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American Mineralogist; August-September 2007; v. 92; no. 8-9; p. 1411-1419; DOI: 10.2138/am.2007.2498
© 2007 Mineralogical Society of America
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Microbial reduction of structural Fe3+ in nontronite by a thermophilic bacterium and its role in promoting the smectite to illite reaction

Gengxin Zhang1, Hailiang Dong1,*, Jinwook Kim2 and D.D. Eberl3

1 Department of Geology, Miami University, Oxford, Ohio 45056, U.S.A.
2 Naval Research Laboratory, Seafloor Sciences Branch, Stennis Space Center, Mississippi 39529, U.S.A.
3 U.S. Geological Survey, Boulder, Colorado 80303, U.S.A.

Correspondence: * E-mail: dongh{at}muohio.edu

The illitization process of Fe-rich smectite (nontronite NAu-2) promoted by microbial reduction of structural Fe3+ was investigated by using a thermophilic metal-reducing bacterium, Thermoanaerobacter ethanolicus, isolated from the deep subsurface. T. ethanolicus was incubated with lactate as the sole electron donor and structural Fe3+ in nontronite as the sole electron acceptor, and anthraquinone-2, 6-disulfonate (AQDS) as an electron shuttle in a growth medium (pH 6.2 and 9.2, 65 °C) with or without an external supply of Al and K sources. With an external supply of Al and K, the extent of reduction of Fe3+ in NAu-2 was 43.7 and 40.4% at pH 6.2 and 9.2, respectively. X-ray diffraction and scanning and transmission electron microscopy revealed formation of discrete illite at pH 9.2 with external Al and K sources, while mixed layers of illite/smectite or highly charged smectite were detected under other conditions. The morphology of biogenic illite evolved from lath and flake to pseudo-hexagonal shape. An external supply of Al and K under alkaline conditions enhances the smectite-illite reaction during microbial Fe3+ reduction of smectite. Biogenic SiO2 was observed as a result of bioreduction under all conditions. The microbially promoted smectite-illite reaction proceeds via dissolution of smectite and precipitation of illite. Thermophilic iron reducing bacteria have a significant role in promoting the smectite to illite reaction under conditions common in sedimentary basins.

Key Words: Dissolution • illite • microbial Fe3+ reduction • nontronite • precipitation • sedimentary basin • smectite • Thermoanaerobacter ethanolicus




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