Functional Morphology of the Cave Bear (Ursus Spelaeus) Mandible: a 3D Geometric Morphometric Analysis
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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 . -
Morphometric Analyses of Cave Bear Mandibles (Carnivora, Ursidae)
Revue de Paléobiologie, Genève (décembre 2018) 37 (2): 379-393 ISSN 0253-6730 Morphometric analyses of cave bear mandibles (Carnivora, Ursidae) Gennady F. BARYSHNIKOV1*, Andrei Yu. PUZACHENKO2 & Svetlana V. BARYSHNIKOVA1 1 Zoological Institute, Russian Academy of Sciences, Universitetskaya nab. 1, 199034 Saint Petersburg, Russia 2 Institute of Geography, Russian Academy of Sciences, Staromonetnyi per. 29, 109017 Moscow, Russia * Corresponding author: E-mail: [email protected] Abstract Morphometric variability of cave and brown bears and their ancestors (Ursus minimus and U. etruscus) is examined using multivariate statistics based on measurements of 679 mandibles from 90 localities in Northern Eurasia. The variability is dependent on sexual dimorphism in size: it is well seen in big cave bears (U. spelaeus, U. kanivetz = ingressus, U. kudarensis), whose males are nearly 25% larger than females. In the morphological space, we identified two main types of mandibles: the “arctoid” type [U. minimus, U. etruscus, U. arctos, U. rodei (?)], and the “spelaeoid” type (U. spelaeus spelaeus, U. s. eremus, U. kanivetz, U. kudarensis). The intermediate “deningeroid” type includes U. deningeri, U. savini, U. rossicus (males), and U. spelaeus ladinicus. An additional unit is formed by female sample of U. rossicus. The mandible bones are less informative for understanding of cave bear evolution, because in comparison to crania, they have a rather simple shape. Keywords Ursus, cave bears, morphometrics, variations, mandible, evolution, adaptation, Pleistocene. Résumé Analyse morphométrique de la mandibule chez les ours des cavernes. - La variabilité morphométrique des ours des cavernes, des ours bruns et de leurs ancêtres (Ursus minimus et U. etruscus) est étudiée à partir des mesures de 679 mandibules de 90 sites d’Eurasie du nord, à l’aide des méthodes d’analyses statistiques multivariées. -
Univerzita Karlova V Praze Přírodovědecká Fakulta
Univerzita Karlova v Praze Přírodovědecká fakulta Katedra zoologie Aneta Marková Stabilní isotopy ve studiu potravy Ursidae, včetně fosilních forem Stable isotopes in study of diet in Ursidae, including fossil taxa Bakalářská práce Školitel: prof. RNDr. Ivan Horáček CSc. Konzultant: Mgr. Jan Wagner Praha, 2011 1 Čestné prohlášení: Prohlašuji, že jsem závěrečnou práci zpracovala samostatně a že jsem uvedla všechny použité informační zdroje a literaturu. Tato práce ani její podstatná část nebyla předložena k získání jiného nebo stejného akademického titulu. V Praze, 18. 8. 2011 ............................................................. Aneta Marková 2 Poděkování: Na tomto místě chci poděkovat svému školiteli prof. RNDr. Ivanu Horáčkovi, CSc a konzultantovi Mgr. Janu Wagnerovi především za výběr tématu bakalářské práce a pomoc při jejím zpracování. Děkuji také svým nejbližším za jejich podporu. 3 Abstrakt Složení potravy u zástupců čeledi medvědovitých (Ursidae) je často diskutovaným tématem. Dodnes však panují určité nejistoty o trofické úrovni některých fosilních skupin. Velmi užitečnou metodou, která napomáhá k určení trofické úrovně u fosilních druhů medvědů a k určení relativního zastoupení rostlinné a živočišné složky potravy u druhů recentních, je analýza stabilních izotopů. Tato práce shrnuje poznatky o metodických přístupech a možnostech využití stabilních izotopů 13C a 15N ve studiu potravní ekologie medvědovitých. Výsledky analýz stabilních izotopů jsou prezentovány spolu s výsledky získanými jinými metodami. Pozornost je věnována skupinám, pro které existují relevantní izotopová data, se zvláštním zaměřením na medvědy jeskynní, jejichž trofická úroveň je v závěru zhodnocena za pomoci analýz stabilních izotopů i v kontextu evolučním a nutričním. Klíčová slova: stabilní isotopy, potrava, potravní ekologie, Ursidae Abstract Composition of food of members of the family Ursidae is often discussed topic. -
