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Fig. 6. The herrerasaurian dinosauriform Herrerasaurus ischigualastensis Reig, 1963 in A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution

Fig. 6. The herrerasaurian dinosauriform Herrerasaurus ischigualastensis Reig, 1963 (PVL 2566) from Carnian, Late Triassic, Ischigualasto Formation, Hoyada de Ischigualasto, San Juan Province, Argentina; ilium in lateral view.

Fig. 3 in A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution

Fig. 3. The herrerasaurian dinosauriform Caseosaurus crosbyensis Hunt, Lucas, Heckert, Sullivan, and Lockley, 1998 (NMMNH P-35995) from Synder Quarry, Rio Arriba County, New Mexico, USA; Carnian, Late Triassic; right ilium in lateral (A) and medial (B) views.

Fig. 5 in A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution

Fig. 5. Reduced strict consensus tree produced when Caseosaurus crosbyensis (in bold) was added to the dataset of Cabreira et al. (2016).

Fig. 2 in A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution

Fig. 2. The holotype of the herrerasaurian dinosauriform Caseosaurus crosbyensis Hunt, Lucas, Heckert, Sullivan, and Lockley, 1998 (UMMP 8870) from Tecovas Formation, Crosby County, Texas, USA; Carnian, Late Triassic; right ilium in lateral view; stereopair. Image credit: Adam Rountrey, Museum of Paleontology, University of Michigan, Ann Arbor, USA.

Fig. 14 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 14. Strict consensus of 34 trees. Length = 2219, CI = 0.2881, RI – 0.7500. 100 taxa are included. Goniopholididae are monophyletic, with Calsoyasuchus the most basal form. Goniopholis forms a paraphyletic group with respect to Anteophthalmosuchus. Sunosuchus is polyphyletic, spread among several groups including Eutretauranosuchus, Kansajsuchus, and the European goniopholidids. All European goniopholidids form a monophyletic group to the exclusion of the Asian and North American forms. Tomistoma and Gavialis cluster together to the exclusion of Alligator.

Fig. 7. Crocodylomorph Kansajsuchus extensus Efimov, 1975 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 7. Crocodylomorph Kansajsuchus extensus Efimov, 1975 frontoparietal region from the Santonian (Upper Cretaceous) of Fergana, Tajikistan, PIN 2399-308, in posterior (A), ventral (B), anterior (C), dorsal (D), and lateral (E) views, clearly demonstrating the trapezoidal shape of the skull roof, and the near-circular fenestrae.

Fig. 6. Crocodylomorph Kansajsuchus extensus Efimov, 1975 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 6. Crocodylomorph Kansajsuchus extensus Efimov, 1975 specimens from the Santonian (Upper Cretaceous) of Fergana, Tajikistan. A. Portion of frontal bone and posterior end of nasal, PIN 2399-310. B. Broken portion of a left maxilla, PIN 2399-307. C. Anterior section of right nasal bone, PIN 2399-306. D. Example of dorsal dermal osteoderm, PIN 2399-312. In ventral (A –D ) and dorsal (A –D ) views.

Fig. 1 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 1. Adult crocodylomorph "Sunosuchus" thailandicus Buffetaut and Ingavat, 1980, PIN 4174-1, from the Tithonian (Upper Jurassic) of Shar Teeg, Mongolia. A. Rostrum, quadrates, and occipital condyle in dorsal aspect. B, C. Rostrum and mandible in left (B) and right (C) views. Photographs (A 1 –C 1) and explanatory drawings (A –C ).

Fig. 13 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 13. Strict consensus of 324 trees. Length = 2305, CI = 0.2872, RI = 0.7497. 102 crocodilomorph taxa are included. The inclusion of "Sunosuchus" thailandicus and material formerly ascribed to Turanosuchus aralensis results in a large polytomy including Eusuchia, Goniopholididae, Pholidosauridae, and Metriorhynchidae. Relationships within Goniopholididae for the most part collapse. A notable exception is the association of Eutretauranosuchus and "Sunosuchus" junggarensis, which suggests that this is a very strongly supported relationship.

Fig. 2 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 2. Crocodylomorph "Sunosuchus" thailandicus Buffetaut and Ingavat, 1980 dentition, PIN 4174-1, from the Tithonian (Upper Jurassic) of Shar Teeg, Mongolia. A. Rostrum in palatal aspect. Photograph (A1) and explanatory drawing (A2). B. Anterior mandible in dorsal view, from symphysis to the anterior edge of the external mandibular fenestra.

