Find research datasets worth reusing

Fig. 8 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 8. 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 anterior (A1), lateral (A2), posterior (A3), medial (A4), proximal (A5), and distal (A6) views. B. SM-PW9B-40, proximal left tibia in lateral view. Arrow indicates vertical ridge on the tibia.

Fig. 3 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 3. Coelurosaurian theropod Phuwiangvenator yaemniyomi gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. A. SM-PW9A-1, atlantal intercentrum in anterior (A1) and posterior (A2) views. B. SM-PW9B-12, dorsal vertebra in left lateral (B1), anterior (B2), ventral (B3), and posterior (B4) views.

Fig. 1 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 1. Three hypotheses of the phylogenetic position of Megaraptora. Megaraptora as derived Carcharodontosauria (Benson et al. 2010; Carrano et al. 2012); basal Coelurosauria (Novas et al. 2015; Apestiguea et al. 2016; Delcourt and Grillo 2018); and basal Tyrannosauroidea (Novas et al. 2012a, 2013; Porfiri et al. 2014; Cau 2018). The tree is modified from Ezcurra and Novas (2016). Bolded are theropods found in Thailand.

Fig. 7 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 7. 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-3, manual phalanx I-1 in ventral (A1) and proximal (A3) views; line drawing in ventral view (A2). B. SM-PW9B-19, manual ungual I-2 in medial (B1), distal (B2), lateral (B3), proximal (B4), dorsal (B5), and ventral (B6) views. Arrow indicates the longitudinal ventral furrow.

Fig. 17 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 17. 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 astragalocalcaneum in anterior (A2), medial (A3), lateral (A4), and distal (A5) views; line drawing in anterior view (A1).

Fig. 14 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 14. Coelurosaurian theropod Phuwiangvenator yaemniyomi gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. SM-PW9B-10, right pedal ungual IV-5 in lateral (A1) and ventral (A2) views.

Fig. 13 in Two new basal coelurosaurian theropod dinosaurs from the Lower Cretaceous Sao Khua Formation of Thailand

Fig. 13. Coelurosaurian theropod Phuwiangvenator yaemniyomi gen. et sp. nov. from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. SM-PW9B-11 (A), SM-PW9B-7 (B), SM-PW9B-8 (C), SM-PW9B-22 (D), SM-PW9B-5 (E), SM-PW9B-9 (F), SM-PW9B-19 (G), SM-PW9B-6 (H), SM-PW9B-45 (I), SM-PW9B-10 (J); right pedal phalanges (B, C, E, F, H, I) and unguals (A, D, G, J), in ventral (A1–J1) and dorsal (A2–J2) views; line drawings in dorsal view (A3–J3). Dashed lines are the reconstruction of pedal phalanges III-1, IV-2, and IV-3 and pedal unguals II-3 and III-4.

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. 4 in Unusual theropod eggshells from the Early Cretaceous Blesa Formation of the Iberian Range, Spain

Fig. 4. Variations in outer surface ornamentation of prismatoolithid therapod eggshell Trigonoolithus amoae oogen. et oosp. nov. from La Cantalera 1 site, Early Barremian. Eggshells showing triangular (A–C) and rounded ornamentation (D–F). Pristine eggshells showing well-preserved ornamentation (A, D). Lightly eroded eggshells showing degradation (B, E). Eroded eggshells showing coalescence of triangles (C, F). A. MPZ 2012/740. B. MPZ 2012/742. C. MPZ 2012/743. D. MPZ 2012/731. E. MPZ 2012/729. F. MPZ 2012/728. Scale bar 1000 μm.

Fig. 5 in Unusual theropod eggshells from the Early Cretaceous Blesa Formation of the Iberian Range, Spain

Fig. 5. Strict consensus trees showing the hypothesized phylogenetic position of Trigonoolithus amoe oogen. et oosp. nov. from La Cantalera 1 site, Early Barremian. A. Matrix of Varricchio and Jackson (2004). Strict consensus of six equally parsimonious trees of 38 steps was recovered (C.I. 0.737; R.I. 0.853; R.C. 0.629). B. Matrix of Grellet-Tinner and Makovicky (2006). Strict consensus tree of three equally most parsimonious trees of 36 steps (C.I. 0.750; R.I. 0.852; R.C. 0.639). C. Matrix of Zelenitsky and Therrien (2008b). Most parsimonious tree of 18 steps (C.I. 1.000; R.I. 1.000; R.C.1.000). D. LópezMartínez and Vicens (2012) version of the dataset: a new analysis of Prismatoolithidae using the matrix of Zelenitsky and Therrien (2008) and adding the new oogenus Sankofa and the Patagonian eggs of Bajo de la Carpa (Schweitzer et al. 2002). Strict consensus of seven equally parsimonious trees of 19 steps (C.I. 0.947; R.I. 0.958; R.C. 0.907). All trees show Trigonoolithus placed in polytomy or at the base of the "Prismatoolithidae+avian eggs" clade.

Fig. 1 in Unusual theropod eggshells from the Early Cretaceous Blesa Formation of the Iberian Range, Spain

Fig. 1. Geographical and geological location of the site of La Cantalera 1 (early Barremian, Teruel, Spain), modified from Canudo et al. (2010). A. Simplified geological map of the Iberian Peninsula. B. Palaeogeographic subbasins (Ol, Oliete; Pa, Las Parras; Ga, Galve; Mo, Morella; Pe, Perelló; Sa, Salzedella; Pg, Peñagolosa) within the Maestrazgo Basin and active faults during Early Cretaceous sedimentation, modified from Salas et al. (2001). C. Detailed location of the La Cantalera site near the village of Josa, Teruel. D. Geological map of the La Cantalera area with the local geological units.

Fig. 3 in Unusual theropod eggshells from the Early Cretaceous Blesa Formation of the Iberian Range, Spain

Fig. 3. Thin-sections of prismatoolithid therapod eggshell Trigonoolithus amoae oogen. et oosp. nov. from La Cantalera 1 site, Early Barremian. A. MPZ 2012/856, light microphotograph. B. MPZ 2012/862, light microphotograph (B 1), microphotograph showing eggshell under cross-polars (B 2). C. MPZ2012/850, cathodoluminescence image showing dark blue luminescence except for some orange tones in the mammillary layer, probably due to the high amount of organic matter in this area. Scale bars 500 μm.

Fig. 4 in The first non-avian theropod from the Czech Republic

Fig. 4. Non-avian theropod tooth, IGS-MJ-0001 (Orionides indet.) from Upper Jurassic (Oxfordian), Švédské šance (Brno-Slatina), Czech Republic. A. Tooth in labial view. B. Detail of the serrations on the mesial carina; with the cellae filled with matrix and clear absence of the complexes of interdenticular sulci and caudae. C. Tooth crown from the mesial view.

Fig. 5 in The first non-avian theropod from the Czech Republic

Fig. 5. Non-avian theropod tooth, IGS-MJ-0001 (Orionides indet.) from Upper Jurassic (Oxfordian), Švédské šance (Brno-Slatina), Czech Republic. Detail of the serrations on the distal carina from the labial view.