Marcus rate theory applied to enzymatic proton transfer

The hydration of CO(2) and the dehydration of HCO(3)(-) catalyzed by the carbonic anhydrases is accompanied by the transfer of protons between solution and the zinc-bound water molecule in the active site. This transfer is facilitated by amino acid residues of the enzyme which act as intramolecular proton shuttles; variants of carbonic anhydrase lacking such shuttle residues are enhanced or rescued in catalysis by intermolecular proton transfer from donors such as imidazole in solution. The resulting rate constants for proton transfer when compared with the values of the pK(a) of the donor and acceptor give Bronsted plots of high curvature. These data are described by Marcus theory which shows an intrinsic barrier for proton transfer from 1 to 2 kcal/mol and work terms or thermodynamic contributions to the free energy of reaction from 4 to10 kcal/mol. The interpretation of these Marcus parameters is discussed in terms of the well-studied pathway of the catalysis and structure of the enzymes.     

Prokaryotic carbonic anhydrases

Carbonic anhydrases catalyze the reversible hydration of CO(2) [CO(2)+H(2)Oright harpoon over left harpoon HCO(3)(-)+H(+)]. Since the discovery of this zinc (Zn) metalloenzyme in erythrocytes over 65 years ago, carbonic anhydrase has not only been found in virtually all mammalian tissues but is also abundant in plants and green unicellular algae. The enzyme is important to many eukaryotic physiological processes such as respiration, CO(2) transport and photosynthesis. Although ubiquitous in highly evolved organisms from the Eukarya domain, the enzyme has received scant attention in prokaryotes from the Bacteria and Archaea domains and has been purified from only five species since it was first identified in Neisseria sicca in 1963. Recent work has shown that carbonic anhydrase is widespread in metabolically diverse species from both the Archaea and Bacteria domains indicating that the enzyme has a more extensive and fundamental role in prokaryotic biology than previously recognized. A remarkable feature of carbonic anhydrase is the existence of three distinct classes (designated alpha, beta and gamma) that have no significant sequence identity and were invented independently. Thus, the carbonic anhydrase classes are excellent examples of convergent evolution of catalytic function. Genes encoding enzymes from all three classes have been identified in the prokaryotes with the beta and gamma classes predominating. All of the mammalian isozymes (including the 10 human isozymes) belong to the alpha class; however, only nine alpha class carbonic anhydrase genes have thus far been found in the Bacteria domain and none in the Archaea domain. The beta class is comprised of enzymes from the chloroplasts of both monocotyledonous and dicotyledonous plants as well as enzymes from phylogenetically diverse species from the Archaea and Bacteria domains. The only gamma class carbonic anhydrase that has thus far been isolated and characterized is from the methanoarchaeon Methanosarcina thermophila. Interestingly, many prokaryotes contain carbonic anhydrase genes from more than one class; some even contain genes from all three known classes. In addition, some prokaryotes contain multiple genes encoding carbonic anhydrases from the same class. The presence of multiple carbonic anhydrase genes within a species underscores the importance of this enzyme in prokaryotic physiology; however, the role(s) of this enzyme is still largely unknown. Even though most of the information known about the function(s) of carbonic anhydrase primarily relates to its role in cyanobacterial CO(2) fixation, the prokaryotic enzyme has also been shown to function in cyanate degradation and the survival of intracellular pathogens within their host. Investigations into prokaryotic carbonic anhydrase have already led to the identification of a new class (gamma) and future research will undoubtedly reveal novel functions for carbonic anhydrase in prokaryotes.     

Proton transfer to residues of basic pK(a) during catalysis by carbonic anhydrase.

The maximal velocity in the hydration of CO(2) catalyzed by the carbonic anhydrases in well-buffered solutions is limited by an intramolecular proton transfer from zinc-bound water to acceptor groups of the enzyme and hence to buffer in solution. Stopped-flow spectrophotometry was used to accumulate evidence that this maximal velocity is affected by residues of basic pK(a), near 8 to above 9, in catalysis of the hydration of CO(2) by carbonic anhydrases III, IV, V, and VII. A mutant of carbonic anhydrase II containing the replacement His-64-->Ala, which removes the prominent histidine proton shuttle (with pK(a) near 7), allows better observation of these basic groups. We suggest this feature of catalysis is general for the human and animal carbonic anhydrases and is due to residues of basic pK(a), predominantly lysines and tyrosines more distant from the zinc than His-64, that act as proton acceptors. These groups supplement the well-studied proton transfer from zinc-bound water to His-64 in the most efficient of the carbonic anhydrases, isozymes II, IV, and VII.     

