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      Tracing intensive fish and meat consumption using Zn isotope ratios: evidence from a historical Breton population (Rennes, France)

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          Abstract

          Here we report Sr and Zn isotope ratios of teeth of medieval to early modern Breton people a population whose diet is known from historical, archeological and collagen isotope data. Most of the population, buried in the Dominican convent of Rennes, France, consists of parliamentary nobles, wealthy commoners and ecclesiastics, who had a diet rich in animal products. Our aim is to assess how the Zn isotope ratios of their teeth compare to those of other French historical populations previously studied, which were characterized by cereal-based diets, and those of modern French individuals, who daily eat animal products. We describe a clear offset (∼0.35‰) between local and non-local human individuals in Zn isotope ratios. The δ 66Zn tooth values of local individuals overlap that of modern French people, and are lower than those of local carnivores. Non-local δ 66Zn values are similar to those of historical individuals analyzed previously. We conclude the lower Zn isotope ratios of local humans relative to the associated fauna can be explained by the consumption of carnivorous fish and pork, in agreement with historical, zooarchaeological and collagen (C, N, S) isotope data. Zn isotopes could therefore be a tracer of fish and/or substantial meat consumption in ancient populations.

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          Nitrogen isotopes and the trophic level of humans in archaeology

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            Dietary factors influencing zinc absorption.

            Marginal zinc deficiency and suboptimal zinc status have been recognized in many groups of the population in both less developed and industrialized countries. Although the cause in some cases may be inadequate dietary intake of zinc, inhibitors of zinc absorption are most likely the most common causative factor. Phytate, which is present in staple foods like cereals, corn and rice, has a strong negative effect on zinc absorption from composite meals. Inositol hexaphosphates and pentaphosphates are the phytate forms that exert these negative effects, whereas the lower phosphates have no or little effect on zinc absorption. The removal or reduction of phytate by enzyme (phytase) treatment, precipitation methods, germination, fermentation or plant breeding/genetic engineering markedly improves zinc absorption. Iron can have a negative effect on zinc absorption, if given together in a supplement, whereas no effect is observed when the same amounts are present in a meal as fortificants. Cadmium, which is increasing in the environment, also inhibits zinc absorption. The amount of protein in a meal has a positive effect on zinc absorption, but individual proteins may act differently; e.g., casein has a modest inhibitory effect of zinc absorption compared with other protein sources. Amino acids, such as histidine and methionine, and other low-molecular-weight ions, such as EDTA and organic acids (e.g., citrate), are known to have a positive effect on zinc absorption and have been used for zinc supplements. Knowledge about dietary factors that inhibit zinc absorption and about ways to overcome or remove these factors is essential when designing strategies to improve the zinc nutrition of vulnerable groups.
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              Carbon and nitrogen stable isotope analysis of northwest European horse bone and tooth collagen, 40,000BP–present: Palaeoclimatic interpretations

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                Author and article information

                Contributors
                klervia_jaouen@eva.mpg.de
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                22 March 2018
                22 March 2018
                2018
                : 8
                : 5077
                Affiliations
                [1 ]ISNI 0000 0001 2159 1813, GRID grid.419518.0, Department of Human Evolution, , Max Planck Institute for Evolutionary Anthropology, ; Leipzig, Germany
                [2 ]INRAP, Cesson-Sévigné, France
                [3 ]ISNI 0000 0001 0723 035X, GRID grid.15781.3a, AMIS, UMR 5288, , Université Paul Sabatier, ; Toulouse, France
                [4 ]ISNI 0000000121885934, GRID grid.5335.0, Department of Earth Sciences, , University of Cambridge, ; Cambridge, United Kingdom
                [5 ]ISNI 0000 0001 2308 1657, GRID grid.462844.8, CNRS/MNHN/Sorbonne Universités, ; UMR 7209 Paris, France
                [6 ]ISNI 0000 0004 0638 3479, GRID grid.414295.f, Department of Forensic Medicine, , CHU Toulouse Rangueil, ; Toulouse, France
                [7 ]ISNI 0000 0004 1936 7494, GRID grid.61971.38, Department of Archaeology, , Simon Fraser University, ; Vancouver, Canada
                [8 ]ISNI 0000 0001 2190 1447, GRID grid.10392.39, Department of Geosciences, , University of Tübingen, ; Tübingen, Germany
                Article
                23249
                10.1038/s41598-018-23249-x
                5864724
                29568045
                2303e62a-3644-410b-bebf-2ea1073281e0
                © The Author(s) 2018

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 2 October 2017
                : 8 March 2018
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