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New light on the Anglo-Saxon succession: two cemeteries and their dates.


Archaeologists in every country have problems arguing for and against cultural and demographic continuity. Key questions relating to migrations reflect on the past and present identities of peoples and nations, and can be answered differently according to current ideological perspectives and theories about the meaning of cultural variation. In Europe, this has been especially important in the interpretation of the character and impact of the transition from the Roman Empire to the early medieval 'barbarian' successor states, including Anglo-Saxon England (Hills 2003). The debate has fluctuated between the traditional scenario of large-scale population replacement (significant immigration or invasion) to explanations constructed in terms of changes in the material representation of identities driven by social, economic and political change (Hakenbeck 2007; Harke 2007; Hills 2003, 2007).

The chronology of Anglo-Saxon cemeteries is still largely based on artefact typology supported by small-scale radiocarbon dating. These provide loose frameworks which give social models much room for manoeuvre. There is a large-scale project now in hand to provide radiocarbon dates for burials of the sixth century onwards (Scull & Bayliss 1999) and other kinds of scientific evidence is increasingly deployed in these debates, such as genetics and isotopic variation, in the belief that these will provide some much needed objectivity. However, reliance on limited samples, sometimes analysed during early stages of the development of new techniques, can introduce misleading conclusions, sometimes with very wide implications for interpretation.

This paper illustrates the problem by means of a re-assessment of the chronology of two cemeteries in the Thames Valley, Queenford Farm and Wally Corner, Berinsfield, which both lie to the north of Dorchester-on-Thames in Oxfordshire, UK. Both were partially excavated in advance of gravel quarrying, respectively in 1972 and 1981, and in 1974 and 1975 (Chambers 1987; Boyle et al. 1995). Initially the cemeteries were designated as belonging to two different cultural traditions, Queenford Farm to the Romano-British tradition and Berinsfield to the Anglo-Saxon, according to burial practices which are usually seen as chronologically consecutive, and possibly representing ethnically distinct populations.

However, based on radiocarbon dating from Queenford Farm, and artefact chronology from Berinsfield, it was subsequently argued that both cemeteries were in use during the fifth and sixth centuries AD and were therefore at least partially contemporary. The possibility that Britons and Anglo-Saxons existed as neighbouring and contemporary communities has attracted considerable attention and has been used to support an argument that 'apartheid' existed in early Anglo-Saxon England (Booth et al. 2007: 226; Harke 2007: 16).

As in all attempts at the explanation of culture change, the structure of the debate is affected by the quality of the evidence. These two cemeteries have the potential to provide key evidence about replacement/interaction strategies between British and Anglo-Saxon populations, but the arguments that can be deployed depend directly on the precision with which they can be dated. In other words, it is essential first to examine how far these cemeteries really could have been contemporary.

The sites

The Thames Valley is an area with significant evidence for early Anglo-Saxon contact, with a number of cemeteries producing grave-goods of fifth-century type. This region has long been the subject of archaeological fieldwork and research relating to the early Anglo-Saxon period (Hawkes 1986; Booth et al. 2007). Around Dorchester a series of late Roman cemeteries have been partially investigated (Booth 2001) and to the south of Dorchester, the well known early fifth-century burials from Dyke Hills were found with both late Roman belt equipment and early Germanic brooches (Kirk & Leeds 1952-53).

The sites examined by us lie to the north of Dorchester-on-Thames, Oxon, UK (Figure 1), and were both excavated by the Oxford Archaeological Unit in advance of their destruction (Chambers 1987; Boyle et al. 1995). Maps of the Dorchester region show that up to and including 1960 little quarrying had taken place, whereas by 1975 extensive quarries had removed most of the archaeological evidence for both sites.

