Jans Danny, De Weer Paul, Srinivas S P, Larivière Els, Simaels Jeannine, Van Driessche Willy
Laboratory of Physiology, K. U. Leuven, Campus Gasthuisberg O/N, B-3000 Leuven, Belgium.
J Physiol. 2002 May 15;541(Pt 1):91-101. doi: 10.1113/jphysiol.2001.013199.
Polarized renal A6 epithelia respond to hyposmotic shock with an increase in transepithelial capacitance (C(T)) that is inhibited by extracellular Mg(2+). Elevation of free cytosolic [Ca(2+)] (Ca(2+)) is known to increase C(T). Therefore, we examined Ca(2+) dynamics and their sensitivity to extracellular Mg(2+) during hyposmotic conditions. Fura-2-loaded A6 monolayers, cultured on permeable supports were subjected to a sudden reduction in osmolality at both the basolateral and apical membranes from 260 to 140 mosmol (kg H(2)O)(-1). Reduction of apical osmolality alone did not affect Ca(2+). In the absence of extracellular Mg(2+), the hyposmotic shock induced a biphasic rise in Ca(2+). The first phase peaked within 40 s and Ca(2+) increased from 245 +/- 12 to 606 +/- 24 nM. This phase was unaffected by removal of extracellular Ca(2+), but was abolished by activating P2Y receptors with basolateral ATP or by exposing the cells to the phospholipase C (PLC) inhibitor U73122 prior to the osmotic shock. Suramin also severely attenuated this first phase, suggesting that the first phase of the Ca(2+) rise followed swelling-induced ATP release. The PLC inhibitor, the ATP treatment or suramin did not affect a second rise of Ca(2+) to a maximum of 628 +/- 31 nM. The second phase depended on Ca(2+) in the basolateral perfusate and was largely suppressed by 2 mM basolateral Mg(2+). Acute exposure of the basolateral membrane to Mg(2+) during the upstroke of the second phase caused a rapid decline in Ca(2+). Basolateral Mg(2+) inhibited Ca(2+) entry in a dose-dependent manner with an inhibition constant (K(i)) of 0.60 mM. These results show that polarized A6 epithelia respond to hyposmotic shock by Ca(2+) release from inositol trisphosphate-sensitive stores, followed by basolateral Ca(2+) influx through a Mg(2+)-sensitive pathway. The second phase of the Ca(2+) response is independent of the initial intracellular Ca(2+) release and therefore constitutes non-capacitative Ca(2+) entry.
极化的肾A6上皮细胞对低渗休克的反应是跨上皮电容(C(T))增加,而细胞外Mg(2+)可抑制这种增加。已知游离胞质[Ca(2+)](Ca(2+))升高会增加C(T)。因此,我们研究了低渗条件下Ca(2+)的动态变化及其对细胞外Mg(2+)的敏感性。在可渗透支持物上培养的用Fura-2负载的A6单层细胞,其基底外侧膜和顶端膜的渗透压突然从260 mosmol(kg H(2)O)(-1)降至140 mosmol(kg H(2)O)(-1)。仅降低顶端渗透压不会影响Ca(2+)。在没有细胞外Mg(2+)的情况下,低渗休克诱导Ca(2+)出现双相升高。第一阶段在40秒内达到峰值,Ca(2+)从245±12 nM增加到606±24 nM。该阶段不受细胞外Ca(2+)去除的影响,但在用基底外侧ATP激活P2Y受体或在渗透压休克前将细胞暴露于磷脂酶C(PLC)抑制剂U73122时被消除。苏拉明也严重减弱了这第一阶段,表明Ca(2+)升高的第一阶段是由肿胀诱导的ATP释放引起的。PLC抑制剂、ATP处理或苏拉明均不影响Ca(2+)的第二次升高,其最大值为628±31 nM。第二阶段依赖于基底外侧灌流液中的Ca(2+),并在很大程度上被2 mM基底外侧Mg(2+)抑制。在第二阶段上升过程中,基底外侧膜急性暴露于Mg(2+)会导致Ca(2+)迅速下降。基底外侧Mg(2+)以剂量依赖方式抑制Ca(2+)内流,抑制常数(K(i))为0.60 mM。这些结果表明,极化的A6上皮细胞通过从肌醇三磷酸敏感储存库释放Ca(2+)来响应低渗休克,随后通过Mg(2+)敏感途径进行基底外侧Ca(2+)内流。Ca(2+)反应的第二阶段独立于初始的细胞内Ca(2+)释放,因此构成非容量性Ca(2+)内流。
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