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来自淡水湖沉积物的甲烷营养菌分离株的分子特征分析

Molecular characterization of methanotrophic isolates from freshwater lake sediment.

作者信息

Auman A J, Stolyar S, Costello A M, Lidstrom M E

机构信息

Departments of Microbiology, University of Washington, Seattle, Washington 98195, USA.

出版信息

Appl Environ Microbiol. 2000 Dec;66(12):5259-66. doi: 10.1128/AEM.66.12.5259-5266.2000.

DOI:10.1128/AEM.66.12.5259-5266.2000
PMID:11097900
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC92454/
Abstract

Profiles of dissolved O(2) and methane with increasing depth were generated for Lake Washington sediment, which suggested the zone of methane oxidation is limited to the top 0.8 cm of the sediment. Methane oxidation potentials were measured for 0.5-cm layers down to 1.5 cm and found to be relatively constant at 270 to 350 micromol/liter of sediment/h. Approximately 65% of the methane was oxidized to cell material or metabolites, a signature suggestive of type I methanotrophs. Eleven methanotroph strains were isolated from the lake sediment and analyzed. Five of these strains classed as type I, while six were classed as type II strains by 16S rRNA gene sequence analysis. Southern hybridization analysis with oligonucleotide probes detected, on average, one to two copies of pmoA and one to three copies of 16S rRNA genes. Only one restriction length polymorphism pattern was shown for pmoA genes in each isolate, and in cases where, sequencing was done, the pmoA copies were found to be almost identical. PCR primers were developed for mmoX which amplified 1.2-kb regions from all six strains that tested positive for cytoplasmic soluble methane mono-oxygenase (sMMO) activity. Phylogenetic analysis of the translated PCR products with published mmoX sequences showed that MmoX falls into two distinct clusters, one containing the orthologs from type I strains and another containing the orthologs from type II strains. The presence of sMMO-containing Methylomonas strains in a pristine freshwater lake environment suggests that these methanotrophs are more widespread than has been previously thought.

摘要

针对华盛顿湖沉积物生成了溶解氧和甲烷随深度增加的分布图,这表明甲烷氧化带仅限于沉积物顶部0.8厘米处。对沉积物中向下至1.5厘米的0.5厘米层进行了甲烷氧化电位测量,发现其相对恒定,为270至350微摩尔/升沉积物/小时。大约65%的甲烷被氧化为细胞物质或代谢产物,这是I型甲烷氧化菌的特征。从湖泊沉积物中分离并分析了11株甲烷氧化菌菌株。通过16S rRNA基因序列分析,其中5株菌株被归类为I型,而6株被归类为II型菌株。用寡核苷酸探针进行的Southern杂交分析平均检测到一到两个pmoA拷贝和一到三个16S rRNA基因拷贝。每个分离物中pmoA基因仅显示一种限制性长度多态性模式,在进行测序的情况下,发现pmoA拷贝几乎相同。开发了用于mmoX的PCR引物,该引物从所有6株对细胞质可溶性甲烷单加氧酶(sMMO)活性检测呈阳性的菌株中扩增出1.2 kb区域。将翻译后的PCR产物与已发表的mmoX序列进行系统发育分析,结果表明MmoX分为两个不同的簇,一个包含来自I型菌株的直系同源物,另一个包含来自II型菌株的直系同源物。在原始淡水湖环境中存在含sMMO的甲基单胞菌菌株,这表明这些甲烷氧化菌比以前认为的分布更广泛。