Abstract
Pseudogymnoascus destructans (Pd), the causative agent of bat white‐nose syndrome, persists in cave soils and acts as a chronic source of infection, yet the environmental processes governing this reservoir remain unclear. We performed seasonal sampling of bat cave soils in Northeast China and combined metagenomic, untargeted metabolomic and physicochemical analyses to identify drivers of Pd loads. Pd abundance tracked strong seasonal gradients in temperature, soil water content, electrical conductivity and nitrogen availability. The microbial community structure exhibited pronounced seasonal variation, primarily associated with pH, and was governed predominantly by stochastic ecological processes. Nitrogen‐cycling genes showed a switch from nitrogen fixation and nitrification in summer to denitrification and nitrate reduction in winter. Antibiotic resistance genes and mobile genetic elements covaried with core bacterial taxa, while antifungal metabolites such as tetracycline, glycitin and chrysin were positively associated with putatively antagonistic genera (e.g., Rhodanobacter , Pseudomonas , Streptomyces , and Bacillus ), indicating a microbe–metabolite defence network. Structural equation modelling revealed a temperature‐driven cascade linking nutrient cycling, microbial communities, metabolite profiles and Pd loads. Our results show that seasonal dynamics of Pd in cave soils emerge from interactions between climate‐regulated soil processes and microbe–metabolite feedbacks, with implications for environmental control of pathogenic fungi.