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Increased production of carbon dioxide (CO2) leads to higher concentrations of CO2 in the atmosphere, which is then absorbed by the oceans. When CO2 dissolves in seawater, it reacts with water to form carbonic acid, which dissociates into bicarbonate and hydrogen ions. The increase in hydrogen ions lowers the pH of the water, resulting in ocean acidification. This change in pH can negatively impact marine life, particularly organisms that rely on calcium carbonate for their shells and skeletons.

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2d ago

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