Andrew Yee
November 18th 05, 03:38 PM
Marketing and Communications Division
Australian National University
Canberra, Australia
Further Information:
Professor Mark Harrison
Director, Research School of Earth Sciences
T: 02 6125 2487
Amanda Morgan
Media Liaison
Tel: 02 6125 5575 / 0416 249 245
Friday, 18 November 2005
There was no such thing as hell on Earth
New ANU research is set to radically overturn the conventional wisdom that
early Earth was a hellish planet barren of continents.
An international research team led by Professor Mark Harrison of the
Research School of Earth Sciences analysed unique 4 to 4.35
billion-year-old minerals from outback Australia and found evidence that a
fringe theory detailing the development of continents during the first 500
million years of Earth history -- the Hadean ('hellish') Eon -- is likely
to be correct.
The research, published in the latest edition of Science, follows on from
results by Professor Harrison and his colleagues published earlier this
year that confirmed that our planet was also likely to have had oceans
during most of the Hadean.
"A new picture of early Earth is emerging," Professor Harrison said. "We
have evidence that the Earth's early surface supported water -- the key
ingredient in making our planet habitable. We have evidence that this
water interacted with continent-forming magmas throughout the Hadean.
"And now we have evidence that massive amounts of continental crust were
produced almost immediately upon Earth formation. The Hadean Earth may
have looked much like it does today rather than our imagined view of a
desiccated world devoid of continents."
Professor Harrison and his team gathered their evidence from zircons, the
oldest known minerals on Earth. These ancient grains, typically about the
width of a human hair, are found only in the Murchison region of Western
Australia. The team analysed the isotopic properties of the element
hafnium in about 100 tiny zircons that are as old as 4.35 billion years.
Conventionally, it has been believed that the Earth's continents developed
slowly over a long period of time beginning about 4 billion years ago --
or 500 million years after the planet formed.
However, hafnium isotope variations produced by the radioactive decay of
an isotope of lutetium indicate many of these ancient zircons formed in a
continental setting within about 100 million years of Earth formation.
"The evidence points to almost immediate development of continent followed
by its rapid recycling back into the mantle via a process akin to modern
plate tectonics," according to Professor Harrison.
The isotopic imprint left on the mantle by early melting shows up again in
younger zircons -- providing evidence that they have tapped the same
source. This suggests that the amount of mantle processed to make
continent must have been enormous.
"The results are consistent with the Earth hosting a similar mass of
continental crust as the present day at 4.5-4.4 billion years.
"This is a radical departure from conventional wisdom regarding the Hadean
Earth," said Professor Harrison.
"But these ancient zircons represent the only geological record we have
for that period of Earth history and thus the stories they tell take
precedence over myths that arose in the absence of observational
evidence."
"The simplest explanation of all the evidence is that essentially from its
formation, the planet fell into a dynamic regime that has persisted to the
present day."
Australian National University
Canberra, Australia
Further Information:
Professor Mark Harrison
Director, Research School of Earth Sciences
T: 02 6125 2487
Amanda Morgan
Media Liaison
Tel: 02 6125 5575 / 0416 249 245
Friday, 18 November 2005
There was no such thing as hell on Earth
New ANU research is set to radically overturn the conventional wisdom that
early Earth was a hellish planet barren of continents.
An international research team led by Professor Mark Harrison of the
Research School of Earth Sciences analysed unique 4 to 4.35
billion-year-old minerals from outback Australia and found evidence that a
fringe theory detailing the development of continents during the first 500
million years of Earth history -- the Hadean ('hellish') Eon -- is likely
to be correct.
The research, published in the latest edition of Science, follows on from
results by Professor Harrison and his colleagues published earlier this
year that confirmed that our planet was also likely to have had oceans
during most of the Hadean.
"A new picture of early Earth is emerging," Professor Harrison said. "We
have evidence that the Earth's early surface supported water -- the key
ingredient in making our planet habitable. We have evidence that this
water interacted with continent-forming magmas throughout the Hadean.
"And now we have evidence that massive amounts of continental crust were
produced almost immediately upon Earth formation. The Hadean Earth may
have looked much like it does today rather than our imagined view of a
desiccated world devoid of continents."
Professor Harrison and his team gathered their evidence from zircons, the
oldest known minerals on Earth. These ancient grains, typically about the
width of a human hair, are found only in the Murchison region of Western
Australia. The team analysed the isotopic properties of the element
hafnium in about 100 tiny zircons that are as old as 4.35 billion years.
Conventionally, it has been believed that the Earth's continents developed
slowly over a long period of time beginning about 4 billion years ago --
or 500 million years after the planet formed.
However, hafnium isotope variations produced by the radioactive decay of
an isotope of lutetium indicate many of these ancient zircons formed in a
continental setting within about 100 million years of Earth formation.
"The evidence points to almost immediate development of continent followed
by its rapid recycling back into the mantle via a process akin to modern
plate tectonics," according to Professor Harrison.
The isotopic imprint left on the mantle by early melting shows up again in
younger zircons -- providing evidence that they have tapped the same
source. This suggests that the amount of mantle processed to make
continent must have been enormous.
"The results are consistent with the Earth hosting a similar mass of
continental crust as the present day at 4.5-4.4 billion years.
"This is a radical departure from conventional wisdom regarding the Hadean
Earth," said Professor Harrison.
"But these ancient zircons represent the only geological record we have
for that period of Earth history and thus the stories they tell take
precedence over myths that arose in the absence of observational
evidence."
"The simplest explanation of all the evidence is that essentially from its
formation, the planet fell into a dynamic regime that has persisted to the
present day."