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Formation of Sphalerite (ZnS) Deposits in Natural Biofilms of Sulfate-Reducing Bacteria
Matthias Labrenz,1Gregory K. Druschel,1Tamara Thomsen-Ebert,2Benjamin Gilbert,3Susan A. Welch,1Kenneth M. Kemner,4Graham A. Logan,5Roger E. Summons,5Gelsomina De Stasio,3Philip L. Bond,1Barry Lai,4Shelly D. Kelly,4Jillian F. Banfield1*
Abundant, micrometer-scale, spherical aggregates of 2- to 5-nanometer-diameter sphalerite (ZnS) particles formed within
naturalbiofilms dominated by relatively aerotolerant sulfate-reducingbacteria of the family Desulfobacteriaceae. The biofilm zinc
concentrationis about 106 times that of associated
groundwater (0.09 to 1.1 parts per millionzinc). Sphalerite also
concentrates arsenic (0.01 weight %) andselenium (0.004 weight %).
The almost monomineralic product resultsfrom buffering of sulfide
concentrations at low values by sphaleriteprecipitation. These results
show how microbes control metal concentrationsin groundwater- and
wetland-based remediation systems and suggestbiological routes for
formation of some low-temperature ZnS deposits.
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.
*
To whom correspondence should be addressed. E-mail:
jill{at}geology.wisc.edu
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[DOI: 10.1126/science.290.5497.1711] |Summary »|Full Text »
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