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This study presents new models on the origin, speed and mode of the wave-of-advance leading to the definitive occupation of Europe’s outskirts by Anatomically Modern Humans, during the Gravettian, between c. 37 and 30 ka ago. These models provide the estimation for possible demic dispersal routes for AMH at a stable spread rate of c. 0.7 km/year, with the likely origin in Central Europe at the site of Geissenklosterle in Germany and reaching all areas of the European landscape. The results imply that: 1. The arrival of the Gravettian populations into the far eastern European plains and to southern Iberia found regions with very low human occupation or even devoid of hominins; 2. Human demography was likely lower than previous estimates for the Upper Paleolithic; 3. The likely early AMH paths across Europe followed the European central plains and the Mediterranean coast to reach to the ends of the Italian and Iberian peninsulas.

Evidence for the first Neolithic population in central Portugal dates to as early as c. 7600 cal BP. These first farmers were exogenous groups arriving to the Atlantic coast from the Mediterranean Sea. For a few centuries there seems to have occurred an overlap in the region between the Mesolithic Muge hunter-gatherers and the regional early Neolithic populations. While the trajectory of these first farmers seems to be well established, the fate of the Mesolithic populations is unknown and in generally assumed as resulting in extinction. The recent results from research in the Muge Mesolithic shellmounds (Tagus valley) with the new recovery of various loci with Neolithic occupations including human burials, human DNA, and Strontium analyses seem to indicate evidence of cultural and genetic integration between the Mesolithic and Neolithic populations. This paper will focus on the Mesolithic-Neolithic transition in Portuguese Estremadura and examines the hypothesis that human resilience promoted the cultural and biological integration of the Mesolithic groups into the new exogenous Neolithic communities in central Portugal.

Located at the crossroads of two rather different ecological and cultural worlds (Mediterranean Spain and Portuguese Atlantic), the site of Vale Boi (Algarve, Portugal) is a crucial element in understanding the economic and social traits of the communities that inhabited Southwestern Iberia during the Last Glacial Maximum (LGM). Combining an open-air with a rockshelter component, Vale Boi presents a lengthy Solutrean record starting with a Proto-Solutrean phase followed by a set of occupations in the 25 to 20.3 ka cal BP time-span. The very rich and well preserved assemblages proved that the site was treated, throughout, as a seasonal residential camp and although a striking combination of exogenous cultural traits has been identified, regional adaptive idiosyncrasies are quite evident. This paper focuses on the results of the lithics, fauna, beads and portable art analysis from Vale Boi, and their impact on the comprehension of the LGM ecodynamics in Southwestern Iberia.

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