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The uptake of Ca2+ by liver mitochondria, when phosphate movement is inhibited, occurs when Co2 is present and not in its absence. Uptake of Ca2+ to form CaCO3 yields 2H+/Ca2+. Heart mitochondria, when phosphate movement is inhibited, will take up Ca2+ with the exact equivalent of hydroxybutyrate, lactate or acetate. By providing a carrier for Cl- with tributyltin, a stoicheiometric uptake of Cl- with the Ca2+ takes place. The uptakes appear to occur without significant pH change; there appears to be no CO2-dependent uptake into heart mitochondria. Oxygenation of anaerobic heart mitochondria, in the presence of an inhibitor of phosphate movement and of generation of phosphate from internal ATP, does not yield significant change of external acidity in relation to the amount of O2 added. Use of Bromothymol Blue as an indicator of the distribution of a weak acid anion confirms that the transient nature of the response of the dye distribution to Ca2+ is connected with movement of endogenous phosphate. Bromothymol Blue accumulated in response to Ca2+ is discharged when entry of the Ca2+ (in the presence of mersalyl) is mediated with nigericin. It is concluded that Ca2+ uptakes will occur alternatively with the equivalent of anions or in exchange for endogenous K+ and that proton production is connected with the changes of ionization of phosphate (unless phosphate movement is inhibited) and in liver mitochondria with the hydration of CO2.

Anion/calcium ion ratios and proton production in some mitochondrial calcium ion uptakes