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Journal articles on the topic 'Ursus deningeri'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

De Torres Pérez-Hidalgo, Trinidad. "La región auditiva en los osos del pleistoceno europeo." Spanish Journal of Palaeontology 2, no. 1 (2022): 41. http://dx.doi.org/10.7203/sjp.25214.

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Este trabajo trata de la descripción y comparación de las principales características morfológicas de la región auditiva de los grandes osos del Pleistoceno europeo: Ursus prearctos Boule, Ursus deningeri von Reichenau, Ursus spelaeus Rosenmüller-Heinroth y Ursus arctos Linneo. Además de una serie de diferencias morfológicas menores, de origen e importancia inciertos, las más importantes son: bulla tympánica con la cara ventral aplanada y septum indiviso sin septas en U. prearctos y U.arctos, mientras que en las especies espeloides, U. deningeri y fundamentalmente U. spelaeus, la cara ventral

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2

Valdiosera, Cristina, Nuria García, Love Dalén, et al. "Typing single polymorphic nucleotides in mitochondrial DNA as a way to access Middle Pleistocene DNA." Biology Letters 2, no. 4 (2006): 601–3. http://dx.doi.org/10.1098/rsbl.2006.0515.

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In this study, we have used a technique designed to target short fragments containing informative mitochondrial substitutions to extend the temporal limits of DNA recovery and study the molecular phylogeny of Ursus deningeri . We present a cladistic analysis using DNA recovered from 400 kyr old U. deningeri remains, which demonstrates U. deningeri 's relation to Ursus spelaeus . This study extends the limits of recovery from skeletal remains by almost 300 kyr. Plant material from permafrost environments has yielded DNA of this age in earlier studies, and our data suggest that DNA in teeth from

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3

MARCISZAK, Adrian, Małgorzata KOT, Katarzyna ZARZECKA-SZUBIŃSKA, and Grzegorz LIPECKI. "Ursidae (Carnivora, Mammalia) from Tunel Wielki Cave (southern Poland)." Comptes Rendus Palevol 24, no. 14 (2025): 241–302. https://doi.org/10.5852/cr-palevol2025v24a14.

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The presence of two ursids, <em>Ursus deningeri hercynicus</em> Rode, 1935 and<em> Ursus arctos taubachensis</em> Rode, 1935, was documented from the Tunel Wielki Cave. Of them, <em>Ursus deningeri hercynicus</em> is represented by almost all skeletal elements, with the predominance of isolated teeth, metapodials and phalanges. The analysis performed shows that the remains of this bear subspecies from Tunel Wielki have intermediate morphological features and metric values between individuals recorded in the materials from the early-mid (MIS 19-13) and late Middle Pleistocene (MIS 12-9) localit

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4

Chagneau, Jean. "Les Ursidés." Gallia préhistoire. Suppléments 27, no. 1 (1989): 69–76. http://dx.doi.org/10.3406/galip.1989.2559.

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The Ursids at La Baume de Gigny belong to three species : Ursus deningeri, represented by a relatively archaic form in the lower stratigraphie unit (layers XXVI and XXV) where the remains appear to be in a secondary context. Ursus spelaeus, recognised in the middle stratigraphie unit (layers XIX, XVII and XV) as well as in the upper unit where its specific characteristics are clearly attested. Ursus arctos, the remains of which belong to the wurmian layers (XVI, XV, XII and VI), a half-mandible having been discovered in the holocene layer III

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5

Tchernov, Eitan, and Evangelia Tsoukala. "Middle Pleistocene (Early Toringian) Carnivore Remains from Northern Israel." Quaternary Research 48, no. 1 (1997): 122–36. http://dx.doi.org/10.1006/qres.1997.1901.

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Seventy well-preserved fossil remains from deposits of an eroded karstic cave in the Upper Galilee of northern Israel includeUrsus deningeri(Ursidae),Canis lupus cf.mosbachensis (Canidae),Crocuta crocuta cf. praespelaea (Hyaenidae), Panthera leo cf. spelaea (Felidae), and Dama sp. (Cervidae). This assemblage probably dates to the Early Toringian (MQ2, Middle Pleistocene). Ursus deningeri and Panthera leo cf. spelaeahave never before been recorded south of the Taurus–Zagros mountain chain. We correlate the carnivore faunule with some Near Eastern and southern Levantine sites and assume that onl

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6

Wagner, Jan, Qigao Jiangzuo, Jadranka Mauch Lenardić, and Jinyi Liu. "Taxonomic revision of bears from the locality Šandalja I (Croatia) and its biostratigraphic consequences." Fossil Imprint 73, no. 3-4 (2017): 533–44. http://dx.doi.org/10.2478/if-2017-0028.

