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Trends in Selenium Utilization in Marine Microbial World Revealed through the Analysis of the Global Ocean Sampling (GOS) Project

机译:通过全球海洋取样(GOs)项目分析揭示海洋微生物世界硒利用趋势

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摘要

Selenium is an important trace element that occurs in proteins in the form of selenocysteine (Sec) and in tRNAs in the form of selenouridine. Recent large-scale metagenomics projects provide an opportunity for understanding global trends in trace element utilization. Herein, we characterized the selenoproteome of the microbial marine community derived from the Global Ocean Sampling (GOS) expedition. More than 3,600 selenoprotein gene sequences belonging to 58 protein families were detected, including sequences representing 7 newly identified selenoprotein families, such as homologs of ferredoxin– thioredoxin reductase and serine protease. In addition, a new eukaryotic selenoprotein family, thiol reductase GILT, was identified. Most GOS selenoprotein families originated from Cys-containing thiol oxidoreductases. In both Pacific and Atlantic microbial communities, SelW-like and SelD were the most widespread selenoproteins. Geographic location had little influence on Sec utilization as measured by selenoprotein variety and the number of selenoprotein genes detected; however, both higher temperature and marine (as opposed to freshwater and other aquatic) environment were associated with increased use of this amino acid. Selenoproteins were also detected with preference for either environment. We identified novel fusion forms of several selenoproteins that highlight redox activities of these proteins. Almost half of Cys-containing SelDs were fused with NADH dehydrogenase, whereas such SelD forms were rare in terrestrial organisms. The selenouridine utilization trait was also analyzed and showed an independent evolutionary relationship with Sec utilization. Overall, our study provides insights into global trends in microbial selenium utilization in marine environments.
机译:硒是一种重要的微量元素,以硒代半胱氨酸(Sec)的形式存在于蛋白质中,以硒硒酸的形式存在于tRNA中。最近的大规模宏基因组学项目为理解微量元素利用的全球趋势提供了机会。在这里,我们表征了源自全球海洋采样(GOS)考察的微生物海洋群落的硒蛋白质组。检测到属于58个蛋白质家族的3,600多种硒蛋白基因序列,包括代表7个新发现的硒蛋白家族的序列,例如铁氧还蛋白-硫氧还蛋白还原酶和丝氨酸蛋白酶的同源物。另外,鉴定了新的真核硒蛋白家族,巯基还原酶GILT。大多数GOS硒蛋白家族起源于含Cys的巯基氧化还原酶。在太平洋和大西洋微生物群落中,类SelW和SelD是最广泛的硒蛋白。用硒蛋白的种类和检测到的硒蛋白基因的数量来衡量,地理位置对Sec的利用几乎没有影响。但是,高温和海洋环境(与淡水和其他水生环境相反)都与这种氨基酸的使用增加有关。还优选在任一环境中都检测到硒蛋白。我们确定了几种硒蛋白的新型融合形式,这些融合蛋白突出了这些蛋白质的氧化还原活性。几乎一半的含Cys的SelD与NADH脱氢酶融合,而这种SelD形式在陆地生物中很少见。还分析了硒亚尿苷的利用特性,并显示出与Sec利用的独立进化关系。总体而言,我们的研究提供了有关海洋环境中微生物硒利用的全球趋势的见解。

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