Findley J E, Akagi J M
J Bacteriol. 1970 Sep;103(3):741-4. doi: 10.1128/jb.103.3.741-744.1970.
Studies with (35)S-labeled substrates were conducted to investigate the pathway involved in the reduction of sulfite to sulfide by cell-free extracts of the sulfate-reducing organism Desulfovibrio vulgaris. The results showed that accumulation of thiosulfate occurred when crude extracts were incubated under appropriate conditions with sulfite as substrate. With labeled sulfite as substrate, thiosulfate with equal distribution of radioactivity in both sulfur atoms was formed. When the rates of formation of (35)S(2-) from inner- and outer-labeled thiosulfate were compared, the rate of formation from outer-labeled thiosulfate was greater. Time studies with S-(35)SO(3) (2-) showed an increase of (35)S(2-) with time and an increasing ratio of doubly labeled to inner labeled thiosulfate remaining in the reaction mixture. From these studies it is concluded that thiosulfate is a stable intermediate formed from sulfite during the reduction of sulfate by D. vulgaris. Both sulfur atoms are derived from sulfite; during the utilization of thiosulfate, the outer sulfur is reduced to sulfide and the inner sulfur recycles through a sulfite pool.
采用(35)S标记的底物进行研究,以探究硫酸盐还原菌普通脱硫弧菌的无细胞提取物将亚硫酸盐还原为硫化物所涉及的途径。结果表明,当粗提取物在适当条件下以亚硫酸盐为底物进行孵育时,会出现硫代硫酸盐的积累。以标记的亚硫酸盐为底物时,会形成硫代硫酸盐,其两个硫原子中的放射性分布均匀。当比较内标记和外标记硫代硫酸盐生成(35)S(2-)的速率时,外标记硫代硫酸盐的生成速率更高。用S-(35)SO(3)(2-)进行的时间研究表明,(35)S(2-)随时间增加,反应混合物中剩余的双标记硫代硫酸盐与内标记硫代硫酸盐的比例也在增加。从这些研究中可以得出结论,硫代硫酸盐是普通脱硫弧菌在将硫酸盐还原过程中由亚硫酸盐形成的稳定中间体。两个硫原子均来源于亚硫酸盐;在硫代硫酸盐的利用过程中,外部的硫被还原为硫化物,内部的硫通过亚硫酸盐池进行循环。