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First, it forms carbonic acid. Then, this carbonic acid breaks apart or dissociates producing bicarbonate ions and hydrogen ions. Ocean acidification results from an increased concentration of hydrogen ions and a reduction in carbonate ions due to the absorption of increased amounts of CO2.
Carbon dioxide and seawater Water and carbon dioxide combine to form carbonic acid (H2CO3), a weak acid that breaks (or dissociates) into hydrogen ions (H+) and bicarbonate ions (HCO3-).
. Thinking about your answer from question (a), if excess CO2 results in an excess of hydrogen ions in seawater what will happen to carbonate? Some of the excess Hydrogen ions will combine with carbonate to form bicarbonate therefore reducing the availability of carbonate to marine organisms.
When carbon dioxide (CO2) is absorbed by seawater, chemical reactions occur that reduce seawater pH, carbonate ion concentration, and saturation states of biologically important calcium carbonate minerals. These chemical reactions are termed ocean acidification or OA for short.
When CO2 is absorbed by seawater, a series of chemical reactions occur resulting in the increased concentration of hydrogen ions. This increase causes the seawater to become more acidic and causes carbonate ions to be relatively less abundant.

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Ocean acidification can negatively affect marine life, causing organisms shells and skeletons made from calcium carbonate to dissolve. The more acidic the ocean, the faster the shells dissolve.
For good reason, ocean acidification is sometimes called osteoporosis of the sea. Ocean acidification can create conditions that eat away at the minerals used by oysters, clams, lobsters, shrimp, coral reefs, and other marine life to build their shells and skeletons. Human health is also a concern.

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