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Fig. 1. Adult Saurolophus skulls compared. A. Saurolophus angustirostris Rozhdestvensky, 1952 in Cranial osteology and ontogeny of Saurolophus angustirostris from the Late Cretaceous of Mongolia with comments on Saurolophus osborni from Canada
Fig. 1. Adult Saurolophus skulls compared. A. Saurolophus angustirostris Rozhdestvensky, 1952, based on MPC 100/706, late Campanian–?Maastrichtian Nemegt Formation, Mongolia; in lateral (A1), posterior (A2), and dorsal (A3) view. Skull roof with crest removed as denoted by cross−hatching (A4). B. Skull of Saurolophus osborni Brown, 1912, AMNH 5220, Maastrichtian Horseshoe Canyon Formation, Alberta, Canada; in lateral view. Dashed lines imply inferred margins.
Fig. 11 in Cranial osteology and ontogeny of Saurolophus angustirostris from the Late Cretaceous of Mongolia with comments on Saurolophus osborni from Canada
Fig. 11. Strict consensus tree showing the phylogenetic position of Saurolophus angustirostris Rozhdestvensky, 1952. RI = 0.87, CI = 0.84, and RCI = 0.74. Values at the base of nodes refer to bootstrap and decay indices, respectively.
Fig. 10 in Cranial osteology and ontogeny of Saurolophus angustirostris from the Late Cretaceous of Mongolia with comments on Saurolophus osborni from Canada
Fig. 10. Partial sclerotic ring within right orbit of hadrosaurid dinosaur Saurolophus angustirostris Rozhdestvensky, 1952, PIN 551/8, late Campanian–?Maastrichtian Nemegt Formation, Mongolia. Photograph (A), explanatory drawing (B). Grey regions in B denote matrix. Dorsal is up.
Fig. 6 in Cranial osteology and ontogeny of Saurolophus angustirostris from the Late Cretaceous of Mongolia with comments on Saurolophus osborni from Canada
Fig. 6. Dorsal oblique view of juvenile Saurolophus angustirostris Rozhdestvensky, 1952, ZPAL MgD−1/159, late Campanian–?Maastrichtian Nemegt Formation, Mongolia; skull roof. Photograph (A) and explanatory drawing (B). Shading indicates matrix.
Fig. 12 in Cranial osteology and ontogeny of Saurolophus angustirostris from the Late Cretaceous of Mongolia with comments on Saurolophus osborni from Canada
Fig. 12. Ontogenetic series of Saurolophus angustirostris Rozhdestvensky, 1952 skulls (late Campanian–?Maastrichtian Nemegt Formation, Mongolia) with associated neurocranial (and select dermatocranial) changes. Specimens are placed on the scale bar as a percentage of length of the largest specimen. Specimens are to scale.
Fig. 5 in Cranial osteology and ontogeny of Saurolophus angustirostris from the Late Cretaceous of Mongolia with comments on Saurolophus osborni from Canada
Fig. 5. Comparison of quadrates of Saurolophus in lateral view. A. Right quadrate of Saurolophus angustirostris Rozhdestvensky, 1952, ZPAL MgD−1/163, late Campanian–?Maastrichtian Nemegt Formation, Mongolia. B. Left quadrate of Saurolophus osborni Brown, 1912, AMNH 5220, Maastrichtian Horseshoe Canyon Formation, Alberta, Canada; modified from Bell (2011). Grey regions indicate broken surfaces. Dorsal is up.
Fig. 9 in Cranial osteology and ontogeny of Saurolophus angustirostris from the Late Cretaceous of Mongolia with comments on Saurolophus osborni from Canada
Fig. 9. Right dentary of hadrosaurid dinosaur Saurolophus angustirostris Rozhdestvensky, 1952, PIN 551/407, late Campanian–?Maastrichtian Nemegt Formation, Mongolia. A. Right dentary in lingual view. B. Explanatory drawing of the same. C. Lingual view of dentary teeth from the middle of the tooth row.
Fig. 6 in Braincase anatomy of the titanosaurian sauropod Lirainosaurus astibiae from the Late Cretaceous of the Iberian Peninsula
Fig. 6. The titanosaurian sauropod Lirainosaurus astibiae Sanz, Powell, Le Loeuff, Martínez, and Pereda Suberbiola, 1999 from the Late Cretaceous of Laño (northern Spain), referred braincase (MCNA 13913). Stereopairs in right lateral view.
Fig. 7 in Braincase anatomy of the titanosaurian sauropod Lirainosaurus astibiae from the Late Cretaceous of the Iberian Peninsula
Fig. 7. The titanosaurian sauropod Lirainosaurus astibiae Sanz, Powell, Le Loeuff, Martínez, and Pereda Suberbiola, 1999 from the Late Cretaceous of Laño (northern Spain), referred braincase (MCNA 13913). Interpretive photographs in dorsal (A), ventral (B) and posterior (C) views.
Fig. 5 in Braincase anatomy of the titanosaurian sauropod Lirainosaurus astibiae from the Late Cretaceous of the Iberian Peninsula
Fig. 5. The titanosaurian sauropod Lirainosaurus astibiae Sanz, Powell, Le Loeuff, Martínez, and Pereda Suberbiola, 1999 from the Late Cretaceous of Laño (northern Spain), referred braincase (MCNA 13913). Stereopairs in posterior (A) and anterior (B) views.
