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Palaeo-environmental and dietary analysis of intestinal contents of a mammoth calf (Yamal Peninsula,northwest Siberia)
Authors:Bas van Geel  Daniel C Fisher  Adam N Rountrey  Jan van Arkel  Joost F Duivenvoorden  Aline M Nieman  Guido BA van Reenen  Alexei N Tikhonov  Bernard Buigues  Barbara Gravendeel
Institution:1. Department of Geosciences, Boise State University, Boise, ID 83725, USA;2. Department of Biology and Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98195, USA;3. Department of Organismal Biology and Anatomy, University of Chicago, Chicago, IL 60637, USA;4. Departamente de Paleontología de Vertebrados, Universidad Nacional de La Plata (CONICET), La Plata B1900FWA, Argentina;1. Dept. of Archaeology, University of Exeter, Laver Bldg., North Park Rd., Exeter, EX4 4QE, UK;2. Institute of Geography, School of GeoSciences, University of Edinburgh, Drummond Street, Edinburgh, EH8 9XP, UK;3. Museo de Historia Natural Noel Kempff Mercado, Universidad Autónoma Gabriel René Moreno, Av. Irala 565, Casilla 2489, Santa Cruz, Bolivia;4. Department of Geography, College of Science, Swansea University, Swansea, SA2 8PP, UK;5. Center for Applied Biodiversity Science (CABS) at Conservation International, 1919 M Street NW, Washingtion, DC, 20036, USA
Abstract:Intestinal samples from the one-month-old Siberian mammoth calf ‘Lyuba’ were studied using light microscopy and ancient DNA to reconstruct its palaeo-environment and diet. The palynological record indicates a ‘mammoth steppe’. At least some pollen of arboreal taxa was reworked, and thus the presence of trees on the landscape is uncertain. In addition to visual comparison of 11 microfossil spectra, a PCA analysis contributed to diet reconstruction. This yielded two clusters: one of samples from the small intestine and the other of large-intestine samples, indicating compositional differences in food remains along the intestinal tract, possibly reflecting different episodes of ingestion. Based on observed morphological damage we conclude that the cyperaceous plant remains and some remains of dwarf willows were originally eaten by a mature mammoth, most likely Lyuba’s mother. The mammoth calf probably unintentionally swallowed well-preserved mosses and mineral particles while eating fecal material deposited on a soil surface covered with mosses. Coprophagy may have been a common habit for mammoths, and we therefore propose that fecal material should not be used to infer season of death of mammoths. DNA sequences of trnL and rbcL genes amplified from ancient DNA extracted from intestinal samples confirmed and supplemented plant identifications based on microfossils and macro-remains. Results from different extraction methods and barcoding markers complemented each other and show the value of longer protocols in addition to fast and commercially available extraction kits.
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