Anthony Romilio, the University of Queensland's (UQ) PhD candidate led the study of thousands of small dinosaur tracks at Lark Quarry Conservation Park, central-western Queensland.
The 95-98 million-year-old tracks are preserved in thin beds of siltstone and sandstone deposited in a shallow river when the area was part of a vast, forested floodplain, he said.
"Many of the tracks are nothing more than elongated grooves and probably formed when the claws of swimming dinosaurs scratched the river bottom," Romilio said in a statement.
"Some of the more unusual tracks include 'tippy-toe' traces -- this is where fully buoyed dinosaurs made deep, near vertical scratch marks with their toes as they propelled themselves through the water," he said.
"It's difficult to see how tracks such as these could have been made by running or walking animals.
"If that was the case we would expect to see a much flatter impression of the foot preserved in the sediment."
Romilio said that similar looking swim traces made by different sized dinosaurs also indicated fluctuations in the depth of the water.
"The smallest swim traces indicate a minimum water depth of about 14 cm, while much larger ones indicate depths of more than 40 cm," Romilio said.
Unless the water level fluctuated, it's hard to envisage how the different sized swim traces could have been preserved on the one surface, he said.
"Some of the larger tracks are much more consistent with walking animals, and we suspect these dinosaurs were wading through the shallow water."
He also said the swimming dinosaur tracks at Lark Quarry belonged to small, two-legged herbivorous dinosaurs known as ornithopods.
