(2020). Morphological Convergence Obscures Functional Diversity in Sabre-Toothed Carnivores
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O Ssakach Drapieżnych – Część 2 - Kotokształtne
PAN Muzeum Ziemi – O ssakach drapieżnych – część 2 - kotokształtne O ssakach drapieżnych - część 2 - kotokształtne W niniejszym artykule przyjrzymy się ewolucji i zróżnicowaniu zwierząt reprezentujących jedną z dwóch głównych gałęzi ewolucyjnych w obrębie drapieżnych (Carnivora). Na wczesnym etapie ewolucji, drapieżne podzieliły się (ryc. 1) na psokształtne (Caniformia) oraz kotokształtne (Feliformia). Paradoksalnie, w obydwu grupach występują (bądź występowały w przeszłości) formy, które bardziej przypominają psy, bądź bardziej przypominają koty. Ryc. 1. Uproszczone drzewo pokrewieństw ewolucyjnych współczesnych grup drapieżnych (Carnivora). Ryc. Michał Loba, na podstawie Nyakatura i Bininda-Emonds, 2012. Tym, co w rzeczywistości dzieli te dwie grupy na poziomie anatomicznym jest budowa komory ucha środkowego (bulla tympanica, łac.; ryc. 2). U drapieżnych komora ta jest budowa przede wszystkim przez dwie kości – tylną kaudalną kość entotympaniczną i kość ektotympaniczną. U kotokształtnych, w miejscu ich spotkania się ze sobą powstaje ciągła przegroda. Obydwie części komory kontaktują się ze sobą tylko za pośrednictwem małego okienka. U psokształtnych 1 PAN Muzeum Ziemi – O ssakach drapieżnych – część 2 - kotokształtne Ryc. 2. Widziane od spodu czaszki: A. baribala (Ursus americanus, Ursidae, Caniformia), B. żenety zwyczajnej (Genetta genetta, Viverridae, Feliformia). Strzałkami zaznaczono komorę ucha środkowego u niedźwiedzia i miejsce występowania przegrody w komorze żenety. Zdj. (A, B) Phil Myers, Animal Diversity Web (CC BY-NC-SA -
Origin and Beyond
EVOLUTION ORIGIN ANDBEYOND Gould, who alerted him to the fact the Galapagos finches ORIGIN AND BEYOND were distinct but closely related species. Darwin investigated ALFRED RUSSEL WALLACE (1823–1913) the breeding and artificial selection of domesticated animals, and learned about species, time, and the fossil record from despite the inspiration and wealth of data he had gathered during his years aboard the Alfred Russel Wallace was a school teacher and naturalist who gave up teaching the anatomist Richard Owen, who had worked on many of to earn his living as a professional collector of exotic plants and animals from beagle, darwin took many years to formulate his theory and ready it for publication – Darwin’s vertebrate specimens and, in 1842, had “invented” the tropics. He collected extensively in South America, and from 1854 in the so long, in fact, that he was almost beaten to publication. nevertheless, when it dinosaurs as a separate category of reptiles. islands of the Malay archipelago. From these experiences, Wallace realized By 1842, Darwin’s evolutionary ideas were sufficiently emerged, darwin’s work had a profound effect. that species exist in variant advanced for him to produce a 35-page sketch and, by forms and that changes in 1844, a 250-page synthesis, a copy of which he sent in 1847 the environment could lead During a long life, Charles After his five-year round the world voyage, Darwin arrived Darwin saw himself largely as a geologist, and published to the botanist, Joseph Dalton Hooker. This trusted friend to the loss of any ill-adapted Darwin wrote numerous back at the family home in Shrewsbury on 5 October 1836. -
Gorgonopsia: Rubidgeinae) with Implications for the Identity of This Species
Rediscovery of the holotype of Clelandina major Broom, 1948 (Gorgonopsia: Rubidgeinae) with implications for the identity of this species Christian F. Kammerer North Carolina Museum of Natural Sciences, 11 W. Jones Street, Raleigh, North Carolina 27604, U.S.A., and Evolutionary Studies Institute, University of the Witwatersrand, Private Bag 3, WITS, Johannesburg, 2050 South Africa E-mail: [email protected] Received 7 November 2017. Accepted 8 December 2017 No specimen number was given for the holotype of the rubidgeine gorgonopsian species Clelandina major Broom, 1948 in its original description. Historically, a specimen in the Rubidge Collection (RC 94) was considered to represent Broom’s type specimen for C. major. However, recent study has revealed that the holotype of C. major is in fact a different specimen