|Schematic reconstruction of the pelvis, Barsbold & Perle 1980|
Enigmosaurus (meaning "Enigma lizard" or "Enigmatic lizard") is a genus of therizinosaur theropod dinosaur that lived in Asia during the Late Cretaceous period. It was a medium-sized, ground-dwelling, bipedal herbivorous that represents the third therizinosaur taxon from the Bayan Shireh Formation, although it is known from the lower part. The genus is monotypic, including only the type species E. mongoliensis, known from a well preserved pelvis and other tentative body remains.
Discovery and naming
The holotype, IGM 100/84, was discovered at the Khara Khutul locality in the Bayan Shireh Formation (sometimes called Baynshire Formation or the Baynshirenskaya Svita), southeastern Mongolia, dating from the Late Cretaceous period, and first reported in 1979 on a pelvic comparison with other theropod dinosaurs. At the time, little was known about therizinosaurs. In 1980, it was mentioned again, this time in the new infraorder created by the mongolian paleontologists Rinchen Barsbold and Altangerel Perle: Segnosauria. Nicknamed as the "Dinosaur from Khara Khutul", it was shortly described and included into the Segnosauria.
Three years later, the type species, Enigmosaurus mongoliensis, was named and described in 1983 by Barsbold. The preserved elements consist of a partial skeleton, lacking the skull, that includes a well preserved pelvic girdle with other postcrania. The generic name, Enigmosaurus, was stated to be derived from Greek αίνιγμα (aínigma, meaning enigma) and σαῦρος (sauros, meaning lizard), in reference to the aberratic and unusual shape of its pelvis. The specific name, mongoliensis, refers to the country of its discovery, Mongolia. There are some therizinosaur fossil findings at the Iren Dabasu Formation that could be referable to Enigmosaurus.
Possible synonymy with Erlikosaurus
Some paleontologists proposed that Enigmosaurus was likely the same animal as Erlikosaurus, since both were found in the same geologic formation, Enigmosaurus is known from pelvic remains, whereas the pelvis of Erlikosaurus is unknown and distinguishing traits between them were absent; if proven, this would make Enigmosaurus a junior synonym of Erlikosaurus. However, the Enigmosaurus pelvis doesn't resemble that of Segnosaurus as would be expected for the connection with Erlikosaurus, and there is a huge size difference. In addition, both genera are known from different strata (lower and upper), and they are considered to be distinct animals by most authors.
The holotype pelvis is in relatively good preservation, compromising the sacral vertebrae, partial illium, right and left pubis and the left ischium. The pelvis is somewhat large as a whole and opisthopubic. The illium is widely positioned and turned externally; it preserves a large cubic process in the posterodorsal area. Elongated pubic peduncles are present in the illium; the ischial peduncles are more reduced though. The distal end of the pubis is elongated, recurved and stocky. The ischium, is slightly shorter than the pubis and parallel to it, with a narrow shaft. The obturator process on the front edge of the ischium is horizontally elongated and low. Open edges are appreciable on the large trochanteric fossa. Apparently, the sacrum preserves six vertebrae, with elongated transverse processes. For instance, its pelvis is very particular compared to other therizinosaur relatives, featuring areas of bone resorption and bone remodeling on the illium. These specific traits may indicate the advanced age of the individual, if true, the fusion of the obturator process and pubic body could be discarded as an authentic autapomorphy for the species. Zanno and colleagues noted that more analyses are required to settle this enigma.
Enigmosaurus was a relatively large-bodied therizinosaur, with an estimated length of 5 m (16 ft) and a weight between 454 to 907 kg (1,001 to 2,000 lb). Although it is commonly known from the pelvis, several remains not mentioned in the original description of the holotype were labelled under the same specimen number (IGM 100/84). These elements are in poor condition compared to the pelvis, and they were not measured and illustrated: proximal end of a femur; large femoral shaft, might be a tibial shaft; some ribs; distal end of a humerus; a tentative radius and the proximal end of an ulna. The femur however, was not found in association with the holotype individual, therefore it should be assigned to therizinosauria incertae sedis; the other remains might pertain to the holotype. A very large left femur, measuring 105 cm (1,050 mm) long, was labelled with the same specimen number too, however, it was not associated with the holotype due to its large size (larger than the pelvis itself). Nevertheless, it seems to approach the size of the closer Segnosaurus.
As noted by Barsbold in the original description of Enigmosaurus, it can recognised by the following characteristics:
- The pubis and ischium are short.
- Elongated margin in the anterior presymphyseal region of the distal pubis.
- Prominent cranial and caudal processes on the dorsoventrally somewhat flattened pubic boot.
- The pubic feet are fused, being medially elongated, a medial expansion forms a V-shaped structure.
- The medial fusion of the obturator process and pubic body, forms a tetraradiate process.
