Methylotrophic Methanogenesis Governs the Biogenic Coal Bed Methane Formation in Eastern Ordos Basin, China
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Appl Microbiol Biotechnol (2012) 96:1587–1597 DOI 10.1007/s00253-012-3889-3 ENVIRONMENTAL BIOTECHNOLOGY Methylotrophic methanogenesis governs the biogenic coal bed methane formation in Eastern Ordos Basin, China Hongguang Guo & Zhisheng Yu & Ruyin Liu & Hongxun Zhang & Qiding Zhong & Zhenghe Xiong Received: 23 October 2011 /Revised: 29 December 2011 /Accepted: 2 January 2012 /Published online: 28 January 2012 # Springer-Verlag 2012 Abstract To identify the methanogenic pathways present in a biodegradation of coal by methylotrophic methanogens and deep coal bed methane (CBM) reservoir associated with East- syntrophic bacteria, as well as thermogenic CBM production, ern Ordos Basin in China, a series of geochemical and micro- contributed to the Liulin CBM reserves associated with the biological studies was performed using gas and water samples Eastern Ordos Basin. produced from the Liulin CBM reservoir. The composition and stable isotopic ratios of CBM implied a mixed biogenic Keywords Coal bed methane . Methanogenesis . Deep and thermogenic origin of the methane. Archaeal 16S rRNA subsurface environment . Ordos Basin gene analysis revealed the dominance of the methylotrophic methanogen Methanolobus in the water produced. The high potential of methane production by methylotrophic methano- Introduction gens was found in the enrichments using the water samples amended with methanol and incubated at 25 and 35 °C. Coal bed methane (CBM) is a major clean energy resource Methylotrophic methanogens were the dominant archaea in worldwide and which is being intensively developed in many both enrichments as shown by polymerase chain reaction countries. CBM is generally understood to be formed by (PCR)–denaturing gradient gel electrophoresis (DGGE). Bac- microbial degradation of coal (biogenic origin) or thermal terial 16S rRNA gene analysis revealed that fermentative, decomposition of coal (thermogenic origin), which is typically sulfate-reducing, and nitrate-reducing bacteria inhabiting the analyzed by such standard geochemical technologies as plot- water produced were a factor in coal biodegradation to fuel ting hydrocarbon gas composition C1/(C2+C3)(C1–C3,meth- methanogens. These results suggested that past and ongoing ane, ethane, propane) versus stable carbon isotope ratios of 13 methane δ C–CH4 (Bernard et al. 1978). Biogenic CBM has been reported to be present in various reservoirs with mixed H. Guo : Z. Yu (*) : R. Liu : H. Zhang College of Resources and Environment, biogenic and thermogenic CBM or predominantly biogenic Graduate University of Chinese Academy of Sciences, CBM, e.g., in the San Juan Basin (Scott et al. 1994), in the 19 A Yuquan Road, Illinois Basin (Strapoć et al. 2007), and in the Powder River ’ Beijing 100049, People s Republic of China Basin (Flores et al. 2008). It is generally accepted that bio- e-mail: [email protected] genic CBM is the end product of coal biodegradation by H. Zhang methanogenic archaea and syntrophic bacteria inhabiting coal Research Center for Eco-Environmental Sciences, beds. These microorganisms are essential for artificially stim- Chinese Academy of Sciences, ulating the regeneration of biogenic CBM (Green et al. 2008; 18 Shuangqing Road, Beijing 100085, People’s Republic of China Harris et al. 2008; Pfeiffer et al. 2010). Thus, it is essential : to explore the existence of biogenic CBM to more fully Q. Zhong Z. Xiong understand the microorganisms involved in the formation of Food Analysis using Isotope Technology Lab, China National biogenic CBM. Research Institute of Food and Fermentation Industries, 32 Xiaoyun Road, Some systemic studies have evaluated the microbial com- Beijing 100027, People’s Republic of China munities inhabiting the CBM reservoirs containing biogenic 1588 Appl Microbiol Biotechnol (2012) 96:1587–1597 CBM. Sampling gas and water produced in the Illinois The Ordos Basin, situated in central China within the Basin, Strapoć et al. (2007, 2008) demonstrated the predom- Yellow River drainage basin (Fig. 1), is one of the largest inance of biogenic CBM formed via hydrogentrophic meth- CBM reservoirs and a principal target area for CBM explo- anogenesis by a population of Methanocorpusculum using ration and development in China. However, there is limited geochemical and microbiological methods. It was found that understanding on the origin of CBM and of the microbial methanogens were also present in water produced from communities related to CBM in the Ordos Basin. In this other reservoirs, e.g., the Powder River Basin (Green et al. study, we sought preliminary identification of the origin of 2008), the Gippsland Basin (Midgley et al. 2010), and CBM using the chemical and stable