Durrington Walls to West Amesbury by way of Stonehenge: a major transformation of the Holocene landscape

2012 ◽  
Vol 92 ◽  
pp. 1-36 ◽  
Author(s):  
Charles French ◽  
Rob Scaife ◽  
Michael J Allen ◽  
Mike Parker Pearson ◽  
Josh Pollard ◽  
...  

A new sequence of Holocene landscape change has been discovered through an investigation of sediment sequences, palaeosols, pollen and molluscan data discovered during the Stonehenge Riverside Project. The early post-glacial vegetational succession in the Avon valley at Durrington Walls was apparently slow and partial, with intermittent woodland modification and the opening-up of this landscape in the later Mesolithic and earlier Neolithic, though a strong element of pine lingered into the third millennium bc. There appears to have been a major hiatus around 2900 cal bc, coincident with the beginnings of demonstrable human activities at Durrington Walls, but slightly after activity started at Stonehenge. This was reflected in episodic increases in channel sedimentation and tree and shrub clearance, leading to a more open downland, with greater indications of anthropogenic activity, and an increasingly wet floodplain with sedges and alder along the river's edge. Nonetheless, a localized woodland cover remained in the vicinity of Durrington Walls throughout the third and second millennia bc, perhaps on the higher parts of the downs, while stable grassland, with rendzina soils, predominated on the downland slopes, and alder–hazel carr woodland and sedges continued to fringe the wet floodplain. This evidence is strongly indicative of a stable and managed landscape in Neolithic and Bronze Age times. It is not until c 800–500 cal bc that this landscape was completely cleared, except for the marshy-sedge fringe of the floodplain, and that colluvial sedimentation began in earnest associated with increased arable agriculture, a situation that continued through Roman and historic times.

Author(s):  
A. Tuba Ökse

This article presents data on the Early Bronze Age (EBA) of southeastern Anatolia. The EBA chronology of southeastern Anatolia is parallel to northern Syrian chronologies. The traditional EBA I-III chronology of Anatolia is based on the Tarsus sequence and the EBA I-IV chronology of northwestern Syria on the Amuq and Tell Mardikh sequences. The distribution of ceramic groups and special vessel types reflects geographical and chronological differences throughout the third millennium BCE. The relative chronologies of geographical zones and individual periods are based mainly on ceramic distributions; absolute dates obtained from radiocarbon analyses are rare.


2000 ◽  
Vol 80 (1) ◽  
pp. 27-65 ◽  
Author(s):  
Stuart Needham

The discovery of a pair of armlets from Lockington and the re-dating of the Mold cape, add substance to a tradition of embossed goldworking in Early Bronze Age Britain. It is seen to be distinct in morphology, distribution and decoration from the other previously defined traditions of goldworking of the Copper and Early Bronze Ages, which are reviewed here. However, a case is made for its emergence from early objects employing ‘reversible relief to execute decoration and others with small-scale corrugated morphology. Emergence in the closing stages of the third millennium BC is related also to a parallel development in the embossing of occasional bronze ornaments. Subsequent developments in embossed goldwork and the spread of the technique to parts of the Continent are summarized. The conclusions address the problem of interpreting continuity of craft skills against a very sparse record of relevant finds through time and space.


2016 ◽  
Vol 96 (2) ◽  
pp. 131-163 ◽  
Author(s):  
Frieda S. Zuidhoff ◽  
Johanna A.A. Bos

AbstractDuring several archaeological excavations on a river terrace of the river Meuse near the village of Lomm (southeast Netherlands) information was gathered for a reconstruction of the sedimentation and vegetation history during the Holocene. Various geoarchaeological methods – geomorphological, micromorphological and botanical analyses – were applied, while accelerator mass spectrometry (AMS) 14C and optically stimulated luminescence (OSL) dating provided an accurate chronology for the sediments.During the Early Holocene, many former braided river channels were deepened due to climate amelioration. Later, river flow concentrated in one main river channel to the west, at the location of the modern Meuse. The other channels were only active during floods, and infilling continued until the Bronze Age. Because of the higher setting of the Lomm terrace, it was only occasionally flooded and therefore formed an excellent location for habitation. Humans adapted to the changing landscape, as most remains were found on the higher river terraces or their slopes, a short distance from the Maas river. The Lomm terrace was more or less continuously inhabited from the Mesolithic onwards.During the Early Holocene, river terraces were initially densely forested with birch and pine. From the Boreal (Mesolithic) onwards, dense mixed forests with deciduous shrubs and trees such as hazel, oak, elm and lime developed. During the Atlantic (Meso/Neolithic), the deciduous forests became dominated by oak. Due to human activities from the Late Subboreal (Late Bronze Age) onwards, forests slowly became more open, yet remained relatively dense in comparison to other Dutch areas. The botanical data, however, show that within the Lomm study area there was a large difference in the composition, distribution and openness of the vegetation. The spatial variation in openness came into existence during the Late Bronze Age, as soon as the higher areas started to be used for human activities (i.e. habitation, agriculture and livestock herding). Due to human activities, the northern part of the study area became very open during the Early Roman period. In the lower-situated areas of the southern part, however, forests remained present much longer, until the Early Middle Ages. Due to large-scale deforestation in the Lomm area and hinterland during the Roman period and Middle Ages, the sediment load of the river increased, large floods occurred and overbank sediments were deposited, burying the archaeological remains. The largest increase in sedimentation occurred after the Middle Ages.


