{"@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/1390282680197309824.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4096/jssj.73.121"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"026086577"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/026086577"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I026086577"}},{"identifier":{"@type":"NAID","@value":"130004940411"}}],"dc:title":[{"@language":"ja","@value":"半遠洋性泥の有機炭素沈積流量変化，最終氷期末期〜後氷期，南海トラフ沿い前弧海盆の例"},{"@language":"en","@value":"Accumulation rate of organic carbon in hemipelagic mud, examples from the forearc basins along the Nankai Trough Japan during the last glacial maximum to deglaciation"},{"@language":"ja-Kana","@value":"ハンエンヨウセイ デイ ノ ユウキ タンソチンセキ リュウリョウ ヘンカ,サイシュウヒョウ キマツキ~コウヒョウキ,ナンカイ トラフ ゾイ ゼン コカイボン ノ レイ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"In this study, variations of organic carbon accumulation rate in hemipelagic mud during the end of last glacial period to deglaciation were examined in the two different depositional environments in the forearc basins along the Nankai Trough, such as on the deep-sea fan which connected submarine canyon and deep-sea floor where is far from the canyon mouth.  The sediment of deep-sea fan contained several turbidite layers during the end of last glacial period, and the depositional frequencies of turbidites were decrease with sea-level rise during the deglaciation.  On the other hand, turbidites were not recognized in the deep-sea floor sediments that were deposited far from the submarine canyon.  The accumulation rate of organic carbon and terrigenous contents were high during the end of last glacial period, while those were low and the most of organic carbon is marine origin in the both depositional environments during the deglaciation."},{"@language":"ja","@value":"この論文では，南海トラフ沿いの前弧海盆周辺において，海底扇状地のタービダイトを含む堆積物と海底谷から離れた海盆底のタービダイトを含まない堆積物を対象に，半遠洋性泥に含まれる有機炭素の沈積流量変化に注目して，それらの堆積場による違いと時代変化を検討した．海水準変動の影響を受けてタービダイトの堆積頻度が変化する場所でも，タービダイトは認められず半遠洋性泥が連続して堆積したと見られる場所でも，半遠洋性泥に含まれる有機炭素の沈積流量は同様の変化を示した．すなわち，最終氷期最盛期末期には有機炭素沈積流量が大きく，陸源有機炭素の割合が比較的高い．後氷期以降には有機炭素沈積流量は小さくなりそのほとんどが海洋プランクトン起源の有機炭素であった．"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326220392320","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40356423"},{"@type":"NRID","@value":"1000040356423"},{"@type":"NDL_AUTHOR_ID","@value":"00884527"},{"@type":"NRID","@value":"9000021563626"},{"@type":"NRID","@value":"9000386336934"},{"@type":"NRID","@value":"9000254061942"},{"@type":"NRID","@value":"9000262362945"},{"@type":"NRID","@value":"9000391784965"},{"@type":"NRID","@value":"9000347136123"},{"@type":"NRID","@value":"9000018366682"},{"@type":"NRID","@value":"9000365017237"},{"@type":"NRID","@value":"9000002496683"},{"@type":"NRID","@value":"9000006909446"},{"@type":"NRID","@value":"9000370281520"},{"@type":"NRID","@value":"9000002479732"},{"@type":"NRID","@value":"9000386338342"},{"@type":"NRID","@value":"9000386336844"},{"@type":"NRID","@value":"9000241768267"},{"@type":"NRID","@value":"9000018706973"},{"@type":"NRID","@value":"9000391785294"},{"@type":"NRID","@value":"9000386336810"},{"@type":"NRID","@value":"9000254262707"},{"@type":"NRID","@value":"9000409996117"},{"@type":"NRID","@value":"9000018657099"},{"@type":"NRID","@value":"9000020575420"},{"@type":"NRID","@value":"9000245917819"},{"@type":"NRID","@value":"9000389942736"},{"@type":"NRID","@value":"9000403550595"},{"@type":"NRID","@value":"9000399571587"},{"@type":"NRID","@value":"9000009939105"},{"@type":"NRID","@value":"9000018350496"},{"@type":"NRID","@value":"9000386338335"},{"@type":"NRID","@value":"9000345426790"},{"@type":"NRID","@value":"9000399376861"},{"@type":"NRID","@value":"9000018862115"},{"@type":"NRID","@value":"9000019030045"},{"@type":"NRID","@value":"9000004617781"},{"@type":"NRID","@value":"9000316693026"},{"@type":"NRID","@value":"9000283115991"},{"@type":"NRID","@value":"9000018393723"},{"@type":"NRID","@value":"9000001058157"},{"@type":"NRID","@value":"9000014233943"},{"@type":"NRID","@value":"9000391785124"},{"@type":"NRID","@value":"9000014442973"},{"@type":"NRID","@value":"9000403551372"},{"@type":"NRID","@value":"9000258409947"},{"@type":"NRID","@value":"9000254585792"},{"@type":"NRID","@value":"9000389439277"},{"@type":"NRID","@value":"9000386338042"},{"@type":"NRID","@value":"9000403550288"},{"@type":"NRID","@value":"9000410949824"},{"@type":"NRID","@value":"9000240102741"},{"@type":"NRID","@value":"9000403550195"},{"@type":"NRID","@value":"9000009972636"},{"@type":"NRID","@value":"9000001086746"},{"@type":"NRID","@value":"9000237765739"},{"@type":"NRID","@value":"9000398150798"},{"@type":"NRID","@value":"9000016658940"},{"@type":"NRID","@value":"9000414373459"},{"@type":"NRID","@value":"9000386337059"},{"@type":"NRID","@value":"9000386337056"},{"@type":"NRID","@value":"9000386337032"},{"@type":"NRID","@value":"9000258408389"},{"@type":"NRID","@value":"9000241764500"},{"@type":"NRID","@value":"9000254585910"},{"@type":"NRID","@value":"9000414200628"},{"@type":"NRID","@value":"9000410949823"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/linkike00"}],"foaf:name":[{"@language":"ja","@value":"池原 