The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies
International audience As compared to the late Pleistocene, Alkenone-based sea surface temperature (SST) in the Benguela region revealed relatively warm and stable SST recorded between ∼3.5 and 2.0 Ma, and coincide with a period of increasing biological productivity as revealed by increasing deposit...
Published in: | Geochemistry, Geophysics, Geosystems |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2014
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Subjects: | |
Online Access: | https://amu.hal.science/hal-01472057 https://amu.hal.science/hal-01472057/document https://amu.hal.science/hal-01472057/file/The_late_Pliocene_Benguela_upwelling_status_revisited_by%20means_ofmultiple_temperature_proxies_1.pdf https://doi.org/10.1002/2013GC004940 |
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ftcollegfrance:oai:HAL:hal-01472057v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Collège de France: HAL |
op_collection_id |
ftcollegfrance |
language |
English |
topic |
temperature proxies Benguela region Pleistocene [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
temperature proxies Benguela region Pleistocene [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Leduc, Guillaume Garbe-Schönberg, Dieter Regenberg, Marcus Contoux, Camille Etourneau, Johan Schneider, Ralph The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies |
topic_facet |
temperature proxies Benguela region Pleistocene [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience As compared to the late Pleistocene, Alkenone-based sea surface temperature (SST) in the Benguela region revealed relatively warm and stable SST recorded between ∼3.5 and 2.0 Ma, and coincide with a period of increasing biological productivity as revealed by increasing deposition of biogenic opal. We assess how the hydrological patterns recorded in SST proxies are embedded in the geological record by performing a proxy-proxy comparison. We used Laser-Ablation Inductively Coupled Plasma-Mass Spectrometry to measure the Mg/Ca on the planktonic foraminifera species Globigerina bulloides, allowing in situ measurements of Mg/Ca on individual foraminiferal tests. Mg/Ca-derived temperatures provide much colder temperatures than alkenone-derived SST by up to 10°C. We build a scenario involving contrasting sensitivities of paleothermometers upon the annual cycle, namely alkenones preferentially capturing SST when the surface ocean is warmer than the mean-annual average SST, and G. bulloides capturing SST when upwelling intensifies. Multichamber analysis also suggests that G. bulloides migrates below the sea surface while calcifying its last chambers prior to gametogenesis, allowing the extraction of both surface and subsurface temperature from Mg/Ca measured on different chambers. The range of temperatures recorded between our multiple SST proxies is supported by the range of temperatures simulated with a general circulation model when different seasons, different water depth and different orbital configurations occurring during the late Pliocene are considered. A greater seasonal cycle in SST during the Pliocene can account for alkenone and Mg/Ca-derived temperature contrast, pointing to a radically different mode of upwelling activity in the Benguela region compared to today. |
author2 |
Institute of Geosciences Kiel Christian-Albrechts-Universität zu Kiel = Christian-Albrechts University of Kiel = Université Christian-Albrechts de Kiel (CAU) Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-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) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Leduc, Guillaume Garbe-Schönberg, Dieter Regenberg, Marcus Contoux, Camille Etourneau, Johan Schneider, Ralph |
author_facet |
Leduc, Guillaume Garbe-Schönberg, Dieter Regenberg, Marcus Contoux, Camille Etourneau, Johan Schneider, Ralph |
author_sort |
Leduc, Guillaume |
title |
The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies |
title_short |
The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies |
title_full |
The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies |
title_fullStr |
The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies |
title_full_unstemmed |
The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies |
title_sort |
late pliocene benguela upwelling status revisited by means of multiple temperature proxies |
publisher |
HAL CCSD |
publishDate |
2014 |
url |
