Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera
International audience The Mediterranean Sea is a semi-enclosed basin characterized by arid conditions and connected to the North Atlantic through the Strait of Gibraltar (sill depth of ∼300 m). This generates a Mediterranean thermohaline circulation where the inflow of relatively fresh and cold sur...
Published in: | Paleoceanography and Paleoclimatology |
---|---|
Main Authors: | , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2021
|
Subjects: | |
Online Access: | https://hal.science/hal-03227533 https://hal.science/hal-03227533/document https://hal.science/hal-03227533/file/Colin%20et%20al%202021.pdf https://doi.org/10.1029/2020pa004153 |
id |
ftecolephe:oai:HAL:hal-03227533v1 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
EPHE (Ecole pratique des hautes études, Paris): HAL |
op_collection_id |
ftecolephe |
language |
English |
topic |
PANOPLY [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
PANOPLY [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Colin, Christophe Duhamel, Maxence Siani, Giuseppe Dubois‐dauphin, Quentin Ducassou, Emmanuelle Liu, Zhifei Wu, Jiawang Revel, Marie Dapoigny, Arnaud Douville, Éric Taviani, Marco Montagna, Paolo Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera |
topic_facet |
PANOPLY [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 The Mediterranean Sea is a semi-enclosed basin characterized by arid conditions and connected to the North Atlantic through the Strait of Gibraltar (sill depth of ∼300 m). This generates a Mediterranean thermohaline circulation where the inflow of relatively fresh and cold surface Atlantic water (AW) is transformed into intermediate and deep waters in the Gulf of Lions, the Adriatic Sea, the Levantine Basin and the Aegean Sea (Robinson et al., 2001; Schroeder et al., 2012). In particular, the Levantine Intermediate Water (LIW) is formed in the Cyprus-Rhodes area from where it spreads westwards into the entire Mediterranean Sea at water depths of between ∼150 and 700 m (Lascaratos et al., 1993; Malanotte-Rizzoli et al., 1999). This overturning circulation is associated with an outflow of saltier and warmer intermediate water into the North Atlantic corresponding to the Mediterranean Outflow Water (MOW) (Robinson et al., 2001; Schroeder et al., 2012). Because the MOW contains up to ∼80% of LIW, the water mass formation in the Levantine Sea plays an important role for the salty outflow to the North Atlantic through the Strait of Gibraltar. A link between the intensification of the MOW and the intensity of the Atlantic Meridional Overturning Circulation (AMOC) has been proposed ( |
author2 |
Géosciences Paris Saclay (GEOPS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Tongji University Géoazur (GEOAZUR 7329) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur Université Côte d'Azur (UniCA)-Université Côte d'Azur (UniCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD France-Sud ) 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)) Istituto di Science Marine (ISMAR ) National Research Council of Italy Stazione Zoologica Anton Dohrn (SZN) Woods Hole Oceanographic Institution (WHOI) Institute of Polar Sciences Venezia-Mestre (CNR-ISP) Lamont-Doherty Earth Observatory (LDEO) Columbia University New York ANR-19-CE01-0019,MEDSENS,Sensibilité de la circulation thermohaline en Mer Méditerranée : leçons du passé pour le futur(2019) |
format |
Article in Journal/Newspaper |
author |
Colin, Christophe Duhamel, Maxence Siani, Giuseppe Dubois‐dauphin, Quentin Ducassou, Emmanuelle Liu, Zhifei Wu, Jiawang Revel, Marie Dapoigny, Arnaud Douville, Éric Taviani, Marco Montagna, Paolo |
author_facet |
Colin, Christophe Duhamel, Maxence Siani, Giuseppe Dubois‐dauphin, Quentin Ducassou, Emmanuelle Liu, Zhifei Wu, Jiawang Revel, Marie Dapoigny, Arnaud Douville, Éric Taviani, Marco Montagna, Paolo |
author_sort |
Colin, Christophe |
title |
Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera |
title_short |
Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera |
title_full |
Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera |
title_fullStr |
Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera |
title_full_unstemmed |
Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera |
title_sort |
