广域古菌界                        
                
                                
                        
                            生物                        
                
                                
                        
                            古细菌                        
                
                                
                        
                            甲烷                        
                
                                
                        
                            门                        
                
                                
                        
                            微生物代谢                        
                
                                
                        
                            生态学                        
                
                                
                        
                            产甲烷                        
                
                                
                        
                            细菌                        
                
                                
                        
                            遗传学                        
                
                        
                    
            作者
            
                Paul N. Evans,Joel A. Boyd,Andy O Leu,Ben J. Woodcroft,Donovan H. Parks,Philip Hugenholtz,Gene W. Tyson            
         
                    
        
    
            
            标识
            
                                    DOI:10.1038/s41579-018-0136-7
                                    
                                
                                 
         
        
                
            摘要
            
            Methane is a key compound in the global carbon cycle that influences both nutrient cycling and the Earth's climate. A limited number of microorganisms control the flux of biologically generated methane, including methane-metabolizing archaea that either produce or consume methane. Methanogenic and methanotrophic archaea belonging to the phylum Euryarchaeota share a genetically similar, interrelated pathway for methane metabolism. The key enzyme in this pathway, the methyl-coenzyme M reductase (Mcr) complex, catalyses the last step in methanogenesis and the first step in methanotrophy. The discovery of mcr and divergent mcr-like genes in new euryarchaeotal lineages and novel archaeal phyla challenges long-held views of the evolutionary origin of this metabolism within the Euryarchaeota. Divergent mcr-like genes have recently been shown to oxidize short-chain alkanes, indicating that these complexes have evolved to metabolize substrates other than methane. In this Review, we examine the diversity, metabolism and evolutionary history of mcr-containing archaea in light of these recent discoveries.
         
            
 
                 
                
                    
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