Mitochondrial Genomes Reveal an Explosive Radiation of Extinct And
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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 . -
A Partial Short-Faced Bear Skeleton from an Ozark Cave with Comments on the Paleobiology of the Species
Blaine W. Schubert and James E. Kaufmann - A partial short-faced bear skeleton from an Ozark cave with comments on the paleobiology of the species. Journal of Cave and Karst Studies 65(2): 101-110. A PARTIAL SHORT-FACED BEAR SKELETON FROM AN OZARK CAVE WITH COMMENTS ON THE PALEOBIOLOGY OF THE SPECIES BLAINE W. SCHUBERT Environmental Dynamics, 113 Ozark Hall, University of Arkansas, Fayetteville, AR 72701, and Geology Section, Research and Collections, Illinois State Museum, Springfield, IL 62703 USA JAMES E. KAUFMANN Department of Geology and Geophysics, University of Missouri-Rolla, Rolla, MO 65409 USA Portions of an extinct giant short-faced bear, Arctodus simus, were recovered from a remote area with- in an Ozark cave, herein named Big Bear Cave. The partially articulated skeleton was found in banded silt and clay sediments near a small entrenched stream. The sediment covered and preserved skeletal ele- ments of low vertical relief (e.g., feet) in articulation. Examination of a thin layer of manganese and clay under and adjacent to some skeletal remains revealed fossilized hair. The manganese in this layer is con- sidered to be a by-product of microorganisms feeding on the bear carcass. Although the skeleton was incomplete, the recovered material represents one of the more complete skeletons for this species. The stage of epiphyseal fusion in the skeleton indicates an osteologically immature individual. The specimen is considered to be a female because measurements of teeth and fused postcranial elements lie at the small end of the size range for A. simus. Like all other bears, the giant short-faced bear is sexually dimorphic. -
A Bibliography of Klamath Mountains Geology, California and Oregon
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY A bibliography of Klamath Mountains geology, California and Oregon, listing authors from Aalto to Zucca for the years 1849 to mid-1995 Compiled by William P. Irwin Menlo Park, California Open-File Report 95-558 1995 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. PREFACE This bibliography of Klamath Mountains geology was begun, although not in a systematic or comprehensive way, when, in 1953, I was assigned the task of preparing a report on the geology and mineral resources of the drainage basins of the Trinity, Klamath, and Eel Rivers in northwestern California. During the following 40 or more years, I maintained an active interest in the Klamath Mountains region and continued to collect bibliographic references to the various reports and maps of Klamath geology that came to my attention. When I retired in 1989 and became a Geologist Emeritus with the Geological Survey, I had a large amount of bibliographic material in my files. Believing that a comprehensive bibliography of a region is a valuable research tool, I have expended substantial effort to make this bibliography of the Klamath Mountains as complete as is reasonably feasible. My aim was to include all published reports and maps that pertain primarily to the Klamath Mountains, as well as all pertinent doctoral and master's theses. -
Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,***
Woodburne, M.O.; Cione, A.L.; and Tonni, E.P., 2006, Central American provincialism and the 73 Great American Biotic Interchange, in Carranza-Castañeda, Óscar, and Lindsay, E.H., eds., Ad- vances in late Tertiary vertebrate paleontology in Mexico and the Great American Biotic In- terchange: Universidad Nacional Autónoma de México, Instituto de Geología and Centro de Geociencias, Publicación Especial 4, p. 73–101. CENTRAL AMERICAN PROVINCIALISM AND THE GREAT AMERICAN BIOTIC INTERCHANGE Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,*** ABSTRACT The age and phyletic context of mammals that dispersed between North