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- W4200436622 abstract "Establishing when, and from where, carbon, nitrogen and water were delivered to Earth is a fundamental objective in understanding the origin of habitable planets such as Earth. Yet, volatile delivery to Earth remains controversial1–5. Krypton isotopes provide insights on volatile delivery owing to their substantial isotopic variations among sources6–10, although pervasive atmospheric contamination has hampered analytical efforts. Here we present the full suite of krypton isotopes from the deep mantle of the Galápagos and Iceland plumes, which have the most primitive helium, neon and tungsten isotopic compositions11–16. Except for 86Kr, the krypton isotopic compositions are similar to a mixture of chondritic and atmospheric krypton. These results suggest early accretion of carbonaceous material by proto-Earth and rule out any combination of hydrodynamic loss with outgassing of the deep or shallow mantle to explain atmospheric noble gases. Unexpectedly, the deep-mantle sources have a deficit in the neutron-rich 86Kr relative to the average composition of carbonaceous meteorites, which suggests a nucleosynthetic anomaly. Although the relative depletion of neutron-rich isotopes on Earth compared with carbonaceous meteorites has been documented for a range of refractory elements1,17,18, our observations suggest such a depletion for a volatile element. This finding indicates that accretion of volatile and refractory elements occurred simultaneously, with krypton recording concomitant accretion of non-solar volatiles from more than one type of material, possibly including outer Solar System planetesimals. The krypton isotopic pattern of Earth’s deep mantle indicates that volatile-rich material from the outer Solar System was delivered early in Earth’s accretion history." @default.
- W4200436622 created "2021-12-31" @default.
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- W4200436622 creator A5082774350 @default.
- W4200436622 date "2021-12-15" @default.
- W4200436622 modified "2023-10-01" @default.
- W4200436622 title "Deep-mantle krypton reveals Earth’s early accretion of carbonaceous matter" @default.
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- W4200436622 doi "https://doi.org/10.1038/s41586-021-04092-z" @default.
- W4200436622 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/34912082" @default.
- W4200436622 hasPublicationYear "2021" @default.
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