Chemical composition of ferromanganese nodules from the Black Sea

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Autores principales: Baturin, Gleb N, Gorshkov, Anatoly I, Magazina, Larissa O, Bogdanova, Olga Yu
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2002
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author Baturin, Gleb N
Gorshkov, Anatoly I
Magazina, Larissa O
Bogdanova, Olga Yu
author_facet Baturin, Gleb N
Gorshkov, Anatoly I
Magazina, Larissa O
Bogdanova, Olga Yu
collection Datos científicos de ciencias marinas y ambientales
contents Ferruginate shells and tubular worm burrows from the oxygenated zone of the Black Sea (Kalamit Bay and Danube River mouth) are studied by transmission and scanning electron microscopy combined with analyses of elemental composition. Iron and manganese oxyhydroxide nodules considered here are enriched in phosphorus. They contain variable amounts of terrigenous and biogenic material derived from host sediments. Oxyhydroxides are mainly characterized by colloform structure, whereas globular and crystalline structures are less common. The dominating iron phase is represented by ferroxyhite and protoferroxyhite, whereas the manganese phase is composed of Fe-free vernadite. Concentrations of Mn, As, and Mo are 12-18 times higher relative to sediments, while concentrations of Fe, P, Ni, and Co increase 5-7 times during nodule formation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_783709
institution PANGAEA
language en
publishDate 2002
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of ferromanganese nodules from the Black Sea
Baturin, Gleb N
Gorshkov, Anatoly I
Magazina, Larissa O
Bogdanova, Olga Yu
Archive of Ocean Data; ARCOD; Black Sea; MULT; Multiple investigations; Vy8-798; Vy8-800; Vy8-802; Vy8-848
Ferruginate shells and tubular worm burrows from the oxygenated zone of the Black Sea (Kalamit Bay and Danube River mouth) are studied by transmission and scanning electron microscopy combined with analyses of elemental composition. Iron and manganese oxyhydroxide nodules considered here are enriched in phosphorus. They contain variable amounts of terrigenous and biogenic material derived from host sediments. Oxyhydroxides are mainly characterized by colloform structure, whereas globular and crystalline structures are less common. The dominating iron phase is represented by ferroxyhite and protoferroxyhite, whereas the manganese phase is composed of Fe-free vernadite. Concentrations of Mn, As, and Mo are 12-18 times higher relative to sediments, while concentrations of Fe, P, Ni, and Co increase 5-7 times during nodule formation.
title Chemical composition of ferromanganese nodules from the Black Sea
topic Archive of Ocean Data; ARCOD; Black Sea; MULT; Multiple investigations; Vy8-798; Vy8-800; Vy8-802; Vy8-848
url https://doi.org/10.1594/PANGAEA.783709