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FIGURE 8 in A fossil locality predictive model using weighted suitability analysis for the Early Cretaceous Cedar Mountain Formation, Utah, USA
FIGURE 8. Number of cells assigned to each fossil potential value for the model. TABLE 6. Reclassified values for OLI/TIRS bands for revised model.
FIGURE 5 in A fossil locality predictive model using weighted suitability analysis for the Early Cretaceous Cedar Mountain Formation, Utah, USA
FIGURE 5. Differences of means between fossil localities and Cedar Mountain Formation (X1-X2). TABLE 3. Reclassified values for OLI/TIRS bands used in weighted suitability analysis.
FIGURE 1 in A fossil locality predictive model using weighted suitability analysis for the Early Cretaceous Cedar Mountain Formation, Utah, USA
FIGURE 1. Early Cretaceous Cedar Mountain Formation surface exposure, elevation, and fossil localities.
FIGURE 11 in A fossil locality predictive model using weighted suitability analysis for the Early Cretaceous Cedar Mountain Formation, Utah, USA
FIGURE 11. Comparison of aspects between the entire Cedar Mountain Formation and BYU fossil localities.
Fig. 9 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 9. Scapulocoracoids and scapulae of sauropod dinosaurs, scaled to same length of scapular blade from posterior point of glenoid to posterior margin of blade. A. Mamenchisaurus youngi Young and Zhao, 1972, holotype ZDM0083, left scapulocoracoid, modified from Ouyang and Ye (2002: fig. 22). B. Diplodocus longus Hatcher, 1901, USNM 10865, right scapulocoracoid reversed, photograph by MPT. C. Camarasaurus supremus Cope, 1877, AMNH 5761 Sc. 1, left scapula, and AMNH 5761 Cor. 1, left coracoid, probably associated, modified from Osborn and Mook (1921: figs. 75, 81a). D. Giraffatitan brancai (Janensch, 1914), HMN Sa 9, left scapula, modified from Janensch (1961: pl. 15: 1). E. Rapetosaurus krausi Curry Rogers and Forster, 2001, holotype FMNH PR 2209, right scapula reversed, modified from Curry Rogers (2009: fig. 32). F. Brontomerus mcintoshi gen. et sp. nov. OMNH 27761, left scapula, tentatively reconstructed after Giraffatitan brancai.
Fig. 5 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 5. Damaged presacral vertebra of the camarasauromorph sauropod Brontomerus mcintoshi gen. et sp. nov. from the Lower Cretaceous Cedar Mountain Formation of Utah, OMNH 66429, in dorsal view, as photograph (A) and interpretive drawing (B). Shading indicates air spaces.
Fig. 7 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 7. First right dorsal rib of the camarasauromorph sauropod Brontomerus mcintoshi gen. et sp. nov. from the Lower Cretaceous Cedar Mountain Formation of Utah, OMNH 27766 in posterior view: head of rib, showing pneumatic invasion of shaft (A) and complete rib, showing laterally directed curvature of shaft (B).
Fig. 2 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 2. Left ilium of the camarasauromorph sauropod Brontomerus mcintoshi gen. et sp. nov. from the Lower Cretaceous Cedar Mountain Formation of Utah, type specimen OMNH 66430 in lateral view reconstructed from the three fragments (A), and ventral view (B).
Fig. 3 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 3. Ilia of sauropod dinosaurs, scaled to same total length. A. Mamenchisaurus hochuanensis Young and Zhao, 1972, holotype CCG V 20401, right ilium reversed, modified from Young and Zhao (1972: pl. 6: 1a). B. Diplodocus carnegii Hatcher, 1901, CM 94, right ilium reversed, modified from Hatcher (1901: pl. 10: 1). C. Camarasaurus supremus Cope, 1877, AMNH 5761 Il. 1, left ilium, modified from Osborn and Mook (1921: fig. 87). D. Giraffatitan brancai (Janensch, 1914), HMN J1, left ilium, modified from Janensch (1961: pl. E: 2). E. Rapetosaurus krausi Curry Rogers and Forster, 2001, holotype FMNH PR 2209, left ilium, modified from Curry Rogers (2009: fig. 39B). F. Brontomerus mcintoshi gen. et sp. nov. holotype OMNH 66430, left ilium.
