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Figure 22 in The theropod dinosaur Elaphrosaurus bambergi Janensch, 1920, from the Late Jurassic of Tendaguru, Tanzania
Figure 22. Left astragalocalcaneum of Elaphrosaurus bambergi in proximal (A, stereophotographs), anterior (B, stereophotographs), distal (C, stereophotographs), posterior (D, stereophotographs), medial (E), and lateral (F) views. Abbreviations: ag, anterior groove; asc, broken base of ascending process; d, depression; ff, fibular facet; ltf, lateral tibial facet; mtf, medial tibial facet; tf, triangular flange. Scale bars: 1 cm.
Figure 24 in The theropod dinosaur Elaphrosaurus bambergi Janensch, 1920, from the Late Jurassic of Tendaguru, Tanzania
Figure 24. Phylogenetic relationships of Elaphrosaurus bambergi: results of a phylogenetic analysis of 31 theropod taxa and 216 morphological characters. A, strict consensus of 129 360 equally parsimonious trees; B, Adams consensus (see text for details).
Figure 8 in The early evolution of titanosauriform sauropod dinosaurs
Figure 8. Titanosauriform palaeobiogeography. The Early Cretaceous is characterized by some endemism, with mostly brachiosaurids in North America, mostly euhelopodids in Asia, and mostly titanosaurs in South America. Palaeogeographical reconstructions modified from Blakey (2006).
Figure 1 in The early evolution of titanosauriform sauropod dinosaurs
Figure 1. Titanosauriform discoveries plotted in five-year bins. Note the dramatic increase in naming in recent years. The skull and body of Giraffatitan (modified from Wilson & Sereno, 1998) highlight basal titanosauriform anatomy.
Figure 4 in The early evolution of titanosauriform sauropod dinosaurs
Figure 4. Character maps for some cladistic analyses of sauropod dinosaurs. The analysis presented in this study incorporates few cranial characters, reflecting the poor fossil record for titanosauriform skulls and standing in contrast to the pattern of character distribution in Diplodocoidea. Analyses that are wider in scope such as that of Wilson (2002) have a more even distribution of characters throughout the body.
Figure 3 in The early evolution of titanosauriform sauropod dinosaurs
Figure 3. Parsed versions of the cladograms presented in Figure 2, with their authors listed near their root. Only taxa appearing in at least half of those analyses are included here. A strict consensus of these analyses with and without Euhelopus is shown at the bottom left and bottom right of the figure, respectively. mdt, more derived titanosaurs.
Figure 2 in The early evolution of titanosauriform sauropod dinosaurs
Figure 2. Selected previous cladistic hypotheses for the relationships of basal titanosauriforms, with their authors listed near their root. mdt, more derived titanosaurs. Numbers near each node indicate decay indices calculated in PAUP*.
Figure 6 in The early evolution of titanosauriform sauropod dinosaurs
Figure 6. Phylogenetic hypothesis presented in this study plotted on a geological timescale (Gradstein, Ogg & Smith, 2004), with relevant clade names (Table 1) labelled. Selected synapomorphies highlighting some nodes are shown. Brachiosauridae: quadratojugal with triangular ventral prong (shown here in Europasaurus), twisted maxillary teeth (shown here in Giraffatitan), bevelled distal end of metatarsal IV (shown here in Sonorasaurus). Somphospondyli: somphospondylus vertebral pneumaticity, consisting of subcentimetre and submillimetre cells and walls, respectively, that permeate the vertebra (shown here in Saruoposeidon). Euhelopodidae: cervical vertebrae with bifid neural spines, pendant cervical ribs, a thick, vertically orientated epipophyseal–prezygapophyseal lamina, a 'kinked' intrapostzygapophyseal lamina (shown here in Erketu). Titanosauria: plate-like ischium (shown here in Andesaurus). Also shown here are a short ischium (a synapomorphy of Sauroposeidon plus more derived somphospondyls) and a raised tubercle on the lateral ischium (a titanosauriform synapomorphy).
