Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint
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author: Eliza Cook, Anna J. Bourne, Dorthe Dahl-Jensen, Sune O. Rasmussen, Anders Svensson, Thomas Blunier, Bo Møllesøe Vinther, Christo Buizert, Jeffrey P. Severinghaus, Trevor J. Popp, Siwan Davies, Matthias Bigler, Henrik Clausen, Peter M. Abbott, Edward J. Brook, Myriam Guillevic
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