Data from meteorites and NASA’s Spirit rover has revealed new information about the chemical composition and evolution of Mars, suggesting that Mars had an oxygen-rich atmosphere 4 billion years ago.
Differences between Martian meteorites and rocks examined by a NASA rover can be explained if Mars had an oxygen-rich atmosphere 4 billion years ago – well before the rise of atmospheric oxygen on Earth 2.5 billion years ago.
Scientists from Oxford University investigated the compositions of Martian meteorites found on Earth and data from NASA’s ‘Spirit’ rover that examined surface rocks in the Gusev crater on Mars. The fact that the surface rocks are five times richer in nickel than the meteorites was puzzling and had cast doubt on whether the meteorites are typical volcanic products of the red planet.
‘What we have shown is that both meteorites and surface volcanic rocks are consistent with similar origins in the deep interior of Mars but that the surface rocks come from a more oxygen-rich environment, probably caused by recycling of oxygen-rich materials into the interior,’ said Professor Bernard Wood, of Oxford University’s Department of Earth Sciences, who led the research reported in this week’s Nature.
‘This result is surprising because while the meteorites are geologically ‘young’, around 180 million to 1.4 billion years old, the Spirit rover was analyzing a very old part of Mars, more than 3.7 billion years old.’
Whilst it is possible that the geological composition of Mars varies immensely from region to region the researchers believe that it is more likely that the differences arise through a process known as subduction – in which material is recycled into the interior. They suggest that the Martian surface was oxidized very early in the history of the planet and that, through subduction, this oxygen-rich material was drawn into the shallow interior and recycled back to the surface during eruptions 4 billion years ago. The meteorites, by contrast, are much younger volcanic rocks that emerged from deeper within the planet and so were less influenced by this process.
Professor Wood said: ‘The implication is that Mars had an oxygen-rich atmosphere at a time, about 4 billion years ago, well before the rise of atmospheric oxygen on earth around 2.5 billion years ago. As oxidation is what gives Mars its distinctive color it is likely that the ‘red planet’ was wet, warm and rusty billions of years before Earth’s atmosphere became oxygen rich.’
A report of the research, entitled ‘Volcanism on Mars controlled by early oxidation of the upper mantle’, is published in this week’s Nature. The research was carried out by James Tuff, Dr Jon Wade, and Professor Bernard Wood at Oxford University’s Department of Earth Sciences and was supported by the Science and Technology Facilities Council (STFC) and the European Research Council.
Publication: J. Tuff, J. Wade & B. J. Wood, “Volcanism on Mars controlled by early oxidation of the upper mantle,” Nature 498, 342–345, (20 June 2013); doi:10.1038/nature12225
Source: Oxford University