{"refrec":{"BRefID":233831,"RR":"<b>De Man, E.; Van Simaeys, S.; De Meuter, F.; King, C.; Steurbaut, E.</b> (2004). Oligocene benthic foraminiferal zonation for the southern North Sea Basin. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 74 suppl</i>: 177-195","BEntID":225516,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 74 suppl</i>: 177-195","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"De Man, E.; Van Simaeys, S.; De Meuter, F.; King, C.; Steurbaut, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"De Man, E. <i>et al.</i>","Englishabstract":"In the scope of the ratification of an international reference boundary for the Rupelian-Chattian transition, it is important to evaluate both stages in their original stratotype areas. In this study, quantitative analysis of benthic foraminifera of several boreholes in the historical Rupelian stratotype area enables recognition of biostratigraphic events in the upper Rupelian and the Chattian: we present a coherent biostratigraphic scheme for the Oligocene southern North Sea Basin. The Rupelian-Chattian interval is subdivided into eleven biozones, of which the lowermost four (interval I-IV) were defined by GRIMM & STEURBAUT (2001) and the overlying seven (interval V-XI) are newly defined herein. A correlation between the Oligocene benthic foraminiferal zonation scheme for the southern North Sea Basin and the adjacent areas is established. Finally, some potential problems for the future decision on an international reference boundary for the Rupelian-Chattian are discussed.","AbstractOtherLang":"Dans le cadre de la ratification d'une limite internationale pour la transition Rupelien-Chattien, il est important d'évaluer ces deux étages dans leurs stratotypes originaux. Dans ce travail une analyse quantitative des foraminifères provenant de plusieurs sondages réalisés aux alentours du stratotype historique du Rupelien permet de distinguer une série d'événements biostratigraphiques dans le Rupelien supérieur el le Chattien. Un schéma biostratigraphique cohérent basé sur les foraminifères est présenté pour l'Oligocène de la Belgique. L'intervalle Rupelien-Chattien est divisée en onze biozones, dont quatre (intervalle I-IV) onl été définies par GRIMM & STEURBAUT (2001) et les sept autres (intervalle V-XI) sont introduites ici pour la première fois. La relation entre le schéma belge et d'autres schémas biostratigraphiques basés sur des foraminifères benthiques est mise en évidence. Finalement, quelques problèmes possibles sur la décision future d'une limite internationale pour le Rupelien-Chattien sont discutés.","BibLvlCode":"AS","StandardTitle":"Oligocene benthic foraminiferal zonation for the southern North Sea Basin","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":"Foraminifera, Rupelian-Chattian boundary, Belgium, biostratigraphy","OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2014-02-25","DateCreate":"2014-02-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":233831,"PubliDate":2004,"Pagination":"177-195","XtraPublOfAnaID":null,"ISBN":null,"Volume":"74 suppl","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":64308,"SerRR":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. 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