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Linking of Microorganisms to Phenanthrene Metabolism in Soil by Analysis of 13C-Labeled Cell Lipids

机译:通过13 C-标记细胞脂质的分析将微生物与土壤中的菲代谢联系起来

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摘要

Phenanthrene-metabolizing soil microbial communities were characterized by examining mineralization of [14C]phenanthrene, by most-probable-number (MPN) counting, by 16S-23S spacer DNA analysis of the numerically dominant, culturable phenanthrene-degrading isolates, and by examining incorporation of [13C]phenanthrene-derived carbon into sterols and polar lipid fatty acids (PLFAs). An unpolluted agricultural soil, a roadside soil diffusely polluted with polycyclic aromatic hydrocarbons (PAHs), and two highly PAH-polluted soils from industrial sites were analyzed. Microbial phenanthrene degraders were not detected by MPN counting in the agricultural soil and the roadside soil. In the industrial soils, phenanthrene degraders constituted 0.04 and 3.6% of the total number of CFU. 16S-23S spacer DNA analysis followed by partial 16S DNA sequencing of representative isolates from one of the industrial soils showed that one-half of the isolates belonged to the genus Sphingomonas and the other half were closely related to an unclassified beta-proteobacterium. The 13C-PLFA profiles of the two industrial soils were relatively similar and resembled the profiles of phenanthrene-degrading Sphingomonas reference strains and unclassified beta-proteobacterium isolates but did not match the profiles of Pseudomonas, Mycobacterium, or Nocardia reference strains. The 13C-PLFA profiles of phenanthrene degraders in the agricultural soil and the roadside soil were different from each other and different from the profiles of the highly polluted industrial soils. Only in the roadside soil were 10me/12me18:0 PLFAs enriched in 13C, suggesting that actinomycetes metabolized phenanthrene in this soil. The 13C-PLFA profiles of the unpolluted agricultural soil did not resemble the profiles of any of the reference strains. In all of the soils investigated, no excess 13C was recovered in the 18:2ω6,9 PLFA, suggesting that fungi did not contribute significantly to assimilation of [13C]phenanthrene.
机译:通过[ 14 C]菲的矿化作用,最大概率数(MPN)计数,通过16S-23S间隔DNA分析数字优势,可培养的菲来表征菲代谢土壤微生物群落降解分离物,并研究将[ 13 C]菲衍生的碳掺入固醇和极性脂质脂肪酸(PLFA)中。分析了未污染的农业土壤,被多环芳烃(PAHs)分散污染的路边土壤,以及来自工业现场的两种高PAH污染土壤。通过MPN计数在农业土壤和路边土壤中未检测到微生物菲降解物。在工业土壤中,菲降解物占CFU总数的0.04%和3.6%。通过对16S-23S间隔DNA进行分析,然后对其中一种工业土壤中的代表性分离株进行16S DNA局部测序,结果表明,分离株的一半属于鞘氨醇单胞菌属,另一半与未分类的β-变形杆菌密切相关。两种工业土壤的 13 C-PLFA谱图相对相似,类似于菲降解的鞘氨醇单胞菌参考菌株和未分类的β变形杆菌分离株的谱图,但与假单胞菌,分枝杆菌或诺卡氏菌参考菌株。农业土壤和路旁土壤中菲降解物的 13 C-PLFA分布图互不相同,也不同于高污染工业土壤的分布图。仅在路旁土壤中10me / 12me18:0 PLFA富含 13 C,这表明放线菌在该土壤中代谢了菲。未污染的农业土壤的 13 C-PLFA谱图与任何参考菌株的谱图都不相似。在所有调查的土壤中,18:2ω6,9PLFA中均未回收过量的 13 C,这表明真菌对[ 13 C]的吸收没有明显的作用。菲。

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