Corals that glow with the flow.Corals that glow with the flow Like trees with rings, corals embody a record of past environments. Wide growth bands and dense skeletal colonies of corals mark times when the temperature, sea level and climate were to their liking. Last year, Peter Isdale of the Australian Institute of Marine Science The Australian Institute of Marine Science (AIMS) is a state-of-the-art tropical marine research centre located primarily at Cape Ferguson, 50km south of Townsville in North Queensland, Australia. It was established in 1972, by the Commonwealth of Australia. in Queensland disocvered that Porites corals of the Great Barrier Reef Great Barrier Reef, largest complex of coral reef in the world, c.1,250 mi (2,000 km) long, in the Coral Sea, forming a natural breakwater for the coast of Queensland, NE Australia. house yet another clue to the past: bands that fluoresce fluo·resce intr.v. fluo·resced, fluo·resc·ing, fluo·resc·es To undergo, produce, or show fluorescence. [Back-formation from fluorescence. yellow-green when the coral is exposed to ultraviolet light Ultraviolet light A portion of the light spectrum not visible to the eye. Two bands of the UV spectrum, UVA and UVB, are used to treat psoriasis and other skin diseases. . In the May 30 NATURE, he and colleague Kevin Boto bo·to n. pl. bo·tos See Amazon dolphin. [Portuguese bôto.] examine the origin of these bands. The researchers knew that all regions of the corals contain fulvic acids, derived from organic matter most probably in seawater seawater Water that makes up the oceans and seas. Seawater is a complex mixture of 96.5% water, 2.5% salts, and small amounts of other substances. Much of the world's magnesium is recovered from seawater, as are large quantities of bromine. , that give off a blue background fluorescence. They found that the yellow-green bands also contain fulvic acids, but with a greater proportion of low-molecular-mass compounds. These compounds, they suspect, originate on the land because the timing, width and intensity of the yellow-green bands match peaks in rainfall and coastal runoff and because only the corals situated within 20 kilometers of the shore have the yellow-green bands. Indeed, Boto and Isdale were able to induce yellow-green fluorescene in fast-growing corals by incubating them in a mixture of seawater and fulvic acid extracted from local soils. The researchers conclude that the wide distribution of Porites corals combined with the ubiquity of fulvic compounds in rivers and runoff suggests that fluorescent banding is common in near-shore corals. This means that centuries of rainfall and runoff data are available in corals the world over. |
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