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甲基酸驱动的甲形成及其与北大西洋寡量化地区初级生产的联系
Jan N von Arx1, Abiel T Kidane2, Miriam Philippi2,3
1Max Planck Institute for Marine Microbiology, Bremen, Germany. jarx@mpi-bremen.de.
Nature communications
|October 16, 2023
概括
微生物在低营养水中使用甲基酸作为,意外地产生甲. 这一过程在海洋中具有重要意义.
科学领域:
- 海洋微生物生态学
- 生物地质化学循环是什么
- 海洋学 海洋学 海洋学
背景情况:
- 酸盐是海洋表面水中的限制性营养素.
- 微生物甲基酸的利用可以在含氧水中产生甲,一种温室气体.
- 通过甲基酸盐的有氧甲形成还不太清楚.
研究的目的:
- 在西热带北大西洋研究甲基酸驱动的甲形成.
- 确定控制有氧甲产生的因素.
- 评估甲基酸在海洋碳循环中的生态意义.
主要方法:
- 在上层水柱中测量了甲基酸驱动的甲形成率.
- 评估了酸盐供应对甲生产的影响.
- 分析了与酸盐利用相关的微生物社区组成和基因表达.
主要成果:
- 观察到甲基酸驱动的甲形成的高潜在率 (中位数为0.4nmol甲L-1d-1).
- 即使添加了酸盐,甲的形成仍然存在,这表明正在进行的利用.
- 关键的微生物种群,包括Pelagibacterales和SAR116,拥有并表达用于甲基酸盐利用的基因.
- 阿尔法蛋白细菌对酸盐的利用在更深的海底变得更加显著.
结论:
- 甲基酸盐是寡质海洋中重要的源.
- 甲基酸盐的微生物甲生产发生在有氧水中,并且具有生态相关性.
- 酸盐的利用对海洋生态系统中的碳固定有着显著的贡献.
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