气候变化领域集成服务门户(CCPortal): Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia

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DOI	10.1016/j.earscirev.2019.103069
	Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia
	Panin A.V.; Astakhov V.I.; Lotsari E.; Komatsu G.; Lang J.; Winsemann J.
发表日期	2020
ISSN	0012-8797
卷号	201
英文摘要	The Middle and Late Pleistocene glaciations of northern Eurasia had a great impact on the evolution of the modern drainage system. This paper presents a review and synthesis on the palaeogeography of glacial lakes, their drainage and impact on the re-organization of the drainage systems during the last two glacial-interglacial cycles. We will focus on four regions: (1) northern Central Europe and Fennoscandia, (2) the central part of the East European Plain, (3) the west Siberian Plain and (4) the Aral – Caspian – Black Sea area. The main findings of the last decade(s) include the improved chronology of some major river system formation and of meltwater overflows across the continental drainage divides. Major drainage systems of the north-central and west-central part of the East European Plain (upper Volga, upper Dnieper) formed due to overspill of glacial lakes in late MIS 6 with a partial re-organization (upper Dnieper) in MIS 2. The Aral – Caspian – Black Sea cascade acted as a sink for glacial meltwater from the north. The major meltwater yield to the Aral and Caspian seas occurred in MIS 6 and late MIS 5. In MIS 2, the meltwater delivery via the Volga valley into the Caspian Sea was low and therefore had only a minor influence on the sea level. Considerable meltwater discharge to the Black Sea through the Dnieper River system occurred around the maximal stage of the MIS 2 glaciation and ceased very quickly after the onset of deglaciation. © 2020 Elsevier B.V.
语种	英语
scopus关键词	chronology; drainage; flood; glacial lake; glacial-interglacial cycle; glaciation; marine isotope stage; meltwater; outburst; paleoclimate; Quaternary; river system; Aral Sea; Black Sea; Fennoscandia; Russian Plain
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209726
作者单位	Institute of Geography RAS, Staromonetniy Lane, 29, Moscow, 119017, Russian Federation; Faculty of Geography, Lomonosov Moscow State University, Lengory 1, Moscow, 119991, Russian Federation; Russian Geological Research Institute (VSEGEI), Sredniy Prospect 74, St. Petersburg, 199106, Russian Federation; Institute of Earth Sciences, St. Petersburg University, Universitetskaya Nab. 7/9, St. Petersburg, 199034, Russian Federation; Department of Geographical and Historical Studies, University of Eastern Finland, Joensuu, FI-80101, Finland; Department of Geography and Geology, University of Turku, Turun YliopistoFI-20014, Finland; International Research School of Planetary Sciences, Università d'Annunzio, Pescara, 65127, Italy; Leibniz Universität Hannover, Institut für Geologie, Callinstr. 30, Hannover, D-30167, Germany
推荐引用方式 GB/T 7714	Panin A.V.,Astakhov V.I.,Lotsari E.,et al. Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia[J],2020,201.
APA	Panin A.V.,Astakhov V.I.,Lotsari E.,Komatsu G.,Lang J.,&Winsemann J..(2020).Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia.EARTH-SCIENCE REVIEWS,201.
MLA	Panin A.V.,et al."Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia".EARTH-SCIENCE REVIEWS 201(2020).