由Exiguobacterium从海洋沉积物的元素硫的不成比例
Xiao-Tong Wu1,2, Min Qiu1,2,3, Yu-Qin He1,2
1Key Laboratory of Urban Environment and Health, Ningbo Observation and Research Station, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, P. R. China.
ISME communications
|October 13, 2025
概括
微生物过程的元素硫不成比例,是由Exiguobacterium细菌促进的. 这项研究揭示了这种古老的新陈代谢存在于细菌中,扩大了其已知的遗传分布.
科学领域:
- 微生物学 微生物学
- 生物地质化学生物地质化学
- 进化生物学 进化生物学
背景情况:
- 元素硫不成比例是一种古老的微生物代谢过程.
- 元素硫不相称的基因分布尚未完全理解.
- Exiguobacterium是一种在各种环境中发现的属.
研究的目的:
- 为了丰富和识别能够产生元素硫不成比例的微生物.
- 调查Exiguobacterium在元素硫不成比例中的作用.
- 探索这种新陈代谢过程在古代细菌类中的进化影响.
主要方法:
- 细菌群体的丰富文化. 细菌群体的丰富文化.
- 16S rRNA基因测序用于社区分析.
- 基因组分析分析以确定关键基因.
主要成果:
- 一个因元素硫不成比例而丰富的细菌群体是由Exiguobacterium (99.45%) 主导的.
- 已经证明,exiguobacterium通过元素硫不成比例促进了硫酸盐和硫化物的形成.
- 罗达尼斯类硫转移酶基因在实验小组中明显更为丰富,使他们参与了这个过程.
结论:
- 这项研究提供了第一个证据,证明细菌对元素硫不成比例.
- 这些发现表明,细菌和/或 Firmicutes 可能代表古老的细菌类.
- 埃克西瓜细菌的流行表明,元素硫和硫酸盐之间的微生物转化可能在生态系统中广泛存在.
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