Planktonic foraminifera and stable isotope record of ODP Site 162-980 ...
Detailed faunal, isotopic, and lithic marine records provide new insight into the stability and climate progression of the last interglacial period, Marine Isotope Stage (MIS) 5, which peaked approximately 125,000 years ago. In the eastern subpolar North Atlantic, at the latitude of Ireland, intergl...
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ftdatacite:10.1594/pangaea.742858 2024-04-28T08:29:52+00:00 Planktonic foraminifera and stable isotope record of ODP Site 162-980 ... Oppo, Delia W McManus, Jerry F Cullen, James L 2006 application/zip https://dx.doi.org/10.1594/pangaea.742858 https://doi.pangaea.de/10.1594/PANGAEA.742858 en eng PANGAEA ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.txt https://dx.doi.org/10.1016/j.quascirev.2006.07.006 ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.txt Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Leg162 Joides Resolution Ocean Drilling Program ODP article Supplementary Publication Series of Datasets Collection 2006 ftdatacite https://doi.org/10.1594/pangaea.74285810.1016/j.quascirev.2006.07.006 2024-04-02T10:00:39Z Detailed faunal, isotopic, and lithic marine records provide new insight into the stability and climate progression of the last interglacial period, Marine Isotope Stage (MIS) 5, which peaked approximately 125,000 years ago. In the eastern subpolar North Atlantic, at the latitude of Ireland, interglacial warmth of the ice volume minimum of substage 5e (MIS 5e) lasted ~10,000 years (10 ka) and its demise occurred in two cooling steps. The first cooling step marked the end of the climatic optimum, which was 2-3 ka long. Minor ice rafting accompanied each cooling step; the second, larger, step encompassing cold events C26 and C25 was previously identified in the northwestern Atlantic. Approximately 4 °C of cooling occurred between peak interglacial warmth and C25, and the region experienced an additional temporary cooling of at least 1-2 °C during C24, a cooling event associated with widespread ice rafting in the North Atlantic. Beginning with C24, MIS 5 was characterized by oscillations of at least 1-2 °C ... : Supplement to: Oppo, Delia W; McManus, Jerry F; Cullen, James L (2006): Evolution and demise of the Last Interglacial warmth in the subpolar North Atlantic. Quaternary Science Reviews, 25(23-24), 3268-3277 ... Article in Journal/Newspaper North Atlantic Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Composite Core Leg162 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Composite Core Leg162 Joides Resolution Ocean Drilling Program ODP Oppo, Delia W McManus, Jerry F Cullen, James L Planktonic foraminifera and stable isotope record of ODP Site 162-980 ... |
topic_facet |
Composite Core Leg162 Joides Resolution Ocean Drilling Program ODP |
description |
Detailed faunal, isotopic, and lithic marine records provide new insight into the stability and climate progression of the last interglacial period, Marine Isotope Stage (MIS) 5, which peaked approximately 125,000 years ago. In the eastern subpolar North Atlantic, at the latitude of Ireland, interglacial warmth of the ice volume minimum of substage 5e (MIS 5e) lasted ~10,000 years (10 ka) and its demise occurred in two cooling steps. The first cooling step marked the end of the climatic optimum, which was 2-3 ka long. Minor ice rafting accompanied each cooling step; the second, larger, step encompassing cold events C26 and C25 was previously identified in the northwestern Atlantic. Approximately 4 °C of cooling occurred between peak interglacial warmth and C25, and the region experienced an additional temporary cooling of at least 1-2 °C during C24, a cooling event associated with widespread ice rafting in the North Atlantic. Beginning with C24, MIS 5 was characterized by oscillations of at least 1-2 °C ... : Supplement to: Oppo, Delia W; McManus, Jerry F; Cullen, James L (2006): Evolution and demise of the Last Interglacial warmth in the subpolar North Atlantic. Quaternary Science Reviews, 25(23-24), 3268-3277 ... |
format |
Article in Journal/Newspaper |
author |
Oppo, Delia W McManus, Jerry F Cullen, James L |
author_facet |
Oppo, Delia W McManus, Jerry F Cullen, James L |
author_sort |
Oppo, Delia W |
title |
Planktonic foraminifera and stable isotope record of ODP Site 162-980 ... |
title_short |
Planktonic foraminifera and stable isotope record of ODP Site 162-980 ... |
title_full |
Planktonic foraminifera and stable isotope record of ODP Site 162-980 ... |
title_fullStr |
Planktonic foraminifera and stable isotope record of ODP Site 162-980 ... |
title_full_unstemmed |
Planktonic foraminifera and stable isotope record of ODP Site 162-980 ... |
title_sort |
planktonic foraminifera and stable isotope record of odp site 162-980 ... |
publisher |
PANGAEA |
publishDate |
2006 |
url |
https://dx.doi.org/10.1594/pangaea.742858 https://doi.pangaea.de/10.1594/PANGAEA.742858 |
genre |
North Atlantic Planktonic foraminifera |
genre_facet |
North Atlantic Planktonic foraminifera |
op_relation |
ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.txt https://dx.doi.org/10.1016/j.quascirev.2006.07.006 ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.txt |
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.74285810.1016/j.quascirev.2006.07.006 |
_version_ |
1797587931437727744 |