Vegetation Science is a scientific discipline devoted to the study of vegetation at all levels of complexity spanning populations, plant communities and biomes. It attempts to explain vegetation patterns and the processes governing vegetation assembly and dynamics in all temporal and spatial scales. Vegetation analysis serves to record anthropo-zoogenic effects and portrays similarly structured vegetation formations with characteristic vegetation complexes and plant communities. These plant communities consist of recognisable and reproducible associations of plant types which are subject to natural laws under the same ecological conditions. Wherever one finds similar habitat conditions in comparable bioregions or floristic zones on the planet, similar communities exist and can be typified. Such determinative plant community-habitat-type systems possess high bioindicator value for different biotic and abiotic habitat conditions. The floristic compositions and structure of plant communities and biotope-types can be categorised, and such vegetation units can be abstracted as elementary types, marked by their characteristic species combination under certain habitat-dependent conditions. Phytosociology provides the scientific background and method to address these questions. It was established by Josias Braun-Blanquet (Braun-Blanquet J. 1918. Eine pflanzengeographische Exkursion durch Unterengadin und in den schweizerischen Nationalpark. Beitr Geobot Landesaufnahme 4: 1-80.) and promoted for example in Germany by Reinhold Tü xen (Tü xen R. 1937. Die Pflanzengesellschaften Nord-Westdeutschlands. Mitt. Flor. Soz. Arbeitsgemein. Nieders. 3, Hannover, 170 p.). The Flora-Fauna-Habitat-Guideline (FFH-Natura 2000), enacted on 21 May 1992 established homogenous criteria for endangered biotypes throughout Europe, founded on a modern phytosociological basis.Phytosociological terminology also forms the basis of biotype-differentiation in the UNESCO Convention on Biodiversity (COP9). Vegetation science is a socially and politically critical discipline, serving to benefit and progress human society and sustainable usage of its natural resources.
The effects of biodiversity on ecosystem functions have been extensively studied, but little is known about the effects of ecosystem functions on biodiversity. This knowledge is important for understanding biodiversity-ecosystem functioning relationships. Desertification reversal is a significant global challenge, but the factors that play key roles in this process remain unclear. Here, using data sampled from areas undergoing desertification reversal, we identify the dominant soil factors that play a role in vegetation recovery with ordinary least squares and structural equation modelling. We found that ecosystem functions related to the cycling of soil carbon (organic C, SOC), nitrogen (total N, TN), and potassium (available K, AK) had the most substantial effects on vegetation recovery. The effects of these ecosystem functions were simultaneously influenced by the soil clay, silt and coarse sand fractions and the soil water content. Our findings suggest that K plays a critical role in ecosystem functioning and is a limiting factor in desertification reversal. Our results provide a scientific basis for desertification reversal. Specifically, we found that plant biodiversity may be regulated by N, phosphorus (P) and K cycling. Collectively, biodiversity may respond to ecosystem functions, the conservation and enhancement of which can promote the recovery of vegetation.
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