"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years
International audience A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC) through a stratigraphic match between EDML and EDC that consists of 322 volca...
Main Authors: | , , , , , , , , , , , , , , , , , , , |
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Other Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2007
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Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-00330760 https://hal.archives-ouvertes.fr/hal-00330760/document https://hal.archives-ouvertes.fr/hal-00330760/file/cp-3-475-2007.pdf |
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ftccsdartic:oai:HAL:hal-00330760v1 |
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openpolar |
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Open Polar |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Ruth, U. Barnola, J.-M. Beer, J. Bigler, M. Blunier, T. Castellano, E. Fischer, H. Fundel, F. Huybrechts, P. Kaufmann, P. Kipfstuhl, S. Lambrecht, A. Morganti, A. Oerter, H. Parrenin, F. Rybak, O. Severi, M. Udisti, R. Wilhelms, F. Wolff, E. "EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years |
topic_facet |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC) through a stratigraphic match between EDML and EDC that consists of 322 volcanic match points over the last 128 ka. The EDC3 chronology comprises a glaciological model at EDC, which is constrained and later selectively tuned using primary dating information from EDC as well as from EDML, the latter being transferred using the tight stratigraphic link between the two cores. Finally, EDML1 was built by exporting EDC3 to EDML. For ages younger than 41 ka BP the new synchronized time scale EDML1/EDC3 is based on dated volcanic events and on a match to the Greenlandic ice core chronology GICC05 via 10 Be and methane. The internal consistency between EDML1 and EDC3 is estimated to be typically ~6 years and always less than 450 years over the last 128 ka (always less than 130 years over the last 60 ka), which reflects an unprecedented synchrony of time scales. EDML1 ends at 150 ka BP (2417 m depth) because the match between EDML and EDC becomes ambiguous further down. This hints at a complex ice flow history for the deepest 350 m of the EDML ice core. |
author2 |
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Swiss Federal Institute of Aquatic Science and Technology Swiss Federal institute of aquatic science and technology Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern Bern -Universität Bern Bern Ice and Climate Research Department of Chemistry Departement Geografie British Antarctic Survey (BAS) Natural Environment Research Council (NERC) |
format |
Article in Journal/Newspaper |
author |
Ruth, U. Barnola, J.-M. Beer, J. Bigler, M. Blunier, T. Castellano, E. Fischer, H. Fundel, F. Huybrechts, P. Kaufmann, P. Kipfstuhl, S. Lambrecht, A. Morganti, A. Oerter, H. Parrenin, F. Rybak, O. Severi, M. Udisti, R. Wilhelms, F. Wolff, E. |
author_facet |
Ruth, U. Barnola, J.-M. Beer, J. Bigler, M. Blunier, T. Castellano, E. Fischer, H. Fundel, F. Huybrechts, P. Kaufmann, P. Kipfstuhl, S. Lambrecht, A. Morganti, A. Oerter, H. Parrenin, F. Rybak, O. Severi, M. Udisti, R. Wilhelms, F. Wolff, E. |
author_sort |
Ruth, U. |
title |
"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years |
title_short |
"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years |
title_full |
"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years |
title_fullStr |
"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years |
title_full_unstemmed |
"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years |
title_sort |
"edml1": a chronology for the epica deep ice core from dronning maud land, antarctica, over the last 150 000 years |
publisher |
HAL CCSD |
publishDate |
2007 |
url |
https://hal.archives-ouvertes.fr/hal-00330760 https://hal.archives-ouvertes.fr/hal-00330760/document https://hal.archives-ouvertes.fr/hal-00330760/file/cp-3-475-2007.pdf |
geographic |
Dronning Maud Land |
geographic_facet |
Dronning Maud Land |
genre |
Antarc* Antarctica Dronning Maud Land EPICA greenlandic ice core |
genre_facet |
Antarc* Antarctica Dronning Maud Land EPICA greenlandic ice core |
op_source |
ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.archives-ouvertes.fr/hal-00330760 Climate of the Past, European Geosciences Union (EGU), 2007, 3 (3), pp.475-484 |
op_relation |
hal-00330760 https://hal.archives-ouvertes.fr/hal-00330760 https://hal.archives-ouvertes.fr/hal-00330760/document https://hal.archives-ouvertes.fr/hal-00330760/file/cp-3-475-2007.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1766255324244738048 |
spelling |
ftccsdartic:oai:HAL:hal-00330760v1 2023-05-15T13:51:27+02:00 "EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years Ruth, U. Barnola, J.-M. Beer, J. Bigler, M. Blunier, T. Castellano, E. Fischer, H. Fundel, F. Huybrechts, P. Kaufmann, P. Kipfstuhl, S. Lambrecht, A. Morganti, A. Oerter, H. Parrenin, F. Rybak, O. Severi, M. Udisti, R. Wilhelms, F. Wolff, E. Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Swiss Federal Institute of Aquatic Science and Technology Swiss Federal institute of aquatic science and technology Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern Bern -Universität Bern Bern Ice and Climate Research Department of Chemistry Departement Geografie British Antarctic Survey (BAS) Natural Environment Research Council (NERC) 2007-08-07 https://hal.archives-ouvertes.fr/hal-00330760 https://hal.archives-ouvertes.fr/hal-00330760/document https://hal.archives-ouvertes.fr/hal-00330760/file/cp-3-475-2007.pdf en eng HAL CCSD European Geosciences Union (EGU) hal-00330760 https://hal.archives-ouvertes.fr/hal-00330760 https://hal.archives-ouvertes.fr/hal-00330760/document https://hal.archives-ouvertes.fr/hal-00330760/file/cp-3-475-2007.pdf info:eu-repo/semantics/OpenAccess ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.archives-ouvertes.fr/hal-00330760 Climate of the Past, European Geosciences Union (EGU), 2007, 3 (3), pp.475-484 [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2007 ftccsdartic 2021-10-24T20:40:56Z International audience A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice core from Dome-C (EDC) through a stratigraphic match between EDML and EDC that consists of 322 volcanic match points over the last 128 ka. The EDC3 chronology comprises a glaciological model at EDC, which is constrained and later selectively tuned using primary dating information from EDC as well as from EDML, the latter being transferred using the tight stratigraphic link between the two cores. Finally, EDML1 was built by exporting EDC3 to EDML. For ages younger than 41 ka BP the new synchronized time scale EDML1/EDC3 is based on dated volcanic events and on a match to the Greenlandic ice core chronology GICC05 via 10 Be and methane. The internal consistency between EDML1 and EDC3 is estimated to be typically ~6 years and always less than 450 years over the last 128 ka (always less than 130 years over the last 60 ka), which reflects an unprecedented synchrony of time scales. EDML1 ends at 150 ka BP (2417 m depth) because the match between EDML and EDC becomes ambiguous further down. This hints at a complex ice flow history for the deepest 350 m of the EDML ice core. Article in Journal/Newspaper Antarc* Antarctica Dronning Maud Land EPICA greenlandic ice core Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Dronning Maud Land |