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Since the Industrial Revolution, surface ocean waters have become 30% more acidic due to the absorption of carbon dioxide, which disrupts the formation of coral reefs and the shells and skeletons of marine organisms.

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Additional insights we found via NOAA
About 30% of the carbon dioxide released into the atmosphere is absorbed by oceans, where it dissolves in water to form carbonic acid.
Because carbonic acid is weak, it splits into bicarbonate and hydrogen ions, and the latter binds to available carbonate, preventing it from being used by calcifying organisms to build various structures.
Increased ocean acidification is expected to accelerate the dissolution of marine organisms' shells, impair some fish's ability to detect predators, and destroy suitable habitats for various ocean species, thereby substantially impacting food webs.
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