Neolithic Europe - Archaeology

Archaeology

Archeologists believe that food-producing societies first emerged in the Levantine region of southwest Asia at the close of the mini-Ice Age around 12,000 BC, and developed into a number of regionally distinctive cultures by the eighth millennium BC. Remains of food-producing societies in the Aegean have been carbon-dated to around 6500 BC at Knossos, Franchthi Cave, and a number of mainland sites in Thessaly. Neolithic groups appear soon afterwards in the Balkans and south-central Europe. The Neolithic cultures of southeastern Europe (the Balkans, Italy, and the Aegean) show some continuity with groups in southwest Asia and Anatolia (e.g., Çatalhöyük).

Current evidence suggests that Neolithic material culture was introduced to Europe via western Anatolia, and that similarities in cultures of North Africa and the Pontic steppes are due to diffusion out of Europe. All Neolithic sites in Europe contain ceramics, and contain the plants and animals domesticated in Southwest Asia: einkorn, emmer, barley, lentils, pigs, goats, sheep, and cattle. Genetic data suggest that no independent domestication of animals took place in Neolithic Europe, and that all domesticated animals were originally domesticated in Southwest Asia. The only domesticate not from Southwest Asia was broomcorn millet, domesticated in East Asia.

Archaeologists seem to agree that the culture of the early Neolithic is relatively homogeneous, compared both to the late Mesolithic and the later Neolithic. The diffusion across Europe, from the Aegean to Britain, took about 2,500 years (6500 BC - 4000 BC). The Baltic region was penetrated a bit later, around 3500 BC, and there was also a delay in settling the Pannonian plain. In general, colonization shows a "saltatory" pattern, as the Neolithic advanced from one patch of fertile alluvial soil to another, bypassing mountainous areas. Analysis of radiocarbon dates show clearly that Mesolithic and Neolithic populations lived side by side for as much as a millennium in many parts of Europe, especially in the Iberian peninsula and along the Atlantic coast.

With some exceptions, population levels rose rapidly at the beginning of the Neolithic until they reached the carrying capacity. This was followed by a population crash of "enormous magnitude" after 5000 BC, with levels remaining low during the next 1500 years. Populations began to rise after 3500 BC, with further dips and rises occurring between 3000 and 2500 BC but varying in date between regions.