Age determination of lake Holzmar sediments

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 co...

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Main Authors: Zolitschka, Bernd, Brauer, Achim, Stockhausen, Hagen, Lang, Andreas, Negendank, Jörg F W
Format: Dataset
Language:English
Published: PANGAEA 2000
Subjects:
HZM
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.734904
https://doi.org/10.1594/PANGAEA.734904
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.734904
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.734904 2023-05-15T16:24:26+02:00 Age determination of lake Holzmar sediments Zolitschka, Bernd Brauer, Achim Stockhausen, Hagen Lang, Andreas Negendank, Jörg F W LATITUDE: 50.120304 * LONGITUDE: 6.879628 2000-03-09 application/zip, 4 datasets https://doi.pangaea.de/10.1594/PANGAEA.734904 https://doi.org/10.1594/PANGAEA.734904 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.734904 https://doi.org/10.1594/PANGAEA.734904 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Zolitschka, Bernd; Brauer, Achim; Stockhausen, Hagen; Lang, Andreas; Negendank, Jörg F W (2000): Annually dated late Weichselian continental paleoclimate record from the Eifel, Germany. Geology, 28(9), 783-786, https://doi.org/10.1130/0091-7613(2000)28%3C783:ADLWCP%3E2.0.CO;2 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 Dataset 2000 ftpangaea https://doi.org/10.1594/PANGAEA.734904 https://doi.org/10.1130/0091-7613(2000)28%3C783:ADLWCP%3E2.0.CO;2 2023-01-20T07:31:41Z 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. Dataset Greenland Greenland ice core Greenland Ice core Project Greenland Ice Sheet Project GRIP ice core Ice Sheet PANGAEA - Data Publisher for Earth & Environmental Science Greenland ENVELOPE(6.879628,6.879628,50.120304,50.120304)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
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
spellingShingle 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
Zolitschka, Bernd
Brauer, Achim
Stockhausen, Hagen
Lang, Andreas
Negendank, Jörg F W
Age determination of lake Holzmar sediments
topic_facet 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
description 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
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
author_sort Zolitschka, Bernd
title Age determination of lake Holzmar sediments
title_short Age determination of lake Holzmar sediments
title_full Age determination of lake Holzmar sediments
title_fullStr Age determination of lake Holzmar sediments
title_full_unstemmed Age determination of lake Holzmar sediments
title_sort age determination of lake holzmar sediments
publisher PANGAEA
publishDate 2000
url https://doi.pangaea.de/10.1594/PANGAEA.734904
https://doi.org/10.1594/PANGAEA.734904
op_coverage LATITUDE: 50.120304 * LONGITUDE: 6.879628
long_lat ENVELOPE(6.879628,6.879628,50.120304,50.120304)
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland ice core
Greenland Ice core Project
Greenland Ice Sheet Project
GRIP
ice core
Ice Sheet
genre_facet Greenland
Greenland ice core
Greenland Ice core Project
Greenland Ice Sheet Project
GRIP
ice core
Ice Sheet
op_source Supplement to: Zolitschka, Bernd; Brauer, Achim; Stockhausen, Hagen; Lang, Andreas; Negendank, Jörg F W (2000): Annually dated late Weichselian continental paleoclimate record from the Eifel, Germany. Geology, 28(9), 783-786, https://doi.org/10.1130/0091-7613(2000)28%3C783:ADLWCP%3E2.0.CO;2
op_relation https://doi.pangaea.de/10.1594/PANGAEA.734904
https://doi.org/10.1594/PANGAEA.734904
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.734904
https://doi.org/10.1130/0091-7613(2000)28%3C783:ADLWCP%3E2.0.CO;2
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