2018
DOI: 10.1111/arcm.12361
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Lead Isotope Analysis of Tooth Enamel from a Viking Age Mass Grave in Southern Britain and the Constraints it Places on the Origin of the Individuals

Abstract: Lead analysis of tooth enamel from individuals recovered from a Viking Age burial pit in southern England provides further evidence for their childhood origins outside Britain. All except one of the men have very low Pb concentrations that exclude anthropogenic Pb exposure. Strontium and oxygen isotope compositions identify a core group of men who have Pb isotope compositions of 208Pb/206Pb = 2.065 ± 0.021 (n = 20, 2SD) that, when compared with data from European soils, appear to exclude a childhood in the Sca… Show more

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Cited by 10 publications
(4 citation statements)
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“…In Britain, most individuals recovered from the late Viking Age sites of Ridgway Hill, Dorset, and St. John’s College, Oxford 13 show ancestries typical of those seen in Viking Age southern Scandinavia, suggesting that those executed could have been predominantly migrants or members of Viking raiding parties from Scandinavia (Figure 4g). In agreement with these genetic ancestry profiles, strontium and oxygen analyses of the individuals from Ridgway Hill and St. John’s College have suggested childhood origins outside of Britain, and potentially in peninsular Scandinavia, particularly the island of Öland 63,64 , or parts of northern continental Europe 65 . Notably, VK166 (SK 1891) from St. John’s College is a slight outlier in terms of both genetic ancestry, which is best explained by groups from Iron Age Austria, France, and Germany and Sarmatian-related populations from Russia, and the stable isotope analysis, where the oxygen results are suggest a more continental origin and the strontium suggests he spent his childhood on more radiogenic geology.…”
Section: Resultsmentioning
confidence: 62%
“…In Britain, most individuals recovered from the late Viking Age sites of Ridgway Hill, Dorset, and St. John’s College, Oxford 13 show ancestries typical of those seen in Viking Age southern Scandinavia, suggesting that those executed could have been predominantly migrants or members of Viking raiding parties from Scandinavia (Figure 4g). In agreement with these genetic ancestry profiles, strontium and oxygen analyses of the individuals from Ridgway Hill and St. John’s College have suggested childhood origins outside of Britain, and potentially in peninsular Scandinavia, particularly the island of Öland 63,64 , or parts of northern continental Europe 65 . Notably, VK166 (SK 1891) from St. John’s College is a slight outlier in terms of both genetic ancestry, which is best explained by groups from Iron Age Austria, France, and Germany and Sarmatian-related populations from Russia, and the stable isotope analysis, where the oxygen results are suggest a more continental origin and the strontium suggests he spent his childhood on more radiogenic geology.…”
Section: Resultsmentioning
confidence: 62%
“…[ 47 53 ]. The values exhibited by both populations also contrast with those recorded in enamel from individuals who had migrated to temperate locations from regions with a cold climate, such as the migrant individuals of Early Medieval date excavated in Dorset, England or Dublin, Ireland ( figure 2 ) [ 48 51 ].…”
Section: Discussionmentioning
confidence: 99%
“…As a consequence of the above factors, oxygen isotope analysis of enamel from human populations is useful for making broader scale distinctions, for differentiating individuals who originate from regions of much colder climate and have very low δ 18 O carbonate values, (<24.5‰, or δ 18 O phosphate VSMOW values < 15.5‰) from those who sourced their childhood dietary resources from temperate locations e.g. [47][48][49][50][51][52][53].…”
Section: δ 18 O Carbonate and δ 13 C Carbonate Analysismentioning
confidence: 99%
“…The regional designations in Figure 1 were created to limit the use of current political boundaries and the problematic use of ethnic identifiers for past geo-political zones, while also incorporating some of the environmental and geological variation across Europe. The zonation resulted from plotting the sites to look for spatial clustering and adjusting these with δ 18 O and 87/86 Sr isoscapes (Evans et al, 2010, 2012, 2018; Bataille et al, 2020), as well as cultural factors such as grave good styles and linguistic aspects (for details see Leggett et al, 2021).…”
Section: Methodsmentioning
confidence: 99%