Berit Valentin Eriksen

The European Final Palaeolithic witnessed marked changes in almost all societal domains. Despite a rich body of evidence, our knowledge of palaeodemographic processes and regional population dynamics still needs to be improved. In this study, we present regionally differentiated estimates of absolute numbers and population densities for the Greenland Interstadial 1d-a (GI-1d-a; 14-12.7 ka BP) and the Greenland Stadial 1 (GS-1; 12.7-11.6 ka BP) for Southern, Western, Northern and Central Europe. The data were obtained by applying the Cologne Protocol, a geostatistical approach for estimating prehistoric population size and density, to a newly compiled dataset of Final Palaeolithic sites. On a large spatio-temporal scale, we observe a shift of the main areas of human occupation from the Franco-Cantabrian region, which was intensely occupied during most phases of the preceding Upper Palaeolithic, to regions north of the Alps. At smaller scales, we observe divergent regional trends in the Final Palaeolithic meta-population: during GI 1d-a, a decreasing population in southwestern Europe and an increasing population in north-eastern Central Europe. For the first time since the dispersal of anatomically modern humans into Europe, we see that Central Europe becomes the dominant demographic growth area. Subsequently, the climatic cooling of GS-1 coincides with a pronounced population decline in most parts of the study area. An apparent increase in population density occurs only in north-eastern Central Europe and north-eastern Italy. Our estimates suggest that the total population was reduced by half. Similar results, with a relationship between decreasing temperatures and decreasing populations, have already been observed for the late phase of the Gravettian, when populations were reduced to only one third of those estimated for the early phase. Yet, in contrast to the collapse of local populations during the late Gravettian, the increase in population densities in Central Europe during GS-1 indicates population movements eastwards, possibly in response to deteriorating climatic conditions, particularly in western regions during the Younger Dryas.

This chapter starts with a theoretical introduction to the concept of the creation and perception of cultural landscapes. Niche construction theory and human agency, often treated as controverse concepts are discussed as complementary aspects of human environment relations. The DPSIR framework (the concept of Driving forces, Pressures, States, Impacts and Responses) is applied as valuable approach for the explanation of the transformations in human behaviour in reaction to environmental developments. Aspects of intended and unintended reactions to human agency and action are discussed as well as the temporal and spatial scales of transformations that consequently occured. Therefore, four examples are presented from case studies within the CRC 1266. The Palaeolithic and Mesolithic use of natural resources will have left visible but short-lived traces in the landscape as first steps towards a cultural landscape. The role of humans in the spread of plants and the influence of human action on the plant distribution and composition are discussed in this context. The Neolithic transformation shows a new dimension of changes in the landscape. The producing economy leads to a wide range of resource extractions that enable a much higher population being nourished by the manipulated environment with anthropogenic open land as a new landscape element or niche. Bronze Age progression and intensification of land use in many areas lead to soil degradation and the widespread expansion of heathlands. Even though the process was too slow to be perceived consciously, associated economic adaptations to this new type of cultural landscape are observable. The fourth example explains an unexpected positive aspect of deforestation. In the context of Neolithic Trypillian megasites the soil developed towards a deep and fertile Chernozem. The role of earthworms is discussed as key factor for the soil development in the transition from a forest and forest steppe towards the agrarian steppe of today. The difference between human agency and human action is discussed for the presented examples as the awareness of the consequences of human behaviour very much depends the velocity of changes and human perception.

This chapter explores research pertaining to the possible evidence of copper tools being used in flint knapping processes in early metal-using societies in South Scandinavia. The existence and use of copper as a flint working tool in prehistoric Scandinavian contexts has often been proposed and accepted, but no real study on the implementation as such or the effects on the knapping process has been conducted. In the absence of archaeological evidence, the proof and interpretation must rely on secondary markers, such as technical attributes or trace elements on the flint. Research so far has analysed finished tools to detect and verify the use of copper. This study offers a different approach, relying on production flakes to get a deeper understanding of the production process itself and thus investigating the effects copper knapping tools would have had.

The Baltic Sea basins, some of which only submerged in the mid-Holocene, preserve Stone Age structures that did not survive on land. Yet, the discovery of these features is challenging and requires cross-disciplinary approaches between archeology and marine geosciences. Here, we combine shipborne and autonomousunderwater vehicle hydroacoustic data with up to a centimeter range resolution, sedimentological samples, and optical images to explore a Stone Age megastructure located in 21 m water depth in the Bay of Mecklenburg, Germany. The structure is made of 1,673 individual stones which are usually less than 1 m in height, placed side by side over a distance of 971 m in a way that argues against a natural origin by glacial transport or ice push ridges. Running adjacent to the sunken shoreline of a paleolake (or bog), whose youngest phase was dated to 9,143 ±36 ka B.P., the stonewall was likely used for hunting the Eurasian reindeer (Rangifer tarandus) during the Younger Dryas or early Pre-Boreal. It was built by hunter–gatherer groups that roamed the region after the retreat of the Weichselian Ice Sheet. Comparable Stone Age megastructures have become known worldwide in recent times but are almost unknown in Europe. The site represents one of the oldest documented man-made hunting structures on Earth, and ranges among the largest known Stone Age structure in Europe. It will become important for understanding subsistence strategies, mobility patterns, and inspire discussions concerning the territorial development in the Western Baltic Sea region.

