Iron toxicity is a major constraint to rice production, particularly in
highly-weathered soils of inland valleys in sub-Saharan Africa where the
rice area is rapidly expanding. Although there is wide variation in
tolerance in the rice germplasm, progress in introgressing tolerance
traits into high-yielding germplasm has been slow owing to the
complexity of tolerance mechanisms and large genotype by environment
effects. We review current understanding of tolerance mechanisms,
particularly those involving below-ground plant-soil interactions, which
to date have been less studied than above-ground mechanisms. We cover
processes in the rhizosphere linked to exclusion of toxic ferrous iron
by oxidation, and resulting effects on the mobility of nutrient ions. We
also cover the molecular physiology of below-ground processes
controlling Fe retention in roots and root-shoot transport, and also
plant Fe sensing. We conclude that future breeding programs should be
based on well-characterised molecular markers for tolerance traits. To
successfully identify such markers, the complex tolerance response
should be broken down into its components based on understanding of
tolerance mechanisms, and tailored screening methods developed for
individual mechanisms.