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Publication date: July 2016Source:Journal of Archaeological Science, Volume 71 Author(s): Thomas S. DyeThe tempo plot, a statistical graphic designed for the archaeological study of rhythms of the long term that embodies a theory of archaeological evidence for the occurrence of events, is introduced. The graphic summarizes the tempo of change in the occurrence of archaeological events using the model states generated by the Markov Chain Monte Carlo routine at the heart of Bayesian calibration software. Tempo plots are applied to the archaeological record of Hawai‘i to expose rhythms of i) tradition in taro pond-field construction, ii) innovation in temple construction, and iii) fashion in the harvest of branch coral for use as a religious offering. Rhythms of the long term identify a hitherto unrecognized transformation of religious practice in Hawai‘i, establish temporal coincidence in temple construction in leeward sections of Maui and Hawai‘i Islands previously described as regionally idiosyncratic, suggest shallow temporal limits to the use of the direct historical approach in Hawai‘i, and disclose processes at work in the political economy recorded at the time of western Contact.

Publication date: August 2016Source:Journal of Archaeological Science, Volume 72 Author(s): Daniel García Rivero, Jesús María Jurado Núñez, Ruth TaylorThis paper addresses the plain common pottery associated with Beaker contexts in the Southwest of the Iberian Peninsula. The detailed systematic study focuses on the pottery assemblage provided by one of the region’s most important settlements, San Blas (Badajoz, Spain), while comparisons are made with other important sites in the study area. By means of the stratigraphic, typological and statistical analysis of the data, the main patterns of change in this material culture throughout the temporal sequence are identified and the historical explanatory factors are inferred. Specifically, during the second half of the 3rd millennium cal BC, an important change took place in the management of economic risk, which is materialised by a significant reduction in food storage and by the more immediate direct or indirect consumption of resources. We suggest that these patterns reflect a shift towards a short-term projection of the future, in a context with strong evidence of instability.

Publication date: Available online 22 July 2016Source:Journal of Archaeological Science Author(s): Tim Denham, Elle GronoKuk Swamp is a globally significant archaeological site of early agriculture in the highlands of Papua New Guinea. Mixed-method and multi-scalar investigations of the stratigraphy and selected feature fills at Kuk were instrumental in determining the character of plant exploitation and agricultural practices there during the early and mid Holocene. In this paper, macro-scale (field recording), meso-scale (X-radiography) and micro-scale (thin section micromorphology) analyses are presented in summary form for a stratigraphic column, as well as for a palaeochannel and palaeosurfaces associated with plant exploitation at c.10,000 cal BP and cultivation at 7000–6400 cal BP. Major and minor stratigraphic units have been characterised, primary and secondary formation processes differentiated, and the anthropic associations of specific stratigraphic units determined, especially in regards to cultivation. The Kuk research highlights several methodological problems with the investigation of early cultivation on allophane-rich soils in tropical environments.

Publication date: August 2016Source:Journal of Archaeological Science, Volume 72 Author(s): Benjamin S. Arbuckle, Max D. Price, Hitomi Hongo, Banu ÖksüzIn this paper we address the timing of and mechanisms for the appearance of domestic cattle in the Eastern Fertile Crescent (EFC) region of SW Asia through the analysis of new and previously published species abundance and biometric data from 86 archaeofaunal assemblages. We find that Bos exploitation was a minor component of animal economies in the EFC in the late Pleistocene and early Holocene but increased dramatically in the sixth millennium BC. Moreover, biometric data indicate that small-sized Bos, likely representing domesticates, appear suddenly in the region without any transitional forms in the early to mid sixth millennium BC. This suggests that domestic cattle were imported into the EFC, possibly associated with the spread of the Halaf archaeological culture, several millennia after they first appear in the neighboring northern Levant.

