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Host-linked soil viral ecology along a permafrost thaw gradient

机译:多年冻土融化梯度下与宿主相关的土壤病毒生态学

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摘要

Climate change threatens to release abundant carbon that is sequestered at high latitudes, but the constraints on microbial metabolisms that mediate the release of methane and carbon dioxide are poorly understood. The role of viruses, which are known to affect microbial dynamics, metabolism and biogeochemistry in the oceans, remains largely unexplored in soil. Here, we aimed to investigate how viruses influence microbial ecology and carbon metabolism in peatland soils along a permafrost thaw gradient in Sweden. We recovered 1,907 viral populations (genomes and large genome fragments) from 197 bulk soil and size-fractionated metagenomes, 58% of which were detected in metatranscriptomes and presumed to be active. In silico predictions linked 35% of the viruses to microbial host populations, highlighting likely viral predators of key carbon-cycling microorganisms, including methanogens and methanotrophs. Lineage-specific virus/host ratios varied, suggesting that viral infection dynamics may differentially impact microbial responses to a changing climate. Virus-encoded glycoside hydrolases, including an endomannanase with confirmed functional activity, indicated that viruses influence complex carbon degradation and that viral abundances were significant predictors of methane dynamics. These findings suggest that viruses may impact ecosystem function in climate-critical, terrestrial habitats and identify multiple potential viral contributions to soil carbon cycling.
机译:气候变化有可能释放出高纬度螯合的丰富碳,但是人们对调解甲烷和二氧化碳释放的微生物代谢的限制知之甚少。众所周知,病毒的作用会影响海洋中的微生物动力学,新陈代谢和生物地球化学,但在土壤中却尚未被充分研究。在这里,我们旨在调查病毒如何沿瑞典多年冻土融化梯度影响泥炭地土壤中的微生物生态和碳代谢。我们从197个大块土壤和大小分级的元基因组中恢复了1,907个病毒种群(基因组和大的基因组片段),其中58%在元转录组中被检测到并被认为具有活性。在计算机模拟中,将35%的病毒与微生物宿主种群联系在一起,突显了关键的碳循环微生物(包括产甲烷菌和甲烷营养菌)的病毒掠食者。特定于谱系的病毒/宿主比率各不相同,这表明病毒感染动态可能会不同地影响微生物对气候变化的反应。病毒编码的糖苷水解酶(包括具有确定的功能活性的内甘露聚糖酶)表明,病毒会影响复杂的碳降解,并且病毒丰度是甲烷动力学的重要预测因子。这些发现表明,病毒可能会影响关键气候的陆地生境中的生态系统功能,并确定病毒对土壤碳循环的多种潜在贡献。

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