Phylogenetic Signal Analysis in the Basicranium of Ursidae (Carnivora, Mammalia)
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The Carnivora (Mammalia) from the Middle Miocene Locality of Gračanica (Bugojno Basin, Gornji Vakuf, Bosnia and Herzegovina)
Palaeobiodiversity and Palaeoenvironments https://doi.org/10.1007/s12549-018-0353-0 ORIGINAL PAPER The Carnivora (Mammalia) from the middle Miocene locality of Gračanica (Bugojno Basin, Gornji Vakuf, Bosnia and Herzegovina) Katharina Bastl1,2 & Doris Nagel2 & Michael Morlo3 & Ursula B. Göhlich4 Received: 23 March 2018 /Revised: 4 June 2018 /Accepted: 18 September 2018 # The Author(s) 2018 Abstract The Carnivora (Mammalia) yielded in the coal mine Gračanica in Bosnia and Herzegovina are composed of the caniform families Amphicyonidae (Amphicyon giganteus), Ursidae (Hemicyon goeriachensis, Ursavus brevirhinus) and Mustelidae (indet.) and the feliform family Percrocutidae (Percrocuta miocenica). The site is of middle Miocene age and the biostratigraphical interpretation based on molluscs indicates Langhium, correlating Mammal Zone MN 5. The carnivore faunal assemblage suggests a possible assignement to MN 6 defined by the late occurrence of A. giganteus and the early occurrence of H. goeriachensis and P. miocenica. Despite the scarcity of remains belonging to the order Carnivora, the fossils suggest a diverse fauna including omnivores, mesocarnivores and hypercarnivores of a meat/bone diet as well as Carnivora of small (Mustelidae indet.) to large size (A. giganteus). Faunal similarities can be found with Prebreza (Serbia), Mordoğan, Çandır, Paşalar and Inönü (all Turkey), which are of comparable age. The absence of Felidae is worthy of remark, but could be explained by the general scarcity of carnivoran fossils. Gračanica records the most eastern European occurrence of H. goeriachensis and the first occurrence of A. giganteus outside central Europe except for Namibia (Africa). The Gračanica Carnivora fauna is mostly composed of European elements. Keywords Amphicyon . Hemicyon . -
Oldowan Scavengers Vs. Acheulian Hunters: What Does the Faunal Record Say?
Opinion Glob J Arch & Anthropol Volume 6 Issue 1 - August 2018 Copyright © All rights are reserved by Bienvenido Martínez Navarro DOI: 10.19080/GJAA.2018.06.555679 Oldowan Scavengers Vs. Acheulian Hunters: What Does the Faunal Record Say? Bienvenido Martínez-Navarro* ICREA at the Catalan Institute of Human Paleoecology and Social Evolution-IPHES, Rovira i Virgili University (URV), 43007 Tarragona, Spain Submission: August 15, 2018; Published: August 22, 2018 *Corresponding author: Bienvenido Martínez-Navarro, ICREA at the Catalan Institute of Human Paleoecology and Social Evolution-IPHES, Rovira i Virgili University (URV), 43007 Tarragona, Spain, Email: Keywords: Oldowan; Acheulian; Scavengers; Hunters; Late Pliocene; Early Pleistocene; Middle Pleistocene; Europe; Asia; Africa; Archaeology; Omnivorous; Artifacts; Pebbles; Mammals; Buffalo; Hippo; Rhino; Horse; Elephant Opinion until the end of the Pleistocene. It was also the same for lions and Between 3 and 2 million years ago, our eastern African spotted hyenas. ancestors became omnivorous. A biped primate with mostly vegetarian eating strategy changed and started to eat animal food, meat and fat coming from the carcasses of large mammals, eat meat and fat, their possibilities for dispersal increased Once humans have developed their abilities to find and developing at the beginning a scavenging behavior. This was exponentially and, around 2 million-years-ago, humans were only possible thanks to the development of one extrasomatic able to disperse out of Africa and colonize the middle latitudes of Eurasia, as it is recorded at the site of Dmanisi in the Caucasus to cut and dismember the carcasses and percussion tools to evolution, the cultural technology making lithic artifacts, flakes break the bones and extract the marrow content. -
