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Phuwiangosaurus

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Phuwiangosaurus
Temporal range: late Valanginian-early Hauterivian,
~133.6–132.1 Ma
↓
Femur
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: †Sauropodomorpha
Clade: †Sauropoda
Clade: †Macronaria
Family: †Euhelopodidae
Genus: †Phuwiangosaurus
Martin, Buffetaut and Suteethorn, 1994
Species:
†P. sirindhornae
Binomial name
†Phuwiangosaurus sirindhornae
Martin, Buffetaut and Suteethorn, 1994

Phuwiangosaurus (meaning "Phu Wiang lizard") is a genus of titanosaur dinosaur from the Early Cretaceous (Valanginian-Hauterivian) Sao Khua Formation of Thailand. The type species, P. sirindhornae, was described by Martin, Buffetaut, and Suteethorn in a 1993 press release[1] and was formally named in 1994.[2] The species was named to honor Princess Maha Chakri Sirindhorn of Thailand, who was interested in the geology and palaeontology of Thailand, while the genus was named after the Phu Wiang area, where the fossil was discovered.

Phuwiangosaurus was originally assigned to Titanosauria, but more recent studies have placed it in a more basal position within the Titanosauriformes. Phylogenetic analyses presented by D'Emic (2012), Mannion et al. (2013), and Mocho et al. (2014) resolve Phuwiangosaurus within the Euhelopodidae, alongside genera such as Euhelopus and Tangvayosaurus.[3][4][5] Other analyses have failed to find support for such a grouping,[6] including some finding it to be paraphyletic at the base of Somphospondyli.[4][7]

Discovery and naming

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The type specimen of Phuwiangosaurus sirindhornae was discovered in Phu Wiang National Park in 1982, and excavated and prepared over the next several years. The specimen was described as representing a new genus and species, Phuwiangosaurus sirindhornae, by Valérie Martin, Eric Buffetaut, and Varavudh Suteethorn in 1994. The genus name refers to its discovery in Phu Wiang, and the species name honors Princess Maha Chakri Sirindhorn of Thailand for her interest in the paleontology of the country.[8]

Fossil specimens

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Phuwiangosaurus sirindhornae is known from several specimens, all of which were found in the Sao Khua Formation of Thailand.[9][10][11] The holotype, SM PW 1, is a partial skeleton of an adult individual, which consists of three cervical vertebrae, three dorsal vertebrae, ribs, a chevron, both scapulae, a coracoid, the left humerus, the left ulna, both ilia, ischia, pubes, and femora, and the left fibula.[12] A dorsal vertebra and a caudal vertebra excavated at the same site years later probably belong to the same specimen.[13] The most complete skeleton, SM K11, represents a half-grown individual and is about 60% complete, including a partial skull.[14] Other partial skeletons and isolated bones have been described as well.[9][11] In 2020, Cashmore et al. calculated that, overall, 65% of the skeletal anatomy of Phuwiangosaurus sirindhornae was known.[15] Numerous bones of baby Phuwiangosaurus have been found, which is a rarity for sauropods.[16] Though specimens of a wide range of ages are known, no old individuals that had reached their maximum body size are known.[17]

Description

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Size compared to a human

Phuwiangosaurus was a mid-sized sauropod, roughly 15 to 20 metres (49 to 66 ft) long.[18] Its mass has been estimated at 17 tonnes.[19] The teeth are slender and peg-like, with the tooth height from base to tip being on average over four times greater than the width of the base of the tooth. They are slenderer than the teeth of other euhelopodids, with their proportions more closely resembling the teeth of diplodocoids and titanosaurs.[20] The neck of Phuwiangosaurus was probably composed of 13 vertebrae. The lengths of the vertebrae increase up to the middle of the neck, with the eighth cervical vertebra being the longest, and then decrease again. The cervical neural spines are bifurcated from the seventh cervical vertebra onward.[21] The sacrum was composed of five vertebrae.[22]

Paleoecology

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Life restoration of a Phuwiangosaurus herd in the Sao Khua Formation environment, with the spinosaurid dinosaur Siamosaurus (right) and the crocodyliform Sunosuchus (middle left)

