Geothelphusa, Stimpson, 1858
publication ID |
https://doi.org/ 10.1080/00222930600773378 |
publication LSID |
lsid:zoobank.org:pub:6F322CD1-99BC-4C38-9D41-F1352981F10D |
persistent identifier |
https://treatment.plazi.org/id/164A7D59-1D7F-FFAD-22F8-FF51708C27A0 |
treatment provided by |
Carolina |
scientific name |
Geothelphusa |
status |
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Geothelphusa View in CoL grandioIJata new species
( Figures 4 View Figure 4 , 5a View Figure 5 , 8b View Figure 8 )
Potamon (Geothelphusa) leυicerυix: Miyake and Minei 1965, p 377.
Geothelphusa View in CoL leυicerυix: Minei 1968, p 99, Figure 11; Minei 1973, p 211, Figures 6 View Figure 6 , 9 View Figure 9 (C, D) (partim); Sakai 1976, p 558 (English text), 346 (Japanese text) (partim); Gima and Shokita 1980, p 9, Figures 7 View Figure 7 , 8 View Figure 8 ; Minei 1981, p 80, Tables 2, 3 Plate 3 (lower) (partim); Miyake 1983, p 244, plate 51; Shokita 1990, Table 2 (partim); Anonymous 1991, p 219 (partim); Suzuki and Sato 1994, p 114 (partim); Shy et al. 1994, p 784; Ng and Shokita 1995, p 3; Anonymous 1996, p 362 (partim); Shokita 1996, p 348, Photograph 1; Yoshigou 1999, p 20, Plate 1(F) (partim); Segawa 2000, p 243, Table 1, Figures 1 View Figure 1 , 2 View Figure 2 (partim); Shokita et al. 2002, p 446 (partim); Kasai and Naruse 2003, p 283, Figures 67B, 71, 72 (partim); Naruse 2005a, p 190 (partim); Shokita 2005b, p 56 (partim), Plate 3 (middle right).
Material examined
Holotype: one male, CL 40.5 mm, ZLKU m. 1094, Fusato, Tamagusuku Village , coll. H. Minei, 25 June 1972 . Paratypes: eight males, CL 8.7–42.7 mm, two females, CL 19.9– 34.2 mm, three juveniles, CL 9.6–12.3 mm, ZLKU m. 1094, data same as holotype ; one male, CL 43.9 mm, ZRC 2006.0075 View Materials , Taiho River, Ohgimi Village , coll. S. Shokita et al., 3 December 1994 ; one male, CL 44.8 mm, ZRC 2006.0076 View Materials , Ohkuni Forest Road, north of Iji , coll. T. Naruse, 5 July 2001 ; one male, CL 43.8 mm, RUMF-ZC-140, Yona River, Kunigami Village , coll. S. Shokita, August 1983 ; two males, CL 29.2–29.7 mm, RUMF- ZC-141, near Ishiyama, Hedo, Kunigami Village , coll. S. Shokita, Y. Fujita, T. Nagai, H. Kawaguchi and Md. S. Islam, December 1998 ; one male, CL 41.5 mm, RUMF-ZC-142, Oshi River, Ohgimi Village , coll. S. Shokita, Y. Fujita, T. Nagai, H. Kawaguchi, and Md. S. Islam, 27 December 1998 ; one female, CL 27.1 mm, RUMF-ZC-143, east of Benoki Dam reserve, Kunigami Village , T. Naruse, 27 November 2001 ; one male, CL 37.6 mm, NSMT, Ohkuni Forest Road, between Hiji and Iji , coll. T. Naruse, 5 July 2001 ; one female, CL 34.0 mm, NSMT, Ohkuni Forest Road, Kunigami Village , coll. H. Kawauchi, 8 July 2000 . Others : four males, CL 30.0– 37.1 mm, three females, CL 32.1–41.5 mm, ZLKU C20007, data same as holotype ; two males, CL 38.4–40.6 mm, one female, CL 44.0 mm, ZLKU 10987 , Mt Yanbaru-Yama, Tamagusuku Village , coll. H. Minei, 26 June 1962 ; one female, CL 35.8 mm (31 August 1961), two females, CL 40.9–43.8 mm (26 June 1962), ZLKU 11020 , Mt Yanbaru-Yama, Tamagusuku Village , coll. H. Minei ; one male, CL 35.2 mm, ZLKU C20004, Fusato, Tamagusuku Village , coll. H. Minei, 25 June 1972 ; one male, CL 45.8 mm, ZLKU 9666 , Mt Meiji-Yama , coll. Kazuo Koba, 5 August 1956 ; one female, CL 39.4 mm, ZLKU 9667 , Mt Meiji-Yama , coll. K. Koba, 5 August 1956 . Fossil material: one palm, RUMF, Chinen Village , 2001, coll. M. Moriguchi. All specimens from Okinawa Island .
