OLIGOCENE CALCAREOUS PLANKTON FROM THE KRONOTSKII PENINSULA, EASTERN KAMCHATKA

dc.contributor.author	Stupin S.I.
dc.contributor.author	Shcherbinina E.A.
dc.contributor.author	Vitukhin D.I.
dc.contributor.author	Serova M.Ya.
dc.contributor.author	Tsukanov N.V.
dc.contributor.author	Pachkalov A.S.
dc.date.accessioned	2020-12-31T03:44:30Z
dc.date.available	2020-12-31T03:44:30Z
dc.date.issued	1998
dc.identifier	https://elibrary.ru/item.asp?id=13297624
dc.identifier.citation	Stratigraphy and Geological Correlation, 1998, , 5, 509-519
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21844
dc.description.abstract	Planktonic foraminifers and calcareous nannoplankton were first recorded along with benthic foraminifers in the Upper Paleogene section of the Kronotskii Peninsula, eastern Kamchatka. The fauna permits the assignment of the enclosing sediments to the Globigerina ampliapertura Zone of the foraminifer zonation of Bolli and Saunders, (1985) and to the nannoplankton zones CP17-CP18 of the Lower Oligocene. The sporadic occurrence of calcareous plankton in Oligocene sediments of high latitudes was most likely a consequence of the World Ocean level rise and relative climatic warming.
dc.subject	Oligocene	en
dc.title	OLIGOCENE CALCAREOUS PLANKTON FROM THE KRONOTSKII PENINSULA, EASTERN KAMCHATKA
dc.type	Статья
dc.subject.age	Cenozoic::Paleogene::Oligocene	en
dc.subject.age	Кайнозой::Палеоген::Олигоцен	ru

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