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Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records

Datos Bibliográficos

ID23322750
AutoresMike Walker (0000-0001-6702-7628, University of Wales Trinity Saint David, autor de correspondencia), Sigfús Johnsen, S J Johnsen (University of Copenhagen), Sune O Rasmussen (0000-0002-4177-3611, University of Copenhagen), Trevor Popp (University of Copenhagen), Jørgen Peder Steffensen (0000-0002-5516-1093, University of Copenhagen), Jørgen‐Peder Steffensen, Phil Gibbard (University of Cambridge), Wim Hoek (0000-0001-7313-100X, Utrecht University), J J Lowe (0000-0003-4644-702X, Royal Holloway University of London), John Lowe (0000-0002-8468-9276), John Andrews (0000-0002-6122-2788), John T Andrews (0000-0003-3169-5979, Institute of Arctic and Alpine Research), Svante Björck (0000-0001-8824-9000, Lund University), Les C Cwynar (University of New Brunswick), Konrad A Hughen (0000-0003-3201-934X, Woods Hole Oceanographic Institution), Konrad Hughen, Peter Kershaw (0000-0002-9478-0567, Monash University), Bernd Kromer (0000-0003-1058-4436, Heidelberg University), Thomas Litt (0000-0001-7401-5406, University of Bonn), David J Lowe (0000-0002-2547-6019, University of Waikato), Takeshi Nakagawa (0000-0001-5533-3169, Newcastle University), Rewi Newnham (0000-0002-6044-8945, University of Plymouth), Jakob Schwander (University of Bern)
Año2009
Volumen24
Número1
Páginas3-17
Fecha de publicación2009-01-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaJournal of Quaternary Science (JOURNAL)
Identificadores de la revistaISSN: 0267-8179 • E-ISSN: 1099-1417
EditorialWiley (PUBLISHER • GB)
DOI10.1002/jqs.1227
OpenAlexW2113660406
IdiomaEN
Citas recibidas149
Referencias citadas102

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. This climatic event is most clearly reflected in an abrupt shift in deuterium excess values, accompanied by more gradual changes in δ 18 O, dust concentration, a range of chemical species, and annual layer thickness. A timescale based on multi‐parameter annual layer counting provides an age of 11 700 calendar yr b2 k (before AD 2000) for the base of the Holocene, with a maximum counting error of 99 yr. A proposal that an archived core from this unique sequence should constitute the Global Stratotype Section and Point (GSSP) for the base of the Holocene Series/Epoch (Quaternary System/Period) has been ratified by the International Union of Geological Sciences. Five auxiliary stratotypes for the Pleistocene–Holocene boundary have also been recognised. Copyright © 2008 John Wiley & Sons, Ltd.

Climatology · Geography · Global Boundary Stratotype Section and Point · Holocene · Ice core · Physical geography · Pleistocene · Stage (stratigraphy) · Stratotype · Younger Dryas · Cryospheric studies and observations · Geology · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Paleontology

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