in the McGregor Museum in Kimberley (MMK 5031). The morphology of this specimen is consistent with the genus Clelandina, contra work based on RC 94 that considered C. major referable to Aelurognathus. Clelandina major is here considered synonymous with the type species Clelandina rubidgei. MMK 5031 represents only the fifth known specimen of this rare and unusual gorgonopsian. Keywords: Synapsida, Therapsida, Gorgonopsia, Permian, holotype, taxonomy. Palaeontologia africana 2017. ©2017 Christian F.Kammerer. This is an open-access article published under the Creative Commons Attribution 4.0 Unported License (CC BY4.0). To view a copy of the license, please visit http://creativecommons.org/licenses/by/4.0/. This license permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. The article is permanently archived at: http://wiredspace.wits.ac.za/handle/10539/23480 INTRODUCTION provided no specimen numbers for the holotypes of Clelandina is one of the rarest and most unusual C. -
Systematic Position and Taxonomy of Pipistrellus Deserti (Chiroptera: Vespertilionidae)
Mammalia 2015; 79(4): 419–438 Petr Benda*, Tommy Andriollo and Manuel Ruedi Systematic position and taxonomy of Pipistrellus deserti (Chiroptera: Vespertilionidae) Abstract: Pipistrellus deserti is a small, pale-coloured bat DOI 10.1515/mammalia-2014-0024 occurring in the most arid parts of the Sahara, in Morocco, Received February 26, 2014; accepted August 22, 2014; previously published online September 17, 2014 Algeria, Libya, Egypt, and the Sudan, and marginally also in sub-Saharan Africa. Although most authors consider P. deserti as a full species, others regard it as a subspe- cies, or even as a junior synonym of Pipistrellus kuhlii. We Introduction analysed the topotype material of P. deserti from Libya using both morphologic and molecular characters, and The Desert pipistrelle, Pipistrellus deserti, was described compared them with samples from other Saharan coun- by Thomas (1902: 4) as “a small buff-coloured desert ally tries and with P. kuhlii from around the Mediterranean. of P. kuhli” on the basis of a male obtained from Murzuq, The Libyan samples of deserti are morphologically very Fezzan, south-western Libya. Thomas differentiated similar to other populations from arid parts of North his P. deserti from P. kuhlii practically only on the basis Africa (Morocco, Algeria, Egypt, Sudan), but differ mark- of smaller size (e.g., a forearm length 29.5 mm or great- edly in the size of most skull dimensions when compared est skull length 11.6 mm). For a long time, Thomas’ (1902) to P. kuhlii sampled in more mesic areas. However, phy- report remained the only authenticated record of P. -
'Felis' Pamiri Ozansoy, 1959 (Carnivora, Felidae) from the Upper Miocene Of
1 Re-appraisal of 'Felis' pamiri Ozansoy, 1959 (Carnivora, Felidae) from the upper Miocene of 2 Turkey: the earliest pantherin cat? 3 4 Denis GERAADS and Stéphane PEIGNE 5 Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (UMR 7207), Sorbonne 6 Universités, MNHN, CNRS, UPMC, CP 38, 8 rue Buffon, 75231 PARIS Cedex 05, France 7 8 Running head: 'Felis' pamiri from Turkey 9 10 Abstract 11 Although the divergence of the Panthera clade from other Felidae might be as old as the 12 earliest middle Miocene, its fossil record before the Pliocene is virtually non-existent. Here we 13 reassess the affinities of a felid from the early upper Miocene of Turkey, known by well-preserved 14 associated upper and lower dentitions. We conclude that it belongs to the same genus 15 (Miopanthera Kretzoi, 1938) as the middle Miocene 'Styriofelis' lorteti (Gaillard, 1899), and that 16 this genus is close to, if not part of, the Panthera clade. 17 18 Keywords: Carnivora – Felidae – Pantherini – Phylogeny – Upper Miocene – Turkey 19 20 Introduction 21 The Felidae can be divided in two subfamilies (Johnson et al. 2006; Werdelin et al. 2010) 22 Felinae (= Pantherinae, or big cats, plus Felinae, or smaller cats, in e.g., Wilson and Mittermeier 23 2009) and Machairodontinae, although their monophyly is hard to demonstrate, the second one 24 being extinct. The Neogene fossil record of the Machairodontinae, or saber-toothed felids, is 25 satisfactory, but that of other members of the family, conveniently called conical-toothed felids 26 (although several of them have compressed, flattened canines) is much more patchy. -
