MAGNETOCHRONOLOGY OF THE CLIMATIC OPTIMUM AT THE EARLY-MIDDLE MIOCENE TRANSITION IN NORTHEAST RUSSIA

dc.contributor.author	Shilo N.A.
dc.contributor.author	Minyuk P.S.
dc.date.accessioned	2024-11-02T11:08:00Z
dc.date.available	2024-11-02T11:08:00Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524337
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1014-1016
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46391
dc.description.abstract	The Miocene was characterized by sharp climatic fluctuations. Among them, the most significant (for high latitudes) fluctuations are termed climatic optimums I, II, and III. Optimum I, which marks the Early–Middle Miocene transition, has been comprehensively studied within and beyond Northeast Russia. In the Russian literature, Optimum I is known as the “beech” horizon first defined by Kartashova based on palynological data. This horizon, a reliable reference unit for the Miocene, is recognized in almost all regions of Northeast Russia with Lower–Middle Miocene sediments.
dc.subject	Miocene
dc.title	MAGNETOCHRONOLOGY OF THE CLIMATIC OPTIMUM AT THE EARLY-MIDDLE MIOCENE TRANSITION IN NORTHEAST RUSSIA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070026
dc.subject.age	Cenozoic::Neogene::Miocene
dc.subject.age	Кайнозой::Неоген::Миоцен

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