Mechanism of sodium independent calcium efflux from rat liver mitochondria.

Abstract

On the basis of primarily two types of observations, it has been suggested that the Na+-independent Ca2+ efflux mechanism of rat liver mitochondria is a passive Ca2+-2H+ exchanger. First, when a pulse of acid is added to a suspension of mitochondria loaded with Ca2+, a pulse of intramitochondrial Ca2+ is often released, even in the presence of the inhibitor of mitochondrial Ca2+ influx, ruthenium red. Second, at a pH near 7, the stoichiometry of Ca2+ released to H+ taken up by Ca2+-loaded mitochondria, following treatment with ruthenium red, has been observed to be 1:2. This evidence for a Ca2+-2H+ exchanger is reexamined here by studying the release of Ca2+ upon acidification of the medium by addition of buffer, the dependence of liver mitochondrial Ca2+ efflux on external medium pH and intramitochondrial pH, and the Ca2+-Ca2+ exchange properties of the Ca2+ efflux mechanism. These studies show no pulse of mitochondrial Ca2+ efflux when pH is abruptly lowered by addition of buffer. The stoichiometry between Ca2+ and H+ fluxes is found to be highly pH dependent. The reported 1:2 stoichiometry between Ca2+ efflux and H+ influx is only observed at one pH. Furthermore, the rate of Ca2+ efflux from mitochondria is found to increase only very slightly at most as suspension pH is decreased. The rate of Ca2+ efflux is not found to increase with increasing intramitochondrial pH. Finally, no Ca2+-Ca2+ isotope exchange can be demonstrated over the Na+-independent efflux mechanism (i.e., in the presence of ruthenium red). It is concluded that these data do not support the hypothesis that the Na+-independent Ca2+ efflux mechanism is a passive Ca2+-2H+ exchanger.