Cellular dissolution at hypha- and spore-mineral interfaces revealing unrecognized mechanisms and scales of fungal weathering
By Zi-bo Li, Lianwen Liu, Jun Chen, H. Teng. 2016
89 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Ecology, Ecology, Evolution, Behavior and Systematics
View Paper: https://www.semanticscholar.org/paper/d16744b6b73838da5f65853630240c78bd3901bb
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In Earth-Surface Processes
In Ecology
In Ecology, Evolution, Behavior and Systematics
Citations in the corpus
- Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale (2020, background): “More recent studies of lizardite dissolution by fungal cells, using confocal laser scanning microscopy (CLSM) (Li et al., 2016), suggest that biomechanical forces of hyphal growth are indispensable for fungal weathering and strong enough to breach the mineral lattice.”
- Clay minerals interaction with microorganisms: a review (2017, background): “Li et al. (2016) estimated that 40–50% of the dissolved mass of lizardite in a culture in water medium of the fungus T. flavus (isolated from the rhizospheric soil in a serpentine mine) was caused by direct contact of spores and hyphae of the fungus with the mineral surface.”
- Microbial Interaction with Clay Minerals and Its Environmental and Biotechnological Implications (2020, background): “In the experimental study of the nature of fungal weathering of lizardite [(Mg, Fe, Ni)3Si2O5(OH)4], the dissolution of this silicate mineral and Mg, Si, Fe and Ni release were found to be driven by the over-excretion of oxalic acid and siderophores by the indigenous fungus Talaromyces flavus [153].”