identifier	taxonID	type	CVterm	format	language	title	description	additionalInformationURL	UsageTerms	rights	Owner	contributor	creator	bibliographicCitation
03B9555BFFFA68543ED5F9FAFBC71ADF.text	03B9555BFFFA68543ED5F9FAFBC71ADF.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Austinograea Hessler & Martin 1989	<div><p>Genus  Austinograea Hessler &amp; Martin, 1989</p><p>TYPE SPECIES. —  Austinograea williamsi Hessler &amp; Martin, 1989, by original designation and monotypy.</p><p>REMARKS</p><p>The genus  Austinograea currently consists of four species in the western Pacific: 1)  A. williamsi Hessler &amp; Martin, 1989, which seems to be confined to the northwestern Pacific, in the Mariana Back-Arc Basin (just west of the Mariana Island Arc) and found in abundance in snail beds filling the vent openings of the Mariana Trough; 2)  A. alayseae, originally collected from the Lau Back-Arc Basin, subsequently found distributed across hydrothermal vent areas in the Southwest Pacific Ocean, e.g. along the Eastern Lau Spreading Center and also reported from the North Fiji Basin, Tonga Arc and Manus Basin (see below); 3)  A. hourdezi, a widespread species encountered in the southwestern Pacific from numerous vent fields of the Lau and North Fiji Back-Arc Basins, now identified in the Woodlark Basin (see still from the video 190527174907236_15_1080 of La Scala vent Site) (Fig. 8A) and which cohabits with  A. alayseae at a number of sites (see below); and 4) and the rare and enigmatic  A. jolliveti from the southwestern Pacific, collected so far only from one site in the Lau Basin (ABE Site) and one site in the North Fiji Basin (Mussel Valley Site). Another species,  A. rodriguezensis Tsuchida &amp; Hashimoto, 2002, is located well apart, in the western Indian Ocean. The new  Austinograea found in the Woodlarlk and Manus Basins described here would be the sixth species of the genus.</p></div>	https://treatment.plazi.org/id/03B9555BFFFA68543ED5F9FAFBC71ADF	Public Domain	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.		Plazi	Guinot, Danièle	Guinot, Danièle (2025): Austinograea chubacarc n. sp. from the Manus and Woodlark Basins (western Pacific), and new records of A. alayseae Guinot, 1990 and A. hourdezi Guinot & Segonzac, 2018 (Crustacea, Decapoda, Brachyura, Bythograeidae). Zoosystema 47 (12): 167-184, DOI: 10.5252/zoosystema2025v47a12, URL: https://sciencepress.mnhn.fr/sites/default/files/articles/pdf/zoosystema2025v47a12.pdf
03B9555BFFFA685C3DCFFCDCFB551A9F.text	03B9555BFFFA685C3DCFFCDCFB551A9F.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Austinograea chubacarc Guinot 2025	<div><p>Austinograea chubacarc n. sp.</p><p>(Figs 3-7; 8A, B)</p><p>urn:lsid:zoobank.org:act: 4946C58F-0337-4C49-8898-CF60271B3265</p><p>Austinograea sp. – Boulart et al. 2022: 7, 8,?fig. 5c, e.</p><p>Crabs – Hourdez &amp; Jollivet 2023: 74, tables 10, 11.</p><p>TYPE LOCALITY. — Woodlark Basin, La Scala vent Field.</p><p>TYPE MATERIAL. — Holotype. SW Pacific • ♂ 22.8 × 35.7 mm, right-handed; Woodlark, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=155.05267&amp;materialsCitation.latitude=-9.79905" title="Search Plazi for locations around (long 155.05267/lat -9.79905)">La Scala vent Field</a>; PL738 - ASPI2; 9°47.943’S, 155°3.160’E; 3388 m; 27.V.2019; CHUBACARC 2019 cruise; Hourdez det.  Austinograea; Chu-025 writen on carapace; MNHN-IU-2024-6548.</p><p>Paratypes. SW Pacific • 1 ♂ 6. 3 × 8.1 mm, right-handed, 1 juvenile ♂ 9.8 × 14.6mm, 1 ♀ 8.5 × 12.4 mm; Woodlark, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=155.05267&amp;materialsCitation.latitude=-9.79905" title="Search Plazi for locations around (long 155.05267/lat -9.79905)">La Scala vent Field</a>; PL738 - ASPI3; 9°47.943’S, 155°3.160’E; 3374 m; 27.V.2019; CHUBACARC 2019 cruise; Hourdez det.  Austinograea hourdezi; MNHN-IU-2024-6549  •  1 ♀ 13.5 × 19, 3 mm; same data as for preceding; Chu-026 writen on carapace; MNHN-IU-2024-6550 •   1 ♀ 24.7 × 39.2 mm, with two chelae gaping; Woodlark, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=155.05273&amp;materialsCitation.latitude=-9.79905" title="Search Plazi for locations around (long 155.05273/lat -9.79905)">La Scala</a>, PL738 - GBT10; 9°47.943’S, 155°3.164’E; 3388 m; 27.V.2019; CHUBACARC 2019 cruise CHU-027; MNHN-IU-2024-6092  •  1 ♀ 28.6 × 45.7 mm, right-handed, but cutter bigger than crusher; same data as for preceding; CHU-028; MNHN-IU-2018-5228 •  1 ♀ 18.2 × 28.3 mm, slightly right-handed; same data as for preceding; CHU-029; MNHN-IU-2024-6090 •  1 ♀ 17.7 × 28.3 mm, with two cutters; same data as for preceding; CHU-030; MNHN-IU-2024-6089 •   1♂ 15.6 × 25.0 mm, right-handed; same data as for preceding; det.  