Returning to the Kamp Mound Group (11C12): Results from Geomagnetic Survey and High-Density Topographic Mapping in Calhoun County,Illinois

This article addresses the use of high-density topographic mapping and geomagnetic fieldwork as part of an ongoing research program focused on evaluating the role of monumental architecture in the construction and maintenance of differing scales of community during Middle (ca. 50 cal B.C.–cal A.D. 400) and Late (ca. cal A.D. 400–1000) Woodland periods in the Lower Illinois River Valley. At the 2013 Center for American Archeology and Arizona State University field school, a 2.46-ha area at the Kamp Mound Group (11C12) containing Mounds 1, 6, 7, 8, and 9 was surveyed using magnetic fluxgate gradiometry and mapped using a high-density robotic total station. Our survey results demonstrate that highly disturbed mounds have significant interpretable structure that can be used as primary data to better understand spatial attributes related to evaluating site organization, distribution of activity areas in nonmounded space, and internal mound structure and composition.     

Open-area excavations at the Mitchell Prehistoric Indian Village,South Dakota (A.D. 1000–1150): New interpretations of site function from interdwelling areas

Abstract

Excavations at the Mitchell Prehistoric Indian Village (A.D. 1000–1150), an Initial Middle Missouri period Plains earthen lodge village site in eastern South Dakota, revealed new data regarding the lifeways and cultural systems of its prehistoric inhabitants. While extensive excavations had been conducted at the site and at a large number of other Middle Missouri sites prior to the present project, our open-area approach revealed new and significantly different information. New features in the areas between the dwellings were uncovered, features that are rarely studied in the context of the Middle Missouri cultural tradition. Other finds included Mississippian-influenced ceramics, Avonlea projectile points, and ceremonial goods that indicate long-distance cultural interaction. The discovery of large, complex features in the interdwelling areas of the site changes our understanding of Middle Missouri lifeways and settlement structure.     

Palaeoecology and Archaeology of the Village of Uukuniemi,Eastern Finland

Abstract

In the present article, pollen analytical results from Lake Kirkkolampi are presented and compared with results provided by archaeological material. Pollen analysis is connected with the archaeological research project at Papinniemi in Uukuniemi. Papinniemi is one of the numerous Greek Orthodox settlements that existed in Karelia in the fourteenth to seventeenth centuries. Archaeological evidence of settlement preceding this period is very scarce, and in this respect Uukuniemi represents a typical area in eastern Finland. There is no archaeological evidence of permanent settlement in Uukuniemi from the Early Metal Period (c. 1800 bc–ad 400), the Middle Iron Age (c. ad 400–800) or from the Late Iron Age (c. ad 800–1300). Pollen analysis demonstrated the onset of cultivation c. cal ad 300. Marked intensification of agricultural activities and cultivation in permanent fields took place around cal ad 800. A shift in land-use practises, including a declining use of fire, is visible at cal ad 1520–1600. The discrepancy between archaeological and palaeoecological records raises several questions, and the problems of Early Metal Period and Iron Age populations, as well as settlement continuity, are discussed.     

Settlements and Seafaring: Reflections on the Integration of Boats and Settlements Among Marine Foragers in Early Mesolithic Norway and the Yámana of Tierra del Fuego

The abundant Early Mesolithic (11,500–10,000 cal. BP) settlements at the raised shorelines in Norway and Sweden represent the earliest documented marine foragers in northern Europe. In the Scandinavian seascapes, both traveling and subsistence depended on seaworthy vessels. However, this highly mobile lifestyle was likewise dependent on settlements on firm ground. Departing from actor-network theory and symmetrical archaeology, I explore the structural relations between extensive use of boats, basic co-residing units, and activity patterns at settlements. The empiric basis for my study is the excavated Early Mesolithic coastal sites in the Ormen Lange project in Central Norway, dated to ca. 11,000–10,800 cal. BP. I suggest that the structural uniformity that is observed in the settlements may be related to the dependency on boats for subsistence activities as well as transport and settlements, creating human-thing dynamics that interlocked co-residents and boat crews, logistics, and activity patterns. This dynamic regime is also explored with ethnohistorical and archaeological references to the Yámana in the Beagle Channel, Tierra del Fuego, Argentina.     

