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
- Authors: Zakharov Y.D.1, Horacek M.2, Shigeta Y.3, Popov A.M.1, Maekawa T.4
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Affiliations:
- Far East Geological Institute, Far East Branch
- BLT Wieselburg Research Center Francisco-Josephinum
- National Museum of Nature and Science
- Kumamoto University
- Issue: Vol 478, No 2 (2018)
- Pages: 161-165
- Section: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192140
- DOI: https://doi.org/10.1134/S1028334X18020204
- ID: 192140
Cite item
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.
About the authors
Y. D. Zakharov
Far East Geological Institute, Far East Branch
Author for correspondence.
Email: yurizakh@mail.ru
Russian Federation, Vladivostok, 690022
M. Horacek
BLT Wieselburg Research Center Francisco-Josephinum
Email: yurizakh@mail.ru
Austria, Wieselburg, 3250
Y. Shigeta
National Museum of Nature and Science
Email: yurizakh@mail.ru
Japan, Tsukuba, 305-0005
A. M. Popov
Far East Geological Institute, Far East Branch
Email: yurizakh@mail.ru
Russian Federation, Vladivostok, 690022
T. Maekawa
Kumamoto University
Email: yurizakh@mail.ru
Japan, Kurokami, 860-8555
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