首页> 美国卫生研究院文献>Applied and Environmental Microbiology >Active Autotrophic Ammonia-Oxidizing Bacteria in Biofilm Enrichments from Simulated Creek Ecosystems at Two Ammonium Concentrations Respond to Temperature Manipulation
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Active Autotrophic Ammonia-Oxidizing Bacteria in Biofilm Enrichments from Simulated Creek Ecosystems at Two Ammonium Concentrations Respond to Temperature Manipulation

机译:在两个铵浓度下模拟温度的生态系统在生物膜浓缩物中的活性自养氨氧化细菌对温度的控制响应

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摘要

The first step of nitrification, the oxidation of ammonia to nitrite, is important for reducing eutrophication in freshwater environments when coupled with anammox (anaerobic ammonium oxidation) or denitrification. We analyzed active formerly biofilm-associated aerobic ammonia-oxidizing communities originating from Ammerbach (AS) and Leutra South (LS) stream water (683 ± 550 [mean ± standard deviation] and 16 ± 7 μM NH4+, respectively) that were developed in a flow-channel experiment and incubated under three temperature regimens. By stable-isotope probing using 13CO2, we found that members of the Bacteria and not Archaea were the functionally dominant autotrophic ammonia oxidizers at all temperatures under relatively high ammonium loads. The copy numbers of bacterial amoA genes in 13C-labeled DNA were lower at 30°C than at 13°C in both stream enrichment cultures. However, the community composition of the ammonia-oxidizing bacteria (AOB) in the 13C-labeled DNA responded differently to temperature manipulation at two ammonium concentrations. In LS enrichments incubated at the in situ temperature (13°C), Nitrosomonas oligotropha-like sequences were retrieved with sequences from Nitrosospira AmoA cluster 4, while the proportion of Nitrosospira sequences increased at higher temperatures. In AS enrichments incubated at 13°C and 20°C, AmoA cluster 4 sequences were dominant; Nitrosomonas nitrosa-like sequences dominated at 30°C. Biofilm-associated AOB communities were affected differentially by temperature at two relatively high ammonium concentrations, implicating them in a potential role in governing contaminated freshwater AOB distributions.
机译:硝化的第一步是将氨氧化为亚硝酸盐,这对于减少厌氧氨氧化(厌氧铵氧化)或反硝化作用在淡水环境中的富营养化至关重要。我们分析了源自Ammerbach(AS)和Leutra South(LS)溪流水(683±550 [平均值±标准偏差]和16±7μMNH4 + )的活跃的,以前与生物膜相关的需氧氨氧化社区。 ,分别在流道实验中开发并在三种温度方案下孵育。通过使用 13 CO2进行稳定同位素探测,我们发现,在较高的铵负载下,在所有温度下,细菌而不是古细菌都是功能上占优势的自养氨氧化器。在两种流富集培养中, 13 C标记的DNA中细菌amoA基因的拷贝数在30°C时均低于13°C。然而, 13 C标记的DNA中氨氧化细菌(AOB)的群落组成在两种铵浓度下对温度操纵的反应不同。在原位温度(13°C)下孵育的LS富集液中,亚硝化单胞菌类似的序列被从亚硝基螺菌AmoA簇4的序列中检索出来,而亚硝基螺菌序列的比例在较高温度下增加。在13°C和20°C孵育的AS富集中,AmoA簇4个序列占主导地位。亚硝基亚硝基亚种序列在30℃下占主导。在两个相对较高的铵浓度下,与生物膜相关的AOB群落受到温度的差异影响,这暗示它们在控制受污染的淡水AOB分布中具有潜在作用。

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