Department of Chemistry and Chemical Biology, Rutgers University, Piscataway, NJ 08854, USA.
Philos Trans R Soc Lond B Biol Sci. 2013 Jun 10;368(1622):20120257. doi: 10.1098/rstb.2012.0257. Print 2013 Jul 19.
Oxidoreductases play a central role in catalysing enzymatic electron-transfer reactions across the tree of life. To first order, the equilibrium thermodynamic properties of these proteins are governed by protein folds associated with specific transition metals and ligands at the active site. A global analysis of holoenzyme structures and functions suggests that there are fewer than approximately 500 fundamental oxidoreductases, which can be further clustered into 35 unique groups. These catalysts evolved in prokaryotes early in the Earth's history and are largely responsible for the emergence of non-equilibrium biogeochemical cycles on the planet's surface. Although the evolutionary history of the amino acid sequences in the oxidoreductases is very difficult to reconstruct due to gene duplication and horizontal gene transfer, the evolution of the folds in the catalytic sites can potentially be used to infer the history of these enzymes. Using a novel, yet simple analysis of the secondary structures associated with the ligands in oxidoreductases, we developed a structural phylogeny of these enzymes. The results of this 'composome' analysis suggest an early split from a basal set of a small group of proteins dominated by loop structures into two families of oxidoreductases, one dominated by α-helices and the second by β-sheets. The structural evolutionary patterns in both clades trace redox gradients and increased hydrogen bond energy in the active sites. The overall pattern suggests that the evolution of the oxidoreductases led to decreased entropy in the transition metal folds over approximately 2.5 billion years, allowing the enzymes to use increasingly oxidized substrates with high specificity.
氧化还原酶在催化生命之树中跨越酶电子转移反应方面发挥着核心作用。首先,这些蛋白质的平衡热力学性质受与活性部位特定过渡金属和配体相关的蛋白质折叠控制。对全酶结构和功能的全局分析表明,基本的氧化还原酶少于约 500 种,可以进一步聚类为 35 个独特的组。这些催化剂在地球历史早期的原核生物中进化,并且在很大程度上负责地球上非平衡生物地球化学循环的出现。尽管由于基因复制和水平基因转移,氧化还原酶中氨基酸序列的进化历史非常难以重建,但催化部位折叠的进化可以潜在地用于推断这些酶的历史。我们使用一种新颖而简单的分析方法,分析氧化还原酶中与配体相关的二级结构,开发了这些酶的结构系统发育。这种“复合分析”的结果表明,它们从由环结构主导的一小组蛋白质的基本集合中早期分离出来,分为两类氧化还原酶,一类由α-螺旋主导,另一类由β-折叠主导。两个分支中的结构进化模式都追踪了活性部位的氧化还原梯度和氢键能量的增加。总体模式表明,氧化还原酶的进化导致过渡金属折叠中的熵在大约 25 亿年的时间内降低,从而使酶能够以高特异性使用越来越氧化的底物。