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• W2018156694 abstract "Changes in the upwelling and degassing of carbon from the Southern Ocean form one of the leading hypotheses for the cause of glacial-interglacial changes in atmospheric carbon dioxide. We present a 25,000-year-long Southern Ocean radiocarbon record reconstructed from deep-sea corals, which shows radiocarbon-depleted waters during the glacial period and through the early deglaciation. This depletion and associated deep stratification disappeared by ~14.6 ka (thousand years ago), consistent with the transfer of carbon from the deep ocean to the surface ocean and atmosphere via a Southern Ocean ventilation event. Given this evidence for carbon exchange in the Southern Ocean, we show that existing deep-ocean radiocarbon records from the glacial period are sufficiently depleted to explain the ~190 per mil drop in atmospheric radiocarbon between ~17 and 14.5 ka." @default.
• W2018156694 created "2016-06-24" @default.
• W2018156694 creator A5015259127 @default.
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• W2018156694 date "2012-02-03" @default.
• W2018156694 modified "2023-10-10" @default.
• W2018156694 title "The Southern Ocean’s Role in Carbon Exchange During the Last Deglaciation" @default.
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• W2018156694 doi "https://doi.org/10.1126/science.1208163" @default.
• W2018156694 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/22174131" @default.
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