Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals

International audience Variations of the Sub-Polar Gyre (SPG) and the Sub-Tropical Gyre (STG) circulation during the Holocene are believed to be related to regional and global climate over this time period. To improve our understanding of these phenomena we provide new constraints on variations in s...

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Published in:Marine Geology
Main Authors: Dubois-Dauphin, Quentin, Colin, Christophe, Elliot, Mary, Dapoigny, Arnaud, Douville, Eric
Other Authors: Géosciences Paris Sud (GEOPS), Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), 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), Géochrononologie Traceurs Archéométrie (GEOTRAC), 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)), ANR-17-EURE-0006,IPSL-CGS,IPSL Climate graduate school(2017), ANR-10-LABX-0018,L-IPSL,LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes(2010)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
Online Access:https://hal.science/hal-02149410
https://hal.science/hal-02149410/document
https://hal.science/hal-02149410/file/1-s2.0-S0025322718302810-am.pdf
https://doi.org/10.1016/j.margeo.2019.01.004
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institution Open Polar
collection Portail HAL-ANR (Agence Nationale de la Recherche)
op_collection_id ftanrparis
language English
topic Panoply
[SDU]Sciences of the Universe [physics]
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle Panoply
[SDU]Sciences of the Universe [physics]
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Dubois-Dauphin, Quentin
Colin, Christophe
Elliot, Mary
Dapoigny, Arnaud
Douville, Eric
Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals
topic_facet Panoply
[SDU]Sciences of the Universe [physics]
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience Variations of the Sub-Polar Gyre (SPG) and the Sub-Tropical Gyre (STG) circulation during the Holocene are believed to be related to regional and global climate over this time period. To improve our understanding of these phenomena we provide new constraints on variations in surface circulation patterns using neodymium isotopes (εNd) on precisely U-Th dated coral fragments of L. pertusa. The fragments were retrieved from two sediment cores taken from cold-water coral (CWC) mounds at ~ 127–134 m water depth in the Mingulay Reef Complex located on the Western British continental shelf. The results have been combined with εNd analyzed on seawater samples from two stations located on the continental shelf and margin in order to establish whether εNd is a reliable proxy of the ocean circulation variations and notably of the relative contribution of water originating from the SPG and STG. εNd values in CWCs from the Mingulay Reef Complex range from −14.5 ± 0.4 to −11.8 ± 0.3, highlighting two major variations. Unradiogenic εNd values (−14.5 ± 0.4) indicate a higher contribution of water from the SPG around 2.8 ka. Conversely, more radiogenic values at 3.4 ka (−11.8 ± 0.3) point to a declining SPG strength, accompanied by stronger northward penetration of STG water along the western European margin transported by the Shelf Edge Current (SEC) and/or cooler and fresher waters from the interior Seas. The eastward extension of the SPG at 2.8 ka is associated with lower 14C reservoir age (200 yrs) compared to periods associated with a higher contribution of STG waters. This indicates that 14C reservoir ages are mainly a function of vertical mixing of the sub-surface of the ocean. As stronger vertical ventilation is not associated with a higher proportion of local radiogenic surface water, we hypothesize it could represent vertical ventilation in the North-Eastern Atlantic. Active SPG is associated with a better ventilation of the water masses within the SPG and warmer climatic conditions in Northern ...
