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Recent advances in the application of molecular genetic approaches have emphasized our potentially huge underestimate of microbial diversity in a range of natural environments 1 . These approaches, however, give no direct information about the biogeochemical processes in which microorganisms are active 2 . Here we describe an approach to directly link specific environmental microbial processes with the organisms involved, based on the stable-carbon-isotope labelling of individual lipid biomarkers. We demonstrate this approach in aquatic sediments and provide evidence for the identity of the bacteria involved in two important biogeochemical processes: sulphate reduction coupled to acetate oxidation in estuarine and brackish sediments 3 , 4 , and methane oxidation in a freshwater sediment 5 . Our results suggest that acetate added in a 13C-labelled form was predominantly consumed by sulphate-reducing bacteria similar to the Gram-positive Desulfotomaculum acetoxidans and not by a population of the more widely studied Gram-negative Desulfobacter spp. Furthermore, 13C-methane labelling experiments suggest that type I methanotrophic bacteria dominate methane oxidation at the freshwater site.
Nature – Springer Journals
Published: Apr 23, 1998
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