Prehistoric Archaeological Sites Research Articles

Enhanced dietary reconstruction of Korean prehistoric populations by combining δ13C and δ15N amino acids of bone collagen.

Compound specific stable isotope analysis of amino acids (CSIA-AA) is a powerful tool for determining dietary behaviors in complex environments and improving dietary reconstructions. Here, we conducted CSIA-AA on human (n = 32) and animal (n = 13) remains from two prehistoric archaeological sites (Mumun, Imdang) to assess in more detail the dietary sources consumed by prehistoric Korean populations. Results of estimated trophic position (TP) using Δ15NGlx-Phe show that the Imdang individuals consumed aquatic resources, as well as terrestrial resources. Principal component analysis (PCA) using δ13C and δ15N essential amino acid (EAA) values show that the Imdang humans closely cluster with game birds and terrestrial herbivores, whilst the Mumun humans closely cluster with C4 plants. Quantitative estimation by a Bayesian mixing model (MixSIAR) indicates that the Imdang humans derived a large proportion of their proteins from terrestrial animals and marine fish, whereas the main protein sources for the Mumun humans were C4 plants and terrestrial animals. Additionally, the comparison between the EAA and bulk isotope models shows that there is a tendency to overestimate the consumption of plant proteins when using bulk isotopic data. Our CSIA-AA approach reveals that in prehistoric Korea there were clear differences in human diets through time. This study adds to a growing body of literature that demonstrates the potential of CSIA-AA to provide more accurate estimations of protein consumption in mixed diets than previous bulk isotopic studies.

Preliminary Study on Microbial Deterioration Control and Effectiveness Evaluation in the Neolithic Prehistoric Archaeological Site of Dadiwan, Northwest China

Microbial deterioration as one of the widespread problems in archaeological site museums significantly affects their safety and exhibits. This paper systemically investigated the environments and conditions of microbial outbreaks in the Dadiwan No. F901 site museum, which is a representative archaeological site of prehistoric Yangshao culture. The morphology and harmful characteristics of the outbreak microorganisms were analyzed by microscopic techniques. The ultraviolet resistance of harmful microorganisms was also studied. Combining these findings with the original facilities of the site museum, a scientific and reasonable project was proposed to control and prevent the activity of harmful microorganisms. In addition, a 1% OIT/DCOIT biocide concentration was applied to inhibit microorganism-caused deterioration, in combination with mechanical removal based on laboratory tests and screening in situ. The effectiveness of microbial control was assessed using a portable microscope, ATP bioluminescence assay, and color difference detection. As a long-lasting preventive measure for microbial deterioration, an ultraviolet sterilization system can efficaciously prevent the re-outbreak of microbial deterioration to form a relatively stable dynamic balance for the surroundings of the site. This study is a resultful exploration in terms of microbial control and plays an important role in the sustainable protection of archaeological site museums.

The Caucasus and the Middle East in the early Holocene (According to recent archaeological research)

The article provides a comprehensive account of two significant prehistoric archaeological sites located in Adjara - Kobuleti village and Khutsubani, including their history, modern investigations, and findings. The authors highlight that bone remains were not uncovered during the excavation of Stone Age archaeological sites due to the soil'speculiarities. These remains could have shed light on the hunting environment of that era. Stone artifacts provide insight into the lives of ancient hunter-gatherers in our regionThus, a thorough examination of the stone industry is very important. According to this analysis the authors, a fascinating conclusion is drawn regarding the origins of the Western Transcaucasia stone industry. During the early Holocene era, a new method of stone processing and various types of tools emerged within the aforementioned region. This innovative approach was originally developed in the territory of Iran and Iraq. It's a Mlefaatien culture, which comprises of many significant sites. After conducting a techno-typological analysis of the stone complex, it is believed that hand pressure techniques, backed microblades, Kashkashok side-blow blade-flakes, grooved tools etc. emerged in Western Georgia result of the great migration process from Middle East in the beginning of the 10th millennia BC. This view is supported by the complete range of precise dates, which accurately reflect the migrations ways and times of the early migrants. Additional inquiries in this field, conducted in the future, will undoubtedly uncover even more fascinating insights.

