Zda je potřeba kosit středoevropská slatiniště sycená podzemní vodou, jsme zkoumali pomocí 7 dlouhodobých terénních experimentů. Výsledky ukazují, že pravidelné obhospodařování je podobně důležité pro jejich zachování jako trvalé zamokření a nenarušený vodní režim. Důvodem je jejich vznik v současné podobě často až po odlesnění člověkem, což ukazují výsledky makrozbytkové analýzy.

K dalšímu čtení v Živě

Proč jsou rašeliniště kyselá? (2018, 3)

Použitá literatura

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HÁJKOVÁ, Petra, et al. Origin and contrasting succession pathways of the Western Carpathian calcareous fens revealed by plant and mollusc macrofossils. Boreas, 2012, 41.4: 690-706.

HÁJKOVÁ, Petra, et al. Using multi-proxy palaeoecology to test a relict status of refugial populations of calcareous-fen species in the Western Carpathians. The Holocene, 2015, 25.4: 702-715.

HÁJKOVÁ, Petra, et al. Can relict-rich communities be of an anthropogenic origin? Palaeoecological insight into conservation strategy for endangered Carpathian travertine fens. Quaternary Science Reviews, 2020, 234: 106241.

JAMRICHOVÁ, Eva, et al. Landscape history, calcareous fen development and historical events in the Slovak Eastern Carpathians. Vegetation history and archaeobotany, 2014, 23.5: 497-513.

KLIMEŠ, Leoš; KLIMEŠOVÁ, Jitka. The effects of mowing and fertilization on carbohydrate reserves and regrowth of grasses: do they promote plant coexistence in species-rich meadows?. Evolutionary Ecology, 2001, 15.4: 363-382.

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ROLEČEK, Jan, et al. Conservation targets from the perspective of a palaeoecological reconstruction: the case study of Dářko peat bog in the Czech Republic. Preslia, 2020, 92.2: 87-114.

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We investigated whether it is necessary to mow Central European mires saturated with groundwater using 7 long-term field experiments. The results show that regular management is just as important for their preservation as permanent waterlogging and an undisturbed water regime. The reason for this is that they often originated in their current form after deforestation by humans, as shown by the results of macrofossil analysis.