Natural isoforms of the Photosystem II D1 subunit differ in photoassembly efficiency of the water-oxidizing complex

Oxygenic photosynthesis efficiency at increasing solar flux is limited by light-induced damage (photoinhibition) of Photosystem II (PSII), primarily targeting the D1 reaction center subunit. Some cyanobacteria contain two natural isoforms of D1 that function better under low light (D1:1) or high light (D1:2). Herein, rates and yields of photoassembly of the Mn4CaO5 water-oxidizing complex (WOC) from the free inorganic cofactors (Mn(2+), Ca(2+), water, electron acceptor) and apo-WOC-PSII are shown to differ significantly: D1:1 apo-WOC-PSII exhibits a 2.3-fold faster rate-limiting step of photoassembly and up to seven-fold faster rate to the first light-stable Mn(3+) intermediate, IM1*, but with a much higher rate of photoinhibition than D1:2. Conversely, D1:2 apo-WOC-PSII assembles slower but has up to seven-fold higher yield, achieved by a higher quantum yield of charge separation and slower photoinhibition rate. These results confirm and extend previous observations of the two holoenzymes: D1:2-PSII has a greater quantum yield of primary charge separation, faster [P680 (+) Q A (-) ] charge recombination and less photoinhibition that results in a slower rate and higher yield of photoassembly of its apo-WOC-PSII complex. In contrast, D1:1-PSII has a lower quantum yield of primary charge separation, a slower [P680 (+) Q A (-) ] charge recombination rate, and faster photoinhibition that together result in higher rate but lower yield of photoassembly at higher light intensities. Cyanobacterial PSII reaction centers that contain the high- and low-light D1 isoforms can tailor performance to optimize photosynthesis at varying light conditions, with similar consequences on their photoassembly kinetics and yield. These different efficiencies of photoassembly versus photoinhibition impose differential costs for biosynthesis as a function of light intensity.

Inactivation of nitrate reductase alters metabolic branching of carbohydrate fermentation in the cyanobacterium Synechococcus sp. strain PCC 7002

To produce cellular energy, cyanobacteria reduce nitrate as the preferred pathway over proton reduction (H2 evolution) by catabolizing glycogen under dark anaerobic conditions. This competition lowers H2 production by consuming a large fraction of the reducing equivalents (NADPH and NADH). To eliminate this competition, we constructed a knockout mutant of nitrate reductase, encoded by narB, in Synechococcus sp. PCC 7002. As expected, ΔnarB was able to take up intracellular nitrate but was unable to reduce it to nitrite or ammonia, and was unable to grow photoautotrophically on nitrate. During photoautotrophic growth on urea, ΔnarB significantly redirects biomass accumulation into glycogen at the expense of protein accumulation. During subsequent dark fermentation, metabolite concentrations--both the adenylate cellular energy charge (∼ATP) and the redox poise (NAD(P)H/NAD(P))--were independent of nitrate availability in ΔnarB, in contrast to the wild type (WT) control. The ΔnarB strain diverted more reducing equivalents from glycogen catabolism into reduced products, mainly H2 and d-lactate, by 6-fold (2.8% yield) and 2-fold (82.3% yield), respectively, than WT. Continuous removal of H2 from the fermentation medium (milking) further boosted net H2 production by 7-fold in ΔnarB, at the expense of less excreted lactate, resulting in a 49-fold combined increase in the net H2 evolution rate during 2 days of fermentation compared to the WT. The absence of nitrate reductase eliminated the inductive effect of nitrate addition on rerouting carbohydrate catabolism from glycolysis to the oxidative pentose phosphate (OPP) pathway, indicating that intracellular redox poise and not nitrate itself acts as the control switch for carbon flux branching between pathways.

Engineered Photosystem II reaction centers optimize photochemistry versus photoprotection at different solar intensities

The D1 protein of Photosystem II (PSII) provides most of the ligating amino acid residues for the Mn4CaO5 water-oxidizing complex (WOC) and half of the reaction center cofactors, and it is present as two isoforms in the cyanobacterium Synechococcus elongatus PCC 7942. These isoforms, D1:1 and D1:2, confer functional advantages for photosynthetic growth at low and high light intensities, respectively. D1:1, D1:2, and seven point mutations in the D1:2 background that are native to D1:1 were expressed in the green alga Chlamydomonas reinhardtii. We used these nine strains to show that those strains that confer a higher yield of PSII charge separation under light-limiting conditions (where charge recombination is significant) have less efficient photochemical turnover, measured in terms of both a lower WOC turnover probability and a longer WOC cycle period. Conversely, these same strains under light saturation (where charge recombination does not compete) confer a correspondingly faster O2 evolution rate and greater protection against photoinhibition. Taken together, the data clearly establish that PSII primary charge separation is a trade-off between photochemical productivity (water oxidation and plastoquinone reduction) and charge recombination (photoprotection). These trade-offs add up to a significant growth advantage for the two natural isoforms. These insights provide fundamental design principles for engineering of PSII reaction centers with optimal photochemical efficiencies for growth at low versus high light intensities.

