|
ИСТИНА |
Войти в систему Регистрация |
ИСТИНА ЦЭМИ РАН |
||
The foraminiferal zonal scale of the Devonian-Carboniferous boundary beds in Russia and Western Kazakhstan and its correlation with ammonoid and conodont scalesстатья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 8 декабря 2021 г.
- Авторы: Kulagina E.I., Zaytseva E.L., Vevel Ya A., Stepanova T.I., Gibshman N.B., Nikolaeva S.V., Kononova L.I., Plotitsyn A.N.
- Журнал: Palaeobiodiversity and Palaeoenvironments
- Том: 101
- Год издания: 2021
- Издательство: Springer Verlag
- Местоположение издательства: Germany
- Первая страница: 561
- Последняя страница: 588
- DOI: 10.1007/s12549-020-00439-y
- Аннотация: This paper reviews the foraminiferal biostratigraphy of the Devonian Carboniferous (D-C) boundary beds in Russia and Western Kazakhstan. The regional records of the zonal successions of Russia are summarised from sections and boreholes of the Volga-Urals Subregion of the Hast European Platform (Syzran no. 401 Borehole, Melekesskaya no.l Borehole); Timan-Pcchora Province of the East European Platform (Kamenka Section); South Urals (Sikaza, Zigan, Ryauzyak and Dzcrzhinka sections); Middle Urals (Pcrshino Section); and West Siberia, Vagai-Ishim Basin (Borehole no. 1 Kurgan-Uspenskaya), and the zonal successions of Western Kazakhstan arc summarised from the Mugodzhary Mountains. Three foraminiferal biozones can be defined in the interval comprising the latest Devonian and earliestCarboniferous: Quasiendothyra kobeitusana Zone, the Tournayellina pseudobeata remnant Quasiendothyra Zone, and the Earlandia minima Zone. The D-C boundary interval is situated within the Tournayellina pseudobeala-tenMMvM. Quasiendothyra Zone. A correlation with the ammonoid and conodont zonations is proposed, which is useful for correlating deep-water and shallow-water successions.
- Добавил в систему: Зайцева Елена Леонидовна