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Emausaurus

From Wikipedia, the free encyclopedia
Extinct genus of thyreophoran dinosaurs

Emausaurus
Temporal range: EarlyToarcian
~183–182 MaTenuicostatum
Dentary bone ofEmausaurus ernsti
Scientific classificationEdit this classification
Kingdom:Animalia
Phylum:Chordata
Class:Reptilia
Clade:Dinosauria
Clade:Ornithischia
Clade:Genasauria
Clade:Thyreophora
Genus:Emausaurus
Haubold, 1990
Species:
E. ernsti
Binomial name
Emausaurus ernsti
Haubold, 1990

Emausaurus is agenus ofthyreophoran or armoreddinosaur from theEarly Jurassic (EarlyToarcian). Its fossils have been found in theLehmhagen Member, inMecklenburg-Vorpommern, northernGermany.Emausaurus is the only knownToarcian thyreophoran, as well as the only dinosaur from the zone of the same age with a formal name.[1]

Discovery and naming

[edit]
Profile at Grimmen with Emausaurus horizon marked

Thetype and only species,E. ernsti, was named and described byHartmut Haubold in 1990.[2] Thegeneric name is composed of anacronym ofErnst Moritz Arndt University of Greifswald and theGreeksauros/σαυρος (lizard). Thespecific name is derived from the name of geologist Werner Ernst, who acquired theholotype specimen,SGWG 85, in the summer of 1963 from foreman Werner Wollin at a loam pit nearGrimmen, in strata dating from theToarcian. It is known by the right side of the skull, the right lower jaw, caudal vertebrae, neural arches, a radius, a metatarsal, a claw, fragments of ribs, scutes, and plates, known as EMAU SGWG 85.[1]

Description

[edit]
Size compared to a human

Emausaurus was probably a semi-bipedal to quadrupedal animal, being covered in an armor ofosteoderms across the body. Like other thyreophorans, it probably was an herbivore, specifically a low dwelling one, with a diet associated with ground flora, such ascycads andBennettitales.[1] The body length of the holotype juvenile individual ofEmausaurus has been estimated at 2–2.5 m (6.6–8.2 ft), with a body mass of 50–90 kg (110–200 lb).[3][4][1] The adult length has been estimated at 3–4 m (9.8–13.1 ft), with a body mass up to 240 kg (530 lb).[1] Some recent data suggest the holotype may be from a subadult rather than a juvenile.[5] Most of the reconstruction has been based onScelidosaurus, although it is possible thatEmausaurus was a more bipedal animal, as some of the young specimens ofScelidosaurus were thought to be. Adult forms probably were more quadrupedal. Unfortunately, the type specimen is too incomplete to infer a mode of locomotion.[6] Armor includes three conical scutes and one tall, spiny element.[7] In 2019, David Norman examined the morphology ofScelidosaurus, comparing it withEmausaurus. InEmausaurus, the maxilla has, overall, a similar morphology to that seen inScelidosaurus. The disarticulated maxilla ofEmausaurus exhibits an anteromedially directed robust process with which it met its counterpart in the midline, creating a wedge-like structure, with no obvious offset between the alveolar margins. InEmausaurus, the structure of the frontals is not well preserved. In outline, its proportions resemble those ofScelidosaurus, but the same is true of manyOrnithischia. The lacrimal bone ofEmausaurus is incomplete, but includes a long, curved jugal process that evidently wrapped itself around the anterior tip of the jugal.[8]Very little is known of the postcraniumEmausaurus, recovering parts like a multipartite odontoid (sutured to the axis centrum), similar to that ofScelidosaurus.[9]Emausaurus has a series of assigned osteoderms, but lacks likeScutellosaurus 'scapular osteoderms'. The major series of osteoderms found appear to come from the tail or the dorsal section.[10]

Classification

[edit]

