Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4
Here we use high-precision carbon isotope data (δ 13 C-CO 2 ) to show atmospheric CO 2 during Marine Isotope Stage 4 (MIS 4, ~70.5-59 ka) was controlled by a succession of millennial-scale processes. Enriched δ 13 C-CO 2 during peak glaciation suggests increased ocean carbon storage. Variations in δ...
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Veröffentlicht in: | Nature communications 2022-09, Vol.13 (1), p.5443-5443, Article 5443 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Here we use high-precision carbon isotope data (δ
13
C-CO
2
) to show atmospheric CO
2
during Marine Isotope Stage 4 (MIS 4, ~70.5-59 ka) was controlled by a succession of millennial-scale processes. Enriched δ
13
C-CO
2
during peak glaciation suggests increased ocean carbon storage. Variations in δ
13
C-CO
2
in early MIS 4 suggest multiple processes were active during CO
2
drawdown, potentially including decreased land carbon and decreased Southern Ocean air-sea gas exchange superposed on increased ocean carbon storage. CO
2
remained low during MIS 4 while δ
13
C-CO
2
fluctuations suggest changes in Southern Ocean and North Atlantic air-sea gas exchange. A 7 ppm increase in CO
2
at the onset of Dansgaard-Oeschger event 19 (72.1 ka) and 27 ppm increase in CO
2
during late MIS 4 (Heinrich Stadial 6, ~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.
Summary for general audience: We used carbon stable isotope data from an Antarctic ice core to evaluate which mechanisms caused changes in atmospheric carbon dioxide 74-59 thousand years ago, including a ~40 ppm decrease at the beginning of the last ice age. |
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ISSN: | 2041-1723 2041-1723 |
DOI: | 10.1038/s41467-022-33166-3 |