Abstract

The human skull of Rhünda in Central Germany is one of the rare human remains belonging to the cold episode of the Younger Dryas or GS-1 based on direct radiocarbon dating (10,200±60 uncal BP GrA-15947). The return of periglacial conditions from northern France to northern Germany favoured the expansion of the reindeer herds, as testified by their numerous remains found at the Ahrensburgian sites. The isotopic composition of the collagen (δ13Ccoll and δ15Ncoll) of the Rhünda individual provides insight into the relative dietary contribution of terrestrial ungulates, such as reindeer, compared to the intake of aquatic resources. The systematic higher δ13Ccoll values found for reindeer compared to horse during the Younger Dryas in northern Germany, the Ardennes and south-western England result from a different diet specialization, i.e. the high consumption of lichen by reindeer. The isotopic pattern evidenced in the Pleniglacial reflects such a niche partitioning, while the isotopic pattern of the Late-Glacial Interstadial reveals overlapping ranges in 13C abundances in the different ungulates species, resulting most likely from a decrease in niche diversity. Despite their isotopic variability linked to trophic position and habitat, the freshwater fishes of the Belgian Ardennes show systematic higher δ15Ncoll values (6.6 to 11.7‰) than those of the terrestrial ungulates (<5‰) of the same region and surrounding areas. The high δ15Ncoll value of the Rhünda human (13‰) can thus be explained by an important consumption of freshwater resources, while the δ13Ccoll value (−20.5‰) is too low to consider a significant input of anadromous fishes and their marine-influenced isotopic signature. The application of a Bayesian model confirms this pattern with a minimum contribution of 40% of aquatic resources as protein source for the human diet. In contrast, the input of protein of terrestrial origin hardly exceeded 40% of horse and 20% of reindeer meat consumption. Although existing archaeological and isotopic evidence already suggests a significant use of aquatic resources during the Late-Glacial, the human of Rhünda illustrates an intensive exploitation of the freshwater ecosystem at a time and latitude where the access to palatable plants must have been challenging.

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