Arbuscular mycorrhizae respond to elevated atmospheric CO2 after long‐term exposure: evidence from a CO2 spring in New Zealand supports the resource balance model

By Matthias C. Rillig, G. Y. Hernandez, P. Newton. 2000

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Global Potential of Soil Carbon Sequestration to Mitigate the Greenhouse Effect (2003, background): “Mycorrhizal fungi also contribute to SOC sequestration and increases aggregation (Rillig et al., 1999, 2000, 2001, 2002).”
A connection between fungal hydrophobins and soil water repellency (2005, background): “…GRSP layer at the water-air interface in pot cultures, presence of GRSP in river foam (Harner et al., 2004), localization of glomalin to the hyphal and spore wall of AMF (Driver et al., 2005), and very high concentrations of GRSP in some soils prone to extreme hydrophobicity (Rillig et al., 2000).”
Microsite differences in fungal hyphal length, glomalin, and soil aggregate stability in semiarid Mediterranean steppes (2003, background): “…measured in only a few natural ecosystems so far (e.g. several grasslands, deciduous and tropical forest, shrubland; Wright and Upadhyaya, 1998; Rillig et al., 1999, 2000, 2001; Bird et al., 2002), and little is known about variability (horizontal and vertical) of soil glomalin pools,…”