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Fig. 1 in Origin and significance of Late Cretaceous bioevents: Examples from the Cenomanian

Fig. 1. Palaeogeography of the study area on the NW European epicontinental shelf (map modified after Philip and Floquet 2000).

Fig. 5 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 5. Schematized parietals of centrosaurine ceratopsids in dorsal view, showing possible homologies for the first four epiparietal loci. A. Albertaceratops nesmoi Ryan, 2007. B. Spinops sternbergorum gen. et sp. nov. C. Centrosaurus apertus Lambe, 1902. D. Styracosaurus albertensis Lambe, 1913. E. Rubeosaurus ovatus Gilmore, 1930. F. Einiosaurus procurvicornus Sampson, 1995. Numbers indicate locus positions. For A and B, the numbers on the right side of the parietal indicate numbering under the "traditional" scheme; numbers on the left side indicate numbering under the revised scheme proposed here. Locus numbering is the same in both the traditional and revised schemes for C, D, E, and F, and are thus presented only on the left side of the parietal for those taxa. Not to scale.

Fig. 4 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 4. Partial skull of the centrosaurine ceratopsid Spinops sternbergorum gen. et sp. nov. from the Campanian of Dinosaur Provincial Park, southern Alberta, NHMUK R16306; in right lateral (A), rostral (B), and dorsal (C) views.

Fig. 3 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 3. Centrosaurine ceratopsid Spinops sternbergorum gen. et sp. nov. from the Campanian of Dinosaur Provincial Park, southern Alberta. A. Partial right squamosal in lateral view, NHMUK R16309. B. Partial parietal with adherent bone fragments in dorsal view, NHMUK R16308. C. Partial parietal in dorsal (C1), rostral (C2), and left lateral (C3) views, holotype NHMUK R16307.

Fig. 1 in A new centrosaurine from the Late Cretaceous of Alberta, Canada, and the evolution of parietal ornamentation in horned dinosaurs

Fig. 1. Map showing the presumed location of the Spinops sternbergorum gen. et sp. nov. type locality within the area informally called the "Steveville badlands," Dinosaur Provincial Park, Alberta Canada. Charles Sternberg (unpublished data in NHMUK archives) indicated that the bone bed was one mile below the mouth of Berry Creek, and the estimated area that this covers is indicated by the grey semi−circle. Intense prospecting on the east side of the river has failed to relocate the quarry, and badlands on the west side are outside of the Park boundary and currently inaccessible for prospecting. The indicated southeast Park boundary does not include the margins of two major coulees in this region that are also within the Park. Note that the quarry for the holotype of Styracosaurus albertensis Lambe, 1913 (CMN 344) is in the southeast part of the Park. The inset photograph, courtesy of David Eberth, shows a typical view of the contact between the Dinosaur Park Formation (DPF) and Oldman Formation (OF) near the Steveville badlands.

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Fig. 3 in Ammonite faunal dynamics across bio-events during the mid- and Late Cretaceous along the Russian Pacific coast

Fig. 3. Changes in the number of Cretaceous ammonite species from Far East Russia, arranged in the ten most speciose families: non−heteromorphs (Phylloceratidae, Tetragonitidae, Gaudryceratidae, Pachydiscidae, Kossmaticeratidae) and heteromorphs (Scaphitidae, Baculitidae, Turrilitidae, Nostoceratidae, Diplomoceratidae). Abbreviations: low., lower; mid., middle; up., upper.

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Fig. 4 in Ammonite faunal dynamics across bio-events during the mid- and Late Cretaceous along the Russian Pacific coast

Fig. 4. Regional bio−events recorded in ammonite assemblages from Far East Russian regions (present paper); regional palaeotemperature curves modified after Zakharov et al. (1998, 1999, 2005); generalised scheme of records of transgression and regression from Sakhalin and northeast Russia; global bio−events (Kauffmann and Hart 1995); global sea level curves by Haq et al. (1987); global palaeotemperature curves by Skelton (2003). Stages are shown without calibration to absolute time. Abbreviations: C–T, Cenomanian–Turonian boundary; Cr–Pg, Cretaceous Paleogene boundary; OAE, Oxygen Anoxic Event.

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Fig. 3 in A new eutherian mammal from the Late Cretaceous of Kazakhstan

Fig. 3. Strict consensus of the two most parsimonious trees (CI = 0.25, RI = 0.55) based on the dataset of Wible et al. (2009), as modified by Archibald and Averianov (2012), and including Zhalmouzia Averianov and Archibald gen. nov. The tree has been pruned to focus on the relationships of Zhalmouzia Averianov and Archibald gen. nov. and closely related taxa Numbers above and below nodes represent characters and character states, respectively. Only unambiguous synapomorphies are shown. Note that all of the characters are homoplastic, i.e., parallelisms or reversals. For further details see SOM: Sup- plementary Online Material available at http://app.pan.pl/SOM/app59-Averianov_etal_SOM.pdf.

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Fig. 1 in A new eutherian mammal from the Late Cretaceous of Kazakhstan

Fig. 1. Maps of the Late Cretaceous locality of Shakh Shakh in Kazakhstan. A. Northeast Aral Sea area with the position of the Shakh Shakh locality marked by an asterisk (modified from Averianov 2007b). B. Locality map (I, Shakh Shakh 1; II, Shakh Shakh 2) from Rozhdestvensky (1964: fig. 1) and Suslov (1982: fig. 1), superimposed on a Google Earth image of the area; the red beds of the Bostobe Formation are clearly visible on the photograph. C. Vertebrate localities in this area based on Malakhov et al. 2009: fig. 5); 1, Shakh-Shakh 2; 2, Shakh-Shakh 1; 3, Bird Site; 4, Turtle Site; 5, Forest; 6, Forest 2; 7, Shakh Shakh 3.

