Deep-sea archives that include intermediate-lived radioactive ⁶⁰Fe particles suggest the occurrence of several recent supernovae inside the present-day volume of the Local Bubble during the last ~ 10 Myr. The isotope ⁶⁰Fe is mainly produced in massive stars and ejected in supernova explosions, which should always result in a sizeable yield of ²⁶Al from the same objects. ⁶⁰Fe and ²⁶Al decay with lifetimes of 3.82 and 1.05 Myr, and emit γ-rays at 1332 and 1809 keV, respectively. These γ-rays have been measured as diffuse glow of the Milky Way, and would also be expected from inside the Local Bubble as foreground emission. Based on two scenarios, one employing a geometrical model and the other state-of-the-art hydrodynamics simulations, we estimate the expected fluxes of the 1332 and 1809 keV γ-ray lines, as well as the resulting 511 keV line from positron annihilation due to the ²⁶Al β⁺-decay. We find fluxes in the range of 10⁻⁶-10⁻⁵\,ph\,cm⁻²\,s⁻¹ for all three lines with isotropic contributions of 10-50%. We show that these fluxes are within reach for the upcoming COSI-SMEX γ-ray telescope over its nominal satellite mission duration of 2 yr. Given the Local Bubble models considered, we conclude that in the case of 10-20 Myr-old superbubbles, the distributions of ⁶⁰Fe and ²⁶Al are not co-spatial - an assumption usually made in γ-ray data analyses. In fact, this should be taken into account however when analysing individual nearby targets for their ⁶⁰Fe to ²⁶Al flux ratio as this gauges the stellar evolution models and the age of the superbubbles. A flux ratio measured for the Local Bubble could further constrain models of ⁶⁰Fe deposition on Earth and its moon.
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