Cladistic analyses have shown thatEmausaurus was a basal member of theThyreophora, more derived thanScutellosaurus, but less thanScelidosaurus.[11]Scelidosaurus,Emausaurus, andScutellosaurus cluster at the base of most trees because they can be scored for only a restricted number of anatomical characters.[12]The cladistic status of the specimen is relatively controversial due to its young nature. It is clearly a member of the Thyreophora, but its position may be modified if an adult specimen is found.Emausaurus may be more derived thanScelidosaurus, or even be a sister taxon toStegosauria.[13] The general consensus has establishedEmausaurus as a non-eurypodan stem thyreophoran, along withScutellosaurus andScelidosaurus reinforced by almost all subsequent systematic reviews of ornithischian–thyreophoran relationships.[14] BeingEmausaurus andScutellosaurus more basal thanScelidosaurus.[14]Emausaurus has been put on an outgroup to Ankylosauria, withScelidosaurus and the basal stegosaurHuayangosaurus.[15] Vickaryous et al. (2004), did the default phylogenetic analysis for ingroup ankylosaurs, due to including cranial and postcranial characters, a wide range of taxa and made no in-group relationships, although this analysis used the holotypeLesothosaurus andHuayangosaurus as outgroups, ignoringScelidosaurus andEmausaurus.[14] In 2020, Norman found thatScelidosaurus, along withScutellosaurus andEmausaurus, are positioned on the stem ofAnkylosauria, rather than on the stem ofThyreophora, withEmausaurus as the basal sister-taxon toScelidosaurus.[16] This is becauseEmausaurus possesses a dorsal margin of the dentary sinuous in lateral view and neither elongated nor squat proportions of metacarpal 1 'medium'.[16] Alternatively,Emausaurus may be a basal sister-taxon toScutellosaurus, but taking the similarities betweenEmausaurus andScelidosaurus this is less likely.[16] Yet this was contested the same year with the description of +70 specimens ofScutellosaurus, whereEmausaurus was found as sister taxon of this last one and both with strong evidence for a phylogenetic placement within Thyreophora but outside ofThyreophoroidea.[6] A cladogram following the results of Norman (2020) is shown below:

Thyreophora

Paleoecology

[edit]
Restoration ofEmausaurus being attacked by an unnamed theropod belonging to theOrionides
Lehmhagen Member biota

Emausaurus has a sinuous jaw profile, more advanced in ankylosauromorphs, unlike the rectilinear morphology seen in the more basal genusScutellosaurus.[16] The changes to the jaw are considered a series of modifications reflecting changes in the diet and evolution of the food processing of this dinosaur compared to its ancestors. It seems to be adapted to eat Coriaceous flora, such as bennettites and cycads, abundant on the coevalSorthat Formation, where probably this taxon lived.[17] The rest of the skeleton of this genus is poorly presented, with for example the vertebrae showing no evidence of the proportional changes in the height of the neural arches and spines seen on stegosaurs.[16] The animal was covered in osteoderms, although the few found give no indication of how extensively they were distributed across the torso.[16]Emausaurus, based on the proportions of the preserved metacarpals that the forelimb shows adaptations for weight support, rather than grasping, having ungual phalanges that are conical and only slightly decurved.[16]The partially known proximal pedal phalanges are short and block-like, with near the same proportions seen in the pes ofScelidosaurus.[16] A series of characters that together are suggestive of graviportality and quadrupedality, makingEmausaurus a low roaming herbivore. Pseudo-bipedality is not discarded, with the animal able to reach slightly taller flora.[16] Later works however have criticised this assumption given the relationships withScutellosaurus are more likely and recommend to not infer bipedality or quadrupedality as the taxon is incomplete.[6]

Paleoenvironment

[edit]

The holotype ofEmausaurus was found in the so-called "Emausaurus type site", which represents a shale ingression from theLehmhagen Member, dated from the Lower Toarcian.[18] The site is a boundary composed of bituminous shale,[2] representing an ancient seashore-influenced environment, probably lagoonal, and contemporaneous with theSorthat Formation of the same region. Fossil wood has been found in the same location, includingdriftwood and others related to theAraucariaceae, present in other European environments of Toarcian age.[2] The invertebrate fauna consists of insects, bivalves, sea snails and ammonites (Tiltoniceras,Eleganticeras andLobolytoceras).[2] The vertebrate fauna is also diverse, with fossils of the fish generaSaurorhynchus,[19]Grimmenichthys,[20] andGrimmenodon.[21] Reptile fossils include indeterminateichthyosaurs andplesiosaurs,rhomaleosaurid plesiosaurs, indeterminatemesoeucrocodylians (probably related toSichuanosuchus), indeterminatethalattosuchians,[22] a possiblepterosaur,[23] and theropod andgravisaurian sauropod material, the latter related to the north AfricanTazoudasaurus.[24] A later discovery includes a thyreophoran osteoderm, interpreted as representing a lateral of the neck or shoulder region.[5]

