First published online August 25, 2003
Waterborne iron acquisition by a freshwater teleost fish, zebrafish Danio rerio
Nicolas R. Bury1,2,* and
Martin Grosell1,
1 Zoophysiological Laboratory, The August Krogh Institute, University of
Copenhagen, Denmark
2 King's College London, School of Health and Life Sciences, Franklin
Wilkins Building, 150 Stamford Street, London, SE1 9NN, UK

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Fig. 1. Temporal pattern of gill (filled circles) and body (open circles) iron
accumulation when iron is presented at 16.5 nmol l-1 in the form of
59FeCl3. Values are means ± S.E.M.,
N=10-16. *Significant differences between the gill iron counts and
uptake into the body (P<0.05; ANOVA followed by
a least-significance difference test). The inset illustrates the relative
contributions that the gills and body make to the total 59Fe
accumulation during the exposure period.
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Fig. 2. Concentration-dependent iron accumulation in (A) the gills and (B) body of
zebrafish in the absence (filled circles) and presence of 2 µmol
l-1 DTT (open circles). Values are means ±
S.E.M., N=10-32. Iron uptake into the gills in the absence
of DTT at [Fe]<40 nmol l-1 showed Michaelis-Menten kinetics.
Above [Fe]=40 nmol l-1 the branchial iron uptake was linear. The
pattern of concentration-dependent branchial gill Fe accumulation in the
presence of DTT best fitted a linear regression (see text).
Concentration-dependent iron accumulation in the body of the zebrafish in the
absence and presence of DTT followed a sigmoidal uptake pattern.
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Fig. 3. The effects of various divalent cations (Co2+, Ni2+,
Pb2+, Cu2+, Cd2+, Zn2+,
Mn2+) on iron uptake into the gills (filled bars) and body (open
bars) of zebrafish in the absence (A) and presence (B) of 2 µmol
l-1 DTT. The iron concentration was 18.6 nmol l-1 and
nominal metal concentrations 200 nmol l-1. Values are means
± S.E.M., N=10-18. *Significant reduction in iron
uptake; significant induction in iron uptake compared to
control fish (Con) (P<0.05; Student t-test, using
untransformed data).
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Fig. 4. Whole body depuration pattern of 59Fe in zebrafish over a 28-day
period. Fish were loaded for 24 h in water containing 21 nmol
l-159Fe. These fish were then washed in isotope-free
water and placed into clean water; they were fed every other day. Values are
means ± S.E.M., N=10. The loss kinetics best fitted
a two-component exponential model (Sigma Plot 2001), where
y=75.5(e-2.21t)+10.2(e-0.0525t),
r2=1. The radiotracer biological half-life for the
short-lived component, t1/2=0.31 days, and the long-lived
component, t1/2=13.2 days.
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© The Company of Biologists Ltd 2003