Koolasuchus

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Koolasuchus
Temporal range: Early Cretaceous (Aptian), 120  Ma
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Koolasuchus mandibles.jpg
Holotype mandibles
Scientific classification OOjs UI icon edit-ltr.svg
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 genus of brachyopoid temnospondyl in the family Chigutisauridae. Fossils have been found from Victoria, Australia and date back 125-120 million years ago to Barremian-Aptian stages of the Early Cretaceous. Koolasuchus is the youngest known temnospondyl. It is known from several fragments of the skull and other bones such as vertebrae, ribs, and pectoral elements. The type species Koolasuchus cleelandi was named in 1997. K. cleelandi was adopted as the fossil emblem for the state of Victoria, Australia on 13 January 2022. [1]

Contents

History

Life restoration Koolasuchus.png
Life restoration

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. [2] In 1991, additional remains were reported including NMV-PI86040, an intercentrum (part of the vertebra) and NMV-PI86101, an isolated skull roof bone, likely representing either a frontal, a supratemporal or a parietal. The intercentrum unquestionably confirmed that temnospondyls were present in the Strzelecki Group. The morphology of the skull roof bone lead to the authors suggesting that the temnospondyl was either a member of Plagiosauridae or Brachyopoidea. [3]

Koolasuchus was named in 1997 from the Aptian aged Wonthaggi Formation of Strzelecki Group in Victoria. [4] It is known from four fragments of the lower jaw and several postcranial bones, including ribs, vertebrae, a fibula, and parts of the pectoral girdle. A jawbone was found in 1978 in a fossil site known as the Punch Bowl near the town of San Remo. Later specimens were found in 1989 on the nearby Rowell's Beach. A partial skull is also known but has not been fully prepared. Koolasuchus was named for the palaeontologist Lesley Kool. The name is also a pun on the word "cool" in reference to the cold climate of its environment. [5] The type species K. cleelandi is named after geologist Mike Cleeland. [6]

Description

Size estimation of Koolasuchus based on Siderops Koolasuchus scaling.png
Size estimation of Koolasuchus based on Siderops

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

Restoration of Koolasuchus swimming through a stream of water Koolasuchus in a stream.jpg
Restoration of Koolasuchus swimming through a stream of water

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]

Related Research Articles

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"Labyrinthodontia" is an informal grouping of extinct predatory amphibians which were major components of ecosystems in the late Paleozoic and early Mesozoic eras. Traditionally considered a subclass of the class Amphibia, modern classification systems recognize that labyrinthodonts are not a formal natural group (clade) exclusive of other tetrapods. Instead, they consistute an evolutionary grade, ancestral to living tetrapods such as lissamphibians and amniotes. "Labyrinthodont"-grade vertebrates evolved from lobe-finned fishes in the Devonian, though a formal boundary between fish and amphibian is difficult to define at this point in time.

<span class="mw-page-title-main">Temnospondyli</span> Ancestors of modern amphibians adapted to life on land

Temnospondyli or temnospondyls is a diverse ancient order of small to giant tetrapods—often considered primitive amphibians—that flourished worldwide during the Carboniferous, Permian and Triassic periods, with fossils being found on every continent. A few species continued into the Jurassic and Early Cretaceous periods, but all had gone extinct by the Late Cretaceous. During about 210 million years of evolutionary history, they adapted to a wide range of habitats, including freshwater, terrestrial, and even coastal marine environments. Their life history is well understood, with fossils known from the larval stage, metamorphosis and maturity. Most temnospondyls were semiaquatic, although some were almost fully terrestrial, returning to the water only to breed. These temnospondyls were some of the first vertebrates fully adapted to life on land. Although temnospondyls are amphibians, many had characteristics such as scales and armour-like bony plates that distinguish them from the modern soft-bodied lissamphibians.

<span class="mw-page-title-main">Stereospondyli</span> Extinct suborder of amphibians

The Stereospondyli are a group of extinct temnospondyl amphibians that existed primarily during the Mesozoic period. They are known from all seven continents and were common components of many Triassic ecosystems, likely filling a similar ecological niche to modern crocodilians prior to the diversification of pseudosuchian archosaurs.

<i>Eryosuchus</i> Extinct genus of temnospondyls

Eryosuchus is an extinct genus of capitosauroid temnospondyl from the Middle Triassic of northern Russia. It was a very large predator: the largest specimen known could reach up to 3.5 m (11.5 ft) in length, with a skull over 1 m long.

<i>Cyclotosaurus</i> Extinct genus of temnospondyls

Cyclotosaurus is an extinct genus of temnospondyl within the family Mastodonsauridae. It was of great size for an amphibian, had an elongated skull up to 56 cm (22 in).

<span class="mw-page-title-main">Chigutisauridae</span> Extinct family of temnospondyls

Chigutisauridae is an extinct family of large temnospondyls. The only genera recognized as belonging to Chigutisauridae at the current time are all from Gondwana. Chigutisaurids first appeared during the Early Triassic in Australia. During the Late Triassic they became widely distributed in Gondwana, with fossils found in South Africa, India and South America. Koolasuchus from the Early Cretaceous of Australia represents the youngest known temnospondyl.