New evidence on the introduction,cultivation and processing of hemp (Cannabis sativa L.) in southern Sweden

Subfossil remains of Cannabis sativa L. (hemp) have been found at Lindängelund in the region of Malmö, southern Sweden. These represent the earliest robust evidence so far for hemp retting in Scandinavia. Finds of seeds, stems and pollen of C. sativa from a waterlogged context on a settlement dating to the Roman Iron Age demonstrate that the plant was locally cultivated and processed during the 1st–2nd centuries AD. An introductory phase in Scandinavia is proposed (c. AD 1–400) during which the cultivation of hemp was apparently small scale and processing was probably carried out within settlements. In the succeeding centuries, c. AD 400–550 (the Migration Period), remains of hemp are mostly found in pollen records from lake sediments, and less frequently in the archaeological record. This could indicate that the process of hemp retting relocated from settlements to lakes shores where activity became larger in scale and more integrated with the prevailing agricultural system.     

THE BILTMORE MOUND AND HOPEWELLIAN MOUND USE IN THE SOUTHERN APPALACHIANS

Abstract

Biltmore Mound, located on the Swannanoa River in Asheville, North Carolina, was constructed over a Connestee phase habitation, the earliest evidence dating to about A.D. 300. Mound construction began sometime between A.D. 400 and 550, with the second to last mound stage constructed about A.D. 580–600. Because of the diverse contexts and the excellent preservation of faunal remains, we are able to provide some insights into Connestee ritualism at Biltmore Mound. The Biltmore Mound was a platform used to support large public structures for ritual and ceremonial activities. It was constructed of varying colored and textured soils from a variety of source areas that arguably had symbolic importance. The mound was primarily built out (rather than up) with several mantles that may have comprised a complete ritual cycle of mound construction.     

CHRONOLOGY,SITE FORMATION,AND THE WOODLAND-MISSISSIPPIAN TRANSITION AT BAYSHORE HOMES,FLORIDA

Bayshore Homes (8PI41) is a large mound and midden complex on Florida’s west-central Gulf Coast that was investigated originally by William Sears in the 1950s. From 1999 to 2009, the authors conducted survey, test excavations, and soil coring to address questions regarding site formation, chronology, and cultural affiliation. Radiocarbon dates and ceramic analysis indicate two separate occupations during the Woodland and Mississippi periods, cal. A.D. 140–565 and cal. A.D. 890–1390 (2 sigma). The earlier occupation is associated with the Manasota archaeological culture, sand-tempered plain pottery, burials in midden deposits, and interments in a sand mound accompanied by Weeden Island–related mortuary ceramics. The later occupation is associated with Weeden Island–related decorated and Pinellas Plain ceramics in midden deposits and represents the transition from terminal Weeden Island to the Englewood phase of Early Safety Harbor. A large burial mound and a platform mound are associated with this period of site use. Our results also indicate that the unusual ceramic sequence identified by Sears in the site’s large shoreline shell midden is the result of redeposition, which occurred sometime after cal. A.D. 1220. Possible explanations for the redeposition event include monumental mound construction or the elevation of the midden ridge to serve as a foundation for structures to protect them from rising sea levels or storm surges.     

From mess to matrix and beyond: estimating the size of settlements in the Ptolemaic Fayum/Egypt

This article seeks to introduce a new methodological approach to estimate population size of settlements in the Graeco-Roman Fayum/Egypt (330 BC–400 AD). The aim is to represent and analyse the relationship of settlements and the facilities they provide. We suggest turning the information commonly contained in traditional site gazetteers into presence–absence matrices of selected facilities. We then use these facility matrices to estimate the size of ancient settlements through linear regression. The equation is initially tested on medieval settlements in Norwich and East Anglia (England) and later applied to a settlement-facility matrix for the Ptolemaic period (330–30 BC). The results from the medieval data show the validity of the approach with a complete data set. The circumstance that the Ptolemaic data is fragmented and incomplete naturally adds a small, but acceptable error to the estimates.     

