Aims: Soil bacterial communities serve as pivotal links sustaining plant–soil interaction processes. They play essential roles in regulating soil biogeochemical cycles, facilitating plant community succession, and driving the restoration of soil ecological functions. Currently, the compositional shifts, diversity patterns, functional succession, and underlying factors of soil bacterial communities during vegetation restoration in degraded high-altitude forest ecosystems remain poorly understood.
Methods: We investigated degraded post-fire forest sites of Yulong Snow Mountain in Northwest Yunnan, China. Vegetation was restored using the native tree species Abies georgei and sub-shrub Paeonia delavayi for 1-year, 3-year, and 6-year, with bare ground formed by post-fire forest undergoing natural succession as a control. The physicochemical properties of the rhizosphere soil of Paeonia delavayi were characterized, and Illumina MiSeq high-throughput sequencing was employed to analyze the composition, diversity, functional succession and their relations of soil bacterial communities across different restoration years.
Results: (1) The soil organic carbon (SOC), total nitrogen (TN), available nitrogen (AN), total phosphorus (TP), and soil moisture content (SMC) in 3-year restoration sites were significantly lower than those in bare ground. Conversely, total potassium (TK) and pH were significantly higher than those in 1-year and 6-year restoration sites and bare ground. Available phosphorus (AP) and available potassium (AK) in 6-year restoration sites were significantly higher than those in bare ground. (2) Shannon-Wiener diversity index, Simpson diversity index, and Pielou evenness index of soil bacterial communities were significantly lower in 3-year and 6-year restoration than in 1-year restoration and bare ground, though Chao1 index showed no significant differences across restoration years. β-diversity showed significant alterations across restoration years. Compared with bare ground, the relative abundances of Pseudomonadota, Acidobacteriota, and Verrucomicrobiota decreased significantly, whereas Actinomycetota and Gemmatimonadota increased significantly. Chloroflexota peaked in 1-year restoration. The relative abundances of Bradyrhizobium and Mycobacterium (involved in nitrogen cycling) and Gemmatimonas (involved in phosphorus cycling) in 3-year restoration sites were significantly higher than those in bare ground, whereas the relative abundances of Reyranella and Bacillus (biocontrol-associated genera) in 6-year restoration sites were significantly lower than those in bare ground. (3) Redundancy analysis indicated that AN, AK, TK, TN, SOC, SMC, and pH significantly shaped bacterial community composition. Structural equation modeling demonstrated that: soil bacterial community diversity exhibited a significant negative correlation with restoration years, while SOC indirectly influenced the community composition by regulating total nutrient content and pH. Conversely, restoration years positively enhanced soil bacterial community composition through indirect effects on available nutrients.
Conclusion: A critical shift in the rhizosphere soil of Paeonia delavayi—encompassing physicochemical characteristics, bacterial diversity, abundance of dominant species, and the composition of functional groups—occurred at the 3-year mark of restoration in the degraded post-fire forest. We hypothesized that soil available nutrients continuously improved with restoration years, and the bacterial community composition improved significantly in the later stages of vegetation restoration.