Stratigraphic Data of the Middle – Late Permian on Russian Platform Données Stratigraphiques Sur Le Permien Moyen Et Supérieur De La Plate-Forme Russe
Geobios 36 (2003) 533–558 www.elsevier.com/locate/geobio Stratigraphic data of the Middle – Late Permian on Russian Platform Données stratigraphiques sur le Permien moyen et supérieur de la Plate-forme russe Vladimir P. Gorsky a, Ekaterina A. Gusseva a,†, Sylvie Crasquin-Soleau b,*, Jean Broutin c a All-Russian Geological Research Institute (VSEGEI), Sredny pr. 74, St. Petersburg, 199106, Russia b CNRS, FRE2400, université Pierre-et-Marie-Curie, département de géologie sédimentaire, T.15–25, E.4, case 104, 75252 Paris cedex 05, France c Université Pierre-et-Marie-Curie, laboratoire de paléobotanique et paléoécologie, IFR101–CNRS, 12, rue Cuvier, 75005 Paris, France Received 12 November 2001; accepted 2 December 2002 Abstract This paper presents the litho– and biostratigraphic data and correlations of the Middle and Late Permian (Ufimian, Kazanian and Tatarian) on the Russian Platform. The lithological descriptions and the paleontological content (foraminifera, bivalves, ostracods, brachiopods, vertebrates, plants and acritarchs) of the different units are exposed from the Barents Sea up to the Caspian Sea. © 2003 E´ ditions scientifiques et médicales Elsevier SAS. All rights reserved. Résumé Cet article présente les descriptions et les corrélations litho– et biostratigraphiques du Permien moyen et supérieur (Ufimien, Kazanien, Tatarien) de la Plate-forme russe depuis la mer de Barents jusqu’à la mer Caspienne. Les descriptions lithologiques et le contenu paléontologique (foraminifères, bivalves, ostracodes, brachiopodes, vertébrés, plantes et acritarches) des différentes unités sont exposés. © 2003 E´ ditions scientifiques et médicales Elsevier SAS. All rights reserved. Keywords: Stratigraphic data; Correlations; Middle and Late Permian; Russian Platform; Ostracods; Plants Mots clés : Données stratigraphiques ; Corrélations ; Permien moyen et supérieur ; Plate-forme russe ; Ostracodes ; Plantes 1. -
A New Species of Paramachaerodus (Mammalia, Carnivora, Felidae
PalZ (2017) 91:409–426 DOI 10.1007/s12542-017-0371-7 RESEARCH PAPER A new species of Paramachaerodus (Mammalia, Carnivora, Felidae) from the late Miocene of China and Bulgaria, and revision of Promegantereon Kretzoi, 1938 and Paramachaerodus Pilgrim, 1913 1,2 3 Yu Li • Nikolai Spassov Received: 17 March 2016 / Accepted: 10 June 2017 / Published online: 18 August 2017 Ó Pala¨ontologische Gesellschaft 2017 Abstract New Machairodontinae material from the late Keywords Machairodontinae Á Paramachaerodus Miocene localities of Hezheng (China) and Hadjidimovo transasiaticus sp. nov. Á Promegantereon Á Late Miocene Á (Bulgaria) represents a new species of Paramachaerodus China Á Bulgaria Pilgrim. Both localities are similar in age and suggest that the new species had a very large geographic range Kurzfassung Neues Material von Machairodontinae aus extending from northwestern China adjacent to the Tibetan den obermioza¨nen Fundstellen Hezheng (China) und Plateau (Gansu Province) to southeastern Europe or prob- Hadjidimovo (Bulgarien) repra¨sentiert eine neue Art, die ably to all of southern Europe. The new species—Para- der Gattung Paramachaerodus Pilgrim zugeordnet werden machaerodus transasiaticus sp. nov is characterized by a kann. Die beiden Fundstellen sind altersgleich und deuten combination of features of ‘‘Promegantereon’’ and Para- darauf hin, dass die neue Art ein sehr ausgedehntes Areal machaerodus. This specific morphology, as well as the age von Nordwest-China, im benachbarten Hochland von Tibet of the Hezheng and Hadjidimovo (early Turolian, after the (Provinz Gansu), bis Su¨dost-Europa oder mo¨glicherweise European Land Mammal Ages) put the new species in auch ganz Su¨deuropa besiedelt hat. Die neue Art – Para- intermediary position between ‘‘Promegantereon’’ and machaerodus transasiaticus sp. -
Pelycosauria Y Therapsida
