Proton Uptake Pathway Research Articles

Structural characterization of proton-pumping rhodopsin lacking a cytoplasmic proton donor residue by X-ray crystallography

DTG/DTS rhodopsin, which was named based on a three-residue motif (DTG or DTS) that is important for its function, is a light-driven proton-pumping microbial rhodopsin using a retinal chromophore. In contrast to other light-driven ion-pumping rhodopsins, DTG/DTS rhodopsin does not have a cytoplasmic proton donor residue, such as Asp, Glu, or Lys. Because of the lack of cytoplasmic proton donor residue, proton directly binds to the retinal chromophore from the cytoplasmic solvent. However, mutational experiments that showed the complicated effects of mutations were not able to clarify the roles played by each residue, and the detail of proton uptake pathway is unclear because of the lack of structural information. To understand the proton transport mechanism of DTG/DTS rhodopsin, here we report the three-dimensional structure of one of the DTG/DTS rhodopsins, PspR from Pseudomonas putida, by X-ray crystallography. We show that the structure of the cytoplasmic side of the protein is significantly different from that of bacteriorhodopsin, the best-characterized proton-pumping rhodopsin, and large cytoplasmic cavities were observed. We propose that these hydrophilic cytoplasmic cavities enable direct proton uptake from the cytoplasmic solvent without the need for a specialized cytoplasmic donor residue. The introduction of carboxylic residues homologous to the cytoplasmic donors in other proton-pumping rhodopsins resulted in higher pumping activity with less pH dependence, suggesting that DTG/DTS rhodopsins are advantageous for producing energy and avoiding intracellular alkalization in soil and plant-associated bacteria.

Proton transfer in the D-channel of cytochrome c oxidase modeled by a transition network approach

BackgroundDetermination of proton uptake pathways in Cytochrome c Oxidase is difficult due to the complexity of the system. The transition networks approach allows sampling of proton transfer pathways without predefined reaction coordinate. MethodsComputation of the proton transfer pathways in a model of the D-channel of cytochrome c oxidase has been performed by a transition network approach that combines discrete, optimisation based and molecular dynamics based sampling. ResultsThe optimal pathway involves an opening of the so-called asparagine gate, hydration of the asparagine region, the formation of a hydrogen-bonded chain, and finally concerted proton hole transport along this chain. The optimal pathway finds the protonation of residue H26 close to the channel entrance favourable for lowering the transition energies of subsequent steps, in particular, opening of the Asn gate and formation of a hydrogen-bonded chain. Residue Y33 plays an important role in shuttling the transferred proton hole. ConclusionsThe optimal pathway found by the transition network approach shows the same important characteristics as pathways determined earlier by other methods. The computed barrier and reaction energies are also in good agreement with previous studies. The transition network approach provides an alternative to explore pathways in complex systems. General significanceThe correct function of the enzyme as oxidase and proton pump depends on the interplay of several redox and proton transport steps. Understanding the proton transport mechanism is therefore key to understanding the protein's function. The complex nature of long- distances proton transfer through a protein requires a non-trivial simulation strategy.

Outcomes of pregnancy after bariatric surgery: a systematic review of systematic reviews

The heme‑copper oxidases (HCuOs) are terminal components of the respiratory chain, catalyzing oxygen reduction coupled to the generation of a proton motive force. The C-family HCuOs, found in many pathogenic bacteria under low oxygen tension, utilize a single proton uptake pathway to deliver protons both for O2 reduction and for proton pumping. This pathway, called the KC-pathway, starts at Glu-49P in the accessory subunit CcoP, and connects into the catalytic subunit CcoN via the polar residues Tyr-(Y)-227, Asn (N)-293, Ser (S)-244, Tyr (Y)-321 and internal water molecules, and continues to the active site. However, although the residues are known to be functionally important, little is known about the mechanism and dynamics of proton transfer in the KC-pathway. Here, we studied variants of Y227, N293 and Y321. Our results show that in the N293L variant, proton-coupled electron transfer is slowed during single-turnover oxygen reduction, and moreover it shows a pH dependence that is not observed in wildtype. This suggests that there is a shift in the pKa of an internal proton donor into an experimentally accessible range, from >10 in wildtype to ~8.8 in N293L. Furthermore, we show that there are distinct roles for the conserved Y321 and Y227. In Y321F, proton uptake from bulk solution is greatly impaired, whereas Y227F shows wildtype-like rates and retains ~50% turnover activity. These tyrosines have evolutionary counterparts in the K-pathway of B-family HCuOs, but they do not have the same roles, indicating diversity in the proton transfer dynamics in the HCuO superfamily.

