Late Cretaceous terrestrial ecosystems in southern Europe are relatively po
orly known, although much progress has been made during the past decade, pr
incipally with regard to the microvertebrate components of these ecosystems
. The Maastrichtian terrestrial deposits of the Hateg Basin, at the eastern
most end of the South European archipelago and well known for reptilian fos
sils (e.g., turtles, crocodilians, pterosaurs and dinosaurs), have been tho
roughly screened during the past five years. Important microvertebrate asse
mblages, both quantitatively and qualitatively speaking, were found at Pui
(Sinpetru Formation), Tustea and, particularly, Valioara (Densus-Ciula Form
ation). Several new taxa are noted here for the first time for the Hateg Ba
sin, including gars, discoglossids, albanerpetontids, scincomorphan and ang
uimorphan lizards; dromaeosaurids and multituberculates are confirmed. Most
of the microvertebrate remains are poorly preserved and precise systematic
assignment has proved difficult. The Hateg fauna appears to be primitive a
nd endemic, with a Neopangean core composition, and suggests a composite pa
laeobiogeographic origin for the Late Cretaceous European ecosystems, confi
rming conclusions reached in studies of the larger vertebrates.