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Figure 3 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran

Figure 3. Outcrop of Chehrabad tracksite, photographed by the quadcopter UAV, and its sketch, extracted from high-resolution UAV photos. The lower highlighted part of the slab was traced on transparent plastic (Fig. 4). Scale bar represents 1 m. Quadrangles show position of Fig. 9a–d.

Figure 4. CMN 59667 in An ankylosaurian dinosaur from the Cenomanian Dunvegan Formation of northeastern British Columbia, Canada

Figure 4. CMN 59667 compared to other ankylosaur dorsal vertebrae. (a) Right lateral view of isolated neural arch of CMN 59667, Ankylosauria indet. (b) Left lateral view of third dorsal vertebra from AMNH 5337, Euoplocephalus tutus. (c) Left lateral view of seventh dorsal vertebra of AMNH 5895, Ankylosaurus magniventris. Abbreviations are as follows: c – centrum; d – diapophysis; ns – neural spine; p – parapophysis; poz – postzygapophysis; prz – prezygapophysis; tp – transverse process.

Figure 5 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran

Figure 5. (a–d) Ichnospecies Felipeda lynxi photographed in the lower part of the slab of the tracksite, preserved as convex hyporelief. Scale equals millimeters (mm) in (a) and centimeters (cm) in (b)–(d).

Figure 4 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran

Figure 4. Carnivore and bird footprints in the lower part of the slab in detail: MC, mud-crack cast; GC, groove cast; CT, crawling trace.

Figure 2. CMN 59667 in An ankylosaurian dinosaur from the Cenomanian Dunvegan Formation of northeastern British Columbia, Canada

Figure 2. CMN 59667, block including portions of two ankylosaur dorsal vertebrae and two probable ankylosaur ribs. (a) Photograph and (b) interpretive illustration of isolated centrum (lateral view) and isolated neural arch (oblique dorsolateral view). (c) Reverse side of block, showing remains of two ribs and parts of the vertebrae, and (d) interpretive illustration of the same. Abbreviations are as follows: c – centrum; d – diapophysis; ns – neural spine; pz – postzygapophysis; tp – transverse process; r1 – rib 1; r2 – rib 2; ri1 – impression of rib 1.

Figure 1. CMN 59667 in An ankylosaurian dinosaur from the Cenomanian Dunvegan Formation of northeastern British Columbia, Canada

Figure 1. CMN 59667 was collected along the Pine River in northeastern British Columbia, approximately 1.6 km downstream of its junction with the Murray River. Sedimentological and palaeontological features in this area suggest these are outcrops of the upper two-thirds of allomember E of the Dunvegan Formation. (a) Location of the collection site for CMN 59667 in British Columbia, Canada, indicated by a red star (inset map shows location in western Canada). (b) Tetrapodosaurus pes natural cast (RBCM P1473) discovered at this site; anterior is to the right. (c) RBCM P1028, sample with Metasequoia leaf and obovate or elliptical angiosperm leaf with entire margin (leaf morphotype 122; Ash et al., 1999). (d) RBCM P1030, palmately lobed angiosperm leaf (leaf morphotypes 140–143; Ash et al., 1999). (e) Cliff-forming outcrops on the eastern bank of the Pine River, 1.6 km from its junction with the Murray River, as viewed from the west bank. (f) Gymnosperm cone in cross section (not collected), observed on the west bank of the Pine River.

Figure 3 in An ankylosaurian dinosaur from the Cenomanian Dunvegan Formation of northeastern British Columbia, Canada

Figure 3. Details of vertebrae of CMN 59667. (a) Right lateral view of isolated neural arch (with oblique ventrolateral view of adhering isolated centrum), showing the diapophyseal sulcus on the transverse process. (b) Axial view of the isolated centrum, broken at its approximate mid-length, showing strong constriction of the centrum. (c) Ventral view of the transverse process of the isolated neural arch, showing the diapophyseal sulcus. Abbreviations are as follows: c – centrum; d – diapophysis; ns – neural spine; pz – postzygapophysis; tp – transverse process.

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Figure 3 in An insect wing discovered in the Early Permian Taiyuan Formation (Shanxi Province, China)

Figure 3. Putative stem-Orthoptera from the Taiyuan Formation (SXMG IV 0480): (a) interpretative drawing (see text for alternative interpretation) and (b) photograph (flipped horizontally).

Figure 2 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran

Figure 2. Stratigraphic column of URF in the west of Zanjan Province with three vertebrate footprints bearing lithohorizons. The Chehrabad tracksite is in the second lithohorizon.

