Evaluating prehistoric finds of Arrhenatherum elatius var. bulbosum in north-western and central Europe with an emphasis on the first Neolithic finds in Northern Germany

The swollen basal internodes of the grass species Arrhenatherum elatius var. bulbosum (tuber oat grass) are recorded here for the first time for Neolithic Germany. These charred bulbs occurred in the Late Neolithic soil mantle of the megalithic tomb of Albersdorf-Brutkamp LA 5. They are interpreted as most probably originating from the natural vegetation on and around the grave mound. The bulbs were possibly charred in the course of a ritual fire. However, their use as gathered plants and their intentional deposition in a secondary burial ritual during the Late Neolithic cannot be excluded with any certainty. Identification criteria for Arrhenatherum bulbs as well as the ecological requirements of the species are introduced here. Furthermore, prehistoric bulb finds from north-western and central Europe, and different interpretations concerning the occurrence of Arrhenatherum in different archaeological contexts, are discussed. The compilation of finds from literature and excavation reports shows that bulbs of Arrhenatherum were found rather infrequently in the Neolithic. Most commonly, charred bulbs of A. elatius var. bulbosum are detected in Bronze Age cremation graves. In the Iron Age, however, they mainly occur in domestic sites. This shows that the interpretation of the plant remains is dependent on their archaeological context. A ritual meaning of the bulbs has to be considered in the interpretation, but they may also have contributed to people’s daily diet. This evaluation of bulb finds in prehistoric and historic contexts contributes to the debate on the relevance of plant gathering in early economies and in ritual activities.     

Possible shell beads from the Middle Stone Age layers of Sibudu Cave,South Africa

Recent excavations at Sibudu Cave, KwaZulu-Natal, South Africa, uncovered an Iron Age horizon below which is a complex 3 m thick Middle Stone Age sequence with post-Howiesons Poort, Howiesons Poort, Still Bay and pre-Still Bay layers. Available OSL ages indicate that the Howiesons Poort occupation is older than 60 ky and the Still Bay older than 70 ky. Here we present the archaeological context and the taphonomic analysis of six Afrolittorina africana, three of which bear perforations, from the Still Bay and Howiesons Poort layers of this site. The single specimen from the latter cultural horizon comes from the lowermost layer attributed to this technocomplex. This and the depositional context of this layer suggest that this shell derives, as do the other five, from the Still Bay occupation layers. Taphonomic analysis of the archaeological specimens based on present day Afrolittorina africana biocoenoses, microscopic examination, morphometry, experimental perforation of modern shells, and a review of the natural agents that may accumulate marine shells at inland sites, indicate probable human involvement in the collection, transport, modification, and abandonment of Afrolittorina africana in Sibudu. If confirmed by future discoveries these shells would corroborate the use of personal ornaments, already attested at Blombos Cave, Western Cape Province, by Still Bay populations. The apparent absence of ornaments at Howiesons Poort sites raises the question of the mechanisms that have led to cultural modernity since it seems to contradict the scenario according to which cultural innovations recorded at Middle Stone Age sites reflect a process of continuous accretion and elaboration interpreted as the behavioural corollary of the emergence of anatomically modern humans.     

Chronology during the Bronze Age in the archaeological site Tell Qubr Abu al-‘Atiq, Syria

Archaeosediments are deposits with a direct or indirect anthropogenic component. They provide useful information about past human activities and interaction with the environment. When other materials, such as pottery, are present in archaeosediment layers, the combination of TL ages from pottery and OSL ages from sediments can provide complete data about the occupation and evolution of an archaeological setting. In Mesopotamia, tells are mounds formed by the debris of human occupation and the accumulation of muddy sediments mainly due to the decomposition of mud bricks in ancient towns. Many other materials such as pottery fragments, bones and charcoal can be found in the sediment layers. The combination of OSL, TL and radiocarbon ages can be very useful in the case of the Bronze Age Period in Syria, allowing the occupation sequence of such archaeological sites to be reconstructed. Tell Qubr Abu al-’Atiq, is located on the left bank of the Middle Euphrates River (Syria). The archaeological artefacts found in the sediment layers (pottery) collected during excavations in two areas of the site, indicated the occupation of the tell during the Early and Late Bronze Age by typological pottery classification. The radiocarbon ages of charcoal indicate that human occupation fits the archaeological hypothesis, providing an older and maximum occupation period between 2800 and 2300 BC and a younger period between 1400 and 900 BC. OSL dating of sediments shows ages younger than charcoal, while TL ages of pottery are generally older than sediment and charcoal ages. This can be explained as the different materials correspond to different events. The charcoal and pottery correspond to occupation periods, while sediments correspond to the further destruction of the site.     

