Elemental sulfur reduction in the deep-sea vent thermophile, Thermovibrio ammonificans.
Elemental sulfur reduction in the deep-sea vent thermophile, Thermovibrio ammonificans.
复制标题
深海喷口嗜热菌、氨化热弧菌中元素硫的还原。
DOI:
10.1111/1462-2920.14280
复制
发表时间:
2018
影响因子:
5.1
通讯作者:
Vetriani,Costantino
中科院分区:
文献类型:
--
作者:
Jelen,Benjamin;Giovannelli,Donato;Falkowski,PaulG;Vetriani,Costantino
The reduction of elemental sulfur is an important energy‐conserving pathway in prokaryotes inhabiting geothermal environments, where sulfur respiration contributes to sulfur biogeochemical cycling. Despite this, the pathways through which elemental sulfur is reduced to hydrogen sulfide remain unclear in most microorganisms. We integrated growth experiments usingThermovibrio ammonificans, a deep‐sea vent thermophile that conserves energy from the oxidation of hydrogen and reduction of both nitrate and elemental sulfur, with comparative transcriptomic and proteomic approaches, coupled with scanning electron microscopy. Our results revealed that two members of the FAD‐dependent pyridine nucleotide disulfide reductase family, similar to sulfide‐quinone reductase and to NADH‐dependent sulfur reductase (NSR), respectively, are over‐expressed during sulfur respiration. Scanning electron micrographs and sulfur sequestration experiments indicated that direct access ofT. ammonificansto sulfur particles strongly promoted growth. The sulfur metabolism ofT. ammonificansappears to require abiotic transition from bulk elemental sulfur to polysulfide to nanoparticulate sulfur at an acidic pH, coupled to biological hydrogen oxidation. A coupled biotic‐abiotic mechanism for sulfur respiration is put forward, mediated by an NSR‐like protein as the terminal reductase.