The time course of Ca
2+ uptake by the SR was compared with those of formation and decomposition of a phosphorylated intermediate, EP, in the Ca
2+, Mg
2+-dependent ATPase reaction [EC 3. 6. 1. 3]. Ca
2+ uptake was measured by the Millipore filtration method, using
45CaCl
2 as a substrate. The SR was allowed to react with 10μM ATP at 0°C in the presence of 20μM CaCl
2 without adding MgCl
2. Under the conditions used, the formation and decomposition of EP could be measured separately, since the rate of EP formation was much higher than that of its decomposition. The following results were obtained.
1. When EP formation and Ca
2+ uptake by the SR were terminated by adding 1mM EGTA+2.5mM MgCl
2, EP was rapidly decomposed into E+P
i. Ca
2+ uptake consisted of two phases: a rapid, initial one and a slow, steady one, which was almost linear with time. The time course of the former corresponded to that of EP formation, and that of the latter to P
i liberation before the addition of EGTA+MgCl
2. During both phases, the molar ratio of Ca
2+ uptake/ATP hydrolysis was about 1/1.
2. When the reaction was stopped by adding 1mM EGTA+0.25mM ADP, ATP was formed immediately from EP and ADP. The time course of Ca
2+ uptake showed only a slow, steady phase, corresponding to that of P
i liberation before the addition of EGTA+ADP. The molar ration of Ca
2+ uptake/ATP hydrolysis was smaller than 1/1.
3. After Ca
2+ uptake had been stopped by adding 1Mm EGTA+10μM ADP, the time course of release of Ca
2+ ions from the SR was measured by adding 20mM MgCl
2 after various intervals, since the release was stopped by adding MgCl
2. The time course observed corresponded to that of disappearance of EP.
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