Cretaceous Theropods from India: a Review of Specimens Described by Huene and Matley (1933)
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
Factors Controlling Detrital Mineralogy of the Sandstone of the Lameta Formation (Cretaceous), Jabalpur Area, Madhya Pradesh, India
FactorsProc Indian Controlling Natn Sci Acad Detrital 74 No.2 Mineralogy pp. 51-56 (2008)of the Sandstone of the Lameta Formation 51 Research Paper Factors Controlling Detrital Mineralogy of the Sandstone of the Lameta Formation (Cretaceous), Jabalpur Area, Madhya Pradesh, India AHM AHMAD ANSARI*, SM SAYEED** and AF KHAN*** Department of Geology, Aligarh Muslim University, Aligarh 202 002 (UP) (Received 7 February 2008; Accepted 6 May 2008) Cretaceous (Maastrichtian) deposits of the Lameta Formation crop out along the eastern part of Jabalpur basin on isolated hills and along the banks of Narmada River near Jabalpur city. The quartzarenite composition with little amounts of feldspar, mica, rock fragments and heavy minerals, are medium to fine grained, moderately sorted to poorly sorted and subangular to subrounded. The study suggests that palaeoclimate, distance of transport and source rock composition influenced the detrital mineralogy of the sandstone. By using Suttner and Dutta diagram, the mean values of the ratio were plotted and that indicate a humid Paleoclimate in this area. The plate tectonic setting and provenance of the sandstone were interpreted using the Dickinson’s method of detrital modes and Qt-F-L, Qm-F-Lt, Qp-Lv-Ls and Qm-P-K triangular diagrams. The petrofacies analysis of the Lameta Formation suggest mainly craton interior in a rifted continental margin basin setting. The plot of various quartz types on diamond diagram after [17] reflects Plutonic terrain. The probable provenance of these sandstones is Mahakoshal and Jabalpur Groups. Key Words: Cretaceous; Lameta Formation; Jabalpur; Mineralogy; Madhya Pradesh; India 1. Introduction Table 1. Stratigraphy of Lameta Formation, Jabalpur area (Madhya Pradesh); Tandon et al. -
A Partial Skeleton of the Tyrannosaurid Dinosaur Aublysodon the Upper Cretaceous of New Mexico Thomas M
J. Paleont., 64(6), 1990, pp. 1026-1032 Copyright © 1990, The Paleontological Society 0022-3360/90/0064-1026S03.00 A PARTIAL SKELETON OF THE TYRANNOSAURID DINOSAUR AUBLYSODON THE UPPER CRETACEOUS OF NEW MEXICO THOMAS M. LEHMAN AND KENNETH CARPENTER Department of Geosciences, Texas Tech University, Lubbock 79409, and Department of Earth Sciences, Denver Museum of Natural History, City Park, Denver, Colorado 80205 Abstract—A fragmentary tyrannosaurid skull and postcranial skeleton from the Kirtland Shale of northwestern New Mexico is the most complete specimen of a carnivorous dinosaur known from these strata. The specimen is identified as Aublysodon cf. A. mirandus on the basis of its narrow frontals, V-shaped frontal-parietal suture, and nondenticulate incisiform premaxillary tooth. The D-shaped cross section of the premaxillary tooth, rugose postorbital, well-developed footed pubis, and proximally constricted third metatarsal confirm the assignment of Aublysodon to the Tyrannosauridae. The limb bones are gracile and similar in proportions to those of Albertosaurus', however, the tibia and metatarsals are shorter relative to the femur. The distal end of the tibia exhibits a unique medial emargination not reported in other tyrannosaurids. INTRODUCTION imen (OMNH 10131) was collected in San Juan County, New Mexico, northeast of Chaco Canyon in June, 1940, by J. W. arge carnivorous dinosaurs were first reported from Up Stovall and D. E. Savage of the University of Oklahoma. The per Cretaceous continental deposits in the San Juan Basin remains comprise several skull fragments, an incomplete den Lof northwestern New Mexico by Barnum Brown (1910, p. 268)tary, parts of both femora, a tibia, pubis, metatarsals, several who found “disassociated limb bones .. -
Sereno 20060098.Vp
Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger PAUL C. SERENO and STEPHEN L. BRUSATTE Sereno, P.C. and Brusatte, S.L. 2008. Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger. Acta Palaeontologica Polonica 53 (1): 15–46. We report the discovery of basal abelisaurid and carcharodontosaurid theropods from the mid Cretaceous (Aptian– Albian, ca. 112 Ma) Elrhaz Formation of the Niger Republic. The abelisaurid, Kryptops palaios gen. et sp. nov., is repre− sented by a single individual preserving the maxilla, pelvic girdle, vertebrae and ribs. Several features, including a maxilla textured externally by impressed vascular grooves and a narrow antorbital fossa, clearly place Kryptops palaios within Abelisauridae as its oldest known member. The carcharodontosaurid, Eocarcharia dinops gen. et sp. nov., is repre− sented by several cranial bones and isolated teeth. Phylogenetic analysis places it as a basal carcharodontosaurid, similar to Acrocanthosaurus and less derived than Carcharodontosaurus and Giganotosaurus. The discovery of these taxa sug− gests that large body size and many of the derived cranial features of abelisaurids and carcharodontosaurids had already evolved by the mid Cretaceous. The presence of a close relative of the North American genus Acrocanthosaurus on Af− rica suggests that carcharodontosaurids had already achieved a trans−Tethyan distribution by the mid Cretaceous. Key words: Theropod, abelisaurid, allosauroid, carcharodontosaurid, Kryptops, Eocarcharia, Cretaceous, Africa. Paul C. Sereno [[email protected]], Department of Organismal Biology and Anatomy, University of Chicago, 1027 E. 57th Street, Chicago, Illinois, 60637, USA; Stephen L. Brusatte [[email protected]], Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, United Kingdom. -
Early Cretaceous) Wessex Formation of the Isle of Wight, Southern England
A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wessex Formation of the Isle of Wight, southern England STEVEN C. SWEETMAN and JAMES D. GARDNER Sweetman, S.C. and Gardner, J.D. 2013. A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wes− sex Formation of the Isle of Wight, southern England. Acta Palaeontologica Polonica 58 (2): 295–324. A new albanerpetontid, Wesserpeton evansae gen. et sp. nov., from the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England, is described. Wesserpeton is established on the basis of a unique combination of primitive and derived characters relating to the frontals and jaws which render it distinct from currently recognized albanerpetontid genera: Albanerpeton (Late Cretaceous to Pliocene of Europe, Early Cretaceous to Paleocene of North America and Late Cretaceous of Asia); Celtedens (Late Jurassic to Early Cretaceous of Europe); and Anoualerpeton (Middle Jurassic of Europe and Early Cretaceous of North Africa). Although Wesserpeton exhibits considerable intraspecific variation in characters pertaining to the jaws and, to a lesser extent, frontals, the new taxon differs from Celtedens in the shape of the internasal process and gross morphology of the frontals in dorsal or ventral view. It differs from Anoualerpeton in the lack of pronounced heterodonty of dentary and maxillary teeth; and in the more medial loca− tion and direction of opening of the suprapalatal pit. The new taxon cannot be referred to Albanerpeton on the basis of the morphology of the frontals. Wesserpeton currently represents the youngest record of Albanerpetontidae in Britain. Key words: Lissamphibia, Albanerpetontidae, microvertebrates, Cretaceous, Britain. Steven C. -
Brains and Intelligence
BRAINS AND INTELLIGENCE The EQ or Encephalization Quotient is a simple way of measuring an animal's intelligence. EQ is the ratio of the brain weight of the animal to the brain weight of a "typical" animal of the same body weight. Assuming that smarter animals have larger brains to body ratios than less intelligent ones, this helps determine the relative intelligence of extinct animals. In general, warm-blooded animals (like mammals) have a higher EQ than cold-blooded ones (like reptiles and fish). Birds and mammals have brains that are about 10 times bigger than those of bony fish, amphibians, and reptiles of the same body size. The