氧气同位素O2的分离 甲和氨单氧基酶的消耗
Carolina F M de Carvalho1, Maartje A H J van Kessel2, Arjan Pol2
1Department of Environmental Sciences, University of Basel, 4056 Basel, Switzerland.
ACS environmental Au
|January 26, 2026
概括
微生物甲和氨氧化不能解释在水环境中观察到的溶解氧 (O2) 同位素分化的差异. 这些过程涉及溶性甲单氧化酶 (sMMO),颗粒甲单氧化酶 (pMMO) 和氨单氧化酶 (AMO) 等酶,产生类似于异质呼吸的分离值.
科学领域:
- 环境科学 环境科学
- 生物地质化学生物地质化学
- 微生物学 微生物学
背景情况:
- 稳定的同位素分离溶解氧 (O2) 对于建模水生生态系统健康至关重要.
- 实验室和现场O2消耗同位素分离值之间存在差异.
研究的目的:
- 调查微生物甲和氨氧化是否有助于观察到的O2同位素分离差异.
- 确定参与甲和氨氧化的关键酶的体内18ε值.
主要方法:
- 用甲变性和comammox细菌进行实验,以估计体内18ε值.
- 专注于酶:可溶性甲单氧化酶 (sMMO),颗粒甲单氧化酶 (pMMO) 和氨单氧化酶 (AMO).
主要成果:
- 对于pMMO和AMO的18ε值为-18 ± 12到-24 ± 5 ‰,相当于异质呼吸.
- 对于sMMO的18ε值为-22 ± 2 ‰,类似于但比以前报告的更为负.
- 这些微生物氧化途径并不能解释观察到的in situ与实验室分化差异.
结论:
- 根据sMMO,pMMO或AMO的氧气消耗并不能解释不同的同位素分离值.
- 在O2同位素分成中的差异很可能是由于基质扩散限制.
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