Two attempts to measure the isotopic composition of oxygen in the Sun from particles trapped in lunar soils give very different results. A rethink of why the Solar System is as it is might be required.
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References
Ireland, T. R., Holden, P., Norman, M. D. & Clark, J. Nature 440, 776–778 (2006).
Hashizume, K. & Chaussidon, M. Nature 434, 619–622 (2005).
Clayton, R. N., Grossman, L. & Mayeda, T. K. Science 182, 485–488 (1973).
Thiemens, M. H. & Heidenreich, J. E. III Science 219, 1073–1075 (1983).
Clayton, R. N. Nature 415, 460–461 (2002).
Hashizume, K. et al. Astrophys. J. 600, 480–484 (2004).
Hashizume, K., Marty, B. & Wieler, R. Earth Planet. Sci. Lett. 202, 201–216 (2002).
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Huss, G. When the dust unsettles. Nature 440, 751–752 (2006). https://doi.org/10.1038/440751a
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DOI: https://doi.org/10.1038/440751a
