Cloning and sequencing of the gene encoding glutamine synthetase I from the archaeum Pyrococcus woesei: anomalous phylogenies inferred from analysis of archaeal and bacterial glutamine synthetase I sequences

Abstract

The gene glnA encoding glutamine synthetase I (GSI) from the archaeum Pyrococcus woesei was cloned and sequenced with the Sulfolobus solfataricus glnA gene as the probe. An operon reading frame of 448 amino acids was identified within a DNA segment of 1,528 bp. The encoded protein was 49% identical with the GSI of Methanococcus voltae and exhibited conserved regions characteristic of the GSI family. The P. woesei GSI was aligned with available homologs from other archaea (S. solfataricus, M. voltae) and with representative sequences from cyanobacteria, proteobacteria, and gram-positive bacteria. Phylogenetic trees were constructed from both the amino acid and the nucleotide sequence alignments. In accordance with the sequence similarities, archaeal and bacterial sequences did not segregate on a phylogeny. On the basis of sequence signatures, the GSI trees could be subdivided into two ensembles. One encompassed the GSI of cyanobacteria and proteobacteria, but also that of the high-G + C gram-positive bacterium Streptomyces coelicolor (all of which are regulated by the reversible adenylylation of the enzyme subunits); the other embraced the GSI of the three archaea as well as that of the low-G + C gram-positive bacteria (Clostridium acetobutilycum, Bacillus subtilis) and Thermotoga maritima (none of which are regulated by subunit adenylylation). The GSIs of the Thermotoga and the Bacillus-Clostridium lineages shared a direct common ancestor with that of P. woesei and the methanogens and were unrelated to their homologs from cyanobacteria, proteobacteria, and S. coelicolor. The possibility is presented that the GSI gene arose among the archaea and was then laterally transferred from some early methanogen to a Thermotoga-like organism. However, the relationship of the cyanobacterial-proteobacterial GSIs to the Thermotoga GSI and the GSI of low-G+C gram-positive bacteria remains unexplained.