The Queenford Farm cemetery lay within a rectangular enclosure, identified in air photographs in the 1930s, to the west of Queenford Mill (Durham & Rowley 1972). Excavation in 1972 in advance of gravel quarrying identified 188 graves, of which 82 were excavated and further excavation took place in 1981 in advance of road construction, when a further 102 graves were identified, of which another 82 were excavated. Many other graves are known to have been destroyed through quarrying without record, and it was estimated that the cemetery could have originally contained over 2000 graves (Chambers 1987). The cemetery contained unfurnished inhumations laid out with heads to the west in rows within a rectangular enclosure. Late Roman pottery, mostly abraded sherds, occurred within grave-fills and features and as a scatter across the site. Iron coffin fittings and nails occurred in a number of burials. The only recorded grave-good is a double-sided bone comb of late Roman type. There is nothing in the burial rite to suggest this was other than a normal late Roman cemetery, which would be expected to have gone out of use before Anglo-Saxon burial practice became the norm in the region during the later fifth century AD. Five radiocarbon dates were obtained from human bone, one from the 1972 burials giving a date of 420+100 years (Durham & Rowley 1972: 37) and four from the 1981 burials, measured by liquid scintillation counting (HAR-5325, HAR-5350, HAR-5324, HAR-5351). These were calculated to give a group mean calibrated date at 1[sigma] of AD 530-550, 2[sigma] AD 430-630 (Chambers 1987: 58). Queenford Farm has been discussed in connection with the evidence for health and burial practice in late Roman and Anglo-Saxon cemeteries (Harman et al. 1981) and in most reviews of Roman burials in Britain, especially in Oxfordshire (Harman et al. 1978; Booth 2001).


Berinsfield is a modern settlement, built in the mid-twentieth century, but named after the Anglo-Saxon Birinus, first bishop of the West Saxons, whose see was at Dorchester (Boyle et al. 1995: 144). The cemetery at Wally Comer lies south-east of Berinsfield within a complex of prehistoric and Roman features, first identified in aerial photographs in the 1930s. It was excavated in 1974 and 1975 in advance of gravel quarrying. One hundred inhumation graves were excavated, containing 114 burials and four cremations, estimated as half to two-thirds of the original cemetery. Many of the graves contained grave-goods of typical Anglo-Saxon type, including weapons and jewellery, which can be dated typologically from the early/mid-fifth century AD to late sixth/early seventh century AD. A detailed report on the cemetery has been published which included specialist reports on finds and human remains (Boyle et al. 1995). It was argued that the site was polyfocal, and that family or household groups can be identified. The social and ethnic composition of this cemetery has been the subject of research by Heinrich Harke (Harke 1992, 1995), and more recently by Duncan Sayer (Sayer 2007). Harke argued that a difference between native and non-native males at Berinsfield was evidenced by a link between the presence or absence of weapons, and stature, and epigenetic traits suggesting familial groupings. However, the situation is complicated by the fact that there is also an age-related distinction, in that males buried without weapons were all over 30 years in age (Harke 1995: 69). The age-related difference is also reflected in diet (Privat et al. 2002: 787).

The distance between the two cemeteries as excavated appears to be approximately 600m, but may have been originally less as neither the southern edge of Wally Corner nor the northern edge of Queenford Farm was archaeologically defined. Aerial photographs suggest the unenclosed cemetery at Wally Comer extended south into areas quarried away without excavation (Boyle et al. 1995: 6). Most Anglo-Saxon cemeteries and all but the major urban Roman cemeteries were small, so it is not likely that the two sites originally formed part of one cemetery. At Queenford Farm, burial appears to have been originally contained within a rectangular ditched enclosure, as at other late Roman cemeteries, for example Church Piece, Warborough (Harman et al. 1978: Figure 1) and Wasperton, Warwickshire (Carver et al. 2009).

Osteological comparison of those buried at Berinsfield with local late Roman cemeteries including Queenford Farm (Harman in Boyle et al. 1995: 108) suggests those buried at Berinsfield were slightly taller but had lower life expectancy than the late Roman populations. At Queenford Farm females were relatively smaller than elsewhere and a higher proportion of child burials was found than in other local cemeteries of either period (Harman et al. 1981: 148-9). Both sites have been the subject of research into dietary patterns, involving successful collagen extraction and stable isotope analysis (Privat et al. 2002; Fuller et al. 2006). These studies suggest that the two populations were following different dietary practices. Overall, isotopic values for Berinsfield and Queenford Farm showed significant difference, with Queenford Farm higher in both [delta][sup.13]C and [delta][sup.15]N values (Berinsfield mean [delta][sup.13]C = -20.1 [+ or -] 0.2 [per thousand], mean [delta][sup.15]N = + 9.8 [+ or -] 0.8 [per thousand]; Queenford Farm mean [delta][sup.13]C = -19.6 [+ or -] 0.4 [per thousand], mean [delta][sup.15]N = +10.3 [+ or -] 0.8 [per thousand]; Student's t-test, p < 0.001 for both [delta][sup.13]C and [delta][sup.15]N). Furthermore, at Queenford Farto, sex-related differences were identified, whereas this was not the case at Berinsfield, where status differences in diet seemed more apparent. These two populations therefore appear different in several respects. However, Gowland's research on skeletal material across southern Britain from this time period, including these two cemeteries, concluded that osteological variation appeared to relate more to geographical rather than chronological separation, in this case between these Oxfordshire cemeteries and others from Hampshire (Gowland 2007).


