Rare earth elements from the Atlantic Sector ...

We present a Rare Earth Elements (REE) record at decadal resolution determined in the EPICA ice core drilled in Dronning Maud Land (EDML) in the Atlantic Sector of the East Antarctic Plateau, covering the transition from the last glacial age (LGA) to the early Holocene (26 600-7500 yr BP). Additiona...

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Main Authors: Wegner, Anna, Gabrielli, Paolo, Wilhelms-Dick, Dorothee, Ruth, Urs, Kriews, Michael, De Deckker, Patrick, Barbante, Carlo, Cozzi, Giulio, Delmonte, Barbara, Fischer, Hubertus
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.756834
https://doi.pangaea.de/10.1594/PANGAEA.756834
id ftdatacite:10.1594/pangaea.756834
record_format openpolar
spelling ftdatacite:10.1594/pangaea.756834 2024-09-15T17:47:17+00:00 Rare earth elements from the Atlantic Sector ... Wegner, Anna Gabrielli, Paolo Wilhelms-Dick, Dorothee Ruth, Urs Kriews, Michael De Deckker, Patrick Barbante, Carlo Cozzi, Giulio Delmonte, Barbara Fischer, Hubertus 2012 application/zip https://dx.doi.org/10.1594/pangaea.756834 https://doi.pangaea.de/10.1594/PANGAEA.756834 en eng PANGAEA https://dx.doi.org/10.5194/cp-8-135-2012 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 EPICA drill EPICA-Campaigns Kohnen Station European Project for Ice Coring in Antarctica EPICA article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.75683410.5194/cp-8-135-2012 2024-08-01T10:52:43Z We present a Rare Earth Elements (REE) record at decadal resolution determined in the EPICA ice core drilled in Dronning Maud Land (EDML) in the Atlantic Sector of the East Antarctic Plateau, covering the transition from the last glacial age (LGA) to the early Holocene (26 600-7500 yr BP). Additionally, samples from potential source areas (PSAs) for Antarctic dust were analysed for their REE characteristics. The dust provenance is discussed by comparing the REE fingerprints in the ice core and the PSAs samples. We find a shift in REE composition at 15 200 yr BP in the ice core samples. Before 15 200 yr BP, the dust composition is very uniform and its provenance was likely to be dominated by a South American source. After 15 200 yr BP, multiple sources such as Australia and New Zealand become relatively more important, albeit South America is possibly still an important dust supplier. A similar change in the dust characteristics was observed in the EPICA Dome C ice core at around ~15 000 yr BP. A return to ... : Supplement to: Wegner, Anna; Gabrielli, Paolo; Wilhelms-Dick, Dorothee; Ruth, Urs; Kriews, Michael; De Deckker, Patrick; Barbante, Carlo; Cozzi, Giulio; Delmonte, Barbara; Fischer, H (2012): Change in dust variability in the Atlantic sector of Antarctica at the end of the last deglaciation. Climate of the Past, 8(1), 135-147 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Dronning Maud Land EPICA ice core DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic EPICA drill
EPICA-Campaigns
Kohnen Station
European Project for Ice Coring in Antarctica EPICA
spellingShingle EPICA drill
EPICA-Campaigns
Kohnen Station
European Project for Ice Coring in Antarctica EPICA
Wegner, Anna
Gabrielli, Paolo
Wilhelms-Dick, Dorothee
Ruth, Urs
Kriews, Michael
De Deckker, Patrick
Barbante, Carlo
Cozzi, Giulio
Delmonte, Barbara
Fischer, Hubertus
Rare earth elements from the Atlantic Sector ...
topic_facet EPICA drill
EPICA-Campaigns
Kohnen Station
European Project for Ice Coring in Antarctica EPICA
description We present a Rare Earth Elements (REE) record at decadal resolution determined in the EPICA ice core drilled in Dronning Maud Land (EDML) in the Atlantic Sector of the East Antarctic Plateau, covering the transition from the last glacial age (LGA) to the early Holocene (26 600-7500 yr BP). Additionally, samples from potential source areas (PSAs) for Antarctic dust were analysed for their REE characteristics. The dust provenance is discussed by comparing the REE fingerprints in the ice core and the PSAs samples. We find a shift in REE composition at 15 200 yr BP in the ice core samples. Before 15 200 yr BP, the dust composition is very uniform and its provenance was likely to be dominated by a South American source. After 15 200 yr BP, multiple sources such as Australia and New Zealand become relatively more important, albeit South America is possibly still an important dust supplier. A similar change in the dust characteristics was observed in the EPICA Dome C ice core at around ~15 000 yr BP. A return to ... : Supplement to: Wegner, Anna; Gabrielli, Paolo; Wilhelms-Dick, Dorothee; Ruth, Urs; Kriews, Michael; De Deckker, Patrick; Barbante, Carlo; Cozzi, Giulio; Delmonte, Barbara; Fischer, H (2012): Change in dust variability in the Atlantic sector of Antarctica at the end of the last deglaciation. Climate of the Past, 8(1), 135-147 ...
format Article in Journal/Newspaper
author Wegner, Anna
Gabrielli, Paolo
Wilhelms-Dick, Dorothee
Ruth, Urs
Kriews, Michael
De Deckker, Patrick
Barbante, Carlo
Cozzi, Giulio
Delmonte, Barbara
Fischer, Hubertus
author_facet Wegner, Anna
Gabrielli, Paolo
Wilhelms-Dick, Dorothee
Ruth, Urs
Kriews, Michael
De Deckker, Patrick
Barbante, Carlo
Cozzi, Giulio
Delmonte, Barbara
Fischer, Hubertus
author_sort Wegner, Anna
title Rare earth elements from the Atlantic Sector ...
title_short Rare earth elements from the Atlantic Sector ...
title_full Rare earth elements from the Atlantic Sector ...
title_fullStr Rare earth elements from the Atlantic Sector ...
title_full_unstemmed Rare earth elements from the Atlantic Sector ...
title_sort rare earth elements from the atlantic sector ...
publisher PANGAEA
publishDate 2012
url https://dx.doi.org/10.1594/pangaea.756834
https://doi.pangaea.de/10.1594/PANGAEA.756834
genre Antarc*
Antarctic
Antarctica
Dronning Maud Land
EPICA
ice core
genre_facet Antarc*
Antarctic
Antarctica
Dronning Maud Land
EPICA
ice core
op_relation https://dx.doi.org/10.5194/cp-8-135-2012
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.75683410.5194/cp-8-135-2012
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