Beneath the surface: Evolution of methane activity in the bacterial multicomponent monooxygenases.

The bacterial multicomponent monooxygenase (BMM) family has evolved to oxidise a wide array of hydrocarbon substrates of importance to environmental emissions and biotechnology: foremost amongst these is methane, which requires among the most powerful oxidant in biology to activate. To understand how the BMM evolved methane oxidation activity, we investigated the changes in the enzyme family at different levels: operonic, phylogenetic analysis of the catalytic hydroxylase, subunit or folding factor presence, and sequence-function analysis across the entirety of the BMM phylogeny. Our results show that the BMM evolution of new activities was enabled by incremental increases in oxidative power of the active site, and these occur in multiple branches of the hydroxylase phylogenetic tree. While the hydroxylase primary sequence changes that resulted in increased oxidative power of the enzyme appear to be minor, the principle evolutionary advances enabling methane activity occurred in the other components of the BMM complex and in the recruitment of stability proteins. We propose that enzyme assembly and stabilization factors have independently-evolved multiple times in the BMM family to support enzymes that oxidise increasingly difficult substrates. Herein, we show an important example of evolution of catalytic function where modifications to the active site and substrate accessibility, which are the usual focus of enzyme evolution, are overshadowed by broader scale changes to structural stabilization and non-catalytic unit development. Retracing macroscale changes during enzyme evolution, as demonstrated here, should find ready application to other enzyme systems and in protein design.

Horizontal gene transfer of three co-inherited methane monooxygenase systems gave rise to methanotrophy in the Proteobacteria.

The critical role that bacterial methanotrophs have in regulating the environmental concentrations of the potent greenhouse gas, methane, under aerobic conditions is dependent on monooxygenase enzymes which oxidise the substrate as both a carbon and energy source. Despite the importance of these organisms, the evolutionary origins of aerobic methane oxidation capability and its relationship to proteobacterial evolution is not well understood. Here we investigated the phylogenetic relationship of proteobacterial methanotrophs with related, non-methanotrophic bacteria using 16S rRNA and the evolution of two forms of methane monooxygenase: membrane bound (pMMO and pXMO) and cytoplasmic (sMMO). Through analysis we have concluded that extant proteobacterial methanotrophs evolved from up to five ancestral species, and that all three methane monooxygenase systems, pMMO, pXMO and sMMO, were likely present in the ancestral species (although pXMO and sMMO are not present in most of the present day methanotrophs). Here we propose that the three monooxygenase systems entered the ancestral species by horizontal gene transfer, with these likely to have pre-existing physiological and metabolic attributes that supported conversion to methanotrophy. Further, we suggest that prior to these enzyme systems developing methane oxidation capabilities, the membrane-bound and cytoplasmic monooxygenases were already both functionally and phylogenetically associated. These results not only suggest that sMMO and pXMO have a far greater role in methanotrophic evolution than previously understood but also implies that the co-inheritance of membrane bound and cytoplasmic monooxygenases have roles additional to that of supporting methanotrophy.