Ocean acidification is the ongoing decrease in the pH of the Earth's oceans, caused by the uptake of carbon dioxide (CO2) from the atmosphere. When CO2 dissolves in seawater, it reacts to form carbonic acid, which lowers ocean pH and leads to a more acidic environment. This subtle shift in ocean chemistry can have profound effects on marine life, particularly organisms with calcium carbonate shells or skeletons, like corals and shellfish, making it harder for them to grow and survive.
The significance of ocean acidification extends beyond marine ecosystems; it has serious implications for human societies that rely on the ocean's bounty. Fisheries and aquacultures face potential collapse, threatening food security for millions of people. Moreover, as acidification alters marine food webs and biodiversity, it compromises the ocean's ability to regulate climate—a role that is already under strain from increasing global temperatures. Understanding and addressing ocean acidification is crucial not only for preserving marine life but also for maintaining the economic and climatic stability upon which humanity depends.