We chose to date relatively late burials from Queenford Farm (on stratigraphical grounds) and early burials from Berinsfield (based on grave-good typology), in order to establish the degree, if any, of overlap. We selected adults, matching age and sex where possible, from burials where collagen has already been successfully extracted during the earlier stable isotopic analysis.

At Queenford Farm we sampled five burials from within the rectangular enclosure and therefore likely to be more representative of its main period of use (F32/32, F55/55, F56/56, F57/57, F36/217). We sampled the two burials from a small stratigraphically later enclosure (F10/196, F11/197) one of which was found with the only grave-good from the site, a late Roman bone comb, and one of the burials that cut the small enclosure, F106/256, which is stratigraphically the latest in this sequence. These three are likely to be amongst the latest burials from the cemetery and possibly of relatively higher status as they are distinguished by a separate mortuary enclosure. Further burials lay to the south of both enclosures, from where we sampled two burials (F 120/263, F44/225). At Berinsfield, the cemetery is divided into three overlapping phases, spanning the later fifth to early seventh centuries AD. We chose a total of ten graves: 20 and 64, the only two dated to Phase 1; 1 and 8, the only two dated to transitional Phase 1/2; and six from Phase 2 (5, 6, 18, 35, 73, 121).

Samples were AMS [sup.14]C dated by the Oxford Radiocarbon Accelerator Unit. Full details and results of all samples analysed are listed in Table 1. All samples dated were of rib fragments, save for two samples from Berinsfield (that from Grave 1 was a long bone fragment, and from Grave 64 was a skull fragment). We chose to use mainly rib fragments to minimise problems associated with the long turnover time associated with long bones (Hedges et al. 2007). One of the samples (Berinsfield F56/56) was dated twice as part of ORADS standard procedure, with very good agreement between the repeat measurements. All Queenford Farm samples were successfully dated, but only five of the Berinsfield samples yielded sufficient collagen for a date. The dates were calibrated using OxCal 4.0.5 (Bronk Ramsey 1995, 2001) using the IntCal04 atmospheric curve (Reimer et al. 2004), and statistical analyses of the dates were carried out using Calib v5.0.1 (Stuiver et al. 2005).

Results (Table 1, Figure 2)

The calibrated dates of the ten samples from Queenford Farto span AD 254-426 (1[sigma]), AD 240-531 (2[sigma]), which is typical of that expected for a Late Roman cemetery. This range is substantially earlier than that obtained from the original five dates. Given the advances in dating techniques and sample pre-treatment chemistry over the last 20 years, we consider that the new dates obtained are likely to be the more accurate. Overall, the patterning of the dates parallels that of the stratigraphy. Those of the seven burials assumed to be from the main phase form a tight group (AD254-408, 1[sigma]), with the two burials from the small enclosure (F10/grave 196 and F 11/grave 197) giving slightly later dates, and the date of the stratigraphically latest burial cutting the small enclosure (F 106/grave 256) is marginally later still (Table 1, Figure 2). However, this pattern is not statistically significant, as all dates are the same at the 95% confidence level (t = 5.900188, [X.sub.i]2(p < 0.05) = 18.3, df = 10). The only grave-good, the double-sided bone comb buried with grave 197, was dated to the late fourth century AD by reference to burials with combs from Lankhills, Winchester (Clarke 1979: 368-9).

The five successful dates from Berinsfield are of Graves 20 (Phase 1), 1 and 8 (Phase 1/2), and 35 and 73 (Phase 2), and, when calibrated, span AD 385-538 (l[sigma]), AD 344-556 (2[sigma]). The dates of Graves 1 and 8 (Phase 1/2) are slightly earlier than those of Graves 20, 35 and 73 (Figure 2), however, all five dates are statistically the same at the 95% confidence level (t = 5.520201, [X.sub.i]2(p < 0.05) = 9.49, df = 4). These [sup.14]C dates are not inconsistent with those suggested on the basis of artefact typology. At Berinsfield, Grave 20 was dated to Phase 1, up to the last quarter of the fifth century, on the basis of the spearhead of Swanton type B2, a type unusual for Britain with a central rib, a feature current in continental and Scandinavian spearheads of the Roman Iron Age. Grave 1 contained an early type of shield boss, Grave 8 an equal-armed brooch, both graves were assigned either to Phase 1 or to an early part of Phase 2, i.e. up to the end of the fifth century. The equal-armed brooch is an unusual type, put late in the sequence by Evison as ah insular development (Evison 1977). This brooch has an exact parallel in a brooch found by a metal-detectorist at Burnham Market in north Norfolk (Gurney 2002). Grave 35 contained a pair of disc brooches, and 73 a pair of five scroll saucer brooches, both assigned to Phase 2, late fifth- mid-sixth century. The analysis of glass beads by Brugmann (Brugmann 2004) puts Grave 8 in her Phase A, AD 450-580, and Grave 35 in A2, AD 480-580.

