Nedoceratops’: an Example of a Transitional Morphology
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Investigating Sexual Dimorphism in Ceratopsid Horncores
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2013-01-25 Investigating Sexual Dimorphism in Ceratopsid Horncores Borkovic, Benjamin Borkovic, B. (2013). Investigating Sexual Dimorphism in Ceratopsid Horncores (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/26635 http://hdl.handle.net/11023/498 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Investigating Sexual Dimorphism in Ceratopsid Horncores by Benjamin Borkovic A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JANUARY, 2013 © Benjamin Borkovic 2013 Abstract Evidence for sexual dimorphism was investigated in the horncores of two ceratopsid dinosaurs, Triceratops and Centrosaurus apertus. A review of studies of sexual dimorphism in the vertebrate fossil record revealed methods that were selected for use in ceratopsids. Mountain goats, bison, and pronghorn were selected as exemplar taxa for a proof of principle study that tested the selected methods, and informed and guided the investigation of sexual dimorphism in dinosaurs. Skulls of these exemplar taxa were measured in museum collections, and methods of analysing morphological variation were tested for their ability to demonstrate sexual dimorphism in their horns and horncores. -
A Revision of the Ceratopsia Or Horned Dinosaurs
MEMOIRS OF THE PEABODY MUSEUM OF NATURAL HISTORY VOLUME III, 1 A.R1 A REVISION orf tneth< CERATOPSIA OR HORNED DINOSAURS BY RICHARD SWANN LULL STERLING PROFESSOR OF PALEONTOLOGY AND DIRECTOR OF PEABODY MUSEUM, YALE UNIVERSITY LVXET NEW HAVEN, CONN. *933 MEMOIRS OF THE PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY Volume I. Odontornithes: A Monograph on the Extinct Toothed Birds of North America. By Othniel Charles Marsh. Pp. i-ix, 1-201, pis. 1-34, text figs. 1-40. 1880. To be obtained from the Peabody Museum. Price $3. Volume II. Part 1. Brachiospongidae : A Memoir on a Group of Silurian Sponges. By Charles Emerson Beecher. Pp. 1-28, pis. 1-6, text figs. 1-4. 1889. To be obtained from the Peabody Museum. Price $1. Volume III. Part 1. American Mesozoic Mammalia. By George Gaylord Simp- son. Pp. i-xvi, 1-171, pis. 1-32, text figs. 1-62. 1929. To be obtained from the Yale University Press, New Haven, Conn. Price $5. Part 2. A Remarkable Ground Sloth. By Richard Swann Lull. Pp. i-x, 1-20, pis. 1-9, text figs. 1-3. 1929. To be obtained from the Yale University Press, New Haven, Conn. Price $1. Part 3. A Revision of the Ceratopsia or Horned Dinosaurs. By Richard Swann Lull. Pp. i-xii, 1-175, pis. I-XVII, text figs. 1-42. 1933. To be obtained from the Peabody Museum. Price $5 (bound in cloth), $4 (bound in paper). Part 4. The Merycoidodontidae, an Extinct Group of Ruminant Mammals. By Malcolm Rutherford Thorpe. In preparation. -
A Census of Dinosaur Fossils Recovered from the Hell Creek and Lance Formations (Maastrichtian)
The Journal of Paleontological Sciences: JPS.C.2019.01 1 TAKING COUNT: A Census of Dinosaur Fossils Recovered From the Hell Creek and Lance Formations (Maastrichtian). ______________________________________________________________________________________ Walter W. Stein- President, PaleoAdventures 1432 Mill St.. Belle Fourche, SD 57717. [email protected] 605-210-1275 ABSTRACT: A census of Hell Creek and Lance Formation dinosaur remains was conducted from April, 2017 through February of 2018. Online databases were reviewed and curators and collections managers interviewed in an effort to determine how much material had been collected over the past 130+ years of exploration. The results of this new census has led to numerous observations regarding the quantity, quality, and locations of the total collection, as well as ancillary data on the faunal diversity and density of Late Cretaceous dinosaur populations. By reviewing the available data, it was also possible to make general observations regarding the current state of certain exploration programs, the nature of collection bias present in those collections and the availability of today's online databases. A total of 653 distinct, associated and/or articulated remains (skulls and partial skeletons) were located. Ceratopsid skulls and partial skeletons (mostly identified as Triceratops) were the most numerous, tallying over 335+ specimens. Hadrosaurids (Edmontosaurus) were second with at least 149 associated and/or articulated remains. Tyrannosaurids (Tyrannosaurus and Nanotyrannus) were third with a total of 71 associated and/or articulated specimens currently known to exist. Basal ornithopods (Thescelosaurus) were also well represented by at least 42 known associated and/or articulated remains. The remaining associated and/or articulated specimens, included pachycephalosaurids (18), ankylosaurids (6) nodosaurids (6), ornithomimids (13), oviraptorosaurids (9), dromaeosaurids (1) and troodontids (1). -
Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5. -
Raptors in Action 1 Suggested Pre-Visit Activities
PROGRAM OVERVIEW TOPIC: Small theropods commonly known as “raptors.” THEME: Explore the adaptations that made raptors unique and successful, like claws, intelligence, vision, speed, and hollow bones. PROGRAM DESCRIPTION: Razor-sharp teeth and sickle-like claws are just a few of the characteristics that have made raptors famous. Working in groups, students will build a working model of a raptor leg and then bring it to life while competing in a relay race that simulates the hunting techniques of these carnivorous animals. AUDIENCE: Grades 3–6 CURRICULUM CONNECTIONS: Grade 3 Science: Building with a Variety of Materials Grade 3–6 Math: Patterns and Relations Grade 4 Science: Building Devices and Vehicles that Move Grade 6 Science: Evidence and Investigation PROGRAM ObJECTIVES: 1. Students will understand the adaptations that contributed to the success of small theropods. 2. Students will explore the function of the muscles used in vertebrate movement and the mechanics of how a raptor leg works. 3. Students will understand the function of the raptorial claw. 4. Students will discover connections between small theropod dinosaurs and birds. SUGGESTED PRE-VISIT ACTIVITIES UNDERstANDING CLADIstICS Animals and plants are often referred to as part of a family or group. For example, the dog is part of the canine family (along with wolves, coyotes, foxes, etc.). Scientists group living things together based on relationships to gain insight into where they came from. This helps us identify common ancestors of different organisms. This method of grouping is called “cladistics.” Cladistics is a system that uses branches like a family tree to show how organisms are related to one another. -
Dinosaurs, Pollen, and the Cretaceous-Tertiary Boundary in the San Juan Basin Robert M
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/56 Dinosaurs, pollen, and the Cretaceous-Tertiary boundary in the San Juan Basin Robert M. Sullivan, Spencer G. Lucas, and Dennis R. Braman, 2005, pp. 395-407 in: Geology of the Chama Basin, Lucas, Spencer G.; Zeigler, Kate E.; Lueth, Virgil W.; Owen, Donald E.; [eds.], New Mexico Geological Society 56th Annual Fall Field Conference Guidebook, 456 p. This is one of many related papers that were included in the 2005 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. -
Dinosaur Hall Scavenger Hunt We Hope You Enjoy Your Visit to the Museum Today
Dinosaur Hall Scavenger Hunt We hope you enjoy your visit to the museum today. Use this scavenger hunt to explore Dinosaur Hall. Each answer can only be used once! 1. Find at least one animal in Dinosaur Hall that is NOT a dinosaur. Elasmosaurus (above information desk, has flippers, marine reptile), Mosasaur (two Tylosaurus and the Plioplatecarpus, marine reptiles), Sea Turtles, Ichthyosaurus skull, the fish Xiphactinus, Pteranodon (above Time Machine, winged, flying reptile), elephant, various human specimens 2. Find an animal in Dinosaur Hall that did NOT live at the same time as the dinosaurs. Elephant (the leg bone can be found on the right side of Dinosaur Hall as you enter). Human arm bones, same location 3. Find a dinosaur that was a carnivore (ate other animals). Tyrannosaurus rex, Herrerasaurus, Dilophosaurus, Acrocanthosaurus, Giganotosaurus, Deinonychus, Velociraptor, Albertosaurus 4. Find a dinosaur that was an herbivore (ate plants). Torosaurus, Avaceratops, Hadrosaurus foulkii, Chasmosaurus, Corythosaurus, Parasaurolophus, Stegosaurus, Triceratops, Tenontosaurus 5. What fossil(s) are the staff in the Paleo Lab working on? Answers will vary. The Academy takes part in uncovering fossils from all over the world. 