“…The existence in the roots of dicotyledonous plants of an obligatory Fe reduction step from Fe(III) to Fe(II) prior to Fe root uptake was demonstrated first by Chaney et al (1972). The reduction of Fe(III) to Fe(II) is carried out by one or several specialized enzyme(s) located in the root cell plasma membrane (PM), the ferric-chelate reductase(s) (FC-R) (Bienfait, 1985(Bienfait, , 1988Cakmak et al, 1987;Rubinstein and Luster, 1993;Moog and Brü ggemann, 1994;Susín et al, 1996;Robinson et al, 1998Robinson et al, , 1999. Dicotyledonous plant species have the so-called strategy I (Marschner, 1995), that includes, among other mechanisms, the development of an increased capacity to reduce Fe.…”