Global wildfires occurring with ever escalating frequency and intensity profoundly disrupt soil phosphorus (P) cycling in forest ecosystems. The impact of plant species on post-fire soil P transformation, particularly in alpine forests, remains largely unexplored. This study addressed this gap by investigating both bulk soils (BS) and root-zone soils (RS) across three plant species (shrub: Sophora davidii and Quercus aquifolioides, tree: Pinus densata) in the alpine forest of the eastern Tibetan Plateau, three years after a wildfire event. We examined variations in soil P fractions under varying wildfire intensities using the modified Hedley sequential extraction method. Compared to unburned soils, the burned soils exhibited significantly reduced organic P (Po) but increased inorganic P (Pi) concentrations in BS. However, both Pi and Po concentrations decreased in the burned RS, particularly for S. davidii and P. densata, indicating the effects of biological P utilization. The increased specific phosphatase activity and the ratio of carbon to Po suggested increased P limitation in the post-fire environment. Notably, the N2-fixer S. davidii primarily reduced labile P fractions through direct plant P uptake, while conifer tree species P. densata tended to deplete all extractable P fractions, probably through diverse P utilization strategies. Conversely, Q. aquifolioides did not significantly alter soil P fractions, likely due to its fire-resistant properties. These species-dependent impacts on post-fire P fractions were further corroborated by their distinct influences on soil and microbial traits. Our findings underscore the critical roles of functional-specific plant species in post-fire soil P dynamics in alpine forests, with conifer trees exhibiting the best P mining and utilization capacity.