Least Intelligent Dinosaurs: The primitive dinosaurs belonging to the group sauropodomorpha (which included Massospondylus, Riojasaurus, and others) were among the least intelligent of the dinosaurs, with an EQ of about 0.05 (Hopson, 1980). Smartest Dinosaurs: The Troodontids (like Troödon) were probably the smartest dinosaurs, followed by the dromaeosaurid dinosaurs (the "raptors," which included Dromeosaurus, Velociraptor, Deinonychus, and others) had the highest EQ among the dinosaurs, about 5.8 (Hopson, 1980). The Encephalization Quotient was developed by the psychologist Harry J. Jerison in the 1970's. J. A. Hopson (a paleontologist from the University of Chicago) did further development of the EQ concept using brain casts of many dinosaurs. Hopson found that theropods (especially Troodontids) had higher EQ's than plant-eating dinosaurs. The lowest EQ's belonged to sauropods, ankylosaurs, and stegosaurids. A SECOND BRAIN? It used to be thought that the large sauropods (like Brachiosaurus and Apatosaurus) and the ornithischian Stegosaurus had a second brain. -
A Troodontid Dinosaur from the Latest Cretaceous of India
ARTICLE Received 14 Dec 2012 | Accepted 7 Mar 2013 | Published 16 Apr 2013 DOI: 10.1038/ncomms2716 A troodontid dinosaur from the latest Cretaceous of India A. Goswami1,2, G.V.R. Prasad3, O. Verma4, J.J. Flynn5 & R.B.J. Benson6 Troodontid dinosaurs share a close ancestry with birds and were distributed widely across Laurasia during the Cretaceous. Hundreds of occurrences of troodontid bones, and their highly distinctive teeth, are known from North America, Europe and Asia. Thus far, however, they remain unknown from Gondwanan landmasses. Here we report the discovery of a troodontid tooth from the uppermost Cretaceous Kallamedu Formation in the Cauvery Basin of South India. This is the first Gondwanan record for troodontids, extending their geographic range by nearly 10,000 km, and representing the first confirmed non-avian tetanuran dinosaur from the Indian subcontinent. This small-bodied maniraptoran dinosaur is an unexpected and distinctly ‘Laurasian’ component of an otherwise typical ‘Gondwanan’ tetrapod assemblage, including notosuchian crocodiles, abelisauroid dinosaurs and gondwanathere mammals. This discovery raises the question of whether troodontids dispersed to India from Laurasia in the Late Cretaceous, or whether a broader Gondwanan distribution of troodontids remains to be discovered. 1 Department of Genetics, Evolution, and Environment, University College London, London WC1E 6BT, UK. 2 Department of Earth Sciences, University College London, London WC1E 6BT, UK. 3 Department of Geology, Centre for Advanced Studies, University of Delhi, New Delhi 110 007, India. 4 Geology Discipline Group, School of Sciences, Indira Gandhi National Open University, New Delhi 110 068, India. 5 Division of Paleontology and Richard Gilder Graduate School, American Museum of Natural History, New York, New York 10024, USA. -
Dinosaurs British Isles
DINOSAURS of the BRITISH ISLES Dean R. Lomax & Nobumichi Tamura Foreword by Dr Paul M. Barrett (Natural History Museum, London) Skeletal reconstructions by Scott Hartman, Jaime A. Headden & Gregory S. Paul Life and scene reconstructions by Nobumichi Tamura & James McKay CONTENTS Foreword by Dr Paul M. Barrett.............................................................................10 Foreword by the authors........................................................................................11 Acknowledgements................................................................................................12 Museum and institutional abbreviations...............................................................13 Introduction: An age-old interest..........................................................................16 What is a dinosaur?................................................................................................18 The question of birds and the ‘extinction’ of the dinosaurs..................................25 The age of dinosaurs..............................................................................................30 Taxonomy: The naming of species.......................................................................34 Dinosaur classification...........................................................................................37 Saurischian dinosaurs............................................................................................39 Theropoda............................................................................................................39 -
