Dinosaurs were Mesozoic land oviparous much less than Reptiles much greater
than with parasagittal members. Rich dinosaur egg deposits can be found wi
thin continental rocks from usually upper cretaceous, especially in the Sou
th of France, North of Spain, but also in China, Mongolia (Gobi desert), In
dia, and in North (Montana) and South America (Argentina). The study of fos
sil egg shells (especially microstructure) allows to define several ootaxon
s (parataxonomy) and to refine the stratigraphical chronology of the thick
and red clay and sandstone strata which characterize, especially in France
and Spain, the end of Mesozoic. Associated to the study of the layings (str
uctered or not), of the nests, and of the rare but precious in ovo embryos,
it suggests possible hypotheses on the parental behaviour of these fascina
ting animals. In addition, it enlightens the causes of their disappearance
which are still fiercely discussed.