Chapter 4 Iron Dynamics in the Rhizosphere: Consequences for Plant Health and Nutrition
By A. Robin, G. Vansuyt, P. Hinsinger, J. Meyer, J. Briat, P. Lemanceau. 2008
133 citations recorded by the source corpus.
Subfields: Plant Science, Renewable Energy, Sustainability and the Environment, Soil Science
View Paper: https://www.semanticscholar.org/paper/30238350e5095ba6761981ce7e4144f3873bcd69
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Citations in the corpus
- Preserving the nutritional quality of crop plants under a changing climate: importance and strategies (2019, background): “Expanding this knowledge to Fe is of particular interest because of its major role in the photosynthetic process and because its bioavailability to plants is often limited, particularly in calcareous soils, which represent 30% of cultivated soils (Briat et al. 2015; Robin et al. 2008).”
- Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective (2009, background): “Robin et al. (2008) stress that this is an efficient strategy to maximise the positive impact on Fe acquisition by minimising the breakdown of phytosiderophores by rhizosphere microorganisms, in agreement with model calculations of Darrah (1991).”
- Mechanisms Used by Plant Growth-Promoting Bacteria (2011, background): “Siderophores are involved both in plant growth promotion and health protection (Robin et al. 2008).”
- Microbial ACC-Deaminase: Prospects and Applications for Inducing Salt Tolerance in Plants (2010, background): “Various other workers have also mentioned the microbial synthesis of siderophores and their role in enhancing Fe uptake (Mori et al., 1991; Arora et al., 2001; Whipps, 2001; Robin et al., 2008).”
- Rhizospheric organic compounds in the soil–microorganism–plant system: their role in iron availability (2014, background): “As can be seen in Table 1, in addition to high-affinity ligands, microorganisms and plants also produce a range of lower-affinity ligands such as phenolics and organic acids (Jones et al., 1996; Reichard et al., 2005; Robin et al., 2008).”
- Rhizosphere: biophysics, biogeochemistry and ecological relevance (2009, background): “The most nutrient-efficient microorganisms are thereby efficiently selected in the rhizosphere (Marschner et al. 2006; Calvaruso et al. 2007; Robin et al. 2008; Lemanceau et al 2009).”
- Linking 3D Soil Structure and Plant-Microbe-Soil Carbon Transfer in the Rhizosphere (2018, background): “Specific mechanisms, such as acidification, reduction, and/or chelation increase iron dissolution and bioavailability in the rhizosphere (Robin et al., 2008).”
- Effect of Trichoderma asperellum strain T34 on iron, copper, manganese, and zinc uptake by wheat grown on a calcareous medium (2011, background): “Effectiveness in the control of soil-borne plant diseases has been ascribed, at least in part, to competition for limiting nutrients between beneficial microbes and pathogenic organisms (Borrero et al. 2004; Bakker et al. 2007; Robin et al. 2008; Lemanceau et al. 2009; Hartmann et al. 2009).”
- Acquisition of phosphorus and nitrogen in the rhizosphere and plant growth promotion by microorganisms (2009, background): “Roots of strategy II type plants (e.g. the Graminaceae; Marschner 1995; Robin et al. 2008) secrete phytosiderophores (Fe-chelators) which bind Fe3+ and maintain its concentration in soil solution (see Lemanceau et al. 2009).”