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Introduction Phytoplankton photosynthesis accounts for nearly half of the earth’s primary productivity. However, in the oligotrophic ocean gyres, their growth is constrained by limited amounts of bioavailable nitrogen (N) (Behrenfeld et al., 2006).
Abstract Nickel is a biologically essential element for marine life, with the potential to influence diverse processes, including methanogenesis, nitrogen uptake and coral health, in both modern and past oceans. However, an incomplete view of oceanic Ni cycling has stymied understanding of how Ni may impact marine life in these modern and ancient oceans.
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