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Abstract:
This study investigated the development of biological soil crust (biocrust) covers in an early successional subtropical forest ecosystem and their impact on soil erosion. Within a biodiversity and ecosystem functioning experiment in Southeast China (BEF China), sediment discharge and runoff measurements were conducted with micro-scale runoff plots under natural rainfall and biocrust covers were surveyed over a five-year period.
Results showed that biocrusts occurred widely in our experimental forest ecosystem and developed from initial light cyanobacteria- and algae-dominated crusts to later-stage bryophyte-dominated crusts in only three years. Biocrust covers were still increasing after six years of tree growth. Within later stage crusts, 25 bryophyte species were determined. The development of biocrusts was significantly influenced by the surrounding vegetation cover and terrain attributes. Besides high crown cover and leaf area index, the development of biocrusts was favoured by low slope gradients, slope orientations towards the incident sunlight and the altitude of the research plots. Our measurements showed, that bryophyte-dominated biocrusts were importantly decreasing soil erosion and more effective in erosion reduction than abiotic soil surface covers. Hence, their significant role to mitigate sediment discharge and runoff generation in mesic forest environments and their ability to quickly colonize gaps in higher vegetation layers are of particular interest for soil erosion control in early stage forest plantations. A detailed record of different biocrust species and their functional influence on soil erosion processes as well as a thorough monitoring of biocrust covers under closing tree canopy in subtropical forests is required in further studies.