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 Mn(4)CaO(5) 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 O(2) 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 O(2) than either cyanobacterial D1 isoform. D1:2-PSII makes more O(2) 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 S(3) 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.

Young research investigators honored at the 2012 Gordon Research Conference on photosynthesis

We provide a News Report on the 2012 Gordon Research Conference on Photosynthesis held at Davidson College, North Carolina during July 8-13 that focuses on four young investigators who were presented awards during the conference.

Enhancing biological hydrogen production from cyanobacteria by removal of excreted products

Hydrogen is produced by a [NiFe]-hydrogenase in the cyanobacterium Arthrospira (Spirulina) maxima during autofermentation of photosynthetically accumulated glycogen under dark anaerobic conditions. Herein we show that elimination of H₂ backpressure by continuous H₂ removal ("milking") can significantly increase the yield of H₂ in this strain. We show that "milking" by continuous selective consumption of H₂ using an electrochemical cell produces the maximum increase in H₂ yield (11-fold) and H₂ rate (3.4-fold), which is considerably larger than through "milking" by non-selective dilution of the biomass in media (increases H₂ yield 3.7-fold and rate 3.1-fold). Exhaustive autofermentation under electrochemical milking conditions consumes >98% of glycogen and 27.6% of biomass over 7-8 days and extracts 39% of the energy content in glycogen as H₂. Non-selective dilution stimulates H₂ production by shifting intracellular equilibria competing for NADH from excreted products and terminal electron sinks into H₂ production. Adding a mixture of the carbon fermentative products shifts the equilibria towards reactants, resulting in increased intracellular NADH and an increased H₂ yield (1.4-fold). H₂ production is sustained for a period of time up to 7days, after which the PSII activity of the cells decreases by 80-90%, but can be restored by regeneration under photoautotrophic growth.

Metabolic pathways for photobiological hydrogen production by nitrogenase- and hydrogenase-containing unicellular cyanobacteria Cyanothece

Current biotechnological interest in nitrogen-fixing cyanobacteria stems from their robust respiration and capacity to produce hydrogen. Here we quantify both dark- and light-induced H(2) effluxes by Cyanothece sp. Miami BG 043511 and establish their respective origins. Dark, anoxic H(2) production occurs via hydrogenase utilizing reductant from glycolytic catabolism of carbohydrates (autofermentation). Photo-H(2) is shown to occur via nitrogenase and requires illumination of PSI, whereas production of O(2) by co-illumination of PSII is inhibitory to nitrogenase above a threshold pO(2). Carbohydrate also serves as the major source of reductant for the PSI pathway mediated via nonphotochemical reduction of the plastoquinone pool by NADH dehydrogenases type-1 and type-2 (NDH-1 and NDH-2). Redirection of this reductant flux exclusively through the proton-coupled NDH-1 by inhibition of NDH-2 with flavone increases the photo-H(2) production rate by 2-fold (at the expense of the dark-H(2) rate), due to production of additional ATP (via the proton gradient). Comparison of photobiological hydrogen rates, yields, and energy conversion efficiencies reveals opportunities for improvement.

Calcium controls the assembly of the photosynthetic water-oxidizing complex: a cadmium(II) inorganic mutant of the Mn4Ca core

