Khananshvili D, Weil-Maslansky E
Department of Physiology and Pharmacology, Sackler School of Medicine, Tel-Aviv University, Ramat-Aviv, Israel.
Biochemistry. 1994 Jan 11;33(1):312-9. doi: 10.1021/bi00167a041.
The exchange cycle of the cardiac Na(+)-Ca2+ exchanger can be described as separate steps of Ca2+ and Na+ transport [Khananshvili, D. (1990) Biochemistry 29, 2437-2442]. In order to determine the relative rates of Na+ and Ca2+ movement during the Na(+)-Ca2+ and Ca(2+)-Ca2+ exchange modes, the ratios (R) of Na(+)-Ca2+/Ca(2+)-Ca2+ exchanges were estimated with saturating concentrations of ions at both sides of the membrane. The effect of extravesicular pH and voltage (potassium valinomycin) on the initial rates (t = 1 s) of Na(+)-Ca2+ and Ca(2+)-Ca2+ exchange were investigated by assuming that, under the conditions tested, the intravesicular pH (pH 7.4) is not affected. Na(+)- or Ca(2+)-preloaded sarcolemma vesicles were diluted rapidly in assay medium containing 45Ca and buffer (pH 5.0-10.9), and the reaction of 45Ca uptake was quenched by using a semi-rapid-mixing device. Under conditions in which [45Ca]o = [Ca]i = 250 microM, the pH-dependent curve of Ca(2+)-Ca2+ exchange shows a bell shape in the acidic range (pKa1 = 5.1 +/- 0.1 and pKa2 = 6.5 +/- 0.2) followed by activation of the exchange in the alkaline range (pKa3 = 10.0 +/- 0.2). With [45Ca]o = 250 microM and [Na]i = 160 mM, the Na(+)-Ca2+ exchange increases monotonically from pH 5.0 to 9.5 (pKa1 = 5.1 +/- 0.1, pKa2 = 7.2 +/- 0.2, and pKa3 = 9.1 +/- 0.2). At pH < 6.1, the ratio of Na(+)-Ca2+/Ca(2+)-Ca2+ exchange is close to unity (R approximately 1), while it increases to R = 3-4 in the range of pH 7.1-9.3.(ABSTRACT TRUNCATED AT 250 WORDS)
心脏钠钙交换体的交换循环可描述为钙和钠转运的独立步骤[Khananshvili, D. (1990) Biochemistry 29, 2437 - 2442]。为了确定钠钙交换和钙钙交换模式下钠和钙移动的相对速率,在膜两侧离子浓度饱和的情况下估算钠钙交换/钙钙交换的比率(R)。通过假设在所测试的条件下泡内pH(pH 7.4)不受影响,研究了细胞外pH和电压(缬氨霉素钾)对钠钙交换和钙钙交换初始速率(t = 1 s)的影响。将钠预载或钙预载的肌膜囊泡在含有45Ca和缓冲液(pH 5.0 - 10.9)的测定培养基中快速稀释,并使用半快速混合装置淬灭45Ca摄取反应。在[45Ca]o = [Ca]i = 250 microM的条件下,钙钙交换的pH依赖性曲线在酸性范围内呈钟形(pKa1 = 5.1 ± 0.1和pKa2 = 6.5 ± 0.2),随后在碱性范围内交换被激活(pKa3 = 10.0 ± 0.2)。当[45Ca]o = 250 microM且[Na]i = 160 mM时,钠钙交换从pH 5.0到9.5单调增加(pKa1 = 5.1 ± 0.1,pKa2 = 7.2 ± 0.2,pKa3 = 9.1 ± 0.2)。在pH < 6.1时,钠钙交换/钙钙交换的比率接近1(R约为1),而在pH 7.1 - 9.3范围内增加到R = 3 - 4。(摘要截于250字)