Publication date: June 2016Source:Journal of Archaeological Science, Volume 70 Author(s): M. Willmes, L. Kinsley, M.-H. Moncel, R.A. Armstrong, M. Aubert, S. Eggins, R. GrünStrontium isotope ratios measured in fossil human teeth are a powerful tool to investigate past mobility patterns. In order to apply this method, the sample needs to be investigated for possible diagenetic alteration and a least destructive analytical technique needs to be employed for the isotopic analysis. We tested the useability of U, Th, and Zn distribution maps to identify zones of diagenetic overprint in human teeth. Areas with elevated U concentrations in enamel were directly associated with diagenetic alterations in the Sr isotopic composition. Once suitable domains within the tooth are identified, strontium isotope ratios can be determined either with micro-drilling followed by TIMS analysis or in situ LA-MC-ICP-MS. Obtaining accurate 87Sr/86Sr isotope ratios from LA-MC-ICP-MS is complicated by the potential occurrence of a significant direct interference on mass 87 from a polyatomic compound. We found that this polyatomic compound is present in our analytical setup but is Ar rather than Ca based, as was previously suggested. The effect of this interference can be significantly reduced by tuning the instrument for reduced oxide levels. We applied this improved analytical protocol to a range of human and animal teeth and compared the results with micro-drilling strontium isotopic analysis using TIMS. Tuning for reduced oxide levels allowed the measurement of accurate strontium isotope ratios from human and animal tooth enamel and dentine, even at low Sr concentrations. The average offset between laser ablation and solution analysis using the improved analytical protocol is 38 ± 394 ppm (n = 21, 2σ). LA-MC-ICP-MS thus provides a powerful alternative to micro-drilling TIMS for the analysis of fossil human teeth. This method can be used to untangle diagenetic overprint from the intra-tooth isotopic variability, which results from genuine changes in 87Sr/86Sr isotope ratios related to changes in food source, and by extension mobility.

Publication date: June 2016Source:Journal of Archaeological Science, Volume 70 Author(s): Francesco d’Errico, Laure Dayet Bouillot, Marcos García-Diez, Africa Pitarch Martí, Daniel Garrido Pimentel, João ZilhãoThe red disks from El Castillo Cave are among the earliest known cave paintings. Here, we combine the morphometric and technological study of red disks from two areas located at the end of the cave with the microscopic, elemental, and mineralogical analysis of the pigment and compare the results obtained with observations derived from experimental replication. Ergonomic constraints imply that a number of disks were made by adults, and the differences in pigment texture and composition suggest that they correspond to an accumulation through time of panels made by different persons who shared neither the same technical know-how nor, very possibly, the same symbolic system.

Publication date: September 2016Source:Journal of Archaeological Science, Volume 73 Author(s): Rowin J. van Lanen, Esther Jansma, Jan van Doesburg, Bert J. GroenewoudtTo what extent long-distance transport in north-western Europe changed after the Roman period is generally unknown. Few historical sources are available and existing archaeological records are unclear and sometimes conflicting. Traditionally, research on the long-distance exchange of goods mostly has focussed on the spatial analyses of luxery goods such as jewellery, weapons and religious artefacts. Relatively little attention has been paid to the spatial modelling of common exchange networks and transport routes.In this study we used a dendroarchaeological approach to model long-distance transport of oak (a common good) to the Roman and early-medieval Netherlands. By combining established and newly-derived provenances of imported timbers with data on Roman and early-medieval route networks, we were able to reconstruct: (a) Roman and early-medieval exchange networks of imported timbers, (b) changing transport routes and (c) spatially shifting frequent-travel zones. The findings were compared with distribution patterns of other commodities for daily use: pottery and stone household goods.Results show that in the early and middle-Roman periods (12 BCE – CE 270) timbers were imported from the German Rhineland, the Ardennes and the Scheldt region. We have no evidence for wood import to the current Netherlands during the late-Roman period and first phase of the Early Middle Ages (CE 270–525). In the following centuries, between CE 525–900, oak again was brought to the current Netherlands, this time exclusively originating from the German Rhineland. This pattern significantly changed during the last phase of the Early Middle Ages (CE 900–1050) when timbers were derived from the Ardennes only. We used these patterns to calculate changes in long-distance transport routes and frequent-travel zones in the research area. Through our analyses existing data on Roman and early-medieval route networks could be expanded and improved. The calculated wood-transport patterns agree well with the distribution of imported pottery and (other) household goods in these periods.

