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During the restoration of the Radium cinema located in the old Town of Zurich, a stratigraphic sequence of medieval fireplaces came to light. Based on ceramic finds, a preliminary age of about 1000 AD was assigned. In this paper we show the results from archaeomagnetic and radiocarbon dating, which combined with the stratigraphic information yield a better constrain of the period of use of these fireplaces. Whilst the radiocarbon technique continues to be the most widespread methodology for dating young archeological artifacts, archaeomagnetic dating is becoming increasingly more established in Europe thanks to the increased number of available measurements. A Bayesian model on the period of use of these fireplaces was produced with OxCal, by a combination of magnetic and radiocarbon ages, together with the stratigraphic information. The results show that the fireplaces were probably used during 1 to 2 generations (e.g. 20–40 years each), and are in good agreement with the archaeological context of this site. To make use of the magnetic measurements for future reconstructions of the field, we carried out an additional age model using only the radiocarbon and the stratigraphic information. Although some of the structures show large directional scatter due to poor baking in antiquity, the results confirm the trend of the geomagnetic field around 1000 AD.

Tell Seker al-Aheimar, located in the Upper Khabur, northeastern Syria, is an early Neolithic settlement that chrono-culturally spans from the Pre-Pottery Neolithic B (PPNB) to the Proto-Hassuna period (Pottery Neolithic). The site is one of the largest and best documented Neolithic sites in this relatively poorly investigated region in Upper Mesopotamia. Among the occupation sequence of the site with well-defined architectural phases, the Late PPNB settlement (late 8th to early 7th millennium cal. BC) is characterized by an extensive mud-brick architecture, which comprises large multi-roomed rectangular buildings and gypsum-plastered floors. Our research questions center on the identification of domestic activities and their spatial distributions in the site through integrated studies of phytoliths and dung spherulites using an ethnoarchaeological approach. The ethnoarchaeological research included the study of agricultural and dung remains obtained from modern domestic structures from the top of the tell and the modern village of Seker al-Aheimar. The examined activity areas and materials comprised indoor storage and processing spaces, open areas, fireplaces, building materials and livestock enclosures. We use the ethnoarchaeological results to interpret the distributions of both phytolith and spherulite concentrations in archaeological contexts in terms of domestic activities that took place both within and outside buildings. Building spaces and their adjacent areas showed material accumulation resulting from household debris, including food remains, construction materials, matting, hearth cleaning and fuel residues. Indoor activities included the use of certain areas for storage, cereal-processing and cooking. The identification of livestock dung remains in fireplaces suggests the use of dung as a fuel source. We compare these new results with our previous studies of different phases and areas of the site to discuss diachronic and spatial trends in Neolithic household behaviors at Tell Seker al-Aheimar.

The archaeological site “Le Parc du Château” located close to the town of Auneau in the central part of the Paris Basin and 60 km southwest of Paris, was excavated for nearly 20 years, starting in 1979. In addition to Neolithic occupations, the site became famous for its very specific Mesolithic occupations, covering an area of at least 200 m2 and characterized by the presence of more than 70 pits. These features show diverse morphologies and functions: burials, intentional deposits, fireplaces and cooking pits, wedging features, sandstone extraction pits, rubbish pits and possible storage structures. They are attributed to different Mesolithic phases, from the end of the Early Mesolithic to the Late Mesolithic (according to microlith typology and radiocarbon dates). Most of the 70 Mesolithic pits yielded very well-preserved faunal remains in different proportions. The recent analysis of the faunal remains was undertaken, in connection with the analyses of other Mesolithic archaeological features and lithic artifacts in order to better understand the nature of the occupations at Auneau. This constitutes a central question for the understanding of the site itself and concerns the question of mobility patterns during the Mesolithic. This paper focuses on the zooarchaeological analysis of the two main pits excavated at Auneau, both attributed to the Middle Mesolithic. The detailed analysis of both assemblages yielded significant results regarding the function and use of the features, the nature and cycle of occupations involved and, more generally, the characterization of the site. These results offer the opportunity to discuss the question of possible specific sedentism events during the Mesolithic, and also to discuss the role and function of Mesolithic pits.

