M. Shenker et al., CHEMICAL-STRUCTURE AND BIOLOGICAL-ACTIVITY OF A SIDEROPHORE PRODUCED BY RHIZOPUS-ARRHIZUS, Soil Science Society of America journal, 59(3), 1995, pp. 837-843
Rhizopus arrhizus grown on low-Fe medium produces a siderophore, the c
hemical structure of which was determined by means of H-1 nuclear magn
etic resonance (NMR), C-13 NMR, and circular dichroism spectroscopy. T
he siderophore was identified as (1-oxo-3-hydroxy-3,4-dicarboxybutyl)-
diaminobutane chemically identical to rhizoferrin produced by Rhizopus
microsporus. Growth promotion of R. arrhizus by several unferrated ch
elates in Fe-limited medium was studied in microtitration plates. The
impact of rhizoferrin was much more pronounced than the effect of othe
r siderophores. This growth promotion was used as a bioassay for the d
etection of rhizoferrin. Purified Fe-rhizoferrin was found to be a ver
y efficient Fe source for tomato plants [Lycopersicon lycopersicon (L.
) Karsten] in nutrient solutions. Uptake and translocation of Fe-55 me
diated by rhizoferrin in a short-term (10-h) experiment were at levels
higher than those obtained by other microbial siderophores. Iron-rhiz
oferrin acted similarly to the synthetic chelate FeEDDHA [ethylenediam
ine di(o-hydroxyphenylacetic acid)] on remedy of chlorosis in a long-t
erm (14-d) experiment.