“…Excess ultraviolet-B radiation (UV-B, ultraviolet, 280-315 nm) is known to induce a stress response in plants and has effects on the biosphere at the level of genes, species, and ecosystems (Neale et al, 2021). Although the Montreal Protocol has been successful in both reducing the abundance of ozone-depleting substances in the atmosphere and allowing the subsequent recovery of stratospheric ozone (Solomon et al, 2016), there is widespread interest in understanding how variations in atmospheric-ozone concentrations, and the associated changes in UV-B radiation, have affected plant and ecosystem functioning in the geological past (Jardine et al, 2020(Jardine et al, , 2016Lomax et al, 2008;Rozema, Blokker, Mayoral Fuertes, & Broekman, 2009;Rozema et al, 2001;Willis, Bennett, & Birks, 2009). Yet despite the fact that UV-B is an essential variable for understanding dynamics of the Earth system, quantitative reconstructions of UV-B radiation beyond the instrumental record have remained elusive.…”