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Abstract Šandalja I palaeocave (“fossil” cave), situated in the southern part of the Istrian peninsula (Croatia), is a well-known locality due to the abundant fossil remains extracted from the bone breccia. It is broadly accepted that the fauna is Middle Villafranchian in age. Since the beginning, the taxonomic status of bear remains has caused controversy and, as a consequence, different authors listed between one to three bear species from this site. Detailed revision of dental material confirmed the presence of two bear species – Ursus thibetanus and U. deningeri. On the other hand, the pre

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7

Prat-Vericat, Maria, Isaac Rufí, Manel Llenas, and Joan Madurell-Malapeira. "Middle Pleistocene Ursus deningeri from Grotte de la Carrière (Réseau Lachambre, Têt Valley, Eastern Pyrenees)." Journal of Iberian Geology 46, no. 2 (2020): 163–75. http://dx.doi.org/10.1007/s41513-020-00124-1.

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8

Spassov, Nikolai, Latinka Hristova, Stefanka Ivanova, and Ivan Georgiev. "First record of the “small cave bear” in Bulgaria and the taxonomic status of bears of the Ursus savini Andrews – Ursus rossicus Borissiak group." Fossil Imprint 73, no. 3-4 (2017): 275–91. http://dx.doi.org/10.2478/if-2017-0015.

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Abstract The discovery of rich, well preserved skull material in the latest Middle Pleistocene deposits of Mishin Kamik cave (N-W Bulgaria) presents an opportunity for a new analysis of the taxonomy and the phylogeny of the so called “small cave bears”. Not all the small cave bears known would have necessarily had a common origin, the size decrease could be related in a number of cases to a parallelism. The bear from Mishin Kamik is identical with “Ursus rossicus” Borissiak from Krasnodar (S. Russia). Both these samples must be referred to U. savini Andrews from Bacton near Cromer (England). T

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9

van Heteren, Anneke H., Mikel Arlegi, Elena Santos, Juan-Luis Arsuaga, and Asier Gómez-Olivencia. "Cranial and mandibular morphology of Middle Pleistocene cave bears (Ursus deningeri): implications for diet and evolution." Historical Biology 31, no. 4 (2018): 485–99. http://dx.doi.org/10.1080/08912963.2018.1487965.

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10

Diedrich, Cajus. "Holotype skulls, stratigraphy, bone taphonomy and excavation history in the Zoolithen Cave and new theory about Esper’s “great deluge”." E&G Quaternary Science Journal 63, no. 1 (2014): 78–98. http://dx.doi.org/10.3285/eg.63.1.05.

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Abstract. Kurzfassung: Die Zoolithenhöhle liegt entlang des Wiesenttals (Oberfranken, Bayern, Süd-Deutschland) und hat eine lange „Spatenforschungs“-Historie. Die Fundstelle ist von internationaler Bedeutung aufgrund ihrer fünf validen Holotypen-Eiszeittier-Schädeln des „Höhlenbären“ sowie Top-Prädatoren (Eiszeit-Löwe, -Hyäne, -Wolf und -Rotwolf). Das große Höhlensystem entwickelte sich auf drei Etagen und hat drei fluviale Haupt-Sedimentsequenzen inklusive zwei Haupt-Speleothem-Genesephasen unter wechselnden Ponor-, Trocken- und Nassphasen während des Oligozän/Miozän (Neogen) über das Pliozän

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11

Koufos, George, George Konidaris, and Katerina Harvati. "Revisiting Ursus etruscus (Carnivora, Mammalia) from the Early Pleistocene of Greece with description of new material." Quaternary International 497, no. 2018 (2017): 222–39. https://doi.org/10.5281/zenodo.3569153.

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The Villafranchian ursids of Greece are scanty, represented by a few isolated teeth and bones. During our last field campaigns in the Mygdonia Basin (Macedonia, Greece) we discovered an almost complete cranium, as well as some cranial, dental and postcranial remains, which are presented in this article. The new material originates from the locality Tsiotra Vryssi (TSR), dated to the late Villafranchian (1.8–1.2 Ma). The specimens are described and compared with ursids from various European localities; their morphological characters and dimensions place it with Ursus etruscus Cuvier, 1823

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12

Döppes, Doris, and Wilfried Rosendahl. "On a special bone discovery from the Middle Pleistocene Mosbach-Sands/Hesse – a contribution to the pathology of Ursus deningeri Reichenau, 1904." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 92 (April 6, 2010): 25–34. http://dx.doi.org/10.1127/jmogv/92/2010/25.

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13

Baryshnikov, Gennady F., and Andrey Yu Puzachenko. "Morphometric analysis of metacarpal and metatarsal bones of cave bears (Carnivora, Ursidae)." Fossil Imprint 73, no. 1-2 (2017): 7–47. http://dx.doi.org/10.2478/if-2017-0001.

