Geochemistry, grain sizes and radiocarbon age of sediment core Lz1005 from Amery Oasis, East Antarctica

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Autores principales: Hultzsch, Nadja, Wagner, Bernd, Diekmann, Bernhard, White, Duanne A
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2008
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author Hultzsch, Nadja
Wagner, Bernd
Diekmann, Bernhard
White, Duanne A
author_facet Hultzsch, Nadja
Wagner, Bernd
Diekmann, Bernhard
White, Duanne A
collection Datos científicos de ciencias marinas y ambientales
contents The clay mineralogical composition of a 552 cm long sediment core from Lake Terrasovoje in Amery Oasis, East Antarctica, was analysed and compared with that in surface sediments from other locations in the vicinity. The lower part of the sediment core is formed by sub- and proglacial sediments with a dominance of smectite and illite, and lower amounts of kaolinite and chlorite. The upper part of the core is deposited after 12 500 cal yr bp and mainly composed of illite and kaolinite, with low amounts of smectite and chlorite, such as found in samples from rock outcrops and covering sediments throughout Amery Oasis. The clay composition in the lower section of core Lz1005 suggest that the basin of Lake Terrasovoje was filled by a 150-200 m thickened Nemesis Glacier prior to 12 500 cal yr bp rather than by local ice caps.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_847418
institution PANGAEA
language en
publishDate 2008
publisher PANGAEA
record_format pangaea
spellingShingle Geochemistry, grain sizes and radiocarbon age of sediment core Lz1005 from Amery Oasis, East Antarctica
Hultzsch, Nadja
Wagner, Bernd
Diekmann, Bernhard
White, Duanne A
AmeryOasis2001/2002; AWI_PerDyn; COMPCORE; Composite Core; Lake Terrasovoje, East Antarctica; Lz1005; Permafrost Research (Periglacial Dynamics) @ AWI; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Sampling/drilling in lake; SPP1158
The clay mineralogical composition of a 552 cm long sediment core from Lake Terrasovoje in Amery Oasis, East Antarctica, was analysed and compared with that in surface sediments from other locations in the vicinity. The lower part of the sediment core is formed by sub- and proglacial sediments with a dominance of smectite and illite, and lower amounts of kaolinite and chlorite. The upper part of the core is deposited after 12 500 cal yr bp and mainly composed of illite and kaolinite, with low amounts of smectite and chlorite, such as found in samples from rock outcrops and covering sediments throughout Amery Oasis. The clay composition in the lower section of core Lz1005 suggest that the basin of Lake Terrasovoje was filled by a 150-200 m thickened Nemesis Glacier prior to 12 500 cal yr bp rather than by local ice caps.
title Geochemistry, grain sizes and radiocarbon age of sediment core Lz1005 from Amery Oasis, East Antarctica
topic AmeryOasis2001/2002; AWI_PerDyn; COMPCORE; Composite Core; Lake Terrasovoje, East Antarctica; Lz1005; Permafrost Research (Periglacial Dynamics) @ AWI; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Sampling/drilling in lake; SPP1158
url https://doi.org/10.1594/PANGAEA.847418