土壤氧化还原作用驱动热带雨林土壤中的病毒-寄主群落动态和植物生物量退化

Gareth Trubl, Ikaia Leleiwi, Ashley Campbell, Jeffrey A Kimbrel, Amrita Bhattacharyya, Robert Riley, Rex R Malmstrom, Steven J Blazewicz, Jennifer Pett-Ridge
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引用次数: 0

摘要

背景:潮湿的热带森林土壤储存着大量的有机碳,并循环着三分之一以上的陆地净初级生产力。这些土壤中的微生物群对温室气体有着全球性的影响,并能忍受由高还原剂、高土壤湿度和限制氧气扩散的细粒土壤所驱动的极具活力的氧化还原环境。然而,热带土壤微生物群落,尤其是病毒-宿主之间的相互作用,其特征还很不明显,而且随着高强度干旱和降水事件使土壤氧化还原条件的可预测性降低,我们对这些微生物群落将如何影响未来的土壤碳循环知之甚少。研究结果为了研究土壤氧化还原条件的变化对活跃病毒群落以及病毒与微生物相互作用的影响,我们利用波多黎各卢基略实验森林的土壤进行了为期 44 天的氧化还原控制实验,并用富含 13C 的植物生物质进行了改良。我们对 10 个大体元基因组和 85 个稳定同位素探测目标元基因组进行了测序,这些目标元基因组是通过提取整个群落 DNA、进行密度分馏和霰弹枪测序生成的。通过组装病毒和微生物基因组,我们获得了 5,420 个病毒种群(vOTUs)和 927 个中高质量的元基因组,这些基因组横跨 25 个细菌门。值得注意的是,超过一半(54%)的 vOTU 富含 13C,突显了它们在微生物降解植物废弃物过程中的积极作用。这些活跃的 vOTU 主要感染假单胞菌门、酸性杆菌门和放线菌门,其中 57% 的 vOTU 是特定氧化还原处理所独有的。缺氧样本显示出最独特的病毒群落,通过携带氧化还原特异性糖苷水解酶来调节宿主新陈代谢的可能性增加。然而,超过三分之一的 vOTUs 存在于所有氧化还原条件下,这表明在这些自然经历动态氧化还原条件的土壤中,存在着对世界性病毒的选择。结论我们的研究证明了氧化还原条件如何影响土壤中的病毒群落和病毒与宿主之间的相互作用。通过在稳定同位素探测目标元基因组上应用不同的 DNA 组装方法,并在各种氧化还原条件下培养土壤,我们确定了不同的病毒种群,并观察到病毒群落组成和功能的显著变化。这些发现凸显了病毒在不同环境条件下微生物碳降解过程中的特殊作用,为我们深入了解病毒对碳循环的贡献以及对气候变化的广泛影响提供了重要依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil redox drives virus-host community dynamics and plant biomass degradation in tropical rainforest soils
Background: Wet tropical forest soils store a vast amount of organic carbon and cycle over a third of terrestrial net primary production. The microbiomes of these soils have a global impact on greenhouse gases and tolerate a remarkably dynamic redox environment-driven by high availability of reductant, high soil moisture, and fine-textured soils that limit oxygen diffusion. Yet tropical soil microbiomes, particularly virus-host interactions, remain poorly characterized, and we have little understanding of how they will shape future soil carbon cycling as high-intensity drought and precipitation events make soil redox conditions less predictable. Results: To investigate the effects of shifting soil redox conditions on active viral communities and virus-microbe interactions, we conducted a 44-day redox manipulation experiment using soils from the Luquillo Experimental Forest, Puerto Rico, amended with 13C-enriched plant biomass. We sequenced 10 bulk metagenomes and 85 stable isotope probing targeted metagenomes generated by extracting whole community DNA, performing density fractionation, and conducting shotgun sequencing. Viral and microbial genomes were assembled resulting in 5,420 viral populations (vOTUs) and 927 medium-to-high-quality metagenome-assembled genomes across 25 bacterial phyla. Notably, over half (54%) of the vOTUs were 13C-enriched, highlighting their active role in microbial degradation of plant litter. These active vOTUs primarily infected bacterial phyla Pseudomonadota, Acidobacteriota, and Actinomycetota, and 57% were unique to a particular redox treatment. The anoxic samples exhibited the most distinct viral communities, with an increased potential for modulating host metabolism by carrying redox-specific glycoside hydrolases. However, over a third of the vOTUs were present in all redox conditions, suggesting selection for cosmopolitan viruses occurs in these soils that naturally experience dynamic redox conditions. Conclusions: Our study demonstrates how redox conditions shape viral communities and virus-host interactions in soils. By applying different DNA assembly methods on stable isotope probing targeted metagenomes and incubating soils under various redox regimes, we identified distinct viral populations and observed significant variations in viral community composition and function. These findings highlight the specialized roles of viruses in microbial carbon degradation under diverse environmental conditions, providing important insights into their contributions to carbon cycling and the broader implications for climate change.
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