Elevated atmospheric carbon dioxide concentration: effects of increased carbon input in a Lolium perenne soil on microorganisms and decomposition

By J. van Ginkel, A. Gorissen, D. Polci. 2000

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Distribution and turnover of recently fixed photosynthate in ryegrass rhizospheres (2004, background): “…by a number of physiological (e.g., plant growth stage, defoliation) and environmental (e.g., temperature, CO2 concentration, soil fertility, soil texture, and light intensity) factors (Martin and Kemp, 1980; Merckx et al., 1985; Whipps, 1985; van Ginkel et al., 1997, 2000; Hütsch et al., 2002).”
Sequestration and turnover of bacterial‐ and fungal‐derived carbon in a temperate grassland soil under long‐term elevated atmospheric pCO2 (2006, background): “Van Ginkel et al. (2000) reported that the turnover of plant-derived 14C in soil was not affected by elevated pCO2 levels.”
Review of estimation of plant rhizodeposition and their contribution to soil organic matter formation (2004, background): “A part of this C remains adsorbed on clay minerals and SOM (2 – 4%), or is incorporated in rhizosphere microorganisms (0.8 – 3.2%, Kuzyakov et al., 2000a; ca. 2%, Van Ginkel et al., 2000; Domanski et al., 2001).”
The role of abiotic factors modulating the plant-microbe-soil interactions: toward sustainable agriculture. A review (2017, background): “Previous studies have demonstrated reductions in pasture microbial decomposition rates after exposure to high concentrations of CO2 (Van Ginkel et al., 2000; Gustavo Santoyo, Claudia Hernández-Pacheco, Julie Hernández-Salmerón, and Rocio Hernández-León Spanish Journal of Agricultural Research March…”