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首页> 外文期刊>FEMS Microbiology Ecology >Contribution of aerobic anoxygenic phototrophic bacteria to total organic carbon pool in aquatic system of subtropical karst catchments, Southwest China: evidence from hydrochemical and microbiological study
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Contribution of aerobic anoxygenic phototrophic bacteria to total organic carbon pool in aquatic system of subtropical karst catchments, Southwest China: evidence from hydrochemical and microbiological study

机译:西南西南亚热带岩溶集水系统水产系统中有氧缺氧性光养细菌的贡献:来自水化学和微生物研究的证据

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摘要

Aerobic anoxygenic phototrophic bacteria may play a particular role in carbon cycling of aquatic systems. However, little is known about the interaction between aerobic anoxygenic phototrophic bacteria and hydrochemistry in groundwater-surface water exchange systems of subtropical karst catchments. We carried out a detailed study on the abundance of aerobic anoxygenic phototrophic bacteria and bacterioplankton, hydrochemistry and taxonomy of bacterioplankton in the Maocun watershed, Southwest China, an area with karst geological background. Our results revealed that bacteria are the important contributors to total organic carbon source/sequestration in the groundwater-surface water of this area. The aerobic anoxygenic phototrophic bacteria, including beta-Proteobacteria, also appear in the studied water system. In addition to that, the genus Polynucleobacter of the phototropic beta-Proteobacteria shows a close link with those sampling sites by presenting bacterial origin organic carbon on CCA biplot and is found to be positively correlated with total nitrogen, dissolved oxygen and pH (r = 0.860, 0.747 and 0.813, respectively) in the Maocun watershed. The results suggest that Polynucleobacter might be involved in the production of organic carbon and might act as the negative feedback on global warming.
机译:有氧缺氧性光营养细菌可能在水生系统的碳循环中发挥特殊作用。然而,关于亚热带喀斯特集水区的地下水表面水交换系统中有氧缺氧性光养细菌和水化之间的相互作用几乎熟知。我们对大量的有氧缺氧型光营养细菌和菌株的细菌和菌株植物学,水利化学和分类学的毛村流域,西南部,西南部,喀斯特地质背景。我们的研究结果表明,细菌是该地区地下水地水中总有机碳源/封存的重要贡献者。在研究的水系统中出现了有氧缺氧性光养细菌,包括β-植物菌。除此之外,光致β-蛋白的多核酸杆菌通过在CCA双针上呈现细菌来源的有机碳,发现与那些取样位点的密切联系,并发现与总氮,溶解氧和pH正面相关(r = 0.860在Maocun流域分别为0.747和0.813。结果表明,多核杆可能涉及有机碳的生产,并且可以作为全球变暖的负反馈。

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