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Stylophora pistillata, a well-studied stony coral common in the Indo-Pacific. (Credit: Kevin Wyman/Rutgers)

climate change

Climate change won’t stop stony corals from making rock

New research suggests stony corals may fare better under the acidic ocean conditions caused by climate change than once thought.

“The bottom line is that corals will make rock even under adverse conditions,” says Paul G. Falkowski, a professor who leads the Environmental Biophysics and Molecular Ecology Laboratory at Rutgers University-New Brunswick.

“They will probably make rock even as the ocean becomes slightly acidic from the burning of fossil fuels.”

“They’re more resilient than we give them credit for.”

Using a materials science approach, the team tapped several high-tech imaging methods to show that corals use acid-rich proteins to build rock-hard skeletons made of calcium carbonate minerals.

“What we’re showing is that the decades-old general model for how corals make rock is wrong,” Falkowski says. “This very careful study very precisely shows that corals will secrete proteins, and the proteins are what really forms the mineral, and the proteins are very acidic, which will surprise a lot of people.”

Corals are largely colonial organisms that harbor hundreds to hundreds of thousands of polyps (animals). Reefs built by stony, shallow-water coral species are among the world’s most diverse ecosystems. Thousands of species of fish and other sea life rely on reefs for survival, and thousands of human communities count on reefs for food, protection, and jobs, according to the National Oceanic and Atmospheric Administration.

But corals face several environmental threats over the long-run: potentially deadly bleaching from global warming and rapid temperature changes; nutrient pollution; the physical destruction of coral reefs; and ocean acidification linked to carbon dioxide emissions, Falkowski says.

The ocean absorbs carbon dioxide from fossil fuel burning and land use changes, leading to lower pH and greater acidity, according to NOAA. Ocean acidification is reducing levels of calcium carbonate minerals in many areas, which will likely hamper the ability of some organisms to create and maintain their shells.

According to the study, there are two main hypotheses about how stony corals build their stony skeletons. One is through largely physical and chemical processes and the other is through a biologically driven process.

Fat shows how coral ‘babies’ cope with warmer water

Rutgers scientists examined Stylophora pistillata—a well-studied stony coral common in the Indo-Pacific—using ultra-high-resolution 3D imaging and 2D nuclear magnetic resonance (NMR) spectroscopy. They showed that stony corals precipitate minerals through a biologically driven process.

“As far as I know, we were unique in the world in using a coordinated set of techniques to understand the ultrastructure of coral skeletons,” Falkowski says. The techniques included Raman imaging and spectroscopy, and scanning helium ion microscopy.

The scientists found that random nanoparticles are deposited in coral microenvironments enriched in organic material. The nanoparticles accumulate and form stony structures made of calcium carbonate—known as aragonite—by growing crystals. The NMR imaging results show that coral acid-rich proteins are the main drivers.

The proteins function at a pH (a measure of acidity and alkalinity) of about 8.5 to 7, and “that environment, to them, is still perfectly fine,” Falkowski says. The ocean normally has a pH of 8.1 or 8.2 and in the coming century or so that may drop to 7.8, but stony corals will still be able to make rock.

“For stony corals, we’re fairly confident that the acidification issue is exaggerated,” he says. “They’re more resilient than we give them credit for.”

5,000-year-old corals are now threatened

The study appears in the journal Science. Other study authors are from the Newark and New Brunswick campuses of Rutgers University and from the American Museum of Natural History in New York City.

Source: Rutgers University

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