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• W12152025 endingPage "154" @default.
• W12152025 startingPage "135" @default.
• W12152025 abstract "espanolSe estudian un conjunto de asociaciones palinologicas obtenidas en materiales del Cretacico Inferior de la Subcuenca de Oliete, correspondientes a la Formacion Escucha (Cordillera Iberica, provincia de Teruel, Espana). La sucesion sedimentaria estudiada se deposito en un medio costero complejo en el cual se depositaron sedimentos ricos en materia organica. La medicion y correlacion detallada de secciones estratigraficas ha permitido establecer la localizacion estratigrafica detallada de las muestras con contenido palinologico. Las secciones estudiadas contienen asociaciones de miosporas abundantes y diversas, y unicamente el nivel mas basal (M1) muestra quistes de dinoflagelados. En total se han identificado mas de 130 taxones entre los que se encuentran algunos significativos marcadores biostratigraficos. Por una parte, la presencia de ciertas esporas trilete como Appendicisporites concentricus, Cicatricosisporites crassistriatus, C. mohrioides, C. patapscoensis, C. subrotundus y Phlebopterisporites globosus, ademas de varios tipos de granos de polen de angiospermas primitivas (Afropollis, Asteropollis, Clavatipollenites, Liliacidites, Brenneripollis-Pennipollis y Stellatopollis, asi como escasos granos tricolpados) permiten atribuir una edad Aptiense Superior a los materiales estudiados. Por otra, la identificacion de las especies de dinoflagelados Cyclonephelium compactum, Criboperidinium aceras, Apteodinium vectense and Surculosphaeridium? longifurcatum senala una edad Aptiense Superior�Albiense Inferior para el nivel estudiado mas basal. Estos nuevos datos bioestratigraficos asignan una edad mas antigua a la ultima unidad sinrift (Fm. Escucha) de la Cuenca Iberica. EnglishPalynomorph assemblages of a Lower Cretaceous organic matter-rich sedimentary succession (Oliete Sub-basin, Iberian Ranges, Province of Teruel, Spain) from a complex coastal sedimentary environment are described. Detailed stratigraphic analyses were performed and correlations established in order to precisely record the stratigraphic location of the studied palynological samples. The studied sections contained abundant, well-diversified miospore assemblages. One level (M1) contained an interesting assemblage of dinoflagellate cysts. More than 130 taxa were identified including biostratigraphically significant biomarkers. On the one hand, the presence of Appendicisporites concentricus, Cicatricosisporites crassistriatus, C. mohrioides, C. patapscoensis, C. subrotundus and Phlebopterisporites globosus, as well as several angiosperm pollen types (Afropollis, Asteropollis, Clavatipollenites, Liliacidites, Brenneripollis- Pennipollis and Stellatopollis, occurring with rare and poorly diversified tricolpate forms), suggests an Upper Aptian age for the studied material. On the other, the dinoflagellates Cyclonephelium compactum, Criboperidinium aceras, Apteodinium vectense and Surculosphaeridium? longifurcatum indicate an Upper Aptian�Lower Albian age for the oldest level studied. These new biostratigraphic data assign an older age to the latest synrift unit (Escucha Formation) of the Iberian Basin." @default.
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• W12152025 date "2007-01-01" @default.
• W12152025 modified "2023-10-03" @default.
• W12152025 title "Palynology and biostratigraphy of the Escucha Formation in the Early Cretaceous Oliete Sub-basin, Teruel, Spain" @default.
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