Publication date: June 2016Source:Journal of Archaeological Science, Volume 70 Author(s): M. Benvenuti, A. Orlando, D. Borrini, L. Chiarantini, P. Costagliola, C. Mazzotta, V. RimondiIron deposits from Elba Island (Tuscan Archipelago) were extensively exploited since the 1st millennium BC: both raw iron ore and smelted blooms were extensively traded through the Mediterranean region. Within the frame of the multidisciplinary research Project “AITHALE” (from the Greek name for Elba Island), we have performed a series of archaeometallurgical experiments primarily to investigate the traceability of Elban iron ores during the various steps of the chaîne opératoire of bloomery iron production. Results of experiments performed both in the field (reconstruction of a bloomery furnace) and in the laboratory (smelting experiments carried out in a gas mixing furnace) are discussed in the text. Slags produced by smelting of W-Sn-rich iron (hematite) ores, like those from Elba island, show the presence of these elements in phases of their own, either relic (scheelite, ferberite, cassiterite) and/or newly formed (iron-tin alloys). Iron bloom obtained from this kind of iron ore could also bear evidence of the peculiar geochemistry of smelted ore, with tungsten preferentially associated with slag inclusions and tin eventually enriched in the metallic phase.

Publication date: September 2016Source:Journal of Archaeological Science, Volume 73 Author(s): F. Pagliaro, F. Nardecchia, F. Gugliermetti, F. BisegnaThe indoor microclimate of ancient storage buildings has been widely investigated since they could reach optimal conditions for goods preservation only through passive systems. However it is difficult to fully understand the real behaviour of these systems since they are often not existing anymore nowadays: this is the case of the warehouses of Portus, an archaeological site originally composed of about 300 storage-rooms. A significant amount of important information, like the one related to shape and structure, are not available for the archaeologists who investigate the site. A detailed analysis of these buildings has been carried out in order to assess the optimal indoor microclimate for wheat storage. Different hypotheses focusing on the presence of openings have been developed, even if the archaeologists suppose that the rooms were completely closed. The combination of numerical tools and historical research allowed to formulate, test and validate a hypothesis regarding the architecture and the operation of these ancient buildings. In the present paper, conjugated heat transfer in different configurations of the warehouses of Portus has been numerically studied, taking into account the models subjected to different transient temperatures as a consequence of the summer outdoor microclimate. This work aims to propose and validate archaeological and structural hypotheses regarding the functioning of storage-rooms in Ancient Rome, through an improved and optimized definition of the reconstruction of one of the warehouses of Portus.

Publication date: Available online 17 June 2016Source:Journal of Archaeological Science Author(s): Richard I. Macphail, Elizabeth Graham, John Crowther, Simon TurnerMarco Gonzalez, on the south-west end of the island of Ambergris Caye, Belize, has well-preserved Maya archaeological stratigraphy dating from Preclassic times (ca. 300 B.C.) to the Late Classic period (ca. A.D. 550/600 to 700/760). Although later occupations are recorded by house platforms and inhumations (Terminal Classic to Early Postclassic), and use of the site continued until the 16th century A.D., intact stratigraphy is rare in these cases owing to a greater degree of disturbance. Nonetheless, understanding site formation entails accounting for all processes, including disturbance. The site’s depositional sequence—as revealed through soil micromorphology and chemistry and detailed here—has yielded critical information in two spheres of research. As regards archaeology and the elucidation of Maya activities on the caye over time, soil micromorphology has contributed beyond measure to what we have been able to distinguish as material remains of cultural activity. Detailed descriptions of the nature of the material remains has in turn helped us to clarify or alter interpretations based on artefacts that have been identified or sediments characterised according to traditional recovery techniques. The other major sphere in which soil micromorphology and chemistry play a critical role is in assessment of the environmental impact of human activity, which enables us to construct and test hypotheses concerning how the site formed over time; what materials and elements contributed to the character of the sediments, especially in the formation of a specific Maya Dark Earth type that is developed from carbonate rich deposits; and how the modern surface soils acquired the appearance of a Dark Earth, but essentially differ from them. In terms of agricultural soil sustainability, the Marco Gonzalez surface soil is neo-formed by a woodland vegetation drawing upon the nutrients and constituents present in both the Dark Earth and underlying better preserved stratified deposits.