Proton transfer within the active-site cavity of carbonic anhydrase III

The maximal turnover rate of CO2 hydration catalyzed by the carbonic anhydrases is limited by proton transfer steps from the zinc-bound water to solution, steps that regenerate the catalytically active zinc-bound hydroxide. Catalysis of CO2 hydration by wild-type human carbonic anhydrase III (HCA III) (k(cat) = 2 ms (-1)) is the least efficient among the carbonic anhydrases in its class, in part because it lacks an efficient proton shuttle residue. We have used site-directed mutagenesis to test positions within the active-site cavity of HCA III for their ability to carry out proton transfer by replacing various residues with histidine. Catalysis by wild-type HCA III and these six variants was determined from the initial velocity of hydration of CO2 measured by stopped-flow spectrophotometry and from the exchange of 18O between CO2 and H2O at chemical equilibrium by mass spectrometry. The results show that histidine at three positions (Lys64His, Arg67His and Phe131His) have the capacity to transfer protons during catalysis, enhancing maximal velocity of CO2 hydration and 18O exchange from 4- to 15-fold compared with wild-type HCA III. Histidine residues at the other three positions (Trp5His, Tyr7His, Phe20His) showed no firm evidence for proton transfer. These results are discussed in terms of the stereochemistry of the active-site cavity and possible proton transfer pathways.     

The catalytic properties of human carbonic anhydrase IX.

Human carbonic anhydrase IX (CA IX) is an integral membrane protein and a member of the alpha class of carbonic anhydrases that includes the human and animal enzymes. We have prepared a truncated, recombinant form of human CA IX of 255 residues consistent with full-length human CA II, among the most efficient of the carbonic anhydrases. Catalysis by and inhibition of this form of human CA IX has been investigated using stopped-flow spectrophotometry and 18O exchange measured by mass spectrometry. In kinetic constants for the hydration of CO2, CA IX closely resembled CA II with maximal proton transfer-dependent 18O exchange near 1 micros(-1) and kcat/Km near 55 microM(-1) x s(-1). Human CA IX was very strongly inhibited by three classic sulfonamides and cyanate, with inhibition constants that are close to those for CA II.     

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.     

Crystal structure of the "cab"-type beta class carbonic anhydrase from the archaeon Methanobacterium thermoautotrophicum

The structure of the "cab"-type beta class carbonic anhydrase from the archaeon Methanobacterium thermoautotrophicum (Cab) has been determined to 2.1-A resolution using the multiwavelength anomalous diffraction phasing technique. Cab exists as a dimer with a subunit fold similar to that observed in "plant"-type beta class carbonic anhydrases. The active site zinc is coordinated by protein ligands Cys(32), His(87), and Cys(90), with the tetrahedral coordination completed by a water molecule. The major difference between plant- and cab-type beta class carbonic anhydrases is in the organization of the hydrophobic pocket. The structure reveals a Hepes buffer molecule bound 8 A away from the active site zinc, which suggests a possible proton transfer pathway from the active site to the solvent.     