Perturbation of the catalytic inorganic core (Mn4Ca1OxCly) of the photosystem II-water-oxidizing complex (PSII-WOC) isolated from spinach is examined by substitution of Ca2+ with cadmium(II) during core assembly. Cd2+ inhibits the yield of reconstitution of O2-evolution activity, called photoactivation, starting from the free inorganic cofactors and the cofactor-depleted apo-WOC-PSII complex. Ca2+ affinity increases following photooxidation of the first Mn2+ to Mn3+ bound to the 'high-affinity' site. Ca2+ binding occurs in the dark and is the slowest overall step of photoactivation (IM1-->IM1* step). Cd2+ competitively blocks the binding of Ca2+ to its functional site with 10- to 30-fold higher affinity, but does not influence the binding of Mn2+ to its high-affinity site. By contrast, even 10-fold higher concentrations of Cd2+ have no effect on O2-evolution activity in intact PSII-WOC. Paradoxically, Cd2+ both inhibits photoactivation yield, while accelerating the rate of photoassembly of active centres 10-fold relative to Ca2+. Cd2+ increases the kinetic stability of the photooxidized Mn3+ assembly intermediate(s) by twofold (mean lifetime for dark decay). The rate data provide evidence that Cd2+ binding following photooxidation of the first Mn3+, IM1-->IM1*, causes three outcomes: (i) a longer intermediate lifetime that slows IM1 decay to IM0 by charge recombination, (ii) 10-fold higher probability of attaining the degrees of freedom (either or both cofactor and protein d.f.) needed to bind and photooxidize the remaining 3 Mn2+ that form the functional cluster, and (iii) increased lability of Cd2+ following Mn4 cluster assembly results in (re)exchange of Cd2+ by Ca2+ which restores active O2-evolving centres. Prior EPR spectroscopic data provide evidence for an oxo-bridged assembly intermediate, Mn3+(mu-O2(-))Ca2+, for IM1*. We postulate an analogous inhibited intermediate with Cd2+ replacing Ca2+.

Photoassembly of the Water-Oxidizing Complex in Photosystem II

The light-driven steps in the biogenesis and repair of the inorganic core comprising the O(2)-evolving center of oxygenic photosynthesis (photosystem II water-oxidation complex, PSII-WOC) are reviewed. These steps, known collectively as photoactivation, involve the photoassembly of the free inorganic cofactors to the cofactor-depleted PSII-(apo-WOC) driven by light and produce the active O(2)-evolving core comprised of Mn(4)CaO(x)Cl(y). We focus on the functional role of the inorganic components as seen through the competition with non-native cofactors ("inorganic mutants") on water oxidation activity, the rate of the photoassembly reaction, and on structural insights gained from EPR spectroscopy of trapped intermediates formed in the initial steps of the assembly reaction. A chemical mechanism for the initial steps in photoactivation is given that is based on these data. Photoactivation experiments offer the powerful insights gained from replacement of the native cofactors, which together with the recent X-ray structural data for the resting holoenzyme provide a deeper understanding of the chemistry of water oxidation. We also review some new directions in research that photoactivation studies have inspired that look at the evolutionary history of this remarkable catalyst.

Bicarbonate Is a Native Cofactor for Assembly of the Manganese Cluster of the Photosynthetic Water Oxidizing Complex. Kinetics of Reconstitution of O2 Evolution by Photoactivation,

Assembly of the inorganic core (Mn(4)O(x)Ca(1)Cl(y)) of the water oxidizing enzyme of oxygenic photosynthesis generates O(2) evolution capacity via the photodriven binding and photooxidation of the free inorganic cofactors within the cofactor-depleted enzyme (apo-WOC-PSII) by a process called photoactivation. Using in vitro photoactivation of spinach PSII membranes, we identify a new lower affinity site for bicarbonate interaction in the WOC. Bicarbonate addition causes a 300% stimulation of the rate and a 50% increase in yield of photoassembled PSII centers when using Mn(2+) and Ca(2+) concentrations that are 10-50-fold larger range than previously examined. Maintenance of a fixed Mn(2+)/Ca(2+) ratio (1:500) produces the fastest rates and highest yields of photoactivation, which has implications for intracellular cofactor homeostasis. A two-step (biexponential) model is shown to accurately fit the assembly kinetics over a 200-fold range of Mn(2+) concentrations. The first step, the binding and photooxidation of Mn(2+) to Mn(3+), is specifically stimulated via formation of a ternary complex between Mn(2+), bicarbonate, and apo-WOC-PSII, having a proposed stoichiometry of [Mn(2+)(HCO(3)(-))]. This low-affinity bicarbonate complex is thermodynamically easier to oxidize than the aqua precursor, [Mn(2+)(OH(2))]. The photooxidized intermediate, [Mn(3+)(HCO(3)(-))], is longer lived and increases the photoactivation yield by suppressing irreversible photodamage to the cofactor-free apo-WOC-PSII (photoinhibition). Bicarbonate does not affect the second (rate-limiting) dark step of photoactivation, attributed to a protein conformational change. Together with the previously characterized high-affinity site, these results reveal that bicarbonate is a multifunctional "native" cofactor important for photoactivation and photoprotection of the WOC-PSII complex.

