Image: COURTESY OF C. FRED T. ANDRUS |
Using tiny bone fragments from fossilized fish, scientists have traced the roots of the climate phenomenon known as El Ni¿o, the intermittent warming of ocean waters off the coast of Peru that can affect weather worldwide. According to a report published in the current issue of the journal Science, modern El Ni¿o conditions arose around 5,000 years ago.
Previous research based on fossilized mollusk remains had suggested that El Ni¿o conditions did not exist thousands of years ago, but those findings were preliminary. In the current study, C. Fred T. Andrus of the University of Georgia and colleagues analyzed isotopes of oxygen present in the ear stones, or otoliths (see micrograph at right), of a species of catfish that lives off the coast of Peru and does not migrate. Like tree rings, otoliths grow concentrically and incorporate elements indicative of the environment in which they formed. "By looking at the entire otolith," co-author Douglas E. Crowe of the University of Georgia explains, "we can reconstruct the water temperature history throughout the life of the fish, from season to season and year to year."
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In this case, the researchers focused on the amount of oxygen isotope 18 in the otoliths--an indicator of the water temperature in which the fish lived. The team examined fossils recovered from two Peruvian archaeological sites approximately 6,000 years old and found that ocean temperatures then were on average three to four degrees Celsius warmer and less variable than current sea temperatures are.
The findings illustrate the variability inherent in global climate, Andrus observes. "Our research shows that the current El Ni¿o cycle is significantly different from what it was five to eight thousand years ago," he says. "Our hope is that our data can be used to build accurate predictive models of future El Ni¿o events."