Austinograea sp., CHU-031; MNHN-IU-2024-6036  •  5 ♀, 1 ♀ 14.6 × 22.2 mm; with two cutters; same data as for preceding; CHU-032; MNHN-IU-2024-6091 •   1 ♂ 14.0 × 22.4 mm, right-handed; same data as for preceding; Hourdez det.  Austinograea; CHU-033; MNHN-IU-2024-6032  •   1 ♂ (right-handed) 14.3 × 22.4 mm; same data as for preceding; det.  Austinograea; CHU-034 writen on carapace; MNHN-IU-2024-6022  •   1 juvenile ♂ 11.8 × 18.3 mm, right-handed; same data as for preceding; Hourdez det.  Austinograea sp.; MNHN-IU-2024-6034  •  1 ♂ 10.0 × 15.3 mm (without chelipeds); same data as for preceding; MNHN-IU-2018-5227 .</p><p>OTHER MATERIAL. —  SW Pacific •   1 ♂ 14 × 21.6 mm, left-handed (gonopods detached); Manus Basin, Pacmanus, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=151.67424&amp;materialsCitation.latitude=-3.7303166" title="Search Plazi for locations around (long 151.67424/lat -3.7303166)">Solwara</a> 8, PL733 - ASPI7; 3°43.819’S, 151°40.454’E; c. 1750 m; 18.V.2019; CHUBACARC 2019 cruise; MNHN-IU-2024-6086  •  1 ♂ 10.3 × 15.9 mm, right-handed; MNHN-IU-2024-6088 •  1 ♀ 22.5 × 34.6 mm; slightly right-handed, unreadable numbers writen on carapace; MNHN-IU-2024-6087.</p><p>ETYMOLOGY. — The expedition name CHUBACARC 2019 cruise rhymes with one StarWars character; and the specific name  chubacarc is an oblique reference to  Chewbacca, the furry hero of the popular American Star Wars saga by George Lucas (Lucas film), alluding to the dense setae on the internal surface of the cheliped palm of the species. The name is used as a noun in apposition.</p><p>DESCRIPTION</p><p>Carapace</p><p>Carapace tranversely elliptical, flat. Dorsal surface with regions indistinct, smooth, except for a few granules on frontal and suborbital regions; may have very sparse, extremely short setae, only discernible at high magnification. Front not protuding, straight or slightly convex, bluntly pointed medially (see Variations), with tiny granules. Anterolateral margin marked by rounded edge, slightly granular proximally. Posterolateral margins convergent. Posterior margin slightly concave. Proepistome sunken, very thin. Margin of epistome formed of two minutely granular, moderately concave lobes, with a median projection. Pterygostomial lobe tuberculous; pterygostomial region smooth. Subhepatic regions covered by patches of setae (see Variations).</p><p>Cephalic structures</p><p>Eyes, antennules and antennae recessed. Suborbital plate absent. Orbit not delimited, only an orbital area that extends as groove lateral to region containing vestigial eyestalks and antennae; outer side of orbital area tuberculated. Eyestalk not moveable, showing as fixed piece fused to floor of orbital region; no cornea, no pigment. Antennules folded horizontally. Antenna inserted in wide supraorbital notch; urinary article fixed, broad, recessed; basal article (2 + 3) cylindrical, moveable, recessed; article 4 slightly elongated, inclined; flagellum short, curved.</p><p>Third maxillipeds</p><p>Third maxillipeds closing buccal cavity, except anteriorly where there is a gap between them and pterygostomial lobe. Ischium long, with marked longitudinal internal groove. Merus short: external margin entirely and regularly curved, oblique, without marked angle; distal part distinctly narrower and produced; internal margin with proximal half produced as squarish lobe. Carpus inserted in notch of antero-internal margin of merus; propodus thick, developed; dactylus thick and moderately extending beyond articulaion of ischium/merus; inner margins of propodus and dactylus with some brush-like setae. Mxp3 coxa with only proximal portion visible, its lateral projection hidden by junction of thoracic sternum (sternite 4) with pterygostome. Exopod with relatively long flagellum.