Kasimovian (Upper Pennsylvanian) Conodonts of the Shcherbatovka Section (Oka-Tsna Swell)
- Авторы: Goreva N.V.1, Alekseev A.S.2,3, Leontiev D.I.4
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Учреждения:
- Geological Institute, Russian Academy of Sciences
- Lomonosov Moscow State University
- Borissiak Paleontological Institute, Russian Academy of Sciences
- Karpinsky Russian Geological Research Institute
- Выпуск: Том 53, № 8 (2019)
- Страницы: 827-831
- Раздел: Article
- URL: https://journals.rcsi.science/0031-0301/article/view/168837
- DOI: https://doi.org/10.1134/S0031030119080070
- ID: 168837
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Аннотация
Kasimovian (Upper Pennsylvanian) conodonts are studied from the Shcherbatovka section (Oka-Tsna Swell, Ryazan Region). The Khamovnikian and Dorogomilovian substages are exposed in this section. The presence of the conodonts Idiognathodus turbatus and I. heckeli was established in the deeper-water facies, compared to the type area of the Khamovnikian Substage. These species are considered as the potential markers for the lower boundary of the global Kasimovian Stage of the Carboniferous. A similar assemblage is established in the sections of US Midcontinent and South China.
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N. Goreva
Geological Institute, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: n.v.goreva@mail.ru
Россия, Moscow, 119017
A. Alekseev
Lomonosov Moscow State University; Borissiak Paleontological Institute, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: aaleks@geol.msu.ru
Россия, Moscow, 119991; Moscow, 117647
D. Leontiev
Karpinsky Russian Geological Research Institute
Автор, ответственный за переписку.
Email: denis.leontew@yandex.ru
Россия, St. Petersburg, 199106
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