Methane-utilizing bacteria (methanotrophs) are a diverse group of gram
-negative bacteria that are related to other members of the Proteobact
eria. These bacteria are classified into three groups based on the pat
hways used for assimilation of formaldehyde, the major source of cell
carbon, and other physiological and morphological features. The type I
and type X methanotrophs are found within the gamma subdivision of th
e Proteobacteria and employ tile ribulose monophosphate pathway for fo
rmaldehyde assimilation, whereas type II methanotrophs, which employ t
he serine pathway for formaldehyde assimilation, form a coherent clust
er within the beta subdivision of the Proteobacteria. Methanotrophic b
acteria are ubiquitous. The growth of type II bacteria appears to be f
avored in environments that contain relatively high levels of methane,
low levels of dissolved oxygen, and limiting concentrations of combin
ed nitrogen and/or copper. Type I methanotrophs appear to be dominant
in environments in which methane is limiting and combined nitrogen and
copper levels are relatively high. These bacteria serve as biofilters
for the oxidation of methane produced in anaerobic environments, and
when oxygen is present in soils, atmospheric methane is oxidized. Thei
r activities in nature are greatly influenced by agricultural practice
s and other human activities. Recent evidence indicates that naturally
occurring uncultured methanotrophs represent new genera. Methanotroph
s that are capable of oxidizing methane at atmospheric levels exhibit
methane oxidation kinetics different from those of methanotrophs avail
able in pure cultures. A limited number of methanotrophs have the gene
tic capacity to synthesize a soluble methane monooxygenase which catal
yzes the rapid oxidation of environmental pollutants including trichlo
roethylene.