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Marine Isotopic Stage 3 in Northeastern Europe: Geochronology and Eventsстатья
Информация о цитировании статьи получена из
Web of Science
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 23 января 2020 г.
- Авторы: Zaretskaya N.E., Korsakova O.P., Panin A.V.
- Журнал: Russian Geology and Geophysics
- Том: 60
- Номер: 8
- Год издания: 2019
- Издательство: ELSEVIER SCIENCE BV
- Местоположение издательства: PO BOX 211, AMSTERDAM, NETHERLANDS, 1000 AE
- Первая страница: 911
- Последняя страница: 925
- DOI: 10.15372/RGG2019056
- Аннотация: The paper presents new lithological, geochronological, and biostratigraphic data on the studied sections of the Middle Valdai interstadial sediments in the sections of two terraces in the basin of the Severnaya Dvina River and on the southern coast of the Kola Region and its southwestern part. The obtained data are correlated with the data available for other regions of northeastern Europe. TheSevernaya Dvina River was found to have flowed into a marine reservoir existed in the White Sea basin throughout the Middle Valdai time corresponding to Marine Isotopic Stage 3 (MIS 3). The alluvial sedimentation in the river catchment area occurred in an environment of base level instability and permanently changing climate. In northeastern Europe, the warmest (optimum) intervals are related to the time spans of 47–43 and 31.3–29.2 cal. ka BP. In general, the available data point to 12 warming and cooling episodes in northeastern Europe.
- Добавил в систему: Зарецкая Наталия Евгеньевна
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