Affiliation:
1. Departments of Microbiology1 and
2. Chemical Engineering,2 University of Washington, Seattle, Washington 98195
Abstract
ABSTRACT
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 μmol/liter of sediment/h. Approximately 65% of the methane was oxidized to cell material or metabolites, a signature suggestive of type I methanotrophs. Eleven methanotroph strains were isolated from the lake sediment and analyzed. Five of these strains classed as type I, while six were classed as type II strains by 16S rRNA gene sequence analysis. Southern hybridization analysis with oligonucleotide probes detected, on average, 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
which amplified 1.2-kb regions from all six strains that tested positive for cytoplasmic soluble methane mono-oxygenase (sMMO) activity. Phylogenetic analysis of the translated PCR products with published
mmoX
sequences showed that 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 freshwater lake environment suggests that these methanotrophs are more widespread than has been previously thought.
Publisher
American Society for Microbiology
Subject
Ecology,Applied Microbiology and Biotechnology,Food Science,Biotechnology
Cited by
197 articles.
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