</p><p>Chelipeds</p><p>Chelipeds heteromorphic: distinctive heterochely (also in females, see below) and marked heterodonty, with two types of chelae. Major chela (crusher, see below) stout and short, with blunt tips, gaping in large males; minor chela (cutter, see below) narrower, with elongate, more pointed fingers. Ischio-basis glabrous or with potentially very small setal patch. Merus relatively short, triangular in cross section; anterior border sinuous, with strong teeth; merus glabrous in males; in contrast, in females usually each with patch of setae (see Variations). Carpus glabrous on outer part, with patch of setae only along margin articulating on propodus or more developed; surface pitted. Propodus of both chelae having outer surface of palm near base of dactylus either with two coalescing spots of variable dark colour or with a single elongated spot (actually composed of two more or less coalescing spots) and another one rounded forming a depression (see holotype Fig. 3E, G), these spots more or less distinct, tending to fade, then disappearing (see Variations, below). Spots absent in females (see below). Inner surface of both chelae and fixed finger with a depressed surface on half posterior part; on internal median part of palm, thick, wellcircumscribed patch of dense light brown setae, extending thinly along occluding margins.</p><p>Crusher. Palm convex, inflated, smooth, pitted, with one or two more or less distinct spots, with depressed posterior portion on inner posterior surface. Fingers thick, not gaping at occluding margins, with blunt tips; two main, proximal and median, teeth on occluding margin of dactylus, becoming blunt in large males as holotype; a marked subproximal tooth and two smaller ones on occluding margin of fixed finger, becoming blunt, and only one remaining in large males as holotype. Median surface of thick dactylus of major male chela hollowed out by deep depression extending distally into fissure, becoming thinner and up to subdistal portion of dactylus (see Variations), this character constituting the most distinctive trait of the species. In females, such a depression absent, but more or less replaced along most part of dactylus by thin, interrupted line. In males, dark colour extending over approximately two-thirds of dactylus and most part of fixed finger.</p><p>Cutter. Palm elongate, with subparallel borders; surface smooth, except for two spots of different size and shape (one as a depression, like in holotype) near base of dactylus, more or less similar to those of crusher. Both fingers not gaping at occluding margins; dactylus elongate, hollowed, with occluding margin smooth; fixed finger very thick, depressed on inner surface; occluding margin nearly straight, with two or three small teeth, decreasing in size gradually forward, becoming blunt in large individuals. In males, dark colour extending over approximately most part of both dactylus and fixed finger, but sometimes fading.</p><p>In females, both chelae either similar and showing as two elongate and thin cutters or slightly heteromorphic and showing as a crusher and a cutter but without significant differences between them. Palm and fixed finger with posterior half part markedly depressed. Fingers very long, narrow, without depression on superior margin of dactylus, sometimes being replaced by thin interrupted line along most of dactylus of crusher; this line sometimes indistinct, for example in female 22.5 × 34.6 mm, MNHN-IU-2024-6087 (Fig. 7C, D), with dark (reddish) colour very marked, located only in subdistal tips of both dactylus and fixed finger. Inner surface of palm with well circumscribed thick patch of dense light brown setae, weakly extending along occluding margins; patches of setae also present on ischio-basis and proximal part of carpus and merus.</p><p>Ambulatory legs</p><p>P2-P5 shorter than chelipeds; P3 and P4 longest. Ischio-basis, merus and propodus with thick patches of dense setae on ventral margins (thicker on P2 and P3, weak on P5), mixed with sparse longer setae; superior border of carpus and propodus fringed with setae. Dactyli relatively stout, also with patches of short setae.</p><p>Thoracic sternum</p><p>Thoracic sternum with incomplete sutures 4/5-7/8, separared by short gap; suture 2/3 complete. Median line only along sternite 8. Junction of sternite 4 with pterygostome only represented by short juxtaposition. At level of antero-external portion of sternite 4 and of episternites 5, 6, 7, some setal patches in males, denser in young adult females, and, in larger females, becoming well circumscribed patches with decreasing size from front to back. Press-button of locking mechanism very acute, close to suture 5/6.</p><p>Pleon</p><p>Male pleon of six free somites and telson, regularly triangular; pleonal somites 1, 2 dorsally exposed; pleonal somite 3 widest; pleonal somite 6 longest; telson triangular, slightly rounded distally. On posterior angles of somite 6, a deep socket delineated by raised, thick margin.