and South America during the past 9 m.y. is summarized. The presence of a Central American province of cladogenesis and faunal differentiation is explored. One apparent aspect of such a province is to delay dispersals of some taxa northward from Mexico into the continental United States, largely during the Blancan. Examples are recognized among the various xenar- thrans, and cervid artiodactyls. Whereas the concept of a Central American province has been mentioned in past investigations it is upgraded here. Paratoceras (protoceratid artio- dactyl) and rhynchotheriine proboscideans provide perhaps the most compelling examples of Central American cladogenesis (late Arikareean to early Barstovian and Hemphillian to Rancholabrean, respectively), but this category includes Hemphillian sigmodontine rodents, and perhaps a variety of carnivores and ungulates from Honduras in the medial Miocene, as well as peccaries and equids from Mexico. For South America, Mexican canids and hy- drochoerid rodents may have had an earlier development in Mexico. Remarkably, the first South American immigrants to Mexico (after the Miocene heralds; the xenarthrans Plaina and Glossotherium) apparently dispersed northward at the same time as the first Holarctic taxa dispersed to South America (sigmodontine rodents and the tayassuid artiodactyls). -
Faced Bear, Arctotherium, from the Pleistocene of California
I. RELATIONSHIPS AND STRUCTURE OF THE SHORT~ FACED BEAR, ARCTOTHERIUM, FROM THE PLEISTOCENE OF CALIFORNIA. By JOHN C. MERRIAM and CHESTER STOCK. With ten plates and five text-figures. 1 CONTENTS. PAGE Introduct-ion. 3 Systematic position of Arctotherium and its allies with relation to the typical Ursidae. 4 Origin of the Tremarctinae. 5 Summary of species of Arctotherium in the Pleistocene of North America. 7 Occurrence in California of arctotheres and associated faunas . 9 Potter Creek Cave. 9 Rancho La Brea. 10 McKittrick. .......... .... .......... ....... ...... ................. 11 Odontolo~Y. and osteology of Arctotherium. 11 DentitiOn . 11 Axial skeleton. 16 Appendicular skeleton. 21 Bibliography . 34 2 RELATIONSHIPS AND STRUCTURE OF THE SHORT-FACED BEAR, ARCTOTHERIUM, FROM THE PLEISTOCENE OF CALIFORNIA. BY JoHN C . MERRIAM AND CHESTER STocK. INTRODUCTION. The peculiar short-faced Californian bear, known as Arctotherium simum, was described by Cope in 1879 from a single specimen, con sisting of a skull minus the lower jaw, found by J. A. Richardson in 1878 in Potter Creek Cave on the McCloud River in northern California. Since the description of A. simum, a nearly perfect skull with lower jaw and a large quantity of additional material, representing nearly all parts of the skeleton and dentition of this species, has been obtained from the deposits of Potter Creek Cave as a result of further work carried on for the University of California by E. L. Furlong and by W. J. Sinclair in 1902 and 1903. Splendid material of Arctotherium has also been secured in the Pleistocene asphalt beds at Rancho La Brea by the Los Angeles Museum of History, Science, and Art. -
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. -
Download Vol. 37, No. 15
THEFOSSIIL RECORD OFARCTODUS PRLSTINUS (URSIDAES TREMARCTINAE) IN FLORIDA Steven D. Emsliet ABSTRACT ,€17841 Bnd posteranial~ :elements of.at least eight individuals of Arcrodus pristinus (Unidae: TremarctkIBe))913~ ret?9'~51 hom Eeisey Shell' Pit, an early Irvingtonian vertebrate'locality within a marine shell'bedj.pental m4Fremeritstindicate that two distinct sizes, presumably representing malds and fanales, are,regqgoizable@ntte collectio~ This bear tentatively is referred,from. 13 localities in Floridii, ranging jin age fromflate Bjancan to lat, Irvingipman, and is a biochronological indicat6r for this period. Another tremf#®e bew, Tremarctosf;oridanus, sofar is knoBn only from Rancholabrean localities initioiidiDand may,have,ecologically,rsplaced A. pristinus. RESUMEN Je reportan eleinentos craneales y post craneales pertenecientes a por lo mqos ocho individuos de *rodus',prisiinus ,(Wisidae: Tremarctinae) provenientes del depdsito de conchuelas de Ikisey, una Ipcalidad ds Wttebrados del Irvingtoniano temprano contenido en una capa de conchuelas marinas. Las mediciones,dental*{inaican la presencia de dos diferentes tamailds, los cualdspresatiblemante ~resentan a mactios ,y, hemBras eb la colecdi6n, Este osd' bs t6ntativamente teferido a 13 Ilocalidades en 1Florida, itba**i,86 eir edad: datia al Balnban6 tatdio hasta ) Irvingtoniano tardio, siendo un indicador bid¢fohol&~66:de:attipetiodo. Otto oso tremarctino, Tremdrctodoridanus, es conocido hasta ahorats616 pWi lodlidadss f Banchol abreangen florida, pudiendo haber reemplazado ecoltgicamente a A. pris tinus. 1 Thejauthor.ista<Couitesy.turator. Flolida Mpsum of N,tural·Hi~tory, University of Fld,ida, P. 0. Box 1 17800, Gunciville FL 32611- 7860,,Ij.5.A.,~nd 633istanl Proffssorin the Department Scien=, Westem State College, Gunnison CO 81230, U.S.A. -
A Late Miocene Ursavus Skull from Guanghe, Gansu, China
-302 第52卷 第3期 古 脊 椎 动 物 学 报 pp. 265 2014年7月 VERTEBRATA PALASIATICA figs. 1-9 A Late Miocene Ursavus skull from Guanghe, Gansu, China QIU Zhan-Xiang DENG Tao WANG Ban-Yue (Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 [email protected]) Abstract An almost complete Ursavus skull in association with its mandible is described. The skull was recently found from upper part of Liushu Formation in Linxia Basin. Its stratigraphic level and geologic age are correlated to the late Bahean ALMA/S, ~8 Ma. It represents a new species, here named Ursavus tedfordi. Cladistic analysis is conducted using the TNT software, based on a matrix of 11 taxa and 37 characters. The tree 5 of the 8 most parsimonious trees is chosen as the most reliable to reflect the phylogenetic history of the ursid clade. As the tree 5 shows, after divergence from the Oligocene-Early Miocene hemicyonids (Cephalogale), the ursid clade first yielded two stem-taxa: Ballusia elmensis and B. orientalis, the latter of which being an aberrant branch. Then, two major subclades emerged: one comprising Kretzoiarctos, Agriarctos and Ailurarctos, the other containing all Ursavus species and their descendants including all living bears (excluding Ailuropoda). Kretzoiarctos may not be the direct ancestral form of the giant panda as Abella and colleagues (2012) suggested, but the ancestral form of the lineage of Indarctos (+Agriotherium ?). Among the numerous Ursavus species, U. tedfordi is the most advanced and closest related to the living bears (excluding Ailuropoda) in morphology, however, might belong to a side-branch, judging by the autapomorphies possessed by it. -
False Thumb” of Tremarctos Ornatus (Carnivora, Ursidae, Tremarctinae): Phylogenetic and Functional Implications
Estudios Geológicos, 62 (1) enero-diciembre 2006, 389-394 ISSN: 0367-0449 Anatomy of the “false thumb” of Tremarctos ornatus (Carnivora, Ursidae, Tremarctinae): phylogenetic and functional implications M. J. Salesa1, G. Siliceo1, M. Antón1, J. Abella1, 2, P. Montoya2, J. Morales1 ABSTRACT We describe for the first time the radial sesamoid or “false thumb” of the spectacled bear (Tremarctos ornatus), showing its great morphological similarities with that of the giant panda (Ailuropoda melanoleu- ca) and the differences with that of the rest of the Ursidae. This points to the existence of a common ori- gin for this structure in both species, but considering the accepted phylogenies of ursids, the sharing of a “false thumb” in T. ornatus and A. melanoleuca would be a plesiomorphy for these groups, whereas in the rest of the ursids the radial sesamoid was probably reduced, lacking the specialised function that this bone has in Tremarctinae and Ailuropodinae. Key words: Panda, radial sesamoid, Ursidae, Ailuridae, Anatomy, Tremarctos. RESUMEN Se describe por primera vez el sesamoideo radial o “falso pulgar” del oso de anteojos (Tremarctos ornatus), mostrando la gran similitud morfológica con el del panda gigante (Ailuropoda melanoleuca) y las diferencias que presenta con el resto de los Ursidae. Esto apunta a la existencia de un origen común para esta estructura en ambas especies, pero considerando las filogenias aceptadas de Ursidae, la pre- sencia de falso pulgar en T. ornatus y A. melanoleuca sería una simplesiomorfía respecto al resto de úrsidos, en los cuales el sesamoideo radial nunca aumentó de tamaño, careciendo de la especializada función que posee en Tremarctinae y Ailuropodinae. -
