D1-S169A substitution of photosystem II reveals a novel S2-state structure

In photosystem II (PSII), photosynthetic water oxidation occurs at the O₂-evolving complex (OEC), a tetramanganese-calcium cluster that cycles through light-induced redox intermediates (S₀–S₄) to produce oxygen from two substrate water molecules. The OEC is surrounded by a hydrogen-bonded network of amino-acid residues that plays a crucial role in proton transfer and substrate water delivery. Previously, we found that D1-S169 was crucial for water oxidation and its mutation to alanine perturbed the hydrogen-bonding network. In this study, we demonstrate that the activation energy for the S₂ to S₁ transition of D1-S169A PSII is higher than wild-type PSII with a ~1.7–2.7× slower rate of charge recombination with Q_A⁻ relative to wild-type PSII. Arrhenius analysis of the decay kinetics shows an E_a of 5.87 ± 1.15 kcal mol⁻¹ for decay back to the S₁ state, compared to 0.80 ± 0.13 kcal mol⁻¹ for the wild-type S₂ state. In addition, we find that ammonia does not affect the S₂-state EPR signal, indicating that ammonia does not bind to the Mn cluster in D1-S169A PSII. Finally, a QM/MM analysis indicates that an additional water molecule binds to the Mn4 ion in place of an oxo ligand O5 in the S₂ state of D1-S169A PSII. The altered S₂ state of D1-S169A PSII provides insight into the S₂➔S₃ state transition.     

Application of the Marcus theory for analysis of the temperature dependence of the reactions leading to photosynthetic water oxidation: results and implications

The temperature dependence of donor side reactions was analysed within the framework of the Marcus theory of nonadiabatic electron transfer. The following results were obtained for PS II membrane fragments from spinach: (1) the reorganisation energy of P680^+? reduction by Y_Z is of the order of 0.5?eV in samples with a functionally fully competent water oxidising complex (WOC); (2) destruction of the WOC by Tris-washing gives rise to a drastic increase of λ to values of the order of 1.6?eV; (3) the reorganisation energies of the oxidation steps in the WOC are dependent, on the redox states S _i with values of about 0.6?eV for the reactions Y_Z ^OX S ₀→Y_Z S ₁ and Y_Z ^OX S ₁→Y_Z S ₂, 1.6?eV for the reaction Y_Z ^OX S ₂→Y_Z S ₃ and 1.1?eV (above a characteristic temperature u_c of about 6??°C) for the reaction Y_Z ^OX S ₃→→Y_Z S ₀+O₂. Using an empirical rate constant-distance relationship, the van der Waals distance between Y_Z and P680 was found to be about 10?Å, independent of the presence or absence of the WOC, whereas the distance between Y_Z and the manganese cluster in the WOC was ≥15?Å. Based on the calculated activation energies the environment of Y_Z is inferred to be almost "dry" and hydrophobic when the WOC is intact but becomes enriched with water molecules after WOC destruction. Furthermore, it is concluded that the transition S ₂→S ₃ is an electron transfer reaction gated by a conformational change, i.e. it comprises significant structural changes of functional relevance. Measurements of kinetic H/D isotope exchange effects support the idea that none of these reactions is gated by the break of a covalent O-H bond. The implications of these findings for the mechanism of water oxidation are discussed.     

PsbP-induced protein conformational changes around Cl<Superscript>−</Superscript> ions in the water oxidizing center of photosystem II

PsbP is an extrinsic protein of PSII having a function of Ca²⁺ and Cl^? retention in the water-oxidizing center (WOC). In order to understand the mechanism how PsbP regulates the Cl^? binding in WOC, we examined the effect of PsbP depletion on the protein structures around the Cl^? sites using Fourier transform infrared (FTIR) spectroscopy. Light-induced FTIR difference spectra upon the S¹→S₂ transition were obtained using Cl^?-bound and NO₃^?-substituted PSII membranes in the presence and absence of PsbP. A clear difference in the amide I band changes by PsbP depletion was observed between Cl^?-bound and NO₃^?-substituted PSII samples, indicating that PsbP binding perturbed the protein conformations around the Cl^?ion(s) in WOC. It is suggested that PsbP stabilizes the Cl^? binding by regulating the dissociation constant of Cl^? and/or an energy barrier of Cl^? dissociation through protein conformational changes around the Cl^? ion(s).     

