δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2
Abrupt millennial-scale climate change events of the last deglaciation (i.e. Heinrich Stadial 1 and the Younger Dryas) were accompanied by marked increases in atmospheric CO2 (CO2atm) and decreases in its stable carbon isotopic ratios (δ13C), i.e. δ13CO2atm, presumably due to outgassing from the oce...
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00010348 2023-05-15T17:34:43+02:00 δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 Campos, Marília C. Chiessi, Cristiano M. Voigt, Ines Piola, Alberto R. Kuhnert, Henning Mulitza, Stefan 2017-04 electronic https://doi.org/10.5194/cp-13-345-2017 https://noa.gwlb.de/receive/cop_mods_00010348 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010305/cp-13-345-2017.pdf https://cp.copernicus.org/articles/13/345/2017/cp-13-345-2017.pdf eng eng Copernicus Publications Climate of the Past -- http://www.copernicus.org/EGU/cp/cp/published_papers.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2217985 -- 1814-9332 https://doi.org/10.5194/cp-13-345-2017 https://noa.gwlb.de/receive/cop_mods_00010348 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010305/cp-13-345-2017.pdf https://cp.copernicus.org/articles/13/345/2017/cp-13-345-2017.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2017 ftnonlinearchiv https://doi.org/10.5194/cp-13-345-2017 2022-02-08T22:57:06Z Abrupt millennial-scale climate change events of the last deglaciation (i.e. Heinrich Stadial 1 and the Younger Dryas) were accompanied by marked increases in atmospheric CO2 (CO2atm) and decreases in its stable carbon isotopic ratios (δ13C), i.e. δ13CO2atm, presumably due to outgassing from the ocean. However, information on the preceding Heinrich Stadials during the last glacial period is scarce. Here we present δ13C records from two species of planktonic foraminifera from the western South Atlantic that reveal major decreases (up to 1 ‰) during Heinrich Stadials 3 and 2. These δ13C decreases are most likely related to millennial-scale periods of weakening of the Atlantic meridional overturning circulation and the consequent increase (decrease) in CO2atm (δ13CO2atm). We hypothesise two mechanisms that could account for the decreases observed in our records, namely strengthening of Southern Ocean deep-water ventilation and weakening of the biological pump. Additionally, we suggest that air–sea gas exchange could have contributed to the observed δ13C decreases. Together with other lines of evidence, our data are consistent with the hypothesis that the CO2 added to the atmosphere during abrupt millennial-scale climate change events of the last glacial period also originated in the ocean and reached the atmosphere by outgassing. The temporal evolution of δ13C during Heinrich Stadials 3 and 2 in our records is characterized by two relative minima separated by a relative maximum. This w structure is also found in North Atlantic and South American records, further suggesting that such a structure is a pervasive feature of Heinrich Stadial 2 and, possibly, also Heinrich Stadial 3. Article in Journal/Newspaper North Atlantic Planktonic foraminifera Southern Ocean Niedersächsisches Online-Archiv NOA Southern Ocean Climate of the Past 13 4 345 358 |
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Niedersächsisches Online-Archiv NOA |
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English |
topic |
article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Campos, Marília C. Chiessi, Cristiano M. Voigt, Ines Piola, Alberto R. Kuhnert, Henning Mulitza, Stefan δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 |
topic_facet |
article Verlagsveröffentlichung |
description |
Abrupt millennial-scale climate change events of the last deglaciation (i.e. Heinrich Stadial 1 and the Younger Dryas) were accompanied by marked increases in atmospheric CO2 (CO2atm) and decreases in its stable carbon isotopic ratios (δ13C), i.e. δ13CO2atm, presumably due to outgassing from the ocean. However, information on the preceding Heinrich Stadials during the last glacial period is scarce. Here we present δ13C records from two species of planktonic foraminifera from the western South Atlantic that reveal major decreases (up to 1 ‰) during Heinrich Stadials 3 and 2. These δ13C decreases are most likely related to millennial-scale periods of weakening of the Atlantic meridional overturning circulation and the consequent increase (decrease) in CO2atm (δ13CO2atm). We hypothesise two mechanisms that could account for the decreases observed in our records, namely strengthening of Southern Ocean deep-water ventilation and weakening of the biological pump. Additionally, we suggest that air–sea gas exchange could have contributed to the observed δ13C decreases. Together with other lines of evidence, our data are consistent with the hypothesis that the CO2 added to the atmosphere during abrupt millennial-scale climate change events of the last glacial period also originated in the ocean and reached the atmosphere by outgassing. The temporal evolution of δ13C during Heinrich Stadials 3 and 2 in our records is characterized by two relative minima separated by a relative maximum. This w structure is also found in North Atlantic and South American records, further suggesting that such a structure is a pervasive feature of Heinrich Stadial 2 and, possibly, also Heinrich Stadial 3. |
format |
Article in Journal/Newspaper |
author |
Campos, Marília C. Chiessi, Cristiano M. Voigt, Ines Piola, Alberto R. Kuhnert, Henning Mulitza, Stefan |
author_facet |
Campos, Marília C. Chiessi, Cristiano M. Voigt, Ines Piola, Alberto R. Kuhnert, Henning Mulitza, Stefan |
author_sort |
Campos, Marília C. |
title |
δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 |
title_short |
δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 |
title_full |
δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 |
title_fullStr |
δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 |
title_full_unstemmed |
δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 |
title_sort |
δ13c decreases in the upper western south atlantic during heinrich stadials 3 and 2 |
publisher |
Copernicus Publications |
publishDate |
2017 |
url |
https://doi.org/10.5194/cp-13-345-2017 https://noa.gwlb.de/receive/cop_mods_00010348 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010305/cp-13-345-2017.pdf https://cp.copernicus.org/articles/13/345/2017/cp-13-345-2017.pdf |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
North Atlantic Planktonic foraminifera Southern Ocean |
genre_facet |
North Atlantic Planktonic foraminifera Southern Ocean |
op_relation |
Climate of the Past -- http://www.copernicus.org/EGU/cp/cp/published_papers.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2217985 -- 1814-9332 https://doi.org/10.5194/cp-13-345-2017 https://noa.gwlb.de/receive/cop_mods_00010348 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00010305/cp-13-345-2017.pdf https://cp.copernicus.org/articles/13/345/2017/cp-13-345-2017.pdf |
op_rights |
uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/cp-13-345-2017 |
container_title |
Climate of the Past |
container_volume |
13 |
container_issue |
4 |
container_start_page |
345 |
op_container_end_page |
358 |
_version_ |
1766133635243573248 |