Australian Fauna Prehistory

Eric Anglès

‘Historic account of Australian dinosaurs and thecodonts.’

‘Historic account of Australian dinosaurs and thecodonts.’

‘Historic account of Australian dinosaurs and thecodonts.’

‘Historic account of Australian dinosaurs and thecodonts.’

‘Historic account of Australian dinosaurs and thecodonts.’

Dinosaurs and Thecodonts

Dinosaurs and Thecodonts

Dinosaurs and Thecodonts

Dinosaurs and Thecodonts

Dinosaurs and Thecodonts

As we examine Australian geology, there is abundant evidence of ancient life that once thrived and dominated. We find layers of sedimentary material that tell a story of our past, our geological chronology and within these layers of this stratification, rests the fossil evidence of times past.

Carnarvon National Park is a hotspot for large carnivorous (not vegetarian) thecodonts (amphibians) that dominated the dinosaurs. Winton’s Lark Quarry Conservation Park, with over 3,300 dinosaur tracks, is the only known site of a dinosaur stampede on the planet.

By air, land and sea, thecodonts and dinosaurs ruled the Australian landscape, throughout the Triassic Period (206 to 248 Million Years Ago), Jurassic Period (144 to 206 Million Years Ago) and Cretaceous Period (65 to 144 Million Years Ago), over a period of 183 million years.

Prior to this time, Pangea, a supercontinent comprised of all the landmasses of all the continents of the earth, separated into two main supercontinents 200 to 180 million years ago, Laurasia of the Northern Hemisphere and Gondwana of the Southern Hemisphere (including Australia) and intersecting in time at the end of the Triassic Period and the beginning of the Jurassic Period.

Thecodonts, the close relation of the “modern day crocodile” are a direct ancestor of the dinosaurs and in most of Gondwana, during the Triassic Period, reptiles were the dominant form of life on land. In Australia, however, Thecodonts ruled as evidenced by the Crater Site at the Carnarvon National Park, containing fossils that date from the Triassic Period.

From here, an isolated island called Sahul, is a combined landmass including Australia, New Guinea and Tasmania that separated, 60, 000 years ago to form what we see today.

Below is a brief list of known thecodonts and dinosaurs that have graced our prehistory:

Thecodonts

Thecodonts

Thecodonts

Thecodonts

Thecodonts

Kalisuchus Rewanensis (carnivore)
230 MY | 3 M Long, 1 M High

Dicynodont (herbivore)
230 MY | 1 M Long, 0.5 M High

Dinosaurs

Dinosaurs

Dinosaurs

Dinosaurs

Dinosaurs

Ozraptor (carnivore)
170 MY | 3 M Long, 3 M High

Rhoetosaurus (herbivore)
190 MY | 15 M Long, 7 M High

Atlascopcosaurus (herbivore)
115 MY | 3 M Long, 1 M High

Australovenator (carnivore)
95 MY | 6 M Long, 2 M High

Austrosaurus (herbivore)
110 MY | 20 M Long, 4 M High

Diamantinasaurus (herbivore)
100 MY | 16 M Long, 2.5 M High

Fulgurotherium (herbivore)
110 MY | 1.5 M Long, 2 M High

Kakuru (omnivore)
120 MY | 2.5 M Long, 1 M High

Leaellynasaura (herbivore)
115 MY | 3.5 M Long, 1 M High

Minmi (herbivore)
119 MY | 2 M Long, 1 M High

Muttaburrasaurus (herbivore)
112 MY | 7 M Long, 2.5 M High

Qantassaurus (herbivore)
115 MY | 2 M Long, 1 M High

Rapator (carnivore)
105 MY | 9 M Long, 4 M High

Serendipaceratops (herbivore)
118 MY | 2 M Long, 1 M High

Timimus (omnivore)
106 MY | 3.5 M Long, 1.5 M High

Wintonotitan (herbivore)
100 MY | 15 M Long, 3 M High

Atlascopcosaurus loadsi

Australovenator wintonensis

Qantassaurus