Jia Chunhua, Zhou Guixiang, Ma Ling, Qiu Xiuwen, Zhang Jiabao, Wang Jingkuan, Zhang Congzhi, Chen Lin, Ma Donghao, Zhao Zhanhui, Xue Zaiqi
Northeast Key Laboratory of Conservation and Improvement of Cultivated Land (Shenyang), Ministry of Agriculture and Rural Affairs, College of Land and Environment, Shenyang Agricultural University, Shenyang, China.
Fengqiu Experimental Station of National Ecosystem Research Network of China, State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China.
Front Microbiol. 2024 Jan 9;14:1337507. doi: 10.3389/fmicb.2023.1337507. eCollection 2023.
Ammonia oxidizing archaea (AOA) and ammonia oxidizing bacteria (AOB) have been proven to be key microorganisms driving the ammonia oxidation process. However, under different fertilization practices, there is a lack of research on the impact of interaction between predators and AOA or AOB on nitrogen cycling at the multi-trophic level.
In this study, a network-oriented microscopic culture experiment was established based on four different long-term fertilization practices soils. We used the nitrification inhibitors 2-phenyl-4,4,5,5-tetramethylimidazoline-1-oxide-3-oxyl (PTIO) and 3, 4-Dimethylpyrazole phosphate (DMPP) inhibited AOA and AOB, respectively, to explore the impact of interaction between protists and AOA or AOB on nitrogen transformation.
The results showed that long-term nitrogen application promoted the potential nitrification rate (PNR) and nitrous oxide (NO) emission, and significantly increased the gene abundance of AOB, but had no obvious effect on AOA gene abundance. DMPP significantly reduced NO emission and PNR, while PTIO had no obvious effect on them. Accordingly, in the multi-trophic microbial network, Cercozoa and Proteobacteria were identified as keystone taxa of protists and AOB, respectively, and were significantly positively correlated with NO, PNR and nitrate nitrogen. However, Nitrososphaerota archaeon as the keystone species of AOA, had an obvious negative linkage to these indicators. The structural equation model (SEM) showed that AOA and AOB may be competitors to each other. Protists may promote AOB diversity through direct trophic interaction with AOA.
The interaction pattern between protists and ammonia-oxidizing microorganisms significantly affects potential nitrification rate and NO emission, which has important implications for soil nitrogen cycle.
氨氧化古菌(AOA)和氨氧化细菌(AOB)已被证明是驱动氨氧化过程的关键微生物。然而,在不同施肥方式下,关于捕食者与AOA或AOB之间的相互作用对多营养级氮循环影响的研究尚显不足。
本研究基于四种不同长期施肥方式的土壤建立了面向网络的微观培养实验。我们分别使用硝化抑制剂2-苯基-4,4,5,5-四甲基咪唑啉-1-氧化物-3-氧基(PTIO)和3,4-二甲基吡唑磷酸盐(DMPP)抑制AOA和AOB,以探究原生生物与AOA或AOB之间的相互作用对氮转化的影响。
结果表明,长期施氮促进了潜在硝化速率(PNR)和氧化亚氮(NO)排放,并显著增加了AOB的基因丰度,但对AOA基因丰度无明显影响。DMPP显著降低了NO排放和PNR,而PTIO对它们无明显影响。相应地,在多营养级微生物网络中,Cercozoa和变形菌分别被确定为原生生物和AOB的关键类群,并且与NO、PNR和硝态氮显著正相关。然而,作为AOA关键物种的亚硝化泉古菌与这些指标存在明显的负相关联系。结构方程模型(SEM)表明,AOA和AOB可能相互竞争。原生生物可能通过与AOA的直接营养相互作用促进AOB多样性。
原生生物与氨氧化微生物之间的相互作用模式显著影响潜在硝化速率和NO排放,这对土壤氮循环具有重要意义。