State Key Laboratory of Bioreactor Engineering, Institute of Applied Chemistry, East China University of Science and Technology, Shanghai, People's Republic of China.
Ecotoxicology. 2012 Aug;21(6):1680-91. doi: 10.1007/s10646-012-0949-5. Epub 2012 Jun 12.
Despite the knowledge on anaerobic degradation of hydrocarbons and signature metabolites in the oil reservoirs, little is known about the functioning microbes and the related biochemical pathways involved, especially about the methanogenic communities. In the present study, a methanogenic consortium enriched from high-temperature oil reservoir production water and incubated at 55 °C with a mixture of long chain n-alkanes (C(15)-C(20)) as the sole carbon and energy sources was characterized. Biodegradation of n-alkanes was observed as methane production in the alkanes-amended methanogenic enrichment reached 141.47 μmol above the controls after 749 days of incubation, corresponding to 17 % of the theoretical total. GC-MS analysis confirmed the presence of putative downstream metabolites probably from the anaerobic biodegradation of n-alkanes and indicating an incomplete conversion of the n-alkanes to methane. Enrichment cultures taken at different incubation times were subjected to microbial community analysis. Both 16S rRNA gene clone libraries and DGGE profiles showed that alkanes-degrading community was dynamic during incubation. The dominant bacterial species in the enrichment cultures were affiliated with Firmicutes members clustering with thermophilic syntrophic bacteria of the genera Moorella sp. and Gelria sp. Other represented within the bacterial community were members of the Leptospiraceae, Thermodesulfobiaceae, Thermotogaceae, Chloroflexi, Bacteroidetes and Candidate Division OP1. The archaeal community was predominantly represented by members of the phyla Crenarchaeota and Euryarchaeota. Corresponding sequences within the Euryarchaeota were associated with methanogens clustering with orders Methanomicrobiales, Methanosarcinales and Methanobacteriales. On the other hand, PCR amplification for detection of functional genes encoding the alkylsuccinate synthase α-subunit (assA) was positive in the enrichment cultures. Moreover, the appearance of a new assA gene sequence identified in day 749 supported the establishment of a functioning microbial species in the enrichment. Our results indicate that n-alkanes are converted to methane slowly by a microbial community enriched from oilfield production water and fumarate addition is most likely the initial activation step of n-alkanes degradation under thermophilic methanogenic conditions.
尽管人们已经了解了油藏中烃类物质和特征代谢物的厌氧降解过程,但对于相关功能微生物及其生化途径知之甚少,尤其是产甲烷微生物群落。本研究从高温油藏采出水的产甲烷菌富集物中分离得到了一种产甲烷菌混合菌群,该菌群在 55°C 下以长链正构烷烃(C(15)-C(20))作为唯一的碳源和能源进行培养。实验结果表明,在 749 天的培养时间内,添加正构烷烃的产甲烷菌富集物中的甲烷生成量比对照组高出 141.47 μmol,占理论总产量的 17%。GC-MS 分析证实了可能来自于正构烷烃的厌氧生物降解的下游代谢产物的存在,并表明正构烷烃向甲烷的转化并不完全。在不同的培养时间取样的富集培养物用于微生物群落分析。16S rRNA 基因克隆文库和 DGGE 图谱均表明,在培养过程中,烷烃降解群落是动态的。富集培养物中的优势细菌种属属于厚壁菌门(Firmicutes),与 Moorella sp. 和 Gelria sp. 等嗜热共营养菌密切相关。细菌群落中还包括螺旋体科(Leptospiraceae)、硫还原菌科(Thermodesulfobiaceae)、热球菌科(Thermotogaceae)、绿弯菌门(Chloroflexi)、拟杆菌门(Bacteroidetes)和候选门 OP1。古菌群落主要由泉古菌门(Crenarchaeota)和广古菌门(Euryarchaeota)的成员组成。广古菌门中对应的序列与甲烷微菌目(Methanomicrobiales)、甲烷杆菌目(Methanosarcinales)和甲烷杆菌目(Methanobacteriales)中的产甲烷菌聚类。另一方面,在富集培养物中,检测编码烷基琥珀酸合酶α亚基(assA)的功能基因的 PCR 扩增呈阳性。此外,在第 749 天出现的一个新的 assA 基因序列表明,在富集物中建立了一个功能微生物物种。本研究结果表明,从油田采出水富集的微生物群落可缓慢地将正构烷烃转化为甲烷,富马酸盐的添加很可能是在嗜热产甲烷条件下正构烷烃降解的初始激活步骤。