Archaeological material and ethnic identification. A study of Lappish material from Varanger,Norway

The term Lappish Iron Age has been established in Scandinavian archaeology but the ethnic affiliation of the body of archaeological material labelled so has never been discussed in detail. In this article two questions arc discussed: Is it possible from archaeological material to verify a hypothesis about a specific ethnic affiliation? And is it appropriate to refer to this archaeological material as iron age finds? A general discussion about problems involved in identifying ethnic groups is given, after a brief presentation of the empirical material. Attention is drawn to Barth's analysis, where he shows that the cultural content seems to be of two orders: (i) overt signs and signals, and (ii) basic value orientations. The discussion is carried out in accordance with these two orders. It is argued that this analysis cannot provide us with information about a specific ethnic affiliation; although it cannot tell us which group, it can verify that the material in question does represent one specific ethnic group. If we want to identify one specific ethnic group we have to use other sources besides the archaeological record. The use of sources like written documents, linguistics, place names and physical anthropology is discussed. The conclusion is drawn that by the use of various sources we can trace the identity of one specific ethnic group.     

Living on the Edge? Transformation of a Marginal Pleistocene Landscape Into a Settlement Area in the Northeastern Part of the Netherlands

ABSTRACT

This paper will examine settlement location during the Iron Age in the northeast part of the Netherlands, an area shaped by Pleistocene geology. In recent years, a number of Late Iron Age/Early Roman settlements situated on the low lying slopes of sand ridges and nearby stream ridges revealed traces of an earlier Iron Age occupation. Palynological data revealed that this part of the landscape was used by humans before it was transformed into an area of settlement. An analysis of excavation data from two key sites at Denekamp-De Borchert and Groningen-Helpermaar, as well as other known sites, lead to the conclusion that the transformation of ‘peripheral landscapes’ into permanent settlement locations was preceded by a phase of arable cultivation which left no trace of permanent habitation. It is also suggested that the impact of human behaviour on the natural landscape in the Early and Middle Iron Age was much bigger than previously anticipated. When excavating this type of settlement areas dating to the Late Iron Age, archaeologists must be aware that only of a small group of archaeological features exist. The proposed model for the choice of settlement location may be more widespread, because of similarities in landscape between the study area presented here and other landscapes in Northwest-Europe (e.g. parts of Germany and Denmark).     

Archaeological and Historical Materials as a Means to Explore Finnish Crop History

ABSTRACT

In Northern Europe, barley (Hordeum vulgare L.) has been cultivated for almost 6000 years. Thus far, 150-year-old grains from historical collections have been used to investigate the distribution of barley diversity and how the species has spread across the region. Genetic studies of archaeobotanical material from agrarian sites could potentially clarify earlier migration patterns and cast further light on the origin of barley landraces. In this study, we aimed to evaluate different archaeological and historical materials with respect to DNA content, and to explore connections between Late Iron Age and medieval barley populations and historical samples of barley landraces in north-west Europe. The material analysed consisted of archaeological samples of charred barley grains from four sites in southern Finland, and historical material, with 33 samples obtained from two herbaria and the seed collections of the Swedish museum of cultural history.

The DNA concentrations obtained from charred archaeological barley remains were too low for successful KASP genotyping confirming previously reported difficulties in obtaining aDNA from charred remains. Historical samples from herbaria and seed collection confirmed previously shown strong genetic differentiation between two-row and six-row barley. Six-row barley accessions from northern and southern Finland tended to cluster apart, while no geographical structuring was observed among two-row barley. Genotyping of functional markers revealed that the majority of barley cultivated in Finland in the late nineteenth and early twentieth century was late-flowering under increasing day-length, supporting previous findings from northern European barley.     

