Constanza Aguado-Norese, Jonathan E Maldonado, Christian Hodar, Gabriel Galvez, Daniel E Palma, Verónica Cambiazo, Mauricio Gonzalez
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引用次数: 0
Abstract
Background: In plants, root exudates selectively influence the growth of bacteria that colonize the rhizosphere. Bacterial communities associated with root systems are involved in macro and micronutrients cycling and organic matter transformation. In particular, iron is an essential micronutrient required for the proper functioning of iron-containing enzymes in processes such as photosynthesis, respiration, biomolecule synthesis, redox homeostasis, and cell growth in plants. However, the impact of changes of iron availability on the structure and set of ecological interactions taking place in the rhizosphere remains poorly understood. In this study, field experiments were conducted to compare the effects of iron supplementation (0.1 and 0.5 mM of FeSO4) on the assembly of the bacterial community of rhizosphere soil and bulk soil in a perennial grass present in the Andes steppe of Atacama Desert.
Results: The results indicated that the difference in beta diversity between bulk soil and rhizosphere soil detected before supplementation did not persist after iron supplementation, in addition, co-occurrence networks showed a significant reduction in negative interactions among soil bacteria, mainly in rare taxa (< 0.1% relative abundance).
Conclusions: These observations suggest that iron availability contributes to the differentiation between bulk soil and rhizosphere bacterial communities, a process that is linked to significant changes in the relative abundance of more abundant species (> 0.1% relative abundance) and with a decrease in the negative interactions in both compartments after metal exposure. The differential effect of iron on the competition/cooperation ratio between bulk soils and the rhizosphere microbiome supports the hypothesis that the host limits the degree of cooperation that can be achieved by the bacterial community associated with an organ dedicated to nutrient absorption.
背景:在植物中,根分泌物选择性地影响定植在根际的细菌的生长。与根系相关的细菌群落参与宏量和微量养分循环和有机质转化。特别是,铁是植物光合作用、呼吸、生物分子合成、氧化还原稳态和细胞生长等过程中含铁酶正常运作所必需的微量营养素。然而,铁有效性的变化对发生在根际的结构和生态相互作用的影响仍然知之甚少。本研究通过田间试验比较了补铁(0.1和0.5 mM FeSO4)对阿塔卡马沙漠安第斯草原多年生草地根际土壤和块状土壤细菌群落组成的影响。结果:结果表明,补铁前块状土壤与根际土壤β多样性的差异在补铁后不再持续,土壤细菌之间的负相互作用显著减少,主要是在稀有类群中(结论:这些观察结果表明,铁的有效性有助于块状土壤和根际细菌群落之间的分化,这一过程与更丰富的物种的相对丰度(> 0.1%相对丰度)的显著变化有关,并且与金属暴露后两个区室的负相互作用减少有关。铁对大块土壤和根际微生物组之间竞争/合作比率的不同影响支持了这样的假设,即宿主限制了与专门吸收养分的器官相关的细菌群落可以实现的合作程度。
期刊介绍:
Microorganisms, omnipresent across Earth's diverse environments, play a crucial role in adapting to external changes, influencing Earth's systems and cycles, and contributing significantly to agricultural practices. Through applied microbiology, they offer solutions to various everyday needs. Environmental Microbiome recognizes the universal presence and significance of microorganisms, inviting submissions that explore the diverse facets of environmental and applied microbiological research.