A functional role for tyrosine-D in assembly of the inorganic core of the water oxidase complex of photosystem II and the kinetics of water oxidation

The role of D2-Tyr160 (Y(D)), a photooxidizable residue in the D2 reaction center polypeptide of photosystem II (PSII), was investigated in both wild type and a mutant strain (D2-Tyr160Phe) in which phenylalanine replaces Y(D) in the cyanobacterium Synechocystis sp. (strain PCC 6803). Y(D) is the symmetry-related tyrosine that is homologous to the essential photoactive Tyr161(Y(Z)) of the D1 polypeptide of PSII. We compared the flash-induced yield of O(2) in intact, functional PSII centers from both wild-type and mutant PSII core complexes. The yield of O(2) in the intact holo-enzyme was found to be identical in the mutant and wild-type PSII cores using long (saturating) pulses or continuous illumination, but was observed to be appreciably reduced in the mutant using short (nonsaturating) light pulses (<50 ms). We also compared the rates of the first two kinetically resolved steps of photoactivation. Photoactivation is the assembly process for binding of the inorganic cofactors to the apo-water oxidation/PSII complex (apo-WOC-PSII) and their light-induced photooxidation to form the functional Mn(4)Ca(1)Cl(x)() core required for O(2) evolution. We show that the D2-Tyr160Phe mutant cores can assemble a functional WOC from the free inorganic cofactors, but at a much slower rate and with reduced quantum efficiency vs wild-type PSII cores. Both of these observations imply that the presence of Y(D)(*) leads to a more efficient photooxidation of the Mn cluster relative to deactivation (reductive processes). One possible explanation for this behavior is that the phenolic proton on Y(D) is retained within the reaction center following Y(D) oxidation. The positive charge, likely shared by D2-His189 and other residues, raises the reduction potential of P(680)(+)/P(680), thereby increasing the driving force for the oxidation of Mn(4)Y(Z). There is, therefore, a competitive advantage to organisms that retain the Y(D) residue, possibly explaining its retention in all sequences of psbD (encoding the D2 polypeptide) known to date. We also find that the sequence of metal binding steps during assembly of apo-WOC-PSII centers in cyanobacteria cores differs from that in higher plants. This is seen by a reduced calcium affinity at its effector site and reduced competition for binding to the Mn(II) site, resulting in acceleration of the initial lagtime by Ca(2+), in contrast to retardation in spinach. Ca(2+) binding to its effector site promotes the stability of the photointermediates (IM1 and above) by suppressing unproductive decay.

The inorganic biochemistry of photosynthetic oxygen evolution/water oxidation

At the request of the organizer of this special edition, we have attempted to do several things in this manuscript: (1) we present a mini-review of recent, selected, works on the light-induced inorganic biogenesis (photoactivation), composition and structure of the inorganic core responsible for photosynthetic water oxidation; (2) we summarize a new proposal for the evolutionary origin of the water oxidation catalyst which postulates a key role for bicarbonate in formation of the inorganic core; (3) we summarize published studies and present new results on what has been learned from studies of 'inorganic mutants' in which the endogenous cofactors (Mn(n+), Ca2+, Cl-) are substituted; (4) the first DeltapH changes measured during the photoactivation process are reported and used to develop a model for the stepwise photo-assembly process; (5) a comparative analysis is given of data in the literature on the kinetics of substrate water exchange and peroxide binding/dismutation which support a mechanistic model for water oxidation in general; (6) we discuss alternative interpretations of data in the literature with a view to forecast new avenues where progress is needed.

