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Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint [期刊论文]
Quaternary Science Reviews, 2014-01-01, 106
Seierstad I.K.;  Abbott P.M.;  Bigler M.;  Blunier T.;  Bourne A.J.;  Brook E.;  Buchardt S.L.;  Buizert C.;  Clausen H.B.;  Cook E.;  Dahl-Jensen D.;  Davies S.M.;  Guillevic M.;  Johnsen S.J.;  Pedersen D.S.;  Popp T.J.;  Rasmussen S.O.;  Severinghaus J.P.;  Svensson A.;  Vinther B.M.
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