Coupling between biota and earth materials in the critical zone

By R. Amundson, D. Richter, G. Humphreys, E. Jobbágy, J. Gaillardet. 2007

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Metals, minerals and microbes: geomicrobiology and bioremediation. (2010, unknown): “Direct and indirect physical, chemical and biochemical mechanisms are involved in mineral biodeterioration by microbes (Sand, 1997; Edwards et al., 2005; Amundson et al., 2007; Lian et al., 2008a, b; Uroz et al., 2009) (Figs 1 and 2).”
Clay minerals interaction with microorganisms: a review (2017, background): “For example, respiration of plants and microorganisms in soils can generate partial pressures of CO2 in the soil gas several orders of magnitude greater than that in the atmosphere due to slow gas diffusion (Amundson et al., 2007).”
Crossing Disciplines and Scales to Understand the Critical Zone (2007, background): “…of this issue, our colleagues discuss how geochemical patterns are established through processes occurring at the mineral–water interface (Chorover et al. 2007), as well as how they are affected by biota (Amundson et al. 2007), dust (Derry and Chadwick 2007), and erosion (Anderson et al. 2007).”