STRUCTURE, FUNCTION, AND EVOLUTION OF THE FAMILY OF SUPEROXIDE-DISMUTASE PROTEINS FROM HALOPHILIC ARCHAEBACTERIA

The protein sequences of seven members of the superoxide dismutase (SOD) family from halophilic archaebacteria have been aligned and compared with each other and with the homologous Mn and Fe SOD sequences from eubacteria and the methanogenic archaebacterium Methanobacterium thermoautotrophicum. Of 1'' common residues in the SOD proteins from halophilic archaebacteria, 125 are conserved in all seven sequences, and 64 of these are encoded by single unique triplets. The 74 remaining positions exhibit a high degree of variability, and for almost half of these, the encoding triplets are connected by at least two nonsynonymous nucleotide substitutions. The majority of nucleotide substitutions within the seven genes are nonsynonymous and result in amino acid replacement in the respective protein; silent third-codon-position (synonymous) substitutions are unexpectedly rare. Halophilic SODs contain 30 specific residues that are not found at the corresponding positions of the methanogenic or eubacterial SOD proteins. Seven of these are replacements of highly conserved amino acids in eubacterial SODs that are believed to play an important role in the three-dimensional structure of the protein. Residues implicated in formation of the active site, catalysis, and metal ion binding are conserved in all Mn and Fe SODs. Molecular phylogenies based on parsimony and neighbor-joining methods coherently group the halophile sequences but surprisingly fail to distinguish between the Mn SOD of Escherichia coli and the Fe SOD of M. thermoautotrophicum as the outgroup. These comparisons indicate that as a group, the SODs of halophilic archaebacteria have many unique and characteristic features. At the same time, the patterns of nucleotide substitution and amino acid replacement indicate that these genes and the proteins that they encode continue to be subject to strong and changing selection. This selection may be related to the presence of oxygen radicals and the inter- and intracellular composition and concentration of metal cations.