changes in the intermediate water masses of the mediterranean sea during the last climatic cycle—new constraints from neodymium isotopes in foraminifera |
publisher |
HAL CCSD |
publishDate |
2021 |
url |
https://hal.science/hal-03227533 https://hal.science/hal-03227533/document https://hal.science/hal-03227533/file/Colin%20et%20al%202021.pdf https://doi.org/10.1029/2020pa004153 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
ISSN: 2572-4525 EISSN: 1944-9186 Paleoceanography and Paleoclimatology https://hal.science/hal-03227533 Paleoceanography and Paleoclimatology, 2021, 36 (4), pp.e2020PA004153. ⟨10.1029/2020pa004153⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2020pa004153 hal-03227533 https://hal.science/hal-03227533 https://hal.science/hal-03227533/document https://hal.science/hal-03227533/file/Colin%20et%20al%202021.pdf doi:10.1029/2020pa004153 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2020pa004153 |
container_title |
Paleoceanography and Paleoclimatology |
container_volume |
36 |
container_issue |
4 |
_version_ |
1801379626191159296 |
spelling |
ftecolephe:oai:HAL:hal-03227533v1 2024-06-09T07:48:04+00:00 Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera Colin, Christophe Duhamel, Maxence Siani, Giuseppe Dubois‐dauphin, Quentin Ducassou, Emmanuelle Liu, Zhifei Wu, Jiawang Revel, Marie Dapoigny, Arnaud Douville, Éric Taviani, Marco Montagna, Paolo Géosciences Paris Saclay (GEOPS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Tongji University Géoazur (GEOAZUR 7329) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur Université Côte d'Azur (UniCA)-Université Côte d'Azur (UniCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD France-Sud ) 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)) Istituto di Science Marine (ISMAR ) National Research Council of Italy Stazione Zoologica Anton Dohrn (SZN) Woods Hole Oceanographic Institution (WHOI) Institute of Polar Sciences Venezia-Mestre (CNR-ISP) Lamont-Doherty Earth Observatory (LDEO) Columbia University New York ANR-19-CE01-0019,MEDSENS,Sensibilité de la circulation thermohaline en Mer Méditerranée : leçons du passé pour le futur(2019) 2021 https://hal.science/hal-03227533 https://hal.science/hal-03227533/document https://hal.science/hal-03227533/file/Colin%20et%20al%202021.pdf https://doi.org/10.1029/2020pa004153 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2020pa004153 hal-03227533 https://hal.science/hal-03227533 https://hal.science/hal-03227533/document https://hal.science/hal-03227533/file/Colin%20et%20al%202021.pdf doi:10.1029/2020pa004153 info:eu-repo/semantics/OpenAccess ISSN: 2572-4525 EISSN: 1944-9186 Paleoceanography and Paleoclimatology https://hal.science/hal-03227533 Paleoceanography and Paleoclimatology, 2021, 36 (4), pp.e2020PA004153. ⟨10.1029/2020pa004153⟩ PANOPLY [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 2021 ftecolephe https://doi.org/10.1029/2020pa004153 2024-05-16T10:56:29Z International audience The Mediterranean Sea is a semi-enclosed basin characterized by arid conditions and connected to the North Atlantic through the Strait of Gibraltar (sill depth of ∼300 m). This generates a Mediterranean thermohaline circulation where the inflow of relatively fresh and cold surface Atlantic water (AW) is transformed into intermediate and deep waters in the Gulf of Lions, the Adriatic Sea, the Levantine Basin and the Aegean Sea (Robinson et al., 2001; Schroeder et al., 2012). In particular, the Levantine Intermediate Water (LIW) is formed in the Cyprus-Rhodes area from where it spreads westwards into the entire Mediterranean Sea at water depths of between ∼150 and 700 m (Lascaratos et al., 1993; Malanotte-Rizzoli et al., 1999). This overturning circulation is associated with an outflow of saltier and warmer intermediate water into the North Atlantic corresponding to the Mediterranean Outflow Water (MOW) (Robinson et al., 2001; Schroeder et al., 2012). Because the MOW contains up to ∼80% of LIW, the water mass formation in the Levantine Sea plays an important role for the salty outflow to the North Atlantic through the Strait of Gibraltar. A link between the intensification of the MOW and the intensity of the Atlantic Meridional Overturning Circulation (AMOC) has been proposed ( Article in Journal/Newspaper North Atlantic EPHE (Ecole pratique des hautes études, Paris): HAL Paleoceanography and Paleoclimatology 36 4 |