The main divergence between the radiocarbon and artefact dates is that Grave 20, attributed to Phase 1, is indistinguishable from Graves 73 and 35 (Phase 2), and is later than Graves 1 and 8, both attributed to Phase 1 or 2, so perhaps Grave 20 now should be re-assigned to Phase 2.


The [sup.14]C results give a date range which covers all of the fifth century and the first half of the sixth. While this is compatible with current typological chronologies it provides some encouragement to reconsider the mid-fifth-century starting point often assumed for Anglo-Saxon burials, as do [sup.14]C dates recently produced for apparently Anglo-Saxon cremations at Wasperton which are also earlier than expected (Carver et al. 2009: 47).


Some cemeteries from southern England have produced radiocarbon dates spanning from the Roman period into the seventh century AD. At Cannington, Somerset, the main use of the cemetery was dated to between the late third and late seventh centuries AD (Rahtz et al. 2000:391), while at Tolpuddle Bali, Dorset, radiocarbon dates suggested use between c. AD 400-700 (Hearne & Birbeck 1999: 227). However, Somerset and west Dorset lie outside the area of initial Anglo-Saxon contact and settlement, and basic continuity of the local British populations might be assumed there, so continuity of 'Romano-British' type cemeteries is not surprising. Only Wasperton, in the Avon Valley in Warwickshire (Carver et al. 2009) has so far produced convincing evidence for both Romano-British and Anglo-Saxon burials succeeding each other within the same cemetery.

The main period of use at Queenford Farm is in the fourth and into the fifth century AD, whilst at Berinsfield it is in the fifth into the sixth century AD, suggesting that the two cemeteries succeeded each other. The seven early samples from Queenford Farm and the three later ones from Berinsfield are different at the 95% confidence level (t = 55.19817, [X.sub.i]2(p < 0.05) = 19.7, df = 11). Although we obtained no overlapping dates from the two cemeteries, the later dates from Queenford Farm and the early dates from Berinsfield all fall in the early fifth century: the three later Queenford Farm dates and the two earliest dates from Berinsfield are the same at the 95% confidence level (t = 3.97433, [X.sub.i] 2(p < 0.05) = 9.49, df = 4, OxA-V-2217-55, OxA-V-2218-6, OxA-V-2217-57, OXA-18187 and OxA-18188). This suggests that while the use of one cemetery followed the other, there may have been a brief transition period when both were in use.

It is important to note that calibrating the dates is complicated by the shape of the calibration curve for this period, in which a steep slope (AD 400-440) is preceded by radiocarbon wiggles (AD 250-300 and AD 350-370) and followed by a plateau (AD 440-530). But whilst the calibration curve can distort things, it does not alter the fact that these two occupations are successive. That said, there seems to be a degree of closeness, witnessed by the determinations (one from each site: OxA-18188 and OxA-X-2217-57) that appear close to one another in the steeper section of the calibration curve between the bulk of the two results (between c. AD 400-440), spanning the period between the two cemeteries.

How does this result affect current views of the Roman-Saxon transition in Britain? Discussion of genetic evidence is currently focused on the extent to which modern English populations are descended from Germanic immigrants rather than native British (e.g. Weale et al. 2002; Capelli et al. 2003). Alternative proposals are for violent population replacement, or for interaction and acculturation, or, most recently, apartheid, allowing a few dominant males to 'father the nation' (Thomas et al. 2006). The genetic replacement model aligns with traditional historical accounts, while archaeological interpretations have for some decades favoured ah acculturation model. The 'apartheid' model is an attempt to reconcile these two, by showing how a relatively small incoming dominant male population could be ancestral to a majority of the later population.

