(Table 1) Age of sediments with anomalously high Hg concentrations in core BDP-98, Lake Baikal

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Auteurs principaux: Gelety, V F, Kalmykov, G V, Parkhomenko, IYu
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2007
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author Gelety, V F
Kalmykov, G V
Parkhomenko, IYu
author_facet Gelety, V F
Kalmykov, G V
Parkhomenko, IYu
collection Datos científicos de ciencias marinas y ambientales
contents Mercury distribution was examined in the sediments of Lake Baikal that were sampled within the scope of the Baikal Drilling International Project in 1996-1999. The Hg concentrations in the ancient sediments are close to those in the modern sediments with the exception of a few peak values, whose ages coincide with those of active volcanism in adjacent areas. Mercury was demonstrated to be contained in the sediments in the adsorbed Hg0 mode, predominantly in relation with organic matter. When the organic matter of the bottom sediments is decomposed in the course of lithification, Hg is retained in the sediments adsorbed on the residual organic matter, and the concentration of this element corresponds to its initial content in the bottom sediments during their accumulation. Mercury concentrations in lithologically distinct bottom sediments of Lake Baikal and its sediments as a whole depend on the climate. Sediments that were formed during warm periods of time contain more Hg than those produced during cold periods or glaciation. Periodical variations in the Hg concentrations in the bottom sediments of Lake Baikal reflect the variations in the contents of this element in the Earth's atmosphere in the Late Cenozoic, which were, in turn, controlled by the climatic variations on the planet and, thus, can be used for detailed reconstructions of variations in the average global temperature near the planet's surface.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_792851
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Age of sediments with anomalously high Hg concentrations in core BDP-98, Lake Baikal
Gelety, V F
Kalmykov, G V
Parkhomenko, IYu
Age, standard deviation; Age model, optional; Archive of Ocean Data; ARCOD; Baikal Lake; BDP1998; BDP-98; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Mercury; Sample ID; Sampling/drilling in lake
Mercury distribution was examined in the sediments of Lake Baikal that were sampled within the scope of the Baikal Drilling International Project in 1996-1999. The Hg concentrations in the ancient sediments are close to those in the modern sediments with the exception of a few peak values, whose ages coincide with those of active volcanism in adjacent areas. Mercury was demonstrated to be contained in the sediments in the adsorbed Hg0 mode, predominantly in relation with organic matter. When the organic matter of the bottom sediments is decomposed in the course of lithification, Hg is retained in the sediments adsorbed on the residual organic matter, and the concentration of this element corresponds to its initial content in the bottom sediments during their accumulation. Mercury concentrations in lithologically distinct bottom sediments of Lake Baikal and its sediments as a whole depend on the climate. Sediments that were formed during warm periods of time contain more Hg than those produced during cold periods or glaciation. Periodical variations in the Hg concentrations in the bottom sediments of Lake Baikal reflect the variations in the contents of this element in the Earth's atmosphere in the Late Cenozoic, which were, in turn, controlled by the climatic variations on the planet and, thus, can be used for detailed reconstructions of variations in the average global temperature near the planet's surface.
title (Table 1) Age of sediments with anomalously high Hg concentrations in core BDP-98, Lake Baikal
topic Age, standard deviation; Age model, optional; Archive of Ocean Data; ARCOD; Baikal Lake; BDP1998; BDP-98; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Mercury; Sample ID; Sampling/drilling in lake
url https://doi.org/10.1594/PANGAEA.792851