We present a method for extraction of active methane (CH4)-oxidizing b
acteria from soil samples. The method is based on physical dispersion
of bacteria from the soil particles followed by separation of bacteria
and soil particles by floatation in the density media Nycodenz or Per
coll. Separation on Nycodenz produced very pure bacterial suspensions
while separation on Percoll produced rather impure suspensions. Howeve
r, more than 60% of the methane-oxidizing activity was irreversibly in
hibited in the procedure using Nycodenz compared to less than 10% irre
versible inhibition when Percoll was employed. The bacterial suspensio
ns extracted from soil can be used to study the physiology and ecology
of soil bacteria that oxidize methane at atmospheric concentrations.
Our data indicated that these bacteria are extremely difficult to disl
odge from particles compared to the majority of bacteria in soil. Tent
atively, we interpret the strong attachment to long residence time (i.
e. slow turnover) of the methane-oxidizing bacteria. A slow turnover/g
rowth rate would explain why soil disturbances, like cultivation, have
a long lasting effect on the oxidation of atmospheric methane in soil
.