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) 相似文献   

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.     

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]+.     

Multiflash experiments reveal a new kinetic phase of photosystem II manganese cluster assembly in Synechocystis sp. PCC6803 in vivo

The assembly of Mn(2+) ions into the H(2)O oxidation complex (WOC) of the photosystem II (PSII) reaction center is a light-driven process, termed photoactivation. According to the "two-quantum" model, photoactivation involves two light-driven charge separations coupled to the photooxidation of Mn(2+) in order to form the first stable intermediate in a process that culminates in the oxidative assembly of four Mn(2+) ions and one Ca(2+) ion to form the active, higher valence (Mn(4)-Ca) center of the WOC. To better define the kinetics of the dark rearrangement and to gain some understanding of the basis for the very low quantum yield of the overall process, photoactivation experiments, involving different flash patterns, were conducted with Synechocystis sp. PCC6803. It was found that even the so-called first stable intermediate is readily lost during protracted (1-10 s) dark periods during photoactivation of Synechocystis cells. Low concentrations of the electron acceptor, DCBQ, improved the stability of the dark intermediates. The unstable photoactivation intermediates formed early in the photoactivation process were not, however, stabilized by the addition of Ca(2+), although the overall yield of photoactivation is enhanced by the additional Ca(2+). Measurements of the kinetics of fluorescence yield verify that Q(A)(-) to Q(B) electron transfer rates change during the course of photoactivation as the high potential form of Q(A)(-) is converted to the low potential form and show that DCBQ acts as an efficient electron acceptor from Q(A)(-) even while in its high potential form. In addition the approximately 150 ms phase corresponding to the originally described dark rearrangement of photoactivation, repetitive, double flash experiments, with a 10 s intervening dark period, reveals a faster, 15 ms phase that is accentuated by DCBQ.     

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+.     

Hydrogencarbonate is not a tightly bound constituent of the water-oxidizing complex in photosystem II

Since the end of the 1950s hydrogencarbonate ('bicarbonate') is discussed as a possible cofactor of photosynthetic water-splitting, and in a recent X-ray crystallography model of photosystem II (PSII) it was displayed as a ligand of the Mn(4)O(x)Ca cluster. Employing membrane-inlet mass spectrometry (MIMS) and isotope labelling we confirm the release of less than one (~0.3) HCO(3)(-) per PSII upon addition of formate. The same amount of HCO(3)(-) release is observed upon formate addition to Mn-depleted PSII samples. This suggests that formate does not replace HCO(3)(-) from the donor side, but only from the non-heme iron at the acceptor side of PSII. The absence of a firmly bound HCO(3)(-) is corroborated by showing that a reductive destruction of the Mn(4)O(x)Ca cluster inside the MIMS cell by NH(2)OH addition does not lead to any CO(2)/HCO(3)(-) release. We note that even after an essentially complete HCO(3)(-)/CO(2) removal from the sample medium by extensive degassing in the MIMS cell the PSII samples retain > or =75% of their initial flash-induced O(2)-evolving capacity. We therefore conclude that HCO(3)(-) has only 'indirect' effects on water-splitting in PSII, possibly by being part of a proton relay network and/or by participating in assembly and stabilization of the water-oxidizing complex.     

Spectroscopic evidence for Ca2+ involvement in the assembly of the Mn4Ca cluster in the photosynthetic water-oxidizing complex