Mechanism of proton transfer through the KC proton pathway in the Vibrio cholerae cbb3 terminal oxidase

The heme‑copper oxidases (HCuOs) are terminal components of the respiratory chain, catalyzing oxygen reduction coupled to the generation of a proton motive force. The C-family HCuOs, found in many pathogenic bacteria under low oxygen tension, utilize a single proton uptake pathway to deliver protons both for O2 reduction and for proton pumping. This pathway, called the KC-pathway, starts at Glu-49P in the accessory subunit CcoP, and connects into the catalytic subunit CcoN via the polar residues Tyr-(Y)-227, Asn (N)-293, Ser (S)-244, Tyr (Y)-321 and internal water molecules, and continues to the active site. However, although the residues are known to be functionally important, little is known about the mechanism and dynamics of proton transfer in the KC-pathway. Here, we studied variants of Y227, N293 and Y321. Our results show that in the N293L variant, proton-coupled electron transfer is slowed during single-turnover oxygen reduction, and moreover it shows a pH dependence that is not observed in wildtype. This suggests that there is a shift in the pKa of an internal proton donor into an experimentally accessible range, from >10 in wildtype to ~8.8 in N293L. Furthermore, we show that there are distinct roles for the conserved Y321 and Y227. In Y321F, proton uptake from bulk solution is greatly impaired, whereas Y227F shows wildtype-like rates and retains ~50% turnover activity. These tyrosines have evolutionary counterparts in the K-pathway of B-family HCuOs, but they do not have the same roles, indicating diversity in the proton transfer dynamics in the HCuO superfamily.

The cytochrome b Zn binding amino acid residue histidine 291 is essential for ubihydroquinone oxidation at the Qo site of bacterial cytochrome bc1

The ubiquinol:cytochrome (cyt) c oxidoreductase (or cyt bc1) is an important membrane protein complex in photosynthetic and respiratory energy transduction. In bacteria such as Rhodobacter capsulatus it is constituted of three subunits: the iron-sulfur protein, cyt b and cyt c1, which form two catalytic domains, the Qo (hydroquinone (QH2) oxidation) and Qi (quinone (Q) reduction) sites. At the Qo site, the pathways of bifurcated electron transfers emanating from QH2 oxidation are known, but the associated proton release routes are not well defined. In energy transducing complexes, Zn2+ binding amino acid residues often correlate with proton uptake or release pathways. Earlier, using combined EXAFS and structural studies, we identified Zn coordinating residues of mitochondrial and bacterial cyt bc1. In this work, using the genetically tractable bacterial cyt bc1, we substituted each of the proposed Zn binding residues with non-protonatable side chains. Among these mutants, only the His291Leu substitution destroyed almost completely the Qo site catalysis without perturbing significantly the redox properties of the cofactors or the assembly of the complex. In this mutant, which is unable to support photosynthetic growth, the bifurcated electron transfer reactions that result from QH2 oxidation at the Qo site, as well as the associated proton(s) release, were dramatically impaired. Based on these findings, on the putative role of His291 in liganding Zn, and on its solvent exposed and highly conserved position, we propose that His291 of cyt b is critical for proton release associated to QH2 oxidation at the Qo site of cyt bc1.

Electrochemistry suggests proton access from the exit site to the binuclear center in Paracoccus denitrificans cytochrome c oxidase pathway variants

Two different pathways through which protons access cytochrome c oxidase operate during oxygen reduction from the mitochondrial matrix, or the bacterial cytoplasm. Here, we use electrocatalytic current measurements to follow oxygen reduction coupled to proton uptake in cytochrome c oxidase isolated from Paracoccus denitrificans. Wild type enzyme and site-specific variants with defects in both proton uptake pathways (K354M, D124N and K354M/D124N) were immobilized on gold nanoparticles, and oxygen reduction was probed electrochemically in the presence of varying concentrations of Zn2+ ions, which are known to inhibit both the entry and the exit proton pathways in the enzyme. Our data suggest that under these conditions substrate protons gain access to the oxygen reduction site via the exit pathway.

