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Marine phytoplankton and the changing ocean iron cycle

Author

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  • D. A. Hutchins

    (Marine and Environmental Biology Section, University of Southern California)

  • P. W. Boyd

    (Institute for Marine and Antarctic Studies, University of Tasmania)

Abstract

Changes in the ocean affect the biogeochemical cycle of iron, which in turn impacts phytoplankton growth. This Perspective discusses what research is needed to predict the future marine iron cycle.

Suggested Citation

  • D. A. Hutchins & P. W. Boyd, 2016. "Marine phytoplankton and the changing ocean iron cycle," Nature Climate Change, Nature, vol. 6(12), pages 1072-1079, December.
  • Handle: RePEc:nat:natcli:v:6:y:2016:i:12:d:10.1038_nclimate3147
    DOI: 10.1038/nclimate3147
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    Cited by:

    1. Xuelian Xia & Yanguo Teng & Yuanzheng Zhai, 2022. "Biogeochemistry of Iron Enrichment in Groundwater: An Indicator of Environmental Pollution and Its Management," Sustainability, MDPI, vol. 14(12), pages 1-14, June.
    2. Robert H. Lampe & Tyler H. Coale & Kiefer O. Forsch & Loay J. Jabre & Samuel Kekuewa & Erin M. Bertrand & Aleš Horák & Miroslav Oborník & Ariel J. Rabines & Elden Rowland & Hong Zheng & Andreas J. And, 2023. "Short-term acidification promotes diverse iron acquisition and conservation mechanisms in upwelling-associated phytoplankton," Nature Communications, Nature, vol. 14(1), pages 1-19, December.

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