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维利奇卡组甲烷消耗生物群落的动态:环境与富集研究

Dynamics of Methane-Consuming Biomes from Wieliczka Formation: Environmental and Enrichment Studies.

作者信息

Goraj Weronika, Pytlak Anna, Grządziel Jarosław, Gałązka Anna, Stępniewska Zofia, Szafranek-Nakonieczna Anna

机构信息

Department of Biology and Biotechnology of Microorganisms, Faculty of Medicine, The John Paul II Catholic University of Lublin, Str. Konstantynów 1I, 20-708 Lublin, Poland.

Institute of Agrophysics, Polish Academy of Sciences, Doświadczalna 4, 20-280 Lublin, Poland.

出版信息

Biology (Basel). 2023 Nov 11;12(11):1420. doi: 10.3390/biology12111420.

Abstract

The rocks surrounding Wieliczka salt deposits are an extreme, deep subsurface ecosystem that as we studied previously harbors many microorganisms, including methanotrophs. In the presented research bacterial community structure of the Wieliczka Salt Mine was determined as well as the methanotrophic activity of the natural microbiome. Finally, an enrichment culture of methane-consuming methanotrophs was obtained. The research material used in this study consisted of rocks surrounding salt deposits in the Wieliczka Salt Mine. DNA was extracted directly from the pristine rock material, as well as from rocks incubated in an atmosphere containing methane and mineral medium, and from a methanotrophic enrichment culture from this ecosystem. As a result, the study describes the composition of the microbiome in the rocks surrounding the salt deposits, while also explaining how biodiversity changes during the enrichment culture of the methanotrophic bacterial community. The contribution of methanotrophic bacteria ranged from 2.614% in the environmental sample to 64.696% in the bacterial culture. The methanotrophic enrichment culture was predominantly composed of methanotrophs from the genera (48.848%) and (15.636%) with methane oxidation rates from 3.353 ± 0.105 to 4.200 ± 0.505 µmol CH day.

摘要

维利奇卡盐矿周围的岩石是一个极端的深层地下生态系统,正如我们之前研究所发现的,这里栖息着许多微生物,包括甲烷氧化菌。在本研究中,我们确定了维利奇卡盐矿的细菌群落结构以及天然微生物群落的甲烷氧化活性。最后,获得了一种消耗甲烷的甲烷氧化菌富集培养物。本研究使用的研究材料包括维利奇卡盐矿盐矿床周围的岩石。DNA直接从原始岩石材料中提取,也从在含有甲烷和矿物培养基的气氛中培养的岩石以及来自该生态系统的甲烷氧化菌富集培养物中提取。结果,该研究描述了盐矿床周围岩石中微生物群落的组成,同时也解释了在甲烷氧化细菌群落的富集培养过程中生物多样性是如何变化的。甲烷氧化细菌的贡献范围从环境样品中的2.614%到细菌培养物中的64.696%。甲烷氧化富集培养物主要由来自属(48.848%)和属(15.636%)的甲烷氧化菌组成,甲烷氧化速率为3.353±0.105至4.200±0.505 μmol CH 天。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f55b/10669130/e62bee9b7f6c/biology-12-01420-g001.jpg

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