Research news on Ocean Acidification

Ocean acidification is a biologically consequential process driven by the uptake of anthropogenic carbon dioxide (CO₂) by seawater, which lowers pH and alters carbonate chemistry, thereby affecting marine organisms and ecosystems. Increased dissolved CO₂ forms carbonic acid, shifting equilibria among CO₂, bicarbonate (HCO₃⁻), and carbonate ions (CO₃²⁻), reducing carbonate availability needed for biogenic calcification in corals, mollusks, echinoderms, and some plankton. This can impair shell and skeleton formation, disrupt acid–base regulation, metabolism, sensory functions, and reproductive success in diverse taxa, and modify species interactions, community structure, and biogeochemical cycles, including primary production and trophic dynamics.

Coral reefs set to stop growing as climate warms

Most coral reefs will soon stop growing and may begin to erode—and almost all will do so if global warming hits 2°C, according to a new study in the western Atlantic. An international team, led by scientists from the University ...

Sharks may be losing deadly teeth to ocean acidification

Sharks can famously replace their teeth, with new ones always growing as they're using up the current set. As sharks rely on their teeth to catch prey, this is vital to the survival of one of the oceans' top predators.