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Autor Pérez Valera, Fernando |
Documentos disponibles escritos por este autor (5)
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In the Cabo Cope Unit (Maláguide Complex, W Aguilas, Murcia), two members have been distinguished within the Triassic Unit. The lower member consists of detritic deposits with interbedded gypsum. The upper member is composed of carbonates. A lev[...]texto impreso
A bioestratigraphic study has been carried out with the aid of ammonoids from the Lower Ladinian of the SE Calasparra section (Eastern of the Betic Cordillera). The section is formed by 89 m of do- lostones and fossiliferous limestones from the [...]texto impreso
Pérez Valera, Fernando ; Pérez López, A. ; Pérez Valera, J. Alberto | Sociedad Geológica de España | 2005The Cehegín Formation (Ladinian) is defined as a formal lithostratigraphic unit to characterize the Muschelkalk facies deposited on intermediate-external area of the southern Iberian continental margin. This formation consists of dark limestones[...]texto impreso
Sauropterygian vertebrate remains from the Ladinian (Middle Triassic) of the proximity of Calasparra (Murcia, Spain) are described here. They represent the first documented Triassic vertebrate remains found in the Province of Murcia, and the fir[...]texto impreso
Baeza Carratalá, José F. ; Pérez Valera, Juan Alberto ; Pérez Valera, Fernando | Polskiej Akademii Nauk, Instytut Paleobiologii | 2018-01Triassic brachiopods from the Betic Range were unknown hitherto. Herein we describe the first brachiopod occurrences in the early Ladinian of this domain referable to a new genus and species Misunithyris goyi derived from three localities of th[...]