Dysommina pygmaea, Tighe & Pogonoski, 2025
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publication ID |
https://doi.org/10.11646/zootaxa.5683.2.6 |
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publication LSID |
lsid:zoobank.org:pub:322362E7-88C8-44F2-9FE7-90AF0276344A |
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persistent identifier |
https://treatment.plazi.org/id/2159DD33-8465-0D27-FF6D-17EA21C9FD6E |
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Plazi |
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scientific name |
Dysommina pygmaea |
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sp. nov. |
Dysommina pygmaea sp. nov.
Figures 1–13 View FIGURE 1 View FIGURE 2 View FIGURE 3 View FIGURE 4 View FIGURE 5 View FIGURE 6 View FIGURE 7 View FIGURE 8 View FIGURE 9 View FIGURE 10 View FIGURE 11 View FIGURE 12 View FIGURE 13 , Table 1
Holotype: NMV A 29681-004 About NMV (adult male, 145 mm TL); Australia: Western Australia: Rowley Shoals, Mermaid L 34 east transect ( 17°02'50"S, 119°39'41"E to 17°03'42"S, 119°41'22"E), RV Southern Surveyor , Station SS 0507/77, depth 424–456 m, captured with beam trawl, 18 June 2007. GoogleMaps
Paratypes: NMV A 29681-009 About NMV ( 169 mm TL, cleared and stained), CSIRO H 6607-01 View Materials (adult female, 147 mm TL), USNM 443847 (adult female, 161 mm TL); all collected with holotype GoogleMaps .
Diagnosis. A species of the genus Dysommina with the following combination of characters: predorsal vertebrae 16, preanal vertebrae 27–28, total vertebrae 122, eye diameter about 12–14% head length, vomerine dentition four large compound teeth set in papillose pads, maxillary and mandibular teeth numerous but small.
Description. Body moderately elongate, slightly compressed in head and trunk. Pectoral fin present; dorsalfin origin behind tip of pectoral fin; anal-fin origin approximately one head length behind pectoral-fin base. Snout projects very slightly beyond tip of lower jaw. Snout plicate, with four main plicae on each side of midline; median first plica L-shaped, extending laterally in front of second plica; second plica curves slightly laterally behind dorsal end of third plica, third and fourth plica smaller and less distinct than others; first supraorbital pore just above dorsal end of second and third plicae. Tip of lower jaw also plicate, with total of 12 plicae although only 8 extend outside of lip onto tip of jaw; two median plicae largest; three lateral plicae on each side of median plicae, reducing slightly in size from interior to exterior; first preopercular-mandibular pore just behind posterior end of third and fourth plicae. Anterior portion of snout and lower jaw extensively covered with papillae; papillae reduced in number posteriorly along head.
Morphometrics: Table 1 gives the summary of morphometrics for the type series. Morphometrics of the holotype: total length (TL) 145 mm, predorsal length 31.0 mm (21.4% TL), preanal length 42.9 mm (29.6% TL), tail length 102 mm (70.3% TL), trunk length 22.0 mm (15.2% TL), body depth (at gill opening) 10.2 mm (7.0% TL), body depth (at anal origin) 10.0 mm (6.9% TL), head length (HL) 20.8 mm (14.3% TL), eye diameter 2.6 mm (12.5% HL), interorbital width 4.0 mm (19.2% HL), snout length 5.7 mm (27.4% HL), upper jaw length 7.5 mm (36.1% HL), lower jaw length 7.2 mm (34.6% HL), pectoral fin length 4.6 mm (22.1% HL).
pore counts, the counts are recorded left/right.
Meristics: Table 1 gives the summary of meristics for the type series. Total vertebrae 122, predorsal vertebrae 16, preanal vertebrae 27–28. Dorsal rays 271–300, anal rays 244–276, anal fin origin at dorsal ray 29–34, pectoral rays 13–15 (based on cleared and stained paratype and CT scanned specimens), caudal rays 15.
