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活性甲基营养菌群落分析:当DNA稳定同位素示踪技术与高通量技术相遇时

Analysis of Active Methylotrophic Communities: When DNA-SIP Meets High-Throughput Technologies.

作者信息

Taubert Martin, Grob Carolina, Howat Alexandra M, Burns Oliver J, Chen Yin, Neufeld Josh D, Murrell J Colin

机构信息

School of Environmental Sciences, University of East Anglia, Norwich Research Park, Norwich, NR4 7TJ, UK.

Institute for Ecology, Friedrich Schiller University Jena, Dornburger Strasse 159, 07743, Jena, Germany.

出版信息

Methods Mol Biol. 2016;1399:235-55. doi: 10.1007/978-1-4939-3369-3_14.

Abstract

Methylotrophs are microorganisms ubiquitous in the environment that can metabolize one-carbon (C1) compounds as carbon and/or energy sources. The activity of these prokaryotes impacts biogeochemical cycles within their respective habitats and can determine whether these habitats act as sources or sinks of C1 compounds. Due to the high importance of C1 compounds, not only in biogeochemical cycles, but also for climatic processes, it is vital to understand the contributions of these microorganisms to carbon cycling in different environments. One of the most challenging questions when investigating methylotrophs, but also in environmental microbiology in general, is which species contribute to the environmental processes of interest, or "who does what, where and when?" Metabolic labeling with C1 compounds substituted with (13)C, a technique called stable isotope probing, is a key method to trace carbon fluxes within methylotrophic communities. The incorporation of (13)C into the biomass of active methylotrophs leads to an increase in the molecular mass of their biomolecules. For DNA-based stable isotope probing (DNA-SIP), labeled and unlabeled DNA is separated by isopycnic ultracentrifugation. The ability to specifically analyze DNA of active methylotrophs from a complex background community by high-throughput sequencing techniques, i.e. targeted metagenomics, is the hallmark strength of DNA-SIP for elucidating ecosystem functioning, and a protocol is detailed in this chapter.

摘要

甲基营养菌是环境中普遍存在的微生物,它们能够将一碳(C1)化合物作为碳源和/或能源进行代谢。这些原核生物的活性会影响其各自栖息地内的生物地球化学循环,并能决定这些栖息地是C1化合物的源还是汇。由于C1化合物不仅在生物地球化学循环中,而且在气候过程中都非常重要,因此了解这些微生物对不同环境中碳循环的贡献至关重要。在研究甲基营养菌时,以及在一般环境微生物学中,最具挑战性的问题之一是哪些物种对感兴趣的环境过程有贡献,或者说“谁在何时何地做了什么?”。用(13)C取代的C1化合物进行代谢标记,即一种称为稳定同位素探测的技术,是追踪甲基营养群落内碳通量的关键方法。(13)C掺入活性甲基营养菌的生物量中会导致其生物分子分子量增加。对于基于DNA的稳定同位素探测(DNA-SIP),标记和未标记的DNA通过等密度超速离心分离。通过高通量测序技术,即靶向宏基因组学,从复杂的背景群落中特异性分析活性甲基营养菌的DNA的能力,是DNA-SIP阐明生态系统功能的标志性优势,本章将详细介绍相关方案。

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