Earliest systematic coal exploitation for fuel extended to ~3600 B.P.

Coal has long fueled human civilizations. The history of systematic coal fuel exploitation has been traced back to the late third millennium before present (post-2500 B.P.). Although sporadic combustion of coal for fuel was reported in some prehistoric archaeological sites, evidence for the systematic exploitation of coal for fuel before 2500 B.P. remains lacking. Here, we report comprehensive understanding for the earliest systematic exploitation of coal for fuel at the Jirentaigoukou site in Xinjiang, northwestern China, at ~3600 B.P. The main body of the site witnessed systematic exploitation of bituminous coals, illustrating a complete chaîne opératoire with selective mining, planned storage, and extensive combustion. Our results transform the knowledge of energy history by extending the upper limit of the systematic exploitation of coal for fuel by approximately a millennium, and provide a precedent of energy transition under intense conflict between social demand and environmental deterioration.

Fires of a House—Burning Events in a Middle Bronze Age Vatya House as Evidenced by Soil Micromorphological Analysis of Anthropogenic Sediments

The investigation of fires and burning within the archaeological record has a long history, and the applied methods are diverse. There have been several investigations of prehistoric archaeological sites, but Middle Bronze Age contexts (2000–1450 BC) of the Carpathian Basin have not been widely studied beyond studies of ritual burning or warfare. In this paper, we aimed to add further details to this topic in the household context via thin-section soil micromorphology and related phytolith and charred plant matter analysis. The combination of these techniques has been proven to be advantageous due to their high-resolution quality, but phytolith analysis of soil/sediment via thin sections (i.e., in fixed environment) has not been largely explored yet. In this study, these methods were used to investigate various burning events that affected a Middle Bronze Age Vatya house within the tell site of Százhalombatta-Földvár, Hungary. Three types of fire/burning events were investigated. One was related to hearth activity, another one to a presumed ‘cleaning’ of the house, and the last one to the termination of the building. In the first two cases, everyday life was under the microscope; the latter was more enigmatic, and probable intentional destruction was demonstrated.

Abu Hureyra, Syria, Part 1: Shock-fractured quartz grains support 12,800-year-old cosmic airburst at the Younger Dryas onset

A previous investigation revealed that shock-fracturing, a form of low-pressure shock metamorphism in quartz grains, can be produced during near-surface atomic airbursts and in cosmic impact structures, most likely at pressures lower than 8 GPa. This discovery implies that similar shock-fracturing may also form in quartz grains exposed to near-surface airbursts by comets and asteroids. Here, we investigate this hypothesis by examining quartz grains in a sedimentary profile from Abu Hureyra, a prehistoric archaeological site in northern Syria. This site was previously proposed to have experienced a nearby, low-altitude cosmic airburst at the onset of the Younger Dryas (~12,800 years ago). The Younger Dryas boundary layer (YDB) at Abu Hureyra has previously been shown to contain a rich assemblage of materials consistent in indicating a cosmic impact. These include anomalously high concentrations of melted micro-spherules displaying increased remanent magnetism; meltglass with low water content indicative of high-temperature melting; nanodiamonds, potentially including lonsdaleite; carbon spherules produced by biomass burning; black carbon or soot; total organic carbon; and abnormally high-temperature melted refractory minerals and elements, including platinum, iridium, chromite, and zircon. To further test this impact hypothesis, we searched for evidence of shocked quartz, a robust, widely accepted indicator of cosmic impacts. We used a comprehensive analytical suite of high-resolution techniques, including transmission electron microscopy (TEM) and electron backscatter diffraction (EBSD), to examine and characterize quartz grains from the YDB layer at Abu Hureyra. Our analyses revealed the presence of quartz grains with sub-planar, sub-parallel, and sub-micron-wide intragranular fractures, most likely produced by mechanical and thermal shock or the combination of both. Furthermore, these fractures are typically filled with amorphous silica (glass), a classic indicator of shock metamorphism. Elemental analyses of the weight percentages of oxygen in the amorphous silica indicate that this could not have formed from the deposition of hydrated silica (e.g., opal and hyalite), which is enhanced in oxygen. Instead, the silica we observed is typically depleted in oxygen, consistent with melting under highly reducing conditions. The shock fractures in quartz grains also display Dauphiné twinning, which sometimes develops during the stress of high temperatures or pressures. This evidence is consistent with the hypothesis that the glass-filled fractures in quartz grains were produced by thermal and mechanical shock during a near-surface cosmic airburst at Abu Hureyra. These glass-filled fractures closely resemble those formed in near-surface atomic airbursts and crater-forming impact events.

