scholarly journals Fossilized fashion and social sparkle. Dutch Bronze Age bracelets in context

2021 ◽  
pp. 43-110
Author(s):  
S. Arnoldussen ◽  
H. Steegstra

This contribution deals with the bronze bracelets found in the Netherlands that are datable between the Late Neolithic and the Middle Iron Age (n=176). We study their context (hoards, funerary contexts, settlements and stray finds), and we relate the specifics of their form and decoration to regional and supraregional traditions. First, we study their role as social signifiers (in reconstructions) of prehistoric identities across those scales, discussing how particular Bronze Age ‘costumes’ or ‘ornament sets’ may have been kept from graves and deposited in alternate ways. Then, we study later prehistoric arm-rings for their potential to indicate the scale, orientation and longevity of supraregional contact networks into which the later prehistoric communities of the Netherlands were integrated.

1978 ◽  
Vol 44 ◽  
pp. 219-308 ◽  
Author(s):  
John Hedges ◽  
David Buckley ◽  
C. Bonsall ◽  
I. A. Kinnes ◽  
J. C. Barrett ◽  
...  

SummaryThe Causewayed Enclosure at Orsett, Essex, was trial trenched in 1975 to determine the state of site preservation and confirm its postulated Neolithic date and site sequence. The enclosure consisted of three incomplete circuits of discontinuous ditch with an associated timber palisade slot lying inside and concentric to the middle ditch. Within the interior was an oval post hole structure of a contemporary date. Quantities of Mildenhall style pottery and flint artifacts of the mid third millennium b.c. were recovered from the primary ditch silts and other features. A small quantity of Late Neolithic/Early Bronze Age wares came from the secondary ditch silts and the interior.Later phases on the site were represented by unenclosed Early Iron Age occupation, a Middle Iron Age sub-rectangular enclosure and Saxon ring-ditch burials.


This paper describes the morphology of a small piece of the Chalk escarpment near Brook in east Kent, and reconstructs its history since the end of the Last Glaciation. The escarpment contains a number of steep-sided valleys, or coombes, with which are associated deposits of chalk debris, filling their bottoms and extending as fans over the Gault Clay plain beyond. Here the fans overlie radiocarbon-dated marsh deposits of zone II (10 000 to 8800 B.C.) of the Late-glacial Period. The debris fans were formed and the coombes were cut very largely during the succeeding zone III (8800 to 8300 B.C.). The fans are the products of frost-shattering, probably transported by a combination of niveo-fluvial action and the release of spring waters; intercalated seams of loess also occur. The molluscs and plants preserved in the Late-glacial deposits give a fairly detailed picture of local conditions. The later history of one of the coombes, the Devil’s Kneadingtrough, is reconstructed. The springs have effected virtually no erosion and have probably always emerged more or less in their present position. In the floor of the coombe the periglacial chalk rubbles of zone III are covered by Postglacial deposits, mainly hillwashes. They are oxidized and yield no pollen, but contain rich faunas of land Mollusca, which are presented in the form of histograms revealing changing local ecological and climatic conditions. During most of the Post-glacial Period, from the end of zone III until about the beginning of zone VIII, very little accumulation took place on the coombe floor. But below the springs there are marsh deposits which span much of this interval. They yield faunas of considerable zoogeographical interest. The approximate beginning of zone VII a (Atlantic Period) is reflected by a calcareous tufa, which overlies a weathering horizon, and represents an increase in spring flow. Two clearance phases are deduced from the molluscan record. The first may have taken place at least as early as the Beaker Period (Late Neolithic/earliest Bronze Age); the second is probably of Iron Age ‘A’ date. In Iron Age times the subsoil was mobilized and a phase of rapid hillwashing began. As a result the valley floor became buried by humic chalk muds. The prime cause of this process was probably the beginning of intensive arable farming on the slopes above the coombe; a possible subsidiary factor may have been the Sub-Atlantic worsening of climate. The muds yield pottery ranging in date from Iron Age ‘Kentish first A’ ( ca . 500 to ca . 300 B.C.) to Romano-British ware of the first or second centuries A.D. Evidence is put forward for a possible climatic oscillation from dry to wet taking place at about the time of Christ. In the later stages of cultivation, possibly in the Roman Era, the valley floor was ploughed and given its present-day form.


1990 ◽  
Vol 56 ◽  
pp. 179-245 ◽  
Author(s):  
D. G. Benson ◽  
J. G. Evans ◽  
G. H. Williams ◽  
T. Darvill ◽  
A. David ◽  
...  

