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Fig. 2 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 2. Map of Thailand (A) and close-up of northeastern Thailand (B) showing the location of Phu Wiang locality, Khon Kaen Province (square) and Phu Wat locality, Nong Bua Lamphu Province (star). Dark gray, Sao Khua Formation outcrops, light gey, Phu Kradung and Khok Kruat formations.

Fig. 10 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 10. Phuwiangvenator yaemniyomi gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. SMPW9A-B17, right (A) and SM-PW9B-18, left (B); astragalocalcaneum in anterior (A2, B2), medial (A3, B3), distal (A4, B4), and lateral (A5, B5) views; line drawings in anterior view (A1, B1). Dashed lines are the reconstruction of the ascending processes of the astragali.

Fig. 4 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 4. Coelurosaurian theropod Phuwiangvenator yaemniyomi gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. SM-PW9B-39, anterior sacral vertebrae in right lateral (A1) and ventral (A2) views; line drawing in ventral view (A3). Arrows indicate ventral sulci, light grey, broken part; dark grey, matrix.

Fig. 9 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 9. Coelurosaurian theropod Phuwiangvenator yaemniyomi gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. A. SM-PW9B-41, right tibia in proximal view. B. SM-PW9B-40, left tibia in distal view. Light grey indicates broken bone.

Fig. 16 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 16. Coelurosaurian theropod Vayuraptor nongbualamphuensis gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wat, Nong Bua Lamphu Province, Thailand. SM-NB A1-2, left tibia with associated astragalocalcaneum in anterior (A1), lateral (A2), posterior (A3), medial (A4), proximal (A5), and distal (A6) view. Arrow indicates vertical ridge on the tibia.

Fig. 15 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 15. Coelurosaurian theropod Vayuraptor nongbualamphuensis gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wat, Nong Bua Lamphu Province, Thailand. PRC-NB A1-11, right coracoid in lateral (A1) and medial (A2) views. Dashed lines are the reconstruction of the posteroventral process of the coracoid.

Fig. 12 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 12. Coelurosaurian theropod Phuwiangvenator yaemniyomi gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. SM-PW9B-44 (A), SM-PW9B-43 (B), SM-PW9B-42 (C); metatarsals in anterior (A1–C1) and proximal (A2–C2) views; line drawings in anterior (A3–C3) and proximal (A4–C4) views; metatarsal III in medial (B5) and distal (B6) views.

Fig. 2 in A Late Triassic dinosaur-dominated ichnofauna from the Tomanová Formation of the Tatra Mountains, Central Europe

Fig. 2. Tridactyl tracks (pes prints) of possibly early ornithischian dinosaurs from the Czerwone Żlebki site, Tomanová Formation (?late Norian–Rhaetian), Poland. A, B. cf. Moyenisauropus isp. C, D. cf. Anomoepus isp. A–C. Specimens left in field. D. Specimen deposited at Tatra Mountains National Park, Zakopane, Poland. Photographs (A1–D1) and drawings (A2–D2). Scale bars 5 cm.

Fig. 7 in A Late Triassic dinosaur-dominated ichnofauna from the Tomanová Formation of the Tatra Mountains, Central Europe

Fig. 7. Dinosaur ichnofauna of the Late Triassic of the Tatra Mountains, Poland and Slovakia. A. cf. Anomoepus isp. and cf. Moyenisauropus isp. Trackmakers: possibly early ornithischian dinosaurs. B. cf. Grallator isp. and Anchisauripus isp. Trackmakers: theropod dinosaurs. C. cf. Kayentapus isp. and cf. Eubrontes isp. Trackmakers: theropod dinosaurs. D.?Sauropodomorpha tracks indet. Trackmakers: "prosauropod" or sauropod dinosaurs. Abbreviation: TL, track length.

Fig. 6 in A Late Triassic dinosaur-dominated ichnofauna from the Tomanová Formation of the Tatra Mountains, Central Europe

Fig. 6.?Sauropodomorph tracks indet. A. Specimen from the Czerwone Żlebki found in 2004, Tomanová Formation (?late Norian– Rhaetian), Poland. B. Specimen from the Červený Ŭplaz found in 2007, Tomanová Formation (?late Norian–Rhaetian), Slovakia. Both specimens left in field. Photographs (A1, B1) and drawings (A2,B2). Scale bars 5 cm.

Fig. 1. A in A Late Triassic dinosaur-dominated ichnofauna from the Tomanová Formation of the Tatra Mountains, Central Europe

Fig. 1. A. The location of this area in Poland. B. Satellite map of the Western Tatra Mountains showing positions of sites at which dinosaur tracks have been recorded. C. Czerwone Żlebki tracksite, Poland. D. Červený Ŭplaz tracksite, Slovakia.

