Interdependence of H+ and K+ fluxes during the Ca2+-pumping activity of sarcoplasmic reticulum vesicles

The release of H⁺ during the oxalate-supported Ca²⁺ uptake in sarcoplasmic reticulum vesicles is kinetically coincident with the initial phase of Ca²⁺ accumulation. The Ca²⁺ uptake is increased and the H⁺ release is decreased in the presence of KCl and other monovalent chloride salts as expected for a H⁺-monovalent cation exchange. The functioning of the Ca²⁺-pump is disturbed by the presence of potassium gluconate and, to a lesser extent, of choline chloride. These salts do not inhibit the ATPase activity of Ca²⁺-permeable vesicles, suggesting a charge imbalance inhibition which is specially relevant in the case of gluconate. Therefore, K⁺, and also Cl^–, appear to be involved in secondary fluxes during the active accumulation of Ca²⁺. The microsomal preparation seems homogeneous with respect to the K⁺-channel, showing an apparent rate constant for K⁺ release of approximately 25 s^–1 measured with the aid of⁸⁶Rb⁺ tracer under equilibrium conditions. A Rb⁺ efflux, sensitive to Ca²⁺-ionophore, can be also detected during the active accumulation of Ca²⁺. The experimental data suggest that both monovalent cations and anions are involved in a charge compensation during the Ca²⁺ uptake and H⁺ release. Fluxes of these highly permeable ions would contribute to cancel the formation of a resting membrane potential through the sarcoplasmic reticulum membrane.