Department of Physics and Center for Interdisciplinary Research on Complex Systems, Northeastern University, Boston, Massachusetts 02115, USA.
J Am Chem Soc. 2010 Mar 3;132(8):2811-20. doi: 10.1021/ja910005b.
Nitrophorin 4 (NP4) is a heme protein that stores and delivers nitric oxide (NO) through pH-sensitive conformational change. This protein uses the ferric state of a highly ruffled heme to bind NO tightly at low pH and release it at high pH. In this work, the rebinding kinetics of NO and CO to NP4 are investigated as a function of iron oxidation state and the acidity of the environment. The geminate recombination process of NO to ferrous NP4 at both pH 5 and pH 7 is dominated by a single approximately 7 ps kinetic phase that we attribute to the rebinding of NO directly from the distal pocket. The lack of pH dependence explains in part why NP4 cannot use the ferrous state to fulfill its function. The kinetic response of ferric NP4NO shows two distinct phases. The relative geminate amplitude of the slower phase increases dramatically as the pH is raised from 5 to 8. We assign the fast phase of NO rebinding to a conformation of the ferric protein with a closed hydrophobic pocket. The slow phase is assigned to the protein in an open conformation with a more hydrophilic heme pocket environment. Analysis of the ultrafast kinetics finds the equilibrium off-rate of NO to be proportional to the open state population as well as the pH-dependent amplitude of escape from the open pocket. When both factors are considered, the off-rate increases by more than an order of magnitude as the pH changes from 5 to 8. The recombination of CO to ferrous NP4 is observed to have a large nonexponential geminate amplitude with rebinding time scales of approximately 10(-11)-10(-9) s at pH 5 and approximately 10(-10)-10(-8) s at pH 7. The nonexponential CO rebinding kinetics at both pH 5 and pH 7 are accounted for using a simple model that has proven effective for understanding CO binding in a variety of other heme systems (Ye, X.; et al. Proc. Natl. Acad. Sci. U.S.A. 2007, 104, 14682).
硝普酚 4(NP4)是一种血红素蛋白,通过 pH 敏感的构象变化储存和输送一氧化氮(NO)。该蛋白利用高度褶皱血红素的三价铁状态在低 pH 下紧密结合 NO,并在高 pH 下释放。在这项工作中,研究了 NP4 与 NO 和 CO 的再结合动力学作为铁氧化态和环境酸度的函数。在 pH 5 和 pH 7 下,亚铁 NP4 与 NO 的复合过程主要由一个大约 7 ps 的动力学相主导,我们将其归因于 NO 直接从远端口袋的再结合。缺乏 pH 依赖性部分解释了为什么 NP4 不能利用亚铁状态来发挥其功能。铁 NP4NO 的动力学响应显示出两个明显的相。随着 pH 从 5 升高到 8,较慢相的相对复合幅度显著增加。我们将 NO 再结合的快相分配给具有封闭疏水性口袋的铁蛋白构象。慢相被分配给具有更亲水血红素口袋环境的开放构象的蛋白质。超快动力学分析发现,NO 的平衡离速与开放状态的种群以及从开放口袋中逃逸的 pH 依赖性幅度成正比。当考虑这两个因素时,随着 pH 从 5 变为 8,离速增加了一个数量级以上。在 pH 5 时,观察到 CO 与亚铁 NP4 的复合具有较大的非指数复合幅度,再结合时间尺度约为 10(-11)-10(-9) s,在 pH 7 时约为 10(-10)-10(-8) s。在 pH 5 和 pH 7 下,非指数 CO 再结合动力学都可以用一个简单的模型来解释,该模型已被证明对理解各种其他血红素系统中的 CO 结合非常有效(Ye, X.; 等人。Proc. Natl. Acad. Sci. U.S.A. 2007, 104, 14682)。