Structural and functional characterization of a putative carbonic anhydrase from Geobacillus kaustophilus reveals its cambialistic function.

Carbonic anhydrases (CA) are the most ubiquitous ancient zinc metalloenzymes known. Here we report the structural and functional analysis of a hypothetical protein GK2848 from Geobacillus kaustophilus. The analysis revealed that it belongs to the γ-class of CA (termed as Cag). Only a limited number of γ-class CA's have been characterized till date. Interestingly Cag contains magnesium at its active site instead of a traditional zinc ion. Based on the structural and sequence comparison with similar γ-CA's the putative active site residues of Cag were identified. This analysis revealed that an important catalytic residue and a proton shuttle residue (Glu62 and Glu84 respectively) of Cam (previously characterized γ-CA from Methanosarcina thermophila) are absent in Cag, however certain other active site residues are conserved both in Cag and Cam. This suggests that Cag uses a different set of residues for the reversible hydration of CO to HCO when compared with Cam. Inductively Coupled Plasma - Optical Emission Spectrometry (ICP-OES) and Mg and Zn NMR studies on Cag and its mutants revealed that either Mg or Zn can occupy the active site which suggests the cambialistic nature of the enzyme.