{"refrec":{"BRefID":23841,"RR":"<b>Frank, M.; Nürnberg, C.C.; Gersonde, R.; Rutgers van der Loeff, M.M.; Bohrmann, G.; Kubik, P.W.; Mangini, A.</b> (1998). No bioproductivity-induced sink for atmospheric CO<sub>2</sub> in the glacial Southern Ocean: evidence from sedimentary fluxes of <sup>10</sup>Be and biogenic Ba, <b><i>in</i></b>: Dehairs, F.A. <i>et al.</i> (Ed.) <i>Integrated Marine System Analysis. European Network for Integrated Marine System Analysis FWO Vlaanderen: Proceedings of the second network meeting (Brussels, May 29-31, 1997).</i> pp. 323-336","BEntID":23841,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Dehairs, F.A. <i>et al.</i> <i>Integrated Marine System Analysis - European Network for Integrated Marine System Analysis FWO Vlaanderen: Proceedings of the second network meeting (Brussels, May 29-31, 1997).</i> pp. 323-336","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Frank, M.; Nürnberg, C.C.; Gersonde, R.; Rutgers van der Loeff, M.M.; Bohrmann, G.; Kubik, P.W.; Mangini, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Frank, M. <i>et al.</i>","Englishabstract":"Recently, <sup>230</sup>Th<sub>ex</sub> normalized radionuclide paleofluxes to South Atlantic sediments were interpreted in terms of a higher biological productivity of glacial Southern Ocean surface waters (Kumar et al. 1995). We present a proxy data set from nearly the same area and claim that the glacial increase of <sup>10</sup>Be deposition was weaker than previously estimated and that the sedimentary <sup>10</sup>Be flux is much better correlated with the flux of detrital particles (Fe) than with biogenic Ba. This suggests that the <sup>10</sup>Be deposition has been more controlled by detrital than biogenic particles and that increased glacial <sup>10</sup>Be scavenging may well be solely explained by increased input of wind-blown dust particles. The export paleoproductivity reconstructed from biogenic barium in the same cores suggests rather an overall glacial decrease of biological productivity than an increase, which implies that a Southem Ocean bioproductivity increase may not serve as an explanation for glacial atmospheric CO<sub>2</sub> drawdown.","AbstractOtherLang":null,"BibLvlCode":"AM","StandardTitle":"No bioproductivity-induced sink for atmospheric CO<sub>2</sub> in the glacial Southern Ocean: evidence from sedimentary fluxes of <sup>10</sup>Be and biogenic Ba","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1998,"MonPub":null,"DateUpdate":"2002-04-03","DateCreate":"2002-04-03","SecASFANote":null,"ConfID":null,"PeerRev":null,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":23841,"PubliDate":1998,"Pagination":"323-336","XtraPublOfAnaID":null,"ISBN":null,"Volume":null,"Issue":null,"BRefMon":20337,"BRefMonRR":"<b>Dehairs, F.A.; Elskens, M.; Goeyens, L. 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