在全球变化下的土壤中的微生物循环基因
Xuewei Wang1, Hui Guo2, Jianing Wang1
1State Key Laboratory of Herbage Improvement and Grassland Agro-Ecosystems, Centre for Grassland Microbiome, College of Pastoral Agriculture Science and Technology, Lanzhou University, Lanzhou, Gansu, China.
Global change biology
|April 15, 2024
概括
气候变化影响了西藏高山土壤中的循环. 气候变暖和降雨量增加促进微生物循环,增加了植物和微生物的P可用性.
科学领域:
- 环境科学 环境科学
- 微生物学 微生物学
- 土壤科学 土壤科学
背景情况:
- 气候变化,特别是气候变暖和降水变化,显著影响了高山生态系统中的生物地球化学循环.
- 在西藏高原的P限高山草原土壤中 (P) 循环对环境变化敏感.
- 气候变化对细菌循环基因 (PCG) 和P转换的影响在这些生态系统中仍然不太清楚.
研究的目的:
- 研究变暖和改变降水对土壤PCG和P转化的单独和综合影响.
- 了解细胞外和细胞内P循环基因对气候变化因素的反应.
- 在不断变化的气候条件下,确定参与P循环的关键微生物代谢途径.
主要方法:
- 用转基因组分析来评估细菌PCG群体.
- 一个操纵实验模拟了变暖和改变了降水场景.
- 测量了土壤中的生物可利用 (Olsen-P) 和有机 (NaOH-Po).
主要成果:
- 变暖和降水增加分别增加了13%和20%的生物可用P (AP),主要是通过增强的有机P水解.
- 降水量减少导致土壤AP减少5.3%.
- PCG的丰富性和丰富性比改变的降水更容易受到变暖的影响,而加热和降水增加的结合显示出积极的影响,而不是单个因素.
结论:
- 变暖,特别是与降水增加相结合时,显著增强微生物P循环,加速细胞外和细胞内过程.
- 特定的细胞内PCG参与酸盐代谢,转移酶系统,氧化酸化和与P池相关的 purin代谢.
- 变暖刺激了带有细胞外P循环基因 (phoD,phoX) 的细菌,促进了高山土壤中的有机P矿化和P生物可用性.
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