[FeFe]-酶成熟:一氧化碳的HydG催化合成
Eric M Shepard1, Benjamin R Duffus, Simon J George
1Department of Chemistry & Biochemistry and Astrobiology Biogeocatalysis Research Center, Montana State University, Bozeman, Montana 59717, USA.
Journal of the American Chemical Society
|June 23, 2010
概括
酶HydG从氨酸中合成一氧化碳 (CO),这是[FeFe]-酶成熟的关键步骤. 这是首次在酶生物合成中证明了酶性CO的产生.
科学领域:
- 生物化学 生物化学
- 酶学 是一种酶学.
- 有机金属化学 有机金属化学
背景情况:
- [FeFe]-酶的活性部位包含一个有机金属H集群.
- 它的生物合成需要辅助蛋白质:HydE,HydG (激进的AdoMet酶) 和HydF (GTPase).
- 一氧化碳 (CO) 是酶活性位点 ([FeFe],[NiFe],[Fe]-only) 中常见的配体.
研究的目的:
- 调查HydG在酶活性部位生物合成中的作用.
- 要确定HydG是否催化一氧化碳 (CO) 的合成.
- 为了确定由HydG生产的二氧化碳基质.
主要方法:
- 使用脱氧血红蛋白作为报告器来检测CO的产生.
- 通过可见光谱仪监测碳氧血球蛋白 (HbCO) 的形成.
- 采用 (13) C-氨酸和里埃变换红外光谱 (FTIR) 来确认CO的来源.
主要成果:
- 证明了HydG催化了CO的合成.
- 确认了氨酸作为HydG.CO生产的基质.
- 在酶成熟过程中提供了酶性CO合成的第一个证据.
结论:
- G负责从氨酸中合成CO的酶.
- 这一发现阐明了[FeFe]-酶复杂成熟途径中的关键步骤.
- 建立了与酶功能相关的CO生产的新型酶途径.
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