</p><p>Penis and gonopods</p><p>Penis emerging from anterior margin of coxo-sternal P5 condyle. Both G1 crossing subdistally, joining at tips, the latter not lodged in special depression but normally ending in relatively wide extremity of sterno-pleonal cavity at this level. G1: slender, faintly curved, with only short, small spiniform setae arranged in two rows along mid-part only. G2: short, a little less half length of G1, bent to slightly less three-quarters of length at level of small setiferous area; flagellum curved, flattened, bladelike.</p><p>Vulvae</p><p>Vulvae big, rounded, occupying most of sternite 5, with thick curved membrane on inner side; large median opening.</p><p>VARIATIONS</p><p>In males, the depression on the superior margin of the major cheliped dactylus is relatively long and deep, both in the right-handed male holotype 22.8 × 35.7 mm (MNHN-IU-2024-6548) (Figs 3E; 8) and in the right-handed paratype male 14.3 × 22.4 mm (MNHN-IU-2024-6022) (Figs 4E, F; 5C) from the Woodlark Basin. Only in a small right-handed paratype male 15.6 × 25.0 mm (MNHN-IU-2024-6036), the depression is shallow and short, as if atrophied (Fig. 6D), whereas in the right-handed juvenile paratype male 11.8 × 18.3 mm (MNHN-IU-2024-6034) the depression of the dactylus is already present and as developed as in the holotype. Such a depression is absent in female chelae (Fig. 7A, C).</p><p>The frontal margin is straight or slightly bluntly pointed medially (Figs 3A; 4A, B, E, F; 5A).</p><p>The degree of setation varies: it is more developed in females, particularly on the subhepatic area and in the latero-anterior angles of sternite 4; there are usually patches of setae on the ischio-basis and carpus of the chelipeds of females and, at less extent, in large males such as the holotype (Fig. 3C); but the merus is glabrous in males (Figs 3C, I; 4C). The setal patch on the suborbital margin is regularly dense (such as in the holotype, Fig. 3B) or denser medially than externally.</p><p>The spots on the outer surface of the male palm are variable but usually present in  Austinograea chubacarc n. sp. from the Woodlark Basin, whereas spots are absent on the chelae of females (Fig. 7C, E). In the right-handed holotype ♂ 22.8 × 35.7 mm (MNHN-IU-2024-6548) (Fig. 3E), the palm of the major chela bears two dark spots, an elongated one with a depression near the base of the dactylus and a rounded one in a depression at its upper middle, whereas the minor chela has two coalescent spots, the upper one with depression (Fig. 3G). Only a trace, difficult to perceive (and not really visible in the photograph), can be guessed on the minor chelae of the right-handed male 14.3 × 22.4 mm (MNHN-IU-2024-6022) (Fig. 4C, E, F). In the right-handed male paratype 14.3 × 22.4 mm (MNHN-IU-2024-6036) (with an atrophied depression), two spots are visible on the palm of the minor chela, whereas only one is clearly visible and a second one barely discernible on the palm of the major chela (Fig. 6D). In  A. chubacarc n. sp. from the Manus Basin, only one spot is clearly visible on each chela of the left-handed male 14 × 21.6 mm (MNHN-IU-2024-6086) and in the right-handed ♂ 10.3 × 15.9 mm (MNHN-IU-2024-6087).</p><p>REMARKS</p><p>Austinograea chubacarc n. sp. differs from all known species of  Austinograea in that the movable finger – the dactylus– of the male major chela has a long, deep depression (it can also be defined as a ‘wide groove’) on its outer superior border (Figs 3E; 4E, F); this depression is absent in females. Such a deeply grooved dactylus is an unusual, unique feature that we have never observed in other brachyuran crabs, and its function remains unclear. It is a singular species character admittedly but it is probably not that weird. Many crabs do have the outer surface of the dactylus lined with narrow grooves and, in some cases, there is a dorsal crest that highlights the longitudinal groove. Are these structures homologous?</p><p>Interestingly, the depression on the dactylus of  A. chubacarc n. sp. can be discerned on the major palm of certain crabs seen in situ from video images (Fig. 8B, close-up).