Biogenesis and repair of the inorganic core (Mn4CaO(x)Cl(y)), in the water-oxidizing complex of photosystem II (WOC-PSII), occurs through the light-induced (re)assembly of its free elementary ions and the apo-WOC-PSII protein, a reaction known as photoactivation. Herein, we use electron paramagnetic resonance (EPR) spectroscopy to characterize changes in the ligand coordination environment of the first photoactivation intermediate, the photo-oxidized Mn3+ bound to apo-WOC-PSII. On the basis of the observed changes in electron Zeeman (g(eff)), 55Mn hyperfine (A(Z)) interaction, and the EPR transition probabilities, the photogenerated Mn3+ is shown to exist in two pH-dependent forms, differing in terms of strength and symmetry of their ligand fields. The transition from an EPR-invisible low-pH form to an EPR-active high-pH form occurs by deprotonation of an ionizable ligand bound to Mn3+, implicated to be a water molecule: [Mn3+ (OH2)] <--> [Mn3+ (OH-)]. In the absence of Ca2+, the EPR-active Mn3+ exhibits a strong pH dependence (pH approximately 6.5-9) of its ligand-field symmetry (rhombicity Delta delta = 10%, derived from g(eff)) and A(Z) (DeltaA(Z) = 22%), attributable to a protein conformational change. Binding of Ca2+ to its effector site eliminates this pH dependence and locks both g(eff) and A(Z) at values observed in the absence of Ca2+ at alkaline pH. Thus, Ca2+ directly controls the coordination environment and binds close to the high-affinity Mn3+, probably sharing a bridging ligand. This Ca2+ effect and the pH-induced changes are consistent with the ionization of the bridging water molecule, predicting that [Mn3+-(mu-O(-2))-Ca2+] or [Mn3+-(mu-OH(-))2-Ca2+] is the first light intermediate in the presence of Ca2+. The formation of this intermediate templates the apo-WOC-PSII for the subsequent rapid cooperative binding and photo-oxidation of three additional Mn2+ ions, forming the active water oxidase.     

Differing responses of the two forms of photosystem II carbonic anhydrase to chloride, cations, and pH

The effects of Cl(-), Mn(2+), Ca(2+), and pH on extrinsic and intrinsic photosystem II carbonic anhydrase activity were compared. Under the conditions of our in vitro experiments, extrinsic CA activity, located on the OEC33 protein, was optimum at about 30 mM Cl(-), and strongly inhibited above this concentration. This enzyme is activated by Mn(2+) and stimulated somewhat by Ca(2+). The OEC33 showed dehydration activity that is optimum at pH 6 or below. In contrast, intrinsic CA activity found in the PSII complex after removal of extrinsic proteins was stimulated by Cl(-) up to 0.4 M. Ca(2+) appears to be the required cofactor, which implies that the location of the intrinsic CA activity is in the immediate vicinity of the CaMn(4) complex. Up to now, intrinsic CA has shown only hydration activity that is nearly pH independent.     

Inorganic cofactor stabilization and retention: the unique functions of the two PsbO subunits of eukaryotic photosystem II

Eukaryotic PsbO, the photosystem II (PSII) manganese-stabilizing protein, has two N-terminal sequences that are required for binding of two copies of the protein to PSII [Popelkova, H., et al. (2002) Biochemistry 41, 10038-10045; Popelkova, H., et al. (2003) Biochemistry 42, 6193-6200]. In the work reported here, a set of selected N-terminal truncation mutants of PsbO that affect subunit binding to PSII were used to determine the effects of PsbO stoichiometry on the Mn, Ca(2+), and Cl(-) cofactors and to characterize the roles of each of the PsbO subunits in PSII function. Results of the experiments with the PsbO-depleted PSII membranes reconstituted with the PsbO deletion mutants showed that the presence of PsbO does not affect Ca(2+) retention by PSII in steady-state assays of activity, nor is it required for Ca(2+) to protect the Mn cluster against reductive inhibition in darkness. In contrast to the results with Ca(2+), PsbO increases the affinity of Cl(-) for the active site of the O(2)-evolving complex (OEC) as expected. These results together with other data on activity retention suggest that PsbO can stabilize the Mn cluster by facilitating retention of Cl(-) in the OEC. The data presented here indicate that each of two copies of PsbO has a distinctive function in PSII. Binding of the first PsbO subunit fully stabilizes the Mn cluster and enhances Cl(-) retention, while binding of the second subunit optimizes Cl(-) retention, which in turn maximizes O(2) evolution activity. Nonspecific binding of some PsbO truncation mutants to PSII has no functional significance.     

A possible role of redox-active histidine in the photoligation of manganese into a photosynthetic O2-evolving enzyme.

