Major and trace element concentrations of sediments from the IODP Exp302 sites ...
We analyzed a suite of sediment samples recovered in the central Arctic Ocean for major, trace, and rare earth elements in order to assess changes in terrigenous source material throughout the Cenozoic. The terrigenous component consists of two end-members. Input from a shale-like composition domina...
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ftdatacite:10.1594/pangaea.787157 2024-09-15T17:53:25+00:00 Major and trace element concentrations of sediments from the IODP Exp302 sites ... Martinez, Nahysa C Murray, Richard W Dickens, Gerald Roy Kölling, Martin 2009 application/zip https://dx.doi.org/10.1594/pangaea.787157 https://doi.pangaea.de/10.1594/PANGAEA.787157 en eng PANGAEA https://dx.doi.org/10.1029/2007pa001567 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Integrated Ocean Drilling Program / International Ocean Discovery Program IODP article Collection Supplementary Publication Series of Datasets 2009 ftdatacite https://doi.org/10.1594/pangaea.78715710.1029/2007pa001567 2024-08-01T10:57:37Z We analyzed a suite of sediment samples recovered in the central Arctic Ocean for major, trace, and rare earth elements in order to assess changes in terrigenous source material throughout the Cenozoic. The terrigenous component consists of two end-members. Input from a shale-like composition dominates bulk sediments, especially those deposited during the Paleocene and since the Miocene, and may represent sediment supply from the eastern Laptev Sea. Therefore, even though the environment and transport mechanisms may have varied from ice free to ice dominated, sequences of the early Paleogene and later Neogene appear to have been influenced by a single major terrigenous source. This suggests similar transport capabilities and trajectories for both ocean and drift currents through significant parts of the Cenozoic. Influence from a more mafic source appears to be more important through the early Eocene to the middle Miocene and most likely represents material from the western Laptev Sea or Kara Sea. Thus, ... : Supplement to: Martinez, Nahysa C; Murray, Richard W; Dickens, Gerald Roy; Kölling, Martin (2009): Discrimination of sources of terrigenous sediment deposited in the central Arctic Ocean through the Cenozoic. Paleoceanography, 24, PA1210 ... Article in Journal/Newspaper Arctic Ocean Kara Sea laptev Laptev Sea DataCite |
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English |
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Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
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Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Martinez, Nahysa C Murray, Richard W Dickens, Gerald Roy Kölling, Martin Major and trace element concentrations of sediments from the IODP Exp302 sites ... |
topic_facet |
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
description |
We analyzed a suite of sediment samples recovered in the central Arctic Ocean for major, trace, and rare earth elements in order to assess changes in terrigenous source material throughout the Cenozoic. The terrigenous component consists of two end-members. Input from a shale-like composition dominates bulk sediments, especially those deposited during the Paleocene and since the Miocene, and may represent sediment supply from the eastern Laptev Sea. Therefore, even though the environment and transport mechanisms may have varied from ice free to ice dominated, sequences of the early Paleogene and later Neogene appear to have been influenced by a single major terrigenous source. This suggests similar transport capabilities and trajectories for both ocean and drift currents through significant parts of the Cenozoic. Influence from a more mafic source appears to be more important through the early Eocene to the middle Miocene and most likely represents material from the western Laptev Sea or Kara Sea. Thus, ... : Supplement to: Martinez, Nahysa C; Murray, Richard W; Dickens, Gerald Roy; Kölling, Martin (2009): Discrimination of sources of terrigenous sediment deposited in the central Arctic Ocean through the Cenozoic. Paleoceanography, 24, PA1210 ... |
format |
Article in Journal/Newspaper |
author |
Martinez, Nahysa C Murray, Richard W Dickens, Gerald Roy Kölling, Martin |
author_facet |
Martinez, Nahysa C Murray, Richard W Dickens, Gerald Roy Kölling, Martin |
author_sort |
Martinez, Nahysa C |
title |
Major and trace element concentrations of sediments from the IODP Exp302 sites ... |
title_short |
Major and trace element concentrations of sediments from the IODP Exp302 sites ... |
title_full |
Major and trace element concentrations of sediments from the IODP Exp302 sites ... |
title_fullStr |
Major and trace element concentrations of sediments from the IODP Exp302 sites ... |
title_full_unstemmed |
Major and trace element concentrations of sediments from the IODP Exp302 sites ... |
title_sort |
major and trace element concentrations of sediments from the iodp exp302 sites ... |
publisher |
PANGAEA |
publishDate |
2009 |
url |
https://dx.doi.org/10.1594/pangaea.787157 https://doi.pangaea.de/10.1594/PANGAEA.787157 |
genre |
Arctic Ocean Kara Sea laptev Laptev Sea |
genre_facet |
Arctic Ocean Kara Sea laptev Laptev Sea |
op_relation |
https://dx.doi.org/10.1029/2007pa001567 |
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.78715710.1029/2007pa001567 |
_version_ |
1810295505432870912 |