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), 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
Language:English
Published: HAL CCSD 2006
Subjects:
Online Access:https://hal.archives-ouvertes.fr/halsde-00339202
https://doi.org/10.1016/j.quascirev.2006.06.011
id ftccsdartic:oai:HAL:halsde-00339202v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language 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⟩
op_relation 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
_version_ 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