Do water–energy dynamics drive plant species richness patterns on the high alpine Tibetan plateau?

Abstract

Knowledge on the spatial distribution of plant species richness and its associated factors is crucial for addressing several ecological problems. Climate factors have long been used to explain species richness patterns across space and time. In this study, we investigated how water and energy variables shape species richness patterns on the alpine Tibetan plateau. An empirical study involving 800 plots of size 1 m² on 80 different sites was conducted across two transects, covering the arid and semi-arid alpine region of the western part of the Tibetan plateau to explore plant species composition and richness in relation to climatic factors at a regional scale. We performed detrended correspondence analysis and generalized linear models to explore the effect of energy and water variables on species composition and species richness, respectively. We used a generalized linear mixed model to investigate the interactive effect of energy variables and water variables on species richness. We found that both energy variables and water variables significantly influenced species richness and composition on the alpine Tibetan plateau and supported the water–energy dynamics (WED) hypothesis. Specificall, plant species richness increased with greater liquid water availability. However, it exhibited a unimodal relationship with potential evapotranspiration. Our results also showed that precipitation played a more substantial role in the model than potential evapotranspiration, but their interaction strengthened the model. In conclusion, this study highlights the dominant role of precipitation in explaining species composition and richness patterns on the alpine Tibetan plateau and suggests conducting research on additional environmental factors affecting water availability in this region.