Leucosyrinx undosa ( Schepman, 1913 ), 2025
publication ID |
https://doi.org/10.5852/ejt.2025.999.2945 |
publication LSID |
lsid:zoobank.org:pub:7BFF2F85-97C9-46A9-9F9C-10AAB06C214C |
persistent identifier |
https://treatment.plazi.org/id/03FCE539-FFD5-3D0F-93D9-FD3E33329B8A |
treatment provided by |
Plazi |
scientific name |
Leucosyrinx undosa ( Schepman, 1913 ) |
status |
comb. nov. |
Leucosyrinx undosa ( Schepman, 1913) comb. nov.
Fig. 33E View Fig
Surcula undosa Schepman, 1913: 61 View in CoL (425), pl. 27 fig. 13a–b.
Comitas undosa – Powell 1969: 282 (23-294), pl. 227 figs 3–4.
Paracomitas undosa View in CoL – Shuto 1970a: 170, pl. 11 figs 8–9.
Type material
Holotype
INDONESIA • Flores Sea ; 7°24′ S, 118°15.2′ E; depth 794 m; NATURALIS, ZMA.MOLL.136841. GoogleMaps
Remarks
In general shell characters, including the position of the anal sinus, the species is referable to Leucosyrinx . Shuto (1970a) transferred it to Paracomitas Powell, 1942 . In our opinion this is unjustified. The genus Paracomitas is characterized and differentiated from Leucosyrinx and Comitas by a protoconch of 2.5 sharply carinated whorls. The protoconch is missing in the holotype of S. undosa , the only known specimen of the species. Therefore, pending additional data, we consider it a species of Leucosyrinx .
Distribution
Type locality.
Doubtful species, attributed herein to Leucosyrinx
The following species are conditionally attributed to Leucosyrinx pending further anatomical data and the collection of additional material. We are taking a conservative approach and will retain the species’ current generic position unless there are significant reasons to transfer them.
“ Leucosyrinx ” caecilia Thiele, 1925
Fig. 34A View Fig
Leucosyrinx caecilia Thiele, 1925: 202 View in CoL (236), pl. 24 (36) fig. 23.
Leucosyrinx caecilia View in CoL – Powell 1969: 337 (23-401), pl. 257 fig. 2.
Type material
Holotype
TANZANIA • Dar-es-Salaam: 6°34′ S, 39°35′ E; depth 404 m; ZMB Mol 109385. GoogleMaps
Remarks
The single known specimen is the juvenile holotype, with SL of 7.5 mm. The anal sinus is typical of Leucosyrinx , but the shoulder is accentuated by two distinct and broad spiral cords that appear wavy on poorly pronounced axial folds. This type of sculpture is not found in other species of the genus, but it is unclear whether these features are characteristics of the juvenile shell or of the species as a whole. We tentatively retain the species within Leucosyrinx , though with some reservations.
Distribution
Type locality.
“ Leucosyrinx ” canyonensis ( Dell, 1956)
Fig. 34B View Fig
Antimelatoma canyonensis Dell, 1956: 142 View in CoL , fig. 196.
Leucosyrinx canyonensis View in CoL – Powell 1979: 230, fig. 53: 3. — Spencer et al. 2011.
Type material
Holotype
NEW ZEALAND • South I., off east Otago; depth 260–350 ftm (= 475–640 m); MNZ, M.009262.
Remarks
The species is characterized by a small shell (SL 9.3 mm in the holotype) with strong spiral cords and a distinct crenulated shoulder carina. It is rather different from known species of Leucosyrinx , but in the absence of any data on anatomy, we retain it in Leucosyrinx with strong doubts.
Distribution
Type locality.
“ Leucosyrinx ” erna Thiele, 1925
Fig. 34C View Fig
Leucosyrinx erna Thiele, 1925: 201 View in CoL (235), pl. 24 (36) fig. 22.
Leucosyrinx erna View in CoL – Powell 1969: 337 (23-401), pl. 257 fig. 1.
Type material
Syntypes
TANZANIA • 3 specs; Zanzibar Channel ; 5°27′ S, 39°19′ E; depth 463 m; ZMB Mol 109384 GoogleMaps .
Remarks
The species is known from three dead-collected and immature shells (maximal SL 7.8 mm). It is characterized by strong and very closely spaced spiral cords below shoulder that was not found in other species of Leucosyrinx , although somewhat similar but broader cords are also found in L. nodulocordata sp. nov. In the absence of any data on anatomy, we retain it in Leucosyrinx with strong doubts.
