Growth rates of Fe-Mn nodules and age and sedimentation rates of host sediments from the Southeast Pacific

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Auteurs principaux: Vlasova, Irina E, Kuptsov, Vladimir M
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1994
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author Vlasova, Irina E
Kuptsov, Vladimir M
author_facet Vlasova, Irina E
Kuptsov, Vladimir M
collection Datos científicos de ciencias marinas y ambientales
contents Growth rates of nine ferromanganese nodules collected from the Southeast Pacific were estimated using the alpha radiogpaphic technigue. Growth rates range from 1 to 16 mm per million years. In three nodules measurements were made on two opposite sides; two of them showed no growth in one of measured directions during the last 300 ky, whereas in the third nodule growth rates on the opposite sides differ by factor 2. Average sedimentation rate of deposits underlying the nodules estimated by the radiocarbon and excess 230Th methods, were 4 mm/1000 years with rather minor variations. Difference between sedimentation rates and nodule growth rates is caused by activity of benthic fauna, as suggested by inversion of radiocarbon dates with depth.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_759580
institution PANGAEA
language en
publishDate 1994
publisher PANGAEA
record_format pangaea
spellingShingle Growth rates of Fe-Mn nodules and age and sedimentation rates of host sediments from the Southeast Pacific
Vlasova, Irina E
Kuptsov, Vladimir M
Archive of Ocean Data; ARCOD; DM14; DM14-1005; DM14-1007; DM14-983; DM14-984; DM14-985; DM14-992; DM14-993; DM14-994; Dmitry Mendeleev; Grab; GRAB; Southeast Pacific
Growth rates of nine ferromanganese nodules collected from the Southeast Pacific were estimated using the alpha radiogpaphic technigue. Growth rates range from 1 to 16 mm per million years. In three nodules measurements were made on two opposite sides; two of them showed no growth in one of measured directions during the last 300 ky, whereas in the third nodule growth rates on the opposite sides differ by factor 2. Average sedimentation rate of deposits underlying the nodules estimated by the radiocarbon and excess 230Th methods, were 4 mm/1000 years with rather minor variations. Difference between sedimentation rates and nodule growth rates is caused by activity of benthic fauna, as suggested by inversion of radiocarbon dates with depth.
title Growth rates of Fe-Mn nodules and age and sedimentation rates of host sediments from the Southeast Pacific
topic Archive of Ocean Data; ARCOD; DM14; DM14-1005; DM14-1007; DM14-983; DM14-984; DM14-985; DM14-992; DM14-993; DM14-994; Dmitry Mendeleev; Grab; GRAB; Southeast Pacific
url https://doi.org/10.1594/PANGAEA.759580