Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems
International audience Patagonia is ideally situated to reconstruct past migrations of the southern westerly winds (SWWs) due to itssoutherly maritime location. The SWWs are an important driver of Southern Ocean upwelling and their strengthand latitudinal position changed during the Holocene, leadin...
Published in: | Global and Planetary Change |
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Main Authors: | , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2023
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Subjects: | |
Online Access: | https://hal.science/hal-04287379 https://doi.org/10.1016/j.gloplacha.2023.104050 |
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ftinstagro:oai:HAL:hal-04287379v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Portail HAL Institut Agro |
op_collection_id |
ftinstagro |
language |
English |
topic |
Holocene Speleothems Stable isotopes Southern westerly winds Patagonia [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry |
spellingShingle |
Holocene Speleothems Stable isotopes Southern westerly winds Patagonia [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry Nehme, C. Todisco, D. Breitenbach, S.F.M. Couchoud, Isabelle Marchegiano, M. Peral, M. Vonhof, H. Hellstrom, J. Tjallingii, R. Claeys, P. Borrero, L. Martin, F. Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems |
topic_facet |
Holocene Speleothems Stable isotopes Southern westerly winds Patagonia [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry |
description |
International audience Patagonia is ideally situated to reconstruct past migrations of the southern westerly winds (SWWs) due to itssoutherly maritime location. The SWWs are an important driver of Southern Ocean upwelling and their strengthand latitudinal position changed during the Holocene, leading thus to different responses of the vegetation topast climate changes along the Chilean continental margin. A new speleothem record from Cueva Chica (51◦S) isinvestigated to reconstruct past climatic changes throughout the Holocene in conjunction with other marine andpaleoenvironmental records of the region and better constrain the regional paleoclimatic evolutions of SWWs.Samples comprising both a flowstone core and a stalagmite were radiometrically dated (U–Th & 14C) toconstruct age-depth models for the highly-resolved proxy profiles (δ13C, δ18O, chemical composition). TheCueva Chica record provides a highly-resolved isotopic and elemental curves for the last 12 ka, albeit with ahiatus from 5.8 to 4 ka BP. The multi-proxy analysis suggests three climatic regimes throughout the Holocene inSouthern Patagonia: i) an early Holocene wet period (with the exception of two dry excursions at 10.5 ka and 8.5ka BP), ii) a mid-Holocene dry period and iii), a return to generally wet conditions over the late Holocene. Theglobal drivers for these tri-phased climatic regimes are likely related to oceanic and South polar feedbacks. Theearly Holocene was the warmest period and might be attributable to changes in global ocean circulation whichinvolved a rise in air T◦ and a strength in SWW from 50◦S, and therefore higher precipitations over landmass.After 9 ka BP, an intensified deglaciation dynamic along the Antarctic Peninsula is concordant with increasingsummer insolation in the Southern hemisphere, leading to a poleward shift of the SWWs in response to globalwarming and thus to a reduction in moisture supply from the Pacific onto the Patagonian shore. After 5 ka BP, agradual SST decline is consistent with an equatorward ... |
author2 |
Identité et Différenciation de l’Espace, de l’Environnement et des Sociétés (IDEES) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-Université Le Havre Normandie (ULH) Normandie Université (NU)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche Interdisciplinaire Homme et Société (IRIHS) Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Normandie Université (NU)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU) University of Northumbria at Newcastle United Kingdom Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Analytical, Environmental and Geo- Chemistry Vrije Universiteit Brussel (VUB) 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) Max Planck Institute for Chemistry (MPIC) Max-Planck-Gesellschaft School of Earth Sciences Melbourne Faculty of Science Melbourne University of Melbourne-University of Melbourne German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ) Science et Technologie du Lait et de l'Oeuf (STLO) Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro Rennes Angers Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro) Centre National Interprofessionnel de l'Economie Laitière Paris (CNIEL) |
format |
Article in Journal/Newspaper |
author |
Nehme, C. Todisco, D. Breitenbach, S.F.M. Couchoud, Isabelle Marchegiano, M. Peral, M. Vonhof, H. Hellstrom, J. Tjallingii, R. Claeys, P. Borrero, L. Martin, F. |
author_facet |
Nehme, C. Todisco, D. Breitenbach, S.F.M. Couchoud, Isabelle Marchegiano, M. Peral, M. Vonhof, H. Hellstrom, J. Tjallingii, R. Claeys, P. Borrero, L. Martin, F. |
author_sort |
Nehme, C. |
title |
Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems |
title_short |
Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems |
title_full |
Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems |
title_fullStr |
Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems |
title_full_unstemmed |
Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems |
title_sort |
holocene hydroclimate variability along the southern patagonian margin (chile) reconstructed from cueva chica speleothems |
