Possible Implications of Relatively High Levels of Initial $^{60}$Fe in Iron Meteorites for the Non-Carbonaceous -- Carbonaceous Meteorite Dichotomy and Solar Nebula Formation
Alan P. Boss

TL;DR
This paper explores how high initial levels of $^{60}$Fe in iron meteorites suggest a supernova injection into the early solar system, potentially explaining the meteorite compositional dichotomy and solar nebula formation processes.
Contribution
It proposes a supernova-triggered collapse model that accounts for elevated $^{60}$Fe levels and the non-carbonaceous -- carbonaceous meteorite dichotomy in the solar nebula.
Findings
Supernova injection explains high $^{60}$Fe levels in meteorites.
Hydrodynamical models support shock-triggered collapse of presolar cloud.
Protostar/disk system encounters distant molecular cloud regions within 1 Myr.
Abstract
Cook et al. (2021) found that iron meteorites have an initial abundance ratio of the short-lived isotope Fe to the stable isotope Fe of Fe/Fe . This appears to require the injection of live Fe from a Type II supernova (SN II) into the presolar molecular cloud core, as the observed ratio is over a factor of ten times higher than would be expected to be found in the ambient interstellar medium (ISM) as a result of galactic chemical evolution. The supernova triggering and injection scenario offers a ready explanation for an elevated initial Fe level, and in addition provides a physical mechanism for explaining the non-carbonaceous -- carbonaceous (NC-CC) dichotomy of meteorites. The NC-CC scenario hypothesizes the solar nebula first accreted material that was enriched in supernova-derived nuclides, and then…
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Taxonomy
TopicsAstro and Planetary Science · Astrophysics and Star Formation Studies · Gamma-ray bursts and supernovae
