Size and Distribution of the Population in Late Bronze Age Messenia: Some Statistical Approaches

Abstract

The region of Messenia in extreme SW Greece has recently received unusual attention not only from archaeologists but also from philologists, historians, and various social and natural scientists. This article represents an attempt to synthesize some of the data thus generated in order to explore the locational concerns of the inhabitants in the Late Bronze Age (1600-1100 B.C.). Some statistical techniques are used to generate a prediction of the regional population, to investigate the differential distribution of the population over the varied landscape, and to attempt to understand the significance of the population distribution in terms of the social and economic organization of the developed kingdom of Pylos (13th century B.C.).     

Characterization of organic media in the wall-paintings of the “Palace of Nestor” at Pylos,Greece: evidence for a secco painting techniques in the Bronze Age

This paper presents the results of an investigation of organic binding media detected in samples from the Mycenaean wall-paintings at the “Palace of Nestor” in Pylos (Western Messenia, Greece): samples dated from the Late Bronze Age (ca. 1200 BC). This is the first scientific study to be conducted on organic binding media in Mycenanean painting, and it is a study that aims to contribute significantly towards our understanding of the original painting techniques used during the Bronze Age. The analytical procedures employed for the detection and characterization of the organic substances preserved within the paint layers (proteinaceous materials, lipids and plant gums), were based on chromatography/mass spectrometry techniques (PY–GC/MS, GC/MS). The most significant results, highlighting an a secco painting technique, are herein reported and discussed.     

PARALLELS and CONTRASTS IN the BRONZE AGE of the PELOPONNESE

Summary: The provinces of the north-east Peloponnese, Laconia, and Messenia are chosen for comparison, as likely to have been always the most significant in the Peloponnese. Differences in the observable patterns of site-distribution are pointed out, which seem to conflict with the models suggested in Bintliff 1977 and to suggest a degree of local variation. the histories of the three provinces through the Bronze Age, so far as they can be outlined, have features in common but can be shown to vary at several significant points, strengthening this suggestion.     

The Bronze Age landscape of the Bjäre peninsula,southern Sweden,and its relationship to burial mounds

Palaeoecological analyses from a small fen deposit, combined with pollen analysis from buried soil profiles under prehistoric burial mounds, have been used to investigate the timing and vegetation change associated with the Holocene development of a cultural landscape in southern Sweden. Traditional pollen analysis is complemented with plant macrofossil analysis and soil pollen analysis from within and in close proximity to the burial mounds in the coastal Bjäre peninsula, well known for its high density of well-preserved Bronze Age monuments. The vegetation development is linked to the construction of the burial mounds. A marked increase of cultural impact on the landscape is recorded during the Neolithic–Bronze Age transition and estimates of landscape openness suggest that by the onset of the Bronze Age, forest cover was only 20–40%, falling to 10% in the immediate vicinity of the burial mounds themselves. The coastal strip appears to have been affected by human activity to a greater extent and at an earlier date than sites from further inland in southern Sweden and the Bronze Age burial mounds were most likely designed to be visible in a largely deforested landscape.     

Bronze Age Field Systems in the Thames Valley

In the last two decades excavation along the River Thames has shown the remarkable survival of Bronze Age field systems. A managed farming landscape emerged in this lowland area during the Middle Bronze Age and continued to develop until the end of the Late Bronze Age. In the latter period the field systems were divided into several regional groups in each of which there was a high status settlement and a concentration of river metalwork. They provide evidence for a predominantly pastoral economy in the Thames Valley on a scale which may have supported an increasingly hierarchical society. Settlements and field systems were abandoned during the Late Bronze Age, and by the Bronze Age–Iron Age transition new sites were largely confined to the extreme upper reaches of the Thames, an area which had been peripheral to the alliance and exchange system that had operated downstream.     

