Purpose: Wild re, an increasing disturbance in peatlands, could dramatically change carbon stocks and reshape plant/microbial communities, with longlasting effects on peatland functions. Soil fungi are important in controlling the belowground carbon and nutrient cycling in peatlands; however, the impact of altered re regimes on these fungi is still unclear.Methods: Here we assessed fungal abundance, composition, and diversity across four soil depths (0-5 cm, 6-10 cm, 11-15 cm, 16-20 cm) under lowintensity and high-intensity re in a subtropical peatland in the southeastern USA.Results: Low-intensity re signi cantly increased fungal Shannon diversity and the saprotrophic fungal composition in the 0-5 cm soil layer immediately and then retracted within 2 years. Such hump-shaped pattern, however, were not observed in deeper soils. The dominant fungal class Archaeorhizomycetes declined initially and then returned to pre-low-intensity res levels at 0-5 cm depths. Time since low-intensity re was a primary driver of fungal composition in the 0-10 cm soil depth, while geographical distance among sites affected the deeper soils (11-20 cm). The fungal Shannon diversity failed to recover to the unburned state even after 30 years after high-intensity re, especially in 6-20 cm soil depths. Strati cation patterns of the fungal community was diminished by high-intensity re. Soil properties (either phenolics or carbon) were the primary drivers in shaping fungal community reassembly after highintensity re across all soil depths. Conclusion: Collectively, the fungal communities seem to be highly resilient to low-intensity re, but not to high-intensity re in our shrub bog peatlands.