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Bull. Soc. belge Géol., Paléont., Hydrol. T. 79 fasc. 2 pp. 167-174 Bruxelles 1970 Bull. Belg. Ver. Geol., Paleont., Hydrol. V. 79 deel 2 blz. 167-174 Brussel 1970 MAMMALS OF THE CRAG AND FOREST BED B. McW1LLIAMs SuMMARY. In the Red and Norwich Crags mastodonts gradually give way to the southern elephant, large caballine horses and deer of the Euctenoceros group become common. Large rodents are represented by Castor, Trogontherium and rarely Hystrix; small forms include species of Mimomys. Carnivores include hyaena, sabre-toothed cat, leopard, polecat, otter, bear, seal and walrus. The Cromer Forest Bed Series had steppe and forest forms of the southern elephant and the mastodont has been lost. Severa! species of giant deer become widespread and among the many rodents are a. number of voles which develop rootless cheek teeth. The mole is common. Warmth indicators include a monkey, and more commonly hippopotamus. Possible indicators of cold include glutton and musk ox. Rhinoceros is widespread, and it is a time of rapid evolution for the elk. Carnivores include hyaena, bear, glutton, polecat, marten, wold and seal. The interpretation of mammalian finds from is represented by bones which resemble the the Crags and Forest Bed is not an easy mole remains but are about twice their size. matter. A proportion of the remains have been derived from eatlier horizons, others are Order Primates discovered loose in modern coastal deposits, and early collectors often kept inadequate The order is represented at this period m records. Owing to the uncertain processes of England by a single record of Macaca sp., the fossilisation or inadequate collecting there are distal end of a teft humerus from a sandy many gaps in our knowledge of the mammal horizon of the Cromerian at West Runton, ian faunas of these times. -
Cave Bear Ecology and Interactions With
CAVEBEAR ECOLOGYAND INTERACTIONSWITH PLEISTOCENE HUMANS MARYC. STINER, Department of Anthropology,Building 30, Universityof Arizona,Tucson, AZ 85721, USA,email: [email protected] Abstract:Human ancestors (Homo spp.), cave bears(Ursus deningeri, U. spelaeus), andbrown bears (U. arctos) have coexisted in Eurasiafor at least one million years, andbear remains and Paleolithic artifacts frequently are found in the same caves. The prevalenceof cave bearbones in some sites is especiallystriking, as thesebears were exceptionallylarge relative to archaichumans. Do artifact-bearassociations in cave depositsindicate predation on cave bearsby earlyhuman hunters, or do they testify simply to earlyhumans' and cave bears'common interest in naturalshelters, occupied on different schedules?Answering these and other questions aboutthe circumstancesof human-cave bear associationsis made possible in partby expectations developedfrom research on modem bearecology, time-scaledfor paleontologicand archaeologic applications. Here I review availableknowledge on Paleolithichuman-bear relations with a special focus on cave bears(Middle Pleistocene U. deningeri)from YarimburgazCave, Turkey.Multiple lines of evidence show thatcave bearand human use of caves were temporallyindependent events; the apparentspatial associations between human artifacts andcave bearbones areexplained principally by slow sedimentationrates relative to the pace of biogenicaccumulation and bears' bed preparationhabits. Hibernation-linkedbehaviors and population characteristics of cave -
299947 108 1964.Pdf
SOCIETAS PRO FAUNA ET FLORA FE.NNICA SOCIETAS PRO FAUNA ET FLORA FENNICA ACTA ZOOLOGICA FENNICA 108 Bjom Kurten: The evolution of the Polar Bear, U rsus maritimus Phipps p- ) A. ~NA ET • .P A .fJl!N'NICA_ HELSINKI-HELSINGFORS 1964 ACTA ZOOLOGICA FENNICA 1-45 vide Acta Zoologica Fennica 45-50. 46-59 vide Acta Zoologica Fennica 60-93. 60. Alex. Luther: Untersuchungen an rhahdocoelen Turbellarien. IX. Zur Kenntnis einiger Typhloplaniden. X. "Ober Astrotorhynchus bifidus (M'Int). 42 S. (1950). 61. T. H. Jilrri: Die Kleinmarlinenbestiinde in ihren Beziehungen zu der Umwelt (Coregonus albula L.). 116 S. (1950). 62. Pontus Palmgren: Die Spinnenfauna Finnlands und Ostfennoskandiens. Ill. Xysticidae und Philodromidae. 43 S. (1950). 63. Sven Nordberg: Researches on the bird fauna of the marine zone in the Aland Archipelago. 62 pp. (1950). 64. Floriano Papil "Ober einige Typhloplaninen (Turbellaria neorhabdocoela). 20 S. (1951). 65. Einari Merikallio: On the numbers of land-birds in Finland. 16 pp. (1951). 66. K. 0. Donner: The visual acuity of some Passerine birds. 40 pp. (1951). 67. Lars von Haartman: Der Trauerfliegenschniipper. II. Populationsprobleme. 60S. (1951). 68. Erie Fabrieius: Zur Ethologie junger Anatiden. 178 S. (1951). 69. Tor G. Karling: Studien iiber Kalyptorhynchien (Turbellaria). IV. Einige Euka lyptorhynchia. 49 S. (1952). 70. L. Benick t: Pilzkiifer und Kliferpilze. Okologische und statistische Untersuchun gen. 250 S. (1952). 71. Bo-Jungar Wikgren: Osmotic regulation in some aquatic animals with special reference to the influence of temperature. 102 pp. (1953). 72. Wollram Noodt: Entromostracen aus dem Litoral und dem Kiistengrundwasser des Finnischen Meerbusens. 12 S. (1953). 73. -
