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Chronic Physical Disturbance Substantially Alters the Response of Biological Soil Crusts to a Wetting Pulse as Characterized by Metatranscriptomic Sequencing

机译:慢性物理扰动实质上改变了生物土壤结皮对湿润脉冲的响应这是由超转录组测序表征的

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摘要

Biological soil crusts (biocrusts) are microbial communities that are a feature of arid surface soils worldwide. In drylands where precipitation is pulsed and ephemeral, the ability of biocrust microbiota to rapidly initiate metabolic activity is critical to their survival. Community gene expression was compared after a short duration (1 h) wetting pulse in both intact and soils disturbed by chronic foot trampling. Across the metatranscriptomes the majority of transcripts were cyanobacterial in origin, suggesting that cyanobacteria accounted for the bulk of the transcriptionally active cells. Chronic trampling substantially altered the functional profile of the metatranscriptomes, specifically resulting in a significant decrease in transcripts for nitrogen fixation. Soil depth (biocrust and below crust) was a relatively small factor in differentiating the metatranscriptomes, suggesting that the metabolically active bacteria were similar between shallow soil horizons. The dry samples were consistently enriched for hydrogenase genes, indicating that molecular hydrogen may serve as an energy source for the desiccated soil communities. The water pulse was associated with a restructuring of the metatranscriptome, particularly for the biocrusts. Biocrusts increased transcripts for photosynthesis and carbon fixation, suggesting a rapid resuscitation upon wetting. In contrast, the trampled surface soils showed a much smaller response to wetting, indicating that trampling altered the metabolic response of the community. Finally, several biogeochemical cycling genes in carbon and nitrogen cycling were assessed for their change in abundance due to wetting in the biocrusts. Different transcripts encoding the same gene product did not show a consensus response, with some more abundant in dry or wet biocrusts, highlighting the challenges in relating transcript abundance to biogeochemical cycling rates. These observations demonstrate that metatranscriptome sequencing was able to distinguish alterations in the function of arid soil microbial communities at two varying temporal scales, a long-term ecosystems disturbance through foot trampling, and a short term wetting pulse. Thus, community metatranscriptomes have the potential to inform studies on the response and resilience of biocrusts to various environmental perturbations.
机译:生物土壤结皮(生物结皮)是微生物群落,是全世界干旱表层土壤的特征。在干旱是短暂且短暂的干旱地区,生物结壳微生物群快速启动代谢活性的能力对其生存至关重要。在完整的土壤和被慢性践踏扰乱的土壤中,在短时间(1小时)的润湿脉冲后,比较了社区基因的表达。在整个转录组中,大多数转录本起源于蓝细菌,这表明蓝细菌占了转录活性细胞的大部分。长期践踏大大改变了元转录组的功能,特别是固氮转录本显着减少。在区分元转录组时,土壤深度(生物结皮和地壳以下)是一个相对较小的因素,表明在浅层土壤中代谢活性细菌相似。干燥的样品始终富含氢化酶基因,表明分子氢可以作为干燥土壤群落的能源。水脉冲与超转录组的重组有关,特别是对于生物结壳。生物结皮增加了用于光合作用和碳固定的转录本,表明润湿后会迅速复苏。相反,被践踏的表层土壤对润湿的响应要小得多,这表明践踏改变了群落的代谢响应。最后,评估了碳循环和氮循环中的几个生物地球化学循环基因的丰度变化,这些基因是由于生物结皮被润湿而导致的。编码相同基因产物的不同转录本未显示出共有应答,在干或湿生物结皮中有更多的应答,突显了将转录本丰度与生物地球化学循环速率相关的挑战。这些观察结果表明,转录组测序能够在两个不同的时间尺度上区分干旱土壤微生物群落功能的变化,即通过踩踏造成的长期生态系统干扰以及短期的润湿脉冲。因此,社区转录组有可能为有关生物壳对各种环境扰动的反应和复原力的研究提供信息。

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