Metabolism mediates the flow of matter and energy through the biosphere. We examined how metabolic evolution shapes ecosystems by reconstructing it in the globally abundant oceanic phytoplankter Prochlorococcus. To understand what drove observed evolutionary patterns, we interpreted them in the context of its population dynamics, growth rate, and light adaptation, and the size and macromolecular and elemental composition of cells. This multilevel view suggests that, over the course of evolution, there was a steady increase in Prochlorococcus' metabolic rate and excretion of organic carbon. We derived a mathematical framework that suggests these adaptations lower the minimal subsistence nutrient concentration of cells, which results in a drawdown of nutrients in oceanic surface waters. This, in turn, increases total ecosystem biomass and promotes the coevolution of all cells in the ecosystem. Additional reconstructions suggest that Prochlorococcus and the dominant cooccurring heterotrophic bacterium SAR11 form a coevolved mutualism that maximizes their collective metabolic rate by recycling organic carbon through complementary excretion and uptake pathways. Moreover, the metabolic codependencies of Prochlorococcus and SAR11 are highly similar to those of chloroplasts and mitochondria within plant cells. These observations lead us to propose a general theory relating metabolic evolution to the self-amplification and selforganization of the biosphere. We discuss the implications of this framework for the evolution of Earth's biogeochemical cycles and the rise of atmospheric oxygen. metabolic evolution | Prochlorococcus | microbial oceanography | mutualism | Earth history M etabolism sustains the nonequilibrium chemical order of the biosphere by continually supplying the energy and building blocks of all cells on Earth (1-5). Here we ask: How does cellular metabolic evolution shape the mass and energy flows of ecosystems? The oceanic phytoplankter Prochlorococcus (6), the most abundant photosynthetic cell on Earth (7,8), provides an ideal model system for addressing this question. Prochlorococcus and its deeper-branching sister lineage marine Synechococcus make up the marine picocyanobacteria and have a characteristic biogeography (9). Prochlorococcus "ecotypes" have geographically (10, 11) and seasonally (12) dynamic populations that in warm, stable stratified water columns always return to the same general structure: Recently diverging highlight-adapted (HL) ecotypes are most abundant toward the surface, whereas deeper branching low-light-adapted (LL) ecotypes are most abundant at depth (10-14) (Fig. 1).What selective forces drove this niche partitioning in Prochlorococcus, and what were the consequences for the ocean ecosystem in general? To address these questions, we reconstructed (15, 16) (Fig. 2) the evolution of core metabolism in strains representing the major clades of Prochlorococcus. To interpret the observed patterns, we developed an evolutionary framework that illuminates the driving forces that produc...