<i>Pelorocephalus</i> Extinct genus of amphibians

Pelorocephalus is an extinct genus of chigutisaurid temnospondyls. It is known from the Late Triassic (Carnian) Cacheutá Formation of the Cuyo Basin and the Ischigualasto Formation of the Ischigualasto-Villa Unión Basin, both in northwestern Argentina. Four species are currently recognized: the type species P. mendozensis, which was named in 1944, P. tenax, which was named in 1949 as a species of Chigutisaurus and reassigned to Pelorocephalus in 1999, and P. cacheutensis, which was named in 1953 as another species of Chigutisaurus and reassigned to Pelorocephalus along with P. tenax. A fourth species, P. ischigualastensis, was named in 1975 after the formation it was found in. The species P. tunuyanensis was named in 1948 but has since been synonymized with P. mendozensis.

<i>Siderops</i> Extinct genus of amphibians

Siderops is an extinct genus of chigutisaurid temnospondyl from Early Jurassic of Australia, containing the species S. kehli.

<span class="mw-page-title-main">Brachyopoidea</span> Extinct superfamily of temnospondyls

Brachyopoidea is a superfamily of temnospondyls that lived during the Mesozoic. It contains the families Brachyopidae and Chigutisauridae. The earliest records of brachyopids are from the Lower Triassic in Australia. The latest-surviving member of the superfamily is the chigutisaurid Koolasuchus from the Early Cretaceous of Australia.

<span class="mw-page-title-main">Lydekkerinidae</span> Extinct family of temnospondyls

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<span class="mw-page-title-main">Mastodonsauridae</span> Extinct family of temnospondyls

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<span class="mw-page-title-main">Limnarchia</span> Extinct clade of temnospondyls

Limnarchia is a clade of temnospondyls. It includes the mostly Carboniferous-Permian age Dvinosauria and the mostly Permian-Triassic age Stereospondylomorpha. The clade was named in a 2000 phylogenetic analysis of stereospondyls and their relatives. Limnarchia means "lake rulers" in Greek, in reference to their aquatic lifestyles and long existence over a span of approximately 200 million years from the Late Carboniferous to the Early Cretaceous. In phylogenetic terms, Limnarchia is a stem-based taxon including all temnospondyls more closely related to Parotosuchus than to Eryops. It is the sister group of the clade Euskelia, which is all temnospondyls more closely related to Eryops than to Parotosuchus. Limnarchians represent an evolutionary radiation of temnospondyls into aquatic environments, while euskelians represent a radiation into terrestrial environments. While many euskelians were adapted to life on land with strong limbs and bony scutes, most limnarchians were better adapted for the water with poorly developed limbs and lateral line sensory systems in their skulls.

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<i>Galleonosaurus</i> Extinct genus of dinosaurs

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References

  1. Government of Victoria (13 January 2022). "Proclamations" (PDF). Victoria Government Gazette. p. G42. Retrieved 15 January 2022.
  2. Jupp, R.; Warren, A. A. (1986-01-01). "The mandibles of the Triassic temnospondyl amphibians". Alcheringa: An Australasian Journal of Palaeontology. 10 (2): 99–124. doi:10.1080/03115518608619164. ISSN   0311-5518.
  3. Warren, A.A.; Kool, L.; Cleeland, M.; Rich, T.H.; Rich, P. Vickers (January 1991). "An Early Cretaceous labyrinthodont". Alcheringa: An Australasian Journal of Palaeontology. 15 (4): 327–332. doi:10.1080/03115519108619027. ISSN   0311-5518.
  4. 1 2 Warren, A.A.; Rich, P.V.; Rich, T.H. (1997). "The last, last labyrinthodonts?". Palaeontographica A. 247 (1–4): 1–24. doi:10.1127/pala/247/1997/1. S2CID   247068275.
  5. 1 2 Rich, T.H.V.; Rich, P.V. (2000). Dinosaurs of Darkness. Bloomington: Indiana University Press. p. 222. ISBN   978-0-253-33773-3.
  6. "Life in the Shadows, Non-reptilian life in Mesozoic Australia". geocities. Archived from the original on 2008-02-20. Retrieved 2008-08-09.
  7. Kear, Benjamin P.; Hamilton-Bruce, Robert J. (2011-04-19). Dinosaurs in Australia: Mesozoic Life from the Southern Continent. Csiro Publishing. ISBN   978-0-643-10231-6.
  8. Martin, A.J. (2009). "Dinosaur burrows in the Otway Group (Albian) of Victoria, Australia, and their relation to Cretaceous polar environments" (PDF). Cretaceous Research. 30 (2009): 1223–1237. doi:10.1016/j.cretres.2009.06.003. Archived from the original (PDF) on 2011-07-19. Retrieved 2011-04-20.
  9. Hart, Lachlan J.; Gee, Bryan M.; Smith, Patrick M.; McCurry, Matthew R. (2023-08-03). "A new chigutisaurid (Brachyopoidea, Temnospondyli) with soft tissue preservation from the Triassic Sydney Basin, New South Wales, Australia". Journal of Vertebrate Paleontology. doi: 10.1080/02724634.2023.2232829 . ISSN   0272-4634.
  10. Warren, A.; Marsicano, C. (2000). "A phylogeny of the Brachyopoidea (Temnospondyli, Stereospondyli)". Journal of Vertebrate Paleontology. 20 (3): 462–483. doi:10.1671/0272-4634(2000)020[0462:APOTBT]2.0.CO;2. hdl: 11336/93649 . S2CID   86107783.
  11. Steyer, J.S.; Damiani, R. (2005). "A giant brachyopoid temnospondyl from the Upper Triassic or Lower Jurassic of Lesotho". Bulletin de la Société Géologique de France. 176 (3): 243–248. doi:10.2113/176.3.243.