los ammonites del tithonico superior berriasense de la zona subbetica

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VMVECHRVBUMUHitU1 1U3ILEVueltas medias.Vueltas externas.Camara de habitacion.Region ventral.Borde umbilical.Muralla umbilical.Holotipo.Lobulos umbilicales.ILobulo interno.Lobulo lateral.Lobulo externo, ventral о sifonal.Simplisphinctes alcobitensen.sp. T . G A .1.21. (Hit.).H= 23mm. (penultima sutura)T .G .Ber.1.lbFig-336
S U P E R F A M I L I A PER ISPHINCTACEAE S T E I N M A N N , 1890F A M I L I A S I M O C E R A T I D A E S P A T H , 1924SUBFAMILIA SIMOCERATINAE SPATH, 1924Muestra esta subfamilia su maxima expansion en los niveles superiores del Tithonicoinferior у sus ultimos representantes, igualmente tipicos у escasos, estan acantonadosen la base del Tithonico superior. Para un conocimiento global de esta subfamiliaremito al lector a ZIEGLER (1959) у OLORIZ (1976).GENERO CORDUBICERAS OLORIZ Y TAVERA, 1979Sinonimia: Baeticoceras GEYSSANT, ENAY у BUSNARDO, 1979.Especie tipo: Cordubiceras geminatum (OLORIZ у TAVERA).Piagnosis: Simoceratinae dimorfo con costillas geminadas.Consideraciones: OLORIZ у TAVERA (l979) у GEYSSANT (1979) (diagnosis generica de Baeticocerasatribuida a GEYSSANT, ENAY у BUSNARDO 1979), describen casi simultaneamente la existenciade un subgenero nuevo (Simoceras (Cordubiceras)), -genero para la autora francesa(Baeticoceras)- en las Cordilleras Beticas. Se ofrecen sendas diagnosis que a la vistadel material posteriormente recolectado у que aqui se estudia, quedan incompletas e imprecisas.Sin duda la mas complete es la de GEYSSANT, pero sin embargo es erronea en cuantoa las vueltas internas se refiere. En GEYSSANT (1979 p.5) podemos leer: "... Sur les toursinternes, cotes fines, denses et de faible relief...". En Cordubiceras nexus n.sp. sepuede constatar сото existe un nucleo perisphinctoide (tipo "nebrodites") hasta los 10mm.сото minimo у que ya a los 20mm. presenta totalmente conformado el estadio "volanense"tipico.En cuanto al dimorfismo aqui se acepta totalmente у se describen dos nuevasespecies, una macroconcha: Cordubiceras maius n.sp., quizas par dimorfico de Cordubicerasnexus n.sp. (microconcha). Ahora bien, сото en cualquier caso estos lazos de parentescoson imposibles de poner de manifiesto, se ha optado por separar en especies diferenteslas dos morfologias (macro у microconcha) que GEYSSANT, en otros casos, reune bajo unamisma denominacion especifica.37
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TABLA I aDe los Berriasellinae esta
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INTRODUCCIONComo bien senala YIN TS
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Fig.27S ESPANA SE FRANCIA TUNEZ SUL
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INTRODUCCIONEn el presente capitulo
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L A M I N A 15Fig.l. Zittelia krant
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LAMINA 38Fig.l. El enaella cu la re
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LAMINA 43Fig.l. Fauriella floquinen
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los ammonites del tithonico superior berriasense de la zona subbetica

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