The type specimen ofPhuwiangosaurus 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 honorsPrincess Maha Chakri Sirindhorn ofThailand for her interest in the paleontology of the country.[3]
Phuwiangosaurus sirindhornae is known from several specimens, all of which were found in theSao Khua Formation of Thailand.[4][5][6] Theholotype, 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.[7] A dorsal vertebra and a caudal vertebra excavated at the same site years later probably belong to the same specimen.[8] The most complete skeleton, SM K11, represents a half-grown individual and is about 60% complete, including a partial skull.[9] Other partial skeletons and isolated bones have been described as well.[4][6] In 2020, Cashmore et al. calculated that, overall, 65% of the skeletal anatomy ofPhuwiangosaurus sirindhornae was known.[10] Numerous bones of babyPhuwiangosaurus have been found, which is a rarity for sauropods.[11] Though specimens of a wide range of ages are known, no old individuals that had reached their maximum body size are known.[12]
Phuwiangosaurus was a mid-sized sauropod, roughly 15 to 20 metres (49 to 66 ft) long.[13] Its mass has been estimated at 17 tonnes.[14] 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 ofdiplodocoids andtitanosaurs.[15] The braincase ofPhuwiangosaurus exhibits characteristics intermediate between those of basal somphospondyls and titanosaurs.[16] The neck ofPhuwiangosaurus 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.[17] Thesacrum was composed of five vertebrae.[18]
Phuwiangosaurus was originally assigned toTitanosauria, but more recent studies have placed it in a morebasal position within the Titanosauriformes. Phylogenetic analyses presented by D'Emic (2012), Mannionet al. (2013), and Mochoet al. (2014) resolvePhuwiangosaurus within theEuhelopodidae, alongside genera such asEuhelopus andTangvayosaurus.[19][20][21] Other analyses have failed to find support for such a grouping,[22] including some finding it to beparaphyletic at the base of Somphospondyli.[20][23]
The Sao Khua Formation, where fossils ofPhuwiangosaurus have been found, was deposited 133.6 to 132.1 million years ago, and represents a floodplain environment in a humid, subtropical climate.[24] The Sao Khua dinosaur assemblage includes the large theropodsSiamotyrannus,Phuwiangvenator,Vayuraptor, andSiamosaurus, and theornithomimosaurKinnareemimus.[25] Other unidentified sauropods, different fromPhuwiangosaurus, were present in the ecosystem. These sauropods include aEuhelopus-like taxon[26] and a possible brachiosaurid.[6]Ornithischian dinosaurs are not known from the Sao Khua Formation, although they are known from roughly contemporary environments in other parts of Asia.[27] Non-dinosaurian members of the fauna included crocodilians, turtles, fish, and sharks.[6] There is evidence that theropods fed onPhuwiangosaurus.[28]
^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.
^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.
Kaikaew, Siripat; Suteethorn, Varavudh; Deesri, Uthumpom; Suteethorn, Suravech (2022-12-01). "The endocast of Phuwiangosaurus sirindhornae from the Lower Cretaceous of Thailand".Cretaceous Research.144.doi:10.1016/j.cretres.2022.105434.ISSN0195-6671.
Martin, Valérie (1994). "Baby sauropods from the Sao Khua Formation (Lower Cretaceous) in northeastern Thailand".Gaia.10:147–153.ISSN0871-5424.
Martin, Valérie; Buffetaut, Eric; Suteethorn, Varavudh (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. Série II. Sciences de la terre et des planètes.319 (9):1085–1092.ISSN1251-8050.
Martin, V.; Suteethorn, V.; Buffetaut, E. (1999). "Description of the type and referred material of Phuwiangosaurus sirindhornae Martin, Buffetaut and Suteethorn, 1994, a sauropod from the Lower Cretaceous of Thailand".Oryctos.2:39–91.
Suteethorn, Suravech; Le Loeuff, Jean; Buffetaut, Eric; Suteethorn, Varavudh (2010-04-01). "Description of topotypes of Phuwiangosaurus sirindhornae, a sauropod from the Sao Khua Formation (Early Cretaceous) of Thailand, and their phylogenetic implications".Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen.256 (1):109–121.Bibcode:2010NJGPA.256..109S.doi:10.1127/0077-7749/2010/0036.ISSN0077-7749.
Tucker, Ryan T.; Hyland, Ethan G.; Gates, Terry A.; King, M. Ryan; Roberts, Eric M.; Foley, Elliot K.; Berndt, David; Hanta, Rattanaphorn; Khansubha, Sasa-on; Aswasereelert, Wasinee; Zanno, Lindsay E. (2022-06-13). "Age, depositional history, and paleoclimatic setting of Early Cretaceous dinosaur assemblages from the Sao Khua Formation (Khorat Group), Thailand".Palaeogeography, Palaeoclimatology, Palaeoecology.601 111107.Bibcode:2022PPP...60111107T.doi:10.1016/j.palaeo.2022.111107.ISSN0031-0182.S2CID249702713.
