Tsai J, Gerstein M, Levitt M
Department of Structural Biology, Stanford University, California 94305-5126, USA.
Protein Sci. 1997 Dec;6(12):2606-16. doi: 10.1002/pro.5560061212.
To investigate the nature of hydrophobic collapse considered to be the driving force in protein folding, we have simulated aqueous solutions of two model hydrophobic solutes, methane and isobutylene. Using a novel methodology for determining contacts, we can precisely follow hydrophobic aggregation as it proceeds through three stages: dispersed, transition, and collapsed. Theoretical modeling of the cluster formation observed by simulation indicates that this aggregation is cooperative and that the simulations favor the formation of a single cluster midway through the transition stage. This defines a minimum solute hydrophobic core volume. We compare this with protein hydrophobic core volumes determined from solved crystal structures. Our analysis shows that the solute core volume roughly estimates the minimum core size required for independent hydrophobic stabilization of a protein and defines a limiting concentration of nonpolar residues that can cause hydrophobic collapse. These results suggest that the physical forces driving aggregation of hydrophobic molecules in water is indeed responsible for protein folding.
为了研究被认为是蛋白质折叠驱动力的疏水塌缩的本质,我们模拟了两种模型疏水溶质(甲烷和异丁烯)的水溶液。使用一种确定接触的新方法,我们能够精确跟踪疏水聚集过程,该过程经历三个阶段:分散、转变和塌缩。模拟观察到的团簇形成的理论模型表明,这种聚集是协同的,并且模拟结果支持在转变阶段中期形成单个团簇。这定义了一个最小溶质疏水核心体积。我们将其与从已解析的晶体结构确定的蛋白质疏水核心体积进行比较。我们的分析表明,溶质核心体积大致估计了蛋白质独立疏水稳定所需的最小核心尺寸,并定义了可导致疏水塌缩的非极性残基的极限浓度。这些结果表明,驱动水中疏水分子聚集的物理力确实是蛋白质折叠的原因。