Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ...
In order to study the modern sea surface characteristics of the sub-polar North Pacific and the Bering Sea, i.e. sea surface temperature (SST) and sea ice cover, surface sediments recovered during the RV Sonne Expedition 202 in 2009 were analysed. To distinguish between marine and terrestrial organi...
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ftdatacite:10.1594/pangaea.804518 2023-10-01T03:51:39+02:00 Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ... Méheust, Marie Fahl, Kirsten Stein, Ruediger 2013 application/zip https://dx.doi.org/10.1594/pangaea.804518 https://doi.pangaea.de/10.1594/PANGAEA.804518 en eng PANGAEA https://dx.doi.org/10.1016/j.orggeochem.2013.01.008 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Supplementary Publication Series of Datasets article Collection 2013 ftdatacite https://doi.org/10.1594/pangaea.80451810.1016/j.orggeochem.2013.01.008 2023-09-04T14:52:34Z In order to study the modern sea surface characteristics of the sub-polar North Pacific and the Bering Sea, i.e. sea surface temperature (SST) and sea ice cover, surface sediments recovered during the RV Sonne Expedition 202 in 2009 were analysed. To distinguish between marine and terrestrial organic carbon, hydrogen index values, long chain n-alkanes and specific sterols have been determined. The results show that in the Bering Sea, especially on the sea slope, the organic carbon source is mainly caused by high primary production. In the North Pacific, on the other hand, the organic material originates predominantly from terrestrial higher plants, probably related to dust input from Asia. SST has been reconstructed using the modified alkenone unsaturation index. Calibration from Müller et al. (1998, doi:10.1016/S0016-7037(98)00097-0) offers the most reliable estimate of mean annual temperature in the central North Pacific but does not correlate with mean annual temperature throughout the study area. In the ... : Supplement to: Méheust, Marie; Fahl, Kirsten; Stein, Ruediger (2013): Variability in modern sea surface temperature, sea ice and terrigenous input in the sub-polar North Pacific and Bering Sea: Reconstruction from biomarker data. Organic Geochemistry, 57, 54-64 ... Article in Journal/Newspaper Antarc* Antarctic Arctic Bering Sea Sea ice DataCite Metadata Store (German National Library of Science and Technology) Antarctic Arctic Bering Sea Pacific |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
English |
topic |
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Méheust, Marie Fahl, Kirsten Stein, Ruediger Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ... |
topic_facet |
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
In order to study the modern sea surface characteristics of the sub-polar North Pacific and the Bering Sea, i.e. sea surface temperature (SST) and sea ice cover, surface sediments recovered during the RV Sonne Expedition 202 in 2009 were analysed. To distinguish between marine and terrestrial organic carbon, hydrogen index values, long chain n-alkanes and specific sterols have been determined. The results show that in the Bering Sea, especially on the sea slope, the organic carbon source is mainly caused by high primary production. In the North Pacific, on the other hand, the organic material originates predominantly from terrestrial higher plants, probably related to dust input from Asia. SST has been reconstructed using the modified alkenone unsaturation index. Calibration from Müller et al. (1998, doi:10.1016/S0016-7037(98)00097-0) offers the most reliable estimate of mean annual temperature in the central North Pacific but does not correlate with mean annual temperature throughout the study area. In the ... : Supplement to: Méheust, Marie; Fahl, Kirsten; Stein, Ruediger (2013): Variability in modern sea surface temperature, sea ice and terrigenous input in the sub-polar North Pacific and Bering Sea: Reconstruction from biomarker data. Organic Geochemistry, 57, 54-64 ... |
format |
Article in Journal/Newspaper |
author |
Méheust, Marie Fahl, Kirsten Stein, Ruediger |
author_facet |
Méheust, Marie Fahl, Kirsten Stein, Ruediger |
author_sort |
Méheust, Marie |
title |
Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ... |
title_short |
Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ... |
title_full |
Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ... |
title_fullStr |
Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ... |
title_full_unstemmed |
Biomarker distributions and calculated sea surface temperatures from the North Pacific Ocean ... |
title_sort |
biomarker distributions and calculated sea surface temperatures from the north pacific ocean ... |
publisher |
PANGAEA |
publishDate |
2013 |
url |
https://dx.doi.org/10.1594/pangaea.804518 https://doi.pangaea.de/10.1594/PANGAEA.804518 |
geographic |
Antarctic Arctic Bering Sea Pacific |
geographic_facet |
Antarctic Arctic Bering Sea Pacific |
genre |
Antarc* Antarctic Arctic Bering Sea Sea ice |
genre_facet |
Antarc* Antarctic Arctic Bering Sea Sea ice |
op_relation |
https://dx.doi.org/10.1016/j.orggeochem.2013.01.008 |
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.80451810.1016/j.orggeochem.2013.01.008 |
_version_ |
1778516815784181760 |