Oxygen isotope anomalies of the sun and the original environment of the solar system

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Abstract

We present results from a model of oxygen isotopic anomaly production through selective photodissociation of CO within the collapsing proto-solar cloud. Our model produces a proto-Sun with a wide range of Δ17O values depending on the intensity of the ultraviolet radiation field. Dramatically different results from two recent solar wind oxygen isotope measurements indicate that a variety of compositions remain possible for the solar oxygen isotope composition. However, constrained by other measurements from comets and meteorites, our models imply the birth of the Sun in a stellar cluster with an enhanced radiation field and are therefore consistent with a supernova source for 60Fe in meteorites. © The Meteoritical Society, 2008.

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Lee, J. E., Bergin, E. A., & Lyons, J. R. (2008). Oxygen isotope anomalies of the sun and the original environment of the solar system. Meteoritics and Planetary Science, 43(8), 1351–1362. https://doi.org/10.1111/j.1945-5100.2008.tb00702.x

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