A 60 000 year Greenland stratigraphic ice core chronology
International audience The Greenland Ice Core Chronology 2005 (GICC05) is a time scale based on annual layer counting of high-resolution records from Greenland ice cores. Whereas the Holocene part of the time scale is based on various records from the DYE-3, the GRIP, and the NorthGRIP ice cores, th...
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Other Authors: | , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2008
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Online Access: | https://hal.science/hal-00330768 https://hal.science/hal-00330768/document https://hal.science/hal-00330768/file/cp-4-47-2008.pdf |
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ftunivnantes:oai:HAL:hal-00330768v1 |
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Open Polar |
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Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
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 Svensson, A. Andersen, K. K. Bigler, M. Clausen, H. B. Dahl-Jensen, D. Davies, S. M. Johnsen, S. J. Muscheler, R. Parrenin, F. Rasmussen, S. O. Röthlisberger, R. Seierstad, I. Steffensen, J. P. Vinther, B. M. A 60 000 year Greenland stratigraphic ice core chronology |
topic_facet |
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience The Greenland Ice Core Chronology 2005 (GICC05) is a time scale based on annual layer counting of high-resolution records from Greenland ice cores. Whereas the Holocene part of the time scale is based on various records from the DYE-3, the GRIP, and the NorthGRIP ice cores, the glacial part is solely based on NorthGRIP records. Here we present an 18 ka extension of the time scale such that GICC05 continuously covers the past 60 ka. The new section of the time scale places the onset of Greenland Interstadial 12 (GI-12) at 46.9±1.0 ka b2k (before year AD 2000), the North Atlantic Ash Zone II layer in GI-15 at 55.4±1.2 ka b2k, and the onset of GI-17 at 59.4±1.3 ka b2k. The error estimates are derived from the accumulated number of uncertain annual layers. In the 40–60 ka interval, the new time scale has a discrepancy with the Meese-Sowers GISP2 time scale of up to 2.4 ka. Assuming that the Greenland climatic events are synchronous with those seen in the Chinese Hulu Cave speleothem record, GICC05 compares well to the time scale of that record with absolute age differences of less than 800 years throughout the 60 ka period. The new time scale is generally in close agreement with other independently dated records and reference horizons, such as the Laschamp geomagnetic excursion, the French Villars Cave and the Austrian Kleegruben Cave speleothem records, suggesting high accuracy of both event durations and absolute age estimates. |
author2 |
Centre for Ice and Climate Copenhagen Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)-Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) Department of Geography Swansea University GeoBiosphere Science Centre Quaternary Sciences Laboratoire de glaciologie et géophysique de l'environnement (LGGE) 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 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)-Centre National de la Recherche Scientifique (CNRS) British Antarctic Survey (BAS) Natural Environment Research Council (NERC) Climate Research Unit School of Environmental Sciences |
format |
Article in Journal/Newspaper |
author |
Svensson, A. Andersen, K. K. Bigler, M. Clausen, H. B. Dahl-Jensen, D. Davies, S. M. Johnsen, S. J. Muscheler, R. Parrenin, F. Rasmussen, S. O. Röthlisberger, R. Seierstad, I. Steffensen, J. P. Vinther, B. M. |
author_facet |
Svensson, A. Andersen, K. K. Bigler, M. Clausen, H. B. Dahl-Jensen, D. Davies, S. M. Johnsen, S. J. Muscheler, R. Parrenin, F. Rasmussen, S. O. Röthlisberger, R. Seierstad, I. Steffensen, J. P. Vinther, B. M. |
author_sort |
Svensson, A. |
title |
A 60 000 year Greenland stratigraphic ice core chronology |
title_short |
A 60 000 year Greenland stratigraphic ice core chronology |
title_full |
A 60 000 year Greenland stratigraphic ice core chronology |
title_fullStr |
A 60 000 year Greenland stratigraphic ice core chronology |
