWLEDGEMENTS My thanks go to Dr Eugene Balon for kindly allowing me to examine the specimens he collected. Dr P. H. Greenwood read the manuscript and offered much valuable advice. Mrs M. Clarke processed the statistical data under the guidance of Dr M. Hills. The uncredited drawings of whole fish are the work of Miss M. Holloway. The pharyngeal bones were drawn by G. Howes, who with the assistance of Mrs Clarke provided me with the radiographs. REFERENCES BANISTER, K. E. 1972. On the cyprinid fish Barbus alluaudi Pellegrini : a possible inter- generic hybrid from Africa. Bull. Br. Mus. nat. Hist. (Zool.) 24 (5) : 261-290. 1973- A revision of the large Barbus (Pisces, Cyprinidae) of East and Central Africa. Bull. Br. Mus. nat. Hist. (Zool.) 26 (i) : 1-148. BERRY, P. Y. & Low, M. P. 1970. Comparative studies on some aspects of the morphology and histology of Ctenopharyngodon idellus, Aristichthys nobilis and their hybrid (Cyprinidae). Copeia (4) : 708-727. BOULENGER, G. A. 1909. Catalogue of the freshwater fishes of Africa in the British Museum (Natural History) 1. London. 1911. Catalogue of the freshwater fishes of Africa in the British Museum (Natural History) 2. London. GAIGHER, I. G. 1975. The occurrence of 'Varicorhinus' and 'rubberlip' mouth forms in the small scaled yellowfish, Barbus polylepis. Piscator (92) : 162. GROENEWALD, A. A. v. J. 1958. A revision of the genera Barbus and Varicorhinus (Pisces, Cyprinidae) in Transvaal. Ann. Transv. Mus. 23 (3) : 263-330. HOLCIK, J. & DE WITT, J. J. D. ig62a. Character of Rhodeus ocellatus and Acheilognathus lanceolatus hybrids. Copeia (2) : 277-390. ig62b. The taxonomic characters of the hybrid Rhodeus. Copeia (4) : 777-778. HUBBS, CARL L. 1955. Hybridisation between fish species in nature. Syst. Zool. 4 (i) : 1-20. HUBBS, LAURA & JOHNSON, R. E. 1943. Hybridisation in nature between species of Catostomid fishes. Contr. Lab. vertebr. Biol. Univ. Mich. 22 : 1-76. MILLER, R. R. 1952. Hybridisation in nature between the fish genera Catostomus and Xyrauchen. Pap. Mich. Acad. Sci. 38 : 207-233. JUBB, R. A. 1968. The Barbus and Varicorhinus species (Pisces : Cyprinidae) of Transvaal. Ann. Transv. Mus. 26 (4) : 79-97. POLL, M. 1953. Lac Tanganika (poissons non Cichlidae). Result, scient. Explor. hydrobiol. lac Tanganika 3 (5 A) : 1-251. SCHULTZ, L. P. & SCHAEFFER, M. B. 1936. Descriptions of new intergeneric hybrids between certain cyprinid fishes of the northwestern United States. Proc. biol. Soc. Wash. 49 : i-io. WORTHINGTON, E. B. & RiCARDO, C. K. 1937- The fish of Lake Tanganyika (other than Cichlidae). Proc. zool. Soc. Lond. (4) : 1061-1112. DR K. E. BANISTER Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 5BD PLATE i A hybrid (top) of 133 mm SL, Varicorhinus tanganicae (centre) and Barbus tropidolepis (bottom). A LIST OF SUPPLEMENTS TO THE ZOOLOGICAL SERIES OF THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) 1. KAY, E. ALISON. Marine Molluscs in the Cuming Collection British Museum (Natural History) described by William Harper Pease. Pp. 96 ; 14 Plates. 1965. (Out of Print.) 2. WHITEHEAD, P. J. P. The Clupeoid Fishes described by Lacepede, Cuvier and Valenciennes. Pp. 180 ; n Plates, 15 Text-figures. 1967. £4.80. 3. TAYLOR, J. D., KENNEDY, W. J. & HALL, A. The Shell Structure and Mineralogy of the Bivalvia. Introduction. Nuculacea-Trigonacea. Pp. 125 ; 29 Plates, 77 Text-figures. 1969. £5.40. 4. HAYNES, J. R. Cardigan Bay Recent Foraminifera (Cruises of the R.V. Antur) 1962-1964. Pp. 245 ; 33 Plates, 47 Text-figures. 1973. £11.90. 5. WHITEHEAD, P. J. P. The Clupeoid Fishes of the Guianas. Pp. 227 ; 72 Text-figures. 1973. £10.65. 6. GREENWOOD, P. H. The Cichlid Fishes of Lake Victoria, East Africa : the Biology and Evolution of a Species Flock. Pp. 134 ; i Plate, 77 Text-figures. 1974. £3.75. Hardback edition £6.00. Printed in Great Britain by John Wright and Sons Ltd. at The Stonebridge Press, Bristol BS4 5NU Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 PLATE i PLATE 2 Ventral views of the head of Barbus tropidolepis (left), Varicorhinus tanganicae (centre) and a hybrid of 133 mm SL (right). Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 PLATE 2 TWO NEW SPECIES OF LARGE BARBUS (PISCES, CYPRINIDAE) FROM CENTRAL AFRICA By K. E. BANISTER SYNOPSIS Two new species of large Barbus from central Africa are described : Barbus huloti from the Lake Albert basin and Barbus humphri from the Ituri system. Barbus huloti is aligned with Barbus somereni and Barbus mirabilis but the affinities of Barbus humphri are uncertain. INTRODUCTION DURING a recent visit to the Institute Royale des Sciences Naturelles, Brussels, I found in the collections two series of specimens labelled Barbus altianalis from localities in which this species was unknown. Further examination showed that each series represented a new species. The series from the Vuda River (a feeder stream of Lake Albert) is particularly interesting because it represents only the second known species of large Barbus from that lake basin. Notes on counts and measurements The standard length (SL) was taken in the usual manner. The lateral line count (LL) was taken from the first pore-bearing scale behind the head to the scale lying lateral to the end of the hypurals. The body depth (D) is the maximum body depth, usually to be found just in front of the dorsal fin. The anterior limit for the head length (H) and snout length (Snt) was the premaxillary symphysis, with the pre- maxillae retracted. The posterior limit for the snout is the anterior margin of the orbit and for the head length is the most posterior part of the bony edge of the operculum. The term 'mouth width' (MW) refers to the width across the lower jaw at the level of the angle of the mouth. The pectoral fin length (Pet) is the total length of the fin, measured in a straight line from the base of the first fin ray to the distal extremity of the fin. The measurements were taken in this way because of the ease of so doing with dial calipers, which were used on all fish except the smallest, when dividers were used. The caudal peduncle length (CP1) is the horizontal distance from the posterior angle of the base of the last anal ray to the end of the hypurals and the caudal peduncle depth (CPd) is the least depth of that part. The interorbital width (IO) was measured as the least distance between the bony edges of the interorbital space. The eye diameter (I) is the horizontal diameter of the visible part of the eye. Dsp symbolizes the height of the dorsal fin from the base of the first spine to the distal extremity of the longest fin ray. With any measure- ments which were repeatable on both sides of the fish (e.g. the anterior barbel, Ab, Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 Issued 28 October 1976 ii 192 K. E. BANISTER or posterior barbel, Pb) the larger was taken except in cases where a deformity was obvious. The majority of measurements were taken to the nearest millimetre ; the exceptions were some measurements made on small fishes ; these were taken to the nearest half millimetre. The mean is symbolized by x, the standard deviation by s.d., the standard error by s.e. and the number of fish in the sample by n. DESCRIPTION OF SPECIES Barbus huloti sp. nov. HOLOTYPE. The holotype is a fish of 140 mm SL, no. 13289.558 in the collections of the Institute Royale des Sciences Naturelles, Brussels. Ten specimens ex no. 13288 are paratypes, as is BMNH. 1975.4. 30 :i. These fishes were collected by M. Hulot on 4 August 1953 at Zega on the Vuda River, Lake Albert ( = Lake Mobuto Sese Seko) basin, Zaire, i°44'N, 3O°45'E. DESCRIPTION. The description is based on 36 specimens, 68-282 mm SL. n X s.d. s.e. range SL - - - - 68 -282 mm D 35 28-1 1-8 o-3 25-0-33-7 H 36 27-5 i'3 0-2 22-6-29-4 I 36 6-4 0-8 O-I 4-2- 7-9 10 36 7-8 0-7 O-I 6-6- 9-6 MW 35 6-5 0-6 O-I 5-8- 8-2 Pet 36 22-5 1-4 0-2 19-5-26-1 CP1 36 16-9 i'3 0-2 13-3-19-1 CPd 36 n-9 0-6 O-I 10-8-13-5 Snt 36 8-6 0-9 O-I 6-3-10-0 Ab 36 6-1 1*4 0-2 3-1- 8-6 Pb 36 7'3 i-i O-2 4-8-10-2 Dsp 34 25-4 2-8 o-5 19-1-30-9 S-d 12 49-3 i'5 0-4 46-3-52-8 S-p 12 52-1 i'4 0-4 50-8-55-4 Unless stated otherwise all measurements are expressed as a percentage of the standard length. The body is compressed and shallow with the ventral profile gently convex from the gill isthmus to the anal fin base (Fig. i). The mouth (PI. i) is subterminal or ventral. The lower jaw is long with a curved buccal edge. Usually a thin mental lobe is present but in a few specimens this is greatly reduced, although the lip is always continuous. The skin of the lips, snout, base of the barbels and adjacent gular regions has a velvety texture caused by large numbers of minute papillae. Sections were cut of the papillae but the state of preservation of the tissues was inadequate for detailed histological examination. The larger specimens (above about 120 mm SL) have tubercle scars on the skin of the cheeks. In a few of the largest fishes two rows of tubercles are present on the anal fin and small scattered TWO NEW SPECIES OF BARBUS 193 2cm FIG. i. Barbus huloti, holotype, 140 mm SL. tubercles, or their scars, are present on the top of the head. The eyes are protuberant in most specimens but this may be a post-mortem effect of perhaps the result of the fishes having been collected by dynamiting. A few specimens (see PL i) have a few poorly developed rows of pit organs on their cheeks. The vertebrae in the twelve specimens radiographed number 18 + 21 (fi), 19 + 20 (13), 19 + 21 (14), 20 + 20 (13) or 20 + 21 (fi). This count includes the vertebrae incorporated in the Weberian mechanism. Dorsal fin. There are 4 unbranched rays and 8 (17) or 9 (129) branched rays. The last unbranched ray is thickened into a smooth, straight spine (£ = 25-4; s.d. = 2-8; s.e. = o-5 ; range 19-1-30-9). Most specimens have a sheath of scales covering the bases of the simple rays and the first five or six branched rays. The dorsal fin origin is in advance of the pelvic fin origin. The anal fin has 3 unbranched rays and 4 branched rays (136). Squamation. In the lateral line series there are 24 (12), 25 (14), 26 (17), 27 (fn), 28 (19) or 29 (13) scales. From the dorsal mid-line to the lateral line there are 4^ (f6) or 5^ (130) scales and from the lateral line to the mid-ventral line there are 4| (115), 5 (fi) or 5 1 (fn) scales. Between the lateral line and the base of the ventral fin there are 2 (fi), 2\ (122) or 3 (17) scales. Scale counts are not obtainable on all specimens. There are 12 (136) scales around the least circumference of the caudal peduncle. The scale striations are disposed radially on the anterior scales but are parallel or slightly convergent on the posterior scales (Fig. 2). Pharyngeal bones and teeth (Fig. 3). The pharyngeal teeth number 2.3.5-5.3.2 in all the 12 specimens examined. There is no significant change in the shape of the pharyngeal teeth with an increase in the size of the fish. The second tooth of the inner row is always mammiliform and never develops a molariform crown. The 194 K. E. BANISTER 2 mm FIG. 2. Barnus huloti, scale striations. Above, the third scale from the row above the lateral line ; below, the fifteenth scale from the same row. mean tip-to-tip length of the pharyngeal bones of a specimen of 164 mm SL is 17-0 mm and that of a specimen 216 mm SL is 23-5 mm. Gill-rakers. In 12 specimens examined there are 10 (fi), n (f2), 12 (f3) or 13 (f6) gill-rakers on the lower limb of the first gill-arch. The gill-rakers are slightly curved and obtusely pointed. TWO NEW SPECIES OF BARBUS 195 Coloration. Alcohol-preserved specimens are dark brown dorsally and paler on the flanks and belly. The centre of each scale is lighter than the edges. Diffuse dark pigment is present in the proximal part of the membrane of all fins. The lateral line is more conspicuous on the caudal peduncle where it is paler than the background. ETYMOLOGY. This species is named in honour of the collector, M. Hulot. DISTRIBUTION. This species is known only from pot-holes in the bed of the Vuda River, a feeder stream of Lake Albert, i°44'N, 30°45'E, Zaire. DIAGNOSIS AND AFFINITIES. The only other species of large Barbus recorded from the Lake Albert basin is Barbus bynni (Banister, 1973 : 27). This nilotic 5mm FIG. 3. Barbus huloti : left pharyngeal bone of the holotype. ig6 K. E. BANISTER species is, by its massive dorsal spine, deep body and parallel, sinuous striations on the scales, easily distinguished from Barbus huloti. Superficially, Barbus huloti resembles Barbus altianalis, subspecies of which are found in Lake Victoria (including Lake Kyoga), Lake Kivu and Lakes Edward and George and their feeder streams. Meristic and morphometric differences between the three subspecies are small (see Banister, 1973), but meristic and morphometric data for specimens of two of the three subspecies within the size range of the Barbus huloti sample are given in Tables i and 2. The main differences between Barbus TABLE i Comparisons of the mean and range of certain characters in Barbus altianalis and B. huloti B. a. radcliffii B. a. eduardianus B. huloti n = 18 n = 33 n = 36 X range x range X range SL (mm) 90-282 68-280 68-282 I 7-9 5-0-10-0 8-8 6-4-11-5 6-4 4-2- 7-9 Ab 5'3 3-6- 8-6 4-2 2-2- 6-4 6-2 3-1- 8-6 Pb 6-4 4'5- 9-6 5'7 3'9- 7'7 7'3 4-8-10-2 Dsp 19-9 13-6-30-4 18-9 13-2-25-0 25-4 19-1-30-9 TABLE 2 A comparison of the number of scales in the lateral line series in Barbus altianalis radcliffii (B. a. r.), B. a. eduardianus (B. a. e.) and B. huloti (B. h.) No. of scales 24 25 26 27 28 29 30 31 32 33 34 35 36 B. a. r. 1353 4 B. a. e. 362644 i B. h. 2 4 7 ii 9 3 altianalis and Barbus huloti are in scale number as well as in the eye, barbel length and length of dorsal spine. There are, in addition, some less quantifiable differences between Barbus huloti and Barbus altianalis. The latter species has never been observed to develop tubercles, nor to have papillae around the mouth. The scale striations of Barbus altianalis are more or less parallel and their direction does not vary with the position of the scale on the body. The pharyngeal bones and teeth of Barbus altianalis vary in shape and size (with the diet), a phenomenon not yet observed in Barbus huloti. An attempt to explain the absence of Barbus altianalis from Lake Albert was made by Banister (1973 : 22) and the arguments given there form an essential background to the current problem. The central part of this problem is to determine the likelihood of Barbus altianalis populations having moved from Lake Edward via the Semliki River into Lake Albert in the last 8000-10 ooo years. This date coincides with the cessation of the Katwe vulcanicity (Bishop, 1969), an event contemporaneous with the fish extinctions in Lake Edward (Greenwood, 1959 ', Kendall, 1969). Hitherto there has been no evidence of any faunal interchange via TWO NEW SPECIES OF BARBUS 197 the Semliki River since that time. This is rather puzzling, especially if the latter river is compared with the Ruzizi River. The Ruzizi River dates, in more or less its present form, from about 13 ooo B.P. (see evidence summarized in Banister, 1973) so that in each case the time scale is of the same order of magnitude. However, the slope of the two rivers is very different ; the Ruzizi drops approximately 590 m in 120 km whilst the Semliki only drops approximately 290 m in 220 km. Yet one fish, Barilius moori (see Poll, 1952), is known to have ascended the steeper Ruzizi River. Barbus altianalis altianalis has not descended the Ruzizi River into Lake Tanganyika although it has been reported from the Sange River, a tributary of the Ruzizi (Poll, 1952). A known ascent of the Ruzizi River would suggest that current speed alone is unlikely to be a barrier to migration along the gentler Semliki River. Fryer (1968) postulated that cold water flowing down the Ruwenzori mountains into the Semliki may form an effective barrier. However, Beadle (1974 : 139, 177, 181) points out that the main drop in the Semliki River bed is confined to a small distance and he thinks that it is these rapids and not the temperature that are the main barrier to the movement of fishes. Another factor to consider is the rate of evolution of Barbus altianalis. It is assumed that this species was originally confined to the headwaters of the River Zaire before tectonic movements resulted in the formation of the lakes (Banister, 1973). The three subspecies have diverged but little from each other since their initial isolation. The time of their separation and isolation is in the region of 100 ooo B.P. (the date of the Bufumbiro volcanoes - see Banister, 1973). Within the three subspecies there is no evidence of a potential for tachytelic evolution such that a population with Barbus altianalis characters would manifest Barbus huloti characters within 10 ooo years. There is no morphological nor palaeozoogeo- graphical evidence that indicates a sufficiently close relationship between Barbus altianalis and Barbus huloti to justify the inclusion of these species within the same supraspecific complex. Barbus somereni Boulenger, 1911 and Barbus mirabilis Pappenheim & Boulenger, 1914 live in the streams of, respectively, the Ruwenzori mountains and the Ituri system. They both have scales on which the striation pattern differs with the position of the scale on the body. Barbus huloti displays the same phenomenon. There are certain characters present in Barbus huloti that are not found in the other two species ; these include papillae around the mouth, a long dorsal spine, a slender body and tubercles on the cheeks. Barbus somereni and Barbus mirabilis both have bulky bodies and a higher modal number of branched rays in the dorsal fin (9 or 10 compared with 8 or 9). The presence of variable scale striation patterns in the three species is regarded as a synapomorphic character indicating that Barbus huloti is more closely related to Barbus somereni and Barbus mirabilis than to Barbus altianalis. This character is interpreted as synapomorphic because (a) it is of infrequent occurrence and (b) it is theoretically derivable from the commoner condition of sinuous, parallel striations. Geographically, there is nothing inconsistent in such a relationship. Barbus somereni lives in fast-flowing streams up to altitudes of 1750 m (Greenwood, 1966). I98 K. E. BANISTER Barbus mirabilis comes from the Ituri River to the west of the rift valley. Barbus huloti is found in a fast-flowing feeder stream of Lake Albert on the floor of the rift valley. It was supposed (Banister, 1973) that Barbus somereni and Barbus mirabilis are the descendants of a once homogeneous population found in the upper reaches of the formerly more extensive Zaire system. Barbus huloti could, therefore, represent a segment of this population that became isolated on the floor of the rift valley. The fishes of the Ituri system are poorly known (see below). The Ituri catchment is largely separated from the Lake Albert catchment area by the scarp wall of the rift valley. Only at the south-west part of the lake and towards the Semliki River is the scarp less severe. There the feeder streams of Lake Albert extend westwards and the relatively low watershed offers the possibility that at some time in the past there may have been movement of fishes between Lake Albert and the Ituri system. Barbus somereni has not, to date, been recorded from Ruwenzori streams flowing into the Semliki River. On the available information I align Barbus huloti with Barbus somereni and Barbus mirabilis. Whether each species represents an isolated population of a widespread ancestral species or whether Barbus huloti is an evolved isolated population of one of the other two species cannot, at the moment, be determined. Barbus humphri sp. nov. HOLOTYPE. The holotype (Fig. 4) is a fish of 145 mm SL, no. 13289.559 in the collections of the Institute Royale des Sciences Naturelles, Brussels. Ten specimens ex no. 13289 are paratypes, as is BMNH. 1975. 4.30:2. These specimens were collected with some 500 others in the River Tabie, North Kivu district, Zaire, about 25 km south of Beni. DESCRIPTION. The description is based on 12 specimens of 82-214 mm SL. X SL D 25-8 H 27-2 I 5-4 IO 7-8 MW 6-6 Pet 19-4 CP1 16-2 CPd 10-8 Snt 8-7 Ab 6-9 Pb 7-8 Dsp 22-9 S-d 46-8 S-p 51-1 Unless stated otherwise all measurements are expressed as a percentage of the standard length. The body is shallow, thick and terete. Almost all the specimens have a conspicuous coating of mucus. The snout is blunt with, in larger fishes, a few very s.d. s.e. range - - 82 -214 mm 1-8 °'5 24-0-30-3 i*5 0-4 24-9-30-3 0-8 O-2 4'2- 7'3 0-6 O-2 6-9- 9-0 0-7 O-2 5-9- 7-8 1-3 0-4 17-3-22-1 i'3 0-4 13-4-18-2 0-4 o-i 9-7-11-3 0-5 o-i 7'9- 9-5 1-3 0-4 4-7- 8-8 0-9 0-3 6-1- 9-2 1-8 0-9 15-9-28-0 1-8 °'5 44-9-50-7 1-8 °'5 48-3-54-0 TWO NEW SPECIES OF BARBUS 199 2cm FIG. 4. Barbus humphri, holotype, 145 mm SL. small tubercles on its lateral faces. The horseshoe-shaped mouth is subterminal and has an uninterrupted lower lip. A small mental lobe is occasionally present. The vertebrae in 12 specimens radiographed number 18 + 21 (fi), 19 +19 (£2), 19 + 20 (12), 19 + 21 (12), 20 + 19 (£2), 21 + 18 (12) or 21 + 19 (i). Dorsal fin. There are 4 simple rays (fi2), the last of these a stout, rather blunt spine, sometimes shorter than the longest branched rays. A raised sheath of scales is always present at the base of the simple rays, and in a few specimens it extends posteriorly to about the mid-point of the fin. There are 9 (fi2) branched rays. The dorsal fin is in front of the pelvic fin origin. Squamation. In the lateral line series there are 22 (f4), 23 (13), 24 (f4) or 25 (fi) scales. There are 4! (fi2) scale rows between the dorsal mid-line and the lateral line. Between the lateral line and the ventral mid-line there are 4^ (fi2) scale rows. From the lateral line to the base of the pelvic fin there are 2,\ (fi2) scale rows. There are 12 (fi2) scales around the least circumference of the caudal peduncle. The scales bear parallel striations (Fig. 5). Pharyngeal bones and teeth. The pharyngeal teeth number 2.3.5-5.3.2 in the 12 specimens examined. The first tooth (Fig. 6) of the inner row is small and com- pressed, i.e. longer than wide (length taken in the plane of the anterior edentulous process, width horizontally at 90° to that plane). The second tooth is also compressed, little enlarged and with a mamilliform crown. The third, fourth and fifth teeth approach a circular cross-section and become progressively more recurvUL The teeth of the second and third rows resemble the posterior teeth of the inner row. The mean tip-to-tip measurement of the pharyngeal bones of a fish of 165 mm SL is 12-8 mm and that of a specimen of 214 mm SL is 19-2 mm. Gill-rakers. In the 12 specimens examined there are 10 (13), n (f8) or 12 (fi) gill-rakers on the lower limb of the first gill-arch. The gill-rakers are scimitar shaped with small conical processes on the leading edge. K. E. BANISTER 2mm FIG. 5. Barbus humphri : fifth scale from the row above the lateral line of a specimen of 145 mm SL. Coloration. Alcohol-preserved specimens are dark brown above, paler beneath. The scales on the flanks are dark edged. Traces of dark pigment remain on the pelvic, pectoral and anal fins. ETYMOLOGY. This species is named in honour of Dr P. Humphry Greenwood for his services to African ichthyology. DISTRIBUTION. This species is known only from the type locality, the River Tabie about 25 km south of Beni, North Kivu district, Zaire. FIG. 6. Barbus humphri : left pharyngeal bone. TWO NEW SPECIES OF BARBUS 201 DIAGNOSIS AND AFFINITIES. The large Barbus species of the head waters of the Zaire system are poorly known, especially in the Ituri region. Only four species, Barbus fasolt Pappenheim, Barbus mawambi Pappenheim, Barbus mirabilis Pappenheim & Boulenger, and Barbus mawambiensis Steindachner, are recorded from the Ituri region. Barbus paucisquamatus Pellegrin and Barbus longifilis Pellegrin are known from rivers in the Lowa system to the west of Lake Kivu (and to the south of the Ituri system). The outstanding feature of Barbus humphri is the low number of lateral line scales. Barbus fasolt can also be easily distinguished from Barbus humphri because it has a flexible last simple ray in the dorsal fin. Barbus mawambi has more scales in the lateral line series (29 fide Pappenheim & Boulenger, 1914 ; cf. 22-25 m B- humphri) and 10 branched rays in the dorsal fin (cf. 9). Barbus mirabilis is a bulky-bodied fish with 28 scales in the lateral line series and a variable pattern of striations on the scales (see p. 197). Barbus mawambiensis, the only other species recorded from the Ituri system, presents a problem. This species was described as Barbus hindii var. mawambiensis by Steindachner (1911) on the basis of seven, now untraceable, specimens. His description, as well as his determination of this form as a variety of Barbus hindii, draws attention to the superficial resemblance between these specimens and Barbus hindii ( = Barbus oxyrhynchus) from the Athi-Tana system in East Africa. The differences given by Steindachner between Barbus hindii var. mawambiensis and Barbus hindii are a deeper caudal peduncle in the former (Cpl/Cpd 1-0-1-9 '> c^- 1-5-1-67) and more (sic) scales in the lateral line (21-24) than in Barbus hindii. (Boulenger, 1902, gives 25-29 scales in Barbus hindii.) This is perplexing informa- tion, since the range of the Cpl/Cpd ratios for the four syntypes of Barbus hindii was quoted by Boulenger (1902) as i^-if, while my own measurements give a mean of 1-38. The mean Cpl/Cpd ratio for all the Barbus oxrhynchus specimens used in an earlier study (n = io8) was 1-32 (Banister, 1973). The syntypes of Barbus hindii have 25 (f2) or 26 (f2) scales in the lateral line series ; the range for Barbus oxyrhynchus is 21-28 scales : 21 (fi), 22 (fio), 23 (fi5), 24 (£36), 25 (130), 26 (f8), 27 (f6) or 28 (fi). Unfortunately, the types of Barbus hindii var. mawambiensis are untraceable, which prevents the corroboration of Steindachner 's data. The specimens were deposited in the Vienna Museum, but a recent search by the curator, Dr Kahsbauer, and myself failed to find them. In 1912 Steindachner redescribed Barbus hindii var. mawambiensis as Barbus mawanbiensis based on a sample of fish from the Ja River, Cameroon. The spelling (mawanbiensis) for the specific name must be regarded as a misprint for mawambiensis There are inconsistencies between his 1911 and 1912 accounts, e.g. in 1912 he states that there are fewer scales in the lateral line series of Barbus mawambiensis than in Barbus hindii - the reverse, but correct, interpretation of the 1911 information. It is, of course, possible that Steindachner muddled scale size with scale number. He does not give the size, nor the number of the specimens examined, merely their locality - the Ja River, Cameroon. In 1914 Steindachner published another paper on a collection of fishes from the Ja River. Included in this is a further description of Barbus mawambiensis based 202 K. E. BANISTER on (in translation) 'three small examples from the Ja River, via Dr Haberer and from the Ituri via Herr Grauer'. The confusion is further increased by the statement that the largest of the three fishes is illustrated, although the scale on the figure shows that the smallest of the three fish is figured. (Boulenger, 1916, rightly pointed out that on Steindachner's pi. 3, figs i and 3 have been transposed.) Tables of measurements for each of the three specimens are given but which specimen or specimens was or were from the Ja River, and which from the Ituri, is not stated. The Ja and Ituri rivers are both in the Zaire system and are tributaries of respectively the Sangha and Aruwimi rivers which flow into the north side of the Zaire some 1000 km apart. Generally, the large Barbus spp. are found in the upper reaches of the tributaries, not in the main stream (pers. obs.). The two localities are some 1600 km distant and are separated by a wide sluggish river with few favourable habitats for large Barbus spp. Trewavas (1974 : 344) comments that the fauna of the Ja River has much in common with the rivers of Cameroon (therefore not with the Zaire system) and is also of the opinion that Steindachner's Barbus mawambiensis from the Ja resemble Barbus batesii. Although it is not known which of Steindachner's specimens came from which locality (see above), I agree with Trewavas that the Barbus spp. from the Ja are more likely to be related to those of west Africa (e.g. Barbus batesii} than to those of central Africa. Thys van den Audenaerde (1966 : 90) compared the fauna of the upper Ja (above Molundu) with that of the Nyong River and from the faunistic and geographical evidence concluded that the upper part of the Ja had been captured by the Sangha from the upper part of the Nyong. He describes the fauna below Molundu as typically central Congolese ( = Zairoise) . The only information given by Steindachner is that his specimens came from the Molundu district. It would seem that the presence of the same species of large Barbus in the Ituri and Ja rivers is most unlikely and would present some zoogeographical enigmas. The concept of Barbus mawambiensis as based on the points of agreement in Steindachner's three descriptions seems to indicate that there is a species of fish in the Ituri River which superficially resembles Barbus hindii but has a low number of lateral line scales. There are two specimens in the collections of the British Museum, nos. 1944.12.4:2-3 collected by Ricardo and Owen in the Epulu River (Ituri system) which have these characters and have been identified as Barbus mawambiensis. If this determination is correct then they can be distinguished from Barbus humphri by a stronger dorsal spine and a much deeper, more compressed body. These two fish also closely resemble Steindachner's figured specimen. However, the identification of these two fishes must remain tentative until the syntypes of Barbus mawambiensis are found. At the moment I can find no close relatives to Barbus humphri ; further collections from the Ituri may help to settle its relationships. ACKNOWLEDGEMENTS I am most grateful to M. J. P. Gosse of the Institute Royale des Sciences Naturelles in Brussels for drawing my attention to these fishes and for giving me the opportunity TWO NEW SPECIES OF BARBUS 203 to examine them. Valuable comments on the manuscript were provided by Drs P. H. Greenwood and P. J. P. Whitehead. Mrs M. Clarke assisted most efficiently with the calculations. The drawings are the work of Miss M. Holloway and Mr G. Howes. REFERENCES BANISTER, K. E. 1973. A revision of the large Barbus (Pisces, Cyprinidae) of East and Central Africa. Studies on African Cyprinidae II. Bull. Br. Mus. nat. Hist. (Zool) 26 (i): 1-148. BEADLE, L. C. 1974. The inland waters of tropical Africa. London. BISHOP, W. W. 1969. Pleistocene stratigraphy in Uganda. Mem. geol. Surv. Uganda 10: 1-128. BOULENGER, G. A. 1902. On the fishes collected by Mr. S. L. Hinde in the Kenya district, East Africa with descriptions of four new species. Proc. zool. Soc. Lond. : 221-224. 1916. Catalogite of the freshwater fishes of Africa in the British Museum (Natural History) 4. London. FRYER, G. 1968. The parasitic Crustacea of African freshwater fishes : their biology and evolution. /. Zool. Lond. 156 : 45-95. GREENWOOD, P. H. 1959. Quaternary fish fossils. Explor. Pare natn. Albert Miss. J. de Heinzlin de Braucourt 4 (i) : 1-80. 1966. The fishes of Uganda, 2nd edn. Kampala, the Uganda Society. KENDALL, R. L. 1969. An ecological history of the Lake Victoria basin. Ecol. Monogr. 39 (2) : 121-176. PAPPENHEIM, P. & BOULENGER, A. G. 1914. Fische. Wiss. Ergebn. dt. ZentAfr. Exped. Zool. (5), Zoologie 3 : 225-260. POLL, M. 1952. Poissons de rivieres de la region des lacs Tanganika et Kivu recueillis par G. Marlier. Rev. Zool. Bot. afr. 46 (3-4) : 221-236. STEINDACHNER, F. 1911. . . . iiber einige neue und seltene afrikanische siisswasser Fische. Anz. Akad. Wiss. Wien 48 : 531-535. 1912. Zur Fischfauna des Dscha, eines sekundaren Nebenflusses des Congo im Bezirke Molundu des siidlichen Kamerun. Anz. Akad. Wiss. Wien 49 : 443-449. 1914. Zur Fischfauna des Dscha, eines sekundaren Nebenflusses des Congo im Bezirke Molundu Kamerun. Denkschr. Akad. Wiss. Wien 89 : 1-64. THYS VAN DEN AUDENAERDE D. F. E. 1966. Les Tilapia (Pisces, Cichlidae) du Sud-Cameroun et du Gabon, etude systematique. Ann. Mus. r. Afr. entr. 8° Zool. 153 : 1-95. TREWAVAS, E. 1974. The freshwater fishes of rivers Mungo and Meme and lakes Kotto, Mboandong and Soden, West Cameroon. Bull. Br. Mus. nat. Hist. (Zool.) 26 (5) : 331-419. DR K. E. BANISTER Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 PLATE i Barbus huloti : ventral view of the head of a specimen of 214 mm SL to show the mouth, the papillae and the pit lines on the cheeks. Bull. Br. Mus. nat. Hist. (Zool.) 30, 5 PLATE i GENERAL 2 6 NOV i97( MISCELLANEA BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 6 LONDON: 1976 MISCELLANEA Pp 205-268 ; 9 Plates ; 19 Text-figures BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 6 LONDON: 1976 THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be completed within one calender year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30 No. 6 of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation : Bull. Br. Mus. nat. Hist. (Zool.) ISSN 0007-1498 Trustees of the British Museum (Natural History), 1976 BRITISH MUSEUM (NATURAL HISTORY) Issued 25 November, 1976 Price £6-75 CONTENTS Page A new genus and two new species of copepod parasitic on freshwater fishes. By G. A. BOXSHALL .......... 209 A new species of Chonopeltis (Crustacea : Branchiura) from southern Africa. By G. A. BOXSHALL .......... 217 Microlaophonte trisetosa sp. nov., a new harpacticoid copepod from southern Florida. By G. A. BOXSHALL ........ 223 A new species of Amphithoe (Pleonexes) (Amphipoda : Amphithoidae) from the north-east Atlantic with a redescription of A. (P.) gammaroides (Bate). By R. J. LINCOLN 229 The first zoeal stage of Scopimera crabricauda Alcock (Crustacea, Brachyura, Ocypodidae). By A. L. RICE ........ 243 Asterozoa from Amsterdam and St Paul Islands, southern Indian Ocean. By AILSA M. CLARK .......... 