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Fig. 7 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 7. Braincase of the ginglymodian fish Isanichthys lertboosi sp. nov., KS34-380; Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand; in ventral view. A. Photograph. B. Semi-interpretative line drawing.

Fig. 15 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 15. Ginglymodian fish Isanichthys lertboosi sp. nov., KS36-2 (holotype); Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand. A. Pectoral fin. B. Pelvic fin.

Fig. 16 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 16. Ginglymodian fish Isanichthys lertboosi sp. nov.; Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand. A. KS36-2, dorsal fin in dorsal view. B. KS36-2, dorsal fin in lateral view. C. KS36-3, dorsal fin in lateral view. All branchings and segmentations of the rays are not drawn, although present, because they are hardly visible on the specimen.

Fig. 5 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 5. Skull of the ginglymodian fish Isanichthys lertboosi sp. nov., KS34-281; Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand; in left (A) and right (B) lateral views. Photographs (A 1, B 1) and semi-interpretative line drawings (A 2, B 2).

Fig. 3 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 3. Skull of the ginglymodian fish Isanichthys lertboosi sp. nov., KS36-2 (holotype); Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand; in left (A) and right (B) lateral views. Photographs (A1, B1) and semi-interpretative line drawings (A2, B2).

Fig. 1. A in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 1. A. Schematic map of Thailand with the Isan region (frame) showing the outcrops of the Phu Kradung Formation in black and the localisation of the site of Phu Noi. B. Landscape showing the localization of the Phu Noi excavation site (circle) in the hilly lanscape surrounded by rice pads. C, D. Views of the excavations in Phu Noi in February 2010. The fish specimens are extracted with the plaster jacket technique.

Fig. 14 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 14. Ginglymodian fish Isanichthys lertboosi sp. nov.; Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand. Reconstructions of the skull with the path of sensory canals. A. KS36-3. B. KS34-281. The head is 200 mm in average length.

Fig. 13 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 13. Snout region and coronoid dentition of the ginglymodian fish Isanichthys lertboosi sp. nov., KS36-2; Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand. A. Snout region in ventral view. The grey area corresponds to matrix; the shade area corresponds to the reconstructed limit. B. Coronoid dentition in left lateral view. Photographs (A 1, B 1) and semi-interpretative line drawings (A 2, B 2).

Fig. 4 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 4. Photographs (A 1, B 1) and semi-interpretative line drawings of the skull (A 2, B 2) of the ginglymodian fish Isanichthys lertboosi sp. nov., KS36-3; Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand; in left (A) and right (B) lateral views.

Fig. 2 in A new species of the ginglymodian fish Isanichthys from the Late Jurassic Phu Kradung Formation, northeastern Thailand

Fig. 2. Holotype of the ginglymodian fish Isanichthys lertboosi sp. nov., KS36-2 (holotype); Phu Kradung Formation, Late Jurassic; Kalasin Province, Northeastern Thailand; in left lateral view. A. Photograph. B. Semi-interpretative line drawing.

Fig. 5 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 5. Digital (A) and scanning electron microscope (B–E) photographies of the five larger specimens from the Langenberg quarry (Kimmeridgian, Late Jurassic): DFMMh/ FV658 (A), DFMMh/ FV707.1 (B), DFMMh/ FV383 (C), DFMMh/ FV 530 (D), and DFMMh/ FV 382 (E).

Fig. 4 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 4. Photographs of the five larger specimens from the Langenberg quarry (Kimmeridgian, Late Jurassic). A. DFMMh/FV 530 in lingual view. B. DFMMh/FV 383 in lingual view. C. DFMMh/FV707.1 in labial view. D. DFMMh/FV 382 in lingual view. E. DFMMh/FV658 in lingual view.

Fig. 1 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 1. Geographic location of Langenberg quarry ("Rohstoffbetriebe Oker") east of Oker (Goslar), Harz Mountains, Germany (from Mudroch and Thies 1996).

Fig. 2 in Velociraptorine dromaeosaurid teeth from the Kimmeridgian (Late Jurassic) of Germany

Fig. 2. The lithostratigraphic log of the Kimmeridgian of the Langenberg quarry near Oker, Harz Mountains, Germany. The examined theropod teeth were found in bed 83 together with skeletal remains of Europasaurus holgeri (modified after Thies et al. 2007).

Fig. 2 in Foraminiferal assemblages as palaeoenvironmental bioindicators in Late Jurassic epicontinental platforms: Relation with trophic conditions

Fig. 2. Mean values of the proportions of test type and life habit of the foraminiferal assemblages in the examples studied from Boreal (Inner Moray Firth Basin) (A) and Tethyan (Prebetic) domains (B).

Fig. 1 in Foraminiferal assemblages as palaeoenvironmental bioindicators in Late Jurassic epicontinental platforms: Relation with trophic conditions

Fig. 1. Location of the sections studied Brora, Riogazas−Chorro, and Navalperal (A) with geological sketch of northeastern Scotland (B) and southeastern Spain (C), lithological columns (D) with detailed sample locations (reviewed in black circle and new in white circle), and palaeogeographic reconstruction of the western Tethys during the Callovian–Oxfordian transition (E).

Fig. 5 in Foraminiferal assemblages as palaeoenvironmental bioindicators in Late Jurassic epicontinental platforms: Relation with trophic conditions

Fig. 5. Palaeoecological reconstruction of foraminiferal assemblages from lumpy lithofacies group and marl−limestone rhythmite, and changes in selected palaeoenvironmental features (organic matter content, oxygenation, sedimentation rate, consolidation of substrate and relative distance to shore). Legends of foraminifera and pie−diagrams are in Table 2 and Fig. 3.

Fig. 4 in Foraminiferal assemblages as palaeoenvironmental bioindicators in Late Jurassic epicontinental platforms: Relation with trophic conditions

Fig. 4. Palaeoecological model of foraminiferal assemblages from Brora Brick Clay and Fascally Siltstone members, and changes in selected palaeoenvironmental features (organic matter content, oxygenation, sedimentation rate and relative distance to shore). The model tries to give a rough idea about what was deeper and shallower, but the Brora Brick Clay and Fascally Siltstone are not contemporaneous. Legends of foraminifera and pie−diagrams are in Table 2 and Fig. 3.

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Fig. 5 in The soft-tissue attachment scars in Late Jurassic ammonites from Central Russia

Fig. 5. Lateral attachment structures on Kachpurites cheremkhensis Mitta, Michailova, and Sumin 1999 shells from Late Volgian (Kachpurites fulgens Zone), Yaroslavl region, Cheremukha locality. A. MSU 113/3, whole shell with a scar at the middle section of the body chamber and a lateral sinus, which is located ventro-laterally not far from the aperture. B. MSU 113/10, shell with the apertural part of the body chamber not preserved, the scars are slightly asymmetric. C. MSU 113/36, fragment of the body chamber of ribbed macroconch, with scars on both sides of the shell. The scar demonstrate ventro-lateral projection on its front part. Asterisks mark the base of the body chamber. Photographs (A1–C1) and explanatory drawings (A2–C2).