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The Bearded Vulture (Gypaetus barbatus ) as an Accumulator of Archaeological Bones. Late Glacial Assemblages and Present-day Reference Data in Corsica (Western Mediterranean)
Institution:1. Institute of Archaeological Science, University of Hamburg, Germany;2. Terra Mare, Excavation & Research (www.terra-mare.net), Schleswig, Germany;3. Department of Ecology and Evolution, University Frankfurt, Germany;4. WWF Germany, Berlin, Germany;5. Centre for Baltic and Scandinavian Archaeology (ZBSA), Schleswig, Germany;1. RSPB Centre for Conservation Science, Royal Society for the Protection of Birds, The David Attenborough Building, Pembroke Street, Cambridge CB2 3QZ, United Kingdom;2. Bulgarian Society for Protection of Birds/BirdLife Bulgaria, Yavorov Complex, bl. 71, vh. 4, PO Box 50, 1111 Sofia, Bulgaria;3. Hellenic Ornithological Society/BirdLife Greece, Themistokleous 80, GR-10681 Athens, Greece;4. WWF Greece, 21 Lempesi, GR-117 43 Athens, Greece;5. Department of Biological Applications and Technologies, University of Ioannina, 45110 Ioannina, Greece;6. Macedonian Museum of Natural History, Blvd. Ilinden 86, 1000 Skopje, Macedonia;1. Institut Català de Paleoecologia Humana i Evolució Social (IPHES), C. Marcel·lí Domingo s/n, Campus Sescelades URV (Edifici W3), 43007 Tarragona, Spain;2. Área de Prehistoria, Universidad Rovira i Virgili (URV), Avenida de Cataluña 35, 43002 Tarragona, Spain;3. Equipo Primeros Pobladores de Extremadura, Casa de la Cultura Rodríguez Moñino, Avda. Cervantes s/n, 10003 Cáceres, Spain;4. Institució Catalana de Recerca i Estudis Avançats (ICREA), Barcelona, Spain;5. GQP-CG, Grupo Quaternário e Pré-História do Centro de Geociências (uI&D 73 e FCT), Portugal;6. Unit associated to Consejo Superior de Investigaciones Científicas (CSIC), Spain;7. Institute of Vertebrate Paleontology and Paleoanthropology of Beijing (IVPP), China;1. Department of Life Sciences and Systems Biology, University of Turin, Turin, Italy;2. BioArCh, University of York, Heslington, York, United Kingdom;3. Natural History Museum, University of Copenhagen, Copenhagen, Denmark;4. Instituto Internacional de Investigaciones Prehistóricas de Cantabria (Universidad de Cantabria-Gobierno de Cantabria-Banco Santander), Santander, Spain;5. Department of Anthropology, University of New Mexico Albuquerque, NM, USA;6. Nuffield Department of Medicine, Target Discovery Institute, University of Oxford, Oxford, United Kingdom;1. School of Biology, Sir Harold Mitchell Building, University of St Andrews, Fife KY16 9TH, United Kingdom;2. Institute of Tropical Forest Conservation, Mbarara University of Science and Technology, PO Box 44, Kabale, Uganda;3. Department of Zoology, Makerere University, PO Box 7298, Kampala, Uganda;4. NatureUganda, PO Box 27034, Kampala, Uganda;5. Uganda Wildlife Authority, PO Box 3530, Kampala, Uganda;6. Ecological Trends Alliance, PO Box 36839, Kampala, Uganda
Abstract:Assemblages of 751 bone remains of an endemic Corsican deer (Megaloceros cazioti) from Late Glacial layers at Luri- Grı̀tulu cave (Northern Corsica) show an uncommon taphonomic pattern, mainly characterized by high dominance of third phalanxes and high rate of digestion marks. The authors demonstrate that this pattern cannot result from accumulation by human beings or by large mammal carnivores. The bearded vulture, which is able to accumulate large mammal bones in its nest and the presence of which is attested in the faunal remains at Grı́tulu, is the principal putative accumulator. In order to test this hypothesis, bone contents from 11 nests of modern Corsican bearded vultures (871 bone remains, i.e., more than 105 individual carcasses) are analysed from a taphonomic point of view. They are mainly characterized by overwhelming quantities of third phalanxes from middle-size ruminants, abundance and location of digestion marks around proximal articulations, and few bone flakes. A comparison of the Grı́tulu cave assemblages with these new present-day reference data leads to the conclusion that they have actually been accumulated by Late Glacial bearded vultures. Small discrepancies can, however, be explained by differences in food availability between the Late Glacial and modern times.
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