The Maastrichtian is the last stage of the Cretaceous period, and therefore of the Mesozoic era. It spanned from 72.1 to 66 Ma (million years ago). The Maastrichtian Stage was preceded by the Campanian Stage and succeeded by the Danian Stage of the Paleogene Period. The Maastrichtian is named after the Dutch city Maastricht, where many fossils from the period—most notably those of the mosasaur—were discovered. Image:Mantell's Iguanodon restoration.jpg This article is a . You can help My English Wiki by expanding it.
Attributes | Values |
---|---|
rdfs:label |
|
rdfs:comment |
|
dcterms:subject | |
dbkwik:fossil/prop...iPageUsesTemplate | |
abstract |
|
is fossil range of |