Plant Root Responses to Three Abundant Soil Minerals: Silicon, Aluminum and Iron

By J. Ma. 2005

196 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/6b782f13399e9d93a873b32d0bf783bc26a80849

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In Plant Science

Citations in the corpus

Siderophores in environmental research: roles and applications (2014, background): “These plants secrete Fe(III)-chelating compounds called phytosiderophores that form specific strong complexes with Fe(III) (Ma, 2005).”
Release of plant-borne flavonoids into the rhizosphere and their role in plant nutrition (2010, background): “The involvement of MATE transporters in vacuolar uptake of flavonoid glucosides has been recently confirmed in the cases of Arabidopsis (TT12) and Medicago truncatula (MATE1) by Marinova et al. (2007) and Zhao and Dixon (2009).”
Chapter 4 Iron Dynamics in the Rhizosphere: Consequences for Plant Health and Nutrition (2008, background): “Iron is the fourth most abundant element in the earth’s crust after oxygen, silicon, and aluminium (Louet, 1986; Ma, 2005).”
Mechanisms Used by Plant Growth-Promoting Bacteria (2011, background): “Iron is the fourth most abundant element on earth (Ma 2005); however, in aerobic soils, iron is mostly precipitated as hydroxides, oxyhydroxides, and oxides so that the amount of iron available for assimilation by living organisms is very low, ranging from 10 7 to 10 23 M at pH 3.”
Root Development and Nutrient Uptake (2006, background): “This progress helps us better understand plant strategies to overcome mineral nutrient stress (Ma, 2005), and offer a real possibility to genetically improve crop productivity in problem soils.”
Drought Stress and Plant Nutrition (2010, background): “L 1 in the form of silicic acid (Marschner 1995; Ma 2005), while its concentration in plants has broader values (ranging from 0.1 to 10.0% of Si in dry weight) (Ma and Takahashi 2002).”
Bacteria and fungi can contribute to nutrients bioavailability and aggregate formation in degraded soils. (2016, unknown): “Moreover, in soil, ferrous (Fe2+) is oxidized to Fe3+ thereby forming insoluble compounds and leaving a very low amount of iron for microbial or plant assimilation (Ma, 2005).”
Plant Growth-Promoting Bacteria: Mechanisms and Applications (2012, background): “because ferric ion or Fe, which is the predominant form in nature, is only sparingly soluble so that the amount of iron available for assimilation by living organisms is extremely low [43].”
Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective (2009, background): “and other micronutrients, especially from calcareous soil (Römheld 1987; Ma 2005; Robin et al. 2008).”