Dental remains of Lower Miocene small rodents from Napak (Uganda): Afrocricetodontidae,Myophiomyidae, Kenyamyidae and Sciuridae |
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Affiliation: | 1. CR2P-UMR 7207 MNHN-CNRS-Sorbonne Université, Sorbonne Université, Campus Pierre et Marie Curie T.46-56, E.5, case 104, 4, Place Jussieu, 75252 Paris cedex 05, France;2. ISTeP-UMR 7193 Sorbonne Université-CNRS, Sorbonne Université, Campus Pierre et Marie Curie T.56-55, E.5, case 116, 4, Place Jussieu, 75252 Paris cedex 05, France;3. CR2P-UMR 7207 MNHN-CNRS-Sorbonne Université, Département Origines & Evolution, Muséum National d’Histoire Naturelle, CP 38, 43, rue Buffon, 75005 Paris, France;1. Natural Sciences Museum Piatra Neamţ, Petru Rareş No. 26, 610119 Piatra Neamţ, Romania;2. Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, 16500 Prague 6, Czech Republic;3. “Alexandru Ioan Cuza” University of Iaşi, Department of Geology, 20A Carol I Blv, 700505 Iaşi, Romania;4. Dipartimento di Scienze della Terra, Università degli Studi di Torino, Via Valperga Caluso, 35, 10125 Torino, Italy;5. Institute of Geology and Palaeontology, Charles University, Albertov 6, 12843 Prague 2, Czech Republic;1. Dipartimento di Scienze Chimiche e Geologiche, Università di Cagliari, 51, via Trentino, 09127 Cagliari, Italy;2. Centro Studi di Storia Naturale del Mediterraneo, Museo di Storia Naturale Aquilegia – GeoMuseo Monte Arci “Stefano Incani”, Via San Francesco, 09090 Masullas, Italy;3. P.AR.C., loc. S. Antine, 08030 Genoni, Italy;4. Dipartimento di Scienze della Terra, Università di Torino, 35, via Valperga Caluso, 10125 Torino, Italy;5. Institut Català de Paleontologia Miquel Crusafont, Universitat Autònoma de Barcelona, Edifici ICTA-ICP, Carrer de les Columnes s/n, Campus de la UAB, 08193 Cerdanyola del Vallès, Barcelona, Spain;1. Northeastern Research Institute of Petrified Wood and Mineral Resources, Nakhon Ratchasima Rajabhat University, 30000 Nakhon Ratchasima, Thailand;2. Biology Program, Faculty of Science and Technology, Nakhon Ratchasima Rajabhat University, 30000 Nakhon Ratchasima, Thailand;3. Palaeontological Research and Education Centre, Mahasarakham University, 44150 Maha Sarakham, Thailand;4. Department of Biology, Faculty of Science, Mahasarakham University, 44150 Maha Sarakham, Thailand;5. Independent Researcher, 10900 Bangkok, Thailand;6. Institut des sciences de l’évolution de Montpellier, Université de Montpellier, UMR UM-CNRS-IRD-EPHE, 2, place Eugène-Bataillon, 34095 Montpellier cedex 5, France;1. Jurassica Museum, Fontenais 21, 2900 Porrentruy, Switzerland;2. Department of Geosciences, Earth Sciences, University of Fribourg, Chemin du Musée 6, Pérolles, 1700 Fribourg, Switzerland;3. 22, avenue Condorcet, 69100 Villeurbanne, France;4. Naturhistorisches Museum Basel, Augustinergasse 2, 4001 Basel, Switzerland;1. Palaeontological Research and Education Centre, Mahasarakham University, Mahasarakham 44150, Thailand;2. Prehistoric Population and Cultural Dynamics in Highland Pang Mapha Project 6 th Floor, Princess Maha Chakri Sirindhorn Anthropology Centre, 20 Baromaratchachonnani Road, Taling Chan, Bangkok 10170, Thailand |
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Abstract: | The Early Miocene sites of Napak (Uganda), which have been prospected by the Uganda Palaeontology Expedition since 1985, have yielded abundant fossil remains, including a rich and diverse rodent fauna. Ever since the work of Lavocat (1973) on the East African Miocene rodents, which focused mainly on the Kenyan remains (but included some material from Napak discovered by Bishop during the 1950s and 1960s), few studies have been made on the Ugandan specimens. This lack provides motivation for further study of Napak micro-mammals, especially the abundant rodents, which were collected at five sites, Napak IV, V, XV, XXX and XXXI. The fossils described here are attributed to six species representing four families: Afrocricetodontidae (Afrocricetodon songhori, Protarsomys macinnesi), Myophiomyidae (Myophiomys arambourgi), Kenyamyidae (Simonimys genovefae, Kenyamys mariae) and Sciuridae (Vulcanisciurus africanus). Comparison of the dentition of extant and extinct taxa allows us to propose dietary hypotheses (granivory, herbivory and omnivory) for these rodents. In addition, the fossil rodents associated with other fauna from the same localities suggest a more-or-less dense forest environment with clearings, and the probable presence of a humid climate at the time of deposition. |
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Keywords: | Rodentia Uganda East Africa Lower Miocene Napak Dental structure Palaeoenvironment Rodentia Ouganda Afrique orientale Miocène inférieur Napak Structure dentaire Paléoenvironnement |
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