Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4
Here we use high-precision carbon isotope data (delta C-13-CO2) to show atmospheric CO2 during Marine Isotope Stage 4 (MIS 4, similar to 70.5-59 ka) was controlled by a succession of millennial-scale processes. Enriched delta C-13-CO2 during peak glaciation suggests increased ocean carbon storage. V...
Published in: | Nature Communications |
---|---|
Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2022
|
Subjects: | |
Online Access: | https://curis.ku.dk/portal/da/publications/multiple-carbon-cycle-mechanisms-associated-with-the-glaciation-of-marine-isotope-stage-4(7dbd0899-43a6-4639-986a-9ba068905e9e).html https://doi.org/10.1038/s41467-022-33166-3 https://curis.ku.dk/ws/files/320756916/s41467_022_33166_3.pdf |
id |
ftcopenhagenunip:oai:pure.atira.dk:publications/7dbd0899-43a6-4639-986a-9ba068905e9e |
---|---|
record_format |
openpolar |
spelling |
ftcopenhagenunip:oai:pure.atira.dk:publications/7dbd0899-43a6-4639-986a-9ba068905e9e 2024-06-09T07:40:05+00:00 Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 Menking, James A. Shackleton, Sarah A. Bauska, Thomas K. Buffen, Aron M. Brook, Edward J. Barker, Stephen Severinghaus, Jeffrey P. Dyonisius, Michael N. Petrenko, Vasilii V. 2022-09-16 application/pdf https://curis.ku.dk/portal/da/publications/multiple-carbon-cycle-mechanisms-associated-with-the-glaciation-of-marine-isotope-stage-4(7dbd0899-43a6-4639-986a-9ba068905e9e).html https://doi.org/10.1038/s41467-022-33166-3 https://curis.ku.dk/ws/files/320756916/s41467_022_33166_3.pdf eng eng info:eu-repo/semantics/openAccess Menking , J A , Shackleton , S A , Bauska , T K , Buffen , A M , Brook , E J , Barker , S , Severinghaus , J P , Dyonisius , M N & Petrenko , V V 2022 , ' Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 ' , Nature Communications , vol. 13 , no. 1 , 5443 . https://doi.org/10.1038/s41467-022-33166-3 ATMOSPHERIC NITROUS-OXIDE DEEP SOUTHERN-OCEAN ANTARCTIC ICE POLAR ICE OVERTURNING CIRCULATION CHRONOLOGY AICC2012 IRON FERTILIZATION CO2 VARIABILITY DEGLACIAL RISE TAYLOR GLACIER article 2022 ftcopenhagenunip https://doi.org/10.1038/s41467-022-33166-3 2024-05-16T11:29:25Z Here we use high-precision carbon isotope data (delta C-13-CO2) to show atmospheric CO2 during Marine Isotope Stage 4 (MIS 4, similar to 70.5-59 ka) was controlled by a succession of millennial-scale processes. Enriched delta C-13-CO2 during peak glaciation suggests increased ocean carbon storage. Variations in delta C-13-CO2 in early MIS 4 suggest multiple processes were active during CO2 drawdown, potentially including decreased land carbon and decreased Southern Ocean air-sea gas exchange superposed on increased ocean carbon storage. CO2 remained low during MIS 4 while delta C-13-CO2 fluctuations suggest changes in Southern Ocean and North Atlantic air-sea gas exchange. A 7 ppm increase in CO2 at the onset of Dansgaard-Oeschger event 19 (72.1 ka) and 27 ppm increase in CO2 during late MIS 4 (Heinrich Stadial 6, similar to 63.5-60 ka) involved additions of isotopically light carbon to the atmosphere. The terrestrial biosphere and Southern Ocean air-sea gas exchange are possible sources, with the latter event also involving decreased ocean carbon storage. Article in Journal/Newspaper Antarc* Antarctic North Atlantic Southern Ocean Taylor Glacier University of Copenhagen: Research Antarctic Southern Ocean Taylor Glacier ENVELOPE(162.167,162.167,-77.733,-77.733) Nature Communications 13 1 |
institution |
Open Polar |
collection |
University of Copenhagen: Research |
op_collection_id |
ftcopenhagenunip |
language |
English |
topic |
ATMOSPHERIC NITROUS-OXIDE DEEP SOUTHERN-OCEAN ANTARCTIC ICE POLAR ICE OVERTURNING CIRCULATION CHRONOLOGY AICC2012 IRON FERTILIZATION CO2 VARIABILITY DEGLACIAL RISE TAYLOR GLACIER |
