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), 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), Université de Versailles-Saint Quentin en Yvelines, Amaëlle Landais
Format: Doctoral or Postdoctoral Thesis
Language:French
Published: HAL CCSD 2015
Subjects:
Online Access:https://tel.archives-ouvertes.fr/tel-01245451
https://tel.archives-ouvertes.fr/tel-01245451/document
https://tel.archives-ouvertes.fr/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf
id ftccsdartic:oai:HAL:tel-01245451v1
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 French
topic Air isotopic composition
Greenland
Ice cores
Antarctic
Datation
Orbital tuning
Variations glaciaire-interglaciaires
Glacial-interglacial variations
Synchronisation orbitale
Composition isotopique de l'air
Carottes de glace
Groenland
Antarctique
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle Air isotopic composition
Greenland
Ice cores
Antarctic
Datation
Orbital tuning
Variations glaciaire-interglaciaires
Glacial-interglacial variations
Synchronisation orbitale
Composition isotopique de l'air
Carottes de glace
Groenland
Antarctique
[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 Air isotopic composition
Greenland
Ice cores
Antarctic
Datation
Orbital tuning
Variations glaciaire-interglaciaires
Glacial-interglacial variations
Synchronisation orbitale
Composition isotopique de l'air
Carottes de glace
Groenland
Antarctique
[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)
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)
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://tel.archives-ouvertes.fr/tel-01245451
https://tel.archives-ouvertes.fr/tel-01245451/document
https://tel.archives-ouvertes.fr/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf
long_lat ENVELOPE(39.700,39.700,-77.317,-77.317)
ENVELOPE(158.000,158.000,-73.000,-73.000)
geographic Antarctic
Dome F
Greenland
Talos Dome
The Antarctic
geographic_facet Antarctic
Dome F
Greenland
Talos Dome
The Antarctic
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://tel.archives-ouvertes.fr/tel-01245451
Climatologie. Université de Versailles-Saint Quentin en Yvelines, 2015. Français. ⟨NNT : 2015VERS013V⟩
op_relation NNT: 2015VERS013V
tel-01245451
https://tel.archives-ouvertes.fr/tel-01245451
https://tel.archives-ouvertes.fr/tel-01245451/document
https://tel.archives-ouvertes.fr/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf
op_rights info:eu-repo/semantics/OpenAccess
_version_ 1766252310025994240
spelling ftccsdartic:oai:HAL:tel-01245451v1 2023-05-15T13:49:48+02:00 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) 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) Université de Versailles-Saint Quentin en Yvelines Amaëlle Landais 2015-01-29 https://tel.archives-ouvertes.fr/tel-01245451 https://tel.archives-ouvertes.fr/tel-01245451/document https://tel.archives-ouvertes.fr/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf fr fre HAL CCSD NNT: 2015VERS013V tel-01245451 https://tel.archives-ouvertes.fr/tel-01245451 https://tel.archives-ouvertes.fr/tel-01245451/document https://tel.archives-ouvertes.fr/tel-01245451/file/pdf2star-1450194526-2015VERS013V.pdf info:eu-repo/semantics/OpenAccess https://tel.archives-ouvertes.fr/tel-01245451 Climatologie. Université de Versailles-Saint Quentin en Yvelines, 2015. Français. ⟨NNT : 2015VERS013V⟩ Air isotopic composition Greenland Ice cores Antarctic Datation Orbital tuning Variations glaciaire-interglaciaires Glacial-interglacial variations Synchronisation orbitale Composition isotopique de l'air Carottes de glace Groenland Antarctique [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/doctoralThesis Theses 2015 ftccsdartic 2021-12-19T02:49:40Z 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 Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Antarctic Dome F ENVELOPE(39.700,39.700,-77.317,-77.317) Greenland Talos Dome ENVELOPE(158.000,158.000,-73.000,-73.000) The Antarctic