Community-weighted mean traits but not functional diversity determine the changes of soil properties during wetland drying on the Tibetan Plateau
Abstract. Climate change and human activities have caused a shift in vegetation composition and soil biogeochemical cycles of alpine wetlands on the Tibetan Plateau. The primary goal of this study was to test for associations between community-weighted mean (CWM) trait and functional diversity, and soil properties during wetland drying. We collected soil samples and investigated the above-ground vegetation in swamp, swamp meadow and typical meadow; four CWM trait values (specific leaf area, SLA; leaf dry matter content, LDMC; leaf area, LA; and mature plant height, MPH) for 42 common species were measured across the three habitats; three components of functional diversity (functional richness; functional evenness; and functional divergence) were also quantified in these sites. Our results showed that the drying of the wetland dramatically altered plant community and soil properties. There was a significant correlation between CWM of traits and soil properties, but not a significant correlation between functional diversity and soil properties. Our results further showed that CWM-LA, CWM-SLA and CWM-LDMC had positive correlations with soil readily available nutrients (available nitrogen, AN; available phosphorus, AP), but negative correlations with total soil nutrients (soil organic carbon, SOC; total nitrogen TN; and total phosphorus, TP). Our study demonstrated that simple, quantitative plant functional traits, but not functional diversity, are directly related to soil C / N properties, and likely play an important role in plant-soil interactions, and our results also suggest that functional identity of species may be more important than functional diversity in influencing ecosystem processes during wetland drying.