Geochemistry of IODP Site 306-U1314 ...

Integrated Ocean Drilling Program (IODP) Site U1314 of the North Atlantic is a critical sedimentary archive record of subpolar deep water from the southern Gardar Drift for which we derived an age model of orbital resolution for the last 1.8 Ma. This chronology combined with high-resolution (cm scal...

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Main Authors: Gruetzner, Jens, Higgins, Sean M
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.770384
https://doi.pangaea.de/10.1594/PANGAEA.770384
id ftdatacite:10.1594/pangaea.770384
record_format openpolar
spelling ftdatacite:10.1594/pangaea.770384 2024-09-30T14:37:25+00:00 Geochemistry of IODP Site 306-U1314 ... Gruetzner, Jens Higgins, Sean M 2010 application/zip https://dx.doi.org/10.1594/pangaea.770384 https://doi.pangaea.de/10.1594/PANGAEA.770384 en eng PANGAEA https://dx.doi.org/10.1029/2009pa001873 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Exp306 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Collection Supplementary Publication Series of Datasets article 2010 ftdatacite https://doi.org/10.1594/pangaea.77038410.1029/2009pa001873 2024-09-02T08:39:17Z Integrated Ocean Drilling Program (IODP) Site U1314 of the North Atlantic is a critical sedimentary archive record of subpolar deep water from the southern Gardar Drift for which we derived an age model of orbital resolution for the last 1.8 Ma. This chronology combined with high-resolution (cm scale) X-ray fluorescence core scanning measurements of major elements allows tracking changes in terrigenous provenance during the last 1.1 Ma. Low Potassium to Titanium (K/Ti) ratios reflect enhanced transport of basalt-derived titanomagnetites during warm climate intervals, while high K/Ti ratios indicate a dominance of acidic sediment sources typical for glacial and stadial events. Changes in K/Ti and magnetic concentration at Site 1314 are coeval with fluctuations in smectite content and grain size data from nearby piston cores, suggesting that the provenance changes are mainly controlled by variable flow of the Iceland-Scotland Overflow Water, an important branch of North Atlantic Deep Water. Furthermore, K/Ti ... : Supplement to: Gruetzner, Jens; Higgins, Sean M (2010): Threshold behavior of millennial scale variability in deep water hydrography inferred from a 1.1 Ma long record of sediment provenance at the southern Gardar Drift. Paleoceanography, 25, PA4204 ... Article in Journal/Newspaper Iceland North Atlantic Deep Water North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Exp306
Joides Resolution
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
spellingShingle Composite Core
Exp306
Joides Resolution
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Gruetzner, Jens
Higgins, Sean M
Geochemistry of IODP Site 306-U1314 ...
topic_facet Composite Core
Exp306
Joides Resolution
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
description Integrated Ocean Drilling Program (IODP) Site U1314 of the North Atlantic is a critical sedimentary archive record of subpolar deep water from the southern Gardar Drift for which we derived an age model of orbital resolution for the last 1.8 Ma. This chronology combined with high-resolution (cm scale) X-ray fluorescence core scanning measurements of major elements allows tracking changes in terrigenous provenance during the last 1.1 Ma. Low Potassium to Titanium (K/Ti) ratios reflect enhanced transport of basalt-derived titanomagnetites during warm climate intervals, while high K/Ti ratios indicate a dominance of acidic sediment sources typical for glacial and stadial events. Changes in K/Ti and magnetic concentration at Site 1314 are coeval with fluctuations in smectite content and grain size data from nearby piston cores, suggesting that the provenance changes are mainly controlled by variable flow of the Iceland-Scotland Overflow Water, an important branch of North Atlantic Deep Water. Furthermore, K/Ti ... : Supplement to: Gruetzner, Jens; Higgins, Sean M (2010): Threshold behavior of millennial scale variability in deep water hydrography inferred from a 1.1 Ma long record of sediment provenance at the southern Gardar Drift. Paleoceanography, 25, PA4204 ...
format Article in Journal/Newspaper
author Gruetzner, Jens
Higgins, Sean M
author_facet Gruetzner, Jens
Higgins, Sean M
author_sort Gruetzner, Jens
title Geochemistry of IODP Site 306-U1314 ...
title_short Geochemistry of IODP Site 306-U1314 ...
title_full Geochemistry of IODP Site 306-U1314 ...
title_fullStr Geochemistry of IODP Site 306-U1314 ...
title_full_unstemmed Geochemistry of IODP Site 306-U1314 ...
title_sort geochemistry of iodp site 306-u1314 ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.770384
https://doi.pangaea.de/10.1594/PANGAEA.770384
genre Iceland
North Atlantic Deep Water
North Atlantic
genre_facet Iceland
North Atlantic Deep Water
North Atlantic
op_relation https://dx.doi.org/10.1029/2009pa001873
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.77038410.1029/2009pa001873
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