A new mechanism-based inhibitor of photosynthetic water oxidation: acetone hydrazone. 2. Kinetic probes

The mechanism of photosynthetic water oxidation in spinach was investigated with a newly developed inhibitor of the water-oxidizing complex, acetone hydrazone (AceH), (CH3)2CNNH2 [Tso, J., Petrouleas, V., & Dismukes, G.C. (1990) Biochemistry (preceding paper in this issue)], by using fluorescence induction and single-turnover flashes to monitor O2 yield and thermoluminescence intensity. AceH binds slowly (1-3 min) in the dark to the S1 (resting) oxidation state of the water-oxidizing complex in thylakoids and PSII membranes. Once bound, it causes a two-flash delay in the pattern of O2 release seen in a train of flashes. This is initiated by reduction of manganese in the S2 oxidation state of the complex in a fast reaction (less than 0.5 s). In thylakoid membranes which have been partially inhibited at low AceH concentrations (less than 2 mM) the inhibition can be reversed by a single flash and a subsequent dark period. This behavior can be explained by two sequential one-electron oxidation steps: S1.AceHhv----S2.AceH in equilibrium S1.AceH+hv----S2.AceH+----S1 + AceH2+ Dissociation of the unobserved radical intermediate, AceH+, from S1 is proposed to account for the recovery from inhibition after one flash. In contrast, recovery from inhibition after a single flash is not observed in detergent-isolated PSII membranes or in intact thylakoid membranes at higher AceH concentrations (greater than 2 mM), where the two-flash delay in O2 release is seen. This suggests either a concerted two-electron process, S2----S0, or tight binding of AceH+ to S1.(ABSTRACT TRUNCATED AT 250 WORDS)     

Mechanism of photoinhibition of photosynthetic water oxidation by Cl- depletion and F- substitution: oxidation of a protein residue

New evidence on the chloride requirement for photosynthetic O2 evolution has indicated that Cl- facilitates oxidation of the manganese cluster by the photosystem II (PSII) Tyr-Z+ radical. Illumination above 250 K of spinach PSII centers which are inhibited in O2 evolution by either Cl- depletion or F- substitution produces a new EPR signal which has magnetic characteristics similar to one recently discovered in samples inhibited by depletion of Ca2+ only [Boussac et al. (1989) Biochemistry 28, 8984; Sivaraja et al. (1989) Biochemistry 28, 9459]. The physiological roles of Cl- and Ca2+ in water oxidation are thus linked. The characteristics include a nearly isotropic g = 2.00 +/- 0.005, a symmetric line shape with line width = 16 +/- 2 mT, almost stoichiometric spin concentration relative to Try-D+ = 0.6 +/- 0.3 spin/PSII, very rapid spin relaxation at all temperatures measured down to 6 K, and an undetectable change in magnetic susceptibility upon formation (less than 1 mu B2). The signal appears to originate from a spin doublet (radical) in magnetic dipolar contact with a transition-metal ion, most probably a photooxidized protein residue within 10 A of the Mn cluster (Mn-proximal radical). It is distinct from the three other protein-bound radical-type electron donors found in the PSII reaction center: Tyr-D+, Tyr-Z+, and C+. This signal photoaccumulates to a stable level under continuous illumination at 270 K and decays only after illumination stops.(ABSTRACT TRUNCATED AT 250 WORDS)     

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]+.     

Enhancement by chloride ions of photoactivation of oxygen evolution in manganese-depleted photosystem II membranes

