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Applied and Environmental Microbiology, January 2009, p. 242-245, Vol. 75, No. 1
0099-2240/09/$08.00+0 doi:10.1128/AEM.01462-08
Copyright © 2009, American Society for Microbiology. All Rights Reserved.
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Department of Microbiology, University of Massachusetts, Amherst, Massachusetts,1 School of Oceanography, University of Washington, Seattle, Washington,2 Molecular and Cellular Biology Program, University of Massachusetts, Amherst, Massachusetts3
Received 30 June 2008/ Accepted 24 October 2008
The abundances of hyperthermophilic heterotrophs, methanogens, and autotrophic reducers of amorphous Fe(III) oxide in 18 samples of deep-sea hydrothermal vent sulfide chimneys of the Endeavour Segment were measured. The results indicate that conditions favor the growth of iron reducers toward the interiors of these deposits and that of heterotrophs toward the outer surfaces near high-temperature polychaete worms (Paralvinella sulfincola).
Published ahead of print on 31 October 2008.
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