{"refrec":{"BRefID":249694,"RR":"<b>Bultynck, P.; Helsen, S.; Hayduckiewich, J.</b> (1998). Conodont succession and biofacies in upper Frasnian formations (Devonian) from the southern and central parts of the Dinant Synclinorium (Belgium) - (Timing of facies shifting and correlation with late Frasnian events). <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 68</i>: 25-75","BEntID":241393,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 68</i>: 25-75","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bultynck, P.; Helsen, S.; Hayduckiewich, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bultynck, P. <i>et al.</i>","Englishabstract":"Early <i>rhenana</i>, Late <i>rhenana</i> and <i>linguiformis</i> Conodont Zones are recognised in the upper Frasnian Neuville, Valisettes and Matagne Formations of southern Belgium, and documented by their index-taxa. The age of the base of the Matagne Formation shifts from the Early and Late <i>rhenana</i> Zones in the southern Dinant Basin into the <i>linguiformis</i> Zone in the more northerly Philippeville Massif. In the first area conodont biofacies analyses reveal a deepening of the shelf below the base of the diachronic Matagne Formation; within the lower part Of the Matagne shales biofacies analyses indicate shallowing depositional conditions followed by a progressive deepening. The Lower Kellwasser Event is situated close to the base of the Matagne Formation in the southern part of the Dinant Synclinorium and at the base of the Valisettes Formation in the Philippeville Massif. The Upper Kellwasser Event is correlated with the base of the Matagne Formation in the latter area.","AbstractOtherLang":"Les Zones inférieure et supérieure à <i>Palmatolepis rhenana</i> et la Zone à <i>P. linguiformis</i>, toutes identifiées par la présence de l'espèce-guide, sont reconnues dans les Formations de Neuville, des Valisettes et de Matagne, appartenant au Frasnien supérieur du sud de la Belgique. La base de la Formation de Matagne est diachronique. Au bord sud du Synclinorium de Dinant, elle se situe dans un intervalle couvrant le sommet de la Zone à <i>P. rhenana</i> inférieure et la base de la Zone à <i>P. rhenana supérieure</i>. Dans le Massif de Philippeville, plus au nord, elle appartient à la Zone à <i>P. linguiformis</i>. L'étude de la succession des biofacies à conodontes dans la première région, indique un approfondissement de la plate-forme continentale sous la base de la Formation de Matagne; dans la partie inférieure de cette formation, l'environnement redevient moins profond puis progressivement plus profond. Au bord sud du Synclinorium de Dinant, l'événement Kellwasser inférieur est proche de la base de la Formation de Matagne et dans le Massif de Philippeville il se situe à la base de la Formation des Valisettes, dans cette dernière région l'événement Kellwasser supérieur correspond à la base de la Formation de Matagne.","BibLvlCode":"AS","StandardTitle":"Conodont succession and biofacies in upper Frasnian formations (Devonian) from the southern and central parts of the Dinant Synclinorium (Belgium) - (Timing of facies shifting and correlation with late Frasnian events)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-02 08:58:19.190595","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Conodonts, biostratigraphy, biofacies, late Frasnian, Belgium, Conodontes, biostratigraphie, Frasnien, Belgique","OtherDescriptors":null,"Notes":null,"AnaPub":1998,"MonPub":null,"DateUpdate":"2015-09-07","DateCreate":"2015-09-07","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":249694,"PubliDate":1998,"Pagination":"25-75","XtraPublOfAnaID":null,"ISBN":null,"Volume":"68","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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