{"title":"深海沉积物和冰芯如何提供第四纪气候变化记录的分析","authors":"M. Ball","doi":"10.1080/00167487.2021.1970933","DOIUrl":null,"url":null,"abstract":"Introduction This article explores the range of methods available to analyse ice and deep-sea sediment cores. It also explores the value of such cores in the context of reconstructing a record of Quaternary climate change, or paleoclimatic reconstruction. Paleoclimatic reconstruction is an extremely important and useful field of research due to the practical benefits it provides for the study of climate change.","PeriodicalId":46568,"journal":{"name":"Geography","volume":"106 1","pages":"154 - 160"},"PeriodicalIF":1.4000,"publicationDate":"2021-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"An analysis of how deep-sea sediments and ice cores provide a record of Quaternary climate change\",\"authors\":\"M. Ball\",\"doi\":\"10.1080/00167487.2021.1970933\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Introduction This article explores the range of methods available to analyse ice and deep-sea sediment cores. It also explores the value of such cores in the context of reconstructing a record of Quaternary climate change, or paleoclimatic reconstruction. Paleoclimatic reconstruction is an extremely important and useful field of research due to the practical benefits it provides for the study of climate change.\",\"PeriodicalId\":46568,\"journal\":{\"name\":\"Geography\",\"volume\":\"106 1\",\"pages\":\"154 - 160\"},\"PeriodicalIF\":1.4000,\"publicationDate\":\"2021-09-02\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geography\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1080/00167487.2021.1970933\",\"RegionNum\":4,\"RegionCategory\":\"社会学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOGRAPHY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geography","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1080/00167487.2021.1970933","RegionNum":4,"RegionCategory":"社会学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOGRAPHY","Score":null,"Total":0}
An analysis of how deep-sea sediments and ice cores provide a record of Quaternary climate change
Introduction This article explores the range of methods available to analyse ice and deep-sea sediment cores. It also explores the value of such cores in the context of reconstructing a record of Quaternary climate change, or paleoclimatic reconstruction. Paleoclimatic reconstruction is an extremely important and useful field of research due to the practical benefits it provides for the study of climate change.
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