The Mn cluster that catalyzes photosynthetic oxygen evolution was removed from the photosystem II (PSII) complex by treating PSII membranes with 1.0 mM NH2OH with concomitant inactivation of oxygen evolution. The cluster was reconstituted by incubating the treated membranes with 1.0 mM Mn2+, 20 mM Ca2+, 10 microM 2,6-dichlorophenolindophenol, and Cl- under illumination with continuous or flashing light to restore the oxygen-evolving capacity. This light-dependent activation (photoactivation) of oxygen evolution did not occur to a significant extent at 3 mM Cl-, but markedly accelerated at higher Cl- concentrations without showing a saturation phenomenon even at 1 M Cl-. At 10 mM Cl- only about 10% of the oxygen-evolving activity before NH2OH treatment was restored by 5-min illumination with continuous light, whereas at 600 mM Cl- about 60% of the original activity was recovered. This acceleration resulted from at least two different actions of Cl-: (1) stabilization of the intermediate state involved in the photoactivation process and (2) increase in the quantum yield of photoactivation. The stabilization of the intermediate was saturated at about 150 mM Cl-, whereas the increase in yield did not show saturation. The Cl(-)-induced increase in quantum yield did not involve any changes in the affinity of either Mn2+ binding or Ca2+ binding for photoactivation, but was rather ascribed to a protective effect of Cl- against inhibition of photoactivation by high concentrations of Mn2+. We also found that removal of the extrinsic 33-kDa protein from the PSII complex increased the Cl- requirement for photoactivation.     

Characteristic changes of the S2/S1 difference FTIR spectrum induced by Ca2+ depletion and metal cation substitution in the photosynthetic oxygen-evolving complex

Effects of Ca2+ depletion and substitution with other metal cations on the structure of the protein matrices of the oxygen-evolving complex (OEC) and their corresponding changes upon the S1 to S2 transition were examined using Fourier transform infrared (FTIR) spectroscopy. Ca2+ depletion and further supplementation with Li+, Na+, Mg2+, Ca2+, or Sr2+ did not significantly affect the typical vibrational features in the double difference S2/S1 spectrum, including the symmetric [1365(+)/1404(-) cm(-1)] and the asymmetric [1587(+)/1566(-) cm(-1)] stretching modes of the carboxylate ligand and the amide I and II modes of the backbone polypeptides. On the other hand, supplementation with K+, Rb+, Cs+, or Ba2+ significantly modified the S2/S1 spectrum, in which the carboxylate modes disappeared and the amide I and II modes were modified. Results indicate that the binding of metal cations that have ionic radii larger than that of Ca2+ to the Ca2+ site induces perturbations in the protein matrices in the vicinity of the Mn cluster to interrupt the characteristic structural and/or conformational changes upon the oxidation of the Mn cluster accompanied with the S1 to S2 transition. The spectrum was also altered by the supplementation of Cd2+, which has an ionic radius comparable to that of Ca2+. A single-pulse-induced S2/S1 difference spectrum revealed that bands that have been assigned to the vibrational modes for the Y(Z) tyrosine and the histidine ligand for the Mn cluster were not induced in the K+-supplemented membranes, although the histidine band is likely to be preserved in the Ca2+-depleted membranes. The Y(Z) band was considerably small in the double difference S2/S1 spectrum in the Ca2+-depleted and the cation-substituted membranes but distinctively present in the Sr2+- or Ca2+-replenished membranes. Furthermore, cation supplementation induced several new bands that disappeared following the Ca2+ replenishment. These results suggest that the proper organization of the hydrogen bond network within OEC for the water oxidation chemistry requires the Ca2+ ion and indicate that the role of Ca2+ is not purely structurally defined by the physical properties of the ion, such as valence and ionic radius. On the basis of these and other findings, we propose that Ca2+ is necessary for the formation of the hydrogen bond network that is involved in the reaction step of water oxidation.     

Catalytic properties of phenol carboxylase. In vitro study of CO2: 4-hydroxybenzoate isotope exchange reaction

