State of translocated Ca2+ by sarcoplasmic reticulum inferred from kinetic analysis of calcium oxalate precipitation

Uptake of Ca²⁺ by sarcoplasmic reticulum in the presence of oxalate displays biphasic kinetics. An initial phase of normal uptake is followed by a second phase coincident with precipitation of calcium oxalate inside the vesicles. The precipitation rate induced by actively transported Ca²⁺ is depressed by increasing the added Ca²⁺ concentration. This correlates linearly with the reciprocal of precipitation rate. Therefore, a maximal limit rate could be extrapolated at zero Ca²⁺ ($\text{V}{}_0$). The rate of precipitation, also a function of added amount protein, gives a linear correlation in a double reciprocal plot. Thus, it was possible to estimate the maximal precipitation rate occurring at infinite protein concentration ($\text{V}{}^{\mathrm{\infty }}$). With the combined extrapolated values a maximal expected precipitation rate could be calculated ($\text{V}{}_0{}^{\mathrm{\infty }}$). Kinetics of calcium oxalate precipitation was studied in the absence of calcium uptake and empirical equations relating the rate of precipitation with the added Ca²⁺ were established. Entering $\text{V}{}_0{}^{\mathrm{\infty }}$ in the equations, an internal free Ca²⁺ concentration of approx. 2.5 mM was estimated. Additionally, it is shown that the ionophore X-537A does not supress the Ca²⁺ uptake, if added during the oxalate-dependent phase, albeit the uptake proceeds at a slower rate after the release of approx. 70 nmol Ca²⁺/mg protein. This amount presumably equals the internal free Ca²⁺ not sequestered by oxalate, producing a maximal concentration approx. 14 mM. Taking into account low affinity binding of internal binding sites and the transmembrane Ca²⁺ gradients built up during the uptake of Ca²⁺, values of free Ca²⁺ ranging from 3 to 6 mM, approaching those estimated by the precipitation analysis, could be estimated.