{"@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/1360021391860581888.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2022pa004588"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2022PA004588"}},{"identifier":{"@type":"HANDLE","@value":"10261/345928"}},{"identifier":{"@type":"HANDLE","@value":"11370/700d559d-09e1-4712-97a5-5cbe3fa02e3e"}},{"identifier":{"@type":"HANDLE","@value":"10481/84906"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Orbital Forcing and Evolution of the Southern African Monsoon From Late Miocene to Early Pliocene"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The late Miocene‐early Pliocene (7.4‐4.5 Ma) is a key interval in Earth's history where intense reorganization of atmospheric and ocean circulation occurred within a global cooling scenario. The Southern African monsoon (SAFM) potentially played an important role in climate systems variability during this interval. However, the dynamics of this important atmospheric system is poorly understood due to the scarcity of continuous records. Here, we present an exceptional continuous late Miocene to early Pliocene reconstruction of SAFM based on elemental geochemistry (Ca/Ti and Si/K ratios), stable isotope geochemistry (δ<jats:sup>18</jats:sup>O and δ<jats:sup>13</jats:sup>C recorded in the planktonic foraminifera<jats:italic>Orbulina universa</jats:italic>), and marine sediment grain size data from the International Ocean Discovery Program (IODP) Site U1476 located at the entrance of the Mozambique Channel. Spectral characteristics of the Si/K ratio (fluvial input) was used to identify the main orbital forcing controlling SAFM. Precession cycles governed precipitation from 7.4 to ∼6.9 Ma and during the early Pliocene. From ∼6.9 to ∼5.9 Ma, the precession and long eccentricity cycles drove the SAFM. The major Antarctic ice sheet expansion across this interval appear to influence the isotopic records of<jats:italic>O. universa</jats:italic>imprinting its long‐term variability signal as a response to the ocean and atmospheric reorganization. Precession cycles markedly weakened from 5.9 to 5.3 Ma, almost the same period when the Mediterranean Outflow Water ceased. These findings highlight important teleconnections among the SAFM, Mediterranean Sea, and other tropical regions.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380021391860581760","@type":"Researcher","foaf:name":[{"@value":"Allana Queiroz de Azevedo"}],"jpcoar:affiliationName":[{"@value":"Programa de Pós‐Graduação em Geoquímica Universidade Federal Fluminense Rio de Janeiro Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581762","@type":"Researcher","foaf:name":[{"@value":"Francisco J. Jiménez‐Espejo"}],"jpcoar:affiliationName":[{"@value":"Instituto Andaluz de Ciencias de la Tierra Consejo Superior de Investigaciones Científicas‐Universidad de Granada Armilla Spain"},{"@value":"Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581771","@type":"Researcher","foaf:name":[{"@value":"Francesca Bulian"}],"jpcoar:affiliationName":[{"@value":"Department of Geology Universidad de Salamanca Salamanca Spain"},{"@value":"Groningen Institute of Archeology University of Groningen Groningen The Netherlands"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581768","@type":"Researcher","foaf:name":[{"@value":"Francisco J. Sierro"}],"jpcoar:affiliationName":[{"@value":"Department of Geology Universidad de Salamanca Salamanca Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581766","@type":"Researcher","foaf:name":[{"@value":"Deborah Tangunan"}],"jpcoar:affiliationName":[{"@value":"School of Earth and Environmental Sciences Cardiff University Cardiff UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581767","@type":"Researcher","foaf:name":[{"@value":"Yasuhiro Takashimizu"}],"jpcoar:affiliationName":[{"@value":"Mathematical and Natural Sciences Niigata University Niigata Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581633","@type":"Researcher","foaf:name":[{"@value":"Ana Luiza S. Albuquerque"}],"jpcoar:affiliationName":[{"@value":"Programa de Pós‐Graduação em Geoquímica Universidade Federal Fluminense Rio de Janeiro Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801202143616","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80774075"},{"@type":"NRID","@value":"1000080774075"},{"@type":"KAKEN_RESEARCHERS","@value":"70501857"},{"@type":"NRID","@value":"1000070501857"},{"@type":"NDL_AUTHOR_ID","@value":"01067616"},{"@type":"NRID","@value":"9000264235311"},{"@type":"NRID","@value":"9000399851176"},{"@type":"NRID","@value":"9000011123084"},{"@type":"NRID","@value":"9000253608938"},{"@type":"NRID","@value":"9000406354725"},{"@type":"NRID","@value":"9000018214768"},{"@type":"NRID","@value":"9000388473682"},{"@type":"NRID","@value":"9000258407393"},{"@type":"NRID","@value":"9000405523518"},{"@type":"NRID","@value":"9000415325701"},{"@type":"NRID","@value":"9000000695549"},{"@type":"NRID","@value":"9000254177463"},{"@type":"NRID","@value":"9000398624685"},{"@type":"NRID","@value":"9000383075982"},{"@type":"NRID","@value":"9000024282496"},{"@type":"NRID","@value":"9000254622457"},{"@type":"NRID","@value":"9000254177093"},{"@type":"NRID","@value":"9000252911225"},{"@type":"NRID","@value":"9000254622971"},{"@type":"NRID","@value":"9000412670548"},{"@type":"NRID","@value":"9000253624445"},{"@type":"NRID","@value":"9000402078311"},{"@type":"NRID","@value":"9000018454007"},{"@type":"NRID","@value":"9000345371670"},{"@type":"NRID","@value":"9000404787089"},{"@type":"NRID