Paleoceanography of the Barents Sea during the Holocene
International audience [1] We measured the oxygen isotopic composition of planktonic and benthic foraminifera in three cores collected at key positions to reconstruct the paleoceanography of the Barents Sea: core ASV 880 on the path of the northern branch of Atlantic water inflowing from the Arctic...
Published in: | Paleoceanography |
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Format: | Article in Journal/Newspaper |
Language: | English |
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2005
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Online Access: | https://hal.archives-ouvertes.fr/hal-02498084 https://hal.archives-ouvertes.fr/hal-02498084/document https://hal.archives-ouvertes.fr/hal-02498084/file/2004PA001116.pdf https://doi.org/10.1029/2004PA001116 |
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ftccsdartic:oai:HAL:hal-02498084v1 2023-05-15T15:09:56+02:00 Paleoceanography of the Barents Sea during the Holocene Duplessy, J.C. Cortijo, E. Ivanova, E., Khusid, T. Labeyrie, L. Levitan, M. Murdmaa, I. Paterne, M. Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Paléocéanographie (PALEOCEAN) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) St. Petersburg State Polytechnical University Géochrononologie Traceurs Archéométrie (GEOTRAC) 2005-12 https://hal.archives-ouvertes.fr/hal-02498084 https://hal.archives-ouvertes.fr/hal-02498084/document https://hal.archives-ouvertes.fr/hal-02498084/file/2004PA001116.pdf https://doi.org/10.1029/2004PA001116 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2004PA001116 hal-02498084 https://hal.archives-ouvertes.fr/hal-02498084 https://hal.archives-ouvertes.fr/hal-02498084/document https://hal.archives-ouvertes.fr/hal-02498084/file/2004PA001116.pdf doi:10.1029/2004PA001116 info:eu-repo/semantics/OpenAccess ISSN: 0883-8305 Paleoceanography https://hal.archives-ouvertes.fr/hal-02498084 Paleoceanography, American Geophysical Union, 2005, 20 (4), pp.n/a-n/a. ⟨10.1029/2004PA001116⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2005 ftccsdartic https://doi.org/10.1029/2004PA001116 2021-12-19T00:52:16Z International audience [1] We measured the oxygen isotopic composition of planktonic and benthic foraminifera in three cores collected at key positions to reconstruct the paleoceanography of the Barents Sea: core ASV 880 on the path of the northern branch of Atlantic water inflowing from the Arctic Ocean, core ASV 1200 in the central basin near the polar front, and core ASV 1157 in the main area of brine formation. Modern seawater d 18 O measurements show that far from the coast, d 18 O variations are linearly linked to the salinity changes associated with sea ice melting. The foraminifer d 18 O records are dated by 14 C measurements performed on mollusk shells, and they provide a detailed reconstruction of the paleoceanographic evolution of the Barents Sea during the Holocene. Four main steps were recognized: the terminal phase of the deglaciation with melting of the main glaciers, which were located on the surrounding continent and islands, the short thermal optimum from 7.8 ka B.P. to 6.8 ka B.P., a cold mid-Holocene phase with a large reduction of the inflow of Atlantic water, and the inception of the modern hydrological pattern by 4.7 ka B.P. Brine water formation was active during the whole Holocene. The paleoclimatic evolution of the Barents Sea was driven by both high-latitude summer insolation and the intensity of the Atlantic water inflow. Article in Journal/Newspaper Arctic Arctic Ocean Barents Sea Foraminifera* Sea ice Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Arctic Ocean Barents Sea Central Basin ENVELOPE(43.000,43.000,73.500,73.500) Paleoceanography 20 4 n/a n/a |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Duplessy, J.C. Cortijo, E. Ivanova, E., Khusid, T. Labeyrie, L. Levitan, M. Murdmaa, I. Paterne, M. Paleoceanography of the Barents Sea during the Holocene |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience [1] We measured the oxygen isotopic composition of planktonic and benthic foraminifera in three cores collected at key positions to reconstruct the paleoceanography of the Barents Sea: core ASV 880 on the path of the northern branch of Atlantic water inflowing from the Arctic Ocean, core ASV 1200 in the central basin near the polar front, and core ASV 1157 in the main area of brine formation. Modern seawater d 18 O measurements show that far from the coast, d 18 O variations are linearly linked to the salinity changes associated with sea ice melting. The foraminifer d 18 O records are dated by 14 C measurements performed on mollusk shells, and they provide a detailed reconstruction of the paleoceanographic evolution of the Barents Sea during the Holocene. Four main steps were recognized: the terminal phase of the deglaciation with melting of the main glaciers, which were located on the surrounding continent and islands, the short thermal optimum from 7.8 ka B.P. to 6.8 ka B.P., a cold mid-Holocene phase with a large reduction of the inflow of Atlantic water, and the inception of the modern hydrological pattern by 4.7 ka B.P. Brine water formation was active during the whole Holocene. The paleoclimatic evolution of the Barents Sea was driven by both high-latitude summer insolation and the intensity of the Atlantic water inflow. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Paléocéanographie (PALEOCEAN) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) St. Petersburg State Polytechnical University Géochrononologie Traceurs Archéométrie (GEOTRAC) |
format |
Article in Journal/Newspaper |
author |
Duplessy, J.C. Cortijo, E. Ivanova, E., Khusid, T. Labeyrie, L. Levitan, M. Murdmaa, I. Paterne, M. |
author_facet |
Duplessy, J.C. Cortijo, E. Ivanova, E., Khusid, T. Labeyrie, L. Levitan, M. Murdmaa, I. Paterne, M. |
author_sort |
Duplessy, J.C. |
title |
Paleoceanography of the Barents Sea during the Holocene |
title_short |
Paleoceanography of the Barents Sea during the Holocene |
title_full |
Paleoceanography of the Barents Sea during the Holocene |
title_fullStr |
Paleoceanography of the Barents Sea during the Holocene |
title_full_unstemmed |
Paleoceanography of the Barents Sea during the Holocene |
title_sort |
paleoceanography of the barents sea during the holocene |
publisher |
HAL CCSD |
publishDate |
2005 |
url |
https://hal.archives-ouvertes.fr/hal-02498084 https://hal.archives-ouvertes.fr/hal-02498084/document https://hal.archives-ouvertes.fr/hal-02498084/file/2004PA001116.pdf https://doi.org/10.1029/2004PA001116 |
long_lat |
ENVELOPE(43.000,43.000,73.500,73.500) |
geographic |
Arctic Arctic Ocean Barents Sea Central Basin |
geographic_facet |
Arctic Arctic Ocean Barents Sea Central Basin |
genre |
Arctic Arctic Ocean Barents Sea Foraminifera* Sea ice |
genre_facet |
Arctic Arctic Ocean Barents Sea Foraminifera* Sea ice |
op_source |
ISSN: 0883-8305 Paleoceanography https://hal.archives-ouvertes.fr/hal-02498084 Paleoceanography, American Geophysical Union, 2005, 20 (4), pp.n/a-n/a. ⟨10.1029/2004PA001116⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2004PA001116 hal-02498084 https://hal.archives-ouvertes.fr/hal-02498084 https://hal.archives-ouvertes.fr/hal-02498084/document https://hal.archives-ouvertes.fr/hal-02498084/file/2004PA001116.pdf doi:10.1029/2004PA001116 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2004PA001116 |
container_title |
Paleoceanography |
container_volume |
20 |
container_issue |
4 |
container_start_page |
n/a |
op_container_end_page |
n/a |
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1766341023240290304 |