Enigmosaurus was by the describers assigned to a separate Enigmosauridae (now obsolete) due to its aberrant pelvis, but later considered a member of the Segnosauridae which are today called the Therizinosauridae. Lindsay Zanno in 2010 recovered a position more basal in the Therizinosauroidea.
The remains of Enigmosaurus were found in sediments that were deposited during the Late Cretaceous period on the Bayan Shireh Formation, Khara Khutul locality. Being a therizinosaur, it was likely a slow herbivore and/or omnivore, as suggested by most authors all over the time. The biodiversity across the formation was characterized by therizinosaurs, as seen on the remains of Enigmosaurus, Erlikosaurus and Segnosaurus. The holotype location, Khara Khutul, has also yielded the contemporary Segnosaurus and an unnamed velociraptorine. Most of the remaining paleofauna from this formation is known from Uppper strata, whereas Enigmosaurus is known from Lower strata.
At the locality, diverse paleoflora has been discovered, such as Cornaceae reported with Bothrocaryum gobience and Nyssoidea mongolica as fine representatives. Numerous fossil fruits findings at the locality reflect the large presence of Angiosperm plants on the formation. The unearthed fruits bear some resemblance with Abelmoschus esculentus, however, definitive taxonomic affinities are quite unclear.
- Timeline of therizinosaur research
- Rinchen Barsbold
- Glossary of dinosaur anatomy
- Anatomical terms of location
- Barsbold, R. (1979). "Opisthopubic pelvis in the carnivorous dinosaurs". Nature. 279: 792–793. doi:10.1038/279792a0.
- Barsbold, R.; Perle, A. (1980). "Segnosauria, a new suborder of carnivorous dinosaurs" (PDF). Acta Palaeontologica Polonica. 25 (2): 190–192.
- Barsbold, R. (1983). "Хищные динозавры мела Монголии" [Carnivorous dinosaurs from the Cretaceous of Mongolia] (PDF). Transactions of the Joint Soviet-Mongolian Paleontological Expedition (in Russian). 19: 89. Translated paper
- Currie, P. J.; Eberth, D. A. (1993). "Palaeontology, sedimentology and palaeoecology of the Iren Dabasu Formation (Upper Cretaceous), Inner Mongolia, People's Republic of China". Cretaceous Research. 14 (2): 138. doi:10.1006/cres.1993.1011.
- Clark, J. M.; Maryańska, T.; Barsbold, R. (2004). "Therizinosauroidea". The Dinosauria. University of California Press. p. 159.
- Paul, G. S. (2010). The Princeton Field Guide to Dinosaurs. Princeton University Press. p. 159. ISBN 978-0-6911-3720-9.
- Dodson, P. (1993). "Erlikosaurus". The Age of Dinosaurs. Publications International, LTD. p. 142. ISBN 0-7853-0443-6.
- Clark, J. M.; Perle, A.; Norell, M. (1994). "The skull of Erlicosaurus andrewsi, a Late Cretaceous "Segnosaur" (Theropoda, Therizinosauridae) from Mongolia". American Museum Novitates. 3115: 1–39. hdl:2246/3712.
- Khishigjav Tsogtbaatar; David B. Weishampel; David C. Evans; Mahito Watabe (2019). "A new hadrosauroid (Dinosauria: Ornithopoda) from the Late Cretaceous Baynshire Formation of the Gobi Desert (Mongolia)". PLoS ONE. 14 (4): e0208480. Bibcode:2019PLoSO..1408480T. doi:10.1371/journal.pone.0208480. PMC 6469754. PMID 30995236.
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- Zanno, L. E.; Tsogtbaatar, K.; Chinzorig, T.; Gates, T. A. (2016). "Specializations of the mandibular anatomy and dentition of Segnosaurus galbinensis (Theropoda: Therizinosauria)". PeerJ. 4: e1885. doi:10.7717/peerj.1885. PMC 4824891. PMID 27069815.
- Macaluso, L.; Tschopp, E.; Mannion, P. (2018). "Evolutionary changes in pubic orientation in dinosaurs are more strongly correlated with the ventilation system than with herbivory". Palaeontology. 61 (5): 703–719. doi:10.1111/pala.12362.
- Lee, Y. M.; Lee, H. J.; Kobayashi, Y.; Carabajal, A. P.; Barsbold, R.; Fiorillo, A. R.; Tsogtbaatar, K. (2019). "Unusual locomotion behaviour preserved within a crocodyliform trackway from the Upper Cretaceous Bayanshiree Formation of Mongolia and its palaeobiological implications". Palaeogeography, Palaeoclimatology, Palaeoecology. 533 (109353): 2. doi:10.1016/j.palaeo.2019.109239.
- Kubota, K.; Barsbold, R. (2007). "New dromaeosaurid (Dinosauria Theropoda) from the Upper Cretaceous Bayanshiree Formation of Mongolia". Journal of Vertebrate Paleontology. 27 (suppl. to 3): 102A. doi:10.1080/02724634.2007.10010458.
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