Pleuriocardia (Incacardium) schneideri, DeVries, 2019

DeVries, Thomas J., 2019, Early Paleogene brackish-water molluscs from the Caballas Formation of the East Pisco Basin (Southern Peru), Journal of Natural History 53 (25), pp. 1533-1584 : 1550-1551

publication ID

https://doi.org/ 10.1080/00222933.2018.1524032

DOI

https://doi.org/10.5281/zenodo.3691677

persistent identifier

https://treatment.plazi.org/id/03BB2338-E35A-E228-FED3-A02C5E88FE70

treatment provided by

Valdenar

scientific name

Pleuriocardia (Incacardium) schneideri
status

sp. nov.

Pleuriocardia (Incacardium) schneideri sp. nov.

( Figure 3 View Figure 3 (l – q))

Diagnosis

Shell ovate to elongate. Broad posterior sulcus extends from umbones to ventral margin. Ribs numerous with bulbous spines centred on ribs.

Description

Shell thin, to about 25 mm long, trapezoidal, H:L = 0.75. Subequilateral, umbones highly inflated; remainder of valves convex, excepting broad sulcus in front of weak posterior umbonal ridge and excepting irregular commarginal inflexions of curvature, especially ventrally. Beaks orthocline, orthogyrate on juveniles, overhanging hinge line; prosocline on adults. Posterior ligament narrow, less than half the length of posterodorsal margin. Dorsal margin sloping sharply anteriorly, less steeply posteriorly. Anterior broadly rounded; posterior with angled umbonal ridge. Anterodorsal and umbonal areas with 18 – 20 strong radial ribs, triangular in cross section, broader across middle of valve. U-shaped interspaces with weakly and irregularly raised commarginal growth lines. Posterodorsal flattened surface with 5 – 6 smaller triangular ribs, equal to each other in size. Circular or elongate bulbous spines or knobs rise from tops of radial ribs across middle three-fifths of valve; knobs more common at inflexions points, intersections with strong commarginal growth lines, and on specific radial ribs; other knobs randomly placed. Hinge plate and teeth not visible.

Remarks

Specimens of Pleuriocardia (Incacardium) schneideri sp. nov. differ from the Late Cretaceous type species, P. (Incacardium) mellisum Olsson, 1944 , in having fewer ribs in front of the posterior umbonal ridge (20 – 22, rather than 28) and interspaces that have a rounded profile, not triangular. The Caballas Formation species differs from the late Campanian to early Maastrichtian Pleuriocardia (Incacardium) trechmanni Schneider, 1999 , from Jamaica, in being longer than high, having fewer ribs anterior to the posterior umbonal ridge (20 – 22, rather than 25), and having nodes that are smaller, less bulbous, and more often aligned on the intersection of radial ribs with strong commarginal growth lines.

Etymology

Named in recognition of Jay A. Schneider, authority on the phylogeny of Incacardium and other cardiids.

Material

UWBM 107573 , holotype, left valve, B8772 (type locality), L (21.5), H 20.6, W (12.3) ; remainder are paratypes: UWBM 107574 , B8770, L 25.0, H 25.4, W 14.4 (pair) ; UWBM 107575 , B8769, L (13.7), H 11.8, W 11.5 (pair) ; UWBM 107576 , mould of left valve, B8769, L (25.5), H (19.4), W (4.9) ; MUSM INV 245 , B8772, L (19.1), H (19.1), W (9.2) (pair) ; MUSM INV 246 , mould of right valve, B8772, L (20.4), H (18.9), W (6.0) (pair) ; MUSM INV 247 , B8772, L (21.1), H (16.9), W (11.8) (pair).

Occurrence

Lower Paleogene, Cuenca Member, Caballas Formation, East Pisco Basin, southern Peru.

Kingdom

Animalia

Phylum

Mollusca

Class

Bivalvia

Order

Venerida

SuperFamily

Cardioidea

Family

Cardiidae

Genus

Pleuriocardia

SubGenus

Incacardium

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