Clarifying the Roles of Cardiolipin

Cardiolipins (CL) are uniquely structured double lipids that are universally found in membranes which couple electron transport and phosphorylation. The proposed roles of CL in these membranes include mainly two aspects: the effects on the structure and dynamics of the membranes' lipid component and the interplay with membrane-associated proteins. In previous work, we have studied both of these aspects by utilizing atomistic molecular dynamics simulations, starting with the general effects of CL on membrane properties and the interplay with ions [1], further moving on to the interactions with the membrane-embedded respiratory complex cyt bc1 [2]. The latter model system that is of greater interest comprises the entire cyt bc1 dimer of the purple photosynthetic bacterium Rhodobacter capsulatus embedded in a lipid bilayer, whose lipid composition mimics that of the inner mitochondrial membrane. Intriguingly CLs were observed to diffuse spontaneously to the dimer interface and to the immediate vicinity of the catalytic Qi-sites [2]. This observation is in agreement with experimental data, as CLs are indeed located close to the Qi-sites in several X-ray crystal structures of the complex. Importantly, our observations support the proposed role of CL in delivering protons for the non-reduced substrate forms in the active site.In ongoing work that we discuss here we focus more specifically on the roles of individual components of the proposed proton uptake pathway (CL, water, and individual protein residues) and on the atom-level reaction mechanism in the binding pocket. To this end, further MD simulations, QM calculations, and cite-directed mutagenesis experiments were employed. We also discuss whether there is a plausible pathway for substrate movement between the active sites through the lipid-filled insides of the complex, and the role of oxidative stress in cyt bc1 behavior.

Crystal structure of deltarhodopsin‐3 from Haloterrigena thermotolerans

Deltarhodopsin, a new member of the microbial rhodopsin family, functions as a light-driven proton pump. Here, we report the three-dimensional structure of deltarhodopsin (dR3) from Haloterrigena thermotolerans at 2.7 Å resolution. A crystal belonging to space group R32 (a, b = 111.71 Å, c = 198.25 Å) was obtained by the membrane fusion method. In this crystal, dR3 forms a trimeric structure as observed for bacteriorhodopsin (bR). Structural comparison of dR with bR showed that the inner part (the proton release and uptake pathways) is highly conserved. Meanwhile, residues in the protein-protein contact region are largely altered so that the diameter of the trimeric structure at the cytoplasmic side is noticeably larger in dR3. Unlike bR, dR3 possesses a helical segment at the C-terminal region that fills the space between the AB and EF loops. A significant difference is also seen in the FG loop, which is one residue longer in dR3. Another peculiar property of dR3 is a highly crowded distribution of positively charged residues on the cytoplasmic surface, which may be relevant to a specific interaction with some cytoplasmic component.

Quinone-dependent proton transfer pathways in the photosynthetic cytochrome b 6 f complex

As much as two-thirds of the proton gradient used for transmembrane free energy storage in oxygenic photosynthesis is generated by the cytochrome b6f complex. The proton uptake pathway from the electrochemically negative (n) aqueous phase to the n-side quinone binding site of the complex, and a probable route for proton exit to the positive phase resulting from quinol oxidation, are defined in a 2.70-Å crystal structure and in structures with quinone analog inhibitors at 3.07 Å (tridecyl-stigmatellin) and 3.25-Å (2-nonyl-4-hydroxyquinoline N-oxide) resolution. The simplest n-side proton pathway extends from the aqueous phase via Asp20 and Arg207 (cytochrome b6 subunit) to quinone bound axially to heme c(n). On the positive side, the heme-proximal Glu78 (subunit IV), which accepts protons from plastosemiquinone, defines a route for H(+) transfer to the aqueous phase. These pathways provide a structure-based description of the quinone-mediated proton transfer responsible for generation of the transmembrane electrochemical potential gradient in oxygenic photosynthesis.

