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Autotrophic Ammonia-Oxidizing Bacteria Contribute Minimally to Nitrification in a Nitrogen-Impacted Forested Ecosystem

机译:自养氨氧化细菌对氮影响的森林生态系统中的硝化作用贡献最小

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摘要

Deposition rates of atmospheric nitrogenous pollutants to forests in the San Bernardino Mountains range east of Los Angeles, California, are the highest reported in North America. Acidic soils from the west end of the range are N-saturated and have elevated rates of N-mineralization, nitrification, and nitrate leaching. We assessed the impact of this heavy nitrogen load on autotrophic ammonia-oxidizing communities by investigating their composition, abundance, and activity. Analysis of 177 cloned β-Proteobacteria ammonia oxidizer 16S rRNA genes from highly to moderately N-impacted soils revealed similar levels of species composition; all of the soils supported the previously characterized Nitrosospira clusters 2, 3, and 4. Ammonia oxidizer abundance measured by quantitative PCR was also similar among the soils. However, rates of potential nitrification activity were greater for N-saturated soils than for soils collected from a less impacted site, but autotrophic (i.e., acetylene-sensitive) activity was low in all soils examined. N-saturated soils incubated for 30 days with ammonium accumulated additional soluble ammonium, whereas less-N-impacted soils had a net loss of ammonium. Lastly, nitrite production by cultivated Nitrosospira multiformis, an autotrophic ammonia-oxidizing bacterium adapted to relatively high ammonium concentrations, was significantly inhibited in pH-controlled slurries of sterilized soils amended with ammonium despite the maintenance of optimal ammonia-oxidizing conditions. Together, these results showed that factors other than autotrophic ammonia oxidizers contributed to high nitrification rates in these N-impacted forest soils and, unlike many other environments, differences in nitrogen content and soil pH did not favor particular autotrophic ammonia oxidizer groups.
机译:在加利福尼亚州洛杉矶以东的圣贝纳迪诺山脉范围内,大气含氮污染物在森林中的沉积率是北美最高的。该范围西端的酸性土壤是N饱和的,并且N矿化,硝化和硝酸盐浸出的速率较高。通过研究它们的组成,丰度和活性,我们评估了重氮负荷对自养氨氧化社区的影响。分析了从高至中度氮影响土壤中的177个克隆的β-Proteobacteria氨氧化器16S rRNA基因,发现相似的物种组成水平;所有土壤均支持先前表征的硝化螺菌菌簇2、3和4。通过定量PCR测定的氨氧化剂丰度在土壤中也相似。但是,N饱和土壤的潜在硝化活性速率要高于从受影响较小的地点收集的土壤,但是在所有检测的土壤中,自养(即对乙炔敏感)活性较低。与铵盐一起温育30天的N饱和土壤会累积额外的可溶性铵盐,而受N较少影响的土壤则有氨的净损失。最后,尽管适应氨水的最佳条件得以维持,但在用铵改良的无菌土壤的pH控制泥浆中,通过培养的硝化螺旋体(一种适应于较高铵浓度的自养氨氧化细菌)产生的亚硝酸盐被显着抑制。总之,这些结果表明,在这些受氮影响的森林土壤中,除了自养氨氧化剂以外的其他因素也导致了较高的硝化率,并且与许多其他环境不同,氮含量和土壤pH的差异不利于特定的自养氨氧化剂组。

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