Pelycosauria y Therapsida Los amniotos pueden dividirse en dos líneas principales: Los synapsidos (de quienes provienen los mamíferos) y los Sauropsidos (de quienes provienen “rep;les” y aves). Los Synápsidos poseen una apertura (fenestra) en el cráneo, detrás del ojo, debajo de la unión entre los huesos postorbital y escamoso. Comparten un ancestro en común más reciente con un mamífero que con una lagar;ja. Filogené;camente, no pertenecen a rep;lia, pero a la mayoría se les conoce como “rep;les semejantes a mamíferos” Anapsida Synapsida Diapsida “Parapsida” o “Euryapsida” (Diapsida modificados) SYNAPSIDA: -COMPARTEN UN ACMR CON MAMÍFEROS QUE CON REPTILES -FENESTRA TEMPORAL, BAJO POSTORBITAL-ESCAMOSO -REGION OCCIPITAL POSTERIORMENTE INCLINADA (NO VERTICAL) -SUPRATEMPORAL SE CONECTA AL POSTORBITAL PETROLACOSAURUS ARCHAEOTHYRIS (synapsida) -CENTRALE MEDIAL (MC) BIEN DESARROLLADO EN EL TARSO -PRESENCIA DE DOS HUESOS CORONOIDES (LADO MEDIAL MANDÍBULA) Tradicionalmente se discuten cuatro “tipos fundamnetales” de synapsidos, que en efecto son grupos sucesivamente sucesivamente anidados “Pelycosaurios” (parafilético, se usa para hablar de synapsidos basales) Carbonífero Superior- Terápsidos. Pérmico-Triásico Pérmico. Muy “reptilianos” aún Modificaciones craneales y posturales importantes Cynodontes. Pérmico superior, Triásico Mamíferos. Triásico Muy similares a mamíferos Oído interno tres huesos Dinastías synapsidas Meg Dynasty 1: Pelicosaurios del Pérmico inferior Meg Dynasty 2: Terápsidos del Pérmico superior-Triásico inferior Meg Dynasty 3: Mamíferos del Cenozoico Los primeros synápsidos (basales) se conocen colectivamente como un grupo “parafilético”, los Pelycosaurios (P en la figura) que excluyen a sus descendientes Terápsidos. Los pelycosaurios presentan abundantes dientes en el paladar. Reconstruc;on of Pangaea showing anteosaurid dinocephalians and platyoposaurid temnospondyles during the Middle Permian. Probable dispersal routes are indicated by red arrows. -
ARSTANOSAURUS Species Undescribed AVIMIMUS Portentosus
Dinosaur Casts Specimen List ARSTANOSAURUS species undescribed Meaning of Name: Reptile from Arstan Well Classification: ORNITHOPODA; Hadrosauridae, Hadrosaurinae Age: Late Cretaceous (Santonian) Bayn Shireh Formation, 85 million years ago Locality: Gobi Desert, Peoples' Republic of Mongolia Size: l5cm in length AVIMIMUS portentosus Partial skeleton. In position as if found in field Meaning of Name: Bird Mimic Classification: THEROPODA; relationships uncertain Age: Late Cretaceous (Campanian) Djadokhta Formation, 75 million years ago Locality: Gobi Desert, Peoples' Republic of Mongolia Size: l00cm in length reconstructed Skeleton www.gondwanastudios.com BAGACERATOPS rozhdestvenskyi Meaning of Name: Small horned face Classification: CERATOPSIA; Neoceratopsia; Protoceratopsidae Age: Late Cretaceous (Campanian), Barun Goyot Formation, 75 million years ago Locality: Gobi Desert, Southern Khermin Tsav, Mongolia Size: 3.5cm in length BIARMOSUCHUS tener Meaning of Name: Crocodile from Biarmia, an ancient country in the Perm region. Classification: THERAPSIDA; Eotheriodontia; Family Biarmosuchidae Age: Late Permian, Zone I, 225 million years ago Locality: Ocher, Perm Region, Russia Size: 75cm in length Half skeleton encased in sediment, as found in the field. BULLOCKORNIS planei (Demon Duck of Doom) Meaning of Name: Bird from Bullock Creek Classification: Flightless Bird Age: 12 million years Locality: Northern Territory, Australia Size: 250cm in height www.gondwanastudios.com CATOPSALIS djadochtatherium Meaning of Name: Beast from Djadokhta -
Gorgonopsians, an Attempt Based on a Re-Examination of the Cranial Anatomy of the Type Material and a Comparison of All the Specimens Available 2
ON THE CLASSIFICATION OF THE GORGONOPSIA by D. Sigogneau 1 The work here summarized represents an attempt to review the South African Gorgonopsians, an attempt based on a re-examination of the cranial anatomy of the type material and a comparison of all the specimens available 2. The possible origin of the group from the Russian eotheriodonts is discussed in conclusion. When one realizes what a tremendous amount of material Broom had to deal with, one cannot help but be impressed by the synthesis at which he was able to arrive and which remains to-day largely valid. He masterfully recognized the major taxonomic boundaries and their significance, perceiving within each group the affinities uniting the different constituents. However, his inner feeling that it was his duty to make known each and every specimen examined by him led