Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ...
Abstract. The identification of sediment sources to the ocean is a prerequisite to using marine sediment cores to extract information on past climate and ocean circulation. Sr and Nd isotopes are classical tools with which to trace source provenance. Despite considerable interest in the Arctic Ocean...
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ftdatacite:10.17863/cam.25750 2024-02-04T09:57:33+01:00 Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ... Hindshaw, RS Tosca, NJ Piotrowski, AM Tipper, ET 2018 https://dx.doi.org/10.17863/cam.25750 https://www.repository.cam.ac.uk/handle/1810/278404 en eng Copernicus GmbH open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3703 Geochemistry 3705 Geology 14 Life Below Water Article ScholarlyArticle JournalArticle article-journal 2018 ftdatacite https://doi.org/10.17863/cam.25750 2024-01-05T13:51:49Z Abstract. The identification of sediment sources to the ocean is a prerequisite to using marine sediment cores to extract information on past climate and ocean circulation. Sr and Nd isotopes are classical tools with which to trace source provenance. Despite considerable interest in the Arctic Ocean, the circum-Arctic source regions are poorly characterised in terms of their Sr and Nd isotopic compositions. In this study we present Sr and Nd isotope data from the Paleogene Central Basin sediments of Svalbard, including the first published data of stream suspended sediments from Svalbard. The stream suspended sediments exhibit considerable isotopic variation (εNd = −20.6 to −13.4; 87Sr ∕ 86Sr = 0.73421 to 0.74704) which can be related to the depositional history of the sedimentary formations from which they are derived. In combination with analysis of the clay mineralogy of catchment rocks and sediments, we suggest that the Central Basin sedimentary rocks were derived from two sources. One source is ... Article in Journal/Newspaper Arctic Arctic Ocean Svalbard DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Central Basin ENVELOPE(43.000,43.000,73.500,73.500) Svalbard |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3703 Geochemistry 3705 Geology 14 Life Below Water |
spellingShingle |
37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3703 Geochemistry 3705 Geology 14 Life Below Water Hindshaw, RS Tosca, NJ Piotrowski, AM Tipper, ET Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ... |
topic_facet |
37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3703 Geochemistry 3705 Geology 14 Life Below Water |
description |
Abstract. The identification of sediment sources to the ocean is a prerequisite to using marine sediment cores to extract information on past climate and ocean circulation. Sr and Nd isotopes are classical tools with which to trace source provenance. Despite considerable interest in the Arctic Ocean, the circum-Arctic source regions are poorly characterised in terms of their Sr and Nd isotopic compositions. In this study we present Sr and Nd isotope data from the Paleogene Central Basin sediments of Svalbard, including the first published data of stream suspended sediments from Svalbard. The stream suspended sediments exhibit considerable isotopic variation (εNd = −20.6 to −13.4; 87Sr ∕ 86Sr = 0.73421 to 0.74704) which can be related to the depositional history of the sedimentary formations from which they are derived. In combination with analysis of the clay mineralogy of catchment rocks and sediments, we suggest that the Central Basin sedimentary rocks were derived from two sources. One source is ... |
format |
Article in Journal/Newspaper |
author |
Hindshaw, RS Tosca, NJ Piotrowski, AM Tipper, ET |
author_facet |
Hindshaw, RS Tosca, NJ Piotrowski, AM Tipper, ET |
author_sort |
Hindshaw, RS |
title |
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ... |
title_short |
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ... |
title_full |
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ... |
title_fullStr |
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ... |
title_full_unstemmed |
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard) ... |
title_sort |
clay mineralogy, strontium and neodymium isotope ratios in the sediments of two high arctic catchments (svalbard) ... |
publisher |
Copernicus GmbH |
publishDate |
2018 |
url |
https://dx.doi.org/10.17863/cam.25750 https://www.repository.cam.ac.uk/handle/1810/278404 |
long_lat |
ENVELOPE(43.000,43.000,73.500,73.500) |
geographic |
Arctic Arctic Ocean Central Basin Svalbard |
geographic_facet |
Arctic Arctic Ocean Central Basin Svalbard |
genre |
Arctic Arctic Ocean Svalbard |
genre_facet |
Arctic Arctic Ocean Svalbard |
op_rights |
open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.25750 |
_version_ |
1789961891521495040 |