The first estimation of Fleuve Manche palaeoriver discharge during the last deglaciation: Evidence for Fennoscandian ice sheet meltwater flow in the English Channel ca 20-18 ka ago

The Fleuve Manche (English Channel) palaeoriver represents the largest river system that drained the European continent during Pleistocene lowstands, particularly during the Elsterian (Marine Isotope Stage 12) and Saalian Drenthe (MIS 6) glaciations when extensive ice advances into the North Sea are...

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Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Toucanne, Samuel, Zaragosi, Sebastien, Bourillet, Jean-francois, Marieu, Vincent, Cremer, Michel, Kageyama, Masa, Van Vliet-lanoe, Brigitte, Eynaud, Frederique, Turon, Jean-louis, Gibbard, Philip L.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science Bv 2010
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00002/11310/7858.pdf
https://doi.org/10.1016/j.epsl.2009.12.050
https://archimer.ifremer.fr/doc/00002/11310/