来自五个不同的深海沟的沉积物中的微生物群落结构和代谢特征
Yao Xiao1,2, Hao Liu1,3, Ziying Wu1
1State Key Laboratory of Deep-Sea Science and Intelligent Technology, Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, China.
Frontiers in microbiology
|December 19, 2025
概括
深海微生物在高压下表现出较低的生长效率,将碳转移到维持呼吸. 这凸显了需要实地测量来理解海洋碳循环的必要性.
科学领域:
- 海洋微生物学 海洋微生物学
- 深海生态 深海生态
- 生物地质化学循环是什么
背景情况:
- 微生物生长效率 (MGE) 是了解海洋碳流和生物地球化学循环的关键.
- 深海沟微生物的代谢特征在很大程度上是未知的.
- 深海沟是研究微生物适应的独特环境.
研究的目的:
- 在五个深海沟中调查微生物社区结构和代谢特征.
- 确定高水静压 (HHP) 对微生物生长效率和碳分配的影响.
- 评估地理隔离和环境因素在微生物生物地理学中的作用.
主要方法:
- 微生物社区结构的Illumina高通量测序.
- 对于功能性基因丰度的定量PCR.
- 对代谢活动的H-氨酸的纳入和电子运输系统分析.
- 在现场和大气压 (AP) 测量.
主要成果:
- 微生物社区结构和功能基因的显著沟间变异.
- 玛丽亚纳和雅普海沟的呼吸率较高与有机碳输入增加有关.
- 在所有沟中,在HHP下持续降低 prokaryotic 生长效率 (PGE).
- 惠普将碳分配从生物质生产转移到维护呼吸.
结论:
- 地理隔离和环境过器驱动深海沟中的微生物生物地理.
- 高水静压从根本上限制了深海碳转化效率.
- 基因组潜力不足以预测碳循环速率;现场生理测量是必不可少的.
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