Fig. 5: Back flux under sulfate limitation or with variable starting butane concentrations.
From: Back flux during anaerobic oxidation of butane supports archaea-mediated alkanogenesis

A, D Temporal evolution of measured concentrations of butane (C4H10, circles) and sulfide (HS–, diamonds), along with trend lines fitted using the first-order dynamic model. Gray shades indicate measurements from low-sulfate incubations (5 mmol/L sulfate) with three different starting 13C-bicarbonate concentrations (A; 1.12%, 50%, and 98%), or from incubations with two different initial butane concentrations (D; 3 mmol l−1 vs. 6 mmol l−1). B, E Development of isotope compositions of butane (\({{{\rm{\delta }}}}^{13}{{{\rm{C}}}}_{{{{\rm{C}}}}_{4}{{{\rm{H}}}}_{10}}\)). Color shades represent the same incubation conditions as in A; Error bars in B, E, are standard deviations of technical replicates (n = 3). C, F Ratio of back flux relative to the net AOB rate (f−/fnet) and Gibbs free energy change of the overall AOB reaction (∆G) estimated from measured concentrations and/or isotope compositions. Black lines show calculated values for low-sulfate assays with 50% 13C-bicarbonate (C) and for low-butane assays (F). The f−/fnet and ∆G calculated for the assay with 6 mmol l−1 C4H10 98% 13C-bicarbonate, and 28 mmol l−1 sulfate are shown for comparison (grey lines in C, F). The shaded envelopes in (C, F) indicate the 95% confidence interval of estimated values. Source data are provided as a Source Data file.