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Fig. 2 in A new eutherian mammal from the Late Cretaceous of Kazakhstan

Fig. 2. Eutherian mammals from Shakh Shakh, Kazakhstan, Late Cretaceous. A. Zhalmouzia bazhanovi Averianov and Archibald gen. et sp. nov., ZIN 100639, holotype, left dentary fragment with m2–3 in situ and alveoli for c, p1–5 and m1, in labial (A1), occlusal (A2, stereopair), and lingual (A3) views. B. Beleutinus orlovi Bazhanov, 1972, IZK I-751/III-1962, holotype, heavily abraded right m1–3 in labial view (modified from Nesov et al. 2004: pl. 1: 1a).

Fig. 8 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 8. Single most parsimonious tree derived from maximum parsimony analysis of 49 hadrosauroid species, highlighting the position of Saurolophus morrisi sp. nov. within saurolophine hadrosaurids. Numbers above the branches indicate decay indices (Bremer support), whereas those below indicate bootstrap frequencies. Lambeeosaurinae is collapsed into a single branch for clarity; lambeosaurine interrelationships recovered were identical to those in Fig. 7.

Fig. 1 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 1. Partial right postorbital of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2852), lower Maastrichtian Moreno Formation of San Benito County, California, USA, showing the autapomorphic ornamentation of its jugal process. Posterior (A) and right lateral (B) views.

Fig. 5 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 5. Appendicular elements of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2760, a subadult), lower Maastrichtian Moreno Formation of Panoche Hills, Fresno County, California, USA. A. Partial left scapula and coracoid in lateral view. B. Partially articulated forelimb elements. C. Proximal segment of right tibia in lateral view. D. Distal fragments of femora. E. Right metatarsal III in dorsal view.

Fig. 3 in Late Cretaceous gastropod egg capsules from the Netherlands preserved by bioimmuration

Fig. 3. Plot of measurements of Late Cretaceous and selected Recent neritid egg capsules (data from Kano and Fukumori 2010).

Fig. 2. A, B in Late Cretaceous gastropod egg capsules from the Netherlands preserved by bioimmuration

Fig. 2. A, B. Late Cretaceous gastropod egg capsules from the late Maastrichtian (Late Cretaceous) of Maastricht, the Netherlands, preserved by bioimmuration (NHMM JJ 13778). A. Aggregate of bioimmured egg capsules, probably the capsule bases, with an eroded basal wall of a cheilostome bryozoan colony, showing the zooid interiors (arrowed) (A1). Close−up view of the egg capsules shown in the centre of A1, with clearly visible outlines of cheilostome zooids within and around the egg capsules, shown by dotted lines (A2). B. Aggregate of presumably unhatched (left) and hatched, in a form of bases (right), egg capsules (B1). The arrow points to the eroded basal wall of a bioimmuring cheilostome bryozoan colony. Close−up views of presumably hatched (B2) and unhatched (B3) egg capsules shown in B1. C. Hatched and unhatched egg capsules of the Recent neritid gastropod species Neritina iris Mousson, 1849, on the shell exterior of a live gastropod Septaria porcellana (Linné, 1758), Kagoshima Bay, Japan (photograph courtesy of Yasunori Kano). Scale bars: A1, B1 1 mm; A2, B2, B3 200 µm; C 5 mm.

Fig. 3 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 3. Right posterolateral view of the frontal of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2760, a subadult), lower Maastrichtian Moreno Formation of Panoche Hills, Fresno County, California, USA, showing the eroded remnant of the buttressing base of the posterodorsal frontal ramus.

Fig. 7 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 7. Strict consensus tree of the three most parsimonious trees derived from maximum parsimony analysis of 49 hadrosauroid species. LACM/CIT 2760 and 2852 were coded as separate OTUs and their position within Saurolophinae in highlighted in the cladogram. Numbers above the branches indicate decay indices (Bremer support), whereas those below indicate bootstrap frequencies.

Fig. 9 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 9. Comparison of the general skull and premaxillary morphology of two hadrosaurid dinosaurs Saurolophus osborni Brown, 1912, holotype AMNH 5220 (A) and Saurolophus morrisi sp. nov., holotype LACM/CIT 2852 (B), highlighting characters shared by these two taxa. Skull in right lateral view (A1, B1), right premaxilla in lateral view (A2, B2).The white inscription on the premaxilla denote the abbreviation for that bone, painted by the curatorial staff back in the early twentieth century.

Fig. 6 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 6. Appendicular elements of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2852), lower Maastrichtian Moreno Formation of San Benito County, California, USA. A. Partial right scapula in lateral view. B. Right ulna in lateral view and possible manual phalanx II−1 in dorsal view. C. Right metatarsal III in dorsal (C1) and lateral (C2) views.

Fig. 2 in A new species of saurolophine hadrosaurid dinosaur from the Late Cretaceous of the Pacific coast of North America

Fig. 2. Partial skull roof of a hadrosaurid dinosaur Saurolophus morrisi sp. nov. (LACM/CIT 2760, a subadult), lower Maastrichtian Moreno Formation of Panoche Hills, Fresno County, California, USA. Dorsal (A) and ventral (B) views. Photographs (A1, B1) and interpretative drawings (A2, B2).