Deprotonation of D96 in Bacteriorhodopsin Opens the Proton Uptake Pathway

Despite extensive investigation, the precise mechanism controlling the opening of the cytoplasmic proton uptake pathway in bacteriorhodopsin (bR) has remained a mystery. From an analysis of the X-ray structure of the D96G/F171C/F219L triple mutant of bR and 60 independent molecular dynamics simulations of bR photointermediates, we report that the deprotonation of D96, a key residue in proton transfer reactions, serves two roles that occur sequentially. First, D96 donates a proton to the Schiff base. Subsequently, the deprotonation of D96 serves to "unlatch" the cytoplasmic side. The latching function of D96 appears to be remarkably robust, functioning to open hydration channels inall photointermediate structures. These results suggest that the protonation state of D96 may be the critical biophysical cue controlling the opening and closing of the cytoplasmic half-channel in bR. We suspect that this protonation-switch mechanism could also be utilized in other proton pumps to minimize backflow and reinforce directionality.

An Anhydrous Proton Transfer Pathway in the Cytochrome B6F Complex

Cytochrome b6f, a hetero-oligomeric energy transducing membrane protein complex, catalyzes proton-coupled electron transfer reactions of the substrate quinone to generate as much as two-thirds of the total proton gradient used for ATP synthesis in oxygenic photosynthesis. Proton transfer pathways within b6f have remained unidentified due to limitations of crystallographic resolution1,2,3,4,5. using new crystallographic information based on a 2.70 A crystal structure of the native complex, and structures obtained in the presence of quinone analogue inhibitors, tridecyl-stigmatellin (TDS) and 2-nonyl-4-hydroxyquinoline-N-oxide (NQNO) (resolution 3.07 A and 3.25 A respectively) seen in close proximity to heme cn on the electrochemically negative (n) side of the b6f complex, an anhydrous proton uptake pathway is defined that delivers protons from the n-side aqueous phase to plastoquinone bound at heme cn. A hydrated channel is identified on the electrochemically positive (p) side of the complex, that may provide a route for proton exit to the p-side aqueous phase. These n- and p-side pathways contribute to the first complete description of quinone-mediated trans-membrane proton transfer.1. Kurisu et al. 2003, 2Stroebel et al. 2003, 3Yan et al. 2006, 4Yamashita et al. 2007, 5Baniulis et al. 2009View Large Image | View Hi-Res Image | Download PowerPoint Slide

Proton transfer in the quinol-dependent nitric oxide reductase from Geobacillus stearothermophilus during reduction of oxygen

Bacterial nitric oxide reductases (NOR) are integral membrane proteins that catalyse the reduction of nitric oxide to nitrous oxide, often as a step in the process of denitrification. Most functional data has been obtained with NORs that receive their electrons from a soluble cytochrome c in the periplasm and are hence termed cNOR. Very recently, the structure of a different type of NOR, the quinol-dependent (q)-NOR from the thermophilic bacterium Geobacillus stearothermophilus was solved to atomic resolution [Y. Matsumoto, T. Tosha, A.V. Pisliakov, T. Hino, H. Sugimoto, S. Nagano, Y. Sugita and Y. Shiro, Nat. Struct. Mol. Biol. 19 (2012) 238–246]. In this study, we have investigated the reaction between this qNOR and oxygen. Our results show that, like some cNORs, the G. stearothermophilus qNOR is capable of O2 reduction with a turnover of ~3electronss−1 at 40°C. Furthermore, using the so-called flow-flash technique, we show that the fully reduced (with three available electrons) qNOR reacts with oxygen in a reaction with a time constant of 1.8ms that oxidises the low-spin heme b. This reaction is coupled to proton uptake from solution and presumably forms a ferryl intermediate at the active site. The pH dependence of the reaction is markedly different from a corresponding reaction in cNOR from Paracoccus denitrificans, indicating that possibly the proton uptake mechanism and/or pathway differs between qNOR and cNOR. This study furthermore forms the basis for investigation of the proton transfer pathway in qNOR using both variants with putative proton transfer elements modified and measurements of the vectorial nature of the proton transfer. This article is part of a Special Issue entitled: 17th European Bioenergetics Conference (EBEC 2012).

