Because of the rise in atmospheric oxygen 2.3 billion years ago (Gya) and the subsequent changes in oceanic redox state over the last 2.3-1 Gya, trace metal bioavailability in marine environments has changed dramatically. Although theorized to have influenced the biological usage of metals leaving discernable genomic signals, a thorough and quantitative test of this hypothesis has been lacking. Using structural bioinformatics and whole-genome sequences, the Fe-, Zn-, Mn-, and Co-binding metallomes of 23 Archaea, 233 Bacteria, and 57 Eukarya were constructed. These metallomes reveal that the overall abundances of these metalbinding structures scale to proteome size as power laws with a unique set of slopes for each Superkingdom of Life. The differences in the power describing the abundances of Fe-, Mn-, Zn-, and Co-binding proteins in the proteomes of Prokaryotes and Eukaryotes are similar to the theorized changes in the abundances of these metals after the oxygenation of oceanic deep waters. This phenomenon suggests that Prokarya and Eukarya evolved in anoxic and oxic environments, respectively, a hypothesis further supported by structures and functions of Fe-binding proteins in each Superkingdom. Also observed is a proliferation in the diversity of Zn-binding protein structures involved in protein-DNA and protein-protein interactions within Eukarya, an event unlikely to occur in either an anoxic or euxinic environment where Zn concentrations would be vanishingly low. We hypothesize that these conserved trends are proteomic imprints of changes in trace metal bioavailability in the ancient ocean that highlight a major evolutionary shift in biological trace metal usage.bioinorganic chemistry ͉ evolution ͉ fold families ͉ structural bioinformatics T he emergence of oxygenic photosynthesis is associated with major changes in global biogeochemistry and metabolism (1, 2). In particular, the rise in atmospheric oxygen Ϸ2.3 billion years ago (Gya) (3, 4) potentially led to the oxygenation of the entire ocean (5), whereas an alternative theory proposes that the deep ocean became euxinic (anoxic and sulfidic) Ϸ1.8 Gya (6, 7), before an oxygenation of deep waters Ϸ1 Gya (8). Putting aside for now when and where, these changes in the overall redox state of the ocean would dramatically influence trace metal chemistry and bioavailability, with an anoxic ocean being characterized by relatively high Fe, Mn, and Co but low Zn concentrations (9) (Fig. 4, which is published as supporting information on the PNAS web site). A euxinic ocean would have comparatively lower concentrations of all of these metals, particularly Zn (9) (Fig. 4). The oxygenation of oceanic deep waters would have dramatically increased Zn concentrations, with concomitant yet less severe decreases in Fe, Mn, and Co levels (9) (Fig. 4). As postulated by Williams and Frausto da Silva (10), these drastic shifts in metal bioavailability theoretically influenced the selection of trace elements for biological usage, leaving a record within the genomes and proteomes ...