The structure of beta-carbonic anhydrase from the carboxysomal shell reveals a distinct subclass with one active site for the price of two

CsoSCA (formerly CsoS3) is a bacterial carbonic anhydrase localized in the shell of a cellular microcompartment called the carboxysome, where it converts HCO(3)(-) to CO(2) for use in carbon fixation by ribulose-bisphosphate carboxylase/oxygenase (RuBisCO). CsoSCA lacks significant sequence similarity to any of the four known classes of carbonic anhydrase (alpha, beta, gamma, or delta), and so it was initially classified as belonging to a new class, epsilon. The crystal structure of CsoSCA from Halothiobacillus neapolitanus reveals that it is actually a representative member of a new subclass of beta-carbonic anhydrases, distinguished by a lack of active site pairing. Whereas a typical beta-carbonic anhydrase maintains a pair of active sites organized within a two-fold symmetric homodimer or pair of fused, homologous domains, the two domains in CsoSCA have diverged to the point that only one domain in the pair retains a viable active site. We suggest that this defunct and somewhat diminished domain has evolved a new function, specific to its carboxysomal environment. Despite the level of sequence divergence that separates CsoSCA from the other two subclasses of beta-carbonic anhydrases, there is a remarkable level of structural similarity among active site regions, which suggests a common catalytic mechanism for the interconversion of HCO(3)(-) and CO(2). Crystal packing analysis suggests that CsoSCA exists within the carboxysome shell either as a homodimer or as extended filaments.     

Activation of carbonic anhydrase II by active-site incorporation of histidine analogs

The hydration of CO2 catalyzed by human carbonic anhydrase II (HCA II) is accompanied by proton transfer from the zinc-bound water of the enzyme to solution. We have replaced the proton shuttling residue His 64 with Ala and placed cysteine residues within the active-site cavity by mutating sites Trp 5, Asn 62, Ile 91, and Phe 131. These mutants were modified at the single inserted cysteine with imidazole analogs to introduce new potential shuttle groups. Catalysis by these modified mutants was determined by stopped-flow and 18O-exchange methods. Specificity in proton transfer was demonstrated; only modifications of the Cys 131-containing mutant showed enhancement in the proton transfer step of catalysis compared with unmodified Cys 131-containing mutant. Modifications at other sites resulted in up to 3-fold enhancement in rates of CO2 hydration, with apparent second-order rate constants near 350 microM(-1) s(-1). These are among the largest values of kcat/Km observed for a carbonic anhydrase.     

Fine tuning of the catalytic properties of carbonic anhydrase. Studies of a Thr200----His variant of human isoenzyme II

The active sites of carbonic anhydrases I contain a unique histidine residue at sequence position 200. To test the hypothesis that His200 is essential for the isoenzyme-specific catalytic and inhibitor-binding properties of carbonic anhydrases I, a variant of human carbonic anhydrase II, having His200 for Thr200, was prepared by oligonucleotide-directed mutagenesis. The variant has a circular dichroic spectrum that is indistinguishable from that of the parent enzyme. The kinetics of CO2 hydration and HCO3- dehydration has been investigated. The results show that the amino acid substitution has led to changes of catalytic parameters as well as Ki values for anion inhibition in the expected directions towards the values for isoenzyme I. However, the maximal 4-nitrophenyl acetate hydrolase activity of the variant is higher than for any naturally occurring carbonic anhydrase studied so far. A detailed analysis of the kinetic observations suggests that the modification has resulted in a change of the step that limits the maximal rate of CO2 hydration at saturating buffer concentrations. This rate-limiting step is an intramolecular proton transfer in unmodified isoenzyme II and, presumably, HCO3- dissociation in the variant and in human isoenzyme I. A free-energy profile for the dominating pathway of CO2 hydration at high pH was constructed. The results suggest that the major effect of His200 is a stabilization of the enzyme-HCO3- complex by about 7.5 kJ/mol (variant) and 6.1 kJ/mol (human isoenzyme I) relative to unmodified isoenzyme II, while proton transfer between the metal site and the reaction medium is only marginally affected by the amino acid replacement.     

