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Two types of Fractionation: Kinetic and Equilibrium

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Hydrogen V-SMOW standard mean ocean water. Carbon V-PDB Pee Dee belemnite ... Jeffrey F. Kelly, , Viorel Atudorei, Zachary D. Sharp and Deborah M. Finch ... – PowerPoint PPT presentation

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Title: Two types of Fractionation: Kinetic and Equilibrium


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Two types of Fractionation Kinetic and
Equilibrium
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How it's done!
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EXAMPLE OF CO2
Mass Isotopomer 44 12C16O16O 45 13C16
O16O 12C17O16O 12C16O17O 46 13C17O16O
13C16O17O 12C17O17O 12C18O16O
12C16O18O
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The delta notation (not del)
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Alpha a
C18O H216O C16O H218O
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Example of calcite
CaCO3 phosphoric acid ? CO2 H2O
dissolved calcium phosphate
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THERMOMETRY
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Standards
Hydrogen V-SMOW standard mean ocean
water Carbon V-PDB Pee Dee belemnite Nitrogen A
ir air Oxygen V-SMOW, V-PDB Sulfur CDT
(V-CTD?) Cañon Diablo troilite
d18OSMOW 1.03091 d18OPDB 30.91
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Applications
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METEORIC WATER
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Altitude Effect
Seasonal Effect
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Hydrogen Isotope Contours of Meteoric Water
Sheppard et al., 1979
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Migration Studies Birds, for example
Insights into Wilson's Warbler migration from
analyses of hydrogen stable-isotope
ratios Jeffrey F. Kelly, , Viorel Atudorei,
Zachary D. Sharp and Deborah M. Finch
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White Crowned Sparrows
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Wilsons Warblers
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Positive correlation between migration and dD
value
The warblers from the north arrive first
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Winter breeding latitude vs dD value. Positive
correlation indicates that there is a leapfrog
migration
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Conclusions
  • The dD values of Wilson Warblers can be used to
    determine the approximate latitude where they
    molt.
  • Wilson Warblers from the North arrive in New
    Mexico before those from the South
  • The warblers arriving from the north also fly the
    farthest south. They leapfrog their southern
    neighbors
  • To obtain this information from tagging would
    have been extremely difficult. Using stable
    isotopes, every bird gives information

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Proportion of hydrogen incorporated from body
water
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Preliminary Conclusions
  • Only a small fraction of hydrogen incorporated in
    proteins comes from water. The rest is from
    reorganized proteins.
  • The dD value of protein in hair is close to that
    of the drinking water, suggesting that the
    fractionation is low, and/or the dD value of my
    food is different from the water so that the
    fractionation effect exactly cancels out.
  • It takes about 10 days for body water to exchange
    its hydrogen isotopes
  • Hair has a 8 day delay from body water

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Oxygen isotope study of fossil horse teeth,
paleoclimate info.
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Partial Conclusions
  • The d18O values of biogenic phosphate can be used
    for paleoclimate work
  • The tape recorder growth of horse teeth allows
    for them to be used for determining seasonal
    temperature variations in the distant past.
  • In Texas, the climate was the same 8 million
    years ago as it is today

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Carbon Isotopes in Plants
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Evidence for a change in climate 8 million years
ago
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Lake Greifen, Switzerland, showing effect of
biological pump grey is winter profile
After McKenzie (1985)
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Kangaroo Rats do not change betweeen years
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  • We can use carnivores and herbivores to assess
    relative humidity in the distant past
  • We can estimate what was the diet of a poorly
    understood animal

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