PLANKTONIC FORAMINIFERS FROM SEDIMENTS OF THE SOUTHEASTERN OKHOTSK SEA (THE LAST 20000 YEARS)

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dc.contributor.author Chekhovskaya M.P.
dc.contributor.author Basov I.A.
dc.date.accessioned 2021-01-12T05:13:30Z
dc.date.available 2021-01-12T05:13:30Z
dc.date.issued 1999
dc.identifier https://elibrary.ru/item.asp?id=13321671
dc.identifier.citation Stratigraphy and Geological Correlation, 1999, , 2, 190-200
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/22714
dc.description.abstract Analysis of the taxonomic composition of planktonic foraminifers and oxygen isotope composition in their shells from the sedimentary core section V34-90, taken from the eastern slope of the Akademii Nauk SSSR Rise in the southeastern Okhotsk Sea, were used to investigate climatic and hydrologic changes in the basin for the last 20000 years according to radiocarbon dating. Periods of glaciation (20000-12500 years ago), deglaciation (12500-800 years ago) with a clearly expressed cooling event (Younger Dryas, about 10800 years ago), and postglaciation (last 8000 years) were distinguished.
dc.title PLANKTONIC FORAMINIFERS FROM SEDIMENTS OF THE SOUTHEASTERN OKHOTSK SEA (THE LAST 20000 YEARS)
dc.type Статья


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