Phenol is metabolized in a denitrifying bacterium in the absence of molecular oxygen via para-carboxylation to 4-hydroxybenzoate (biological Kolbe-Schmitt synthesis). The enzyme system catalyzing the presumptive carboxylation of phenol, tentatively named 'phenol carboxylase', catalyzes an isotope exchange between 14CO2 and the carboxyl group of 4-hydroxybenzoate (specific activity 0.1 mumol 14CO2 incorporated into 4-hydroxybenzoate x min-1 x mg-1 cell protein) which is considered a partial reaction of the overall enzyme catalysis; 14C from [14C]phenol was not exchanged into 4-hydroxybenzoate ring positions to a significant extent. The 14CO2 isotope exchange reaction was studied in vitro. The reaction was dependent on the substrates CO2 and 4-hydroxybenzoate and required K+ and Mn2+. The actual substrate was CO2 rather than HCO3-. The apparent Km values were 1 mM dissolved CO2, 0.2 mM 4-hydroxybenzoate, 2 mM K+, and 0.1 mM Mn2+. The cationic cocatalysts could be substituted by ions of similar ionic radius: K+ could be replaced to some extent by Rb+, but not by Li+, Na+, Cs+, or NH4+; Mn2+ could be replaced to some extent by Fe2+ greater than Mg2+, Co2+, but not by Ni2+, Zn2+, Ca2+, or Cu2+. The exchange reaction was not strictly specific for 4-hydroxybenzoate, however it required a p-hydroxyl group; derivatives of 4-hydroxybenzoate with OH, CH3 or Cl substituents in m-position did react, whereas those with substitutions in the o-position were inactive or were inhibitory. The enzyme was induced when cells were grown on phenol, but not on 4-hydroxybenzoate. Comparison of SDS/PAGE protein patterns of cells grown on phenol or 4-hydroxybenzoate revealed several additional protein bands in phenol-grown cells. The possible role of similar enzymes in the anaerobic metabolism of phenolic compounds is discussed.     

Improvement by benzoquinones of the quantum yield of photoactivation of photosynthetic oxygen evolution: direct evidence for the two-quantum mechanism.

Effects of eight differently substituted 1,4-benzoquinones (BQs) on the quantum yield of photoactivation of oxygen evolution (reconstitution of the Mn cluster) were examined with wheat photosystem II (PSII) membranes depleted of the Mn cluster by treatment with 1.0 mM NH2OH. Illumination with 10 flashes at 0.25-s intervals of the PSII membranes in the presence of 2.0 mM Mn2+, 20 mM Ca2+, and 1.2 M Cl- restored 14% of oxygen-evolving activity destroyed by the NH2OH treatment. Among the benzoquinones tested, DBMIB (2,5-dibromo-3-methyl-6-isopropyl-BQ) and tetramethyl-BQ did not enhance the activity recovery, but all the others doubled the recovery when present at their optimal concentrations during illumination. The order of effectiveness was tetrabromo-, phenyl-, and 2,6-dichloro-BQs greater than or equal to 2,5-dichloro-BQ greater than tetrachloro-BQ greater than 2,5-dimethyl-BQ, though the differences were small. This order reflects their efficiencies as electron acceptors of PSII. This finding, together with others, suggests that the enhancement of activity recovery results from rapid oxidation by the benzoquinones of the reduced form of the quinone acceptors in PSII, QA- and QB-, which cause loss of an oxidized intermediate through charge-recombination reaction with Mn3+. The flash-number dependence of the recovery of oxygen-evolving activity indicated that the activity was not restored after one flash but recovered significantly after illumination with two flashes and then further increased upon additional flashes. This provides direct evidence that the minimum quantum requirement for photoactivation is two.     

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.     

Mechanism of irreversible inhibition of O2 evolution in photosystem II by Tris(hydroxymethyl)aminomethane.

The dark reaction of tris(hydroxymethyl)aminomethane (Tris) with the O2-evolving center of photosystem II (PSII) in the S1 state causes irreversible inhibition of O2 evolution. Similar inhibition is observed for several other amines: NH3, CH3NH2, (CH3)2NH, ethanolamine, and 2-amino-2-ethyl-1,3-propanediol. In PSII membranes, both depleted of the 17- and 23-kDa polypeptides and undepleted, the rate of reaction of Tris depends inversely upon the Cl- concentration. However, the rate of reaction of Tris is about 2-fold greater with PSII membranes depleted of the 17- and 23-kDa polypeptides than with undepleted PSII membranes. We have used low-temperature electron paramagnetic resonance (EPR) spectroscopy to study the effect of Tris on the oxidation state of the Mn complex in the O2-evolving center, to monitor the electron-donation reactions in Tris-treated samples, and to observe any loss of the Mn complex (forming Mn2+ ions) after Tris treatment. We find that Tris treatment causes loss of electron-donation ability from the Mn complex at the same rate as inhibition of O2 evolution and that Mn2+ ions are released. We conclude that Tris reduces the Mn complex to labile Mn2+ ions, without generating any kinetically stable, partially reduced intermediates, and that the reaction occurs at the Cl(-)-sensitive site previously characterized in studies of the reversible inhibition of O2 evolution by amines.     

