{"@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/1360005518173438592.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2019jb018466"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2019JB018466"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB018466"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019JB018466"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB018466"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Relative Sea‐Level Changes Over the Past Centuries in the Central Ryukyu Arc Inferred From Coral Microatolls"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>This study focuses on Okinawa and Yoron islands, in order to better understand tectonics in the Ryukyu Arc related to the subduction zone. We used coral microatolls—known for their centimetric accuracy in the record of relative sea‐level (RSL) changes—to reconstruct RSL changes over the last century from living microatolls. A fossil microatoll in Yoron was used to discuss possible RSL changes beyond the last century. The signal consists of emergence whose rate varies through time, interrupted by decadal to multidecadal periods of sudden and/or gradual submergence and by interannual sea‐level falls. Comparison with other existing RSL records in the arc highlights RSL variability along the arc. This pattern contrasts with the homogeneous and linear absolute regional sea‐level rise, implying that this latter signal cannot fully explain our observations and that an additional process is required. We suggest the subduction zone as a possible source for generating centimetric scale RSL changes observed in coral microatolls. We tested how the Ryukyu megathrust could explain our observations with elastic dislocation modeling. The emergence trend could be explained by interseismic loading on the plate interface with a minimum coupling rate of 25%, which is higher than previous estimates based on short instrumental records. As for the submergence events that occurred regularly in the coral record, we show that they could be explained by slow slip events on the shallower part of the megathrust or in the transition zone. Such process could accommodate a significant part of the total convergence.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380005518173438976","@type":"Researcher","foaf:name":[{"@value":"J. Weil‐Accardo"}],"jpcoar:affiliationName":[{"@value":"Now at CEREGE Aix‐Marseille University  Aix‐en Provence France"},{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438720","@type":"Researcher","foaf:name":[{"@value":"N. Feuillet"}],"jpcoar:affiliationName":[{"@value":"Institut de Physique du Globe de Paris Sorbonne Paris University, Paris‐Diderot University, UMR 7154  Paris France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173439107","@type":"Researcher","foaf:name":[{"@value":"K. Satake"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438726","@type":"Researcher","foaf:name":[{"@value":"T. Goto"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438723","@type":"Researcher","foaf:name":[{"@value":"K. Goto"}],"jpcoar:affiliationName":[{"@value":"International Research Institute of Disaster Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438850","@type":"Researcher","foaf:name":[{"@value":"T. Harada"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438851","@type":"Researcher","foaf:name":[{"@value":"H. Kayanne"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science University of Tokyo  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438721","@type":"Researcher","foaf:name":[{"@value":"M. Nakamura"}],"jpcoar:affiliationName":[{"@value":"Faculty of Science University of the Ryukyus  Okinawa Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438979","@type":"Researcher","foaf:name":[{"@value":"N. Ramos"}],"jpcoar:affiliationName":[{"@value":"National Institute of Geological Sciences University of the Philippines‐Diliman  Quezon City Philippines"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173439104","@type":"Researcher","foaf:name":[{"@value":"J.‐M. Saurel"}],"jpcoar:affiliationName":[{"@value":"Institut de Physique du Globe de Paris Sorbonne Paris University, Paris‐Diderot University, UMR 7154  Paris France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438725","@type":"Researcher","foaf:name":[{"@value":"K. Sowa"}],"jpcoar:affiliationName":[{"@value":"Japan Agency for Marine‐Earth Science and Technology  Kanagawa Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173439105","@type":"Researcher","foaf:name":[{"@value":"S.‐C. Liu"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences National Taiwan University  Taipei Taiwan ROC"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173438848","@type":"Researcher","foaf:name":[{"@value":"T.‐L. Yu"}],"jpcoar:affiliationName":[{"@value":"Now at CEREGE Aix‐Marseille University  Aix‐en Provence France"},{"@value":"Department of Geosciences National Taiwan University  Taipei Taiwan ROC"},{"@value":"Research Center for Future Earth National Taiwan University  Taipei Taiwan ROC"}]},{"@id":"https://cir.nii.ac.jp/crid/1380005518173439108","@type":"Researcher","foaf:name":[{"@value":"C.‐C. Shen"}],"jpcoar:affiliationName":[{"@value":"Now at CEREGE Aix‐Marseille University  Aix‐en Provence France"},{"@value":"Department of Geosciences National Taiwan University  Taipei Taiwan ROC"},{"@value":"Research Center for Future Earth National Taiwan University  Taipei Taiwan ROC"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1893116918046175375","@type":"Researcher","foaf:name":[{"@value":"Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1893116918046175373","@type":"Researcher","foaf:name":[{"@value":"The University of Tokyo 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Sendai"}]},{"@id":"https://cir.nii.ac.jp/crid/1891147691428088066","@type":"Researcher","foaf:name":[{"@value":"National Taiwan University Taiwan (NTU)"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union 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