Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13
International audience A new method to reconstruct past climatic conditions between 130 and 100 ka BP from pollen and isotopic data is applied to a previously unanalyzed Grande Pile core, GPXXI. We applied the inverse mode to the Biome4 vegetation model. The method utilizes delta C-13, measured in p...
Published in: | Quaternary Science Reviews |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2006
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Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/halsde-00339202 https://doi.org/10.1016/j.quascirev.2006.06.011 |
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ftccsdartic:oai:HAL:halsde-00339202v1 |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
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English |
topic |
HEAT-FLUX OCEAN CIRCULATION NORDIC SEAS ARCTIC ECOSYSTEMS LAST INTERGLACIAL PERIOD SEDIMENTARY ORGANIC-MATTER EUROPEAN POLLEN RECORDS NORTH-ATLANTIC CLIMATE-CHANGE FLUCTUATIONS [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
HEAT-FLUX OCEAN CIRCULATION NORDIC SEAS ARCTIC ECOSYSTEMS LAST INTERGLACIAL PERIOD SEDIMENTARY ORGANIC-MATTER EUROPEAN POLLEN RECORDS NORTH-ATLANTIC CLIMATE-CHANGE FLUCTUATIONS [SDE.MCG]Environmental Sciences/Global Changes Rousseau, Denis-Didier Hatté, Christine Guiot, Joel Duzer, Danièle Schevin, Patrick Kukla, G. Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13 |
topic_facet |
HEAT-FLUX OCEAN CIRCULATION NORDIC SEAS ARCTIC ECOSYSTEMS LAST INTERGLACIAL PERIOD SEDIMENTARY ORGANIC-MATTER EUROPEAN POLLEN RECORDS NORTH-ATLANTIC CLIMATE-CHANGE FLUCTUATIONS [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience A new method to reconstruct past climatic conditions between 130 and 100 ka BP from pollen and isotopic data is applied to a previously unanalyzed Grande Pile core, GPXXI. We applied the inverse mode to the Biome4 vegetation model. The method utilizes delta C-13, measured in parallel to the pollen samples as a constraint for the model. First the biomes and the delta C-13 simulated by the model are compared with the biome allocation of the pollen data. The delta C-13 to be simulated takes into account the degradation effect on the preserved organic matter. This procedure allows the reconstruction of the mean annual temperature and precipitation as well as the mean temperatures of the warmest and coldest months. We show that during the Eemian sensu stricto, the reconstructed precipitation is similar to modern values with low variability. The cold stadials and the penultimate glaciation are characterized by very low precipitation amounts. The temperature estimates, however, indicate differences with several oscillations identified. The peak values are reached at about 124-125 ka BP, but two other warm intervals are also identified. The variations in temperature appear to be related to sea-surface temperature oscillations in the North Atlantic region and are also in agreement with the timing of ice sheet build-up in the Northern Hemisphere. Seasonal variations are also identified in the estimated temperatures of the warmest and coldest months. (c) 2006 Elsevier Ltd. All rights reserved. |
author2 |
Institut des Sciences de l'Evolution de Montpellier (UMR ISEM) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement IRD : UR226 Lamont-Doherty Earth Observatory (LDEO) Columbia University New York Lehrstuhl für Geomorphologie Universität Bayreuth 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) Géochrononologie Traceurs Archéométrie (GEOTRAC) 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) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA) |
format |
Article in Journal/Newspaper |
author |
Rousseau, Denis-Didier Hatté, Christine Guiot, Joel Duzer, Danièle Schevin, Patrick Kukla, G. |
author_facet |
Rousseau, Denis-Didier Hatté, Christine Guiot, Joel Duzer, Danièle Schevin, Patrick Kukla, G. |
author_sort |
Rousseau, Denis-Didier |
title |
Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13 |
title_short |
Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13 |
title_full |
Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13 |
title_fullStr |
Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13 |
title_full_unstemmed |
Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13 |
title_sort |
reconstruction of the grande pile eemian using inverse modeling of biomes and delta c-13 |
publisher |
HAL CCSD |
publishDate |
2006 |
url |
https://hal.archives-ouvertes.fr/halsde-00339202 https://doi.org/10.1016/j.quascirev.2006.06.011 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change Ice Sheet Nordic Seas North Atlantic |
genre_facet |
Arctic Climate change Ice Sheet Nordic Seas North Atlantic |
op_source |
ISSN: 0277-3791 Quaternary Science Reviews https://hal.archives-ouvertes.fr/halsde-00339202 Quaternary Science Reviews, Elsevier, 2006, 25 (21-22), pp.2806-2819. ⟨10.1016/j.quascirev.2006.06.011⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2006.06.011 halsde-00339202 https://hal.archives-ouvertes.fr/halsde-00339202 doi:10.1016/j.quascirev.2006.06.011 |
op_doi |
https://doi.org/10.1016/j.quascirev.2006.06.011 |
container_title |
Quaternary Science Reviews |
container_volume |
25 |
container_issue |
21-22 |
container_start_page |
2806 |
op_container_end_page |
2819 |
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1766342490007273472 |
spelling |
ftccsdartic:oai:HAL:halsde-00339202v1 2023-05-15T15:11:40+02:00 Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and delta C-13 Rousseau, Denis-Didier Hatté, Christine Guiot, Joel Duzer, Danièle Schevin, Patrick Kukla, G. Institut des Sciences de l'Evolution de Montpellier (UMR ISEM) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement IRD : UR226 Lamont-Doherty Earth Observatory (LDEO) Columbia University New York Lehrstuhl für Geomorphologie Universität Bayreuth 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) Géochrononologie Traceurs Archéométrie (GEOTRAC) 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) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA) 2006-11 https://hal.archives-ouvertes.fr/halsde-00339202 https://doi.org/10.1016/j.quascirev.2006.06.011 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2006.06.011 halsde-00339202 https://hal.archives-ouvertes.fr/halsde-00339202 doi:10.1016/j.quascirev.2006.06.011 ISSN: 0277-3791 Quaternary Science Reviews https://hal.archives-ouvertes.fr/halsde-00339202 Quaternary Science Reviews, Elsevier, 2006, 25 (21-22), pp.2806-2819. ⟨10.1016/j.quascirev.2006.06.011⟩ HEAT-FLUX OCEAN CIRCULATION NORDIC SEAS ARCTIC ECOSYSTEMS LAST INTERGLACIAL PERIOD SEDIMENTARY ORGANIC-MATTER EUROPEAN POLLEN RECORDS NORTH-ATLANTIC CLIMATE-CHANGE FLUCTUATIONS [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2006 ftccsdartic https://doi.org/10.1016/j.quascirev.2006.06.011 2021-12-19T04:08:17Z International audience A new method to reconstruct past climatic conditions between 130 and 100 ka BP from pollen and isotopic data is applied to a previously unanalyzed Grande Pile core, GPXXI. We applied the inverse mode to the Biome4 vegetation model. The method utilizes delta C-13, measured in parallel to the pollen samples as a constraint for the model. First the biomes and the delta C-13 simulated by the model are compared with the biome allocation of the pollen data. The delta C-13 to be simulated takes into account the degradation effect on the preserved organic matter. This procedure allows the reconstruction of the mean annual temperature and precipitation as well as the mean temperatures of the warmest and coldest months. We show that during the Eemian sensu stricto, the reconstructed precipitation is similar to modern values with low variability. The cold stadials and the penultimate glaciation are characterized by very low precipitation amounts. The temperature estimates, however, indicate differences with several oscillations identified. The peak values are reached at about 124-125 ka BP, but two other warm intervals are also identified. The variations in temperature appear to be related to sea-surface temperature oscillations in the North Atlantic region and are also in agreement with the timing of ice sheet build-up in the Northern Hemisphere. Seasonal variations are also identified in the estimated temperatures of the warmest and coldest months. (c) 2006 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Arctic Climate change Ice Sheet Nordic Seas North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Quaternary Science Reviews 25 21-22 2806 2819 |