Intricate Role of Water in Proton Transport through Cytochrome c Oxidase

Cytochrome c oxidase (CytcO), the final electron acceptor in the respiratory chain, catalyzes the reduction of O(2) to H(2)O while simultaneously pumping protons across the inner mitochondrial or bacterial membrane to maintain a transmembrane electrochemical gradient that drives, for example, ATP synthesis. In this work mutations that were predicted to alter proton translocation and enzyme activity in preliminary computational studies are characterized with extensive experimental and computational analysis. The mutations were introduced in the D pathway, one of two proton-uptake pathways, in CytcO from Rhodobacter sphaeroides . Serine residues 200 and 201, which are hydrogen-bonded to crystallographically resolved water molecules halfway up the D pathway, were replaced by more bulky hydrophobic residues (Ser200Ile, Ser200Val/Ser201Val, and Ser200Val/Ser201Tyr) to query the effects of changing the local structure on enzyme activity as well as proton uptake, release, and intermediate transitions. In addition, the effects of these mutations on internal proton transfer were investigated by blocking proton uptake at the pathway entrance (Asp132Asn replacement in addition to the above-mentioned mutations). Even though the overall activities of all mutant CytcO's were lowered, both the Ser200Ile and Ser200Val/Ser201Val variants maintained the ability to pump protons. The lowered activities were shown to be due to slowed oxidation kinetics during the P(R) → F and F → O transitions (P(R) is the "peroxy" intermediate formed at the catalytic site upon reaction of the four-electron-reduced CytcO with O(2), F is the oxoferryl intermediate, and O is the fully oxidized CytcO). Furthermore, the P(R) → F transition is shown to be essentially pH independent up to pH 12 (i.e., the apparent pK(a) of Glu286 is increased from 9.4 by at least 3 pK(a) units) in the Ser200Val/Ser201Val mutant. Explicit simulations of proton transport in the mutated enzymes revealed that the solvation dynamics can cause intriguing energetic consequences and hence provide mechanistic insights that would never be detected in static structures or simulations of the system with fixed protonation states (i.e., lacking explicit proton transport). The results are discussed in terms of the proton-pumping mechanism of CytcO.

The ATP Synthase a-subunit of Extreme Alkaliphiles Is a Distinct Variant: MUTATIONS IN THE CRITICAL ALKALIPHILE-SPECIFIC RESIDUE LYS-180 AND OTHER RESIDUES THAT SUPPORT ALKALIPHILE OXIDATIVE PHOSPHORYLATION

A lysine residue in the putative proton uptake pathway of the ATP synthase a-subunit is found only in alkaliphilic Bacillus species and is proposed to play roles in proton capture, retention and passage to the synthase rotor. Here, Lys-180 was replaced with alanine (Ala), glycine (Gly), cysteine (Cys), arginine (Arg), or histidine (His) in the chromosome of alkaliphilic Bacillus pseudofirmus OF4. All mutants exhibited octylglucoside-stimulated ATPase activity and β-subunit levels at least as high as wild-type. Purified mutant F(1)F(0)-ATP synthases all contained substantial a-subunit levels. The mutants exhibited diverse patterns of native (no octylglucoside) ATPase activity and a range of defects in malate growth and in vitro ATP synthesis at pH 10.5. ATP synthesis by the Ala, Gly, and His mutants was also impaired at pH 7.5 in the presence of a protonophoric uncoupler. Thus Lys-180 plays a role when the protonmotive force is reduced at near neutral, not just at high pH. The Arg mutant exhibited no ATP synthesis activity in the alkaliphile setting although activity was reported for a K180R mutant of a thermoalkaliphile synthase (McMillan, D. G., Keis, S., Dimroth, P., and Cook, G. M. (2007) J. Biol. Chem. 282, 17395-17404). The hypothesis that a-subunits from extreme alkaliphiles and the thermoalkaliphile represent distinct variants was supported by demonstration of the importance of additional alkaliphile-specific a-subunit residues, not found in the thermoalkaliphile, for malate growth of B. pseudofirmus OF4. Finally, a mutant B. pseudofirmus OF4 synthase with switched positions of Lys-180 (helix 4) and Gly-212 (helix 5) retained significant coupled synthase activity accompanied by proton leakiness.