247 Restriction of the family Poraniidae, sensu Spencer & Wright, 1966 (Echinodermata : Asteroidea). By F. H. C. HOTCHKISS & AILSA M. CLARK 263 A NEW GENUS AND TWO NEW SPECIES OF COPEPOD PARASITIC ON FRESHWATER FISHES By G. A. BOXSHALL INTRODUCTION THE distribution of known species of lernaeid parasites of freshwater fishes in the Old World is notably patchy, with the majority of species known either from Africa or from eastern Asia. Between these two foci, in the region extending from India to the Mediterranean Sea, relatively few species have been recorded. It is probable that this paucity merely reflects the lack of fieldwork in this region ; thus the discovery of two new species, one from Iraq and the other from India, belonging to a new genus of lernaeid comes as no surprise. DESCRIPTION OF NEW GENUS AND SPECIES PSEUDOLAMPROGLENA gen. nov. DIAGNOSIS. Lernaeidae. First pedigerous somite partially incorporated into cephalothorax. Second to fourth pedigerous somites distinct, each subdivided into anterior and posterior portions by a transverse groove. Genital complex comprising fused fifth pedigerous somite and genital somite. Genital apertures on dorsal surface of genital complex. Maxilla 2-segmented, inflated distal segment bearing single claw medially. Maxilliped small, flattened and lying in groove posterior and lateral to maxilla; 3-segmented with terminal segment bearing weak setiform spine (s) medially. Maxilliped bases connected by fleshy ridge. Thoracic legs 1-4 biramous, with 3-segmented exopod and 2-segmented endopod. Leg 5 a simple lobe with 2 apical setae. Parasitic on gills of freshwater teleosts. Male unknown. Type species P. annulata sp. nov. Pseudolamproglena annulata sp. nov. (Figs la-g, 2a-e) DIAGNOSIS, Body cylindrical and distinctly segmented (Fig. la, b). Cephalo- thorax broad, dorsal surface concave in holotype, comprising 20-25% °f total body length. Anterior portion of first pedigerous somite incorporated into cephalothorax ; posterior portion free, rounded dorsally and narrower than both cephalothorax and second pedigerous somite. Second to fourth pedigerous somites separated by intersegmental sutures and subdivided into anterior and posterior portions by a transverse groove. Thoracic legs located anterior to groove. Thoracic somites increasing in size posteriorly. Genital complex small, narrower than fourth Bull. Br. Mus. nat. Hist. (Zool.1 30, 6 Issued 25 November 1976 G. A. BOXSHALL O2mm g FIG. I. Pseudolamproglena annulata sp. nov. female : (a) dorsal entire ; (b) lateral entire ; (c) cephalothorax, postero-ventral ; (d) antennule, ventral ; (e) oral region, ventral ; (f) maxilla, lateral ; (g) maxilla, ventral. Bar scale : a, b, 0-5 mm ; c, 0-2 mm ; e, o-i mm ; d, f, g, 50 (j.m. COPEPOD PARASITES OF FRESHWATER FISHES 211 pedigerous somite and with genital apertures situated dorso-laterally. Abdomen elongate, consisting of 2 indistinctly divided somites. Posterior margin of anal somite bilobed bearing medially directed furcal rami. Total body length from i '74 to 2-20 mm, with a mean of 1-97 mm (based on 2 specimens). Egg strings uniseriate, containing up to 14 eggs. Eggs maturing in oviduct visible through body wall of second to fourth pedigerous somites. Antennule (Fig. id) situated on ventral surface near anterior margin of cephalo- thorax, directed postero-laterally. Segmentation obscure with only the apical segment clearly delimited. Armature comprising 14 setae on anterior margin of proximal segment, 4 setae on distal segment and 2 aesthetasc-like structures, one on each segment. Antenna apparently absent. Oral region occupied by large trilobed structure (Fig. le), probably representing the labrum, anterior to which lies a transverse ridge. Maxillule absent. Maxilla (Fig. if, g) 2-segmented, proximal segment providing a broad base for swollen, gobular distal segment. Entire surface of distal segment ornamented with minute tubercles. Single, dorsally curved spine present on medial surface of segment. Maxilliped inconspicuous, dorso-ventrally flattened and lying in a groove in cephalo- thorax (Fig. ic, 2a). Indistinctly 3-segmented with a broad base, elongated middle segment and subquadrate terminal segment ; single setiform spine located on medial surface. Maxilliped bases connected by ridge of tissue. Thoracic legs 1-4 (Fig. 2b, c) similar, biramous. Sympod projecting from body surface, bearing single seta lateral to exopod base. Endopod indistinctly 2-segmented, exopod 3-segmented. Leg i armature comprising 2 unequal setae at tip endopod, 2 at tip exopod and i lateral spine on basal segment of exopod. Legs 2-4 unarmed apart from i lateral spine on basal segment of exopod. Leg 5 (Fig. 2e) a simple process with 2 apical setae. Furcal ramus bearing 4 setae (Fig. 2d) ; i on lateral margin, i on medial margin and i at each posterior corner. Two small papillae present on distal margin. ETYMOLOGY. The generic name proposed indicates a close affinity to the genus Lamproglena Nordmann. The specific name alludes to the very distinct segmen- tation in this species. MATERIAL EXAMINED. Type material 2 ovigerous $$. Holotype $ reg. no. 1975.800 ; paratype reg. no. 1975.801 deposited in the collections of the British Museum (Natural History). The material was obtained from the gills of Cyprinion macrostomus (caught in the river Tigris at Mosul, Iraq) present in the British Museum (Natural History) collections. Additional material : 5 ??, all either damaged or incomplete, collected by Mr Z. I. Fattohy from the gills of C. macrostomus from the same locality. Three of these specimens donated to the British Museum (Natural History) by Mr Fattohy and Dr M. H. Kasim (Mosul University). Pseudolamproglena simplex sp. nov. (Figs 2f-i, 3a-d) DIAGNOSIS. Body segmentation and tagmosis as in P. annulata but less distinct and without intersegmental sutures between the pedigerous somites (Fig. 2f, g). G. A. BOXSHALL 50pm 0-5mm FIG. 2. Pseudolamproglena anmilata sp. nov. female : (a) maxilliped, ventral ; (b) leg i, ventral ; (c) leg 4, ventral ; (d) furcal ramus, ventral ; (e) genital complex, ventral. Pseudolamproglena simplex sp. nov. female : (f ) dorsal entire ; (g) lateral entire ; (h) antennule, ventral ; (i) antenna, lateral. Bar scale : a-d, h, i, 50 [xm ; e, 0-2 mm ; f, g, 0-5 mm. COPEPOD PARASITES OF FRESHWATER FISHES 213 50>inn FIG. 3. Pseudolamproglena simplex sp. nov. female : (a) cephalothorax, ventral ; (b) maxilla, ventral ; (c) maxilliped, ventral ; (d) furcal ramus, ventral. Bar scale : a, 0-2 mm ; b-d, 50 (im. Cephalothorax comprising about 20% of total body length. Cephalothorax with prominent anterior ridge visible from the dorsal aspect. Second to fourth pedigerous somites similar in width. Genital complex of holotype (a gravid female) with conspicuous dorsal swellings marking the genital apertures. Total body length from 1-93 to 2-45 mm, with a mean of 2-25 mm (based on 5 specimens). Only i specimen ovigerous, egg string containing 20 eggs. Mature eggs in oviduct visible in second to fourth pedigerous somites. Position of all cephalic appendages illustrated in Fig. 3a. Antennule 2-segmented (Fig. 2h) ; large basal segment bearing 10 setae on anterior margin and i on posterior margin, apical segment armed with 8 setae and an aesthetasc-like structure. Antenna (Fig. 21) curved posteriorly, indistinctly 2-segmented and carrying an apical armature of about 5 setae. 2i4 G- A- BOXSHALL Oral region occupied by simple hemispherical lobe, probably representing the labrum (Fig. 3a). Transverse ridge present on ventral surface anterior to labrum. Maxillule (Fig. 3a) an unarmed fleshy process situated lateral to labrum. Maxilla 2-segmented with broad basal segment and massive, inflated distal segment. Distal segment (Fig. 3b) marked by transverse constriction and armed with single curved spine on medial surface. Maxilliped indistinctly 3-segmented (Fig. 3c). Basal segments of maxilliped pair connected by transverse ridge on ventral surface. Middle segment elongate, cylindrical. Terminal segment armed with 2 basal setae on postero-medial surface. Thoracic legs 1-4 similar to those of P. annulata both in segmentation and armature. Leg 5 positioned anteriorly on ventral surface of genital complex, comprising a simple process bearing 2 apical setae. Furcal rami (Fig. 31) armed with 6 marginal setae ; i lateral, i medial and 4 distal. ETYMOLOGY. The specific name refers to the simple, hemispherical structure of the lobe in the oral region. MATERIAL EXAMINED. 6$$ (i ovigerous). Holotype $ reg. no. 1975.803; 5 paratypes reg. nos 1975.804-808. deposited in the collections of the British Museum (Natural History). All specimens collected by Mr M. K. Jyoti from the gills of Labeo diplostomus caught in Dal Lake, Kashmir, India. HOST-PARASITE RELATIONSHIPS The two attached P. annulata observed were located on the anterior surface of the posterior hemibranch of gills 2 and 3. A single primary gill filament had been grasped between the maxillae and secured by the insertion of the spines. P. simplex attaches to the host in an identical manner but nearer to the distal tip of the gill filament than P. annulata. In both species the maxilla appears to be the only attachment organ and the massive development of this limb presumably compensates for the reduction of the maxilliped. The host tissue response to the presence of the parasite was negligible in P. simplex infections. Different degrees of epithelial hypertrophy were observed associated with the two specimens of P. annulata, with a localized, minor response in one case and, in the other, a massive response which resulted in the parasite being completely enclosed by host tissue to the level of the genital complex. It has been suggested (Sproston et al., 1950) that envelopment of the parasite provides additional security to the attachment of the parasite. REMARKS The new genus can be readily assigned to the subfamily Lamprogleninae of the family Lernaeidae. Of the two other genera in this subfamily, Lamproglena Nordmann and Lamproglenoides Fryer, the new genus is more closely allied to the former. Although the genus Lamproglena comprises a quite heterogeneous group of species the two new species could not be included within this genus without an unacceptable broadening of the generic diagnosis. The genus Pseudolamproglena is COPEPOD PARASITES OF FRESHWATER FISHES 215 erected to contain these two species which form a well-defined group distinguishable from species of Lamproglena by the structure and armature of the maxillae and maxillipeds and by their distinctive somitic segmentation. Fryer (1968) recognized several evolutionary trends within the Lernaeidae. Amongst these are the suppression of external signs of segmentation and tagmosis, the development of a 'neck', reduction of antennules and antennae and the reduction of the number of terminal spines on the maxilliped. Pseudolamproglena exhibits a mosaic of primitive and advanced characters with respect to these trends. It retains a primitive degree of external somitic segmentation and tagmosis combined with the specialized condition of the maxilla and maxilliped and, in P. annulata, with the apparent absence of the antenna. This combination of characters suggests that Pseudolamproglena diverged from the ancestral Lamproglena-like stock at an early date and that specialized adaptations of the mouthparts evolved independently. ACKNOWLEDGEMENTS I would like to thank Dr G. Fryer for his valuable comments on some of these specimens and Dr R. J. Lincoln for his criticism of the manuscript. I am grateful to Mr Z. Fattohy and Dr M. H. Kasim (Mosul University, Iraq) whose donation first brought P. annulata to my attention. REFERENCES FRYER, G. 1968. The parasitic Crustacea of African freshwater fishes ; their biology and distribution. /. Zool., Lond. 156 : 45-95. SPROSTON, N. G., YIN, W. Y. & Hu, Y. T. 1950. The genus Lamproglena (Copepoda para- sitica). The discovery of the life histories and males of two Chinese species from food fishes, revealing their relationship with Lernaea and of both to the Cyclopoidea. Sinensia, Shanghai (n.s.) 1 : 51-84. DR G. A. BOXSHALL Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON swy 560 A NEW SPECIES OF CHONOPELTIS (CRUSTACEA: BRANCHIURA) FROM SOUTHERN AFRICA By G. A. BOXSHALL INTRODUCTION THE genus Chonopeltis Thiele, 1901 is endemic to Africa and comprises seven known species. The southernmost record of this genus is that of C. meridionalis Fryer from the Limpopo river system in Rhodesia (Fryer, 1968). It was interesting, therefore, to discover some specimens of Chonopeltis in a collection of crustaceans parasitic on freshwater fishes of the Orange river system. The specimens represent a new species which is described below. DESCRIPTION OF NEW SPECIES Chonopeltis australis sp. nov. DIAGNOSIS. With characters of genus. Female body squat, with 2 longitudinal bands of pigment spots on thorax. Second maxilla with scale-covered prominence on proximal portion. Leg 3 less than twice as long as leg 4. Male lacking posterior projections on leg 2 sympod and lacking process on exopod of leg 4. DESCRIPTION. Adult female. General appearance squat (Figs la, 2a), large trifoliate carapace comprising about 54% of total body length. Lateral lobes of carapace extending posteriorly to cover the bases of leg 2 ; oval respiratory areas on ventral surface of each lateral lobe similar to other species of genus. Chitinous supporting rods present in anterior lobe of carapace. Eyes small ; ocellus small, distance between ocellus and eyes equal to interocular distance. Segmentation of thorax distinct. Two longitudinal bands of dark pigment spots present on thorax, dorsal to uteri. Abdomen comprising 20-24% of total body length. Furcal rami minute. Spermathecae short, extending to level of bifurcation of abdomen in some specimens. First antenna (Fig. 2e) slender, indistinctly 5-segmented ; apical segment bearing 3 spines. Mandible (Fig. 2b) curved, bearing 3-4 rows of denticles on convex surface and a row of spinules on concave margin. Suckers (first maxillae) as in other species of the genus. Second maxillae (Fig. 2d) with a 2-segmented proximal portion and 3-segmented distal portion ; scale-covered prominence present on posterior surface near apex of second segment opposing a small elevated region on third segment ; 2 small claws situated in depression at tip of terminal segment. Legs 1-4 biramous ; sympod and both rami armed with single rows of setae ; legs 1-3 similar in size, leg 4 about two-thirds as large as leg 3. Natatory lobes of leg 4 (Fig. 2c) extensive, meeting at ventral midline, with spinules present on posterior and medial margins. Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 Issued 25 November 1976 218 G. A. BOXSHALL FIG. i. Chonopeltis australis sp. nov. : (a) adult female, dorsal ; (b) adult male, dorsal. A NEW SPECIES OF CHONOPELTIS 219 0-1mm •2mm FIG. 2. Chonopeltis australis sp. nov. : (a) adult female, ventral ; (b) mandible, ventral ; (c) natatory lobes female, ventral ; (d) second maxilla female, ventral ; (e) first antenna female, ventral. G. A. BOXSHALL FIG. 3. Chonopeltis australis sp. nov. male : (a) leg 2 ; (b) leg 3 ; (c) leg 4. Body length 5-0-8-9 mm, with a mean of 6-8 mm (based on 8 specimens). Adult male. Carapace comprising about 57% and abdomen about 34% of total body length (Fig. ib). Anterior appendages as in female. Legs 2-4 showing sexual characters ; leg 2 without any projections on posterior margin of sympod (Fig. 3a) ; sympod of leg 3 (Fig. 3b) bearing an extensive marginal flap posteriorly ; leg 4 (Fig. 3c) with an antero-laterally directed conical process on sympod, exopod simple without any processes. A NEW SPECIES OF CHONOPELTIS 221 Body length 3-8-5-8 mm, with a mean of 4-5 mm (based on 8 specimens). MATERIAL EXAMINED. 9$$ (i damaged) and 8<$$ specimens. Holotype $ reg. no. 1975.1092 ; paratypes reg. nos 1975.1093-1108 ; deposited in the collections of the British Museum (Natural History). DISTRIBUTION. C. australis was collected from the body surface of Labeo capensis Smith and L. rosae Steindachner caught at two sites : near Vereeniging on the Vaal river and near Potchefstroom, in the Boskop Dam reservoir on the Mooi river. Both the Vaal and the Mooi are part of the Orange river system. REMARKS. The new species can readily be placed in a group of species, together with Chonopeltis brevis Fryer and C. meridionalis, which is characterized by the possession of two longitudinal bands of pigment spots on the thorax. Also in common with these species C. australis is found externally on the host. This is in keeping with the suggestion made by Fryer (1964) that the pigment bands serve to protect developing eggs in the uteri from intense illumination and are therefore found only in species of Chonopeltis which are external body surface parasites. The males of C. australis can be distinguished from those of C. brevis and C. meridionalis by the absence both of any posterior projections on the sympod of leg 2 and of any process on the exopod of leg 4. The females of these three species are very similar and trivial morphological characters must be used to distinguish between them. In C. brevis leg 3 is more than twice as long as leg 4 whereas in C. australis and C. meridionalis it is less than twice as long. The natatory lobes of leg 4 in C. meridionalis are rounded and less extensive laterally than in C. australis. In addition the scale-covered prominence on the proximal portion of the second maxilla of C. australis is a distinctive character. The structure of the second maxilla of C. australis suggests that it is able to function in a prehensile manner although it is not so obviously prehensile as in C. schoudeteni Brian and C.flaccifrons Fryer, both of which possess a large digitiform process on the proximal portion of the appendage. ACKNOWLEDGEMENTS I would like to thank Dr H. Schoonbee (Rand Afrikaans University, Johannesburg) for donating the material to the Museum and for providing data on the distribution of the species and Dr G. Fryer (Freshwater Biological Association) for reading and commenting upon the manuscript. REFERENCES FRYER, G. 1964. Further studies on the parasitic Crustacea of African freshwater fishes. Proc. zool. Soc. Lond. 143 : 79-102. 1968. The parasitic Crustacea of African freshwater fishes ; their biology and distri- bution. /. Zool., Lond. 156 : 45-95. DR G. A. BOXSHALL Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SWy 5BD 13 MICROLAOPHONTE TRISETOSA SP. NOV., A NEW HARPACTICOID COPEPOD FROM SOUTHERN FLORIDA By G. A. BOXSHALL INTRODUCTION THE copepod described below was isolated by Dr J. D. George (British Museum (Natural History)) from laboratory cultures of the polychaete Capitellides giardi Mesnil. Dr J. Fell and Mrs R. Hendrix (University of Miami) originally established the cultures by inoculating agar plates with decomposing mangrove leaves during investigations into the fungi and nematodes of the southern Florida red mangrove forest detrital system. The cultures have been successfully maintained since August 1972 and the culture technique, together with certain aspects of the biology of the new harpacticoid species, is described in detail by George (1976). The material upon which this study is based was provided by Dr George in July 1975. It was examined both by phase contrast microscopy and by scanning electron microscopy (SEM). Drawings were made with the aid of a camera lucida and from SEM photographs. DESCRIPTION OF NEW SPECIES Microlaophonte trisetosa sp. nov. TYPES. Holotype $ registration no. 1975.1255, allotype <$ registration no. 1975.1256, paratypes registration nos 1975.1257-1267 ; deposited in the collections of the British Museum (Natural History). Cultures established using material collected near Matheson Hammock, Miami, Florida, U.S.A. ADULT FEMALE. Body slender, cylindrical, with somites clearly denned (Fig. la-c). Cephalothorax about as long as 3 succeeding somites combined, with sensillae around its lateral and posterior margins. Rostrum short, with 2 sensillae. Each thoracic somite with a row of sensillae dorsally and laterally along the posterior margin. Genital double somite subdivided by a continuous dorsal and lateral chitinous strip armed with sensillae, posterior margin of double somite also provided with sensillae except on mid-ventral portion. Antepenultimate somite similarly provided with sensillae ; penultimate somite without sensillae but with a continuous ventro-lateral and ventral row of spinules. Anal somite with a sensilla on each side of the operculum and with a row of spinules ventrally and ventro-laterally around the bases of the caudal rami. Bull. BY. Mus. nat. Hist. (Zool.) 30, 6 Issued 25 November 1976 224 G. A. BOXSHALL FIG. i. Microlaophonte trisetosa sp. nov. : (a) female, dorsal ; (b) abdomen, ventral (c) abdomen, lateral ; (d) male, dorsal ; (e) abdomen, ventral ; (f ) abdomen, lateral. A NEW HARPACTICOID FROM FLORIDA 225 FIG. 2. Microlaophonte trisetosa sp. nov. : (a) female first antenna, dorsal ; (b) second antenna, ventral ; (c) mandible, posterior ; (d) first maxilla, posterior ; (e) second maxilla, posterior ; (f ) maxilliped, ventral ; (g) leg i, anterior ; (h) leg 2, anterior ; (i) leg 3, anterior ; (j) leg 4, anterior. 226 FIG. 3. Microlaophonte trisetosa sp. nov. : (a) female leg 5, anterior ; (b) caudal ramus, ventral ; (c) male leg 3, anterior ; (d) first antenna, dorsal ; (e) leg 5, ventral. Caudal rami (Fig. 3b) not markedly divergent, about 2 times longer than broad ; with a pointed process at the postero-lateral angle ; whole surface with densely scattered minute spinules. First antenna (Fig. 2a) 6-segmented, third segment longest, about 3 times longer than fourth which carries a long aesthetasc ; last segment longer than 2 preceding segments combined. Second antenna (Fig. 2b). Coxa unarmed ; allobasis with a plumose seta on outer margin ; exopod small bearing i lateral and 2 apical plumose setae. Endopod becoming flattened distally, with a dense covering of spinules and i distal spine on anterior margin, 4 strong spines and 2 geniculate setae on the distal margin and 2 spinule rows near apex on ventral surface. Mandible (Fig. 2c). Praecoxa provided with a bidentate pars incisiva and a strong spine terminally and a slender seta subterminally. Palp i-segmented with 1 apical and 3 lateral setae. First maxilla (Fig. 2d). Arthrite of praecoxa with a proximal row of slender spinules and, along the distal margin, i very robust spine with spinules, about 5 slender spines and a spinulate seta. Coxa with a proximal row of spinules and 2 terminal setae, i spinulate distally ; basis with 3 apical setae, i strong and distally spinulate ; endopod represented by 4 setae. Second maxilla (Fig. 2e). Syncoxa with 3 endites : proximal endite short with a single seta ; middle endite with 2 stout setae ; distal endite with 3 setae. A row of A NEW HARPACTICOID FROM FLORIDA 227 spinules and a patch of minute denticles also present at outer corner of syncoxa. Basis drawn out into a slightly curved claw accompanied by i anterior, i posterior and 2 dorsal setae ; endopod represented by 3 setae. Maxilliped (Fig. 21). Basis with a single seta ; endopod 2-segmented with apical segment forming a slender claw bearing a spinule basally. Leg i (Fig. 2g) . Coxa with spinule row along outer margin ; basis with proximal spinule row around a small anterior tubercle, a spinule row near base of endopod, another row near base of exopod and 2 setae, i located on outer margin proximal to the exopod and the other on the anterior surface near the inner margin. Exopod i-segmented, although in some specimens an incipient subdivision is apparent, with i proximal and 2 distal setae on the outer margin, i short and 2 long setae on the distal margin and a distal spinule row. Endopod well developed ; first segment long with spinules on proximal portion of inner margin, second segment with spinules on inner and outer edges ; third segment forming a curved claw. Legs 2-4 (Fig. 2h-j). Coxa unarmed ; basis with an outer seta and a single spinule row on ventral surface between bases of rami. Exopod 3-segmented ; first and second segments similar in length and longer than third ; rows of spinules present on all exopod segments. Endopod 2-segmented ; first segment larger, with minute spinules on lateral surface and longer hairs on inner surface ; second segment of leg 2 with a conspicuous proximal spinule ; endopod of leg 4 shorter, not reaching beyond end of second exopod segment. Spine and seta formula : EXOPOD ENDOPOD i 2 3 i 2 o I 212 o 2 2 O o I 222 o 3 2 I o I 222 o 221 Leg 2 Legs Leg 4 Spines and setae closely approximated and exact point of insertion on internal or distal margin sometimes difficult to discern. Leg 5 (Fig. 3a). Baseoendopod longer than exopod ; anterior surface with many rows of spinules ; outer margin with a single seta, inner margin with 2 proximal spinules, i seta at the base of the endopod portion and a spine and a long seta distally ; distal margin with i seta and 2 spines. Exopod with 4 spinules on anterior surface and with 6 setae around the outer and distal margins. Ovisac with 6-10 eggs. Body length of female ranging from 0-47 to 0-51 mm, with a mean of 0-49 mm. ADULT MALE. Body more slender and shorter than female (Fig. id-f). Ornamen- tation of abdominal somites similar to female but with additional ventral spinule rows located anterior to the sensillae on the ante- and penultimate somites. First antenna (Fig. 3d) 6-segmented, subchirocerate ; aesthetasc present on fourth segment. Legs 2 and 4 as in female but outer spines on exopod longer and more robust ; inner seta on second exopod segment usually absent from leg 4. Leg 3 (Fig. 3c) with 3-segmented endopod ; second segment with a mucroniform process at outer distal corner, third segment with 4 setae. 228 G. A. BOXSHALL Leg 5 (Fig. 3e). Baseoendopod with a spinule row on inner margin, a long seta on outer margin and some scattered spinules located anterior and lateral to base of exopod; exopod broader than long, with a row of spinules, i seta at outer distal corner and 3 distal setae. Leg 6. Each leg comprising a long outer seta and a short inner seta. Mean body length 0-40 mm, with a range of 0-38 to 0-43 mm. VARIATION. Ten specimens of each sex were dissected to examine possible variation in the armature of legs 2-4. No variation was found in the female. In the male the inner seta of exopod segment 2 was present on leg 2 in all 10 specimens, on leg 3 in 5 specimens and on leg 4 in only 2 specimens. No other variability was observed. REMARKS The new species is provisionally assigned to the genus Microlaophonte Vervoort, 1964 in the subfamily Laophontinae. There are marked differences between the new species and M. spongicola Vervoort, 1964, the type and only species of the genus, but these are not sufficient to justify the establishment of a new genus. However, M. spongicola is known only from the female (Vervoort, 1964) and the eventual discovery of the male may necessitate the removal of M. trisetosa from the genus if the male secondary sexual characters are found to differ significantly from those of M. trisetosa. The spine and seta formula of legs 2-4 is of diagnostic importance at the generic level in the Laophontidae. The formulae of M. spongicola and M. trisetosa differ primarily in the presence of an additional internal seta on the second endopod segment of legs 2 and 3 in the latter species. However, the absence of the small innermost seta on this segment in M. spongicola may only be apparent as Vervoort (1964) states that small setae may have been obscured by the hairs on the endopod. The two species can be readily separated by the presence in M. trisetosa of 3 setae on the exopod of the second antenna (the character alluded to in the specific name), of 6 setae on the exopod of leg 5 in the female and by the i-segmented nature of the exopod of leg I. ACKNOWLEDGEMENTS I am indebted to Dr George for providing the material for this study and to Dr R. J. Lincoln for his critical reading of the manuscript. REFERENCES GEORGE, J D. (1976) The mass culture of benthic polychaetes and harpacticoid copepods on agar. Proceedings of the tenth European Symposium on Marine Biology. VERVOORT, W. 1964. Free-living Copepoda from Ifaluk Atoll in the Caroline Islands. Bull. U.S. natn. Mus. no. 236 : 1-431. DR G. A. BOXSHALL Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SWy 5BD A NEW SPECIES OF AMPHITHOE (PLEONEXES) (AMPHIPODA: AMPHITHOIDAE) FROM THE NORTH-EAST ATLANTIC WITH A REDESCRIPTION OF A. (P.) GAMMAROIDES (BATE) By ROGER J. LINCOLN INTRODUCTION A SHORT review of the subgenus Pleonexes is given in a recent paper by Mateus & Afonso (1974) together with a table of comparative characters for the six recognized species. Pleonexes was only recently relegated from the familiar generic status to that of a subgenus by Barnard (1970) on the evidence of a gradation of characters between Amphithoe and Pleonexes. The subgenus is identified in the Atlantic by the marked expansion of the propodus of pereopods 5-7 and the pair of prominent hooked spines on the distal margin of the telson, although an examination of all Amphithoe species reveals a gradation of these characters which suggests that Pleonexes may not be a valid subgenus. Only three species of Amphithoe (Pleonexes) are recognized from the north-east Atlantic and Mediterranean, namely A. (P.) bicuspis (Heller) from the Adriatic, A. (P.) pomboi Mateus & Afonso from the Azores and A. (P.) gammaroides (Bate), which is the only widespread species recorded along the coast of Europe from southern Norway to the western Mediterranean and including the British Isles. After examining the amphipods in the British Museum (Natural History) as part of the preparation for a new handbook on the amphipod fauna of the British Isles, it is clear that there are in fact two quite distinct species of Pleonexes in collections from British localities. The two species differ considerably in body size and especially in the relative proportions and robust nature of the antennae, as well as other structural characters. Collections from more northerly areas, especially Shetland Isles and the west coast of Scotland, consist only of the larger of the two species which is the true gammaroides, while material from the south coast of England, southern and south- western Ireland belongs mostly to the new and smaller species which is described below as Amphithoe (Pleonexes) neglectus n. sp. The confusion over the identification of the two species can probably be explained by the fact that Sars (1894), in his excellent monograph on the amphipods of Norway, figured the female of the true gammaroides (actually a specimen from southern Norway originally ascribed to Sunamphithoe hamulus by Boeck but now recognized to be a synonym of gammaroides) , while his figures of the male are not of gammaroides but the new species, neglectus. Fortunately, Sars offers an explanation of this in his Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 Issued 25 November 1976 230 ROGER J. LINCOLN text (page 584) where he states that he had no male specimen of gammaroides from Norway and had illustrated material collected in France. Two other species should be referred to the synonymy of gammaroides, namely Sunamphithoe longicornis Boeck and Sunamphithoe hamulus Bate. An examination of the type 5. hamulus has shown it to be the female of gammaroides and not of Sunamphithoe conformata Bate as proposed by Stebbing (1906). DESCRIPTION OF SPECIES Amphithoe (Pleonexes) neglectus n. sp. (Figs la ; 2a-h ; sa-g ; 4a-g) Pleonexes gammaroides : Sars, 1894 : 5^2 (Part), pi- 207 (cj) ; Stebbing, 1906 : 642 (part). DIAGNOSIS. Length up to 5 mm ; antennae subequal, moderately setose, equal to half body length or less. Gnathopod I propodus elongate oval. Gnathopod 2 ischium without distinct lobe on anterior margin ; in male propodus broadly oval, tumid, palmar surface concave with distinct inner and outer palmar margin, delimited from posterior margin by rounded angle. Pereopod 5 basis very much expanded, broader than long. Telson with prominent marginal hooks and pair of mediolateral setae. DESCRIPTION. Length 4-5 mm, body rather slender, compressed, urosome segment I with pair of dorsal setules (Fig. la) ; colour in spirit whitish with scattered dark chromatophores on body, coxal plates, basal segments of pereopods and antennal peduncles. Coxal plates 1-5 moderately large, distal margins rounded with numerous small setules ; coxal plate i produced slightly forwards ; plate 2 with anterior margin very broadly rounded ; plate 4 entire, not excavate posteriorly ; plate 5 with small posterior lobe, and large anterior lobe about equal to length of plate 4. Epimeral plates 1-3 rounded ; plates 2-3 (Fig. 4c) with small setule inset in posterodistal margin. Head with lateral lobes broadly convex, only moderately produced ; eyes small and rounded, visual elements distinct. Antennae (Fig. 2a, b) relatively short and setose, equal or little less than half body length, of subequal length or with antenna i little longer than 2 ; accessory flagellum absent ; antenna i peduncle article i robust with 2-3 distoventral, and 1-2 small mid-ventral, spinules ; article 2 little shorter than i ; article 3 about half length of 2 ; flagellum about 15 to i8-articulate, each article with distinct elongate aesthetasc ; antenna 2 more robust than i especially in male, peduncle articles 4 and 5 subequal, or article 5 slightly longer than 4 ; flagellum moderately setose, shorter or equal to peduncle article 5, about Q-articulate with proximal articles often swollen (Fig. 2b). Upper lip entire, margin rounded, setulose. Mandible with distinct molar ; left mandible (Fig. 2f) with 5 spines in spine-row, right mandible (Fig. 2g) with 4 spines ; palp 3-articulate, article i short, article 2 with single large distal seta, article 3 with group of about 9 large terminal setae. Lower lip (Fig. 2c) with inner and outer lobes distinct, setulose. Maxilla i (Fig. 2d) inner plate very small with single small seta, outer plate with about 9 robust spines ; palp 2-articulate, article i very short, article 2 elongate and curved, reaching beyond apex of outer plate with 2-3 small NEW SPECIES OF AMPHITHOE 231 FIG. i. (a) Amphithoe (Pleonexes) neglectus n. sp. male, entire ; (b) Amphithoe (Pleonexes) gammaroides (Bate), male, entire. terminal spines. Maxilla 2 (Fig. 2e) inner plate with several long, inner-marginal, plumose setae ; inner margin also fringed with fine short setules ; outer plate longer than inner, outer and distal margins fringed with fine short setules, distal margin with several long setae. Maxilliped (Fig. 2h) inner plate short ; outer plate elongate oval with inner margin finely serrate, marginal spines increasing in length distally ; palp 4-articulate, setose. Gnathopod i (Figs 3a, 41) generally similar in male and female ; 232 ROGER J. LINCOLN a 0 -5mm FIG. 2. Amphithce (Pleonexes) neglectus n. sp. male ; (a) head and antennae ; (b) head and antennae, robust ; (c) lower lip ; (d) maxilla i ; (e) maxilla 2 ; (f ) left mandible ; (g) right mandible ; (h) maxilliped. NEW SPECIES OF AMPHITHOE 233 FIG. 3. Amphithoe (Pleonexes) neglectus n. sp. male ; (a) gnathopod i ; (b) gnathopod 2 (c) gnathopod 2, propodus ; (d) gnathopod 2, propodus, small male ; (e) pereopod 3 (f ) pereopod 4 ; (g) pereopod 5. 