In 2025, the Potsdam Institute for Climate Impact Research determined that the ocean acidification planetary boundary had been breached for the first time, degrading the ocean’s ability to stabilise the global climate and pushing humanity and marine life beyond the agreed safe zone.
The ocean absorbs at least a quarter of the carbon dioxide released into the atmosphere, driving chemical changes that visibly affect marine life and ocean chemistry. Yet despite decades of research, a fundamental question remains difficult to answer: how exactly is ocean acidification changing marine ecosystems?
The Global Ocean Acidification Observing Network (GOA-ON)’s Biology Working Group has worked for years to demonstrate the real-world biological impacts of ocean acidification. Alongside observations and experience from marine communities, abundant evidence from laboratory experiments shows how different organisms respond to acidification. Coral reefs have eroded, lost biodiversity and become overgrown with algae; acidification is known to make it more difficult and energetically demanding for calcifying organisms, such as corals and shellfish, to grow and maintain their normal structures. What’s missing, however, is substantial long-term, quantifiable data to connect those responses to what is happening to the chemistry of seawater across the entire ocean.

From the lab to the ocean
“We know in theory that ocean acidification affects biological organisms in certain ways,” says Natalija Suhareva, a researcher on the IOC-UNESCO Ocean Acidification Research for Sustainability project. “We know which groups of species are more sensitive to ocean acidification, which are less sensitive, and which could even benefit from ocean acidification, thanks to evidence from experimental work.” But laboratory experiments cannot reproduce the full complexity of the ocean. “Reality is much more complex, so we don’t actually know how it happens in the real world. We only know how it happens in a controlled environment.”
The challenge, therefore, was to find a way of connecting changes in ocean chemistry with changes in marine biology. In 2023, GOA-ON published a framework that proposed a new way of approaching the problem: rather than comparing absolute states, researchers should compare rates of change in carbon chemistry with rates of change in biology. “We saw this as an opportunity to develop a new methodology that shows how these two different metrics correlated with each other,” says Steve Widdicombe, director of the Sharjah Marine Science Research Centre at University of Khorfakkan, UAE, and co-chair of GOA-ON.
The framework identified five biological traits that could be measured: calcification and calcifiers; primary production; heterotrophic secondary production; biodiversity or ecosystem composition; and genetic adaptation. In 2024, the Ocean Acidification - proof of concept for new research strategies project, supported by the Velux Foundation, set out to put that framework into practice. Dr Suhareva and the team began by looking for long-term time series in which biological and chemical observations could be aligned across comparable periods, geographical scales and sampling frequencies.
What they found was a much more serious data gap than expected. In September 2026, the GOA-ON Data Explorer portal contained 799 records of existing time series around the world, but once the researchers had applied filters for duration and frequency of monitoring, carbon chemistry and associated biological measurements, the number fell rapidly. To qualify, datasets needed more than 15 years of carbon chemistry monitoring (excluding the unfinished year of 2026), observations more frequent than once a month and some associated biological data. “Out of nearly 800, fewer than ten records passed all of our filters,” says Dr Suhareva. But incomplete or outdated information in the portal can leave suitable records overlooked, so the findings do not mean that other time series don’t exist. The duration threshold is also a practical screening choice: as monitoring continues, additional records could cross it as early as next year.
Some biological datasets stretched back decades but lacked sufficiently long or consistent carbon chemistry records to accompany them. Other datasets appeared to be long running, but had been sampled too infrequently or inconsistently to provide a reliable time series. “Some claims of longevity were spurious in terms of how often and how consistently they were sampling, making them unreliable,” explains Professor Widdicombe. “The more datasets we examined, the more we had to discard.”

Obstacles to ocean monitoring
The problem is particularly acute in coastal waters, where conditions can vary dramatically over relatively small distances. “Data from the open ocean is very good, but it’s much more complicated in the coastal zone,” says Helen Findlay, biological oceanographer at Plymouth Marine Laboratory and co-lead on the OSPAR Commission’s Ocean Acidification Quality Status Report. Coastal waters are influenced by run-off, rainfall, pollutants and nutrients, as well as highly productive ecosystems such as phytoplankton, kelp forests and seagrasses. Seasonality adds another layer of complexity: whether water is stratified or continually mixing can substantially affect rates of change.
Geology also matters. A river flowing through chalk will interact with seawater differently from one flowing over granite. In regions with olivine-rich geology, freshwater inputs can contribute to much higher alkalinity. “You can see why it's so difficult to model, but you can also see why it’s so important to be location-specific,” says Professor Findlay. “There’s no one correct way of understanding the processes that are going on.” Ocean acidification occurs alongside climate change, marine heatwaves, erosion, pollution and countless other processes, making it difficult to separate the effects of individual stressors.
The challenge is not only to establish new monitoring programmes. Existing ones also need to be preserved for long enough to deliver the necessary data. “Sustained observation projects are under massive pressure,” says Professor Widdicombe. “The UN recognises the value of the Global Ocean Observing System in producing comprehensive measurements, but governments are just not putting enough investment into observing the ocean.”
The consequences can be seen in the data. One of the datasets that passed the project’s filters was the CARIACO Ocean Time Series from Cariaco Basin, Venezuela, where frequent observations provided more than 20 years of biological and chemical data. But the monitoring programme stopped in 2017. “If the programme had continued, we would by now already have 30 years of data, fully equipped with both biology and chemistry,” says Dr Suhareva. “It is a great loss.”

