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Gandititan is a basal titanosaurian sauropod dinosaur from the Late Cretaceous of what is now China. It was a long-necked herbivore, typical of sauropods, with a relatively short tail, a characteristic of titanosaurs compared to other sauropods. Titanosauria have a wide range of body sizes, and Gandititan falls around the middle, slightly on the smaller side. Discovered with a fairly well articluated spine from neck to tail, Gandititan is estimated at about 14 m in total body length.
Skeletal reconstruction of the Sauropod dinosaur Abdarainurus barsboldi based on holotype PIN 5669/1, as figured in Averianov and Lopatin, 2020. Outline is based on related Sauropods, modified from SlvrHwk.
Identifier: mythslegendsofba00spenuoft (find matches) Title: Myths and legends of Babylonia & Assyria Year: 1916 (1910s) Authors: Spence, Lewis, 1874-1955 Subjects: Assyro-Babylonian religion Mythology, Assyro-Babylonian Legends Cults Publisher: London : Harrap Contributing Library: Kelly - University of Toronto Digitizing Sponsor: MSN View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: himself to his other son, Anu, god ofthe sky. Speak to the great dragon, he urgedhim ; speak to her, my son, and her anger will beassuaged and her wrath vanish. Duly obedient,Anu betook himself to the realm of Tiawath toreason with her, but the monster snarled at him sofiercely that in dread he turned his back upon herand departed. Next came Nudimmud to her, butwith no better success. At length the gods decidedthat one of their number, called Merodach, shouldundertake the task of combating Tiawath theterrible. Merodach asked that it might be writtenthat he should be victorious, and this was grantedhim. He was then given rule over the entire universe,and to test whether or not the greatest power hadpassed to him a garment was placed in the midstof the gods and Merodach spoke words commandingthat it should disappear. Straightway it vanishedand was not. Once more spake the god, and thegarment re-appeared before the eyes of the dwellersin heaven. The portion of the epic which describes7^ Text Appearing After Image: ' Note About Images Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.
Anterior caudal vertebrae of Caieiria allocaudata (MCT 1719-R). In (1) left lateral; (2) anterior; (3) dorsal; (4) right lateral; (5) posterior and (6) ventral views. Abbreviations: ns, neural spine; pocdf, postzygapophyseal centrodiapophyseal fossa prz, prezygapophyses; sprl, spinoprezygapophyseal lamina; tp, transverse process.
Atamatitan chilensis, holotipo proveniente de estratos de Formación Tolar (Cretácico Superior), El Abra, Región de Antofagasta. A) SGO.PV.961f húmero derecho carente de porción distal en vista anterior, B) SGO. PV.957 vista posterior; C) fémur derecho en vista anterior, D) vita posterior, M) vista distal; E) SGO.PV.961e placa esternal en vista dorsal?, F) vista ventral?; G) SGO.PV.961d costilla en vista anterior, H) vista posterior; I) SGO. PV.961a, vértebra dorsal en vista lateral derecha, J) vista craneal; K) SGO.PV.961b, vértebra dorsal en vista lateral derecha, L) vista craneal; O) fragmento articular de centro vertebral asociado en vista posterior; N) SGO.PV.961c, vértebra caudal en vista ventral, P) vista ventrolateral. Abreviaciones anatómicas: 4t, cuarto trocánter; cap, capitulum; cdp, cresta deltopectoral; cf, cóndilo fibular; cl, comba lateral; cn, canal neural; ct, cóndilo tibial; dp, diapófisis; pan, pedúnculo de arco neural; pl, pleurocelo; prz, prezigapófisis; tm, tubérculo mayor; tub, tuberculum. Barra de escala para A-M , O = 10 cm. Barra de escala para N, P = 5 cm.
