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. 2000 Jul;66(7):2888–2897. doi: 10.1128/aem.66.7.2888-2897.2000

FIG. 3.

FIG. 3

Vertical profiles of organic matter mineralization rates in Black Sea sediments from station I (top) to station IV (bottom). Circles, ΣCO2 production; squares, NH4+ accumulation; diamonds, sulfate reduction. Error bars indicate standard errors from linear regressions (ΣCO2 and NH4+) and standard deviations of triplicate sulfate reduction rates. Note different scales for different processes. At each station, the three scales are plotted at the ratio 11.2:1:5.6 for ΣCO2 production/NH4+ accumulation/sulfate reduction, corresponding to the inferred stoichiometric ratio of these processes during sulfate reduction (see text for details).