isotopic signatures of the Alberta Basin (Penner et al. 2010). Furthermore, CBM. Culture-independent and culture-dependent methods enrichment studies demonstrated that native methanogens were also used to explore the pathway of biogenic CBM indicated the production of methane by supplementing formation in a deep CBM reservoir associated with the water samples with nutrients and substrates for methano- Ordos Basin. gens (Green et al. 2008; Midgley et al. 2010). It has been reported that acetotrophic and hydrogenotrophic methanogen- eses were the dominant pathways for the production of meth- Materials and methods ane in CBM reservoirs (Strapoć et al. 2011). However, as one of the pathways for producing methane by methanogens, Study site and sample collection methylotrophic methanogenesis was rarely reported in CBM formation (Shimizu et al. 2007;Strapoć et al. Water and gas samples were collected from deep wells in the 2010). Liulin District which is located in the middle part of the Fig. 1 Location of the Liulin District in China. The map is modified from Ding et al. (2011) Appl Microbiol Biotechnol (2012) 96:1587–1597 1589 Eastern Ordos Basin (Fig. 1). It is the first experimental base The PCR products of the archaeal and bacterial 16S of CBM exploration and development in China (Su et al. rRNA genes were cloned and transformed into competent 2003). The wells were drilled down to about 700 m below Escherichia coli DH5α cells using pGEM-T Easy Vector the ground surface and constructed with tight steel pipes. (Promega Corporation, Madison, WI, USA). Recombinant Water samples were collected from five CBM-producing pGEM-T Easy vectors were checked for 16S rRNA ampli- wells (SXLL-2, SXLL-3, SXLL-4, SXLL-6, and SXLL-9). con inserts by PCR using M13 primers. For the archaeal To prevent contamination by air and steel pipes, the water library, the right-inserted recombinant clones were se- produced was continuously pumped for more than 5 days quenced. For the bacterial library, the correct clones were before sampling. Water samples were collected into au- analyzed by amplified ribosomal DNA restriction analysis toclaved glass bottles, carefully maintaining air in the (ARDRA) using restriction enzyme Msp I (NEB) as de- headspaces clean. Bottles were then tightly sealed and scribed by Steven et al. (2007). For each restriction fragment immediately transported on ice to the laboratory. The gas length polymorphism (RFLP) type, one representative clone samples from four CBM-producing wells (SXLL-2, SXLL-3, was chosen at random and sequenced. SXLL-6, and SXLL-9) were collected at the well sites through water displacement into inverted bottles. The bottles were Sequencing and phylogenetic analyses tightly sealed with butyl rubber stoppers underwater to prevent air contamination. The sequences of inserted PCR products selected from recombinant colonies were determined on an Applied Bio- Physical and chemical analysis systems 3730xl (Applied Biosytems, Darmstadt, Germany) using M13 primers. The operational taxonomic units Cations were determined by utilizing an inductively coupled (OTUs) for the archaeal clone library were determined using plasma optical emission spectrometer (Spectro Analytical Mothur software (Schloss et al. 2009). A 3% distance level Instruments, Kleve, Germany). Anions were determined by between sequences was used as the cutoff to define distinct ion chromatography (Metrohm Ltd, Herisau, Switzerland), ex- OTUs. Sequences for each archaeal OTU and bacterial + cept that NH4 was analyzed by utilizing a colorimetrical RFLP type were then compared with NCBI nucleotide se- method. Concentrations of H2,O2,CO2,N2,CH4,C2H6,and quence database using NCBI BLAST (http://www.ncbi.nlm. C3H8 in the gas samples were determined using the Agilent nih.gov/BLAST/). Sequences were aligned by Clustal X 3000A Micro gas chromatograph (GC) (Agilent Technologies). (Thompson et al. 1997). A phylogenetic tree was con- 13 13 The stable isotopic ratios of the C(δ C) of the CH4 structed in the MEGA 4 software using the neighbor- and CO2 in the gas samples were measured by an online joining method and bootstrap resampling analysis for CH4 extraction system, Trace GC Ultra™ (Thermo Electron 1,000 repeats (Tamura et al. 2007). Corporation, Austin, TX, USA), a combustion furnace (ce- ramic tube packed with CuO, NiO, and Pt wires), and Real-time PCR analysis ThermoQuest DeltaplusXL isotope ratio mass spectrometer (Thermo Finnigan). The δ13C derived was determined with The 16S rRNA genes from Methanolobus species and Clos- reference to Vienna PeeDee Belemnite samples. The preci- tridium species were respectively amplified using primer sets sion of the determination was ±0.1‰. AR-8F and AR-958R (DeLong 1992) and BAC-27F and BAC-1492R (Lane 1991) to construct the plasmids to be used Archaeal and bacterial 16S rRNA gene analysis