Bicarbonate accelerates assembly of the inorganic core of the water-oxidizing complex in manganese-depleted photosystem II: a proposed biogeochemical role for atmospheric carbon dioxide in oxygenic photosynthesis

The proposed role for bicarbonate (HCO(3)(-)) as an intrinsic cofactor within the water-oxidizing complex (WOC) of photosystem II (PSII) [Klimov et al. (1997) Biochemistry 36, 16277-16281] was tested by investigation of its influence on the kinetics and yield of photoactivation, the light-induced assembly of the functional inorganic core (Mn(4)O(y)Ca(1)Cl(x)) starting from the cofactor-depleted apo-WOC-PSII center and free Mn(2+), Ca(2+), and Cl(-). Two binding sites for bicarbonate were found that stimulate photoactivation by accelerating the formation and suppressing the decay, respectively, of the first light-induced assembly intermediate, IM(1) [apo-WOC-Mn(OH)(2)(+)]. A high-affinity bicarbonate site (K(D) </= 10 microM) stimulates both the rate of recovery of O(2) evolving centers and decreases (by a factor of 1.2-3) t(lag), the time for formation of IM(1). This stimulation involves enhanced binding of the initial Mn(2+) and occurs only at concentrations of Mn(2+) at or below the stoichiometric requirements for water oxidation (</=4 Mn/PSII) and disappears above 4 Mn/PSII. The absence of an effect from added bicarbonate on photoactivation kinetics and yield at saturating concentrations of Mn(2+) and Ca(2+) may be due to the availability of atmospheric bicarbonate dissolved in the buffers (approximately 4 microM at pH 6.0) sufficient for photoactivation. The second bicarbonate site also stimulates the rate of formation of IM(1) but has much lower affinity (K(D) approximately millimolar) and becomes observable only at low concentrations of Ca(2+) that are limiting for photoactivation. This stimulation effect appears to occur by complexation of free Ca(2+), thereby reducing its activity in competing with Mn(2+) in the formation of IM(1). Bicarbonate had no effect on the calcium effector site responsible for the rate-limiting dark step of photoactivation (Ca(2+) binding to IM(1)). Four interpretations of the high-affinity bicarbonate effect may be advanced as testable hypotheses: bicarbonate may (1) act as an integral cofactor within the WOC (possible ligand to the first Mn), (2) act as a Bronsted base to accelerate proton release during formation of either the dark precursor [apo-WOC-Mn(OH)(+)] or IM(1) [apo-WOC-Mn(OH)(2)(+)], (3) directly deliver one or more hydroxide ions during formation of the latter two species (with release of CO(2)), or (4) act as a membrane-soluble anion that electrostatically elevates the local concentration of Mn(2+) in PSII. These results support a possible biogeochemical role for bicarbonate in the evolution of the first oxygenic photosynthetic organism. An improvement in the illumination method for photoactivation is presented in which light flashes of increasing duration are used to extend the pre-steady-state lag phase and to suppress photoinhibition, thereby improving the accuracy of t(lag) determination.

Remarkable affinity and selectivity for Cs+ and uranyl (UO22+) binding to the manganese site of the apo-water oxidation complex of photosystem II

The size and charge density requirements for metal ion binding to the high-affinity Mn2+ site of the apo-water oxidizing complex (WOC) of spinach photosystem II (PSII) were studied by comparing the relative binding affinities of alkali metal cations, divalent metals (Mg2+, Ca2+, Mn2+, Sr2+), and the oxo-cation UO22+. Cation binding to the apo-WOC-PSII protein was measured by: (1) inhibition of the rate and yield of photoactivation, the light-induced recovery of O2 evolution by assembly of the functional Mn4Ca1Clx, core from its constituent inorganic cofactors (Mn2+, Ca2+, and Cl-); and by (2) inhibition of the PSII-mediated light-induced electron transfer from Mn2+ to an electron acceptor (DCIP). Together, these methods enable discrimination between inhibition at the high- and low-affinity Mn2+ sites and the Ca2+ site of the apo-WOC-PSII. Unexpectedly strong binding of large alkali cations (Cs+ >> Rb+ > K+ > Na+ > Li+) was found to smoothly correlate with decreasing cation charge density, exhibiting one of the largest Cs+/Li+ selectivities (>/=5000) for any known chelator. Both photoactivation and electron-transfer measurements at selected Mn2+ and Ca2+ concentrations reveal that Cs+ binds to the high-affinity Mn2+ site with a slightly greater affinity (2-3-fold at pH 6.0) than Mn2+, while binding about 10(4)-fold more weakly to the Ca2+-specific site required for reassembly of functional O2 evolving centers. In contrast to Cs+, divalent cations larger than Mn2+ bind considerably more weakly to the high-affinity Mn2+ site (Mn2+ >> Ca2+ > Sr2+). Their affinities correlate with the hydrolysis constant for formation of the metal hydroxide by hydrolysis of water: Me2+aq --> [MeOH]+aq + H+aq. Along with the strong stimulation of the rate of photoactivation by alkaline pH, these metal cation trends support the interpretation that [MnOH]+ is the active species that forms upon binding of Mn2+aq to apo-WOC. Further support for this interpretation is found by the unusually strong inhibition of Mn2+ photooxidation by the linear uranyl cation (UO22+). The intrinsic binding constant for [MnOH]+ to apo-WOC was determined using a thermodynamic cycle to be K = 4.0 x 10(15) M-1 (at pH 6.0), consistent with a high-affinity, preorganized, multidentate coordination site. We propose that the selectivity for binding [MnOH]+, a linear low charge-density monocation, vs symmetrical Me2+ dications is functionally important for assembly of the WOC by enabling: (1) discrimination against higher charge density alkaline earth cations (Mg2+ and Ca2+) and smaller alkali metal cations (Na+ and K+) that are present in considerably greater abundance in vivo, and thus would suppress photoactivation; and (2) higher affinity binding of the one Ca2+ ion or the remaining three Mn2+ ions via coordination to form mu-hydroxo-bridged intermediates, apo-WOC-[Mn(mu-OH)2Mn]3+ or apo-WOC-[Mn(mu-OH)Ca]3+, during subsequent assembly steps of the native Mn4Ca1Clx core. In contrast to more acidic Me2+ divalent ion inhibitors of the high-affinity Mn2+ site, like Ca2+ and Sr2+, Cs+ does not accelerate the decay of the first light-induced intermediate, IM1, formed during photoactivation (attributed to apo-WOC-[Mn(OH)2]+). The inability of Cs+ to promote decay of IM1, despite having comparable affinity as Mn2+, is consistent with its considerably weaker Lewis acidity, resulting in the reprotonation of IM1 by water becoming the rate-limiting step for decay prior to displacement of Mn2+. All four different lines of evidence provide a self-consistent picture indicating that the initial step in assembly of the WOC involves high-affinity binding of [MnOH]+.