This file represents a possible life appearance of the Indian Titanosaurian Sauropod dinosaur Jainosaurus septentrionalis from the Late Cretaceous (Maastrichtian) of India, belonging to the Lameta Formation. References used: Huene & Matley (1933) Hunt et al. (1995) Gunnar Bivens' skeletal diagram Wilson et al. (2008) "Reassessment of Sauropod Dinosaur Jainosaurus (="Antarctosaurus") Septentrionalis from the Upper Cretaceous of India"
Uriash kadici n. gen. n. sp. holotype, femora. Large fragment of right femur SZRFH Ob.3103 (individual C) in A, anterior; B, medial; C, posterior; and D, lateral views. Small fragment of left femur SZRFH Ob.3103 (individual C) in E, posterior; and F, medial views. The numbers 7* and 8 indicate the autapomorphies described in the text: femoral shaft starts to transversely expand distally at a point close to its midlength; and hypertrophied femoral fourth trochanter. Scale bar equals 200 mm.
Presentación de una nueva especie de dinosaurio, denominado Arackar licanantay, en el Museo Nacional de Historia Natural (MNHN) de Chile. Esta nueva especie es el tercer dinosaurio no aviar descrito en Chile, después de Atacamatitan chilensis y Chilesaurus diegosuarezi.
Udelartitan is a titanosaurian sauropod from the Late Cretaceous of what is now Uruguay. It had the typical sauropod body plan, standing on four thick pillar-like legs, and possessing a long neck. Titanosaurs are a very diverse group, Udelartitan was a small one, estimated at only 15 m in body length. Though a skull has yet to be discovered, it probably had peglike teeth, and a large gut for processing vegetation.
Museum of Zoology of the University of São Paulo, Brazil
Restoration of Zhuchengtitan zangjiazhuangensis from the Late Cretaceous of China
Qunkasaura is a titanosaurian sauropod dinosaur that lived approximately 75 million years ago in the Late Cretaceous of what is now Spain. Specifically, it is a saltasaurid titanosaur, and its discovery marks the first instance of two distinct lineages of this group present in the same locality. In the Late Cretaceous, Europe was a large archipelago, and the coexistence of these differing lineages indicates that saltasaurids arrived in the Iberian Peninsula much later than other groups of dinosaurs.
Skeletons of Bonatitan and Austroraptor at the Museo Argentino de Ciencias Naturales Bernardino Rivadavia
Saltasaurus (which means "lizard from Salta") was a sauropod dinosaur of the Late Cretaceous Period. Relatively small among sauropods, though still massive by human standards, it was characterized by a diplodocid-like head
Saltasaurus (which means "lizard from Salta") was a sauropod dinosaur of the Late Cretaceous Period. Relatively small among sauropods, though still massive by human standards, it was characterized by a diplodocid-like head
Saltasaurus (which means "lizard from Salta") was a sauropod dinosaur of the Late Cretaceous Period. Relatively small among sauropods, though still massive by human standards, it was characterized by a diplodocid-like head
Saltasaurus (which means "lizard from Salta") was a sauropod dinosaur of the Late Cretaceous Period. Relatively small among sauropods, though still massive by human standards, it was characterized by a diplodocid-like head
Saltasaurus (which means "lizard from Salta") was a sauropod dinosaur of the Late Cretaceous Period. Relatively small among sauropods, though still massive by human standards, it was characterized by a diplodocid-like head
Saltasaurus (which means "lizard from Salta") was a sauropod dinosaur of the Late Cretaceous Period. Relatively small among sauropods, though still massive by human standards, it was characterized by a diplodocid-like head
Saltasaurus (which means "lizard from Salta") was a sauropod dinosaur of the Late Cretaceous Period. Relatively small among sauropods, though still massive by human standards, it was characterized by a diplodocid-like head
A visual representation of Yamanasaurus lojaensis, first dinosaur discovered in Ecuador
Reconstruction of the holotype skull (PIN 3906/2) of the Late Cretaceous sauropod Quaesitosaurus orientalis. Based on Kurzanov & Bannikov 1983,[1] missing elements restored after Nemegtosaurus.[2] Color Key Preserved Missing References ↑ (1983). "A new sauropod from the Upper Cretaceous of Mongolia". Paleontological Journal 2: 90−96. ↑ (2005). "Redescription of the mongolian sauropod Nemegtosaurus mongoliensis nowinski (dinosauria: Saurischia) and comments on late cretaceous sauropod diversity". Journal of Systematic Palaeontology 3 (3): 283−318. DOI:10.1017/S1477201905001628.
