(3,26,34,49,53,56). It has also been observed to occur in diverse ecosystems including activated sewage sludge (37), anoxic aquifer sediments (6,24,26,48), and marine sediments (45). Solid-phase Fe(II) species [including sorbed Fe(II) as well as Fe(II) sulfides, carbonates, and phosphates] often represent a large fraction of Fe(II) in anoxic aquifers (12). Both dissolved and solid forms of Fe(II) are known to be susceptible to anaerobic oxidation (27,33,45,61), with different biogenic Fe(III) (hydr)oxide mineral phases (including goethite, lepidocrocite, ferrihydrite, magnetite, and green rust) produced under similar physical and chemical conditions (11,33,34,48,54). The reason for the previously observed mineralogical differences in biogenic Fe(III) (hydr)oxide phases is unclear, but the chemical form of Fe(II) and the Fe(II) oxidation rate appear to exert control on the mineralogy for abiotically produced Fe(III) (hydr)oxides (19,60).The crystallinity of Fe(III) (hydr)oxide mineral phases strongly influences their susceptibility to microbiological reduction as well as their ability to act as a chemical oxidant (22,28,29,35,44,62). For instance, the poorly crystalline Fe(III) (hydr)oxide ferrihydrite is biologically reduced to a greater extent than the crystalline (and more thermodynamically stable) hematite (29,35,62). Therefore, the mineralogy of Fe(III) (hydr)oxide products of nitrate-dependent Fe(II) oxidation may have a profound impact on the cycling of Fe in anoxic environments.Here, we report on the characterization of a Klebsiella species (designated strain FW33AN) from a nitrate-and radionuclide-contaminated aquifer that is capable of anaerobic, nitrate-dependent Fe(II) oxidation. Strain FW33AN was previously shown to produce goethite by nitrate-dependent Fe(II) oxidation (48), and we show here that the chemical form of Fe(II) substrate and the rate of Fe(II) oxidation influence the mineralogy of biogenic Fe(III) (hydr)oxide products.
MATERIALS AND METHODSIsolation of strain FW33AN from FRC groundwater. During push-pull tests to stimulate nitrate and U(VI) reduction at the Oak Ridge Field Research Center (FRC) in Oak Ridge, TN (30), biomass that had accumulated in injection well FW033 was collected, refrigerated, and shipped to the University of Oklahoma where it was stored at 4°C for less than one week. A 4-(2-hydroxyethyl)-1-piperazineethanesulfonic acid (HEPES)-buffered (50 mM, pH 7) solid medium was used that contained 0.8 g/liter NaCl, 1 g/liter NH 4 Cl, 0.1 g/liter KCl, 0.03 g/liter KH 2 PO 4 , 0.2 g/liter MgSO 4 · 7H 2 O, and 0.04 g/liter CaCl 2 · 2H 2 O, vitamins, and trace metals (57). Acetate (30 mM CH 3 COONa) was provided as an electron donor, nitrate (20 mM NaNO 3 ) was the sole terminal electron acceptor, and agar (20 g/liter) was used as a solidifying agent. Plates were prepared under oxic conditions before transfer to an anoxic glovebag (Coy Laboratory Products, Grass Lake, MI) where they equilibrated overnight. Biomass-containing groundwater samples were serially diluted and spread on...