Active microbial taxa preferentially assimilate inorganic nitrogen in acidic upland soils using a 15N-DNA-SIP approach
文献类型： 外文期刊
作者： Liu, Ran 1 ; Han, Cheng 1 ; Kang, Yu 3 ; Jiang, Yunbin 1 ; Deng, Huan 4 ; Liu, Kailou 5 ; Zhang, Jinbo 1 ; Zhong, Wenhui 1 ;
作者机构： 1.Nanjing Normal Univ, Sch Geog Sci, Jiangsu Prov Key Lab Mat Cycling & Pollut Control, Nanjing 210023, Peoples R China
2.Jiangsu Ctr Collaborat Innovat Geog Informat Resou, Nanjing 210023, Peoples R China
3.Enshi Tujia&Miao Autonomous Prefecture Acad Agr Sc, Enshi 445000, Peoples R China
4.Nanjing Normal Univ, Sch Environm, Nanjing 210023, Peoples R China
5.Jiangxi Inst Red Soil & Germplasm Resources, Nanchang 331717, Peoples R China
关键词： Inorganic nitrogen immobilization; Soil nitrogen retention; Organic nitrogen; Active microorganisms; 15 N isotope labeling
期刊名称：SOIL BIOLOGY & BIOCHEMISTRY （ 影响因子：9.7； 五年影响因子：10.2 ）
ISSN： 0038-0717
年卷期： 2024 年 188 卷
页码：
收录情况： SCI
摘要： Soil endogenous nitrogen is an essential source of crop nitrogen supply. Nitrogen assimilation is a vital transformation process that maintains nitrogen availability and promotes the mineralization of endogenous organic nitrogen in acidic soils. However, the dominant microbial populations that assimilate NH4+ and NO3- in acidic upland soils were unknown, and their response to long -term fertilization remained unclear. In this study, 15N- labeled NH4+ and NO3- were added to acidic upland soils characterized by long -term (32 years) differentiation in organic matter inputs. Glucose was added to facilitate nitrogen assimilation, and a nitrification inhibitor (dicyandiamide, DCD) was added to distinguish the contribution of NH4+ and NO3- assimilation. Results showed that soil inorganic N assimilation mainly occurred in the first week after inorganic N addition. Soil net inorganic N assimilation rates were 0.006-0.42 mg N kg -1 d-1 in the NH4+, NO3- and NH4++DCD treatments. The analysis of 15N -DNA -based stable isotope probing (SIP) found that the majority of inorganic N assimilation in our soils was conducted by a limited number of active microbial taxa, which accounted for 1.4%-2.0% of the entire bacterial community and 15.7%-28.8% of the fungal community. The dominant bacteria governing inorganic N assimilation in acidic upland soils included Bacillus, Burkholderia-Caballeronia-Paraburkholderia and Micrococcaceae. The primary fungi included Penicillium, Chaetomium, Aspergillus, and Fusarium. No obvious bias was detected in nitrogen assimilation rates and the dominant microbial taxa for NH4+-N and NO3- -N. Compared with unfertilized soil, long -term organic matter input decreased the dominating N assimilating microbial taxa. These findings demonstrate the feasibility of 15N -DNA -SIP technology in soil nitrogen cycling research and suggest the importance of active microbial taxa in acidic agricultural soil nitrogen retention and loss.
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