Instituto de Tecnologia Química e Biológica António Xavier, Universidade Nova de Lisboa, Oeiras 2780-156, Portugal.
Proc Natl Acad Sci U S A. 2024 Feb 6;121(6):e2313650121. doi: 10.1073/pnas.2313650121. Epub 2024 Jan 29.
Microbial dissimilatory sulfate reduction (DSR) is a key process in the Earth biogeochemical sulfur cycle. In spite of its importance to the sulfur and carbon cycles, industrial processes, and human health, it is still not clear how reduction of sulfate to sulfide is coupled to energy conservation. A central step in the pathway is the reduction of sulfite by the DsrAB dissimilatory sulfite reductase, which leads to the production of a DsrC-trisulfide. A membrane-bound complex, DsrMKJOP, is present in most organisms that have DsrAB and DsrC, and its involvement in energy conservation has been inferred from sequence analysis, but its precise function was so far not determined. Here, we present studies revealing that the DsrMKJOP complex of the sulfate reducer works as a menadiol:DsrC-trisulfide oxidoreductase. Our results reveal a close interaction between the DsrC-trisulfide and the DsrMKJOP complex and show that electrons from the quinone pool reduce consecutively the DsrM hemes , the DsrK noncubane [4Fe-4S] catalytic center, and finally the DsrC-trisulfide with concomitant release of sulfide. These results clarify the role of this widespread respiratory membrane complex and support the suggestion that DsrMKJOP contributes to energy conservation upon reduction of the DsrC-trisulfide in the last step of DSR.
微生物异化硫酸盐还原(DSR)是地球生物地球化学硫循环中的关键过程。尽管它对硫和碳循环、工业过程和人类健康都很重要,但目前仍不清楚硫酸盐还原为硫化物如何与能量守恒相关联。该途径的一个中心步骤是 DsrAB 异化亚硫酸盐还原酶还原亚硫酸盐,导致 DsrC-三硫化物的产生。大多数具有 DsrAB 和 DsrC 的生物体中都存在一种膜结合复合物 DsrMKJOP,其在能量守恒中的参与已从序列分析中推断出来,但迄今为止其确切功能尚未确定。在这里,我们介绍了一些研究揭示了硫酸盐还原菌的 DsrMKJOP 复合物作为 二羟丙酮:DsrC-三硫化物氧化还原酶的作用。我们的研究结果揭示了 DsrC-三硫化物与 DsrMKJOP 复合物之间的密切相互作用,并表明来自醌库的电子依次还原 DsrC-三硫化物中的 DsrM 血红素、DsrK 非笼形 [4Fe-4S] 催化中心,最后还原 DsrC-三硫化物,同时释放硫化物。这些结果阐明了这种广泛存在的呼吸膜复合物的作用,并支持了 DsrMKJOP 在 DSR 的最后一步中还原 DsrC-三硫化物时有助于能量守恒的观点。