CO2浓度增加对长白山森林土壤甲烷氧化影响

大气CO2浓度升高可能对森林土壤的甲烷(CH4)氧化速率产生影响.本文采用开顶箱技术,对连续6年高浓度CO2(500 μmol·mol-1)处理的长白山森林典型树种蒙古栎树下土壤CH4氧化速率进行研究,并利用CH4氧化菌的16S rRNA特异性引物以及CH4单加氧酶功能基因引物分析了土壤中CH4氧化菌的群落结构与数量.结果表明:CO2浓度增高后,生长季土壤甲烷氧化量与对照和裸地相比分别降低了4％和22％;基于16S rRNA特异性引物的DGGE分析表明,CO2浓度增高导致两类甲烷氧化菌的多样性指数降低;CO2浓度增高对土壤中Ⅰ类甲烷氧化菌数量无显著影响,而使土壤中Ⅱ类甲烷氧化菌数量显著减少,功能基因pmoA拷贝数与对照和裸地相比分别降低了15％和46％.CO2浓度增高导致森林土壤甲烷氧化菌数量与活性降低,土壤含水量的增加可能是导致这一现象的主要原因.     

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。     

低氧生境中好氧甲烷氧化菌的缺氧耐受机理及种群结构研究进展

甲烷生物氧化在全球大气甲烷平衡和温室气体的控制中起着重要作用.氧气是甲烷生物氧化过程中的重要影响因素之一.生境中氧浓度不仅影响好氧甲烷氧化菌的种群结构、活性及甲烷碳的分配,而且好氧甲烷氧化菌在不同氧浓度下具有不同的代谢途径.理解低氧生境中好氧甲烷氧化菌的缺氧耐受机理和甲烷生物氧化过程,对甲烷驱动型生态系统的碳循环和生物多样性有着重要意义.本文以好氧甲烷氧化菌为对象,综述了低氧生境中好氧甲烷氧化菌的活性及其种群结构、好氧甲烷氧化菌的缺氧耐受机理以及低氧生境中甲烷氧化菌与非甲烷氧化菌的关系,并对今后的研究方向进行了展望.     

Aerobic methanotrophs from the coastal thermal springs of Lake Baikal

The number, activity, and diversity of aerobic methanotrophic bacteria in the sediments of three coastal thermal springs of Lake Baikal were analyzed. The average number of methanotrophs was 10³–10⁴ cells per 1 cm³ of sediment. The highest number of methanotrophs (10⁸ cells/cm³ of silt) and the highest potential rate of methane uptake [7.7 nmol CH₄/(cm³ day)] were revealed in sediments from the Sukhaya thermal spring. The methods of molecular ecology (DGGE, FISH, analysis of pmoA gene fragments) showed the predominance in most enrichment cultures of methanotrophs of type II, i.e., of the genera Methylocystis and Methylosinus. In only one enrichment culture (from the Sukhaya thermal spring), a type I methanotroph was revealed; its similarity to Methylococcus capsulatus Bath did not exceed 80%. These results demonstrate a widespread occurrence and high activity of the aerobic methanotrophic community in the coastal thermal springs of Lake Baikal.     

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.     

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.     

甲烷氧化菌20Z利用Embden-Meyerhof-Parnas途径高效同化甲烷

为了探究γ-变形菌纲 (Gammaproteobacteria) 甲烷氧化菌Methylomicrobium alcaliphilum 20Z的甲烷同化代谢过程。文中整合RNA-seq、LC-MS技术并结合13C标记策略对核酮糖单磷酸途径 (Ribulose monophosphate pathway) 及下游途径展开系统组学分析。M. alcaliphilum 20Z代谢物组定量分析表明Entner-Doudoroff (EDD) 途径的中间代谢物6-磷酸葡萄糖的浓度是(150.95±28.75) μmol/L,2-酮-3-脱氧-6-磷酸葡糖酸浓度低于质谱定量分析检测限,而Embden-Meyerhof-Parnas (EMP) 途径中果糖1,6-二磷酸、甘油醛-3-磷酸/二羟丙酮磷酸和磷酸烯醇式丙酮酸的浓度分别是 (1 142.02±302.88) μmol/L、(1 866.76±388.55) μmol/L和 (3 067.57±898.13) μmol/L。通过EDD和EMP途径的代谢物13C同位素动态富集研究,进一步揭示3位标记丙酮酸丰度是1位标记丙酮酸丰度的4~6倍。最后,基因表达比较分析发现EMP途径的关键基因 (如：fbaA、tpiA、gap和pykA) 的表达水平 (RPKM) 分别是2 479.2、2 493.9、2 274.6和1 846.0,而EDD途径中基因 (如：pgi、eda和edd) 的RPKM仅是263.8、341.2和225.4。综合上述结果阐明EMP途径才是M. alcaliphilum 20Z进行甲烷同化的关键通路。EMP途径代谢功能的全新阐述不但改变对Gammaproteobacteria甲烷氧化菌甲烷同化模式的传统认知,而且为甲烷高效生物催化转化提供重要的理论基础。     

Diversity and activity of methanotrophs in alkaline soil from a Chinese coal mine

Culture-independent molecular biological techniques, including 16S rRNA gene and functional gene clone libraries and microarray analyses using pmoA (encoding a key subunit of particulate methane monooxygenase), were applied to investigate the methanotroph community structure in alkaline soil from a Chinese coal mine. This environment contained a high diversity of methanotrophs, including the type II methanotrophs Methylosinus / Methylocystis , type I methanotrophs related to Methylobacter / Methylosoma and Methylococcus , and a number of as yet uncultivated methanotrophs. In order to identify the metabolically active methane-oxidizing bacteria from this alkaline environment, DNA stable isotope probing (DNA-SIP) experiments using ¹³CH₄ were carried out. This showed that both type I and type II methanotrophs were active, together with methanotrophs related to Methylocella , which had previously been found only in acidic environments. Methylotrophs, including Methylopila and Hyphomicrobium , were also detected in soil DNA and after DNA-SIP experiments. DNA sequence information on the most abundant, active methanotrophs in this alkaline soil will facilitate the design of oligonucleotide probes to monitor enrichment cultures when isolating key alkaliphilic methanotrophs from such environments.