RT Journal Article
T1 Presencia de Teredolites Leymerie 1842 en el yacimiento con dinosaurios ANA (Cretácico Inferior, Cinctorres, Castellón)
T1 Teredolites Leymerie 1842 from site with dinosaurs ANA (Lower Cretaceous, Cinctorres, Castellón)
A1 Poza, Begoña
A1 Santos Cubedo, Andrés
A1 Santisteban, Carlos de
A1 Suñer, Maite
AB The ANA fossil site (Cinctorres, Castellón) is placed in the Arcillas de Morella Formation (early Aptian,Lower Cretaceous) of the Maestrat basin. Dinosaur fossils were recovered in it. The Arcillas de MorellaFormation in the sector of Cinctorres has 57 meters of thickness. It is formed by six facies organized in aminimum of twelve parasequences in four depositional sequences. Three of these sequences include incisedvalleys. The ANA fossil site is located in the infill of the third incised valley. Here, several tree trunks havebeen recovered in those the ichnospecie Teredolites clavatus Leymerie, 1842 has been identified. Thisichnogenus is indicative of open marine and marginal marine environments. Its presence in different levelsof the Arcillas de Morella Formation (Teulería Milian, Mas de la Parreta quarry and ANA) allows us toidentify only periods of transgression. It would not correlate the series, neither would be an indication ofthe lateral extent of the deposits with bored logs
PB Universidad de Huelva
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7480
UL http://hdl.handle.net/10272/7480
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026