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Analysis of Facultative Lithotroph Distribution and Diversity on Volcanic Deposits by Use of the Large Subunit of Ribulose 15-Bisphosphate Carboxylase/Oxygenase

机译:利用核糖15-双磷酸磷酸羧化酶/加氧酶的大亚基分析火山岩的兼性岩溶体分布和多样性

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摘要

A 492- to 495-bp fragment of the gene coding for the large subunit of the form I ribulose 1,5-bisphosphate carboxylase/oxygenase (RubisCO) (rbcL) was amplified by PCR from facultatively lithotrophic aerobic CO-oxidizing bacteria, colorless and purple sulfide-oxidizing microbial mats, and genomic DNA extracts from tephra and ash deposits from Kilauea volcano, for which atmospheric CO and hydrogen have been previously documented as important substrates. PCR products from the mats and volcanic sites were used to construct rbcL clone libraries. Phylogenetic analyses showed that the rbcL sequences from all isolates clustered with form IC rbcL sequences derived from facultative lithotrophs. In contrast, the microbial mat clone sequences clustered with sequences from obligate lithotrophs representative of form IA rbcL. Clone sequences from volcanic sites fell within the form IC clade, suggesting that these sites were dominated by facultative lithotrophs, an observation consistent with biogeochemical patterns at the sites. Based on phylogenetic and statistical analyses, clone libraries differed significantly among volcanic sites, indicating that they support distinct lithotrophic assemblages. Although some of the clone sequences were similar to known rbcL sequences, most were novel. Based on nucleotide diversity and average pairwise difference, a forested site and an 1894 lava flow were found to support the most diverse and least diverse lithotrophic populations, respectively. These indices of diversity were not correlated with rates of atmospheric CO and hydrogen uptake but were correlated with estimates of respiration and microbial biomass.
机译:编码I型核糖1,5-双磷酸羧化酶/加氧酶(RubisCO)(rbcL)的大亚基的基因的492至495 bp片段通过PCR扩增了兼性石化的需氧CO氧化细菌,无色氧化紫色硫化物的微生物垫,以及来自提夫拉的基因组DNA提取物和基拉韦厄火山的灰烬沉积物,以前已证明大气中的CO和氢是重要的底物。来自垫子和火山位点的PCR产物用于构建rbcL克隆文库。系统发育分析表明,所有分离株的rbcL序列都与来源于兼性石养体的IC rbcL序列聚集在一起。相反,微生物垫克隆序列与来自代表形式IA rbcL的专性石藻的序列聚集。来自火山位点的克隆序列属于IC进化枝形式,这表明这些位点由兼性岩溶体占主导地位,这一观察结果与该位点的生物地球化学模式一致。根据系统发育和统计分析,克隆文库在火山位点之间存在显着差异,表明它们支持截然不同的岩石营养组合。尽管某些克隆序列与已知的rbcL序列相似,但大多数是新颖的。根据核苷酸多样性和平均成对差异,发现林区和1894年的熔岩流分别支持最多样化和最不多样化的石营养种群。这些多样性指数与大气中CO和氢的吸收速率无关,但与呼吸和微生物生物量的估计相关。

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