</p><p>The overall shapes and occlusal geometries of the cheliped dactylus (which probably correspond strongly with diet) and its micro- and ultrastructure have been described in detail, with each cheliped having a range of mechanical advantages at its disposal and a diversity in occlusive design (e.g. Brown et al. 1979: 157; Masunari et al. 2015, 2020). Agnew (2008), who investigated the evolutionary patterns of the dactylus in decapod crustaceans, including the fossils (where the mobile finger is often the only represented remnant in fossil assemblages), and Fujiwara &amp; Kawai (2016), for whom the decapod chela is a suitable structure to analyse the evolutionary process of functional diversifications, do not mention the existence of such a curious feature (namely the wide groove on the dactylus) that cannot alter in any way – apparently – the crushing, chipping, gripping and pinching abilities of the dactylus.</p><p>Austinogeaea chubacarc n. sp. has fairly strong chelae in both males (Figs 3 A-C, E-H; 4A, C E, F; 5C-F; 6D) and females (Fig. 7 A-F), admittedly, without any teeth and complex armouring; however, it seems clear that chelae are used for competition and for foraging. Chelipeds, sexually dimorphic, also play a role in reproduction: although they are much less robust in males than in females, they hold the female firmly during mating (see below, Fig. 8C).</p><p>In  Austinograea chubacarc n. sp., the outer surface of the palm may bear, near the base of the dactylus of the major and minor chelae, more-or-less coloured spots: either very dark and partly in the form of depressions, as in the male right-handed holotype 22.8 × 35.7 mm (Fig. 3E, G) and paratype 15.6 × 25.0 mm (Fig. 6D); or superficial and tending to fade or even disappear, as for example in the right-handed paratype male 14.3 × 22.4 mm (Fig. 4E, F and see Variations). There are also two characteristic depressions on the propodus of male chelae, crusher and cutter, of  A. hourdezi (Guinot &amp; Segonzac 2018: figs 3A; 4A, B; 5E, G), similarly located in all the individuals examined, variously delineated by a raised margin and appearing fairly deep or shallower, and almost always coloured, appearing as dark spots. As in  A. chubacarc n. sp., the spots are absent in the females of  A. hourdezi (Guinot &amp; Segonzac 2018: fig. 7E, G).</p><p>Austinograea chubacarc n. sp. shares with  A. hourdezi the following characters: setal patches on the inner surface of the palm of the major and minor chelae in both sexes, on the subhepatic region and on the inner surface of the legs; triangular male pleon.  Austinograea chubacarc n. sp. and  A. hourdezi differ in the following characters: G1 slightly curved in  A. chubacarc n. sp., straighter in  A. hourdezi; flagellum of G2 proportionally shorter in  A. chubacarc n. sp. (see Fig. 6 A-C); merus of mxp3 shorter in  A. chubacarc n. sp. (Figs 4B, F; 5A, C); merus of the chelipeds cylindrical and weakly toothed in  A. hourdezi (Guinot &amp; Segonzac 2018: fig. 5A), instead of being shorter and with marked teeth in  A. chubacarc n. sp. (Fig. 3A, B); thoracic sternum completely glabrous in male  A. hourdezi (Guinot &amp; Segonzac 2018: fig. 5C, D), whereas it has tufts of setae on the antero-external portion of sternite 4 and at level of episternites 5, 6, 7 in male  A. chubacarc n. sp. (Figs 3I; 4D); ischio-basis and carpus of chelipeds may bear small setal patches in males and females of  A. chubacarc n. sp. (Figs 3C; 7G, respectively), but not in  A. hourdezi .</p><p>In  Austinograea chubacarc n. sp. the tips of the G1s, crossing subdistally, normally end in the relatively wide extremity of the sterno-pleonal cavity at this level, instead to end in the extremity of the sterno-pleonal cavity that is narrower at this level in  A. hourdezi (Guinot &amp; Segonzac 2018: figs 4C, 6C). These two dispositions differ significantly from that of  A. alayseae, in which Guinot (1990: 884, 891, fig. 2C) described the extremities of the G1 as joining in a small deep, well-delineated depression (d) at the narrow end of the sterno-pleonal cavity. In  A. jolliveti, the morphology is quite different:the G1s are directed obliquely, separated even at their tips, and the sterno-pleonal cavity is not excavated distally, without a small special distal depression to receive the distant G1 tips (see Guinot &amp; Segonzac 2018: figs 9B-D; 11C-E).  