References

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  1. ^abcdeHaubold, H. (1991). "Der Greifswalder DinosaurierEmausaurus".Fundgrube.27 (2):51–60.
  2. ^abcdHaubold, H. (1990)."Ein neuer Dinosaurier (Ornithischia, Thyreophora) aus dem Unteren Jura des nördlichen Mitteleuropa".Revue de Paléobiologie.9 (1):149–177. Retrieved24 October 2021.
  3. ^Holtz, Thomas R. Jr. (2012).Dinosaurs: The Most Complete, Up-to-Date Encyclopedia for Dinosaur Lovers of All Ages(PDF).Winter 2011 Appendix
  4. ^Paul, Gregory S. (2016).The Princeton Field Guide to Dinosaurs. Princeton University Press. p. 242.ISBN 978-1-78684-190-2.OCLC 985402380.
  5. ^abSchade, Marco; Ansorge, Jörg (2022)."New thyreophoran dinosaur material from the Early Jurassic of northeastern Germany".Paläontologische Zeitschrift.96 (1–14):303–311.Bibcode:2022PalZ...96..303S.doi:10.1007/s12542-022-00605-x.S2CID 246040635.
  6. ^abcBreeden III, B. T; Raven, T. J; Butler, R. J.; Rowe, T. B.; Maidment, S. C. (2021)."The anatomy and palaeobiology of the early armoured dinosaurScutellosaurus lawleri (Ornithischia: Thyreophora) from the Kayenta Formation (Lower Jurassic) of Arizona".Royal Society Open Science.8 (7) 201676.Bibcode:2021RSOS....801676B.doi:10.1098/rsos.201676.PMC 8292774.PMID 34295511.
  7. ^Norman, D.B.; Witmer, L.M. & Weishampel, D.B. (2004). "Basal Thyreophora". In Weishampel, D.B.; Dodson, P. & Osmólska, H. (eds.).The Dinosauria, 2nd Edition. University of Californian Press. pp. 335–342.ISBN 0-520-24209-2.
  8. ^Norman, D. B. (2019)."Scelidosaurus harrisonii from the Early Jurassic of Dorset, England: cranial anatomy".Zoological Journal of the Linnean Society.188 (1):1–81.doi:10.1093/zoolinnean/zlz074. Retrieved17 November 2021.
  9. ^Norman, D. B. (2019)."Scelidosaurus harrisonii from the Early Jurassic of Dorset, England: postcranial skeleton".Zoological Journal of the Linnean Society.189 (1):47–157.doi:10.1093/zoolinnean/zlz078. Retrieved17 November 2021.
  10. ^Norman, D. B. (2020)."Scelidosaurus harrisonii from the Early Jurassic of Dorset, England: the dermal skeleton".Zoological Journal of the Linnean Society.190 (1):1–53.doi:10.1093/zoolinnean/zlz085. Retrieved17 November 2021.
  11. ^Sereno, P. C. (1997)."The origin and evolution of dinosaurs"(PDF).Annual Review of Earth and Planetary Sciences.25 (1):435–489.Bibcode:1997AREPS..25..435S.doi:10.1146/annurev.earth.25.1.435.
  12. ^Butler, R.J.; Upchurch, P.; Norman, D.B. (2008). "The phylogeny of the ornithischian dinosaurs".Journal of Systematic Palaeontology.6 (1):1–40.Bibcode:2008JSPal...6....1B.doi:10.1017/S1477201907002271.S2CID 86728076.
  13. ^Stumpf, S.; Meng, S. (2013)."Dinosaurier aus Nordostdeutschland: Verschleppt".Biologie in unserer Zeit.43 (6):362–368.doi:10.1002/biuz.201310521.S2CID 83200480. Retrieved24 October 2021.
  14. ^abcCoombs, W.P.; Maryańska, T. (1990). "Ankylosauria".The Dinosauria.1 (1):456–483.
  15. ^Witmer, Hill R.V.; Norell, L.M. (2003). "A new specimen of Pinacosaurus grangeri (Dinosauria: Ornithischia) from the Late Cretaceous of Mongolia: ontogeny and phylogeny of ankylosaurs".American Museum Novitates (1):1–29.
