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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. -
PDF of Manuscript and Figures
The triple origin of whales DAVID PETERS Independent Researcher 311 Collinsville Avenue, Collinsville, IL 62234, USA [email protected] 314-323-7776 July 13, 2018 RH: PETERS—TRIPLE ORIGIN OF WHALES Keywords: Cetacea, Mysticeti, Odontoceti, Phylogenetic analyis ABSTRACT—Workers presume the traditional whale clade, Cetacea, is monophyletic when they support a hypothesis of relationships for baleen whales (Mysticeti) rooted on stem members of the toothed whale clade (Odontoceti). Here a wider gamut phylogenetic analysis recovers Archaeoceti + Odontoceti far apart from Mysticeti and right whales apart from other mysticetes. The three whale clades had semi-aquatic ancestors with four limbs. The clade Odontoceti arises from a lineage that includes archaeocetids, pakicetids, tenrecs, elephant shrews and anagalids: all predators. The clade Mysticeti arises from a lineage that includes desmostylians, anthracobunids, cambaytheres, hippos and mesonychids: none predators. Right whales are derived from a sister to Desmostylus. Other mysticetes arise from a sister to the RBCM specimen attributed to Behemotops. Basal mysticetes include Caperea (for right whales) and Miocaperea (for all other mysticetes). Cetotheres are not related to aetiocetids. Whales and hippos are not related to artiodactyls. Rather the artiodactyl-type ankle found in basal archaeocetes is also found in the tenrec/odontocete clade. Former mesonychids, Sinonyx and Andrewsarchus, nest close to tenrecs. These are novel observations and hypotheses of mammal interrelationships based on morphology and a wide gamut taxon list that includes relevant taxa that prior studies ignored. Here some taxa are tested together for the first time, so they nest together for the first time. INTRODUCTION Marx and Fordyce (2015) reported the genesis of the baleen whale clade (Mysticeti) extended back to Zygorhiza, Physeter and other toothed whales (Archaeoceti + Odontoceti). -
Barren Ridge FEIS-Volume IV Paleo Tech Rpt Final March
March 2011 BARREN RIDGE RENEWABLE TRANSMISSION PROJECT Paleontological Resources Assessment Report PROJECT NUMBER: 115244 PROJECT CONTACT: MIKE STRAND EMAIL: [email protected] PHONE: 714-507-2710 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT Paleontological Resources Assessment Report PREPARED FOR: LOS ANGELES DEPARTMENT OF WATER AND POWER 111 NORTH HOPE STREET LOS ANGELES, CA 90012 PREPARED BY: POWER ENGINEERS, INC. 731 EAST BALL ROAD, SUITE 100 ANAHEIM, CA 92805 DEPARTMENT OF PALEOSERVICES SAN DIEGO NATURAL HISTORY MUSEUM PO BOX 121390 SAN DIEGO, CA 92112 ANA 032-030 (PER-02) LADWP (MARCH 2011) SB 115244 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT TABLE OF CONTENTS 1.0 INTRODUCTION ........................................................................................................................... 1 1.1 STUDY PERSONNEL ....................................................................................................................... 2 1.2 PROJECT DESCRIPTION .................................................................................................................. 2 1.2.1 Construction of New 230 kV Double-Circuit Transmission Line ........................................ 4 1.2.2 Addition of New 230 kV Circuit ......................................................................................... 14 1.2.3 Reconductoring of Existing Transmission Line .................................................................. 14 1.2.4 Construction of New Switching Station ............................................................................. -
Proceedings of the United States National Museum
