Brereton P S, Verhagen M F, Zhou Z H, Adams M W
Department of Biochemistry and Molecular Biology, University of Georgia, Athens 30602-7229, USA.
Biochemistry. 1998 May 19;37(20):7351-62. doi: 10.1021/bi972864b.
The ferredoxin (7.5 kDa) of the hyperthermophilic archaeon, Pyrococcus furiosus, contains a single [4Fe-4S]1+,2+ cluster that is coordinated by three Cys and one Asp residue rather than the expected four Cys. The role of this Asp residue was investigated using a series of mutants, D14X, where X = C, S, H, N, V, and Y, prepared by heterologous gene expression in Escherichia coli. While the recombinant form of the wild-type and the D14S and D14C mutants contained a [4Fe-4S]1+,2+ cluster, the D14V, D14H, D14Y, and D14N proteins contained a [3Fe-4S]0,+ center, as determined by visible spectroscopy and electrochemistry. The redox potentials (at pH 7.0, 23 degrees C) of the D14C and D14S mutants were decreased by 58 and 133 mV, respectively, compared to those of the wild-type 4Fe-ferredoxin (Em -368 mV), while those of the 3Fe-protein mutants (including the 3Fe-form of the D14S, generated by chemical oxidation) were between 15 and 118 mV more positive than that of wild-type 3Fe-form (obtained by chemical oxidation, Em -203 mV). The reduction potentials of all of the 3Fe-forms, except the D14S mutant, showed a pH response over the range 3.0-10.0 with a pK of 3.3-4.7, and this was assigned to cluster protonation. The D14H mutant and the wild-type 3Fe-proteins showed an additional pK (both at 5.9) assumed to arise from protonation of the amino acid side chain. With the 4Fe-proteins, there was no dramatic change in the potentials of the wild-type or D14C form, while the pH response of the D14S mutant (pK 4.75) was ascribed to protonation of the serinate. While the ferredoxin variants exhibited a range of thermal stabilities (measured at 80 degrees C, pH 2.5), none of them showed any temperature-dependent transitions (0-80 degrees C) in their reduction potentials, and there was no correlation between the calculated DeltaS degrees' values and the absorbance maximum, reduction potential, or hydrophobicity of residue 14. In contrast, there was a linear correlation between the DeltaH degrees' value and reduction potential. Kinetic analyses were carried out at 80 degrees C using the ferredoxin as either an electron acceptor to pyruvate oxidoreductase (POR) or as an electron donor to ferredoxin:NADP oxidoreductase (FNOR, both from P. furiosus). The data showed that the reduction potential of the ferredoxin, rather than cluster type or the nature of the residue at position 14, appears to be the predominant factor in determining efficiency of electron transfer in both systems. However, compared to all the variants, the reduction potential of WT Fd makes it the most appropriate protein to both accept electrons from POR and donate them to FNOR.
嗜热古菌激烈火球菌(Pyrococcus furiosus)的铁氧化还原蛋白(7.5 kDa)含有一个单一的[4Fe-4S]1 +,2 +簇,该簇由三个半胱氨酸(Cys)残基和一个天冬氨酸(Asp)残基配位,而不是预期的四个半胱氨酸残基。使用一系列通过在大肠杆菌中进行异源基因表达制备的D14X突变体(其中X = C、S、H、N、V和Y)研究了这个天冬氨酸残基的作用。虽然野生型以及D14S和D14C突变体的重组形式含有一个[4Fe-4S]1 +,2 +簇,但通过可见光谱和电化学测定,D14V、D14H、D14Y和D14N蛋白含有一个[3Fe-4S]0,+中心。与野生型4Fe-铁氧化还原蛋白(Em -368 mV)相比,D14C和D14S突变体的氧化还原电位(在pH 7.0、23摄氏度下)分别降低了58和133 mV,而3Fe-蛋白突变体(包括通过化学氧化产生的D14S的3Fe形式)的氧化还原电位比野生型3Fe形式(通过化学氧化获得,Em -203 mV)正15至118 mV。除D14S突变体外,所有3Fe形式的还原电位在3.0 - 10.0范围内显示出pH响应,pK为3.3 - 4.7,这归因于簇质子化。D14H突变体和野生型3Fe蛋白显示出另一个pK(均为5.9),推测是由氨基酸侧链的质子化引起的。对于4Fe-蛋白,野生型或D14C形式的电位没有显著变化,而D14S突变体的pH响应(pK 4.75)归因于丝氨酸盐的质子化。虽然铁氧化还原蛋白变体表现出一系列热稳定性(在80摄氏度、pH 2.5下测量),但它们在还原电位方面均未显示出任何温度依赖性转变(0 - 80摄氏度),并且计算出的ΔS°值与残基14的吸光度最大值、还原电位或疏水性之间没有相关性。相反,ΔH°值与还原电位之间存在线性相关性。在80摄氏度下使用铁氧化还原蛋白作为丙酮酸氧化还原酶(POR,均来自激烈火球菌)的电子受体或作为铁氧化还原蛋白:NADP氧化还原酶(FNOR,均来自激烈火球菌)的电子供体进行了动力学分析。数据表明,铁氧化还原蛋白的还原电位,而不是簇类型或第14位残基的性质,似乎是决定两个系统中电子转移效率的主要因素。然而,与所有变体相比,野生型铁氧化还原蛋白(WT Fd)的还原电位使其成为最适合从POR接受电子并将其捐赠给FNOR的蛋白质。