Excavations of sites spanning the Beaker to early Roman periods at Stackpole Warren, Dyfed, are described. The sites are in an area of blown sand which enhanced their preservation and led to the separation of several horizons. The earliest is a buried soil beneath the blown sand which contained Mesolithic to Bronze Age artefacts. At site A, there was a roundhouse associated with Early Bronze Age pottery and dated to 1620±70 and 1400±70 BC uncal., and two other roundhouses, one possibly of Beaker age. After a period of soil formation, a ritual complex of Later Bronze Age date was established, this contemporary with the earliest besanding of the area; it included a stone setting of more than 2000 small stones, an alignment of small water-worn stones and a standing stone. A cremation gave a latest date of 940±70 BC uncal. Other Later Bronze Age activity is recorded at site G/J in the form of a rectangular enclosure, possibly unfinished.Late Iron Age to early Romano-British settlement was present at sites A and B, consisting of scatters of occupation debris, burnt mounds, cooking pits, hearths and houses, some of stone, some of timber, all taking place in an area being intermittently besanded.Peripheral to the religious and domestic sites, a field system was excavated. The earliest phase was a linear earthwork from which a C14 date of 400±70 BC uncal. was obtained from charcoal in the ditch. After the decay of this, rectangular fields with stone walls were laid out, one along the line of the erstwhile earthwork, this taking place around the end of the Iron Age as dated by C14 of charcoal directly beneath a wall to 90±70 BC uncal. Some of the fields had been cultivated by a succession of cross- and one-way-ploughing, others used for cattle.An assemblage of 763 flints included a few Mesolithic artefacts but was mostly of Late Neolithic and Bronze Age date. A succession of ceramic assemblages included a small Middle Neolithic group (4 vessels), two distinct Beaker groups, one early (Lanting and van der Waals steps 1–3 (8 vessels), one late (steps 3–6) (45 vessels), an Early Bronze Age group of collared urns (43 vessels) and a Later Bronze Age group (26 vessels).Environmental data was not prolific but there was a small quantity of animal bone, mostly cattle and sheep, and cereal grain, mostly barley with some wheat. Marine molluscs were present but sparsely utilized and there was no other indication of the exploitation of the coastal resources such as seals, birds, fish andiseaweed. Land Mollusca indicated open country from the Iron Age onwards when the record begins.The importance of the site is in the ritual complex from site A, the succession of Iron Age/Romano-British occupation horizons, the succession of ceramic assemblages, the field system and the fact that blown sand horizons have allowed the preservation and separation of the sequence much of which would have been at best conflated in to a single horizon or at worst destroyed. Otherwise, there is no evidence that the site was in any way special with regard to the relationship of human activity and sand deposition until the Middle Ages when the area was used as a rabbit warren. Nor was the coastal location important, at least as could be determined by the results. This was a representative of a succession of later prehistoric farming communities and their various domestic, ritual and sepulchral activities in lowland Dyfed.


1994 ◽  
Vol 1 (2) ◽  
pp. 124-125 ◽  
Author(s):  
Stephen Shennan

Lohof's paper represents an interesting and important attempt to analyse and interpret Late Neolithic and earlier Bronze Age burial practices in the Netherlands. His suggestions are of wide relevance, not least because the phenomena he discusses were widely distributed over much of Europe. In what follows I wish to raise a number of issues which I think need clarifying, in order to elicit his response.


The Holocene ◽  
2020 ◽  
Vol 30 (12) ◽  
pp. 1780-1800
Author(s):  
Alfredo Mayoral ◽  
Salomé Granai ◽  
Anne-Lise Develle ◽  
Jean-Luc Peiry ◽  
Yannick Miras ◽  
...  

