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

Autor: Philip L. Gibbard, Vincent Marieu, Frédérique Eynaud, Sébastien Zaragosi, Samuel Toucanne, Jean-Louis Turon, Brigitte Van Vliet-Lanoë, Michel Cremer, Jean-François Bourillet, Masa Kageyama

Publikováno v: Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2010, 290 (3-4), pp.459-473. ⟨10.1016/j.epsl.2009.12.050⟩
Earth and Planetary Science Letters, 2010, 290 (3-4), pp.459-473. ⟨10.1016/j.epsl.2009.12.050⟩
Earth And Planetary Science Letters (0012-821X) (Elsevier Science Bv), 2010-02, Vol. 290, N. 3-4, P. 459-473

International audience; 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 Dren

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0b6bff14c358ec7c4d5d4e965596c4dc
https://hal-insu.archives-ouvertes.fr/insu-00467035