Transport and control of Ca2+ by pigeon erythrocytes. I. Survey of some cell responses to a range of A23187 doses in the presence of Ca2+

Cells were subjected to a range of 45Ca2+ influx loads with A23187. We measured cell 45Ca2+ with time and A23187 dose, and the apparent 45Ca2+ influxes (identical to "J(in,app)") at Ca2+ steady state. We also measured endogeneous exchangeable and total cell Ca2+, which were 50 and 17-220 microM respectively. The effects of A23187 and Ca2+ on cell ATP, swelling, net Cl- permeability, and cell morphology were measured. These were modest and do not affect our conclusions. J(in,app) congruent to 3 X 10(-4) A23187]2.9 X Ca2+(o)]mumoles/l X min with 92-552 microM Ca2+(o)] (identical to external Ca2+ concentration) and 0-7 microM A23187. J(in,app) was increased an order of magnitude by vanadate and is probably much less than the true influx. The least unlikely explanation found for the high A23187] exponent, 2.9, was that most of the Ca2+ crossing the membrane is expelled by the pump before it can move deeper into the cell. Calcium pumping increased rapidly in response to increased influx, but the steady state cell 45Ca2+ was approximately proportional to J(in,app) rather than approximately constant between 10 and 120 mumoles/l X min with 184 microM Ca2+(o)]. This is not the result expected from a simple feedback mechanism. At high A23187 doses the pump appears fully activated resulting in a linear relation between cell/medium 45Ca2+ and A23187]-2. From the plot we calculated alpha identical to free/total exchangeable Ca2+ = 0.38 +/- 0.08 (n = 3) and a maximum pump rate, "Pmax" = 78 mumole/l X min. Pmax is underestimated insofar as J(in,app) is less than the true influx.