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通过中子散射研究氘代紫膜中水合水的动力学。

Dynamics of hydration water in deuterated purple membranes explored by neutron scattering.

作者信息

Wood K, Plazanet M, Gabel F, Kessler B, Oesterhelt D, Zaccai G, Weik M

机构信息

Laboratoire de Biophysique Moléculaire, Institut de Biologie Structurale CEA-CNRS-UJF, 41 rue Jules Horowitz, 38027 Grenoble Cedex 1, France.

出版信息

Eur Biophys J. 2008 Jun;37(5):619-26. doi: 10.1007/s00249-008-0285-0. Epub 2008 Feb 20.

Abstract

The function and dynamics of proteins depend on their direct environment, and much evidence has pointed to a strong coupling between water and protein motions. Recently however, neutron scattering measurements on deuterated and natural-abundance purple membrane (PM), hydrated in H2O and D2O, respectively, revealed that membrane and water motions on the ns-ps time scale are not directly coupled below 260 K (Wood et al. in Proc Natl Acad Sci USA 104:18049-18054, 2007). In the initial study, samples with a high level of hydration were measured. Here, we have measured the dynamics of PM and water separately, at a low-hydration level corresponding to the first layer of hydration water only. As in the case of the higher hydration samples previously studied, the dynamics of PM and water display different temperature dependencies, with a transition in the hydration water at 200 K not triggering a transition in the membrane at the same temperature. Furthermore, neutron diffraction experiments were carried out to monitor the lamellar spacing of a flash-cooled deuterated PM stack hydrated in H2O as a function of temperature. At 200 K, a sudden decrease in lamellar spacing indicated the onset of long-range translational water diffusion in the second hydration layer as has already been observed on flash-cooled natural-abundance PM stacks hydrated in D2O (Weik et al. in J Mol Biol 275:632-634, 2005), excluding thus a notable isotope effect. Our results reinforce the notion that membrane-protein dynamics may be less strongly coupled to hydration water motions than the dynamics of soluble proteins.

摘要

蛋白质的功能和动力学取决于其直接环境,并且有很多证据表明水与蛋白质运动之间存在强耦合。然而,最近分别在H₂O和D₂O中水合的氘代和天然丰度紫膜(PM)的中子散射测量结果显示,在260 K以下,纳秒至皮秒时间尺度上的膜和水运动并非直接耦合(Wood等人,《美国国家科学院院刊》104:18049 - 18054, 2007)。在最初的研究中,测量的是高水合水平的样品。在此,我们分别测量了仅对应于第一层水合水的低水合水平下PM和水的动力学。与之前研究的高水合样品情况一样,PM和水的动力学表现出不同的温度依赖性,水合水在200 K时的转变并未在相同温度下引发膜的转变。此外,进行了中子衍射实验,以监测在H₂O中快速冷却的氘代PM堆叠的层间距随温度的变化。在200 K时,层间距突然减小表明在第二水合层中开始了长程平移水扩散,这与在D₂O中快速冷却的天然丰度PM堆叠中已经观察到的情况相同(Weik等人,《分子生物学杂志》275:632 - 634, 2005),因此排除了显著的同位素效应。我们的结果强化了这样一种观点,即膜蛋白动力学与水合水运动的耦合可能不如可溶性蛋白动力学那样紧密。

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