Peat formation potential of temperate fens increases with hydrological stability

Peat formation is the key process responsible for carbon sequestration in peatlands. In rich fens, peat is formed by brown mosses and belowground biomass of vascular plants. However, the impact of ecohydrological settings on the contribution of mosses and belowground biomass to peat formation remain...

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Veröffentlicht in:	The Science of the total environment 2024-10, Vol.947, p.174617, Article 174617
Hauptverfasser:	Jaszczuk, Izabela, Jabłońska, Ewa, Kozub, Łukasz, Tanneberger, Franziska, Aggenbach, Camiel, Seeber, Elke, van Diggelen, Rudy, Kreyling, Juergen, Silvennoinen, Hanna M., Kotowski, Wiktor
Format:	Artikel
Sprache:	eng
Schlagworte:	aboveground biomass belowground biomass Belowground biomass of vascular plants Biomass biomass production Biomass surplus Brown mosses Bryophyta - growth & development Carbon Sequestration environment Environmental Monitoring eutrophication fens hydrologic cycle Hydrology peat Peat formation peatlands phytomass Poland Rich fen Soil - chemistry vascular plants vegetation gradient Water level fluctuations Wetlands
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