All living things need phosphorus to survive. However, its low availability in soil is often a limiting factor for plant and microbial growth. Microorganisms in the plant root-soil interface (rhizosphere) can convert non-labile phosphorus into bioavailable forms. One way microbes do this is the mineralization of organic phosphorus compounds like phytate. Rising atmospheric CO₂ levels may accelerate mineralization, but the molecular mechanisms are not yet understood. Recent research confirmed that elevated CO₂ (eCO₂) increased the mineralization of phytate in the rhizosphere of wheat. Tracing the carbon flow showed that plants grown under eCO₂ increased the release of bioavailable carbon belowground, which corresponded to increased microbial growth and altered community composition. The bacterial community under eCO₂ favored groups of bacteria capable of degrading aromatic phosphorus compounds and the mycorrhizal fungi benefited from the increased supply of phosphorus and carbon. This proliferation of bacteria and mycorrhiza likely drove increased competition for phosphorus, further increasing the need to mineralize it. While further research into the potential synergies between symbiotic mycorrhizas and rhizosphere bacteria is needed, these results suggest that accelerated mineralization in crop rhizospheres under eCO₂ is likely due to the stimulation of microbial carbon and phosphorus metabolisms.