World Biogeography
Ocean acidification refers to the process by which the ocean becomes more acidic due to increased levels of carbon dioxide (CO2) in the atmosphere. As CO2 is absorbed by seawater, it reacts to form carbonic acid, leading to a decrease in pH levels. This change in ocean chemistry can have profound impacts on marine life, particularly organisms that rely on calcium carbonate for their shells and skeletons, connecting it directly to climate change and biodiversity loss.
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