Search

The paper presents new research on an assemblage of metallurgical crucibles used in the assay of minerals at colonial Jamestown. The aim of the study is to explore the range of chemical operations carried out at the site of the first permanent British settlement in America, for which little is known in the documents. The results show that the colonists used high-quality Hessian crucibles to perform tests on different types of complex polymetallic sulphides. This was done to (1) prospect for potential silver and copper ores and (2) to find suitable sources of zinc and tin to be alloyed into brass and bronze through cementation with imported copper offcuts. This study makes a relevant contribution to the growing field of the archaeology of early chemistry and mineral prospection as well as the archaeology of early European colonies in the New World. In particular, material culture can shed fresh light on how European settlers reacted to the many challenges of a new and unfamiliar natural environment and how they tried to make sense and exploit it for financial profit. [ABSTRACT FROM AUTHOR]

The Middle-to-Upper Paleolithic transition in Europe covers the last millennia of Neanderthal life together with the appearance and expansion of Modern Human populations. Culturally, it is defined by the Late Middle Paleolithic succession, and by Early Upper Paleolithic complexes like the Châtelperronian (southwestern Europe), the Protoaurignacian, and the Early Aurignacian. Up to now, the southern boundary for the transition has been established as being situated between France and Iberia, in the Cantabrian façade and Pyrenees. According to this, the central and southern territories of Iberia are claimed to have been the refuge of the last Neanderthals for some additional millennia after they were replaced by anatomically Modern Humans on the rest of the continent. In this paper, we present the Middle-to-Upper Paleolithic transition sequence from Cova Foradada (Tarragona), a cave on the Catalan Mediterranean coastline. Archaeological research has documented a stratigraphic sequence containing a succession of very short-term occupations pertaining to the Châtelperronian, Early Aurignacian, and Gravettian. Cova Foradada therefore represents the southernmost Châtelperronian–Early Aurignacian sequence ever documented in Europe, significantly enlarging the territorial distribution of both cultures and providing an important geographical and chronological reference for understanding Neanderthal disappearance and the complete expansion of anatomically Modern Humans. [ABSTRACT FROM AUTHOR]

The preservation of palaeoenvironmental and archeological records in cave and rock shelter contexts is often called into question for Pleistocene sequences. Records are always fragmentary and the preservation of sediments and archaeological remains is partial and differential, according to site history. The karst deposits are often frequently described as disturbed due to post-depositional processes and phases of erosion over time. However, taphonomical analyses and some very well-preserved evidence attest to the capacity of caves to record data. Systematic and interdisciplinary fieldwork and studies allow for the reconstruction of some characteristics of Neanderthal occupations in their biostratigraphical and geochronological context. The geographic area under consideration here is the Rhône Valley. The right bank of the Middle Rhône Valley has yielded more than ten Middle Palaeolithic sites. Some of them have been studied recently through interdisciplinary fieldwork, providing new data on the end of the Middle Pleistocene and the beginning of the Upper Pleistocene. For this paper, we focus on four sites dated from the end of MIS 5, MIS 4 and the beginning of MIS 3, containing layers with evidence of Neanderthal occupations: Saint-Marcel, Abri du Maras, Abri des Pêcheurs and Le Figuier. All these sites are rock shelters or cave chambers and porches belonging to a karst system. The aim of our research program is to provide as much data as possible on Neanderthal occupations in their environmental contexts, in order to describe subsistence strategies and land use throughout time and potential links with climatic changes. In this paper, we evaluate the feasibility of assessing the relationship between climatic change and behaviour during the Middle Palaeolithic by describing the main archaeological material and palaeoenvironmental records of these four sites. Then, in the discussion, we conjointly examine the data from each site to assess this key question, even though the low resolution of cave and rock shelter records makes it difficult to establish an accurate chronology for human occupations and to provide a detailed description of the environment around the site for each human occupation. [ABSTRACT FROM AUTHOR]

