“…This finding is confirmed by a thorough investigation of the Talos Dome ice core (TALDICE, East Antarctica), where jarosite is found below 1000 m deep and interpreted as the result of acidic, water-limited weathering of dust (Baccolo et al, 2021). Since Fe biogeochemistry is strongly coupled with the global carbon cycle, this element receives considerable attention from the ice core community (Wolff et al, 2006;Conway et al, 2015;Hooper et al, 2019), and methods have been developed to measure its concentration and speciation (Spolaor et al, 2013;Burgay et al, 2019). Nevertheless, the effects of post-depositional processes in ice cores on its geochemistry are still poorly investigated.…”