Phytoplankton productivity depends on the replenishment of nutrients in ocean surface waters. An explanation for a region of strikingly low productivity invokes a little-considered aspect of the nutrient cycle.
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References
Palter, J. B., Lozier, M. S. & Barber, R. T. Nature 437, 687–692 ( 2005).
Williams, R. G. & Follows, M. J. in Ocean Biogeochemistry: A JGOFS Synthesis (ed. Fasham, M.) 19–50 (Springer, New York, 2003).
Lévy, M., Lehahn, Y. et al. J. Geophys. Res. 110, doi:10.1029/2004JC002771 ( 2005).
Williams, R. G., Roussenov, V. & Follows, M. J. presented at ASLO Summer Meeting, Santiago de Compostela, 19–24 June 2005; Glob. Biogeochem. Cycles (submitted).
Sarmiento, J. L. et al. Nature 427, 56–60 ( 2004).
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Lévy, M. Nutrients in remote mode. Nature 437, 629–631 (2005). https://doi.org/10.1038/437628a
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DOI: https://doi.org/10.1038/437628a