肥施肥促进与矿物相关的土壤有机碳形成与形原体相关
Lin Chen1, Xiuli Xin1, Jingwang Li1,2
1Fengqiu Experimental Station of National Ecosystem Research Network of China, Institute of Soil Science, Chinese Academy of Sciences, East Beijing Road No. 71, Nanjing, 210008, Jiangsu Province, China.
Microbial ecology
|July 4, 2023
概括
化肥通过增强微生物活动和原生菌种群,显著提高了土壤有机碳的积累. 这项研究突出了原生植物在促进农业土壤碳捕集中的作用.
科学领域:
- 土壤科学 土壤科学
- 微生物学 微生物学
- 生态生态学 生态生态学
背景情况:
- 长期施肥会影响土壤有机碳 (C) 的积累.
- 细菌在形成矿物相关有机C (MAOC) 中发挥着关键作用.
- 在受精过程中,原生体对MAOC形成的影响还不太清楚.
研究的目的:
- 研究 (N) 和 (P) 施肥对MAOC形成的影响.
- 探索MAOC形成和长期受精的耕地土壤中的原生群体之间的关系.
- 评估P受精对微生物C同化和原生体丰度的影响.
主要方法:
- 微观宇宙实验使用13C-葡萄糖标记土壤从长期受精实地试验.
- 对13C-MAOC含量,原生体和细菌群体组成以及细菌功能基因丰度的分析.
- 研究原生体和细菌之间的共发生网络,并进行相关性分析.
主要成果:
- 长期受精,特别是P受精,显著增加了13C-MAOC含量.
- P补充丰富的原生体 (Amoebozoa,Cercozoa) 和细菌 (Acidobacteriota,Bacteroidota,Gammaproteobacteria) 种群. 在这种情况下,P补充丰富的原生体 (Amoebozoa,Cercozoa) 和细菌 (Acidobacteriota,Bacteroidota,Gammaproteobacteria) 种群.
- 形原生群体与细菌群体,功能基因和13C-MAOC含量有很强的相关性;P受精增强了细菌的13C同化,与Cercozoa负相关.
结论:
- 化肥显著增强了与矿物相关的有机C (MAOC) 的形成,部分由形原体介导.
- 在受精制度下,原生群体与细菌动力学和碳循环密切相关.
- 这项研究建议利用原生植物的潜力,改善农业生态系统的地下碳积累.
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