Erketu
Temporal range: Late Cretaceous,
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Skeletal reconstruction of the holotype
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: †Sauropodomorpha
Clade: †Sauropoda
Clade: †Macronaria
Clade: †Titanosauriformes
Clade: †Somphospondyli
Genus: †Erketu
Ksepka & Norell 2006
Type species
†Erketu ellisoni
Ksepka & Norell 2006

Erketu (meaning "Erketü Tengri") is a genus of somphospondylan sauropod dinosaur that lived in Asia during the Late Cretaceous roughly between 96 million and 89 million years ago. Its fossils were found in Mongolia between 2002 and 2003 during a field expedition and first described in 2006; later on in 2010 due to some cervicals that were left behind in the expedition. Erketu represents one of the first sauropods described from the Bayan Shireh Formation. The elongated cervical vertebrae of Erketu indicates that it was the sauropod with the longest neck relative to its body size.

Discovery and naming

The first remains of Erketu were found back in 2002 by the American Museum of Natural History–Mongolian Academy of Sciences expedition conducted in Mongolia. The team discovered the outcrops of the new locality Bor Guvé, which overlies the Khara Kuthul locality and therefore is referable to the Bayan Shireh Formation. The unearthed specimen, IGM 100/1803, was found in exposure at the sediments of Bor Guvé, mainly composed by sandstone and interbedded grey siltstones, suggesting a fluvial environment that is consistent with the Bayan Shireh Formation. Collected elements are mainly represented by cervical vertebrae and postcranial remains, such as the partial right sternum, tibia and fibula with astragalus and calcaneum.[1]

The remains became the holotype for the new genus and species Erketu ellisoni, first described in 2006 by Daniel Ksepka and Mark Norell of the American Museum of Natural History. The generic name of this particular sauropod species is named after the creator god (tengri) of the Mongolian shamanism, Erketü. The specific name, ellisoni, is in honor to the American Museum of Natural History's senior principal paleoartist, and close friend of Norell: Mick Ellison.[1] In 2003 the team returned to the site and recovered three additional cervicals that were left behind during the first field expedition, and consequently described in 2010.[2]

Description

Four cervical vertebrae from the holotype

Erketu was a relatively large sauropod, with an estimated length of 15 m (49 ft) and a weight of 5 t (11,000 lb).[3] Its neck was estimated to be twice as long as its body, which may be a record for neck to body ratio. The exact ratio is unknown, because no dorsal vertebrae of E. ellisoni have been reported, although some hindlimb material suggests the approximate size of the body. The long neck of Erketu is the result of the individual vertebrae being greatly elongated; it is unknown if the number of cervical vertebrae was increased. Erketu is also diagnosed by bifurcate anterior cervical neural spines, another unusual trait for a titanosauriform. The preserved cervicals include the atlas, axis and C3 to C9, however, the sixth is missing, giving a total of eight preserved cervical vertebrae.[1][2]

Size comparison with a human

The preserved sternum is rather thickened at some borders and shows a very deep lateral edge, it measures about 530 mm (53 cm) long. The right hindlimb elements were nicely found in articulation and they resemble those of Gobititan. The tibia is very straight, measuring 710 mm (71 cm) in total length, it has slightly expanded ends and in comparison to that of Opisthocoelicaudia, the anterior and distal expansions are not very developed. The fibula is longer than the tibia with a length of 750 mm (75 cm), however, it appears to be broken on the distal end of one of the trochanters.[1]

Classification

The phylogenetic analysis of sauropods performed by its describers indicates that Erketu is a basal somphospondylian (the clade of all macronarians closer to titanosaurs than to brachiosaurids), and is most closely related to Titanosauria, being a close relative of Euhelopus.[1]

During the description of Europatitan in 2017, a new cladistic analysis was performed. Here, Erketu was recovered in a polytomy along Chubutisaurus within the Somphospondyli:[4]

Somphospondyli

Europatitan eastwoodi

Tendaguria tanzaniensis

Sauroposeidon proteles

Chubutisaurus insignis

Erketu ellisoni

Titanosauria

Paleoecology

Erketu compared to the known Dinosauria of the Bayan Shireh Formation (Erketu in brown, third from left)

The remains of Erketu are attributed to the Bayan Shireh Formation,[2] which is believed to have been dominated by fluvial and lacrustine environments, such as large meanders and lakes but also a notorious semi-arid climate.[5][6] The age is estimated to be around 95.9 ± 6.0 million to 89.6 ± 4.0 million years ago, Cenomanian to Santonian epochs.[7][8] Here, Erketu lived alongside diverse dinosaur fauna, such as the predators Achillobator[9] and potentially Alectrosaurus,[10] the abundant hadrosauroid Gobihadros,[11] heavy armored Talarurus and Tsagantegia,[12] and the well-known therizinosaurs Erlikosaurus and Segnosaurus.[13] The locality of Erketu has also yielded an indeterminate/unnamed titanosaur and very abundant fossilized fruits.[1][2] Some ecological niches were filled by several dinosaurs, such as the browsers Erlikosaurus, Segnosaurus[13] and Tsagantegia; in contrast, Talarurus was a grazer.[12] Erketu in the other hand, due to its very long neck, was likely a high browser.[3]

