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首页> 外文期刊>Frontiers in Microbiology >The Relationship between pH and Bacterial Communities in a Single Karst Ecosystem and Its Implication for Soil Acidification
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The Relationship between pH and Bacterial Communities in a Single Karst Ecosystem and Its Implication for Soil Acidification

机译:单一岩溶生态系统中pH与细菌群落的关系及其对土壤酸化的意义

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Enhanced monsoon duration and soil acidification from acid rain are expected to impact the distribution of microbial communities in surface and subsurface environments, although these impacts are poorly understood for most systems. In central China, soluble carbonate bedrock forms extensive karst landscapes. Current predictions are that the amount of monsoonal precipitation and acid rainfall in central China will increase, which is expected to lead to changes in the pH balance of karst ecosystems. To evaluate the role of pH, total organic carbon, and other geochemical parameters (e.g., Ca~(2+), Mg~(2+), NH_(4)~(+), NO_(x), SO_(4)~(2-)) in shaping bacterial communities within a single karst system in central China, samples were collected from the thin surface soils overlying Heshang Cave, cave sediments, and weathered cave passage rocks from the entrance, twilight, and dark zones, as well as from epikarstic drip waters inside the cave. Illumina sequencing of 16S rRNA genes and multivariate statistical analyses revealed that each tested community was distinct and the community variability was significantly correlated with pH, total organic carbon, and potassium concentrations. Specifically, surface soils were dominated by Acidobacteria, Verrucomicrobia and Planctomycetes, and diversity significantly decreased with acidic pH values. Nitrospirae, Gemmatimonadetes, Firmicutes, and Chloroflexi were unique to cave sediments, while Actinobacteria and Proteobacteria dominated weathered rocks and drip waters, respectively. The results reveal important implications regarding the effects of acidification on bacterial communities in karst areas, and on the control of pH in shaping bacterial communities throughout a karst system. Increased water flux into and through karst habitats due to monsoonal precipitation may result in deeper penetration of acidic solutions into karst and shift the bacterial communities inside the cave in the future.
机译:季风持续时间的延长和酸雨对土壤酸化的影响预计会影响表层和地下环境中微生物群落的分布,尽管大多数系统对这些影响的了解很少。在中国中部,可溶性碳酸盐基岩形成了广泛的岩溶景观。当前的预测是,中国中部的季风降水和酸雨数量将增加,这有望导致喀斯特生态系统的pH平衡发生变化。评估pH,总有机碳和其他地球化学参数(例如Ca〜(2 +),Mg〜(2 +),NH_(4)〜(+),NO_(x),SO_(4)的作用〜(2-))在中国中部单一岩溶系统中形成细菌群落时,从河上洞,洞穴沉积物和风化的洞穴通道岩石的薄薄表层土壤中采集了样品,这些岩石分别来自入口,暮光和暗区。以及来自洞穴内部的岩溶滴水。 Illumina对16S rRNA基因的测序和多变量统计分析表明,每个测试的群落都是不同的,并且群落变异性与pH值,总有机碳和钾浓度显着相关。具体而言,表层土壤以酸性细菌,疣状微生物和扁平菌为主导,其多样性随酸性pH值而显着降低。硝化螺旋菌,双歧杆菌,硬毛菌和绿屈挠菌是洞穴沉积物所独有的,而放线菌和变形杆菌分别支配着风化的岩石和滴水。结果表明,酸化对岩溶区细菌群落的影响以及整个岩溶系统中塑造细菌群落的pH值控制具有重要意义。由于季风性降水,流入和穿过喀斯特生境的水通量增加,可能会导致酸性溶液更深地渗入喀斯特,并在将来改变洞穴内的细菌群落。

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