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Landscape modification by Last Interglacial Neanderthals.
Roebroeks, Wil; MacDonald, Katharine; Scherjon, Fulco; Bakels, Corrie; Kindler, Lutz; Nikulina, Anastasia; Pop, Eduard; Gaudzinski-Windheuser, Sabine.
Afiliación
  • Roebroeks W; Faculty of Archaeology, Leiden University, P.O. Box 9514, 2300 RA Leiden, Netherlands.
  • MacDonald K; Faculty of Archaeology, Leiden University, P.O. Box 9514, 2300 RA Leiden, Netherlands.
  • Scherjon F; Faculty of Archaeology, Leiden University, P.O. Box 9514, 2300 RA Leiden, Netherlands.
  • Bakels C; Faculty of Archaeology, Leiden University, P.O. Box 9514, 2300 RA Leiden, Netherlands.
  • Kindler L; MONREPOS Archaeological Research Centre and Museum for Human Behavioural Evolution, Schloss Monrepos, 56567 Neuwied, Germany.
  • Nikulina A; Institute of Ancient Studies, Pre- and Protohistoric Archaeology, Johannes Gutenberg-University Mainz, Schönborner Hof, Schillerstraße 11, 55116 Mainz, Germany.
  • Pop E; Faculty of Archaeology, Leiden University, P.O. Box 9514, 2300 RA Leiden, Netherlands.
  • Gaudzinski-Windheuser S; Faculty of Archaeology, Leiden University, P.O. Box 9514, 2300 RA Leiden, Netherlands.
Sci Adv ; 7(51): eabj5567, 2021 Dec 17.
Article en En | MEDLINE | ID: mdl-34910514
ABSTRACT
Little is known about the antiquity, nature, and scale of Pleistocene hunter-gatherer impact on their ecosystems, despite the importance for studies of conservation and human evolution. Such impact is likely to be limited, mainly because of low population densities, and challenging to detect and interpret in terms of cause-effect dynamics. We present high-resolution paleoenvironmental and archaeological data from the Last Interglacial locality of Neumark-Nord (Germany). Among the factors that shaped vegetation structure and succession in this lake landscape, we identify a distinct ecological footprint of hominin activities, including fire use. We compare these data with evidence from archaeological and baseline sites from the same region. At Neumark-Nord, notably open vegetation coincides with a virtually continuous c. 2000-year-long hominin presence, and the comparative data strongly suggest that hominins were a contributing factor. With an age of c. 125,000 years, Neumark-Nord provides an early example of a hominin role in vegetation transformation.

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Tipo de estudio: Prognostic_studies Idioma: En Revista: Sci Adv Año: 2021 Tipo del documento: Article País de afiliación: Países Bajos

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Tipo de estudio: Prognostic_studies Idioma: En Revista: Sci Adv Año: 2021 Tipo del documento: Article País de afiliación: Países Bajos