Phyllodon

 Phyllodon (meaning "leaf tooth") was a genusof small ornithischian dinosaur from the Kimmeridgian-age Upper Jurassic Camadas de Guimarota Formation of Leiria, Portugaland possibly also the Chipping Norton Limestone of England.[1] It may have been closely related to contemporaneous dinosaurs in North America.

Phyllodon
Temporal range: Kimmeridgian155 Ma 
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
Late Jurassic
Phyllodon.jpg
Tooth
Scientific classificationedit
Kingdom:Animalia
Phylum:Chordata
Clade:Dinosauria
Order:Ornithischia
Clade:Neornithischia
Genus:Phyllodon
Thulborn, 1973
Species:
P. henkeli
Binomial name
Phyllodon henkeli
Thulborn, 1973

This genus is known from teeth and possibly partial lower jaws. The name is also in usefor a genus of modern moss, but this is not considered to be a problem because the two organisms are in two different kingdoms.

HistoryEdit

Phyllodon is based on MGSP G5, a partial lower jaw tooth recovered from a lignite marlin a mine near the city of Leiria. Richard Thulborn, who described the genus, added an upper beak tooth (MGSP G2). He regarded the new genus as a hypsilophodontid, and presented a conjectural restoration of the tooth arrangement.[2] Peter Galton, reviewing Late Jurassic North American hypsilophodontids a few years later, found that the Phyllodon teeth best matched those of Nanosaurus, and agreed with a hypsilophodontid identity because the lower jaw tooth is asymmetric in front and back views.[3]

Because of the sparse material, Phyllodonhas often been tossed off as a dubious basalornithopod of uncertain affinities.[4][5]However, more material that might belong to this genus has been recovered from the original locality and described. Included in this material are over 120 more teeth from all parts of the jaw and four partial lower jaws with the teeth lost. Oliver Rauhut, who described the new material, tentatively identified the lower jaws as Phyllodon due to there being no other similar dinosaurs found at the locality. The teeth were very small (up to 3 millimeters across, or 0.1 inches) and possibly juvenile. He also found additional diagnostic characteristics for Phyllodon in the new material, including very tall upper jawteeth, indicating that it could be a valid genus after all. After comparing it to other hypsilophodonts, he found that it best matched the roughly contemporaneous Drinker of the North American Morrison Formation, with various details suggesting that they were closely related.[6] Similarly, Galton found its teeth to be similar to those of Drinker and Nanosaurus in his 2006 review.[7]

PaleobiologyEdit

As a hypsilophodontid or other basal ornithopod, Phyllodon would have been a bipedal herbivore. Its size has not been estimated, but as most adult hypsilophodonts were 1–2 meters (3.3–6.6 ft) long,[5] this genus would probably have been of similar size. Its similarity to the North American Drinker and Nanosaurus is another piece of evidence linking Late Jurassic Portuguese dinosaur faunas with the contemporaneous Morrison Formation dinosaurs.[8]


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 Metasyntactic variable, which is released under the 
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