Members of upland soil cluster alpha (USC␣) are assumed to be methanotrophic bacteria (MB) adapted to the trace level of atmospheric methane. So far, these MB have eluded all cultivation attempts. While the 16S rRNA phylogeny of USC␣ members is still not known, phylogenies constructed for the active-site polypeptide (encoded by pmoA) of particulate methane monooxygenase (pMMO) placed USC␣ next to the alphaproteobacterial Methylocapsa acidiphila B2. To assess whether the pmoA tree reflects the evolutionary identity of USC␣, a 42-kb genomic contig of a USC␣ representative was obtained from acidic forest soil by screening a metagenomic fosmid library of 250,000 clones using pmoA-targeted PCR. For comparison, a 101-kb genomic contig from M. acidiphila was analyzed, including the pmo operon. The following three lines of evidence confirmed a close phylogenetic relationship between USC␣ and M. acidiphila: (i) tetranucleotide frequency patterns of 5-kb genomic subfragments, (ii) annotation and comparative analysis of the genomic fragments against all completely sequenced genomes available in public domain databases, and (iii) three single gene phylogenies constructed using the deduced amino acid sequences of a putative prephenate dehydratase, a staphylococcallike nuclease, and a putative zinc metalloprotease. A comparative analysis of the pmo operons of USC␣ and M. acidiphila corroborated previous reports that both the pmo operon structure and the predicted secondary structure of deduced pMMO are highly conserved among all MB.The only biological sink for atmospheric CH 4 is its consumption in oxic soils (7,51). Recently, the global terrestrial sink was estimated at 29 Tg year Ϫ1 , with a wide range of uncertainty (7 to Ͼ100 Tg CH 4 year Ϫ1 ) (51). Atmospheric CH 4 is consumed in forest, agricultural, and other upland soils by aerobic methanotrophic bacteria (MB). The CH 4 -consuming activity of these MB is significant because the magnitude of atmospheric CH 4 uptake in oxic soils is similar to the estimated excess of emissions over sinks in recent years of 37 Tg year Ϫ1 (28). Moreover, methanotrophic activity is highly susceptible to disturbance by human activities (32, 51).Cultured MB are divided into two groups, namely, type I (further divided into types I and X) and type II. They differ in their phylogenetic affiliations (Gammaproteobacteria versus Alphaproteobacteria) and in diverse biochemical and ultrastructural characteristics (23). However, this traditional concept of methanotroph classification has become much more complex by recent descriptions of the genera Methylocella (9,12,17) and Methylocapsa (11). These acidophilic MB, although considered members of the type II MB, possess several unique morphological and physiological characteristics, and based on 16S rRNA phylogeny, Methylocella and Methylocapsa are more closely related to acidophilic heterotrophic bacteria of the genus Beijerinckia than to alphaproteobacterial type II MB of the Methylosinus/Methylocystis group.Methane monooxygenase (MMO) catalyzes the...