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Biol. Bull. 204: 186-191. (April 2003)
© 2003 Marine Biological Laboratory

Genomic Markers of Ancient Anaerobic Microbial Pathways: Sulfate Reduction, Methanogenesis, and Methane Oxidation

Andreas Teske1,*,{ddagger}, Ashita Dhillon2 and Mitchell L. Sogin2

1 Biology Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543
2 Josephine Bay Paul Center for Comparative Molecular Biology and Evolution, Marine Biological Laboratory, Woods Hole, Massachusetts 02543

* To whom correspondence should be addressed. E-mail: teske{at}email. unc.edu

Genomic markers for anaerobic microbial processes in marine sediments—sulfate reduction, methanogenesis, and anaerobic methane oxidation—reveal the structure of sulfate-reducing, methanogenic, and methane-oxidizing microbial communities (including uncultured members); they allow inferences about the evolution of these ancient microbial pathways; and they open genomic windows into extreme microbial habitats, such as deep subsurface sediments and hydrothermal vents, that are analogs for the early Earth and for extraterrestrial microbiota.




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