The Carnivore Remains from the Sima De Los Huesos Middle Pleistocene Site
N. Garcia & The carnivore remains from the Sima de J. L. Arsuaga los Huesos Middle Pleistocene site Departamento de Paleontologia, (Sierra de Atapuerca, Spain) Facultad de Ciencias Geologicas, U.A. de Paleoantropologia & Instituto de View metadata, citation and similar papersRemain ats ocore.ac.ukf carnivores from the Sima de los Huesos sitebrought representin to you gby a t COREleast Geologia Economica, Universidad 158 adult individuals of a primitive (i.e., not very speleoid) form of Ursus Complutense de Madrid, Ciudad provided by Servicio de Coordinación de Bibliotecas de la... deningeri Von Reichenau 1906, have been recovered through the 1995 field Universitaria, 28040 Madrid, Spain season. These new finds extend our knowledge of this group in the Sierra de Atapuerca Middle Pleistocene. Material previously classified as Cuoninae T. Torres indet. is now assigned to Canis lupus and a third metatarsal assigned in 1987 to Departamento de Ingenieria Geoldgica, Panthera cf. gombaszoegensis, is in our opinion only attributable to Panthera sp. The Escuela Tecnica Superior de Ingenieros family Mustelidae is added to the faunal list and includes Maites sp. and a de Minas, Universidad Politecnica smaller species. The presence of Panthera leo cf. fossilis, Lynxpardina spelaea and de Madrid, Rios Rosas 21, Fells silvestris, is confirmed. The presence of a not very speloid Ursus deningeri, 28003 Madrid, Spain together with the rest of the carnivore assemblage, points to a not very late Middle Pleistocene age, i.e., oxygen isotope stage 7 or older. Relative frequencies of skeletal elements for the bear and fox samples are without major biases. The age structure of the bear sample, based on dental wear stages, does not follow the typical hibernation mortality profile and resembles a cata strophic profile. -
The Genus Ursus in Eurasia: Dispersal Events and Stratigraphical Significance
Riv. It. Paleont. Strat. v. 98 n,4 pp. 487-494 Marzo 7993 THE GENUS URSUS IN EURASIA: DISPERSAL EVENTS AND STRATIGRAPHICAL SIGNIFICANCE MARCO RUSTIONI* 6. PAUL MAZZA** Ke vuords: Urszs, PIio-Pleistocene. Eurasia. Riassunto. Sulla base dei risultati di precedenti studi condotti dagli stessi autori vengono riconosciuti cinque gruppi principali di orsi: Ursus gr. ninimus - thihtanus (orsi neri), Ursus gr. etuscus (orsi erruschi), Ursus gr. arctos (orsi bruni), Ursus gr, deningeri - spelaeus (orsi delle caverne) e Ursus gr. maitimus (orsi bianchi). Gli orsi neri sembrano essere scomparsi dall'Europa durante il Pliocene superiore, immigrarono nuovamente in Europa all'inizio del Pleistocene medio e scomparvero definitivamente dall'Europa all'inizio del Pleistocene superiore. Gli orsi etruschi sono presenti più o meno contemporaneamente nelle aree meridionali dell'Europa e dell'Asia nel corso del Pliocene superiore. La linea asiatica sembra scomparire alla fine di questo periodo, mentre il ceppo europeo soprawisse, dando origine, nel corso del Pleistocene inferiore, ai rappresentanti più evoluti. Gli orsi bruni si sono probabilmente originati in Asia. Questo gruppo si diffuse ampiamente nella regione oloartica differenziandòsi in un gran numero di varietà e presumibilmente raggiunse I'Europa alla fine del Pleistocene inferiore. L'arrivo degli orsi bruni in Europa è un evento significativo, che all'incirca coincise con il grande rinnovamento faunistico del passaggio Pleistocene inferiore-Pleistocene medio. Gli orsi bruni soppiantarono gli orsi etruschi, tipici dei contesti faunistici villafranchiani, e dettero origine alla linea degli orsi delle caverne. Gli orsi delle caverne ebbero grande successo in Europa nel Pleistocene medio e superiore e scomparvero alla fine dell'ultima glaciazione quaternaria o nel corso del primo Olocene. -
New Data on Large Mammals of the Pleistocene Trlica Fauna, Montenegro, the Central Balkans I
