Morrosaurus

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Morrosaurus
Temporal range: Maastrichtian
~70–66  Ma
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Morrosaurus.jpg
Life restoration
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade:† Ornithischia
Clade:† Neornithischia
Clade:† Ornithopoda
Clade:† Elasmaria
Genus:† Morrosaurus
Rozadilla et al., 2016
Species:
†M. antarcticus
Binomial name
†Morrosaurus antarcticus
Rozadilla et al. , 2016

Morrosaurus is an extinct genus of herbivorous elasmarian dinosaur that lived in the late Cretaceous in Antarctica. The only known species is the type Morrosaurus antarcticus. [1]

Contents

Discovery

In 2002, the Argentine paleontologist Fernando Novas reported the discovery of a partial skeleton of a euornithopod in Antarctica. [2] In 2016 these remains were the basis for naming the type species Morrosaurus antarcticus, named and described by Sebastian Rozadilla, Federico Lisandro Agnolin, Fernando Emilio Novas, Alexis Rolando Aranciaga Mauro, Matthew J. Motta, Juan Manuel Lirio Marcelo, and Pablo Isasi. The genus name refers to the site of El Morro on James Ross Island, where the remains of the species were found. The specific name refers to Antarctica. [1]

The holotype specimen MACN Pv 197, was found in a layer of the Snow Hill Island Formation (Cape Lambe, previously assigned to the Lopez de Bertodano Formation), dating to the Maastrichtian age. The remains consists in a right hind leg, including the top of the femur, the lower end of the femur, the upper part of the tibia, the underside of the tibia, the upper half of the foot, the bottom of the midfoot and the top of the first joint of the third toe. [1]

Description

Size compared to a human. Morrosaurus size chart.jpg
Size compared to a human.

The only known specimen, thought to represent an adult, is estimated to have belong to an individual 4.5–5 metres (15–16 ft) in length. [3] This makes it larger and more robust in skeletal build than many of its relatives, including the fellow Antarctic genus Trinisaura , [1] only 1.5 metres (4.9 ft) in length. [3] The fragmentary nature of the material precludes saying much about the preserved regions. It is united anatomically with other elasmarians by the strongly compressed outer front edge of the greater trochanter , lacking the distinct cleft and thick edge seen in other types of ornithopod. Other uniting traits of elasmarians seen in the humerus and vertebrae cannot be evaluated in Morrosaurus due to their lack of preservation in the genus. The femur seems to have been rather gracile, though more stout than in Trinisaura, as was the elongate foot, with the central third metatarsal being larger than the others. [1]

A series of distinctive features characterizes the genus. Two of these are autapomorphies, completely unique traits acquired by the taxon. In bottom view, the greater trochanter near the top of the femur forms an S-shape, with the back edge thick across and the front edge thin, similar to the condition seen in other elasmarians Anabisetia , Notohypsilophodon , and Gasparinisaura but displayed to a more extreme extent. The fourth metatarsal bone has a prominent rearward projection that wraps around the third metatarsal, likewise similar but more developed to the condition seen in Gasparinisaura as well as Kangnasaurus , a genus with overall similar morphology and proportions to Morrosaurus. In addition, there is a unique combination of two features that by themselves are not unique features. In the femur, the lesser trochanter is positioned forward and to the outside of the greater trochanter. In the tibia, medial malleolus has a triangular shape from the front and a concave surface from the same angle. [1]

Phylogeny

Morrosaurus was classified in the group Iguanodontia, as a basal member of Euiguanodontia. This in turn formed a clade with other ornithopods of Patagonia and Antarctica, particularly Trinisaura , Gasparinisaura , Anabisetia , Notohypsilophodon , Talenkauen and Macrogryphosaurus in a group called Elasmaria, whose members are distinguished by their adaptation to a running lifestyle which would be reflected by the narrow foot with a thin fourth metatarsal which indicates a high speed running; subsequently expanded chevrons, a feature that is associated with a greater surface area for attachment of the lateral muscles of the tail, which would give good control of the movements of this; and a curved humerus which demonstrates the absence of a deltopectoral ridge and therefore that the front leg was not used for walking. It cannot be determined, however, if Morrosaurus itself possessed these characteristics due to their limited remains. The existence of this clade may indicate that Patagonia, Antarctica and Australia shared the same type of fauna. The exact phylogenetic relationships within this clade could not be identified, except for Gasparinisaura, which proved to be the most basal member of group. [1]