Austinograea chubacarc n. sp. can be distinguished from  A. williamsi by the G1 (Fig. 6A, B) that is more curved than that, straighter, of  A. williamsi (see Hessler &amp; Martin 1989: fig. 14a, c, d; Tsuchida &amp; Fujikura 2000: figs 6; 7A; Tsuchida &amp; Hashimoto 2002: fig. 8). In  A. rodriguezensis Tsuchida &amp; Hashimoto, 2000, the G1s are nearly straight (Tsuchida &amp; Hashimoto 2002: fig. 8), but it is not known whether or not they meet at their tips: we can predict that they are distant. Note that in  Gandalfus puia and  G. yunohana the tips of the G1s reach the extremity of the sterno-abdominal cavity that is relatively wide at this level.</p><p>The G2 of  A. chubacarc n. sp. (Fig. 6B, C) is short, a little less half the length of G1, bent at a slightly less three-quarters of the length.</p><p>The most diagnostic feature of  A. chubacarc n. sp. remains the depression on the cheliped dactylus of males (Figs 3E; 4E, F).</p><p>The larval morphology may in the future confirm the distinction of  Austinograea chubacarc n. sp. It was carried out in certain vent species from the Indian Ocean and the western Pacific: megalopa of  Austinograea rodriguezensis from the Indian Ocean (Demidow et al. 2021); 16 pre-zoeal stages and first zoeal stage of  A. rodriguezensis from Kairei Hydrothermal Vent field (Kihara et al. 2024), with a welldeveloped spinature on carapace and plenoal somites, not only attributed to defence from predators but considered an effective adaptation that helps in the dispersal of the zoeal stages to maintain the resident population; first zoeal stage of  Gandalfus yunohana (Nakajima et al. 2010); and three zoeal stages and megalopa of the same species (Hamasaki et al. 2010), with larval data supporting the recognition of  Austinograea and  Gandalfus as two distinct clades comprising  A. rodriguezensis and  G. yunohana, respectively (Kihara et al. 2024).</p><p>A phylogenetic analysis based on the CHUBACARC material was published by Chabert (2021: 26, 27, 32, table 2) for her master thesis. We support the Chabert’s result (Chabert 2021: 11, 26, 32, table 2) that the specimens from the Woodlark Basin identified as ‘Gen. sp. B’ would be a new species: they could well belong to  A. chubacarc n. sp.</p></div>	https://treatment.plazi.org/id/03B9555BFFFA685C3DCFFCDCFB551A9F	Public Domain	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.		Plazi	Guinot, Danièle	Guinot, Danièle (2025): Austinograea chubacarc n. sp. from the Manus and Woodlark Basins (western Pacific), and new records of A. alayseae Guinot, 1990 and A. hourdezi Guinot & Segonzac, 2018 (Crustacea, Decapoda, Brachyura, Bythograeidae). Zoosystema 47 (12): 167-184, DOI: 10.5252/zoosystema2025v47a12, URL: https://sciencepress.mnhn.fr/sites/default/files/articles/pdf/zoosystema2025v47a12.pdf
03B9555BFFF2685C3DF7FD1CFA231FE4.text	03B9555BFFF2685C3DF7FD1CFA231FE4.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Austinograea hourdezi Guinot & Segonzac 2018	<div><p>Austinograea hourdezi Guinot &amp; Segonzac, 2018</p><p>Austinograea hourdezi Guinot &amp; Segonzac, 2018: 880, figs 3A; 4A-E; 5A-H; 6A-E; 7A-H. — Lee et al. 2019a: fig. 1B, D. — Chabert 2021: table 2.</p><p>MATERIAL EXAMINED. —   3 ♀ 28.0 × 44.1 mm, 28.6 × 44.6 mm, 25.0 × 38.6 mm; Lau Basin, Tow Cam; PL730 – Panier; 20°19.080’S, 176°8.264’W; 2710 m; 26.IV.2019; CHUBACARC 2019 cruise; Hourdez det.  Austinograea; MNHN-IU-2024-6023.</p><p>REMARKS</p><p>The Tow Cam Site in the Lau Basin is the type locality of  Austinograea hourdezi, a widespread species in the southwestern Pacific, found in numerous vent fields of the Lau and North Fiji Back-Arc Basins (Guinot &amp; Segonzac 2018: 80).</p><p>In a still from the video 190527174907236_15_1080 https://video.ifremer.fr/index) of the La Scala vent Field, PL738 (Fig. 8A),  A. hourdezi is easily recognised by the thick patch of setae on the inner surface of the chelipedal palm: its presence is confimed in the Woodlark Basin at the La Scala vent Field, where it coexists with  A. chubacarc n. sp.</p><p>Chabert (2021: table 2), using a barcode approach with the cytochrome c oxidase subunit I (COI) gene, identified  Austinograea aff. hourdezi in the Woodlark Basin, and  A. hourdezi in the North Fiji. In addition, she identified  A. aff. williamsi in the Manus and Lau Basins, but we cannot determine which species they correspond to. S. Hourdez plans to carry out the correspondence between these genetic results and the different bythograeid species, after the publication of this paper (pers. comm.).</p><p>We did not identify  A. williamsi among the bythograeids collected during the CHUBACARC 2019 cruise, and so far the species appears to be endemic to the Mariana Trough, a back-arc basin in the northwest Pacific (Fig. 1) (Kojima &amp; Watanabe 2015).