publisher |
HAL CCSD |
publishDate |
2023 |
url |
https://hal.science/hal-04287379 https://doi.org/10.1016/j.gloplacha.2023.104050 |
long_lat |
ENVELOPE(-57.050,-57.050,-63.350,-63.350) ENVELOPE(-62.600,-62.600,-64.150,-64.150) |
geographic |
Antarctic Antarctic Peninsula Chica Cueva Pacific Patagonia Southern Ocean The Antarctic |
geographic_facet |
Antarctic Antarctic Peninsula Chica Cueva Pacific Patagonia Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctic Peninsula Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Southern Ocean |
op_source |
ISSN: 0921-8181 Global and Planetary Change https://hal.science/hal-04287379 Global and Planetary Change, 2023, 222, pp.104050. ⟨10.1016/j.gloplacha.2023.104050⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gloplacha.2023.104050 hal-04287379 https://hal.science/hal-04287379 doi:10.1016/j.gloplacha.2023.104050 |
op_doi |
https://doi.org/10.1016/j.gloplacha.2023.104050 |
container_title |
Global and Planetary Change |
container_volume |
222 |
container_start_page |
104050 |
_version_ |
1785579174157615104 |
spelling |
ftinstagro:oai:HAL:hal-04287379v1 2023-12-17T10:18:45+01:00 Holocene hydroclimate variability along the Southern Patagonian margin (Chile) reconstructed from Cueva Chica speleothems Nehme, C. Todisco, D. Breitenbach, S.F.M. Couchoud, Isabelle Marchegiano, M. Peral, M. Vonhof, H. Hellstrom, J. Tjallingii, R. Claeys, P. Borrero, L. Martin, F. Identité et Différenciation de l’Espace, de l’Environnement et des Sociétés (IDEES) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-Université Le Havre Normandie (ULH) Normandie Université (NU)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche Interdisciplinaire Homme et Société (IRIHS) Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Normandie Université (NU)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU) University of Northumbria at Newcastle United Kingdom Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Analytical, Environmental and Geo- Chemistry Vrije Universiteit Brussel (VUB) 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) Max Planck Institute for Chemistry (MPIC) Max-Planck-Gesellschaft School of Earth Sciences Melbourne Faculty of Science Melbourne University of Melbourne-University of Melbourne German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ) Science et Technologie du Lait et de l'Oeuf (STLO) Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro Rennes Angers Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro) Centre National Interprofessionnel de l'Economie Laitière Paris (CNIEL) 2023-02-03 https://hal.science/hal-04287379 https://doi.org/10.1016/j.gloplacha.2023.104050 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gloplacha.2023.104050 hal-04287379 https://hal.science/hal-04287379 doi:10.1016/j.gloplacha.2023.104050 ISSN: 0921-8181 Global and Planetary Change https://hal.science/hal-04287379 Global and Planetary Change, 2023, 222, pp.104050. ⟨10.1016/j.gloplacha.2023.104050⟩ Holocene Speleothems Stable isotopes Southern westerly winds Patagonia [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry info:eu-repo/semantics/article Journal articles 2023 ftinstagro https://doi.org/10.1016/j.gloplacha.2023.104050 2023-11-18T22:27:43Z International audience Patagonia is ideally situated to reconstruct past migrations of the southern westerly winds (SWWs) due to itssoutherly maritime location. The SWWs are an important driver of Southern Ocean upwelling and their strengthand latitudinal position changed during the Holocene, leading thus to different responses of the vegetation topast climate changes along the Chilean continental margin. A new speleothem record from Cueva Chica (51◦S) isinvestigated to reconstruct past climatic changes throughout the Holocene in conjunction with other marine andpaleoenvironmental records of the region and better constrain the regional paleoclimatic evolutions of SWWs.Samples comprising both a flowstone core and a stalagmite were radiometrically dated (U–Th & 14C) toconstruct age-depth models for the highly-resolved proxy profiles (δ13C, δ18O, chemical composition). TheCueva Chica record provides a highly-resolved isotopic and elemental curves for the last 12 ka, albeit with ahiatus from 5.8 to 4 ka BP. The multi-proxy analysis suggests three climatic regimes throughout the Holocene inSouthern Patagonia: i) an early Holocene wet period (with the exception of two dry excursions at 10.5 ka and 8.5ka BP), ii) a mid-Holocene dry period and iii), a return to generally wet conditions over the late Holocene. Theglobal drivers for these tri-phased climatic regimes are likely related to oceanic and South polar feedbacks. Theearly Holocene was the warmest period and might be attributable to changes in global ocean circulation whichinvolved a rise in air T◦ and a strength in SWW from 50◦S, and therefore higher precipitations over landmass.After 9 ka BP, an intensified deglaciation dynamic along the Antarctic Peninsula is concordant with increasingsummer insolation in the Southern hemisphere, leading to a poleward shift of the SWWs in response to globalwarming and thus to a reduction in moisture supply from the Pacific onto the Patagonian shore. After 5 ka BP, agradual SST decline is consistent with an equatorward ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Southern Ocean Portail HAL Institut Agro Antarctic Antarctic Peninsula Chica ENVELOPE(-57.050,-57.050,-63.350,-63.350) Cueva ENVELOPE(-62.600,-62.600,-64.150,-64.150) Pacific Patagonia Southern Ocean The Antarctic Global and Planetary Change 222 104050 |