If Queenford Farm and Berinsfield were contemporary, this would provide evidence for the survival of a Romano-British population in the Thames Valley into the sixth century AD, and also for separation of the two populations, probably native and immigrant, or perhaps pagan and Christian, in burial. If the cemeteries do not overlap in date, we see two consecutive cemeteries in close proximity, implying that cultural factors operating on one community might have played as strong a role in change as population replacement. In either case, these cemeteries provide a rare opportunity for comparison between two successive populations in the same place, not many generations apart, but with different burial practices.


The [sup.14]C dates for our samples broadly confirm conventional wisdom in separating late Roman from early Anglo-Saxon burials. They do not support the earlier [sup.14]C dates which suggested Queenford Farm continued in use as late as the sixth century AD. Instead, they indicate that the main use of this site lay within the fourth century AD, whereas the sampled burials from Berinsfield belong to the fifth and sixth centuries AD. This distinction in date corresponds to expectation for the chronological sequence from late Roman to early Anglo-Saxon. It appears therefore that these two cemeteries do not provide evidence for long term co-existence of two separate populations, and thus provide no support for the 'apartheid' model in early Anglo-Saxon England. However, there is both artefactual and 14C evidence for a contiguous succession in the first half of the fifth century. The bone comb from Queenford Farm and the supporting arm brooch from Berinsfield Grave 64 could both date to the later fourth or early fifth centuries. The [sup.14]C dates thus allow for a succession without hiatus between the end of the Queenford Farm sequence and the start of Berinsfield during the first part of the fifth century. The start of a new cemetery at Berinsfield demonstrates a new approach to burial, focusing on grave furnishings. It came into use while the last burials at Queenford Farm were taking place. Changes in burial practice and in the location of cemeteries have happened often within recorded history without a major population change, and we could be seeing such a shift here, with a move by the local population over a generation from one burial site to the other. However, the continental influence apparent within the Berinsfield grave assemblages does support arguments for new arrivals, while the biological evidence, even if not securely linked to ethnic origins, at least suggests some significant differences (for example in diet and stature) between the two populations.

Although we have demonstrated the weakness of the basis for arguing that these two sites were contemporary, this should not be seen as an argument against the deployment of scientific evidence in relation to population history, but instead as a call for the use of a range of precise techniques applied to larger samples which do have the potential to provide new answers to old questions.


This project was supported by a NERC ORADS grant 2006/2/6. Permission to resample the bones was kindly given by Alison Roberts and the curators of the Ashmolean Museum, Oxford (Berinsfield) and Christiane Jeuckens, Manager of the Oxfordshire Museums Resource Centre (Queenford Farm). We are grateful to the Oxford Archaeological Unit Ltd. for permission to reproduce Figure 1. Thanks to Cameron Petrie, Marc Vander Linden and Tom Higham for their assistance with interpretation of the dates, and the editor and two referees for helpful comments. TO'C is grateful to the Wellcome Trust for financial support.

Received: 30 January 2009; Accepted: 1 March 2009; Revised: 13 March 2009


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C.M. Hills & T.C. O'Connell *

* Department of Archaeology, University of Cambridge, Downing Street, Cambridge CB2 3DZ, UK
Table 1. Results of all samples analysed.

