Taphonomic study in Argentinian Patagonia: analysis of variability through time and space in the Central Plateau (Santa Cruz Province)

The basin of the Zanjón Rojo and Blanco is located in the northeast of the Central Plateau of Santa Cruz province (Argentina). Each sector of the basin has specific characteristics which represent different microenvironments. We have studied two different archeological contexts in the period from the Final Pleistocene to Late Holocene in each of these sectors. In this paper, we analyze the effects of different taphonomic processes and agents on the zooarcheological assemblages in order to evaluate the role played by those that can redeposit or move bones pre- and post-depositionally during site formation in this sector of Patagonia. The bone specimens that were analyzed come from two stratigraphic contexts with wide sequences of human occupation; one is AEP-1 at Piedra Museo and the other is Cueva Maripe at La Primavera, located in the lower and upper sectors of the basin, respectively. The comparison between both sites was based on different modification patterns identified on bone surfaces for the different phases of settlement in Patagonia. The results showed complex and different taphonomic histories in both sites, and while the main processes involved in bone movement were roots and rodents, both had little significance in comparison with others, such as manganese and carbonate.     

Terrestrial and maritime taphonomy: differential effects on spatial distribution of a Late Pleistocene continental drowned faunal bone assemblage from the Pacific coast of Chile

Site GNL Quintero 1 (GNLQ1), located on the central coast of Chile, is the only documented Late Pleistocene drowned terrestrial site along the Pacific Coast of South America. Faunal evidence at the site is varied, and so far, remains of the following taxa have been found: extinct Camelidae, Cervidae, Equidae, Mylodontidae, Xenarthra, but also Myocastoridae, Canidae and Octodontidae. Both geological and paleoenvironmental data indicate that GNLQ1 developed in a floodplain or low-energy environment during the Last Glacial Maximum (LGM). Prior to the post-glacial rising of the sea level, the site would have been located several kilometres inland as the paleoshoreline was farther out on the continental shelf. In accordance with this background, the present study addresses the analysis of the spatial distribution of the bone deposits of GNLQ1 by considering both scenarios, the terrestrial phase related to the formation and modification of the fossil assemblage prior to the transgression, and the marine phase, subsequent to inundation. Results indicate modifications related to low-energy flow environment and carnivore activity dominated during the terrestrial phase and the action of marine organisms during the marine phase. Other taphonomic modifications are not easily attributable to either one or the other environmental context.     

Miliacin in palaeosols from an Early Iron Age in Ukraine reveal in situ cultivation of broomcorn millet

During the archaeobotanical investigation of Scythian–Sarmatian period (Early Iron Age), pits with crop processing waste, discovered in the floodplain of Donets River, eastern Ukraine, and charred remains of cereal grains, dominated by broomcorn millet, were recorded. The grains from the pits were radiocarbon dated to the fifth to first century BC. Those pits are distant from any known contemporaneous settlement. The apparent disconnection of these pits from any local settlement suggests that (1) millet was brought from other locations by mobile groups, or (2) millet was cultivated locally by populations whose settlements have left no discernible archaeological trace. The analysis of molecular biomarkers preserved in palaeosols that are stratigraphically connected to the pits revealed high levels of miliacin, a molecule that can be preserved in ancient soils and sediments, and that is consistent with broomcorn millet (Panicum miliaceum). High levels in miliacin in soils stratigraphically connected to the pits are interpreted as the result of a large biomass of P. miliaceum produced at time of soil formation. Our biogeochemical results applied to a palaeosol thus attest to the in situ cultivation of crops dominated by the broomcorn millet during the early Iron Age in the floodplain of Donets River. Biochemical examination of soils and palaeosols can thus provide useful information on past dynamics of land-use by ancient population, especially when settlements or macrobotanical remains are absent.     

