Siderophore
A
Siderophore
(greek for iron carrier) is an
iron
chelating
compound secreted by
microorganisms
. Iron
Fe
3+
ions
have a very low solubility at
neutral
pH
and therefore cannot be utilized by organisms. Siderophores dissolve these ions as soluble
Fe
3+
complexes
that can be taken up by
active transport
mechanisms. Many siderophores are
nonribosomal peptides
. Other strategies to enhance iron solubility and uptake are the
acidification
of the surrounding (e.g. used by plant roots) or the
extracellular
reduction
of
Fe
3+
into the more soluble
Fe
2+
ions. Examples of siderophores produced by various
bacteria
and
fungi
are
ferrichrome
(
Ustilago
sphaerogena
),
enterobactin
(
Escherichia coli
), enterobactin and
bacillibactin
(
Bacillus subtilis
),
ferrioxamine B
(
Streptomyces
pilosus
),
fusarinine C
(
Fusarium
roseum
),
yersiniabactin
(
Yersinia pestis
), vibriobactin (
Vibrio cholerae
), or
pseudobactin
(
Pseudomonas
B 10
).
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