Zixin Chen, Kai Dong, Julian Helfenstein, Dafeng Hui, Constantin M. Zohner, Frank Hagedorn, Manuel Delgado‐Baquerizo, Adam R. Martin, Jiguang Feng, Nan Yang, Xinli Chen, Laurent Augusto, Qin Deng, Enqing Hou, Mingkai Jiang, Qingshui Yu, Haihua Shen, Jordi Sardans, Josep Peñuelas, Hans Lambers, Jingyun Fang, Zhengbing Yan
Anthropogenic phosphorus (P) inputs are rapidly altering terrestrial P cycling through plant - soil - microbial interactions; however, global patterns and underlying mechanisms driving these changes remain poorly understood. By performing a global meta-analysis of 1315 observations from 176 studies across diverse natural terrestrial ecosystems, we found that P addition increased P concentrations in foliage, stems, roots, and litter by 62%, 114%, 100% and 63%, respectively. Soil total P, plant-available P, and microbial P concentrations rose by 43%, 221%, and 70%, while leaf P-resorption efficiency and soil phosphatase activity declined by 23% and 15%, respectively. Stem P and soil phosphatase activity exhibited consistent trends across tropical, temperate, and boreal zones, suggesting climate-specific P acquisition strategies. In addition, foliar P responses diverged among ecosystem and plant functional types. These responses were primarily regulated by background soil total P concentration, precipitation, soil pH, and P addition duration and rate. Our findings provide critical insights into the potential consequences of increasing anthropogenic P inputs in natural terrestrial ecosystems, improving our understanding of nutrient cycling and informing future ecosystem management under ongoing global change.