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Doklady Earth Sciences

, Volume 481, Issue 1, pp 862–865 | Cite as

First Findings of Trace Fossils from the Tavda Formation (Middle–Upper Eocene) in the Southwestern Part of Western Siberia

  • I. I. Nesterov
  • Ya. S. Trubin
  • P. V. Smirnov
  • P. A. Yan
Geology
  • 11 Downloads

Abstract

Trace fossils have been found for the first time in the Tavda Formation shallow marine facies, and their possible indicative value has been evaluated. The results of the ichnofossil study suggest that the Tavda Basin had low hydrodynamics. Under these conditions boreal and thetic waters of different characteristics were blended, which caused periodic formation of thermohaline water stratification and anoxic conditions in bottom water levels. Such periodic events conditioned mass extinctions of a wide variety of the Eocene marine biota thus preconditioning the development of freshwater fauna in the upper levels of the Tavda Sea along with saturation of the index beds of the Tavda Formation with micro- and macrofossils.

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References

  1. 1.
    L. B. Bakieva, Palynology and Stratigraphy of Paleogene of West Siberian Trans-Ural and Central Lithofacies Regions (Tyumen State Oil and Gas Univ., Tyumen, 2005) [in Russian].Google Scholar
  2. 2.
    O. N. Vasil’eva, Tr. Inst. Geol. Geokhim. im. Akad. A. N. Zavaritskogo, No. 162, 8–20 (2015).Google Scholar
  3. 3.
    V. A. Grossgeim and I. A. Korobkov, Stratigraphy of the USSR. Paleogene System (Nedra, Moscow, 1975) [in Russian].Google Scholar
  4. 4.
    V. M. Podobina and A. I. Chernyshov, Vestn. Tomsk. Gos. Univ., No. 354, 216–220 (2012).Google Scholar
  5. 5.
    Unified Regional Stratigraphical Sectional Planes of Neogene and Paleogene Deposits in the West Siberian Plain. Explanatory Note (Siberian Sci. Res. Inst. Geol., Geophys., Miner, Raw Mater., Novosibirsk, 2001) [in Russian].Google Scholar
  6. 6.
    M. A. Akhmetiev, Russ. Geol. Geophys. 52 (10), 1075–1091 (2011).CrossRefGoogle Scholar
  7. 7.
    M. A. Akhmet’ev, G. N. Aleksandrova, V. N. Beniamovskii, D. I. Vitukhin, Z. I. Glezer, Z. N. Gnibidenko, V. D. Dergachev, Zh. A. Dolya, N. I. Zaporozhets, G. E. Kozlova, I. A. Kul’kova, I. A. Nikolaeva, M. N. Ovechkina, E. P. Radionova, and N. I. Strel’-nikova, Stratigr. Geol. Correl. 12 (5), 495–513 (2004).Google Scholar
  8. 8.
    M. A. Akhmet’ev, G. N. Aleksandrova, E. O. Amon, V. N. Beniamovskii, E. M. Bugrova, O. N. Vasil’eva, Z. I. Glezer, V. I. Zhelezko, N. I. Zaporozhets, G. E. Kozlova, I. A. Nikolaeva, T. V. Oreshkina, L. A. Panova, E. P. Radionova, N. I. Strel’nikova, and A. I. Yakovleva, Stratigr. Geol. Correl. 9 (2), 132–158 (2001).Google Scholar
  9. 9.
    R. G. Bromley and A. A. Ekdale, Science 224, 872–874 (1984).CrossRefGoogle Scholar
  10. 10.
    R. G. Bromley, Trace Fossils. Biology, Taphonomy and Applications (Chapman and Hall, London, 1996).Google Scholar
  11. 11.
    T. P. Malyshkina, Paleontol. J. 46 (4), 392–399 (2012).CrossRefGoogle Scholar
  12. 12.
    N. I. Zaporozhets and M. A. Akhmetiev, Stratigr. Geol. Correl. 21 (1), 107–130 (2013).CrossRefGoogle Scholar

Copyright information

© Pleiades Publishing, Ltd. 2018

Authors and Affiliations

  • I. I. Nesterov
    • 1
  • Ya. S. Trubin
    • 1
  • P. V. Smirnov
    • 1
    • 2
  • P. A. Yan
    • 3
  1. 1.Tyumen Industrial UniversityTyumenRussia
  2. 2.Clausthal University of TechnologyClausthal-ZellerfeldGermany
  3. 3.Trofimuk Institute of Oil and gas geology and Geophysics, Siberian BranchRussian Academy of ScienceNovosibirskRussia

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