See also

References

  1. 1 2 3 4 5 6 Ksepka, D. T.; Norell, M. A. (2006). "Erketu ellisoni, a long-necked sauropod from Bor Guvé (Dornogov Aimag, Mongolia)" (PDF). American Museum Novitates (3508): 1−16. doi:10.1206/0003-0082(2006)3508[1:EEALSF]2.0.CO;2. hdl:2246/5783.
  2. 1 2 3 4 Ksepka, D. T.; Norell, M. A. (2010). "The Illusory Evidence for Asian Brachiosauridae: New Material of Erketu ellisoni and a Phylogenetic Reappraisal of Basal Titanosauriformes" (PDF). American Museum Novitates (3700): 1–27. doi:10.1206/3700.2. hdl:2246/6087. S2CID 86254470.
  3. 1 2 Paul, G. S. (2016). The Princeton Field Guide to Dinosaurs (2nd ed.). Princeton, New Jersey: Princeton University Press. pp. 223−224. ISBN 9780691167664.
  4. ↑ Fernández-Baldor, F. T.; Canudo, J. I.; Huerta, P.; Moreno-Azanza, M.; Montero, D. (2017). "Europatitan eastwoodi, a new sauropod from the lower Cretaceous of Iberia in the initial radiation of somphospondylans in Laurasia". PeerJ. 5: e3409. doi:10.7717/peerj.3409. PMC 5490465. PMID 28674644.
  5. ↑ Ishigaki, S.; Tsogtbaatar, K.; Saneyoshi, M.; Mainbayar, B.; Aoki, K.; Ulziitseren, S.; Imayama, T.; Takahashi, A.; Toyoda, S.; Bayardorj, C.; Buyantegsh, B.; Batsukh, J.; Purevsuren, B.; Asai, H.; Tsutanaga, S.; Fujii, K. (2016). "Report of the Okayama University of Science - Mongolian Institute of Paleontology and Geology Joint Expedition in 2016" (PDF). Bulletin of Research Institute of Natural Sciences (42): 33−46.
  6. ↑ Slowiak, J.; Szczygielski, T.; Ginter, M.; Fostowicz-Frelik, L. (2020). "Uninterrupted growth in a non‐polar hadrosaur explains the gigantism among duck‐billed dinosaurs". Palaeontology. 63 (4): 579–599. doi:10.1111/pala.12473.
  7. ↑ Danilov, I. G.; Hirayama, R.; Sukhanov, V. B.; Suzuki, S.; Watabe, M.; Vitek, N. S. (2014). "Cretaceous soft-shelled turtles (Trionychidae) of Mongolia: new diversity, records and a revision". Journal of Systematic Palaeontology. 12 (7): 799–832. doi:10.1080/14772019.2013.847870. S2CID 86304259.
  8. ↑ Kurumada, Y.; Aoki, S.; Aoki, K.; Kato, D.; Saneyoshi, M.; Tsogtbaatar, K.; Windley, B. F.; Ishigaki, S. (2020). "Calcite U–Pb age of the Cretaceous vertebrate‐bearing Bayn Shire Formation in the Eastern Gobi Desert of Mongolia: usefulness of caliche for age determination". Terra Nova. 32 (4): 246–252. doi:10.1111/ter.12456.
  9. ↑ Perle, A.; Norell, M. A.; Clark, J. (1999). "A new maniraptoran Theropod−Achillobator giganticus (Dromaeosauridae)−from the Upper Cretaceous of Burkhant, Mongolia". Contributions from the Geology and Mineralogy Chair, National Museum of Mongolia (101): 1–105. OCLC 69865262.
  10. ↑ Perle, A. (1977). "O pervoy nakhodke Alektrozavra (Tyrannosauridae, Theropoda) iz pozdnego Mela Mongolii" [On the first discovery of Alectrosaurus (Tyrannosauridae, Theropoda) in the Late Cretaceous of Mongolia]. Shinzhlekh Ukhaany Akademi Geologiin Khureelen (in Russian). 3 (3): 104–113.
  11. ↑ Tsogtbaatar, K.; Weishampel, D. B.; Evans, D. C.; Watabe, M. (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.
  12. 1 2 Park, J. (2020). "Additional skulls of Talarurus plicatospineus (Dinosauria: Ankylosauridae) and implications for paleobiogeography and paleoecology of armored dinosaurs". Cretaceous Research. 108: e104340. doi:10.1016/j.cretres.2019.104340.
  13. 1 2 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.
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