Ca++-ionophore-induced dissipation of intracellular proton gradients in rat thymocytes

Rat thymocytes incorporate large amounts of acridine orange at concentrations of approximately 10 microM in about 10 minutes at 37 degrees C. The addition of (NH4)2SO4 (at a final concentration of several mMolars) releases about 30% of the incorporated dye into the medium. The NH4+-releasable dye uptake is almost completely abolished by 20 minutes' incubation with 4 microM of the Ca++-ionophore A23187. Dye uptake is associated with an absorbance change at 492 mm and thus may be followed spectrophotometrically. However, NH4+ at the above concentrations or nigericin (0.5 mg/ml) completely annul this change in absorbance, indicating that it reflects only the accumulation of the dye within the acidic cellular compartments. In a Ca++-containing physiological saline, the addition of A23187 (at a final concentration of 8 microM) at the end of the dye uptake phase initiated a reversal in the absorbance change; in the absence of Ca++, reversal occurred at a much lower rate. Incubation of cells for 30 minutes with 2 microM A23187 in Ca++-containing saline completely abolished NH4+-sensitive dye uptake; less A23187 (0.5 microM) and like or a longer incubation period brought about a striking decrease in NH4+-sensitive dye uptake. Similar results were obtained with cells suspended in RPLM 1640 medium. In the absence of external Ca++, A23187 impaired cell capacity to incorporate dye in a delta pH-dependent manner, but a longer incubation time or higher concentrations of the ionophore were required to obtain a comparable effect. It is thus concluded that the ionophore dissipates intracellular pH gradients by an intracellular divalent cation (Ca++ or also Mg++)-H+ exchange.