Functional Hydration and Conformational Gating of Proton Uptake in Cytochrome c Oxidase

Cytochrome c oxidase couples the reduction of dioxygen to proton pumping against an electrochemical gradient. The D-channel, a 25-Å-long cavity, provides the principal pathway for the uptake of chemical and pumped protons. A water chain is thought to mediate the relay of protons via a Grotthuss mechanism through the D-channel, but it is interrupted at N139 in all available crystallographic structures. We use free-energy simulations to examine the proton uptake pathway in the wild type and in single-point mutants N139V and N139A, in which redox and pumping activities are compromised. We present a general approach for the calculation of water occupancy in protein cavities and demonstrate that combining efficient sampling algorithms with long simulation times (hundreds of nanoseconds) is required to achieve statistical convergence of equilibrium properties in the protein interior. The relative population of different conformational and hydration states of the D-channel is characterized. Results shed light on the role of N139 in the mechanism of proton uptake and clarify the physical basis for inactive phenotypes. The conformational isomerization of the N139 side chain is shown to act as a gate controlling the formation of a functional water chain or “proton wire.” In the closed state of N139, the spatial distribution of water in the D-channel is consistent with available crystallographic models. However, a metastable state of N139 opens up a narrow bottleneck in which 50% occupancy by a water molecule establishes a proton pathway throughout the D-channel. Results for N139V suggest that blockage of proton uptake resulting from persistent interruption of the water pathway is the cause of this mutant's marginal oxidase activity. In contrast, results for N139A indicate that the D-channel is a continuously hydrated cavity, implying that the decoupling of oxidase activity from proton pumping measured in this mutant is not due to interruption of the proton relay chain.

Identification of FTIR Bands Due to Internal Water Molecules around the Quinone Binding Sites in the Reaction Center from Rhodobacter sphaeroides

The bacterial reaction center (RC) is a membrane protein complex that performs photosynthetic electron transfer from a bacteriochlorophyll dimer to quinone acceptors Q(A) and Q(B). Q(B) accepts electrons from the primary quinone, Q(A), in two sequential electron transfer reactions coupled to uptake of a proton from solution. It has been suggested that water molecules along the proton uptake pathway are protonated upon quinone reduction on the basis of FTIR difference spectra [Breton, J., and Nabedryk, E. (1998) Photosynth. Res. 55, 301-307]. We examined the possible involvement of water molecules in the photoreaction processes by studying (18)O water isotope effects on FTIR difference spectra resulting from formation of Q(A)(-) and Q(B)(-). Continuum bands in D(2)O due to Q(B)(-) formation in the 2300-1800 cm(-1) region did not show spectral shifts by (18)O water in the wild-type (WT) RC, suggesting that these bands do not originate from (protonated) water. In contrast, the Q(B)(-)/Q(B) spectrum of the EQ-L212 mutant RC showed a spectral shift of a band near 2100 cm(-1) due to (18)O water substitution, consistent with protonation of internal water. FTIR shifts due to (18)O water were also observed following formation of Q(A)(-) and Q(B)(-) in the spectral region of 3700-3500 cm(-1) characteristic of weakly hydrogen bonded water. The water responsible for the Q(B)(-) change was localized near Glu-L212 by spectral shifts in mutant RCs. The weakly hydrogen bonded water perturbed by quinone reduction may play a role in stabilizing the charge-separated state.

Effect of Xenon Binding to a Hydrophobic Cavity on the Proton Pumping Cycle in Bacteriorhodopsin

To understand the functional role of apolar cavities in bacteriorhodopsin, a light-driven proton pump found in Halobacterium salinarum, we investigated the crystal structure in pressurized xenon or krypton. Diffraction data from the P622 crystal showed that one Xe or Kr atom binds to a preexisting hydrophobic cavity buried between helices C and D, located at the same depth from the membrane surface as Asp96, a key residue in the proton uptake pathway. The occupation fraction of Xe or Kr was calculated as approximately 0.32 at a pressure of 1 MPa. In the unphotolyzed state, the binding of Xe or Kr caused no large deformation of the cavity. However, the proton pumping cycle was greatly perturbed when an aqueous suspension of purple membrane was pressurized with xenon gas; that is, the decay of the M state was accelerated significantly (~5 times at full occupancy), while the decay of an equilibrium state of N and O was slightly decelerated. A similar but much smaller perturbation in the reaction kinetics was observed upon pressurization with krypton gas. In a glycerol/water mixture, xenon-induced acceleration of M decay became less significant in proportion to the water activity. Together with the structure of the xenon-bound protein, these observations suggest that xenon binding helps water molecules permeate into apolar cavities in the proton uptake pathway, thereby accelerating the water-mediated proton transfer from Asp96 to the Schiff base.