234 ROGER J. LINCOLN basis robust, narrow proximally with posterior margin rather angular, anterodistal angle with small rounded lobe ; merus with few distal setae ; carpus much shorter than propodus, anterior margin convex with large median spine and 1-2 large distal spines, posterior margin rounded with few long setae ; propodus elongate oval, palm convex and poorly defined from posterior margin, delimited by single large spine, distal margin of palm with single curved striated spine close to base of dactylus, posterior and palmar margins moderately setose ; dactylus little longer than palm, inner margin toothed. Gnathopod 2 female (Fig. 4g) little larger and more robust than i ; basis with large anterodistal lobe bearing 1-2 small spinules ; carpus with posterior lobe rather slender and produced ; propodus broadly oval, anterior margin with 4-5 small groups of setae, palm convex, oblique, delimited from posterior margin by obtuse angle and single large spine ; posterior and palmar margins strongly setose, palmar margin with single curved, striated, spine close to base of dactylus. Gnathopod 2 male (Fig. 3b) very much larger and more robust than in female ; basis with very large anterodistal lobe bearing 2-3 small spines ; carpus very short with slender posterior lobe, anterior margin with strong median and distal spines ; propodus very broad and robust, anterior margin strongly convex with several small groups of setae or spines, palm complex with concave surface between distinct inner and outer palmar margins (Fig. 3c), delimited by obtuse angle and single stout spine ; in smaller specimens the outer palmar margin may be indistinct (Fig. 3d) ; palm weakly setose with single striated spine close to base of dactylus. Pereopods 3-4 (Fig. 36, f) basis narrowly oval, anterior and posterior margins weakly setose ; merus broad distally ; carpus short ; propodus about equal to length of merus, tapering distally ; dactylus weakly curved and about half length of propodus ; merus, carpus and propodus with few long setae. Pereopod 5 (Fig. 3g) basis broader than long with very large posterior lobe, anterior margin with several short spines ; merus little longer than carpus ; propodus broad distally, palm with 3-4 short, and i long curved, striated spines ; inner and outer palmar surface with small group of long setae. Pereopod 6 (Fig. 4a) more elongate than 5 ; basis with moderately large posterior lobe which narrows distally to produce sinuous posterior margin ; merus, carpus and propodus similar to pereopod 5 only more elongate. Pereopod 7 (Fig. 4b) slightly longer than 6 ; basis narrowly oval with only small posterior lobe and convex posterior margin. Uropods (Fig. 4d) short and spinose. Uropod i peduncle with 3 distomarginal spines and many long outer-marginal setae, distoventral angle with short blunt process ; outer ramus with about 3 marginal spines and small group of terminal spines ; inner ramus equal to length of outer, with only small group of apical spines. Uropod 2 peduncle with 2 distomarginal spines ; outer ramus with 2 marginal spines ; inner ramus equal to length of outer, with only apical spines. Uropod 3 (Fig. 4e) peduncle robust with single distal spine ; outer ramus with pair of large curved spines and finely denticulate dorsal margin ; inner ramus with small apical spine and about 6 long setae. Telson fleshy, entire, with distinct distolateral hooks and pair of mediolateral setae. HOLOTYPE. Portsmouth, twice carapace length) than in S. globosus ( < twice carapace length). Second, these spines are completely naked in 5. crabricauda whereas Aikawa describes them as 'sparsely toothed' in 5. globosus. Finally, according to Aikawa's fig. 52, abdominal somites 3 and 4 in 5. globosus lack the small but clear posterio-lateral spines present in 5. crabricauda. The available descriptions of the larval stages of other members of the Scopimerinae (see Rice, 1975) are not sufficiently detailed to enable generic characters within the sub-family to be discussed. Nevertheless, it seems that the zoeae of the three genera Scopimera, Ilyoplax and Dotilla may be distinguished between by the lengths of their dorsal and rostral carapace spines relative to the carapace length, these spines being 246 A. L. RICE longest in Scopimera, shorter in Ilyoplax, and shortest in Dotilla. This variation in carapace spine length is reflected in a difference in overall size, the first zoeae of S. crabricauda and S. globosus being more than 2 mm from the tip of the dorsal spine to the tip of the rostral spine, whereas in the described first stages of Ilyoplax and Dotilla species this dimension is little more than i mm. Finally, the wing-like expansions of the fifth abdominal somite in the zoeae of Dotilla species (see Ramadan, 1940 ; Gohar & Al-kholy, 1957 ; Rajabai, 1959) clearly distinguish them from the known larvae of both Scopimera and Ilyoplax. REFERENCES AIKAWA, H. 1929. On the larval forms of some Brachyura. Rec. oceanogr. Wks Jap. 9 : 87- 162. ALCOCK, A. 1900. Materials for a carcinological fauna of India. No. 6. Brachyura, Cato- metopa or Grapsoidea. /. Asiat. Soc. Bengal 69 : 279-456. GOHAR, H. A. F. & AL-KHOLY, A. A. 1957. The larvae of some brachyuran Crustacea. Publs mar. biol. Stn. Ghardaqa 9 : 146-176. KEMP, S. W. 1919. Notes on Crustacea Decapoda in the Indian Museum. XII. Scopi- merinae. Rec. Indian Mus. 16 : 305-348. RAJABAI, K. G. 1959. Studies on the larval development of the Brachyura. I. The early and post larval development of Dotilla blanfordi Alcock. Ann. Mag. nat. Hist. ser. 13, 2 : 129-135. RAMADAN, M. M. 1940. On the first zoeal stage of Dotilla sulcata (ForskSl). Ann. Mag. nat. Hist. ser. n, 5 : 253-255. RICE, A. L. 1975. The first zoeal stages of Cancer pagurus L., Pinnotheres pisum (Pennant) and Macrophthalmus depressus Riippell (Crustacea, Decapoda, Brachyura). Bull. Br. Mus. nat. Hist. (Zool.) 28 : 237-247. STEPHENSEN, K. 1945. The Brachyura of the Iranian Gulf. Dan. Scient. Invest. Iran 4 : 57- 257- DR A. L. RICE INSTITUTE OF OCEANOGRAPHIC SCIENCES WORMLEY GODALMING SURREY ASTEROZOA FROM AMSTERDAM AND ST PAUL ISLANDS, SOUTHERN INDIAN OCEAN By AILSA M. CLARK SYNOPSIS Asteroids and ophiuroids collected recently around Amsterdam and St Paul Islands by French scientific collectors in association with lobster fishing vessels are reported. One new species of asteroid, a goniasterid named Sphaeriodiscus mirabilis, is described and the systematic position of another asteroid, named Culcita veneris by Perrier (1879) but now confirmed as better placed in Spoladaster, is discussed at some length with comments on related Poraniidae. Besides a third asteroid and one ophiuroid species previously recorded, four other ophiuroids new to these islands are also found to occur there. INTRODUCTION THE interesting collection of Asterozoa which forms the basis for this report was sent to the British Museum by Dr P. M. Arnaud of the Station Marine d'Endoume in Marseille. The material was primarily collected by Dr J. Beurois in 1971-72 but a few additional specimens originated from P. M. Arnaud, P. Noel, R. Vranckx, M. Segonzac and the fishing vessel Maria Martina. Financial support for the collectors came from Terres Australes et Antarctique Frangaises and logistic support from S.A.P.M.E.R. (Societe Anonyme de Peche Maritime et de Ravitaillement), to which institutions thanks are also due. Hitherto the only published records of Asterozoa from these remote islands in the Indian Ocean (c. 38°S, 77^°E) were based on material from two sources. Firstly the French Transit of Venus Expedition, 1874-75 (naturalist C. Velain), from which two ^asteroids, named as Asterina exigua (Lamarck) and Culcita veneris sp. nov., were reported by Perrier (1879). Secondly the German South Polar (Gauss) Expedition of 1901-3, which evidently took only the first asteroid, recorded as Patiriella exigua by Doderlein (1927), and one ophiuroid, recorded as Amphipholis minor by Hertz (1927). Dartnall (1971) confirmed that the Gauss asteroids are conspecific with Patiriella exigua (Lamarck) from South Africa and temperate Australia, when he split off tropical records of P. exigua as a distinct species. In contrast, Perrier's second asteroid and the new species now described appear to be endemic to these isolated islands. Thanks to offshore work by lobster fishing vessels on the shelf around these islands to a depth of about 300 m and to painstaking collecting from washings of encrusting organisms, one fine new species of goniasterid starfish and four additional species of ophiuroids are included in the present material. Unfortunately most of the ophiuroids are very small and not in good condition and one amphiurid is not Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 Issued 25 November 1976 15 248 A. M. CLARK identifiable to species. However, the other three indicate an affinity with the ophiuroid fauna of south and south-east Africa in similar latitudes up-current in the West Wind Drift. This accords with the distribution of some other benthic invertebrates. DESCRIPTION OF SPECIES ASTEROIDEA Sphaeriodiscus mirabilis sp. nov. (Pis i and 2) MATERIAL. Vicinity of St Paul and Amsterdam Islands at 200-300 metres, fishing vessel Maria Martina, 1971, the holotype, B.M. reg. no. 1976.1.12.1. DESCRIPTION. R/r 70/45 mm = 1-56/1. The breadth of the swollen arm tip is c. 26 mm. The area of abactinal plates is almost pentagonal. After preservation in spirit it is sunken below the raised rim of the superomarginal plates. Distally the abactinal plates are hexagonal and fairly regular in arrangement in longitudinal and diagonal series but interstitial plates are found proximally to about two-thirds R from the centre and as these become larger and more numerous towards the centre the regular arrangement is lost. A mid-radial row of plates is j ust discernible, though proximally its constituent plates are all separated. Conversely the plates of the interradial rows are nearly all contiguous. All the plates are flat-topped and covered with a pavement of close polygonal flat-topped granules, numbering about 70 on the larger plates. Papulae are wide- spread except close to the superomarginals and in interradial bands. The madreporite is triangular with two angles truncated to form an irregular pentagon. It lies at about one-third r from the centre. The superomarginal plates number only four in each series (i.e. eight on each of the five sides) with the exception of one series where a short extra plate occurs between the second and third. In some of the other series at this same position a triangular abactinal plate is partially inserted between these two marginals, possibly reinforcing this vulnerable area. The two inner superomarginals are elongated tangentially, rectangular in outline and slightly raised at the joints, though in general with a part-cylindrical section. The third plate is abruptly enlarged and swollen, extended radially to meet its fellow ; together with the two smaller fourth superomarginals of each ray these make the upper side of a discrete broad rounded knob. The sutures between the third and fourth plates are oblique to the midradial line and the fourth plates are unequal in size so that the sutures are asymmetrical in all five cases. The inferomarginals match the upper series in general but individual plates may be slightly misaligned ; also there is an additional fifth plate in each series, bordering the small spout-like terminal plate. The third to fifth plates participate in the knob-like expansion of the tip. The more convex areas of the swollen marginals are mostly naked with only scattered granules over most of their surface and these sunk into sockets in the plates ; only peripherally is the granulation continuous, as it ASTEROZOA FROM THE SOUTHERN INDIAN OCEAN 249 is on the first two (interradial) plates. The suture between the two marginal series is distinctly above the ambitus so that the inferomarginals are clearly visible from above but this may be due to contraction of the upper side during preservation. The actinal plates in the distal halves of the rays form regular longitudinal series but proximally the arrangement becomes irregular because of the development and enlargement of interstitial plates. All the plates are fully covered with polygonal flat-topped granules distinctly coarser than the abactinal ones with the peripheral row discrete, even to the naked eye. The adambulacral plates mostly bear five short blunt-tipped furrow spines, aligned vertically, sometimes four or (distally) six. These stand out slightly from the lower surface but are backed by several series of shorter 'spines' transitional to granules, all angular in section. No pedicellariae can be distinguished. AFFINITIES. This handsome goniasterid with its limited number of marginal plates has a considerable resemblance to those individuals of Pentagonaster pulchellus Gray, from temperate Australasia, with swollen arm tips (such as the holotype shown in Gray's pi. 8, fig. 3, 1866). Pentagonaster differs however in having the abactinal plates with only peripheral granules and their centres more or less markedly convex ; also the individual marginal plates are rounded at the angles, not rectangular. There is also a remarkable resemblance to the Jurassic Miopentagonaster calloviensis Mercier in the very broad rounded arm tips, though again in that fossil species it is only the distalmost marginal of each series (together with the enlarged terminal plate in this case) that forms the expansion. The interradial marginals of M. calloviensis number only four on each of the five sides and appear rectangular in dorsal view, as in S. mirabilis. However, judging from the great variation in the breadth of the arm tips in various goniasterid species such as Pentagonaster pulchellus and Tosia australis I think it likely that other specimens from the Amsterdam/St Paul area may prove to have more pointed arm tips. This is the case in the holotype of Sphaeriodiscus scotocryptus Fisher, 1913, from the Philippine Islands. It too has an almost complete granule covering, except on the centres of the marginal plates, a basically pentagonal form but for projecting tips to the rays and a limited number of marginal plates - in this case at R 32 mm five superomarginals with the three rectangular proximal ones of each series forming the sides of the body and the two distal ones contiguous mid- radially with their corresponding plates and forming the arm tip. Apart from these narrow arm tips and the additional marginal plate in each series at a smaller total size, 5. scotocryptus differs from the new species in having seven to ten furrow spines on each plate, besides numerous pedicellariae, though this last may not be a specific character. Of the other species of Sphaeriodiscus, the type species, Sphaeriodiscus bourgeti (Perrier, 1885) from off north-west Africa, also has four superomarginals but the first one is relatively short (tangentially) and the second is distinctly more swollen though not meeting its fellow midradially, the third plate is still convex but smaller than the second so that the outline is approximately pentagonal. The largest of Perrier's specimens had R 35 mm. H. L. Clark (1926) has recorded a specimen with R 27 mm 250 A. M. CLARK from off Natal in 420 m as S. bourgeti, expressing surprise about the extension of range to the south-east side of South Africa. The fourth superomarginals are only just beginning to appear and the arm tips are somewhat swollen, vertically if not horizontally, at least, judging from the measurements. He compared it with a syntype and with Perrier's figures and found no significant difference, so the Natal specimen presumably also has the second superomarginal distinctly larger and more swollen than the first, a condition also found by Madsen (1958) in a specimen of 5. bourgeti from the Cape Verde area and difficult to reconcile with the close similarity of the first two marginals in 5. mirabilis. Madsen compared 5. bourgeti with a small specimen of 5. placenta (Miiller & Troschel, 1842), known from wide- spread localities in the Atlantic and Mediterranean, the main difference in the latter being the similarity of the consecutive superomarginals of which the fourth is already well developed. 5. placenta is known to reach a size of nearly 90 mm R and at the same time to increase the number of marginals in each series to a maximum of nine superomarginals, though more often five to seven ; two to five of the distal ones may be contiguous midradially and the arm tip may be broadened in some specimens as shown in Tortonese's fig. 72 (1965) of a Mediterranean example. In the Pacific, Sphaeriodiscus inaequalis (Gray, 1847), supposedly from Amboina or New Guinea, has an even more diminutive first marginal in both upper and lower series than 5. bourgeti in comparison with the second and third plates, which are markedly elevated with more or less tabulate raised areas, also on the corresponding inferomarginals, though at the same time the arms taper to a blunt point since the distal superomarginals are hardly at all expanded horizontally. At R only 21 mm, as in the holotype and only recorded specimen, there are only three or four supero- marginals in each series. Owing probably to abrasion of the surface, this specimen does not show the characteristic 'peppered' appearance of the barer parts of the marginals of Sphaeriodiscus due to the recessed isolated granules, but this appearance is very conspicuous in Fisher's photograph (1906) of the holotype of Sphaeriodiscus ammophilus, from the Hawaiian Islands. At R only 24 mm this has but three superomarginals and the third is relatively small yet, though the first is hardly at all smaller than the second. The form is pentagonal. LOCALITY. Unfortunately a small element of doubt exists concerning the type locality of S. mirabilis. Although the specimen came to Dr Arnaud together with invertebrates characteristic of the shelf in the vicinity of Amsterdam and St Paul Islands at 200-300 metres, the Maria Martina had also worked off South Africa and Reunion Islands. If it should prove that specimens of Sphaeriodiscus from Natal are conspecific with S. mirabilis rather than with S. bourgeti and no further material from these two remote islands is forthcoming, then the species may have to be deleted from their fauna. Patiriella exigua (Lamarck, 1816) Psterias exigua Lamarck, 1816 : 554. Asterina exigua : Perrier, 1879 : 47. Aatiriella exigua : Doderlein, 1927 : 296 ; Dartnall, 1971 : 40-43, pi. 4, fig. c. ASTEROZOA FROM THE SOUTHERN INDIAN OCEAN 251 MATERIAL. Amsterdam Island : mostly from the north side in the vicinity of La Roche Godon, under or on mid- or sub-littoral stones or in pools at low water, 60 specimens. St Paul Island : from the crater, mostly the north-east part near the entrance, on or under sub-littoral or sometimes mid-littoral stones or from scrapings, usually with white or green algae, ascidians or sponges and often with Amphipholis squamata and Amphiura capensis, in specimens. NOTES. Of the total of 171 specimens, two are four-rayed and two are six-rayed. Six out of 48 specimens from Beurois' station St Paul 8a (from the north-east part of the crater among lower mid-littoral and sub-littoral stones) appear more or less deformed, one having abnormally short rays and the interradii convex, making an ovate outline ; the other five have one or sometimes two rays aborted or possibly regenerated, their other four (or three) rays aligned at right angles to each other. The smallest specimens have R c. 0-5 mm and three pairs of tube feet in each ray. Spoladaster veneris (Perrier) (Fig. i ; PL 3, figs i, 2 ; PI. 4, figs i, 2 ; PL 5, figs i, 2 ; PL 6) Culcita veneris Perrier, 1879 : 47-49, pi. 4 ; Mortensen, 1933 : 249, 250 ; Arnaud & Beurois, 1972 : 874 [Non C. veneris : Bell, 1905 : 248.] Spoladaster ? veneris : Fisher, 1940 : 136 ; A. M. Clark, 1952 : 208. MATERIAL. Amsterdam Island : off east coast at 'BMG', in lobster pot, depth unknown, possibly 10-50 metres, with gastropods Ranella olearium and Charonia lampas pustulata, i specimen ; no details, i specimen ; from washings of the large bryozoan Turbicollopora redoutei, sponges, gorgonians, the scleractinian coral Caryophyllia prof undo. , alcyonarians, etc. at 80-100 metres, i juvenile. St Paul Island : off east coast in lobster pots, c. 300 metres, 3 specimens ; north- west coast at La Chaussee du Phoques, 10-50 metres ?, 2 specimens ; near Roche Nord, in lobster pot, i specimen ; various parts of the crater (the type locality) at 0-5-1 -0 metre and in sublittoral scrapings, sometimes with the gastropods Ranella and Charonia and with echinoids, 5 specimens. DESCRIPTION. A photograph of a live specimen (PL 6, fig. i) shows a distinctly stellate form, R/r c. i-8/i, whereas the preserved specimens all appear more nearly pentagonal with R/r i -2-1 -5/1. There must therefore be considerable contraction across the interradii marginally in preservation, possibly correlated with bending upwards of the arm tips, the resultant form having a close superficial resemblance to a Culcita. The collectors of Perrier's type material noted a considerable ability of the live animals to vary the shape of their outlines and degree of inflation of the upper side, which was also noted by the recent collectors. When inflated the whole appearance is said to be very like an orange, with which the bright colour of the upper side also agrees ; the lower side is paler. In the live specimen photographed the madreporite shows up clearly about midway from the centre to the indented inter- radial edge but in preserved specimens it appears at a quarter to a third r from the centre. The enlargement of an arm in life (PL 6, fig. 2) shows a very 'shaggy' effect 252 A. M. CLARK produced by the extended papulae, which appear to arise all over the upper side except for narrow bands, notably in the interradii and in the centre, with only the slightest indication of grouping as in the meshes of a reticulum. In specimens preserved in alcohol the papulae are more or less retracted. A rough texture can be felt through the pustular skin, produced by numerous fine spinelets, which are invisible unless the specimen is partially or completely dried. These are isolated in the body wall, not based on skeletal plates. Indeed, X-radiography of an adult shows that the only abactinal plates of any density remaining are a few at the tips of the rays. The spinelets have the shape shown in Fig. i(a). On the upper surface the spinelets are fairly evenly scattered but on the sides of the body they tend to become aligned in vertical series. At the junction of abactinal and actinal areas below the ambitus, where the papulae cease abruptly, this linear arrangement is even more marked and the pustular skin covering forms folds with narrow grooves between leading to the adambulacral furrows. Some of these series branch or anastomose. In wet specimens there is usually a distinct change in the contours where the actinal and abactinal areas meet, with a slight horizontal ridge where one would expect to find the inferomarginal series of plates. Drying tends to emphasize this and may bring out a second apparently reinforced band just above. However, there is no trace of a separate intermarginal band of papulae, such as occurs in Porania. X-radiographs show no marginal plates at all (PI. 5, figs i, 2), nor do drying, dissolv- ing the body wall or xylol treatment reveal any vestiges of marginal plates, even viewing from the inside of the body wall (PI. 3, fig. i), except at the tips of the rays. The external change in contours must therefore be due to reinforcing bands of connective or muscle tissue. The actinal spinelets are similar in form to the abactinal ones and are similarly isolated in the body wall. The X-radiographs taken fail to show up any actinal plates but special treatment or viewing from inside reveals that in each V-shaped interradial area adjoining the oral plates and the proximal adambulacrals is a small triangular patch of hollow, extremely thin-walled, rounded actinal plates (Fig. ic). More distally there are traces of two, possibly three, partial series of plates running parallel to the inferomarginal series but these are not complete interradially in any of the areas treated and usually only the youngest plates adjoining the adambulacral plates are at all distinct. Presumably these actinal plates are progressively reduced during growth. None of these vestigial plates bear any enlarged spinelets or spines. The adradial ends of the actinal pustular folds envelop the subambulacral spines as well ; these number two on one or two proximal plates but one on the rest. There are two separately sheathed spines bordering the furrow on most plates. The oral plates usually have four furrow spines and one larger subambulacral spine, though larger specimens, R 60 + mm, may have two. The juvenile specimen (Fig. ig, h) has R/r 1-5/1-3 mm (excluding the length of the marginal fringe of spinelets). The margin is formed entirely by the relatively large inferomarginal plates, four on each of the five sides, and the terminal plates. The adjacent plates dorsally (presumably superomarginals) are markedly convex at their outer edges. There are two midradial plates on each ray and a ring of five larger primary interradial plates around a small central area including the anus. All these ASTEROZOA FROM THE SOUTHERN INDIAN OCEAN 253 FIG. i. Spoladaster veneris (Perrier). (a-f) St. AMS-IO4- R c. 55 mm. (a) Abactinal spinelet. (b) Jaw and adjacent four adambulacral plates, denuded except for major spines, (c) Proximal apex of one ventral interradius partly dried and cleared with xylene to show pustular folds (somewhat shrunken) with isolated spinelets and under- lying reduced actinal plates, (d) Odontophore, viewed ventrally. (e, f) An isolated proximal adambulacral plate from the left side of a ray in aboral and adoral views, the furrow spines arose opposite the letter 'f (g, h) St. AMS-g6. Juvenile partly dried (some abactinal spinelets probably lost). (The scale equals c. I mm for a, c. 4 mm for b and c, c. 3 mm for d-f and 2 mm for g and h.) plates bear spaced rugose spinelets, mostly about three times as long as broad and slightly waisted. On the inferomarginals the spinelets graduate to the horizontal fringe of spinelets bordering the entire animal, which is interrupted only at the distal ends of the furrows. The ventral side is quite flat. The inferomarginals are com- pletely naked ventrally and the two first ones in each interradius cover most of the 254 A- M- CLARK interradial area together with the single actinal plate proximal to them. Two of the five actinal plates bear a single median distal spinelet but the other three are com- pletely bare. There are six pairs of podia in each ray. Except for the first plate, the adambulacrals bear three spines in a more or less straight line at right angles to the furrow. The first plates may have four spines, the second one aligned obliquely to the first and clearly potentially a furrow spine. Presumably during further growth the second spine on the succeeding plates also shifts to the furrow edge of the plate. The oral plates already have four furrow spines and one suboral, as in most adults. The general appearance of this specimen is remarkably like the holotype of Marginaster fimbriatus Sladen, 1889, as shown in Sladen's pi. 58, figs 4-6 ; that has R 6 mm and was collected to the north of Ireland. According to Ludwig it is conspecific with Marginaster capreensis from the Mediterranean but I consider that its affinities are much more likely to be with Poraniomorpha. The only difference between M. fimbriatus and this juvenile from the Indian Ocean is the development of a second row of actinal plates, which would be expected at the larger size. There is no question that this small specimen could be a young Patiriella exigua since there are examples of that species of comparable size and they show a much more granuliform armament, with single shorter adambulacral spines. Also the contours are quite different, the abactinal side rising vertically above the relatively smaller and more numerous inferomarginal plates. GENERIC POSITION. Perrier described this species as belonging to a separate section of the genus Culcita (now included in the tropical shallow-water family Oreasteridae of the order Valvatida), this section being characterized by the fleshy body wall concealing the skeleton. He also noted affinities with Asteropsis (currently aligned near the Poraniidae in the order Spinulosida) . In 1905 Bell identified a fleshy pentagonal South African asteroid as Culcita veneris but Mortensen (1933) referred this specimen to Cryaster brachyactis H. L. Clark, 1923, also from South Africa. At the same time Mortensen pointed out that Culcita veneris is not a Culcita but probably belongs to the Asteropidae or perhaps the Cryasteridae, though in a footnote he doubts the distinction of these two nominal families. In 1940 Fisher demonstrated that Cryaster antarcticus Koehler, 1906, the type- species of that genus, is congeneric with Perknaster fuscus Sladen, 1889 and so referable to the family Ganeriidae. However, he recognized that this affiliation does not extend to Cryaster brachyactis, for which he established a new nominal genus Spoladaster, referring it to the Asteropidae 'in the vicinity of Tylaster' . On the strength of Mortensen's comments, Fisher noted that Culcita veneris can probably also be referred to Spoladaster, an idea shared by me in 1952, when I suggested also that the South African Tylaster meridionalis Mortensen, 1933 might be based on smaller specimens of Spoladaster brachyactis. If this last premise proves true, then the problem is whether the species from South Africa and from Amsterdam and St Paul Islands are congeneric with Tylaster willei Danielssen & Koren, 1881, from the deep Norwegian Sea, this being the type species of Tylaster. More immediately there is still a possibility that specimens from Amsterdam and St Paul Islands could be conspecific with those from South Africa, in spite of ASTEROZOA FROM THE SOUTHERN INDIAN OCEAN 255 Mortensen's denial of this (probably without seeing specimens from the islands). Zoogeographically this would be quite likely in view of the fact that Patiriella exigua, one of the two other asteroids known from these isolated islands, is also found in southern Africa, though it occurs also in temperate Australia. In addition, at least two species of ophiuroids, as well as the cosmopolitan Amphipholis squamata, are here recorded as common to this island group and to either South Africa or southern Mozambique. However, the specimen of Spoladaster brachyactis in the British Museum collections from False Bay shows a distinct grouping of abactinal papulae in the meshes of an irregular reticulum, as described by H. L. Clark in the holotype. Also there is a separate horizontal band of papulae laterally in what should be the intermarginal area (PI. 3, fig. 3, top). H. L. Clark describes 'innumerable minute' abactinal plates bearing the spinelets in the holotype, though Fisher found in the paratype that abactinal plates of any sort are only present at the arm tips and I am unable to find such plates in the general abactinal body wall either. H. L. Clark also describes a series of 'rather large plates buried in the skin' between abactinal and actinal areas, i.e. inferomarginal plates, while Fisher found that the paratype has 'fairly large phanerozonid inferomarginal plates imbedded in the leather body wall'. However, the X-radiograph taken of the British Museum specimen shows no trace of any marginal plates (PI. 5, fig. 3), though the external view (PI. 4, fig. 3) shows that some short inferomarginal spines are present. Unfortunately this is the only South African specimen now in the British Museum collections and I hesitate to mutilate it further to ascertain if any rudiments of marginal or actinal plates, as described by Fisher, are visible on the inside of the body wall. In Mortensen's smaller holotype of Tylaster meridionalis from South Africa with R 28 mm there is a continuous marginal fringe of short spines, with a parallel series of a few similar actinal spines close by on the distal part of each actinal area mid-interradially. In another specimen (presumably of similar or smaller size since it was not selected as holotype) which he dried, Mortensen made visible three or four irregular series of actinal plates. The Cape Town University specimen with R c. 80 mm which I referred to Spoladaster brachyactis in 1952 has numerous actinal spines, which would be much coarser than the micro- scopical actinal spinelets of the Amsterdam/St Paul material. Finally, the adambulacral plates of 5. brachyactis (and of Tylaster meridionalis - if distinct) bear only one furrow spine apart from the subambulacral spine, whereas the Amsterdam/ St Paul specimens have two furrow spines. I have no doubt therefore that the latter specimens are specifically distinct, so that 5. veneris is a species endemic to the islands. The differences can be summed up as follows : Spoladaster veneris Spoladaster brachyactis No separate intermarginal band of An intermarginal band of papulae papulae laterally distinct No enlarged spines at the junction of Some inferomarginal spines usually the abactinal and actinal areas, nor present and in smaller specimens (R on the actinal areas c. 35 mm) also some actinal spines Two furrow spines on most Furrow spines usually single adambulacral plates 256 A. M. CLARK The problem remains as to whether or not these two species should be regarded as congeneric with one of the northern hemisphere genera such as Tylaster or Poraniomorpha, both of Danielssen & Koren, 1881. Unfortunately only a single young specimen of Tylaster willei is in the British Museum collections. This is the smaller specimen from Norwegian North Atlantic Expedition station 200 (7i°25'N ; i5°4i'E, 1134 metres). It has R only c. 12 mm. The triangular arms are curled up dorsally but the form is markedly stellate rather than pentagonal. There are prominent inferomarginal and actinal spines similar in size to the adambulacral spines. The species was very well described by Danielssen & Koren in 1884 (pp. 64-67, pi. n, figs 1-6), presumably on the basis of the single larger specimen, which was from the same station as this one. R is given as 40 mm and R/r can be calculated as i-6/i, the form again being markedly stellate. Drying of the dorsal body wall revealed numerous isolated spinelets, described as needle-like but appearing to be quite capitate in their pi. n, fig. 3. Viewing the body wall from the inside showed a horizontal series of rudimentary isolated lateral plates which were assumed to be the superomarginals and below these three series of more regular small plates linked by connective tissue, also approximately horizontal, the upper one of the three being taken for the inferomarginals and bearing externally a horizontal series of marginal spines in groups of usually three corresponding to the plates. Many of the actinal plates also bear similar but single spines forming several series, while there are some scattered additional proximal actinal spines. Tylaster willei thus seems intermediate in form and skeletal development between the Spoladaster spp. and the wide-ranging genus Porania, the latter having a usually stellate form and an articulated skeleton. Not surprisingly, the Amsterdam/St Paul species is remarkably similar to some North Atlantic pentagonal cushion-like specimens which were likewise ascribed to Culcita under the name Culcita borealis Sussbach & Breckner, 1911, from the area of the Shetlands, which name Farran (1913) also gave to some specimens from the west of Ireland. In 1914 Verrill established a new nominal genus Cukitopsis for C. borealis, pointing out that its affinities are with Tylaster and Chondraster of the family Poraniidae (which he kept distinct from the