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The Resilience of Microbial Community under Drying and Rewetting Cycles of Three Forest Soils

机译:三种森林土壤干湿循环下微生物群落的复原力

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摘要

Forest soil ecosystems are associated with large pools and fluxes of carbon (C) and nitrogen (N), which could be strongly affected by variation in rainfall events under current climate change. Understanding how dry and wet cycle events might influence the metabolic state of indigenous soil microbes is crucial for predicting forest soil responses to environmental change. We used 454 pyrosequencing and quantitative PCR to address how present (DNA-based) and potentially active (RNA-based) soil bacterial communities might response to the changes in water availability across three different forest types located in two continents (Africa and Asia) under controlled drying and rewetting cycles. Sequencing of rRNA gene and transcript indicated that Proteobacteria, Actinobacteria, and Acidobacteria were the most responsive phyla to changes in water availability. We defined the ratio of rRNA transcript to rRNA gene abundance as a key indicator of potential microbial activity and we found that this ratio was increased following soil dry-down process whereas it decreased after soil rewetting. Following rewetting Crenarchaeota-like 16S rRNA gene transcript increased in some forest soils and this was linked to increases in soil nitrate levels suggesting greater nitrification rates under higher soil water availability. Changes in the relative abundance of (1) different microbial phyla and classes, and (2) 16S and amoA genes were found to be site- and taxa-specific and might have been driven by different life-strategies. Overall, we found that, after rewetting, the structure of the present and potentially active bacterial community structure as well as the abundance of bacterial (16S), archaeal (16S) and ammonia oxidizers (amoA), all returned to pre-dry-down levels. This suggests that microbial taxa have the ability to recover from desiccation, a critical response, which will contribute to maintaining microbial biodiversity in harsh ecosystems under environmental perturbations, such as significant changes in water availability.
机译:森林土壤生态系统与大量的碳和碳和氮(N)库和通量有关,在当前气候变化下,降雨事件的变化可能会严重影响碳和氮的流量。了解干湿循环事件如何影响土著土壤微生物的代谢状态对于预测森林土壤对环境变化的响应至关重要。我们使用了454种焦磷酸测序和定量PCR来解决在以下两个洲(非洲和亚洲)的三种不同森林类型中,现有的(基于DNA的)和潜在活跃的(基于RNA的)土壤细菌群落可能对水利用变化的反应。控制干燥和再润湿的周期。 rRNA基因和转录物的测序表明,Proteobacteria,Actinobacteria和Acidobacteria是对水利用量变化最敏感的门。我们将rRNA转录本与rRNA基因丰度之比定义为潜在微生物活性的关键指标,我们发现该比值在土壤干燥过程后增加,而在土壤重新湿润后降低。重新润湿后,某些森林土壤中的Crenarchaeota样16S rRNA基因转录物增加,这与土壤硝酸盐水平的增加有关,表明在较高土壤水分利用率下硝化率更高。 (1)不同微生物门和类别的相对丰度的变化,以及(2)16S和amoA基因的相对丰度的变化是位点和分类群特异性的,并且可能是由不同的生命策略驱动的。总体而言,我们发现,在重新润湿后,当前和可能具有活性的细菌群落结构的结构以及大量细菌(16S),古细菌(16S)和氨氧化剂(amoA)均返回到干燥前状态。水平。这表明微生物分类群具有从干燥中恢复的能力,这是一种重要的反应,这将有助于在环境扰动下,如水资源的显着变化,在恶劣的生态系统中维持微生物的生物多样性。

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