GROUP OF SUOI BA ARCHAEOLOGICAL SITES (DAK NONG PROVINCE): DOCUMENTS, PERCEPTION, AND DISCUSSION

This article introduces the results of investigations and surveys from 2006 to 2017 of the group of Suoi Ba archaeological sites in Nhan Co commune, Dak R’Lap district (Dak Nong). The results reveal eight prehistoric archaeological sites in the Suoi Ba area, which are distributed over an area of about 20 hectares, equivalent to the size of an ancient village, and date from 3,500 to 2,000 years BP. In this study, the authors systematize materials, assess historical-cultural values, briefly outline the prehistoric cultural process at Suoi Ba during the late Neolithic and early Metal Age in Dak Nong, and discuss issues related to Suoi Ba relics in a broader context.

Geochemical Indication of Functional Zones at the Archaeological Sites of Eastern Europe

The article considers a new approach for determining the functional zones of the prehistoric archaeological sites in Eastern Europe by the method of geochemical indication: the use of mathematical statistics for processing the geochemical data of cultural deposits at archaeological sites, and the identification of groups of interrelated chemical elements and compounds that reflects the processes of natural sedimentation and anthropogenic activity. It makes it possible to separate the lithological and anthropogenic components. This approach is important for the identification of geochemical element groups associated with different functional zones. The reconstructions were conducted at the Neolithic, Early Metal Age, and the Bronze-Early Iron Age sites in Eastern Europe. Abnormal concentrations of the association (P2O5antr, CaOantr and Srantr) in sediments are attributed to zones of accumulation of bone remains. Anomalous concentrations of a group of elements (K2Oantr, Rbantr) in deposits are associated with wood ash and fireplaces, ash residues from ritual activities, and fires. The group of elements (Ba, MnO, Corg) reflects the accumulation of humus and organic remains, and can characterize areas with food residues, skins, and rotten wood. With the help of the distribution of the main lithological elements (SiO2, Al2O3) in sediments, it is possible to reconstruct the paleorelief at the sites.

Late Pleistocene aeolian deposition and human occupation on the eastern edge of the deglacial corridor, northeastern Alberta, Canada

AbstractThe lower Athabasca River basin in northeastern Alberta contains one of the highest known concentrations of prehistoric archaeological sites in the boreal forests of western Canada. This is due to the combination of readily available sources of lithic raw material stone near a major travel corridor, and extensive archaeological survey conducted in advance of oil sands mining. Typological studies have proposed immediate post-glacial occupations that were contemporaneous with, or immediately followed, the catastrophic glacial Lake Agassiz flood through the area at the end of the Pleistocene. Here, we complement the typology age estimates by using stratigraphic relations and infrared stimulated luminescence (IRSL) dating of aeolian material to determine the age of initial human occupation, and reconstruct the environment encountered by early inhabitants of the region. We find that the first occupations in our study area took place near the Pleistocene-Holocene boundary (ca. 11.3 ± 0.8 ka BP), shortly after catastrophic flooding from Lake Agassiz. The post-flood environment was dominated by cold climatic conditions that supported permafrost, presumably during the late Pleistocene, and underwent significant aeolian deposition. Our results indicate that this area represents a portion of the eastern edge of the deglacial corridor into which plants, animals, and humans dispersed following retreat of the Laurentide Ice Sheet.

