Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data
International audience High-temporal resolution pollen record from the Alboran Sea ODP Site 976, pollen-based quantitative climate reconstruction and biomisation show that changes of Mediterranean vegetation have been clearly modulated by short and long term variability during the last 25 000 years....
Published in: | Climate of the Past |
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Main Authors: | , , , , , , |
Other Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2009
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Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-00419566 https://hal.archives-ouvertes.fr/hal-00419566/document https://hal.archives-ouvertes.fr/hal-00419566/file/cp-5-503-2009.pdf https://doi.org/10.5194/cp-5-503-2009 |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
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English |
topic |
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Combourieu-Nebout, Nathalie Peyron, Odile Dormoy, Isabelle Desprat, Stéphanie Beaudouin, Célia Kotthoff, Ulrich Marret, Fabienne Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data |
topic_facet |
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience High-temporal resolution pollen record from the Alboran Sea ODP Site 976, pollen-based quantitative climate reconstruction and biomisation show that changes of Mediterranean vegetation have been clearly modulated by short and long term variability during the last 25 000 years. The reliability of the quantitative climate reconstruction from marine pollen spectra has been tested using 22 marine core-top samples from the Mediterranean. The ODP Site 976 pollen record and climatic reconstruction confirm that Mediterranean environments have a rapid response to the climatic fluctuations during the last Termination. The western Mediterranean vegetation response appears nearly synchronous with North Atlantic variability during the last deglaciation as well as during the Holocene. High-resolution analyses of the ODP Site 976 pollen record show a cooling trend during the Bölling/Allerød period. In addition, this period is marked by two warm episodes bracketing a cooling event that represent the Bölling-Older Dryas-Allerød succession. During the Holocene, recurrent declines of the forest cover over the Alboran Sea borderlands indicate climate events that correlate well with several events of increased Mediterranean dryness observed on the continent and with Mediterranean Sea cooling episodes detected by alkenone-based sea surface temperature reconstructions. These events clearly reflect the response of the Mediterranean vegetation to the North Atlantic Holocene cold events. |
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) Laboratoire Chrono-environnement - CNRS - UBFC (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) Department of Geosciences Universität Hamburg (UHH) Department of Geography University of Liverpool The publication of this article is financed by CNRS-INSU |
format |
Article in Journal/Newspaper |
author |
Combourieu-Nebout, Nathalie Peyron, Odile Dormoy, Isabelle Desprat, Stéphanie Beaudouin, Célia Kotthoff, Ulrich Marret, Fabienne |
author_facet |
Combourieu-Nebout, Nathalie Peyron, Odile Dormoy, Isabelle Desprat, Stéphanie Beaudouin, Célia Kotthoff, Ulrich Marret, Fabienne |
author_sort |
Combourieu-Nebout, Nathalie |
title |
Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data |
title_short |
Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data |
title_full |
Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data |
title_fullStr |
Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data |
title_full_unstemmed |
Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data |
title_sort |
rapid climatic variability in the west mediterranean during the last 25 000 years from high resolution pollen data |
publisher |
HAL CCSD |
publishDate |
2009 |
url |
https://hal.archives-ouvertes.fr/hal-00419566 https://hal.archives-ouvertes.fr/hal-00419566/document https://hal.archives-ouvertes.fr/hal-00419566/file/cp-5-503-2009.pdf https://doi.org/10.5194/cp-5-503-2009 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.archives-ouvertes.fr/hal-00419566 Climate of the Past, European Geosciences Union (EGU), 2009, 5 (3), pp.503-521. ⟨10.5194/cp-5-503-2009⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-5-503-2009 hal-00419566 https://hal.archives-ouvertes.fr/hal-00419566 https://hal.archives-ouvertes.fr/hal-00419566/document https://hal.archives-ouvertes.fr/hal-00419566/file/cp-5-503-2009.pdf doi:10.5194/cp-5-503-2009 |
op_rights |
http://creativecommons.org/licenses/by-nc/ info:eu-repo/semantics/OpenAccess |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.5194/cp-5-503-2009 |
container_title |
Climate of the Past |
container_volume |
5 |
container_issue |
3 |
container_start_page |
503 |
op_container_end_page |
521 |
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1766128015584002048 |
spelling |
ftccsdartic:oai:HAL:hal-00419566v1 2023-05-15T17:30:53+02:00 Rapid climatic variability in the west Mediterranean during the last 25 000 years from high resolution pollen data Combourieu-Nebout, Nathalie Peyron, Odile Dormoy, Isabelle Desprat, Stéphanie Beaudouin, Célia Kotthoff, Ulrich Marret, Fabienne 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) Laboratoire Chrono-environnement - CNRS - UBFC (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) Department of Geosciences Universität Hamburg (UHH) Department of Geography University of Liverpool The publication of this article is financed by CNRS-INSU 2009 https://hal.archives-ouvertes.fr/hal-00419566 https://hal.archives-ouvertes.fr/hal-00419566/document https://hal.archives-ouvertes.fr/hal-00419566/file/cp-5-503-2009.pdf https://doi.org/10.5194/cp-5-503-2009 en eng HAL CCSD European Geosciences Union (EGU) info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-5-503-2009 hal-00419566 https://hal.archives-ouvertes.fr/hal-00419566 https://hal.archives-ouvertes.fr/hal-00419566/document https://hal.archives-ouvertes.fr/hal-00419566/file/cp-5-503-2009.pdf doi:10.5194/cp-5-503-2009 http://creativecommons.org/licenses/by-nc/ info:eu-repo/semantics/OpenAccess CC-BY-NC ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.archives-ouvertes.fr/hal-00419566 Climate of the Past, European Geosciences Union (EGU), 2009, 5 (3), pp.503-521. ⟨10.5194/cp-5-503-2009⟩ [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2009 ftccsdartic https://doi.org/10.5194/cp-5-503-2009 2021-12-19T00:59:43Z International audience High-temporal resolution pollen record from the Alboran Sea ODP Site 976, pollen-based quantitative climate reconstruction and biomisation show that changes of Mediterranean vegetation have been clearly modulated by short and long term variability during the last 25 000 years. The reliability of the quantitative climate reconstruction from marine pollen spectra has been tested using 22 marine core-top samples from the Mediterranean. The ODP Site 976 pollen record and climatic reconstruction confirm that Mediterranean environments have a rapid response to the climatic fluctuations during the last Termination. The western Mediterranean vegetation response appears nearly synchronous with North Atlantic variability during the last deglaciation as well as during the Holocene. High-resolution analyses of the ODP Site 976 pollen record show a cooling trend during the Bölling/Allerød period. In addition, this period is marked by two warm episodes bracketing a cooling event that represent the Bölling-Older Dryas-Allerød succession. During the Holocene, recurrent declines of the forest cover over the Alboran Sea borderlands indicate climate events that correlate well with several events of increased Mediterranean dryness observed on the continent and with Mediterranean Sea cooling episodes detected by alkenone-based sea surface temperature reconstructions. These events clearly reflect the response of the Mediterranean vegetation to the North Atlantic Holocene cold events. Article in Journal/Newspaper North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Climate of the Past 5 3 503 521 |