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Fig. 3 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 3. Drainage map of southwest South Dakota showing the rivers and creeks mentioned in early accounts of western exploration of part of what was then known as the Nebraska Territory. The numbers 1 and 2 indicate Sage Creek and Bear Creek, respectively, two of the collecting localities of Meek and Hayden in 1853.

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Fig. 2 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 2. Upper Cretaceous (Campanian and Maastrichtian) ammonite biostratigraphy of the U.S. Western Interior showing the zones of Baculites compressus and B. cuneatus (Cobban et al., 2006). The absolute ages are derived from 40Ar/39Ar analyses of bentonites containing sanidines. In North America, the Campanian is divided into three parts. The Campanian/Maastrichtian boundary is currently placed in the middle of the B. eliasi Zone, based on recent work in Tercis, France, and the Vistula River Valley, Poland (Remin, 2009).

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Fig. 1 in Scaphites Of The ''Nodosus Group'' From The Upper Cretaceous (Campanian) Of The Western Interior Of North America

Fig. 1. Map of the upper Campanian Baculites compressus Zone showing the shoreline along the western margin of the Western Interior Seaway. The shoreline is dashed, for example, in eastern Wyoming, because of a lack of data. The dots indicate localities of B. compressus. Numbers refer to USGS Mesozoic localities, as listed below, except for locality 1 (Geological Survey of Canada). See appendix 1 for a description of localities. 1. GSC C-186877 (Jerzykiewicz, 1996); 2. D4129–32; 3. D4125–27; 4. D4120; 5. 7325, D2553, D3634; 6. 9866; 7. 23990; 8. 24178; 9. D3819, D3820; 10. D3827; 11. D6854; 12. 4710, 6037; 13. D3624; 14. D3083; 15. D490; 16. D4138; 17. D764; 18. D76; 19. D3595, D3599; 20. D4209; 21. 21577, D5659; 22. D782; 23. D780; 24. D2632, D2633; 25. D3575; 26. D3578; 27. 21224; 28. D3443; 29. 23057; 30. D1055; 31. D4994; 32. D1598, D2393; 33. D3074; 34. D1594, 23072; 35. D13708; 36. D2618; 37. D213; 38. D1661; 39. D1657; 40. D13791; 41. D4968; 42. D13507; 43. D13508; 44. D4965; 45. D4101; 46. D8782; 47. D5037; 48. D8378; 49. D9637, D9640; 50. D9677; 51. D5991; 52. D1351; 53. D8089; 54. D4497; 55. D8068; 56. D2723; 57. D2941; 58. D337; 59. D40; 60. D271, D280; 61. D8004; 62. D8874; 63. D1080; 64. D615; 65. D440.

FIG. 1. — Micropora mikesmithi n in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 1. — Micropora mikesmithi n. sp.: A-C, paratype, NHMUK PI BZ 8363, Aubeterre Fm, rock face behind car-park, Aubeterre-sur-Dronne, Charente: A, part of the colony; B, group of autozooids with avicularia distal of the orifices; C, autozooid at the growing edge; D-E, holotype, NHMUK PI BZ 8809, Aubeterre Fm, Archiac, Charente-Maritime: D, part of the colony; E, three ovicellate autozooids lacking an associated avicularium, and one infertile autozooid (left) with an avicularium; F, paratype, NHMUK PI BZ 8655, Aubeterre Fm, roadcutting at junction of D5 and C18, east of Saint-Privat-des-Prés, Dordogne, orifice and avicularium. Scale bars: A, D, 500 μm; B, E, 200 μm; C, F, 100 μm.

