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Identification of Novel Methane- Ethane- and Propane-Oxidizing Bacteria at Marine Hydrocarbon Seeps by Stable Isotope Probing

机译:稳定同位素探测在海洋油气渗漏中鉴定新型甲烷乙烷和丙烷氧化细菌

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摘要

Marine hydrocarbon seeps supply oil and gas to microorganisms in sediments and overlying water. We used stable isotope probing (SIP) to identify aerobic bacteria oxidizing gaseous hydrocarbons in surface sediment from the Coal Oil Point seep field located offshore of Santa Barbara, California. After incubating sediment with 13C-labeled methane, ethane, or propane, we confirmed the incorporation of 13C into fatty acids and DNA. Terminal restriction fragment length polymorphism (T-RFLP) analysis and sequencing of the 16S rRNA and particulate methane monooxygenase (pmoA) genes in 13C-DNA revealed groups of microbes not previously thought to contribute to methane, ethane, or propane oxidation. First, 13C methane was primarily assimilated by Gammaproteobacteria species from the family Methylococcaceae, Gammaproteobacteria related to Methylophaga, and Betaproteobacteria from the family Methylophilaceae. Species of the latter two genera have not been previously shown to oxidize methane and may have been cross-feeding on methanol, but species of both genera were heavily labeled after just 3 days. pmoA sequences were affiliated with species of Methylococcaceae, but most were not closely related to cultured methanotrophs. Second, 13C ethane was consumed by members of a novel group of Methylococcaceae. Growth with ethane as the major carbon source has not previously been observed in members of the Methylococcaceae; a highly divergent pmoA-like gene detected in the 13C-labeled DNA may encode an ethane monooxygenase. Third, 13C propane was consumed by members of a group of unclassified Gammaproteobacteria species not previously linked to propane oxidation. This study identifies several bacterial lineages as participants in the oxidation of gaseous hydrocarbons in marine seeps and supports the idea of an alternate function for some pmoA-like genes.
机译:海洋碳氢化合物的渗漏为沉积物和上覆水中的微生物提供了石油和天然气。我们使用稳定同位素探测(SIP)来识别需氧细菌,该细菌将位于加利福尼亚州圣塔芭芭拉(Santa Barbara)海上的Coal Oil Point渗漏场中地表沉积物中的气态烃氧化。用 13 C标记的甲烷,乙烷或丙烷孵育沉淀物后,我们证实了 13 C掺入脂肪酸和DNA中。 13 C-DNA中16S rRNA和颗粒甲烷单加氧酶(pmoA)基因的末端限制性片段长度多态性(T-RFLP)分析和测序揭示了以前不认为与甲烷,乙烷有关的微生物群,或丙烷氧化。首先, 13 C甲烷主要被甲基球菌科的丙种细菌,与甲基噬菌体有关的丙种细菌和嗜甲基菌科的Beta细菌同化。后两个属的物种以前没有显示过氧化甲烷的作用,并且可能已经在甲醇上交叉进料,但是两个属的物种在短短3天后就被严重标记。 pmoA序列与甲基球菌科物种有关,但大多数与培养的甲烷营养菌没有密切关系。第二, 13 乙烷被一组新的甲基球菌科成员消耗。以前从未在甲基球菌科成员中观察到以乙烷为主要碳源的生长。在 13 C标记的DNA中检测到的高度不同的pmoA样基因可能编码乙烷单加氧酶。第三, 13 C丙烷被先前未与丙烷氧化相关的一组未分类的γ-变形细菌的成员消耗。这项研究确定了几种细菌谱系参与了海洋渗透物中气态碳氢化合物的氧化,并支持了某些pmoA样基因的替代功能。

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