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. -
Growth Trajectories in the Cave Bear and Its Extant
Fuchs et al. BMC Evolutionary Biology (2015) 15:239 DOI 10.1186/s12862-015-0521-z RESEARCH ARTICLE Open Access Growth trajectories in the cave bear and its extant relatives: an examination of ontogenetic patterns in phylogeny Manuela Fuchs, Madeleine Geiger*, Madlen Stange and Marcelo R. Sánchez-Villagra Abstract Background: The study of postnatal ontogeny can provide insights into evolution by offering an understanding of how growth trajectories have evolved resulting in adult morphological disparity. The Ursus lineage is a good subject for studying cranial and mandibular shape and size variation in relation to postnatal ontogeny and phylogeny because it is at the same time not diverse but the species exhibit different feeding ecologies. Cranial and mandibular shapes of Ursus arctos (brown bear), U. maritimus (polar bear), U. americanus (American black bear), and the extinct U. spelaeus (cave bear) were examined, using a three-dimensional geometric morphometric approach. Additionally, ontogenetic series of crania and mandibles of U. arctos and U. spelaeus ranging from newborns to senile age were sampled. Results: The distribution of specimens in morphospace allowed to distinguish species and age classes and the ontogenetic trajectories U. arctos and U. spelaeus were found to be more similar than expected by chance. Cranial shape changes during ontogeny are largely size related whereas the evolution of cranial shape disparity in this clade appears to be more influenced by dietary adaptation than by size and phylogeny. The different feeding ecologies are reflected in different cranial and mandibular shapes among species. Conclusions: The cranial and mandibular shape disparity in the Ursus lineage appears to be more influenced by adaptation to diet than by size or phylogeny. -
Pleistocene Panthera Leo Spelaea
Quaternaire, 22, (2), 2011, p. 105-127 PLEISTOCENE PANTHERA LEO SPELAEA (GOLDFUSS 1810) REMAINS FROM THE BALVE CAVE (NW GERMANY) – A CAVE BEAR, HYENA DEN AND MIDDLE PALAEOLITHIC HUMAN CAVE – AND REVIEW OF THE SAUERLAND KARST LION CAVE SITES n Cajus G. DIEDRICH 1 ABSTRACT Pleistocene remains of Panthera leo spelaea (Goldfuss 1810) from Balve Cave (Sauerland Karst, NW-Germany), one of the most famous Middle Palaeolithic Neandertalian cave sites in Europe, and also a hyena and cave bear den, belong to the most im- portant felid sites of the Sauerland Karst. The stratigraphy, macrofaunal assemblages and Palaeolithic stone artefacts range from the final Saalian (late Middle Pleistocene, Acheulean) over the Middle Palaeolithic (Micoquian/Mousterian), and to the final Palaeolithic (Magdalénien) of the Weichselian (Upper Pleistocene). Most lion bones from Balve Cave can be identified as early to middle Upper Pleistocene in age. From this cave, a relatively large amount of hyena remains, and many chewed, and punctured herbivorous and carnivorous bones, especially those of woolly rhinoceros, indicate periodic den use of Crocuta crocuta spelaea. In addition to those of the Balve Cave, nearly all lion remains in the Sauerland Karst caves were found in hyena den bone assemblages, except those described here material from the Keppler Cave cave bear den. Late Pleistocene spotted hyenas imported most probably Panthera leo spelaea body parts, or scavenged on lion carcasses in caves, a suggestion which is supported by comparisons with other cave sites in the Sauerland Karst. The complex taphonomic situation of lion remains in hyena den bone assemblages and cave bear dens seem to have resulted from antagonistic hyena-lion conflicts and cave bear hunting by lions in caves, in which all cases lions may sometimes have been killed and finally consumed by hyenas. -
