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...
Published in: | Journal of Quaternary Science |
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Main Authors: | , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
John Wiley & Sons Inc.
2009
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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 |
institution | Open Polar |
language | English |
op_collection_id | ftulundlup |
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. |
record_format | openpolar |
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 |