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兔胆囊内的细胞内氯离子活性:钠梯度在驱动“上坡”氯离子转运中作用的直接证据。

Intracellular chloride activities in rabbit gallbladder: direct evidence for the role of the sodium-gradient in energizing "uphill" chloride transport.

作者信息

Duffey M E, Turnheim K, Frizzell R A, Schultz S G

出版信息

J Membr Biol. 1978 Sep 19;42(3):229-45. doi: 10.1007/BF01870360.

Abstract

Intracellular chloride activities, (Cl)c, in rabbit gallbladder were determined by using conventional (Kcl-filled) microelectrodes and Cl-selective, liquid ion-exchanger, microelectrodes. The results indicated that in the presence of a normal Ringer's solution, (Cl)c averages 35mM; this value is 2.3 times that predicted for an equilibrium distribution across the mucosal and baso-lateral membranes. On the other hand, when the tissue is bathed by Na-free solutions, (Cl)c declines to a value that does not differ significantly from that predicted for an equilibrium distribution. These results, together with those of Frizzell et al. (J. Gen. Physiol. 65:769, 1975) provide, for the first time, compelling evidence that (i) the movement of Cl from the mucosal solution into the cell is directed against an electrochemical potential difference (23mV); and (ii) this movement is energized by coupling to the entry of Na down a steep electrochemical potential difference. Finally, our data suggest that (i) Cl exit from the cell across the basolateral membrane may be coupled to the co-transport of a cation or the countertransport of an anion; and (ii) the mechanism responsible for active Na extrusion from the cell across the baso-lateral membrane is rheogenic (electrogenic), and is not the result of a neutral Na-K exchange.

摘要

采用传统的(填充氯化钾的)微电极和氯离子选择性液体离子交换微电极,测定了兔胆囊内的细胞内氯离子活性((Cl)c)。结果表明,在正常林格氏液存在的情况下,(Cl)c平均为35mM;该值是根据黏膜和基底外侧膜平衡分布预测值的2.3倍。另一方面,当组织用无钠溶液灌注时,(Cl)c下降到与平衡分布预测值无显著差异的值。这些结果与弗里泽尔等人(《普通生理学杂志》65:769, 1975)的结果一起,首次提供了令人信服的证据,即:(i) 氯离子从黏膜溶液进入细胞的移动是逆着电化学势差(23mV)进行的;(ii) 这种移动是通过与钠离子顺着陡峭的电化学势差进入细胞相偶联而获得能量的。最后,我们的数据表明:(i) 氯离子从细胞穿过基底外侧膜的排出可能与阳离子的协同转运或阴离子的反向转运相偶联;(ii) 负责钠离子从细胞穿过基底外侧膜主动排出的机制是生电的(电致的),而不是中性钠钾交换的结果。

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