The Quina flaking system is a relatively new Middle Palaeolithic lithic technocomplex recognized and studied until now only in Southwestern France. It has been argued that this technology was...Show moreThe Quina flaking system is a relatively new Middle Palaeolithic lithic technocomplex recognized and studied until now only in Southwestern France. It has been argued that this technology was developed by Neanderthal groups to cope with the decreasing global temperatures and the environmental changes of the last glaciation. The Quina system, until now, is largely unattested in North Europe, where the glacial climate was more pronounced. Why is a technology evolved for the survival in cold environments absent in regions particularly affected by the glaciation? The presence of this technology in the Northern fringes of the Neanderthals’ ecological niche might shed light on the reasons behind Neanderthals’ technological behaviour. It might further provide important clues for a better understanding of whether the variability in the Middle Palaeolithic archaeological record derives from cultural diversity or functional/technical necessities or other factors. This research identifies, through quantitative and qualitative analyses, and comparative studies of lithic materials, the technological traces of unretouched flakes from the site of Colmont-Ponderosa (South Limburg, the Netherlands). This study confirms that at some point during the last glaciation, the Neanderthal groups were users of the Quina technology. The presence of this technology in the North and at such a distance (around seven-hundred kilometers) from the closest certain Quina sites might be the result of techno-cultural convergence. But it might also indicate the point of origin of this technology, which was later dispersed to the Sout, when the environment became too harsh, or it might indicate a dispersal from the South to the North. To confirm this hypothesis a re-evaluation of other Northern assemblages is necessary: if the Quina technology is present at Colmont-Ponderosa, it could be present elsewhere, overlooked because of the relative novelty of the Quina technocomplex.Show less
Climate change has had an influence on hominin evolution for quite some time and led to several speciation and adaptation events. With the later hominin species climate change has less of an impact...Show moreClimate change has had an influence on hominin evolution for quite some time and led to several speciation and adaptation events. With the later hominin species climate change has less of an impact, and extinction theories for the Neanderthals tend to lean in other directions. Despite this, the role of climate change in the Neanderthal extinction is not clear. Older research tended to be focused on global climate records that might not be representative of the smaller climate differences across highly geographically diverse continents. This research provides an overview of local palaeoenvironmental reconstructions for the period of the Middle to Upper Palaeolithic transition in research from 2015-2021 and focuses on the different proxies and climate factors, the stability of the climate, the scale of the research performed, and the perceived influence of climate change on local Neanderthal extinctions. These will be compared per major region (Iberian Peninsula, Apennine Peninsula, Balkan Peninsula, and mid-latitude Europe) in order to determine if any patterns exist. The results show a diversity in the applied proxies and a general trend of deteriorating climate around the time of the Neanderthal extinction. The majority of the research concludes that climate change did not play a major role in the Neanderthal extinction. Despite this, there are some anomalous locations that do not agree with the general consensus this overview produced. Future research at these locations could provide information to nuance the current picture of climate change or corroborate the overall consensus.Show less
The Neanderthal extinction is not fully understood and there is no common consensus on the date of the demise of Neanderthals in Europe. In the Crimean peninsula, located in south-eastern Europe,...Show moreThe Neanderthal extinction is not fully understood and there is no common consensus on the date of the demise of Neanderthals in Europe. In the Crimean peninsula, located in south-eastern Europe, there is evidence for a longer persistence. This thesis investigates the late Neanderthal persistence on the Crimean peninsula. The foraging radius and the settlement patterns of the Crimean Micoquian and the Western Crimean Mousterian are discussed together with analysis of the known radiocarbon dates to gain understanding of the correlation between them. To test the hypothesis that the foraging radius impacted the longer persistence of Neanderthals populations, secondary literature has been analyzed regarding the environmental, lithic and faunal assemblages. The results show that the foraging radius is difficult to determine but it did not have a major influence on the persistence of Neanderthals in Crimea. The radiocarbon datings together with the environmental data concur with the later persistence of Neanderthal populations. Moreover, the Crimean Micoquian was highly adapted in Crimea and especially the mountainous region. The adaptation together with the seasonal movement of prey led to more interaction between Neanderthal populations, which resulted in a potentially higher fitness. This needs to be tested in future research by, for example, the extraction of aDNA from samples of soil of Late Middle Palaeolithic sites. The limitations with this method of testing are the lack of Neanderthal fossils dating to this late period and the presence of palimpsest in many of the Late Middle Palaeolithic sites. Additionally, Russian and Ukrainian literature from previous excavations needs to be translated and re-evaluated to gain more knowledge about the Crimean Middle Palaeolithic as a whole.Show less
Research master thesis | Archaeology (research) (MA/MSc)
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A database of Neanderthal raw material transports and fauna from assemblages across Europe has been compiled with the aim to explore the evolution of the Neanderthals’ mobility behaviour with...Show moreA database of Neanderthal raw material transports and fauna from assemblages across Europe has been compiled with the aim to explore the evolution of the Neanderthals’ mobility behaviour with regard to the environment from the beginning of the Late Saalian (191 ka BP) to the demise of Neanderthals (40 ka BP). Mobility, as observed from the lithic transports in the Palaeolithic, is often interpreted as mirroring the social organisation of a group. As the study of Neanderthal mobility normally focuses on the maximum transport distances of lithics, such a methodology is seen as inadequate because three equifinal processes (subsistence activity, social transactions, and semi-random lithic scavenging) can account for these distances. Here, two different indicators of Neanderthal mobility are created based on the transport distances, quantities, and number of utilised raw material sources. These mobility variables and their relationship to the changing environment are then analysed using novel statistical techniques.Show less
