Paleoceanography data of sediment core GS15-198-36-CC in the Denmark Strait

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Autori principali: Sessford, Evangeline, Tisserand, Amandine, Risebrobakken, Bjørg, Andersson, Carin, Dokken, Trond, Jansen, Eystein
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2018
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author Sessford, Evangeline
Tisserand, Amandine
Risebrobakken, Bjørg
Andersson, Carin
Dokken, Trond
Jansen, Eystein
author_facet Sessford, Evangeline
Tisserand, Amandine
Risebrobakken, Bjørg
Andersson, Carin
Dokken, Trond
Jansen, Eystein
collection Datos científicos de ciencias marinas y ambientales
contents The GS15-198-36CC sediment core, retrieved from the northern bank of the Greenland-Iceland Ridge, exhibits a 30-year temporal resolution during the Dansgaard-Oeschger events 8-5 (40-30 ka). Multiple proxy records were measured for this time period: magnetic susceptibility, oxygen and carbon isotopes for N. pachyderma and C. neoteretis, absolute abundance of benthic species C. neoteretis and E. excavatum, and trace element ratios of benthic species C. neoteretis. The age model for GS15-198-46CC relies on the published age model established for core PS2644-5 by using magnetic susceptibility tie points (https://doi.org/10.1594/PANGAEA.846287). The chronology is refined by stratigraphically tuning the marine magnetic record to the NGRIP δ18O record. The Mg/Ca record, which is the first for benthic species during this time period in this region, indicate warm intermediate water in the Denmark Strait during stadials and cooler water during interstadials. However, while the stadials are quite stable periods, the interstadials exhibit an instability of the water column, rapidly warming and cooling within the first half of the interstadial, and gradually warming throughout the second half. These data are supported by the stable isotopes and absolute abundance counts of the same species, C. neoteretis.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_888443
institution PANGAEA
language en
publishDate 2018
publisher PANGAEA
record_format pangaea
spellingShingle Paleoceanography data of sediment core GS15-198-36-CC in the Denmark Strait
Sessford, Evangeline
Tisserand, Amandine
Risebrobakken, Bjørg
Andersson, Carin
Dokken, Trond
Jansen, Eystein
58GS20150719; CALYPSO; Calypso Corer; G. O. Sars (2003); GS15-198; GS15-198-36-CC; Nordic Seas
The GS15-198-36CC sediment core, retrieved from the northern bank of the Greenland-Iceland Ridge, exhibits a 30-year temporal resolution during the Dansgaard-Oeschger events 8-5 (40-30 ka). Multiple proxy records were measured for this time period: magnetic susceptibility, oxygen and carbon isotopes for N. pachyderma and C. neoteretis, absolute abundance of benthic species C. neoteretis and E. excavatum, and trace element ratios of benthic species C. neoteretis. The age model for GS15-198-46CC relies on the published age model established for core PS2644-5 by using magnetic susceptibility tie points (https://doi.org/10.1594/PANGAEA.846287). The chronology is refined by stratigraphically tuning the marine magnetic record to the NGRIP δ18O record. The Mg/Ca record, which is the first for benthic species during this time period in this region, indicate warm intermediate water in the Denmark Strait during stadials and cooler water during interstadials. However, while the stadials are quite stable periods, the interstadials exhibit an instability of the water column, rapidly warming and cooling within the first half of the interstadial, and gradually warming throughout the second half. These data are supported by the stable isotopes and absolute abundance counts of the same species, C. neoteretis.
title Paleoceanography data of sediment core GS15-198-36-CC in the Denmark Strait
topic 58GS20150719; CALYPSO; Calypso Corer; G. O. Sars (2003); GS15-198; GS15-198-36-CC; Nordic Seas
url https://doi.org/10.1594/PANGAEA.888443