Age determination of lake Holzmar sediments

Fuente: PANGAEA
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Autores principales: Zolitschka, Bernd, Brauer, Achim, Stockhausen, Hagen, Lang, Andreas, Negendank, Jörg F W
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2000
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author Zolitschka, Bernd
Brauer, Achim
Stockhausen, Hagen
Lang, Andreas
Negendank, Jörg F W
author_facet Zolitschka, Bernd
Brauer, Achim
Stockhausen, Hagen
Lang, Andreas
Negendank, Jörg F W
collection Datos científicos de ciencias marinas y ambientales
contents A record extending back to 23 220 calendar yr B.P. was obtained from varved sediments from Lake Holzmaar, Germany, by applying multiple dating methods and interlake comparison with Meerfelder Maar. Variations in the Weichselian inorganic carbon content resulting from intensified eolian activities coincide with proxy parameters of dust accumulation in Greenland. The timing for the end of the last glacial maximum at Holzmaar agrees with the Greenland Ice Sheet Project (GISP2) data but suggests dating discrepancies with the Greenland Ice Core Project data (GRIP). Assuming that periods of maximum dust deposition in the Eifel and Greenland coincide with ice advances in northeastern Germany, the Holzmaar record provides a means of dating three late Weichselian terminal moraines.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_734904
institution PANGAEA
language en
publishDate 2000
publisher PANGAEA
record_format pangaea
spellingShingle Age determination of lake Holzmar sediments
Zolitschka, Bernd
Brauer, Achim
Stockhausen, Hagen
Lang, Andreas
Negendank, Jörg F W
Changes in the Geo-Biosphere during the last 15000 years; Climate in Historical Times; COMPCORE; Composite Core; GeoBio15k; Holzmaar; HZM; KIHZ; Sampling/drilling in lake
A record extending back to 23 220 calendar yr B.P. was obtained from varved sediments from Lake Holzmaar, Germany, by applying multiple dating methods and interlake comparison with Meerfelder Maar. Variations in the Weichselian inorganic carbon content resulting from intensified eolian activities coincide with proxy parameters of dust accumulation in Greenland. The timing for the end of the last glacial maximum at Holzmaar agrees with the Greenland Ice Sheet Project (GISP2) data but suggests dating discrepancies with the Greenland Ice Core Project data (GRIP). Assuming that periods of maximum dust deposition in the Eifel and Greenland coincide with ice advances in northeastern Germany, the Holzmaar record provides a means of dating three late Weichselian terminal moraines.
title Age determination of lake Holzmar sediments
topic Changes in the Geo-Biosphere during the last 15000 years; Climate in Historical Times; COMPCORE; Composite Core; GeoBio15k; Holzmaar; HZM; KIHZ; Sampling/drilling in lake
url https://doi.org/10.1594/PANGAEA.734904