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The Last Glacial-Interglacial Transition

Episodes 2008年第2期31卷 226-229页

作者： wim Z. hoek Department of Physical Geography Faculty of Geosciences Utrecht University Heidelberglaan 2 NL 3508 TC Utrecht The Netherlands.

The Last Glacial-Interglacial Transition is one of the most intensively studied periods in Earth History. The rapid climate and environmental changes that occurred during the transition can be used to test ideas about the functioning of our climate system. The stratigraphy of this period has been thoroughly investigated and, in particular, the recently proposed event stratigraphy for the Last Glacial-Interglacial Transition based on the Greenland ice core records serves as a tool for synchronisation of records from the ice, marine and terrestrial environment.

关键词：冰河-间冰期转换周期地球气候

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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

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Episodes 2008年第2期31卷 264-267页

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

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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