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Craters on Vesta and Ceres could tell Jupiter's age
EUROPEAN PLANETARY SCIENCE CONGRESS NEWS RELEASE Posted: September 14, 2009

Crater patterns on Vesta and Ceres could help pinpoint when Jupiter began to form during the evolution of the early Solar System. A study modeling the cratering history of the largest two objects in the asteroid belt, which are believed to be among the oldest in the Solar System, indicates that the type and distribution of craters would show marked changes at different stages of Jupiter's development. Results will be presented by Dr. Diego Turrini at the European Planetary Science Congress in Potsdam, Germany, on Monday 14 September.
The study, carried out by scientists at the Italian National Institute
for Astrophysics in Rome, explored the hypothesis that one or both
objects formed during Jupiter's formation by modeling their cratering
histories during the birth of the giant planet. Their simulation
described Jupiter's formation in three stages: an initial accretion of
its core followed by a stage of rapid gas accretion. This is, in turn,
followed by a phase where the gas accretion slows down while the giant
planet reaches its final mass. During the last two phases Jupiter's
gravitational pull starts to affect more and more distant objects. For
each of these phases, the team simulated how Jupiter affected the
orbits of asteroids and comets from the inner and outer Solar System,
and the likelihood of them being moved onto a collision path with
Vesta or Ceres.
"We found that the stage of Jupiter's development made a big
difference on the speed of impacts and the origin of potential
impactors. When Jupiter's core approaches its critical mass, it causes
a sharp increase in low-velocity impacts from small, rocky bodies
orbiting nearby to Vesta and Ceres which lead to intense and uniform
crater distribution patterns. These low-speed collisions may have
helped Vesta and Ceres gather mass. Once Jupiter's core has formed and
the planet starts to rapidly accrete gas, it deflects more distant
objects onto a collision course with Ceres and Vesta and the impacts
become more energetic. Although rocky objects from the inner Solar
System are the dominant impactors at this stage, the higher energies
of collisions with icy bodies from the outer Solar System make the
biggest mark," said Dr. Turrini.
The third stage of Jupiter's formation is complicated by a period
known as the Late Heavy Bombardment, which occurred around 3.8 to 4.1
billion years ago. During this time a significant number of objects,
rich in organic compounds, from the outer Solar System were injected
on planet-crossing orbits with the giant planets and may have reached
the Asteroid Belt. In addition, Jupiter is thought to have migrated in
its orbit around this time, which would have caused an addition flux
of impactors on Vesta and Ceres.
The team will have an opportunity to confirm their results when NASA's
Dawn space mission reaches Vesta in 2011 and then flies on for a
further rendezvous with Ceres in 2015. Dawn will gather information on
the structure and the surface morphology of the two asteroids and send
back high-resolution images of crater patterns.
"If we can see evidence of an underlying intense, uniform crater
pattern, it will support the theory that one or both of these minor
planets formed during the final phases of Jupiter accretion, provided
that they aren't obliterated by the later heavy bombardment. Dawn will
also measure concentrations of organic material, which may give us
further information about the collisional history with organic-rich
objects from the outer Solar System," said Dr. Turrini.
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