A B S T Ra C T S O F T H E O Ra L and Poster Presentations
Abstracts of the oral and poster presentations (in alphabetic order) see Addenda, p. 271 11th ICAZ International Conference. Paris, 23-28 August 2010 81 82 11th ICAZ International Conference. Paris, 23-28 August 2010 ABRAMS Grégory1, BONJEAN ABUHELALEH Bellal1, AL NAHAR Maysoon2, Dominique1, Di Modica Kévin1 & PATOU- BERRUTI Gabriele Luigi Francesco, MATHIS Marylène2 CANCELLIERI Emanuele1 & THUN 1, Centre de recherches de la grotte Scladina, 339D Rue Fond des Vaux, 5300 Andenne, HOHENSTEIN Ursula1 Belgique, [email protected]; [email protected] ; [email protected] 2, Institut de Paléontologie Humaine, Département Préhistoire du Muséum National d’Histoire 1, Department of Biology and Evolution, University of Ferrara, Corso Ercole I d’Este 32, Ferrara Naturelle, 1 Rue René Panhard, 75013 Paris, France, [email protected] (FE: 44100), Italy, [email protected] 2, Department of Archaeology, University of Jordan. Amman 11942 Jordan, maysnahar@gmail. com Les os brûlés de l’ensemble sédimentaire 1A de Scladina (Andenne, Belgique) : apports naturels ou restes de foyer Study of Bone artefacts and use techniques from the Neo- néandertalien ? lithic Jordanian site; Tell Abu Suwwan (PPNB-PN) L’ensemble sédimentaire 1A de la grotte Scladina, daté par 14C entre In this paper we would like to present the experimental study car- 40 et 37.000 B.P., recèle les traces d’une occupation par les Néan- ried out in order to reproduce the bone artifacts coming from the dertaliens qui contient environ 3.500 artefacts lithiques ainsi que Neolithic site Tell Abu Suwwan-Jordan. This experimental project plusieurs milliers de restes fauniques, attribués majoritairement au aims to complete the archaeozoological analysis of the bone arti- Cheval pour les herbivores. -
Heavy Reliance on Plants for Romanian Cave Bears Evidenced by Amino Acid Nitrogen Isotope Analysis Yuichi I
www.nature.com/scientificreports OPEN Heavy reliance on plants for Romanian cave bears evidenced by amino acid nitrogen isotope analysis Yuichi I. Naito 1,2*, Ioana N. Meleg3*, Marius Robu 3, Marius Vlaicu3, Dorothée G. Drucker 4, Christoph Wißing1, Michael Hofreiter5, Axel Barlow 5,6 & Hervé Bocherens 1,4 Heavy reliance on plants is rare in Carnivora and mostly limited to relatively small species in subtropical settings. The feeding behaviors of extinct cave bears living during Pleistocene cold periods at middle latitudes have been intensely studied using various approaches including isotopic analyses of fossil collagen. In contrast to cave bears from all other regions in Europe, some individuals from Romania show exceptionally high δ15N values that might be indicative of meat consumption. Herbivory on plants with high δ15N values cannot be ruled out based on this method, however. Here we apply an approach using the δ15N values of individual amino acids from collagen that ofsets the baseline δ15N variation among environments. The analysis yielded strong signals of reliance on plants for Romanian cave bears based on the δ15N values of glutamate and phenylalanine. These results could suggest that the high variability in bulk collagen δ15N values observed among cave bears in Romania refects niche partitioning but in a general trophic context of herbivory. Bears represent the largest terrestrial members within the Carnivora alive today and the vast majority of them have carnivorous or omnivorous feeding habits. Until around 25,000 years ago, the coldest period in the Pleistocene, additional, now extinct bear species were living1–4, among which the so-called cave bears, a very large type of bear that formed the sister lineage of extant brown bears and polar bears (e.g., ref. -