Historical context and chronology of Bronze Age land enclosure on Dartmoor,UK

The upland of Dartmoor, southwest England, is one of the flagship prehistoric landscapes within Britain owing to the excellent survival of extensive prehistoric coaxial field systems. Archaeological surveys and rescue excavations during the 1970s and 1980s did much to further the understanding of this landscape; however, much remains to be explored, in particular the chronology of enclosure, the nature of the pre-enclosure landscape and the relationship between Bronze Age communities and their environment. Reconsideration of this landscape is important, given the place it holds in our understanding of subdivision of the landscape across northwest Europe during prehistory. This paper presents new palaeoecological data recovered as part of an integrated archaeological and palaeoecological project on northeast Dartmoor. The sequences detailed here include the first dated Neolithic period palaeoenvironmental data from within the prehistoric enclosed land on the moor, providing a longer-term context for enclosure. Neolithic groups are implicated in the first establishment of heathland in the study area at around 3630–3370 cal BC. During the early Bronze Age, reestablishment of hazel scrub in the study area implies reduced use of the upland, although it is not clear whether this is local or indicative of the wider landscape. A combination of pollen and fungal spore data indicates a substantial shift to species-rich grassland with grazing animals at c.1480 cal BC in a phase that lasted 400 years. The later Bronze Age and early Iron Age are characterised by low intensity use of the upland. These data provide new chronological data for land cover change on Dartmoor and whilst they broadly confirm existing models of upland land use in later prehistory, their proximity to the standing archaeology affords a more nuanced interpretation of local change.     

Two Traditions of Bronze Age Burial in the Stonehenge Landscape

A study of the size of round barrows in relation to their position in the Stonehenge landscape allows us to define two types of mound, here termed 'Conspicuous' and 'Inconspicuous'. Conspicuous barrows are large and prominently located, whilst inconspicuous barrows are smaller and less strikingly placed. Inconspicuous barrows were associated mainly with funerary urns and were constructed throughout the Early and Middle Bronze Ages. Conspicuous barrows contain a wider range of grave goods and were mainly built in the later part of the Early Bronze Age. The Conspicuous barrows were impressive features of the prehistoric landscape and may have been built there because of the long-established significance of some of the local monuments, including Stonehenge itself. They contain exotic grave goods and could have been the burial places of a wider population. By contrast, the Inconspicuous barrows appear to be associated with settlement areas. They contain a range of ceramic grave goods which extend throughout the Early and Middle Bronze Ages and may have been built by the people who were living in the area. The latter tradition is the longer lived and retained its importance into the Middle Bronze Age when more conspicuous mounds were no longer built.     

Genesis,age and archaeological significance of a pedosediment in the depression around Tell Mozan,Syria

A pedosedimentological profile from the ditch surrounding the lower town of the Bronze Age site of Mozan is investigated for its soil and sedimentological characteristics and has been dated in order to gain information on the use of the ditch and on the landscape development surrounding the settlement. The depression did not contain large amounts of water (flowing or stagnant) and probably was used for agricultural purposes. Accumulation – that in part includes anthropogenically-derived, redeposited, and bioturbated debris – started at around 2800 cal. BC or later, and was especially intensive at some time between 2800 and 1000 cal. BC. Deposition may have been caused by intensive agricultural use of the landscape during the urban explosion of the Early Bronze Age or in the early Middle Bronze Age.     

OFFSHORE FINDS FROM THE BRONZE AGE IN NORTH-WESTERN EUROPE: THE SHIPWRECK SCENARIO REVISITED

Summary.   This article challenges received thinking relating to the interpretation of Bronze Age finds from the seabed in the waters of north-western Europe, especially the North Sea and Channel area. Metal objects recovered from the sea are traditionally presumed to be the result of shipwrecks. As such, their interpretation as casual, if unfortunate loss is unquestioned. However, abandoning the shipwreck scenario as a remnant of the 'sacred vs profane' heuristic, it is suggested that offshore finds could provide insight into deliberate Bronze Age maritime practice, rather than misadventure. Certain patterning in the data of offshore finds, including affinities with hoards on terra firma , urges another interpretive framework – that of considering the sea as a place for deposition. This appeared to be the case particularly in regions which experienced an intensity of maritime interaction, such as the Channel area during the later Bronze Age. From this it is hypothesized that rather than being considered outside the Bronze Age social realm, the sea, especially in the MBA to earlier LBA in the Channel area, was incorporated into Bronze Age cosmology in similar ways to other zones in the landscape.     