Archaeobotanical inference of Bronze Age land use and land cover in the eastern Mediterranean

Charcoal and charred seeds at five Bronze Age archaeological sites discern ancient land use in the eastern Mediterranean. Seed frequencies of orchard crops, annual cereals and pulses, and wild or weedy plants are used to characterize plant utilization at different archaeological sites on the island of Cyprus, in the Rift Valley of Jordan, and in the Jabbul Plain and along the upper Euphrates River valley in Syria. Seed to charcoal ratios provide proxies to determine the relative usage of dung versus wood for fuel across the ancient Mediterranean landscape. Greater charcoal and lower charred seed values are interpreted to represent a wooded environment, while higher amounts of charred seeds and minimal wood charcoal suggest a much great use of dung as a fuel source. Interestingly, Politiko-Troullia (Cyprus, Cypriot archaeological sites are, by convention, named for the nearest modern village (Politiko), followed by an italicized toponym (Troullia) referring to the plot of land that incorporates the site) has the lowest seed to charcoal ratio, suggesting its residents primarily burned wood and that the landscape surrounding Troullia remained relatively wooded during the Bronze Age. In contrast, villagers at Tell el-Hayyat (Jordan) utilized a mixture of wood and dung, in contrast to Tell Abu en-Ni’aj (Jordan), and especially Umm el-Marra and Tell es-Sweyhat (Syria), where inhabitants relied solely on dung fuel. Comparative analysis and interpretation of seed and charcoal evidence thus illustrates the variety of fuel use strategies necessitated by the dynamic and diverse Bronze Age landscapes of the Eastern Mediterranean.     

Dynamics of pioneer colonisation in the Early Iron Age in the Duero basin (Central Iberia,Spain): Integrating archaeological and palynological records

Abstract

This study addresses the earliest strategies of permanent occupation in the mountainous regions bordering Northern Meseta in inland Iberia. This piece of work gathers together and discusses archaeological information about settlement in the Late Bronze Age and Early Iron Age and previously published high-resolution palynological cores from three study areas. Its major goal is to assess both archaeological and pollen records in order to gain a better understanding of the dynamics of occupation and transformation of these upland settings. Until cal 700 BC there are no clear signs of permanence in the highlands surrounding the Duero basin, but from that point onwards various initiatives of small-scale spontaneous colonisation have been identified. Colonisation in the Iron Age involved pastoralism, cereal agriculture and a significant use of forestry resources, causing a major anthropogenic impact with irreversible consequences. The outlined account constitutes the first synthetic overview at a macro-regional scale on the beginnings of the integrated and diversified strategies implemented in these upland regions.     

Iron Working in the Vicinity of Weybridge,Surrey

Abstract

The presence of eighteenth-century iron working mills and the coincidental local, but limited, source of iron in the Weybridge area of Surrey, has led a number of authors to suggest that these mills smelted locally extracted iron ore. The present author has described elsewhere the occurrence of the ore and indicated that extraction was in pre-mediaeval times, probably during the Iron Age. In further support of this theory, the original records of Iron Age archaeological sites in the area are shown to reveal positive evidence of iron working. The history of the iron mills throughout their restricted period of iron working is also described, and at each site a close association between the fabrication of iron, and brass and copper products, where the metal is of undoubted extraneous origin, is evident.     

Early ironworking in Iron Age South India: New evidence for the social organization of production from northern Karnataka

Abstract

Iron production was integral to political and ritual practices during the South Indian Iron Age (ca. 1200–300 b.c.), yet the investigation of the social relations of metals production during this period has been overshadowed by studies of iron consumption, particularly of iron objects in megalithic mortuary contexts. Recent archaeological research in the Tungabhadra River Corridor, Karnataka, has revealed iron production debris within and between settlements in more ephemeral occupational contexts, such as rockshelters. One notable discovery is the earliest ironworking facility in South India at Bukkasagara. The regional pattern suggests that iron production involved at least two classes of specialist producers—smelters and smiths—who exercised varying degrees of control over the practice and products of their craft. It also suggests that iron production was an important component in the construction and negotiation of Iron Age social differences, affiliations, and inequalities.     