FIG. 3 in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 3. — Dimorphomicropora voigti Ducasse & Vigneaux, 1960: A, lectotype, UB C.B.993 (Ducasse & Vigneaux 1960: fig. 1), probably Aubeterre Fm, Meschers, Charente-Maritime, branch with large polymorphic zooid near base; B, E, F, NHMUK PI BZ 8767, Aubeterre Fm, Pointe de Suzac, Meschers; B, branch; E, autozooids near base of branch; F, detail of an orifice; C, G, NHMUK PI BZ 8768, Aubeterre Fm, Pointe de Suzac, Meschers; C, branch with a large polymorphic zooid near the centre; G, detail of polymorph; D, paralectotype, UB C.B.994 (Ducasse & Vigneaux 1960: fig. 2), probably Aubeterre Fm, Meschers, Charente-Maritime; H, NHMUK PI BZ 8769, Aubeterre Fm, Pointe de Suzac, Meschers, Charente-Maritime, dilated branch with a cluster of ovicellate zooids. Scale bars: A, B, C, D, H, 500 μm; E, 200 μm; F, G, 100 μm.

FIG. 4 in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 4. — Dimorphomicropora crestulata (Ducasse, 1958): A, holotype (Ducasse 1958: pl. 7, fig. 3), UB C.B.917 Ducasse Collection, probably Barbezieux Fm (foram biozone CVI), RN 730, close to police station, Mirambeau, Charente-Maritime, dilated branch with ovicellate zooids; B, C, NHMUK PI BZ 8271, Aubeterre Fm, cliff north of town, Meschers, Charente-Maritime; B, well-preserved branch; C, detail of autozooids; D, NHMUK PI BZ 8272, Aubeterre Fm, cliff north of town, Meschers, branch. Scale bars: A, 500 μm; B, C, D, 200 μm.

FIG. 2. — Platelinella solea n. gen. et n in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 2. — Platelinella solea n. gen. et n. sp.: A-E, holotype, NHMUK PI BZ 8564, Biron Fm, Caillaud (north side), Talmont, Charente-Maritime: A, part of the colony; B, group of zooids; C, zooid with narrow distal opercular shelf; D, group of zooids, one with a slightly enlarged orifice (upper centre); E, broken zooid revealing two distal and two distolateral septular pores; F, paratype, NHMUK PI BZ 8848, Biron Fm, Caillaud (south side), Talmont, Charente-Maritime, group of zooids. Scale bars: A, 1 mm; B, D, F, 500 μm; C, E 100 μm.

Fig. 6 in New Late Cretaceous microvertebrate assemblage from the Campanian-Maastrichtian Williams Fork Formation, northwestern Colorado, USA, and its paleoenvironmental implications

Fig. 6. Representative reptile (A–C, E) and amphibian (D) teeth from the J&M site, Colorado, USA, Williams Fork Formation, Campanian–Maastrichtian, Upper Cretaceous. A–C. cf. Brachychampsa sp. A. MWC 9577, gracile morph tooth crown in lateral (A1) and occlusal (A2) views. B. MWC 9578, robust morph tooth crown in lateral (B1) and occlusal (B2) views. C. MWC 9579, robust morph tooth crown in lateral (C1) and occlusal (C2) views. D. Tetrapoda indet., MWC 8877, jaw fragment with teeth in lateral (D1) and occlusal (D2) views. E. Peneteius sp., MWC 8871, tooth crown with root in mesial (E1), lateral (E2), and occlusal (E3) views.

Fig. 8. Representative mammalian teeth from the J&M in New Late Cretaceous microvertebrate assemblage from the Campanian-Maastrichtian Williams Fork Formation, northwestern Colorado, USA, and its paleoenvironmental implications

Fig. 8. Representative mammalian teeth from the J&M site, Colorado, USA, Williams Fork Formation, Campanian–Maastrichtian, Upper Cretaceous. A. Meniscoessus sp., MWC 8848, incisor crown in labial (A1) and lingual (A1) views. B. Multituberculata indet., MWC 8863, tooth crown in occlusal (B1), lingual (B2), and distal (B3) views. C. cf. Cimolodon nitidus Marsh, 1889, MWC 8860, left p4 tooth crown in occlusal (C1), labial (C2), and lingual (C3) views. D.?Leptalestes cooki (Clemens, 1966), MWC 8859, tooth crown in occlusal (D1), labial (D2), and lingual (D3) views.

