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Bacteria play key roles in the carbon cycle. In many sediments and peatlands, methanotrophic bacteria consume a portion of released methane, reducing the emissions of this potent greenhouse gas. In marine oxygen minimum zones (OMZ) and other anoxic settings, anaerobic ammonium oxidizing (anammox) bacteria remove bioavailable nitrogen while performing chemoautotrophic carbon fixation. Methanotrophic and anammox bacteria synthesize a wide number of complex bacteriohopanepolyols (BHPs), comprising notably several stereoisomers of bacteriohopanetetrols (BHT), which are used as biomarker lipids. While BHT-17β(H), 21β(H), 22R, 32R, 33R, 34S (BHT-34S) is ubiquitous in the environment, its 34R stereoisomer (BHT-17β(H), 21β(H), 22R, 32R, 33R, 34R; BHT-34R) has only five known producers: the freshwater anammox genera ‘Candidatus Brocadia’, the aerobic acidic peatland methanotroph Methylocella palustris, the nitrogen-fixing aerobic bacteria Frankia spp., and the aerobic acetic acid-producing bacteria Acetobacter pasteurianus and Komagataeibacter xylinus. BHT-x—another BHT isomer of unknown stereochemistry—has only one known producer, the marine anammox bacteria ‘Candidatus Scalindua’ (Schwartz-Narbonne et al., 2020). The occurrence and extent of these different carbon cycle processes can be assessed by measuring the concentrations of these BHT stereoisomers and changes in their δ13C values (Hemingway et al., 2018; Lengger et al., 2019).However, the 13C fractionation associated with the different carbon assimilation pathways of these bacteria has been minimally assessed, resulting in poorly constrained ranges in δ13C values and difficulty in interpreting isotope results.We used a gas chromatography-combustion-isotope ratio mass spectrometry (GC-C-IRMS) method to measure the δ13C of BHT-34S, BHT34R, and BHT-x of cultured bacteria (‘Ca. Scalindua’, ‘Ca. Brocadia’, Methylocella tundrae, Frankia spp., and Komagataeibacter xylinus). These δ13C values were combined with bulk isotopic measurements of the bacterial biomass and δ13C analyses of the bacterial growth substrates to establish carbon isotopic fractionation from substrate to biomass to BHT lipid. We demonstrated that bacteria using different metabolic pathways produced distinct fractionation factors between substrate and BHTs, which potentially allows for distinguishing BHT-34R produced by ‘Ca. Brocadia’ and methanotrophs from other freshwater producers (e.g. in peatlands). Measurement of BHT-specific fractionation factors allowed us to better constrain the contribution of anammox bacteria to fixed carbon in OMZ. This work expands the application of BHT isomers to isotopically identify carbon cycle processes. ReferencesHemingway, Jordon D., et al. "A novel method to measure the 13C composition of intact bacteriohopanepolyols." Organic Geochemistry 123 (2018): 144-147.Lengger, Sabine K., et al. "Dark carbon fixation in the Arabian Sea oxygen minimum zone contributes to sedimentary organic carbon (SOM)." Global Biogeochemical Cycles 33.12 (2019): 1715-1732.Schwartz-Narbonne, Rachel, et al. "A unique bacteriohopanetetrol stereoisomer of marine anammox." Organic Geochemistry (2020): 103994. |