We analysed the late-Holocene pedo-sedimentary archives of La Narse de la Sauvetat, a hydromorphic depression in the southern Limagne plain (central France), where chronologically accurate studies are scarce. The multi-proxy geoarchaeological and palaeoenvironmental analysis of two cores from different areas of the basin was carried out through sedimentological, geochemical, micromorphological and malacological investigations. Integration of these datasets supported by a robust radiocarbon-based chronology allowed discussion of socio-environmental interactions and anthropogenic impacts from Late Neolithic to Early Middle Ages. Until the Middle Bronze Age, there was no clear evidence of anthropogenic impact on soils and hydro-sedimentary dynamics of the catchment, but two peaks of high alluvial activity probably related to the 4.2 and 3.5 kyr. BP climate events were first recorded in Limagne. Significant anthropogenic impacts started in the Late Bronze Age with increased erosion of the surrounding volcanic slopes. However, a major threshold was reached c. 2600 cal BP with a sharp increase in the catchment erosion interpreted as resulting from strong anthropogenic environmental changes related to agricultural activities and drainage. This implies an anthropogenic forcing on soils and hydro-sedimentary systems much earlier than was usually considered in Limagne. These impacts then gradually increased during Late Iron Age and Roman periods, but environmental effects were certainly contained by progress in agricultural management. Late Antiquity environmental changes are consistent with regional trend to drainage deterioration in lowlands, but marked asynchrony in this landscape change suggests that societal factors implying differential land management were certainly predominant here.


1989 ◽  
Vol 55 (1) ◽  
pp. 89-134 ◽  
Author(s):  
William Britnell ◽  
Jenny Britnell ◽  
Timothy C. Darvill ◽  
Stephen Greep ◽  
Elizabeth Healey ◽  
...  

The report on partial rescue excavations of the Collfryn enclosure between 1980–82 presents a summary of the first large-scale investigation of one of the numerous semi-defensive cropmark and earthwork enclosure sites in the upper Severn valley in mid-Wales. Earlier prehistoric activity of an ephemeral nature is represented by a scattering of Mesolithic and Late Neolithic or early Bronze Age flintwork, and by a pit containing sherds of several different Beaker vessels. The first enclosed settlement, constructed in about the 3rd century bc probably consisted of three widely-spaced concentric ditches, associated with banks of simple dump construction, having a single gated entranceway on the downhill side. It covered an area of about 2.5 ha and appears to have been of a relatively high social status, and appropriate in size for a single extended-family group. This was subsequently reduced in about the 1st century bc to a double-ditched enclosure, by the recutting of the original inner ditch and the cutting of a new ditch immediately outside it. The habitation area between the 3rd and 1st centuries bc probably focused on timber buildings in the central enclosure of about 0.4 ha, whose gradually evolving pattern appears to have comprised between 3–4 roundhouses and 4–5 four-posters at any one time. Little excavation was undertaken between the outer ditches of the first phase settlement, but these are assumed to have been used as stock enclosures. A mixed farming economy is suggested by cattle, sheep/goat and pig remains, and remains of glume wheats, barley and oats. Industries included small-scale iron and bronze-working. The Iron Age settlement was essentially aceramic, although there are significant quantities of a coarse, oxidized ceramic probably representing salt traded from production centres in the Cheshire Plain. The entranceway was remodelled in about the late 1st or early 2nd, century AD by means of a timber-lined passage linked to a new gate on the line of the inner bank. There is equivocal evidence of continued occupation within the inner enclosure continuing until at least the mid-4th century AD, possibly at a comparatively low social level, associated with domestic structures of uncertain form sited on earlier roundhouse platforms, and including some four-posters and possible six-posters. Drainage ditches were dug across parts of the site during the Medieval and post-Medieval periods, which were associated with various structures, including a corn-drying kiln inserted into the inner enclosure bank in the 15th century.


1997 ◽  
Vol 63 ◽  
pp. 221-259 ◽  
Author(s):  
M. Parker Pearson ◽  
R.E. Sydes ◽  
S. Boardman ◽  
B. Brayshay ◽  
P.C. Buckland ◽  
...  

The Early Iron Age enclosures and associated sites on Sutton Common on the western edge of the Humberhead Levels contain an exceptional variety of archaeological data of importance not only to the region but for the study of later prehistory in the British Isles. Few other later prehistoric British sites outside the East Anglian fens and the Somerset Levels have thus far produced the quantity and quality of organically preserved archaeological materials that have been found, despite the small scale of the investigations to date. The excavations have provided an opportunity to integrate a variety of environmental analyses, of wood, pollen, beetles, waterlogged and carbonised plant remains, and of soil micromorphology, to address archaeological questions about the character, use, and environment of this Early Iron Age marsh fort. The site is comprised of a timber palisaded enclosure and a succeeding multivallate enclosure linked to a smaller enclosure by a timber alignment across a palaeochannel, with associated finds ranging in date from the Middle Bronze Age to the Roman and medieval periods. Among the four adjacent archaeological sites is an Early Mesolithic occupation site, also with organic preservation, and there is a Late Neolithic site beneath the large enclosure. Desiccation throughout the common is leading to the damage and loss of wooden and organic remains. It is hoped that the publication of these results, of investigations between 1987 and 1993, will lead to a fuller investigation taking place.


