δ18O · Measure of the deviation in the ratio of stable isotopes oxygen-18 and oxygen-16

δ¹⁸O

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Measure of the deviation in the ratio of stable isotopes oxygen-18 and oxygen-16

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The GISP2 δ18O Climate Record of the Past 16,500 Years and the Role of the Sun, Ocean, and Volcanoes

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Early (≥4.5 Ga) formation of terrestrial crust: Lu–Hf, δ18O, and Ti thermometry results for Hadean zircons

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In geochemistry, paleoclimatology and paleoceanography δ18O or delta-O-18 is a measure of the deviation in ratio of stable isotopes oxygen-18 (18O) and oxygen-16 (16O).

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Oxygen-18

Oxygen-16

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