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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Online Access: | https://dx.doi.org/10.1594/pangaea.868668 https://doi.pangaea.de/10.1594/PANGAEA.868668 |
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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 |
_version_ |
1789333359775711232 |