Kq. Gao et Lh. Hou, IGUANIANS FROM THE UPPER CRETACEOUS DJADOCHTA FORMATION, GOBI DESERT,CHINA, Journal of vertebrate paleontology, 15(1), 1995, pp. 57-78
Newly discovered lizard fossils from the Upper Cretaceous Djadochta Fo
rmation in the Gobi Desert of Inner Mongolia China, include early igua
nids and agamids that are taxonomically and biogeographically importan
t. Two iguanids reported here, Anchaurosaurus gilmorei, gen. et sp. no
v. and Xihaina aquilonia, gen. et sp. nov.. document the geologically
earliest record of the family from Asia, and extend the fossil record
of the group by 11-13 Myr. The geological age and primitive structure
of these Cretaceous iguanids, coupled with other material of the same
group from the slightly younger Barun Goyot Formation, suggest that th
e group had a long evolutionary history on ?he northern continents, an
d hence, challenge the widely accepted South American origin hypothesi
s of the Iguanidae (sensu late). Three taxa of agamids are documented
in the new collection: Mimeosaurus crassus Gilmore, 1943, Priscagama g
obiensis Borsuk-Bialynicka and Moody, 1984, and Pleurodontagama aenigm
atodes Borsuk-Bialynicka and Moody, 1984. Several well-preserved skull
s of M. crassus show a structure that requires a taxonomic revision of
this genus. Priscagama and Pleurodontagama are poorly documented. It
has been long held that the iguanids and agamids have different center
s of origin, and that the two groups have been separated geographicall
y from one another since the beginning of their evolution. With the di
scoveries of new iguanids and agamids together from the Gobi, it is no
w dear that the two families were sympatric during their early evoluti
on on the northern continents.