Fig. 4 in A Late Triassic dinosaur-dominated ichnofauna from the Tomanová Formation of the Tatra Mountains, Central Europe

Fig. 4. Tridactyl tracks (pes prints) of small to large theropod dinosaurs. cf. Kayentapus isp. A, B. Specimens from Červený Üplaz site, Tomanová Formation (?late Norian–Rhaetian), Slovakia. C, D. Specimens from Czerwone Żlebki site, Tomanová Formation (?late Norian–Rhaetian), Poland. A. Specimen Z 14 296 housed at Slovak National Museum, Bratislava, Slovakia. B, D. Specimens left in field. C. Specimen deposited at Tatra Mountains National Park, Zakopane, Poland. Photographs (A1–D1) and drawings (A2–D2). Scale bars 5 cm.

Fig. 5 in A Late Triassic dinosaur-dominated ichnofauna from the Tomanová Formation of the Tatra Mountains, Central Europe

Fig. 5. Tridactyl track (pes print) cf. Eubrontes isp. from Červený Ŭplaz site, Tomanová Formation (?late Norian–Rhaetian), Slovakia. Specimen left in field. Photograph (A) and drawing (B). Scale bars 5 cm.

Fig. 3 in A Late Triassic dinosaur-dominated ichnofauna from the Tomanová Formation of the Tatra Mountains, Central Europe

Fig. 3. Tridactyl tracks (pes prints) of small to medium sized theropod dinosaurs. A. cf. Grallator isp. B–E Anchisauripus isp. A, E. Specimens from Czerwone Żlebki site, Tomanová Formation (?late Norian–Rhaetian), Poland. B–D. Specimens from Červený Ŭplaz site, Tomanová Formation (?late Norian–Rhaetian), Slovakia. A, C, E. Specimens left in field. B. Specimen Z 14 297 housed at Slovak National Museum, Bratislava, Slovakia. D. Specimen deposited at Tatra Mountains National Park, Zakopane, Poland. Photographs (A1–E1) and drawings (A2–E2). Scale bars 5 cm.

Fig. 2 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 2. Reconstruction of the skull of Spinops sternbergorum gen. et sp. nov. from the Campanian of Dinosaur Provincial Park, southern Alberta, in right lateral view. Preserved elements are stippled; missing portions are dotted and modeled after Centrosaurus apertus.

Fig. 6 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 6. Phylogenetic hypotheses for relationships within Ceratopsidae, focusing on Centrosaurinae. A. Strict reduced consensus tree using "traditional" codings for the epiparietal homologies in selected centrosaurines (see text), with Sinoceratops zhuchengensis and Rubeosaurus ovatus removed. B. Strict consensus tree using "new" codings for epiparietal homologies, following a posteriori deletion of Sinoceratops zhuchengensis and Centrosaurus brinkmani. At selected nodes, the top number indicates Bremer support and the bottom number indicates bootstrap support values above 50%.

Fig. 6. Ankylosaurid dinosaur Pinacosaurus grangeri Gilmore, 1933 in Hands, feet, and behaviour in Pinacosaurus (Dinosauria: Ankylosauridae)

Fig. 6. Ankylosaurid dinosaur Pinacosaurus grangeri Gilmore, 1933 (MPC 100/1310) from the Alagteeg Formation (Upper Cretaceous) of Alag Teeg, Mongolia. Outline of left metacarpus and proximal phalanges in proximal (A) and anterior (B) views.

Fig. 5 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 5. Schematized parietals of centrosaurine ceratopsids in dorsal view, showing possible homologies for the first four epiparietal loci. A. Albertaceratops nesmoi Ryan, 2007. B. Spinops sternbergorum gen. et sp. nov. C. Centrosaurus apertus Lambe, 1902. D. Styracosaurus albertensis Lambe, 1913. E. Rubeosaurus ovatus Gilmore, 1930. F. Einiosaurus procurvicornus Sampson, 1995. Numbers indicate locus positions. For A and B, the numbers on the right side of the parietal indicate numbering under the "traditional" scheme; numbers on the left side indicate numbering under the revised scheme proposed here. Locus numbering is the same in both the traditional and revised schemes for C, D, E, and F, and are thus presented only on the left side of the parietal for those taxa. Not to scale.

Fig. 4 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 4. Partial skull of the centrosaurine ceratopsid Spinops sternbergorum gen. et sp. nov. from the Campanian of Dinosaur Provincial Park, southern Alberta, NHMUK R16306; in right lateral (A), rostral (B), and dorsal (C) views.

Fig. 3 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 3. Centrosaurine ceratopsid Spinops sternbergorum gen. et sp. nov. from the Campanian of Dinosaur Provincial Park, southern Alberta. A. Partial right squamosal in lateral view, NHMUK R16309. B. Partial parietal with adherent bone fragments in dorsal view, NHMUK R16308. C. Partial parietal in dorsal (C1), rostral (C2), and left lateral (C3) views, holotype NHMUK R16307.