Broomcorn millet (Panicum miliaceum L.) is not one of the founder crops domesticated in Southwest Asia in the early Holocene, but was domesticated in northeast China by 6000 bc. in europe, millet was reported in Early Neolithic contexts formed by 6000 bc, but recent radiocarbon dating of a dozen 'early' grains cast doubt on these claims. Archaeobotanical evidence reveals that millet was common in Europe from the 2nd millennium bc, when major societal and economic transformations took place in the Bronze Age. We conducted an extensive programme of AMS-dating of charred broomcorn millet grains from 75 prehistoric sites in Europe. Our Bayesian model reveals that millet cultivation began in europe at the earliest during the sixteenth century bc, and spread rapidly during the fifteenth/ fourteenth centuries bc. Broomcorn millet succeeds in exceptionally wide range of growing conditions and completes its lifecycle in less than three summer months. Offering an additional harvest and thus surplus food/fodder, it likely was a transformative innovation in European prehistoric agriculture previously based mainly on (winter) cropping of wheat and barley. We provide a new, high-resolution chronological framework for this key agricultural development that likely contributed to far-reaching changes in lifestyle in late 2nd millennium bc europe.

The aim of this article is to view the spatial distribution of Upper Dniester Basin’s (Western Ukraine) barrows and to interpret their location principles. These monuments were often situated on the flattened summits of watershed ridges or hills. It appeared also that some of them were located on upper parts of gentle slopes of not more than 8° of inclination. Mounds appear within linear and group-linear arrangements and were rarely observed as clusters, while more specific adjustments to their location were dependant on local terrain morphology. Barrow alignments run along the elevated ridges, while clustered groups were situated in places where erosive indentations or denudation cavities prevented barrows from stretching in a linear pattern. It can be noted that during the spatial development of barrow alignments, more attention was paid to the intervisibility between the mounds, than to their visibility from other places in the landscape. The potential of observing at least one of the following groups of tumuli from every embankment indicates the direction of movement within the framework of the barrow landscape, perhaps augmented in the past by the presence of paths or “roads”. Examples of analogous or similar, in a certain sense even universal, practices in shaping barrow landscapes were documented also from various parts of Eurasia. Therefore, it is argued these traits were shared by all “barrow societies” and their origins can be traced to the steppe zone. Specific and repeatable patterns of barrow arrangements are a manifestation of certain knowledge and skills, transmitted over generations and immortalized in the landscape that symbolized the incorporation of territory by “barrow societies”. Characteristic mound alignments became a cultural code or institution, as it were – an instrument of familiarising previously unknown landscapes, facilitating movement and simultaneously expressing continuity of kin-lineages.

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Objective: In this work we aim to investigate the origins and genetic affinities of Bronze Age populations (2,400-1,100 BC) from the region of southern Poland and to trace maternal kinship patterns present in the burials of those populations by the use of complete mitochondrial genomes. Materials and methods: We performed ancient DNA analyses for Bronze Age individuals from present-day Poland associated with the Strzyżow culture, the Mierzanowice culture, and the Trzciniec Cultural circle. To obtain complete mitochondrial genomes, we sequenced genomic libraries using Illumina platform. Additionally, hybridization capture was used to enrich some of the samples for mitochondrial DNA. AMS 14 C-dating was conducted for 51 individuals to verify chronological and cultural attribution of the analyzed samples. Results: Complete ancient mitochondrial genomes were generated for 80 of the Bronze Age individuals from present-day Poland. The results of the population genetic analyses indicate close maternal genetic affinity between Mierzanowice, Trzciniec,

The genomic landscape of Stone Age Europe was shaped by multiple migratory waves and population replacements, but different regions do not all show the same patterns. To refine our understanding of the population dynamics before and after the dawn of the Neolithic, we generated and analyzed genomic sequence data from human remains of 56 individuals from the Mesolithic, Neolithic and Eneolithic across Central and Eastern Europe. We found that Mesolithic European populations formed a geographically widespread isolation-by-distance zone ranging from Central Europe to Siberia, which was already established 10 000 years ago. We also found contrasting patterns of population continuity during the Neolithic transition: people around the lower Dnipro Valley region, Ukraine, showed continuity over 4 000 years, from the Mesolithic to the end of Neolithic, in contrast to almost all other parts of Europe where population turnover drove this cultural change, including vast areas of Central Europe and around the Danube River.

The genomic landscape of Stone Age Europe was shaped by multiple migratory waves and population replacements, but different regions do not all show similar patterns. To refine our understanding of the population dynamics before and after the dawn of the Neolithic, we generated and analyzed genomic sequence data from human remains of 56 individuals from the Mesolithic, Neolithic, and Eneolithic across Central and Eastern Europe. We found that Mesolithic European populations formed a geographically widespread isolation-by-distance zone ranging from Central Europe to Siberia, which was already established 10,000 years ago. We found contrasting patterns of population continuity during the Neolithic transition: people around the lower Dnipro Valley region, Ukraine, showed continuity over 4000 years, from the Mesolithic to the end of the Neolithic, in contrast to almost all other parts of Europe where population turnover drove this cultural change, including vast areas of Central Europe and around the Danube River.