| Abstract: | The rate of Ca2+ efflux was determined with 45Ca2+ -loaded sarcoplasmic reticulum vesicles (mainly with the light fraction of vesicles) at pH 6.5 and 0 degrees C. The efflux depended on external Ca2+, Mg2+, ATP and ADP, but it was not activated by AMP. The results indicate that the efflux is derived from Ca2+ -Ca2+ exchange mediated by the phosphoenzyme (EP) of membrane-bound Ca2+ -ATPase. EP was formed with Ca2+ -loaded vesicles (light fraction) under similar conditions without added ADP. The subsequent addition of EGTA and ADP induced triphasic EP dephosphorylation. Three species of EP (EP1, EP2, and EP3) were distinguished on the basis of this dephosphorylation kinetics, EP1, EP2, and EP3, corresponding to the first, second, and third phases of the dephosphorylation. Dephosphorylation of EP1 and EP2 resulted in stoichiometric ATP formation, while dephosphorylation of EP3 led to stoichiometric Pi liberation. The rate of Ca2+ efflux was compatible with that of EP2 dephosphorylation, whereas it was much lower than the rate of EP1 dephosphorylation and much higher than the rate of EP3 dephosphorylation. The intravesicular Ca2+ concentration dependence of the rate of EP2 dephosphorylation agreed with that of the rate of Ca2+ efflux. The results suggest that isomerization between EP1 and EP2 is the rate-limiting process in the Ca2+ -Ca2+ exchange and that EP3 is not involved in this exchange. |
