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":0,"journal":{"name":"","volume":null,"pages":null},"PeriodicalIF":0.0,"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\":0,\"journal\":{\"name\":\"\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0,\"publicationDate\":\"2017-11-30\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.29041/STRAT.14.1-4.443-456\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.29041/STRAT.14.1-4.443-456","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}