Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies
We discovered the first peat section covering the entire Holocene in the Hrubý Jeseník Mountains. We analysed pollen, plant macrofossils (more abundant in bottom layers), testate amoebae (more abundant in upper layers), peat stratigraphy and chemistry. The mire started to develop as a calcium-rich p...
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Online Access: | https://doi.org/10.1016/j.yqres.2014.04.017 http://hdl.handle.net/11104/0236319 |
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ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0431752 2024-09-15T17:59:51+00:00 Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies Dudová, L. (Lydie) Hájková, P. (Petra) Opravilová, V. Hájek, M. (Michal) 2014 https://doi.org/10.1016/j.yqres.2014.04.017 http://hdl.handle.net/11104/0236319 eng eng doi:10.1016/j.yqres.2014.04.017 urn:pissn: 0033-5894 urn:eissn: 1096-0287 http://hdl.handle.net/11104/0236319 fen-bog transition transfer functions macrofossil and pollen analysis info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2014 ftczacademyscien https://doi.org/10.1016/j.yqres.2014.04.017 2024-08-19T05:32:59Z We discovered the first peat section covering the entire Holocene in the Hrubý Jeseník Mountains. We analysed pollen, plant macrofossils (more abundant in bottom layers), testate amoebae (more abundant in upper layers), peat stratigraphy and chemistry. The mire started to develop as a calcium-rich percolation fen with some species recently considered to be postglacial relicts (Meesia triquetra, Betula nana), shifted into ombrotrophy around 7450 cal yr BP by autogenic succession and changed into a pauperised, nutrient-enriched spruce woodland due to modern forestry activities. Further, we found that the landscape development differed from other Hercynian mountains located westward. This is represented by Pinus cembra and Larix during the Pleistocene/Holocene transition, the early expansion of spruce around 10,450 cal yr BP, and survival of Larix during the climatic optimum. From a methodological viewpoint we demonstrated how using multiple biotic proxies and extensive training sets in transfer functions may overcome taphonomic problems. Article in Journal/Newspaper Betula nana The Czech Academy of Sciences: Publication Activity (ASEP) Quaternary Research 82 1 107 120 |
institution |
Open Polar |
collection |
The Czech Academy of Sciences: Publication Activity (ASEP) |
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ftczacademyscien |
language |
English |
topic |
fen-bog transition transfer functions macrofossil and pollen analysis |
spellingShingle |
fen-bog transition transfer functions macrofossil and pollen analysis Dudová, L. (Lydie) Hájková, P. (Petra) Opravilová, V. Hájek, M. (Michal) Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies |
topic_facet |
fen-bog transition transfer functions macrofossil and pollen analysis |
description |
We discovered the first peat section covering the entire Holocene in the Hrubý Jeseník Mountains. We analysed pollen, plant macrofossils (more abundant in bottom layers), testate amoebae (more abundant in upper layers), peat stratigraphy and chemistry. The mire started to develop as a calcium-rich percolation fen with some species recently considered to be postglacial relicts (Meesia triquetra, Betula nana), shifted into ombrotrophy around 7450 cal yr BP by autogenic succession and changed into a pauperised, nutrient-enriched spruce woodland due to modern forestry activities. Further, we found that the landscape development differed from other Hercynian mountains located westward. This is represented by Pinus cembra and Larix during the Pleistocene/Holocene transition, the early expansion of spruce around 10,450 cal yr BP, and survival of Larix during the climatic optimum. From a methodological viewpoint we demonstrated how using multiple biotic proxies and extensive training sets in transfer functions may overcome taphonomic problems. |
format |
Article in Journal/Newspaper |
author |
Dudová, L. (Lydie) Hájková, P. (Petra) Opravilová, V. Hájek, M. (Michal) |
author_facet |
Dudová, L. (Lydie) Hájková, P. (Petra) Opravilová, V. Hájek, M. (Michal) |
author_sort |
Dudová, L. (Lydie) |
title |
Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies |
title_short |
Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies |
title_full |
Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies |
title_fullStr |
Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies |
title_full_unstemmed |
Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies |
title_sort |
holocene history and environmental reconstruction of a hercynian mire and surrounding mountain landscape based on multiple proxies |
publishDate |
2014 |
url |
https://doi.org/10.1016/j.yqres.2014.04.017 http://hdl.handle.net/11104/0236319 |
genre |
Betula nana |
genre_facet |
Betula nana |
op_relation |
doi:10.1016/j.yqres.2014.04.017 urn:pissn: 0033-5894 urn:eissn: 1096-0287 http://hdl.handle.net/11104/0236319 |
op_doi |
https://doi.org/10.1016/j.yqres.2014.04.017 |
container_title |
Quaternary Research |
container_volume |
82 |
container_issue |
1 |
container_start_page |
107 |
op_container_end_page |
120 |
_version_ |
1810436974958346240 |