Page 4: Research news on ocean acidification

Ocean acidification is the ongoing decrease in ocean pH caused primarily by uptake of anthropogenic CO₂ from the atmosphere, leading to shifts in the seawater carbonate system. Dissolved CO₂ forms carbonic acid, which dissociates to release hydrogen ions and convert carbonate ions to bicarbonate, reducing carbonate saturation states critical for calcifying organisms (e.g., corals, coccolithophores, mollusks). Research focuses on quantifying pH and aragonite/calcite saturation changes, organismal and ecosystem responses, biogeochemical feedbacks, and interactions with other stressors such as warming and deoxygenation, using observations, laboratory experiments, mesocosms, and Earth system models.

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