The Phu Kradung Formation sediments were deposited in a lake-dominated floodplain cut by meandering and occasionally braided river channels.[2]
The Phu Kradung Formation is considered, on the basis of recent vertebrae fossil discoveries, to be Late Jurassic in age. However, new palynology and biostratigraphic data suggests an age of Early Cretaceous for the upper section.[2][3]
More recent datations trought detrital zircon U–Pb ages of samples from the conglomerates have stablished a lowermost age of late Early Jurassic (Toarcian), with a maximum depositional age of 180 Ma, which is older than the previously estimated Late Jurassic–Berriasian age based on fossil evidence.[4] This discrepancy suggests the absence of syn-depositional zircons. The zircon data also help clarify the timing of the Indosinian III Event, placing the Indosinian III Unconformity between 201 and 182 Ma, marking a hiatus of about 20 million years. The Phu Kradung Formation deposition likely occurred after the Nam Phong Formation and may correlate with the Upper part of the last in the Khorat Basin subsurface.[4]
Dinosaur remains have been recovered from this formation, although few have been referred to a specific genus.[5][6]
Chalawan, an extinctgenus of pholidosauridmesoeucrocodylian, is currently known solely from its holotype, a nearly complete mandible collected in the early 1980s from a road-cut near the town of Nong Bua Lamphu in the upper part of the Phu Kradung Formation. This single specimen is the most well preserved vertebrate fossil that has been found from the formation. It contains a single species, Chalawan thailandicus.[7]
12Hara, Hidetoshi; Charoentitirat, Thasinee; Tokiwa, Tetsuya; Kurihara, Toshiyuki; Suzuki, Keisuke; Sardsud, Apsorn (2024). "Record of the Indosinian Orogeny from conglomerates and detrital zircon U–Pb ages of the western Indochina Block, central Thailand". Gondwana Research. 128: 368–389. doi:10.1016/j.gr.2023.11.009. ISSN1342-937X.
1234Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
↑Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp.ISBN0-520-24209-2.
↑Chowchuvech, Wongwech; Manitkoon, Sita; Chanthasit, Phornphen; Ketwetsuriya, Chatchalerm (15 September 2026). "Sauropod teeth from the Khorat Group of Thailand suggest the faunal replacement of sauropod dinosaurs across the Late Jurassic–Early Cretaceous". Historical Biology. 0 (0): 1–27. doi:10.1080/08912963.2026.2710631.
12Samathi, Adun; Chanthasit, Phornphen; Sander, Paul Martin (2019-07-01). "A review of theropod dinosaurs from the Late Jurassic to mid-Cretaceous of Southeast Asia". Annales de Paléontologie. Palaeobiodiversity of Southeast Asia, issue 1. 105 (3): 201–215. Bibcode:2019AnPal.105..201S. doi:10.1016/j.annpal.2019.03.003. ISSN0753-3969. S2CID197574833.
↑Buffetaut, Eric; Suteethorn, Varavudh; Tong, Haiyan (24 January 2001). "The first thyreophoran dinosaur from Southeast Asia: a stegosaur vertebra from the Late Jurassic Phu Kradung Formation of Thailand". Neues Jahrbuch für Geologie und Paläontologie - Monatshefte. 2001 (2): 95–102. doi:10.1127/njgpm/2001/2001/95.
↑Ulansky, R. E., 2014. Evolution of the stegosaurs (Dinosauria; Ornithischia). Dinologia, 35 pp. [in Russian]. PDF.
↑Peter M. Galton; Kenneth Carpenter (2016). "The plated dinosaur Stegosaurus longispinus Gilmore, 1914 (Dinosauria: Ornithischia; Upper Jurassic, western USA), type species of Alcovasaurus n. gen". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 279 (2): 185–208. doi:10.1127/njgpa/2016/0551.
↑Deesri, Uthumporn; Jintasakul, Pratueng; Cavin, Lionel (2016-11-01). "A new Ginglymodi (Actinopterygii, Holostei) from the Late Jurassic–Early Cretaceous of Thailand, with comments on the early diversification of Lepisosteiformes in Southeast Asia". Journal of Vertebrate Paleontology. 36 (6) e1225747. Bibcode:2016JVPal..36E5747D. doi:10.1080/02724634.2016.1225747. ISSN0272-4634. S2CID89359438.