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Dataset of oxygen, carbon, and strontium isotope values from the Imperial Roman site of Velia (ca. 1st-2nd c. CE), Italy

机译:来自Velia帝国罗马现场的氧气,碳和锶同位素值的数据集(CA.1ST-2ND C. CE),意大利

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The oxygen (δ18Ocarbonate), strontium (87Sr/86Sr), and previously unpublished carbon (δ13Ccarbonate) isotope data presented herein from the Imperial Roman site of Velia (ca. 1st to 2nd c. CE) were obtained from the dental enamel of human permanent second molars (M2). In total, the permanent M2s of 20 individuals (10 male and 10 female) were sampled at the Museo delle Civiltà in Rome (formerly the Museo Nazionale Preistorico Etnografico “L. Pigorini”) and were subsequently processed and analysed at McMaster University. A subsample of teeth (n=5) was initially subjected to Fourier transform infrared spectroscopy (FTIR) analysis to assess for diagenetic alteration through calculation of crystallinity index (CI) values. Subsequently, tooth enamel was analysed for δ13Ccarbonateand δ18Ocarbonate(VPDB) using a VG OPTIMA Isocarb isotope ratio mass spectrometer (IRMS) at McMaster Research for Stable Isotopologues (MRSI), and87Sr/86Sr was measured by dynamic multi-collection using a thermal ionization mass spectrometer (TIMS) in the School of Geography and Earth Sciences. The dental enamel isotope data presented represent the first δ18O, δ13Ccarbonate, and87Sr/86Sr values analysed from Imperial Roman Campania to date, providing data of use for comparative analyses of δ18O, δ13C, and87Sr/86Sr values within the region and for assisting in documenting human mobility in archaeological contexts. Full interpretation of the δ18O and87Sr/86Sr data presented here is provided in “Imperial Roman mobility and migration at Velia (1stto 2ndc. CE) in southern Italy” .
机译:氧气(δ18碳酸盐),锶(87sr / 86sr)和先前未发表的碳(Δ13carbonate)同位素数据来自Velia帝国罗马(Ca.1st至2nd c. ce)中获得的人类永久性牙釉质第二臼齿(M2)。总共有20个人(10名男性和10名女性)在罗马的Museo delleCiviltà上抽样(以前的Museo Nazionale Preistoricoo etnografico“L. Pigolini”),并随后在麦克马斯特大学进行了处理和分析。最初对牙齿(n = 5)的牙齿(n = 5)进行傅里叶变换红外光谱(FTIR)分析,以通过计算结晶度指数(CI)值来评估成岩变化。随后,使用Vg Optima Isocarb同位素比率质谱仪(IRMS)在McMaster研究中分析牙釉质的Δ13ccarbonaTeandΔ18碳酸酯(VPDB),用于稳定同位素(MRSI),使用热电电离质谱仪通过动态多收集测量87SR / 86SR (TIMS)在地理和地球科学学校。呈现的牙科搪瓷同位素数据代表迄今为止从帝国罗马坎帕尼亚分析的第一Δ18O,δ13cc碳酸盐和87sr / 86sr值,提供了该地区内Δ18o,δ13c,和87sr / 86sr值的比较分析的使用数据,并辅助记录人类考古背景下的流动性。本文提供的“在意大利南部的威廉罗马流动性和迁移”中提供了完全解释此处的Δ18O和87SR/ 86SR数据“。

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