PLIOCENE-PLEISTOCENE DIATOMS AND ENVIRONMENTS IN THE NORTHERN TARTAR STRAIT

dc.contributor.author	Oreshkina T.V.
dc.date.accessioned	2020-12-01T08:34:50Z
dc.date.available	2020-12-01T08:34:50Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=13244527
dc.identifier.citation	Stratigraphy and Geological Correlation, 1996, , 3, 287-293
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19979
dc.description.abstract	Diatoms from a 34-m-thick member of Pliocene-Pleistocene sediments in the near-continental part of the Tartar Strait were studied. The beginning of the Pliocene was characterized by marine neritic environments indicating the stable influence of the Sea of Okhotsk waters. Warm-water environments were characteristic of the interval of 4.4-3.2 Ma, which is evidenced by subtropical diatom species. Their presence evidently reflects the periodically strong influence of warm Pacific waters and a weakening connection with the Sea of Okhotsk. The role of tectonics and climatic fluctuations was also considered.
dc.subject	Pliocene	en
dc.subject	Pleistocene	en
dc.title	PLIOCENE-PLEISTOCENE DIATOMS AND ENVIRONMENTS IN THE NORTHERN TARTAR STRAIT
dc.type	Статья
dc.subject.age	Cenozoic::Neogene::Pliocene	en
dc.subject.age	Кайнозой::Четвертичная::Плейстоцен	ru
dc.subject.age	Cenozoic::Quaternary::Pleistocene	en
dc.subject.age	Кайнозой::Неоген::Плиоцен	ru

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