New insights into the neolithisation process in southwest Europe according to spatial density analysis from calibrated radiocarbon dates

The agricultural way of life spreads throughout Europe via two main routes: the Danube corridor and the Mediterranean basin. Current archaeological literature describes the arrival to the Western Mediterranean as a rapid process which involves both demic and cultural models, and in this regard, the dispersal movement has been investigated using mathematical models, where the key factors are time and space. In this work, we have created a compilation of all available radiocarbon dates for the whole of Iberia, in order to draw a chronological series of maps to illustrate temporal and spatial patterns in the neolithisation process. The maps were prepared by calculating the calibrated 14C date probability density curves, as a proxy to show the spatial dynamics of the last hunter-gatherers and first farmers. Several scholars have pointed out problems linked with the variability of samples, such as the overrepresentation of some sites, the degree of regional research, the nature of the dated samples and above all the archaeological context, but we are confident that the selected dates, after applying some filters and statistical protocols, constitute a good way to approach settlement spatial patterns in Iberia at the time of the neolithisation process

Population dynamics during the Neolithic transition and the onset of megalithism in Portugal according to summed probability distribution of radiocarbon determinations

As field data accumulates, the study of Neolithic Portugal has been receiving increasing attention recently, from material culture and subsistence to ideology. However, little is known about population dynamics. In this paper, we use a judicious selection of radiocarbon determinations to evaluate demographic phenomena within the 9.500-5.000 cal BP range (thus, starting in the Late Mesolithic) making use of "summed probability distribution" analysis. In greater Portugal, results show a negative deviation (i.e. demographic decrease) at 6.400-6.300 cal BP and a positive deviation (i.e. demographic increase) at 5.350-4.950 cal BP. These can be explained, respectively, by the impact of farming about one millennium after its introduction (confirming the "Neolithic demographic transition" model) and by the full establishment of the "secondary products revolution" in the Late Neolithic. However, individual analyses of the northern and southern halves of the country-i.e. using the Mondego river valley as an ecological-geographical divide-show rather contrasting trajectories, with scarce Mesolithic populations and a demographic increase in the megalithism in the North, whereas in the South a demographic crisis occurred at the onset of megalithism (which remains to be fully explained) being followed in the Late Neolithic by a sharp demographic increase. Further summed probability distribution analyses of radiocarbon determinations, particularly if combined with other populational proxies, will be able in the future to detect other demographic events taking place in space and time.Juan de la Cierva postdoctoral grant [FJCI-2016-30588]Catalonian government [PGC2018-096943-B-C21]Spanish governmentSpanish GovernmentEuropean Commission [2017-SGR-1302]APOSTD Postdoctoral grant by the Valencian government [APOST/2019/179]info:eu-repo/semantics/publishedVersio