Molecular and Environmental Science Research Group, Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, Saskatchewan, S7N 5E2, Canada.
J Phys Chem B. 2010 Mar 11;114(9):3266-75. doi: 10.1021/jp908731f.
The physiologically vital enzyme sulfite oxidase employs rapid intramolecular electron transfer between a molybdenum ion in the C-terminal domain (the site of sulfite oxidation) and a heme moeity in the N-terminal domain to complete its catalytic cycle. Crystal structures of the enzyme show C- and N-terminal domain orientations that are not consistent with rapid intramolecular electron transfer. Domain motion has been postulated to explain this discrepancy. In the present work we employ molecular dynamics simulations to understand the large-scale domain motions of the enzyme. We observe motion of the N-terminal domain into an orientation similar to that postulated for rapid electron transfer. Our simulations also probe the dynamics of the active site and surrounding residues, adding a further level of structural and thermodynamic detail in understanding sulfite oxidase function.
生理上重要的酶亚硫酸盐氧化酶利用钼离子在 C 末端结构域(亚硫酸盐氧化部位)和 N 末端结构域中的血红素基团之间的快速分子内电子转移来完成其催化循环。酶的晶体结构显示 C 端和 N 端结构域的取向与快速分子内电子转移不一致。已经提出结构域运动来解释这种差异。在本工作中,我们采用分子动力学模拟来理解酶的大规模结构域运动。我们观察到 N 末端结构域的运动进入到类似于快速电子转移所假定的构象。我们的模拟还探测了活性位点和周围残基的动力学,为理解亚硫酸盐氧化酶的功能增加了结构和热力学细节的另一个层次。