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Biodegradation of Petroleum Hydrocarbons in Seawater at Low Temperatures (0-5 degrees C) and Bacterial Communities Associated with Degradation.

机译:低温(0-5摄氏度)海水中石油碳氢化合物的生物降解以及与降解相关的细菌群落。

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In this study biodegradation of hydrocarbons in thin oil films was investigated in seawater at low temperatures, 0 and 5 degrees C. Heterotrophic (HM) or oil-degrading (ODM) microorganisms enriched at the two temperatures showed 16S rRNA sequence similarities to several bacteria of Arctic or Antarctic origin. Biodegradation experiments were conducted with a crude mineral oil immobilized as thin films on hydrophobic Fluortex adsorbents in nutrient-enriched or sterile seawater. Chemical and respirometric analysis of hydrocarbon depletion showed that naphthalene and other small aromatic hydrocarbons (HCs) were primarily biodegraded after dissolution to the water phase, while biodegradation of larger polyaromatic hydrocarbons (PAH) and C(10)-C(36) n-alkanes, including n-hexadecane, was associated primarily with the oil films. Biodegradation of PAH and n-alkanes was significant at both 0 and 5 degrees C, but was decreased for several compounds at the lower temperature. n-Hexadecane biodegradation at the twotemperatures was comparable at the end of the experiments, but was delayed at 0 degrees C. Investigations of bacterial communities in seawater and on adsorbents by PCR amplification of 16S rRNA gene fragments and DGGE analysis indicated that predominant bacteria in the seawater gradually adhered to the oil-coated adsorbents during biodegradation at both temperatures. Sequence analysis of most DGGE bands aligned to members of the phyla Proteobacteria (Gammaproteobacteria) or Bacteroidetes. Most sequences from experiments at 0 degrees C revealed affiliations to members of Arctic or Antarctic consortia, while no such homology was detected for sequences from degradation experiment run at 5 degrees C. In conclusion, marine microbial communities from cold seawater have potentials for oil film HC degradation at temperatures
机译:在这项研究中,研究了在低温,0和5摄氏度的海水中对油膜中碳氢化合物的生物降解。在这两个温度下富集的异养(HM)或油降解(ODM)微生物显示出与几种细菌的16S rRNA序列相似性北极或南极起源。生物降解实验是通过在营养丰富的或无菌的海水中以疏水性Fluortex吸附剂上的薄膜形式固定的粗矿物油进行的。碳氢化合物耗竭的化学和呼吸分析表明,萘和其他小芳烃(HCs)溶解至水相后主要被生物降解,而较大的聚芳烃(PAH)和C(10)-C(36)正构烷烃则被生物降解。 ,包括正十六烷,主要与油膜有关。 PAH和正构烷烃的生物降解在0和5摄氏度均很明显,但在较低温度下几种化合物的生物降解却降低了。在两个温度下正十六烷的生物降解在实验结束时是可比的,但在0摄氏度时被延迟。通过16S rRNA基因片段的PCR扩增和DGGE分析,对海水和吸附剂上的细菌群落进行了研究,结果表明,在两个温度下的生物降解过程中,海水逐渐粘附在涂油的吸附剂上。大多数DGGE谱带的序列分析都与门的Proteobacteria(Gammaproteobacteria)或拟杆菌(Bacteroidetes)成员对齐。在0摄氏度的实验中,大多数序列显示出与北极或南极财团的隶属关系,而在5摄氏度的降解实验中,未发现此类同源性。总之,来自冷海水的海洋微生物群落具有油膜HC的潜力。在温度

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