Ocean acidification may be impacting coral reefs in the Florida Keys

Researchers say reefs are dissolving sooner than previously thought

2 May 2016

Joint Release

WASHINGTON, DC—Limestone that forms the foundation of coral reefs along the Florida Reef Tract is dissolving during the fall and winter months on many reefs in the Florida Keys, according to a new study. The research showed that the upper Florida Keys were the most impacted by the annual loss of reef.

The extensive thickets of staghorn corals at Carysfort Reef, approximately six nautical miles east of Key Largo, Florida, are gone today and replaced by a structure-less bottom littered with the decaying skeletons of staghorn coral. Credit: Chris Langdon.

The extensive thickets of staghorn corals at Carysfort Reef, approximately six nautical miles east of Key Largo, Florida, are gone today and replaced by a structure-less bottom littered with the decaying skeletons of staghorn coral.
Credit: Chris Langdon.

Each year the oceans absorb carbon dioxide from the atmosphere and become more acidic, a process called ocean acidification.  Projections, based largely on laboratory studies, led scientists to predict that ocean pH would not fall low enough to cause reefs to start dissolving until 2050-2060.

For two years, the researchers collected water samples along the 200-kilometer (124-mile) stretch of the Florida Reef Tract north of Biscayne National Park to the Looe Key National Marine Sanctuary. The data provide a snapshot on the health of the reefs and establish a baseline from which future changes can be judged.

The results showed reef dissolution is a significant problem on reefs in the upper Keys with the loss of limestone exceeding the amount the corals are able to produce on an annual basis. As a result, these reefs are expected to begin wasting away, leaving less habitat for commercially- and recreationally-important fish species. Florida Keys’ reefs have an estimated asset value of $7.6 billion. The study was accepted for publication today in the journal Global Biogeochemical Cycles, a journal of the American Geophysical Union.

In the natural scheme of things in the spring and summer months, environmental conditions in the ocean such as water temperature, light and seagrass growth are favorable for the growth of coral limestone. During the fall and winter, low light and temperature conditions along with the annual decomposition of seagrass result in a slowing, or small-scale loss of reef growth.

However, as atmospheric carbon dioxide is absorbed by seawater, ocean pH declines. The result is that the natural summer growth cycle of coral is no longer large enough to offset the effects of dissolution from ocean acidification.

“We don’t have as much time as we previously thought,” said Chris Langdon, professor of marine biology and ecology at the University of Miami Rosensteil School of Marine & Atmospheric Science and a senior author of the study. “The reefs are beginning to dissolve away.”

“This is one more reason why we need to get serious about reducing carbon dioxide emission sooner rather than later,” Langdon said.

The data for the study were collected in 2009-2010. The researchers suggest that a more recent analysis should be conducted to see how the reefs are faring today.

“The worst bleaching years on record in the Florida Keys were 2014-2015, so there’s a chance the reefs could be worse now,” Langdon said.

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Title

“Dynamics of carbonate chemistry, production and calcification of the Florida Reef Tract (2009-2010): evidence for seasonal dissolution”

Authors:
Nancy Muehllehner, Chris Langdon, Alyson Venti: Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, U.S.A.;

David Kadko: Florida International University, Miami, Florida, U.S.A.

Contact Information for the Authors:
Chris Langdon: +1 (305) 421-4614, clangdon@rsmas.miami.edu


AGU Contact:

Lauren Lipuma
+1 (202) 777-7396
llipuma@agu.org

University of Miami Contact:
Diana Udel
+1 (305) 421-4704
dudel@rsmas.miami.edu