L’abri-sous-roche Paléolithique moyen de Mutzig, Rain (Bas-Rhin, F) : reprise des travaux

Detrey, Jean; Guélat, Michel; Hauck, Thomas; Rentzel, Philippe; Vigreux, Thomas

doi:10.3406/bspf.2010.13955

Cited by 1 publication

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“…Current excavations involve an area of 50 m 2 . Excavations began in 2009, with the first season of fieldwork focused on re-opening the trenches dug by Jean Sainty in the 1990s (Detrey et al 2009). The excavations were then extended progressively from both sides of this trench (Koehler et al 2013(Koehler et al , 2016b.…”

Section: History Of Discoveriesmentioning

confidence: 99%

The Middle Paleolithic Occupations of Mutzig-Rain (Alsace, France)

Koehler¹,

Wegmüller²,

Audiard³

et al. 2024

The Rhine During the Middle Paleolithic: Boundary or Corridor?

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The Paleolithic site of Mutzig, discovered by chance in 1992 (Sainty 1992), has been the focus of several excavations since 2009. Located in Alsace (Bas-Rhin, France), it is presently one of only a handful of sites reliably attributed to the Middle Paleolithic in this area, thus providing rare evidence for a zone still relatively unknown for Early Prehistoric remains. The excellent preservation of the remains and the long stratigraphic sequence, with 6 to 8 in situ archaeological levels, make Mutzig a potential reference site for environmental and behavioral analyses for the Middle Paleolithic of the region. At least four archaeological levels contain burnt elements, and one level features a hearth structure. Taken together, the archaeological material, which is abundant in each of the different layers, forms an assemblage of more than 3000 faunal remains and more than 1500 lithic artifacts. Analyses of this site provide valuable insights into the environment and Neandertal ways of life in Alsace. We provide here only general results, with more detailed descriptions of the lithic and faunal remains presented in Diemer (this volume) and Sévêque (this volume). The faunal remains recovered from the human occupations in Levels 5 and 7 reflect the same relatively cold steppe-like environmental context and include reindeer, woolly mammoth, steppe horse, steppe bison and woolly rhinoceros. Small vertebrates also indicate a cold climate, though not related to the Pleniglacial. Confirmed isotopic data, from oxygen and carbon isotope measurements of horse and mammoth teeth, indicate temperatures lower than those of today and an open environment. Levels 9 and 10, however, tend to reveal a more temperate climate. The available OSL and ESR/U-series dates place the Mutzig occupations within the Early Weichselian Glacial (MIS 5, ca. 90,000 BP), an attribution which biometric analyses and the large and small fauna record tend to corroborate (Koehler et al. 2016a).

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Section: History Of Discoveriesmentioning

confidence: 99%