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Appl Environ Microbiol, April 1998, p. 1504-1509, Vol. 64, No. 4
0099-2240/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
Recovery of Humic-Reducing Bacteria from a
Diversity of Environments
John D.
Coates,1,*
Debra J.
Ellis,2,
Elizabeth L.
Blunt-Harris,2
Catherine V.
Gaw,2
Eric E.
Roden,3 and
Derek R.
Lovley2
Department of Microbiology, Southern Illinois
University, Carbondale, Illinois 629011;
Department of Microbiology, University of Massachusetts,
Amherst, Massachusetts 010032; and
Department of Biological Sciences, University of Alabama,
Tuscaloosa, Alabama 35487-02063
Received 23 September 1997/Accepted 28 January 1998
To evaluate which microorganisms might be responsible for microbial
reduction of humic substances in sedimentary environments, humic-reducing bacteria were isolated from a variety of sediment types.
These included lake sediments, pristine and contaminated wetland
sediments, and marine sediments. In each of the sediment types, all of
the humic reducers recovered with acetate as the electron donor and the
humic substance analog, 2,6-anthraquinone disulfonate (AQDS), as the
electron acceptor were members of the family
Geobacteraceae. This was true whether the AQDS-reducing bacteria were enriched prior to isolation on solid media or were recovered from the highest positive dilutions of sediments in liquid
media. All of the isolates tested not only conserved energy to support
growth from acetate oxidation coupled to AQDS reduction but also could
oxidize acetate with highly purified soil humic acids as the sole
electron acceptor. All of the isolates tested were also able to grow
with Fe(III) serving as the sole electron acceptor. This is consistent
with previous studies that have suggested that the capacity for Fe(III)
reduction is a common feature of all members of the
Geobacteraceae. These studies demonstrate that the
potential for microbial humic substance reduction can be found in a
wide variety of sediment types and suggest that
Geobacteraceae species might be important humic-reducing
organisms in sediments.
*
Corresponding author. Mailing address: Department of
Microbiology, Southern Illinois University, Carbondale, IL 62901. Phone: (618) 453-6132. Fax: (618) 453-8036. E-mail:
jcoates{at}micro.siu.edu.

Present address: American Type Culture Collection, Rockville, MD
20852.
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