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

Y. D. Zakharov; M. Horacek; Y. Shigeta; A. M. Popov; T. Maekawa

doi:10.1134/S1028334X18020204

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

Авторлар: Zakharov Y.D.¹, Horacek M.², Shigeta Y.³, Popov A.M.¹, Maekawa T.⁴
Мекемелер:
1. Far East Geological Institute, Far East Branch
2. BLT Wieselburg Research Center Francisco-Josephinum
3. National Museum of Nature and Science
4. Kumamoto University
Шығарылым: Том 478, № 2 (2018)
Беттер: 161-165
Бөлім: Geology
URL: https://ogarev-online.ru/1028-334X/article/view/192140
DOI: https://doi.org/10.1134/S1028334X18020204
ID: 192140

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Аннотация

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.