Asteropidae) . Ostergren (1904), Grieg (1907) and Koehler (1909) emphasized that Poraniomorpha hispida (M. Sars in G. O. Sars, 1872) is a very variable species, Koehler including records from both sides of the Atlantic in his lengthy synonymy. In 1927 Grieg referred Culcitopsis borealis to the synonymy of P. hispida and Mortensen (1927) agreed that 'there is hardly any doubt' this is correct. Most subsequent workers have accepted Mortensen's judgement so that the synonymy of this species includes the following : Goniaster hispida M. Sars in G. O. Sars, 1872 : 28 (R of the holotype n mm) : Storm, 1881 : 90. Asterina borealis Verrill, 1878 : 213 (R 12 mm). Porania spinulosa Verrill, 1879 : 202 (R 40 mm). Poraniomorpha rosea Danielssen & Koren, 1881 : 189 (Re. 27 mm, judging from the scale of the figures). Rhegaster murrayi Sladen, 1883 : 156 ; 1889 : 368 (R 14-3 mm). Lasiaster villosus Sladen, 1889 : 372 (R 10-5 mm). ASTEROZOA FROM THE SOUTHERN INDIAN OCEAN 257 Poraniomorpha hispida : Ostergren, 1904 : 615 ; Koehler, 1909 : 100 ; Grieg, 1927 : 129 (with forma borealis Sussbach & Breckner) ; Mortensen, 1927 : 92. Poraniomorpha (Lasiaster) hispida : Grieg, 1907 : 40. Culcita borealis Sussbach & Breckner, 1911 : 217 (R 40 mm) ; Farran, 1913 : 15. Poraniomorpha villosa : Farran, 1913 : 17. Culcitopsis borealis (Sussbach & Breckner) Verrill, 1914 : 21. Rhegaster borealis (Verrill) Verrill, 1914 : 17. As shown by the R measurements for the holotype of each nominal species included above, most of them are based on relatively small specimens, the exceptions being Porania spinulosa, Poraniomorpha rosea and Culcita borealis. This is very unfortun- ate since small specimens of poraniids may give an exaggerated impression of the extent of skeletal development in the adult, as the evidence suggests there is often a tendency for progressive resorption with growth. It is significant that there are several other North Atlantic poraniids with markedly reduced skeletons, namely C hondr aster grandis (Verrill, 1879), Chondraster hermanni Madsen, 1959 (treated as a subgenus of Porania}, Pseudoporania stormi Dons, 1936, Sphaeraster berthae and Sphaeraster bjorlykkei Dons, 1938 - the last nominal genus preoccupied and subse- quently renamed Sphaeriaster by Dons, all based on relatively huge specimens with R at least 80 mm and often 100 mm or even more. Madsen (1959) considers that all these are congeneric. I believe that their large size is responsible at least in part for their very reduced skeletons. The X-radiographs given by Dons and Madsen indicate that their material completely lacks abactinal and actinal plates of any substance and only Dons' Pseudoporania stormi has vestiges of supero- and infero- marginal plates. The holotype of Poraniomorpha hispida is described as pentagonal in form, R/r i -2/i, flat below and convex above, with both marginal series of plates distinct (probably by their contours). It came from the Lofoten Islands, off northern Norway. A larger specimen, R 40 mm, from Trondheim Fjord further south, presented to the British Museum by Storm, agrees well with this description (PI. 3, fig. 4 ; PI. 4, fig. 4 ; PI. 5, fig. 4). It was X-radiographed for comparison with Spoladaster brachyactis and 5. veneris, revealing very well-developed series of block- like supero- and inferomarginal plates outlining what appears to be an almost continuous pavement of slightly spaced plates, apparently mainly actinal plates but probably also some superimposed abactinals. In contrast, a cushion-like specimen in the British Museum collections, from the warm area of the Faeroe Channel, halved and dried (PI. 4, fig. 5) shows only vestigial microscopic abactinal platelets on the inside of the body wall, small isolated superomarginals barely distinguishable interradially, slightly less reduced but still discontinuous inferomarginals and two well-separated series of isolated actinal plates with a group of additional proximal ones in each area. The inferomarginals and actinals are clearly in process of resorption, most of them being crescentiform or ring-shaped. This degree of skeletal reduction approximates to that shown by Spoladaster and at the same time makes it difficult to regard C. borealis as conspecific with well- calcified specimens of Poraniomorpha hispida such as the one from Trondheim Fjord. Although he did not mention Poraniomorpha in his 1959 paper, Madsen's remarks on 258 A. M. CLARK the variations of the northern Porania pulvillus suggest that the distinction between that and Poraniomorpha is by no means sharp and needs further study, especially of growth changes. Until this can be done for the northern poraniids and the various taxa can be redefined, it seems unwise to alter further the nomenclature of these two southern species, which I accordingly propose to leave under the name of Spoladaster. OPHIUROIDEA Amphipholis squamata (Delle Chiaje, 1829) Asterias squamata Delle Chiaje, 1829 : 74, 77, figs 1-4. Amphipholis minor : Hertz, 1927 : 35. Amphipholis squamata : Mortensen, 1933 : 364-365. MATERIAL. Amsterdam Island : mostly from mid- to sub-littoral, in algae or coralligenous substrates or rock pools from various parts of the shore, some from grab hauls off the east coast down to 80 metres, others from stomachs of fishes such as Acantholatris monodactylus, 135 specimens. St Paul Island : from washings of algae and Laminaria roots, east coast towards Roche Quille, 3-4 metres, 24 specimens ; washed from Macrocystis roots, 62 specimens ; from various parts of the crater, mostly under sublittoral stones or in washings from sponges, algae, bryozoa, compound ascidians, etc., 150 specimens. Sea-mount south-east of St Paul Island : with compound ascidians, the scler- actinian coral Caryophyllia profundi and bryozoa at 120 metres, i specimen. NOTES. Most of these specimens are very small and in poor condition. Some were mixed with Amphiura capensis and also with young Patiriella exigua. Mortensen has already pointed out that the Amphipholis from St Paul Island crater recorded by Hertz are not distinguishable from A . squamata, the only cosmo- politan echinoderm. Amphiura capensis Ljungman, 1867 Amphiura capensis Ljungman, 1867 : 320 ; Mortensen, 1933 : 348-350. MATERIAL. Amsterdam Island : washed from coralligenous bottom at 35 metres, north-east coast, i specimen ; from stranded laminarians, near La Cale, north coast, 3 specimens. St Paul Island : from Macrocystis and Laminaria roots, 23 specimens ; from various parts of the crater, usually under sublittoral stones, 29 specimens. NOTES. Most of the specimens from the crater of St Paul Island were taken with Amphipholis squamata and some also with young Patiriella exigua. All are small, the disc diameter not exceeding 4 mm. The arm spines number up to five proximally and are markedly flattened and spatulate. Some specimens have the disc scaling deficient near the oral shields, as shown also in many South African specimens. This species is easily distinguished from Amphipholis squamata by the radial shields being only contiguous distally, the arm spines being more numerous and a different shape and the distal oral papillae and tentacle scales being single. ASTEROZOA FROM THE SOUTHERN INDIAN OCEAN 259 These records represent an extension of range from southern Africa, where Amphiura capensis is known from Luderitz Bay to Natal. Amphiura sp. MATERIAL. St Paul Island : on coarse sandy bottom with Venus at 50-80 metres off the north-east coast, 4 specimens. Sea-mount south-east of St Paul Island : with compound ascidians, Caryophyllia and bryozoa at 120 metres, 2 specimens. NOTES. Unfortunately all these specimens are in poor condition. The disc was probably fully scaled, the radial shields about a third as long as the disc radius and contiguous for their distal third, inwardly divergent. The oral shields are as long as broad or slightly longer, with the distal lobe shorter than the proximal angle. The distal oral papilla is blunt. The dorsal arm plates are fan-shaped. There are four tapering but blunt-tipped arm spines. The tentacle scales mostly number two but one specimen has more pores with only a single small scale. None of these characters are particularly distinctive. This species does not agree with any so far recorded from southern Africa, judging from these specimens. Ophiactis sp. probably O. savignyi Miiller & Troschel, 1842 MATERIAL. Amsterdam Island : dredged on consolidated bottom at 40-50 metres off north coast, i specimen. St Paul Island : washed from various coralligenous encrusting organisms, com- pound ascidians, Caryophyllia, bryozoa, etc. at 60-80 metres off the north-east coast, i specimen. NOTES. Both specimens are fissiparous with six arms ; one has three arms larger and three regenerating, the other has two and four. Even the larger specimen has the disc diameter only just exceeding i mm. The disc scales are relatively coarse at this small size and the proportions of the radial shields not obvious - partly due to the regeneration. One specimen has disc spines, the other has not. Some of the jaws have two distal oral papillae on at least one side, elsewhere there is only one distinct papilla. The dorsal arm plates are fan- shaped but the distal curve is flattened medially. There are four rugose arm spines, all but the uppermost one truncated. The occurrence of two distal oral papillae in some cases and the shape of the arm spines make it almost certain that these two small specimens are referable to the 'tropicopolitan' Ophiactis savignyi, which ranges down the coast of East Africa to Natal. Ophiocoma pusilla (Brock, 1888) Ophiomastix pusilla Brock, 1888 : 499. Ophiocoma pusilla : Devaney, 1970 : 25-28. MATERIAL. Amsterdam Island : on consolidated bottom at 40-50 metres off the north coast, i specimen. 260 A. M. CLARK Sea-mount south-east of St Paul Island : with compound ascidians, Caryophyllia and bryozoa at 120 metres, 10 specimens. NOTES. The largest specimen has disc diameter 7-5 mm and is the only one to show the swollen-tipped arm spines on a few segments beyond the arm bases so characteristic of this diminutive species of Ophiocoma. The granulation of the disc distinguishes this from any of the other species recorded from these two islands. Ophiocoma pusilla is known from isolated records throughout the tropical Indo- West Pacific, as far south in East Africa as Inhaca, southern Mozambique. It is usually found in coral heads, mostly in shallow water but possibly down to just over 100 metres. Because of its furtive habits and likelihood of confusion with other species of Ophiocoma, it may well have been overlooked at greater depths. One of the two localities at which this species was collected is common to the Ophiactis discussed above. If this really is Ophiactis savignyi, as seems very likely, then the extension of range to Amsterdam and St Paul Islands of another tropical reef species is not surprising. REFERENCES Papers not marked with an asterisk relate only to North Atlantic Poraniidae. *ARNAUD, P. M. & BEUROIS, J. 1971 [1972]. Premiere signalisation des genres Charonia et Ranella aux iles St-Paul et Amsterdam (Ocean Indien) et revision du genre Argobuccinum (Gastropoda Cymatiidae). Tethys 3 (4) : 865-874. *BELL, F. J. 1905. The Echinoderma found off the coast of South Africa. 2. Asteroidea. Marine Invest. S. Afr. 3 : 241-253. *BROCK, J. 1888. Die Ophiuridenfauna des indischen Archipels. Z. wiss. Zool. 47 : 465-539. *CLARK, A. M. 1952. Some Echinoderms from South Africa. Trans R. Soc. S. Afr. 33 : 193- 221, 3 figs, pi. 17. *CLARK, H. L. 1923. The Echinoderm fauna of South Africa. Ann. S. Afr. Mus. 13 : 221- 435, 4 figs, pis 8-13. * 1926. Echinoderms from the South African Fisheries and Marine Biological Survey. 2. Sea-stars (Asteroidea). Rep. Fish. mar. biol. Surv. Un. S. Afr. No. 4 : Spec. Rep. No. 7 : 1-34, 7 pis. DANIELSSEN, D. C. & KOREN, T. 1881 . Fra den norske Nordhavs-expedition : Echinodermer. Nyt. Mag. Naturvid. 26 : 177-195, 2 pis. — 1884. Asteroidea. Norwegian North- Atlantic Expedition, 1876-1878. Zoology. n8pp., 15 pis. Christiana. *DARTNALL, A. J. 1971. Australian sea stars of the genus Patiriella (Asteroidea, Asterinidae) . Proc. Linn. Soc. N.S.W. 96 : 39-49, i fig., 2 pis. *DELLE CHIAJE, S. 1829. Asteria. Memorie sulla storia e notomia degli animali senza vertebre del Regno di Napoli, 3 : 74-81. Napoli. *DEVANEY, D. M. 1970. Studies on ophiocomid brittlestars. i. Smithson. Contr. Zool. No. 51 : 1-41, 49 pis. *DODERLEIN, L. 1927. Die Seesterne der deutschen Siidpolar-Expedition, 1901-1903. Dt. Sudpol. Eyped. 19, Zool. n : 291-301, 4 pis. FARRAN, G. P. 1913. The deep-water Asteroidea, Ophiuroidea and Echinoidea of the west coast of Ireland. Sclent. Invest. Fish. Brch Ire. 1912 (6) : 1-66, 17 figs, 2 pis. *FISHER, W. K. 1906. The starfishes of the Hawaiian Islands. Bull. U.S. Fish. Comm. 23 (3) : 987-1130, 49 pis. ASTEROZOA FROM THE SOUTHERN INDIAN OCEAN 261 *FISHER, W. K. 1940. Asteroidea. Discovery Rep. 20 : 69-306, 23 pis. *GRAY, J. E. 1866. Synopsis of the species of starfish in the British Museum, iv+iy pp., 1 6 pis. London. GRIEG, J. A. 1907. Echinodermen von dem norwegischen Fischereidampfer "Michael Sars" in den Jahren 1900-1903 gesammelt. Asteroidea. Bergens Mus. Aarb. 1906 (13) : i- 87, 10 figs, 2 pis. 1927. Echinoderms from the west coast of Norway. Nyt Mag. Naturvid. 65 : 127- 136, 6 figs. *HERTZ, M. 1927. Die Ophiuriden der deutschen Siidpolar-Expedition, 1901-1903. Dt. Sudpol. Exped. 19, Zool. n : 1-56, 9 pis. KOEHLER, R. 1909. Echinoderms provenant des campagnes du yacht "Princesse Alice". Result. Camp, scient. Prince Albert 34 : 1-317, 32 pis. *LAMARCK, J. B. P. A. DE 1816. Radiare Echinodermes. Histoire naturelle des Animaux sans Vertebres, Ed. i, 2 : 522-568 ; 3 : 1-76. Paris. *LJUNGMAN, A. 1867. Ophiuroidea viventia hue usque cognita enumerat. Ofvers. K. VetenskAkad. Fdrh. Stockh. 23 : 303-336. *MADSEN, F. J. 1958. On Sphaeriodiscus placenta and a few other sea-stars from W. Africa. Bull. Inst.fr. Afr. noire 20A : 90-94, 4 figs. 1959. On a new North Atlantic sea-star, Chondraster hermanni n. sp., with some re- marks on related forms. Vidensk. Meddr dansk naturh. Foren. 121 : 153-160, 4 figs. MORTENSEN, T. 1927. Handbook of the Echinoderms of the British Isles. 1x4-471 pp., 269 figs. London. * 1933- Echinoderms of South Africa (Asteroidea and Ophiuroidea). Vidensk. Meddr dansk naturh. Foren. 93 : 215-400, 91 figs, 12 pis. *MULLER, J. & TROSCHEL, F. H. 1842. System der Asteriden. xx+134 pp., 12 pis. Braun- schweig. OSTERGREN, H. 1904. Ueber die arktischen Seesterne. Zool. Anz. 27 : 615-616. *PERRIER, E. 1879. Les Stellerides de 1'ile Saint-Paul. Arch. zool. exp. gen. 31 : 47-49, pi. 4. SARS, G. O. 1872. Nye Echinodermer fra den Norske Kyst. Fork. VidenskSelsk. Krist. 1871 : 1-31. SLADEN, W. P. 1883. The Asteroidea of H.M.S. "Challenger" Expedition. 2. /. Linn. Soc. Zool. 17 : 214-269. 1889. Asteroidea. Rep. scient. Results Voy. Challenger. Zool. 30: 1-935, 118 pis. STORM, V. 1881. Bidrag til Kundskab om Throndhjemsfjordens Fauna. 3. K. nor she Vidensk. Selsk. Skr. 1880 : 73-96. SUSSBACH, S. & BRECKNER, A. 1911. Die Seeigel, Seesterne und Schlangensterne der Nord- und Ostsee. Wiss. Meeresunters. Kiel N.S. 12 : 167-300, 3 pis. *TORTONESE, E. 1965. Echinodermata. Faunad' Italia. 6 : xv + 422 pp., i86figs. Bologna. VERRILL, A. E. 1878. Notice of recent additions to the marine fauna of the eastern coast of North America. Amer. J. Sci. 16 : 207-215, 371-378. 1879. Notice of recent additions to the marine Invertebrata of the northeastern coast of America. Proc. U.S. natn. Mus. 2 : 165-205. 1914. Revision of some genera and species of starfishes, with descriptions of a few new genera. Ann. Mag. nat. Hist. 14 : 13-22, i pi. AILSA M. CLARK Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 530 PLATE i Sphaeriodiscus mirabilis sp. nov. Holotype in dorsal view (scale in mm). Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 PLATE i 16 PLATE 2 Sphaeriodiscus mirabilis sp. nov. Holotype in ventral view (scale in mm). Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 PLATE 2 16* PLATE 3 FIGS i & 2 (right). Spoladaster veneris (Perrier). B.M. reg. no. 1975.12.4.164, 165. St. ST PAUL-yi, dried half specimen opened out, R 58 mm, viewed internally ; intact specimen, R 52 mm, viewed dorsally. FIG. 3 (top left). Spoladaster brachyactis (H. L. Clark). 1904.4.20.133, False Bay, South Africa, R 58 mm, viewed dorsally. FIG. 4 (bottom left). Poraniomorpha hispida (M. Sars). 91.4.15.1, Trondheim Fjord, Norway, R 40 mm, viewed dorsally. (See PI. 4 for scale.) Bull. Br. Mus. nat. Hist. (Zool.) 30. 6 PLATE 3 PLATE 4 FIGS i & 2 (right). Spoladaster veneris. FIG. 3 (top left). Spoladaster brachyactis. FIG. 4 (bottom left). Poraniomorpha hispida ; all as in PL 3 but in external or ventral views. FIG. 5 (centre). Poraniomorpha hispida forma borealis (Sussbach & Breckner), 1974.1.4.1, Faeroe Channel, west of Wyville Thomson Ridge, dried half specimen, side view (scale in mm). Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 PLATE 4 PLATE 5 FIGS i & 2 (right). Spoladaster veneris. FIG. 3 (top left). Spoladaster brachyactis. FIG. 4 (bottom left). Poraniomorpha hispida ; all as in PI. 3, X-radiographs. Bull. BY. Mus. mat. Hist. (Zool.) 30, 6 PLATE 5 PLATE 6 Spoladaster veneris (Perrier). Live whole specimen and one ray in dorsal view, photographed by Dr Beurois. (Superimposed on black.) Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 PLATE 6 RESTRICTION OF THE FAMILY PORANIIDAE, SENSU SPENCER & WRIGHT, 1966 (ECHINODERMATA : ASTEROIDEA) By FREDERICK H. C. HOTCHKISS AND AILSA M. CLARK SYNOPSIS The amalgamation of two families of asteroids under the name Poraniidae in the Asterozoa section of the Treatise on invertebrate paleontology by Spencer & Wright (1966) is here rejected on the basis of the fundamentally different arrangement of the actinal plates in the two groups of genera concerned. INTRODUCTION THE initiative for this note and the observation on which it is based came from one of us (F. H. C. H.), the history of the problem being dealt with by the other. The specimens used to illustrate it were specially prepared (by treatment with KOH followed by glycerine to increase the transparency of the normally opaque skin and reveal the skeleton) by Mr R. H. Harris of the Histology and Preservation Section of the Zoology Department, British Museum (Natural History), and photographed to emphasize further the skeletal structure by Mr P. A. Richens of the Photographic Unit of the Museum, to whom we are indebted. HISTORY In 1840 three nominal genera of stellate, thick-skinned asteroids were described : (1) Aster ope Miiller & Troschel (i84oa) with type Asterias carinifera Lamarck, 1816, by monotypy, renamed Asteropsis by the same authors (i84ob) several months later (without explanation but presumably because they had found the first name preoccupied) ; (2) Gymnasteria Gray for G. spinosa and G. inermis spp. nov. ; and (3) Porania Gray for 'Asterias gibbosa Leach', said to be Leach 1817 but probably from an MS catalogue of the British Museum collections. (This is not the same species as Asterias gibbosa Pennant, 1777, which Gray gives as Asterina gibbosa on the next page.) Gray's paper was published in December, 1840 and post-dated both of Miiller & Troschel's (see Fisher, 1908). In their main work, the System der Asteriden in 1842, Miiller and Troschel cited both Gymnasteria and Porania as synonyms of Asteropsis. They included in the genus A. carinifera (Lamarck), Asteropsis ctenacantha sp. nov. (referred to the synonymy of Porania pulvillus (O. F. Miiller) by Perrier, 1875), Asterias pulvillus Bull. BY. Mus. nat. Hist. (Zool.) 30, 6 Issued 25 November 1976 264 F- H- c- HOTCHKISS AND A. M. CLARK O. F. Muller, 1788, with synonym Porania gibbosa Gray, and Asterias vernicina Lamarck, 1816 ; also in a postscript Gray's Gymnasteria spinosa and G. inermis, which they thought to be conspecific at least with each other. After study of Gray's types of G. spinosa and G. inermis in the British Museum collections, Perrier (1875 : 285) referred both to the synonymy of Asterias carinifera Lamarck. This should automatically have relegated Gymnasteria Gray where it belongs in the synonymy of Asteropsis Muller & Troschel. Although Perrier was aware of Muller & Troschel's usage of Asteropsis in 1840 before Gray's of Gymnasteria (see 1875 : 9-10), for some reason he retained the name Gymnasteria for A. carinifera and at the same time improperly emended Asteropsis to include only Asterias vernicina Lamarck, ineligible as type-species since not included in 1840. Since he simultaneously synonymized Petricia punctata Gray, 1847, the type species of Petricia Gray, with A . vernicina, this move dispensed with a valid generic name while perpetuating at the same time an invalid one. Unfortunately Sladen was apparently unaware that Muller & Troschel had used Asteropsis already in 1840 and perpetuated Perrier's errors until they were pointed out by Fisher (1908 and 1911 : 247, 248) when he noted that Asterope Muller & Troschel, 1840 is not invalidated by Asterope Philippi, 1840, having been published at least two months earlier. He therefore referred Gymnasteria Gray to the synonymy of Asterope, rejected Asteropsis as superfluous and revived Petricia Gray from synonymy. As for the family position of these genera, in 1875 Perrier included Porania, Asteropsis (emended), Dermasterias nov. and Gymnasteria at the end of the Goni- asteridae, following them with the Asterinidae and implying some affinity with the latter family. In 1879 Viguier referred the first three genera to the Asterinidae. However, in 1884 Perrier divided the families of asteroids into named orders, placing the Asterinidae in the order Spinulosae but establishing a new family Gymnasteriadae in the order Valvulatae (p. 165) (although on p. 154 he lists a family Asteropsidae in the order Valvatae !). Included in the Gymnasteriadae were Gymnasteria, Porania, Asteropsis, Dermasterias and Marginaster gen. nov. In the Challenger report, Sladen (1889 : 355-356) adopted Gymnasteriidae (with corrected spelling) and added Tylaster and Poraniomorpha, both of Danielssen & Koren, 1881, also Rhegaster Sladen, 1883 and Lasiaster gen. nov. ; he commented on the affinity of some of these with the Asterinidae. After discovery of the echinasterid which he called Poraniopsis, Perrier in 1891 (pp. 107, 163) removed Porania from the Gymnasteriidae to the Asterinidae, adjacent to the Echinasteridae in the order Spinulosae. He made no mention in the discussion of Porania that it should be referred to a family of its own but in 1894 (p. 163) took this action, though citing 'Poraniidae Perrier, 1891'. This is more puzzling because in his preliminary discussion on classification in the 1894 Travailleur and Talisman report he makes not the slightest mention of Poraniidae and indeed lists Marginaster pentagonus (the only relevant species collected by these vessels) under the family Pentagonasteridae (i.e. Goniasteridae) on p. 30. On p. 163 he placed Poraniidae in the Spinulosae and included in it Porania, Tylaster, Poraniomorpha, Marginaster, Rhegaster and Lasiaster. This would leave only Gymnasteria, Asteropsis and RESTRICTION OF PORANIIDAE (ASTEROIDEA) 265 Dermasterias in the family Gymnasteriidae, which is listed on p. 327 under the order Valvata [sic]). Having in 1908 renamed as Asteropidae Perrier's Gymnasteriidae, in 1911 Fisher referred Porania and its relatives to the Asteropidae. Verrill (1914 : 304) expressed doubt about this because of affinity of Porania with the Asterinidae and in 1919 Fisher separated them again, though removing also Dermasterias to the Poraniidae, leaving only Asterope and Petricia in the Asteropidae. In the years following, several new nominal genera were added to the Poraniidae, while others were synonymized. Mortensen (1933 : 249) included under the heading Asteropidae Tylaster meridionalis and 'Cry aster' brachyactis (both more closely related to Porania than to Asterope) ; then Fisher (1940 : 136) named a new genus Spoladaster for C. brachyactis, again giving the family as Asteropidae (while on p. 154 he deals separately with the family Poraniidae) a treatment also followed by A. M. Clark in 1952. H. L. Clark (1946 : 109) also evidently considered that Poraniidae and Asteropidae can be kept distinct. However, Madsen (1959 1153) refers to Porania under Asteropidae, order Spinulosa. Spencer & Wright (1966 : U6g) in the Treatise on invertebrate paleontology again unite the two groups of genera but under the name Poraniidae Perrier, 1894, in the order Spinulosida. They also show that Asterope Miiller & Troschel is after all invalid, being preoccupied by Asterope Hiibner, 1819, an insect, and must be replaced by Asteropsis (a fact noted independently by A. M. Clark in 1967). TAXONOMY Clearly with so much anomalous treatment it is time that this problem was re-examined by further study of the skeleton obscured beneath the thick skin of these asteroids. The use of X-radiography by Dons (1936, 1938) and Madsen (1959) has revealed the extent of reduction of the skeleton in some species related to Porania and even more to Poraniomorpha but it is comparison between the better-calcified Porania itself and Asteropsis that is needed. Examination revealed that there are two fundamentally different arrangements of the plates in the triangular actinal intermediate areas under each side of the arm among the genera of Poraniidae sensu Spencer & Wright. In Porania itself and also Poraniomorpha and Tylaster, for instance, the arrangement consists of rows of actinal plates running parallel to the inferomarginals, the zone of plate addition is adjacent to the adambulacrals and the shortest row is in the proximal part of the interradial area near the oral plates (PI. i). Conversely, in Asteropsis, Dermasterias and Petricia the arrangement consists of rows of plates running parallel to the adambulacrals, the zone of addition is adjacent to the inferomarginals and the shortest row adjoins the interradial inferomarginals in the distal part of the interradial area (PI. 2 ; PI. 3). The second pattern is the usual one in the families of the order Valvatida (e.g. Goniasteridae and Oreasteridae) as well as in some Spinulosida (e.g. Asterinidae). It is therefore possible to divide the genera concerned into two distinct groups. In the cases where the actinal plates are either few and irregular (e.g. the diminutive species referred to Marginaster*) or extremely reduced (e.g. Spoladaster and Tylaster) * Which I think may all prove to be based on juveniles of other Poraniid genera. A. M. C. 266 F. H. C. HOTCHKISS AND A. M. CLARK by resorption in adults, the pattern can be estimated by the locus of plate formation, judged by the sizes of the plates or the positions of the surviving plates when the older ones have been resorbed. The two groups of genera are as follows : ASTEROPSEIDAE*Hotchkiss & Clark, 1976 Asteropsis Miiller & Troschel, 1840 Dermasterias Perrier, 1875 Petricia Gray, 1847 PORANIIDAE Perrier, 1894 Porania Gray, 1840 Chondraster Verrill, 1895 Marginaster Perrier, 1881 Poraniella Verrill, 1914 Poraniomorpha Danielssen & Koren, 1881 Poranisca Verrill, 1914 Pseudoporania Dons, 1936 Sphaeriaster Dons, 1939 Spoladaster Fisher, 1940 Tylaster Danielssen & Koren, 1881 The Triassic genus Trichasteropsis Eck, 1879 (illustrated by Spencer & Wright, 1966, fig. 43-3a-c) has poraniid actinal growth gradients and should be transferred to the Poraniidae from the Palasterinidae (order Paxillosida) . Concerning the Ordovician somasteroid Chinianaster levyi Thoral, Spencer's reconstruction of this (1951, fig. 7 ; Spencer & Wright, 1966, fig. 39.4) shows poraniid- I' II Fig. i. Fig. 2. FIG. i. Diagram showing orientation and polarity of growth gradients as observed by Fell. FIG. 2. Diagram showing orientation and polarity of growth gradients observed in Poraniidae. *This family name is based on Asteropsis Miiller & Troschel, 18405, which is the earliest available name to replace Asterope Mtiller & Troschel, i84oa, and is a senior subjective synonym of Gymnasteria Gray, (Dec.), 1840 (see Miiller & Troschel, 1842 : 65). Asteropsidae Perrier (1884:154) is not valid under Article 55 of the Code because he exluded the the type-species, A. carinifera Lamarck, from the type- genus, Asteropsis. Gymnasteriidae (as Gymnasteriadae) Perrier (1884 1165), based on the junior synonym, though adopted by some nineteenth century authors, has not been used for nearly 70 years and may be considered to have lost all claims to validity under Article 40. The inserted ' e ' in Asteropseidae derives from the genitive singular root Asteropse-. We are indebted to Dr R. V. Melville for help with this nomenclatorial problem. RESTRICTION OF PORANIIDAE (ASTEROIDEA) 267 like growth gradients, the shortest longitudinal series adjoining the ambulacra proximally. This contrasts with Fell's 'inferred appearance' of the same species (1963, fig. nD), where minor differences in the sutures result in an asteropseid arrangement, conforming with his theories on the phylogeny of asteroids (Fig. i). If Spencer is proved correct, then Fell's growth gradient argument for crinoid ancestry of the Asterozoa is seriously undermined. REFERENCES CLARK, A. M. 1952. Some echinoderms from South Africa. Trans. R. Soc. S. Afr. 33 (2) : 193-221, 3 figs, i pi. 1967. Echinoderms from the Red Sea. Part 2. Bull. Sea Fish Res. Stn Israel 41 : 26- 58, 5 figs- CLARK, H. L. 1946. The Echinoderm fauna of Australia. Publs Carnegie Instn No. 566 : 567. DONS, C. 1936. Zoologische Notizen. 26. Pseudoporania stormi n. gen., n. sp. K. norske Vidensk. Selsk. Fork. 8 : 17-20, 4 figs. 1938. Zoologische Notizen. 35. Sphaeraster Berthae n. gen., n sp. 36. Sphaeraster Bjorlykkei n. sp. K. norske Vidensk. Selsk. Fork. 10 : 161-164, figs I-6 ; 165-168, figs 1-6. ECK, H. 1879. Bermerkungen zu den Mittheilungen des Herrn H. Pholig 'Aspidura ein meso- izoisches Ophiuriden-genus' und iiber die Lagerstatte der Ophiuren im Muschelkalke. Z. geol. Ges. 31 : 35-40. FELL, H. B. 1963. The phylogeny of sea-stars. Phil. Trans. R. Soc. B246 : 381-435, 19 figs, 2 pis. FISHER, W. K. 1908. Some necessary changes in the generic names of starfishes. Zool. Anz. 33 : 356~359- 1911. Asteroidea of the North Pacific and adjacent waters, i. Phanerozonia and Spinulosa. Bull. U.S. natn. Mus. 76 (i) : vi + 4i9, 122 pis. 1919. Starfishes of the Philippine Seas and adjacent waters. Bull. U.S. natn. Mus. 100(3) : 1-546, 156 pis. 1940. Asteroidea. Discovery Rep. 20 : 69-306, 23 pis. GRAY, J. E. 1840. A synopsis of the genera and species of the class Hypostoma (Asterias, Linn.). Ann. Mag. nat. Hist. 6 : 175-184 (Nov. ) ; 275-290 (Dec.). 1847. Descriptions of some new genera and species of Asteriadae. Proc. zool. Soc. Lond. 1847 : 72-83. (Also in : Ann. Mag. nat. Hist. 20 : 193-204.) MADSEN, F. J. 1959. On a new North Atlantic sea-star, Chondraster hermanni n. sp., with some remarks on related forms. Vidensk. Meddr dansk naturh. Foren. 121 : 153-160, 4 figs. MORTENSEN, T. 1933- Echinoderms of South Africa (Asteroidea and Ophiuroidea) . Vidensk. Meddr dansk naturh. Foren. 93 : 215-400, 91 figs, 12 pis. MULLER, J. & TROSCHEL, F. H. i84oa [No title.] Mber. Akad. Wiss. Berl. 1840 : 100-106 (April). i84ob. Ueber die Gattungen der Asterien. Arch. Naturgesch. 6 (i) : 318-326 (Sept. ?). 1842. System der Asteriden. xx+ 134 pp., 12 pis. Braunschweig. PERRIER, E. 1875. Revision de la collection de Stelldrides du Museum d'Histoire Naturelle de Paris. Paris. 384 pp. (Also in : Archs Zool. exp. gen. 4 (1875) : 265-450 ; 5 (1876) : i- 104, 209-309.) 1884. Memoire sur les Etoiles de Mer recueillies dans la Mer des Antilles et le Golfe de Mexique durant les expeditions de dragage faites sous la direction de M. Alexandre Agassiz. Nouv. Archs Mus. Hist. nat. Paris (2) 6 : 127-276, 10 pis. 1891. Echinodermes. i. Stellerides. Mission Sclent. Cap Horn 6. Zool. 1-198, 13 pis. 1894. Stellerides. Expeditions Scientifiques du Travailleur et du Talisman. 431 pp., 26 pis. Paris. 268 F. H. C. HOTCHKISS AND A. M. CLARK 1889. Asteroidea. Rep. scient. Results Voy. Challenger. Zool. 30 11-935, Early Palaeozoic starfish. Phil. Trans. R. Soc. 6235:87-129, 28 SLADEN, W. P. 118 pis. SPENCER, W. K. figs, 7 pis. & WRIGHT, C. W. 1966. Asterozoans. In : Moore, R. C. (ed.) Treatise on invertebrate paleontology. PtU. Echinodermata, 3 (i) Geological Society of America Inc. : University of Kansas Press. U4-Uio7, 89 figs. VERRILL, A. E. 1914. Monograph of the shallow-water starfishes of the North Pacific coast from the Arctic Ocean to California. Harriman Alaska Ser. 14 : 1-408, no pis. VIGUIER, C. 1879. Anatomic comparee du squelette des Stelle'rides. Archs Zool. exp. gin. 7 : 33-250, 12 pis. FREDERICK H. C. HOTCHKISS Division of Natural Sciences STATE UNIVERSITY OF NEW YORK COLLEGE AT PURCHASE P.O. Box 337 PURCHASE, NEW YORK 10577 U.S.A. AILSA M. CLARK Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 530 PLATE i Porania antarctica glabra Sladen. B.M. reg. no. 1948.3.16.408. Discovery Investigations St. 366, South Sandwich Islands (x i). Bull. By. Mus. nat. Hist. (Zool.) 30, 6 PLATE i 18 PLATE 2 Asteropsis carinifera (Lamarck). 1964.8.17.84. Red Sea (x i). Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 PLATE 2 PLATE 3 Petricia vernicina (Lamarck). 1963.4.19.6. Port Noarlunga, South Australia (x i). Bull. Br. Mus. nat. Hist. (Zool.) 30, 6 PLATE 3 A LIST OF SUPPLEMENTS TO THE ZOOLOGICAL SERIES OF THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) 1. KAY, E. ALISON. Marine Molluscs in the Cuming Collection British Museum (Natural History) described by William Harper Pease. Pp. 96 ; 14 Plates. 1965. (Out of Print.) 2. WHITEHEAD, P. J. P. The Clupeoid Fishes described by Lacepede, Cuvier and Valenciennes. Pp. 180 ; u Plates, 15 Text-figures. 1967. £4.80 3. TAYLOR, J. D., KENNEDY, W. J. & HALL, A. The Shell Structure and Mineralogy of the Bivalvia. Introduction. Nuculacea-Trigonacea. Pp. 125 ; 29 Plates, 77 Text-figures. 1969. £5.40. 4. HAYNES, J. R. Cardigan Bay Recent Foraminifera (Cruises of the R.V. Antur) 1962-1964. Pp. 245 ; 33 Plates, 47 Text-figures. 1973. £11.90. 5. WHITEHEAD, P. J. P. The Clupeoid Fishes of the Guianas. Pp. 227 ; 72 Text-figures. 1973. £10.65. 6. GREENWOOD, P. H. The Cichlid Fishes of Lake Victoria, East Africa : the Biology and Evolution of a Species Flock. Pp. 134 ; i Plate, 77 Text-figures. 1974. £3-75. Hardback edition £6. Printed in Great Britain by John Wright and Sons Ltd. at The Stonebridge Press, Bristol BS4 5NU 2 6 NOV J976 LIBRARY VARIATION IN EURASIAN OF THE GENUS CROCIDURA (INSECTIVORA : SORICIDAE) P. D. JENKINS BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 7 LONDON: 1976 VARIATION IN EURASIAN SHREWS OF THE GENUS CROCIDURA (INSECTIVORA:SORICIDAE) BY PAULINA D. JENKINS Pp 269-309 ; 14 Text-figures BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 7 LONDON: 1976 THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be completed within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30 No. 7 of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation Bull. Br. Mus. nat. Hist. (Zool.). ISSN 0007-1498 Trustees of the British Museum (Natural History), 1976 BRITISH MUSEUM (NATURAL HISTORY) Issued 25 November, 1976 Price {3.30 VARIATION IN EURASIAN SHREWS OF THE GENUS CROCIDURA (INSECTIVORA:SORICIDAE) By P. D. JENKINS CONTENTS Page SYNOPSIS ............ 