舍瓦内拉
富马酸还原酶
硒
无氧呼吸
硫氧还蛋白还原酶
周质间隙
硝酸还原酶
希瓦氏菌属
还原酶
亚硝酸盐还原酶
生物化学
化学
细菌
生物
酶
琥珀酸脱氢酶
硫氧还蛋白
大肠杆菌
有机化学
基因
遗传学
作者
Dao Bo Li,Yuan Cheng,Chao Wu,Wen‐Wei Li,Na Li,Zong Chuang Yang,Zhong Hua Tong,Han Yu
摘要
In situ reduction of selenite to elemental selenium (Se(0)), by microorganisms in sediments and soils is an important process and greatly affects the environmental distribution and the biological effects of selenium. However, the mechanism behind such a biological process remains unrevealed yet. Here we use Shewanella oneidensis MR-1, a widely-distributed dissimilatory metal-reducing bacterium with a powerful and diverse respiration capability, to evaluate the involvement of anaerobic respiration system in the microbial selenite reduction. With mutants analysis, we identify fumarate reductase FccA as the terminal reductase of selenite in periplasm. Moreover, we find that such a reduction is dependent on central respiration c-type cytochrome CymA. In contrast, nitrate reductase, nitrite reductase, and the Mtr electron transfer pathway do not work as selenite reductases. These findings reveal a previously unrecognized role of anaerobic respiration reductases of S. oneidensis MR-1 in selenite reduction and geochemical cycles of selenium in sediments and soils.
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