REDEFINING THE NORTHERN BRITISH IRON AGE

Summary.   Unlike Southern Britain, the Iron Age in Northern Britain spans two millennia from the introduction of iron technology to the Norse settlements. Northern Britain is divided into a series of geographical and archaeological regions, including for the pre-Roman Earlier Iron Age the whole of aceramic and non-coin-using northern England. Despite a wealth of settlement evidence, the Earlier Iron Age lacks diagnostic material assemblages, even in the ceramic Atlantic regions, where radiocarbon dating is now confirming the origins of Atlantic Roundhouses in the mid-first millennium BC. External connections may have been long-distance, reflecting a complex variety of selective connections. For the Later Iron Age, interpretation based upon historical sources has inhibited a proper archaeological evaluation of the 'Picts' and of the traditional view of Dalriadic settlement in Argyll, both of which are now under review.     

Neolithic and Bronze-Age Herders of Pupićina Cave,Croatia

Abstract

Pupi?ina Cave (Croatia) preserves an important archaeological sequence spanning 12,000 years. Here we present and discuss the results of extensive excavations in post-Mesolithic deposits.Pupi?ina Cave,located in NE Istria in a region rich in caves and in prehistoric settlement, has well-dated evidence from the Middle Neolithic, Late Neolithic, Middle Bronze Age, Iron Age, and Roman periods. Visitors to the cave in the Middle Neolithic ca. 5500–5000 in calibrated years B.C (cal B.C.) left typical Danilo/Vla?ka pottery and kept herds of sheep and goats during the spring. Mortality profiles suggest that herds were managed for milk production. During the Late Neolithic (ca. 4550–4150 cal B.C.) Hvar pottery appears along with lithic artifacts from great distances (e.g.,Lipari). Herds of sheep and goats were managed for meat as were cattle and pigs. There was a major hiatus in occupation between the Late Neolithic and the Middle Bronze Age. Middle Bronze Age (ca. 1775–1400 cal B.C.) deposits are found only in one large pit. Pottery is dominated by drinking vessels, and faunal use is the same as in the Late Neolithic. The cave was used primarily as an animal pen during the Iron Age (1st millennium B.C.).     

POST-COLLAPSE: THE RE-EMERGENCE OF POLITY IN IRON AGE BOĞAZKÖY, CENTRAL ANATOLIA

How communities reorganize after collapse is drawing increasing attention across a wide spectrum of disciplines. Iron Age Boğazköy provides an archaeological case study of urban and political regeneration after the widespread collapse of eastern Mediterranean Late Bronze Age empires in the early twelfth century BC. Recent work at Boğazköy has significantly expanded our understanding of long-term occupation in north central Anatolia. This work counters previous suggestions that Boğazköy was abandoned after the collapse of the Hittite Empire during the Early Iron Age. In this paper, we focus on the Iron Age occupations at the site to show how growth in the scale and complexity of ceramic production and trade during this period provides another line of evidence for economic and political re-emergence. Based on the increasing diversity of non-local ceramics and ceramic emulations during the Iron Age, we suggest that only in the Late Iron Age, 500–700 years after Hittite collapse, did Boğazköy re-emerge as a significant polity in central Anatolia.     

Roman Remains Discovered at Avenches,the Chief City of the Helvetii

More iron objects have been found in East Yorkshire than in any other part of Iron Age Britain of comparable size, largely in the burials of the Arras Culture, named after the excavations at Arras near Market Weighton (1815–17). The region also contains one of Britain's largest prehistoric iron production centres, contemporary with the Arras Culture. This article aims to contribute to re-establishing early iron production and consumption, and its social and economic significance in the archaeological mainstream, and demonstrate the importance of understanding ironworking for the Iron Age landscape.     