author2 Géosciences Paris Sud (GEOPS)
Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG)
Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST)
Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
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)
Géochrononologie Traceurs Archéométrie (GEOTRAC)
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))
ANR-17-EURE-0006,IPSL-CGS,IPSL Climate graduate school(2017)
ANR-10-LABX-0018,L-IPSL,LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes(2010)
format Article in Journal/Newspaper
author Dubois-Dauphin, Quentin
Colin, Christophe
Elliot, Mary
Dapoigny, Arnaud
Douville, Eric
author_facet Dubois-Dauphin, Quentin
Colin, Christophe
Elliot, Mary
Dapoigny, Arnaud
Douville, Eric
author_sort Dubois-Dauphin, Quentin
title Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals
title_short Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals
title_full Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals
title_fullStr Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals
title_full_unstemmed Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals
title_sort holocene shifts in sub-surface water circulation of the north-east atlantic inferred from nd isotopic composition in cold-water corals
publisher HAL CCSD
publishDate 2019
url https://hal.science/hal-02149410
https://hal.science/hal-02149410/document
https://hal.science/hal-02149410/file/1-s2.0-S0025322718302810-am.pdf
https://doi.org/10.1016/j.margeo.2019.01.004
genre North East Atlantic
genre_facet North East Atlantic
op_source ISSN: 0025-3227
Marine Geology
https://hal.science/hal-02149410
Marine Geology, 2019, 410, pp.135-145. ⟨10.1016/j.margeo.2019.01.004⟩
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doi:10.1016/j.margeo.2019.01.004
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1016/j.margeo.2019.01.004
container_title Marine Geology
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spelling ftanrparis:oai:HAL:hal-02149410v1 2024-09-09T19:58:33+00:00 Holocene shifts in sub-surface water circulation of the North-East Atlantic inferred from Nd isotopic composition in cold-water corals Dubois-Dauphin, Quentin Colin, Christophe Elliot, Mary Dapoigny, Arnaud Douville, Eric Géosciences Paris Sud (GEOPS) Université Paris-Sud - Paris 11 (UP11)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG) Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST) Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 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) Géochrononologie Traceurs Archéométrie (GEOTRAC) 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)) ANR-17-EURE-0006,IPSL-CGS,IPSL Climate graduate school(2017) ANR-10-LABX-0018,L-IPSL,LabEx Institut Pierre Simon Laplace (IPSL): Understand climate and anticipate future changes(2010) 2019-04 https://hal.science/hal-02149410 https://hal.science/hal-02149410/document https://hal.science/hal-02149410/file/1-s2.0-S0025322718302810-am.pdf https://doi.org/10.1016/j.margeo.2019.01.004 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.margeo.2019.01.004 hal-02149410 https://hal.science/hal-02149410 https://hal.science/hal-02149410/document https://hal.science/hal-02149410/file/1-s2.0-S0025322718302810-am.pdf doi:10.1016/j.margeo.2019.01.004 info:eu-repo/semantics/OpenAccess ISSN: 0025-3227 Marine Geology https://hal.science/hal-02149410 Marine Geology, 2019, 410, pp.135-145. ⟨10.1016/j.margeo.2019.01.004⟩ Panoply [SDU]Sciences of the Universe [physics] [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2019 ftanrparis https://doi.org/10.1016/j.margeo.2019.01.004 2024-07-12T11:07:27Z International audience Variations of the Sub-Polar Gyre (SPG) and the Sub-Tropical Gyre (STG) circulation during the Holocene are believed to be related to regional and global climate over this time period. To improve our understanding of these phenomena we provide new constraints on variations in surface circulation patterns using neodymium isotopes (εNd) on precisely U-Th dated coral fragments of L. pertusa. The fragments were retrieved from two sediment cores taken from cold-water coral (CWC) mounds at ~ 127–134 m water depth in the Mingulay Reef Complex located on the Western British continental shelf. The results have been combined with εNd analyzed on seawater samples from two stations located on the continental shelf and margin in order to establish whether εNd is a reliable proxy of the ocean circulation variations and notably of the relative contribution of water originating from the SPG and STG. εNd values in CWCs from the Mingulay Reef Complex range from −14.5 ± 0.4 to −11.8 ± 0.3, highlighting two major variations. Unradiogenic εNd values (−14.5 ± 0.4) indicate a higher contribution of water from the SPG around 2.8 ka. Conversely, more radiogenic values at 3.4 ka (−11.8 ± 0.3) point to a declining SPG strength, accompanied by stronger northward penetration of STG water along the western European margin transported by the Shelf Edge Current (SEC) and/or cooler and fresher waters from the interior Seas. The eastward extension of the SPG at 2.8 ka is associated with lower 14C reservoir age (200 yrs) compared to periods associated with a higher contribution of STG waters. This indicates that 14C reservoir ages are mainly a function of vertical mixing of the sub-surface of the ocean. As stronger vertical ventilation is not associated with a higher proportion of local radiogenic surface water, we hypothesize it could represent vertical ventilation in the North-Eastern Atlantic. Active SPG is associated with a better ventilation of the water masses within the SPG and warmer climatic conditions in Northern ... Article in Journal/Newspaper North East Atlantic Portail HAL-ANR (Agence Nationale de la Recherche) Marine Geology 410 135 145