Microbial physiological traits are key determinants of soil organic carbon (SOC) accumulation under long-term fertilization, yet their adaptability to carbon (C) and nutrient gradients, and the corresponding C feedback effects, remain largely unexplored. Here, we conducted a 33-year field experiment with mineral and mineral-organic combined fertilization (NPKM) across two contrasting soil types (nutrient-rich vs. nutrient-poor). The 18O-H2O tracer method and amino sugar biomarker approaches were used to explore the trends of microbial C use efficiency (CUE) and microbial C pump efficacy (MCP), while metagenomic analysis and environmental variables were integrated to clarify the intrinsic and extrinsic effects of long-term fertilization on these microbial traits. Our results revealed divergent responses of SOC fractions to NPKM across soil types: relative to the control (CK), NPKM increased particulate organic carbon (POC) by 130% in nutrient-rich soils, the 33.46% rise in mineral-associated organic carbon (MAOC); in contrast, only MAOC exhibited a significant increase (80.86%) in nutrient-poor soils. Further analysis confirmed that microbial physiological traits drove the changes in POC and MAOC depending on soil nutrient status under long-term fertilization. Specifically, in nutrient-poor soils, NPKM enhanced MAOC by increasing CUE (100%) and MCP (45.34%), an effect mediated by C-degradation functional genes. In nutrient-rich soils, NPKM promoted POC by improving CUE (48.48%), a process regulated by abiotic factors. These findings highlight that initial nutrient levels regulate microbial physiological traits, thereby dictating the accumulation dynamics of different C fractions, which offers a theoretical basis for targeted agricultural C management strategies.
扫码关注我们
求助内容:
应助结果提醒方式:
