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Bordalo da Rocha, Rogério ; Mattioli, Emanuela ; Duarte, Luís Vitor ; Pittet, Bernard ; Elmi, Serge ; Mouterde, René ; Cabral, Maria Cristina ; Comas Rengifo, María José ; Gómez Fernández, Juan José ; Goy, Antonio ; Hesselbo, Stephen P. ; Jenkyns, Hugh C ; Littler, Kate ; Mailliot, Samuel ; Veiga de Oliveira, Luiz Carlos ; Osete López, María Luisa ; Perilli, Nicola ; Pinto, Susana ; Ruget, Christiane | International Union of Geological Sciences (IUGS) | 2016-10The Global Stratotype Section and Point (GSSP) for the base of Toarcian Stage, Lower Jurassic, is placed at the base of micritic limestone bed 15e at Ponta do Trovão (Peniche, Lusitanian Basin, Portugal; coordinates: 39°22’15’’N, 9°23’07’’W), 80[...]texto impreso
Perilli, Nicola ; Comas Rengifo, María José | Università degli Studi, Milano. Istituto di Geologia | 2002Common and diverse calcareous nannofossìl assemblages were found in two continuous and expanded successions, sedimented on hemipelagic carbonate ramp. Based on refined ammonite biostratigraphy closely spaced sampling and semiquantitative analysi[...]texto impreso
Perilli, Nicola ; Comas Rengifo, María José ; Goy, Antonio | Università degli Studi di Milano, Italy | 2004-04Based on a continuous succession of ammonite and calcareous nannofossil assemblages, the main purpose of this paper is the correlation between ammonite and calcareous nannofossil zone boundaries in two expanded sections from the Basque-Cantabria[...]texto impreso
Perilli, Nicola ; Comas Rengifo, María José ; Goy, Antonio | Università degli Studi, Milano. Istituto di Geologia | 2004Based on a continuous succession of ammonite and calcareous nannofossil assemblages, the main purpose of this paper is the correlation between amnronite and calcareous nannofossil zone boundaries in two expanded sections from the Basque-Cantabri[...]texto impreso
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Comas-Rengifo, María José ; Gómez Fernández, Juan José ; Goy, Antonio ; Herrero Matesanz, Concepción ; Perilli, Nicola ; Rodrigo, A. | Universidad Complutense de Madrid. Departamento de Estratigrafía | 1999En este trabajo se detallan las características locales de las unidades litoestigráficas del Jurásico Inferior de la Cuenca Ibérica en las proximidades de Almonacid de la Cuba y de Belchite (Zaragoza), así como, las de la «Unidad de Almonacid de[...]texto impreso
Fraguas Herráez, Ángela Raquel ; Comas Rengifo, María José ; Perilli, Nicola | Universidad Complutense de Madrid, Servicio de Publicaciones | 2007-12-29Se estudian los nanofósiles calcáreos identificados en materiales del Pliensbachiense de la sección de Tudanca (Cuenca Vasco-Cantábrica, España). Se han reconocido doscientos catorce niveles estratigráficos constituidos, fundamentalmente, por un[...]texto impreso
Fraguas Herráez, Ángela Raquel ; Comas Rengifo, María José ; Perilli, Nicola | Società toscana di scienze naturali (Pisa) | 2008The target of this paper is to study the succession of the Pliensbachian calcareous nannofossil assemblages recovered from the Santotis section (Northern Spain) in order to calibrate the biohorizons against the ammonite zones. In this section, o[...]texto impreso
Cresta, S. ; Goy, Antonio ; Ureta Gil, María Soledad ; Arias Fernández, María del Carmen ; Barrón López, Eduardo ; Bernard García, Julio ; Canales Fernández, María Luisa ; Garcia Joral, Fernando ; García Romero, Emilia ; Gialanella, P.R. ; Gómez Fernández, Juan José ; González, J.A. ; Herrero Matesanz, Concepción ; Martínez Gutiérrez, Gemma ; Osete López, María Luisa ; Perilli, Nicola ; Villalain, J.J. | International Union of Geological Sciences | 2001The Global Boundary Stratotype Section and Point (GSSP) for the Aalenian Stage, formally defined at the base of bed FZ107 in the Fuentelsaz section, Castilian Branch of the Iberian Range (Spain), has been ratified by the IUGS. Multidisciplinary [...]