</p><p>Lee et al. (2019a), who determined the COI sequence of  Austinograea hourdezi from three hydrothermal vent regions in the North Fiji Basin, found that all were identical. Lee et al. (2019b: 10, tables 3, 4, S1 table) obtained sequences of two mitochondrial genes (COI and 16S rDNA) of the species.</p></div>	https://treatment.plazi.org/id/03B9555BFFF2685C3DF7FD1CFA231FE4	Public Domain	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.		Plazi	Guinot, Danièle	Guinot, Danièle (2025): Austinograea chubacarc n. sp. from the Manus and Woodlark Basins (western Pacific), and new records of A. alayseae Guinot, 1990 and A. hourdezi Guinot & Segonzac, 2018 (Crustacea, Decapoda, Brachyura, Bythograeidae). Zoosystema 47 (12): 167-184, DOI: 10.5252/zoosystema2025v47a12, URL: https://sciencepress.mnhn.fr/sites/default/files/articles/pdf/zoosystema2025v47a12.pdf
03B9555BFFF3685D3F01FF1EFB991D02.text	03B9555BFFF3685D3F01FF1EFB991D02.taxon	http://purl.org/dc/dcmitype/Text	http://rs.tdwg.org/ontology/voc/SPMInfoItems#GeneralDescription	text/html	en	Austinograea alayseae Guinot 1990	<div><p>Austinograea alayseae Guinot, 1990</p><p>Austinograea alayseae Guinot, 1990: 880, 898, figs 1-3, pl. 1 figs A-F. — Guinot &amp; Segonzac 2018: 75, 79, 76, 78, 96 (key), 99, 100, 101. — Tsuchida &amp; Fujikura 2000: 407, 413. — Tsuchida &amp; Hashimoto 2002: 643, 646, 647, 649 (key), figs 5, 6, 8. — Kim et al. 2013: 1, 2, 5-9, fig. 2, tables 1-3. — Lee et al. 2019b: 2, 3, 6-11, figs 1-3, tables 2, 3-5, S1.</p><p>MATERIAL EXAMINED. —   SW Pacific • 1 young ♀, without chelae; Manus Basin, PL 733 - PBT7; SnowCap / <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=151.67474&amp;materialsCitation.latitude=-3.72105" title="Search Plazi for locations around (long 151.67474/lat -3.72105)">Big</a> papi; 3°43.263’S, 151°40.485’E; 1669 m; 19.V.2019; CHU-512; MNHN-IU-2024-6027  •   1 very small ♀ with one chelae; Manus Basin, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=151.67291&amp;materialsCitation.latitude=-3.7173333" title="Search Plazi for locations around (long 151.67291/lat -3.7173333)">Pacmanus</a>; PL734 - ASPI3; 3°43.040’S, 151°40.375’E; 1769 m; 19.V.2019; MNHN-IU-2024-6081  •   1 ♀ 16.3 × 24.6 mm, native right-handed; Manus Basin; PL736 - Aspi 7, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=152.1015&amp;materialsCitation.latitude=-3.7992833" title="Search Plazi for locations around (long 152.1015/lat -3.7992833)">North Su</a> / <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=152.1015&amp;materialsCitation.latitude=-3.7992833" title="Search Plazi for locations around (long 152.1015/lat -3.7992833)">Solwara</a> 1; 3° 47.957’S, 152°6.090’E; 1195 m; 23.V.2019; CHU-510; Hourdez det.  Austinograea; MNHN-IU-2024-6024  •   4 ♀: 1 ♀ 33.9 × 53.2 mm, left-handed, CHU-660; 1 ♀ 30,6 × 48.3 mm, with two cutters, the left being bigger, CHU-661, 1 ♀ 28.5 × 35 mm, with two cutters, the left being bigger, 1 ♀ 28.8 × 45.4 mm, native right-handed; PL736 – GBT3, North Su / <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=152.101&amp;materialsCitation.latitude=-3.7990334" title="Search Plazi for locations around (long 152.101/lat -3.7990334)">Solwara</a> 1, PL736 - GBT3; 3°47.942’S, 152°6.060’E; 1210 m; 22.V.2019; Hourdez det.  Austinograea sp., CHU-662; MNHN-IU-2024-6028  •   1 ♀ 35.5 × 57.7 mm, left-handed; Manus Basin; PL736 - GBT4, North Su / <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=152.1015&amp;materialsCitation.latitude=-3.7992833" title="Search Plazi for locations around (long 152.1015/lat -3.7992833)">Solwara</a> 1; 3°47.957’S, 152°6.090’E; 1195 m; 23.V.2019, Hourdez det.  Austinograea; CHU-509; MNHN-IU-2024-6030  •   1 ♂ 9.7 × 14.2 mm, right-handed; Manus <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=151.6811&amp;materialsCitation.latitude=-3.7274833" title="Search Plazi for locations around (long 151.6811/lat -3.7274833)">Basin</a>; PL734 - GBT4; 3°43.649’S, 151°40.866’E; 1725 m; 19.V.2019; Roman’s Ruins / Solwara 6, 7 and 8; Hourdez det.  Austinograea; CHU-513; MNHN-IU-2024-6025  •   1 ♀ 12.0 × 18.0 mm, native right-handed; same data as for preceding; Hourdez det.  Austinograea, CHU-514 MNHN-IU-2024-6029  •   1 ♀ 26.2 × 41.2 mm, native right-handed; Manus Basin; PL737 - Panier, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=152.10524&amp;materialsCitation.latitude=-3.8094168" title="Search Plazi for locations around (long 152.10524/lat -3.8094168)">South Su</a>, <a href="https://tb.plazi.org/GgServer/search?materialsCitation.longitude=152.10524&amp;materialsCitation.latitude=-3.8094168" title="Search Plazi for locations around (long 152.10524/lat -3.8094168)">Pacmanus area</a>; 3°48.565’S, 152°6.314’E; 1330 m; 24.V.2019; Hourdez det.  