In this paper a fossiliferous assemblage coming from Puerto Villamil (Isabela, Galápagos) is examined. The sandy sediments chiefly contain a molluscan association besides arthropod pincers, spicules of siliceous sponges, sea urchin spines, barnacle plates, rare foraminifers and abraded fragments of corals and briozoa. The mollusk assemblage represents a subtidal community associated with coral reefs and is dominated by Panamic forms. The modern aspect of this fauna and the radiometric ages till now proposed suggest a Pleistocene age for the Villamil deposits, although the presence of the extinct species Pegophysema spherica, for the first time reported from Isabela, might indicate a Pliocene age
Crassostrea specimens recognized in the Pleistocene sediments of Ecuador represent the first fossil ...
A succession of 150 m thick sediments, belonging to the Canoa Formation, was studied. Some specifica...
Tbis paper describes tbe fossils, materials and paleoenviromnental conditions found in some outcrops...
Studies carried on in the last several years allow us to date the Canoa Formation as Late Pliocene. ...
Studies carried on in the last several years allow us to date the Canoa Formation as Late Pliocene. ...
The early Pliocene sediments of the Súa Member (Onzole Formation) are spectacularly exposed along co...
Early Pleistocene strata are well exposed along the uplifted eastern margin of the Esmeraldas–Caraqu...
Early Pleistocene strata are well exposed along the uplifted eastern margin of the Esmeraldas-Caraqu...
Here is reported fauna from a Middle Miocene limestone deposit of the Cojímar Formation near the tow...
During the Quaternary the southern tip of South America was affected by several glaciations which mi...
Transgressive shallow-marine strata of the Súa Member are well exposed along the sea-cliffs of Súa (...
A new fossiliferous site is described south of Manta on the north coast of Ecuador. Estuarine sedime...
A new fossiliferous site is described south of Manta on the north coast of Ecuador. Estuarine sedime...
The exceptional assemblage of cirripedes from the Late Pliocene-Pleistocene sediments of Canoa and T...
Excluding the families Bulimulidae and Succineidae, 27 species of land shells were identified in the...
Crassostrea specimens recognized in the Pleistocene sediments of Ecuador represent the first fossil ...
A succession of 150 m thick sediments, belonging to the Canoa Formation, was studied. Some specifica...
Tbis paper describes tbe fossils, materials and paleoenviromnental conditions found in some outcrops...
Studies carried on in the last several years allow us to date the Canoa Formation as Late Pliocene. ...
Studies carried on in the last several years allow us to date the Canoa Formation as Late Pliocene. ...
The early Pliocene sediments of the Súa Member (Onzole Formation) are spectacularly exposed along co...
Early Pleistocene strata are well exposed along the uplifted eastern margin of the Esmeraldas–Caraqu...
Early Pleistocene strata are well exposed along the uplifted eastern margin of the Esmeraldas-Caraqu...
Here is reported fauna from a Middle Miocene limestone deposit of the Cojímar Formation near the tow...
During the Quaternary the southern tip of South America was affected by several glaciations which mi...
Transgressive shallow-marine strata of the Súa Member are well exposed along the sea-cliffs of Súa (...
A new fossiliferous site is described south of Manta on the north coast of Ecuador. Estuarine sedime...
A new fossiliferous site is described south of Manta on the north coast of Ecuador. Estuarine sedime...
The exceptional assemblage of cirripedes from the Late Pliocene-Pleistocene sediments of Canoa and T...
Excluding the families Bulimulidae and Succineidae, 27 species of land shells were identified in the...
Crassostrea specimens recognized in the Pleistocene sediments of Ecuador represent the first fossil ...
A succession of 150 m thick sediments, belonging to the Canoa Formation, was studied. Some specifica...
Tbis paper describes tbe fossils, materials and paleoenviromnental conditions found in some outcrops...