CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ...
We present new d13C measurements of atmospheric CO2 covering the last glacial/interglacial cycle, complementing previous records covering Terminations I and II. Most prominent in the new record is a significant depletion in d13C(atm) of 0.5 permil occurring during marine isotope stage (MIS) 4, follo...
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Online Access: | https://dx.doi.org/10.1594/pangaea.859181 https://doi.pangaea.de/10.1594/PANGAEA.859181 |
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ftdatacite:10.1594/pangaea.859181 2024-04-28T08:02:13+00:00 CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... Eggleston, Sarah Schmitt, Jochen Bereiter, Bernhard Schneider, Robert Fischer, Hubertus 2016 application/zip https://dx.doi.org/10.1594/pangaea.859181 https://doi.pangaea.de/10.1594/PANGAEA.859181 en eng PANGAEA https://swisscovery.slsp.ch/discovery/search?query=lds02,contains,(IDSBB)006061992DSV01&tab=41SLSP_NETWORK&search_scope=DN_and_CI&vid=41SLSP_NETWORK:VU1_UNION https://dx.doi.org/10.1002/2015pa002874 https://dx.doi.org/10.5194/cp-9-1715-2013 https://dx.doi.org/10.1073/pnas.1204069109 https://dx.doi.org/10.1016/j.epsl.2010.06.023 https://swisscovery.slsp.ch/discovery/search?query=lds02,contains,(IDSBB)006061992DSV01&tab=41SLSP_NETWORK&search_scope=DN_and_CI&vid=41SLSP_NETWORK:VU1_UNION https://dx.doi.org/10.5194/cp-9-1733-2013 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 European Project for Ice Coring in Antarctica EPICA Talos Dome Ice Core TALDICE article Supplementary Publication Series of Datasets Collection 2016 ftdatacite https://doi.org/10.1594/pangaea.85918110.1002/2015pa00287410.5194/cp-9-1715-201310.1073/pnas.120406910910.1016/j.epsl.2010.06.02310.5194/cp-9-1733-2013 2024-04-02T11:09:43Z We present new d13C measurements of atmospheric CO2 covering the last glacial/interglacial cycle, complementing previous records covering Terminations I and II. Most prominent in the new record is a significant depletion in d13C(atm) of 0.5 permil occurring during marine isotope stage (MIS) 4, followed by an enrichment of the same magnitude at the beginning of MIS 3. Such a significant excursion in the record is otherwise only observed at glacial terminations, suggesting that similar processes were at play, such as changing sea surface temperatures, changes in marine biological export in the Southern Ocean (SO) due to variations in aeolian iron fluxes, changes in the Atlantic meridional overturning circulation, upwelling of deep water in the SO, and long-term trends in terrestrial carbon storage. Based on previous modeling studies, we propose constraints on some of these processes during specific time intervals. The decrease in d13C(atm) at the end of MIS 4 starting approximately 64 kyr B.P. was accompanied ... : These data complement previously published d13CO2 datasets: * Schmitt, J et al. (2012): Measurements of stable carbon isotope ratios of CO2 over the last 24000 years and CO2 concentration measurements on Antarctic ice cores using three different methods. doi:10.1594/PANGAEA.772713. * Schneider, R et al. (2013): A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the glacial inception. doi:10.1594/PANGAEA.817041. The CO2 concentration and stable isotope data were measured on the following three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950: European Project for Ice Coring in Antarctica (EPICA) Dome C (EDC) (lat = -75.10, lon = 123.40) EPICA Dronning Maud Land (EDML) (lat = -75.00, lon = 0.07) Talos Dome (lat = -72.82, lon = 159.18) ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Dronning Maud Land EPICA ice core Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
European Project for Ice Coring in Antarctica EPICA Talos Dome Ice Core TALDICE |
spellingShingle |
European Project for Ice Coring in Antarctica EPICA Talos Dome Ice Core TALDICE Eggleston, Sarah Schmitt, Jochen Bereiter, Bernhard Schneider, Robert Fischer, Hubertus CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... |
topic_facet |
European Project for Ice Coring in Antarctica EPICA Talos Dome Ice Core TALDICE |
description |
We present new d13C measurements of atmospheric CO2 covering the last glacial/interglacial cycle, complementing previous records covering Terminations I and II. Most prominent in the new record is a significant depletion in d13C(atm) of 0.5 permil occurring during marine isotope stage (MIS) 4, followed by an enrichment of the same magnitude at the beginning of MIS 3. Such a significant excursion in the record is otherwise only observed at glacial terminations, suggesting that similar processes were at play, such as changing sea surface temperatures, changes in marine biological export in the Southern Ocean (SO) due to variations in aeolian iron fluxes, changes in the Atlantic meridional overturning circulation, upwelling of deep water in the SO, and long-term trends in terrestrial carbon storage. Based on previous modeling studies, we propose constraints on some of these processes during specific time intervals. The decrease in d13C(atm) at the end of MIS 4 starting approximately 64 kyr B.P. was accompanied ... : These data complement previously published d13CO2 datasets: * Schmitt, J et al. (2012): Measurements of stable carbon isotope ratios of CO2 over the last 24000 years and CO2 concentration measurements on Antarctic ice cores using three different methods. doi:10.1594/PANGAEA.772713. * Schneider, R et al. (2013): A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the glacial inception. doi:10.1594/PANGAEA.817041. The CO2 concentration and stable isotope data were measured on the following three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950: European Project for Ice Coring in Antarctica (EPICA) Dome C (EDC) (lat = -75.10, lon = 123.40) EPICA Dronning Maud Land (EDML) (lat = -75.00, lon = 0.07) Talos Dome (lat = -72.82, lon = 159.18) ... |
format |
Article in Journal/Newspaper |
author |
Eggleston, Sarah Schmitt, Jochen Bereiter, Bernhard Schneider, Robert Fischer, Hubertus |
author_facet |
Eggleston, Sarah Schmitt, Jochen Bereiter, Bernhard Schneider, Robert Fischer, Hubertus |
author_sort |
Eggleston, Sarah |
title |
CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... |
title_short |
CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... |
title_full |
CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... |
title_fullStr |
CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... |
title_full_unstemmed |
CO2 concentration and stable isotope ratios of three Antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... |
title_sort |
co2 concentration and stable isotope ratios of three antarctic ice cores covering the period from 149.4 - 1.5 kyr before 1950 ... |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://dx.doi.org/10.1594/pangaea.859181 https://doi.pangaea.de/10.1594/PANGAEA.859181 |
genre |
Antarc* Antarctic Antarctica Dronning Maud Land EPICA ice core Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica Dronning Maud Land EPICA ice core Southern Ocean |
op_relation |
https://swisscovery.slsp.ch/discovery/search?query=lds02,contains,(IDSBB)006061992DSV01&tab=41SLSP_NETWORK&search_scope=DN_and_CI&vid=41SLSP_NETWORK:VU1_UNION https://dx.doi.org/10.1002/2015pa002874 https://dx.doi.org/10.5194/cp-9-1715-2013 https://dx.doi.org/10.1073/pnas.1204069109 https://dx.doi.org/10.1016/j.epsl.2010.06.023 https://swisscovery.slsp.ch/discovery/search?query=lds02,contains,(IDSBB)006061992DSV01&tab=41SLSP_NETWORK&search_scope=DN_and_CI&vid=41SLSP_NETWORK:VU1_UNION https://dx.doi.org/10.5194/cp-9-1733-2013 |
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.85918110.1002/2015pa00287410.5194/cp-9-1715-201310.1073/pnas.120406910910.1016/j.epsl.2010.06.02310.5194/cp-9-1733-2013 |
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