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A Neoceratopsian Dinosaur from the Early Cretaceous of Mongolia And
ARTICLE https://doi.org/10.1038/s42003-020-01222-7 OPEN A neoceratopsian dinosaur from the early Cretaceous of Mongolia and the early evolution of ceratopsia ✉ Congyu Yu 1 , Albert Prieto-Marquez2, Tsogtbaatar Chinzorig 3,4, Zorigt Badamkhatan4,5 & Mark Norell1 1234567890():,; Ceratopsia is a diverse dinosaur clade from the Middle Jurassic to Late Cretaceous with early diversification in East Asia. However, the phylogeny of basal ceratopsians remains unclear. Here we report a new basal neoceratopsian dinosaur Beg tse based on a partial skull from Baruunbayan, Ömnögovi aimag, Mongolia. Beg is diagnosed by a unique combination of primitive and derived characters including a primitively deep premaxilla with four pre- maxillary teeth, a trapezoidal antorbital fossa with a poorly delineated anterior margin, very short dentary with an expanded and shallow groove on lateral surface, the derived presence of a robust jugal having a foramen on its anteromedial surface, and five equally spaced tubercles on the lateral ridge of the surangular. This is to our knowledge the earliest known occurrence of basal neoceratopsian in Mongolia, where this group was previously only known from Late Cretaceous strata. Phylogenetic analysis indicates that it is sister to all other neoceratopsian dinosaurs. 1 Division of Vertebrate Paleontology, American Museum of Natural History, New York 10024, USA. 2 Institut Català de Paleontologia Miquel Crusafont, ICTA-ICP, Edifici Z, c/de les Columnes s/n Campus de la Universitat Autònoma de Barcelona, 08193 Cerdanyola del Vallès Sabadell, Barcelona, Spain. 3 Department of Biological Sciences, North Carolina State University, Raleigh, NC 27695, USA. 4 Institute of Paleontology, Mongolian Academy of Sciences, ✉ Ulaanbaatar 15160, Mongolia. -
And the Origin and Evolution of the Ankylosaur Pelvis
Pelvis of Gargoyleosaurus (Dinosauria: Ankylosauria) and the Origin and Evolution of the Ankylosaur Pelvis Kenneth Carpenter1,2*, Tony DiCroce3, Billy Kinneer3, Robert Simon4 1 Prehistoric Museum, Utah State University – Eastern, Price, Utah, United States of America, 2 Geology Section, University of Colorado Museum, Boulder, Colorado, United States of America, 3 Denver Museum of Nature and Science, Denver, Colorado, United States of America, 4 Dinosaur Safaris Inc., Ashland, Virginia, United States of America Abstract Discovery of a pelvis attributed to the Late Jurassic armor-plated dinosaur Gargoyleosaurus sheds new light on the origin of the peculiar non-vertical, broad, flaring pelvis of ankylosaurs. It further substantiates separation of the two ankylosaurs from the Morrison Formation of the western United States, Gargoyleosaurus and Mymoorapelta. Although horizontally oriented and lacking the medial curve of the preacetabular process seen in Mymoorapelta, the new ilium shows little of the lateral flaring seen in the pelvis of Cretaceous ankylosaurs. Comparison with the basal thyreophoran Scelidosaurus demonstrates that the ilium in ankylosaurs did not develop entirely by lateral rotation as is commonly believed. Rather, the preacetabular process rotated medially and ventrally and the postacetabular process rotated in opposition, i.e., lateral and ventrally. Thus, the dorsal surfaces of the preacetabular and postacetabular processes are not homologous. In contrast, a series of juvenile Stegosaurus ilia show that the postacetabular process rotated dorsally ontogenetically. Thus, the pelvis of the two major types of Thyreophora most likely developed independently. Examination of other ornithischians show that a non-vertical ilium had developed independently in several different lineages, including ceratopsids, pachycephalosaurs, and iguanodonts. -