Characterization of constitutive and acid-induced outwardly rectifying chloride currents in immortalized mouse distal tubular cells

Thiazides block Na⁺ reabsorption while enhancing Ca²⁺ reabsorption in the kidney. As previously demonstrated in immortalized mouse distal convoluted tubule (MDCT) cells, chlorothiazide application induced a robust plasma membrane hyperpolarization, which increased Ca²⁺ uptake. This essential thiazide-induced hyperpolarization was prevented by the Cl⁻ channel inhibitor 5-Nitro-2-(3-phenylpropylamino) benzoic acid (NPPB), implicating NPPB-sensitive Cl⁻ channels, however the nature of these Cl⁻ channels has been rarely described in the literature. Here we show that MDCT cells express a dominant, outwardly rectifying Cl⁻ current at extracellular pH 7.4. This constitutive Cl⁻ current was more permeable to larger anions (Eisenman sequence I; I⁻ > Br⁻ ≥ Cl⁻) and was substantially inhibited by > 100 mM [Ca²⁺]_o, which distinguished it from ClC-K2/barttin. Moreover, the constitutive Cl⁻ current was blocked by NPPB, along with other Cl⁻ channel inhibitors (4,4′-diisothiocyanatostilbene-2,2′-disulfonate, DIDS; flufenamic acid, FFA). Subjecting the MDCT cells to an acidic extracellular solution (pH < 5.5) induced a substantially larger outwardly rectifying NPPB-sensitive Cl⁻ current. This acid-induced Cl⁻ current was also anion permeable (I⁻ > Br⁻ > Cl⁻), but was distinguished from the constitutive Cl⁻ current by its rectification characteristics, ion sensitivities, and response to FFA. In addition, we have identified similar outwardly rectifying and acid-sensitive currents in immortalized cells from the inner medullary collecting duct (mIMCD-3 cells). Expression of an acid-induced Cl⁻ current would be particularly relevant in the acidic IMCD (pH < 5.5). To our knowledge, the properties of these Cl⁻ currents are unique and provide the mechanisms to account for the Cl⁻ efflux previously speculated to be present in MDCT cells.     

Inhibition of the catalase reaction of Photosystem II by anions

A new binding site for anions which inhibit the water oxidizing complex (WOC) of Photosystem II in spinach has been identified. Anions which bind to this site inhibit the flash-induced S₂/S₀ catalase reaction (2H₂O₂2H₂O+O₂) of the WOC by displacing hydrogen peroxide. Using a mass spectrometer and gas permeable membrane to detect the ³²O₂ product, the yield and lifetime of the active state of the flash-induced catalase (to be referred to simply as flash-catalase) reaction were measured after forming the S₂ or S₀-states by a short flash. The increase in flash-catalase activity with H₂O₂ concentration exhibits a K_m=10–20 mM, and originates from an increase in the lifetime by 20-fold of the active state. The increased lifetime in the presence of peroxide is ascribed to formation of the long-lived S₀-state at the expense of the unstable S₂-state. The anion inhibition site differs from the chloride site involved in stimulating the photolytic water oxidation reaction (2H₂OO₂+4e^-+4H⁺). Whereas water oxidation requires Cl^- and is inhibited with increasing effectiveness by F^-CN^-N₃ ^-, the flash-catalase reaction is weakly inhibited by Cl^-, and with increasing effectiveness by F^-CN^-, N₃ ^-. Unlike water oxidation, chloride is unable to suppress or reverse inhibition of the flash-catalase reaction caused by these anions. The inhibitor effectiveness correlates with the pK_a of the conjugate acid, suggesting that the protonated species may be the active inhibitor. The reduced activity arises from a shortening of the lifetime of the flash-induced catalase active state by 3–10 fold owing to stronger anion binding in the flash-induced states, S₂ and S₀, than in the dark S-states, S₁ and S_-1. To account for the paradoxical result that higher anion concentrations are required to inhibit at lower H₂O₂ concentrations, where S₂ forms initially after the flash, than at higher H₂O₂ concentrations, where S₀ forms initially after the flash, stronger anion binding to the S₀-state than to the S₂-state is proposed. A kinetic model is given which accounts for these equilibria with anions and H₂O₂. The rate constant for the formation/release of O₂ by reduction of S₂ in the WOC is <0.4 s^-1.Abbreviations ADRY acceleration of the deactivation reactions of the water splitting enzyme system Y - BTP bis [tris(hydroxymethyl)methylamino]-propane - CCCP carbonylcyanide m-chlorophenylhyrazone - DCBQ 2,5-dichlorobenzoquinone - DMBQ 2,3-dimethylbenzoquinone - WOC water oxidizing complex     

