A section of Vendian in the east of West Siberian Plate ( based on data from the Borehole Vostok 3)
A.E. Kontorovich a , A.I. Varlamov b , D.V. Grazhdankin a , G.A. Karlova a , A.G. Klets a , V.A. Kontorovicha, S.V. Saraeva, A.A. Terleev a , S.Yu. Belyaev a , I.V. Varaksina a , A.S. Efimovc, B.B. Kochneva, K.E. Nagovitsin a , A.A. Postnikova, Yu.F. Filippova
a Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the RAS, 3 prosp. Akad. Koptyuga, Novosibirsk, 630090, Russia
b Ministry of Natural Resources of the Russian Federation, Moscow
c Siberian Research Institute of Geology, Geophysics, and Mineral Resources, 67 Krasnyi prosp., Novosibirsk, 630091, Russia
Keywords: Neoproterozoic; Vendian; Cambrian; West Siberian Plate; Pre-Yenisei petroliferous subprovince
Pages: 932-939
Abstract
The Borehole Vostok 3 drilled in the east of the West Siberian Plate (Tomsk Region) revealed a Vendian section in the depth range 5002-3870 m, which was subdivided into the Poiga, Kotodzha, and Raiga Formations based on geological, geophysical, and paleontological data. In the Kotodzha and Raiga Formations, typical Upper Vendian fossils of Cloudina hartmanae and Namacalathus sp. were found along with diverse Platysolenites, which are commonly considered to be of zonal significance in Lower Cambrian strata. Hence, the stratigraphic interval with abundant diverse Platysolenites has a wider stratigraphic range than it was believed earlier and seems to cover the Upper Vendian and Lower Cambrian deposits. The Borehole Vostok 3 is the first Siberian occurrence of the fossils Namacalathus , the world's fourth occurrence of the Cloudina-Namacalathus association, and the first site where coexisting Platysolenites and typical Vendian organisms have been found. Therefore, the borehole provides one of the most informative (in paleontological context) Upper Vendian sections.
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