Chemical modification of carbonic anhydrase II with acrolein

We have reacted acrolein with human carbonic anhydrase II using conditions reported to result in maximal formylethylation of exposed histidine and lysine residues (Pocker, Y., and Janji?, N. (1988) J. Biol. Chem. 263, 6169-6176). Pocker and Janji? proposed that the decrease by 95-98% in the steady-state turnover number for the hydration of CO2 caused by this chemical modification is due predominantly to the alkylation of one residue, the imidazole side chain of histidine 64. We measured the rate of 18O exchange between CO2 and water catalyzed by these enzymes at chemical equilibrium using membrane inlet mass spectrometry. The catalyzed rate of interconversion of CO2 and HCO3- at chemical equilibrium was the same for the acrolein-modified and the unmodified carbonic anhydrases, but the rate of release of 18O-labeled water from the active site had decreased by as much as 85% for the acrolein-modified enzyme. The 18O-exchange kinetics catalyzed by the acrolein-modified carbonic anhydrase II was similar to that catalyzed by a mutant human carbonic anhydrase II in which histidine at residue 64 was replaced with alanine. Moreover, modification of this mutant carbonic anhydrase II with acrolein did not alter to a significant extent its 18O-exchange pattern. These results support the proposal of Pocker and Janji? and the suggested role of histidine 64 in carbonic anhydrase II as a proton shuttle residue that transfers a proton from zinc-bound water to buffer in solution.     

Properties of intramolecular proton transfer in carbonic anhydrase III.

We investigated the efficiency of glutamic acid 64 and aspartic acid 64 as proton donors to the zinc-bound hydroxide in a series of site-specific mutants of human carbonic anhydrase III (HCA III). Rate constants for this intramolecular proton transfer, a step in the catalyzed dehydration of bicarbonate, were determined from the proton-transfer-dependent rates of release of H2 18O from the enzyme measured by mass spectrometry. The free energy plots representing these rate constants could be fit by the Marcus rate theory, resulting in an intrinsic barrier for the proton transfer of deltaG0++ = 2.2 +/- 0.5 kcal/mol, and a work function or thermodynamic contribution to the free energy of reaction wr = 10.8 +/- 0.1 kcal/mol. These values are very similar in magnitude to the Marcus parameters describing intramolecular proton transfer from His64 and His67 to the zinc-bound hydroxide in mutants of HCA III. That result and the equivalent efficiency of Glu64 and Asp64 as proton donors in the catalysis by CA III demonstrate a lack of specificity in proton transfer from these sites, which is indirect evidence of a number of proton conduction pathways through different structures of intervening water chains. The dominance of the thermodynamic contribution or work function for all of these proton transfers is consistent with the view that formation and breaking of hydrogen bonds in such water chains is a limiting factor for proton translocation.     

A plant-type (beta-class) carbonic anhydrase in the thermophilic methanoarchaeon Methanobacterium thermoautotrophicum.

Carbonic anhydrase, a zinc enzyme catalyzing the interconversion of carbon dioxide and bicarbonate, is nearly ubiquitous in the tissues of highly evolved eukaryotes. Here we report on the first known plant-type (beta-class) carbonic anhydrase in the archaea. The Methanobacterium thermoautotrophicum DeltaH cab gene was hyperexpressed in Escherichia coli, and the heterologously produced protein was purified 13-fold to apparent homogeneity. The enzyme, designated Cab, is thermostable at temperatures up to 75 degrees C. No esterase activity was detected with p-phenylacetate as the substrate. The enzyme is an apparent tetramer containing approximately one zinc per subunit, as determined by plasma emission spectroscopy. Cab has a CO(2) hydration activity with a k(cat) of 1.7 x 10(4) s(-1) and K(m) for CO(2) of 2.9 mM at pH 8.5 and 25 degrees C. Western blot analysis indicates that Cab (beta class) is expressed in M. thermoautotrophicum; moreover, a protein cross-reacting to antiserum raised against the gamma carbonic anhydrase from Methanosarcina thermophila was detected. These results show that beta-class carbonic anhydrases extend not only into the Archaea domain but also into the thermophilic prokaryotes.     

Structure and catalysis by carbonic anhydrase II: role of active-site tryptophan 5

The tryptophan residue Trp5, highly conserved in the α class of carbonic anhydrases including human carbonic anhydrase II (HCA II), is positioned at the entrance of the active site cavity and forms a π-stacking interaction with the imidazole ring of the proton shuttle His64 in its outward orientation. We have observed that replacement of Trp5 in HCA II caused significant structural changes, as determined by X-ray diffraction, in the conformation of 11 residues at the N-terminus and in the orientation of the proton shuttle residue His64. Most significantly, two variants W5H and W5E HCA II had His64 predominantly outward in orientation, while W5F and wild type showed the superposition of both outward and inward orientations in crystal structures. Although Trp5 influences the orientation of the proton shuttle His64, this orientation had no significant effect on the rate constant for proton transfer near 1 μs⁻¹, determined by exchange of ¹⁸O between CO₂ and water measured by mass spectrometry. The apparent values of the pK_a of the zinc-bound water and the proton shuttle residue suggest that different active-site conformations influence the two stages of catalysis, the proton transfer stage and the interconversion of CO₂ and bicarbonate.     

