The effect of the ionophore A23187 on Mg2+ and Ca2+ movements and internal pH of isolated intact chloroplasts

The transmembrane distribution of galactolipids in chloroplast thylakoids is universal in a wide variety of temperate climate plants

The transmembrane distribution of monogalactosyldiacylglycerol and digalactosyldiacylglycerol was determined in chloroplast thylakoids from a range of temperate climate plants. These plants included dicotyledons, monocotyledons, C16:3 and C18:3 plants and herbicide-resistant species. In all the thylakoids examined monogalactosyldiacylglycerol was enriched in the outer leaflet (53-65%) while digalactosyldiacylglycerol was highly enriched in the inner leaflet (78-90%). The non-bilayer forming monogalactosyldiacylglycerol represented 55-81% of the total acyl lipids of the outer monolayer. The relative acyl lipid composition of both leaflets of the thylakoid membrane indicates that the lamellar structure is strongly favored in the inner monolayer, whereas the outer one presents a metastable character which allows the probable coexistence of both lamellar and non-lamellar phases. The consequence of this asymmetry for the stability and function of the thylakoid membrane is discussed.

Evidence for direct roles of calcium in photosynthesis

Calcium may function directly in several aspects of photosynthesis. It appears to modulate activity of the phosphatase enzymes in the carbon reduction cycle and also to regulate chloroplast NAD+ kinase activity through a calmodulin-like protein. Some evidence supports a calcium function in the water-splitting complex, and other evidence indicates a reaction center function in photosystem II. Calcium in reaction center II may be tightly bound in chloroplasts and weakly bound in blue-green algal thylakoids. Free calcium concentration in stroma is probably less than 10(-6) M, although the absolute concentration is not yet known. Intrathylakoid calcium content is likely very high. Stromal calcium may regulate several enzyme activities, while intrathylakoid calcium may promote photosystem II constitutively. Results to date demonstrate the need for more attention to cation composition in studies of both light and dark reactions of photosynthesis, and the need to identify free calcium levels in chloroplasts.

Conditions limiting the use of ionophore A23187 as a probe of divalent cation involvement in biological reactions. Evidence from the slow fluorescence quenching of type A spinach chloroplasts

The conditions under which ionophore A23187 can be used as a probe of Mg2+ involvement in the reactions of intact (Type A) spinach chloroplasts have been investigated by monitoring ionophore-induced reversal of slow fluorescence quenching. The following observations were made: (1) A23187-dependent reversal of quenching is a strong function of pH. This is consistent with competition between protons and divalent cations for the carboxylic acid moiety of the ionophore. (2) In the presence of exogenous Mg2+, quenching reversal by A23187 is significantly slowed. It is suggested that formation of the dimeric A23187 . Mg2+ complex delays action of the ionophore at the thylakoid membrane by slowing equilibration of the ionophore among chloroplast membrane phases. (3) In the absence of Mg2+, significant interaction of A23187 with certain monovalent cations--Li+ and Na+, but not K+--is observed. Evaluations of the interaction of ionophore A23187 with specific biological systems and inferences of divalent cation involvement, or lack thereof, must take these limitations into account.

Calcium and photosynthetic oxygen evolution in cyanobacteria

Calcium activation of oxygen evolution from French-press preparations of Phormidium luridum is largely reversible upon removal of added Ca(2+). Activation occurs via a first-order binding with a dissociation constant of 2.8 mM. An 8-fold increase in oxygen evolution rate observed upon Ca(2+) addition is accounted for by a 4-fold increase in the number of active photosynthetic units, and a doubling of turnover rate. While both Ca(2+) and Mg(2+) stimulate turnover, unit activation is Ca(2+) specific. Under optimal conditions, 30% of the units functioning in the intact cell can be recovered in the Ca(2+) -activated preparation. The Ca(2+) requirement of P. luridum preparations is not relieved by proton-carrying uncouplers, or by rate-saturating concentrations of the Hill acceptor, ferricyanide. Taken together with the reported stimulation by Ca(2+) of oxygen evolution in the presence of DCMU (Piccioni, R.G. and Mauzerall, D.C. (1976) Biochim. Biophys. Acta 423, 605--609) these observations strongly suggest a site of Ca(2+) action within Photosystem II. The pronounced specificity of the Ca(2+) requirement appears in preparations of other cyanobacteria (Anabaena flos-aquae and Anacystis nidulans) but not in the eucaryote Chlorella vulgaris. While milder cell-disruption methods bring about some Ca(2+) dependence in P. luridum, French-press treatment is required for maximal expression of Ca(2+) -specific effects. French-press breakage causes a release of endogenous Ca(2+) from cells, supporting the view that added Ca(2+) restores oxygen evolution by satisfying a physiological requirement for the cation.