{"@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/1363670320435546752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0016-7037(97)00169-5"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0016703797001695?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0016703797001695?httpAccept=text/plain"}}],"dc:title":[{"@value":"Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381412890074111621","@type":"Researcher","foaf:name":[{"@value":"Sang-Tae Kim"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320435546753","@type":"Researcher","foaf:name":[{"@value":"James R. O'Neil"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167037"}],"prism:publicationName":[{"@value":"Geochimica et Cosmochimica Acta"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1997-08","prism:volume":"61","prism:number":"16","prism:startingPage":"3461","prism:endingPage":"3475"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0016703797001695?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0016703797001695?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-30","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/1360002215857649408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrothermal carbonate chimneys from a continental rift (Afar Rift): Mineralogy, geochemistry, and mode of formation"}]},{"@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/1360004232469445632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature and seawater isotopic controls on two stalagmite records since 83 ka from maritime Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233533383424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tracking the migration of the Indian continent using the carbonate clumped isotope technique on Phanerozoic soil carbonates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168797177216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nitrogenous Altered Volcanic Glasses as Targets for Mars Sample Return: Examples From Antarctica and Iceland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017279838991232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Determination of temperature-dependent otolith oxygen stable isotope fractionation on chum salmon Oncorhynchus keta based on rearing experiment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282206565248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentological and geochemical properties of authigenic carbonates in Kyushu, Japan: Implications for the transition from semi-arid to humid climate during the Eocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282213499008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid and precise measurement of carbonate clumped isotopes using laser spectroscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021389805550080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oxygen isotopes of the <scp>Japanese</scp> stalagmites as global and local paleoclimate proxies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021389812583296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Millennial-scale paleotemperature change in the Japan Sea during Marine Isotope Stage 3: Impact of meridional oscillation of the subpolar front"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689327699456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evaluation of oxygen isotope and Mg/Ca ratios in high‐magnesium calcite from benthic foraminifera as a proxy for water temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690893102336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oxygen isotopic ratios of primordial water in carbonaceous chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285706367424896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oxygen and carbon isotope records of cultured freshwater pearl mussel Hyriopsis sp. shell from Lake Kasumigaura, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707128234880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature dependence of δ 18 O in otolith of juvenile Japanese sardine: Laboratory rearing experiment with micro-scale analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707446021632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A 500,000 year record of Indian summer monsoon dynamics recorded by eastern equatorial Indian Ocean upper water-column structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285714381410304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Otolith δ18O of Pacific bluefin tuna Thunnus orientalis as an indicator of ambient water temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285715168219264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variation in stable carbon and oxygen isotopes of individual benthic foraminifera: tracers for quantifying the magnitude of isotopic disequilibrium"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617811355904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Genesis and diagenesis of travertine, Futamata hot spring, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643734529920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Glendonite concretion formation due to dead organism decomposition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298755605834880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Relationship Between the Global Mean Deep‐Sea and Surface Temperature During the Early Eocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298757205290240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Isotopic evidence concerning the habitat of Nautilus macromphalus in New Caledonia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905607539584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A review of benthic foraminiferal oxygen and carbon isotopes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165890632320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Comprehensive study of carbon and oxygen isotopic compositions, trace element abundances, and cathodoluminescence intensities of calcite in the Murchison CM chondrite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166017534976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mg/Ca and δ18O in the brackish shallow-water benthic foraminifer Ammonia ‘beccarii’"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182054555008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mineralogical, geochemical and isotopic characterization of authigenic carbonates from the methane-bearing sediments of the Bering Sea continental margin (IODP Expedition 323, Sites U1343–U1345)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567187546299648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Carbon and Oxygen Isotope Records from Tridacna derasa Shells: Toward Establishing a Reliable Proxy for Sea Surface Environments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568466840957440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Resetting Southern Tibet: The serious challenge of obtaining primary records of Paleoaltimetry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640867432192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature and depth distribution of Japanese eel eggs estimated using otolith oxygen stable isotopes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657031017984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oxygen isotopic distribution along the otolith growth axis by secondary ion mass spectrometry: Applications for studying ontogenetic change in the depth inhabited by deep-sea fishes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065755648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Clumped isotope signatures of methane-derived authigenic carbonate presenting equilibrium values of their formation temperatures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657096796288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Precise oxygen and hydrogen isotope determination in nanoliter quantities of speleothem inclusion water by cavity ring-down spectroscopic techniques"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657096914432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of elevated CO2 on shell 13C and 18O content and growth rates in the clam Scapharca broughtonii"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657096930816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seasonal temperature changes obtained from carbonate clumped isotopes of annually laminated tufas from Japan: Discrepancy between natural and synthetic calcites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657283122560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Calibration between temperature and Mg/Ca and oxygen isotope ratios in high-magnesium calcite tests of asexually reproduced juveniles of large benthic foraminifers"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657350150912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cool