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FIGURE 3 in The effects of lithification on fossil assemblage biodiversity and composition: An experimental test

FIGURE 3. Classical (A) and coverage-based (B) rarefaction of the Fort Thompson Formation samples. In each panel, the red curve marks the lithified sample, and the blue curve marks the corresponding unlithified replicate sample. The gray curves mark other unlithified samples taken from different horizons of the same formation at the same outcrop. The red and blue bands mark 95% confidence intervals.

FIGURE 7 in The effects of lithification on fossil assemblage biodiversity and composition: An experimental test

FIGURE 7. Relative abundances of the ten most abundant species in the overall dataset. Relative abundance is plotted on a square-root scale so that low values can be more easily distinguished. A. Bermont Formation. B. Fort Thompson Formation.

FIGURE 6. Principal coordinates analysis. The eigenvalues for the first two axes accounted for 72 in The effects of lithification on fossil assemblage biodiversity and composition: An experimental test

FIGURE 6. Principal coordinates analysis. The eigenvalues for the first two axes accounted for 72% of the variation in the data.

FIGURE 5 in The effects of lithification on fossil assemblage biodiversity and composition: An experimental test

FIGURE 5. Percentage of individuals in each sample belonging to small-shelled species, defined as less than 15 mm. A. Bermont Formation. B. Fort Thompson Formation.

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Fig. 1 in The invasive white ginger lily (Hedichium coronarium) simplifies the trait composition of an insect assemblage in the littoral zone of a Savanna reservoir

Fig. 1. Location and characterization of plant composition banks of Fazzari reservoir in the Brazilian Savanna (Cerrado Biome, Brazil).

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Fig. 3 in The invasive white ginger lily (Hedichium coronarium) simplifies the trait composition of an insect assemblage in the littoral zone of a Savanna reservoir

Fig. 3. The average values of CWM-trait values of aquatic insect assemblages in invaded and non-invaded banks by white ginger lily of a reservoir in Brazilian Savanna (Cerrado Biome). A – CWM-FFG, B – CWM-feed, C – CWM-habit, D – CWM body length. CWM, Community level Weight-Mean.

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FIGURE 2 in First early Eocene lizards from Spain and a study of the compositional changes between late Mesozoic and early Cenozoic Iberian lizard assemblages

FIGURE 2. Paleogeographic map of Western Europe during the early Eocene (modified from Marandat et al., 2012) and situation of the Catalan localities yielding material described in the text and other contemporaneous European fossil sites. Note that the localities of the Southern Pyrenean Basin (Escarlà, La Roca, Masia de l'Hereuet, Barranc del Fusteró and Font del Torricó) are geographically very close, although situated in different sub-basins (see text).

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FIGURE 1. Selected lizard and amphisbaenian material from studied localities. 1-2 in First early Eocene lizards from Spain and a study of the compositional changes between late Mesozoic and early Cenozoic Iberian lizard assemblages

FIGURE 1. Selected lizard and amphisbaenian material from studied localities. 1-2, Geiseltaliellus sp.: 1, left dentary (IPS 49740); 2, maxilla (IPS 83552); 3-4, Iguanidae indet.: 3, fragment of dentary (IPS 83535) with one preserved tooth, 4, fragment of?maxilla with four preserved teeth (IPS 49756); 5-6, Agamidae indet.: 5, Fragment of toothbearing bone preserving one tooth (IPS 83546), 6, fragment of dentary preserving two teeth (IPS 83543). 7-8, Gekkota indet.: 7, posterior portion of left dentary (IPS 59559), 8, anterior portion of left dentary (IPS 83520); 9, Scincoidea (?Scincidae) indet., fragment of right dentary (IPS 49752); 10,?Lacertidae indet., fragment of tooth-bearing bone perserving two teeth (IPS 49762); 11, Amphisbaenia indet., vertebra (IPS 59529); 12, cf. Placosaurus sp., partial parietal with fused osteoderms (IPS 59567); 13, Glyptosaurini indet., skull osteoderm (IPS 83532); 14, Glyptosaurinae indet., body osteoderm (IPS 83533); 15-18, Anguinae indet.: 15, keeled body osteoderm (IPS 83540), 16, unkeeled body osteoderm (IPS 83533), 17, partial parietal (IPS 83557), 18, vertebra (IPS 59538); 19-20, "Necrosauridae" indet.: 19, partial left dentary (IPS 83545), 20, osteoderm (IPS 49741). 1, 2, 5, 6, 11, 15 and 17-20 from Masia de l'Hereuet (MP8+9); 3, 4, 7, 8, 10 and 14 from La Morera (MP10); 12 from Escarlà (MP10); 13 and 16 from Font del Torricó. 1-10 and 19 in labial view; 11-12, 17 in dorsal view; 13-16 and 20 in external view; 18 in ventral view.

