在无氧湖泊沉积物中,藻类和巨生物在甲基生成上的有机物质的可变促进
Tong Wang1, Maidina Zhumabieke2, Nan Zhang3
1State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, PR China; University of Chinese Academy of Sciences, Beijing, 100049, PR China.
Environmental research
|August 20, 2023
概括
藻类有机物刺激了湖泊沉积物中的更多的甲产量,而不是巨型生物有机物. 这凸显了藻类繁殖增加对湖泊甲释放的影响.
科学领域:
- 环境科学 环境科学
- 微生物学 微生物学
- 地质化学 地质化学
背景情况:
- 浅湖是大气中甲 (CH4) 的重要自然来源.
- 在湖泊沉积物中输入的本土有机物 (OM) 推动了甲基生成.
- 藻类与宏观植物OM对甲基生成的独特影响仍然不清楚.
研究的目的:
- 研究藻类和宏观植物OM对甲生产的差异影响.
- 分析这些OM类型对湖泊沉积物中甲性考古社区的影响.
- 为了比较两个不同的浅层环保湖的这些效应:Chaohu湖和Taihu湖.
主要方法:
- 一个148天的化实验,使用来自湖和太湖的沉积物.
- 在沉积物中添加藻类和巨型植物起源的有机物质 (OM).
- 定期监测甲 (CH4) 产量,并通过qPCR和高通量测序对甲原体进行终结化分析.
主要成果:
- 在两种湖泊沉积物中,藻类OM显著刺激了CH4的产生,超过了宏观植物OM.
- 宏观植物OM在两个湖泊中促进了相对较大的CH4产量,而藻类OM在湖中显示出更大的刺激.
- 宏观性OM增加了mcrA基因拷贝 (17.0-20.1倍) 并促进了乙类甲原体,而藻类OM对mcrA和甲原体结构的影响因湖泊而异.
结论:
- 与宏观植物OM相比,藻类OM是浅湖沉积物中甲生产的更强大的刺激剂.
- OM的起源不同地影响甲生产途径和甲产生的社区.
- 藻类繁殖的增加,加上巨型植物种群的减少,可能会导致湖泊中甲释放的增加,这需要进一步调查.
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