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. 2021 May 25;15(11):3339–3356. doi: 10.1038/s41396-021-01001-0

Fig. 4. Biogeochemical activity measurements of photosynthetic and hydrogenotrophic processes in biocrusts and topsoils collected along the aridity gradient.

Fig. 4

a Rates of H2 oxidation under dry and wet conditions based on gas chromatography. Six biologically independent biocrust and topsoil samples were incubated per climatic zone. b Rates of carbon fixation in wet biocrust and topsoil samples based on tracing 14C-labelled CO2 incorporation. Three processes are shown: dark carbon assimilation (i.e., basal rate of CO2 incorporation under dark ambient conditions due to carbon fixation or anaplerotic processes); photosynthetic carbon fixation (i.e., amount of additional CO2 fixed under light ambient conditions); and hydrogenotrophic CO2 fixation (amount of additional CO2 fixed under dark H2-enriched conditions). For both biocrusts and topsoils, six biologically independent samples were pooled for each climatic zone and experiments were performed in technical triplicates. For both panels, rates are normalized to 16S rRNA gene copy number as a proxy for biomass (unadjusted rates shown in Fig. S9). Boxplots show median, upper and lower quartile, and minimum and maximum values.