The case for ocean iron fertilization field trials

Solving the climate-ocean crisis requires both cutting emissions and pursuing carbon dioxide removal (CDR). Past ocean iron fertilization (OIF) experiments in some parts of the ocean have shown that small additions of iron can enhance phytoplankton growth and CO 2 drawdown. However, prior experiments did not assess the efficacy, durability, or feasibility of OIF for CDR, and broader ecological and biogeochemical responses were not evaluated given the short duration and limited spatial scales. The next generation of OIF field trials must be larger (ca. 1000 km 2 ) and longer (>3–6 months) to observe the full response and return to baseline conditions. Potential risks will be assessed, while using community engagement and co-design to create go/no-go decision points. Planning and extrapolating impacts on regional and global scales will require modeling, with the overall goal to provide unbiased assessments and open-source protocols that can guide responsible and rigorous decision-making for any further OIF.

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Publication Details

Journal
Dialogues on climate change.
Published
2026-02-04
DOI
https://doi.org/10.1177/29768659261420631
Citations
1
Primary Topic
Marine and coastal ecosystems
Type
article
Field-Weighted Citation Impact
28.32
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article

The case for ocean iron fertilization field trials

Angelicque White, Kilaparti Ramakrishna, Margaret Estapa, Dennis J. McGillicuddy et al.
1 citations
Dialogues on climate change.
Marine and coastal ecosystems
28.32
article

The case for ocean iron fertilization field trials

Angelicque White, Kilaparti Ramakrishna, Margaret Estapa, Dennis J. McGillicuddy, Melissa Omand, David M. Karl, Katherine M. Roche, Jay Thomas Cullen, Daniele Bianchi, Christine Klaas, Jun Nishioka, Sarah R. Smith, Mark B. Wells, Dou Li, Zihua Liu, Joo-Eun Yoon, Wil Burns, Seth John, Ken O. Buesseler, Fei Chai, Peng Xiu, Paul J. Morris, Makio Honda, David A. Siegel
article en
1 citations

Abstract

Solving the climate-ocean crisis requires both cutting emissions and pursuing carbon dioxide removal (CDR). Past ocean iron fertilization (OIF) experiments in some parts of the ocean have shown that small additions of iron can enhance phytoplankton growth and CO 2 drawdown. However, prior experiments did not assess the efficacy, durability, or feasibility of OIF for CDR, and broader ecological and biogeochemical responses were not evaluated given the short duration and limited spatial scales. The next generation of OIF field trials must be larger (ca. 1000 km 2 ) and longer (>3–6 months) to observe the full response and return to baseline conditions. Potential risks will be assessed, while using community engagement and co-design to create go/no-go decision points. Planning and extrapolating impacts on regional and global scales will require modeling, with the overall goal to provide unbiased assessments and open-source protocols that can guide responsible and rigorous decision-making for any further OIF.

Dialogues on climate change.
University of Southern California (US), University of Hawaiʻi at Mānoa (US), Japan Agency for Marine-Earth Science and Technology (JP), University of California, Santa Barbara (US), University of California, Los Angeles (US), University of Rhode Island (US), American University (US), Xiamen University (CN), Hokkaido University (JP), University of Victoria (CA), Bigelow Laboratory for Ocean Sciences (US), California Southern University (US), Korea Polar Research Institute (KR), San Jose State University (US), Woods Hole Oceanographic Institution (US), University of Maine (US)
Openalex Percentile: Top 1%
Marine and coastal ecosystems
28.32
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