Nodosauridae

 Nodosauridae is a family of ankylosauriandinosaurs, from the Late Jurassic to the Late Cretaceous period of what are now North America, Europe, Asia, Africa, and Antarctica.

Nodosaurids
Temporal range: Late Jurassic - Late Cretaceous155–66 Ma 
PreꞒ
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S
D
C
P
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J
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Pg
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Gargoy.jpg
Gargoyleosaurus skeleton cast
Scientific classificatione
Kingdom:Animalia
Phylum:Chordata
Clade:Dinosauria
Order:Ornithischia
Suborder:Ankylosauria
Family:Nodosauridae
Marsh, 1890
Subgroups
  • Acantholipan
  • Acanthopholis
  • Animantarx
  • Anoplosaurus
  • Antarctopelta
  • Borealopelta
  • Denversaurus
  • Dongyangopelta
  • Edmontonia
  • Europelta
  • Glyptodontopelta
  • Hungarosaurus
  • Hylaeosaurus
  • Invictarx
  • Mymoorapelta
  • Niobrarasaurus
  • Nodosaurus
  • Panoplosaurus
  • Pawpawsaurus
  • Peloroplites
  • Priconodon?
  • Propanoplosaurus
  • Rhadinosaurus
  • Sauroplites
  • Sauropelta
  • Silvisaurus
  • Stegopelta
  • Struthiosaurus
  • Polacanthinae
Synonyms

Acanthopholididae Nopcsa, 1902
Acanthopholidae Nopcsa, 1917
?Hylaeosauridae Nopcsa, 1902
Polacanthidae Wieland, 1911Palaeoscincidae Nopcsa, 1918
Panoplosauridae Nopcsa, 1929
Struthiosauridae Kuhn, 1966
Edmontoniidae Bakker, 1988

DescriptionEdit

The holotype of Borealopelta on display at the Royal Tyrrell Museum in Alberta.

Nodosaurids, like their close relatives the ankylosaurids, were heavily armored dinosaurs adorned with rows of bony armor nodules and spines (osteoderms), which were covered in keratin sheaths. All nodosaurids, like other ankylosaurians, were medium-sized to large, heavily built, quadrupedalherbivorous dinosaurs, possessing small, leaf-shaped teeth. Unlike ankylosaurids, nodosaurids lacked mace-like tail clubs, instead having flexible tail tips. Many nodosaurids had spikes projecting outward from their shoulders. One particularly well-preserved nodosaurid "mummy", known as the Suncor nodosaur (Borealopelta), preserved a nearly complete set of armor in life position, as well as the keratin covering and mineralized remains of the underlying skin, which indicate the animal had red and white camouflage.[1][2]

ClassificationEdit

The family Nodosauridae was erected by Othniel Charles Marsh in 1890, and anchored on the genus Nodosaurus.[3][4]

The clade Nodosauridae was first defined by Paul Sereno in 1998 as "all ankylosaurs closer to Panoplosaurus than to Ankylosaurus," a definition followed by Vickaryous, Teresa Maryańska, and Weishampel in 2004. Vickaryous et al. considered two genera of nodosaurids to be of uncertain placement (incertae sedis): Struthiosaurus and Animantarx, and considered the most primitive member of the Nodosauridae to be Cedarpelta.[5] The cladogram below follows the most resolved topology from a 2011 analysis by paleontologists Richard S. Thompson, Jolyon C. Parish, Susannah C. R. Maidment and Paul M. Barrett.[6] The placement of Polacanthinae follows its original definition by Kenneth Carpenter in 2001.[7]

