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Isolation and identification of methanogen-specific DNA from blanket bog peat by PCR amplification and sequence analysis.

机译:通过PCR扩增和序列分析从橡皮泥泥炭中分离和鉴定产甲烷菌特异性DNA。

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摘要

The presence of methanogenic bacteria was assessed in peat and soil cores taken from upland moors. The sampling area was largely covered by blanket bog peat together with small areas of red-brown limestone and peaty gley. A 30-cm-deep core of each soil type was taken, and DNA was extracted from 5-cm transverse sections. Purified DNA was subjected to PCR amplification with primers IAf and 1100Ar, which specifically amplify 1.1 kb of the archaeal 16S rRNA gene, and ME1 and ME2, which were designed to amplify a 0.75-kb region of the alpha-subunit gene for methyl coenzyme M reductase (MCR). Amplification with both primer pairs was obtained only with DNA extracted from the two deepest sections of the blanket bog peat core. This is consistent with the notion that anaerobiosis is required for activity and survival of the methanogen population. PCR products from both amplifications were cloned, and the resulting transformants were screened with specific oligonucleotide probes internal to the MCR or archaeal 16S rRNA PCR product. Plasmid DNA was extracted from probe-positive clones of both types and the insert was sequenced. The DNA sequences of 8 MCR clones were identical, as were those of 16 of the 17 16S rRNA clones. One clone showed marked variation from the remainder in specific regions of the sequence. From a comparison of these two different 16S rRNA sequences, an oligonucleotide was synthesized that was 100% homologous to a sequence region of the first 16 clones but had six mismatches with the variant. This probe was used to screen primary populations of PCR clones, and all of those that were probe negative were checked for the presence of inserts, which were then sequenced. By using this strategy, further novel methanogen 16S rRNA variants were identified and analyzed. The sequences recovered from the peat formed two clusters on the end of long branches within the methanogen radiation that are distinct from each other. These cannot be placed directly with sequences from any cultured taxa for which sequence information is available.
机译:评估了产自高地沼泽地的泥炭和土壤核心中产甲烷菌的存在。取样区域大部分被沼泽泥炭覆盖,还有一小部分的红棕色石灰石和灰泥岩。取每种土壤类型深30厘米的岩心,并从5厘米的横断面提取DNA。纯化的DNA用引物IAf和1100Ar进行PCR扩增,所述引物IAf和1100Ar特异性地扩增1.1 kb的古细菌16S rRNA基因,而ME1和ME2则被设计用于扩增甲基辅酶M的α-亚基基因的0.75 kb区域。还原酶(MCR)。仅从从毯子沼泽泥炭核的两个最深部分提取的DNA中获得两个引物对的扩增。这与产甲烷菌种群的活动和生存需要厌氧菌的观点是一致的。克隆来自两种扩增的PCR产物,并用MCR或古细菌16S rRNA PCR产物内部的特异性寡核苷酸探针筛选所得转化体。从两种类型的探针阳性克隆中提取质粒DNA,并对插入片段进行测序。 8个MCR克隆的DNA序列与17个16S rRNA克隆中的16个的DNA序列相同。一个克隆在序列的特定区域显示出与其余部分明显的差异。通过比较这两个不同的16S rRNA序列,合成了与前16个克隆的序列区域100%同源但与该变体具有6个错配的寡核苷酸。该探针用于筛选PCR克隆的主要种群,并检查所有探针阴性的插入片段的存在,然后对其进行测序。通过使用这种策略,进一步确定和分析了新型的产甲烷菌16S rRNA变体。从泥炭中回收的序列在产甲烷剂辐射内的长分支末端形成了两个簇,这两个簇彼此不同。这些序列不能直接与任何可获得序列信息的培养生物分类中的序列放在一起。

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