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Paleocene Deposits of the Yamato Rise (Sea of Japan) and Their Formation Conditions

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Abstract

A palynological assemblage, which was identified during micropaleontological study of the oldest Cenozoic sedimentary cover of the Sea of Japan found at the Yamato Rise, allowed the substantiation of the late Paleocene (59.2–56.0 Ma) age of host deposits. The findings of only marine microfossils in these deposits, the high values of paleosalinity indicators (B, B/Ga), the chemical composition of authigenic minerals, as well as the presence of organic aggregates similar to marine algae, prove a marine genesis of these deposits. It is suggested that sedimentation occurred at the periphery of an epicontinental shallow marine basin under a subtropical climate.

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ACKNOWLEDGMENTS

We are grateful to L.V. Osipova for chemical-technical treatment of samples, V.K. Annin for the identification of foraminifers, and N.K. Vagina for help in preparation of the manuscript.

Funding

This work was supported by the Ministry of Science and Higher Education (project no. 121021700342-9).

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Authors and Affiliations

  1. Il’ichev Pacific Oceanological Institute, Far Eastern Branch, Russian Academy of Sciences, 690041, Vladivostok, Russia

    E. P. Terekhov & I. B. Tsoy

  2. Federal Scientific Center of the East Asia Terrestrial Biodiversity, Far Eastern Branch, Russian Academy of Sciences, 690022, Vladivostok, Russia

    V. S. Markevich

  3. Far East Geological Institute, Far Eastern Branch, Russian Academy of Sciences, 690000, Vladivostok, Russia

    N. N. Barinov

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  1. E. P. Terekhov
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Terekhov, E.P., Markevich, V.S., Tsoy, I.B. et al. Paleocene Deposits of the Yamato Rise (Sea of Japan) and Their Formation Conditions. Russ. J. of Pac. Geol. 17, 147–163 (2023). https://doi.org/10.1134/S1819714023020069

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