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北极海水中和海冰中石油化合物的原位生物降解、光氧化和溶解。

In situ biodegradation, photooxidation and dissolution of petroleum compounds in Arctic seawater and sea ice.

机构信息

Arctic Research Centre, Aarhus University, Aarhus, Denmark; Section for Microbiology and Center for Geomicrobiology, Department of Bioscience, Aarhus University, Aarhus, Denmark.

Department of Plant and Environmental Sciences, Faculty of Science, University of Copenhagen, Copenhagen, Denmark.

出版信息

Water Res. 2019 Jan 1;148:459-468. doi: 10.1016/j.watres.2018.10.066. Epub 2018 Oct 29.

Abstract

In pristine sea ice-covered Arctic waters the potential of natural attenuation of oil spills has yet to be uncovered, but increasing shipping and oil exploitation may bring along unprecedented risks of oil spills. We deployed adsorbents coated with thin oil films for up to 2.5 month in ice-covered seawater and sea ice in Godthaab Fjord, SW Greenland, to simulate and investigate in situ biodegradation and photooxidation of dispersed oil. GC-MS-based chemometric methods for oil fingerprinting were used to identify characteristic signatures for dissolution, biodegradation and photooxidation. In sub-zero temperature seawater, fast degradation of n-alkanes was observed with estimated half-life times of ∼7 days. PCR amplicon sequencing and qPCR quantification of bacterial genes showed that a biofilm with a diverse microbial community colonised the oil films, yet a population related to the psychrophilic hydrocarbonoclastic gammaproteobacterium Oleispira antarctica seemed to play a key role in n-alkane degradation. Although Oleispira populations were also present in sea ice, we found that biofilms in sea ice had 25 to 100 times lower bacterial densities than in seawater, which explained the non-detectable n-alkane degradation in sea ice. Fingerprinting revealed that photooxidation, but not biodegradation, transformed polycyclic aromatic compounds through 50 cm-thick sea ice and in the upper water column with removal rates up to ∼1% per day. Overall, our results showed a fast biodegradation of n-alkanes in sea ice-covered seawater, but suggested that oils spills will expose the Arctic ecosystem to bio-recalcitrant PACs over prolonged periods of time.

摘要

在原始的海冰覆盖的北极水域中,尚未发现石油泄漏的自然衰减潜力,但不断增加的航运和石油开采可能会带来前所未有的石油泄漏风险。我们在格陵兰 SW 戈特霍布峡湾的冰覆盖海水中和海冰中部署了涂有薄油膜的吸附剂,以模拟和研究分散油的原位生物降解和光氧化。我们使用基于 GC-MS 的化学计量方法对油指纹进行分析,以识别溶解、生物降解和光氧化的特征特征。在亚零温度海水中,观察到 n-烷烃的快速降解,估计半衰期约为 7 天。PCR 扩增子测序和 qPCR 定量细菌基因表明,生物膜中存在一个具有多样微生物群落的生物膜,但一个与嗜冷烃降解γ变形菌 Oleispira antarctica 相关的种群似乎在 n-烷烃降解中发挥了关键作用。尽管 Oleispira 种群也存在于海冰中,但我们发现海冰中的生物膜的细菌密度比海水中低 25 到 100 倍,这解释了海冰中无法检测到的 n-烷烃降解。指纹分析表明,光氧化,而不是生物降解,通过 50cm 厚的海冰和上层水柱转化多环芳烃,去除率高达每天约 1%。总的来说,我们的结果表明,在海冰覆盖的海水中,n-烷烃的生物降解速度很快,但这表明,石油泄漏将使北极生态系统在较长时间内暴露于生物难降解的 PAHs 中。

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