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基于牙釉质构建等景观图以估计巴西人类来源。

Building an isoscape based on tooth enamel for human provenance estimation in Brazil.

作者信息

de Oliveira Mascarenhas Ricardo, Sena-Souza João Paulo, Bernasconi Stefano M, McKenzie Judith A, Vasconcelos Crisógono, Muniz Taís Ribeiro, Nogueira E Silva Matheus Pereira, da Silva Salvador Fábio Augusto, Rumbelsperger Anelize Manuela Bahniuk

机构信息

Brazilian Federal Police, Technical-Scientific Section, R. Profa. Sandália Monzon 210, 82640-040, Curitiba, PR, Brazil; Laboratory of Mineral and Rock Analysis (LAMIR), Department of Geology, Federal University of Paraná, PO Box 19062, 81531-980 Curitiba, PR, Brazil.

Department of Geosciences, State University of Montes Claros (Unimontes), Campus Universitário Prof. Darcy Ribeiro, Av. Prof. Rui Braga, s/n - Vila Mauriceia, 39401-089 Montes Claros, MG, Brazil.

出版信息

Forensic Sci Int. 2022 Jan;330:111109. doi: 10.1016/j.forsciint.2021.111109. Epub 2021 Nov 24.

Abstract

In this study, we present a correlation between δO values of carbonate in tooth enamel samples from the modern Brazilian population and the available δO data for the meteoric water from the Global Network of Isotopes in Precipitation (GNIP). Tooth enamel from 119 Brazilian individuals from five different regions of the country were analyzed. The δO isoscape obtained is in good agreement with the isoscape based on regional meteoric and drinking water. The regression matrix obtained for the δO values of the carbonate tooth enamel and meteoric water was used to build an isoscape using the regression-kriging approach. Our data show that Brazil can be divided in two main regions with respect to the δO values of the carbonate tooth enamel: (1) the most easterly part of the northeast region, which is characterized by a warm and dry climate and (2) the remainder of the country, stretching from the Amazon rain forest to the more southernly regions. The data herein reported can be used for forensic purposes related to human identification.

摘要

在本研究中,我们展示了现代巴西人群牙釉质样本中碳酸盐的δO值与全球降水同位素网络(GNIP)中大气降水的可用δO数据之间的相关性。分析了来自巴西五个不同地区的119名个体的牙釉质。所得的δO等浓度线图与基于区域大气降水和饮用水的等浓度线图高度吻合。利用回归克里金法,将碳酸盐牙釉质和大气降水的δO值所得的回归矩阵用于构建等浓度线图。我们的数据表明,就碳酸盐牙釉质的δO值而言,巴西可分为两个主要区域:(1)东北部地区最东部,其特点是气候温暖干燥;(2)该国其余地区,从亚马逊雨林延伸至更南部地区。本文报道的数据可用于与人类识别相关的法医目的。

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