Obtusoconus vostokovae (Vassiljeva, 1990)

Kouchinsky, Artem, Bengtson, Stefan, Landing, Ed, Steiner, Michael, Vendrasco, Michael & Ziegler, Karen, 2017, Terreneuvian stratigraphy and faunas from the Anabar Uplift, Siberia, Acta Palaeontologica Polonica 62 (2), pp. 311-440 : 339-340

publication ID

https://doi.org/ 10.4202/app.00289.2016

persistent identifier

https://treatment.plazi.org/id/03AD87A8-FF87-6D3A-FCCF-F893674081D4

treatment provided by

Felipe

scientific name

Obtusoconus vostokovae
status

 

Obtusoconus vostokovae View in CoL (Vasil’eva, 1990)

Fig. 13F View Fig .

Material.—Twelve internal moulds, including figured SMNH Mo181976, from sample 5a/34.5 (section 96-5a, Fig. 2 View Fig ), Emyaksin Formation (SOM 1), Anabar Uplift, Siberian Platform, Russia. Correlated with the lower part of Cambrian Stage 2.

Description.—Bilaterally symmetrical, rapidly expanding orthoconic shells with broad oval aperture (length/width ratio of ca. 1.5) and a globular slightly displaced protoconch. The inner shell surface (as replicated on the internal moulds) has wide and low concentric folds.

Remarks.—The form is originally known as Stephaconus vostokovae Vasil’eva, 1990, from the Emyaksin Formation, Udzha River, northern Siberian Platform, from the Tommotian Stage (after Vasil’eva 1990). Obtusoconus vostokovae is distinguished from other species of the genus by a relatively broader shell and larger globular protoconch.

Stratigraphic and geographic range.— Cambrian Stage 2 of the Siberian Platform.

Kingdom

Animalia

Phylum

Mollusca

Family

Scenellidae

Genus

Obtusoconus

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