Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ...

Contents of Fe, Mn, Al, P, and rare earth elements (REE) in ferruginous nodules and host sediments of the eastern Barents Sea were studied. A direct Fe-P correlation in reactive components of the sediments and nodules was found. The nodules were shown to be formed through Fe(II) oxidation in the sur...

Full description

Bibliographic Details
Main Authors: Strekopytov, Stanislav V, Dubinin, Alexander V
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.761137
https://doi.pangaea.de/10.1594/PANGAEA.761137
id ftdatacite:10.1594/pangaea.761137
record_format openpolar
spelling ftdatacite:10.1594/pangaea.761137 2024-09-09T19:32:04+00:00 Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ... Strekopytov, Stanislav V Dubinin, Alexander V 2001 application/zip https://dx.doi.org/10.1594/pangaea.761137 https://doi.pangaea.de/10.1594/PANGAEA.761137 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Box corer Grab ASV11 Akademik Sergey Vavilov Archive of Ocean Data ARCOD article Collection Supplementary Publication Series of Datasets 2001 ftdatacite https://doi.org/10.1594/pangaea.761137 2024-08-01T10:54:23Z Contents of Fe, Mn, Al, P, and rare earth elements (REE) in ferruginous nodules and host sediments of the eastern Barents Sea were studied. A direct Fe-P correlation in reactive components of the sediments and nodules was found. The nodules were shown to be formed through Fe(II) oxidation in the surface layer of sediments and cementation of terrigenous fraction of sediments by Fe(III) oxyhydroxides. The latter accumulate phosphorus due to processes of sorption - co-precipitation, by forming Fe(III) hydrophosphates. REE composition in the sediments and nodules normalized to NASC contents is characterized by increased proportion of light REE that may be caused by regional features of their sources. Due to significant share of terrigenous matter in the Fe nodules (up to 65% for Nd), REE composition of bulk samples is similar to that of host sediments. A negative cerium anomaly in composition of reactive REE may result from REE sorption from seawater. REE bulk composition of a ferruginous crust is closer to that ... : Supplement to: Strekopytov, Stanislav V; Dubinin, Alexander V (2001): On the geochemistry of ferriginous concretions of the Barents Sea. Translated from Okeanologiya, 2001, 41(3), 386-393, Oceanology, 41(3), 367-374 ... Article in Journal/Newspaper Barents Sea DataCite Barents Sea
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Box corer
Grab
ASV11
Akademik Sergey Vavilov
Archive of Ocean Data ARCOD
spellingShingle Box corer
Grab
ASV11
Akademik Sergey Vavilov
Archive of Ocean Data ARCOD
Strekopytov, Stanislav V
Dubinin, Alexander V
Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ...
topic_facet Box corer
Grab
ASV11
Akademik Sergey Vavilov
Archive of Ocean Data ARCOD
description Contents of Fe, Mn, Al, P, and rare earth elements (REE) in ferruginous nodules and host sediments of the eastern Barents Sea were studied. A direct Fe-P correlation in reactive components of the sediments and nodules was found. The nodules were shown to be formed through Fe(II) oxidation in the surface layer of sediments and cementation of terrigenous fraction of sediments by Fe(III) oxyhydroxides. The latter accumulate phosphorus due to processes of sorption - co-precipitation, by forming Fe(III) hydrophosphates. REE composition in the sediments and nodules normalized to NASC contents is characterized by increased proportion of light REE that may be caused by regional features of their sources. Due to significant share of terrigenous matter in the Fe nodules (up to 65% for Nd), REE composition of bulk samples is similar to that of host sediments. A negative cerium anomaly in composition of reactive REE may result from REE sorption from seawater. REE bulk composition of a ferruginous crust is closer to that ... : Supplement to: Strekopytov, Stanislav V; Dubinin, Alexander V (2001): On the geochemistry of ferriginous concretions of the Barents Sea. Translated from Okeanologiya, 2001, 41(3), 386-393, Oceanology, 41(3), 367-374 ...
format Article in Journal/Newspaper
author Strekopytov, Stanislav V
Dubinin, Alexander V
author_facet Strekopytov, Stanislav V
Dubinin, Alexander V
author_sort Strekopytov, Stanislav V
title Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ...
title_short Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ...
title_full Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ...
title_fullStr Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ...
title_full_unstemmed Major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the Barents Sea ...
title_sort major and rare earth element contents and their speciations in ferruginous nodules and host sediments from the barents sea ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.761137
https://doi.pangaea.de/10.1594/PANGAEA.761137
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
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.761137
_version_ 1809900865313570816