Dissolved organic matter (DOM) plays a key role in forest carbon biogeochemistry by linking soil organic carbon (SOC) sequestration and water fluxes, which is further shaped by elevated atmospheric nitrogen (N) deposition. Although enhanced SOC sequestration was evidenced in tropical forests...

　　World-wide, forests are experiencing drought-induced mortality. However, physiological adaptation to drought is highly variable, which may lead to differential mortality patterns and alter community structure. In this study, saplings of four common tree species (Ormosia pinnata, Dalbergia od...

　　Climate warming has significantly altered the phenology of plants in recent decades. However, in contrast to the widely reported warming-induced extension of vegetative growing season, the response of fruit development period (FDP) from flowering to fruiting remains largely unexplored, parti...

　　Warming affects the carbon cycle process of the terrestrial ecosystem by affecting the counterbalance between carbon input and output, and the stability of the carbon pool. Although most studies showed that warming decreased soil organic carbon (SOC) content, there is still great uncertainty...

　　Phosphorus (P) is one of the most important limiting nutrients in terrestrial ecosystems. The soils represent the largest P reserve (He et al., 2021a), which P storage determines the form and supply of soil P to plants, potential affecting the function of forest ecosystems. However, our unde...