Catalytic enhancement of human carbonic anhydrase III by replacement of phenylalanine-198 with leucine

Carbonic anhydrase III, a cytosolic enzyme found predominantly in skeletal muscle, has a turnover rate for CO2 hydration 500-fold lower and a KI for inhibition by acetazolamide 700-fold higher (at pH 7.2) than those of red cell carbonic anhydrase II. Mutants of human carbonic anhydrase III were made by replacing three residues near the active site with amino acids known to be at the corresponding positions in isozyme II (Lys-64----His, Arg-67----Asn, and Phe-198----Leu). Catalytic properties were measured by stopped-flow spectrophotometry and 18O exchange between CO2 and water using mass spectrometry. The triple mutant of isozyme III had a turnover rate for CO2 hydration 500-fold higher than wild-type carbonic anhydrase III. The binding constants, KI, for sulfonamide inhibitors of the mutants containing Leu-198 were comparable to those of carbonic anhydrase II. The mutations at residues 64, 67, and 198 were catalytically independent; the lowered energy barrier for the triple mutant was the sum of the energy changes for each of the single mutants. Moreover, the triple mutant of isozyme III catalyzed the hydrolysis of 4-nitrophenyl acetate with a specific activity and pH dependence similar to those of isozyme II. Phe-198 is thus a major contributor to the low CO2 hydration activity, the weak binding of acetazolamide, and the low pKa of the zinc-bound water in carbonic anhydrase III. Intramolecular proton transfer involving His-64 was necessary for maximal turnover.     

Structural and kinetic analysis of proton shuttle residues in the active site of human carbonic anhydrase III

We report the X-ray crystal structures and rate constants for proton transfer in site-specific mutants of human carbonic anhydrase III (HCA III) that place a histidine residue in the active-site cavity: K64H, R67H, and K64H-R67N HCA III. Prior evidence from the exchange of 18O between CO2 and water measured by mass spectrometry shows each mutant to have enhanced proton transfer in catalysis compared with wild-type HCA III. However, His64 in K64H and K64H-R67N HCA III have at most a capacity for proton transfer that is only 13% that of His64 in HCA II. This reduced rate in mutants of HCA III is associated with a constrained side-chain conformation of His64, which is oriented outward, away from the active-site zinc in the crystal structures. This conformation appears stabilized by a prominent pi stacking interaction of the imidazole ring of His64 with the indole ring of Trp5 in mutants of HCA III. This single orientation of His64 in K64H HCA III predominates also in a double mutant K64H-R67N HCA III, indicating that the positive charge of Arg67 does not influence the observed conformation of His64 in the crystal structure. Hence, the structures and catalytic activity of these mutants of HCA III containing His64 account only in small part for the lower activity of this isozyme compared with HCA II. His67 in R67H HCA III was also shown to be a proton shuttle residue, having a capacity for proton transfer that was approximately four times that of His64 in K64H HCA III. This is most likely due to its proximity and orientation inward towards the zinc-bound solvent. These results emphasize the significance of side chain orientation and range of available conformational states as characteristics of an efficient proton shuttle in carbonic anhydrase.     

