[Abstract] This paper deal with the biostratinomic processes and fossildiagenetic processes which affected the bone rest of Pleistocene age from the Liñares Sur carstic cave. AH show that the active processes was creepy ...

[Abstract] The Plateau ofSanta ir Comba is a very degraded rest ofan old surface (Late-Mesozoic -Paleogene), ofcomplex history. It has a mean altitude of400 m, and it is located in the western part of the Coruñan province. ...

[Abstract] The present paper srudy the evolution of the lower part of the Tambre Basin duting the Neogene. The basin, the fluvial network and a group of features are analyzed, such as the asymmetry of the net, the ...

[Abstract] Galicia, in theNWofthe Iberian Peninsula, was a transit area for the migrating large mammals during the Upper Quaternary. These migrations were praduced by the c1imatic changes that characterize this periodo A ...

[Abstract] The lake of Villaseca is located in the foothills of the southern Cantabrian Mountains, nearby Villaseca de Laciana (León,NWIberian Peninsula). This lake has a glacier origin and has been formed due to the ...

[Abstract] A paleobocanic scudy ofcwo Galician sierras, Coure! siecra and Queixa-Invernadoiro sierra is presenced here. A palynological scudy ofche Laguna Lucenza was carried ouC in che Coure! sierra. Eighc radiocarbon ...

[Abstract] The Andringirra Massif is a srratoide granite on the south of the Isle of Madagascar. Is a residual reliefwhich represents one ofthe last remnants of the Gondwana surface at the island egraded after the break ...