PALYNOLOGICAL CHARACTERISTICS OF THE BOTTOM SEDIMENTS OF THE SOUTHERN BARENTS SEA

dc.contributor.author	Sharapova A.Yu.
dc.date.accessioned	2025-05-10T04:38:22Z
dc.date.available	2025-05-10T04:38:22Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=13506842
dc.identifier.citation	Paleontological Journal, 2006, 40, Suppl. 5,
dc.identifier.issn	0031-0301
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/49207
dc.description.abstract	The distribution of spores and pollen grains was studied in nine sections of bottom sediments up to 50 m thick, in the southern Barents Sea. The Early Cretaceous, Pleistocene, and Holocene ages of the enclosing sediments are determined by palynological analysis. Three Holocene provinces were recognized and traced along the beds, which were formed in the Early, Middle, and Late Holocene according to the scheme of Neishtadt (1957). © Pleiades Publishing, Inc. 2006.
dc.subject	BARENTS SEA
dc.subject	HOLOCENE
dc.subject	PALYNOLOGICAL ANALYSIS
dc.title	PALYNOLOGICAL CHARACTERISTICS OF THE BOTTOM SEDIMENTS OF THE SOUTHERN BARENTS SEA
dc.type	Статья
dc.identifier.doi	10.1134/S0031030106110141
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен

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