271 INTRODUCTION ........... 271 MATERIALS ........... 272 METHODS ............ 274 CANONICAL VARIATE ANALYSIS ........ 276 IDENTIFICATION .......... 279 VARIATION AND SYSTEMATICS ........ 282 C. fuliginosa ........... 282 C. horsfieldi ........... 285 C. suaveolens ........... 286 C. zarudnyi ........... 289 C. russula ........... 291 C. dsinezumi ........... 295 C. attenuata . . . . . . . . . . . 295 C. leucodon ........... 297 C. lasiura ........... 301 OTHER SPECIES RECORDED FROM THE AREAS OF STUDY BUT NOT INCLUDED IN THE ANALYSIS .......... 3O2 ACKNOWLEDGEMENTS ......... 306 REFERENCES ........... 306 SYNOPSIS An investigation including the use of a canonical variate analysis is made into the relationships between various species of Crocidura occurring in Eurasia. The status of species and their geographical variation are examined and keys are provided to aid segregation of species. C. suaveolens is the most widespread species. C. zarudnyi is regarded as a distinct species showing some affinity to C. suaveolens and to Asian C. russula. C. russula is divisible into two main groups - Europe/ Algeria and western Asia. The latter group is close to some populations of C. suaveolens. The European /Algerian group shows some association with western Asian C. leucodon. The Japanese form, C. dsinezumi, while somewhat similar to some populations of C. suaveolens and Asian C. russula, is sufficiently distinct to retain specific status. C. leucodon is also divided into European and western Asian groups and the Iranian caspica is considered to be a subspecies of the latter group. The affinities of the western Asian group of C. leucodon and C. lasiura are discussed. C. fuliginosa trichura is assigned to C. attenuata. C. dracula is allocated to C. fuliginosa and some of the forms recorded from Indonesia are considered to belong to this species. C. horsfieldi is compared with C. suaveolens but retained as a distinct species. Short notes are made on other species occurring in the area. INTRODUCTION WHITE-TOOTHED shrews of the genus Crocidura occur mainly southwards from latitude 53°N in the Palaearctic, Oriental and Ethiopian regions. This report is concerned with those species from the first two regions. 19* 272 P. D. JENKINS Ellerman & Morrison-Scott (1966) recognized only fourteen species amongst the forty four species names recorded from the Palaearctic and Indian regions. Chasen (1940) listed twenty nine species names from the Malaysian subregion of the Oriental region. It is possible that the same species occur under different names in different areas, so comparison over the entire area was considered necessary. New forms have frequently been described from single specimens but only rarely figured and with inadequate descriptions. Information on colour of pelage, external dimensions and a few skull measurements does not seem to provide adequate diagnoses ; while diagnostic characters that vary from species to species, yet are intraspecifically constant, are distinctly lacking in this genus. This report describes geographical variation between populations occurring throughout Eurasia. A canonical variate analysis has been used to investigate relationships between populations. This type of analysis allows metrical characters of a large number of samples to be handled simultaneously but is limited to those specimens possessing all the necessary characters. The results have been correlated with all other available information and some changes to the existing taxonomy are suggested. MATERIALS The collections of the British Museum (Natural History) (BMNH) contain 740 specimens from Eurasia. All of these were examined and, for the sake of completeness, specimens of North African C. russula and C. suaveolens (which are mainly distributed in Europe and Asia) were included. In addition the following specimens from other institutions have been examined : Harrison Zoological Museum, Sevenoaks : C. russula - 28, C. russula caspica - 3, C. leucodon judaica - 2, C. lasia - i ; United States National Museum : C. zarudnyi - 9, C. pergrisea - 2 ; Naturhistorisches Museum, Vienna : C. pergrisea arispa - i. C. olivieri, C. religiosa and C. floweri from Egypt have been excluded because they are confined to Africa and are readily distinguished from Eurasian species. Since the BMNH collections do not contain any of the eight species listed by Taylor (1934) from the Philippine Islands these have also been excluded. For the canonical variate analysis (CVA) the number of available specimens was reduced to 526, since the method demanded specimens complete for all of the characters included. In the CVA the group of specimens from each locality is referred to by the term operational taxonomic unit (OTU) followed by the number of the group (see Table i and Fig. i). TABLE i Populations entered in the canonical variate analysis No. of OTU Locality specimens Current species name 1 Isles of Scilly 10 C. suaveolens cassiteridum 2 Jersey and Sark 9 C. suaveolens 3 Guernsey and Alderney 15 C. russula peta VARIATION IN EURASIAN CROCIDURA 273 TABLE i (Cont.) No. of OTU Locality Specimens 4 France ii 5 France J4 6 Spain 7 7 Portugal 8 8 Algeria 16 9 Algeria 4 10 Germany, Belgium and 17 Holland ii Germany 9 12 Switzerland 8 13 Switzerland 19 14 Switzerland 8 15 Sicily 5 16 Sardinia 9 17 Corsica ii 18 Rumania and Hungary 5 19 Yugoslavia 15 20 Yugoslavia 21 21 Greece 8 22 Turkey ii 23 Turkey 15 24 Lebanon ii 25 Israel 16 26 Lebanon and Israel 7 27 Iran 7 28 Afghanistan 5 29 Pakistan 8 30 Russian Turkestan 18 31 Kashmir 6 32 Punjab ii 33 Sri Lanka J4 34 Darjeeling M 35 Bhutan 7 36 Assam 20 37 Burma 8 38 Malaya 16 39 Borneo 7 40 Christmas Island 10 (io°3i'S. io5°33'E) 41 Yunnan 8 42 Yunnan 4 43 N. Vietnam 20 44 China 9 45 Korea 16 46 Korea 15 47 Japan 14 Current species name C. russula russula C. leucodon leucodon C. russula pulchra C. russula pulchra C. russula agilis C. suaveolens whitakeri C. russula russula C. leucodon leucodon C. suaveolens mimula C. russula russula C. leucodon leucodon C. sicula C. russula ichnusae C. russula cyrnensis C. suaveolens mimula C. suaveolens mimula C. leucodon C. suaveolens mimula C. russula monacha C. leucodon lasia C. russula C. russula C. leucodon judaica C. russula caspica unnamed C. zarudnyi C. suaveolens ilensis C. russula pullata unnamed C. horsfieldi C. attenuata rubricosa C. attenuata rubricosa C. attenuata rubricosa C. attenuata C. malayana C. fuliginosa baluensis C. fuliginosa trichura C. dracula C. suaveolens C. dracula C. attenuata attenuata C. suaveolens shantungensis C. lasiura C. russula dsinezumi 274 P. D. JENKINS FIG. i. Distribution map of samples entered in the canonical variate analysis. METHODS Characters were taken exclusively from skins and skulls because there are very few shrew skeletons in the BMNH collections, while the paucity and age of alcoholic specimens preclude the use of anatomical characters such as those of the male reproductive tract which have been used successfully by other authors (Vinogradov, 1958 ; Martin, 1967). The following characters were examined with the abbrevia- tions used in the text in brackets. Head and body length (HB) Tail length (TL) Hindfoot length Ear length Weight Colour of pelage Condylobasal length (CBL) Length of upper toothrow (UTL) Combined length of upper incisor and uni- cuspids Lingual length of upper unicuspids Labial length of upper unicuspids at cingula (LLU) Width across maxillae at level of second molar (MB) Height of rostrum Lacrymal breadth Interorbital breadth (IB) Postglenoid breadth (PB) Braincase breadth (BB) Height of braincase Length of mandible (excluding incisor) Height of mandible at coronoid process Length of mandibular toothrow (excluding incisor) Shape of teeth VARIATION IN EURASIAN CROCIDURA 275 Skin measurements were taken from collectors' notes on the specimen labels, which are notoriously fallible because they are difficult to measure accurately and consistently and the measuring technique varies from one collector to another. However, skin measurements are still useful as long as these disadvantages are taken into account and since they have been extensively used in the taxonomy of this group their inclusion was considered necessary. The effect of using skin measurements was checked by running the CVA twice, first including head and body, tail and hindfoot length and secondly omitting these three characters. The results were found to be comparable so only the former analysis is described here. The toothrow and anterior part of the skull are less frequently damaged than the posterior. Since the CVA requires possession of all characters by each specimen either the number of specimens or number of characters had to be reduced ; the latter course was considered preferable. The excluded characters were examined and incorporated with the results of the CVA at a later stage. The following characters were selected for the CVA and found to show little correlation with each other (see Table 2) : 1. Length of upper toothrow ; 2. Combined length of upper incisor and unicuspids ; 3. Lingual length of upper unicuspids ; 4. Labial length of upper unicuspids at cingula ; 5. Width across maxillae at level of second molar ; 6. Head and body length ; 7. Tail length ; 8. Hindfoot length. TABLE 2 Correlation matrix of characters used in the canonical variate analysis Character No. Length of upper toothrow (i) i-oo Combined length of upper incisor (2) 0-43 i-oo and unicuspids Lingual length of upper unicuspids (3) 0-60 0-40 i-oo Labial length of upper unicuspids (4) 0-55 0-38 0-60 i-oo at cingula Width of maxillae at level of second (5) 0-50 0-22 0-34 0-32 i-oo molar Head and body length (6) 0-20 0-09 0-12 0-16 0-27 i-oo Tail length (7) 0-35 0-08 0-28 0-27 0-24 0-32 i-oo Hindfoot length (8) 0-33 0-15 0-24 0-24 0-29 0-30 0-37 i-oo (i) (2) (3) (4) (5) (6) (7) (8) The CVA programs used were part of the CLASP package provided by J. C. Gower, Statistics Department, Rothamsted Experimental Station. The data, which may be thought of as a 'plot' in eight dimensions, are translated into visible form by the following treatment. The CVA program seeks a plane in this eight-dimensional space which, when the group means are projected on to the plane, best reproduces 276 P. D. JENKINS the Mahalanobis' distances between groups. The Mahalanobis' generalized distances (D2) are akin to phenetic distances but take some account of intraspecific variation and correlation of characters (see Sneath & Sokal, 1973). If the variation between the projected group means is almost as large as the total variation in eight dimensions then the representation on the plane will be a good one. In the first analysis (a) the variation on the plane was 84% of the total and therefore the plot of group means on this plane gives a fairly accurate overall picture of the relationships between them. The following relevant information is produced by the program : (i) Correlation matrix between characters for all specimens. (2) Distance matrix (D2) or Mahalanobis' distances which are an index of dissimilarity between OTUs (see Table 8). CANONICAL VARIATE ANALYSIS (a) FIRST ANALYSIS OF ALL OTUs The results of the first analysis are summarized in Fig. 2, in which OTUs are plotted on a plane which accounts for 84% of the variation, suggesting a reasonable representation of the actual relationships. Circles are calculated to include 90% of the individual specimens that combine to give the group mean, while the boundaries of currently recognized species groups are indicated by lines of differing texture (see key on figure). OTUs Malaya (38), Borneo (39), Yunnan (41) and N. Vietnam (40) overlap but are well separated from all others and may be regarded as a distinct species, herein- after referred to as C. fuliginosa. The remaining groups are disposed in a Y-shaped pattern, those at the extreme of each limb being clearly distinct. (1) Top right - Darjeeling (34), Bhutan (35), Assam (36), China (44) correspond with C. attenuata, and Christmas Island specimens (40), C. fuliginosa trichura, are associated with this group. Burma (37) is also usually thought to belong to this species and is positioned closest to it despite showing no overlap at the 90% level. (2) Lower centre - Isles of Scilly (i), Jersey and Sark (2), Rumania and Hungary (18), Yugoslavia (19), Greece (21), Russian Turkestan (30), Yunnan (42) and Korea (45) correspond with the classic concept of C. suaveolens. Showing overlap with this group is Pakistan (29) currently regarded as a distinct species, C. zarudnyi. Sri Lanka (33), C. horsfieldi, lies close to this group but does not overlap with it. C. dsinezumi from Japan (47) overlaps with C. suaveolens, C. russula and C. zarudnyi. (3) The remainder form a central group extending to the top left which corresponds with the russula-leucodon complex, with leucodon falling at the extreme left. Those in the upper portion of this group include specimens from Turkey (23) and also Israel and Lebanon (26) and Iran (27) whose affinities are doubtful. The Korean OTU (46), C. lasiura, overlaps with the group at the extreme upper left. (b) SECOND ANALYSIS OF 42 OTUs (5 OMITTED) The analysis was repeated but five OTUs were omitted to improve resolution (see Fig. 3). Those excluded were Malaya (38), Borneo (39), Yunnan (41) and VARIATION IN EURASIAN CROCIDURA 277 FIG. 2. First analysis of all OTUs. C.fuliginosa - upper centre of figure ; C. russula - central group (stippled) ; C. leucodon - extreme left of central group ; C. attenuata - extreme right of central group ; C. suaveolens - lower centre of central group ; other species currently regarded as distinct - broken circles. P. D. JENKINS -5- — T 1 1 1 1 1 1 T 0 5 FIG. 3. Second analysis of 42 OTUs. C. russula - central group (stippled) ; C. leucodon - upper left of central group ; C. attenuata - lower right of central group ; C. suaveolens - lower left of central group ; other species currently regarded as distinct - broken circles. VARIATION IN EURASIAN CROCIDURA 279 N. Vietnam (42) which form a distinct group, C. fuliginosa, and also Burma (37) which is separated from any other OTU. The plane in this analysis includes 82% of the variation. The species groups still overlap but to a lesser extent. (1) Lower right - OTUs Darjeeling (34), Bhutan (35), Assam (36), China (44) form the loosely knit C. attenuata, with which Christmas Island (40) is associated. (2) Lower left - OTUs overlapping in the suaveolens group remain as before. C. zarudnyi overlaps with this group and C. dsinezumi overlaps with both groups and also with C. russula. (3) The russula- leucodon complex is better spaced in this figure. C. russula falls roughly into two subgroups with most European OTUs in the upper part of the figure and Asian ones occurring lower down. C. leucodon lies at the top left. IDENTIFICATION All available information including that from the previous section is assembled here and correlated with the existing taxonomic groupings. The species recognized are : Crocidura fuliginosa - including malayana, baluensis and dracula. Crocidura horsfieldi Crocidura suaveolens Crocidura zarudnyi Crocidura russula - two groups Crocidura dsinezumi Crocidura attenuata - including C. fuliginosa trichura Crocidura leucodon - two groups Crocidura lasiura In any one locality where two or more species occur they are usually easy to separate. An exception to this is found in Switzerland where three species occur. C. suaveolens is readily distinguished but C. russula and C. leucodon are only clearly separable on the basis of pelage colour. In the majority of species some populations show overlap with at least one other species and therefore an exclusive diagnosis covering the entire region is impossible. Even when the range of the genus is divided into 'European', 'eastern Asian' and an intermediate zone from Turkey east to Sri Lanka, the construction of keys presents considerable difficulties. For example, the separation of fuliginosa from other species of Crocidura depends mainly on skull length. Although the key is somewhat unsatisfactory because of the overlap in size, the degree of separation is adequate in most cases, as may be seen in Fig. 4. A similar situation obtains in other examples of overlap. Thus while the three keys given below are not a completely accurate identification guide, they may be used to discriminate with a reasonable degree of confidence between the species from a region, particularly when a series of specimens is available. 280 P. D. JENKINS C.suaveolens C.horslieldi C.dsinezumi C.russula C.attenuata C.lasiura C.fuliginosa 15-0 2C.O -o condylobasal length FIG. 4. Condylobasal length in species of Crocidura from eastern Asia, showing mean (vertical bar), range (horizontal line), one and two standard deviations (rectangles). Confirmation of identification should be sought by reference to the additional data provided in the text. 1. KEY TO THE EUROPEAN SPECIES OF CROCIDURA 1 Bicoloured, pale ventral surface sharply differentiated from dark dorsum along flanks . ......... C. leucodon - No sharp differentiation between dorsal and ventral colour ..... 2 2 Average smaller, labial length of upper unicuspids up to 2-0 mm . . C. suaveolens - Average larger, labial length of upper unicuspids usually over 2-0 mm . C. russula Note, (a) Where C. suaveolens and russula are sympatric, they may be distinguished on the basis of size and usually by differences in the shape of the large upper premolar. (b) C. russula from Corsica may be distinguished from those from elsewhere in Europe by the dis- tinctive shape of the large upper premolar (see text and Fig. 5), and from C. suaveolens only by a com- bination of several characters. However, C. suaveolens is not recorded from Corsica. 2. KEY TO THE SPECIES OF CROCIDURA OCCURRING FROM TURKEY IN THE WEST TO SRI LANKA IN THE EAST i Bicoloured, pale ventral colour differentiated from dark dorsal colour along flanks or, when unicoloured, size large (upper toothrow over 8-8 mm, width across maxillae at M2 over 6-0 mm) ......... C. leucodon VARIATION IN EURASIAN CROCIDURA 281 (a) (b) (c) (d) FIG. 5. Large upper premolar of European species of Crocidura. (a) C. suaveolens - Austria ; (b) C. russula - Corsica ; (c) C. russula - France ; (d) C. leucodon - France. No sharp differentiation between dorsal and ventral colour ; smaller (upper toothrow length less than 8-8 mm, width across maxillae at M2 less than 6-0 mm . . 2 2 Lingual region of large upper premolar relatively narrow and lobed (see Fig. 6) ; labial length of upper unicuspids greater than 1-8 mm . . . C. russula Premolar not so shaped, labial length of upper unicuspids less than i -9 mm . . 3 3 Sri Lanka. Skull small and narrow, width across maxillae at M? less than 5-1 mm. Ratio of tail length to upper toothrow length 6-5-7-5 : i . . . C. horsfieldi - Other localities. Width of maxillae at M2 greater than 5-0 mm. Ratio of tail length to upper toothrow length 3-4-5-2 : i (suaveolens) or if greater (4-8-7-1 : i) colour of pelage very pale (zarudnyi) ........ C. suaveolens C. zarudnyi Note, (a) The separation of C. russula and the unicoloured C. leucodon caspica from Iran is not complete as there is a small overlap in size of the characters used. However, most specimens seen can be identified by the key above. (b) C. suaveolens and C. zarudnyi are difficult to distinguish, see discussion in text under C. zarudnyi. FIG. 6. Large upper premolar of species of Crocidura occurring from Turkey in the west to Sri Lanka in the east, (a) C. suaveolens - Russian Turkestan ; (b) C. russula - Turkey ; (c) C. leucodon - Turkey ; (d) C. zarudnyi - Pakistan ; (e) C. horsfieldi - Sri Lanka. 282 3- i P. D. JENKINS KEY TO EASTERN ASIAN SPECIES OF CROCID URA Large, condylobasal length over 21 -o mm ...... C.fuliginosa - Smaller, condylobasal length less than 21-6 mm, where greater than 21-0 mm, tail 48-58% of head and body length (lasiura) or 59-92% (fuliginosa) . Only one specimen of attenuata has a condylobasal length greater than 21-0 mm - see Fig. 4 and text .............. 2 2 Upper toothrow length 9-0-10-2 mm, tail length 34-49 mm, 48-58% of head and body length, ear margins densely furred . . . . . . . C. lasiura - Upper toothrow length 7-8-9-8 mm, tail length 50-88 mm, 69-108% of head and body length, ear margins not densely furred ..... C. attenuata - Upper toothrow length 7-4-8-8 mm, tail length 37-51 mm, 54-76% of head and body length, ear margins not densely furred ........ 3 3 Width of braincase over 8-8 mm ....... C. russula - Width of braincase usually less than 8-8 mm . . . . . . . 4 4 Japanese, width of braincase 8-1-8-8 mm, condylobasal length over 16-8 mm C. dsinezumi - Elsewhere, width of braincase less than 8-5 mm (if from Tsushima Islands or Korea, width of braincase less than 8-2 mm and condylobasal length less than 16-9 mm) 5 5 Ratio of tail length to upper toothrow length less than 5-8 : i . C. suaveolens - Ratio of tail length to upper toothrow length over 5-7:1 . . . C. horsfleldi Note, (a) Separation of C. russula from C. attenuata depends on a combination of characters, see text, (b) It is possible to distinguish C. dsinezumi from C. suaveolens occurring in nearby areas, see text. C. dsinezumi is geographically separated from C. russula and C. horsfieldi and a combination of characters serve to distinguish these species. (e) FIG. 7. Large upper premolar of Crocidura from eastern Asia, (a) C. suaveolens - Korea ; (b) C. russula - Punjab ; (c) C. attenuata - Assam ; (d) C. lasiura - Korea ; (e) C. dsinezumi - Japan ; (f) C. fuliginosa - N. Vietnam. VARIATION AND SYSTEMATICS Crocidura fuliginosa (Blyth, 1855) This is the only group that is completely distinct from all others. It includes three forms previously regarded as separate species but here associated with C. VARIATION IN EURASIAN CROCIDURA 283 fuliginosa from Burma. These are C. malayana from Malaya (38), C. baluensis from Borneo (39) and C. dracula from Yunnan (41) and N. Vietnam (43). Populations from Yunnan and N. Vietnam are very similar to each other and are currently known as C. dracula. They have a D2 value of 1-5 which is very low and reflects their conspecificity. These populations resemble specimens from Borneo and Malaya which, with a D2 value between them of 2-69, are also very similar. The range of D2 values within the group goes up to 4-3 but this is still fairly low when the geographical distance between populations and ecological barriers are taken into consideration, see distribution map (Fig. 8). FIG. 8. Distribution of C. fuliginosa. Broken lines - exact distribution uncertain. The results of the CVA may be correlated with characters not employed in the numerical analysis. This group contains some of the largest specimens in the genus. Those from Borneo are the largest while the greatest size range occurs in Malaya. Populations from Yunnan and N. Vietnam, are more similar in appearance and size to each other than to populations from Malaya or Borneo. Size range is given in Table 6. A large number of distinct species have been described from many of the separate islands off the Malay Peninsula. The BMNH houses most of the holotypes of these, which have been compared with mainland specimens and those from Borneo. The 284 P. D. JENKINS holotypes fall within the range of this group. Some of these island forms may not even be distinct subspecies but no definite conclusions can be based on the few specimens available. Unfortunately I have not seen the holotype of C. fuliginosa which was collected from Schwe Gyen, Pegu, Burma, and is lodged in the Calcutta Museum. Banks (1931) recorded it as the commonest lowland shrew in Borneo and Chasen (1940) accepted a brown form in the lowlands of Malaya as fuliginosa and a darker form as malayana. The name C. fuliginosa is the subject of some confusion. Blyth's (1855) original description is rather scanty and there is some doubt whether the subsequent description by Anderson (1881) refers to the same specimen, especially as different terminology is used for measurements. The statement by Lindsay (1929) '. . . . the specific name of fuliginosus which Blyth plainly applied to a Suncus' is erroneous since Suncus is defined as possessing four upper unicuspids. Medway (1965) has attempted to elucidate the situation but there is still some doubt about the identity of the holotype, particularly as some label mixing may have occurred in the past. This report confirms the view of Medway (1965) who allocated Malayan specimens of malayana and Bornean foetida, kelabit and baluensis to C. fuliginosa. This name is also applicable to the large specimens from the offshore islands of Malaysia as well as to specimens of dracula from Yunnan and N. Vietnam. C. fuliginosa is recorded from S. Vietnam by Van Peenan, Ryan & Light (1969) which suggests a fairly continuous distribution from Yunnan in the north, lower Burma, N. and S. Vietnam to the Malay Peninsula and Borneo (see Fig. 8). A limited number of specimens indicate that this species is also present on the islands of Sumatra, Java and Sulawesi. The following subspecific groups are suggested in addition to C. f. fuliginosa from Burma : Crocidura fuliginosa malayana Robinson and Kloss, 1911. Mainland of Malaya. Probable synonyms of C./. malayana from the offshore islands of the Malay Peninsula are : Crocidura aoris Robinson, 1912. Aor Island. Crocidura klossii Robinson, 1912. Great Redang Island. Crocidura negligens Robinson & Kloss, 1914. Samui Island. Crocidura maporensis Robinson & Kloss, 1916. Mapor Island. Crocidura gravida Kloss, 1917. Dayang Bunting Island. Crocidura tionis Kloss, 1917. Tioman Island. Crocidura aagaardi Kloss, 1917. Bang Nara, Patani, southern Thailand. Crocidura fuliginosa baluensis Thomas, 1898. Borneo. Probable synonyms are : Crocidura foetida Peters, 1870. Borneo. This name would predate C. f. baluensis as the correct subspecific name. Crocidura fuliginosa kelabit Medway, 1963. Bario, Baram District, Sarawak. VARIATION IN EURASIAN CROCIDURA 285 Crocidura fuliginosa dracula Thomas, 1912. Yunnan. Crocidura praedax Thomas, 1923. Likiang Valley, Central Yunnan. Crocidura grisescens Howell, 1928. Kuatun, Fokien, South-eastern China (listed as a synonym of C. dracula by Ellerman & Morrison- Scott, 1966). Crocidura dracula mansumensis Carter, 1942. Mansum, northern Burma. Other species occurring in the same area as C. fuliginosa, but readily distinguished by their small size, are C. suaveolens in Yunnan and N. Vietnam (condylobasal length 15-2-17-5 mm) and C. monticola in Borneo (condylobasal length of one specimen only 15-2 mm). Condylobasal length of C. fuliginosa is over 21.0 mm. C. attenuata is also sympatric at least in the northern part of the range but is usually distinguish- able on the basis of small size. While there are no members of both species from the same area in the BMNH collections, specimens from relatively close areas, such as fuliginosa from Yunnan and N. Vietnam and Chinese attenuata, are distinct. Overlap in size occurs in some large specimens of attenuata from Assam and Burma and a few small fuliginosa from Malaya. Crocidura horsfieldi (Tomes, 1856) Only one OTU of this species, Sri Lanka (33), was entered in the CVA. It is rather similar to C. suaveolens but can be distinguished by the following features : the skull is relatively short and narrow and in these proportions it is most similar to populations of C. suaveolens from Tsushima Island (Japan), N. Vietnam and Korea but consider- ably smaller than the remaining populations (see Table 3). The tail is proportion- ately much longer than in C. suaveolens, the ratio of tail length to upper toothrow length ranging from 3-4 to 6-1 : i in the latter and from 6-5 to 7-5 : I in C. horsfieldi. The upper premolar is small and comparatively narrow (see Fig. 6) . The distribution of the nominate form and the other subspecies of C. horsfieldi listed by Ellerman & Morrison-Scott (1966) is given in Fig. 9. Of these the holotype of C. h. indochinensis, in the BMNH collections, agrees very well with specimens of C. horsfieldi from Sri Lanka and there seems little doubt that it is correctly assigned to this species. There is also a single specimen of C. watasei and this too is very similar to Sri Lanka specimens ; Imaizumi (1970) gives the Japanese distribution of this subspecies. Two skulls from Taiwan are larger than Sri Lanka specimens (see Table 3). Another subspecies, C. h. wuchihensis, described from Hainan, differs slightly from specimens from Sri Lanka (condylobasal length 15-5-15-7 mm, skull width 7-8 mm, tail 67% of head and body length). The subspecies recorded are : C. h. horsfieldi (Tomes, 1856). Sri Lanka. C. h. indochinensis Robinson and Kloss, 1922. Dalat, S. Annam. C. h. watasei Kuroda, 1924. Liukiu Islands. C. h. tadae Tokuda and Kano, 1936. Koto-sho, island E. of Taiwan. C. h. wuchihensis Wang, 1966. Mt Wuchih, Hainan Island. The only other species recorded from Sri Lanka is C. miya Phillips, 1929 which is a much larger shrew, condylobasal length of holotype 19-7 mm, upper toothrow 286 P. D. JENKINS length 8-7 mm, braincase damaged but width across maxilla at second molar 5-9 mm (see p. 302). TABLE 3 Size range of C. horsfieldi, C. suaveolens, C. russula, C. zarudnyi and C. dsinezumi C. horsfieldi Sri Lanka Taiwan C suaveolens Korea, Tsushima, N. Vietnam Europe, Algeria, Russian Turkestan, Yunnan C. russula Asia Europe C . zarudnyi Pakistan, Punjab, Turkey, Iran C. dsinezumi Japan Upper Width of Condylobasal toothrow maxillae at M2, Braincase length, mm length, mm mm breadth, mm 16-2-17-2 6-8-7-4 4-8-5-1 7-4-7-8 x 16-60 X7-05 x 5-00 x 7-60 17-8 7-5 and 8-0 5-5 8-5 15-2-16-9 6-7-7-7 4-7-5-3 7-0-8-2 x 16-03 f 7-17 x 4-98 X7-74 15-7-18-1 6-9-8-4 4-8-5-8 7-7-8-8 x 16-89 x 7-59 x 5-28 x 8-1 I7-5-I9-5 7-6-8-8 5-2-6-0 8-4-9-4 x 18-39 x 8-28 X5-65 x 8-91 17-5-20-1 7-6-9-2 5-4-6-5 8-5-9-5 x 18-79 x 8-48 x5-89 x8-97 16-1-18-8 7-1-8-3 S-o-5-5 7-8-8-5 x 17-69 X7-78 X5-3Q x8-25 16-8-18-4 7-4-8-1 5-1-5-9 8-1-8-9 x 16-03 x 7-82 X5-5Q x8-53 Crocidura suaveolens (Pallas, 1811) The following OTUs are included in this species : Isles of Scilly (i), Jersey and Sark (2), Algeria (9), Switzerland (12), Rumania and Hungary (18), Yugoslavia (19), Greece (21), Russian Turkestan (30), Yunnan (42) and Korea (45). The suaveolens group has a very large distributional range but geographical variation is not very pronounced and most Mahalanobis' distances are corre- spondingly low, varying from 2 to 3. The European group of Switzerland (12), Rumania and Hungary (18), Yugoslavia (19) and Greece (21) have low D2 values of 2'03-2-87. The Algerian, Russian Turkestan and Yunnan populations are similar in size to European ones ; the remaining Asian populations from Korea, Tsushima (Japan) and N. Vietnam are on average smaller, see Table 3. In this species there is rather more colour variation than in most of the others. Most are greyish-brown often with a slightly paler venter but certain populations, notably those occurring in arid habitats such as Russian Turkestan, Algeria and Israel, have a strikingly pale grey or fawn dorsum and a still paler venter. Another character which is probably ecologically linked is the densely furred ear margins which distinguish Korean specimens (though nearby specimens from Tsushima, Japan, lack this character) and also specimens from Russian Turkestan, especially those from Semiretchensk. In Korea this character may be subject to a certain amount of seasonal variation ; the ears of specimens in summer pelage in VARIATION IN EURASIAN CROCIDURA 287 C.suaveolens FIG. 9. Distribution of C. suaveolens, C. zarudnyi and C. horsfieldi. distribution uncertain. Broken lines - exact August, September and early October are only slightly haired, while by late November, December and January specimens have winter pelage and densely furred ears. Geographical proximity does not always correspond with low values of D2, especially where ecological barriers are involved. For example, island populations such as the Isles of Scilly (i) and Jersey and Sark (2) are relatively close to each other but the D2 value is 3-15. Specimens from the Isles of Scilly are most similar to those from Yugoslavia (19), with a D2 value of 1-96, while those from Jersey and Sark are most similar to Pakistan (29) specimens of C. zarudnyi with a D2 value of 2-94. Delany & Healy (1966), in their study of Crocidura of the Channel Islands and the Isles of Scilly, also found that populations from Jersey and Sark can be distin- guished from each other and that Channel Island populations are very distinct from those from the Isles of Scilly. In summary, European mainland populations are generally more homogeneous than the island populations, the Algerian or the Asian populations which are sampled from well-separated areas. However, despite this geographical variation there is little doubt that the populations are truly representatives of one very widespread species probably with an almost continuous distribution over its range (see Fig. 9). 