Bahariasaurus
| Bahariasaurus Temporal range: Late Cretaceous,
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| Vertebra of Bahariasaurus from specimen 1912 VIII 62 | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | Saurischia |
| Clade: | Theropoda |
| Family: | †Bahariasauridae |
| Genus: | †Bahariasaurus Stromer, 1934 |
| Species: | †B. ingens
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| Binomial name | |
| †Bahariasaurus ingens Stromer, 1934
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| Synonyms | |
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Bahariasaurus is an enigmatic genus of large theropod dinosaur. The genus is known to have included at least 1 species, Bahariasaurus ingens (meaning "huge Bahariya lizard"), which was found in North African rock layers dating to the Cenomanian and Turonian ages of the Late Cretaceous. The only fossils confidently assigned to Bahariasaurus were found in the Bahariya Formation of the Bahariya (Arabic: الواحة البحرية meaning the "northern oasis") oasis in Egypt by Ernst Stromer but were destroyed during a World War II bombing raid with the same raid taking out the holotype of Spinosaurus and Aegyptosaurus among other animals found in the Bahariya Formation. While there have been more fossils assigned to the genus such as some from the Farak Formation of Niger, these remains are referred to with much less certainty.[1] Bahariasaurus is, by most estimations, one of the largest theropods, approaching the height and length of other large bodied theropods such as Tyrannosaurus rex and the contemporaneous Carcharodontosaurus. The aforementioned estimations tend to put it at around 11–12.2 metres (36–40 ft) in length and 4-4.8 tonnes in overall weight.[2][3][4]
History
[edit]Bahariasaurus was found during the 1910s during an expedition to Egypt's Baharija Formation led by Markgraf and Stromer, and the holotype, specimen 1912 VIII 62, was discovered in 1911.[5] The type species, B. ingens, was described by Ernst Stromer in 1934.[6] It was considered to be potentially the largest known theropod. This specimen was destroyed in an air raid during World War II on the night of 23/24 April 1944.
The questionable remains of Bahariasaurus from the Farak Formation of Niger, which consist of a proximal caudal centrum (65 mm), two mid caudal centra and three mid caudal centra (from different individuals) were discovered some time later during the 20th century and described by de Lapparent in 1960.[1][7] It is possible that these remains may have belonged to another unrelated theropod.
Description
[edit]Bahariasaurus was a notably large theropod. The type species, B. ingens, is only known from post-cranial material. The two centra of the posterior dorsal vertebrae are ~157% and 189% longer than they are tall, and ~82% and ~95% wider than they are tall. [1] All preserved sacrals have a longitudinally elongate pleurocoel and a ventral median groove, which is unknown in any ceratosaurs. The last sacral vertebrae known from Bahariasaurus implies that there was no greater fusion of the vertebrae after that.[6] The 22.5 cm long vertebra of Bahariasaurus 1912 VIII 62 is the longest dorsal vertebra among all theropods, 12.5% longer than that of Sue.[4]
Classification
[edit]The exact taxonomic placement of Bahariasaurus is uncertain, although it has been variously assigned to several theropod groups, including the Carcharodontosauridae[8] and the superfamily Tyrannosauroidea.[9] The smaller contemporaneous theropod Deltadromeus could potentially be synonymous with Bahariasaurus. If this assumption is correct, Bahariasaurus would possibly represent the largest ceratosaur as recent studies consider Deltadromeus a ceratosaur, specifically a noasaurid.[2] More specimens would be needed to more accurately classify it and determine its relationship to Deltadromeus.
However, the taxon has posterior dorsal and sacral pleurocoels, a proximally placed interpubic fenestra and ventrally-grooved sacrals, which makes the taxon unlikely to be a ceratosaur.[10]
If added to the phylogenetic analysis of Carrano (2012), it is recovered as an indeterminate tetanuran.
