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Soil Aggregate Microbial Communities: Towards Understanding Microbiome Interactions at Biologically Relevant Scales

机译:土壤聚集体微生物群落:在生物学相关尺度上了解微生物组相互作用

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摘要

Soils contain a tangle of minerals, water, nutrients, gases, plant roots, decaying organic matter, and microorganisms which work together to cycle nutrients and support terrestrial plant growth. Most soil microorganisms live in periodically interconnected communities closely associated with soil aggregates, i.e., small (<2 mm), strongly bound clusters of minerals and organic carbon that persist through mechanical disruptions and wetting events. Their spatial structure is important for biogeochemical cycling, and we cannot reliably predict soil biological activities and variability by studying bulk soils alone. To fully understand the biogeochemical processes at work in soils, it is necessary to understand the micrometerscale interactions that occur between soil particles and their microbial inhabitants. Here, we review the current state of knowledge regarding soil aggregate microbial communities and identify areas of opportunity to study soil ecosystems at a scale relevant to individual cells. We present a framework for understanding aggregate communities as "microbial villages" that are periodically connected through wetting events, allowing for the transfer of genetic material, metabolites, and viruses. We describe both top-down (whole community) and bottom-up (reductionist) strategies for studying these communities. Understanding this requires combining "model system" approaches (e.g., developing mock community artificial aggregates), field observations of natural communities, and broader study of community interactions to include understudied community members, like viruses. Initial studies suggest that aggregate-based approaches are a critical next step for developing a predictive understanding of how geochemical and community interactions govern microbial community structure and nutrient cycling in soil.
机译:土壤中含有矿物质、水、养分、气体、植物根系、腐烂的有机物和微生物,它们共同作用以循环养分并支持陆生植物的生长。大多数土壤微生物生活在与土壤团聚体密切相关的周期性相互联系的群落中,即通过机械破坏和润湿事件持续存在的小型(<2 毫米)强结合的矿物质和有机碳簇。它们的空间结构对生物地球化学循环具有重要意义,仅通过研究块状土壤无法可靠地预测土壤的生物活动和变异性。为了充分了解土壤中起作用的生物地球化学过程,有必要了解土壤颗粒与其微生物居民之间发生的微米级相互作用。在这里,我们回顾了有关土壤聚集体微生物群落的当前知识状况,并确定了在与单个细胞相关的规模上研究土壤生态系统的机会领域。我们提出了一个框架,将聚集群落理解为“微生物村”,这些村庄通过润湿事件周期性地连接,允许遗传物质、代谢物和病毒的转移。我们描述了自上而下(整个社区)和自下而上(还原论)研究这些社区的策略。要理解这一点,需要结合“模型系统”方法(例如,开发模拟群落人工聚集体),对自然群落的实地观察,以及对群落相互作用的更广泛研究,以包括未被充分研究的社区成员,如病毒。初步研究表明,基于聚集体的方法是预测地球化学和群落相互作用如何控制土壤中微生物群落结构和养分循环的关键下一步。

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