不断流动的各种热友细菌进入寒冷的北极海底
Casey Hubert1, Alexander Loy, Maren Nickel
1Biogeochemistry Group, Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, D-28359 Bremen, Germany. chubert@mpi-bremen.de
概括
寒冷的北极海洋沉积物每年接收超过108热友细菌子. 这些休眠的微生物起源于温暖的地下环境,在温度上升时可以迅速消耗有机物质,影响海洋微生物的多样性.
科学领域:
- 微生物学 微生物学
- 海洋生物学 海洋生物学
- 地质化学 地质化学
背景情况:
- 微生物存在于不适合它们代谢的环境中.
- 了解这些错位的微生物揭示了分散机制,并塑造了微生物多样性.
研究的目的:
- 量化热友细菌流入北极海洋沉积物的数量.
- 为了确定这些热友细菌的起源和运输机制.
主要方法:
- 使用内胞发芽实验来估计细菌供应率.
- 对已识别的细菌进行了植物遗传学和代谢分析.
主要成果:
- 在北极海洋沉积物中检测到热友的Firmicutes细菌 (超过10^8子/m^2/年) 的稳定供应.
- 这些细菌在低温时代谢不活跃,但在50°C时积极降解有机物质.
- 遗传学分析表明,它们起源于温暖的地下石油储库和海洋地生态系统.
结论:
- 海底液流很可能会将热友细菌从温暖的地下环境运送到寒冷的海洋.
- 这些运输途径显著影响海洋微生物群落的组成.
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