Methane is a major greenhouse gas linked to global warming; however, patterns of in situ methane oxidation by methaneoxidizing bacteria (methanotrophs), nature's main biological mechanism for methane suppression, are often inconsistent with laboratory predictions. For example, one would expect a strong relationship between methanotroph ecology and Cu level because methanotrophs require Cu to sustain particulate methane monooxygenase (pMMO), the most efficient enzyme for methane oxidation. However, no correlation has been observed in nature, which is surprising because methane monooxygenase (MMO) gene expression has been unequivocally linked to Cu availability. Here we provide a fundamental explanation for this lack of correlation. We propose that MMO expression in nature is largely controlled by solid-phase Cu geochemistry and the relative ability of Cu acquisition systems in methanotrophs, such as methanobactins (mb), to obtain Cu from mineral sources. To test this hypothesis, RT-PCR expression assays were developed for Methylosinus trichosporium OB3b (which produces mb) to quantify pMMO, soluble MMO (the alternate MMO expressed when Cu is ''unavailable''), and 16S-rRNA gene expression under progressively more stringent Cu supply conditions. When Cu was provided as CuCl2, pMMO transcript levels increased significantly consistent with laboratory work. However, when Cu was provided as Cu-doped iron oxide, pMMO transcript levels increased only when mb was also present. Finally, when Cu was provided as Cu-doped borosilicate glass, pMMO transcription patterns varied depending on the ambient mb:Cu supply ratio. Cu geochemistry clearly influences MMO expression in terrestrial systems, and, as such, local Cu mineralogy might provide an explanation for methane oxidation patterns in the natural environment.methanotroph ͉ bioweathering ͉ methane oxidation ͉ particulate methane monooxygenase ͉ real-time RT-PCR M ethane-oxidizing bacteria (methanotrophs) are nature's primary biological mechanism for reducing levels of atmospheric methane, the second most important greenhouse gas associated with global warming (1). However, habitat factors that influence methanotroph ecology and, implicitly, in situ methane oxidation rates are poorly understood despite extensive recent studies (2-5). Moisture content, pH, and oxygen, methane, and nitrogen levels have all been studied and conditionally shown to influence methanotrophic activity, but none of these factors provides a consistent explanation for the distribution of methane-oxidizing organisms in nature. Interestingly, copper (Cu), which is central to metabolism in methanotrophic bacteria (2), has not been studied in detail in situ, which is very surprising because Cu is an essential component of particulate methane monooxygenase (pMMO), the most efficient enzyme at methane catalysis. Furthermore, Cu regulates methane monooxygenase (MMO) expression in methanotrophs that express both pMMO and soluble MMO (sMMO; the alternate methane-oxidation enzyme in many organisms), and also aff...