Two New Stegosaur Specimens from the Upper Jurassic Morrison Formation of Montana, USA
Editors' choice Two new stegosaur specimens from the Upper Jurassic Morrison Formation of Montana, USA D. CARY WOODRUFF, DAVID TREXLER, and SUSANNAH C.R. MAIDMENT Woodruff, D.C., Trexler, D., and Maidment, S.C.R. 2019. Two new stegosaur specimens from the Upper Jurassic Morrison Formation of Montana, USA. Acta Palaeontologica Polonica 64 (3): 461–480. Two partial skeletons from Montana represent the northernmost occurrences of Stegosauria within North America. One of these specimens represents the northernmost dinosaur fossil ever recovered from the Morrison Formation. Consisting of fragmentary cranial and postcranial remains, these specimens are contributing to our knowledge of the record and distribution of dinosaurs within the Morrison Formation from Montana. While the stegosaurs of the Morrison Formation consist of Alcovasaurus, Hesperosaurus, and Stegosaurus, the only positively identified stegosaur from Montana thus far is Hesperosaurus. Unfortunately, neither of these new specimens exhibit diagnostic autapomorphies. Nonetheless, these specimens are important data points due to their geographic significance, and some aspects of their morphologies are striking. In one specimen, the teeth express a high degree of wear usually unobserved within this clade—potentially illuminating the progression of the chewing motion in derived stegosaurs. Other morphologies, though not histologically examined in this analysis, have the potential to be important indicators for maturational inferences. In suite with other specimens from the northern extent of the formation, these specimens contribute to the ongoing discussion that body size may be latitudinally significant for stegosaurs—an intriguing geographical hypothesis which further emphasizes that size is not an undeviating proxy for maturity in dinosaurs. Key words: Dinosauria, Thyreophora, Stegosauria, Jurassic, Morrison Formation, USA, Montana. -
Stegosaurus Scelidosaurus Huayangosaurus Cheeks: No
Huayangosaurus Scelidosaurus Stegosaurus Cheeks: No reptile has ever had a ‘buccinator’ muscle Answer: highly flexible tongue Brains 0.001% of stegosaur body weight Compared to 1.8% in humans (1000x larger per unit body weight!) Brains Brains Locomotion Graviportal Locomotion Elephantine hind feet (weight-bearing) Shin bones fused with astragalus/ calcaneum Femur: Long compared to humerus Columnar Facultative Tripodality? Stocky forelimbs- could be used for turning/posturing (Bakker) Dermal Armour? Pattern of plates and spines is species-specific Plates paired or staggered (Stegosaurus) Plates were probably not for defense... not tough enough Rotation? Surface markings => symmetrical. Rotation unlikely Potential uses: Thermoregulation? Warm up (ectotherms), Cool down (endotherms) Signaling? positioned for maximal lateral visibility Sexual Selection Mate Recognition Grooves for blood vessels Sexual dimorphism Differences between males and females of the same species **New finding** published in 2015 Stegosaurus Morrison formation, Colorado Dinosaur Sex Figuring out how Stegosaurus even could have mated is a prickly subject. Females were just as well-armored as males, and it is unlikely that males mounted the females from the back. A different technique was necessary. Perhaps they angled so that they faced belly to belly, some have guessed, or maybe, as suggested by Timothy Isles in a recent paper, males faced away from standing females and backed up (a rather tricky maneuver!). The simplest technique yet proposed is that the female lay down on her side and the male approached standing up, thereby avoiding all those plates and spikes. However the Stegosaurus pair accomplished the feat, though, it was most likely brief—only as long as was needed for the exchange of genetic material. -
