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产甲烷古菌中氧化还原驱动的质子转运

Redox-driven proton translocation in methanogenic Archaea.

作者信息

Deppenmeier U

机构信息

Institut für Mikrobiologie und Genetik, Universität Göttingen, Germany.

出版信息

Cell Mol Life Sci. 2002 Sep;59(9):1513-33. doi: 10.1007/s00018-002-8526-3.

Abstract

Methanogenic archaea of the genus Methanosarcina are able to utilize H2 + CO2, methylated C1 compounds or acetate as energy and carbon source, thereby producing methane as the major end product. The methanogenic pathways lead to the formation of a mixed disulfide derived from coenzyme M and coenzyme B. This disulfide is of major importance for methanogens because it is the terminal electron acceptor of a branched respiratory chain. Molecular hydrogen, reduced coenzyme F420 or reduced ferredoxin are used as electron donors. Four enzymes are involved in the membrane-bound electron transport system of Methanosarcina species, all of which are involved in the generation of an electrochemical proton gradient that is used for ATP synthesis. This review focuses on the membrane-bound electron transport chains of Methanosarcina species with respect to the biochemical and genetic characteristics of the unusual energy transducing enzymes. Furthermore, the review addresses questions concerning the relationship between methanogenic proteins and components of respiratory chains found in bacteria and eukarya.

摘要

甲烷八叠球菌属的产甲烷古菌能够利用H2 + CO2、甲基化C1化合物或乙酸盐作为能量和碳源,从而产生甲烷作为主要终产物。产甲烷途径导致形成一种由辅酶M和辅酶B衍生的混合二硫键。这种二硫键对产甲烷菌至关重要,因为它是分支呼吸链的末端电子受体。分子氢、还原型辅酶F420或还原型铁氧还蛋白用作电子供体。四种酶参与甲烷八叠球菌属的膜结合电子传递系统,所有这些酶都参与用于ATP合成的电化学质子梯度的产生。本综述重点关注甲烷八叠球菌属的膜结合电子传递链,涉及这些不寻常的能量转换酶的生化和遗传特征。此外,该综述还探讨了有关产甲烷蛋白与细菌和真核生物中发现的呼吸链成分之间关系的问题。

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Redox-driven proton translocation in methanogenic Archaea.产甲烷古菌中氧化还原驱动的质子转运
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