Abstract
Sources and sinks of methane were studied in the Mayombe forest, a tropical evergreen forest located in a mountainous region in central Africa. Important methane emissions, reaching 6×1013 molecules/cm2/s, were measured in flooded lowlands where soil characteristics: pH and redox potential, favor the growth of methanogenic bacteria. However, basically, soils of this region constitute a sink of atmospheric methane with uptake rates ranging from 1010 to 1011 molecules/cm2/s. Methane emission from termite nests was also studied; it appeared to be a minor component of the methane budget. CH4 concentrations were measured inside the forest and in the surrounding atmosphere, CO2 being used as a qualitative tracer of air exchanges. In spite of intense but scattered and size‐limited sources this environment seems to be a net sink of atmospheric methane.
Published Version
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