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Since 1933, carbonic anhydrase research has focused on enzymes from mammals (␣ class) and plants (␤ class); however, two additional classes (␥ and ␦) were discovered recently. Cam, from the procaryote Methanosarcina thermophila, is the prototype of the ␥ class and the first carbonic anhydrase to be characterized from either an anaerobic organism or the Archaea domain. All of the enzymes characterized from the four classes have been purified aerobically and are reported to contain a catalytic zinc. Herein, we report the anaerobic reconstitution of apo- Research in the intervening years has shown that CA is one of the most widely distributed enzymes in nature (2, 3) and continues to be intensely investigated. Amino acid sequence comparisons identify four classes (␣, ␤, ␥, and ␦) of independent origins (4). Isozymes of the ␣ class are found in virtually all mammalian tissues where they function in diverse essential processes. The ␤ class is ubiquitous in plants and algae, where it is indispensable for the acquisition and concentration of CO 2 for photosynthesis. CA plays a role in the sequestration of atmospheric CO 2 in carbonates, and the global cycles of silicon and carbon are linked by CA in diatoms (5); thus, CA plays an important role in major geochemical and atmospheric processes. Members of the ␤ and ␥ classes are wide spread in physiologically diverse procaryotes from both the Bacteria and Archaea domains. Indeed, the genome of Escherichia coli contains two ␥ class homologs and two ␤ class homologs (2).Cam, from the procaryote Methanosarcina thermophila, is the prototype of the ␥ class and the first CA to be characterized from either an anaerobic organism or the Archaea domain (6). Sequence analyses approximate the evolution of the ␥ class at the estimated time of the origin of life (2). The crystal structure of Cam purified aerobically from E. coli reveals a homotrimer with a subunit fold composed of a left-handed ␤-helix motif followed by short and long ␣-helix structures (7). Each of the three active sites contain three histidines that coordinate a zinc ion. Two of the metal-binding histidines are donated by one monomer, and the third histidine from an adjacent monomer. Other residues in the active site of Cam are also donated from adjacent monomer faces and bear no resemblance to residues in the active site of the well characterized ␣ class CAs for which specific functions have been assigned.Kinetic investigations of the ␣ class CAs reveal a "zinc hydroxide" mechanism for catalysis (8) that also extends to both the ␤ and ␥ classes (9, 10). The overall enzyme-catalyzed reaction occurs in two mechanistically distinct steps,where E is enzyme, and B is buffer. The first step is the interconversion between CO 2 and bicarbonate (Equations 2 and 3) involving a nucleophilic attack of the zinc-bound hydroxyl on the CO 2 molecule. The second step is regeneration of the zinc-bound hydroxide, which involves intramolecular proton transfer from the zinc-bound water to a proton shuttle residue (Equation 4) and interm...

Four glutamate residues in the prototypic gamma-class carbonic anhydrase from Methanosarcina thermophila (Cam) were characterized by site-directed mutagenesis and chemical rescue studies. Alanine substitution indicated that an external loop residue, Glu 84, and an internal active site residue, Glu 62, are both important for CO(2) hydration activity. Two other external loop residues, Glu 88 and Glu 89, are less important for enzyme function. The two E84D and -H variants exhibited significant activity relative to wild-type activity in pH 7.5 MOPS buffer, suggesting that the original glutamate residue could be substituted with other ionizable residues with similar pK(a) values. The E84A, -C, -K, -Q, -S, and -Y variants exhibited large decreases in k(cat) values in pH 7.5 MOPS buffer, but only exhibited small changes in k(cat)/K(m). These same six variants were all chemically rescued by pH 7.5 imidazole buffer, with 23-46-fold increases in the apparent k(cat). These results are consistent with Glu 84 functioning as a proton shuttle residue. The E62D variant exhibited a 3-fold decrease in k(cat) and a 2-fold decrease in k(cat)/K(m) relative to those of the wild type in pH 7.5 MOPS buffer, while other substitutions (E62A, -C, -H, -Q, -T, and -Y) resulted in much larger decreases in both k(cat) and k(cat)/K(m). Imidazole did not significantly increase the k(cat) values and slightly decreased the k(cat)/K(m) values of most of the Glu 62 variants. These results indicate a primary preference for a carboxylate group at position 62, and support a proposed catalytic role for residue Glu 62 in the CO(2) hydration step, but do not definitively establish its role in the proton transport step.