SINEOAMPHISBAENA HEXATABULARIS, AN AMPHISBAENIAN (DIAPSIDA, SQUAMATA)FROM THE UPPER CRETACEOUS REDBEDS AT BAYAN-MANDAHU (INNER-MONGOLIA, PEOPLES-REPUBLIC-OF-CHINA), AND COMMENTS ON THE PHYLOGENETIC-RELATIONSHIPS OF THE AMPHISBAENIA
Xc. Wu et al., SINEOAMPHISBAENA HEXATABULARIS, AN AMPHISBAENIAN (DIAPSIDA, SQUAMATA)FROM THE UPPER CRETACEOUS REDBEDS AT BAYAN-MANDAHU (INNER-MONGOLIA, PEOPLES-REPUBLIC-OF-CHINA), AND COMMENTS ON THE PHYLOGENETIC-RELATIONSHIPS OF THE AMPHISBAENIA, Canadian journal of earth sciences, 33(4), 1996, pp. 541-577
Sineoamphisbaena hexatabularis Wu et al., 1993 is the earliest known a
mphisbaenian represented by well-preserved cranial and postcranial mat
erial. It reveals a mosaic of generalized lizard-like features and amp
hisbaenian characters. Most distinctive of the latter are features of
cranial consolidation adaptive for a fossorial way of life. Phylogenet
ic analyses strongly confirm the monophyly of the Amphisbaenia inclusi
ve of S. hexatabularis. The Amphisbaenia is diagnosed by a suite of ap
omorphic characters. The available evidence suggests a probable Amphis
baenia-Macrocephalosauridae relationship within the Scincomorpha. This
is supported primarily by the unique modifications of the palate and
temporal region of the skull. It is argued here that the Amphisbaenia
evolved in Central Asia during the Cretaceous, in response to the tran
sition from a perennial lacustrine environment to a dry, semiarid eoli
an environment. The relatively primitive morphology indicates that S.
hexatabularis was not permanently subterranean. The further derived mo
difications of later forms are associated with tunneling in an environ
ment of more compact soils.