Martian meteorite may hold clues to water on the Red Planet
Published: 24 May 2010
Scientists are examining fragments of a Martian meteorite to try to establish when water was freely flowing on the red planet.
Scientists are examining fragments of a Martian meteorite to try to establish when water was freely flowing on the red planet.
Using powerful electron microscopes, Dr Martin Lee and colleagues at the University of Glasgow are painstakingly scanning a tiny chunk of a meteorite called Nakhla, which fell to Earth in 1911, reputedly hitting a dog in Egypt.
The team is looking for minerals within the meteorite that might have been carried there by water seeping through tiny pores in the rock which then crystallised.
Dr Lee, a senior lecturer in Geographical and Earth Sciences, said: “When the minerals crystallise they contain certain elements which are radioactive and therefore decay over time – potassium, for example, which decays to form argon.
"By measuring the levels of argon we are able to determine roughly when the minerals grew and hence when the water deposited them there.
“Meteorites like this offer the best way of analysing the Martian environment and geological history as there’s more of Mars on Earth than we could ever bring back from the planet itself.
"It’s possible that we might even find bits of water trapped within rocks, and maybe some traces of organic material within that."
The three-year project has been funded with £530,000 from the Science and Technology Facilities Council and is being undertaken in collaboration with Finlay Stuart, senior lecturer in isotope geoscience, and Darren Mark, research fellow at the Natural Environment Research Council Argon Isotope Facility at SUERC – the Scottish Universities Environmental Research Centre, based in East Kilbride, which is operated by the Universities of Glasgow and Edinburgh.
For more information contact Stuart Forsyth in the University of Glasgow Media Relations Office on 0141 330 4831 or email
s.forsyth@admin.gla.ac.uk
First published: 24 May 2010
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