Our previous experiments with a histidine modifier suggest that in Mn-depleted photosystem (PS) II a histidine residue is photooxidized and charge recombination between the oxidized histidine and QA-emits the thermoluminescence AT-band [Ono, T., & Inoue, Y. (1991) FEBS Lett. 278, 183-186]. By use of the AT-band as an index for histidine oxidation, and EPR signals IIf and IIs as indexes for tyrosine oxidation, we studied the role of this putative redox-active histidine in the photoactivation of the O2-evolving enzyme in NH2OH-treated PSII. The following results have been obtained. (i) Strong-light photoinhibition of NH2OH-treated PSII quickly impaired both capabilities of photoactivation and AT-band emission with almost the same half-inhibition time of 1-2 s, while signal IIf was well retained and signal IIs was not affected at all after complete loss of photoactivation capability. (ii) The capability of exogenous Mn2+ photooxidation was relatively sensitive to strong-light photoinhibition, but DPC was relatively sensitive to strong-light photoinhibition, but DPC photooxidation was highly resistant. (iii) Weak-light photoinhibition simultaneously impaired the capabilities of photoactivation, AT-band emission, and signal IIf with the same half-inhibition time of 1 min, leaving signal IIs unaffected. (iv) It was inferred that the putative redox-active histidine is essential for the photooxidation of coordinated Mn2+, the probable initial step of photoactivation, and its photodamage results in the loss of the capabilities of photoactivation and AT-band emission. Based on these, a scheme of electron transfer on the donor side of PSII involving histidine oxidation via Z+ is proposed.     

Functional characterization and metal ion specificity of the metal-citrate complex transporter from Streptomyces coelicolor

Secondary transporters of citrate in complex with metal ions belong to the bacterial CitMHS family, about which little is known. The transport of metal-citrate complexes in Streptomyces coelicolor has been investigated. The best cofactor for citrate uptake in Streptomyces coelicolor is Fe(3+), but uptake was also noted for Ca(2+), Pb(2+), Ba(2+), and Mn(2+). Uptake was not observed with the Mg(2+), Ni(2+), or Co(2+) cofactor. The transportation of iron- and calcium-citrate makes these systems unique among the CitMHS family members reported to date. No complementary uptake akin to that observed for the CitH (Ca(2+), Ba(2+), Sr(2+)) and CitM (Mg(2+), Ni(2+), Mn(2+), Co(2+), Zn(2+)) systems of Bacillus subtilis was noted. Competitive experiments using EGTA confirmed that metal-citrate complex formation promoted citrate uptake. Uptake of free citrate was not observed. The open reading frame postulated as being responsible for the metal-citrate transport observed in Streptomyces coelicolor was cloned and overexpressed in Escherichia coli strains with the primary Fe(3+)-citrate transport system (fecABCDE) removed. Functional expression was successful, with uptake of Ca(2+)-citrate, Fe(3+)-citrate, and Pb(2+)-citrate observed. No free-citrate transport was observed in IPTG (isopropyl-beta-d-thiogalactopyranoside)-induced or -uninduced E. coli. Metabolism of the Fe(3+)-citrate and Ca(2+)-citrate complexes, but not the Pb(2+)-citrate complex, was observed. Rationalization is based on the difference in metal-complex coordination upon binding of the metal by citrate.     

Highly efficient photoactivation of Mn-depleted photosystem II by imidazole-liganded manganese complexes

The oxygen-evolving complex (OEC) of Mn-depleted photosystem II (PSII) can be reconstituted in the presence of exogenous Mn or a Mn complex under weak illumination, a process called photoactivation. Synthetic Mn complexes could provide a powerful system to analyze the assembly of the OEC. In this work, four mononuclear Mn complexes, [(terpy)₂Mn^II(OOCH₃)]·2H₂O (where terpy is 2,2′:6′,2″-terpyridine), Mn^II(bzimpy)₂, Mn^II(bp)₂(CH₃CH₂OH)₂ [where bzimpy is 2,6-bis(2-benzimidazol-2-yl)pyridine] and [Mn^III(HL)(L)(py)(CH₃OH)]CH₃OH (where py is pyridine) were used in photoactivation experiments. Measurements of the photoreduction of 2,6-dichorophenolindophenol and oxygen evolution demonstrate that photoactivation is more efficient when Mn complexes are used instead of MnCl₂ in reconstructed PSII preparations. The most efficient recoveries of oxygen evolution and electron transport activities are obtained from a complex, [Mn^III(HL)(L)(py)(CH₃OH)]CH₃OH, that contains both imidazole and phenol groups. Its recovery of the rate of oxygen evolution is as high as 79% even in the absence of the 33-kDa peptide. The imidazole ligands of the Mn complex probably accelerate P ₆₈₀ ^•+ reduction and consequently facilitate the process of photoactivation. Also, the strong intermolecular hydrogen bond probably facilitates interaction with the Mn-depleted PSII via reorganization of the hydrogen-bonding network, and therefore promotes the recovery of oxygen evolution and electron transport activities.     

