Fungal transformations of uranium oxides
Article first published online: 28 MAR 2007
Volume 9, Issue 7, pages 1696–1710, July 2007
How to Cite
Fomina, M., Charnock, J. M., Hillier, S., Alvarez, R. and Gadd, G. M. (2007), Fungal transformations of uranium oxides. Environmental Microbiology, 9: 1696–1710. doi: 10.1111/j.1462-2920.2007.01288.x
- Issue published online: 28 MAR 2007
- Article first published online: 28 MAR 2007
- Received 21 November, 2006; accepted 7 February, 2007.
The biogeochemical activities of free-living and symbiotic fungi must be acknowledged in attempts to understand uranium cycling and dispersal in the environment. Although the near-surface geochemistry of uranium is very complex and a wide variety of mineral phases is known, uranium trioxide (UO3) and triuranium octaoxide (U3O8) can be used as well characterized models in the study of biotransformations. We have used a complex methodological approach involving advanced solid state speciation and scanning electron microscopy to study the ability of saprotrophic, ericoid and ectomycorrhizal fungi to transform these model oxides. This study has revealed that fungi exhibit a high uranium oxide tolerance, and possess the ability to solubilize UO3 and U3O8 and to accumulate uranium within the mycelium to over 80 mg (g dry weight)−1 biomass. X-ray absorption spectroscopy of uranium speciation within the biomass showed that in most of the fungi the uranyl ion was coordinated to phosphate ligands, but in ectomycorrhizal fungi mixed phosphate/carboxylate coordination was observed. Abundant uranium precipitates associated with phosphorus were found in the mycelium and encrusted the hyphae. Some of the fungi caused the biomineralization of well-crystallized uranyl phosphate minerals of the meta-autunite group. This is the first experimental evidence for fungal transformations of uranium solids and the production of secondary mycogenic uranium minerals.