Ocean Acidification and the Chemistry of Planetary Change
Ocean Acidification and the Chemistry of Planetary Change explains why ocean acidification is one of the clearest chemical expressions of planetary change. The article shows how rising atmospheric carbon dioxide dissolves into seawater, lowers pH, reduces carbonate ion availability, and weakens aragonite saturation states needed by many marine organisms. It examines carbonate chemistry, calcification, coral reefs, planktonic organisms, shellfish coasts, polar waters, upwelling systems, ecosystem vulnerability, and the boundary’s updated status as a transgressed planetary boundary in the 2025 Planetary Health Check. It also connects acidification to climate change, biosphere integrity, nutrient pollution, freshwater change, and coastal governance, with mathematical, Python, and R workflows for carbonate-risk diagnostics.