  16. ^abcdefghiNorman, D. B. (2020)."Scelidosaurus harrisonii (Dinosauria: Ornithischia) from the Early Jurassic of Dorset, England: biology and phylogenetic relationships".Zoological Journal of the Linnean Society.192 (1):1–86. Retrieved17 November 2021.
  17. ^McElwain, J. C.; Wade-Murphy, J.; Hesselbo, S. P. (2005)."Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals".Nature.435 (7041):479–482.Bibcode:2005Natur.435..479M.doi:10.1038/nature03618.PMID 15917805.S2CID 4339259. Retrieved8 September 2021.
  18. ^Ernst, W. (1967). "Die Liastongrube Grimmen. Sediment, Makrofauna und Stratigraphie".Ein Überblick Geologie.16 (1):550–569.
  19. ^Maxwell, E. E.; Stumpf, S. (2017)."Revision ofSaurorhynchus (Actinopterygii: Saurichthyidae) from the Early Jurassic of England and Germany".European Journal of Taxonomy (321):1–29.doi:10.5852/ejt.2017.321. Retrieved24 October 2021.
  20. ^Konwert, M.; Hörnig, M. (2018)."Grimmenichthys ansorgei, gen. et sp. nov. (Teleostei, "Pholidophoriformes"), and other "pholidophoriform" fishes from the early Toarcian of Grimmen (Mecklenburg-Western Pomerania, Germany)".Journal of Vertebrate Paleontology.38 (3):1–16.doi:10.1080/02724634.2018.1451872.hdl:11336/84457.S2CID 90344418. Retrieved24 October 2021.
  21. ^Stumpf, S.; Ansorge, J.; Pfaff, C; Kriwet, J. (2017)."Early Jurassic diversification of pycnodontiform fishes (Actinopterygii, Neopterygii) after the end-Triassic extinction event: evidence from a new genus and species, Grimmenodon aureum".Journal of Vertebrate Paleontology.37 (4) e1344679.Bibcode:2017JVPal..37E4679S.doi:10.1080/02724634.2017.1344679.PMC 5646184.PMID 29170576.
  22. ^Stumpf, Sebastian (2017).A synoptic review of the vertebrate fauna from the "Green Series"(Toarcian) of northeastern Germany with descriptions of new taxa: A contribution to the knowledge of Early Jurassic vertebrate palaeobiodiversity patterns(PDF) (PhD Thesis). Greifswald University. pp. 1–47. Retrieved9 September 2021.
  23. ^Schade, Marco; Ansorge, Jörg (2024)."Enigmatic fragment possibly marks the first pterosaur record from the Lower Toarcian of Grimmen, NE Germany".PalZ.doi:10.1007/s12542-024-00698-6.
  24. ^Stumpf, Sebastian; Ansorge, Jörg; Krempien, Wilfried (2015)."Gravisaurian sauropod remains from the marine late Early Jurassic (Lower Toarcian) of North-Eastern Germany".Geobios.48 (3):271–279.Bibcode:2015Geobi..48..271S.doi:10.1016/j.geobios.2015.04.001. Retrieved30 July 2021.

External links

[edit]
Avemetatarsalia
Ornithischia
    • see below↓
Heterodontosauridae
Thyreophora
Ankylosauria
Stegosauria
Thescelosauridae
Ornithopoda
Marginocephalia
Ceratopsia
Pachycephalosauria
Laquintasaura venezuelae

Heterodontosaurus tuckiScutellosaurus lawleriKulindadromeus zabaikalicus

Thescelosaurus neglectus
See also
Nomina dubia
Incertae sedis
Other taxa
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Emausaurus
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