Browsing REV - CLXL - Vol. 22 (1997) by Author "Vidal Romaní, Juan Ramón"
Now showing items 1-7 of 7
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Análisis tafonómico de la muestra ósea de Liñares sur (Lugo, Galicia)
López González, F.; Grandal-d'Anglade, Aurora; Vidal Romaní, Juan Ramón (Universidade da Coruña, 1997)[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 ... -
Condicionantes en la distribución de macromamíferos en Galicia (NW Península Ibérica) durante el Cuaternario superior
Grandal-d'Anglade, Aurora; López González, F.; Vidal Romaní, Juan Ramón (Universidade da Coruña, 1997)[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 ... -
Contribución al conocimiento de la vegetación holocena en el NO de la Península Ibérica (Galicia, España)
Santos-Fidalgo, Luisa; Vidal Romaní, Juan Ramón; Jalut, G. (Universidade da Coruña, 1997)[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 ... -
Evolución neógena de la cuenca baja del Tambre
Pagés Valcarlos, J. L.; Vidal Romaní, Juan Ramón (Universidade da Coruña, 1997)[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 ... -
Evolución postglaciar de la laguna de Villaseca (NW de la Península Ibérica) a partir del análisis de diatomeas
Leira, Manel; Bao, Roberto; Vidal Romaní, Juan Ramón (Universidade da Coruña, 1997)[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 ... -
La extremidad occidental de la superficie fundamental de Galicia: La Meseta de Santa Comba
Pagés Valcarlos, J. L.; Vidal Romaní, Juan Ramón (Universidade da Coruña, 1997)[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. ... -
Géomorphologue granitique du Massif de l'Andringitra: Sa relation avec l'évolution de l'Île pendant le Cénozoïque
Vidal Romaní, Juan Ramón; Ramanohison, H.; Rabenandrasana, S. (Universidade da Coruña, 1997)[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 ...
