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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. 13 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 13. Palaeogeographic distribution of the reef-building laminar stromatoporoid genera during the Givetian and Frasnian (Middle–Late Devonian). Localities: 1, Northwest Territories, Canada (MacNeil and Jones 2016); 2, Dinant Basin, southern Belgium (Da Silva et al. 2011a, b); 3, Anti‐Atlas, Morocco (Jakubowicz et al. 2019); 4, Esfahan, central Iran (Mistiaen and Gholamalian 2000); 5, Guizhou, South China; 6, Canning Basin, western Australia (Cockbain 1984); 7, Queensland, eastern Australia (Cook 1999). Palaeogeographic map is based on Golonka (2002).
Fig. 2 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 2. Field photographs of the Jiwozhai reef. A. A panoramic view of the whole reef unit, with a white rectangle indicating the studied area. Note the reverse fault in the east. B. A general view shows the studied area of the reef unit. C. Enlarged field photo of the reef fragment marked in B, showing the thick or thin laminar stromatoporoids (undulating dashed line) covered on branching tabulate corals (triangles), solitary rugose corals (crosses), dendroid stromatoporoids (squares), bulbous stromatoporoid (circled line), and clay-rich micrites (fine grained sediments between the metazoan skeletons). D. An example of polished block of the Jiwozhai reef limestone showing toppled dendroid or laminar Stachyodes fasciculata Dong in Dong et al., 1989, and encrusting Stictostroma saginatum (Lecompte, 1951) in the upper area. Note the conspicuous digitation of mamelons of Stictostroma saginatum (Lecompte, 1951) in the lower right corner. Sti, Stictostroma saginatum (Lecompte, 1951); Sta, Stachyodes fasciculata Dong in Dong et al., 1989; Tha, Thamnopora cf. pansiensis Tchi, 1966.
Fig. 11 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 11. Stromatoporoid Stachyodes fasciculata Dong in Dong et al., 1989, from the Jiwozhai reef, Jiwozhai Member, Dushan Formation, Givetian, Middle Devonian; Dushan, Guizhou, South China. A. NIGP 177060; longitudinal section and tangential section of the dendroid form. B. NIGP 177061; longitudinal section showing the thick pachysteles and thin pachystromes. C. NIGP 177062; C1, longitudinal section of the bulbous form; C2, enlargement of C1, illustrating regular skeleton; C3, tangential section showing the autotubes and astrorhizal canals; C4, enlargement of C2, showing the coarsely striated microstructure (arrow).
Fig. 9 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 9. Stromatoporoids from the Jiwozhai reef, Jiwozhai Member, Dushan Formation, Givetian, Middle Devonian; Dushan, Guizhou, South China. A, B.?Habrostroma laminosum (Lecompte, 1952) A. NIGP 177055; longitudinal section of the laminar form; B. NIGP 177056; B1, longitudinal section of the high domical form; B2, poor preservation of tangential section showing the dense structure; B3, enlargement of B1, showing possible microreticulate microstructure (arrow). C. Parallelopora sp., NIGP 177057; C1, longitudinal section, note the microreticulate microstructure; C2, tangential section showing the autotubes.
Fig. 5. Stromatoporoid Gerronostromaria grossum Dong, 1974, NIGP 177047 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 5. Stromatoporoid Gerronostromaria grossum Dong, 1974, NIGP 177047, from the Jiwozhai reef, Jiwozhai Member, Dushan Formation, Givetian, Middle Devonian; Dushan, Guizhou, South China. A1, longitudinal section, note the well differentiated network constructed by thin laminae and pillars; A2, tangential section showing the distinct mamelons; A3, enlargement of A1, illustrating the common occurrence of the diagenetic "clinoreticular" microstructure inside the continuous pillars; A4, enlargement of A2, showing the isolated pillars.
Fig. 1 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 1. Location and stratigraphy of the Jiwozhai reef in Dushan County, Guizhou, South China. A. Map showing southern Guizhou and northern Guangxi and the studied area in China. B. Locality of the Jiwozhai reef in Dushan County. C. Depositional successions and fossil assemblages of the supposed uppermost Eifelian to lowermost Frasnian in Dushan, Guizhou province (modified after Liao et al. 1979; Liao 2003). Abbreviations: Ei, Eifelian; Fr., Frasnian.
Fig. 2 in Palaeobiogeographical implications of the first fossil wood flora from the Jurassic of Turkey
Fig. 2. Generalized columnar section of the studied regions (Gümüşhane section modified from Vincent et al. 2018; Olur-Oltu section modified from Konak and Hakyemez 2008 and Kara-Gülbay et al. 2018). Abbreviations: DUT, Dutlu village of the city of Oltu in the province of Erzurum, Turkey; GED, the site of Edire in the province of Gümüşhane, Turkey; GUM, the Beyçam district of the province of Gümüşhane, Turkey; YES, Yeşilbağlar village of the city of Oltu in the province of Erzurum, Turkey. Triassic rocks are not observed in the Eastern Sakarya zone. So we left this section blank in the figure.
