The cave site of Moula-Guercy, 80 meters above the modern Rhone River, was occupied by Neanderthals approximately 100,000 years ago. Excavations since 1991 have yielded rich paleontological, paleobotanical, and archaeological assemblages, including parts of six Neanderthals. The Neanderthals are contemporary with stone tools and faunal remains in the same tightly controlled stratigraphic and spatial contexts. The inference of Neanderthal cannibalism at Moula-Guercy is based on comparative analysis of hominid and ungulate bone spatial distributions, modifications by stone tools, and skeletal part representations.

Six Middle Palaeolithic sites (Lazaret, Madonna dell'Arma, Caverna delle Fate, Arma delle Manie, Santa Lucia Superiore and San Francesco), dated from Oxygen Isotopic Stages 6 to 3 (OIS 6 to 3), have been studied from a zooarchaeological and palaeoecological point of view. The sites have yielded faunal assemblages rich in cervids, generally dominated by Cervus elaphus. The frequency of other ungulate taxa is inextricably linked to the topography of each site, as well as to climatic and environmental conditions. Taphonomic analysis indicates that humans were the main agents of accumulation of the large mammal remains. Mortality and seasonality data show various patterns of age distribution of the ungulate species, and suggest that there is no relation between the occupation season of these sites and the hunting of a particular species. The dominance of red deer can be explained by their natural abundance and by their high rendering in terms of hunting transport, meat quantity, and other useful materials like skins, tendons, and soon. Neanderthal subsistence strategies do not show any evolution in the studied area during the period of Oxygen Isotopic Stages 6 to 3.

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The first “Out of Africa” migrations represent a seminal event in the history of humankind. At the gates of Europe, the first appearance of Hominins is recorded in Georgia, 1.8 million years ago (Ma); however, the picture of migration across the continent remains incomplete. Vallonnet Cave (France) is a Lower Paleolithic prehistoric site with traces of hominin activities including lithic remains and cut-marks on mammal bones. Here, we apply the uranium-lead (U-Pb) methods to two flowstones to date the intervening archaeological levels. The U-Pb data, coupled with paleomagnetic constraints, provide an age range from 1.2 to 1.1 Ma. The results conclusively demonstrate that Vallonnet Cave is one of the oldest European prehistoric sites in France with early hominin occupations associated with an Epivillafranchian fauna. Combined with data from other archaeological sites, the new precise chronology suggests a widespread occupation the Northern Mediterranean to Southwestern Europe at ~1.2 Ma.

Investigating diet breadth is critical for understanding how archaicHomopopulations, including Neanderthals, competed for seasonally scarce resources. The current consensus in Western Europe is that ungulates formed the bulk of the human diet during the Lower and Middle Paleolithic, while small fast prey taxa were virtually ignored. Here, we present a multisite taphonomic study of leporid assemblages from Southern France that supports frequent exploitation of small fast game during marine isotope stages 11 to 3. Along with recent evidence from Iberia, our results indicate that the consumption of small fast game was more common prior to the Upper Paleolithic than previously thought and that archaic hominins from the northwestern Mediterranean had broader diets than those from adjacent regions. Although likely of secondary importance relative to ungulates, the frequent exploitation of leporids documented here implies that human diet breadths were substantially more variable within Europe than assumed by current evolutionary models.