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南极利文斯顿岛土壤中土著微生物对菲的生物降解作用。

Biodegradation of phenanthrene by indigenous microorganisms in soils from Livingstone Island, Antarctica.

机构信息

Lancaster Environment Centre, Lancaster University, Lancaster, UK.

出版信息

FEMS Microbiol Lett. 2012 Apr;329(1):69-77. doi: 10.1111/j.1574-6968.2012.02501.x. Epub 2012 Feb 23.

Abstract

Biodegradation of polycyclic aromatic hydrocarbons (PAHs) in soils has been linked to history of exposure to PAHs and prevailing environmental conditions. This work assessed the capacity of indigenous microorganisms in soils collected in Livingstone Island (South Shetlands Islands, Antarctica) with no history of pollution (∑PAHs: 0.14-1.47 ng g(-1) dw) to degrade (14) C-phenanhthrene at 4, 12 and 22 °C. The study provides evidence of the presence of phenanthrene-degrading microorganisms in all studied soils. Generally, the percentage of (14) C-phenanhthrene mineralized increased with increasing temperature. The highest extent of (14) C-phenanhthrene mineralization (47.93%) was observed in the slurried system at 22 °C. This work supports findings of the presence of PAH-degrading microorganisms in uncontaminated soils and suggests the case is the same for uncontaminated Antarctic remote soils.

摘要

土壤中多环芳烃(PAHs)的生物降解与 PAHs 的暴露史和环境条件有关。本研究评估了没有污染史的利文斯顿岛(南设得兰群岛,南极洲)土壤中土著微生物在 4、12 和 22°C 下降解(14)C-菲的能力(∑PAHs:0.14-1.47ngg(-1) dw)。该研究提供了证据证明所有研究土壤中都存在菲降解微生物。一般来说,随着温度的升高,(14)C-菲的矿化百分比增加。在 22°C 的泥浆体系中,(14)C-菲的最大矿化程度(47.93%)。这项工作支持了在未受污染的土壤中存在 PAH 降解微生物的发现,并表明在未受污染的南极偏远土壤中也是如此。

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