We consider a specific continuous-spin Gibbs distribution μt=0 for a
double-well potential that allows for ferromagnetic ordering. We study the
time-evolution of this initial measure under independent diffusions. For `high
temperature' initial measures we prove that the time-evoved measure μt
is Gibbsian for all t. For `low temperature' initial measures we prove that
μt stays Gibbsian for small enough times t, but loses its Gibbsian
character for large enough t. In contrast to the analogous situation for
discrete-spin Gibbs measures, there is no recovery of the Gibbs property for
large t in the presence of a non-vanishing external magnetic field. All of
our results hold for any dimension d≥2. This example suggests more
generally that time-evolved continuous-spin models tend to be non-Gibbsian more
easily than their discrete-spin counterparts