Winton Formation
Stratigraphic range: Late Albian-Early Turonian
~
TypeGeological formation
Unit ofRolling Downs Group
UnderliesUnconformity with Quaternary Lake Eyre Basin sediments
OverliesMackunda Formation,[1] Oodndatta Formation
Thickness<100 m (330 ft) at the margin
1,200 m (3,900 ft) in the centre
Lithology
PrimarySandstone, siltstone, claystone
OtherConglomerate, coal
Location
Coordinates22°18′S 143°06′E / 22.3°S 143.1°E / -22.3; 143.1
Approximate paleocoordinates51°48′S 134°06′E / 51.8°S 134.1°E / -51.8; 134.1
Region Queensland
Country Australia
ExtentEromanga Basin
Type section
Named forWinton, Queensland
Named byWhitehouse
LocationBores in and around Winton
Year defined1955

Formation distribution within Australia

The Winton Formation is a Cretaceous geological formation in central-western Queensland, Australia. It is late Albian to early Turonian in age.[2] The formation blankets large areas of central-western Queensland. It consists of sedimentary rocks such as sandstone, siltstone and claystone. The sediments that make up these rocks represent the remnants of the river plains that filled the basin left by the Eromanga Sea - an inland sea that covered large parts of Queensland and central Australia at least four times during the Early Cretaceous. Great meandering rivers, forest pools and swamps, creeks, lakes and coastal estuaries all left behind different types of sediment.

In some areas, the Winton Formation is over 400 metres thick. To bring with them such a huge amount of sediment, the rivers that flowed across these plains must have been comparable in size to the present-day Amazon or Mississippi rivers. As more and more sediment was brought in, the margins of the inland sea slowly contracted. By around 95 million years ago, the deposition was complete and the inland sea would never be seen again.

By virtue of its age and the environmental conditions under which the rocks it consists of were deposited, the Winton Formation represents one of the richest sources of dinosaur fossils anywhere in Australia.

Fauna

A fossil footprint-(ichnite), Wintonopus, found with two other dinosaur genera footprints at the Lark Quarry in Australia, c.f. Tyrannosauropus and Skartopus, have been found in the Winton Formation.

Dipnoi

Dipnoi of the Winton Formation
TaxaSpeciesPresenceMaterialNotesImages
Metaceratodus wollastoni[3] M. wollastoni Isolated tooth plates
Metaceratodus ellioti[3] M. ellioti Isolated tooth plates
Metaceratodus bonei[3] M. bonei Isolated tooth plates

Actinopterygii

Actinopterygii of the Winton Formation
TaxaSpeciesPresenceMaterialNotesImages
Cladocyclus[4] C. geddesi Nearly complete skull and partial skeleton

Squamates

Squamates of the Winton Formation
TaxaSpeciesPresenceMaterialNotesImages
Varanoidea[5] Indeterminate A damaged posterior trunk vertebra Originally considered as dolichosaurid (cf. Coniasaurus),[6] but reassigined

Crocodyliformes

Crocodyliformes of the Winton Formation
TaxaSpeciesPresenceMaterialNotesImages
Confractosuchus[7] C. sauroktonos Nearly complete skeleton preserving a juvenile ornithopod in its abdomen
Isisfordia I. duncani Nearly complete skeleton and partial skull, referred complete skull