6. Find a dinosaur that was discovered in New Jersey. What is special about this dinosaur? Hadrosaurus foulkii (New Jersey) First dinosaur mounted for public display in the world 7. Find a dinosaur that may have had protective body armor. Ankylosaurus, Stegosaurus, Triceratops, Torosaurus, Avaceratops, Chasmosaurus 8. Find a dinosaur that is smaller than Tyrannosaurus rex. Tenontosaurus, Deinonychus, Avaceratops, Velociraptor, Struthiomimus 9. Find a dinosaur that may have used physical displays (parts of its body) for communication. -
Pebblego Animals Article List
PebbleGo Animals Article List AMPHIBIANS Hawks Iguanodon Compsognathus Sauroposeidon Frogs Herons Kentrosaurus Cryolophosaurus Suuwassea Mudpuppies Humboldt Penguins Kritosaurus Dahalokely Thecodontosaurus Newts Hummingbirds Lambeosaurus Daspletosaurus Salamanders Ibises Leaellynasaura Deinocheirus FISH Toads King Penguins Leptoceratops Deinonychus Angelfish Kingfishers Lexovisaurus Deltadromeus Barracudas ANIMAL BEHAVIOR Kiwis Lophorhothon Eoraptor Basking Sharks Animal Communication Little Penguins Maiasaura Eotyrannus Blue Sharks Animals in the Fall Loons Microceratus Falcarius Catfish Hibernation Macaroni Penguins Micropachycephalosaurus Gallimimus Clown Fish Migration Macaws Minmi Gasosaurus Coelacanths Nocturnal Animals Magellanic Penguins Montanoceratops Giganotosaurus Eels Orioles Muttaburrasaurus Guanlong Great White Sharks ANIMAL Ostriches Nedoceratops Herrerasaurus Hammerhead Sharks CLASSIFICATION Owls Nodosaurus Incisivosaurus Mako Sharks About Amphibians Parrots Olorotitan Labocania Megamouth Sharks About Birds Peacocks Oryctodromeus Liliensternus Nurse Sharks About Fish Pelicans Ouranosaurus Masiakasaurus Parrotfish About Insects Pheasants Pachycephalosaurus Metriacanthosaurus Piranhas About Invertebrates Puffins Pachyrhinosaurus Microraptor Puffer Fish About Mammals Quetzals Parasaurolophus Neovenator Salmon About Reptiles Robins Pawpawsaurus Ornithomimus Sea Horses About Spiders Rockhopper Penguins Polacanthus Ozraptor Swordfish Royal Penguins Protoceratops Protarchaeopteryx Stingrays ANIMAL HABITATS Snares Penguins Saurolophus -
A Remarkable Short-Snouted Horned Dinosaur from the Late Cretaceous (Late Campanian) of Southern Laramidia Rspb.Royalsocietypublishing.Org Scott D
A remarkable short-snouted horned dinosaur from the Late Cretaceous (late Campanian) of southern Laramidia rspb.royalsocietypublishing.org Scott D. Sampson1,2,3, Eric K. Lund2,3,4, Mark A. Loewen2,3, Andrew A. Farke5 and Katherine E. Clayton3 1Denver Museum of Nature and Science, 2001 Colorado Boulevard, Denver, CO 80205, USA 2Department of Geology and Geophysics, University of Utah, 115 S 1460 East, Salt Lake City, UT 84112, USA 3Natural History Museum of Utah, University of Utah, 301 Wakara Way, Salt Lake City, UT 84108, USA Research 4Department of Biomedical Sciences, Ohio University, Heritage College of Osteopathic Medicine, Athens, OH 45701, USA Cite this article: Sampson SD, Lund EK, 5Raymond M. Alf Museum of Paleontology, 1175 West Baseline Road, Claremont, CA 91711, USA Loewen MA, Farke AA, Clayton KE. 2013 A remarkable short-snouted horned dinosaur The fossil record of centrosaurine ceratopsids is largely restricted to the from the Late Cretaceous (late Campanian) of northern region of western North America (Alberta, Montana and Alaska). Exceptions consist of single taxa from Utah (Diabloceratops) and China southern Laramidia. Proc R Soc B 280: (Sinoceratops), plus otherwise fragmentary remains from the southern 20131186. Western Interior of North America. Here, we describe a remarkable new http://dx.doi.org/10.1098/rspb.2013.1186 taxon, Nasutoceratops titusi n. gen. et sp., from the late Campanian Kaiparowits Formation of Utah, represented by multiple specimens, including a nearly complete skull and partial postcranial skeleton. Autapomorphies include an enlarged narial region, pneumatic nasal ornamentation, abbreviated snout Received: 13 May 2013 and elongate, rostrolaterally directed supraorbital horncores. -