Fig. 6 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 6. Mid−caudal vertebra of the camarasauromorph sauropod Brontomerus mcintoshi gen. et sp. nov. from the Lower Cretaceous Cedar Mountain Formation of Utah, OMNH 61248 in dorsal (A), anterior (B), left lateral (C), posterior (D), and ventral (E) views.
Fig. 4 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 4. Measurement protocol for sauropod ilia as illustrated in Fig. 3 and shown in Table 4. Total length is measured along the longest axis of the ilium; lengths of preacetabular and postacetabular lobes are measured parallel to this axis, and extend from the extremity of the lobe to the anterior margin of the pubic peduncle and posterior margin of the ischiadic peduncle respectively. Supracetabular height is measured perpendicular to the longest axis, and extends from the highest point of the acetabulum to the point level with the highest part of the ilium.
Fig. 1 in A new sauropod dinosaur from the Lower Cretaceous Cedar Mountain Formation, Utah, USA
Fig. 1. Skeletal inventory of the camarasauromorph sauropod Brontomerus mcintoshi gen. et sp. nov. from the Lower Cretaceous Cedar Mountain Formation of Utah, in left lateral view. Preserved elements are white, missing elements are reconstructed in gray. After a Camarasaurus grandis reconstruction kindly provided by Scott Hartman.
Fig. 5 in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 5. Radiodontan euarthropod Stanleycaris hirpex Caron, Gaines, Mángano, Streng, and Daley, 2010 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada. A. ROM 59975 (paratype). B. ROM 59976 (paratype). Abbreviation: Pn, podomere n.
Fig. 4. Lobopodian Aysheaia pedunculata Walcott, 1911, USNM 365608 in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 4. Lobopodian Aysheaia pedunculata Walcott, 1911, USNM 365608 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada; in cross-polarized light (A), cross-polarized light, red and yellow channels reduced (B).
Fig. 3 in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 3. Comparison between terminal spines and vetral blades of Stanleycaris and oral papillae and lobopodous limbs of Aysheaia. A. Stanleycaris sp., KUMIP 153923 from the Wheeler Formation (Cambrian Series 3, Drumian), Utah, USA; anterior end showing recurved terminal spines (A1), ventral blade (A2). B. Aysheaia pedunculata Walcott, 1911, USNM 189199 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada; anterior end showing anterior appendages and oral papillae. C, D. Stanleycaris hirpex Caron, Gaines, Mángano, Streng, and Daley, 2010 from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada. C. ROM 59975 (paratype), ventral blade. D. USNM 83942, trunk section and lobopods. Abbreviation: Pn, podomere n.
Fig. 1. A in Aysheaia prolata from the Utah Wheeler Formation (Drumian, Cambrian) is a frontal appendage of the radiodontan Stanleycaris
Fig. 1. A. Radiodontan euarthropod Stanleycaris sp., KUMIP 153923 from the Wheeler Formation (Cambrian Series 3, Drumian), Utah, USA; non-polarized light (A1), cross-polarized light, red and yellow channels reduced (A2), cross polarized light (A3), cross-polarized light, red and yellow channels enhanced (A4). B. Stanleycaris hirpex Caron, Gaines, Mángano, Streng, and Daley, 2010, ROM 59944 (holotype) from the Stephen Formation (Cambrian Series 3, Stage 5), British Columbia, Canada; cross-polarized light (B1), black and white (B2). dorsal spines the anterior end, as also observed in in Stanleycaris hirpex (compare Fig. 3A2 and 3C). The ventral blades lack compaction wrinkles often preserved on limbs of A. pedunculata P1 P7 P11 P4 (Figs. 3D, 4; Ma et al. 2014: fig. 5B). The terminal spines at the anterior end of the specimen are short, recurved, and terminal P1 spines have a sharp termination. This morphology is similar to that of the spines in S. hirpex, and quite unlike the straight and sediment less robust oral papillae of A. pedunculata (compare Fig. 3A1 layer auxiliary spines and 3B). It should be noted that Robison (1985) studied the 5 mm ventral blades specimen before the extent of radiodontan frontal appendage Fig. 2. Explanatory drawing of radiodontan euarthropod Stanleycaris morphological diversity was known (e.g., Daley and Budd sp., KUMIP 153923 from the Wheeler Formation (Cambrian Series 3, 2010; Caron et al. 2010), and so lacked the appropriate con- Drumian), Utah, USA. Hachure direction indicates lower sediment level. text for correctly interpreting KUMIP 153923. Dotted lines indicate expected path of incomplete ventral blades.