The Lieth Moor area, located in the district of Pinneberg, Schleswig-Holstein, Germany, is a hotspot of Late Palaeolithic settlement activity. The exceptional abundance of archaeological sites is commonly attributed to the presence of a large palaeolake. However, in the Weichselian Late glacial, there were numerous large lakes in Schleswig-Holstein. Thus, a well-founded explanation for the find concentration in Lieth Moor is still lacking, and forming a research desideratum until today. To improve our understanding of this Late Pleistocene landscape and its appeal to hunter–gatherer groups of that time, we conducted a large-scale archaeogeophysical study focusing on a possible ford of the potential palaeolake. We employed Ground-Penetrating Radar and Electromagnetic Induction measurements, supplemented by existing legacy drill-probing data, to identify and map limnic gyttja (organic lake mud) sediments and their spatial distribution within the area. The findings of our study indicate that during the Late Pleistocene to Early Holocene, the Lieth Moor area comprised a cluster of small ponds rather than a continuous lake. These ponds likely interconnected during periods of increased water levels. The presence of dry islands within the region corresponds with archaeological evidence, suggesting that Late Palaeolithic communities visited some of these islands. The absence of the previously postulated palaeolake places the known findings within a completely new palaeoenvironmental context: instead of the previously suspected ford, we assume that the proximity to the Elbe Palaeovalley played a decisive role in the repeated habitation of Lieth Moor. This area, rich in fresh water and fish, along with the dune chain situated to the west, serving as both a vantage point and windbreak, presented an ideal location for awaiting animals migrating along the river Elbe and/or as a resting place within the settlement system of mobile hunter–fisher–gatherer groups.

Bone points were one of the major hunting implements in northern European hunter-gatherer societies. They differ in shapes, types, and manufacturing techniques. In this paper, we investigate 22 bone points from the territory of Lithuania, by studying their morpho-technological characteristics, direct dates, and adhesive residues. The majority are isolated finds, but four points were selected from excavated archaeological sites dated between the 5th and 3rd millennia cal BC. Most of the points belong to the barbed points category, but six slotted points were also studied. Of the 22, 16 previously undated points were sampled for accelerator mass spectrometry radiocarbon (AMS 14C) dating. The results of 10 successfully dated samples are discussed together with previously published 14C dates of bone points from the same region. ATR-FTIR analysis of adhesive residues from six points suggest that birch bark tar was used to haft barbed points and lithic inserts. The results reveal the diversity of types of Early Holocene bone points in the territory of Lithuania, while the slotted and Kunda-type bone points fall into narrow timeframes.

Late Pleistocene hunter-gatherer groups had to cope with extensive climatic changes. When glaciers melted and water levels rose, large areas were flooded. Familiar landscapes disappeared whereas other areas were slowly made available for colonization. Human groups exploiting these pristine territories were few and their settlements scant. Tracking the movements of these elusive pioneers requires the collaborative effort of several scientific disciplines.

Bjerre 7 is a modest Late Bronze Age house in Thy, Denmark. Excellent preservation and full-recovery techniques provided comprehensive evidence of farm self-sufficiency, local exchange, and amber collection for trade. Spatial analyses of ceramics, lithics, plant macrofossils, and amber identified distinctive activity areas at both ends of the house and outside. Routines are discussed for refuse disposal, ceramic use in everyday activities, ad hoc knapping and use of flint tools, plant processing, and amber storage. The household was economically generalized and largely self-sufficient, with limited specialization. Located close to the North Sea, the householders collected raw amber for trade. Metal was obtained from outside for a small-scale, household industry. Although some division of labour is likely, it seems that the whole household engaged in the diverse activities identified on site.

Location modeling, both inductive and deductive, is widely used in archaeology to predict or investigate the spatial distribution of sites. The commonality among these approaches is their consideration of only spatial effects of the first order (i.e., the interaction of the locations with the site characteristics). Second-order effects (i.e., the interaction of locations with each other) are rarely considered. We introduce a deductive approach to investigating such second-order effects using linguistic hypotheses about settling behavior in the Final Palaeolithic. A Poisson process was used to simulate a point distribution using expert knowledge of two distinct hunter–gatherer groups, namely, reindeer hunters and elk hunters. The modeled points and point densities were compared with the actual finds. The G-, F-, and K-function, which allow for the identification of second-order effects of varying intensity for different periods, were applied. The results reveal differences between the two investigated groups, with the reindeer hunters showing location-related interaction patterns, indicating a spatial memory of the preferred locations over an extended period of time. Overall, this paper shows that second-order effects occur in the geographical modeling of archaeological finds and should be taken into account by using approaches such as the one presented in this paper.