NADH:Ubiquinone Oxidoreductase of Vibrio alginolyticus: Purification, Properties, and Reconstitution of the Na+ Pump
详细信息    查看全文
文摘
The Na+-activated NADH:ubiquinoneoxidoreductase of Vibrio alginolyticus wasextractedfrom the membranes with lauryldimethylamine-N-oxide andpurified by two successive anion exchangecolumns. This preparation, yielding four major and several minorstained bands after SDS-PAGE, retainedthe NADH-dehydrogenase activity (with menadione as an artificialelectron acceptor) and ubiquinone-1(Q) reductase activity. On further fractionation of the enzyme,the Q-reductase activity essentiallydisappeared. Chemical analyses revealed the presence of FAD butnot FMN, of non-heme iron and ofacid-labile sulfur and tightly-bound ubiquinone-8 in the purifiedQ-reductase preparation. The participationof an iron-sulfur cluster of the [2Fe-2S] type in the electrontranslocation was demonstrated by theappearance of a typical EPR signal for this prosthetic group after thereduction of Q-reductase with NADH.A strong EPR signal typical for a radical observed upon reductionof the enzyme might arise from theformation of quinone radicals. In the absence ofNa+, the path of the electrons apparently ends withthereduction of ubiquinone-1 to the semiquinone derivative which in thepresence of O2 becomes reoxidizedwith concomitant formation of superoxide radicals. In the presenceof Na+, these oxygen radicals are notformed and the semiquinone is further reduced to the quinol derivative.These results indicate that theNa+-dependent step in the electron transfer catalyzed byNADH:ubiquinone oxidoreductase is the reductionof ubisemiquinone to ubiquinol. After reconstitution of thepurified Q-reductase into proteoliposomes,NADH oxidation by ubiquinone-1 was coupled to Na+transport with an apparent stoichiometry of 0.5Na+ per NADH oxidized. The transport was stimulatedby valinomycin (+K+) or by the uncouplercarbonylcyanide m-chlorophenylhydrazone (CCCP). The transportof Na+ is therefore a primary event and doesnot involve the intermediate formation of a protongradient.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700