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Figure 74 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 74: Photographs of hemispermatophore mating plug of Thorellius cristimanus, Autlán, Jalisco, Mexico. Distal barb is seen on right side of images, showing delicate curved teeth which face inwards when embedded in the hemispermatophore capsular area, the ventral side.

Figures 19–22 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figures 19–22: Paravaejovis pumilis, male, Ciudad Constitución, Baja California Sur, Mexico, showing diagnostic characters. 19. Chela, ventral view, showing neobothriotaxy. 20. Femur, dorsointernal view, showing trichobothria configuration, note midsegment position of e and d located distal to i (trichobothria connected by white lines). 21. Chelicera, ventral view, showing serrula and lack of ventral dentition on ventral edge of movable finger. 22. Chelal movable finger denticle edge, showing seven ID denticles and enlarged MD denticles approximating size of OD denticles.

Figure 15 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 15: Trichobothrial pattern of Vaejovis janssi, male, Isla Socorro, Mexico (after Soleglad & Fet, 2005: figs. 20–26, in part).

Figure 10 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 10: Trichobothrial pattern of Syntropis williamsi, female holotype, Los Aripes, Baja California Sur, Mexico (after Soleglad et al., 2007: fig. 15).

Figure 11 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 11: Trichobothrial pattern of Kochius punctipalpi punctipalpi, female, Cabo San Lucas, Baja California Sur, Mexico.

Figure 14 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 14: Pedipalp trichobothrial pattern of Vaejovis mexicanus, female neotype, Mexico City, Mexico (after Fet & Soleglad, 2007: fig. 7).

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Figure 47 in Contributions to scorpion systematics. II. Stahnkeini, a new tribe in scorpion family Vaejovidae (Scorpiones: Chactoidea)

Figure 47: Map showing distribution of genus Stahnkeus. Individual localities based on specimens examined, Williams (1970a, 1980: fig. 98, in part), Berke (1987, in part) and Sissom & Stockwell (1991).

Figure 17 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 17: Histogram showing position of chelal trichobothrium Dt in relation to the palm length (Dt_pos/Palm_L: Dt_pos measured from palm base). More than 100 species and subspecies of family Vaejovidae and subfamily Uroctoninae (Chactidae) are represented. The extreme basal position of Dt in Uroctoninae is shown in contrast with Vaejovidae since at one time genus Uroctonus was considered a vaejovid. Vertical arrow indicates palm midpoint (i.e., ratio = 0.500). See Fig. 1 for explanation of histogram components.

Figure 6 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 6: Trichobothrial pattern of Vejovoidus longiunguis, female, Las Bombas, Baja California Sur, Mexico.

Figure 5 in Contributions to scorpion systematics. III. Subfamilies Smeringurinae and Syntropinae (Scorpiones: Vaejovidae)

Figure 5: Trichobothrial pattern of Smeringurus grandis, female, Oakies Landing, Baja California, Mexico.

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Fig. 3 in The systematics of Late Jurassic tyrannosauroid theropods from Europe and North America

Fig. 3. Autapomorphies of tyrannosauroids Juratyrant langhami Benson, 2008, Kimmeridge Clay, Dorset England, Late Jurassic (early Tithonian) (A, B) and Stokesosaurus clevelandi Madsen, 1974, Morrison Formation, Utah, USA, Late Jurassic (early Tithonian) (C). A. Right pubis (OUMNH J.3311−22) in lateral view, with the autapomorphic lateral fossa denoted. B. Left ischium (OUMNH J.3311−25) in lateral (B1) and anterior (B2) views, with an inset close up (2.5× magnification) of the autapomorphic folded proximal region of the ischial apron (B3). The autapomorphic convex ischial tubercle is also denoted. C. Pubic peduncle of the left ilium (UMNH 2938) in medial view, with the autapomorphic swollen rim indicated.

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Fig. 2 in The systematics of Late Jurassic tyrannosauroid theropods from Europe and North America