Mechanistic and structural aspects of photosynthetic water oxidation

Conclusions on the functional and structural organisation of photosynthetic water oxidation are gathered from a critical survey of the wealth of data reported in the literature and author's own experimental research: (1) the water oxidising complex (WOC) contains a tetranuclear manganese cluster of dimer of dimers' structure and functional heterogeneity of the metal centers, (2) the four step univalent oxidative pathway leading to water oxidation into molecular oxygen and four protons comprises only manganese, tyrosine Y_Z of polypeptide Dl and the substrate as redox active species, (3) the redox transitions S₀→ S₁ and S₁→ S₂ are manganese centered whereas S₂→ S₃ is most likely a ligand-centered reaction, (4) there exist several lines of evidence for a marked structural change that accompanies the redox transition S₂→ S₃, (5) one Ca²⁺ is an indispensible constituent of a functionally competent WOC while the role of Cl is much less clear and a direct participation disputable, (6) substrate water is most likely bound in all redox states S₀,…,S₃ and exchangeable with the bulk phase. The protonation state is determined by the redox state S₁ and the protein microenvironment. A mechanism is proposed for water oxidation in the WOC that is based on three key postulates: (1) water oxidation takes place in the first coordination sphere of one manganese dimer [Mn_aMn_b]; (2) the essential O-O bond is preformed in S₃ as part of a rapid redox isomerism S₃(I)→S₃(II) where in S₃(II) a nuclear geometry and electronic configuration is attained that corresponds to a peroxidic-type species; and (3) S₃(II) is an ‘entatic state’ for the formation of complexed dioxygen triggered by Y_Z^OX induced electron abstraction from the WOC and electronic redistribution to S₀(O₂).     

Concerted involvement of cooperative proton–electron linkage and water production in the proton pump of cytochrome c oxidase

In cytochrome c oxidase, oxido-reductions of heme a/Cu_A and heme a₃/Cu_B are cooperatively linked to proton transfer at acid/base groups in the enzyme. H⁺/e⁻ cooperative linkage at Fe_a3/Cu_B is envisaged to be involved in proton pump mechanisms confined to the binuclear center. Models have also been proposed which involve a role in proton pumping of cooperative H⁺/e⁻ linkage at heme a (and Cu_A). Observations will be presented on: (i) proton consumption in the reduction of molecular oxygen to H₂O in soluble bovine heart cytochrome c oxidase; (ii) proton release/uptake associated with anaerobic oxidation/reduction of heme a/Cu_A and heme a₃/Cu_B in the soluble oxidase; (iii) H⁺ release in the external phase (i.e. H⁺ pumping) associated with the oxidative (R → O transition), reductive (O → R transition) and a full catalytic cycle (R → O → R transition) of membrane-reconstituted cytochrome c oxidase. A model is presented in which cooperative H⁺/e⁻ linkage at heme a/Cu_A and heme a₃/Cu_B with acid/base clusters, C₁ and C₂ respectively, and protonmotive steps of the reduction of O₂ to water are involved in proton pumping.     

