Soil fertility controls ectomycorrhizal mycelial traits in alpine forests receiving nitrogen deposition

菌丝体 生物 生物量(生态学) 农学 外生菌根 营养物 生态系统 菌根 生态学 植物 共生 遗传学 细菌
作者
Wanji Guo,Junxiang Ding,Qitong Wang,Mingzhen Yin,Xiaomin Zhu,Qing Liu,Ziliang Zhang,Huajun Yin
出处
期刊:Soil Biology & Biochemistry [Elsevier]
卷期号:161: 108386-108386 被引量:30
标识
DOI:10.1016/j.soilbio.2021.108386
摘要

Anthropogenic nitrogen (N) deposition is known to profoundly alter the dynamics of mycelial traits of ectomycorrhizal (ECM) fungi in forest ecosystems. The site-specific change in mycelial traits in forests receiving N deposition led us to hypothesize that growth and functional traits of ECM mycelia are controlled by soil nutrient availability in these forests. In this study, we conducted a N fertilization experiment in two alpine forests (Picea asperata Mast. and Pinus armandii Franch.) on the eastern Tibetan Plateau, China, to assess the responses of mycelial growth traits (biomass, production, density and turnover) and functional traits (exploration type and hydrophobicity) to N addition. We quantified the turnover and production of mycelia by determining mycelial biomass in sequentially harvested in-growth mesh bags and by applying mathematical models. We also captured the changes in mycelium exploration type and hydrophobicity by characterizing the ECM fungal community composition. Nitrogen addition promoted mycelial growth, with 79% more mycelial production, 39% greater biomass, and 73% higher density in the P. armandii stand with lower soil N availability (18 mg mineral N kg−1), but N addition repressed the mycelial growth in the P. asperata stand with higher soil N availability (30 mg mineral N kg−1). Additionally, N deposition increased the abundance of genera belonging to 'Contact-Short' and 'Contact-Medium' explorers and reduced that of 'Medium-Long' explorers in the P. armandii stand. N deposition had opposite effect on mycelial functional traits in the P. asperata stand. Collectively, this confirms that the responses of mycelial dynamics to N deposition in forests largely depend on native soil nutrient availability.

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