Slowly activating vacuolar channels can not mediate Ca2+-induced Ca2+ release

In order to test the hypothesis that slowly activating vacuolar (SV) channels mediate Ca²⁺-induced Ca²⁺ release the voltage- and Ca²⁺-dependence of these K⁺ and Ca²⁺- permeable channels were studied in a quantitative manner. The patch-clamp technique was applied to barley (Hordeum vulgare L.) mesophyll vacuoles in the whole vacuole and vacuolar-free patch configuration. Under symmetrical ionic conditions the current-voltage relationship of the open SV channel was characterized by a pronounced inward rectification. The single channel current amplitude was not affected by changes in cytosolic Ca²⁺ whereas an increase in vacuolar Ca²⁺ decreased the unitary current in a voltage-dependent manner. The SV channel open-probability increased with positive potentials and elevated cytosolic Ca²⁺, but not with elevated cytosolic Mg²⁺. An increase of cytosolic Ca²⁺ shifted the half-activation potential to more negative voltages, whereas an increase of vacuolar Ca²⁺ shifted the half-activation potential to more positive voltages. At physiological vacuolar Ca²⁺ activities (50 μM to 2 mM) changes in cytosolic Ca²⁺ (5 μM to 2 mM) revealed an exponential dependence of the SV channel open-probability on the electrochemical potential gradient for Ca²⁺ (Δμ_Ca). At the Ca²⁺ equilibrium potential (Δμ_Ca = 0) the open-probability was as low as 0.4%. Higher open-probabilities required net Ca²⁺ motive forces which would drive Ca²⁺ influx into the vacuole. Under conditions favouring Ca²⁺ release from the vacuole, however, the open-probability further decreased. Based on quantitative analysis, it was concluded that the SV channel is not suited for Ca²⁺-induced Ca²⁺ release from the vacuole.