Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ...
Planktic foraminiferal census data, faunal sea surface temperatures (SSTs) and oxygen isotopic and lithic records from a site in the northeast Atlantic were analyzed to study the interglacial dynamics of Marine Isotope Stage (MIS) 11, a period thought to closely resemble the Holocene on the basis of...
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ftdatacite:10.1594/pangaea.675504 2024-09-30T14:40:01+00:00 Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ... Kandiano, Evgenia S Bauch, Henning A 2007 application/zip https://dx.doi.org/10.1594/pangaea.675504 https://doi.pangaea.de/10.1594/PANGAEA.675504 en eng PANGAEA https://dx.doi.org/10.1016/j.yqres.2007.07.009 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type M17/2 Meteor 1986 Collection Supplementary Publication Series of Datasets article 2007 ftdatacite https://doi.org/10.1594/pangaea.67550410.1016/j.yqres.2007.07.009 2024-09-02T08:40:50Z Planktic foraminiferal census data, faunal sea surface temperatures (SSTs) and oxygen isotopic and lithic records from a site in the northeast Atlantic were analyzed to study the interglacial dynamics of Marine Isotope Stage (MIS) 11, a period thought to closely resemble the Holocene on the basis of orbital forcing. Interglacial conditions during MIS 11 persisted for approximately 26 ka. After the main deglacial meltwater processes ceased, a 10- to 12-ka-long transitional period marked by significant water mass circulation changes occurred before surface waters finally reached their thermal maximum. This SST peak occurred between 400 and 397 ka, inferred from the abundance of the most thermophilic foraminiferal species and was coincident with lowest sea level according to benthic isotope values. The ensuing stepwise SST decrease characterizes the overall climate deterioration preceding the increase in global ice volume by ab. 3 ka. This cooling trend was followed by a more pronounced cold event that began at ... : Supplement to: Kandiano, Evgenia S; Bauch, Henning A (2007): Phase relationship and surface water mass change in the Northeast Atlantic during Marine Isotope Stage 11 (MIS 11). Quaternary Research, 68(3), 445-455 ... Article in Journal/Newspaper Northeast Atlantic DataCite |
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English |
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Gravity corer Kiel type M17/2 Meteor 1986 |
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Gravity corer Kiel type M17/2 Meteor 1986 Kandiano, Evgenia S Bauch, Henning A Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ... |
topic_facet |
Gravity corer Kiel type M17/2 Meteor 1986 |
description |
Planktic foraminiferal census data, faunal sea surface temperatures (SSTs) and oxygen isotopic and lithic records from a site in the northeast Atlantic were analyzed to study the interglacial dynamics of Marine Isotope Stage (MIS) 11, a period thought to closely resemble the Holocene on the basis of orbital forcing. Interglacial conditions during MIS 11 persisted for approximately 26 ka. After the main deglacial meltwater processes ceased, a 10- to 12-ka-long transitional period marked by significant water mass circulation changes occurred before surface waters finally reached their thermal maximum. This SST peak occurred between 400 and 397 ka, inferred from the abundance of the most thermophilic foraminiferal species and was coincident with lowest sea level according to benthic isotope values. The ensuing stepwise SST decrease characterizes the overall climate deterioration preceding the increase in global ice volume by ab. 3 ka. This cooling trend was followed by a more pronounced cold event that began at ... : Supplement to: Kandiano, Evgenia S; Bauch, Henning A (2007): Phase relationship and surface water mass change in the Northeast Atlantic during Marine Isotope Stage 11 (MIS 11). Quaternary Research, 68(3), 445-455 ... |
format |
Article in Journal/Newspaper |
author |
Kandiano, Evgenia S Bauch, Henning A |
author_facet |
Kandiano, Evgenia S Bauch, Henning A |
author_sort |
Kandiano, Evgenia S |
title |
Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ... |
title_short |
Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ... |
title_full |
Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ... |
title_fullStr |
Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ... |
title_full_unstemmed |
Ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site GIK23414 ... |
title_sort |
ice rafted debris, planktic foraminifera and reconstructed sea surface temperatures from site gik23414 ... |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.675504 https://doi.pangaea.de/10.1594/PANGAEA.675504 |
genre |
Northeast Atlantic |
genre_facet |
Northeast Atlantic |
op_relation |
https://dx.doi.org/10.1016/j.yqres.2007.07.009 |
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.67550410.1016/j.yqres.2007.07.009 |
_version_ |
1811642569242705920 |