Composition of phosphorites from the ocean floor and ocean islands

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1. Verfasser: Baturin, Gleb N
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Sprache:en
Veröffentlicht: PANGAEA 2001
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author Baturin, Gleb N
author_facet Baturin, Gleb N
collection Datos científicos de ciencias marinas y ambientales
contents Rhenium contents were determined in 12 samples of oceanic phosphorites using kinetic and ICP-MS techniques, the latter of which appeared to be more correct. Rhenium contents in phosphorites from the ocean floor varied from 3 to 50 ppb, whereas that in phosphorites from the Christmas and Nauru islands are 1.3 and less <1 ppb, respectively and are similar to average rhenium content in sedimentary rocks (about 1 ppb). Rhenium does not show any relationship with phosphorus, aluminosilicates, or iron and manganese oxyhydroxides, but a correlation trend with organic carbon and total sulfur (partially bound in pyrite) is revealed. Enclosing reduced biogenic sediments enriched in hydrogenic rhenium serve as a primary rhenium source for phosphorites. Rhenium concentration in phosphorites possibly depends on duration of their presence in reduced environment and on conditions of their subsequent exposure on the ocean floor.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_761621
institution PANGAEA
language en
publishDate 2001
publisher PANGAEA
record_format pangaea
spellingShingle Composition of phosphorites from the ocean floor and ocean islands
Baturin, Gleb N
Archive of Ocean Data; ARCOD; Bat-2001-1215; Bat-2001-195; Bat-2001-2046; Bat-2001-250; Bat-2001-3150; Bat-2001-540; Bat-2001-770; Bat-2001-L-412; Bat-2001-N-3; Blake Plateau, Atlantic Ocean; Chile shelf; Christmas Island; Inner Namibia shelf; Morocco shelf; Nauru Island; Outer Namibia shelf; Yamato Rise, Sea of Japan
Rhenium contents were determined in 12 samples of oceanic phosphorites using kinetic and ICP-MS techniques, the latter of which appeared to be more correct. Rhenium contents in phosphorites from the ocean floor varied from 3 to 50 ppb, whereas that in phosphorites from the Christmas and Nauru islands are 1.3 and less <1 ppb, respectively and are similar to average rhenium content in sedimentary rocks (about 1 ppb). Rhenium does not show any relationship with phosphorus, aluminosilicates, or iron and manganese oxyhydroxides, but a correlation trend with organic carbon and total sulfur (partially bound in pyrite) is revealed. Enclosing reduced biogenic sediments enriched in hydrogenic rhenium serve as a primary rhenium source for phosphorites. Rhenium concentration in phosphorites possibly depends on duration of their presence in reduced environment and on conditions of their subsequent exposure on the ocean floor.
title Composition of phosphorites from the ocean floor and ocean islands
topic Archive of Ocean Data; ARCOD; Bat-2001-1215; Bat-2001-195; Bat-2001-2046; Bat-2001-250; Bat-2001-3150; Bat-2001-540; Bat-2001-770; Bat-2001-L-412; Bat-2001-N-3; Blake Plateau, Atlantic Ocean; Chile shelf; Christmas Island; Inner Namibia shelf; Morocco shelf; Nauru Island; Outer Namibia shelf; Yamato Rise, Sea of Japan
url https://doi.org/10.1594/PANGAEA.761621