Nodosauridae

Antarctopelta

Mymoorapelta

Hylaeosaurus

Anoplosaurus

Tatankacephalus

Horshamosaurus

Polacanthinae

Gargoyleosaurus

Hoplitosaurus

Gastonia

Peloroplites

Polacanthus

Struthiosaurus

Zhejiangosaurus

Hungarosaurus

Animantarx

Niobrarasaurus

Nodosaurus

Pawpawsaurus

Sauropelta

Silvisaurus

Stegopelta

Texasetes

Edmontonia

Panoplosaurus


TimelineEdit

21st century in paleontology20th century in paleontology19th century in paleontology2090s in paleontology2080s in paleontology2070s in paleontology2060s in paleontology2050s in paleontology2040s in paleontology2030s in paleontology2020s in paleontology2010s in paleontology2000s in paleontology1990s in paleontology1980s in paleontology1970s in paleontology1960s in paleontology1950s in paleontology1940s in paleontology1930s in paleontology1920s in paleontology1910s in paleontology1900s in paleontology1890s in paleontology1880s in paleontology1870s in paleontology1860s in paleontology1850s in paleontology1840s in paleontology1830s in paleontology1820s in paleontologyPolacanthusPeloroplitesHoplitosaurusGastoniaGargoyleosaurusZhejiangosaurusTexasetesTatankacephalusStruthiosaurusStegopeltaSilvisaurusSauropeltaPropanoplosaurusPawpawsaurusPanoplosaurusNodosaurusNiobrarasaurusMymoorapeltaInvictarxHylaeosaurusHungarosaurusGlyptodontopeltaEdmontoniaDenversaurusBorealopeltaAntarctopeltaAnoplosaurusAnimantarxAcantholipan21st century in paleontology20th century in paleontology19th century in paleontology2090s in paleontology2080s in paleontology2070s in paleontology2060s in paleontology2050s in paleontology2040s in paleontology2030s in paleontology2020s in paleontology2010s in paleontology2000s in paleontology1990s in paleontology1980s in paleontology1970s in paleontology1960s in paleontology1950s in paleontology1940s in paleontology1930s in paleontology1920s in paleontology1910s in paleontology1900s in paleontology1890s in paleontology1880s in paleontology1870s in paleontology1860s in paleontology1850s in paleontology1840s in paleontology1830s in paleontology1820s in paleontology


BiogeographyEdit

The near simultaneous appearance of nodosaurids in both North America and Europe is worthy of consideration. Europeltais the oldest nodosaurid from Europe, it is derived from the lower Albian Escucha Formation. The oldest western North American nodosaurid is Sauropelta, from the lower Albian Little Sheep Mudstone Member of the Cloverly Formation, at an age of 108.5±0.2 million years. Eastern North American fossils seem older. Teeth of Priconodon crassus from the Arundel Clay of the Potomac Group of Maryland, which dates near the Aptian–Albian boundary. The Propanoplosaurus hatchling from the base of the underlying Patuxent Formation, dating to the upper Aptian, is the oldest known nodosaurid.[3]

Polacanthids are known from pre-Aptian fauna from both Europe and North America. The timing of the appearance of nodosaurids on both continents indicates that the origins of the clade preceded the isolation of North America and Europe, pushing the group's date of evolution back to at least the "middle" Aptian. The separation of Nodosauridae into European Struthiosaurinae and North American Nodosaurinae by the end of the Aptian provides a revised date for the isolation of the continents from each other by rising sealevels.[3]

Below is a table showing the age difference between continents. North American nodosaurids are teal, European nodosaurids are green, European polacanthids are blue, and North American polacanthids are brown. Other nodosaurids or polacanthids are black. This table supports the observations by Kirkland et al. (2013).[3]

CretaceousJurassicLate CretaceousEarly CretaceousLate JurassicMiddle JurassicEarly JurassicDenversaurusGlyptodontopeltaAntarctopeltaPanoplosaurusEdmontoniaStruthiosaurusHungarosaurusNiobrarasaurusSilvisaurusTexasetesPawpawsaurusZhejiangosaurusDongyangopeltaAnoplosaurusStegopeltaNodosaurusPeloroplitesAnimantarxTatankacephalusSauropeltaEuropeltaBorealopeltaPriconodonPropanoplosaurusGastoniaPolacanthusHoplitosaurusHylaeosaurusGargoyleosaurusMymoorapeltaCretaceousJurassicLate CretaceousEarly CretaceousLate JurassicMiddle JurassicEarly Jurassic
  • James Kirkland et al. (2013) consider MymoorapeltaGargoyleosaurusHylaeosaurusPolacanthusHoplitosaurusand Gastonia to be polacanthids, outside of Nodosauridae.[3]

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 Metasyntactic variable, which is released under the 
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