Cladogram based in the phylogenetic analysis of Rozadilla et al., 2016:

Palaeobiology

Metatarsals of ornithopods from above; these bones in Morrosaurus (C) and other elasmarians (A, B, D, E, P) demonstrate their developed running abilities and have been studied to evaluate their growth rates Ornithopod right metatarsi.jpg
Metatarsals of ornithopods from above; these bones in Morrosaurus (C) and other elasmarians (A, B, D, E, P) demonstrate their developed running abilities and have been studied to evaluate their growth rates

Based on the hindlimb anatomy of Morrosaurus and other elasmarians, notably the slim metatarsus , it's thought they were very capable runners, distinguishing them from other herbivorous dinosaurs they lived alongside. Elements of relatives not preserved in Morrosaurus such as expanded chevrons and distinctive bony intercostal plates along the torso would've further aided their cursorial abilities by improving tail balance and musculature control as well as breathing efficiency. [1] This developed tail musculature and running ability of elasmarians is noted as more developed in elasmarian taxa than in other ornithopods such as Hypsilophodon . [4]

In 2020 a study was conducted on the growth rate of Morrosaurus, and its relative Trinisaura , through use of histological study of thin samples from the holotype fibula and fourth metatarsal . Ornithischian dinosaurs living in polar regions in the Northern Hemisphere (such as Edmontosaurus and Pachyrhinosaurus typically show different growth rates than relatives from lower latitutes, owing to the extreme temperatures of their environments, but studies have failed to find the same signs in Antarctic animals. The study confirmed this pattern in elasmarians, with comparison with South American elasmarian Gasparinisaura finding incredibly similar histology to the Antarctic genera. All three show rapid growth with periodic interruptions, variation in growth marks, and changes in growth rate across their life cycle, growing slower as they aged. Similar growth strategies are reported in other ornithopods from much lower latitudes. This indicates that rather than adapting their growth physiology in response to the cold, southern environments they lived in, elasmarians were able to succeed in such ecosystems due to the existing possession of necessary adaptations to thrive there. Higher growth rate was noted in Morrosaurus as compared to Trinisaura, consistent with being a larger species. Additionally, it was found the animals reached their sexual maturity well before their skeletal maturity, and ceased growth at a later point than did, consistent with other dinosaurs. [3] Neonatal fossils of elasmarians from Australia, which offer strong evidence of elasmarians living year round in high-latitude conditions rather than being migratory in nature, were similarly found to display growth rates very similar to those of other ornithopods such as Orodromeus . [5]

Palaeobiogeography

Proximity of the southern continents when Morrosaurus lived allowed faunal interchange Paleogeography Gondwana - Late Cretaceous-Early Paleogene - around 85-63 Ma.jpg
Proximity of the southern continents when Morrosaurus lived allowed faunal interchange

The discovery of Morrosaurus was concurrent with the first evidence of a previously hypothesized uniting clade of ornithopod dinosaurs from the continents that had comprised Gondwana. The distinction between fauna of this part of the world as compared with the northern hemisphere equivalent Laurasia had long been noted, but evidence was traditionally lacking for a biogeographic link for dinosaurs between the different Gondwanan regions. Brazil and Northern Africa shared a fauna distinct from that of Patagonia, and each of these distinct from that of India and Madagascar; likewise, Australia, New Zealand, and Antarctic seemed connected to the exclusion of the others. [1] This contrasted with existing recognition of links between the flora and marine invertebrate fauna between Patagonia, Antarctica, Australia, and New Zealand, termed the Weddellian Bioprovince. [1] [6]

The recognition of Morrosaurus and Trinisaura as Antarctic elasmarians closely related to animals from South America constituted important evidence of such ties between these continents existing in dinosaurs as well. [1] This would be bolstered by later studies producing firmer evidence of Australian ornithopods as also belonging to the group, as well as possibly Kangnasaurus from Africa. [4] [7] Similar biogeographic patterns have been observed in megaraptoran theropods, diamantinasaurian sauropods, and parankylosaurian ankylosaurs. [1] [8] [9] These discoveries of connected endemic Gondwanan ecosystems have overturned the traditional view of the southern continents, including the fauna seen in Late Cretaceous Antarctic, acting as a refugium for animals more successful elsewhere earlier in the Cretaceous. [6]

