{"@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/1363670320227455616.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.marmicro.2007.06.002"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0377839807000655?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0377839807000655?httpAccept=text/plain"}}],"dc:title":[{"@value":"The vertical distribution of Radiolaria in the waters surrounding Japan"}],"description":[{"notation":[{"@value":"Abstract   Geographic and vertical distribution patterns of living Radiolaria are closely related to the characters of the water column. We studied living Radiolaria in samples collected at closely spaced depth intervals in the waters surrounding Japan in order to understand their vertical distribution and its controlling factors. Such information is needed to reconstruct past vertical water mass structure. The Japanese Islands are surrounded by the marginal Japan Sea and the North Pacific Ocean, and from approximately 46° N to 26° N. They thus extend across a large latitudinal range and are exposed to a similarly wide range of environmental conditions, inducing the warm Kuroshio, Tsushima, and Tsugaru Currents and the cold Oyashio Current.  We performed plankton tows (mesh size 63 mm) from late May to early June 2002 at eight sites, sampling the upper 200 m of the water column, at seven depth intervals.  We recognized five radiolarian assemblages: the Upper Surface Assemblage (0–40 m), the Lower Surface Assemblage (40–80 m), the Surface Assemblage (0–80 m), the Subsurface Assemblage (80–200 m), and the Lower Surface–Subsurface Assemblage (40–200 m) groups.  Pseudodictyophimus gracilipes  and  Tetrapyle octacantha  (juvenile) show “tropical submergence”, i.e. they live at the surface in high latitudes and at greater depth in low latitudes. Four taxa live at specific temperature and salinity:  Acrosphaera spinosa ,  Larcopyle butschlii ,  Challengeron diodon , and  Stichocorys seriata . Four taxa are associated with characteristic temperatures:  Neosemantis distephanus ,  Arachnocorys umbellifura ,  Antarctissa  sp. 1, and  Saccospyris conithorax ."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320227455617","@type":"Researcher","foaf:name":[{"@value":"Yoshiyuki Ishitani"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320227455616","@type":"Researcher","foaf:name":[{"@value":"Kozo Takahashi"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03778398"}],"prism:publicationName":[{"@value":"Marine Micropaleontology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2007-12","prism:volume":"65","prism:number":"3-4","prism:startingPage":"113","prism:endingPage":"136"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0377839807000655?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0377839807000655?httpAccept=text/plain"}],"createdAt":"2007-06-18","modifiedAt":"2019-04-29","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232352976896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Early to Middle Pleistocene paleoceanographic history of southern Japan based on radiolarian data from IODP Exp. 314/315 Sites C0001 and C0002"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232352980864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vertical distribution of polycystine radiolarians in the northern East China Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690869088896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two distinct lineages in the radiolarian Order Spumellaria having different ecological preferences"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567189021056128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Polycystine Radiolarians in the Tsushima Strait in Autumn of 2006"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640822509824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fifteen year time-series of radiolarian fluxes and environmental conditions in the Bering Sea and the central subarctic Pacific, 1990–2005"}]},{"@id":"https://cir.nii.ac.jp/crid/1360847873792758912","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Middle to Upper Pleistocene Polycystine Radiolarians from Hole 902-C9001C, Northwestern Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360847873792796416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Active Floating with Buoyancy of Pseudopodia Versus Passive Floating by Hydrodynamic Drag Force: A Case Study of the Flat-Shaped Spumellarian Radiolarian Dictyocoryne"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654739305984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New northwest Pacific radiolarian data as a tool to estimate past sea surface and intermediate water temperatures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657492502272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Uncovering sibling species in Radiolaria: Evidence for ecological partitioning in a marine planktonic protist"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660707031680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A New Phaeodarian Species Discovered from the Japan Sea Proper Water, <i>Auloscena pleuroclada</i> sp. nov. (Aulosphaeridae, Phaeosphaerida, Phaeodaria)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663997901440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Polycystine Radiolarians Vertical Distribution in the Subtropical Northwest Pacific during Spring 2015 (KS15-4)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848665120032256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Flux variations and vertical distributions of siliceous Rhizaria (Radiolaria and Phaeodaria) in the western Arctic Ocean: indices of environmental changes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848665121800704","@type":"Article","resourceType":"preprint","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Flux variations and vertical distributions of microzooplankton (Radiolaria) in the western Arctic Ocean: environmental indices in a warming Arctic"}]},{"@id":"https://cir.nii.ac.jp/crid/1521699230479723776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Radiolarian assemblages in surface sediments of the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1523388080428113920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A morphological analysis of the flat-shaped spumellarian radiolarian Dictyocoryne : morpho-functional insights into planktonic mode of life"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892142892928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Pliocene to recent history of the Kuroshio and Tsushima Currents : a multi-proxy approach"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2007.06.002"},{"@type":"OPENAIRE","@value":"doi_dedup___::287c1c5d82e76eeec07724af3d24c358"},{"@type":"CROSSREF","@value":"10.2517/2018pr023_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.2517/2015pr030_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2015.05.001_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.2517/2019pr020_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.2517/1342-8144-14.1.019_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.2517/2015pr003_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0045-6_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1002/2017pa003087_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1111/jeu.12274_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.5194/bg-12-2019-2015_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.5194/bgd-11-16645-2014_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.2517/2019pr019_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1016/j.dsr2.2011.12.003_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2016.03.004_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1016/j.dsr2.2011.12.005_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"},{"@type":"CROSSREF","@value":"10.1016/j.ympev.2014.05.021_references_DOI_BHWyeeeYo5CZh4qvV1Zl0tZMMtF"}]}