The Ca2+ permeability of sarcoplasmic reticulum vesicles I. Ca2+ outflow in the non-energized state of the calcium pump

Passive Ca²⁺ permeability of sarcoplasmic reticulum vesicles has been studied after maximal loading with Ca²⁺ (150–200 nmol/mg protein) in the presence of Ca²⁺, MgATP and an ATP generating system of limited capacity. Outflow of accumulated Ca²⁺ in the non-energized state of the system was studied by depletion of the medium of one of the substrates, either MgATP (by complete consumption) or Ca²⁺ (by complexation with EGTA). It was found that Ca²⁺ outflow under these conditions is relatively slow and independent of the medium concentration of Ca²⁺ (5·10^?9–5·10^?5 M) or MgATP (0.7–730 μM). Outflow curves were steep at the beginning of the outflow phase (30–60 nmol/min per mg protein), and outflow proceeded at a much lower rate below 100 nmol Ca²⁺/mg protein. Outflow could be completely inhibited by La³⁺. The Ca²⁺ release curves are not compatible with simple diffusion, and cannot be accounted for by Ca²⁺ binding inside the vesicles. Neither are our observations consistent with permeation mediated via the Ca²⁺ translocation sites involved in active transport. We suggest that non-energized Ca²⁺ outflow may proceed by a process of ion-exchange through negatively charged, water-filled channels in the membrane, the properties of which are altered by a high intravesicular concentration of Ca²⁺.