2001 ◽  
Vol 4 (3) ◽  
pp. 346-366 ◽  
Author(s):  
Natalia I. Shishlina

This article is devoted to the understanding of the importance of seasonal use of grasslands in the occupation of the Eurasian steppe during the Bronze Age. The pilot section of the research is Kalmykia – a steppe situated between the lower Volga and the Don rivers. We have to look at specific strategies of using local environments, river valleys, upland plateaux, and open steppe lands. During the third millennium BC, pastoralists of the Yamnaya and Catacomb cultures began to exploit the Eurasian steppe grasslands and they had to take advantage of the seasonal variation in steppe vegetation to create a sustainable economy. Seasonal use of grasslands became the main feature of the definition of pastoralism. This is the first time that early steppe materials have been analysed for seasonal data. On the basis of a combination of the seasonal data, settlement data and recent chronological information, a preliminary reconstruction is presented of two contrasting periods of land use for the third millennium BC.


1999 ◽  
Vol 49 ◽  
pp. 177-187 ◽  
Author(s):  
Ünsal Yalçın

The beginning of the Iron Age is generally dated to the last quarter of the second millennium BC in Anatolia and the Near East. The development of iron metallurgy allowed many tools and weapons to be produced in this period. The earliest iron finds, which are not more than a dozen, occur in the third millennium BC in Anatolia (Waldbaum 1980 discusses these early finds). Considering that pure iron occurs rarely in nature, the most important question is: what were these objects made of? Preliminary analyses of a few Bronze Age finds show that some of them contain nickel. Because of this it is generally accepted and frequently cited that these finds were made of meteoric iron.


Author(s):  
Kimberly D. Williams ◽  
Lesley A. Gregoricka

The shift between Hafit (ca. 3100–2700 BC) and Umm an-Nar (ca. 2700–2000 BC) mortuary traditions on the Oman Peninsula is poorly understood, primarily because the semi-nomadic communities of this liminal period left little to the archaeological record, with the exception of monumental tombs. Because of the ambiguity surrounding this transition, tombs from this time are typically classified as either ‘Hafit’ or ‘Umm an-Nar’ without regard for the considerable geographic and temporal variation in tomb structure and membership throughout southeastern Arabia. Recent survey and excavation of a Bronze Age necropolis at Al Khubayb in the Sultanate of Oman have revealed Transitional tombs that—far from exhibiting a simplified dichotomy—represent a blurring of the traditionally discrete boundaries dividing the Hafit and Umm an-Nar periods. Bioarchaeological analyses of tombs at Al Khubayb further enable researchers to make a distinction between tomb types and elucidate the process by which mortuary treatments changed. Over the late fourth and into the early third millennium BC, these entombment practices changed from (a) relatively small, roughly-hewn limestone tombs known as Hafit-type cairns to (b) Transitional tombs displaying features intermediary to both Hafit and Umm an-Nar period mortuary structures to (c) large, expertly-constructed Umm an-Nar communal tombs.


2000 ◽  
Vol 3 (2) ◽  
pp. 167-187 ◽  
Author(s):  
David Frankel

During the third millennium cal BC, there were major changes in many aspects of Cypriot material culture, technology and economy which characterize the division between the Chalcolithic and early Bronze Age on the island. Many innovations can be traced to Anatolian antecedents. These include a very wide array of domestic as well as agricultural and industrial technologies. Their nature and range make it possible to argue strongly for the movement of people to the island, rather than for other mechanisms of technology transfer and culture change. This identification of an intrusive group, with distinctive patterns of behaviour (habitus), opens up questions of prehistoric ethnicity, and the processes by which the initial maintenance of different lifeways by indigenous and settler communities eventually gave way to a common cultural system.


Antiquity ◽  
1976 ◽  
Vol 50 (197) ◽  
pp. 14-19 ◽  
Author(s):  
V. M. Masson

On the resumption of excavation in the autumn of 1972, a funerary complex belonging to a community of priests was discovered among a group of religious buildings in the early urban Bronze Age centre of Altin-depe in South Turkmenia. All the material found there dates from the early stages of Namazga V, or, using the accepted chronology, from the end of the third millennium BC (Masson, 1973, 481). It had previously been established that the chief building of this religious group was a stepped, tower-like edifice which had clearly been built in the style of the Mesopotamian ziggurats and had been rebuilt three times in the course of its existence (Masson and Sarianidi, 1972, 117–18). The funerary complex excavated in 1972 corresponds chronologically to the first, relatively small, ziggurat and was situated southeast of it.


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