在西藏高原永久土解期间,改变微生物群落结构和功能潜力
Xiaotong Tang1, Miao Zhang2, Zhengkun Fang1
1State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China.
FEMS microbiology ecology
|September 28, 2023
概括
由于变暖而导致的西藏永久土融化改变了微生物群落. 这种转变加速了这些敏感的高山生态系统的碳分解和甲释放.
科学领域:
- 环境微生物学环境微生物学
- 永久土科学 永久土科学
- 气候变化研究研究 气候变化研究
背景情况:
- 西藏高原的永久土储存了大量的碳.
- 温度的升温威胁到永久土的稳定性和碳捕获.
- 在西藏高原,微生物对永久土融化的反应尚不清楚.
研究的目的:
- 为了比较微生物群落和功能潜力在解西藏永久土.
- 研究气候变暖对微生物多样性和稳定性的影响.
- 评估碳降解和甲基生成基因的变化.
主要方法:
- 高通量定量PCR (qPCR) 分析.
- 微生物社区的概况.
- 功能基因 (例如mcrA) 的分析.
主要成果:
- 随着永久土的解,微生物多样性下降.
- 克洛洛,细菌,欧亚古和巴斯亚古的丰富性增加.
- 碳降解和甲基生成的基因,包括mcrA,呈现出更多的丰度.
- 甲原与甲的比率增加,表明甲产量增加.
结论:
- 西藏永久土中的微生物群落对变暖很敏感.
- 永久土的解促进了微生物活动,加速了碳的释放,特别是甲.
- 这些变化对全球碳预算和气候监管构成风险.
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