Posts Tagged Middle Palaeolithic

Warrimont, de, J.P.L.M.N. 2007. Prospecting Middle Palaeolithic open-air sites in the Dutch-Belgian border area near Maastricht. – PalArch’s Journal of Archaeology of Northwest Europe 1, 3: 40-89

Abstract Since 1981 a series of brickyard quarries to the north and west of Maastricht, in the municipalities of Maastricht (The Netherlands) and Lanaken (Belgium), have been intensively and successfully prospected for human artefacts and faunal remains from the Pleistocene by scrutinising the vertical sections of exposed loess, which in many places is over ten m deep. These efforts were accompanied by extensive geostratigraphic surveys, which have been crucially important in dating the finds and reconstructing the palaeolandscape. Excavation programmes as well as ancillary studies were subsequently carried out at three of these quarries: Maastricht-Belvédère, Veldwezelt-Hezerwater and Kesselt-Op de Schans, each of which yielded multiple Middle Palaeolithic occupation horizons. This article describes the history of these excavations and studies, looking in some detail at the preliminary prospecting work that led to the discovery of this wealth of archaeological open-air sites. A separate description is provided of the litho- and chronostratigraphic frameworks of the three quarries, which has been key in establishing the chronology of Pleistocene occupation of this area. There is particular focus on the landscape and traces of occupation during the Belvédère Interglacial complex at Maastricht-Belvédère and the Weichselian Glacial at Veldwezelt-Hezerwater. The traces of fire and the macrofaunal remains encountered in the respective archaeological horizons are also discussed, and in particular their significance: are these natural phenomena or evidence of interventions by Pleistocene humans?


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Stapert, D. 2007. Neanderthal children and their flints. – PalArch’s Journal of Archaeology of Northwest Europe 1, 2: 16-39

Abstract As pioneer studies at the Magdalenian sites of Pincevent and Etiolles have shown, refitting analyses can reveal the presence of those learning the craft of flint knapping, i.e. children. This approach was successful especially at Upper Palaeolithic sites. Learners can be recognized by their incompetent flaking, and also by typical beginners’ errors such as ‘face battering’ and ‘stacked steps,’ as shown in experiments by Shelley (1990). For reasons unknown to me, and in contrast to the Upper Palaeolithic, it is quite unusual to come across children in the literature about the Lower and Middle Palaeolithic. In most cases, ‘flint failures’ from these periods are attributed to poor-quality raw material. In this paper it is argued, by means of several examples, that in many cases children may be responsible. In his monograph about the main Saalian find level in the Maastricht-Belvédère quarry, De Loecker (2006) mentions that at Site K relatively many cores show phenomena such as stacked steps and face battering. It is suggested that this reflects the presence of children practising their flint knapping skills, rather than the poor quality of the local raw material. The absence of the classic Levallois technology, and the use of the simpler discoidal cores instead, may also be seen in this light. This article describes a series of implements from several sites of the Rhenen Industry in The Netherlands, dating from the Early Middle Palaeolithic. A ‘pic’ and a handaxe-like core reveal incompetent flaking, and the pic-like object also shows ‘face battering’ on both faces. These artefacts, as well as several small cores and a ‘micro-Levallois-flake,’ are interpreted a specimens made by learners in the art of flint working. A miniature handaxe, only 4.4 cm long, is tentatively interpreted as an instructive toy made by an adult for a child. Finally, a few enigmatic objects from the Late Middle Palaeolithic in the northern parts of The Netherlands are also interpreted as pieces worked by children. In the discussion chapter, the literature is searched for further possible examples of this phenomenon. It is concluded that the activities of children are overlooked in studies of the older phases of the Palaeolithic. + erratum.


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Bringmans, P.M.M.A. 2007. First evidence of Neanderthal presence in Northwest Europe during the Late Saalian ‘Zeifen. – PalArch’s Journal of Archaeology of Northwest Europe 1, 1: 1-15

Abstract The Middle Pleistocene to Late Pleistocene transition (MIS 6/5e transition), which has been observed within the loamy sediments of the VLL and VLB sites at Veldwezelt-Hezerwater, was a period of remarkable change in both climate and environment. Indeed, the incipient VLL-VLB soil horizons at Veldwezelt-Hezerwater seem to represent Late Saalian phases of pedogenesis under boreal conditions just prior to the MIS 6/5e transition. The pedostratigraphical position provides a firm basis to conclude that the VLL and VLB soil horizons at Veldwezelt-Hezerwater represent the terrestrial equivalent of the Late Saalian ‘Zeifen Interstadial’ (MIS 6.01), whereas the capping GSL unit seems to represent the terrestrial equivalent of the so-called ‘Kattegat Stadial’. Indeed, assuming that Northwest Europe was too hostile for humans during the extremes of MIS 6 and given the pattern highlighted by Gamble (1986) that Northwest Europe seems to be a bit of a wasteland during MIS 5e, then the VLL and VLB sites at Veldwezelt-Hezerwater offer unique snapshots of people appearing in Northwest Europe for a short spell (MIS 6.01) and then going away again. Indeed, during the period of climatic amelioration during the ‘Zeifen Interstadial’ (ca. 133,000 years BP), which followed the Saalian Glacial Maximum (ca. 135,000 years BP), Northwest Europe probably saw a significant demographic expansion and the development of ‘new’ Middle Palaeolithic technologies. During the Middle Pleistocene to Late Pleistocene transition phase, semi-rotating parallel/prismatic and opportunistic core reduction strategies and ‘small tools’ were in place at the VLL site at Veldwezelt-Hezerwater. So-called ‘expedient’ core reduction strategies wereused to flake locally-found low-quality lithic raw materials. At the VLB site at Veldwezelt-Hezerwater, the same trend towards ‘parallel’ core reduction was also present. However, it is very interesting to see that at the VLB site, Levallois core reduction has also been attested.


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