Ping Qin, Xu Sheng, He Xingyuan, Sun Sining
CAS Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; University of Chinese Academy of Sciences, Beijing 100049, China.
CAS Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; University of Chinese Academy of Sciences, Beijing 100049, China; Liaoning Shenyang Urban Ecosystem Observation and Research Station, Shenyang 110164, China.
Sci Total Environ. 2025 Jun 25;983:179705. doi: 10.1016/j.scitotenv.2025.179705. Epub 2025 May 21.
Litter chemical traits critically regulate decomposition dynamics and are highly responsive to atmospheric nitrogen (N) deposition, yet the magnitude of their responses and their mechanistic roles in decomposition under N enrichment remain uncertain. Here, we synthesized data from 80 studies to quantify the effects of N addition on litter chemistry and decomposition rates. Our analysis reveals that N addition significantly increases litter N (+34.6 %) and phosphorus (P, +18.5 %) concentrations, while reducing lignin (-2.2 %), cellulose (-2.2 %), and hemicellulose (-2.7 %). Moreover, key stoichiometric ratios-C/N (-23.8 %) and lignin/N (-25.4 %)-decreased, thereby enhancing litter quality. These shifts were more pronounced in herbaceous plants and grassland ecosystems compared to woody plants and forests. Nitrogen enrichment accelerated decomposition of herbaceous plant litter in both common-site and in-situ experiments but had no significant effect on woody plant litter. Decomposition rates (k) in herbaceous plant litter correlated strongly with initial traits-including N, phosphorus (P), calcium (Ca), cellulose, and stoichiometric ratios-whereas woody litter decomposition depended primarily on Ca. Our findings reveal that plant functional types and ecosystems govern decomposition responses to N deposition: grasslands exhibit accelerated decomposition via improved litter quality, while forests exhibit attenuated or even negative decomposition responses due to microbial suppression and inhibition of lignin degradation under. Integrating these trait-mediated mechanisms into biogeochemical models will refine predictions of carbon and nutrient cycling under global N enrichment, particularly in contrasting grassland and forest ecosystems.
凋落物化学特性严格调控分解动态,并且对大气氮(N)沉降高度敏感,然而在氮富集条件下其响应程度及其在分解过程中的作用机制仍不明确。在此,我们综合了80项研究的数据,以量化氮添加对凋落物化学性质和分解速率的影响。我们的分析表明,添加氮显著增加了凋落物的氮含量(+34.6%)和磷(P,+18.5%)含量,同时降低了木质素(-2.2%)、纤维素(-2.2%)和半纤维素(-2.7%)的含量。此外,关键化学计量比——碳氮比(-23.8%)和木质素氮比(-25.4%)——降低,从而提高了凋落物质量。与木本植物和森林相比,这些变化在草本植物和草地生态系统中更为明显。在常见地点和原位实验中,氮富集均加速了草本植物凋落物的分解,但对木本植物凋落物没有显著影响。草本植物凋落物的分解速率(k)与初始特性——包括氮、磷(P)、钙(Ca)、纤维素和化学计量比——密切相关,而木本凋落物的分解主要取决于钙。我们的研究结果表明,植物功能类型和生态系统决定了对氮沉降的分解响应:草地通过改善凋落物质量表现出加速分解,而森林由于微生物抑制和对木质素降解的抑制,表现出分解响应减弱甚至为负。将这些由特性介导的机制纳入生物地球化学模型,将改进对全球氮富集下碳和养分循环的预测,特别是在对比明显的草地和森林生态系统中。