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. 1998 Mar;64(3):1143–1146. doi: 10.1128/aem.64.3.1143-1146.1998

FIG. 1.

FIG. 1

Oxidation of atmospheric methane by the St culture. At 0 h, laboratory air replaced the 17% CH4 and 1.7% CO2 growth condition. Single pulses of methanol were added after 20.1 h (833 μM final concentration) and after 139.3 h (83.3 μM final concentration), as indicated by the arrows. Note the logarithmic vertical axis.