''Entradasuchus'' (meaning "Entrada
andstone and Ranchcrocodile") is a
genus of
crocodyliform, an early member of the group including
crocodilians. The only known specimen was found in rocks of the
Middle Jurassic
The Middle Jurassic is the second epoch of the Jurassic Period. It lasted from about 174.1 to 163.5 million years ago. Fossils of land-dwelling animals, such as dinosaurs, from the Middle Jurassic are relatively rare, but geological formations co ...
Entrada Sandstone
The Entrada Sandstone is a formation in the San Rafael Group found in the U.S. states of Wyoming, Colorado, northwest New Mexico, northeast Arizona, and southeast Utah. Part of the Colorado Plateau, this formation was deposited during the Jurass ...
of Entrada Ranch,
Grand County,
Utah. Middle Jurassic terrestrial
tetrapods are very rare, and ''Entradasuchus'' was the first unequivocal North American Middle Jurassic nonmarine tetrapod known from body fossils when it was described (1995).
Description
''Entradasuchus'' is
based on CU-MWC 183-11, a skeleton including at least the upper surfaces of the skull, articulated
armor scutes from the neck to the tail, and some limb bones, all preserved in top (
dorsal) view. The exact composition of the specimen was unknown at the time of its description, because it is preserved in
sandstone that is harder than the
calcite
Calcite is a Carbonate minerals, carbonate mineral and the most stable Polymorphism (materials science), polymorph of calcium carbonate (CaCO3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on ...
that has replaced the bones, which makes preparation difficult. Additionally, much of the visible part of the skeleton is represented by mold impressions of eroded bones. The block containing the specimen weathered from canyon walls and probably came from the middle Moab Member of the Entrada Sandstone, dated to the very late middle
Callovian of the Middle Jurassic. The Moab Member of the Entrada Sandstone represents an inland dune (
eolian) setting.
[
The skull of CU-MWC 183-11 is distinguished by the width of the posterior portion. Approximately 42 pairs of scutes ran down the midline of the back. The first pair behind the skull were square, but those on the back and tail were rectangular and had short spiny projections on their posterior outside corners. These spines inspired the name of the type species: ''E. spinosus''. CU-MWC 183-11 was not a large animal, with a skull only a few centimeters or inches long. This small size and the form of the skull could indicate it was a juvenile, but the fusion of the parietals in the skull and the generally small size of animals found in settings like the upper Entrada Sandstone suggest it was an adult. Adrian Hunt and ]Martin Lockley
Martin G. Lockley (born 1950) is a Welsh palaeontologist. He was educated in the United Kingdom where he obtained degrees (BSc and PhD) and post-doctoral experience in Geology in the 1970s. Since 1980 he has been a professor at the University ...
, who described ''Entradasuchus'' in 1995, classified it as Crocodyliformes '' incertae sedis''.[
The type specimen is curated at the Museum of Western Colorado in Fruita, Colorado.
]
References
{{Taxonbar, from=Q5380653
Middle Jurassic reptiles of North America
Middle Jurassic crocodylomorphs
Prehistoric pseudosuchian genera