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Alejandro Kramarz,Eduardo Bellosi,Mariano Bond,Analía M. Forasiepi,Juan Carlos Fernicola,Guillermo Aguirrezabala,Daniella Teixeira de Rezende
Pág. 238 - 272
The Paleogene terrestrial faunal succession and its associated bearing volcaniclastic deposits has been exhaustively studied in central Patagonia, but there is still no acceptable litho-bio-chronostratigraphic ordering for the extra-Andean North Patagoni...
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José G Vargas-Hernández,Jovanna Nathalie Cervantes-Guzmán,Elba Lizbeth García Guerra
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Carolina Náñez,Norberto Malumián
Pág. 183 - 210
At the Bajada del Jagüel and Opaso sections (Añelo low, Neuquén basin), the Maastrichtian to Danian mudstones of the Jagüel Formation, are overlain by a succession of ostreid coquinas, sandstones, and mudstones. This succession has been usually referred ...
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José Luis Espinoza Bolaños, Henry Hernández Vega, Diana Jiménez Bolaños
Pág. 1 - 27
Se presenta un estudio de movilidad ciclista en distritos del cantón de Puntarenas con mayor cantidad de ciclistas involucrados en colisiones (Barranca, El Roble, Chacarita y Puntarenas). Se logró caracterizar la población ciclista dentro del área de est...
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Eduardo S. Bellosi,J. Marcelo Krause
Pág. 29 - 48
Climate-driven changes in terrestrial environments and biomes after the Early Eocene Climatic Optimum are poorly documented from southern continents. Particularly, Middle Eocene-Early Oligocene leaf and pollen data from Central Patagonia (46oS, Argentina...
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María Teresa Dozo,Martín Ciancio,Pablo José Bouza,Gastón Martínez
Pág. 224 - 247
The continental fossil mammals found in Barrancas Blancas, (near Camarones, Southeast of Chubut Province, Argentina) constitute a new faunal association from the Paleogene of Patagonia. From the base to the top, the outcrop in this locality is composed o...
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R. Alessandro, A. Gallo, M. Barranca, S. Principe, S. Taverna, G. Duro, G. Cassata, M. Becchi, S. Fontana, and G. De Leo
Pág. 1773 - 1778
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