Removal of Mn from spinach chloroplasts by sodium cyanide and the binding of Mn2+ to Mn-depleted chloroplasts.

Manganese and copper were released from spinach chloroplasts by NaCN-treatment, though iron was not affected. The Hill reaction activity was also inhibited by this treatment, but was partially recovered by the addition of either Mn2+ or Cu2+, but not of Fe3+. The interaction of Mn2+ with manganese-depleted chloroplasts by NaCN-treatment was studied using 54Mn2+. A Scatchard plot shows the high and low affinity binding sites of Mn2+ on NaCN-treated chloroplast membrane; high affinity binding being specific for NaCN-treated chloroplast with a binding constant, KH, of 1.9 X 10(5) M-1, and a maximum binding number, NH, of 0.0016 g-atom per mole of chlorophyll. The low binding site was also found on untreated chloroplasts; its binding constant, KL, being 1.2 X 10(4) M-1, and its maximum binding number, NL, of 0.0112 g-atom per mole oc chlorophyll at pH 8.2 NH was proportional to the degree of the removal of Mn by NaCN-treatment and was constant at pH 4--9. NL markedly increased at a high pH with a midpoint of pH 7.9 indicating the exposure of a new, similar binding site. Light illumination partially inhibited the binding of Mn2+. Within 1 min in the dark the binding reaction reached equilibrium in the absence of pyrophosphate, however, 20 min were required to transform into pyrophosphate-resistant form. The pH dependence of the binding of Mn2+ with pKa 7.2 and the ineffectiveness of p-chloromercuribenzoate suggest the possible ligand of Mn2+ is the imidazole nitrogen of the histidine residue.     

Ca2+ depletion from the photosynthetic water-oxidizing complex reveals photooxidation of a protein residue.

A new intermediate in the water-oxidizing reaction has been observed in spinach photosystem II (PSII) membranes that are depleted of Ca2+ from the site which is conformationally coupled to the manganese cluster comprising the water-oxidizing complex (WOC). It gives rise to a recently identified EPR signal (symmetric line shape with width 163 +/- 5 G, g = 2.004 +/- 0.005), which forms in samples inhibited either by depletion of Ca2+ [Boussac, A., Zimmerman, J.-L., & 28, 8984-8989; Sivaraja, M., Tso, J., & Dismukes, G.C. (1989) Biochemistry 28 9459-9464] or by substitution of Cl- by F- (Baumgarten, Philo, and Dismukes, submitted for publication). Further characterization of this EPR signal has revealed the following: (1) it forms independently of the local structure of the PSII acceptors; (2) it arises from photooxidation of a PSII species that donates an electron to Tyr-Z+ or to the Mn cluster in competition with an exogenous donor (DPC); (3) the Curie temperature dependence of the intensity suggests an isolated doublet ground state, attributable to a spin S = 1/2 radical; (4) the electron spin orientation relaxes 1000-fold more rapidly than typical for a free radical, exhibiting a strong temperature dependence of P1/2 (half-saturation power approximately T3.4) and a broad inhomogeneous line width; (5) it yields an undetectable change in the magnetic susceptibility upon formation by a laser flash; (6) it disappears in parallel with release of Mn during reduction with NH2OH, indicating that it forms only in the presence of the modified Mn cluster. (ABSTRACT TRUNCATED AT 250 WORDS)     

EPR studies of the water oxidizing complex in the S1 and the higher S states: the manganese cluster and Y(Z) radical

The parallel polarization electron paramagnetic resonance (EPR) method has been applied to investigate manganese EPR signals of native S1 and S3 states of the water oxidizing complex (WOC) in photosystem (PS) II. The EPR signals in both states were assigned to thermally excited states with S=1, from which zero-field interaction parameters D and E were derived. Three kinds of signals, the doublet signal, the singlet-like signal and g=11-15 signal, were detected in Ca2+-depleted PS II. The g=11-15 signal was observed by parallel and perpendicular modes and assigned to a higher oxidation state beyond S2 in Ca2+-depleted PS II. The singlet-like signal was associated with the g=11-15 signal but not with the Y(Z) (the tyrosine residue 161 of the D1 polypeptide in PS II) radical. The doublet signal was associated with the Y(Z) radical as proved by pulsed electron nuclear double resonance (ENDOR) and ENDOR-induced EPR. The electron transfer mechanism relevant to the role of Y(Z) radical was discussed.     