Calcium regulated chloride permeabilities in primary cultures of rabbit colonocytes

To determine if calcium-dependent secretagogues directly act on epithelial cells to elicit CI⁻ secretion, their effects on CI⁻ transport and intracellular Ca²⁺ concentrations ([Ca²⁺]_i) were determined in primary cultures of rabbit distal colonic crypt cells. The Cl⁻ sensitive fluorescent probe, 6-methoxyquinolyl acetoethyl ester, MQAE and the Ca²⁺-sensitive fluorescent probe, fura-2AM were used to assess Cl⁻ transport and [Ca²⁺]_i, respectively. Basal Cl⁻ transport (0.274 ± 0.09 mM/sec) was inhibited significantly by the Cl⁻ channel blocker diphenylamine-2-carboxylate (DPC, 50 μM, 0.068 ± 0.02 mM/sec; P < 0.001) and the Na⁺/K⁺/2Cl⁻ cotransport inhibitor furosemide (1 μM, 0.137 ± 0.04 mM/sec; P < 0.01). Ion substitution studies using different halides revealed the basal influx to be I⁻ > F⁻ ≥ Cl⁻ > Br⁻. DPC inhibited I⁻ influx by ∼50%, F⁻ influx by 80%, Cl⁻ influx by 85%, and Br⁻ influx by 90%. Furosemide significantly inhibited influx of Br⁻ (84%) and Cl⁻ (81%) but not of F⁻ and I⁻. The effects of agents known to alter biological response by increasing [Ca²⁺]_i in other epithelial systems were used to stimulate Cl⁻ transport. Cl⁻ influx in mM/second was stimulated by 1 μM histamine (0.58 ± 0.05), 10 μM neurotensin (2.07 ± 0.32), 1 μM serotonin (1.63 ± 0.28), and 0.1 μM of the Ca²⁺ ionophore A23187 (2.05 ± 0.40). The Cl⁻ permeability stimulated by neurotensin, serotonin, and A23187 was partially blocked by DPC or furosemide added alone or in combination. Histamine-induced Cl⁻ influx was significantly inhibited by only furosemide. Indomethacin blocked histamine-stimulated Cl⁻ permeability but had no effect on the actions of the other agents. These studies, focusing on isolated colonocytes without the contribution of submucosal elements, reveal that (1) histamine stimulates Cl⁻ transport by activating the Na⁺/K⁺/2Cl⁻ cotransporter via a cyclooxygenase-dependent pathway; (2) neurotensin, serotonin, and A23187 activate both Cl⁻ channels and the cotransporter, and their actions are cyclooxygenase-independent. © 1996 Wiley-Liss, Inc.     

Substitution of chloride by bromide modifies the low-temperature tyrosine Z oxidation in active photosystem II

Chloride is an essential cofactor for photosynthetic water oxidation. However, its location and functional roles in active photosystem II are still a matter of debate. We have investigated this issue by studying the effects of Cl⁻ replacement by Br⁻ in active PSII. In Br⁻ substituted samples, Cl⁻ is effectively replaced by Br⁻ in the presence of 1.2 M NaBr under room light with protection of anaerobic atmosphere followed by dialysis. The following results have been obtained. i) The oxygen-evolving activities of the Br⁻-PSII samples are significantly lower than that of the Cl⁻-PSII samples; ii) The same S₂ multiline EPR signals are observed in both Br⁻ and Cl⁻-PSII samples; iii) The amplitudes of the visible light induced S₁Tyr_Z^• and S₂Tyr_Z^• EPR signals are significantly decreased after Br⁻ substitution; the S₁Tyr_Z^• EPR signal is up-shifted about 8 G, whereas the S₂Tyr_Z^• signal is down-shifted about 12 G after Br⁻ substitution. These results imply that the redox properties of Tyr_Z and spin interactions between Tyr_Z^• and Mn-cluster could be significantly modified due to Br⁻ substitution. It is suggested that Cl⁻/Br⁻ probably coordinates to the Ca²⁺ ion of the Mn-cluster in active photosystem II.     

Probing the proton release by Photosystem II in the S1 to S2 high-spin transition

