{"refrec":{"BRefID":75534,"RR":"<b>Bassett, S.E.; Milne, G.A.; Mitrovica, J.X.; Clark, P.U.</b> (2005). Ice sheet and solid earth influences on far-field sea-level histories. <i>Science (Wash.) 309(5736)</i>: 925-928. <a href=\"https://dx.doi.org/10.1126/science.1111575\" target=\"_blank\">https://dx.doi.org/10.1126/science.1111575</a>","BEntID":306669,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 309(5736)</i>: 925-928. <a href=\"https://dx.doi.org/10.1126/science.1111575\" target=\"_blank\">https://dx.doi.org/10.1126/science.1111575</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bassett, S.E.; Milne, G.A.; Mitrovica, J.X.; Clark, P.U.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bassett, S.E. <i>et al.</i>","Englishabstract":"Previous predictions of sea-level change subsequent to the last glacial maximum show significant, systematic discrepancies between observations at Tahiti, Huon Peninsula, and Sunda Shelf during Lateglacial time (~14,000 to 9000 calibrated years before the present). We demonstrate that a model of glacial isostatic adjustment characterized by both a high-viscosity lower mantle (4  x 10²² Pa s) and a large contribution from the Antarctic ice sheet to meltwater pulse IA (~15-meters eustatic equivalent) resolves these discrepancies. 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