Calcium induces binding and formation of a spin-coupled dimanganese(II,II) center in the apo-water oxidation complex of photosystem II as precursor to the functional tetra-Mn/Ca cluster

Two new intermediates are described which form in the dark as precursors to the light-induced assembly of the photosynthetic water oxidation complex (WOC) from the inorganic components. Mn2+ binds to the apo-WOC-PSII protein in the absence of calcium at a high-affinity site. By using a hydrophobic chelator to remove Mn2+ and Ca2+ from the WOC and nonspecific Fe3+, a new EPR signal becomes visible upon binding of Mn2+ to this site, characterized by six-line 55Mn hyperfine structure (DeltaHpp = 96 +/- 1 G) and effective g = 8.3. These features indicate a high-spin electronic ground state (S = 5/2) for Mn2+ and a strong ligand field with large anisotropy. This signal is eliminated if excess Ca2+ or Mg2+ is present. A second Mn2+ EPR signal forms in place of this signal upon addition of Ca2+ in the dark. The yield of this Ca-induced Mn signal is optimum at a ratio of 2 Mn/PSII, and saturates with increasing [Ca2+] >/= 8 mM, exhibiting a calcium dissociation constant of KD = 1.4 mM. The EPR signal of the Ca-induced Mn center at 25 K is asymmetric with major g value of approximately 2.04 (DeltaHpp = 380 G) and a shoulder near g approximately 3.1. It also exhibits resolved 55Mn hyperfine splitting with separation DeltaHpp = 42-45 G. These spectral features are diagnostic of a variety of weakly interacting Mn2(II, II) pairs with electronic spins that are magnetic dipolar coupled in the range of intermanganese separations 4.1 +/- 0.4 A, and commonly associated with one or two carboxylate bridges. The calcium requirement for induction of the Mn2(II,II) signal matches the value observed for steady-state O2 evolution (Michaelis constant, KM approximately 1.4 mM), and for light-induced assembly of the WOC by photoactivation. The Ca-induced Mn2(II,II) center is a more efficient electron donor to the photooxidized tyrosine radical, TyrZ+, than is the mononuclear Mn center present in the absence of Ca2+. The Ca-induced Mn2(II,II) signal serves as a precursor for photoactivation of the functional WOC and is abolished by the presence of Mg2+. Formation of the Mn2(II,II) EPR signal by addition of Ca2+ correlates with reduction of flash-induced catalase activity, indicating that calcium modulates the accessibility or reactivity of the Mn2(II,II) core with H2O2. We propose that calcium organizes the binding site for Mn ions in the apo-WOC protein and may even interact directly with the Mn2(II,II) pair via solvent or protein-derived bridging ligands.

