Obtusoconus vostokovae (Vassiljeva, 1990)
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.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.