The dissipation of the solar nebula constrained by impacts and core cooling in planetesimals - Nature Astronomy

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The dissipation of the solar nebula constrained by impacts and core cooling in planetesimals - Nature Astronomy
France Dernières Nouvelles,France Actualités
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The chaotic early phase of the solarsystem ETH_en NatureAstronomy

Rapid cooling of planetesimal cores has been inferred for several iron meteorite parent bodies on the basis of metallographic cooling rates, and linked to the loss of their insulating mantles during impacts. However, the timing of these disruptive events is poorly constrained. Here, we used the short-livedAg decay system to date rapid core cooling by determining Pd–Ag ages for iron meteorites. We show that closure times for the iron meteorites equate to cooling in the time frame ~7.8–11.

7 Myr after calcium–aluminium-rich inclusion formation, and that they indicate that an energetic inner Solar System persisted at this time. This probably results from the dissipation of gas in the protoplanetary disk, after which the damping effect of gas drag ceases. An early giant planet instability between 5 and 14 Myr after calcium–aluminium-rich inclusion formation could have reinforced this effect.

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