Anthropogenic iron alters the spring phytoplankton bloom in the North Pacific transition zone

Industrial activities have increased the supply of iron to the ocean, but the magnitude of anthropogenic input and its ecological consequences are not well-constrained by observations. Across four expeditions to the North Pacific transition zone, we document a repeated supply of isotopically light iron from an atmospheric source in spring, reflecting an estimated 39 ± 9 % anthropogenic contribution to the surface ocean iron budget. Expression of iron-stress genes in metatranscriptomes, and evidence for colimitation of ecosystem productivity by iron and nitrogen, indicates that enhanced iron supply should spur spring phytoplankton blooms, accelerating the seasonal drawdown of nitrate delivered by winter mixing. This effect is consistent with regional trends in satellite ocean color, which show a shorter, more intense spring bloom period, followed by an earlier arrival of oligotrophic conditions in summer. Continued iron emissions may contribute to poleward shifts in transitional marine ecosystems, compounding the anticipated impacts from ocean warming and stratification.

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Publication Details

Journal
Proceedings of the National Academy of Sciences
Published
2025-06-02
DOI
https://doi.org/10.1073/pnas.2418201122
Citations
5
Primary Topic
Marine and coastal ecosystems
Type
article
Field-Weighted Citation Impact
8.97

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article

Anthropogenic iron alters the spring phytoplankton bloom in the North Pacific transition zone

Nathan T. Lanning, Angelicque White, Rhea K. Foreman, Tim M. Conway et al.
5 citations
Proceedings of the National Academy of Sciences
Marine and coastal ecosystems
8.97
article

Anthropogenic iron alters the spring phytoplankton bloom in the North Pacific transition zone

Nathan T. Lanning, Angelicque White, Rhea K. Foreman, Tim M. Conway, Nicholas J. Hawco, Sacha Coesel, Jessica N. Fitzsimmons, Benedetto Barone, James G. Allen, David M. Karl, Daniela König, Paulina Pinedo‐González, Randelle M. Bundy, L. W. Juranek, Emily Seelen, Ryan D. Groussman, Xiaopeng Bian, Seth G. John, Shun‐Chung Yang, E. Virginia Armbrust, Matthias Sieber
article en
5 citations

Abstract

Industrial activities have increased the supply of iron to the ocean, but the magnitude of anthropogenic input and its ecological consequences are not well-constrained by observations. Across four expeditions to the North Pacific transition zone, we document a repeated supply of isotopically light iron from an atmospheric source in spring, reflecting an estimated 39 ± 9 % anthropogenic contribution to the surface ocean iron budget. Expression of iron-stress genes in metatranscriptomes, and evidence for colimitation of ecosystem productivity by iron and nitrogen, indicates that enhanced iron supply should spur spring phytoplankton blooms, accelerating the seasonal drawdown of nitrate delivered by winter mixing. This effect is consistent with regional trends in satellite ocean color, which show a shorter, more intense spring bloom period, followed by an earlier arrival of oligotrophic conditions in summer. Continued iron emissions may contribute to poleward shifts in transitional marine ecosystems, compounding the anticipated impacts from ocean warming and stratification.

Proceedings of the National Academy of SciencesVol. 122(23)
University of Southern California (US), University of Hawaiʻi at Mānoa (US), Statewide California Earthquake Center (US), Oregon State University (US), University of Alaska Fairbanks (US), University of Washington (US), University of South Florida (US), University of South Florida St. Petersburg (US), College of Marin (US), Texas A&M University (US)
National Science Foundation, Simons Foundation
Life below water
Openalex Percentile: Top 2%
Marine and coastal ecosystems
8.97
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