土壤碳
丛枝菌根真菌
生态系统
环境科学
共生
陆地生态系统
菌根真菌
全球变暖
气候变化
氮气
总有机碳
土壤有机质
全球变化
农学
生物
碳纤维
生态学
氮气循环
陆生植物
丛枝菌根
菌根
植物
土壤生物学
球囊菌门
化学
微生物种群生物学
丛枝菌根
土壤水分
土壤化学
碳循环
生物地球化学
δ13C
作者
Yunpeng Qiu,Yunfeng Zhao,Bianbian Wang,Xi Xu,Tangqing He,Kangcheng Zhang,Tongshuo Bai,Zhen Li,Chenglong Ye,Christopher J. Gillespie,Xiaodong Wang,Yexin Zhao,Lijin Guo,Kaiyun Qian,Huaihai Chen,Xinxin Cao,Shuqi Wu,Liang Guo,Ripley H. Tisdale,Alex Woodley
标识
DOI:10.1038/s41467-026-69301-7
摘要
Plant roots and arbuscular mycorrhizal fungi (AMF) form a ubiquitous symbiosis in terrestrial ecosystems and critically affect soil organic carbon (SOC) dynamics. However, how roots and AMF mediate the impact of reactive nitrogen (Nr) and climate warming on SOC remains unclear. Using a multi-year Nr addition and simulated warming experiment in a semi-arid grassland, we show that Nr input and warming alter SOC by reshaping plant communities and inducing multidimensional tradeoffs among fine-root traits and AMF communities. Stable isotope (13C) tracing revealed that Nr- and warming-induced changes in roots and AMF reduced C input belowground, and mineral-associated organic C and microbial necromass in soil, while stimulating organic C decomposition. Nr input also increased soil N:P ratios and shifted AMF communities toward taxa with finer extraradical hyphae, weakening SOC protection. Together, these findings highlight root-AMF interactions as critical regulators and improve predictions of long-term SOC dynamics under future climate change.
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