{"@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/1361699994338714240.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.sedgeo.2008.01.011"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073808002108?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073808002108?httpAccept=text/plain"}}],"dc:title":[{"@value":"Holocene coral reef development under windward and leeward locations at Ishigaki Island, Ryukyu Islands, Japan"}],"description":[{"notation":[{"@value":"Abstract   Coral reef growth is largely controlled by the wave energy associated with ocean swells and local winds. This growth has responded to changes in wave conditions that evolved in concert with Holocene sea-level changes. We analyzed Holocene facies of the Ibaruma and Fukido reefs of Ishigaki Island, southern Ryukyu Islands, in the context of temporal and spatial changes in wave conditions by comparing present-day coral assemblages and internal (fossil) reef facies. Four major coral assemblages that developed under different wave-energy conditions were recognized. Six cores recorded a Holocene reef sequence consisting of four sedimentary facies that differed in the relative volumes of four coral taxa: Acropora digitifera and Acropora hyacinthus, and lesser amounts of Favia stelligera and Montastrea curta. Holocene windward reef growth began at 7820 cal. years BP after flooding of the Pleistocene reef limestone surface; the ensuing reef growth kept up with the rapid sea-level rise. A vertical growth rate of 7.5 m/1000 years during reef nucleation and early growth stages decreased to 3.5 m/1000 years during the main stage of reef framework development. The uppermost part of the windward reef consisted of a very robust framework, unlike the open framework of the leeward reef. Ages indicated that the uppermost leeward reef was ca. 3000 years younger than the uppermost windward reef. These variations in facies development and timing were caused by differences in local wind-driven wave conditions."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030003658305253504","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000019087346"},{"@type":"NRID","@value":"9000020648334"},{"@type":"NRID","@value":"9000258216854"},{"@type":"NRID","@value":"9000255330471"},{"@type":"NRID","@value":"9000383701046"},{"@type":"NRID","@value":"9000258414859"},{"@type":"NRID","@value":"9000259324141"},{"@type":"NRID","@value":"9000020107604"},{"@type":"NRID","@value":"9000283626627"},{"@type":"NRID","@value":"9000258416652"},{"@type":"NRID","@value":"9000347166586"},{"@type":"KAKEN_RESEARCHERS","@value":"90555038"},{"@type":"NRID","@value":"1000090555038"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0139370"}],"foaf:name":[{"@value":"Chuki Hongo"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994338714240","@type":"Researcher","foaf:name":[{"@value":"Hajime Kayanne"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00370738"}],"prism:publicationName":[{"@value":"Sedimentary Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2009-02","prism:volume":"214","prism:number":"1-4","prism:startingPage":"62","prism:endingPage":"73"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0037073808002108?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0037073808002108?httpAccept=text/plain"}],"createdAt":"2008-10-29","modifiedAt":"2025-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215296685568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous dissolved organic nitrogen supply over a coral reef: first evidence from nitrogen stable 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Yakushima Island, Japan"},{"@language":"ja-Kana","@value":"ヤクシマ エンガンイキ ノ ガンバン ロトウ ニ オケル タンイツ ワレメ ナイ ノ ジュウテンブツ ノ ネンダイチ ト ソノ ヘンドウ ヨウイン ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207458944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-resolution Holocene Sea-level Change Based on Coral Reefs and Hermatypic Corals"},{"@language":"ja","@value":"サンゴ礁と造礁サンゴを用いた完新世の高精度海面変動復元にむけて"},{"@language":"ja-Kana","@value":"サンゴショウ ト ゾウショウサンゴ オ モチイタ カンシン セイ ノ コウセイド カイメン ヘンドウ フクゲン ニ ムケテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213692032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Problems and perspectives regarding drilling through coral reefs: the reconstruction of Holocene coral-reef 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