Bronze Age landscape dynamics: spatially detailed pollen analysis from a ceremonial complex

The late Neolithic and early Bronze Age are periods marked by the construction of conspicuous concentrations of ‘ritual’ complexes, used for funerary rituals, seasonal gatherings and communal activities. Understanding the environmental context of monuments may provide detailed insights into relationships between the physical environment and the activities undertaken at individual monuments. Raised burial mounds (barrows) are generally assumed to have been constructed in open landscapes (the so-called ‘landscape openness’ hypothesis) thus rendering them highly visible in the surrounding landscape. This paper seeks to test to what extent vegetation (and in particular openness) around a dense concentration of barrows was actively managed, using three pollen sequences in close spatial juxtaposition to the archaeology. The local vegetation histories, supported by radiocarbon dating, demonstrate spatial differences in vegetation pattern both during the time of monument construction and use (c. 2000–1500 cal BC) and during subsequent periods. They do not support the ‘landscape openness’ hypothesis. This suggests that there is no single ‘blueprint’ for vegetation structure on and around these types of monument complexes. There is no evidence for major restructuring of the landscape during the early Bronze Age. The data describe a major transformation of the vegetation around 1500 cal BC (the Middle Bronze Age) in an area not known for archaeology of this date. This serves to emphasize the role of palaeoecology in augmenting the archaeological record of landscape re-organisation and transformation in prehistory.     

The Early Bronze Age funerary archaeological landscape of western Ja'alan: results of three seasons of investigation

This paper presents the results of three seasons of investigations in the western part of Ja'alan in the southern al‐Sharqyiah Governorate in the Sultanate of Oman. The results highlight the importance of this part of Ja'alan during the Early Bronze Age (EBA), particularly the Hafit period and provide us with important information about the funerary archaeological landscape during this period. The results also reveal important aspects of landscape utilisation and occupation during this time and add to our knowledge of the cultural and economic facets of the earliest Bronze Age societies. The distribution of tombs in the landscape suggests that they were constructed by nomadic or semi‐nomadic pastoral groups that shifted from one location to another in search of grazing for their livestock. The availability and seasonality of natural resources such as water, pasture and game made it necessary for them to mark their tribal territory with their funerary structures.     

NEOLITHIC SOILS, MIDDENS AND ALLUVIUM IN THE LOWER WELLAND VALLEY

Summary. The soil micromorphological analysis of buried soils and probable 'midden' deposits buried beneath alluvium from six sites in the lower Welland valley between Maxey and Etton (Cambridgeshire) has revealed a deforested early Neolithic landscape which quickly became subject to seasonal alluviation. This paper suggests that the Neolithic/Bronze Age use of this landscape is directly related to its interpretation as an alluviated floodplain rather than an alluviated, former dry-land landscape.     

Testing micro-regional variability in the Holocene shaping of high mountain cultural landscapes: a palaeoenvironmental case-study in the eastern Pyrenees

Previous research acknowledges the ancient and complex land-use history of European mountainous areas, which are characterised by a remarkable regional variability in terms of human practices and patterns of occupation during the Holocene. However, the combined palaeoenvironmental and archaeological study of highland human management at a micro-regional scale remains a largely unexplored research field, especially in the Pyrenees. A combined pollen, stomata, non-pollen palynomorphs (NPPs) and macrocharcoal study was carried out at three nearby alpine and subalpine peat basins from a relatively small territory (ca.1700 ha) at the Madriu valley (Andorra, eastern Pyrenees), following a fine spatial-resolution strategy. The purpose was to test the suitability of high altitudinal palaeoecological sequences when reconstructing past small-scale land-use variability. The palaeoecological results of those peat records are compared and further integrated with archaeological local data, and together underline the marked complexity of high mountain land-use system over the Holocene period. Main phases of micro-regional land-use and landscape variability can be distinguished from the middle Neolithic to the early Bronze Age and from the Roman Period to the Modern Era. Conversely, several phases of homogeneous landscape management are distinguishable during the early Neolithic, and from the late Bronze to the late Iron Age. Results drawn from this study show that landscape variability is not necessarily connected to topographic or climatic parameters, and underline the role of social, economical and cultural parameters in the land-use organisation and the landscape shaping of high mountain spaces since Prehistory.     

