NEW MATERIAL OF IKECHOSAURUS-SUNAILINAE (REPTILIA, CHORISTODIRA) FROMTHE EARLY CRETACEOUS LAOHONGDONG FORMATION, ORDOS BASIN, INNER-MONGOLIA, AND THE INTERRELATIONSHIPS OF THE GENUS
Db. Brinkman et Zm. Dong, NEW MATERIAL OF IKECHOSAURUS-SUNAILINAE (REPTILIA, CHORISTODIRA) FROMTHE EARLY CRETACEOUS LAOHONGDONG FORMATION, ORDOS BASIN, INNER-MONGOLIA, AND THE INTERRELATIONSHIPS OF THE GENUS, Canadian journal of earth sciences, 30(10-11), 1993, pp. 2153-2162
New material of Ikechosaurus sunailinae from the Early Cretaceous Laoh
ongdong Formation of the Ordos Basin, Inner Mongolia, People's Republi
c of China, is described. This material, which includes well-preserved
articulated skeletons and a series of isolated elements, demonstrates
that Ikechosaurus is more closely related to Champsosaurus than to Si
moedosaurus, sharing with Champsosaurus the presence of an elongate sn
out, anteriorly constricted parasphenoid with the foramen canalis caro
ticus internus located in or near the suture between the parasphenoid
and the pterygoid, an anterior extension of the anterior end of the ju
gal, and an elongate symphysis including the splenial. Ikechosaurus is
primitive relative to Champsosaurus in the anterior position of the i
nternal narial openings, in the less strongly flared temporal region w
ith the temporal openings placed largely above one another, in the abs
ence of fenestra in the occiput between the parietal and squamosal, an
d in the interpterygoid vacuity bordered posteriorly by the basispheno
id. Ikechosaurus and Tchoiria are at a similar grade of evolution, but
can be separated by details in the arrangement of bone forming the sk
ull roof.