{"refrec":{"BRefID":330722,"RR":"<b>Chen, T.; Robinson, L.F.; Burke, A.; Claxton, L.M.; Hain, M.P.; Li, T.; Rae, J.W.B.; Stewart, J.; Knowles, T.D.J.; Fornari, D.J.; Harpp, K.S.</b> (2020). Persistently well-ventilated intermediate-depth ocean through the last deglaciation. <i>Nature Geoscience 13(11)</i>: 733-738. <a href=\"https://dx.doi.org/10.1038/s41561-020-0638-6\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-020-0638-6</a>","BEntID":324332,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 13(11)</i>: 733-738. <a href=\"https://dx.doi.org/10.1038/s41561-020-0638-6\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-020-0638-6</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Chen, T.; Robinson, L.F.; Burke, A.; Claxton, L.M.; Hain, M.P.; Li, T.; Rae, J.W.B.; Stewart, J.; Knowles, T.D.J.; Fornari, D.J.; Harpp, K.S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Chen, T. <i>et al.</i>","Englishabstract":"During the last deglaciation (~18–11 thousand years ago), existing radiocarbon (<sup>14</sup>C) reconstructions of intermediate waters in the mid- to low-latitude oceans show widely diverging trends, with some broadly tracking the atmosphere and others suggesting extreme depletions. These discrepancies cloud our understanding of the deglacial carbon cycle because of the diversity of hypotheses needed to explain these diverging records, for example, injections of <sup>14</sup>C-dead geological carbon, mixing of extremely isolated waters from the abyssal ocean or changes in sites of deep-water ventilation. Here we present absolutely dated deglacial deep-sea coral <sup>14</sup>C records of intermediate waters from the Galápagos Platform—close to the largest reported deglacial <sup>14</sup>C depletions—together with data from the low-latitude Atlantic. Our records indicate coherent, well-equilibrated intermediate-water <sup>14</sup>C ventilation in both oceans relative to the atmosphere throughout the deglaciation. 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