Bopp Charlotte E, Kohler Hans-Peter E, Hofstetter Thomas B
Eawag, Swiss Federal Institute of Aquatic Science and Technology; Institute of Biogeochemistry and Pollutant Dynamics (IBP), ETH Zurich.
Eawag, Swiss Federal Institute of Aquatic Science and Technology; Institute of Biogeochemistry and Pollutant Dynamics (IBP), ETH Zurich;, Email:
Chimia (Aarau). 2020 Mar 25;74(3):108-114. doi: 10.2533/chimia.2020.108.
Enzymatic oxygenations initiate biodegradation processes of many organic soil and water contaminants. Even though many biochemical aspects of oxygenation reactions are well-known, quantifying rates of oxidative contaminant removal as well as the extent of oxygenation remains a major challenge. Because enzymes use different strategies to activate O₂, reactions leading to substrate oxygenation are not necessarily limiting the rate of contaminant removal. Moreover, oxygenases react along unproductive pathways without substrate metabolism leading to O₂ uncoupling. Here, we identify the critical features of the catalytic cycles of selected oxygenases that determine rates and extents of biodegradation. We focus most specifically on Rieske dioxygenases, a subfamily of mononuclear non-heme ferrous iron oxygenases, because of their ability to hydroxylate unactivated aromatic structures and thus initiate the transformation of the most persistent organic contaminants. We illustrate that the rate-determining steps in their catalytic cycles range from O₂ activation to substrate hydroxylation, depending on the extent of O-O cleavage that is required for generating the reactive Fe-oxygen species. The extent of O₂ uncoupling, on the other hand, is highly substrate-specific and potentially modulated by adaptive responses to oxidative stress. Understanding the kinetic mechanisms of oxygenases will be key to assess organic contaminant biotransformation quantitatively.
酶促氧化作用引发了许多有机土壤和水体污染物的生物降解过程。尽管氧化反应的许多生化方面已为人熟知,但量化氧化污染物的去除速率以及氧化程度仍然是一项重大挑战。由于酶采用不同策略激活O₂,导致底物氧化的反应不一定限制污染物的去除速率。此外,加氧酶会沿着无底物代谢的非生产性途径反应,导致O₂解偶联。在此,我们确定了选定加氧酶催化循环的关键特征,这些特征决定了生物降解的速率和程度。我们特别关注 Rieske 双加氧酶,它是单核非血红素亚铁加氧酶的一个亚家族,因为它们能够羟基化未活化的芳香结构,从而启动最持久有机污染物的转化。我们表明,其催化循环中的速率决定步骤从O₂激活到底物羟基化不等,这取决于生成活性铁-氧物种所需的O-O裂解程度。另一方面,O₂解偶联的程度具有高度的底物特异性,并可能受到对氧化应激的适应性反应的调节。了解加氧酶的动力学机制将是定量评估有机污染物生物转化的关键。