Sheep wool in Bronze Age and Iron Age Europe

This study presents the results of a series of wool measurements from Bronze Age and Iron Age skins and textiles from Hallstatt, and Bronze Age textiles from Scandinavia and the Balkans. A new method of classification that was set up and applied on mostly mineralised Iron Age material has now been applied to a large body of non-mineralised material from the Bronze and Iron Ages. Three types of microscopes were used and their advantages and disadvantages assessed. The results of the investigation cast new light on sheep breeding and fibre processing in prehistoric Europe, and suggest that different sheep breeds existed in Bronze Age Europe.     

Pastoralist Mobility in Bronze Age Landscapes of Northern Kazakhstan: 87Sr/86Sr and δ18O Analyses of Human Dentition from Bestamak and Lisakovsk

ABSTRACT

The role of migration and mobility of people across the steppe has often been cited as key to Bronze Age developments across Eurasia, including the emergence of complex societies in the steppe and the spread of material culture. The central Eurasian steppe (CES) is a focal point for the investigation of the shifting nature of pastoral societies because of the clear transition in archaeological patterning that occurred from the Middle (MBA) to Late Bronze Age (LBA). The spread of LBA (1700–1400?cal BC) Andronovo cultural materials found across wide swaths of the steppe provide indirect evidence for broad scale interactions, but the degree to which people moved across the landscape remains poorly understood. This study takes a first step into documenting human movement during these critical periods through strontium (⁸⁷Sr/⁸⁶Sr) and oxygen (δ¹⁸O) isotopic analyses of tooth enamel recovered from human individuals buried in the cemeteries of Bestamak (MBA) and Lisakovsk (LBA) in northern Kazakhstan. Strontium isotope results, referenced against the distribution of contemporary bioavailable strontium in the vicinity of both sites, suggest local communities engaged in small-scale mobility with limited ranges. Reduced strontium and oxygen isotopic variation visible in humans from Lisakovsk suggests mobility decreased from the Middle to Late Bronze Age likely indicative of a shift in resource and landscape use over time.     

Bronze Age Barrows: Factors Influencing Their Survival and Destruction

This paper analyses the influences on the survival of Bronze Age round barrows in two regions of southern Britain, the Upper Thames Valley and the Stonehenge Environs. It is clear that persistent arable farming in the medieval period had a highly destructive effect on these burial mounds. This can be seen despite later agricultural activity. Other factors such as the type of barrows can also be important factors in the survival and destruction of these burial mounds. Nevertheless, when analysing the distribution of these Bronze Age monuments, later historic land use must be considered as well as the contemporary prehistoric landscape.     

Neolithic and Bronze Age Agriculture in Southern Scandinavia – Recent Archaeobotanical Evidence from Denmark

Abstract

This paper presents archaeobotanical studies from the Danish regions of Thy, northern Schleswig and Djursland. The data are discussed in the light of developments in the landscape and in house architecture; comparisons are made with the contemporary situation in southern Sweden. Pollen analysis reveals that Thy was more or less treeless by the end of the Neolithic, whereas Djursland maintained its forests for a further 1500 years; the situation in northern Schleswig lies somewhere in between. Developments in house architecture are very similar in the three areas. The shift from two-aisled to three-aisled houses occurred in period I/II of the Bronze Age and phosphate analyses suggest that the earliest Danish byre dates from the beginning of period II.

Crop plant assemblages are dominated by naked barley and emmer and remain remarkably stable from the Single Grave Culture to the Late Bronze Age in Thy, from the Middle Neolithic to the middle of the Bronze Age in northern Schleswig, and from the Late Neolithic to the Late Bronze Age on Djursland. Other crops come and go – einkorn, bread wheat, spelt, millet, flax, oats and gold of pleasure. Hulled barley is largely conspicuous by its absence. Well-developed arable weed floras appear first in the Early Bronze Age – arable weeds are very scarce at Neolithic sites. There is evidence of improvement of arable soils using fen peat and household refuse and manure. The situation appears somewhat more complex in Denmark than that described for Sweden. The most striking difference is seen in the behaviour of hulled barley, which becomes massively dominant in Sweden in the course of the Bronze Age, whereas its role in Denmark is much more modest.     