1999 ◽  
Vol 65 ◽  
pp. 17-46 ◽  
Author(s):  
Gordon J. Barclay

It is 50 years since Stuart Piggott excavated the prehistoric complex at Cairnpapple. At that time there were few excavated parallels in Scotland, and interpretation inevitably relied heavily on sites excavated in southern Britain. Much more locally relevant data are now available and the sequence at Cairnpapple can now be reassessed its regional context.Piggott identified five Periods, commencing with a stone setting, ‘cove’ and cremation cemetery of ‘Late Neolithic date’ around ‘c. 2500 B.C.’. Period II was a henge monument, consisting of a ‘circle’ of standing stones with ceremonial burials in association, and an encircling ditch with external bank – ‘Of Beaker date, probably c. 1700 B.C.’ Period III comprised the primary cairn, containing two cist-burials ‘Of Middle Bronze Age date, probably c. 1500 B.C.’ Period IV involved the doubling of the size of the cairn, with two cremated burials in inverted cinerary urns. ‘Of final Middle Bronze Age or native Late Bronze Age date, probably c. 1000 B.C.’ Period V comprised four graves ‘possibly Early Iron Age within the first couple of centuries A.D.’The present paper, using comparable material from elsewhere in Scotland, argues for a revised phasing: Phase 1, comprises the deposition of earlier Neolithic plain bowl sherds and axehead fragments with a series of hearths. This is comparable to ‘structured deposition’ noted on other sites of this period. Phase 2 involved the construction of the henge – a setting of 24 uprights – probably of timber rather than stone, probably followed by the encircling henge ditch and bank. The ‘cove’ is discussed in the context of comparable features in Scotland. Phase 3 saw the construction of a series of graves, including the monumental ‘North Grave’, which was probably encased in a cairn. Piggott's ‘Period III’ cairn was then built, followed by the ‘Period IV’ cairn. The urn burials seem likely to have been inserted into the surface of this mound, which may have covered a burial (since disturbed) on the top of the Period III mound, or may have been a deliberate monumentalising of it. The four graves identified as Iron Age by Piggott seem more likely to be from the early Christian period.The reassessment of Piggott's report emphasises the value of the writing of a clear, and sufficiently detailed account. While no report can be wholly objective it can be seen that Piggott's striving for objectivity led him to write a paper that is of lasting value.


The Holocene ◽  
2016 ◽  
Vol 27 (2) ◽  
pp. 181-196 ◽  
Author(s):  
Benjamin Dietre ◽  
Christoph Walser ◽  
Werner Kofler ◽  
Katja Kothieringer ◽  
Irka Hajdas ◽  
...  

Agro-pastoral activities in the past act as environmental legacy and have shaped the current cultural landscape in the European Alps. This study reports about prehistoric fire incidents and their impact on the flora and vegetation near the village of Ardez in the Lower Engadine Valley (Switzerland) since the Late Neolithic Period. Pollen, charcoal particles and non-pollen palynomorphs preserved in the Saglias and Cutüra peat bog stratigraphies were quantified and the results compared with the regional archaeological evidence. Anthropogenic deforestation using fire started around 4850 cal. BP at Saglias and aimed at establishing first cultivated crop fields (e.g. cereals) and small pastoral areas as implied by the positive correlation coefficients between charcoal particles and cultural and pastoral pollen indicators, as well as spores of coprophilous fungi. Pressure on the natural environment by humans and livestock continued until 3650 cal. BP and was followed by reforestation processes until 3400 cal. BP because of climatic deterioration. Thereafter, a new, continuous cultivation/pastoral phase was recorded for the Middle to Late Bronze Age (3400–2800 cal. BP). After rather minor human impact during the Iron Age and Roman Period, intensive agriculture was recorded for the Medieval Period. The area around Ardez was used for crop cultivation from about 1000 cal. BP until the start of the ‘Little Ice Age’ (600 cal. BP). Despite a land-use reorganisation, the following gradual decrease in agricultural activities led to the extant mixture of a cultivated, grazed and forested landscape in the Lower Engadine. In addition, this study demonstrates the excellent value of the fungus Gelasinospora as a highly local marker of past and today’s fire incidents, as well as of the use of micro-charcoals from pollen slides and macro-charcoals (>150 µm) from pollen sample residues for the reconstruction of short- and long-term fire histories.


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