The necessary condition of mineral genesis Ц is rather high level of geo chemical accumulation by bacterial communities from the water not only the more important for life chemical elements (C, H, N, S, P and Cl) and necessary for life components: ions Na, K, Ca, Mg, transition ((Fe, Cr, Ni, Cu, Zn at al.) and precious metals, lantanoids in biochemical classifications, also referred to biophily elements. Cooperative interaction of various types and groups microorganisms, making local oxidizing and alkaline geochemical barriers provides selective character of chemical elements bioaccumulation processes from water medium. Normally, high content starting level of micro-components in waters of alkaline mineral sources, soda and salt lakes quite meets the need of bacteria in the transition metals. In case of latter deficit in water, the resource of these elements are the enriched by them the rests of water and ground vegetation, decomposed and oxidized by bacteria-destructors (saprophytes and cellulitics).