The dynamics of mitochondrial Ca fluxes

We have investigated the kinetics of mitochondrial Ca²⁺ influx and efflux and their dependence on cytosolic [Ca²⁺] and [Na⁺] using low-Ca²⁺-affinity aequorin. The rate of Ca²⁺ release from mitochondria increased linearly with mitochondrial [Ca²⁺] ([Ca²⁺]_M). Na⁺-dependent Ca²⁺ release was predominant al low [Ca²⁺]_M but saturated at [Ca²⁺]_M around 400 μM, while Na⁺-independent Ca²⁺ release was very slow at [Ca²⁺]_M below 200 μM, and then increased at higher [Ca²⁺]_M, perhaps through the opening of a new pathway. Half-maximal activation of Na⁺-dependent Ca²⁺ release occurred at 5-10 mM [Na⁺], within the physiological range of cytosolic [Na⁺]. Ca²⁺ entry rates were comparable in size to Ca²⁺ exit rates at cytosolic [Ca²⁺] ([Ca²⁺]_c) below 7 μM, but the rate of uptake was dramatically accelerated at higher [Ca²⁺]_c. As a consequence, the presence of [Na⁺] considerably reduced the rate of [Ca²⁺]_M increase at [Ca²⁺]_c below 7 μM, but its effect was hardly appreciable at 10 μM [Ca²⁺]_c. Exit rates were more dependent on the temperature than uptake rates, thus making the [Ca²⁺]_M transients to be much more prolonged at lower temperature. Our kinetic data suggest that mitochondria have little high affinity Ca²⁺ buffering, and comparison of our results with data on total mitochondrial Ca²⁺ fluxes indicate that the mitochondrial Ca²⁺ bound/Ca²⁺ free ratio is around 10- to 100-fold for most of the observed [Ca²⁺]_M range and suggest that massive phosphate precipitation can only occur when [Ca²⁺]_M reaches the millimolar range.