Figure 5 in The early evolution of titanosauriform sauropod dinosaurs
Figure 5. Cladistic hypothesis presented in this study. The cladogram is a strict consensus of nine equally parsimonious trees. Clade names as defined by phylogenetic taxonomy (Table 1; Wilson & Upchurch, 2003) are listed beside each node.
Figure 7 in The early evolution of titanosauriform sauropod dinosaurs
Figure 7. Purported early 'titanosaur' species in comparison with a basal titanosauriform (Giraffatitan). The caudal vertebral procoely of 'Iuticosaurus' and curved/raised ulnar olecranon of 'Pelorosaurus' becklesii are indistinguishable from the situation in Giraffatitan. Scale bars: Giraffatitan vertebra = 5 cm; 'Iuticosaurus', Giraffatitan ulna, and 'Pelotosaurus' becklesii = 10 cm.
Figure 24 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 24. Time-correlated phylogeny for basal ornithopod taxa illustrating relative abundance through time. Note the Maastrichtian radiation of Thescelosaurus in North America and Zalmoxes in Europe. The iguanodontian radiation is represented as a single line because of size constraints. Al, Albian; Ap, Aptian; Ba, Barremian; Be, Berriasian; Ca, Campanian; Ce, Cenomanian; Co, Coniacian; H, Hauterivian; LJ, Late Jurassic; M, Maastrichtian; MJ, Middle Jurassic; S, Santonian; T, Turonian; V, Valanginian. Modified from Weishampel et al., 2003.
Figure 23 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 23. The single most-parsimonious tree (tree length 361 steps) recovered from the cladistic analysis using the implicit enumeration search option in TNT. Bootstap values (1000 replicates) above 50% are reported below the branches, and Bremer support values greater than 1 are reported above.
Figure 22 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 22. Left pes of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in dorsal (A), plantar (B), and proximal (C) views. Dashed lines indicate the extrapolated margins of the pes. See list in text for an explanation of anatomical abbreviations. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction. Roman numerals denote digit number.
Figure 21 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 21. Left tibia, fibula, astragalus calcaneum, and distal lateral tarsal of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in anterior (A), posterior (B), medial (C), lateral (D), proximal (E), and distal (F) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 19 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 19. Right pubis of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in dorsal (A), ventral (B), medial (C), and lateral (D) views. Dashed lines indicate the extrapolated margins of the element. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 16. A in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 16. A left rib of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in anterior (A), posterior (B), medial (C), and lateral (D) views, and showing flattened and rugose posterior margin (E). Lateral view shows cross-sectional shape along the shaft, with the lateral surface facing upwards. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. White areas represent plaster reconstruction.
Figure 20 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 20. Left femur of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in anterior (A), posterior (B), medial (C), lateral (D), proximal (E), and distal (D) views. Dashed lines indicate the extrapolated margins of the element. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 18 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 18. Left ilium of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in lateral (A), medial (B), dorsal (C), and ventral (D) views. Dashed lines indicate extrapolated margins of the element. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
Figure 17 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 17. Distal portions of ribs of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in posterior (A) and anterior (B) views, illustrating rugose texture of posterior margin.
Figure 14 in A new basal ornithopod dinosaur (Frenchman Formation, Saskatchewan, Canada), and implications for late Maastrichtian ornithischian diversity in North America
Figure 14. Sixth dorsal vertebra of the holotype of Thescelosaurus assiniboiensis sp. nov., RSM P 1225.1, in right lateral (A), left lateral (B), posterior (C), anterior (D), dorsal (E), and ventral (F) views. See list in text for an explanation of anatomical abbreviations. Primes indicate illustrations of photographed elements. Dashed lines indicate extrapolated margins of the element. Hatched areas represent incomplete bone surface. White areas represent plaster reconstruction.
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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.