Flood-stack of combined sediment record ELSA ...

This study reconstructs the main flood phases in central Europe from event layers in sediment cores from Holocene Eifel maar lakes and Pleistocene dry maar structures. These reconstructions are combined with recent gauge time-series to cover the entire precipitation extremes of the last 60 000 years...

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Bibliographic Details
Main Authors: Brunck, Heiko, Sirocko, Frank, Albert, Johannes
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
Age
Online Access:https://dx.doi.org/10.1594/pangaea.868668
https://doi.pangaea.de/10.1594/PANGAEA.868668
id ftdatacite:10.1594/pangaea.868668
record_format openpolar
spelling ftdatacite:10.1594/pangaea.868668 2024-01-28T10:06:28+01:00 Flood-stack of combined sediment record ELSA ... Brunck, Heiko Sirocko, Frank Albert, Johannes 2016 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.868668 https://doi.pangaea.de/10.1594/PANGAEA.868668 en eng PANGAEA https://elsa-project.de/ https://dx.doi.org/10.1016/j.gloplacha.2015.12.003 https://dx.doi.org/10.1016/j.gloplacha.2015.07.012 https://dx.doi.org/10.1016/j.gloplacha.2016.03.011 https://dx.doi.org/10.1016/j.gloplacha.2016.03.005 https://elsa-project.de/ Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Age Age, minimum/young Age, maximum/old Index dataset Dataset Supplementary Dataset 2016 ftdatacite https://doi.org/10.1594/pangaea.86866810.1016/j.gloplacha.2015.12.00310.1016/j.gloplacha.2015.07.01210.1016/j.gloplacha.2016.03.01110.1016/j.gloplacha.2016.03.005 2024-01-04T14:12:45Z This study reconstructs the main flood phases in central Europe from event layers in sediment cores from Holocene Eifel maar lakes and Pleistocene dry maar structures. These reconstructions are combined with recent gauge time-series to cover the entire precipitation extremes of the last 60 000 years. In general, Eifel maar sediments are perfectly suited for the preservation of event layers since the deep water in the maar lakes is seasonal anoxic and therefore, bioturbation is low. However, the preservation of annual lamination is only preserved in Holzmaar and Ulmener Maar; the other cores are dated by 14C, magnetostratigraphy, tephra markers and ice core tuning. The cores were drilled in the Eifel region of central western Germany, which represents a climatic homogenous region from Belgium to Poland and all across Central Europe.A total of 233 flood layers over 7.5 mm were detected in all analysed cores. The stratigraphic classification of the flood events follows the newly defined Landscape Evolution ... : Sediment core combination: AU2 (Aueler Maar Lat.: 50.28383, Long.: 6.59574. elevation: 453, recovery: 123 m, Gauß-Krüger coordinate system: 2542455/5572017) + HM1 (Holzmaar Lat.: 50.1203, Long.: 6.87963, elevation: 425, recovery: 10 m, Gauß-Krüger coordinate system: 2562900/5554030) ... Dataset ice core DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Age
Age, minimum/young
Age, maximum/old
Index
spellingShingle Age
Age, minimum/young
Age, maximum/old
Index
Brunck, Heiko
Sirocko, Frank
Albert, Johannes
Flood-stack of combined sediment record ELSA ...
topic_facet Age
Age, minimum/young
Age, maximum/old
Index
description This study reconstructs the main flood phases in central Europe from event layers in sediment cores from Holocene Eifel maar lakes and Pleistocene dry maar structures. These reconstructions are combined with recent gauge time-series to cover the entire precipitation extremes of the last 60 000 years. In general, Eifel maar sediments are perfectly suited for the preservation of event layers since the deep water in the maar lakes is seasonal anoxic and therefore, bioturbation is low. However, the preservation of annual lamination is only preserved in Holzmaar and Ulmener Maar; the other cores are dated by 14C, magnetostratigraphy, tephra markers and ice core tuning. The cores were drilled in the Eifel region of central western Germany, which represents a climatic homogenous region from Belgium to Poland and all across Central Europe.A total of 233 flood layers over 7.5 mm were detected in all analysed cores. The stratigraphic classification of the flood events follows the newly defined Landscape Evolution ... : Sediment core combination: AU2 (Aueler Maar Lat.: 50.28383, Long.: 6.59574. elevation: 453, recovery: 123 m, Gauß-Krüger coordinate system: 2542455/5572017) + HM1 (Holzmaar Lat.: 50.1203, Long.: 6.87963, elevation: 425, recovery: 10 m, Gauß-Krüger coordinate system: 2562900/5554030) ...
format Dataset
author Brunck, Heiko
Sirocko, Frank
Albert, Johannes
author_facet Brunck, Heiko
Sirocko, Frank
Albert, Johannes
author_sort Brunck, Heiko
title Flood-stack of combined sediment record ELSA ...
title_short Flood-stack of combined sediment record ELSA ...
title_full Flood-stack of combined sediment record ELSA ...
title_fullStr Flood-stack of combined sediment record ELSA ...
title_full_unstemmed Flood-stack of combined sediment record ELSA ...
title_sort flood-stack of combined sediment record elsa ...
publisher PANGAEA
publishDate 2016
url https://dx.doi.org/10.1594/pangaea.868668
https://doi.pangaea.de/10.1594/PANGAEA.868668
genre ice core
genre_facet ice core
op_relation https://elsa-project.de/
https://dx.doi.org/10.1016/j.gloplacha.2015.12.003
https://dx.doi.org/10.1016/j.gloplacha.2015.07.012
https://dx.doi.org/10.1016/j.gloplacha.2016.03.011
https://dx.doi.org/10.1016/j.gloplacha.2016.03.005
https://elsa-project.de/
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.86866810.1016/j.gloplacha.2015.12.00310.1016/j.gloplacha.2015.07.01210.1016/j.gloplacha.2016.03.01110.1016/j.gloplacha.2016.03.005
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