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DNA识别中的水分子II:色氨酸操纵子结构与水合作用的分子动力学视角

Water molecules in DNA recognition II: a molecular dynamics view of the structure and hydration of the trp operator.

作者信息

Bonvin A M, Sunnerhagen M, Otting G, van Gunsteren W F

机构信息

Laboratory of Physical Chemistry, Swiss Federal Institute of Technology Zürich, Zürich, CH-8092, Switzerland.

出版信息

J Mol Biol. 1998 Oct 2;282(4):859-73. doi: 10.1006/jmbi.1998.2034.

Abstract

The structure and hydration of the DNA duplex d-(AGCGTACTAGTACGCT)2 corresponding to the trp operator fragment used in the crystal structure of the half site complex (PDB entry 1TRR) was studied by a 1.4 ns molecular dynamics simulation in water. The simulation, starting from a B-DNA conformation, used a non-bonded cutoff of 1.4 nm with a reaction field correction and resulted in a stable trajectory. The average DNA conformation obtained was closer to the ones found in the crystal structures of the complexes (PDB entries 1TRO and 1TRR) than to the crystal structure of unbound trp operator (Nucleic Acid Database entry BDJ061). The DNA hydration was characterized in terms of hydrogen bond percentages and corresponding residence times. The residence times of water molecules within 0.35 nm of the DNA non-exchangeable protons were calculated for comparison with NMR measurements of intermolecular water-DNA NOEs and nuclear magnetic relaxation dispersion measurements. No significant difference was found between major and minor groove hydration. The DNA donors and acceptors were hydrogen bonded to water molecules for 77(+/-19)% of the time on average. The average residence time of the hydrogen bonded water molecules was 11(+/-11) ps with a maximum of 223 ps. When all water molecules within NOE distance (0.35 nm) of non-exchangeable protons were considered, the average residence times increased to an average of 100(+/-4) ps and a maximum of 608 ps. These results agree with the experimental NMR results of Sunnerhagen et al. which did not show any evidence for water molecules bound with more than 1 ns residence time on the DNA surface. The exchange of hydration water from the DNA occurred in the major groove primarily through direct exchange with the bulk solvent, while access to and from the minor groove frequently proceeded via pathways involving ribose O3' and O4' and phosphate O2P oxygen atoms. The most common water diffusion pathways in the minor groove were perpendicular to the groove direction. In general, water molecules visited only a limited number of sites in the DNA grooves before exiting. The hydrogen bonding sites, where hydrogen bonds could be formed with donor and acceptor groups of the DNA, were filled with water molecules with an average B-factor value of 0.58 mn2. No special values were observed at any of the sites, where water molecules were observed both in the trp repressor/operator co-crystals and in the crystal structure of unbound DNA.

摘要

通过在水中进行1.4纳秒的分子动力学模拟,研究了与半位点复合物晶体结构(蛋白质数据银行条目1TRR)中使用的色氨酸操纵子片段相对应的DNA双链体d-(AGCGTACTAGTACGCT)2的结构和水合作用。该模拟从B型DNA构象开始,使用1.4纳米的非键合截止距离并进行反应场校正,得到了一条稳定的轨迹。所获得的平均DNA构象更接近于复合物晶体结构(蛋白质数据银行条目1TRO和1TRR)中的构象,而不是未结合的色氨酸操纵子的晶体结构(核酸数据库条目BDJ061)。根据氢键百分比和相应的停留时间对DNA水合作用进行了表征。计算了DNA不可交换质子0.35纳米范围内水分子的停留时间,以便与分子间水-DNA核Overhauser效应(NOE)的核磁共振测量以及核磁共振弛豫色散测量结果进行比较。在大沟和小沟水合作用之间未发现显著差异。DNA供体和受体平均有77(±19)%的时间与水分子形成氢键。氢键结合水分子的平均停留时间为11(±11)皮秒,最长为223皮秒。当考虑不可交换质子的NOE距离(0.35纳米)内的所有水分子时,平均停留时间增加到平均100(±4)皮秒,最长为608皮秒。这些结果与Sunnerhagen等人的实验核磁共振结果一致,该结果未显示有任何证据表明水分子在DNA表面的停留时间超过1纳秒。DNA水合水的交换主要在大沟中通过与本体溶剂的直接交换发生,而进出小沟的过程通常通过涉及核糖O3'和O4'以及磷酸O2P氧原子的途径进行。小沟中最常见的水扩散途径垂直于沟的方向。一般来说,水分子在离开之前仅访问DNA沟中有限数量的位点。可以与DNA供体和受体基团形成氢键的氢键结合位点被水分子占据,平均B因子值为0.58埃²。在色氨酸阻遏蛋白/操纵子共晶体和未结合DNA的晶体结构中都观察到水分子的任何位点,均未观察到特殊值。

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