Mycorrhizal weathering: A true case of mineral plant nutrition?

By N. van Breemen, R. Finlay, U. Lundström, A. Jongmans, R. Giesler, M. Olsson. 2000

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Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale (2020, background): “The widespread occurrence of tubular pores, 3–10 µm in diameter, has been demonstrated in weatherable minerals in podzol surface soils and shallow granitic rock under European coniferous forests (van Breemen et al., 2000; Jongmans et al., 1997; Landeweert et al., 2001).”
Defining nutritional constraints on carbon cycling in boreal forests – towards a less `phytocentric' perspective (2002, background): “It has been speculated that microbial communities associated with mycorrhizal mycelium may contribute to both these processes (Perez–Moreno and Read, 2000; Van Breemen et al., 2000).”
Endophytic bacteria in cacti seeds can improve the development of cactus seedlings (2009, background): “Dissolved products are translocated by the host plant roots, bypassing the soil solution and bypassing competition for nutrient uptake by other organisms (van Breemen et al., 2000).”
The mycorrhizal-associated nutrient economy: a new framework for predicting carbon-nutrient couplings in temperate forests. (2013, background): “However, the C : N of leaves and litter are the only parameters that differ across temperate forest PFTs (Oleson et al., 2010; Brovkin et al., 2012).”