Big Bend National Park, TexasUnited States. National Park Service. Division of Publications
History
Big Bend National Park, Texas
United States. National Park Service. Division of Publications
Big Bend National Park (Tex.)
Tramping about on all fours and peaceably cropping land plants were
bizarre looking horned dinosaurs with turtle-like beaks. For their
weight they must have had the most powerful jaws of any backboned animal
that ever lived. Armored species included one that looked like a horned
toad the size of a dump truck. Another sported a huge lump of bone on
the end of its tail, still another a thick lump of bone above a brain no
bigger than the end of your little finger. The world’s largest
crocodile, a 15-meter (50-foot) creature with 15-centimeter (6-inch)
teeth, turned up in the park, but remarkably few bones of meat-eating
dinosaurs have ever been found. One of the Earth’s great mysteries is
why, at the top of their terrific form, the dominant dinosaurs died out?
This happened in a geologically short time all around the globe. Perhaps
it was because the highly specialized reptiles couldn’t cope with
changes in their environment as the world climate grew cooler and more
continental. No one really knows.
When the Age of Mammals began some 64 million years ago, Big Bend lay on
an alluvial floodplain where summers were moist and winters were mild.
Shallow rivers meandered between natural levees wooded with flowering
plants, sycamore, stinking cedar, and tree ferns. Garfish swam in rivers
and isolated ponds, while small lakes and swamps lingered on in meander
cutoffs and abandoned river channels. It was a land where seasonal
floods alternated with dry periods and where, during protracted dry
spells, treeless areas invaded the forest.
The Fossil Record
Garfish and turtles in the Rio Grande give us a hint about life here
50 million years ago. Then they swam in waters haunted by crocodiles
and visited by the modern horse’s earliest ancestor, Hyracotherium;
the hippo-like Coryhodon; and Phenacodus, an early species of ungulate
related to both hoofed and clawed mammals.
Fossils of these and other animals belie dry and barren Tornillo
Flat’s earlier Eocene life as a lushly vegetated landscape, as
depicted in this reconstruction.
At the time of this scene the dinosaurs (“terrible lizards”) had been
extinct for 15 million years. Their fossils occur here too. Remains of
the giant Pterosaur have been found. These “winged lizards” were
flying reptiles whose 11-meter (36-foot) wingspan exceeded that of
small jet fighters. The wing was a featherless membrane stretched out
from the reptile’s body to the tip of its greatly enlarged fourth
digit. Fossil remains of Brontosaurus, Allosaurus, Icthyosaur, and
others have been found. Fossil Ammonites (see page 67), related to
today’s sea-dwelling chambered nautilus, represent the even earlier
period when today’s Big Bend was covered by a shallow inland sea.
Sample fossils are displayed in a shelter off the Marathon entrance
road near Tornillo Creek bridge.
[Illustration: Pterosaur]
[Illustration: Extinct mammals.]
Public-domain text, read in full here on John Shaqi.
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