Park Sheldon, Saven Jeffery G
Makineni Theoretical Laboratories, Department of Chemistry, University of Pennsylvania, Philadelphia, Pennsylvania 19104, USA.
Proteins. 2005 Aug 15;60(3):450-63. doi: 10.1002/prot.20511.
Buried solvent molecules are common in the core of globular proteins and contribute to structural stability. Folding necessitates the burial of polar backbone atoms in the protein core, whose hydrogen-bonding capacities should be satisfied on average. Whereas the residues in alpha-helices and beta-sheets form systematic main-chain hydrogen bonds, the residues in turns, coils and loops often contain polar atoms that fail to form intramolecular hydrogen bonds. The statistical analysis of 842 high resolution protein structures shows that well-resolved, internal water molecules preferentially reside near residues without alpha-helical and beta-sheet secondary structures. These buried waters most often form primary hydrogen bonds to main-chain atoms not involved in intramolecular hydrogen bonds, providing strong evidence that hydrating main-chain atoms is a key structural role of buried water molecules. Additionally, the average B-factor of protein atoms hydrogen-bonded to waters is smaller than that of protein atoms forming intramolecular hydrogen bonds, and the average B-factor of water molecules involved in primary hydrogen bonds with main-chain atoms is smaller than the average B-factor of water molecules involved in secondary hydrogen bonds to protein atoms that form concurrent intramolecular hydrogen bonds. To study the structural coupling between internal waters and buried polar atoms in detail we simulated the dynamics of wild-type FKBP12, in which a buried water, Wat137, forms one side-chain and multiple main-chain hydrogen bonds. We mutated E60, whose side-chain hydrogen bonds with Wat137, to Q, N, S or A, to modulate the multiplicity and geometry of hydrogen bonds to the water. Mutating E60 to a residue that is unable to form a hydrogen bond with Wat137 results in reorientation of the water molecule and leads to a structural readjustment of residues that are both near and distant to the water. We predict that the E60A mutation will result in a significantly reduced affinity of FKBP12 for its ligand FK506. The propensity of internal waters to hydrogen bond to buried polar atoms suggests that ordered water molecules may constitute fundamental structural components of proteins, particularly in regions where alpha-helical or beta-sheet secondary structure is not present.
埋藏的溶剂分子在球状蛋白质的核心部位很常见,有助于结构稳定性。蛋白质折叠需要将极性主链原子埋藏在蛋白质核心中,其氢键结合能力平均应得到满足。虽然α-螺旋和β-折叠中的残基形成系统的主链氢键,但转角、卷曲和环中的残基通常含有未能形成分子内氢键的极性原子。对842个高分辨率蛋白质结构的统计分析表明,解析良好的内部水分子优先位于没有α-螺旋和β-折叠二级结构的残基附近。这些埋藏的水分子最常与不参与分子内氢键的主链原子形成一级氢键,有力地证明了水合主链原子是埋藏水分子的关键结构作用。此外,与水形成氢键的蛋白质原子的平均B因子小于形成分子内氢键的蛋白质原子的平均B因子,与主链原子形成一级氢键的水分子的平均B因子小于与形成同时存在的分子内氢键的蛋白质原子形成二级氢键的水分子的平均B因子。为了详细研究内部水分子与埋藏的极性原子之间的结构耦合,我们模拟了野生型FKBP12 的动力学,其中一个埋藏的水分子Wat137 形成一个侧链和多个主链氢键。我们将与Wat137 形成侧链氢键 的E60 突变为Q、N、S 或A,以调节与水的氢键的多重性和几何形状。将E60 突变为无法与Wat137 形成氢键的残基会导致水分子重新定向,并导致与水附近和远处的残基发生结构调整。我们预测E60A 突变将导致FKBP12 对其配体FK506 的亲和力显著降低。内部水分子与埋藏的极性原子形成氢键的倾向表明,有序水分子可能构成蛋白质的基本结构成分,特别是在不存在α-螺旋或β-折叠二级结构的区域。