来自黑海地毯的甲基-辅酶M减少酶的结构,这些地毯无氧氧化甲
Seigo Shima1, Martin Krueger, Tobias Weinert
1Max Planck Institute for Terrestrial Microbiology, Karl-Frisch-Strasse 10, D-35043 Marburg, Germany. shima@mpi-marburg.mpg.de
Nature
|November 29, 2011
概括
研究人员阐明了甲氧化甲 (AOM) 的甲激活酶的结构. 这种酶,ANME-1 MCR,与其甲原性对应物共享基质,但具有不同的特征.
科学领域:
- 微生物学和生物化学
- 结构生物学 结构生物学
- 生物地质化学生物地质化学
背景情况:
- 甲 (AOM) 与硫酸盐的无氧氧化是一种关键的微生物过程,由无氧甲类古生物 (ANME) 和减少硫酸盐的细菌组成的联盟驱动.
- 负责ANME古生物中的甲激活的酶被认为是甲基辅酶M减少酶 (MCR) 的同类物,也存在于甲原古生物中.
研究的目的:
- 为了确定ANME-1 MCR复合体的X射线结构.
- 了解AOM中甲激活的结构基础.
- 为了比较ANME-1 MCR与甲原性古生物的MCR.
主要方法:
- 从黑海收集的微生物联盟中净化ANME-1 MCR.
- 在280kDa的ANME-1 MCR复合体中结晶.
- 进行X射线衍射分析以确定2.1 Å分辨率的结构.
主要成果:
- 成功确定了ANME-1 MCR复合体的X射线结构.
- 发现ANME-1 MCR与辅酶M和辅酶B及其基质复合在一起.
- 与甲原性MCR相比,确定了关键的结构差异,包括F430修饰,富含氨酸的补丁和改变的翻译后修饰.
结论:
- 这项研究为ANME古物中的甲激活酶提供了第一个结构洞察力.
- 鉴定到的结构变化表明,ANME-1 MCR应适应其在AOM中的作用.
- 这些发现提升了我们对微生物甲循环和酶进化的理解.
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