Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area

International audience We present here the results of the analysis of 22 elements or compounds in a large block of prehistoric blue ice more than 12000 years old collected at a coastal ablation area in east Antarctica. Successive veneer layers chiselled in sequence from the exterior to the center ha...

Full description

Bibliographic Details
Published in:Atmospheric Environment (1967)
Main Authors: Boutron, Claude, Leclerc, Michel, Risler, Nicolas
Other Authors: 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), Centre des Faibles Radioactivités (CFR), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 1984
Subjects:
Online Access:https://hal.science/hal-03516176
https://doi.org/10.1016/0004-6981(84)90372-X
_version_ 1821770819709173760
author Boutron, Claude
Leclerc, Michel
Risler, Nicolas
author2 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)
Centre des Faibles Radioactivités (CFR)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS)
author_facet Boutron, Claude
Leclerc, Michel
Risler, Nicolas
author_sort Boutron, Claude
collection Université Grenoble Alpes: HAL
container_issue 9
container_start_page 1947
container_title Atmospheric Environment (1967)
container_volume 18
description International audience We present here the results of the analysis of 22 elements or compounds in a large block of prehistoric blue ice more than 12000 years old collected at a coastal ablation area in east Antarctica. Successive veneer layers chiselled in sequence from the exterior to the center have been analysed separately in order to determine the contamination characteristics of the block.Concentrations measured in the central parts probably represent the original concentrations in the prehistoric blue ice, thus giving estimates of pre-man natural reference, levels of these elements or compounds in Antarctic precipitations. For the enriched elements Cd, Cu, Zn, Au, Se and for SO4, concentrations are shown not to differ significantly from those presently observed in surface snow in the central plateau areas from which the ice is thought to originate. This suggests that the remote polar regions of the southern hemisphere are still little affected by global pollution for these elements and for S compounds. For crustal derived elements, concentrations in prehistoric ice are found to be significantly higher than those in present day snow; this confirms that crustal flux to the Antarctic continent was higher during Wisconsin times than now.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctica
East Antarctica
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
geographic Antarctic
The Antarctic
East Antarctica
geographic_facet Antarctic
The Antarctic
East Antarctica
id ftunigrenoble:oai:HAL:hal-03516176v1
institution Open Polar
language English
op_collection_id ftunigrenoble
op_container_end_page 1953
op_doi https://doi.org/10.1016/0004-6981(84)90372-X
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/0004-6981(84)90372-X
op_source ISSN: 0004-6981
Atmospheric environment
https://hal.science/hal-03516176
Atmospheric environment, 1984, 18 (9), pp.1947-1953. ⟨10.1016/0004-6981(84)90372-X⟩
publishDate 1984
publisher HAL CCSD
record_format openpolar
spelling ftunigrenoble:oai:HAL:hal-03516176v1 2025-01-16T19:37:43+00:00 Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area Boutron, Claude Leclerc, Michel Risler, Nicolas 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) Centre des Faibles Radioactivités (CFR) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS) 1984-01 https://hal.science/hal-03516176 https://doi.org/10.1016/0004-6981(84)90372-X en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/0004-6981(84)90372-X ISSN: 0004-6981 Atmospheric environment https://hal.science/hal-03516176 Atmospheric environment, 1984, 18 (9), pp.1947-1953. ⟨10.1016/0004-6981(84)90372-X⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 1984 ftunigrenoble https://doi.org/10.1016/0004-6981(84)90372-X 2024-12-03T02:09:44Z International audience We present here the results of the analysis of 22 elements or compounds in a large block of prehistoric blue ice more than 12000 years old collected at a coastal ablation area in east Antarctica. Successive veneer layers chiselled in sequence from the exterior to the center have been analysed separately in order to determine the contamination characteristics of the block.Concentrations measured in the central parts probably represent the original concentrations in the prehistoric blue ice, thus giving estimates of pre-man natural reference, levels of these elements or compounds in Antarctic precipitations. For the enriched elements Cd, Cu, Zn, Au, Se and for SO4, concentrations are shown not to differ significantly from those presently observed in surface snow in the central plateau areas from which the ice is thought to originate. This suggests that the remote polar regions of the southern hemisphere are still little affected by global pollution for these elements and for S compounds. For crustal derived elements, concentrations in prehistoric ice are found to be significantly higher than those in present day snow; this confirms that crustal flux to the Antarctic continent was higher during Wisconsin times than now. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Université Grenoble Alpes: HAL Antarctic The Antarctic East Antarctica Atmospheric Environment (1967) 18 9 1947 1953
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Boutron, Claude
Leclerc, Michel
Risler, Nicolas
Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area
title Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area
title_full Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area
title_fullStr Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area
title_full_unstemmed Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area
title_short Atmospheric trace elements in Antarctic prehistoric ice collected at a coastal ablation area
title_sort atmospheric trace elements in antarctic prehistoric ice collected at a coastal ablation area
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
url https://hal.science/hal-03516176
https://doi.org/10.1016/0004-6981(84)90372-X