spellingShingle |
ATMOSPHERIC NITROUS-OXIDE DEEP SOUTHERN-OCEAN ANTARCTIC ICE POLAR ICE OVERTURNING CIRCULATION CHRONOLOGY AICC2012 IRON FERTILIZATION CO2 VARIABILITY DEGLACIAL RISE TAYLOR GLACIER Menking, James A. Shackleton, Sarah A. Bauska, Thomas K. Buffen, Aron M. Brook, Edward J. Barker, Stephen Severinghaus, Jeffrey P. Dyonisius, Michael N. Petrenko, Vasilii V. Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 |
topic_facet |
ATMOSPHERIC NITROUS-OXIDE DEEP SOUTHERN-OCEAN ANTARCTIC ICE POLAR ICE OVERTURNING CIRCULATION CHRONOLOGY AICC2012 IRON FERTILIZATION CO2 VARIABILITY DEGLACIAL RISE TAYLOR GLACIER |
description |
Here we use high-precision carbon isotope data (delta C-13-CO2) to show atmospheric CO2 during Marine Isotope Stage 4 (MIS 4, similar to 70.5-59 ka) was controlled by a succession of millennial-scale processes. Enriched delta C-13-CO2 during peak glaciation suggests increased ocean carbon storage. Variations in delta C-13-CO2 in early MIS 4 suggest multiple processes were active during CO2 drawdown, potentially including decreased land carbon and decreased Southern Ocean air-sea gas exchange superposed on increased ocean carbon storage. CO2 remained low during MIS 4 while delta C-13-CO2 fluctuations suggest changes in Southern Ocean and North Atlantic air-sea gas exchange. A 7 ppm increase in CO2 at the onset of Dansgaard-Oeschger event 19 (72.1 ka) and 27 ppm increase in CO2 during late MIS 4 (Heinrich Stadial 6, similar to 63.5-60 ka) involved additions of isotopically light carbon to the atmosphere. The terrestrial biosphere and Southern Ocean air-sea gas exchange are possible sources, with the latter event also involving decreased ocean carbon storage. |
format |
Article in Journal/Newspaper |
author |
Menking, James A. Shackleton, Sarah A. Bauska, Thomas K. Buffen, Aron M. Brook, Edward J. Barker, Stephen Severinghaus, Jeffrey P. Dyonisius, Michael N. Petrenko, Vasilii V. |
author_facet |
Menking, James A. Shackleton, Sarah A. Bauska, Thomas K. Buffen, Aron M. Brook, Edward J. Barker, Stephen Severinghaus, Jeffrey P. Dyonisius, Michael N. Petrenko, Vasilii V. |
author_sort |
Menking, James A. |
title |
Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 |
title_short |
Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 |
title_full |
Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 |
title_fullStr |
Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 |
title_full_unstemmed |
Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 |
title_sort |
multiple carbon cycle mechanisms associated with the glaciation of marine isotope stage 4 |
publishDate |
2022 |
url |
https://curis.ku.dk/portal/da/publications/multiple-carbon-cycle-mechanisms-associated-with-the-glaciation-of-marine-isotope-stage-4(7dbd0899-43a6-4639-986a-9ba068905e9e).html https://doi.org/10.1038/s41467-022-33166-3 https://curis.ku.dk/ws/files/320756916/s41467_022_33166_3.pdf |
long_lat |
ENVELOPE(162.167,162.167,-77.733,-77.733) |
geographic |
Antarctic Southern Ocean Taylor Glacier |
geographic_facet |
Antarctic Southern Ocean Taylor Glacier |
genre |
Antarc* Antarctic North Atlantic Southern Ocean Taylor Glacier |
genre_facet |
Antarc* Antarctic North Atlantic Southern Ocean Taylor Glacier |
op_source |
Menking , J A , Shackleton , S A , Bauska , T K , Buffen , A M , Brook , E J , Barker , S , Severinghaus , J P , Dyonisius , M N & Petrenko , V V 2022 , ' Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4 ' , Nature Communications , vol. 13 , no. 1 , 5443 . https://doi.org/10.1038/s41467-022-33166-3 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1038/s41467-022-33166-3 |
container_title |
Nature Communications |
container_volume |
13 |
container_issue |
1 |
_version_ |
1801383584656785408 |