Sample details Site Phase Sex Age

Grave 20 Berinsfield 1 M 45+

Grave 64 Berinsfield 1 ? 1-1.5

Grave 1 Berinsfield 1/2 M 20-25

Grave 8 Berinsfield 1/2 F 25-30

Grave 35 Berinsfield 2 ? 11-12

Grave 73 Berinsfield 2 F 20-25

Grave 121 Berinsfield 2 M adult

Grave 5 Berinsfield 2 F 20-25

Grave 6 Berinsfield 2 M 25-30

Grave 18 Berinsfield 2 F 17-23

F32/grave 32 Queenford Farm M 35-40

F55/grave 55 Queenford Farm M 25-30

F56/grave 56 Queenford Farm F 20-25

F56/grave 56 Queenford Farm F 20-25

F57/grave 57 Queenford Farm F 20-25 rib

F36/grave 217 Queenford Farm F 35-40

F44/grave 225 Queenford Farm M 20-25

F120/grave 263 Queenford Farm M 45+

F10/grave 196 Queenford Farm late F 20-25

F11/grave 197 Queenford Farm late F 40+

F106/grave 256 Queenford Farm latest M 20-24

Sample details Bone type Date code

Grave 20 rib OxA-18186

Grave 64 skull frag

Grave 1 long bone OxA-18187

Grave 8 rib OxA-18188

Grave 35 rib OxA-18189

Grave 73 rib OxA-18214

Grave 121 rib

Grave 5 rib

Grave 6 rib

Grave 18 rib

F32/grave 32 rib OxA-V-2217-49

F55/grave 55 rib OxA-V-2217-50

F56/grave 56 rib 0~1-V-2217-51

F56/grave 56 rib OxA-V-2217-52

F57/grave 57 OxA-V-2217-53 1708 [+ or -] 28

F36/grave 217 rib OxA-V 2217-54

F44/grave 225 rib OxA-V 2217-56

F120/grave 263 rib OxA-17353

F10/grave 196 rib OxA-V 2217-55

F11/grave 197 rib OxA-V 2218-6

F106/grave 256 rib OxA-V 2217-57

Sample details [sup.14]C date yr BP Calibrated date 1[sigma]

Grave 20 1565 [+ or -] 24 AD 435 (49.5%) AD 492
 AD 508 (9.3%) AD 519
 AD 528 (9.4%) AD 538

Grave 64 failed

Grave 1 1614 [+ or -] 25 AD 406 (32.2%) AD 440
 AD 486 (36.0%) AD 532

Grave 8 1635 [+ or -] 26 AD 385 (59.9%) AD 434
 AD 494 (6.4%) AD 506
 AD 522 (1.9%) AD 526

Grave 35 1583 [+ or -] 25 AD 430 (26.4%) AD 465
 AD 482 (41.8%) AD 533

Grave 73 1569 [+ or -] 29 AD 434 (47.8%) AD 493
 AD 506 (11.9%) AD 521
 AD 526 (8.5%) AD 537

Grave 121 failed

Grave 5 failed

Grave 6 failed

Grave 18 failed

F32/grave 32 1686 [+ or -] 29 AD 267 (2.6%) AD 271
 AD 336 (6S.6%) AD 406

F55/grave 55 1731 [+ or -] 29 AD 254 (68.2%) AD 344

F56/grave 56 1692 -F 28 AD 264 (6.7%) AD 274
 AD 334 (61.5%) AD 400

F56/grave 56 1683 ?- 28 AD 337 (68.2%) AD 408

F57/grave 57 AD 260 (16.9%) AD 282 AD 255 (95.4%) AD 405
 AD 324 (51.3%) AD 386

F36/grave 217 1711 [+ or -] 29 AD 260 (19.1%) AD 284
 AD 323 (49.1%) AD 385

F44/grave 225 1703 [+ or -] 28 AD 261 (14.2%) AD 280
 AD 326 (54.0%) AD 391

F120/grave 263 1710 [+ or -] 29 AD 260 (18.2%) AD 282
 AD 324 (50.0%) AD 385

F10/grave 196 1671 [+ or -] 28 AD 344 (68.2%) AD 414

F11/grave 197 1676 [+ or -] 26 AD 344 (68.2%) AD 409

F106/grave 256 1654 [+ or -] 29 AD 350 (12.6%) AD 368
 AD 380 (55.6%) AD 426

Sample details Calibrated date 2[sigma]

Grave 20 AD 426 (95.4%) AD 552

Grave 64

Grave 1 AD 396 (95.4%) AD 535

Grave 8 AD 344 (76.0%) AD 466
 AD 480 (19.4%) AD 534

Grave 35 AD 420 (95.4%) AD 540

Grave 73 AD 421 (95.4%) AD 556

Grave 121

Grave 5

Grave 6

Grave 18

F32/grave 32 AD 258 (16.8%) AD 298
 AD 318 (78.6%) AD 420

F55/grave 55 AD 240 (95.4%) AD 390

F56/grave 56 AD 257 (20.0%) AD 300
 AD 318 (75.4%) AD 416

F56/grave 56 AD 258 (14.3%) AD 296
 AD 321 (81.1%) AD 421

F57/grave 57

F36/grave 217 AD 253 (95.4%) AD 402

F44/grave 225 AD 255 (95.4%) AD 410

F120/grave 263 AD 254 (95.4%) AD 404

F10/grave 196 AD 259 (9.0%) AD 295
 AD 321 (86.4%) AD 429

F11/grave 197 AD 259 (8.6%) AD 284
 AD 322 (86.8%) AD 425

F106/grave 256 AD 260 (3.4%) AD 282
 AD 324 (85.9%) AD 440
 AD 486 (6.0%) AD 531
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Title Annotation:Research
Author:Hills, C.M.; O'Connell, T.C.
Article Type:Report
Geographic Code:4EUUK
Date:Dec 1, 2009
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