{"refrec":{"BRefID":311483,"RR":"<b>Männik, P.; Maekawa, T.; Tanaka, G.; Komatsu, T.; Siveter, D.; Williams, M.; Hints, O.; Vandenbroucke, T.R.A.</b> (2018). The Ordovician and Silurian conodonts of Japan: their biostratigraphical and paleobiogeographical significance. <i>Island Arc 27(6)</i>: e12269. <a href=\"https://dx.doi.org/10.1111/iar.12269\" target=\"_blank\">https://dx.doi.org/10.1111/iar.12269</a>","BEntID":303846,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Island Arc 27(6)</i>: e12269. <a href=\"https://dx.doi.org/10.1111/iar.12269\" target=\"_blank\">https://dx.doi.org/10.1111/iar.12269</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Männik, P.; Maekawa, T.; Tanaka, G.; Komatsu, T.; Siveter, D.; Williams, M.; Hints, O.; Vandenbroucke, T.R.A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Männik, P. <i>et al.</i>","Englishabstract":"Conodont‐bearing Ordovician and Silurian rocks have a wide geographical distribution in Japan. They are exposed on Honshu, Shikoku, and Kyushu islands. Two recently studied samples from Gionyama, in Kyushu, yield conodont assemblages of Telychian (<i>Distomodus</i> sp., <i>Apsidognathus</i> sp. (cf. <i>A. tuberculatus arcticus</i>), <i>Oulodus</i> cf. <i>rectangulus</i>, <i>Ozarkodina</i> cf. <i>waugoolaensis</i>, <i>Panderodus</i> cf. <i>amplicostatus</i>) and probably the earliest Sheinwoodian (?<i>Distomodus</i> sp. (cf. <i>D. staurognathoides</i>), <i>Ozarkodina</i> sp., <i>Oulodus</i> sp., <i>Walliserodus</i> sp. (cf. <i>Walliserodus</i> sp. nov. c Männik), <i>Panderodus</i> sp.) ages, providing further biostratigraphical constraints for the age of the Gionyama Formation in the Kurosegawa Terrane. Most of the conodont taxa identified have wide paleobiogeographical distribution, but probable occurrence of <i>Oulodus rectangulus</i>, <i>Ozarkodina waugoolaensis</i>, and <i>Panderodus amplicostatus</i> suggests a relationship between Australia, the South China paleocontinent, and the Kurosegawa Terrane of ‘Proto‐Japan’ during the Silurian. These paleogeographic interpretations agree with the existing notions based on rugose corals.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The Ordovician and Silurian conodonts of Japan: their biostratigraphical and paleobiogeographical significance","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"biostratigraphy; conodonts; Japan; Ordovician; Silurian","OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2019-06-05","DateCreate":"2019-05-28","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000452486400001","VABBcode":null,"OpenAcc":0,"DOI":"10.1111/iar.12269"},"refs":null,"anarec":{"AnaID":311483,"PubliDate":2018,"Pagination":"e12269","XtraPublOfAnaID":null,"ISBN":null,"Volume":"27","Issue":"6","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":270863,"SerRR":"Island Arc. 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