An endoplasmic reticulum-bound Ca(2+)/Mn(2+) pump,ECA1, supports plant growth and confers tolerance to Mn(2+) stress

Plants can grow in soils containing highly variable amounts of mineral nutrients, like Ca(2+) and Mn(2+), though the mechanisms of adaptation are poorly understood. Here, we report the first genetic study to determine in vivo functions of a Ca(2+) pump in plants. Homozygous mutants of Arabidopsis harboring a T-DNA disruption in ECA1 showed a 4-fold reduction in endoplasmic reticulum-type calcium pump activity. Surprisingly, the phenotype of mutant plants was indistinguishable from wild type when grown on standard nutrient medium containing 1.5 mM Ca(2+) and 50 microM Mn(2+). However, mutants grew poorly on medium with low Ca(2+) (0.2 mM) or high Mn(2+) (0.5 mM). On high Mn(2+), the mutants failed to elongate their root hairs, suggesting impairment in tip growth processes. Expression of the wild-type gene (CAMV35S::ECA1) reversed these conditional phenotypes. The activity of ECA1 was examined by expression in a yeast (Saccharomyces cerevisiae) mutant, K616, which harbors a deletion of its endogenous calcium pumps. In vitro assays demonstrated that Ca(2+), Mn(2+), and Zn(2+) stimulated formation of a phosphoenzyme intermediate, consistent with the translocation of these ions by the pump. ECA1 provided increased tolerance of yeast mutant to toxic levels of Mn(2+) (1 mM) and Zn(2+)(3 mM), consistent with removal of these ions from the cytoplasm. These results show that despite the potential redundancy of multiple Ca(2+) pumps and Ca(2+)/H(+) antiporters in Arabidopsis, pumping of Ca(2+) and Mn(2+) by ECA1 into the endoplasmic reticulum is required to support plant growth under conditions of Ca(2+) deficiency or Mn(2+) toxicity.     

Identification of a Mn-O-Mn cluster vibrational mode of the oxygen-evolving complex in photosystem II by low-frequency FTIR spectroscopy

We have developed conditions for recording the low-frequency S(2)/S(1) Fourier transform infrared difference spectrum of hydrated PSII samples. By exchanging PSII samples with buffered (18)O water, we found that a positive band at 606 cm(-)(1) in the S(2)/S(1) spectrum in (16)O water is clearly downshifted to 596 cm(-)(1) in (18)O water. By taking double-difference (S(2)/S(1) and (16)O minus (18)O) spectra, we assign the 606 cm(-)(1) mode to an S(2) mode and also identify a corresponding S(1) mode at about 625 cm(-)(1). In addition, by Sr and (44)Ca substitution experiments, we found that the 606 cm(-)(1) mode is upshifted to about 618 cm(-)(1) by Sr(2+) substitution but that this mode is not affected by substitution with the (44)Ca isotope. On the basis of these results and also on the basis of studies of Mn model compounds, we assign the 625 cm(-)(1) mode in the S(1) state and the 606 cm(-)(1) mode in the S(2) state to a Mn-O-Mn cluster vibration of the oxygen-evolving complex (OEC) in PSII. This structure may include additional bridge(s), which could be another oxo, carboxylato(s), or atoms derived from an amino acid side chain. Our results indicate that the bridged oxygen atom shown in this Mn-O-Mn cluster is exchangeable and accessible by water. The downshift in the Mn-O-Mn cluster vibration as manganese is oxidized during the S(1) --> S(2) transition is counterintuitive; we discuss possible origins of this behavior. Our results also indicate that Sr(2+) substitution in PSII causes a small structural perturbation that affects the bond strength of the Mn-O-Mn cluster in the PSII OEC. This suggests that Sr(2+), and by inference, Ca(2+), communicates with, but is not integral to, the manganese core.     

