Abstract Nitrogen (N) input is one of the key global change contributors that has profound effects on the carbon (C) and N cycling of wetland ecosystems. However, the information is very limited on the response patterns of wetland productivity to N input-induced changes in elemental stoichiometric composition. Here we investigated the effects of global N input on the stoichiometry and productivity of wetland ecosystems using 103 individual data points from 74 studies. The results showed that global N input significantly enhanced wetland aboveground and belowground productivity by 45.5% and 21.7%, respectively. N input significantly altered C and N content of plant, soil and microbes: C content increased significantly in plant roots (4.9%), soil (4.8%), and microbes (29.3%), but decreased significantly in plant stems (0.8%); also, C content in plant leaf tissue showed no significant change. While N content increased significantly in all components. N input generally enhances wetland productivity and reduces C:N ratios across ecosystem components, but its effect intensity is modulated by multiple environmental factors. More critically, statistical analysis reveals that changes in C/N stoichiometry in plant stems—rather than in plant leaves or roots—constitute the core mechanism linking N input to wetland productivity responses. This mechanism explains 31.0% and 56.3% of the variation in above-ground and below-ground productivity, respectively. Our meta-analysis shows that plant stems stoichiometry under N input is key factor to wetland productivity. These responding processes contribute to a better understanding of the N input induced changes in wetland productivity, and improve ecosystem modeling.
Lu et al. (2026) studied this question.