Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW)
C/O-stable isotope composition (VPDB) of speleothems from the Makkaronihalle of the Hüttenbläserschacht Cave in Iserlohn shows a clear separation between glacial and interglacial calcites. In contrast to normal speleothems (stalagmites, excentriques, crystals in cave ponds, draperies; δ18O: –4.0 to...
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ftsubggeo:oai:e-docs.geo-leo.de:11858/00-1735-0000-0029-65E1-8 2024-06-09T07:46:39+00:00 Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW) Richter, K., Detlev Goll, Kristina Grebe, Witold Niedermayr, Andrea Platte, Alexander Scholz, Denis 2015-11-18 http://hdl.handle.net/11858/00-1735-0000-0029-65E1-8 https://doi.org/10.3285/eg.64.2.02 deu ger Geozon Science Media E&G – Quaternary Science Journal E&G – Quaternary Science Journal; Vol.64 Geologische Wissenschaften doi:10.3285/eg.64.2.02 http://hdl.handle.net/11858/00-1735-0000-0029-65E1-8 Geozon Science Media ddc:551.7 permafrost Cryogenic calcites C/O isotopes Upper Weichselian ice caves north-western Germany doc-type:article Verlagsversion 2015 ftsubggeo https://doi.org/10.3285/eg.64.2.02 2024-05-10T04:57:48Z C/O-stable isotope composition (VPDB) of speleothems from the Makkaronihalle of the Hüttenbläserschacht Cave in Iserlohn shows a clear separation between glacial and interglacial calcites. In contrast to normal speleothems (stalagmites, excentriques, crystals in cave ponds, draperies; δ18O: –4.0 to –6.1 ‰, δ13C: –4.9 to –10.9 ‰), rhombohedral crystal sinter and spherulitic speleoparticles are characterised by lower δ18O (–8.9 to –17.9 ‰) and higher δ13C values (+0.7 to –6.1 ‰). This suggests that these speleogenetic particles were formed in slowly freezing waterpools on ice during the transition from a stadial to an interstadial phase. Precise 230Th/U-dating shows younger Weichselian ages of 28.6 to 33.0 ka for these speleogenetic particles from north-west Germany. These formation periods indicate freezing conditions overlain by 34 m of hostrock and provide the minimum depth of permafrost penetration for the younger Weichselian in the area of the northern Sauerland (north-west Germany). research Article in Journal/Newspaper Ice permafrost GEO-LEOe-docs (FID GEO) E&G Quaternary Science Journal 64 2 67 81 |
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Open Polar |
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GEO-LEOe-docs (FID GEO) |
op_collection_id |
ftsubggeo |
language |
German |
topic |
ddc:551.7 permafrost Cryogenic calcites C/O isotopes Upper Weichselian ice caves north-western Germany |
spellingShingle |
ddc:551.7 permafrost Cryogenic calcites C/O isotopes Upper Weichselian ice caves north-western Germany Richter, K., Detlev Goll, Kristina Grebe, Witold Niedermayr, Andrea Platte, Alexander Scholz, Denis Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW) |
topic_facet |
ddc:551.7 permafrost Cryogenic calcites C/O isotopes Upper Weichselian ice caves north-western Germany |
description |
C/O-stable isotope composition (VPDB) of speleothems from the Makkaronihalle of the Hüttenbläserschacht Cave in Iserlohn shows a clear separation between glacial and interglacial calcites. In contrast to normal speleothems (stalagmites, excentriques, crystals in cave ponds, draperies; δ18O: –4.0 to –6.1 ‰, δ13C: –4.9 to –10.9 ‰), rhombohedral crystal sinter and spherulitic speleoparticles are characterised by lower δ18O (–8.9 to –17.9 ‰) and higher δ13C values (+0.7 to –6.1 ‰). This suggests that these speleogenetic particles were formed in slowly freezing waterpools on ice during the transition from a stadial to an interstadial phase. Precise 230Th/U-dating shows younger Weichselian ages of 28.6 to 33.0 ka for these speleogenetic particles from north-west Germany. These formation periods indicate freezing conditions overlain by 34 m of hostrock and provide the minimum depth of permafrost penetration for the younger Weichselian in the area of the northern Sauerland (north-west Germany). research |
format |
Article in Journal/Newspaper |
author |
Richter, K., Detlev Goll, Kristina Grebe, Witold Niedermayr, Andrea Platte, Alexander Scholz, Denis |
author_facet |
Richter, K., Detlev Goll, Kristina Grebe, Witold Niedermayr, Andrea Platte, Alexander Scholz, Denis |
author_sort |
Richter, K., Detlev |
title |
Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW) |
title_short |
Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW) |
title_full |
Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW) |
title_fullStr |
Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW) |
title_full_unstemmed |
Weichselzeitliche Kryocalcite als Hinweise für Eisseen in der Hüttenbläserschachthöhle (Iserlohn/NRW) |
title_sort |
weichselzeitliche kryocalcite als hinweise für eisseen in der hüttenbläserschachthöhle (iserlohn/nrw) |
publisher |
Geozon Science Media |
publishDate |
2015 |
url |
http://hdl.handle.net/11858/00-1735-0000-0029-65E1-8 https://doi.org/10.3285/eg.64.2.02 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_relation |
E&G – Quaternary Science Journal E&G – Quaternary Science Journal; Vol.64 Geologische Wissenschaften doi:10.3285/eg.64.2.02 http://hdl.handle.net/11858/00-1735-0000-0029-65E1-8 |
op_rights |
Geozon Science Media |
op_doi |
https://doi.org/10.3285/eg.64.2.02 |
container_title |
E&G Quaternary Science Journal |
container_volume |
64 |
container_issue |
2 |
container_start_page |
67 |
op_container_end_page |
81 |
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1801376605810982912 |