Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551
New geochronometers are needed for sediments of the Arctic Ocean spanning at least the last half million years, largely because oxygen-isotope stratigraphy is relatively ineffective in this ocean, and because other dating techniques require significant assumptions about sedimentation rates. Multi-al...
Main Author: | |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA - Data Publisher for Earth & Environmental Science
2007
|
Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.669644 https://doi.pangaea.de/10.1594/PANGAEA.669644 |
id |
ftdatacite:10.1594/pangaea.669644 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.1594/pangaea.669644 2023-05-15T14:42:11+02:00 Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551 Berger, Glenn W 2007 application/zip https://dx.doi.org/10.1594/pangaea.669644 https://doi.pangaea.de/10.1594/PANGAEA.669644 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1016/j.quascirev.2005.07.024 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Box corer Giant gravity corer Kasten corer Gravity corer Kiel type Giant box corer Giant piston corer ARK-IV/3 ARK-VIII/3 Polarstern article Supplementary Collection of Datasets Collection 2007 ftdatacite https://doi.org/10.1594/pangaea.669644 https://doi.org/10.1016/j.quascirev.2005.07.024 2022-02-09T13:23:14Z New geochronometers are needed for sediments of the Arctic Ocean spanning at least the last half million years, largely because oxygen-isotope stratigraphy is relatively ineffective in this ocean, and because other dating techniques require significant assumptions about sedimentation rates. Multi-aliquot luminescence sediment-dating procedures were applied to polymineral, fine-silt samples from 9 core-top and 37 deeper samples from 20 cores representing 19 sites across the Arctic Ocean. Most samples have independent age assignments and other known properties (e.g., % coarse fraction, % carbonate, U-Th isotopes). Thick-source alpha-particle counting indicates that for most regions the contribution of measured unsupported 230Th and 231Pa to calculated dose rates is Article in Journal/Newspaper Arctic Arctic Ocean DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Box corer Giant gravity corer Kasten corer Gravity corer Kiel type Giant box corer Giant piston corer ARK-IV/3 ARK-VIII/3 Polarstern |
spellingShingle |
Box corer Giant gravity corer Kasten corer Gravity corer Kiel type Giant box corer Giant piston corer ARK-IV/3 ARK-VIII/3 Polarstern Berger, Glenn W Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551 |
topic_facet |
Box corer Giant gravity corer Kasten corer Gravity corer Kiel type Giant box corer Giant piston corer ARK-IV/3 ARK-VIII/3 Polarstern |
description |
New geochronometers are needed for sediments of the Arctic Ocean spanning at least the last half million years, largely because oxygen-isotope stratigraphy is relatively ineffective in this ocean, and because other dating techniques require significant assumptions about sedimentation rates. Multi-aliquot luminescence sediment-dating procedures were applied to polymineral, fine-silt samples from 9 core-top and 37 deeper samples from 20 cores representing 19 sites across the Arctic Ocean. Most samples have independent age assignments and other known properties (e.g., % coarse fraction, % carbonate, U-Th isotopes). Thick-source alpha-particle counting indicates that for most regions the contribution of measured unsupported 230Th and 231Pa to calculated dose rates is |
format |
Article in Journal/Newspaper |
author |
Berger, Glenn W |
author_facet |
Berger, Glenn W |
author_sort |
Berger, Glenn W |
title |
Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551 |
title_short |
Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551 |
title_full |
Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551 |
title_fullStr |
Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551 |
title_full_unstemmed |
Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean, supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551 |
title_sort |
fine-silt luminescence dating and mineral composition of sediments from the arctic ocean, supplement to: berger, glenn w (2006): trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. quaternary science reviews, 25(19-20), 2529-2551 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.669644 https://doi.pangaea.de/10.1594/PANGAEA.669644 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean |
genre_facet |
Arctic Arctic Ocean |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2005.07.024 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.669644 https://doi.org/10.1016/j.quascirev.2005.07.024 |
_version_ |
1766313891201024000 |