{"refrec":{"BRefID":233595,"RR":"<b>Gouwy, S.; Bultynck, P.</b> (2000). Graphic correlation of Frasnian sections (Upper Devonian) in the Ardennes, Belgium. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 70</i>: 25-52","BEntID":225280,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 70</i>: 25-52","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gouwy, S.; Bultynck, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gouwy, S.; Bultynck, P.","Englishabstract":"A high-resolution correlation of 10 Frasnian sections in the Belgian Ardennes is made using the graphic correlation method. The measured ranges of 85 conodont taxa, 48 coral taxa. 29 brachiopod taxa and one stromatoporoid taxon have been assembled into a chronostratigraphic framework. The Ardennes Frasnian Regional Composite developed in this study provides a higher stratigraphic resolution than the traditionally used conodont zonation. It allows a subdivision of the Frasnian into 532 composite standard units derived from the standard reference section in the southern part of the Dinant Synclinorium, completed with a section in the Philippeville Massif for the uppermost part of the Frasnian that is not exposed in the southern part of the Dinant Synclinorium, units 332-532. By correlating the sections using time-equivalent lines, the diachronous pattern of the deposits becomes clearly visible. The combination of this pattern and the conodont biofacies changes in the sections were used to recognise four major third order (500.000y-5m.y.) transgression-regression cycles. The first one, starting in the latest Givetian (Early <i>falsiovalis</i> Zone), continues through the transitans Zone and ends in the lower part of the <i>punctata Zone</i>. The second and third T-R cycles cover the <i>punctata</i> and <i>hassi</i> sl Zones, the <i>jamieae</i> Zone and the major part of the Early <i>rhenana</i> Zone. The fourth cycle (superimposed by a few minor cycles) starts in the early <i>rhenana</i> Zone and continues till the <i>triangularis</i> Zone. The first, second and fourth cycles are considered eustatic. Through graphic correlation of the Composite Standard (CS) of the Frasnian (KLAPPER, 1997) with the regional composite of the Ardennes, new data are added to the CS of the Frasnian and some already incorporated ranges are extended.","AbstractOtherLang":"Une corrélation à haute résolution de 10 coupes frasniennes en Ardenne belge a été réalisée en utilisant la méthode de Corrélation Graphique. Les extensions stratigraphiques mesurées de 85 espèces de conodontes, 48 espèces de coraux, 29 espèces de brachiopodes et 1 espèce de stromatoporoïde, présentes dans ces coupes, ont été réunies dans un cadre chonostratigraphique et une coupe composée régionale en Ardenne a été établie. Cette coupe composée fournit une plus grande résolution stratigraphique que la zonation traditionnelle à conodontes. Cela permet de diviser le Frasnien en 532 unités de temps standard dérivées d'une coupe de référence composée située au bord sud du Synclinorium de Dinant et complétée par une coupe dans le Massif de Philippeville, pour le sommet du Frasnien qui n'est pas exposé au bord sud du Synclinorium de Dinant (unités 332-532). La nature diachroniquedes ensembles sédimentaires ressort clairement de la corrélation basée sur des lignes d'équivalence de temps. La combinaison de ces ensembles et de la succession des biofacies à conodontes dans les coupes permet de reconnaître quatre grands cycles T-R de 3ième ordre 500.000y-5m.y.. Le premier, qui commence au sommet du Givetien (Zone à <i>falsiovalis</i> inférieure) continue jusque dans la partie inférieure de la Zone à <i>punctata</i>. Les deuxième et le troisième cycles couvrent les Zones à <i>punctata</i>, à <i>hassi</i> sl, à <i>jamieae</i> et la plus grande partie de la Zone à <i>rhenana</i> inférieure. Le quatrième cycle (comprenant quelques cycles mineurs) commence dans la Zone à <i>rhenana</i> inférieure el continue jusque la Zone à <i>triangularis</i>. Les premier, deuxième el quatrième cycles sont considérés comme des cycles eustatiques. En corrélant la Coupe Composée Standard du Frasnien (KLAPPER, 1997) avec la Coupe Composée Régional en Ardenne, des données nouvelles sont ajoutées à la première et quelques extensions sont étendues.","BibLvlCode":"AS","StandardTitle":"Graphic correlation of Frasnian sections (Upper Devonian) in the Ardennes, Belgium","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-02 08:33:14.980000","timezone_type":1,"timezone":"+00:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Frasnian, Ardennes, graphic correlation, T-R-cycles, conodonts","OtherDescriptors":null,"Notes":null,"AnaPub":2000,"MonPub":null,"DateUpdate":"2014-02-14","DateCreate":"2014-02-14","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":233595,"PubliDate":2000,"Pagination":"25-52","XtraPublOfAnaID":null,"ISBN":null,"Volume":"70","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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