Key Laboratory of Marine Biogenetic Resources, The Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, Fujian, China.
Environ Microbiol. 2008 Aug;10(8):2138-49. doi: 10.1111/j.1462-2920.2008.01637.x. Epub 2008 Apr 25.
The bacteria involved in the biodegradation of polycyclic aromatic hydrocarbons (PAHs) in deep sea subsurface environments are largely unknown. In order to reveal their biodiversity, sediments from 2.2 m under the bottom surface at a water depth of 3542 m were sampled on the Middle Atlantic Ridge with a gravity column sampler. The sediments were promptly enriched with either crude oil or a mixture of PAHs (naphthalene, phenanthrene and pyrene) as the sole carbon source, and further enriched with the PAH mixture mentioned above in the lab. The resulting consortia were named C2CO and C2PPN respectively. Their bacterial composition was analysed with plate cultivation, PCR-DGGE and 16S rDNA library analysis. On plates, isolates belonging to Pseudoalteromonas, Halomonas, Marinobacter, Thalassospira and Tistrella dominated the culturable populations. With PCR-DGGE, five major bands closely related to Cycloclasticus, Alteromonas, Thalassospira, Alcanivorax and Rhodospirillaceae were detected in consortium C2CO, while only one major band of Cycloclasticus was detected in consortium C2PPN. In addition, the dynamics of community structure in response to aromatic substrate alterations were examined. As a result, three ribotypes of Cycloclasticus were detected by 16S rDNA library analysis, one which played a key role in phenanthrene degradation; two Alteromonas bacteria dominated the naphthalene reselected consortium. Although bacteria of the two genera grew as the main members of the communities, none of them were isolated, probably owing to their poor cultivability. These results confirm that bacteria of Cycloclasticus are important obligate PAH degraders in marine environments, and coexist with other degrading bacteria that inhabit the deep subsurface sediment of the Atlantic. This supports the view that PAH accumulation and bioattenuation occur in remote areas consistently and continuously.
在深海海底环境中参与多环芳烃(PAHs)生物降解的细菌在很大程度上是未知的。为了揭示它们的生物多样性,在中大西洋脊上,使用重力柱状采样器从水深 3542 米的海底表面以下 2.2 米处采集了沉积物。这些沉积物立即用原油或 PAH(萘、菲和芘)混合物作为唯一的碳源进行了富集,并在实验室中进一步用上述 PAH 混合物进行了富集。由此产生的联合体分别命名为 C2CO 和 C2PPN。使用平板培养、PCR-DGGE 和 16S rDNA 文库分析对它们的细菌组成进行了分析。在平板上,属于假交替单胞菌、盐单胞菌、海洋杆菌、海洋螺旋菌和 Tistrella 的分离物主导着可培养种群。通过 PCR-DGGE,在 C2CO 联合体中检测到与环糊精单胞菌、交替单胞菌、海洋螺旋菌、Alcanivorax 和红螺菌科密切相关的五个主要条带,而在 C2PPN 联合体中仅检测到一个主要的环糊精条带。此外,还研究了群落结构对芳香基质变化的响应动力学。结果,通过 16S rDNA 文库分析检测到三个环糊精单胞菌的核糖体类型,其中一个在菲降解中起关键作用;两个交替单胞菌主导着萘再选择联合体。虽然这两个属的细菌作为群落的主要成员生长,但它们都没有被分离出来,可能是因为它们的可培养性差。这些结果证实,环糊精细菌是海洋环境中重要的多环芳烃降解菌,与栖息在大西洋深海海底沉积物中的其他降解菌共存。这支持了在偏远地区持续不断地发生 PAH 积累和生物衰减的观点。