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The physical structure of soil: Determinant and consequence of trophic interactions

机译:土壤的物理结构:营养互动的决定因素及其后果

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Trophic interactions play a vital role in soil functioning and are increasingly considered as important drivers of the soil microbiome and biogeochemical cycles. In the last decade, novel tools to decipher the structure of soil food webs have provided unprecedent advance in describing complex trophic interactions. Yet, the major challenge remains to understand the drivers of the trophic interactions. Evidence suggests that small scale soil physical structure may offer a unifying framework for understanding the nature and patterns of trophic interactions in soils. Here, we review the current knowledge of how restrictions on soil organisms' ability to sense and access food resources/prey inherent to soil physical structure essentially shape trophic interactions. We focus primarily on organisms unable to deform the soil and create pores themselves, such as bacteria, fungi, protists, nematodes and microarthropods, and consider pore geometry, connectivity and hydration status as main descriptors of the soil physical structure. We point that the soil physical structure appears to mostly limit the sensing and accessibility to food resources/prey, with negative effects on bottom up controls. The main mechanisms are (i) the reduced transport of sensing molecules, notably volatiles, through the soil matrix and (ii) the wide presence of refuges leading to pore size segregation of consumer/predators and food sources/prey in pores of contrasting size. In addition, variations in the connectivity of the soil pores and the water film is suggested as a central aspect driving encounter probability between consumers/predator and food source/prey and hence locally decrease or increase top-down controls. Constraints imposed by the soil physical structure on trophic interactions are thought to be major drivers of the soil diversity and local community assemblage, notably by favoring a variety of adaptations to feed in this dark labyrinth (food specialists/flexible/generalists) and by limiting competitive exclusion through limited encounter probability of consumers. We conclude with possible future ways for an interdisciplinary and more quantitative research merging soil physics and soil food web ecology.
机译:营养性互动在土壤运作中发挥着至关重要的作用,越来越多地被视为土壤微生物组和生物地球化学循环的重要司机。在过去的十年中,破译土壤食物网结构的新型工具已经提供了前所未有的进展,以描述复杂的营养互动。然而,主要挑战仍然是为了了解营养互动的司机。证据表明,小规模的土壤物理结构可以提供统一的框架,以了解土壤中营养互动的性质和模式。在这里,我们审查了目前关于土壤生物的限制的知识,了解和获得土壤物理结构固有的遗传学资源/猎物的限制基本形状营养互动。我们主要关注生物体无法变形土壤,并创造毛孔本身,如细菌,真菌,原子师,线虫和微型接触,并考虑孔隙几何形状,连接和水合地位作为土壤物理结构的主要描述符。我们指出土壤物理结构主要限制对食品资源/猎物的传感和可访问性,对自下而上控制有负面影响。主要机制是(i)通过土壤基质和(ii)通过土壤基质和(ii)难度的巨大存在,导致消费者/捕食者和食物来源/毛孔孔的孔隙尺寸的孔径分离的广泛存在。另外,建议土壤孔和水膜的连接性的变化作为驾驶消费者/捕食者和食物源/猎物之间的概率的中心方面,并且因此局部减少或增加自上而下的控制。土壤物理结构对营养互动的限制被认为是土壤多样性和当地社区组合的主要驱动因素,特别是通过有利于在这款黑暗的迷宫(食品专家/灵活/通用专家)中饲养各种适应,并通过限制竞争力通过有限的消费者遭遇概率排除。我们结束了跨学科和更多的定量研究合并土壤物理和土壤食品Web生态学的可能性。

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