{"@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/1360004229805504128.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016gc006449"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GC006449"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GC006449"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016GC006449"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Brucite chimney formation and carbonate alteration at the<scp>S</scp>hinkai<scp>S</scp>eep<scp>F</scp>ield, a serpentinite‐hosted vent system in the<scp>s</scp>outhern<scp>M</scp>ariana forearc"}],"description":[{"notation":[{"@value":"Brucite-carbonate chimneys were discovered from the deepest known (∼5700 m depth) serpentinite-hosted ecosystem – the Shinkai Seep Field (SSF) in the southern Mariana forearc. Textural observations and geochemical analysis reveal three types (I-III) of chimneys formed by the precipitation and dissolution of constitutive minerals. Type I chimneys are bright white to light yellow, have a spiky crystalline and wrinkled surface with microbial mat and contain more brucite; these formed as a result of rapid precipitation under high fluid discharge conditions. Type II chimneys exhibit white to dull brown coloration, tuberous textures like vascular bundles, and are covered with grayish microbial mats and dense colonies of Phyllochaetopterus. This type of chimney is characterized by inner brucite-rich and outer carbonate rich zones and is thought to have precipitated from lower fluid discharge conditions than type I chimneys. Type III chimneys are ivory colored, have surface depressions and lack living microbial mats or animals. This type of chimney mainly consists of carbonate, and is in a dissolution stage. Stable carbon isotope compositions of carbonates in the two types (I and II) of active chimneys are extremely 13C-enriched (up to +24.1‰), which may reflect biological 12C consumption under extremely low dissolved inorganic carbon concentration in alkaline fluid. Type III chimneys have 13C compositions indicating re-equilibration with seawater. Our findings demonstrate for the first time that carbonate chimneys can be form below carbonate compensation depth and provide new insights about linked geologic, hydrologic, and biological processes of the global deep-sea serpentinite-hosted vent systems. This article is protected by copyright. All rights reserved."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229805504645","@type":"Researcher","foaf:name":[{"@value":"T. Okumura"}],"jpcoar:affiliationName":[{"@value":"Department of Subsurface Geobiological Analysis and Research (D‐SUGAR)Japan Agency for Marine‐Earth Science and TechnologyYokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504522","@type":"Researcher","foaf:name":[{"@value":"Y. Ohara"}],"jpcoar:affiliationName":[{"@value":"Department of Subsurface Geobiological Analysis and Research (D‐SUGAR)Japan Agency for Marine‐Earth Science and TechnologyYokosuka Japan"},{"@value":"Hydrographic and Oceanographic Department of Japan Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504640","@type":"Researcher","foaf:name":[{"@value":"R. J. Stern"}],"jpcoar:affiliationName":[{"@value":"Geosciences DepartmentUniversity of Texas at DallasRichardson Texas USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504139","@type":"Researcher","foaf:name":[{"@value":"T. Yamanaka"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Natural Science and TechnologyOkayama UniversityOkayama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504404","@type":"Researcher","foaf:name":[{"@value":"Y. Onishi"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Natural Science and TechnologyOkayama UniversityOkayama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504260","@type":"Researcher","foaf:name":[{"@value":"H. Watanabe"}],"jpcoar:affiliationName":[{"@value":"Marine Biodiversity Research ProgramJapan Agency for Marine‐Earth Science and TechnologyYokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504517","@type":"Researcher","foaf:name":[{"@value":"C. Chen"}],"jpcoar:affiliationName":[{"@value":"Department of Subsurface Geobiological Analysis and Research (D‐SUGAR)Japan Agency for Marine‐Earth Science and TechnologyYokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504264","@type":"Researcher","foaf:name":[{"@value":"S. H. Bloomer"}],"jpcoar:affiliationName":[{"@value":"Oregon State UniversityCorvallis Oregon USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504397","@type":"Researcher","foaf:name":[{"@value":"I. Pujana"}],"jpcoar:affiliationName":[{"@value":"Geosciences DepartmentUniversity of Texas at DallasRichardson Texas USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504140","@type":"Researcher","foaf:name":[{"@value":"S. Sakai"}],"jpcoar:affiliationName":[{"@value":"Institute of BiogeosciencesJapan Agency for Marine‐Earth Science and Technology Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504395","@type":"Researcher","foaf:name":[{"@value":"T. Ishii"}],"jpcoar:affiliationName":[{"@value":"Fukada Geological Institute Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805504144","@type":"Researcher","foaf:name":[{"@value":"K. Takai"}],"jpcoar:affiliationName":[{"@value":"Department of Subsurface Geobiological Analysis and Research (D‐SUGAR)Japan Agency for Marine‐Earth Science and TechnologyYokosuka Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"15252027"},{"@type":"EISSN","@value":"15252027"}],"prism:publicationName":[{"@value":"Geochemistry, Geophysics, Geosystems"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2016-09","prism:volume":"17","prism:number":"9","prism:startingPage":"3775","prism:endingPage":"3796"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://creativecommons.org/licenses/by-nc-nd/4.0/","http://creativecommons.org/licenses/by-nc-nd/4.0/","http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GC006449"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GC006449"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016GC006449"}],"createdAt":"2016-09-10","modifiedAt":"2022-07-08","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781833389440","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H05468"},{"@type":"JGN","@value":"JP15H05468"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H05468/"}],"notation":[{"@language":"ja","@value":"化学合成微生物群集によるストロマトライト形成の検証"},{"@language":"en","@value":"Investigation 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