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The carbon cycle in seawater involves the absorption of atmospheric carbon dioxide (CO2) by the ocean, where it dissolves and reacts with water to form carbonic acid. This process leads to the formation of bicarbonate and carbonate ions, which are utilized by marine organisms for processes like photosynthesis and shell formation. Carbon is also exchanged between the ocean and the atmosphere through various biological and physical processes, including respiration, decomposition, and ocean currents. Ultimately, carbon can be sequestered in deep ocean sediments, helping to regulate global carbon levels over long periods.

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3d ago

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