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247 results for “Large mammals”
FIGURE 13 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 13. Scatter diagram showing the ratio of lower carnassial (m1) length (Lm1) and breadth (B m1) in late Pleistocene and Recent Mustela nivalis from Poland. The Solna Jama Cave specimen displays a moderately large size, with the length of m1 less than 4 mm, typical of the late Pleistocene and postglacial period.
FIGURE 12 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 12. Scatter diagram showing the ratio of total calvarium length to zygomatic breadth in extant Mustela nivalis from Poland, compared with the fossil specimen from Solna Jama Cave.
FIGURE 11 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 11. Skulls of Mustela nivalis from Poland: recent specimens (1-3) and the fossil from Solna Jama Cave (4). 1, robust, adult male; 2, adult female; 3, young, adult female; and 4, adult female. Note fully developed sagittal crest in individual from Solna Jama Cave, indicating fully mature age. Scale bar equals 10 mm.
FIGURE 7 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 7. Scatter diagram showing the ratio of m1 trigonid breadth (B tri) to m1 talonid breadth (B tal) in the forms of Gulo: G. schlosseri and G. gulo. Data from Döppes (2001): late Pleistocene G. gulo and recent G. gulo; data from Marciszak (2012): G. schlosseri and late Pleistocene G. gulo (part).
FIGURE 4 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 4. Gulo gulo cranium from Solna Jama Cave (JSJ/Gg/1-1) in dorsal view (left) compared with a cranium from a large modern male from Scandinavia (right) from collection of Natural History Museum University of Wrocław (coll. no. M/500328). Scale bar equals 10 mm.
FIGURE 10 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 10. Scatter diagram showing the ratio of mandiblar height (measured after m1) to m1 length in fossil and extant Mustela eversmanii and Mu. putorius. Data from Marciszak (2012) and references therein.
FIGURE 6 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 6. Metacarpals (mtcp) and metatarsals (mtts) of Gulo gulo from Solna Jama Cave. From left to right: right mtcp III (JSJ/Gg/1-29), left mtcp V (JSJ/GG/1-31), left mtts II (JSJ/Gg/1-33), left mtts III (JSJ/Gg/1-34), left mtts IV (JSJ/Gg/1-35) and right mtts V (JSJ/Gg/1-36). Scale bar equals 10 mm.
FIGURE 9 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 9. Right mandible of Mustela eversmanii (JSJ/Mev/1) from Solna Jama Cave. Note relatively short and robust body mandible and massiveness of the symphysal area. Scale bar equals 10 mm.
FIGURE 5 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 5. Gulo gulo cranium from Solna Jama Cave (JSJ/Gg/1-1) in ventral view (left) compared with a cranium from a large modern male from Scandinavia (right) from collection of Natural History Museum University of Wrocław (coll. no. M/500328). Note particularly powerful dentition of the individual from Solna Jama Cave in comparison with recent G. gulo. Scale bar equals 10 mm.
FIGURE 8 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 8. Occurrence of members of the genus Gulo in the late Quaternary of Poland (after Marciszak, 2012 and references therein). Red dot: Gulo schlosseri; black dot: G. gulo from late middle Pleistocene (3-5) and late Pleistocene-Holocene (3-12). Localities: 1, Żabia Cave; 2, Kozi Grzbiet; 3, Biśnik Cave; 4, Cave no. 4 on the Birów Hill; 5, Deszczowa Cave; 6, Nietoperzowa Cave, Ciemna Cave; 7, Mamutowa Cave; 8, Borsuka Cave; 9, Cave in Czarkowa; 10, Niedźwiedzia Cave; 11, Północna Duża Cave, Naciekowa Cave; and 12, Solna Jama Cave.
FIGURE 2 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 2. Environs of Solna Jama Cave entrance (1), showing the fissured crystalline limestones, in which the cave developed. The "Wolverine Niche" (2) and the corrosion, phreatic features of the cave passage (3). The "Wolverine Niche" is the place in the cave, where partially preserved skeleton of particularly large Gulo gulo was found (Photo by K. Stefaniak).
FIGURE 1 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 1. Location of Solna Jama Cave in Europe indicated by red star (1), in Poland marked by red square (2), in the environs of Gniewoszów village indicated by red star (3) and map of the site (4) after Pulina (1996) and Stefaniak et al. (2009).
