Fisher K, Lowe D J, Thorneley R N
AFRC Institute of Plant Science Research, Nitrogen Fixation Laboratory, University of Sussex, Brighton, U.K.
Biochem J. 1991 Oct 1;279 ( Pt 1)(Pt 1):81-5. doi: 10.1042/bj2790081.
The pre-steady-state kinetics of H2 evolution from Klebsiella pneumoniae nitrogenase functioning at 23 degrees C, pH 7.4, under conditions of extremely low electron flux through the MoFe-protein exhibited a lag phase of several minutes duration. The approach to a steady-state rate of H2 evolution was accompanied by a 50% decrease in the amplitude of the MoFe-protein e.p.r. signal. These kinetics have been simulated using our published kinetic model for nitrogenase [Lowe & Thorneley (1984) Biochem. J. 224, 877-886], which was developed using data obtained with nitrogenase functioning at high electron fluxes. The e.p.r. data showed that the rate of complex-formation between reduced Fe-protein and the MoFe-protein (k+1 = 5 x 10(7) M-1.s-1) is the same for the resting (E0) and one-electron-reduced (E1H) states of the MoFe-protein. Stopped-flow spectrophotometry also showed that electron transfer from the Fe-protein to the MoFe-protein in states E0 and E1H occurs at the same rate (kobs. = 140 s-1). These data support our previous assumption that the rate constants that define the 'Fe-protein cycle' are independent of the level of reduction of the MoFe-protein.
在极低电子通量通过钼铁蛋白的条件下,肺炎克雷伯氏菌固氮酶在23摄氏度、pH 7.4时产生氢气的预稳态动力学表现出持续数分钟的延迟期。氢气产生速率达到稳态的过程伴随着钼铁蛋白电子顺磁共振信号幅度降低50%。利用我们已发表的固氮酶动力学模型[Lowe & Thorneley (1984) Biochem. J. 224, 877 - 886]对这些动力学进行了模拟,该模型是利用在高电子通量下运行的固氮酶所获得的数据开发的。电子顺磁共振数据表明,还原态铁蛋白与钼铁蛋白之间的复合物形成速率(k+1 = 5×10(7) M-1·s-1)对于钼铁蛋白的静止态(E0)和单电子还原态(E1H)是相同的。停流分光光度法也表明,在E0和E1H状态下,电子从铁蛋白转移到钼铁蛋白的速率相同(kobs. = 140 s-1)。这些数据支持了我们之前的假设,即定义“铁蛋白循环”的速率常数与钼铁蛋白的还原水平无关。