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Pattern of elemental release during the granite dissolution can be changed by aerobic heterotrophic bacterial strains isolated from Damma Glacier (Central Alps) deglaciated granite sand
Lapanje, A., Wimmersberger, C., Furrer, G., Brunner, I., & Frey, B. (2012). Pattern of elemental release during the granite dissolution can be changed by aerobic heterotrophic bacterial strains isolated from Damma Glacier (Central Alps) deglaciated granite sand. Microbial Ecology, 63(4), 865-882. https://doi.org/10.1007/s00248-011-9976-7