Synchronization of the NGRIP, GRIP, and GISP2 ice cores ...

We here present a synchronization of the NGRIP, GRIP, and GISP2 ice cores based mainly on volcanic events over the period 14.9-32.45 ka b2k (before AD 2000), corresponding to Marine Isotope Stage 2 (MIS 2) and the end of MIS 3. The matching provides a basis for applying the recent NGRIP-based Greenl...

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Main Authors: Rasmussen, Sune Olander, Seierstad, Inger K, Andersen, Katrine K, Bigler, Matthias, Dahl-Jensen, Dorthe, Johnsen, Sigfús Jóhann
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.786240
https://doi.pangaea.de/10.1594/PANGAEA.786240
id ftdatacite:10.1594/pangaea.786240
record_format openpolar
spelling ftdatacite:10.1594/pangaea.786240 2024-09-09T19:41:07+00:00 Synchronization of the NGRIP, GRIP, and GISP2 ice cores ... Rasmussen, Sune Olander Seierstad, Inger K Andersen, Katrine K Bigler, Matthias Dahl-Jensen, Dorthe Johnsen, Sigfús Jóhann 2008 application/zip https://dx.doi.org/10.1594/pangaea.786240 https://doi.pangaea.de/10.1594/PANGAEA.786240 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2007.01.016 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Greenland Ice Core Projects GRIP/GISP/NGRIP article Collection Supplementary Publication Series of Datasets 2008 ftdatacite https://doi.org/10.1594/pangaea.78624010.1016/j.quascirev.2007.01.016 2024-08-01T10:51:52Z We here present a synchronization of the NGRIP, GRIP, and GISP2 ice cores based mainly on volcanic events over the period 14.9-32.45 ka b2k (before AD 2000), corresponding to Marine Isotope Stage 2 (MIS 2) and the end of MIS 3. The matching provides a basis for applying the recent NGRIP-based Greenland Ice Core Chronology 2005 (GICC05) time scale to the GRIP and GISP2 ice cores, thereby making it possible to compare the synchronized palaeoclimate profiles of the cores in detail and to identify relative accumulation differences between the cores. Based on the matching, a period of anomalous high accumulation rates in the GISP2 ice core is detected within the period 16.5-18.3 ka b2k. The d18O and [Ca2+] profiles of the three cores are presented on the common GICC05 time scale and generally show excellent agreement across the stadial-interstadial transitions and across the two characteristic dust events in Greenland Stadial 3. However, large differences between the d18O and [Ca2+] profiles of the three cores ... : Supplement to: Rasmussen, Sune Olander; Seierstad, Inger K; Andersen, Katrine K; Bigler, Matthias; Dahl-Jensen, Dorthe; Johnsen, Sigfús Jóhann (2008): Synchronization of the NGRIP, GRIP, and GISP2 ice cores across MIS 2 and palaeoclimatic implications. Quaternary Science Reviews, 27(1-2), 18-28 ... Article in Journal/Newspaper GISP Greenland Greenland ice core GRIP ice core NGRIP DataCite Greenland Rasmussen ENVELOPE(-64.084,-64.084,-65.248,-65.248)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Greenland Ice Core Projects GRIP/GISP/NGRIP
spellingShingle Greenland Ice Core Projects GRIP/GISP/NGRIP
Rasmussen, Sune Olander
Seierstad, Inger K
Andersen, Katrine K
Bigler, Matthias
Dahl-Jensen, Dorthe
Johnsen, Sigfús Jóhann
Synchronization of the NGRIP, GRIP, and GISP2 ice cores ...
topic_facet Greenland Ice Core Projects GRIP/GISP/NGRIP
description We here present a synchronization of the NGRIP, GRIP, and GISP2 ice cores based mainly on volcanic events over the period 14.9-32.45 ka b2k (before AD 2000), corresponding to Marine Isotope Stage 2 (MIS 2) and the end of MIS 3. The matching provides a basis for applying the recent NGRIP-based Greenland Ice Core Chronology 2005 (GICC05) time scale to the GRIP and GISP2 ice cores, thereby making it possible to compare the synchronized palaeoclimate profiles of the cores in detail and to identify relative accumulation differences between the cores. Based on the matching, a period of anomalous high accumulation rates in the GISP2 ice core is detected within the period 16.5-18.3 ka b2k. The d18O and [Ca2+] profiles of the three cores are presented on the common GICC05 time scale and generally show excellent agreement across the stadial-interstadial transitions and across the two characteristic dust events in Greenland Stadial 3. However, large differences between the d18O and [Ca2+] profiles of the three cores ... : Supplement to: Rasmussen, Sune Olander; Seierstad, Inger K; Andersen, Katrine K; Bigler, Matthias; Dahl-Jensen, Dorthe; Johnsen, Sigfús Jóhann (2008): Synchronization of the NGRIP, GRIP, and GISP2 ice cores across MIS 2 and palaeoclimatic implications. Quaternary Science Reviews, 27(1-2), 18-28 ...
format Article in Journal/Newspaper
author Rasmussen, Sune Olander
Seierstad, Inger K
Andersen, Katrine K
Bigler, Matthias
Dahl-Jensen, Dorthe
Johnsen, Sigfús Jóhann
author_facet Rasmussen, Sune Olander
Seierstad, Inger K
Andersen, Katrine K
Bigler, Matthias
Dahl-Jensen, Dorthe
Johnsen, Sigfús Jóhann
author_sort Rasmussen, Sune Olander
title Synchronization of the NGRIP, GRIP, and GISP2 ice cores ...
title_short Synchronization of the NGRIP, GRIP, and GISP2 ice cores ...
title_full Synchronization of the NGRIP, GRIP, and GISP2 ice cores ...
title_fullStr Synchronization of the NGRIP, GRIP, and GISP2 ice cores ...
title_full_unstemmed Synchronization of the NGRIP, GRIP, and GISP2 ice cores ...
title_sort synchronization of the ngrip, grip, and gisp2 ice cores ...
publisher PANGAEA
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.786240
https://doi.pangaea.de/10.1594/PANGAEA.786240
long_lat ENVELOPE(-64.084,-64.084,-65.248,-65.248)
geographic Greenland
Rasmussen
geographic_facet Greenland
Rasmussen
genre GISP
Greenland
Greenland ice core
GRIP
ice core
NGRIP
genre_facet GISP
Greenland
Greenland ice core
GRIP
ice core
NGRIP
op_relation https://dx.doi.org/10.1016/j.quascirev.2007.01.016
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.78624010.1016/j.quascirev.2007.01.016
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