W. Bruggemann et al., IRON UPTAKE BY LEAF MESOPHYLL-CELLS - THE ROLE OF THE PLASMA MEMBRANE-BOUND FERRIC-CHELATE REDUCTASE, Planta, 190(2), 1993, pp. 151-155
The uptake of Fe-59 from FeCl3, ferric (Fe3+) citrate (FeCitr) and Fe3
+-EDTA (FeEDTA) was studied in leaf mesophyll of Vigna unguiculata (L.
) Walp. Uptake rates decreased in the order FeCl3>FeCitr much greater
than FeEDTA, and uptake depended on an obligatory reduction step of Fe
3+ to Fe2+, after which the ion could be taken up independently of the
chelator, citrate. Uptake was strongly increased by photosyntheticall
y active light (lambda > 630 nm), and kinetic analysis revealed satura
tion kinetics with a K(m) (FeCitr) of 80-110 muM. In the presence of a
n external Fe2+ scavenger, bathophenanthroline disulfonate, the mesoph
yll also reduced external FeCitr with a K(m) of approx. 50-60 muM. The
reduction rates for FeCitr were five- to eightfold higher than necess
ary for uptake. Purified plasma membranes from leaves revealed an NADH
-dependent FeCitr- and FeEDTA-reductase activity, which had a pH optim
um of 6.5-6.8 and a K(m) of approx. 20 muM for NADH. Under anaerobic c
onditions, a K(m) of 130-170 muM for ferric chelates was obtained, whi
le in the presence of oxygen a K(m) (FeCitr) of approx. 100 muM was fo
und. It is concluded that the leaf plasma membrane provides a ferric-c
helate-reductase activity, which plays a crucial role in iron uptake o
f leaf cells. Under in-vivo conditions, however, reactive oxygen speci
es or strong (blue) light may also contribute to the obligatory reduct
ion of Fe3+ prior to uptake.