Granulifusus discrepans
Authors/Creators
- 1. Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Leninski prospect 33, 119071, Moscow, Russian Federation. Institut de Systématique, Evolution, Biodiversité ISYEB - UMR 7205 - CNRS, MNHN, UPMC, EPHE, Muséum national d'Histoire naturelle, Sorbonne Universités, 57 rue Cuvier, CP 26, F- 75005, Paris, France. Academy of Natural Sciences of Drexel University, 1900 Benjamin Franklin Parkway, Philadelphia, PA 19103 - 1195, USA.
Description
Granulifusus discrepans (Kuroda & Habe, 1961)
Figs 3 A–E, 4A
Pseudolatirus discrepans Azuma, 1960: 45 (ex Kuroda MS). nomen nudum.
Pseudolatirus discrepans – Kuroda & Habe in Habe 1961: 66, pl. 33, fig. 6. — Habe 1962: 102, pl. 33, fig. 6. — Higo, Callomon & Gotō 2001: 87, fig. G3002 (holotype illustrated). — Mallard & Robin 2017: 152.
Granulifusus discrepans – Poppe 2008: pl. 343, fig. 1.
Molecular diagnosis
A molecular diagnosis is given in Table 2.
Type material
Holotype
JAPAN: off Cape Ashizuri, southwestern Shikoku (NSMT Mo 40377) (not seen).
Sequenced material
SOLOMON SEA: 1 lv, MADEEP, stn CP4337, SE Ainto Bay, New Britain, 06°07’ S, 149°17’ E, 287– 447 m (MNHN IM-2013-46327).
PHILIPPINES: AURORA 2007, 1 lv, stn CP2657, 16°01′ N, 121°51′ E, 342–358 m (MNHN IM-2007- 34604); 2 lv, stn CP2673, 15°01′ N, 121°45′ E, 431–493 m (MNHN IM-2007-34583, MNHN IM-2007- 34488); 2 lv, stn CP2732, 15°27′ N, 121°36′ E, 556 m (MNHN IM-2007-34580, MNHN IM-2007-34581).
Other examined material
PAPUA NEW GUINEA: 1 lv, PAPUA NIUGINI, stn CP3949, 5°12′ S, 145°51′ E, 380–407 m (MHNH 2013-15374, not sequenced); 1 lv, stn CP4023, 5°22′ S; 145°48′ E, 340–385 m (MNHN IM-2013-9777, not sequenced).
Description
Shell large, with multispiral protoconch of 2.75 conical, smooth, convex, grayish whorls, last ¼ whorl with 6–7 rounded axial riblets progressing in strength, protoconch/teleoconch boundary without varix, defined by appearance of spiral sculpture. Protoconch diameter 960 µm, exposed height 890 µm (Fig. 3E). Teleoconch with regularly convex whorls, upper ones slightly angulated, with long slightly sinuous to nearly straight siphonal canal; aperture in young specimens with 3–4 plicae, in adult with a single columellar plica, delimitating siphonal canal, and sometimes with indistinct parietal tooth. Axial sculpture of distinct axial ribs, 7–8 per whorl on upper whorls, obsolete on posterior whorls in shells over 50 mm. Spiral sculpture of 2–3 raised cords on periphery of upper whorls and numerous thin riblets of even strength. On posterior whorls, cords obsolete and some riblets more pronounced. Background colour tan, with darker brown spiral bands along suture.
Radula (MNHN IM-2013-46327, SL 18.2 mm, Fig. 4A) 1.83 mm in length (32% of AL without canal), of 75 transverse rows of teeth, of which 35 nascent. Radula narrow, distance between outer edges of lateral teeth about 65 µm (1.12% of AL). Lateral teeth medium broad, arcuate, with attenuated outer anterior corner, producing short ‘handle’. Lateral teeth with five closely spaced, slightly curved cusps similar in length, small outermost cusp (seen on lower right lateral tooth on Fig. 4A), and much smaller but distinct innermost cusp. Central tooth small, very narrow, trapezoid, with three subequal cusps. Narrow but distinct transverse folds of radular membrane situated serially between rows of lateral teeth. Couto (2016: fig. 58) illustrated the radula of an adult specimen (SL 66 mm). The lateral teeth were relatively much broader, with 6 main cusps nearly identical in size and an additional innermost cusp. The radula had a similar width (1.1% of AL, measurements taken from photo) to the one studied herein; the differences in teeth morphology can possibly be explained by ontogenetic variability.
Distribution
From Japan throughout the East China Sea to the Philippines and the Solomons.
Remarks
This is the largest species of Granulifusus, which attains a shell length over 90 mm (http://www.conchology.be, last accessed 6 Mar. 2017). Due to the ontogenic change in sculpture pattern, the shell morphology differs from that in other Recent members of the genus, but the radula is similar. Young specimens bear a superficial resemblance to specimens of the Miocene species Pseudolatirus bilineatus of similar size (compare Fig. 3C, G with Fig. 3 D’, F’).
Notes
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Linked records
Additional details
Identifiers
Biodiversity
- Collection code
- NSMT
- Scientific name authorship
- Kuroda & Habe
- Kingdom
- Animalia
- Phylum
- Mollusca
- Order
- Neogastropoda
- Family
- Fasciolariidae
- Genus
- Granulifusus
- Species
- discrepans
- Taxon rank
- species
- Type status
- holotype
- Taxonomic concept label
- Granulifusus discrepans (Kuroda, 1961) sec. Kantor, Fedosov, Snyder & Bouchet, 2018
References
- Habe T. 1961. Coloured Illustrations of the Shells of Japan. Vol. II. Hoikusha, Osaka.
- Azuma M. 1960. A Catalogue of the Shell-bearing Mollusca of Okinoshima, Kashiwajima and the adjacent Area (Tosa Province) Shikoku, Japan. Tosa-Wan Kai-Rui Bun-Ken Kan-Ko-Kai. Tosa Bay Malacological Literature Publication Committee.
- Habe T. 1962. Coloured Illustrations of the Shells of Japan. Vol. II, 2 nd edition. Hoikusha, Osaka.
- Higo S., Callomon P. & Goto Y. 2001. Catalogue and Bibliography of the marine Shell-bearing Mollusca of Japan. Gastropoda, Bivalvia, Polyplacophora, Scaphopoda. Type Figures. Elle Scientific Publications, Osaka-fu, Japan.
- Mallard D. & Robin A. 2017. Recent Fasciolariidae. Association Francaise de Conchiologie, Paris and Conchbooks, Harxheim.
- Poppe G. T. 2008. Philippine Marine Mollusks. Vol. 2. (Gastropoda - Part 2). Conchbooks, Harxheim.
- Poppe G. T. & Tagaro S. P. 2006. A new Fusinus from the Philippines. Visaya 1: 48 - 50.
- Cossignani T. 2017. Pseudolatirus jeanpierrevezzaroi nuova specie dal Vietnam. Malacologia, Mostra Mondiale 95: 14 - 15.
- Okutani T. 1975. Glimpse of benthic molluscan fauna occupying the submarine bank, Kurose, near Hachijo Island, Japan. Venus, Japanese Journal of Malacology 33: 185 - 205.