{"@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/1362825896323966464.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0016-7037(00)00374-4"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0016703700003744?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0016703700003744?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"80012160255"}}],"dc:title":[{"@value":"Carbon isotopic distribution of methane in deep-sea hydrothermal plume, Myojin Knoll Caldera, Izu-Bonin arc: implications for microbial methane oxidation in the oceans and applications to heat flux estimation"}],"description":[{"notation":[{"@value":"The concentration and stable carbon isotopic composition (δ13C) of methane have been measured for both seafloor hydrothermal venting fluids and effluent plume waters supplied from the vents at the Myojin Knoll Caldera, Izu-Bonin arc, in the western North Pacific. The hydrothermal end-member concentrations and δ13C of methane show near-homogeneity among vents: 41.2 (μmol/kg) and −16.3 ± 0.8 (‰PDB), respectively, while those in the effluent plume are stratified in the caldera and vertically exhibit a large variation (2.1–11 (nmol/kg) and −29.0 to −11.3 (‰PDB), respectively). Comparison of concentration and δ13C data between vent fluids and plume waters suggest that the methane is not conserved but microbially oxidized along with the plume. Gradual decrease of diffusive methane flux in proportion to distance from the vent fields supports the occurrence of significant microbial oxidation within the plume. Assuming steady state emission of methane from the vents, (1) kinetic isotope effect due to the microbial oxidation (k12/k13); (2) methane flux from the vents (Fvents); (3) heat flux from the vents (Q); and (4) average turnover time of hydrothermal methane (Tall) are estimated to be k12/k13 = 1.005 ± 0.001, Fvents = 90–340 (mol/d), Q = 30–110 (MW), and Tall = 60–240 (d), respectively. The estimated turnover times, however, are not uniform within the water column. Around the vents, a turnover time of less than 50 d for methane is one of the shortest values in the pelagic ocean, while those at the distant points correspond to values more typical for deep ocean water."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825896323966465","@type":"Researcher","foaf:name":[{"@value":"Urumu Tsunogai"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896323966464","@type":"Researcher","foaf:name":[{"@value":"Naohiro Yoshida"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896323966593","@type":"Researcher","foaf:name":[{"@value":"Junichiro Ishibashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896323966592","@type":"Researcher","foaf:name":[{"@value":"Toshitaka Gamo"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167037"}],"prism:publicationName":[{"@value":"Geochimica et Cosmochimica Acta"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2000-07","prism:volume":"64","prism:number":"14","prism:startingPage":"2439","prism:endingPage":"2452"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0016703700003744?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0016703700003744?httpAccept=text/plain"}],"createdAt":"2002-07-25","modifiedAt":"2019-04-28","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338803637760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quantifying the effects of clear-cutting and strip-cutting on nitrate dynamics in a forested watershed using triple oxygen isotopes as tracers"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001338805661696","@type":"Article","resourceType":"学術雑誌論文(journal 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Signatures"},{"@value":"化学合成がうみだすもうひとつの深海生態系　　深海化学合成生物群集から出現するベントスのエネルギー獲得戦略：　　軟体部の炭素，窒素および硫黄の安定同位体組成による解析"},{"@language":"ja-Kana","@value":"シンカイ カガク ゴウセイ セイブツ グンシュウ カラ シュツゲン スル ベントス ノ エネルギー カクトク センリャク ナンタイブ ノ タンソ チッソ オヨビ イオウ ノ アンテイ ドウイタイ ソセイ ニ ヨル カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204551654016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Discovery of a new hydrothermal venting site in the southernmost Mariana Arc: Al-rich hydrothermal plumes and white smoker activity associated with biogenic methane"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204552998528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204553003392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Origin and fate of deep-sea seeping methane bubbles at Kuroshima Knoll, Ryukyu forearc region, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204553111296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemical characteristics of hydrothermal fluids at Hatoma Knoll in the southern Okinawa Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205741197824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"超微量の炭素同位体比測定による海底熱水・冷湧水溶存気体に関する研究"},{"@language":"en","@value":"Stable carbon isotopic studies of volatile components in seafloor venting hydrothermal and cold seep fluids, using CF-IRMS"},{"@value":"2000年度日本地球化学会奨励賞受賞記念論文 超微量の炭素同位体比測定による海底熱水・冷湧水溶存気体に関する研究"},{"@language":"ja-Kana","@value":"2000ネンド ニホン チキュウ カガクカイ ショウレイショウ ジュショウ キネン ロンブン チョウビリョウ ノ タンソ ドウイタイヒ ソクテイ ニ ヨル カイテイ ネッスイ レイユウスイ ヨウゾン キタイ ニ カンスル ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205821916288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"深海底熱水孔環境における極限環境微生物の分布・生息量・多様性・生理機能"},{"@language":"en","@value":"Distribution, activity, diversity, and physiological characteristics of extremophiles in deep-sea hydrothermal environments"},{"@language":"ja-Kana","@value":"シンカイテイ ネッスイコウ カンキョウ ニ オケル キョクゲン カンキョウ ビセイブツ ノ ブンプ セイソクリョウ タヨウセイ セイリ キノウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390021920649535744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Oceanographic Studies Using Dissolved Gases as Chemical Tracers"},{"@language":"ja","@value":"海水中の溶存気体をトレーサーとする海洋学的研究"},{"@value":"2005年度日本海洋学会賞受賞記念論文 海水中の溶存気体をトレーサーとする海洋学的研究"},{"@language":"ja-Kana","@value":"2005ネンド ニホン カイヨウ ガッカイショウ ジュショウ キネン ロンブン カイスイチュウ ノ ヨウゾン キタイ オ トレーサー ト スル カイヨウガクテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679205337728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Environmental and Ecological Impact on Deep-sea Environment from Deep-sea Hydrothermal System"},{"@language":"ja","@value":"熱水活動が海洋環境と深海生態系にもたらす影響"},{"@language":"ja-Kana","@value":"ネッスイ カツドウ ガ カイヨウ カンキョウ ト シンカイ セイタイケイ ニ モタラス エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280301696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"海水中のメタンを指標に用いた三宅島周辺海底における火山活動調査の結果について"},{"@language":"en","@value":"Geochemical Exploration of 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