How do changes in the carbon cycle affect the oceans?
Carbon dioxide is dissolved from the atmosphere into the oceans as a part of the carbon cycle.
CO2 in oceans is used by marine organisms like phytoplankton and seaweed through photosynthesis to make calcium carbonate shells and skeletons.
Increased levels of CO2 can lead to increased levels of acidity in the oceans, as the oceans initially absorb more CO2. This can have adverse effects on marine life.
Increased global temperatures could mean that marine life sensitive to temperature such as phytoplankton cannot survive in the oceans. This causes their numbers to decrease, and so less CO2 is absorbed from the atmosphere because less is needed for them for photosynthesis.
Warmer water is less able to absorb CO2, so as temperatures rise less CO2 is dissolved into the oceans.