Page 2: 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.

River chemistry insights may boost coastal ocean modeling

Rivers deliver freshwater, nutrients, and carbon to Earth's oceans, influencing the chemistry of coastal seawater worldwide. Notably, a river's alkalinity and the levels of dissolved inorganic carbon it brings to the sea ...

Q&A: The future of corals and what X-rays can tell us

This summer, it was all over the media. Driven by the climate crisis, the oceans have now also passed a critical point: The absorption of CO2 is making the oceans increasingly acidic.

page 2 from 5