Geochemical Aspects of Phytosiderophore‐Promoted Iron Acquisition by Plants

By S. Kraemer, David E. Crowley, Ruben Kretzschmar. 2006

122 citations recorded by the source corpus.

Subfields: Plant Science, Renewable Energy, Sustainability and the Environment

View Paper: https://www.semanticscholar.org/paper/337052a71a6fbfe194282f04408d54189ef6ae46

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Plant Science

1. Stefano Cesco
2. R. Pinton
3. N. Tomasi
4. J. Briat
5. S. Kraemer
6. S. Holmström
7. P. Dennis
8. Engy Ahmed

Citations in the corpus

• Release of plant-borne flavonoids into the rhizosphere and their role in plant nutrition (2010, background): “Strategy I is carried out by all higher plants, exceptGramineae, and involves physiological changes, such as increased excretion of protons (Bienfait 1985; Guerinot and Ying 1994; see Ma 2005 as review) and organic compounds (Marschner 1995), enhanced Fe (III)-reducing capacity mainly dependent on a”
• Metallophores and Trace Metal Biogeochemistry (2015, background): “2005; Vraspir and Butler 2009), agronomy (Kraemer et al. 2006), environmental science (Kraemer 2004), and medicine (Hider and Kong 2010).”
• Rhizospheric organic compounds in the soil–microorganism–plant system: their role in iron availability (2014, background): “These latter complexes, in order to be exploited by plants, must have a sufficiently large redox potential for enzymatic reduction (Strategy I) or a sufficiently small thermodynamic stability to undergo ligand-exchange reactions with PSs (Strategy II) (Kraemer et al., 2006; Figures 1, 2).”
• Chapter 4 Iron Dynamics in the Rhizosphere: Consequences for Plant Health and Nutrition (2008, background): “Such competition of metals for phytosiderophores is less likely to occur in the case of microbial siderophores, which generally show a greater specificity for ferric iron and a much higher stability constant than for other metal cations (Kraemer et al., 2006; Parker et al., 2005).”
• Root exudation of sugars, amino acids, and organic acids by maize as affected by nitrogen, phosphorus, potassium, and iron deficiency (2011, background): “, 1997) or indirectly by the formation of labile FeIII complexes with organic acids that facilitate subsequent ligand exchange (Kraemer et al., 2006).”
• Iron dynamics in the rhizosphere as a case study for analyzing interactions between soils, plants and microbes (2009, background): “An important factor controlling iron availability is the solubility (Lindsay 1979) and dissolution rates (Kraemer et al. 2006) of pedogenic Fe(III)oxides, 514 Plant Soil (2009) 321:513–535”
• Siderophores in environmental research: roles and applications (2014, background): “barley and wheat) have developed an efficient strategy for acquiring Fe from insoluble sources (Kraemer et al., 2006).”