https://amu.hal.science/hal-01472057 https://amu.hal.science/hal-01472057/document https://amu.hal.science/hal-01472057/file/The_late_Pliocene_Benguela_upwelling_status_revisited_by%20means_ofmultiple_temperature_proxies_1.pdf https://doi.org/10.1002/2013GC004940 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://amu.hal.science/hal-01472057 Geochemistry, Geophysics, Geosystems, 2014, 15 (2), pp.475-491. ⟨10.1002/2013GC004940⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/2013GC004940 hal-01472057 https://amu.hal.science/hal-01472057 https://amu.hal.science/hal-01472057/document https://amu.hal.science/hal-01472057/file/The_late_Pliocene_Benguela_upwelling_status_revisited_by%20means_ofmultiple_temperature_proxies_1.pdf doi:10.1002/2013GC004940 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1002/2013GC004940 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
15 |
container_issue |
2 |
container_start_page |
475 |
op_container_end_page |
491 |
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1810472687918645248 |
spelling |
ftcollegfrance:oai:HAL:hal-01472057v1 2024-09-15T18:31:05+00:00 The late Pliocene Benguela upwelling status revisited by means of multiple temperature proxies Leduc, Guillaume Garbe-Schönberg, Dieter Regenberg, Marcus Contoux, Camille Etourneau, Johan Schneider, Ralph Institute of Geosciences Kiel Christian-Albrechts-Universität zu Kiel = Christian-Albrechts University of Kiel = Université Christian-Albrechts de Kiel (CAU) Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-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) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2014 https://amu.hal.science/hal-01472057 https://amu.hal.science/hal-01472057/document https://amu.hal.science/hal-01472057/file/The_late_Pliocene_Benguela_upwelling_status_revisited_by%20means_ofmultiple_temperature_proxies_1.pdf https://doi.org/10.1002/2013GC004940 en eng HAL CCSD AGU and the Geochemical Society info:eu-repo/semantics/altIdentifier/doi/10.1002/2013GC004940 hal-01472057 https://amu.hal.science/hal-01472057 https://amu.hal.science/hal-01472057/document https://amu.hal.science/hal-01472057/file/The_late_Pliocene_Benguela_upwelling_status_revisited_by%20means_ofmultiple_temperature_proxies_1.pdf doi:10.1002/2013GC004940 info:eu-repo/semantics/OpenAccess EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://amu.hal.science/hal-01472057 Geochemistry, Geophysics, Geosystems, 2014, 15 (2), pp.475-491. ⟨10.1002/2013GC004940⟩ temperature proxies Benguela region Pleistocene [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [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 2014 ftcollegfrance https://doi.org/10.1002/2013GC004940 2024-08-01T23:31:27Z International audience As compared to the late Pleistocene, Alkenone-based sea surface temperature (SST) in the Benguela region revealed relatively warm and stable SST recorded between ∼3.5 and 2.0 Ma, and coincide with a period of increasing biological productivity as revealed by increasing deposition of biogenic opal. We assess how the hydrological patterns recorded in SST proxies are embedded in the geological record by performing a proxy-proxy comparison. We used Laser-Ablation Inductively Coupled Plasma-Mass Spectrometry to measure the Mg/Ca on the planktonic foraminifera species Globigerina bulloides, allowing in situ measurements of Mg/Ca on individual foraminiferal tests. Mg/Ca-derived temperatures provide much colder temperatures than alkenone-derived SST by up to 10°C. We build a scenario involving contrasting sensitivities of paleothermometers upon the annual cycle, namely alkenones preferentially capturing SST when the surface ocean is warmer than the mean-annual average SST, and G. bulloides capturing SST when upwelling intensifies. Multichamber analysis also suggests that G. bulloides migrates below the sea surface while calcifying its last chambers prior to gametogenesis, allowing the extraction of both surface and subsurface temperature from Mg/Ca measured on different chambers. The range of temperatures recorded between our multiple SST proxies is supported by the range of temperatures simulated with a general circulation model when different seasons, different water depth and different orbital configurations occurring during the late Pliocene are considered. A greater seasonal cycle in SST during the Pliocene can account for alkenone and Mg/Ca-derived temperature contrast, pointing to a radically different mode of upwelling activity in the Benguela region compared to today. Article in Journal/Newspaper Planktonic foraminifera Collège de France: HAL Geochemistry, Geophysics, Geosystems 15 2 475 491 |