Early Solar System irradiation quantified by linked vanadium and beryllium isotope variations in meteorites
Paolo A. Sossi, Frederic Moynier, Marc Chaussidon, Johan Villeneuve,, Chizu Kato, Matthieu Gounelle

TL;DR
This study uses vanadium and beryllium isotope variations in meteorites to quantify early Solar System irradiation, revealing that refractory dust was irradiated by solar cosmic rays from gradual flares for less than 300 years near the protoSun.
Contribution
It provides the first direct isotopic evidence linking vanadium and beryllium variations to early Solar System irradiation conditions, specifically from gradual solar flares.
Findings
50V excesses up to 4.4 per mil in CAIs co-vary with 10Be abundance
Refractory dust was irradiated by solar cosmic rays for less than 300 years
Irradiation occurred at about 0.1 au from the protoSun
Abstract
X-ray emission in young stellar objects (YSOs) is orders of magnitude more intense than in main sequence stars1,2, suggestive of cosmic ray irradiation of surrounding accretion disks. Protoplanetary disk irradiation has been detected around YSOs by HERSCHEL3. In our solar system, short-lived 10Be (half-life = 1.39 My4), which cannot be produced by stellar nucleosynthesis, was discovered in the oldest solar system solids, the calcium-aluminium-rich inclusions (CAIs)5. The high 10Be abundance, as well as detection of other irradiation tracers6,7, suggest 10Be likely originates from cosmic ray irradiation caused by solar flares8. Nevertheless, the nature of these flares (gradual or impulsive), the target (gas or dust), and the duration and location of irradiation remain unknown. Here we use the vanadium isotopic composition, together with initial 10Be abundance to quantify irradiation…
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