Koolasuchus
Koolasuchus | |
---|---|
Holotype mandibles | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Order: | †Temnospondyli |
Suborder: | †Stereospondyli |
Family: | †Chigutisauridae |
Genus: | †Koolasuchus Warren et al., 1997 |
Type species | |
†Koolasuchus cleelandi Warren et al., 1997
|
Koolasuchus is an extinct
History
The first fossil of temnospondyls found in the Strzelecki Group was NMV-PI56988, the posterior fragment of a jaw, collected around 1980. The jaw fragment was first mentioned in a 1986 publication by Anne Warren and R. Jupp, who did not definitively identify it as that of a temnospondyl due to the Cretaceous age of the specimen, much younger than any other known temnospondyl specimen at the time.
Koolasuchus was named in 1997 from the
Description
Koolasuchus was a large, aquatic temnospondyl, measuring up to 3 metres (9.8 ft) in length and weighing up to 500 kilograms (1,100 lb).[7][8][9] Like other chigutisaurids, it had a wide, rounded head and tabular horns projecting from the back of the skull.[10] Although represented by incomplete material, the skull was likely 65 centimetres (26 in) long.[11]
Koolasuchus is distinguished from other temnospondyls aside from Siderops and Hadrokkosaurus by having the ramus of the mandible "articular is excluded from the dorsal surface of the postglenoid area by a suture between the surangular and the prearticular", and is distinguished from those two taxa by a lack of coronoid teeth.[4]
Paleobiology
Koolasuchus inhabited rift valleys in southern Australia during the Early Cretaceous. During this time the area was below the Antarctic Circle, and temperatures were relatively cool for the Mesozoic. Based on the coarse-grained rocks in which remains were found, Koolasuchus likely lived in fast-moving streams. As a large aquatic predator, it was similar in lifestyle to crocodilians. Although eusuchians and kin were common during the Early Cretaceous, they were absent from southern Australia 120 million years ago, possibly because of the cold climate. By 110 Mya, represented by rocks in the Dinosaur Cove fossil locality, temperatures had warmed and crocodilians had returned to the area. These crocodilians likely displaced Koolasuchus, leading to its disappearance in younger rocks.[5]
References
- ^ Government of Victoria (13 January 2022). "Proclamations" (PDF). Victoria Government Gazette. p. G42. Retrieved 15 January 2022.
- ISSN 0311-5518.
- ISSN 0311-5518.
- ^ S2CID 247068275.
- ^ ISBN 978-0-253-33773-3.
- ^ "Life in the Shadows, Non-reptilian life in Mesozoic Australia". geocities. Archived from the original on 2008-02-20. Retrieved 2008-08-09.
- ISBN 978-0-643-10231-6.
- doi:10.1016/j.cretres.2009.06.003. Archived from the original(PDF) on 2011-07-19. Retrieved 2011-04-20.
- ISSN 0272-4634.
- S2CID 86107783.
- .