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The Global Stratotype Section and Point (GSSP) for the base of the Holocene Series/Epoch (Quaternary System/Period) in the NGRIP ice core 总被引:4,自引:0,他引:4
Mike Walker ;Sigfus Johnsen ;Sune Olander Rasmussen ;Jorgen-Peder Steffensen ;Trevor Popp ;Philip Gibbard ;Wim Hoek ;John Lowe ;John Andrews ;Svante Bjorck ;Les Cwynar ;Konrad Hughen ;Peter Kershaw ;Bernd Kromer ;Thomas Litt ;David J. Lowe ;Takeshi Nakagawa ;Rewi Newnham ;Jakob Schwander 《《幕》》2008,31(2):264-267
The Greenland ice core from NorthGRIP (NGRIP) contains a proxy climate record across the Pleistocene-Holocene boundary of unprecedented clarity and resolution. Analysis of an array of physical and chemical parameters within the ice enables the base of the Holocene, as reflected in the first signs of climatic warming at the end of the Younger Dryas/Greenland Stadial 1 cold phase, to be located with a high degree of precision. 相似文献