ISSN 00310301, Paleontological Journal, 2015, Vol. 49, No. 6, pp. 651–667. © Pleiades Publishing, Ltd., 2015. Original Russian Text © I.A. Vislobokova, A.K. Agadjanian, 2015, published in Paleontologicheskii Zhurnal, 2015, No. 6, pp. 86–102. New Data on Large Mammals of the Pleistocene Trlica Fauna, Montenegro, the Central Balkans I. A. Vislobokova and A. K. Agadjanian Borissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia email: [email protected], [email protected] Received September 18, 2014 Abstract—A brief review of 38 members of four orders, Carnivora, Proboscidea, Perissodactyla, and Artio dactyla, from the Pleistocene Trlica locality (Montenegro), based on the material of excavation in 2010–2014 is provided. Two faunal levels (TRL11–10 and TRL6–5) which are referred to two different stages of faunal evolution in the Central Balkans are recognized. These are (1) late Early Pleistocene (Late Villafranchian) and (2) very late Early Pleistocene–early Middle Pleistocene (Epivillafranchian–Early Galerian). Keywords: large mammals, Early–Middle Pleistocene, Central Balkans DOI: 10.1134/S0031030115060143 INTRODUCTION of the Middle Pleistocene (Dimitrijevic, 1990; Forsten The study of the mammal fauna from the Trlica and Dimitrijevic, 2002–2003; Dimitrijevic et al., locality (Central Balkans, northern Montenegro), sit 2006); the MNQ20–MNQ22 zones (Codrea and uated 2.5 km from Pljevlja, provides new information Dimitrijevic, 1997); terminal Early Pleistocene improving the knowledge of historical development of (CrégutBonnoure and Dimitrijevic, 2006; Argant the terrestrial biota of Europe in the Pleistocene and and Dimitrijevic, 2007), Mimomys savinipusillus biochronology. In addition, this study is of interest Zone (Bogicevic and Nenadic, 2008); or Epivillafran in connection with the fact that Trlica belongs to chian (Kahlke et al., 2011). -
Retreat and Extinction of the Late Pleistocene Cave Bear (Ursus Spelaeus Sensu Lato)
Sci Nat (2016) 103:92 DOI 10.1007/s00114-016-1414-8 ORIGINAL PAPER Retreat and extinction of the Late Pleistocene cave bear (Ursus spelaeus sensu lato) Mateusz Baca1,2 & Danijela Popović3 & Krzysztof Stefaniak4 & Adrian Marciszak4 & Mikołaj Urbanowski5 & Adam Nadachowski6 & Paweł Mackiewicz7 Received: 8 July 2016 /Revised: 18 September 2016 /Accepted: 20 September 2016 # The Author(s) 2016. This article is published with open access at Springerlink.com Abstract The cave bear (Ursus spelaeus sensu lato) is a typical decrease in the cave bear records with cooling indicate that the representative of Pleistocene megafauna which became extinct at drastic climatic changes were responsible for its extinction. the end of the Last Glacial. Detailed knowledge of cave bear Climate deterioration lowered vegetation productivity, on which extinction could explain this spectacular ecological transforma- the cave bear strongly depended as a strict herbivore. The distri- tion. The paper provides a report on the youngest remains of the bution of the last cave bear records in Europe suggests that this cave bear dated to 20,930 ± 140 14C years before present (BP). animal was vanishing by fragmentation into subpopulations oc- Ancient DNA analyses proved its affiliation to the Ursus cupying small habitats. One of them was the Kraków- ingressus haplotype. Using this record and 205 other dates, we Częstochowa Upland in Poland, where we discovered the latest determined, following eight approaches, the extinction time of record of the cave bear and also two other, younger than 25,000 this mammal at 26,100–24,300 cal. years BP. The time is only 14C years BP. -
Factsheet Giant Panda
Giant panda (Ailuropoda melanoleuca) The giant panda, the rarest of bear species, is found in mountainous areas in China. They mainly live on the east side of the Tibetan Plateau. Origin The giant panda is classified under the subfamily of Ailuropodinae and is the only existing representative of this family. Two subspecies have been recognized, Ailuropoda melanoleuca melanoleuca and Ailuropoda melanoleuca qinlingensis, or the small panda (also red panda) and the giant panda. The classification of the giant panda has been the subject of some debate: a diet consisting of bamboo, ambiguity as regards their ancestors and different anatomic characteristics all gave rise to uncertainty within the scientific community on whether the giant panda was indeed a true bear. Genetic research suggests that the panda is a real bear and therefore part of the Ursidae family. However, some doubt will always remain and a few experts believe that the giant panda and the small