The escalating global demand for sustainable agriculture necessitates the development of effective biological alternatives to conventional chemical fertilizers, particularly those addressing phosphorus (P) use efficiency. This study focused on the isolation and detailed characterization of phosphate-solubilizing fungi from soil or compost to evaluate their impact and potential for use as biofertilizers. Fungal isolation was performed using serial dilution from various sources, followed by molecular and morphological characterization to identify promising strains. Four strains were ultimately selected and identified using morphological, biochemical, and molecular techniques: Aspergillus flavus (CM1), Penicillium crustosum (C3), Penicillium fellutanum (C4), and Metarhizium robertsii (J1). The most active strain was initially tested in liquid and solid media supplemented with synthetic P (Ca 3 (PO 4 ) 2 ) and was evaluated by measuring fungal biomass and P titration. This strain demonstrated good growth and activity, supporting an optimal temperature of 25°C, a pH of 3, an ammonium concentration of 1.5 g/L, and a glucose addition of 25.0 g/L. The biofertilization potential of the selected strains was then comprehensively evaluated through controlled experiments, including the optimization of growing conditions, quanti fication of soluble P under hermetic storage in soil, and measurement of soil fungal populations to assess their impact. P transformation experiments conducted in hermetic jars showed that CM1 had the highest CO 2 release (approximately 7115.30 mg CO 2 /100 g soil) and the highest soluble P levels at the final sampling time (78.85 mg/L), thus outperforming the other strains. Furthermore, in soil hermetic jars, CM1 (reaching up to 26×10 4 CFU (colony forming units)/g soil) and C4 significantly enhanced soil microbial activity and P bioavailability. These results clearly highlight the potential of the selected fungal strains as biofertilizers to improve P availability and boost crop productivity in P-deficient soils.
Ammeri et al. (Sun,) studied this question.