Development of Predictive Geoarchaeological Models to Locate and Assess the Preservation Potential of Submerged Prehistoric Sites Using Remote Sensing, Palaeoenvironmental Analysis, and GIS

Using the Mesolithic site of Tudse Hage in the Great Belt of Denmark, this paper proposes a generic stepwise process to create geoarchaeological models that output seamless morphology maps in a GIS. This was achieved using remote sensing databases and the collection of marine geophysical data, above and below the seabed. On the basis of these data, key areas, with sediment sequences representative of the postglacial transgression surfaces, were identified. Core samples were taken for palaeoenvironmental analysis and dating that enabled a reconstruction of the relative sea-level changes. Using this information, palaeogeographic coastline maps of the Kongemose, late Kongemose, Ertebølle, and Neolithic periods in the Tudse Hage area were prepared, and potential hotspots for archaeological sites were proposed. Since their inundation, submerged prehistoric archaeological sites have been, and are, dynamic, with anthropogenic and natural processes affecting their stability and preservation. With the advocation of in situ preservation as a means of managing underwater cultural heritage, predicting where sites have survived these processes, and where they can be found, in advance of subsea development or other anthropogenic exploitation, is essential. Future natural threats to sites preserved in situ were determined through the modelling of seabed currents and sediment erosion.

Underground Environments, Worldviews, and Sustainable Stewardship

This paper examines an aspect of a value-based approach to underground built heritage (UBH). A key tool for the manager of any built heritage today is the mapping of its manifold values for different audiences, to inform their management strategy. This paper first reviews an important paradigm shift that has occurred in the humanities and in cultural heritage management, leading to the recognition of the centrality of the worldviews and lived experience of the different members that make up communities. Drawing on a selection of examples from the literature, it then demonstrates how many UBH sites across a wide spectrum of cultures acquired cosmological and cultic value and significance in a way that is qualitatively different to most built heritage sites above ground. The spectrum of challenges that this poses to the UBH site manager is then outlined by reviewing literature on a selection of UBH examples, from prehistoric archaeological sites to living religious sites. Some key guiding principles are proposed for the management of these different scenarios. Culturally sensitive management that respects the existing value systems of local communities is indispensable wherever such communities are present. Decision-makers need to be keenly aware of these value systems and need to recognize, empower, and complement existing traditional systems of stewardship.

Predicting wildfire impacts on the prehistoric archaeological record of the Jemez Mountains, New Mexico, USA

BackgroundWildfires of uncharacteristic severity, a consequence of climate changes and accumulated fuels, can cause amplified or novel impacts to archaeological resources. The archaeological record includes physical features associated with human activity; these exist within ecological landscapes and provide a unique long-term perspective on human–environment interactions. The potential for fire-caused damage to archaeological materials is of major concern because these resources are irreplaceable and non-renewable, have social or religious significance for living peoples, and are protected by an extensive body of legislation. Although previous studies have modeled ecological burn severity as a function of environmental setting and climate, the fidelity of these variables as predictors of archaeological fire effects has not been evaluated. This study, focused on prehistoric archaeological sites in a fire-prone and archaeologically rich landscape in the Jemez Mountains of New Mexico, USA, identified the environmental and climate variables that best predict observed fire severity and fire effects to archaeological features and artifacts.ResultsMachine learning models (Random Forest) indicate that topography and variables related to pre-fire weather and fuel condition are important predictors of fire effects and severity at archaeological sites. Fire effects were more likely to be present when fire-season weather was warmer and drier than average and within sites located in sloped, treed settings. Topographic predictors were highly important for distinguishing unburned, moderate, and high site burn severity as classified in post-fire archaeological assessments. High-severity impacts were more likely at archaeological sites with southern orientation or on warmer, steeper, slopes with less accumulated surface moisture, likely associated with lower fuel moistures and high potential for spreading fire.ConclusionsModels for predicting where and when fires may negatively affect the archaeological record can be used to prioritize fuel treatments, inform fire management plans, and guide post-fire rehabilitation efforts, thus aiding in cultural resource preservation.

