The effects of the alkali metal ions Na+, K+, Rb+, and Cs+ on ATP-dependent Ca2+ uptake, [3H]Inositol 1,4,5-trisphosphate (InsP3) binding, and quantal InsP3-induced Ca2+ release were investigated using rat cerebellar microsomes. Both the ion species and concentration affected the ability of the microsomes to support Ca2+ uptake with K+ being mot effective (3.8 nmol of Ca2+/min/mg at 100 mM K+). The order of efficacy of the other ions was as follows: K+ > Na+ > Rb+ = Cs+ >> Li+. The binding of [3H]InsP3 to cerebellar microsomes was, however, affected little by the presence of these ions. All these alkali metal ions (except Li+) supported InsP3-induced Ca2+ release at concentrations above 25 mM; however, the extent of Ca2+ release (expressed as a percent Ca2+ release compared with that released by the ionophore A23187) was dependent upon the ion species present. Again K+ was more potent than the other ions at facilitating InsP3-induced Ca2+ release (order of efficacy: K+ > Rb+ > Na+ > Cs+), although the concentration of InsP3 required to induce half-maximal Ca2+ release (IC50) was not significantly altered. Over the ion concentration range tested (25-100 mM), the extent of InsP3-induced Ca2+ release with both K+ and Rb+ increased in a linear fashion, while Na+ showed only a slight increase and Cs+ showed no increase over this range. The effect of K+ concentration on quantal Ca2+ release was to alter the extent of release rather than the IC50 InsP3 concentration. Using stopped-flow techniques, the effects of InsP3 and K+ concentrations on the kinetics of InsP3-induced Ca2+ release were shown to exhibit a monoexponential process in this microsomal preparation. The rate constants for Ca2+ release increased with InsP3 concentration (0.11 s-1 at 0.02 microM InsP3 to 0.5 s-1 at 40 microM InsP3); however, the relationship between the fractional extent of release and rate constants for release did not change in a similar way with InsP3 concentration. Although the fractional extent of Ca2+ release increased with K+ concentration, the rate constants for release over this K+ concentration range were unaffected. This observation leads us to question the role of K+ as a counter ion required for Ca2+ release, and we therefore postulate a role for K+ (and the other alkali metal ions) as a "co-factor" required for channel opening.