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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. -
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. -
Preliminary Report on the Octocorals (Cnidaria: Anthozoa: Octocorallia) from the Ogasawara Islands
国立科博専報，(52), pp. 65–94 , 2018 年 3 月 28 日 Mem. Natl. Mus. Nat. Sci., Tokyo, (52), pp. 65–94, March 28, 2018 Preliminary Report on the Octocorals (Cnidaria: Anthozoa: Octocorallia) from the Ogasawara Islands Yukimitsu Imahara1* and Hiroshi Namikawa2 1Wakayama Laboratory, Biological Institute on Kuroshio, 300–11 Kire, Wakayama, Wakayama 640–0351, Japan *E-mail: [email protected] 2Showa Memorial Institute, National Museum of Nature and Science, 4–1–1 Amakubo, Tsukuba, Ibaraki 305–0005, Japan Abstract. Approximately 400 octocoral specimens were collected from the Ogasawara Islands by SCUBA diving during 2013–2016 and by dredging surveys by the R/V Koyo of the Tokyo Met- ropolitan Ogasawara Fisheries Center in 2014 as part of the project “Biological Properties of Bio- diversity Hotspots in Japan” at the National Museum of Nature and Science. Here we report on 52 lots of these octocoral specimens that have been identified to 42 species thus far. The specimens include seven species of three genera in two families of Stolonifera, 25 species of ten genera in two families of Alcyoniina, one species of Scleraxonia, and nine species of four genera in three families of Pennatulacea. Among them, three species of Stolonifera: Clavularia cf. durum Hick- son, C. cf. margaritiferae Thomson & Henderson and C. cf. repens Thomson & Henderson, and five species of Alcyoniina: Lobophytum variatum Tixier-Durivault, L. cf. mirabile Tixier- Durivault, Lohowia koosi Alderslade, Sarcophyton cf. boletiforme Tixier-Durivault and Sinularia linnei Ofwegen, are new to Japan. In particular, Lohowia koosi is the first discovery since the orig- inal description from the east coast of Australia. -
New Heterodontosaurid Remains from the Cañadón Asfalto Formation: Cursoriality and the Functional Importance of the Pes in Small Heterodontosaurids
Journal of Paleontology, 90(3), 2016, p. 555–577 Copyright © 2016, The Paleontological Society 0022-3360/16/0088-0906 doi: 10.1017/jpa.2016.24 New heterodontosaurid remains from the Cañadón Asfalto Formation: cursoriality and the functional importance of the pes in small heterodontosaurids Marcos G. Becerra,1 Diego Pol,1 Oliver W.M. Rauhut,2 and Ignacio A. Cerda3 1CONICET- Museo Palaeontológico Egidio Feruglio, Fontana 140, Trelew, Chubut 9100, Argentina 〈[email protected]〉; 〈[email protected]〉 2SNSB, Bayerische Staatssammlung für Paläontologie und Geologie and Department of Earth and Environmental Sciences, LMU München, Richard-Wagner-Str. 10, Munich 80333, Germany 〈[email protected]〉 3CONICET- Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Museo Carlos Ameghino, Belgrano 1700, Paraje Pichi Ruca (predio Marabunta), Cipolletti, Río Negro, Argentina 〈[email protected]〉 Abstract.—New ornithischian remains reported here (MPEF-PV 3826) include two complete metatarsi with associated phalanges and caudal vertebrae, from the late Toarcian levels of the Cañadón Asfalto Formation. We conclude that these fossil remains represent a bipedal heterodontosaurid but lack diagnostic characters to identify them at the species level, although they probably represent remains of Manidens condorensis, known from the same locality. Histological features suggest a subadult ontogenetic stage for the individual. A cluster analysis based on pedal measurements identifies similarities of this specimen with heterodontosaurid taxa and the inclusion of the new material in a phylogenetic analysis with expanded character sampling on pedal remains confirms the described specimen as a heterodontosaurid. Finally, uncommon features of the digits (length proportions among nonungual phalanges of digit III, and claw features) are also quantitatively compared to several ornithischians, theropods, and birds, suggesting that this may represent a bipedal cursorial heterodontosaurid with gracile and grasping feet and long digits. -
