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Nitrogen and phosphorus differentially control marine biomass production and stoichiometry

Author

Listed:
  • Emily A. Seelen

    (Department of Earth Science
    College of Fisheries and Ocean Sciences)

  • Samantha J. Gleich

    (Department of Biological Sciences)

  • William Kumler

    (School of Oceanography)

  • Hanna S. Anderson

    (Columbia University
    Department of Earth and Environmental Science)

  • Xiaopeng Bian

    (Department of Earth Science)

  • Karin M. Björkman

    (Department of Oceanography)

  • David A. Caron

    (Department of Biological Sciences)

  • Sonya T. Dyhrman

    (Columbia University
    Department of Earth and Environmental Science)

  • Sara Ferrón

    (Department of Oceanography)

  • Zoe V. Finkel

    (Department of Oceanography)

  • Sheean T. Haley

    (Columbia University)

  • Ying-Yu Hu

    (Department of Oceanography)

  • Anitra E. Ingalls

    (School of Oceanography)

  • Andrew J. Irwin

    (Department of Mathematics & Statistics)

  • David M. Karl

    (Department of Oceanography)

  • Kyeong Pil Kong

    (Department of Earth Science)

  • Daniel P. Lowenstein

    (Department of Marine Chemistry and Geochemistry
    WHOI Joint Program in Oceanography/Applied Ocean Science and Engineering)

  • Andrés E. Salazar Estrada

    (Department of Oceanography)

  • Emily Townsend

    (Department of Earth Science)

  • John C. Tracey

    (Columbia University)

  • Kendra Turk-Kubo

    (Ocean Sciences Department)

  • Benjamin A. S. Mooy

    (Department of Marine Chemistry and Geochemistry)

  • Seth G. John

    (Department of Earth Science)

Abstract

Globally averaged, surface particulate nitrogen and phosphorus approximate the 16:1, N:P “Redfield ratio.” In observations, N:P ratios vary latitudinally at ranges attributable to both phytoplankton community composition and physiological acclimation, but their relative contributions to the N:P ratio remain unclear. Here, results from a 29-day mesocosm experiment highlight how inorganic nitrogen and/or phosphorus nutrient supply can affect the bulk particle stoichiometry of a North Pacific Subtropical Gyre plankton community. Nitrogen additions, with and without phosphorus, increase total productivity and diatom abundance, whereas treatments with just phosphorus additions remain similar to the no-nutrient addition control. Continual nitrogen supply without phosphorus results in higher particulate N:P ratios than expected based on the phytoplankton community present. Several P-stress markers identified in those treatments highlight the importance of acclimation in extending particulate N:P ratios beyond the Redfield ratio. Phytoplankton’s ability to maintain growth under P-stress conditions has implications for global carbon cycling.

Suggested Citation

  • Emily A. Seelen & Samantha J. Gleich & William Kumler & Hanna S. Anderson & Xiaopeng Bian & Karin M. Björkman & David A. Caron & Sonya T. Dyhrman & Sara Ferrón & Zoe V. Finkel & Sheean T. Haley & Ying, 2025. "Nitrogen and phosphorus differentially control marine biomass production and stoichiometry," Nature Communications, Nature, vol. 16(1), pages 1-13, December.
  • Handle: RePEc:nat:natcom:v:16:y:2025:i:1:d:10.1038_s41467-025-61061-0
    DOI: 10.1038/s41467-025-61061-0
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    References listed on IDEAS

    as
    1. Michael W. Lomas & Nicholas R. Bates & Rodney J. Johnson & Deborah K. Steinberg & Tatsuro Tanioka, 2022. "Adaptive carbon export response to warming in the Sargasso Sea," Nature Communications, Nature, vol. 13(1), pages 1-10, December.
    2. Thomas S. Weber & Curtis Deutsch, 2010. "Ocean nutrient ratios governed by plankton biogeography," Nature, Nature, vol. 467(7315), pages 550-554, September.
    Full references (including those not matched with items on IDEAS)

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