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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Main Authors: Hindshaw, RS, Tosca, NJ, Piotrowski, AM, Tipper, ET
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2018
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.25750
https://www.repository.cam.ac.uk/handle/1810/278404
id ftdatacite:10.17863/cam.25750
record_format openpolar
spelling 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
institution 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
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