Enhancement of the catalytic properties of human carbonic anhydrase III by site-directed mutagenesis

Among the seven known isozymes of carbonic anhydrase in higher vertebrates, isozyme III is the least efficient in catalytic hydration of CO2 and the least susceptible to inhibition by sulfonamides. We have investigated the role of two basic residues near the active site of human carbonic anhydrase III (HCA III), lysine 64 and arginine 67, to determine whether they can account for some of the unique properties of this isozyme. Site-directed mutagenesis was used to replace these residues with histidine 64 and asparagine 67, the amino acids present at the corresponding positions of HCA II, the most efficient of the carbonic anhydrase isozymes. Catalysis by wild-type HCA III and mutants was determined from the initial velocity of hydration of CO2 at steady state by stopped-flow spectrophotometry and from the exchange of 18O between CO2 and water at chemical equilibrium by mass spectrometry. We have shown that histidine 64 functions as a proton shuttle in carbonic anhydrase by substituting histidine for lysine 64 in HCA III. The enhanced CO2 hydration activity and pH profile of the resulting mutant support this role for histidine 64 in the catalytic mechanism and suggest an approach that may be useful in investigating the mechanistic roles of active-site residues in other isozyme groups. Replacing arginine 67 in HCA III by asparagine enhanced catalysis of CO2 hydration 3-fold compared with that of wild-type HCA III, and the pH profile of the resulting mutant was consistent with a proton transfer role for lysine 64. Neither replacement enhanced the weak inhibition of HCA III by acetazolamide or the catalytic hydrolysis of 4-nitrophenyl acetate.     

Proton transfer in catalysis and the role of proton shuttles in carbonic anhydrase

The undisputed role of His64 in proton transfer during catalysis by carbonic anhydrases in the α class has raised questions concerning the details of its mechanism. The highly conserved residues Tyr7, Asn62, and Asn67 in the active-site cavity function to fine tune the properties of proton transfer by human carbonic anhydrase II (HCA II). For example, hydrophobic residues at these positions favor an inward orientation of His64 and a low pK_a for its imidazole side chain. It appears that the predominant manner in which this fine tuning is achieved in rate constants for proton transfer is through the difference in pK_a between His64 and the zinc-bound solvent molecule. Other properties of the active-site cavity, such as inward and outward conformers of His64, appear associated with the change in ΔpK_a; however, there is no strong evidence to date that the inward and outward orientations of His64 are in themselves requirements for facile proton transfer in carbonic anhydrase.     

Hydration of CO2 by carbonic anhydrase: intramolecular proton transfer between Zn2+-bound H2O and histidine 64 in human carbonic anhydrase II

The energy barrier for the intramolecular proton transfer between zinc-bound water and His 64 in the active site of human carbonic anhydrase II (HCA II) has been studied at the partial retention of diatomic differential overlap (PRDDO) level. The most important stabilizing factor for the intramolecular proton transfer is the zinc ion, which lowers the pKa of zinc-bound water and electrostatically repels the proton. The energy barrier of 127.5 kcal/mol for proton transfer between a water dimer is completely removed in the presence of the zinc ion. The zinc ligands, which donate electrons to the zinc ion, raise the barrier slightly to 34 kcal/mol for a 4-coordinated zinc complex including three imidazole ligands from His 94, His 96, and His 119 and to 54 kcal/mol for the 5-coordinated zinc complex including the fifth water ligand. A few model calculations indicate that these energy barriers are expected to be reduced to within experimental range (approximately 10 kcal/mol) when large basis set, correlation energies, and molecular dynamics are considered. The proton-transfer group, which functions as proton receiver in the intramolecular proton transfer, helps to attract the proton; and the partially ordered active site water molecules are important for proton relay function.     

Structure of a dimeric fungal α-type carbonic anhydrase

The crystal structure of Aspergillus oryzae carbonic anhydrase (AoCA) was determined at 2.7 Å resolution and it revealed a dimer, which only has precedents in the α class in two membrane and cancer-associated enzymes. α carbonic anhydrases are underrepresented in fungi compared to the β class, this being the first structural representative. The overall fold and zinc binding site resemble other well studied carbonic anhydrases. A major difference is that the histidine, thought to be the major proton shuttle residue in most mammalian enzymes, is replaced by a phenylalanine in AoCA. This finding poses intriguing questions as to the biological functions of fungal α carbonic anhydrases, which are promising candidates for biotechnological applications.Structured summaryAoCA binds to AoCA by molecular sieving (View interaction)AoCA binds to AoCA X-ray crystallography (View interaction)