Abstract: Amino acid racemization, used as a method of relative and quantitative dating of fossils, evaluates the degree of postmortem conversion of l to d amino acid enantiomers. While extensively utilized, this method has garnered confusion due to controversial age estimates for human fossils in North America in the 1970s. This paper explains the age controversy and aftermath, current chromatographic methods used in research, mathematical calibration models, and a short synopsis of other dating techniques in geochronology and archaeometry. [ABSTRACT FROM AUTHOR]

This paper focuses on the technological characteristics of Keilmesser with a lateral tranchet blow modification on the cutting edge. It examines the underlying technological production of these bifacial objects: this implies the evaluation of their working stage succession, as well as produced forms necessary for the execution of tranchet blow performance. Furthermore, it offers a techno-morphological description of these enigmatic tools. The Keilmesser with tranchet blow and corresponding blanks of tranchet blows from Grotte de la Verpillière I in Germolles (Saône-et-Loire, France) are used as case study. The collection of Keilmesser with tranchet blow and corresponding blanks of tranchet blow has been massively expanded with new fieldwork and the review of ancient assemblages. The majority of the pieces were made on blanks from local raw material. The evaluation of the underlying production concept shows that a Keilmesser with tranchet blow, regardless of the wide range of morphologies and matrix size, always consists of specific parts that are necessary for the production sequence and the assumed function. The production of these pieces follows highly specific working stages, some of which can be interchanged in sequence. However, it is always the goal to obtain a low-angled cutting edge. The performance of a tranchet blow is not only an integral part of production, but it is rather the aim of the entire production. [ABSTRACT FROM AUTHOR]

The Southern Montane Forest-Grassland mosaic ecosystem in the humid subtropics southern Rift Valley of Africa comprised the environmental context for a large area in which modern human evolution and dispersal occurred. Variable climatic conditions during the Late Pleistocene have ranged between humid and hyperarid, changing the character of the ecosystem and transforming it at different points in time into a barrier, a refuge, and a corridor between southern and eastern African populations. Alluvial fans presently blanket the areas adjacent to major river systems, which were key areas of prehistoric human habitation. These sets of variables have created conditions that are both challenging and advantageous to conduct archaeological research. Lateritic soil development has resulted in poor organic preservation and facilitated insect bioturbation, which has demanded an integrated micro-macro scale approach to building a reliable geochronology. An integrated field and analytical methodology has also been employed to identify the nature and degree of post-depositional movement in alluvial deposits, which preserve a wide range of spatial integrity levels in buried stone artifact assemblages between 47 and 30 ka in Karonga, northern Malawi. This paper describes the methodological advances taken toward understanding open-air Middle Stone Age archaeology in sub-tropical Africa, and explores the inferential potential for understanding Pleistocene human ecology in the important southern Rift Valley region. [ABSTRACT FROM AUTHOR]

Archaeological radiocarbon databases are being increasingly used as a proxy of past demographic trends. In this paper we compile and analyze an extensive database of paleoecological information and 14 C dates from archaeological sites in northwestern Patagonia (Argentina, South America). On this basis, we assess the regional distribution of human populations since the late Pleistocene, and their relation with the evolution of Patagonian climate and landscapes. We explore the spatial and temporal distribution of evidence and discuss sampling biases affecting the record in different ecological contexts. The analysis is set in the frame of three main ecological regions that have implications for human subsistence: Andean forest, grass steppe, and shrub steppe. The intensity of the archaeological signal differs among these regions through time, being stronger and more homogeneous in the grass steppe. In the Andean forest and the shrub steppe the signal is weaker and even absent during short periods of the middle Holocene. We suggest likely sampling biases contributing to these tendencies, since these three regions present variable research cover and intensity. On the other hand, we also suggest that these differences may reflect variations in the intensity of human occupation, in favor of more attractive environments for hunting (i.e., areas where guanaco are generally more abundant). This macro-regional synthesis of the paleoecology and archaeology of northwestern Patagonia provides a platform for developing future oriented research. [ABSTRACT FROM AUTHOR]