Coloration: Live coloration ( Figure 1A View FIGURE 1 ): body medium brown with irregular blotching on body slightly darker, head and area of gill opening very dark (probably from poor exposure of photograph since there is no concentration of melanophores in these areas after preservation), gut cavity slightly darker, overlain with iridophores producing a greenish silver sheen, fins very light and almost unpigmented. Coloration after preservation ( Figure 1B View FIGURE 1 ): body overall light tan, dotted with numerous small melanophores, gut cavity with slightly fewer but larger melanophores, internal gut cavity darker due to peritoneal pigmentation, two pairs of deep mid-lateral pigment spots near vertebrae 57–59 and 63–65 (probably representing remnants of larval pigment), fins light with little pigment.
Cephalic-lateralis pores ( Fig. 2B View FIGURE 2 ): supraorbital 3; adnasal 1, infraorbital 4, preoperculomandibular 6. Lateral-line pores absent.
Dentition ( Figs. 3–6 View FIGURE 3 View FIGURE 4 View FIGURE 5 View FIGURE 6 ). Intermaxillary teeth absent. Four relatively large, compound vomerine teeth ( Figs. 3–4 View FIGURE 3 View FIGURE 4 ) set in papillose pads, fourth usually slightly smaller than the first three teeth on the palate. Mandibular teeth ( Fig. 5 View FIGURE 5 ) set in a band composed of 5–6 irregular rows anteriorly and decreasing gradually to 3–4 rows posteriorly, teeth increasing in size gradually from outer to inner with approximately 28–30 teeth in inner row. Maxillary teeth similar ( Fig. 6 View FIGURE 6 ) but set in a band composed of 5–6 irregular rows anteriorly and decreasing gradually to 2–3 rows posteriorly, teeth increasing in size gradually from outer to inner row with approximately 37–42 teeth in inner row.
Osteology ( Figs. 7–12 View FIGURE 7 View FIGURE 8 View FIGURE 9 View FIGURE 10 View FIGURE 11 View FIGURE 12 ). The osteology of Dysommina pygmaea is nearly identical to that of D. rugosa described by Robins and Robins (1970). Fig. 7 View FIGURE 7 shows the osteology of the head of D. pygmaea in dorsal, lateral and ventral views. Details of the osteology are discussed individually in the sections below.
Cephalic lateralis ( Fig. 8 View FIGURE 8 ). There are 11 cephalic-lateralis ossicles on the dorsal surface of the head, posterior to the eye and along the upper jaw. The anteriormost on the dorsal surface is associated with supraorbital lateralis pores 2 and 3. The next on the dorsal surface is the nasal ossicle which supports the dorsal portion of the nasal chamber. There are two very small ossicles along the portion of the supraorbital canal above the eye and two ossicles on the postocular portion of the infraorbital canal, but there are no pores associated with them. There are five ossicles associated with the infraorbital canal. The first, anterior most is on the adnasal branch of the infraorbital and the adnasal pore is near its distal end. The first infraorbital pore is anterior to the next infraorbital ossicle, near the junction of the adnasal branch with the main infraorbital canal. The second infraorbital pore is between the second and third infraorbital ossicles. The third infraorbital pore is posterior to the third infraorbital ossicle and the final infraorbital pore is anterior to the fifth infraorbital ossicle. Despite the lack of lateral line pores, there are 4–5 very small lateral-line ossicles in the dorsal branchial region posterior to the skull. These are probably vestigial but may still support the anterior portion of the lateralis nerve as there are superficial sensory papillae along the region of the lateral line despite the lack of open pores.
Neurocranium ( Fig. 9 View FIGURE 9 ). The skull of D. pygmaea is completely ossified with little cartilage and shows a generalized anguilliform pattern with the fused ethmovomer. The frontals are fused and cover nearly half of the dorsal surface of the skull. The remainder of the dorsal surface of the skull is composed of the paired parietals, pterotics, epiotics, sphenotics and the single, median supraoccipital. The ventral portion of the skull is composed of the fused ethmovomer, the parasphenoid, the prootics, the exoccipitals and the basioccipital. In addition, the lateral portions of the pterosphenoids, pterootics and sphenotics are visible in the ventral view. The dorsal portion of the orbit is formed primarily by the frontal. The ethmovomer forms the anterior margin of the orbit while the ventral and posterior margins are formed primarily by the parasphenoid. Robins and Robins (1970) reported that the basisphenoid and parasphenoid are fused in D. rugosa , but this could not be confirmed in D. pygmaea as there was no autogenous basisphenoid visible on the scan. The lack of an autogenous basisphenoid is not unique to D. rugosa and D. pygmaea as Robins and Robins (1970) also reported that the basisphenoid and parasphenoid are fused in Dysomma anguillare .
