Department of Plant Pathology, University of California, Davis, CA, USA.
Physical and Life Sciences Directorate, Lawrence Livermore National Laboratory, Livermore, CA, USA.
Nat Ecol Evol. 2023 Nov;7(11):1809-1822. doi: 10.1038/s41559-023-02207-5. Epub 2023 Sep 28.
As central members of soil trophic networks, viruses have the potential to drive substantial microbial mortality and nutrient turnover. Pinpointing viral contributions to terrestrial ecosystem processes remains a challenge, as temporal dynamics are difficult to unravel in the spatially and physicochemically heterogeneous soil environment. In Mediterranean grasslands, the first rainfall after seasonal drought provides an ecosystem reset, triggering microbial activity during a tractable window for capturing short-term dynamics. Here, we simulated precipitation in microcosms from four distinct dry grassland soils and generated 144 viromes, 84 metagenomes and 84 16S ribosomal RNA gene amplicon datasets to characterize viral, prokaryotic and relic DNA dynamics over 10 days. Vastly different viral communities in each soil followed remarkably similar successional trajectories. Wet-up triggered a significant increase in viral richness, followed by extensive compositional turnover. Temporal succession in prokaryotic communities was much less pronounced, perhaps suggesting differences in the scales of activity captured by viromes (representing recently produced, ephemeral viral particles) and total DNA. Still, differences in the relative abundances of Actinobacteria (enriched in dry soils) and Proteobacteria (enriched in wetted soils) matched those of their predicted phages, indicating viral predation of dominant bacterial taxa. Rewetting also rapidly depleted relic DNA, which subsequently reaccumulated, indicating substantial new microbial mortality in the days after wet-up, particularly of the taxa putatively under phage predation. Production of abundant, diverse viral particles via microbial host cell lysis appears to be a conserved feature of the early response to soil rewetting, and results suggest the potential for 'Cull-the-Winner' dynamics, whereby viruses infect and cull but do not decimate dominant host populations.
作为土壤营养网络的核心成员,病毒具有驱动大量微生物死亡和养分转化的潜力。确定病毒对陆地生态系统过程的贡献仍然是一个挑战,因为在空间和物理化学异质的土壤环境中,时间动态难以解决。在地中海草原,季节性干旱后的第一场雨为生态系统重置提供了条件,在可追踪的短期动态窗口中引发微生物活动。在这里,我们模拟了来自四个不同干燥草原土壤的微宇宙中的降水,并生成了 144 个病毒组、84 个宏基因组和 84 个 16S 核糖体 RNA 基因扩增子数据集,以在 10 天内描述病毒、原核生物和 relic DNA 的动态变化。每个土壤中的病毒群落差异很大,但遵循着非常相似的演替轨迹。湿化引发了病毒丰富度的显著增加,随后是广泛的组成性转变。原核生物群落的时间演替则不那么明显,这也许表明病毒组(代表最近产生的、短暂的病毒颗粒)和总 DNA 所捕获的活动规模存在差异。尽管如此,放线菌(在干燥土壤中富集)和变形菌(在湿润土壤中富集)的相对丰度差异与它们预测的噬菌体相对应,表明病毒捕食了优势细菌类群。再湿润还迅速耗尽了 relic DNA,随后又重新积累,表明在再湿润后的几天内,大量新的微生物死亡,特别是那些推测受到噬菌体捕食的分类群。通过微生物宿主细胞裂解产生丰富多样的病毒颗粒,似乎是土壤再湿润早期反应的一个保守特征,研究结果表明了“优胜劣汰”动态的潜力,即病毒感染并淘汰但不会消灭优势宿主种群。