Central functions of bicarbonate in S-type anion channel activation and OST1 protein kinase in CO2 signal transduction in guard cell

Plants respond to elevated CO(2) via carbonic anhydrases that mediate stomatal closing, but little is known about the early signalling mechanisms following the initial CO(2) response. It remains unclear whether CO(2), HCO(3)(-) or a combination activates downstream signalling. Here, we demonstrate that bicarbonate functions as a small-molecule activator of SLAC1 anion channels in guard cells. Elevated intracellular [HCO(3)(-)](i) with low [CO(2)] and [H(+)] activated S-type anion currents, whereas low [HCO(3)(-)](i) at high [CO(2)] and [H(+)] did not. Bicarbonate enhanced the intracellular Ca(2+) sensitivity of S-type anion channel activation in wild-type and ht1-2 kinase mutant guard cells. ht1-2 mutant guard cells exhibited enhanced bicarbonate sensitivity of S-type anion channel activation. The OST1 protein kinase has been reported not to affect CO(2) signalling. Unexpectedly, OST1 loss-of-function alleles showed strongly impaired CO(2)-induced stomatal closing and HCO(3)(-) activation of anion channels. Moreover, PYR/RCAR abscisic acid (ABA) receptor mutants slowed but did not abolish CO(2)/HCO(3)(-) signalling, redefining the convergence point of CO(2) and ABA signalling. A new working model of the sequence of CO(2) signalling events in gas exchange regulation is presented.     

Intermediates in assembly by photoactivation after thermally accelerated disassembly of the manganese complex of photosynthetic water oxidation

The Mn4Ca complex bound to photosystem II (PSII) is the active site of photosynthetic water oxidation. Its assembly involves binding and light-driven oxidation of manganese, a process denoted as photoactivation. The disassembly of the Mn complex is a thermally activated process involving distinct intermediates. Starting from intermediate states of the disassembly, which was initiated by a temperature jump to 47 degrees C, we photoactivated PSII membrane particles and monitored the activity recovery by O2 polarography and delayed chlorophyll fluorescence measurements. Oxidation state and structural features of the formed intermediates of the Mn complex were assayed by X-ray absorption spectroscopy at the Mn K-edge. The photoactivation time courses, which exhibit a lag phase characteristic of intermediate formation only when starting with the apo-PSII, suggest that within approximately 5 min of photoactivation of apo-PSII, a binuclear Mn complex is formed. It is proposed that a MnIII2(di-mu-oxo) complex is a key intermediate both in the disassembly and in the assembly reaction paths.     

Assembly and disassembly of the photosystem II manganese cluster reversibly alters the coupling of the reaction center with the light-harvesting phycobilisome

The light-driven oxidative assembly of Mn (2+) ions into the H 2O oxidation complex (WOC) of the photosystem II (PSII) reaction center is termed photoactivation. The fluorescence yield characteristics of Synechocystis sp. PCC6803 cells undergoing photoactivation showed that basal fluorescence, F 0, exhibited a characteristic decline when red, but not blue, measuring light was employed. This result was traced to a progressive increase in the coupling of the phycobilisome (PBS) to the PSII reaction center as determined by observing the changes in room temperature and 77 K fluorescence emission spectra that accompany photoactivation. The results support the hypothesis that strong energetic coupling of the PBS to the PSII reaction center depends upon the formation of an active WOC, which presumably diminishes the likelihood of photodamage to reaction centers that have either lost an intact Mn cluster or are in the process of assembling an active WOC.     

Bicarbonate requirement for the water-oxidizing complex of photosystem II

It is well established that bicarbonate stimulates electron transfer between the primary and secondary electron acceptors, Q(A) and Q(B), in formate-inhibited photosystem II; the non-heme Fe between Q(A) and Q(B) plays an essential role in the bicarbonate binding. Strong evidence of a bicarbonate requirement for the water-oxidizing complex (WOC), both O2 evolving and assembling from apo-WOC and Mn2+, of photosystem II (PSII) preparations has been presented in a number of publications during the last 5 years. The following explanations for the involvement of bicarbonate in the events on the donor side of PSII are considered: (1) bicarbonate serves as an electron donor (alternative to water or as a way of involvement of water molecules in the oxidative reactions) to the Mn-containing O2 center; (2) bicarbonate facilitates reassembly of the WOC from apo-WOC and Mn2+ due to formation of the complexes MnHCO3+ and Mn(HCO3)2 leading to an easier oxidation of Mn2+ with PSII; (3) bicarbonate is an integral component of the WOC essential for its function and stability; it may be considered a direct ligand to the Mn cluster; (4) the WOC is stabilized by bicarbonate through its binding to other components of PSII.     

