Towards radiocarbon dating of ice cores

Instruments and Methods International audience A recently developed dating method for glacier ice, based on the analysis of radiocarbon in carbonaceous aerosol particles, is thoroughly investigated. We discuss the potential of this method to achieve a reliable dating using examples from a mid- and a...

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Published in:Journal of Glaciology
Main Authors: Sigl, M., Jenk, T. M., Kellerhals, T., Szidat, S., Gäggeler, H. W., Wacker, L., Synal, H.-A., Boutron, Claude, F., Barbante, C., Gabrieli, J., Schwikowski, M.
Other Authors: Paul Scherrer Institute (PSI), Department of Chemistry and Biochemistry, Universität Bern = University of Bern = Université de Berne (UNIBE), Oeschger Centre for Climate Change Research (OCCR), 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), Ion Beam Physics, ETH Hönggerberg, 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), Institute for the Dynamics of Environmental Processes-CNR, Environmental Sciences Department, University of Ca’ Foscari Venice, Italy, Supported by the National Centre of Competence in Research (NCCR) climate programme of the Swiss National Science Foundation (projects VITA and VIVALDI), the European Union Framework Programme 6 (FP6) project MILLENNIUM (017008) and the Istituto Nazionale per la Ricerca Scientifica e Tecnolo`gica sulla Montagna (INRM).
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2009
Subjects:
Online Access:https://insu.hal.science/insu-00498241
https://insu.hal.science/insu-00498241/document
https://insu.hal.science/insu-00498241/file/towards-radiocarbon-dating-of-ice-cores.pdf
https://doi.org/10.3189/002214309790794922
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record_format openpolar
institution Open Polar
collection Université Grenoble Alpes: HAL
op_collection_id ftunigrenoble
language English
topic [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
spellingShingle [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
Sigl, M.
Jenk, T. M.
Kellerhals, T.
Szidat, S.
Gäggeler, H. W.
Wacker, L.
Synal, H.-A.
Boutron, Claude, F.
Barbante, C.
Gabrieli, J.
Schwikowski, M.
Towards radiocarbon dating of ice cores
topic_facet [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
description Instruments and Methods International audience A recently developed dating method for glacier ice, based on the analysis of radiocarbon in carbonaceous aerosol particles, is thoroughly investigated. We discuss the potential of this method to achieve a reliable dating using examples from a mid- and a low-latitude ice core. Two series of samples from Colle Gnifetti (4450 m a.s.l., Swiss Alps) and Nevado Illimani (6300 m a.s.l., Bolivian Andes) demonstrate that the 14C ages deduced from the water-insoluble organic carbon fraction represent the age of the ice. Sample sizes ranged between 7 and 100 μg carbon. For validation we compare our results with those from independent dating. This new method is thought to have major implications for dating non-polar ice cores in the future, as it provides complementary age information for time periods not accessible with common dating techniques.
author2 Paul Scherrer Institute (PSI)
Department of Chemistry and Biochemistry
Universität Bern = University of Bern = Université de Berne (UNIBE)
Oeschger Centre for Climate Change Research (OCCR)
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)
Ion Beam Physics
ETH Hönggerberg
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)
Institute for the Dynamics of Environmental Processes-CNR
Environmental Sciences Department
University of Ca’ Foscari Venice, Italy
Supported by the National Centre of Competence in Research (NCCR) climate programme of the Swiss National Science Foundation (projects VITA and VIVALDI), the European Union Framework Programme 6 (FP6) project MILLENNIUM (017008) and the Istituto Nazionale per la Ricerca Scientifica e Tecnolo`gica sulla Montagna (INRM).
format Article in Journal/Newspaper
author Sigl, M.
Jenk, T. M.
Kellerhals, T.
Szidat, S.
Gäggeler, H. W.
Wacker, L.
Synal, H.-A.
Boutron, Claude, F.
Barbante, C.
Gabrieli, J.
Schwikowski, M.
author_facet Sigl, M.
Jenk, T. M.
Kellerhals, T.
Szidat, S.
Gäggeler, H. W.
Wacker, L.
Synal, H.-A.
Boutron, Claude, F.
Barbante, C.
Gabrieli, J.
