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Julie Granger, Maria G. Prokopenko, Calvin W. Mordy and Daniel M. Sigman The proportion of remineralized nitrate on the ice-covered eastern Bering Sea shelf evidenced from the oxygen isotope ratio of nitrate Global Biogeochemical Cycles 27

Article first published online: 24 SEP 2013 | DOI: 10.1002/gbc.20075

Key Points

  • Nitrate 18O/16O ratios decrease shoreward in ice-covered shelf waters
  • Nitrate inshore originates from nitrification in situ
  • Remineralization dominates seasonal nutrient replenishment on much of the shelf

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