“…For example, the following conversions by microorganisms have been reported: selenate, selinite, tellurate, and tellurite to elemental forms; vanadate to a vanadyl compound; molybdate and molybdenum trioxide to a molybdenum blue compound; arsenate to arsenite; mercuric chloride to elemental mercury; chromate ions to chromic ions that are precipitates at neutral pH; pentavalent and trivalent bismuth to an elemental form; lead dioxide to its divalent state; osmium tetroxide to the osmate ion; osmium dioxide and trivalent osmium to the metal; and hexavalent uranium to the tetravalent state; hexavalent Pu to the tetravalent form, petavalent neptunium to the tetravalent form, and heptavalent technetium to tetravalent form (Mohagheghi, Updegraff, & Goldhaber, 1985;Lovley, 1993;Woolfolk & Whitely, 1962;Kauffman, Laughlin, & Baldwin, 1986;Francis, Dodge, Gillow, & Cline, 1991a;Francis, Dodge, & Gillow, 1991b;Francis, Dodge, Lu, Halada, & Clayton, 1994;Francis, Dodge, & Gillow, 2008;Neu, Icopini, & Boukhalfa, 2005;Deo, Rittmann, & Reed, 2011). The reduction of an element from a higher to a lower oxidation state or to elemental form affects its solubility, so resulting in the precipitation of several metals.…”