Distribution
Type locality.
“ Leucosyrinx ” sansibarica Thiele, 1925
Fig. 34D–F View Fig
Leucosyrinx sansibarica Thiele, 1925: 181 View in CoL (215), pl. 24 (36) fig. 1.
Brachytoma griffithii (not Gray, 1833) – von Martens 1904: 84. — Thiele 1904: 173, pl. 9 fig. 73. Leucosyrinx sansibarica View in CoL – Powell 1969: 340 (23-404), pl. 258 fig. 5.
Type material
Syntypes
EAST AFRICA • 2 specs; Pembakanal; 5°24′ S, 39°19′ E; depth 818 m; Valdivia, stn 246 (2 dead); ZMB GoogleMaps ?.
GULF OF ADEN • 2 specs; 13°2′ N, 46°41′ E; depth 1469 m; Valdivia, stn 271; ZMB Mol 60089, ZMB Mol 109387 GoogleMaps .
Remarks
The species was established for Brachytoma griffithii sensu von Martens (1904) , not Gray, 1833. Von Martens (1904) cited material from two Valdivia stations: station 246 (Pemba Channel, off Zanzibar) and station 271 in the Gulf of Aden. Two dead specimens were collected at the first station, while several live specimens were collected at station 271. Thiele (1904: 173, pl. 9 fig. 73) illustrated the radula of the species without indicating the exact specimen, describing a radula typical of Comispira with a large central formation. Von Martens (1904) proposed a variety, gracilior, for specimens from off Zanzibar. When Thiele (1925) renamed the species Leucosyrinx sansibarica , he did not designate a holotype or a type series, nor did he provide a formal description, but from the specific epithet, it can be inferred he referred to the specimens from station 246. His illustration aligns with var. gracilior as described by von Martens, 1904 (“Martens distinguished a var. gracilior , which I have illustrated in Figure 1 View Fig .”—my translation).
We were unable to examine the specimens from the station 246, but the specimens from the station 271 in the Gulf of Aden are not conspecific. While one specimen represents the typical Leucosyrinx (ZMB Mol 60089, Fig. 34E View Fig ), the other, with a row of subsutural knobs, belongs to Comispira (ZMB Mol 109387, Fig. 34F View Fig ), rather similar to C. obtusigemmata (see below). The specimen illustrated by Thiele (1925) ( Fig. 34D View Fig ) is generally similar to the specimen of Leucosyrinx from the Gulf of Aden ( Fig. 34E View Fig ), differing mainly in its slenderer shell (a variable intraspecific character in Leucosyrinx ) and a much shallower anal sinus. It should be noted that in several of Thiele’s (1925) line drawings, the illustrated anal sinus does not match the actual sinus in the same specimen. We therefore consider L. sansibarica as belonging to the genus, although a final decision requires examining the illustrated specimen (currently unavailable) and designating a lectotype.
Distribution
Tanzania to Gulf of Aden, 818–1469 m.
Species excluded from Leucosyrinx and Comitas
As demonstrated here, previously to the current work, there was no clear distinction between Leucosyrinx and Comitas . Numerous species of Leucosyrinx were erroneously attributed to Comitas by Powell (1969) and are reallocated in this work. The following Indo-Pacific species were previously attributed to either Leucosyrinx or Comitas , but we are excluding them on different grounds. The species are listed in alphabetical order by their specific epithet. The species that we consider as belonging to Comitas are not treated here.
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Kingdom |
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Phylum |
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Class |
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Order |
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Family |
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Genus |
Leucosyrinx undosa ( Schepman, 1913 )
Kantor, Yuri I., Fedosov, Alexander & Puillandre, Nicolas 2025 |
Leucosyrinx canyonensis
Powell A. W. B. 1979: 230 |
Paracomitas undosa
Shuto T. 1970: 170 |
Comitas undosa
Powell A. W. B. 1969: 282 |
Leucosyrinx caecilia
Powell A. W. B. 1969: 337 |
Leucosyrinx erna
Powell A. W. B. 1969: 337 |
Antimelatoma canyonensis
Dell R. K. 1956: 142 |
Leucosyrinx caecilia
Thiele J. 1925: 202 |
Leucosyrinx erna
Thiele J. 1925: 201 |
Leucosyrinx sansibarica
Thiele J. 1925: 181 |
Surcula undosa
Schepman M. M. 1913: 61 |
Brachytoma griffithii
Powell A. W. B. 1969: 340 |
Thiele J. 1904: 173 |