δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ...
Deep ice core chronologies have been improved over the past years through the addition of new age constraints. However, dating methods are still associated with large uncertainties for ice cores from the East Antarctic plateau where layer counting is not possible. Indeed, an uncertainty up to 6 ka i...
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ftdatacite:10.1594/pangaea.887327 2024-09-15T17:45:31+00:00 δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ... Extier, Thomas Landais, Amaëlle Bréant, Camille Prié, F Bazin, Lucie Dreyfus, Gabrielle Roche, Didier M Leuenberger, Markus Christian 2018 application/zip https://dx.doi.org/10.1594/pangaea.887327 https://doi.pangaea.de/10.1594/PANGAEA.887327 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2018.02.008 https://dx.doi.org/10.5194/cp-12-729-2016 https://dx.doi.org/10.5194/cp-3-341-2007 https://dx.doi.org/10.1016/j.epsl.2008.07.008 https://dx.doi.org/10.1038/ngeo1985 https://dx.doi.org/10.5194/cp-8-191-2012 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig European Project for Ice Coring in Antarctica EPICA article Collection Supplementary Publication Series of Datasets 2018 ftdatacite https://doi.org/10.1594/pangaea.88732710.1016/j.quascirev.2018.02.00810.5194/cp-12-729-201610.5194/cp-3-341-200710.1016/j.epsl.2008.07.00810.1038/ngeo198510.5194/cp-8-191-2012 2024-08-01T10:56:44Z Deep ice core chronologies have been improved over the past years through the addition of new age constraints. However, dating methods are still associated with large uncertainties for ice cores from the East Antarctic plateau where layer counting is not possible. Indeed, an uncertainty up to 6 ka is associated with AICC2012 chronology of EPICA Dome C (EDC) ice core, which mostly arises from uncertainty on the delay between changes recorded in d18Oatm and in June 21st insolation variations at 65°N used for ice core orbital dating. Consequently, we need to enhance the knowledge of this delay to improve ice core chronologies. We present new high-resolution EDC d18Oatm record (153-374 ka) and dO2/N2 measurements (163-332 ka) performed on well-stored ice to provide continuous records of d18Oatm and dO2/N2 between 100 and 800 ka. The comparison of d18Oatm with the d18Ocalcite from East Asian speleothems shows that both signals present similar orbital and millennial variabilities, which may represent shifts in the ... : Supplement to: Extier, Thomas; Landais, Amaëlle; Bréant, Camille; Prié, F; Bazin, Lucie; Dreyfus, Gabrielle; Roche, Didier M; Leuenberger, Markus Christian (2018): On the use of d18O atm for ice core dating. Quaternary Science Reviews, 185, 244-257 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica EPICA ice core DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig European Project for Ice Coring in Antarctica EPICA |
spellingShingle |
Drilling/drill rig European Project for Ice Coring in Antarctica EPICA Extier, Thomas Landais, Amaëlle Bréant, Camille Prié, F Bazin, Lucie Dreyfus, Gabrielle Roche, Didier M Leuenberger, Markus Christian δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ... |
topic_facet |
Drilling/drill rig European Project for Ice Coring in Antarctica EPICA |
description |
Deep ice core chronologies have been improved over the past years through the addition of new age constraints. However, dating methods are still associated with large uncertainties for ice cores from the East Antarctic plateau where layer counting is not possible. Indeed, an uncertainty up to 6 ka is associated with AICC2012 chronology of EPICA Dome C (EDC) ice core, which mostly arises from uncertainty on the delay between changes recorded in d18Oatm and in June 21st insolation variations at 65°N used for ice core orbital dating. Consequently, we need to enhance the knowledge of this delay to improve ice core chronologies. We present new high-resolution EDC d18Oatm record (153-374 ka) and dO2/N2 measurements (163-332 ka) performed on well-stored ice to provide continuous records of d18Oatm and dO2/N2 between 100 and 800 ka. The comparison of d18Oatm with the d18Ocalcite from East Asian speleothems shows that both signals present similar orbital and millennial variabilities, which may represent shifts in the ... : Supplement to: Extier, Thomas; Landais, Amaëlle; Bréant, Camille; Prié, F; Bazin, Lucie; Dreyfus, Gabrielle; Roche, Didier M; Leuenberger, Markus Christian (2018): On the use of d18O atm for ice core dating. Quaternary Science Reviews, 185, 244-257 ... |
format |
Article in Journal/Newspaper |
author |
Extier, Thomas Landais, Amaëlle Bréant, Camille Prié, F Bazin, Lucie Dreyfus, Gabrielle Roche, Didier M Leuenberger, Markus Christian |
author_facet |
Extier, Thomas Landais, Amaëlle Bréant, Camille Prié, F Bazin, Lucie Dreyfus, Gabrielle Roche, Didier M Leuenberger, Markus Christian |
author_sort |
Extier, Thomas |
title |
δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ... |
title_short |
δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ... |
title_full |
δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ... |
title_fullStr |
δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ... |
title_full_unstemmed |
δ¹⁸Oatm and dO2/N2 records between 100-800 ka from EPICA Dome C ice core on AICC2012 chronology ... |
title_sort |
δ¹⁸oatm and do2/n2 records between 100-800 ka from epica dome c ice core on aicc2012 chronology ... |
publisher |
PANGAEA |
publishDate |
2018 |
url |
https://dx.doi.org/10.1594/pangaea.887327 https://doi.pangaea.de/10.1594/PANGAEA.887327 |
genre |
Antarc* Antarctic Antarctica EPICA ice core |
genre_facet |
Antarc* Antarctic Antarctica EPICA ice core |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2018.02.008 https://dx.doi.org/10.5194/cp-12-729-2016 https://dx.doi.org/10.5194/cp-3-341-2007 https://dx.doi.org/10.1016/j.epsl.2008.07.008 https://dx.doi.org/10.1038/ngeo1985 https://dx.doi.org/10.5194/cp-8-191-2012 |
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.88732710.1016/j.quascirev.2018.02.00810.5194/cp-12-729-201610.5194/cp-3-341-200710.1016/j.epsl.2008.07.00810.1038/ngeo198510.5194/cp-8-191-2012 |
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1810493382696370176 |