http://www.scientificamerican.com/blog/post.cfm?id=meteorite-nugget-pushes-back-age-of-2010-08-23


A new analysis of a meteorite shows that an inclusion within the carbonaceous 
stone is older than any known material in the solar system. The finding pushes 
back the estimated age of the solar system to 4.568 billion years, older than 
previous estimates by up to 1.9 million years.

A piece of the meteorite, known as Northwest Africa 2364, was purchased in 2004 
in Morocco and is now part of a collection at Northern Arizona University in 
Flagstaff, Ariz. About 150 miles south of Flagstaff, two researchers at the 
Arizona State University Center for Meteorite Studies in Tempe, Audrey Bouvier 
andMeenakshi Wadhwa, dated an especially primitive piece of the meteorite known 
as a calcium-aluminum-rich inclusion, or CAI. Their findings appeared online 
August 22 in Nature Geoscience.

Bouvier and Wadhwa measured the meteorite's ratio of two lead isotopes, whose 
relative proportions change on geologic timescales. Each variety of lead is a 
decay product of uranium, but the two parent uranium isotopes have very 
different half-lives: uranium 238 decays to lead 206 with a half-life of about 
4.5 billion years, whereas uranium 235 decays to lead 207 with a half-life of 
about 700 million years. So the relative abundances of lead 206 and 207 can be 
used—along with some calibration for initial uranium abundances—to determine 
the age of ancient objects. 

The balance of lead isotopes in the Northwest Africa 2364 meteorite point to an 
age of 4,568,200,000 years, plus or minus a few hundred thousand years. Taking 
the measurement uncertainties into account, that is between 300,000 and 1.9 
million years more ancient than the oldest CAIs found in other meteorites. The 
lead-derived age of Northwest Africa 2364, Bouvier and Wadhwa write, is "the 
oldest absolute age yet obtained for any Solar System material and is, 
therefore, the best estimate for the time of formation of the Solar System."
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