The stoichiometry and kinetics of the proton release were investigated during each transition of the S-state cycle in Photosystem II (PSII) from Thermosynechococcus elongatus containing either a Mn₄CaO₅ (PSII/Ca) or a Mn₄SrO₅ (PSII/Sr) cluster. The measurements were done at pH 6.0 and pH 7.0 knowing that, in PSII/Ca at pH 6.0 and pH 7.0 and in PSII/Sr at pH 6.0, the flash-induced S₂-state is in a low-spin configuration (S₂^LS) whereas in PSII/Sr at pH 7.0, the S₂-state is in a high-spin configuration (S₂^HS) in half of the centers. Two measurements were done; the time-resolved flash dependent i) absorption of either bromocresol purple at pH 6.0 or neutral red at pH 7.0 and ii) electrochromism in the Soret band of P_D1 at 440 nm. The fittings of the oscillations with a period of four indicate that one proton is released in the S₁ to S₂^HS transition in PSII/Sr at pH 7.0. It has previously been suggested that the proton released in the S₂^LS to S₃ transition would be released in a S₂^LSTyr_Z^? → S₂^HSTyr_Z^? transition before the electron transfer from the cluster to Tyr_Z^? occurs. The release of a proton in the S₁Tyr_Z^? → S₂^HSTyr_Z transition would logically imply that this proton release is missing in the S₂^HSTyr_Z^? to S₃Tyr_Z transition. Instead, the proton release in the S₁ to S₂^HS transition in PSII/Sr at pH 7.0 was mainly done at the expense of the proton release in the S₃ to S₀ and S₀ to S₁ transitions. However, at pH 7.0, the electrochromism of P_D1 seems larger in PSII/Sr when compared to PSII/Ca in the S₃ state. This points to the complex link between proton movements in and immediately around the Mn₄ cluster and the mechanism leading to the release of protons into the bulk.     

Simultaneous functional expression of swelling and forskolin-activated chloride currents in primary cultures of rabbit distal convoluted tubule

Ionic Cl⁻ currents induced by cell swelling and forskolin were studied in primary cultures of rabbit distal convoluted tubule (DCTb) by the whole-cell patch clamp technique. We identified a Cl⁻ conductance activated by cell swelling with an hyperosmotic pipette solution. The initial current exhibited an outwardly rectifying I-V relationship, whereas steady state current showed strong decay at depolarized membrane potentials. The ion selectivity was I⁻ > Br⁻ > Cl⁻ > > glutamate. The forskolin-activated Cl⁻ conductance demonstrated a linear I-V relationship and its ion selectivity was Br⁻ > Cl⁻ > I⁻ > glutamate. This last conductance could be related to the CFTR (cystic fibrosis transmembrane conductance regulator) previously identified in these cells. NPPB inhibited both Cl⁻ currents, and DIDS inhibited only the swelling-activated Cl⁻ current. Forskolin had no effect on the activation of the swelling-activated Cl⁻ current. In DCTb cells which exhibited swelling-activated Cl⁻ currents subsequently inhibited by DIDS, forskolin could activate CFTR related Cl⁻ currents. In the continuous presence of I⁻ which inhibited CFTR conductance, forskolin did not modify the swelling-activated current. The results suggest that both Cl⁻ conductances could be co-expressed in the same DCTb cell and that CFTR did not modulate the swelling-activated conductance.     

Photoconsumption of molecular oxygen on both donor and acceptor sides of photosystem II in Mn-depleted subchloroplast membrane fragments

Oxygen consumption in Mn-depleted photosystem II (PSII) preparations under continuous and pulsed illumination is investigated. It is shown that removal of manganese from the water-oxidizing complex (WOC) by high pH treatment leads to a 6-fold increase in the rate of O₂ photoconsumption. The use of exogenous electron acceptors and donors to PSII shows that in Mn-depleted PSII preparations along with the well-known effect of O₂ photoreduction on the acceptor side of PSII, there is light-induced O₂ consumption on the donor side of PSII (nearly 30% and 70%, respectively). It is suggested that the light-induced O₂ uptake on the donor side of PSII is related to interaction of O₂ with radicals produced by photooxidation of organic molecules. The study of flash-induced O₂ uptake finds that removal of Mn from the WOC leads to O₂ photoconsumption with maximum in the first flash, and its yield is comparable with the yield of O₂ evolution on the third flash measured in the PSII samples before Mn removal. The flash-induced O₂ uptake is drastically (by a factor of 1.8) activated by catalytic concentration (5-10 μM, corresponding to 2-4 Mn per RC) of Mn²⁺, while at higher concentrations (> 100 μM) Mn²⁺ inhibits the O₂ photoconsumption (like other electron donors: ferrocyanide and diphenylcarbazide). Inhibitory pre-illumination of the Mn-depleted PSII preparations (resulting in the loss of electron donation from Mn²⁺) leads to both suppression of flash-induced O₂ uptake and disappearance of the Mn-induced activation of the O₂ photoconsumption. We assume that the light-induced O₂ uptake in Mn-depleted PSII preparations may reflect not only the negative processes leading to photoinhibition but also possible participation of O₂ or its reactive forms in the formation of the inorganic core of the WOC.     

