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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Main Authors: Martinez, Nahysa C, Murray, Richard W, Dickens, Gerald Roy, Kölling, Martin
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.787157
https://doi.pangaea.de/10.1594/PANGAEA.787157
id ftdatacite:10.1594/pangaea.787157
record_format openpolar
spelling 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
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
spellingShingle 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
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