Fig. 3 in A new occurrence of Dakotasuchus kingi from the Late Cretaceous of Utah, USA, and the diagnostic utility of postcranial characters in Crocodyliformes
Fig. 3. Comparative morphology of coracoids (A–D) and dorsal scutes E–H) in coelognathosuchians from the medial Cretaceous of North America. Right coracoids in lateral view and right dorsal scutes in ventral view. A, E. Dakotasuchus kingi Mehl, 1941, OMNH 34500, Mussentuchit Member of the Cedar Mountain Formation (Cenomanian), Utah, USA. B, F. Dakotasuchus kingi Mehl, 1941, KWU uncatalogued (holotype), Dakota Formation (Cenomanian), Kansas, USA. C, G. Woodbinesuchus byersmauricei Lee, 1997, SMU 74626 (holotype), Woodbine Formation Cenomanian), Texas, USA. D, H. Terminonaris robusta Wu, Russell, and Cumbaa, 2001, SMNH P2411.1 (coracoid is inverted), Keld Member of the Favel Formation (Turonian), Saskatchewan, Canada. Images modified from Mehl (1941), Lee (1997), and Wu et al. (2001). Images are not to scale.
Fig. 2. Representative elements ofgoniopholidid crocodyliform Dakotasuchus kingi Mehl, 1941, OMNH 34500 from OMNH locality V828 in A new occurrence of Dakotasuchus kingi from the Late Cretaceous of Utah, USA, and the diagnostic utility of postcranial characters in Crocodyliformes
Fig. 2. Representative elements ofgoniopholidid crocodyliform Dakotasuchus kingi Mehl, 1941, OMNH 34500 from OMNH locality V828, Mussentuchit Member, Cedar Mountain Formation, Cenomanian. A. Right cervical rib in ventral (A1) and dorsal (A2) views. B. Right coracoid in lateral (B1), caudal (B2), and medial (B3) views. C. Dorsal vertebra in cranial (C1), caudal (C2), lateral (C3), and dorsal (C4) views. D. Right radius in medial (D1) and lateral (D2) views. E. Dorsal scute in dorsal (E1) and ventral (E2) views. F. Ventral scute in dorsal (F1) and ventral (F2) views. G. Close-up views of neural canal in dorsal vertebrae, illustrating distinctive heart shape (white arrows); G1, OMNH 34500 vertebra in caudal view; G2, D. kingi holotype vertebra mold in cranial view. H. Tooth in labiolingual (H1), basal (H2), and mesiodistal (H3) views.
Fig. 1 in A new occurrence of Dakotasuchus kingi from the Late Cretaceous of Utah, USA, and the diagnostic utility of postcranial characters in Crocodyliformes
Fig. 1. Map of the western United States (A) with the approximate locations of the holotype in Salina, Kansas (KWU uncatalogued; circle) and referred specimen in Emery County, Utah (OMNH 34500; star) and map of Emery County (B) with the approximate location of V868 (star) and the distribution of the Mussentuchit Member (grey area) (modified from Cifelli et al. 1999).
Fig. 17 in Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery
Fig. 17. Comprehensive model of the Spathian (Lower Triassic) Virgin Formation as recorded in south−western Utah. A. Distribution of sedimentary facies and faunal assemblages. B. Diversity gradient along the general environmental gradient.
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