Oxidative stress caused by pyocyanin impairs CFTR Cl− transport in human bronchial epithelial cells

Pyocyanin (N-methyl-1-hydroxyphenazine), a redox-active virulence factor produced by the human pathogen Pseudomonas aeruginosa, is known to compromise mucociliary clearance. Exposure of human bronchial epithelial cells to pyocyanin increased the rate of cellular release of H₂O₂ threefold above the endogenous H₂O₂ production. Real-time measurements of the redox potential of the cytosolic compartment using the redox sensor roGFP1 showed that pyocyanin (100 μM) oxidized the cytosol from a resting value of − 318 ± 5 mV by 48.0 ± 4.6 mV within 2 h; a comparable oxidation was induced by 100 μM H₂O₂. Whereas resting Cl⁻ secretion was slightly activated by pyocyanin (to 10% of maximal currents), forskolin-stimulated Cl⁻ secretion was inhibited by 86%. The decline was linearly related to the cytosolic redox potential (1.8% inhibition/mV oxidation). Cystic fibrosis bronchial epithelial cells homozygous for ΔF508 CFTR failed to secrete Cl⁻ in response to pyocyanin or H₂O₂, indicating that these oxidants specifically target the CFTR and not other Cl⁻ conductances. Treatment with pyocyanin also decreased total cellular glutathione levels to 62% and cellular ATP levels to 46% after 24 h. We conclude that pyocyanin is a key factor that redox cycles in the cytosol, generates H₂O₂, depletes glutathione and ATP, and impairs CFTR function in Pseudomonas-infected lungs.     

Oxidative photosynthetic water splitting: energetics,kinetics and mechanism

This minireview is an attempt to summarize our current knowledge on oxidative water splitting in photosynthesis. Based on the extended Kok model (Kok, Forbush, McGloin (1970) Photochem Photobiol 11:457–476) as a framework, the energetics and kinetics of two different types of reactions comprising the overall process are discussed: (i) P680^+• reduction by the redox active tyrosine Y_Z of polypeptide D1 and (ii) Y_z^ox induced oxidation of the four step sequence in the water oxidizing complex (WOC) leading to the formation of molecular oxygen. The mode of coupling between electron transport (ET) and proton transfer (PT) is of key mechanistic relevance for the redox turnover of Y_Z and the reactions within the WOC. The peculiar energetics of the oxidation steps in the WOC assure that redox state S₁ is thermodynamically most stable. This is a general feature in all oxygen evolving photosynthetic organisms and assumed to be of physiological relevance. The reaction coordinate of oxidative water splitting is discussed on the basis of the available information about the Gibbs energy differences between the individual redox states S _i+1 and S _i and the data reported for the activation energies of the individual oxidation steps in the WOC. Finally, an attempt is made to cast our current state of knowledge into a mechanism of oxidative water splitting with special emphasis on the formation of the essential O–O bond and on the active role of the protein in tuning the local proton activity that depends on time and redox state S _i . The O–O linkage is assumed to take place at the level of a complexed peroxide.     

Interactions between permeant and blocking anions inside the CFTR chloride channel pore

Binding of cytoplasmic anionic open channel blockers within the cystic fibrosis transmembrane conductance regulator (CFTR) Cl⁻ channel is antagonized by extracellular Cl⁻. In the present work, patch clamp recording was used to investigate the interaction between extracellular Cl⁻ (and other anions) and cytoplasmic Pt(NO₂)₄^2 − ions inside the CFTR channel pore. In constitutively open (E1371Q-CFTR) channels, these different anions bind to two separate sites, located in the outer and inner vestibules of the pore respectively, in a mutually antagonistic fashion. A mutation in the inner vestibule (I344K) that greatly increased Pt(NO₂)₄^2 − binding affinity also greatly strengthened antagonistic Cl⁻:blocker interactions as well as the voltage-dependence of block. Quantitative analysis of ion binding affinity suggested that the I344K mutation strengthened interactions not only with intracellular Pt(NO₂)₄^2 − ions but also with extracellular Cl⁻, and that altered blocker Cl⁻- and voltage-dependence were due to the introduction of a novel type of antagonistic ion:ion interaction inside the pore that was independent of Cl⁻ binding in the outer vestibule. It is proposed that this mutation alters the arrangement of anion binding sites inside the pore, allowing both Cl⁻ and Pt(NO₂)₄^2 − to bind concurrently within the inner vestibule in a strongly mutually antagonistic fashion. However, the I344K mutation does not increase single channel conductance following disruption of Cl⁻ binding in the outer vestibule in R334Q channels. Implications for the arrangement of ion binding sites in the pore, and their functional consequences for blocker binding and for rapid Cl⁻ permeation, are discussed.     

