通过从化古Nitrosopumilus maritimus中通过酶性氧化物产生氧化
Robert W Voland1, Hongsen Wang1, Héctor D Abruña1
1Department of Chemistry and Chemical Biology, Baker Laboratory, Cornell University, Ithaca, NY 14853.
概括
氨氧化古生物 (AOA) 通过一种新发现的酶Nmar_1354.4产生氧化 (N2O). 这种酶产生氧化物 (HNO),导致N2O的形成,解释了微生物N2O排放的主要来源.
科学领域:
- 微生物学 微生物学
- 生物化学 生化学
- 环境科学 环境科学
背景情况:
- 氨氧化古生物 (AOA) 是全球丰富的微生物.
- AOA是氧化 (N2O) 排放的重要来源.
- 对于AOA产生的N2O生产的特定生化途径在很大程度上是未知的.
研究的目的:
- 研究AOA中代谢的酶机制.
- 为了确定AOA N2O排放的生物化学来源.
- 描述一种参与AOA循环的新型酶.
主要方法:
- 从Nitrosopumilus maritimus*获得的多铜氧化酶Nmar_1354的重组表达和净化.
- 酶性测试以确定Nmar_1354.4的基质特异性和产物.
- 生产的氧化物 (HNO) 下游反应的表征.
主要成果:
- Nmar_1354催化氧胺 (NH2OH) 的氧化,产生氧 (HNO).
- 这种反应将NH2OH氧化与二氧化物 (O2) 减少相结合.
- HNO通过与NH2OH的反应转化为N2并通过二元化转化为N2O,为N2O释放提供了一条途径.
结论:
- 确定了AOA生产N2O的可信酶源.
- 揭示了一种用于产生氧化物 (HNO) 的新型酶途径.
- 表明HNO在微生物循环,细胞信号和能量转导中的作用.
相关概念视频
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