Pollen analysis in the context of clearance cairns from boreal forests – a reflection of past cultivation and pastoral farming

The former agricultural use of two sites located in the boreal forest of eastern Norway is investigated through pollen analysis. A peat profile was taken from the vicinity in each of two clearance cairn fields where several cairns were analysed for pollen. The pollen samples from the peat profiles give an environmental context for the pollen samples from the clearance cairns, and this combination of samples assists in evaluating the management practices that were in place on the cairn fields during different time periods. In both study areas cultivation layers under the clearance cairns are dated to the Late Roman Iron Age (cal. AD 200–400), while the oldest clearance cairns are dated to the Migration period (cal. AD 400–570), and a second phase of clearance cairn establishment is dated to the Medieval period (cal. AD 1030–1537). Abandonment of the two cairn fields is dated to c. AD 1700. Pioneer trees were a feature on or around the clearance cairn fields during most of the Iron Age, whereas the cairn fields were more open in medieval times. The investigation suggests that cereal cultivation on the clearance cairn fields is difficult to detect in local peat deposits, and that caution is needed when interpreting lack of Cerealia pollen. Management practices on the cairn fields are discussed and a change in management practice is indicated in association with medieval intensification.     

Palaeogeographical reconstructions of Lake Maliq (Korça Basin,Albania) between 14,000 BP and 2000 BP

Since the early 1990s, excavations of a protohistoric lakeside settlement in the Korça basin carried out by a French–Albanian archaeological team have induced geomorphological and palynological studies about the sedimentary records of Lake Maliq. These studies allow us to distinguish a series of centennial-scale high and low lake level events between 4200 and 4000 cal BP (2899–2637 BC/2843–2416 BC) and 2600 cal BP (822–671 BC), probably due to large-scale climate changes (in the Mediterranean basin). In addition, the sediment sequence also gives evidence of a millennial-scale trend of lake level rise. It appears to be an interplay between lake level rises and falls against tectonic subsidence of the basin allowing accommodation space for sediment deposition.The variations of the lake's level and the lake's surface area influenced the development and the abandonment of the nearby lakeside settlements (like the tell of Sovjan). In order to prepare an archaeological survey around the now dried up lake, we made a 3D model of the Holocene deposit from the lake including these lake level results, geomorphological mapping, excavation data, numerous core logs, AMS ¹⁴C dating and SRTM DEM data. The GIS model allowed us to propose four palaeogeographical reconstructions of the extension of Lake Maliq: around 14,000 BP, during the Mesolithic (around 9000 BP – 8781–8542 BC), the Early/Middle Bronze Age transition (around 3800 BP – 2310–2042 BC) and the Iron Age (2600 BP – 822–671 BC). A map of the thickness of the sediments above potential archaeological layers is also proposed.     

Absolute chronology of fluvial events in the Upper Dnieper River system and its palaeogeographic implications

A set of 121 radiocarbon and OSL dates has been compiled from the Upper Dnieper River and tributary valleys, Western European Russia. Each date was attributed according to geomorphic/sedimentological events and classes of fluvial activity. Summed probability density functions for each class were used to establish phases of increasing and reducing fluvial activity. The oldest detected reduction of fluvial activity was probably due to glacial damming at LGM. Within the Holocene three palaeohydrological epochs of millennial-scale were found: (1) high activity at 12,000–8,000 cal BP marked by large river palaeochannels; (2) low activity at 8,000–3,000 cal BP marked by formation of zonal-type soils on -floodplains; short episodes of high floods occurred between 6,500—4,400 cal BP; (3) contrasting hydrological oscillations since 3,000 cal BP with periods of high floods between 3,000–2,300 (2,000) and 900–100 cal BP separated by long interval of low floods 2,300 (2,000)-900 cal BP when floodplains were not inundated — zonal-type soils were developing and permanent settlements existed on floodplains. In the last millennium, four centennial-scale intervals were found: high flooding intervals are mid-11–mid-15^th century and mid-17–mid-20^th century. Intervals of flood activity similar to the present-day were: mid-15–mid-17^th century and since mid-19^th century till present. In the context of palaeohydrological changes, discussed are selected palaeogeographic issues such as: position of the glacial boundary at LGM, role of changing amounts of river runoff in the Black Sea level changes, floodplain occupation by Early Medieval population.     