Fig. 3. Representative non-batoid chondrichthyans from the J&M in New Late Cretaceous microvertebrate assemblage from the Campanian-Maastrichtian Williams Fork Formation, northwestern Colorado, USA, and its paleoenvironmental implications

Fig. 3. Representative non-batoid chondrichthyans from the J&M site, Colorado, USA, Williams Fork Formation, Campanian–Maastrichtian, Upper Cretaceous. A–D. Lonchidion griffisi Case, 1987. A. MWC 8851, tooth crown in labial (A1) and occlusal (A2) views. B. MWC 9580, fragmentary tooth crown in labial (B1) and occlusal (B2) views. C. MWC 9581, fragmentary tooth crown in lingual (C1), labial (C2), and occlusal (C3) views. D. MWC 9582, fragmentary tooth crown in labial (D1) and occlusal (D2) views. E, F. Cantioscyllium markaguntensis Kirkland, Eaton, and Brinkman, 2013. E. MWC 8866, tooth crown in labial (E1) and occlusal (E2) views. F. MWC 9586, tooth crown in labial (F1) and lingual (F2) views. G, H. cf. Chilloscyllium sp. G. MWC 8850, morph 1 tooth crown in mesial (G1) and labial (G2) views. H. MWC 9576, morph 2 tooth crown in mesial (H1) and labial (H2) views. I . Hybodontoidea gen. et sp. indet., MWC 9800, dorsal fin spine in lateral view.

Fig. 5. Representative osteichthyan teeth from the J&M in New Late Cretaceous microvertebrate assemblage from the Campanian-Maastrichtian Williams Fork Formation, northwestern Colorado, USA, and its paleoenvironmental implications

Fig. 5. Representative osteichthyan teeth from the J&M site, Colorado, USA, Williams Fork Formation, Campanian–Maastrichtian, Upper Cretaceous. A, E. Paralbula casei Estes, 1969b. A. MWC 8855, tooth crown in occlusal (A1), basal (A2), and mesial (A3) views. E. MWC 8856, tooth crown in occlusal view. B. cf. Melvius sp., MWC 8867, tooth crown in labial view. C. Pycnodontiformes gen. et sp. indet., MWC 8873, tooth plate fragment in occlusal (C) view. D. Actinopterygii indet., MWC 8867, tooth crown in lateral (D) view. F. Dipnoi indet., MWC 8885, toothplate fragment in lateral view.

Fig. 7. Representative theropod dinosaur teeth from the J&M in New Late Cretaceous microvertebrate assemblage from the Campanian-Maastrichtian Williams Fork Formation, northwestern Colorado, USA, and its paleoenvironmental implications

Fig. 7. Representative theropod dinosaur teeth from the J&M site, Colorado, USA, Williams Fork Formation, Campanian–Maastrichtian, Upper Cretaceous. A. cf. Richardoestesia sp., MWC 8865, tooth crown in labial view (A1), mesial (A2) and distal (A3) serration detail views. B. Dromaeosauridae indet., MWC 8872, tooth crown fragment in lingual (B1), distal (B2) and mesial (B3) serration detail views. C. Hadrosauridae indet., MWC 8896, tooth crown in occlusal (C1) and lateral (C2) views.

Fig. 1 in New Late Cretaceous microvertebrate assemblage from the Campanian-Maastrichtian Williams Fork Formation, northwestern Colorado, USA, and its paleoenvironmental implications

Fig. 1. Index maps showing the location of the J&M site in northwestern Colorado. A. Shaded relief map of the western United States highlighting Colorado. B. The position of the study area in northwestern Colorado. C. Digital elevation model of the study area, star denotes location of the J&M site. Precise locality data on file at MWC (see text).

