Plant succession and rhizosphere microbial communities in a recently deglaciated alpine terrain

By D. Tscherko, Ute Hammesfahr, G. Zeltner, E. Kandeler, R. Böcker. 2005

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Interactions among soil, plants, and microorganisms drive secondary succession in a dry environment (2014, background): “activity, as reported for primary succession (Tscherko et al., 2005).”
Abundance of narG, nirS, nirK, and nosZ Genes of Denitrifying Bacteria during Primary Successions of a Glacier Foreland (2006, methodology): “Plant growth is very limited in the early primary successional stage: plants cover only up to 5% of the soil surface and do not significantly change the activity and biomass of rhizosphere microorganisms (26).”
Methods for evaluating human impact on soil microorganisms based on their activity, biomass, and diversity in agricultural soils (2006, background): “Sometimes a large variety of soil enzymes has been measured (Kandeler et al, 1997; Tscherko et al., 2005).”