Stay up to date with notifications from The Independent

Notifications can be managed in browser preferences.

Cold and wet: the latest theory about Mars

Reuters
Wednesday 20 May 2009 16:56 BST
Comments
(Reuters)

Your support helps us to tell the story

Our mission is to deliver unbiased, fact-based reporting that holds power to account and exposes the truth.

Whether $5 or $50, every contribution counts.

Support us to deliver journalism without an agenda.

Head shot of Louise Thomas

Louise Thomas

Editor

Mars may have once been both cold and wet, researchers said today, suggesting a freezing Martian landscape could still have produced water needed to sustain life.

There has been debate over the issue because with some researchers believing water likely formed many features of the planet's landscape and others pointing to evidence indicating that early Mars was cold with temperatures well below the freezing point of water.

Using a computer model, Alberto Fairen of Universidad Autonoma in Madrid and colleagues showed that both could have been possible because fluids containing dissolved minerals would have remained liquid at temperatures well below 273 degrees Kelvin - the freezing point of pure water.

"Our results are compatible with Mars lander and orbiter data and with climate modelling, and suggest a cold and wet early Mars," they wrote in the journal Nature.

The presence of water on Mars is a hot topic for scientists. They have presented strong evidence of huge deposits of frozen water at the Martian poles and point to geological features that indicate large bodies of water have flowed on the planet's surface in the distant past.

Other scientists have said images and computer simulations strongly suggest a landslide of sand and gravel are more likely explanations for the bright deposits in gullies that have been proposed as strong evidence of water flow.

Water is a key to the question of whether life, even in the form of microbes, ever existed on Mars. On Earth, all known forms of life require water.

Feiren and colleagues, including scientists from NASA's Ames Research Center in California, chose compositions based on weathered basalts for the Martian fluids in their model to match the chemical compositions of rock found at Mars landing sites.

This analysis showed that a number of minerals could have lowered the melting point of water in a frozen Martian environment and help explain the early Mars climate paradox, they said.

"The stability against freezing of Martian fluids can explain saline water activity on the surface of Mars at mean global temperatures well below 273 Kelvin," they wrote.

Join our commenting forum

Join thought-provoking conversations, follow other Independent readers and see their replies

Comments

Thank you for registering

Please refresh the page or navigate to another page on the site to be automatically logged inPlease refresh your browser to be logged in