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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Online Access: | https://dx.doi.org/10.1594/pangaea.786240 https://doi.pangaea.de/10.1594/PANGAEA.786240 |
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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 |
_version_ |
1809910580573634560 |