在中国的湖泊中以温度为媒介的微生物碳利用.
Yao Guo1,2, Songsong Gu2,3, Kaixuan Wu1,2
1State Key Laboratory of Freshwater Ecology and Biotechnology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan, the People's Republic of China.
Global change biology
|July 10, 2023
概括
温度升温通过改变细菌群落及其相互作用来促进水生微生物的碳使用. 这项研究揭示了湖泊中的微生物如何适应气候变化,影响碳循环.
科学领域:
- 环境微生物学环境微生物学
- 水生生态学 水生生态学
- 生物地质化学循环是什么
背景情况:
- 微生物对于水生碳循环至关重要.
- 了解微生物对大面积温度变化的功能反应是有限的.
研究的目的:
- 探索微生物群落如何沿着温度梯度利用碳基板.
- 为了确定推动这些变化的生态机制,以应对气候变化.
主要方法:
- 在中国的47个湖泊中使用了空间替代时间的方法.
- 分析了微生物群落的组成和碳基质利用在~15°C的温度梯度.
主要成果:
- 温暖的湖泊显示碳度较低,碳利用率更高.
- 细菌群体的转变 (增加的菌,Actinobacteriota;减少的蛋白菌) 与温度相关.
- 核心微生物物种发生了变化,影响了氨基酸,碳水化合物和一般碳基质的利用.
结论:
- 温度通过改变微生物群落结构和相互作用,显著调节水中碳利用.
- 识别核心物种为未来变暖下内陆水域潜在的碳捕获提供了见解.
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