Interactive effects of depth and differential irrigation on soil microbiome composition and functioning

D. Naylor, Katherine Naasko, Montana L. Smith, Sneha P. Couvillion, C. Nicora, Jesse Trejo, S. Fransen, R. Danczak, R. Mcclure, K. Hofmockel, J. Jansson
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引用次数: 2

Abstract

Two factors that are well-known to influence soil microbiomes are the depth of the soil as well as the level of moisture. Previous works have demonstrated that climate change will increase the incidence of drought in soils, but it is unknown how fluctuations in moisture availability affect soil microbiome composition and functioning down the depth profile. Here, we investigated soil and wheatgrass rhizosphere microbiomes in a single common field setting under four different levels of irrigation (100%, 75%, 50%, and 25%) and three depths (0-5 cm, 5-15 cm, and 15-25 cm from the surface). We demonstrated that there is a significant interactive effect between depth and irrigation, where changes in soil moisture more strongly affect soil microbiomes at the surface layer than at deeper layers. This was true for not only microbiome community composition and diversity metrics, but also for functional profiles (transcriptomic and metabolomic datasets). Meanwhile, in rhizosphere communities the influence of irrigation was similar across the different depths. However, for the ‘Alkar’ wheatgrass cultivar, the rhizosphere microbial communities responded more strongly to changes in irrigation level than did the communities for the ‘Jose’ cultivar rhizosphere. The lessened response of deeper soil microbiomes to changes in irrigation may be due to higher incidence of slow-growing, stress-resistant microbes. These results demonstrate that the soil microbiome response to moisture content is depth-dependent. As such, it will be optimal for soil microbiome studies to incorporate deeper as well as surface soils, to get a more accurate picture of the soil microbiome response to stress.
深度和差速灌溉对土壤微生物组成和功能的交互影响
众所周知,影响土壤微生物群的两个因素是土壤的深度和湿度。先前的研究表明,气候变化将增加土壤干旱的发生率,但尚不清楚水分有效性的波动如何影响土壤微生物组的组成和深度剖面的功能。在此,我们研究了在四种不同灌溉水平(100%、75%、50%和25%)和三种深度(0-5 cm、5-15 cm和15-25 cm)的单一普通农田环境下的土壤和小麦根际微生物群。我们证明了深度和灌溉之间存在显著的交互效应,土壤湿度的变化对表层土壤微生物组的影响比对深层土壤微生物组的影响更大。这不仅适用于微生物群落组成和多样性指标,也适用于功能谱(转录组学和代谢组学数据集)。同时,在根际群落中,灌溉对不同深度的影响相似。然而,“Alkar”品种根际微生物群落对灌溉水平变化的响应强于“Jose”品种根际微生物群落。深层土壤微生物组对灌溉变化的反应较弱,可能是由于生长缓慢、抗胁迫的微生物发生率较高。这些结果表明,土壤微生物组对水分含量的响应是深度依赖的。因此,土壤微生物组的研究最好结合深层土壤和表层土壤,以便更准确地了解土壤微生物组对压力的反应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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