Transitional Evolutionary Forms in Chasmosaurine Ceratopsid Dinosaurs: Evidence from the Campanian of New Mexico
Transitional evolutionary forms in chasmosaurine ceratopsid dinosaurs: evidence from the Campanian of New Mexico Denver W. Fowler1,2 and Elizabeth A. Freedman Fowler1,2,3 1 Badlands Dinosaur Museum, Dickinson Museum Center, Dickinson, ND, USA 2 Museum of the Rockies, Montana State University, Bozeman, MT, USA 3 Department of Natural Sciences, Dickinson State University, Dickinson, ND, USA ABSTRACT Three new chasmosaurines from the Kirtland Formation (~75.0–73.4 Ma), New Mexico, form morphological and stratigraphic intermediates between Pentaceratops (~74.7–75 Ma, Fruitland Formation, New Mexico) and Anchiceratops (~72–71 Ma, Horseshoe Canyon Formation, Alberta). The new specimens exhibit gradual enclosure of the parietal embayment that characterizes Pentaceratops, providing support for the phylogenetic hypothesis that Pentaceratops and Anchiceratops are closely related. This stepwise change of morphologic characters observed in chasmosaurine taxa that do not overlap stratigraphically is supportive of evolution by anagenesis. Recently published hypotheses that place Pentaceratops and Anchiceratops into separate clades are not supported. This phylogenetic relationship demonstrates unrestricted movement of large-bodied taxa between hitherto purported northern and southern provinces in the late Campanian, weakening support for the hypothesis of extreme faunal provincialism in the Late Cretaceous Western Interior. Subjects Evolutionary Studies, Paleontology Submitted 20 November 2019 Keywords Dinosaur, Cretaceous, Pentaceratops, Anchiceratops, Ceratopsidae, Chasmosaurinae, Accepted 7 May 2020 Anagenesis, Diversity Published 5 June 2020 Corresponding author INTRODUCTION Denver W. Fowler, [email protected] Intermediate or “transitional” fossils are an expected product of evolution, and are Academic editor especially celebrated when they occur within major evolutionary transitions (Anderson & Fabien Knoll Sues, 2007; Wellnhofer, 2010; Daeschler, Shubin & Jenkins, 2006). -
Evolutionary Trends in Triceratops from the Hell Creek Formation, Montana
Evolutionary trends in Triceratops from the Hell Creek Formation, Montana John B. Scannellaa,b,1, Denver W. Fowlera,b, Mark B. Goodwinc, and John R. Hornera,b aMuseum of the Rockies and bDepartment of Earth Sciences, Montana State University, Bozeman, MT 59717; and cMuseum of Paleontology, University of California, Berkeley, CA 94720 Edited by Gene Hunt, Smithsonian Institution, Washington, DC, and accepted by the Editorial Board June 1, 2014 (received for review July 16, 2013) The placement of over 50 skulls of the well-known horned consideration of morphological variation in a detailed stratigraphic dinosaur Triceratops within a stratigraphic framework for the Up- context is necessary to reassess systematic hypotheses. per Cretaceous Hell Creek Formation (HCF) of Montana reveals the evolutionary transformation of this genus. Specimens referable to Results the two recognized morphospecies of Triceratops, T. horridus and Stratigraphic placement of Triceratops specimens within the HCF T. prorsus, are stratigraphically separated within the HCF with the reveals previously undocumented shifts in morphology. The T. prorsus morphology recovered in the upper third of the forma- HCF is divided into three stratigraphic units: the lower third tion and T. horridus found lower in the formation. Hypotheses (L3), middle third (M3), and upper third (U3) (1, 21). The that these morphospecies represent sexual or ontogenetic variation stratigraphic separation of Triceratops morphospecies is apparent within a single species are thus untenable. Stratigraphic placement with specimens referable to T. prorsus (following Forster) (12) – of specimens appears to reveal ancestor descendant relationships. found in U3 and T. horridus recovered only lower in the HCF. Transitional morphologies are found in the middle unit of the for- Specimens from the upper part of M3 exhibit a combination of Triceratops mation, a finding that is consistent with the evolution of T.