Three billion year old zircon microcrystals found in Ontario
are proving to be a new record of the processes that formed continents
and their natural resources, including gold and diamonds.
The recent discovery was made by an international team
of researchers led by Earth Sciences professor Desmond Moser at The University of
Western Ontario. Measuring no more than the width of a human hair, the
200-million-year growth span of these ancient microcrystals is longer
than any previously discovered.
The findings provide a new record of planetary evolution and
contradict previous experimental predictions that the crystals would
change when exposed to heat and pressure upon burial in the deep Earth.
Instead, they have an incredible 'memory' of their time below
volcanoes, of transport to the shores of ancient oceans and of their
burial beneath now-extinct mountain ranges billions of years before the
time of dinosaurs.
Containing trace amounts of uranium, the crystals continued to grow
over hundreds of millions of years, even as the planet evolved and
underwent a series of dramatic shifts. "The oldest pieces of our planet
are crystals of zircon," says Moser. "These crystals are the memory
cells of the Earth and with our study we can now say they are an
accurate recorder of planetary evolution over eons -- in the same way
that rings on an old tree can record changes in a forest over
hundreds of years."
Keeping with the tree analogy, Moser found that these crystals had
roughly circular growth zones that he was able to date and analyze with
specialized equipment, ion probes. These zones track the formation of the early
North American continent, from its beginning as a series of volcanic
island chains, to its eventual fusion into a large, thick continental
plate that became the core of North America.
As the crystals formed around the same time as gold, diamond and
other metal deposits, this research provides not only insight into the
formation of Earth itself, it can also help answer the question, "Did
plate tectonics operate early in our planet's history or did some other
process create the large metal and diamond deposits of the Canadian
Shield?" "It also provides a new tool for dating the appearance of
oceans on other rocky planets like Mars, where Rover results indicate
zircon crystals should exist" says Moser.
Over the course of millions of years, the crystals have been pushed
back to the surface from depths of 30 kilometres by a series of pushes
on the edges of the original continent, which give us globally-rare
exposures in northern Ontario. "It's not every day you find a piece of
the deep Earth that you can walk around on and explore," Moser says.
Moser's findings are further detailed in the March issue of Geology, published by the Geological Society of America.
Adapted from materials provided by University of Western Ontario.