{"@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/1361418520168959488.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s00338-003-0323-4"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s00338-003-0323-4.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s00338-003-0323-4/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s00338-003-0323-4"}},{"identifier":{"@type":"HANDLE","@value":"1885/74986"}}],"dc:title":[{"@value":"Skeletal isotope microprofiles of growth perturbations in Porites corals during the 1997?1998 mass bleaching event"}],"description":[{"notation":[{"@value":"Severe coral bleaching occurred throughout the tropics in 1997/98. We report high-resolution skeletal oxygen isotope (δ18O) and carbon isotope (δ13C) microprofiles for bleached corals from Pandora Reef, Great Barrier Reef, and Ishigaki Island, Japan, in order to examine the ability of Porites corals to record clear signals of bleaching. Analysis of the annual cycle in δ18O revealed abrupt reductions in skeletal extension immediately after the 1997–98 summer temperature maximum, indicating that bleaching inhibits coral calcification. Skeletal δ13C in the Ishigaki corals showed lower values during bleaching, indicating depressed coral metabolism associated with a reduction in calcification. In contrast, microprofiles of skeletal δ13C from the shaded sides of Pandora Reef corals exhibited little change, possibly because algal photosynthesis was already slow prior to bleaching, thus subduing the 13C-response to bleaching. Comparison of δ18O microprofiles from bleached corals with instrumental temperature records showed that Porites corals can recover following 5 months with little skeletogenesis. The results indicate that isotopic microprofiling may be the key to identifying gaps in coral growth that are diagnostic of past bleaching events. We have tested this hypothesis using blue UV fluorescent bands to guide us to coral skeleton where isotope microprofiling identifies bleaching events in 1986, 1989, and 1990. These events, detected by proxy, suggest that coral bleaching may have occurred more commonly on Ishigaki Island than previously recorded."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004230880237319","@type":"Researcher","foaf:name":[{"@value":"A. Suzuki"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520168959491","@type":"Researcher","foaf:name":[{"@value":"M. K. Gagan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520168959489","@type":"Researcher","foaf:name":[{"@value":"K. Fabricius"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520168959490","@type":"Researcher","foaf:name":[{"@value":"P. J. Isdale"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520168959492","@type":"Researcher","foaf:name":[{"@value":"I. Yukino"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520168959493","@type":"Researcher","foaf:name":[{"@value":"H. Kawahata"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"07224028"},{"@type":"EISSN","@value":"14320975"}],"prism:publicationName":[{"@value":"Coral Reefs"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2003-12-01","prism:volume":"22","prism:number":"4","prism:startingPage":"357","prism:endingPage":"369"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s00338-003-0323-4.pdf"},{"@id":"http://link.springer.com/article/10.1007/s00338-003-0323-4/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s00338-003-0323-4"}],"createdAt":"2003-12-23","modifiedAt":"2019-05-28","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Porites","dc:title":"Porites"},{"@id":"https://cir.nii.ac.jp/all?q=Aquatic%20Science","dc:title":"Aquatic Science"},{"@id":"https://cir.nii.ac.jp/all?q=Great%20Barrier%20Reef","dc:title":"Great Barrier Reef"},{"@id":"https://cir.nii.ac.jp/all?q=Skeletogenesis","dc:title":"Skeletogenesis"},{"@id":"https://cir.nii.ac.jp/all?q=skeleton","dc:title":"skeleton"},{"@id":"https://cir.nii.ac.jp/all?q=oxygen%20isotope","dc:title":"oxygen isotope"},{"@id":"https://cir.nii.ac.jp/all?q=Photosynthesis","dc:title":"Photosynthesis"},{"@id":"https://cir.nii.ac.jp/all?q=Invertebrata","dc:title":"Invertebrata"},{"@id":"https://cir.nii.ac.jp/all?q=Porites%20Carbon%20isotopes","dc:title":"Porites Carbon isotopes"},{"@id":"https://cir.nii.ac.jp/all?q=algae","dc:title":"algae"},{"@id":"https://cir.nii.ac.jp/all?q=Pacific%20Ocean","dc:title":"Pacific Ocean"},{"@id":"https://cir.nii.ac.jp/all?q=Australasia","dc:title":"Australasia"},{"@id":"https://cir.nii.ac.jp/all?q=Australia","dc:title":"Australia"},{"@id":"https://cir.nii.ac.jp/all?q=coral%20bleaching","dc:title":"coral bleaching"},{"@id":"https://cir.nii.ac.jp/all?q=Anthozoa","dc:title":"Anthozoa"},{"@id":"https://cir.nii.ac.jp/all?q=Oxygen%20isotopes","dc:title":"Oxygen isotopes"},{"@id":"https://cir.nii.ac.jp/all?q=Coral%20Sea","dc:title":"Coral Sea"},{"@id":"https://cir.nii.ac.jp/all?q=Queensland","dc:title":"Queensland"},{"@id":"https://cir.nii.ac.jp/all?q=Keywords:%20coral","dc:title":"Keywords: coral"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050285299931820288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A simple role of coral-algal symbiosis in coral calcification based on multiple geochemical tracers"},{"@value":"The simple role of coral-algal symbiosis in coral calcification is based on multiple geochemical tracers"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456409729792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influence of Land Development on Holocene Porites Coral Calcification at Nagura Bay, Ishigaki Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229807527808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multidecadal oceanographic changes in the western <scp>P</scp>acific detected through high‐resolution bomb‐derived radiocarbon measurements on corals"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230880235648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frontiers of Coral-Based Sclerochronological Studies in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231175786240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mg isotope fractionation in biogenic carbonates of deep-sea coral, benthic foraminifera, and hermatypic coral"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231209642624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evaluation of Mn and Fe in coral skeletons (Porites spp.) as proxies for sediment loading and