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Skilful projection of the impacts of global changes on marine systems depends on better representation of the mechanisms that link processes across scales from the sub-microscopic to the oceanic. The diversity, complexity and range of scales over which the life histories of bacteria, primary producers and animals play out in the oceans makes this is a daunting challenge. However, a recent paper on the increasing abundance of picocyanobacteria in NE Atlantic shelf waters in summer (Schmidt et al. 202 provides an example of our ability
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