Mars, Earth and Moon from 'unique planetary nursery' (Forwarded)



Press Office
University of Oxford
Oxford, U.K.

Contact: Press Office
telephone: 01865 280528
fax: 01865 280535

25 Mar 08

Mars, Earth and Moon from 'unique planetary nursery'

A study of meteorites suggests that Mars, the Earth and the Moon share a
common composition from 'growing up' in a unique planetary nursery in the
inner solar system.

The finding could lead to a rethink of how the inner solar system formed.

The international team of scientists, which includes Professor Alex Halliday
from Oxford University's Department of Earth Sciences, report in Nature how
they analysed 16 meteorites that fell to Earth from Mars. They found that
the amounts of neodymium-142 these contain are subtly different from those
of objects found in the asteroid belt. This isotopic fingerprint is proof
that the chemistry of the inner solar system was different even for elements
that are hard to vapourise.

Professor Halliday said: "The Earth, Moon and Mars appear to have formed in
a part of the inner solar system with a ratio of samarium to neodymium that
is around 5 per cent more than could be found in the asteroid belt. It is
this 'family resemblance' that we see today when we compare oceanic basalts
from Earth with Moon rocks and Martian meteorites. Such differences may be
the result of the erosion of planetary crusts during formation events,
alternatively, this composition arose from the sorting of clouds of
partially melted droplets or grains -- known as 'chondrules'."

Earth has a long geological history of recycling the materials that make up
its crust and mantle, which could help explain why its composition is
different from that of other planetary bodies -- it could, for example, have
deeply buried reservoirs of certain elements. However Mars and the Moon are
believed to have been nothing like as active during their lifespan: making
it much more difficult for any theory involving material recycling to
explain why their composition should differ from other planetary bodies and
yet have such similarities with the composition of the Earth.

Professor Halliday said: "What our results suggest is that the sorting of
the elements that make up these planets may have happened at a much earlier
stage than had been believed. It may even be that this sorting happened in
the accretion disk out of which Mars and the early Earth first formed. What
we can say is that the composition of these worlds is inconsistent with them
simply forming out of large 'lumps' of stony meteorites, like those we see
today in the asteroid belt."
.



Relevant Pages

  • Re: Bigelows BA300 as a Martian spaceship?
    ... Smithsonian archives with the superior William Moon mind that knows ... cost more propellant *and* keep you in space longer. ... to a: earth escape trajectory. ... A Mars Free Return Trajectory entails boosting with enough speed to ...
    (sci.space.policy)
  • Re: We choose to go to the moon
    ... place and the surface of the moon is even worse. ... The telemetry it sends back to Earth can be used to decide on the best course of action - that is pretty much how it is done today. ... Using robots to work in hostile environments where we cannot function is standard practice on Earth. ... On the surface of Mars you need decent sensors and telemetry. ...
    (sci.astro.amateur)
  • Re: Ice on Mars South Pole Is Deep and Wide
    ... they should be talking to us about our somewhat salty old moon that's ... life might have once upon a time existed on Mars, ... An Earth w/o magnetosphere, w/o moon is simply a much larger Mars. ... Even if we're talking 1% Earth wet, Mars is missing most of its salt. ...
    (sci.space.policy)
  • Re: Giant alien head on the tarmac
    ... Xerxes, was the king of Mars, ... And so my mother, who married Zeus, was one of Xerxes' daughters. ... So about 65 million years ago, they fly the moon here to earth. ...
    (sci.astro)
  • Re: planetary heat losses
    ... which shines down upon their flat Earth, ... That way the moon could have been completely molten all at ... after its formation when none of the other planets have been able to ... of whatever core energy, such as per whatever's leaving its physically ...
    (sci.space.history)