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Simulation shows how declines in coral reef calcification could affect future ocean carbon sink capabilities

Simulation shows how declines in coral reef calcification could affect future ocean carbon sink capabilities
Carbon uptake enhancement extends beyond the regions of coral reefs. The (A), mean ocean anthropogenic carbon uptake in 2081 to 2099 of RCP4.5 and the (B), coral reef-driven anomaly in ocean anthropogenic carbon uptake in 2081 to 2099 of RCP4.5150. Stippling indicates the distribution of coral reefs. Credit: Proceedings of the National Academy of Sciences (2025). DOI: 10.1073/pnas.2501562122

A team of meteorologists, Earth scientists and oceanographers at Sorbonne Université, working with one colleague from Université Paris-Saclay and another from Université Brest, all in France, has developed a simulation that they believe shows how declining coral reef calcification could slow global warming.

In their study, in the journal Proceedings of the National Academy of Sciences, the group used data from prior predictions regarding the loss of coral reefs due to to build a model that simulates how much less would be released from the ocean into the atmosphere, and its possible impact on .

Prior research has shown that corals and the reefs they build in the world's oceans are at risk due to increased ocean acidification caused by an increase in carbon dioxide. Such acidification has been found to cause bleaching and harms the ability of corals to build carbonate skeletons which form reefs.

Corals behave opposite that of land-based plants—instead of absorbing carbon dioxide as they grow, corals release it as their calcium-carbonate-based skeletons grow. That carbon dioxide then makes its way to the surface, where it is released into the atmosphere, contributing to global warming. Because of that, the loss of coral calcification is expected to allow the oceans to absorb more carbon dioxide.

In this new effort, the research team used existing data to create a showing how much the planet would benefit (regarding carbon levels only) if different percentages of the world's corals were to die due to heightened levels of carbon dioxide in the water.

The research team found that the world's oceans would be able to absorb between 1 and 5% more carbon by 2100 based on current carbon emission estimates and the rate of die-off. They also found the percentage could increase by up to 13% by 2300.

The researchers note that their simulation did not take into consideration other factors that could change the rate of decline of corals. They also note that the loss of corals, while potentially helpful in slowing global warming, would be catastrophic to the animals that live among the reefs they build, possibly altering the ocean in ways that have not yet been discovered.

More information: Lester Kwiatkowski et al, Declining coral calcification to enhance twenty-first-century ocean carbon uptake by gigatonnes, Proceedings of the National Academy of Sciences (2025).

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Citation: Simulation shows how declines in coral reef calcification could affect future ocean carbon sink capabilities (2025, June 3) retrieved 3 June 2025 from /news/2025-06-simulation-declines-coral-reef-calcification.html
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