Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4
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- s41467-022-33166-3
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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.
Original language | English |
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Article number | 5443 |
Journal | Nature Communications |
Volume | 13 |
Issue number | 1 |
Number of pages | 10 |
ISSN | 2041-1723 |
DOIs | |
Publication status | Published - 16 Sep 2022 |
- ATMOSPHERIC NITROUS-OXIDE, DEEP SOUTHERN-OCEAN, ANTARCTIC ICE, POLAR ICE, OVERTURNING CIRCULATION, CHRONOLOGY AICC2012, IRON FERTILIZATION, CO2 VARIABILITY, DEGLACIAL RISE, TAYLOR GLACIER
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