Hunter–Gatherer Cattle-Keepers of Early Neolithic El Adam Type from Nabta Playa: Latest Discoveries from Site E–06–1

Further Neolithic encampments and settlements have been explored by the Combined Prehistoric Expedition in the Nabta Playa Basin on the South–Western Desert border around 100 km west of the Nile Valley. The perfectly preserved stratigraphic setting of the new site, numerous hearths and traces of dwellings, rich cultural material including pottery, radiocarbon dates and presence of bone remains render site E–06–1 an exception on the map of settlements of El Adam communities.     

Geochemical Characterization of Lapita Pottery Via Inductively Coupled Plasma–mass Spectrometry (ICP–MS)

We have obtained high‐resolution elemental data on Lapita ceramics (3200–2700 cal year bp ) from Fiji, Tonga and New Ireland using chemistry‐based inductively coupled plasma–mass spectrometry (ICP–MS). These data show clear elemental distinctions between Lapita pottery manufactured in Fiji, Tonga and New Ireland, and demonstrate significant elemental variation in Fijian ceramics collected from settlements in close proximity to one another. Therefore, we anticipate that ICP–MS will become an effective technique for tracking the transfer of Lapita pottery within and between different island groups in Oceania.     

Mid- to late-Holocene vegetational and land-use change in the Hadrian's Wall region: a radiocarbon-dated pollen sequence from Crag Lough,Northumberland, England

Pollen, charcoal and sedimentological analyses of a radiocarbon-dated sediment sequence from Crag Lough, by Hadrian's Wall, northern England, are used to reconstruct vegetational and land-use change since ca. 3000 cal BC. Clearance of Quercus and Corylus avellana woodland began at ca. 2600 cal BC, followed by a substantial decline of Alnus glutinosa and spread of Calluna vulgaris at ca. 400 cal BC. Local cereal cultivation occurred sporadically from ca. 2200 cal BC, with a decline (perhaps associated with climatic deterioration) at ca. 900 cal BC, then an increase at ca. 600 cal BC. Secale cereale was grown in the area from approximately the first to fifth centuries AD, followed by a second phase from ca. AD 1250–1700, when it was accompanied by Cannabis sativa.The sequence is interpreted in the light of the archaeological record, particularly in relation to the impact of Roman military activity in the area. The most significant episodes of woodland clearance occurred in the late Neolithic/early Bronze Age period and then in the middle Iron Age, creating a patchwork of woodland, heather moorland, pasture and arable land by the Roman period. The main changes in the Roman period were a decline in the extent of Betula woodland and perhaps the local introduction of Secale cereale cultivation. Local land management practices involving fire seem to have been suspended in the Roman period, but resumed afterwards. The end of the Roman period may have been accompanied by a shift towards pastoral land-use and abandonment of less favourable agricultural land, but the effect was minor compared to that at other sites in the region. Later shifts in land use may relate to climate variability, as reconstructed from several mires in northern England.     

Multiproxy environmental archaeology of Neolithic settlements at Osłonki,Poland, 5500–4000 BC

Abstract

Archaeological research on Neolithic settlements (ca. 5500–4000 cal BC) at and near Os?onki, Poland, is complemented by palaeoenvironmental investigations in three basins with biogenic sediments adjacent to the archaeological sites. Research included sedimentology, palynology, malacology and cladoceran analysis. Complementary lines of evidence indicate that Linear Pottery pioneer farmers of the late 6th millennium BC caused minimal environmental impact, but intensive settlement and land use by the Brze?? Kujawski Group during the 5th millennium BC triggered pronounced human-induced effects on the local landscape. Of particular significance is the evidence for erosion and aeolian ablation of exposed soil in the vicinity of the Neolithic settlements, presumably reflecting widespread land clearance, agricultural activity and settlement construction.     

