Effect of Slope Aspect on Plant Above‐ and Belowground Functional Traits of Alpine Meadow on the Qinghai‐Tibet Plateau, China

Abstract

AbstractSlope aspects could cause significant differences in microclimate (e.g., radiation and moisture) and edaphic properties (e.g., soil nutrients content) in rugged landscapes. Therefore, understanding the variations of the above‐ and belowground functional traits on hillslope scales and their driving factors are essential for disentangling the plant adaptive strategies to local environmental factors. Based on the measurements of community weighted mean traits of alpine meadow from 15 hillslopes (eight south‐facing and seven north‐facing) in the Qinghai Lake watershed, northeastern Qinghai‐Tibet Plateau, China, we found that the aboveground morphological traits that is, specific leaf area and leaf dry matter content, and belowground stoichiometric traits, that is, root carbon content (RCC), root nitrogen content (RNC), root phosphorus content (RPC) and RCC: RNC, varied significantly between slope aspects. Hierarchical partitioning indicated that the slope aspect contributed the most to the variations of aboveground morphological and belowground stoichiometric traits, whereas soil properties were the major contributor to aboveground phosphorous‐related traits and belowground morphological traits. Both above‐ and belowground traits displayed a two‐dimensional variation on the hillslope scale. Additionally, the above‐ and belowground traits were weakly coordinated. In general, alpine meadow on the south‐facing slopes tended to adopt the conservative strategy, while acquisitive strategy was preferred by that on the north‐facing slopes. These findings can improve our understanding of spatial variations of functional traits at fine scales, and we highlighted that it is helpful to integrate both above‐ and belowground traits dimensions in disentangling the ecological process and predicting ecosystem function under changing climate.