“…The perturbations imposed on the model are designed to assess the sensitivity of marine Se isotope systematics to large departures from baseline Se cycling in the modern ocean. Using the same model across geological time assumes that assimilatory uptake of Se was an important biochemical pathway throughout, and that Se was incorporated into the biochemistry of cells during the emergence and evolution of life, possibly even before S (Hengeveld, 2007;Hengeveld and Fedonkin, 2007;Rao et al, 2003;Romero et al, 2005;Sun and Caetano-Anollés, 2009). Because the modern Se cycle is dominated by assimilatory reduction and oxidative recycling of DISe, we focus on perturbations where (1) assimilatory DISe uptake in the surface waters is decreased (Perturbation 1), (2) oxidative recycling in the water column and sediments is inhibited (Perturbation 2), (3) dissimilatory Se reduction is increased (Perturbation 3), and (4) the previous perturbations are combined (Perturbation 4 = Perturbations 1 + 2 + 3, Perturbation 5 = Perturbations 1 + 2).…”