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

机译:亚热带森林土壤细菌和真菌群落对氮和磷输入的响应的差异机制

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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.
机译:大气中氮(N)的沉积和磷(P)的添加均可改变土壤细菌和真菌的群落结构,从而对生态系统功能产生影响。然而,尚不清楚哪个因子在调节细菌和真菌群落对氮和磷富集的反应中起重要作用。我们进行了一个模拟N和P输入(10 g N·m −2 ·yr −1 NH4NO3或10 g P·m −2 < / sup>·yr −1 NaH2PO4),并比较了它们对土壤细菌和真菌物种丰富度和群落组成的影响。结果表明,氮的添加分别使NH4 + 和Al 3 + 分别增加99.6%和57.4%,从而导致土壤pH从4.18下降。治疗5年后降至3.75。磷的添加分别使Al 3 + 和有效磷增加27.0%和10倍,但对土壤pH值没有影响。氮的添加显着降低了细菌物种的丰富度和香农指数,并导致细菌群落组成发生了显着变化,而磷的添加却没有。氮和磷的添加均未改变真菌物种的丰富度,香农指数和真菌群落组成。结构方程模型表明,细菌群落组成的变化与土壤酸性阳离子的增加有关。土壤养分的主成分得分与真菌群落组成呈显着正相关。我们的结果表明,氮和磷的添加以不同的方式影响亚热带森林中的细菌和真菌群落。这些发现凸显了亚热带森林土壤微生物群落的多样性将如何取决于人为氮沉积和磷富集的未来情况,以及细菌群落对氮添加的特别敏感性。

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