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.     

What Are the Oxidation States of Manganese Required To Catalyze Photosynthetic Water Oxidation?

Photosynthetic O(2) production from water is catalyzed by a cluster of four manganese ions and a tyrosine residue that comprise the redox-active components of the water-oxidizing complex (WOC) of photosystem II (PSII) in all known oxygenic phototrophs. Knowledge of the oxidation states is indispensable for understanding the fundamental principles of catalysis by PSII and the catalytic mechanism of the WOC. Previous spectroscopic studies and redox titrations predicted the net oxidation state of the S(0) state to be (Mn(III))(3)Mn(IV). We have refined a previously developed photoassembly procedure that directly determines the number of oxidizing equivalents needed to assemble the Mn(4)Ca core of WOC during photoassembly, starting from free Mn(II) and the Mn-depleted apo-WOC complex. This experiment entails counting the number of light flashes required to produce the first O(2) molecules during photoassembly. Unlike spectroscopic methods, this process does not require reference to synthetic model complexes. We find the number of photoassembly intermediates required to reach the lowest oxidation state of the WOC, S(0), to be three, indicating a net oxidation state three equivalents above four Mn(II), formally (Mn(III))(3)Mn(II), whereas the O(2) releasing state, S(4), corresponds formally to (Mn(IV))(3)Mn(III). The results from this study have major implications for proposed mechanisms of photosynthetic water oxidation.     

Effect of substitution inert metal complexes on calcineurin.

As a substitute for M(H2O)2+6, Co(NH3)3+6 was found to activate calcineurin with para-nitrophenyl phosphate as substrate. Kinetics for calcineurin catalyzed hydrolysis of para-nitrophenyl phosphate at pH 7.0 with Mn2+, Mg2+, Co2+, and Co(NH3)3+6 were compared. Although kcat and Km were different with the metals, values of kcat/Km were nearly identical for Mn2+ and Mg2+, but lower for Co2+ and Co(NH3)3+6. The concentration of each metal providing half-maximal activation, designated Kact, was evaluated as 15.9 mM for Co(NH3)3+6, compared to Kact = 0.17 mM for Mn2+ and Co2+ and 6.3 mM for Mg2+, respectively. Comparing kcat/Kcat showed that Co(NH3)3+6 was a 170-fold poorer activator of calcineurin than was Mn2+, but only 1.5-fold poorer than Mg2+. Activation by Co(NH3)3+6 indicated that activation of calcineurin by exogenous metal ions can proceed via an outer coordination sphere reaction mechanism with no requirement for the direct coordination of substrate by metal. Because Co(NH3)3+6 was found to support calcineurin activity, the related compound [Co-(ethylenediamine)3]3+ (or Co(en)3+3) was tested as a possible activator. Co(en)3+3 did not support calcineurin activity but did inhibit calcineurin. Co(en)3+3 showed competitive inhibition kinetics with either Mn2+ or pNPP as the varied ligand and the other at a fixed, subsaturating concentration. Inorganic phosphate was used as a known competitive inhibitor to pNPP (B. L. Martin and D. J. Graves, J. Biol. Chem. 261, 14545-14550, 1986) and showed uncompetitive inhibition with Mn2+ as the varied ligand. These patterns are consistent with the mechanism of ligand binding to calcineurin being ordered with metal preceding substrate. Prior formation of a metal-substrate complex was not required for association with calcineurin.     