Schwikowski, M.
author_sort Sigl, M.
title Towards radiocarbon dating of ice cores
title_short Towards radiocarbon dating of ice cores
title_full Towards radiocarbon dating of ice cores
title_fullStr Towards radiocarbon dating of ice cores
title_full_unstemmed Towards radiocarbon dating of ice cores
title_sort towards radiocarbon dating of ice cores
publisher HAL CCSD
publishDate 2009
url https://insu.hal.science/insu-00498241
https://insu.hal.science/insu-00498241/document
https://insu.hal.science/insu-00498241/file/towards-radiocarbon-dating-of-ice-cores.pdf
https://doi.org/10.3189/002214309790794922
genre ice core
Journal of Glaciology
genre_facet ice core
Journal of Glaciology
op_source ISSN: 0022-1430
EISSN: 1727-5652
Journal of Glaciology
https://insu.hal.science/insu-00498241
Journal of Glaciology, 2009, 55 (194), pp.985-996. ⟨10.3189/002214309790794922⟩
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https://insu.hal.science/insu-00498241
https://insu.hal.science/insu-00498241/document
https://insu.hal.science/insu-00498241/file/towards-radiocarbon-dating-of-ice-cores.pdf
doi:10.3189/002214309790794922
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container_title Journal of Glaciology
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spelling ftunigrenoble:oai:HAL:insu-00498241v1 2024-09-09T19:44:54+00:00 Towards radiocarbon dating of ice cores Sigl, M. Jenk, T. M. Kellerhals, T. Szidat, S. Gäggeler, H. W. Wacker, L. Synal, H.-A. Boutron, Claude, F. Barbante, C. Gabrieli, J. Schwikowski, M. Paul Scherrer Institute (PSI) Department of Chemistry and Biochemistry Universität Bern = University of Bern = Université de Berne (UNIBE) Oeschger Centre for Climate Change Research (OCCR) 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) Ion Beam Physics ETH Hönggerberg 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) Institute for the Dynamics of Environmental Processes-CNR Environmental Sciences Department University of Ca’ Foscari Venice, Italy Supported by the National Centre of Competence in Research (NCCR) climate programme of the Swiss National Science Foundation (projects VITA and VIVALDI), the European Union Framework Programme 6 (FP6) project MILLENNIUM (017008) and the Istituto Nazionale per la Ricerca Scientifica e Tecnolo`gica sulla Montagna (INRM). 2009 https://insu.hal.science/insu-00498241 https://insu.hal.science/insu-00498241/document https://insu.hal.science/insu-00498241/file/towards-radiocarbon-dating-of-ice-cores.pdf https://doi.org/10.3189/002214309790794922 en eng HAL CCSD International Glaciological Society info:eu-repo/semantics/altIdentifier/doi/10.3189/002214309790794922 insu-00498241 https://insu.hal.science/insu-00498241 https://insu.hal.science/insu-00498241/document https://insu.hal.science/insu-00498241/file/towards-radiocarbon-dating-of-ice-cores.pdf doi:10.3189/002214309790794922 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0022-1430 EISSN: 1727-5652 Journal of Glaciology https://insu.hal.science/insu-00498241 Journal of Glaciology, 2009, 55 (194), pp.985-996. ⟨10.3189/002214309790794922⟩ [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2009 ftunigrenoble https://doi.org/10.3189/002214309790794922 2024-07-29T23:39:57Z Instruments and Methods International audience A recently developed dating method for glacier ice, based on the analysis of radiocarbon in carbonaceous aerosol particles, is thoroughly investigated. We discuss the potential of this method to achieve a reliable dating using examples from a mid- and a low-latitude ice core. Two series of samples from Colle Gnifetti (4450 m a.s.l., Swiss Alps) and Nevado Illimani (6300 m a.s.l., Bolivian Andes) demonstrate that the 14C ages deduced from the water-insoluble organic carbon fraction represent the age of the ice. Sample sizes ranged between 7 and 100 μg carbon. For validation we compare our results with those from independent dating. This new method is thought to have major implications for dating non-polar ice cores in the future, as it provides complementary age information for time periods not accessible with common dating techniques. Article in Journal/Newspaper ice core Journal of Glaciology Université Grenoble Alpes: HAL Journal of Glaciology 55 194 985 996