","@value":"9000283529494"},{"@type":"NRID","@value":"9000266433676"},{"@type":"NRID","@value":"9000254625669"},{"@type":"NRID","@value":"9000402078297"},{"@type":"NRID","@value":"9000024340017"},{"@type":"NRID","@value":"9000253620239"},{"@type":"NRID","@value":"9000399820436"},{"@type":"NRID","@value":"9000307260838"},{"@type":"NRID","@value":"9000254627957"},{"@type":"NRID","@value":"9000409477093"},{"@type":"NRID","@value":"9000411514590"},{"@type":"NRID","@value":"9000024284808"},{"@type":"NRID","@value":"9000413573199"},{"@type":"NRID","@value":"9000015231499"},{"@type":"NRID","@value":"9000378113409"},{"@type":"NRID","@value":"9000311506527"},{"@type":"NRID","@value":"9000345330310"},{"@type":"NRID","@value":"9000412600220"},{"@type":"NRID","@value":"9000019072065"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/kkubota"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/kubota-k"}],"foaf:name":[{"@value":"Kaoru Kubota"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581773","@type":"Researcher","foaf:name":[{"@value":"Carlota Escutia"}],"jpcoar:affiliationName":[{"@value":"Instituto Andaluz de Ciencias de la Tierra Consejo Superior de Investigaciones Científicas‐Universidad de Granada Armilla Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581772","@type":"Researcher","foaf:name":[{"@value":"Richard D. Norris"}],"jpcoar:affiliationName":[{"@value":"Scripps Institution of Oceanography University of California San Diego San Diego CA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581765","@type":"Researcher","foaf:name":[{"@value":"Sidney R. Hemming"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Environmental Sciences Lamont‐Doherty Earth Observatory New York NY USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021391860581769","@type":"Researcher","foaf:name":[{"@value":"Ian R. Hall"}],"jpcoar:affiliationName":[{"@value":"School of Earth and Environmental Sciences Cardiff University Cardiff UK"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1891992115473518466","@type":"Researcher","foaf:name":[{"@value":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (Brasil)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115473518468","@type":"Researcher","foaf:name":[{"@value":"Ministerio de Ciencia e Innovación (España)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115473518464","@type":"Researcher","foaf:name":[{"@value":"Universidad de Granada"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115473518469","@type":"Researcher","foaf:name":[{"@value":"Universidad de Salamanca"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115473518470","@type":"Researcher","foaf:name":[{"@value":"CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT)"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115473518465","@type":"Researcher","foaf:name":[{"@value":"International Ocean Discovery Program"}]},{"@id":"https://cir.nii.ac.jp/crid/1891992115473518467","@type":"Researcher","foaf:name":[{"@value":"Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"25724517"},{"@type":"EISSN","@value":"25724525"}],"prism:publicationName":[{"@value":"Paleoceanography and Paleoclimatology"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2023-08-29","prism:volume":"38","prism:number":"9"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://creativecommons.org/licenses/by-nc-nd/4.0/"],"url":[{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2022PA004588"}],"createdAt":"2023-08-18","modifiedAt":"2023-12-19","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=International%20Ocean%20Discovery%20Program","dc:title":"International Ocean Discovery Program"},{"@id":"https://cir.nii.ac.jp/all?q=Miocene/Pliocene","dc:title":"Miocene/Pliocene"},{"@id":"https://cir.nii.ac.jp/all?q=orbital%20forcing","dc:title":"orbital forcing"},{"@id":"https://cir.nii.ac.jp/all?q=Messinian%20Salinity%20Crisis","dc:title":"Messinian Salinity Crisis"},{"@id":"https://cir.nii.ac.jp/all?q=Southern%20African%20Monsoon","dc:title":"Southern African Monsoon"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040285300695321728","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"20H01978"},{"@type":"JGN","@value":"JP20H01978"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20H01978/"}],"notation":[{"@language":"ja","@value":"過去７００万年間の大気中二酸化炭素濃度の連続記録の作成"},{"@language":"en","@value":"Establishment of continuous atmospheric CO2 record for the past 7 million years"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002218436371072","@type":"Article","resourceType":"学術雑誌論文(journal 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simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565164304673664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Indonesian Throughflow drove Australian climate from humid Pliocene to arid Pleistocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093919623808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Planktonic foraminifera stable isotopes and water column structure: Disentangling ecological signals"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095831132800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Eddies and variability in the Mozambique Channel"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580237025753216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New Record of Dust Input and Provenance During Glacial Periods in Western Australia Shelf (IODP Expedition 356, Site U1461) from the Middle 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