288 P. D. JENKINS Of the subspecies listed from the Palaearctic and Indian region by Ellerman & Morrison-Scott (1966), the U.S.S.R. by Gureev (1971), China by Allen (1938) (listed under C. ilensis) and Japan by Imaizumi (1970), the following have been examined : C. s. mimula Miller, igoib. Western Europe (12, 18, 19, 21). C. s. cassiteridum Hinton, 1924. Isles of Scilly (i). C. s. whitakeri de Winton, 1897. Morocco, Algeria (9). C. s. ilensis Miller, igoic. Russian Turkestan to Mongolia (30). C. s. shantungensis Miller, I90ic. Korea, Tsushima Islands (Japan), China (45). Also samples from Jersey and Sark (2) and Yunnan (42). Mahalanobis' distances between some populations of C. suaveolens (Isles of Scilly (i), Yugoslavia (19), Greece (21), Russian Turkestan (30) and Yunnan (42)) 9-0- 8-0- x X X X X O 9 O O O T Y Y O 80 9-0 upper toothrow length FIG. 10. Comparison of skull size. C. russula (Asia and Corsica) • ; C. suaveolens (Isles of Scilly, Greece, Russian Turkestan, Yunnan) T ; C. dsinezumi x ; C. zarudnyi O- VARIATION IN EURASIAN CROCIDURA 289 and others of the Asian subgroup of russula (Lebanon (24), Israel (25), Afghanistan (28) and Punjab (32) and also Corsica (17)) range from 2-25 to 5-48. Some of these are fairly low but since the sample populations are geographically well separated their similarity is unlikely to reflect any true relationship. Yunnan (42) , for example, has D2 values under 3-0 with Afghanistan (28), Corsica (17), Punjab (32), Lebanon (24) and Israel (25) ; Afghanistan has D2 values under 3.0 with the Isles of Scilly (i), Russian Turkestan (30) and Yunnan (42). Compared with Asian and Corsican russula these populations of suaveolens have somewhat smaller skulls (see Fig. 10 and Table 3) and shorter tails (TL 27-48 mm, x 35-3 mm ; in the Asian and Corsican russula TL 36-52 mm, x 44-79 mm). Richter (1970) decided to treat the entire species of C. suaveolens as a third sub- specific group of C. russula, the other two being russula and gueldenstaedti. He postulated that the suaveolens subspecies group is merely a 'steppe form' of the gueldenstaedti subspecies group and that suaveolens has only secondarily come to inhabit the area occupied by the russula subspecies group in western Europe. While it is true that some populations of suaveolens mentioned above are similar to some members of Richter's gueldenstaedti subspecies group, it is possible to distinguish the two species where they occur together. Furthermore, there is usually no difficulty in distinguishing suaveolens from the subspecies that Richter places in the russula subspecies group, especially where they are sympatric, so C. suaveolens should be treated as a separate species. Crocidura zarudnyi Ognev, 1928 Crocidura pergrisea Miller, 1913 One OTU of C. zarudnyi from Pakistan (29) was entered in the CVA but several specimens from other localities were also examined. Because only two specimens of C. pergrisea were seen, they were not placed in the CVA but they have been examined and are briefly commented on here. Specimens from Pakistan are currently regarded either as a distinct species, C. zarudnyi Ognev, 1928, type locality Baluchistan border (see Hassinger, 1970 ; Spitzenberger, 1971), or as a subspecies of C. pergrisea Miller, 1913 from Baltistan (see Ellerman & Morrison-Scott, 1966). The Pakistan (29) specimens are geo- graphically fairly close to specimens of C. suaveolens from Russian Turkestan (30) and to Asian russula from Afghanistan (28) and Punjab (32), although they are probably ecologically isolated by the rocky, desert habitat and the surrounding mountainous terrain. The D2 values between Pakistan (29) and Punjab (32) and Israel (25) are fairly low, 3-5, but the Pakistan specimens are most similar to those of C. suaveolens from Jersey and Sark (2) with a D2 value of 2-94. Despite the similarity to various populations of C. suaveolens from Greece, Russian Turkestan, Yunnan, the Channel Islands and the Isles of Scilly, the only relevant comparison is with the Russian Turkestan specimens of C. suaveolens which have shorter tails on average (TL 27-40 mm, x 32-2 mm ; in C. zarudnyi 36-57 mm, x 49-2 mm). The shape of the upper premolar is similar to that of specimens of Asian C. russula, though it is slightly smaller (see Fig. 6). 2QO P. D. JENKINS Miller (1913) described four specimens from Skoro Loomba, Shigar, Baltistan (2900 m), giving them the name C. pergrisea. Ognev (1928) first used the name C. zarudnyi for a new species which he had formerly described under a preoccupied name (1921). This new species, represented by one specimen, was collected in East Iran on the Baluchistan border. Ellerman & Morrison-Scott (1966) examined three specimens from Baluchistan which they believed to be zarudnyi and placed this as a subspecies of pergrisea. Lay (1967) allocated to C. pergrisea six specimens from Iran, which Hassinger (1970) re-identified as C. zarudnyi. Hassinger made a preliminary study of the C. zarudnyi- pergrisea group and concluded that they were distinct species. He also described a new subspecies, C. zarudnyi streetorum, from Afghanistan. Richter (1970) tentatively assigned both zarudnyi and pergrisea to the subspecies group gueldenstaedti of C. russula. Spitzenberger (1971) gave measurements of three subspecies of C. pergrisea (the nominate form C. p. pergrisea, C. p. serezkeyensis Laptev, 1929 from the Pamirs and a new subspecies from Turkey, C. p. arispd) as well as C. zarudnyi and distinguished them from both C. russula and C. suaveolens by the light colour of the pelage and the relatively long tail. Gureev (1971) also recorded C. zarudnyi as a separate species from C. pergrisea. Hassinger (1973) amplified his previous discussion by comparing Afghan specimens with other species, still concluding that C. pergrisea and C. zarudnyi are two separate species. He distinguished C. zarudnyi from C. russula by its smaller size and from both C. russula and C. suaveolens by the relatively long tail and pale coloration. The habitat of C. zarudnyi in Afghanistan is reported to be drier than that of either C. russula or C. suaveolens. TABLE 4 Comparison of various samples of C. zarudnyi with C. pergrisea C. zarudnyi holotype 18-8 C. zarudnyi Pakistan 16-1-18-7 n = ii x 17-6 C. zarudnyi Iran n = 2 !7'4» 18-7 C. zarudnyi Punjab n = i C. pergrisea arispa holotype Turkey 17-7 C. p. pergrisea Baltistan original series 19-0- 19-4 C. p. pergrisea Baltistan n = 2 19-2 Upper Condylobasal toothrow length length mm mm 8-3 7-15-8-2 x 7-8 7-8, 7-9 7'5 7'5 8-6 8-4 Source Length of when not Width of mandible- measured braincase excluding Ix personally 8-3 Ognev (1928) 8-7-9-2 x 9-0 8-0, 8-3 9-0, 9-2 8-9 8-25 9-0 8-8-8-9 Miller (1913) 8-8 9-6, 9-7 VARIATION IN EURASIAN CROCIDURA 291 Table 4 shows that Baltistan specimens of C. p. pergrisea (two specimens measured personally plus measurements from the original description) are distinctly larger in most characters than all populations of C. zarudnyi. On these criteria the holotype of C. p. arispa from Turkey should be placed in the latter group as C. zarudnyi arispa. Although the specimens from Baltistan might be considered as a montane form of zarudnyi and, despite the fact that three specimens are not an adequate sample from which to draw conclusions, they are probably best regarded as examples of a distinct species, C. pergrisea. Although rather similar to the Asian subgroup of C. russula, specimens of C. zarudnyi may usually be separated on size (see Fig. 10 and Table 3) as well as colour and labial length of upper unicuspids (1-45-1-9 mm, x 1-77 mm in C. zarudnyi ; 1-8-2-3 mm, x 2>I6 mm in Asian C. russula). However, separation from C. suaveolens is not so easy, the only useful characters being the pale pelage colour of C. zarudnyi which is paralleled by several populations of C. suaveolens from Russian Turkestan, Algeria, Israel and also specimens from Central Gobi, Mongolia, described by Allen (1938) under the name of C. ilensis lar (which Ellerman & Morrison-Scott (1966) believed to be a subspecies of suaveolens}. This character may reflect adaptation to local environment rather than phylogenetic affinity. The other character is the relatively long tail which is also not an exclusive character (ratio of TL : UTL 3-4-5-2 : i in C. suaveolens ; 4-8-7-1 : I in C. zarudnyi). Both C. suaveolens and C. zarudnyi have been recorded from Iran (Lay, 1967), Turkey (Spitzenberger, 1970, 1971) and Afghanistan (Hassinger, 1970, 1973) but not from the same habitats, and while the mean skull size is usually greater for specimens of C. zarudnyi than C. suaveolens the only distinct character is the greater tail length of the former. The evidence suggests that C. zarudnyi is fairly closely related to C. suaveolens and may be simply an ecological form of it, but for the present it is retained as a distinct species. Crocidura russula (Hermann, 1780) The OTUs that belong to this species fall into two groups roughly equivalent to a geographical division into European and Asian forms, except that the Corsican (17) population appears to belong to the latter group and Algeria to the former. Apart from these anomalous OTUs the European group consists of Guernsey and Alderney (3), France (4), Spain (6), Portugal (7), Germany, Belgium and Holland (10), Switzerland (13), Sicily (15), Sardinia (16) and also Algeria (8) ; the Asian group includes Turkey (22), Lebanon (24), Israel (25), Afghanistan (28), Kashmir (31) and Punjab (32). Fig. ii gives the distribution of this species and shows the wide geographical separation of the two subgroups. The main characters for distinguishing these groups are the differences in relative tail length, length of the upper unicuspids (LLU 2-0-2-5 mm, x 2-25 mm ; TL 28-46 mm, x 38-35 mm in the European/ Algerian group ; LLU 1-8-2-3 mm> x 2'16 mm ; TL 36-51 mm, x 45-33 mm in the Asian group). The premolar in mainland European populations has a very broad, squarish lingual portion in comparison with the narrow lobed appearance 2Q2 P. D. JENKINS C.russula Europe/ Algeria FIG. ii. Distribution of C. russula, C. dsinezumi and C. attenuata. distribution uncertain. Broken lines -exact characteristic of the Asian subgroup and Corsica (see Figs 5, 6 and 7). Skull size in the Asian subgroup is also on average slightly smaller than in the European/ Algerian group, see Table 3. OTUs of the European subgroup are fairly similar to each other with D2 values of 1-3. In particular Spain (6) and Portugal (7) are very alike with a D2 of 1-23, as are France (4) and Germany, Belgium and Holland (10) with a D2 of 1-42. The Algerian population, although separated from the European mainland and Sardinia, is nevertheless very similar as reflected by the low D2 values of 2-42-2-86. As in C. suaveolens the greatest variation is shown by island populations, especially Sicily (15), Sardinia (16) and Corsica (17) where the D2 values range from 3-92 between Sicily and Corsica, 3-95 between Sicily and Sardinia and 5-74 between Sardinia and Corsica. Specimens from Sicily have short narrow skulls in comparison with those from Sardinia which also have fairly well-spaced upper unicuspids (see Table 5). Specimens from Sicily are most similar to Spanish specimens with a D2 value of 1-96, while those from Sardinia are closest to those from France and Germany, Belgium and Holland with D2 values respectively of 2-14 and 2-2. In spite of their close proximity to Sardinia and the European mainland, Corsican specimens show much more similarity to the Asian subgroup than to the European VARIATION IN EURASIAN CROCIDURA 293 one. D2 values between Corsica and the Asian subgroup are very low, varying from 1-44 to 2-33, while the lowest D2 between Corsica and any member of the European group is 2-89 for Spain. The Corsican population is compared with those from Sicily and Sardinia in Table 5. However, the resemblance of the Corsican population to members of the Asian subgroup is unlikely to indicate a correspondingly close relationship. It is more likely to be allied to European mainland and nearby island populations despite the dissimilarity, which is probably a reflection of an isolated island population evolving along different lines. TABLE 5 Variation between island populations of C. russula Corsica Sicily Sardinia (n = 15) (n = 5) (n = 9) Condylobasal length, mm 17-5-19-1 18-0-18-3 18-3-19-1 x 18-10 x 18-10 x 18-75 Upper too throw length, mm 7-7-8-7 8-1-8-3 8-3-8-9 x 8-21 x 8-23 x 8-62 Labial length of unicuspids, mm 1-9-2-3 2-1-2-2 2-3-2-5 x 2-06 x 2-16 x 2-42 Braincase breadth, mm 8-4-8-9 8-5-8-7 9-o-9'3 x 8-72 x 8-63 x 9-16 Tail length, mm 40-49 3J-41 33-4° x 44-8 x 35-0 x 36-7 The Asian subgroup of C. russula has a wide distribution but shows very low D2 values of 1-2. The adjacent Israel (25) and Lebanon (24) populations are very similar, with a D2 value of 1-68, and although geographically separated, populations from Lebanon and Punjab (32) are also similar with a D2 value of 1-83. Although geographically fairly close together Punjab and Kashmir (31) differ slightly, for while Punjab is fairly typical of the group Kashmir specimens are at the upper limit of the size range (e.g. UTL 7-4-8-7 mm, x 8-25 mm for Punjab ; 8-6-8-8 mm, x 8-73 mm for Kashmir). The earliest name for the Asiatic group is C. gueldenstaedti Pallas, 1811 from the Caucasus. This form has been considered conspecific with European C. russula (from which it is geographically separated) by Kuzyakin (1944, 1965), Ellerman & Morrison-Scott (1966), Spitzenberger (1970), Felten, Spitzenberger & Storch (1973) and Richter (1970). The last placed East Mediterranean forms of russula in the same subspecies group as gueldenstaedti. C. gueldenstaedti has been regarded as specifically distinct by Vinogradov (1958), Gureev (1971) and Kock (1974). Vinogradov presumably contrasted the structure of the external genitalia of both European russula and gueldenstaedti, although only producing evidence about the latter. The character he did use was the difference in relative tail length. Without actually examining any specimens of gueldenstaedti from the Caucasus, I hesitate to use this name as the senior synonym of any of the subspecies listed here, 294 P. D. JENKINS although accepting its usage by other authors for C. r. monacha of Turkey as probably correct. For the same reason it seems incorrect to use it as a blanket name as Richter did, especially as some of the subspecies he included in that group appear fairly distinct. Also it is not necessarily correct to ally Asian forms with Mediter- ranean island forms which may have originated from any of many possible sources and which are presumably fairly isolated genetically. For example, although Corsican animals very closely resemble populations from Lebanon and Punjab they are also similar to Spanish specimens (see above, p. 293). The following subspecies have been examined and fall into two groups ; European group C. r. russula (Hermann, 1780). European mainland (4, 10, 13). C. r. pulchra Cabrera, 1907. Spain, Portugal (6, 7). C. r. peta Montagu & Pickford, 1923. Guernsey, Herm and Alderney (3). C. r. ichnusae Festa, 1912. Sardinia (16). C. r. sicula Miller, igoia. Sicily (15). C. r. cyrnensis Miller, 1907. Corsica (17). Associated with this group is C. r. agilis Levaillant, 1867. Algeria (8). Asian group C. r. monacha Thomas, 1906 (probably C. r. gueldenstaedti Pallas, 1811 see above). Turkey (22). C. r, pullata Miller, 1911. Kashmir (31). Also samples from Lebanon (24), Israel (25) and Punjab (32). The affinities of C. russula and C. suaveolens have been discussed previously under C. suaveolens and those of C. russula and C. leucodon are dealt with in the account of C. leucodon. Punjab (32) Dar.eeling (341 Bhutan (35) FIG. 12. D2 values between the closest geographical populations of C. russula and C. attenuata. VARIATION IN EURASIAN CROCIDURA 295 C. attenuata may be distinguished from C. russula by the longer tail (TL 36-51 mm, x 45-33 mm in Asian russula ; 50-79 mm, x 62-94 mm in C. attenuata). Kashmir (31) and Punjab (32) populations of the Asian subgroup of russula mark the eastern limit of this group, while Darjeeling (34) and Bhutan (35) are the westernmost populations of C. attenuata. The D2 values between these four populations are shown in Fig. 12. The lowest figure, which is between Punjab (32) and Bhutan (35), does not in this case represent great similarity as specimens from Punjab may usually be distin- guished from Bhutan specimens by their slightly broader skulls and shorter tails (IB 4-2-4-5 mm, PB 6-0-6-4 mm> TL 40-51 mm in Punjab specimens of C. russula ; IB 3-9-4-2 mm, PB 5-7-6-1 mm, TL 52-63 mm in Bhutan specimens of C. attenuata). Crocidura dsinezumi Temminck, 1844 Specimens from Japan (47), currently regarded either as a distinct species, C. dsinezumi, or as a subspecies of C. russula, emerge in the CVA close to certain OTUs of both the Asian subgroup of C. russula and C. suaveolens. The Japanese specimens may be distinguished from their nearest neighbours of C. suaveolens occurring in Korea and Tsushima Islands, which are smaller, see Table 3. Although geo- graphically well separated from other samples of C. suaveolens, the Japanese popula- tion shows low D2 values with some OTUs, such as Jersey and Sark (2) and Greece (21), of 2-7. Low D2 values are also shown between Japan and the Asian subgroup of C. russula, for example Punjab (32) with 2-7, Lebanon (24) with 2-8. The size of the skull is within the upper limits of C. suaveolens but only just within the lower limits of Asian russula (see Fig. 10), while the tail is relatively long and within the range of Asian russula (TL 37-50 mm, x 44-6 mm). The Japanese population was described as a distinct species, C. dsinezumi, but was treated as a subspecies of C. russula by Ellerman & Morrison-Scott (1966). Imaizumi (1970) regards C. dsinezumi as a distinct species and separable from C. suaveolens occurring in China, Korea and the Tsushima Islands. This view seems preferable and it is considered here to be a separate species. Crocidura attenuata Milne-Edwards, 1872 This species includes the following OTUs : Darjeeling (34), Bhutan (35), Assam (36), Burma (37), China (44) and also Christmas Island (40). Specimens from Christmas Island have hitherto been assigned to C. fuliginosa trichura. The distribution of C. attenuata is shown in Fig. n. D2 values between Darjeeling, Bhutan, Assam and China range from 2-43 to 3-47, which, while not as low as in some groups, nevertheless indicate a fairly high degree of relationship, especially when the geographical distances and variation in ecological conditions are taken into account. Darjeeling, Bhutan and Assam are at least partially isolated from each other by the mountainous terrain and separated from Burma and China by distance and differing habitats. The Burmese population is 296 P. D. JENKINS separated from any group other than C. attenuata by very high values of D2. The lowest D2 value is 4-84 with Assam and 4-91 with Darjeeling. Christmas Island is a considerable distance from the main distribution area of C. attenuata but it shows relatively low D2 values of 3-65-4-73 with Darjeeling, Bhutan, Assam and Burma. It shows no similarity to any other group entered in the CVA and may be readily distinguished from both the small and very large species oi Crocidura occurring in Indonesia, which is the nearest area where shrews of this genus occur. A single specimen from Java and three from Sumatra closely resemble both Christmas Island specimens and other populations of C. attenuata, which suggests that this species may also be present, under different names and rarely recorded, in some parts of Indonesia. This would make the presence of attenuata in Christmas Island more likely, as a representative at the extreme limit of a species having a discontinuous distribution from Asia down through the Indonesian chain. The Mahalanobis' distances are a reflection of the range of variation in this group, for example, in populations from Bhutan and Christmas Island the anterior part of the skull is fairly narrow (MB 5-2-5-9 mm, x 5-5 mm) but the posterior part of the skull in the latter population is wider than in the former (PB 5-7-6-1 mm, x 5-84 mm in Bhutan ; 6-1-6-5 mm> x 6-32 mm in Christmas Island) - see Fig. 13. Measure- ments for the species are given in Table 6. 6-0- O * * * ** o D DO • • O o DOT O 8 5-5 6-5 width across maxillae at FIG. 13. Variation in skull width in populations of C. attenuata. Darjeeling • ; Bhutan * ; Assam O ; Burma Q ; China T ; Christmas Island VARIATION IN EURASIAN CROCIDURA 297 C. attenuata has apparently been confused with C. fuliginosa in the past and it seems likely that the latter name has been used at various times to refer to quite different animals. For example, Blanford (1888) synonymized C. rubricosa and C. kingiana (currently regarded as subspecies of C. attenuata) with C. fuliginosa, giving the distribution as Eastern Himalayas, Assam and Tenasserim (Burma). Thomas (1889) gave the distribution of C. fuliginosa as Himalayas through Burma to Java and in this paper Dobson described a new shrew from Christmas Island as a geographical race - C. fuliginosa trichura. The holotype and ten other specimens from Christmas Island are in the BMNH ; information given above indicates close association with C. attenuata and certainly none with the group referred to as C. fuliginosa in this report. The correct name for the Christmas Island Crocidura is thus C. attenuata trichura, The following subspecies have been examined : C. a. attenuata Milne-Edwards, 1872. China and Hainan (44). C. a rubricosa Anderson, 1877. Assam, Himalayas (34, 35, 36). C. a. trichura Dobson, 1888. Christmas Island (40) - formerly attributed to C. fuliginosa trichura. Also a sample from Burma (37), an attenuata whose affinities are uncertain at sub- specific level. The affinities of this species with members of the Asian subgroup of C. russula have been discussed previously under the latter species. Key 3 (p. 282) and Fig. 7 give the characters for separating C. attenuata from C. fuliginosa and others occurring in the area. TABLE 6 Size range of C. attenuata, C. leucodon, C. lasiura and C. fuliginosa Upper Width of Braincase Condylobasal toothrow maxillae at breadth, length, mm length, mm M2, mm mm 18-3-20-6 7-8-9-8 5-2-6-5 8-2-10-0 x 19-95 x 8-79 xs-Sg x 9-12 17-8-19-9 8-0-9-2 5-7-6-5 8-6-9-5 x 18-74 x 8-60 x 6-15 x 9-11 19-0-21-4 8-8-10-2 5-8-6-8 8-8-10-2 x 19-96 x 9-18 x 6-29 X9'45 18-6-21-6 9-2-10-3 6-2-7-0 9-1-10-2 x 20-77 X9-74 x6-85 X9-67 21-3-25-0 9-4-11-5 6-2-7-8 9-5-11-1 x 22-80 x 10-40 x 6-90 X IO-IO C. aitenuata Asia C. leucodon France, Germany, Yugoslavia Switzerland, Asia Minor C. lasiura Korea C. fuliginosa Asia, Malaysia Crocidura leucodon (Hermann, 1780) Fig. 14 gives the distribution of this species. The OTUs are : France (5), Germany (n), Switzerland (14), Yugoslavia (20), Turkey (23), Israel and Lebanon P. D. JENKINS C.leucodon C tas.ura FIG. 14. Distribution of C. leucodon and C. lasiura. uncertain. Broken lines -exact distribution (26) and also Iran (27) which has hitherto been regarded as a subspecies of russula - C. r. caspica. This is a loosely knit group exhibiting a large range in variation. Those showing greatest association are European populations from France (5), Germany (n) and Yugoslavia (20) which have D2 values between i and 3. French and German populations in particular have crowded unicuspids (LLU 1-8-2-1 mm, x 1-93 mm), while this measurement in the Yugoslavian population is 1-9-2-3 mm, x 2-05 mm. Skins usually show a sharp delineation along the flanks between the dark dorsal and pale ventral colour. Although hitherto believed to belong to C. russula, Iranian specimens can be readily distinguished from that group - see last section of this species account. The Iranian population is very similar to that from Turkey with a D2 value of 2-4. Both Iranian and Turkish specimens on average have larger skulls with uncrowded unicuspids in comparison with their European counterparts (LLU 2-1-2-55 mm, x 2-23 mm). Turkish specimens have a dark dorsum and paler venter although not so definitely bicoloured as European specimens, while Iranian specimens differ markedly in their very dark dorsal and ventral surface. Specimens from Israel and Lebanon are most similar to those from Turkey and Iran, although the D2 value is rather high. They fall within the range on skull size and the pelage colour resembles that of Turkish specimens. VARIATION IN EURASIAN CROCIDURA 299 Although Swiss specimens might be expected to be most similar to nearby populations from France and Germany, Mahalanobis' distances are from 3 to 4, while the D2 values between Swiss and Turkish populations is 2-26 and between Switzerland and Iran 2-77. Variation between the two subgroups is shown in Table 6. Turkish specimens are associated with other OTUs in this group by D2 values of 2-5 and they represent C. leucodon lasia which has a chequered history. It was originally described by Thomas (1906) as a subspecies of C. leucodon, though he later (1907) declared it distinct enough to be a full species - C. lasia. Bobrinskii et al. (1944) decided it was a subspecies of the Korean C. lasiura, an opinion with which Ellerman & Morrison-Scott (1951) concurred, although in the second edition Bobrinskii (1965) included it as a distinct species -- C. lasia. Vinogradov (1958), examining the external genitalia, was unable to differentiate lasia from C. leucodon although C. lasiura was found to be distinguishable. Lay (1967) and Gureev (1971) also regard it as a subspecies of C. leucodon and this seems the best arrangement since it is fairly similar to, though relatively larger than, the European members of C. leucodon. It is quite similar to specimens of C. lasiura (D2 value of 3-03) but the considerable discontinuity of distribution and Vinogradov's findings discourage the view that they might belong to the same species. Specimens from Iran, including the holotype of C. russula caspica, are most similar to C. leucodon lasia from Turkey and other members of the leucodon group. In 1951 Ellerman & Morrison-Scott noted that caspica might represent C. lasiura (in which species they had placed C. leucodon lasia}. However, Bobrinskii (1965), Lay (1967) and Richter (1970) placed it with C. russula in the gueldenstaedti subspecies group with a number of other subspecies which in this report belong to the Asian subgroup of C. russula and are readily distinguished from Iran specimens. Finally, Gureev (1971) included C. r. caspica, together with C. r. monacha, in synonymy with C. gueldenstaedti. This last seems very suspect since specimens of C. r. monacha from Turkey may be distinguished from Iran specimens on many characters (see Table 7) . Despite the marked colour difference I believe these specimens from Iran should be regarded as a subspecies of C. leucodon - C. leucodon caspica - close to C. leucodon lasia. Another subspecies, C. leucodon persica, also occurs in Iran. The holotype and one other specimen are in the BMNH. They resemble European members of leucodon in size and colour and are easily distinguished from Iran specimens of C. 1. caspica. However, while all specimens seen of C. I. caspica are from low alti- tudes (the type series from under 25 m), C. I. persica appears to be a high altitude subspecies since the holotype was collected at 1980 m. The resemblance of specimens from Israel and Lebanon to C. russula from Central Europe was noted by Thomas (1919) in his original description of C. russula judaica. In 1951 Ellerman & Morrison-Scott suggested the possible inclusion of this form with C. lasiura (along with lasia}. Harrison (1963) considered it to be a local form of C. leucodon and this view is supported by the resemblance to specimens of C. leucodon from Turkey and Iran (see Table 7). 3oo P. D. JENKINS a a o C Q CTj *"rt "2 « - ,li c I 1 1 .1 ^ il>£| ^M ^<» o ""Q £3 CM r ON N vO CM ON fi 3 ^ rt I O i X I ^ I aj '*••> t^0? O ^ClS.ONMVOMON g S «0 I P I 00 O N I iX ob '^ o '^ ON '^ °p ro 5 <0 £^> — O »S ^ . TH 1 ON 2 ? °P rf 6 ro o •*• ;; >r> . . w . 1 vO 1 ON O^ _-. « ro Tf ro O H 1 0H M ob ^5 «X • IX S'X o o 3 I *O .2 ^l" julations Q en , • 1-1 S^0^ 8 a ^c- ?lf 5 • 00 P « V M . 1 00 ob N i • O^- in . M vO ^O ON ON N ^ ^ ^ 'X ob '* H M VO Tf a 0 1 "3 I ? c 1 M n-'X 1 " S 00 s S £ •*i 00 ^ 0) • j i 0) . i W) rt CD "o & B 'X X3 OH OnX! 1 C 1 rt ^ 6 o3 en ^ | f l_! en b c3 OH 1 o 1 0 « s a £ 8 O rC O ^^ t. r> O B o Q 1 ^~ 5 c S 1 | 8 0 ^ w PC VARIATION IN EURASIAN CROCIDURA 301 The following subspecies have been examined and fall into two main groups : C. 1. leucodon (Hermann, 1780). Most of Europe (5, n, 20). C. I. persica Thomas, 1907. Elburz Mountains, Iran. The second subgroup includes : C, I. lasia Thomas, 1906. Turkey, Transcaucasia (23). C. I. judaica Thomas, 1919. Israel and Lebanon (26). C. /. caspica Thomas, 1907. S. coast of Caspian Sea, Northern Iran (27). A sample from Switzerland (14) of uncertain affinity. Keys i and 2 give the characters that are useful in distinguishing C. leucodon from other species occurring in the area. Despite the original naming of Iranian specimens as C. russula, they are particularly similar to specimens of C. leucodon lasia from Turkey mentioned above and can be readily distinguished from the Asian subgroup of C. russula by their more robust, longer and broader skulls. They are rather similar to the European subgroup of C. russula, but the skulls are on average slightly larger and the resemblance is unlikely to be a true indication of relationship. Table 5 gives a comparison of these populations. Swiss specimens of C. leucodon are most closely associated in the analysis with Swiss specimens of C. russula at a very low D2 value of 1-64 and with other European members of that species at D2 values of 2-3. In Switzerland individual specimens of the two species are not readily distinguished from each other except on the basis of colour. Specimens of leucodon fall in the upper part of the russula size range (CBL 18-0-19-9 mm, x 19-01 mm ; BB 8-5-9-4 mm, x 9-13 mm in russula ; CBL 19-2-19-8 mm, x 19-5 mm ; BB 9-2-9-5 mm, x 9-38 mm in leucodon}. This problem in Switzerland obviously requires very careful investigation into ecology, behaviour and genetics to try to establish the true relationship between these species. Crocidura lasiura Dobson, 1890 The distribution of this species, represented in this report by the Korean population (46), is given in Fig. 14. Korea is geographically isolated from Middle Asian populations of C. leucodon, yet the D2 value between Korea and Turkey (23) is comparatively low, at 3-03. The range in skull size is similar for Korean and Turkish populations but on average Korean specimens have larger skulls, see Table 6. In Korean specimens the ventral pelage colour is only slightly paler than the dark dorsum, in contrast to the more marked differentiation in Turkish specimens. In this study C. lasiura was represented by a large series from Korea, including the holotype of C. I. thomasi. In the CVA this sample showed some affinity to C. leucodon lasia (23) with a D2 value of 3-03, but diverged more from C. leucodon caspica (27), a D2 value of 4-77, and C. leucodon judaica (26) a D2 value of 6-38. Ellerman & Morrison-Scott (1966) also noted this similarity but the evidence of dissimilarity in penis structure (Vinogradov, 1958) strongly suggests that it should be retained as a distinct species. 302 P. D. JENKINS The subspecies examined was : C. lasiura thomasi Sowerby, 1917. Korea (46). See Key (p. 282) for comparison with other species in the surrounding area. OTHER SPECIES RECORDED FROM THE AREAS OF STUDY BUT NOT INCLUDED IN THE ANALYSIS The following species recorded from Eurasia are either absent from the collection or there are too few specimens for inclusion in the previous account. C. hispida Thomas, 1913. Middle Andaman Island, Bay of Bengal. The BMNH houses the holotype, which is a very large animal, (CBL 27-4 mm) much larger than any of the species described in this account and with the tail longer than the head and body. It is also distinguished by its semi-spinous pelage. C. andamanensis Miller, 1902. South Andaman Island, Bay of Bengal. No specimens apart from a small hair sample which differs from other species in that some of the hairs are flattened, although they are not so broad as the hairs of C. hispida, and there is no mention in the original description of the pelage being spinous. From the description of the holotype it appears to be comparable in size, though slightly smaller than C. hispida (CBL 25-6 mm). C. nicobarica Miller, 1902. Great Nicobar Island, Bay of Bengal. No specimens apart from a small hair sample which contains flattened, broadened, hairs resembling those of C. hispida but less spinous. The condylobasal length of the holotype given in the original description is 27-0 mm. C. miya Phillips, 1929. Sri Lanka. The skin and skull of the holotype are in the collection of the BMNH. The specimen is distinguished by the proportionately very long tail but in other respects it is very similar to C. attenuata (CBL 19-7 mm, UTL 8-7 mm, MB 5-9 mm, HB 79 mm, TL 88 mm). C. caudata Miller, igoia. Palermo, Sicily. No specimens examined. Kahmann & Einlechner (1959) believe that this is a subspecies of C. russula. C. balearica Miller, 1907. Minorca, Balearic Islands. Kahmann & Vesmanis (1974) consider this to be a subspecies of C. suaveolens. From the U.S.S.R. Gureev (1971) records the following species which I have not seen : C. ognevi Stroganov, 1956. Altai. C. pamirensis Ognev, 1928. Lake Drum vicinity, southern slopes of Pamir Mountain Range. C. armenica Gureev, 1963. 14 km down river from Garni, Armenia. C. dinniki Ognev, 1921. Stavropol'. From Japan Imaizumi (1970) records : C. orii Kuroda, 1924. Amami-Oshima, Riukiu Islands. Preliminary examination of examples of the following forms recorded from Sumatra and Java by Chasen suggests that they represent C. fuliginosa : C. villosa Robinson & Kloss, 1918. Sumatra. Holotype in BMNH. VARIATION IN EURASIAN CROCIDURA 303 C. brunnea Jentink, 1888. Sumatra, Java. Holotype of C. b. brunnea and ten specimens of C. b. pudjonica loaned by Leiden Museum. C. brevicauda Jentink, 1890. Java. Holotype and fifteen specimens loaned by Leiden Museum. C. orientals Jentink, 1890. Java. Holotype and eight specimens loaned by Leiden Museum. C. melanorhyncha Jentink, 1910. Java. Holotype and one other specimen loaned by Leiden Museum. The following species recorded from the Malaysian region have also been subject to a preliminary examination and may be easily separated from C. fuliginosa by their small size (CBL 15-2-19-5 mm). C. monticola Peters, 1870. Java, Borneo, Lombok, Sumbawa, Komodo, Flores, Sumba and ? Timor. There is only one specimen in the BMNH collections. C. aequicauda Robinson & Kloss, 1918. Sumatra, Malay Peninsula. Holotype in BMNH. C. beccarii Dobson, 1886. Sumatra. One damaged specimen only. C. bartelsii Jentink, 1910. Java. Four specimens loaned by Leiden Museum. C. maxi Sody, 1936. Java. One damaged specimen loaned by Leiden Museum. C. minuta Otten, 1917. Java. Two badly damaged specimens loaned by Leiden Museum. Of these bartelsii is probably conspecific with monticola. It is possible that maxi and minuta might also belong to this species, although more specimens are required to furnish any definite conclusions. I have seen none of the remaining species listed by Chasen : C. paradoxura Dobson, 1886. Sumatra. C. neglecta Jentink, 1888. Sumatra. C. weberi Jentink, 1890. Sumatra. C. lepidura Lyon, 1908. Sumatra. C. vosmaeri Jentink, 1888. Banka Island. There are several unidentified specimens from Sulawesi which fall within the range of C. fuliginosa although this species has not previously been described from there. Laurie & Hill (1954) list the following species, none of which has been examined : C. elongata Miller & Hollister, 1921. North eastern Sulawesi. C. nigripes Miller & Hollister, 1921. North eastern Sulawesi. C. rhoditis Miller & Hollister, 1921. North eastern Sulawesi. C. lea Miller & Hollister, 1921. North eastern Sulawesi. C. levicula Miller & Hollister, 1921. Middle Sulawesi. C. tenuis (Miiller, 1839). Timor. Taylor (1934) records eight species from the Philippines of which the BMNH houses examples of only the first one : C. grayi Dobson, 1890. Luzon and Benguet, Philippines. Holotype and two other specimens in the BMNH (CBL 18-6-20-0 mm, UTL 8-5-9-1 mm, BB 9-3-9-5 mm, 304 P. D. JENKINS TABLE 8 Mahalanobis' distances. The 47 OTUs are numbered as in Table i 3 4 5 6 7 8 9 10 ii 12 13 14 15 16 I 2 3 4 5 6 7 8 9 10 ii 12 13 o-o 4'9 6-2 6-2 4'5 4'4 5-8 3-6 6-6 5'5 2-7 6-0 o-o 6-4 7-9 7-6 6-4 6-4 8-1 5'3 8-4 6-9 7-5 o-o 2-O 4-8 1-9 2-O 3'7 6-3 2-6 4'9 6-5 2-7 o-o 4'4 2-0 2'5 2'5 7-1 7-8 2-O o-o 4-8 5'5 4'7 6-1 4'5 2-8 8-1 3'5 o-o 1-2 2-4 5-9 2-9 5'2 2-6 o-o 2-8 5'9 5'3 5'7 3'3 o-o 6-3 2-9 5'4 7'4 3-0 o-o 7'5 5'3 4-0 6-8 o-o 4'9 8-3 1-8 o-o 6-9 4'3 o-o 7-6 o-o 14 6-9 8-5 4-0 3'2 3'4 4-1 4'7 3'9 7-5 2-4 4-2 8-7 1-6 o-o 15 4-6 6-5 2-7 3-0 4'7 2-O 2-6 3-3 5-6 3'3 4'9 6'2 2-7 3-8 o-o 16 7-2 9-2 3'5 2-1 6-0 3'i 2-9 2-8 8-1 2-2 6-4 8-5 3-4 4'4 4-0 o-o 17 3-1 4-2 3'4 4'5 5-7 2-9 3-2 4'7 5'7 5'2 5'9 4'9 4'5 5-8 3'9 57 18 3'2 4-1 6-4 7'4 7-4 5-8 5'4 6-9 3'4 7-9 6-4 2-2 7'3 8-4 5'7 8-1 19 2'0 3'4 5'3 6-7 7-2 5-0 4-6 6-5 3'9 7-2 6'2 2-O 6-8 7-9 5-2 7-5 20 5-6 7'5 4-2 3-6 1-9 3-8 4'5 3'5 6-2 3-6 3'3 7'7 2-9 3-0 3'9 5-o 21 3-1 3'9 4'5 5-6 6-5 3-8 3-8 5-6 4'5 6-2 6-0 3'5 5'5 6-8 3-6 6-4 22 4'7 5'5 3'5 4-1 6-1 2-8 3'4 4'5 6-9 4-8 6-7 6-1 4-0 5'3 3'7 5'2 23 8-0 9'3 5'3 4'4 3'4 5'3 6-2 4'9 8-6 4-0 5'3 9-9 3-1 2-3 5'4 5-8 24 3'7 4'4 3'3 4'5 6-3 3-1 3'3 5-0 6-2 5'4 6-5 5-0 4-8 6-2 4'3 5'7 25 3'3 4-6 4-0 5'0 6-7 3'2 3-1 4-8 5'9 5'7 6-7 4'4 5'3 6-7 4'5 5'7 26 9'3 II-2 5'9 4'i 5-6 5-7 6-0 4-2 9-7 3-8 6-8 10-9 4'4 4'3 6-5 4-0 27 7'4 8-5 4'7 3'7 4-0 4'4 5-1 4-2 8-1 3'7 5-6 9-0 2-5 2-8 4-6 4-8 28 2'6 3-6 3-6 4'7 4-6 3'3 3-6 4-8 4-6 5-1 4'3 4-2 4-1 5-1 3'7 6-0 29 3-7 2-9 6-9 8-2 8-6 6-4 6-4 8-0 6-4 8-9 8-4 3-8 8-1 9'3 7-2 9-1 30 2-7 4-0 6-1 7-0 5'9 5'5 5'5 6-2 3'4 7-1 4-8 3'3 6-2 6-9 5'3 7'9 31 4'7 5'9 3'9 4-i 4'9 3'3 3'7 4'i 6-7 4-7 57 6-5 3'9 5'i 4'7 5'3 32 3'5 3-8 4'i 5'2 6-0 3'7 3'9 5'3 5'9 5'7 6-0 4'5 4-8 6-1 4'5 6-3 33 6-0 5'3 8-7 10-2 n-5 8-5 8-2 10-2 8-2 II'O II'O 5'2 10-6 I2'O 9-2 10-9 34 8-2 7-9 8-2 8-6 10-0 7-6 8-0 8-8 10-6 9'5 II-2 9-2 8-7 10-0 8-7 9-5 35 5'9 5-6 6-6 7'4 9-0 6-0 6-3 7-6 8-3 8'4 9-6 6-6 7-6 9-0 7-0 8-4 36 8-0 7'7 6-6 7-0 8-9 6-4 6-9 7'9 10-4 7-9 IO'O 9-2 7-2 8-5 7'5 8-1 37 10-8 10-7 9'5 9-8 11-7 9-6 9-9 10-5 12-9 10-5 I2'8 ii-9 10-3 II'2 10-8 10-7 38 10-9 ii-7 8-4 7'7 8-6 8-3 9-1 8-5 12-9 7-7 IO'2 12-9 7-5 7'5 9-1 8-6 39 13-1 13-6 10-4 9-7 IO-2 10-6 n-4 10-8 14-9 9-7 II-9 15-2 9'5 9'3 II'2 10-7 40 10-0 9-2 10-0 10-7 12-6 9-7 9-9 n-i 12-3 ii-7 13-5 10-4 II-O 12-4 10-8 "•5 41 11-7 n-8 9'3 8-9 9'4 9'5 10-3 10-0 13-3 9'3 II-2 13-5 8-7 8-9 10-3 10-3 42 2-4 3-7 3'9 5-2 6-0 3'7 3'2 5-2 4-2 5'7 5'i 2-9 5'2 6-4 4'3 6-0 43 I2'I I2'O 9-8 9'5 9-8 IO-I 10-8 10-7 13-8 9-8 "•5 13-8 9-1 9-2 10-7 10-8 44 6-4 6-9 5'3 5'5 7-1 4-8 5'5 6-0 8-7 6-5 8-4 8-1 5'7 6-9 6-0 6-8 45 3'3 3'3 7'5 8-8 9-1 6-9 6-8 8-3 47 9'4 8'2 2-0 8-7 9-7 7-0 9-6 46 9-8 II'O 7-9 7-0 5'4 7'7 8-6 7-2 10-5 6-5 7-1 ii'9 5'7 4'7 7-6 8-2 47 3'3 2-7 5'i 6-5 7-3 4-8 5'i 6-8 5'7 7-2 7-2 4-0 6-2 7-5 4'9 7'8 VARIATION IN EURASIAN CROCIDURA 305 TABLE 8 (Cont.) 