Luis V. Rey & Gondwana Studios
EXHIBITION BY LUIS V. REY & GONDWANA STUDIOS HORNS, SPIKES, QUILLS AND FEATHERS. THE SECRET IS IN THE SKIN! Not long ago, our knowledge of dinosaurs was based almost completely on the assumptions we made from their internal body structure. Bones and possible muscle and tendon attachments were what scientists used mostly for reconstructing their anatomy. The rest, including the colours, were left to the imagination… and needless to say the skins were lizard-like and the colours grey, green and brown prevailed. We are breaking the mould with this Dinosaur runners, massive horned faces and Revolution! tank-like monsters had to live with and defend themselves against the teeth and claws of the Thanks to a vast web of new research, that this Feathery Menace... a menace that sometimes time emphasises also skin and ornaments, we reached gigantic proportions in the shape of are now able to get a glimpse of the true, bizarre Tyrannosaurus… or in the shape of outlandish, and complex nature of the evolution of the massive ornithomimids with gigantic claws Dinosauria. like the newly re-discovered Deinocheirus, reconstructed here for the first time in full. We have always known that the Dinosauria was subdivided in two main groups, according All of them are well represented and mostly to their pelvic structure: Saurischia spectacularly mounted in this exhibition. The and Ornithischia. But they had many things exhibits are backed with close-to-life-sized in common, including structures made of a murals of all the protagonist species, fully special family of fibrous proteins called keratin fleshed and feathered and restored in living and that covered their skin in the form of spikes, breathing colours. -
An Ankylosaurid Dinosaur from Mongolia with in Situ Armour and Keratinous Scale Impressions
An ankylosaurid dinosaur from Mongolia with in situ armour and keratinous scale impressions VICTORIA M. ARBOUR, NICOLAI L. LECH−HERNES, TOM E. GULDBERG, JØRN H. HURUM, and PHILIP J. CURRIE Arbour, V.M., Lech−Hernes, N.L., Guldberg, T.E., Hurum, J.H., and Currie P.J. 2013. An ankylosaurid dinosaur from Mongolia with in situ armour and keratinous scale impressions. Acta Palaeontologica Polonica 58 (1): 55–64. A Mongolian ankylosaurid specimen identified as Tarchia gigantea is an articulated skeleton including dorsal ribs, the sacrum, a nearly complete caudal series, and in situ osteoderms. The tail is the longest complete tail of any known ankylosaurid. Remarkably, the specimen is also the first Mongolian ankylosaurid that preserves impressions of the keratinous scales overlying the bony osteoderms. This specimen provides new information on the shape, texture, and ar− rangement of osteoderms. Large flat, keeled osteoderms are found over the pelvis, and osteoderms along the tail include large keeled osteoderms, elongate osteoderms lacking distinct apices, and medium−sized, oval osteoderms. The specimen differs in some respects from other Tarchia gigantea specimens, including the morphology of the neural spines of the tail club handle and several of the largest osteoderms. Key words: Dinosauria, Ankylosauria, Ankylosauridae, Tarchia, Saichania, Late Cretaceous, Mongolia. Victoria M. Arbour [[email protected]] and Philip J. Currie [[email protected]], Department of Biological Sciences, CW 405 Biological Sciences Building, University of Alberta, Edmonton, Alberta, Canada, T6G 2E9; Nicolai L. Lech−Hernes [nicolai.lech−[email protected]], Bayerngas Norge, Postboks 73, N−0216 Oslo, Norway; Tom E. Guldberg [[email protected]], Fossekleiva 9, N−3075 Berger, Norway; Jørn H. -
