Composition of sedimentary material from the bottom and the area surrounding the Lake Untersee, East Antarctica

This paper presents data on geographic and geologic conditions of modern sedimentation in the Lake Untersee, the largest lake in the East Antarctica. Geochemical and sedimentation data indicate that the leading mechanism supplying aluminosilicate sedimentary material to the surface layer of bottom sediments is seasonal melting of the Anuchin glacier and the mountain glacier on the southeastern part of the valley hosting the lake. Strongly reduced conditions in the lowermost 25 m of the water column in the smaller of two depressions of the lake bottom were favorable for enrichment of the bottom sediments in bacteriogenic organic matter, Mo, Au, and Pd. H2S-contaminated water results to significant enrichment of the sediments only in redox-sensitive elements that are able to migrate in anionic complexes and precipitate (co-precipitate) as sulfides.

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Cite this as

Levitan, Mikhail A, Girin, Yury P, Luksha, V L, Kubrakova, I V, Roshchina, I A, Sattler, Birgit, Tyutyunnik, O A, Chudetsky, MYu (2011). Dataset: Composition of sedimentary material from the bottom and the area surrounding the Lake Untersee, East Antarctica. https://doi.org/10.1594/PANGAEA.811555

DOI retrieved: 2011

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-3.0
Source https://doi.org/10.1594/PANGAEA.811555
Author Levitan, Mikhail A
Given Name Mikhail A
Family Name Levitan
More Authors
Girin, Yury P
Luksha, V L
Kubrakova, I V
Roshchina, I A
Sattler, Birgit
Tyutyunnik, O A
Chudetsky, MYu
Source Creation 2011
Publication Year 2011
Resource Type application/zip - filename: Levitan_2011
Subject Areas
Name: Chemistry

Name: Lithosphere

Related Identifiers
Title: Modern sedimentation system of Lake Untersee, East Antarctica
Identifier: https://doi.org/10.1134/S0016702911050077
Type: DOI
Relation: References
Year: 2011
Source: Translated from Geokhimiya, 2011, 49(5), 483-505
Authors: Levitan Mikhail A , Girin Yury P , Luksha V L , Kubrakova I V , Roshchina I A , Sattler Birgit , Tyutyunnik O A , Chudetsky MYu .