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. -
International Bear News
International Bear News Quarterly Newsletter of the International Association for Bear Research and Management (IBA) and the IUCN/SSC Bear Specialist Group Spring 2013 Vol. 22 no. 1 Ms. Jayanthi Natarajan (front row center), Union Minister for Environment and Forests, Government of India, opened the 21st IBA Conference in New Delhi, India that was attended by 373 delegates from 35 nations. Read more about the conference proceedings on page 21. IBA website: www.bearbiology.org Table of Contents IBA Student Forum 3 International Bear News, ISSN #1064-1564 29 Truman’s List Serve Council News Eurasia 4 From the President 30 News From Project “Rehabilitation, Release 6 Research and Conservation Grants and Behavioral/Ecology Research of Asiatic black (Ursus thibetanus) and Brown Bears (Ursus arctos) in Sikhote-Alin (Russian Far Bear Specialist Group East) 7 New Chairs Selected for Bear Specialist 31 A Novel Interaction Between a Sun Bear Group Expert Teams and Pangolin in the Wild 11 Bear Specialist Group Coordinating 32 Climate Change – No Thanks: German Committee (2013) Kids are Concerned About Polar Bears 12 Expert Teams of Bear Specialist Group 34 M13 and the Fate of Bears in Switzerland: Report on Projects A Short Note 16 New Co-Chair of Sloth Bear Expert Team Models BSG T-shirts with Students 17 Vietnam Bear Rescue Centre Prevails Americas against Eviction Challenge 35 Using Landscape-Scale Habitat Suitability 18 Irma: The “Swimmer” Brown Bear of Modeling to Identify Recovery Areas Kastoria Lake, Greece for the Louisiana Black Bear (Ursus -
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. -
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1.08 1.19 1.46 Nimravus brachyops Nandinia binotata Neofelis nebulosa 115 Panthera onca 111 114 Panthera atrox 113 Uncia uncia 116 Panthera leo 112 Panthera pardus Panthera tigris Lynx issiodorensis 220 Lynx rufus 221 Lynx pardinus 222 223 Lynx canadensis Lynx lynx 119 Acinonyx jubatus 110 225 226 Puma concolor Puma yagouaroundi 224 Felis nigripes 228 Felis chaus 229 Felis margarita 118 330 227 331Felis catus Felis silvestris 332 Otocolobus manul Prionailurus bengalensis Felis rexroadensis 99 117 334 335 Leopardus pardalis 44 333 Leopardus wiedii 336 Leopardus geoffroyi Leopardus tigrinus 337 Pardofelis marmorata Pardofelis temminckii 440 Pseudaelurus intrepidus Pseudaelurus stouti 88 339 Nimravides pedionomus 442 443 Nimravides galiani 22 338 441 Nimravides thinobates Pseudaelurus marshi Pseudaelurus validus 446 Machairodus alberdiae 77 Machairodus coloradensis 445 Homotherium serum 447 444 448 Smilodon fatalis Smilodon gracilis 66 Pseudaelurus quadridentatus Barbourofelis morrisi 449 Barbourofelis whitfordi 550 551 Barbourofelis fricki Barbourofelis loveorum Stenogale Hemigalus derbyanus 554 555 Arctictis binturong 55 Paradoxurus hermaphroditus Genetta victoriae 553 558 Genetta maculata 559 557 660 Genetta genetta Genetta servalina Poiana richardsonii 556 Civettictis civetta 662 Viverra tangalunga 661 663 552 Viverra zibetha Viverricula indica Crocuta crocuta 666 667 Hyaena brunnea 665 Hyaena hyaena Proteles cristata Fossa fossana 664 669 770 Cryptoprocta ferox Salanoia concolor 668 772 Crossarchus alexandri 33 Suricata suricatta 775