globalchange  > 过去全球变化的重建
DOI: 10.1134/S086959381904004X
WOS记录号: WOS:000482239600005
论文题名:
Changes in the Landscape and Climate of Eastern Europe in the Early Pleistocene
作者: Pisareva, V. V.1; Faustova, M. A.1; Zyuganova, I. S.1; Karpukhina, N. V.1; Zakharov, A. L.1; Konstantinov, E. A.1; Semenov, V. V.1; Kurbanov, R. N.1,2
通讯作者: Pisareva, V. V.
刊名: STRATIGRAPHY AND GEOLOGICAL CORRELATION
ISSN: 0869-5938
EISSN: 1555-6263
出版年: 2019
卷: 27, 期:4, 页码:475-497
语种: 英语
英文关键词: East European Plain ; lower boundary of the Quaternary ; Paleopleistocene ; Eopleistocene ; Early Neopleistocene ; glaciation ; interglacial period ; interstadial ; till ; soil ; loess ; fossil flora and fauna ; correlation
WOS关键词: FLORA
WOS学科分类: Geology ; Paleontology
WOS研究方向: Geology ; Paleontology
英文摘要:

In the context of shifting the boundary of the Quaternary down to the level of 2.6 Ma and including the Gelasian Stage in the Quaternary System, the systematization of the original and published data on the geology and paleogeography of the Late Pliocene and Early Pleistocene of Eastern Europe has been carried out. It was established that, at the boundary of the Gauss and Matuyama paleomagnetic epochs, along with the general trend toward cooling and aridization, profound landscape and climate changes occurred and rhythmic fluctuations of the climate intensified. During the period from 2.6 to 1.8 Ma, corresponding to the Gelasian (pre-Tiglian and Tiglian of Western Europe or Paleopleistocene of Eastern Europe), there appeared subarctic landscapes. In the Eopleistocene (1.8-0.78 Ma) and the Early Neopleistocene (0.78-0.42 Ma), the climate became colder, and climatic zonality repeatedly underwent a complex restructuring, gradually approaching the modern one. Glacial deposits (layers of till) occurring in Eastern Europe date back to the Paleopleistocene. Evidence indicates that there were at least three independent glaciations in the Eopleistocene (1.8-0.78 Ma) and possibly four in the Early Neopleistocene. On the basis of studies of stratotypic sections, paragenetic links were established between sediments of different age within glacial and periglacial areas, and the paleogeographic events of the Early Pleistocene of Eastern Europe were correlated with those within the Western European region.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/140986
Appears in Collections:过去全球变化的重建

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作者单位: 1.Russian Acad Sci, Inst Geog, Moscow, Russia
2.Moscow MV Lomonosov State Univ, Moscow, Russia

Recommended Citation:
Pisareva, V. V.,Faustova, M. A.,Zyuganova, I. S.,et al. Changes in the Landscape and Climate of Eastern Europe in the Early Pleistocene[J]. STRATIGRAPHY AND GEOLOGICAL CORRELATION,2019-01-01,27(4):475-497
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