Timeline

Heritage classified

Key figures

Origin and history

Fontéchevade Cave, located 2 km northwest of Montbron (Charente), is a 30 m long U-shaped natural tunnel. It opens in a valley facing south-west, near the Tardoire, and is at the edge of the communes of Montbron and Orgedeuil. Its geographical environment makes it a strategic site for studying prehistoric occupations, with nearby caves such as Montgaudier (1.5 km) and Placard (4.8 km). Ranked a Historic Monument in 1933, it is a key testimony of lifestyles and human migration during the Paleolithic period.

The excavations, initiated in 1870 by archaeologists such as Pair, Fermond, and Durousseau-Dugontier, intensified in the 20th century, notably under the direction of Germaine Henri-Martin (1937-1955). In 1947, the latter exhumed a cranial cap attributed to a pre-Neanderthalian, considered the oldest human bone discovered in Charente. The archaeological layers, dated from the Tayacian (about 150,000 years old), the Moustarian and the Aurignacian, reveal a continuous and diversified occupation, marked by stone tools (races, burins) and wildlife remains (rhinoceros, hyenas, turtles).

The stratigraphy of Fontéchevade, initially divided into six layers by Henri-Martin, has been revised to include eight, illustrating distinct climatic phases (interglacial Riss-Würm). Human remains include, in addition to the pre-Neanderthal skull, teeth and bones attributed to Homo sapiens (Aurignacian), as well as a Musterian metatarsian. The cave also delivered bone objects (sagay) and a varied lithic industry, reflecting techniques adapted to local resources. Its role as a habitat and place of passage makes it a central site for understanding the cultural transitions of Paleolithic in New Aquitaine.

The fauna discovered in Fontéchevade shows a contrasting environment, ranging from cold steppes (lemmings, Merck rhinoceros) to temperate forests (deams, cervids). These remains, combined with tayacian (chopping-tools) or mossterian (bifaces), suggest human adaptations to climate change. The Aurignacian layers, with their scrapers and burins, mark the emergence of more sophisticated technologies, while perigordian traces (points of the Gravette) extend its occupation to the upper Paleolithic. The cave remains a reference for the study of interactions between humans and ecosystems during Prehistory.

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