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Biotic changes in a eustatic cyclothem: Domodedovo Formation (Moscovian, Carboniferous) of Peski quarries, Moscow Region

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Abstract

Stacking lithofacies in the Domodedovo Formation of Peski quarries show prominent changes in paleodepth and depositional environment. Distribution in the section of fusulinoids, algae, conodonts, and macrofossils are revealed. Among the latter, brachiopods and bryozoans are discussed in most detail.

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Authors and Affiliations

  1. Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997, Russia

    P. B. Kabanov, D. V. Baranova, R. V. Gorjunova, S. S. Lazarev & V. G. Malkov

  2. Geological Faculty, Moscow State University, Vorob’evy gory, Moscow, GSP-3, 119992, Russia

    A. S. Alekseev

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  1. P. B. Kabanov
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  2. A. S. Alekseev
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  3. D. V. Baranova
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  4. R. V. Gorjunova
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  5. S. S. Lazarev
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  6. V. G. Malkov
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Original Russian Text © P.B. Kabanov, A.S. Alekseev, D.V. Baranova, R.V. Gorjunova, S.S. Lazarev, V.G. Malkov, 2006, published in Paleontologicheskii Zhurnal, 2006, No. 4, pp. 3–19.

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Kabanov, P.B., Alekseev, A.S., Baranova, D.V. et al. Biotic changes in a eustatic cyclothem: Domodedovo Formation (Moscovian, Carboniferous) of Peski quarries, Moscow Region. Paleontol. J. 40, 351–368 (2006). https://doi.org/10.1134/S0031030106040010

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  • DOI: https://doi.org/10.1134/S0031030106040010

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