Publication: Conodontos telychienses (Silúrico inferior) del sinclinal del Guadarranque (Zona Centroibérica, Macizo Hespérico)
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1991-07
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Sociedad Española de Paleontología
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Abstract
Se refiere el hallazgo de los primeros conodontos silúricos id entificables taxonómicamente de la Zona Cenlroibérica del Macizo Hespérico. El material estudiado procede de las ampelitas de la Formación Guadarranquejo, en el Sinclinal del Guadarranque y es referido al Telychiense en base a los grapto litos asociados.
Silurian conodonts, taxonomically identifiables, from the Cent ral-Iberian Zone of the Hesperian Massif are described for the first time. The conodonts coming from the black shales of the Guadarranquejo Formation at Guadarranque Syncline, are Telychian in age for lhe associated graptolites.
Silurian conodonts, taxonomically identifiables, from the Cent ral-Iberian Zone of the Hesperian Massif are described for the first time. The conodonts coming from the black shales of the Guadarranquejo Formation at Guadarranque Syncline, are Telychian in age for lhe associated graptolites.