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马尔马拉海高污染缺氧海洋沉积物中细菌和古菌群落的生物地理分布及多样性

Biogeographical distribution and diversity of bacterial and archaeal communities within highly polluted anoxic marine sediments from the Marmara Sea.

作者信息

Cetecioğlu Zeynep, Ince Bahar Kasapgil, Kolukirik Mustafa, Ince Orhan

机构信息

Istanbul Technical University, Department of Environmental Engineering, 34469 Istanbul, Turkey.

出版信息

Mar Pollut Bull. 2009 Aug;58(3):384-95. doi: 10.1016/j.marpolbul.2008.10.009. Epub 2008 Dec 4.

Abstract

Physicochemical and microbiological characterization of anoxic sediments taken from seven highly polluted sites of the Marmara Sea was carried out. The 16S rRNA based microbial community structure analyses were performed using domain-specific PCR followed by denaturant gradient gel electrophoresis (DGGE) and sequencing of characteristic bands. The results showed that the microbial communities in these sediments were diverse and evenly distributed. Relating the prokaryotic and geochemical variables through statistical tools revealed that the microbial diversity in the sediments significantly related to depth, and S, Mn and Fe content of the sediments. Fermentative bacteria, denitrifying bacteria and hydrogenotrophic methanogens were dominant whereas sulfate reducing bacteria were absent in the DGGE patterns. This unusual microbial community structure implied that the newly discovered anaerobic methane oxidation coupled to denitrification process may occur in these subseafloor environments.

摘要

对取自马尔马拉海七个高度污染地点的缺氧沉积物进行了物理化学和微生物特征分析。基于16S rRNA的微生物群落结构分析采用域特异性PCR,随后进行变性梯度凝胶电泳(DGGE)和特征条带测序。结果表明,这些沉积物中的微生物群落多样且分布均匀。通过统计工具将原核生物和地球化学变量联系起来,结果显示沉积物中的微生物多样性与深度以及沉积物中的硫、锰和铁含量显著相关。发酵细菌、反硝化细菌和氢营养型产甲烷菌占主导地位,而DGGE图谱中不存在硫酸盐还原细菌。这种不寻常的微生物群落结构表明,新发现的与反硝化过程耦合的厌氧甲烷氧化可能发生在这些海底环境中。

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