Spondylopecten (Plesiopecten) subspinosus (Schlotheim, 1820)

Fuersich, Franz T., Alberti, Matthias, Pandey, Dhirendra K. & Ayoub-Hannaa, Wagih S., 2022, Jurassic bivalves from the Spiti area of the Himalayas, northern India, Zitteliana 96, pp. 153-178 : 153

publication ID

https://dx.doi.org/10.3897/zitteliana.96.87253

publication LSID

lsid:zoobank.org:pub:191199E0-7F3E-4E09-A377-4ADFBF93A248

persistent identifier

https://treatment.plazi.org/id/4749B57D-9B67-532F-99BF-D7A99CE6914B

treatment provided by

Zitteliana by Pensoft

scientific name

Spondylopecten (Plesiopecten) subspinosus (Schlotheim, 1820)
status

 

Spondylopecten (Plesiopecten) subspinosus (Schlotheim, 1820) View in CoL

Plate 4, fig. 3 View Plate 4

1820 Pectinites subspinosus - Schlotheim: 223.

1938 Plesiopecten subspinosus (Schlotheim) - Weir: 50, pl. 3, fig. 18.

1952 Chlamys (Plesiopecten) subspinosa (Schlotheim) - Cox: 18, pl. 1, figs 9-12.

1995 Spondylopecten (Plesiopecten) subspinosus ( Schlotheim 1820) - Jaitly et al.: 194, pl. 18, figs 14-15.

Material.

One composite mould of a right valve and one external mould from the upper part of the lower member at the Hikkim-Kaza road (SNSB-BSPG 2020 XCIX 23).

Description.

Specimens small (H: 5.4 mm; K: 5.8 mm), suborbicular, equilateral, weakly inflated. Auricles large, distinctly separated from disk, anterior one incomplete. Surface of composite mould covered with 11-13 positive radial structures interpreted herein as corresponding to radial ribs, which are angular and show a tendency to bifurcate towards the ventral margin.

Remarks.

Despite the poor preservation of the specimens (lack of shell), they can be safely assigned to S. (Plesiopecten) subspinosus , based on the number and angularity of their ribs (compare Johnson 1984, p. 84).

Kingdom

Animalia

Phylum

Mollusca

Class

Bivalvia

SubClass

Protobranchia

Order

Pectinida

Family

Pectinidae

Genus

Spondylopecten