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Away from benthic and aeolian resources, metal hits phytoplankton primarily when iron-rich subsurface oceans enter the euphotic area. Here, eddy-resolving physical/biogeochemical simulations of a seasonally-forced, open-Southern-Ocean ecosystem expose that mesoscale and submesoscale isopycnal stirring effects a cross-mixed-layer-base transport of metal that sustains main productivity. The eddy-driven iron supply and therefore productivity enhance with design resolution. We show the eddy flux co

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