title_full_unstemmed |
A 60 000 year Greenland stratigraphic ice core chronology |
title_sort |
60 000 year greenland stratigraphic ice core chronology |
publisher |
HAL CCSD |
publishDate |
2008 |
url |
https://hal.science/hal-00330768 https://hal.science/hal-00330768/document https://hal.science/hal-00330768/file/cp-4-47-2008.pdf |
long_lat |
ENVELOPE(8.610,8.610,62.837,62.837) |
geographic |
Greenland Hulu |
geographic_facet |
Greenland Hulu |
genre |
Dye 3 Dye-3 Greenland Greenland ice core Greenland ice cores GRIP ice core North Atlantic |
genre_facet |
Dye 3 Dye-3 Greenland Greenland ice core Greenland ice cores GRIP ice core North Atlantic |
op_source |
ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.science/hal-00330768 Climate of the Past, 2008, 4 (1), pp.47-57 |
op_relation |
hal-00330768 https://hal.science/hal-00330768 https://hal.science/hal-00330768/document https://hal.science/hal-00330768/file/cp-4-47-2008.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1766398730933633024 |
spelling |
ftunivnantes:oai:HAL:hal-00330768v1 2023-05-15T16:03:05+02:00 A 60 000 year Greenland stratigraphic ice core chronology Svensson, A. Andersen, K. K. Bigler, M. Clausen, H. B. Dahl-Jensen, D. Davies, S. M. Johnsen, S. J. Muscheler, R. Parrenin, F. Rasmussen, S. O. Röthlisberger, R. Seierstad, I. Steffensen, J. P. Vinther, B. M. Centre for Ice and Climate Copenhagen Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)-Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) Department of Geography Swansea University GeoBiosphere Science Centre Quaternary Sciences Laboratoire de glaciologie et géophysique de l'environnement (LGGE) 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 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)-Centre National de la Recherche Scientifique (CNRS) British Antarctic Survey (BAS) Natural Environment Research Council (NERC) Climate Research Unit School of Environmental Sciences 2008-03-31 https://hal.science/hal-00330768 https://hal.science/hal-00330768/document https://hal.science/hal-00330768/file/cp-4-47-2008.pdf en eng HAL CCSD European Geosciences Union (EGU) hal-00330768 https://hal.science/hal-00330768 https://hal.science/hal-00330768/document https://hal.science/hal-00330768/file/cp-4-47-2008.pdf info:eu-repo/semantics/OpenAccess ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.science/hal-00330768 Climate of the Past, 2008, 4 (1), pp.47-57 [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 2008 ftunivnantes 2023-02-08T04:16:52Z International audience The Greenland Ice Core Chronology 2005 (GICC05) is a time scale based on annual layer counting of high-resolution records from Greenland ice cores. Whereas the Holocene part of the time scale is based on various records from the DYE-3, the GRIP, and the NorthGRIP ice cores, the glacial part is solely based on NorthGRIP records. Here we present an 18 ka extension of the time scale such that GICC05 continuously covers the past 60 ka. The new section of the time scale places the onset of Greenland Interstadial 12 (GI-12) at 46.9±1.0 ka b2k (before year AD 2000), the North Atlantic Ash Zone II layer in GI-15 at 55.4±1.2 ka b2k, and the onset of GI-17 at 59.4±1.3 ka b2k. The error estimates are derived from the accumulated number of uncertain annual layers. In the 40–60 ka interval, the new time scale has a discrepancy with the Meese-Sowers GISP2 time scale of up to 2.4 ka. Assuming that the Greenland climatic events are synchronous with those seen in the Chinese Hulu Cave speleothem record, GICC05 compares well to the time scale of that record with absolute age differences of less than 800 years throughout the 60 ka period. The new time scale is generally in close agreement with other independently dated records and reference horizons, such as the Laschamp geomagnetic excursion, the French Villars Cave and the Austrian Kleegruben Cave speleothem records, suggesting high accuracy of both event durations and absolute age estimates. Article in Journal/Newspaper Dye 3 Dye-3 Greenland Greenland ice core Greenland ice cores GRIP ice core North Atlantic Université de Nantes: HAL-UNIV-NANTES Greenland Hulu ENVELOPE(8.610,8.610,62.837,62.837) |