The changing system of European cities and regions

This paper analyses the current structure of the system of European cities and regions, relations within the system and how it is changing. Cluster analysis distinguished eight regional types: metropolitan, semi‐peripheral and peripheral service regions; central, semi‐peripheral, peripheral and collapsed industrial regions; and agricultural regions. The core of European industrial societies proves to be almost identical with the city belt that dominated economic development in pre‐industrial Europe. Two possible paths of change are discussed: delocalization of simpler, labour cost‐intensive activities towards the periphery (delocalization hypothesis), or structural changes in industrial core regions and persisting marginal status in the periphery (restructuring hypothesis). Neither hypothesis could be confirmed or rejected unequivocally: there were indicators for the continuing importance of urban service centres but no peripheral industrialization for the continuing dominance of industrial core regions while undergoing structural changes. It is concluded that there are hardly any signs of convergence between core and peripheral regions.     

Miliacin in palaeosols from an Early Iron Age in Ukraine reveal in situ cultivation of broomcorn millet

During the archaeobotanical investigation of Scythian–Sarmatian period (Early Iron Age), pits with crop processing waste, discovered in the floodplain of Donets River, eastern Ukraine, and charred remains of cereal grains, dominated by broomcorn millet, were recorded. The grains from the pits were radiocarbon dated to the fifth to first century BC. Those pits are distant from any known contemporaneous settlement. The apparent disconnection of these pits from any local settlement suggests that (1) millet was brought from other locations by mobile groups, or (2) millet was cultivated locally by populations whose settlements have left no discernible archaeological trace. The analysis of molecular biomarkers preserved in palaeosols that are stratigraphically connected to the pits revealed high levels of miliacin, a molecule that can be preserved in ancient soils and sediments, and that is consistent with broomcorn millet (Panicum miliaceum). High levels in miliacin in soils stratigraphically connected to the pits are interpreted as the result of a large biomass of P. miliaceum produced at time of soil formation. Our biogeochemical results applied to a palaeosol thus attest to the in situ cultivation of crops dominated by the broomcorn millet during the early Iron Age in the floodplain of Donets River. Biochemical examination of soils and palaeosols can thus provide useful information on past dynamics of land-use by ancient population, especially when settlements or macrobotanical remains are absent.