Characterization of the overall and local dynamics of a protein with intermediate rotational anisotropy: Differentiating between conformational exchange and anisotropic diffusion in the B3 domain of protein G

被引:121
作者
Hall, JB [1 ]
Fushman, D [1 ]
机构
[1] Univ Maryland, Dept Chem & Biochem, Ctr Biomol Struct & Org, College Pk, MD 20742 USA
关键词
anisotropic rotational diffusion; conformational exchange; CSA/dipolar cross-correlation; hydrodynamic calculations; immunoglobulin-binding domain; protein dynamics; protein G;
D O I
10.1023/A:1025467918856
中图分类号
Q5 [生物化学]; Q7 [分子生物学];
学科分类号
071010 ; 081704 ;
摘要
Because the overall tumbling provides a major contribution to protein spectral densities measured in solution, the choice of a proper model for this motion is critical for accurate analysis of protein dynamics. Here we study the overall and backbone dynamics of the B3 domain of protein G using N-15 relaxation measurements and show that the picture of local motions is markedly dependent on the model of overall tumbling. The main difference is in the interpretation of the elevated R-2 values in the alpha-helix: the isotropic model results in conformational exchange throughout the entire helix, whereas no exchange is predicted by anisotropic models that place the longitudinal axis of diffusion tensor almost parallel to the helix axis. Due to small size (fast tumbling) of the protein, the T-1 values have low sensitivity to NH bond orientation. The diffusion tensor derived from orientation dependence of R-2/R-1 is anisotropic (D-par/D-perp = 1.4), with a small rhombic component. In order to distinguish the correct picture of motion, we apply model-independent methods that are sensitive to conformational exchange and do not require knowledge of protein structure or assumptions about its dynamics. A comparison of the CSA/dipolar cross-correlation rate constants with N-15 relaxation rates and the estimation of R-ex terms from relaxation data at 9.4 and 14.1 T indicate no conformational exchange in the helix, in support of the anisotropic models. The experimentally derived diffusion tensor is in excellent agreement with theoretical predictions from hydrodynamic calculations; a detailed comparison with various hydrodynamic models revealed optimal parameters for hydrodynamic calculations.
引用
收藏
页码:261 / 275
页数:15
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