New technique to establish ancient fossil age
T.C. Partridge and R.J. Clarke, researchers from the University of the Witwatersrand in South Africa, were confronted with a mixed blessing when, in 1997, they discovered a nearly complete skeleton of what appeared to be an Australopithecus buried in the sediments on the floor of the Sterkfontein cave in central South Africa. The fossil was well preserved, but its age was uncertain. It was more than 2 million years old, but how much more? The answer to that question would affect theories of how and when Australopithecus spread through Africa.
"Their initial estimate of 3.3 million years provoked a lot of controversy," Granger said. "Few thought that Australopithecus had traveled so far so long ago, and scientists wanted more proof. If the estimate was accurate, it might require a rethinking of human prehistory."
A firmer answer would require the innovative use of a particle accelerator half a world away at Purdue in Indiana, where Granger was using radioactive isotopes in sediment to determine the age of rivers and caves.
Dating fossils by examining the minute quantities of radioactive elements they contain is not a new technique in archaeology. Carbon-14, a radioactive isotope that slowly decays as centuries pass, has been a common benchmark for dating many human fossils; the more carbon-14 has decayed in a sample, the older it must be. The speed at which carbon-14 decays, called its half-life, is only 5,730 years. This means that after a few millennia, the isotope is no longer useful to mark a fossil's age.
"Once your fossil is older than 50,000 years, its carbon-14 is nearly gone," Granger said. "We knew the South African fossils were at least 2 million years old, so it was clear we needed another way to establish their age."
Granger, a physics major as an undergraduate, eventually became an earth scientist when he developed an interest in studying the age and changes in mountains and river beds, geological formations that are often many millions of years old. Rather than use carbon-14 to date his landscapes, he looked for isotopes with far longer half-lives - and found them in aluminum-26 and beryllium-10. These elements often form in common quartz when it is on the Earth's surface and exposed to cosmic rays.
"When radiation from outer space strikes silicon and oxygen atoms in a quartz crystal, they split into aluminum-26 and beryllium-10, both of which have half-lives of around a million years," Granger said. "Because they decay so slowly, they allow you to reach back much further in history than you can using carbon-14."
The use of aluminum and beryllium for radiometric dating had only been around for a few years when Granger began to use it on cave sediments. The technique was not widely known outside geological circles, so when he heard about the Australopithecus discovery, he contacted the South African scientists who found the skeleton and asked if he could be of assistance.
"It was the first time this method had been used to determine the age of something that had been alive," Granger said. "But based on the evidence, we found that the fossil was even older than the initial estimate."
Granger and Caffee, of Purdue's physics department, analyzed samples of the skeleton in Purdue's accelerator mass spectrometer, a device capable of detecting the infinitesimal quantities of radioactive aluminum and beryllium in the samples.
"We found that the skeleton was between 3.5 and 4.5 million years old," Granger said. "That's admittedly quite a large window of possibility, but even if it's on the young side, it still puts Australopithecus in southern Africa far earlier than expected."
The significance for anthropologists would be the possibility that mankind's earliest ancestors were a different species than scientists generally believe.
Tuesday, July 29, 2003
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