Anthropogenic changes to seawater buffer capacity combined with natural reef metabolism induce extreme future coral reef CO2 conditions

Ocean acidification, via an anthropogenic increase in seawater carbon dioxide (CO2), is potentially a major threat to coral reefs and other marine ecosystems. However, our understanding of how natural short-term diurnal CO2 variability in coral reefs influences longer term anthropogenic ocean acidification remains unclear. Here, we combine observed natural carbonate chemistry variability with future carbonate chemistry predictions for a coral reef flat in the Great Barrier Reef based on the RCP8.5 CO2 emissions scenario…

Resource type: article

Resource format: webpage

Wiley, 1 January 2013. Resource.


  • Reset

Subscribe

OA-ICC Highlights


%d bloggers like this: