Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication]
International audience Li, V, Cr, Mn, Co, As, Rb, Sr, Ba, Bi and U were determined by inductively coupled plasma sector field mass spectrometry (ICP-SFMS) in various sections of the 3623 m Vostok deep Antarctic ice core dated from 4600 to 410,000 years BP, which corresponds to the last four climatic...
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ftunivnantes:oai:HAL:insu-00562246v1 2023-05-15T13:58:17+02:00 Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication] Gabrielli, Paolo Planchon, Frédéric Hong, Sungmin Lee, Khang Hyun Hur, Soon Do Barbante, Carlo Ferrari, Christophe P. Petit, Jean Robert Lipenkov, Vladimir Y. Cescon, Paolo Boutron, Claude F. 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 University of Ca’ Foscari Venice, Italy Korea Polar Research Institute (KOPRI) Environmental Sciences Department Polytech Grenoble (Institut Universitaire de France) Université Joseph Fourier - Grenoble 1 (UJF) Arctic and Antarctic Research Institute (AARI) Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet) ENEA the Institut Universitaire de France 2005-05 https://hal-insu.archives-ouvertes.fr/insu-00562246 https://doi.org/10.1016/J.EPSL.2005.03.001 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/J.EPSL.2005.03.001 insu-00562246 https://hal-insu.archives-ouvertes.fr/insu-00562246 BIBCODE: 2005E&PSL.234.249G doi:10.1016/J.EPSL.2005.03.001 ISSN: 0012-821X Earth and Planetary Science Letters https://hal-insu.archives-ouvertes.fr/insu-00562246 Earth and Planetary Science Letters, 2005, 234, pp.249-259. ⟨10.1016/J.EPSL.2005.03.001⟩ Vostok trace elements ice climate [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2005 ftunivnantes https://doi.org/10.1016/J.EPSL.2005.03.001 2023-03-01T00:30:58Z International audience Li, V, Cr, Mn, Co, As, Rb, Sr, Ba, Bi and U were determined by inductively coupled plasma sector field mass spectrometry (ICP-SFMS) in various sections of the 3623 m Vostok deep Antarctic ice core dated from 4600 to 410,000 years BP, which corresponds to the last four climatic cycles back to isotopic stage 11.3. Concentrations of all elements were found to be highly variable with low values during interglacial periods and warm interstadials and much higher values during the coldest periods of the last four ice ages. Crustal enrichment factors suggest various sources for the different elements. Rock and soil dust is the dominant source of V, Mn, Rb, Ba and U whatever the period, and of Li, Cr, Co, Sr and As during cold periods. Sea salt aerosol, together with aeolian dust, also contributes significantly to Sr whereas volcanic emissions could provide a significant input for As and Bi especially during warm periods. Article in Journal/Newspaper Antarc* Antarctic ice core Université de Nantes: HAL-UNIV-NANTES Antarctic Earth and Planetary Science Letters 234 1-2 249 259 |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
Vostok trace elements ice climate [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
spellingShingle |
Vostok trace elements ice climate [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology Gabrielli, Paolo Planchon, Frédéric Hong, Sungmin Lee, Khang Hyun Hur, Soon Do Barbante, Carlo Ferrari, Christophe P. Petit, Jean Robert Lipenkov, Vladimir Y. Cescon, Paolo Boutron, Claude F. Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication] |
topic_facet |
Vostok trace elements ice climate [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
description |
International audience Li, V, Cr, Mn, Co, As, Rb, Sr, Ba, Bi and U were determined by inductively coupled plasma sector field mass spectrometry (ICP-SFMS) in various sections of the 3623 m Vostok deep Antarctic ice core dated from 4600 to 410,000 years BP, which corresponds to the last four climatic cycles back to isotopic stage 11.3. Concentrations of all elements were found to be highly variable with low values during interglacial periods and warm interstadials and much higher values during the coldest periods of the last four ice ages. Crustal enrichment factors suggest various sources for the different elements. Rock and soil dust is the dominant source of V, Mn, Rb, Ba and U whatever the period, and of Li, Cr, Co, Sr and As during cold periods. Sea salt aerosol, together with aeolian dust, also contributes significantly to Sr whereas volcanic emissions could provide a significant input for As and Bi especially during warm periods. |
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) Institute for the Dynamics of Environmental Processes-CNR University of Ca’ Foscari Venice, Italy Korea Polar Research Institute (KOPRI) Environmental Sciences Department Polytech Grenoble (Institut Universitaire de France) Université Joseph Fourier - Grenoble 1 (UJF) Arctic and Antarctic Research Institute (AARI) Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet) ENEA the Institut Universitaire de France |
format |
Article in Journal/Newspaper |
author |
Gabrielli, Paolo Planchon, Frédéric Hong, Sungmin Lee, Khang Hyun Hur, Soon Do Barbante, Carlo Ferrari, Christophe P. Petit, Jean Robert Lipenkov, Vladimir Y. Cescon, Paolo Boutron, Claude F. |
author_facet |
Gabrielli, Paolo Planchon, Frédéric Hong, Sungmin Lee, Khang Hyun Hur, Soon Do Barbante, Carlo Ferrari, Christophe P. Petit, Jean Robert Lipenkov, Vladimir Y. Cescon, Paolo Boutron, Claude F. |
author_sort |
Gabrielli, Paolo |
title |
Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication] |
title_short |
Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication] |
title_full |
Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication] |
title_fullStr |
Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication] |
title_full_unstemmed |
Trace elements in Vostok Antarctic ice during the last four climatic cycles [rapid communication] |
title_sort |
trace elements in vostok antarctic ice during the last four climatic cycles [rapid communication] |
publisher |
HAL CCSD |
publishDate |
2005 |
url |
https://hal-insu.archives-ouvertes.fr/insu-00562246 https://doi.org/10.1016/J.EPSL.2005.03.001 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic ice core |
genre_facet |
Antarc* Antarctic ice core |
op_source |
ISSN: 0012-821X Earth and Planetary Science Letters https://hal-insu.archives-ouvertes.fr/insu-00562246 Earth and Planetary Science Letters, 2005, 234, pp.249-259. ⟨10.1016/J.EPSL.2005.03.001⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/J.EPSL.2005.03.001 insu-00562246 https://hal-insu.archives-ouvertes.fr/insu-00562246 BIBCODE: 2005E&PSL.234.249G doi:10.1016/J.EPSL.2005.03.001 |
op_doi |
https://doi.org/10.1016/J.EPSL.2005.03.001 |
container_title |
Earth and Planetary Science Letters |
container_volume |
234 |
container_issue |
1-2 |
container_start_page |
249 |
op_container_end_page |
259 |
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1766266527976259584 |