The Princeton Field Guide to Dinosaurs, Second Edition
MASS ESTIMATES - DINOSAURS ETC (largely based on models) taxon k model femur length* model volume ml x specific gravity = model mass g specimen (modeled 1st):kilograms:femur(or other long bone length)usually in decameters kg = femur(or other long bone)length(usually in decameters)3 x k k = model volume in ml x specific gravity(usually for whole model) then divided/model femur(or other long bone)length3 (in most models femur in decameters is 0.5253 = 0.145) In sauropods the neck is assigned a distinct specific gravity; in dinosaurs with large feathers their mass is added separately; in dinosaurs with flight ablity the mass of the fight muscles is calculated separately as a range of possiblities SAUROPODS k femur trunk neck tail total neck x 0.6 rest x0.9 & legs & head super titanosaur femur:~55000-60000:~25:00 Argentinosaurus ~4 PVPH-1:~55000:~24.00 Futalognkosaurus ~3.5-4 MUCPv-323:~25000:19.80 (note:downsize correction since 2nd edition) Dreadnoughtus ~3.8 “ ~520 ~75 50 ~645 0.45+.513=.558 MPM-PV 1156:~26000:19.10 Giraffatitan 3.45 .525 480 75 25 580 .045+.455=.500 HMN MB.R.2181:31500(neck 2800):~20.90 “XV2”:~45000:~23.50 Brachiosaurus ~4.15 " ~590 ~75 ~25 ~700 " +.554=~.600 FMNH P25107:~35000:20.30 Europasaurus ~3.2 “ ~465 ~39 ~23 ~527 .023+.440=~.463 composite:~760:~6.20 Camarasaurus 4.0 " 542 51 55 648 .041+.537=.578 CMNH 11393:14200(neck 1000):15.25 AMNH 5761:~23000:18.00 juv 3.5 " 486 40 55 581 .024+.487=.511 CMNH 11338:640:5.67 Chuanjiesaurus ~4.1 “ ~550 ~105 ~38 ~693 .063+.530=.593 Lfch 1001:~10700:13.75 2 M. -
External Anatomy
SALMONIDS IN THE CLASSROOM: SALMON DISSECTION EXTERNAL ANATOMY Shape l Salmon are streamlined to move easily through water. Water has much more resistance to movement than air does, so it takes more energy to move through water. A streamlined shape saves the fish energy. Fins l Salmon have eight fins including the tail. They are made up of a fan of bone- like spines with a thin skin stretched between them. The fins are embedded in the salmon’s muscle, not linked to other bones, as limbs are in people. This gives them a great deal of flexibility and manoeuverability. l Each fin has a different function. The caudal or tail, is the largest and most powerful. It pushes from side to side and moves the fish forward in a wavy path. l The dorsal fin acts like a keel on a ship. It keeps the fish upright, and it also controls the direction the fish moves in. l The anal fin also helps keep the fish stable and upright. l The pectoral and pelvic fins are fused for steering and for balance. They can also move the fish up and down in the water. l The adipose fin has no known function. It is sometimes clipped off in hatchery fish to help identify the fish when they return or are caught. Slime l Many fish, including salmon, have a layer of slime covering their body. The slime layer helps fish to: ¡ slip away from predators, such as bears. ¡ slip over rocks to avoid injuries ¡ slide easily through water when swimming ¡ protect them from fungi, parasites, disease and pollutants in the water Scales Remove a scale by scraping backwards with a knife. -
The Systematic Position of the Enigmatic Thyreophoran Dinosaur Paranthodon Africanus, and the Use of Basal Exemplifiers in Phyl
