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Microbial Community Stratification Linked to Utilization of Carbohydrates and Phosphorus Limitation in a Boreal Peatland at Marcell Experimental Forest, Minnesota, USA

机译:美国明尼苏达州马塞尔实验森林中的北方泥炭地微生物群落分层与碳水化合物利用和磷含量的限制

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This study investigated the abundance, distribution, and composition of microbial communities at the watershed scale in a boreal peatland within the Marcell Experimental Forest (MEF), Minnesota, USA. Through a close coupling of next-generation sequencing, biogeochemistry, and advanced analytical chemistry, a biogeochemical hot spot was revealed in the mesotelm (30- to 50-cm depth) as a pronounced shift in microbial community composition in parallel with elevated peat decomposition. The relative abundance of Acidobacteria and the Syntrophobacteraceae , including known hydrocarbon-utilizing genera, was positively correlated with carbohydrate and organic acid content, showing a maximum in the mesotelm. The abundance of Archaea (primarily crenarchaeal groups 1.1c and 1.3) increased with depth, reaching up to 60% of total small-subunit (SSU) rRNA gene sequences in the deep peat below the 75-cm depth. Stable isotope geochemistry and potential rates of methane production paralleled vertical changes in methanogen community composition to indicate a predominance of acetoclastic methanogenesis mediated by the Methanosarcinales in the mesotelm, while hydrogen-utilizing methanogens predominated in the deeper catotelm. RNA-derived pyrosequence libraries corroborated DNA sequence data to indicate that the above-mentioned microbial groups are metabolically active in the mid-depth zone. Fungi showed a maximum in rRNA gene abundance above the 30-cm depth, which comprised only an average of 0.1% of total bacterial and archaeal rRNA gene abundance, indicating prokaryotic dominance. Ratios of C to P enzyme activities approached 0.5 at the acrotelm and catotelm, indicating phosphorus limitation. In contrast, P limitation pressure appeared to be relieved in the mesotelm, likely due to P solubilization by microbial production of organic acids and C-P lyases. Based on path analysis and the modeling of community spatial turnover, we hypothesize that P limitation outweighs N limitation at MEF, and microbial communities are structured by the dominant shrub, Chamaedaphne calyculata , which may act as a carbon source for major consumers in the peatland.
机译:这项研究调查了美国明尼苏达州马赛尔实验森林(MEF)内北方泥炭地分水岭规模的微生物群落的丰度,分布和组成。通过下一代测序,生物地球化学和高级分析化学的紧密结合,在中胚层(深度为30至50 cm)中发现了一个生物地球化学热点,这是微生物群落组成的明显变化,同时泥炭分解增加。酸性细菌和滑膜细菌科的相对丰度,包括已知的利用烃类,与碳水化合物和有机酸含量呈正相关,在中膜中表现出最大值。随着深度的增加,古细菌的数量(主要是科的1.1c和1.3组)随着深度的增加而增加,在深度小于75 cm的深泥炭中达到了全部小亚基(SSU)rRNA基因序列的60%。稳定的同位素地球化学和甲烷生成的潜在速率与产甲烷菌群落组成的垂直变化平行,这表明中生甲烷中由产甲烷甲烷菌介导的乙酰碎屑甲烷化作用占主导地位,而利用氢的产甲烷菌在较深的类别中占主导地位。 RNA衍生的焦磷酸序列文库证实了DNA序列数据,表明上述微生物群在中深度区域具有代谢活性。真菌在30厘米深度以上显示出最大的rRNA基因丰度,仅平均占细菌和古细菌rRNA基因丰度的0.1%,表明原核生物占优势。丙烯醛和类胡萝卜素的C与P酶活性之比接近0.5,表明磷限制。相比之下,中膜中的P限制压力似乎得到了缓解,这可能是由于微生物通过生产有机酸和C-P裂解酶而使P溶解所致。基于路径分析和社区空间转换模型,我们假设MEF的P限制大于N限制,微生物群落由优势灌木Chamaedaphne calyculata构成,该灌木可能是泥炭地主要消费者的碳源。

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