Lenatoechia octjabrensis, Modzalevskaya, 2003

Modzalevskaya, Tatiana L., 2003, Silurian and Devonian brachiopods from Severnaya Zemlya (Russian Arctic), Geodiversitas 25 (1), pp. 73-107 : 87-88

publication ID

https://doi.org/ 10.5281/zenodo.5375016

persistent identifier

https://treatment.plazi.org/id/03A0162A-E949-FFA6-DAE3-FA7579221DD4

treatment provided by

Marcus

scientific name

Lenatoechia octjabrensis
status

sp. nov.

Lenatoechia octjabrensis n. sp. ( Figs 14 View FIG J-P, R, S; 16)

HOLOTYPE. — N 40/12991, CNIGR Museum , St. Petersburg ( Fig. 14 View FIG N-P), conjoined valves; L = 8.8 mm, W = 8.3 mm, T = 7.2 mm.

ETYMOLOGY. — After the October Revolution Island . TYPE LOCALITY. — Loc. 11, Matusevich River, October Revolution Island ; Samojlovich Formation.

AGE. —?Llandovery-Wenlock.

MATERIAL EXAMINED. — Mainly conjoined valves of good preservation, one specimen from loc. 11, bed 6B, 10 specimens from loc. 2, bed 66, Matusevich River ; 65 specimens from loc. 117v, Ushakov River , October Revolution Island ( Männik et al. 2002: figs 1, 2, 5) ; Samojlovich Formation.

MEASUREMENTS (IN MM). — L = 4.7-8, W = 5.7-8.3, T = 4.6-7.2.

DIAGNOSIS. — Shells subtriangular in outline, strongly biconvex in lateral profile; costae rounded, low and numerous; anterior margin uniplicate.

DESCRIPTION

Shells small, equally (strongly) biconvex, with subtriangular outline and numerous ribs. Ventral umbo and pointed beak incurved, narrow, with delthyrium closed by deltidial plates. Ventral sinus and dorsal fold weakly developed, anterior margin uniplicate. Surface covered by rounded, equal and high ribs (in total 35) with the width of the ribs exceeding their interspaces. Ventral valve with long dental plates and massive teeth. The dorsal interior contains a discrete cardinal plate and septalium, supported by broad, massive, short septum, that extends approximately half the valve length ( Fig. 16 View FIG ).

COMPARISON

The pattern of the ribs, weakly developed sinus, fold, and uniplicated anterior margin are similar to those of Lenatoechia ramosa ( Nikiforova, 1961) from the Talikit and Omnutakh formations of East Siberia ( Nikiforova & Andreeva 1961: 207, pl. XLIV, figs 8, 9). The new species differs from L. ramosa by having smaller size and possessing a subtriangular outline.

T

Tavera, Department of Geology and Geophysics

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