Continental Complexities: a Multidisciplinary Introduction to Africa
Continental Complexities A Multidisciplinary Introduction to Africa By Dr. Ibigbolade Simon Aderibigbe and Dr. Akinloye Ojo Included in this preview: • Table of Contents • Chapter 1 & 2 For additional information on adopting this book for your class, please contact us at 800.200.3908 x501 or via e-mail at [email protected] Dpoujofoubm!Dpnqmfyjujft A MULTIDISCIPLINARY INTRODUCTION TO AFRICA Revised Edition Edited by Ibigbolade Aderibigbe and Akinloye Ojo University of Georgia Bassim Hamadeh, CEO and Publisher Christopher Foster, General Vice President Michael Simpson, Vice President of Acquisitions Jessica Knott, Managing Editor Kevin Fahey, Cognella Marketing Manager Jess Busch, Senior Graphic Designer Zina Craft , Acquisitions Editor Jamie Giganti, Project Editor Brian Fahey, Licensing Associate Copyright © 2013 by Cognella, Inc. All rights reserved. No part of this publication may be reprinted, reproduced, transmitted, or utilized in any form or by any electronic, mechanical, or other means, now known or hereaft er invented, including photocopying, microfi lming, and recording, or in any information retrieval system without the written permission of Cognella, Inc. First published in the United States of America in 2013 by Cognella, Inc. Trademark Notice: Product or corporate names may be trademarks or registered trademarks, and are used only for identifi cation and explanation without intent to infringe. Printed in the United States of America ISBN: 978-1-62131-133-1 (pbk) Contents The Study of Africa: An Introduction 1 Ibigbolade Aderibigbe -
KENNETH CARPENTER, Ph.D. Director and Curator Of
KENNETH CARPENTER, Ph.D. Director and Curator of Paleontology Prehistoric Museum Utah State University - College of Eastern Utah 155 East Main Street Price, Utah 84501 Education May, 1996. Ph.D., Geology University of Colorado, Boulder, CO. Dissertation “Sharon Springs Member, Pierre Shale (Lower Campanian) depositional environment and origin of it' s Vertebrate fauna, with a review of North American plesiosaurs” 251 p. May, 1980. B.S. in Geology, University of Colorado, Boulder, CO. Aug-Dec. 1977 Apprenticeship, Smithsonian Inst., Washington DC Professional Museum Experience 1975 – 1980: University of Colorado Museum, Boulder, CO. 1983 – 1984: Mississippi Museum of Natural History, Jackson, MS. 1984 – 1986: Academy of Natural Sciences of Philadelphia, Philadelphia. 1986: Carnegie Museum of Natural History, Pittsburgh, PA. 1986: Oklahoma Museum of Natural History, Norman, OK. 1987 – 1989: Museum of the Rockies, Bozeman, MT. 1989 – 1996: Chief Preparator, Denver Museum of Nature and Science, Denver, CO. 1996 – 2010: Chief Preparator, and Curator of Vertebrate Paleontology, Denver Museum of Nature and Science, Denver, CO. 2006 – 2007; 2008-2009: Acting Department Head, Chief Preparator, and Curator of Vertebrate Paleontology, Denver Museum of Nature and Science, Denver, CO. 2010 – present: Director, Prehistoric Museum, Price, UT 2010 – present: Associate Vice Chancellor, Utah State University Professional Services: 1991 – 1998: Science Advisor, Garden Park Paleontological Society 1994: Senior Organizer, Symposium "The Upper Jurassic Morrison Formation: An Interdisciplinary Study" 1996: Scientific Consultant Walking With Dinosaurs , BBC, England 2000: Scientific Consultant Ballad of Big Al , BBC, England 2000 – 2003: Associate Editor, Journal of Vertebrate Paleontology 2001 – 2003: Associate Editor, Earth Sciences History journal 2003 – present: Scientific Advisor, HAN Project 21 Dinosaur Expos, Tokyo, Japan. -
