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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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
Subjects:
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
id ftceafr:oai:HAL:hal-03118211v1
record_format openpolar
institution Open Polar
collection HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives)
op_collection_id ftceafr
language English
topic [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Irvali, Nil
Ninnemann, Ulysses
Galaasen, Eirik
Rosenthal, Yair
Kroon, Dick
Oppo, Delia
Kleiven, Helga
Darling, Kate
Kissel, Catherine
Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)
topic_facet [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description 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.
author2 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
author Irvali, Nil
Ninnemann, Ulysses
Galaasen, Eirik
Rosenthal, Yair
Kroon, Dick
Oppo, Delia
Kleiven, Helga
Darling, Kate
Kissel, Catherine
author_facet Irvali, Nil
Ninnemann, Ulysses
Galaasen, Eirik
Rosenthal, Yair
Kroon, Dick
Oppo, Delia
Kleiven, Helga
Darling, Kate
Kissel, Catherine
author_sort Irvali, Nil
title Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)
title_short Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)
title_full Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)
title_fullStr Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)
title_full_unstemmed Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)
title_sort rapid switches in subpolar north atlantic hydrography and climate during the last interglacial (mis 5e)
publisher HAL CCSD
publishDate 2012
url 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
geographic Greenland
geographic_facet Greenland
genre East Greenland
east greenland current
Greenland
Ice Sheet
North Atlantic
genre_facet East Greenland
east greenland current
Greenland
Ice Sheet
North Atlantic
op_source ISSN: 0883-8305
Paleoceanography
https://hal.science/hal-03118211
Paleoceanography, 2012, 27 (2), pp.PA2207. ⟨10.1029/2011PA002244⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2011PA002244
hal-03118211
https://hal.science/hal-03118211
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op_rights info:eu-repo/semantics/OpenAccess
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container_title Paleoceanography
container_volume 27
container_issue 2
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spelling ftceafr:oai:HAL:hal-03118211v1 2024-06-09T07:45:40+00:00 Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e) Irvali, Nil Ninnemann, Ulysses Galaasen, Eirik Rosenthal, Yair Kroon, Dick Oppo, Delia Kleiven, Helga Darling, Kate Kissel, Catherine 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) 2012 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 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2011PA002244 hal-03118211 https://hal.science/hal-03118211 https://hal.science/hal-03118211/document https://hal.science/hal-03118211/file/2011PA002244.pdf doi:10.1029/2011PA002244 info:eu-repo/semantics/OpenAccess ISSN: 0883-8305 Paleoceanography https://hal.science/hal-03118211 Paleoceanography, 2012, 27 (2), pp.PA2207. ⟨10.1029/2011PA002244⟩ [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2012 ftceafr https://doi.org/10.1029/2011PA002244 2024-05-16T14:35:30Z 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. Article in Journal/Newspaper East Greenland east greenland current Greenland Ice Sheet North Atlantic HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Greenland Paleoceanography 27 2 n/a n/a