Branded Axes,Thrown into a Pool? The Hoogeloon Hoard and the Shape‐Based Bronze Economy of the North‐West European Bronze Age

One of the biggest challenges for students of the European Bronze Age is to understand the reason behind the massive deposition of large amounts of recyclable metal in non‐metalliferous regions. Such depositions are particularly puzzling when material was buried in a manner which directly seems to denote trade itself, in so‐called ‘trade hoards’. Based on observations on a recent find of such a hoard, in Hoogeloon (NL), we move to an overview of Bronze Age metalwork economy in general and the deposition of trade stock in particular. We argue that Middle Bronze Age metalwork circulation in North‐west Europe may be understood as an aes formatum system, with the serially produced axes in hoards displaying a koiné having a particular social evaluation: a ‘brand’. We suggest that objects were selected by brands for their deposition in the landscape and that this ‘ritual’ act was integral to the ‘practical’ economy of circulation.     

The Abandonment of the ZH-Mozartstrasse Early Bronze Age Lake-settlement. GIS Computer Simulation of the Lake-level Fluctuation Hypothesis

Although 'lake-dwellings' existed from the middle of the fifth millennium to the eighth century BC, the entire phenomenon was not a continuous one. There are several periods when the lake shores were abandoned and subsequently reoccupied. The pattern of occupation depends on cultural as well as environmental factors, amongst them the topography and the climate.
Unlike the southern part of the Alps, which seems to have had a more regular occupational pattern throughout the Neolithic and the Bronze Age, the northern Alpine region shows a marked discontinuity along most of the lake shores. Two relevant breaks in lake-shore occupation are known within the northern Alpine region Bronze Age. The first occurred between the 24th and the 20th centuries BC, and the second from the 15th to the middle of the 12th century BC.
The Early Bronze Age site of ZH-Mozartstrasse, situated on the western extreme of Lake Zurich (Switzerland), was abandoned immediately before the beginning of the second major occupational gap in 1503 BC. Two other Early Bronze Age sites namely Bodman-Schachen 1 on Lake Constance, and Arbon-Bleiche 2 on the Swiss part (the southern shore) of the same lake, follow a similar chronology in occupation; and they were both abandoned in the last decade of the 16th century BC.
A possible cause of abandonment is discussed in this paper using an environmental approach related to an abrupt change of climatic conditions which resulted in an increase of the lake levels which forced those prehistoric populations to leave the proximity of the lake shores. Following the implications of pollen and sedimental analyses, the transformation of the Bronze Age landscape caused by the lake water invasion will be simulated with the help of CAD and GIS computer programs.     

Climate deterioration and land-use change in the first millennium BC: perspectives from the British palynological record

Climate deterioration at around the time of the Bronze Age/Iron Age transition has for long been argued to have resulted in upland abandonment in northern and western Britain, and recent research has provided evidence that a major climate downturn from 850 cal BC caused settlement abandonment in western Europe and potentially worldwide. It is, however, unclear to what extent only ‘marginal’ sites were affected, due to the lack of any systematic attempt to view the evidence for settlement and land-use change across a range of landscape types with differing sensitivities to environmental change. This paper addresses this issue by an evaluation of 75 pollen sequences spanning the late Bronze Age and early Iron Age in Britain to assess whether climatic deterioration was sufficient to cause widespread land abandonment. The results provide no evidence for wholesale land-use change at this time; the overall picture is one of continuity of land use or even increased agricultural activity. There are, however, hints of regional variability, with a greater tendency to abandonment of upland areas in Wales, and signs of woodland regeneration in agriculturally productive areas of lowland central southern England. The latter pattern may reflect a combination of rising ground-water levels affecting local land-use in the immediate vicinity of the mires which provide the source of the pollen data, against a backdrop of regional-scale social and economic changes at the Bronze Age-Iron Age transition.