In the 2016 description and analysis of the megaraptoran Aoniraptor, Bahariasaurus was found, along with Gualicho, Aoniraptor and Deltadromeus to probably form a family in the still poorly understood clade known as the Megaraptora and are different from the more derived megaraptorids.[11]
In 2016, Gregory S. Paul suggested that Deltadromeus may be a juvenile specimen of Bahariasaurus, but that their relationship is uncertain and to be determined. A 2020 study found that a referred fossil of Bahariasaurus belongs to Deltadromeus, leaving Bahariasaurus to be regarded as a nomen dubium by the authors.[12]
However, Cau (2024) included the Bahariasaurus type specimen in a phylogenetic analysis and recovered it in a monophyletic clade near the base of Ceratosauria along with Aoniraptor, Deltadromeus, and Gualicho, with Elaphrosaurus as the sister taxon to this clade.[13]
Paleobiology
[edit]
Bahariasaurus was one of four giant theropods known from the Bahariya Formation, the other three being the allosauroid Carcharodontosaurus and the spinosaurids Spinosaurus and Sigilmassasaurus, though the validity of Sigilmassasaurus is currently being debated as it may be a junior synonym of Spinosaurus. It is likely the predators in the Bahariya Formation exhibited niche-partitioning in order to avoid competition so that they could coexist in the same environment.[14]
References
[edit]- ^ a b c "Megalosauroidea". www.theropoddatabase.com. Retrieved 2020-12-10.
- ^ a b Holtz, Thomas R. Jr. (2008) Dinosaurs: The Most Complete, Up-to-Date Encyclopedia for Dinosaur Lovers of All Ages Supplementary Information
- ^ Paul, Gregory S. (2016). The Princeton Field Guide to Dinosaurs. Princeton University Press. p. 81. ISBN 978-1-78684-190-2. OCLC 985402380.
- ^ a b Dinosaur Facts and Figures. 2019-06-25. ISBN 978-0-691-18031-1.
- ^ Josh., Smith (2013). The lost dinosaurs of egypt. Random House. ISBN 978-1-58836-117-2. OCLC 869562622.
- ^ a b Stromer, E. (1934). "Ergebnisse der Forschungsreisen Prof. E. Stromers in den Wüsten Ägyptens. II. Wirbeltier-Reste der Baharije-Stufe (unterstes Cenoman)." 13. Dinosauria. Abhandlungen der Bayerischen Akademie der Wissenschaften, Mathematisch-naturwissenschaftliche Abteilung n.f., 22: 1–79.
- ^ de Lapparent A. F. (1960) "The dinosaurs of the “Continental Intercalaire” of the central Sahara". Memoirs of the Geological Society of France 39: 1-60.
- ^ Rauhut, (1995). "Zur systematischen Stellung der afrikanischen Theropoden Carcharodontosaurus Stromer 1931 und Bahariasaurus Stromer 1934." Berliner geowissenschaftliche Abhandlungen, E16 (Gundolf-Ernst-Festschrift): 357-375.
- ^ Chure, (2000). "A new species of Allosaurus from the Morrison Formation of Dinosaur National Monument (Utah-Colorado) and a revision of the theropod family Allosauridae." Ph.D. dissertation, Columbia University, 1-964.
- ^ Mortimer, Mickey (2014-09-17). "The Theropod Database Blog: No giant Egyptian Deltadromeus". The Theropod Database Blog. Retrieved 2023-12-03.
- ^ Matías J. Motta; Alexis M. Aranciaga Rolando; Sebastián Rozadilla; Federico E. Agnolín; Nicolás R. Chimento; Federico Brissón Egli & Fernando E. Novas (2016). "New theropod fauna from the Upper Cretaceous (Huincul Formation) of northwestern Patagonia, Argentina". New Mexico Museum of Natural History and Science Bulletin. 71: 231–253.
- ^ Ibrahim, Nizar; Sereno, Paul C.; Varricchio, David J.; Martill, David M.; Dutheil, Didier B.; Unwin, David M.; Baidder, Lahssen; Larsson, Hans C.E.; Zouhri, Samir; Kaoukaya, Abdelhadi (2020-04-21). "Geology and paleontology of the Upper Cretaceous Kem Kem Group of eastern Morocco". ZooKeys (928): 1–216. doi:10.3897/zookeys.928.47517. ISSN 1313-2989. PMC 7188693. PMID 32362741.
- ^ Cau, Andrea (2024). "A Unified Framework for Predatory Dinosaur Macroevolution" (PDF). Bollettino della Società Paleontologica Italiana. 63 (1): 1–19. doi:10.4435/BSPI.2024.08. ISSN 0375-7633.
- ^ Farlow Pianka, James, Eric (2002). "Body Size Overlap, Habitat Partitioning and Living Space Requirements of Terrestrial Vertebrate Predators: Implications for the Paleoecology of Large Theropod Dinosaurs". Historical Biology. 16: 21–40. doi:10.1080/0891296031000154687. S2CID 18114585.
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