Subsistence practices in an arid environment: a geoarchaeological investigation in an Iron Age site,the Negev Highlands,Israel

The Negev Highlands (southern Israel) is an arid zone characterized by settlement oscillations. One settlement peak occurred in the early Iron Age IIA (late 10th and early 9th centuries BC). The most conspicuous structure in many sites of this period is an oval compound comprised of an internal courtyard surrounded by rooms. Two hypotheses for the function of these oval compounds are that they served as Israelite fortresses which guarded the southern border and routes of the Solomonic kingdom, or that they represent local agro-pastoral groups. In order to gather more information regarding the subsistence practices conducted in these oval compounds, we carried out a small-scale excavation at the site of Atar Haroa. We focused on sediment sampling and used several geoarchaeological, as well as isotopic, techniques in order to identify macroscopic and microscopic remains related to animal husbandry and crop agriculture. The remains identified from the archaeological sediments were compared with modern reference materials collected from abandoned Bedouin camps. The excavation included two half rooms and several test pits in the courtyard of the oval compound, featuring one Iron Age occupation level composed of gray sediments and relatively small amounts of pottery, bones and macro-botanical charred remains. Micromorphological, mineralogical, dung spherulite and isotopic analyses carried out on the gray occupational sediments from the rooms show that they originate from wood ash and dung, both used as fuel. Similar analyses of the gray sediments in the courtyard show that they originate only from degraded livestock dung. Phytolith analyses show that the gray anthropogenic sediments have similar concentrations of phytoliths as in control (yellowish) sediments and in the dung of winter free-grazing desert livestock and lichen-grazing black dwarf Bedouin goats. Phytoliths indicative of cereal crops are completely absent in the archaeological dung remains, indicating that cereal crops were not processed by the site inhabitants. Based on ethnographic and archaeological parallels, and on the presence of grinding stones and absence of sickle blades in the excavated rooms, we infer that the inhabitants at the oval compound at Atar Haroa subsisted on livestock herding and bought or exchanged cereal grains. Our results support the hypothesis that the inhabitants at the oval compound at Atar Haroa were desert-adapted pastoralists, rather than garrisoned soldiers.     

Environment and Subsistence of the Early Inhabitants of Coastal Southwestern Nigeria

From where did the early inhabitants of the Badagry coastal area of southwestern Nigeria originate? Has the area been occupied from “ancient times,” as claimed by oral traditions? What was the nature of the environment and subsistence of these early inhabitants? Excavations at Apa, west of Badagry, provided answers to these questions. A radiocarbon date of 2670 ± 90 bp showed that human occupation there is at least 3000 years old, and implied occupation during the Late Stone Age. The occupation was in two phases: a prehistoric phase, during which Apa site 1 (Ap1) was occupied, and an historic phase, with occupation of Apa site 2 (Ap2). Sedimentological and archaeological data also showed that the environment at the beginning of occupation was similar to today. The presence of a groundstone axe, charred palm kernels, and charcoal at the Ap1 site is interpreted to imply the clearing and burning of vegetation, probably preparatory to planting and the exploitation of oil palm (Elaeis guineensis) from about 2670 ± 90 bp. D'où sont venus les premiers habitants de la région côtiere Badagry du sud-ouest du Nigeria? Est-il vrai que la région a été occupé depuis les temps anciennes, comme confirme les traditions orales? Quelle étaient la nature de l'environnement et du subsistence de ces habitants préhistoriques? Des fouilles archéologiques à Apa, a l'ouest de Badagry, ont fourni des réponses nécessaires à ces questions. Un date radiocarbone de 2670 ± 90 bp a montré que les activités humaines de ce site date au moins de 3000 années, qui indique que l'occupation des habitants à c'endroit étais durant la periode de l'Age de la Pierre Recent. L'occupation de cette region était en deux phases: un phase prehistorique, la période pendant lequelle le site d'Apa 1 (Ap1) était occupé, et la phase historique, qui a marqué l'occupation du deuxième site d'Apa 2 (Ap2). Les données de la sedimentologie et de l'archéologie ont aussi montrent que l'environnement au commencement d'occupation était similaire de nos jours. On pense que la presence d'un hache “groundstone,” de l'amande de palmier et du charbon à la site d'Ap1 indiques la déstruction de la vegetation, preparant probablement la terre pour la semence et l'exploitation du l'huile de palme (Elaeis guineensis) d'environ de 2670 ± 90 bp.     

