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The Costa Rica Dome (CRD) is a wind‐driven upwelling feature in the eastern tropical Pacific that supports unusually high concentrations (> 10 6 cells mL −1 ) of the picocyanobacteria Prochlorococcus and Synechococcus . To understand what causes this unusual phytoplankton bloom, we conducted a comprehensive survey of the hydrography, picophytoplankton population structure, and trace metal chemistry of the CRD and surrounding o...
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