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Oxidation of aromatic contaminants coupled to microbial iron reduction

Nature volume 339, pages 297–300 (1989)Cite this article

Abstract

THE contamination of sub-surface water supplies with aromatic compounds is a significant environmental concern1,2. As these contaminated sub-surface environments are generally anaerobic, the microbial oxidation of aromatic compounds coupled to nitrate reduction, sulphate reduction and methane production has been studied intensively1–7. In addition, geochemical evidence suggests that Fe(III) can be an important electron acceptor for the oxidation of aromatic compounds in anaerobic groundwater. Until now, only abiological mechanisms for the oxidation of aromatic compounds with Fe(III) have been reported8–12. Here we show that in aquatic sediments, microbial activity is necessary for the oxidation of model aromatic compounds coupled to Fe(III) reduction. Furthermore, a pure culture of the Fe(III)-reducing bacterium GS-15 can obtain energy for growth by oxidizing benzoate, toluene, phenol or p-cresol with Fe(III) as the sole electron acceptor. These results extend the known physiological capabilities of Fe(III)-reducing organisms and provide the first example of an organism of any type which can oxidize an aromatic hydrocarbon anaerobically.

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Authors and Affiliations

  1. Water Resources Division, US Geological Survey, Reston, Virginia, 22092, USA

    Derek R. Lovley, Mary Jo Baedecker, Debra J. Lonergan, Isabella M. Cozzarelli & Elizabeth J. P. Phillips

  2. Department of Geology, Syracuse University, Syracuse, New York, 13244, USA

    Donald I. Siegel

Authors
  1. Derek R. Lovley
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  2. Mary Jo Baedecker
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  3. Debra J. Lonergan
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  4. Isabella M. Cozzarelli
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  5. Elizabeth J. P. Phillips
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  6. Donald I. Siegel
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Lovley, D., Baedecker, M., Lonergan, D. et al. Oxidation of aromatic contaminants coupled to microbial iron reduction. Nature 339, 297–300 (1989). https://doi.org/10.1038/339297a0

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