Fig. 2: Methane consumption and resulting stable isotope fractionation in incubated canal waters. | Nature Communications

Fig. 2: Methane consumption and resulting stable isotope fractionation in incubated canal waters.

From: Fate of methane in canals draining tropical peatlands

Fig. 2

A Across incubated waters, δ13C-CH4 increased as the percent of initial CH4 consumed increased. Each data point shows the mean change over ~50 hours of incubation ± standard error of replicates (Table S1). B Histogram of αox values calculated from incubation data. Source data are provided as a Source Data file.

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