More VRML Chelates
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Mugineic acid is an amino acid excreted by some graminaceous (grassy) plants under
conditions of iron deficiency as part of a strategy of solubilizing Fe from the root
environment for uptake by the plant. Mugineic acid is closely related to its
biochemical precursor,
nicotinamine, and to a number of other compounds that also have been identified as
phytosiderophores in graminaceous plants: 3-hydroxymugineic acid, 2'-deoxymugineic acid, avenic acid,
and distichonic acid.
The binding coordinating groups are two amine-N, two
carboxylate-O, and one a-hydroxycarboxylate site (two O), a total of 2 N's
and 4 O's, forming a tight octahedron in which the central Fe(III) atom resides.
CPK Color Key: gray, carbon; red, oxygen; blue, nitrogen; purple, iron. Hydrogen
atoms have been removed for clarity.
The effectiveness of mugineic acid under iron-deficient conditions is dependent not only upon
the iron chelating properties of the Fe-mugineic acid complex itself but also upon the presence of a
plant membrane carrier that recognizes and absorbs the Fe-mugineic acid complex almost exclusively.
Further reading:
Ma, JF, and K Nomoto. 1996. Effective regulation of iron
acquisition in graminaceous plants. The role of mugineic acids as phytosiderophores.
Physiol. Plant. 97:609-617.
Mino, Y, et al. 1983. Mugineic acid-iron(III) complex and its structurally
analogous cobalt(III) complex: Characterization and implication for absorption and transport of iron
in graminaceous plants. J. Am. Chem. Soc. 105:4671-4676. [crystal structure]
Phillip Barak
(pwbarak@facstaff.wisc.edu),
Dept. of Soil Science,
University of Wisconsin-Madison. All rights reserved to author.
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Last modified (NoFrame version) 28 July 1997.