0000000000240178

AUTHOR

María E. Dies

showing 2 related works from this author

Trace and soft body fossils from the Pedroche Formation (Ovetian, Lower Cambrian of the Sierra de Córdoba, S Spain) and their relation to the Pedroch…

2006

The low Lower Cambrian rocks from the Sierra de Cordoba contain one of the best successions in Europe, which consists of well exposed mixed facies with abundant fossil assemblages showing long stratigraphical ranges throughout the Pedroche Formation. These assemblages include diverse Ovetian archaeocyaths, trilobites, small shelly fossils, calcimicrobes, trace fossils and stromatolites. Trace fossils are still poorly known, and thus they are the main objective of this work. Ichnological data are obtained from the Arroyo de Pedroche 1, Arroyo de Pedroche 2 and Puente de Hierro sections. Trace fossils include the ichnogenera Bergaueria, aff. Bilinichnus, Cochlichnus, aff. Cosmorhaphe?, Cylind…

PlanolitesbiologyPaleontologyTrace fossilBiostratigraphybiology.organism_classificationTrilobiteSkolithosPaleontologyDiplichnitesSpace and Planetary SciencePaleoecologyRusophycusGeologyGeobios
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‘‘Distinguishing eustatic and epeirogenic controls on Lower-Middle Cambrian boundary successions in West Gondwana (Morocco and Iberia)’’, by Ed Landi…

2008

GondwanaPaleontologyStratigraphyBoundary (topology)GeologyEpeirogenic movementSedimentologyGeologySedimentology
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