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The carbonate clasts from the Mount Wegener Formation provide sedimentological, diagenetic and palaeontological evidences of the destruction and resedimentation of a hidden/unknown Cambrian carbonate shallow-water record at the Coats Land region[...]texto impreso
Quijada, I. Emma ; Benito Moreno, María Isabel ; Suárez González, Pablo ; Rodríguez Martínez, Marta ; Campos Soto, Sonia | Elsevier | 2020-10Peritidal carbonate-evaporite successions, since they are developed in the transition between continental and marine realms, provide essential keys for palaeobathymetric and palaeoclimatic interpretations. As a result, several facies models have[...]texto impreso
Benito Moreno, María Isabel ; Suárez González, Pablo ; Campos Soto, Sonia ; Rodríguez Martínez, Marta | Springer | 2020The Lower Cretaceous Leza Formation is an essentially carbonate unit deposited at the northernmost active margin of the Cameros Basin (N Spain) under an extensional tectonic regime. This unit is composed of freshwater, marine-influenced, margina[...]texto impreso
Perejón, Antonio ; Rodríguez Martínez, Marta ; Moreno-Eiris, Elena ; Menéndez, Silvia ; Reitner, Joachim | Taylor & Francis | 2019This study records the first occurrence of a lower Cambrian archaeocyathan fauna in limestone cobbles from Carboniferous glacigenic deposits of the Dwyka Group of the Aranos Basin in Namibia. Petrographic and microfacies analysis of 17 large, mi[...]texto impreso
In the southern Central Iberian Zone, unconformably lying on the Cadomian folded Lower Alcudian-Domo Extremeño Supergroup the most complete succession of late Ediacaran rocks crops out at the Sierra de la Zarzuela syncline. The purpose of this c[...]texto impreso
In the Central Iberian Zone of the Iberian Massif, the Los Navalucillos Formation, interpreted as tidal and shallow-marine carbonate deposits, contains a significant archaeocyathan faunal assemblage. Two new characteristic exposures are describe[...]
