"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 volc...

Full description

Bibliographic Details
Main Authors: 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.
Other Authors: 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
Language:English
Published: HAL CCSD 2007
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00330729
https://hal.archives-ouvertes.fr/hal-00330729/document
https://hal.archives-ouvertes.fr/hal-00330729/file/cpd-3-549-2007.pdf
id ftccsdartic:oai:HAL:hal-00330729v1
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 [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 EDML1/EDC3 is based on dated volcanic events and on a match to the Greenlandic GICC05 time scale 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 to a complex ice flow history for the deepest 350 m of the EDML ice core, which amongst other reasons may be caused by spatial variations of the geothermal heat flux.
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-00330729
https://hal.archives-ouvertes.fr/hal-00330729/document
https://hal.archives-ouvertes.fr/hal-00330729/file/cpd-3-549-2007.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: 1814-9340
EISSN: 1814-9359
Climate of the Past Discussions
https://hal.archives-ouvertes.fr/hal-00330729
Climate of the Past Discussions, European Geosciences Union (EGU), 2007, 3 (2), pp.549-574
op_relation hal-00330729
https://hal.archives-ouvertes.fr/hal-00330729
https://hal.archives-ouvertes.fr/hal-00330729/document
https://hal.archives-ouvertes.fr/hal-00330729/file/cpd-3-549-2007.pdf
op_rights info:eu-repo/semantics/OpenAccess
_version_ 1766255324654731264
spelling ftccsdartic:oai:HAL:hal-00330729v1 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) 2007-03-12 https://hal.archives-ouvertes.fr/hal-00330729 https://hal.archives-ouvertes.fr/hal-00330729/document https://hal.archives-ouvertes.fr/hal-00330729/file/cpd-3-549-2007.pdf en eng HAL CCSD European Geosciences Union (EGU) hal-00330729 https://hal.archives-ouvertes.fr/hal-00330729 https://hal.archives-ouvertes.fr/hal-00330729/document https://hal.archives-ouvertes.fr/hal-00330729/file/cpd-3-549-2007.pdf info:eu-repo/semantics/OpenAccess ISSN: 1814-9340 EISSN: 1814-9359 Climate of the Past Discussions https://hal.archives-ouvertes.fr/hal-00330729 Climate of the Past Discussions, European Geosciences Union (EGU), 2007, 3 (2), pp.549-574 [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 2021-10-24T20:41:12Z 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 EDML1/EDC3 is based on dated volcanic events and on a match to the Greenlandic GICC05 time scale 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 to a complex ice flow history for the deepest 350 m of the EDML ice core, which amongst other reasons may be caused by spatial variations of the geothermal heat flux. 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