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http://hdl.handle.net/2183/6350 Presencia del wenlock inferior en la Sierra de Tamames (Salamanca)
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Jiménez Fuentes, Emiliano
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Cadernos do Laboratorio Xeolóxico de Laxe, 1983, 6: 65-70 ISBN: 84-7492-204-6
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Abstract
[Resumen] A la presencia de 4 niveles graptolíticos en· la Sierra de Tamames (Salamanca) (Llanvirniense Inferior, Llandoveriense Medio, Llandoveriense Superior y Ludloviense Inferior), se añade el Wenlock Inferior (Zonas murchisoni-riccartoniensis) y se precisa el Ludlow Inferior (zona nilssoni). No se ha encontrado aún el Wenlock Superior, tan característico en otras regiones del NW Peninsular
[Abstract] Amonograptids fauna coming from the post-Llandove rian of the Tamames Syncline, in the Salamanca pro vince (Spain), is described in this paper. This fauna belongs to two stratigraphic units: the Lower Wenlock (murchisoni-riccartoniensis zone) and the Lower Ludlow (nilssoni zone). However, the typical graptolite fauna of the Upper Wenlock, so characteristic of the NW of the Iberian Peninsula has not been found yet
[Abstract] Amonograptids fauna coming from the post-Llandove rian of the Tamames Syncline, in the Salamanca pro vince (Spain), is described in this paper. This fauna belongs to two stratigraphic units: the Lower Wenlock (murchisoni-riccartoniensis zone) and the Lower Ludlow (nilssoni zone). However, the typical graptolite fauna of the Upper Wenlock, so characteristic of the NW of the Iberian Peninsula has not been found yet