The Equipment of the Tyrolean Iceman: Innovation versus Adaptation in the Cultural Evolution of Prehistoric Technologies.

This study argues that the equipment of the Tyrolean Iceman offers a unique perspective for understanding the macroevolutionary-scale functional continuity between later Pleistocene and Holocene human technologies. The Iceman was discovered in 1991 in the Ötztal Alps and can be dated to around 3300 BC, corresponding to the North Italian early Copper Age. In his gear there are several technologies which are rarely found at prehistoric archaeological sites, including archery equipment, a complete set of clothing, and a personal tool kit. Our paper will discuss this technological assemblage within the framework of cultural evolutionary theories (subsequently abbreviated as CET). According to the concept of cumulative culture, tools and technologies may become the subject of cultural "descent with modification" which leads to the emergence of complex technological innovations. In conventional narratives, the Neolithic represents the single greatest macroevolutionary transition in human cultural evolution, accompanied by a whole set of novel innovations and encompassing the transition to agriculture. However, as we highlight, the Iceman's equipment includes several technologies with a pre-Neolithic cultural origin. Earlier variants of these technologies were used by cultural groups belonging to the Mesolithic and even the Upper and Middle Paleolithic. Our main goal will be to present an explanatory framework for this macroevolutionary-scale technological continuity. In order to achieve this goal, we explore the heuristic value of two basic concepts of cultural evolutionary explanations-namely, the concepts of innovation and adaptation. Building on this background, we present an overview of the data currently available on the evolutionary history of each technological adaptation found in the equipment of the Iceman. Our results suggest that these technologies were not primarily cultural innovations, but simultaneously they were "obligatory" functional adaptations with a deep evolutionary history.

Territorial Assessment of the East Kazakhstan Geo/Ecotourism: Sustainable Travel Prospects in the Southern Altai Area

In spite of picturesque landscapes, natural beauties and authentic traditional lifestyles to be seen in East Kazakhstan, tourism is far from being developed. The Kazakh Altai (called the Kazakh Switzerland) is one the most colourful parts of the country and, indeed, all Central Asia. The attractiveness of this geographically isolated region (formerly a part of the Imperial Russia), consisting of rocky semi-deserts, vast parkland-steppes, and rugged mountain terrains, is reflected in its distinctive geological and geomorphological character, its pristine nature, and its extraordinary geodiversity and biodiversity. This study presents a roster of geotourism and ecotourism loci for the broader Altai area within a framework of sustainable development. The modelled assessment of the tourism and recreation potential is based upon multi-proxy analyses of GIS, DEM, and cartographic data. It integrates the most appealing natural (biotic and abiotic) site-specific natural features across all physiographic zones within a broad region. The most significant and representative geosites fall within three geographic sectors suitable for geo- and ecotourism. Prospects for travel to these places are enhanced by the presence of numerous prehistoric archaeological sites and historical monuments, which document the rich, multi-ethnic background of Kazakhstan and the ancient Silk Road that traverses it. These geological, environmental and cultural resources, and the regional geoheritage and environmental conservation concepts have been figured into strategies for economic growth of rural Kazakhstan. Visitors travelling to this most appealing region are constrained by climate of pronounced continentality, seasonality, geographic accessibility, the international border-zone regulations and a lack of services of an international standard.

