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Atomic Force Microscopy of the fungi-mineral interface: applications in mineral dissolution, weathering and biogeochemistry

机译:真菌-矿物界面的原子力显微镜:在矿物溶解,风化和生物地球化学中的应用

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摘要

The interaction between mycorrhizal fungi and minerals is of fundamental importance in affecting the geochemical carbon cycle and CO2 concentration in the atmosphere, alongside roles in soil creation and the release of nutrients. The symbiosis between the fungi and the plant, supported by photosynthesis in the host plant, has as one of its key features the interfacial zone where mineral and fungi come into contact. At this interface, the organism exudes a complex mixture of organic acids, chelating molecules, protons, and extracellular polysaccharide. In this review, examples will be given of recent Atomic Force Microscopy experiments to monitor the colonization of phyllosilicate minerals in sterile controlled microcosm environments containing only tree seedlings, mineral chips and mycorrhizal fungi. The surface activity of the colonizing fungal hyphae is extensive and complex. In complementary experiments involving exposure of minerals surfaces to single organic acids, it has been possible to monitor dissolution at the unit cell level and to extract activation energies for specific dissolution processes, for example 49 kJ mol(-1) for 100 mM oxalic acid acting upon a biotite sample. The link between these simpler model experiments and the whole microcosm studies is illustrated partly by observations of fungal-colonized mineral surfaces from microcosms after careful removal of the organism and biolayer. These mineral surfaces give clear indications of basal plane modification and fungal weathering.
机译:菌根真菌和矿物质之间的相互作用对于影响地球化学碳循环和大气中的CO2浓度,以及在土壤创建和养分释放中的作用至关重要。真菌与植物之间的共生,在寄主植物中通过光合作用得到支持,其主要特征之一是矿物和真菌接触的界面区域。在这个界面上,生物体散发出有机酸,螯合分子,质子和细胞外多糖的复杂混合物。在这篇综述中,将列举一些最新的原子力显微镜实验的例子,以监测在仅含树苗,矿物碎屑和菌根真菌的无菌控制微观环境中叶硅酸盐矿物的定殖。定殖真菌菌丝的表面活性广泛而复杂。在涉及使矿物表面暴露于单一有机酸的补充实验中,可以监测晶胞水平的溶解并提取特定溶解过程的活化能,例如对于100 mM草酸起作用的49 kJ mol(-1)在黑云母样品上。这些更简单的模型实验与整个微观研究之间的联系部分通过仔细观察去除生物体和生物层后从微观的真菌定殖的矿物表面得到说明。这些矿物表面清楚地表明了基础平面的变化和真菌的风化作用。

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