Earth-Science Reviews, volume 201, pages 103069
Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia
Panin A. V.
1
,
Astakhov Valery
2
,
Lotsari Eliisa S.
3, 4
,
Komatsu Goro
5
,
Lang Jörg
6
,
Winsemann Jutta
6
5
International Research School of Planetary Sciences, Università d'Annunzio, Pescara 65127, Italy.
|
6
Leibniz Universität Hannover, Institut für Geologie, Callinstr. 30, D-30167 Hannover, Germany
|
Publication type: Journal Article
Publication date: 2020-02-01
Journal:
Earth-Science Reviews
Quartile SCImago
Q1
Quartile WOS
Q1
Impact factor: 12.1
ISSN: 00128252
General Earth and Planetary Sciences
Abstract
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.
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1
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Citations by publishers
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2
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1 publication, 2.78%
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Finnish Zoological and Botanical Publishing Board, 1, 2.78%
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1 publication, 2.78%
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1 publication, 2.78%
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1 publication, 2.78%
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Copernicus
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1 publication, 2.78%
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Springer Nature
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Springer Nature
1 publication, 2.78%
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2
4
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14
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- We do not take into account publications that without a DOI.
- Statistics recalculated only for publications connected to researchers, organizations and labs registered on the platform.
- Statistics recalculated weekly.
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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. 2020. Vol. 201. p. 103069.
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Panin A. V., Astakhov V., Lotsari E. S., Komatsu G., Lang J., Winsemann J. Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia // Earth-Science Reviews. 2020. Vol. 201. p. 103069.
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TY - JOUR
DO - 10.1016/j.earscirev.2019.103069
UR - https://doi.org/10.1016%2Fj.earscirev.2019.103069
TI - Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia
T2 - Earth-Science Reviews
AU - Panin, A. V.
AU - Astakhov, Valery
AU - Lotsari, Eliisa S.
AU - Komatsu, Goro
AU - Lang, Jörg
AU - Winsemann, Jutta
PY - 2020
DA - 2020/02/01 00:00:00
PB - Elsevier
SP - 103069
VL - 201
SN - 0012-8252
ER -
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@article{2020_Panin,
author = {A. V. Panin and Valery Astakhov and Eliisa S. Lotsari and Goro Komatsu and Jörg Lang and Jutta Winsemann},
title = {Middle and Late Quaternary glacial lake-outburst floods, drainage diversions and reorganization of fluvial systems in northwestern Eurasia},
journal = {Earth-Science Reviews},
year = {2020},
volume = {201},
publisher = {Elsevier},
month = {feb},
url = {https://doi.org/10.1016%2Fj.earscirev.2019.103069},
pages = {103069},
doi = {10.1016/j.earscirev.2019.103069}
}
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