微生物通过不同的途径在透性和凝聚性沉积物中氧化葡萄糖
Tess F Hutchinson1, Adam J Kessler2, Wei Wen Wong1
1Water Studies, School of Chemistry, Monash University, Clayton, VIC 3800, Australia.
The ISME journal
|February 16, 2024
概括
葡萄糖的微生物发酵,脱离呼吸,在海洋沉积物中占主导地位,氧气水平波动. 在透性沉积物中观察到的这一过程与泥环境中的完全氧化不同.
科学领域:
- 海洋微生物学 海洋微生物学
- 生物地质化学循环是什么
- 环境科学环境科学
背景情况:
- 海洋沉积物中的有机物微生物降解通常涉及发酵,其次是氧化.
- 脱离外部电子受体的发酵被假设为具有可变氧气的环境.
研究的目的:
- 在海洋沉积物中提供未结合发酵的直接证据.
- 在不同的条件下量化呼吸和发酵的相对贡献.
主要方法:
- 开发和应用一种新的差异标记的葡萄糖同位素测定方法.
- 对透性 (沙) 和凝聚性 (泥) 沉积物的分析.
- 四种细菌分离物的化.
主要成果:
- 透沉积物中的微生物群体通过无氧状态下通过Embden-Meyerhof-Parnas通道表现出未结合的发酵,持续时间长达160小时.
- 在泥沉积物中的社区主要在无氧条件下将葡萄糖完全氧化为二氧化碳.
- 在透沉积物中,在氧气条件下意外观察到发酵.
结论:
- 微生物群落在可变的氧气环境中利用未合的发酵在过渡性无氧期间代谢有机物质.
- 沉积物类型和氧气可变性显著影响微生物代谢途径.
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