Oxygen Enhancement of bactericidal activity of rifamycin SV on Escherichia coli and aerobic oxidation of rifamycin SV to rifamycin S catalyzed by manganous ions: the role of superoxide

Oxygen enhanced the bactericidal activity of rifamycin SV to Escherichia coli K12. Anaerobically grown cells, which had a low level of superoxide dismutase, were more susceptible to the bactericidal activity than aerobically grown cells, which contained a high level of superoxide dismutase. Oxygen also enhanced the inhibition of RNA polymerase activity of rifamycin SV, when Mn2+ was used as a cofactor. Rifamycin S was reduced to rifamycin SV by NADPH catalyzed by cell-free extracts of Escherichia coli K12. These results indicate that the inhibition of bacterial growth by rifamycin SV is due to the production of active species of oxygen resulting from the oxidation-reduction cycle of rifamycin SV in the cells. The aerobic oxidation of rifamycin SV to rifamycin S was induced by metal ions, such as Mn2+, Cu2+, and Co2+. The most effective metal ion was Mn2+. In the presence of Mn2+, accompanying the consumption of 1 mol of oxygen and the oxidation of 1 mol of rifamycin SV, 1 mol of hydrogen peroxide and 1 mol of rifamycin S were formed. Superoxide was generated during the autoxidation of rifamycin SV. Superoxide dismutase inhibited the formation of rifamycin S, but scavengers for hydrogen peroxide and the hydroxyl radical did not affect the oxidation. A mechanism of Mn2+-catalyzed oxidation of rifamycin SV is proposed and its relation to bactericidal activity is discussed.     

Probing the functional role of Ca2+ in the oxygen-evolving complex of photosystem II by metal ion inhibition

Photosynthetic oxygen evolution in photosystem II (PSII) takes place in the oxygen-evolving complex (OEC) that is comprised of a tetranuclear manganese cluster (Mn4), a redox-active tyrosine residue (YZ), and Ca2+ and Cl- cofactors. The OEC is successively oxidized by the absorption of 4 quanta of light that results in the oxidation of water and the release of O2. Ca2+ is an essential cofactor in the water-oxidation reaction, as its depletion causes the loss of the oxygen-evolution activity in PSII. In recent X-ray crystal structures, Ca2+ has been revealed to be associated with the Mn4 cluster of PSII. Although several mechanisms have been proposed for the water-oxidation reaction of PSII, the role of Ca2+ in oxygen evolution remains unclear. In this study, we probe the role of Ca2+ in oxygen evolution by monitoring the S1 to S2 state transition in PSII membranes and PSII core complexes upon inhibition of oxygen evolution by Dy3+, Cu2+, and Cd2+ ions. By using a cation-exchange procedure in which Ca2+ is not removed prior to addition of the studied cations, we achieve a high degree of reversible inhibition of PSII membranes and PSII core complexes by Dy3+, Cu2+, and Cd2+ ions. EPR spectroscopy is used to quantitate the number of bound Dy3+ and Cu2+ ions per PSII center and to determine the proximity of Dy3+ to other paramagnetic centers in PSII. We observe, for the first time, the S2 state multiline electron paramagnetic resonance (EPR) signal in Dy3+- and Cd2+-inhibited PSII and conclude that the Ca2+ cofactor is not specifically required for the S1 to S2 state transition of PSII. This observation provides direct support for the proposal that Ca2+ plays a structural role in the early S-state transitions, which can be fulfilled by other cations of similar ionic radius, and that the functional role of Ca2+ to activate water in the O-O bond-forming reaction that occurs in the final step of the S state cycle can only be fulfilled by Ca2+ and Sr2+, which have similar Lewis acidities.     

