We examined the potential use of natural-abundance stable carbon isotope ratios of lipids for determining substrate usage by sulfate-reducing bacteria (SRB). Four SRB were grown under autotrophic, mixotrophic, or heterotrophic growth conditions, and the ␦ 13 C values of their individual fatty acids (FA) were determined. The FA were usually 13 C depleted in relation to biomass, with ⌬␦ 13 C (FA ؊ biomass) of ؊4 to ؊17‰; the greatest depletion occurred during heterotrophic growth. The exception was Desulfotomaculum acetoxidans, for which substrate limitation resulted in biomass and FA becoming isotopically heavier than the acetate substrate. The Sulfate-reducing bacteria (SRB) are common and functionally important members of anaerobic microbial communities. SRB populations can be identified and quantified by using molecular and phylogenetic approaches (8,20,25). When combined with measurements of rates of biogeochemical cycling and with an understanding of the physiology of these microbes through isolation and pure-culture studies, these approaches can reveal much about the roles of SRB in a variety of habitats (5,19,23,33). Although the use of stable sulfur isotopes and sensitive measurements of sulfide production have addressed the role of SRB in sulfur transformations (9, 24), little is known about the direct effect of these organisms on carbon flow in microbial communities. It is generally well recognized that SRB are important in reprocessing organic matter and can degrade a wide variety of organic substrates. Several SRB can also grow autotrophically in the absence of organic compounds (4, 29, 38). Molecular genetic and physiological studies can indicate which SRB are present in an environment as well as their potential capabilities, but such studies do not determine which carbon transformations the SRB are actually carrying out in a particular environment. The use of stable-or radioisotope-labeled substrates can reveal flows and rates of transformations (2, 3, 26) but are limited in application, because their use might alter the natural abundance of key substrates and our ability to introduce these substrates into natural environments is limited. However, the study of stable isotopic compositions, at natural abundance, is a potential way to circumvent this problem and to determine the carbon substrates actually used by SRB.We had previously grown four different SRB and determined the isotope fractionation factors for biomass production during autotrophic, mixotrophic, and heterotrophic growth (17). In order to use stable carbon isotopes to assess the mode of growth of SRB in natural environments, we needed an analysis that was more specific than bulk biomass. SRB are typical bacteria in that their membranes are composed primarily of phospholipids with ester-bound fatty acids (PLFA) that can be analyzed as fatty acid methyl esters (FAME). Several genera of SRB possess PLFA with unusual structures that are useful as biomarkers (1, 32, 35), and we have for the first time determined the ␦ 13 C values of individ...