Formation of Sphalerite (ZnS) Deposits in Natural Biofilms of Sulfate-Reducing Bacteria

Author:

Labrenz Matthias1,Druschel Gregory K.1,Thomsen-Ebert Tamara2,Gilbert Benjamin3,Welch Susan A.1,Kemner Kenneth M.4,Logan Graham A.5,Summons Roger E.5,Stasio Gelsomina De3,Bond Philip L.1,Lai Barry4,Kelly Shelly D.4,Banfield Jillian F.1

Affiliation:

1. Department of Geology and Geophysics, University of Wisconsin–Madison, 1215 West Dayton Street, Madison, WI 53706, USA.

2. Diversions Scuba, Madison, WI 53705, USA.

3. Department of Physics, University of Wisconsin–Madison, 1150 University Avenue, Madison, WI 53706, USA.

4. Argonne National Laboratory, Argonne, IL 60439, USA.

5. Australian Geological Survey Organisation, GPO Box 378, Canberra ACT 2601, Australia.

Abstract

Abundant, micrometer-scale, spherical aggregates of 2- to 5-nanometer-diameter sphalerite (ZnS) particles formed within natural biofilms dominated by relatively aerotolerant sulfate-reducing bacteria of the family Desulfobacteriaceae. The biofilm zinc concentration is about 10 6 times that of associated groundwater (0.09 to 1.1 parts per million zinc). Sphalerite also concentrates arsenic (0.01 weight %) and selenium (0.004 weight %). The almost monomineralic product results from buffering of sulfide concentrations at low values by sphalerite precipitation. These results show how microbes control metal concentrations in groundwater- and wetland-based remediation systems and suggest biological routes for formation of some low-temperature ZnS deposits.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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