The AQP-3 water channel is a pivotal modulator of glycerol-induced chloride channel activation in nasopharyngeal carcinoma cells

Aquaporin (AQP) and chloride channels are ubiquitous in virtually all living cells, playing pivotal roles in cell proliferation, migration and apoptosis. We previously reported that AQP-3 aquaglyceroporin and ClC-3 chloride channels could form complexes to regulate cell volume in nasopharyngeal carcinoma cells. In this study, the roles of AQP-3 in their hetero-complexes were further investigated. Glycerol entered the cells via AQP-3 and induced two different Cl⁻ currents through cell swelling-dependent or -independent pathways. The swelling-dependent Cl⁻ current was significantly inhibited by pretreatment with CuCl₂ and AQP-3-siRNA. After siRNA-induced AQP-3 knock-down, the 140 mM glycerol isoosmotic solution swelled cells by 22% (45% in AQP-3-intact cells) and induced a smaller Cl⁻ current; this current was smaller than that activated by 8% cell volume swelling, which induced by the 140 mM glycerol hyperosmotic solution in AQP-3-intact cells. This suggests that the interaction between AQP-3 and ClC-3 plays an important role in cell volume regulation and that AQP-3 may be a modulator that opens volume-regulated chloride channels. The swelling-independent Cl⁻ current, which was activated by extracellular glycerol, was reduced by CuCl₂ and AQP-3-siRNA pretreatment. Dialyzing glycerol into cells via the pipette directly induced the swelling-independent Cl⁻ current; however this current was blocked by AQP-3 down-regulation, suggesting AQP-3 is essential for the opening of chloride channels. In conclusion, AQP-3 is the pathway for water, glycerol and other small solutes to enter cells, and it may be an essential modulator for the gating of chloride channels.     

Natural Variants of Photosystem II Subunit D1 Tune Photochemical Fitness to Solar Intensity

Photosystem II (PSII) is composed of six core polypeptides that make up the minimal unit capable of performing the primary photochemistry of light-driven charge separation and water oxidation in all oxygenic phototrophs. The D1 subunit of this complex contains most of the ligating amino acid residues for the Mn₄CaO₅ core of the water-oxidizing complex (WOC). Most cyanobacteria have 3–5 copies of the psbA gene coding for at least two isoforms of D1, whereas algae and plants have only one isoform. Synechococcus elongatus PCC 7942 contains two D1 isoforms; D1:1 is expressed under low light conditions, and D1:2 is up-regulated in high light or stress conditions. Using a heterologous psbA expression system in the green alga Chlamydomonas reinhardtii, we have measured growth rate, WOC cycle efficiency, and O₂ yield as a function of D1:1, D1:2, or the native algal D1 isoform. D1:1-PSII cells outcompete D1:2-PSII cells and accumulate more biomass in light-limiting conditions. However, D1:2-PSII cells easily outcompete D1:1-PSII cells at high light intensities. The native C. reinhardtii-PSII WOC cycles less efficiently at all light intensities and produces less O₂ than either cyanobacterial D1 isoform. D1:2-PSII makes more O₂ per saturating flash than D1:1-PSII, but it exhibits lower WOC cycling efficiency at low light intensities due to a 40% faster charge recombination rate in the S₃ state. These functional advantages of D1:1-PSII and D1:2-PSII at low and high light regimes, respectively, can be explained by differences in predicted redox potentials of PSII electron acceptors that control kinetic performance.     

