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强直刺激后原位跨肌浆网Ca2+和Mg2+运动的电子探针X射线微量分析。

Electron probe X-ray microanalysis of post-tetanic Ca2+ and Mg2+ movements across the sarcoplasmic reticulum in situ.

作者信息

Somlyo A V, McClellan G, Gonzalez-Serratos H, Somlyo A P

出版信息

J Biol Chem. 1985 Jun 10;260(11):6801-7.

PMID:3158652
Abstract

Ca2+ and Mg2+ movements across the sarcoplasmic reticulum (SR) of frog skeletal muscle fibers were measured in situ by electron probe microanalysis of muscles rapidly frozen following a tetanus. At 400 ms following a 1.2-s tetanus at room temperature, the force had relaxed to base-line, and 0.3 mmol of Ca2+/liter of cytoplasmic H2O had been pumped by the SR, indicating that the in situ pumping of the SR Ca-ATPase is sufficiently high to account for the removal of Ca2+ from the Ca2+-specific sites of troponin (0.18 mmol of Ca2+-specific sites/liter of cytoplasmic H2O) and for the rate of relaxation from a tetanus at room temperature. The half-time of the return of the total 1.0 mmol of Ca2+/liter of cytoplasmic H2O released during a tetanus was 1.1 s, comparable to the slow Koff rate of Ca2+ from (carp) parvalbumin (1.0 s-1) and consistent with the hypothesis that the return of this Ca2+ to the terminal cisternae is rate-limited by the Ca2+ off-rate from parvalbumin. The return of the Mg2+ taken up by the terminal cisternae during a tetanus to resting levels was significantly slower than the time course of the Ca2+ movements, suggesting that the Mg2+ permeability of the SR in situ is low and may be transiently increased during tetanic stimulation.

摘要

通过对强直收缩后快速冷冻的肌肉进行电子探针微量分析,在原位测量了蛙骨骼肌纤维中钙离子(Ca2+)和镁离子(Mg2+)跨肌浆网(SR)的移动情况。在室温下进行1.2秒强直收缩后400毫秒时,张力已松弛至基线,肌浆网已将0.3毫摩尔Ca2+/升细胞质水泵出,这表明肌浆网Ca-ATP酶的原位泵浦能力足够高,足以解释从肌钙蛋白的Ca2+特异性位点去除Ca2+(0.18毫摩尔Ca2+特异性位点/升细胞质水)以及室温下强直收缩后的松弛速率。强直收缩期间释放的1.0毫摩尔Ca2+/升细胞质水中,总Ca2+返回的半衰期为1.1秒,与(鲤鱼)小清蛋白中Ca2+的缓慢解离速率(1.0秒-1)相当,并且与该Ca2+返回终末池受小清蛋白Ca2+解离速率限制的假说一致。强直收缩期间终末池摄取的Mg2+恢复到静息水平的速度明显慢于Ca2+移动的时间进程,这表明原位肌浆网对Mg2+的通透性较低,并且在强直刺激期间可能会短暂增加。

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