Abelisaurus Comahuensis 321 Acanthodiscus Sp. 60, 64
Index Page numbers in italic denote figure. Page numbers in bold denote tables. Abelisaurus comahuensis 321 structure 45-50 Acanthodiscus sp. 60, 64 Andean Fold and Thrust Belt 37-53 Acantholissonia gerthi 61 tectonic evolution 50-53 aeolian facies tectonic framework 39 Huitrin Formation 145, 151-152, 157 Andes, Neuqu6n 2, 3, 5, 6 Troncoso Member 163-164, 167, 168 morphostructural units 38 aeolian systems, flooded 168, 169, 170, 172, stratigraphy 40 174-182 tectonic evolution, 15-32, 37-39, 51 Aeolosaurus 318 interaction with Neuqu6n Basin 29-30 Aetostreon 200, 305 Andes, topography 37 Afropollis 76 Andesaurus delgadoi 318, 320 Agrio Fold and Thrust Belt 3, 16, 18, 29, 30 andesite 21, 23, 26, 42, 44 development 41 anoxia see dysoxia-anoxia stratigraphy 39-40, 40, 42 Aphrodina 199 structure 39, 42-44, 47 Aphrodina quintucoensis 302 uplift Late Cretaceous 43-44 Aptea notialis 75 Agrio Formation Araucariacites australis 74, 75, 76 ammonite biostratigraphy 58, 61, 63, 65, 66, Araucarioxylon 95,273-276 67 arc morphostructural units 38 bedding cycles 232, 234-247 Arenicolites 193, 196 calcareous nannofossil biostratigraphy 68, 71, Argentiniceras noduliferum 62 72 biozone 58, 61 highstand systems tract 154 Asteriacites 90, 91,270 lithofacies 295,296, 297, 298-302 Asterosoma 86 92 marine facies 142-143, 144, 153 Auca Mahuida volcano 25, 30 organic facies 251-263 Aucasaurus garridoi 321 palaeoecology 310, 311,312 Auquilco evaporites 42 palaeoenvironment 309- 310, 311, Avil6 Member 141,253, 298 312-313 ammonites 66 palynomorph biostratigraphy 74, -
The Origin and Early Evolution of Dinosaurs
Biol. Rev. (2010), 85, pp. 55–110. 55 doi:10.1111/j.1469-185X.2009.00094.x The origin and early evolution of dinosaurs Max C. Langer1∗,MartinD.Ezcurra2, Jonathas S. Bittencourt1 and Fernando E. Novas2,3 1Departamento de Biologia, FFCLRP, Universidade de S˜ao Paulo; Av. Bandeirantes 3900, Ribeir˜ao Preto-SP, Brazil 2Laboratorio de Anatomia Comparada y Evoluci´on de los Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Avda. Angel Gallardo 470, Cdad. de Buenos Aires, Argentina 3CONICET (Consejo Nacional de Investigaciones Cient´ıficas y T´ecnicas); Avda. Rivadavia 1917 - Cdad. de Buenos Aires, Argentina (Received 28 November 2008; revised 09 July 2009; accepted 14 July 2009) ABSTRACT The oldest unequivocal records of Dinosauria were unearthed from Late Triassic rocks (approximately 230 Ma) accumulated over extensional rift basins in southwestern Pangea. The better known of these are Herrerasaurus ischigualastensis, Pisanosaurus mertii, Eoraptor lunensis,andPanphagia protos from the Ischigualasto Formation, Argentina, and Staurikosaurus pricei and Saturnalia tupiniquim from the Santa Maria Formation, Brazil. No uncontroversial dinosaur body fossils are known from older strata, but the Middle Triassic origin of the lineage may be inferred from both the footprint record and its sister-group relation to Ladinian basal dinosauromorphs. These include the typical Marasuchus lilloensis, more basal forms such as Lagerpeton and Dromomeron, as well as silesaurids: a possibly monophyletic group composed of Mid-Late Triassic forms that may represent immediate sister taxa to dinosaurs. The first phylogenetic definition to fit the current understanding of Dinosauria as a node-based taxon solely composed of mutually exclusive Saurischia and Ornithischia was given as ‘‘all descendants of the most recent common ancestor of birds and Triceratops’’. -
Plumulitid Machaeridian Remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia
NORWEGIAN JOURNAL OF GEOLOGY Plumulitid mochoeridion remains from the Silurion, Arctic Russio 53 Plumulitid machaeridian remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia Anette E.S. Hogstrom, Olga K. Bogolepova & Alexander P. Gubanov Hogstrom, A.E.S., Bogolepova, O.K. and Gubanov, A.P.: Plumulitid machaeridian remains from the Silurian (Telychian) of Sevemaya Zemlya, Arc tic Russia. Norsk Geologisk Tidsskrift, Vol. 82, pp. 53-55. Trondheim 2002, ISSN 029-196X. The machaeridian genus Plumulites is reported for the first time from the Severnaya ZemlyaArchipelago of Arctic Russia, where it occurs in limes tone concretions within the Sredninskaya Formation. Graptolites fromthe same concretions indicate the late crispus- griestoniensisBiozones of the mid Telychian (Uandovery). Similarities to plumulitid sclerites from the Upper Ordovician of the Tairnyr Peninsula promotes further interest in machaeridian faunas fromthis region. A.E.S. Hogstromi, O.K. Bogolepova and A.P. Gubanov, Historical Geology & Palaeontology, Dept. of Earth Sciences, Uppsala University, Norbyviigen 22, SE-752 36, Uppsala, Sweden. I Temporaryaddress: Dept. of Earth Sciences, Wills Memorial Building, Queen's Road, Bristol BSB l RJ, UK. lntroduction Stratigraphy and locality The global record of Silurian machaeridians is limited, Machaeridians discussed herein originate from the but includes rare articulated specimens, and more com Lower Silurian Sredninskaya Formation (Matukhin et monly isolated sclerites that have been found in Britain al. 1999). To avoid nomenclatural questions, it should (de Koninck 1857; Woodward 1865; Withers 1926 and be noted that these rocks were previously referred to as Adrain et al. 1991), the Baltic Region (Aurivillius 1892; the Golomaynnaya Formation (Menner et al. -
A Phylogenetic Analysis of the Basal Ornithischia (Reptilia, Dinosauria)
A PHYLOGENETIC ANALYSIS OF THE BASAL ORNITHISCHIA (REPTILIA, DINOSAURIA) Marc Richard Spencer A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements of the degree of MASTER OF SCIENCE December 2007 Committee: Margaret M. Yacobucci, Advisor Don C. Steinker Daniel M. Pavuk © 2007 Marc Richard Spencer All Rights Reserved iii ABSTRACT Margaret M. Yacobucci, Advisor The placement of Lesothosaurus diagnosticus and the Heterodontosauridae within the Ornithischia has been problematic. Historically, Lesothosaurus has been regarded as a basal ornithischian dinosaur, the sister taxon to the Genasauria. Recent phylogenetic analyses, however, have placed Lesothosaurus as a more derived ornithischian within the Genasauria. The Fabrosauridae, of which Lesothosaurus was considered a member, has never been phylogenetically corroborated and has been considered a paraphyletic assemblage. Prior to recent phylogenetic analyses, the problematic Heterodontosauridae was placed within the Ornithopoda as the sister taxon to the Euornithopoda. The heterodontosaurids have also been considered as the basal member of the Cerapoda (Ornithopoda + Marginocephalia), the sister taxon to the Marginocephalia, and as the sister taxon to the Genasauria. To reevaluate the placement of these taxa, along with other basal ornithischians and more derived subclades, a phylogenetic analysis of 19 taxonomic units, including two outgroup taxa, was performed. Analysis of 97 characters and their associated character states culled, modified, and/or rescored from published literature based on published descriptions, produced four most parsimonious trees. Consistency and retention indices were calculated and a bootstrap analysis was performed to determine the relative support for the resultant phylogeny. The Ornithischia was recovered with Pisanosaurus as its basalmost member. -
Comprehensive Phylogenomic Analyses Resolve Cnidarian Relationships and the Origins of Key Organismal Traits
