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      Quantitative assessment of Pb sources in isotopic mixtures using a Bayesian mixing model

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          Abstract

          Lead (Pb) isotopes provide valuable insights into the origin of Pb within a sample, typically allowing for reliable fingerprinting of their source. This is useful for a variety of applications, from tracing sources of pollution-related Pb, to the origins of Pb in archaeological artefacts. However, current approaches investigate source proportions via graphical means, or simple mixing models. As such, an approach, which quantitatively assesses source proportions and fingerprints the signature of analysed Pb, especially for larger numbers of sources, would be valuable. Here we use an advanced Bayesian isotope mixing model for three such applications: tracing dust sources in pre-anthropogenic environmental samples, tracking changing ore exploitation during the Roman period, and identifying the source of Pb in a Roman-age mining artefact. These examples indicate this approach can understand changing Pb sources deposited during both pre-anthropogenic times, when natural cycling of Pb dominated, and the Roman period, one marked by significant anthropogenic pollution. Our archaeometric investigation indicates clear input of Pb from Romanian ores previously speculated, but not proven, to have been the Pb source. Our approach can be applied to a range of disciplines, providing a new method for robustly tracing sources of Pb observed within a variety of environments.

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          Low-Level Environmental Lead Exposure and Children’s Intellectual Function: An International Pooled Analysis

          Lead is a confirmed neurotoxin, but questions remain about lead-associated intellectual deficits at blood lead levels < 10 μg/dL and whether lower exposures are, for a given change in exposure, associated with greater deficits. The objective of this study was to examine the association of intelligence test scores and blood lead concentration, especially for children who had maximal measured blood lead levels < 10 μg/dL. We examined data collected from 1,333 children who participated in seven international population-based longitudinal cohort studies, followed from birth or infancy until 5–10 years of age. The full-scale IQ score was the primary outcome measure. The geometric mean blood lead concentration of the children peaked at 17.8 μg/dL and declined to 9.4 μg/dL by 5–7 years of age; 244 (18%) children had a maximal blood lead concentration < 10 μg/dL, and 103 (8%) had a maximal blood lead concentration < 7.5 μg/dL. After adjustment for covariates, we found an inverse relationship between blood lead concentration and IQ score. Using a log-linear model, we found a 6.9 IQ point decrement [95% confidence interval (CI), 4.2–9.4] associated with an increase in concurrent blood lead levels from 2.4 to 30 μg/dL. The estimated IQ point decrements associated with an increase in blood lead from 2.4 to 10 μg/dL, 10 to 20 μg/dL, and 20 to 30 μg/dL were 3.9 (95% CI, 2.4–5.3), 1.9 (95% CI, 1.2–2.6), and 1.1 (95% CI, 0.7–1.5), respectively. For a given increase in blood lead, the lead-associated intellectual decrement for children with a maximal blood lead level < 7.5 μg/dL was significantly greater than that observed for those with a maximal blood lead level ≥7.5 μg/dL (p = 0.015). We conclude that environmental lead exposure in children who have maximal blood lead levels < 7.5 μg/dL is associated with intellectual deficits.
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            Best practices for use of stable isotope mixing models in food-web studies

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              The Nubase evaluation of nuclear and decay properties

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                Author and article information

                Contributors
                j.longman@soton.ac.uk
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                18 April 2018
                18 April 2018
                2018
                : 8
                : 6154
                Affiliations
                [1 ]ISNI 0000000121965555, GRID grid.42629.3b, Department of Geography and Environmental Sciences, , Northumbria University, ; Newcastle-upon-Tyne, NE1 8ST United Kingdom
                [2 ]School of Ocean and Earth Sciences, University of Southampton, National Oceanography Centre, Waterfront Campus, Southampton, SO14 3ZH United Kingdom
                [3 ]ISNI 0000 0004 1937 1389, GRID grid.418333.e, Romanian Academy, Institute of Speleology, ; Clinicilor 5, Cluj-Napoca, Romania
                [4 ]EcoIsoMix.com, Corvallis, Oregon, USA
                [5 ]ISNI 0000 0001 2112 9282, GRID grid.4444.0, CNRS, Université Grenoble Alpes, Institut des Sciences de la Terre, ; UMR 5275 CNRS Grenoble, France
                [6 ]Institut de Physique du Globe de Paris, Université Sorbonne Paris Cité, CNRS UMR 7154 Paris, France
                [7 ]ISNI 0000 0004 1937 1397, GRID grid.7399.4, Faculty of Biology and Geology, , University Babeş-Bolyai, ; 1M. Kogălniceanu str., 400084 Cluj-Napoca, Romania
                Author information
                http://orcid.org/0000-0002-2725-2617
                http://orcid.org/0000-0001-9730-0007
                Article
                24474
                10.1038/s41598-018-24474-0
                5906678
                29670142
                c20d8f58-47e8-4cb2-a9ea-8c7985eb6ec0
                © 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
                : 31 January 2018
                : 26 March 2018
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