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The Journal of Adam Mickiewicz University

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Volume 17, Issue 2

The Danian and Selandian calcareous benthic foraminiferal assemblages and biostratigraphy of Western Siberia

Vera Podobina
Published Online: 2011-07-04 | DOI: https://doi.org/10.2478/v10118-011-0006-5

The Danian and Selandian calcareous benthic foraminiferal assemblages and biostratigraphy of Western Siberia

Danian and Selandian successions in western Siberia are rich in calcareous benthic foraminifers. The assemblages with a constant systematic composition that have the widest lateral occurrence are distinguished as foraminiferal zones. The Brotzenella praeacuta Zone was established in the low-carbonate, clayey beds that form the transition from the Gankinskaya Suite to the Talitskaya Suite. These transitional beds are assigned to the Danian. The calcareous benthic foraminifers in this zone occur mainly together with agglutinated forms. The zone is traced along the areas of the largest subsidence of the Mesozoic-Cenozoic basin, principally in depressions. The transition from the Cretaceous to the Palaeogene is represented by a continuous succession, in which the Danian deposits escaped from erosion and were found to contain the B. praeacuta assemblage. In Danian rocks with a shallow-marine facies (near Beryozovo and in the Ust'-Tym depression, Fig. 1), the Bathysiphon nodosarieformis - Glomospira charoides assemblage occurs. It is dominated by primitive forms in addition to more advanced tests (mainly Late Maastrichtian relic species).

The overlying Selandian (Middle Palaeocene) foraminiferal assemblages are assigned to the Talitskaya Suite. The Ammoscalaria friabilis assemblage is widely spread and is represented mainly by agglutinated quartz-siliceous forms. Beds with these species are attributed to the Ammoscalaria friabilis Zone, which can be correlated with beds in the East containing Cyclammina coksuvorovae. The Cibicidoides proprius assemblage is known from the lower and middle beds of the Talitskaya Suite in Transuralia, the Omsk Depression and more south-eastern areas; the species of this assemblage are characteristic of the Selandian.

Keywords: benthic foraminifera; Danian; Selandian; Western Siberia

  • Aleskerova, Z.T., Li, P.F., Osyko, T.I., Rostovtsev, N.N. & Tolstikhina, M.A., 1957. Stratigrafiya mezozoyskikh i tretichnykh otlozheniy zapadnosibirskoy nizmennosti. [Stratigraphy of the Mesozoic and Tertiary deposits of the West-Siberian Plain]. Sovetskaya Geologiya (Soviet Geology) 55, 146-172. [in Russian]Google Scholar

  • Berggren, W.A. & Pearson, P.N., 2005. A revised tropical to subtropical Paleogene planktonic foraminiferal zonation. Journal of Foraminiferal Research 35, 279-298.Google Scholar

  • Brotzen, F., 1948. The Swedish Paleocene and its foraminiferal fauna. Sveriges Geologiska Undersökning, Ser. C 493 (Årsbok 42/2), 140 pp., 19 plates.Google Scholar

  • Dain, L.G., 1961. Nekotoryie vidy foraminifer melovykh otlozheniy Shumikhinskogo rayona Chelyabinskoy oblasti [Some foraminiferal species from the Cretaceous deposits of the Shumikhinskian District of the Cheliabinsk Region]. [In:] L.P. Grozdilova & I.N. Ionina (Eds): Microfauna of the USSR. Collection 12. Gostoptekhizdat, Leningrad, 4-42, 2 plates. [in Russian]Google Scholar

  • Freiman, E.V., 1960. O novom datsko-paleotsenovom komplekse foraminifer Zapadnoy Sibiri [On a new Danian-Palaeocene foraminiferal assemblage of Western Siberia]. [In:] Proceedings of SNIIGGMS (Proceedings of Siberian Research Institute of Geology, Geophysics & Minerals) 8, 212-215. [in Russian]Google Scholar

  • Interdepartmental Stratigraphic Committee of Russia, 2001. Unifitsirovannaya regional'naya stratigraficheskaya skhema paleogenovykh i neogenovykh otlozheniy zapadnosibirskoy nizmennosti. [Unified regional stratigraphic scheme of the Palaeogene and Neogene deposits of the West-Siberian plain], 2001. Siberian Research Institute of Geology, Geophysics and Mineral Resources (SNIIGGiMS), Novosibirsk. [in Russian]Google Scholar

  • Lipman, R. Kh., Burtman, E.S. & Khokhlova, I.A., 1960. Stratigrafiya i fauna paleogenovykh otlozheniy zapadnosibirskoy nizmennosti. [Stratigraphy and fauna of the Palaeogene deposits of the West Siberian Plain]. Proceedings of All Union Geological Institute (VSEGEI), new series 28, 231 pp., 23 plates. [in Russian]Google Scholar

