In the Amazon floodplain large areas of unvegetatedlake sediments are exposed to air during low water. Imeasured methane fluxes from exposed sediments of anAmazonian floodplain lake and assessed the regulatingfactors. Methane emission decreased from values between 10 and 40 mol CH₄ m^{minus 2} h^{minus 1}to zero when the sediments were exposed to air. Meanfluxes were about 3.7 mol CH₄m^{minus 2} h^{minus 1}. Fluxes were low compared tomeasurements taken from flooded habitats makingexposed lake sediments a negligible source ofatmospheric CH₄. This was mainly due to the lackof ebullition which governs methane flux in theflooded phase. Methane oxidation at the sedimentsurface consumed up to 75% of the methane enteringthe oxidised zone. Compared with CO₂ emissionmethane turnover was of minor importance for the carbon budget of the sediments.