Differential ecological stoichiometry of leaf and fine root litter decomposition under ozone stress

HOU Xiaofan, MA Chenhan, SUN Yuqian, GAO Yuhan, LI Pin   

  1. State Key Laboratory of Efficient Production of Forest Resources、The Key Laboratory for Silviculture and Conservation of Ministry of Education, Key Laboratory for Silviculture and Forest Ecosystem of State Forestry and Grassland Administration, Beijing forestry university 100083, China
  • Received:2025-06-18 Revised:2025-10-28
  • Contact: LI, Pin
  • Supported by:
    Supported by the National Natural Science Foundation of China(32271673); and the 5·5 Engineering Research & Innovation Team Project of Beijing Forestry University(BLRC2023B06); the National Natural Science Foundation of China(32271673); the 5·5 Engineering Research & Innovation Team Project of Beijing Forestry University(No: BLRC2023B06)

Abstract: Aims Elevated atmospheric ozone (O₃) concentrations significantly affect plant nutrient allocation, thereby regulating litter decomposition. However, the stoichiometric responses of leaf and fine root litters to O₃ stress remain unclear. This study aimed to investigate how elevated O₃ influences the dynamics and regulatory mechanisms of carbon (C), nitrogen (N), and phosphorus (P) stoichiometry during the decomposition of leaf and fine root litter. Methods A 12-month decomposition experiment was conducted using Koelreuteria paniculata and Camellia sinensis at the O₃-FACE platform in Yanqing, Beijing. Two O₃ treatments were applied: ambient air (NF) and elevated O₃ (NF60, ambient air + 60 ppb O₃). At four decomposition stages (T0, T1, T3, and T12), we measured litter C, N, and P concentrations and stoichiometric ratios (C/N, C/P, N/P). Important findings Elevated O₃ significantly altered the initial stoichiometric structure and residual characteristics of the litter. Under NF60, the initial C/N ratio of K. paniculata leaves increased by 7.6%, while N/P decreased by 17.7%, leading to a 10.3% increase in residue mass after 12 months. For C. sinensis fine roots, P concentration increased by 11.1% and C/P decreased by 14.5%, indicating enhanced P redistribution. Litter residue was significantly correlated with C/N, C/P, and N/P ratios (P < 0.05). During decomposition, the N/P ratio in K. paniculata and C. sinensis leaves increased by 43.6%–68.0% and 52.9%–59.3%, respectively, suggesting strengthened phosphorus limitation in later stages, consistent with the “Growth Rate Hypothesis” and the “N:P Threshold Hypothesis.” Elevated O₃ induces a “high-C/low-P” stoichiometric pattern, exacerbating microbial nutrient limitation and slowing carbon mineralization. Leaves and fine roots exhibit contrasting responses: K. paniculata leaves are more constrained by P availability, while C. sinensis fine roots maintain higher decomposition efficiency through enhanced P redistribution. These findings highlight organ-specific adaptive strategies to O₃ stress and provide novel insights into stoichiometric regulation of litter decomposition under global change.

Key words: Ecological stoichiometry, Litter decomposition, Ozone stress, C/N/P, Leaves and fine roots