{"refrec":{"BRefID":198257,"RR":"<b>Rose, K.A.; Sikes, E.L.; Guilderson, T.P.; Shane, P.; Hill, T.M.; Zahn, R.; Spero, H.J.</b> (2010). Upper-ocean-to-atmosphere radiocarbon offsets imply fast deglacial carbon dioxide release. <i>Nature (Lond.) 466(7310)</i>: 1093-1097. <a href=\"https://dx.doi.org/10.1038/nature09288\" target=\"_blank\">https://dx.doi.org/10.1038/nature09288</a>","BEntID":190628,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 466(7310)</i>: 1093-1097. <a href=\"https://dx.doi.org/10.1038/nature09288\" target=\"_blank\">https://dx.doi.org/10.1038/nature09288</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Rose, K.A.; Sikes, E.L.; Guilderson, T.P.; Shane, P.; Hill, T.M.; Zahn, R.; Spero, H.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Rose, K.A. <i>et al.</i>","Englishabstract":"At the end of the last ice age, rising atmospheric CO2 levels coincided with a decline in radiocarbon activity, suggesting the release of highly radiocarbon-depleted CO2  from the deep ocean to the atmosphere. 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