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Factors Influencing Observed Variations in the Structure of Bacterial Communities On Calcite Formations in Kartchner Caverns, AZ, USA

机译:影响美国亚利桑那州卡特纳洞穴中方解石形成细菌群落结构变化的因素

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Kartchner Caverns is an oligotrophic subterranean environment that hosts a wide diversity of actively growing calcite speleothems (secondary mineral deposits). In a previous study, we demonstrated that bacterial communities extracted from these surfaces are quite complex and vary between formations. In the current study, we evaluated the influence of several environmental variables on the superficial bacterial community structure of 10 active formations located in close proximity to one another in a small room of Kartchner Caverns State Park, Arizona, USA. Physical (color, dimensions) and chemical (elemental profile and organic carbon concentration) properties, as well as the DGGE-based bacterial community structure of the formations were analyzed. While elemental concentration was found to vary among the formations, the differences in the community structure could not be correlated with concentrations of either organic carbon or any of the elements evaluated. In contrast, the locations of formations within a distinct region of the cave as well as the relative location of specific formations within a single room were found to have a significant influence on the bacterial community structure of the formations evaluated. Interestingly, Canonical Correspondence Analysis suggests an association between the observed drip pathways (drip lines) feeding the formations (as determined by the patterns of soda straws and small stalactites that reveal water flow patterns) and the bacterial community structure of the respective formations. The results presented here indicate that a broad range of formations fed by a diversity of drip sources must be sampled to fully characterize the community composition of bacteria present on the surfaces of calcite formations in carbonate caves.View full textDownload full textKeywordscarbonate cave, speleotherm, bacterial community structure, oligotrophic, drip waterRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/01490451.2011.581326
机译:卡特纳洞穴(Kartchner Caverns)是一种贫营养的地下环境,拥有各种各样活跃生长的方解石speleothem(次生矿床)。在先前的研究中,我们证明了从这些表面提取的细菌群落非常复杂,并且在地层之间也有所不同。在当前的研究中,我们评估了几个环境变量对位于美国亚利桑那州Kartchner Caverns State Park的一间小房间中彼此相邻的10个活跃地层的表面细菌群落结构的影响。分析了物理(颜色,尺寸)和化学(元素分布和有机碳浓度)特性,以及基于DGGE的地层细菌群落结构。虽然发现元素浓度在地层之间有所不同,但群落结构的差异与有机碳或任何评估元素的浓度均不相关。相反,发现洞穴的不同区域内的地层位置以及单个房间内特定地层的相对位置对所评估地层的细菌群落结构具有重要影响。有趣的是,规范对应分析表明,观察到的供入地层的滴水路径(滴水线)(由苏打管和揭示水流模式的小钟乳石的模式确定)与各个地层的细菌群落结构之间存在关联。此处给出的结果表明,必须采样由多种滴灌源补给的各种地层,才能充分表征碳酸盐洞穴中方解石层表面存在的细菌群落组成。查看全文下载全文关键词社区结构,贫营养性,滴水-4dff56cd6bb1830b“};添加到候选列表链接永久链接http://dx.doi.org/10.1080/01490451.2011.581326

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