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Diversity, evolution, and horizontal gene transfer (HGT) in soda lakes

机译:苏打湖中的多样性,进化和水平基因转移(HGT)

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Soap Lake is a hypersaline, alkaline lake in Central Washington State (USA). For the past five years the lake has been the site of an NSF Microbial Observatory project devoted to identifying critical geochemical and microbial characteristics of the monimolimnion sediment and water column, and has demonstrated rich multispecies communities occupy all areas of the lake. Soap Lake and similar soda lakes are subject to repeated transient periods of extreme evaporation characterized by significant repetitive alterations in salinity, pH, and total water volume, yet maintain high genetic and metabolic diversity. It has been argued that this repetitive cycle for salinity, alkalinity, and sulfur concentration has been a major driver for prokaryote evolution and diversity. The rapidity of wet-dry cycling places special demands on genome evolution, requirements that are beyond the relatively conservative eukaryotic evolutionary strategy of serial alteration of existing gene sequences in a relatively stable genome. Although HGT is most likely responsible for adding a significant amount of noise to the genetic record, analysis of HGT activity can also provide us with a much-needed probe for exploration of prokaryotic genome evolution and the origin of diversity. Packaging of genetic information within the protective protein capsid of a bacteriophage would seem preferable to exposing naked DNA to the highly alkaline conditions in the lake. In this study, we present preliminary data demonstrating the presence of a diverse group of phage integrases in Soap Lake. Integrase is the viral enzyme responsible for the insertion of phage DNA into the bacterial host's chromosome. The presence of the integrase sequence in bacterial chromosomes is evidence of lysogeny, and the diversity of integrase sequences reported here suggests a wide variety of temperate phage exist in this system, and are especially active in transition zones.
机译:肥皂湖是华盛顿州中部(美国)中的碱性碱性湖泊。在过去的五年中,湖泊已成为NSF微生物天文台项目的网站,致力于识别单摩尔沉积物和水柱的关键地球化学和微生物特征,并证明了丰富的多数社区占据了湖的所有地区。肥皂湖和类似的苏打湖受到重复瞬时蒸发的,其特征在于盐度,pH和总水量的显着重复改变,但保持高遗传和代谢多样性。已经认为这种重复循环盐度,碱度和硫浓度是前核演化和多样性的主要驱动因素。湿循环的快速性地对基因组进化的特殊要求,超出了相对稳定的基因组中现有基因序列串行变化的相对保守真核进化策略的要求。虽然HGT最有可能对遗传记录添加大量噪声,但HGT活性的分析还可以为我们提供一种急需的探针,用于探索原核基因组进化和多样性的起源。遗传信息的包装在噬菌体的保护蛋白衣壳中似乎优选将裸体DNA暴露于湖中的高度碱性条件下。在这项研究中,我们提出了初步数据,证明了肥皂湖中不同噬菌体整合酶的存在。整合酶是负责将噬菌体DNA插入细菌宿主染色体的病毒酶。细菌染色体中整合酶序列的存在是溶酶体的证据,这里报道的整合酶序列的多样性表明该系统中存在各种温度噬菌体,并且在过渡区中特别活跃。

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