{"title":"Oxygen isotope composition of Mesoproterozoic (~1360 Ma) seawater constrained by clumped isotopes of North China limestones","authors":"Pingping Li, Fang Hao, Shijie He, Haobo Chai, Yongfei Jiao, Yaxuan Gao, Huayao Zou","doi":"10.1126/sciadv.adu6693","DOIUrl":null,"url":null,"abstract":"The oxygen isotope composition (δ <jats:sup>18</jats:sup> O) of Phanerozoic seawater has been widely investigated, but the δ <jats:sup>18</jats:sup> O values of Precambrian seawater remain poorly constrained, with ongoing debate over whether they were substantially lower than those of Phanerozoic seawater. To address this question, we analyzed the clumped isotopes of limestones from the North China Craton to reconstruct Mesoproterozoic seawater temperature and δ <jats:sup>18</jats:sup> O values. Our results indicate that the Mesoproterozoic seawater had a temperature of 26.9° ± 0.4°C and a δ <jats:sup>18</jats:sup> O value of −6.3 ± 0.2 per mil (relative to standard mean ocean water). This δ <jats:sup>18</jats:sup> O estimate aligns with previous inferences from geochemical modeling, marine iron oxides, and oxygen isotope ensembles, supporting the hypothesis that Mesoproterozoic seawater was isotopically lighter than its Phanerozoic counterpart. These findings provide insights into the Earth’s paleoclimate and the evolution of seawater composition during the Mesoproterozoic era.","PeriodicalId":21609,"journal":{"name":"Science Advances","volume":"101 1","pages":""},"PeriodicalIF":12.5000,"publicationDate":"2025-10-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Science Advances","FirstCategoryId":"103","ListUrlMain":"https://doi.org/10.1126/sciadv.adu6693","RegionNum":1,"RegionCategory":"综合性期刊","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"MULTIDISCIPLINARY SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
The oxygen isotope composition (δ 18 O) of Phanerozoic seawater has been widely investigated, but the δ 18 O values of Precambrian seawater remain poorly constrained, with ongoing debate over whether they were substantially lower than those of Phanerozoic seawater. To address this question, we analyzed the clumped isotopes of limestones from the North China Craton to reconstruct Mesoproterozoic seawater temperature and δ 18 O values. Our results indicate that the Mesoproterozoic seawater had a temperature of 26.9° ± 0.4°C and a δ 18 O value of −6.3 ± 0.2 per mil (relative to standard mean ocean water). This δ 18 O estimate aligns with previous inferences from geochemical modeling, marine iron oxides, and oxygen isotope ensembles, supporting the hypothesis that Mesoproterozoic seawater was isotopically lighter than its Phanerozoic counterpart. These findings provide insights into the Earth’s paleoclimate and the evolution of seawater composition during the Mesoproterozoic era.
期刊介绍:
Science Advances, an open-access journal by AAAS, publishes impactful research in diverse scientific areas. It aims for fair, fast, and expert peer review, providing freely accessible research to readers. Led by distinguished scientists, the journal supports AAAS's mission by extending Science magazine's capacity to identify and promote significant advances. Evolving digital publishing technologies play a crucial role in advancing AAAS's global mission for science communication and benefitting humankind.