him to neglect somewhat their preparation and to establish types insufficiently described or justified. Quite apart from that, the number of specimens accumulated for over a hundred years naturally de manded a re-organization of the different infra-orders; I was offered by Dr. A. S. Brink, fonner Assistant Director of the Bernard Price Institute for Palaeontological Research of Johannesburg, the opportunity to disentangle the Gorgonopsians. After four years of reflection I emerged in 1967 with a provisional classification, the sole pretention of which being to present some new morphological data. The material consists of about 150 specimens, formerly distributed in 67 genera and 108 species. Except for the North American material, every specimen has been re-examined, often further prepared, and drawn and photographed. -
Lab 10-Carboniferous+Perm-Online
Lab 10: Carboniferous/Permian Observations How This Lab Will Work 1. Open a Word doc or similar on your computer 2. At various points I will ask you to answer a question based on the activities in this lab. 3. I will indicate these points by this symbol: Please answer these questions in your Word doc. 4. After you have assembled the answers into your Word doc, go to the course Canvas page. 5. On the module for this week there is a link to TurnItIn. 6. Please upload your document using the TurnInIt. 7. That completes the lab assignment. :) Reminder on Observation Project Please remember that as we go through these, you should be using these fossils to construct your lab observation project, which was detailed last time. Easy to put off, hard to catch up. ;) Topics Today: 1. Introduction to Carboniferous-Permian 2. Phylum Rhizaria: Fusulinida 3. Phylum Bryozoa: Archimedes 4. Phylum Plantae: Glossopteris 5. Phylum Plantae: Lepidodendron 6. Phylum Plantae: Calamites 7. Phylum Arthropoda: Meganeuropsis 8. Phylum Arthropoda: Arthropleura 9. Phylum Chordata: Helicoprion 10. Phylum Chordata: Eryops 11. Phylum Chordata: Dimetrodon 12. Phylum Chordata: Lystrosaurus 13. Phylum Chordata: Gorgonopsia Geology 121 Lab 10: Carboniferous-Permian, page 1 of 7 Introduction to Carboniferous-Permian In today’s lab we’ll look at specimens from the Carboniferous and the Permian. The Carboniferous was period of high O2 and high CO2. It is typically divided in North America into the Mississippian and the Pennsylvanian, so a sketch of today’s time periods looks like this: Permian Pennsylvanian Carboniferous Mississippian These time periods saw developments of some things we haven’t seen before—namely, land animals, foraminifera, and forests of land plants. -
Permian Monsters: Life Before the Dinosaurs’
Life Before the Dinosaurs Introducing the Permian, its bizarre creatures and the greatest extinction Earth ever experienced. A Travelling Exhibition Blending Art and Science Exhibition Overview Step back in time 290 million years when bizarre-looking animals dominated life on land and sea, and find out about the greatest extinction the world has ever seen in ‘Permian Monsters: Life before the Dinosaurs’. This unique exhibition brings the past back to life with fossilized skeletons and full size life models of the animals that ruled the world millions of years before the age of dinosaurs, in a time known as the Permian. The Permian period ended with the largest extinction Earth ever experienced, which wiped out 90% of all species on the planet. The cause of the end-Permian extinction had baffled scientists for the past 20 years but a recent discovery shed new light on the cause of this catastrophe: global warming. Find out how this familiar phenomenon, started by a huge volcanic eruption, set off a chain of events that led to the greatest extinction on Earth. The exhibition blends art and science with a collection of new artwork which offers a glimpse back in time through the eyes of award winning paleo-artist Julius Csotonyi. View fossilised skeletons and reconstructed models of these amazing but bizarre creatures that dominated land and sea; and dig and identify fossils in the interactive dig pits throughout the exhibition. ‘Permian Monsters’ showcases an amazing collection of fossils and models from this relatively unknown time period, from giant insects, bizarre looking sharks to strange reptiles with mammal-like characteristics.