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Ectomycorrhizal Fungi and Mineral Interactions in the Rhizosphere of Scots and Red Pine Seedlings

机译:苏格兰和红松幼苗根际中的菌根真菌和矿物质相互作用

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Ectomycorrhizal fungi and associated bacteria play a key role in plant-driven mineral weathering and uptake of mineral-derived nutrients in the rhizosphere. The goal of this study was to investigate the physical and chemical characteristics of bacteria-fungi-mineral interactions in biofilms of Scots and red pine rhizospheres. In three experiments, seedlings were grown in columns containing silica sand amended with biotite and calcium-feldspar, and inoculated with pure cultures of ectomycorrhizal fungi or a soil slurry. Uninoculated seedlings and unplanted abiotic columns served as controls. After nine months, the columns were destructively sampled and the minerals were analyzed using scanning electron and atomic force microscopy. Element release rates were determined from cation concentrations of input and output waters, soil exchange sites, and plant biomass, then normalized to geometric surface area of minerals in each column. The results revealed that various ectomycorrhizal fungal species stimulate silicate dissolution, and biofilm formation occurred at low levels, but direct surface attachment and etching by fungal hyphae was a minor contributor to the overall cation release from the minerals in comparison to other environmental conditions such as water applications (rain events), which varied among the experiments. This research highlights the importance of experimental design details for future exploration of these relationships.
机译:外生菌根真菌和相关细菌在植物驱动的矿物风化和根际中矿物源养分的吸收中起着关键作用。这项研究的目的是调查苏格兰和赤松根际生物膜中细菌-真菌-矿物质相互作用的物理和化学特性。在三个实验中,将幼苗种植在含有用黑云母和钙长石修饰的硅砂的柱子中,并接种外生菌根真菌或土壤浆的纯培养物。未接种的幼苗和未种植的非生物柱用作对照。 9个月后,对柱子进行了破坏性采样,并使用扫描电子和原子力显微镜对矿物进行了分析。根据进水和出水,土壤交换位点和植物生物量的阳离子浓度确定元素释放速率,然后将其标准化为每列中矿物质的几何表面积。结果表明,各种外生菌根真菌会刺激硅酸盐的溶解,并且生物膜的形成水平较低,但是与其他环境条件(例如水)相比,直接表面附着和真菌菌丝的蚀刻对矿物质中阳离子释放的总体贡献较小。应用(降雨事件),在实验之间有所不同。这项研究强调了实验设计细节对于未来探索这些关系的重要性。

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