研"},{"@language":"en","@value":"Ikehara Ken"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geology and Geoinformation, Geological Survey of Japan, AIST"},{"@language":"ja","@value":"産業技術総合研究所地質情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658617851008","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80401298"},{"@type":"NRID","@value":"1000080401298"},{"@type":"NRID","@value":"9000004606146"},{"@type":"NRID","@value":"9000018986609"},{"@type":"NRID","@value":"9000347166481"},{"@type":"NRID","@value":"9000283590885"},{"@type":"NRID","@value":"9000009416327"},{"@type":"NRID","@value":"9000256721588"},{"@type":"NRID","@value":"9000386338339"},{"@type":"NRID","@value":"9000345426706"},{"@type":"NRID","@value":"9000350559559"},{"@type":"NRID","@value":"9000256721376"},{"@type":"NRID","@value":"9000350559803"},{"@type":"NRID","@value":"9000283726536"},{"@type":"NRID","@value":"9000256721500"},{"@type":"NRID","@value":"9000283904025"},{"@type":"NRID","@value":"9000017395962"},{"@type":"NRID","@value":"9000017552832"},{"@type":"NRID","@value":"9000256721520"},{"@type":"NRID","@value":"9000256721449"},{"@type":"NRID","@value":"9000256721459"},{"@type":"NRID","@value":"9000403551384"},{"@type":"NRID","@value":"9000326270636"},{"@type":"NRID","@value":"9000283904042"},{"@type":"NRID","@value":"9000361693205"},{"@type":"NRID","@value":"9000258411603"},{"@type":"NRID","@value":"9000256721492"},{"@type":"NRID","@value":"9000347136124"},{"@type":"NRID","@value":"9000347136980"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/-oa"}],"foaf:name":[{"@language":"ja","@value":"大村 亜希子"},{"@language":"en","@value":"Omura Akiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"JSPS Research Fellow, Graduate School of Frontier Science, The University of Tokyo"},{"@language":"ja","@value":"日本学術振興会特別研究員，東京大学大学院新領域創成科学研究科"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"1342310X"},{"@type":"EISSN","@value":"18829457"},{"@type":"CODEN","@value":"TAKEF6"},{"@type":"NDL_BIB_ID","@value":"000000099615"},{"@type":"ISSN","@value":"1342310X"},{"@type":"LISSN","@value":"1342310X"},{"@type":"NCID","@value":"AA11155966"}],"prism:publicationName":[{"@language":"ja","@value":"堆積学研究"},{"@language":"en","@value":"Journal of the Sedimentological Society of Japan"},{"@language":"en","@value":"Jour. Sed. Soc. Japan"},{"@language":"en","@value":"Journal of the Sedimentological Society of Japan"},{"@language":"ja","@value":"堆積学研究"}],"dc:publisher":[{"@language":"en","@value":"The Sedimentological Society of Japan"},{"@language":"ja","@value":"日本堆積学会"}],"prism:publicationDate":"2014","prism:volume":"73","prism:number":"2","prism:startingPage":"121","prism:endingPage":"135"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/026086577"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I026086577"}],"availableAt":"2014","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=deep-sea%20basin","dc:title":"deep-sea basin"},{"@id":"https://cir.nii.ac.jp/all?q=last%20deglaciation","dc:title":"last deglaciation"},{"@id":"https://cir.nii.ac.jp/all?q=organic%20carbon%20accumulation%20rate","dc:title":"organic carbon accumulation rate"},{"@id":"https://cir.nii.ac.jp/all?q=relative%20sea-level%20rise","dc:title":"relative sea-level rise"},{"@id":"https://cir.nii.ac.jp/all?q=turbidite","dc:title":"turbidite"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002215941876096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Millennial-scale variations of sea-ice expansion in the southwestern part of the Okhotsk Sea during the past 120 kyr: Age model and ice-rafted debris in IMAGES Core MD01-2412"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142932663040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stable isotopic characterization of organic carbon accumulation on the Amazon continental shelf"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143906407936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"THE ISOTOPIC COMPOSITION OF REDUCED ORGANIC 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