Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)

International audience At the peak of the previous interglacial period, North Atlantic and subpolar climate shared many features in common with projections of our future climate, including warmer‐than‐present conditions and a diminished Greenland Ice Sheet (GIS). Here we portray changes in North Atl...

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Bibliographic Details
Published in:Paleoceanography
Main Authors: Irvali, Nil, Ninnemann, Ulysses, Galaasen, Eirik, Rosenthal, Yair, Kroon, Dick, Oppo, Delia, Kleiven, Helga, Darling, Kate, Kissel, Catherine
Other Authors: Bjerknes Centre for Climate Research (BCCR), Department of Biological Sciences Bergen (BIO / UiB), University of Bergen (UiB)-University of Bergen (UiB), Rutgers, The State University of New Jersey New Brunswick (RU), Rutgers University System (Rutgers), School of Geosciences Edinburgh, University of Edinburgh (Edin.), Woods Hole Oceanographic Institution (WHOI), Climat et Magnétisme (CLIMAG), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2012
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Online Access:https://hal.science/hal-03118211
https://hal.science/hal-03118211/document
https://hal.science/hal-03118211/file/2011PA002244.pdf
https://doi.org/10.1029/2011PA002244
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Summary:International audience At the peak of the previous interglacial period, North Atlantic and subpolar climate shared many features in common with projections of our future climate, including warmer‐than‐present conditions and a diminished Greenland Ice Sheet (GIS). Here we portray changes in North Atlantic hydrography linked with Greenland climate during Marine Isotope Stage (MIS) 5e using (sub)centennially sampled records of planktonic foraminiferal isotopes and assemblage counts and ice‐rafted debris counts, as well as modern analog technique and Mg/Ca‐based paleothermometry. We use the core MD03‐2664 recovered from a high accumulation rate site (∼34 cm/kyr) on the Eirik sediment drift (57°26.34′N, 48°36.35′W). The results indicate that surface waters off southern Greenland were ∼3–5°C warmer than today during early MIS 5e. These anomalously warm sea surface temperatures (SSTs) prevailed until the isotopic peak of MIS 5e when they were interrupted by a cooling event beginning at ∼126 kyr BP. This interglacial cooling event is followed by a gradual warming with SSTs subsequently plateauing just below early MIS 5e values. A planktonic δ18O minimum during the cooling event indicates that marked freshening of the surface waters accompanied the cooling. We suggest that switches in the subpolar gyre hydrography occurred during a warmer climate, involving regional changes in freshwater fluxes/balance and East Greenland Current influence in the study area. The nature of these hydrographic transitions suggests that they are most likely related to large‐scale circulation dynamics, potentially amplified by GIS meltwater influences.