Abstract
Paleotemperature scales were calculated by H. C. Urey and others in the 1950s to assess past temperatures, and later work using the stable isotopes of oxygen, hydrogen, and carbon employed standards such as Peedee belemnite (PDB) and Standard Mean Ocean Water (SMOW). Subsequently, subjects as diverse as ice volume and paleotemperatures, oceanic ice and sediment cores, Pleistocene/Holocene climatic changes, and isotope chronostratigraphy extending back to the Precambrian were investigated.
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Bowen, R. (2011). Isotopic Paleoclimatology. In: Vértes, A., Nagy, S., Klencsár, Z., Lovas, R.G., Rösch, F. (eds) Handbook of Nuclear Chemistry. Springer, Boston, MA. https://doi.org/10.1007/978-1-4419-0720-2_16
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