1 The systematic position of the enigmatic thyreophoran dinosaur Paranthodon africanus, 2 and the use of basal exemplifiers in phylogenetic analysis 3 4 Thomas J. Raven1,2 ,3 and Susannah C. R. Maidment2 ,3 5 61Department of Earth Science & Engineering, Imperial College London, UK 72School of Environment & Technology, University of Brighton, UK 8 3Department of Earth Sciences, Natural History Museum, London, UK 9 10Corresponding author: Thomas J. Raven 11 12Email address: [email protected] 13 14 15 16 17 18 19 20 21ABSTRACT 22 23The first African dinosaur to be discovered, Paranthodon africanus was found in 1845 in the 24Lower Cretaceous of South Africa. Taxonomically assigned to numerous groups since discovery, 25in 1981 it was described as a stegosaur, a group of armoured ornithischian dinosaurs 26characterised by bizarre plates and spines extending from the neck to the tail. This assignment 27that has been subsequently accepted. The type material consists of a premaxilla, maxilla, a nasal, 28and a vertebra, and contains no synapomorphies of Stegosauria. Several features of the maxilla 29and dentition are reminiscent of Ankylosauria, the sister-taxon to Stegosauria, and the premaxilla 30appears superficially similar to that of some ornithopods. The vertebral material has never been 31described, and since the last description of the specimen, there have been numerous discoveries 32of thyreophoran material potentially pertinent to establishing the taxonomic assignment of the 33specimen. An investigation of the taxonomic and systematic position of Paranthodon is therefore 34warranted. This study provides a detailed re-description, including the first description of the 35vertebra. Numerous phylogenetic analyses demonstrate that the systematic position of 36Paranthodon is highly labile and subject to change depending on which exemplifier for the clade 37Stegosauria is used. -
Síntesis Del Registro Fósil De Dinosaurios Tireóforos En Gondwana
ISSN 2469-0228 www.peapaleontologica.org.ar SÍNTESIS DEL REGISTRO FÓSIL DE DINOSAURIOS TIREÓFOROS EN GONDWANA XABIER PEREDA-SUBERBIOLA 1 IGNACIO DÍAZ-MARTÍNEZ 2 LEONARDO SALGADO 2 SILVINA DE VALAIS 2 1Universidad del País Vasco/Euskal Herriko Unibertsitatea, Facultad de Ciencia y Tecnología, Departamento de Estratigrafía y Paleontología, Apartado 644, 48080 Bilbao, España. 2CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Av. General Roca 1242, 8332 General Roca, Río Negro, Ar gentina. Recibido: 21 de Julio 2015 - Aceptado: 26 de Agosto de 2015 Para citar este artículo: Xabier Pereda-Suberbiola, Ignacio Díaz-Martínez, Leonardo Salgado y Silvina De Valais (2015). Síntesis del registro fósil de dinosaurios tireóforos en Gondwana . En: M. Fernández y Y. Herrera (Eds.) Reptiles Extintos - Volumen en Homenaje a Zulma Gasparini . Publicación Electrónica de la Asociación Paleon - tológica Argentina 15(1): 90–107. Link a este artículo: http://dx.doi.org/ 10.5710/PEAPA.21.07.2015.101 DESPLAZARSE HACIA ABAJO PARA ACCEDER AL ARTÍCULO Asociación Paleontológica Argentina Maipú 645 1º piso, C1006ACG, Buenos Aires República Argentina Tel/Fax (54-11) 4326-7563 Web: www.apaleontologica.org.ar Otros artículos en Publicación Electrónica de la APA 15(1): de la Fuente & Sterli Paulina Carabajal Pol & Leardi ESTADO DEL CONOCIMIENTO DE GUIA PARA EL ESTUDIO DE LA DIVERSITY PATTERNS OF LAS TORTUGAS EXTINTAS DEL NEUROANATOMÍA DE DINOSAURIOS NOTOSUCHIA (CROCODYLIFORMES, TERRITORIO ARGENTINO: UNA SAURISCHIA, CON ENFASIS EN MESOEUCROCODYLIA) DURING PERSPECTIVA HISTÓRICA. FORMAS SUDAMERICANAS. THE CRETACEOUS OF GONDWANA. Año 2015 - Volumen 15(1): 90-107 VOLUMEN TEMÁTICO ISSN 2469-0228 SÍNTESIS DEL REGISTRO FÓSIL DE DINOSAURIOS TIREÓFOROS EN GONDWANA XABIER PEREDA-SUBERBIOLA 1, IGNACIO DÍAZ-MARTÍNEZ 2, LEONARDO SALGADO 2 Y SILVINA DE VALAIS 2 1Universidad del País Vasco/Euskal Herriko Unibertsitatea, Facultad de Ciencia y Tecnología, Departamento de Estratigrafía y Paleontología, Apartado 644, 48080 Bilbao, España. -
Notes on Plated Dinosaurs (Ornithischia: Stegosauria), Mostly