Histories of deposition: creating chronologies for the Late Bronze Age–Early Iron Age transition in Southern Britain

The Late Bronze Age–Early Iron Age midden sites of Southern Britain are amongst the richest archaeological sites in the country. The organic accumulations contain substantial quantities of animal bone, decorated ceramics, metalwork and other objects; the often deep stratigraphy allows for changes in material culture and depositional practices, food production and consumption, and shifts in social identities, to be traced through time. The well-stratified assemblages also provide useful materials for dating the deposits. This has been problematic, however, as the majority of samples produce unhelpfully broad calibrated radiocarbon dates, due to the effects of the earlier Iron Age plateau in the calibration curve, which spans c. 800–400 BC. Interpretation has relied on current understandings of the associated pottery and metalwork, which placed most midden sites somewhere between the tenth and the seventh/mid-sixth centuries cal BC (c. 1000–600/550 cal BC), but the end-date of these traditions is particularly uncertain. This article addresses this issue by presenting the results of a new dating programme for East Chisenbury in Wiltshire, southern England. Twenty-eight radiocarbon determinations were obtained and combined with the site stratigraphy in a Bayesian chronological model. The results have transformed the chronology of the site, with the end of the occupation sequence being pulled forward some one-hundred years, to the mid-to-late fifth century cal BC. These new chronologies have significant implications for our understanding of the Late Bronze Age–Early Iron Age transition and require a revision of the currently accepted chronology of post-Deverel Rimbury decorated wares in south-central England.     

Impulses of agro-pastoralism in the 4th and 3rd millennia BC on the south-western coastal rim of Norway

Abstract

A review of the available archaeological and palaeoecological evidence from the coastal heathlands of south-western Norway was compiled to reveal the processes of neolithisation proceeding from the Early Neolithic towards the generally accepted breakthrough in the Late Neolithic, 2500/2350 cal. BC. South-western Norway then became part of the Scandinavian, and thus the European, agricultural complex. Three phases of forest clearance are recorded — from 4000–3600 cal. BC, 2500–2200 cal. BC and 1900–1400 cal. BC. Deforestation was intentional and followed a regional pattern linked to the geology and topography of the land. In the first period (4000–2500 cal. BC), forage from broad-leaved trees was important, while cereal cultivation was scarcely recorded. Agro-Neolithic (here referring to agriculturally-related Neolithic) artefacts and eco-facts belonging to the Funnel Beaker and Battle Axe culture are rare, but pervasive. They must primarily be considered to be status indicators with a ritual function; the hunter-gatherer economy still dominated. The breakthrough in agro-pastoral production in the Late Neolithic was complex and the result of interactions between several variables, i.e. a) deforestation resulting from agriculture being practised for nearly 1500 years b) experience with small-scale agriculture through generations and c) intensified exchange systems with other South Scandinavian regions. From 2500/2350 cal. BC onwards, two distinct environmental courses are noticeable in all pollen diagrams from the study area, indicating expansion in pastoralism, either towards heath or towards grassland and permanent fields.     

