{"title":"Precise U–Pb chronology of tooth enamels of index fossils of Miocene fauna","authors":"Pu Zhang , Yangfan Li , Guoqi Liu , Zhe Zhang","doi":"10.1016/j.apgeochem.2025.106457","DOIUrl":null,"url":null,"abstract":"<div><div>Five fossil beds containing fossil specimens of <em>Hipparion chiai,</em> which is the most widespread index fossil in Late Miocene strata in northern China, were identified. The biological apatite (carbonated hydroxyapatite) in the teeth fossils of <em>Hipparion chiai</em> has a high μ value (initial <sup>238</sup>U/<sup>204</sup>Pb<sub>i</sub>) and limited Th content. The fossilized tooth enamels remain relatively unchanged due to their resistance to diagenetic alterations. Here, for the first time, we precisely dated six fossil teeth of <em>Hipparion chiai</em> from the Wangdafuliang section in Fugu, Shaanxi Province, using <strong>the</strong> LA-ICP-MS U–Pb geochronology method. The U–Pb dates obtained from the six fossil teeth of <em>Hipparion chiai</em> range from 6.87 ± 0.13 Ma to 7.71 ± 0.39 Ma (2 s), with an average of 7.26 Ma. <strong>The a</strong>ges of the tooth enamels of a <em>Samotherium</em> sp. and a <em>Rhinocerotidae</em> (genus and species unidentified) are consistent with the ages of the tooth enamels of the <em>Hipparion chiai</em>. The analytical method developed for this study provides a new benchmark for dating Neogene fossils.</div></div>","PeriodicalId":8064,"journal":{"name":"Applied Geochemistry","volume":"189 ","pages":"Article 106457"},"PeriodicalIF":3.4000,"publicationDate":"2025-05-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Geochemistry","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0883292725001805","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Five fossil beds containing fossil specimens of Hipparion chiai, which is the most widespread index fossil in Late Miocene strata in northern China, were identified. The biological apatite (carbonated hydroxyapatite) in the teeth fossils of Hipparion chiai has a high μ value (initial 238U/204Pbi) and limited Th content. The fossilized tooth enamels remain relatively unchanged due to their resistance to diagenetic alterations. Here, for the first time, we precisely dated six fossil teeth of Hipparion chiai from the Wangdafuliang section in Fugu, Shaanxi Province, using the LA-ICP-MS U–Pb geochronology method. The U–Pb dates obtained from the six fossil teeth of Hipparion chiai range from 6.87 ± 0.13 Ma to 7.71 ± 0.39 Ma (2 s), with an average of 7.26 Ma. The ages of the tooth enamels of a Samotherium sp. and a Rhinocerotidae (genus and species unidentified) are consistent with the ages of the tooth enamels of the Hipparion chiai. The analytical method developed for this study provides a new benchmark for dating Neogene fossils.
期刊介绍:
Applied Geochemistry is an international journal devoted to publication of original research papers, rapid research communications and selected review papers in geochemistry and urban geochemistry which have some practical application to an aspect of human endeavour, such as the preservation of the environment, health, waste disposal and the search for resources. Papers on applications of inorganic, organic and isotope geochemistry and geochemical processes are therefore welcome provided they meet the main criterion. Spatial and temporal monitoring case studies are only of interest to our international readership if they present new ideas of broad application.
Topics covered include: (1) Environmental geochemistry (including natural and anthropogenic aspects, and protection and remediation strategies); (2) Hydrogeochemistry (surface and groundwater); (3) Medical (urban) geochemistry; (4) The search for energy resources (in particular unconventional oil and gas or emerging metal resources); (5) Energy exploitation (in particular geothermal energy and CCS); (6) Upgrading of energy and mineral resources where there is a direct geochemical application; and (7) Waste disposal, including nuclear waste disposal.