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Dynamics of Conodont Ecogeochemistry and Turnover of Pelagic Ecosystems during the Hangenberg Crisis and Recovery (Using the Example of Northeastern Laurussia)

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Abstract

Changes in the nearshore pelagic ecosystems at the Devonian–Carboniferous boundary are considered. These changes are reconstructed based on conodont ecogeochemistry, carbon isotopic composition of marine carbonates, and abundance of the unilocular foraminifer Bisphaera.

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Authors and Affiliations

  1. Institute of Geology of Komi Science Centre of the Ural Branch of the Russian Academy of Sciences, 167982, Syktyvkar, Russia

    A. V. Zhuravlev

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  1. A. V. Zhuravlev
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Correspondence to A. V. Zhuravlev.

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Translated by S. Avodkova

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Zhuravlev, A.V. Dynamics of Conodont Ecogeochemistry and Turnover of Pelagic Ecosystems during the Hangenberg Crisis and Recovery (Using the Example of Northeastern Laurussia). Paleontol. J. 56, 1026–1028 (2022). https://doi.org/10.1134/S0031030122090088

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  • DOI: https://doi.org/10.1134/S0031030122090088

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