  • Podobina, V.M., 1975. Foraminifery verkhnego mela i paleogena zapadnosibirskoy nizmennosti, ikh znacheniye dlya stratigrafii. [The Late Cretaceous and Palaeogene foraminifers of the West-Siberian Plain and their significance for the stratigraphy]. Tomsk University Press, Tomsk, 264 pp., 40 plates. [in Russian]Google Scholar

  • Podobina V.M., 1990. Novyie dannyie po biostratigrafii paleotsena Zapadnoy Sibiri [New data on the Palaeocene biostratigraphy of western Siberia]. Byulleten' Moskovskogo obshchestva ispytateley prirody [Bulletin of the Moscow Society of Nature Testers], Geology branch 65/5, 61-67. [in Russian]Google Scholar

  • Podobina, V.M., 1992. Datskiy yarus Zapadnoy Sibiri [The Danian stage of western Siberia]. [In:] V.M. Podobina (Ed.): Materials on paleontology and stratigraphy of Western Siberia. Tomsk University Press, Tomsk, 80-83. [in Russian]Google Scholar

  • Podobina, V.M., 1998. Foraminifery i biostratigrafiya paleogena Zapadnoy Sibiri [Palaeogene Foraminifera and biostratigraphy of western Siberia]. "NTL" Press, Tomsk, 338 pp., 62 plates. [in Russian]Google Scholar

  • Podobina, V.M., 2003. Paleocene biota of the West Siberian. [In:] S.L. Wing, P.L. Gingerich, B. Schmitz & E. Thomas (Eds): Causes and consequences of globally warm climates in the early Paleogene. Geological Society of America Special Paper 369, 181-204.Google Scholar

  • Podobina, V.M., 2006. Novyie dannyie po stratigrafii i foraminifery morskogo paleogena yugo-vostoka Zapadnoy Sibiri [Recent data on the stratigraphy and the marine Palaeogene foraminifers of south-eastern western Siberia]. [In:] Geology and mineral resources of South Siberia. Bulletin of Tomsk State University (Vestnik TGU) 104: 17-21. [in Russian]Google Scholar

  • Podobina V.M., 2008. Paleocene foraminifera and biostratigraphy of Western Siberia. [In:] M.A. Kaminski & R. Coccioni (Eds): Proceedings of the 7th International Workshop on Agglutinated Foraminifera. Grzybowski Foundation Special Publication 13, 183-198, 3 plates.Google Scholar

  • Podobina, V.M., 2009. Foraminifery, biostratigrafiya verkhnego mela i paleogena Zapadnoy Sibiri [Foraminifers, biostratigraphy of the Upper Cretaceous and Palaeogene of western Siberia]. Tomsk State University Press, Tomsk, 432 pp., 73 plates. [in Russian]Google Scholar

  • Podobina, V.M. & Kseneva, T.G., 2005. Upper Cretaceous zonal stratigraphy of the West Siberian Plain based on foraminifera. Cretaceous Research 26, 133-143.Google Scholar

  • Shatskiy, S.B., 1973. Marine and continental Palaeogene of Siberia. Novosibirsk, Nauka, 140 pp. [in Russian].Google Scholar

  • Stratigraphic Code of Russia, 2006. Chapter VII, item VII.10. St.-Petersburg, VSEGEI Press. [in Russian]Google Scholar

  • Subbotina, N.N. [Ed.], 1964. Foraminifery melovykh i paleogenovykh otlozheniy zapadnosibirskoy nizmennosti. [Foraminifera of Cretaceous and Palaeogene deposits of the West-Siberian Plain]. Nedra, Leningrad, 456 pp., 66 plates. [in Russian]Google Scholar

  • Subbotina, N.N. & Kiselman, E.N., 1961. Mikrofaunisticheskaya zona Anomalina praeacuta v zapadnosibirskoy nizmennosti. [The microfaunal Anomalina praeacuta Zone in the West-Siberian Plain]. [In:] N.N. Rostovtsev (Ed.): Resolutions and proceedings of the interdepartmental session on the revision and refinement of the stratigraphic maps of the West-Siberian Plain. Gostoptekhizdat, Leningrad, 243-252. [in Russian]Google Scholar

  • Vasilenko, V.P., 1954. Anomalinidy. Iskopayemiye foraminifery SSSR. [Anomalinidae. The fossil Foraminifera of the USSR]. Proceedings of VNIGRI 80. Gostoptekhizdat, Leningrad, 280 pp., 36 plates. [in Russian]Google Scholar

About the article

Published Online: 2011-07-04

Published in Print: 2011-06-01

Citation Information: Geologos, Volume 17, Issue 2, Pages 97–110, ISSN (Online) 2080-6574, ISSN (Print) 1426-8981, DOI: https://doi.org/10.2478/v10118-011-0006-5.

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