Implications for Predatory Dinosaur Macroecology and Ontogeny in Later Late Cretaceous Asiamerica
Canadian Journal of Earth Sciences Theropod Guild Structure and the Tyrannosaurid Niche Assimilation Hypothesis: Implications for Predatory Dinosaur Macroecology and Ontogeny in later Late Cretaceous Asiamerica Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2020-0174.R1 Manuscript Type: Article Date Submitted by the 04-Jan-2021 Author: Complete List of Authors: Holtz, Thomas; University of Maryland at College Park, Department of Geology; NationalDraft Museum of Natural History, Department of Geology Keyword: Dinosaur, Ontogeny, Theropod, Paleocology, Mesozoic, Tyrannosauridae Is the invited manuscript for consideration in a Special Tribute to Dale Russell Issue? : © The Author(s) or their Institution(s) Page 1 of 91 Canadian Journal of Earth Sciences 1 Theropod Guild Structure and the Tyrannosaurid Niche Assimilation Hypothesis: 2 Implications for Predatory Dinosaur Macroecology and Ontogeny in later Late Cretaceous 3 Asiamerica 4 5 6 Thomas R. Holtz, Jr. 7 8 Department of Geology, University of Maryland, College Park, MD 20742 USA 9 Department of Paleobiology, National Museum of Natural History, Washington, DC 20013 USA 10 Email address: [email protected] 11 ORCID: 0000-0002-2906-4900 Draft 12 13 Thomas R. Holtz, Jr. 14 Department of Geology 15 8000 Regents Drive 16 University of Maryland 17 College Park, MD 20742 18 USA 19 Phone: 1-301-405-4084 20 Fax: 1-301-314-9661 21 Email address: [email protected] 22 23 1 © The Author(s) or their Institution(s) Canadian Journal of Earth Sciences Page 2 of 91 24 ABSTRACT 25 Well-sampled dinosaur communities from the Jurassic through the early Late Cretaceous show 26 greater taxonomic diversity among larger (>50kg) theropod taxa than communities of the 27 Campano-Maastrichtian, particularly to those of eastern/central Asia and Laramidia. -
Abelisaurid Pedal Unguals from the Late Cretaceous of India
AsociaciónPaleontológicaArgentina.PublicaciónEspecial7 ISSN0328-347X VIIInternationalSymposiumon MesozoicTerrestrialEcosystems:145-149Buenos. Aires,30-6-2001 AbeliSaurid Pedal unguals from the Late Cretaceous of India Fernando E. NOVAS!and Saswati BANDYOPADHYAY2 Abstraet. The ungual phalanges of theropod dinosaurs discovered in the Lameta Formation (Maastrichtian),centralIndia,exhibitdistinctivecharactersunknownin othertheropods.Hence,their tax- onomic identificationremained obscure since their original description in 1933.Recent discoveriesof abelisauridtheropods in Patagoniaindicate that the phalangesfromIndia belong to the foot of the~e~i- nosaurs. New informationon the foot skeletonof this group of CretaceousGondwanan predators lS m- cluded herein. Key words. Theropoda. Abelisauridae. Unguals. Cretaceous. Gondwana. IntroducTion Xenotarsosaurus; Bonaparte and Novas, 1985; Martínez et al., 1986; Bonaparte et al., 1990), India The Late Cretaceous (Maastrichtian) Lameta ilndosuchus; Chatterjee and Rudra, 1996), and Formation of central India has yielded dissociated el- Madagascar (Majungatholus; Sampson et al., 1998). ements of a variety of predatory dinosaurs. The ma- This considerable amount of information about terials were described by Frederich von Huene (in abelisaurid anatomy has served as a valuable guide Huene and Matley, 1933), who recognized nine to resolve confusing taxonomic aspects of the Indian theropod species from a fossil quarry at Bara Simla theropods. Hill (Madhya Pradesh, India). They are: lndosuchus Currently, lndosuchus, lndosaurus, and also rapiorius Huene, Indosaurus matleyi Huene, Compso- Laeoisuchue, are interpreted as members of suchus solus Huene, Laeoisuchus indicus Huene, Abelisauridae (Bonaparte and Novas, 1985; Molnar, [ubbulpuria tenuis Huene, Coeluroides largus Huene, 1990; Chatterjee and Rudra, 1996; Sampson et al., Dryptosauroides grandis Huene, Ornithomimoides mo- 1998; Novas and Bandyopadhyay, 1999). Moreover, bilis Huene, and Ornithomimoides (?) barasimlensis the controversial taxa "Compsosuchus", "Drypto- Huene. -
