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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
作者姓名: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
作者单位:[1]Department of Archaeology and Anthropology, University of Wales, Lampeter, Wales SA48 7ED, UK.; [2]Centre for Ice and Climatel The Niels Bohr Institute, University of Copenhagen, Juliane Maries Vej 30, DK2100 Copenhagen, Denmark.; [3]Stable Isotope Laboratory, Institute of Arctic and Alpine Research, University of Colorado, Boulder, Co 80302, USA.; [4]Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK.; [5]Department-of Physical Geography, University of Utrecht, Heidelberglaan 2, 3508 TC Utrecht, The Netherlands.; [6]Department of Geography, Royal Holloway, University of London, Egham, Surrey TW20 0EX, UK.; [7]Institute for Arctic and Alpine Research, University of Colorado, Campus Box, 450, Boulder, Co 80309, USA.; [8]GeoBiosphere Science Centre, Quaternary Sciences, Lund University, S/51veg 12, SE-223 62 Lund, Sweden.; [9]Department of Biology, University of New Brunswick, Fredericton, New Brunswick, Canada E3B 6E1.; [10]Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.; [11]School of Geography and Environmental Science, Monash University, Victoria 3800, Australia.; [12]Heidelberg Academy of Sciences, University of Heidelberg, 1NF 229, D-69120 Heidelberg, Germany.; [13]Institute for Palaeontology, University of Bonn, Nussallee 8, D-53115, Bonn, Germany.; [14]Department of Earth and Ocean Sciences, University of Waikato, Private Bag 3105, Hamilton, New Zealand.; [15]Department of Geography, University of Newcastle, Newcastle-upon-Tyne NE 1 7RU, UK.; [16]School of Geography, University of Plymouth, Drake Circus, Plymouth PIA 8AA, UK.; [17]Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.
摘    要: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.

关 键 词:地球  全新世  第四纪地质时代  周期
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