钕同位素比值和正d13C偏移:解释Laurentia晚奥陶世早期海洋与气候变化之间的联系

{"title":"钕同位素比值和正d13C偏移:解释Laurentia晚奥陶世早期海洋与气候变化之间的联系","authors":"Zachary Wright, Page C. Quinton, E. Martin, S. Leslie, K. MacLeod, A. Herrmann","doi":"10.29041/STRAT.14.1-4.443-456","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":51180,"journal":{"name":"Stratigraphy","volume":"5 1","pages":"443-456"},"PeriodicalIF":0.9000,"publicationDate":"2017-11-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"Neodymium isotope ratios and a positive d13C excursion: interpreting the connection between oceanographic and climate changes during the early Late Ordovician of Laurentia\",\"authors\":\"Zachary Wright, Page C. Quinton, E. Martin, S. Leslie, K. MacLeod, A. Herrmann\",\"doi\":\"10.29041/STRAT.14.1-4.443-456\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":51180,\"journal\":{\"name\":\"Stratigraphy\",\"volume\":\"5 1\",\"pages\":\"443-456\"},\"PeriodicalIF\":0.9000,\"publicationDate\":\"2017-11-30\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Stratigraphy\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.29041/STRAT.14.1-4.443-456\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Stratigraphy","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.29041/STRAT.14.1-4.443-456","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOLOGY","Score":null,"Total":0}