We may not be
totally sunk by this:
Although the atmospheric concentration of methane - the second most important trace-gas contributor to global warming next to CO2 - has more than doubled since pre-industrial times, its rate of increase has slowed considerably over the last few decades (Steele et al., 1992). Prinn et al. (1992) suggest that one of the major causes of the slowdown is the increasing magnitude of methane oxidation by methanotrophic bacteria in the aerobic zones of soils, the magnitude of which phenomenon is believed to be equivalent to the annual input of methane to the atmosphere (Watson et al., 1992). Hence, as Tamai et al. note, "this biological sink plays an important role in modulating global warming."
http://www.co2science.org/scripts/CO2ScienceB2C/articles/V6/N38/B2.jspNot to say that this mechanism will necessarily work fast enough. A sudden shot of large volumes of methane could very likely overwhelm this system. But there is some hope here that the impact will be lessened a bit.
(One could take a wild-ass-guess from the above chart that at abput 1992 the population of the bacteria caught up with rising methane levels, and the exponential-looking period from 92 through 2000 is influenced by a population growth curve in an ample supply environment, with the flat period being the point at which the methane "food supply" became a limit on the population.)
Of course, what happens when populations of these bacterium become large over the long term, biospheres adjust to their population size and come to rely on them in other capacities, and then methane concentrations fall precipitously as the supply "runs out" is another matter entirely.
Of course, we won't find many of these bacteria in desert "soil" which is another worry as deserts grow. The article says forests do this job the best.