Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ...
TEX86 (tetraether index of 86 carbon atoms) is an organic paleotemperatureproxy based on the relative abundances of thaumarcheal isoprenoid glycerol dialkyl glycerol tetraethers (iGDGTs). The calibration is based on global core top sediments. The global core top calibrations of TEX86 are often not r...
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ftdatacite:10.1594/pangaea.894308 2024-09-15T17:36:41+00:00 Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ... Schukies, Julian 2018 application/zip https://dx.doi.org/10.1594/pangaea.894308 https://doi.pangaea.de/10.1594/PANGAEA.894308 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 article Collection Supplementary Publication Series of Datasets 2018 ftdatacite https://doi.org/10.1594/pangaea.894308 2024-08-01T10:59:23Z TEX86 (tetraether index of 86 carbon atoms) is an organic paleotemperatureproxy based on the relative abundances of thaumarcheal isoprenoid glycerol dialkyl glycerol tetraethers (iGDGTs). The calibration is based on global core top sediments. The global core top calibrations of TEX86 are often not reliable for reconstructions of watertemperatures in regions with distinct hydrographic conditions. In the area of the continental edge of Newfoundland (Northwest Atlantic), hydrographic conditions are mainly determined by the Labrador- and the North Atlantic Current. Thus, the region differs from the global ocean. In this study the accuracy of temperature estimations of TEX86 was tested at the realm of the continental edge off Newfoundland. For this purpose, GDGT distribution in suspended particulate matter of water surface and core top sediments was analysed. Based on the GDGT composition, the influence of the regional environmental factors on the TEX86 proxy was investigated. Based on TEX-signals of the samples, ... : Supplement to: Schukies, Julian (2018): Prüfung der Anwendbarkeit des TEX86 in Proben partikulären organischen Materials und Oberflächensedimenten im Bereich des Zusammentreffens von Nordatlantik- und Labradorstrom am Kontinentalhang vor Neufundland, NW Atlantik. Master thesis, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany (unpublished) ... Article in Journal/Newspaper Alfred Wegener Institute Newfoundland north atlantic current North Atlantic Northwest Atlantic DataCite |
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English |
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TEX86 (tetraether index of 86 carbon atoms) is an organic paleotemperatureproxy based on the relative abundances of thaumarcheal isoprenoid glycerol dialkyl glycerol tetraethers (iGDGTs). The calibration is based on global core top sediments. The global core top calibrations of TEX86 are often not reliable for reconstructions of watertemperatures in regions with distinct hydrographic conditions. In the area of the continental edge of Newfoundland (Northwest Atlantic), hydrographic conditions are mainly determined by the Labrador- and the North Atlantic Current. Thus, the region differs from the global ocean. In this study the accuracy of temperature estimations of TEX86 was tested at the realm of the continental edge off Newfoundland. For this purpose, GDGT distribution in suspended particulate matter of water surface and core top sediments was analysed. Based on the GDGT composition, the influence of the regional environmental factors on the TEX86 proxy was investigated. Based on TEX-signals of the samples, ... : Supplement to: Schukies, Julian (2018): Prüfung der Anwendbarkeit des TEX86 in Proben partikulären organischen Materials und Oberflächensedimenten im Bereich des Zusammentreffens von Nordatlantik- und Labradorstrom am Kontinentalhang vor Neufundland, NW Atlantik. Master thesis, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany (unpublished) ... |
format |
Article in Journal/Newspaper |
author |
Schukies, Julian |
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Schukies, Julian Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ... |
author_facet |
Schukies, Julian |
author_sort |
Schukies, Julian |
title |
Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ... |
title_short |
Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ... |
title_full |
Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ... |
title_fullStr |
Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ... |
title_full_unstemmed |
Organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off Newfoundland during Maria S. Merian Expedition MSM39 in June 2014 ... |
title_sort |
organic paleotemperature proxies in suspended particulate matter and sediment core tops from continatal slope off newfoundland during maria s. merian expedition msm39 in june 2014 ... |
publisher |
PANGAEA |
publishDate |
2018 |
url |
https://dx.doi.org/10.1594/pangaea.894308 https://doi.pangaea.de/10.1594/PANGAEA.894308 |
genre |
Alfred Wegener Institute Newfoundland north atlantic current North Atlantic Northwest Atlantic |
genre_facet |
Alfred Wegener Institute Newfoundland north atlantic current North Atlantic Northwest Atlantic |
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.894308 |
_version_ |
1810491313743724544 |