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 17 o-o i8 5-1 o-o 19 4-0 2-O o-o 20 4-8 7-1 6-7 o-o 21 3'3 2-9 2-7 6-0 o-o 22 2-0 6-4 5-5 5'3 4-1 o-o 23 6-5 9-6 9-2 3'3 8-0 6-0 o-o 24 1-3 5-5 4'3 5'7 3-6 2-0 6-9 o-o 25 1-5 4-7 3'7 5-8 3'4 2-7 7-6 1-7 o-o 26 7-7 10-4 10-0 5-0 9-1 7-2 4'4 7-9 8-1 o-o 27 5'5 8-6 8-4 3-8 6-8 4-6 2-4 5-8 6-3 4-2 o-o 82 2-1 4'3 3-6 4'i 3-0 3'3 6-0 2-8 3-0 7'7 5'2 o-o 29 3-8 4-8 4-0 8-1 4-6 5'2 9-9 4-0 3'5 II-2 8-9 4-4 o-o 30 4-6 3-0 3'4 5-5 3-8 5-8 7-9 5"4 4'9 9'4 7-3 3-0 5-o o-o 31 2-3 6-5 5'7 4-0 5'2 2-9 5-2 2-9 3-0 6-1 4'3 3-0 5-3 5-4 o-o 32 1*4 4'9 4-2 5'4 3'4 2-3 6-7 1-8 2-1 8-1 5'5 1-9 3-5 4'3 2-6 o-o 33 6-5 6-4 5'4 10-9 6-5 7-5 12-8 6-1 5-8 .13-6 n-7 7-4 3-8 7-9 8-3 6-5 34 5-7 9-6 8-8 9'3 7-9 5'3 9-7 5-6 5'7 10-7 8-3 7-4 6-1 9'5 5'9 5-7 35 3'9 7-2 6-4 8-4 5'5 3'9 9'3 3'5 3'7 10-3 7-9 5-6 3'9 7-5 5'i 3'9 36 5'i 9'5 8-6 8-3 7'3 4'4 8-3 4-8 5'5 9'4 6-9 6-7 6-7 9'3 5'2 5'2 37 8-4 12-5 11-4 n-i 10-7 7'9 10-8 7'9 8-5 II-2 10-0 10-0 9-2 12-4 8-2 8-7 38 8-4 12-8 n-9 7-8 10-7 7-7 6-3 8-7 9-2 7-4 6-6 9-2 ii-i n-6 7-1 8-8 39 10-6 15-0 14-2 9'7 12-9 10-0 7-8 10-9 n-6 9-2 8-5 11-4 13-4 13-7 9-4 ii-o 40 7-9 n-i 10-3 I2-I 9'5 7'4 12-3 7'3 7'7 13-1 10-8 9-6 7-4 n-6 8-6 7-8 4i 9-0 13-5 12-7 9-1 11-4 8-4 7'4 9-1 10-0 9-1 7'5 10-0 n-3 12-5 8-0 9-3 42 2-9 3-1 2-2 5'5 2-7 4-2 7'7 3-0 2-7 8-3 6-7 2-2 4-1 3'4 4-1 2-8 43 9'5 13-9 I3-I 9'7 n-8 8-8 7-9 9-6 10-5 9-7 7'9 10-3 n-7 12-8 8-5 9-6 44 3'5 8-2 7-3 6-3 6-2 3-0 6-7 3-6 4-1 7-9 5'5 5'2 5'9 7'7 3'4 4'0 45 5'3 3-0 2-9 8-6 4-1 6-5 10-8 5-6 4'9 I2-I 9-9 5-1 3'4 4-1 7-1 5-2 46 8-4 u-6 II-2 5'2 10-1 8-0 3-0 9-1 9-6 6-4 4-8 7-9 n-6 9'4 7-i 8-6 47 2-8 4-6 3-8 6-8 2-8 3'5 8-3 2-9 3'3 IO-I 7-2 3'2 3-2 4'7 4-9 2-7 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 33 o-o 34 7-8 o-o 35 5-4 3-0 o-o 36 8-5 2-7 3-6 o-o 37 9'9 4'9 6-4 4-8 o-o 38 13-6 7'7 9'3 6-4 8-4 o-o 39 15-8 9-8 "'5 8-4 9-8 2-7 o-o 40 7-6 3'7 4'2 4-7 4'7 10-4 12-2 o-o 4i 13-6 7-2 9-1 5'9 7-1 3'7 3'7 9-2 o-o 42 6-2 8-0 5'7 7'5 10-4 10-7 12-9 9-7 11-4 o-o 43 14-0 7-9 9-6 6-4 7-6 4'3 4-0 9-6 1-5 n-7 o-o 44 8-2 3'3 3'5 2-4 6-1 6-3 8-5 6-1 6-4 6-2 7-1 o-o 45 4'5 8-8 6-2 9-2 n-8 I3-3 15-5 9-9 13-7 4'3 14-1 8-1 o-o 46 14-7 II-O n-i 9-8 I2-I 6-1 7-2 I3-9 7'7 9.9 8-0 8-3 12-5 o-o 47 5'3 6-3 3-8 5'9 9-2 IO-2 12-3 7'7 10-4 3'7 10-7 5'i 3'9 10-1 o-o 306 P. D. JENKINS HB of holotype 68 mm, TL of holotype 51 mm). This species seems very similar to C. attenuata. C. parvacauda Taylor, 1934. Cotabato, Philippines. C. halconus Miller, 191 ib. Mindoro, Philippines. C. beatus Miller, 191 ib. Mindanao, Philippines. C. mindorus Miller, 191 ib. Mindoro, Philippines. C. grandis Miller, 191 ib. Mindanao, Philippines. C. palawanensis Taylor, 1934. Palawan, Philippines. C. edwardsiana Trouessart, 1880. Jolo, Sulu Archipelago, Philippines. ACKNOWLEDGEMENTS For the loan of specimens vital to this study, I am indebted to Dr C. O. Handley of the United States National Museum, Dr D. L. Harrison of the Harrison Zoological Museum, Sevenoaks, Dr A. M. Husson of the Rijksmuseum van Natuurlijke Historic, Leiden, and Dr F. Spitzenberger of the Naturhistorisches Museum, Vienna. My thanks are due to Linda Jackson of Rothamsted Experimental Station, who was responsible for running the computer program. I am especially grateful to Dr M. Hills of the Biometrics Section, BMNH, who has given freely of his knowledge and time in the mathematical studies involved, to Mr J. E. Hill and Mr I. R. Bishop O.B.E. of the Mammal Section, BMNH, for their advice and encouragement at every stage of the work and to Dr G. B. Corbet, Deputy Keeper of Zoology, BMNH, for his valued criticism of the manuscript. REFERENCES ALLEN, G. M. 1938. The mammals of China and Mongolia. Parti. New York. ANDERSON, J. 1877. Description of some new and little known Asiatic shrews in the Indian Museum, Calcutta. /. Asiat. Soc. Beng. 46 (2) : 280. 1 88 1. Catalogue of Mammalia in the Indian Museum, Calcutta. Part i. Calcutta. BANKS, E. 1931. A popular account of the mammals of Borneo. /. Malay. Brch R. Asiat. Soc. 9 (2) : 1-139, 9 pis. BLANFORD, W. T. 1888. The fauna of British India, including Ceylon and Burma. London. BLYTH, E. 1855. Proceedings of the Asiatic Society of Bengal for May 1855. /. Asiat. Soc. Beng. 24 (4) : 362. 1856. 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MEDWAY, LORD. 1965. Mammals of Borneo, field keys and an annotated checklist. /. Malay. Brch R. Asiat. Soc. (1963) 36 part 3 : 1-193, 34 Pls. J maP- MILLER, G. S. igoia. Five new shrews from Europe. Proc. biol. Soc. Wash. 14 : 41-45. A new shrew from Switzerland. Proc. biol. Soc. Wash. 14 : 95. Descriptions of three new Asiatic shrews. Proc. biol. Soc. Wash. 14 : 157-159. 1902. The mammals of the Andaman and Nicobar Islands. Proc. U.S. natn. Mus. 24 : 751-795, 2 pis. 1907. Some new European Insectivora and Carnivora. Ann. Mag. nat. Hist. (7) 20 : 389-398. 191 la. Two new shrews from Kashmir. Proc. biol. Soc. Wash. 24 : 241. 191 ib. Descriptions of two new genera and sixteen new species of mammals from the Philippine Islands. Proc. U.S. natn. Mus. 38 : 391-404, 3 pi. 1913. A new shrew from Baltistan. Proc. biol. Soc. Wash. 26 : 113. & HOLLISTER, N. 1921. Twenty new mammals collected by H. C. Raven in Celebes. Proc. biol. Soc. Wash. 34 : 93-104. MILNE-EDWARDS, A. 1872. Recherches pour servir a I'histoire naturelle des Mammiferes. Paris. MONTAGU, I. G. S. & PICKFORD, G. 1923. On the Guernsey Crocidura. Proc. zool. Soc. Lond. 1923 : 1044. MULLER. 1839. In TEMMINCK, C. J. Verhandeling over de Natuurlijke Geschiedenis der Nederlandsche overzeesche bizittingen, door de Leden der Natuurkundige Commissie in Indie, 1 : 26, 50. Holland. OGNEV, S. I. 1921. Materials for the systematics of insectivorous mammals of Russia. Ezheg. zool. Muz. 22 : 311-350. 1928. [Mammals of eastern Europe and northern Asia. Vol. i. Insectivora and Chiroptera.] Moscow, Leningrad. OSBORN, D. J. 1965. Hedgehogs and shrews of Turkey. Proc. U.S. natn. Mus. 117 (3517) : 553-566. OTTEN, L. 1917. Over de biologic van Mus concolor. Meded.burgerl.geneesk.Dienst.Ned.-Ind. (6) : 82-119. PALLAS, P. S. 1811. Zoographia Rosso-Asiatica i. Leningrad. PETERS, W. 1870. Uber neue Arten von Spitzmausen des Konigl. zoologischen Museums aus Ceylon, Malacca, Borneo, China, Luzon und Ostafrika. Mber. 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New mammals from French Indo-China and Siam. Ann. Mag. nat. Hist. (9) 9 : 87-99- SHAW, T-H., WANG SUNG, Lu, C-K. & CHANG, L-K. 1966. A survey of the mammals of Hainan Island, China. Ada zootax. sin. 3 : 260-276. SNEATH, P. H. A. & SOKAL, R. R. 1973. Numerical taxonomy. San Francisco. SODY, H. J. V. 1936. Seventeen new generic, specific and subspecific names for Dutch East Indian mammals. Natuurk. Tijdschr. Ned.-Indie, 96 : 42-55. SOWERBY, A. DE CARLE. 1917. On a new species of shrew from Corea. Ann. Mag. nat. Hist. (8) 20 : 318. SPITZENBERGER, F. 1970. Zur Verbreitung und Systematik tiirkischer Crocidurinae (Insecti- vora, Mammalia). Annln. naturh. Mus. Wien. 74 : 233-252. 1971- Eine neue, tiergeographisch bemerkenswerte Crocidura (Insectivora, Mammalia) aus der Tiirkei. Annln. naturh. Mus. Wien 75 : 539-552. STROGANOV, S. U. 1956. Materials on the systematics of Siberian mammals. Trudy biol. Inst. zapad.-sib. Fil. Akad. Nauk. SSSR 1 : 3-10. TAYLOR, E. H. 1934. 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A bat and a new shrew from Koto-Sho (Botel Tobago). Annotnes zool. jap. 15 : 427-432 2 figs. TOMES, R. F. 1856. In Blyth, E. Memoir on the Indian species of shrews. Ann. Mag. nat. Hist. (2) 17 : 23. TROUESSART, E.-L. 1880. Description d'une espece nouvelle de musaraigne de la collection du Museum de Paris. Naturaliste, 1 (42) : 330. VAN PEENAN, P. F. D., RYAN, P. F. & LIGHT, R. H. 1969. Preliminary identification manual for mammals of South Vietnam. Washington. VINOGRADOV, B. S. 1958. On the structure of external genitalia in white-toothed shrews (Genus Crocidura, Insectivora, Mammalia) as a classificatory character. Zool. Zh. 37 (8) : 1236-1243. WANG, S. see SHAW, T-H., WANG SUNG, Lu, C-K. & CHANG, L-K. 1966. P. D. JENKINS Department of Zoology BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 A LIST OF SUPPLEMENTS TO THE ZOOLOGICAL SERIES OF THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) 1. KAY, E. ALISON. Marine Molluscs in the Cuming Collection British Museum (Natural History) described by William Harper Pease. Pp. 96 ; 14 Plates. 1965. (Out of Print.) 2. WHITEHEAD, P. J. P. The Clupeoid Fishes described by Lacepede, Cuvier and Valenciennes. Pp. 180 ; n Plates, 15 Text-figures. 1967. £4. 3. TAYLOR, J. D., KENNEDY, W. J. & HALL, A. The Shell Structure and Mineralogy of the Bivalvia. Introduction. Nuculacea-Trigonacea. Pp. 125 ; 29 Plates, 77 Text-figures. 1969. £4.50. 4. HAYNES, J. R. Cardigan Bay Recent Foraminifera (Cruises of the R.V. Antur) 1962-1964. Pp. 245 ; 33 Plates, 47 Text-figures. 1973. £10.80. 5. WHITEHEAD, P. J. P. The Clupeoid Fishes of the Guianas. Pp. 227 ; 72 Text-figures. 1973. £9-7O- 6. GREENWOOD, P. H. The Cichlid Fishes of Lake Victoria, East Africa : the Biology and Evolution of a Species Flock. Pp. 134 ; i Plate, 77 Text-figures. 1974. £375. Hardback edition £6. Printed in Great Britain by John Wright and Sons Ltd. at The Stonebridge Press, Bristol BS4 5NU . <£- . "* BIOLOGY AND FINE STRUCTURED OF CRYPTODIFFLUGIA OVIFORMIS (RHIZOPODEA : PROTOZOA) R. H. HEDLEY, C. G. OGDEN AND N. J. MORDAN BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 8 LONDON: 1977 f , . BIOLOGY AND FINE STRUCTURE OF CRYPTODIFFLUGIA OVIFORMIS j&^ (RHIZOPODEA : PROTOZOA) BY RONALD HENDERSON HEDLEY, COLIN GERALD OGDEN AND NICOLA JANE MORDAN Pp. 311-328; 6 Plates, 3 Text-figures BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 8 LONDON: 1977 THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be completed within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30, No. 8, of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation : Bull. Br. Mus. nat. Hist. (Zool.) ISSN 0007-1498 Trustees of the British Museum (Natural History), 1977 BRITISH MUSEUM (NATURAL HISTORY) Issued 27 January, 1977 Price £2.75 BIOLOGY AND FINE STRUCTURE OF , CRYPTODIFFLUGIA OVIFORMIS (RHIZOPODEA : PROTOZOA) By R. H. HEDLEY, C. G. OGDEN and N. J. MORDAN CONTENTS SYNOPSIS ........... 313 INTRODUCTION .......... 313 Previous work - taxonomy . . . . . . . . 314 Previous work - biology . . . . . . . . 315 MATERIAL AND METHODS . . . . . . . . . 316 DISTRIBUTION ........... 318 SHELL STRUCTURE AND COMPOSITION ....... 318 CYTOPLASM ........... 320 PSEUDOPODIA ........... 322 REPRODUCTION .......... 323 CYST ............ 326 ACKNOWLEDGEMENTS ......... 326 REFERENCES ........... 326 SYNOPSIS Cryptodifflugia oviformis, a cosmopolitan freshwater, moss and soil inhabiting testacean has been established in clonal culture with a doubling time of between 29 and 41 hours ; it is capable of reproducing in a 14 parts per thousand saline solution. The shell is shown to have two components, a thin outer organic layer and a thick inner, non-crystalline calcareous layer. The process of reproduction by simple division and the fine structure of the vegetative stage are described in detail. Ultrastructural features of special interest are the presence of calcareous inclusions in the mitochondria ; and a storage area for polysaccharide material within the cytoplasm. Cryptodifflugia operculata of Page (1966) is considered to be a synonym of Cryptodifflugia oviformis Penard (1890). INTRODUCTION THE main characters used in the classification of testate amoebae are the form, structure and composition of the shell and the form of the pseudopodia. The sheDs are generally reported as being either purely organic, arenaceous, or sili- ceous with occasional reports of forms secreting calcareous shells being unsub- stantiated. Until relatively recently information on the biology of many testate amoebae has been known only from infrequent observations on living animals, usually isolated as individuals during ecological or faunal surveys of freshwater habitats. The establishment and study of clonal cultures in this laboratory of certain species with siliceous shells (Hedley & Ogden, 1973, iQ74a ; Hedley et al., 1974) have contributed to our understanding of their biology and shell structure. 3H R- H. HEDLEY, C. G. OGDEN & N. J. MORDAN Recent ultrastructural studies on arenaceous forms (Netzel, iQ72a ; Eckert & McGee-Russell, 1974) and on organic forms (Griffin, 1972 ; Netzel, 19720, I975a, b) have contributed towards the understanding of their shell formation. Species attributed to the genus Cryptodifflugia Penard, 1890, are possibly the smallest and most widely distributed of testate amoebae. There has been some doubt amongst protozoologists regarding the structure and composition of the shell in these animals with previous descriptions (Penard, 1890 ; Deflandre, 1953 ; Grospietsch, 1964 ; Page, 1966) reporting it as chitinous, smooth, hyaline and rigid. The present work describes some aspects of the biology and shell structure of Cryptodifflugia oviformis Penard, 1890, an unusual testacean in that it is now reported as possessing a calcareous shell. Previous work - taxonomy The genus Cryptodifflugia was erected by Penard (1890) for the reception of a new species C. oviformis. Penard (1902) later amended his initial description and described two further species, C. compressa and C. sacculus. These three species were redescribed and illustrated by Playfair (1917) with five new species, C. minuta, C. angulata, C. valida, C. crenulata and C. pusilla, and four varieties, all from ponds or swamps in Australia. Zacharias (1903) reported a new species, C. turfacea, which sometimes had two apertures each having a distinct rim or collar. Another new species, C. voigti, described by Schmidt (1926) was observed to have an apertural rim and particles adhering to the shell surface. Deflandre (1953) emended the generic diagnosis of both Cryptodifflugia Penard, 1890 and Difflugiella Cash, 1904, using the degree of compression of the shell as a main character. These emendations included the transfer of the type species, C. oviformis, of the genus Cryptodifflugia to the genus Difflugiella. Several authors, Bonnet & Thomas (1955, 1960), Thomas (1959), Grospietsch (1964) and Schonborn (1965), have agreed with Deflandre's changes. For example, Thomas (1959) redescribed D. oviformis (Penard, 1890) and tabulated the previously reported measurements of this species. In a review of the genera Cryptodifflugia and Difflu- giella, Grospietsch (1964) agreed with Deflandre (1953) and gave keys to the species of both genera. Whilst Schonborn (1965) described four new species of Difflu- giella and redescribed D. crenulata (Playfair, 1917), D. oviformis (Penard, 1890) and D. voigti (Schmidt, 1926). Page (1966) reviewed the genus Cryptodifflugia and concluded that Deflandre's emendations were unjustified. He based his opinion on the original descriptions of Difflugiella and Cryptodifflugia which showed the former to have a flexible shell, whilst the latter had a rigid shell. Recent ultrastructural studies on Difflugiella sp. by Griffin (1972), and the present work, support the view that this feature is a good taxonomic character. Page (1966) used the presence of an operculum in the aperture of encysted animals of a new species C. operculata to distinguish it from C. oviformis. This feature had not been previously described and it is difficult to determine whether its omission in earlier descriptions was due to oversight, as the operculum is often difficult to BIOLOGY OF CRYPTODIFFLUGIA OVIFORMIS 315 see with the optical microscope, or to the absence of encysted animals in the material examined by other authors. As a result of an examination of the two available cultures of C. operculata and C. oviformis (from this laboratory), Dr Page has suggested in a personal communi- cation that the presence of an operculum may not be a good specific character, as it appears to be present in most encysted animals. Our own studies show that the structure of the shell and the fine structure of the cytoplasm in the two forms are indistinguishable. It is suggested therefore that C. operculata be regarded as a synonym of C. oviformis. Previous work - biology In his original description of Cryptodifflugia oviformis, Penard (1890) reported that the cytoplasm rilled the shell and contained one nucleus, a contractile vacuole close to the nucleus and 'numerous brilliant granules'. Similar 'brilliant' or 'coarse' granules found in C. operculata have been shown by Page (1966) to react positively with supravital Janus green from which he concluded that they are mitochondria. Penard (1890) observed that the form of the small number of pseudopodia of C. oviformis changed rapidly and later (Penard, 1902) described the pseudopodia as straight structures without ramifications. The arrangement and length of the pseudopodia in C. oviformis are described by Schonborn (1965), who also observed that the rate of locomotion varied from 34 to 40 (jim/min. According to Page (1966) there are between two and five pseudopodia in C. operculata that extend from a mass of cytoplasm outside the aperture. Both this mass and the cytoplasm appear to be free from coarse granules. Although these pseudopodia appear to be filose all seem to have rounded ends. The rate of locomotion of ten individuals ranged from 14 (jurn/min to 28 [jun/min. United individuals were described as 'conjugating tests' by Penard (1902) in which one shell always appears empty whilst the other shell, usually the larger, contains a rounded mass of cytoplasm separated from the aperture by a 'chitinous' diaphragm. Penard suggests that this could be a resting stage during which the animal constructs a new shell that gradually hardens. Playfair (1917) has described similar united individuals of C. oviformis as encysted forms. The process of binary fission has been described for C. operculata by Page (1966), in which most of the cytoplasm to form the daughter cell is extruded before nuclear division begins and is followed by the formation of a new shell around the daughter. Nuclear division from prophase to anaphase takes place in the aboral region of the parent and the daughter nucleus moves into the extruded cytoplasm in late telophase. Both the nuclear membrane and the nucleolus disappear before metaphase and no centrioles are seen. It also appears that most of the granules pass into the extruded cytoplasm and few are left in the parent. Penard (1890, 1902) described an encysted form of C. oviformis in which the cyto- plasm was concentrated and contained in the aboral region behind a cyst-membrane. A similar cyst has been described by Schonborn (1965). Page (1966) reported this type of cyst only once in C. operculata, but regularly found cysts in which the 316 R. H. HEDLEY, C. G. OGDEN & N. J. MORDAN aperture was sealed. In these latter forms the cytoplasm filled the shell, the contractile vacuole disappears and the aperture is blocked by a lens-shaped oper- culum. At encystment the operculum is either rejected from the shell or ingested within the cytoplasm. MATERIALS AND METHODS Cryptodifflugia oviformis was isolated from a sample of moss, Eurhynchium praelongum, taken from the bark of a tree at Cilpost Farm, Whitland, Carmarthen- shire, Wales, in July 1968. Rough cultures were obtained by aUowing small portions of this sample to stand, covered by a shallow layer of culture medium, at room temperature 18-20 °C. Agnotobiotic cultures were kept in small plastic containers on a thin substrate of agar (i per cent agar agar in distilled water) with a sterilized wheat grain added prior to setting and covered with a layer of culture medium. The medium was a 5 per cent (w/v) solution of sterilized soil extract in distilled water. Clonal cultures were established by isolating single active animals, and one such clone has been used subsequently to produce the working cultures. This clone has been deposited with, and is now maintained at, the Culture Centre of Algae and Protozoa, The Natural Environment Research Council, Cambridge, England (Reg. No. 1514/2). Specimens of C. operculata obtained from the Culture Centre for Algae and Protozoa (Reg. No. 1514/1), which were initially isolated by Page (1966), have been maintained in a manner similar to C. oviformis. Under these conditions C. oviformis remains active for approximately 4 weeks, after this time mobility decreases and encysted forms predominate. Cultures may also be maintained on an agar agar substrate, streaked with the bacterium Klebsiella pneumoniae, but without a covering fluid. Such cultures, kept on agar slopes in closed universal bottles at 9 °C, may be sub-cultured successfully after 6 months (Dr F. C. Page, personal communication) . Cultures have been established using a graded (v/v) series of seawater to fresh- water culture medium as the overlying culture fluid to the normal agar substrate. The initial experiments were made with i, 2, 5 and 10 per cent seawater to fresh- water mixtures, and in all cases active reproducing animals were observed. In subsequent experiments with higher concentrations of seawater it was found that cultures could be maintained in media up to and including 40 per cent seawater, which is the equivalent of a 14 parts per thousand saline solution. Optical microscopy Live animals were examined by both phase-contrast and bright-field illumination. Scanning electron microscopy Specimens taken from 4 or 5 weeks old cultures were cleaned by taking them individually through several changes of distilled water, using a single-hair brush. BIOLOGY OF CRYPTODIFFLUGIA OVIFORMIS 317 They were allowed to dry and then transferred onto a previously cleaned cover-slip. These prepared cover-slips were mounted on a standard Stereoscan stub using an electrically conductive paint, 'Silver Dag', prior to being coated evenly with gold. The stubs were examined on a Cambridge Stereoscan Mkll operating at 10 kV and the results recorded on Ilford H?4 film. Preparations to display pseudopodia were obtained by fixing specimens in situ using the following method. The agar substrate in a culture vessel was wetted with a minimal quantity of culture medium, and a small number of specimens from a fresh culture were placed on this surface. After a short time the animals resumed their normal activities. The vessel was then quickly flooded with 3 per cent glutaraldehyde in cacodylic acid buffer, and left for 15 minutes. The agar surface was washed with the same buffer and selected squares were cut out and allowed to air dry. These squares were mounted on a standard Stereoscan stub using Araldite and processed as previously described. Specimens from a culture vessel were air dried on pieces of spectographically standardized carbon rod for the analysis of inorganic chemical elements. Previous trials with this carbon rod had shown that it gave a minimal elemental background count. The pieces of rod were attached to Stereoscan stubs with Araldite. Stubs were then examined in a Cambridge Stereoscan coupled to an Ortec solid-state energy dispersive X-ray analyser, operating at 15 kV for 400 or 1000 seconds. Electron probe analysis was carried out on specimens taken from a culture vessel and allowed to air dry onto a Stereoscan stub with a short shaft. They were coated with a thin layer of carbon and examined in a modified Cambridge Geoscan, operating at 20 kV with a specimen current of o-i x io~7 amps. Transmission electron microscopy Specimens taken from cultures, approximately 2 or 3 weeks old, were fixed at room temperature for 12 minutes in i per cent glutaraldehyde in 0-025 M cacodylic acid buffer, followed by 7 minutes in 3 per cent glutaraldehyde in the same buffer. After several rinses in o-i M cacodylic acid buffer, they were post-fixed for 12 minutes in i per cent osmium tetroxide in distilled water. Some specimens were conventionally fixed, but before dehydration were treated with a chelating agent, 5% EDTA, for 15 minutes. The material was dehydrated, and embedded in Epon 812. Sections were cut on a Porter Blum MT2 ultramicrotome using a Du Pont diamond knife, stained in a saturated alcoholic solution of uranyl acetate and Reynold's lead citrate, and examined in an AEI 6B electron microscope operating at 60 kV. The results were recorded on Ilford EM6 plates. The periodic acid/thiosemicarbazide/silver proteinate technique (Thiery, 1967) was carried out on thin sections mounted on gold grids. After treatment with i per cent periodic acid for 20 minutes at room temperature followed by several washes in distilled water, the sections were left for either 40 minutes or 18 hours in a i per cent solution of thiosemicarbazide in 10 per cent acetic acid. They were washed thoroughly in several changes of 10 per cent acetic acid followed by several rinses in distilled water, before treatment with i per cent solution of silver 3i8 R. H. HEDLEY, C. G. OGDEN & N. J. MORDAN proteinate for 30 minutes in the dark. The grids were washed in distilled water before examination. Thick, unstained sections, coated with carbon, were analysed for elemental composition in an AEI EMMA-4 analytical electron microscope, equipped with a minilens, operating at 80 kV with a probe size of 0-06 [zA. DISTRIBUTION C. oviformis is commonly found in damp and wet mosses, standing water, on aquatic plants, various soils and forest litter. A list of locality records and references was given by Bonnet & Thomas (1960). Additional localities were given by several authors, Hoogenraad & Groot (1952), Stepanek (1963) and Bonnet (1966). The following list shows the geographically widespread distribution : EUROPE : England, Wales, Scotland, Ireland, France, Belgium, Holland, Germany, Iceland, Lapland, Italy, Czechoslovakia, Hungary, Bulgaria, Russia. NORTH AMERICA : United States of America and Canada. SOUTH AMERICA : Columbia and Chile. AFRICA : Cameroun and the Congo. ASIA : Siberia. AUSTRALASIA : Australia and New Zealand. SHELL STRUCTURE AND COMPOSITION Based on measurements from a hundred specimens the ovoid, rigid and smooth shells of C. oviformis vary in length from 14-5 to 22-2 (j,m and in diameter from 12-8 to 17-6 (Am. The single, terminal and circular aperture has a diameter of between 3-2 and 6-4 pun and is surrounded by a thin collar (PL i, fig. A). Ultrastructural observations show that the shell wall varies in thickness, between individuals, from 150 to 260 nm and that it is divided into two distinct layers. A thin outer organic layer, which is usually no more than 20 nm thick, and a thick inner layer of electron-dense calcined material. These layers appear to have a uniform thickness over most of the shell surface (Fig. i), but in the apertural region there is a slight thickening of the calcified layer and an extension of the organic layer to form a circular collar (Fig. 2). This organic collar is strengthened at the internal face by a continuation of the calcified layer (PI. i, fig. B). Examination of the complete shell wall at the ultrastructural level is difficult because the calcified layer is not penetrated by the embedding resin, and as a result is either fractured or torn in thin sections (PI. 2). Whole shells, examined with an Ortec X-ray analytical attachment to the Stereo- scan, showed significant elemental peaks for silicon, potassium and calcium, the last mentioned being pronounced. Semi-quantitative electron probe microanalysis of shells indicated that the calcium count-rate was high, and demonstrated a weak line for silicon corresponding to not more than i per cent. Sectioned material examined with the X-ray analytical electron microscope, EMMA, using a standard of calcium carbonate, gave significant intensities from the calcified layer. This BIOLOGY OF CRYPTODIFFLUGIA OVIFORMIS 319 microbody contractile vacuole nucleus 'storage' area Golgi mitochondrion dense endoplasmic reticulum food vacuoles FIG. i. Diagram of the vegetative stage of C. oviformis showing the arrangement of the main organelles. organic collar organic layer calcareous layer - shell wall FIG. 2. Diagram of the apertural collar with a section cut away to show the relationship of the organic and calcareous layers. 