在阿尔卑斯山草原退化过程中将土壤有机碳矿化与微生物相互作用联系起来
Yang Hu1, Xinya Sun2, Haolin Zhang2
1College of Natural Resources and Environment, Northwest A&F University, Yangling, 712100, China; College of Resources and Environment, Xinjiang Agricultural University, Urumqi, 830052, China.
Journal of environmental management
|September 25, 2025
概括
草地退化加快了土壤有机碳 (SOC) 损失,通过增强微生物代谢能力和网络复杂性,特别是真菌. 这凸显了草原生态系统和土壤碳储存的风险.
科学领域:
- 生态生态学 生态生态学
- 土壤科学 土壤科学
- 微生物学 微生物学
背景情况:
- 草原的退化导致了土壤有机碳 (SOC) 的显著损失.
- 土壤微生物及其相互作用在降解过程中的SOC动态中的作用尚未完全理解.
研究的目的:
- 研究草原退化对土壤微生物群落 (细菌,真菌,原生菌) 的影响.
- 揭示微生物网络,代谢活动和SOC矿化之间的关系.
- 了解对青海-西高原的影响.
主要方法:
- 建立了四个草原退化横段.
- 分析了土壤微生物社区的组成和结构.
- 测量了SOC累积矿化率和微生物代谢指标 (CO2释放,酶活性).
- 评估微生物网络的复杂性和相互作用.
主要成果:
- 草原退化增加了SOC累积矿化率 (4.5-47%) 和微生物代谢能力 (10%增加了三倍).
- 微生物网络复杂性增加,真菌和跨王国复杂性显著增加.
- 细菌和原生体网络的复杂性下降.
- 增强的真菌相互作用表明密集的利基重叠和高效的代谢网络.
结论:
- 草地退化加快了SOC的分解和损失,通过增强微生物活动和真菌网络的复杂性.
- 微生物网络的复杂性和代谢能力可以作为评估SOC损失风险和降解严重性的指标.
- 更好的理解有助于预测和管理草原生态系统中的土壤碳动态.
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