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. 2019 Mar 20;13(8):1920–1932. doi: 10.1038/s41396-019-0387-y

Fig. 2.

Fig. 2

Quantitative PCR (qPCR) measurements of dsrB abundance in sediment, dsrB abundance as a fraction of 16S rRNA gene abundance, radiotracer measurements of sulfate reduction rates, and mean cellular sulfate reduction rates based on bulk radiotracer measurements divided by dsrB qPCR abundance. Lower limits of bioturbation are taken from the bioturbation study from the same expedition [37]