Fig. 4 in Braincase anatomy of the titanosaurian sauropod Lirainosaurus astibiae from the Late Cretaceous of the Iberian Peninsula
Fig. 4. The titanosaurian sauropod Lirainosaurus astibiae Sanz, Powell, Le Loeuff, Martínez, and Pereda Suberbiola, 1999 from the Late Cretaceous of Laño (northern Spain), paratypic braincase (MCNA 7439). Interpretive line drawings in posterior (A), anterior (B), and right lateral (C) views. Grey area indicates iron oxides.
Fig. 2 in Braincase anatomy of the titanosaurian sauropod Lirainosaurus astibiae from the Late Cretaceous of the Iberian Peninsula
Fig. 2. The titanosaurian sauropod Lirainosaurus astibiae Sanz, Powell, Le Loeuff, Martínez, and Pereda Suberbiola, 1999 from the Late Cretaceous of Laño (northern Spain), paratypic braincase (MCNA 7439). Stereopairs in posterior (A) and anterior (B) views.
Fig.1 in A Euenantiornithine Bird from the Late Cretaceous Ha eg Basin of Romania
Fig.1. Geography of the Haţeg Basin, Western Romania, showing the position (star) of the microvertebrate bone bed that yielded the specimens discussed in this paper. Grey areas show post Late Cretaceous tectogenesis ("Laramian") sedimentary basins: I, Rusca Montana Basin; II, Strei Basin; III, Haţeg Basin; IV, Petrosani Basin.
Fig. 2 in A Euenantiornithine Bird from the Late Cretaceous Ha eg Basin of Romania
Fig. 2. Enantiornithine bird humeri from Romania, Haţeg Basin, Upper Cretaceous. A. NVEN 1, right humerus in cranial (A1), caudal (A2), and distal (A3) views. B. NVEN 2, left proximal humerus in cranial (B1), caudal (B2), and proximal (B3) views.
Fig. 3 in A Euenantiornithine Bird from the Late Cretaceous Ha eg Basin of Romania
Fig. 3. Drawings of enantionithine humeri for comparison. A. NVEN 1, right humerus in cranial (A1) and caudal (A2) views. B. Enantiornis leali Walker, Buffetaut, and Dyke, 2007, in cranial (B1) and caudal (B2) views. C. Pengornis houi Zhou, Clarke, and Zhang, 2008, right humerus in caudal view. D. Martinavis vincei Walker and Dyke, 2010, left humerus in cranial (D1) and caudal (D2) views. E.Concornis lacustri Sanz, Chiappe, and Buscalioni, 1995, right humerus in cranial view. F. Eoenantiornis buhleri Hou, Martin, Zhou, and Feduccia, 2000, left humerus in caudal view. Scale bars 10 mm.
Fig. 3 in Borings formed by Late Cretaceous endobiontic foraminifers within larger benthic foraminifers
Fig. 3. Four paratypes of Curvichnus semorbis igen. et isp. nov. in Orbitoides tests showing variability of the shape. A. MGUH 26409. B. MGUH 26410. C. MGUH 26411 (arrow). D. MGUH 26412. Split tests of Orbitoides with outlines of Curvichnus marked by dashed lines (A1, B1, C1, D1). Reconstructions of the shape of Curvichnus (A2, B2, C2, D2). Scale bars 1 mm.
Fig. 4 in Borings formed by Late Cretaceous endobiontic foraminifers within larger benthic foraminifers
Fig. 4. Talpinella cunicularia and Curvichnus semorbis isp. nov. in relation to diagenesis. MGUH 26408. A. Test remains of Talpinella cunicularia. Scale 200 mm. B. Close−up of the test surrounded by a fringe of spar cement. Scale 10 µm. C. Spar cement inside Curvichnus semorbis isp. nov. The latter delineated by stippled lines. Scale 100 µm. D. Close−up of the cement. Scale 10 µm.
Fig. 2 in Borings formed by Late Cretaceous endobiontic foraminifers within larger benthic foraminifers
Fig. 2. Two specimens of Curvichnus semorbis igen. et isp. nov. in tests of Orbitoides. A. MGUH 26407, holotype. B. MGUH 26408, paratype. Split tests of Orbitoides penetrated by Curvichnus, marked by dashed lines (A1, B1). Reconstruction of the shape of Curvichnus (A2, B2). Close−up of bifurcation (A3). B3. Close−up of boring section of Orbitoides with remains of Talpinella cunicularia (arrows). Scale bars 1 mm.
Fig. 1 in Borings formed by Late Cretaceous endobiontic foraminifers within larger benthic foraminifers
Fig. 1. Outline of the foraminifer Talpinella cunicularia and its trace within the equatorial layer of Orbitoides. A. Cross−section parallel to the equatorial layer. The trace, which may have bifurcated ends, forms around the embryonic apparatus of Orbitoides. Resorption may have removed early chamber walls of T. cunicularia (stippled lines). After Baumfalk et al. (1982). B. Cross−section perpendicular to the equatorial layer of which the trace is confined to. The equatorial layer of chamberlets is flanked by layers of lateral chamberlets. Adapted from Görmüş and Sagular (1998). Not to scale.
Fig. 26 in A new ornithomimid dinosaur with gregarious habits from the Late Cretaceous of China
Fig. 26. Histogram of femur lengths of Sinornithomimus dongi gen. et sp. nov. (Table 5). Kurtotic distribution curves are drawn for all samples (dashed line) and for juveniles (solid line).
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.