The non-selective slow vacuolar (SV) channel can dominate tonoplast conductance, making it necessary to tightly control its activity. Applying the patch-clamp technique to vacuoles from sugar beet (Beta vulgaris L.) taproots we studied the effect of divalent cations on the vacuolar side of the SV channel. Our results show that the SV channel has two independent binding sites for vacuolar divalent cations, (i) a less selective one, inside the channel pore, binding to which impedes channel conductance, and (ii) a Ca(2+)-selective one outside the membrane-spanning part of the channel protein, binding to which stabilizes the channel's closed conformations. Vacuolar Ca2+ and Mg2+ almost indiscriminately blocked ion fluxes through the open channel pore, decreasing measured single-channel current amplitudes. This low-affinity block displays marked voltage dependence, characteristic of a 'permeable blocker'. Vacuolar Ca(2+)-with a much higher affinity than Mg(2+)-slows down SV channel activation and shifts the voltage dependence to more (cytosol) positive potentials. A quantitative analysis results in a model that exactly describes the Ca(2+)-specific effects on the SV channel activation kinetics and voltage gating. According to this model, multiple (approximately three) divalent cations bind with a high affinity at the luminal interface of the membrane to the channel protein, favoring the occupancy of one of the SV channel's closed states (C2). Transition to another closed state (C1) diminishes the effective number of bound cations, probably due to mutual repulsion, and channel opening is accompanied by a decrease of binding affinity. Hence, the open state (O) is destabilized with respect to the two closed states, C1 and C2, in the presence of Ca2+ at the vacuolar side. The specificity for Ca2+ compared to Mg2+ is explained in terms of different binding affinities for these cations. In this study we demonstrate that vacuolar Ca2+ is a crucial regulator to restrict SV channel activity to a physiologically meaningful range, which is less than 0.1% of maximum SV channel activity.

Ca2+, Mg2+, and K+ activities in red beet (Beta vulgaris L.) vacuoles were evaluated using conventional ion-selective microelectrodes and, in the case of Ca2+, by non-invasive ion flux measurements (MIFE) as well. The mean vacuolar Ca2+ activity was ∼0.2 mM. Modulation of the slow vacuolar (SV) channel voltage dependence by Ca2+ in the absence and presence of other cations at their physiological concentrations was studied by patch-clamp in excised tonoplast patches. Lowering pH at the vacuolar side from 7.5 to 5.5 (at zero vacuolar Ca2+) did not affect the channel voltage dependence, but abolished sensitivity to luminal Ca2+ within a physiological range of concentrations (0.1–1.0 mM). Aggregation of the physiological vacuolar Na+ (60 mM) and Mg2+ (8 mM) concentrations also results in the SV channel becoming almost insensitive to vacuolar Ca2+ variation in a range from nanomoles to 0.1 mM. At physiological cation concentrations at the vacuolar side, cytosolic Ca2+ activates the SV channel in a voltage-independent manner with Kd=0.7–1.5 μM. Comparison of the vacuolar Ca2+ fluxes measured by both the MIFE technique and from estimating the SV channel activity in attached patches, suggests that, at resting membrane potentials, even at elevated (20 μM) cytosolic Ca2+, only 0.5% of SV channels are open. This mediates a Ca2+ release of only a few pA per vacuole (∼0.1 pA per single SV channel). Overall, our data suggest that the release of Ca2+ through SV channels makes little contribution to a global cytosolic Ca2+ signal.

In this work, direct effects of cytosolic polyamines on the two principle vacuolar ion channels were studied by means of patch-clamp technique. Fast and slow activating vacuolar channels were analyzed on membrane patches isolated from vacuoles of the red beet taproot. The potency of the fast and of the slow vacuolar channel blockage by polyamines decreased with a decrease of the polycation charge, spermine4+ > spermidine3+ > putrescine2+. In contrast to the inhibition of the fast vacuolar channel, the blockage of the slow vacuolar channel by polyamines displayed a pronounced voltage-dependence. Hence, in the presence of high concentration of polyamines the slow vacuolar channel was converted into a strong inward rectifier as evidenced by its unitary current-voltage characteristic. The blockage of the slow vacuolar channel by polyamines was relieved at a large depolarization, in line with the permeation of polyamines through this channel. The voltage-dependence of blockage was analyzed in terms of the conventional model, assuming a single binding site for polyamines within the channel pore. Taking advantage of a simple linear structure of naturally occurring polyamines, conclusions on a possible architecture of the slow vacuolar channel pore were drawn. The role of common polyamines in regulation of vacuolar ion transport was discussed.

The conduction properties of individual physiologically important cations Na+, K+, Mg2+, and Ca2+ were determined in the slowly activating (SV) channel of sugar beet vacuoles. Current-voltage relationships of the open channel were measured on excised tonoplast patches in a continuous manner by applying a +/-140 mV ramp-wave protocol. Applying KCl gradients of either direction across the patch we have determined that the relative Cl- to K+ permeability was < or =1%. Symmetrical increase of the concentration of tested cation caused an increase of the single channel conductance followed by saturation. Fitting of binding isotherms at zero voltage to the Michaelis-Menten equation resulted in values of maximal conductance of 300, 385, 18, and 13 pS, and of apparent dissociation constants of 64, 103, 0.04, and 0.08 mm for Na+, K+, Mg2+, and Ca2+, respectively. Deviations from the single-ion occupancy mechanism are documented, and alternative models of permeation are discussed. The magnitude of currents carried by divalent cations at low concentrations can be explained by an unrealistically wide (approximately 140 A) radius of the pore entrance. We propose instead a fixed negative charge in the pore vestibules, which concentrates the cations in their proximity. The conduction properties of the SV channel are compared with reported characteristics of voltage-dependent Ca2+-permeable channels, and consequences for a possible reduction of postulated multiplicity of Ca2+ pathways across the tonoplast are drawn.

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