Dinosaurs

Dinosaurs of the Winton Formation
TaxaSpeciesPresenceMaterialNotesImages
Australotitan[8] A. cooperensis A partial scapula, humeri, ulna, pubes, ischia, femora, presacral vertebral centrum fragments, and rib fragments. A large diamantinasaurian sauropod that possesses a mosaic of features shared with titanosaurians with similar geographical and temporal range.
Australovenator[9] A. wintonensis Dentaries, dorsal ribs and rib fragments, gastralial ribs and fragments, partial ilium, ulnae, radius, manus metacarpals, unguals, femur, tibiae, fibula, astragalus, metatarsals, pedal phalanges, humeri, radiale, distal carpal, and manual phalanxes. A megaraptoran theropod known from postcranial and cranial material.
Wintonotitan[9] W. wattsi[9] A scapula, both humeri, both ulnae, both radii, near complete metacarpus preserving complete metacarpals II–V with proximal half of metacarpal I, fragmentary dorsal and sacral vertebrae and ribs, partial ilium, ischium, caudal vertebral series including anterior caudals, middle caudals, posterior caudals, proximal chevrons, and numerous unidentifiable fragments. A titanosaur that is likely to be closely related to Australotitan, Diamantinasaurus and Savannasaurus.
Diamantinasaurus [9] D. matildae[9] A squamosal, quadrates, braincase, surangular, atlas intercentrum axis, cervical vertebrae, middle cervical neural arch, co-ossified sacral centra, cervical ribs, dorsal vertebrae, numerous dorsal ribs, fragmentary gastralia, coalesced sacral vertebrae, isolated sacral processes, scapula, coracoid, partial sternal plate, humeri, ulnae, radius, metacarpals I–V, manual phalanges, ilium, pubes, both ischia, femur, tibia, fibula, astragalus, and numerous fragments. A diamantinasaurian sauropod known from partial cranial material.
Savannasaurus[10] S. elliottorum[10] Posterior cervical vertebrae, cervical ribs, dorsal vertebrae, dorsal ribs, sacral vertebrae with processes, partial caudal vertebrae, fragmentary scapula, coracoid, sternal plates, incomplete humeri, shattered ulna, radius, metacarpals I–V, metacarpal IV, manual phalanges, fragments of ilia, pubes, ischia, astragalus, metatarsal III, and associated fragments. A wide-bodied sauropod that was well adapted to the wet, temperate floodplain environment it inhabited.
Ornithopoda Undescribed A nearly complete skull and mandible and at least three partial postcranial skeletons.[11] Small-bodied, recovered as part of "a diverse clade of Gondwanan ornithopods that includes taxa from Australia, South America, and Antarctica"
Titanosauriformes Undescribed Partial skull, consisting of a braincase, quadrates, quadratojugals, a left squamosal, postorbitals, and several unprepared elements. associated with a hind limb[12]
Sauropoda[7] Indeterminate Poorly preserved remains associated with the holotype of Confractosuchus[7]
Neornithischia Indeterminate Tooth[13]
Ornithopoda[7] Indeterminate Digested remains associated with the holotype of Confractosuchus[7]
Ankylosauria[14] Indeterminate Three isolated teeth from left and right dentary and right maxilla
Megaraptoridae[15] Indeterminate A partial skeleton, consisting of caudal vertebrae, metatarsals, a phalanx, and numerous unidentifiable fragments.

Pterosaurs

Pterosaurs of the Winton Formation
TaxaSpeciesPresenceMaterialNotesImages
Ferrodraco[16] F. lentoni A partial premaxillae, maxillae and dentaries, partial frontal, mandibular articular region comprising the surangular, angular and articular, partial cervical vertebrae, partial scapulocoracoid, partial ulna, partial radius, proximal and distal carpals, metacarpal IV, proximal end of metacarpal IV, fragmentary non-wing manual phalanges, partial first wing phalanx (IV-1), and associated fragments. The most complete pterosaur from Australia and the youngest known anhanguerian.

Flora

Flora of the Winton Formation[17]
TaxaSpeciesPresenceMaterialNotesImages
Marchantites M. marguerita Liverwort
Equisetites Indeterminate Axes Horsetail
Aff. Lygodium? Indeterminate Fern pinna
Phyllopteroides P. macclymontae Numerous pinnule impressions A fern belonging to the family Osmundaceae
Microphyllopteris cf. M. gleichenoides Frond fragment impression A fern belonging to the family Gleicheniaceae
Tempskya T. judithae Permineralized false trunks A tree fern
Otozamites cf. O. bengalensis Leaves Member of Bennettitales
Ptilophyllum Indeterminate
Pterostoma Indeterminate A possible cycad
Ginkgo G. wintonensis, four other possible species Leaf impressions (G. wintonensis) Dispersed cuticle A gingophyte, genus extant.
Taeniopteris Indeterminate Leaf impression A member of Pentoxylales, youngest record of the group in Australia
Emwadea E. microcarpa Seed cones A member of Araucariaceae, more closely related to Agathis and Wollemia than Araucaria.[18]
Austrosequoia A. wintonensis Cones and leaved axes A member of Cupressaceae
Araucariaceae Indeterminate Leaves
Cheirolepidiaceae Four taxa Dispersed cuticle
Lovellea L. wintonensis Permineralised flower A member of Laurales
Angiospermae Indeterminate Leaf impressions, cuticle fragments At least ten distinct types, belonging to both monocots and dicotyledons