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Abstract For the first time, morphometric variation has been studied in metacarpal and metatarsal bones of all known taxa of cave bears, which belong to different molecular genetic groups (deningeri, kudarensis, spelaeus, and ingressus haplotypes). The examined material involves nearly three thousand specimens from 28 localities of Europe, the Urals, Caucasus, and Central Asia. For comparison we used samples of fossil and recent Ursus arctos, as well as U. etruscus, regarded as a common ancestor of brown bears and cave bears. Methods of univariate and multivariate statistical analyses of metap

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14

Tikhonova, E. P., and S. A. Sablina. "Our Mother. To mark the centenary of the birth of Gulsyuma Khusyainovna Nuraeva (Urusova) (July 15, 1920 – October 14, 2008)." Proceedings of the Zoological Institute RAS 323, no. 1 (2019): 45–60. http://dx.doi.org/10.31610/trudyzin/2019.323.1.45.

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This article is dedicated to the oldest member of Zoological Institute of the Russian Academy of Sciences and her biography. She devoted her life to the service of science and preservation of collection of osteology department in theriology laboratory. With her own hands she boiled, cleaned and prepared countless exhibit items for storing, expert examination and displaying in the museum. Skillfully reuniting bone fragments found by paleontologists, she assembled numerous skeletal elements and even whole skulls of fossil animals. She was making plaster models from the most precious pieces, so t

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15

Wagner, J., and M. Gasparik. "Research history of Pleistocene faunas in Gombasek quarry (Slovakia), with comments to the type specimen and the type locality of Ursus deningeri gombaszogensis Kretzoi, 1938." Fragmenta Palaeontologica Hungarica 31 (2014): 125–43. http://dx.doi.org/10.17111/fragmpalhung.2014.31.125.

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16

Stiner, Mary C., Hema Achyuthan, Güven Arsebük, et al. "Reconstructing cave bear paleoecology from skeletons: a cross-disciplinary study of middle Pleistocene bears from Yarimburgaz Cave, Turkey." Paleobiology 24, no. 1 (1998): 74–98. http://dx.doi.org/10.1017/s0094837300019989.

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Cave bears, an extinct subgenus (Spelearctos) of Ursus, were versatile enough to inhabit large areas of the northern hemisphere during the middle and late Pleistocene, yet they had evolved a specialized dentition that emphasized grinding functions, implying a heavy dietary reliance on tough, fibrous foods (i.e., plants). Isotope studies have yielded conflicting results on cave bear diet, however, often without consideration of the provenance of the samples or the possible contradictions that taphonomic and morphologic evidence might pose to dietary interpretations. It is likely that cave bear

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17

MARCISZAK, Adrian, Małgorzata KOT, Katarzyna ZARZECKA-SZUBIŃSKA, and Grzegorz LIPECKI. "Ursidae (Carnivora, Mammalia) from Tunel Wielki Cave (southern Poland)." Comptes Rendus Palevol 24, no. 14 (2025). https://doi.org/10.5852/cr-palevol2025v24a14.

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The presence of two ursids, Ursus deningeri hercynicus Rode, 1935 and Ursus arctos taubachensis Rode, 1935, was documented from the Tunel Wielki Cave. Of them, Ursus deningeri hercynicus is represented by almost all skeletal elements, with the predominance of isolated teeth, metapodials and phalanges. The analysis performed shows that the remains of this bear subspecies from Tunel Wielki have intermediate morphological features and metric values between individuals recorded in the materials from the early-mid (MIS 19-13) and late Middle Pleistocene (MIS 12-9) localities. A set of features sugg

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18

de Alvarado, Mónica Villalba, María Prat-Vericat, Martín Arriolabengoa, Joan Madurell Malapeira, and Asier Gómez-Olivencia. "The mandible of Salbatore II: A new Ursus deningeri site in the northern Iberian Peninsula." Geobios, December 2024. https://doi.org/10.1016/j.geobios.2024.08.019.

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19

Lipar, Matej, Irena Zupanič Pajnič, Marko Cotman, et al. "DNA, spectroscopic and geochemical analyses of bone fragments and associated speleothems in Postojna cave, Slovenia." Acta Carsologica 49, no. 2-3 (2020). http://dx.doi.org/10.3986/ac.v49i2-3.7970.

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a loose/broken stalagmite containing small fragments of cemented bones were collected from the Postojna Cave to investigate whether deoxyribonucleic acid (DNA) can be determined. The study is complemented by the Fourier-transform infrared spectroscopy - attenuated total reflectance (FTIR-ATR) analysis in order to determine the alteration of the bones and to test whether this analysis can be used as an indicator of possible DNA preservation. In addition, geochemical analyses were conducted in order to determine whether the associated flowstone/stalagmite is suitable for elucidating the timing o

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20

Rodríguez-Almagro, Manuel, Asier Gómez-Olivencia, Mónica Villalba de Alvarado, Juan Luis Arsuaga, and Nohemi Sala. "Taphonomic study of the cave bears (Ursus cf. deningeri and U. spelaeus) from the Sima I of the El Polvorín cave (Northern Iberian Peninsula)." Quaternary Science Advances, February 2024, 100171. http://dx.doi.org/10.1016/j.qsa.2024.100171.

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