WETLANDS, both natural and agricultural, contribute an estimated 40 to
50% of the total methane emitted to the atmosphere each year. Recent
efforts in atmospheric modelling1 and attempts to constrain CH4 source
strengths2 have indicated the need to delineate the processes respons
ible for the large variations in emission rates found within and acros
s wetland types. Numerous biogeochemical factors are known to affect t
he activity of methanogenic bacteria3,4 and although there has been so
me success in relating water level5-7 and temperature8,9 to CH4 emissi
ons within particular systems, these variables are insufficient for pr
edicting emissions across a variety of wetlands2,10. From simultaneous
measurements of CO2 and CH4 exchange in wetlands extending from subar
ctic peatlands to subtropical marshes, we report here a positive corre
lation between CH4 emission and net ecosystem production and suggest t
hat net ecosystem production is a master variable, integrating many fa
ctors which control CH4 emission in vegetated wetlands. We find that a
bout 3 per cent of the daily net ecosystem production is emitted back
to the atmosphere as CH4. With projected stimulation of primary produc
tion and soil microbial activity in wetlands associated with elevated
atmospheric CO2 concentrations11, we envisage the potential for increa
sing CH4 emissions from inundated wetlands, further enhancing the gree
nhouse effect.