In 2011 Clarkson and Hiscock (2011) presented several regression models for flakes with different platform types used to estimate original flake mass based on platform surface area and external...Show moreIn 2011 Clarkson and Hiscock (2011) presented several regression models for flakes with different platform types used to estimate original flake mass based on platform surface area and external platform angle in order to measure reduction intensity on lithic tools. In addition to subsampling and adding external platform surface area, Clarkson and Hiscock increased the accuracy of the regression models by using a 3D laser scanner to measure platform surface area. Most previous studies multiplied platform width and thickness as an estimate of platform surface area. In this thesis, the regression models created by Clarkson and Hiscock were tested on an archaeological sample from Colmont-Ponderosa, a Middle Palaeolithic site in Limburg, the Netherlands. Instead of a 3D laser scanner, photogrammetry was used to create 3D models. It was found that Clarkson and Hiscock’s models are not applicable on the Colmont-Ponderosa sample. New models were created using the same procedure as Clarkson and Hiscock. In addition to platform type subgroups, flake shape subgroups were made. Creating subsamples based on platform type did not influence the correlation between mass and platform surface area. Subsampling based on flake shape resulted in slightly increased correlation, probably because broader flakes have a higher mass to platform surface area than other flakes. Even though a positive linear correlation between external platform angle and mass was found, this variable was not very influential on the final regression models. It was concluded that the newly created regression models are much better at predicting original flake mass for the Colmont-Ponderosa sample. Mass predictions of individual flakes are still not very accurate, which might result in faulty results when introducing new data.Show less
Research master thesis | Archaeology (research) (MA/MSc)
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The production of bifacial tools is one of the main technological strategies practiced throughout both the Lower and Middle Palaeolithic of northwestern Europe (MIS 15 – 3; ca. 600-35 ka BP)....Show moreThe production of bifacial tools is one of the main technological strategies practiced throughout both the Lower and Middle Palaeolithic of northwestern Europe (MIS 15 – 3; ca. 600-35 ka BP). Within the broad definition of this tool category, there exist wide variation in morphological and technological properties. Additionally, the occurrence of particular biface types seems to vary, both chronologically, as well as geographically. Nowadays, many archaeologists focus on the steering mechanisms behind the observed variations and in doing so apply different methodologies. The bifacial objects used in this thesis to address these broader theoretical questions come from the southern Netherlands, a thus far marginally explored area when it comes to Palaeolithic archaeology. Published data on bifaces is combined with object registrations in the national database (ARCHIS) and primary descriptions of bifacial objects by the author to form a comprehensive dataset of 122 bifacial objects in total. Primarily, these objects are typologically classified with the help of a synthesized methodological framework that combines the main northwestern European typological traditions. The outcome of this analysis shows that the overall typological variation in bifacial objects from the southern Netherlands is more diverse than currently envisaged, which has direct consequences for the conceptualization of Lower and Middle Palaeolithic occupation of the research area. Consecutively, hypotheses for the observed variations in bifacial tool morphology are explored. Despite the limited chronostratigraphic information available for basically all objects, the combined analysis of associated geological formations, their age implications, and the distribution of particular tool types throughout norhtwestern Europe suggests that chronological differentiation in bifacial tool morphology occurs in the research area. At the same time, this explanation does not seem to fully explain the overall variation. Therefore, the technological aspects of morphological variation are explored as well. Scar pattern analysis is performed on four bifaces and shows that these all display long and extended artefact biographies during which likely different phases of use, re-use and recycling occurred. Based on the technological properties of the overall dataset it is proposed that economizing behaviours, in combination with different functional desires, have strongly affected biface morphology in the research area. The final hypothesis explaining variation is that of socio-cultural interactions. A re-analysis of bifacial tools from Sint Geertruid, previously used in such models by other researchers, in combination with their depositional context shows that the current dataset is unsuited for contributing to supra-regional contemporaneous cultural interactions between Neanderthal groups. This examination of the bifacial record of the southern Netherlands has shown that this material has higher potential for understanding hominin occupation and behaviour in this particular region than is currently being exploited. Finally, some suggestions for how to come to such understandings are proposed.Show less
The research examines Neanderthal fossil sites containing more than one individual and investigates the existence of Neanderthal mortuary spaces, a place associated with death, among them. An...Show moreThe research examines Neanderthal fossil sites containing more than one individual and investigates the existence of Neanderthal mortuary spaces, a place associated with death, among them. An overview of Neanderthal fossil sites with respect to the number of individuals indicates that almost 50% contains more than one individuals. The ones with more than five individuals are studied in detail concerning the main features of mortuary space: multiple burial, spatial organization and temporal restriction. At least three sites (La Ferrassie, Shanidar and Amud) appear to be mortuary spaces. On these sites multiple burial and spatial organization are evident but temporal restriction is hard to detect in the existing documentation. No general patterns were detected but traditions within sites are clear. Local natural elements are highly involved in burial structures and in spatial organization, indicating creative landscape use, which could account for the locality of traditions. The existence of mortuary space suggests modernity in Neanderthals behaviour. It also implies that mortuary behaviour emerged gradually and existed in elaborate ways in other species than ours.Show less