Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations

In order to study the climate variations recorded by ice cores, it is necessary to have precise chronologies for the ice and gas phases. The aim of this work has been to improve ice cores chronologies, covering the last 800 000 years, through new measurements of the isotopic composition of the air δ...

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Main Author: Bazin, Lucie
Other Authors: 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), Université de Versailles-Saint Quentin en Yvelines, Amaëlle Landais
Format: Doctoral or Postdoctoral Thesis
Language:French
Published: HAL CCSD 2015
Subjects:
Online Access:https://theses.hal.science/tel-01245451
https://theses.hal.science/tel-01245451/document
https://theses.hal.science/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf
id ftinsu:oai:HAL:tel-01245451v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language French
topic Antarctic
Greenland
Ice cores
Air isotopic composition
Datation
Orbital tuning
Variations glaciaire-interglaciaires
Antarctique
Groenland
Carottes de glace
Composition isotopique de l'air
Synchronisation orbitale
Glacial-interglacial variations
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle Antarctic
Greenland
Ice cores
Air isotopic composition
Datation
Orbital tuning
Variations glaciaire-interglaciaires
Antarctique
Groenland
Carottes de glace
Composition isotopique de l'air
Synchronisation orbitale
Glacial-interglacial variations
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Bazin, Lucie
Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations
topic_facet Antarctic
Greenland
Ice cores
Air isotopic composition
Datation
Orbital tuning
Variations glaciaire-interglaciaires
Antarctique
Groenland
Carottes de glace
Composition isotopique de l'air
Synchronisation orbitale
Glacial-interglacial variations
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description In order to study the climate variations recorded by ice cores, it is necessary to have precise chronologies for the ice and gas phases. The aim of this work has been to improve ice cores chronologies, covering the last 800 000 years, through new measurements of the isotopic composition of the air δ15N, δ18Oatm et δO2/N2) trapped in EPICA Dome C (EDC) ice core and the use of the Datice dating tool.The first important result of this PhD has been the production of the Antarctic Ice Core Chronology (AICC2012), common for EDC, Vostok, EPICA Droning Maud Land (EDML), TALos Dome ICE core (TALDICE) and NorthGRIP ice cores. The bipolar see-saw theory is still valid on the new chronology. The AICC2012 chronology gives an age for Termination II in good agreement with other climate archives. Moreover, the duration of interglacial periods is unchanged compared to EDC3. While building the AICC2012 chronology, we have pointed out several limitations. Since then, we have improved Datice in order to correctly integrate constraints deduced from layer counting and their associated uncertainties. These improvements permit to build coherent chronologies respecting the underlying hypotheses of Datice. Moreover, we propose a new parameterization of the uncertainty associated with the background thinning function based on ice mechanical properties of EDC ice core. Finally, we were able to deduce new age constraints thanks to the new measurements of δO2/N2 and δ18Oatm performed on well-conserved ice from EDC. A multi-proxy comparison of Vostok, EDC and Dome F ice cores over MIS 5 has highlighted a possible influence of local climatic parameters on δO2/N2. The analysis of the delay between δ18Oatm and precession shows some variability over the last 800 ka. We propose that the delay between δ18Oatm and precession is increased during periods associated with Heinrich events. The results obtained during this PhD should be used for the next ice core coherent chronology. Afin d’étudier les variations climatiques enregistrées par les ...
