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DHPS-Sulfolyase (HpsG) 催化全球丰富的二羟丙基砜硫酸盐厌氧降解的机制见解。

Mechanistic Insights into the Anaerobic Degradation of Globally Abundant Dihydroxypropanesulfonate Catalyzed by the DHPS-Sulfolyase (HpsG).

机构信息

School of Chemistry and Chemical Engineering, Shandong University, Jinan, Shandong 250100, China.

出版信息

J Chem Inf Model. 2022 Jun 13;62(11):2880-2888. doi: 10.1021/acs.jcim.2c00174. Epub 2022 May 18.

Abstract

2()-Dihydroxypropanesulfonate (DHPS) is the main abundant organosulfonate in the biosphere generated by the microbial degradation of the abundant organosulfur species 6-deoxy-6-sulfo-d-glucopyranose (sulfoquinovose, SQ). Massive amounts of DHPS can also be produced by the highly abundant oceanic diatoms. The quantity of degradation DHPS is so large that it has become an important part of the earth's sulfur. The recently characterized O2-sensitive glycyl radical enzyme DHPS-sulfolyase HpsG in anaerobic bacteria was found to be capable of cleaving the C-S bond of DHPS under anaerobic conditions. However, the detailed degradation mechanism is still unclear. Here, on the basis of the crystal structure of HpsG, we constructed the computational model and performed QM/MM calculations to illuminate the anaerobic degradation mechanism of DHPS. Our calculations revealed that the degradation reaction follows an unusual radical-dependent mechanism that does not require a conserved Glu464 to deprotonate the C2 hydroxyl of substrate to promote the C-S cleavage; instead, after the first hydrogen abstraction triggered by the thiyl radical (Cys462), the C-S bond in 2()-dihydroxypropanesulfonate can directly collapse. Thus, conserved Glu464 mainly plays a role in stabilizing the substrate and reaction intermediate by forming a hydrogen bond. After the release of the sulfonic acid group from the protein environment, the deprotonated Glu464 spontaneously accepts a proton from the C2 hydroxyl of the substrate radical. Our findings clarified an unusual C-S cleavage mechanism involved in the DHPS degradation reaction catalyzed by GREs.

摘要

2-羟丙基磺酸盐 (DHPS) 是由微生物降解丰富的有机硫物种 6-脱氧-6-磺基-D-吡喃葡萄糖 (磺基奎诺糖,SQ) 产生的生物圈中主要的丰富有机磺酸盐。大量的 DHPS 也可以由丰富的海洋硅藻产生。DHPS 的降解量如此之大,以至于它已成为地球硫的重要组成部分。最近在厌氧细菌中鉴定出的对 O2 敏感的甘氨酰基自由基酶 DHPS-磺基裂解酶 HpsG 能够在厌氧条件下裂解 DHPS 的 C-S 键。然而,其详细的降解机制仍不清楚。在这里,基于 HpsG 的晶体结构,我们构建了计算模型并进行了 QM/MM 计算,以阐明 DHPS 的厌氧降解机制。我们的计算表明,降解反应遵循一种不寻常的自由基依赖机制,该机制不需要保守的 Glu464 去质子化底物的 C2 羟基以促进 C-S 断裂;相反,在硫基自由基 (Cys462) 引发的第一次氢提取之后,2-羟丙基磺酸盐中的 C-S 键可以直接坍塌。因此,保守的 Glu464 主要通过形成氢键来稳定底物和反应中间体。在磺酸基团从蛋白质环境中释放后,去质子化的 Glu464 自发地从底物自由基的 C2 羟基接受质子。我们的研究结果阐明了 GRE 催化的 DHPS 降解反应中涉及的一种不寻常的 C-S 断裂机制。

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