Ocean acidification is mostly caused by the ocean absorbing CO2. The
ocean takes up around 30% of CO2 in the atmosphere, so as human activities pump out CO2, they are forcing more of it into the oceans. CO2 dissolves in the ocean, creating carbonic acid and releasing hydrogen ions. Acidity levels are based on the number of hydrogen ions dissolved in water, so as the ocean absorbs more CO2, it becomes more acidic.
The hydrogen ions bond with carbonate ions in the ocean to form bicarbonate, which reduces the carbonate available to marine life like corals, clams and plankton. These animals need carbonate for their bones, shells and other natural structures, which they make out of calcium carbonate (CaCO3). Researchers measure
aragonite — one of the soluble forms of CaCO3 — to track ocean acidity levels.