DESCRIPTION OF TWO SQUALODONTS RECENTLY DIS- COVERED IN THE CALVERT CLIFFS, ^LVRYLAND; AND NOTES ON THE SHARK-TOOTHED CETACEANS. By Remington Kellogg, Of the Bureau of Biological Survey, United States Departynent of Agriculture. INTRODUCTION. When the study of paleontology was less advanced than it is at present, any announcement of the discovery of prehistoric animals unlike the living indigenous fauna was usually received with some suspicion. In spite of this distrust, many attempts were made by the early writers to explain the presence of fossil remains of marine mammals in strata above the sea level or at some distance from the seashore. In one of these treatises ' is found what is, apparently, the first notice of the occurrence of fossil remains referable to shark- toothed cetaceans. The author of this work figures a fragment of a mandible, obtained from the tufa of Malta, which possesses three serrate double-rooted molar teeth. Squalodonts as such were first brought to the attention of ]mleon- tologists in 1840, by J. P. S. Grateloup, ' a French naturalist primarily interested in marine invertebrates. In the original description of Squalodon, Grateloup held the view that this rostral fragment from Leognan, France, belonged to some large saurian related to Iguanodon. Following the anouncement of this discovery. Von Meyer ^ called at- tention to the teeth of this fossil, and concluded that the specimen was referable to some flesh-eating cetacean. A year later, Grateloup* concurred in this opinion. One other specimen should be mentioned in this connection, but, unfortunately, its relationships are quite uncer- tain. This specimen consists of a single tooth which was thought to bear resemblance to some pinniped by Von Meyer ^ and named Pachy- odon mirahilis. -
How to Cite Complete Issue More Information About This Article
Boletín de la Sociedad Geológica Mexicana ISSN: 1405-3322 Sociedad Geológica Mexicana, A.C. Hernández Cisneros, Atzcalli Ehécatl; González Barba, Gerardo; Fordyce, Robert Ewan Oligocene cetaceans from Baja California Sur, Mexico Boletín de la Sociedad Geológica Mexicana, vol. 69, no. 1, January-April, 2017, pp. 149-173 Sociedad Geológica Mexicana, A.C. Available in: http://www.redalyc.org/articulo.oa?id=94350664007 How to cite Complete issue Scientific Information System Redalyc More information about this article Network of Scientific Journals from Latin America and the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Project academic non-profit, developed under the open access initiative Boletín de la Sociedad Geológica Mexicana / 2017 / 149 Oligocene cetaceans from Baja California Sur, Mexico Atzcalli Ehécatl Hernández Cisneros, Gerardo González Barba, Robert Ewan Fordyce ABSTRACT Atzcalli Ehecatl Hernández Cisneros ABSTRACT RESUMEN [email protected] Museo de Historia Natural de la Universidad Autónoma de Baja California Sur, Univer- Baja California Sur has an import- Baja California Sur tiene un importante re- sidad Autónoma de Baja California Sur, ant Cenozoic marine fossil record gistro de fósiles marinos del Cenozoico que Carretera al Sur Km 5.5, Apartado Postal which includes diverse but poorly incluye los restos poco conocidos de cetáceos 19-B, C.P. 23080, La Paz, Baja California Sur, México. known Oligocene cetaceans from del Oligoceno de México. En este estudio Instituto Politécnico Nacional, Centro Inter- Mexico. Here we review the cetacean ofrecemos más detalles sobre estos fósiles de disciplinario de Ciencias Marinas (CICMAR), fossil record including new observa- cetáceos, incluyendo nuevas observaciones Av. Instituto Politécnico Nacional s/n, Col. -
Miocene Leatherback Turtle Material of the Genus Psephophorus (Testudines: Dermochelyoidea) from the Gram Formation (Denmark)
