菌根 - 沙普罗特罗夫相互作用和碳循环在树叶球
Binu M Tripathi1,2, Juan Piñeiro1,3, Chansotheary Dang1
1Division of Plant and Soil Sciences, West Virginia University, Morgantown, West Virginia, USA.
Global change biology
|April 2, 2025
概括
在未来的全球变化下,土壤碳储存可能在状菌根 (AM) 土壤中比生菌根 (ECM) 土壤更多地增加. 这是由于微生物对增加的根排液的反应不同,影响土壤有机物质.
科学领域:
- 土壤科学 土壤科学
- 微生物生态学 微生物生态学
- 全球变化生物学
背景情况:
- 由于气候变化,预计土壤的不稳定碳输入量将增加.
- 菌根真菌对微生物对增加碳输入的反应的影响尚不清楚.
- 了解这些相互作用对于预测土壤有机物动态至关重要.
研究的目的:
- 为了研究状菌根 (AM) 和生态菌根 (ECM) 关联如何影响细菌群落和土壤有机物 (SOM) 生物地质化学在增加的可变碳输入下.
- 为了比较细菌生长和土壤呼吸在AM和ECM土壤中接收合成根排泄物的反应.
主要方法:
- 使用18O-H2O进行定量稳定同位素探测.
- 合成根排泄物被添加到树木的根球土壤中,含有AM和ECM真菌的不同度 (0, 250, 500, 1000μg Cg soil-1).
- 测量了细菌生长特征,微生物生物质碳 (MBC) 和土壤呼吸.
主要成果:
- 在AM和ECM土壤中,土壤呼吸随着排泄物添加而增加.
- 微生物生物质碳 (MBC) 在AM土壤中增加,但在ECM土壤中减少.
- 在AM土壤中的排泄物增强了细菌生长率和生物质生产,而在ECM土壤中,MBC死亡率增加了.
结论:
- 在AM和ECM根球土壤中的细菌群体对增加的可变碳输入表现出不同的反应.
- 在未来的全球变化场景下,AM土壤可能会积累更多的土壤有机碳 (SOC),原因是微生物生长和生物质生产的增强.
- 在ECM土壤中,可能会出现微生物死亡率的增加,这可能会限制SOC的增加.
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