{"@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/1361699994323325696.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2001pa000725"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001PA000725"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001PA000725"}},{"identifier":{"@type":"NAID","@value":"30013357934"}}],"dc:title":[{"@value":"Stacked 2.6‐Ma grain size record from the Chinese loess based on five sections and correlation with the deep‐sea δ<sup>18</sup>O record"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>This study aims to establish a stacked climate record of the Quaternary period from the Chinese loess sequence and to address the forcing mechanisms for the regional climate history of the Loess Plateau by correlating the stacked record with a composite δ<jats:sup>18</jats:sup>O record in deep‐sea sediments. A total of 18,352 samples were obtained from five loess sections, located at Baoji, Lingtai, Jingchuan, Puxian, and Pingliang in the southern and middle Loess Plateau. These yielded high‐resolution grain size records. Between‐section correlation of these shows that although small depositional hiatuses are present in places within a single section, most parts of the sections display near‐continuous dust deposition throughout the Quaternary. The grain size records were tuned simultaneously to the theoretical variations in obliquity and precession of the Earth’s orbit. The grain size records plotted on their orbital timescales were then averaged to form a stacked loess grain size time series, termed the “Chiloparts” record. This resolves most of the orbital timescale paleoclimate events buried in the loess‐soil sequences of the southern and middle Loess Plateau and can be used as a regional archive of the Pleistocene climate history in the Loess Plateau. Comparison of the “Chiloparts” record with a composite marine δ<jats:sup>18</jats:sup>O record shows that for the past 1.8 Ma, the loess‐paleosol record can be correlated almost cycle by cycle with the marine record. Several discrepancies in the climatic events between the two records have also been identified, implying that regional forcing mechanisms may have played a part in the climatic evolution of the Chinese Loess Plateau.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380286993351168903","@type":"Researcher","foaf:name":[{"@value":"Z. L. Ding"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Geophysics Chinese Academy of Sciences  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994323325698","@type":"Researcher","foaf:name":[{"@value":"E. Derbyshire"}],"jpcoar:affiliationName":[{"@value":"Centre for Quaternary Research, Department of Geography Royal Holloway, University of London  Egham UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994323325696","@type":"Researcher","foaf:name":[{"@value":"S. L. Yang"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Geophysics Chinese Academy of Sciences  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994323325700","@type":"Researcher","foaf:name":[{"@value":"Z. W. Yu"}],"jpcoar:affiliationName":[{"@value":"Department of Resource Exploitation and Engineering China University of Mining and Technology  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994323325701","@type":"Researcher","foaf:name":[{"@value":"S. F. Xiong"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Geophysics Chinese Academy of Sciences  Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994323325699","@type":"Researcher","foaf:name":[{"@value":"T. S. Liu"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Geophysics Chinese Academy of Sciences  Beijing China"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08838305"},{"@type":"EISSN","@value":"19449186"}],"prism:publicationName":[{"@value":"Paleoceanography"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2002-08-06","prism:volume":"17","prism:number":"3","prism:startingPage":"5"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001PA000725"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001PA000725"}],"createdAt":"2002-10-27","modifiedAt":"2023-10-16","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050012570391873408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A centennial-resolution terrestrial climatostratigraphy and Matuyama–Brunhes transition record from a loess sequence in China"}]},{"@id":"https://cir.nii.ac.jp/crid/1050294045369569280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Intensified East Asian winter monsoon during the last geomagnetic reversal transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232419843456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New insights into magnetic enhancement mechanism in Chinese paleosols"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142733548160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Constraining the transgression history in the Bohai Coast China since the Middle Pleistocene by luminescence dating"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707396540032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global cooling in marine climates and local tectonic events in Southwest Japan at the Plio–Pleistocene boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658216003456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multiple rapid polarity swings during the Matuyama‐Brunhes transition from two high‐resolution loess‐paleosol records"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660683910400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reliability of Relative Paleointensity Recorded in Chinese Loess–Paleosol Sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204549464192","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An EPR study on mollusk shells from loess-paleosol sequences in the Loess Plateau, central China"},{"@language":"ja-Kana","@value":"EPR study on mollusk shells from loess paleosol sequences in the Loess Plateau central China"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217874944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Pliocene magneto- and climatostratigraphic evolution toward the onset of the Quaternary in East Asia"},{"@language":"ja","@value":"古地磁気・古気候層序からみた東アジアの第四紀の始まり"},{"@language":"ja-Kana","@value":"コ チジキ ・ コ キコウソウ ジョ カラ ミタ ヒガシアジア ノ ダイシキ ノ ハジマリ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2001pa000725"},{"@type":"CIA","@value":"30013357934"},{"@type":"CROSSREF","@value":"10.1016/j.margeo.2019.105980_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00337-z_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.1038/s41598-019-45466-8_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2012.11.016_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2012.05.025_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.1029/2009jb006301_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.1111/j.1755-6724.2012.00747.x_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.2343/geochemj.39.61_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2011.0008_references_DOI_1x8m1RAmuZzvH9v7Q817N1bILgO"}]}