Differential mechanisms underlying responses of soil bacterial and fungal communities to nitrogen and phosphorus inputs in a subtropical forest

物种丰富度 生态系统 微生物种群生物学 土壤pH值 热带和亚热带湿润阔叶林 亚热带 营养物 作文(语言) 生态学 生物 多样性指数 群落结构 氮气 农学 植物 化学 土壤水分 细菌 遗传学 语言学 哲学 有机化学
作者
Yong Li,Dashuan Tian,Jinsong Wang,Shuli Niu,Jing Tian,Denglong Ha,Yuxi Qu,Guangwei Jing,Xiaoming Kang,Bing Song
出处
期刊:PeerJ [PeerJ, Inc.]
卷期号:7: e7631-e7631 被引量:32
标识
DOI:10.7717/peerj.7631
摘要

Atmospheric nitrogen (N) deposition and phosphorus (P) addition both can change soil bacterial and fungal community structure with a consequent impact on ecosystem functions. However, which factor plays an important role in regulating responses of bacterial and fungal community to N and P enrichments remains unclear. We conducted a manipulative experiment to simulate N and P inputs (10 g N · m-2 · yr-1 NH4NO3 or 10 g P · m-2 · yr-1 NaH2PO4) and compared their effects on soil bacterial and fungal species richness and community composition. The results showed that the addition of N significantly increased NH4+ and Al3+ by 99.6% and 57.4%, respectively, and consequently led to a decline in soil pH from 4.18 to 3.75 after a 5-year treatment. P addition increased Al3+ and available P by 27.0% and 10-fold, respectively, but had no effect on soil pH. N addition significantly decreased bacterial species richness and Shannon index and resulted in a substantial shift of bacterial community composition, whereas P addition did not. Neither N nor P addition changed fungal species richness, Shannon index, and fungal community composition. A structural equation model showed that the shift in bacterial community composition was related to an increase in soil acid cations. The principal component scores of soil nutrients showed a significantly positive relationship with fungal community composition. Our results suggest that N and P additions affect soil bacterial and fungal communities in different ways in subtropical forest. These findings highlight how the diversity of microbial communities of subtropical forest soil will depend on future scenarios of anthropogenic N deposition and P enrichment, with a particular sensitivity of bacterial community to N addition.
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