ISSN: 0211-8327 Studia Palaeocheloniologica IV: pp. 205-216 MIOCENE LEATHERBACK TURTLE MATERIAL OF THE GENUS PSEPHOPHORUS (TESTUDINES: DERMOCHELYOIDEA) FROM THE GRAM FORMATION (DENMARK) [Tortugas de cuero miocénicas del género Psephophorus (Testudines: Dermochelyoidea) de la Formación Gram (Dinamarca)] Hans-Volker KARL 1,2, Bent E. K. LINDOW 3 & Thomas TÜT K EN 4 1 Thüringisches Landesamt für Denkmalpflege und Archäologie (TLDA). Humboldtstr. 11. D-99423, Weimar, Germany. Email: [email protected] 2c\o Geobiology, Center of Earth Sciences at the University of Göttingen. Goldschmidtstraße 3. DE-37077 Göttingen, Germany 3 Natural History Museum of Denmark. University of Copenhagen. Øster Voldgade 5-7. DK-1350 Copenhagen K, Denmark. Email: [email protected] 4 Emmy Noether-Gruppe “Knochengeochemie”. Steinmann Institut für Geologie, Mineralogie und Paläontologie. Arbeitsbereich Mineralogie-Petrologie. Rheinische Friedrich-Wilhelms-Universität Bonn. Poppelsdorfer Schloß. 53115 Bonn, Germany. (FECHA DE RECEPCIÓN: 2011-01-12) BIBLID [0211-8327 (2012) Vol. espec. 9; 205-216] ABSTRACT: Several specimens of fossil leatherback turtle from the upper Miocene (Tortonian) Gram Formation are described and illustrated scientifically for the first time. The specimens are all referred to the taxon Psephophorus polygonus and constitute the northernmost occurrence of this taxon in the geological record. Additionally, they indicate that leatherback turtles were a common constituent of the marine fauna of the Late Miocene North Sea Basin. Key words: Testudines, Psephophorus, Miocene, Gram Formation, Denmark. RESUMEN: Se describen y figuran por primera vez algunos ejemplares de tortugas de cuero fósiles del Mioceno superior (Tortoniense) de la Formación Gram, en © Ediciones Universidad de Salamanca Studia Palaeocheloniologica IV (Stud. Geol. Salmant. -
The Upper Miocene Deurne Member of the Diest
GEOLOGICA BELGICA (2020) 23/3-4: 219-252 The upper Miocene Deurne Member of the Diest Formation revisited: unexpected results from the study of a large temporary outcrop near Antwerp International Airport, Belgium Stijn GOOLAERTS1,*, Jef DE CEUSTER2, Frederik H. MOLLEN3, Bert GIJSEN3, Mark BOSSELAERS1, Olivier LAMBERT1, Alfred UCHMAN4, Michiel VAN HERCK5, Rieko ADRIAENS6, Rik HOUTHUYS7, Stephen LOUWYE8, Yaana BRUNEEL5, Jan ELSEN5 & Kristiaan HOEDEMAKERS1 1 OD Earth & History of Life, Scientific Heritage Service and OD Natural Environment, Royal Belgian Institute of Natural Sciences, Belgium; [email protected]; [email protected]; [email protected]; [email protected]. 2 Veldstraat 42, 2160 Wommelgem, Belgium; [email protected]. 3 Elasmobranch Research Belgium, Rehaegenstraat 4, 2820 Bonheiden, Belgium; [email protected]; [email protected]. 4 Faculty of Geography and Geology, Institute of Geological Sciences, Jagiellonian University, Gronostajowa 3a, 30-387 Kraków, Poland; [email protected]. 5 Department of Earth & Environmental Sciences, KU Leuven, Belgium; [email protected]; [email protected]; [email protected]. 6 Q Mineral, Heverlee, Belgium; [email protected]. 7 Independent consultant, Halle, Belgium; [email protected]. 8 Department of Geology, Campus Sterre, S8, Krijgslaan 281, 9000 Gent, Belgium; [email protected]. * corresponding author. ABSTRACT. A 5.50 m thick interval of fossiliferous intensely bioturbated -
The Taxonomic and Evolutionary History of Fossil and Modern Balaenopteroid Mysticetes
Journal of Mammalian Evolution, Vol. 12, Nos. 1/2, June 2005 (C 2005) DOI: 10.1007/s10914-005-6944-3 The Taxonomic and Evolutionary History of Fossil and Modern Balaenopteroid Mysticetes Thomas A. Demer´ e,´ 1,4 Annalisa Berta,2 and Michael R. McGowen2,3 Balaenopteroids (Balaenopteridae + Eschrichtiidae) are a diverse lineage of living mysticetes, with seven to ten species divided between three genera (Megaptera, Balaenoptera and Eschrichtius). Extant members of the Balaenopteridae (Balaenoptera and Megaptera) are characterized by their engulfment feeding behavior, which is associated with a number of unique cranial, mandibular, and soft anatomical characters. The Eschrichtiidae employ suction feeding, which is associated with arched rostra and short, coarse baleen. The recognition of these and other characters in fossil balaenopteroids, when viewed in a phylogenetic framework, provides a means for assessing the evolutionary history of this clade, including its origin and diversification. The earliest fossil balaenopterids include incomplete crania from the early late Miocene (7–10 Ma) of the North Pacific Ocean Basin. Our preliminary phylogenetic results indicate that the basal taxon, “Megaptera” miocaena should be reassigned to a new genus based on its possession of primitive and derived characters. The late late Miocene (5–7 Ma) balaenopterid record, except for Parabalaenoptera baulinensis and Balaenoptera siberi, is largely undescribed and consists of fossil specimens from the North and South Pacific and North Atlantic Ocean basins. The Pliocene record (2–5 Ma) is very diverse and consists of numerous named, but problematic, taxa from Italy and Belgium, as well as unnamed taxa from the North and South Pacific and eastern North Atlantic Ocean basins. -