See also

References

  1. ↑ "Water resources - Availability - Queensland". Archived from the original on 3 June 2011. Retrieved 1 May 2011.
  2. ↑ Tucker, Ryan T.; Roberts, Eric M.; Hu, Yi; Kemp, Anthony I.S.; Salisbury, Steven W. (September 2013). "Detrital zircon age constraints for the Winton Formation, Queensland: Contextualizing Australia's Late Cretaceous dinosaur faunas". Gondwana Research. 24 (2): 767–779. Bibcode:2013GondR..24..767T. doi:10.1016/j.gr.2012.12.009. ISSN 1342-937X.
  3. 1 2 3 Kemp, A (1997). "Four Species of Metaceratodus (Osteichthyes: Dipnoi, Family Ceratodontidae) from Australian Mesozoic and Cenozoic Deposits". Journal of Vertebrate Paleontology. 79 (1): 26–33. Bibcode:1997JVPal..17...26K. doi:10.1080/02724634.1997.10010949.
  4. ↑ Berrell R, Alvarado-Ortega J, Yabumoto Y, Salisbury SW (2014). "First record of the ichthyodectiform fish Cladocyclus from eastern Gondwana: A new species from the Lower Cretaceous of Queensland, Australia". Acta Palaeontologica Polonica. 59 (4): 903–920. doi:10.4202/app.2012.0019.
  5. ↑ Kear, Benjamin P. (30 July 2016). "Cretaceous marine amniotes of Australia: perspectives on a decade of new research". Memoirs of Museum Victoria. 74: 17–28. doi:10.24199/j.mmv.2016.74.03.
  6. ↑ Scanlon, John D.; Hucknull, Scott (2008). "A dolichosaurid lizard from the latest Albian (mid-Cretaceous) Winton Formation, Queensland, Australia". Proceedings of the Second Mosasaur Meeting. 3. 3: 131–136.
  7. 1 2 3 4 5 White, M.A.; Bell, P.R.; Campione, N.E.; Sansalone, G.; Brougham, T.; Bevitt, J.J.; Molnar, R.E.; Cook, A.G.; Wroe, S.; Elliott, D.A. (2022). "Abdominal contents reveal Cretaceous crocodyliforms ate dinosaurs". Gondwana Research. 106: 281–302. Bibcode:2022GondR.106..281W. doi:10.1016/j.gr.2022.01.016. S2CID 246756546.
  8. ↑ Hocknull SA, Wilkinson M, Lawrence RA, Konstantinov V, Mackenzie S, Mackenzie R (2021). "A new giant sauropod, Australotitan cooperensis gen. et sp. nov., from the mid-Cretaceous of Australia". PeerJ. 9: e11317. doi:10.7717/peerj.11317. PMC 8191491. PMID 34164230.
  9. 1 2 3 4 5 Hocknull, SA; White, MA; Tischler, TR; Cook, AG; Calleja, ND; et al. (2009). "New Mid-Cretaceous (Latest Albian) Dinosaurs from Winton, Queensland, Australia". PLOS ONE. 4 (7): e6190. Bibcode:2009PLoSO...4.6190H. doi:10.1371/journal.pone.0006190. PMC 2703565. PMID 19584929.
  10. 1 2 Poropat, S.F.; Mannion, P.D.; Upchurch, P.; Hocknull, S.A.; Kear, B.P.; Kundrát, M.; Tischler, T.R.; Sloan, T.; Sinapius, G.H.K.; Elliott, J.A.; Elliott, D.A. (2016). "New Australian sauropods shed light on Cretaceous dinosaur palaeobiogeography". Scientific Reports. 6: 34467. Bibcode:2016NatSR...634467P. doi:10.1038/srep34467. PMC 5072287. PMID 27763598.
