Université Paris-Saclay, Géosciences Paris Sud, UMR 8148,
CNRS, Rue du Belvédère, 91405 Orsay, France
Stéphanie Duchamp-Alphonse
Université Paris-Saclay, Géosciences Paris Sud, UMR 8148,
CNRS, Rue du Belvédère, 91405 Orsay, France
Masa Kageyama
Laboratoire des Sciences du Climat et de l'Environnement, UMR 8112,
CEA/CNRS/UVSQ, Université Paris-Saclay, Centre CEA-Saclay, Orme des Merisiers, 91191 Gif-sur-Yvette, France
Franck Bassinot
Laboratoire des Sciences du Climat et de l'Environnement, UMR 8112,
CEA/CNRS/UVSQ, Université Paris-Saclay, Centre CEA-Saclay, Orme des Merisiers, 91191 Gif-sur-Yvette, France
Centre de Recherche et d'Enseignement de Géosciences de
l'Environnement, UMR 7330, CNRS/IRD/Aix-Marseille Université, Av. Louis
Philibert, BP80, 13545 Aix-en-Provence, France
Christophe Colin
Université Paris-Saclay, Géosciences Paris Sud, UMR 8148,
CNRS, Rue du Belvédère, 91405 Orsay, France
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1,938
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Total article views: 3,820 (including HTML, PDF, and XML)
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Total article views: 2,904 (including HTML, PDF, and XML)
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We provide a high-resolution primary productivity (PP) record of the northeastern Bay of Bengal over the last 26 000 years. Combined with climate model outputs, we show that PP over the glacial period is controlled by river input nutrients under low sea level conditions and after the Last Glacial Maximum is controlled by upper seawater salinity stratification related to monsoon precipitation. During the deglaciation the Atlantic meridional overturning circulation is the main forcing factor.
We provide a high-resolution primary productivity (PP) record of the northeastern Bay of Bengal...