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FIGURE 3 in First early Eocene lizards from Spain and a study of the compositional changes between late Mesozoic and early Cenozoic Iberian lizard assemblages

FIGURE 3. Distribution of lizard and amphisbaenian taxa from the latest Cretaceous to the late Eocene in the Iberian Peninsula. Records from Font del Torricó are omitted because its exact age inside the early Eocene is unknown. Black squares indicate unambiguous records, whereas grey squares indicate uncertainty. LaMa: Late Maastrichtian; eLaMa: earliest Late Maastrichtian; E/LaMa: Early or Late Maastrichtian; Late Campanian.

Fig. 29 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 29. Globaura venusta: A–C, IGM 3/164, nearly complete skull with mandibles from Khulsan, dorsal, ventral, and right lateral views; D–F, IGM 3/160, nearly complete skull with mandibles from Ukhaa Tolgod, dorsal, ventral, and left lateral views.

Fig. 25 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 25. Skull of Parmeosaurus scutatus, new genus and species: A–C, IGM 3/139, incomplete skull with mandibles, dorsal, ventral, and right lateral views; D–F, IGM 3/140, incomplete skull with mandibles, dorsal, ventral, and left lateral views.

Fig. 28 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 28. Scincomorpha, family incertae sedis, Slavoia darevskii: A, B, IGM 3/154, incomplete skull with mandible and partial postcranial skeleton from Khulsan, dorsal and ventral views; C, IGM 3/145, nearly complete skull with mandibles and partial postcranial skeleton from Ukhaa Tolgod, dorsal view D, IGM 3/146, incomplete skull with mandibles and articulated postcranial skeleton from Ukhaa Tolgod dorsal view.

Fig. 37 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 37. Virtually complete lizard skeleton from Ukhaa Tolgod, dorsal view (courtesy of Amy Davidson).

Fig. 36 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 36. Exceptional preservation of lizard specimens at Ukhaa Tolgod: A, SEM photograph of unworn dentary teeth of IGM 3/50 (Carusia intermedia), ×20; B, higher magnification of three posterior teeth in lingual view, ×50; C, undistorted braincase of a possible iguanian, arrows pointing to lateral semicircular canal.

Fig. 19 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 19. Tchingisaurus multivagus: A–C, IGM 3/129, incomplete skull with mandibles, dorsal, left and right lateral views.

Fig. 24 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 24.?Scincoidea, family incertae sedis, Parmeosaurus scutatus, new genus and species: A, B, IGM 3/138 (holotype), skull with articulated postcranial skeleton from Ukhaa Tolgod, dorsal and ventral views.

Fig. 15 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 15. Scincomorpha, Teiidae (Polyglyphanodontinae), Adamisaurus magnidentatus: A– C, IGM 3/116, nearly complete skull with mandibles from Tugrugeen Shireh, dorsal, left and right lateral views.

Fig. 14 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 14. Gekkota incertae sedis, Myrmecodaptria microphagosa, new genus and species: A–C, IGM 3/95 (holotype), incomplete skull with mandibles from Ukhaa Tolgod, left lateral, dorsal, and ventral views.

Fig. 13 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 13. Iguania incertae sedis, Isodontosaurus gracilis: A, B, IGM 3/91, cranial part of a skeleton preserved in concretion from Tugrugeen Shireh, dorsal and left lateral views; C, D, IGM 3/92, incomplete skull with mandibles from Tugrugeen Shireh, dorsal and ventral views.

Fig. 12 in Taxonomic Composition And Systematics Of Late Cretaceous Lizard Assemblages From Ukhaa Tolgod And Adjacent Localities, Mongolian Gobi Desert

Fig. 12. Iguania incertae sedis, Isodontosaurus gracilis: A–C, IGM 3/84, incomplete skull with mandibles from Ukhaa Tolgod, dorsal, ventral, and lateral views.