author2 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)
Université de Versailles-Saint Quentin en Yvelines
Amaëlle Landais
format Doctoral or Postdoctoral Thesis
author Bazin, Lucie
author_facet Bazin, Lucie
author_sort Bazin, Lucie
title Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations
title_short Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations
title_full Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations
title_fullStr Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations
title_full_unstemmed Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations
title_sort isotopic composition of air trapped in epica dome c and talos dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations
publisher HAL CCSD
publishDate 2015
url https://theses.hal.science/tel-01245451
https://theses.hal.science/tel-01245451/document
https://theses.hal.science/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf
genre Antarc*
Antarctic
Antarctique*
EPICA
Greenland
Greenland ice cores
Groenland
ice core
genre_facet Antarc*
Antarctic
Antarctique*
EPICA
Greenland
Greenland ice cores
Groenland
ice core
op_source https://theses.hal.science/tel-01245451
Climatologie. Université de Versailles-Saint Quentin en Yvelines, 2015. Français. ⟨NNT : 2015VERS013V⟩
op_relation NNT: 2015VERS013V
tel-01245451
https://theses.hal.science/tel-01245451
https://theses.hal.science/tel-01245451/document
https://theses.hal.science/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf
op_rights info:eu-repo/semantics/OpenAccess
_version_ 1797586025016459264
spelling ftinsu:oai:HAL:tel-01245451v1 2024-04-28T07:56:59+00:00 Isotopic composition of air trapped in EPICA Dome C and Talos Dome ice cores in order to constrain the influence of orbital forcing and greenhouse gases on glacial–interglacial variations Analyse de l’air piégé dans les carottes de glace de Dôme C et Talos Dôme pour mieux contraindre le rôle du forçage orbital et des gaz à effet de serre dans les variations glaciaire-interglaciaire Bazin, Lucie 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) Université de Versailles-Saint Quentin en Yvelines Amaëlle Landais 2015-01-29 https://theses.hal.science/tel-01245451 https://theses.hal.science/tel-01245451/document https://theses.hal.science/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf fr fre HAL CCSD NNT: 2015VERS013V tel-01245451 https://theses.hal.science/tel-01245451 https://theses.hal.science/tel-01245451/document https://theses.hal.science/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf info:eu-repo/semantics/OpenAccess https://theses.hal.science/tel-01245451 Climatologie. Université de Versailles-Saint Quentin en Yvelines, 2015. Français. ⟨NNT : 2015VERS013V⟩ Antarctic Greenland Ice cores Air isotopic composition Datation Orbital tuning Variations glaciaire-interglaciaires Antarctique Groenland Carottes de glace Composition isotopique de l'air Synchronisation orbitale Glacial-interglacial variations [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/doctoralThesis Theses 2015 ftinsu 2024-04-05T00:49:39Z In order to study the climate variations recorded by ice cores, it is necessary to have precise chronologies for the ice and gas phases. The aim of this work has been to improve ice cores chronologies, covering the last 800 000 years, through new measurements of the isotopic composition of the air δ15N, δ18Oatm et δO2/N2) trapped in EPICA Dome C (EDC) ice core and the use of the Datice dating tool.The first important result of this PhD has been the production of the Antarctic Ice Core Chronology (AICC2012), common for EDC, Vostok, EPICA Droning Maud Land (EDML), TALos Dome ICE core (TALDICE) and NorthGRIP ice cores. The bipolar see-saw theory is still valid on the new chronology. The AICC2012 chronology gives an age for Termination II in good agreement with other climate archives. Moreover, the duration of interglacial periods is unchanged compared to EDC3. While building the AICC2012 chronology, we have pointed out several limitations. Since then, we have improved Datice in order to correctly integrate constraints deduced from layer counting and their associated uncertainties. These improvements permit to build coherent chronologies respecting the underlying hypotheses of Datice. Moreover, we propose a new parameterization of the uncertainty associated with the background thinning function based on ice mechanical properties of EDC ice core. Finally, we were able to deduce new age constraints thanks to the new measurements of δO2/N2 and δ18Oatm performed on well-conserved ice from EDC. A multi-proxy comparison of Vostok, EDC and Dome F ice cores over MIS 5 has highlighted a possible influence of local climatic parameters on δO2/N2. The analysis of the delay between δ18Oatm and precession shows some variability over the last 800 ka. We propose that the delay between δ18Oatm and precession is increased during periods associated with Heinrich events. The results obtained during this PhD should be used for the next ice core coherent chronology. Afin d’étudier les variations climatiques enregistrées par les ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctique* EPICA Greenland Greenland ice cores Groenland ice core Institut national des sciences de l'Univers: HAL-INSU