FIGURE 3. Ursus arctos priscus m2 in Large mammals (carnivores, artiodactyls) from Solna Jama Cave (Bystrzyckie Mts, Southwestern Poland) in the context of faunal changes in the postglacial period of Central Europe
FIGURE 3. Ursus arctos priscus m2 (JSJ/Ua/1) from Solna Jama Cave in occlusal view. Note robust build and arctoid shape of tooth, with only slightly expanded, buccal margin of the talonid. Scale bar equals 10 mm.
Fig. 14 in Late Miocene large mammals from Yulafli, Thrace region, Turkey, and their biogeographic implications
Fig. 14. Map (slightly modified from Vasiliev et al. 2004) of the Tethys (dark grey) and Paratethys (light grey) region in early late Miocene times, showing the main mammalian localities with and without Dorcatherium, and the tentative extent of the provinces discussed in the text. 1, North−Western Province; 2, North−Dacian Province; 3, Balkano−Iranian (= Sub−Paratethyan) Province; 4, Greek Macedonian Province; 5, Eastern Aegean Province; 6, Anatolian Province.
Fig. 13 in Late Miocene large mammals from Yulafli, Thrace region, Turkey, and their biogeographic implications
Fig. 13. Plot of length vs. distal width of the metacarpal of some large late Miocene Giraffidae. Black symbols are for "Palaeogiraffa", others are for Samotherium.
Fig. 9 in Late Miocene large mammals from Yulafli, Thrace region, Turkey, and their biogeographic implications
Fig. 9. Measurements of the cross−section of the lower i2s in various Proboscideans. From Tassy (1986: fig. 14) and y = Yulafll.
Fig. 2 in Late Miocene large mammals from Yulafli, Thrace region, Turkey, and their biogeographic implications
Fig. 2. Indarctos arctoides, TTMEU−CY−46, Yulafli, Turkey, Vallesian, late Miocene. Left mandibular ramus, lateral (A) and occlusal (B) views of p2–m2 (stereo).
Text-fig. 2. ONM T-68, Arsinoitherium cf. zitteli right upper molar fragment from the divide between Oued Cherichera and Oued Grigema, Central Tunisia. a) distal view (apical part towards bottom of page), b) lingual view (apex down, distal surface to right of page) (note the almost vertical enamel-dentine junction), c) occlusal view (lingual part towards top of page). in Arsinoitherium (Embrithopoda) And Other Large Mammals And Plants From The Oligocene Of Tunisia
Text-fig. 2. ONM T-68, Arsinoitherium cf. zitteli right upper molar fragment from the divide between Oued Cherichera and Oued Grigema, Central Tunisia. a) distal view (apical part towards bottom of page), b) lingual view (apex down, distal surface to right of page) (note the almost vertical enamel-dentine junction), c) occlusal view (lingual part towards top of page).
Text-fig. 8. Palaeogene terrestrial fossiliferous deposits of Africa. Note the position of the Tunisian Oligocene deposits, and their obvious interest in terms of geographic position and age (data for the Palaeogene of North Africa are from Tabuce et al. 2000, 2001, 2011, Delmer et al. 2006, Coster et al. 2012, Yans et al. 2014, Solé et al. 2016). Note that Nakwai (Kenya) is no longer considered to be Oligocene. in Arsinoitherium (Embrithopoda) And Other Large Mammals And Plants From The Oligocene Of Tunisia
Text-fig. 8. Palaeogene terrestrial fossiliferous deposits of Africa. Note the position of the Tunisian Oligocene deposits, and their obvious interest in terms of geographic position and age (data for the Palaeogene of North Africa are from Tabuce et al. 2000, 2001, 2011, Delmer et al. 2006, Coster et al. 2012, Yans et al. 2014, Solé et al. 2016). Note that Nakwai (Kenya) is no longer considered to be Oligocene.
Text-fig. 5. Fossil mammals from the Oligocene of Djebel Bou Gobrine, Tunisia, stored in the ONM Museum, El Charguia, Tunis. a–b) (?)Phiomia sp. maxilla containing parts of two upper molars (probably M1/ and M2/) (a – occlusal view, b – buccal view); c–d) anthracothere distal tibia in coarse sand matrix (c – plantar view, d – distal view) (all in scale). in Arsinoitherium (Embrithopoda) And Other Large Mammals And Plants From The Oligocene Of Tunisia
Text-fig. 5. Fossil mammals from the Oligocene of Djebel Bou Gobrine, Tunisia, stored in the ONM Museum, El Charguia, Tunis. a–b) (?)Phiomia sp. maxilla containing parts of two upper molars (probably M1/ and M2/) (a – occlusal view, b – buccal view); c–d) anthracothere distal tibia in coarse sand matrix (c – plantar view, d – distal view) (all in scale).
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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