Abstract-Ca2ϩ influx via Ca 2ϩ current (I Ca ) during the action potential (AP) was determined at 25°C and 35°C in isolated rabbit ventricular myocytes using AP clamp. Contaminating currents through Na ϩ and K ϩ channels were eliminated by using Na ϩ -and K ϩ -free solutions, respectively. DIDS (0.2 mmol/L) was used to block Ca 2ϩ -activated chloride current (I Cl(Ca) ). When the sarcoplasmic reticulum (SR) was depleted of Ca 2ϩ by preexposure to 10 mmol/L caffeine, total Ca 2ϩ entry via I Ca during the AP was Ϸ12 mol/L cytosol (at both 25°C and 35°C). Similar Ca 2ϩ influx at 35°C and 25°C resulted from a combination of higher and faster peak I Ca , offset by more rapid I Ca inactivation at 35°C. During repeated AP clamps, the SR gradually fills with Ca 2ϩ , and consequent SR Ca 2ϩ release accelerates I Ca inactivation during the AP. During APs and contractions in steady state, total Ca 2ϩ influx via I Ca was reduced by Ϸ50% but was again unaltered by temperature (5.6Ϯ0.2 mol/L cytosol at 25°C, 6.0Ϯ0.2 mol/L cytosol at 35°C). Thus, SR Ca 2ϩ release is responsible for sufficient I Ca inactivation to cut total Ca 2ϩ influx in half. However, because of the kinetic differences in I Ca , the amount of Ca 2ϩ influx during the first 10 ms, which presumably triggers SR Ca 2ϩ release, is much greater at 35°C. I Ca during a first pulse, given just after the SR was emptied with caffeine, was subtracted from I Ca during each of 9 subsequent pulses, which loaded the SR. These difference currents reflect I Ca inactivation due to SR Ca 2ϩ release and thus indicate the time course of local [Ca 2ϩ ] in the subsarcolemmal space near Ca 2ϩ channels produced by SR Ca 2ϩ release (eg, maximal at 20 ms after the AP activation at 35°C). Furthermore, the rate of change of this difference current may reflect the rate of SR Ca 2ϩ release as sensed by L-type Ca 2ϩ channels. These results suggest that peak SR Ca 2ϩ release occurs within 2.5 or 5 ms of AP upstroke at 35°C and 25°C, respectively. I Cl(Ca) might also indicate local [Ca 2ϩ ], and at 35°C in the absence of DIDS (when I Cl(Ca) is prominent), peak I Cl(Ca) also occurred at a time comparable to the peak I Ca difference current. We conclude that SR Ca 2ϩ release decreases the Ca 2ϩ influx during the AP by Ϸ50% (at both 25°C and 35°C) and that changes in I Ca (and I Cl(Ca) ), which depend on SR Ca 2ϩ release, provide information about local subsarcolemmal [Ca 2ϩ ]. The full text of this article is available at http://www.circresaha.org. (Circ Res. 1999;85:e7-e16.)