reconstruction of 50 yrs of land use on Ishigaki Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298755640737920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recent Relative Sea‐Level Changes Recorded by Coral Microatolls in Southern Ryukyus Islands, Japan: Implication for the Seismic Cycle of the Megathrust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088707968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Growth-rate influences on coral climate proxies tested by a multiple colony culture experiment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182957959168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine Reservoir Effects Deduced from <sup>14</sup>C Dates on Pottery Residues, Bones, and Molluskan Shells from the Hamanaka 2 Archaeological Site, Rebun Island, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185955838720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami recurrence revealed by Porites coral boulders in the southern Ryukyu Islands, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641760353408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermoluminescence of coral skeletons: a high-sensitivity proxy of diagenetic alteration of aragonite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660727508608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of acidified seawater on calcification, photosynthetic efficiencies and the recovery processes from strong light exposure in the coral <i>Stylophora pistillata</i>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849942791398784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Insight into Western Pacific Circulation from South China Sea Coral Skeletal Radiocarbon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815502951424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Assessment of chemical compositions in coral skeletons (Acropora digitifera and Porites australiensis) as temperature proxies"}]},{"@id":"https://cir.nii.ac.jp/crid/1363101970105489024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Non-bleached colonies of massive\n                    <i>Porites</i>\n                    may attract fishes for selective grazing during mass bleaching events"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204484856704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coral skeletal luminescence- its causes and availability as a paleoenvironmental proxy"},{"@language":"ja","@value":"サンゴ骨格の発光バンドの発光原因と環境指標としての可能性"},{"@language":"ja-Kana","@value":"サンゴ コッカク ノ ハッコウ バンド ノ ハッコウ ゲンイン ト カンキョウ シヒョウ ト シテ ノ カノウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204552336640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Skeletal isotopic responses of the Scleractinian coral <i>Isopora palifera </i>to experimentally controlled water temperatures"},{"@value":"Skeletal isotopic responses of the Scleractinian coral Isopora palifera to experimentally controlled water temperatures"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204553609600","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mid-Holocene sea-surface temperature reconstruction using fossil corals from Kume Island, Ryukyu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204554088320","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coral growth-rate insensitive Sr/Ca as a robust temperature recorder at the extreme latitudinal limits of <i>Porites</i>"},{"@value":"Coral growth-rate insensitive Sr/Ca as a robust temperature recorder at the extreme latitudinal limits of Porites"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205299558272","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoclimate reconstruction and future forecast based on coral skeletal climatology"},{"@value":"サンゴ骨格分析による過去の気候変遷の復元"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680271536384","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoclimate reconstruction and future forecast based on coral skeletal climatology"},{"@language":"ja","@value":"サンゴ骨格分析による過去の気候変遷の復元"}]},{"@id":"https://cir.nii.ac.jp/crid/1390291767808286464","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A review of the influence of ocean acidification on marine organisms in coral reefs"},{"@language":"ja","@value":"海洋酸性化がサンゴ礁域の石灰化生物に及ぼす影響"},{"@language":"ja-Kana","@value":"カイヨウ サンセイカ ガ サンゴショウイキ ノ セッカイカ セイブツ ニ オヨボス エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942136465280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Perspective on the response of marine calcifiers to global warming and ocean acidification : behavior of corals and foraminifera in a high CO2 world “hot house”"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s00338-003-0323-4"},{"@type":"OPENAIRE","@value":"doi_dedup___::9a9a26b0cb4bb86bd6a4d470926b4c17"},{"@type":"CROSSREF","@value":"10.1002/2017gc006854_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1007/978-981-10-6473-9_6_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1007/s00216-011-5264-0_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1007/s00338-014-1128-3_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.5571/syntheng.5.78_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0259_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.3755/jcrs.12.1_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0317_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1029/2022gc010587_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1017/rdc.2016.93_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1130/g34415.1_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0207_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.19.1_21_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1038/s41598-017-18269-y_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1111/maec.12444_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0239-9_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1371/journal.pone.0088790_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1017/rdc.2019.145_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.5571/synth.5.80_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2018.05.016_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.3389/fmars.2024.1329924_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.11.046_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"},{"@type":"CROSSREF","@value":"10.7717/peerj.3470_references_DOI_KX9jvqwzQhaziDcJyMIRUykjMkh"}]}