Comprehensive phylogenomic analyses resolve cnidarian relationships and the origins of key organismal traits Ehsan Kayal1,2, Bastian Bentlage1,3, M. Sabrina Pankey5, Aki H. Ohdera4, Monica Medina4, David C. Plachetzki5*, Allen G. Collins1,6, Joseph F. Ryan7,8* Authors Institutions: 1. Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution 2. UPMC, CNRS, FR2424, ABiMS, Station Biologique, 29680 Roscoff, France 3. Marine Laboratory, university of Guam, UOG Station, Mangilao, GU 96923, USA 4. Department of Biology, Pennsylvania State University, University Park, PA, USA 5. Department of Molecular, Cellular and Biomedical Sciences, University of New Hampshire, Durham, NH, USA 6. National Systematics Laboratory, NOAA Fisheries, National Museum of Natural History, Smithsonian Institution 7. Whitney Laboratory for Marine Bioscience, University of Florida, St Augustine, FL, USA 8. Department of Biology, University of Florida, Gainesville, FL, USA PeerJ Preprints | https://doi.org/10.7287/peerj.preprints.3172v1 | CC BY 4.0 Open Access | rec: 21 Aug 2017, publ: 21 Aug 20171 Abstract Background: The phylogeny of Cnidaria has been a source of debate for decades, during which nearly all-possible relationships among the major lineages have been proposed. The ecological success of Cnidaria is predicated on several fascinating organismal innovations including symbiosis, colonial body plans and elaborate life histories, however, understanding the origins and subsequent diversification of these traits remains difficult due to persistent uncertainty surrounding the evolutionary relationships within Cnidaria. While recent phylogenomic studies have advanced our knowledge of the cnidarian tree of life, no analysis to date has included genome scale data for each major cnidarian lineage. Results: Here we describe a well-supported hypothesis for cnidarian phylogeny based on phylogenomic analyses of new and existing genome scale data that includes representatives of all cnidarian classes. -
Vertebrate Remains Are Relatively Well Known in Late Jurassic Deposits of Western Cuba. the Fossil Specimens That Have Been Coll
Paleontología Mexicana, 3 (65): 24-39 (versión impresa), 4: 24-39 (versión electrónica) Catalogue of late jurassiC VerteBrate (pisCes, reptilian) speCiMens froM western CuBa Manuel Iturralde-Vinent ¹, *, Yasmani Ceballos Izquierdo ² A BSTRACT Vertebrate remains are relatively well known in Late Jurassic deposits of western Cuba. The fossil specimens that have been collected so far are dispersed in museum collections around the world and some have been lost throughout the years. A reas- sessment of the fossil material stored in some of these museums’ collections has generated new data about the fossil-bearing lo- calities and greatly increased the number of formally identified specimens. The identified bone elements and taxa suggest a high vertebrate diversity dominated by actinopterygians and reptiles, including: long-necked plesiosaurs, pliosaurs, metriorhynchid crocodilians, pleurodiran turtles, ichthyosaurs, pterosaurs, and sauropod dinosaurs. This assemblage is commonly associated with unidentified remains of terrestrial plants and rare microor- ganisms, as well as numerous marine invertebrates such as am- monites, belemnites, pelecypods, brachiopods, and ostracods. This fossil assemblage is particularly valuable because it includes the most complete marine reptile record of a chronostratigraphic interval, which is poor in vertebrate remains elsewhere. In this contribution, the current status of the available vertebrate fossil specimens from the Late Jurassic of western Cuba is provided, along with a brief description of the fossil materials. Key words: Late Jurassic, Oxfordian, dinosaur, marine reptiles, fish, western Cuba. I NTRODUCTION Since the early 20th century, different groups of collectors have discovered 1 Retired curator, Museo a relatively rich and diverse vertebrate assemblage in the Late Jurassic stra- Nacional de Historia Natural, ta of western Cuba, which has been only partially investigated (Brown and Havana, Cuba.