HÁJKOVÁ, Petra, Ab GROOTJANS, Mariusz LAMENTOWICZ, Eliška RYBNÍČKOVÁ, Mikulas MADARAS, Věra OPRAVILOVÁ, Dierk MICHAELIS, Michal HÁJEK, Hans JOOSTEN a Leslaw WOLEJKO. How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire. JOURNAL OF QUATERNARY SCIENCE. MALDEN: WILEY-BLACKWELL, 2012, roč. 27, č. 3, s. 233-243. ISSN 0267-8179. Dostupné z: https://dx.doi.org/10.1002/jqs.1534. |
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@article{1075372, author = {Hájková, Petra and Grootjans, Ab and Lamentowicz, Mariusz and Rybníčková, Eliška and Madaras, Mikulas and Opravilová, Věra and Michaelis, Dierk and Hájek, Michal and Joosten, Hans and Wolejko, Leslaw}, article_location = {MALDEN}, article_number = {3}, doi = {http://dx.doi.org/10.1002/jqs.1534}, keywords = {Holocene; succession; mire}, language = {eng}, issn = {0267-8179}, journal = {JOURNAL OF QUATERNARY SCIENCE}, title = {How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire}, volume = {27}, year = {2012} }
TY - JOUR ID - 1075372 AU - Hájková, Petra - Grootjans, Ab - Lamentowicz, Mariusz - Rybníčková, Eliška - Madaras, Mikulas - Opravilová, Věra - Michaelis, Dierk - Hájek, Michal - Joosten, Hans - Wolejko, Leslaw PY - 2012 TI - How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire JF - JOURNAL OF QUATERNARY SCIENCE VL - 27 IS - 3 SP - 233-243 EP - 233-243 PB - WILEY-BLACKWELL SN - 02678179 KW - Holocene KW - succession KW - mire N2 - 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. ER -
HÁJKOVÁ, Petra, Ab GROOTJANS, Mariusz LAMENTOWICZ, Eliška RYBNÍČKOVÁ, Mikulas MADARAS, Věra OPRAVILOVÁ, Dierk MICHAELIS, Michal HÁJEK, Hans JOOSTEN a Leslaw WOLEJKO. How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire. \textit{JOURNAL OF QUATERNARY SCIENCE}. MALDEN: WILEY-BLACKWELL, 2012, roč.~27, č.~3, s.~233-243. ISSN~0267-8179. Dostupné z: https://dx.doi.org/10.1002/jqs.1534.
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