Suspensorium ( Fig. 10 View FIGURE 10 ). The hyomandibular is inclined slightly posteriorly and articulates with the neurocranium anteriorly with a hemispherical “ball and socket” joint underneath the sphenotic and posteriorly in a groove along the ventral surface of the pterotic. The hyomandibular and quadrate articulate in a complex interdigitated suture with a long triangular process of the hyomandibular extending nearly to the articulation of the quadrate with the articular. The pterygoid is relatively stout but does not articulate the hyomandibular or quadrate. It is embedded within connective tissue or muscle and extends to near the posterior end of the maxilla. The opercular series is complete with all four elements present although greatly reduced in ossification especially along the margins. The opercle articulates with the hyomandibular through a bottle-neck articular condyle. The subopercle has an anterior arm that does not appear to articulate with any other bone of the opercular series. It becomes more laterally flattened posteriorly and curves around the ventral margin of the opercle. The preopercle lies along the posterior margin of the hyomandibular and is slightly tube-like to house the preopercular branch of the cephalic lateralis. The interopercle is a quadrilateral-shaped bone that is ventral and medial to the rest of the opercular series.
Hyoid arch ( Fig. 11 View FIGURE 11 ). A median basihyal is present with paired hypohyals, anterior ceratohyals and posterior ceratohyals. The hypohyals are small cylindrical bones with a small ventral flange and are articulated to the anterior tip of the anterior ceratohyals. The anterior ceratohyals are also cylindrical with a narrow splint of bone extending onto the dorsal surface of the posterior ceratohyals. The posterior ceratohyals are cylindrical anteriorly but become laterally flattened and curve dorsally posteriorly. There are 12–13 branchiostegal rays (14 on the right arch of the holotype). The first originates at the end of the anterior ceratohyal, the second on the interspace between the anterior and posterior ceratohyals and the rest on the posterior ceratohyal. The last two are laterally flattened and curve up and around the opercle posteriorly, with the last ray nearly closing a circle.
Pectoral fin ( Fig. 12 View FIGURE 12 ). The CT scan of the pectoral girdle shows the following elements: cleithrum, coracoid, four actinosts and 13 fin rays. The range of pectoral-ray counts from both scanned specimens and the cleared and stained specimen is 13–15 rays. Examination of the cleared and stained specimen also showed a lightly stained cartilaginous element just dorsal to the coracoid which is probably the scapula. Because of the cartilaginous nature of this element, it did not show up in the CT scans.
Branchial arches ( Fig. 13 View FIGURE 13 ). Bones of the gill arches are the following: one unpaired median basibranchial, two pairs of hypobranchials, five pairs of ceratobranchials, four pairs of epibranchials, one pair of infrapharyngobranchials and two pairs of pharyngobranchial toothplates. Both lower and upper pharyngobranchial toothplates are roughly ovoid and covered with small, conical teeth. Robins and Robins (1970) reported that, in D. rugosa , there were two pairs of infrapharyngobranchials and that both lower and upper pharyngobranchial toothplates are single bones. In D. pygmaea , there is only a single pair of infrapharyngobranchials. In addition, the upper pharyngobranchial toothplates consist of two bones.The main bone of the toothplate is the upper pharyngobranchial 4 which is the largest and completely toothed. Anterior to this bone is a small elongate, sub-triangular bone (upper pharyngobranchial 3) which is closely associated (and possibly partially fused) with infrapharyngobranchial 3. Evidence that this is part of the upper pharyngobranchial toothplate is shown in Fig. 13D View FIGURE 13 which shows a single tooth on the right upper pharyngobranchial 3 of USNM 443847.
Comparative remarks. Dysommina pygmaea can be distinguished from all other described species in the genus by its low vertebral count (122 versus 123–132 in D. rugosa , 137–141 in D. orientalis , and 133–134 in D. brevis ) and higher predorsal vertebral count (16 versus 13–15 in D. rugosa , 11–12 in D. orientalis , and 12–13 in D. brevis ). D. pygmaea also has a lower dorsal-ray count anterior to the anal-fin origin (29–34 versus 36–57 in D. rugosa , 51–60 in D. orientalis , and 41–42 in D. brevis ). The coloration of D. pygmaea upon preservation is light tan overall with no dark pigmentation posteriorly on the anal base, anal fin, or caudal fin. All other species in the genus Dysommina are reported to have dark pigment somewhere posteriorly on the anal fin or caudal fin. In addition, the holotype and two of the paratypes of D. pygmaea are fully adult at a much smaller size than any other species in the genus. Maximum known size for D. pygmaea is 17 cm TL vs 32 cm TL for D. brevis , 35 cm TL for D. rugosa and 63 cm SL for D. orientalis .