Quantitative kinetic model for photoassembly of the photosynthetic water oxidase from its inorganic constituents: requirements for manganese and calcium in the kinetically resolved steps,

The process of photoactivation, the assembly of a functional water-oxidizing complex (WOC) from the apoproteins of photosystem II of higher plants and inorganic cofactors (Mn2+, Ca2+, and Cl-), was known from earlier works to be a two-step kinetic process, requiring two light-induced processes separated by a slower dark period. However, these steps had not been directly resolved in any kinetic experiment, until development of an ultrasensitive polarographic O2 electrode and synthesis of an improved chelator for cofactor removal allowed direct kinetic resolution of the first pre-steady state intermediate [Ananyev, G. M. & Dismukes, G. C. (1996a) Biochemistry 35, 4102-4109]. Herein, the dependence of the rates of each of the first two light steps and the dark step of photoactivation was directly determined in spinach PSII membranes over a range of calcium and manganese concentrations at least 10-fold lower than those possible using commercial O2 electrodes. The following results were obtained. (1) One Mn2+ ion binds and is photooxidized to Mn3+ at a high-affinity site, forming the first light-induced intermediate, IM1. Formation of IM1 is coupled to the dissociation of a bound Ca2+ ion either located in the Mn site or coupled to it. (2) The inhibition constant for Ca2+ dissociation from this site is equal to 1.5 mM. (3) The dissociation constant of Mn2+ at this high-affinity site is equal to 8 microM at the optimum calcium concentration for O2-evolving activity of 8 mM, in agreement with the high-affinity site for electron donation to PSII. (4) Prior to the next photolytic step, one Ca2+ ion must bind at its effector site so that stable photooxidation of a second Mn2+ ion can occur, forming the second light-induced intermediate, IM2. This dark process is the rate-determining step. (5) The Michaelis constant for recovery of O2 evolution by Ca2+ binding at this effector site (Km) is equal to 1.4 mM, a value that is the same as that measured for the calcium requirement for O2 evolution in intact PSII. (6) The low quantum yield for the formation of IM2 from IM1 increases linearly with the duration of the dark period up to the longest period we could examine (10 s). Accordingly, the rate limitation in the second photolytic step originates from a slow calcium-induced dark rearrangement of the first intermediate, IM1, which we propose to be a protein conformational change that allows stable binding of the next Mn2+ ion. We further propose that the single Ca2+ ion which is required for assembly of the Mn4 cluster is equivalent to the Ca2+ ion which functions at the "gatekeeper" site in intact O2-evolving centers, where it plays a role in limiting substrate access to the Mn4 cluster [Sivaraja, M., et al. (1989) Biochemistry 28, 9459-9464; Tso, J., et al., (1991) Biochemistry 30, 4734-4739]. A molecular model for photoactivation is proposed and discussed.

High-resolution kinetic studies of the reassembly of the tetra-manganese cluster of photosynthetic water oxidation: proton equilibrium, cations, and electrostatics

