PALEOGENE CLIMATIC FLUCTUATIONS AND BIOTIC MIGRATIONS IN THE NORTH PACIFIC

dc.contributor.author	Beniamovskii V.N.
dc.contributor.author	Gladenkov Yu.B.
dc.date.accessioned	2020-11-30T07:39:35Z
dc.date.available	2020-11-30T07:39:35Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=13233078
dc.identifier.citation	Stratigraphy and Geological Correlation, 1996, , 5, 480-495
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19943
dc.description.abstract	Analysis of the Paleogene planktonic foraminifers from the sections of Kamchatka, Koryak Highland, the North Pacific, and Japan revealed several age levels of the occurrences of warm-water (subtropical) assemblages: late Danian, late Thanetian-early Ypresian, early Lutetian, early Bartonian, and early Priabonian. Appearance of these assemblages at high latitudes can be attributed to climatic warmings that led to their long-distance (up to 2000 or 2500 km) migrations in the northern direction. Some past climatic fluctuations can be correlated with eustatic sea-level oscillations. A high rate of migrations and relatively short duration of warming phases in comparison with cooling phases are recorded.
dc.subject	Paleogene	en
dc.title	PALEOGENE CLIMATIC FLUCTUATIONS AND BIOTIC MIGRATIONS IN THE NORTH PACIFIC
dc.type	Статья
dc.subject.age	Cenozoic::Paleogene	en
dc.subject.age	Кайнозой::Палеоген	ru

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