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      On the Use of Biomineral Oxygen Isotope Data to Identify Human Migrants in the Archaeological Record: Intra-Sample Variation, Statistical Methods and Geographical Considerations

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          Abstract

          Oxygen isotope analysis of archaeological skeletal remains is an increasingly popular tool to study past human migrations. It is based on the assumption that human body chemistry preserves the δ 18O of precipitation in such a way as to be a useful technique for identifying migrants and, potentially, their homelands. In this study, the first such global survey, we draw on published human tooth enamel and bone bioapatite data to explore the validity of using oxygen isotope analyses to identify migrants in the archaeological record. We use human δ 18O results to show that there are large variations in human oxygen isotope values within a population sample. This may relate to physiological factors influencing the preservation of the primary isotope signal, or due to human activities (such as brewing, boiling, stewing, differential access to water sources and so on) causing variation in ingested water and food isotope values. We compare the number of outliers identified using various statistical methods. We determine that the most appropriate method for identifying migrants is dependent on the data but is likely to be the IQR or median absolute deviation from the median under most archaeological circumstances. Finally, through a spatial assessment of the dataset, we show that the degree of overlap in human isotope values from different locations across Europe is such that identifying individuals’ homelands on the basis of oxygen isotope analysis alone is not possible for the regions analysed to date. Oxygen isotope analysis is a valid method for identifying first-generation migrants from an archaeological site when used appropriately, however it is difficult to identify migrants using statistical methods for a sample size of less than c. 25 individuals. In the absence of local previous analyses, each sample should be treated as an individual dataset and statistical techniques can be used to identify migrants, but in most cases pinpointing a specific homeland should not be attempted.

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          Most cited references15

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          Stable carbon and oxygen isotopes in human tooth enamel: identifying breastfeeding and weaning in prehistory.

          This paper investigates the utility of stable carbon and oxygen isotopes in human dental enamel to reveal patterns of breastfeeding and weaning in prehistory. Enamel preserves a record of childhood diet that can be studied in adult skeletons. Comparing different teeth, we used delta13C to document the introduction of solid foods to infant diets and delta18O to monitor the decline of breastfeeding. We report enamel carbonate delta13C and delta18O of 33 first molars, 35 premolars, and 25 third molars from 35 burials from Kaminaljuyú, an early state in the valley of Guatemala. The skeletons span from Middle Preclassic through Late Postclassic occupations, ca. 700 B.C. to 1500 A.D. Sections of enamel were removed from each tooth spanning from the cusp to the cemento-enamel junction. Stable isotope ratios were measured on CO2 liberated by reaction of enamel with H3PO4 in an automated carbonate system attached to a VG Optima mass spectrometer. Within a skeleton, teeth developing at older ages are more enriched in 13C and more depleted in 18O than teeth developing at younger ages. Premolars average 0.5/1000 [corrected] higher in delta13C than first molars from the same skeleton (P = 0.0001), but third molars are not significantly enriched over premolars. The shift from first molars to premolars may be due to the shift to solid foods from lipid-rich milk. After 2 years, when premolars begin to mineralize, the delta13C in childhood diets did not change systematically. First molars and premolars are similar in delta18O, but third molars average 0.7/1000 [corrected] lower than first molars (P = 0.0001) and 0.5/1000 [corrected] lower than premolars (P = 0.0003). First molar and premolar delta18O is heavier, because breast milk is more enriched in 18O than is drinking water. Hence, many children continued to nurse during the period of premolar formation. Together, these results indicate that Kaminaljuyú children had begun to eat solid maize foods before the age of 2 years but continued to drink breast milk until much later.
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            Oxygen isotope fractionation between human phosphate and water revisited.

