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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Carbon stable isotope patterns of cyclic terpenoids: A comparison of cultured alkaliphilic aerobic methanotrophic bacteria and methane-seep environments
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Carbon stable isotope patterns of cyclic terpenoids: A comparison of cultured alkaliphilic aerobic methanotrophic bacteria and methane-seep environments

机译:环状萜件的碳稳定同位素图案:培养碱性有氧型培养细菌和甲烷渗透环境的比较

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摘要

Aerobic methanotrophic bacteria are known to synthesize a variety of cyclic terpenoids which are typified by C-13-depleted, methane-derived carbon. This peculiarity facilitates identification of methanotroph biomarkers in natural samples. However, the current biomarker database does not always allow biomarker patterns of marine samples to be assigned to the different types of aerobic methanotrophs. To overcome this shortcoming, the carbon stable isotope composition of cyclic terpenoids of two strains of the Type I methanotroph genus Methylomicrobium was analyzed. Other than aerobic methanotrophs used for biomarker studies in the past, these two strains deriving from soda lake environments are able to tolerate the conditions typifying marine environments including high alkalinity and salinity. The cyclic terpenoid inventory of the two strains comprises 4-methyl steroids, 3-methyl- and desmethyl bacteriohopanepolyols (aminotetrol and aminotriol), and tetrahymanol, all of which are C-13-depleted. The average carbon isotope fractionation between methane and the respective lipid (Delta delta C-13(terpenoied-methane)) is found to be -25 parts per thousand for M. kenyense and -16 parts per thousand for M. alcaliphilum. These data shed new light on the previously reported compound and carbon stable isotope patterns of cyclic terpenoids from methane-seep environments. Particularly, C-13-depleted tetrahymanol and gammacerane are reinterpreted as biomarkers of aerobic methanotrophic bacteria based on their occurrence in methane-seep deposits in association with other biomarkers of aerobic methanotrophs. The use of delta C-13 values of anaerobic methane-oxidizing archaea (ANME) lipids for the reconstruction of the isotopic composition of parent methane allows us to calculate the Delta delta C-13(terpenoied-methane) even for ancient seep environments. With this calculation, Type I and Type II methanotrophs can be discriminated, representing a new approach to better characterize past methanotrophy at seeps and possibly other marine environments. (C) 2019 Elsevier Ltd. All rights reserved.
机译:已知有氧甲脂肪营养细菌合成各种环状三萜,其典型的C-13耗尽,甲烷衍生的碳。这种特殊性有助于鉴定天然样品中的甲蛋白酶生物标志物。然而,目前的生物标志物数据库并不总是允许将海洋样品的生物标志物模式分配给不同类型的有氧甲虫萎缩。为了克服这种缺点,分析了I型甲蛋白甲基丙酮属甲基微粒素的两种菌株的环状三萜类化合物的碳稳定同位素组成。除了过去用于生物标志物研究的有氧甲蛋白,这两种菌株源于苏打水域环境,能够耐受典型的海洋环境的条件,包括高碱度和盐度。两种菌株的环状三萜类化物包含4-甲基类固醇,3-甲基 - 和去甲基菌磷溶胶(Aminotetrol和氨基氨基)和四氧酚,所有这些都是C-13耗尽。发现甲烷和各种脂质(Delta Delta C-13(Terpenoied-Methane))之间的平均碳同位素分级为-25份千分比,M. kenyense和-16份均为千分之一的M.Alcaliphilum。这些数据在甲烷渗透环境中阐述了先前报道的复合和碳稳定同位素模式的新光。特别是,C-13耗尽的四镁酚和γ甲烷被重新诠释为有氧型培养细菌的生物标志物,基于其与有氧甲蛋白的其他生物标志物相关的甲烷-eIepp沉积物的发生。使用Delta C-13值的厌氧甲烷氧化古(ANME)脂质用于重建亲本甲烷的同位素组合物,甚至可以为古老的渗透环境计算Delta Delta C-13(Terpenoied-甲烷)。通过这种计算,可以区分I型和II型甲胰蛋白,代表更好地表征PEEPS和可能的其他海洋环境的甲基萎缩的新方法。 (c)2019年elestvier有限公司保留所有权利。

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