As the atmosphere warms, so does the ocean, and the extra heat can affect the metabolism of corals. Extreme temperatures can lead to so-called bleaching of coral. In addition, according to laboratory studies, these reef-builders and other organisms that construct skeletons out of calcium carbonate are affected by the increasing acidity created when the sea absorbs carbon dioxide.
Now, a study that began with marine geochemist Jacob Silverman's doctoral research at the Hebrew University of Jerusalem, Israel, has made a quantitative link between atmospheric levels of CO2 and the fate of coral. Currently a postdoc at the Carnegie Institution Department of Global Ecology in Stanford, California, Silverman looked at how nutrients were affecting photosynthesis, respiration, and calcification on the kilometer-long Eilat reef in the Red Sea north of Egypt.
Silverman and his colleagues determined the relationship among the rate of calcification, water temperature, and the concentration of carbonate ions. Corals use these ions to build their skeletons, and the available amount falls with stronger acidity. They also showed how the calcification rate affected the amount of live coral on the reef. The resulting equations, or "rate law," is described in the current issue of Geophysical Research Letters. The group confirmed the equations with measurements from studies done at other reefs from the 1970s to 1990s."
ORIGINAL SOURCE: ScienceNOW
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