In 1947, in his classical paper on the thermodynamic properties of isotopic substances, H. C. Urey [1] laid the foundation of modern isotope geochemistry. At the same time, A. O. Nier [2] designed a new mass spectrometer which allowed the measurement of small differences in isotope abundance ratios. A modification in the Nier-type mass spectrometer and a refinement in instrumentation techniques by McKinney et al. [3] finally initiated stable isotope studies of the type that will be discussed in this review.
CITATION STYLE
Degens, E. T. (1969). Biogeochemistry of Stable Carbon Isotopes. In Organic Geochemistry (pp. 304–329). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-87734-6_14
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