With the exception of the grasses, plants rely on a reduction-based iron (Fe) uptake system that is compromised by high soil pH, leading to severe chlorosis and reduced yield in crop plants. We recently reported that iron deficiency triggers the production of secondary metabolites that are beneficial for Fe uptake in particular at high external pH when iron is present but not readily available. The exact function of these metabolites, however, remains enigmatic. Here, we speculate on the mechanism by which secondary metabolites secreted by roots from Fe-deficient plants improve Fe acquisition. We suggest that the production and excretion of Iron Binding Compounds (IBCs) constitute an integrative, pH-insensitive component of the reduction-based iron uptake strategy in plants.Although iron (Fe) is generally present in large amounts, in aerobic soils Fe tends to form oxyhydrates of low solubility, in particular at neutral or high pH. When atmospheric oxygen increased as a result of the evolution of photosynthesis, plants were forced to evolve strategies that improve Fe acquisition, which was chiefly achieved by increasing the solubility of immobile Fe pools. All plant species except the grasses have employed a mechanism that includes reduction of ferric chelates, mediated by a plasma membrane-bound oxidoreductase (FRO2 in Arabidopsis). The reduction of Fe(III) weakens the stability of the chelate and the released Fe(II) is taken up by a ZIP family transporter (IRT1).2 A drawback of this strategy is that it works best at a slightly acidic pH and is strongly impaired in soils with high pH.3 This is partly counteracted by induction of a P-type H + -ATPase that provides a favorable pH environment (AHA2).
4Excretion of organic compounds, mainly phenolics or flavins, have been associated with the Fe deficiency response since the early seventies, 5,6 but were later considered to be of minor importance and, with some notable exceptions (e.g., the massive production of riboflavin and riboflavin derivatives by some species), 7,8 were largely neglected in studies related to iron acquisition processes in model species such as Arabidopsis. Nevertheless, the frequent observation of this phenomenon led to speculations on the function of these compounds in Fe acquisition, comprising effects on the microbiome in the rhizosphere, a function (for flavins) in electron transport during the reduction of Fe(III), chelation of Fe, and chemical reduction of Fe(III). The first clear-cut evidence for a function of Fe deficiency-induced root secretions in Fe uptake was provided by Jin et al. showing that phenolics secreted by red clover roots facilitated the acquisition of Fe bound to anionic residues in the apoplast.9 Similarly, transgenic rice plants overexpressing the phenolic efflux transporter PEZ1 grew better on soils with high pH and poor Fe solubility.10 In Arabidopsis, robust induction of the phenylpropanoid pathway, both at the transcript and protein levels, 11,12 indicating that in roots of Fe-deficient plants phenolic compounds ar...