Depth tie points and ages 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.830906
https://doi.pangaea.de/10.1594/PANGAEA.830906
id ftdatacite:10.1594/pangaea.830906
record_format openpolar
spelling ftdatacite:10.1594/pangaea.830906 2024-09-15T18:14:10+00:00 Depth tie points and ages of IODP Site 306-U1314 ... Gruetzner, Jens Higgins, Sean M 2010 application/zip https://dx.doi.org/10.1594/pangaea.830906 https://doi.pangaea.de/10.1594/PANGAEA.830906 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 Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2010 ftdatacite https://doi.org/10.1594/pangaea.83090610.1029/2009pa001873 2024-08-01T11:01:35Z 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(4), 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 Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Ocean Drilling Program ODP
spellingShingle Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Ocean Drilling Program ODP
Gruetzner, Jens
Higgins, Sean M
Depth tie points and ages of IODP Site 306-U1314 ...
topic_facet Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Ocean Drilling Program ODP
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(4), PA4204 ...
format Article in Journal/Newspaper
author Gruetzner, Jens
Higgins, Sean M
author_facet Gruetzner, Jens
Higgins, Sean M
author_sort Gruetzner, Jens
title Depth tie points and ages of IODP Site 306-U1314 ...
title_short Depth tie points and ages of IODP Site 306-U1314 ...
title_full Depth tie points and ages of IODP Site 306-U1314 ...
title_fullStr Depth tie points and ages of IODP Site 306-U1314 ...
title_full_unstemmed Depth tie points and ages of IODP Site 306-U1314 ...
title_sort depth tie points and ages of iodp site 306-u1314 ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.830906
https://doi.pangaea.de/10.1594/PANGAEA.830906
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.83090610.1029/2009pa001873
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