Fig. 4 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 4. Pie charts illustrating palaeoecological parameters of the stromatoporiod fauna. A. External morphology. B. Thickness. C. Substrate types. D. Thickness of growth interruption. Abbreviations: Ger, Gerronostromaria grossum Dong, 1974; Cla, Clathrocoilona spissa (Lecompte, 1951);?Hab, Habrostroma laminosum (Lecompte, 1952); Par, Parallelopora sp.; Pse, Pseudotrupetostroma porosum (Yang and Dong, 1979); Sal, Salairella buecheliensis (Bargatzky, 1881); Sta, Stachyodes sp.; Stac, Stachyodes costulata Lecompte, 1952; Staf, Stachyodes fasciculata Dong in Dong et al., 1989; Sti, Stictostroma saginatum (Lecompte, 1951); Syn, Synthetostroma actinostromoides Lecompte, 1951.
Fig. 4 in Palaeobiogeographical implications of the first fossil wood flora from the Jurassic of Turkey
Fig. 4. Araucariacean wood sections of Agathoxylon sp. type 1 (ISTO-FW-00217) from Jurassic of the Beycam locality of the province of Gümüshane, Turkey. A1–A3, uni- to triseriate of intertracheary radial pits; A4, A5, predominantly araucariod type cross-field pits.
Fig. 3 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 3. Schematic vertical section of stromatoporoids in the Jiwozhai reef (Huang et al. 2020) showing the spatial distribution of different stromatoporoids, note the predominance of the Gerronostromaria grossum Dong, 1974, in the laminar form stromatoporoids. 1, Gerronostromaria grossum Dong, 1974; 2, Clathrocoilona spissa (Lecompte, 1951); 3,?Habrostroma laminosum (Lecompte, 1952); 4, Parallelopora sp.; 5, Pseudotrupetostroma porosum (Yang and Dong, 1979); 6, Salairella buecheliensis (Bargatzky, 1881); 7, Stachyodes costulata Lecompte, 1952; 8, Stachyodes fasciculata Dong in Dong et al., 1989; 9, Stachyodes sp.; 10, Stictostroma saginatum (Lecompte, 1951); 11, Synthetostroma actinostromoides Lecompte, 1951. Black, stromatoporoids; gray, other organisms between stromatoporoids.
Fig. 1. A in Palaeobiogeographical implications of the first fossil wood flora from the Jurassic of Turkey
Fig. 1. A. Geographic location (inset) and regional tectonic setting of Turkey (after Okay and Tüysüz 1999). B, C. Simplified geological map of the Gümüşhane region (B, after Kandemir 2004), the Olur-Oltu region (C, after Konak and Hakyemez 2008) and location of the Jurassic wood sites.
Fig. 12 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 12. Stromatoporoid Stachyodes sp. NIGP 177063, from the Jiwozhai reef, Jiwozhai Member, Dushan Formation, Givetian, Middle Devonian; Dushan, Guizhou, South China. A1, longitudinal section; A2, tangential section, note the autotubes and conspicuous astrorhizal canals; A3, enlargement of A1, note the coarsely striated microstructure (arrow); A4, enlargement of the upper middle part of A2, note the probably striated microstructure (arrow); A5, enlargement of the lower left part of A2, note the black dots in the tangential section.
Fig. 8 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 8. Stromatoporoids from the Jiwozhai reef, Jiwozhai Member, Dushan Formation, Givetian, Middle Devonian; Dushan, Guizhou, South China. A. Pseudotrupetostroma porosum (Yang and Dong, 1979), NIGP 177053; A1, longitudinal section; A2, tangential section; A3, enlargement of longitudinal section showing coarsely cellular microstructure coated tangential elements (arrows). B. Salairella buecheliensis (Bargatzky, 1881), NIGP 177054; B1, longitudinal section, note the predominance of the pachysteles in the right standard area and amalgamated structure in the left oblique orientation of the thin section; B2, tangential section, note the autotubes in the upper middle area; B3, enlargement of B1 showing coarsely cellular microstructure (arrows) partially transformed into melanospheric microstructure; such features demonstrate the likely diagenetic character of these microstructures and therefore their unreliability as taxonomic discriminators.
Fig. 7 in Stromatoporoids from a Middle Devonian reef in South China and their palaeoecological implication
Fig. 7. Stromatoporoids from the Jiwozhai reef, Jiwozhai Member, Dushan Formation, Givetian, Middle Devonian; Dushan, Guizhou, South China. A, B. Stictostroma saginatum (Lecompte, 1951) A. NIGP 177050; A1, tangential section showing the isolated pillars and locally irregular skeleton; A2, longitudinal section, note the prominently vertically erected mamelon; A3, enlargement of A2, note the coarsely ordinicellular microstructure (arrows). B. NIGP 177051; longitudinal section, note the encrusting skeleton over Thamnopora sp. debris and a solitary rugose coral. C. Synthetostroma actinostromoides Lecompte, 1951, NIGP 177052; C1, longitudinal section; C2, tangential section.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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