CaCO₃ and SrCO₃ bioprecipitation by fungi isolated from calcareous soil

The urease-positive fungi Pestalotiopsis sp. and Myrothecium gramineum, isolated from calcareous soil, were examined for their properties of CaCO₃ and SrCO₃ biomineralization. After incubation in media amended with urea and CaCl₂ and/or SrCl₂, calcite (CaCO₃), strontianite (SrCO₃), vaterite in different forms [CaCO₃, (Ca_xSr_1−x)CO₃] and olekminskite [Sr(Sr,Ca)(CO₃)₂] were precipitated, and fungal ‘footprints’ were observed on mineral surfaces. The amorphous precipitate mediated by Pestalotiopsis sp. grown with urea and equivalent concentrations of CaCl₂ and SrCl₂ was identified as hydrated Ca and Sr carbonates by Fourier transform infrared spectroscopy. Liquid media experiments showed M. gramineum possessed the highest Sr²⁺ removal ability, and ∼ 49% of supplied Sr²⁺ was removed from solution when grown in media amended with urea and 50 mM SrCl₂. Furthermore, this organism could also precipitate 56% of the available Ca²⁺ and 28% of the Sr²⁺ in the form of CaCO₃, SrCO₃ and (Ca_xSr_1−x)CO₃ when incubated in urea-amended media and equivalent CaCl₂ and SrCl₂ concentrations. This is the first report of biomineralization of olekminskite and coprecipitation of Sr into vaterite mediated by fungi. These findings suggest that urease-positive fungi could play an important role in the environmental fate, bioremediation or biorecovery of Sr or other metals and radionuclides that form insoluble carbonates.