Using Dynamic Image Analysis as a Method for Discerning Microdebitage from Natural Soils in Archaeological Soil Samples

ABSTRACT Unlike larger stone tools and debitage, the analysis of microdebitage (measuring less than 6 mm) allows for identifying likely areas where stone tools were manufactured at prehistoric archaeological sites. The tedious, time-consuming, and costly nature of microdebitage, however, has overshadowed its data potential, making most archaeologists wary of implementing this method. To alleviate these issues, this study introduces an experimental protocol using Dynamic Image Analysis (DIA) as a potential method for differentiating between microdebitage and natural soils within archaeological soil samples. In this study, a particle analyzer was employed to test whether microdebitage can be quantifiably identified within archaeological soil samples without the need for flotation and manual sorting. The results of the Multivariate Analysis of Variance (MANOVA) test demonstrate significant differences (p < 0.001) between the lithic and soil datasets, indicating that DIA is a viable and promising method for differentiating between microdebitage and natural soils within archaeological soil samples.

Vinča Burials in the Research of Miloje M. Vasić

Miloje M. Vasić (1869–1956) is considered to be the founding father of Serbian archaeology. This paper directly challenges, as based on detailed archival research, the prevailing view that his excavation of the Vinča archaeological site is a model standard for Serbian archaeology. Instead, Vasić’s handling of the excavation was selective, non-systematic and destructive when viewed today from the perspective of modern practices.&#x0D; Vasić originally gained authority based on the discovery of Vinča, a prehistoric archaeological site that contains layers from the Neolithic to the middle ages. In his zeal to uncover “prehistory”, he deliberately ignored the other archaeological layers present. The most significant example of neglected archaeological remains is his excavations of Vinča’s medieval cemetery where he did not document observations systematically. This prioritization of the importance of one archaeological period over another was reflected in the further development of archaeology in Serbia, so that medieval archaeology was treated as marginal and second-rate compared to others.&#x0D; The aim of this paper, therefore, is to contextualize Vasić’s approach through the methods used in the history of archaeology. The key research question thereof is how Miloje M. Vasić failed to document the burials at the Vinča site, which is the consequent reason why there is little to no documented evidence of them.&#x0D; The theoretical and methodological basis of the analysis is based on the approach of Gavin Lucas who views the creation of the primary field documentation as testimony. Lucas notes that the debate concerning knowledge production had drifted from merely an epistemological issue to a phenomenon centered around archaeological practice. Here the key questions have come to concern the social and material setting of knowledge production and not the objective coherence of the argument.&#x0D; Burials that were noted in Vasić’s documentation are categorized into four groups: 1) unwanted or medieval burials; 2) incidental burials originating from prehistory 3) an “ossuary” from Vinča containing nine skeletons and 4) imagined multiple cremations based on one found cremation. Therefore, even while documenting several “lateral” prehistoric graves, he entirely omitted any thorough documentation of the medieval cemetery, considering them of less import.&#x0D; If there is any lesson that may be learned from this journey through the history of archaeological practice, it is that archaeological documentation as a form of testimony should be done ethically, adequately and responsibly. It should not be done according to the practices of the “bad science” of its founding-fathers.

“The early days” – underwater prehistoric archaeology in the USA and Canada

Here, we present a historical review of important published studies of submerged prehistoric sites in North America prior to 1990. Prior to that point, a review of mid-twentieth century literature on the subdiscipline demonstrates that “prehistoric” was not a significant element in practice. In the U.S.A. and Canada, very few professional papers or articles were published on the topic of submerged prehistoric archaeological sites until mid-century or later. Most early studies were written by avocational archaeologists or specialists from other disciplines interested in archaeology. This changed in the 1970s, when formal surveys, reports, and publications written by academically trained archaeologists increasingly appeared in peer-reviewed journals and edited volumes. By the 1980s the establishment of underwater prehistoric archaeology as new sub-discipline was well underway. This review is designed to give the reader a brief overview of the discipline as it matured, though we lack the space to provide a full critical analysis here.

