Flash-induced consumption of molecular oxygen on the donor side of photosystem II in Mn-depleted subchloroplast membrane fragments: specific effects of manganese and calcium ions.

It has been shown that removal of manganese from the water-oxidizing complex (WOC) of photosystem II (PSII) leads to flash-induced oxygen consumption (FIOC) which is activated by low concentration of Mn(2+) (Yanykin et al., Biochim Biophys Acta 1797:516-523, 2010). In the present work, we examined the effect of transition and non-transition divalent metal ions on FIOC in Mn-depleted PSII (apo-WOC-PSII) preparations. It was shown that only Mn(2+) ions are able to activate FIOC while other transition metal ions (Fe(2+), V(2+) and Cr(2+)) capable of electron donation to the apo-WOC-PSII suppressed the photoconsumption of O2. Co(2+) ions with a high redox potential (E (0) for Co(2+)/Co(3+) is 1.8 V) showed no effect. Non-transition metal ions Ca(2+) by Mg(2+) did not stimulate FIOC. However, Ca(2+) (in contrast to Mg(2+)) showed an additional activation effect in the presence of exogenic Mn(2+). The Ca(2+) effect depended on the concentration of both Mn(2+) and Ca(2+). The Ca effect was only observed when: (1) the activation of FIOC induced by Mn(2+) did not reach its maximum, (2) the concentration of Ca(2+) did not exceed 40 µM; at higher concentrations Ca(2+) inhibited the Mn(2+)-activated O2 photoconsumption. Replacement of Ca(2+) by Mg(2+) led to a suppression of Mn(2+)-activated O2 photoconsumption; while, addition of Ca(2+) resulted in elimination of the Mg(2+) inhibitory effect and activation of FIOC. Thus, only Mn(2+) and Ca(2+) (which are constituents of the WOC) have specific effects of activation of FIOC in apo-WOC-PSII preparations. Possible reactions involving Mn(2+) and Ca(2+) which could lead to the activation of FIOC in the apo-WOC-PSII are discussed.

Photoconsumption of oxygen in photosystem II preparations under impairment of the water-oxidizing complex.

Oxygen consumption in photosystem II (PSII) preparations in the light was 2 micromol O2/h per mg Chl at weakly acidic and at neutral pH values. It increased fourfold to fivefold at pH 8.5-9.0. The addition of either artificial electron donors for PSII such as MnCl2 or diphenylcarbazide, or diuron as an inhibitor of electron transfer from QA, the primary bound quinone acceptor, to QB, the secondary bound quinone acceptor of PSII, resulted in a decrease in oxygen consumption rate at basic pH to value close to ones measured at pH 6.5. Such additions did not affect oxygen consumption at lower pH values. The induction of variable chlorophyll fluorescence yield in the light differed greatly at pH 6.5 and 8.5. While at pH 6.5 the fluorescence yield, after an initial fast rise almost to Fmax, only slightly decreased, at pH 8.5 after such a rise it dropped promptly to a low value. The additions of the artificial electron donors at pH 8.5 resulted in the induction kinetics close to that observed at pH 6.5. These data indicate impairment of electron donation to P680+ that could be caused by damage to the water oxidation system at basic pH values. In experiments with PSII preparations treated with Tris to destroy the water-oxidizing complex, photoconsumption of oxygen in the entire pH region was close to the values in untreated preparations at basic pH. In untreated preparations the rate of light-induced oxygen consumption decreased in the presence of catalase, which decomposes H2O2, as well as in the presence of electron acceptor potassium ferricyanide. From these data it is suggested that the light-induced oxygen consumption in PSII is caused by two processes, by an interaction of O2 with organic radicals, which were formed due to oxidation of components of the donor side of this photosystem (proteins, lipids, pigments) by cation-radical P680+, as well as by oxygen reduction by still unidentified components of PSII.

Oxygen reduction in a plastoquinone pool of isolated pea thylakoids.

Oxygen uptake in isolated pea thylakoids in the presence of an inhibitor of plastoquinol oxidation by b (6)/f-complex dinitrophenylether of 2-iodo-4-nitrothymol (DNP-INT) was studied. The rate of oxygen uptake in the absence of DNP-INT had a distinct maximum at pH 5.0 followed by a decline to pH 6.5 and posterior slow rise, while in the presence of an inhibitor it increased at an increasing pH from 4.5 to 6.5 and then kept close to the rate in its absence up to pH 8.5. Gramicidin D substantially affected the oxygen uptake rate in the absence of DNP-INT, and only slightly in its presence. Such differences pointed to the presence of special oxygen reduction site(s) in photosynthetic electron transport chain 'before' cytochrome complex. Oxygen uptake in membrane fragments of Photosystem II (BBY-particles) was low and did not depend on pH. This did not support the participation of Q(B) in oxygen reduction in DNP-INT-treated thylakoids. Oxygen uptake in thylakoids in the presence of DNP-INT was inhibited by DCMU as well as by catalase in whole pH range. The catalase effect indicated that oxygen uptake was the result of dioxygen reduction by electrons derived from water, and that H(2)O(2) was a final product of this reduction. Photoreduction of Cyt c in the presence of DNP-INT was partly inhibited by superoxide dismutase (SOD), and this pointed to superoxide formation. The latter was confirmed by a rise of the oxygen uptake rate in the presence of ascorbate and by suppression of this rise by SOD. Both tests showed that the detectable superoxide radicals averaged 20-25% of potentially formed superoxide radicals the quantity of which was calculated from the oxygen uptake rate. The obtained data implies that the oxygen reduction takes place in a plastoquinone pool and occurs mainly inside the membrane, where superoxide can be consumed in concomitant reactions. A scheme for oxygen reduction in a plastoquinone pool in thylakoid membranes is proposed.

[Effect of high magnesium ion concentration on the electron transport rate and proton exchange in thylakoid membranes in higher plants]. / Vliianie vysokikh kontsentratsii ionov magniia na skorost' élektronnogo transporta i protonnyi obmen v tilakoidnykh membranakh vyshikh rastenii.

The effects of magnesium ion concentration on the rate of electron transport in isolated pea thylakoids were investigated in the pH range from 4.0 up to 8.0. In the absence of magnesium ions in the medium and in the presence of 5 mM MgCl2 in the experiments not only without added artificial acceptors but also with ferricyanide or methylviologen as an acceptor, this rate had a well-expressed maximum at pH 5.0. It was shown that, after depression to minimal values at pH 5.5-6.5, it gradually rose with increasing pH. An increase in magnesium ion concentration up to 20 mM essentially affected the electron transfer rate: it decreased somewhat at pH 4.0-5.0 but increased at higher pH values. At this magnesium ion concentration, the maximum rate was at pH 6.0-6.5 and the minimum, at pH 7.0. Subsequent rise upon increasing pH to 8.0 was expressed more sharply. The influence of high magnesium ion concentration on the rate of electron transport was not observed in the presence of gramicidin D. It was found that without uncoupler, the changes in the electron transfer rate under the influence of magnesium ions correlated to the changes in the first-order rate constant of the proton efflux from thylakoids. It is supposed that the change in the ability of thylakoids to keep protons by the action of magnesium ions is the result of electrostatic interactions of these ions with the charges on the external surface of membranes. A possible role of regulation of the electron transport rate by magnesium ions in vivo is discussed.