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...

Full description

Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Rousseau, Denis-Didier, Hatté, Christine, Guiot, Joel, Duzer, Danièle, Schevin, Patrick, Kukla, G.
Other Authors: Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS), 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), 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), Géochrononologie Traceurs Archéométrie (GEOTRAC), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), 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)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2006
Subjects:
Online Access:https://hal.science/halsde-00339202
https://doi.org/10.1016/j.quascirev.2006.06.011
id ftunimontpellier:oai:HAL:halsde-00339202v1
record_format openpolar
institution Open Polar
collection Université de Montpellier: HAL
op_collection_id ftunimontpellier
language English
topic LAST INTERGLACIAL PERIOD
SEDIMENTARY ORGANIC-MATTER
EUROPEAN POLLEN RECORDS
NORTH-ATLANTIC
CLIMATE-CHANGE
NORDIC SEAS
ARCTIC ECOSYSTEMS
OCEAN CIRCULATION
HEAT-FLUX
FLUCTUATIONS
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle LAST INTERGLACIAL PERIOD
SEDIMENTARY ORGANIC-MATTER
EUROPEAN POLLEN RECORDS
NORTH-ATLANTIC
CLIMATE-CHANGE
NORDIC SEAS
ARCTIC ECOSYSTEMS
OCEAN CIRCULATION
HEAT-FLUX
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 LAST INTERGLACIAL PERIOD
SEDIMENTARY ORGANIC-MATTER
EUROPEAN POLLEN RECORDS
NORTH-ATLANTIC
CLIMATE-CHANGE
NORDIC SEAS
ARCTIC ECOSYSTEMS
OCEAN CIRCULATION
HEAT-FLUX
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)
Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS)
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)
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)
Géochrononologie Traceurs Archéométrie (GEOTRAC)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
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)
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.science/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
EISSN: 1873-457X
Quaternary Science Reviews
https://hal.science/halsde-00339202
Quaternary Science Reviews, 2006, 25 (21-22), pp.2806-2819. ⟨10.1016/j.quascirev.2006.06.011⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2006.06.011
halsde-00339202
https://hal.science/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
_version_ 1802641622613098496
spelling ftunimontpellier:oai:HAL:halsde-00339202v1 2024-06-23T07:50:43+00:00 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) Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS) 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) 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) Géochrononologie Traceurs Archéométrie (GEOTRAC) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) 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) 2006-11 https://hal.science/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.science/halsde-00339202 doi:10.1016/j.quascirev.2006.06.011 ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/halsde-00339202 Quaternary Science Reviews, 2006, 25 (21-22), pp.2806-2819. ⟨10.1016/j.quascirev.2006.06.011⟩ LAST INTERGLACIAL PERIOD SEDIMENTARY ORGANIC-MATTER EUROPEAN POLLEN RECORDS NORTH-ATLANTIC CLIMATE-CHANGE NORDIC SEAS ARCTIC ECOSYSTEMS OCEAN CIRCULATION HEAT-FLUX FLUCTUATIONS [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2006 ftunimontpellier https://doi.org/10.1016/j.quascirev.2006.06.011 2024-06-10T14:23:08Z 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 Université de Montpellier: HAL Arctic Quaternary Science Reviews 25 21-22 2806 2819