{"refrec":{"BRefID":212924,"RR":"<b>Burke, A.; Robinson, L.F.</b> (2012). The Southern Ocean’s role in carbon exchange during the last deglaciation. <i>Science (Wash.) 335(6068)</i>: 557-561. <a href=\"http://dx.doi.org/10.1126/science.1208163\" target=\"_blank\">http://dx.doi.org/10.1126/science.1208163</a>","BEntID":204821,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 335(6068)</i>: 557-561. <a href=\"https://dx.doi.org/10.1126/science.1208163\" target=\"_blank\">https://dx.doi.org/10.1126/science.1208163</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Burke, A.; Robinson, L.F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Burke, A.; Robinson, L.F.","Englishabstract":"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.                     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