在K+通道的选择性过器周围的水占用率的定量分析,在不同的封闭模式下
Markus Weingarth1, Elwin A W van der Cruijsen, Jared Ostmeyer
1NMR Spectroscopy, Bijvoet Center for Biomolecular Research, Department of Chemistry, Faculty of Science, Utrecht University , 3584 CH Utrecht, The Netherlands.
Journal of the American Chemical Society
|January 14, 2014
概括
由于埋藏的水分子,通道的恢复速度很慢. 这些水分子在无活性状态下存在,但在导电状态下不存在,解释了缓慢的动力学.
科学领域:
- 生物物理学的生物物理.
- 结构生物学 结构生物学
- 离子通道功能的功能
背景情况:
- 从无活化中恢复 (K+) 通道非常缓慢,发生在几秒钟内.
- 假设这种缓慢的恢复与水分子在道的选择性过器中的行为有关.
- 以前的研究表明埋水有作用,但缺乏直接的实验证据.
研究的目的:
- 阐明水分子在选择性过器背后在K+通道缓慢恢复中的作用.
- 绘制一个嵌入膜的K+通道在不同封闭状态中的水的空间和时间分布图.
- 提供直接的实验证据,证明水对通道关动力学的影响.
主要方法:
- 固态核磁共振 (ssNMR) 谱学,包括在完全质子化通道上的质子检测ssNMR.
- 长分子动力学 (MD) 模拟.
- 计算和实验方法的整合.
主要成果:
- 一张高分辨率的地图显示,在非激活的选择性过器后面存在具有较长停留时间的埋水分子,这解释了缓慢的恢复.
- 过器后面的区域在导电状态下被湿.
- 在埋藏和散装水之间确定了一条水交换通道,这对于功能影响至关重要.
- 观察到围绕过器的额外有序的水分子,通过通道门调节.
结论:
- 在选择性过器后面,埋藏的水分子具有很长的停留时间,这就是K+通道缓慢恢复动力学的原因.
- 这种埋水的存在和缺失直接影响了道的功能.
- 水分子在K+通道封闭和失活中起着关键的,动态调节的作用.
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