See also

Related Research Articles

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References

  1. 1 2 3 4 5 6 7 8 9 10 11 12 Rozadilla, Sebastián; Agnolin, Federico L.; Novas, Fernando E.; Rolando, Alexis M.Aranciaga; Motta, Matías J.; Lirio, Juan M.; Isasi, Marcelo P. (2016). "A new ornithopod (Dinosauria, Ornithischia) from the Upper Cretaceous of Antarctica and its palaeobiogeographical implications". Cretaceous Research. 57: 311–324. Bibcode:2016CrRes..57..311R. doi:10.1016/j.cretres.2015.09.009. hdl: 11336/46572 .
  2. ↑ Novas, F.E.; Cambiaso, A.V.; Lirio, J.; Núñez, H. (2002). "Paleobiogeografía de los dinosaurios cretácicos polares de Gondwana". Ameghiniana (Resúmenes). 39 (4): 15R.
  3. 1 2 3 Garcia-Marsà, Jordi A.; Cerroni, Mauricio A.; Rozadilla, Sebastián; Cerda, Ignacio A.; Reguero, Marcelo A.; Coria, Rodolfo A.; Novas, Fernando E. (2020). "Biological implications of the bone microstructure of the Antarctic ornithopods Trinisaura and Morrosaurus (Dinosauria, Ornithischia)". Cretaceous Research. 116: 104605. Bibcode:2020CrRes.11604605G. doi:10.1016/j.cretres.2020.104605.
  4. 1 2 Herne, M.C.; Tait, A.M; Weisbecker, V.; Hall, M.; Nair, J.P; Cleeland, M.; Salisbury, S.W. (2018). "A new small-bodied ornithopod (Dinosauria, Ornithischia) from a deep, high-energy Early Cretaceous river of the Australian–Antarctic rift system". PeerJ. 5: e4113. doi: 10.7717/peerj.4113 . PMC   5767335 . PMID   29340228.
  5. ↑ Kitchener, Justin L.; Campione, Nicolás E.; Smith, Elizabeth T.; Bell, Phil R. (2019). "High-latitude neonate and perinate ornithopods from the mid-Cretaceous of southeastern Australia". Scientific Reports. 9 (1): 19600. Bibcode:2019NatSR...919600K. doi: 10.1038/s41598-019-56069-8 . PMC   6925213 . PMID   31862946.
  6. 1 2 Lamanna, Matthew C.; Case, Judd A.; Roberts, Eric M.; Victouria M., Arbour; Ely, Ricard C.; Salisbury Steven W.; Clarke, Julia A.; Malinzak, D. Edward; West, Abagael R.; O'Connor, Patrick M. (2019). "Late Cretaceous non-avian dinosaurs from the James Ross Basin, Antarctica: description of new material, updated synthesis, biostratigraphy, and paleobiogeography". Advances in Polar Science. 30 (3): 228–250. doi:10.13679/j.advps.2019.0007.
  7. ↑ Herne, Matthew C.; Nair, Jay P.; Evans, Alistair R.; Tait, Alan M. (2019). "New small-bodied ornithopods (Dinosauria, Neornithischia) from the Early Cretaceous Wonthaggi Formation (Strzelecki Group) of the Australian-Antarctic rift system, with revision of Qantassaurus intrepidus Rich and Vickers-Rich, 1999". Journal of Paleontology. 93 (3): 543–584. Bibcode:2019JPal...93..543H. doi: 10.1017/jpa.2018.95 .
  8. ↑ Poropat, Stephen F; Kundrát, Martin; Mannion, Philip D; Upchurch, Paul; Tischler, Travis R; Elliott, David A (20 January 2021). "Second specimen of the Late Cretaceous Australian sauropod dinosaur Diamantinasaurus matildae provides new anatomical information on the skull and neck of early titanosaurs". Zoological Journal of the Linnean Society. 192 (2): 610–674. doi: 10.1093/zoolinnean/zlaa173 . ISSN   0024-4082.
  9. ↑ Soto-Acuña, Sergio; Vargas, Alexander O.; Kaluza, Jonatan; Leppe, Marcelo A.; Botelho, Joao F.; Palma-Liberona, José; Simon-Gutstein, Carolina; Fernández, Roy A.; Ortiz, Héctor; Milla, Verónica; et al. (2021). "Bizarre tail weaponry in a transitional ankylosaur from subantarctic Chile" (PDF). Nature. 600 (7888): 259–263. Bibcode:2021Natur.600..259S. doi:10.1038/s41586-021-04147-1. PMID   34853468. S2CID   244799975.
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