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斯坦因和摩尔奖演讲。脱辅基肌红蛋白的熔球态中间体与蛋白质折叠过程。

Stein and Moore Award address. The molten globule intermediate of apomyoglobin and the process of protein folding.

作者信息

Barrick D, Baldwin R L

机构信息

Department of Biochemistry, Beckman Center, Stanford University, California 94305-5307.

出版信息

Protein Sci. 1993 Jun;2(6):869-76. doi: 10.1002/pro.5560020601.

Abstract

The molten globule model for the beginning of the folding process, which originated with Kuwajima's studies of alpha-lactalbumin (Kuwajima, K., 1989, Proteins Struct. Funct. Genet. 6, 87-103, and references therein), states that, for those proteins that exhibit equilibrium molten globule intermediates, the molten globule is a major kinetic intermediate near the start of the folding pathway. Pulsed hydrogen-deuterium exchange measurements confirm this model for apomyoglobin (Jennings, P.A. & Wright, P.E., in prep.). The energetics of the acid-induced unfolding transition, which have been determined by fitting a minimal three-state model (N<-->I<-->U; N = native, I = molten globule intermediate, U = unfolded) show that I is more stable than U at neutral pH (Barrick, D. & Baldwin, R.L., 1993, Biochemistry 32, in press), which provides an explanation for why I is formed from U at the start of folding. Hydrogen exchange rates measured by two-dimensional NMR for individual peptide NH protons, taken together with the CD spectrum of I, indicate that moderately stable helices are present in I at the locations of the A, G, and H helices of native myoglobin (Hughson, F.M., Wright, P.E., & Baldwin, R.L., 1990, Science 249, 1544-1548). Directed mutagnesis experiments indicate that the interactions between the A, G, and H helices in I are loose (Hughson, F.M., Barrick, D., & Baldwin, R.L., 1991, Biochemistry 30, 4113-4118), which can explain why I is formed rapidly from U at the start of folding.(ABSTRACT TRUNCATED AT 250 WORDS)

摘要

折叠过程起始阶段的熔球模型源于久岛对α-乳白蛋白的研究(久岛,K.,1989年,《蛋白质结构、功能与遗传学》6,87 - 103,及其中参考文献),该模型指出,对于那些呈现平衡熔球中间体的蛋白质,熔球是折叠途径起始附近的主要动力学中间体。脉冲氢 - 氘交换测量证实了脱辅基肌红蛋白的这一模型(詹宁斯,P.A.和赖特,P.E.,正在准备中)。通过拟合一个最小化的三态模型(N<-->I<-->U;N = 天然态,I = 熔球中间体,U = 未折叠态)所确定的酸诱导去折叠转变的能量学表明,在中性pH条件下I比U更稳定(巴里克,D.和鲍德温,R.L.,1993年,《生物化学》32,即将发表),这解释了为什么在折叠起始时I是由U形成的。通过二维核磁共振测量的单个肽NH质子的氢交换速率,连同I的圆二色光谱表明,在天然肌红蛋白的A、G和H螺旋位置,I中存在适度稳定的螺旋(休森,F.M.,赖特,P.E.和鲍德温,R.L.,1990年,《科学》249,1544 - 1548)。定点诱变实验表明,I中A、G和H螺旋之间的相互作用是松散的(休森,F.M.,巴里克,D.和鲍德温,R.L.,1991年,《生物化学》30,4113 - 4118),这可以解释为什么在折叠起始时I能迅速由U形成。(摘要截短于250字)

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