Linking Global Patterns of Nitrogen Resorption with Nitrogen Mineralization During Litter Decomposition

The nitrogen (N) cycle in terrestrial ecosystems is strongly influenced by resorption prior to litter fall and by mineralization after litter fall. Although both resorption and mineralization make N available to plants and are influenced by climate, their linkage in a changing environment remains largely unknown. Here, we show that, at the global scale, increasing N resorption efficiency has a negative effect on the N mineralization rate. With increasing temperature and precipitation, the increasing rate of the N cycle is closely related to the shift from the more conservative resorption pathway to an acquiring mineralization pathway. Furthermore, systems with faster N-cycle rates support plants with higher foliar N:P ratios and microbes with lower fungi:bacteria ratios. We highlight the importance of considering the geographic pattern and the dynamic interaction between N resorption and N mineralization, which should be incorporated into earth-system models to improve the simulation of nutrient constraints on ecosystem productivity.