Cultivation History Beyond the Periphery: Early Agriculture in the North European Boreal Forest

We have investigated the environmental history of human occupation and the development of agriculture in the eastern interior Lake District of Finland. The material consists of archaeological data, which is reviewed in topographical and agrogeological context, and pollen analytical evidence of agricultural indices from eight precisely dated (varved) lake sediment sequences. Before the Viking Age, archaeological evidence, consisting of stray finds, dwelling sites, and graves, is very scarce. Iron Age finds are clearly confined to the lowland environs with silty and clayey soils. During the Viking Age, the number of stray finds multiplies and the first cemeteries are established. Comparison between Viking and Crusade Period finds reveals a topographic shift toward higher locations and morainic soils. Most of the cup-stones are located on upland sites—that is, not in connection with known Iron Age sites. These are interpreted as medieval indicators of slash-and-burn farming of the fertile but stony supraaquatic morainic soils. There is pollen analytical evidence of sporadic cultivation in the area from the Bronze Age onward. Afterca. AD 700, the occurrence of cereal pollen grains becomes regular but remains discontinuous at each site until after the turn of the millennium. There is then an exponential rise in the cereal pollen rain, indicating a fully agricultural population.     

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.     

Molecular markers for the discrimination of Triticum turgidum L. subsp. dicoccum (Schrank ex Schübl.) Thell. and Triticum timopheevii (Zhuk.) Zhuk. subsp. timopheevii

The persistent uncertainty on the classification of the “new” glume wheat found in Neolithic and Bronze Age sites from Greece and other European settlements might be resolved only through analysis of its ancient DNA. Tools able to discriminate among different Triticum species on the basis of scarce, very damaged DNA, are therefore essential. While current attempts concentrate on DNA fragments sequencing and comparison, in some instances PCR-based selective amplification techniques might offer a cheaper and quicker alternative. The purpose of this research was therefore the identification of species-specific primers, able to distinguish caryopses of Triticum timopheevii subsp. timopheevii from those of Triticum turgidum subsp. dicoccum. Primers and their working conditions were defined and optimized using DNA from modern accessions. The ribosomal primers ITS1 tim and ITS2 tim, and the nuclear primer acetyl-coenzyme A tim clearly discriminated the sequences of Triticum timopheevii from other species. Finally, Neolithic charred wheat grains found in the sites of Sammardenchia (Pozzuolo del Friuli, Udine) and La Marmotta (Lago di Bracciano, Roma), belonging to the “new” wheat type or to emmer, were tested with the three selected primers. However, the results were not conclusive, because the samples analysed were apparently too degraded to yield useful DNA.     

Reconstructing Iron Age Community Dynamics in Eski?ehir Province, Central Turkey

Current understanding of the Iron Age polity of Phrygia in Central Anatolia is primarily based on excavations and survey in the region of the Phrygian capital of Gordion. In order to expand our knowledge of the Phrygian polity, we assess the scale and nature of Iron Age communities in the western (Eski?ehir) region of Phrygia. We address the challenge of interpreting ceramics derived from large-scale archaeological survey by utilizing Neutron Activation Analysis (NAA) of ceramics from 12 sites across the region collected by the Eski?ehir archaeological survey project as well as an excavated assemblage from ?ar H?yük. While the uniformity in ceramic technology and styles suggest the region is part of the larger Phrygian community, NAA results reveal that (a) ceramic production was regionally highly localized with limited evidence of standardization during the Iron Age and (b) based on evidence of community interaction it is possible to establish a partial chronological sequence of development. These results have implications not only for understanding the internal dynamics within the Phrygian core but also for developing a methodology for comparing ancient polities using commensurate units of interacting communities. The present study is part of the larger Anatolian Iron Age Ceramics project (http://www.une.edu.au/a-ia).