Dinosaur Species List E to M
Dinosaur Species List E to M E F G • Echinodon becklesii • Fabrosaurus australis • Gallimimus bullatus • Edmarka rex • Frenguellisaurus • Garudimimus brevipes • Edmontonia longiceps ischigualastensis • Gasosaurus constructus • Edmontonia rugosidens • Fulengia youngi • Gasparinisaura • Edmontosaurus annectens • Fulgurotherium australe cincosaltensis • Edmontosaurus regalis • Genusaurus sisteronis • Edmontosaurus • Genyodectes serus saskatchewanensis • Geranosaurus atavus • Einiosaurus procurvicornis • Gigantosaurus africanus • Elaphrosaurus bambergi • Giganotosaurus carolinii • Elaphrosaurus gautieri • Gigantosaurus dixeyi • Elaphrosaurus iguidiensis • Gigantosaurus megalonyx • Elmisaurus elegans • Gigantosaurus robustus • Elmisaurus rarus • Gigantoscelus • Elopteryx nopcsai molengraaffi • Elosaurus parvus • Gilmoreosaurus • Emausaurus ernsti mongoliensis • Embasaurus minax • Giraffotitan altithorax • Enigmosaurus • Gongbusaurus shiyii mongoliensis • Gongbusaurus • Eoceratops canadensis wucaiwanensis • Eoraptor lunensis • Gorgosaurus lancensis • Epachthosaurus sciuttoi • Gorgosaurus lancinator • Epanterias amplexus • Gorgosaurus libratus • Erectopus sauvagei • "Gorgosaurus" novojilovi • Erectopus superbus • Gorgosaurus sternbergi • Erlikosaurus andrewsi • Goyocephale lattimorei • Eucamerotus foxi • Gravitholus albertae • Eucercosaurus • Gresslyosaurus ingens tanyspondylus • Gresslyosaurus robustus • Eucnemesaurus fortis • Gresslyosaurus torgeri • Euhelopus zdanskyi • Gryponyx africanus • Euoplocephalus tutus • Gryponyx taylori • Euronychodon -
Late Cretaceous) Record of Ornithischia from Africa Matthew .C Lamanna University of Pennsylvania
University of Pennsylvania ScholarlyCommons Departmental Papers (EES) Department of Earth and Environmental Science September 2004 From dinosaurs to dyrosaurids (Crocodyliformes): Removal of the post-Cenomanian (Late Cretaceous) record of Ornithischia from Africa Matthew .C Lamanna University of Pennsylvania Joshua B. Smith University of Pennsylvania, [email protected] Yousry S. Attia Egyptian Geological Survey and Mining Authority Peter Dodson University of Pennsylvania, [email protected] Follow this and additional works at: http://repository.upenn.edu/ees_papers Recommended Citation Lamanna, M. C., Smith, J. B., Attia, Y. S., & Dodson, P. (2004). From dinosaurs to dyrosaurids (Crocodyliformes): Removal of the post-Cenomanian (Late Cretaceous) record of Ornithischia from Africa . Retrieved from http://repository.upenn.edu/ees_papers/31 Copyright The ocS iety of Vertebrate Paleontology. Use for profit not allowed. Reprinted from: Journal of Vertebrate Paleontology, Volume 24, Issue 3, 2004, pages 764-768. Publisher URL: http://www.vertpaleo.org/ This paper is posted at ScholarlyCommons. http://repository.upenn.edu/ees_papers/31 For more information, please contact [email protected]. From dinosaurs to dyrosaurids (Crocodyliformes): Removal of the post- Cenomanian (Late Cretaceous) record of Ornithischia from Africa Abstract Ornithischian dinosaurs are uncommon elements in Late Cretaceous faunal assemblages of many Gondwanan landmasses, particularly Africa. The best-documented post-Cenomanian record of purported ornithischian body fossils from Africa consists of a left umeh rus, with associated cranial and costal fragments, from the Santonian-Campanian Quseir Formation of Kharga Oasis, Egypt (Fig. 1 ) (Awad and Ghobrial, 1966). We show that this specimen pertains instead to a dyrosaurid crocodyliform, and restrict known African ornithischian body fossils to pre-Turonian sediments.