  11. ↑ AN EXCEPTIONALLY PRESERVED SMALL-BODIED ORNITHOPOD DINOSAUR FROM THE LOWER CRETACEOUS (UPPER ALBIAN) WINTON FORMATION OF ISISFORD, CENTRAL-WESTERN QUEENSLAND, AUSTRALIA, AND THE DIVERSIFICATION OF GONDWANAN ORNITHOPODS SALISBURY, Steven W., University of Queensland, Brisbane, Australia; HERNE, Matthew C., University of New England, Armidale, Australia; LAMANNA, Matthew C., Carnegie Museum of Natural History, Pittsburgh, PA, United States of America; NAIR, Jay P., University of Queensland, Brisbane, Australia; SYME, Caitlin, University of Queensland, Brisbane, Australia; WITMER, Lawrence M., Ohio Univ, Athens, OH, United States of America SVP conference abstracts 2019
  12. ↑ NEW SAUROPOD DINOSAUR DISCOVERIES IN THE LOWER UPPER CRETACEOUS WINTON FORMATION (CENOMANIAN– LOWER TURONIAN) OF QUEENSLAND, AUSTRALIA: IMPLICATIONS FOR TITANOSAURIAN EVOLUTION POROPAT, Stephen F., Swinburne University of Technology, Hawthorn, Australia; MANNION, Philip D., University College London, London, England; UPCHURCH, Paul, University College London, London, United Kingdom; ELLIOTT, David A., Australian Age of Dinosaurs Museum of Natural History, Winton, Australia SVP conference abstracts 2019
  13. ↑ "Hypsilophodontid (Dinosauria:Ornithischia) from latest Albian, Winton Formation, central Queensland". Memoirs of the Queensland Museum. 52.
  14. ↑ Leahey, Lucy G.; Salisbury, Steven W. (June 2013). "First evidence of ankylosaurian dinosaurs (Ornithischia: Thyreophora) from the mid-Cretaceous (late Albian–Cenomanian) Winton Formation of Queensland, Australia". Alcheringa: An Australasian Journal of Palaeontology. 37 (2): 249–257. doi:10.1080/03115518.2013.743703. ISSN 0311-5518. S2CID 129461328.
  15. ↑ White, Matt A.; Bell, Phil R.; Poropat, Stephen F.; Pentland, Adele H.; Rigby, Samantha L.; Cook, Alex G.; Sloan, Trish; Elliott, David A. (2020). "New theropod remains and implications for megaraptorid diversity in the Winton Formation (lower Upper Cretaceous), Queensland, Australia". Royal Society Open Science. 7 (1): 191462. Bibcode:2020RSOS....791462W. doi:10.1098/rsos.191462. PMC 7029900. PMID 32218963.
  16. ↑ Pentland, Adele H.; Poropat, Stephen F.; Tischler, Travis R.; Sloan, Trish; Elliott, Robert A.; Elliott, Harry A.; Elliott, Judy A.; Elliott, David A. (December 2019). "Ferrodraco lentoni gen. et sp. nov., a new ornithocheirid pterosaur from the Winton Formation (Cenomanian–lower Turonian) of Queensland, Australia". Scientific Reports. 9 (1): 13454. Bibcode:2019NatSR...913454P. doi:10.1038/s41598-019-49789-4. ISSN 2045-2322. PMC 6776501. PMID 31582757.
  17. ↑ McLoughlin, Stephen; Pott, Christian; Elliott, David (September 2010). "The Winton Formation flora (Albian–Cenomanian, Eromanga Basin): implications for vascular plant diversification and decline in the Australian Cretaceous". Alcheringa: An Australasian Journal of Palaeontology. 34 (3): 303–323. doi:10.1080/03115511003669944. ISSN 0311-5518. S2CID 129098756.
  18. ↑ Dettmann, Mary E.; Clifford, H. Trevor; Peters, Mark (June 2012). "Emwadea microcarpa gen. et sp. nov.—anatomically preserved araucarian seed cones from the Winton Formation (late Albian), western Queensland, Australia". Alcheringa: An Australasian Journal of Palaeontology. 36 (2): 217–237. doi:10.1080/03115518.2012.622155. ISSN 0311-5518. S2CID 129171237.
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