“…Oceans cover 70% of the surface of our planet and are home to myriad bacterial species that are responsible for many of Earth’s crucial biogeochemical functions ( 1, 2 ), including fixing carbon and nitrogen, recycling nutrients and dissolved organic matter, and degrading biomass. Surveys of the ocean microbiome over broad spatial and temporal scales have revealed repeatable patterns across seasons ( 3–6 ), latitude ( 7 ), and depth ( 8 ), which have been linked to a variety of environmental factors, including temperature ( 3, 4, 8, 9 ), water mixing ( 10, 11 ), nutrient availability ( 12 ), light ( 13 ), and the occurrence of phytoplankton blooms ( 6 ). Nevertheless, general principles underlying the compositional turnover of vital marine bacterial communities are lacking, impairing our ability to predict the response of ocean systems to future environmental changes.…”