Comammox and ammonia-oxidizing archaea dominated the nitrification under different nitrogen fertilizer levels in acid purple soil of Southwest China

IF 5 2区 农林科学 Q1 SOIL SCIENCE Applied Soil Ecology Pub Date : 2025-02-08 DOI:10.1016/j.apsoil.2025.105941
Jun Xie , Jianguo Jiang , Jie Lu , Wencai Dai , Huarong Guo , Yuanxue Chen , Rong Huang , Zifang Wang , Ming Gao
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Abstract

Ammoxidation represents the initial phase of nitrification and the rate-limiting step of the whole process, primarily influenced by complete ammonia oxidizers (comammox), ammonia-oxidizing archaea (AOA), and ammonia-oxidizing bacteria (AOB). However, in the co-existence of comammox, AOA and AOB, the dominant microorganism of ammoxidation process remains unclear. To elucidate the relative roles of these ammonia oxidizers in ammoxidation under sustained N application, we conducted a long-term fertilization experiment involving five N application rates (0 kg·ha−1, N0; 90 kg·ha−1, N1; 180 kg·ha−1, N2, 270 kg·ha−1, N3; 360 kg·ha−1, N4) and determined the potential nitrification rate (PNR), soil chemical properties, and the diversity and community structure of ammonia oxidizers. Compared to N0, the N application treatments enhanced the PNR, soil organic carbon (SOC), total nitrogen (TN), ammonium (NH4+), nitrate (NO3), and reduced pH and available phosphorus (AP). Furthermore, the four N application treatments increased the shannon index of AOA, AOB and comammox, while also altered the β-diversity of these groups, and N4 treatments increased the Chao1 index of these groups. The proportion of Archaeo (AOA), Nitrosospira (AOB), and Nitrospira (comammox) increasing progressively as N fertilizer dosage increased, while the proportion of Crenarchaeota (AOA) and Bacteria (AOB) exhibited a declining trend. Redundancy analysis indicated that N application influences the composition of AOA through the pH and AP, the composition of AOB via SOC and NO3, and the composition of comammox through pH. The results of structural equation model showed that PNR was significantly affected by N rate, pH, AOA α-diversity and comammox α-diversity. In addition, the standardized total effect of AOA α-diversity (0.41) and comammox α-diversity (0.53) on PNR is much greater than that of AOB (0.064). Consequently, comammox may preferentially inhabit acidic and nutrient-poor soil environments, AOA and comammox were identified as the principal contributors to ammoxidation in acid soil under long-term treatment with different N fertilizer levels.
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不同氮肥水平下西南酸性紫色土壤的硝化作用以Comammox和氨氧化古菌为主
氨氧化反应是硝化反应的初始阶段,是整个过程的限速步骤,主要受完全氨氧化菌(comammox)、氨氧化古菌(AOA)和氨氧化细菌(AOB)的影响。然而,在comammox、AOA和AOB共存的情况下,氨氧化过程的优势微生物尚不清楚。为了阐明这些氨氧化剂在持续施氮条件下氨氧化中的相对作用,我们进行了5种施氮量(0 kg·ha−1,N0;90 kg·ha−1,N1;180 kg·ha - 1, N2, 270 kg·ha - 1, N3;360 kg·ha−1,N4),测定潜在硝化速率(PNR)、土壤化学性质以及氨氧化剂的多样性和群落结构。与氮肥处理相比,施氮处理提高了PNR、土壤有机碳(SOC)、全氮(TN)、铵态氮(NH4+)、硝态氮(NO3−),降低了pH和速效磷(AP)。4种施氮处理增加了AOA、AOB和comammox的shannon指数,同时也改变了这些组β-多样性,N4处理增加了这些组的Chao1指数。随着施氮量的增加,古菌(AOA)、亚硝基螺旋体(AOB)和硝基螺旋体(comammox)的比例逐渐增加,绿古菌(AOA)和细菌(AOB)的比例呈下降趋势。冗余分析表明,施氮通过pH和AP影响AOA的组成,通过SOC和NO3−影响AOB的组成,通过pH影响comammox的组成。结构方程模型结果表明,N率、pH、AOA α-多样性和comammox α-多样性对PNR有显著影响。此外,AOA α-多样性(0.41)和comammox α-多样性(0.53)对PNR的标准化总效应远大于AOB(0.064)。综上所述,不同氮肥水平长期处理酸性土壤氨氧化的主要因子为AOA和comammox。
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来源期刊
Applied Soil Ecology
Applied Soil Ecology 农林科学-土壤科学
CiteScore
9.70
自引率
4.20%
发文量
363
审稿时长
5.3 months
期刊介绍: Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.
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