Electrostatic control of proton pumping in cytochrome c oxidase

As part of the mitochondrial respiratory chain, cytochrome c oxidase utilizes the energy produced by the reduction of O 2 to water to fuel vectorial proton transport. The mechanism coupling proton pumping to redox chemistry is unknown. Recent advances have provided evidence that each of the four observable transitions in the complex catalytic cycle consists of a similar sequence of events. However, the physico-chemical basis underlying this recurring sequence has not been identified. We identify this recurring pattern based on a comprehensive model of the catalytic cycle derived from the analysis of oxygen chemistry and available experimental evidence. The catalytic cycle involves the periodic repetition of a sequence of three states differing in the spatial distribution of charge in the active site: [0|1], [1|0], and [1|1], where the total charge of heme a and the binuclear center appears on the left and on the right, respectively. This sequence recurs four times per turnover despite differences in the redox chemistry. This model leads to a simple, robust, and reproducible sequence of electron and proton transfer steps and rationalizes the pumping mechanism in terms of electrostatic coupling of proton translocation to redox chemistry. Continuum electrostatic calculations support the proposed mechanism and suggest an electrostatic origin for the decoupled and inactive phenotypes of ionic mutants in the principal proton-uptake pathway.

Crystal Structures of Archaerhodopsin-1 and -2: Common Structural Motif in Archaeal Light-driven Proton Pumps

Archaerhodopsin-1 and -2 (aR-1 and aR-2) are light-driven proton pumps found in Halorubrum sp. aus-1 and -2, which share 55-58% sequence identity with bacteriorhodopsin (bR), a proton pump found in Halobacterium salinarum. In this study, aR-1 and aR-2 were crystallized into 3D crystals belonging to P4(3)2(1)2 (a = b = 128.1 A, c = 117.6 A) and C222(1) (a = 122.9 A, b = 139.5 A, c = 108.1 A), respectively. In both the crystals, the asymmetric unit contains two protein molecules with slightly different conformations. Each subunit is composed of seven helical segments as seen in bR but, unlike bR, aR-1 as well as aR-2 has a unique omega loop near the N terminus. It is found that the proton pathway in the extracellular half (i.e. the proton release channel) is more opened in aR-2 than in aR-1 or bR. This structural difference accounts for a large variation in the pKa of the acid purple-to-blue transition among the three proton pumps. All the aromatic residues surrounding the retinal polyene chain are conserved among the three proton pumps, confirming a previous argument that these residues are required for the stereo-specificity of the retinal isomerization. In the cytoplasmic half, the region surrounded by helices B, C and G is highly conserved, while the structural conservation is very low for residues extruded from helices E and F. Structural conservation of the hydrophobic residues located on the proton uptake pathway suggests that their precise arrangement is necessary to prevent a backward flow of proton in the presence of a large pH gradient and membrane potential. An empty cavity is commonly seen in the vicinity of Leu93 contacting the retinal C13 methyl. Existence of such a cavity is required to allow a large rotation of the side-chain of Leu93 at the early stage of the photocycle, which has been shown to accompany water translocation across the Schiff base.

Water dynamics simulation as a tool for probing proton transfer pathways in a heptahelical membrane protein

The proton transfer pathway in a heptahelical membrane protein, the light-driven proton pump bacteriorhodopsin (BR), is probed by a combined approach of structural analysis of recent X-ray models and molecular dynamics (MD) simulations that provide the diffusion pathways of internal and external water molecules. Analyzing the hydrogen-bond contact frequencies of the water molecules with protein groups, the complete proton pathway through the protein is probed. Beside the well-known proton binding sites in the protein interior-the protonated Schiff base, Asp85 and Asp96, and the H(5)O(2) (+) complex stabilized by Glu204 and Glu194-the proton release and uptake pathways to the protein surfaces are described in great detail. Further residues were identified, by mutation of which the proposed pathways can be verified. In addition the diffusion pathway of water 502 from Lys216 to Asp96 is shown to cover the positions of the intruding waters 503 and 504 in the N-intermediate. The transiently established water chain in the N-state provides a proton pathway from Asp96 to the Schiff base in the M- to N-transition in a Grotthus-like mechanism, as concluded earlier from time-resolved Fourier transform infrared experiments [le Coutre et al., Proc Nat Acad Sci USA 1995;92:4962-4966].