Chemical composition of Fe-Mn nodules from the Pacific Ocean

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Auteurs principaux: Baturin, Gleb N, Shevchenko, Alla Ya
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1987
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author Baturin, Gleb N
Shevchenko, Alla Ya
author_facet Baturin, Gleb N
Shevchenko, Alla Ya
collection Datos científicos de ciencias marinas y ambientales
contents Calcareous and siliceous biogenic components have been studied in deep-water iron-manganese nodules from the northern and southern Pacific Ocean. Calcareous material consists of foraminifera remains, calcareous algae, and coccolithophorids, whereas siliceous material consists of remains of radiolarians and diatoms, as well as sponge spicules. Structures similar in morphology to coccal and filiform bacteria have been found in both outer and inner sections of the nodules indicating that microorganisms may be directly or indirectly involved in their development.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_756571
institution PANGAEA
language en
publishDate 1987
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of Fe-Mn nodules from the Pacific Ocean
Baturin, Gleb N
Shevchenko, Alla Ya
Archive of Ocean Data; ARCOD; Atomic absorption spectrometry (AAS); Copper; DM-1664; DM28; DM28-2520-8; Dmitry Mendeleev; Eastern Basin, Pacific Ocean; Elevation of event; Equatorial Pacific; Event label; Grab; GRAB; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese dioxide; MULT; Multiple investigations; Nickel; Pacific Ocean; Titanium dioxide; Vityaz (ex-Mars); Vityaz-43; VITYAZ5996; Vy-666-1; Vy-666-12; Vy-666-16; Wet chemistry
Calcareous and siliceous biogenic components have been studied in deep-water iron-manganese nodules from the northern and southern Pacific Ocean. Calcareous material consists of foraminifera remains, calcareous algae, and coccolithophorids, whereas siliceous material consists of remains of radiolarians and diatoms, as well as sponge spicules. Structures similar in morphology to coccal and filiform bacteria have been found in both outer and inner sections of the nodules indicating that microorganisms may be directly or indirectly involved in their development.
title Chemical composition of Fe-Mn nodules from the Pacific Ocean
topic Archive of Ocean Data; ARCOD; Atomic absorption spectrometry (AAS); Copper; DM-1664; DM28; DM28-2520-8; Dmitry Mendeleev; Eastern Basin, Pacific Ocean; Elevation of event; Equatorial Pacific; Event label; Grab; GRAB; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Manganese dioxide; MULT; Multiple investigations; Nickel; Pacific Ocean; Titanium dioxide; Vityaz (ex-Mars); Vityaz-43; VITYAZ5996; Vy-666-1; Vy-666-12; Vy-666-16; Wet chemistry
url https://doi.org/10.1594/PANGAEA.756571