Linking plants to rocks: ectomycorrhizal fungi mobilize nutrients from minerals.

By R. Landeweert, E. Hoffland, R. Finlay, T. Kuyper, N. Breemen. Trends in Ecology & Evolution, 2001

730 citations recorded by the source corpus.

Subfields: Insect Science, Nature and Landscape Conservation, Plant Science

View Paper: https://www.semanticscholar.org/paper/63002030bb80d353496fc16fc1eafb557f64c9e7

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Insect Science

1. R. Finlay
2. Petr Baldrian
3. R. Bardgett
4. J. Dighton
5. Sarah E. Smith
6. F. Andrew Smith
7. Marcel G. A. van der Heijden
8. Geoffrey M. Gadd

In Nature and Landscape Conservation

1. R. Finlay
2. Sarah E. Smith
3. F. Andrew Smith
4. P. Hinsinger
5. Marcel G. A. van der Heijden
6. Jean-François Ponge
7. J. Dighton
8. H. Lambers

In Plant Science

1. R. Finlay
2. Petr Baldrian
3. F. Andrew Smith
4. H. Lambers
5. Geoffrey M. Gadd
6. Sarah E. Smith
7. P. Hinsinger
8. J. Jansa

Citations in the corpus

• Decreased soil organic P fraction associated with ectomycorrhizal fungal activity to meet increased P demand under N application in a subtropical forest ecosystem (2017, background): “…(AMF) and ectomycorrhizal fungi (EMF) associated with plant roots can accelerate the mineralization of soil organic P by excreting organic acids, phenolic compounds, protons, and P-targeting enzymes (Landeweert et al. 2001; Richardson and Simpson 2011; Becquer et al. 2014; Rosling et al. 2015).”
• Soil acidification and adaptations of plants and microorganisms in Bornean tropical forests (2014, background): “To solubilize recalcitrant nutrients, plant roots and microorganisms can release organic acids and enzymes into the soil solution (Landeweert et al. 2001; Sinsabaugh et al. 2002; van Schoïl et al. 2008).”
• Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective (2009, background): “However, it may well be the case when the source of Ca is the weathering of other Ca-bearing minerals, e.g., plagioclase feldspars (Cromack et al. 1979; Landeweert et al. 2001).”
• The unseen majority: soil microbes as drivers of plant diversity and productivity in terrestrial ecosystems. (2008, background): “Other routes by which microbes can alter plant nutrient availability include weathering of soils via the exudation of organic acids (Landeweert et al. 2001) and the solubilization of various forms of precipitated P; on the basis of laboratory assays, it was shown that P-solubilizing bacteria may…”
• Oxalate production by fungi: significance in geomycology, biodeterioration and bioremediation (2014, background): “Mycorrhizal fungi can exhibit considerable mineral bioweathering properties with effects on metal mobility (Landeweert et al., 2001; Martino et al., 2003a,b; Hoffland et al., 2004; Bonneville et al., 2009, 2011; Smits et al., 2012; McMaster, 2012).”
• Rock-eating mycorrhizas: their role in plant nutrition and biogeochemical cycles (2008, background): “…and the potential weathering capacity of EcM fungi raised novel questions regarding roles of EcM fungi in plant nutrition (especially uptake of base cations), biogeochemical processes and pedogenesis i.e. podzolisation (Van Breemen et al. 2000a; Van Breemen et al. 2000b; Landeweert et al. 2001).”
• The role of fungi in weathering (2004, background): “Ectomycorrhizal fungi show a larger array of LMWOAs, including citrate and malate (Landeweert et al. 2001).”