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68 results for “ornithopod dinosaurs”
Figure 22 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 22. Left pes of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in dorsal (A), plantar (B), and proximal (C) views. Dashed lines indicate the extrapolated margins of the pes. See list in text for an explanation of anatomical abbreviations. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction. Roman numerals denote digit number.
Figure 21 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 21. Left tibia, fibula, astragalus calcaneum, and distal lateral tarsal of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in anterior (A), posterior (B), medial (C), lateral (D), proximal (E), and distal (F) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 19 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 19. Right pubis of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in dorsal (A), ventral (B), medial (C), and lateral (D) views. Dashed lines indicate the extrapolated margins of the element. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 16. A in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 16. A left rib of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in anterior (A), posterior (B), medial (C), and lateral (D) views, and showing flattened and rugose posterior margin (E). Lateral view shows cross-sectional shape along the shaft, with the lateral surface facing upwards. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. White areas represent plaster reconstruction.
Figure 20 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 20. Left femur of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in anterior (A), posterior (B), medial (C), lateral (D), proximal (E), and distal (D) views. Dashed lines indicate the extrapolated margins of the element. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 18 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 18. Left ilium of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in lateral (A), medial (B), dorsal (C), and ventral (D) views. Dashed lines indicate extrapolated margins of the element. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 17 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 17. Distal portions of ribs of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in posterior (A) and anterior (B) views, illustrating rugose texture of posterior margin.
Figure 14 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 14. Sixth dorsal vertebra of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in right lateral (A), left lateral (B), posterior (C), anterior (D), dorsal (E), and ventral (F) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 15 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 15. Fused sacral vertebrae of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in left lateral (A) and dorsal (B) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 13 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 13. Dorsal vertebral series of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in dorsal (A) and left lateral (B) views. Anterior vertebrae show the dissociation of neural arches and centra. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 11 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 11. Braincase of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in anterior (A), posterior (B), internal ventral (C), internal dorsal (D), ventral (E), dorsal (F), and left lateral (G) views. See list in text for an explanation of anatomical abbreviations. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction. Roman numerals denote cranial nerve foramina.
Figure 7 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 7. Left jugal of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in right (A) and left (B) lateral views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element.
Figure 12 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 12. Left quadrate of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in medial (A), anterior (B), posterior (C), and lateral (D) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface.
Figure 10 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 10. Right dentary of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in medial (A), dorsal (B), lateral (C), and ventral (D) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface.
Figure 2 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 2. Chronostratigraphy of the Late Cretaceous of Alberta, Saskatchewan, and Montana, Wyoming, and North and South Dakota, showing approximate time equivalence. Numbers on the left are in millions of years before present. Formations in white are terrestrial, and those in grey are marine; DMT, Drumheller Marine Tongue. Complied from Eberth, 2004; Brinkman DB. 2003; Koppelhus EB, Braman DR. 2010; Hamblin and Abrahamson, 1996; McIver 2002.
Figure 6 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 6. Left squamosal of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in dorsal (A), ventral (B), medial (C), and lateral (D) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 5 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 5. Left palpebral of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in ventral (A), dorsal (B), lateral (C), and medial (D) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element.
Figure 4 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 4. The skull roof of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in dorsal (A) and ventral (B) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface. White area represents plaster reconstruction.
Figure 1 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 1. Diagrams of the skeletons of relatively complete articulated Thescelosaurus specimens (A–I) and Parksosaurus (J), showing their comparative size and degree of completeness. Bones present in each specimen are represented in white. A, LACM 33542; B, SDSM 7210; C, MOR 979; D, NCSM 15728; E, USNM 7757; F, USNM 7758; G, CMN 8537; H, LACM 33543; I, RSM P 1225.1; J, ROM 804. Skeletons are scaled isometrically based on femur and tibia length, when available. Skeletons lacking both tibiae and femora were scaled using the following elements: anteroposterior thickness of orbit for SDSM 7210; length of the dentary for LACM 33543; and length of the humerus for USNM 7758. Proportions for specimens of Thescelosaurus represent those of USNM 7757, and do not illustrate proportional changes that would be evident because of allometric scaling. Scale equals 1 m. Modified from Boyd et al. 2009.
Figure 8 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 8. Right pterygoid of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in medial (A), lateral (B), dorsal (C), and ventral (D) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface.
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International Brain Laboratory public data
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