About: How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire     Goto   Sponge   NotDistinct   Permalink

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  • 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.
  • 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. (en)
Title
  • How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire
  • How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire (en)
skos:prefLabel
  • How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire
  • How a Sphagnum fuscum-dominated bog changed into a calcareous fen: the unique Holocene history of a Slovak spring-fed mire (en)
skos:notation
  • RIV/67985939:_____/12:00381626!RIV13-AV0-67985939
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GAP504/11/0429), S, Z(AV0Z60050516), Z(MSM0021622416)
http://linked.open...iv/cisloPeriodika
  • 3
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 139661
http://linked.open...ai/riv/idVysledku
  • RIV/67985939:_____/12:00381626
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Holocene; succession; mire (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
http://linked.open...ontrolniKodProRIV
  • [06516486BD87]
http://linked.open...i/riv/nazevZdroje
  • Journal of Quaternary Science
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 27
http://linked.open...iv/tvurceVysledku
  • Hájková, Petra
  • Hájek, Michal
  • Opravilová, V.
  • Wolejko, L.
  • Grootjans, A. B.
  • Joosten, H.
  • Lamentowicz, M.
  • Madaras, M.
  • Michaelis, D.
  • Rybníčková, E.
http://linked.open...ain/vavai/riv/wos
  • 000303058700001
http://linked.open...n/vavai/riv/zamer
issn
  • 0267-8179
number of pages
http://bibframe.org/vocab/doi
  • 10.1002/jqs.1534
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