DUDOVÁ, Lydie, Petra HÁJKOVÁ, Věra OPRAVILOVÁ and Michal HÁJEK. Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies. Quaternary Research. Elsevier, 2014, vol. 82, No 1, p. 107-120. ISSN 0033-5894. Available from: https://dx.doi.org/10.1016/j.yqres.2014.04.017.
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Basic information
Original name Holocene history and environmental reconstruction of a Hercynian mire and surrounding mountain landscape based on multiple proxies
Authors DUDOVÁ, Lydie (203 Czech Republic, guarantor, belonging to the institution), Petra HÁJKOVÁ (203 Czech Republic, belonging to the institution), Věra OPRAVILOVÁ (203 Czech Republic, belonging to the institution) and Michal HÁJEK (203 Czech Republic, belonging to the institution).
Edition Quaternary Research, Elsevier, 2014, 0033-5894.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10600 1.6 Biological sciences
Country of publisher United States of America
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 2.544
RIV identification code RIV/00216224:14310/14:00073965
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1016/j.yqres.2014.04.017
UT WoS 000339138400011
Keywords (in Czech) přechod slatina-vrchoviště; přenosové funkce; pylová a makrozbytková analýza
Keywords in English fen-bog transition; transfer functions; macrofossil and pollen analysis
Tags AKR, rivok
Tags International impact, Reviewed
Changed by Changed by: prof. Mgr. Michal Hájek, Ph.D., učo 16868. Changed: 16/2/2018 14:58.
Abstract
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.
Links
GA206/08/0389, research and development projectName: Současné a historické změny na horských rašeliništních Sudet
Investor: Czech Science Foundation, Past and present changes in Sudeten mountain bogs
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