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Better Living through Biochemistry Enhanced Diffusive Flux as a Measure of Bioavailable Aquatic Iron

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Title: Better Living through Biochemistry Enhanced Diffusive Flux as a Measure of Bioavailable Aquatic Iron


1
Better Living Through Biochemistry
Enhanced Diffusive Flux
as a Measure of
Bioavailable Aquatic Iron Concentration
By Brian Gaas
2
On the Menu
  • Project Summary
  • Justification
  • Background
  • Fe chemistry
  • Biological Fe uptake
  • Diffusive flux model
  • Objectives
  • Methods
  • Genetic modification
  • 55Fe uptake
  • Flux calculation
  • Conclusion

D.F.
55Fe
T.w.
3
Project Summary
  • Determination of bioavailable Fe in marine
    systems
  • Based on diffusion rate from medium to cell
    surface as function of concentration gradient

Q (D/l) (Cs Cm)
55Fe uptake
Hydrodynamic modeling
Genetic engineering
The Unknown
  • Just add seawater and voila! Instant
    bioavailable Fe concentrations!

4
Who Ordered This?
  • Iron (Fe) micronutrient, capable of limiting
    community plankton growth in HNLC regions
  • Assays exist to determine total Fe concentration,
    speciation, and potential Fe limitation
  • But, populations can differ in relation to Fe
    quotas
  • To measure the amount of bioavailable Fe,
    irrespective of the Fe demand of the organism, a
    different method must be employed.

5
Place Settings Fe Chemistry
  • Biological, physical and chemical processes all
    affect Fe biogeochemistry and speciation
  • Almost all dissolved Fe is Fe (III)
  • Fe(OH)x at surface ocean pH (8.2) and surface
    temperature (25C)
  • Fe(OH)2 and Fe(OH)30
  • Many confounding factors to determining Fe
    concentration
  • Filter size
  • Oxidation state change
  • Fe hydroxide precipitation Fe(OH)x, Fe(OOH),
    Fe2O3
  • Temperature, pH, light
  • Organic complexes! 99.9 total Fe (III)

6
Marinobactin siderophore (peptide-based)
Hydroxamate siderophore (ferrichrome)
Humic acid
7
Place Settings Biological Use
  • Fe deficiencies and excesses can limit
    phytoplankton growth
  • Not all forms of Fe are available for uptake
  • Fe (III) Fe(OH)x
  • Colloidal iron has no direct biological use
  • Not all Fe is taken up
  • Internal Fe requirement
  • Surface-bound transporters
  • Siderophores
  • Phytotransferrin
  • Michaelis-Menten equation describe Fe uptake
    kinetics

8
Place Settings Flux Model
  • Maximum diffusion 8 mean cell radius
  • QR 4pR2JR 14.4pRD(?C)
  • QR rate of transport to the cell
  • JR nutrient flux at cell surface
  • R mean cell radius
  • D diffusivity constant
  • ?C concentration difference between medium and
    cell surface
  • Non-spherical shape of a centric diatom does not
    change the calculations significantly

9
Genetic engineering of T. weissflogii
Flux-derived Fe values compared to inorganic Fe
measurements
55Fe uptake kinetics
The Master Plan
Field testing
Cm -QR/(14.4pRD) Cs
Mass culturing of evil Super-Plankton for world
domination
Flux calculation for bioavailable Fe
10
Methods and Associated Madness
Part 1 Gene Jockeying
GATTACGCTCTCTAATGAGAGA
11
Methods and Associated Madness
Part 2 Nuke em All!
Section A incubation
24hrs


Low Fe AQUIL
55FeCl3
Modified T. w.
RadQUIL
Culture
Section B kinetics
Liquid scintillation counting


Uptake Rate
Saturation Curve
10min 3hr cell filtration
Ti(III) citrate EDTA
12
Methods and Associated Madness
Part 2, cont Glow-in-the-dark weissflogii?
Section C diffusion differences
L.S.C.


Uptake Rate
Culture
Diffusion ligand
Ti(III) citrate EDTA
Section D non-equilibrium control
L.S.C.


Uptake Rate
Culture
Strong ligand
Ti(III) citrate EDTA
13
Methods and Associated Madness
Part 3 Fluxing flocculations, Batman!
Cm -QR/(14.4pRD) Cs
CM bioavailable Fe concentration QR rate of
transport to the cell (flux) p
3.1415926535897932384626433832795 R mean
cell radius D diffusivity constant Cs
cell surface bioavailable Fe concentration
Unknown
55Fe uptake
Natural constant
Microscope
Literature
Genetically set to zero
14
In Conclusion
  • Fe is an important element with wide-ranging
    effects, especially on oceanic biology
  • Current methodologies do not give a sufficiently
    accurate measure of bioavailable Fe
  • The 55Fe flux approach will be valuable for
    determining Fe limitation, as well as for
    understanding Fe-involved biogeochemical processes

15
To Inquire, or Not to InquireAny Other Questions?
?
16
Youve Gone Too Far!Go Back, Go Back!
17
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