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N and C Isotopic Compositions of the Lower Triassic of Southern Primorye and Reconstruction of Habitat Conditions of Marine Organisms after Mass Extinction at the End of the Permian

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Abstract

Data on the N and C isotopic composition are presented for the Lower Triassic claystones of the Abrek section of southern Primorye (Far East). The results showed five N isotopic intervals and several negative C isotopic excursions of the Induan–lower Olenekian stages of the Abrek section.

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Authors and Affiliations

  1. Far East Geological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, 690022, Russia

    Y. D. Zakharov & A. M. Popov

  2. BLT Wieselburg Research Center Francisco-Josephinum, Wieselburg, 3250, Austria

    M. Horacek

  3. National Museum of Nature and Science, Tsukuba, 305-0005, Japan

    Y. Shigeta

  4. Kumamoto University, Kurokami, 860-8555, Japan

    T. Maekawa

Authors
  1. Y. D. Zakharov
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  2. M. Horacek
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  3. Y. Shigeta
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  4. A. M. Popov
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  5. T. Maekawa
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Corresponding author

Correspondence to Y. D. Zakharov.

Additional information

Original Russian Text © Y.D. Zakharov, M. Horacek, Y. Shigeta, A.M. Popov, T. Maekawa, 2018, published in Doklady Akademii Nauk, 2018, Vol. 478, No. 5, pp. 556–560.

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Zakharov, Y.D., Horacek, M., Shigeta, Y. et al. N and C Isotopic Compositions of the Lower Triassic of Southern Primorye and Reconstruction of Habitat Conditions of Marine Organisms after Mass Extinction at the End of the Permian. Dokl. Earth Sc. 478, 161–165 (2018). https://doi.org/10.1134/S1028334X18020204

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  • DOI: https://doi.org/10.1134/S1028334X18020204

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