A RECONSTRUCTION OF THE CLIMATE AND VEGETATION OF NORTHEASTERN SIBERIA BASED ON LAKE SEDIMENTS

dc.contributor.author	Lozhkin A.V.
dc.contributor.author	Anderson P.A.
dc.date.accessioned	2025-05-19T06:45:56Z
dc.date.available	2025-05-19T06:45:56Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=13514100
dc.identifier.citation	Paleontological Journal, 2006, 40, Suppl. 5, S622-S628
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/49252
dc.description.abstract	Detailed palynological analysis of glacial, tectonic, and crater lakes of northeastern Siberia reveals continuous records of the changing vegetation during one or several climatic cycles of the Pleistocene and in the Holocene. The most continuous records in the mountain areas of the region are those of Lake Elikchan-4 (northern Okhotsk Sea Region). Pollen records of Lake El’gygytgyn, which was formed by the impact of a meteorite in the northern Chukchi Peninsula, reflect the response of land vegetation to the global climatic impact during the last 300 ka.
dc.title	A RECONSTRUCTION OF THE CLIMATE AND VEGETATION OF NORTHEASTERN SIBERIA BASED ON LAKE SEDIMENTS
dc.type	Статья
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен
dc.subject.age	Cenozoic::Quaternary::Pleistocene
dc.subject.age	Кайнозой::Четвертичная::Плейстоцен

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