'Dinosaur Dance Floor' Discovered in Arizona

More than 1,000 dinosaur footprints along with tail-drag marks have been discovered along the Arizona-Utah border. The incredibly rare concentration of beastly tracks likely belonged to at least four different species of dinosaurs, ranging from youngsters to adults.

The tracks range in length from 1 to 20 inches (2.5 to 51 centimeters).

"The different size tracks may tell us that we are seeing mothers walking around with babies," said researcher Winston Seiler, a geologist at the University of Utah.

The tracks were laid about 190 million years ago in what is now the Vermilion Cliffs National Monument.

"There must have been more than one kind of dinosaur there," said researcher Marjorie Chan, professor and chair of geology and geophysics at the University of Utah. "It was a place that attracted a crowd, kind of like a dance floor."

While the site is covered in sand dunes now, the researchers say the tracks are within what was a network of wet, low watering holes between the dunes.

In fact, the tracks provide more evidence of wet intervals during the Early Jurassic Period, when the U.S. Southwest was covered with a field of sand dunes larger than the Sahara Desert.

Chan and her colleagues, including Seiler, described the dinosaur track site in the October issue of the international paleontology journal Palaios.

By studying the shapes and sizes of the tracks, Seiler suggests four dinosaur species gathered at the watering hole, though the researchers have yet to match the prints with specific species.

Currently, the tracks are named for their particular shapes and include:

Numerous dinosaur track sites have been found in the western United States and elsewhere around the world.

For instance, tracks from a herd of 11 giant sauropod dinosaurs were discovered in the ancient coastal mudflats of Yemen. But the new discovery is rare in the density of tracks.

"Unlike other trackways that may have several to dozens of footprint impressions, this particular surface has more than 1,000," Seiler and Chan write.

Chan first visited the site of the dinosaur tracks in 2005 with a U.S. Bureau of Land Management ranger who was puzzled by them. Chan initially called them potholes, which are erosion features common in desert sandstone. "But I knew that wasn't the whole story because of the high concentration and because they weren't anywhere else nearby but along that one surface."

One unnamed reviewer of the Palaios study still believes the holes are erosion features, according to a statement released today by the University of Utah.

In 2006, Seiler saw the tracks and had similar thoughts.

"At first glance, they look like weathering pits — a field of odd potholes," he said. "But within about five minutes of wandering around, I realized these were dinosaur footprints."

Source  Fox News. 

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