N. Jb. Geol. Paläont. Abh. 282/1 (2016), 1–25 Article Stuttgart, October 2016 Notes on plated dinosaurs (Ornithischia: Stegosauria), mostly on der- mal armor from Middle and Upper Jurassic of England (also France, Iberia), with a revised diagnosis for Loricatosaurus priscus (Callovian, England) Peter M. Galton With 7 figures Abstract: In basal thyreophorans there is no equivalent to the small based slender dermal tail spines of stegosaurs, which differ in several respects from the lateral dorsal spines of nodosaurid ankylosaurs, and large based stocky spikes are restricted to a few genera of stegosaurs. Several isolated spines and spikes from England (Middle and Upper Jurassic), Portugal (Upper Jurassic) and Spain (Lower Cretaceous), previously re-identified as Thyreophora indet., are Stegosauria indet. Where available, cross-sections shows a thick layer of compact bone with a well-defined central canal as in old adult individuals of Stegosaurus (Upper Jurassic, USA) in which, in addition to display, they functioned as weapons. This stronger construction also favored their preservation as isolated bones. It contrasts with a thin layer of compact bone filled with cancellous bone for the spines of adult and younger individuals of Stegosaurus and of ankylosaurs. The preservation of an isolated pair of spines and of spikes indicates that their bases were bound together. Two columnar femora with a finger-like anterior trochanter from England (Middle and Upper Jurassic) are also re-identified as Stegosauria indet., as are the remains of a juvenile individual from Portugal (Upper Jurassic). The autapomorphies of Lori- catosaurus priscus (NOPCSA, 1911) (England, Middle Jurassic: Middle Callovian) include characters observed in the anterior and mid-caudal vertebrae, posterior pubic process and dermal armor (spine plate, small based body spine). -
A Reassessment of the Purported Ankylosaurian Dinosaur Bienosaurus Lufengensis from the Lower Lufeng Formation of Yunnan, China
A reassessment of the purported ankylosaurian dinosaur Bienosaurus lufengensis from the Lower Lufeng Formation of Yunnan, China THOMAS J. RAVEN, PAUL M. BARRETT, XING XU, and SUSANNAH C.R. MAIDMENT Raven, T.J., Barrett, P.M., Xu, X., and Maidment, S.C.R. 2019. A reassessment of the purported ankylosaurian dinosaur Bienosaurus lufengensis from the Lower Lufeng Formation of Yunnan, China. Acta Palaeontologica Polonica 64 (2): 335–342. The earliest definitive ornithischian dinosaurs are from the Early Jurassic and are rare components of early dinosaur faunas. The Lower Lufeng Formation (Hettangian–Sinemurian) of Yunnan Province, China, has yielded a diverse Early Jurassic terrestrial vertebrate fauna. This includes several incomplete specimens have been referred to Ornithischia, including the type specimen of the thyreophoran “Tatisaurus” and other generically indeterminate material. The highly fragmentary Lufeng ornithischian Bienosaurus lufengensis was described briefly in 2001 and identified as an ankylo- saurian dinosaur. Recent studies have cast doubt on this hypothesis, however, and given that the referral of Bienosaurus to Ankylosauria would result in an extensive ghost-lineage extending between it and the first definitive eurypodans (ankylosaurs + stegosaurs) in the Middle Jurassic, the holotype specimen is re-examined and re-described. We identify Bienosaurus as a probable thyreophoran dinosaur, although the fragmentary nature of the material and the absence of autapomorphies means that the specimen should be regarded as a nomen dubium. Key words: Dinosauria, Ornithischia, Thyreophora, anatomy, Jurassic, Lufeng Formation, Yunnan, China. Thomas J. Raven [[email protected]], Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK; School of Environment and Technology, University of Brighton, Lewes Road, Brighton BN1 4JG, UK.