Fig. 5. Forelimb bones of the titanosaurian sauropod Bustingorrytitan shiva gen. et sp. nov. from “Bustingorry II” site, Neuquén Province, Argentina, upper Cenomanian. A. Left coracoid (holotype, MMCH-Pv 59/13) in lateral view. B. Left scapula (holotype, MMCH-Pv 59/11) in lateral view. C. Left humerus (holotype, MMCH-Pv 59/21) in proximal (C1), anterior (C2), and distal (C3) views. D. Right radius (holotype, MMCH-Pv 59/22) in posterior view. E. Left sternal plate (holotype, MMCH-Pv 59/15) in dorsal view. F. Articulated metacarpals I–V (holotype, MMCH-Pv 59/25–29) in proximal (F1), anterior (F2) and distal (F3) views. G. Right ulna (holotype, MMCH-Pv 59/23) in medial (G1) and proximal (G2) views. Abbreviations: cf, coracoid foramen; gas, glenoid articular surface; igl, infraglenoid lip; I–V, metacarpals. Scale bars 200 mm.
Restoration of Borealosaurus a potentially titanosaur dinosaur from the Cretaceous of China
Jaw of Bonitasaura (bottom) compared to that of Baalsaurus (top)
Restoration of the Chinese theropod "Sinopliosaurus fusuiensis" as a generalized spinosaurid. Silhouette of the holotype tooth is visible.
dent de Globidens aegyptiacus et dent de Mosasaurus beaugei montrant les cavités de la dent de remplacement
Henan Geological Museum, Zhengzhou, China. Complete indexed photo collection at WorldHistoryPics.com.
Muestras de dinosaurios en tamaño real a cuando existieron. El gran tiranosaurio, que habito hace millones de años la zona de Bagua en Amazonas. El carnotaurus (carnívoro feroz), el velociraptor y el lewisuchus, pequeño antecesor de los dinosaurios.
Ahvaytum bahndooiveche scale comparison using Mbiresaurus raathi as reference from Lovelace et al., 2025
Comparison of the digit III/footprint length ratio for Eubrontes of the same size in America, Europe, and China. American specimens: (a) Eubrontes giganteus AC 15/3, type specimens (Lockley 2009); (b) Eubrontes giganteus AC 45/1 (Olsen et al. 1998); (c) Utah Eubrontes 1 (Lockley et al. 1998); (d) Utah Eubrontes 2 (T3) (Lockley et al. 2021); (e) Connecticut Eubrontes (Ishigaki and Fujisaki 1989); (f) Eubrontes (?) glenrosensis (Adams et al. 2010); European specimen: (g) Eubrontes veillonensis (de Lapparent and Montenat 1967); Chinese specimens: (h) Eubrontes pareschequier (Xing et al. 2009a, 2014b); (i) Eubrontes zigongensis (Xing et al. 2014c); (j) Eubrontes platypus (Hitchcock 1858) Xiyang specimen (Yang and Yang 1987); (k) Eubrontes monax (Zhen et al. 1986; Lockley et al. 2013); (l) Eubrontes xiyangensis (Zhen et al. 1986; Lockley et al. 2013); (m) Changpeipus carbonicus (Xing et al. 2014b); (n) Eubrontes nianpanshanensis (Xing et al. 2016b); (o) Lufengopus dongi (Lü et al. 2006; Xing et al. 2014d); (p) Eubrontes (?) glenrosensis Hailiutu specimen (Li et al. 2010; Xing et al. 2021); (q) Lockleypus luanpingeris (Xing et al. 2018e); (r) Chapus lockleyi (Li et al. 2006); (s) Asianopodus pulvinicalyx (Matsukawa et al. 2005); (t) Asianopodus robustus (Li et al. 2011; Lockley et al. 2018); (u) Eubrontes nobitai (This study); (v) Eubrontes HX-T3 (Xing et al. 2015b); (w) Eubrontes BJA-T4 (Xing et al. 2016c)
Cleveland Museum of Natural History Coelophysis block, originally AMNH Block XII collected in 1948 by Colbert and crew.
