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

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...

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Published in:Journal of Quaternary Science
Main Authors: Walker, Mike, Johnsen, Sigfus, Rasmussen, Sune Olander, Popp, Trevor, Steffensen, Jorgen-Peder, Gibbard, Phil, Hoek, Wim, Lowe, John, Andrews, John, Björck, Svante, Cwynar, Les C., Hughen, Konrad, Kershaw, Peter, Kromer, Bernd, Litt, Thomas, Lowe, David J., Nakagawa, Takeshi, Newnham, Rewi, Schwander, Jakob
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Inc. 2009
Subjects:
Online Access:https://lup.lub.lu.se/record/1312496
https://doi.org/10.1002/jqs.1227
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author Walker, Mike
Johnsen, Sigfus
Rasmussen, Sune Olander
Popp, Trevor
Steffensen, Jorgen-Peder
Gibbard, Phil
Hoek, Wim
Lowe, John
Andrews, John
Björck, Svante
Cwynar, Les C.
Hughen, Konrad
Kershaw, Peter
Kromer, Bernd
Litt, Thomas
Lowe, David J.
Nakagawa, Takeshi
Newnham, Rewi
Schwander, Jakob
author_facet Walker, Mike
Johnsen, Sigfus
Rasmussen, Sune Olander
Popp, Trevor
Steffensen, Jorgen-Peder
Gibbard, Phil
Hoek, Wim
Lowe, John
Andrews, John
Björck, Svante
Cwynar, Les C.
Hughen, Konrad
Kershaw, Peter
Kromer, Bernd
Litt, Thomas
Lowe, David J.
Nakagawa, Takeshi
Newnham, Rewi
Schwander, Jakob
author_sort Walker, Mike
collection Lund University Publications (LUP)
container_issue 1
container_start_page 3
container_title Journal of Quaternary Science
container_volume 24
description 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 delta O-18, 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 b2k (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 (C) 2008 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
genre Greenland
Greenland ice core
ice core
NGRIP
genre_facet Greenland
Greenland ice core
ice core
NGRIP
geographic Greenland
geographic_facet Greenland
id ftulundlup:oai:lup.lub.lu.se:a9afffd7-0945-4c09-b88e-a31f93937b8f
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language English
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op_container_end_page 17
op_doi https://doi.org/10.1002/jqs.1227
op_relation https://lup.lub.lu.se/record/1312496
http://dx.doi.org/10.1002/jqs.1227
wos:000262615700002
scopus:65349194580
op_source Journal of Quaternary Science; 24(1), pp 3-17 (2009)
ISSN: 1099-1417
publishDate 2009
publisher John Wiley & Sons Inc.
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spelling ftulundlup:oai:lup.lub.lu.se:a9afffd7-0945-4c09-b88e-a31f93937b8f 2025-04-06T14:53:44+00:00 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 Walker, Mike Johnsen, Sigfus Rasmussen, Sune Olander Popp, Trevor Steffensen, Jorgen-Peder Gibbard, Phil Hoek, Wim Lowe, John Andrews, John Björck, Svante Cwynar, Les C. Hughen, Konrad Kershaw, Peter Kromer, Bernd Litt, Thomas Lowe, David J. Nakagawa, Takeshi Newnham, Rewi Schwander, Jakob 2009 https://lup.lub.lu.se/record/1312496 https://doi.org/10.1002/jqs.1227 eng eng John Wiley & Sons Inc. https://lup.lub.lu.se/record/1312496 http://dx.doi.org/10.1002/jqs.1227 wos:000262615700002 scopus:65349194580 Journal of Quaternary Science; 24(1), pp 3-17 (2009) ISSN: 1099-1417 Geology auxiliary stratotypes NGRIP ice core Holocene boundary Global Stratotype Section and Point contributiontojournal/systematicreview info:eu-repo/semantics/article text 2009 ftulundlup https://doi.org/10.1002/jqs.1227 2025-03-11T14:07:57Z 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 delta O-18, 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 b2k (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 (C) 2008 John Wiley & Sons, Ltd. Article in Journal/Newspaper Greenland Greenland ice core ice core NGRIP Lund University Publications (LUP) Greenland Journal of Quaternary Science 24 1 3 17
spellingShingle Geology
auxiliary stratotypes
NGRIP ice core
Holocene boundary
Global Stratotype Section and Point
Walker, Mike
Johnsen, Sigfus
Rasmussen, Sune Olander
Popp, Trevor
Steffensen, Jorgen-Peder
Gibbard, Phil
Hoek, Wim
Lowe, John
Andrews, John
Björck, Svante
Cwynar, Les C.
Hughen, Konrad
Kershaw, Peter
Kromer, Bernd
Litt, Thomas
Lowe, David J.
Nakagawa, Takeshi
Newnham, Rewi
Schwander, Jakob
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
title 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
title_full 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
title_fullStr 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
title_full_unstemmed 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
title_short 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
title_sort 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
topic Geology
auxiliary stratotypes
NGRIP ice core
Holocene boundary
Global Stratotype Section and Point
topic_facet Geology
auxiliary stratotypes
NGRIP ice core
Holocene boundary
Global Stratotype Section and Point
url https://lup.lub.lu.se/record/1312496
https://doi.org/10.1002/jqs.1227