Fig. 3 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 3 Upper Cretaceous (middle Campanian) microfacies of sample GKL 39. Pa = Paracoskinolina klokovaensis n. sp., Pal = Paleodictyoconus senonicus Moullade & Viallard, Di = Dicyclina schlumbergeri Munier-Chalmas.

Fig. 6 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 6 Comparison of Paracoskinolina species with one horizontal partition in the marginal zone: a P. klokovaensis sp. nov., b P. reicheli Guillaume, 1956. c P. arcuata (Arnaud-Vanneau 1976). D = test diameter, H = test height, n = number of chambers per last 0.5 mm axial length, h = chamber height (all data except D/H in mm). * measured from original illustrations. Stratigraphy of the two Lower Cretaceous species according to Clavel et al. (2014).

Fig. 2 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 2 Upper Cretaceous successions of Klokova Mountain, SW Greece (see Fleury, 1970, fig. 1, for details) with the distribution of some benthic foraminifers (A-B: Senalveolina aubouini Fleury, sample GKL 43; C-D Accordiella conica Farinacci, sample GKL 43x, without scale). Note: the lower/middle Campanian boundary is approximately placed at the LAD of K. tergestina (Frijia et al., 2015, fig. 15). For microfacies of sample GKL 39 see Figure 3.

Fig. 1 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 1 Geographic sketch map showing the location of Klokova mountains on the opposite side of the Gulf of Corinth facing Patra. This is the type-locality of Paracoskinolina klokovaensis n. sp.

Fig. 4 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 4 Coskinolinidae (a, d, g, j) and Orbitolinidae (b-c, e-f, h-i, k-l) from the Campanian of Klokova Mountain SW Greece (a-f, h-l) and Brač Island, Croatia (g). Lepinoconus chiocchinii Cruz-Abad et al. a Oblique section. d Broken transverse section. g, j Subaxial sections. Paleodictyoconus senonicus Moullade & Viallard b, e Oblique transverse sections. c, f Subaxial sections. Calvezicionus lecalvezae Caus & Cornella. h, k Oblique sections. i Oblique section passing the biloculine, slightly inclined megalospheric embryo. Dictyoconella complanata Henson. l Oblique section in the plane of compression. Abbreviations: b = beam, de = deuteroconch, f = foramen, p = protoconch, pi = pillar, s = septum. Thin sections: GKL 43 (a, j, i, l), GKL 43x (d, k), GKL 39 (b-c, e, h), GKL 39x (f).

Fig. 7 in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 7 Central Mediterranean area (modified from Google Earth) with occurrences of Campanian Orbitolinidae-Coskinolinidae. 1: Zambetakis-Lekkas and Alexopoulos (2007) 2: Fleury (1970, 1980, this work) 3: Mount Biokovo (Sokač et al., 2012) 4: Brač Island (Gušić and Jelaska, 1990; CvetkoTešović et al., 2001) 5-7: Moro et al. (2016) 8: Luperto-Sinni (1976) 9: Frijia et al. (2015) 10: CruzAbad et al. (2017).

Fig. 5 Paracoskinolina klokovaensis n in Agglutinated Conical Foraminifera (Orbitolinidae, Coskinolinidae) From The Upper Cretaceous (Campanian) Of Greece, With Description Of Paracoskinolina Klokovaensis N. Sp.

Fig. 5 Paracoskinolina klokovaensis n. sp., from the late early-middle Campanian of Mount Klokova, SW Greece (a-f, h-j) and Brač Island, Croatia (g). a Axial section. b-c, f-g Subaxial sections. d Oblique transverse section. h Oblique section. i Tangential section. j Axial section, holotype specimen. Abbreviations: b = beam, f = foramen, ib = intercalary beam, pi = pillar, r = rafter. Thin sections: a GKL 39 (1754) (from Fleury, 1970, pl. 1, fig. 2), b-j GKL 39 (3357).