The sarcoplasmic reticulum Ca(2+)-ATPase transports Ca(2+) using the energy derived from ATP hydrolysis. During catalysis, part of the energy is used to translocate Ca(2+) across the membrane, and part is dissipated as heat. At 35 degrees C the heat released during the hydrolysis of each ATP molecule varies depending on the formation of a Ca(2+) gradient across the membrane. With leaky vesicles (no gradient) the heat released varies between 9 and 12 kcal/mol of ATP cleaved, and with intact vesicles (gradient), the heat released increases to 20-24 kcal/mol of ATP. After Ca(2+) accumulation, 82% of the Ca(2+)-ATPase activity is not coupled to Ca(2+) transport, and the ratio between Ca(2+) transported and ATP cleaved is 0.3. The addition of 20% dimethyl sulfoxide (v/v) to the medium or decreasing the temperature from 35 to 20 degrees C abolishes the difference of heat produced during ATP hydrolysis in the presence and absence of a gradient. This is accompanied by a simultaneous inhibition of the uncoupled ATPase activity and an increase of the Ca(2+)/ATP ratio from 0.3 to 1.3-1.4. It is concluded that the uncoupled Ca(2+)-ATPase is responsible for both the low Ca(2+)/ATP ratio measured during transport and the difference of heat produced during ATP hydrolysis in the presence and absence of a gradient.
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Barata et al. (2002) studied this question.
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