<sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and Risks

During the last forty years, the use of strontium isotopes in archaeology and biogeochemical research has spread widely. These isotopes, alone or in combination with others, can contribute to trace past and present environmental conditions. However, the interpretation of the isotopic values of stron...

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Main Authors: Mattia Rossi, Paola Iacumin, Gianpiero Venturelli
Format: Article
Language:English
Published: MDPI AG 2024-01-01
Series:Quaternary
Subjects:
Online Access:https://www.mdpi.com/2571-550X/7/1/6
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author Mattia Rossi
Paola Iacumin
Gianpiero Venturelli
author_facet Mattia Rossi
Paola Iacumin
Gianpiero Venturelli
author_sort Mattia Rossi
collection DOAJ
description During the last forty years, the use of strontium isotopes in archaeology and biogeochemical research has spread widely. These isotopes, alone or in combination with others, can contribute to trace past and present environmental conditions. However, the interpretation of the isotopic values of strontium is not always simple and requires good knowledge of geochemistry and geology. This short paper on the use of strontium isotopes is aimed at those who use this tool (archaeologists, but not only) but who do not have a thorough knowledge of mineralogy, geology, and geochemistry necessary for a good understanding of natural processes involving these isotopes. We report basic knowledge and suggestions for the correct use of these isotopes. The isotopic characteristics of bio-assimilable strontium depend not so much on the isotopic characteristics of the bulk rock as, rather, on those of its more soluble minerals. Before studying human, animal and plant remains, the state of conservation and any conditions of isotopic pollution should be carefully checked. Samples should be collected according to random sampling rules. The data should be treated by a statistical approach. To make comparisons between different areas, it should be borne in mind that the study of current soils can be misleading since the mineralogical modification of soil over time can be very rapid.
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spelling doaj.art-eb664a423fd14dd8a497cce1582fa74b2024-03-27T14:01:53ZengMDPI AGQuaternary2571-550X2024-01-0171610.3390/quat7010006<sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and RisksMattia Rossi0Paola Iacumin1Gianpiero Venturelli2Department of Chemical, Life and Environmental Sustainability Sciences, Earth Sciences Section, University of Parma, 43100 Parma, ItalyDepartment of Chemical, Life and Environmental Sustainability Sciences, Earth Sciences Section, University of Parma, 43100 Parma, ItalyDepartment of Chemical, Life and Environmental Sustainability Sciences, Earth Sciences Section, University of Parma, 43100 Parma, ItalyDuring the last forty years, the use of strontium isotopes in archaeology and biogeochemical research has spread widely. These isotopes, alone or in combination with others, can contribute to trace past and present environmental conditions. However, the interpretation of the isotopic values of strontium is not always simple and requires good knowledge of geochemistry and geology. This short paper on the use of strontium isotopes is aimed at those who use this tool (archaeologists, but not only) but who do not have a thorough knowledge of mineralogy, geology, and geochemistry necessary for a good understanding of natural processes involving these isotopes. We report basic knowledge and suggestions for the correct use of these isotopes. The isotopic characteristics of bio-assimilable strontium depend not so much on the isotopic characteristics of the bulk rock as, rather, on those of its more soluble minerals. Before studying human, animal and plant remains, the state of conservation and any conditions of isotopic pollution should be carefully checked. Samples should be collected according to random sampling rules. The data should be treated by a statistical approach. To make comparisons between different areas, it should be borne in mind that the study of current soils can be misleading since the mineralogical modification of soil over time can be very rapid.https://www.mdpi.com/2571-550X/7/1/6<sup>87</sup>Sr/<sup>86</sup>Srarchaeologyenvironmentmineral dissolutionbioavailable Sr
spellingShingle Mattia Rossi
Paola Iacumin
Gianpiero Venturelli
<sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and Risks
Quaternary
<sup>87</sup>Sr/<sup>86</sup>Sr
archaeology
environment
mineral dissolution
bioavailable Sr
title <sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and Risks
title_full <sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and Risks
title_fullStr <sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and Risks
title_full_unstemmed <sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and Risks
title_short <sup>87</sup>Sr/<sup>86</sup>Sr Isotope Ratio as a Tool in Archaeological Investigation: Limits and Risks
title_sort sup 87 sup sr sup 86 sup sr isotope ratio as a tool in archaeological investigation limits and risks
topic <sup>87</sup>Sr/<sup>86</sup>Sr
archaeology
environment
mineral dissolution
bioavailable Sr
url https://www.mdpi.com/2571-550X/7/1/6
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