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Ammonia concentration determines differential growth of ammonia-oxidising archaea and bacteria in soil microcosms

机译:氨的浓度决定土壤微观世界中氨氧化古细菌和细菌的差异生长

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摘要

The first step of nitrification, oxidation of ammonia to nitrite, is performed by both ammonia-oxidising archaea (AOA) and ammonia-oxidising bacteria (AOB) in soil, but their relative contributions to ammonia oxidation and existence in distinct ecological niches remain to be determined. To determine whether available ammonia concentration has a differential effect on AOA and AOB growth, soil microcosms were incubated for 28 days with ammonium at three concentrations: native (control), intermediate (20 μg NH4+-N per gram of soil) and high (200 μg NH4+-N per gram of soil). Quantitative PCR demonstrated growth of AOA at all concentrations, whereas AOB growth was prominent only at the highest concentration. Similarly, denaturing gradient gel electrophoresis (DGGE) analysis revealed changes in AOA communities at all ammonium concentrations, whereas AOB communities changed significantly only at the highest ammonium concentration. These results provide evidence that ammonia concentration contributes to the definition of distinct ecological niches of AOA and AOB in soil.
机译:硝化的第一步是将氨氧化成亚硝酸盐,这是由土壤中的氨氧化古细菌(AOA)和氨氧化细菌(AOB)共同完成的,但是它们对氨氧化的相对贡献以及在独特的生态位中的存在仍有待进一步研究。决心。为了确定可利用的氨水浓度是否对AOA和AOB生长有不同的影响,将土壤微观世界与以下三种浓度的铵盐一起温育28天:天然(对照),中间(20μgNH4 + -N (每克土壤200μgNH4 + -N)和高。定量PCR显示在所有浓度下AOA的生长,而仅在最高浓度下AOB的生长才显着。同样,变性梯度凝胶电泳(DGGE)分析显示在所有铵浓度下AOA群落均发生变化,而仅在最高铵浓度下AOB群落发生显着变化。这些结果提供了氨浓度有助于土壤中AOA和AOB独特生态位的定义的证据。

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