The evolutionary patterns shown by continental fossil plant assemblages dur
ing extinction and palaeodiversification events are quite different from th
e ones evidenced in the animal realm. These events are, moreover, rarely sy
nchronous for plants and animals. A global approach to the Phanerozoic and,
more importantly, a study of the terrestrial flora during the Jurassic and
the Early Cretaceous at a different scale, illustrates these points. Plant
evolution is not, however, independant of ecological factors, either bioti
c or abiotic. The diversification of Angiosperms and Pinaceae during the Me
sozoic is, therefore, significant. Based on their biological peculiarities,
plants have speciation possibilities quite different from those of animals
. Although well known by the geneticists, these possibilities are regularly
underestimated by phylogeneticists, though they are evidences that evoluti
on can be reticulate.