            The oxygen isotope composition of human phosphatic tissues (delta18OP) has great potential for reconstructing climate and population migration, but this technique has not been applied to early human evolution. To facilitate this application we analyzed delta18OP values of modern human teeth collected at 12 sites located at latitudes ranging from 4 degrees N to 70 degrees N together with the corresponding oxygen composition of tap waters (delta18OW) from these areas. In addition, the delta18O of some raw and boiled foods were determined and simple mass balance calculations were performed to investigate the impact of solid food consumption on the oxygen isotope composition of the total ingested water (drinking water+solid food water). The results, along with those from three, smaller published data sets, can be considered as random estimates of a unique delta18OW/delta18OP linear relationship: delta18OW=1.54(+/-0.09)xdelta18OP-33.72(+/-1.51)(R2=0.87: p [H0:R2=0]=2x10(-19)). The delta18O of cooked food is higher than that of the drinking water. As a consequence, in a modern diet the delta18O of ingested water is +1.05 to 1.2 per thousand higher than that of drinking water in the area. In meat-dominated and cereal-free diets, which may have been the diets of some of our early ancestors, the shift is a little higher and the application of the regression equation would slightly overestimate delta18OW in these cases.
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              The oxygen isotope relationship between the phosphate and structural carbonate fractions of human bioapatite.

              Oxygen isotope analysis of archaeological human dental enamel is widely used as a proxy for the drinking water composition (δ(18)O(DW)) of the individual and thus can be used as an indicator of their childhood place of origin. In this paper we demonstrate the robustness of structural carbonate oxygen isotope values (δ(18)O(C)) in bioapatite to preserve the life signal of human tooth enamel by comparing it with phosphate oxygen isotope values (δ(18)O(P)) derived from the same archaeological human tooth enamel samples.

                Author and article information

                Contributors
                Role: Editor
                Journal
                PLoS One
                PLoS ONE
                plos
                plosone
                PLoS ONE
                Public Library of Science (San Francisco, CA USA )
                1932-6203
                28 April 2016
                2016
                : 11
                : 4
                : e0153850
                Affiliations
                [1 ]McDonald Institute for Archaeological Research, University of Cambridge, Cambridge, United Kingdom
                [2 ]Department of Archaeology & Anthropology, University of Cambridge, Cambridge, United Kingdom
                Museo Nazionale Preistorico Etnografico 'L. Pigorini', ITALY
                Author notes

                Competing Interests: The authors have declared that no competing interests exist.

                Analyzed the data: EL TCO. Wrote the paper: EL TCO. Conceived the study: EL TCO. Collated the database: EL.

                Article
                PONE-D-15-52218
                10.1371/journal.pone.0153850
                4849641
                27124001
                77ea5aaa-c609-4e2b-a347-baa70524095e
                © 2016 Lightfoot, O’Connell

                This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

                History
                : 11 December 2015
                : 5 April 2016
                Page count
                Figures: 10, Tables: 2, Pages: 29
                Funding
                Funded by: funder-id http://dx.doi.org/10.13039/501100000267, Arts and Humanities Research Council;
                Award ID: AHRC 2006/127308
                Award Recipient :
                The authors have no support or funding to report.
                Categories
                Research Article
                Physical Sciences
                Chemistry
                Chemical Elements
                Oxygen
                Physical Sciences
                Physics
                Particle Physics
                Composite Particles
                Atoms
                Isotopes
                Social Sciences
                Archaeology
                Biology and Life Sciences
                Physiology
                Digestive Physiology
                Dentition
                Medicine and Health Sciences
                Physiology
                Digestive Physiology
                Dentition
                Physical Sciences
                Mathematics
                Statistics (Mathematics)
                Statistical Data
                Physical Sciences
                Chemistry
                Chemical Compounds
                Phosphates
                People and Places
                Geographical Locations
                Europe
                Research and Analysis Methods
                Mathematical and Statistical Techniques
                Statistical Methods
                Physical Sciences
                Mathematics
                Statistics (Mathematics)
                Statistical Methods
                Custom metadata
                All data files are available from the University of Cambridge data repository ( https://www.repository.cam.ac.uk/handle/1810/252773).

                Uncategorized
                Uncategorized

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