Effect of bicarbonate on the water-oxidizing complex of photosystem II in the super-reduced S-states

It is shown that the hydrazine-induced transition of the water-oxidizing complex (WOC) to super-reduced S-states depends on the presence of bicarbonate in the medium so that after a 20 min treatment of isolated spinach thylakoids with 3 mM NH₂NH₂ at 20 °C in the CO₂/HCO₃⁻-depleted buffer the S-state populations are: 42% of S₋₃, 42% of S₋₂, 16% of S₋₁ and even formal S₋₄ state is reached, while in the presence of 2 mM NaHCO₃, the same treatment produces 30% of S₋₃, 38% of S₋₂, and 32% of S₋₁ and there is no indication of the S₋₄ state. Bicarbonate requirement for the oxygen-evolving activity, very low in untreated thylakoids, considerably increases upon the transition of the WOC to the super-reduced S-states, and the requirement becomes low again when the WOC returns back to the normal S-states using pre-illumination. The results are discussed as a possible indication of ligation of bicarbonate to manganese ions within the WOC.     

Function of plastoquinone in heat stress reactions of plants

The effect of high temperature treatment (40 °C, 3 h, illumination at 100 μmol m^− 2 s^− 1) on the photosynthetic electron flow in barley seedlings of different age was investigated. Thermoinduced inhibition of the liner electron flow due to partial impairment of the water oxidizing complex (WOC) and the increase in the extent of Q_A⁻ reoxidation by Tyr_z^ox in thylakoids isolated from 4-day-old leaves was shown by measurements of oxygen evolution using benzoquinone or potassium ferricyanide as electron acceptors, as well as by following Q_A⁻ reoxidation kinetics in the absence and presence of exogenous electron acceptors, DCBQ and DMBQ. Using HPLC analysis, an increase in the oxidation of the photoactive plastoquinone pool in young leaves under heating was shown. In older, 11-day-old leaves, heat treatment limited both photosynthetic electron flow and oxygen evolution. The same effects of heat shock on oxygen evolution caused an inhibition of electron flow on the donor side of PSII only. However, a rise in the proportion of PSII with Q_A⁻ reoxidized through recombination with the S₂/S₃ state of the WOC was observed. The addition of exogenous electron acceptors (DCBQ and DMBQ) and a donor (DPC) showed that the thermoinduced decrease in the electron transport rate was caused by an impediment of electron flow from Q_A⁻ to acceptor pool. The decrease in size of the photoactive PQ-pool and a change in the proportions of oxidized and reduced PQ in older leaves under heat treatment were shown. It was suggested that a thermoinduced change of the redox state of the PQ-pool and a redistribution of plastoquinone molecules between photoactive and non-photoactive pools are the mechanisms which reflect and regulate the response of the photosynthetic apparatus under heat stress conditions.     

Desiccation tolerant lichens facilitate in vivo H/D isotope effect measurements in oxygenic photosynthesis

We have used the desiccation-tolerant lichen Flavoparmelia caperata, containing the green algal photobiont Trebouxia gelatinosa, to examine H/D isotope effects in Photosystem II in vivo. Artifact-free H/D isotope effects on both PSII primary charge separation and water oxidation yields were determined as a function of flash rate from chlorophyll-a variable fluorescence yields. Intact lichens could be reversibly dehydrated/re-hydrated with H₂O/D₂O repeatedly without loss of O₂ evolution, unlike all isolated PSII preparations. Above a threshold flash rate, PSII charge separation decreases sharply in both D₂O and H₂O, reflecting loss of excitation migration and capture by PSII. Changes in H/D coordinates further slow charge separation in D₂O (?23% at 120?Hz), attributed to reoxidation of the primary acceptor Q_A^?. At intermediate flash rates (5–50?Hz) D₂O decreases water oxidation efficiency (O₂ evolution) by ?2–5%. No significant isotopic difference is observed at slow flash rates (<5?Hz) where charge recombination dominates. Slower D₂O diffusion, changes in hydrogen bonding networks, and shifts in the pK_a's of ionizable residues may all contribute to these systematic variations of H/D isotope effects. Lichens' reversible desiccation tolerance allows highly reproducible H/D exchange kinetics in PSII reactions to be studied in vivo for the first time.