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Optical dating of a Fimic Anthrosol in the southern Netherlands
Institution:1. Institute for Biodiversity and Ecosystem Dynamics, Faculty of Science, University of Amsterdam, Nieuwe Achtergracht 166, NL-1018 WV Amsterdam, Netherlands;2. Institute of Geography and Earth Sciences, University of Wales, Aberystwyth, Ceredigion SY23 3DB, UK;1. Département de Préhistoire du Muséum National d’Histoire Naturelle, UMR 7194 CNRS, 1 rue René Panhard, 75013 Paris, France;2. Department of Applied Physics, Okayama University of Science, 1-1 Ridai, Okayama 700-0005, Japan;3. Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, D-04103 Leipzig, Germany;4. Bureau de Recherches Géologiques et Minières, GEO/G2R, BP 36009, 45060 Orléans Cedex 2, France;5. Centro Nacional de Investigación sobre la Evolución Humana (CENIEH) Paseo de Atapuerca, n°3 09002, Burgos, Spain;1. Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, 3012 Bern, Switzerland;2. Oeschger Centre for Climate Change Research, University of Bern, Zaehringerstrasse 25, 3012 Bern, Switzerland;3. Department of Physical Geography and Quaternary Geology, Stockholm University, 10691 Stockholm, Sweden;1. Department of Chemical and Geological Sciences, University of Cagliari, Cagliari, Italy;2. Nordic Laboratory for Luminescence Dating, Department of Geoscience, University of Aarhus, DTU Risø Campus, Roskilde, Denmark;3. Center for Nuclear Technologies, Technical University of Denmark, Risø Campus, Denmark;4. Institute for Biometeorology, National Research Council of Italy, Sassari, Italy;5. Department of Architecture, Design and Planning, University of Sassari, Sassari, Italy;6. CNR-Institute of Geosciences and Earth Resources, CNR, Via Moruzzi 1, 56124 Pisa, Italy;1. Leibniz Institute for Applied Geophysics (LIAG), Stilleweg 2, 30655 Hannover, Germany;2. Department of Geography, RWTH Aachen University, Templergraben 55, 52056 Aachen, Germany;1. MOE Laboratory for Earth Surface Processes, Department of Geography, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China;2. Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China;3. Ordos Antiquity & Archaeology Institution, Ordos, Inner Mongolia Autonomous Region 017200, China;1. Leibniz Institute for Applied Geophysics, Stilleweg 2, Hannover 30655, Germany;2. Kogakkan University, 1704 Kodakushimoto-cho, Ise, 516-8555 Japan;3. Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, D-04103 Leipzig, Germany;4. Center for Nuclear Technologies, Technical University of Denmark, DTU Risø Campus, DK-4000, Roskilde, Denmark
Abstract:Plaggen agriculture was the dominant land use system in the Pleistocene cover sand area of Northwest Europe before the introduction of chemical fertilisers. In today's landscape Fimic horizons and driftsand deposits are characteristic survivors of plaggen agriculture. The age and accumulation rate of these phenomena cannot be satisfactorily determined by conventional methods like pollen analysis and radiocarbon dating. The results of optical dating applied to a Fimic horizon of a plaggen soil near Weert (Netherlands) are compared with those from conventional methods.
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