GEOTHERMIC ESTIMATES OF THE AMPLITUDES OF HOLOCENE WARMING IN EUROPE

Demezhko D.Yu.; Utkin V.I.; Ryvkin D.G.; Duchkov A.D.

dc.contributor.author	Demezhko D.Yu.
dc.contributor.author	Utkin V.I.
dc.contributor.author	Ryvkin D.G.
dc.contributor.author	Duchkov A.D.
dc.date.accessioned	2024-11-09T08:38:28Z
dc.date.available	2024-11-09T08:38:28Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13530911
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 259-261
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46470
dc.description.abstract	Periodic alternation of ice ages and warm interglacial periods is a characteristic feature of the Earth’s climatic system in the Quaternary Period. This is testified by the data from oxygen isotopic analysis on deep-sea sediment and ice cores. At the same time, the mechanism of glaciation fluctuations remains unclear in many respects. Indications of the spatial distribution of climate characteristics during the periods of its global changes are needed to understand more clearly the causes of these fluctuations. The last climate change occurred approximately 10 000 yr ago in the beginning of the modern interglacial period (Holocene). In our paper, we analyze the spatial distribution of geothermic estimates of the amplitudes of Holocene warming in Europe.
dc.subject	Holocene
dc.title	GEOTHERMIC ESTIMATES OF THE AMPLITUDES OF HOLOCENE WARMING IN EUROPE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020243
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен