Plant use and local vegetation patterns during the second half of the Late Pleistocene in southwestern Germany
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  • 作者:Simone Riehl ; Elena Marinova…
  • 关键词:Upper Paleolithic ; Central Europe ; Pollen ; Plant macrofossils ; Phytoliths
  • 刊名:Archaeological and Anthropological Sciences
  • 出版年:2015
  • 出版时间:June 2015
  • 年:2015
  • 卷:7
  • 期:2
  • 页码:151-167
  • 全文大小:6,055 KB
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  • 作者单位:Simone Riehl (1) (3)
    Elena Marinova (2) (6)
    Katleen Deckers (3)
    Maria Malina (4)
    Nicholas J. Conard (1) (5)

    1. Senckenberg Center of Human Evolution and Palaeoecology, University of Tübingen, Rümelinstr. 23, 72070, Tübingen, Germany
    3. Institut für Naturwissenschaftliche Arch?ologie, University of Tübingen, Rümelinstr. 23, 72070, Tübingen, Germany
    2. Center for Archaeological Sciences, Katholieke Universiteit Leuven, Celestijnenlaan 200E, 3001, Leuven, Belgium
    6. Department Palaeontology, Royal Belgian Institute for Natural Sciences, Rue Vautier 29, B-1000, Brussels, Belgium
    4. Heidelberg Academy of Sciences and Humanities, University of Tübingen, Rümelinstr. 23, 72070, Tübingen, Germany
    5. Institut für ?ltere Urgeschichte, University of Tübingen, Schloss Hohentübingen, 72070, Tübingen, Germany
  • 刊物主题:Earth Sciences, general; Archaeology; Chemistry/Food Science, general; Geography (general); Life Sciences, general; Anthropology;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1866-9565
文摘
In light of recent discoveries of early figurative art in Paleolithic sites of southwestern Germany, gaining an improved understanding of biological, cultural, and social development of these hunter-gatherer populations under past environmental conditions is essential. The analysis of botanical micro- and macrofossils from the Hohle Fels Cave contributes to the limited floral record from this region. These data suggest generally open vegetation, with the presence of wood near Hohle Fels, as indicated by pollen, phytoliths, and evidence from wood charcoal throughout the whole sequence of occupation. The Aurignacian horizons (early Upper Paleolithic, starting around 44,200?calibrated years before present (cal yr BP) correlate with prevailing shrub tundra. Few arboreal pollen in the transitional section from the Aurignacian to the Gravettian horizons (middle Upper Paleolithic, until ca. 32?cal?yr BP) supports the model of an interglacial tundra with a mosaic of cold steppe elements and some patches of woody species. In the Gravettian, the macrobotanical and the palynological records indicate colder climatic conditions and a generally reduced presence of wood patches. Few seed remains, mostly of the Asteraceae and Poaceae families suggesting the use of these plants. The collection of bearberry (Arctostaphylos sp.) for specific purposes is indicated by large amounts of bark fragments.

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