Zoologica Fennica
SOCIETAS PRO FAUNA ET FLORA FENNICA lACTA ZOOLOGICA FENNICA 144 Miguel Crusafont Pair6 and Bjorn Kurten: Bears and Bear-Dogs from the Vallesian of the Valles-Penedes Basin, Spain Helstngl Yllopl ton et Aki.das o HELSINKI-HELSINGFORS 1976 ACTA ZOOLOGICA FENNICA 1-45 vide Acta Zoologica Fennica 45-50. 46-59 vide Acta Zoologica Fennica 60-93. 60-99 vide Acta Zoologica Fennica 100-125. 100. MARrA REuTER: Untersuchungen iiber Rassenbildung bei Gyratrix hermaphroditus (Turbellaria Neorhabdocoela). 32 S. (1961). 101. MARrA REuTER: Index Generalis Seriei Acta Zoologica Fennica 51-100 (194&-- 1961). 63 s. (1964). 102. WALTER HAcKMAN: Studies on the dipterous fauna in burrows of voles (Microtus, Oethrionomys) in Finland. 64 pp. (1963). 103. A. M. ]. EvERS: Dber die Entstehung der Excitatoren und deren Bedeutung fiir die Evolution der Malachiidae (Col.). 24 S. (1963). 104. ]oHAN REUTER: The international concentration in some hypotrichous Ciliates and its dependence on the external concentration. 94 pp. (1963). 105. GoRAN BERGMAN and KAr Ono DoNNER: An analysis of the spring migration of the Common Scoter and the Long-tailed Duck in southern Finland. 59 pp. (1964). 106. HENRrK OsTERHOLM: The significance of distance receptors in the feeding behaviour of the Fox, Vulpes vulpes L. 31 pp. (1964). 107. BJORN KuRTEN: The Carnivora of the Palestine caves. 74 pp. (1965). 108. BJORN KuRTEN: The evolution of the Polar Bear, Ursus maritimus Phipps. 30 pp. (1964). 109. FRANK S. ToMPA: Factors determining the numbers of song sparrows, Melospiza melodia (Wilson), on Mandarte Island, B. C., Canada. 73 pp. (1964). 110. PoNTUS PALMGREN: Die Spinnenfauna der Gegend von Kilpisjiirvi in Lappland. -
Presence of Arctotherium (Carnivora, Ursidae, Tremarctinae) in a Pre
Estudios Geológicos julio-diciembre 2015, 71(2), e041 ISSN-L: 0367-0449 doi: http://dx.doi.org/10.3989/egeol.42011.357 Presence of Arctotherium (Carnivora, Ursidae, Tremarctinae) in a pre-cultural level of Baño Nuevo-1 cave (Central Patagonia, Chile) Presencia de Arctotherium (Carnivora, Ursidae, Tremarctinae) en un nivel pre-cultural de cueva Baño Nuevo-1 (Patagonia Central, Chile) P. López Mendoza1, F. Mena Larraín2, E. Bostelmann3 1 Departamento de Antropología, Facultad de Ciencias Sociales, Universidad de Chile and ARQMAR-Centre for Maritime Archaeology Research of the Southeastern Pacific, Ignacio Carrera Pinto N° 1045, Ñuñoa, Santiago, Chile. Email: [email protected] 2 Centro de Investigación en Ecosistemas de la Patagonia (CIEP; CONICYT-Regional R10C 1003), Simpson 471, Coyhaique, Chile. Email: [email protected] 3 Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile. Isla Teja s/n, Valdivia, Chile. E-mail: [email protected] ABSTRACT The description of an I3 assigned to Arctotherium sp. obtained from the Baño Nuevo-1 site (Central Patagonia, Chile) is presented. The finding was recovered from Layer 5 and it is associated to Macrauchenia sp., Lama guani- coe, Felidae, Camelidae, Equidae and Mylodontidae, within a sterile deposit of cultural material, dated between ca. 13.500 and 11.200 BP. Despite the fact that it is only a single specimen, such finding extends the known distribution for the genus in Chile. Keywords: Ursidae; Arctotherium; Late Pleistocene; Central Patagonia. RESUMEN Se presenta la descripción de un I3 asignado a Arctotherium sp. proveniente del sitio Baño Nuevo-1 (Patagonia Central, Chile). El hallazgo fue realizado en la Capa 5 y está asociado a restos de Macrauchenia sp., Lama guani- coe, Felidae, Camelidae, Equidae y Mylodontidae dentro de un depósito estéril de material cultural, datado entre los ca.