ABSTRACT. Two hypotheses were tested: (1) microbial dephosphorylation of phytate in the presence of Ca 2+ ions will result in the precipitation of hydroxyapatite-like crystals and (2) precipitation of calcium-phosphate crystals on and between sand-like particles can cause cementation. A growing culture of the dimorphic phytase-active yeast Arxula adeninivorans was introduced into a column filled with quartz particles and subsequently a liquid growth medium amended with calcium phytate was pumped through the column resulting in increased strength and stiffness of the quartz particle matrix. Environmental scanning electron microscope analysis combined with energy-dispersive X-ray measurement revealed cementation of the quartz particles by calcium-phosphate crystals. This microbial mineralization process could provide a novel approach to improving the mechanical properties like strength and stiffness of sandy soils. Microbial metabolic activities often contribute to selective cementation processes by producing relatively insoluble organic and inorganic compounds. Microbially induced biomineralization, such as calcite (CaCO 3 ) and calcium hydroxyapatite [Ca 5 (PO 4 ) 3 OH] precipitation, has been described in a wide variety of environments (Boquet et al. 1973;Schmittner and Giresse 1999;Belzer et al. 2006;Canaveras et al. 2006;Kremer et al. 2008). The formation of calcium hydroxyapatite has received considerable attention as a result of its importance in biological calcification. Calcium phosphates are the main constituent of teeth and bones and have been found in pathological mineral deposits in the form of urinary and kidney stones.The importance of microbially induced cementation has been widely recognized in petroleum, geological and civil engineering (Dejong et al. 2006;Ivanov and Chu 2008). There is a growing interest in methods to improve the mechanical properties of sandy soils using microbially induced biochemical reactions in the subsurface (Whiffin et al. 2007). These methods simulate natural diagenetic processes that transform loose sand to sandstone. It has been documented that cracks in rock formations, especially in oil reservoirs, could be remediated by microbial mineral precipitation (Jack 1991).Phytic acid salts or phytates (myo-inositol hexakisphosphates) are abundant plant constituents. They typically account for 60-90 % of total seed phosphorus. Phytate is a natural by-product of fermentation processes and a waste product in the fermentation industry.Phytases, a specific group of phosphatases, catalyze hydrolysis of the phosphate ester bonds of phytates (by the addition of water) (Cosgrove 1966;Mullaney et al. 2000). They have been found in various eukaryotic and prokaryotic microorganisms (Lassen et al. 2001;Lim et al. 2007). Extracellular phytases from several filamentous fungi and yeasts have been studied in detail. The dimorphic yeast A.a. can utilize phytate as a sole C and P source by secreting high level of phytase into its environment (Sano et al. 1999).This paper aims to explore the po...