Main evolutionary steps proposed for the morphofunctional and postural changes of the sauropod pedes. (A) Sauropod body mass through time (in metric tons) based on the sauropod body mass estimations of (41) (NB: data lacking for the second half of the Upper Cretaceous so illustrated here faded, in continuity with the data recorded in the Cretaceous). Schematic outlines of selected large specimens illustrated in the curve, including (from left to right) P. engelhardti, Vulcanodon karibaensis, R. brownei, G. brancai, Cedarosaurus weiskopfae, and Notocolossus gonzalezparejasi. (B) Projected evolutionary changes occurring in the sauropod pes associated with trend in body mass, including 1, skeletal and functional digitigrade pedal posture among basal non-sauropod sauropodomorphs with an incipient soft tissue pad (ISP) (see figs. S34 and S35); 2 and 3, expansion of a well-developed soft tissue pad beneath the elevated pedal bones (SP), resulting in a functionally plantigrade pes + retention of skeletal posture within a range of digitigrady; 4, retention of a soft tissue pad and yet undetermined trend toward more elevated bones; 5, conservation of the neomorphic soft tissue pad within all lineages. Selected examples of well-preserved non-sauropod sauropodomorph and sauropod pedal tracks illustrated above the trends, including (from left to right) Evazoum siriguii; Pseudotetrasauropus bipedoida, Eosauropus isp., Lavinipes cheminii; Kalosauropus pollex, Liujianpus shunan, Polyonyx gomesi; Parabrontopodus mcintoshi; Brontopodus birdi; Titanopodus mendozensis; and unnamed Asian sauropod track. Source of adapted drawing and notes are listed in table S9 and data S2.
Main evolutionary steps proposed for the morphofunctional and postural changes of the sauropod pedes. (A) Sauropod body mass through time (in metric tons) based on the sauropod body mass estimations of (41) (NB: data lacking for the second half of the Upper Cretaceous so illustrated here faded, in continuity with the data recorded in the Cretaceous). Schematic outlines of selected large specimens illustrated in the curve, including (from left to right) P. engelhardti, Vulcanodon karibaensis, R. brownei, G. brancai, Cedarosaurus weiskopfae, and Notocolossus gonzalezparejasi. (B) Projected evolutionary changes occurring in the sauropod pes associated with trend in body mass, including 1, skeletal and functional digitigrade pedal posture among basal non-sauropod sauropodomorphs with an incipient soft tissue pad (ISP) (see figs. S34 and S35); 2 and 3, expansion of a well-developed soft tissue pad beneath the elevated pedal bones (SP), resulting in a functionally plantigrade pes + retention of skeletal posture within a range of digitigrady; 4, retention of a soft tissue pad and yet undetermined trend toward more elevated bones; 5, conservation of the neomorphic soft tissue pad within all lineages. Selected examples of well-preserved non-sauropod sauropodomorph and sauropod pedal tracks illustrated above the trends, including (from left to right) Evazoum siriguii; Pseudotetrasauropus bipedoida, Eosauropus isp., Lavinipes cheminii; Kalosauropus pollex, Liujianpus shunan, Polyonyx gomesi; Parabrontopodus mcintoshi; Brontopodus birdi; Titanopodus mendozensis; and unnamed Asian sauropod track. Source of adapted drawing and notes are listed in table S9 and data S2.
Cast of the holotype trackway of Eosauropus, a probable sauropodomorph dinosaur ichnogenus, on display at the Museum of Western Colorado’s Dinosaur Journey Museum in Fruita, Colorado
Iguanodon bernissartensis ; rechtervoetbeenderen over een voetafdruk (Iguanodontipus burreyi). Door Louis Dollo (1905).
Title: A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey .. Identifier: CUbiodiversity600397-9082 (find matches) Year: 1889 (1880s) Authors: Lesley, J. P. (J. Peter), 1819-1903; Pennsylvania. Board of Commissioners for the Second Geological Survey Subjects: Paleontology Publisher: Harrisburg, Board of Commissioners for the Geological Survey Contributing Library: Cornell University Library Digitizing Sponsor: Mann Library, Cornell View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: 697 Plec. Plectropterna angusta, Hitchcock, Icht. Mass. page 110, lias. f-) itch cock ^ Idithuolo^ij McLSS. Text Appearing After Image: I'lfrtroplerria, Note About Images Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.
