The Effect of Body Size Evolution and Ecology on Encephalization in Cave Bears and Extant Relatives Kristof Veitschegger
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Selective Foraging on Bromeliads by Andean Bears in the Ecuadorian Pa´Ramo
SHORT COMMUNICATION N DeMay et al. Selective foraging on bromeliads by Andean bears in the Ecuadorian pa´ramo Stephanie M. DeMay1,4, David A. Roon2, locating new resource sites, quality of known sites, Janet L. Rachlow2, and Rodrigo Cisneros3 avoiding predation, temporal variance in resource availability) at multiple scales (Compton et al. 2002, 1Environmental Science Program, University of Idaho, Fortin et al. 2003, Sergio et al. 2003, Bee et al. 2009). Moscow, ID 83844-3006, USA Optimal foraging theory predicts that the resultant 2Department of Fish and Wildlife Sciences, University of foraging patterns will be based on maximizing Idaho, Moscow, ID 83844-1136, USA energy uptake per unit of effort expended (Pyke et al. 3 Departamento de Ciencias Naturales, Universidad 1977, Hamilton and Bunnell 1987). Bailey at al. Te´cnica Particular de Loja, Loja, Ecuador (1996) described a spatial hierarchy for considering foraging behavior and the mechanisms that influence Abstract: The Andean bear (Tremarctos ornatus), decisions. The smallest scale is a bite of food, the only extant ursid in South America, lives in followed by feeding station, patch, feeding site, pa´ramo and montane forest ecosystems and is camp, and home range. Foraging decisions at each classified as vulnerable on the International Union scale have a wide range of ecological consequences, for Conservation of Nature Red List (Goldstein et from defining niche occupancy to affecting patterns al. 2008). In Podocarpus National Park in southern of competition and coexistence and constraining Ecuador, Andean bears exhibit patchy foraging adaptive potential. behavior on Puya eryngioides, a small terrestrial Foraging strategies are particularly interesting in bromeliad. -
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. -
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. -
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. -
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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. -
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. -
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 -
Chapter 1 - Introduction
EURASIAN MIDDLE AND LATE MIOCENE HOMINOID PALEOBIOGEOGRAPHY AND THE GEOGRAPHIC ORIGINS OF THE HOMININAE by Mariam C. Nargolwalla A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Anthropology University of Toronto © Copyright by M. Nargolwalla (2009) Eurasian Middle and Late Miocene Hominoid Paleobiogeography and the Geographic Origins of the Homininae Mariam C. Nargolwalla Doctor of Philosophy Department of Anthropology University of Toronto 2009 Abstract The origin and diversification of great apes and humans is among the most researched and debated series of events in the evolutionary history of the Primates. A fundamental part of understanding these events involves reconstructing paleoenvironmental and paleogeographic patterns in the Eurasian Miocene; a time period and geographic expanse rich in evidence of lineage origins and dispersals of numerous mammalian lineages, including apes. Traditionally, the geographic origin of the African ape and human lineage is considered to have occurred in Africa, however, an alternative hypothesis favouring a Eurasian origin has been proposed. This hypothesis suggests that that after an initial dispersal from Africa to Eurasia at ~17Ma and subsequent radiation from Spain to China, fossil apes disperse back to Africa at least once and found the African ape and human lineage in the late Miocene. The purpose of this study is to test the Eurasian origin hypothesis through the analysis of spatial and temporal patterns of distribution, in situ evolution, interprovincial and intercontinental dispersals of Eurasian terrestrial mammals in response to environmental factors. Using the NOW and Paleobiology databases, together with data collected through survey and excavation of middle and late Miocene vertebrate localities in Hungary and Romania, taphonomic bias and sampling completeness of Eurasian faunas are assessed. -
Cranial Morphological Distinctiveness Between Ursus Arctos and U
East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2017 Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus Benjamin James Hillesheim East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Biodiversity Commons, Evolution Commons, and the Paleontology Commons Recommended Citation Hillesheim, Benjamin James, "Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus" (2017). Electronic Theses and Dissertations. Paper 3261. https://dc.etsu.edu/etd/3261 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus ____________________________________ A thesis presented to the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences ____________________________________ by Benjamin Hillesheim May 2017 ____________________________________ Dr. Blaine W. Schubert, Chair Dr. Steven C. Wallace Dr. Josh X. Samuels Keywords: Ursidae, Geometric morphometrics, Ursus americanus, Ursus arctos, Last Glacial Maximum ABSTRACT Cranial Morphological Distinctiveness Between Ursus arctos and U. americanus by Benjamin J. Hillesheim Despite being separated by millions of years of evolution, black bears (Ursus americanus) and brown bears (Ursus arctos) can be difficult to distinguish based on skeletal and dental material alone. Complicating matters, some Late Pleistocene U. americanus are significantly larger in size than their modern relatives, obscuring the identification of the two bears. -
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.