Shastasaurus
Temporal range: Middle-Late Triassic,
Partial skull of Shastasaurus pacificus (UCMP 9017)
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Order: †Ichthyosauria
Suborder: †Longipinnati
Node: †Merriamosauria
Family: †Shastasauridae
Merriam, 1895
Genus: †Shastasaurus
Merriam, 1895
Type species
†Shastasaurus pacificus
Merriam, 1895
Species

†S. pacificus
Merriam, 1895
†S.? liangae
(Yin et al., 2000 [originally Guanlingsaurus])
†S.? sikanniensis
(Nicholls & Manabe, 2004 [originally Shonisaurus])

Synonyms
  •  ?Guanlingsaurus Yin et al., 2000

Shastasaurus ("Mount Shasta lizard") is an extinct genus of ichthyosaur from the middle and late Triassic.[2] Specimens have been found in the United States, Canada, and China.[3]

Description

Size of Shonisaurus popularis (green) and S. sikanniensis (red), a possible species of Shastasaurus, compared with a human

Shastasaurus lived during the late Triassic period. The type species Shastasaurus pacificus is known from California. S. pacificus was a medium-sized ichthyosaur, measuring over 7 metres (23 ft) in length.[4] A second possible species of Shastasaurus, S. sikanniensis, is known from the Pardonet Formation British Columbia, dating to the middle Norian age (about 210 million years ago).[5] S. sikanniensis is one of the largest ichthyosaurs, measuring up to 21 metres (69 ft) in length and weighing 81.5 metric tons (89.8 short tons).[6]

Shastasaurus was highly specialized, and differed considerably from other ichthyosaurs. It was very slender in profile. S. sikanniensis had a ribcage slightly less than 2 metres (6.6 ft) deep despite a distance of over 7 metres (23 ft) between its flippers.[5] Due to its unusually short, toothless snout (compared to the long, toothed, dolphin-like snouts of most ichthyosaurs) it was proposed that Shastasaurus was a suction feeder, feeding primarily on soft-bodied cephalopods,[7] although current research indicates ichthyosaur jaws do not fit the suction-feeding profile.[8]

It is unknown whether Shastasaurus had a dorsal fin; however, the more basal ichthyosaur Mixosaurus had a dorsal fin.[9] The upper fluke of the tail was probably much less developed than the shark-like tails found in later species.[10]

Species and synonyms

Restoration of S. pacificus

The type species of Shastasaurus is S. pacificus, from the late Carnian of northern California. It is known only from fragmentary remains, which have led to the assumption that it was a 'normal' ichthyosaur in terms of proportions, especially skull proportions. Several species of long-snouted ichthyosaur were referred to Shastasaurus based on this misinterpretation, but are now placed in other genera (including Callawayia and Guizhouichthyosaurus).[7]

S. sikanniensis specimen, Royal Tyrrell Museum

Shastasaurus may include a second species, Shastasaurus liangae. It is known from several good specimens, and was originally placed in the separate genus Guanlingsaurus. Complete skulls show that it had an unusual short and toothless snout. S. pacificus probably also had a short snout, although its skull is incompletely known.[7] S. sikanniensis was originally described in 2004 as a large species of Shonisaurus. However, this classification was not based on any phylogenetic analysis, and the authors also noted similarities with Shastasaurus. The first study testing its relationships, in 2011, supported the hypothesis that it was indeed more closely related to Shastasaurus than to Shonisaurus, and it was reclassified as Shastasaurus sikanniensis.[7] However, a 2013 analysis supported the original classification, finding it more closely related to Shonisaurus than to Shastasaurus.[11] In the 2019 study, S. sikanniensis was pertained within the genus Shastasaurus.[12] In the 2021 analysis, S. sikanniensis forms a clade with Shonisaurus, indicating that it is closer to Shonisaurus than to Shastasaurus.[13] Specimens belonging to S. sikanniensis have been found in the Pardonet Formation British Columbia, dating to the middle Norian age (about 210 million years ago).[5]

In 2009, Shang & Li reclassified the species Guizhouichthyosaurus tangae as Shastasaurus tangae. However, later analysis showed that Guizhouichthyosaurus was in fact closer to more advanced ichthyosaurs, and so cannot be considered a species of Shastasaurus.[7]

Dubious species that were referred to this genus include S. carinthiacus (Huene, 1925) from the Austrian Alps and S. neubigi (Sander, 1997) from the German Muschelkalk.[3] S. neubigi, however, was re-described and reassigned to its own genus, Phantomosaurus.[14]

Synonyms of S. / G. liangae:
Guanlingichthyosaurus[15] liangae Wang et al., 2008 (lapsus calami)

Synonyms of S. pacificus:
Shastasaurus alexandrae Merriam, 1902
Shastasaurus osmonti Merriam, 1902

