{"@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/1361418521461925376.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2004jc002555"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JC002555"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JC002555"}},{"identifier":{"@type":"NAID","@value":"30013350324"}}],"dc:title":[{"@value":"Interannual and decadal variability of the western Pacific sea surface condition for the years 1787–2000: Reconstruction based on stable isotope record from a Guam coral"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We present a monthly resolved, 213‐year stable isotope time series from a coral from Guam (13°N, 145°E), which is located on the northern edge of the western Pacific warm pool. Oxygen isotopic composition of the coral skeleton (δ<jats:sup>18</jats:sup>O<jats:sub>coral</jats:sub>) shows seasonal, interannual, and decadal variability, which documents significant oceanographic changes related to thermal and hydrologic variations in this region. The δ<jats:sup>18</jats:sup>O<jats:sub>coral</jats:sub> anomaly reflects sea surface temperature (SST) anomaly and sea surface salinity (SSS) anomaly with significant <jats:italic>r</jats:italic> values of −0.69 and 0.49, respectively, which are strongly linked to oceanographic changes that occur during El Niño–Southern Oscillation (ENSO) warm and cool phases. We identified 46 ENSO warm (El Niño) and 53 cool phases (La Niña) in the coral record, which are consistent with those phases reconstructed by Niño 3.4 SST anomaly. Spectral analyses of the δ<jats:sup>18</jats:sup>O<jats:sub>coral</jats:sub> anomaly record for the years 1790–1999 identified significant peaks around ∼3 to ∼7 years. These results indicate that the Guam coral has recorded ENSO periodicity. The δ<jats:sup>18</jats:sup>O<jats:sub>coral</jats:sub> anomaly shows decadal variability of ∼15‐ to ∼45‐year periodicity with significant shifts (<0.2‰) from warmer to cooler condition and vice versa. An accumulative decrease in δ<jats:sup>18</jats:sup>O<jats:sub>coral</jats:sub> time series may imply ∼0.75°C warming of SST and ∼0.23‰ freshening of seawater δ<jats:sup>18</jats:sup>O, corresponding to a decrease of SSS by ∼0.85, in the northwestern tropical Pacific over the last 2 centuries.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276180662656","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00400242"},{"@type":"NRID","@value":"1000000400242"},{"@type":"NRID","@value":"9000391785057"},{"@type":"NRID","@value":"9000258401869"},{"@type":"NRID","@value":"9000370282298"},{"@type":"NRID","@value":"9000350561242"},{"@type":"NRID","@value":"9000347188031"},{"@type":"NRID","@value":"9000412128009"},{"@type":"NRID","@value":"9000383701043"},{"@type":"NRID","@value":"9000383701049"},{"@type":"NRID","@value":"9000412057286"},{"@type":"NRID","@value":"9000345296584"},{"@type":"NRID","@value":"9000258408825"},{"@type":"NRID","@value":"9000257917321"},{"@type":"NRID","@value":"9000347225816"},{"@type":"NRID","@value":"9000019189092"},{"@type":"NRID","@value":"9000398987888"},{"@type":"NRID","@value":"9000256911114"},{"@type":"NRID","@value":"9000283725860"},{"@type":"NRID","@value":"9000396132634"},{"@type":"NRID","@value":"9000258415570"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/70000-22516"}],"foaf:name":[{"@value":"Ryuji Asami"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Paleontology, Graduate School of Science Tohoku University  Sendai 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Yamada"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Paleontology, Graduate School of Science Tohoku University  Sendai 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Iryu"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Paleontology, Graduate School of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016869606943363","@type":"Researcher","foaf:name":[{"@value":"Terrence M. Quinn"}],"jpcoar:affiliationName":[{"@value":"College of Marine Science University of South Florida  St. Petersburg Florida USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016869606943361","@type":"Researcher","foaf:name":[{"@value":"Christopher P. Meyer"}],"jpcoar:affiliationName":[{"@value":"Florida Museum of Natural History University of Florida  Gainesville Florida USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016869606943360","@type":"Researcher","foaf:name":[{"@value":"Gustav Paulay"}],"jpcoar:affiliationName":[{"@value":"Florida Museum of Natural History University of Florida  Gainesville Florida USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2005-05","prism:volume":"110","prism:number":"C5","prism:startingPage":"226"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JC002555"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JC002555"}],"createdAt":"2005-05-26","modifiedAt":"2023-10-12","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=western%20Pacific%20warm%20pool","dc:title":"western Pacific warm pool"},{"@id":"https://cir.nii.ac.jp/all?q=Life%20Sciences","dc:title":"Life Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=Marine%20Biology","dc:title":"Marine Biology"},{"@id":"https://cir.nii.ac.jp/all?q=551","dc:title":"551"},{"@id":"https://cir.nii.ac.jp/all?q=coral","dc:title":"coral"},{"@id":"https://cir.nii.ac.jp/all?q=decadal%20variability","dc:title":"decadal variability"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215937152768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Intraspecific variations in carbon-isotope and oxygen-isotope compositions of a brachiopod Basiliola lucida collected off Okinawa-jima, southwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216846337408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A global multiproxy database for temperature reconstructions of the Common Era"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232352826880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ocean acidification trend in the tropical North Pacific since the mid-20th century reconstructed from a coral 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skeletons for the last several centuries: Reconstruction of interannual, decadal-multidecadal, and centennial variability"},{"@language":"ja-Kana","@value":"カコ スウヒャクネンカン ノ コ キコウ コ カイヨウ ヘンドウ オ キロク スル ゲンセイ サンゴ スウネン スウジュウネン スケール ノ ヘンドウ ト チョウキ ヘンドウ ノ フクゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763121636352","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Theme session “Marine science researches of Okinawa Research Core for Highly Innovative Discipline Science (ORCHIDS) project”"},{"@language":"ja","@value":"テーマセッション報告　琉球大学高度統合型熱帯海洋科学技術イノベーション創出研究拠点形成事業（ORCHIDS）プロジェクトにおける海洋科学研究の取組み"},{"@value":"琉球大学高度統合型熱帯海洋科学技術イノベーション創出研究拠点形成事業(ORCHIDS)プロジェクトにおける海洋科学研究の取組み"},{"@language":"ja-Kana","@value":"リュウキュウ ダイガク コウド トウゴウガタ ネッタイ カイヨウ カガク ギジュツ イノベーション ソウシュツ ケンキュウ キョテン ケイセイ ジギョウ(ORCHIDS)プロジェクト ニ オケル カイヨウ カガク ケンキュウ ノ 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