Journal of Plant Ecology

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  • 收稿日期:2026-05-30 修回日期:2026-08-27 接受日期:2026-10-02

Microbial-derived carbon outweighs plant-derived carbon in soil carbon accumulation under woody intercropping in tea plantations

Sheng Tang1, Kang Ni2, Yaqin Long3*, Qingxu Ma4, Xiu Liu1, Lifeng Ma2, Yuanzhi Shi2, Linbo Chen3*, Xiangde Yang2*, Jianyun Ruan2   

  1. 1. Anhui Province Key Lab of Farmland Ecological Conservation and Nutrient Utilization;
    Anhui Province Engineering and Technology Research Center of Intelligent Manufacture and Efficient Utilization of Green Phosphorus Fertilizer, College of Resources and Environment, Anhui Agricultural University, Hefei, 230036, P. R. China;
    2. Tea Research Institute, Chinese Academy of Agricultural Sciences, State Key Laboratory of Tea Plant Germplasm Innovation and Resource Utilization, Hangzhou 310008, China;
    3. Yunnan Key Laboratory of Tea Science, Tea Research Institution, Yunnan Academy of Agricultural Sciences, Kunming 650200, China;
    4. Ministry of Education Key Lab of Environmental Remediation and Ecosystem Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
    *Corresponding author: Linbo Chen (chenlinbo2002@sina.com); Xiangde Yang(yangxd@tricaas.com)
  • Received:2026-05-30 Revised:2026-08-27 Accepted:2026-10-02
  • Supported by:
    This research was supported by the Yunnan provincial special fund for the construction of a science and technology innovation base (202402AE090015), National Key Research and Development Program of China (2021YFD1601100), China Agriculture Research System of MOF and MARA (CARS-18), and National Natural Science Foundation of China (32402680, 42407459, U24A20575).

Abstract: Soil organic carbon (SOC) sequestration in agroecosystems is critical for climate change mitigation, yet the microbial pathways through which plant diversity influences SOC accumulation remain poorly understood. Using a multisite paired observational survey combined with multi-omics analyses, we investigated the microbial mechanisms underlying soil carbon dynamics in tea (Camellia sinensis) plantations under woody intercropping. Compared with monoculture, intercropping increased SOC and particulate organic carbon (POC) by 33.5% and 43.3%, respectively, whereas mineral-associated organic carbon (MAOC) remained unchanged. Microbial necromass carbon—particularly fungal necromass—increased significantly, while plant-derived carbon did not differ between treatments, suggesting that the observed carbon accumulation was primarily derived from microbial transformation rather than increased plant-derived inputs. Intercropping intensified microbial nitrogen limitation, increased the relative abundance of N-cycling functional genes, and shifted fungal community composition from Ascomycota towards Basidiomycota. Random forest modeling further revealed that NO3- was the strongest predictor of POC variation, whereas microbial necromass carbon was the strongest predictor of MAOC variation, suggesting that N availability and microbial transformation processes differentially regulate the accumulation of distinct SOC fractions. Collectively, our findings demonstrate that microbial-derived carbon contributes more than plant-derived carbon to soil carbon accumulation under woody intercropping, and that microbial necromass plays a particularly important role in predicting the accumulation of the more persistent MAOC pool. These results highlight microbial N limitation as a potential ecological linkage between plant diversity and soil carbon persistence, and provide a trait-based framework for managing plant–microbe interactions to enhance carbon sequestration in perennial agroforestry systems.

Key words: carbon sequestration, intercropping, nitrogen limitation, soil organic carbon, tea plantation