Alisson L. Oliveira , Maria Helena B.M. Hollanda , Mark D. Schmitz , Antomat A. Macêdo Filho , Elisabetta Erba , James L. Crowley
{"title":"赤道大西洋岩浆省(EQUAMP)高精度年代学:与Paraná-Etendeka岩浆省和Weissert事件的时间相关性","authors":"Alisson L. Oliveira , Maria Helena B.M. Hollanda , Mark D. Schmitz , Antomat A. Macêdo Filho , Elisabetta Erba , James L. Crowley","doi":"10.1016/j.epsl.2025.119330","DOIUrl":null,"url":null,"abstract":"<div><div>The Equatorial Atlantic Magmatic Province (EQUAMP) is an intrusive large igneous province (LIP) related to the dismembering of the West Gondwana supercontinent and early opening stage of the South Atlantic Ocean. Here, we present the first set of high-precision (at the 100 ka-level) U-Pb zircon geochronology for the EQUAMP by the chemical abrasion isotope dilution thermal ionization mass spectrometry method. Based on our results, the EQUAMP was emplaced in a short time interval, between 133.805 ± 0.021 Ma and 133.071 ± 0.031 Ma and appears to be coeval with the Paraná Etendeka Magmatic Province (∼134.5–132.0 Ma). Both LIPs are currently exposed at the margins of the South Atlantic Ocean and could have jointly contributed greenhouse gasses and fresh mafic exposures susceptible to chemical weathering that ultimately fertilized the oceans, cooled the Earth, affected calcareous nannoplankton and produced a paleoclimate disturbance — the Valanginian Weissert Event.</div></div>","PeriodicalId":11481,"journal":{"name":"Earth and Planetary Science Letters","volume":"658 ","pages":"Article 119330"},"PeriodicalIF":4.8000,"publicationDate":"2025-03-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"High-precision geochronology of the Equatorial Atlantic Magmatic Province (EQUAMP): Temporal correlations with the Paraná-Etendeka Magmatic Province and the Weissert Event\",\"authors\":\"Alisson L. Oliveira , Maria Helena B.M. Hollanda , Mark D. Schmitz , Antomat A. Macêdo Filho , Elisabetta Erba , James L. Crowley\",\"doi\":\"10.1016/j.epsl.2025.119330\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The Equatorial Atlantic Magmatic Province (EQUAMP) is an intrusive large igneous province (LIP) related to the dismembering of the West Gondwana supercontinent and early opening stage of the South Atlantic Ocean. Here, we present the first set of high-precision (at the 100 ka-level) U-Pb zircon geochronology for the EQUAMP by the chemical abrasion isotope dilution thermal ionization mass spectrometry method. Based on our results, the EQUAMP was emplaced in a short time interval, between 133.805 ± 0.021 Ma and 133.071 ± 0.031 Ma and appears to be coeval with the Paraná Etendeka Magmatic Province (∼134.5–132.0 Ma). Both LIPs are currently exposed at the margins of the South Atlantic Ocean and could have jointly contributed greenhouse gasses and fresh mafic exposures susceptible to chemical weathering that ultimately fertilized the oceans, cooled the Earth, affected calcareous nannoplankton and produced a paleoclimate disturbance — the Valanginian Weissert Event.</div></div>\",\"PeriodicalId\":11481,\"journal\":{\"name\":\"Earth and Planetary Science Letters\",\"volume\":\"658 \",\"pages\":\"Article 119330\"},\"PeriodicalIF\":4.8000,\"publicationDate\":\"2025-03-27\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Earth and Planetary Science Letters\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0012821X25001293\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth and Planetary Science Letters","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0012821X25001293","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
High-precision geochronology of the Equatorial Atlantic Magmatic Province (EQUAMP): Temporal correlations with the Paraná-Etendeka Magmatic Province and the Weissert Event
The Equatorial Atlantic Magmatic Province (EQUAMP) is an intrusive large igneous province (LIP) related to the dismembering of the West Gondwana supercontinent and early opening stage of the South Atlantic Ocean. Here, we present the first set of high-precision (at the 100 ka-level) U-Pb zircon geochronology for the EQUAMP by the chemical abrasion isotope dilution thermal ionization mass spectrometry method. Based on our results, the EQUAMP was emplaced in a short time interval, between 133.805 ± 0.021 Ma and 133.071 ± 0.031 Ma and appears to be coeval with the Paraná Etendeka Magmatic Province (∼134.5–132.0 Ma). Both LIPs are currently exposed at the margins of the South Atlantic Ocean and could have jointly contributed greenhouse gasses and fresh mafic exposures susceptible to chemical weathering that ultimately fertilized the oceans, cooled the Earth, affected calcareous nannoplankton and produced a paleoclimate disturbance — the Valanginian Weissert Event.
期刊介绍:
Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.