Comparatiυe material
Geothelphusa tenuimanus : all specimens examined in Naruse et al. (2004a).
Description of adult
Carapace ( Figure 4a, b View Figure 4 ) oval, strongly convex longitudinally; surface including anterolateral margin smooth, cervical groove very shallow, H-shaped gastric groove distinct, postorbital and epigastric cristae absent, postorbital and epigastric regions raised posteriorly gradually, small pit present on posterior part of external orbital angle. Front directed downwards, frontal margin cristate, not granulated; orbital margins cristate, not granulated or granulated on outer third, supraorbital margin L-shaped in dorsal view; epibranchial tooth low, demarcated by interrupted crista, low crista confluent with epibranchial tooth but separate from external orbital angle; anterolateral margin barely cristate, not granulated. Suborbital, subhepatic, and pterygostomial regions ( Figure 8b View Figure 8 ) smooth, no granulation visible on vertical groove and epimeral sulcus. Eye with relatively small cornea, subdistal width of cornea as wide as base of peduncle in frontal view.
Chelae of large male asymmetrical in size and shape, major chela with wide, thick, and reticulated manus, movable finger long, curved, with large gape when fingers closed.
Ambulatory legs glabrous, propodi with elliptical cross-section, two longitudinal rows of spines on inner margins; dactyli with rectangular cross-section, each margin with row of spines, inner margins with short, stout, sharp spines, outer margins with short, stout, rounded spine, subdistal spine of outer dorsal margin of fourth ambulatory dactylus stout, rounded, smaller than terminal spine.
Male abdominal segments and telson triangular, telson slightly bell-shaped, reaching imaginary line joining proximal fifth of chelipedal coxae.
G1 ( Figure 4c, d View Figure 4 ) stout; subterminal segment curving outwards, distal part wider than proximal part, with knob on outer proximal angle; synovial membrane wide; terminal segment directed outwards, subdistal margin narrower than distal margin of subterminal segment, uneven.
Variation
In one female specimen (RUMF-ZC-143, CL 27.1 mm), the carapace is relatively flatter; with frontal margin convex medially and along both outer angles; the external orbital angle and epibranchial tooth are connected by a crista; the anterolateral margin has very low granules; the anterolateral region possesses very shallow grooves, appearing rugose; the pit behind the external orbital angle is relatively shallower; and there is a row of spines present on the outer margin of the ambulatory propodi.
Colour
Geothelphusa grandioυata is maroon to olive in colour in life. Some individuals are coloured a bluish slate-grey on the cardiac region, sides of the carapace, and third maxillipeds.
Habitat
Geothelphusa grandioυata occurs near middle to upper reaches of the banks or along small swamps in submontane areas. It also digs deep burrows adjacent to areas with water seeping out. On the basis of our collections, large individuals seem to prefer burrows which have at least some water in the bottom, but medium-sized individuals (e.g. a female, RUMF-ZC- 143, CL 27.1 mm; a male, RUMF-ZC-141, CL 29.7 mm) have been obtained from totally dried burrows ( T. Naruse, unpublished data; T. Nagai, personal communication).
Distribution
Okinawa Island, the Central Ryukyu Islands, Japan.
Etymology
The species name is derived from the Latin ‘‘ grandis ’’ (for large) and ‘‘ oυatus ’’ (for ovalshaped), suggesting the large body size and the strongly swollen carapace.
Remarks
Geothelphusa grandioυata has been regarded as G. leυicerυix since Miyake and Minei (1965). However, G. grandioυata can clearly be differentiated from G. leυicerυix s. str. by its proportionately wider G1 (versus more slender in G. leυicerυix), the wider synovial membrane of the G1 (versus more slender), and the shape of the inner margin between terminal and subterminal segment of the G1 (uneven versus smooth).
A fossil of a large brachyuran manus ( Figure 5a View Figure 5 , RUMF, palm length 28.6+ mm, palm width 23.7+ mm) was discovered in the limestone fissure sediments of the southern part of Okinawa Island, where fossils of G. tenuimanus have been collected ( Naruse et al. 2004a). The discovered manus can be identified as that of G. leυicerυix species group by its large size [versus palm length, 18.6 mm (RUMF-GF-11); palm width,18.0 mm ( MFM 142451) in G. tenuimanus ] ( Figure 5b View Figure 5 ). Since G. grandioυata is the only member of G. leυicerυix species group known from Okinawa Island, the fossil manus is most probably that of G. grandioυata. Naruse et al. (2004a) estimated that the geological age of the fossils of G. tenuimanus was late Pleistocene.
T |
Tavera, Department of Geology and Geophysics |
NSMT |
National Science Museum (Natural History) |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Geothelphusa
Naruse, Tohru, Shokita, Shigemitsu & Ng, Peter K. L. 2006 |
Geothelphusa
Stimpson 1858 |