4.4
bn year old zircon reveals life on Earth appeared earlier than
believed
RT,
24
February, 2014
Ancient
zircon crystals, discovered in Australia in 2001, have now been
proved to be our planet’s oldest known substance. The 4.4
billion-year-old gem offers clues that Earth could have become
habitable much earlier than previously believed.
Aside
from being just a cool fact to know, this recent discovery (available
in the journal, Nature
Geoscience)
gives scientists at the University of Wisconsin a new insight into
our planet’s infancy.
There
are now grounds to suggest that Earth cooled down much sooner, and
that life appeared way before many scientists had thought.
"We
have no evidence that life existed then. We have no evidence that it
didn't,” Wisconsin geoscience professor and report lead, Professor
John Valley, told Reuters. “But there is no reason why life could
not have existed on Earth 4.3 billion years ago," he
added.
The
oldest fossil records of life are stromatolites produced by an
archaic form of bacteria from about 3.4 billion years ago.
Scientists
believe that thanks to low enough temperatures, Earth had a
hydrosphere and possibly early life even before 4.3 billion years
ago. In fact, there is even a theory of a "cool
early Earth.”
Professor
Valley says their discovery really strengthens this notion.
“The
study reinforces our conclusion that Earth had a hydrosphere before
4.3 billion years ago, and possibly life not long after,” John
Valley is quoted as saying in the press-release.
Image from wisc.edu
Valley’s
discovery undermines this idea.
This
4.4 billion-year-old zircon crystal proves that the Earth cooled from
a ball of magma and formed continents much earlier.
He
and his team confirmed that our planet first developed a crust just
160 million years after the formation of our solar system.
“Our
samples formed after the magma oceans cooled and prove that these
events were very early,” he
wrote.
But
his team still has no answer to the main question: "One
of the things that we're really interested in is: when did the Earth
first become habitable for life? When did it cool off enough that
life might have emerged?" Professor
Valley said.
So,
how did the University of Wisconsin scientists make their
breakthrough findings?
They
used two different age-determining techniques on the tiny zircon
crystal, as small as 200 by 400 microns, about twice the diameter of
a human hair, extracted from a rock outcrop in the Jack Hills region,
Western Australia, in 2001.
But
first they used a widely-accepted dating technique based on
determining the radioactive decay of uranium to lead in a mineral
sample.
Valley
and his colleagues then looked at lead atoms in zircon using a new
technique called atom-probe tomography in conjunction with secondary
ion mass spectrometry. It helped them identify individual atoms of
lead in the crystal and then determine the age and thermal history of
zircon by estimating the mass of lead atoms.
And
so it was confirmed that the zircon is indeed 4.4 billion years old.
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