This research attempted to answer the following question: ‘What was the function of the Mesolithic small (<88,5mm) barbed bone points from the North Sea and what does this contribute to our...Show moreThis research attempted to answer the following question: ‘What was the function of the Mesolithic small (<88,5mm) barbed bone points from the North Sea and what does this contribute to our understanding of subsistence strategies of the inhabitants of the North Sea Basin?’ In order to answer this question an assemblage of 28 archaeological small barbed bone points – that originate from the North Sea in front of the Dutch coast of Zuid-Holland – was studied. This thesis started in chapter 1 with an outline of research that was already conducted on these points by Verhart (1986; 1988; 2000) Tsiopelas (2010) and Spithoven (2016). Thereafter, it was explained in chapter 2 how the research was conducted: literature research, experimental archaeology and use wear analysis. In chapter 3, it was outlined how these points fit within the archaeological context: Mesolithic Doggerland. The shooting experiment conducted for this research was discussed in chapter 4 and in chapter 5 the results of this experiment were compared with the results of the use wear analysis. The use wear analysis was conducted on 28 archaeological points in comparison to six experimental points from the shooting experiment. In chapter 6, the social factors which could have influenced the life history of the points were discussed, as well as their function and the representativeness of this research. In the concluding chapter of this thesis (7) the research question was answered followed by a review of the used methods and suggestions for future research. The function of the small barbed bone points from Mesolithic Doggerland could be inferred from the use wear analysis. The points are all (heavily) curated weapon tips. They have developed a high degree of wear and about half of the studied points have remains of reworked barbs present as well. The research area is only a small area of Mesolithic Doggerland which already yielded about 800 of these small barbed bone/antler points. The curation of these points, the function as weapon tips and the overrepresentation within the archaeological record of Mesolithic Doggerland suggests that these weapons were used very frequently. Therefore, it can be inferred that hunting was one an important subsistence strategy. The most used hunting weapon could have been the bow and arrow because the small points are interpreted as arrowheads. However, the use wear analysis could not confirm that the points were specifically used as arrowheads.Show less
During the last ice age, the North Sea was a dry land. Following the deglaciation, it became inundated because of the rising sea levels roughly 8 millennia ago. The North Sea region was inhabited...Show moreDuring the last ice age, the North Sea was a dry land. Following the deglaciation, it became inundated because of the rising sea levels roughly 8 millennia ago. The North Sea region was inhabited by humans and animals and provides major archaeological insights. In this thesis, an analysis of the carbon (δ13C) and nitrogen (δ15N) stable isotopes of 14C dated skeletal remains from the North Sea is performed. The research question is to evaluate the potential outcome for paleo-ecological reconstructions during the Late Pleistocene and the Early Holocene, and contributions regarding human societies - in particular subsistence. The material consists for the most part of mammal skeletal remains, dating from the maximum of the 14C range (ca. 45,000 BP) to the Early Holocene. An overview of the data generated on the basis of all available measurements is given, focusing on stable isotopes. The data are discussed from various perspectives, such as the composition and biases of the database that is used in this thesis. An interesting observation is the difference in diet between Late Pleistocene and Early Holocene terrestrial mammals. This is caused by differences in the consumption of vegetation and suggests a change of landscape during this timerange. The isotope analysis of the North Sea material does confirm pre-existing hypotheses regarding dietary differences between animals. It also confirms the picture of how the North Sea area looked like many years ago: terrestrial and marine ecosystems dominated the Late Pleistocene landscape, after which it became more wet during the Early Holocene with the emergence of freshwater environments, the expansion of the marine environment and subsequent gradual disappearance of the terrestrial ecosystem. The potential of applying stable isotope research for paleo-ecological reconstructions is therefore clearly shown, even when it is based on a relatively limited sample of animal bones available.Show less
