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Oxygen isotope fractionations between dissolved inorganic carbon

Oxygen isotope fractionations between pure water and solutions of various ions

Oxygen isotope fractionations between various minerals and calcite

Oxygen isotope profiles across a garnet from Tierra del Fuego, Chile, showing general 0.5 c increase in from core to rim. This zoning is

Oxygen isotope ratio in world-wide precipitation vs. monthly average air temperature, showing that for every point on the line in

Oxygen isotope ratio vs. temperature in S. gigantea.

Oxygen isotope ratio vs. time in S. gigantea, measured for each year.

Oxygen isotope ratios in 250 years of S. gigantea ring sequence from

Oxygen isotope ratios in a sequence of German oaks, a.d. 1350-1950 .

Oxygen isotope ratios in C. japonica calibrated for temperature change using temperatures obtained from .

Oxygen isotope ratios in sequential samples from the same modern shell over a 1-year period. Each circle represents one sample samples taken at 0.5 mm intervals. The reverse order of the seasons is based on the growth of the shell from left to right

Oxygen isotope seasonality in Asia. Strong monsoonal precipitation exists in areas where summer precipitation is more negative than winter precipitation .

Oxygen isotope zoning from fossil equid teeth from the Rattlesnake Formation. .

Oxygen isotope-incorporation studies.

Oxygen isotopes in CM and CO chondrite CAIs. .

Oxygen isotopes in CV3 chondrite CAIs. Data in .

Oxygen isotopes in minerals within individual CR chondrite CAIs. Data taken from the much larger data set of Aleon et al reproduced by permission of the Meteoritical Society from Meteorit. Planet. Sci. 2002, 37,

Oxygen isotopic composition of atmospheric species measured to date indicating for these materials the fractionation is better described as anomalous rather than mass independent

Oxygen isotopic composition of limestones and calcitic shells during geologic history. Triangles and circles represent samples with good and poor age assignment, respectively .

Oxygen isotopic composition of product CO2 generated through UV photolysis of CO. The results are plotted in three-oxygen isotope space on a logarithmic scale to accommodate the non-linearity in 8 scale for large 8 values.

Oxygen isotopic composition of silicates formed in the smoke chamber of the Goddard Space Flight Center in a three-isotope plot.

Oxygen isotopic composition of whole-rock chondrites according to group. Plotted are a O vs. 5 0 obtained by the BrFs method most data are obtained in the laboratory of R. Clayton possibly indicating genetic affinities. On this plot, mass-dependent fractionation lines are horizontal. The carbonaceons chondrite anhydrous minerals CCAM

Oxygen isotopic compositions in martian meteorites define a distinct mass fractionation line from that of terrestrial geologic materials. Open circles are mean values of Clayton and Mayeda .

Oxygen isotopic compositions of CAIs in CH chondrites data sources

Oxygen isotopic compositions of chondmles from all classes of chondritic meteorites



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