Fig. 2. The phylogenetic relationships of tyrannosauroids, based on a revised analysis of the Brusatte et al. (2010) dataset. Details of the analysis are described in the text and the dataset is presented in SOM. The cladogram shown here is the single most parsimonious tree recovered by the analysis, with the wildcard taxon Aviatyrannis excluded (570 steps, CI = 0.640, RI = 0.835). Numbers next to nodes denote bootstrap percentages (based on 1000 replicates) and Bremer support. Note that Stokesosaurus clevelandi and "S." langhami (here referred to by its new genus name, Juratyrant) are not found as sister taxa, and therefore a monophyletic Stokesosaurus is not recovered. When Aviatyrannis is included in the analysis, the strict consensus of nine most parsimonious trees (not figured) shows identical and fully resolved relationships among Xiongguanlong and all more derived taxa. However, Stokesosaurus clevelandi, "S." langhami, and Eotyrannus, form a polytomy. This clade, in turn, is part of a large basal polytomy that also includes the Xiongguanlong + more derived clade, Dilong, Aviatyrannis, Guanlong, Kileskus, Proceratosaurus, and Sinotyrannus. On the figured cladogram, the following unambiguous synapomorphies support major clades, with character numbering following that in the character list of Brusatte et al. (2010) and SOM: all tyrannosauroids more derived than Dilong (33, 41, 49, 80, 180, 181, 196, 198, 221, 239, 241, 244, 257, 274, 281, 289, 290); the clade of S. clevelandi, Juratyrant, and Eotyrannus (258, 310, 311, 313); the clade of Juratyrant and Eotyrannus (no unambiguous synapomorphies).

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Fig. 1 in The systematics of Late Jurassic tyrannosauroid theropods from Europe and North America

Fig. 1. Ilia of basal non−tyrannosaurid tyrannosauroids with a posterodorsally inclined ridge on the lateral surface of the ilium. A. Right ilium (reversed) of Juratyrant langhami Benson, 2008 (OUMNH J.3311−21), Kimmeridge Clay, Dorset England, Late Jurassic (early Tithonian). B. Left ilium of Stokesosaurus clevelandi, Madsen 1974 (UMNH VP 7473), Morrison Formation, Utah, USA, Late Jurassic (early Tithonian). C. Left ilium of Eotyrannus lengi Hutt, Naish, Martill, Barker, and Newberry, 2001 (MIWG 1997.550), Wessex Formation, Isle of Wight, England, Early Cretaceous (Barremian). All in lateral view. Arrows denote the lateral ridge.

Fig. 2 in New remains attributable to the holotype of the sauropod dinosaur Neuquensaurus australis, with implications for saltasaurine systematics

Fig. 2. Holotypic sacrum of the sauropod Neuquensaurus australis (Lydekker, 1893), MLP Ly 1 and 7, from the Late Cretaceous of Neuquén, Argentina. Stereophotographs and line drawings in ventral view. The abbreviations (s1–s7) indicate sacral vertebral identity. Dashed lines indicate missing bone, and dotted lines indicate intervertebral sutures.

Fig. 1 in New remains attributable to the holotype of the sauropod dinosaur Neuquensaurus australis, with implications for saltasaurine systematics

Fig. 1. Holotypic sacrum of the sauropod Neuquensaurus australis (Lydekker, 1893), MLP Ly 1 and 7, from the Late Cretaceous of Neuquén, Argentina. Posterior view of sixth sacral vertebra and anterior view of seventh sacral vertebra showing corresponding matrix, which snaps together when the vertebrae are articulated. The abbreviations (s6–s7) indicate sacral vertebral identity. Dashed lines indicate missing bone.

Fig. 4 in New remains attributable to the holotype of the sauropod dinosaur Neuquensaurus australis, with implications for saltasaurine systematics

Fig. 4. Holotypic sacrum of the sauropod Neuquensaurus australis (Lydekker, 1893), MLP Ly 1 and 7, from the Late Cretaceous of Neuquén, Argentina in right lateral view. The abbreviations (s1–s7) indicate sacral vertebral identity. Dashed lines indicate missing bone.

Fig. 5 in New remains attributable to the holotype of the sauropod dinosaur Neuquensaurus australis, with implications for saltasaurine systematics

Fig. 5. Holotypic seventh sacral vertebra of the sauropod Neuquensaurus australis (Lydekker, 1893), MLP Ly 1, from the Late Cretaceous of Neuquén, Argentina in left lateral (A), ventral (B), anterior (C), right lateral (D), dorsal (E), and posterior (F) views.

Fig. 8. Sauropod sacrum PVL 4017−18 in New remains attributable to the holotype of the sauropod dinosaur Neuquensaurus australis, with implications for saltasaurine systematics

Fig. 8. Sauropod sacrum PVL 4017−18 from the Saltasaurus loricatus quarry at El Brete, Argentina. Stereophotographs in right lateral view, with anterior towards the top. The abbreviations s1 and s7 indicate sacral vertebral identity.

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Fig. 37 in Systematic Revision Of The Troglomorphic North American Scorpion Family Typhlochactidae (Scorpiones: Chactoidea)

Fig. 37. Typhlochactas sissomi Francke et al., 2009, subadult ³ holotype (IBUNAM), sinistral pedipalp femur (A) and patella (B–D) showing carinae and distribution of trichobothria. A, B. Dorsal aspect. C. External aspect. D. Ventral aspect. Scales 5 0.5 mm.