Coral Reefs Unlikely to Survive in Acid Oceans
Posted on December 22, 2007
We've all heard that global warming will generate devastating floods and droughts. We are familiar with the warnings about rising sea levels. We know that countless scientists and scientific organizations believe global warming is real and that climate change is something humans are going to have to deal with on an increasing basis over the coming decades. What's less understood by both global warming believers and global warming deniers is what carbon emissions are doing to our oceans.
Our carbon emissions are not just heating up the globe. They are also changing the chemistry of our oceans. This change is putting coral reefs including Australia's Great Barrief Reef at risk. This could soon be fatal to coral reefs, which are havens for marine biodiversity and underpin the economies of many coastal communities. Scientists from the Carnegie Institution's Department of Global Ecology have calculated that if current carbon dioxide emission trends continue, by mid-century 98% of present-day reef habitats will be bathed in water too acidic for reef growth. Among the first victims will be Australia's Great Barrier Reef, the world's largest organic structure.
Chemical oceanographers Ken Caldeira and Long Cao presented their results in a multi-author paper in the December 14 issue of Science and at the annual meeting of American Geophysical Union in San Francisco on the same date. The work is based on computer simulations of ocean chemistry under levels of atmospheric CO2 ranging from 280 parts per million (pre-industrial levels) to 5000 ppm. Present levels are 380 ppm and rapidly rising due to accelerating emissions from human activities, primarily the burning of fossil fuels.
"About a third of the carbon dioxide put into the atmosphere is absorbed by the oceans," says Caldeira, "which helps slow greenhouse warming, but is a major pollutant of the oceans." The researchers say the absorbed CO2 produces carbonic acid - the same acid that gives soft drinks their fizz - making certain minerals called carbonate minerals dissolve more readily in seawater. This is especially true for aragonite, the mineral used by corals and many other marine organisms to grow their skeletons.
"Before the industrial revolution, over 98% of warm water coral reefs were bathed with open ocean waters 3.5 times supersaturated with aragonite, meaning that corals could easily extract it to build reefs," says Cao. "But if atmospheric CO2 stabilizes at 550 ppm -- and even that would take concerted international effort to achieve -- no existing coral reef will remain in such an environment." The chemical changes will impact some regions sooner than others. At greatest risk are the Great Barrier Reef and the Caribbean Sea.
The scientists also say that carbon dioxide's chemical effects on the ocean are largely independent of its effects on climate. This means that measures to mitigate warming short of reducing emissions will be of little help in slowing acidification of our oceans. The scientists warn that prevention continued ocean acidification may require even more drastic emissions cuts than have been presented for climate change.
"These changes come at a time when reefs are already stressed by climate change, overfishing, and other types of pollution," says Caldeira, "so unless we take action soon there is a very real possibility that coral reefs - and everything that depends on them -will not survive this century."