Local diversity in settlement,demography and subsistence across the southern Indian Neolithic-Iron Age transition: site growth and abandonment at Sanganakallu-Kupgal

The Southern Indian Neolithic-Iron Age transition demonstrates considerable regional variability in settlement location, density, and size. While researchers have shown that the region around the Tungabhadra and Krishna River basins displays significant subsistence and demographic continuity, and intensification, from the Neolithic into the Iron Age ca. 1200 cal. BC, archaeological and chronometric records in the Sanganakallu region point to hilltop village expansion during the Late Neolithic and ‘Megalithic’ transition period (ca. 1400–1200 cal. BC) prior to apparent abandonment ca. 1200 cal. BC, with little evidence for the introduction of iron technology into the region. We suggest that the difference in these settlement histories is a result of differential access to stable water resources during a period of weakening and fluctuating monsoon across a generally arid landscape. Here, we describe well-dated, integrated chronological, archaeobotanical, archaeozoological and archaeological survey datasets from the Sanganakallu-Kupgal site complex that together demonstrate an intensification of settlement, subsistence and craft production on local hilltops prior to almost complete abandonment ca. 1200 cal. BC. Although the southern Deccan region as a whole may have witnessed demographic increase, as well as subsistence and cultural continuity, at this time, this broader pattern of continuity and resilience is punctuated by local examples of abandonment and mobility driven by an increasing practical and political concern with water.     

Finding millet in the Roman world

Examining the evidence for millet in the Roman empire, during the period, circa 753 bc–610 ad, presents a number of challenges: a handful of scant mentions in the ancient surviving agrarian texts, only a few fortuitous preserved archaeological finds and limited archaeobotanical and isotopic evidence. Ancient agrarian texts note millet’s ecological preferences and multiple uses. Recent archaeobotanical and isotopic evidence has shown that millet was being used throughout the Roman period. The compiled data suggests that millet consumption was a more complex issue than the ancient sources alone would lead one to believe. Using the recent archaeobotanical study of Insula VI.I from the city of Pompeii, as a case study, the status and role of millet in the Roman world is examined and placed within its economic, cultural and social background across time and space in the Roman world.     

Clay Tobacco Pipes from a Colonial Refuse Deposit in Fort San Severino,Matanzas Province,Cuba

This article provides a detailed study of clay tobacco pipes excavated from a refuse deposit at Fort San Severino, Matanzas city, Cuba. The pipes date to the late eighteenth through the nineteenth century and are dominated by reed-stem typology. The collection includes Dutch, British, Spanish, and Balkan specimens. The study of these pipes contribute to the archaeology of clay pipes in Cuba and provide insight into the socioeconomics of pipe culture at fort San Severino. Moreover, it brings special attention to the occurrence of western Mediterranean reed-stem tobacco pipes, yet to be studied from other Spanish sites in the Caribbean.     

A Place for Convicts: The Fremantle Lunatic Asylum,Western Australia and John Conolly’s “Ideal” Asylum

This article considers the mid to late nineteenth-century world of the Fremantle Lunatic Asylum, Western Australia. By examining the built environment of the asylum and the uses of spaces within its walls, it is possible to understand not just the experiences of the inmates, but to highlight attitudes towards the insane. The asylum was built under authority of the British Government, and later transferred to the Western Australian Government’s care. Reflecting on this volume’s theme of colonial institutions, this article will highlight the effects of center and periphery relationships on life within the asylum.     

A Landscape of Assimilation and Resistance: The Mount Pleasant Indian Industrial Boarding School

In the late nineteenth century the United States Federal government established off-reservation boarding schools that sought to accomplish an internal colonialism of American Indian communities by forcefully assimilating them into mainstream American culture. The landscape of these institutions was a primary tool to achieve their assimilationist goals. This research examines the Mount Pleasant Indian Industrial Boarding School through archival, archaeological and oral history evidence. The landscape and material record of this school also indicate that students vigorously resisted the institution.     

Classifications of Sacred Space: A New Understanding of Mass Rock Sites in Ireland

As locations of a distinctively Catholic faith, Mass Rocks are important historical, ritual and counter-cultural sites that present a tangible connection to Ireland’s rich heritage for contemporary society. Recent authors have begun to fill a gap in published literature yet few go beyond traditional assumptions. This paper offers a more contemporary approach to the study of Mass Rocks based on extensive field research in county Cork. It argues for the introduction of new and innovative classifications that expand the accepted archaeological definition and proposes a set of criteria for the more robust verification of potential sites.