{"@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/1363670319745033344.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5194/cp-7-361-2011"}},{"identifier":{"@type":"URI","@value":"https://cp.copernicus.org/articles/7/361/2011/cp-7-361-2011.pdf"}}],"dc:title":[{"@value":"Interglacial and glacial variability from the last 800 ka in marine, ice and terrestrial archives"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Abstract. We have compiled 37 ice, marine and terrestrial palaeoclimate records covering the last 800 000 years in order to assess the pattern of glacial and interglacial strength, and termination amplitude. Records were selected based on their length, completeness and resolution, and their age models were updated, where required, by alignment to the LR04 benthic δ18O stack. The resulting compilation allows comparison of individual glacial to interglacial transitions with confidence, but the level of synchronisation is inadequate for discussion of temporal phasing. The comparison of interglacials and glacials concentrates on the peaks immediately before and after terminations; particularly strong and weak glacials and interglacials have been identified. This confirms that strong interglacials are confined to the last 450 ka, and that this is a globally robust pattern; however weak interglacials (i.e. marine isotope stage 7) can still occur in this later period. Strong glacial periods are also concentrated in the recent half of the records, although marine isotope stage 16 is strong in many δ18O records. Strong interglacials, particularly in the marine isotopic records, tend to follow strong glacials, suggesting that we should not expect interglacial strength to be strongly influenced by the instantaneous astronomical forcing. Many interglacials have a complex structure, with multiple peaks and troughs whose origin needs to be understood. However this compilation emphasises the under-representation of terrestrial environments and highlights the need for long palaeoclimate records from these areas. The main result of this work is the compiled datasets and maps of interglacial strength which provide a target for modelling studies and for conceptual understanding.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380580230606410121","@type":"Researcher","foaf:name":[{"@value":"N. Lang"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319745033344","@type":"Researcher","foaf:name":[{"@value":"E. W. Wolff"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18149332"}],"prism:publicationName":[{"@value":"Climate of the Past"}],"dc:publisher":[{"@value":"Copernicus GmbH"}],"prism:publicationDate":"2011-04-21","prism:volume":"7","prism:number":"2","prism:startingPage":"361","prism:endingPage":"380"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/3.0/"],"url":[{"@id":"https://cp.copernicus.org/articles/7/361/2011/cp-7-361-2011.pdf"}],"createdAt":"2011-04-21","modifiedAt":"2025-02-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050008763985565824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoclimatic and paleoceanographic records through Marine Isotope Stage 19 at the Chiba composite section, central Japan: A key reference for the EarlyeMiddle Pleistocene Subseries boundary"},{"@value":"Paleoclimatic and paleoceanographic records through Marine Isotope Stage 19 at the Chiba composite section, central Japan: A key reference for the Early–Middle Pleistocene Subseries boundary"},{"@value":"Paleoclimatic and paleoceanographic records of Marine Isotope Stage 19 at the Chiba composite section, central Japan: a reference for the Early–Middle Pleistocene boundary"},{"@value":"Paleoclimatic and paleoceanographic records of Marine Isotope Stage 19 at the Chiba composite section, central Japan: a reference for the Early-Middle Pleisotocene boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168721777280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sea Surface Temperatures in the Indian Sub‐Antarctic Southern Ocean for the Last Four Interglacial Periods"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707396584576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanographic history of the Northwest Pacific Ocean over the past 740 kyr, discerned from radiolarian fauna"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092477017344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"PMIP4/CMIP6 last interglacial simulations using three  different versions of MIROC: importance of vegetation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639280307840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interglacials of the last 800,000 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658396468608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266996491136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long-chain alkenones in the Shimosa Group reveal palaeotemperatures of the Pleistocene interglacial Palaeo-Tokyo Bays"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.5194/cp-7-361-2011"},{"@type":"CROSSREF","@value":"10.1029/2020gl090994_references_DOI_SQ7hWsPOkd6vRlQVzXyySAd1kr9"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2018.04.022_references_DOI_SQ7hWsPOkd6vRlQVzXyySAd1kr9"},{"@type":"CROSSREF","@value":"10.5194/cp-17-21-2021_references_DOI_SQ7hWsPOkd6vRlQVzXyySAd1kr9"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00499-y_references_DOI_SQ7hWsPOkd6vRlQVzXyySAd1kr9"},{"@type":"CROSSREF","@value":"10.1002/2015rg000482_references_DOI_SQ7hWsPOkd6vRlQVzXyySAd1kr9"},{"@type":"CROSSREF","@value":"10.1038/s41467-018-03328-3_references_DOI_SQ7hWsPOkd6vRlQVzXyySAd1kr9"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2013.12.036_references_DOI_SQ7hWsPOkd6vRlQVzXyySAd1kr9"}]}