See also

References

  1. ↑ "†Shastasaurus Merriam 1895 (ichthyosaur)". Paleobiology Database. Fossilworks. Retrieved 17 December 2021.
  2. ↑ Hilton, Richard P., Dinosaurs and Other Mesozoic Animals of California, University of California Press, Berkeley 2003 ISBN 0-520-23315-8, at pages 90-91.
  3. 1 2 Shang Qing-Hua, Li Chun (2009). "On the occurrence of the ichthyosaur Shastasaurus in the Guanling Biota (Late Triassic), Guizhou, China" (PDF). Vertebrata PalAsiatica. 47 (3): 178–193.
  4. ↑ Michael W. Maisch and Andreas T. Matzke (2000). "The Ichthyosauria" (PDF). Stuttgarter Beiträge zur Naturkunde: Serie B. 298: 1–159. Archived from the original (PDF) on 2011-07-18.
  5. 1 2 3 Nicholls, E.L.; Manabe, M. (2004). "Giant ichthyosaurs of the Triassic - a new species of Shonisaurus from the Pardonet Formation (Norian: Late Triassic) of British Columbia". Journal of Vertebrate Paleontology. 24 (3): 838–849. doi:10.1671/0272-4634(2004)024[0838:GIOTTN]2.0.CO;2.
  6. ↑ Sander, P.M.; Griebeler, E.M.; Klein, N.; Juarbe, J.V.; Wintrich, T.; Revell, L.J.; Schmitz, L. (2021). "Early giant reveals faster evolution of large body size in ichthyosaurs than in cetaceans" (PDF). Science. 374 (6575): eabf5787. doi:10.1126/science.abf5787. PMID 34941418. S2CID 245444783.
  7. 1 2 3 4 5 Sander P, Chen X, Cheng L, Wang X (2011). Claessens L (ed.). "Short-Snouted Toothless Ichthyosaur from China Suggests Late Triassic Diversification of Suction Feeding Ichthyosaurs". PLOS ONE. 6 (5): e19480. Bibcode:2011PLoSO...619480S. doi:10.1371/journal.pone.0019480. PMC 3100301. PMID 21625429.
  8. ↑ Motani R, Tomita T, Maxwell E, Jiang D, Sander P (2013). "Absence of Suction Feeding Ichthyosaurs and Its Implications for Triassic Mesopelagic Paleoecology". PLOS ONE. 8 (12): e66075. Bibcode:2013PLoSO...866075M. doi:10.1371/journal.pone.0066075. PMC 3859474. PMID 24348983.
  9. ↑ Renesto, Silvio; Dal Sasso, Cristiano; Fogliazza, Fabio; Ragni, Cinzia (2020). "New findings reveal that the middle Triassic ichthyosaur Mixosaurus cornalianus is the oldest amniote with a dorsal fin". Acta Palaeontologica Polonica. 65. doi:10.4202/app.00731.2020. ISSN 0567-7920.
  10. ↑ Wallace, D.R. (2008). Neptune's Ark: From Ichthyosaurs to Orcas. University of California Press, 282pp.
  11. ↑ Ji, C.; Jiang, D. Y.; Motani, R.; Hao, W. C.; Sun, Z. Y.; Cai, T. (2013). "A new juvenile specimen of Guanlingsaurus (Ichthyosauria, Shastasauridae) from the Upper Triassic of southwestern China". Journal of Vertebrate Paleontology. 33 (2): 340–348. doi:10.1080/02724634.2013.723082. S2CID 83784699.
  12. ↑ Moon, B. (2019). "A new phylogeny of ichthyosaurs (Reptilia: Diapsida)". Journal of Systematic Palaeontology. 17: 1–27.
  13. ↑ Bindellini G; Wolniewicz AS; Miedema F; Scheyer TM (2021). "Cranial anatomy of Besanosaurus leptorhynchus Dal Sasso & Pinna, 1996 (Reptilia: Ichthyosauria) from the Middle Triassic Besano Formation of Monte San Giorgio, Italy/Switzerland: taxonomic and palaeobiological implications". PeerJ. 9 (e11179). doi:10.7717/peerj.11179. hdl:11573/1682932.
  14. ↑ Maisch, M. W.; Matzke, A. T. (2006). "The braincase of Phantomosaurus neubigi (Sander, 1997), an unusual ichthyosaur from the Middle Triassic of Germany". Journal of Vertebrate Paleontology. 26 (3): 598–607. doi:10.1671/0272-4634(2006)26[598:TBOPNS]2.0.CO;2.
  15. ↑ Xiaofeng, W.; Bachmann, G. H.; Hagdorn, H.; Sander, P. M.; Cuny, G.; Xiaohong, C.; Chuanshang, W.; Lide, C.; Long, C.; Fansong, M.; Guanghong, X. U. (2008). "The Late Triassic Black Shales of the Guanling Area, Guizhou Province, South-West China: A Unique Marine Reptile and Pelagic Crinoid Fossil Lagerstätte". Palaeontology. 51: 27–61. doi:10.1111/j.1475-4983.2007.00735.x.
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