panda form a separate family altogether. Others disagree completely and believe that the panda is not a true bear but related to the raccoon. Opinions differ greatly on this subject. One could say that the small panda is indeed related to the raccoon and their relatives. Habitat The giant panda is found only in the impenetrable bamboo forests in the mountains at an elevation of 1,400 to 4,000 meter. Appearance The giant panda is very recognizable by its distinct black and white coloration. They have black patches around the eyes, making the eyes look unusually big. Another, less conspicuous, characteristic is the existence of a sixth finger: the panda has six fingers on the forelimbs instead of five. -
Giant Panda's 'Cousin' Lived in Spain 9 May 2012
Giant panda's 'cousin' lived in Spain 9 May 2012 have had dark fur with white spots mainly on the chest, around the eyes and possibly close to the tail. "This fur pattern is considered primitive for bears, such as that of the giant panda whose white spots are so big that it actually seems to be white with black spots," states Abella. Agriarctos beatrix, from the Ursidae family and related to giant pandas, would have lived in the forest and could have been more sessile that those bears that tend to hunt more, such as the brown or polar bears. According to researchers, the extinct bear would have escaped from other larger Illustration of Agriarctos beatrix. Image: SINC carnivores by climbing up trees. The expert highlights that "its diet would have been similar to that of the sun bear or the spectacled A team of Spanish scientists have found a new bear that only eat vegetables and fruit and ursid fossil species in the area of Nombrevilla in sometimes vertebrates, insects, honey and dead Zaragoza, Spain. Agriarctos beatrix was a small animals." plantigrade omnivore and was genetically related to giant pandas, according to the authors of the "We know that it was a different species to those study. documented up until now because of its morphological differences and the size of its teeth," The fossil remains of a new ursid species, confirms the scientist. "We have compared it with Agriarctos beatrix, have been discovered in the species of the same kind (Agriarctos) and similar Nombrevilla 2 site in the province of Zaragoza, kinds from the same period (Ursavus and Spain. -
On the Occurrence of the Scimitar-Toothed Cat, Homotherium Latidens (Carnivora; Felidae), at Kents Cavern, England
Journal of Archaeological Science 40 (2013) 1629e1635 Contents lists available at SciVerse ScienceDirect Journal of Archaeological Science journal homepage: http://www.elsevier.com/locate/jas On the occurrence of the scimitar-toothed cat, Homotherium latidens (Carnivora; Felidae), at Kents Cavern, England Donald A. McFarlane a,*, Joyce Lundberg b a W.M. Keck Science Center, The Claremont Colleges, 925 North Mills Avenue, Claremont, CA 91711, USA b Department of Geography and Environmental Studies, Carleton University, Ottawa, ON K1S 5B6, Canada article info abstract Article history: Teeth of Homotherium latidens recovered from late Pleistocene sediments, Kents Cavern, England have Received 10 July 2012 long been the source of controversy. H. latidens is conspicuously absent from other late Pleistocene cave Received in revised form deposits in Britain, and is widely thought to have been extirpated from the region during the isotope 19 October 2012 stage 10 glacial period. Here we present high spatial resolution analyses of fluorine and uranium uptake Accepted 25 October 2012 profiles in teeth of three species from the same cave. The H. latidens tooth is clearly distinguished from the unambiguously provenanced Late Pleistocene hyaena and Middle Pleistocene cave bear teeth. These Keywords: results are consistent with the theory that the H. latidens teeth originated at an exogenous location, were Quaternary Cave probably transported to Kents Cavern as Palaeolithic trade goods, and were buried in Kents Cavern in Palaeontology Palaeolithic times. Fluorine Ó 2012 Elsevier Ltd. All rights reserved. Uranium Palaeolithic 1. Introduction latest marine isotope stage (MIS) 12 or earliest MIS 11 age (Lundberg and McFarlane, 2007). The Breccia has also yielded Kents1 Cavern, located on the southwest coast of England in human artifacts (Lowe, 1916) of late Cromerian (MIS 13) age which a suburb of the town of Torquay (50.4677 N, 3.5028 W, Fig.