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FIG. 3 in New ctenodactyloid rodents from the Erlian Basin, Nei Mongol, China, and the phylogenetic relationships of Eocene Asian ctenodactyloids

FIG. 3. Fragmentary maxillae and mandibles of Tamquammys wilsoni in occlusal view. A, V17790, a right maxilla with P3–M3; B, V17785.1, a right maxilla with P3–M2; C, V17786.2, a right mandible with p4–m3; D, V17787.5, a right mandible with dp4–m2.

FIG. 2 in New ctenodactyloid rodents from the Erlian Basin, Nei Mongol, China, and the phylogenetic relationships of Eocene Asian ctenodactyloids

FIG. 2. Stratigraphic distribution of ctenodactyloid taxa in the Huheboerhe-Nuhetingboerhe area, plotted on a composite section modified from Wang et al. (2010). Fossil horizons are denoted as, in ascending order, NM-1 to NM-4 in the Nomogen Formation, AS-1 to AS-6 in the Arshanto Formation, and IM-1 to IM-2 in the Irdin Manha Formation) (modified from Wang et al., 2010: fig. 2). Black squares indicate occurrences of ctenodactyloid species from the fossil horizons that were described in this study.

FIG. 5 in New ctenodactyloid rodents from the Erlian Basin, Nei Mongol, China, and the phylogenetic relationships of Eocene Asian ctenodactyloids

FIG. 5. Cheek teeth of Tamquammys robustus. A, V17770.1, an adult left maxillary fragment with M1–3; B, V17772.5, an adult right mandible fragment with p4–m3; C, V17773.5, a juvenile right mandible fragment with dp4–m3.

FIG. 1 in New ctenodactyloid rodents from the Erlian Basin, Nei Mongol, China, and the phylogenetic relationships of Eocene Asian ctenodactyloids

FIG. 1. Diagram showing the terminology applied to ctenodactyloid dental morphology (anterior to the left and labial to the top) (modified from Wang, 1997; Tong, 1997; Meng and Wyss, 2001).

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Figure 3 in The phylogenetic relationships of Chalcosiinae (Lepidoptera, Zygaenoidea, Zygaenidae)

Figure 3. Diagram that interprets Alberti's (1954) concept of the relationships of 'Hauptstamm II of Zygaenidae' and the tribal classification of Chalcosiinae. Characters used to define each tribe: Chalcosiini: valvae and uncus keeled, A8 specialized, aedeagus stout and curved. Cyclosiini: uncus pointed, valvae elongated, aedeagus slender, median vein forked. Agalopini: uncus slender, valvae elongated, median vein straight or forked. Heteropanini: Lycaenidae-like, ovipositor not so developed, ductus seminalis arising from ductus bursae Aglaopini: R3–5 not anastomosed, genitalia similar to Elcysma. The following genera were not included because material was not available: Allocaprima, Allocyclosia, Atelesia, Barbaroscia, Boradiopsis, Clematoessa, Cryptophysophilus, Cyanidia, Doclea, Docleomorpha, Eucormopsis, Euxanthopyge, Hadrionella, Hemiscia, Herpidia, Herpolasia, Heterusinula, Isocrambia, Mimascaptesyle, Opisoplatia, Panherpina, Phlebohecta, Sciodoclea, Scotopais and Thaumastophleps.

Figure 6 in A new choristodere (Reptilia: Diapsida) from the Lower Cretaceous of western Liaoning Province, China, and phylogenetic relationships of Monjurosuchidae

Figure 6. Comparison of the two equally parsimonious trees (TL = 123 steps; CI = 0.85; RI = 0.87) derived from analysis of data presented in Appendices 1 and 2.

Figure 5 in A new choristodere (Reptilia: Diapsida) from the Lower Cretaceous of western Liaoning Province, China, and phylogenetic relationships of Monjurosuchidae

Figure 5. Philydrosaurus proseilus gen. et sp. nov., pelvic girdle, hind limbs and anterior caudal vertebrae of the holotype (PKUP V2001). Double arrows pointing to the ischium spike.

Figure 4 in A new choristodere (Reptilia: Diapsida) from the Lower Cretaceous of western Liaoning Province, China, and phylogenetic relationships of Monjurosuchidae

Figure 4. Philydrosaurus proseilus gen. et sp. nov., pectoral girdle and fore limb of the holotype (PKUP V2001). Note arrows pointing to ect- and entepicondylar foramina.

Figure 3 in A new choristodere (Reptilia: Diapsida) from the Lower Cretaceous of western Liaoning Province, China, and phylogenetic relationships of Monjurosuchidae

Figure 3. Philydrosaurus proseilus gen. et sp. nov., photograph and line drawing of the holotype skull and mandibles (PKUP V2001).

Figure 1 in A new choristodere (Reptilia: Diapsida) from the Lower Cretaceous of western Liaoning Province, China, and phylogenetic relationships of Monjurosuchidae

Figure 1. Map showing geographical location of monjurosuchid fossil sites in China: Shangheshou near Chaoyang, Jingangshan (Zaocishan) near Yixian, Doutai near Yixian, and Niuyingzi and Dawangzhangzi near Lingyuan.

Figure 2 in A new choristodere (Reptilia: Diapsida) from the Lower Cretaceous of western Liaoning Province, China, and phylogenetic relationships of Monjurosuchidae

Figure 2. Philydrosaurus proseilus gen. et sp. nov., holotype (PKUP V2001) from Shangheshou near Chaoyang, western Liaoning Province; Early Cretaceous Chiufotang Formation.