Fig. 11 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 11. Poorly preserved mandibular symphysis of?Goniopholididae gen. et sp. indet. (previously Turanosuchus aralensis Efimov, 1988) from the Upper Cretaceous of Kazakhstan, PIN 2229-507, in dorsal view, with majority of tooth alveoli present but damaged. For full explanation see text.

Fig. 5. Crocodylomorph Kansajsuchus extensus Efimov, 1975 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 5. Crocodylomorph Kansajsuchus extensus Efimov, 1975, holotype, PIN 2399-301 from the Santonian (Upper Cretaceous) of Fergana, Tajikistan. Right premaxilla of an adult crocodilian in dorsal (A), lateral (B), and ventral (C) views. Photographs (A1–C1) and explanatory drawings (A2–C2).

Fig. 12 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 12.?Goniopholididae gen. et sp. indet. (previously Turanosuchus aralensis Efimov, 1988) from the Santonian (Upper Cretaceous) of the Zhirkindek Formation, Kazakhstan, material formerly attributed to Turanosuchus aralensis Efimov, 1988. A. Section of left dentary, PIN 2229-506, including two complete and two incomplete alveoli in dorsal (A1) and lateral (A2) views. B. Dermal osteoderm, PIN 2229-503, in dorsal (B1) and ventral (B2) views. C. Fragmented right maxilla, PIN 2229-502 (demonstrating the sinusoidal condition also seen in PIN 4174-1), in ventral (C1) and dorsal (C2) views. D. Posterior portion of left mandible, PIN 2229-501, in dorsal (D1), lateral (D2), and medial (D3) views.

Fig. 9. Crocodylomorph Kansajsuchus extensus Efimov, 1975 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 9. Crocodylomorph Kansajsuchus extensus Efimov, 1975 left angular region of the mandible. Specimens from the Santonian (Upper Cretaceous) of Fergana, Tajikistan, PIN 2399-453, in ventral (A), dorsal (B), medial (C), and lateral (D) views.

Fig. 8. Crocodylomorph Kansajsuchus extensus Efimov, 1975 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 8. Crocodylomorph Kansajsuchus extensus Efimov, 1975 basioccipital region and quadrate, preserving several nerve and vascular foramina. Specimens from the Santonian (Upper Cretaceous) of Fergana, Tajikistan. A. PIN 2399-308 (second part) in posterior (A1), ventral (A2), and dorsal (A3) views. B. PIN 2399-468, a quadrate in posterior (B1), dorsal (B2), and ventral (B3) views.

Fig. 3 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 3. Crocodylomorph "Sunosuchus" thailandicus Buffetaut and Ingavat, 1980, PIN 4174-1, from the Tithonian (Upper Jurassic) of Shar Teeg, Mongolia. Occipital condyle in lateral (A) and posterior (B) views.

Fig. 4 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 4. Teeth of crocodylomorphs from the Cretaceous of Central Asia. A. "Sunosuchus" thailandicus Buffetaut and Ingavat, 1980, left mandibular tooth of PIN 4174-1. Tooth is from mid-mandible and is similar in size to all of the other mandibular teeth, which show little size variation. B, C. Kansajsuchus extensus Efimov, 1975. B. Caniniform tooth of PIN 2399-313 in anterior (B1), posterior (B2), and lateral (B3) views. The tooth is characterized by prominent ridges, including a distinctive "double keel" on the posterior side of the tooth. The tooth is from the anterior part of the jaw. C. Molariform tooth of PIN 2399-314 in posterior (C1), anterior (C2), and lateral (C3) views. The tooth shares the ridges characteristic of Kansajsuchus, including a less prominent version of the double keel, but is blunter, and derived from the posterior part of the jaw.

Fig. 10. Crocodylomorph Kansajsuchus extensus Efimov, 1975 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications

Fig. 10. Crocodylomorph Kansajsuchus extensus Efimov, 1975 postcranial material from the Santonian (Upper Cretaceous) of Fergana, Tajikistan. A. Cervical vertebra, PIN 2399-304, in anterior (A 1) and lateral (A 2) views. B. Left femur, PIN 2399-318, in posterior (B ) and lateral (B ) views.

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Fig. 1 in Late Palaeozoic foliage from China displays affinities to Cycadales rather than to Bennettitales necessitating a re-evaluation of the Palaeozoic Pterophyllum species

Fig. 1. Map of NE China and Korea showing the localities from which Pseudoctenis samchokense fossils have been collected (grey symbols) and the locality from which Primocycas chinensis fossils have been described (black symbol).