Find research datasets worth reusing

FIG. 10 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 10. Looking south from the base of the Zos Canyon section. The arrow indicates the Red Rum sublocality.

FIG. 9. B in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 9. B. Shared diagnostic character (6) a shallow depression along the midline nasal suture anterior to the orbits on the dorsal surface of the skull.

FIG. 9. A in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 9. A. Comparison of IGM 100/3181 (top) with the holotype of Haya griva (IGM 100/2017, bottom). Shared diagnostic characters (Makovicky et al., 2011) are: (1) homodont unserrated premaxillary teeth, (2) the lack of a rugose rhamphothecal pad on the anterior surface of the premaxilla, (3) the presence of a triangular maxillary fenestra, (4) a jugal with a bifurcated (forklike) posterior ramus where it abuts the quadratojugal, (5) the presence of a quadratojugal foramen.

FIG. 4. A in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 4. A. Premaxillary tooth of IGM 100/3181 in mesial and distal views. Its precise orientation cannot be determined as it was found as float during preparation. B. Cheek tooth of IGM 100/3181. Its precise orientation cannot be determined as it was found as float during preparation, and is compatible with the morphology of both upper and lower teeth of referred Haya specimens.

FIG. 3 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 3. The left side of the cranium of IGM 100/3181, with interpretive drawing. Abbreviations are listed in appendix 1.

FIG. 1 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 1. Map of Mongolia showing the relative positions of the Javkhlant Formation exposures and Zos Canyon beds (near Ukhaa Tolgod). Zos Canyon is 7 km northwest of the Ukhaa Tolgod locality. See Pol and Norell (2004a: fig. 1) for detail.

Fig. 13 in A New Crocodyliform from Zos Canyon, Mongolia

Fig. 13. Lower jaws of the holotype of Zosuchus davidsoni IGM 100/1305 in dorsal (A) and ventral (B) views.

FIG. 6. A. IGM 100 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 6. A. IGM 100/3181.Two carpals in unknown orientation. B. Metacarpal I and manual phalanx I-1 in dorsal view. C. Metacarpal II or III and manual phalanx in dorsal view. D. Manual phalanx in dorsal view. E. Three ungual phalanges in partial dorsal view.

FIG. 12 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 12. Looking south toward Red Rum (arrow) at the intermediate white beds of Zos Canyon.

FIG. 13 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 13. The Red Rum sublocality, looking west-southwest.

FIG. 14 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 14. Looking northwest from the Red Rum sublocality toward the discovery site (arrow).

FIG. 11 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 11. Looking south at the basalmost fluvial red sands at Zos Canyon.

FIG. 7 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 7. Ventral view of the preserved dorsal vertebrae of IGM 100/3181. Anterior is to the right.

FIG. 5 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 5. The radius (top) and ulna (bottom) of IGM 100/3181.

FIG. 2. IGM 100 in A new specimen of the ornithischian dinosaur Haya griva, cross-Gobi geologic correlation, and the age of the Zos Canyon beds

FIG. 2. IGM 100/3181, a partial skeleton of Haya griva.

Fig. 15 in A New Crocodyliform from Zos Canyon, Mongolia

Fig. 15. Strict consensus of the six most parsimonious hypotheses obtained with Nona.

Fig. 12 in A New Crocodyliform from Zos Canyon, Mongolia

Fig. 12. Posterior region of skull of specimen IGM 100/1306 in ventral view.

Fig. 16. Artzosuchus brachycephalus GIN PST 10 in A New Crocodyliform from Zos Canyon, Mongolia

Fig. 16. Artzosuchus brachycephalus GIN PST 10/23, taken from Efimov (1983).

Fig. 6 in A New Crocodyliform from Zos Canyon, Mongolia

Fig. 6. Skull of specimen IGM 100/1304 in dorsal (A) and ventral (B) views.

Fig. 11 in A New Crocodyliform from Zos Canyon, Mongolia

Fig. 11. Palatal region specimen of IGM 100/1306 in posterodorsal view.