A New Species of Middle Miocene Baleen Whale from the Nupinai Group, Hikatagawa Formation of Hokkaido, Japan
A new species of Middle Miocene baleen whale from the Nupinai Group, Hikatagawa Formation of Hokkaido, Japan Yoshihiro Tanaka1,2,3, Tatsuro Ando4 and Hiroshi Sawamura4 1 Osaka Museum of Natural History, Osaka, Japan 2 Hokkaido University Museum, Sapporo, Japan 3 Numata Fossil Museum, Hokkaido, Japan 4 Ashoro Museum of Paleontology, Hokkaido, Japan ABSTRACT A fossil whale from the Hikatagawa Formation (Middle Miocene, 15.2–11.5 Ma) of Hokkaido, Japan is described as a new genus and species Taikicetus inouei and its phylogenetic position is examined. Consistent with the result of Marx, Lambert & de Muizon (2017), the Cetotheriidae form a clade with the Balaenopteroidea, and “a clade comprising Isanacetus, Parietobalaena and related taxa” is located basal to the Balaenopteroidea + Cetotheriidae clade. Taikicetus inouei is placed in the clade with most of members of “Cetotheres” sensu lato comprising Isanacetus, Parietobalaena and related taxa. Taikicetus inouei can be distinguished from the other members of “Cetotheres” sensu lato in having an anteriorly swollen short zygomatic process, high triangular coronoid process, and angular process, which does not reach as far posterior as the mandibular condyle. Taikicetus inouei is only record of “Cetotheres” sensu lato from Hokkaido, Japan and the northern-most records of “Cetotheres” sensu lato in Japan. Subjects Evolutionary Studies, Paleontology Keywords Fossil, Baleen whale, New genus, New species, Mysticeti Submitted 27 February 2018 INTRODUCTION Accepted 18 May 2018 Published 26 June 2018 The systematics of the Cetotheriidae have been controversial. The family Cetotheriidae Corresponding author was originally established by Brandt (1872) with limited use until Miller (1923) stated the Yoshihiro Tanaka, context of Cetotheriidae as “Cetotherium and related genera” without defining the [email protected] contents. -
The Biology of Marine Mammals
Romero, A. 2009. The Biology of Marine Mammals. The Biology of Marine Mammals Aldemaro Romero, Ph.D. Arkansas State University Jonesboro, AR 2009 2 INTRODUCTION Dear students, 3 Chapter 1 Introduction to Marine Mammals 1.1. Overture Humans have always been fascinated with marine mammals. These creatures have been the basis of mythical tales since Antiquity. For centuries naturalists classified them as fish. Today they are symbols of the environmental movement as well as the source of heated controversies: whether we are dealing with the clubbing pub seals in the Arctic or whaling by industrialized nations, marine mammals continue to be a hot issue in science, politics, economics, and ethics. But if we want to better understand these issues, we need to learn more about marine mammal biology. The problem is that, despite increased research efforts, only in the last two decades we have made significant progress in learning about these creatures. And yet, that knowledge is largely limited to a handful of species because they are either relatively easy to observe in nature or because they can be studied in captivity. Still, because of television documentaries, ‘coffee-table’ books, displays in many aquaria around the world, and a growing whale and dolphin watching industry, people believe that they have a certain familiarity with many species of marine mammals (for more on the relationship between humans and marine mammals such as whales, see Ellis 1991, Forestell 2002). As late as 2002, a new species of beaked whale was being reported (Delbout et al. 2002), in 2003 a new species of baleen whale was described (Wada et al. -
