氨氧化与暗DIC固定之间的时空空间和温度依赖的断开在深度寡头性康斯坦茨湖的DIC固定
Jade Bosviel1, Katharina Kitzinger2,3, Francesca Vulcano1
1Leibniz Institute DSMZ - German Collection of Microorganisms and Cell Cultures, Inhoffenstr. 7B, Braunschweig D-38124, Germany.
ISME communications
|November 26, 2025
概括
尽管有假设,但氨氧化和深湖中的暗碳固定并没有直接联系. 氨氧化古生物 (AOA) 对碳固定起到最小的作用,而其他微生物则起到更大的作用.
科学领域:
- 临界技术 临界技术
- 微生物生态学 微生物生态学
- 生物地质化学生物地质化学
背景情况:
- 深奥的寡质湖含有全球大部分湖水.
- 氨氧化和暗溶解无机碳 (DIC) 固定是关键的低气质过程.
- 据推测,氨氧化古生物 (AOA) 将这些过程联系在一起.
研究的目的:
- 研究康斯坦斯湖的低膜中氨氧化和黑暗DIC固定之间的关系.
- 量化AOA对这些过程的贡献.
- 确定负责黑暗DIC固定的微生物群.
主要方法:
- 基于稳定同位素的活性测量在热线下面和中央的 hypolimnion.
- 季节性监测氨氧化和DIC固定速率.
- 温度操纵实验和元转录组分析.
主要成果:
- 氨氧化和暗DIC固定速率因季节和空间而异,有不同的温度最佳.
- 在整体DIC固定中,AOA的贡献仅为11%.
- 转录组学揭示了密码体,蓝藻细菌和其他细菌,而不是AOA,是DIC固定的主要驱动因素.
结论:
- 氨氧化和暗色DIC固定在寡型湖海波林尼亚中脱.
- 淡水AOA在黑暗DIC固定中起到较小的作用.
- 非化微生物可能利用卡尔文循环在黑暗中的氧化还原平衡.
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