Student sample for assessment
Written by a Year 9 student in Perth, Western Australia, Australia.
Ocean acidification is the process by which the ocean becomes less alkaline—more acidic—as it absorbs carbon dioxide from the atmosphere. When CO2 dissolves in seawater, it forms carbonic acid, which lowers the ocean's pH. Scientists measure this by comparing pH levels over time. Before industrialisation, the ocean's pH was approximately 8.2, but it has since fallen to 8.1. Although this seems like a small change, it represents a 26 per cent increase in acidity, demonstrating how even tiny shifts in pH can have significant effects on marine chemistry. This acidification is caused primarily by human activities. The ocean absorbs approximately 25 to 30 per cent of the carbon dioxide that humans emit through burning fossil fuels, manufacturing and agriculture. As human CO2 emissions have increased dramatically since the Industrial Revolution, so has the amount of CO2 the ocean absorbs. The ocean acts as a carbon sink, absorbing excess CO2 that would otherwise accumulate in the atmosphere. While this absorption slows atmospheric climate change, it comes at a cost to ocean chemistry and the organisms that depend on it. Ocean acidification directly harms marine organisms that build shells and skeletons from calcium carbonate, including oysters, mussels, corals and certain types of plankton. As the ocean becomes more acidic, it becomes harder for these organisms to form and maintain their calcium carbonate structures. This is particularly devastating for coral reefs, which support approximately 25 per cent of all marine species. Coral reefs have already experienced multiple mass bleaching events due to warming waters, and acidification adds another stress. When foundational species like plankton and corals are threatened, entire ecosystems collapse, affecting fish populations and the food chains that depend on them.