Nursery in the Oligocene Charleston Embayment, South Carolina, USA
Palaeontologia Electronica palaeo-electronica.org A megatoothed shark (Carcharocles angustidens) nursery in the Oligocene Charleston Embayment, South Carolina, USA Addison E. Miller, Matthew L. Gibson, and Robert W. Boessenecker ABSTRACT Many extant sharks are cosmopolitan as adults but inhabit nursery areas as youngsters - often shallow, dynamic ecosystems with abundant prey for neonates and juveniles. Megatoothed sharks (Otodontidae) were the largest sharks of all time, and nursery areas have been demonstrated for Carcharocles megalodon in the Miocene of Panama, Spain, Florida, and Maryland. An earlier study hypothesized a nursery area for Carcharocles angustidens in the upper Oligocene (23-25 Ma) Chandler Bridge For- mation of Charleston, South Carolina. We tested this by reporting and analyzing two collections (n=127) dominated by small teeth of C. angustidens from the Chandler Bridge Formation and some teeth from the underlying lower Oligocene (29-26.57 Ma) Ashley Formation (n=9). Correcting for tooth position, published body length estimation equations yielded body length estimates of 1.5-6.5 m for most individuals. Size-based assignment to age classes (neonates, juveniles, adults) is modified from the larger C. megalodon and scaled based on the largest available specimens of C. angustidens, reported herein. These assemblages are dominated by small individuals (juveniles and neonates) and include few adults. The Oligocene Charleston embayment therefore represents the first documented paleo-nursery area for C. angustidens. Addison Miller. Department of Geology and Environmental Geosciences, College of Charleston, Charleston, South Carolina 29424, USA. [email protected] Matthew Gibson. Charleston Museum, Charleston, South Carolina 29403, USA. [email protected] Robert Boessenecker, Mace Brown Museum of Natural History and Department of Geology and Environmental Geosciences, College of Charleston, Charleston, South Carolina 29424, USA. -
Gigantism Precedes Filter Feeding in Baleen Whale Evolution
1 This is the preprint version of the following article: Fordyce, R.E., and Marx, F.G. (2018). Gigantism 2 precedes filter feeding in baleen whale evolution. Curr Biol 28, 1670-1676.e1672, which has been 3 published in final form at https://www.cell.com/current-biology/fulltext/S0960-9822(18)30455- 4 X?_returnURL=https%3A%2F%2Flinkinghub.elsevier.com%2Fretrieve%2Fpii%2FS096098221830455X 5 %3Fshowall%3Dtrue 6 7 Gigantism precedes filter feeding in baleen whale evolution 8 R. Ewan Fordyce1,2 and Felix G. Marx3-5* 9 1Department of Geology, University of Otago, Dunedin, New Zealand 10 2Departments of Vertebrate Zoology and Paleobiology, National Museum of Natural History, Smithsonian Institution, 11 Washington DC, USA 12 5Directorate of Earth and History of Life, Royal Belgian Institute of Natural Sciences, Brussels, Belgium 13 3School of Biological Sciences, Monash University, Clayton, Victoria, Australia 14 4Geosciences, Museum Victoria, Melbourne, Australia 15 *E-mail: [email protected] 16 17 SUMMARY 18 Baleen whales (Mysticeti) are the largest animals on Earth, thanks to their ability to filter feed vast 19 amounts of small prey from seawater. Whales appeared during the latest Eocene, but evidence of 20 their early evolution remains both sparse and controversial [1, 2], with several models competing 21 to explain the origin of baleen-based bulk feeding [3-6]. Here, we describe a virtually complete 22 skull of Llanocetus denticrenatus, the second-oldest (ca 34 Ma) mysticete known. The new 23 material represents the same individual as the type and only specimen, a fragmentary mandible. 24 Phylogenetic analysis groups Llanocetus with the oldest mysticete, Mystacodon selenensis [2], 25 into the basal family Llanocetidae.