A closer look at the active site of gamma-class carbonic anhydrases: high-resolution crystallographic studies of the carbonic anhydrase from Methanosarcina thermophila.

The prototype of the gamma-class of carbonic anhydrase has been characterized from the methanogenic archaeon Methanosarcina thermophila. Previously reported kinetic studies of the gamma-class carbonic anhydrase are consistent with this enzyme having a reaction mechanism similar to that of the mammalian alpha-class carbonic anhydrase. However, the overall folds of these two enzymes are dissimilar, and apart from the zinc-coordinating histidines, the active site residues bear little resemblance to one another. The crystal structures of zinc-containing and cobalt-substituted gamma-class carbonic anhydrases from M. thermophila are reported here between 1.46 and 1.95 A resolution in the unbound form and cocrystallized with either SO(4)(2)(-) or HCO(3)(-). Relative to the tetrahedral coordination geometry seen at the active site in the alpha-class of carbonic anhydrases, the active site of the gamma-class enzyme contains additional metal-bound water ligands, so the overall coordination geometry is trigonal bipyramidal for the zinc-containing enzyme and octahedral for the cobalt-substituted enzyme. Ligands bound to the active site all make contacts with the side chain of Glu 62 in manners that suggest the side chain is likely protonated. In the uncomplexed zinc-containing enzyme, the side chains of Glu 62 and Glu 84 appear to share a proton; additionally, Glu 84 exhibits multiple conformations. This suggests that Glu 84 may act as a proton shuttle, which is an important aspect of the reaction mechanism of alpha-class carbonic anhydrases. A hydrophobic pocket on the surface of the enzyme may participate in the trapping of CO(2) at the active site. On the basis of the coordination geometry at the active site, ligand binding modes, the behavior of the side chains of Glu 62 and Glu 84, and analogies to the well-characterized alpha-class of carbonic anhydrases, a more-defined reaction mechanism is proposed for the gamma-class of carbonic anhydrases.

Kinetic and spectroscopic characterization of the gamma-carbonic anhydrase from the methanoarchaeon Methanosarcina thermophila.

The zinc and cobalt forms of the prototypic gamma-carbonic anhydrase from Methanosarcina thermophila were characterized by extended X-ray absorption fine structure (EXAFS) and the kinetics were investigated using steady-state spectrophotometric and (18)O exchange equilibrium assays. EXAFS results indicate that cobalt isomorphously replaces zinc and that the metals coordinate three histidines and two or three water molecules. The efficiency of either Zn-Cam or Co-Cam for CO(2) hydration (k(cat)/K(m)) was severalfold greater than HCO(3-) dehydration at physiological pH values, a result consistent with the proposed physiological function for Cam during growth on acetate. For both Zn- and Co-Cam, the steady-state parameter k(cat) for CO(2) hydration was pH-dependent with a pK(a) of 6.5-6.8, whereas k(cat)/K(m) was dependent on two ionizations with pK(a) values of 6.7-6.9 and 8.2-8.4. The (18)O exchange assay also identified two ionizable groups in the pH profile of k(cat)/K(m) with apparent pK(a) values of 6.0 and 8.1. The steady-state parameter k(cat) (CO(2) hydration) is buffer-dependent in a saturable manner at pH 8. 2, and the kinetic analysis suggested a ping-pong mechanism in which buffer is the second substrate. The calculated rate constant for intermolecular proton transfer is 3 x 10(7) M(-1) s(-1). At saturating buffer concentrations and pH 8.5, k(cat) is 2.6-fold higher in H(2)O than in D(2)O, suggesting that an intramolecular proton transfer step is at least partially rate-determining. At high pH (pH > 8), k(cat)/K(m) is not dependent on buffer and no solvent hydrogen isotope effect was observed, consistent with a zinc hydroxide mechanism. Therefore, at high pH the catalytic mechanism of Cam appears to resemble that of human CAII, despite significant structural differences in the active sites of these two unrelated enzymes.

Characterization of heterologously produced carbonic anhydrase from Methanosarcina thermophila.

The gene encoding carbonic anhydrase from Methanosarcina thermophila was hyperexpressed in Escherichia coli, and the heterologously produced enzyme was purified 14-fold to apparent homogeneity. The enzyme purified from E. coli has properties (specific activity, inhibitor sensitivity, and thermostability) similar to those of the authentic enzyme isolated from M. thermophila; however, a discrepancy in molecular mass suggests that the carbonic anhydrase is posttranslationally modified in either E. coli or M. thermophila. Both the authentic and heterologously produced enzymes were stable to heating at 55 degrees C for 15 min but were inactivated at higher temperatures. No esterase activity was detected with p-nitrophenylacetate as the substrate. Plasma emission spectroscopy revealed approximately 0.6 Zn per subunit. As judged from the estimated native molecular mass, the enzyme is either a trimer or a tetramer. Western blot (immunoblot) analysis of cell extract proteins from M. thermophila indicates that the levels of carbonic anhydrase are regulated in response to the growth substrate, with protein levels higher in acetate than in methanol- or trimethylamine-grown cells.

A left-hand beta-helix revealed by the crystal structure of a carbonic anhydrase from the archaeon Methanosarcina thermophila.

A carbonic anhydrase from the thermophilic archaeon Methanosarcina thermophila that exhibits no significant sequence similarity to known carbonic anhydrases has recently been characterized. Here we present the structure of this enzyme, which adopts a left-handed parallel beta-helix fold. This fold is of particular interest since it contains only left-handed crossover connections between the parallel beta-strands, which so far have been observed very infrequently. The active form of the enzyme is a trimer with three zinc-containing active sites, each located at the interface between two monomers. While the arrangement of active site groups differs between this enzyme and the carbonic anhydrases from higher vertebrates, there are structural similarities in the zinc coordination environment, suggestive of convergent evolution dictated by the chemical requirements for catalysis of the same reaction. Based on sequence similarities, the structure of this enzyme is the prototype of a new class of carbonic anhydrases with representatives in all three phylogenetic domains of life.

A carbonic anhydrase from the archaeon Methanosarcina thermophila.

Carbonic anhydrase (CA) from acetate-grown Methanosarcina thermophila was purified > 10,000-fold (22% recovery) to apparent homogeneity with a specific activity of 4872 units/mg. The estimated native molecular mass of the enzyme is 84 kDa based on gel filtration chromatography. SDS/PAGE revealed one protein band with an apparent molecular mass of 40 kDa. The M. thermophila CA is less sensitive than human CA isozyme II toward inhibition by sulfonamides and monovalent ions. The gene encoding this CA was cloned into pUC18 and sequenced. Escherichia coli harboring the recombinant plasmid expresses CA activity (2.3 units/mg of cell extract protein). Comparison of the deduced amino acid sequence with the N-terminal sequence of the purified protein shows that the gene encodes an additional 34 N-terminal residues with properties characteristic of signal peptides in secretory proteins. The calculated molecular mass (22.9 kDa) and pI (4.0) suggest that SDS/PAGE overestimates the subunit size and that the native enzyme is a tetramer. To our knowledge, the deduced amino acid sequence has no significant identity to any known CA but has 35% sequence identity to the first 197 deduced N-terminal amino acids of a proposed CO2-concentrating-mechanism protein from Synechococcus PCC7942 and 28% sequence identity to the deduced sequence of ferripyochelin binding protein from Pseudomonas aeruginosa. Thus, our results indicate that this archaeal CA represents a distinct class of CAs and provide a basis to determine physiological roles for CA in acetotrophic anaerobes.