The kinetics of pulsed-light photoactivation, the light-induced reassembly of the water-oxidizing complex (WOC) of PSII in the presence of essential inorganic cofactors, has been studied using two improvements: a new efficient chelator, N,N,N',N'-tetrapropionato-1,3-bis(aminomethyl)benzene (TPDBA), for complete extraction of {Mn4} and Ca2+ and an ultrasensitive polarographic cell for O2 detection [Ananyev, G.M., & Dismukes, G.C. (1996) Biochemistry 35, 4102-4109]. Measurements have been made of the initial half-time, t1/2 (sum of the lag time for formation of the first intermediate, IM1, plus the half-time for formation of the second intermediate, IM2), and the steady-state yield, Yss, for recovery of O2 evolution (proportional to the number of active centers). The following conclusions have been reached: (1) cations (Ca2+, Mg2+, and Na+) slow the rate of photoactivation, even though Ca2+ is essential for activity. Two distinct mechanisms appear to be involved: binding to one or both of the first two Mn(2+)-specific sites and screening of negative charges on apo-WOC that are responsible for concentrating Mn2+ ions by electrostatic steering; (2) the Michaelis constant for the calcium requirement for Yss at sufficiently low Mn2+ concentrations (8 microM) that competition at the calcium site does not occur is K(m) = 1.4 mM. Numerically, K(m) is the same for reactivation of O2 evolution in Ca-depleted PSII membranes which retain four Mn ions; (3) in the absence of Ca2+ but in the presence of saturating amounts of Mn2+ (8 Mn/apo-WOC) and Cl-(35 mM) assembly of a stable tetra-Mn cluster occurs neither under illumination nor in the dark after subsequent addition of CaCl2. However, in the presence of suboptimal concentrations of calcium required for maximum Yss, calcium-dependent assembly of stable yet inactive clusters occurs in the light; (4) protons in equilibrium with the buffer greatly increase the half-time 3-fold between pH 6.75 and 5.4, indicating ionization of one or more protons from the first photo-oxidized intermediate formed prior to the rate-limiting step (photo-oxidation of the second Mn2+); (5) the lipophilic membrane soluble anion tetraphenylboron (TPB-), a known reductant of intact WOC, increases the half-time 2.5-fold (< or = 40 microM) and paradoxically stimulates Yss by 50% at 20 microM concentration. These results suggest that TPB- increases the local concentration of Mn2+ adjacent to apo-WOC (Yss increase), while also reducing the S2 and S3 states of the intact WOC at higher concentrations (t1/2 increase). The effects of anions and cations indicates that overcoming the surface potential of the membrane/protein PSII complex may play an important role in the kinetics of reassembly of the {Mn4} cluster; (6) the ratio Y4/Y3 in the kinetics of O2 evolution from a series of single-turnover flashes, a ratio that typically reflects the probability of misses (alpha), grows noticeably larger with increasing extent of recovery of O2 evolving activity and also with increase in the amount of Mn2+, indicating competition between substrate water and excess Mn2+ for reduction of the functional {Mn4} cluster. On the basis of these results, we extend the model for photoactivation to include the antagonistic effects of H+ and Ca2+ in the formation of the first two intermediates.

Assembly of the tetra-Mn site of photosynthetic water oxidation by photoactivation: Mn stoichiometry and detection of a new intermediate

The process of photoactivation, the assembly of the water-oxidizing complex (WOC) of photosystem II (PSII) membranes, has been examined using two major improvements in methodology. First a new lipophilic chelator, N,N,N',N'-tetrapropionate-1,3-bis(aminomethyl)benzene (TPDBA), has been used that permits complete extraction of both manganese and calcium and the three extrinsic WOC polypeptides while minimizing damage to the apo-PSII protein and, importantly, eliminating the need to use reductants. Second, an ultrasensitive, fast-response, polarographic cell and detection system were built. The apparatus features (a) an ultrabright red light-emitted diode (LED) for controlling the light intensity, pulse duration, and dark intervals, features critical for minimization of photoinhibition; (b) a microvolume (5 microL) O2 polarographic cell (Clark type) fitted with a thin silicone membrane for rapid response (100 ms); and (c) DC/AC preamplifier integrated into the microcell and interfaced to a bandpass AC amplifier. The sensitivity enables detection of approximately 5 x 10(-14) mol of O2 per flash at a signal to noise = 5/1. These improvements permit 100-fold lower Mn concentrations to be explored. Under optimum conditions, complete recovery of O2-evolving activity could be restored compared to that of PSII membranes depleted of the three extrinsic polypeptides (35% Vmax vs intact PSII). Titration of the photoactivation steady-state O2 yield, Yss, and the half-time for recovery, t1/2, vs Mn concentration demonstrate that 4.0 Mn/P680 are cooperatively taken up at 95% restoration of Yss and that 1.1-1.2 Mn atoms are involved in the rate-limiting photolytic step under steady-state conditions. Due to minimization of photoihibition, this intermediate exhibits a single exponential recovery kinetic over the entire population of PSII centers. Mn atoms in excess of 4 Mn/P680 accelerate the rate of photoactivation but decrease the yield above 8-10 Mn/P680. Maxima in both Yss and t1/2 are observed at similar electrochemical potentials of the medium, 380 and 340 mV, respectively. We attribute this maximum to either elimination of a recombination reaction between the redox-active tyrosine-161 of the D1 polypeptide (Y(Z)+) and an electron acceptor, possibly cytochrome b559, or stabilization of an intermediate in photoactivation. At low Mn2+ concentrations, a new pre-steady-state kinetic intermediate which binds fewer than 4 Mn atoms can be directly observed. This early kinetic phase has a rate that depends on Mn concentration and is independent of the electron acceptor identity and concentration.