320 R. H. HEDLEY, C. G. OGDEN & N. J. MORDAN layer also gave significant intensities for phosphorus, using sodium dihydrogen orthophosphate as a standard. Further attempts to analyse the composition of the calcified layer, using whole shells for X-ray diffraction and sectioned specimens for electron diffraction, were inconclusive but suggest that this material is mainly amorphous. Dr K. M. Towe (Smithsonian Institution, Washington, D.C., U.S.A.), who kindly undertook the electron diffraction analysis, suggested that the material was either amorphous or exceptionally beam-sensitive as it was unstable. He ruled out the possibility of the beam sensitivity being associated with the presence of an oxalate because there was no inversion to calcium oxide. In conclusion, we suggest that in all probability the calcified layer is amorphous calcium phosphate. When whole specimens are immersed in either dilute nitric or hydrochloric acids or with 5% EDTA the major part of the shell dissolves. That which remains is the thin organic layer, delimiting the shape of the shell, and the organic thick- ening in the apertural region. In an attempt to demonstrate the fine structure of the organic layer, animals were fixed normally but before dehydration were decalcified by treatment with 5% EDTA for 10 minutes (PL i, fig. C). The organic layer revealed by this method is a membrane-like structure which is thickened and folded at the aperture to form a collar (PL i, fig. D). Specimens stained with the periodic acid/thiosemicarbazide/silver proteinate technique to demonstrate reactive hydroxyl groups show that the organic layer is composed of two thin, closely opposed, distinct membrane-like structures (PL i, fig. E), with a high carbo- hydrate content. Abnormal forms occur in cultures and represent about 3 per cent of the population. These are usually large forms, two or three times the size of a normal animal, and have two or more apertures (PL i, fig. F). The shell of these animals is characterized by an uneven distribution and thickness of the outer organic covering (PL i, fig. F ; PL 6, fig. C). CYTOPLASM The cytoplasm normally occupies the whole of the shell cavity (Fig. i ; PL 2) and is enclosed by a plasmalemma. The single nucleus is normally spherical, between 4-3 and 5-1 (xm in diameter, and is enclosed by two tripartite membranes. The nuclear matrix is granular with small, densely stained concentrations of chromatin scattered throughout and a dense nucleolus that is usually situated centrally. The nucleus is surrounded by a densely stained mass of granular endo- plasmic reticulum (Fig. i). This region of endoplasmic reticulum appears more electron-dense than the surrounding cytoplasm due to the concentration of ribosomes. Two or three contractile vacuoles may be present in the mid-body region (PL 3, fig. A). The area surrounding these vacuoles is free of ribosomes but has numerous small vesicles which are often continuous with the lumen of the vacuole. The contractile vacuoles lie at the periphery of the cytoplasm and dis- charge directly into the shell cavity. Specimens in 2-week-old cultures discharged their contractile vacuoles at periods that ranged from 25 to 33 seconds between systole and diastole. These periods increased in animals from 6-week-old cultures BIOLOGY OF CRYPTODIFFLUGIA OVIFORMIS 321 to range from 28 to 41 seconds. Numerous food vacuoles, which have a single unit membrane and may contain food organisms or waste material, occupy the apertural end of the cytoplasm (PI. 2). The mitochondria are ovoid or spherical, with tubular cristae, a dense granular matrix and they are distributed at random throughout the cytoplasm. Frequently large, spherical, electron-dense inclusions occur between the outer and inner mito- chondrial membranes (PL 3, figs A and B). These inclusions are naturally electron- dense in sections from specimens fixed in glutaraldehyde but without subsequent treatment with heavy metals, and show similar fracture patterns to those some- times seen in the electron-dense shell wall. We believe that these mitochondrial inclusions are the 'brilliant' or 'coarse' granules described by earlier workers. Analysis of these inclusions using the X-ray analytical electron microscope EMMA gave significant intensities for calcium and phosphorus which correspond to those produced by the shell. These calcareous inclusions dissolve in 5% EDTA. As many as 6 Golgi bodies may be present in one animal and they are usually associated with concentrations of granular endoplasmic reticulum. Each dictyo- some is composed of a stack of 3 to 6 saccules (PI. 3, fig. C) which are usually concave and centrally flattened, whilst the matrix around these saccules may be noticeably less dense than the surrounding cytoplasm. Condensations of a substance, which is electron-dense with normal staining procedures, occur in the central areas of the saccules. This material appears as if it may pass to the outer margins of the saccules where they form spherical protrusions, which are budded off as smooth membrane-bound vesicles (PI. 3, fig. C). At the inner face of the dictyosome, vesicles containing an electron-lucent material are formed (PI. 3, fig. E). These vesicles are slightly larger than those containing electron-dense material and are lined by a thin layer of an electron-dense material (PI. 3, fig. D). A third type of vesicle is often present in the dense granular endoplasmic reticulum (PI. 4, fig. A). These vesicles are large, usually have electron-lucent contents, but are occasionally seen to contain an electron-dense material (PI. 4, fig. D), and are often surrounded by a band of endoplasmic reticulum. Similar vesicles to these have been previously reported in Trinema linear e (Hedley & Ogden, I974a). On the basis of their distribution within the cytoplasm it is postulated that these three types of vesicles move through the cytoplasm along two distinct pathways. The large electron-lucent vesicles would pass through the central cytoplasm, whilst the smaller vesicles would pass around the less dense peripheral region to become incorporated at sites that are considered to be possible storage areas (PI. 4, figs B and D). In the trophic animal there may be as many as three such storage areas, usually found on a level or posterior to the nucleus in the aboral region (PI. 4, fig. C). These regions are electron-lucent and do not appear to have any limiting membrane. When sections are treated with the periodic acid/thiosemicarbazide/silver proteinate technique the storage areas stain strongly, which might suggest that they are regions rich in carbodyrate. The small electron-lucent vesicles also contain the stain, but in these it is confined to the lining of the vesicles (PI. 4, fig. B). The saccules of the Golgi apparatus are sometimes stained, as are the vesicles that are 322 R. H. HEDLEY, C. G. OGDEN & N. J. MORDAN detached at their margins, but this staining is less positive (PL 4, fig. B). Similar results after using this technique were obtained from specimens which had been decalcified with EDTA prior to embedding. Microbodies are present in most of the specimens examined. They are oval or spherical, varying between 0-25 and 0-44 [xm in diameter, have a dense matrix and a single unit membrane. They may contain either one or two tubular-like elements, between 19 and 24 nm in diameter (PL 4, fig. E), or a rectangular structure of parallel lines with a spatial distance of 8 nm between each line (PL 4, fig. F). Similar tubular-like elements in microbodies have been reported in the testate amoeba Trinema lineare (Hedley & Ogden, iQ74a), and in various Foraminifera by Hedley & Wakefield (in Hruban & Rechcigl, 1969) and Febvre-Chevalier (1971). Lattice-like structures within microbodies have been previously described in the Foraminifera Shepheardella taeniformis and Globigerina bulloides by Hedley et al. (1967) and Febvre-Chevalier (1971). PSEUDOPODIA In recent classifications (Loeblich & Tappan, 1961 ; Honigberg et al., 1964) the class Rhizopodea has been divided - using the form of the pseudopodia as the distinguishing character - into three subclasses ; the Lobosia, Filosia and Granulo- reticulosa. In both classifications the superfamily Cryptodiffmgiacea is included in the sub-class Lobosia. Previous studies (Penard, 1902 ; Page, 1966) demonstrate that the pseudopodia of C. oviformis appear to be intermediate in form between lobose and filose structures. Recognizing this difficulty, Deflandre (1953) erected a new sub-order the Reticulolobosa, but this has not been adopted in subsequent classifications. In actively moving specimens of C. oviformis the pseudopodia are numerous, relatively long and appear to taper and have small branches. All these features are normally associated with filose pseudopodia (PL 5, fig. A). Micrographs of whole animals which had been found with the pseudopodia extended (PL 5, fig. C) indicate that in addition to the main filose pseudopodia as seen with optical microscopy there are numerous ultrastructural pseudopodia or pseudopodial strands. These may or may not be connected to form a reticulum. These ultrastructural pseudopodia are similar to those seen in the granuloreticulose pseudopodia described for various foraminiferans by Hedley et al. (1967), Marszalek (1969) and Lengsfeld (1969). Each pseudopodium appears to consist of ground-plasm, limited by a unit mem- brane, often containing bands of thick microfilaments and small electron-dense concentrations (PL 5, fig. B). In addition, some sections of pseudopodia contain strands of endoplasmic reticulum, Golgi bodies, membrane-bound vesicles and mitochondria, some of which may contain electron-dense calcium inclusions. The bands of thick microfilaments vary from 25 to 33 nm in diameter and are about 0-4 |zm long (PL 5, fig. B). Microfilaments are sometimes found concentrated to form adhesion plaques at points of contact between opposing pseudopodia (PL 5, fig. D). We suggest that this reaction is probably restricted to contact between BIOLOGY OF CRYPTODIFFLUGIA OVIFORMIS 323 pseudopodia from different animals. Similar adhesion plaques have been reported in species of Euglypha by Hedley & Ogden (1973, 19740). The fine structure of the pseudopodia of C. oviformis is similar to that reported for other testate amoebae (Wohlman & Allen, 1968 ; Griffin, 1972 ; Eckert & McGee-Russell, 1973 ; Hedley & Ogden, 1973, I974a) and naked amoebae (Comly, 1973 ; Taylor et al., 1973 ; Rinaldi & Hrebenda, 1975) in having microfilaments as a structural element. Wohlman & Allen (1968) and Eckert & McGee-Russell (1973) suggest that both thin and thick microfilaments are associated with pseudopodia extension and contraction in Difflugia, and similar studies on slime moulds and naked amoebae by Komnick et al. (1972, 1973) suggest that the uptake and release of calcium ions by microfilaments plays an important role in cytoplasmic streaming. Another role for both types of microfilaments, that of cellular wound healing, has recently been suggested by Jeon & Jeon (1975) from studies on Amoeba proteus. REPRODUCTION The length of time required to double the population (doubling time) was esti- mated from three identical cultures established and maintained under similar conditions. Growth curves produced from observations made at regular intervals showed that the doubling time is between 29 and 41 hours. The formation of a daughter cell by binary fission begins with an elongation of the cytoplasm of the parent shell to form a thick trunk which emerges from the aperture (Fig. 3-1). This trunk expands until the cytoplasm has reached about half the size of the parent shell. There is then a slight contraction, followed by further expansion until it reaches a size equivalent to that of the parent shell. At about this time the first indication of the transfer of cytoplasmic organelles becomes apparent, with the rapid passage of the dense granules into the daughter. The parent cytoplasm contracts slightly and is less active for a period of approxi- mately i minute. The daughter then collapses slightly and the granules return to the parent. The rapid movement of the granules between the parent and daughter is repeated, and finally most of the granules are passed into the daughter with only one or two remaining in the parent (Fig. 3-6). The cytoplasm in the parent is reduced, to about one-third its normal volume and is situated at the aboral region of the shell, whilst the daughter cell appears to have reached full size. The connection between the two animals is reduced to a thin thread (Fig. 3-8). As the parental cytoplasm moves towards the apertural region of the shell, the connection between the parent and daughter is severed. Pseudopodia emerge from the parent and the two animals separate, the daughter remaining quiescent for periods in excess of 45 minutes from the time of separation. The process of granular exchange takes place between 15 and 25 minutes after the first stages of division. Contractile vacuoles appear in the daughter after about 20 minutes, and the nuclei appear in both animals after about 30-35 minutes. Often animals appear to start dividing only to cease at various stages, including stages that are almost half the parental size. These abortive products are rejected R. H. HEDLEY, C. G. OGDEN & N. J. MORDAN start 22 mins. 15 mins. 8 23 mins. 16-5 mins. 24 mins. 10 1 7 mins. # 29 mins. 11 18 mins. ^^-^' 35 mins. 19 mins. FIG. 3. Diagram showing the progressive stages in the formation of a daughter cell. At stage i the animal appears to rest for up to 15 minutes. Stages 2-7 represent the cyto- plasmic contractions and rapid interchange of dense granules between the parent and daughter. Stage 5 shows the first indication of a thin shell (pecked line) surrounding the daughter, although this is probably present at an earlier stage. By stage 9 the cytoplasm has been divided between the parent and daughter and at stage 12 the parent moves away. BIOLOGY OF CRYPTODIFFLUGIA OVIFORMIS 325 by the parent to become isolated, rounded lumps of cytoplasm, which are often seen in the cultures. The first indication of a shell surrounding the newly formed daughter cell is a thin organic layer, indications of which are first seen after the start of granular exchange between parent and daughter. Nevertheless, it is possible that this organic layer is present around the initial extrusion of cytoplasm at the beginning of division. The formation of the shell in C. oviformis is probably dependent on the accumulation within the parent of reservoirs of an acid mucopolysaccharide and calcium ions. The organic material we believe is produced by both the Golgi complexes and the dense endoplasmic reticulum, and is stored in the cytoplasm at the storage areas (PI. 3, fig. A ; PL 4, fig. B). The fusion of vesicles to form storage areas appears to represent a process of intake and assimilation. There is no evidence to suggest how this material is distributed from this reservoir, but the storage areas are absent in young daughter cells. A similar aggregation of vesicles rich in poly- saccharides has been demonstrated by Holtrop (1972) in cartilage cells of the epiphy- seal plate, where the protein polysaccharide complex was considered to assemble before it was extruded into the matrix. Calcification of the shell appears to start shortly after division. During the early stages of calcification the shells often have an irregular outline (PL 6, fig. B), and they appear to be flexible. This initial shell wall has a diffuse appearance, with some small concentrations of electron-dense material on the inner surface (PL 5, fig. E). When the parent and daughter cells have finally divided they separate and the aperture of the daughter is sealed by a thin, fibrous organic membrane (PL 6, fig. A). In the cytoplasm of the daughter cell the usual membrane-limited profiles of endoplasmic reticulum are absent and it appears to be a mass of free ribosomes. The small circles of ribosomes that are seen (PL 5, fig. E) are possibly the initial stages in the reformation of these profiles. In C. oviformis it has been possible to locate only one site where calcium is con- centrated. This is between the outer and inner mitochondrial membranes where it is stored as spherical inclusions of amorphous calcium phosphate (PL 3, fig. B). Most of these mitochondria pass at division into the daughter cell. Several young animals examined shortly after division contain mitochondria without inclusions and in such cases the matrix of the mitochondria appears to be homogeneous, the cristae are not readily resolved, and the outer mitochondrial membrane is seen to have small swellings (PL 5, fig. F). It has been established by Wasserman & Kallfelz (1970) that calcium ions are actively transported across mitochondrial membranes, and a model for this transport has been proposed by Rasmussen (1966). Previous investigations (Greenawalt et al., 1964 ; Greenawalt & Carafoli, 1966 ; Thomas & Greenawalt, 1968) on calcium-rich granules in mitochondria suggest that formation takes place in three stages. First at the inner membrane surfaces, especially on the cristae, followed by free granules in the matrix and finally the granules grow by accumulation. Opinions differ over the factors that induce concentrations of calcium in the mitochondria of the ciliated protozoan Spirostomum ambiguum, where they have been considered to be a mobile endoskeleton (Bien, 1967), a metabolic store of 326 R. H. HEDLEY, C. G. OGDEN & N. J. MORDAN phosphate (Pautard, 1970), or concentrations of waste calcium (Jones, 1967, 1969). But in vertebrates it has been suggested that similar mitochondrial inclusions to those demonstrated here in C. oviformis are involved in mineralization of deer antlers (Sayegh et al., 1974) and eggshell formation in chickens (Hohman & Schraer, 1966). CYST After 4 or 5 weeks encysted animals appear in cultures. Such animals have a distinct operculum forming a seal across the aperture (PL 6, fig. E) and the ultra- structure of this operculum is a finely fibrillar matrix interspersed with small naturally electron-dense bodies (PI. 6, fig. D). Results from periodic acid-Schiff tests carried out by Page (1966) suggest that the operculum is mainly of a poly- saccharide nature. ACKNOWLEDGEMENTS We would like to thank Dr F. Page of the Culture Centre for Algae and Protozoa, NERC, Cambridge, for his helpful discussions on the identification of C. oviformis, Dr K. M. 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Struktur und Ultrastruktur von Arcella vulgaris var. multinucleata (Rhizopoda, Testacea). Arch. Protistenk. 117 : 219-245. - I975b. Morphologic und Ultrastruktur von Centropyxis discoides (Rhizopoda, Testacea). Arch. Protistenk. 117 : 369-392. PAGE, F. C. 1966. Cryptodifflugia operculata n. sp. (Rhizopodea: Arcellinida, Cryptodifflu- giidae) and the status of the genus Cryptodifflugia. Trans. Am. microsoc. Soc. 85 : 506-515. PAUTARD, F. G. E. 1970. Calcification in unicellular organisms. In Biological Calcification : Cellular and Molecular Aspects, pp. 105-201. North-Holland, Amsterdam. PENARD, E. 1890. Etudes sue les Rhizopodes d'eau douce. Mem. Soc. Phys. Hist. nat. Geneve 31 : 1-230. — 1902. Faune Rhizopodique du Bassin du Ldman. Geneva. 700 pp. PLAYFAIR, G. J. 1917. Rhizopods of Sidney and Lismore. Proc. Linn. Soc. N.S.W. 42 : 328 R. H. HEDLEY, C. G. OGDEN & N. J. MORDAN RASMUSSEN, H. 1966. Mitochondrial ion transport : Mechanism and physiological signi- ficance. Fed. 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Les Thecamoebiens muscicoles et terricoles : notions d'6cologie generate et comparative. P.-v. Soc. linn. Bordeaux 89 : 27-53. THOMAS, R. S. & GREENAWALT, J. W. 1968. Microincineration, electron microscopy, and electron diffraction of calcium phosphate loaded mitochondria. /. Cell Biol. 39 : 55-76. WASSERMAN, R. H. & KALLFELZ, F. A. 1970. Transport of calcium across biological mem- branes. In Biological Calcification: Cellular and Molecular Aspects, pp. 313-345. North- Holland, Amsterdam. WOHLMAN, A. & ALLEN, R. D. 1968. Structural organization associated with pseudopod extension and contraction during cell locomotion in Difflugia. J. Cell Sci. 3 : 105-114. ZACHARIAS, O. 1903. Zurr Kenntnis der niederen Flora und Fauna holsteinischer Moorsumpfe. ForschBer. biol. Stn Plon 10 : 223-289. DR R. H. HEDLEY C. G. OGDEN NICOLA J. MORDAN BRITISH MUSEUM (NATURAL HISTORY) CROMWELL ROAD LONDON SW7 560 PLATE i Cryptodifflugia oviformis FIG. A. Specimen to illustrate the circular aperture and the apertural collar (arrowed) . x 2500 FIG. B. Section showing one side of the apertural collar. Note that the calcareous layer continues as a border (arrow) to the organic collar (oc). x 30 100 FIG. C. Section through the aperture of a specimen treated with EDTA to remove the calcareous layer. Note the thin organic layer (ol) and thickened collar (oc). x 5800 FIG. D. Section through aperture of specimen treated with EDTA, to show the extension of the organic layer (ol) to form the collar. x 27 ooo FIG. E. Section of shell wall stained with thiosemicarbazide/silver proteinate, showing silver deposited at the organic layer (ol). The gap (g) represents the calcareous layer removed during the staining technique. x 24 ooo FIG. F. Abnormal shell showing irregular patterning of the shell and two apertural openings (arrowed). x 1600 Bull. Br. Mus. nat. Hist. (Zool.) 30, 8 PLATE i PLATE 2 Cryptodifflugia oviformis Section through the aperture of a whole specimen to show the nucleus (n), Golgi bodies (G), granular endoplasmic reticulum (ger) and food vacuoles (fv). x 8600 Bull. Br. Mus. nat. Hist. (Zool.) 30, 8 PLATE 2 PLATE 3 Cryptodifflugia oviformis FIG. A. Section to show the nucleus (n), contractile vacuoles (cv), storage area (sa) and mitochondria containing calcareous inclusions (me) . x 7800 FIG. B. Section of a mitochondrion (m) with a calcareous inclusion. x 15 600 FIG. C. Section through a Golgi body to illustrate the formation of vesicles with electron- dense contents at the margin of the saccules (arrowed). x 44 600 FIG. D. Section showing membrane-bound vesicles (mbv) with a thin electron-dense lining and an electron-lucent centre. x 44 600 FIG. E. Two Golgi bodies (G) in a region of dense endoplasmic reticulum. Note the presence of membrane-bound vesicles (mbv) at the inner face of the saccules. x 30 100 Bull. Br. Mus. nat. Hist. (Zool.) 30, 8 PLATE 3 PLATE 4 Cryptodifflugia oviformis FIG. A. Section to illustrate a large electron-lucent vesicle (Iv) and the associated band of endoplasmic reticulum (er). x n 500 FIG. B. Section stained with thiosemicarbazide/silver proteinate, showing silver deposited at the storage areas (sa), Golgi bodies (G) and the membrane-bound vesicles (mbv). x 10 ooo FIG. C. Transverse section showing the position of the storage areas (sa), food vacuole (fv), contractile vacuoles (cv) and nucleus (n) . x 7800 FIG. D. A typical storage area showing three types of vesicles, electron-dense (ed), membrane-bound (mbv) and large vesicles (Iv). Note that the large vesicles contain an electron- dense material. x 13 500 FIG. E. Section through a microbody with tubular elements. x 75 600 FIG. F. Section through a microbody containing a lattice-like structure. x 90 600 Bull. Br. Mus. nat. Hist. (Zool.) 30, 8 PLATE 4 PLATE 5 Cryptodifflugia oviformis FIG. A. Specimen on an agar surface to illustrate the pseudopodia extended. x 960 FIG. B. Section through a pseudopodium containing mitochondria (m), bundles of micro- filaments (mf ) and small electron-dense concentrations (arrowed) . x 44 600 FIG. C. Section of a specimen to illustrate the range and abundance of pseudopodia. X4300 FIG. D. Section through two pseudopodia showing that the opposed membranes are parallel in the region of contact. Note the thickening of those membranes (arrowed) and the bundles of microfilaments (mf). x 15 ooo FIG. E. Section of partially calcified daughter cell, showing the organic layer (ol) with small concentrations of electron-dense material at the inner surface. x 20 100 FIG. F. Section of a mitochondrian with a homogeneous matrix and apparent absence of cristae. A swelling of the membrane is arrowed. x 30 100 Bull. Br. Mus. nal. Hist. (Zool.) 30 PLATE 6 Cryptodifflugia oviformis FIG. A. Section through the aperture of a partially calcified daughter cell. Note the thin shell wall (sw), the band of fibrillar organic material (fm) sealing the aperture and the vesicles containing electron-dense material (arrowed). x 20 100 FIG. B. Section of a young daughter cell illustrating the irregular outline of the uncalcified shell. x 5800 FIG. C. Section of shell wall of abnormal specimen. Note the folded organic layer (ol) and the small concentrations of calcified material on the inner surface (arrowed). x 30 100 FIG. D. Section through an aperture (ap) sealed with an operculum (op). x 28 400 FIG. E. Light micrograph showing the operculum (op) in the apertural opening. x 2000 Bull. Br. Mus. nat. Hist. (Zool.) 30, 8 PLATE 6 sw A LIST OF SUPPLEMENTS TO THE ZOOLOGICAL SERIES OF THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) 1. KAY, E. ALISON. Marine Molluscs in the Cuming Collection British Museum (Natural History) described by William Harper Pease. Pp. 96 ; 14 Plates. 1965. (Out of Print.) 2. WHITEHEAD, P. J. P. The Clupeoid Fishes described by Lacepede, Cuvier and Valenciennes. Pp. 180 ; n Plates, 15 Text-figures. 1967. £4-80. 3. TAYLOR, J. D., KENNEDY, W. J. & HALL, A. The Shell Structure and Mineralogy of the Bivalvia. Introduction. Nuculacea-Trigonacea. Pp. 125 ; 29 Plates, 77 Text-figures. 1969. £5-40. 4. HAYNES, J. R. Cardigan Bay Recent Foraminifera (Cruises of the R.V. Antur] 1962-1964. Pp. 245 ; 33 Plates, 47 Text-figures. 1973. £11-90. 5. WHITEHEAD, P. J. P. The Clupeoid Fishes of the Guianas. Pp. 227 ; 72 Text-figures . 1 973 . £10-65. 6. GREENWOOD, P. H. The Cichlid Fishes of Lake Victoria, East Africa : the Biology and Evolution of a Species Flock. Pp. 134 ; i Plate, 77 Text-figures. 1974. £3-75. Hardback edition £6. Printed in Great Britain by John Wright and Sons Ltd. at The Stonebridge Press, Bristol BS4 5NU ( 2iJANlOT THE LARVAL AND POST-LARVAL^^ DEVELOPMENT OF THE SCORPION SPIDER CRAB, INACHUS DORSETTENSIS (PENNANT) (FAMILY : MAJIDAE), REARED IN THE LABORATORY R. W. INGLE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 9 LONDON: 1977 V 25 JAN 1977 THE LARVAL AND POST-LARVAL .LIBRARY DEVELOPMENT OF THE SCORPION SPI CRAB, INACHUS DORSETTENSIS (PENNANT) (FAMILY : MAJIDAE), REARED IN THE LABORATORY BY R. W. INGLE Pp. 329-348 ; 10 Text-figures BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) ZOOLOGY Vol. 30 No. 9 LONDON: 197? THE BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY), instituted in 1949, is issued in Jive series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be com- pleted within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 30, No. 9, of the Zoology series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation Bull. Br. Mus. nat. Hist. (Zool.) ISSN 0007-1498 Trustees of the British Museum (Natural History), 1977 BRITISH MUSEUM (NATURAL HISTORY) Issued 27 January, 1977 Price £2.00 This issue ends Volume 30. THE LARVAL AND POST-LARVAL DEVELOPMENT OF THE SCORPION SPIDER CRAB, INACHUS DORSETTENSIS (PENNANT) (FAMILY : MAJIDAE), REARED IN THE LABORATORY By R. W. INGLE INTRODUCTION THE Scorpion Spider Crab, Inachus dorsettensis (Pennant), occurs from Norway, through the north Atlantic to the Mediterranean and along the west and South African coasts as far as Natal, being confined to littoral waters to depths of 550 m (Monod, 1956 : 529). It is reported from hard to muddy substrates (Christiansen, 1969 : 102) although in British waters it has been taken chiefly in areas of sandy- mud (Marine Biological Association, 1957 : 260 ; Hartnoll, 1963 : 434). In British waters this species breeds throughout the year (Lebour, 1928 : 502). Although adults of the three British Inachus species are readily distinguishable from each other, the larval and post-larval stages cannot be reliably identified at present because of the lack of adequate descriptions. Recently I. dorsettensis was reared to ninth crab stage in the laboratory and the early developmental stages are described in detail below. MATERIAL AND METHODS Larvae were hatched from crabs collected on or near the Eddystone Grounds, off Plymouth, Devonshire, England, and were reared using the method described by Rice & Ingle (1975 : 104). Larvae and moults were preserved in 70% alcohol and in 5% buffered formal- saline. Dissections were made in polyvinyl-lactophenol/lignin pink medium. Drawings and measurements were made with the aid of a camera lucida. The measurements taken were : dorsal spine length (D.S.) = distance between tip of dorsal spine and rostrum, and carapace length (C.L.) = distance between base of eyestalk and posterio-lateral margin of carapace. Between 5 and 10 suitable specimens of each stage were measured. Sizes given under Dimensions are those for the smallest and the largest specimens. RESULTS Most females hatched their total brood within a period of 36 hours ; a few took up to 48 hours. All successfully reared larvae hatched as free-swimming zoeae. The small percentage that hatched as pre-zoeae all died within 24 hours. 332 R. W. INGLE FIG. i. Inachus dorsettensis, lateral and frontal aspects of zoeal stages : (a), (b) first zoea and (c), (d) second zoea ; (e) basal part of dorsal spine of first zoea ; (f ) majid spine of first zoea. Scales in millimetres. LARVAL DEVELOPMENT OF INACHUS DORSETTENSIS 333 FIG. 2. Inachus dorsettensis, (a), (b) antennule ; (c), (d) antenna ; (e), (f ) mandible ; (g), (h) maxillule ; (i), (j) maxilla of : (a), (c), (e), (g), (i) first zoea and (b), (d), (f), (h), (j) second zoea. Scales in millimetres. 334 R- W. INGLE DESCRIPTIONS Inachus dorsettensis (Pennant) LARVAL REFERENCES. Inachus scorpio Claus, 1876 : Taf. X, fig. 8 (ist zoea) ; non Inachus scorpio Cano, 1893 : Taf. 35, fig. 7 (ist zoea) = /. thoracicus (Roux) ; Inachus dorsettensis Lebour, 1927 : 795 ; PI. I, figs i, 4-6 (pre-zoea), fig. 7 (ist zoea), PI. II, figs i, 4-7, PL IV, figs i, 3 (and zoea), PL II, fig. 10, PL III, figs i, 7, 8, PL IV, figs 2, 4 (megalopa), PL III, fig. 8 (ist- 3rd crab) ; 1928 : 546, PL III, fig. 5 (ist zoea, col. fig.), PL XV, fig. 4 (ist crab), fig. 5 (2nd crab) ; Heegaard, 1963 : 471 (ist zoea), PL XVII (coloured fig.), text-figs 70-76. FIRST ZOEA Dimensions : D.S. 1-9-2-0 mm ; C.L. 0-9-1-0 mm. Carapace (Fig. la, b) : Dorsal spine well developed, apically curved, armed with minute spinules most numerous at base (Fig. le). Rostral and lateral spines absent. Dorso-median elevation (D.E.) prominent ; majid spine (M.S.) plumose, arising from inner ventral carapace margin and well developed (Fig. if), posterio- ventral margin of carapace spinulate. Eyes : Partly fused to carapace. Antennule (Fig. 2a) : Unsegmented with two terminal aesthetascs and 2 setae. Antenna (Fig. 2c) : Spinous process (S.P.) about f length of dorsal spine, distal £ invested with minute spinules. Exopod as long as spinous process with 2 median spines, distal \ spinulate. Endopod about ^ length of spinous process. Mandible (Fig. 2e) : Incisor and molar process developed, palp absent. Maxillule (Fig. 2g) : Endopod 2-segmented, distal segment about 4x length of proximal and with 4 distal setae ; basal endite (B.E.) with 5 setosed spines and 2 setae, coxal endite with 7 plumose setae. Maxilla (Fig. 21) : Endopod (E.N.) narrow, apex truncate with 3 long and i (outer- most) short plumose setae ; basal endite (B.E.) bilobed with 7-8 plumose setae ; coxal endite bilobed with 7 plumose setae, inner margin invested with fine setules. Scaphognathite with 10 plumose setae, distal one very stout, posterior lobe short. First maxilliped (Fig. 3a) : Basis with 9 setae (arranged 2, 2, 2, 3), endopod 5- segmented with 3, 2, i, 2, 4 + i setae respectively ; exopod incipiently 2-segmented, distally with 4 terminal plumose setae. Second maxilliped (Fig. 3b) : Basis devoid of setae, endopod 3-segmented with o, i, 3 + i setae respectively, distal segment about 3 x length of proximal, exopod incipiently segmented, distally with 4 plumose setae. Third maxilliped (Fig. 30, MX) : Represented as a small unsegmented bud. Peraeopods (Fig. 30) : Conspicuous, ist incipiently chelate, 2nd~5th unsegmented as terminally acute finger-like projections. Abdomen (Fig. 4a, b) : 5-segmented + telson. Segments 2-5 with incipient pleopod buds ; 2nd segment with pair of forwardly directed dorso-lateral processes, segments 3-5 each with a pair of long posterior dorso-lateral spines and with posterior ventro- lateral margins rounded to truncate. Posterio-dorsal margin of segments 2-5 each with a pair of small setae. Telson forks long, not diverging posteriorly, lateral spines (L.S.) long, nearly % length of forks, both invested with minute spinules ; each half of telson posterior margin convex, with 3 plumose setae. LARVAL DEVELOPMENT OF INACHUS DORSETTENSIS 335 FIG. 3. Inachus dorsettensis, (a), (d) first maxilliped ; (b), (e) second maxilliped ; third maxilliped and peraeopods of : (a)-(c) first zoea and (d)-(f) second zoea. in millimetres. (c), (f) Scale 336 R. W. INGLE FIG. 4. Inachus dorsettensis, abdomen, dorsal (a), (c) and lateral (b), (d) aspects of (a), (b) first zoea and (c), (d) second zoea ; (e) right half of telson of second zoea ; (f ) anten- nule of megalopa ; (g) antennule of first crab. Scales in millimetres. LARVAL DEVELOPMENT OF INACHUS DORSETTENSIS 337 SECOND ZOEA Dimensions : D.S. 1-7-1-8 mm ; C.L. 1-2-1-3 mm. Carapace (Fig. ic, d) : Dorsal spine slightly more curved and shorter than in first stage, dorso-median elevation more pronounced and now with 2 rows of 3 setae ; rostrum pronounced, ocular eaves developed. Eyes : Now stalked. Antennule (Fig. 2b) : Now with 3 terminal aesthetascs and 3 setae. Antenna (Fig. 2d) : Endopod now about \ length of spinous process. Mandible (Fig. 2f ) : Distal margin of incisor process cut into rounded teeth. Maxillule (Fig. 2h) : Outer margin of basal endite now with a plumose seta, distal margin now with 3 setae. Maxilla (Fig. 2J) : Outermost plumose seta of endopod longer than in first stage ; basal endite with 9 plumose setae ; scaphognathite with 17 plumose setae, distal one no longer stout. First maxilliped (Fig. 3d) : Exopod now with 6 terminal plumose setae. Second maxilliped (Fig. 3e) : Exopod now with 6 terminal plumose setae. Third maxilliped (Fig. 3f ) : Now a pronounced bilobed bud. Peraeopods (Fig. 3f ) : 2nd~5th incipiently segmented. Abdomen (Fig. 40, d) : Segments 2-5 with well-developed pleopod buds, dorso- lateral processes on 2nd segment longer than in first stage and with terminal spinules ; posterior dorso-lateral spines shorter than in first stage ; telson forks diverging posteriorly, spinules (Fig. 46) conspicuous. MEGALOPA Dimensions : C.L. 1-1-1-2 mm. Carapace (Fig. loa) : Longer than broad, narrowing anteriorly. Front with a pair of widely spaced anteriorly directed acute frontal horns and medially with an obtuse protuberance ; protogastric region with 3 transverse low tubercules, outer- most 2 spined ; cardiac with 3 spines transversely placed, intestinal with a low posteriorly placed tubercule. Eyes : Large and long, cornea well developed. Antennule (Fig. 4f) : Peduncle 3-segmented, exopod (EX) not demarcated from peduncle, with 4 aesthetascs and 2 setae, endopod vestigial. Antenna (Fig. 5d) : 6-segmented, flagellum not demarcated from peduncle. First segment with ventrally directed spine and outwardly directed obtuse process, 3rd segment with i seta, 5th segment longest with 4 terminal setae, 6th with 2 long and i short terminal setae. Mandible (Fig. 5a) : Incisor process well developed, molar reduced, now with 3- segmented mandibular palp, distal segment with 1-2 setae. Maxillule (Fig. 5b) : Endopod now reduced, unsegmented ; basal endite with 6 spines and 5-7 setae, spines thinner than in zoeal stages. Maxilla (Fig. 5c) : Endopod reduced to terminally acute process ; basal endite slightly bilobed with 9-10 plumose setae ; coxal endite slightly bilobed with 5 plumose setae. Scaphognathite with 22 plumose setae shorter than in zoeal stages. First maxilliped (Fig. 6a) : Coxal endite (C.E.) bilobed, invested with i and 4 setae 338 R. W. INGLE FIG. 5. Inachus dorsettensis, (a) mandible, (b) maxillule, (c) maxilla and (d) antenna of megalopa ; (e) antenna and (f ) endopod of maxilla of first crab. Scale in millimetres. LARVAL DEVELOPMENT OF INACHUS DORSETTENSIS 339 FIG. 6. Inachus dorsettensis, first maxilliped of (a) megalopa and (b) first crab ; second maxilliped (c) of megalopa and (d) endopod of second maxilliped of first crab. Scale in millimetres. 340 R. W. INGLE respectively ; inner margin of basis (B.S.) with 5 setae. Exopod long, stout, 2- segmented, distally with 4 long terminal plumose setae ; endopod curved with 1-2 subapical setae, epipod short, bilobed. Second maxilliped (Fig. 6c) : Basal and coxal segments not separated, endopod 5- segmented, ist segment not completely demarcated from 2nd, 3rd with i, 4th with 3 dorso-external setae, 5th with 4 setosed spines. Exopod long, stout, 2-segmented, distal segment with 4 plumose setae, epipod short, bilobed. Third maxilliped (Fig. 7a) : Basis slightly demarcated from coxa, inner margin of coxal segment with i spine and i seta, ischium with 3-5 acute spines or processes and 6 setae with additional 2 on outer surface ; merus with a small blunt anterio- internal spine on inner surface, merus to dactylus setosed as shown in figure. Peraeopods, cheliped (Fig. 7c) : Inner margin of ischium/basis with 3 stout curved spines, merus with 3 stout spines, carpus inner margin with i small spine, propodus distal half, inner margin sharp, slightly cristate, setal investment as shown in figure. Peraeopods 2-5 (Fig. 8b) dactylus distally spinulate, much longer than propodus + carpus, basis of peraeopods 2-3 with stout curved spine, merus of peraeopods 2-4 and sometimes ischium with long spines decreasing in size distally ; setal and spinule investment as shown in Fig. 8b. Abdomen (Fig. 8a, loa) : Sub-cylindrical 5-segmented + telson. Posterio-dorsal margins of segments 2-5 with pair of acute spines (P.D.) decreasing in size on suc- cessive segments ; segment 3 with i pair and 4 and 5 with 2 pairs of additional minute spinules ; dorsal surface of segments 2 and 3 with a median spine. A pair of well-developed pleopods on segments 2-5, exopods (Fig. gc) long, each with 8 terminal plumose setae ; endopod short with 2 coupling hooks on each pleopod. FIRST CRAB Dimensions : C.L. 1-4-1-5 mm. Carapace : Longer than broad, narrowing anteriorly, invested with numerous setae of varying lengths (Fig. lob). Anteriorly directed frontal horns broader than in megalopa, apices setosed. Hepatic and outer epibranchial regions swollen, each with a spine ; meso-metagastric and cardiac regions swollen, latter with a pair of small tubercules. Eyes : Large and broad, cornea well developed. Antennule (Fig. 4g) : Exopod now with 3 incipient segments, terminal with 5 aesthetascs and one seta ; endopod with 3 incipient segments, terminal with 3 setae. Antenna (Fig. 5e) : Now y-segmented, flagellum not demarcated from peduncle ; ist segment longest, inner margin with ventrally directed spine shorter than in megalopa and 2 additional smaller spines on inner margin, outer margin with 2 plumose setae ; 2nd and 3rd segments each with 2 setae, 5th with i, 6th with 3, 7th with apex indistinctly segmented. Mandibles, maxilhde and maxilla : As in megalopa. First maxilliped (Fig. 6b) : Coxal segment with 8 setae, no longer bilobed, demar- cated from basis which has 11-12 setae, endopod distally expanded into broad lobe with 2-3 marginal setae, epipod longer than in megalopa with 1-2 setae. LARVAL DEVELOPMENT OF INACHUS DORSETTENSIS 341 FIG. 7. Inachus dorsettensis, third maxilliped of (a) megalopa and (b) first crab ; cheliped of (c) megalopa and (d) first crab. Scales in millimetres. 342 R. W. INGLE FIG. 8. Inachus dorsettensis, (a) abdomen (b) peraeopods 2-5 of megalopa ; abdomen (c) of second crab, (d) of third crab cj, (e) of fourth crab ? and (f ) of fourth crab