Profiles of dissolved O-2 and methane with increasing depth were generated
for Lake Washington sediment, which suggested the zone of methane oxidation
is limited to the top 0.8 cm of the sediment. Methane oxidation potentials
were measured for 0.5-cm layers down to 1.5 cm and found to be relatively
constant at 270 to 350 mu mol/liter of sediment/h, Approximately 65% of the
methane was oxidized to cell material or metabolites, a signature suggesti
ve of type I methanotrophs. Eleven methanotroph strains were isolated from
the lake sediment and analyzed. Five of these strains classed as type I, wh
ile six were classed as type II strains by 16S rRNA gene sequence analysis.
Southern hybridization analysis with oligonucleotide probes detected, on a
verage, one to two copies of pmoA and one to three copies of 16S rRNA genes
. Only one restriction length polymorphism pattern was shown for pmoA genes
in each isolate, and in cases where, sequencing was done, the pmoA copies
were found to be almost identical. PCR primers were developed for mmoX whic
h amplified 1.2-kb regions from all six strains that tested positive for cy
toplasmic soluble methane mono-oxygenase (sMMO) activity. Phylogenetic anal
ysis of the translated PCR products with published mmoX sequences showed th
at MmoX falls into two distinct clusters, one containing the orthologs from
type I strains and another containing the orthologs from type II strains.
The presence of sMMO-containing Methylomonas strains in a pristine freshwat
er lake environment suggests that these methanotrophs are more widespread t
han has been previously thought.