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Methanogenic Community Was Stable in Two Contrasting Freshwater Marshes Exposed to Elevated Atmospheric CO2

机译:在暴露于大气CO2升高的两个不同的淡水沼泽中产甲烷群落保持稳定

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摘要

The effects of elevated atmospheric CO2 concentration on soil microbial communities have been previously recorded. However, limited information is available regarding the response of methanogenic communities to elevated CO2 in freshwater marshes. Using high-throughput sequencing and real-time quantitative PCR, we compared the abundance and community structure of methanogens in different compartments (bulk soil, rhizosphere soil, and roots) of Calamagrostis angustifolia and Carex lasiocarpa growing marshes under ambient (380 ppm) and elevated CO2 (700 ppm) atmospheres. C. lasiocarpa rhizosphere was a hotspot for potential methane production, based on the 10-fold higher abundance of the mcrA genes per dry weight. The two marshes and their compartments were occupied by different methanogenic communities. In the C. lasiocarpa marsh, archaeal family Methanobacteriaceae, Rice Cluster II, and Methanosaetaceae co-dominated in the bulk soil, while Methanobacteriaceae was the exclusively dominant methanogen in the rhizosphere soil and roots. Families Methanosarcinaceae and Methanocellaceae dominated in the bulk soil of C. angustifolia marsh. Conversely, Methanosarcinaceae and Methanocellaceae together with Methanobacteriaceae dominated in the rhizosphere soil and roots, respectively, in the C. angustifolia marsh. Elevated atmospheric CO2 increased plant photosynthesis and belowground biomass of C. lasiocarpa and C. angustifolia marshes. However, it did not significantly change the abundance (based on mcrA qPCR), diversity, or community structure (based on high-throughput sequencing) of methanogens in any of the compartments, irrespective of plant type. Our findings suggest that the population and species of the dominant methanogens had weak responses to elevated atmospheric CO2. However, minor changes in specific methanogenic taxa occurred under elevated atmospheric CO2. Despite minor changes, methanogenic communities in different compartments of two contrasting freshwater marshes were rather stable under elevated atmospheric CO2.
机译:先前已经记录了大气中二氧化碳浓度升高对土壤微生物群落的影响。但是,关于产甲烷群落对淡水沼泽中CO2浓度升高的反应的信息很少。使用高通量测序和实时定量PCR,我们比较了在环境(380 ppm)和升高的环境下生长的沼泽地卡拉麦格氏霉和苔藓的不同区室(大块土壤,根际土壤和根)产甲烷菌的丰度和群落结构二氧化碳(700 ppm)气氛。基于每干重的mcrA基因丰度高10倍,C。lasiocarpa根际是潜在甲烷生产的热点。这两个沼泽和它们的车厢被不同的产甲烷群落占据。在角果沼泽中,古细菌家族的甲烷细菌科,水稻簇II和甲烷藻科在整个土壤中共同占优势,而甲烷细菌科是根际土壤和根中唯一占主导地位的产甲烷菌。斑节菜沼泽地的大部分土壤中,甲烷菌科和甲烷菌科占主导地位。相反,甲烷八叠球菌科和甲烷菌科以及甲烷菌科分别在根际土壤和根系中占据了优势。升高的大气CO2会增加C. lasiocarpa和 C的植物光合作用和地下生物量。 Angustifolia 沼泽。但是,无论植物类型如何,它都不会显着改变任何隔室中产甲烷菌的丰度(基于 mcr A qPCR),多样性或群落结构(基于高通量测序)。我们的发现表明,主要产甲烷菌的种群和种类对大气CO2升高的响应较弱。但是,在大气CO2升高的情况下,特定产甲烷菌类发生了微小变化。尽管变化不大,但在大气CO2升高的情况下,两个形成鲜明对比的淡水沼泽不同隔间的产甲烷菌群落相当稳定。

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