One of the largest and best known sites of the Central European Gravettian is the Krakow Spadzista site. This article summarizes archaeological, palaeontological, and zooarchaeological data from the site, obtained in the course of more than 40 years of excavations and studies. The site is known mainly from the discovery of the large mammoth bone accumulation in trench B. During field work conducted in a few trenches located close to this assemblage, numerous human artifacts and faunal remains were found. On the basis of analyses of lithic materials, faunal remains, and radiometric data it is concluded that the Krakow Spadzista site was frequently re-occupied during a few weeks or months, by groups of Gravettian hunters in the period 24–22,000 rcyBP This short-term camp site was related to mammoth hunting. The analysis allowed identification of three possible activity zones, characterized by the presence of different groups of flint tools, fireplaces, and different faunal assemblages: a camp area, a lithic workshop, and an animal-processing area, besides the well known accumulation of mammoth bones.

An analysis of energy use by Neanderthals in Northern Europe during the mild Eem interglacial period is carried out with consideration of the metabolic energy production required for compensating energy losses during sleep, at daily settlement activities and during hunting expeditions, including transport of food from slain animals back to the settlement. Additional energy sources for heat, security and cooking are derived from fireplaces in the open or within shelters such as caves or huts. The analysis leads to insights not available from archaeological findings that are mostly limited to durable items such as those made of stone: Even during the benign Eem period, Neanderthals faced a considerable heat-loss problem. Wearing tailored clothes or some similar measure was necessary for survival. An animal skin across the shoulder would not have sufficed to survive even average cold winter temperatures and body cooling by convection caused by wind. Clothes and particularly footwear had to be sewn together tightly in order to prevent intrusion of water or snow. The analysis of hunting activity evolvement in real time further shows that during summer warmth, transport of meat back to the base settlement would not be possible without some technique to avoid that the meat rots. The only likely technique is meat drying at the killing site, which indicates further skills in Neanderthal societies that have not been identified by other routes of investigation.

During the last 15 years, charcoal analysis of archaeological sites in north-western France has been carried out in conjunction with systematic and detailed dendrological examination. By considering these extrinsic criteria in association with the analytical results, palaeo-ethnographic and palaeo-environmental information can be obtained. The charcoals are classically identified under the microscope on the basis of their cellular structure. This examination is associated with an observation of the ligneous structure on transverse sections using a binocular lens. When charcoal fragments are large enough, the growth ring widths are measured. Tree ring curvature is also noted. Finally, alteration by fusion or radial cracks, the presence of fungal hyphae, and insect degradation are also recorded. Results are thus obtained on the nature of fuel used in domestic fireplaces and kilns. The selection of timbers and their catchment areas are also revealed. The average width of the growth rings in oak charcoal from domestic hearths coming from about forty sites in north-western France shows a significant increase from 6000 to 2000 BP. There is a similar increase in the number of heliophilic taxa used from the Neolithic to the Iron Age. This implies that the environment became more and more open because of use by society. The interpretation of the dendrology results applied to charcoal analyses is obtained through a convergence of criteria. Thus, charcoal analysis can provide more than just an identification of the species used, and can yield fundamental information on the interaction of society with the environment.

In the cover sand area of the NW European plain very little is known about fireplaces within Mesolithic settlement areas. Yet the frequent occurrence of burnt ecofacts (hazelnut shells and bone) and artefacts (flint and quartzite) clearly indicates the presence of (surface) hearths on nearly every campsite. Most of these hearths are non-structured and are thus barely visible in the soil. Furthermore in most spatial studies minimal effort has been made to locate these ‘invisible’ hearths as accurately as possible. This paper discusses the potential and modalities of detailed spatial analysis of burnt artefacts and ecofacts, using recently obtained archaeological and experimental evidences. It is concluded that such an analysis can offer interesting insights into the dynamics of Mesolithic hearths.