“…However, if we assume that Al and Fe concentrations in these reactors equaled the detection limits of the method (0.1 and 0.9 lmol/L, respectively), then we estimate that abundances of Al-F and Fe-F complexes in the biotic reactors exceeded those in the control reactors by $3 to 5 and 1-2 orders of magnitude, respectively. Formation of Al-F and Fe-F complexes can enhance the solubility and dissolution rate of Al-and Fe-bearing minerals by lowering the activities of Al and Fe in solution (Pulfer et al, 1984;Ž utić and Stumm, 1984;Plankey et al, 1986;Haidouti, 1995;Phillips et al, 1997;Kraemer et al, 1998;Nordin et al, 1999;Harouiya and Oelkers, 2004;Wolff-Boenisch et al, 2004;Petrunic and Al, 2005). Our experiments therefore point to a potentially important bioweathering mechanism where actively metabolizing heterotrophic bacteria increase Al, and to a lesser extent, Fe release from granite by first accelerating the dissolution of co-existing, F-bearing trace phases.…”