Better data for better decisions
The west coast of North America demonstrates what can happen when there is a direct economic incentive to understand changing ocean conditions. In 2005, shellfisheries began to observe alarming productivity declines linked to ocean acidification; this helped to drive investment in monitoring programmes such as the Pacific Ocean Acidification Project. In 2013, the US Integrated Ocean Observation System Ocean Technology Transition project, in collaboration with the National Oceanic and Atmospheric Administration’s Ocean Acidification Programme, funded five ocean acidification sensor development projects to inform and support the protection of the shellfish industry. “That example showed how local stakeholders and rights-holders who care about the issue can make a big difference in pushing for funding to support relevant monitoring,” says Professor Findlay. GOA-ON has invested in building capacity and training people around the world to engage in ocean observation and monitoring. However, the challenge now is to maintain—and fund—that work year after year. “As old-school as it might be, there is still no substitute for going out and measuring stuff consistently, at high enough frequency and over a sustained period of time,” insists Professor Widdicombe.
Scientists are increasingly emphasising the relevance of ocean acidification to stakeholders, in the hope of building the investment needed to improve monitoring. Aquaculture has already been affected by changing ocean conditions, with some operations adapting their practices in response. More detailed information about the rate and location of acidification could also help inform decisions about where to designate marine protected areas and how to approach marine spatial planning.
Accurate acidification data will become even more important as interest in marine carbon dioxide removal grows. Decisions about deploying ocean-based carbon removal technologies require an understanding of the underlying carbonate chemistry, particularly in coastal waters where conditions can vary considerably over relatively small distances. More broadly, understanding how quickly and where ocean conditions are changing is increasingly important for climate adaptation and marine management. “In everything from climate change adaptation to marine spatial planning and marine protected areas, the whole climate-smart revolution relies on us understanding how things are changing, over what timescale, and what the most appropriate decisions would be,” says Professor Widdicombe.

Monitoring systems for the future
The project has now developed tools that allow researchers to test their own datasets and describe their time series using the methodology. But it has also exposed the scarcity of datasets to which the approach can currently be applied. The researchers therefore have two clear messages: existing long-term observations need to be protected; and new monitoring needs must be designed with future applications in mind. “If we are now entering an era of longer, more frequently sampled carbonate chemistry time series, let’s think in advance about how to marry chemistry with biology to better understand biological responses to ocean acidification,” says Dr Suhareva. Doing so will require closer communication between oceanographic and biological communities. “Oceanographic and biological observations are often collected separately, sometimes by different organisations,” Dr Suhareva adds. Better co-ordination could allow biological observations to be built around existing chemical monitoring stations, creating aligned datasets capable of showing how ecosystems change alongside ocean chemistry.
That principle is being taken forward through a new European Commission project, Safeguarding from Acidification: Feedbacks and Ecosystem Services for European and Global Action (SAFESEA), led by Professor Findlay. One of its central questions is: what do stakeholders need from the ocean acidification community to make informed decisions? And, in turn, what data and modelling are required to support those decisions? “We’ll be taking specific guidance from stakeholders to think about what additional coastal and open-ocean data is needed,” explains Professor Findlay. The project will seek to improve coastal monitoring and incorporate more complex chemical models into coastal models, with the aim of better capturing the processes taking place in these highly variable environments.
Better data could also help translate existing international commitments into measurable results. Target 8 of the Kunming-Montreal Global Biodiversity Framework calls on countries to minimise the impacts of climate change and ocean acidification on biodiversity, yet there is currently no clear indicator for measuring the impact of ocean acidification on biodiversity. “Other targets within that framework had very good and very closely related numerical indicators to measure countries’ progress, but there was no such indicator for acidification,” says Professor Findlay. “Even within the international biodiversity protection community, there’s no guidance on ocean acidification beyond ‘please try and do something’.”
Developing better, data-informed indicators would not solve the underlying problem, but it could provide a way to track change, assess progress and identify where further action or investment is needed. The challenge now is to ensure that monitoring is sustained long enough to connect changes in ocean chemistry with their consequences for ecosystems and the decisions that depend on them.
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Back to Blue is an initiative of Economist Enterprise and The Nippon Foundation, two organisations that share a common understanding of the need to improve evidence-based approaches and solutions to the pressing issues faced by the ocean, and to restoring ocean health and promoting sustainability
