甲烷生物利用及嗜甲烷菌的工程改造

作为来源广泛、储量丰富的有机碳一气体,甲烷被认为是下一代工业生物技术中最具潜力的碳原料之一。嗜甲烷菌能够利用其体内的甲烷单加氧化酶,将甲烷作为唯一的碳源和能源进行生长和代谢,这为温室气体减排及其开发利用提供了新的策略。目前,嗜甲烷菌生物催化体系的相关研究已开展多年,随着系统生物学和合成生物学的快速发展,利用代谢工程合理改造嗜甲烷菌代谢途径以提高甲烷转化效率,已经实现了生物转化甲烷制备多种大宗化学品和生物燃料。本文详细讨论并介绍了嗜甲烷菌催化氧化甲烷的相关代谢途径、高效细胞工厂构建及部分化学品生物合成的最新研究进展,并对甲烷生物转化未来的发展方向和面临的技术挑战进行了讨论和展望。     

好氧甲烷氧化菌生态学研究进展

好氧甲烷氧化菌是一群以甲烷为碳源和能源的细菌。好氧甲烷氧化菌在自然环境中分布广泛,人类已从土壤、淡水和海洋沉积、泥炭沼泽、热泉、海水和南极环境分离到甲烷氧化菌的纯培养。好氧甲烷氧化菌可分为14个属,包括研究较为深入的隶属于变形菌门Alpha和Gamma纲的细菌,以及属于疣微菌门的极端嗜热嗜酸甲烷氧化菌。最近,好氧甲烷氧化菌还被发现存在于苔藓类植物（尤其是泥炭苔藓）共生体中,兼性营养好氧甲烷氧化菌也被发现。本文通过对好氧甲烷氧化菌的分类、生理生化特征、分子生物学检测方法以及微生物生态学中的研究成果的总结与分析,以及对甲烷氧化菌研究所面临的问题进行讨论,以期为今后进一步开展好氧甲烷氧化菌及其在碳循环中的作用研究提供参考。     

Dynamic investigation and modeling of the nitrogen cometabolism in Methylococcus capsulatus ( Bath)

The methanotrophic bacterium Methylococcus capsulatus is capable of assimilating methane and oxygen into protein-rich biomass, however, the diverse metabolism of the microorganism also allows for several undesired cometabolic side-reactions to occur. In this study, the ammonia cometabolism in Methylococcus capsulatus is investigated using pulse experiments. Surprisingly Methylococcus capsulatus oxidizes ammonia to nitrate through a yet unknown mechanism and fixes molecular nitrogen even at a high dissolved oxygen tension. The observed phenomena can be modeled using 14 ordinary differential equations and 18 kinetic parameters, of which 6 were revealed by Morris screening to be identifiable from the experimental data. Monte Carlo simulations showed that the model was robust and accurate even with uncertainty in the parameter values as confirmed by statistical error analysis.     

DNA-based analysis of planktonic methanotrophs in a stratified lake

1. The assemblage of planktonic methanotrophs in a stratified freshwater lake was investigated. Vertical patterns were analysed by denaturing gradient gel electrophoresis, using the primer pair specific for 16S rRNA genes of type I methanotrophs.
2. The resulting banding patterns could be divided into three distinct groups, and sequenced bands were all related to the Methylobacter species. No amplicon was obtained with the primer pair specific for type II methanotrophs.
3. Cloning analysis of the pmoA gene was performed using samples from three water depths (epilimnion, metalimnion and hypolimnion). The compositions of the clone libraries from the three depths were distinct from each other but all three libraries were dominated by clones related to Methylobacter species.     

Unexpected stimulation of soil methane uptake as emergent property of agricultural soils following bio‐based residue application

Intensification of agriculture to meet the global food, feed, and bioenergy demand entail increasing re‐investment of carbon compounds (residues) into agro‐systems to prevent decline of soil quality and fertility. However, agricultural intensification decreases soil methane uptake, reducing, and even causing the loss of the methane sink function. In contrast to wetland agricultural soils (rice paddies), the methanotrophic potential in well‐aerated agricultural soils have received little attention, presumably due to the anticipated low or negligible methane uptake capacity in these soils. Consequently, a detailed study verifying or refuting this assumption is still lacking. Exemplifying a typical agricultural practice, we determined the impact of bio‐based residue application on soil methane flux, and determined the methanotrophic potential, including a qualitative (diagnostic microarray) and quantitative (group‐specific qPCR assays) analysis of the methanotrophic community after residue amendments over 2 months. Unexpectedly, after amendments with specific residues, we detected a significant transient stimulation of methane uptake confirmed by both the methane flux measurements and methane oxidation assay. This stimulation was apparently a result of induced cell‐specific activity, rather than growth of the methanotroph population. Although transient, the heightened methane uptake offsets up to 16% of total gaseous CO₂ emitted during the incubation. The methanotrophic community, predominantly comprised of Methylosinus may facilitate methane oxidation in the agricultural soils. While agricultural soils are generally regarded as a net methane source or a relatively weak methane sink, our results show that methane oxidation rate can be stimulated, leading to higher soil methane uptake. Hence, even if agriculture exerts an adverse impact on soil methane uptake, implementing carefully designed management strategies (e.g. repeated application of specific residues) may compensate for the loss of the methane sink function following land‐use change.     