The Sao Khua Formation, where fossils of Phuwiangosaurus have been found, was deposited 133.6 to 132.1 million years ago, and represents a floodplain environment in a humid, subtropical climate.[23] The Sao Khua dinosaur assemblage includes the large theropods Siamotyrannus, Phuwiangvenator, Vayuraptor, and Siamosaurus, and the ornithomimosaur Kinnareemimus.[24] Other unidentified sauropods, different from Phuwiangosaurus, were present in the ecosystem. These sauropods include a Euhelopus-like taxon[25] and a possible brachiosaurid.[11] Ornithischian dinosaurs are not known from the Sao Khua Formation, although they are known from roughly contemporary environments in other parts of Asia.[26] Non-dinosaurian members of the fauna included crocodilians, turtles, fish, and sharks.[11] There is evidence that theropods fed on Phuwiangosaurus.[27]

References

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  1. ^ Martin, V.; E. Buffeataut; V. Suteethorn (1993). "Jurassic sauropod dinosaurs of Thailand: a preliminary report". In T. Thanasutipital (ed.). Proceedings of the International Symposium on Biostratigraphy of mainland Southeast Asia. Chiang Mai University. pp. 415–425.
  2. ^ Martin, V.; E. Buffeataut; V. Suteethorn (1994). "A new genus of sauropod dinosaur from the Sao Khua formation (Late Jurassic or early Cretaceous) of northeastern Thailand". Comptes rendus de l'Académie des Sciences de Paris. 319 (2): 1085–1092.
  3. ^ D'Emic, M. D. (2012). "The early evolution of titanosauriform sauropod dinosaurs". Zoological Journal of the Linnean Society. 166 (3): 624–671. doi:10.1111/j.1096-3642.2012.00853.x. hdl:2027.42/94293.
  4. ^ a b Mannion, P. D.; Upchurch, P.; Barnes, R. N.; Mateus, O. (2013). "Osteology of the Late Jurassic Portuguese sauropod dinosaur Lusotitan atalaiensis (Macronaria) and the evolutionary history of basal titanosauriforms". Zoological Journal of the Linnean Society. 168: 98–206. doi:10.1111/zoj.12029.
  5. ^ Mocho, P.; Royo-Torres, R.; Ortega, F. (2014). "Phylogenetic reassessment of Lourinhasaurus alenquerensis, a basal Macronaria (Sauropoda) from the Upper Jurassic of Portugal". Zoological Journal of the Linnean Society. 170 (4): 875–916. doi:10.1111/zoj.12113.
  6. ^ D'Emic, M. D. (2013). "Revision of the sauropod dinosaurs of the Lower Cretaceous Trinity Group, southern USA, with the description of a new genus". Journal of Systematic Palaeontology. 11 (6): 707–726. doi:10.1080/14772019.2012.667446. S2CID 84742205.
  7. ^ Zaher, H.; Pol, D.; Carvalho, A.B.; Nascimento, P.M.; Riccomini, C.; Larson, P.; Juarez-Valieri, R.; Pires-Domingues, R.; da Silva Jr, N.J.; de Almeida Campos, D. (2011). "A complete skull of Early Cretaceous sauropod and the evolution of advanced titanosaurians". PLOS ONE. 6 (2): e16663. Bibcode:2011PLoSO...616663Z. doi:10.1371/journal.pone.0016663. PMC 3034730. PMID 21326881.
  8. ^ Martin, Buffetaut & Suteethorn 1994, p. 1089.
  9. ^ a b Martin, Suteethorn & Buffetaut 1999.
  10. ^ Suteethorn et al. 2009.
  11. ^ a b c d Samathi et al. 2023.
  12. ^ Suteethorn et al. 2009, pp. 195.
  13. ^ Suteethorn et al. 2010, p. 116.
  14. ^ Suteethorn et al. 2009, pp. 193–195.
  15. ^ Cashmore et al. 2020.
  16. ^ Martin 1994, pp. 151.
  17. ^ Klein, Sander & Suteethorn 2009, pp. 225–226.
  18. ^ Martin, Suteethorn & Buffetaut 1999, p. 42.
  19. ^ Paul 2010, p. 205.
  20. ^ D'Emic et al. 2013, p. 27.
  21. ^ Suteethorn et al. 2009, p. 203.
  22. ^ Suteethorn et al. 2009, p. 207.
  23. ^ Tucker et al. 2022.
  24. ^ Tucker et al. 2022, p. 15.
  25. ^ Buffetaut et al. 2002, p. 99.
  26. ^ Tucker et al. 2022, p. 17.
  27. ^ Suteethorn et al. 2009, pp. 193–194.

Works cited

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