Etymology. The specific name pygmaea is the feminized form of the Latin noun pygmaeus meaning ‘‘dwarf” and refers to the small adult size of this species. A noun in apposition.
Ecology. The types were collected with a beam trawl deployed into a strong current. The beam trawl was successfully retrieved after a minor hookup on the rocky bottom with a good catch returned including some hard bottomed animals (glass sponges and stalked crinoids). Benthic fish genera collected with the types included Chlorophthalmus, Hymenocephalus, Setarches and Symphurus . Ross and Quattrini (2007), Ross et al. (2015a) and Ross et al. (2015b) reported the Dysommina rugosa was found primarily in complex, hard-bottomed habitats including rock fields, canyon walls, mixed hard-soft bottom, seeps and deep-water coral reefs. It is likely that D. pygmaea also inhabits similar habitats.
Distribution. Dysommina pygmaea is known only from the four specimens that were collected at a single trawl station near Rowley Shoals off Western Australia. The species is almost certainly more widely distributed in the eastern Indian Ocean but may remain rare in collections due to its rugged habitat which is difficult to sample.
Comparative materials. Dysommina rugosa (n=64): USNM 131594 About USNM ( holotype, 196 mm TL), Atlantic Ocean, United States, Georgia, off Cumberland Island , 30°53’00"N, 79°42’30"W, 273 fms ( 499 m), 5 May 1886 GoogleMaps . USNM 44324 About USNM ( 1, 283 mm TL), Atlantic Ocean, United States, Georgia, off Savannah, 31°09’00"N, 79°33’30"W, 644 m, 5 May 1886 GoogleMaps . USNM 179213 About USNM ( 1, 194 mm TL), Gulf of Mexico , off Florida, 28°16'N, 85°50'W, 439 m, 3 Dec 1962 GoogleMaps . USNM 190541 About USNM ( 1, 265 mm TL), Gulf of Mexico, Florida Keys, southwest of Dry Tortugas, 24°28'N, 83°24'W, 329 m, 7 Jun 1959 GoogleMaps . USNM 193552 About USNM ( 1, 213 mm TL), Caribbean Sea, off Belize, 16°58'N, 87°53'W, 250–400 fms ( 457– 732 m), 10 Jun 1962 GoogleMaps . USNM 200776 About USNM ( 1, 248 mm TL), Atlantic Ocean, east coast of Florida, 29°59'N, 80°09'W, 347 m, 21 Nov. 1965 GoogleMaps . USNM 441960 About USNM ( 1, 226 mm TL) , USNM 441961 About USNM ( 1, 224 mm TL), Atlantic Ocean, off Maryland, Baltimore Canyon seep, 38°02’53"N, 73°49’19"W, 398 m, 16 May 2013 GoogleMaps . USNM 441962 About USNM ( 1, 249 mm TL), Atlantic Ocean, off Maryland, Baltimore Canyon seep, 38°02’57.1"N, 73°49’19.6"W, 414 m, 7 Sep 2012 GoogleMaps . NCSM 115346 View Materials (1, 96 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia A, ca. 197.3–197.6 kilometers E of Wilmington, 34°19'42"N, 75°47'59"W, 370–407 m, 15 Jun 2004 GoogleMaps . NCSM 115347 View Materials ( 1, 180 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia B, ca. 90.6–91.2 kilometers SE of Beaufort, 34°13'55"N, 75°52'01"W, 419–430 m, 20 Sep 2006 GoogleMaps . NCSM 115348 View Materials (2, 128– 157 mm TL), Atlantic Ocean, off North Carolina, Lophelia B site, ca. 75.7 kilometers SE Cape Lookout , 34°10'50"N, 75°53'28"W, 