2.229 billion years: Scientists date world's oldest meteor crater

phys.org | 11/20/2019 | Staff
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A crater in western Australia was formed by a meteor strike more than 2.2 billion years ago and is the world's oldest known impact site, new research published Wednesday shows.

The study marks the first time that the Yarrabubba crater has been precisely dated, at 2.229 billion years old, and means it is 200 million years older than any similar site known on Earth.

Revelation - Possibility - Impact - Earth - Climate

The revelation also raises the intriguing possibility that the massive impact could have significantly altered the Earth's climate, helping end a period of global "deep freeze".

Scientists had long suspected that Yarrabubba, in a remote part of the outback, dated back several billion years.

Craters - Sites - Erosion - Events - Earthquakes

But dating ancient craters is not easy: the sites tend to be poorly preserved because erosion and tectonic events such as earthquakes have "progressively erased into the geologic past", the researchers wrote in their paper, published in the journal Nature Communications on Wednesday.

And even where craters are still present, determining their age is complex.

Date - Yarrabubba - Team - Evidence - Shock

To date Yarrabubba precisely, the team hunted for evidence of "shock recrystallisation" in minerals at the site—essentially where the massive impact of the meteor had altered the structure of materials including zircon and monazite.

'SHRIMP dating'

Record - Minerals - Microscopic - Grains - Scanning

But finding that record in the minerals involved searching for microscopic grains, using a high-tech scanning process known as Sensitive High Resolution Ion Micro Probe or SHRIMP dating.

Once identified, uranium in the grains helped the scientists determine a precise date, which they found coincided with a period when the planet emerged from a global deep freeze known as "Snowball Earth".

Deposits - Rock - Record - Years - Yarrabubba

"Glacial deposits are absent from the rock record for around 400 million years after the Yarrabubba impact," Chris Kirkland, a professor at Curtin University's School of Earth and Planetary Sciences who was involved in the study, told AFP.

"The impact fits within the context of Earth moving out of frigid conditions."

The...
(Excerpt) Read more at: phys.org
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