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First isolation of a type II methanotroph from a soda lake

机译:首次从苏打湖中分离出II型甲烷营养菌

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摘要

Soda lakes are alkaline environments, often with high mineralization. In microbial communities of alkaline and saline reservoirs, members of the genera Methylomicrobium and Methylobacter, type I methanotrophs using the most efficient ribulose monophosphate (RMF) pathway for assimilation of e 1 compounds, are the major aerobic methanotrophs [1]. This is probably the result of selective pressure of high alkalinity and salinity, which require additional expenditure of energy to maintain ionic homeostasis. Moreover, in the course of enrichment and isolation of pure cultures, enhanced content of mineral salts favored the most adapted forms. Since no type II methanotrophs have been isolated by approaches that considered in situ conditions and the physiological differences between two main methanotrophic groups, their existence in soda lakes seemed doubtful. However, recent molecular biological studies of soda lakes of Mongolia, Southeastern Transbaikalia, and the United States suggested the presence of type II methanotrophs (with the serine pathway of carbon assimilation) [2–4]. The goal of the present work was therefore isolation and primary characterization of a morphotype II methanotroph from a Southeastern Transbaikalia soda lake.
机译:苏打湖是碱性环境,通常具有高矿化度。在碱性和盐水库的微生物群落中,主要的需氧甲烷氧化菌是甲基化微生物和甲基细菌属的成员,它们是利用最有效的核糖单磷酸(RMF)途径同化e 1化合物的I型甲烷氧化菌。这可能是高碱度和盐度选择性压力的结果,这需要额外的能量消耗才能维持离子稳态。此外,在纯培养物的富集和分离过程中,矿盐含量的增加有利于最适合的形式。由于尚未通过考虑原位条件和两个主要甲烷营养族之间的生理差异的方法分离出II型甲烷营养菌,因此它们在苏打湖中的存在似乎令人怀疑。但是,最近对蒙古,东南贝加卡利亚东南部和美国的苏打湖进行的分子生物学研究表明,存在II型甲烷营养生物(具有碳同化的丝氨酸途径)[2-4]。因此,本工作的目的是从东南部的Transbaikalia汽水湖中分离并表征II型甲烷营养菌。

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