First archaeointensity results from Ecuador with rock magnetic analyses and 14C dates to constrain the geomagnetic field evolution in South America: Enhancing the knowledge of geomagnetic field intensity

Archaeomagnetic records from low-latitude sites are very scarce. Thus, the information about the geomagnetic field evolution in South America or Ecuador is sparse and more data are needed to constrain the field evolution in South America. In this study we present new absolute archaeointensity results from a set of 14C well-dated (i.e. calibrated ages) prehistoric archaeological sites in northern Ecuador (South America). Potsherd fragments were sampled during archaeological excavations of 2 earthen mounds in the vicinity of Atuntaqui and Otavalo cities, and pits at La Chimba site. The pottery covers 2 distinct archaeological periods defined as 1) Ecuadorian Formative period (700 BC – 1AD) and 2) the prehistoric Late period (1250–1505/1525 AD). Successful archaeointensity determinations were obtained from 56 sherds using the Thellier-Coe protocol and their rock magnetic properties.The absolute palaeointensity determinations have yielded AI values of 43.6 ± 1.3 μT for Atuntaqui, 34.2 ± 1.4 μT for the Otavalo Mound 3 (lower charcoal lens), 39.5 ± 1.4 μT for Otavalo Mound 3 (upper charcoal lens) and a range of absolute archaeointensities from 7.0 ± 0.97 μT up to 42.2 ± 2.06 μT, with a mean average of 21.20 ± 1.15 μT for La Chimba. Archaeointensity (AI) determinations of the successful mean abolute archaeointensity for the early phase (700–440BC) excavation levels 27.8 ± 1.315 μT, middle levels phase (440–40BC), 15.07 ± 0.78 μT and the late levels phase (44BC-250AD) 25.52 ± 1.575 μT. These results are in good correlation with the data from Palpa in South Peru as well as a few data results from Colombia, South America.

Distinguishing the taphonomic signature of wolves from humans and other predators on small prey assemblages

The study of human subsistence strategies in prehistoric hunter-gatherer communities is essential to understanding the evolution of human behaviour. An important topic of interest is the expansion of dietary breadth, resulting in the procurement of a larger number of small game species. However, to make accurate interpretations of human subsistence, the correct identification of the agents responsible for archaeofaunal assemblages is crucial, and actualistic studies that establish the taphonomic signature of the different predators are indispensable. Despite being one of the most ubiquitous carnivores in prehistoric archaeological sites, the role of wolves (Canis lupus) as agents responsible for small-prey accumulations has never been examined. The aims of this study are to analyse the taphonomic patterns left by wolves on rabbit remains and to put forward a series of criteria that can help distinguish assemblages produced by this carnivore from those accumulated by people or by other predators. Our results reveal that wolves ingest and consume the whole rabbit carcass, with the consequence that all rabbit remains accumulated by wolves come from the scats. The referential framework provided in this study will make it possible to discriminate wolves as agents of fossil rabbit accumulations.

Identification of woodland management by analysis of roundwood age and diameter: Neolithic case studies

It is often presumed that woodland management, i.e. pollarding and coppicing, was practised in prehistory, but the precise beginning and the details of such practices in the past are unknown. This is because, in contrast to historical times, from which written and iconographic sources are available, prehistoric archaeological sites rarely yield direct evidence of intentional woodland management. Since it is regularly suggested that people practised woodland management at least from the Neolithic onwards, this study brings together data for wood assemblages from six Neolithic sites in Denmark, the Netherlands, Slovenia and Spain, with the aim of investigating whether these provide evidence of woodland management. The method applied here is roundwood age and diameter analysis, based on an earlier developed model that has been tested on modern trees. None of the investigated European Neolithic sites provides evidence of woodland management. Various possible explanations for this outcome are discussed.