自然湿地土壤产甲烷菌和甲烷氧化菌多样性的分子检测

自然湿地是CH4排放的重要来源之一。产甲烷菌和甲烷氧化菌是介导自然湿地甲烷循环的重要功能菌群。开展产甲烷菌和甲烷氧化菌多样性的检测研究有助于揭示微生物介导的甲烷循环以及自然湿地甲烷排放的时空异质性。传统基于培养的检测方法已被证实无法充分描述产甲烷菌和甲烷氧化菌的多样性,而分子检测方法为自然湿地土壤产甲烷菌和甲烷氧化菌的多样性检测提供了一种更准确和科学的工具。本文综述了自然湿地土壤产甲烷菌和甲烷氧化菌的定性和定量分子检测方法,包括末端限制性片段长度多态性（T-RFLP）、变性梯度凝胶电泳（DGGE）、荧光原位杂交（FISH）和实时定量PCR（real-time qPCR）,重点分析了分子检测中两类重要的标记基因,总结了不同类型自然湿地产甲烷菌和甲烷氧化菌群落多样性的最新成果,提出了我国在该领域今后应深入研究探讨的一些问题及建议。     

Response of methanotrophic communities to afforestation and reforestation in New Zealand

Methanotrophs use methane (CH₄) as a carbon source. They are particularly active in temperate forest soils. However, the rate of change of CH₄ oxidation in soil with afforestation or reforestation is poorly understood. Here, soil CH₄ oxidation was examined in New Zealand volcanic soils under regenerating native forests following burning, and in a mature native forest. Results were compared with data for pasture to pine land-use change at nearby sites. We show that following soil disturbance, as little as 47 years may be needed for development of a stable methanotrophic community similar to that in the undisturbed native forest soil. Corresponding soil CH₄-oxidation rates in the regenerating forest soil have the potential to reach those of the mature forest, but climo-edaphic fators appear limiting. The observed changes in CH₄-oxidation rate were directly linked to a prior shift in methanotrophic communities, which suggests microbial control of the terrestrial CH₄ flux and identifies the need to account for this response to afforestation and reforestation in global prediction of CH₄ emission.     

Cloning,Purification, and Characterization of Diaminobutyrate Acetyltransferase from the Halotolerant Methanotroph <Emphasis Type="Italic">Methylomicrobium alcaliphilum</Emphasis> 20Z

L-2,4-Diaminobutyrate (DAB) acetyltransferase (DABAcT) catalyzes one of the key reactions of biosynthesis of the bacterial osmoprotectant ectoine--acetylation of L-2,4-DAB yielding Ngamma-acetyl-2,4-DAB. Gene ectA encoding DABAcT was cloned from DNA of the halotolerant methanotroph Methylomicrobium alcaliphilum 20Z and expressed in Escherichia coli with an additional six His residues at the C-terminus. Homogeneous enzyme preparation with specific activity 200 U/mg was obtained by affinity metal-chelating chromatography. DABAcT was found to be a homodimer with molecular mass 40 kD. The enzyme is most active at pH 9.5 and 20 degrees C, and its activity increased threefold in the presence of 0.1-0.2 M NaCl or 0.2 M KCl. The Km values of recombinant DABAcT measured at the optimal pH and temperature in the presence of 0.2 M KCl were 460 and 36.6 microM for L-2,4-DAB and acetyl-CoA, respectively. The enzyme is specific for L-2,4-DAB and acetyl-CoA and is also active against propionyl-CoA (20%). Zn2+ and Cd2+ at 1 mM concentration completely inhibit the recombinant enzyme; 10 mM ATP inhibits 26% of the enzyme activity, whereas EDTA, o-phenanthroline, ADP, NAD(P), and NAD(P)H do not significantly effect the enzyme activity. The possible participation of DABAcT in regulation of ectoine biosynthesis in M. alcaliphilum 20Z is discussed.     

Diversity of soluble methane monooxygenase-containing methanotrophs isolated from polluted environments

Methanotrophs were enriched and isolated from polluted environments in Canada and Germany. Enrichments in low copper media were designed to specifically encourage growth of soluble methane monooxygenase (sMMO) containing organisms. The 10 isolates were characterized physiologically and genetically with one type I and nine type II methanotrophs being identified. Three key genes: 16S rRNA; pmoA and mmoX, encoding for the particulate and soluble methane monooxygenases respectively, were cloned from the isolates and sequenced. Phylogenetic analysis of these sequences identified strains, which were closely related to Methylococcus capsulatus, Methylocystis sp., Methylosinus sporium and Methylosinus trichosporium. Diversity of sMMO-containing methanotrophs detected in this and previous studies was rather narrow, both genetically and physiologically, suggesting possible constraints on genetic diversity of sMMO due to essential conservation of enzyme function.