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Matthieu Bressac and Cécile Guieu Post-depositional processes: What really happens to new atmospheric iron in the ocean's surface? Global Biogeochemical Cycles 27

Version of Record online: 30 AUG 2013 | DOI: 10.1002/gbc.20076

Key Points

  • Atmospheric iron dissolution is driven by the dissolved organic matter pool
  • Seawater biogeochemical conditions are a key determinant of iron solubility
  • Lithogenic carbon pump is likely a major pathway for organic carbon export

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