首页> 外文期刊>The ISME journal emultidisciplinary journal of microbial ecology >Hydrocarbon degradation and response of seafloor sediment bacterial community in the northern Gulf of Mexico to light Louisiana sweet crude oil
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Hydrocarbon degradation and response of seafloor sediment bacterial community in the northern Gulf of Mexico to light Louisiana sweet crude oil

机译:墨西哥北部海湾湾海底沉积物群落的烃劣化与响应光路易斯安那州甜原油

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The Deepwater Horizon (DWH) blowout resulted in the deposition to the seafloor of up to 4.9% of 200 million gallons of oil released into the Gulf of Mexico. The petroleum hydrocarbon concentrations near the wellhead were high immediately after the spill, but returned to background levels a few years after the spill. Microbial communities in the seafloor are thought to be responsible for the degradation of hydrocarbons, however, our knowledge is primarily based upon gene diversity surveys and hydrocarbon concentration in field sediment samples. Here, we investigated the oil degradation potential and changes in bacterial community by amending seafloor sediment collected near the DWH site with crude oil and both oil and Corexit dispersant. Polycyclic aromatic hydrocarbons were rapidly degraded during the first 30 days of incubation, while alkanes were degraded more slowly. With the degradation of hydrocarbons, the relative abundances of Colwelliaceae, Alteromonadaceae, Methylococales, Alcanivorax, Bacteriovorax, and Phaeobacter increased remarkably. However, the abundances of oil-degrading bacteria changed with oil chemistry. Colwelliaceae decreased with increasing oil degradation, whereas Alcanivorax and Methylococcales increased considerably. We assembled seven genomes from the metagenome, including ones belonging to Colwellia, Alteromonadaceae, Rhodobacteraceae, the newly reported genus Woeseia, and candidate phylum NC10, all of which possess a repertoire of genes for hydrocarbon degradation. Moreover, genes related to hydrocarbon degradation were highly enriched in the oiled treatment, suggesting that the hydrocarbons were biodegraded, and that the indigenous microflora have a remarkable potential for the natural attenuation of spilled oil in the deep-sea surface sediment.
机译:深水地平线(DWH)爆发导致海​​底沉积高达42%的200万加仑的石油进入墨西哥湾。井中附近的石油烃浓度立即高,但在溢出后几年返回到背景水平。海底的微生物社区被认为是烃的降解负责,然而,我们的知识主要基于野生沉积物样品中的基因多样性调查和烃浓度。在这里,我们调查了通过修改DWH现场收集的海底沉积物,用原油和石油和核心分散剂修改海底沉积物,调查了细菌群落的油退化潜力和变化。在孵育的前30天期间,多环芳烃迅速降解,而烷烃更慢地降解。随着碳氢化合物的降解,Colwelliveae,AlterOmonadaceae,甲基CoGoRAX,嗜酸盐,菌毒和磷酸杆菌的相对丰度显着增加。然而,油脂细菌的丰度随石油化学改变。 Colwelliveae随着油性降解的增加而降低,而Alcanivorax和甲基环球菌显着增加。我们组装了来自梅塔蛋白酶的七种基因组,包括属于Colwellia,anthoromonadaceae,乳杆菌痤疮,新报告的沃西氏菌和候选Phylum NC10,所有这些都具有用于烃降解的曲目。此外,与烃降解有关的基因在油酸处理中高度富集,表明烃是生物降解的,并且本土微生物的含量具有显着的深海地表沉积物中溢油的巨大潜力。

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