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Figure 2 in An insect wing discovered in the Early Permian Taiyuan Formation (Shanxi Province, China)

Figure 2. The stratigraphic column of the Taiyuan Formation, near Yangquan City, Shanxi Province, China. The arrow indicates the fossil horizon.

Figure 1 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran

Figure 1. Location and geological map: (a) Location of Zanjan Province in Iran, (b) location of the study area in the west of Zanjan, (c) outcrop of Upper Red Formation (URF) in the Chehrabad area, and (d) geological map of the URF and location of studied tracksite. Base geological map by Lotfi (2001) (with permission).

opencc-by-4.0Aug 2014View details →

Figure 1 in The stratigraphic importance of the brontothere (cf. Diplacodon elatus) in the Brennan Basin Member of the Duchesne River Formation of Utah

Figure 1. (a) Photograph of location of fossil discovered in situ. (b) Terminology used in the description of the upper molar. (c) Image of the specimen of cf. Diplacodon elatus collected from the Brennan Basin Member of the Duchesne River Formation. See the Supplement.

Figure 9 in The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada - a review of previously described taxa and a description of a new genus and species

Figure 9. Scales from †Lambeia pectinatus (YPM 8664). Scales are from region B3 (see Fig. 8) and have pectinated posterior and ventral margins. (a) Photograph of scales from latex peel; (b) illustration of scales.

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Figure 4 in The stratigraphic importance of the brontothere (cf. Diplacodon elatus) in the Brennan Basin Member of the Duchesne River Formation of Utah

Figure 4. Stratigraphic position of brontotheres in northeastern Utah. Measure section of Uinta Formation based on Townsend et al. (2006).

Figure 6 in The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada - a review of previously described taxa and a description of a new genus and species

Figure 6. Reconstruction of the head of †Lambeia pectinatus detailing bones and ganoine ornamentation. Illustration based on type and only specimen, YPM 8664. Abbreviations: ao, antorbital; aop, accessory opercular bones; br, branchiostegal rays; cl, cleithrum; d, dentary; dh, dermohyal; dpt, dermopterotic; dsp, dermosphenotic; ex, extrascapular; io, infraorbital; lg, lateral gular; mdr, median dorsal rostral; mg, median gular; mx, maxilla; n, nasal; op, operculum; p, parietal; pc, postcleithrum; pop, preoperculum; pp, post-parietal; ps, presupracleithrum; pt, posttemporal; sc, sclerotic; scl, supracleithrum; so, suborbital; sop, suboperculum; sup, supraorbital; vr-pmx; ventral rostro-premaxilla. Dark gray filled circles represent sensory pores; light gray areas represent areas of infilling; dashed lines represent areas of ambiguity and reconstruction.

Figure 3 in The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada - a review of previously described taxa and a description of a new genus and species

Figure 3. Illustrations of type specimens of Jackson's (1851) original species from the Albert Formation of New Brunswick, Canada. (a) †Rhadinichthys (†Palaeoniscum) alberti, illustration of MCZ 5082; (b) †Rhadinichthys (†Palaeoniscum) cairnsii, illustration of MCZ 5084; (c) †Elonichthys brownii, illustration of MCZ 5083. Dashed lines represent areas of ambiguity that have been reconstructed. Scale bars equal 5 mm.

Figure 1 in The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada - a review of previously described taxa and a description of a new genus and species

Figure 1. Map of locality. (a) Map of North America; box highlights area enlarged in (b). (b) Close up of New Brunswick, Canada. Dashed line indicates Albert County, where the majority of the specimens were collected. Black dot indicates Hillsborough, the site at which the original material described by Jackson was collected. Scale bar equals 50 km; (a) not to scale. Map modified from Google Maps, Map Data: ' 2015 Google.

Figure 10 in The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada - a review of previously described taxa and a description of a new genus and species

Figure 10. Photographs of the fins of †Lambeia pectinatus (YPM 8664). (a) Pectoral fin; (b) pelvic fin; (c) anal fin. All photographs depict the latex peel of YPM 8664. Scale bars equal 5 mm.

Figure 5 in The lower actinopterygian fauna from the Lower Carboniferous Albert shale formation of New Brunswick, Canada - a review of previously described taxa and a description of a new genus and species

Figure 5. Photographs of the lateral view of the head of the latex peel of type specimen of †Lambeia pectinatus, YPM 8664. Scale bars equal 5 mm.