Vegetation changes and human action from the Neolithic to the Bronze Age (7000–4000 B.P.) in Alicante,Spain, based on charcoal analysis

Charcoal analysis reveals various palaeo-ecological phases from the Neolithic to the Bronze Age. Agriculture starts about 7000 B.P. in favourable ecological conditions. Most of the charcoal spectra from sites on the coast represent thermomediterranean holm-oak forest; those from the inland mountains represent mesome-diterranean holm-oak forest. The Neolithic I Impressed Ware people were the first to clear the forest to plant their crops. This clearance of primary woodland resulted in the development of secondary vegetation of pine woods or scrub. The scrub reached its maximum during the Bell Beaker phase and Bronze Age in the Cova de les Cendres. In the Neolithic II open air sites, the percentages of Quercus ilex/coccifera remain high. This may be the result of a different exploitation of the land, or suitable conditions for the growth and survival of the vegetation.     

Prehistory of plant growing and collecting in northern Italy, based on seed remains from the early Neolithic to the Chalcolithic (c. 5600–2100 cal b.c.)

The stages of the early Neolithic and the spread of agriculture in northern Italy are difficult to determine and basically still unclear, since this region was influenced by deeply different cultures coming from both the Mediterranean coasts and the Balkans. The complex interrelations due to the contributions from both cultures are reinterpreted here thanks to recent data, modifying a picture which 15 years ago was believed to be definite. According to radiocarbon chronology, the appearance of the earliest farming communities in northern Italy should be dated around 5600–5500 cal b.c. Early farmers cultivated several cereal and pulse taxa, of which the more important were Hordeum vulgare/distichum, Triticum dicoccum, T. monococcum, T. aestivum/durum/turgidum, Lens culinaris and Pisum sp. In addition they gathered many wild plants. The spread of agriculture was a rapid phenomenon and within a few centuries agriculture was established into the Alps. Little is known about the middle and late Neolithic, with the Square-mouthed pottery culture “Bocca Quadrata”, from c. 5100 cal b.c. onwards, since most of the archaeological features discovered up to the present have produced only a few plant remains. We demonstrate the introduction of poppy and a few other innovations like a slightly increased cultivation of free-threshing cereals and flax. Archaeobotanical analyses from Chalcolithic or Copper Age settlements, from c. 3500 cal b.c. onwards, are even scarcer and a comparison with the earlier Neolithic settlements does not yet seem possible.     

The significance of climate fluctuations for lake level changes and shifts in subsistence economy during the late Neolithic (4300–2400 b.c.) in central Europe

In the last decades, data on the economy and environment of the Neolithic period of lake dwellings (4300–2400 b.c.) in central Europe has increased considerably and also palaeoecological data on lake level fluctuations has been thoroughly elaborated. Lake shores were mainly settled during warm and rather dry climate periods which caused a fall in the lake levels. Nevertheless, there were strong and partly very short-term shifts in the economy during the lake-dwelling period. These can be recognised only because the settlement layers can be very precisely dated by dendrochronology. In this article we discuss in an interdisciplinary way the possible interrelations between climatic and economic changes. To explain the latter, we assume crop failures as the main reason, which caused intensified hunting and gathering. There are three different possibilities which might explain this: cold and wet summers, severe droughts during spring and summer, or local over-exploitation of soils in densely settled areas.     

On the origins and spread of Olea europaea L. (olive) domestication: evidence for shape variation of olive stones at Ugarit,Late Bronze Age,Syria—a window on the Mediterranean Basin and on the westward diffusion of olive varieties

Charred archaeological stones of Olea europaea L. (olive) from Late Bronze Age Ugarit, Syria, were analyzed with geometric morphometry and compared with a morphological differentiation model established on the basis of analyses of modern spontaneous (uncultivated) olive populations and cultivated varieties of various origins within the Mediterranean Basin. The results allow a reinterpretation of the east–west morphological diversity previously observed in wild olives. The archaeobotanical data were compared in detail to the partly geographically structured modern morphological diversity of the cultivated olive. Ancient morphotypes could be distinguished, among which one is dominant in the assemblage. Their diffusion from east to west is shown, and their time of arrival in the northwestern Mediterranean can be evaluated by comparison to archaeological material from that area. Combining morphometric and genetic data, modern reference and archaeological material also guides us in understanding the mechanisms that prevailed in the long-term agrobiodiversity of the olive.