The Global Last Glacial Maximum: the Eastern North Atlantic (marine sediments) and the Greenland Ice Sheet climatic signal

This chapter summarises the environmental changes that accompanied the rapid growth of the Northern Hemisphere ice sheets c. 35–30 cal ka BP and their maximum extent c. 29–19 cal ka BP, with a special focus on the European continent and its surrounding margins.

Bibliographic Details
Main Authors: Toucanne, Samuel, Landais, Amaelle, Naughton, Filipa, Rodrigues, Teresa, Vazquez Riveiros, Natalia, Sanchez Goni, Maria Fernanda
Other Authors: Geo-Ocean (GEO-OCEAN), Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Format: Book Part
Language:English
Published: HAL CCSD 2022
Subjects:
[SDU]Sciences of the Universe [physics]
Greenland
Ice Sheet
North Atlantic
Online Access:https://hal.science/hal-04309674
https://doi.org/10.1016/B978-0-12-823498-3.00052-2
Description
Summary:This chapter summarises the environmental changes that accompanied the rapid growth of the Northern Hemisphere ice sheets c. 35–30 cal ka BP and their maximum extent c. 29–19 cal ka BP, with a special focus on the European continent and its surrounding margins.

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