Role of second metal ion in establishing active conformations of concanavalin A

The stoichiometry of Mn2+ binding to concanavalin A was found to be influenced by temperature, pH, and the presence or absence of saccharide. Demetalized concanavalin A binds one Mn2+ (S1 site) at 5 degrees C, pH 6.5, and two Mn2+ at 25 degrees C (S1 and S2 sites). The association constants for Mn2+ are 6.2 x 10(5) and 3.7 x 10(4) M-1 for the S1 and S2 sites, respectively, at 25 degrees C. Concanavalin A with one Mn2+ bound per monomer remains in an open conformation and exhibits a relatively high water proton relaxation rate. Concanavalin A with two Mn2+ ions remains in a closed conformation characterized by a lower relaxation rate. The rate of binding of the second Mn2+ to concanavalin A as determined by ESR and the rate of conversion of open form to closed form (folding over) as determined by proton relaxation rate measurements gave an identical rate constant of 80.0 +/- 5.8 M-1 h-1 at 17 degrees C. Ca2+, Sr2+, and high levels of methyl alpha-D-mannopyranoside also induce folding of concanavalin A. Ca2+ is not catalytic but stoichiometric in causing the folding. Mn2+ in the S1 site can be displaced by Ni2+, Co2+, and Zn2+, and Mn2+ in the S2 site can be displaced by Ca2+ and Sr2+. Concanavalin A with Ni2+, Co2+, Zn2+, or Mn2+ in the S1 site and Ca2+ or Sr2+ in the S2 site has a higher affinity for methylumbelliferyl alpha-D-mannopyranoside than Ni-Mn-, Co-Mn-, Zn-Mn-, and Cd-Cd-concanavalin A.     

Crystal structure of cadaverine dihydrochloride monohydrate.

The structure of cadaverine dihydrochloride monohydrate has been determined by X-ray crystallography with the following features: NH3+ (CH2)5NH3+.2Cl-.H2O, formula weight 191.1, monoclinic, P2, a = 11.814(2)A, b = 4.517(2)A, c = 20.370(3)A, beta = 106.56 degrees (1): V = 1041.9(2)A3; lambda = 1.541A; mu = 53.41; T = 296 degrees; Z = 4, Dx = 1.218 g.cm-3, R = 0.101 for 1383 observed reflections. The crystal is highly pseudo-symmetric with 2 molecules of cadaverine, 4 chloride ions and 2 partially disordered water molecules present in the asymmetric unit. Though both the cadaverine molecules in the asymmetric unit have an all trans conformation, the carbon backbones are slightly bent. Between the concave surfaces of two bent cadaverine molecules exists water channels all along the short b axis. The water molecules present in the channels are partially disordered.     

Interaction of sodium and potassium ions with Na+,K+-ATPase. II. General properties of ouabain-sensitive K+ binding

General properties of ouabain-sensitive K+ binding to purified Na+,K+-ATPase [EC 3.6.1.3] were studied by a centrifugation method with 42K+. 1) The affinity for K+ was constant at pH values higher than 6.4, and decreased at pH values lower than 6.4. 2) Mg2+ competitively inhibited the K+ binding. The dissociation constant (Kd) for Mg2+ of the enzyme was estimated to be about 1 mM, and the ratio of Kd for Mg2+ to Kd for K+ was 120 : 1. The order of inhibitory efficiency of divalent cations toward the K+ binding was Ba2+ congruent to Ca2+ greater than Zn2+ congruent to Mn2+ greater than Sr2+ greater than Co2+ greater than Ni2+ greater than Mg2+. 3) The order of displacement efficiency of monovalent cations toward the K+ binding in the presence or absence of Mg2+ was Tl+ greater than Rb+ greater than or equal to (K+) greater than NH4+ greater than or equal to Cs+ greater than Na+ greater than Li+. The inhibition patterns of Na+ and Li+ were different from those of other monovalent cations, which competitively inhibited the K+ binding. 4) The K+ binding was not influenced by different anions, such as Cl-, SO4(2-), NO3-, acetate, and glycylglycine, which were used for preparing imidazole buffers. 5) Gramicidin D and valinomycin did not affect the K+ binding, though the former (10 micrograms/ml) inhibited the Na+,K+-ATPase activity by about half. Among various inhibitors of the ATPase, 0.1 mM p-chloromercuribenzoate and 0.1 mM tri-n-butyltin chloride completely inhibited the K+ binding. Oligomycin (10 micrograms/ml) and 10 mM N-ethylmaleimide had no effect on the K+ binding. In the presence of Na+, however, oligomycin decreased the K+ binding by increasing the inhibitory effect of Na+, whether Mg2+ was present or not. 6) ATP, adenylylimido diphosphate and ADP each at 0.2 mM decreased the K+ binding to about one-fourth of the original level at 10 microM K+ without MgCl2 and at 60 microM K+ with 5 mM MgCl2. On the other hand, AMP, Pi, and p-nitrophenylphosphate each at 0.2 mM had little effect on the K+ binding.