A, Akmechetosauropus makhkamovi (redrawn from [56]); B, Amblydactylus gethingi (redrawn from [8]); C, Amblydactylus kortmeyeri (redrawn from [57]); D, Apulosauripus federicianus (redrawn from [62]); E, Babatagosauropus bulini (redrawn from [56]); F, Bonaparteichnium tali (redrawn from [66]); G, Brachyguanodonipus prejanensis (redrawn from [68]); H, Camptosaurichnus fasolae (redrawn from [70]); I, Camptosauropus vialovi (redrawn from [74]); J, Caririchnium magnificum (redrawn from [11]); K, Caririchnium leonardii (redrawn from [76]); L-M, Caririchnium protohadrosaurichnos (redrawn from [78]); N, Caririchnium lotus (redrawn from [81]); O, Caririchnium kyoungsookimi (redrawn from [80]); P, Gigantoshiraminesauropus matsuoi (redrawn from [82]); Q, Gypsichnites pacensis (redrawn from [8]); R, Hadrosaurichnoides igeensis (redrawn from [92]); S, Hadrosaurichnus australis (redrawn from [93]); T, Hadrosaurichnus titicaensis (redrawn from [96]); U, Hadrosauripeda hauboldi (redrawn from [98]); V, Hadrosauropodus langstoni (redrawn from [24]); W, Hadrosauropodus nanxiongensis (redrawn from [99]); X, Iguanodonichnus frenkii (redrawn from [70]); Y, Iguanodonipus cuadrupedae (redrawn from [68]).
Remake of the original picture of the Drzewica Formation. Terrestrial environment of the Pliensbachian-Toarcian boundary of Fennoscandinavia Inland environment of the Bornholm Coast, nearby the German realm of the Ciechocinek Formation. Includes Ciechocinek Formation (Lower Toarcian, Bones) and Drzwica Formation (Latest Pliensbachian, Footprints) Fauna Sorthat Formation environment, fluvial influenced mainland with Cheirolepidaceae and Bennetitales as dominant flora Dinosaurs are based on material found on various locations of Northern Germany, and Footprints of the underliying Drzewica Formation at the Holy Cross Mountains, connected with Bornholm at the time. Dinosaur Species appeared: Megalosauripus isp. Large Footprints (+65 cm) found on the Drzewica Formation. There is a dorsal vertebrae on the German Margin of the Ciechocinek Formation assigend to Megalosauria (Huene, 1966). Gravisauria spp. representing the Grimmen Sauropod reported on 2014, as a taxon related with Tazoudasaurus. Barapasaurus-like footprints are know from the Drzewica Formation. Coelophysoidea spp. based on coeval Anchisauripus tracks from the Holy Cross Mountains. Basal Ornithischan, related to Eocursor, based on a crouching trace (Gerard Dariusz Gierlinski, Martin G. Lockley, Grzegorz Niedźwiedzki:2009). Massospondylidae spp. based on Otozum-like tracks.
Heterodontosaurus tucki life restoration. Integument based on the related Tianyulong, proportions based on photos of specimen SAM-PK-K1332 and skeletal reconstruction by Gregory S. Paul (The Princeton Field Guide to Dinosaurs, 2010, p. 240).
Life restoration of Diodorus scytobrachion. Based on the holotype remains[1] and those of more complete relatives.[2][3] External look based on inferences for basal dinosauromorphs[4] and the mythical mušḫuššu.
Attenborosaurus conybeari, a plesiosaur from the Early Jurassic of England, pencil drawing
Attenborosaurus conybeari, a plesiosaur from the Early Jurassic of England, pencil drawing
Attenborosaurus conybeari, a plesiosaur from the Early Jurassic of England, pencil drawing
Simple drawing of Ankylosaurus magniventris, a North American Cretaceous ankylosaurid. Based on skeletal reconstruction in Paul 2010.