Da. Adams, TRINACROMERUM BONNERI, NEW SPECIES, LAST AND FASTEST PLIOSAUR OF THE WESTERN INTERIOR SEAWAY, The Texas journal of science, 49(3), 1997, pp. 179-198
The Pierre Shale represents the final days of the Western Interior Sea
way before its regression at the end of the Mesozoic, and records the
last of the marine reptiles that dominated the seas much as their cont
emporary dinosaur counterparts dominated the land. Trinacromerum bonne
ri, n. sp., is the first pliosaur (short-necked plesiosaur) to be desc
ribed from this formation in the northern Great Plains; as such it rep
resents the final radiation of polycotylid pliosaurs in North America.
Pliosaurs have long been regarded as particularly high-speed swimmers
, but T. bonneri carried this trend to an extreme. Development of the
longest wingfins known in pliosaurs maximized its velocity. Unique lim
b and vertebral structures resisted pressures of the surrounding water
that were generated by its own swimming velocity. Such adaptations in
clude tongue-and-groove articular surfaces between critical limb eleme
nts and highly interlocking cervical vertebrae.