河流水环境中的有氧甲合成和动态
Abdullah M Alowaifeer1, Qian Wang2, Brian Bothner3
1Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, Montana, USA.
概括
河流中的有氧生物生成甲生产与光合作用微生物和温度有关. 河流微生物可以将甲基化胺转化为甲,其度每天和季节性变化.
科学领域:
- 环境微生物学 环境微生物学
- 生物地质化学生物地质化学
- 河流生态 河流生态
背景情况:
- 空气生物基甲生产越来越被认为是自然环境中的重要过程.
- 了解河流中的甲来源对于准确的环境评估和气候建模至关重要.
- 以前的研究已经强调了微生物活动,有机物和甲循环之间的潜在联系.
研究的目的:
- 在自由流动的河流系统中研究有氧生物生成甲产生的现象.
- 确定甲度,环境因素,光合作用微生物和甲基化胺之间的关系.
- 评估河流微生物组在甲合成中的代谢潜力.
主要方法:
- 在黄石河中监测了甲度,与温度,甲基 (Chl a) 和甲基化胺相关.
- 在不同河流区域 (边缘与开放流) 进行了白天测量和地表流量评估.
- 实验室实验涉及将河水添加糖氨酸贝他因 (GB) 或甲基胺 (MMA) 来评估甲产量.
主要成果:
- 甲度与温度和Chl a正相关,在夜间达到峰值,在阳光高峰期间最低.
- 与开放式流动相比,在静止的边缘水域观察到更高的甲流量.
- 虽然甲基化氨基存在,但在微生物溶解事件中它们的释放与甲的增加没有相关性;然而,增加GB或MMA显著增加了甲的产生.
结论:
- 光营养微生物在河流环境中的甲合成中发挥着作用.
- 河流的微生物组显示出将甲基胺转化为甲的代谢能力.
- 河流甲度表现出动态的日间和季节性变化.
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