Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ...

Near-surface sediments from the equatorial east Atlantic and the Norwegian Sea exhibit pronounced shear strength maxima in profiles from the peak Holocene and Pleistocene. These semi-indurated layers start to occur at 8-102 cm below the sediment surface and can be explained neither by the modal comp...

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Bibliographic Details
Main Authors: Kassens, Heidemarie, Sarnthein, Michael
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
M65
Online Access:https://dx.doi.org/10.1594/pangaea.696097
https://doi.pangaea.de/10.1594/PANGAEA.696097
id ftdatacite:10.1594/pangaea.696097
record_format openpolar
spelling ftdatacite:10.1594/pangaea.696097 2024-09-15T18:26:44+00:00 Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ... Kassens, Heidemarie Sarnthein, Michael 1989 application/zip https://dx.doi.org/10.1594/pangaea.696097 https://doi.pangaea.de/10.1594/PANGAEA.696097 en eng PANGAEA https://dx.doi.org/10.1029/pa004i003p00253 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box corer Box corer Gravity corer Kasten corer M65 ANT-IV/1c M2/2 Meteor 1964 Polarstern Meteor 1986 Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 1989 ftdatacite https://doi.org/10.1594/pangaea.69609710.1029/pa004i003p00253 2024-07-03T13:10:33Z Near-surface sediments from the equatorial east Atlantic and the Norwegian Sea exhibit pronounced shear strength maxima in profiles from the peak Holocene and Pleistocene. These semi-indurated layers start to occur at 8-102 cm below the sediment surface and can be explained neither by the modal composition nor by the effective overburden pressure of the sediments. However, scanning electron microscope and microprobe data exhibit micritic crusts and crystal carpets, which are clearly restricted to (undisturbed) samples from indurated layers and form a manifest explanation for their origin. The minerals precipitated comprise calcite, aragonite, and in samples more proximal to the African continent SiO2 needles, and needles of as yet unidentified K-Mg-Fe-Al silicates, crusts of which dominate the indurated layers in the Norwegian Sea. By their stratigraphic position in deep-sea sediments the carbonate-based shear strength maxima are tentatively ascribed to dissolved adjacent pteropod layers from the early ... : Supplement to: Kassens, Heidemarie; Sarnthein, Michael (1989): A link between paleoceanography, early diagenetic cementation, and shear strength maxima in Late Quaternary deep-sea sediments? Paleoceanography, 4(3), 253-269 ... Article in Journal/Newspaper Norwegian Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Giant box corer
Box corer
Gravity corer
Kasten corer
M65
ANT-IV/1c
M2/2
Meteor 1964
Polarstern
Meteor 1986
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
Quaternary Environment of the Eurasian North QUEEN
spellingShingle Giant box corer
Box corer
Gravity corer
Kasten corer
M65
ANT-IV/1c
M2/2
Meteor 1964
Polarstern
Meteor 1986
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
Quaternary Environment of the Eurasian North QUEEN
Kassens, Heidemarie
Sarnthein, Michael
Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ...
topic_facet Giant box corer
Box corer
Gravity corer
Kasten corer
M65
ANT-IV/1c
M2/2
Meteor 1964
Polarstern
Meteor 1986
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
Quaternary Environment of the Eurasian North QUEEN
description Near-surface sediments from the equatorial east Atlantic and the Norwegian Sea exhibit pronounced shear strength maxima in profiles from the peak Holocene and Pleistocene. These semi-indurated layers start to occur at 8-102 cm below the sediment surface and can be explained neither by the modal composition nor by the effective overburden pressure of the sediments. However, scanning electron microscope and microprobe data exhibit micritic crusts and crystal carpets, which are clearly restricted to (undisturbed) samples from indurated layers and form a manifest explanation for their origin. The minerals precipitated comprise calcite, aragonite, and in samples more proximal to the African continent SiO2 needles, and needles of as yet unidentified K-Mg-Fe-Al silicates, crusts of which dominate the indurated layers in the Norwegian Sea. By their stratigraphic position in deep-sea sediments the carbonate-based shear strength maxima are tentatively ascribed to dissolved adjacent pteropod layers from the early ... : Supplement to: Kassens, Heidemarie; Sarnthein, Michael (1989): A link between paleoceanography, early diagenetic cementation, and shear strength maxima in Late Quaternary deep-sea sediments? Paleoceanography, 4(3), 253-269 ...
format Article in Journal/Newspaper
author Kassens, Heidemarie
Sarnthein, Michael
author_facet Kassens, Heidemarie
Sarnthein, Michael
author_sort Kassens, Heidemarie
title Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ...
title_short Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ...
title_full Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ...
title_fullStr Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ...
title_full_unstemmed Grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial Atlantic and the Norwegian Sea ...
title_sort grain size distribution, carbon content and wet bulk density of sediment cores in the equatorial atlantic and the norwegian sea ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.696097
https://doi.pangaea.de/10.1594/PANGAEA.696097
genre Norwegian Sea
genre_facet Norwegian Sea
op_relation https://dx.doi.org/10.1029/pa004i003p00253
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.69609710.1029/pa004i003p00253
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