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Source: Peer-reviewedNature Communications1 source

As One Pacific Coast Turned More Acidic, Its Plankton Thinned Out

Environment

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A wind-bent conifer on a dark headland in front of a smooth blue expanse of water, with a flat-topped island on the horizon at twilight.
A wind-bent conifer frames the strait from the mainland headland, with the study site low on the horizon (illustrative)."Cape Flattery Lighthouse, Tatoosh Island (Neah Bay, Washington)" by @CarShowShooter, via flickr, BY-NC-SA · CC-BY-NC-SA-2.0

Writing in Nature Communications on Oct. 22, 2026, a University of Chicago team reports that seawater off a Washington island has turned steadily more acidic over 24 years, and that dissolved silicon and the chlorophyll marking plankton growth fell across the same record.

The study is a field test of something seen mostly in tanks: as seawater acidifies, the glassy shells of dead algae dissolve more slowly, so less silicon returns for the next generation to build with. Diatoms, the single-celled algae that make those shells, supply about 40% of the ocean's primary production, the growth at the base of its food webs. Models had put this kind of loss near the end of the century; the authors read their record as showing it already underway in some productive waters.

Scientific figure in five panels: a time series of pH, the dissolved silicon to nitrogen ratio and chlorophyll all declining across 24 years at Tatoosh Island, with two scatter plots showing pH against silicon to nitrogen and silicon to nitrogen against chlorophyll.
Annual averages at Tatoosh Island, Washington, over the 24-year record: pH, the dissolved silicon-to-nitrogen ratio and chlorophyll all fall (A), and the three track one another (B and C). Fig. 2 from J. Timothy Wootton, Madeleine O. Tanda, E. Maximilliana Bogan, Leo C. Gaskins, Anna M. Wootton, Catherine A. Pfister (2026), "Ocean acidification, reduced silicate availability and declines in Ocean productivity", Nature Communications — CC BY-NC-ND 4.0, resized

The measurements come from Tatoosh Island, in the Makah Tribal Nation off northwest Washington, where water samples and half-hourly instrument readings have been collected throughout. J. Timothy Wootton, Catherine A. Pfister and colleagues report that pH there fell by 0.027 units a year, that the dissolved silicon-to-nitrogen ratio they track fell 56%, and that chlorophyll fell 92%. They describe that pH slide as far faster than equilibrium with the rising atmosphere would produce, and treat the site as an early window on wider ocean change. The three declines move together across the years, an association in one coastline's record rather than a controlled experiment.

Conceptual diagram with arrows linking atmospheric carbon dioxide, dissolved carbon dioxide and carbonic acid in seawater, silica weathering and sedimentation, and diatom production, with three labeled competing hypotheses.
The mechanism the team set out to test: dissolved carbon dioxide lowers pH, which can slow silica recycling and leave diatoms short of the silicon they build their shells from. Fig. 1 from J. Timothy Wootton, Madeleine O. Tanda, E. Maximilliana Bogan, Leo C. Gaskins, Anna M. Wootton, Catherine A. Pfister (2026), "Ocean acidification, reduced silicate availability and declines in Ocean productivity", Nature Communications — CC BY-NC-ND 4.0, resized

The team also checked other drivers: surface salinity fell by 0.89 parts per thousand but showed no significant tie to the silicon ratio, a standard coastal upwelling index showed no trend, and flow in the nearest gauged rivers did not change. Nitrogen and phosphate held steady. With upwelling, salinity and river flow statistically removed, both relationships held, and a model weighing the competing drivers assigns most of the silicon change to the falling pH.

Catch records from NOAA Fisheries for Pacific herring, a plankton-feeding fish, decline across the same years. The nutrient data are posted on the National Science Foundation's BCO-DMO repository and the instrument records on figshare.

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By Oli KotykManaging Editor, Writer

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As One Pacific Coast Turned More Acidic, Its Plankton Thinned Out

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