Austinograea sp.; MNHN-IU-2024-6031  .</p><p>OTHER MATERIAL. — We add one specimen collected in high temperature vent site by the BAMBUS cruise in 2011 (see participants in Bach et al. 2011), and sent to the MNHN in 2011 (see Bach et al. 2011).</p><p>SW Pacific • 1 ♂ 12.9 × 20.5 mm, left-handed; Manus Basin, site Pacmanus, R/V  Sonne; ROV QUEST; BAMBUS cruise; éch. 49 ROV 5, site Solwara 8/Fenway; 03°43.72’S, 151°40.33’E; 1716 m; 9.VII.2011; W. Bach coll., ex-Bremen University collection, M. Segonzac det?  A. alayseae, XII.2011 (but not studied further MNHN-IU-2024-6068).</p><p>REMARKS</p><p>Austinograea alayseae, originally collected in the Lau Back-Arc Basin, west of the Tonga Islands, along the Valu Fa Ridge, at around 176°38’W and between 22°34’S and 22°10’S, at 1750 m depth (Guinot 1990) and already found in the Eastern Lau Spreading Center (Corbera &amp; Segonzac 2010; Podowski et al. 2010; Sen et al. 2013, 2014, 2016) (Fig. 1), is distributed over a wide geographical range. It has been reported from the North Fiji Basin (Jollivet et al. 1989, as bythograeid sp.; Guinot 1997 in Desbruyères &amp; Segonzac 1997; Galkin 1997; Hashimoto et al. 1999, as bythograeid sp.; Guinot &amp; Segonzac 2006 a; Desbruyères et al. 2006; Shields &amp; Segonzac 2007), and from the Tonga Arc and Manus Basin (Lee et al. 2019b). It has been reported from both active and inactive sites (Kowalczyk and Binns sites, respectively) (Erickson et al. 2009).</p><p>All the  Austinograea alayseae material from the CHUBACARC 2019 cruise studied here was collected in abundance in the Manus Basin, and more precisely in the Pacmanus area. Scavenger and carnivore, abundant at vent openings, crawling actively on snail thickets, this species dominates the Manus Basin fauna (Galkin 1992, 1997: fig. 1; Tsuchida &amp; Hashimoto 2002; López-González et al. 2005; Guinot &amp; Segonzac 2006; Lee et al. 2019b: table 2). Females of  A. alayseae are much more numerous and reach a much larger size than males: the maximum size of males in the material from the CHUBACARC 2019 cruise is 14.2 mm carapace wide, that of females is 57.7 mm wide. In the material from the Vai Lili Site of Lau Basin studied by Guinot (1990: 899), the largest male measured 51.3 mm carapace wide, and the largest female 63 mm.</p><p>According to Chabert (2021: 11, 26, 32, table 2), phylogenetic analysis, which allowed her to define the delimitation of nine bythograeoid species in the Woodlark Basin, has demonstrated the presence within the morpho-species  Austinograea alayseae of at least three cryptic species, each with different distributions. Her study recognised in the Woodlark Basin: two specimens of ‘  A. alayseae A’ (also present in the North Fiji and Lau Basins, and the Futuna Volcanic Arc), five specimens of ‘Gen. sp. B’ (apparently endemic to the La Scala vent Field), one specimen of the ‘Gen. sp. C’, and one specimen of ‘  A. aff. hourdezi ’. Unfortunately, from the material analysed by Chabert (2021: table 2, p. 15), we received only the one that identified as ‘  A. alayseae A’. As, we did not obtain the material identified as ‘  A. alayseae B, C and D’, in this article we will leave aside the interpretation of these results.</p><p>In the Manus Basin, Chabert (2021: 27, 32, table 2) did not report a ‘Gen. sp. B’ but recognised seven ‘  Austinograea alayseae B’ there, which were not located in any other basin, and one specimen of  A. aff. williamsi, which she also found, with two specimens, in the Lau Basin. The material in our hands, however, does not allow us to relate these various  Austinograea to any known species.</p></div>	https://treatment.plazi.org/id/03B9555BFFF3685D3F01FF1EFB991D02	Public Domain	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.		Plazi	Guinot, Danièle	Guinot, Danièle (2025): Austinograea chubacarc n. sp. from the Manus and Woodlark Basins (western Pacific), and new records of A. alayseae Guinot, 1990 and A. hourdezi Guinot & Segonzac, 2018 (Crustacea, Decapoda, Brachyura, Bythograeidae). Zoosystema 47 (12): 167-184, DOI: 10.5252/zoosystema2025v47a12, URL: https://sciencepress.mnhn.fr/sites/default/files/articles/pdf/zoosystema2025v47a12.pdf