Figure 5 in New taxa of Japanese and New Zealand Eurystomellidae (Phylum Bryozoa) and their phylogenetic relationships

Figure 5. The strict consensus of 39 final trees. Synapomorphies for each clade in the ingroups are indicated by solid bars: lunulitiform colony (1), encrusting colony (1¢), ancestrular attachment without cementation (2), subtatiform ancestrular frontal wall (3), gymnocystal foramina (6), lack of well-formed costae (8), zooid deeper than length (12), undifferentiated proximal corners of orificial anter (13), indented proximolateral corners of orificial poster (15), vestigial excavations in gymnocystal surface (16), small excavations in gymnocystal surface (16¢), lack of medial suture in proximal rim or orifice (18), maternal orifice slightly dimorphic (19), endozooidal brooding of embryos (20), two kenozooidal foramina (22), one central plus two small kenozooidal foramina (22¢), interzooidal communications with pore-chambers (25).

Figure 4 in New taxa of Japanese and New Zealand Eurystomellidae (Phylum Bryozoa) and their phylogenetic relationships

Figure 4. One of the 39 most parsimonious trees obtained from the final analysis carried out by PAUP*. The transformations of all 25 skeletal characters are mapped (cf. Character List).

Figure 3. A–C in New taxa of Japanese and New Zealand Eurystomellidae (Phylum Bryozoa) and their phylogenetic relationships

Figure 3. A–C, Integripeltra shirayamai sp. nov. Saiki-wan, Honshu. A, autozooids, x, 70. B, maternal zooids with foraminate kenozooids distally, ¥116. C, autozooidal orifice with proximal rim partly removed to show how the long crescentic slits are merely the frontal expressions of the proximolateral embayments of the orifice, ¥201. D, E, Integripelta umbonata sp. nov. NZOI Stn Z9697. F, autozooids and a maternal zooid with foraminate distal kenozooid, ¥106. G, prox-

Figure 2. A, B in New taxa of Japanese and New Zealand Eurystomellidae (Phylum Bryozoa) and their phylogenetic relationships

Figure 2. A, B. Integripelta novella sp. nov. Hokkaido, intertidal. A, autozooids and two maternal zooids, the kenozooid distal to the one at left lacking a foramen, ¥89. B, maternal zooid with distal foraminate kenozooid, ¥121. C, D, Integripelta japonica sp. nov. Mi-shimi, Honshu. C, autozooids and maternal zooids, ¥53. D, maternal orifice and kenozooid, ¥211. E, F, Integripelta sextaria sp. nov. NZOI Stn Z9700. E, autozooids and maternal zooids, ¥48. F, autozooidal orifice, ¥181.

Figure 1. A, B in New taxa of Japanese and New Zealand Eurystomellidae (Phylum Bryozoa) and their phylogenetic relationships

Figure 1. A, B, Eurystomella foraminigera. Greta Point, Wellington, intertidal. A, group of zooids, ¥65. B, suboral rim, showing triradiate suture, ¥803. C-E, Eurystomella biperforata sp. nov. C,E, NZOI Stn Z9700. C, group of autozooids, ¥53. D, NZOI Stn Z9677, maternal zooid with distal foraminate kenozooid, ¥95. E, rare zooid with a single foramen, ¥163. F, Eurystomella aupouria sp. nov. NZOI Stn Z9716, ¥63.

Figure 17 in A new species of Halisaurus from the Late Cretaceous phosphates of Morocco, and the phylogenetical relationships of the Halisaurinae (Squamata: Mosasauridae)

Figure 17. Strict consensus tree of six most parsimonious trees (270 steps) showing the phylogenetic relationships of Halisaurus arambourgi sp. nov. and Halisaurinae among Mosasauridae.

Figure 16 in A new species of Halisaurus from the Late Cretaceous phosphates of Morocco, and the phylogenetical relationships of the Halisaurinae (Squamata: Mosasauridae)

Figure 16. Halisaurine skull reconstructions in dorsal view. A, Halisaurus platyspondylus (from Holmes & Sues, 2000); B, Halisaurus ortliebi (from Lingham-Soliar, 1996); C, Halisaurus arambourgi sp. nov.; D, Eonatator sternbergii (from Bardet & Pereda Suberbiola, 2001). Scale bar = 10 cm.

Figure 14 in A new species of Halisaurus from the Late Cretaceous phosphates of Morocco, and the phylogenetical relationships of the Halisaurinae (Squamata: Mosasauridae)

Figure 14. Comparisons of halisaurine quadrates in lateral (above) and posterior (below) views. A, Halisaurus platyspondylus (USNM 442450; from Holmes & Sues, 2000); B, Halisaurus ortliebi (IRSNB R 34; N.B. pers. observ.); C, Halisaurus arambourgi sp. nov. (private collection); D, Eonatator sternbergii (UPI R 163; N.B. pers. observ.). Scale bar = 2 cm.

Figure 6 in A new species of Halisaurus from the Late Cretaceous phosphates of Morocco, and the phylogenetical relationships of the Halisaurinae (Squamata: Mosasauridae)

Figure 6. Halisaurus arambourgi sp. nov. OCP DEK/GE 101, incomplete disarticulated skeleton, Late Cretaceous (Maastrichtian), Oulad Abdoun Basin, Morocco. Scale bar = 10 cm.