Ordovician deposits from the Central Andean Basin cover a vast region with thick exposed sequences in several areas, including the Sierras Subandinas, Cordillera Oriental and Puna geological provinces of northwestern Argentina. This basin was situated along the active margin of a Paleozoic foreland basin in western Gondwana. Continuous sedimentation occurred in different paleoenvironments from east to west: marginal marine settings with estuarine and deltaic deposits (Sierras Subandinas), shallow marine shelf environments with large clastic deposits in the central part (Cordillera Oriental–eastern Puna), and deep marine deposits with volcaniclastic supplies (western Puna). Limited biostratigraphic and chronostratigraphic data from these seq...
Although acritarchs have been studied mostly for stratigraphic purposes (often in sediments devoid o...
Diverse and moderately to well-preserved palynomorph assemblages, composed of 81 organic-walled phyt...
Conodonts recovered from the Devendeus Formation at the Angosto de La Quesera locality (Cordillera O...
Biostratigraphic data from the Precordillera Basin have traditionally been analyzed to contribute to...
International audienceLate Ordovician-early Silurian chitinozoans from the Upper Member of the Salar...
Middle Ordovician acritarchs, including enigmatic, spore-like microfossils, are recorded from the La...
Ordovician clastic sediments of the Central Andean Basin, northwestern Argentina, were deposited in ...
The Hirnantian “glacial horizon” has been recognized across the Central Andean Basin (Puna, Cordille...
Outcrops on the western slope of the La Invernada Range, San Juan Precordillera (W Argentina), were ...
Conodonts recovered from the Devendeus Formation at the Angosto de La Quesera locality (Cordillera O...
New late Tremadocian (Early Ordovician) conodont and graptolite faunas from the eastern and central ...
The Tremadocian graptolite and conodont faunas of the Gondwana Margin recorded at the Eastern Cordil...
New graptolite-trilobite records provide relevant information for the biostratigraphic framework of ...
Trichograptus dilaceratus (Herrmann), Acrograptus gracilis (Törnquist), Expansograptus urbanus (Mons...
his contribution provides new paleontological and stratigraphic data for the Eastern Precordillera (...
Although acritarchs have been studied mostly for stratigraphic purposes (often in sediments devoid o...
Diverse and moderately to well-preserved palynomorph assemblages, composed of 81 organic-walled phyt...
Conodonts recovered from the Devendeus Formation at the Angosto de La Quesera locality (Cordillera O...
Biostratigraphic data from the Precordillera Basin have traditionally been analyzed to contribute to...
International audienceLate Ordovician-early Silurian chitinozoans from the Upper Member of the Salar...
Middle Ordovician acritarchs, including enigmatic, spore-like microfossils, are recorded from the La...
Ordovician clastic sediments of the Central Andean Basin, northwestern Argentina, were deposited in ...
The Hirnantian “glacial horizon” has been recognized across the Central Andean Basin (Puna, Cordille...
Outcrops on the western slope of the La Invernada Range, San Juan Precordillera (W Argentina), were ...
Conodonts recovered from the Devendeus Formation at the Angosto de La Quesera locality (Cordillera O...
New late Tremadocian (Early Ordovician) conodont and graptolite faunas from the eastern and central ...
The Tremadocian graptolite and conodont faunas of the Gondwana Margin recorded at the Eastern Cordil...
New graptolite-trilobite records provide relevant information for the biostratigraphic framework of ...
Trichograptus dilaceratus (Herrmann), Acrograptus gracilis (Törnquist), Expansograptus urbanus (Mons...
his contribution provides new paleontological and stratigraphic data for the Eastern Precordillera (...
Although acritarchs have been studied mostly for stratigraphic purposes (often in sediments devoid o...
Diverse and moderately to well-preserved palynomorph assemblages, composed of 81 organic-walled phyt...
Conodonts recovered from the Devendeus Formation at the Angosto de La Quesera locality (Cordillera O...