{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360011144042533504.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1017/s0954102098000406"}},{"identifier":{"@type":"URI","@value":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102098000406"}}],"dc:title":[{"@value":"Circum-Antarctic coastal environmental shifts during the Late Quaternary reflected by emerged marine deposits"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>This review assesses the circumpolar occurrence of emerged marine macrofossils and sediments from Antarctic coastal areas in relation to Late Quaternary climate changes. Radiocarbon ages of the macrofossils, which are interpreted in view of the complexities of the Antarctic marine radiocarbon reservoir and resolution of this dating technique, show a bimodal distribution. The data indicate that marine species inhabited coastal environments from at least 35 000 to 20 000 yr BP, during Marine Isotope Stage 3 when extensive iceberg calving created a ‘meltwater lid’ over the Southern Ocean. The general absence of these marine species from 20 000 to 8500 yr <jats:sc>BP</jats:sc> coincides with the subsequent advance of the Antarctic ice sheets during the Last Glacial Maximum. Synchronous re-appearance of the Antarctic marine fossils in emerged beaches around the continent, all of which have Holocene marine-limit elevations an order of magnitude lower than those in the Arctic, reflect minimal isostatic rebound as relative sea-level rise decelerated. Antarctic coastal marine habitat changes around the continent also coincided with increasing sea-ice extent and outlet glacial advances during the mid-Holocene. In view of the diverse environmental changes that occurred around the Earth during this period, it is suggested that Antarctic coastal areas were responding to a mid-Holocene climatic shift associated with the hydrological cycle. This synthesis of Late Quaternary emerged marine deposits demonstrates the application of evaluating circum-Antarctic phenomena from the glacial-terrestrial-marine transition zone.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011144042533378","@type":"Researcher","foaf:name":[{"@value":"Paul A. Berkman"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533510","@type":"Researcher","foaf:name":[{"@value":"John T. Andrews"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533380","@type":"Researcher","foaf:name":[{"@value":"Svante Björck"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533505","@type":"Researcher","foaf:name":[{"@value":"Eric A. Colhoun"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533381","@type":"Researcher","foaf:name":[{"@value":"Steven D. Emslie"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533379","@type":"Researcher","foaf:name":[{"@value":"Ian D. Goodwin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533382","@type":"Researcher","foaf:name":[{"@value":"Brenda L. Hall"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533506","@type":"Researcher","foaf:name":[{"@value":"Charles P. Hart"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533376","@type":"Researcher","foaf:name":[{"@value":"Kazuomi Hirakawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533377","@type":"Researcher","foaf:name":[{"@value":"Atsuo Igarashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533508","@type":"Researcher","foaf:name":[{"@value":"Olafur Ingólfsson"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533512","@type":"Researcher","foaf:name":[{"@value":"Jeronimo López-Martínez"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533513","@type":"Researcher","foaf:name":[{"@value":"W. Berry Lyons"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533507","@type":"Researcher","foaf:name":[{"@value":"Mark C.G. Mabin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533504","@type":"Researcher","foaf:name":[{"@value":"Patrick G. Quilty"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144042533511","@type":"Researcher","foaf:name":[{"@value":"Marco Taviani"}]},{"@id":"https://cir.nii.ac.jp/crid/1410009224682928897","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000002383661"},{"@type":"NRID","@value":"9000350540703"},{"@type":"NRID","@value":"9000020837641"},{"@type":"NRID","@value":"9000002237886"},{"@type":"NRID","@value":"9000002392609"},{"@type":"NRID","@value":"9000002205447"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0044861"}],"foaf:name":[{"@value":"Yoshio Yoshida"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"09541020"},{"@type":"EISSN","@value":"13652079"}],"prism:publicationName":[{"@value":"Antarctic Science"}],"dc:publisher":[{"@value":"Cambridge University Press (CUP)"}],"prism:publicationDate":"1998-09","prism:volume":"10","prism:number":"3","prism:startingPage":"345","prism:endingPage":"362"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://www.cambridge.org/core/terms"],"url":[{"@id":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102098000406"}],"createdAt":"2007-12-11","modifiedAt":"2019-04-01","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Holocene","dc:title":"Holocene"},{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=sediments","dc:title":"sediments"},{"@id":"https://cir.nii.ac.jp/all?q=333","dc:title":"333"},{"@id":"https://cir.nii.ac.jp/all?q=Pleistocene","dc:title":"Pleistocene"},{"@id":"https://cir.nii.ac.jp/all?q=radiocarbon","dc:title":"radiocarbon"},{"@id":"https://cir.nii.ac.jp/all?q=Earth%20Sciences","dc:title":"Earth Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=Antarctic","dc:title":"Antarctic"},{"@id":"https://cir.nii.ac.jp/all?q=beaches","dc:title":"beaches"},{"@id":"https://cir.nii.ac.jp/all?q=fossils","dc:title":"fossils"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232102637824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Post-glacial regional climate variability along the East Antarctic coastal margin—Evidence from shallow marine and coastal terrestrial records"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707446128256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ice sheet retreat and glacio-isostatic adjustment in Lützow-Holm Bay, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588381074776960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Pleistocene sea-level constraints across Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680397905664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Holocene paleoenvironmental studies in the Soya Kaigan of Antarctica viewed from Lake Oyako-ike sediment core"},{"@language":"ja","@value":"南極大陸宗谷海岸の親子池湖底堆積物コアによる完新世における古環境学的研究"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892142891648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Biogeochemistry and limnology in Antarctic subglacial weathering : molecular evidence of the linkage between subglacial silica input and primary producers in a perennially ice-covered lake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1017/s0954102098000406"},{"@type":"OPENAIRE","@value":"doi_dedup___::4587dc5077a3a655e5ed389a1015d111"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2017.06.003_references_DOI_97cHuGGB8gTEGPfMijPby0BcOJp"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0036-7_references_DOI_97cHuGGB8gTEGPfMijPby0BcOJp"},{"@type":"CROSSREF","@value":"10.9748/hcs.2013.189_references_DOI_97cHuGGB8gTEGPfMijPby0BcOJp"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2024.108879_references_DOI_97cHuGGB8gTEGPfMijPby0BcOJp"},{"@type":"CROSSREF","@value":"10.1016/j.earscirev.2010.10.006_references_DOI_97cHuGGB8gTEGPfMijPby0BcOJp"}]}