Microbial genomic traits and soil stoichiometry drive nitrogen stabilization in maize–peanut intercropping system
摘要
Legume–cereal intercropping is widely recognised for increasing soil nitrogen (N) stocks, yet the microbial mechanisms driving this N retention remain poorly understood. In this study, we focus on how microbial community genomic traits and soil extractable nutrient stoichiometry impact on soil N accumulation.
MethodsWe conducted a five year maize–peanut field experiment under three N fertilization levels (0, 150, 300 kg N ha⁻1 yr⁻1), we examined soil organic N fractions, microbial community-averaged genomic traits (genome size and Guanine-Cytosine content), and soil extractable nutrient stoichiometry and their relationships.
ResultsIntercropped peanut soils accumulated significantly more total N than monocultures, primarily through reduced amino acid N and elevated recalcitrant fractions (non-hydrolysable N and unidentified hydrolysable N). This enhanced N stabilisation was closely linked to significantly smaller bacterial community-averaged genome sizes in peanut (versus maize) soils and to lower extractable N:carbon (C), N: phosphorus (P), and N: potassium (K) ratios, indicating a relief of microbial C, P, and K limitation. Nitrogen fertilization enlarged bacterial genome size in most treatments, consistent with induced co-limitation by non-N nutrients. Community-averaged genomic traits, especially bacterial genome size, combined with extractable nutrient stoichiometry, showed strong relationships with soil N fractions and provided substantially high predictive power (across several machine-learning algorithms).
ConclusionThese findings reveal that maize–peanut intercropping promotes long-term soil N retention through shifts in microbial life-history traits and nutrient stoichiometry, offering new trait-based predictors of N cycling in low-input agroecosystems.