eastern rim of the North Pacific during Late Cretaceous time: A seep-carbonate paleothermometry from the Nanaimo Group, British Columbia, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660458019584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late <scp>H</scp>olocene coral reef environment recorded in <scp>T</scp>ridacnidae shells from archaeological sites in <scp>O</scp>kinawa‐jima, subtropical southwestern <scp>J</scp>apan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848665122237696","@type":"Article","resourceType":"preprint","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variation in stable carbon and oxygen isotopes of individual benthic foraminifera: tracers for quantifying the vital effect"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849941809493632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Carbon isotopic evolution of aqueous fluids in CM chondrites: Clues from in-situ isotope analyses within calcite grains in Yamato-791198"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567780577280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Formation of coalbed methane and water-dissolved gas in Kushiro Coal Mine, Japan, based on isotopic compositions of gas, groundwater, and calcite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707355841536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vertical habitat shifts of juvenile jack mackerel estimated using otolith oxygen stable isotope"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865816794728192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Impact of High Methane Flux on the Properties of Pore Fluid and Methane-Derived Authigenic Carbonate in the ARAON Mounds, Chukchi Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855113266816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Holocene Temperature Trend Inferred From Oxygen and Carbonate Clumped Isotope Profiles of a Stalagmite Collected From a Maritime Area of Central Honshu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360870485028428544","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Carbonation of oceanic serpentinite related to extensive intraplate magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131418282622592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Equatorial Pacific seawater pCO2 variability since the last glacial period"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412890074111616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coral Sclerochronology: Similarities and Differences in the Coral Isotopic Signatures Between Mesophotic and Shallow-Water Reefs"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694366747789824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Millennial-scale fluctuations in water volume transported by the Tsushima Warm Current in the Japan Sea during the Holocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472583808","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"海生二枚貝類の貝殻を用いた成長線解析・酸素同位体比分析─完新世環境変動の高分解能解析─"},{"@language":"en","@value":"Combined sclerochronological and oxygen isotope analyses of marine bivalve shells to examine high-resolution Holocene environmental changes"},{"@value":"海生二枚貝類の貝殻を用いた成長線解析・酸素同位体比分析 : 完新世環境変動の高分解能解析"},{"@language":"ja-Kana","@value":"カイセイ ニマイガイルイ ノ カイガラ オ モチイタ セイチョウセン カイセキ ・ サンソ ドウイタイヒ ブンセキ : カンシン セイ カンキョウ ヘンドウ ノ コウブンカイノウ カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390586886835658752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"浮遊性有孔虫の酸素同位体比に基づく過去9,600年間の下北半島東方沖の古環境推定"},{"@language":"en","@value":"Paleoenvironmental reconstruction off the Shimokita Peninsula during the past 9,600 years based on planktonic foraminiferal δ<sup>18</sup>O"},{"@language":"ja-Kana","@value":"フユウセイユウコウチュウ ノ サンソ ドウイタイヒ ニ モトズク カコ 9,600ネンカン ノ シモキタ ハントウ トウホウオキ ノ コ カンキョウ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390858131665282176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Large ammonoid shellbed and huge calcareous concretion bed in shallow-marine fine sandstone of the lower Coniacian Ashizawa Formation, Futaba Group, Northeast Japan"},{"@language":"ja","@value":"双葉層群足沢層（上部白亜系コニアシアン階下部）浅海成細粒砂岩の大型アンモナイト密集層と巨大炭酸塩コンクリーション濃集層"}]},{"@id":"https://cir.nii.ac.jp/crid/1521980705982216704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Carbon and oxygen isotope records of Tridacna squamosa shells from two different latitudes in the Ryukyu Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1523669554996656384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Individual migration pathways of modern planktic foraminifers : Chamber-by-chamber assessment of stable isotopes"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942151460992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of ocean environment time series since the late nineteenth century using sclerosponge geochemistry in the northwestern subtropical Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942189472128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"δ18Osw estimate for Globigerinoides ruber from core-top sediments in the East China Sea"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0016-7037(97)00169-5"},{"@type":"CROSSREF","@value":"10.1038/srep22187_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gloplacha.2020.103194_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2018.03.006_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1029/2021je007052_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.3389/fmars.2022.1072068_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00434-7_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2022.106280_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1126/sciadv.abq0611_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1111/iar.12491_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2023.111713_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1002/2016jg003587_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1007/s10933-009-9341-8_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.3354/meps10202_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.5194/bg-9-4353-2012_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2018.10.016_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.2517/2020pr003_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2020.105706_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2021.106075_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2022.0049_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1029/2022pa004532_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1371/journal.pone.0271235_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.4116/jaqua.64.2302_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2024.108896_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1371/journal.pone.0157659_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2018.05.030_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1111/iar.12076_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0048-3_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.5194/bgd-9-6191-2012_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2018.07.004_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.fishres.2017.05.004_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2018.05.016_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2010.11.003_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.coal.2020.103577_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2022.102897_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.3389/fmars.2022.944841_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1111/iar.70002_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1130/b38019.1_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2018.05.024_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1038/s41598-019-49739-0_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.dsr2.2014.03.011_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1007/978-3-319-92735-0_36_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2015.09.017_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2014.08.019_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.4116/jaqua.57.19_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2015.04.010_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gloplacha.2019.103028_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2013.07.031_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2013.03.026_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2017.09.027_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.dsr.2013.10.006_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.2517/2015pr036_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2020.02.003_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.02.005_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2017.10.046_references_DOI_Gwu9EEoYFUVJJyXQIXWnmW0DuFS"}]}