During the Permian Period the area that is now Palo Duro Canyon State
Park, was a nearly-flat land surface along the edge of a restricted sea.
The scarcity of fossils in the Quartermaster Formation indicates that
plant and animal life was sparse. The environment was probably unsuited
for plant life. It is thought that groundwater near the surface
evaporated, leaving large amounts of salt as a residue. Since plants
could not grow, animals would not have frequented the area either.
[Illustration: Figure 6. Headward erosion by the Pecos, Colorado,
Brazos, Red and Canadian Rivers isolate the High Plains by the end
of the Pleistocene (10,000 years ago) and cut Palo Duro Canyon.]
Fossils and rocks of the Tecovas Formation indicate that the sediments
were deposited in a swamp and stream environment (Figure 7). As time
went on and the land continued rising, the climate became drier and some
of the earlier life forms disappeared.
Remains of _Metoposaurus_ (‘_Buettneria_’), the last of a long line of
giant amphibians, are found here. These animals lived in large ponds.
_Metoposaurus_ buried themselves in the bottom of a pond and waited for
fish to pass. With the aid of a third eye in the middle of its head, the
animal could direct its huge mouth to its prey. _Metoposaurus_ was so
bulky that it is thought that it did not leave the water because its
weak legs could not support its weight on land.
Living in shallower areas of the swamp were a group of semiaquatic
reptiles known as phytosaurs. Phytosaurs looked very much like giant
crocodiles with a nostril on the top of their heads, which permitted
them to lie submerged just below the surface of the water. They probably
fed on fish and smaller reptiles. Phytosaurs reached a length of 50
feet.
A heavily armored aetosaur, _Desmatosuchus_ also lived in the Park area
during the Triassic. They attained a length of about 10 feet. These
reptiles probably were herbivorous (plant eating). A unique feature of
_Desmatosuchus_ was a fringe of backward-pointing horns around their
necks. These possibly served to protect them from the carnivorous (meat
eating) phytosaurs.
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