Long-distance provenance for obsidian artifacts of Mesoamerica Preclassic and Early Classic periods found in the Los Naranjos Archaeological Park (Honduras)

Los Naranjos is one of the most important pre-Columbian human settlements of Honduras related to the south-easternmost border of the Mayan civilization. Although the archaeological site mostly spans from 850 BC to 1250 AD, the present obsidian study was only focused on the Preclassic and Early Classic periods (Jaral, 800–400 BC and Edén, 400 BC–550 AD) where undamaged blades and/or retouched obsidian flakes are rare. In this way, the INAA analyses of 17 obsidian samples, compared with major-trace elements data of Honduran and Guatemalan obsidian sources, are mostly representative of waste flakes. Lithic artifacts of Los Naranjos such as sandstones, basalts, and quartzites come from local geological outcrops; whereas, obsidian provenance has to be searched from sources which are located within a radius up to 300 km far away. San Luis, La Esperanza, and Güinope obsidian sources are located in Honduras while the three most exploited Highland Guatemalan obsidian outcrops, which have been dominating long-distance trade in the Maya area mostly for the Classic-Postclassic periods, are San Martin de Jilotepeque, El Chayal, and Ixtepeque. An Ixtepeque provenance, for all the investigated obsidian samples of Preclassic and Early Classic periods found in the Los Naranjos Archaeological Park, was established, thus emphasizing a long-distance source (180 km). This also confirms that Ixtepeque represents the most important provenance of the obsidian artifacts found in archaeological sites of Western and Central-Western Honduras. The possible role played by some of the most important rivers of Guatemala and Honduras as waterway networks of transport was finally pointed out. New INAA chemical data from the Honduran obsidian source of La Esperanza (“Los Hoyos”, 4 samples) are also reported in this paper.     

Dating of 4th millennium BC pile-dwellings on Ljubljansko barje,Slovenia

We present absolute dates of seven late Neolithic pile-dwellings on Ljubljansko barje, Slovenia. They were settled from ca. 3600 to 3332 (±10) and from 3160 to 3071 (±14) cal BC, as shown by investigations of wood using dendrochronology and radiocarbon wiggle-matching. We defined eleven periods of intensive tree felling (and building activities) and one major settlement gap (when no trees were felled) from 3332 to 3160 cal BC. A major settlement gap presumably also followed after 3071 cal BC (i.e., after the end date of the investigated sites). Our investigations included over 2500 pieces of wood, mainly from the piles on which the dwellings were built. Among important wooden artefacts were a wheel with axle (one of the oldest preserved wheels in the world) and two dugout canoes, all from the settlement phase from 3160 to 3100 cal BC. As shown by parallel studies, the economy in the sites was characterized by copper metallurgy, skilful wood processing and use, cultivation of domestic plants, gathering of wild plants, animal husbandry, hunting and fishing. The settlements were contemporaneous with a number of sites in the north of the Alps, the younger ones coincided with the lifetime of the Neolithic Iceman (Ötzi). Since Ljubljansko barje has a strategic position at the crossroads between western central and (south) eastern Europe the presented absolute dates provide a basis for their comparison with other dated contemporaneous sites (in the west), to revise the chronology of similar sites in the (south) east (which are not yet exactly dated), and to evaluate their interconnection and roles in cultural development in prehistory.     

Teardrops at the Lake: Chemistry of New Kingdom to Makuria Glass Beads and Pendants Between the First and Second Nile Cataracts

International expeditions extensively excavated Lower Nubia (between the First and Second Nile Cataracts) before it was submerged under the waters of Lake Nasser and Lake Nubia. The expeditions concentrated on monumental architecture and cemeteries, including sites at Qustul and Serra East, where the New Kingdom, and Napatan, Meroitic, Nobadian, and Makurian-period elites and common people were buried, ca. 1400 BC–AD 1400. Although the finds abound in adornments, including bead imports from Egypt and South India/Sri Lanka, only a few traces of local glass bead-making have been recorded in Nubia so far. Based on results of laser ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) analysis of 76 glass beads, pendants, and chunks from Qustul and Serra East contexts, dated between the New Kingdom and the Makuria Kingdom periods, this paper discusses the composition and provenance of two types of plant-ash soda-lime (v-Na-Ca) glass, two types of mineral soda-lime glass (m-Na-Ca), and two types of mineral-soda-high alumina (m-Na-Al) glass. It also presents the remains of a probable local glass bead-making workshop dated to the period of intensive long-distance bead trade in Northeast Africa, AD 400–600.