Learn About Ocean Acidification

Discover the science of OA to stay aware, take action, and actively engage in adaptation and mitigation efforts.

Close-up of shell-covered barnacles and a small spiral sea snail on the right side.

Understanding OA Essentials

Ocean pH

The pH scale measures acidity and alkalinity. A pH below 7 is acidic, while a pH above 7 is alkaline. Seawater is naturally slightly alkaline, but since pre-industrial times, ocean pH has declined, meaning the ocean is becoming more acidic. Small changes in pH can significantly affect marine biodiversity.
Diagram showing ocean pH changes from 8.2 pre-industrial to 8.1 current to 7.7 future with coral images

Ocean Acidification: The Chemistry

As the ocean absorbs CO₂, pH decreases, and carbonate becomes less available, affecting corals and shell-forming organisms.
Diagram showing ocean acidification chemistry from CO2 absorption to impact on marine life shells and skeletons.

Signals of a Changing Ocean

Changes in seawater chemistry help track ocean acidification over time.

pH (Acidity):

How acidic the water is.

Partial Pressure of CO₂ (pCO₂):

Amount of carbon dioxide dissolved in seawater.

Total Alkalinity (TA)

The ocean’s ability to resist acidification.

Dissolved Inorganic Carbon (DIC)

Total amount of inorganic carbon present in water.

Frequently Asked Questions

Why is OA important in the Caribbean?

It affects coral reefs, seafood, tourism, and coastal protection, things many Caribbean communities depend on. Coastal areas such as mangroves, bays, and lagoons, especially those with limited water exchange or high runoff, can experience stronger acidification. These areas often face multiple stressors like warming, pollution, and Sargassum influxes.

How does ocean acidification impact corals in the Caribbean?

The Caribbean depends heavily on coral reefs for coastal protection, fisheries, and tourism. Ocean acidification weakens coral structures, making reefs more vulnerable to storms and reducing their ability to support marine life and local economies.

Why is the change in average ocean pH from pre-industrial to now so small (0.1 pH units)?

Even small increases in acidity can have big impacts on some marine life. Many studies suggest calcification rates could be reduced between 20-60% at 7.9 pH. This is why actions that slow or reverse acidification even a little can also benefit marine ecosystems.

Why is ocean acidification a management concern?

It affects ecosystem health, fisheries, tourism, and coastal protection, key components of the Caribbean economy. Reducing pollution, managing runoff, and protecting habitats can help mitigate local impacts.

What is Aragonite and Aragonite Saturation State (Ωarag)?

Aragonite is one of the more soluble forms of calcium carbonate and is widely used by marine calcifiers. Aragonite Saturation State is the measurement that indicates how favorable conditions are for organisms to build calcium carbonate structures (e.g. shells and skeletons). Lower values mean more stressful conditions.

What role does Sargassum play in ocean acidification?

When large amounts of Sargassum accumulate and decompose in coastal areas, they consume oxygen and release CO₂. This lowers pH and can intensify local acidification, especially in nearshore environments.

Can ocean acidification be reversed?

Reducing CO₂ emissions is the most effective way to slow this process. Implementing adaptation strategies and local protection such as improving water quality, investing in renewable energy, protecting coastal marine ecosystems, and reducing pollution can help increase resilience.

What is being done in the Caribbean to address ocean acidification?

Efforts include long-term monitoring, research, education, and regional collaboration through initiatives like Cari-CAN. These efforts help improve understanding, increase engagement, inform decision-making, and support adaptation strategies.

How fast is it happening?

Ocean pH has dropped 0.1 units since the industrial era, a 30 percent increase in acidity. In the Caribbean, coastal waters can acidify even faster due to local stressors. This can outpace most marine organisms' ability to adapt.

Who is most affected?

Island nations and coastal communities dependent on fishing face the greatest risk. Small-scale fishers lack resources to adapt. Developing economies bear the burden of a problem created elsewhere.

Need more information?

Reach out to Cari-CAN for research, collaboration, or resources