4.7 Article

A new basal hadrosauroid dinosaur from the Late Cretaceous of Uzbekistan and the early radiation of duck-billed dinosaurs

Journal

PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES
Volume 276, Issue 1667, Pages 2549-2555

Publisher

ROYAL SOC
DOI: 10.1098/rspb.2009.0229

Keywords

Dinosauria; Hadrosauroidea; Cretaceous; Asia; radiation; palaeobiogeography

Funding

  1. National Science Foundation [EAR-9804771, 0207004]
  2. National Geographic Society [5901-97, 6281-98]
  3. US Civilian Research and Development Foundation [RUB1-2860-ST-07]
  4. Directorate For Geosciences
  5. Division Of Earth Sciences [0207004] Funding Source: National Science Foundation

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Levnesovia transoxiana gen. et sp. nov., from the Late Cretaceous (Middle-Late Turonian) of Uzbekistan, is the oldest well-documented taxon referable to Hadrosauroidea sensu Godefroit et al. It differs from a somewhat younger and closely related Bactrosaurus from Inner Mongolia (China) by a tall sagittal crest on the parietals and the absence of club-shaped dorsal neural spines in adult specimens. Levnesovia, Bactrosaurus and possibly Gilmoreosaurus represent the earliest radiation of Hadrosauroidea, which took place during the Cenomanian-Turonian and possibly in North America. The second, Santonian-age radiation of Hadrosauroidea included Aralosaurus, Hadrosauridae and lineages leading to Tanius (Campanian) and Telmatosaurus (Maastrichtian). Hadrosauridae appears to be monophyletic, but Hadrosaurinae and Lambeosaurinae originated in North America and Asia, respectively.

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