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首页> 外文期刊>Applied and Environmental Microbiology >Direct and Indirect Influence of Parental Bedrock on Streambed Microbial Community Structure in Forested Streams
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Direct and Indirect Influence of Parental Bedrock on Streambed Microbial Community Structure in Forested Streams

机译:父母基岩对森林溪流河床微生物群落结构的直接和间接影响

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A correlative study was performed to determine if variation in streambed microbial community structure in low-order forested streams can be directly or indirectly linked to the chemical nature of the parental bedrock of the environments through which the streams flow. Total microbial and photosynthetic biomass (phospholipid phosphate [PLP] and chlorophyll a), community structure (phospholipid fatty acid analysis), and physical and chemical parameters were measured in six streams, three located in sandstone and three in limestone regions of the Bankhead National Forest in northern Alabama. Although stream water flowing through the two different bedrock types differed significantly in chemical composition, there were no significant differences in total microbial and photosynthetic biomass in the sediments. In contrast, sedimentary microbial community structure differed between the bedrock types and was significantly correlated with stream water ion concentrations. A pattern of seasonal variation in microbial community structure was also observed. Further statistical analysis indicated dissolved organic matter (DOM) quality, which was previously shown to be influenced by geological variation, correlated with variation in bacterial community structure. These results indicate that the geology of underlying bedrock influences benthic microbial communities directly via changes in water chemistry and also indirectly via stream water DOM quality.
机译:进行了一项相关研究,以确定低阶森林溪流中溪流微生物群落结构的变化是否可以直接或间接地与溪流所流经的环境的母体基岩的化学性质联系起来。在班克黑德国家森林公园的六个溪流中测量了总的微生物和光合生物量(磷脂磷酸盐[PLP]和叶绿素a),群落结构(磷脂脂肪酸分析)以及理化参数,其中三个位于砂岩中,三个位于石灰岩地区在阿拉巴马州北部。尽管流过两种不同基岩类型的溪流水的化学成分差异显着,但沉积物中总微生物和光合生物量却没有显着差异。相反,沉积微生物群落结构在基岩类型之间不同,并且与溪流水离子浓度显着相关。还观察到了微生物群落结构的季节性变化模式。进一步的统计分析表明,溶解有机物(DOM)的质量先前已显示受地质变异的影响,与细菌群落结构的变异有关。这些结果表明,下层基岩的地质状况直接通过水化学变化影响底栖微生物群落,也间接通过溪流水DOM质量影响。

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