hat
Ogmantasyon nan gaz kabonik atmosferik (CO.)2) konsantrasyon lakòz ogmantasyon nan CO2 depozisyon nan oseyan an sifas, diminye pH la nan dlo lanmè (fè dlo lanmè an plis asid). Rezilta asidifikasyon nan oseyan yo diminye kantite lajan an nan kabonat kalsyòm ki disponib pou koray ak lòt kalsifye òganis maren yo bati vye zo eskèlèt yo ak kokiy. Pwosesis sa a rele asidifikasyon lanmè a epi redwi kapasite yon resif pou devlope ak kenbe tèt ak estrès.
eng
Increases in atmospheric carbon dioxide (CO2) concentrations cause increases in CO2 deposition in the surface ocean, lowering the pH of seawater (making the seawater more acidic). Resulting acidification of the oceans reduces the amount of calcium carbonate available for corals and other calcifying marine organisms to build their skeletons and shells. This process is called ocean acidification and reduces a reef’s ability to grow and withstand stress.