RT Journal Article
T1 Análisis microfaunístico del Cenomaniense de Arceniega (Cuenca Navarro-Cántabra)
T1 Microfaunal analysis of the Cenomanian of Arceniega (Navarro-Cantabrian Basin)
A1 Rodríguez Lázaro, Julio
A1 Barroso Barcenilla, F.
A1 Martín Rubio, Maite
AB The analysis of calcareous micro fauna (foraminifers, ostracods) of the Arceniega Formation allows to decipher different phases on the palaeoenvironmental evolution of this part of the Navarro-Cantabrian Basin during the Cenomanian. The generalised marine ingression of the beginning of the Upper Cretaceous occurred in the region during the deposition of the Arceniega unit, in the early Cenomanian. After an interval with regressive trend, a sustained transgressive phase was developed during the late Cenomanian, which represents the deepest sediments of shelf settlements of the Mesozoic. Some biotic proxies, particularly that of the platycopic ostracod signal, evidence intervals with important influx of hypoxic waters
PB Sociedad Geológica de España
YR 2003
FD 2003
LK http://hdl.handle.net/10272/9026
UL http://hdl.handle.net/10272/9026
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026