Early Earth likely had continents, was habitable, according to new study

http://www.eurekalert.org/pub_releases/2005-11/uoca-eel111605.php

A surprising new study by an international team of researchers has
concluded Earth's continents most likely were in place soon after the
planet was formed, overturning a long-held theory that the early planet was
either moon-like or dominated by oceans.
The team came to the conclusion following an analysis of a rare metal
element known as hafnium in ancient minerals from the Jack Hills in Western
Australia, thought to be among the oldest rocks on Earth. Hafnium is found
in association with zircon crystals in the Jack Hills rocks, which date to
almost 4.4 billion years ago.

"These results support the view that the continental crust had formed by
4.4-4.5 billion years ago and was rapidly recycled into the mantle," the
researchers wrote in Science Express. Led by Professor Mark Harrison of the
Australian National University, the team also included University of
Colorado Assistant Professor Stephen Mojzsis and researchers from the
University of California, Los Angeles and Ecole Normale Superieure
University in France.

The researchers used hafnium as a "tracer" element, using isotopes to infer
the existence of early continental formation on Earth dating to Hadeon Eon,
which took place during the first 500 million years of Earth's history,
said Mojzsis, an assistant professor of geological sciences at CU-Boulder.
Mojzsis also is a member of CU-Boulder's Center for Astrobiology.

"The evidence indicates that there was substantial continental crust on
Earth within its first 100 million years of existence," said Mojzsis. "It
looks like the Earth started off with a bang."

A 2001 study led by Mojzsis published in the journal Nature showed evidence
for the presence of water on Earth's surface roughly 4.3 billion years ago.
"The view we are taking now is that Earth's crust, oceans and atmosphere
were in place very early on, and that a habitable planet was established
rapidly," said Mojzsis.


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