397–450 m, 19 Oct 2005 GoogleMaps . NCSM 115349 View Materials ( 1, 174 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia B, ca. 92.9–93.6 kilometers SE of Beaufort, 34°10'54"N, 75°52'57"W, 458–465 m, 19 Sep 2006 GoogleMaps . NCSM 115350 View Materials ( 1, 176 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia A, ca. 92.4–92.3 kilometers ESE of Beaufort, 34°18'48"N, 75°47'4"W, 389–443 m, 23 Sep 2001 GoogleMaps . NCSM 115351 View Materials ( 1, 184 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia A, ca. 91.2 kilometers ESE of Beaufort, 34°19'25"N, 75°47'30"W, 367–399 m, 22 Sep 2001 GoogleMaps . NCSM 115352 View Materials (4, 80–158 mm TL), Atlantic Ocean, off North Carolina ca. 74.7–75.1 kilometers SE of Cape Lookout, 34°11'12"N, 75°53'49"W, 431 m, 19 Sep 2006 GoogleMaps . NCSM 115353 View Materials ( 1, 193 mm TL), Atlantic Ocean, off Maryland, Baltimore Canyon, ca. 115.7–117.9 kilometers ESE of Ocean City , 38°02'47"N, 73°49'07"W,, 7 Sep 2012 GoogleMaps . NCSM 115354 View Materials (3, 145– 217 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia B, ca. 92.8–92.9 kilometers SE of Beaufort, 34°10'46"N, 75°53'26"W, 450–487 m, 24 Sep 2001 GoogleMaps . NCSM 115355 View Materials (2, 220– 225 mm TL), Atlantic Ocean, off Maryland, Balitimore Canyon, ca. 159.6–159.2 kilometers ESE of Salisbury , 38°02'52"N, 73°49'11"W, 399–443 m, 16 May 2013 GoogleMaps . NCSM 115356 View Materials ( 1, 210 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia A, ca. 90.7–90.3 kilometers ESE of Beaufort, 34°19'06"N, 75°48'13"W, 396–405 m, 10 Aug 2002 GoogleMaps . NCSM 115357 View Materials (15, 166– 206 mm TL), Atlantic Ocean, off North Carolina , Cape Lookout Lophelia B, ca. 91.7–92.3 kilometers SE of Beaufort, 34°11'57"N, 75°52'59"W, 423–443 m, 19 Sep 2006 GoogleMaps . NCSM 115358 View Materials (4, 169– 237 mm TL), Atlantic Ocean, off North Carolina, Cape Lookout , ca. 91.8–91.7 kilometers ESE of Beaufort, 34°17'38"N, 75°48'19"W, 438–439 m, 5 Dec 2009 GoogleMaps . ANSP 94286 About ANSP ( 1, 155 mm TL), Atlantic Ocean, off St. Augustine , 29°56'N, 80°10'W, M GoogleMaps / V Combat sta. 84, 190 fms ( 165 m), 1 September 1956 . ANSP 102469 About ANSP ( 1, 162 mm TL), Atlantic Ocean, Atlantic coast of Florida, 29°53'N, 80°11'W GoogleMaps , R / V Silver Bay sta. 3677, 180 fms ( 329 m), 20 January 1962 . ANSP 106150 About ANSP ( 1, 149 mm TL), Atlantic Ocean, Atlantic coast of Florida, 30°21'N, 79°55'W, 230–250 fms ( 420–457 m) GoogleMaps , R / V Atlantis sta. 3779, 24 February 1940 . ANSP 110079 About ANSP ( 1, 337 mm TL), Atlantic Ocean, Atlantic coast of Florida, 92°53'N, 80°11'W, 175–180 fms ( 320–329 m) , R / V Silver Bay sta. 3669, 18 January 1962 . ANSP 114438 About ANSP ( 1, 245 mm TL), Atlantic Ocean, Gulf of Mexico, Straits of Florida , 24°26'N, 83°31'W, 300 fms ( 549 m) GoogleMaps , R / V Oregon sta. 4373, 7 August 1963 . ANSP 114439 About ANSP ( 1, 218 mm TL), Atlantic Ocean, between Florida and The Bahamas, 26°14'N, 79°30.5'W, 351 fms ( 642 m) GoogleMaps , R / V Gerda sta. 299, 5 April 1964 . ANSP 114440 About ANSP ( 1, 173 mm TL), Atlantic Ocean, Straits of Florida , 24°10'N, 81°39'W, 345 fms ( 631 m) GoogleMaps , R / V Gerda sta. 362, 15 September 1964 . ANSP 114441 About ANSP ( 1, 228 mm TL), Atlantic Ocean, Atlantic coast of Florida, 157–143 fms (287– 262 m) , R / V Gerda sta. 655, 16 July 1965 . ANSP 114442 About ANSP ( 1, 174 mm TL), Atlantic Ocean, Atlantic coast of Florida, 27°08'N, 79°45'W, 220 fms ( 403 m) GoogleMaps , R / V Gerda sta. 652, 16 July 1965 . ANSP 114443 About ANSP ( 1, 166 mm TL), Atlantic Ocean, Atlantic coast of Florida, 29°55'N, 80°11 W, 180–182 fms ( 329–333 m) GoogleMaps , R / V Silver Bay sta. 3675, 19 January 1962 . ANSP 114444 About ANSP ( 1, 338 mm TL), Atlantic Ocean, Atlantic coast of Florida, 29°53'N, 80°11 W, 180 fms ( 329 m) GoogleMaps , R / V Silver Bay sta. 3680, 21 January 1962 . ANSP 114445 About ANSP ( 1, 347 mm TL), Atlantic Ocean, Atlantic coast of Florida, 29°42'N, 80°11 W, 170 fms ( 311 m) GoogleMaps , R / V Silver Bay sta. 3679, 20 January 1962 . ANSP 114449 About ANSP ( 1, 137 mm TL), Atlantic Ocean, Atlantic coast of Florida, 30°40'N, 79°57'W, 210 fms ( 384 m), M GoogleMaps / V Combat sta. 310, 24 April 1957 . ANSP 117045 About ANSP (1, ca. 280 mm TL), Atlantic Ocean, off Florida, 30°2'N, 80°6'W. 215 fms ( 393 m) GoogleMaps , R / V Oregon sta 5761, 20 November 1965 . ANSP 130216 About ANSP ( 1, 268 mm TL), Atlantic Ocean, off coast of North Carolina , 33°56'N, 75°56'W, 340 fms ( 622 m) GoogleMaps , R / V Oregon sta. 11758, 31 January 1972 . ANSP 130217 About ANSP ( 1, 175 mm TL), Atlantic Ocean, off Florida, 30°54'N, 79°40'W, 265 fms ( 485 m) GoogleMaps , R / V Oregon sta 11715, 21 January 1972 . ANSP 130219 About ANSP ( 1, 211 mm TL), Atlantic Ocean, off Georgia, 31°2'N, 79°48'W, 140 fms ( 256 m) GoogleMaps , R / V Oregon sta 11710, 20 January 1972 . ANSP 153725 About ANSP ( 1, 269 mm TL), Atlantic Ocean, Straits of Florida , 24°27'N, 83°25'W, 200 fms ( 366 m) GoogleMaps , R / V Oregon sta 11166, 17 August 1970 .
Dysommina orientalis (n=7): NMMB-P11131 ( holotype, 413 mm TL), collected from Dong-gang fishing port, Pingtung, Taiwan, 13 Sep. 2010 . USNM 441667 About USNM ( paratype, 316 mm TL; formerly NMMB-P14012 ), Dong-gang fishing port, Pingtung, Taiwan, 20 Oct. 2011 ; NMMB-P3847 ( paratype, 290 mm TL; formerly THUP 4077 View Materials ), Dong-gang fishing port, Pingtung, Taiwan, 21 Mar. 1979 ; NMMB-P8361 ( paratype, 258 mm TL), Dong-gang fishing port, Pingtung, Taiwan, 16 Mar. 2005 ; USNM 441750 About USNM ( paratype, 325 mm TL; formerly NSYSU 3028 ), Dong-gang fishing port, Pingtung, Taiwan, Jan. 1996 ; ASIZP 57954 View Materials ( paratype, 238 mm TL), Dong-sha Island , South China Sea, 17 Aug. 1991 ; OMNH-P10000 ( paratype, 625 mm TL), Suruga Bay , Shizuoka Prefecture, Japan, 34°54'N, 138°30.5'E, 300–400 m depth, 17 Dec. 1996 GoogleMaps .
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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