Detailed Information on Publication Record
2012
How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire
HÁJKOVÁ, Petra, Ab GROOTJANS, Mariusz LAMENTOWICZ, Eliška RYBNÍČKOVÁ, Mikulas MADARAS et. al.Basic information
Original name
How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire
Name in Czech
Jak se vrchoviště se Sphagnum fuscum změnilo ve slatiniště: unikátní holocenní historie slovenského prameništního slatiniště
Authors
HÁJKOVÁ, Petra (203 Czech Republic, guarantor, belonging to the institution), Ab GROOTJANS (528 Netherlands), Mariusz LAMENTOWICZ (616 Poland), Eliška RYBNÍČKOVÁ (203 Czech Republic), Mikulas MADARAS (703 Slovakia), Věra OPRAVILOVÁ (203 Czech Republic, belonging to the institution), Dierk MICHAELIS (276 Germany), Michal HÁJEK (203 Czech Republic, belonging to the institution), Hans JOOSTEN (276 Germany) and Leslaw WOLEJKO (616 Poland)
Edition
JOURNAL OF QUATERNARY SCIENCE, MALDEN, WILEY-BLACKWELL, 2012, 0267-8179
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10600 1.6 Biological sciences
Country of publisher
United States of America
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 2.939
RIV identification code
RIV/00216224:14310/12:00057874
Organization unit
Faculty of Science
UT WoS
000303058700001
Keywords (in Czech)
holocén; sukcese; rašeliniště
Keywords in English
Holocene; succession; mire
Tags
International impact, Reviewed
Změněno: 10/4/2013 15:41, Ing. Andrea Mikešková
V originále
Mires develop by autogenic succession from more groundwater-fed to more rainwater-fed. This study describes a similar development in the Early Holocene, followed by a reverse development in the Middle and Late Holocene. Pollen, macrofossil and testate amoeba analyses show that the site started as a minerotrophic open fen woodland. After 10 700 cal a BP autogenic succession led to the accumulation of at least 1?m of Sphagnum fuscum peat. Around 9000 cal a BP, as climate could no longer sustain a stable water regime, the bog desiccated and a fire broke out. The fire removed part of the peat layer and as a consequence relative water levels rose, leading to the establishment of a wet minerotrophic swamp carr. After 600 cal a BP, rapid peat accumulation with calcareous tufa formation resumed as a result of anthropogenic deforestation and hydrological changes in the catchment and resulting increased groundwater discharge.
In Czech
Na základě multi-proxy přístupu jsme zdokumentovali vývoj rašeliniště od vrchoviště po vápnité slatiniště. Takový unikátní vývoj byl zaznamenán na lokalitě Belanské lúky na Slovensku.
Links
| GAP504/11/0429, research and development project |
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| MSM0021622416, plan (intention) |
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