Metal ion requirements for structure and catalysis of an RNA ligase ribozyme

The class I ligase, a ribozyme previously isolated from random sequence, catalyzes a reaction similar to RNA polymerization, positioning its 5'-nucleotide via a Watson-Crick base pair, forming a 3',5'-phosphodiester bond between its 5'-nucleotide and the substrate, and releasing pyrophosphate. Like most ribozymes, it requires metal ions for structure and catalysis. Here, we report the ionic requirements of this self-ligating ribozyme. The ligase requires at least five Mg(2+) for activity and has a [Mg(2+)](1/2) of 70-100 mM. It has an unusual specificity for Mg(2+); there is only marginal activity in Mn(2+) and no detectable activity in Ca(2+), Sr(2+), Ba(2+), Zn(2+), Co(2+), Cd(2+), Pb(2+), Co(NH(3))(6)(3+), or spermine. All tested cations other than Mg(2+), including Mn(2+), inhibit the ribozyme. Hill analysis in the presence of inhibitory cations suggested that Ca(2+) and Co(NH(3))(6)(3+) inhibit by binding at least two sites, but they appear to productively fill a subset of the required sites. Inhibition is not the result of a significant structural change, since the ribozyme assumes a nativelike structure when folded in the presence of Ca(2+) or Co(NH(3))(6)(3+), as observed by hydroxyl-radical mapping. As further support for a nativelike fold in Ca(2+), ribozyme that has been prefolded in Ca(2+) can carry out the self-ligation very quickly upon the addition of Mg(2+). Ligation rates of the prefolded ribozyme were directly measured and proceed at 800 min(-1) at pH 9.0.     

Nucleoside phosphorylation by phosphate minerals

In the presence of formamide, crystal phosphate minerals may act as phosphate donors to nucleosides, yielding both 5'- and, to a lesser extent, 3'-phosphorylated forms. With the mineral Libethenite the formation of 5'-AMP can be as high as 6% of the adenosine input and last for at least 10(3) h. At high concentrations, soluble non-mineral phosphate donors (KH(2)PO(4) or 5'-CMP) afford 2'- and 2':3'-cyclic AMP in addition to 5'-and 3'-AMP. The phosphate minerals analyzed were Herderite Ca[BePO(4)F], Hureaulite Mn(2+)(5)(PO(3)(OH)(2)(PO(4))(2)(H(2)O)(4), Libethenite Cu(2+)(2)(PO(4))(OH), Pyromorphite Pb(5)(PO(4))(3)Cl, Turquoise Cu(2+)Al(6)(PO(4))(4)(OH)(8)(H(2)O)(4), Fluorapatite Ca(5)(PO(4))(3)F, Hydroxylapatite Ca(5)(PO(4))(3)OH, Vivianite Fe(2+)(3)(PO(4))(2)(H(2)O)(8), Cornetite Cu(2+)(3)(PO(4))(OH)(3), Pseudomalachite Cu(2+)(5)(PO(4))(2)(OH)(4), Reichenbachite Cu(2+)(5)(PO(4))(2)(OH)(4), and Ludjibaite Cu(2+)(5)(PO(4))(2)(OH)(4)). Based on their behavior in the formamide-driven nucleoside phosphorylation reaction, these minerals can be characterized as: 1) inactive, 2) low level phosphorylating agents, or 3) active phosphorylating agents. Instances were detected (Libethenite and Hydroxylapatite) in which phosphorylation occurs on the mineral surface, followed by release of the phosphorylated compounds. Libethenite and Cornetite markedly protect the beta-glycosidic bond. Thus, activated nucleic monomers can form in a liquid non-aqueous environment in conditions compatible with the thermodynamics of polymerization, providing a solution to the standard-state Gibbs free energy change (DeltaG degrees ') problem, the major obstacle for polymerizations in the liquid phase in plausible prebiotic scenarios.