{"refrec":{"BRefID":220605,"RR":"<b>Bouckaert, J.; Ziegler, W.</b> (1965). Conodont stratigraphy of the Famennian stage (Upper Devonian) in Belgium. <i>Toelichtende Verhandelingen voor de Geologische Kaart en Mijnkaart van België = Mémoires pour servir à l'explication des cartes géologiques et minières de la Belgique</i>, 5. Hayez: Bruxelles.  62p., 10 pl. pp.","BEntID":212338,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Toelichtende Verhandelingen voor de Geologische Kaart en Mijnkaart van België = Mémoires pour servir à l'explication des cartes géologiques et minières de la Belgique</i>, 5. Hayez: Bruxelles.  62p., 10 pl. pp.","DocTypID":5,"DocType":"Book/Monograph","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bouckaert, J.; Ziegler, W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bouckaert, J.; Ziegler, W.","Englishabstract":null,"AbstractOtherLang":"Einige Profile des Belgischen Famennien wurden auf Conodonten uniersucht. Dabei wurden zahlreiche Conodonten-Zonen von der triangularis-Zone bis zur costatus-Zone nachgewiesen. Die Conodonten wie auch die Conodonten-Zonen sind indentisch mit denen des deutschen Oberdevons. Statigraphisch interessant ist, dass Teile der Famenne-Schiefer, die bisher in das Untere Famennien gestellt wurden, nun in das Obere Famennien gehören (Profile von Aye und Houyet). Der « Macigno de Souverain-Pre .. ist ein gleichaltriger Horizont, der etwa in den höheren Teil der rhomboidea-Zone gehört. Diese Zone wurde auch in den « Schiste de la Famenne» erkannt, die zu einder völlig anderen Faziesentwicklung gehören. Die Grenze zwischen Frasne-Schichten und Famenne-Schichten ist deutlich nur im Profil von Senzeille aufgeschlossen. Die tiefsten Conodonten-Proben aus dem tiefen Famenne-Schiefer (Zone der Camarotoechia lecomptei) gehören in die triangularis-Zone und zwar in eine Teil, der älter ist als Obere triangularis-Zone. Danach dürfte der unterste Teil des Famenne-Schiefers in den höchste Teil der Manticoceras-Stufe gehören. Das Profil Huy 2 w a r mit Hilfe von Foraminiferen durch R. CONIL (1964) als Tnia (Unteres Tournaisien-Sous-Assise d'Etrceungt et de Comblain-au-Pont; syn. : Strunien, Schistes et Calcaires d'Etrceungt, Assise de Comblain-au-Pont) eingestuft worden. Die Conodonten zeigen die costatus-Zone an, wonach der höchste Teil der Chjmenia-Sluie und/oder Teile der Wocklumeria-Siufe vorliegen. 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